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Invited Special Papers |
2Duke University, Department of Biology, Box 90338, Durham, North Carolina 27708 USA; 3Department of Plant Biology, Southern Illinois University, Carbondale, Illinois 62901-6509 USA
Received for publication January 5, 2004. Accepted for publication June 15, 2004.
| ABSTRACT |
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Key Words: Anthocerophyta Bryophyta bryophyte phylogeny hornworts liverworts Marchantiophyta mosses tree of life
| INTRODUCTION |
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Sporophytes of bryophytes are without exception monosporangiate and matrotrophic throughout their life span (Graham and Wilcox, 2000
). Ephemeral and dependent on the gametophyte for nutrition and protection, they never exhibit the modular, indeterminate growth form of the gametophyte generation. In their greatest structural complexity, bryophyte sporophytes consist of a nutritive foot, elongating pedicel or seta, and a single terminal sporangium or capsule. Formative divisions in the embryo produce all precursor components of the sporophyte; i.e., distinct embryonic regions are determined to develop into the three organographic zones of the mature sporophyte: sporangium, seta, and foot. In contrast, an apical meristem initial develops in the embryo of tracheophytes and is subsequently responsible for continuous production of repeated shoot and root modules in these plants (Bierhorst, 1971
; Kato and Imaichi, 1997
). Capsules of bryophytes are structurally elaborate and, in some instances, exhibit complicated mechanisms for spore production and dispersal. Basal sporophyte elongation with nonsynchronized spore production in hornworts, elaters in liverworts, and peristomes of mosses provide examples of this complexity.
General treatments of bryophyte morphology can be found in Leitgeb (18741881)
, Campbell (1895)
, Goebel (1905)
, Smith (1955)
, Parihar (1965), Watson (1971)
, Puri (1973)
, Richardson (1981)
, Schofield (1985)
, and Crum (2001)
. The Manual of Bryology, edited by Verdoorn (1932)
, contains authoritative treatments of selected bryology topics that summarized the state of our knowledge at that time, and the New Manual of Bryology, edited by Schuster (1984)
, provided expanded updates more than fifty years later. Both manuals are still useful. Other edited volumes on various aspects of bryophyte biology especially relevant to the tree of life include Clarke and Duckett (1979)
, Smith (1982)
, and Shaw and Goffinet (2000)
.
The crucial position of bryophytes in embryophyte evolution
An unambiguous conclusion from the multitude of contemporary phylogenetic investigations of streptophytes is that bryophytes are the first green plants to successfully radiate into terrestrial niches. These small, inconspicuous plants have existed for several hundreds of millions of years and have played a prominent role in shaping atmospheric and edaphic change and the subsequent evolution of all forms of plant life on land. Explorations of life history phenomena in bryophytes and a solid understanding of interrelationships among them are necessary to reconstruct the early evolution of embryophytes.
The concept that the embryo/sporophyte evolved in land plants through intercalation of mitotic divisions between fertilization and meiosis is widely accepted (Graham, 1993
; Graham and Wilcox, 2000
). Based on this axiom, land plant evolution proceeded in the direction of progressively more elaborate sporophytes. Although generally true, unconditional acceptance of this trend leads to conclusions that ignore processes of reduction and parallel/convergent evolution, phenomena that have occurred repeatedly during bryophyte diversification (Schuster, 1992
; Niklas, 1997
; Boisselier-Dubayle et al., 2002
). A defining characteristic of embryophytes is the meiotic production of spores in tetrads and sporopollenin-impregnated spore walls. Because of their resistance to degradation, fossil spores have provided valuable clues to the initial stages of land colonization (Taylor, 1995
; Wellman and Gray, 2000
; Wellman et al., 2003
). The earliest confirmed land plant fossils are spores, speculated to be from an ancient liverwort dating to the middle Ordovician, some 475 million years ago (mya) (Wellman et al., 2003
).
Gametophytes of bryophytes also provide critical clues about land plant evolution. Thalloid and filamentous growth forms are shared with pteridophytes, but the completely subterranean and nonphotosynthetic life histories found in many lycophytes and some ferns show no homology in bryophytes (Bierhorst, 1971
). The achlorophyllous gametophyte of the liverwort Cryptothallus is a recent acquisition within a strictly photosynthetic lineage (Renzaglia, 1982
). Unlike pteridophytes, bryophyte gametophytes frequently show organ development (leaf, stem, and rhizome) and extensive tissue differentiation, including conducting and supportive tissues (Hé bant, 1977
; Ligrone et al., 2000
). Production of multicellular gametangia was an innovation in embryophytes that was a necessary precursor to embryo development (Graham and Wilcox, 2000
). Among land plants, only mosses and liverworts produce superficial gametangia, which are variously protected by elaborate appendages, including leaves. Hornworts sequester vulnerable organs in internal compartments (Renzaglia et al., 2000
; Renzaglia and Vaughn, 2000
).
A lack of intermediate forms in both life history phases and the potential to interpret morphological transitions in opposite directions have obscured relationships among bryophytes and pteridophytes. Understanding morphological evolution requires unambiguous establishment of phylogenetic relationships among and within bryophyte lineages. Over the past decade, great strides have been made toward reaching this goal; however, fundamental questions remain.
In addition to elucidating early patterns of morphological diversification in embryophytes, bryophytes are crucial to understanding plant genome evolution. Approximately 66% of genes identified from expressed sequence tag analyses of gene expression in gametophytes of Physcomitrella patens have homologues in the Arabidopsis genome, consistent with the hypothesis that genes expressed in the diploid plant body of angiosperms were expressed in the gametophytes of early land plants and were recruited for sporophytic morphogenesis later in plant phylogeny (Nishiyama et al., 2003
). Phylogenetic and functional analyses of genes expressed in Physcomitrella gametophytes have clarified the phylogenetic history of several important gene families, including MIKC-type MADS-box genes (Krogan and Ashton, 2000
; Henschel et al., 2002
; Hohe et al., 2002
) and homeobox genes (Champagne and Ashton, 2001
). Phylogenetic analyses of the KNOX (homeobox) gene family across the land plant tree of life have provided insights into the history of gene duplication and functional divergence during embryophyte history (Champagne and Ashton, 2001
). Because KNOX genes are involved in expression of meristematic activity in vascular plant sporophytes, functional analyses of KNOX genes in mosses, liverworts, and hornworts are central to understanding evolution of plant development in embryophytes. Comparable studies of genes involved in flower development are underway, and, in the context of phylogenetic analyses of bryophytes, the early evolution of these genes is now a tractable problem for investigation (Himi et al., 2001
).
Relationships among the three lineages
Relationships among the three lineages of bryophytes remain one of the major unresolved questions in plant evolutionary biology (Goffinet, 2000
). Virtually every conceivable hypothesis has been put forth in regards to primary branching patterns at the base of embryophytes. Most commonly, bryophytes are viewed as a grade of three monophyletic lineages, with an uncertain branching order (Mishler et al., 1994
; Qiu et al., 1998
). Controversy often focuses on which bryophyte group is sister to all other embryophytes, with two hypotheses most frequently supported: liverworts as sister to other embryophytes vs. hornworts as the sister group (Mishler et al., 1994
; Hedderson et al., 1996
, 1998
; Malek et al., 1996
; Garbary and Renzaglia, 1998
; Qiu et al., 1998
; Beckert et al., 1999
; Duff and Nickrent, 1999
; Nishiyama and Kato, 1999
; Soltis et al., 1999
; Nickrent et al., 2000
; Renzaglia et al., 2000
; Stech et al., 2003
). A moss-plus-liverwort clade has been recovered in several of these analyses (Hedderson et al., 1996
, 1998
; Nishiyama and Kato, 1999
; Nickrent et al., 2000
; Renzaglia et al., 2000
). Recently, it was postulated that hornworts, not mosses, are the closest living relative of tracheophytes. This speculation finds support in sequence data as well as in structural genomic features (Samigullin et al., 2002
; Kelch et al., in press
). In contrast, recent analyses of amino acid sequences based on entire plastid genomes provided support for a monophyletic bryophyte assemblage; however, these results must be viewed with caution because of severe limitations in taxon sampling (Nishiyama et al., in press
).
The focus of this review is to present the current state of knowledge on phylogenetic relationships within, not among, hornworts, liverworts, and mosses. Emphasis is placed on synthesizing results of recent molecular investigations that have revolutionized interpretations of genetic and morphological diversification within each of these groups. Intriguing new perspectives on character evolution have emerged from these studies.
| ANTHOCEROTOPHYTA |
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Hornworts have remained relatively unexplored at all levels of phylogenetic inquiry (Renzaglia and Vaughn, 2000
; Stech et al., 2003
; Duff et al., in press
). The perception that hornworts are invariable, elusive, and difficult to identify has contributed to the paucity of systematic studies within the group. This small, homogeneous assemblage contains 100150 poorly delineated species (Schuster, 1992
). Concepts of interrelationships among hornworts based on morphology, and the resulting classification schemes, show virtually no consensus at the generic, familial, and ordinal levels (Mishler and Churchill, 1984
; Hasegawa, 1988
; Hässel de Menéndez, 1988
; Schuster, 1992
; Hyvönen and Piippo, 1993
; Renzaglia and Vaughn, 2000
). Twelve genera of hornworts have been named, Anthoceros, Dendroceros, Folioceros, Notothylas, Megaceros, Phaeoceros, Aspiromitus, Hattorioceros, Leiosporoceros, Nothoceros, Mesoceros, and Sphaerosporoceros, of which only the first six are widely recognized.
