A GENETIC MARKER FOR COASTAL DIATOMS BASED ON PSBA
Transcript of A GENETIC MARKER FOR COASTAL DIATOMS BASED ON PSBA
A GENETIC MARKER FOR COASTAL DIATOMS BASED ON PSBA
Meghan E Chafee
A Thesis Submitted to the University of North Carolina Wilmington in Partial Fulfillment
of the Requirements for the Degree of Master of Science
Center for Marine Science
University of North Carolina Wilmington
2008
Approved by
Advisory Committee
Dr. Bongkeun Song
Dr. Lawrence B. Cahoon
Dr. Lynn Leonard
Dr. J. Craig Bailey
Chair
Accepted by
___________________________ Dean, Graduate School
TABLE OF CONTENTS
ABSTRACT ..........................................................................................................iv
ACKNOWLEDGEMENTS..................................................................................... v
LIST OF TABLES .................................................................................................vi
LIST OF FIGURES ..............................................................................................vii
CHAPTER 1: LITERATURE REVIEW .................................................................. 1
Environmental Sampling ............................................................................ 1
Diatoms...................................................................................................... 4
The psbA Gene.......................................................................................... 5
Biodiversity ................................................................................................ 8
Objective.................................................................................................. 11
CHAPTER 2: A GENETIC MARKER FOR MARINE DIATOMS BASED ON PsbA ............................................................................................ 12 INTRODUCTION ..................................................................................... 12
MATERIALS AND METHODS ................................................................. 14
Cultures......................................................................................... 14
Diatom Isolation ............................................................................ 15
DNA Extraction from Cultures ....................................................... 15
Environmental Samples ................................................................ 16
18S Sequence Generation............................................................ 16
Primer Design ............................................................................... 17
psbA Sequence Generation .......................................................... 18
Cloning.......................................................................................... 19
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Allelic Diversity .............................................................................. 19
Distance Analysis.......................................................................... 20
Phylogenetic Analysis......................................................................................... 20
DOTUR Analysis ........................................................................... 21
RESULTS................................................................................................. 22
Isolation and Analysis of Pure Cultures......................................... 22
18S rRNA and psbA Gene Comparisons ...................................... 24
Environmental Sampling ............................................................... 25
DISCUSSION........................................................................................... 26
Primer Specificity .......................................................................... 28
psbA Diversity ............................................................................... 24
CONCLUSIONS...................................................................................... 30
LITERATURE CITED............................................................................... 32
APPENDIX 1............................................................................................ 55
APPENDIX 2............................................................................................ 63
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ABSTRACT
Molecular ecological studies of marine diatoms have been hindered by the
lack of taxon-specific eukaryote genetic markers. Diatoms are among the most
abundant and diverse of all photosynthetic eukaryotes and account for nearly
25% of all global primary productivity. The ability of algae, and of diatoms in
particular, to quickly respond to a wide range of environmental parameters and
their position as the base of food webs make them prime sentinels of
environmental change. Recently a ‘universal’ psbA gene marker was developed
for environmental studies of photosynthetic prokaryotes and eukaryotes. The
objective of this study was to develop a diatom-specific eukaryotic gene marker
based on this ‘universal’ psbA marker to enhance ecological studies of marine
diatoms. Using nucleotide alignments of diatom psbA sequences, an
oligonucleotide primer was designed that amplifies diatoms along with some
other photosynthetic eukaryotes without the inclusion of homologous
cyanobacterial psbA genes. Comparison of psbA and 18S diatom sequences
from unialgal, non-axenic cultures confirms the use of psbA as an accurate
marker for resolving relationships within Phylum Bacillariophyta (diatoms). The
subsequent application of this modified psbA gene marker to environmental DNA
samples from the Cape Fear River Plume showed that primarily diatoms were
amplified from the environment. This marker proves useful in the detection of
highly resolved levels of diversity within Bacillariophyta.
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ACKNOWLEDGEMENTS
Special thanks goes to Kristine Sommer, one of the greatest resources at
the Center for Marine Science. I could not have completed this project without
her and I would not have learned all that I did if not for her patience and
dedication to taking care of her girls. I would also like to thank my lab mates,
Lyndsay Bell for always being so thoughtful, Cory Dashiell for keeping things light
and Erika Schwartz for keeping my cultures alive.
I would also like to thank my Wilmington and Charleston friends for their
encouragement and opportunities to blow off a little steam every now and then. I
must of course thank my family who still has no idea what it is that I do with DNA
but who nevertheless remain proud and supportive.
The National Science Foundation provided funding for this project. The
Coastal Ocean Research and Monitoring Program (CORMP) collected water
samples for this project from the Cape Fear River Plume.
Finally, I would like to thank my advisor Dr. Craig Bailey and my
committee members Drs. Lawrence Cahoon, Bongkeun Song and Lynn Leonard
for their dedication to teaching and for guidance and support throughout this
project.
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LIST OF TABLES
Table Page 1. Forward and reverse primer matrix.............................................................. 41
2. Putative species identifications for CMS diatom cultures ............................ 42
3. psbA allelic diversity for CMS01 (Cylindrotheca cloisterium) ....................... 43
4. psbA allelic diversity for CMS09 (Thalassiosira eccentrica)......................... 44
5. Diversity and predicted richness of the 18S rRNA gene and psbA ............. 45
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LIST OF FIGURES
Figure Page 1. Map of southeastern North Carolina........................................................... 46
2. Sequence chromatograms from cloned isolate CMS01 (Cylindrotheca
cloisterium) ................................................................................................. 47
3. Sequence chromatograms from cloned isolate CMS09 (Thalassiosira
eccentrica) .................................................................................................. 48
4. 18S rRNA gene parsimony phylogeny........................................................ 49
5. psbA parsimony phylogeny......................................................................... 50
6. 18S rRNA and psbA neighbor-joining phylogenies..................................... 51
7. Rarefaction analyses of 18S rRNA and psbA genes .................................. 52
8. Haplotype diversity of psbA sequences...................................................... 53
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CHAPTER 1: LITERATURE REVIEW
Environmental sampling
Ecological studies of microorganisms have resorted to a variety of
techniques to characterize natural assemblages. In the past, delineation of
community structure was based primarily on morphological identification of pure
cultures isolated from the environment. Identification of some microorganisms
requires that live specimens be examined (Butler and Rogerson 1995); however,
cultivation requirements of species widely vary and for many may not be feasible.
The lack of phenotypic traits available for reliable identification also hinders
comprehensive ecologically based studies of microorganisms. Microscopic
analysis at the bright field level is possible for some taxa (Flöder and Burns
2004), but often proves insufficient, and electron microscopy is subsequently
required for classification (Hoepffner and Haas 1990; Johnson and Sieburth
1982). Such techniques are feasible for larger protists that often have distinctive
characters (Andersen et al. 1996) but cannot be used to identify prokaryotes and
small eukaryotes, many of which share a nondescript round shape (Potter et al.
1997). Epifluorescence microscopy or flow cytometry is useful for estimates of
picoplankton abundance but cannot discriminate lower taxonomic levels (Lange
et al. 1996; Li 1994; Li et al. 1983; Simon et al. 1994). Pigment analysis by high-
performance liquid chromatography (HPLC) is widely used to estimate
abundance and diversity (Bidigare and Ondrusek 1996). Although this technique
is useful for generating estimations of biomass for major taxonomic groups based
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on pigment concentrations and their profiles, it does not have a sufficient
resolution for classifications below class levels (Mackey and Holdsworth 1998;
Zapata et al. 2000). Running blind HPLC analyses with no species level
taxonomic information from microscopic identification can result in significant
error where a major bloom species can be misidentified based on pigments alone
(Irigoien et al. 2004). Additionally, pigment concentrations vary among species
(Stolte et al. 2000) and environmental conditions (van Leeuwe and Stefels 1998)
resulting in inaccurate measures of biodiversity and abundance.
As a result of the above technological limitations, it was long suspected
that the biodiversity of microorganisms was inadequately characterized. Culture-
independent DNA sequencing and cloning methods made it technologically and
economically feasible to examine large numbers of sequences that make
ecological studies of microorganisms more meaningful. Giovannoni et al. (1990)
first sequenced 16S ribosomal RNA genes directly from environmental DNA
samples rather than from pure cultures, revealing many prokaryotic species
previously unknown. Since then numerous studies have discovered the
presence of many uncultured prokaryotes (DeLong 1992; Field et al. 1997;
Fuhrman et al. 1992; Moyer et al. 1995; Rooney-Varga et al. 1997), furthering
our understanding of prokaryotic abundance and distribution and their roles in
ecosystems (Fuhrman 2002; Pace 1997).
Ribosomal rRNA was the pioneering gene used extensively in the
detection of microbial diversity from natural communities. Prior to large-scale
eukaryote biodiversity studies, the 16S rRNA gene, designed to be specific for
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bacteria, was applied to environmental nucleic acid samples and resulted in the
amplification of eukaryotic plastid genes (Rappé et al. 1998), which share a
common phylogenetic origin with cyanobacterial (Wolfe et al. 1994). Several of
these plastid genes appeared to be novel phytoplankton lineages and the
molecular tools developed for prokaryotic diversity studies were finally applied to
eukaryotes. This lag can be attributed to the fact that for most protozoa and
microalgae, the defining species-specific morphological characters required for
identification are more obvious than those of prokaryotes, generating a sizeable
group of protistan morphological experts. Although many eukaryotic plankton are
large enough in size to examine with bright field microscopy, the discovery of
phototrophic picoeukaryotes led to a taxonomic challenge similar to that posed
by prokaryotes in which few conspicuous morphological characters are available
for identification (Potter et al. 1997). Since the application of the same
techniques used in prokaryotic studies, many novel eukaryotic lineages have
been uncovered using genetic markers, some of which represent new
phylogenetic lineages (Dawson and Pace 2002; Dièz et al. 2001; Edgecomb et
al. 2002; Guillou et al. 1999; Lopez-Garcia et al. 2001; Massana et al. 2002;
Moon-van der Staay et al. 2000; Moon-van der Staay et al. 2001; Rappé et al.
1998; Stoeck and Epstein 2003; Stoeck et al. 2003).
The expansion of molecular ecological studies has made it abundantly
clear that there exists a much larger amount of prokaryotic and eukaryotic
diversity than has been observed through the conventional techniques described
above. While morphological experts are becoming less common, large-scale
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studies of microorganism ecology are increasing in number, providing the public
databases needed to improve our understanding of interactions between
prokaryotic and eukaryotic communities and their bottom-up effects on higher
trophic levels.
Diatoms
Diatoms are among the most abundant and diverse group of all
photosynthetic eukaryotes. Found in all aquatic environments, these unicellular
chromophyte algae account for nearly half of total marine primary production
(Falkowski et al. 1998) and 25% of all global primary production (Field et al.
1998, Mann 1999). Diatoms (Phylum Bacillariophyta) are a unique group of
heterokont microalgae with a distinctive siliceous cell wall known as a frustule.
Generally diatoms are classified into two groups based on frustule symmetry:
centric and pennate forms. Centric diatoms are radially symmetrical and are
inclined to exhibit a planktonic lifestyle and pennate forms display bilateral
symmetry and tend to inhabit benthic microalgal assemblages. Raphid pennates
possess a raphe or slit through which mucilage is secreted as a substrate to glide
upon. Araphid pennates are bilateral but do not have a raphe (Falciatore and
Bowler 2002; Round et al. 1990).
The importance of diatoms cannot be overemphasized; they have
traditionally been used in many different scientific sub-disciplines. For example,
high-resolution stratigraphic analyses and species abundances for fossil diatoms
are key tools for developing paleolimnological-based reconstructions of past
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biodiversity, trophic status and broad-scale climate change (Bigler and Hall 2002,
2003; Finkel et al. 2005; Smol et al. 2005; Wolfe 2003). Assemblages of extant,
attached diatoms are increasingly being used as biological reporters for
assessing trophic status and water quality in freshwater and coastal marine
systems (de la Rey et al. 2004, Poulíčková et al. 2004; Reavie and Smol 1998;.
Previous studies have demonstrated that diatoms are sensitive and respond
rapidly to changes in nutrient availability and are accurate predictors of other
water quality variables (e.g., chlorophyll a content: Cunningham et al. 2005;
Reavie and Smol 1998; Vaultonburg and Pederson 1994). For these reasons,
diatom indexes are useful monitors of eutrophication and other environmental
change (McCormick and Cairns 1994, Weckström and Juggins 2005, de la Cruz
et al. 2006). The development of more specific eukaryotic gene markers has
potential to improve molecular ecology studies of diatoms that are often
employed in water quality assessment and monitoring programs where the
presence or absence of particular diatom species have been correlated to
specific environmental parameters.
The psbA gene
The lag in development of species-specific eukaryotic genetic markers has
led to a current deficit in eukaryotic environmental sampling studies, thereby
inhibiting the development of large-scale ecologically-based comparisons.
