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Phylogeny and Molecular Evolution of the Green Algae

TLDR
Current understanding of organelle genome evolution in the green algae is summarized, genomic insights into the ecology of oceanic picoplanktonic prasinophytes, molecular mechanisms underlying the evolution of complexity in volvocine green algae, and the Evolution of genetic codes and the translational apparatus in green seaweeds are summarized.
Abstract
The green lineage (Viridiplantae) comprises the green algae and their descendants the land plants, and is one of the major groups of oxygenic photosynthetic eukaryotes. Current hypotheses posit the early divergence of two discrete clades from an ancestral green flagellate. One clade, the Chlorophyta, comprises the early diverging prasinophytes, which gave rise to the core chlorophytes. The other clade, the Streptophyta, includes the charophyte green algae from which the land plants evolved. Multi-marker and genome scale phylogenetic studies have greatly improved our understanding of broad-scale relationships of the green lineage, yet many questions persist, including the branching orders of the prasinophyte lineages, the relationships among core chlorophyte clades (Chlorodendrophyceae, Ulvophyceae, Trebouxiophyceae and Chlorophyceae), and the relationships among the streptophytes. Current phylogenetic hypotheses provide an evolutionary framework for molecular evolutionary studies and comparative genomics. This review summarizes our current understanding of organelle genome evolution in the green algae, genomic insights into the ecology of oceanic picoplanktonic prasinophytes, molecular mechanisms underlying the evolution of complexity in volvocine green algae, and the evolution of genetic codes and the translational apparatus in green seaweeds. Finally, we discuss molecular evolution in the streptophyte lineage, emphasizing the genetic facilitation of land plant origins.

