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AOBPreview originally published online on February 1, 2007
Annals of Botany 2007 99(4):677-701; doi:10.1093/aob/mcl294
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© The Author 2007. Published by Oxford University Press on behalf of the Annals of Botany Company. All rights reserved. For Permissions, please email: journals.permissions@oxfordjournals.org

Nuclear DNA Content Estimates in Green Algal Lineages: Chlorophyta and Streptophyta

Donald F. Kapraun*

Department of Biological Sciences, University of North Carolina–Wilmington, 601 South College Road, Wilmington, NC 28403-5915, USA

* For Correspondence. E-mail: kapraund{at}uncw.edu

Received: 29 March 2006    Returned for revision: 28 July 2006    Accepted: 4 December 2006    Published electronically: 1 February 2007


   ABSTRACT
 TOP
 ABSTRACT
 INTRODUCTION
 METHODS
 RESULTS
 DISCUSSION
 SUMMARY AND CONCLUSIONS
 APPENDIX
 APPENDIX
 ACKNOWLEDGEMENTS
 LITERATURE CITED
 KEY TO REFERENCES 
 

Background and Aims: Consensus higher-level molecular phylogenies present a compelling case that an ancient divergence separates eukaryotic green algae into two major monophyletic lineages, Chlorophyta and Streptophyta, and a residuum of green algae, which have been referred to prasinophytes or micromonadophytes. Nuclear DNA content estimates have been published for less than 1% of the described green algal members of Chlorophyta, which includes multicellular green marine algae and freshwater flagellates (e.g. Chlamydomonas and Volvox). The present investigation summarizes the state of our knowledge and adds substantially to our database of C-values, especially for the streptophyte charophycean lineage which is the sister group of the land plants. A recent list of 2C nuclear DNA contents for isolates and species of green algae is expanded by 72 to 157.

Methods: The DNA-localizing fluorochrome DAPI (4',6-diamidino-2-phenylindole) and red blood cell (chicken erythrocytes) standard were used to estimate 2C values with static microspectrophotometry.

Key Results: In Chlorophyta, including Chlorophyceae, Prasinophyceae, Trebouxiophyceae and Ulvophyceae, 2C DNA estimates range from 0·01 to 5·8 pg. Nuclear DNA content variation trends are noted and discussed for specific problematic taxon pairs, including Ulotrichales–Ulvales, and Cladophorales–Siphonocladales. For Streptophyta, 2C nuclear DNA contents range from 0·2 to 6·4 pg, excluding the highly polyploid Charales and Desmidiales, which have genome sizes of up to 14·8 and 46·8 pg, respectively. Nuclear DNA content data for Streptophyta superimposed on a contemporary molecular phylogeny indicate that early diverging lineages, including some members of Chlorokybales, Coleochaetales and Klebsormidiales, have genomes as small as 0·1–0·5 pg. It is proposed that the streptophyte ancestral nuclear genome common to both the charophyte and the embryophyte lineages can be characterized as 1C = 0·2 pg and 1n = 6.

Conclusions: These data will help pre-screen candidate species for the on-going construction of bacterial artificial chromosome nuclear genome libraries for land plant ancestors. Data for the prasinophyte Mesostigma are of particular interest as this alga reportedly most closely resembles the ‘ancestral green flagellate’. Both mechanistic and ecological processes are discussed that could have produced the observed C-value increase of >100-fold in the charophyte green algae whereas the ancestral genome was conserved in the embryophytes.

Key words: ‘Ancestral green flagellate’ (AGF), C-value enigma, chlorophyta, DNA C-values, nuclear genome size, Streptophyta


   INTRODUCTION
 TOP
 ABSTRACT
 INTRODUCTION
 METHODS
 RESULTS
 DISCUSSION
 SUMMARY AND CONCLUSIONS
 APPENDIX
 APPENDIX
 ACKNOWLEDGEMENTS
 LITERATURE CITED
 KEY TO REFERENCES 
 
Chlorophyta include the eukaryotic green algae, which possess chlorophyll a and b and starch stored inside plastids with stacks of 2–6 thylakoids per band (Bold and Wynne, 1985). Approximately 425 genera and 6500 species have been described (Alexopoulos and Bold, 1967). Simplicity and antiquity of green algae (Chlorophyta) have long been accepted as evidence of their apparent ancestry to land plants (McCourt, 1995). Phylogenetic analyses of molecular markers including 18S rRNA and rbcL (Bhattacharya et al., 1994; McCourt et al., 1995, 1996; Huss and Kranz, 1997; Katana et al., 2001) and morphological data (Mattox and Stewart, 1984) contradict this view and present a compelling case that an ancient and deep divergence separates green plants into two major monophyletic lineages: Chlorophyta and Streptophyta (Turmel et al., 1999; Karol et al., 2001) (Fig. 1).


Figure 1
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FIG. 1. Summary results of combined analysis using morphological, ultrastructural and large- and small-subunit rRNA gene sequences for chlorophyte and streptophyte algae (McCourt, 1995).

 
A third polyphyletic green plant lineage, branching at the base of the Chlorophyta–Streptophyta divergence, includes a residuum of related unicellular micromonadophytes (=prasinophytes) (Kantz et al., 1990; Steinkötter et al., 1994; Karol et al., 2001) (Fig. 1). Although the exact relationship of the prasinophytes to land plants remains unclear (Qiu and Palmer, 1999), it seems likely that a prasinophyte-like scaly flagellate was the common ancestor of both green plant divisions (Friedl, 1997). Nuclear genome size and organization remain largely unknown in the prasinophytes. A 2C genome size estimate of about 10 Mbp reported for Ostreococcus tauri (Prasinophyceae) is one of the smallest among free-living eukaryotic organisms (Courties et al., 1998; Derelle et al., 2002). It is assumed that this small genome is evolutionarily derived rather than ancestral (Courties et al., 1994) as other members of Mamiellaceae (Prasinophyceae) are reported to represent secondarily reduced forms (Daugbjerg et al., 1995). Previously, it was suggested that this apparent miniaturization of prasinophyte nuclear genomes may defeat attempts to use them as a model in reconstruction of an ancstral land plant nucleotype (Cunningham et al., 1998; Oakley and Cunningham, 2000). Consequently, the early branching groups in the charophycean lineage (Soltis et al., 1999), including Chlorokybales, Klebsormidiales and Coleochaetales, may provide the best opportunity for gaining these insights, but there are few published estimates of DNA contents in target members of these orders.

