Cenozoic migration of a desert plant lineage across the North Atlantic.

Previous paleobotanical work concluded that Paleogene elements of the sclerophyllous subhumid vegetation of western Eurasia and western North America were endemic to these disjunct regions, suggesting that the southern areas of the Holarctic flora were isolated at that time. Consequently, molecular studies invoked either parallel adaptation to dry climates from related ancestors, or long-distance dispersal in explaining disjunctions between the two regions, dismissing the contemporaneous migration of dry-adapted lineages via land bridges as unlikely. We report Vauquelinia (Rosaceae), currently endemic to western North America, in Cenozoic strata of western Eurasia. Revision of North American fossils previously assigned to Vauquelinia confirmed a single fossil-species of Vauquelinia and one of its close relative Kageneckia. We established taxonomic relationships of fossil-taxa using diagnostic character combinations shared with modern species and constructed a time-calibrated phylogeny. The fossil record suggests that Vauquelinia, currently endemic to arid and subdesert environments, originated under seasonally arid climates in the Eocene of western North America and subsequently crossed the Paleogene North Atlantic land bridge (NALB) to Europe. This pattern is replicated by other sclerophyllous, dry-adapted and warmth-loving plants, suggesting that several of these taxa potentially crossed the North Atlantic via the NALB during Eocene times.

Viridiplantae Body Plans Viewed Through the Lens of the Fossil Record and Molecular Biology.

A review of the fossil record coupled with insights gained from molecular and developmental biology reveal a series of body plan transformations that gave rise to the first land plants. Across diverse algal clades, including the green algae and their descendants, the plant body plan underwent a unicellul ar $\to$ colonial $\to$ simple multicellular $\to \,\,$complex multicellular transformation series. The colonization of land involved increasing body size and associated cell specialization, including cells capable of hydraulic transport. The evolution of the life-cycle that characterizes all known land plant species involved a divergence in body plan phenotypes between the haploid and diploid generations, one adapted to facilitate sexual reproduction (a free-water dependent gametophyte), and another adapted to the dissemination of spores (a more water-independent sporophyte). The amplification of this phenotypic divergence, combined with indeterminate growth in body size, resulted in a desiccation-adapted branched sporophyte with a cuticularized epidermis, stomates, and vascular tissues. Throughout the evolution of the land plants, the body plans of the sporophyte generation involved "axiation," i.e., the acquisition of a cylindrical geometry and subsequent organographic specializations.

FRUITS AND SEEDS OF THE TERTIARY BRANDON LIGNITE. VII. SARGENTODOXA (SARGENTODOXACEAE).

Seeds of Sargentodoxa (Sargentodoxaceae), a deciduous vine presently restricted to southeastern Asia, are described from the Oligocene Brandon Lignite of Vermont. This is the first report of fossil Sargentodoxaceae. The Sargentodoxaceae are segregated from the Lardizabalaceae, a small family with an unusual modem distribution (six genera in East Asia, two genera in Chile). Given the close relationship of the two families, the discovery of Sargentodoxa in North America, along with one and possibly two other occurrences of Lardizabalaceae in the Northern Hemisphere, raises the possibility that the Lardizabalaceae achieved their present distribution by 1) spreading around the Northern Hemisphere in the early Tertiary as part of the "Boreotropical Flora," followed by 2) long-distance dispersal from north to south in the New World. Other factors argue against this interpretation.

General patterns of taxonomic and biomass partitioning in extant and fossil plant communities.

A central goal of evolutionary ecology is to identify the general features maintaining the diversity of species assemblages. Understanding the taxonomic and ecological characteristics of ecological communities provides a means to develop and test theories about the processes that regulate species coexistence and diversity. Here, using data from woody plant communities from different biogeographic regions, continents and geologic time periods, we show that the number of higher taxa is a general power-function of species richness that is significantly different from randomized assemblages. In general, we find that local communities are characterized by fewer higher taxa than would be expected by chance. The degree of taxonomic diversity is influenced by modes of dispersal and potential biotic interactions. Further, changes in local diversity are accompanied by regular changes in the partitioning of community biomass between taxa that are also described by a power function. Our results indicate that local and regional processes have consistently regulated community diversity and biomass partitioning for millions of years.