Kano, Akihiro et al. (2007): 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

Leg/Site/Hole:
IODP 307
IODP 307 U1316
IODP 307 U1317
IODP 307 U1318
Identifier:
2007-128475
georefid

10.1130/G23917A.1
doi

Creator:
Kano, Akihiro
Hiroshima University, Higashi-Hiroshima, Japan
author

Ferdelman, Timothy G.
Max-Planck-Institute for Marine Microbiology, Federal Republic of Germany
author

Williams, Trevor
Lamont-Doherty Earth Observatory, United States
author

Henriet, Jean-Pierre
Universiteit Gent, Belgium
author

Ishikawa, Tsuyoshi
Japan Agency for Marine-Earth Science and Technology, Japan
author

Kawagoe, Noriko
University of Tsukuba, Japan
author

Takashima, Chiduru
University of Massachusetts, United States
author

Kakizaki, Yoshihiro
Chengdu University of Technology, China
author

Abe, Kohei
author

Sakai, Saburo
author

Browning, Emily L.
author

Li Xianghui
author

Andres, M. S.
author

Bjerager, M.
author

Cragg, B. A.
author

de Mol, B.
author

Dorschel, B.
author

Foubert, A.
author

Frank, T. D.
author

Fuwa, Y.
author

Gaillot, P.
author

Gharib, J. J.
author

Gregg, J. M.
author

Huvenne, V. A. I.
author

Leonide, P.
author

Mangelsdorf, K.
author

Monteys, X.
author

Novosel, I.
author

O'Donnell, R.
author

Rueggeberg, A.
author

Samarkin, V.
author

Sasaki, K.
author

Spivack, A. J.
author

Tanaka, A.
author

Titschack, J.
author

van Rooij, D.
author

Wheeler, A.
author

Identification:
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
2007
Geology (Boulder)
Geological Society of America (GSA), Boulder, CO, United States
35
11
1051-1054
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 Sea-bight, southwest of Ireland, is on Miocene siliciclastics and consists entirely of sediments bearing well-preserved cold-water coral Lophelia pertusa. The (super 87) Sr/ (super 86) Sr 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.
English
Serial
Coverage:Geographic coordinates:
North:51.2600
West:-11.4400East: -11.3300
South:51.2300

Stratigraphy; alkaline earth metals; Anthozoa; Atlantic Ocean; Cenozoic; Challenger Mound; chemostratigraphy; Cnidaria; Coelenterata; cores; cycles; deep-water environment; Expedition 307; glacial environment; glaciomarine environment; growth rates; Integrated Ocean Drilling Program; interglacial environment; Invertebrata; IODP Site 1316; IODP Site 1317; IODP Site 1318; isotope ratios; isotopes; Lophelia pertusa; marine environment; marine sediments; metals; Miocene; mounds; Neogene; North Atlantic; Northeast Atlantic; paleo-oceanography; paleoecology; Pleistocene; Pliocene; Porcupine Basin; Quaternary; reef builders; sediments; Sr-87/Sr-86; stable isotopes; strontium; Tertiary;

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