Diatom biostratigraphy, Argon ages and chronology of ODP Hole 183-1138A

A thick Neogene section was recovered in the upper ~300 m of Ocean Drilling Program Hole 1138A, drilled on the Central Kerguelen Plateau in the Indian sector of the Southern Ocean. Sediment lithologies consist primarily of mixed carbonate and biosiliceous clays and oozes, with several thin (1-3 cm)...

Full description

Bibliographic Details
Main Authors: Bohaty, Steven M, Wise, Sherwood W, Duncan, Robert A, Moore, Leah, Wallace, Paul J
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.785348
https://doi.org/10.1594/PANGAEA.785348
_version_ 1821535785948545024
author Bohaty, Steven M
Wise, Sherwood W
Duncan, Robert A
Moore, Leah
Wallace, Paul J
author_facet Bohaty, Steven M
Wise, Sherwood W
Duncan, Robert A
Moore, Leah
Wallace, Paul J
author_sort Bohaty, Steven M
collection PANGAEA - Data Publisher for Earth & Environmental Science
description A thick Neogene section was recovered in the upper ~300 m of Ocean Drilling Program Hole 1138A, drilled on the Central Kerguelen Plateau in the Indian sector of the Southern Ocean. Sediment lithologies consist primarily of mixed carbonate and biosiliceous clays and oozes, with several thin (1-3 cm) tephra horizons. The tephras are glass rich, well sorted, and dominantly trachytic to rhyolitic in composition. Volcaniclastic material in these horizons is interpreted to have originated from Heard Island, 180 km northwest of Site 1138, and was likely emplaced through both primary ash fall and turbiditic, submarine flows. A Neogene age-depth model for Hole 1138A is constructed primarily from 36 diatom biostratigraphic datums. Nannofossil and planktonic foraminifer biostratigraphy provides supporting age information. Additionally, four high-precision 40Ar-39Ar ages are derived from ash and tephra horizons, and these radiometric ages are in close agreement with the biostratigraphic ages. The integrated age-depth model reveals a reasonably complete lower Miocene to upper Pleistocene section in Hole 1138A, with the exception of a ~1-m.y. hiatus at the Miocene/Pliocene boundary. Another possible hiatus is also identified at the Oligocene/Miocene boundary. High Neogene sedimentation rates and the presence of both calcareous and siliceous microfossils, combined with datable tephra horizons, establish Site 1138 as a suitable target for future drilling legs with paleoceanographic objectives. This report also proposes two new diatom species, Fragilariopsis heardensis and Azpeitia harwoodii, from Pliocene strata of Hole 1138A.
format Other/Unknown Material
genre Heard Island
Southern Ocean
genre_facet Heard Island
Southern Ocean
geographic Southern Ocean
Kerguelen
Heard Island
Indian
geographic_facet Southern Ocean
Kerguelen
Heard Island
Indian
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.785348
institution Open Polar
language English
long_lat ENVELOPE(75.974880,75.974880,-53.551750,-53.551750)
op_collection_id ftpangaea
op_coverage LATITUDE: -53.551750 * LONGITUDE: 75.974880 * DATE/TIME START: 1999-01-07T23:30:00 * DATE/TIME END: 1999-01-31T06:15:00
op_doi https://doi.org/10.1594/PANGAEA.78534810.2973/odp.proc.sr.183.016.2003
op_relation https://doi.pangaea.de/10.1594/PANGAEA.785348
https://doi.org/10.1594/PANGAEA.785348
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_source Supplement to: Bohaty, Steven M; Wise, Sherwood W; Duncan, Robert A; Moore, Leah; Wallace, Paul J (2003): Neogene diatom biostratigraphy, tephra stratigraphy, and chronology of ODP Hole 1138A, Kerguelen Plateau. In: Frey, FA; Coffin, MF; Wallace, PJ; Quilty, PG (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 183, 1-53, https://doi.org/10.2973/odp.proc.sr.183.016.2003
publishDate 2003
publisher PANGAEA