The Second Plant Genome Size workshop and Discussion Meeting [hosted by the Royal Botanic Gardens (RBG), Kew, 8–12 September, 2003] identified major gaps (systematic, regional and plant type) in our knowledge of plant DNA amounts (Bennett and Leitch, 2005a). It was noted that no database was available for algae. This major gap was addressed with a compilation of genome size estimates for 247 species of red, green and brown macroscopic algae (Kapraun, 2005). This report included nuclear DNA content estimates for 95 isolates and species of multicellular green marine algae, which are almost exlusively members of Ulvophyceae (Kapraun, 2005). These data are incorporated into a database of plant genome sizes (Kapraun et al., 2004) available online on the RBG Kew website (http://www.rbgkew.org.uk/cval/homepage.html). In addition, nuclear DNA content data for green algae, both from our continuing investigations and from the literature, are regularly updated at http://www.uncw.edu/people/kapraund/DNA (see links there to ‘Table I. Chlorophyta’ and ‘Appendix I. Chlorophyta’). The present paper includes nuclear genome size estimates for 72 additional isolates and species of green algae. Of this total, 33 resulted from our ongoing research. Unicellular freshwater microalgae that were under-represented or excluded previously (Kapraun, 2005) are emphasized here, especially members of Chlorophyceae and Trebouxiophyceae. A significant effort was made to expand our database for streptophyte algae, which are critical in efforts to reconstruct a hypothetical ancestral nuclear genome for the green algal ancestor of the land plants.

Inclusion of published nuclear DNA content data for green algae in the present report was sometimes problematic. The Second Plant Genome Size workshop and Discussion Meeting (Bennett et al., 2000; Bennett and Leitch, 2005b) identified ‘best practice’ methodology for nuclear genome size estimation in plant tissues. Virtually none of the published genome size data for algae resulted from investigations adhering to all of the best practice recommendations, primarily because measurement of the relatively small algal nuclear genomes requires standard species different from those specified as appropriate for vascular plants (Kapraun, 2005). Flow cytometry of oceanic picoeukaryotes and phytoplankton has resulted in nuclear DNA content estimates from whole cells for numerous algae including members of Chlorophyceae and Prasinophyceae (Simon et al., 1994; Veldhuis et al., 1997). In general, only estimates based on isolated nuclei were included in the present study. A comprehensive discussion of standard species and methods is included in the notes related to the Appendix at the end of this paper.


   METHODS
 TOP
 ABSTRACT
 INTRODUCTION
 METHODS
 RESULTS
 DISCUSSION
 SUMMARY AND CONCLUSIONS
 APPENDIX
 APPENDIX
 ACKNOWLEDGEMENTS
 LITERATURE CITED
 KEY TO REFERENCES 
 
Algal material was fixed in Carnoy's solution and stored in 70 % ethanol at 4 °C. Preserved material was rehydrated in water and softened in 5 % w/v EDTA (Goff and Coleman, 1990) for 30 min to 3 h. Specimens were transferred to cover slips treated with subbing solution, air dried and stained with DAPI (0·5 µg mL–1 4',6-diamidino-2-phenylindole; Sigma Chemical Co.,` St. Louis, MO, USA) as previously described (Goff and Coleman, 1990; Kapraun and Nguyen, 1994). Detailed procedures for microspectrophotometry with DAPI and requirements for reproducible staining have been specified previously (Kapraun, 1994; Kapraun and Nguyen, 1994) using a protocol modified after Goff and Coleman (1990). Microspectrophotometric data for Gallus [chicken erythrocytes or red blood cells (RBC)] with a DNA content of 2·4 pg (Clowes et al., 1983) were used to quantify mean fluorescence intensity (If) values for algal specimens (Kapraun, 1994). DAPI binds by a non-intercalative mechanism to adenine/thymine- (A/T-) rich regions of DNA (Portugal and Waring, 1988). Consequently, RBC are best used as a standard for estimating amounts of DNA when the A/T contents of both standard and experimental DNA are equivalent (Coleman et al., 1981). Gallus has a nuclear DNA base composition of 42–43 mol% G+C (Marmur and Doty, 1962). Limited published data indicate similar mean values of 46 mol% for Chlorophyta (Sueoka, 1961; Olsen et al., 1987; Freshwater et al., 1990; Kooistra et al., 1992; Le Gall et al., 1993; Simon et al., 1994). Algae investigated in this study are assumed to have a similar range of base pair compositions, and linearity is accepted between DAPI–DNA binding in both RBC and algal samples (Le Gall et al., 1993). Nuclear DNA contents were estimated by comparing the If values of the RBC standard and algal sample (Kapraun, 1994). Chlorophyta include taxa with some or all of their cells being multinucleate or endopolyploid (Kapraun and Nguyen, 1994) as well as taxa that exhibit a nuclear ‘incremental size decrease associated with a cascading down of DNA contents’ (Kapraun, 1994). Specific methodologies were developed for specimens to permit assignment of C level and interpretation of If data. Details of materials and methods, as well as information for collection locations, and data for numbers of algal nuclei examined in each sample and estimates of nuclear genome size (pg,±s.d.) are available at http://www.uncw.edu/people/kapraund/DNA.


   RESULTS
 TOP
 ABSTRACT
 INTRODUCTION
 METHODS
 RESULTS
 DISCUSSION
 SUMMARY AND CONCLUSIONS
 APPENDIX
 APPENDIX
 ACKNOWLEDGEMENTS
 LITERATURE CITED
 KEY TO REFERENCES 
 
The present investigation adds nuclear DNA content estimates for 72 species and isolates of green algae to our database of C-values, emphasizing the streptophyte charophycean lineage that is the sister group of land plants. A previous list of 2C nuclear DNA contents in green algae (Kapraun, 2005) is expanded to 157. DNA content estimates, both from the present research and from published information, are presented as picograms (pg) and as megabase pairs (Mbp) (Appendix).

In Chlorophyta, including Chlorophyceae, Trebouxiophyceae, Ulvophyceae and Prasinophyceae (Figs 13), 2C DNA estimates range from 0·01 to 5·8 pg. Significant new data are included in this study (Appendix) for all of the major groups of Ulvophyceae (Fig. 4). In Ulotrichales (Fig. 5), nuclear DNA content data are available for seven species of this large and diverse order (Table 1 online, see Introduction) and suggest that it is characterized by small 2C values of 0·2–0·5 pg (Appendix). Estimates of nuclear DNA contents for species of Ulvales (Fig. 6) range from 2C = 0·14 to 1·1 pg (Appendix). In Trentepohliales, nuclear DNA content estimates of 2C = 1·1–4·1 pg appear to be correlated with a molecular phylogenetic tree derived from small-subunit rRNA gene sequence analysis (Fig. 7). Published 2C nuclear DNA content estimates range from 0·1 to 1·0 pg for most members of Caulerpales. Only species of Halimeda and Codium have substantially larger genomes of 1·0–6·1pg (Fig. 8). Previously published (Kapraun, 2005) and present nuclear DNA content estimates for members of Dasycladales indicate a range of 0·7–3·8 pg (Fig. 9). In the Cladophorales/Siphonocladales complex, nuclear DNA content estimates indicate that members of clade III have relatively small genomes (2C = 0·2–0·7 pg) whereas members of clade II, including the bulk of Siphonocladales, have much larger genomes of 2C = 2·0–5·7 pg (Fig. 10). Isolates of Pithophora spp. have genome sizes of 2C = 1·9 pg (UTEX 1333) and 4·1 pg (UTEX 787), respectively.


