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<title lang=en>Sedimentology, palaeoenvironments and biostratigraphy of the Pliocene-Pleistocene carbonate platform of Grande-Terre (Guadeloupe, Lesser Antilles forearc)</title>
<creator>Cornee, Jean-Jacques</creator>
<creator>Leticee, Jean-Len</creator>
<creator>Munch, Philippe</creator>
<creator>Quillevere, Frederic</creator>
<creator>Lebrun, Jean-Frédéric</creator>
<creator>Moissette, Pierre</creator>
<creator>Braga, Juan-Carlos</creator>
<creator>Melinte-Dobrinescu, Mihaela</creator>
<creator>DE MIN, Lyvane</creator>
<creator>Oudet, Julien</creator>
<creator>Randrianasolo, Auran</creator>
<contributor>Bassins ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Dynamique de la Lithosphere ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE) ; Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Université Claude Bernard Lyon 1 (UCBL) - École normale supérieure - Lyon (ENS Lyon)</contributor>
<contributor>Universidad de Granada (UGR)</contributor>
<contributor>GeoEcoMar, Bucarest ; Université du Québec</contributor>
<description>International audience</description>
<source>ISSN: 1469-3496</source>
<source>EISSN: 1365-3091</source>
<source>Sedimentology</source>
<publisher>Blackwell Publishing</publisher>
<identifier>hal-00760906</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00760906</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00760906</source>
<source>Sedimentology, Blackwell Publishing, 2012, 59 (5), pp.1426-1451. 〈10.1111/j.1365-3091.2011.01311.x〉</source>
<identifier>DOI : 10.1111/j.1365-3091.2011.01311.x</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/j.1365-3091.2011.01311.x</relation>
<language>en</language>
<subject lang=en>Caribbean</subject>
<subject lang=en>Early Quaternary</subject>
<subject lang=en>Late Neogene</subject>
<subject lang=en>sea-level changes</subject>
<subject lang=en>tectonics</subject>
<subject lang=en>tropical carbonates</subject>
<subject>[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Pliocene and Pleistocene deposits from Grande-Terre (Guadeloupe archipelago, French Lesser Antilles) provide a remarkable example of an isolated carbonate system built in an active margin setting, with sedimentation both controlled by rapid sea-level changes and tectonic movements. Based on new field, sedimentological and palaeontological analyses, these deposits have been organized into four sedimentary sequences (S1 to S4) separated by three subaerial erosion surfaces (SB0, SB1 and SB2). Sequences S1 and S2 ('Calcaires inférieurs à rhodolithes') deposited during the late Zanclean to early Gelasian (planktonic foraminiferal Zones PL2 to PL5) in low subsidence conditions, on a distally steepened ramp dipping eastward. Red algal-rich deposits, which dominate the western part of Grande-Terre, change to planktonic foraminifer-rich deposits eastward. Vertical movements of tens of metres were responsible for the formation of SB0 and SB1. Sequence S3 ('Formation volcano-sédimentaire', 'Calcaires supérieurs à rhodolithes' and 'Calcaires à Agaricia') was deposited during the late Piacenzian to early Calabrian (Zones PL5 to PT1a) on a distally steepened, red algal-dominated ramp that changes upward into a homoclinal, coral-dominated ramp. Deposition of Sequence S3 occurred during a eustatic cycle in quiet tectonic conditions. Its uppermost boundary, the major erosion surface SB2, is related to the Cala1 eustatic sea-level fall. Finally, Sequence S4 ('Calcaires à Acropora') probably formed during the Calabrian, developing as a coral-dominated platform during a eustatic cycle in quiet tectonic conditions. The final emergence of the island could then have occurred in late Calabrian times.</description>
<date>2012-08</date>
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