Even with the advent of molecular systematics and a renewed interest in early land plant phylogeny, hornwort sampling has been sparse, with one to three taxa included in most analyses (Katoh et al., 1983
; van de Peer et al., 1990
; Mishler et al., 1994
; Bopp and Capesius, 1996
, 1998
; Hedderson et al., 1996
, 1998
; Malek et al., 1996
; Qiu et al., 1998
; Beckert et al., 1999
; Duff and Nickrent, 1999
; Nishiyama and Kato, 1999
; Soltis et al., 1999
; Nickrent et al., 2000
). Among the dozens of papers on bryophyte phylogeny over the past ten years, there is only one comprehensive molecular analysis of within-hornwort relationships, based on rbcL gene sequences from 20 hornworts (Duff et al., in press
). A second study utilizing the plastid trnL intron sampled nine hornworts but focused on the position of the group among land plants (Stech et al., 2003
). Results of these analyses are congruent and reveal novel but intuitive relationships. The rbcL analysis provided much greater resolution of hornwort interrelations because of more extensive sampling, including additional species of the five genera included in the trnL study and representatives of three other genera (Folioceros, Leiosporoceros, and Nothoceros). The discussion that follows will focus on taxonomic inferences and morphological character evolution that emerge from scrutiny of the consensus phylogenetic pattern supported by these pioneering studies (Fig. 1).
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The sporophyte of Leiosporoceros is elongated and robust, and its anatomy departs significantly from that of other hornworts (Fig. 4A). The suture is highly differentiated and visible as a deep longitudinal groove. The assimilative and sporogenous regions are massive when compared with other hornworts. Several layers of small spore tetrads are surrounded by mucilage and interspersed with groups of large, elongated pseudoelaters (Fig. 5A). Stomata are abundant and appear similar to those in more derived taxa (Fig. 6A). Clearly, the shared traits between Leiosporoceros and other hornworts provide insight about plesiomorphies within the group. For example, stomata and large numbers of antheridia are best interpreted as ancestral hornwort traits. On the other hand, unique morphological traits that characterize Leiosporoceros are presumed autapomorphies and likely reflect the deep evolutionary separation of this genus from other hornworts. Further molecular and morphological studies are required to evaluate these hypotheses.
After Leiosporoceros, Anthoceros plus Folioceros form a clade sister to other hornworts (Fig. 1). Taxonomic treatments have generally recognized a sister relationship between Anthoceros (including Folioceros) and Phaeoceros, placing them in the same family or subfamily. Thus genetic divergence between Anthoceros plus Folioceros and the remaining taxa appears problematic at first glance. Similarities between Anthoceros, Folioceros, and Phaeoceros include rosette-like habits (Fig. 2A), large solitary chloroplasts with well-developed pyrenoids (Fig. 3B), and comparable sporophyte anatomy (Fig. 4B). However, clearly defined features distinguish Anthoceros and Folioceros from other hornworts; these include dorsal lamellae, schizogenous mucilage cavities, and antheridia in large groups of up to 50 per cavity, as compared to 14 (6) antheridia per cavity in other hornworts. Darkly pigmented spores with well-defined trilete marks also serve to differentiate these taxa from other hornworts (Fig. 5B). Molecular evidence that Anthoceros plus Folioceros form a clade sister to all other hornworts (except Leiosporoceros) has reinforced the taxonomic value of diagnostic morphological features that are restricted to these two genera.
Close affinity between Folioceros and Anthoceros is well supported by rbcL data and reflected in most current classifications (Hasegawa, 1988
, 1994
; Schuster, 1992
; Hyvönen and Piippo, 1993
). In contrast, Hässel de Menéndez (1988)
segregated Folioceros into a monotypic family and order based on spore ornamentation and pseudoelaters. Folioceros has thick-walled, reddish brown, highly elongated pseudoelaters, whereas Anthoceros has short, thin-walled multicellular pseudoelaters similar to those of Phaeoceros (Fig. 5D). Additional differences are found in the placenta and chloroplasts of these two taxa (Vaughn et al., 1992
; Vaughn and Hasegawa, 1993
). With only a single species included in the rbcL sequence analysis, it is not possible to evaluate monophyly of Folioceros.
The remaining hornworts form a monophyletic group that includes two well-supported assemblages: Phaeoceros laevis sensu lato (represented in Fig. 1 by P. carolinianus) plus Notothylas and Megaceros plus Dendroceros. A close affinity between Phaeoceros and Notothylas was suggested by Hässel de Menéndez (1988)
, who placed these two genera in the family Notothyladaceae. Both genera have chloroplasts with prominent pyrenoids, spores with an equatorial girdle (Fig. 5C), and 24 (6) antheridia per chamber. However, because of the distinctive sporophyte of Notothylas (Fig. 2D), most systematists have segregated this genus into a monotypic subfamily, family, or order (Singh, 2002
). Notothylas is the only hornwort taxon in which growth of the sporophyte is abbreviated, spore production appears synchronized, stomata are absent, and the columella is normally absent to poorly developed, a combination of characters that indicate affinities with liverworts. Consequently, it has been suggested that the Notothylas sporophyte is plesiomorphic, representing a structural "link" with other bryophytes. Under this interpretation, hornwort radiation involved an elaboration of sporophytes in more derived taxa (Campbell, 1895
; Mishler and Churchill, 1984
; Graham, 1993
; Hyvönen and Piippo, 1993
; Hasegawa, 1994
). An alternative hypothesis, supported by molecular data, is that sporophytes in Notothylas are not representative of the ancestral condition in hornworts but are highly reduced and specialized (Lang, 1907
; Bartlett, 1928
; Proskauer, 1960
; Renzaglia, 1978
; Schofield, 1985
; Schuster, 1992
). Features such as the existence of a relictual and largely nonfunctional suture in some species support the derived nature of the Notothylas sporophyte. If parallel reduction in sporophye complexity occurred among hornwort genera, Notothylas may be polyphyletic (Lange, 1907
; Proskauer, 1960
). An evaluation of this hypothesis requires increased taxon sampling across the hornworts.
Diversity within Phaeoceros is particularly evident in spore morphology (Schuster, 1992
). Phaeoceros laevis s. l., includes species with spiny papillate spores, whereas ornamentation in the remaining species varies from vermiculate to blunt, wartlike projections. As described later, the three representatives of Phaeoceros with vermiculate spores included in molecular analyses are more closely related to Megaceros than to P. laevis s. l.
A close relationship between Megaceros and Dendroceros is evident in morphological characters such as spiraled pseudoelaters (Fig. 5E, F), absence of stomata, and solitary antheridia. The only epiphytic hornwort, Dendroceros, has a thickened, central midrib with perforated wings (Fig. 2B, C); large, central pyrenoids in each plastid; and multicellular spores (Fig. 5E) (Hasegawa, 1980
; Renzaglia and Vaughn, 2000
). Diagnostic features of Megaceros include unicellular green spores with distal mammilla (Fig. 5F), the absence of a pyrenoid, and multiple plastids per cell (Hasegawa, 1983
; Valentine et al., 1986
; Vaughn et al., 1992
). However, as discussed next, the demarcation between Megaceros and Dendroceros is not always well defined, especially with regard to growth form (Proskauer, 1953
; Hässel de Menéndez, 1962
).
A clade containing two species of Dendroceros is sister to a monophyletic assemblage that includes species previously placed in Megaceros, Phaeoceros, Nothoceros, and Dendroceros (Fig. 1). This taxonomically heterogeneous group in turn consists of two clades: the first includes two Old World species of Megaceros, the Austral-Asian M. flagellaris and M. denticulatus (Hasegawa, 1983
; Glenny, 1998
), and the second is an assemblage of species from four generic segregates. Three Phaeoceros species, P. coriaceus (Steph.) Campbell, P. hirticalyx Steph., and Phaeoceros chiloensis (Steph.) Hässel de Menéndez, are included within the second Megaceros clade (Stech et al., 2003
; Duff et al., in press
). All these species have spores with markedly different architecture from those of other Phaeoceros (Fig. 5C). Moreover, these species have monoandrous androecia and multiple chloroplasts that lack pyrenoids, two diagnostic characters of Megaceros (Duff et al., in press
). However, lack of spiraled pseudoelaters, existence of stomata, and yellow, not green, spores are defining features of Phaeoceros. Bartlett (1928)
and Proskauer (1951)
noted that morphological boundaries between Megaceros and Phaeoceros are blurred and that similarities in growth form and chloroplast structure suggest a close relationship between the two. Molecular analyses have indicated that Phaeoceros with vermiculate spores and mamillae on the distal faces are more closely related to Megaceros than to Phaeoceros with papillate spores (P. laevis s. l.) (Fig. 5B).
The crown group of Megaceros consists of M. aenigmaticus, the only North American representative of the genus; M. vincentianus, the only species from the Neotropics; Dendroceros canaliculatus (= M. canaliculatus), and Nothoceros giganteus (= M. giganteus). The last two species have thickened midribs and wings, which accounts for previous, and apparently inappropriate, placements in Dendroceros or the newly delineated Nothoceros. The existence of unicellular, mamillate spores, and plastids devoid of pyrenoids clearly place these species in Megaceros. Thus, scrutiny of the morphology of these seemingly disparate hornwort species reveals features that solidify their inclusion in the Megaceros clade. The well-developed costa and monostromatic wings in these taxa were likely a result of parallel evolution with Dendroceros.
