Description of a partial Dromiceiomimus (Dinosauria: genus · 2019-02-07 · Draft 1 1 Description...

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Draft Description of a partial Dromiceiomimus (Dinosauria: Theropoda) skeleton with comments on the validity of the genus Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2018-0162.R1 Manuscript Type: Article Date Submitted by the Author: 05-Oct-2018 Complete List of Authors: Macdonald, Ian; Royal Tyrrell Museum Currie, Philip J.; University of Alberta, Biological Sciences Keyword: Dromiceiomimus, allometry, ornithomimid, systematics, Ornithomimus Is the invited manuscript for consideration in a Special Issue? : Not applicable (regular submission) https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences

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Description of a partial Dromiceiomimus (Dinosauria: Theropoda) skeleton with comments on the validity of the

genus

Journal: Canadian Journal of Earth Sciences

Manuscript ID cjes-2018-0162.R1

Manuscript Type: Article

Date Submitted by the Author: 05-Oct-2018

Complete List of Authors: Macdonald, Ian; Royal Tyrrell MuseumCurrie, Philip J.; University of Alberta, Biological Sciences

Keyword: Dromiceiomimus, allometry, ornithomimid, systematics, Ornithomimus

Is the invited manuscript for consideration in a Special

Issue? :Not applicable (regular submission)

https://mc06.manuscriptcentral.com/cjes-pubs

Canadian Journal of Earth Sciences

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1 Description of a partial Dromiceiomimus (Dinosauria:

2 Theropoda) skeleton with comments on the validity of the genus

3 Authors: Ian Macdonalda and Philip J. Currieb

4

5 a* Department of Biological Sciences, University of Alberta, Edmonton, Alberta, T5N 2E9,

6 Canada; [email protected]

7 b Department of Biological Sciences, University of Alberta, Edmonton, Alberta, T5N 2E9,

8 Canada; [email protected]

9

10 Corresponding author: Ian Macdonald (e-mail: [email protected]; phone: 647-221-8626;

11 address: 674-6 Ave E, Drumheller, Alberta T0J 0Y5)

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13 * currently affiliated with the department of Preservation and Research, Royal Tyrrell Museum

14 of Palaeontology, Drumheller, Alberta, T0J 0Y0

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20 Description of a partial Dromiceiomimus (Dinosauria: Theropoda) skeleton with comments on

21 the validity of the genus

22 Authors: Ian Macdonald and Philip J. Currie

23 ABSTRACT

24 Dromiceiomimus brevitertius is a North American ornithomimid diagnosed primarily by

25 the ratio of tibia length to femur length. It has recently, and perhaps incorrectly, been considered

26 synonymous with Ornithomimus edmontonicus, with several authors questioning the utility of

27 limb ratios in diagnosing taxa. While isolated ornithomimosaur material is common, specimens

28 with sufficient diagnostic material to explore the question of synonymy are comparatively rare.

29 The putative Dromiceiomimus specimen UALVP 16182 represents one of the few specimens in

30 which diagnostic elements are available. It is therefore an important specimen for assessing the

31 validity of Dromiceiomimus and for examining the utility of using limb proportions to diagnose

32 ornithomimid taxa. In this paper, UALVP 16182 is described, the tibia/femur ratio is examined

33 in closely-related ornithomimid taxa, and the ratio is found to distinguish Dromiceiomimus from

34 Gallimimus, Ornithomimus, and Struthiomimus. A phylogenetic analysis recovered Anserimimus

35 and Ornithomimus as sister taxa with Dromiceiomimus as an outgroup. Comparison of the manus

36 revealed differences in the morphology of metacarpal I and the flexor tubercle of manual ungual

37 II-3. Differences also appear in the surangular and scapula. An examination of stratigraphic

38 positions of various specimens indicates that Dromiceiomimus is generally higher in section than

39 Ornithomimus, although there are too few specimens to be statistically significant. This study

40 agrees with other studies in concluding that limb proportions are roughly isometric in small

41 theropods like ornithomimids and that the tibia/femur ratio may therefore be useful for

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42 diagnosing certain small taxa. These findings suggest that Dromiceiomimus may indeed be a

43 valid taxon.

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45 Key words: Dromiceiomimus, ornithomimid, systematics, allometry

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65 INTRODUCTION

66 Ornithomimosauria is a group of lightly built, cursorial theropods found mainly in the

67 Cretaceous of Asia and North America (Makovicky et al. 2004). They resemble modern ratites

68 like ostriches in their long necks, their small, edentulous skulls (except in basal forms), and their

69 hind limb proportions. The family Ornithomimidae (Marsh, 1890) contains the five Late

70 Cretaceous North American genera Dromiceiomimus (Russell, 1972), Ornithomimus (Marsh,

71 1890), Rativates evadens (McFeeters et al. 2016), Struthiomimus (Osborn, 1917), and

72 Tototlmimus packardensis (Serrano-Brañas et al. 2015). Asian Late Cretaceous ornithomimids

73 include Anserimimus (Barsbold, 1988), Aepyornithomimus (Tsogtbaatar et al. 2017a),

74 Archaeornithomimus (Russell, 1972), Gallimimus (Osmólska et al. 1972), Sinornithomimus

75 (Kobayashi and Lü, 2003), and Qiupalong (Xu et al. 2011). Although Qiupalong, Rativates, and

76 Tototlmimus occur in North America (McFeeters et al. 2017), they are not directly comparable

77 with Dromiceiomimus in the context of this study because of limited, non-overlapping fossil

78 material. The type species of Dromiceiomimus – Dromiceiomimus brevitertius – has recently

79 been considered a synonym of Ornithomimus edmontonicus (e.g. Makovicky et al. 2004; Xu et

80 al. 2011; Cullen et al. 2013), while others retain it as a distinct genus (Russell, 1972; Nicholls

81 and Russell, 1981; Watanabe et al. 2015; van der Reest and Currie, 2017). Despite these different

82 conclusions, Dromiceiomimus brevitertius will be referred to as such for the sake of clarity. In

83 this study, Ornithomimus is defined as O. edmontonicus and O. velox, plus all descendants of

84 their most recent common ancestor.

85 Russell (1972) diagnosed Dromiceiomimus brevitertius primarily on the basis of it having

86 different limb proportions than those of Ornithomimus and Struthiomimus. However, there is

87 disagreement regarding the use of limb proportions for distinguishing ornithomimid taxa.

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88 Nicholls and Russell (1981), despite tentatively affirming Dromiceiomimus as a valid genus,

89 suggest that limb proportions should be avoided as a diagnostic tool when few specimens are

90 available. They do, however, state cautiously that the ratio between the tibia and femur should be

91 regarded as reasonably diagnostic, as does Osmólska et al. (1972). Both Osmólska et al. (1972)

92 and Russell (1972) found that limb proportions among ornithomimids are roughly isometric

93 during ontogeny, although the latter did not employ any criteria besides absolute size to classify

94 ontogenetic stage. However, isometry does seem reasonable in ornithomimids because there is

95 not so great a disparity between the smallest and largest known specimens for most species;

96 proportions do not have to change as much during growth to accommodate an increase in mass.

97 It is reasonable to propose then that the limb proportions of smaller theropods like ornithomimids

98 can be used to distinguish taxa, particularly if those proportions are linked to other skeletal

99 features. UALVP 16182 is one of a limited number of ornithomimid specimens that has the

100 requisite elements for a proportion-based taxon diagnosis and is therefore a useful specimen for

101 testing both the validity of Dromiceiomimus and the utility of limb proportions in diagnosing

102 taxa.

103 UALVP 16182 is an important ornithomimid specimen in that it has both the femur and

104 tibia preserved, a surprisingly rare condition given the abundance of ornithomimid material in

105 the Upper Cretaceous sediments of southern Alberta. Additionally, it is the only

106 Dromiceiomimus brevitertius skeleton for which a manus is preserved. The present study will

107 focus on describing the specimen, which is currently identified on the basis of the tibia/femur

108 ratio as Dromiceiomimus brevitertius, discussing the effectiveness of using that ratio for

109 diagnostic purposes, and commenting on the validity of Dromiceiomimus as a genus.

110

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111 MATERIALS AND METHODS

112 UALVP 16182 is a partial skeleton collected in 1967 by Dr. Richard Fox from what is

113 now known as TMP locality #L2205 (UTM 12U: 366769E; 5757459N (WGS 84)) in the Tolman

114 Member of the Horseshoe Canyon Formation in Dry Island Buffalo Jump Provincial Park east of

115 Huxley, Alberta, Canada (Fig. 1). It was discovered 768 m above sea level, with the tail

116 emerging from the outcrop approximately halfway between prairie level and river level, although

117 laterally removed from either by approximately 500 m (Tanke and Walker, 2011). Besides its

118 palaeontological value, UALVP 16182 is historically noteworthy for being the first dinosaur

119 specimen ever extracted from a field site using a helicopter (Tanke and Walker, 2011). The

120 specimen includes the right nasal, left jugal, right postorbital, posterior halves of the left and

121 right dentaries, left splenial, right surangular, right prearticular, partial hyoid, eight

122 articulated/associated cervical vertebrae, nine articulated dorsal vertebrae, eight articulated

123 proximal caudal vertebrae, ribs, haemal arches, left scapula, ulna, right metacarpal I, left

124 metacarpal II, right metacarpal III, right manual phalanges I-1, II-2 (pathological), II-3, III-3, left

125 manual phalanx II-2, an articulated pelvic girdle, left femur, both tibiae, both fibulae, both

126 astragali, left calcaneum, the left metatarsus, pedal phalanges II-1, II-3, III-2, III-3, III-4, and IV-

127 2.

128 Measurements of UALVP 16182 were taken twice and averaged (Table 1), whereas those

129 of other specimens were taken from various sources (Table 2). The statistical analyses performed

130 were intended to investigate the null hypothesis that there is no significant difference between

131 limb proportions of specimens that have been referred to either Dromiceiomimus or

132 Ornithomimus. In so doing, this study attempts to replicate previous studies that detected a

133 statistical difference in these proportions. If the null hypothesis can be rejected and the issue of

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134 allometry addressed, then it may be reasonable to interpret the ratios as representative of distinct

135 taxa, particularly if these proportions co-occur with other anatomical features. The measurements

136 and proportions were analyzed using a one-tailed t-test with unequal variance to determine

137 whether the limb proportions of Dromiceiomimus, Gallimimus, Ornithomimus and

138 Struthiomimus are significantly different. Although the use of a t-test could be problematic if the

139 elements being compared exhibit allometric growth through ontogeny, an allometric analysis in

140 this study indicates that the limb proportions of the ornithomimid taxa examined were roughly

141 isometric (Table 3). Thus the use of the t-test is justifiable in this case. Allometry of

142 ornithomimid tibia/femur ratios was assessed using output from RMA 1.21 (Bohonak and van

143 der Linde, 2004). The allometric exponents (equivalent to the slopes of the regression lines) were

144 calculated for each of the four ornithomimids in this study and were used in combination with

145 the 95% confidence intervals (CI) to determine whether the ratios exhibited isometry, positive

146 allometry, or negative allometry. The ratios were considered positively allometric if the 95% CI

147 of the slope was greater than 1.0, negatively allometric if the 95% CI of the slope was less than

148 1.0, and isometric if the 95% CI of the slope included 1.0 (Brown and Vavrek, 2015).

149 Because the sample size for possible Dromiceiomimus specimens is small and displays

150 relatively little size variation (12%), it was necessary to assess whether such a sample could be

151 considered representative of a larger, more varied sample. To this end, an ANCOVA test was run

152 using XLStat to compare the regression lines of a highly variable (approximately 71%)

153 Gallimimus sample and a less varied (11.7%) Gallimimus sub-sample comprised of the

154 specimens MPC-D100/14, MPC-D100/52, and MPC-D Field # 950818. It was assumed that if

155 the slopes and y-intercepts were not statistically different then the sub-sample could be regarded

156 as reasonably representative of the full sample. If this was found to be the case, then the limited

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157 Dromiceiomimus sample, and the allometric analysis thereof, could potentially be considered

158 roughly representative of a more variable sample like that of Gallimimus.

159 Measurements taken from the hind limbs (femur, tibia, and metatarsus) were necessary

160 to explore the validity of Dromiceiomimus and the usefulness of limb proportions in diagnosing a

161 taxon. Measurements were log10 transformed before being used in analyses to account for

162 differences in size. The tibia to femur ratios were calculated for four genera (Table 2). One-tailed

163 t-tests with unequal variances were carried out on the tibia/femur ratios of Dromiceiomimus and

164 Gallimimus (D-G), Dromiceiomimus and Ornithomimus (D-O), Dromiceiomimus and

165 Struthiomimus (D-S), Gallimimus and Ornithomimus (G-O) and Ornithomimus and

166 Struthiomimus (O-S).

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168 A phylogenetic test was also conducted with Tree Analysis Using New Technology

169 (TNT; Goloboff et al. 2008) to assess the relationship between Dromiceiomimus and

170 Ornithomimus. The analysis included 285 characters (Appendices 1 and 2). Ten

171 ornithomimosaurian taxa and specimens, one of which was UALVP 16182, were included in the

172 ingroup whereas Allosaurus, Dilophosaurus, Ornitholestes and Tyrannosaurus were used as

173 outgroups for a total of fourteen taxa. The characters used had equal weight and were unordered.

174 A heuristic search with 10,000 replicates was carried out to identify the shortest tree. Bootstrap

175 and Bremer tests were also carried out to assess the degree to which the topology of the resulting

176 tree was supported.

177

178 DESCRIPTION

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179 Several of the skull elements are preserved tightly appressed to the vertebral column in

180 such a way as to prevent their removal. Therefore, the descriptions and figures of these elements

181 are necessarily limited to what is visible.

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183 Nasal

184 The preserved section of the right nasal is narrow, with a transverse width of 9.25 mm

185 and margins that are roughly parallel. The anteroposterior length is unknown due to the

186 incompleteness of the element, only 45 mm of which are preserved. The contact for the other

187 nasal is a straight edge with a shallow groove 21 mm from the posterior border of the narial

188 opening. The contact for the premaxilla is a shallow groove that deepens as it approaches the

189 narial opening and accounts for approximately 1/3 of the transverse width of the nasal in dorsal

190 view.

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192 Jugal

193 The left jugal (Fig. 2) is roughly sigmoidal in lateral view. Its preserved length measured

194 as a straight line between the contact for the lacrimal and the tip of the dorsal process, is 78.9

195 mm. The anterior end is compressed dorsoventrally and concave in dorsal view with a deep pit

196 4.8 mm in diameter at the posterior edge of the concavity. The element bifurcates anteriorly for

197 contacts with the lacrimal and maxilla. The middle suborbital region is shallowly concave on the

198 dorsal margin before becoming laterally compressed and dorsoventrally expanded posteriorly.

199 Posteriorly, the jugal bifurcates into the dorsal and posterior processes for contact with the

200 postorbital and quadratojugal respectively. The contact for the quadratojugal is a groove on the

201 lateral surface of the posterior process.

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203 Postorbital

204 The height of the right postorbital is 45.6 mm, measured as a straight line from the tip of

205 the ventral process to the midpoint of the dorsal margin of the bone. The dorsal portion expands

206 anteroposteriorly until it is triangular. The anterior process is either absent or not preserved,

207 although the edge seems to be intact. The orbital margin forms a smooth C shape whereas the

208 infratemporal margin is sigmoidal due to the projection of the posterior process and the sharp,

209 anterior deflection of the ventral process. The contact for the jugal on the ventral process begins

210 34 mm from the dorsal edge of the postorbital.

