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Spatial dynamics of Chinese Muntjac related to past and future climate fluctuations

Climate fluctuations in the past and in the future are likely to result in population expansions, shifts, or the contraction of the ecological niche of many species, and potentially leading to the changes in their geographical distributions. Prediction of suitable habitats has been developed as a us...

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Autores principales: Sun, Zhonglou, Orozco-terWengel, Pablo, Chen, Guotao, Sun, Ruolei, Sun, Lu, Wang, Hui, Shi, Wenbo, Zhang, Baowei
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Oxford University Press 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8489110/
https://www.ncbi.nlm.nih.gov/pubmed/34616935
http://dx.doi.org/10.1093/cz/zoaa080
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author Sun, Zhonglou
Orozco-terWengel, Pablo
Chen, Guotao
Sun, Ruolei
Sun, Lu
Wang, Hui
Shi, Wenbo
Zhang, Baowei
author_facet Sun, Zhonglou
Orozco-terWengel, Pablo
Chen, Guotao
Sun, Ruolei
Sun, Lu
Wang, Hui
Shi, Wenbo
Zhang, Baowei
author_sort Sun, Zhonglou
collection PubMed
description Climate fluctuations in the past and in the future are likely to result in population expansions, shifts, or the contraction of the ecological niche of many species, and potentially leading to the changes in their geographical distributions. Prediction of suitable habitats has been developed as a useful tool for the assessment of habitat suitability and resource conservation to protect wildlife. Here, we model the ancestral demographic history of the extant modern Chinese Muntjac Muntiacus reevesi populations using approximate Bayesian computation (ABC) and used the maximum entropy model to simulate the past and predict the future spatial dynamics of the species under climate oscillations. Our results indicated that the suitable habitats for the M. reevesi shifted to the Southeast and contracted during the Last Glacial Maximum, whereas they covered a broader and more northern position in the Middle Holocene. The ABC analyses revealed that the modern M. reevesi populations diverged in the Middle Holocene coinciding with the significant contraction of the highly suitable habitat areas. Furthermore, our predictions suggest that the potentially suitable environment distribution for the species will expand under all future climate scenarios. These results indicated that the M. reevesi diverged in the recent time after the glacial period and simultaneously as its habitat’s expanded in the Middle Holocene. Furthermore, the past and future climate fluctuation triggered the change of Chinese muntjac spatial distribution, which has great influence on the Chinese muntjac’s population demographic history.
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spelling pubmed-84891102021-10-05 Spatial dynamics of Chinese Muntjac related to past and future climate fluctuations Sun, Zhonglou Orozco-terWengel, Pablo Chen, Guotao Sun, Ruolei Sun, Lu Wang, Hui Shi, Wenbo Zhang, Baowei Curr Zool Articles Climate fluctuations in the past and in the future are likely to result in population expansions, shifts, or the contraction of the ecological niche of many species, and potentially leading to the changes in their geographical distributions. Prediction of suitable habitats has been developed as a useful tool for the assessment of habitat suitability and resource conservation to protect wildlife. Here, we model the ancestral demographic history of the extant modern Chinese Muntjac Muntiacus reevesi populations using approximate Bayesian computation (ABC) and used the maximum entropy model to simulate the past and predict the future spatial dynamics of the species under climate oscillations. Our results indicated that the suitable habitats for the M. reevesi shifted to the Southeast and contracted during the Last Glacial Maximum, whereas they covered a broader and more northern position in the Middle Holocene. The ABC analyses revealed that the modern M. reevesi populations diverged in the Middle Holocene coinciding with the significant contraction of the highly suitable habitat areas. Furthermore, our predictions suggest that the potentially suitable environment distribution for the species will expand under all future climate scenarios. These results indicated that the M. reevesi diverged in the recent time after the glacial period and simultaneously as its habitat’s expanded in the Middle Holocene. Furthermore, the past and future climate fluctuation triggered the change of Chinese muntjac spatial distribution, which has great influence on the Chinese muntjac’s population demographic history. Oxford University Press 2021-01-12 /pmc/articles/PMC8489110/ /pubmed/34616935 http://dx.doi.org/10.1093/cz/zoaa080 Text en © The Author(s) (2021). Published by Oxford University Press on behalf of Editorial Office, Current Zoology. https://creativecommons.org/licenses/by-nc/4.0/This is an Open Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/by-nc/4.0/ (https://creativecommons.org/licenses/by-nc/4.0/) ), which permits non-commercial re-use, distribution, and reproduction in any medium, provided the original work is properly cited. For commercial re-use, please contact journals.permissions@oup.com
spellingShingle Articles
Sun, Zhonglou
Orozco-terWengel, Pablo
Chen, Guotao
Sun, Ruolei
Sun, Lu
Wang, Hui
Shi, Wenbo
Zhang, Baowei
Spatial dynamics of Chinese Muntjac related to past and future climate fluctuations
title Spatial dynamics of Chinese Muntjac related to past and future climate fluctuations
title_full Spatial dynamics of Chinese Muntjac related to past and future climate fluctuations
title_fullStr Spatial dynamics of Chinese Muntjac related to past and future climate fluctuations
title_full_unstemmed Spatial dynamics of Chinese Muntjac related to past and future climate fluctuations
title_short Spatial dynamics of Chinese Muntjac related to past and future climate fluctuations
title_sort spatial dynamics of chinese muntjac related to past and future climate fluctuations
topic Articles
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8489110/
https://www.ncbi.nlm.nih.gov/pubmed/34616935
http://dx.doi.org/10.1093/cz/zoaa080
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