Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266061, China
Yanguang Liu
Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266061, China
Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266061, China
Leonid Polyak
Byrd Polar and Climate Research Center, The Ohio State University, Columbus, 43210, USA
Yuanhui Huang
Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266061, China
Xisheng Fang
Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
Jianxing Liu
Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266061, China
Jianjun Zou
Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266061, China
Kunshan Wang
Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266061, China
Fuqiang Sun
Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
Xuchen Wang
Key Laboratory of Marine Chemistry Theory and Technology, Ocean University of China, Qingdao, 266100, China
Viewed
Total article views: 4,419 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,487
1,678
254
4,419
372
182
278
HTML: 2,487
PDF: 1,678
XML: 254
Total: 4,419
Supplement: 372
BibTeX: 182
EndNote: 278
Views and downloads (calculated since 16 Jan 2017)
Cumulative views and downloads
(calculated since 16 Jan 2017)
Total article views: 3,576 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,021
1,351
204
3,576
244
176
225
HTML: 2,021
PDF: 1,351
XML: 204
Total: 3,576
Supplement: 244
BibTeX: 176
EndNote: 225
Views and downloads (calculated since 23 May 2017)
Cumulative views and downloads
(calculated since 23 May 2017)
Total article views: 843 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
466
327
50
843
128
6
53
HTML: 466
PDF: 327
XML: 50
Total: 843
Supplement: 128
BibTeX: 6
EndNote: 53
Views and downloads (calculated since 16 Jan 2017)
Cumulative views and downloads
(calculated since 16 Jan 2017)
Viewed (geographical distribution)
Total article views: 4,419 (including HTML, PDF, and XML)
Thereof 4,305 with geography defined
and 114 with unknown origin.
Total article views: 3,576 (including HTML, PDF, and XML)
Thereof 3,445 with geography defined
and 131 with unknown origin.
Total article views: 843 (including HTML, PDF, and XML)
Thereof 843 with geography defined
and 0 with unknown origin.
In this manuscript, we present the results of our study conducted for a sediment core (ARC4-BN05) collected in the Arctic Ocean. Detailed examination of clay and bulk mineralogy along with grain size, content of Ca and Mn, and planktonic foraminiferal numbers in core ARC4–BN05 provides important new information about sedimentary environments and provenance. Based on these proxies, we try to reveal late to middle Pleistocene glacial history.
In this manuscript, we present the results of our study conducted for a sediment core...