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212 Mandible

213 The left dentary (Fig. 2C) was found next to the dorsal vertebrae. It is complete except

214 for the posteroventral tip, and as preserved is 137 mm long. The minimum height, at

215 approximately one third of the length from the front, is 13.7 mm, and the maximum height is

216 20.5 mm near the posterior end. The distance from the buccal edge ventromedially to the back of

217 the symphysis is 20 mm in height. In lateral view, the upper margin is shallowly convex and the

218 lower edge is shallowly concave behind the symphysis, and like other ornithomimids the front of

219 the lower jaw curves anteroventrally. In dorsal view, the dentary curves slightly anterolaterally in

220 the symphysial region so that it has the ‘shovel-like’ appearance described by Osmólska et al.

221 (1972). The symphysis extends well below the lower margin of the dentary to form a

222 conspicuous chin. On the lateral surface of the dentary, there is a row of a dozen foramina below

223 the buccal margin, each of which penetrates the bone and is exposed on both labial and lingual

224 surfaces. The anterior eight foramina are closely associated, and are separated by as little as 2

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225 mm. However, the more posterior ones spread out, and the last two are separated by almost 9

226 mm. The line of foramina is close to the buccal edge anteriorly (about 1.5 mm), but shifts

227 ventrally until the last foramen is 4 mm from the margin. A short (5 mm) canal enters the last

228 foramen from behind. There is a shallow longitudinal trough on the lateral surface of the

229 posterodorsal region of the dentary for the anterior process of the surangular. The latter

230 overlapped the dentary for at least 27 mm, which is much more extensive than the equivalent

231 contact in Gallimimus (Hurum 2001). Another depression along the dorsal margin of the dentary

232 extends almost as far forward and was presumably for the medial intramandibular process of the

233 surangular. The posteroventrally sloping symphysis is 32.5 mm long, but the intramandibular

234 articular surface is only 4.5 mm deep. On the lingual surface, the symphysial articular surface

235 divides posteriorly to outline the tapering anterior limit of the Meckelian groove. The edge of the

236 jaw is sharp, and is delineated ventrally on the medial surface by the remnants of the alveolar

237 shelf. Above the symphysis, the distance between the jaw margin and the shelf is 6.7 mm, but at

238 the back of the dentary the shelf is only 2 mm below the edge of the jaw. A shallow longitudinal

239 trough extends along the dorsal surface of the shelf from the symphysis to the back of the

240 dentary. Ventrally, the shelf overhangs the deep Meckelian canal.

241 The right surangular (Fig. 3A) was recovered in the chest region of the skeleton close to

242 the dentary. The preserved portion is 119 mm long and gently curved. As in other

243 ornithomimids, the dorsal margin is shallowly convex in lateral view. The thin ventral margin

244 has been somewhat damaged above the lateral mandibular fenestra and is difficult to interpret.

245 The anterior margin of the articulation for the accessory condyle of the quadrate is mediolaterally

246 thick (7 mm), sharply defined and vertical. It is about 20 mm anterior to the back of the

247 retroarticular process. The lateral surface of the surangular has a shallow depression on the

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248 posterior third of the bone that extends to the end of the retroarticular process. This marks the

249 contact for the overlapping suture for the posterior extension of the angular. A lateral ridge

250 extends anteroventrally from the top of the glenoid articulation and forms the lateral margin of a

251 depressed area for the adductor musculature (M. adductor mandibulae externus). The posterior

252 surangular foramen is about 3 mm long and sits beneath this ridge. This foramen is supposedly

253 absent in Garudimimus (Kobayashi and Barsbold, 2005a), Harpymimus (Kobayashi and

254 Barsbold, 2005b), Ornithomimus and Sinornithomimus (Kobayashi and Lü, 2003) but is present

255 in Gallimimus and Struthiomimus. The anterior surangular foramen is separated from the

256 posterior surangular foramen by a distance of 34 mm. It opens anteriorly into an elongate,

257 conspicuous groove that extends to the anterior margin of the surangular. The articular was not

258 fused with the surangular.

259 The prearticular is gently arcuate, with a length of 82.4 mm measured as a straight line

260 from the anteroventral tip to the dorsal tip of the posterior end. The middle portion is constricted

261 with the anterior and posterior regions expanding dorsoventrally.

262 A partial hyoid (Fig. 4) was found associated with the left dentary. The posterior end is

263 missing, and the preserved part of the bone is more than 120 mm long. The diameter of the

264 tapering anterior end is 2.6 mm, whereas the diameter is greatest (5 mm) at the posterior end of

265 the preserved section. The anterior end has an oval cross-section, whereas the posterior end of

266 the preserved section is round in section.

267

268 Vertebrae

269 The cervical vertebrae (Fig. 5A, Fig. 6) are shorter dorsoventrally relative to their central

270 lengths than either the dorsals or the caudals. This ratio increases in the more posterior cervicals

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271 until it is similar to the dorsal vertebrae. The centra of the anterior cervicals are long and thin

272 relative to their heights, and the anterior ends flare ventrolaterally to contact the cervical ribs.

273 The transverse processes are short mediolaterally, comparatively wide anteroposteriorly and the

274 distal ends are subrectangular. They have pneumatopores at the bases of the diapophyses, but

275 these are smaller than those of the dorsals and are divided by ridges descending from the distal

276 ends of the transverse processes. In each, one of these ridges extends posteriorly until it forms

277 the ventral margin of the postzygapophysis. The pneumatopore dorsal to the transverse process is

278 simply sunk into the surface rather than being bound by laminae. The transverse processes are

279 confluent with the prezygapophyses. The latter extend more anteriorly from the centrum than in

280 the dorsals, and their articular surfaces are oriented dorsomedially. The postzygapophyses are

281 comparatively short, just barely extending past the centrum, and their articular surfaces face

282 ventrally. In dorsal view, the ridges of the zygapophyses of each cervical form a tall, thin X with

283 the short, subrectangular neural spine in the center. In a representative cervical, the

284 anteroposterior lengths of the neural arch and neural spine are 65.22 mm and 21.98 mm

285 respectively. The more posterior cervicals resemble the dorsals in their proportions and

286 morphology.

287 The dorsal vertebrae (Fig. 5B, Fig. 7) are taller relative to their central lengths compared

288 to the caudals. The anterior dorsals have on both the left and right sides three deep

289 pneumatopores at the bases of short, distally broad, laterally-directed transverse processes. For

290 two anterior dorsals, the average length of the transverse processes was 49.5% of centrum length

291 and the average width of the transverse process was 47.56% of centrum length. The

292 pneumatopores are divided from one another by distinct laminae that converge into the distal end

293 of the transverse process. The neural spines are short, subrectangular, and point dorsally. The

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294 prezygapophyses are short, confluent with the anterior margin of the neural spine and enclose a

295 groove between them that is relatively much deeper than the same features on the caudals. The

296 articular surfaces of the prezygapophyses are oriented dorsally. The postzygapophyses are

297 anteroposteriorly longer than those of the cervicals. They are confluent with the posterior margin

298 of the neural spine and neural arch, and are continuous with the triangular blade that extends

299 posterodorsally. Their articular surfaces are oriented ventrally.

300 The anterior caudal vertebrae (Figs. 5C, D; Fig. 8A, B) lack any visible pneumatization.

301 The nine most anterior caudals have central lengths at least twice as long as their posterior

302 widths, which is consistent with the diagnosis of Dromiceiomimus given by Russell (1972). The

303 transverse processes are directed posterolaterally and broaden at their distal ends. The transverse

304 processes become shorter posteriorly along the tail, with those on the first six caudals being the

305 longest. The neural spines are directed dorsally and are subrectangular with posterior extensions

306 of the distal edges at the top. The prezygapophyses are small, extending approximately 10 mm

307 anterior to the centra, and are confluent with the short neural arches in lateral view. Their

308 articular surfaces face mediodorsally. The postzygapophyses are similarly short and their

309 articular surfaces face lateroventrally. The postzygapophyses are confluent with the

310 posterolateral margins of the neural spine, creating a deep groove between them.

311

312 Ribs

313 Ribs and gastralia (Fig. 9) were recovered with the specimen, but lack any apparent

314 diagnostic characters. About a dozen ribs were found with the specimen.

315

316 Scapula

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317 The scapula is mediolaterally thin and strap-like (Fig. 10). It is expanded where the

318 missing coracoid would articulate, and tapers dorsoposteriorly from that point before expanding

319 dorsoposteriorly again, beginning approximately mid-shaft. The lateral surface is convex. The

320 length measured as a straight line is 260 mm, but is 283 mm along the curved lateral surface. The

321 height of the shaft at its narrowest point is 28.3 mm. The scapular portion of the glenoid faces

322 ventrolaterally and the acromion process has a squared-off outline. In contrast with

323 Ornithomimus but similar to Struthiomimus, the supraglenoid buttress bears an obvious teardrop-

324 shaped depression that is visible in spite of the minor crushing undergone by that portion of the

325 scapula. This feature is poorly developed or absent in Ornithomimus.

326

327 Ulna

328 The right ulna (Fig. 11) is 280 mm long with a midshaft diameter of 9.7 mm (Table 1).

329 The cross section of the midshaft has the appearance of a rounded equilateral triangle. The

330 proximal half is approximately straight whereas the distal half curves increasingly medially

331 towards where the radius would articulate. Proximally, the dorsal edge curves gently up into the

332 olecranon process, which is triangular in lateral view. The ventral edge is roughly straight but

333 inflects dorsally somewhat into the olecranon process. There is a laterally-projecting ridge that

334 begins at the trochlear notch and blends into the rest of the shaft approximately 10 mm distally.

335 This creates a broad depression between this ridge and the olecranon process. The distal end is

336 somewhat dorsoventrally compressed, becoming an acute triangle in cross section with the base

337 of the triangle formed by the slight dorsoventral expansions on the lateral edge.

338

339 Manus

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340 The metacarpals (Fig. 12A) are gracile with length/width ratios of 12.6 for metacarpal I

341 and 14.2 for metacarpal III (Table 4). Metacarpal I is roughly triangular in cross section and is

342 dorsoventrally compressed. Its distal portion is inflected medially in dorsal view at an angle of

343 approximately 25o and twists so that the dorsal edge is inclined somewhat medially. Although

344 the right second metacarpal is not present, the straight shaft of the left second metacarpal

345 suggests that metacarpals I and II are closely appressed for most of their lengths, but diverge

346 distally beyond the inflection of the former. This contrasts with Ornithomimus in which the two

347 bones seem to be appressed for their entire lengths and is more similar to the condition seen in

348 Struthiomimus. Metacarpal I is 101.39 mm long, metacarpal II is 95.85 mm long, and metacarpal

349 III is 92.82 mm long. This condition (Mc I > Mc II > Mc III) is also seen in Ornithomimus. All

350 three metacarpals are strongly asymmetrical in distal view, with the lateral condyles being larger

351 than the medial condyles. The shaft of metacarpal III is circular in cross section.

352 The phalanges are generally similar to those of Ornithomimus. However, the ungual of

353 manual digit II is gently curved, noticeably more so than in ROM 851 (Ornithomimus), which is

354 nearly straight, although similar to TMP 1995.110.0001, another Ornithomimus (Fig. 13). The

355 flexor tubercle is weakly-developed and displaced distally from the articular end. It contrasts

356 with the flexor tubercle of the above-mentioned Ornithomimus specimens wherein this structure

357 is noticeably less prominent.

358 Right phalanx II-2 (Fig. 14) is pathological. The distal end, just proximal to the articular

359 surface, is noticeably inflated and there is a ventrally-projecting spur. There is a fracture

360 extending diagonally through the shaft and the distal portion appears to have been displaced

361 proximally. Despite this, the two portions remained attached although they have since been

362 detached and repositioned somewhat so that the long axes of the segments align, whereas the

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363 proximal segment was originally angled so that the tip was below the ventral surface of the distal

364 segment. The proximal segment has also been shifted proximally by 4.8 mm in relation to the

365 distal segment. The broken edges on both sides of the crack seem smooth which may indicate the

366 presence of a pseudarthrosis. Although it has since been prepared away, there was present what

367 appeared to be large bony callosity beginning approximately midshaft and ending just proximal

368 to the distal articular end. Regrettably, the only photographs that survive of this callosity are not

369 of the highest quality; however, bone texture is still apparent in the swollen area, supporting the

370 interpretation that it is a pathology rather than a concretion.

371

372 Ilium

373 The length of the ilium (Fig. 15A) is 412.5 mm. The length of the anterior portion of the

374 ilium, measured from the midpoint of the anterior edge of the iliac blade to a point directly dorsal

375 to the anterior margin of the acetabulum is 163 mm. The height measured from just anterior to

376 the acetabular margin to the dorsal edge of the iliac blade is 151.5 mm. The anterior end of the

377 ilium curves posteroventrally into a distinct hook-like process that ends just ventral to the dorsal

378 margin of the acetabulum. The supracetabular crest covers the acetabulum dorsally. The

379 postacetabular portion of the ilium is subrectangular in lateral aspect. In ventral view, the brevis

380 fossa is a deep excavation that accommodates the M. caudofemoralis brevis, and the brevis shelf

381 extends ventral to the supraacetabular region resulting in a large overhang, and rendering the

382 brevis fossa invisible in lateral aspect.

383

384 Pubis

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385 The length of the pubis (Fig. 15B) measured from the dorsal corner of the pubic portion

386 of the puboischial contact to the distal end of the shaft is 370 mm. The height of the shaft in

387 lateral aspect is uniform along its entire length, broadening proximally to 52.3 mm distal to the

388 puboischial contact and 52.3 mm distally before it expands into the pubic boot. The shaft is

389 straight until it curves anteriorly close to the pubic boot. Medially, the triangular pubic apron

390 emerges from the shaft 85 mm distal to the bottom of the puboischiadic suture. It expands

391 rapidly to meet its counterpart from the opposite pubis. The conjoined pubic apron extends at

392 least 195 mm distally, and ends just proximal to the pubic boot.

393

394 Ischium

395 The ischium extends posteroventrally and curves anteroventrally at its distal end (Fig.

396 15B). The length measured from the ischial portion of the puboischial contact is 314 mm. The

397 medial face of the ischial shaft extends into a triangular apron 74 mm distal to the ventral edge of

398 the puboischiadic suture. The apron formed by the two ischia extends to the rounded ischial boot.

399 In lateral aspect the shaft is 9.32 mm thick anteroposteriorly and broadens distally to a maximum

400 of 42.98 mm.

401

402 Femur

403 The total length of the femur is 319 mm. The femoral head is directed medially and has a

404 height of 43.5 mm. It is confluent with the greater trochanter, which is separated from the

405 anterior trochanter by a deep notch. On the medial edge of the anterior trochanter is a small,

406 bulbous accessory trochanter. The fourth trochanter is a distinct ridge on the posterior surface,

407 with a proximodistal length of 83.6 mm and a maximum posterior extension of 13.4 mm (Fig.

