Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years ...
The reasons for the early Holocene temperature discrepancy between northern hemispheric model simulations and paleoclimate reconstructions—known as the Holocene temperature conundrum—remain unclear. Using hydrogen isotopes of fluid inclusion water extracted from stalagmites from the Milandre Cave in...
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American Association for the Advancement of Science
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Online Access: | https://dx.doi.org/10.48350/158631 https://boris.unibe.ch/158631/ |
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ftdatacite:10.48350/158631 2024-09-30T14:35:53+00:00 Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years ... Affolter, Stéphane Häuselmann, Anamaria Fleitmann, Dominik Lawrence Edwards, R. Cheng, Hai Leuenberger, Markus 2019 https://dx.doi.org/10.48350/158631 https://boris.unibe.ch/158631/ unknown American Association for the Advancement of Science open access Creative Commons Attribution Non Commercial 4.0 International https://creativecommons.org/licenses/by-nc/4.0/legalcode cc-by-nc-4.0 http://purl.org/coar/access_right/c_abf2 530 Physics 550 Earth sciences & geology Text ScholarlyArticle article-journal journal article 2019 ftdatacite https://doi.org/10.48350/158631 2024-09-02T10:17:31Z The reasons for the early Holocene temperature discrepancy between northern hemispheric model simulations and paleoclimate reconstructions—known as the Holocene temperature conundrum—remain unclear. Using hydrogen isotopes of fluid inclusion water extracted from stalagmites from the Milandre Cave in Switzerland, we established a mid-latitude European mean annual temperature reconstruction for the past 14,000 years. Our Milandre Cave fluid inclusion temperature record (MC-FIT) resembles Greenland and Mediterranean sea surface temperature trends but differs from recent reconstructions obtained from biogenic proxies and climate models. The water isotopes are further synchronized with tropical precipitation records, stressing the Northern Hemisphere signature. Our results support the existence of a European Holocene Thermal Maximum and data-model temperature discrepancies. Moreover, data-data comparison reveals a significant latitudinal temperature gradient within Europe. Last, the MC-FIT record suggests that ... Text Greenland DataCite Greenland |
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530 Physics 550 Earth sciences & geology |
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530 Physics 550 Earth sciences & geology Affolter, Stéphane Häuselmann, Anamaria Fleitmann, Dominik Lawrence Edwards, R. Cheng, Hai Leuenberger, Markus Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years ... |
topic_facet |
530 Physics 550 Earth sciences & geology |
description |
The reasons for the early Holocene temperature discrepancy between northern hemispheric model simulations and paleoclimate reconstructions—known as the Holocene temperature conundrum—remain unclear. Using hydrogen isotopes of fluid inclusion water extracted from stalagmites from the Milandre Cave in Switzerland, we established a mid-latitude European mean annual temperature reconstruction for the past 14,000 years. Our Milandre Cave fluid inclusion temperature record (MC-FIT) resembles Greenland and Mediterranean sea surface temperature trends but differs from recent reconstructions obtained from biogenic proxies and climate models. The water isotopes are further synchronized with tropical precipitation records, stressing the Northern Hemisphere signature. Our results support the existence of a European Holocene Thermal Maximum and data-model temperature discrepancies. Moreover, data-data comparison reveals a significant latitudinal temperature gradient within Europe. Last, the MC-FIT record suggests that ... |
format |
Text |
author |
Affolter, Stéphane Häuselmann, Anamaria Fleitmann, Dominik Lawrence Edwards, R. Cheng, Hai Leuenberger, Markus |
author_facet |
Affolter, Stéphane Häuselmann, Anamaria Fleitmann, Dominik Lawrence Edwards, R. Cheng, Hai Leuenberger, Markus |
author_sort |
Affolter, Stéphane |
title |
Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years ... |
title_short |
Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years ... |
title_full |
Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years ... |
title_fullStr |
Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years ... |
title_full_unstemmed |
Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years ... |
title_sort |
central europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years ... |
publisher |
American Association for the Advancement of Science |
publishDate |
2019 |
url |
https://dx.doi.org/10.48350/158631 https://boris.unibe.ch/158631/ |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland |
genre_facet |
Greenland |
op_rights |
open access Creative Commons Attribution Non Commercial 4.0 International https://creativecommons.org/licenses/by-nc/4.0/legalcode cc-by-nc-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.48350/158631 |
_version_ |
1811639106249162752 |