Data report; Bioerosion in the reef framework, IODP Expedition 310 off Tahiti (Tiarei, Maraa, and Faaa sites)

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doi: 10.2204/iodp.proc.310.201.2009
Author(s): Heindel, Katrin; Westphal, Hildegard; Wisshak, Max
Integrated Ocean Drilling Program, Expedition 310 Scientists
Author Affiliation(s): Primary:
University of Bremen, MARUM-Center for Marine Environmental Sciences, Bremen, Federal Republic of Germany
Other:
Tohoku University, Japan
British Geological Survey, United Kingdom
Université de Montpellier II, France
Institut de Recherche pourl le Développement, France
Scripps Institution of Oceanography, United States
Woods Hole Oceanographic Institution, United States
University of Arizona, United States
Lamont-Doherty Earth Observatory, United States
University of Bremen, Federal Republic of Germany
University of Ryukyus, Japan
Open University, United Kingdom
University of Southern California, United States
Japan Agency for Marine-Earth Science, Japan
Kumamoto University, Japan
University of South Florida, United States
Fukuoka University, Japan
University of Oxford, United Kingdom
Swiss Federal Institute of Technology, Switzerland
Vrije Universiteit Amsterdam, Netherlands
James Cook University of North Queensland, Australia
Kangwon National University, South Korea
University of Tokyo, Japan
Erlangen University, Federal Republic of Germany
Volume Title: Proceedings of the Integrated Ocean Drilling Program; Tahiti sea level; Expedition 310 of the mission-specific drilling platform from and to Papeete, Tahiti, French Polynesia, Sites M0005-M0026, 6 October-16 November 2005
Volume Author(s): Camoin, Gilbert F.; Iryu, Yasufumi; McInroy, David; Asami, Ryuji; Braaksma, Hendrik; Cabioch, Guy; Castillo, Paterno; Cohen, Anne L.; Cole, Julia E.; Deschamps, Pierre; Fairbanks, Richard G.; Felis, Thomas; Fujita, Kazuhiko; Hathorne, E. C.; Lund, Steve P.; Machiyama, Hideaki; Matsuda, Hiroki; Quinn, Terrence M.; Sugihara, Kaoru; Thomas, Alexander; Vasconcelos, Crisogono de Olivera; Verwer, Klaas; Webster, Jody M.; Westphal, Hildegard; Woo, Kyung Sik; Yamada, Tsutomu; Yokoyama, Yusuke
Source: Proceedings of the Integrated Ocean Drilling Program; Tahiti sea level; Expedition 310 of the mission-specific drilling platform from and to Papeete, Tahiti, French Polynesia, Sites M0005-M0026, 6 October-16 November 2005, Gilbert F. Camoin, Yasufumi Iryu, David McInroy, Ryuji Asami, Hendrik Braaksma, Guy Cabioch, Paterno Castillo, Anne L. Cohen, Julia E. Cole, Pierre Deschamps, Richard G. Fairbanks, Thomas Felis, Kazuhiko Fujita, E. C. Hathorne, Steve P. Lund, Hideaki Machiyama, Hiroki Matsuda, Terrence M. Quinn, Kaoru Sugihara, Alexander Thomas, Crisogono de Olivera Vasconcelos, Klaas Verwer, Jody M. Webster, Hildegard Westphal, Kyung Sik Woo, Tsutomu Yamada and Yusuke Yokoyama; Integrated Ocean Drilling Program, Expedition 310 Scientists. Proceedings of the Integrated Ocean Drilling Program, Vol.310. Publisher: IODP Management International, Washington, DC, United States. ISSN: 1930-1014
Note: In English. 25 refs.; illus., incl. sect., 5 tables, sketch map
Summary: The coral reef framework off Tahiti was drilled during Integrated Ocean Drilling Program (IODP) Expedition 310 in order to study environmental change (including sea level rise) following the Last Glacial Maximum (LGM). Cores from sites located in the three drilling areas (Tiarei to the north, Faaa to the west, and Maraa to the southwest of the island of Tahiti) were studied in order to characterize the microbioerosion patterns in the post-LGM deglacial reef framework. A total of 19 samples were examined for information on environmental conditions directly after the demise of the shallow-water corals and during subsequent encrustation by coralline algae and microbialites. Microbioerosion patterns imply that conditions during reef growth were deeper euphotic to dysphotic. The reasons for the largely absent shallow euphotic indications lay in the proposed rapid sea level rise leaving a drowned reef in a "cryptophotic" position of most samples, in enhanced turbidity condensing the photic zonation, or in a combination of these factors. The sea level rise scenario combined with increased nutrient levels are considered the primary factors because entirely cryptophotic conditions of the sediment cores are less probable.
Year of Publication: 2009
Research Program: IODP Integrated Ocean Drilling Program
Key Words: 06 Petrology, Sedimentary; Algae; Bioerosion; Biogenic processes; Biogenic structures; Boreholes; Carbonate rocks; Chlorophyta; Cores; Cyanobacteria; Deglaciation; East Pacific; Endolithic taxa; Erosion; Expedition 310; French Polynesia; Fungi; Ichnofossils; Integrated Ocean Drilling Program; Lebensspuren; Microfossils; Microstructure; Oceania; Pacific Ocean; Paleoenvironment; Plantae; Polynesia; Reefs; SEM data; Sea-level changes; Sedimentary rocks; Sedimentary structures; Society Islands; South Pacific; Southeast Pacific; Tahiti; Tahiti Sea Level Expedition
Coordinates: S180000 S170000 W1490000 W1500000
Record ID: 2009022890
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