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Hurricanes and climate in the Caribbean during the past 3700 years BP

Bibliographic Data

ID12267796
AuthorsBruno Malaizé (0000-0002-5571-9990, Environnements et Paléoenvironnements Océaniques et Continentaux, corresponding author), P Bertran (INRAP, Pessac, France), Pierre Carbonel (Université de Bordeaux), Dominique Bonnissent (0000-0002-0006-6267, Laboratoire Méditerranéen de Préhistoire Europe Afrique), Karine Charlier (Université de Bordeaux), Didier Galop (0000-0003-1746-4760, Université Toulouse - Jean Jaurès), D Imbert (Université Antilles-Guyane, France), Nathalie Serrand (0000-0001-6283-5183, Institut national de recherches archéologiques préventives), Christian Stouvenot (0000-0003-2498-5310, Archéologie et Archéométrie), Ch Stouvenot (Service Régional de l’Archéologie, France), C Pujol (EPOC, Université de Bordeaux 1, France)
Year2011
Volume21
Issue6
Pages911-924
Publication date2011-04-20
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683611400198
OpenAlexW1964045784
LanguageEN
Citations received16
References cited37

A multiproxy analysis of lacustrine sediments cored in Grand-Case Pond at Saint-Martin, north of the Lesser Antilles archipelago, reveals three distinct climatic periods for the last 3700 years. From 3700 to ~2500 yr cal. BP and from 1150 yr cal. BP to the present, carbonate mud deposition occurred in connection with pond lowstands. These periods were also punctuated by severe drought events, marked by gypsum laminae, and hurricane landfalls, leading to marine sand inputs into the pond. The intermediate time interval, from 2500 to 1150 yr cal. BP, is typified by black organic mud deposition, suggesting that hypoxic to anoxic conditions prevailed at the pond bottom. These were probably linked with a perennial pond highstand and reflect more uniform and wetter climatic conditions than today. The carbon isotopic composition of the ostracod Perissocytheridea bisulcata shows that the lowest δ 13 C values are recorded during the hypoxic periods, as a consequence of bacterial recycling of isotopically depleted organic matter. Such a climatic history agrees closely with that documented from other records in the Caribbean area, such as the Cariaco Basin, central coast of Belize or Barbados. By constrast, discrepancies seem to emerge from the comparison between hurricane activity recorded at Saint-Martin on the one hand and Vieques (Puerto Rico) on the other hand. We explain this apparent contradiction by a balance between two distinct storm paths in response to latitudinal shifts of the Intertropical Convergence Zone (ITCZ). Stronger storm activity over the Gulf coast and the inner Caribbean Sea is favoured by a southern position of the ITCZ in connection with dry climatic conditions. Plausible links with the North Atlantic Oscillation (NAO) are also suggested

Archipelago · Climate change · Geography · Intertropical Convergence Zone · Paleoclimatology · Precipitation · Storm · Geological formations and processes · Geology and Paleoclimatology Research · Tropical and Extratropical Cyclones Research · Geology · Oceanography

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Citations per year1.14
Citation span2012 - 2022 (11)
Highly citedNo

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