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Mesozoic biostratigraphic, paleoenvironmental, and paleobiogeographic synthesis, equatorial Atlantic : Côte d'Ivoire-Ghana transform margin Eastern Equatorial Atlantic

Identifieur interne : 00CB58 ( Main/Exploration ); précédent : 00CB57; suivant : 00CB59

Mesozoic biostratigraphic, paleoenvironmental, and paleobiogeographic synthesis, equatorial Atlantic : Côte d'Ivoire-Ghana transform margin Eastern Equatorial Atlantic

Auteurs : M. Moullade [France] ; D. K. Watkins [États-Unis] ; F. E. Oboh-Ikuenobe [États-Unis] ; J.-P. Bellier [France] ; E. Masure [France] ; A. E. L. Holbourn [Allemagne] ; J. Erbacher [Allemagne] ; W. Kuhnt [Allemagne] ; T. Pletsch [Allemagne] ; M. A. Kaminski [Royaume-Uni] ; R. Rauscher [France] ; S. Shafik [Australie] ; O. Yepes [États-Unis] ; J. Dejax [France] ; J. M. Gregg [États-Unis] ; I. C. Shin [Corée du Sud] ; M. Schuler [France]

Source :

RBID : Pascal:00-0307082

Descripteurs français

English descriptors

Abstract

Cretaceous sediments from Ocean Drilling Program Leg 159 on the Cute d'Ivoire-Ghana Marginal Ridge (CIGMR), eastern equatorial Atlantic, are characterized by distinct stratigraphic changes in sedimentary facies associated with changes in the composition of the clayey and organic fractions, as well as of the calcareous nannofossil, radiolarian, foraminiferal, and palynomorph assemblages. In the absence of reliable magnetostratigraphic information, an integrated biostratigraphy provides the only means used to calibrate the geologic history of the Leg 159 area. The existence of marine depositional environments as early as the late Aptian to early Albian close to the Leg 159 drill sites puts constraints on the timing of the opening of the equatorial Atlantic gateway. Marine sedimentation on the ridge suggests that the West African and South American cratons were largely detached at this segment of the margin by the middle to late Albian During the Cenomanian to Coniacian the ridge appears to have remained in an elevated position with concurrent low deposition or condensation (Site 959), high carbonate debris accumulation (Site 960), and even erosion (Site 962). Total organic Carbon measurements and microfaunal data lead us to suggest that, following the early opening of the seaway during the Albian, circulation remained restricted in the fragmented sub-basins of the CIGMR. It probably was not until the Santonian that a deep-water connection and circulation system became established between the Central and the South Atlantic. The sedimentary and faunal record at Site 959 show that a rapid subsidence occurred during the Santonian, with sub-calcite compensation depth conditions maintained until and beyond the Cretaceous/Tertiary boundary.