Figure 2
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FIG. 2. Estimated 2C nuclear DNA contents and 2n chromosome complements (Sarma, 1982) superimposed on a phylogenetic tree for Volvocales based on multiple plastid gene sequences (Nozaki et al., 1999, 2000).

 


Figure 3
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FIG. 3. Estimated 2C nuclear DNA contents superimposed on a phylogenetic tree for Trebouxiophyceae based on 18S rRNA gene sequence analyses (Friedl, 1995; Krienitz et al., 2004).

 


Figure 4
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FIG. 4. Estimated 2C nuclear DNA contents superimposed on a cladogram of Ulvophyceae inferred from small-subunit rRNA gene sequence data (Zechman, 1990).

 


Figure 5
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FIG. 5. Phylogenetic tree of Ulotrichales inferred from 18S rRNA and rbcL gene sequence analysis (Hayden and Waaland, 2002).

 


Figure 6
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FIG. 6. Phylogenetic tree of the Ulvales inferred from 18S rRNA and rbcL gene sequence analysis (Hayden and Waaland, 2002).

 


Figure 7
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FIG. 7. Estimated 2C nuclear DNA content estimates superimposed on a cladogram of Trentepohliales inferred from small-subunit rRNA genes (López-Bautista and Chapman, 2003, 2005).

 


Figure 8
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FIG. 8. Estimated 2C nuclear DNA contents superimposed on a phylogenetic tree for Caulerpales based on cladistical analyses (Vroom et al., 1998; Woolcott et al., 2000). Proposed polyploidy events are indicated by [P].

 


Figure 9
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FIG. 9. Estimated 2C nuclear DNA contents superimposed on a phylogenetic tree for Dasycladales based on rbcL gene sequence analyses (Zechman, 2003; Berger et al., 2003). Proposed polyploidy events are indicated by [P].

 


Figure 10
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FIG. 10. Estimated 2C nuclear DNA contents superimposed on a phylogenetic tree for the Cladophorales/Siphonocladales complex based on 18S rRNA gene sequence analysis (Hanyuda et al., 2002).

 
In Prasinophyceae (Appendix), nuclear genome size estimates of 0·2 and 0·7 pg were obtained for species of Pyramimonas and Tetraselmis, respectively (Appendix), suggesting that at least in these prasinophycean algae, nuclear genome sizes more closely approximate those reported in many other green algae (Kapraun, 2005).

In Streptophyta, 2C nuclear DNA contents range from 0·2 to 6·4 pg, excluding the highly polyploid Charales and Desmidiales, which have genome sizes of up to 14·8 and 46·8 pg, respectively. Nuclear DNA content data for Streptophyta superimposed on a contemporary molecular phylogenetic tree indicate that early diverging lineages, including some members of Chlorokybales, Coleochaetales and Klebsormidiales, have genomes as small as 0·1–0·5 pg. In Mesostigmatales, a genome size of 0·74 pg was estimated for an isolate identified as representing Mesostigama viride (Appendix). In Coleochaete (Coleochaetales) isolates investigated, nuclear DNA content estimates of 1·4, 3·0 and 5·5 pg approximate a doubling sequence, consistent with values that would result from polyploidy. In the present study, a 2C nuclear genome size of 1·2 pg was estimated for Chaetosphaeridium globosum (Appendix). In Klebsormidiales, 2C nuclear genome sizes for Klebsormidium flaccidum and Entransia fimbriata were estimated to be 0·4 and 1·1 pg, respectively (Appendix). An isolate of Klebsormidium nitens from Argentina was found to have an estimated nuclear DNA content of 2C = 0·55 pg (Appendix) or 539 Mbp (using 1 pg = 980 Mbp, Bennett et al., 2000).

In the present study, nuclear DNA content estimates obtained with DAPI microspectrophotometry for five additional species extend the upward range for presumptive 2C nuclei to 46 pg. In a Netrium digitus isolate (UTEX 599), nuclei were too large to be accommodated by the photometer aperture system, but nuclear volume (NV) calculations, as described in the Appendix notes, resulted in a nuclear DNA content estimate of more than 125 pg. This is by far the largest nuclear genome size reported in any green alga (Kapraun, 2005). The present investigation extends the upward range for presumptive 2C nuclei to 7·2 pg in an isolate of Mougeotia transeaui (Fig. 11). The 2C nuclear DNA contents in Charales range from 14·0 to 39·2 pg (Fig. 11).


Figure 11
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FIG. 11. Ranges of 2C nuclear DNA contents superimposed on a consensus molecular phylogenetic tree for the streptophyte green algae and bryophytes based on sequence analyses (Bhattacharya et al., 1994; McCourt et al., 2000; Denboh et al., 2001; Karol et al., 2001; Cimino and Delwiche, 2002; Delwiche et al., 2002; Turmel et al., 2002c; Gontcharov et al., 2003). DNA data for streptophyte algae are from Kapraun (2005) and the Appendix, and for the bryophytes from Renzaglia et al. (1995) and Voglmayr (2000).

 


   DISCUSSION
 TOP
 ABSTRACT
 INTRODUCTION
 METHODS
 RESULTS
 DISCUSSION
 SUMMARY AND CONCLUSIONS
 APPENDIX
 APPENDIX
 ACKNOWLEDGEMENTS
 LITERATURE CITED
 KEY TO REFERENCES 
 
Chlorophyta
Chlorophyta contain the classical ‘green algae’, primarily Chlorophyceae, Trebouxiophyceae (=Pleurastrophyceae) and Ulvophyceae (Mishler et al., 1994; Watanabe et al., 2001) (Fig. 1). All members of this clade have swimming cells with two or four anterior flagellae arising from basal bodies which are arranged cruciately (O'Kelly and Floyd, 1984). Combined analysis of morphology and molecular data strongly supports the monophyly of these three groups (Mishler et al., 1994) and the phylogenetic topology followed below (Krienitz et al., 2004).

Chlorophycean algae
Chlorophyceae apparently arose during the later stages of green algal evolution and are not an early branching lineage (Watanabe et al., 2001). This group includes a predominance of freshwater taxa such as Sphaeropleales (= Chlorococcales; e.g. Scenedesmus), and many of the familiar flagellates such as Volvox and Chlamydomonas (Volvocales). Recently, molecular techniques were used to re-examine phylogenetic relationships in Volvocales (Buchheim et al., 1996, 1997, 2002) as previously deduced by morphological and gene sequence data (Nozaki et al., 1995; Angeler et al., 1999). Volvox has been considered to be the limit of the colonial development in the volvocine series, in which Gonium and unicellular forms such as Chlamydomonas are early branching lineages (Larson et al., 1992). Although much of the evolution in the colonial Volvocales superficially appears to constitute a gradual progression in colonial complexity and in types of sexual reproduction, as in the traditional volvocine lineage hypothesis, reverse evolution must be considered for the origin of certain species of Pleodorina (Nozaki et al., 2000). Apparently, both colonial and unicellular morphotypes have evolved independently in several clades (Nozaki et al., 1995, 1999; Nozaki and Krienitz, 2001). Thus, the traditional view of a unidirectional, monophyletic progression from unicellular, through colonial, to multicellular forms, represented by the sequence Chlamydomonas, Gonium, Pandorina, Eudorina, Pleodorina and Volvox, is not supported by gene sequence analyses (Larson et al., 1992; Lewis and McCourt, 2004).

