Sealevel history recorded in the Pleistocene carbonate sequence in IODP Hole 310‐M0005D, off Tahiti
Identifieur interne : 007187 ( Main/Exploration ); précédent : 007186; suivant : 007188Sealevel history recorded in the Pleistocene carbonate sequence in IODP Hole 310‐M0005D, off Tahiti
Auteurs : Yasufumi Iryu [Japon] ; Yasunari Takahashi [Japon] ; Kazuhiko Fujita [Japon] ; Gilbert Camoin [France] ; Guy Cabioch [France] ; Hiroki Matsuda [Japon] ; Tokiyuki Sato [Japon] ; Kaoru Sugihara [Japon] ; Jody M. Webster [Australie] ; Hildegard Westphal [Allemagne]Source :
- Island Arc [ 1038-4871 ] ; 2010-12.
Descripteurs français
- Wicri :
- topic : Algue.
English descriptors
- KwdEn :
- Acropora, Adey, Agariciids, Algae, Algal, Assemblage, Baba, Bioclastic, Bioclastic packstone, Bioclasts, Blackwell publishing asia, Boykins, Bryozoan, Camoin, Carbonate, Coral, Coral clasts, Coral fragments, Coral framestone, Coralgal, Coralgal framestone, Coralline, Coralline algae, Deglacial, Deglaciation, Diagenetically, Echinoids, Encrusting, Encrusting agariciids, Encrusting foraminifers, Encrusting forms, Encrusting montipora, Foraminifer, Forereef, Forereef rhodoliths, Foslie, Fossil, Framestone, French polynesia, Geniculate, Geniculate coralline algae, Grainstone, Halimeda, Hermatypic corals, Hydrolithon, Hydrolithon onkodes, Insipidum, Iodp, Iodp expedition, Iryu, Keats, Larger foraminifers, Limestone, Lithophyllum, Lithophyllum insipidum adey, Lower interval, Matrix, Mbsf, Mesophyllum, Microbialite, Mollusk, Montaggioni, Montipora, Myriocarpum, Neogoniolithon, Nongeniculate, Nongeniculate coralline algae, Nongeniculate coralline algal assemblages, Oatstone, Ocean drilling program, Older pleistocene sequence, Onkodes, Packstone, Penultimate, Penultimate deglaciation, Pleistocene, Pleistocene sealevel history, Pneophyllum conicum, Pocillopora, Porites, Rhodolith, Rhodoliths, Robust, Ryukyu, Ryukyu group, Ryukyu islands, Sealevel, Sealevel changes, Sealevel drop, Sealevel rise, Second sealevel rise, Sedimentary geology, Setchell, Smaller foraminifers, Solution vugs, Stratigraphic, Subordinate components, Subunit, Tabular, Tabular acropora, Tahiti, Townsend, Upper interval, Verheij, Volcaniclastic, Volcaniclasts, Vugs.
- Teeft :
- Acropora, Adey, Agariciids, Algae, Algal, Assemblage, Baba, Bioclastic, Bioclastic packstone, Bioclasts, Blackwell publishing asia, Boykins, Bryozoan, Camoin, Carbonate, Coral, Coral clasts, Coral fragments, Coral framestone, Coralgal, Coralgal framestone, Coralline, Coralline algae, Deglacial, Deglaciation, Diagenetically, Echinoids, Encrusting, Encrusting agariciids, Encrusting foraminifers, Encrusting forms, Encrusting montipora, Foraminifer, Forereef, Forereef rhodoliths, Foslie, Fossil, Framestone, French polynesia, Geniculate, Geniculate coralline algae, Grainstone, Halimeda, Hermatypic corals, Hydrolithon, Hydrolithon onkodes, Insipidum, Iodp, Iodp expedition, Iryu, Keats, Larger foraminifers, Limestone, Lithophyllum, Lithophyllum insipidum adey, Lower interval, Matrix, Mbsf, Mesophyllum, Microbialite, Mollusk, Montaggioni, Montipora, Myriocarpum, Neogoniolithon, Nongeniculate, Nongeniculate coralline algae, Nongeniculate coralline algal assemblages, Oatstone, Ocean drilling program, Older pleistocene sequence, Onkodes, Packstone, Penultimate, Penultimate deglaciation, Pleistocene, Pleistocene sealevel history, Pneophyllum conicum, Pocillopora, Porites, Rhodolith, Rhodoliths, Robust, Ryukyu, Ryukyu group, Ryukyu islands, Sealevel, Sealevel changes, Sealevel drop, Sealevel rise, Second sealevel rise, Sedimentary geology, Setchell, Smaller foraminifers, Solution vugs, Stratigraphic, Subordinate components, Subunit, Tabular, Tabular acropora, Tahiti, Townsend, Upper interval, Verheij, Volcaniclastic, Volcaniclasts, Vugs.
