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Synthesis: stratigraphy and age control for IODP Sites U1394, U1395, and U1396 offshore Montserrat in the Lesser Antilles

Synthesis: stratigraphy and age control for IODP Sites U1394, U1395, and U1396 offshore Montserrat in the Lesser Antilles
Synthesis: stratigraphy and age control for IODP Sites U1394, U1395, and U1396 offshore Montserrat in the Lesser Antilles
This data report focuses on Holes U1394B, U1395B, and U1396C located offshore Montserrat. These holes were drilled during Integrated Ocean Drilling Program Expedition 340 and contain deposits associated with the growth and decay of the volcanic island of Montserrat. Hole U1394B dates to ~353 ka and is composed of 17 bioclastic turbidites, 24 mixed turbidites, 55 volcaniclastic turbidites, and 32 tephra fall layers within a background stratigraphy of hemipelagic marine mud. Hole U1395B dates to older than 1 Ma and contains 18 bioclastic turbidites, 27 mixed turbidites, 43 volcaniclastic turbidites, and 52 tephra fall layers. The uppermost 7 m of Hole U1396C covers ~1 My of stratigraphy and contains 1 bioclastic turbidite, 1 mixed turbidite, 9 volcaniclastic turbidites, and 13 tephra fall layers. Tephra fall and some volcaniclastic deposits are associated with episodes of island building, whereas bioclastic turbidites, mixed turbidites, and some volcaniclastic turbidites are associated with large landslide events from Montserrat.
1-19
Coussens, M.F.
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Wall-Palmer, D.
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Talling, P.J.
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Watt, S.F.L
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Hatter, S.J.
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Cassidy, M.
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Clare, M.
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Jutzeler, M.
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Hatfield, R.
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McCanta, M.
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Kataoka, K.S.
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Endo, D.
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Palmer, M.R.
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Stinton, A.
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Fujinawa, A.
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Boudon, G.
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Le Friant, A.
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Ishizuka, O.
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Gernon, T.
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Adachi, T.
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Aljahdali, M.
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Breitkreuz, C.
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Frass, A.J.
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Hornbach, M.J.
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Lebas, E.
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Lafuerza, S.
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Maeno, F.
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Manga, M.
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Martinez-Colon, M.
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McManus, J.
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Morgan, S.
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Saito, T.
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Slagle, A.
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Subramanyam, K.S.V.
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Tamura, Y.
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Trofimovs, J.
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Villemant, B.
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Wang, F.
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Coussens, M.F.
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Wall-Palmer, D.
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Watt, S.F.L
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Hatter, S.J.
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Cassidy, M.
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Clare, M.
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Jutzeler, M.
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Hatfield, R.
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McCanta, M.
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Kataoka, K.S.
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Endo, D.
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Palmer, M.R.
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Fujinawa, A.
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Boudon, G.
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Le Friant, A.
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Ishizuka, O.
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Gernon, T.
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Adachi, T.
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Aljahdali, M.
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Breitkreuz, C.
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Frass, A.J.
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Hornbach, M.J.
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Lebas, E.
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Lafuerza, S.
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Maeno, F.
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Manga, M.
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Martinez-Colon, M.
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McManus, J.
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Morgan, S.
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Saito, T.
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Slagle, A.
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Subramanyam, K.S.V.
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Tamura, Y.
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Trofimovs, J.
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Villemant, B.
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Wang, F.
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Coussens, M.F., Wall-Palmer, D., Talling, P.J., Watt, S.F.L, Hatter, S.J., Cassidy, M., Clare, M., Jutzeler, M., Hatfield, R., McCanta, M., Kataoka, K.S., Endo, D., Palmer, M.R., Stinton, A., Fujinawa, A., Boudon, G., Le Friant, A., Ishizuka, O., Gernon, T., Adachi, T., Aljahdali, M., Breitkreuz, C., Frass, A.J., Hornbach, M.J., Lebas, E., Lafuerza, S., Maeno, F., Manga, M., Martinez-Colon, M., McManus, J., Morgan, S., Saito, T., Slagle, A., Subramanyam, K.S.V., Tamura, Y., Trofimovs, J., Villemant, B. and Wang, F. (2016) Synthesis: stratigraphy and age control for IODP Sites U1394, U1395, and U1396 offshore Montserrat in the Lesser Antilles. Proceedings of the Integrated Ocean Drilling Program, 340, 1-19. (doi:10.2204/iodp.proc.340.204.2016).

Record type: Article

Abstract

This data report focuses on Holes U1394B, U1395B, and U1396C located offshore Montserrat. These holes were drilled during Integrated Ocean Drilling Program Expedition 340 and contain deposits associated with the growth and decay of the volcanic island of Montserrat. Hole U1394B dates to ~353 ka and is composed of 17 bioclastic turbidites, 24 mixed turbidites, 55 volcaniclastic turbidites, and 32 tephra fall layers within a background stratigraphy of hemipelagic marine mud. Hole U1395B dates to older than 1 Ma and contains 18 bioclastic turbidites, 27 mixed turbidites, 43 volcaniclastic turbidites, and 52 tephra fall layers. The uppermost 7 m of Hole U1396C covers ~1 My of stratigraphy and contains 1 bioclastic turbidite, 1 mixed turbidite, 9 volcaniclastic turbidites, and 13 tephra fall layers. Tephra fall and some volcaniclastic deposits are associated with episodes of island building, whereas bioclastic turbidites, mixed turbidites, and some volcaniclastic turbidites are associated with large landslide events from Montserrat.

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More information

Accepted/In Press date: 29 September 2015
Published date: 8 January 2016
Organisations: Geology & Geophysics, Geochemistry, Marine Geoscience

Identifiers

Local EPrints ID: 387356
URI: http://eprints.soton.ac.uk/id/eprint/387356
PURE UUID: 97019bf8-5bc9-4110-ac22-35aa7263d95c
ORCID for S.J. Hatter: ORCID iD orcid.org/0000-0003-0760-5275
ORCID for T. Gernon: ORCID iD orcid.org/0000-0002-7717-2092

Catalogue record

Date deposited: 12 Feb 2016 15:09
Last modified: 15 Mar 2024 03:36

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Contributors

Author: M.F. Coussens
Author: D. Wall-Palmer
Author: P.J. Talling
Author: S.F.L Watt
Author: S.J. Hatter ORCID iD
Author: M. Cassidy
Author: M. Clare
Author: M. Jutzeler
Author: R. Hatfield
Author: M. McCanta
Author: K.S. Kataoka
Author: D. Endo
Author: M.R. Palmer
Author: A. Stinton
Author: A. Fujinawa
Author: G. Boudon
Author: A. Le Friant
Author: O. Ishizuka
Author: T. Gernon ORCID iD
Author: T. Adachi
Author: M. Aljahdali
Author: C. Breitkreuz
Author: A.J. Frass
Author: M.J. Hornbach
Author: E. Lebas
Author: S. Lafuerza
Author: F. Maeno
Author: M. Manga
Author: M. Martinez-Colon
Author: J. McManus
Author: S. Morgan
Author: T. Saito
Author: A. Slagle
Author: K.S.V. Subramanyam
Author: Y. Tamura
Author: J. Trofimovs
Author: B. Villemant
Author: F. Wang

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