Aridification signatures from middle–late Eocene pollen indicate widespread drying across the Tibetan Plateau after 40 Ma
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Aridification signatures from middle–late Eocene pollen indicate widespread drying across the Tibetan Plateau after 40 Ma ; year:2020 ; pages:1-42
Climate of the past discussions ; (2020), 1-42
- Creator
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Yuan, Qin
Barbolini, Natasha
Rydin, Catarina
Gao, Dong-Lin
Wei, Hai-Cheng
Fan, Qi-Shun
Qin, Zhan-Jie
Du, Yong-Sheng
Shan, Jun-Jie
Shan, Fa-Shou
Vajda, Vivi
- DOI
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10.5194/cp-2019-138
- URN
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urn:nbn:de:101:1-2020012303581275394051
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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2025-08-14T10:54:55+0200
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Yuan, Qin
- Barbolini, Natasha
- Rydin, Catarina
- Gao, Dong-Lin
- Wei, Hai-Cheng
- Fan, Qi-Shun
- Qin, Zhan-Jie
- Du, Yong-Sheng
- Shan, Jun-Jie
- Shan, Fa-Shou
- Vajda, Vivi
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Aridification signatures from fossil pollen indicate a drying climate in east-central Tibet during the late Eocene
Evidence for a widespread climatic anomaly at around 7.5–7.0 cal ka BP
Observations indicate regionally misleading wetting and drying trends in CMIP6
Urinary, Circulating, and Tissue Biomonitoring Studies Indicate Widespread Exposure to Bisphenol A
Fossil plant stomata indicate decreasing atmospheric CO 2 prior to the Eocene–Oligocene boundary
Increases in the temperature seasonal cycle indicate long-term drying trends in Amazonia
Red clays indicate sub-aerial exposure of the Rio Grande Rise during the Eocene volcanic episode
Chapitre XVI. Formations éocène moyen et éocène inférieur
Atmospheric blocking induced by the strengthened Siberian High led to drying in west Asia during the 4.2 ka BP event – a hypothesis
A meta-analysis on environmental drivers of marine phytoplankton C : N : P
A meta-analysis on environmental drivers of marine phytoplankton C : N : P
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Aridification signatures from fossil pollen indicate a drying climate in east-central Tibet during the late Eocene
Evidence for a widespread climatic anomaly at around 7.5–7.0 cal ka BP
Observations indicate regionally misleading wetting and drying trends in CMIP6
Urinary, Circulating, and Tissue Biomonitoring Studies Indicate Widespread Exposure to Bisphenol A
Fossil plant stomata indicate decreasing atmospheric CO 2 prior to the Eocene–Oligocene boundary
Increases in the temperature seasonal cycle indicate long-term drying trends in Amazonia
Red clays indicate sub-aerial exposure of the Rio Grande Rise during the Eocene volcanic episode
Chapitre XVI. Formations éocène moyen et éocène inférieur
Atmospheric blocking induced by the strengthened Siberian High led to drying in west Asia during the 4.2 ka BP event – a hypothesis
A meta-analysis on environmental drivers of marine phytoplankton C : N : P
A meta-analysis on environmental drivers of marine phytoplankton C : N : P