Ribosomal RNA (rRNA) genes are found universally in all organisms and have
widely been used in the past to characterize evolutionary relationships (Woese
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1987). The rRNA molecules show a high degree of functional constraint among
lineages, which allows for the comparison of evolutionary relationships across
phyla. Although much of the rRNA sequence is conserved, many regions of this
gene vary at different positions and at very different rates among species
providing a more resolved phylogeny of closely related organisms (Woese 1987).
The rRNA gene has proven highly versatile in the types of phylogenetic and
ecological analyses that can be performed. However, rRNA sequence
divergence may not be capable of distinguishing between two closely related
species that are only subtly different from one another. Alternative genetic
markers such as the chloroplast-encoded genes could prove useful in revealing
eukaryotic genetic diversity not detected by 18S rRNA, specifically in
photoautotrophic plankton.
In addition to ribosomal RNA, the ribulose bisphosphate
carboxylase/oxygenase enzyme (RUBISCO), encoded by the rbcL plastid gene,
has been employed in studies of microbial ecology as part of a quantification of
gene expression in the water column (Paul et al. 1999; Pichard and Paul 1991;
Pichard et al. 1993; Pichard et al 1996; Pichard et al. 1997a; Wawrik et al. 2002;
Xu and Tabita 1996). Studies involved in the detection of rbcL diversity in natural
phytoplankton communities, however, are limited in number as well as scope
(Pichard et al. 1997b; Xu and Tabita 1996).
The psbA gene used in this study encodes the D1 protein of photosystem II in all
oxygenic photosynthesizers. Literature regarding psbA in algae is scarce,
however, the nature of this gene could prove useful in a higher resolution
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analysis of more cryptic genetic diversity of photosynthetic organisms. D1 and
D2 proteins form the reaction center heterodimer of PSII (Nanba and Satoh
1986) where oxygen evolution takes place (reviewed in Debus 1992). The D1
protein of photosystem II is continually damaged by light (photoinhibition)
(Osmond et al. 1993). The rapid, light-dependent turnover of D1 replaces
damaged proteins (Kyle 1987), serving as an important response to light stress in
plants and algae.
Zeidner et al. (2003) recently developed a “universal” genetic marker for
psbA that amplifies the D1 protein from prokaryotic cyanobacteria and eukaryotic
algae within environmental DNA samples. Comparison of psbA genes with
nuclear small subunit rRNA genes through use of environmental bacterial
artificial chromosome (BAC) libraries affirmed the phylogenic association
(Zeidner 2003). With support of psbA accuracy, Zeidner et al. (2003) applied this
photosynthetic marker to marine environmental DNA and subsequently amplified
psbA fragments from photosynthetic eukaryotes and cyanobacteria. The
advantage to using psbA instead of rRNA genes is that it eliminates heterotrophs
from analysis and focuses instead on the photoautotrophs. Such a marker could
be particularly beneficial in the ecological study of eukaryotic algae whose
nutritional requirements and role as primary producers make them unique
sentinels of environmental change and overall ecosystem health (McCormick and
Cairns 1994).
The primary practical impediment to employing psbA in a photosynthetic
eukaryote biodiversity study is excluding homologous sequence data from
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prokaryotic cyanobacteria. Cyanobacteria are ubiquitous and numerous in
marine and freshwater environments. Because photosynthetic eukaryotes
derived their chloroplast genome endosymbiotically from a photosynthetic
prokaryote (Wolfe et al. 1994), obtaining a sufficient number of eukaryotic algal
genes through direct sequencings methods from environmental DNA requires
many rounds of cloning. An ideal photosynthetic eukaryote psbA marker would
also eliminate the amplification of cyanobacterial DNA, allowing for a more direct
assessment of the biodiversity of algal assemblages.
Biodiversity
An ongoing debate within scientific communities is the question regarding
the extent of microorganism dispersal and ubiquity. Because of their high
dispersal capabilities and lack of formidable boundaries, microorganisms in
general exhibit an overall low species richness compared to larger organisms
that are more confined to spatial niches (Finlay and Clarke 1999; Finlay 2002).
It was in the nineteenth century that Baas Becking first formulated the hypothesis
that with respect to microorganisms, ‘everything is everywhere, but, the
environment selects’ (Baas Becking 1934). In other words, there is a large
‘seedbank’ of organisms subjected to random global dispersal that subsequently
proliferate wherever conditions are suitable for growth (Finlay 2002). Under this
hypothesis, species samples taken from opposite corners of the world, but with
similar environmental conditions, would be identical. Perhaps microorganism
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genetic differentiation must be examined at a more resolved level in order to
determine the extent of their ubiquity and ecological plasticity (Sarno et al. 2005).
Although microorganisms tend to exhibit wide-ranging dispersal, genetic
and ecological differentiation is becoming more apparent with the application of
appropriate genetic markers and a reexamination of cryptic morphological
characteristics. It has recently been suggested by Sarno et al. (2005) that the
easily identified diatom Skeletonema costatum actually consists of more than one
distinctive morphological species as revealed by light microscopy and scanning
and transmission electron micrograph. Out of eight specimens examined, four
main morphological groups were identified (Sarno et al. 2005). Specimens
belonging to the same morphological species shared identical large subunit
(LSU) rRNA sequences with similar or identical small subunit (SSU) rRNA
sequences. Even though SSU and LSU maximum likelihood phylogenies were
in agreement, their similar topologies may be a result of their close proximity
within rDNA cistrons. Sarno et al. (2005) recommends that phylogenies from
unrelated DNA regions, such as mitochondria or plastid genes, are needed to
confirm patterns revealed by these ribosomal genes. In addition to
morphological and phylogenetic differentiation, variations in seasonal
distributions were found among the species examined, indicating that this
“cosmopolitan” diatom is actually composed of many species that are
differentially selected upon by the environment, confining them to spatial niches.
Samples were collected from a small portion of the Skeletonema costatum
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spatial distribution; there likely remains a higher level of diversity within this
species yet to be uncovered.
Sarno et al. (2005) found genetic and morphological differentiation among
geographically distant populations, however, a study by Rynearson and Armbrust
(2004) found substantial genetic differentiation among populations of the diatom
Ditylum brightwellii within the connected estuaries of the Strait of Juan de Fuca
and Puget Sound (WA, USA). The three genetically distinct populations were
identified by different microsatellite allele distributions and unique alleles.
Isolates from the two most genetically diverged species had identical nuclear 18S
rRNA sequences, indicating a close evolutionary relationship; however, isolates
from two of the populations examined in this study exhibited different
physiological capabilities (i.e., growth rates), suggesting differential selection. In
this particular region, the recirculation of waters within Puget Sound created the
‘geographical barrier’ required for genetic and physiological divergence between
these two populations of diatoms despite their close proximity (Rynearson and
Armbrust 2004). In this study microsatellites were able to detect a level of
diversity not found by 18S rRNA. Although microsatellites are extremely useful in
resolving relationships within species, development can be time consuming. The
direct use of a gene marker is likely to be more efficient and can be more broadly
applied.
Although morphology remains important to the study and classification of
microorganisms, DNA sequencing methods have provided the ultimate
examination of interspecific genetic variation at the level of nucleotide base pair.
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Furthermore, the manipulation of bacteria to separate and clone DNA fragments
has exposed genetic variation within single isolates, potentially revealing multiple
gene haplotypes within a single species. Skeletonema costatum is broadly
distributed and has been extensively studied for more than a century (Sarno et
al. 2005), yet in addition to newfound genetic differentiation, new morphological
characters are still presenting themselves after many microscope hours. With
the use of more appropriate biodiversity gene markers such as psbA,
environmental sampling could prove to be a powerful tool to expose extant levels
of microorganism ubiquity and diversity on a global scale.
Objective
The primary objective of this project is to develop a diatom-specific
eukaryotic genetic marker based on the membrane-encoded psbA gene that can
be applied to ecological studies of coastal diatoms.
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CHAPTER 2: A GENETIC MARKER FOR MARINE DIATOMS BASED ON psbA
INTRODUCTION
Development of taxon-specific prokaryotic genetic markers has preceded
that of the eukaryotes by nearly a decade. In general, prokaryotes are very small
(0.2-2 μm) in size with a nondescript round shape (Potter et al. 1997), many of
which cannot be cultured in the laboratory. For most protozoa and microalgae,
the defining species-specific morphological characters required for identification
are more obvious than those of prokaryotes. The discovery of picoeukaryotes
(0.2-2 μm), however, posed a similar taxonomic challenge where convergent
evolution has resulted in similar phenotypes among distantly related eukaryotic
taxa (Potter et al. 1997).
The recent application of 18S rRNA gene markers to environmental DNA
has revealed many novel eukaryotic lineages (Dawson and Pace 2002; Dièz et
al. 2001; Edgecomb et al. 2002; Guillou et al. 1999; Lopez-Garcia et al. 2001;
Massana et al. 2002; Moon-van der Staay et al. 2000; Moon-van der Staay et al.
2001; Rappé et al. 1998; Stoeck and Epstein 2003; Stoeck et al. 2003). Nearly
every environmental eukaryotic study to date has employed the 18S rRNA gene
marker for assemblage characterization. The 18S rRNA gene is useful in
determining community structure of both heterotrophic and autotrophic
eukaryotes but a genetic marker specific to photoautotrophs would enhance
ecological studies of marine microalgae.
The rbcL gene, which codes for the ribulose bisphosphate
carboxylase/oxygenase enzyme (RUBISCO) responsible for carbon fixation, has
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also been applied to environmental DNA samples. Studies employing RUBISCO
focus largely on the quantification of gene expression of photosynthetic plankton
within the water column (Paul et al. 1999; Pichard and Paul 1991; Pichard et al.
1993; Pichard et al 1996; Pichard et al. 1997a; Wawrik et al. 2002; Xu and Tabita
1996), although some have examined diversity of the rbcL gene in the natural
phytoplankton community (Pichard et al. 1997b; Xu and Tabita 1996). The rbcL
gene, however, has not been employed is any large-scale investigations of
diversity.
Molecular ecological studies of marine diatoms have been hindered by the
lack of taxon-specific eukaryote genetic markers. Diatoms are among the most
diverse of all photosynthetic eukaryotes and account for nearly 25% of all global
primary productivity (Field et al. 1998, Mann 1999). Their characteristic siliceous
frustules preserve well in sediments providing indispensable tools for developing
paleolimnological-based reconstructions of past biodiversity, trophic status and
broad-scale climate change (Bigler and Hall 2002, 2003; Wolfe 2003; Finkel et al.
2005; Smol et al. 2005). The ability of diatoms to quickly respond to a wide
range of environmental parameters and their position at the base of food webs
make them prime sentinels of environmental change (McCormick and Cairns
1994; Weckström and Juggins 2005; de la Cruz et al. 2006). Diatoms have been
employed in environmental monitoring and assessment programs in freshwater
and coastal marine systems (Reavie and Smol 1998; de la Rey et al. 2004,
Poulíckovã et al. 2004). The development of genetic markers that specifically
target this important and diverse group has potential to reveal ecological
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information that is central to their use as monitors of environmental change (e.g.,
eutrophication), particularly in coastal regions where nutrients are delivered in
pulses by rivers.
Zeidner et al. (2003) developed a “universal” genetic marker for the
membrane-embedded psbA gene that amplifies all oxygenic photosynthesizers,
including phototrophic cyanobacteria and eukaryotic algae. The ubiquity of
cyanobacteria in the marine environment complicates biodiversity studies of
eukaryotic algae. Direct application of psbA to environmental samples results in
a clonal library composed primarily of cyanobacteria.
In this study, I developed a new set of psbA gene primers based on those
developed by Zeidner et al. (2003) such that eukaryotic algae are amplified from
pure culture and the environment but cyanobacteria are now eliminated from
clone libraries. When applied to study site CFP6 in the Cape Fear River Plume
off southeastern coastal North Carolina, this modified psbA gene primarily
amplified diatoms from river plume waters. This genetic marker, based on the
psbA gene, is a useful for estimations of biodiversity and proves itself as a
suitable marker for phylogenetic studies of diatoms (Phylum Bacillariophyta).
MATERIALS AND METHODS
Cultures
A total of 30 pure cultures were examined in this study. Six diatom
cultures were obtained from The Provasoli-Guillard National Center for Culture of
Marine Phytoplankton (CCMP, Bigelow, ME, USA) (Appendix 1). Twenty-four
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cultures from other photosynthetic eukaryotes were obtained from CCMP, UTEX
(University of Texas at Austin, TX, USA), SCCAP (The Scandinavian Culture
Centre for Algae and Protozoa, Copenhagen, Denmark), SAG (Culture Collection
of Algae at the University of Göttingen, Göttingen, Germany), MBIC (Marine
Biotechnology Institute Culture Collection, Japan), PCC (Pasteur Culture
Collection of Cyanobacteria, France), NIEHS (The National Institute of
Environmental Health Sciences, NC, USA) and CCAP (Culture Collection of
Algae and Protozoa, Scotland, UK) (Appendix 2).
