Middle to Late Pleistocene Arctic paleoceanographic changes based on sedimentary records from Mendeleev Ridge and Makarov Basin

QUATERNARY SCIENCE REVIEWS

卷:228

Review

Xiao, Wenshen^1,2  Polyak, Leonid³  Wang, Rujian^1,2  Lowemark, Ludvig⁴  Mei, Jing¹  You, Defang¹  Wang, Weiguo⁵  Wu, Li¹  Jin, Xiaobo¹ 

[1] Tongji Univ, State Key Lab Marine Geol, Shanghai 200092, Peoples R China

[2] Univ Corp Polar Res, Beijing 100875, Peoples R China

[3] Ohio State Univ, Byrd Polar & Climate Res Ctr, Columbus, OH 43210 USA

[4] Natl Taiwan Univ, Dept Geosci, POB 13-318, Taipei 106, Taiwan

[5] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China

关键词: Arctic Ocean;    Mendeleev Ridge;    Quaternary stratigraphy;    Sedimentary proxies;    Glaciations;    Interglacials;    Paleocirculation;    Orbital cyclicity;   

DOI  :  10.1016/j.quascirev.2019.106105

来源: Elsevier

【 摘 要 】

Three sediment cores from the Makarov Basin and Mendeleev Ridge off the Siberian margin were analyzed for a number of litho-, bio- and magnetostratigraphic proxies. Correlation to previously studied Arctic records from Mendeleev to Lomonosov ridges enables paleoceanographic reconstructions for the Middle to Late Pleistocene (estimated similar to 0.8 Ma) on orbital time scales. Cyclic changes in lithology corroborated by multiple stratigraphic constraints were tuned to global climate variations based on the manganese content that increases during interglacials, while calcium and zircon were used as proxies for the Laurentide and Eurasian ice sheet inputs. The combined evaluation of glacial and interglacial proxy variabilities provides a coherent picture of the western Arctic Ocean development in the Pleistocene. We suggest that major cyclic changes were driven by summer processes, such as sea-ice retreat and enhanced biological production vs. suppressed ice melt in warmer and colder summers, respectively. A potential link to low latitudes via atmospheric moisture and heat transport is indicated by similarities in the western Arctic Ocean and East Asian monsoon records. Long-term cooling is signified by biogenic proxies related to sea-ice expansion over the western Arctic Ocean with step changes at MIS 11 and 7 (similar to 0.4 and 0.2-0.3 Ma). This transition also features better fossil preservation indicating less corrosive/oxidative bottom waters, probably resulting from a decrease in organic export production and/or weakening of bottom water ventilation under perennial sea ice. The latter was possibly enhanced by atmospheric cooling and increased meltwater fluxes with the growth of circum-Arctic ice sheets. (C) 2019 Elsevier Ltd. All rights reserved.

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