ITPCAS OpenIR  > 图书馆
Prolonged Monsoonal Moisture Availability Preconditioned Glaciation of the Tibetan Plateau During the Mid-Pleistocene Transition
Koutsodendris, A (Koutsodendris, Andreas)1; Sachse, D (Sachse, Dirk)2; Appel, E (Appel, Erwin)3; Herb, C (Herb, Christian)3; Fischer, T (Fischer, Tobias)1; Fang, XM (Fang, Xiaomin)4; Pross, J (Pross, Joerg)1
Source PublicationGEOPHYSICAL RESEARCH LETTERS
2018-12-16
Volume45Issue:23Pages:13020-13030
DOI10.1029/2018GL079303
Abstract

Paleohydrological data comprising pollen assemblages and leaf-wax hydrogen isotopes (dDwax) 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 similar to 900 ka. Our dDwax results indicate a strong influence of proximal (monsoonal) moisture sources during that glacial, in agreement with the intensification of the interhemispheric moisture transport resulting from Antarctic ice volume increase at similar to 900 ka. The consistency of our results with other marine and terrestrial climate data sets suggests that extended glaciation on the Tibetan Plateau may have initiated similar to 500 ka earlier than previously assumed, implying that midlatitude ice sheets actively contributed to global cooling during the Mid-Pleistocene Transition. 

Subject Area地质学
WOS IDWOS:000454296600042
Language英语
Indexed BySCIE
KeywordWestern Qaidam Basin Resolution Pollen Record Drill Core Sg-1 Climate-change Antarctic Climate Hydrogen Isotopes Lake Elgygytgyn Central-asia Ice Volume Pleistocene
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
Cooperation Status国际
ISSN0094-8276
Department大陆碰撞与高原隆升重点实验室
PublisherAMER GEOPHYSICAL UNION
SubtypeArticle
Citation statistics
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/8472
Collection图书馆
Corresponding AuthorKoutsodendris, A (Koutsodendris, Andreas)
Affiliation1.Heidelberg Univ, Inst Earth Sci, Paleoenvironm Dynam Grp, Heidelberg, Germany;
2.GFZ German Res Ctr Geosci, Geomorphol, Potsdam, Germany;
3.Univ Tubingen, Dept Geosci, Tubingen, Germany;
4.Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing, Peoples R China.
Recommended Citation
GB/T 7714
Koutsodendris, A ,Sachse, D ,Appel, E ,et al. Prolonged Monsoonal Moisture Availability Preconditioned Glaciation of the Tibetan Plateau During the Mid-Pleistocene Transition[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(23):13020-13030.
APA Koutsodendris, A .,Sachse, D .,Appel, E .,Herb, C .,Fischer, T .,...&Pross, J .(2018).Prolonged Monsoonal Moisture Availability Preconditioned Glaciation of the Tibetan Plateau During the Mid-Pleistocene Transition.GEOPHYSICAL RESEARCH LETTERS,45(23),13020-13030.
MLA Koutsodendris, A ,et al."Prolonged Monsoonal Moisture Availability Preconditioned Glaciation of the Tibetan Plateau During the Mid-Pleistocene Transition".GEOPHYSICAL RESEARCH LETTERS 45.23(2018):13020-13030.
Files in This Item:
File Name/Size DocType Version Access License
2018010.pdf(1015KB)期刊论文出版稿开放获取CC BY-NC-SAView Application Full Text
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[Koutsodendris, A (Koutsodendris, Andreas)]'s Articles
[Sachse, D (Sachse, Dirk)]'s Articles
[Appel, E (Appel, Erwin)]'s Articles
Baidu academic
Similar articles in Baidu academic
[Koutsodendris, A (Koutsodendris, Andreas)]'s Articles
[Sachse, D (Sachse, Dirk)]'s Articles
[Appel, E (Appel, Erwin)]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Koutsodendris, A (Koutsodendris, Andreas)]'s Articles
[Sachse, D (Sachse, Dirk)]'s Articles
[Appel, E (Appel, Erwin)]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: 2018010.pdf
Format: Adobe PDF
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.