Arid
DOI10.1016/j.gloplacha.2023.104049
Neogene global climate change and East Asian dust sources: Combined rutile geochemistry and zircon U-Pb analysis from the northern Chinese Loess Plateau
Bohm, Katja; Kaakinen, Anu; Stevens, Thomas; Lahaye, Yann; Tang, Hui; Shang, Yuan; Zhang, Hanzhi; Lu, Huayu
通讯作者Bohm, K
来源期刊GLOBAL AND PLANETARY CHANGE
ISSN0921-8181
EISSN1872-6364
出版年2023
卷号221
英文摘要During the late Neogene, global climate underwent a long-term transition to cooler climates that culminated in the Quaternary icehouse conditions. In the East Asian terrestrial realm, atmospheric dustiness increased, and the volume of aeolian dust deposits expanded significantly. The Neogene Red Clay deposits, located on the Chinese Loess Plateau (CLP), provide an exceptional geologic archive to investigate pre-Quaternary climates and envi-ronments. Constraining the provenance of the Red Clay is crucial for unravelling the links between late Neogene Central-East Asian climate, tectonics and desertification. However, Red Clay provenance is highly debated and data are scarce. In this study, we have used a multi-proxy approach at a high sampling resolution to study the provenance of the c. 7-2.6 Ma Baode Red Clay. Our data consist of joint detrital zircon U-Pb ages and detrital rutile trace element geochemistry of the Baode Red Clay, and of a massive rutile geochemistry dataset from 14 potential dust source areas. The data indicate that the Mio-Pliocene and Plio-Pleistocene global climate transi-tions were coupled with gradual dust provenance shifts. We propose these shifts indicate the intensification of East Asian winter monsoon and/or enhanced Central-East Asian drying as a response to global cooling. We also identify temporary Pliocene provenance changes that interrupt the long-term winter monsoon-controlled dust transport at c. 4 Ma and c. 3.5 Ma. Several indicators point to dust transport by the westerly jet at c. 4 Ma, possibly caused by a shift in the jet position as a response to global cooling, and/or enhanced wet deposition caused by intensified summer monsoon. Alternatively, the role of the paleo-Yellow River should be investigated further. We infer the 3.5 Ma provenance signal was caused by increased Yellow River-transported material from eroding Northeastern Tibetan Plateau and/or western CLP. Implications of our results not only shed light on the links between late Cenozoic global climate change and Central-East Asian dust cycle, but also provide detailed information to further investigate the late Neogene regional geomorphology and its effects on dust emission, transport, and deposition. Our combined rutile-zircon analysis also verifies that a multi-proxy single-grain approach that targets different types of primary source rocks is needed for reliable provenance analysis of the CLP dust.
英文关键词Red clay Late Cenozoic Aeolian sediment Multi-proxy single-grain provenance East Asian winter monsoon Westerly jet
类型Article
语种英语
开放获取类型hybrid, Green Published
收录类别SCI-E
WOS记录号WOS:000932496700001
WOS关键词RED CLAY DEPOSITS ; LATE MIOCENE ; TIBETAN PLATEAU ; LATE PLIOCENE ; YELLOW-RIVER ; UPLIFT ; PROVENANCE ; RECORD ; THERMOCHRONOLOGY ; SEDIMENTATION
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/396762
推荐引用方式
GB/T 7714
Bohm, Katja,Kaakinen, Anu,Stevens, Thomas,et al. Neogene global climate change and East Asian dust sources: Combined rutile geochemistry and zircon U-Pb analysis from the northern Chinese Loess Plateau[J],2023,221.
APA Bohm, Katja.,Kaakinen, Anu.,Stevens, Thomas.,Lahaye, Yann.,Tang, Hui.,...&Lu, Huayu.(2023).Neogene global climate change and East Asian dust sources: Combined rutile geochemistry and zircon U-Pb analysis from the northern Chinese Loess Plateau.GLOBAL AND PLANETARY CHANGE,221.
MLA Bohm, Katja,et al."Neogene global climate change and East Asian dust sources: Combined rutile geochemistry and zircon U-Pb analysis from the northern Chinese Loess Plateau".GLOBAL AND PLANETARY CHANGE 221(2023).
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