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408 16A). The medial side of the fourth trochanter is somewhat inflated. Medial from the distal end

409 of the fourth trochanter is a roughly tear-shaped depression 52.5 mm long proximodistally and

410 26.6 mm wide that appears to be a point of muscle attachment. At its widest, the femoral shaft

411 has a transverse diameter of 48.9 mm, but is 45.7 mm at its narrowest point. On the posterior

412 surface near the distal end of the femur is a roughened tuberosity on the midline of the bone, just

413 proximal to where the condyles are divided by the posterior intercondylar groove. The lateral

414 condyle is divided posteriorly by a shallow notch, resulting in a thinner fibular flange that is

415 medial to and extends posteriorly past the main portion of the condyle. A similar shallow notch

416 divides the medial condyle anteriorly into the main portion and a thin flange.

417

418 Tibia

419 The following measurements are for the well-preserved left tibia as the right tibia is

420 taphonomically distorted. The maximum length of the tibia (Fig. 16B), measured along the

421 medial side of the shaft, is 468 mm. The cnemial crest extends anteriorly but curves laterally and

422 has an anteroposterior length of 96.4 mm. The fibular crest is approximately a quarter of the way

423 down the shaft and extends laterally from the lateral edge of the anterior surface. The minimum

424 width of the shaft is 32.8 mm, expanding proximally and distally with a maximum proximal

425 width of 41.6 mm and a distal width of 75.2 mm. The lateral malleolus has a D-shaped

426 depression on the lateral side into which the distal end of the fibula fits. Both the astragali are

427 preserved in place and the left calcaneum is also preserved in life position. The left astragalus is

428 112.4 mm tall, measured as a straight line from the medial side of the base to a point in line with

429 the apex of the ascending process. The ascending process of the left astragalus covers at its base

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430 most of the anterior surface of the tibia, but tapers laterally until it covers only the lateral half of

431 the tibia shaft.

432

433 Fibula

434 The fibula (Fig. 17) is 441.5 mm long (Table 1). The proximal end is mediolaterally

435 compressed with a deep medial concavity and measures 67.5 mm anteroposteriorly. The shaft

436 tapers distally to approximately half that width where it contacts the fibular crest of the tibia and

437 then tapers further to a midshaft width of 11.8 mm before expanding slightly at the distal end.

438 The medial aspect of the shaft is concave proximally and distally, but flat through the middle

439 portion and at the distal end where it contacts the calcaneum.

440

441 Metatarsus

442 The metatarsus (Fig. 16C) is arctometatarsalian as is typical for ornithomimids.

443 Metatarsal III is pinched proximally in anterior view, although it is visible in anterior view for all

444 but the proximal 20 mm. The total length as measured along the anterior surface from the centre

445 of the proximal end to the distal end of metatarsal III is 342 mm. The minimum width across the

446 metatarsus is 46 mm. Metatarsal II is the shortest and in proximal view makes the biggest

447 contribution to the ankle articulation, followed by IV then III. The distal portions of metatarsals

448 II and IV curve medially and laterally, respectively. On the distal end of metatarsal II there is a

449 posterior, roughly circular depression. A similar but shallower and less defined depression is

450 found on metatarsal IV.

451

452 Pes

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453 All phalangial lengths are measured from the centre of the proximal articular surface to

454 the larger condyle of the distal end. Phalanx II-1 (Fig. 18A) is 77.1 mm long and tapers from a

455 proximal height of 38.7 mm to a distal height of 22.8 mm with a slight ventral constriction just

456 proximal to the distal articular surface. The ventral margin is a smooth arc. In proximal view, the

457 shallowly concave proximal articular surface is ovoid with the long axis oriented vertically.

458 There are two ventral processes, the medial being larger, which give the base of the proximal end

459 a bifurcated appearance. These processes create between them a deep sulcus on the ventral

460 surface of the phalanx. Phalanx III-2 (Fig. 18B) is 56.6 mm long and tapers from a proximal

461 height of 23.4 mm to a distal height of 18.3 mm with a strongly convex ventral cross-section of

462 the shaft. In proximal view, the concave proximal end is roughly hemispherical with a flat base.

463 Phalanx III-3 (Fig. 18C) is 44.4 mm long with a proximal height of 20.8 mm and a distal height

464 of 15.5 mm. In proximal view, the proximal articular end is concave and is shaped like an

465 asymmetrical hemisphere. The ventral surface of the proximal end is slightly concave. The

466 ventral margin is concave in lateral view from the midpoint of the shaft until it expands ventrally

467 into the distal articular surface. Phalanx IV-2 (Fig. 18D) is 29.4 mm long with a proximal height

468 of 26 mm and a distal height of 23.1 mm. In proximal view, the proximal articular surface is

469 roughly triangular in outline, and the surface is concave with a strong central, vertically-oriented

470 keel.

471 The unguals (Fig. 18E and F) are triangular in proximal view and have shallow flexor

472 depressions on the ventral surfaces. They possess pointed, laterally-oriented protrusions near the

473 proximal end where the keratin grooves terminate. The ventral margin in lateral view is concave

474 between these protrusions and the proximal end. The complete ungual is 48.7 mm long.

475

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476 RESULTS

477 Due to small sample sizes and the fragmentary nature of many of the specimens, it was

478 not possible to calculate all of the proportions Russell (1972) used to diagnose Dromiceiomimus.

479 Therefore the analysis focused primarily on the femur and tibia measurements, which is in any

480 case the ratio that Nicholls and Russell (1981) considered to be most diagnostic for

481 Dromiceiomimus. The assignment of UALVP 16182 to Dromiceiomimus is based primarily on

482 this ratio; the tibia/femur ratio of UALVP 16182 comports with the same ratio from other

483 specimens assigned to Dromiceiomimus, including the holotype ROM 797 (Table 2), more

484 strongly than with other ornithomimid taxa. Comparison of the tibia/femur ratios for the four

485 taxa using a one-tailed t-test with unequal variance (Table 5), revealed a statistically significant

486 difference between Dromiceiomimus and Gallimimus (P = 0.00016), Dromiceiomimus and

487 Ornithomimus (P = 0.00185), Dromiceiomimus and Struthiomimus (P = 0.00124), and

488 Gallimimus and Struthiomimus (P = 0.03083). Comparison of the ratio for Gallimimus and

489 Ornithomimus (P = 0.05191) fell just short of statistically significant difference and the

490 comparison between Ornithomimus and Struthiomimus revealed no significant difference (P =

491 0.19174). Thus the tibia/femur ratio allows one to delineate between ornithomimid taxa except

492 for Gallimimus and Ornithomimus (although the results are bordering on significance) and

493 Ornithomimus and Struthiomimus.

494 Contrary to Russell (1972), the metatarsal III-femur ratio (Table 6) does not seem to be

495 diagnostic. A one-tailed t-test with unequal variance performed on the ratio (Table 7) yielded

496 results that did not allow rejection of the null hypothesis except between Dromiceiomimus and

497 Gallimimus (D-G: P = 0.03334; D-O: P = 0.10605; D-S: P = 0.05994; G-O: P = 0.31636; G-S: P

498 = 0.37808; O-S: P = 0.29131). The two data points derived from Ornithomimus are similar to

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499 Struthiomimus. Other ratios were either unhelpful or lacked sufficient samples to obtain

500 statistically significant results.

501 A comparison (using an ANCOVA test) of regression lines between a Gallimimus sample

502 in which femur length was highly variable (71%) and a sub-sample in which femur length was

503 minimally variable (11.7%) revealed that neither the slopes (F = 0.62, P = 0.45688) nor the y-

504 intercepts (F = 1.16, P = 0.31287) were significantly different. Output from XLStat indicated

505 that the tibia/femur ratios for the ornithomimid specimens tested were isometric (Table 3), except

506 for Gallimimus which exhibited slight negative allometry. An RMA analysis of the small,

507 minimally variable sub-sample indicated isometry as well.

508 The phylogenetic analysis recovered a single most parsimonious tree with a length of

509 274, CI = 0.766, RI= 0.743 and RC = 0.569 (Fig. 19). Dromiceiomimus (represented by UALVP

510 16182) was recovered as an outgroup to a clade consisting of Anserimimus and Ornithomimus.

511 Bremer support for the ornithomimid clade is strong, but the internal groupings have weak

512 support.

513 DISCUSSION

514 Many ornithomimid taxa have been diagnosed using various differences in limb

515 proportions. Russell (1972) diagnosed Ornithomimus by the following length ratios: presacral

516 vertebral column/hindlimb, humerus/scapula, forearm/femur, tibia/femur, antilium/femur,

517 metatarsus/femur, metacarpal I/metacarpals II and III, manual ungual 3/penultimate phalanx of

518 digit 3. Claessens and Loewen (2015) also diagnosed Ornithomimus using the greater length of

519 metacarpal I compared to metacarpal II and the greater length of metacarpal II compared to

520 metacarpal III

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521 Russell (1972) diagnosed Dromiceiomimus by the following length ratios: presacral vertebral

522 column/hindlimb, humerus/scapula, forearm/femur, antilium/femur, tibia/femur, tibia with

523 astragalus/metatarsal III, metatarsus/femur, and pedal digit 3/femur.

524 Diagnosing taxa on the basis of limb proportions remains problematic because these

525 proportions can vary depending on sex, age, or individual variation (Currie, 2003). This

526 uncertainty can be mitigated when many specimens are available, but, unfortunately, this is not

527 the case with North American ornithomimids. Although many specimens exist, there are

528 comparatively few individuals in which all the elements needed to measure diagnostic

529 proportions have been preserved. In the present study, the only proportion that was measureable

530 in enough specimens to provide statistical significance was the tibia/femur ratio. Before

531 considering the results of comparisons between ornithomimid tibia/femur ratios, however, it was

532 necessary to establish whether or not the ratio was isometric over a range of sizes and whether

533 the Dromiceiomimus sample, despite its low size variability, could be considered roughly

534 representative of a more variable sample. Results from RMA 1.21 (Table 3) indicated that the

535 tibia/femur ratio is generally isometric for the ornithomimids examined, meaning that statistical

536 analysis of this ratio could yield useful results. Gallimimus, in contrast, exhibited very slight

537 negative allometry. This could perhaps be attributed to its larger body size. However, the

538 isometry indicated by an analysis of the smaller, less variable sub-sample implies that the

539 isometry seen in the other taxa is due to lower sample size, making it ‘soft’ isometry (Brown and

540 Vavrek, 2015). Additionally, Brown and Vavrek (2015) found that allometric analyses indicating

541 isometry were of dubious value when the sample size was small.

542 The ANCOVA test indicating a lack of significant difference between the slopes and

543 intercepts of the variable Gallimimus sample and the winnowed sub-sample indicated that the

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544 Dromiceiomimus sample, although limited in size variability, can nonetheless be regarded as

545 representative of a more variable sample. Thus analysis of the tibia/femur ratio, despite the

546 potentially confounding factors that have been discussed, is not without merit.

547 The tibia/femur ratio, while not highly diagnostic, does distinguish Dromiceiomimus

548 from Gallimimus, Ornithomimus, and Struthiomimus (Fig. 20). This is in agreement with

549 Nicholls and Russell (1981) who concluded that Dromiceiomimus could be diagnosed on this

550 basis despite also concluding that limb proportions were not generally reliable along with most

551 of the proportions used by Russell (1972). Osmólska et al. (1972) and Russell (1972) found that

552 limb proportions in ornithomimids did not vary significantly with age. These findings suggest

553 that the separate clustering of Dromiceiomimus and Ornithomimus edmontonicus on the basis of

554 the tibia/femur ratio is evidence for the validity of Dromiceiomimus, and the statistical analysis

555 supports this as well.

556 The differences seen between the tibia/femur ratios of the ornithomimids in this study

557 suggest, as others (Osmólska et al. 1972; Russell, 1972; Nicholls and Russell, 1981) have

558 proposed, that the tibia/femur ratio is diagnostic for ornithomimids. The overlap seen in the error

559 bars (Fig. 20) and the failure of the ratio to distinguish between Ornithomimus and

560 Struthiomimus indicate that caution should still be exercised when diagnosing ornithomimid taxa

561 this way. However, when considered together with other morphological differences, the

562 tibia/femur ratio could still be a useful diagnostic tool. Thus the measurable disparity in

563 tibia/femur ratios between Dromiceiomimus and Ornithomimus edmontonicus, combined with

564 differences in morphology such as those seen in the manus (discussed below), could be sufficient

565 to support Dromiceiomimus as a valid genus.

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566 Even though there were too few sufficiently complete Ornithomimus measured to directly

567 compare the femur-MtIII ratio with Dromiceiomimus, that ratio does seem to separate

568 Dromiceiomimus, Gallimimus, and Struthiomimus to some degree. However the t-test did not

569 reveal a statistically significant difference. Thus, while the femur-MtIII ratio does appear to

570 delineate between these genera to a degree, the ratio cannot be considered sufficiently diagnostic.

571 The manus of UALVP 16182 is generally more similar to Ornithomimus than to

572 Struthiomimus in its proportions (Fig. 12), but exhibits some differences. Metacarpals I and III

573 are slightly more gracile in UALVP 16182 than in Ornithomimus (Table 4) and much more

574 gracile than in Struthiomimus. The manus differs further from that of Ornithomimus in the

575 medial inflection of metacarpal I, resulting in the divergence of the distal portion of metacarpal I

576 from metacarpal II. In Ornithomimus, these two bones are appressed along their entire length. A

577 slight divergence seems to be present in some Ornithomimus specimens, but to a much lesser

578 degree than in UALVP 16182. In fact the divergence of the first metacarpal in UALVP 16182

579 more closely resembles the condition seen in Struthiomimus. However, metacarpal I is longer

580 than metacarpal II (although it should be noted that Mc II is from the left manus) which is in turn

581 longer than metacarpal III, a condition thought to diagnose Ornithomimus as a whole (Claessens

582 and Loewen, 2015; Russell, 1972). If this condition is truly diagnostic for Ornithomimus, then

583 specimens assigned to Dromiceiomimus could instead be referred to as Ornithomimus

584 brevitertius (Russell, 1930). The ungual of UALVP 16182 (Fig. 13A) is noticeably curved in

585 contrast with the straight unguals seen in ROM 851, identified as Ornithomimus edmontonicus

586 (Fig. 13B). However, it resembles the curvature seen in TMP 1995.110.0001 (Fig. 13C), another

587 specimen identified as Ornithomimus. However, in both ROM 851 and TMP 1995.110.0001, the

588 flexor tubercles are low, weakly-developed structures that are barely obvious in lateral aspect. In

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589 contrast, the flexor tubercle of UALVP 16182 is more prominent in lateral view. In this respect it

590 is more similar to the flexor tubercle of Struthiomimus (Fig. 13D). These may be significant

591 differences because there is evidence that ornithomimid manual morphology, including that of

592 the unguals, can be diagnostic at a generic level (Russell, 1972; Nicholls and Russell, 1981;

593 Makovicky et al. 2004; Kobayashi and Barsbold, 2006; Longrich, 2008; Tsogtbaatar et al.

594 2017b; R. Nottrodt, pers. comm., 2017). Manual unguals have not been reported from any

595 Dromiceiomimus brevitertius specimens other than UALVP 16182, although two unguals, one

596 from digit I and the other from either digit II or III, have been reported for Dromiceiomimus

597 samueli (Parks, 1928). The claws differ noticeably from each other, with I-2 being more curved

598 and robust compared to the other ungual. This contrasts with Ornithomimus where all three

599 manual unguals are essentially the same shape and more resembles the condition observed in

600 Struthiomimus. Unfortunately the ungual from digit II or III is too poorly preserved to properly

601 compare the flexor tubercle to that of UALVP 16182 or Ornithomimus specimens.

