Age constraints on the origin and growth history of a deep-water coral mound in the northeast Atlantic drilled during Integrated Ocean Drilling Program Expedition 307

Akihiro Kano, Timothy G. Ferdelman, Trevor Williams, Jean Pierre Henriet, Tsuyoshi Ishikawa, Noriko Kawagoe, Chiduru Takashima, Yoshihiro Kakizaki, Kohei Abe, Saburo Sakai, Emily L. Browing, Xianghui Li, M. S. Andres, M. Bjerager, B. A. Cragg, B. De Mol, B. Dorschel, A. Foubert, T. D. Frank, Y. FuwaP. Gaillot, J. J. Gharib, J. M. Gregg, V. A.I. Huvenne, P. Léonide, K. Mangelsdorf, X. Monteys, I. Novosel, R. O'Donnell, A. Rüggeberg, V. Samarkin, K. Sasaki, A. J. Spivack, A. Tanaka, J. Titschack, D. van Rooij, A. Wheeler

研究成果: Contribution to journalArticle査読

97 被引用数 (Scopus)

抄録

Sr isotope stratigraphy provides a new age model for the first complete section drilled through a deep-water coral mound. The 155-m-long section from Challenger Mound in the Porcupine Seabight, southwest of Ireland, is on Miocene siliciclastics and consists entirely of sediments bearing well-preserved cold-water coral Lophefia pertusa. The 87Sr/86Sr values of 28 coral specimens from the mound show an upward-increasing trend, correspond to ages from 2.6 to 0.5 Ma, and identify a significant hiatus from ca. 1.7 to 1.0 Ma at 23.6 m below seafloor. The age of the basal mound sediments coincides with the intensification of Northern Hemisphere glaciations that set up the modern stratification of the northeast Atlantic and enabled coral growth. Mound growth persisted throughout glacial-interglacial fluctuations, reached a maximum rate (24 cm/k.y.) ca. 2.0 Ma, and ceased at 1.7 Ma. Unlike other buried mounds in Porcupine Seabight, Challenger Mound was only partly covered during its growth interruption, and growth restarted ca. 1.0 Ma.

本文言語英語
ページ(範囲)1051-1054
ページ数4
ジャーナルGeology
35
11
DOI
出版ステータス出版済み - 11 2007

All Science Journal Classification (ASJC) codes

  • 地質学

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