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Open AccessJournal ArticleDOI

Southern Hemisphere Biogeography Inferred by Event-Based Models: Plant versus Animal Patterns

Isabel Sanmartín, +1 more
- 01 Apr 2004 - 
- Vol. 53, Iss: 2, pp 216-243
TLDR
The results confirm the hybrid origin of the South American biota: there has been surprisingly little biotic exchange between the northern tropical and the southern temperate regions of South America, especially for animals.
Abstract
The Southern Hemisphere has traditionally been considered as having a fundamentally vicariant history. The common trans-Pacific disjunctions are usually explained by the sequential breakup of the supercontinent Gondwana during the last 165 million years, causing successive division of an ancestral biota. However, recent biogeographic studies, based on molecular estimates and more accurate paleogeographic reconstructions, indicate that dispersal may have been more important than traditionally assumed. We examined the relative roles played by vicariance and dispersal in shaping Southern Hemisphere biotas by analyzing a large data set of 54 animal and 19 plant phylogenies, including marsupials, ratites, and southern beeches (1,393 terminals). Parsimony-based tree fitting in conjunction with permutation tests was used to examine to what extent Southern Hemisphere biogeographic patterns fit the breakup sequence of Gondwana and to identify concordant dispersal patterns. Consistent with other studies, the animal data are congruent with the geological sequence of Gondwana breakup: (Africa(New Zealand(southern South America, Australia))). Trans-Antarctic dispersal (Australia southern South America) is also significantly more frequent than any other dispersal event in animals, which may be explained by the long period of geological contact between Australia and South America via Antarctica. In contrast, the dominant pattern in plants, (southern South America(Australia, New Zealand)), is better explained by dispersal, particularly the prevalence of trans-Tasman dispersal between New Zealand and Australia. Our results also confirm the hybrid origin of the South American biota: there has been surprisingly little biotic exchange between the northern tropical and the southern temperate regions of South America, especially for animals.

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Global diversity and geography of soil fungi

Leho Tedersoo, +57 more
- 28 Nov 2014 - 
TL;DR: Diversity of most fungal groups peaked in tropical ecosystems, but ectomycorrhizal fungi and several fungal classes were most diverse in temperate or boreal ecosystems, and manyfungal groups exhibited distinct preferences for specific edaphic conditions (such as pH, calcium, or phosphorus).
Journal ArticleDOI

Systematic review of the frog family hylidae, with special reference to hylinae: phylogenetic analysis and taxonomic revision

TL;DR: The present analysis indicates that Hemiphractinae are not related to the other three hylid subfamilies and are therefore removed from the family and tentatively considered a subfamily of the paraphyletic Leptodactylidae.
Journal ArticleDOI

A likelihood framework for inferring the evolution of geographic range on phylogenetic trees

TL;DR: A likelihood framework for inferring the evolution of geographic range on phylogenies that models lineage dispersal and local extinction in a set of discrete areas as stochastic events in continuous time is described.
Journal ArticleDOI

Ectomycorrhizal lifestyle in fungi: global diversity, distribution, and evolution of phylogenetic lineages

TL;DR: In conclusion, EcM fungi are phylogenetically highly diverse, and molecular surveys particularly in tropical and south temperate habitats are likely to supplement to the present figures.
References
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Journal ArticleDOI

Biogeography and phylogeny of the New Zealand cicada genera (Hemiptera: Cicadidae) based on nuclear and mitochondrial DNA data

TL;DR: Determine the geographical and temporal origins of New Zealand cicadas by studying the distribution and behaviour of cicada fossils found in New Zealand.
Journal ArticleDOI

Phanerozoic Australia in the Changing Configuration of Proto-Pangea Through Gondwanaland and Pangea to the Present Dispersed Continents

TL;DR: This paleotectonic phase lacks preserved seafloor spreading so that continental palaeomagnetism, biota and geological facies are the only indicators and physical evidence provides a unique solution for continental reconstruction since 320 Ma.
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