Diatom isolation
Additional diatoms were isolated from the Intracoastal Waterway at the
University of North Carolina’s Center for Marine Science (CMS) (Fig. 1). In total
46 single diatom cells were isolated under an Olympus Bx60 microscope with a
capillary pipette and grown into unialgal, non-axenic cultures in f/2 media at room
temperature (~25°C) (Appendix 1).
DNA extraction from cultures
Diatom cells from CMS/ICW cultures and CCMP culture collections were
harvested by centrifuging at 14,000 rpm and total cellular DNA was extracted as
described by Bailey et al. (1998).
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Environmental samples
Five liters of benthic (~10 m depth) and surface water samples were
collected on 13 June 2007 from the Cape Fear River Plume site CFP6 (Fig. 1).
Water was filtered through 0.45-μm non-sterile Nalgene membrane filters to
collect planktonic biomass and stored at -80°C. DNA was then extracted from
filters as described above.
18S sequence generation
The 18S rRNA gene was amplified from the six diatom cultures from CCMP and
for 34 of the 46 unialgal, non-axenic CMS cultures for comparison with diatom
psbA sequences. PCR reactions were performed in 50 μL volumes with 10 μL of
5X Green GoTaq Reaction Buffer (Promega, Madison, WI), 1 μL 10mM dNTP
(Promega), 0.5 μL 10 μM of the forward and reverse primers, 1.25 units of
GoTaq (Promega), 36.75 μL sterile distilled water and 1 μL DNA template. The
PCR thermocycling program included an initial denaturing step at 94 °C for 4
min, followed by 40 cycles of DNA denaturation at 94 °C for 30 s, primer
annealing at 50 °C for 1 min and fragment extension at 72 °C for 1.5 min. Final
extension ran for an additional 7 min at 72 °C. PCR products were then purified
using StrataPrep PCR Purification Kit (Stratagene, La Jolla, CA) according to the
manufacturer’s instructions.
Partial 18S RNA gene sequences were generated from cleaned PCR
products using BigDye v3.1 Terminator Sequencing Kits (ABI, Foster City, CA)
determined on a 3130 xl Genetic Analyzer (ABI). All sequences were edited in
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Sequencher 4.7 (Gene Codes Corp., Ann Arbor, MI) automatically aligned using
ClustalX (Thompson et al. 1994) and edited by eye in MacClade 4.0 (Maddison
and Maddison 2000). Hypervariable regions were excluded from analysis.
Primer design
Diatom specific primer design based on psbA was initiated by comparing
the psbA gene sequences from the complete chloroplast genomes of diatoms
Odontella sinensis (GenBank Acc. No. Z67753), Phaeodactylum tricornutum
(GenBank Acc. No. EF067920) and Thalassiosira pseudonana (GenBank Acc.
No. EF067921) and from the six diatom CCMP cultures. Eight additional diatom
psbA sequences from Onslow Bay were added and aligned from a previous
study (unpublished data) to aid in primer development. Based on a visual
comparison of conserved regions, a matrix of six forward and six reverse
degenerative primers (Table 1) were tested using diatom cultures from CCMP.
Application of primer combination dF11 (5’- GGT ATT CGT GAG CCT
GTT GC -3’) and dR12 (5’- CCT CCA TAC CTA AAT CAG CAC -3’) to diatom
cultures resulted in positive PCR bands for all cultures. Cloned fragments from
diatom cultures were PCR amplified and sequenced in the forward and reverse
direction. Contigs were BLASTed in GenBank and those closely resembling
diatom sequences were maintained and aligned with previously determined
diatom psbA sequences. The dF11/dR12 primer set was then applied to
environmental DNA from CFP6 and a clonal library was generated.
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With a suite of diatom psbA sequences available, primer specificity was
further streamlined. A second primer combination dsF (5’-GAT TGG TTR AAG
TTG AAA CC-3’) and dsR (5’-AGG TTC TTT ATT ATA YGG TAA-3’)] was
designed that directly amplified CCMP diatom cultures and CMS/ICW diatom
isolates in culture with cyanobacteria without cloning. dsF/dsR primers were
then applied CFP6 environmental samples and a second clonal library was
generated.
psbA sequence generation
The psbA gene was amplified from the six diatom cultures from CCMP, for
all 46 CMS cultures and for the 24 other photosynthetic eukaryote cultures. PCR
amplification and purification of psbA by the dF11/dR12 primer combination was
performed the same as described above for the 18S rRNA gene. A gradient
PCR amplification of the dsF/dsR primer combination showed an annealing
temperature at 45 °C for 1 min to be optimal for this set of primers but all other
thermocycle conditions were the same as described above.
Partial psbA gene sequences were generated from cleaned PCR products
using BigDye v3.1 Terminator Sequencing Kits (ABI, Foster City, CA) determined
on a 3130 xl Genetic Analyzer (ABI). All sequences were edited in Sequencher
4.7 and manually aligned in MacClade 4.0.
18
Cloning
PCR products of the psbA gene were cloned using pGEM-T Easy Vector
Systems Kit (Promega) according to manufacturer’s instructions. Positive
colonies were picked, boiled in 25 μL of distilled water at 99 ºC for 5 min, and
amplified as follows for the dF11/dR12 primer set: initial denaturing step at 95 °C
for 15 min, followed by 35 cycles of DNA denaturation at 94 °C for 1 min, primer
annealing at 50 °C for 1 min and fragment extension at 72 °C for 2 min. Final
extension ran for an additional 7 min at 72 °C. Clones generated from the
dsF/dsR primer set were amplified under the same conditions as above with the
exception of a lower annealing temperature at 45 °C for 1 min. All clonal PCR
products were cleaned using StrataPrep PCR Purification Kit.
Allelic diversity
Two diatom cultures, pennate CMS01 (Cylindrotheca closterium) and
centric CMS09 (Thalassiosira eccentrica), were chosen for analysis of psbA
allelic diversity. A brightline hemacytometer (Sigma, St. Louis, MO, USA) was
used to determine cell counts of each culture. DNA was extracted from ~335,000
cells of each culture for comparison of allelic diversity between species with
different numbers of chloroplasts. PCR amplification, cloning and sequencing
was carried out as described above for the dsF/dsR primer set. Partial psbA
sequences were edited and manually aligned. Segregating sites found in psbA
alignments for the two species were visually confirmed by sequence
chromatograms. Because the sequences were generated in the forward and
19
reverse direction, the changes observed in the alignment could be seen in the
raw sequence data in both directions.
Distance analysis
All psbA sequences used in analyses were generated with the dsF/dsR
primer. Partial 18S rRNA gene and psbA diatom sequences from CMS and
CCMP diatom cultures and GenBank sequences were edited and maintained in
separate alignments. Neighbor-joining trees were generated for each gene using
an uncorrected-p distance and 10,000 neighbor-joining bootstrap replicates.
Partial psbA sequences from CFP6 clonal library, CMS and CCMP diatom
cultures, GenBank diatom sequences and other photosynthetic eukaryote
reference sequences were edited and manually aligned. All analyses in this study
were performed in PAUP* 4.0b10 (Swofford 2002). A neighbor-joining (Saitou
and Nei 1987) psbA haplotype diversity was generated using an uncorrected-p
distance and 1000 neighbor-joining bootstrap replicates.
Phylogenetic analyses
Partial 18S rRNA gene and psbA sequences from CMS diatom isolates
were edited and aligned. Parsimony, maximum likelihood and neighbor-joining
analyses of the 18S rRNA gene and psbA alignments were performed.
Maximum parsimony analyses were generated using a full heuristic search with
10 random sequence additions and TBR branch swapping. ModelTest (Posada
and Crandall 1998) was used to generate the best-fit model of molecular
20
evolution for the maximum likelihood analyses. The model used for the 18S
rRNA gene was TrN (Tamura-Nei: Tamura and Nei 1993) with a proportion of
invariable sites (=0.4982) and with a gamma distribution (α=0.5145). The model
used for psbA was GTR (General Time Reversible: Lanave et al. 1984) with a
proportion of invariable sites (=0.6384) and with a gamma distribution
(α=1.1035). Maximum likelihood bootstrap values were generated using 100 fast
stepwise additions.
DOTUR analysis of 18S rRNA gene and psbA genes
The sequences of the 18S rRNA and psbA genes from CMS and CCMP
diatom cultures and reference diatom sequences from GenBank were used for
distance-based operational taxonomic unit and richness (DOTUR: Scholss and
Handelsman 2005) analysis. DOTUR calculated various diversity indices and
richness estimators. The sequences were aligned with ClustalW (Thompson et
al. 1994). The DNA distance program in the PHYLIP package (Felsenstein
1993) was used to calculate genetic distances with Kimura-2-parameter methods
(Kimura 1980). The distance matrix was then used for the DOTUR analysis.
The determination of operational taxonomic units (OTUs) was based on 1% and
3% genetic differences. Rarefaction curves were generated to compare the
sequence variation between 18S rRNA and psbA genes. The bias-corrected
Chao1 richness estimator (Chao 1984) was used to assess species richness and
the Shannon-Weiner diversity index (Shannon and Weaver 1963) was used to
assess species richness and evenness for the two genes.
21
RESULTS
Isolation and analysis of pure cultures
In total 46 diatoms were isolated from the CMS/ICW and have been
maintained in the laboratory. 18S rRNA gene sequences were obtained for 34 of
these cultures. BLASTn results provided putative identifications (Table 2) for the
previously unknown CMS diatom isolates, and species names were added to
trees to provide reference sequences for anonymous clonal haplotypes in the
psbA haplotype diversity tree. 18S rRNA gene IDs were also used in
phylogenetic comparisons of 18S rRNA and psbA gene sequences from CMS
and CCMP diatom cultures and diatom sequences from GenBank.
The psbA gene was amplified from each CMS diatom isolate using the
first set of primers developed in this study, dF11/dR12. PCR products were
sequenced and upon analysis of direct sequence chromatograms, it was
apparent that multiple psbA sequences were present and that cloning was
necessary to obtain separate sequences. BLASTn search results of cloned psbA
sequences indicated that the diatom cultures were contaminated with
photosynthetic cyanobacteria indicating that the CMS diatom cultures were
unialgal but not axenic. dF11/dR12 was then applied to the environment.
BLASTn results from this clone library indicated that primarily cyanobacteria were
amplified from CFP6 (results not shown).
The second primer set designed, dsF/dsR, directly amplified diatoms from
the CMS cultures contaminated with cyanobacteria without cloning. dsF/dsR
22
was then used to amplify all CMS and CCMP diatom cultures as well as the 24
other photosynthetic eukaryote cultures used as indicators of primer specificity.
Upon application of this primer set to environmental samples from CFP6 it was
found that cyanobacteria had been eliminated from the clone library.
PCR amplification and cloning of CMS cultures with the first primer set
dF11/dR12 resulted in the separation of diatom and cyanobacteria sequences
provided sequence alignments of multiple psbA copies from each diatom culture.
As a result, a significant number of nucleotide substitutions were revealed within
each isolate. Subsequently, two CMS cultures were chosen to determine the
extent of psbA variation within a culture derived from a single diatom cell: CMS01
with 18S BLASTn ID Cylindrotheca closterium and CMS09 with Thalassiosira
eccentrica BLASTn ID. A total of 57 psbA gene fragments were obtained from
the Cylindrotheca closterium clone library and 39 psbA gene fragments were
obtained from the Thalassiosira eccentrica clone library using the second primer
set developed dsF/dsR. Only those sequences containing segregating sites are
shown (Table 3 and Table 4). Sequences were aligned and compared to raw
sequence chromatograms to ensure that the observed segregating sites were
sound and not due to sequencing error (Fig. 2 and 3). Cylindrotheca sp. clones
had 22 segregating sites out of a total of 655 nucleotide positions (with an
estimated 96.6% sequence similarity) with a total of 11 non-synonymous
substitutions (Table 3). Thalassiosira sp. clones had 10 segregating sites out of
a total of 663 nucleotide positions (with an estimated 98.5% sequence similarity)
with 8 non-synonymous substitutions (Table 4).
23
Thalassiosira sp. has many more chloroplasts than Cylindrotheca sp.
Despite this obvious difference, however, Cylindrotheca sp. and Thalassiosira sp.
had nearly equal substitution rates at about 7.3 x 10-4 substitutions/ total sites.
Substitution rates for Thalassiosira sp. were extrapolated to account for the
unequal number of sequences available for the two isolates.
18S rRNA and psbA gene comparisons
The 18S rRNA gene and psbA maximum parsimony and maximum
likelihood phylogenies with supporting maximum parsimony and maximum
likelihood bootstrap values (Fig. 4 and 5) were generated for sequences from
CMS and CCMP diatom cultures and for GenBank diatom sequences.
Topologies for phylogenies of both the 18S rRNA gene and psbA show that the
raphid pennate diatoms are monophyletic, but that the centric and araphid
pennate diatoms are not. A similar topology is observed for each gene in a
neighbor-joining comparison of genetic distance using uncorrected p-distance
(Fig.6) providing confidence in psbA as an appropriate marker for biodiversity
that is also accurate in resolving phylogenetic relationships among the diatoms.