In Chlorophyceae, published DNA content estimates for Sphaeropleales (= Chlorococcales), a widely distributed and much investigated group of algae (Buchheim et al., 2005; McManus and Lewis, 2005), are limited to an early study which cited Scenedesmus obliquus as having a nuclear genome size of 0·4 pg (Charles, 1977). Few nuclear DNA content estimates have been published for Volvocales (Fig. 2). The pioneering investigation of Holm-Hansen (1969) using ‘fluorometric measurement’ estimated 0·6 pg for Dunaliella tertiolecta. Flow cytometry of whole cells gave an estimate of 0·015 pg for this alga (Veldhuis et al., 1997). DNA content estimates of 0·01–0·2 pg are given in the Appendix for three additional species of volvocine green algae.

Although relatively few nuclear DNA content estimates have been published for Volvocales (Fig. 2), chromosome numbers have been published for many species. These range from 2n = 8 to 76, with the vast majority of reported numbers being between 16 and 24 (Sarma, 1982). In general, higher chromosome numbers are associated with colonial forms, and lower chromosome numbers with unicellular forms. Phylogenetic lines giving rise to Volvox include both low (n = 5) and high (n = 22) chromosome complements (Fig. 2). It would be a matter of great interest to augment the small amount of nucleotype data currently available for Volvocales with a more comprehensive investigation comparing nuclear genome size and chromosome numbers with speciation patterns (Schagerl et al., 1999; Coleman 2001). Specifically, do recognized volvocine morphotypes correlate with nucleotype parameters including genome size and chromosome number?

Trebouxiophycean algae
Trebouxiophyceae (=Pleurastrophyceae) includes those Chlorophyta with non-flagellate vegetative cells which are typically unicellular, sarcinoid or filamentous (Friedl, 1995; Henley et al., 2004; Krienitz et al., 2004; Ueno et al., 2005). Phylogenetic analysis of 18S rRNA gene sequences has demonstrated a monophyletic origin for these algae, and a sister group relationship to Chlorophyceae (Lewis, 1997; Handa et al., 2003; Lokhorst et al., 2004) (Fig. 3). Many of the better known members of this group exist in lichen associations, e.g. Dictyochloropsis and Trebouxia (Lewis and McCourt, 2004).

In Trebouxiophyceae, most nuclear DNA content estimates for Chlorellales (Fig. 3) resulted from an investigation using reassociation kinetics and were published as base pairs (Dörr and Huss, 1990). Pulse field gel electrophoresis (Higashiyama and Yamada, 1991), flow cytometry (Wilhelm et al., 1982; Veldhuis et al., 1997; Yamamoto et al., 2001) and microfluorometric analysis (Cattolico and Gibbs, 1975) have been used as well. The genus Nannochloris, and related genera, includes some of the smallest and ultrastructurally simplest phototrophic eukaryotes, with genomes as small as 12·6 Mbp (Arai et al., 1998; Yamamoto et al., 2001). Using 1 pg = 980 Mbp (after Bennett et al., 2000), 2C genome sizes (reported as Mbp) range from 0·02 pg in Picochlorum atomus (as Nannochloris atomus) (Veldhuis et al., 1997) to 1·06 pg in Chlorella fusca (Dörr and Huss, 1990).

Chlorellales
Recent molecular studies have resulted in the dispersal of species traditionally referred to Chlorella over two classes of chlorophytes, Trebouxiophyceae and Chlorophyceae (Huss et al., 1999; Katana et al., 2001; Henley et al., 2004; Krienitz et al., 2004). In the present investigation, Chlorella species included in the Appendix are considered to be trebouxiophycean algae (Huss et al., 1999). Phylogenetic analysis of some ‘Nannochloris-like’ algae resulted in their transfer to other genera, including Marvania and Picochlorum (Henley et al., 2004).

Prasiolales
Recent molecular data support transfer of Prasiola, formerly in the Ulvophyceae, to Trebouxiophyceae (Sherwood et al., 2000; Friedl and O'Kelly, 2002; Naw and Hara, 2002). This development is particularly notable as Prasiola, and the closely related Rosenvingiella (Rindi et al., 2004), often develop morphotypes which mimic Enteromorpha and Ulva (Ulvales). In the present study, the nuclear genome size estimate of 0·9 pg for Prasiola stipitata is assumed to represent the 4C value as blades in this species are reported to be diploid (Cole and Akintobi, 1963). Nuclear DNA content estimates range from 2C = 0·1 to 1·2 pg and indicate no apparent correlation between genome size and phylogeny (Fig. 3).

Ulvophycean algae
Ulvophyceae are primarily marine species, most with larger and more complex morphologies than typically found in Chlorophyceae. Molecular data support a model for Ulvophyceae sensu Mattox and Stewart (1984) with two separate lineages: a clade including Ulothrichales and Ulvales (Hayden and Waaland, 2002; O'Kelly et al., 2004) and a clade with Caulerpales, Cladophorales/Siphonocladales complex, Dasycladales and Trentepohliales (Zechman et al., 1990; Hanyuda et al., 2002) (Fig. 4). In the present report, presentation of orders reflects a consensus of contemporary phylogenetic treatments (Zechman et al., 1990).

Ulotrichales
Ulotrichales as presently delimited (Floyd and O'Kelly, 1990) have been expanded to include Acrosiphoniaciae (sensu Kornmann and Sahling, 1977; Sussmann et al., 1999). Molecular analyses using 18S rDNA and 18S rRNA gene sequence data have confirmed this placement (Watanabe et al., 2001; Lindstrom and Hanic, 2005). Species of Capsosiphon and Monostroma, included in Ulvales by Bliding (1963, 1968), appear to be more closely related to Ulotrichales (Fig. 5). Nuclear DNA content data, available for seven species of this large and diverse order (table 1 online), suggest that it is characterized by small 2C values of 0·2–0·5 pg (Appendix). No correlation between nuclear genome size and phylogenetic position is apparent (Fig. 5). The relatively small genome sizes reported for species in this order are complemented by relatively small chromosome numbers of 2n = 8–24 (Kapraun, 1993).

Ulvales
The emended order Ulvales (O'Kelly et al. 2004) is monophyletic (Fig. 6), but circumscription of several genera, including the familiar Ulva and Enteromorpha (Hayden and Waaland, 2002, 2004; Hiraoka et al., 2003) and Blidingia (Lindstrom and Golden, 2006), remains problematic. In both Ulva and Enteromorpha, blade and tubular thallus morphotypes apparently arose independently several times throughout the evolutionary diversification of the group (Blomster et al., 1998, 1999; Tan et al., 1999; Shimada et al., 2003). Although results from molecular and culture studies suggest that Ulva, Enteromorpha and Chloropelta should not be recognized as separate genera (Hayden et al., 2003; Matsuo et al., 2003, 2005), these familiar taxonomic epithets are retained here for convenience (Appendix). The absence of a correlation between nuclear genome size and chromosome number in these species (Kapraun and Bailey, 1992) suggests a significant role of aneuploidy in their evolution (Kapraun, 2005).

