Biotic interchange between the Indian subcontinent and mainland Asia through time

Biotic interchange after the connection of previously independently evolving floras and faunas is thought to be one of the key factors that shaped global biodiversity as we see it today. However, it was not known how biotic interchange develops over longer time periods of several million years follo...

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Published in	Nature communications Vol. 7; no. 1; pp. 12132 - 6
Main Authors	Klaus, Sebastian, Morley, Robert J., Plath, Martin, Zhang, Ya-Ping, Li, Jia-Tang
Format	Journal Article
Language	English
Published	London Nature Publishing Group UK 04.07.2016 Nature Publishing Group Nature Portfolio
Subjects	704/158/670 704/158/852 704/2151/414 Asia Biota Dispersal Environmental conditions Eocene Fossils Geology Humanities and Social Sciences India multidisciplinary Phylogeny Science Science (multidisciplinary) Time Factors United Kingdom > UK Asia Indian subcontinent China India
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Abstract	Biotic interchange after the connection of previously independently evolving floras and faunas is thought to be one of the key factors that shaped global biodiversity as we see it today. However, it was not known how biotic interchange develops over longer time periods of several million years following the secondary contact of different biotas. Here we present a novel method to investigate the temporal dynamics of biotic interchange based on a phylogeographical meta-analysis by calculating the maximal number of observed dispersal events per million years given the temporal uncertainty of the underlying time-calibrated phylogenies. We show that biotic influx from mainland Asia onto the Indian subcontinent after Eocene continental collision was not a uniform process, but was subject to periods of acceleration, stagnancy and decrease. We discuss potential palaeoenvironmental causes for this fluctuation. The Paleogene continental collision between the Indian subcontinent and Asia initiated biotic interchange over a timescale of millions of years. Klaus et al . develop a phylogeographic method to estimate the dynamics of biotic interchange over these timescales, revealing periods of acceleration, stagnation and decline.
AbstractList	Biotic interchange after the connection of previously independently evolving floras and faunas is thought to be one of the key factors that shaped global biodiversity as we see it today. However, it was not known how biotic interchange develops over longer time periods of several million years following the secondary contact of different biotas. Here we present a novel method to investigate the temporal dynamics of biotic interchange based on a phylogeographical meta-analysis by calculating the maximal number of observed dispersal events per million years given the temporal uncertainty of the underlying time-calibrated phylogenies. We show that biotic influx from mainland Asia onto the Indian subcontinent after Eocene continental collision was not a uniform process, but was subject to periods of acceleration, stagnancy and decrease. We discuss potential palaeoenvironmental causes for this fluctuation. The Paleogene continental collision between the Indian subcontinent and Asia initiated biotic interchange over a timescale of millions of years. Klaus et al . develop a phylogeographic method to estimate the dynamics of biotic interchange over these timescales, revealing periods of acceleration, stagnation and decline. Biotic interchange after the connection of previously independently evolving floras and faunas is thought to be one of the key factors that shaped global biodiversity as we see it today. However, it was not known how biotic interchange develops over longer time periods of several million years following the secondary contact of different biotas. Here we present a novel method to investigate the temporal dynamics of biotic interchange based on a phylogeographical meta-analysis by calculating the maximal number of observed dispersal events per million years given the temporal uncertainty of the underlying time-calibrated phylogenies. We show that biotic influx from mainland Asia onto the Indian subcontinent after Eocene continental collision was not a uniform process, but was subject to periods of acceleration, stagnancy and decrease. We discuss potential palaeoenvironmental causes for this fluctuation. Biotic interchange after the connection of previously independently evolving floras and faunas is thought to be one of the key factors that shaped global biodiversity as we see it today. However, it was not known how biotic interchange develops over longer time periods of several million years following the secondary contact of different biotas. Here we present a novel method to investigate the temporal dynamics of biotic interchange based on a phylogeographical meta-analysis by calculating the maximal number of observed dispersal events per million years given the temporal uncertainty of the underlying time-calibrated phylogenies. We show that biotic influx from mainland Asia onto the Indian subcontinent after Eocene continental collision was not a uniform process, but was subject to periods of acceleration, stagnancy and decrease. We discuss potential palaeoenvironmental causes for this fluctuation.Biotic interchange after the connection of previously independently evolving floras and faunas is thought to be one of the key factors that shaped global biodiversity as we see it today. However, it was not known how biotic interchange develops over longer time periods of several million years following the secondary contact of different biotas. Here we present a novel method to investigate the temporal dynamics of biotic interchange based on a phylogeographical meta-analysis by calculating the maximal number of observed dispersal events per million years given the temporal uncertainty of the underlying time-calibrated phylogenies. We show that biotic influx from mainland Asia onto the Indian subcontinent after Eocene continental collision was not a uniform process, but was subject to periods of acceleration, stagnancy and decrease. We discuss potential palaeoenvironmental causes for this fluctuation. The Paleogene continental collision between the Indian subcontinent and Asia initiated biotic interchange over a timescale of millions of years. Klaus et al. develop a phylogeographic method to estimate the dynamics of biotic interchange over these timescales, revealing periods of acceleration, stagnation and decline.
ArticleNumber	12132
Author	Zhang, Ya-Ping Plath, Martin Morley, Robert J. Li, Jia-Tang Klaus, Sebastian
Author_xml	– sequence: 1 givenname: Sebastian surname: Klaus fullname: Klaus, Sebastian email: klaus@cib.ac.cn organization: Chengdu Institute of Biology, Chinese Academy of Sciences, Department of Ecology and Evolution, J. W. Goethe University – sequence: 2 givenname: Robert J. surname: Morley fullname: Morley, Robert J. organization: Palynova Ltd, Earth Sciences Department, Royal Holloway, University of London – sequence: 3 givenname: Martin surname: Plath fullname: Plath, Martin organization: College of Animal Science and Technology, Northwest A&F University – sequence: 4 givenname: Ya-Ping surname: Zhang fullname: Zhang, Ya-Ping organization: State Key Laboratory of Genetic Resources and Evolution, Kunming Institute of Zoology, Chinese Academy of Sciences – sequence: 5 givenname: Jia-Tang surname: Li fullname: Li, Jia-Tang email: lijt@cib.ac.cn organization: Chengdu Institute of Biology, Chinese Academy of Sciences
BackLink	https://www.ncbi.nlm.nih.gov/pubmed/27373955$$D View this record in MEDLINE/PubMed
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Copyright	The Author(s) 2016 Copyright Nature Publishing Group Jul 2016 Copyright © 2016, Nature Publishing Group, a division of Macmillan Publishers Limited. All Rights Reserved. 2016 Nature Publishing Group, a division of Macmillan Publishers Limited. All Rights Reserved.
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Snippet	Biotic interchange after the connection of previously independently evolving floras and faunas is thought to be one of the key factors that shaped global... The Paleogene continental collision between the Indian subcontinent and Asia initiated biotic interchange over a timescale of millions of years. Klaus et al....
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SubjectTerms	704/158/670 704/158/852 704/2151/414 Asia Biota Dispersal Environmental conditions Eocene Fossils Geology Humanities and Social Sciences India multidisciplinary Phylogeny Science Science (multidisciplinary) Time Factors
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Title	Biotic interchange between the Indian subcontinent and mainland Asia through time
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