Thomas, Alexander L. et al. (2012): Assessing subsidence rates and paleo water-depths for Tahiti reefs using U-Th chronology of altered corals

Leg/Site/Hole:
IODP 310
IODP 310 M0005
Identifier:
2012-045491
georefid

10.1016/j.margeo.2011.12.006
doi

Creator:
Thomas, Alexander L.
Oxford University, Department of Earth Sciences, Oxford, United Kingdom
author

Fujita, Kazuhiko
University of the Ryukyus, Japan
author

Iryu, Yasufumi
Tohoku University, Japan
author

Bard, Edouard
Aix-Marseille Unmiversite, France
author

Cabioch, Guy
Institut de Recherche pour le Developpement, New Caledonia
author

Camoin, Gilbert
University of Arizona, United States
author

Cole, Julia E.
University of Bremen, Germany
author

Deschamps, Pierre
Kumamoto University, Japan
author

Durand, Nicolas
Shizuoka University, Japan
author

Hamelin, Bruno
University of South Florida, United States
author

Heindel, Katrin
Japan Agency for Marine-Earth Science and Technology, Japan
author

Henderson, Gideon M.
Akita University, Japan
author

Mason, Andew J.
Fukuoka University, Japan
author

Matsuda, Hiroki
University of Edinburgh, United Kingdom
author

Menabreaz, Lucie
James Cook University of North Queensland, Australia
author

Omori, Akitoshi
author

Quinn, Terry
author

Sakai, Saburo
author

Sato, Tokiyuki
author

Sugihara, Kaoru
author

Takahashi, Yasunari
author

Thouveny, Nicolas
author

Tudhope, Alexander W.
author

Webster, Jody
author

Westphal, Hildegard
author

Yokoyama, Yusuke
author

Identification:
Assessing subsidence rates and paleo water-depths for Tahiti reefs using U-Th chronology of altered corals
2012
Marine Geology
Elsevier, Amsterdam, Netherlands
295-298
86-94
We present uranium-thorium chronology for a 102m core through a Pleistocene reef at Tahiti (French Polynesia) sampled during IODP Expedition 310 "Tahiti Sea Level". We employ total and partial dissolution procedures on the older coral samples to investigate the diagenetic overprint of the uranium-thorium system. Although alteration of the U-Th system cannot be robustly corrected, diagenetic trends in the U-Th data, combined with sea level and subsidence constraints for the growth of the corals enables the age of critical samples to be constrained to marine isotope stage 9. We use the ages of the corals, together with delta (super 18) O based sea-level histories, to provide maximum constraints on possible paleo water-depths. These depth constraints are then compared to independent depth estimates based on algal and foraminiferal assemblages, microbioerosion patterns, and sedimentary facies, confirming the accuracy of these paleo water-depth estimates. We also use the fact that corals could not have grown above sea level to place a maximum constraint on the subsidence rate of Tahiti to be 0.39mka (super -1) , with the most likely rate being close to the existing minimum estimate of 0.25mka (super -1) . Abstract Copyright (2012) Elsevier, B.V.
English
Serial
Coverage:Geographic coordinates:
North:-17.4600
West:-149.3300East: -149.3300
South:-17.4600

Quaternary geology; Geochronology; absolute age; carbonate rocks; Cenozoic; cores; dates; East Pacific; Expedition 310; French Polynesia; Integrated Ocean Drilling Program; IODP Site M0005; Oceania; Pacific Ocean; paleobathymetry; Pleistocene; Polynesia; Quaternary; rates; reconstruction; reefs; sedimentary rocks; Society Islands; South Pacific; Southeast Pacific; subsidence; Tahiti; Tahiti Sea Level Expedition; Th/U;

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