Trentepohliales
Molecular investigations place members of this order with the second lineage of Ulvophyceae (Mishler et al., 1994; Chapman et al., 1995; Lopez-Bautista and Chapman, 2003), which are otherwise almost exclusively marine. Nuclear DNA content estimates of 2C = 1·1–4·1 pg appear to be correlated with a molecular phylogenetic tree derived from small subunit rRNA gene sequence analysis (Fig. 7). Large-scale discontinuous variation in both reported chromosome complements (n = 4–28) (Appendix) and nuclear DNA contents are indicative of polyploidy in this order (Lopez-Bautista et al., 2000).

Caulerpales
Cladistic analysis of morphological and molecular data supports separation of Caulerpales (Codiales sensu Taylor, 1960) into two clades: (1) the homoplastidic Bryopsidineae, which are generally characterized by diplobiontic life histories and non-holocarpic production of gametes (e.g. Bryopsis and Codium); and (2) the heteroplastidic Halimedineae, which are generally characterized by haplobiontic and diploid life histories and holocarpic production of gametes (e.g. Caulerpa and Halimeda) (Zechman et al., 1990; Vroom et al., 1998; Woolcott et al., 2000). Published 2C nuclear DNA content estimates range from 0·1 to 1·0 pg for most of these algae. Only species of Halimeda and Codium have substantially larger genomes (1·0–6·1pg; Fig. 8). As these two genera are placed in separate clades, it appears that large-scale whole genome increase (polyploidy) arose independently at least twice in the evolution of Caulerpales (Fig. 8).

Dasycladales
Recent molecular investigations based on analyses of rbcL (Zechman, 2003) and 18S rRNA (Berger et al., 2003) gene sequence data revealed three well-supported clades for which morphological synapomorphies exist, but which are not completely in accordance with previous generic concepts. A Polyphysa clade is distinguished from Acetabularia on the basis of cap morphotype and initiation (Berger and Kaever, 1992; Sawitzky et al., 1998). The range of nuclear DNA content estimates for members of Dasycladales (0·7–3·8 pg) (Fig. 9), which suggests large-scale discontinuous variation in all major clades, almost certainly reflects multiple polyploidy events (Kapraun and Buratti, 1998; Kapraun, 2005). It seems noteworthy that similarly large values (approx. 3·2–3·8 pg) were found in the early diverging Neomeris clade as well as in the highly derived Parvocaulis (=Polyphysa) and Acetabularia clades. No correlation is apparent between cap morphotypes (Sawitzky et al., 1998), cap morphogenesis (Kratz et al., 1998) and ‘polyploid’ nucleotypes in Dasycladales.

The Cladophorales/Siphonocladales complex
Cladophorales and Siphonocladales are a related lineage sharing a gradation of ‘architectural’ morphological types (Olsen-Stojkovich et al., 1986; Van den Hoek et al., 1988; Bakker et al., 1994). Contemporary molecular studies (Zechman et al., 1990; Hanyuda et al., 2002) have identified three well-supported clades in this complex: (I) an early diverging assemblage of mostly freshwater species of cladophoracean genera, including Aegagropila, Arnoldiella, Pithophora and Wittrockiella; (II) species belonging primarily to Siphonocladales sensu Børgesen (1913); and (III) the most derived assemblage including species belonging to the cladophoracean genera Chaetomorpha, Cladophora and Rhizoclonium (Fig. 10). Confusingly, the characteristic morphologies associated with the genera Chaetomorpha, Cladophora and Rhizoclonium appear to have evolved several times, independently, in all three clades. Thus, these genera as presently circumscribed are clearly polyphyletic.

Karyological studies indicate that species in the most highly derived cladophoracean clade III (Rhizoclonium, Chaetomorpha and Cladophora sensu stricto), without exception, share a unique constellation of karyotype features including: (1) six basic chromosomes, three of which have median and the other three have submedian centromeres; and (2) almost universal polyploidy, resulting in chromosome complements in most species of x = 12, 18, 24, 30, 36, etc. (Wik-Sjöstedt, 1970; Kapraun and Gargiuolo, 1987a, b; Miyaji, 1999). Species in the siphonocladacean clade II have (1) various combinations of both metacentric and acrocentric chromosomes (Kapraun and Breden, 1988; Bodenbender and Schnetter, 1990; Kapraun and Nguyen, 1994), and (2) chromosome complements consistent with an aneuploid origin: 1n = 8, 12, 14, 16, 18 and 20 (Kapraun, 1993; Kapraun and Nguyen, 1994). Karyological data for basal clade I taxa appear to be limited to species of Pithophora, which have chromosome complements of 18, 24, 30 and 36 (Noor, 1968; Verma, 1979; Sarma, 1982) and relatively long chromosomes, up to 3 µm (Godward, 1966). Nuclear DNA content estimates indicate that members of clade III have relatively small genomes (2C = 0·2–0·7 pg) whereas members of clade II, including the bulk of Siphonocladales, have much larger genomes of 2C = 2·0–5·7 pg (Fig. 10). Isolates of Pithophora spp., representative of clade I, the earliest diverging among Cladophorales/Siphonocladales investigated, have genome sizes of 2C = 1·9 pg (UTEX 1333) and 4·1 pg (UTEX 787). These values almost certainly represent elevated DNA contents in a polyploid sequence, approximating to 2, 4, 8 and 16 pg (Appendix). As it was beyond the scope of the present investigation to determine chromosome numbers for these isolates, the exact ploidy level remains unknown.

Although the cladophoracean morphotype is reported to have evolved independently in all of the clades, the combination of karyotype pattern (n = 6) and nuclear genome size (2C = 0·2–0·7 pg) characteristic of the core clade III of Cladophorales appears to be unique and diagnostic, and may represent synapomorphies (Kapraun, 2005). If it is assumed that small genome size and symmetric karyotype with 1n = 6 is the ancestral condition in the Cladophorales/Siphonocladales complex, then these features have been most faithfully retained in the core cladophoracean algae in clade III. Clade II Siphonocladales, with a genome size increase of approximately an order of magnitude, and specialization of the karyotype by unequal reciprocal translocations (Kapraun and Breden, 1988), appear to be highly derived. Because nuclear volume is strongly correlated with cell size and cell cycle lengths in higher plants (Shuter et al., 1983) it is not surprising that these algae with their large, multinucleate cells and relatively long cell generation times have relatively large genomes (Kapraun and Nguyen, 1994). Clade I taxa (e.g. Pithophora) appear to have retained the ancestral karyotype, but not the theoretical small genome size. Their substantial increase in nuclear genome size, probably through whole genome duplication or polyploidy, may reflect their reliance on asexual reproduction by multinucleate propagules or akinetes (O'Neal and Lembi, 1983).

