Global cooling and enhanced Eocene Asian mid-latitude interior aridity

Simple item page
dc.contributor.authorLi, J. X.
dc.contributor.authorYue, L. P.
dc.contributor.authorRoberts, Andrew P.
dc.contributor.authorHirt, A. M.
dc.contributor.authorPan, F.
dc.contributor.authorGuo, Lin
dc.contributor.authorXu, Y.
dc.contributor.authorXi, R. G.
dc.contributor.authorGuo, Lei
dc.contributor.authorQiang, Xiaoke
dc.contributor.authorGai, C. C.
dc.contributor.authorJiang, Zhaoxia
dc.contributor.authorSun, Z. M.
dc.contributor.authorLiu, Q. S.
dc.date.accessioned2020-04-14T05:51:27Z
dc.date.available2020-04-14T05:51:27Z
dc.date.issued2018
dc.date.updated2019-11-25T07:52:15Z
dc.description.abstractTibetan Plateau uplift has been suggested as the main driving force for mid-latitude Asian inland aridity (AIA) and for deposition of thick aeolian sequences in northern China since the Miocene. However, the relationship between earlier AIA and Tibetan Plateau mountain building is uncertain because of a lack of corresponding thick aeolian sequences with accurate age constraints. We here present results for a continuous aeolian sequence that spans the interval from >51 to 39 Ma from the eastern Xorkol Basin, Altun Shan, northeastern Tibetan Plateau. The basal age of the studied sequence postdates initial uplift of the Tibetan Plateau by several million years. Our results indicate that the local palaeoclimate was teleconnected strongly to the overall global cooling pattern, so that local enhanced aridification recorded by the studied aeolian sequence is dominantly a response to global climatic forcing rather than plateau uplift.en_AU
dc.description.sponsorshipThis study was supported by the National Natural Science Foundation of China (NNSFC Grant Nos. 41002052), the National Key Research and Development Program of China (2016YFA0601903), NNSFC Grant Nos. 41430962, 41072136, 41202133 and 90814005, the “Geological Elite Program” of the China Geological Survey, Land Resources Survey Project (Grant No. 1212011121185), Nonprofit Special Project of Land Resources (Grant No. 201311126) and the Australian Research Council (grant DP110105419).en_AU
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn2041-1723en_AU
dc.identifier.urihttp://hdl.handle.net/1885/202931
dc.language.isoen_AUen_AU
dc.provenanceOpen Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/ licenses/by/4.0/.en_AU
dc.publisherMacmillan Publishers Ltden_AU
dc.relationhttp://purl.org/au-research/grants/arc/DP110105419en_AU
dc.rights© The Author(s) 2018en_AU
dc.rights.licenseCreative Commons Attribution 4.0 International Licenseen_AU
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en_AU
dc.sourceNature Communicationsen_AU
dc.titleGlobal cooling and enhanced Eocene Asian mid-latitude interior aridityen_AU
dc.typeJournal articleen_AU
dcterms.accessRightsOpen Accessen_AU
local.bibliographicCitation.lastpage8en_AU
local.bibliographicCitation.startpage1en_AU
local.contributor.affiliationLi, J X, China Geological Surveyen_AU
local.contributor.affiliationYue, L P, Northwest Universityen_AU
local.contributor.affiliationRoberts, Andrew, College of Science, ANUen_AU
local.contributor.affiliationHirt, A M, Eidgenössische Technische Hochschule Zürichen_AU
local.contributor.affiliationPan, F, China Geological Surveyen_AU
local.contributor.affiliationGuo, Lin, China Geological Surveyen_AU
local.contributor.affiliationXu, Y, China Geological Surveyen_AU
local.contributor.affiliationXi, R G, China Geological Surveyen_AU
local.contributor.affiliationGuo, Lei, China Geological Surveyen_AU
local.contributor.affiliationQiang, Xiaoke, Chinese Academy of Sciencesen_AU
local.contributor.affiliationGai, C C, Chinese Academy of Sciencesen_AU
local.contributor.affiliationJiang, Zhaoxia, College of Science, ANUen_AU
local.contributor.affiliationSun, Z M, Chinese Academy of Geological Sciencesen_AU
local.contributor.affiliationLiu, Q S, Southern University of Science and Technologyen_AU
local.contributor.authoruidRoberts, Andrew, u4817957en_AU
local.contributor.authoruidJiang, Zhaoxia, u1007968en_AU
local.description.notesImported from ARIESen_AU
local.identifier.absfor040605 - Palaeoclimatologyen_AU
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciencesen_AU
local.identifier.ariespublicationu4485658xPUB1748en_AU
local.identifier.citationvolume9en_AU
local.identifier.doi10.1038/s41467-018-05415-xen_AU
local.identifier.scopusID2-s2.0-85051080448
local.identifier.thomsonID000440617500002
local.publisher.urlhttps://www.nature.com/en_AU
local.type.statusPublished Versionen_AU

Downloads

Original bundle

Now showing 1 - 1 of 1
Thumbnail Image
Name:
01_Li_Global_cooling_and_enhanced_2018.pdf
Size:
1.99 MB
Format:
Adobe Portable Document Format
Download

Collections

ANU Research Publications

DSpace software copyright © 2002-2026 LYRASIS