Geochemical evidence for intermediate water circulation in the westernmost Mediterranean over the last 20 kyr BP and its impact on the Mediterranean Outflow
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- 作者：F.J. Jimé ; nez-Espejoa ; fjjspejo@jamstec.go.jp" class="auth_mail" title="E-mail the corresponding author ; M. Pardos-Gené ; b ; mpardos@iact.ugr-csic.es" class="auth_mail" title="E-mail the corresponding author ; F. Martí ; nez-Ruizb ; A. Garcí ; a-Alixc ; Antonio.Garcia-AlixDaroca@glasgow.ac.uk" class="auth_mail" title="E-mail the corresponding author ; T. van de Flierdtd ; tina.vandeflierdt@imperial.ac.uk" class="auth_mail" title="E-mail the corresponding author ; Takashi Toyofukue ; toyofuku@jamstec.go.jp" class="auth_mail" title="E-mail the corresponding author ; Andre Bahrf ; andre.bahr@geow.uni-heidelberg.de" class="auth_mail" title="E-mail the corresponding author ; Katharina Kreissigd ; k.kreissig@imperial.ac.uk" class="auth_mail" title="E-mail the corresponding author
- 关键词：Alboran basin ; Levantine Intermediate Water ; Last Glacial cycle ; Nd isotopes ; Redox conditions ; Mediterranean Outflow
- 刊名：Global and Planetary Change
- 出版年：2015
- 出版时间：December 2015
- 年：2015
- 卷：135
- 期：Complete
- 页码：38-46
- 全文大小：1070 K
文摘
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We interpreted a MOW middle/upper branch influenced by LIW evolution.
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MOW depth and lower core were linked to WMDW and North climate realm.
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A multi-branch MOW could preserve monsoonal and high latitude climate signals.