Investigation of microfossils on sediment core CRP-2 from the Ross Sea, Antarctica ...

Marine diatoms are the primary biostratigraphical and paleoenvironmental tool for interpreting the upper Palaeogene and lower Neogene strata recovered during the second drilling season of the Cape Roberts Project at site CRP-2 in the western Ross Sea, Antarctica. Silicoflagellates, ebridians, and a...

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Main Authors: Scherer, Reed P, Bohaty, Steven M, Harwood, David M
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2000
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.510754
https://doi.pangaea.de/10.1594/PANGAEA.510754
id ftdatacite:10.1594/pangaea.510754
record_format openpolar
spelling ftdatacite:10.1594/pangaea.510754 2024-02-27T08:33:31+00:00 Investigation of microfossils on sediment core CRP-2 from the Ross Sea, Antarctica ... Scherer, Reed P Bohaty, Steven M Harwood, David M 2000 application/zip https://dx.doi.org/10.1594/pangaea.510754 https://doi.pangaea.de/10.1594/PANGAEA.510754 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Core wireline system CRP-2 Sampling/drilling from ice Cape Roberts Project CRP Supplementary Publication Series of Datasets Collection article 2000 ftdatacite https://doi.org/10.1594/pangaea.510754 2024-02-01T16:08:38Z Marine diatoms are the primary biostratigraphical and paleoenvironmental tool for interpreting the upper Palaeogene and lower Neogene strata recovered during the second drilling season of the Cape Roberts Project at site CRP-2 in the western Ross Sea, Antarctica. Silicoflagellates, ebridians, and a chrysophyte cyst provide supporting biostratigraphical information. More than 100 dominantly planktic diatom taxa are recognised. Of these, more than 30 are treated informally, pending SEM examination and formal description. Many other taxa are noted only to generic level. Lower Oligocene (c. 31 Ma) through lower Miocene (c. 18.5 Ma) diatoms occur from 28 mbsf down to 565 mbsf. Below this level, to the bottom of the hole at 624.15 mbsf, diatom assemblages are poorly-preserved and many samples are barren. A biostratigraphic zonal framework, consisting of ten diatom zones, is proposed for the Antarctic continental shelf. Ages inferred from the diatom biostratigraphy correspond well with geochronological data from ... : Supplement to: Scherer, Reed P; Bohaty, Steven M; Harwood, David M (2000): Oligocene and lower Miocene siliceous microfossil biostratigraphy of Cape Roberts Project Core CRP-2/2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(4), 417-442 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica antartic* Ross Sea Victoria Land DataCite Metadata Store (German National Library of Science and Technology) Antarctic Cape Roberts ENVELOPE(-70.467,-70.467,-68.950,-68.950) Harwood ENVELOPE(165.817,165.817,-70.733,-70.733) Ross Sea The Antarctic Victoria Land
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Core wireline system
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
spellingShingle Core wireline system
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
Scherer, Reed P
Bohaty, Steven M
Harwood, David M
Investigation of microfossils on sediment core CRP-2 from the Ross Sea, Antarctica ...
topic_facet Core wireline system
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
description Marine diatoms are the primary biostratigraphical and paleoenvironmental tool for interpreting the upper Palaeogene and lower Neogene strata recovered during the second drilling season of the Cape Roberts Project at site CRP-2 in the western Ross Sea, Antarctica. Silicoflagellates, ebridians, and a chrysophyte cyst provide supporting biostratigraphical information. More than 100 dominantly planktic diatom taxa are recognised. Of these, more than 30 are treated informally, pending SEM examination and formal description. Many other taxa are noted only to generic level. Lower Oligocene (c. 31 Ma) through lower Miocene (c. 18.5 Ma) diatoms occur from 28 mbsf down to 565 mbsf. Below this level, to the bottom of the hole at 624.15 mbsf, diatom assemblages are poorly-preserved and many samples are barren. A biostratigraphic zonal framework, consisting of ten diatom zones, is proposed for the Antarctic continental shelf. Ages inferred from the diatom biostratigraphy correspond well with geochronological data from ... : Supplement to: Scherer, Reed P; Bohaty, Steven M; Harwood, David M (2000): Oligocene and lower Miocene siliceous microfossil biostratigraphy of Cape Roberts Project Core CRP-2/2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(4), 417-442 ...
format Article in Journal/Newspaper
author Scherer, Reed P
Bohaty, Steven M
Harwood, David M
author_facet Scherer, Reed P
Bohaty, Steven M
Harwood, David M
author_sort Scherer, Reed P
title Investigation of microfossils on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_short Investigation of microfossils on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_full Investigation of microfossils on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_fullStr Investigation of microfossils on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_full_unstemmed Investigation of microfossils on sediment core CRP-2 from the Ross Sea, Antarctica ...
title_sort investigation of microfossils on sediment core crp-2 from the ross sea, antarctica ...
publisher PANGAEA
publishDate 2000
url https://dx.doi.org/10.1594/pangaea.510754
https://doi.pangaea.de/10.1594/PANGAEA.510754
long_lat ENVELOPE(-70.467,-70.467,-68.950,-68.950)
ENVELOPE(165.817,165.817,-70.733,-70.733)
geographic Antarctic
Cape Roberts
Harwood
Ross Sea
The Antarctic
Victoria Land
geographic_facet Antarctic
Cape Roberts
Harwood
Ross Sea
The Antarctic
Victoria Land
genre Antarc*
Antarctic
Antarctica
antartic*
Ross Sea
Victoria Land
genre_facet Antarc*
Antarctic
Antarctica
antartic*
Ross Sea
Victoria Land
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.510754
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