22

Type area: ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN, map sheets 101 Eisenerz, 131 Kalwang and 132 Tro-faiach).

Type section: Not defined; typical outcrops are mentioned from the Sauerbrunn- and Weiritzgraben area (heritSch, 1931b; haberFelner & heritSch, 1932a).

Reference section(s): -

Derivation of name: Derived from the color and lithology.

Synonyms: -

Lithology: Black siliceous schists, alaun schists, lydites and rare intercalations of black limestones.

Fossils: Conodonts in limestone intercalations (FlaJS, 1964, 1967).

Origin, facies: Sapropelitic basinal sediments (Schön-laUb, 1982a).

Chronostratigraphic age: Silurian (Llandovery–Ludlow).

Biostratigraphy: amorphognathoides, sagitta and ploeck-ensis conodont zones.

Thickness: 50–80 m (SchönlaUb, 1982a).

Lithostratigraphically higher rank unit: -

Lithostratigraphic subdivision: -

Underlying unit(s): Crinoidal Limestone, Lydites, Arkoses, Schists (SchönlaUb, 1982a).

Overlying unit(s): Cavernous Banded Limestone.

Lateral unit(s): Intercalations of Black Lydites, Alaun Schists with the Orthoceratid Limestone are named “Misch fazies” (SchönlaUb, 1992).

Geographic distribution: E-GWZ; Styria, Eisenerzer Alpen.

Remarks: The graptolites described by heritSch (1931 b) and haberFelner & heritSch (1932a) from the Black Lydites, Alaun Schists were recognized as anorganic re-mains (gräF, 1966).

Complementary references: tollmann (1977), Schön-laUb (1979, 1980a), ebner et al. (1989), SchönlaUb & heiniSch (1993).

„Löchrige Bänderkalke“ / Cavernous Banded LimestoneFritz ebner

Validity: Invalid; not formalized working term (SchönlaUb, 1977b, 1982a).

Type area: ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN, map sheet 101 Eisenerz).

Type section: Not defined.

Reference section(s): -

Derivation of name: According to holes at the surface of the limestones due the weathering of pyrite.

Synonyms: Partim “Bunter Kalk” (SchönlaUb, 1982a).

Lithology: Well bedded and platy, grey sometimes red-dish, spotted limestone with characteristic, cm-sized holes at the surface.

Fossils: Conodonts, rare orthoceratids.

Origin, facies: Pelagic facies.

Chronostratigraphic age: Upper Silurian (Pridoli).

Biostratigraphy: -

Thickness: ~ 20 m.

Lithostratigraphically higher rank unit: -

Lithostratigraphic subdivision: -

Underlying unit(s): Black Lydites, Alaun Schists.

Overlying unit(s): Flaser Limestone.

Lateral unit(s): Lower Polster Limestones.

Geographic distribution: E-GWZ; Styria: Eisenerzer Al-pen.

Remarks: The lithology resembles the upper Silurian “Al-ticola/Megaerella Limestones” of the Carnic Alps (Schön-laUb, 1977b, 1982a). However, the Cavernous Banded Limestone was also compared with upper Devonian flaser limestones of the Carnic Alps (haberFelner, 1935).

Complementary references: Tollmann (1977), Schön-laUb (1980a), ebner et al. (1989), SchönlaUb & heiniSch (1993).

Flaserkalk / Flaser LimestonesFritz ebner

Validity: Invalid; informal working term (SchönlaUb, 1982a).

Type area: ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN, map sheets 101 Eisenerz and 131 Kalwang).

Type section: -

Reference section(s): -

Derivation of name: According to the lithology.

Synonyms: “Erzführender Kalk” (czermaK, 1931); “Bunter Flaser-Bänderkalk und geschieferter Kalk” (SchönlaUb, 1982a).

Lithology: a) in basal parts subordinate thin platy black limestones; b) variegated flaser- and banded limestones and reddish calcareous schists; c) within (b) occasionally layers of grey organodetritic limestones; d) stocks of meta-somatic siderite-ankerite mineralization.

