Biomarker and pollen in core SG-1 from Tibetan Plateau spanning the Mid-Pleistocene Transition ...
Paleohydrological data comprising pollen assemblages and leaf-wax hydrogen isotopes (δDwax) from paleolake sediments in the Qaidam Basin (China) provide evidence for a link between increased moisture availability on the Tibetan Plateau and global cooling during the Mid-Pleistocene Transition. Notabl...
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ftdatacite:10.1594/pangaea.896040 2024-09-09T19:08:16+00:00 Biomarker and pollen in core SG-1 from Tibetan Plateau spanning the Mid-Pleistocene Transition ... Koutsodendris, Andreas Sachse, Dirk Appel, Erwin Herb, Christian Fischer, Tobias Fang, Xiaomin Pross, Jörg 2018 application/zip https://dx.doi.org/10.1594/pangaea.896040 https://doi.pangaea.de/10.1594/PANGAEA.896040 en eng PANGAEA https://dx.doi.org/10.1029/2018gl079303 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Drilling/drill rig Collection Supplementary Publication Series of Datasets article 2018 ftdatacite https://doi.org/10.1594/pangaea.89604010.1029/2018gl079303 2024-06-17T10:03:38Z Paleohydrological data comprising pollen assemblages and leaf-wax hydrogen isotopes (δDwax) from paleolake sediments in the Qaidam Basin (China) provide evidence for a link between increased moisture availability on the Tibetan Plateau and global cooling during the Mid-Pleistocene Transition. Notably, they document the persistence of humid and cold conditions during Marine Isotope Stages 24–22 (936–866 ka) suggesting that boundary conditions favorable for extended glaciation on the Tibetan Plateau first developed at ~900 ka. Our δDwax results indicate a strong influence of proximal (monsoonal) moisture sources during that glacial, in agreement with the intensification of the inter-hemispheric moisture transport resulting from Antarctic ice-volume increase at ~900 ka. The consistency of our results with other marine and terrestrial climate datasets suggests that extended glaciation on the Tibetan Plateau may have initiated ~500 ka earlier than previously assumed, implying that mid-latitude ice sheets actively ... : Supplement to: Koutsodendris, Andreas; Sachse, Dirk; Appel, Erwin; Herb, Christian; Fischer, Tobias; Fang, Xiaomin; Pross, Jörg (2018): Prolonged monsoonal moisture availability preconditioned glaciation of the Tibetan Plateau during the mid‐Pleistocene transition. Geophysical Research Letters, 45, 13020-13030 ... Article in Journal/Newspaper Antarc* Antarctic DataCite Antarctic Andreas ENVELOPE(-60.729,-60.729,-64.008,-64.008) Fang ENVELOPE(167.217,167.217,-77.483,-77.483) |
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English |
topic |
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Drilling/drill rig Koutsodendris, Andreas Sachse, Dirk Appel, Erwin Herb, Christian Fischer, Tobias Fang, Xiaomin Pross, Jörg Biomarker and pollen in core SG-1 from Tibetan Plateau spanning the Mid-Pleistocene Transition ... |
topic_facet |
Drilling/drill rig |
description |
Paleohydrological data comprising pollen assemblages and leaf-wax hydrogen isotopes (δDwax) from paleolake sediments in the Qaidam Basin (China) provide evidence for a link between increased moisture availability on the Tibetan Plateau and global cooling during the Mid-Pleistocene Transition. Notably, they document the persistence of humid and cold conditions during Marine Isotope Stages 24–22 (936–866 ka) suggesting that boundary conditions favorable for extended glaciation on the Tibetan Plateau first developed at ~900 ka. Our δDwax results indicate a strong influence of proximal (monsoonal) moisture sources during that glacial, in agreement with the intensification of the inter-hemispheric moisture transport resulting from Antarctic ice-volume increase at ~900 ka. The consistency of our results with other marine and terrestrial climate datasets suggests that extended glaciation on the Tibetan Plateau may have initiated ~500 ka earlier than previously assumed, implying that mid-latitude ice sheets actively ... : Supplement to: Koutsodendris, Andreas; Sachse, Dirk; Appel, Erwin; Herb, Christian; Fischer, Tobias; Fang, Xiaomin; Pross, Jörg (2018): Prolonged monsoonal moisture availability preconditioned glaciation of the Tibetan Plateau during the mid‐Pleistocene transition. Geophysical Research Letters, 45, 13020-13030 ... |
format |
Article in Journal/Newspaper |
author |
Koutsodendris, Andreas Sachse, Dirk Appel, Erwin Herb, Christian Fischer, Tobias Fang, Xiaomin Pross, Jörg |
author_facet |
Koutsodendris, Andreas Sachse, Dirk Appel, Erwin Herb, Christian Fischer, Tobias Fang, Xiaomin Pross, Jörg |
author_sort |
Koutsodendris, Andreas |
title |
Biomarker and pollen in core SG-1 from Tibetan Plateau spanning the Mid-Pleistocene Transition ... |
title_short |
Biomarker and pollen in core SG-1 from Tibetan Plateau spanning the Mid-Pleistocene Transition ... |
title_full |
Biomarker and pollen in core SG-1 from Tibetan Plateau spanning the Mid-Pleistocene Transition ... |
title_fullStr |
Biomarker and pollen in core SG-1 from Tibetan Plateau spanning the Mid-Pleistocene Transition ... |
title_full_unstemmed |
Biomarker and pollen in core SG-1 from Tibetan Plateau spanning the Mid-Pleistocene Transition ... |
title_sort |
biomarker and pollen in core sg-1 from tibetan plateau spanning the mid-pleistocene transition ... |
publisher |
PANGAEA |
publishDate |
2018 |
url |
https://dx.doi.org/10.1594/pangaea.896040 https://doi.pangaea.de/10.1594/PANGAEA.896040 |
long_lat |
ENVELOPE(-60.729,-60.729,-64.008,-64.008) ENVELOPE(167.217,167.217,-77.483,-77.483) |
geographic |
Antarctic Andreas Fang |
geographic_facet |
Antarctic Andreas Fang |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
https://dx.doi.org/10.1029/2018gl079303 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.89604010.1029/2018gl079303 |
_version_ |
1809822477270908928 |