Inferences about morphological evolution in hornworts from molecular analyses
One intriguing feature of hornworts is the large, solitary chloroplast with a prominent pyrenoid, which is shared with green algae but has no parallel in any other embryophyte group. Within hornworts, pyrenoids appear to have been lost multiple times. Similar pyrenoid losses (and gains) have been described in several algal lineages (Hoham et al., 2002
; Nozaki et al., 2002
). In hornworts, chloroplast compartmentalization characterizes several taxa, including Leiosporoceros and certain species of Phaeoceros, Anthoceros, and Megaceros (Burr, 1970
; Valentine et al., 1986
; Vaughn et al., 1992
; Duff et al., in press
). This arrangement is consistent with a carbon-concentrating mechanism typical of organisms with pyrenoids, including other hornworts (Smith and Griffiths, 1996
, 2000
; Hansen et al., 2002
). It has been speculated that the "pyrenoid-like" area evident in certain hornworts represents a transitional state from presence to complete absence of the pyrenoid (Burr, 1970
). An evolutionary inference supported by this interpretation, in addition to the phylogenetic topology presented in Fig. 1, is that a solitary plastid with a pyrenoid is plesiomorphic in hornworts. In Leiosporoceros, the plastid is solitary but without a pyrenoid, the remnant of which is a compartmentalized organelle with peripherally aggregated starch and centralized grana and plastoglobuli (Fig. 3A). Independent losses of the pyrenoid with or without organellar compartmentalization occurred at least once each in Megaceros, Notothylas, and Anthoceros (Vaughn et al., 1992
; Singh, 2002
; Duff et al., in press
). In Phaeoceros hirticalyx, P. coriaceus, and P. chilioensis, species that are probably better placed in Megaceros, loss of the pyrenoid may be interpreted as preceding the evolution of spiraled pseudoelaters and stomatal loss.
As structures that facilitate gas exchange, stomata are important innovations in the diversification of land plants. Their presence in hornworts has been viewed either as a synapomorphy with mosses and tracheophytes or as a homoplastic acquisition within hornworts (Mishler and Churchill, 1984
; Kenrick and Crane, 1997
; Renzaglia et al., 2000
). The presence of stomata in Leiosporoceros, Anthoceros, and Folioceros supports the contention that these structures are plesiomorphic in hornworts and may be homologous to those in mosses and/or tracheophytes. A clear case of homoplasy is the loss of stomata in at least three, possibly four, hornwort lineages: Notothylas, Dendroceros, and Megaceros. Stomatal loss may have accompanied modifications in sporophyte development, e.g., maturation of the sporophyte within the protective gametophytic involucre where gas exchange is limited (Notothylas, Fig. 2D and Dendroceros, Fig. 2C). Stomatal loss in Megaceros is associated with occurrence of these species in periodically inundated habitats. The existence of P. coriaceus, P. hirticalyx, and P. chiloensis, three terrestrial species with stomata, supports this hypothesis. The topology presented in Fig. 1 necessitates at least two losses of stomata in the Megaceros clade.
The interpretation set forth by Proskauer (1951)
and Schuster (1992)
that mucilage clefts on the ventral side of the gametophyte in hornworts (Fig. 6B) are homologous to sporophytic stomata (Fig. 6A) is not supported by molecular analysis. Absence of mucilage clefts in Leiosporoceros and the specialized function of these structures in all other hornworts indicate that gametophytic "stomata" evolved after hornwort diversification simply as an entryway for the cyanobacterium, Nostoc.
It is reasonable to hypothesize that the habit of extant members of Anthoceros, Leiosporoceros, and Phaeoceros represent the ancestral condition in hornworts and may be related to their common occurrence on exposed soil. Morphological diversity in other taxa likely results from radiation into and consequent adaptations to specialized habitats; e.g., Dendroceros is an epiphyte, and Megaceros is restricted to tropical or temperate sites where it often occurs submerged in streams. Diversification of Dendroceros may be correlated with the evolution of angiosperms, which provided abundant new bark and leaf habitats (Ahonen et al., 2003
). Notothylas is an ephemeral hornwort that grows as a pioneer on soil. Unlike other genera in which spores are wind dispersed, Notothylas spores are dispersed by water or facultatively by insects or other animals, thus eliminating the "need" for vertical elongation of the sporophyte.
| MARCHANTIOPHYTA |
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Unlike hornworts, but comparable to mosses, is the production of a variety of organized external appendages, most of which function in protecting fragile tissues. For example, various mucilage papillae, hairs, scales, bracts, cups, or flask-shaped structures protect the meristem, gemmae, and other vegetative organs. Especially vulnerable are the superficial sex organs that often occur in clusters protected by flaps of tissue, leaf lobes, young leaves, or modified branches (Fig. 9B).
The uniformity and uniqueness of liverwort sporophytes provide compelling evidence for monophylly of hepatics. Unlike mosses and hornworts, sporophytes of liverworts reach maturity within the confines of protective gametophytic tissue that develops from the shoot/thallus (= perigynium or coelocaule) and/or archegonium (= calyptra). Additional gametophytic structures such as perianths, pseudoperianths, bracts, scales, and involucral flaps may further surround the sporophyte and associated protective tissue. In such a milieu, photosynthesis is limited, and the sporophyte derives nourishment from the gametophyte through a placenta. The seta is pale to hyaline, and the capsule is devoid of stomata. The majority of liverwort sporophytes are differentiated into foot, seta, and capsule; in the occasional marchantioid taxon (e.g., Riccia, Corsinia), the seta and/or foot is vestigial or absent. At completion of meiosis and spore development, cells of the seta typically undergo rapid elongation through water imbibition and thus elevate the capsule away from the substrate. Sterile, elongated elaters have hygroscopic, spiraled, inner-wall thickenings, that are strategically interspersed among spores to facilitate their separation and dispersal (Fig. 9E). Capsule dehiscence normally entails a patterned separation into four longitudinal valves, but variations range from two valves through irregular fragments or plates to cleistocarpous capsules.
The backbone of liverwort phylogenetic relationships
Crandall-Stotler and Stotler (2000)
used morphological characters in a cladistic analysis of liverworts. Their analyses included 34 taxa and 61 characters, and they resolved two main lineages: complex thalloids (Marchantiopsida) and simple thalloids plus leafies (Jungermanniopsida: Metzgeriidae, Jungermanniidae, respectively). However, their sampling was not extensive enough to address phylogenetic issues within any of the major clades. There are a few taxa for which placement relative to the three large groups is ambiguous on the basis of morphological, ultrastructural, and chemical features. These include Treubia and Apotreubia (Treubiales), Monoclea (Monocleales), Sphaerocarpos, Geothallus and Riella (Sphaerocarpales), Blasia and Cavicularia (Blasiales), and Haplomitrium (Haplomitriales [Calobryales]). Early molecular analyses of the liverworts were limited to single genomic regions with limited taxon sampling (e.g., Lewis et al., 1997
; Bopp and Capesius, 1998
; Beckert et al., 1999
; Stech and Frey, 2001
) but recent multigene analyses with increased sampling have begun to clarify phylogenetic relations among (and within) the major groups of liverworts. Phylogenetic relationships within Marchantiopsida (complex thalloids) from DNA sequence data were analyzed by Bischler (1998)
, Wheeler (2000)
, and Boisselier-Dubayle et al. (2002)
. Forrest and Crandall-Stotler (in press)
focused on Metzgeriidae (simple thalloids), whereas He-Nygrén et al. (in press)
sampled a wide diversity of liverwort taxa. Davis (in press)
provided the most extensive analysis of relationships among leafy liverwort genera available to date.
Davis (in press)
reconstructed "backbone" relationships among liverworts based on a combined data set including two nuclear, three mitochondrial, and eight loci sequenced from 20 liverworts and three outgroup mosses (Fig. 7). The data were analyzed using maximum parsimony, maximum likelihood, and Bayesian inference, and most of the results were robust to these alternative methods. The liverworts are resolved as monophyletic, as are class Marchantiopsida (complex thalloids) and Jungermanniidae (leafies). Metzgeriidae are resolved as a grade paraphyletic to Jungermanniidae, in agreement with earlier studies. Although Forrest and Crandall-Stotler (in press)
sampled different species, results of their analysis of five plastid loci are congruent with those of Davis (in press)
.