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.785348 2025-01-16T22:18:11+00:00 Diatom biostratigraphy, Argon ages and chronology of ODP Hole 183-1138A Bohaty, Steven M Wise, Sherwood W Duncan, Robert A Moore, Leah Wallace, Paul J LATITUDE: -53.551750 * LONGITUDE: 75.974880 * DATE/TIME START: 1999-01-07T23:30:00 * DATE/TIME END: 1999-01-31T06:15:00 2003 application/zip, 6 datasets https://doi.pangaea.de/10.1594/PANGAEA.785348 https://doi.org/10.1594/PANGAEA.785348 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.785348 https://doi.org/10.1594/PANGAEA.785348 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Bohaty, Steven M; Wise, Sherwood W; Duncan, Robert A; Moore, Leah; Wallace, Paul J (2003): Neogene diatom biostratigraphy, tephra stratigraphy, and chronology of ODP Hole 1138A, Kerguelen Plateau. In: Frey, FA; Coffin, MF; Wallace, PJ; Quilty, PG (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 183, 1-53, https://doi.org/10.2973/odp.proc.sr.183.016.2003 183-1138A DRILL Drilling/drill rig Indian Ocean Joides Resolution Leg183 Ocean Drilling Program ODP dataset publication series 2003 ftpangaea https://doi.org/10.1594/PANGAEA.78534810.2973/odp.proc.sr.183.016.2003 2024-07-24T02:31:21Z A thick Neogene section was recovered in the upper ~300 m of Ocean Drilling Program Hole 1138A, drilled on the Central Kerguelen Plateau in the Indian sector of the Southern Ocean. Sediment lithologies consist primarily of mixed carbonate and biosiliceous clays and oozes, with several thin (1-3 cm) tephra horizons. The tephras are glass rich, well sorted, and dominantly trachytic to rhyolitic in composition. Volcaniclastic material in these horizons is interpreted to have originated from Heard Island, 180 km northwest of Site 1138, and was likely emplaced through both primary ash fall and turbiditic, submarine flows. A Neogene age-depth model for Hole 1138A is constructed primarily from 36 diatom biostratigraphic datums. Nannofossil and planktonic foraminifer biostratigraphy provides supporting age information. Additionally, four high-precision 40Ar-39Ar ages are derived from ash and tephra horizons, and these radiometric ages are in close agreement with the biostratigraphic ages. The integrated age-depth model reveals a reasonably complete lower Miocene to upper Pleistocene section in Hole 1138A, with the exception of a ~1-m.y. hiatus at the Miocene/Pliocene boundary. Another possible hiatus is also identified at the Oligocene/Miocene boundary. High Neogene sedimentation rates and the presence of both calcareous and siliceous microfossils, combined with datable tephra horizons, establish Site 1138 as a suitable target for future drilling legs with paleoceanographic objectives. This report also proposes two new diatom species, Fragilariopsis heardensis and Azpeitia harwoodii, from Pliocene strata of Hole 1138A. Other/Unknown Material Heard Island Southern Ocean PANGAEA - Data Publisher for Earth & Environmental Science Southern Ocean Kerguelen Heard Island Indian ENVELOPE(75.974880,75.974880,-53.551750,-53.551750)
spellingShingle 183-1138A
DRILL
Drilling/drill rig
Indian Ocean
Joides Resolution
Leg183
Ocean Drilling Program
ODP
Bohaty, Steven M
Wise, Sherwood W
Duncan, Robert A
Moore, Leah
Wallace, Paul J
Diatom biostratigraphy, Argon ages and chronology of ODP Hole 183-1138A
title Diatom biostratigraphy, Argon ages and chronology of ODP Hole 183-1138A
title_full Diatom biostratigraphy, Argon ages and chronology of ODP Hole 183-1138A
title_fullStr Diatom biostratigraphy, Argon ages and chronology of ODP Hole 183-1138A
title_full_unstemmed Diatom biostratigraphy, Argon ages and chronology of ODP Hole 183-1138A
title_short Diatom biostratigraphy, Argon ages and chronology of ODP Hole 183-1138A
title_sort diatom biostratigraphy, argon ages and chronology of odp hole 183-1138a
topic 183-1138A
DRILL
Drilling/drill rig
Indian Ocean
Joides Resolution
Leg183
Ocean Drilling Program
ODP
topic_facet 183-1138A
DRILL
Drilling/drill rig
Indian Ocean
Joides Resolution
Leg183
Ocean Drilling Program
ODP
url https://doi.pangaea.de/10.1594/PANGAEA.785348
https://doi.org/10.1594/PANGAEA.785348