Phase lag between Intertropical Convergence Zone migration and subtropical monsoon onset over the northwestern Indian Ocean during Marine Isotopic Substage 6.5 (MIS 6.5)
| Type | Article | ||||||||
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| Date | 2006-12 | ||||||||
| Language | English | ||||||||
| Author(s) | Malaize B.1, Joly C.1, Venec-Peyre M. -T.2, 3, 4, Bassinot F.5, Caillon N.5, Charlier K.1 | ||||||||
| Affiliation(s) | 1 : Univ Bordeaux 1, CNRS, DGO UMR 5805, EPOC, F-33405 Talence, France. 2 : CNRS, UMR 5143, F-75005 Paris, France. 3 : MNHN, UMR 5143, F-75005 Paris, France. 4 : Univ Paris 06, UMR 5143, F-75005 Paris, France. 5 : CEA, CNRS, CFR, Lab Sci Climat & Environm, F-91198 Gif Sur Yvette, France. |
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| Source | Geochemistry Geophysics Geosystems (1525-2027) (Amer Geophysical Union), 2006-12 , Vol. 7 , N. 12/ Q12N08 , P. 1-16 | ||||||||
| DOI | 10.1029/2006GC001353 | ||||||||
| WOS© Times Cited | 8 | ||||||||
| Keyword(s) | paleoclimatology, foraminifera, isotopes, Indian monsoon, ITCZ, sapropels, upwelling | ||||||||
| Abstract | High-resolution faunal and isotopic analyses of foraminifera were performed on core MD96-2073 (10 degrees 94'N, 52 degrees 62'E, 3142 m depth), located close to Socotra Island in the upwelling area of the Somali Basin ( NW Indian Ocean). This work focuses on Marine Isotopic Stage 6.5 in order to reconstruct paleo-upwelling changes and their links with the Arabian Sea summer monsoon and the migration of the Intertropical Convergence Zone (ITCZ). Correspondence and cluster analyses of planktonic foraminiferal abundances, partly controlled by temperature and water mass productivity, together with an upwelling intensification index, show the occurrence of a strong upwelling between 176 and 165 ka. This upwelling intensification responds to a northward migration of the ITCZ. An isotopic depletion in the planktonic foraminifera delta(18)O records occurring between 180 and 167 ka is interpreted as proof of a large salinity decrease in the surface waters, probably linked to a strong input of fresh rainfall waters induced by an intense monsoon activity. The lag between the onset of upwelling intensification and the strong monsoonal impact over the same area suggests a decoupling between both phenomena. The migration of the ITCZ is influenced by obliquity and precessional forcing, while the Arabian Sea summer monsoon precipitation depends only on precessional forcing. | ||||||||
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