Although Haplomitrium has generally been regarded as an early-diverging lineage within the liverworts (Smith, 1955
; Schuster, 1984
; Renzaglia et al., 1994
), the precise placement of this genus remains problematic. The gametophyte of Haplomitrium is erect and radially symmetrical and therefore reminiscent of both jungermannialean liverworts and mosses. Prior to the discovery of antheridia and sporophytes in Takakia (Smith and Davison, 1993
; Renzaglia et al., 1997
), Haplomitrium was considered closely related to Takakia because of gametophytic similarities (Schuster, 1972
, 1984
). More recent molecular and morphological data have come together to solidify the placement of Takakia among mosses (see later). Divergent opinions have been expressed with regard to the relationship of Haplomitrium to other hepatics. A conclusion from Bartholomew-Began's (1990
, 1991)
extensive morphogenetic reevaluation of Haplomitrium was that the genus is a member of the simple thalloid lineage. In their analysis of land plant relationships based on rbcL sequences, Lewis et al. (1997)
noted that the precise position of the genus depended on the data set analyzed (1st and 2nd vs. 3rd positions, all positions, "ts/tv" weighting); Haplomitrium fell out sister to all other embryophytes, sister to all other liverworts, or nested within the liverworts and sister to the leafy taxa. Nuclear 18S rDNA sequences resolved Haplomitrium (without bootstrap support) as sister to the class Jungermanniopsida (i.e., leafies plus simple thalloids; Hedderson et al., 1996
).
Recent multigene analyses have focused on two hypotheses: Haplomitrium is either sister to Jungermanniopsida or sister to all other liverworts. In contrast to almost all other nodes on her tree, Davis (in press)
reported that the placement of Haplomitrium varied among analyses. Under parsimony, likelihood, and Bayesian methods, Haplomitrium is resolved with strong support as sister to Jungermanniopsida (simple thalloids plus leafies), and this inclusive clade is in turn sister to Marchantiopsida (complex thalloids; Fig. 7). However, the most complex heterogeneous Bayesian substitution model, with 21 partitions, yielded Haplomitirum as the sister group to all other liverworts. Forrest and Crandall-Stotler (in press)
and Qiu (2003) reported that Haplomitrium plus Treubia form a clade sister to all other hepatics. However, the sister-group relationship was unsupported. When Treubia was excluded from the analysis by Forrest and Crandall-Stotler (in press)
, the position of Haplomitrium was unresolved. Thus, the affinities of Haplomitrium are not yet satisfactorily resolved; Davis (in press)
felt that the weight of the current evidence supports a position for the genus as sister to the class Jungermanniopsida, whereas Qiu (2003) and Forrest and Crandall-Stotler (in press)
favor a position as sister to all other hepatics.
Although unexpected, the affinity between Treubia and Haplomitrium finds support in morphology. Both are "leafy" taxa with gametangia situated in leaf axils or lobules. Treubia is decisively more dorsiventral, with an oblique to transverse leaf insertion (succubous) and small dorsal lobules (Renzaglia, 1982
), whereas some species of Haplomitrium tend toward anisophylly and succubous insertion (Bartholomew-Begin, 1991
). In both genera, a tetrahedral apical cell is responsible for shoot growth. Perhaps the most compelling evidence for a close relationship between these two genera icomes from the peculiar yet similar sperm cells that they produce. Cladistic analyses based on spermatogenesis consistently recovered a Treubia plus Haplomitrium clade that is sister to the remaining liverworts (Garbary et al., 1993
; Renzaglia and Garbary, 2001
). Stech et al. (2000)
elevated Treubia to class Treubiopsida based on trnL intron sequence divergences between it and other liverworts.
Systematics and phylogeny of the Marchantiopsida (complex thalloid liverworts)
Unlike other hepatic groups, the complex thalloid liverworts include relatively drought-resistant species. Many morphological features of Marchantiopsida indicate xeromorphic adaptations (Schuster, 1992
; Wheeler, 2000
). In addition to air chambers in the dorsal part of the thallus (Fig. 9A), marchantioid liverworts are characterized by two types of rhizoids (smooth and pegged), archegonial involucres, unlobed spore mother cells, four primary androgones in the antheridium, six rows of neck cells in the archegonium, idioblastic oil body cells, ventral thallus scales, unistratose capsule walls, and a simple locomotory apparatus in the small biflagellated sperm cell (Schuster, 1966
, 1992
; Renzaglia et al., 2000
; Renzaglia and Garbary, 2001
). Of these, only features of the sperm appear to be universal in all species.
Although Marchantiopsida are resolved as monophyletic, traditional relationships among taxa generally are not supported by molecular data. The classical morphological separation of this liverwort class into three orders; i.e., Monocleales, Sphaerocarpales, and Marchantiales, is challenged by nucleotide sequence data (Wheeler, 2000
; Boisselier-Dubayle et al., 2002
). Incongruence between morphological and molecular patterns may be attributed to parallel changes in multiple lineages (Boisselier-Dubayle et al., 2002
).
The multigene analyses of Davis (in press
, Fig. 8) and Forrest and Crandall-Stotler (in press)
provided strong support for the placement of Blasia as a member of the complex thalloids, a result that conflicts with the traditional placement of this liverwort within the simple thalloids (Renzaglia, 1982
). Sperm cell features, persistent ventral scales, a small wedge-shaped apical cell, and a Monoclea-like female involucre provide morphological evidence for the inclusion of Blasia in the complex thalloid lineage (Renzaglia and Duckett, 1987
; Pass and Renzaglia, 1995
; Renzaglia and Garbary, 2001
). Previous molecular analyses based on one or two gene sequences do not agree in the placement of Blasia. Stech and Frey (2001)
resolved Blasia as sister to Jungermanniopsida (simple thalloids plus leafies) and described the new class, Blasiopsida. Their study was based solely on trnL intron sequences (ca. 500 bp), and the relationship was without bootstrap support. Wheeler (2000)
found that Blasia grouped with the simple thalloids (Metzgeriidae) based on 26S nrDNA (also without bootstrap support), and He-Nygrén et al. (in press)
resolved Blasia as sister to the remaining liverworts.
After Blasia, Sphaerocarpos is the next divergent taxon (Fig. 8). A position for Sphaerocarpales (Sphaerocarpos, Riella, Geothallus) among complex thalloids is generally supported by morphology (Smith, 1955
; Bishler, 1998
; Crandall-Stotler and Stotler, 2000
; Boisselier-Dubayle et al., 2002
). However, with additional taxon sampling, the sister relationship between Sphaerocarpales and the remaining Marchantiopsida is called into question. Based on LSU rDNA sequences, Wheeler (2000)
and Boisselier-Dubayle et al. (2002)
reported that Sphaerocarpales were placed within Marchantiaceae. Similarly, Sphaerocarpos nested between Neohodgsonia and Marchantia in the five-gene analysis of Forrest and Crandall-Stotler (in press)
. The implication from these results is that the relatively simple morphology of both generations in Spharocarpales may not be plesiomorphic but rather the product of extreme simplification in ephemeral or aquatic habitats.
Air chambers are found in the crown group taxa (Marchantia, Preissia, Targionia, Riccia) (Wheeler, 2000
). One lineage, Monoclea plus Dumortiera, has secondarily reverted to a morphologically simple thallus devoid of chambers, perhaps adaptations to the semi-aquatic habit of these plants (Wheeler, 2000
). The production of archegoniophores (carpocephala) that elevate sporophytes above the gametophyte also evolved within the crown Marchantiopsida group. Independent losses of these structures occurred in riccioid taxa (Riccia, Ricciocarpos, Oxymitra) and Monoclea (Wheeler, 2000
). Reduction in sporophyte complexity is likewise a derived feature of riccioid liverworts (Renzaglia et al., 2000
; Boisselier-Dubayle et al., 2002
). With a jungermannioid-like sporophyte elevated on a fragile and highly elongated seta, Monoclea seems inappropriately placed within this crown group. Additional characters of the genus, including a free nuclear embryo and monoplastidic meiosis in some species (Schofield, 1985
; Renzaglia et al., 1994
), support a more traditional placement of Monoclea in Marchantiopsida. However, congruence among the multigene analyses provided support for Monoclea close to Dumortiera.
Systematics and phylogeny of Metzgeriidae (simple thalloid liverworts)
Clearly not a monophyletic group, Mezgeriidae traditionally include some 30 highly diverse genera of "leafy" and thalloid forms. Although four apical cell types are found in the group (Fig. 10), a unifying feature of apical growth in these plants is development of wings and leaves from a central wedge cell (single initial) that forms in the newly produced apical derivative (Fig. 11A) (Renzaglia, 1982
). Simple thalloid genera are distinguished from leafy liverworts (Jungermanniidae) in that they are anacrogynous: archegonia are produced along the mid-thallus of either the main, lateral, or ventral shoots. Consequently, the apical cell is not transformed into permanent tissue after archegonial development, and sporophytes do not terminate the shoot as in acrogynous Jungermanniidae. Additional features that unify the simple thalloid taxa, but are also found in leafy liverworts, are the development of antheridia from two primary androgones, oil bodies in all cells, lobed sporocytes, smooth rhizoids, and five rows of neck cells per archegonium.
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The apparent affinity between suborder Metzgeriinae (simple thalloid II) and Jungermanniidae ("true" leafy liverworts) in the multigene analyses of both Davis (Fig. 8) and Forrest and Crandall-Stotler (in press)
was unexpected. Members of Metzgeriinae epitomize the simple thalloid condition, with fleshy (Aneuraceae) and midrib-plus-wing (Metzgeriaceae) organizations. All of these thalli develop from a lens-shaped apical cell (Fig. 10C), and no "leafy" forms exist (except perhaps Pleurozia, discussed next). Endogenous branches in Metzgeriaceae are reminiscent of those in leafy liverworts (Renzaglia, 1982
).
