The flickering genes of the last mammoths

Woolly mammoths, Mammuthus primigenius , are arguably the most iconic of the extinct Pleistocene megafauna, and an abundance of large permafrost‐embedded bone and ivory material ( Fig. 1 ) means they were also among the first to yield credible DNA sequences ( Hagelberg et al. 1994 Hoss et al. 1994 )...

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Published in:Molecular Ecology
Main Author: THOMAS, M. G.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
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Online Access:http://dx.doi.org/10.1111/j.1365-294x.2012.05594.x
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spelling crwiley:10.1111/j.1365-294x.2012.05594.x 2024-09-09T19:24:37+00:00 The flickering genes of the last mammoths THOMAS, M. G. 2012 http://dx.doi.org/10.1111/j.1365-294x.2012.05594.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-294X.2012.05594.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-294X.2012.05594.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor http://doi.wiley.com/10.1002/tdm_license_1.1 Molecular Ecology volume 21, issue 14, page 3379-3381 ISSN 0962-1083 1365-294X journal-article 2012 crwiley https://doi.org/10.1111/j.1365-294x.2012.05594.x 2024-08-06T04:16:25Z Woolly mammoths, Mammuthus primigenius , are arguably the most iconic of the extinct Pleistocene megafauna, and an abundance of large permafrost‐embedded bone and ivory material ( Fig. 1 ) means they were also among the first to yield credible DNA sequences ( Hagelberg et al. 1994 Hoss et al. 1994 ). Despite mammoth remains being numerous throughout northern Eurasia and North America, both the earliest and most recent fossils are found in northeast Siberia, with the last known population being confined to Wrangel Island in the Arctic Ocean from around 10,000 years ago until their extinction around 4,000 years ago. The extent to which these Holocene mammoths were descended from the Pleistocene populations of Wrangel Island and the demographic nature of their terminal decline have, until now, remained something of a mystery. In this issue of Molecular Ecology , Nyström et al. (2012) report the first use of autosomal variation to track the decline of the last mammoths and, in doing so, take a significant step towards resolving these questions. The authors genotyped four microsatellite loci in 59 Pleistocene and Holocene mammoths from Wrangel Island and Chukotka in mainland northeastern Siberia and showed that while the Pleistocene‐to‐Holocene transition is associated with a significant reduction in genetic diversity, subsequent levels of variation remain constant until extinction. Such a pattern is somewhat surprising as it indicates that while the last mammoths were confined to only a few Arctic islands, their final extinction on Wrangel Island was not a gradual process resulting from loss of genetic diversity/inbreeding. Instead, it seems they maintained a viable effective population size of around 500 until near their presumably rapid extinction. While the ultimate agent of mammoth extinction remains unknown, the work of Nyström et al. (2012) . suggests that we should be looking for something sudden, like a rapid change in climate/ecology or perhaps the arrival of humans. Sergey Vartanyan during field ... Article in Journal/Newspaper Arctic Arctic Ocean Chukotka permafrost Wrangel Island Siberia Wiley Online Library Arctic Arctic Ocean Wrangel Island ENVELOPE(-179.385,-179.385,71.244,71.244) Molecular Ecology 21 14 3379 3381
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Woolly mammoths, Mammuthus primigenius , are arguably the most iconic of the extinct Pleistocene megafauna, and an abundance of large permafrost‐embedded bone and ivory material ( Fig. 1 ) means they were also among the first to yield credible DNA sequences ( Hagelberg et al. 1994 Hoss et al. 1994 ). Despite mammoth remains being numerous throughout northern Eurasia and North America, both the earliest and most recent fossils are found in northeast Siberia, with the last known population being confined to Wrangel Island in the Arctic Ocean from around 10,000 years ago until their extinction around 4,000 years ago. The extent to which these Holocene mammoths were descended from the Pleistocene populations of Wrangel Island and the demographic nature of their terminal decline have, until now, remained something of a mystery. In this issue of Molecular Ecology , Nyström et al. (2012) report the first use of autosomal variation to track the decline of the last mammoths and, in doing so, take a significant step towards resolving these questions. The authors genotyped four microsatellite loci in 59 Pleistocene and Holocene mammoths from Wrangel Island and Chukotka in mainland northeastern Siberia and showed that while the Pleistocene‐to‐Holocene transition is associated with a significant reduction in genetic diversity, subsequent levels of variation remain constant until extinction. Such a pattern is somewhat surprising as it indicates that while the last mammoths were confined to only a few Arctic islands, their final extinction on Wrangel Island was not a gradual process resulting from loss of genetic diversity/inbreeding. Instead, it seems they maintained a viable effective population size of around 500 until near their presumably rapid extinction. While the ultimate agent of mammoth extinction remains unknown, the work of Nyström et al. (2012) . suggests that we should be looking for something sudden, like a rapid change in climate/ecology or perhaps the arrival of humans. Sergey Vartanyan during field ...
format Article in Journal/Newspaper
author THOMAS, M. G.
spellingShingle THOMAS, M. G.
The flickering genes of the last mammoths
author_facet THOMAS, M. G.
author_sort THOMAS, M. G.
title The flickering genes of the last mammoths
title_short The flickering genes of the last mammoths
title_full The flickering genes of the last mammoths
title_fullStr The flickering genes of the last mammoths
title_full_unstemmed The flickering genes of the last mammoths
title_sort flickering genes of the last mammoths
publisher Wiley
publishDate 2012
url http://dx.doi.org/10.1111/j.1365-294x.2012.05594.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-294X.2012.05594.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-294X.2012.05594.x
long_lat ENVELOPE(-179.385,-179.385,71.244,71.244)
geographic Arctic
Arctic Ocean
Wrangel Island
geographic_facet Arctic
Arctic Ocean
Wrangel Island
genre Arctic
Arctic Ocean
Chukotka
permafrost
Wrangel Island
Siberia
genre_facet Arctic
Arctic Ocean
Chukotka
permafrost
Wrangel Island
Siberia
op_source Molecular Ecology
volume 21, issue 14, page 3379-3381
ISSN 0962-1083 1365-294X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
http://doi.wiley.com/10.1002/tdm_license_1.1
op_doi https://doi.org/10.1111/j.1365-294x.2012.05594.x
container_title Molecular Ecology
container_volume 21
container_issue 14
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