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Critical Reviews in Plant Sciences, 31:1–46, 2012
Copyright
C
Taylor & Francis Group, LLC
ISSN: 0735-2689 print / 1549-7836 online
DOI: 10.1080/07352689.2011.615705
Phylogeny and Molecular Evolution of the Green Algae
Frederik Leliaert,
1
David R. Smith,
2
Herv
´
eMoreau,
3
Matthew D. Herron,
4
Heroen Verbruggen,
1
Charles F. Delwiche,
5
and Olivier De Clerck
1
1
Phycology Research Group, Biology Department, Ghent University 9000, Ghent, Belgium
2
Canadian Institute for Advanced Research, Evolutionary Biology Program, Department of Botany,
University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada
3
Observatoire Oc
´
eanologique, CNRS–Universit
´
e Pierre et Marie Curie 66651, Banyuls sur Mer, France
4
Department of Zoology, University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada
5
Department of Cell Biology and Molecular Genetics and the Maryland Agricultural Experiment Station,
University of Maryland, College Park, MD 20742, USA
Table of Contents
I. THE NATURE AND ORIGINS OF GREEN ALGAE AND LAND PLANTS
.............................................................................2
II. GREEN LINEAGE RELATIONSHIPS
..........................................................................................................................................................5
A. Morphology, Ultrastructure and Molecules
...............................................................................................................................................5
B. Phylogeny of the Green Lineage
...................................................................................................................................................................6
1. Two Main Lineages: Chlorophyta and Streptophyta
........................................................................................................................6
2. Early Diverging Chlorophyta: The Prasinophytes
.............................................................................................................................6
3. The Core Chlorophyta: Ecological and Morphological Diversification
....................................................................................9
4. Streptophyta: Charophyte Green Algae and the Origin of Land Plants
.................................................................................. 15
III. SPREAD OF GREEN GENES IN OTHER EUKARYOTES
............................................................................................................ 17
IV. GREEN ALGAL EVOLUTION: INSIGHTS FROM GENES AND GENOMES
................................................................... 19
A. Organelle Genome Evolution
...................................................................................................................................................................... 20
B. Ecology and Molecular Evolution of Oceanic Picoplanktonic Prasinophytes
........................................................................... 25
C. Genomic Insights into the Evolution of Complexity in Volvocine Green Algae
...................................................................... 26
D. Genetic Codes and the Translational Apparatus in Green Seaweeds ............................................................................................ 29
E. Molecular Evolution in the Streptophyta and the Origin of Land Plants
..................................................................................... 30
V. CONCLUSIONS AND PERSPECTIVES
................................................................................................................................................... 31
ACKNOWLEDGMENTS
................................................................................................................................................................................................ 32
REFERENCES
..................................................................................................................................................................................................................... 32
Address correspondence to Frederik Leliaert, Phycology Research Group, Biology Department, Ghent University, 9000, Ghent, Belgium.
E-mail: frederik.leliaert@gmail.com
1
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2 F. LELIAERT ET AL.
The green lineage (Viridiplantae) comprises the green algae and
their descendants the land plants, and is one of the major groups of
oxygenic photosynthetic eukaryotes. Current hypotheses posit the
early divergence of two discrete clades from an ancestral green flag-
