Articles | Volume 13, issue 8
https://doi.org/10.5194/cp-13-1063-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-1063-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Centennial to millennial climate variability in the far northwestern Pacific (off Kamchatka) and its linkage to the East Asian monsoon and North Atlantic from the Last Glacial Maximum to the early Holocene
Sergey A. Gorbarenko
CORRESPONDING AUTHOR
V.I. Il'ichev Pacific Oceanological Institute, Vladivostok, Russia
Xuefa Shi
Key Laboratory of Marine Sedimentology and Environmental Geology, First
Institute of Oceanography, SOA, Qingdao, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine
Science and Technology, Qingdao, China
Galina Yu. Malakhova
North-East Interdisciplinary Science Research Institute FEB RAS, Magadan, Russia
Aleksandr A. Bosin
V.I. Il'ichev Pacific Oceanological Institute, Vladivostok, Russia
Jianjun Zou
Key Laboratory of Marine Sedimentology and Environmental Geology, First
Institute of Oceanography, SOA, Qingdao, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine
Science and Technology, Qingdao, China
Yanguang Liu
Key Laboratory of Marine Sedimentology and Environmental Geology, First
Institute of Oceanography, SOA, Qingdao, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine
Science and Technology, Qingdao, China
Min-Te Chen
National Taiwan Ocean University, Keelung, Taiwan
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We reconstructed sea ice and organic carbon composition variabilities based on biomarkers and carbon stable isotopes in the northern Chukchi Sea, western Arctic Ocean, over the past 200 years. Under permanent ice cover, organic carbon was dominated by land sources transported by sea ice and ocean currents, while local primary productivity was suppressed by light limitation. Since ice retreated in 20th century, organic carbon from primary production gradually overtook the terrestrial component.
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Large-scale reorganization of global ocean circulation has been documented in a variety of marine archives, including the enhanced North Pacific Intermediate Water NPIW. Our data support both the model- and data-based ideas that the enhanced NPIW mainly developed during cold spells, while an expansion of oxygen-poor zones occurred at warming intervals (Bölling-Alleröd).
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1. We have reconstructed new meridional thermal and precipitation stacked records in the Indo-Pacific Warm Pool (IPWP) during the last termination.
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I. Hessler, S. P. Harrison, M. Kucera, C. Waelbroeck, M.-T. Chen, C. Anderson, A. de Vernal, B. Fréchette, A. Cloke-Hayes, G. Leduc, and L. Londeix
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M. Yamamoto, H. Sai, M.-T. Chen, and M. Zhao
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