One of the most surprising results from the Davis (in press)
analyses was the placement of Pleurozia in Metzgeriinae (simple thalloid II) rather than among the "true" leafy liverworts (Figs. 7, 8). Pleurozia is composed of about 11 species distributed primarily in the tropics. Leaves are complicate-bilobed, and for that reason, Pleurozia has traditionally been included in or near Porellales within the leafy liverworts (Schuster, 1984
; Crandall-Stotler and Stotler, 2000
). However, leaf morphology in Pleurozia is unique in that the leaf lobule is dorsal in orientation, not ventral (Thiers, 1993
), and the plants grow from a lenticular apical cell (Crandall-Stotler, 1976
) rather than a tetrahedral cell as in all "true" leafy liverworts. The placement of Pleurozia in the metzgerioid liverworts indicates that the "leafy" gametophytes of Pleurozia, with their complicatebilobed leaves, may have evolved convergently in a group otherwise characterized by thalloid gametophytes. In contrast to the single leaf initial in simple thalloids that have "leafy" gametophytes (Fig. 11A), leaves of Pleurozia develop from two initial cells, as is typical of leafy liverworts (Fig. 11B; Crandall-Stotler, 1976
). The phylogenetic position of Pleurozia should be further investigated, although its placement within subclass Metzgeriidae is strongly supported by both the 12- and four-locus analyses of Davis (in press)
.
Systematics and phylogeny of the Jungermanniidae (leafy liverworts)
The leafy liverworts, with some 40006000 species, are by far the largest of the liverwort groups. They occur in most terrestrial and aquatic habitats but are especially diverse in high-moisture environments. Many species are epiphytic on bark, and in the tropics, epiphyllous liverworts may cover the leaves of angiosperm trees and shrubs in shaded, high-humidity forests. More than 75% of the liverworts of tropical lowland forests and almost all the epiphylls belong to Lejeuneaceae (Gradstein, 1994
, 1997
). Lejeuneaceae comprise approximately 93 of the 307 genera (30%) of leafy liverworts, and well over 1000 species (Gradstein, 1979
, 1994
, 1997
; Crandall-Stotler and Stotler, 2000
). In lowland equatorial forests, as many as 20 species of Lejeuneaceae may co-occur on a single leaf (Zartman, 2003
). These organisms are important components of tropical forest diversity, and the diversity of epiphylls (almost exclusively Lejeuneaceae) is a sensitive indicator of habitat change associated with forest fragmentation (Zartman, 2003
).
Jungermanniidae are distinguished from Metzgeriidae in having tetrahedral apical cells, gametophytic shoots with (usually) well-differentiated stems and leaves, leaves formed from two initial cells, acrogynous perichaetia (terminating the main stem or branch), bracts and perianths (modified, fused leaves) associated with the perichaetium, and capsules that regularly dehisce into four valves (Crandall-Stotler and Stotler, 2000
). The perianths of leafy liverworts are diverse and provide important taxonomic characters in many genera and families.
Leaves of leafy liverworts may be entire or more often have two large lobes or teeth. They are most commonly differentiated as two rows of lateral leaves and a single row of ventral underleaves (amphigastria; Fig. 9C). Underleaves are frequently small or lacking. Insertion of the lateral leaves may be transverse, or, more commonly, they are oblique and the plants are more or less flattened because the leaves overlap. In plants with incubous leaf orientation, the forward leaf margin overlaps the trailing margin of the next younger leaf, resembling the arrangement of roof shingles (Fig. 9C). In sucubous orientation, forward margins of older leaves are covered by overlapping trailing margins of the younger leaves. In species with complicatebilobed leaves, lateral leaves are each folded to form ventral and dorsal lobes. The dorsal lobe is larger in most taxa, and the ventral lobe may be highly modified into the form of a pouch or helmet-shaped lobule that holds water.
Schuster (1966
, 1984
) assumed that the most primitive liverworts would be the most mosslike, with leafy, radially symmetric gametophytes and therefore placed leafy taxa at the base of his subjectively derived "phylogenetic trees" (e.g., Schuster, 1966
, pp. 406, 696). He considered leafy taxa with radial symmetry and three rows of transversely (or nearly so) inserted leaves (e.g., Herbertineae) to be early diverging groups, and from these he showed the branching of lineages or clusters of lineages with increased anisophylly and more obliquely inserted leaves (Schuster, 1966
, 1972
, 1984
). One group includes Schistochilaceae, Cephaloziaceae, Lepidoziaceae, and Pleuroziaceae, whereas the other progresses through Ptidiaceae to Jungermanniaceae, Frullaniaceae and Lejeuneaceae. (His diagram shows extant families ancestral to other families.) The classification of Crandall-Stotler and Stotler (2000)
has a sequence of families in five orders, Lepicoleales (including Ptilidiaceae, Lepicoleaceae, Schistochilaceae, and Lepidolaenaceae), Jungermanniales (including Herbertaceae, Balantiopsidaceae, Geocalycaceae, Lepidoziaceae, Cephaloziaceae, Jungermanniaceae, and Gymnomitriaceae), Porellales (including Porellaceae, Jubulaceae, and Lejeuneaceae), and the monotypic Radulales and Pleuroziales. Their classification implies similar concepts of evolution in leafy liverworts to those of Schuster.
In a liverwort backbone tree based on 12 loci, Davis (in press)
resolved two major clades within subclass Jungermanniidae (Fig. 7). One clade contains most of the taxa with complicatebilobed, incubous (or transverse) leaves (mainly Porellaceae, Jubulaceae, Radulaceae, and Lejeuneaceae), whereas the other contains the remaining families of leafy liverworts. In a more taxon-extensive analysis that included 81 liverworts, two mosses, and a hornwort, based on sequences from 26S nrDNA, two plastid loci ( psbA and rps4), and mitochondrial nad5, the same two leafy liverwort clades were resolved (Fig. 8). The noncomplicate-bilobed group consists of three subclades for which sister group relationships are ambiguous (A, B, and C in Fig. 8). Species in clade A have incubous or transverse leaf insertion, well-developed underleaves, and multilobed lateral leaves (Davis, in press
). Herbertus, assumed by Schuster (1984)
to be primitive among leafy liverworts, is resolved in a derived position within clade A (Fig. 8). Moreover, other isophyllous taxa (e.g., Anthelia, Triandrophyllum) are also resolved in relatively derived phylogenetic positions. Taxa in clade B have sucubous or transverse leaves and generally lack underleaves; however, lateral leaf shape is variable. Leaf shape, insertion, and underleaf development are highly variable in clade C, but many of the species are characterized by having perichaetia formed in fleshy perigynia or marsupia, which do not occur elsewhere in the leafy liverworts.
Among suborders of leafy liverworts recognized by Schuster (1984)
, only Radulineae and Balantiopsidineae are monophyletic based on the four-locus analysis of Davis (in press)
. The classification of Crandall-Stotler and Stotler (2000)
is also in conflict with many of the phylogenetic inferences from Davis's analysis (Fig. 8). Notably, Lepicoleales are extensively polyphyletic, and Radulales are nested within Porellales. Herbertaceae, Lepidoziaceae, Balantiopsidaceae, Cephaloziaceae, Porellaceae, and Radulaceae are supported as monophyletic. Lejeuniaceae are monophyletic only if Bryopteris is included within them (Bryopteridaceae, fide Crandall-Stotler and Stotler, 2000
). Jungermanniaceae, Gymnomitriaceae, Geocalycaceae, Cephaloziaceae, Lepidolaenaceae are paraphyletic (Davis, in press
).
Inferences about morphological evolution in liverworts from molecular analyses
Leaves or leaflike lobes have evolved in every major group of hepatics. Haplomitrium and Treubia have leafy appendages. Blasia and Sphaerocarpos, taxa within the marchantioid line, have leafy habits. Phyllothallia, Noteroclada, and Pleurozia, with leafy gametophytes, are scattered among simple thalloid taxa. The leaves of these plants are typically succubous to transversely inserted and may be formed from any one of three apical cell types: wedge-shaped, lenticular, or tetrahedral. In Phyllothallia and Noteroclada (Fig. 10A), each leaf develops from a single initial, whereas in Pleurozia there are two initials. A single initial is also responsible for development of wings and lateral thallus in all simple thalloids, complex thalloids, hornworts, and many pteridophyte gametophytes and is thus best viewed as plesiomorphic.
An autapomorphy of the Jungermanniidae is the production of bifid leaves from two leaf initials in a derivative from a tetrahedral apical cell (Fig. 10B). Once "locked" into this pattern of cell divisions, a number of variations on the "typical" bifid leaf of hepatics evolved, including complicatebilobed leaves. A narrower ventral cutting face in the apical cell is associated with a smaller size or absence of underleaves that originate from it. Incubous leaf insertion results from a ventral (downward) tilt of the apical cell (Crandall-Stotler and Stotler, 2000
), a feature that is often correlated with taxa that grow on vertical substrates such as tree bark (e.g., Leujeuniaceae). Conversely, succubous leaf arrangements are correlated with a dorsal (upward) tilt of the growing tip.