Abstract
Material cored during the Integrated Ocean Drilling Program (IODP) Expedition 310 ‘Tahiti Sea Level’ revealed that the fossil reef systems around Tahiti are composed of two major stratigraphic sequences: (i) a last deglacial sequence; and (ii) an older Pleistocene sequence. The older Pleistocene carbonate sequence is composed of reef deposits associated with volcaniclastic sediments and was preserved in Hole 310‐M0005D drilled off Maraa. Within an approximately 70‐m‐thick older Pleistocene sequence (33.22–101.93 m below seafloor; 92.85–161.56 m below present sealevel) in this hole, 11 depositional units are defined by lithological changes, sedimentological features, and paleontological characteristics and are numbered sequentially from the top of the hole downward (Subunits P1–P11). Paleowater depths inferred from nongeniculate coralline algae, combined with those determined by using corals and larger foraminifers, suggest two major sealevel rises during the deposition of the older Pleistocene sequence. Of these, the second sealevel rise is associated with an intervening sealevel drop. It is likely that the second sealevel rise corresponds to that during Termination II (TII, the penultimate deglaciation, from Marine Isotope Stages 6 to 5e). Therefore, the intervening sealevel drop can be correlated with that known as the ‘sealevel reversal’ during TII. Because there are limited data on the Pleistocene reef systems in the tropical South Pacific Ocean, this study provides important information about Pleistocene sealevel history, the evolution of coral reef ecosystems, and the responses of coral reefs to Quaternary climate changes.
Url:
DOI: 10.1111/j.1440-1738.2010.00737.x
Affiliations:
- Allemagne, Australie, France, Japon
- Brême (Land), Nouvelle-Galles du Sud, Provence-Alpes-Côte d'Azur, Région de Tōhoku
- Aix‐en‐Provence, Brême, Sendai, Sydney
- Université de Sydney, Université du Tōhoku
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xml:lang="fr">Japon</country><wicri:regionArea>Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Aobayama, Sendai 980‐8578</wicri:regionArea><orgName type="university">Université du Tōhoku</orgName><placeName><settlement type="city">Sendai</settlement><region type="province">Région de Tōhoku</region></placeName></affiliation></author><author><name sortKey="Fujita, Kazuhiko" sort="Fujita, Kazuhiko" uniqKey="Fujita K" first="Kazuhiko" last="Fujita">Kazuhiko Fujita</name><affiliation wicri:level="1"><country xml:lang="fr">Japon</country><wicri:regionArea>Department of Physics and Earth Sciences, University of the Ryukyus, Okinawa 903‐0213</wicri:regionArea><wicri:noRegion>Okinawa 903‐0213</wicri:noRegion></affiliation></author><author><name sortKey="Camoin, Gilbert" sort="Camoin, Gilbert" uniqKey="Camoin G" first="Gilbert" last="Camoin">Gilbert Camoin</name><affiliation wicri:level="3"><country xml:lang="fr">France</country><wicri:regionArea>Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement, (CEREGE), UMR 6635 CNRS, Europôle Méditerranéen de l'Arbois, BP 80, F‐13545 Aix‐en‐Provence Cedex 4</wicri:regionArea><placeName><region type="region" nuts="2">Provence-Alpes-Côte d'Azur</region><settlement type="city">Aix‐en‐Provence</settlement></placeName></affiliation></author><author><name sortKey="Cabioch, Guy" sort="Cabioch, Guy" uniqKey="Cabioch G" first="Guy" last="Cabioch">Guy Cabioch</name><affiliation wicri:level="1"><country xml:lang="fr">France</country><wicri:regionArea>Institut de Recherche pour le Déloppement, Bondy Cedex</wicri:regionArea><wicri:noRegion>Bondy Cedex</wicri:noRegion><wicri:noRegion>Bondy Cedex</wicri:noRegion></affiliation></author><author><name sortKey="Matsuda, Hiroki" sort="Matsuda, Hiroki" uniqKey="Matsuda H" first="Hiroki" last="Matsuda">Hiroki Matsuda</name><affiliation wicri:level="1"><country xml:lang="fr">Japon</country><wicri:regionArea>Department of Earth Sciences, Graduate School of Technology and Science, Kumamoto University, Kurokami 2‐39‐1, Kumamoto 860‐8555</wicri:regionArea><wicri:noRegion>Kumamoto 