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<s1>Centre de Géochimie de la Surface (CNRS), 1 rue Blessig</s1>
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<sZ>17 aut.</sZ>
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<s1>Department of Geology and Geophysics, University of Missouri-Rolla</s1>
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<country>États-Unis</country>
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<name sortKey="Dejax, J" sort="Dejax, J" uniqKey="Dejax J" first="J." last="Dejax">J. Dejax</name>
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<s1>Laboratoire de Paléontologie, Museum National d'Histoire Naturelle, 8 rue Buffon</s1>
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<country>France</country>
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<region type="region" nuts="2">Île-de-France</region>
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<name sortKey="Gregg, J M" sort="Gregg, J M" uniqKey="Gregg J" first="J. M." last="Gregg">J. M. Gregg</name>
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<s1>Department of Geology and Geophysics, University of Missouri-Rolla</s1>
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<country>États-Unis</country>
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</author>
<author>
<name sortKey="Shin, I C" sort="Shin, I C" uniqKey="Shin I" first="I. C." last="Shin">I. C. Shin</name>
<affiliation wicri:level="1">
<inist:fA14 i1="11">
<s1>Korea Ocean Research and Development Institute, Ansan, P.O. Box 29</s1>
<s2>Seoul 425-600</s2>
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<country>Corée du Sud</country>
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<settlement type="city">Séoul</settlement>
<region type="capital">Région capitale de Séoul</region>
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<name sortKey="Schuler, M" sort="Schuler, M" uniqKey="Schuler M" first="M." last="Schuler">M. Schuler</name>
<affiliation wicri:level="3">
<inist:fA14 i1="08">
<s1>Centre de Géochimie de la Surface (CNRS), 1 rue Blessig</s1>
<s2>67084 Strasbourg</s2>
<s3>FRA</s3>
<sZ>11 aut.</sZ>
<sZ>17 aut.</sZ>
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<country>France</country>
<placeName>
<region type="region" nuts="2">Grand Est</region>
<region type="old region" nuts="2">Alsace (région administrative)</region>
<settlement type="city">Strasbourg</settlement>
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</analytic>
<series>
<title level="j" type="main">Proceedings of the Ocean Drilling Program. Scientific results</title>
<title level="j" type="abbreviated">Proc. Ocean Drill. Program Sci. results</title>
<idno type="ISSN">0884-5891</idno>
<imprint>
<date when="1998">1998</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt>
<title level="j" type="main">Proceedings of the Ocean Drilling Program. Scientific results</title>
<title level="j" type="abbreviated">Proc. Ocean Drill. Program Sci. results</title>
<idno type="ISSN">0884-5891</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass>
<keywords scheme="KwdEn" xml:lang="en">
<term>Albian</term>
<term>Aptian</term>
<term>Cenomanian</term>
<term>Coniacian</term>
<term>Cretaceous</term>
<term>East Atlantic</term>
<term>Equatorial Atlantic</term>
<term>Ghana</term>
<term>Ivory Coast</term>
<term>Mesozoic</term>
<term>Ocean Drilling Program</term>
<term>active continental margins</term>
<term>biostratigraphy</term>
<term>chronostratigraphy</term>
<term>depositional environment</term>
<term>drilling</term>
<term>invertebrates</term>
<term>marine environment</term>
<term>marine sedimentation</term>
<term>paleobiogeography</term>
<term>paleoenvironment</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Ghana</term>
<term>Océan Atlantique Equatorial</term>
<term>Océan Atlantique Est</term>
<term>Côte d'Ivoire</term>
<term>Marge continentale active</term>
<term>Mésozoïque</term>
<term>Crétacé</term>
<term>Forage</term>
<term>ODP</term>
<term>Biostratigraphie</term>
<term>Milieu sédimentation</term>
<term>Aptien</term>
<term>Milieu marin</term>
<term>Sédimentation marine</term>
<term>Albien</term>
<term>Cénomanien</term>
<term>Coniacien</term>
<term>Paléobiogéographie</term>
<term>Chronostratigraphie</term>
<term>Paléoenvironnement</term>
<term>Faune invertébré</term>
<term>ODP Leg 159</term>
</keywords>
<keywords scheme="Wicri" type="geographic" xml:lang="fr">
<term>Ghana</term>
<term>Côte d'Ivoire</term>
</keywords>
<keywords scheme="Wicri" type="topic" xml:lang="fr">
<term>Forage</term>