602 The topological variability of the trees from study to study (e.g. Kobayashi and Lü, 2003;

603 Cullen et al. 2013; Serrano-Brañas et al.2015; McFeeters et al. 2016) indicates that the taxonomy

604 of Ornithomimosauria still requires significant attention. The topology of the current tree is

605 roughly similar to other analyses of ornithomimosaurs. However, Anserimimus and

606 Ornithomimus were recovered as sister taxa with UALVP 16182 as the outgroup. The primary

607 purpose of this analysis was to see whether Dromiceiomimus and Ornithomimus group as sister

608 taxa, which would support their synonymy, or if they group as more distantly related taxa, which

609 would support the retention of separate genera. The current analysis supports the notion that

610 Dromiceiomimus breviterius and Ornithomimus edmontonicus could be distinct given that

611 UALVP 16182 was not recovered as the sister taxon to Ornithomimus. However, the

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612 discrepancies between different analyses suggest that any phylogenetic hypothesis should

613 considered tentative. Among the 96 characters (Appendix 1) for which it was possible to

614 compare both taxa, Dromiceiomimus and Ornithomimus differ in nine instances. These

615 differences appear in features of the skull (108), vertebrae (139, 145), scapula (176), manus

616 (210), and pelvis (219, 220, 231, 242). The morphology of the obturator foramen of the ischium

617 (242) differs between UALVP 16182 and Ornithomimus, but the distribution of this character

618 seems to be variable across different specimens referred to Dromiceiomimus (B. McFeeters, pers.

619 comm., 2018). The presence of a posterior surangular foramen in UALVP 16182 is shared by

620 Struthiomimus but not by Ornithomimus, as is the depression found on the supraglenoid buttress

621 of the scapula. The difference in the morphology of the flexor tubercle and curvature of the

622 manual ungual, as well as the distal divergence of the metacarpals, may be significant as other

623 authors have noted the diagnostic potential of the ornithomimid manus. These anatomical

624 differences may serve to bolster distinctions made on the basis of the difference in the

625 tibia/femur ratio.

626 One possible explanation for two somewhat distinct tibia/femur data clusters that display

627 some overlap in the margins of error is sexual dimorphism. This could also account for the

628 somewhat more gracile metacarpals of UALVP 16182. Although the precise nature of sexual

629 dimorphism is highly variable among the extant phylogenetic bracket for dinosaurs (Barden and

630 Maidment, 2011), sexual dimorphism is far more common than monomorphism

631 (Kaliontzopoulou et al. 2007). It is therefore reasonable to expect it in dinosaurs. Various studies

632 have proposed sexual dimorphism based on femoral morphology. Raath (1990) identified gracile

633 and robust morphs of Coelophysis rhodesiensis femora, and Larson (2008) had similar findings

634 in a study of Tyrannosaurus rex. Barden and Maidment (2011) found what they consider to be

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635 sexual dimorphism among the femora of Kentrosaurus aethiopicus. Although the sample size is

636 limited, the Ornithomimus femoral lengths are greater than those of Dromiceiomimus in all but

637 two instances (ROM 852 and TMP 1995.110.0001, Table 2), and it is possible that the absolute

638 size differences correlate with sexual differences. However, it should be noted that this apparent

639 difference in size may be misleading. A histological analysis by Cullen et al. (2014) concluded,

640 due to the absence of an outer circumferential layer in any of the elements sectioned, that ROM

641 852 (the largest specimen assigned to Dromiceiomimus) had likely not attained full size when it

642 died. Furthermore, recent studies conclude that detecting sexual dimorphism in dinosaurs may

643 not be feasible given the fossil material available. Hone and Mallon (2017) proposed a number of

644 confounding factors. These included the protracted growth periods of most dinosaurs, which

645 cannot be readily accounted for without sample sizes that are not generally available in the fossil

646 record. They found that, even among the relatively sexually dimorphic Alligator mississippiensis

647 and with a priori knowledge of sex, detection of sexual dimorphism remained difficult without a

648 minimum of 35 individuals per sex and controls for age. Mallon (2017) notes that (among other

649 methodological shortcomings) no studies of sexual dimorphism in dinosaurs have included

650 skeletochronological determination of age and also emphasizes the importance of large sample

651 sizes. Mallon (2017) concluded that sexual dimorphism was not supported in any of the nine

652 dinosaur taxa he examined, including Coelophysis, Kentrosaurus, and Tyrannosaurus.

653 The (possibly) longer femora in Ornithomimus could also indicate that the two forms are

654 simply different ontogenetic stages with the younger ontogenetic stage represented by specimens

655 identified as Dromiceiomimus. Again, ontogeny could account for the slightly more gracile

656 metacarpals of UALVP 16182 compared to Ornithomimus. The lack of fusion between the

657 scapula and coracoid and between pelvic elements, as well as the disarticulated preservation of

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658 the skull elements, suggest an immature animal. Examining bone histology could reveal whether

659 Ornithomimus bones are consistently at a later ontogenetic stage than Dromiceiomimus bones.

660 That said, however, the tibia/femur ratio is still able to delineate between the taxa despite the fact

661 that the femoral sizes of Gallimimus and Struthiomimus overlap substantially with those of

662 Dromiceiomimus, as do those of Ornithomimus to a lesser extent (Fig. 20). Furthermore, it is not

663 obvious that morphology of the manus in general should change through ontogeny. Kobayashi

664 and Barsbold (2006) report that the relative size of the manus compared to the humerus in

665 Gallimimus bullatus remains consistent between the smallest and largest specimens, although

666 there is no mention of whether the unguals are notably different.

667 Examining the stratigraphic position of the two genera informs considerations of sexual

668 dimorphism and individual variation. If the two genera were generally separated

669 stratigraphically, this would lend credence to the conclusion that Dromiceiomimus and

670 Ornithomimus edmontonicus are distinct taxa. Unfortunately, relatively few ornithomimid

671 specimens are assigned to a particular genus, but it is apparent that Dromiceiomimus brevitertius

672 is generally found higher in section than Ornithomimus edmontonicus (Fig. 21). There is,

673 however, a slight overlap in the Horsethief Member of the Horseshoe Canyon Formation

674 (Dromiceiomimus specimen ROM 797 and Ornithomimus specimen CMN 8632). The only

675 major outlier to this pattern is the presence in the Oldman Formation of ROM 840, which is

676 assigned by Russell (1972) to Dromiceiomimus samueli. This species was originally identified as

677 Struthiomimus (Parks, 1928) and was synonymized with Ornithomimus edmontonicus by

678 Makovicky et al. (2004). It also lacks the elements required for determining the significant limb

679 ratios that arguably distinguish Dromiceiomimus from Ornithomimus. It is therefore difficult to

680 be sure of how this specimen impacts the overall pattern, although its stratigraphic position may

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681 suggest that it is more closely linked to Ornithomimus. This pattern provides a basis for

682 tentatively rejecting the explanations of sexual dimorphism and individual variation because it

683 would not make sense for different sexual or ontogenetic morphs to be stratigraphically

684 segregated. As noted, however, there are too few specimens assigned to either Dromiceiomimus

685 or Ornithomimus to establish a statistically robust pattern in their relative stratigraphic

686 distributions.

687 Closely related extant animals with very similar morphology can coexist, and thus the

688 idea of Dromiceiomimus and Ornithomimus being distinct but sympatric genera is not

689 unreasonable. One example of coexistence is between mule deer and white-tailed deer in

690 southern Alberta, where these two similar species are found in sympatry. However, there is no

691 competitive interference with one another (Krämer, 1973). Whitney et al. (2011) found that

692 sympatric white-tailed and black-tailed deer, although they have similar diets and habitat use,

693 were able to coexist due to spatial segregation whereby competition is mainly avoided because

694 direct interaction is limited. The difference in manual ungual morphology between the two

695 groups could indicate distinct ecologies (Tsogtbaatar et al. 2017b), which would agree with the

696 idea of similar but separate sympatric genera.

697 Regardless of whether Dromiceiomimus is revealed to be a valid taxon or a synonym of

698 Ornithomimus edmontonicus, it should be noted that there are issues with several of the

699 references cited by various studies in support of the latter case. There appears to be a trend in the

700 literature to consider the two genera synonymous. However, Dromiceiomimus has not been

701 conclusively invalidated in any publication, and so the current consensus on the matter is

702 misleading. The majority of papers consider the genera synonymous without any explicit

703 mention of Dromiceiomimus (e.g. Ji et al. 2003; Longrich, 2008; Varricchio et al. 2008;

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704 Bronowicz, 2011). Cullen et al. (2013) mention Dromiceiomimus specifically and consider it to

705 be synonymous with Ornithomimus edmontonicus, citing Longrich (2008) and Xu et al. (2011)

706 to support this. As noted, Longrich (2008) discusses only Ornithomimus and does not make any

707 explicit mention of Dromiceiomimus. Although this is an implicit synonymy, no support is

708 offered for the synonymy. Therefore, while this paper conforms to the recent trend, it should not

709 be considered as evidence in favour of synonymy. The focus of Cullen et al. (2013), as with

710 papers that implicitly synonymize the two genera, is not on investigating the distinction between

711 Dromiceiomimus and Ornithomimus and thus the confusion is understandable.

712 Xu et al. (2011) also explicitly synonymize the two taxa, citing Makovicky et al. (2004)

713 and Kobayashi et al. (2006). Kobayashi et al. (2006) refer to “some previous studies” which

714 found the ratios used by Russell (1972) to diagnose Dromiceiomimus lacked statistical support.

715 Because Kobayashi et al. (2006) is a presentation abstract, it does not explicitly cite these

716 studies. However these “previous studies” seem likely include Makovicky et al. (2004), which is

717 somewhat problematic (discussed in the next paragraph). Kobayashi et al. (2006) also support

718 synonymy by citing Ornithomimus-like features of Dromiceiomimus specimen CMN 12228,

719 specifically the morphology of the anterior ramus of the postorbital, the dorsal ramus of the

720 quadratojugal and the prequadratic foramen. While synonymy is one explanation for these

721 similarities, they could also be explained by a sister taxon relationship between the two genera or

722 by Dromiceiomimus brevitertius being a species of Ornithomimus.

723 Makovicky et al. (2004) seems to be the root of much of the confusion because several

724 papers either cite this source directly (e.g. Xu et al. 2011) or indirectly (e.g. Cullen et al. 2013).

725 When looking at papers that synonymize Dromiceiomimus brevitertius and Ornithomimus

726 edmontonicus, one finds that they are almost exclusively published after 2004. The issue is that

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727 Makovicky et al. (2004) cite Nicholls and Russell (1981) as an authority for synonymizing the

728 two taxa when in fact Nicholls and Russell (1981) conclude that Dromiceiomimus should be

729 considered a valid taxon. More specifically, Nicholls and Russell (1981) report that while limb

730 proportions may not be diagnostic among ornithomimids in general, they seem to be diagnostic

731 for Dromiceiomimus in particular. The confusion in Makovicky et al. (2004) is also likely the

732 root of the error in Watanabe et al. (2013), who cite Nicholls and Russell (1981) as

733 synonymizing the two genera. Makovicky et al. (2004) also support the synonymy by making

734 reference to a re-examination of the proportions used by Russell (1972) which revealed no

735 statistically significant differences. Unfortunately, the format of The Dinosauria prevented the

736 data from being included in the entry and thus the fact remains that there is still no published

737 data that synonymize Dromiceiomimus and Ornithomimus edmontonicus. Another note of

738 interest is that Dromiceiomimus brevitertius was erected by Parks (1926) and Ornithomimus

739 edmontonicus by Sternberg (1933). Thus, if Dromiceiomimus brevitertius and Ornithomimus

740 edmontonicus are to be considered synonymous, then their designation should properly be

741 Ornithomimus brevitertius (Russell, 1930).

742

743 CONCLUSIONS

744 Whereas Nicholls and Russell (1981) conclude that limb proportions are not necessarily a

745 reliable diagnostic feature, they qualify that statement by saying that the tibia/femur ratio may be

746 diagnostic for Dromiceiomimus. The present study supports these findings and further suggests

747 that limb ratios may be diagnostic for ornithomimids. The t-test provided statistical support for

748 distinguishing Dromiceiomimus from Ornithomimus (as well as other ornithomimids) on the

749 basis of tibia/femur proportions. This statistical difference is present despite the overlap in

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750 absolute femur sizes across the genera examined. The differences in the skull (the presence of a

751 posterior surangular foramen), scapula (depression on supraglenoid buttress), and the manus

752 (strongly divergent metacarpal I, more prominent flexor tubercle in phalanx II-2) could be

753 significant, although of course the small sample size makes it difficult to assess individual and/or

754 sexual variation. Additionally, the apparent stratigraphic separation of Dromiceiomimus

755 brevitertius and Ornithomimus edmontonicus supports a taxonomic distinction. At minimum, this

756 study has replicated the finding that there are two morphs (in terms of tibia/femur ratio) present

757 in specimens generally assigned to Ornithomimus, regardless of whether or not these morphs

758 represent inter- or intraspecific variation. Based on the points discussed, it is not unreasonable to

759 conclude that these two morphs do indeed represent distinct taxa. Although there are doubts

760 regarding the utility of limb ratios in diagnosing taxa, it appears that the tibia/femur ratio,

761 especially when considered in conjunction with other anatomical differences, is useful in

762 distinguishing between ornithomimid taxa. Despite the recent consensus in the literature,

763 Dromiceiomimus has not been invalidated as a genus by any published data and, in light of the

764 present study, it seems advisable, as proposed by Nicholls and Russell (1981), to retain the genus

765 Dromiceiomimus until data are published that do so. Conversely, if the relative lengths of the

766 metacarpals is diagnostic for Ornithomimus as a genus, then it would also be reasonable (based

767 on the findings of this study) to refer to Dromiceiomimus specimens as Ornithomimus

768 brevitertius.

769

770 ACKNOWLEDGEMENTS

771 The authors would like to thank Eilidh Macdonald (who is wonderful), Victoria Arbour, Caleb

772 Brown, Mike Burns, Eva Koppelhus, Rachel Nottrodt, Scott Persons and Tetsuto Miyashita for

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773 providing fruitful discussions and valuable advice as well as being very helpful in general. Yoshi

774 Kobayashi (University of Hokkaido, Japan) provided additional data and suggestions. Thanks

775 also to the reviewers whose input elevated the quality of this paper.

776

777 INSTITUTIONAL ABBREVIATIONS

778 AMNH, American Museum of Natural History, New York; BHI, Black Hills Institute of

779 Geological Research, Hill City, South Dakota; CMN, Canadian Museum of Nature, Ottawa; GI,

780 Geological Institute, Academy of Sciences, Ulan Bator, Mongolia; ROM, Royal Ontario

781 Museum, Toronto; TMP, Royal Tyrrell Museum of Palaeontology, Drumheller, Alberta;

782 UALVP, University of Alberta Laboratory for Vertebrate Paleontology, Edmonton, Alberta;

783 UCMZ (VP), University of Calgary Museum of Zoology, Calgary, Alberta.

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TABLE 1. Measurements taken from UALVP 16182, all of which were taken twice and averaged.