860‐8555</wicri:noRegion></affiliation></author><author><name sortKey="Sato, Tokiyuki" sort="Sato, Tokiyuki" uniqKey="Sato T" first="Tokiyuki" last="Sato">Tokiyuki Sato</name><affiliation wicri:level="1"><country xml:lang="fr">Japon</country><wicri:regionArea>Institute of Applied Earth Sciences, Faculty of Engineering and Resource Science, Akita University, Teagata‐Gakuencho 1‐1</wicri:regionArea><wicri:noRegion>Teagata‐Gakuencho 1‐1</wicri:noRegion></affiliation></author><author><name sortKey="Sugihara, Kaoru" sort="Sugihara, Kaoru" uniqKey="Sugihara K" first="Kaoru" last="Sugihara">Kaoru Sugihara</name><affiliation wicri:level="1"><country xml:lang="fr">Japon</country><wicri:regionArea>Center for Global Environmental Research (CGER), National Institute for Environmental Studies (NIES), 16‐2 Onogawa, Tsukuba, Ibaraki 305‐8506</wicri:regionArea><wicri:noRegion>Ibaraki 305‐8506</wicri:noRegion></affiliation></author><author><name sortKey="Webster, Jody M" sort="Webster, Jody M" uniqKey="Webster J" first="Jody M." last="Webster">Jody M. Webster</name><affiliation wicri:level="4"><country xml:lang="fr">Australie</country><wicri:regionArea>School of Geosciences, The University of Sydney, Sydney, NSW, 2006</wicri:regionArea><orgName type="university">Université de Sydney</orgName><placeName><settlement type="city">Sydney</settlement><region type="état">Nouvelle-Galles du Sud</region></placeName></affiliation></author><author><name sortKey="Westphal, Hildegard" sort="Westphal, Hildegard" uniqKey="Westphal H" first="Hildegard" last="Westphal">Hildegard Westphal</name><affiliation wicri:level="3"><country xml:lang="fr">Allemagne</country><wicri:regionArea>MARUM, Center for Marine Environmental Sciences, Universität Bremen, Leobener Straße, 28359 Bremen</wicri:regionArea><placeName><region type="land" nuts="3">Brême (Land)</region><settlement type="city">Brême</settlement></placeName></affiliation></author></analytic><monogr></monogr><series><title level="j" type="main">Island Arc</title><title level="j" type="alt">ISLARC</title><idno type="ISSN">1038-4871</idno><idno type="eISSN">1440-1738</idno><imprint><biblScope unit="vol">19</biblScope><biblScope unit="issue">4</biblScope><biblScope unit="page" from="690">690</biblScope><biblScope unit="page" to="706">706</biblScope><biblScope unit="page-count">17</biblScope><publisher>Blackwell Publishing Asia</publisher><pubPlace>Melbourne, Australia</pubPlace><date type="published" when="2010-12">2010-12</date></imprint><idno type="ISSN">1038-4871</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">1038-4871</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Acropora</term><term>Adey</term><term>Agariciids</term><term>Algae</term><term>Algal</term><term>Assemblage</term><term>Baba</term><term>Bioclastic</term><term>Bioclastic packstone</term><term>Bioclasts</term><term>Blackwell publishing asia</term><term>Boykins</term><term>Bryozoan</term><term>Camoin</term><term>Carbonate</term><term>Coral</term><term>Coral clasts</term><term>Coral fragments</term><term>Coral framestone</term><term>Coralgal</term><term>Coralgal framestone</term><term>Coralline</term><term>Coralline algae</term><term>Deglacial</term><term>Deglaciation</term><term>Diagenetically</term><term>Echinoids</term><term>Encrusting</term><term>Encrusting agariciids</term><term>Encrusting foraminifers</term><term>Encrusting forms</term><term>Encrusting montipora</term><term>Foraminifer</term><term>Forereef</term><term>Forereef rhodoliths</term><term>Foslie</term><term>Fossil</term><term>Framestone</term><term>French polynesia</term><term>Geniculate</term><term>Geniculate coralline algae</term><term>Grainstone</term><term>Halimeda</term><term>Hermatypic corals</term><term>Hydrolithon</term><term>Hydrolithon onkodes</term><term>Insipidum</term><term>Iodp</term><term>Iodp expedition</term><term>Iryu</term><term>Keats</term><term>Larger foraminifers</term><term>Limestone</term><term>Lithophyllum</term><term>Lithophyllum insipidum adey</term><term>Lower