ellate. One clade, the Chlorophyta, comprises the early diverging
prasinophytes, which gave rise to the core chlorophytes. The other
clade, the Streptophyta, includes the charophyte green algae from
which the land plants evolved. Multi-marker and genome scale
phylogenetic studies have greatly improved our understanding of
broad-scale relationships of the green lineage, yet many questions
persist, including the branching orders of the prasinophyte lin-
eages, the relationships among core chlorophyte clades (Chloroden-
drophyceae, Ulvophyceae, Trebouxiophyceae and Chlorophyceae),
and the relationships among the streptophytes. Current phyloge-
netic hypotheses provide an evolutionary framework for molecular
evolutionary studies and comparative genomics. This review sum-
marizes our current understanding of organelle genome evolution
in the green algae, genomic insights into the ecology of oceanic
picoplanktonic prasinophytes, molecular mechanisms underlying
the evolution of complexity in volvocine green algae, and the evo-
lution of genetic codes and the translational apparatus in green
seaweeds. Finally, we discuss molecular evolution in the strepto-
phyte lineage, emphasizing the genetic facilitation of land plant
origins.
Keywords Chlorophyta, Charophyta, endosymbiosis, molecular evo-
lution, origin of embryophytes, Prasinophyceae, phy-
logeny, Streptophyta
I. THE NATURE AND ORIGINS OF GREEN ALGAE
AND LAND PLANTS
The green lineage or Viridiplantae
1
includes the green algae
and land plants, and is one of the major groups of oxygenic pho-
tosynthetic eukaryotes. Green algae are diverse and ubiquitous
in aquatic and some terrestrial habitats, and they have played
a crucial role in the global ecosystem for hundreds of millions
of years (Falkowski et al., 2004; O’Kelly, 2007; Leliaert et al.,
2011). The evolution of land plants from a green algal ancestor
was a key event in the history of life and has led to dramatic
changes in the earth’s environment, initiating the development
of the entire terrestrial ecosystem (Kenrick and Crane, 1997).
The green lineage originated following an endosymbiotic
event in which a heterotrophic eukaryotic host cell captured a
cyanobacterium that became stably integrated and ultimately
turned into a plastid (Archibald, 2009; Keeling, 2010). This
primary endosymbiosis, which likely happened between 1 and
1.5 billion years ago (Hedges et al., 2004; Yoon et al., 2004),
marked the origin of the earliest oxygenic photosynthetic eu-
karyotes. The subsequent diversification of this primary plastid-
1
Various names have been proposed for the lineage comprising the green
algae and land plants: “Viridiplantae” or “Viridaeplantae” (Cavalier-Smith,
1981, 1998), “Chlorobiota” or “Chlorobionta” (Jeffrey, 1971, 1982), “Chloro-
plastida” (Adl et al. 2005), or simply “green plants” (Sluiman et al., 1983) or
“green lineage.
containing eukaryote gave rise to the green lineage, as well as
the red algae and the glaucophytes. From this starting point, pho-
tosynthesis spread widely among diverse eukaryotic protists via
secondary and tertiary endosymbioses, which involved captures
of either green or red algae by non-photosynthetic protists (Keel-
ing, 2010). Secondary endosymbioses involving green algae as
the autotrophic partner have given rise to three groups of algae:
the chlorarachniophytes, the photosynthetic euglenids and the
“green” dinoflagellates (see section III. Spread of green genes in
other eukaryotes). The other eukaryotic algal groups, the cryp-
tophytes, haptophytes, photosynthetic stramenopiles (e.g., di-
atoms, chrysophytes and brown seaweeds) and dinoflagellates,
have acquired plastids from a red algal ancestor, either by a sin-
gle or multiple endosymbiotic events (Archibald, 2009; Bodyl
et al., 2009; Baurain et al., 2010).
The green lineage is ancient, and dating its origin has been
a difficult task because of the sparse fossil record of the group.
The earliest fossils attributed to green algae date from the Pre-
cambrian (ca. 1200 mya) (Tappan, 1980; Knoll, 2003). The na-
ture of these early fossils, however, remains controversial (e.g.,
Cavalier-Smith, 2006). The resistant outer walls of prasinophyte
cysts (phycomata) are well preserved in fossil deposits and es-
pecially abundant and diverse in the Paleozoic era (ca. 250–
540 mya) (Parke et al., 1978; Tappan, 1980; Colbath,
1983). A filamentous fossil (Proterocladus) from middle
Neoproterozoic deposits (ca. 750 mya) has been attributed
to siphonocladous green algae (Cladophorales) (Butterfield
et al., 1994; Butterfield, 2009), while the oldest reli-
