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Shuhuan Du
Researcher at Chinese Academy of Sciences
Publications - 16
Citations - 59
Shuhuan Du is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Holocene & Monsoon. The author has an hindex of 3, co-authored 13 publications receiving 35 citations.
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Journal ArticleDOI
Kiloyear-scale climate events and evolution during the Last Interglacial, Mu Us Desert, China
Shuhuan Du,Baosheng Li,Baosheng Li,Muhong Chen,David D. Zhang,Rong Xiang,Dongfeng Niu,Xiaohao Wen,Xianjiao Ou +8 more
TL;DR: In this article, the authors used the Milanggouwan stratigraphical section (MGS 5) in the Mu Us Desert to provide high-resolution geological information on environmental variations during the Last Interglacial.
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The present-day atmospheric dust deposition process in the South China Sea
TL;DR: In this paper, the authors investigated the grain size distribution, depositional flux, and features revealed by scanning electron microscopy, combined with 5-day back trajectories to indicate the present-day dust deposition process for the first time.
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Paleotempestology evidence recorded by eolian deposition in the Bohai Sea coastal zone during the last interglacial period
TL;DR: In this article, the authors examined the storm deposits in the eolian sediments of the Bohai Sea coastal zone at middle latitudes, choosing the Miaodao stratigraphic section (MDS) as the target area.
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East Asian monsoon variations on millennial scale during 35,000–25,000 a BP from records of grain size, CaCO3 and organic matter in the Badain Jaran Desert, China
Yihua Guo,Baosheng Li,Baosheng Li,Fengnian Wang,Yi Yang,Yuejun Si,Dongfeng Niu,Xiaohao Wen,Shuhuan Du,Zhiwen Li +9 more
TL;DR: The CGS3a segment of the Chagelebulu section in the southeastern Badain Jaran Desert in China records five and a half sedimentary cycles consisting of aeolian dune sands or loess alternating with overlying fluviolacustrine during 35,000-25,000 a BP as mentioned in this paper.
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Changes in intermediate water conditions in the northern South China Sea using Globorotalia inflata over the last 20 ka
TL;DR: In this paper, the authors present paired Mg/Ca and δ18O data for the planktonic foraminifera Globorotalia inflata from core GHE27L in the northern South China Sea (SCS) to investigate changes in the intermediate water of the SCS over the last 20 ka.