Few conclusions can be drawn at present about the evolution of apical cell shapes and growth forms in liverworts. Transformation from one apical cell type to another readily occurs during development, and this plasticity may have provided fuel for evolutionary change (Renzaglia et al., 2000
). Depending on the position of Haplomitrium in the trees, either a tetrahedral or wedge-shaped cell is plesiomorphic. Similarly, either an upright "leafy" habit or a flattened thallus is ancestral in hepatics; both hypotheses have garnered support (Schuster, 1992
; Mishler and Churchill, 1984
). Outgroup comparisons provide no further resolution of this issue as hornwort and pteridophyte gametophytes are thalloid with wedge-shaped apical cells, whereas mosses are leafy with tetrahedral cells.
Within liverworts, significant evolutionary changes can be inferred at the cellular level based on the consensus topology of recent molecular analyses. Monoplastidic meiosis occurs in all mosses and hornworts. However, it is restricted in liverworts to Haplomitrium, Blasia, and Monoclea (Renzaglia et al., 1994
) and is best interpreted as plesiomorphic. Monoplastidic meiosis involves precise control of plastid division and migration prior to chromosomal separation (Brown and Lemmon, 1990
). Polyplastidic meiosis predominates in liverworts and is a derived state. Similarly, lobed spore mother cells that occur in liverworts such as Haplomitrium, Treubia, and Blasia are shared with other bryophytes and represent a plesiomorphic condition (Brown and Lemmon, 1988
). Sporocyte lobing was lost within Marchantiopsida, whereas spores united in permanent tetrads are viewed as derived within Sphaerocarpales. Among bryophytes, pre-meiotic patterning of spore wall ornamentation occurs in Apotreubia and Haplomitrium and presumably has been lost in more derived liverwort lineages (Brown et al., 1986
). Further ultrastructural studies across a range of hepatic groups are likely to provide new insights into the nature and direction of changes in cellular processes during early land plant evolution.
| BRYOPHYTA |
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Philibert (18841902)
published a series of seminal papers describing variation in the structure of the moss peristome (sporophytic) and distinguished several basic types characterizing large groups of taxa. Fleischer (1923)
developed a radically new classification of moss diversity based on Philibert's peristome observations for his flora of Java and adjacent regions, and variations on this classification were utilized through almost all of the 20th century. The most influential classification utilizing Philibert's observations and Fleischer's taxonomic concepts was Brotherus' (19241925)
worldwide synopsis of mosses for Engler and Prantl's Die natürlichen Pflanzenfamilien. With minor modifications, the Brotherus system formed the basis for moss classification (e.g., Vitt, 1984
) until the last five years, during which insights from molecular analyses have accumulated (Buck and Goffinet, 2000
) (Fig. 12).
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Two basic types of peristome, nematodontous and arthrodontous, are distinguished by whether the teeth are formed from whole dead cells or just remnants of cell walls, respectively. Nematodontous peristomes are heterogeneous in both development and mature structure. The so-called Polytrichum type (Shaw and Robinson, 1984
) consists of 32 or 64 teeth united at their tips by a membranous epiphragm (Fig. 13A E). The teeth are formed from whole cells derived from the innermost four to eight layers of the amphithecium. (Endothecium and amphithecium are embryonic tissues that differentiate early in the ontogeny of bryophyte capsules.). Polytrichum-type peristomes are uniquely characterized by a series of early anticlinal divisions in the amphithecium, and, because peristome development involves remarkably regular alternating anticlinal and periclinal divisions, the amphithecium ends up having double the number of cells compared to arthrodontous and other nematodontous types (Fig. 13B). The Polytrichum-type peristome is further characterized by complex patterns of cell deformation during development (Fig. 13C). The other form of nematodontous peristome, the Tetraphis-type, is simpler in development, including the absence of the additional anticlinal divisions found in the Polytrichum-type (Shaw and Anderson, 1988
), and consists at maturity of four massive teeth derived from the entire amphithecium (Fig. 13D).
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Diplolepideous peristomes may have endostome segments that lie opposite the exostome teeth (the Funaria- or diplolepideous-opposite type; Fig. 13K) or alternate with them (Bryum or diplolepideous-alternate type; Fig. 13F). Endostomes in the Funaria-type consist of relatively massive teeth (reduced or absent in some taxa) without a basal membrane. The endostomes in (well-developed) Bryum-types are more membranous and consist of a basal membrane and 16-keeled segments. Narrow cilia may occur between the endostome segments. Vitt (1981)
argued that peristomes found in Orthotrichaceae constitute another basic type, but this interpretation was not supported by morphological studies of Shaw (1986)
or Goffinet et al. (1999)
.
Peristomes characterizing Buxbaumiaceae and Diphysiaceae have been interpreted as intermediate between nematodontous and arthrodontous types (Edwards, 1979
, 1984
; Vitt, 1984
). In Buxbaumia, outer teeth are derived from whole cells, whereas inner teeth are arthrodontous (Fig. 13E). More than three amphithecial layers contribute to peristomes, as in nematodontous types. The Diphyscium peristome is entirely arthrodontous but is a pleated cone unlike any other arthodontous peristome (Fig. 13H).
Peristomial formulae describe the numbers of cells in the three peristomial layers as revealed by patterns of vertical and horizontal lines visible on mature peristome teeth. These lines represent remnants of anticlinal walls from cells in peristomial layers and thus, numbers of cells in the layers. Formulae specify numbers of cells in the IPL, PPL, and OPL in 1/8 of the capsule's circumference (Edwards, 1984
). Haplolepideous peristomes are characterized by a 4 : 2 : 3 (OPL : PPL : IPL) formula (rarely 4 : 2 : 1), and diplolepideous peristomes by formulae of 4 : 2 : 412 (Edwards, 1984
; Shaw and Rohrer, 1984
). Another significant feature distinguishing peristome types is whether anticlinal walls in IPL are laterally offset with regard to anticlinal walls in PPL (Fig. 13G, J). Offset walls characterize haplolepideous and diplolepideous-alternate peristomes but not the diplolepideous-opposite (Funaria-) type. Anticlinal walls in the Polytrichum-type nematodontous peristomes are not offset (Wenderoth, 1931
), and there is little if any offsetting of the walls in Tetraphis-type nematodontous peristomes (Shaw and Anderson, 1988
). The peristome of Diphyscium has a developmental pattern that conforms in all details to the haplolepideous peristomial type and has a 4 : 2 : 3 formula at maturity despite the unique structure of the mature peristome (Shaw et al., 1987
).
Developmental studies have succeeded (even if based on few taxa) in defining when and how the basic peristome types differ from one another. These studies do not, however, claritfy phylogenetic relationships among the types. One of the central goals of higher-level phylogenetic analyses for mosses has been to resolve these relationships. Much progress has been made, but a full resolution is still forthcoming.
The backbone of moss phylogenetic relationships
Various approaches to resolving relationships among mosses have included taxon-extensive analyses using a single plastid gene (rps4: Goffinet et al., 2001
; rbcL: Tsubota et al., 2002
), and analyses of multigene, multigenomic data sets with more synoptic taxon sampling (Cox et al., 2004
). Both approaches have their merits, but it is clear that resolution of well-supported relationships among the major groups of mosses will not be accomplished using one or a few genes, even if such analyses succeed in placing more genera into monophyletic groups. The best-supported "backbone" for mosses was derived from an analysis of eight genes representing the mitochondrial, plastid, and nuclear genomes of 30 exemplars that represent major lineages based on previous studies (Cox et al., 2004
). The following synopsis is based on that analysis, with discussion of supportive and/or contradictory evidence when appropriate.
With sequences from four species of liverworts as the outgroup, the Bayesian reconstruction presented by Cox et al. (2004)
indicated that Sphagnum and Takakia form a clade sister to all remaining mosses (Fig. 12). A close relationship between Sphagnum and Takakia was also resolved by Hedderson et al. (1998)
, Newton et al. (2000)
, and Yatsentyuk (2001)
from nucleotide sequences, although Newton et al. (2000)
were not able to identify any morphological synapomorphies uniting the two genera. Gametophytes of Sphagnum and Takakia could not be more divergent: those of Takakia are tiny, simple in structure, and reminiscent of liverworts, whereas those of Sphagnum are large and characterized by a number of autapomorphies. The sporophyte of Takakia is mosslike in development (Renzaglia et al., 1997
) with a well-developed seta, a cylindrical capsule, and spiraled dehiscence (Fig. 14), whereas capsules of Sphagnum are ovoid in shape, open by an apical operculum, and are elevated on gametophytic pseudopodia. In the analyses of Cox et al. (2004)
, support for the clade containing Sphagnum and Takakia was lower when substitution patterns were modeled separately for each of the eight genomic regions than when a single model was applied, thus raising the possibility that resolution of the Sphagnum-Takakia clade may be an artifact. Phylogenetic relationships among species within Sphagnopsida (Sphagnum and Ambuchanania) have been described by Shaw (2000)
and Shaw et al. (2003a)
.
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One of the most exciting insights from phylogenetic analyses of mosses is that the monospecific genus, Oedopodium, appears to be sister to all remaining peristomate taxa (Fig. 15). A critical position for Oedopodium corroborates the results of Newton et al. (2000)
from combined analyses of morphology and four plastid DNA regions and of Goffinet et al. (2001)
based on a taxon-extensive analysis of plastid rps4 sequences. Goffinet et al. (2001)
resolved Oedopodium as sister to a clade containing Tetraphidaceae and Polytrichaceae at or near the base of peristomate mosses, but relationships were not fully resolved and without bootstrap support. Newton et al. (2000)
and Magombo (2003)
, based on four plastid DNA regions, resolved Oedopodium, both with moderate to strong bootstrap support, as sister to all peristomate mosses.