able records of the siphonous seaweeds (Bryopsidales,
Dasycladales) and stoneworts (Charophyceae) are from
the Paleozoic (Hall and Delwiche, 2007; Verbruggen et
al., 2009a). The earliest land plant fossils are Mid-
Ordovician in age (ca. 460 mya) (Kenrick and Crane, 1997;
Steemans et al., 2009). Molecular clock analyses have esti-
mated the origin of the green lineage between 700 and 1500
mya (Douzery et al., 2004; Hedges et al., 2004; Berney and
Pawlowski, 2006; Roger and Hug, 2006; Herron et al., 2009).
These estimates are sensitive to differences in methodology and
interpretation of fossils and tend to yield older dates than are
well supported by the fossil record. This could be attributable
to miscalibration of the molecular clock estimates or to tapho-
nomic bias and the difficulty of interpreting fossils with no
modern exemplars. Molecular phylogenetic evidence has pro-
vided a substantially improved understanding of the relation-
ships among major lineages. Reconstruction of ancestral char-
acter states could assist in the reinterpretation of known spec-
imens of uncertain affinity, and this, combined with continued
paleontological investigation, holds out hope for reconciliation
of molecular and fossil evidence.
Green algae are characterized by a number of distinct fea-
tures, many of which are also shared with the land plants (van
den Hoek et al., 1995; Graham et al., 2009). The chloroplasts
are enclosed by a double membrane with thylakoids grouped
in lamellae, and contain chlorophyll a and b along with a
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MOLECULAR EVOLUTION OF GREEN ALGAE 3
set of accessory pigments such as carotenes and xanthophylls.
Pyrenoids, when present, are embedded within the chloroplast
and are surrounded by starch, which is the main reserve polysac-
charide. Most green algae have firm cell walls with a fiber matrix
generally composed of cellulose. The flagellate cells are isokont,
which means that the two flagella are similar in structure, al-
though they may differ in length. The flagellar transition zone
(i.e., the region between the flagellum and its basal body) is
typically characterized by a stellate structure, which is a nine-
pointed star, visible in cross section using an electron micro-
scope, linking nine pairs of microtubules (Melkonian, 1984).
Despite their many unifying features, green algae exhibit
a remarkable variation in morphology and ecology reflect-
ing their evolutionary diversification. Morphological diversity
ranges from the smallest known free-living eukaryote, Ostreo-
coccus tauri, to large, multicellular life forms (Figure 1). Green
algae are especially abundant and diverse in freshwater envi-
ronments, including lakes, ponds, streams and wetlands (John
et al., 2002; Wehr and Sheath, 2003), where they may form
nuisance blooms under conditions of nutrient pollution (Malkin
et al., 2010). Only two green algal groups are well represented
in marine environments. The green seaweeds (Ulvophyceae)
abound in coastal habitats. Some green seaweeds (mainly Ulva)
can form extensive, free-floating coastal blooms, called ‘green
tides’ (Leliaert et al., 2009c); others, like Caulerpa and Codium
are notorious for their invasive nature (Meinesz and Hesse, 1991;
Jousson et al., 2000; Lapointe et al., 2005). The prasinophytes
are planktonic green algae that occur mainly in oceanic environ-
ments and are especially abundant in more eutrophic, near-shore
waters, where they can form monospecific blooms (O’Kelly
et al., 2003; Not et al., 2004). Embryophytes have dominated
the terrestrial environment since the late Ordovician, and some
have become secondarily adapted to aquatic environments, in-
cluding holoaquatic marine species that form extensive beds of
seagrass. Several green algae have adapted to highly specialised
or extreme environments, such as hot or cold deserts (Lewis
and Lewis, 2005; De Wever et al., 2009; Schmidt et al., 2011),
hypersaline habitats (Vinogradova and Darienko, 2008), acidic
waters with extreme concentrations of heavy metals (Zettler
et al., 2002), marine deep waters (Zechman et al., 2010) and
deep-sea hydrothermal vents (Edgcomb et al., 2002). Some
green algal groups, i.e., Trentepohliales, are exclusively terres-
trial and never found in aquatic environments (L
´
opez-Bautista
et al., 2006). Several lineages have engaged in symbiosis with a
diverse range of eukaryotes, including fungi to form lichens, cil-
iates, foraminifers, cnidarians, molluscs (nudibranchs and giant
clams) and vertebrates (Friedl and Bhattacharya, 2002; Lewis
and Muller-Parker, 2004; Kovacevic et al., 2010; Kerney et al.,