Fossils: Conodonts, dacryoconarides (in b); c) crinoids and stromatoporoids.

Origin, facies: Pelagic environment; c) allodapic deposits.

Chronostratigraphic age: Lower Devonian: a) Lochkov-ian; b) Pragian–upper Emsian (middle Dalejeum).

Biostratigraphy: Based on conodonts.

Thickness: a) ~ 30 m; b) 200–250 m; c) 40 m.

Lithostratigraphically higher rank unit: -

Lithostratigraphic subdivision: -

Underlying unit(s): Cavernous Banded Limestone, Ortho-ceratid Limestone.

Overlying unit(s): -

Lateral unit(s): Lower and Upper Polster Limestone, Sau-berg Limestone, ? Massive Limestone.

Geographic distribution: E-GWZ; Styria, Eisenerzer Al-pen.

Remarks: -

Complementary references: tollmann (1977), Schön-laUb (1980a), ebner et al. (1989), SchönlaUb & heiniSch (1993).

Untere Polsterkalke / Lower Polster LimestoneFritz ebner

Validity: Invalid; informal working term (FlaJS & Schön-laUb, 1976).

23

Type area: Eisenerzer Alpen, Polster area; ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN, map sheet 101 Eisenerz).

Type section: Not designated; FlaJS & SchönlaUb (1976) presented a comprehensive description of a sec-tion along the track below the material lift from the foot station (N 47°31’52” / E 14°58’29”) to the Leobner Hütte (N 47°37’00” / E 14°57’42”), ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN, map sheet 101 Eisenerz).

Reference section(s): -

Derivation of name: After the mountain Polster (1,910 m; N 47°31’11” / E 14°58’28”), ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN; map sheet 101 Eisenerz).

Synonyms: “Untere Polsterkalke” (FlaJS & SchönlaUb, 1976); “Rötlicher Bankkalk vom Typus der Polsterkalke” (SchönlaUb, 1982a).

Lithology: At the section mentioned above from bottom to top (FlaJS & SchönlaUb, 1976):3 m bluish grey to violet sparry limestones (similar to the Silurian Orthoceratid Limestones; some meters of “Roh-wand” (= metasomatic ankeritic mineralization) intercalat-ed with 3–4 m greenish and violet schists. The bulk is made up of 45–50 m variegated limestones (light grey to pinkish flamed, ± bedded, weakly banded dense limestone with intercalation of dark, more sparry limestone). In the upper parts 5 m thick “Rohwand” and a band of green schists occur.

Fossils: Conodonts.

Origin, facies: Pelagic environment.

Chronostratigraphic age: (?) uppermost Silurian–lower-most Devonian (Lochkovian).

Biostratigraphy: Icriodus woschmidti – I. postwoschmidti Zone in the upper parts of the unit (FlaJS & SchönlaUb, 1976).

Thickness: Around 65–70 m; the upper variegated part: 45–50 m (FlaJS & SchönlaUb, 1976).

Lithostratigraphically higher rank unit: -

Lithostratigraphic subdivision: -

Underlying unit(s): Orthoceratid Limestone.

Overlying unit(s): Crinoid-Stromatoporoid Limestone.

Lateral unit(s): Flaser Limestones.

Geographic distribution: E-GWZ; Styria, Eisenerzer Al-pen.

Remarks: -

Complementary references: tollmann (1977), Schön-laUb (1979, 1980a, 1982a), ebner et al. (1989), SchönlaUb & heiniSch (1993).

Crinoiden-Stromatoporen-Kalke / Crinoid-Stromatoporoid Limestone

Fritz ebner

Validity: Invalid; informal working term (FlaJS & Schön-laUb, 1976).

Type area: Eisenerzer Alpen, Polster area, ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN, map sheet 101 Eisenerz).

