Deep heat: proxies, miocene ice, and an end in sight for paleoclimate paradoxes?
Abstract: The mid Miocene represents an important target for paleoclimatic study because the atmospheric CO2 concentration ranged from near modern values to ∼800 ppm, while a large, dynamic Antarctic ice sheet was likely to have been present throughout much of this interval. In this special issue, M...
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ftunivfrankfurt:oai:publikationen.ub.uni-frankfurt.de:62005 2023-05-15T13:48:29+02:00 Deep heat: proxies, miocene ice, and an end in sight for paleoclimate paradoxes? Evans, David 2021-02-02 application/octet-stream http://publikationen.ub.uni-frankfurt.de/frontdoor/index/index/docId/62005 https://nbn-resolving.org/urn:nbn:de:hebis:30:3-620056 https://doi.org/10.1029/2020PA004174 http://publikationen.ub.uni-frankfurt.de/files/62005/container.zip eng eng http://publikationen.ub.uni-frankfurt.de/frontdoor/index/index/docId/62005 urn:nbn:de:hebis:30:3-620056 https://nbn-resolving.org/urn:nbn:de:hebis:30:3-620056 https://doi.org/10.1029/2020PA004174 http://publikationen.ub.uni-frankfurt.de/files/62005/container.zip http://creativecommons.org/licenses/by-nc-nd/4.0/de/deed.de info:eu-repo/semantics/restrictedAccess CC-BY-NC-ND ddc:550 article doc-type:article 2021 ftunivfrankfurt https://doi.org/10.1029/2020PA004174 2022-11-13T23:40:53Z Abstract: The mid Miocene represents an important target for paleoclimatic study because the atmospheric CO2 concentration ranged from near modern values to ∼800 ppm, while a large, dynamic Antarctic ice sheet was likely to have been present throughout much of this interval. In this special issue, Modestou et al. (2020) (doi.org/10.1029/2020PA003927) reconstruct deep ocean warmth based on the clumped isotopic composition of benthic foraminifera, a technique that allows the ice volume and thermal components of the benthic oxygen isotope stack to be separated. These data reveal a very warm deep ocean while simultaneously suggesting that continental ice volume may, at times, have been greater than today. Here, I review these results in the context of recent developments in geochemical proxies and ice sheet modeling, and explore how the presence of a large Miocene ice sheet could be reconciled with CO2 at least as high as present. More broadly, I argue that many of the 'paradoxes' that pepper the paleoclimate literature result as much from our imperfect understanding of the proxies, as from our understanding of the climate system. Robust proxies with a well-understood mechanistic basis, as employed by Modestou et al. (2020), as well as advances in model-data comparability usher in a new era of palaeoclimate research; an exciting future of untangling Earth's myriad past climate states awaits. Plain Language Summary: Reconstructing climate variation in Earth's geologic past informs us of the broad features of warm climates, which is relevant to preparing for climate change over the coming centuries. Moreover, these data can be compared to state-of-the-art climate models, which provides a test of the degree to which our models can reproduce warm climate states. A paper recently published in this journal applies a new method in order to reconstruct the temperature of the deep ocean in the middle Miocene (between 17 and 12 million years ago), when the atmospheric CO2 concentration was naturally similar to or higher than ... Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Publication Server of Goethe University Frankfurt am Main Antarctic Paleoceanography and Paleoclimatology 36 3 |
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Publication Server of Goethe University Frankfurt am Main |
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ddc:550 Evans, David Deep heat: proxies, miocene ice, and an end in sight for paleoclimate paradoxes? |
topic_facet |
ddc:550 |
description |
Abstract: The mid Miocene represents an important target for paleoclimatic study because the atmospheric CO2 concentration ranged from near modern values to ∼800 ppm, while a large, dynamic Antarctic ice sheet was likely to have been present throughout much of this interval. In this special issue, Modestou et al. (2020) (doi.org/10.1029/2020PA003927) reconstruct deep ocean warmth based on the clumped isotopic composition of benthic foraminifera, a technique that allows the ice volume and thermal components of the benthic oxygen isotope stack to be separated. These data reveal a very warm deep ocean while simultaneously suggesting that continental ice volume may, at times, have been greater than today. Here, I review these results in the context of recent developments in geochemical proxies and ice sheet modeling, and explore how the presence of a large Miocene ice sheet could be reconciled with CO2 at least as high as present. More broadly, I argue that many of the 'paradoxes' that pepper the paleoclimate literature result as much from our imperfect understanding of the proxies, as from our understanding of the climate system. Robust proxies with a well-understood mechanistic basis, as employed by Modestou et al. (2020), as well as advances in model-data comparability usher in a new era of palaeoclimate research; an exciting future of untangling Earth's myriad past climate states awaits. Plain Language Summary: Reconstructing climate variation in Earth's geologic past informs us of the broad features of warm climates, which is relevant to preparing for climate change over the coming centuries. Moreover, these data can be compared to state-of-the-art climate models, which provides a test of the degree to which our models can reproduce warm climate states. A paper recently published in this journal applies a new method in order to reconstruct the temperature of the deep ocean in the middle Miocene (between 17 and 12 million years ago), when the atmospheric CO2 concentration was naturally similar to or higher than ... |
format |
Article in Journal/Newspaper |
author |
Evans, David |
author_facet |
Evans, David |
author_sort |
Evans, David |
title |
Deep heat: proxies, miocene ice, and an end in sight for paleoclimate paradoxes? |
title_short |
Deep heat: proxies, miocene ice, and an end in sight for paleoclimate paradoxes? |
title_full |
Deep heat: proxies, miocene ice, and an end in sight for paleoclimate paradoxes? |
title_fullStr |
Deep heat: proxies, miocene ice, and an end in sight for paleoclimate paradoxes? |
title_full_unstemmed |
Deep heat: proxies, miocene ice, and an end in sight for paleoclimate paradoxes? |
title_sort |
deep heat: proxies, miocene ice, and an end in sight for paleoclimate paradoxes? |
publishDate |
2021 |
url |
http://publikationen.ub.uni-frankfurt.de/frontdoor/index/index/docId/62005 https://nbn-resolving.org/urn:nbn:de:hebis:30:3-620056 https://doi.org/10.1029/2020PA004174 http://publikationen.ub.uni-frankfurt.de/files/62005/container.zip |
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Antarctic |
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Antarctic |
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Antarc* Antarctic Ice Sheet |
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Antarc* Antarctic Ice Sheet |
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http://publikationen.ub.uni-frankfurt.de/frontdoor/index/index/docId/62005 urn:nbn:de:hebis:30:3-620056 https://nbn-resolving.org/urn:nbn:de:hebis:30:3-620056 https://doi.org/10.1029/2020PA004174 http://publikationen.ub.uni-frankfurt.de/files/62005/container.zip |
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http://creativecommons.org/licenses/by-nc-nd/4.0/de/deed.de info:eu-repo/semantics/restrictedAccess |
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CC-BY-NC-ND |
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Paleoceanography and Paleoclimatology |
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36 |
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