2011). Others have evolved an obligate heterotrophic life style as
parasites or free-living species (Joubert and Rijkenberg, 1971;
Rumpf et al., 1996; Huss et al., 1999; Nedelcu, 2001). The
heterotrophic green alga Prototheca, which grows in sewage
and soil, can cause infections in humans and animals known as
protothecosis (Sudman, 1974).
Several green algae serve as model systems or are of eco-
nomic importance. Melvin Calvin used cultures of Chlorella
to elucidate the light-independent reactions of photosynthesis.
Now known as the Calvin cycle (Calvin and Benson, 1948).
Transplant experiments with the giant-celled Acetabularia, con-
ducted by Joachim H
¨
ammerling, demonstrated that the nucleus
of a cell contains the genetic information that directs cellular
development, and postulated the existence of messenger RNA
before its structure was determined (H
¨
ammerling, 1953). Ac-
etabularia, along with other giant-celled green algae (Valonia,
Chara and Nitella), has also served as an experimental organism
for electro-physiological research and studies of cell morpho-
genesis (Menzel, 1994; Mandoli, 1998; Shepherd et al., 2004;
Bisson et al., 2006; Mine et al., 2008). The charophyte Mougeo-
tia played a key role in outlining the role of phytochrome in
plant development (Winands and Wagner, 1996). The biochem-
istry and physiology of the unicellular, halophilic Dunaliella
salina have been studied in great detail. This alga is among the
most industrially important microalgae because it can produce
massive amounts of β-carotene that can be collected for com-
mercial purposes, and because of its potential as a feedstock for
biofuels production (Oren, 2005; Gouveia and Oliveira, 2009;
Tafresh and Shariati, 2009). The unicellular flagellate Chlamy-
domonas reinhardtii has long been used as a model system
for studying photosynthesis, chloroplast biogenesis, flagellar
assembly and function, cell-cell recognition, circadian rhythm
and cell cycle control because of its well-defined genetics, and
the development of efficient methods for nuclear and chloroplast
transformation (Rochaix, 1995; Harris, 2001; Grossman et al.,
2003; Breton and Kay, 2006). The colonial green alga Volvox
has served as a model for the evolution of multicellularity, cell
differentiation, and colony motility (Kirk, 1998; Kirk, 2003;
Herron and Michod, 2008; Herron et al., 2009).
Analysis of the complete nuclear genome sequence of C.
reinhardtii greatly advanced our understanding of ancient eu-
karyotic features such as the function and biogenesis of chloro-
plasts, flagella and eyespots, and regulation of photosynthe-
sis (Merchant et al., 2007; Kreimer, 2009; Peers et al., 2009).
Genome data are rapidly accumulating and to date seven com-
plete green algal genomes have been sequenced: the prasino-
phytes Ostreococcus tauri (Derelle et al., 2006), O. lucimarinus
(Palenik et al., 2007) and two isolates of Micromonas pusilla
(Worden et al., 2009), the chlorophytes C. reinhardtii (Merchant
et al., 2007) and Volvox carteri (Prochnik et al., 2010), and the
trebouxiophyte Chlorella variabilis (Blanc et al., 2010). Several
other genome projects are ongoing, including the complete se-
quencing of Coccomyxa, Dunaliella, Bathycoccus, Botryococ-
cus and additional Ostreococcus and Micromonas strains (Tiri-
chine and Bowler, 2011). These data provide a great resource for
in-depth analysis of genome organization and the processes of
eukaryotic genome evolution. In addition, green algal genomes
are important sources of information for the evolutionary ori-
gins of plant traits because of their evolutionary relationship to
land plants.
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4 F. LELIAERT ET AL.
FIG. 1. Taxonomical, morphological and ecological diversity among green algae. A: Pterosperma (Pyramimonadales), a marine prasinophyte characterized by
quadriflagellate unicells (photo by Bob Andersen, reproduced under license from microscope.mbl.edu). B: Nephroselmis (Nephroselmidophyceae), a prasinophyte
with bean-shaped cells and two unequal flagella occuring in marine or freshwater environments. C: Palmophyllum (Palmophyllales) forming lobed crusts composed
of coccoid cells embedded in a gelatinous matrix, growing in deep-water marine habitats (photo by Jordi Regas). D: Tetraselmis (Chlorodendrophyceae),
quadriflagellate unicells from marine or freshwater habitats. E: Chlorella (Trebouxiophyceae, Chlorellales), coccoid cells, endosymbiontic inside the single-celled
protozoan Paramecium (photo by Antonio Guill
´
en). F: Oocystis (Trebouxiophyceae, Oocystaceae), small colonies of coccoid cells within a thin mucilaginous