Prasinophycean algae
The prasinophytes or micromonads are primarily marine green flagellates. Some of the more commonly recognized taxa include Halosphaera, Pyramimonas and Tetraselmis. They generally have a single plastid, and often possess the accessory pigment prasinoxanthin. The cell membrane of most forms is covered with one or more layers of scales. There are no unique and defining characteristics for the group other than the above constellation of features (Sym and Pienaar, 1993; Graham and Wilcox, 2000). Prasinophytes have been characterized as the form of cell most closely representing the first green alga, or ‘ancestral green flagellate’ (AGF; Lewis and McCourt, 2004) (Fig. 1). Molecular analyses of 18S rRNA gene sequence data have identified at least seven separate lineages that form a grade at the base of the green algal tree of life (Steinkötter et al., 1994; Fawley et al., 2000; Zignone et al., 2002). Mamiellales include some of the smallest eukaryotes known, e.g. Crustomastix (Lewis and McCourt, 2004). There is some evidence that these algae represent secondarily reduced forms (Daugbjerg et al., 1995).

Nuclear genome size and organization remain largely unknown in Prasinophyceae (Appendix). Pulse field gel electrophoresis was used to obtain 2C nuclear genome size estimates for Ostreococcus tauri of 10·2 Mbp (Courties et al., 1998) and 9·7 Mbp (Derelle et al., 2002), or about one-quarter of the value reported for Chlorella (Higashiyama and Yamada, 1991). Using 1 pg = 980 Mbp (Bennett et al., 2000), Ostreococcus has a 2C genome size of about 0·01 pg. Flow cytometry analysis of isolated nuclei resulted in genome size estimates for Micromonas pusilla of 0·027 pg DNA per cell (Veldhuis et al., 1997) and 0·03 pg DNA per cell (Simon et al., 1994) and for Bathycoccus prasinos of 0·02 pg DNA per cell (Simon et al., 1994). These values were published as femtograms (10–15), but are expressed as picograms (10–12) here for consistency. Similar small genome size estimates based on whole cell flow cytometry measurements published for several additional prasinophyte taxa (Simon et al., 1994; Veldhuis et al., 1997) are not included in the Appendix as whole cell staining induces some non-specific background fluorescence, resulting in DNA content overestimates, typically by a factor of 3 or less (Veldhuis et al., 1997).

Streptophyta
Streptophyta (Bremer et al., 1987) include the charophycean lineage along with bryophytes and tracheophytes (Mishler et al., 1994; Turmel et al., 2002a, b). Numerous ultrastructural and molecular synapomorphies support this charophyte clade (Lewis and McCourt, 2004). However, the topology of the charophyte tree remains elusive (Friedl, 1997; Delwiche et al., 2002). Identification of the charophycean lineage as the sister group of land plants (Manhart and Palmer, 1990) suggests that their common ancestor was a branched, filamentous organism (Cook, 2004) with a haplontic life cycle and oogamous reproduction (Karol et al., 2001).

Charophycean algae
The charophycean lineage (Fig. 11) includes Chlorokybales (Qiu and Palmer, 1999), Klebsormidiales (Karol et al., 2001), Conjugophyta (Desmidiales and Zygnematales) (Hoshaw et al., 1990; McCourt et al., 2000; Denboh et al., 2001), Coleochaetales (Bhattacharya et al., 1994; McCourt, 1995; Cimino and Delwiche, 2002) and Charales (Surek et al., 1994; McCourt et al., 1996). The precise relationship of Mesostigmatales to the charophycean lineage remains unclear (Delwiche et al., 2002). The most important characters that define charophycean algae are the unilateral flagellar root in zooids and open mitosis with a persistent telophase spindle (Mattox and Stewart, 1984). In the present report, presentation of orders reflects a consensus of contemporary phylogenetic treatments (Delwiche et al., 2002; Lewis and McCourt, 2004).

Mesostigmatales
For many years the question of the nature of the AGF, the hypothetical ancestor of all land plants, has been controversially discussed (O'Kelly, 1992). Some researchers associate the AGF with a polyphyletic green plant lineage at the base of the split of Chlorophyta and Streptophyta (Fig. 1), which includes the green alga Mesostigma viride (Turmel et al., 2002a). The exact placement of Mesostigma remains controversial as some phylogenetic analyses include this species with Prasinophyceae (Lemieux et al., 2000; Turmel et al., 2002b), whereas others consider it to be ‘basal’ in the charophycean lineage (Palmer et al., 2004). Whatever the exact position of Mesostigma, there is no doubt that this alga belongs to a deeply diverging lineage given that it represents the first branch in trees inferred from sequences of land plants and all five orders of charophytes (Karol et al., 2001). A significant body of research centred around Mesostigma is emerging that provides insights into the timing of events that restructured both mitochondrial (mtDNA) and plastid DNA genomes during the evolution of green algae (Turmel et al., 2002b) and the transition from charophytes to land plants (Turmel et al., 2002a). Mesostigma plastid DNA is highly similar in size (118–360 bp) and gene organization to the plastid DNAs of land plants (Lemieux et al., 2000). Apparently plastid gene loss is an ongoing process in streptophytes, with independent losses occurring in multiple lineages. By contrast, Mesostigma mtDNA differs greatly at the levels of size (42–424 bp), gene organization and intron content from the bryophytes and land plants sequenced to date. During the evolutionary transition from Mesostigma to the liverwort Marchantia, mtDNA underwent a four-fold increase in size, was rearranged extensively and gained many introns while maintaining a similar gene content (Turmel et al., 2002b).

In the present study, a genome size of 0·74 pg was estimated for an isolate identified as Mesostigama viride (Appendix). In previous investigations of nuclear genome sizes in green algae, data from microspectrophotometry were corroborated with genome size estimates derived from NV data (Kapraun and Nguyen, 1994). Assuming a plant NV of 15 µm3 = 1·0 pg (Sparrow and Nauman, 1973; Kapraun et al., 1988), the NV of 12·6 µm3 calculated for Mesostigma is equivalent to a nuclear genome size of 0·8 pg, which closely approximates the present estimates.

Chlorokybales
This order is characterized by thalli of sarcinoid packets of cells that grow subaerially (Rogers et al., 1980). Chlorokybus atmosphyticus, one of the earliest diverging members of Charophyceae (Karol et al., 2001; Delwiche et al., 2002) (Fig. 11), has a plastid DNA sequence of 149–681 bp that closely resembles the Mesostigma plastid DNA in showing a high degree of putatively ancestral features (Turmel et al., 2002b). Unfortunately, no nuclear DNA content estimates have been published for any member of this important order.

Coleochaetales
Published chromosome numbers for three Coleochaete species (Sarma, 1982) include 1n complements of 24, 36 and 42, which almost certainly represent a polyploid sequence derived from a basic complement of x = 12. It was beyond the scope of the present study to determine chromosome numbers for the Coleochaete isolates investigated. However, the nuclear DNA content estimates of 1·4, 3·0 and 5·5 pg, which approximate a doubling sequence, are consistent with values that would be found in a polyploid sequence.