interval</term><term>Matrix</term><term>Mbsf</term><term>Mesophyllum</term><term>Microbialite</term><term>Mollusk</term><term>Montaggioni</term><term>Montipora</term><term>Myriocarpum</term><term>Neogoniolithon</term><term>Nongeniculate</term><term>Nongeniculate coralline algae</term><term>Nongeniculate coralline algal assemblages</term><term>Oatstone</term><term>Ocean drilling program</term><term>Older pleistocene sequence</term><term>Onkodes</term><term>Packstone</term><term>Penultimate</term><term>Penultimate deglaciation</term><term>Pleistocene</term><term>Pleistocene sealevel history</term><term>Pneophyllum conicum</term><term>Pocillopora</term><term>Porites</term><term>Rhodolith</term><term>Rhodoliths</term><term>Robust</term><term>Ryukyu</term><term>Ryukyu group</term><term>Ryukyu islands</term><term>Sealevel</term><term>Sealevel changes</term><term>Sealevel drop</term><term>Sealevel rise</term><term>Second sealevel rise</term><term>Sedimentary geology</term><term>Setchell</term><term>Smaller foraminifers</term><term>Solution vugs</term><term>Stratigraphic</term><term>Subordinate components</term><term>Subunit</term><term>Tabular</term><term>Tabular acropora</term><term>Tahiti</term><term>Townsend</term><term>Upper interval</term><term>Verheij</term><term>Volcaniclastic</term><term>Volcaniclasts</term><term>Vugs</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Acropora</term><term>Adey</term><term>Agariciids</term><term>Algae</term><term>Algal</term><term>Assemblage</term><term>Baba</term><term>Bioclastic</term><term>Bioclastic packstone</term><term>Bioclasts</term><term>Blackwell publishing asia</term><term>Boykins</term><term>Bryozoan</term><term>Camoin</term><term>Carbonate</term><term>Coral</term><term>Coral clasts</term><term>Coral fragments</term><term>Coral framestone</term><term>Coralgal</term><term>Coralgal framestone</term><term>Coralline</term><term>Coralline algae</term><term>Deglacial</term><term>Deglaciation</term><term>Diagenetically</term><term>Echinoids</term><term>Encrusting</term><term>Encrusting agariciids</term><term>Encrusting foraminifers</term><term>Encrusting forms</term><term>Encrusting montipora</term><term>Foraminifer</term><term>Forereef</term><term>Forereef rhodoliths</term><term>Foslie</term><term>Fossil</term><term>Framestone</term><term>French polynesia</term><term>Geniculate</term><term>Geniculate coralline algae</term><term>Grainstone</term><term>Halimeda</term><term>Hermatypic corals</term><term>Hydrolithon</term><term>Hydrolithon onkodes</term><term>Insipidum</term><term>Iodp</term><term>Iodp expedition</term><term>Iryu</term><term>Keats</term><term>Larger foraminifers</term><term>Limestone</term><term>Lithophyllum</term><term>Lithophyllum insipidum adey</term><term>Lower interval</term><term>Matrix</term><term>Mbsf</term><term>Mesophyllum</term><term>Microbialite</term><term>Mollusk</term><term>Montaggioni</term><term>Montipora</term><term>Myriocarpum</term><term>Neogoniolithon</term><term>Nongeniculate</term><term>Nongeniculate coralline algae</term><term>Nongeniculate coralline algal assemblages</term><term>Oatstone</term><term>Ocean drilling program</term><term>Older pleistocene sequence</term><term>Onkodes</term><term>Packstone</term><term>Penultimate</term><term>Penultimate deglaciation</term><term>Pleistocene</term><term>Pleistocene sealevel history</term><term>Pneophyllum conicum</term><term>Pocillopora</term><term>Porites</term><term>Rhodolith</term><term>Rhodoliths</term><term>Robust</term><term>Ryukyu</term><term>Ryukyu group</term><term>Ryukyu islands</term><term>Sealevel</term><term>Sealevel changes</term><term>Sealevel drop</term><term>Sealevel rise</term><term>Second sealevel rise</term><term>Sedimentary geology</term><term>Setchell</term><term>Smaller foraminifers</term><term>Solution vugs</term><term>Stratigraphic</term><term>Subordinate components</term><term>Subunit</term><term>Tabular</term><term>Tabular acropora</term><term>Tahiti</term><term>Townsend</term><term>Upper