envelope from freshwater habitats (image copyright Microbial Culture Collection, NIES). G: Haematococcus (Chlorophyceae, Chlamydomonadales), a freshwater
biflagellate unicell (photo by William Bourland, reproduced under license from microscope.mbl.edu). H: Pediastrum (Chlorophyceae, Sphaeropleales), a coenobial
colony of non-motile cells arranged in a circular plate, occuring in freshwater habitats. I: Bulbochaete (Chlorophyceae, Oedogoniales), branched filaments with
terminal hair-cells. J: Chaetophora (Chlorophyceae, Chaetophorales), highly branched filaments, occuring in freshwater habitats (H–J: photos by Jason Oyadomari).
K: Ulothrix (Ulvophyceae, Ulotrichales), unbranched filaments from marine or brackish areas (photo by Giuseppe Vago). L: Ulva (Ulvophyceae, Ulvales), sheet-
like plants, mainly from marine habitats (photo by Tom Schils). M: Cladophora (Ulvophyceae, Cladophorales), branched filament with cells containing numerous
chloroplasts and nuclei (photo by Antonio Guill
´
en). N: Boergesenia (Ulvophyceae, Cladophorales), plants composed of giant, multinucleate cells, from tropical
marine habitats (photo by HV). O: Acetabularia (Ulvophyceae, Dasycladales), siphonous plants (i.e. single-celled) differentiated into a stalk and a flattened
cap, with a single giant nucleus situated at the base of the stalk; typically found in subtropical marine habitats (photo by Antoni L
´
opez-Arenas). P: Caulerpa
(Ulvophyceae, Bryopsidophyceae), siphonous plant differentiated into creeping stolons anchored by rhizoids and erect photosynthetic fronds, containing millions
of nuclei; occuring in (sub)tropical marine waters (photo by FL). Q: Klebsormidium (Klebsormidiophyceae), unbranched filamentous charophyte, mainly from
moist terrestrial habits (photo by Jason Oyadomari). R: Spirotaenia, a unicellular charophyte with typical spiral chloroplast; generally growing in acidic freshwater
habitats (photo by Antonio Guill
´
en). S: Nitella (Charophyceae), morphologically complex charophyte from freshwater habitats, consisting of a central stalk
and whorls of branches radiating from nodes that bear oogonia and antheridia (photo by Nadia Abdelahad). T: Micrasterias (Zygnematophyceae, Desmidiales),
characterized by non-motile unicells constricted in two parts with ornamented cell wall; generally found in acidic, oligotrophic freshwater habitats (photo by
Antonio Guill
´
en). U: Coleochaete (Coleochaetophyceae), branched filaments adherent to form a disc-like, parenchymatous thallus; found in freshwater habitats,
often as epiphytes on submerged vascular plants (photo by CFD). (Color figure available online.)
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MOLECULAR EVOLUTION OF GREEN ALGAE 5
Reconstruction of the phylogenetic relationships among
green plants is essential to identifying the innovations under-
lying the diversity of green algae and land plants. Molecular
phylogenetics has dramatically reshaped our views of green al-
gal relationships and evolution. This review summarizes the cur-
rent understanding of green algal phylogeny, focusing primarily
on relationships among the major lineages of green algae, which
are usually classified as divisions, classes and orders. Current
phylogenetic hypotheses have provided an evolutionary frame-
work for molecular evolutionary studies and comparative ge-
nomics. In this review, we highlight a number of topics, includ-
ing the evolution of organellar genomes, ecology and molecular
evolution of marine picoplanktonic prasinophytes, genomic in-
sights into the evolution of complexity in volvocine green algae,
molecular evolution in the green seaweeds, and molecular evo-
lution in the streptophyte green algae and the origin of land
plants.
II. GREEN LINEAGE RELATIONSHIPS
A. Morphology, Ultrastructure and Molecules
Early hypotheses of green algal phylogeny were based on the
concept that evolution follows trends in levels of morphological
complexity (Fritsch, 1935; Fott, 1971). Unicellular flagellates
were believed to have initially evolved into non-motile unicells
(coccoid) and loose packets of cells (sarcinoid), followed by
various multicellular forms and siphonous algae. This hierarchy
reflected the view that the morphologies that are organized in
two- and three-dimensional space require more elaborate devel-
opmental controls, and hence would be expected to appear later
in an evolutionary sequence. In this view the land plants were de-
rived from more complex, filamentous green algae (Blackman,
1900; Pascher, 1914).
A large amount of new information was gathered in the 1970s
