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- W3047008526 abstract "Abstract Genetic isolation due to geographic separation (vicariance) is the best understood cause of vertebrate speciation. Nevertheless, it has never been demonstrated in the fossil record across a wide range of taxa. Here, by reviewing in-depth the available data of the Late Palaeozoic (~ 350–250 million years ago), I reconstructed an early Pangaean junction-disjunction palaeogeographic model and showed that it coincides strongly with time-calibrated cladograms of the Late Palaeozoic synapsids (the primitive ancestors of modern mammals). The temporal development of the vicariant topology seems to fit closely with the emergence rhythm of the recovered synapsid taxa, suggesting vicariance due to Pangaean separation as the cause of early amniote evolution. The inferred vicariant topology also accounts for the observed pattern in the North American marine biostratigraphic units. Accordingly, the model demonstrates the link between the evolution of life on Earth and palaeogeographic evolution and strongly supports allopatric speciation through vicariance as the prominent mode of amniote evolution. Furthermore, correlations between state-of-the-art biochronostratigraphic charts and this palaeogeographic model suggest that the arido-eustasy model can explain the mid-Permian biotic extinction event and depositional cycles, such as the pre-Zechstein of the Central European Basin." @default.
- W3047008526 created "2020-08-10" @default.
- W3047008526 creator A5031306777 @default.
- W3047008526 date "2020-08-04" @default.
- W3047008526 modified "2023-09-25" @default.
- W3047008526 title "An early Pangaean vicariance model for synapsid evolution" @default.
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- W3047008526 doi "https://doi.org/10.1038/s41598-020-70117-8" @default.
- W3047008526 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/7403356" @default.
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- W3047008526 hasPublicationYear "2020" @default.
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