Antarctic Intermediate Water penetration into the Northern Indian Ocean during the last deglaciation
Autor: | Christophe Colin, Arnaud Dapoigny, Zhaojie Yu, F. Bassinot, Shiming Wan, Qiong Wu, Laure Meynadier, Ruifang Ma, Nejib Kallel, Sophie Sépulcre |
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Přispěvatelé: | Géosciences Paris Sud (GEOPS), Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS), Key Laboratory of Marine Geology and Environment [China, Institute of Oceanology [China], Center for Ocean Mega-Science, Chinese Academy of Sciences, Institut de Physique du Globe de Paris (IPGP), Centre National de la Recherche Scientifique (CNRS)-Université de La Réunion (UR)-Université Paris Diderot - Paris 7 (UPD7)-IPG PARIS-Institut national des sciences de l'Univers (INSU - CNRS), College of Oceanography, Hohai University, Unité GEOGLOB, Faculté des Sciences de Sfax, Université de Sfax - University of Sfax-Université de Sfax - University of Sfax, Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Géochrononologie Traceurs Archéométrie (GEOTRAC), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Paléocéanographie (PALEOCEAN), This work was supported by the National Natural Science Foundation of China (41622603 and 41576034), National Programme on Global Change and Air–Sea Interaction (GASI-GEOGE-03), Innovation Project (2016ASKJ13) and Aoshan Talents programme (2017ASTCP-ES01) of Qingdao National Laboratory for Marine Science and Technology and CAS Interdisciplinary Innovation Team, Open Fund of the Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences (No. MGE2018KG01). Z. Yu acknowledges the China Scholarship Council for providing funding for his study in France. This study was supported by the Labex L-IPSL and the MONOPOL projects, which are funded by the ANR (grant nos. ANR-10-LABX-0018 and ANR 2011 Blanc SIMI 5-6 024 04), ANR-10-LABX-0018,L-IPSL,LabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes(2010), ANR-11-BS56-0024,MONOPOL,Paléo-variabilité de la mousson indienne(2011), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Université Paris-Saclay-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS), ANR-10-LABX-0018/10-LABX-0018,L-IPSL,LabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes(2010) |
Jazyk: | angličtina |
Rok vydání: | 2018 |
Předmět: |
010504 meteorology & atmospheric sciences
Climate change [SDU.STU]Sciences of the Universe [physics]/Earth Sciences 010502 geochemistry & geophysics 01 natural sciences Panoply law.invention Foraminifera Geochemistry and Petrology law Earth and Planetary Sciences (miscellaneous) Deglaciation 14. Life underwater Radiocarbon dating 0105 earth and related environmental sciences Carbon dioxide in Earth's atmosphere Antarctic Intermediate Water biology Northern Hemisphere biology.organism_classification Geophysics Oceanography 13. Climate action Space and Planetary Science [SDU]Sciences of the Universe [physics] Upwelling Geology |
Zdroj: | Earth and Planetary Science Letters Earth and Planetary Science Letters, Elsevier, 2018, 500, pp.67-75. ⟨10.1016/j.epsl.2018.08.006⟩ Earth and Planetary Science Letters, 2018, 500, pp.67-75. ⟨10.1016/j.epsl.2018.08.006⟩ |
ISSN: | 0012-821X |
DOI: | 10.1016/j.epsl.2018.08.006⟩ |
Popis: | The two-stage increase in atmospheric carbon dioxide (CO2), and the associated decrease in radiocarbon (14C) during the last deglaciation, are thought to have been linked to enhanced Southern Ocean upwelling and the rapid release of sequestered 14C-depleted CO2. Antarctic Intermediate Water (AAIW), originating from the Southern Ocean, reflects variations in the Southern Ocean and, crucially, mirrors the chemical signature of upwelling deep water. However, the penetration of AAIW into the Northern Indian Ocean and its relationship with deglacial climate changes have not been thoroughly elucidated to date. Here, we present the neodymium isotopic composition ( e Nd ) of mixed planktonic foraminifera from core MD77-176 from an intermediate depth in the Northern Indian Ocean to reconstruct the past evolution of intermediate water during deglaciation. The e Nd record in the Northern Indian Ocean displays two pulse-like shifts towards more radiogenic Southern Ocean values during the deglaciation, and these shifts coincide with excursions in Δ 14 C and e Nd records in the Pacific and Atlantic Oceans. These results suggest invasion of AAIW into the Northern Hemisphere oceans associated with enhanced Southern Ocean ventilation during deglaciation. Our new e Nd record strongly supports the close linkage of AAIW propagation and atmospheric CO2 rise through Southern Ocean ventilation during deglaciation. |
Databáze: | OpenAIRE |
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