and 1980s, mainly from investigations of the fine structures of
green algal cells and life cycles (Round, 1984). These data led
to a thorough reevaluation of evolutionary relationships and a
revised classification of green algae, primarily based on flag-
ellar ultrastructure and processes of mitosis and cell division
(Picket-Heaps and Marchant, 1972; Melkonian, 1982; Mattox
and Stewart, 1984; Melkonian, 1984; O’Kelly and Floyd, 1984a;
O’Kelly and Floyd, 1984b; van den Hoek et al., 1988). These
features, which apply to most (but not all) green algae, were be-
lieved to accurately reflect phylogenetic relationships because
of their involvement in fundamental processes of cell replication
and cell motility, and thus to be less liable to convergent evolu-
tion than gross morphological traits. Ultrastructure-based phylo-
genetic hypotheses posited an early diversification of flagellate
unicells, resulting in a multitude of ancient lineages of flag-
ellates, some of which then evolved into more complex green
algae. Although ultrastructural data have laid the foundations
for a natural classification of the green algae, analyses of these
data have not resolved the phylogenetic relationships among the
main green algal lineages.
The introduction of molecular phylogenetic methods pro-
vided a new framework for reconstructing the evolutionary his-
tory of the green lineage. Analyses of DNA sequence data took
a start in the mid 1980s with the first phylogenies of green plants
inferred from 5.8S nrDNA sequences (Hori et al., 1985; Hori
and Osawa, 1987), soon followed by 18S and 28S nrDNA se-
quence analyses (Gunderson et al., 1987; Perasso et al., 1989;
Buchheim et al., 1990; Zechman et al., 1990; Chapman et al.,
1991; Mishler et al., 1992; Chapman et al., 1998). Riboso-
mal sequences were chosen at the time because enough RNA
could be obtained for direct sequencing and (later) because re-
gions of the gene were conserved enough to make universal
primers. Ribosomal RNA is also found in all known living cells,
and although it is typically present in multiple copies in the
genome, concerted evolution homogenizes sequence diversity,
and consequently is assumed to reduce the risk of sequencing
paralogs. Early molecular studies were pre-PCR and hence in-
volved laboratory cloning and generally few taxa. Since 1990
rapid advancements in techniques in molecular biology (e.g.,
the utilization of PCR) and bioinformatics made it possible
to generate and analyze larger datasets. Nuclear-encoded 18S
rDNA sequences have been, until recently, the primary source
of data for inferring phylogenetic relationships among green al-
gae (Pr
¨
oschold and Leliaert, 2007), supplemented by 28S rDNA
(e.g., Buchheim et al., 2001; Shoup and Lewis, 2003), actin (An
et al., 1999) and the chloroplast genes rbcL, tuf A and atpB
(e.g., Daugbjerg et al., 1994; Daugbjerg et al., 1995; McCourt
et al., 2000; Hayden and Waaland, 2002; Nozaki et al.
, 2003;
Zechman, 2003; Rindi et al., 2007).
These initial molecular phylogenetic investigations have gen-
erally corroborated the ultrastructure-based higher-level classi-
fication of the green algae, but have also revised the circumscrip-
tions of several lineages (McCourt, 1995). However, analyses
of individual genes have only partly resolved the relationships
among the main green algal lineages. It is now clear that a large
number of genes from many species must be analysed to arrive
at a reliable phylogenetic resolution for an ancient group such
as the green algae (Philippe and Telford, 2006). These datasets
have mainly involved concatenated sequences of protein-coding
genes that are shared among green algal chloroplast genomes.
To date, 26 complete green algal plastid genomes have been
sequenced and assembled (Wakasugi et al., 1997; Turmel et
al., 1999b; Lemieux et al., 2000; Maul et al., 2002; Turmel et
al., 2002b; Pombert et al., 2005; Turmel et al., 2005; B
´
elanger
et al., 2006; de Cambiaire et al., 2006; Pombert et al., 2006;
Turmel et al., 2006; de Cambiaire et al., 2007; Lemieux et al.,
2007; Robbens et al., 2007a; Brouard et al., 2008; Turmel et
al., 2008; Turmel et al., 2009a; Turmel et al., 2009b; Zuccarello
et al., 2009; Brouard et al., 2010; Brouard et al., 2011), in
addition to more than 30 angiosperm plastid genomes (Soltis
et al., 2009). Chloroplast genomes are particularly useful for
phylogenetic reconstruction because of their relatively high and
condensed gene content, in comparison to nuclear genomes. Fur-
thermore, in contrast to many nuclear genes that are multi-copy
Downloaded by [University of Gent] at 07:28 14 February 2012

