Bingbin Qin
Ontario Ministry of Natural Resources
15 Papers
12 Citations
Bingbin Qin is an academic researcher from Ontario Ministry of Natural Resources. The author has contributed to research in topics: Geology & Climatology. The author has an hindex of 4, co-authored 6 publications. Previous affiliations of Bingbin Qin include Chinese Academy of Sciences & State Oceanic Administration.
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Papers
Hydrological variability in the western tropical Pacific over the past 700 kyr and its linkage to Northern Hemisphere climatic change
Qi Jia,Tiegang Li,Tiegang Li,Zhifang Xiong,Stephan Steinke,Fuqing Jiang,Fengming Chang,Bingbin Qin +7 more
TL;DR: In this paper, the role of ENSO and ITCZ shifts on the hydroclimate in the western tropical Pacific (WTP) and their linkage to Northern Hemisphere climate change on glacial-interglacial timescales was investigated.
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Calcification of planktonic foraminifer Pulleniatina obliquiloculata controlled by seawater temperature rather than ocean acidification
TL;DR: In this article, the authors investigated the effects of different environmental influences on calcification of the planktonic foraminifer Pulleniatina obliquiloculata.
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An Improved Protocol For Cleaning of Planktonic Foraminifera For Shell Weight Measurement
TL;DR: Foraminiferal shells must be cleaned prior to weight measurements in order to remove detritus trapped within the shell chambers as discussed by the authors, which can be used as a proxy to reconstruct seawater [CO32-] in the past and, therefore, to provide clues regarding the ocean carbon cycle.
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Thermocline dynamics in the northwestern tropical Pacific over the past 700 kyr
Qi Jia,Tiegang Li,Zhifang Xiong,Stephan Steinke,Thomas J. Algeo,Thomas J. Algeo,Fuqing Jiang,Fengming Chang,Bingbin Qin +8 more
TL;DR: In this paper, the authors reported thermocline variations at Site MD06-3047-B in the western Philippine Sea over the last 700 kyr, showing that variations in thermoclines temperature and salinity in the study area were correlated with changes in Earth's obliquity, with warmer and saltier (colder and fresher) waters corresponding to high (low) Earth-axial oblivity.
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