Carbonate deposits on submerged seamounts in the northwestern Pacific Ocean

Hideko Takayanagi, Yasufumi Iryu, Tsutomu Yamada, Motoyoshi Oda, Kazuyuki Yamamoto, Tokiyuki Sato, Shun Chiyonobu, Akira Nishimura, Tsutomu Nakazawa, Satoshi Shiokawa

Research output: Contribution to journalArticlepeer-review

12 Citations (Scopus)

Abstract

The lithology of shallow-water carbonates collected from 19 sites on 16 seamounts in six areas of the northwestern Pacific Ocean using the Deep-sea Boring Machine System are described. The areas include the Amami Plateau, Daito Ridge, Oki-Daito Ridge, Urdaneta Plateau, Kyushu-Palau Ridge and Ogasawara Plateau. Chronological constraint is provided by calcareous nannofossil biostratigraphy, planktonic foraminiferal biostratigraphy, larger foraminiferal biostratigraphy and strontium (Sr) isotope stratigraphy. Large amounts of shallow-water carbonates accumulated on the seamounts during the Oligocene, a relatively cool period, whereas limited carbonate deposits formed during the Early Miocene, a relatively warm period. This might indicate that deposition of shallow-water carbonates on seamounts in the northwestern Pacific Ocean was not necessarily controlled by climatic conditions, but was related to volcanism and tectonics that served as foundations for reef/carbonate-platform formation. Remarkable differences in biotic composition exist between Cretaceous and Cenozoic shallow-water carbonates. Late Cretaceous shallow-water carbonates are distinguished by the occurrence of rudists, solenoporacean algae and microencrusters. Middle Eocene to Early Oligocene shallow-water carbonates are dominated by Halimeda or nummulitid and discocyclinid larger foraminifers. Scleractinian corals became common from the Oligocene onward. Nongeniculate coralline algae and larger foraminifers were common to abundant throughout the Eocene to the Pleistocene. The replacement of major carbonate producers in the shallow-water carbonate factory during post-Cretaceous time is in accordance with previous studies and is considered to reflect a shift in seawater chemistry.

Original languageEnglish
Pages (from-to)394-419
Number of pages26
JournalIsland Arc
Volume16
Issue number3
DOIs
Publication statusPublished - 2007 Sep

Keywords

  • Cenozoic
  • Late Cretaceous
  • Limestone
  • North western Pacific Ocean
  • Seamount
  • Shallow-water carbonate

ASJC Scopus subject areas

  • Geology

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