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Next-generation DNA sequencing.

TL;DR: Next-generation DNA sequencing has the potential to dramatically accelerate biological and biomedical research, by enabling the comprehensive analysis of genomes, transcriptomes and interactomes to become inexpensive, routine and widespread, rather than requiring significant production-scale efforts.
Journal ArticleDOI

Phylogenetic relationships among ascomycetes: evidence from an RNA polymerse II subunit.

TL;DR: Findings show that a slowly evolving protein-coding gene such as RPB2 is useful for diagnosing phylogenetic relationships among fungi, and suggests that fruiting body formation and forcible discharge of ascospores were characters gained early in the evolution of the Ascomycota.
Journal ArticleDOI

The Chlamydomonas Genome Reveals the Evolution of Key Animal and Plant Functions

Sabeeha S. Merchant, +118 more
- 12 Oct 2007 - 
TL;DR: Analyses of the Chlamydomonas genome advance the understanding of the ancestral eukaryotic cell, reveal previously unknown genes associated with photosynthetic and flagellar functions, and establish links between ciliopathy and the composition and function of flagella.
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Phylotranscriptomic analysis of the origin and early diversification of land plants

The Chlamydomonas Genome Reveals the Evolution of Key Animal and Plant Functions

Sabeeha S. Merchant, +118 more
- 12 Oct 2007 - 
Frequently Asked Questions (16)
Q1. What contributions have the authors mentioned in the paper "Phylogeny and molecular evolution of the green algae" ?

Leliaert et al. this paper reported that the green lineage diverged early from the remaining Chlorophyta, but the relationships among these lineages remain largely unresolved, mainly because multi-gene data are only available for a limited number of taxa. 

Ribosomal sequences were chosen at the time because enough RNA could be obtained for direct sequencing and (later) because regions of the gene were conserved enough to make universal primers. 

Because the sporopollenin surrounding the zygotes is highly resistant to degradation and because the shallow freshwater habitats in which they live often create favourable depositional conditions, the stoneworts are well represented in the fossil record (fossilized zygote walls are called gyrogonites). 

A persistent problem in many of the multi-gene phylogenetic investigations thus far is sparse and incomplete taxon sampling, which may result in systematic errors in phylogenetic reconstruction. 

Since 1990 rapid advancements in techniques in molecular biology (e.g., the utilization of PCR) and bioinformatics made it possible to generate and analyze larger datasets. 

Their appeal as a model system stems from the relative simplicity of their development and from the wide range of sizes and degrees of complexity found in extant species. 

Several biochemical innovations have been identified, including synthesis and accumulation of protective “sunscreens,” plant growth hormones, isoprene, phenolics, heat shock proteins, and enhanced DNA repair mechanisms (Waters, 2003; Rensing et al., 2008). 

The two most prominent endosymbioses in eukaryote evolution have involved an alpha-proteobacterial and a cyanobacterial endosymbiont, and have given rise to mitochondria and plastids, respectively (Keeling and Palmer, 2008). 

The marine planktonic compartment of picoeukaryotes has been previously overlooked because of the extremely small size of its constituents (1–3µm). 

Phylogenomic analyses of two diatom genomes revealed that a considerable proportion of nuclear genes are of green algal origin, which is surprising given that diatom plastids are of red algal origin (Moustafa et al., 2009). 

Recent advances in high-throughput DNA sequencing, including Roche-454 and Illumina-Solexa (Shendure and Ji, 2008; Metzker, 2010) facilitate rapid sequencing of organellar genomes, transcriptomes and entire nuclear genomes. 

Additional traits that are uniquely shared by the remaining streptophytes include apical growth (not in the Zygnematophyceae), sexual reproduction, some biochemical features, and similar cellulose-synthesizing rosettes (Tsekos, 1999). 

In addition to facilitating transport of transcripts as mentioned above, the evolution of cytoplasmic streaming in siphonous algae also allowed transport of nutrients and organelles throughout the siphonous algal body. 

the comparable architectures of green algal plastid and mitochondrial DNAs may be a consequence of these genomes having similar mutation rates, as reflected in their similar rates of silent-site substitution. 

Despite this crucial function, not all eukaryotes have this protein, and it has been shown that an elongation factor-like protein (EF-like) can substitute for EF-1α in these taxa (Keeling and Inagaki, 2004). 

This phylogenetic position is further supported by some chloroplast genomic features, such as the presence of introns in two transfer RNAs which is shared between Klebsormidium and the later-diverging streptophyte lineages, and the presence of functional plastid tufA, which is shared with the early-diverging lineages (Baldauf et al., 1990; Baldauf and Palmer, 1990; Manhart and Palmer, 1990; Turmel et al., 2005; Turmel et al., 2007b) (Figure 4).