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Mosses characterized by nematodontous peristomes form a grade paraphyletic to the arthrodontous taxa (Fig. 12). Polytrichales form a monophyletic group sister to the rest of the peristomate mosses; Tetraphis (representing the small family, Tetraphidaceae) is next diverging, then Buxbaumia, and Diphyscium. Monophylly of Polytrichales based on the eight-gene data set corroborated earlier results of Hyvönen et al. (1998)
, Newton et al. (2000)
, and Magombo (2003)
. Tetraphidaceae, characterized by four massive, nematodontous peristome teeth, are not part of the monophyletic Polytrichaceae. This result makes sense in terms of peristome structure and development; Tetraphis does not have the "extra" anticlinal division that characterizes the amphithecial layers of Polytrichaceae (Shaw and Anderson, 1988
) nor the complex pattern of cell malformation that occurs during peristome development in Polytrichaceae. Aside from their nematodontous structure, peristomes of Tetraphidaceae and Polytrichaceae have little in common.
Molecular phylogenetic analyses, as well as peristome structure and development, support the interpretation that Buxbaumia and Diphyscium are intermediate between nematodontous and arthodontous mosses. The two families are paraphyletic to the rest of the arthrodontous clade, forming a bridge from taxa with nematodontous peristomes (Fig. 12). Newton et al. (2000)
resolved Buxbaumia and Tetraphis as a monophyletic group between Polytrichaceae and Diphyscium, but their topology was otherwise similar in the intermediate placement of these taxa between nematodonts and arthrodonts. Goffinet et al. (2001)
resolved Buxbaumia in an unsupported clade with Tetraphidaceae and Oedopodium (in contrast to Fig. 12), but their analysis resolved Diphyscium as sister to arthrodontous taxa (as in Fig. 12). With more extensive taxon sampling within Diphysiaceae, Magombo (2003)
confirmed that the family is monophyletic and corroborated its phylogenetic position between Buxbaumiacae and arthrodontous mosses. A placement of Buxbaumia near the basal node of the Diphyscium-arthrodontous clade is supported by a shared deletion of approximately 200 nucleotides in the rps4 gene (Goffinet et al., 2001
; Cox et al., 2004
). The deletion is absent in nematodonts (Polytrichaceae, Tetraphidaceae) as well as in Oedipodium, Sphagnum, Takakia, Andreaea, and Andreaeobryum.
Relationships within arthrodontous mosses are less well established, and internal branches down the backbone of the arthrodonts in the eight-gene tree are notably short (Fig. 12). If these short branches reflect time rather than a shift in substitution rate, the shape of the tree indicates a rapid radiation of arthrodontous mosses. Arthrodontous taxa are resolved in two lineages. One includes the genus Timmia plus the Encalyptaceae and Funariaceae. Timmiaceae are a small family of Northern Hemisphere mosses with one genus and fewer than 10 species (Brassard, 1979
). The peristome of Timmia is unique, although unambiguously arthrodontous. It has typical diplolepideous exostome teeth, but the endostome consists of a membranous basal membrane from which approximately 64 cilia arise (Fig. 13L); normal endostome segments are not formed. There has been much speculation about homology of cilia in the Timmia endostome (Vitt, 1984
) but little consensus. In the eight-gene tree in Fig. 12, Timmia is sister to a clade containing Encalyptaceae and Funariaceae, which is consistent with the topology recovered from analyses of plastid and mitochondrial sequences (Beckert et al., 1999
, 2001
; Goffinet and Cox, 2000
; Magombo, 2003
). It is possible that sequences from the nuclear genome produce a different position for Timmia as sister to all arthrodontous mosses (Cox and Hedderson, 1999
; Newton et al., 2000
), but support for this potential conflict is weak at present.
Interpretations of peristome structure in Encalypta (Encalyptaceae) have been controversial. Vitt (1984)
suggested that the genus encompasses characteristics of nematodontous and arthrodontous peristomes, including species with diplolepideous-alternate and diplolepideous-opposite types (Vitt, 1984
). Developmental patterns in the sporophytes of and phylogenetic relationships among the peristomially diverse species of Encalypta have not been investigated but might offer insights into peristome evolution. Funariaceae are also diverse in peristome structure, ranging from well developed to absent. When present, however, they consistently have a Funaria-type diplolepideous-opposite morphology. The absence of peristomes in some Funariaceae is generally interpreted as secondary reduction, and phylogenetic analyses do not contradict this conclusion. Some Funariaceae, including the "model organism" Physcomitrella patens (Hedw.) Bruch & Schimp., have cleistocarpous capsules (i.e., no differentiated operculum or peristome).
The eight-gene tree in Fig. 12 indicates a sister-group relationship between taxa characterized by haplolepideous and diplolepideous-alternate peristomes but with weak bootstrap and/or Bayesian support. This is an important relationship in the context of understanding peristome evolution. As noted before, Newton et al. (2000)
found evidence of a close relationship between Encalyptaceae and haplolepideous taxa, but they nevertheless resolved the haplolepideous plus Encalyptaceae clade as sister to the diplolepideous-alternate mosses. Within the diplolepideous-alternate clade, acrocarpous taxa form a paraphyletic grade leading to pleurocarps (Fig. 12). Pleurocarpous mosses form a strongly supported monophyletic group derived from an acrocarpous grade in all analyses with sufficient sampling conducted to date (Buck et al., 2000
; De Luna et al., 2000
; Tsubota et al., 2002
).
Phylogenetic relationships within acrocarpous and cladocarpous mosses
Cox and Hedderson (1999)
reconstructed relationships among acrocarpous mosses with diplolepideous-alternate peristomes based on nuclear 26s rDNA and plastid rps4, and trnL-trnF sequences. Their study upset many long-established taxonomic concepts. In particular, they showed that the large family, Bryaceae, is phylogenetically heterogeneous. Leptobryum, always previously classified in Bryaceae, turned out to be in Meesiaceae, a conclusion corroborated by subsequent studies (Cox et al., 2000
; Goffinet and Cox, 2000
; Goffinet et al., 2001
). Orthodontium was removed from Bryaceae in favor of a placement among (largely unresolved) acrocarpous genera near the base of the pleurocarps. Most striking, however, was their finding that even the core bryaceous genera, Bryum, Brachymenium, Pohlia, Mielichhoferia, do not form a monophyletic group. Pohlia and related genera (e.g., Mielichhoferia, Mniobryum) are part of a clade including taxa traditionally classified in Mniaceae, leaving only Bryum and related genera to form a more restricted Bryaceae. Pohlia has relatively narrow, nonbordered leaves and long leaf cells; Bryum and relatives have broader, frequently bordered leaves and shorter hexagonal or rhombic leaf cells; and Mniaceae are characterized by broader still, sometimes elliptical leaves generally with a strong border and isodiametric cells. The unequivocal placement of Pohlia in Mniaceae could never have been predicted from morphological observations and showed clearly how misleading morphological patterns can be about phylogenetic relationships (notwithstanding many congruent patterns of relationship inferred from morphology and molecular data in the mosses). Moreover, phylogenetic insights gained from molecular analyses raise questions about the nature of large morphological transitions within monophyletic groups such as Mniaceae.
Cladocarpous taxa have archegonia borne on lateral branches, seemingly intermediate between acrocarpous and pleurocarpous architectures (La Farge-England, 1996
). Diverse groups of cladocarps include Hedwigiaceae, Orthotrichaceae, and Rhizogoniaceae. Placement of Orthotrichaceae is also important in the context of interpreting basic peristome types in mosses (discussed earlier). Unfortunately, relationships of Orthotrichaceae are still unresolved, although all studies to date have indicated that the family is nested within groups characterized by diplolepideous-alternate peristomes (Goffinet et al., 2001
), possibly among a group of relatively derived acrocarps from which pleurocarps evolved (Cox and Hedderson, 1999
; Cox et al., 2000
; Tsubota et al., 2002
). Goffinet et al. (2001)
and Cox et al. (2004)
resolved Orthotrichacae as sister to Splachnaceae (the dung mosses). This result has significant support (i.e., >95% posterior probability) in the analyses of Cox et al. (2004)
.
The traditional family Rhizogoniaceae (e.g., Brotherus, 1924
) are consistently resolved as nonmonophyletic by molecular data (Goffinet et al., 2001
). Members of Rhizogoniaeae, however, along with the genera Orthodontium (traditionally placed in Bryaceae; Brotherus, 1924
; Vitt, 1984
) and Aulacomnium, appear to be close to the ancestral acrocarps from which pleurocarpous mosses originated (Cox et al., 2000
; De Luna et al., 2000
; Goffinet et al., 2001
; Tsubota et al., 2002
). These taxa are critical to questions about the origins of pleurocarpy, and progress is being made resolving relationships among taxa traditionally classified in Rhizogoniaceae (A. Newton, British Museum, Natural History, personal communication).
Phylogenetic relationships among pleurocarpous mosses
The pleurocarpous mosses include some 5000 species, approximately 50% of all mosses. Pleurocarps are diverse in tropical forests, although they are also well represented in Northern and Southern Hemisphere temperate regions. It is well established that the pleurocarps are monophyletic and evolved from acrocarpous ancestors (De Luna et al., 2000
; Newton et al., 2000
; Goffinet et al., 2001
; Cox et al., 2004
).
