Late <scp>C</scp> enozoic Polar Glaciations
The Cenozoic geological era has seen the transition from a warm “greenhouse” climate, with limited or absent cryosphere, to one with large ice sheets in either hemisphere. Much of what we know about the evolution and development of Cenozoic glaciations comes from records far removed from the polar r...
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crwiley:10.1002/9781118786352.wbieg0482 2024-03-17T08:58:26+00:00 Late <scp>C</scp> enozoic Polar Glaciations McKay, Rob 2017 http://dx.doi.org/10.1002/9781118786352.wbieg0482 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F9781118786352.wbieg0482 https://onlinelibrary.wiley.com/doi/pdf/10.1002/9781118786352.wbieg0482 unknown Wiley http://doi.wiley.com/10.1002/tdm_license_1.1 http://doi.wiley.com/10.1002/tdm_license_1.1 International Encyclopedia of Geography page 1-9 ISBN 9780470659632 9781118786352 other 2017 crwiley https://doi.org/10.1002/9781118786352.wbieg0482 2024-02-22T00:34:12Z The Cenozoic geological era has seen the transition from a warm “greenhouse” climate, with limited or absent cryosphere, to one with large ice sheets in either hemisphere. Much of what we know about the evolution and development of Cenozoic glaciations comes from records far removed from the polar regions, in particular marine isotope and eustatic sea level records. These records provide a high‐resolution, continuous but indirect record of global ice volume changes through time. However, identifying the geographical distribution of ice sheet evolution in either hemisphere through time has proved difficult due to the sparse, discontinuous, and inaccessible nature of geological records in polar regions. Other/Unknown Material Ice Sheet Wiley Online Library 1 9 |
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The Cenozoic geological era has seen the transition from a warm “greenhouse” climate, with limited or absent cryosphere, to one with large ice sheets in either hemisphere. Much of what we know about the evolution and development of Cenozoic glaciations comes from records far removed from the polar regions, in particular marine isotope and eustatic sea level records. These records provide a high‐resolution, continuous but indirect record of global ice volume changes through time. However, identifying the geographical distribution of ice sheet evolution in either hemisphere through time has proved difficult due to the sparse, discontinuous, and inaccessible nature of geological records in polar regions. |
format |
Other/Unknown Material |
author |
McKay, Rob |
spellingShingle |
McKay, Rob Late <scp>C</scp> enozoic Polar Glaciations |
author_facet |
McKay, Rob |
author_sort |
McKay, Rob |
title |
Late <scp>C</scp> enozoic Polar Glaciations |
title_short |
Late <scp>C</scp> enozoic Polar Glaciations |
title_full |
Late <scp>C</scp> enozoic Polar Glaciations |
title_fullStr |
Late <scp>C</scp> enozoic Polar Glaciations |
title_full_unstemmed |
Late <scp>C</scp> enozoic Polar Glaciations |
title_sort |
late <scp>c</scp> enozoic polar glaciations |
publisher |
Wiley |
publishDate |
2017 |
url |
http://dx.doi.org/10.1002/9781118786352.wbieg0482 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F9781118786352.wbieg0482 https://onlinelibrary.wiley.com/doi/pdf/10.1002/9781118786352.wbieg0482 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
International Encyclopedia of Geography page 1-9 ISBN 9780470659632 9781118786352 |
op_rights |
http://doi.wiley.com/10.1002/tdm_license_1.1 http://doi.wiley.com/10.1002/tdm_license_1.1 |
op_doi |
https://doi.org/10.1002/9781118786352.wbieg0482 |
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9 |
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1793768034116042752 |