Plant extinction excels plant speciation in the Anthropocene

Abstract Background In the past several millenniums, we have domesticated several crop species that are crucial for human civilization, which is a symbol of significant human influence on plant evolution. A pressing question to address is if plant diversity will increase or decrease in this warming...

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Published in:BMC Plant Biology
Main Authors: Gao, Jian-Guo, Liu, Hui, Wang, Ning, Yang, Jing, Zhang, Xiao-Ling
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2020
Subjects:
Online Access:http://dx.doi.org/10.1186/s12870-020-02646-3
https://link.springer.com/content/pdf/10.1186/s12870-020-02646-3.pdf
https://link.springer.com/article/10.1186/s12870-020-02646-3/fulltext.html
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spelling crspringernat:10.1186/s12870-020-02646-3 2023-05-15T15:11:33+02:00 Plant extinction excels plant speciation in the Anthropocene Gao, Jian-Guo Liu, Hui Wang, Ning Yang, Jing Zhang, Xiao-Ling 2020 http://dx.doi.org/10.1186/s12870-020-02646-3 https://link.springer.com/content/pdf/10.1186/s12870-020-02646-3.pdf https://link.springer.com/article/10.1186/s12870-020-02646-3/fulltext.html en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY BMC Plant Biology volume 20, issue 1 ISSN 1471-2229 Plant Science journal-article 2020 crspringernat https://doi.org/10.1186/s12870-020-02646-3 2022-01-04T16:02:53Z Abstract Background In the past several millenniums, we have domesticated several crop species that are crucial for human civilization, which is a symbol of significant human influence on plant evolution. A pressing question to address is if plant diversity will increase or decrease in this warming world since contradictory pieces of evidence exit of accelerating plant speciation and plant extinction in the Anthropocene. Results Comparison may be made of the Anthropocene with the past geological times characterised by a warming climate, e.g., the Palaeocene-Eocene Thermal Maximum (PETM) 55.8 million years ago (Mya)—a period of “crocodiles in the Arctic”, during which plants saw accelerated speciation through autopolyploid speciation. Three accelerators of plant speciation were reasonably identified in the Anthropocene, including cities, polar regions and botanical gardens where new plant species might be accelerating formed through autopolyploid speciation and hybridization. Conclusions However, this kind of positive effect of climate warming on new plant species formation would be thoroughly offset by direct and indirect intensive human exploitation and human disturbances that cause habitat loss, deforestation, land use change, climate change, and pollution, thus leading to higher extinction risk than speciation in the Anthropocene. At last, four research directions are proposed to deepen our understanding of how plant traits affect speciation and extinction, why we need to make good use of polar regions to study the mechanisms of dispersion and invasion, how to maximize the conservation of plant genetics, species, and diverse landscapes and ecosystems and a holistic perspective on plant speciation and extinction is needed to integrate spatiotemporally. Article in Journal/Newspaper Arctic Climate change Springer Nature (via Crossref) Arctic BMC Plant Biology 20 1
institution Open Polar
collection Springer Nature (via Crossref)
op_collection_id crspringernat
language English
topic Plant Science
spellingShingle Plant Science
Gao, Jian-Guo
Liu, Hui
Wang, Ning
Yang, Jing
Zhang, Xiao-Ling
Plant extinction excels plant speciation in the Anthropocene
topic_facet Plant Science
description Abstract Background In the past several millenniums, we have domesticated several crop species that are crucial for human civilization, which is a symbol of significant human influence on plant evolution. A pressing question to address is if plant diversity will increase or decrease in this warming world since contradictory pieces of evidence exit of accelerating plant speciation and plant extinction in the Anthropocene. Results Comparison may be made of the Anthropocene with the past geological times characterised by a warming climate, e.g., the Palaeocene-Eocene Thermal Maximum (PETM) 55.8 million years ago (Mya)—a period of “crocodiles in the Arctic”, during which plants saw accelerated speciation through autopolyploid speciation. Three accelerators of plant speciation were reasonably identified in the Anthropocene, including cities, polar regions and botanical gardens where new plant species might be accelerating formed through autopolyploid speciation and hybridization. Conclusions However, this kind of positive effect of climate warming on new plant species formation would be thoroughly offset by direct and indirect intensive human exploitation and human disturbances that cause habitat loss, deforestation, land use change, climate change, and pollution, thus leading to higher extinction risk than speciation in the Anthropocene. At last, four research directions are proposed to deepen our understanding of how plant traits affect speciation and extinction, why we need to make good use of polar regions to study the mechanisms of dispersion and invasion, how to maximize the conservation of plant genetics, species, and diverse landscapes and ecosystems and a holistic perspective on plant speciation and extinction is needed to integrate spatiotemporally.
format Article in Journal/Newspaper
author Gao, Jian-Guo
Liu, Hui
Wang, Ning
Yang, Jing
Zhang, Xiao-Ling
author_facet Gao, Jian-Guo
Liu, Hui
Wang, Ning
Yang, Jing
Zhang, Xiao-Ling
author_sort Gao, Jian-Guo
title Plant extinction excels plant speciation in the Anthropocene
title_short Plant extinction excels plant speciation in the Anthropocene
title_full Plant extinction excels plant speciation in the Anthropocene
title_fullStr Plant extinction excels plant speciation in the Anthropocene
title_full_unstemmed Plant extinction excels plant speciation in the Anthropocene
title_sort plant extinction excels plant speciation in the anthropocene
publisher Springer Science and Business Media LLC
publishDate 2020
url http://dx.doi.org/10.1186/s12870-020-02646-3
https://link.springer.com/content/pdf/10.1186/s12870-020-02646-3.pdf
https://link.springer.com/article/10.1186/s12870-020-02646-3/fulltext.html
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
genre_facet Arctic
Climate change
op_source BMC Plant Biology
volume 20, issue 1
ISSN 1471-2229
op_rights https://creativecommons.org/licenses/by/4.0
https://creativecommons.org/licenses/by/4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1186/s12870-020-02646-3
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