Type section: Not designated; FlaJS & SchönlaUb (1976) presented a comprehensive description of a sec-

tion along the track below the material lift from the foot station (N 47°31’52” / E 14°58’29”) to the Leobner Hütte (N 47°37’00” / E 14°57’42”), ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN, map sheet 101 Eisenerz).

Reference section(s): -

Derivation of name: Named after the rock forming fossils.

Synonyms: “Crinoiden-Stromatoporen-Horizont” (FlaJS & SchönlaUb, 1976).

Lithology: Dm-bedded, light grey and weakly banded limestones made up of recrystallized fragments of stro-matoporoids (2–30 cm) within a sparry matrix of crinoidal detritus.

Fossils: Stromatoporoids, crinoids, conodonts.

Origin, facies: Allodapic limestones.

Chronostratigraphic age: Lower Devonian (Lochkovian– (?) Emsian) (FlaJS & SchönlaUb, 1976).

Biostratigraphy: -

Thickness: 10–40 m.

Lithostratigraphically higher rank unit: -

Lithostratigraphic subdivision: -

Underlying unit(s): Lower Polster Limestone (FlaJS & SchönlaUb, 1976); Flaser Limestones.

Overlying unit(s): Upper Polster Limestone, Flaser Lime-stones.

Lateral unit(s): -

Geographic distribution: E-GWZ; Styria, Eisenerzer Al-pen, Polster area.

Remarks: -

Complementary references: tollmann (1977), Schön-laUb (1979, 1980a, 1982a), ebner et al. (1989), Schön-laUb & heiniSch (1993).

Obere Polsterkalke / Upper Polster LimestoneFritz ebner

Validity: Invalid; informal working term (FlaJS & Schön-laUb, 1976).

Type area: Eisenerzer Alpen, Polster area, ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN, map sheet 101 Eisenerz).

Type section: Not designated; FlaJS & SchönlaUb (1976) presented a comprehensive description of a sec-tion along the track below the material lift from the foot station (N 47°31’52” / E 14°58’29”) to the Leobner Hütte (N 47°37’00” / E 14°57’42”); ÖK50-UTM, map sheet 4215 Eisenerz (ÖK 50-BMN, map sheet 101 Eisenerz).

Reference section(s): -

Derivation of name: After the mountain Polster (1,910 m; N 47°31’11” / E 14°58’28”) in the Präbichl area; ÖK50-UTM, map sheet 4215 Eisenerz (ÖK50-BMN, map sheet 101 Eisenerz).

Synonyms: -

Lithology: Light violet and pinkish-violet flaserlimestones and banded limestones with layers of up to 60 cm thick or-ganodetritic (stromatoporoids, crinoids) limestones in their lower parts. The uppermost parts, 4 m thick, consist of grey sparry limestone (FlaJS & SchönlaUb, 1976).

Legend

pelagic, offshore, siliciclastic

pelagic, nearshore, calcareous

shallow marin, neritic

terrestrial-continental, coarse clastic

terrestrial-continental, fine clastic

evaporite (chloride, sulphate)

rhyolite, dacite

(basaltic) andesite, trachyandesite

basalt

phyllite

mixed-facies (in corresponding colors)

coal (may include several seams)

position/age doubtful/controversial

equal units

older unit left \ younger unit right

hiatus

unconformity

GSSP

|

\

?

Fm. Formation

© Commission for the Palaeontological and Stratigraphical Research of Austria (CPSA) of the Austrian Academy of Sciencesand Austrian Stratigraphic Commission

Cutout and English adaptation of the "Die Stratigraphische Tabelle von Österreich 2004": Geological Survey of Austria

The Austrian Stratigraphic Chart 2004 - Paleozoic is a supplement of:Hubmann, B., Ebner, F., Ferretti, A., Kido, E., Krainer, K., Neubauer, F., Schönlaub, H.-P. & Suttner, T.J. (2014): The Paleozoic Era(them), 2nd edition. – In: Piller, W.E. [Ed.]: The lithostratigraphic units of the Austrian Stratigraphic Chart 2004 (sedimentary successions) – Vol. I –Abhandlungen der Geologischen Bundesanstalt, 66, 9–133, Wien.