Rarefaction curves were generated based on 41 18S rRNA genes and 50
psbA genes. Rarefaction analysis calculated the same number of OTUs for the
18S rRNA and psbA genes (Fig. 7). Twenty-four OTUs were observed at the 1%
cutoff and 16 were observed at the 3% cutoff for both genes. Richness of both
sequences did not reach saturation based on rarefaction analysis. The
nonparametric Chao1 richness estimator calculated 41 and 75 OTUs based on
24
1% cutoff for 18S rRNA and psbA genes, respectively. However, richness of the
psbA genes was lower than the 18S rRNA genes based on the 3% cutoff. The
Shannon-Weiner richness and evenness index values for psbA genes are lower
than those observed for 18S rRNA gene at both cutoff levels (Table 5).
Environmental sampling
In total, direct sequencing methods were used to determine partial psbA
sequences for 140 diatoms obtained from clone libraries constructed with the
dsF/dsR marker using environmental DNA extracted from surface and bottom
samples collected at CFP6 (Appendix 1, Fig. 8). The average length of the psbA
fragment sequenced in this study was 665 bp.
Diatom psbA sequences from the CFP6 clone library were compiled with
sequences from CMS and CCMP diatom cultures and diatom sequences from
GenBank and Onslow Bay (Appendix 1). Twenty-four other eukaryotic taxa
comprising a phylogenetically diverse assemblage of photoautotrophs were
combined with 13 psbA sequences from GenBank for a total of 37 psbA
sequences from other photosynthetic eukaryotes (Appendix 2) added to analysis
for assessment of primer specificity of photosynthetic groups outside Phylum
Bacillariophyta (diatoms). The neighbor-joining tree of all psbA sequences
analyzed in this study with supporting bootstrap values (Fig. 8) reflects haplotype
diversity at site CFP6. Although the dsF/dsR primers are not specific to diatoms,
a diatom psbA sequence can be distinguished from that of other photosynthetic
eukaryotes; anonymous environmental sequences can be identified as a diatom
25
if it groups within the monophyletic clade of Phylum Bacillariophyta (diatoms).
CMS cultures shown in bold have been putatively identified according to the 18S
rRNA gene sequence BLASTn search. The presence of a branch with a species
name indicates a positively identified reference haplotype from a culture
collection or a GenBank sequence that can be used to infer relationships among
anonymous psbA haplotypes. The application of the photosynthetic eukaryote
specific psbA marker dsF/dsR to site CFP6 on 13 June 2007 revealed that
primarily diatoms are amplified from river plume waters with only three
sequences out of 140 that grouped with other photosynthetic eukaryotes.
DISCUSSION
Primer specificity
The primary goal of this study was to design a diatom-specific maker for
genetic and ecological studies. When tested on pure cultures, the psbA-based
genetic marker developed amplifies some other photosynthetic eukaryotes
including other stramenopiles, chlorophytes, haptophytes, cryptophytes and
rhodophytes; it is not strictly, by definition, diatom-specific. Nevertheless, our
field studies clearly demonstrate that application of these oligonucleotide primers
to environmental samples proves sufficient for ecological studies of marine
diatoms. A diatom sequence can easily be distinguished from other members of
the photosynthetic eukaryotic assemblage based on an analysis of genetic
distance and the grouping of a diatom sequence within the monophyletic
Bacillariophyta clade.
26
Phylogenetic and genetic distance analyses of the 18S rRNA gene
sequences from pure diatom cultures indicates that centric and araphid pennate
diatoms do not form monophyletic groups but that raphid pennates do share a
common ancestor. This pattern has been observed in previous studies that
employed the 18S rRNA gene in determining diatom phylogeny (Kooistra and
Medlin 1996; Medlin et al. 1996; Sorhannus 2007). The same analyses carried
out for diatom psbA sequences show that the two genes share a similar topology,
providing support for the use of psbA as reliable phylogenetic marker to resolve
relationships among diatoms.
Upon neighbor-joining analysis (Fig. 8), it is apparent that diatoms are
primarily amplified from the eukaryotic microalgal assemblage at CFP6 (Fig. 1).
Such a result is not surprising in this high nutrient region. CFP6 is located 7 km
west of the estuary and has depressed nutrient concentrations, indicative of high
biological activity at this site. CFP6 contains high concentrations of nitrate (NO3-)
at 1.36+1.56 μM (Mallin et al. 2005), the form of inorganic nitrogen that often
supports the growth of larger-celled organisms such as diatoms (Franck et al.
2005). Silica, which is vital to diatom growth, shows a strong riverine signal and
while silicate concentrations are higher within the estuary, levels are high enough
to support the growth of diatoms in the surrounding coastal sites with
concentrations at CFP6 at ~5 μM (Mallin et al. 2005).
Because the primer set developed in this study was designed based on
diatom psbA sequences, there likely exists a bias for the preferential
amplification of diatoms from the environment. However, this bias does not
27
appear to preferentially amplify any particular group of diatoms from
environmental samples; all three major morphological groups are represented
from the sample site CFP6. The genetic marker dsF/dsR proves highly useful in
the extraction of diatom sequences from the environment without the inclusion of
homologous cyanobacterial DNA, while also proving accurate for the
establishment of phylogenetic relationships among diatoms for use in studies of
ecology and biodiversity of this globally important group of heterokont algae.
psbA diversity
Substantial allelic diversity of psbA was found in two morphologically
distinct diatom genera. The pennate CMS01 (Cylindrotheca closterium) and
centric CMS09 (Thalassiosira eccentrica) were amplified with psbA and
subsequently cloned to separate alleles. Separate sequence alignments of the
two species show multiple segregating sites within the psbA gene within each
diatom isolate. Sequence chromatograms from the forward and reverse direction
confirm the nucleotide changes; the observed segregating sites are not due to
sequencing error but may arise as a result of PCR bias where Taq polymerase
errors may result in an overestimate in the amount of nucleotide variation.
However, these errors in DNA replication during PCR amplification can be
sufficiently accounted for by the clustering of sequences based on 99% similarity,
as Taq polymerase errors account for about 1% of nucleotide variation (Acinas et
al. 2005). The Cylindrotheca closterium and Thalassiosira eccentrica clones
showed approximately 96.6% and 98.5% sequence similarity, respectively, both
28
outside the range of PCR bias due to Taq polymerase errors. Consequently,
these changes are likely due to mutations that accumulate in the chloroplast
genomes within each diatom cell.
Rarefaction analysis using DOTUR indicates that at 99% and 97%
sequence similarity, the 18S rRNA and psbA genes show the same number of
OTUs. This finding suggests that the variability within these two very different
genes is nearly equal with respect to defining OTUs. However, the Chao1 value
for psbA at the 1% cutoff was three-fold higher than seen for the 3% cutoff. This
high value of gene richness correlates to the high level of allelic diversity found in
the Cylindrotheca and Thalassiosira clone libraries, but does not result it a larger
number of OTUs determined by rarefaction analysis indicating that many of the
sequences are very nearly identical and are thus treated as one taxonomic unit.
Because psbA genes show this high level of variation at the 1% level, either
because of mutational change or Taq polymerase errors, it is advisable to only
include taxa at 99% sequence similarity in phylogenetic and distance analyses
when employing psbA in environmental studies.
Despite these singleton changes in psbA, the alignment analyzed in this
study shows many regions to be highly conserved. Presumably, primary
structure must be maintained to confer full function of the D1 protein. A
substitution that affects primary structure may cause that D1 protein to lose
function. The presence of many more chloroplast genomes and thus psbA copies
within the cell ensures that photosystem II will be provided a functional D1
protein. The nature of chloroplast replication may explain the presence of
29
segregating sites within a single diatom isolate. Unlike the nuclear genome,
chloroplasts divide independently of cellular binary fission (reviewed in
Osteryoung and Nunnari 2003). Multiple chloroplasts can be found within a
single cell. With the separate division of each chloroplast, there likely exists a
higher probability of mutation than for nuclear genomes that are replicated only
upon binary division of the cell.
This finding brings up an interesting question regarding differential rates of
chloroplast genome evolution. Does the presence of more chloroplasts within a
particular diatom species result in faster rates of evolution due to an increase in
mutation pressure? Answering this question would require the measurement of
growth rates in order to determine mutation rates in species with differing
numbers of chloroplasts. Results of such a study may shed light on gene
evolution within the chloroplast genomes of algae, which to date have been
largely underrepresented in the literature.
CONCLUSIONS
The discovery that multiple psbA alleles may be present within diatom
isolates reveals an additional level of genetic diversity that to my knowledge has
not yet been addressed. Such a finding underlies the importance of analyzing
DNA variability at the most resolvable level at which cloning and subsequent
sequencing provides an analysis of distinct alleles of the same gene within a
single isolate. The psbA gene is an excellent molecular marker for the
30
characterization of biodiversity and if applied more broadly to environmental
samples will likely provide a more accurate estimate of microalgal genetic
variation that may also correlate to physical, morphological and ecological
differentiation resulting from natural selection. Key water quality parameters (eg.,
light, nutrients, chlorophyll) can be measured with great precision and accuracy.
These water mass characteristics may very well correlate to specific microalgal
assemblages. In other words, microorganisms may be more confined to spatial
niches than suggested by previous genetic studies. The supplement of a genetic
marker such as psbA that is sensitive to the more cryptic genetic diversity of
planktonic algae may result in a higher resolution analysis of these water masses
with respect to species biodiversity and changes in community structure that
likely correlate to specific environmental parameters.
31
LITERATURE CITED
Acinas, SG, Sarma-Rupavtarm, R, Klepac-Ceraj, V & Polz, MF. 2005. PCR- induced sequence artifacts and bias: Insights from comparison of two 16S rRNA clone libraries constructed from the same sample. Appl. Environ. Microbiol. 71: 8966-8969. Andersen, RA, Bidigare, RR, Keller, MD & Latasa, M. 1996. A comparison of HPLC signatures and electron microscopy observations for oligotrophic waters of the North Atlantic and Pacific Oceans. Deep Sea Res. II. 43: 517-537. Baas Becking, LGM. 1931. Gaia of leven en aarde. The Hague, the Netherlands: Nijhoff. Ambtsrede RU Leiden (in Dutch). Bailey, JC, Bidigare, RR, Christensen, SJ & Andersen, RA. 1998. Phaeothamniophyceae classis nova.: a new lineage of chromophytes based upon photosynthetic pigments, rbcL sequence analysis and ultrastructure. Protist 149: 245-263 Bidigare, RR & Ondrusek, ME. 1996. Spatial and temporal variability of phytoplankton pigment distributions in the central equatorial Pacific Ocean. Deep Sea Res. II. 43: 809-833. Bigler, C and RI Hall. 2002. Diatoms as indicators of climatic and limnological change in Swedish Lapland: a 100-lake calibration set and its validation for paleoecological reconstructions. J. Paleolimnol. 27: 97-115. Bigler, C & Hall R.I. 2003. Diatoms as indicators of July temperature: a validation attempt at century- scale with meteorological data from northern Sweden. Palaeogeography, Palaeoclimatology, Palaeoecology 189: 147-60. Butler, H & Rogerson, A. 1995. Temporal and spatial abundance of naked
amoebae (Gymnamoebae) in marine benthic sediments. J. Eukaryot. Microbiol. 42: 724-730.
Chao, A. 1984. Nonparametric estimation of the number of classes in a population. Scand. J. Stat. 11: 783-791. Cunningham, L, Raymond, B Snape, I & Riddle, MJ. 2005. Benthic diatom communities as indicators of anthropogenic metal contamination at Casey Station, Antarctica. J. Paleolimnol. 33: 499-513. Dawson, SC & Pace, NR. 2002. Novel kingdom-level eukaryotic diversity in anoxic environments. Proc. Natl. Acad. Sci. USA. 99: 8324-8329.
32
Debus, RJ. 1992. The manganese and calcium ions of photosynthetic oxygen evolution. Biochim. Biophys. Acta 1102: 269-352. de la-Cruz J, Pritchard, T, Gordon, G & Ajani, P. 2006. The use of periphytic diatoms as a means of assessing impacts of point source inorganic nutrient pollution in southeastern Australia. Freshwater Biol. 51:951-972. de la Rey, PA, Taylor, JC, Laas, A, van Rensburg, L & Vosloo, A. 2004. Determining the possible application value of diatoms as indicators of general water quality: A comparison with SASS 5. Water SA. 30: 325-332. DeLong, EF. 1992. Archaea in coastal marine environments. Proc. Natl. Acad. Sci. USA. 89: 5685-5689 Dièz, B, Pedros-Alio, C & Massana, R. 2001. Study of genetic diversity of eukaryotic picoplankton in different oceanic regions by small-subunit rRNA gene cloning and sequencing. Appl. Environ. Microbiol. 67: 2932-2941. Edgecomb, VP, Kysela, DT, Teske, A, de Vera Gomez, A & Sogin, ML. 2002. Benthic eukaryotic diversity in the Guaymas Basin hydrothermal vent environment. PNAS. 99: 7658-7662. Falciatore, A & Bowler, C. 2002. Revealing the molecular secrets of diatoms. Annu. Rev. Plant Biol. 53:109-30. Falkowski, PG, Barber, RT & Smetacek, V. 1998. Biogeochemical controls and feedbacks on ocean primary production. Science 281: 200-206. Felsenstein, J. 1993. PHYLIP (Phylogeny Inference Package) version 3.67. Distributed by the author Department of Genetics, University of Washington, Seattle. Field, CB, Behrenfeld, MJ, Randerson, JT & Falkowski, P. 1998. Primary production of the biosphere: integrating terrestrial and oceanic components. Science 281: 237-40. Field, KG, Gordon, D, Whight, T, Rappe, M, Urgach, E, Vergin, K & Giovannoni SJ. 1997. Diversity and depth-specific distribution of SAR11 cluster rRNA genes from marine planktonic bacteria. Appl. Environ. Microbiol. 63: 63- 70. Finkel, ZV, Katz, ME, Wright, JD, Schofield, OME & Falkowski, PG. 2005. Climatically driven macroevolutionary patterns in the size of marine diatoms over the Cenozoic. PNAS 102: 8927-8932.
