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Calculation of the reservoir age from organic and carbonate fractions of sediments in the Gulf of Cariaco (Caribbean Sea)

Authors :
Christian Crouzet
Franck Audemard
Corina Campos
Iliana Aguilar
Pierre Sabatier
Christian Beck
Franco Urbani
Fundación Venezolana de Investigaciones Sismológicas (FUNVISIS)
FUNVISIS
Environnements, Dynamiques et Territoires de la Montagne (EDYTEM)
Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)
Institut des Sciences de la Terre (ISTerre)
Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement [IRD] : UR219-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019])
Source :
Quaternary Geochronology, Quaternary Geochronology, Elsevier, 2017, 38, pp.50-60. ⟨10.1016/j.quageo.2017.01.001⟩
Publication Year :
2017
Publisher :
Elsevier BV, 2017.

Abstract

International audience; A set of 24 AMS 14C measurements were performed on different sediment fractions from short gravity cores taken from the Gulf of Cariaco (northeastern Venezuela) in order to construct a detailed sedimentary archive for recent centuries. A local reservoir effect was expected because of i) strong upwelling from the neighboring Cariaco Trough and anoxia and ii) the specific geomorphological setting related to active faults with seeps and diapirism. Measurements were thus performed on different components: sediment bulk organic fraction (SBOF), pteropods shells (surface water), bivalve shells (bottom), and plant fragments. Based on comparisons of the different results, we discuss different age corrections and calibrations, which lead us to consider a negligible local reservoir correction (ΔR) for the bivalve and pteropod shells, which show no reservoir age for carbonate and an absence of water stratification. However, a local 633 ± 64 yr ΔR appears in the organic fraction of the sediment, and its origin is primary related to the upwelling mechanism

Details

ISSN :
18711014
Volume :
38
Database :
OpenAIRE
Journal :
Quaternary Geochronology
Accession number :
edsair.doi.dedup.....1e5c3f4c2b2934f393c00cccf3609178
Full Text :
https://doi.org/10.1016/j.quageo.2017.01.001