Printing: Grasl Druck & Neue Medien GmbH, Bad Vöslau2014

Ls. Limestone

Austrian Stratigraphic Chart 2004 - Paleozoic(sedimentary successions)

Austrian Stratigraphic CommissionASC

EOL

53.7

44.6

27.7

56.8

60.2

251

PA

LE

OZ

OI

C

260

270

280

290

295

310

320

330

340

350

355

370

380

390

400

410

420

430

440

450

445

460

470

480

500

510

520

530

540542

CHANGHSINGIAN Dorashamian 2.8

CAPITANIAN 5.4

WORDIAN 2.2

ROADIAN 2.6

KUNGURIAN 5.0

ARTINSKIAN 8.8

SAKMARIAN 10.2

ASSELIAN 4.4

U. P

ER

MIA

NLO

PIN

GIA

N

WUCHIAPING-IAN Dzhulfian

6.6

GZHELIAN 4.9

KASIMOVIAN 2.6

MOSKOVIAN 5.2

BASHKIRIAN 6.4

SERPUKHOV-IAN 8.3

VISEAN 18.9

TOURNAISIAN 13.9

MID

. PER

MIA

NG

UADA

LUPI

ANL

OW

ER

PE

RM

IAN

CIS

UR

AL

IAN

U.

CA

RB

ON

IFE

RO

US

P

EN

NS

YL

VA

NIA

N

255

265

275

285

305

315

325

335

345

365

375

385

395

405

416

425

435

455

465

475

490

485

495

505

515

525

535

LO

WE

R

CA

RB

ON

IF

ER

OU

SM

IS

SI

SS

IP

PI

AN

FAMENNIAN 15.3

FRASNIAN 10.8

EIFELIAN 5.7

GIVETIAN 6.5

UP

PE

R

DE

VO

NI

AN

LO

WE

R

DE

VO

NIA

NM

IDD

LED

EV

ON

IAN

EMSIAN 9.5

PRAGIAN 4.2

LOCHKOVIAN 4.8

PRIDOLI 2.7

4.2

LLA

ND

OV

ER

YU

PP

ER

OR

DO

VIC

IAN

UP

PE

RC

AM

BR

IAN

MID

DLE

OR

DO

VIC

IAN

MID

DL

EC

AM

BR

IAN

LO

WE

RO

RD

OV

ICIA

NL

OW

ER

CA

MB

RIA

NLU

D-

LOW

WE

N-

LOC

K

5.5

12.1

DARRIWILIAN

6.8

3.7

7.2

5.1

9.7TREMA-DOCIAN

12.7

12.0

STAGE / AGE

SE

RIE

S /

EP

OC

H

SY

STE

M /

PE

RIO

D

ER

ATH

EM

/E

RA

TIM

E M

a

DU

RA

TIO

N M

a

CA

MB

RI

AN

OR

DO

VI

CI

AN

SI

LU

RI

AN

DE

VO

NI

AN

CA

RB

ON

IF

ER

OU

SP

ER

MI

AN

48

TELYCHIAN

15.5AERONIAN

RHUDDANIAN

HIRNANTIAN

LUDFORDIANGORSTIAN

HOMERIANSHEINWOOD.

Global Classification

359.2

299

Dalejian

Zlichovian

PAIBIAN

29.0

488.3

443.7

291

?

?

?

?

?

Höchkg.Formation

Do

rne

rko

ge

l F

orm

ati

on

Zach

ensp

itz F

m.

Sa

nd

st

on

es

Hahn-graben Formation

Graz Paleozoic

Remschnigg/Sausal

Southern Burgenland

Carboniferous of Nötsch

South Karavanke Mountains

Drau Range

Gurktal Nappe SystemEastern Greywacke ZoneWestern Greywacke Zone

Erl

ach

gra

be

n F

orm

ati

on

Ha

rrb

erg

er

Fm

.