33
Finlay, BJ. 2002. Global dispersal of free-living microbial eukaryote species. Science 296: 1061-1063. Finlay BJ & Clark KJ. 1999. Ubiquitous dispersal of microbial species. Nature 400: 323. Flöder, S & Burns, CW. 2004. Phytoplankton diversity of shallow tidal lakes: influence of periodic salinity changes on diversity and species number of a natural assemblage. J. Phycol. 40: 54-61. Franck, VM, Smith, GJ, Bruland, KW & Brzezinski, MA. 2005. Comparison of size-dependent carbon, nitrate and silicic acid uptake rates in high- and low-iron waters. Limnol. Oceanogr. 50: 825-38. Fuhrman, JA. 2002. Community structure and function in prokaryotic marine plankton. Antonie van Leeuwenhoek 81: 521-527. Fuhrman, JA, McCallum, K & Davis, AA. 1992. Novel major archaebacterial group from marine plankton. Nature. 356: 148-149. Giovannoni, SJ, Britschgi, TB, Moyer, CL & Field, KG. 1990. Genetic diversity in the Sargasso Sea bacterioplankton. Nature. 345: 60-63. Guillou, L, Moon-van der Staay, Claustre, H, Partensky, F and Vaulot, D. 1999. Diversity and abundance of Bolidophyceae (Heterokonta) in two oceanographic regions. Appl. Env. Microbiol. 65: 4528-4536. Hoepffner, N & Hass, LW. 1990. Electron microscopy of nanoplankton from the North Pacific Central Gyre. J. Phycol. 26: 421-439. Irigoien, X, Meyer, B, Harris, R & Harbour, D. 2004. Using HPLC pigment analysis to investigate phytoplankton taxonomy: the importance of knowing your species. Helgoland Marine Research 77-82. Johnson, PW & Sieburth, JM. 1982. Morphology and occurrence of eukaryotic phototrophs of bacterial size in the picoplankton of estuarine and oceanic waters. J. Phycol. 18: 318-327. Kimura, M. 1980. A simple method for estimating evolutionary rates of base substitutions through comparative studies of nucleotide sequences. J. Mol. Evol. 16: 111-120. Kooistra, WHCF and Medlin, LK. 1996. Evolution of the diatoms (Bacillariophyta) IV. Reconstruction of their age from small subunit rRNA coding regions and the fossil record. Mol. Phylogenet. Evol. 6: 391-407.
34
Kyle, DJ. 1987. The biochemical basis of photoinhibition of photosystem II. Photoinhibition. Amsterdam: Elsevier, pp. 197-226. Lanave, C, Preparata, G, Saccone, C & Serio, G. 1984. A new method for calculating evolutionary substitution rates. J. Mol. Evol. 20: 86-93. Lange, M, Guillou, L, Vaulot, D, Simon, N, Amann, RI, Ludwig, W & Medlin, LK. 1996. Identification of the class Prymnesiophyceae and the genus Phaeocystis with ribosomal RNA-targeted nucleic acid probes detected by flow cytometry. J. Phycol. 32: 858-868. Li, WKW. 1994. Primary production of prochlorophytes, cyanobacteria and eukaryotic ultraphytoplankton: measurements from flow cytometric sorting. Limnol. Oceanogr. 39: 169-175. Li, WKW, Subba Rao, DV, Harrison, WG, Smith, JC, Cullen, JJ, Irwin, B & Platt, T. 1983. Autotrophic picoplankton in the tropical ocean. Science 219: 292-295. Lopez-Garcia, P, Rodriguez-Valera, F, Pedros-Alio, C & Moreira, D. 2001. Unexpected diversity of small eukaryotes in deep-sea Antarctic plankton. Nature 409: 603-607. Mackey, DJ, Higgins, HW, Mackey, MD & Holdsworth, D. 1998. Algal class abundances in the western equatorial Pacific: Estimation from HPLC measurements of chloroplast pigments using CHEMTAX. Deep Sea Res. I 1441-1468. Maddison WP & Maddison, DR. 2000. MacClade 4.0: analysis of phylogeny and character evolution. Sinauer, Sunderland, MA Mallin, MA, Burkholder, JM, Cahoon, LB & Posey, MH. 2000. The North and South Carolina coasts. Mar. Poll. Bull. 41: 56-75. Mallin, MA, Cahoon, LB & Durako, MJ. 2005. Contrasting food-web support bases for adjoining river-influenced and non-river influenced continental shelf ecosystems. Estuarine, Coastal and Shelf Science 62: 55-62. Mann, D.G. 1999. The species concept in diatoms. Phycol. Rev. 38: 437-79. Massana, R, Guillou, L, Díez, B & Pedrós-Alió, C. 2002. Unveiling the organisms behind novel eukaryotic ribosomal DNA sequences from the ocean. Appl. Environ. Microbiol. 68: 4554-4558.
35
Medlin, LK, Kooistra, WHCF, Gersonde, R & Wellbrock, U. 1996. Evolution of the diatoms (Bacillariophyta). II. Nuclear-encoded small-subunit rRNA sequence comparisons confirm a paraphyletic origin for the centric diatom. Mol. Biol. Evol. 13: 67-75.
McCormick, PV & Cairns Jr., J. 1994. Algae as indicators of environmental change. J. Appl. Phycol. 6: 509-26. Moon-van der Staay, SY, De Wachter, R & Vaulot, D. 2001. Oceanic 18S rDNA sequences from picoplankton reveal unsuspected eukaryotic diversity. Nature 409: 607-610. Moon-van der Staay, SY, van der Staay, GWM, Guillou, L, Vaulot, D, Claustre, H & Medlin, LK. 2000. Abundance and diversity of prymnesiophytes in the picoplankton community from the equatorial Pacific Ocean inferred from 18S rDNA sequences. Limnol. Oceanogr. 45: 98-109. Moyer, CL, Dobbs, FC & Karl, DM. 1995. Phylogenetic diversity of the bacterial community from a microbial mat at an active hydrothermal vent system, Loihi Seamount, Hawaii. Appl. Environ. Microbiol. 61: 1555-1562 Nanba, O & Satoh, K. 1986. Isolation of photosystem II reactions center consisting of D-1 and D-2 polypeptides and cytochrome b-559. PNAS USA. 84: 109-112. Osmond, CB, Ramus, J, Levavasseur, G, Franklin, LA & Henley, WJ. 1993. Fluorescence quenching during photosynthesis and photoinhibition of Ulva rotundata. Blid. Planta. 106: 97-106. Osteryoung, KW & Nunnari, J. 2003. The division of endosymbiotic organelles. Science. 302: 1698-1704. Pace, Norman R. 1997. A molecular view of the microbial biosphere. Science 276: 734-740. Paul, JH, Pichard, SL & Kang, JB. 1999. Evidence for a clade-specific temporal and spatial separation in ribulose bisphosphate carboxylase gene expression in phytoplankton populations off Cape Hatteras and Bermuda. Limnol. Oceanogr. 44: 12-23. Pichard, SL & Paul, JH. 1991. Detection of gene expression in genetically engineered microorganisms and natural phytoplankton populations in the marine environment by mRNA analysis. Appl. Environ. Microbiol. 57: 1721-1727.
36
Pichard, SL, Frischer, ME & Paul, JH. 1993. Ribulose bisphosphate carboxylase gene expression in subtropical marine phytoplankton populations. Mar. Ecol. Prog. Ser. 101: 55-65. Pichard, SL, Campbell, L. Kang, JB, Tabita, FR, & Paul, JH. 1996. Regulation of ribulose bisphosphate carboxylase gene expression in natural phytoplankton communities. I. Diel rhythms. Mar. Ecol. Prog. Ser. 139: 257-265. Pichard, SL, Campbell, L, Carder, K, Kang, JB, Patch, J, Tabita, FR & Paul, JH. 1997a. Analysis of ribulose bisphosphate carboxylase gene expression in natural phytoplankton communities by group-specific gene probing. Mar. Ecol. Prog. Ser. 149: 239-253. Pichard, SL, Campbell, L & Paul, JH. 1997b. Diversity of the ribulose bisphosphate carboxylase/oxygenase form I gene (rbcL) in natural phytoplankton communities. Environ. Microbiol. 63: 3600-3606. Posada, D and Crandall, KA. 1998. Modeltest: testing the model of DNA substitution. Bioinformatics. 14: 817-818. Potter, D, Lajeunesse, TC, Saunders, W and Anderson, RA. 1997. Convergent evolution masks extensive biodiversity among marine coccoid picoplankton. Biodivers. Conserv. 6: 99-107. Poulíčková, A, Duchoslav, M & Dokulil, M. 2004. Littoral diatom assemblage as bioindicators of lake trophic status: A case study from perialpine lakes in Austria. Eur. J. Phycol. 39: 143-152. Rappé, MS, Suzuki, MT, Vergin, KL & Giovannoni. SJ. 1998. Phylogenetic diversity of ultraplankton plastid small-subunit rRNA genes recovered in environmental nucleic acid samples from the Pacific and Atlantic coasts of the United States. Appl. Environ. Microbiol. 64: 294-303. Reavie, ED & Smol, JP. 1998. Epilithic diatoms of the St. Lawrence River and their relationship to water quality. Can. J. Bot. 76: 251-257. Rooney-Varga, JN, Devereux, R, Evans, RS & Hines, ME. 1997. Seasonal changes in the relative abundance of uncultivated sulfate-reducing bacteria in a salt marsh sediment and in the rhizosphere of Spartina alternifiora. Appl. Environ.Microbiol. 63: 3895-3901. Round, FE, Crawford, RM & Mann, DG. 1990. Diatoms: Biology and morphology of the genera. Cambridge Univ. Press, Cambridge, UK.
37
Rynearson, TA & Armbrust, EV. 2004. Genetic differentiation among populations of the planktonic marine diatom Ditylum brighwellii (Bacillariophyceae). J. Phycol. 40: 34.43. Sarno, D, Koositra, WGCF, Medlin, LK, Percopo, I & Zingone, A. 2005. Diversity in the genus Skeletonema (Bacillariophyceae). II. An assessment of the taxonomy of S. costatum-like species with the description of four new species. J. Phycol. 41: 151-176. Saitou, N & Nei, M. 1987. The neighbor-joining method: A new method for reconstructing phylogenetic trees. Mol. Biol. Evol. 4: 406-425. Schloss, PD and Handelsman, J. 2005. Introducing DOTUR, a computer program for defining operations taxonomic units and estimating species richness. Appl. Envrion. Microbiol. 71: 1501-1506. Shannon, CE & Weaver, W. 1963. The mathematical theory of communication. Urbana, University of Illinois Press. Simon, N, Barlow, RG, Marie, D, Partensky, F & Vaulot, D. 1994. Flow cytometry analysis of oceanic photosynthetic picoeukaryotes. J. Phycol. 30: 922-935. Smol, JP, Wolfe, AP, Birks, HJB, Douglas, MSV, Jones, VJ, Korhola, A, Pienitz, R, Rühland, K, Sorvari, S, Antoniades, D, Brooks, SJ, Fallu, M-A, Hughes, M, Keatley, BE, Laing, TE, Michelutti, N, Nazarova, L, Nyman, M, Paterson, AM, Perren, B, Quinlan, R, Rautio, M, Saulnier-Talbot, É , Siitonen, S, Solovieva, N & Weckström, J. 2005. Climate-driven regime shifts in the biological communities of arctic lakes. PNAS 102: 4397-4402. Sorhannus, U. 2007. A nuclear-encoded small-subunit ribosomal RNA timescale for diatom evolution. Marine Micropaleontology 65: 1-12. Stoeck, T & Epstein, S. 2003. Novel eukaryotic lineages inferred from small- subunit rRNA analyses of oxygen-depleted marine environments. Appl. Environ. Microbiol. 69: 2657-2663. Stoeck, T, Taylor, GT & Epstein, SS. 2003. Novel eukaryotes from the permanently anoxic Cariaco Basin (Caribbean Sea). Appl. Environ. Microbiol. 69: 5656-5663. Stolte, W, Kraay, GW, Noordeloos, AAM & Riegman, R. 2000. Genetic and physiological variation in pigment composition of Emiliania huxleyi (Prymnesiophyceae) and the potential use of its pigment ratios as a quantitative physiological marker. J. Phycol. 36: 529-539.
