Data from: Bison body size and climate change

The relationship between body size and temperature of mammals is poorly resolved, especially for large keystone species such as bison (Bison bison). Bison are well-represented in the fossil record across North America, which provides an opportunity to relate body size to climate within a species. We...

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Main Authors: Martin, Jeff M., Mead, Jim I., Barboza, Perry S.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2018
Subjects:
Kya
Online Access:http://hdl.handle.net/10255/dryad.172833
https://doi.org/10.5061/dryad.hp38ct1
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record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.172833 2023-05-15T16:30:14+02:00 Data from: Bison body size and climate change Martin, Jeff M. Mead, Jim I. Barboza, Perry S. North America Late Quaternary Late Pleistocene Holocene Anthropocene 2018-04-11T17:38:52Z http://hdl.handle.net/10255/dryad.172833 https://doi.org/10.5061/dryad.hp38ct1 unknown doi:10.5061/dryad.hp38ct1/1 doi:10.1002/ece3.4019 doi:10.5061/dryad.hp38ct1 Martin JM, Mead JI, Barboza PS (2018) Bison body size and climate change. Ecology and Evolution 8(9): 4564-4574. http://hdl.handle.net/10255/dryad.172833 Bergmann's rule ungulate body size change climate change fossil North America Article 2018 ftdryad https://doi.org/10.5061/dryad.hp38ct1 https://doi.org/10.5061/dryad.hp38ct1/1 https://doi.org/10.1002/ece3.4019 2020-01-01T16:05:30Z The relationship between body size and temperature of mammals is poorly resolved, especially for large keystone species such as bison (Bison bison). Bison are well-represented in the fossil record across North America, which provides an opportunity to relate body size to climate within a species. We measured the length of a leg bone (calcaneal tuber, DstL) in 849 specimens from 60 localities that were dated by stratigraphy and 14C decay. We estimated body mass (M) as: M = (DstL/11.49) 3. Average annual temperature was estimated from δ18O values in the ice cores from Greenland. Calcaneal tuber length of Bison declined over the last 40,000 years, that is, average body mass was 37% larger (910 ± 50 kg) than today (665 ± 21 kg). Average annual temperature has warmed by 6°C since the Last Glacial Maximum (~24-18 kya) and is predicted to further increase by 4°C by the end of the 21st century. If body size continues to linearly respond to global temperature, Bison body mass will likely decline by an additional 46%, to 357 ± 54 kg, with an increase of 4°C globally. The rate of mass loss is 41 ± 10 kg per °C increase of global temperature. Changes in body size of Bison may be a result of migration, disease, or human harvest but those effects are likely to be local and short-term and not likely to persist over the long-time-scale of the fossil record. The strong correspondence between body size of bison and air temperature is more likely the result of persistent effects on the ability to grow and the consequences of sustaining a large body mass in a warming environment. Continuing rises in global temperature will likely depress body sizes of bison, and perhaps other large grazers, without human intervention. Article in Journal/Newspaper Greenland Bison bison bison Dryad Digital Repository (Duke University) Greenland Kya ENVELOPE(8.308,8.308,63.772,63.772)
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic Bergmann's rule
ungulate
body size change
climate change
fossil
North America
spellingShingle Bergmann's rule
ungulate
body size change
climate change
fossil
North America
Martin, Jeff M.
Mead, Jim I.
Barboza, Perry S.
Data from: Bison body size and climate change
topic_facet Bergmann's rule
ungulate
body size change
climate change
fossil
North America
description The relationship between body size and temperature of mammals is poorly resolved, especially for large keystone species such as bison (Bison bison). Bison are well-represented in the fossil record across North America, which provides an opportunity to relate body size to climate within a species. We measured the length of a leg bone (calcaneal tuber, DstL) in 849 specimens from 60 localities that were dated by stratigraphy and 14C decay. We estimated body mass (M) as: M = (DstL/11.49) 3. Average annual temperature was estimated from δ18O values in the ice cores from Greenland. Calcaneal tuber length of Bison declined over the last 40,000 years, that is, average body mass was 37% larger (910 ± 50 kg) than today (665 ± 21 kg). Average annual temperature has warmed by 6°C since the Last Glacial Maximum (~24-18 kya) and is predicted to further increase by 4°C by the end of the 21st century. If body size continues to linearly respond to global temperature, Bison body mass will likely decline by an additional 46%, to 357 ± 54 kg, with an increase of 4°C globally. The rate of mass loss is 41 ± 10 kg per °C increase of global temperature. Changes in body size of Bison may be a result of migration, disease, or human harvest but those effects are likely to be local and short-term and not likely to persist over the long-time-scale of the fossil record. The strong correspondence between body size of bison and air temperature is more likely the result of persistent effects on the ability to grow and the consequences of sustaining a large body mass in a warming environment. Continuing rises in global temperature will likely depress body sizes of bison, and perhaps other large grazers, without human intervention.
format Article in Journal/Newspaper
author Martin, Jeff M.
Mead, Jim I.
Barboza, Perry S.
author_facet Martin, Jeff M.
Mead, Jim I.
Barboza, Perry S.
author_sort Martin, Jeff M.
title Data from: Bison body size and climate change
title_short Data from: Bison body size and climate change
title_full Data from: Bison body size and climate change
title_fullStr Data from: Bison body size and climate change
title_full_unstemmed Data from: Bison body size and climate change
title_sort data from: bison body size and climate change
publishDate 2018
url http://hdl.handle.net/10255/dryad.172833
https://doi.org/10.5061/dryad.hp38ct1
op_coverage North America
Late Quaternary
Late Pleistocene
Holocene
Anthropocene
long_lat ENVELOPE(8.308,8.308,63.772,63.772)
geographic Greenland
Kya
geographic_facet Greenland
Kya
genre Greenland
Bison bison bison
genre_facet Greenland
Bison bison bison
op_relation doi:10.5061/dryad.hp38ct1/1
doi:10.1002/ece3.4019
doi:10.5061/dryad.hp38ct1
Martin JM, Mead JI, Barboza PS (2018) Bison body size and climate change. Ecology and Evolution 8(9): 4564-4574.
http://hdl.handle.net/10255/dryad.172833
op_doi https://doi.org/10.5061/dryad.hp38ct1
https://doi.org/10.5061/dryad.hp38ct1/1
https://doi.org/10.1002/ece3.4019
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