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: Other/Unknown Material
Language:unknown
Published: Zenodo 2019
Subjects:
Online Access:https://doi.org/10.5061/dryad.hp38ct1
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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.
collection Zenodo
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. Bison body size and climate change dataset Locality information: name, geologic age, latitude, longitude, specimen numbers, specimen voucher list, locality summary statistics, GISP2 temperature, linear osteometrics, species, elevation, etc. Bison_fullDB for MS.xlsx
format Other/Unknown Material
genre Greenland
Bison bison bison
genre_facet Greenland
Bison bison bison
geographic Greenland
Kya
geographic_facet Greenland
Kya
id ftzenodo:oai:zenodo.org:5001540
institution Open Polar
language unknown
long_lat ENVELOPE(8.308,8.308,63.772,63.772)
op_collection_id ftzenodo
op_doi https://doi.org/10.5061/dryad.hp38ct110.1002/ece3.4019
op_relation https://doi.org/10.1002/ece3.4019
https://zenodo.org/communities/dryad
https://doi.org/10.5061/dryad.hp38ct1
oai:zenodo.org:5001540
op_rights info:eu-repo/semantics/openAccess
Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
publishDate 2019
publisher Zenodo
record_format openpolar
spelling ftzenodo:oai:zenodo.org:5001540 2025-01-16T22:13:58+00:00 Data from: Bison body size and climate change Martin, Jeff M. Mead, Jim I. Barboza, Perry S. 2019-02-27 https://doi.org/10.5061/dryad.hp38ct1 unknown Zenodo https://doi.org/10.1002/ece3.4019 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.hp38ct1 oai:zenodo.org:5001540 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode Anthropocene Late Pleistocene Bison bison body size change Late Quaternary Holocene Bergmann's rule info:eu-repo/semantics/other 2019 ftzenodo https://doi.org/10.5061/dryad.hp38ct110.1002/ece3.4019 2024-12-05T08:58:42Z 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. Bison body size and climate change dataset Locality information: name, geologic age, latitude, longitude, specimen numbers, specimen voucher list, locality summary statistics, GISP2 temperature, linear osteometrics, species, elevation, etc. Bison_fullDB for MS.xlsx Other/Unknown Material Greenland Bison bison bison Zenodo Greenland Kya ENVELOPE(8.308,8.308,63.772,63.772)
spellingShingle Anthropocene
Late Pleistocene
Bison bison
body size change
Late Quaternary
Holocene
Bergmann's rule
Martin, Jeff M.
Mead, Jim I.
Barboza, Perry S.
Data from: Bison body size and climate change
title 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_short Data from: Bison body size and climate change
title_sort data from: bison body size and climate change
topic Anthropocene
Late Pleistocene
Bison bison
body size change
Late Quaternary
Holocene
Bergmann's rule
topic_facet Anthropocene
Late Pleistocene
Bison bison
body size change
Late Quaternary
Holocene
Bergmann's rule
url https://doi.org/10.5061/dryad.hp38ct1