38
Swofford, D. L. 2002. Phylogenetic Analysis Using Parsimony (PAUP*). Sinauer, Sunderland, MA. Tamura, K & Nei, M. 1993. Estimation of the number of nucleotide substitutions in the control region of mitochondrial DNA in humans and chimpanzees. Mol. Biol. Evol. 10: 512-526. Thompson, JD, Higgins, DG & Gibson, TJ. 1994. CLUSTAL W: improving the
sensitivity of progressive multiple sequence alignments through sequence weighting, position specific gap penalties and weight matrix choice. Nucl. Acids Res. 22: 4673-4680.
van Leeuwe, MA & Stefels, J. 1998. Effects of iron and light stress on the biochemical composition of Antarctic Phaeocystis sp. (Prymnesiophyceae). II. Pigment composition. J. Phycol. 34: 496-503. Vaultonburg, DL & Pederson, CL. 1994. Spatial and temporal variation of diatom community structure in two east-central Illinois streams. Transactions of the Illinois State Academy of Science 87: 9-27. Wawrik, B, Paul, JH & Tabita, FR. 2002. Real-time PCR quantification of rbcL (ribulose-1,5-bisphosphate carboxylase/oxygenase) mRNA in diatoms and pelagophytes. Environ. Microbiol. 68: 3771-3779. Weckström, K & Juggins, S. 2005. Coastal diatom-environment relationships from the Gulf of Finland, Baltic Sea. J. Phycol. 42: 21-35. Woese, CR. 1987. Bacterial evolution. Microbiol. Rev. 51: 221-271. Wolfe, AP. 2003. Diatom community responses to late-Holocene climatic variability, Baffin Island, Canada: a comparison of numerical approaches. Holocene. 13: 29-37. Wolfe, GR, Cunningham, FX, Durnford, D. Green, B & Gantt, E. 1994. Evidence for a common origin of chloroplasts with light harvesting complexes of different pigmentation. Nature 367: 566-568. Xu, HH & Tabita, FR. 1996. Ribulose bisphosphate carboxylase/oxygenase gene expression and diversity of Lake Erie planktonic microorganisms. Appl. Enivron, Microbiol. 62: 1913-1921. Zapata, M, Rodríguez, F & Garrido, JL. 2000. Separation of chlorophylls and carotenoids from marine phytoplankton: a new HPLC method using a reversed phase C8 column and pyridine-containing mobile phase. Mar. Ecol. Prog. Ser. 195: 29-45.
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40
Zeidner, G, Preston, CM, Delong, EF, Massana, R, Post, AF, Scanlan, DJ & Béjà, O. 2003. Molecular diversity among marine picophytoplankton as revealed by psbA analysis. Env. Microbiol. 5: 212-216.
Table 1. Forward and reverse primer matrix tested on CCMP diatom cultures during initial primer development.
dR10 dR11 dR12 dR13 dR14 dR15 dF10 df10/dR10 df10/dR11 df10/dR12 df10/dR13 df10/dR14 df10/dR15 dF11 dF11/dR10 dF11/dR11 dF11/dR12 dF11/dR13 dF11/dR14 dF11/dR15 dF12 dF12/dR10 dF12/dR11 dF12/dR12 dF12/dR13 dF12/dR14 dF12/dR15 dF13 dF13/dR10 dF13/dR11 dF13/dR12 dF13/dR13 dF13/dR14 dF13/dR15 dF14 dF14/dR10 dF14/dR11 dF14/dR12 dF14/dR13 dF14/dR14 dF14/dR15 dF15 dF15/dR10 dF15/dR11 dF15/dR12 dF15/dR13 dF15/dR14 dF15/dR15
41
Table 2. Putative species identifications for CMS diatom cultures based on 18S rRNA gene sequences.
Culture No. 18S rRNA BLASTn ID Culture No. 18S rRNA BLASTn ID CMS01 Cylindrotheca closterium CMS29 Papiliocellulus elegans CMS02 Licmopha abreviata CMS31 Thalassiosira nordenskioeldii CMS03 Planktoniella sol CMS32 Papiliocellulus elegans CMS07 Navicula sp. CMS33 Skeletonema costatum CMS08 Skeletonema grethae CMS38 Skeletonema tropicum CMS09 Thalassiosira eccentrica CMS39 Navicula sp. CMS11 Navicula sp. CMS40 Skeletonema concavivscula CMS13 Nitzschia communis CMS42 Pleurosigma planktonicum CMS14 Navicula cryptocephala CMS46 Skeletonema tropicum CMS18 Cylindrotheca closterium CMS47 Skeletonema tropicum CMS19 Thalassiosira anguste-lineata CMS48 Skeletonema tropicum CMS20 Leptocylindrus sp. CMS49 Skeletonema tropicum CMS21 Chaetoceros negracile CMS50 Skeletonema tropicum CMS22 Thalassiosira nordenskioeldii CMS51 Thalassiosira frauenfeldii CMS24 Navicula phyllepta CMS52 Skeletonema tropicum CMS25 Skeletonema menzelii CMS54 Cylindrotheca closterium CMS27 Thalassiosira antarctica CMS55 Skeletonema tropicum
42
Table 3. psbA allelic diversity for CMS01 (Cylindrotheca sp.). Each unique psbA sequence was treated as a unique allele. Base pair position of the segregating site is included along with the change in nucleotide. Nucleotide changes are classified as transitions or transversions and changes in amino acid are noted.
Clone No. Segregating
Site Nucleotide
Change Ts/Tr Amino Acid
Change
CMS01C10 43 T-->C Ts F-->S CMS01C02 69 A-->G Ts I-->V CMS01C25 152 T-->G Tv None CMS01C12 195 T-->C Ts F-->L CMS01C18 219 G-->A Ts A-->T CMS01C47 260 A-->G Ts None CMS01C17 293 C-->T Ts None CMS01C14 302 T-->C Ts None CMS01C06 313 T-->C Ts M-->T CMS01C23 324 C-->T Ts Q-->Stop CMS01C19 347 G-->A Ts M-->T CMS01C33 371 T-->C Ts None CMS01C24 416 A-->G Ts S-->P CMS01C10 431 Deletion of T N/A N/A CMS01C19 431 T-->C Ts None CMS01C34 443 A-->G Ts None CMS01C13 465 A-->G Ts N-->D CMS01C19 497 A-->G Ts None CMS01C45 497 A-->G Ts None CMS01C02 504 A-->G Ts N-->D CMS01C28 553 C-->T Ts A-->V CMS01C15 572 T-->C Ts None
43
Table 4. psbA allelic diversity for CMS09 (Thalassiosira sp.). Each unique psbA sequence was treated as a unique allele. Base pair position of the segregating site is included along with the change in nucleotide. Nucleotide changes are classified as transitions or transversions and changes in amino acid are noted.
Clone No. Segregating
Site Nucleotide
Change Ts/Tr Amino Acid
Change
CMS09C10/C11 46 G-->A Ts M-->I CMS09C10/C11 78 T-->C Ts V-->A
CMS09C25 79 T-->A Tv None CMS09C37 191 C-->T Ts R-->C CMS09C04 198 G-->A Ts W-->Stop CMS09C22 224 G-->A Ts V-->I CMS09C37 272 T-->C Ts S-->P CMS09C31 297 G-->A Ts G-->D CMS09C33 340 A-->G Ts None CMS09C05 438 G-->A Ts S-->N
44
45
Table 5. Diversity and predicted richness of the 18S rRNA gene and psbA gene fragments from CMS and CCMP diatom cultures and diatom GenBank sequences as estimated by the Shannon-Weiner diversity index and Chao1 richness estimator computed using DOTUR for 1% and 3 % differences in nucleic acid sequence alignments. Numbers in parentheses are lower and upper 95% confidence intervals for the Choa1 estimator.
No. OTUs Chao1 Shannon-Weiner1% cutoff 3% cutoff 1% cutoff 3% cutoff 1% cutoff 3% cutoff
18S rRNA gene 24 16 41 (29, 80) 31 (19, 80) 2.869 2.32psbA 24 16 75 (39, 198) 25 (18, 56) 2.573 2.166
Wi l m i n g t o n , N C
CFP6
OB27
CMS/ICW
A t l a n t i c O c e a n
?0 3 6 9 121.5
Miles
Fig. 1. Map of southeastern North Carolina. Diatoms were collected from CMS/ICW (Center for Marine Science/ Intercoastal Waterway). Field primer tests were conducted at site CFP6 (Cape Fear River Plume). Diatom psbA sequences obtained from a previous study at OB27 (Onslow Bay) were used in primer development.
46
A) C2
C3 C4 C6 C7 C9 C10 C11 C12
(B) (C) Fig. 2. Alignment and sequence chromatograms from cloned isolate CMS01 (Cylindrotheca closterium). (A) Alignment of psbA sequences. (B) Clone 4 showing the wildtype psbA allele. (C) Clone 10 showing a deletion of T.
47
48
C1 C2 C3 C4 C5 C6 C7 C8 C9
(A) (B) (C) Fig. 3. Alignment and sequence chromatograms from cloned isolate CMS09 (Thalassiosira eccentrica). (A) Alignment of psbA sequences. (B) Clone 5 showing the wildtype psbA allele. (C) Clone 4 showing a substitution of A for G.
49
CMS48CMS52CMS50CMS49CMS38CMS55CMS47CMS46CMS08CMS25CMS33CMS22CMS31Thalassiosira pseudonanaCMS40CMS09CMS19CMS27CMS03Helicotheca tamesisCMS32CMS29Biddulphia sp.Odontella sinensisCMS11CMS39CMS07CMS14CMS24CMS42CMS13Phaeodactylum tricornutumCMS54CMS01CMS18CMS02CMS51Asterionellopsis gracialis (Black Sea)Asterionellopsis gracialis (CA, USA)CMS20Melosira octoganaCMS21Bolidomonas mediterraneaBolidomonas pacifica
18S rRNA BLASTn ID
centr
icra
phid
penn
atear
aphi
dpe
nnate
centr
ic
87
97
100
100100
57
100
50
64 100
100 98
92 72
100 100
76
54
100
93
97
100
69
99
51
100
99
63 99
99
87 71
57
100
64
Skeletonema tropicum
Skeletonema tropicumSkeletonema grethae
Thalassiosira nordenskioeldiiThalassiosira pseudonana
Thalassiosira anguste-lineataThalassiosira antarcticaPlanktoniella solHelicotheca tamesisPapiliocellulus elegansPapiliocellulus elegansBiddulphia sp.Odontella sinensis
Skeletonema tropicumSkeletonema tropicumSkeletonema tropicumSkeletonema tropicumSkeletonema tropicum
Skeletonema tropicum
Skeletonema menzeliiSkeletonema costatumThalassiosira nordenskioeldii
Thalassiosira concavivsculaThalassiosira eccentrica
Navicula sp.Navicula sp.Navicula sp.Navicula cyrptocephalaNavicula phylleptaPleurosigma planktonicumNitzschia communisPhaeodactylum tricornutumCylindrotheca closteriumCylindrotheca closteriumCylindrotheca closteriumLicmopha abbreviataThalassiosira frauenfeldiiAsterionellopsis gracialis (Black Sea)Asterionellopsis gracialis (CA, USA)Leptocylindrus sp.Melosira octoganaChaetoceros neogracile
Fig. 4. 18S rRNA maximum parsimony phylogeny of CMS and CCMP diatom cultures and GenBank diatom sequences. Maximum parsimony bootstrap values are given above the branches and maximum likelihood bootstrap values are given below. CMS diatom cultures are putatively identified and labeled centric, raphid pennate or araphid pennate according to 18S rRNA BLASTn results (right).
50
858675
65746261
77
1001009597
86 92
86 94
84 75
76 80 98
89
66 61
86 84 54
71
CMS11CMS39+CMS44CMS07CMS24CMS14CMS06CMS43CMS04CMS42Navicula salinicolaCMS01CMS18CMS41Phaeodactylum tricornutumCMS13CMS30CMS21CMS52CMS35CMS02CMS45
100100
Asterionellopsis glacialis (Black Sea)Asterionellopsis glacialis (CA, USA)CMS20CMS32CMS29CMS34CMS31Odontella sinensisCMS49CMS55CMS26CMS38CMS51CMS50CMS48CMS10,08,47,46 *CMS23Thalassiosira pseudonanaCMS27CMS25CMS22CMS33CMS09CMS19CMS53CMS40Biddulphia sp. Melosira octogonaHelicotheca tamensisBolidomonas mediterraneaBolidomonas pacifica
psbA 18S rRNA BLASTn ID
Navicula sp. Navicula sp.Navicula sp.Navicula phylleptaNavicula cytptocephala
Pleurosigma planktonicum
Cylindrotheca closteriumCylindrotheca closterium
Nitzschia communis
Chaetoceros neogracileSkeletonema tropicum
Licmorpha abbreviata
*CMS 08 Skeletonema grethae CMS 46,47 Skeletonema tropicum
Leptocylindrus sp.Papiliocellulus elegansPapiliocellulus elegans
Thalassiosira nordenskioeldii
Skeletonema tropicumSkeletonema tropicum
Skeletonema tropicumThalassiosira frauenfeldiiSkeletonema tropicumSkeletonema tropicum
Thalassiosira antarcticaSkeletonema menzeliiThalassiosira nordenskioeldiiSkeletonema costatumThalassiosira eccentricaThalassiosira anguste-lineata
Thalassiosira concavivscula
Fig. 5. psbA maximum parsimony phylogeny of CMS and CCMP diatom cultures and diatom GenBank sequences. Maximum parsimony bootstrap values are given above the branches and maximum likelihood bootstrap values are given below. CMS diatom cultures are putatively identified by 18S rRNA BLASTn results (right).
