Trace element variations in fossil corals from Tahiti collected by IODP Expedition 310: Reconstruction of marine environments during the last deglaciation (15 to 9 ka)

Mayuri Takeuchi, Yusuke Yokoyama, Mariko Harada, Atsushi Suzuki, Hodaka Kawahata, Hiroyuki Matsuzaki, Yasufumi Iryu

Research output: Contribution to journalArticle

12 Citations (Scopus)

Abstract

Climate responses and changes in marine environments during the last deglaciation have been controversial and few paleoceanographic data are available from the tropical South Pacific, though this region is crucial in the investigations of ocean-atmosphere interactions. Integrated Ocean Drilling Program Expedition 310 was conducted to establish the time course of the postglacial sea-level rise at Tahiti in the South Pacific. A principal objective of this expedition was to examine the variation of marine environments during the last deglaciation. As fossil Porites coral is ideal for assessing past marine environments, we selected only Porites specimens from the many coral specimens retrieved, examined them by XRD, and dated them by the 14C method. In all, we obtained 17 pristine Porites specimens composed of only aragonite with ages from 15 to 9 ka. Then, we measured Mg/Ca, Ba/Ca, and U/Ca ratios and Cd contents as proxies for upwelling and sea surface temperature. Higher Ba/Ca ratios and Cd content together with lower reconstructed SSTs using U/Ca ratios in the coral specimens between 12.6 and 9.8 cal ka compared to around 15 cal ka suggest that upwelling and/or entrainment of subsurface water into mixed layer was enhanced around Tahiti during this period. This finding is consistent with previous reports and supports the idea that the South Pacific was characterized by La Niña-like conditions at least from 12.6 to 9.8 cal ka.

Original languageEnglish
Pages (from-to)303-306
Number of pages4
JournalMarine Geology
Volume271
Issue number3-4
DOIs
Publication statusPublished - Jun 15 2010
Externally publishedYes

Fingerprint

last deglaciation
Calcium Carbonate
Sea level
Trace Elements
marine environment
coral
Drilling
trace element
fossil
Water
upwelling
sea surface temperature
aragonite
Ocean Drilling Program
Postglacial
entrainment
Temperature
mixed layer
X-ray diffraction
atmosphere

Keywords

  • deglaciation
  • fossil coral
  • IODP
  • Tahiti
  • upwelling

ASJC Scopus subject areas

  • Oceanography
  • Geochemistry and Petrology
  • Geology

Cite this

Trace element variations in fossil corals from Tahiti collected by IODP Expedition 310 : Reconstruction of marine environments during the last deglaciation (15 to 9 ka). / Takeuchi, Mayuri; Yokoyama, Yusuke; Harada, Mariko; Suzuki, Atsushi; Kawahata, Hodaka; Matsuzaki, Hiroyuki; Iryu, Yasufumi.

In: Marine Geology, Vol. 271, No. 3-4, 15.06.2010, p. 303-306.

Research output: Contribution to journalArticle

Takeuchi, Mayuri ; Yokoyama, Yusuke ; Harada, Mariko ; Suzuki, Atsushi ; Kawahata, Hodaka ; Matsuzaki, Hiroyuki ; Iryu, Yasufumi. / Trace element variations in fossil corals from Tahiti collected by IODP Expedition 310 : Reconstruction of marine environments during the last deglaciation (15 to 9 ka). In: Marine Geology. 2010 ; Vol. 271, No. 3-4. pp. 303-306.
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