interval</term><term>Verheij</term><term>Volcaniclastic</term><term>Volcaniclasts</term><term>Vugs</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Algue</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Material cored during the Integrated Ocean Drilling Program (IODP) Expedition 310 ‘Tahiti Sea Level’ revealed that the fossil reef systems around Tahiti are composed of two major stratigraphic sequences: (i) a last deglacial sequence; and (ii) an older Pleistocene sequence. The older Pleistocene carbonate sequence is composed of reef deposits associated with volcaniclastic sediments and was preserved in Hole 310‐M0005D drilled off Maraa. Within an approximately 70‐m‐thick older Pleistocene sequence (33.22–101.93 m below seafloor; 92.85–161.56 m below present sealevel) in this hole, 11 depositional units are defined by lithological changes, sedimentological features, and paleontological characteristics and are numbered sequentially from the top of the hole downward (Subunits P1–P11). Paleowater depths inferred from nongeniculate coralline algae, combined with those determined by using corals and larger foraminifers, suggest two major sealevel rises during the deposition of the older Pleistocene sequence. Of these, the second sealevel rise is associated with an intervening sealevel drop. It is likely that the second sealevel rise corresponds to that during Termination II (TII, the penultimate deglaciation, from Marine Isotope Stages 6 to 5e). Therefore, the intervening sealevel drop can be correlated with that known as the ‘sealevel reversal’ during TII. Because there are limited data on the Pleistocene reef systems in the tropical South Pacific Ocean, this study provides important information about Pleistocene sealevel history, the evolution of coral reef ecosystems, and the responses of coral reefs to Quaternary climate changes.</div></front></TEI><affiliations><list><country><li>Allemagne</li><li>Australie</li><li>France</li><li>Japon</li></country><region><li>Brême (Land)</li><li>Nouvelle-Galles du Sud</li><li>Provence-Alpes-Côte d'Azur</li><li>Région de Tōhoku</li></region><settlement><li>Aix‐en‐Provence</li><li>Brême</li><li>Sendai</li><li>Sydney</li></settlement><orgName><li>Université de Sydney</li><li>Université du Tōhoku</li></orgName></list><tree><country name="Japon"><noRegion><name sortKey="Iryu, Yasufumi" sort="Iryu, Yasufumi" uniqKey="Iryu Y" first="Yasufumi" last="Iryu">Yasufumi Iryu</name></noRegion><name sortKey="Fujita, Kazuhiko" sort="Fujita, Kazuhiko" uniqKey="Fujita K" first="Kazuhiko" last="Fujita">Kazuhiko Fujita</name><name sortKey="Matsuda, Hiroki" sort="Matsuda, Hiroki" uniqKey="Matsuda H" first="Hiroki" last="Matsuda">Hiroki Matsuda</name><name sortKey="Sato, Tokiyuki" sort="Sato, Tokiyuki" uniqKey="Sato T" first="Tokiyuki" last="Sato">Tokiyuki Sato</name><name sortKey="Sugihara, Kaoru" sort="Sugihara, Kaoru" uniqKey="Sugihara K" first="Kaoru" last="Sugihara">Kaoru Sugihara</name><name sortKey="Takahashi, Yasunari" sort="Takahashi, Yasunari" uniqKey="Takahashi Y" first="Yasunari" last="Takahashi">Yasunari Takahashi</name></country><country name="France"><region name="Provence-Alpes-Côte d'Azur"><name sortKey="Camoin, Gilbert" sort="Camoin, Gilbert" uniqKey="Camoin G" first="Gilbert" last="Camoin">Gilbert Camoin</name></region><name sortKey="Cabioch, Guy" sort="Cabioch, Guy" uniqKey="Cabioch G" first="Guy" last="Cabioch">Guy Cabioch</name></country><country name="Australie"><region name="Nouvelle-Galles du Sud"><name sortKey="Webster, Jody M" sort="Webster, Jody M" uniqKey="Webster J" first="Jody M." last="Webster">Jody M. Webster</name></region></country><country name="Allemagne"><region name="Brême (Land)"><name sortKey="Westphal, Hildegard" sort="Westphal, Hildegard" uniqKey="Westphal H" first="Hildegard" last="Westphal">Hildegard Westphal</name></region></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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|texte= Sealevel history recorded in the Pleistocene carbonate sequence in IODP Hole 310‐M0005D, off Tahiti
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