Dentary preserved length (mm)min height (mm)max height (mm)distance from buccal edge to symphysis (mm)distance of foramina from buccal edge (mm)length of symphysis (mm)depth of intramandibular articular surface (mm)distance between jaw margin and alveolar shelf (mm)

13713.720.5201.5 – 432.54.56.7 (anteriorly) – 2 (posteriorly)

Surangular preserved length (mm)length of overlap with dentary (mm)width of anterior margin of articulation with quadrate (mm)distance between articulation for quadrate and end of retorarticular process (mm)length of posterior surangular foramen (mm)distance between anterior and posterior surangular foramena (mm)

11927720334

Hyoid preserved length (mm)diameter of anterior end (mm)diameter of posterior end of preserved portion (mm)

1202.65

length (mm) 283Scapulaanteroposterior width (mm) 28.3

Ulna length (mm)midshaft diameter (mm)

2809.7

length of mc I (mm) 101.39width of mc I (mm) 8.02length of mc II (mm) 95.85width of mc II (mm) 8.19length of mc III (mm) 92.82

Metacarpals

width of mc III (mm) 6.55length ph I-1 105length ph II-2 (mm) 74.6straight length ph II-3 (mm) 67.51outside curve length ph II-3 (mm) 74.44

Manual phalanges

length ph III-3 (mm) 62.94anteroposterior length (mm) 412.5antilium length (mm) 163

Ilium

height (mm) 151.5length (mm) 369.7Pubisminimum anteroposterior width (mm) 9.3length (mm) 319.3height of head (mm) 43.5fourth trochanter length (mm) 83.58fourth trochanter height (mm) 13.4

Femur

Femur- minimum transverse width (mm) 45.7length (mm) 468.5cnemial crest length (mm) 96.3minimum transverse width (mm) 32.8

Tibia

intermaleolar width (mm) 75.2Fibula length (mm)

fibula head length (mm)minimum shaft width, measured anteroposteriorly (mm)

441.567.511.8

length (mm) 341.5Metatarsusminimum width (mm) 46

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TABLE 2. Femur and tibia lengths of Dromiceiomimus, Gallimimus, Ornithomimus and Struthiomimus, as well as the ratios of the log10 transformed measurements and the sources of the measurements used in this study.

Species Specimen # SourceTibia length (mm)

Femur length (mm)

Tibia/femurLog10

tibia/Log10 femur

D. brevitertius AMNH 5201 Currie pers. obs. 438 387 1.13 1.02D. brevitertius ROM 797 Parks 1926, Clive Coy 470 390 1.21 1.03D. brevitertius UALVP 16182 Macdonald pers. obs 469 410 1.14 1.02

D. brevitertius CMN 12068 Currie pers. obs. (PJC 2004) 493 416 1.19 1.03

D. brevitertius ROM 852 Parks 1933 520 440 1.18 1.03G. bullatus MPC-D100/10 Currie pers. obs. 218 192 1.14 1.02G. bullatus D-I/94 Currie pers. obs. 292 270 1.08 1.01G. bullatus MPC-D KID 499 Currie pers. obs. 350 332 1.05 1.01G. bullatus Zpal MgD-I/1 Currie pers. obs. 384 360 1.07 1.01G. bullatus MPC-D100/14 Currie pers. obs. 403 391 1.03 1.00G. bullatus MPC-D100/52 Currie pers. obs. 400 400 1.00 1.00G. bullatus Field # 950818 Currie pers. obs. 450 443 1.02 1.00G. bullatus MPC-D100/12 Currie pers. obs. 508 500 1.01 1.00

O. edmontonicus TMP 1995.110.0001 Currie pers. obs. 465 425 1.09 1.02

O. edmontonicus ROM 851 Parks 1933, Clive Coy, Russell 72, PJC 2005 475 435 1.09 1.01

O. edmontonicus UALVP 52531 Currie pers. obs. 520 480 1.08 1.01

O. edmontonicus CMN 12441 Currie pers. obs. (PJC 2004) 550 507 1.08 1.01

S. altus AMNH 5385 Currie pers. obs. 408 370 1.10 1.02

S. altus TMP 1990.026.0001 Currie pers. obs. 506 467 1.08 1.01

S. altus AMNH 5339 Osborn 1917 540 480 1.13 1.02

S. altus UCMZ (VP) 1980.1 Currie pers. obs. 556 502 1.11 1.02

S. altus AMNH 5257 Currie pers. obs. 555 512 1.08 1.01S. sedens BHI 1266 van der Reest et al. 2016 700 632 1.12 1.02

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TABLE 3. Allometric analysis of tibia-femur ratio for Dromiceiomimus, Gallimimus, Ornithomimus and Struthiomimus using RMA 1.17.

Taxon R2 Slope Intercept Lower CI Upper CI Growth Pattern

Dromiceiomimus 0.841 1.22 -0.51 0.33 2.12 isometry

Gallimimus 0.996 0.87 0.34 0.82 0.92 -ve allometry

Ornithomimus 0.999 0.95 0.18 0.88 1.01 isometry

Struthiomimus 0.991 1.04 -0.07 0.93 1.15 isometry

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TABLE 4. Ratios of the manus for Dromiceiomimus, Ornithomimus and Struthiomimus derived from measurements which were taken twice and averaged.

Ratio Dromiceiomimus(UALVP 16182)

Ornithomimus(ROM 851)

Struthiomimus(BHI 1266)

Mc I length/Mc I width 12.64 11.40 –Mc III length/Mc III width 14.17 11.76 –Mc I length/Mc III length 1.09 1.06 0.98Mc I length/Femur length 0.25 0.24 0.18Mc III length/Femur length 0.23 0.22 0.19Ph I-1 length/Mc I length 1.04 1.08 1.09Ph I-1 length/Mc III length 1.13 1.14 1.07Ph I-1 length/Ph II-2 length 1.41 1.30 1.24Ph I-1 length/ Ph III-3 length 1.67 1.53 1.56Ph I-1 length/Femur length 0.26 0.26 0.20Ph II-3 outer length/straight length 1.10 1.00 1.07

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TABLE 5. Results from a one-tailed t-test with unequal variance comparing the tibia/femur ratios of different pairs of genera.

Genera t P t critical

Dromiceiomimus (n=5) – Gallimimus (n=8) 5.13 0.00016 1.79

Dromiceiomimus (n=5) – Ornithomimus (n=4) 6.08 0.00185 2.13

Dromiceiomimus (n=5) – Struthiomimus (n=7) 4.99 0.00124 1.94

Gallimimus (n=8) – Ornithomimus (n=4) 1.87 0.05191 1.89

Gallimimus (n=8) – Struthiomimus (n=7) 2.13 0.03083 1.83

Ornithomimus (n=4) – Struthiomimus (n=7) 0.92 0.19174 1.86

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TABLE 6. Metatarsal III and femur lengths (measured twice and averaged) of Dromiceiomimus, Gallimimus, Ornithomimus and Struthiomimus, as well as the ratios of those two elements.

Species Specimen # Mt III length (mm) Femur length (mm) Femur/MtIII

Dromiceiomimus brevitertius CMN 12068 356 416 1.168539

Dromiceiomimus brevitertius ROM 797 298 390 1.308725

Dromiceiomimus brevitertius ROM 852 370 440 1.189189

Dromiceiomimus brevitertius UALVP 16182 341 410 1.202346

Gallimimus bullatus Zpal MgD-I/1 280 360 1.285714

Gallimimus bullatus D-I/8 510 635 1.245098

Gallimimus bullatus D-I/94 220 270 1.227273

Gallimimus bullatus MPC-D100/10 157 192 1.22293

Gallimimus bullatus MPC-D100/11 530 665 1.254717

Gallimimus bullatus MPC-D100/12 360 500 1.388889

Gallimimus bullatus MPC-D100/52 283 400 1.413428

Gallimimus bullatus Field # 950818 305 443 1.452459

Ornithomimus edmontonicus ROM 851 310 435 1.403226

Ornithomimus edmontonicus RTMP 95.110.1 332 425 1.28012

Struthiomimus altus UCMZ (VP) 1980.1 398 502 1.261307

Struthiomimus altus ROM 1790 300 395 1.316667

Struthiomimus altus AMNH 5257 370 512 1.383784

Struthiomimus altus AMNH 5339 370 480 1.297297

Struthiomimus altus RTMP 90.26.1 375 467 1.245333

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TABLE 7. Results from a one-tailed t-test with unequal variance comparing the metatarsal III/femur ratios of different pairs of genera.

Genera t P t critical

Dromiceiomimus (n=4) – Gallimimus (n=8) 2.12 0.03334 1.86

Dromiceiomimus (n=4) – Ornithomimus (n=2) 1.81 0.10605 2.92

Dromiceiomimus (n=4) – Struthiomimus (n=4) 1.81 0.05994 1.94

Gallimimus (n=8) – Ornithomimus (n=2) 0.41 0.36136 2.92

Gallimimus (n=8) – Struthiomimus (n=4) 0.32 0.32014 1.83

Ornithomimus (n=2) – Struthiomimus (n=4) 0.65 0.29131 2.92

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FIGURE 1. Map of the area from which UALVP 16182 was collected. A, an overview of Alberta with an inset of the immediate area surrounding the collection site, including an outline of Dry Island Buffalo Jump Provincial Park. Modified from Google Maps. Scale bar equals 10km; B, a satellite image from Google Maps with the collection site marked by an X. Scale bar equals 1km.

FIGURE 2. Skull elements from UALVP 16182. A, right jugal in dorsolateral view; B, right jugal in lateral view; C, left dentary and splenial in medial view. d, dentary; pn, pneumatopore; qj, quadratojugal; sp, splenial. Shaded grey area represents contact with another bone. Scale bars equal 5cm.

FIGURE 3. Skull elements from UALVP 16182. A, right surangular in lateral view; B, right dentary in medial view; C, right prearticular in medial view; D, right nasal in dorsal view and right postorbital in lateral view. mf, mandibular fenestra. Shaded grey area represents contact with another bone. Scale bars equal 5cm.

FIGURE 4. Hyoid in lateral view. Scale bar equals 5 cm.

FIGURE 5. Vertebrae from UALVP 16182. Light grey indicates matrix A, right lateral view of cervical vertebra; B, left lateral view of seventh dorsal vertebra; C, anterior view of caudal vertebra; D, right lateral view of caudal vertebra. C and D are based primarily on the sixth caudal but are composite images of three proximal caudals. cpf, central pneumatic foramen; id, infradiapophysial fossa; ipo, infrapostzygapophysial fossa; ipr, infraprezygapophysial fossa; ns, neural spine; po, postzygapophyses; pr, prezygapophyses; tr, transverse process. Scale bars equal 5 cm.

FIGURE 6. Cervical vertebrae, arranged from caudalmost to cranialmost. A, dorsal view; B, right lateral view. Scale bar equals 10 cm.

FIGURE 7. Dorsal vertebrae. A, dorsal view; B, right lateral view. Scale bar equals 10 cm.

FIGURE 8. Caudal vertebrae and haemal arches. A, caudal vertebrae in dorsal view; B, caudal vertebrae in right lateral view; C, haemal arches in left lateral view; D, haemal arches in posterior view. Scale bar equals 10 cm.

FIGURE 9. Ribs and gastralia. A, ribs; B, gastralia. Scale bar equals 10 cm.

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FIGURE 10. Left scapula in lateral view. Hashing indicates areas that have been reconstructed. ac, acromion; gl, scapular portion of glenoid; scb, scapular blade. Scale bar equals 10 cm.

FIGURE 11. Right ulna. A, dorsal view; B, lateral view. cp, coronoid process; op, olecranon process; tr, trochlear notch. Scale bar equals 10 cm.

FIGURE 12. Comparison of ornithomimid manus. All appear in lateral view. A is a right manus while B, C, and D are left manus reversed along a vertical axis for more direct comparison with A. A, Dromiceiomimus, UALVP 16182, right manus; B, Ornithomimus, ROM 851; C, Struthiomimus, UCMZ (VP) 1980.1; D, Gallimimus, G.I. No. DPS 100/11. Modified from Nicholls and Russell (1981). Scale bar equals 10 cm.

FIGURE 13. Comparison of ornithomimid manual ungual II-3 in lateral view. A, Dromiceiomimus brevitertius, UALVP 16182; B, Ornithomimus edmontonicus, ROM 851; C, Ornithomimus edmontonicus, TMP 1995.110.0001; D Struthiomimus altus, TMP 1990.026.0001. ft, flexor tubercle; kg, keratin groove. Scale bar equals 5cm.

FIGURE 14. Right manual phalanx II-2. A, right lateral view; B, left lateral view; C, dorsal view; D, ventral view, after the bony callous was prepared away.

FIGURE 15. Pelvic girdle of UALVP 16182. Light grey areas indicate matrix, hashed areas indicate reconstruction. A, left ilium in lateral view; B, pelvic girdle in right lateral view. ac, acetabulum; bf, brevis fossa; bs, brevis shelf; cf, cuppidicus fossa; il, ilum; ip, ischial peduncle; isc, ischium; isa, ischial apron p, pubis; pp, pubic peduncle; pua, pubic apron; ss, supraacetabular shelf. Scale bars equal 10 cm.

FIGURE 16. Hind limb elements of UALVP 16182. Light grey areas indicate matrix, hashed areas indicate reconstruction. A, left femur in posteromedial view; B, left tibia-fibula in medial view; C, left metatarsus in anterior view. Note that Mt II is shifted proximally in the illustration compared to the photograph. This is the result of preparation subsequent to the illustration being done and repositioning of the element into its proper position. a, astragalus; cn, cnemial crest; f, fibula; fh, femoral head; ft, fourth trochanter; ig, intercondylar groove; II, metacarpal II; III, metacarpal III; IV, metacarpal IV; lc, lateral condyle; mc, medial condyle; t, tibia. Scale bars equal 10 cm.

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FIGURE 17. Left tibia-fibula in lateral view. a, astragalus; cal, calcaneum; cn, cnemial crest; f, fibula; fc, fibular crest; t, tibia. Scale bar equals 10 cm.

FIGURE 18. Pedal phalanges. All phalanges appear first in lateral, then dorsal,ventral, proximal and finally distal view. A, Ph II-1; B, Ph III-2; C, Ph III-3; D, Ph IV-2; E, Ph II-3; F, Ph III-4. Scale bar equals 5 cm.

FIGURE 19. Most parsimonious tree recovered from a heuristic analysis of ten ornithomimosaurs and four other theropods outgroups with bootstrap and Bremer values added (Bootstrap/Bremer).

FIGURE 20. Comparison of tibia-femur ratios between Dromiceiomimus, Ornithomimus and Struthiomimus. Ratios were calculated from log10-transformed measurements to account for differences in size. Reduced major axis (RMA) regression lines were calculated to assess how well correlated data clusters were. The different taxa cluster separately despite overlapping in absolute femur size, although the error bars overlap. A and B represent the same data, but the scales of the axes have been altered in B for visual clarity.

FIGURE 21. Stratigraphic position of ornithomimid specimens. Dromiceiomimus specimens seem to appear generally higher in section than Ornithomimus specimens, however the sample of ornithomimids identified to genus is too small to reveal a statistically significant pattern. Specimen locations are based on Table A1 from Eberth et al., 2013. The figure is made in the same style as Figure 6 from Cullen et al., 2013.