Ha

cke

nst

ein

er

Fo

rma

tio

n

H a s e l g e b i r g e

Carnic Alps

Bode

nLi

mes

tone

B e l l e r o p h o nF o r m a t i o n

G r ö d e n F o r m a t i o n

Ta r v i s B r e c c i a

U p p e rP s e u d o s c h w a g e r i n aF o r m a t i o n

T r o g k o f e l L i m e s t o n e

G r e n z l a n d F o r m a t i o n

LowerPseudoschwagerinaFormat ion

A u e r n i g G r o u p

W a i d e g g F o r m a t i o n

Dim

on

Fo

rma

tio

n

Kir

chb

ach

Lim

est

on

e

Plo

tta

Lyd

ite

Kro

nh

of

Lim

est

on

eP

al

L

im

es

to

ne

Fe

ldko

ge

l L

ime

sto

ne

Ko

llin

kofe

l L

ime

sto

ne

Ma

rin

ell

i L

ime

sto

ne

Ke

lle

rgra

t R

ee

f L

ime

sto

ne

Cello

n Li

mes

tone

Frei

kofe

l Lim

esto

ne

Spin

otti

Ls.

Ga

msk

og

el

Lim

est

on

e

Vinz

Lim

esto

ne

Fin

de

nig

Lim

est

on

e

Hohe WarteLs. Ke

llerw

and

Lim

esto

ne

Mid

dle

and

Upp

erBi

scho

falm

Sha

les

Rauchkofel Limestone

Nö

lbli

ng

Fo

rma

tio

n

Ko

k F

orm

ati

on

Megaerella Ls.Alticola Limestone

Cardiola Fm.

Wo

laye

r L

ime

sto

ne

Ug

gw

a L

ime

sto

ne

Plöcken Formation

Ugg

wa

Shal

e

Him

mel

berg

Sand

ston

e

Fleo

ns

Gre

ywac

ke

Com

elic

oPo

rphy

ry

Va l V i s d e n d e F m .

Treßdorf Limestone

B e l l e r o p h o nF o r m a t i o n

G r ö d e n F o r m a t i o n

C l a s t i cT r o g k o f e lF o r m a t i o n

A u e r n i g G r o u p

R a t t e n d o r f F o r m a t i o n

Ho

chw

ipfe

l F

orm

ati

on

L i m e s t o n e s

Cardiola Fm.

Orth

ocer

atid

Lim

esto

ne

Alticola Ls.Cardiola Fm.

PlatyLimestone

Bro

nte

us

Lim

est

on

e

Lim

est

on

es,

Lyd

ite

sS

ha

le,

Lim

est

on

es

Se

ela

nd

Cri

no

ida

l L

ime

sto

ne

Se

eb

erg

Co

ral-

Cri

no

ida

l L

ime

sto

ne

Re

ef

L

ime

st

on

e

N o d u l a r L i m e s t o n e

“ U n t e r e S c h i c h t e n ”

C o q u i n aL i m e s t o n e s

Gr

öd

en

F

or

ma

tio

n

Sta

ng

no

ck F

orm

ati

on

Magdalensberg Group/Kaser Group/“Metadiabase”

Gol

zeck

For

mat

ion

Lowe

r Aue

nDo

lom

ite

Sch

att

loch

Ph

ylli

tes

No

ck G

rou

p

“Cla

stic

Gro

up

”M

ura

u G

rou

pM

urau

Lim

esto

ne (G

rebe

nzen

Lim

esto

ne)

Gu

rkta

l Q

ua

rtzp

hyl

lite

Co

mp

lex

Eis

en

hu

t G

rou

p

Sh

ale

, Ly

dit

e B

recc

ias

UpperAlthofenFormation

Uppe

rAu

en D

olom

ite

Alth

ofen

Lim

esto

ne B

recc

iaRo

sent

al

Form

atio

n

Mid

dle

Auen

Dolo

mite

Hai

der

Mar

ble

(Ade

lsber

g Li

mes

tone

)