CMS48CMS52CMS50CMS46CMS49CMS55CMS38CMS47
CMS08CMS33
CMS25CMS40
CMS19CMS03CMS27
CMS09CMS22
CMS31Thalassiosira pseudonana
CMS32CMS29
Biddulphia sp.Odontella sinensis
Helicotheca tamesisCMS20
Melosira octoganaCMS21
CMS39CMS07
CMS11CMS14CMS24
CMS42CMS54
CMS01CMS18
CMS51CMS13
Phaeodactylum tricornutumAsterionellopsis gracialis (CA, USA)Asterionellopsis gracialis (Black Sea)
CMS02Bolidomonas mediterranea
Bolidomonas pacifica0.005 substitutions/site
psbA
raph
id p
enna
tear
aphid
pe
nnate
centr
ic
centr
ic
raph
id p
enna
tear
aphid
pe
nnate
centric
CMS11CMS39+CMS44
CMS07CMS24CMS14
CMS06CMS43
CMS01CMS18
CMS41Navicula salinicola
CMS04CMS42
CMS13Phaeodactylum tricornutum
CMS30CMS52
CMS35CMS02
CMS45Asterionellopsis glacialis (CA, USA)
Asterionellopsis glacialis (Black Sea)CMS21CMS20
CMS49CMS55CMS48CMS51CMS26CMS38CMS10+CMS08+CMS47+CMS46
CMS50CMS23
Thalassiosira pseudonanaCMS27
CMS53CMS40CMS19
CMS09CMS25CMS22
CMS33CMS32CMS29
CMS34CMS31
Odontella sinensisBiddulphia sp.
Helicotheca tamesisMelosira octogona
Bolidomonas mediterraneaBolidomonas pacifica
0.005 substitutions/site
18S rRNA gene95
10096
100
53
10067
100
63
58
100
67
100
100100
67
9992
10088
100
97
62
81
64
99
5710081
100100
98
9761
60
8793
100
100
96
67
6061
Fig. 6. 18S rRNA and psbA neighbor-joining phylogenies of CMS and CCMP diatom culture sequences and GenBank diatom sequences using uncorrected p-distance with supporting bootstrap values above the branches. Classification of CMS diatom cultures as centric, raphid pennate and araphid pennate diatoms are based on 18S rRNA BLASTn results.
51
52
Fig. 7. Rarefaction curves for the 41 18S rRNA gene sequences and 50 psbA gene sequences. Twenty-four OTUs were observed for each gene at the 1% cutoff and 16 were observed at the 3% cutoff.
CFP6B.60, CFP6B.63CFP6B.62
CFP6S.8CFP6S.48CFP6S.52
CFP6S.47CFP6S.24CFP6S.6CMS51CFP6B.96
CFP6B.8CMS26CMS38CMS 08, CMS10, CMS46, CMS47CMS48CMS49
CMS23CMS50
CMS55Thalassiosira pseudonanaEF460704CMS27CMS33CFP6S.18
CFP6B.42CFP6B.79
CMS22CMS25CFP6B.95
CMS09CFP6B.43
EF460761EF460757
EF460759EF460760EF460755
EF460762CMS40CFP6B.85
CFP6S.22CFP6S.30CFP6S.21
CFP6S.4CFP6S.3
CFP6S.17CFP6B.86
CFP6S.5CFP6S.2
CFP6S.32CMS19CFP6B.19
CFP6B.36CFP6B.16CFP6B.34
CMS29CMS32
CFP6B.39CFP6S.20
CMS34CFP6S.29
CFP6B.110CFP6B.7CFP6B.18CMS31
OB27B34CFP6B.64
Odontella sinensisCFP6B.51Helicotheca tamensis
CFP6B.44Biddulphia sp.
CFP6B.90CFP6B.93
Melosira octogonaCMS53
CFP6B.87OB27BB22
CMS03CFP6B.15CFP6B.46
CFP6B.97CFP6B.48
CFP6B.105Bolidomonas pacifica
Bolidomonas mediterraneaCFP6B.45
OB27SS51CFP6B.5
CFP6B.82CFP6B.59
CFP6S.33CFP6S.34CFP6S.35
CFP6S.39CFP6S.43
CFP6S.31CFP6S.37CFP6B.56, CFP6S.44, CFP6S.45CFP6B.89CFP6B.81
CFP6S.19CFP6B.78CFP6S.25CFP6B.103CFP6S.49CFP6B.107CFP6S.50CFP6B.106
CFP6S.12CFP6S.10CFP6B.88, CFP6B.94, CFP6B.101, CFP6B.108, CFP6B.109Pterocladia filiformisCFP6B.98CFP6B.99CFP6B.91CFP6S.42CFP6S.36CFP6B.92
Ahnfeltia plicataCMS21
CFP6B.37
Skeletonema tropicumSkeletonema tropicum
Skeletonema tropicum
Thalassiosira antarctica
Skeletonema menzelii
CMS 08 Skeletonema grethae CMS 46,47 Skeletonema tropicum
Skeletonema tropicum
Thalassiosira frauenfeldii
Skeletonema costatum
Thalassiosira eccentrica
Thalassiosira nordenskioeldii
Thalassiosira concavivscula
Thalassiosira anguste-lineata
Papilliocellulus elegansPapilliocellulus elegans
Thalassiosira nordenskioeldii
Planktoniella sol
Chaetoceros neogracile
Skeletonema tropicum
18S rRNA BLASTn IDpsbA haplotype diversity
centr
ics
8370
66
96
99
9958
85100
79
77
70
87
61
9983
78
56
85
84
100
100
72
53
54
Fig. 8. Haplotype diversity of all psbA sequences obtained from cultures, environmental clones and GenBank. Evolutionary distances determined using neighbor-joining analysis with an uncorrected p-distance. psbA sequences amplified from unialgal diatom cultures are indicated by bold letters and putatively identified (right) based on 18S rRNA BLASTn results. Diatoms are classified as raphid pennate, araphid pennate and centric. Environmental sequences were processed from the Cape Fear River Plume (CFP) surface (S) and bottom (B) water samples. The black circle indicates the monophyletic Phylum Bacillariophyta (diatoms) clade.
CFP6B.71CFP6B.73CFP6B.74CFP6B.75
CFP6S.1CFP6S.41CFP6S.40
CFP6S.11CFP6B.100CFP6B.104
CFP6B.102CMS41
CMS18CFP6B.22
CFP6B.6CFP6B.47
CMS01CFP6S.51AY176629
CMS11CMS 39, CMS 44CMS07
CMS14CMS24
CMS06CMS43
CFP6B.24CFP6B.80
CFP6B.76CFP6B.77
CFPB6.61CFP6B.49, CFP6.53CFP6B.54CFP6B.13
CFP6B.14CFP6B.69
CMS42CFP6B.65CFP6B.67
Navicula sp.
Navicula sp.
Navicula phyllepta
Cylindrotheca closterium
Cylindrotheca closterium
Navicula sp.
Navicula cyrptpcephala
Pleurosigma planktonicum
CFP6B.58Navicula salinicola
CMS04CMS13
CFP6B.52Phaeodactylum tricornutum
CMS30CFP6B.38CFP6B.41CFP6B.40
CFP6S.9CFP6S.14CMS20CFP6S.13CFP6B.9CFP6S.46
CFP6S.15OB27SS59
CFP6B.84OB27B26
Asterionellopsis glacialis (CA, USA)Asterionellopsis glacialis (Black Sea)
CMS45CFP6B.83
CMS52CFP6S.38
CMS35CMS02
OB27BB43Bumilleriopsis filiformis
Tribonema aequaleGonyostomum semen
Fibrocapsa japonicaOB27SS28
Aureococcus anophagefferensCFP6B.33
OB27SS62CFP6B.72CFP6S.16
Tetraselmis sp.Chlorosarcinopsis gelatinosa
Geminella terricolaCFP6B.68
Chrysochromulina polylepisPleurochrysis carterae
Chrysotila lamellosaEmiliana huxleyi
Phaeocystis antarcticaPavlova gyrans
Pyramonas obovataRhodomonas salina
Protomonas sulcataHemiselmis andersonii
Porphyridium aerugineiumCumagloia andersonii
0.005 substitutions/site
Nitzschia communis
Leptocylindrus sp.
Skeletonema tropicum
Licmopha abbreviata
raph
id p
enna
tece
ntric
arap
hid
penn
ate
arap
hid
penn
ate
Rhodophyta
Cryptophyta
Haptophyta
Chlorophyta
Stramenopiles
Chlorophyta
81
6368
10083
99
6765
100
10074
8989
9992
56
100
98
7995
10051
10098
1009062
9893
65
10093
67
969573
52
8587
10092
100100
94100
Appendix 1. Diatom psbA sequences generated with the dsF/dsR primer and analyzed in this study from CMS and CCMP diatom cultures, CFP6 clone library and GenBank diatom sequences.
Sequence
I.D. Centric/Pennate Origin Clone/ Direct psbA GenBank Acc. No.