Pleurocarpous mosses have traditionally been classified in three orders: Hookeriales, Hypnales, and Leucodontales. There is now little question that Leucodontales, defined primarily on the basis of reduced peristomes (Brotherus, 19241925
; Vitt, 1984
; Buck, 1991
), are nonmonophyletic (Buck et al., 2000
; De Luna et al., 2000
; Tsubota et al., 2002
). Relationships within Hypnales have been recalcitrant to phylogenetic resolution because of short branch lengths at the base of the hypnalean clade (Buck et al., 2000
). Shaw et al. (2003a)
provided molecular evidence that Hypnales underwent a rapid radiation early in their history. Consequently, resolution of family relationships within Hypnales is likely to require a tremendous amounts of nucleotide sequence data and/or comparative information about genome structure. Although relationships among hypnalean families are largely unresolved at present, some apparently monophyletic groups have been identified and generic relationships within them investigated (Chiang and Schaal, 2000
; Quandt et al., 2000
; Tsubota et al., 2001a
, b
; Blöcher and Capesius, 2002
; Pedersen and Hedenäs, 2002
; Stech et al., 2002
; Vanderpoorten et al., 2002a
, b
). A difficult but critical issue confronting phylogenetic analyses of generic relationships within families of hypnalean pleurocarps has been the identification of well-supported monophyletic groups appropriate for detailed investigations.
Buck et al. (in press)
resolved ordinal relationships in the pleurocarps based on four genes (nuclear 26S rDNA, plastid rps4, trnL-trnF, and mitochondrial nad4). They found (with strong support) that a clade including traditional Garovagliaceae and Ptychomniaceae is sister to Hookeriales plus Hypnales. These orders are also supported as monophyletic. On this basis, Buck et al. (in press)
reclassified the pleurocarps in two superorders, the Pychomnianae and Hypnanae. Ptychomnianae include the single order, Ptychomniales (with one family: Ptychomniaceae), whereas Hypnanae encompass Hookeriales and Hypnales. They also resolved familial and generic relationships within the Hookeriales, recognizing seven families, and reconstructed the evolution of morphological characters on the basis of their results. Obtaining phylogenetic resolution within Hookeriales proved less problematic than in Hypnales because Hookeriales do not appear to have undergone the sort of rapid radiation that characterizes Hypnales (Shaw et al., 2003b
). Branch lengths along Hookerialean backbone are substantially longer than in Hypnales.
Inferences about morphological evolution in mosses from molecular phylogenies
Cox et al. (2004)
conservatively stated the morphological implications of their phylogenetic results for the mosses. These inferences are briefly summarized here.
Taxa near the base of the moss tree have the capsule elevated on a gametophytic pseudopodium rather than on a sporophytic seta (i.e., Sphagnum and Andreaea), but the ancestral condition in mosses is ambiguous because Takakia and Andreaeobryum have a seta. Cox et al. (2004)
concluded that the pseudopodium evolved independently in Sphagnum and Andreaea. Because stomata are absent in Takakia, Andreaea, and Andreaeobryum and those of Sphagnum are nonfunctional, Cox et al. also concluded that stomata-like structures in Sphagnum may not be homologous with stomata of more derived mosses or to those of tracheophytes and hornworts. Their presence in some hornworts indicates, to the contrary, that stomata may be homologous in mosses and hornworts, which implies multiple losses in mosses. Alternatively, stomata could have been lost once in the early evolution of mosses and regained in class Bryopsida.
The acrocarpous habit is clearly pleisiotypic in peristomate mosses, but acrocarps are a paraphyletic group within which pleurocarps are nested. Although resolution among cladocarpous taxa is poor, it appears that cladocarpy evolved several times. It may be that hypnalean pleurocarps evolved from a cladocarpous ancestor, but additional resolution among acrocarps near the origin of pleurocarps is needed.
Absence of a peristome in Oedopodium makes the phylogenetic node at which peristomes originated ambiguous, and it is not clear whether nematodontous peristomes of the Polytrichum-type evolved independently of arthrodontous peristomes. The unique anticlinal divisions in the IPL of Polytrichaceae, leading to twice the "normal" number of cells in this layer, may be an apomorphy for that clade. These divisions appear to be characteristic not only of Polytrichum, but also Atrichum and Pogonatum, also in Polytrichaceae (Shaw, L. Anderson, Duke University, and B. Mishler, University of California, Berkeley, unpublished data). These divisions do not occur in the developing sporophyte of Sphagnum or Andreaea (Shaw, unpublished data). Phylogenetic considerations lend support to the hypothesis of Vitt (1984)
that the Funaria-type arthrodontous peristome with opposite exostome and endostome teeth is primitive in arthrodonts. Cox et al. (2004)
noted that although Timmia lacks endostome segments, the most parsimonious interpretation of its endostome (which consists of a basal membrane and cilia), given its phylogenetic position, is that it conforms to the opposite type. Developmental studies of peristomial layers in Timmia are sorely needed. Of critical importance is whether or not anticlinal walls in the PPL and IPL are offset.
The teeth of haplolepideous peristomes develop in positions that would be opposite exostome teeth were the latter formed (clearly shown in Vitt, 1981
). Thus, in terms of development, the single row of teeth in haplolepideous peristomes are homologous with the opposite endostome segments of the Funaria-type. Like Funaria-type endostomes, haplolepideous peristomes also lack a basal membrane and are relatively massive. Groups characterized by haplolepideous and diplolepideous-alternate peristomes appear to be sister groups, implying that asymmetric anticlinal cell divisions in the IPL during peristome development may be a synapomorphy for that clade. Diplolepideous-alternate peristomes have additional anticlinal IPL walls that become offset during development relative to those in the PPL. This pattern is likely a synapomorphy for the clade characterized by such peristomes.
| CONSPECTUS |
|---|
|
|
|---|
The molecular hypothesis presented here on hornworts (Fig. 1) is a critical first step toward a modern phylogenetic understanding for the group. Comprehensive analyses using genes from all three genomes in combination with morphological data, with sampling from all 12 genera of hornworts, are required to verify the novel relationships described earlier. Systematic studies of hornworts have lagged so far behind those of other land plants that any molecular analysis must first begin with a clear delineation of morphological characteristics in the specimens/species that are examined. Worldwide collecting and basic taxonomic evaluations are essential. With their unique adaptations to land, including basal elongation of the sporophyte and internalization of vulnerable tissues, hornworts will continue to provide essential information about early land plant evolution.
A general understanding of liverwort relationships has emerged from recent molecular studies, and this has led to major reinterpretations of evolutionary changes in the group. For example, isophylly in leafy liverworts and conducting tissue in simple thalloid taxa are now clearly seen as derived, not ancestral. However, critical unanswered questions in liverwort phylogeny remain, and these include the position of Haplomitrium (and Treubia), the placement of Pleurozia among the simple thalloid vs. leafy clades, and the precise positions of Sphaerocarpos and Lunularia within the complex thalloid lineage. Relationships among simple thalloid taxa, especially Pellia, Phyllothallia, Calycularia, and Cavicularia (the last sister to Blasia, Renzaglia, 1982
) have not been resolved using multilocus studies to date and will require additional sequences and more taxon sampling. Most striking is the lack of representation of critical genera and families in any one study and the need for a concerted, collaborative effort to obtain and share specimens of poorly known taxa.
Still outstanding questions with regard to moss phylogeny include the relationship among Takakia, Sphagnum, and Andreaea (do they form a monophyletic group sister to all other mosses?), the origin and evolution of the major peristome types, and the nature of the acrocarpous ancestors of pleurocarpous taxa. Fundamental morphological data on Takakia, including embryology, sporophyte development, and apical growth are necessary to identify structural changes within mosses. Additional work on developmental anatomy of peristomes is also needed in conjunction with ongoing phylogenetic work. Development of peristomial cell layers in Oedipodium (which lacks a peristome) is critical, as is the development of the unique Timmia peristome. Resolution of family-level relationships in mosses, especially in closely related pleurocarps, will require expanded data sets based on not just one or two genes, nor even five, but probably 15 to 20. Availability of primers for such multilocus analyses are probably not far off, given the intensive genomic work currently underway on a wide diversity of land plants, including mosses.
Molecular technologies are improving at a rate that is unpredictable and incomprehensible; we speculate that within the next decade most of the phylogenetic questions raised in this review will be resolved. In addition to sequences from multiple genes, complete organellar genomes will soon be available for representatives of each major lineage within bryophytes. Structural features of genomes, including intron presence, and gene order and deletions, likewise will continue to provide informative phylogenetic evidence. Further understanding of the existence and expression of developmental genes, especially homeobox and MADS-box genes, in all three groups of bryophytes will provide clues to the evolution of structural complexity within these plants and evolutionary relationships to more complicated organ systems of tracheophytes. Comparative morphological/ultrastructural studies of living and fossil taxa are required to fill in the gaps in knowledge as well as to fully comprehend structural changes. In addition to perfecting data collection methodologies, the primary challenge that lies ahead is in developing methods of analyzing and combining the large and diverse data sets that are rapidly materializing. Only then will the intricate details of early land plant interrelationships be clearly illuminated.
| FOOTNOTES |
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