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APPENDIX 1 – Characters used in phylogenetic analysis

1. Skull compared with length of neck: 0, neck less than double length of skull; 1, neck at least twice length of skull (Perez-Moreno et al., 1994).

2. Skull vs Femur lengths: 0, falls on or near tyrannosaurid bivariate line y=0.9638x + 0.09; 1, falls well below this line (new, this paper).

3. Hand (mc II plus digit II) to humerus plus radius length: 0, less than 59%; 1, more than 60% (Perez-Moreno et al., 1994).

4. Tibia plus Metatarsal III to Femur lengths in comparison with tyrannosaurids: 0, less than in tyrannosaurids; 1, the same as tyrannosaurids or greater.

5. Narial opening, posterior margin: 0, more anterior than, or nearly reaching anterior border of the antorbital fossa; 1, overlapping.

6. Antorbital fossa, lateral view: 0, dorsal border formed by the lacrimal and maxilla; 1, by the lacrimal and nasal; 2, by maxilla, premaxilla, and lacrimal.

7. Antorbital fenestra size compared with orbit: 0, falls close to tyrannosaurids on line y=1.14x-.05); 1, falls significantly below line; 2, smaller yet (oviraptorids).

8. Lateral temporal fenestra: 0, postorbital bar parallels quadrate, lower temporal fenestra rectangular; 1, jugal and postorbital approach or contact quadratojugal-squamosal flange to constrict fenestra.

9. Upper temporal fossa: 0, limited extension onto dorsal surfaces of frontal and postorbital; 1, covers most of frontal process of the postorbital and extends anteriorly onto dorsal surface of frontal

10. Upper temporal fenestra: 0, bounded laterally and posteriorly by the squamosal; 1, supratemporal fenestra extended as a fossa on to the dorsal surface of the squamosal.

11. External mandibular fenestra: 0, present; 1, reduced; 2, absent.12. Premaxillary symphysis: 0, acute, V-shaped; 1, rounded, U-shaped.13. Premaxilla, crenulate margin on buccal edge of premaxilla: 0, absent; 1, present. Only

applies in taxa with edentulous premaxilla.14. Premaxilla, main body: 0, anteroposteriorly longer than high or approximately as long

as high; 1, significantly higher than long. (Turner, et al., 2012, character 260).15. Premaxilla, maxillary process: 0, contacts nasal to form posterior border of nares; 1,

reduced so that maxilla participates in external naris; 2, extends posteriorly to separate maxilla from nasal behind naris.

16. Premaxilla, maxillary process: 0, posterior end terminates anterior to anterior border of antorbital fossa; 1, extends more posteriorly (Kobayashi and Lü, 2003).

17. Premaxilla: 0, internarial bar rounded; 1, flat.18. Maxilla: 0, participates in external narial opening; 1, separated from opening by

maxilla-nasal contact (Xu et al., 2002).19. Maxilla, series of foramina along ventral edge of lateral surface: 0, present; 1, absent

(Kobayashi and Lü, 2003).20. Maxilla, promaxillary fenestra: 0, absent; 1, present.21. Maxilla, promaxillary fenestra: 0, visible in lateral view; 1, obscured by ascending

ramus of maxilla (Witmer, 1997).22. Maxilla, maxillary fenestra: 0, situated at anterior border of antorbital fossa; 1, situated

posterior to anterior border of fossa.

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23. Maxilla, maxillary fenestra displaced dorsally: 0, absent; 1, present.24. Maxilla, jugal process ventral to antorbital fossa: 0, dorsoventrally shallow; 1,

dorsoventrally deep.25. Maxilla, secondary palate: 0, short; 1, long, with extensive palatal shelves on maxilla.26. Nasals: 0, unfused; 1, at least partially fused.27. Nasals, dorsal surface of nasals: 0, smooth; 1, ornamented with irregular sculpting [taxa

with a mid-line crest are considered inapplicable].28. Nasals in dorsal view: 0, with parallel outer edges posterior to narial region; 1,

hourglass shaped with constriction at midlevel and expanded ends.29. Nasals, series of pneumatic foramina along lateral edge of nasal: 0, absent; 1, present.30. Nasals: 0, narial region apneumatic or poorly pneumatized; 1, with extensive pneumatic

fossae, especially along posterodorsal rim of naris.31. Jugal: 0, does not participate in margin of antorbital fenestra; 1, participates in antorbital

fenestra.32. Jugal, sublacrimal part: 0, tapering; 1, expanded (Turner, 2012, character 262

simplified).33. Jugal pneumatic recess in posteroventral corner of antorbital fossa: 0, present; 1, absent.34. Jugal: 0, medial jugal foramen present on medial surface ventral to postorbital bar; 1,

absent.35. Jugal beneath lower temporal fenestra, 0, at least twice as tall dorsoventrally as it is

wide transversely; 1, rod-like.36. Jugal and postorbital: 0, contribute equally to postorbital bar; 1, ascending process of

jugal reduced and descending process of postorbital ventrally elongate.37. Lacrimal: 0, supraorbital crests in adult individuals absent; 1, dorsal crest above orbit; 2,

dorsal crest present and surmounted by cornual process.38. Lacrimal, enlarged foramen or foramina opening laterally at the angle of the lacrimal

above antorbital fenestra: 0, absent; 1, present.39. Lacrimal posterodorsal process: 0, absent (inverted 'L' shaped); 1, lacrimal 'T' shaped in

lateral view; 2, anterodorsal process much longer than posterior process.40. Lacrimal, prominence on lateral surface: 0, present; 1, absent (Xu et al., 2002).41. Jugal and quadratojugal: 0, separate; 1, jugal fused and not distinguishable from one

another.42. Prefrontal: 0, large, dorsal exposure similar to that of lacrimal; 1, greatly reduced in

size; 2, absent.43. Frontals: 0, narrow posteriorly as a wedge between nasals; 1, end abruptly posteriorly,

suture with nasal transversely oriented.44. Frontal, anterior emargination of supratemporal fossa onto frontal: 0, straight or slightly

curved; 1, strongly sinusoidal and reaching onto postorbital process.45. Frontal, position of frontoparietal suture relative to postorbital processes of frontal: 0,

well posterior; 1, level with; 2, anterior to (Turner, 2012, Character 464).46. Frontal: 0, broadly exposed along orbital margin; 1, excluded from orbital margin as

prefrontal and postorbital almost meet or contact each other.47. Postorbital, anterior process: 0, projects into orbit; 1, does not project into orbit.48. Postorbital, lateral view of anterior frontal process: 0, straight; 1, curves anterodorsally

and dorsal border of temporal bar is dorsally concave.

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49. Postorbital bar: 0, relatively narrow and similar to preorbital bar (lacrimal) in anteroposterior length; 1, anteroposteriorly long and plate-like, about twice as long as preorbital bar.

50. Parietals: 0, separate; 1, fused.51. Parietals: 0, dorsal surface flat, lateral ridge borders supratemporal fenestra; 1, dorsally

convex with low sagittal crest along midline; 2, dorsally convex with well-developed sagittal crest.

52. Squamosal, descending process: 0, parallels quadrate shaft; 1, nearly perpendicular to quadrate shaft.

53. Squamosal, ventral, zygomatic process: 0, elongate, encloses otic process of quadrate, dorsal head of quadrate not visible; 1, short, exposing head of quadrate laterally (Turner, 2012, character 290).

54. Quadratojugal: 0, without horizontal process posteroventral to ascending process (reversed 'L' shape); 1, with process (inverted 'T' or 'Y' shape).

55. Quadratojugal: 0, mediolaterally compressed and flat; 1, with distinct flexure near posterior border, so that posterior edge faces posteriorly rather than laterally.

56. Quadrate: 0, vertical; 1, strongly inclined anteroventrally so that distal end lies far forward of proximal end.

57. Quadrate head: 0, covered by squamosal in lateral view; 1, quadrate cotyle of squamosal open laterally exposing quadrate head.

58. Quadrate: 0, solid; 1, hollow (pneumatic), with foramen on posterior surface.59. Quadrate pneumatization: 0, none; 1, single large pneumatopore on posteromedial

surface of body (Turner, 2012, character 301).60. Quadrate, lateral border of shaft: 0, straight; 1, with broad, triangular process along

lateral edge of shaft contacting squamosal and quadratojugal above enlarged quadrate foramen.

61. Quadrate fenestra: 0, small, slit-like, fully or almost fully enclosed by quadrate; 1, very large, circular with broad participation of quadratojugal in lateral margin; 2, large but contained within quadrate.

62. Quadrate and quadratojugal ascending rami: 0, meet squamosal to form straight border to the lateral temporal fenestra; 1, kinked into fenestra at midheight.

63. Basisphenoid-parasphenoid, base of cultriform process: 0, not highly pneumatized; 1, base of cultriform process (parasphenoid rostrum) expanded and pneumatic (parasphenoid bulla present).

64. Basioccipital, subcondylar recesses: 0, absent; 1, present.65. Prootic, opisthotic crista interfenestralis: 0, confluent with lateral surface of prootic and

opisthotic; 1, distinctly depressed within middle ear opening.66. Basisphenoid in ventral view: 0, basisphenoid longer than wide, or with subequal

proportions; 1, basisphenoid clearly wider than long.67. Basisphenoid recess: 0, present between basisphenoid and basioccipital; 1, entirely

within basisphenoid; 2, absent.68. Basisphenoid with pronounced muscle scars flanking basisphenoid recess: 0, no; 1, yes.69. Basisphenoid, posterior opening of basisphenoid recess: 0, single; 1, divided into two

small, circular foramina by a thin bar of bone.70. Basipterygoid processes: 0, ventral or anteroventrally projecting; 1, lateroventrally

projecting.

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71. Basipterygoid processes: 0, well developed, extending as a distinct process from the base of the basisphenoid; 1, processes abbreviated or absent.

72. Basipterygoid processes: 0, solid; 1, hollow.73. Basipterygoid recesses on dorsolateral surfaces of basipterygoid processes: 0, absent; 1,

present.74. Braincase, accessory tympanic recess dorsal to crista interfenestralis: 0, absent; 1, small

pocket present; 2, extensive with indirect pneumatization.75. Braincase, prootic depression for pneumatic recess: 0, absent; 1, present as dorsally

open fossa on prootic/opisthotic; 2, present as deep, posterolaterally directed concavity.76. Braincase, subotic recess (pneumatic fossa ventral to fenestra ovalis): 0, absent; 1,

present.77. Braincase, preotic pendent: 0, absent; 1, present but small; 2 robust ORDERED (Turner,

2012, character 448).78. Braincase, posterior tympanic recess: 0, absent; 1, present as opening on anterior

surface of paroccipital process; 2, extends into opisthotic posterodorsal to fenestra ovalis, confluent with this fenestra.

79. Braincase, exits of C. N. X-XII: 0, flush with surface of exoccipital; 1, cranial nerve exits located together in a bowl-like depression.

80. Braincase, foramen magnum: 0, subcircular, slightly wider than tall; 1, oval, taller than wide.

81. Braincase, occipital condyle: 0, without constricted neck; 1, subspherical with constricted neck.

82. Supraoccipital, median ridge: 0, absent or low; 1, pronounced, strongly demarcated (Holtz 1998).

83. Basioccipital, basal tubera: 0, far apart, level with or beyond lateral edge of occipital condyle (connected by web of bone or separated by large notch); 1, small, directly below condyle, and separated by narrow notch.

84. Paroccipital process: 0, elongate and slender, with dorsal and ventral edges nearly parallel; 1, process short, deep with convex distal end.

85. Paroccipital process: 0, straight, projects laterally or posterolaterally; 1, distal end curves ventrally, pendant.

86. Paroccipital process: 0, with straight dorsal edge; 1, with dorsal edge twisted anterolaterally at distal end.

87. Vomer: 0, contacts premaxilla; 1, does not contact premaxilla (Turner, 2012, character 279).

88. Ectopterygoid: 0, with constricted opening into fossa; 1, with open ventral fossa in the main body of the element.

89. Ectopterygoid: 0, dorsal recess absent; 1, present.90. Pterygoid flange: 0, well developed; 1, reduced in size or absent.91. Palatine and ectopterygoid: 0, separated by pterygoid; 1, contact.92. Mandibles; 0, occlude for their full length; 1, diverge anteriorly due to kink and

downward deflection in dentary buccal margin.93. Mandible: 0, without coronoid prominence; 1, with coronoid prominence.94. Mandible, accessory mandibular condyle, lateral to lateral condyle of quadrate: 0,

absent; 1, present (Kobayashi and Lü, 2003).

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95. Mandibular fenestra: 0, heart-shaped with a short and wide process of the dentary at the anterior part of the external madibular fenestra; 1, oval shaped.

96. Dentary: 0, subtriangular in lateral view; 1, with subparallel dorsal and ventral edges.97. Dentary, dorsal border in transverse cross-section: 0, rounded and lacks "cutting edge";

1, sharp with "cutting edge"98. Dentary symphyseal region: 0, in line with main part of buccal edge; 1, symphyseal end

downturned leaving gap between upper and lower jaws.99. Dentary: 0, symphyseal region of dentary broad and straight, paralleling lateral margin;

1, medially recurved slightly; 2, strongly recurved medially.100. Dentary: 0, separate interdental plates; 1, interdental plates fused; 1, lost.101. Dentary, posterior end: 0, no posterodorsal process dorsal to external mandibular

fenestra; 1, dorsal process above anterior end of mandibular fenestra; 2, elongate dorsal process extending over most of fenestra.

102. Splenial forms notched anterior margin of internal mandibular fenestra: 0, absent; 1, present.

103. Splenial, posterior extent; 0, ends anterior to external mandibular fenestra; 1, extends posterior to middle of external mandibular fenestra (new character).

104. Coronoid ossification: 0, large; 1, only a thin splint; 2, absent.105. Surangular, laterally inclined flange along dorsal edge for articulation with lateral

process of lateral quadrate condyle: 0, absent; 1, present.106. Surangular, foramen in lateral surface of surangular anterior to mandibular articulation:

0, absent; 1, present; 2, enlarged into a fenestra.107. Surangular, foramen on dorsal edge dorsal to mandibular fenestra: 0, present; 1, absent.108. Surangular, posterior surangular foramen: 0, absent; 1, present.109. Angular: 0, exposed almost to end of mandible in lateral view, reaches or almost

reaches articular; 1, excluded from posterior end, angular suture turns ventrally and meets ventral border of mandible anterior to glenoid.

110. Angular, exposure on medial surface of mandible; 0, virtually none; 1, considerable along the ventral edge of mandible.

111. Articular, tall slender medial, posteromedial or mediodorsal process on retroarticular process: 0, absent; 1, present.

112. Articular, retroarticular process: 0, points posteriorly; 1, curves gently posterodorsally.113. Articular, retroarticular process: 0, short, stout; 1, rod-like, elongate and slender.114. Articular, mandibular articulation surface: 0, as long as distal end of quadrate; 1, two or

more times longer than quadrate surface, allowing anteroposterior movement of mandible.

