Mid-Pleistocene aridity and landscape shifts promoted Palearctic hominin dispersals
- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- Extent
-
1 Online-Ressource.
- Language
-
Englisch
- Bibliographic citation
-
Mid-Pleistocene aridity and landscape shifts promoted Palearctic hominin dispersals ; volume:15 ; number:1 ; day:27 ; month:11 ; year:2024 ; pages:1-13 ; date:12.2024
Nature Communications ; 15, Heft 1 (27.11.2024), 1-13, 12.2024
- Creator
-
Zan, Jinbo
Louys, Julien
Dennell, Robin
Petraglia, Michael D.
Ning, Wenxiao
Fang, Xiaomin
Zhang, Weilin
Hu, Zhe
- Contributor
-
SpringerLink (Online service)
- DOI
-
10.1038/s41467-024-54767-0
- URN
-
urn:nbn:de:101:1-2502122126058.179585956077
- Rights
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
-
17.08.2025, 7:50 AM CEST
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
- Zan, Jinbo
- Louys, Julien
- Dennell, Robin
- Petraglia, Michael D.
- Ning, Wenxiao
- Fang, Xiaomin
- Zhang, Weilin
- Hu, Zhe
- SpringerLink (Online service)
Other Objects (12)
Vegetation-based moisture shifts in Qaidam Basin (NE Tibetan Plateau) during the Mid-Pleistocene Transition
Diverse manifestations of the mid-Pleistocene climate transition
Predicted Pleistocene-Holocene range shifts of the tiger (Panthera tigris)
Pleistocene climate change promoted rapid diversification of aquatic invertebrates in Southeast Australia
Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition
Closure of the Bering Strait caused Mid-Pleistocene Transition cooling
Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis
Role of the North Atlantic circulation in the mid-Pleistocene transition
Change in the North Atlantic circulation associated with the mid-Pleistocene transition
Sea ice dynamics across the Mid-Pleistocene transition in the Bering Sea
The Mid-Pleistocene Transition: a delayed response to an increasing positive feedback?
Author Correction: Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis
Vegetation-based moisture shifts in Qaidam Basin (NE Tibetan Plateau) during the Mid-Pleistocene Transition
Diverse manifestations of the mid-Pleistocene climate transition
Predicted Pleistocene-Holocene range shifts of the tiger (Panthera tigris)
Pleistocene climate change promoted rapid diversification of aquatic invertebrates in Southeast Australia
Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition
Closure of the Bering Strait caused Mid-Pleistocene Transition cooling
Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis
Role of the North Atlantic circulation in the mid-Pleistocene transition
Change in the North Atlantic circulation associated with the mid-Pleistocene transition
Sea ice dynamics across the Mid-Pleistocene transition in the Bering Sea
The Mid-Pleistocene Transition: a delayed response to an increasing positive feedback?
Author Correction: Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis
Vegetation-based moisture shifts in Qaidam Basin (NE Tibetan Plateau) during the Mid-Pleistocene Transition
Diverse manifestations of the mid-Pleistocene climate transition
Predicted Pleistocene-Holocene range shifts of the tiger (Panthera tigris)
Pleistocene climate change promoted rapid diversification of aquatic invertebrates in Southeast Australia
Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition
Closure of the Bering Strait caused Mid-Pleistocene Transition cooling
Onset of Mid-Pleistocene glaciation in the Eastern Himalayan syntaxis
Role of the North Atlantic circulation in the mid-Pleistocene transition
Change in the North Atlantic circulation associated with the mid-Pleistocene transition
Sea ice dynamics across the Mid-Pleistocene transition in the Bering Sea
The Mid-Pleistocene Transition: a delayed response to an increasing positive feedback?