Radiogenic isotopic and clay mineralogical signatures of terrigenous particles as water-mass tracers: New insights into South Atlantic deep circulation during the last termination

QUATERNARY SCIENCE REVIEWS

卷:228

Review

Beny, F.^1,2  Bout-Roumazeilles, V.¹  Davies, G. R.²  Waelbroeck, C.³  Bory, A.¹  Tribovillard, N.¹  Delattre, M.¹  Abraham, R.¹ 

[1] Univ Lille, Lab Oceanol & Geosci, ULCO, CNRS,UMR 8187, F-59655 Villeneuve Dascq, France

[2] Vrije Univ Amsterdam, Dept Earth Sci, Fac Sci, Boelelaan 1085, NL-1081 HV Amsterdam, Netherlands

[3] CEA CNRS UVSQ, UMR 8212, Lab Sci Climat & Environm, LSCE IPSL, Site Orme Merisiers, F-91191 Gif Sur Yvette, France

关键词: Last deglaciation;    Paleoceanography;    Southern Ocean;    South Atlantic;    Radiogenic isotopes;    Clay mineralogy;    Grain size distribution;   

DOI  :  10.1016/j.quascirev.2019.106089

来源: Elsevier

【 摘 要 】

The past evolution of the Southern Ocean, one of the major components of the climatic system, is still a matter of debate. This study provides new insights into the deep Southern Ocean circulation based on the radiogenic isotopes and clay mineralogical signature of the terrigenous fractions transported by the main deep water masses to sediments recovered in core MD07-3076Q from the central South Atlantic. This approach successfully permits: (1) provenance identification of the various grain-size fractions (clay, cohesive silt and sortable silt); (2) assignment of each grain-size fraction to a specific water-mass; (3) reconstruction of past changes in the main deep water-mass pathways. These data document the evolution of deep-water masses in the South Atlantic Ocean during the last deglaciation. The Antarctic Bottom Water (AABW) speed and northward extension were maximum at the end of the Last Glacial Maximum (LGM), associated with strong bottom water production in the Weddell Sea, together with a vigorous Lower Circumpolar Deep Water (LCDW). In contrast the North Atlantic Deep Water (NADW) circulation was weaker than today. The onset of the deglaciation (from 17.5 ka to 15 ka, -Heinrich Stadial 1, HS 1) was marked by weakening and southerly retreat of the AABW and by an increase of mixing between AABW and LCDW. The speed of the AABW remained at its lowest during the Belling Allerod (B/A) and the Younger Dryas (YD), and the LCDW slowed and retreated to the south, while the NADW progressively migrated southward, deepened, and strengthened between the beginning of the Balling Altered and the Holocene (from similar to 15 to 10 ka). (C) 2019 Elsevier Ltd. All rights reserved.

【 授权许可】

Free