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

An 823 m thick glaciomarine Cenozoic section sitting unconformably on the Lower Devonian Beacon Supergroup was recovered in CRP-3. This paper reviews the chronostratigraphical constraints for the Cenozoic section. Between 3 and 480.27 mbsf 23 unconformity bounded cycles of sediment were recorded. Ea...

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Bibliographic Details
Main Authors: Hannah, Mike J, Florindo, Fabio, Harwood, David M, Fielding, Christopher R
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.510773
https://doi.pangaea.de/10.1594/PANGAEA.510773
id ftdatacite:10.1594/pangaea.510773
record_format openpolar
spelling ftdatacite:10.1594/pangaea.510773 2024-02-27T08:33:31+00:00 Chronostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ... Hannah, Mike J Florindo, Fabio Harwood, David M Fielding, Christopher R 2001 application/zip https://dx.doi.org/10.1594/pangaea.510773 https://doi.pangaea.de/10.1594/PANGAEA.510773 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.510773 2024-02-01T16:08:38Z An 823 m thick glaciomarine Cenozoic section sitting unconformably on the Lower Devonian Beacon Supergroup was recovered in CRP-3. This paper reviews the chronostratigraphical constraints for the Cenozoic section. Between 3 and 480.27 mbsf 23 unconformity bounded cycles of sediment were recorded. Each unconformity is thought to represent a hiatus of uncertain duration. Four magnetozones have been recognised from the Cenozoic section. The record is complex with several 'tiny wiggles'' recorded throughout. Biostratigraphical or Sr ages, which could be used to link these magnetozones to the magnetic polarity time scale are restricted to the upper 190 m of sediment. Two diatom datums (Cavitatus jouseanus at 48.9 mbsf and Rhizosolenica antarctica at 68.60 mbsf), together with five Sr-isotope dates derived from molluscan fragments taken from between 10.88 and 190.29 mbsf indicate an early Oligocene (c. 31 Ma) age for this interval. The appearance of a new species of the bivalve ?Adamussium at about 325 mbsf, ... : Supplement to: Hannah, Mike J; Florindo, Fabio; Harwood, David M; Fielding, Christopher R; CRP Science Team (2001): Chronostratigraphy of the CRP-3 drillhole, Victoria Land Basin, Antarctica. Terra Antartica, 8(4), 615-620 ... 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) Hannah ENVELOPE(-60.613,-60.613,-62.654,-62.654) 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
Hannah, Mike J
Florindo, Fabio
Harwood, David M
Fielding, Christopher R
Chronostratigraphy 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 An 823 m thick glaciomarine Cenozoic section sitting unconformably on the Lower Devonian Beacon Supergroup was recovered in CRP-3. This paper reviews the chronostratigraphical constraints for the Cenozoic section. Between 3 and 480.27 mbsf 23 unconformity bounded cycles of sediment were recorded. Each unconformity is thought to represent a hiatus of uncertain duration. Four magnetozones have been recognised from the Cenozoic section. The record is complex with several 'tiny wiggles'' recorded throughout. Biostratigraphical or Sr ages, which could be used to link these magnetozones to the magnetic polarity time scale are restricted to the upper 190 m of sediment. Two diatom datums (Cavitatus jouseanus at 48.9 mbsf and Rhizosolenica antarctica at 68.60 mbsf), together with five Sr-isotope dates derived from molluscan fragments taken from between 10.88 and 190.29 mbsf indicate an early Oligocene (c. 31 Ma) age for this interval. The appearance of a new species of the bivalve ?Adamussium at about 325 mbsf, ... : Supplement to: Hannah, Mike J; Florindo, Fabio; Harwood, David M; Fielding, Christopher R; CRP Science Team (2001): Chronostratigraphy of the CRP-3 drillhole, Victoria Land Basin, Antarctica. Terra Antartica, 8(4), 615-620 ...
format Article in Journal/Newspaper
author Hannah, Mike J
Florindo, Fabio
Harwood, David M
Fielding, Christopher R
author_facet Hannah, Mike J
Florindo, Fabio
Harwood, David M
Fielding, Christopher R
author_sort Hannah, Mike J
title Chronostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_short Chronostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_full Chronostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_fullStr Chronostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_full_unstemmed Chronostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica ...
title_sort chronostratigraphy of sediment core crp-3 from the ross sea, antarctica ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.510773
https://doi.pangaea.de/10.1594/PANGAEA.510773
long_lat ENVELOPE(-70.467,-70.467,-68.950,-68.950)
ENVELOPE(-60.613,-60.613,-62.654,-62.654)
ENVELOPE(165.817,165.817,-70.733,-70.733)
geographic Cape Roberts
Hannah
Harwood
Ross Sea
Victoria Land
geographic_facet Cape Roberts
Hannah
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.510773
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