<term>Milieu marin</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front>
<div type="abstract" xml:lang="en">Cretaceous sediments from Ocean Drilling Program Leg 159 on the Cute d'Ivoire-Ghana Marginal Ridge (CIGMR), eastern equatorial Atlantic, are characterized by distinct stratigraphic changes in sedimentary facies associated with changes in the composition of the clayey and organic fractions, as well as of the calcareous nannofossil, radiolarian, foraminiferal, and palynomorph assemblages. In the absence of reliable magnetostratigraphic information, an integrated biostratigraphy provides the only means used to calibrate the geologic history of the Leg 159 area. The existence of marine depositional environments as early as the late Aptian to early Albian close to the Leg 159 drill sites puts constraints on the timing of the opening of the equatorial Atlantic gateway. Marine sedimentation on the ridge suggests that the West African and South American cratons were largely detached at this segment of the margin by the middle to late Albian During the Cenomanian to Coniacian the ridge appears to have remained in an elevated position with concurrent low deposition or condensation (Site 959), high carbonate debris accumulation (Site 960), and even erosion (Site 962). Total organic Carbon measurements and microfaunal data lead us to suggest that, following the early opening of the seaway during the Albian, circulation remained restricted in the fragmented sub-basins of the CIGMR. It probably was not until the Santonian that a deep-water connection and circulation system became established between the Central and the South Atlantic. The sedimentary and faunal record at Site 959 show that a rapid subsidence occurred during the Santonian, with sub-calcite compensation depth conditions maintained until and beyond the Cretaceous/Tertiary boundary.</div>
</front>
</TEI>
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<list>
<country>
<li>Allemagne</li>
<li>Australie</li>
<li>Corée du Sud</li>
<li>France</li>
<li>Royaume-Uni</li>
<li>États-Unis</li>
</country>
<region>
<li>Alsace (région administrative)</li>
<li>Angleterre</li>
<li>Bade-Wurtemberg</li>
<li>District de Tübingen</li>
<li>Grand Est</li>
<li>Grand Londres</li>
<li>Provence-Alpes-Côte d'Azur</li>
<li>Région capitale de Séoul</li>
<li>Schleswig-Holstein</li>
<li>Île-de-France</li>
</region>
<settlement>
<li>Kiel</li>
<li>Londres</li>
<li>Nice</li>
<li>Paris</li>
<li>Strasbourg</li>
<li>Séoul</li>
<li>Tübingen</li>
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<li>University College de Londres</li>
<li>Université Pierre-et-Marie-Curie</li>
</orgName>
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<name sortKey="Masure, E" sort="Masure, E" uniqKey="Masure E" first="E." last="Masure">E. Masure</name>
<name sortKey="Rauscher, R" sort="Rauscher, R" uniqKey="Rauscher R" first="R." last="Rauscher">R. Rauscher</name>
<name sortKey="Schuler, M" sort="Schuler, M" uniqKey="Schuler M" first="M." last="Schuler">M. Schuler</name>
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<name sortKey="Gregg, J M" sort="Gregg, J M" uniqKey="Gregg J" first="J. M." last="Gregg">J. M. Gregg</name>
<name sortKey="Oboh Ikuenobe, F E" sort="Oboh Ikuenobe, F E" uniqKey="Oboh Ikuenobe F" first="F. E." last="Oboh-Ikuenobe">F. E. Oboh-Ikuenobe</name>
<name sortKey="Yepes, O" sort="Yepes, O" uniqKey="Yepes O" first="O." last="Yepes">O. Yepes</name>
</country>
<country name="Allemagne">
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<name sortKey="Holbourn, A E L" sort="Holbourn, A E L" uniqKey="Holbourn A" first="A. E. L." last="Holbourn">A. E. L. Holbourn</name>
</region>
<name sortKey="Erbacher, J" sort="Erbacher, J" uniqKey="Erbacher J" first="J." last="Erbacher">J. Erbacher</name>
<name sortKey="Kuhnt, W" sort="Kuhnt, W" uniqKey="Kuhnt W" first="W." last="Kuhnt">W. Kuhnt</name>
<name sortKey="Pletsch, T" sort="Pletsch, T" uniqKey="Pletsch T" first="T." last="Pletsch">T. Pletsch</name>
</country>
<country name="Royaume-Uni">
<region name="Angleterre">
<name sortKey="Kaminski, M A" sort="Kaminski, M A" uniqKey="Kaminski M" first="M. A." last="Kaminski">M. A. Kaminski</name>
</region>
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<name sortKey="Shafik, S" sort="Shafik, S" uniqKey="Shafik S" first="S." last="Shafik">S. Shafik</name>
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<name sortKey="Shin, I C" sort="Shin, I C" uniqKey="Shin I" first="I. C." last="Shin">I. C. Shin</name>
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