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Late Miocene wood recovered in Bengal–Nicobar submarine fan sediments by IODP Expedition 362

Late Miocene wood recovered in Bengal–Nicobar submarine fan sediments by IODP Expedition 362
Late Miocene wood recovered in Bengal–Nicobar submarine fan sediments by IODP Expedition 362
Drilling and coring during IODP Expedition 362 in the eastern Indian Ocean encountered probably the largest wood fragment ever recovered in scientific ocean drilling. The wood is Late Miocene in age and buried beneath ∼800 m of siliciclastic mud and sand of the Bengal–Nicobar Fan. The wood is well preserved. Possible origins include the hinterland to the north, with sediment transported as part of the submarine fan sedimentary processes, or the Sunda subduction zone to the east, potentially as a megathrust tsunami deposit.
1816-3459
49-52
Mcneill, Lisa
1fe6a1e0-ca1a-4b6f-8469-309d0f9de0cf
Dugan, Brandon
45d5f697-b2a6-4a88-a24f-1b29b1f4703d
Petronotis, Katerina
96f3f5f9-3f70-4f16-a116-c64232cadc91
Milliken, Kitty
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Francis, Jane
7acba304-8a5d-405c-bedf-a45624b50bd4
Mcneill, Lisa
1fe6a1e0-ca1a-4b6f-8469-309d0f9de0cf
Dugan, Brandon
45d5f697-b2a6-4a88-a24f-1b29b1f4703d
Petronotis, Katerina
96f3f5f9-3f70-4f16-a116-c64232cadc91
Milliken, Kitty
5a9e464f-1044-4e30-b687-576e22debf2c
Francis, Jane
7acba304-8a5d-405c-bedf-a45624b50bd4

Mcneill, Lisa, Dugan, Brandon, Petronotis, Katerina, Milliken, Kitty and Francis, Jane (2020) Late Miocene wood recovered in Bengal–Nicobar submarine fan sediments by IODP Expedition 362. Scientific Drilling, 27, 49-52. (doi:10.5194/sd-27-49-2020).

Record type: Article

Abstract

Drilling and coring during IODP Expedition 362 in the eastern Indian Ocean encountered probably the largest wood fragment ever recovered in scientific ocean drilling. The wood is Late Miocene in age and buried beneath ∼800 m of siliciclastic mud and sand of the Bengal–Nicobar Fan. The wood is well preserved. Possible origins include the hinterland to the north, with sediment transported as part of the submarine fan sedimentary processes, or the Sunda subduction zone to the east, potentially as a megathrust tsunami deposit.

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Accepted/In Press date: 20 January 2020
Published date: 27 May 2020
Additional Information: Funding Information: Financial support. This research has been supported by the Natural Environment Research Council (support to Lisa McNeill, grant no. NE/P01297/1), the U.S. Science Support Program (a Post Expedition Activity award to Brandon Dugan), and by the IODP JRSO (support to Katerina Petronotis, NSF grant no. OCE-1326927). Publisher Copyright: © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.

Identifiers

Local EPrints ID: 444439
URI: http://eprints.soton.ac.uk/id/eprint/444439
ISSN: 1816-3459
PURE UUID: 49758ad1-49de-42d4-b70b-78d1a2b5ce86
ORCID for Lisa Mcneill: ORCID iD orcid.org/0000-0002-8689-5882

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Date deposited: 19 Oct 2020 16:33
Last modified: 17 Mar 2024 02:52

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Contributors

Author: Lisa Mcneill ORCID iD
Author: Brandon Dugan
Author: Katerina Petronotis
Author: Kitty Milliken
Author: Jane Francis

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