Cultured Diatoms Thalassiosira pseudonana Centric GenBank N/A EF067921 Odontella sinensis Centric GenBank N/A Z67753 Phaeodactylum tricornutum Raphid Pennate GenBank N/A EF067920 Asterionellopsis glacialis (CA) Araphid Pennate CCMP134 D XXXXXXXXXXX A. glacialis (Black Sea) Araphid Pennate CCMP135 D XXXXXXXXXXX Biddulphia sp. Centric CCMP147 D XXXXXXXXXXX Melosira octogana Centric CCMP483 D XXXXXXXXXXX Helicotheca tamensis Centric CCMP824 D XXXXXXXXXXX Navicula salinicola Raphid Pennate CCMP1730 D XXXXXXXXXXX CMS01 CMS D XXXXXXXXXXX CMS02 CMS D XXXXXXXXXXX CMS03 CMS D XXXXXXXXXXX CMS04 CMS D XXXXXXXXXXX CMS06 CMS D XXXXXXXXXXX CMS07 CMS D XXXXXXXXXXX CMS08 CMS D XXXXXXXXXXX CMS09 CMS D XXXXXXXXXXX CMS10 CMS D XXXXXXXXXXX CMS11 CMS D XXXXXXXXXXX CMS13 CMS D XXXXXXXXXXX CMS14 CMS D XXXXXXXXXXX
55
CMS18 CMS D XXXXXXXXXXX CMS19 CMS D XXXXXXXXXXX CMS20 CMS D XXXXXXXXXXX CMS21 CMS D XXXXXXXXXXX CMS22 CMS D XXXXXXXXXXX CMS23 CMS D XXXXXXXXXXX CMS24 CMS D XXXXXXXXXXX CMS25 CMS D XXXXXXXXXXX CMS26 CMS D XXXXXXXXXXX CMS27 CMS D XXXXXXXXXXX CMS29 CMS D XXXXXXXXXXX CMS30 CMS D XXXXXXXXXXX CMS31 CMS D XXXXXXXXXXX CMS32 CMS D XXXXXXXXXXX CMS33 CMS D XXXXXXXXXXX CMS34 CMS D XXXXXXXXXXX CMS35 CMS D XXXXXXXXXXX CMS38 CMS D XXXXXXXXXXX CMS39 CMS D XXXXXXXXXXX CMS40 CMS D XXXXXXXXXXX CMS41 CMS D XXXXXXXXXXX CMS42 CMS D XXXXXXXXXXX CMS43 CMS D XXXXXXXXXXX CMS44 CMS D XXXXXXXXXXX CMS45 CMS D XXXXXXXXXXX CMS46 CMS D XXXXXXXXXXX CMS47 CMS D XXXXXXXXXXX CMS48 CMS D XXXXXXXXXXX
56
CMS49 CMS D XXXXXXXXXXX CMS50 CMS D XXXXXXXXXXX CMS51 CMS D XXXXXXXXXXX CMS52 CMS D XXXXXXXXXXX CMS53 CMS D XXXXXXXXXXX CMS55 CMS D XXXXXXXXXXX Environmental DNA Sequences OB27B26 N/A OB27 C XXXXXXXXXXX OB27B34 N/A OB27 C XXXXXXXXXXX OBO27BB22 N/A OB27 C XXXXXXXXXXX OB27BB43 N/A OB27 C XXXXXXXXXXX OB27SS28 N/A OB27 C XXXXXXXXXXX OB27SS51 N/A OB27 C XXXXXXXXXXX OB27SS59 N/A OB27 C XXXXXXXXXXX OB27SS62 N/A OB27 C XXXXXXXXXXX CFP6B.5 N/A CFP6 C XXXXXXXXXXX CFP6B.6 N/A CFP6 C XXXXXXXXXXX CFP6B.7 N/A CFP6 C XXXXXXXXXXX CFP6B.8 N/A CFP6 C XXXXXXXXXXX CFP6B.9 N/A CFP6 C XXXXXXXXXXX CFP6B.13 N/A CFP6 C XXXXXXXXXXX CFP6B.14 N/A CFP6 C XXXXXXXXXXX CFP6B.15 N/A CFP6 C XXXXXXXXXXX CFP6B.16 N/A CFP6 C XXXXXXXXXXX CFP6B.18 N/A CFP6 C XXXXXXXXXXX CFP6B.19 N/A CFP6 C XXXXXXXXXXX CFP6B.22 N/A CFP6 C XXXXXXXXXXX
57
CFP6B.24 N/A CFP6 C XXXXXXXXXXX CFP6B.33 N/A CFP6 C XXXXXXXXXXX CFP6B.34 N/A CFP6 C XXXXXXXXXXX CFP6B.36 N/A CFP6 C XXXXXXXXXXX CFP6B.37 N/A CFP6 C XXXXXXXXXXX CFP6B.38 N/A CFP6 C XXXXXXXXXXX CFP6B.39 N/A CFP6 C XXXXXXXXXXX CFP6B.40 N/A CFP6 C XXXXXXXXXXX CFP6B.41 N/A CFP6 C XXXXXXXXXXX CFP6B.42 N/A CFP6 C XXXXXXXXXXX CFP6B.43 N/A CFP6 C XXXXXXXXXXX CFP6B.44 N/A CFP6 C XXXXXXXXXXX CFP6B.45 N/A CFP6 C XXXXXXXXXXX CFP6B.46 N/A CFP6 C XXXXXXXXXXX CFP6B.47 N/A CFP6 C XXXXXXXXXXX CFP6B.48 N/A CFP6 C XXXXXXXXXXX CFP6B.49 N/A CFP6 C XXXXXXXXXXX CFP6B.51 N/A CFP6 C XXXXXXXXXXX CFP6B.52 N/A CFP6 C XXXXXXXXXXX CFP6B.53 N/A CFP6 C XXXXXXXXXXX CFP6B.54 N/A CFP6 C XXXXXXXXXXX CFP6B.56 N/A CFP6 C XXXXXXXXXXX CFP6B.58 N/A CFP6 C XXXXXXXXXXX CFP6B.59 N/A CFP6 C XXXXXXXXXXX CFP6B.60 N/A CFP6 C XXXXXXXXXXX CFP6B.61 N/A CFP6 C XXXXXXXXXXX CFP6B.62 N/A CFP6 C XXXXXXXXXXX CFP6B.63 N/A CFP6 C XXXXXXXXXXX
58
CFP6B.64 N/A CFP6 C XXXXXXXXXXX CFP6B.65 N/A CFP6 C XXXXXXXXXXX CFP6B.67 N/A CFP6 C XXXXXXXXXXX CFP6B.68 N/A CFP6 C XXXXXXXXXXX CFP6B.69 N/A CFP6 C XXXXXXXXXXX CFP6B.71 N/A CFP6 C XXXXXXXXXXX CFP6B.72 N/A CFP6 C XXXXXXXXXXX CFP6B.73 N/A CFP6 C XXXXXXXXXXX CFP6B.74 N/A CFP6 C XXXXXXXXXXX CFP6B.75 N/A CFP6 C XXXXXXXXXXX CFP6B.76 N/A CFP6 C XXXXXXXXXXX CFP6B.77 N/A CFP6 C XXXXXXXXXXX CFP6B.78 N/A CFP6 C XXXXXXXXXXX CFP6B.79 N/A CFP6 C XXXXXXXXXXX CFP6B.80 N/A CFP6 C XXXXXXXXXXX CFP6B.81 N/A CFP6 C XXXXXXXXXXX CFP6B.82 N/A CFP6 C XXXXXXXXXXX CFP6B.83 N/A CFP6 C XXXXXXXXXXX CFP6B.84 N/A CFP6 C XXXXXXXXXXX CFP6B.85 N/A CFP6 C XXXXXXXXXXX CFP6B.86 N/A CFP6 C XXXXXXXXXXX CFP6B.87 N/A CFP6 C XXXXXXXXXXX CFP6B.88 N/A CFP6 C XXXXXXXXXXX CFP6B.89 N/A CFP6 C XXXXXXXXXXX CFP6B.90 N/A CFP6 C XXXXXXXXXXX CFP6B.91 N/A CFP6 C XXXXXXXXXXX CFP6B.92 N/A CFP6 C XXXXXXXXXXX CFP6B.93 N/A CFP6 C XXXXXXXXXXX
59
CFP6B.94 N/A CFP6 C XXXXXXXXXXX CFP6B.95 N/A CFP6 C XXXXXXXXXXX CFP6B.96 N/A CFP6 C XXXXXXXXXXX CFP6B.97 N/A CFP6 C XXXXXXXXXXX CFP6B.98 N/A CFP6 C XXXXXXXXXXX CFP6B.99 N/A CFP6 C XXXXXXXXXXX CFP6B.100 N/A CFP6 C XXXXXXXXXXX CFP6B.101 N/A CFP6 C XXXXXXXXXXX CFP6B.102 N/A CFP6 C XXXXXXXXXXX CFP6B.103 N/A CFP6 C XXXXXXXXXXX CFP6B.104 N/A CFP6 C XXXXXXXXXXX CFP6B.105 N/A CFP6 C XXXXXXXXXXX CFP6B.106 N/A CFP6 C XXXXXXXXXXX CFP6B.107 N/A CFP6 C XXXXXXXXXXX CFP6B.108 N/A CFP6 C XXXXXXXXXXX CFP6B.109 N/A CFP6 C XXXXXXXXXXX CFP6B.110 N/A CFP6 C XXXXXXXXXXX CFP6S.1 N/A CFP6 C XXXXXXXXXXX CFP6S.2 N/A CFP6 C XXXXXXXXXXX CFP6S.3 N/A CFP6 C XXXXXXXXXXX CFP6S.4 N/A CFP6 C XXXXXXXXXXX CFP6S.5 N/A CFP6 C XXXXXXXXXXX CFP6S.6 N/A CFP6 C XXXXXXXXXXX CFP6S.8 N/A CFP6 C XXXXXXXXXXX CFP6S.9 N/A CFP6 C XXXXXXXXXXX CFP6S.10 N/A CFP6 C XXXXXXXXXXX CFP6S.11 N/A CFP6 C XXXXXXXXXXX CFP6S.12 N/A CFP6 C XXXXXXXXXXX
60
CFP6S.13 N/A CFP6 C XXXXXXXXXXX CFP6S.14 N/A CFP6 C XXXXXXXXXXX CFP6S.15 N/A CFP6 C XXXXXXXXXXX CFP6S.16 N/A CFP6 C XXXXXXXXXXX CFP6S.17 N/A CFP6 C XXXXXXXXXXX CFP6S.18 N/A CFP6 C XXXXXXXXXXX CFP6S.19 N/A CFP6 C XXXXXXXXXXX CFP6S.20 N/A CFP6 C XXXXXXXXXXX CFP6S.21 N/A CFP6 C XXXXXXXXXXX CFP6S.22 N/A CFP6 C XXXXXXXXXXX CFP6S.24 N/A CFP6 C XXXXXXXXXXX CFP6S.25 N/A CFP6 C XXXXXXXXXXX CFP6S.29 N/A CFP6 C XXXXXXXXXXX CFP6S.30 N/A CFP6 C XXXXXXXXXXX CFP6S.31 N/A CFP6 C XXXXXXXXXXX CFP6S.32 N/A CFP6 C XXXXXXXXXXX CFP6S.33 N/A CFP6 C XXXXXXXXXXX CFP6S.34 N/A CFP6 C XXXXXXXXXXX CFP6S.35 N/A CFP6 C XXXXXXXXXXX CFP6S.36 N/A CFP6 C XXXXXXXXXXX CFP6S.37 N/A CFP6 C XXXXXXXXXXX CFP6S.38 N/A CFP6 C XXXXXXXXXXX CFP6S.39 N/A CFP6 C XXXXXXXXXXX CFP6S.40 N/A CFP6 C XXXXXXXXXXX CFP6S.41 N/A CFP6 C XXXXXXXXXXX CFP6S.42 N/A CFP6 C XXXXXXXXXXX CFP6S.43 N/A CFP6 C XXXXXXXXXXX CFP6S.44 N/A CFP6 C XXXXXXXXXXX
61
62
CFP6S.45 N/A CFP6 C XXXXXXXXXXX CFP6S.46 N/A CFP6 C XXXXXXXXXXX CFP6S.47 N/A CFP6 C XXXXXXXXXXX CFP6S.48 N/A CFP6 C XXXXXXXXXXX CFP6S.49 N/A CFP6 C XXXXXXXXXXX CFP6S.50 N/A CFP6 C XXXXXXXXXXX CFP6S.51 N/A CFP6 C XXXXXXXXXXX CFP6S.52 N/A CFP6 C XXXXXXXXXXX Uncultured algal clone RED122-4-8 N/A Zeidner et al. 2003 N/A AY176629 Uncultured isolate JC306 N/A Jiaozhou Bay, N. China N/A EF460704 Uncultured isolate JD819 N/A Jiaozhou Bay, N. China N/A EF460755 Uncultured isolate JA126 N/A Jiaozhou Bay, N. China N/A EF460757 Uncultured isolate JD710 N/A Jiaozhou Bay, N. China N/A EF460759 Uncultured isolate JD810 N/A Jiaozhou Bay, N. China N/A EF460760 Uncultured isolate JD828 N/A Jiaozhou Bay, N. China N/A EF460761 Uncultured isolate JD815 N/A Jiaozhou Bay, N. China N/A EF460762
Appendix 2. Other photosynthetic eukaryote psbA sequences obtained from GenBank and pure cultures from culture collections analyzed in this study for analysis of primer specificity outside Phylum Bacillariophyta (diatoms). Taxon Strain psbA GenBank No.
Bolidophyceae Bolidomonas mediterranea CCMP1867 XXXXXXXX Bolidomonas pacifica CCMP1866 XXXXXXXX
Chlorophyta Chlorosarcinopsis gelatinosa CCMP1511 XXXXXXXX Geminella terricola UTEX2540 XXXXXXXX
Chrysomerophyceae Chrysowaernella hieroglyphica SCCAP K-0368 XXXXXXXX
Chrysophyceae Krematstochrysopsis sp. CCMP260 XXXXXXXX Ochromonas sphaerocystis CCMP586 XXXXXXXX
Cryptophyceae Hemiselmis andersenii CCMP644 XXXXXXXX Proteomonas sulcata CCMP704 XXXXXXXX Rhodomonas salina CCMP1319 XXXXXXXX
Eustigmatophyceae Goniochloris sculpta SAG29.96 XXXXXXXX Unidentified coccoid sp. N/A XXXXXXXX
Dinophyceae Amphidinium gibbosum CCMP120 XXXXXXXX Symbiodinum sp.1 N/A XXXXXXXX
Pelagophyceae Aureococcus anophagefferens CCMP1707 XXXXXXXX
Phaeophyceae Laminaria sp. N/A XXXXXXXX
Pinguiophyceae Pinguiochrysis pyriformis MBIC 10872 XXXXXXXX
Prasinophyceae Pyramimonas obovata CCMP722 XXXXXXXX
63
Tetraselmis sp. CCMP908 XXXXXXXX
Prymnesiophyceae Chrysochromulina polylepis N/A AJ575572 Chrysotila lamellosa CCMP1307 XXXXXXX Emiliania huxleyi PCC 1516 XXXXXXXX Pavlova gyrans N/A AJ575575 Phaeocystis antarctica N/A AY119756 Pluerochrysis carterae N/A AY119757 Rhaphidopyceae Fibrocapsa japonica Gonyostomum semen Rhodophyta Ahnfeltia plicata N/A XXXXXXXX Cumagloia andersonii UTEX1694 XXXXXXXX Porphyridium aerugineum CCMP674 XXXXXXXX Pterocladia lucida N/A XXXXXXXX
Xanthophyceae Bumilleriopsis filiformis N/A X79223 Chloridella miniata UTEX491 XXXXXXXX Chlorocloster engadinensis UTEX307 XXXXXXXX Sphaerosorus compositus CCAP876/1 XXXXXXXX Tribonema aequale N/A AY528860 Tribonema vulgare SCCAPK-0339 XXXXXXXX 1 ex. Siderastrea sp.
64