Molecular evidence includes Chaetosphaeridium globosum in Coleochaetales (Karol et al., 2001). In the present study, a 2C nuclear genome size of 1·2 pg was estimated for this species using microspectrophotometry (Appendix) and 1·23 pg using NV calculations. In Chaetosphaeridium, as in Coleochaete, the ploidy level of the isolates used in this study was not confirmed with chromosome counts.

Klebsormidiales
This order includes species of Klebsormidium and Entransia, which have simple, unbranched filaments with parietal laminate or lobed plastids (Lewis and McCourt, 2004). In the present study, 2C nuclear genome sizes for Klebsormidium flaccidum and Entransia fimbriata were estimated to be 0·4 and 1·1 pg, respectively (Appendix). An isolate of Klebsormidium nitens from Argentina, with a reported chromosome complement of n = 6 (Sánchez-Puerta and Leonardi, 2001), was investigated in the present study and found to have a nuclear DNA content of 2C = 0·55 pg (Appendix) or 539 Mbp. Thus, this species may have most nearly retained the proposed small ancestral nucleotype among extant streptophyte algae sampled.

Desmidiales and Zygnematales
Both the true desmids and the filamentous Zygnemataceae have undergone explosive speciation, resulting in thousands of described species (Prescott et al., 1972, 1977, 1981; Hoshaw and McCourt, 1988) from every continent. These algae represent the most species-rich group of charophytes with approximately 4000 species described (Gerrath, 2003). Two morphological synapomorphies unite the group: (1) the complete absence of flagellae in any life history stage, and (2) sexual reproduction by conjugation (McCourt et al., 2000). Molecular sequence data analyses confirm that the placoderm desmids are monophyletic, and constitute a group separate from the ‘false desmids’ and filamentous forms (McCourt et al., 2000; Gontcharov et al., 2003). Apparently, more complex forms evolved from simple filaments, and morphological switching from unicells to filaments occurred several times (Lewis and McCourt, 2004) (Fig. 11). Recent analysis of rbcL gene sequence data supports monophyly of Spirogyra and Sirogonium, two of the largest genera of filamentous Zygnemataceae (Drummond et al., 2005). The relationship of Desmidiales and Zygnematales to other streptophyte algae remains uncertain. Some molecular studies imply a close relationship between land plants (bryophytes) and conjugating green algae (Turmel et al., 2002a, b) whereas others suggest a more distant, sister group relationship (McCourt et al., 2000; Karol et al., 2001; Cimino and Delwiche, 2002; Delwiche et al., 2002).

Previous published nuclear DNA content estimates for the true desmids (Desmidiales) range from 2C = 1·1 to 20·7 pg (Hamada et al., 1985; Kapraun, 2005). Desmidiales are characterized by extensive polyploidy, with both inter- and intraspecific variation in chromosome complements reported (Hoshaw and McCourt, 1988). For example, published chromosome complements for Netrium digitus range from 1n = approx. 30 to approx. 592 (Sarma, 1982). Consequently, assignment of a C-value to specific DNA content estimates is arbitrary as chromosome counts were not made in this study for any of the isolates used in DNA quantification. In a previous investigation of Desmidiales (Kapraun, 2005), chromosome complements and nuclear DNA contents were found to be highly correlated (r2 = 0·7897), providing circumstantial evidence for the pervasive role of polyploidy in the evolution of this group of charophycean algae.

Previously published 2C nuclear DNA contents in Zygnematales ranged from 0·5 to 4·2 pg (Kapraun, 2005). As in Desmidiales, assignment of a C-value to specific DNA content estimates for isolates of Zygnematales is arbitrary. In general, both chromosome numbers (Sarma, 1982) and nuclear DNA contents (Fig. 11) are smaller in Zygnematales than in Desmidiales. Ploidy level in conjugating green algae may be of taxonomic significance as cell dimensions are considered to be diagnostic (Hoshaw and McCourt, 1988), and cell dimensions are highly correlated with genome size (Wang et al., 2005). Although the nucleotype role in gene expression remains poorly understood (Gregory, 2001, 2005a, b), it seems plausible that some of the described taxa of both desmid and filamentous conjugating green algae represent ploidy races, especially in species-rich genera characterized by a large variation in chromosome complements. It is widely assumed that many desmid genera are probably artificial and often display transitional forms to other genera. A recent molecular investigation of the desmid Staurastrum concluded that (1) the taxonomic significance of some morphological characters has been greatly overestimated, and (2) phylogenetic relationships were in conflict with previous formal and informal classification schemes (Gontcharov and Melkonian, 2005).

Charales
The exact relationship of the charophytes to land plants continues to be a subject of investigation. Several recent multigene phylogenies place Charales as the sister taxon to land plants (Karol et al., 2001; Cimino and Delwiche, 2002; Delwiche et al., 2002). Charales, commonly known as stoneworts or brittleworts, flourish in fresh and brackish water habitats throughout the world (Bold and Wynne, 1985). Charophytes are prone to calcification and have left an abundant fossil record to the Cretaceous and perhaps beyond (Grambast, 1974; Feist et al., 2003). The order is well circumscribed and includes six extant genera (McCourt et al., 1996; Sakayama et al., 2005), remnants of a once diverse but now largely extinct group (Feist et al., 2003). Analysis of 18S rRNA gene sequences indicated a poor correlation between molecular phylogeny and traditional hypotheses based on morphological criteria (Meiers et al., 1999). The base chromosome number for Chara is n = 7 and for Nitella is n = 3. However, many species exhibit polyploidy, with chromosome complements to n = 70 reported (Sarma 1982). Published nuclotype data are limited to five species of Chara (Maszewski and Kolodziejczyk, 1991; Kunachowicz et al., 2001) with 2C nuclear DNA contents ranging from 14·0 to 39·2 pg (Fig. 11). Two of these species, with 2n = 28, have 2C DNA contents of about 14 pg. Cytophotometric measurements of DNA content revealed differences in 1C DNA content between female (7·0 pg) and male (7·4 pg) isolates of Chara tomentosa (Kunachowicz et al., 2001).


   SUMMARY AND CONCLUSIONS
 TOP
 ABSTRACT
 INTRODUCTION
 METHODS
 RESULTS
 DISCUSSION
 SUMMARY AND CONCLUSIONS
 APPENDIX
 APPENDIX
 ACKNOWLEDGEMENTS
 LITERATURE CITED
 KEY TO REFERENCES 
 
DNA C-value remains a key character in biology, biodiversity and molecular investigations as genome size has many important practical implications (Bennett et al., 2000). In general, genome size directly influences the cost and difficulty of sequencing projects, and is therefore a primary consideration in choosing future sequencing subjects (Gregory, 2005a, b). Species with large DNA amounts can make use of standard fingerprinting techniques including AFLP problematic (Fay et al., 2005). Low DNA content (genomes approx. 100 Mpb) has been a major criterion in the selection of algae for genomic and genetic analyses (Peters et al., 2004; Waaland et al., 2004), including bacterial artificial chromosome (BAC) cloning technology, used for large-scale physical mapping and genomic sequencing (Wang et al., 2005). To date, candidate macroalgal (multicellular) species have genomes in the range 127–300 Mpb (Waaland et al., 2004). The present study can provide a great service both by expanding the list of target green algal species with appropriately small genome sizes, and by cautioning against use of taxa that may meet many other criteria for genomics investigations (Waaland et al., 2004), but have genome sizes too large for available technologies.