115. Teeth: 0, constricted between root and crown; 1, edges of root and crown confluent.116. Teeth, premaxilla: 0, present; 1, absent.117. Teeth, premaxilla: 0, subequal to anterior maxillary teeth in size; 1, significantly

smaller.118. Teeth, premaxilla: 0, serrated; 1, unserrated.119. Teeth, premaxilla: 0, basal cross section sub-oval to sub-circular; 1, asymmetrical (J-

shaped in cross section) with flat lingual surface; 2, D-shaped. Ordered.120. Teeth, premaxilla, first tooth size compared with crowns of premaxillary teeth 2 and 3:

0, slightly smaller or same size; 1, much smaller; 2, much larger.

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121. Teeth, premaxilla: 0, second tooth approximately equivalent in size to other premaxillary teeth; 1, second tooth markedly larger than third and fourth premaxillary teeth.

122. Teeth, maxilla: 0, present; 1, edentulous.123. Teeth, maxillary tooth height: 0, highly variable with gaps evident for replacement; 1,

almost isodont with no replacement gaps.124. Teeth, maxilla and dentary: 0, serrated; 1, some without serrations anteriorly (except at

base in Saurornithoides mongoliensis); 2, all without serrations.125. Teeth, maxilla and dentary, tooth size: 0, large; 1, small (25-30 in dentary).126. Teeth, dentary teeth: 0, in separate alveoli; 1, set in open groove; 2, no sockets

(modified).127. Teeth, dentary: 0, present and ziphodont; 1, restricted to front, peglike and thin enamel;

2, absent.128. Vertebrae, anterior postaxial prezygapophyses: 0, straight; 1, anteroposteriorly convex,

flexed ventrally anteriorly (Turner, 2012, character 264).129. Vertebrae pneumatism: 0, cervicals only; 1, cervical centra and anterior dorsals but not

posterior dorsal vertebrae; 2, all presacral centra pneumatic.130. Vertebrae, cervical, axial neural spine: 0, flared transversely; 1, compressed

mediolaterally.131. Vertebrae, cervical, axis, epineurapophyseal processes (on either side of distal end of

neural spine): 0, absent; 1, present.132. Vertebrae, cervical, axial epipophyses: 0, absent or poorly developed, not extending

past posterior rim of postzygopophyses; 1, large and posteriorly directed, extend beyond postzygapophyses.

133. Vertebrae, cervicals, axial neural spine: 0, sheet-like; 1, anteroposteriorly reduced and rod-like (Turner, 2012, character 263).

134. Vertebrae, cervical, epipophyses: 0, distal on postzygapophyses above postzygopophyseal facets; 1, positioned proximal to postzygapophyseal facets.

135. Vertebrae, cervical centra, anterior: 0, posterior intercentral articulation level with or shorter than posterior extent of neural arch; 1, centra extending beyond posterior limit of neural arch.

136. Vertebrae, cervical, hypapophysis (carotid process) on posterior cervicals: 0, absent; 1, present.

137. Vertebrae, cervical, anterior centra: 0, subcircular or square in anterior view; 1, distinctly wider than high, kidney shaped.

138. Vertebrae, cervical neural spines: 0, anteroposteriorly long; 1, short and centered on neural arch, giving arch an 'X' shape in dorsal view.

139. Vertebrae, anteroposterior length of cervical neural spines: 0, more than 1/3 of neural arch length; 1, less than 1/3 of neural arch length (Pérez-Moreno et al., 1994).

140. Vertebrae, cervical centra: 0, one pair of pneumatic openings; 1, two pairs of pneumatic openings.

141. Vertebrae, cervical and anterior trunk vertebrae: 0, amphiplatyan; 1, opisthocoelous; 2, heterocoelous.

142. Vertebrae, dorsal, neural spines: 0, not expanded distally; 1, expanded to form 'spine table'.

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143. Vertebrae, dorsal, anterior trunk vertebrae: 0, with low hypapophyses (carotid processes); 1, with large, prominent hypapophyses.

144. Vertebrae, dorsal, parapophyses of posterior dorsals: 0, flush with neural arch; 1, distinctly projected on pedicels.

145. Vertebrae, dorsal, transverse processes of anterior dorsals: 0, long and thin; 1, short, wide, and only slightly inclined.

146. Vertebrae, dorsal, zygapophyses: 0, abutting above neural canal, opposite hyposphenes meet via lamina; 1, lateral to neural canal, separated by groove for interspinous ligaments, hyposphenes separate.

147. Vertebrae, sacral, number of sacrals: 0, 5 or less; 1, 6; 2, 7; 3, 8; 4, 9.148. Vertebrae, sacral, pleurocoels: 0, absent on sacral vertebrae; 1, present on some sacrals;

2, present on all sacrals.149. Vertebrae, sacral: 0, with unfused zygapophyses; 1, with fused zygapophyses forming a

sinuous ridge in dorsal view.150. Vertebrae, sacral; 0, ventral surface of posterior centra gently rounded, convex; 1,

ventrally flattened, sometimes with shallow sulcus; 2, centrum strongly constricted transversely, ventral surface keeled.

151. Vertebrae, caudal: 0, more than 40; 1, 25-40; 2, no more than 25; 3, very short tail.152. Vertebrae, caudal pygostyle: 0, not present; 1, two or more terminal caudals coossified.153. Vertebrae, caudal neural spines: 0, simple, undivided; 1, separated into anterior and

posterior alae throughout much of caudal sequence.154. Vertebrae, caudal: 0, caudal transition point distal to 10th caudal; 1, between the 7th and

10th vertebrae; 2, proximal to the 7th.155. Vertebrae, caudal, anterior centra: 0, tall, oval in cross section; 1, box-like in caudals I-

V; 2, centra laterally compressed with ventral keel.156. Vertebrae, caudal, neural spines on distal caudals: 0, form a low ridge; 1, spine absent;

2, midline sulcus in center of neural arch.157. Vertebrae, caudal, prezygapophyses of distal caudals: 0, 30-100% centrum length; 1,

long extensions of prezygapophyses (up to 10 vertebral segments long); 2, strongly reduced as in Archaeopteryx.

158. Vertebrae, caudal, midcaudal prezygapophyses: 0, extend less than one half centrum length; 1, extend more than one half but less than one centrum length (Kobayashi and Barsbold, 2005).

159. Haemal arches, anterior chevrons: 0, proximal ends short anteroposteriorly, shaft cylindrical or narrow blade; 1, proximal end elongate anteroposteriorly, flattened and plate-like.

160. Haemal arches, distal caudal chevrons: 0, anteriorly bifurcate; 1, bifurcate at both ends.161. Ribs, shafts of mid-cervical ribs: 0, slender and longer than vertebrae to which they

articulate; 1, broad and shorter than vertebrae.162. Ribs, ossified ventral (sternal) rib segments: 0, absent; 1, present.163. Ribs, ossified uncinate processes: 0, absent; 1, present164. Gastralia: 0, lateral gastral segment shorter than medial one in each arch; 1, distal

segment longer than proximal segment.165. Sternal plates: 0, unossified; 1, ossified (Turner, 2012, character 457).166. Sternum: 0, without distinct lateral xiphoid process posterior to costal margin; 1, with

lateral xiphoid process.

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167. Sternum: 0, anterior edge grooved for reception of coracoids; 1, sternum without grooves.

168. Sternum, articular facet for coracoid (conditions may be determined by the articular facet on coracoid in taxa without ossified sternum): 0, anterolateral or more lateral than anterior; 1, almost anterior

169. Scapula and coracoid, glenoid fossa: 0, faces posteriorly or posterolaterally; 1, laterally.170. Scapula and coracoid: 0, form a continuous arc in anterior and posterior views; 1,

coracoid inflected medially, scapulocoracoid 'L' shaped in lateral view.171. Scapula, acromion process of scapula: 0, large and projects perpendicular to scapular

shaft; 1, deep and broadly rounded; 2, pointed and extends in continuation of anterior edge of scapular blade.

172. Scapula, acromion process: 0, long, either tapering or horizontal triangle; 1, truncated, with deep base but short reach beyond scapular blade and squared-off profile. State 1 occurs in ornithomimids.

173. Scapula, acromion margin: 0, continuous with blade in anterior aspect; 1, anterior edge laterally everted relative to plane of scapular blade.

174. Scapula, acromion process: 0, straight; 1, laterally hooked tip (Turner, 2012, character 355).

175. Scapula, flange on supraglenoid buttress: 0, absent; 1, present.176. Scapula, depression on dorsal surface of supraglenoid buttress of scapula: 0,

weak/absent; 1, present.177. Coracoid, infraglenoid buttress: 0, allingned with posterioir process; 1, offset laterally

from line of posterior process (Kubayashi and Lü, 2003).178. Coracoid in lateral view: 0, subcircular, with shallow ventral blade; 1, subquadrangular

with extensive ventral blade; 2, shallow ventral blade with elongate posteroventral process; 3, 'strut'-like.

179. Coracoid, posterior edge: 0, not or only shallowly indented below glenoid; 1, posterior edge of coracoid deeply notched just ventral to glenoid, glenoid lip everted.

180. Coracoid, posterior process: 0, short; 1, long (Pérez-Moreno et al., 1994).181. Coracoid, biceps tubercle: 0, positioned close to base of posterior process; 1, positioned

more anteriorly (Kobayashi and Lü, 2003).182. Coracoid, posterolateral surface ventral to glenoid fossa: 0, unexpanded; 1, edge

expanded above triangular subglenoid fossa bounded laterally by enlarged coracoid tuber.

183. Coracoid, dorsal surface (= posterior surface of basal maniraptoran theropods): 0, strongly concave; 1, flat to convex (Turner, 2012, character 342).

184. Coracoid, medial surface, area of the foramen n. supracoracoideus (when developed): 0, strongly depressed; 1, flat to convex. (Turner, 2012, character 350).

185. Humerus, proximal end, head in anterior or posterior view: 0, strap-like, articular surface flat, no proximal midline convexity; 1, head domed proximally (Turner, 2012, Character 357)).

186. Humerus, ratio of width of proximal end to total length: 0, greater than 0.2; 1, less than 0.2 (Kobayashi and Lü, 2003).

187. Humerus, internal tuberosity: 0,, pointed; 1, expanded along humeral shaft with straight medial edge

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188. Humerus, deltopectoral crest, anterior view: 0, large with quadrangular proximal end; 1, less pronounced, forming an arc; 2, weakly developed with rounded edges; 3, long, rectangular 4, proximal end of humerus broad, triangular.

189. Humerus, deltopectoral crest, anterior surface: 0, smooth; 1, with distinct muscle scar near lateral edge along distal end of crest for insertion of biceps muscle.

190. Humerus, radial condyle: 0, larger than ulnar condyle; 1, approximately equal; 2, smaller.

191. Humerus, entepicondyle: 0, weak; 1, strong.192. Radius and ulna: 0, well separated; 1, with distinct adherence or syndesmosis distally.193. Radius/Humerus ratio: 0, more than 0.5; 1, less than 0.5 (Turner, 2012, Character 268).194. Ulna, distal articular surface: 0, flat; 1, convex, spherical surface.195. Carpus, lateral proximal carpal (ulnare?): 0, quadrangular; 1, triangular in proximal

view.196. Carpus: 0, two recognizable distal carpals in contact with metacarpals I, II; 1, single

principal distal carpal capping mc I and II or mc II and III.197. Carpus: 0, principal distal carpal semilunate in lateral view with trochlear proximal

surface; 1, discoid, with flat proximal surface.198. Carpus, distal carpal: 0, large, covering proximal ends of metacarpals I and II; 1, small,

covers base of metacarpal I and about half of II; 3, shifted to cover metacarpals II and III.

199. Metacarpal I: 0, less than 55% the length of metacarpal II; 1, 60-94%; 2, 95% or more (modified for ornithomimids).

200. Metacarpal I, distal end: 0, laterally rotated; 1 medially rotated (Pérez-Moreno and Sanz, 1995, pp. 115-117).

201. Metacarpal 1, distal end: 0, ginglymoid articulation with distinct condyles; 1, relatively large convex phalangeal articulation with reduced condyles (Pérez-Moreno and Sanz, 1995, pp. 115-117).

202. Metacarpal I and phalanx I-1 joint: 0, ginglymoid; 1, ginglymous articulation reduced on phalanx 1-1; 2, proximal articulation of I-1 is spherical, smooth.

203. Metacarpal I and II: 0, ginglymoid; 1, rounded; II ginglymoid and mc I shelf (Turner, 2012, character 213).

204. Metacarpal II: 0, shorter than metacarpal III; 1, longer than metacarpal III.205. Manus, phalanx I-1: 0, shorter than metacarpal II; 1, longer than metacarpal II.206. Manus: 0, tetradactyl; 1, tridactyl, or with less digits.207. Manus, phalanx I-1 shaft diameter compared with shaft diameter of radius: 0, less; 1,

greater.208. Manus, third digit: 0, phalanges present; 1, reduced to no more than metacarpal splint.209. Manus, third digit, (III3/III1+III2): 0, less than 1.0; 1, more than 1.0; 2, third finger lost

(Perez-Moreno et al., 1994).210. Manus, unguals: 0, strongly curved, with large flexor tubercles; 1, weakly curved with

weak flexor tubercles displaced distally from articular end; 2, straight with weak flexor tubercles displaced distally from articular end.

211. Manus, unguals with proximodorsal 'lip' (some, not all) - a transverse ridge immediately dorsal to the articulating surface: 0, absent; 1, present.

212. Iliac blades: 0, roughly vertical; 1, inclined dorsomedially, dorsal edges approach or meet each other above sacrum.

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213. Ilium, tuberosity along dorsal edge, dorsal or slightly posterior to acetabulum; 0, absent; 1, present.

214. Ilium, vertical midline ridge on lateral face above acetabulum: 0, absent; 1, present.215. Ilium, pubic and ischiadic peduncles: 0, of comparable anteroposterior lengths at ventral

ends; 1, pubic peduncle expanded, at least twice as wide as ischidiac peduncle.216. Ilium, supraacetabular crest: 0, as a separate process from antitrochanter, forms hood

over femoral head; 1, reduced, not forming hood; 2, absent.217. Ilium, supraacetabular shelf: 0, extends along most or all of the edge of the pubic

peduncle; 1, distinctly offset from acetabular edge of pubic peduncle.218. Ilium, antitrochanter posterior to acetabulum: 0, absent or poorly developed; 1,

prominent.219. Ilium, pubic peduncle articular facet: 0, flexed with two facets set at obtuse angle to

each other; 1, convex; 2, flat or concave.220. Ilium, pubic peduncle of ilium: 0, uniform in anteroposterior length (i.e. unexpanded) in

lateral view; 1, broadly flared toward pubic articular surface.221. Ilium, preacetabular ala, anterior end: 0, gently rounded or straight: 1, strongly convex,

lobate; 2, pointed at anterodorsal corner with concave anteroventral edge; 3, distinctly concave dorsally.

222. Ilium, preacetabular ala, anterior end: 0, straight or concave; 1, with notch at anterodorsal corner.

223. Ilium, preacetabular ala, ventral edge: 0, straight or gently curved; 1, with shallow, obtuse process; 2, process strongly hooked. Ordered.

224. Ilium, preacetabular ala, brevis fossa: 0, shelf-like; 1, deeply concave with lateral overhang.

225. Ilium, preacetabular ala, brevis fossa: 0, shallow with no lateral overhang, medial edge visible in lateral view; 1, well developed full length of postacetabular blade, lateral overhang along full length covers medial edge in lateral view.

