Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...

Early Oligocene siliceous microfossils were recovered in the upper c. 193 m of the CRP-3 drillcore. Although abundance and preservation are highly variable through this section, approximately 130 siliceous microfossil taxa were identified, including diatoms, silicoflagellates, ebridians, chrysophyce...

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Bibliographic Details
Main Authors: Harwood, David M, Bohaty, Steven M
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.510765
https://doi.pangaea.de/10.1594/PANGAEA.510765
id ftdatacite:10.1594/pangaea.510765
record_format openpolar
spelling ftdatacite:10.1594/pangaea.510765 2024-02-27T08:33:31+00:00 Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ... Harwood, David M Bohaty, Steven M 2001 application/zip https://dx.doi.org/10.1594/pangaea.510765 https://doi.pangaea.de/10.1594/PANGAEA.510765 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-3 Sampling/drilling from ice Cape Roberts Project CRP Supplementary Publication Series of Datasets Collection article 2001 ftdatacite https://doi.org/10.1594/pangaea.510765 2024-02-01T16:08:38Z Early Oligocene siliceous microfossils were recovered in the upper c. 193 m of the CRP-3 drillcore. Although abundance and preservation are highly variable through this section, approximately 130 siliceous microfossil taxa were identified, including diatoms, silicoflagellates, ebridians, chrysophycean cysts, and endoskeletal dinoflagellates. Well-preserved and abundant assemblages characterize samples in the upper c. 70 m and indicate deposition in a coastal setting with water depths between 50 and 200 m. Abundance fluctuations over narrow intervals in the upper c. 70 mbsf are interpreted to reflect environmental changes that were either conducive or deleterious to growth and preservation of siliceous microfossils. Only poorly-preserved (dissolved, replaced, and/or fragmented) siliceous microfossils are present from c. 70 to 193 mbsf. Diatom biostratigraphy indicates that the CRP-3 section down to c. 193 mbsf is early Oligocene in age. The lack of significant changes in composition of the siliceous ... : Supplement to: Harwood, David M; Bohaty, Steven M (2001): Early Oligocene siliceous microfossil biostratigraphy of Cape Roberts Project Core CRP-3, Victoria Land Basin, Antarctica. Terra Antartica, 8(4), 315-338 ... Article in Journal/Newspaper Antarc* Antarctica antartic* Ross Sea Victoria Land DataCite Metadata Store (German National Library of Science and Technology) Cape Roberts ENVELOPE(-70.467,-70.467,-68.950,-68.950) Harwood ENVELOPE(165.817,165.817,-70.733,-70.733) Ross Sea 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-3
Sampling/drilling from ice
Cape Roberts Project CRP
spellingShingle Core wireline system
CRP-3
Sampling/drilling from ice
Cape Roberts Project CRP
Harwood, David M
Bohaty, Steven M
Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
topic_facet Core wireline system
CRP-3
Sampling/drilling from ice
Cape Roberts Project CRP
description Early Oligocene siliceous microfossils were recovered in the upper c. 193 m of the CRP-3 drillcore. Although abundance and preservation are highly variable through this section, approximately 130 siliceous microfossil taxa were identified, including diatoms, silicoflagellates, ebridians, chrysophycean cysts, and endoskeletal dinoflagellates. Well-preserved and abundant assemblages characterize samples in the upper c. 70 m and indicate deposition in a coastal setting with water depths between 50 and 200 m. Abundance fluctuations over narrow intervals in the upper c. 70 mbsf are interpreted to reflect environmental changes that were either conducive or deleterious to growth and preservation of siliceous microfossils. Only poorly-preserved (dissolved, replaced, and/or fragmented) siliceous microfossils are present from c. 70 to 193 mbsf. Diatom biostratigraphy indicates that the CRP-3 section down to c. 193 mbsf is early Oligocene in age. The lack of significant changes in composition of the siliceous ... : Supplement to: Harwood, David M; Bohaty, Steven M (2001): Early Oligocene siliceous microfossil biostratigraphy of Cape Roberts Project Core CRP-3, Victoria Land Basin, Antarctica. Terra Antartica, 8(4), 315-338 ...
format Article in Journal/Newspaper
author Harwood, David M
Bohaty, Steven M
author_facet Harwood, David M
Bohaty, Steven M
author_sort Harwood, David M
title Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_short Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_full Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_fullStr Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_full_unstemmed Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_sort biostratigraphy of sediment core crp-3 from the ross sea, antarctica ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.510765
https://doi.pangaea.de/10.1594/PANGAEA.510765
long_lat ENVELOPE(-70.467,-70.467,-68.950,-68.950)
ENVELOPE(165.817,165.817,-70.733,-70.733)
geographic Cape Roberts
Harwood
Ross Sea
Victoria Land
geographic_facet Cape Roberts
Harwood
Ross Sea
Victoria Land
genre Antarc*
Antarctica
antartic*
Ross Sea
Victoria Land
genre_facet Antarc*
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.510765
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