Pran

ker M

etac

last

icsUr

sch

Dolo

mite

(K

aind

orf D

olom

ite)

Möl

blin

g Do

lom

iteLo

wer

Alth

ofen

Lim

esto

ne

Reef-debris Ls.of Althofen

Prä

bich

l For

mat

ion

Silb

ersb

erg

Form

atio

n

Gra

schn

itz F

orm

atio

n

Al

pi

ne

V

er

ru

cc

an

o

Tri

eb

en

ste

in F

orm

ati

on

Sunk

Form

atio

n

Ste

ilb

ach

Fo

rma

tio

n

Eis

en

erz

Fo

rma

tio

nC

rin

oid

al

Lim

es

ton

e

Lim

est

on

e B

recc

ia

Zö

bi

ng

F

or

ma

ti

on

Lower Paleozoicof Zöbing

Sc

ha

tt

be

rg

F

or

ma

ti

on

Do

lom

ite

s, F

lase

r L

ime

sto

ne

s

Sp

ielb

er

g

Do

lom

ite

Sc

hw

az

D

olo

mit

e

Kli

ng

lerk

ar

Fo

rma

tio

n

D o l o m i t e s

Lö

hn

ers

ba

ch F

orm

ati

on O

rthoc

erat

idLi

mes

tone

Do

lom

ite

s,

Lim

est

on

es

wit

h t

uff

s

C o n g l o m e r a t e s

Die

nte

n S

chis

ts

B l a s s e n e c k P o r p h y r y

Fla

ser

Lim

est

on

eS

au

be

rg

Lim

est

on

e

Schists,Lydites

Pla

tyL

ime

sto

ne

Up

pe

r P

ols

ter

Lim

est

on

e

Ma

ssiv

eL

ime

sto

ne

s

C r i n o i d -S t r o m a t o p o r o i dL i m e s t o n e

Ca

vern

ou

s B

an

de

dL

ime

sto

ne

Ra

d S

chis

ts

Fla

ser

Lim

est

on

es

Ort

ho

cera

tid

Lim

est

on

e

PolsterQuartzite

Cyst

oid

Lim

esto

ne

Red Sparitic Ls.

Volca

nics

Lydi

tes,

Ark

oses

, Sch

ists

Pete

rsba

umgr

aben

Fo

rmat

ion

Re

d P

hyl

lite

s

W i l d s c h ö n a u S c h i s t s

Quartzites

KalwangConglomerate

Gerichtsgraben Formation

Kaintal-graben Fm.

Lo

we

r B

isch

ofa

lm S

ha

leKehr

Fm

.

Ko

gle

r F

orm

ati

on

St.

Jako

b F

orm

ati

on

Köts

chbe

rg

Form

atio

n

Hube

nhal

t For

mat

ion

Bam

eder

-, He

igge

rFo

rmat

ion

Tasc

he

n F

orm

ati

on

Schö

ckel

Fm

.Ho

chsc

hlag

Fm

.S

chö

nb

erg

Fo

rma

tio

nS

em

ria

ch F

m.

Parmasegg Formation

Flös

serk

ogel

Fo

rmat

ion

Plab

utsc

h Fo

rmat

ion

Oss

er F

m.

Schw

eine

gg F

m.

Rotm

ülle

r Fm

.F

ah

rne

ck F

m.

Tyrn

auer

alm

Fm

.

Kolle

rkog

el

Form

atio

n

Hoc

hlan

tsch

Fm

.

Ste

inb

erg

Fo

rma

tio

nS

an

ze

nk

og

el

F

or

ma

ti

on

Bä

re

ns

ch

üt

z

Fo

rm

at

io

n

Uppe

r Car

boni

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