226. Ilium, postacetabular ala, lateral view: 0, 'square'; 1, acuminate.227. Ilium, postacetabular ala, cuppedicus fossa: 0, deep, ventrally concave; 1, fossa shallow

or flat, with little or no lateral overhang; 2, absent. See (Hutchinson, 2001) for explanation of related changes in pelvic musculature.

228. Pubis, obturator foramen: 0, present; 1, open to become a notch between pubic shaft and ischiadic peduncle; 2, neither notch nor foramen present.

229. Pubis orientation: 0, propubic; 1, vertical; 2, opisthopubic (posteroventral).230. Pubis, shaft: 0, straight; 1, distal end curves anteriorly, anterior surface of shaft concave;

2, shaft curves posteriorly, anteriorly convex curvature.231. Pubis, apron (shelf on pubic shaft proximal to symphysis): 0, extends medially from

middle of cylindrical shaft; 1, shelf extends medially from anterior edge of anteroposteriorly flattened shaft.

232. Pubis, apron: 0, about half of pubic shaft length; 1, less than 1/3 of shaft length.233. Pubic boot: 0, projects anteriorly and posteriorly; 1, has little or no anterior process; 2,

no anteroposterior projections.234. Pubis, tip of anterior extension of pubic boot: 0, at the level of anterior border of pubic

shaft; 1, more extended anteriorly.235. Pubis, acute angle between pubic shaft and boot: 0, small; 1, large.

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236. Pubis, ventral border of pubic boot: 0, nearly straight or slightly convex; 1, strongly convex with ventral expansion.

237. Ischium to pubis length ratio: 0, more than two-thirds; 1, two-thirds or less of pubis length.

238. Ischium, acetabular rim: 0, convex or beveled; 1, with longitudinal sulcus or depression.239. Ischium: 0, slightly concave or flat proximal articular surface that contacts ilium; 1,

deep socket for reception of peg-like ischial peduncle of ilium.240. Ischium, scar on posterior edge of the proximal end of the ischium 0, absent; 1, present.241. Ischium, obturator process: 0, does not contact pubis; 1, contacts pubis.242. Ischium, obturator foramen: 0, present; 1, reduced to notch; 2, notch or foramen absent,

U shaped gap between pubic peduncle and obturator process.243. Ischium, obturator process: 0, absent; 1, proximal in position; 2, near middle of

ischiadic shaft; 3, at distal end of ischium.244. Ischium, obturator process: 0, square (with distinct posterior edge or notch); 1,

triangular with posterior end confluent with shaft.245. Ischium: 0, rod-like shaft distal to acetabulum; 1, wide, flat, and plate-like shaft.246. Ischium shaft: 0, roughly straight or only gently arced; 1, curves ventrodistally

anteriorly; 2, hooked posteriorly with deeply concave caudal margin.247. Ischium, lateral face of blade: 0, flat, round in rod-like ischia; 1, laterally concave; 2,

with longitudinal ridge subdividing lateral surface into anterior (including obturator process) and posterior parts.

248. Ischium, posterior edge: 0, straight; 1, with proximal median posterior process.249. Ischium, distal ends 0, form symphysis; 1, approach one another but do not form

symphysis; 2, widely separated.250. Ischium, boot (expanded distal end): 0, present; 1, absent.251. Femur/Humerus ratio: 0, more than 2.5; 1, between 1.2 and 2.2; 2, less than 1 (Turner,

2012, character 266).252. Femur, patellar groove: 0, absent; 1, present (Turner, 2012, character 415).253. Femur head: 0, fovea capitalis for attachment of capital ligament; 1, circular fovea

present in center of medial surface; 2, vertical ridges on anterior and posterior edges of medial surface of head.

254. Femur, lesser trochanter: 0, separated from greater trochanter by deep cleft; 1, trochanters separated by small groove; 2, completely fused (or absent) to form a trochanteric crest.

255. Femur, lesser trochanter: 0, alariform; 1, cylindrical in cross section.256. Femur, lesser trochanter height: 0, below height of greater trochanter; 1, level with or

dorsal to top of greater trochanter.257. Femur, lesser trochanter, vertical ridge on lateral face: 0, present; 1, absent.258. Femur, lesser trochanter, accessory trochanteric crest distal to lesser trochanter: 0,

absent; 1, present.259. Femur, lateral ridge: 0, absent or represented only by faint rugosity; 1, distinctly raised

from shaft, mound-like.260. Femur, fourth trochanter: 0, present; 1, absent.261. Femur, anterior surface of distal end of shaft proximal to medial distal condyle: 0,

without longitudinal crest; 1, crest extending from medial condyle.

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262. Tibia, lateral fossa of proximal end (incisura tibialis): 0, deeply notched; 1, wide and shallow, nearly absent.

263. Tibia, medial cnemial crest: 0, absent; 1, present.264. Fibula, medial surface of proximal end: 0, concave along long axis; 1, flat.265. Fibula, deep oval fossa on medial surface of fibula near proximal end: 0, absent; 1,

present.266. Astragalus and calcaneum: 0, separate from tibia; 1, fused to each other and to the tibia

in late ontogeny.267. Astragalus and calcaneum, condyles on distal ends: 0, separated by shallow, indefinite

sulcus; 1, distinct condyles separated by prominent tendinal groove on anterior surface.268. Astragalus, ascending process: 0, tall, extending proximally for at least a quarter of

tibia’s total length; 1, short, extending proximally for less than a quarter of tibia’s total length.

269. Astragalus, ascending process: 0, broad, covering anterior surface of distal tibia; 1, covering only lateral portion of anterior surface of distal tibia.

270. Astragalus, ascending process: 0, confluent with condylar portion; 1, separated by transverse groove or fossa across base.

271. Distal tarsals: 0, separate, not fused to metatarsals; 1, form metatarsal cap with intercondylar prominence that fuses to metatarsus early in postnatal ontogeny.

272. Metatarsus, shafts of major metatarsals: 0, not appressed against each other beyond proximal half; 1, appressed throughout most or all of metatarsus, adjacent surfaces of shafts flattened for contacts.

273. Metatarsus: 0, shaft of mt III with straight medial border in extensor view; 1, with medial expansion forming convexity or bulge along distal part of shaft.

274. Metatarsus, distal end of metatarsal III: 0, smooth, not ginglymoid; 1, with developed ginglymus.

275. Metatarsus, metatarsal I: 0, present; 1, absent (Turner, 2012, character 447).276. Metatarsus, mt I attachment on mt II: 0, middle of medial surface; 1, posterior surface of

distal quarter; 2, medial surface near proximal end; 3, mt I absent.277. Mt II, distal extent relative to MT IV: 0, approximately equal; 1, shorter than mt IV, but

reaching distally further than base of metatarsal IV trochlea; 2, shorter than mt IV, extending to base of mt IV trochlea. (Turner, 2012, #438).

278. Metatarsus, mt III: 0, exposed between mt II and mt IV along entire height; 1, proximal shaft constricted and narrower than mt II or mt IV, exposed along entire height, subarctometatarsal; 2, pinched, arctometatarsal; 3, prox part of mt III lost.

279. Metatarsus, mt III: 0, straight medial border in dorsal view; 1, with a medial expansion forming a convexity or bulge along distal part of the shaft.

280. Metatarsus, mt IV, large, longitudinal flange along posterior or lateral face: 0, absent; 1, present.

281. Metatarsus, mt IV shaft: 0, round or thicker dorsoventrally than wide in cross section; 1, mediolaterally wide and flat in cross section.

282. First pedal digit: 0, present; 1, absent.283. Length of pedal phalanx II-2: 0, more than 60% of pedal phalanx II-1; 1, less.284. Pedal ungual and penultimate phalanx of pedal digit II: 0, similar to those of III; 1,

penultimate phalanx highly modified for hyper-extension, ungual more strongly curved and significantly larger than that of digit III.

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285. Pedal unguals: 0, curved in lateral view, pointed; 1, straight with flat or concave bottoms but pointed tips; 2, flat or concave ventrally, broad and blunt tips.

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APPENDIX 2 – Character matrix used in the analysis and the coded character states. Dashes represent missing data, polymorphisms are indicated by A, (0,1) and B, (1,2)

10 20 30 40 50 60Allosaurus 0010110000 0000100000 1001000-10 0111001100 0010111000 0001001000Anserimimus -–01–––––– ––--–––––– –––––––––– –––––––––– –––––––––– ––––––––––Archaeornith. –––––––––– –––––––––– –––––––––– –––––––––– –––––––––– ––––––1–––Dilophosaurus 00000––0-– 00--000100 -0-0-00000 1-0-001-0- 00---00000 00-00000-0Gallimimus 1101001101 000021111- -100100000 1011-10001 00000-1000 0000011000Garudimimus –––0001100 000021–111 -010100000 00--000-01 00-01-100- 00000--11-Harpymimus 1–1––01-–– 0-0020-11- --0--0000- 1--------1 ----0---0- ----0-----Ornitholestes –1–01–1000 100001--01 0100-00-00 111-00000- 01-00-1000 1001-01001Ornithomimus 1111001101 0000211111 0010100000 1011010001 0000001010 0010011000Pelecanimimus 1–1–0–1-–– 0-002---00 -100--0-00 1--------0 -0----1-0- ––––––––––Shenzhousaurus –0––01–-–1 00002-1100 -000100000 --1---0001 ---000-000 00-–––––––Struthiomimus 1111001101 0000211101 -100100000 1011-10000 00000-1000 0010011--0Tyrannosaurus 0001000110 11-1000101 1001111100 1100001100 0100110011 2101100110UALVP 16182 –––––––––– –––––––––– –––––––––– –––––––––– –––––––––– ––––––––––

70 80 90 100 110 120Allosaurus 0100-00000 0010002010 1000000100 0000010000 00-001010- 000010-000Anserimimus -----1---- –––––––––– –––––––––– -------1-2 -––––––––– ––––––––––Archaeornith. –––––––––– –––––––––– ––0-–––––– –––––––––– ––––1-–––– –1-–––––––Dilophosaurus 0000-10000 000-00-0-0 0-0000---- -00--00000 00-000--0- 000010000-Gallimimus 2-11--1001 0100110100 00000011-0 1101001102 0--211010- 0100-1----Garudimimus 2011---001 01----0--- -0-00011-- 11011011-2 --121-1001 -10--1----Harpymimus –––––––––– –––––––––– –––––––––– -1-11001-0 ----1-000- -0--1-----Ornitholestes -100--0--- 00--1----- 000101-1-- -00--10000 0---0---0- 0000100110Ornithomimus 2--1-01001 01-011-100 000000---- -101101102 0-1-11101- 1100-1----Pelecanimimus ––1–-––––– –––––––––– –––––––––– -00--000-1 ----1---0- ----00011-Shenzhousaurus –––––––––– –––––––––– –––––––––– -101-0-001 0---1----- --0-11----Struthiomimus 2--1--100- 0--011010- --0000-1-0 1101101102 1--2111111 0100-1----Tyrannosaurus 1101-11110 0000002210 1100100100 0000010000 01-0020100 1000101020UALVP 16182 –––––––––– –––––––––– –––––––––– ----101--- ------11-- ––––––––––

130 140 150 160 170 180Allosaurus 0000000010 0110000000 1000000000 0010000000 00-11---00 1000000000Anserimimus –––––22-–– 0-------1- –––––0-––– –––––––1-– ––––––––0- -1--101-11Archaeornith. –––––2––11 00--101100 00000010-1 -000000-0- ––––––––00 -10--102-1Dilophosaurus -000000-10 01-00000-1 0101000000 0010000-00 ––––––––00 100-0--00-Gallimimus -1---22011 -00-101110 00000010-1 1000000100 100-----00 1100111211Garudimimus -1---22101 --0-----0- ------10-- –––––––––– –––––––––– ––––––––––Harpymimus ---2-01111 ------1-0- ------0--- –––––––0-– ––––0-–––– 11--110---Ornitholestes 10--00011- -----011-- 00100100-- --0-010--0 -––––––––– 1––--–––––Ornithomimus -1---22011 -00-101110 0000001001 1000000100 1001----00 1100100211Pelecanimimus 00-2110-0- ––0-–––––– –––––––––– –––––––––– ----0-00-- –––––––2-1Shenzhousaurus -1-2-01-0- –––––––––– 0–-–––0–-– --000---0- –––––––––– ––––––––––Struthiomimus -1---22-11 -0--101110 0000001001 100000010- 10010---00 1101110211Tyrannosaurus 0000000020 1110000-00 0000000100 10-0000100 0--11---00 0001000000UALVP 16182 –––––––––1 -00-1--10- ---01-10-1 --000--1-- –––––––10- 110011----

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190 200 210 220 230 240Allosaurus 0001000000 0000000-00 0000010000 0000000010 0011000100 0-01000000Anserimimus 11---002-2 11--001-20 121011-002 010010111- 0021100-00 -00--00111Archaeornith. 010-100202 0--0-0-111 0111-110-B -110-0101- 0--1000100 01100000-1Dilophosaurus -0----000- -0-0-0010- -0---00000 0000000000 0001002000 001---0000Gallimimus 11001A0202 A100000-11 1211110011 010010-110 0021100100 1000000011Garudimimus –––––––––– –––––––––– –––––1--–– -1-01--110 00--10--00 ---000----Harpymimus 01--1002-1 0100000010 0000110001 -1-0----10 -0---0-1-0 ––––––––1-Ornitholestes ----0-01-- -000------ ––––––0–-- -0-010--20 001101-100 ------0110Ornithomimus 01--110202 0100001-21 1211110012 0100101110 0021100100 1001110011Pelecanimimus –-–––––––– -100-01-11 0011110011 -––––––––0 ––-––––––– ––––––––––Shenzhousaurus –––––––––– –––––0–––– ---0-1-011 01-1101110 001101-100 10000000-1Struthiomimus 01--10020- 0100001-11 1211110011 010010-110 0021100100 000--10-11Tyrannosaurus 001110-10B A010-01-00 000-010120 0101011010 3121000101 0000000111UALVP 16182 –––––––––– –––––––121 1–––––––-1 0100101121 0021100100 00--1-00-1

250 260 270 280 285Allosaurus 0210000000 0000000100 1000000110 0000000000 00000Anserimimus 01110100-- –––––00--- -0-------- 0110130210 011–1Archaeornith. 011100000- -00000--01 000-000--1 0110---210 0––01Dilophosaurus 0-10000000 --0000-000 0100000110 0000-0-0-0 0––00Gallimimus 0111010000 1000000100 1-00100001 0110131210 01101Garudimimus -1--0-0--- -0---0---- –0–––––00– 0110001110 –0100Harpymimus ----010-00 -----0---- –––––––1–– 01001-0100 ––000Ornitholestes 0111-00000 10---0---- –0––-––––– 0100--00-0 –––––Ornithomimus 0111010000 1000000100 1000100001 011013-210 01101Pelecanimimus –––––––––– –––––––––– –––––––––– –––––––––– –––––Shenzhousaurus 0111000000 ---0000100 ---––––––– –––––––––– –––––Struthiomimus 0111010000 1000000100 10001000-1 0110132210 01101Tyrannosaurus 0211000111 0100110100 0000000001 01100002A0 00000UALVP 16182 0211010000 -000000100 1-00100001 0110132210 0–––1

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