Climate change, humans, and the extinction of the woolly mammoth.

Woolly mammoths inhabited Eurasia and North America from late Middle Pleistocene (300 ky BP [300,000 years before present]), surviving through different climatic cycles until they vanished in the Holocene (3.6 ky BP). The debate about why the Late Quaternary extinctions occurred has centred upon env...

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Autores principales: David Nogués-Bravo, Jesús Rodríguez, Joaquín Hortal, Persaram Batra, Miguel B Araújo
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Publicado: Public Library of Science (PLoS) 2008
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Acceso en línea:https://doaj.org/article/8628ce89d28c4e42af6ef07a8eab9d09
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spelling oai:doaj.org-article:8628ce89d28c4e42af6ef07a8eab9d092021-11-25T05:33:25ZClimate change, humans, and the extinction of the woolly mammoth.1544-91731545-788510.1371/journal.pbio.0060079https://doaj.org/article/8628ce89d28c4e42af6ef07a8eab9d092008-04-01T00:00:00Zhttps://www.ncbi.nlm.nih.gov/pmc/articles/pmid/18384234/?tool=EBIhttps://doaj.org/toc/1544-9173https://doaj.org/toc/1545-7885Woolly mammoths inhabited Eurasia and North America from late Middle Pleistocene (300 ky BP [300,000 years before present]), surviving through different climatic cycles until they vanished in the Holocene (3.6 ky BP). The debate about why the Late Quaternary extinctions occurred has centred upon environmental and human-induced effects, or a combination of both. However, testing these two hypotheses-climatic and anthropogenic-has been hampered by the difficulty of generating quantitative estimates of the relationship between the contraction of the mammoth's geographical range and each of the two hypotheses. We combined climate envelope models and a population model with explicit treatment of woolly mammoth-human interactions to measure the extent to which a combination of climate changes and increased human pressures might have led to the extinction of the species in Eurasia. Climate conditions for woolly mammoths were measured across different time periods: 126 ky BP, 42 ky BP, 30 ky BP, 21 ky BP, and 6 ky BP. We show that suitable climate conditions for the mammoth reduced drastically between the Late Pleistocene and the Holocene, and 90% of its geographical range disappeared between 42 ky BP and 6 ky BP, with the remaining suitable areas in the mid-Holocene being mainly restricted to Arctic Siberia, which is where the latest records of woolly mammoths in continental Asia have been found. Results of the population models also show that the collapse of the climatic niche of the mammoth caused a significant drop in their population size, making woolly mammoths more vulnerable to the increasing hunting pressure from human populations. The coincidence of the disappearance of climatically suitable areas for woolly mammoths and the increase in anthropogenic impacts in the Holocene, the coup de grâce, likely set the place and time for the extinction of the woolly mammoth.David Nogués-BravoJesús RodríguezJoaquín HortalPersaram BatraMiguel B AraújoPublic Library of Science (PLoS)articleBiology (General)QH301-705.5ENPLoS Biology, Vol 6, Iss 4, p e79 (2008)
institution DOAJ
collection DOAJ
language EN
topic Biology (General)
QH301-705.5
spellingShingle Biology (General)
QH301-705.5
David Nogués-Bravo
Jesús Rodríguez
Joaquín Hortal
Persaram Batra
Miguel B Araújo
Climate change, humans, and the extinction of the woolly mammoth.
description Woolly mammoths inhabited Eurasia and North America from late Middle Pleistocene (300 ky BP [300,000 years before present]), surviving through different climatic cycles until they vanished in the Holocene (3.6 ky BP). The debate about why the Late Quaternary extinctions occurred has centred upon environmental and human-induced effects, or a combination of both. However, testing these two hypotheses-climatic and anthropogenic-has been hampered by the difficulty of generating quantitative estimates of the relationship between the contraction of the mammoth's geographical range and each of the two hypotheses. We combined climate envelope models and a population model with explicit treatment of woolly mammoth-human interactions to measure the extent to which a combination of climate changes and increased human pressures might have led to the extinction of the species in Eurasia. Climate conditions for woolly mammoths were measured across different time periods: 126 ky BP, 42 ky BP, 30 ky BP, 21 ky BP, and 6 ky BP. We show that suitable climate conditions for the mammoth reduced drastically between the Late Pleistocene and the Holocene, and 90% of its geographical range disappeared between 42 ky BP and 6 ky BP, with the remaining suitable areas in the mid-Holocene being mainly restricted to Arctic Siberia, which is where the latest records of woolly mammoths in continental Asia have been found. Results of the population models also show that the collapse of the climatic niche of the mammoth caused a significant drop in their population size, making woolly mammoths more vulnerable to the increasing hunting pressure from human populations. The coincidence of the disappearance of climatically suitable areas for woolly mammoths and the increase in anthropogenic impacts in the Holocene, the coup de grâce, likely set the place and time for the extinction of the woolly mammoth.
format article
author David Nogués-Bravo
Jesús Rodríguez
Joaquín Hortal
Persaram Batra
Miguel B Araújo
author_facet David Nogués-Bravo
Jesús Rodríguez
Joaquín Hortal
Persaram Batra
Miguel B Araújo
author_sort David Nogués-Bravo
title Climate change, humans, and the extinction of the woolly mammoth.
title_short Climate change, humans, and the extinction of the woolly mammoth.
title_full Climate change, humans, and the extinction of the woolly mammoth.
title_fullStr Climate change, humans, and the extinction of the woolly mammoth.
title_full_unstemmed Climate change, humans, and the extinction of the woolly mammoth.
title_sort climate change, humans, and the extinction of the woolly mammoth.
publisher Public Library of Science (PLoS)
publishDate 2008
url https://doaj.org/article/8628ce89d28c4e42af6ef07a8eab9d09
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