Geochemical evidence for intermediate water circulation in the westernmost Mediterranean over the last 20 </ce:hsp>kyr </ce:hsp>BP and its impact on the Mediterranean Outflow

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-Espejo^a ; ^{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-Ruiz^b ; A. Garcí ; a-Alix^c ; ^{Antonio.Garcia-AlixDaroca@glasgow.ac.uk" class="auth_mail" title="E-mail the corresponding author} ; T. van de Flierdt^d ; ^{tina.vandeflierdt@imperial.ac.uk" class="auth_mail" title="E-mail the corresponding author} ; Takashi Toyofuku^e ; ^{toyofuku@jamstec.go.jp" class="auth_mail" title="E-mail the corresponding author} ; Andre Bahr^f ; ^{andre.bahr@geow.uni-heidelberg.de" class="auth_mail" title="E-mail the corresponding author} ; Katharina Kreissig^d ; ^{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

class="label">•: We interpreted a MOW middle/upper branch influenced by LIW evolution.
class="label">•: MOW depth and lower core were linked to WMDW and North climate realm.
class="label">•: A multi-branch MOW could preserve monsoonal and high latitude climate signals.