Recently, construction and characterization of large-insert BAC libraries has shown promise in the study of how important features in land plants originated and diversified (Liang et al., 2004). Unfortunately, the draft genome sequence available for the green alga Chlamydomonas reinhardtii (Wang et al., 2005) is of limited value in attempts to identify conserved ancestral genes because of the great phylogenetic distance between this chlorophyte and the streptophytes. The present study has indentified several streptophycean algae, including Klebsormidium and Coleochaete, with genome sizes that make them comparably tractable for genomic investigations.

The availability of a DNA C-values database and a consensus higher-level phylogenetic tree for green algae has opened the way for determining evolutionary trends in DNA amounts. Identification of the chlorophytes, streptophytes and prasinophytes as three of the most important extant green algal lineages provides an opportunity to suggest DNA content transformations which have accompanied their evolution, and to call attention to processes which may be unique or diagnostic for each group. Specific trends observed in this study are summarized below.

Summary for Ulvophyceae
Nuclear DNA content data from previously published investigations (Kapraun, 2005) and present research indicate that clade I of Ulvophyceae (Ulotrichales and Ulvales; O'Kelly et al., 2004) is characterized by relatively small nuclear genome sizes, whereas clade II (Caulerpales, Dasycladales, Cladophorales/Siphonocladales and Trentepohliales; Hanyuda et al., 2002) is characterized by substantially larger nuclear genome sizes (Fig. 4). It has been suggested that these differences in genome size ranges reflect the results of aneuploidy vs. polyploidy in clades I and II, respectively (Kapraun, 2005).

Summary for the charophycean lineage
The charophycean green algae are a sister group to land plants (Mishler et al., 1994; McCourt, 1995; McCourt et al., 2000; Lewis and McCourt, 2004). Ultrastructural data are overwhelmingly supported by the analyses of molecular data from nuclear ribosomal repeat units, mainly the small (18S) subunit, but including 5S and large-subunit (25S) rDNA sequences. Plastid genes including rbcL and small- and large-subunit rRNA yield similar results (Lewis and McCourt, 2004). Bryophytes are thought to comprise a grade of three monophyletic lineages (mosses, liverworts and hornworts) of uncertain relationship to each other (Shaw and Renzaglia, 2004) and to vascular plants (Palmer et al., 2004; Groth-Malonek and Knoop, 2005). Although the topology of the charophyte tree remains elusive (Friedl, 1997; Delwiche et al., 2002), comparison of the nucleotypes of charophycean green algae with those of early branching land plants, including bryophytes (Kenrick and Crane, 1997), could provide useful insights into the reconstruction of a common ancestral (generalized) nuclear genome (Pryer et al., 2002).

Hornworts, liverworts and mosses, in general, have nucleotypes characterized by small chromosomes (Inoue and Uchino, 1969) and chromosome complements of 2n ≥ 30 and/or 2C nuclear DNA contents >1 pg (Renzaglia et al., 1995; Voglmayr, 2000) (Fig. 12). Although greater values for both parameters are known in bryophytes, they appear to be restricted to polyploid species and do not contradict the generalization. For example, more than 80 % of the nuclear DNA C-values in mosses were reported to occur in a narrow peak between 0·25 and 0·6 pg (Voglmayr, 2000). It has been suggested that the small DNA amounts and low C-value variation are linked to the biflagellate nature of bryophyte sperm cells (Renzaglia et al., 1995). As nuclear genome size and sperm cell size are tightly correlated (Murray, 2005), and sperm cells are thought to lose motility drastically with increasing size, a strong selection pressure against larger sperm, and therefore also against larger DNA amounts, is hypothesized (Voglmayr, 2000).


Figure 12
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FIG. 12. Comparison of chromosome numbers and nuclear genome sizes in the charophycean and embryophyte lineages. Closed circles: DNA data for streptophyte algae from Kapraun (2005) and the Appendix, and for the bryophytes from Renzaglia et al. (1995) and Voglmayr (2000). Open circles: DNA data from Mandoli (2001).

 
These observations gain additional significance in the context of the suggestion that the common ancestor of all angiosperms may have possessed a small genome (Leitch et al., 1998, 2005). Small genome size in angiosperms appears to be correlated with phenotypic characteristics such as rapid seedling establishment, short minimum generation times, reduced cost of reproduction and an increased reproductive rate (Bennett, 1987; Midgley and Bond, 1991; Bennett and Leitch, 2005a, b). Consequently, small genome size may permit greater evolutionary flexibility (Leitch et al., 1998), whereas larger size and amplification may lead to ‘genomic obesity’ (Bennetzen and Kellogg, 1997; Bennetzen, 2002; Gregory, 2005a; Knight et al., 2005). It is recognized that although nuclear genome size is highly correlated with many cellular and ecological parameters, ‘correlation’ and ‘causation’ are far from interchangeable (Gregory, 2005a, b). The many complex causal factors behind these observations remain obscure.

Published molecular studies have implicated both the conjugating green algae (Turmel et al., 2002a, b) and the charophytes (Karol et al., 2001; Cimino and Delwiche, 2002; Delwiche et al., 2002) as the closest sister group to land plants. Consequently, it is worth noting that published nucleotype data for these charophycean algae suggest that they share a unique constellation of karyotype features that differ substantially from the most closely related bryophytes. Many taxa in Charales, Desmidiales and Zygnematales are highly polyploid (Sarma, 1982; Hoshaw and McCourt, 1988; Kunachowicz et al., 2001) and can be characterized either by chromosome complements of 2n>30 or 2C nuclear DNA contents >1 pg, or both (Fig. 12). In addition, both filamentous and unicellular (desmid) forms of the conjugating green algae have chromosomes with an ‘absence of localized centromeres’ (Godward, 1966) or ‘polycentric chromosomes’ (King, 1960; Sarma, 1982; Hoshaw and McCourt, 1988). Karyotype analyses also indicate an extraordinary range in chromosome lengths, from 1 to 20 µm (King, 1960). Both of these green algal groups typically have asymmetric (specialized) karyotypes and large chromosomes up to 12 µm long (Sarma, 1982; Hoshaw and McCourt, 1988; Kunachowicz et al., 2001), suggesting a structural distinction with land plant karyotypes.

In contrast to the conjugating green algae and charophytes, some extant members of other groups of streptophytes, including Coleochaetales and Klebsormidiales, have an unspecialized nucleotype with both a small genome size and a small chromosome complement. In the present investigation, nuclear DNA content estimates of <1 pg were found in several isolates of Coleochaete,