Impact de la trangression holocene sur la sedimentation dans le detroit de Makassar (Indonesie)

Autre(s) titre(s) Impact of the Holocene transgression on the Quaternary sedimentation in the Makassar Strait (Indonesia)
Type Article
Date 1990
Langue(s) Français
Auteur(s) Gayet J, Carbonel P, Duprat J, Labeyrie L, Faugeres J-C, Gonthier E, Moyes J
Conférence Actes du Colloque Tour du monde Jean Charcot , Paris (France), 2-3 Mar 1989
Source Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1990
Résumé en anglais Biomarker data associated with isotopic curve partial differential super(18)O served to establish a stratigraphic scale and thereby a chronology of fluctuations in the circulation and sedimentation of the Kalimantan continental rise throughout the last climatic cycle. During the glacial maximum, period of low sea-level sediments were deposited by turbidity currents originating from Kalimantan. During deglaciation, during rise of the sea-level and more particularly in the Holocene, material issued from Kalimantan either contributed to the building of the Mahakam delta or was dispersed over the shelf. Sulawesi inputs, less abundant and mineralogically different from Kalimantan material, were observed onto the Kalimantan rise. During this same period, circulation in the Makassar strait slowed down progressively while stratification became more marked and practically permanent in the Holocene.
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Gayet J, Carbonel P, Duprat J, Labeyrie L, Faugeres J-C, Gonthier E, Moyes J (1990). Impact de la trangression holocene sur la sedimentation dans le detroit de Makassar (Indonesie). Oceanologica Acta, Special issue Open Access version : https://archimer.ifremer.fr/doc/00268/37898/