Investigation of Quaternary foraminifera in sediment core CRP-1 from the Ross Sea, Antarctica

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Auteurs principaux: Webb, Peter-Noel, Strong, C Percy
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1998
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_version_ 1867171355497070592
author Webb, Peter-Noel
Strong, C Percy
author_facet Webb, Peter-Noel
Strong, C Percy
collection Datos científicos de ciencias marinas y ambientales
contents Foraminifera are examined in twenty-six samples from a 44 metre succession of Quaternary glacial sediments recovered from the CRP-1 drillhole on Roberts Ridge, southwestern Ross Sea, Antarctica. In situ marine assemblages were documented in at least three of the six lithostratigraphic units, and it is likely that the remaining three interbedded diamicton units are also marine in origin. Peak foraminiferal diversities are documented in Unit 3.1 (73 species) and Unit 2.2 (32 species). Calcareous benthics dominate the assemblages, but may be accompanied by abundant occurrences of the planktonic Neogloboquadrina pachyderma. Low diversity agglutinated faunas appear in the uppermost strata of Units 4.1 and 2.2. A close relationship between lithofacics and foraminiferal biofacies points to marine environments that alternated between proximity to and distance from active glaciers and iceshelf fronts, with associated variations in salinity, sea-surface ice cover and the levels of rainout from debris-laden ice.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_510745
institution PANGAEA
language en
publishDate 1998
publisher PANGAEA
record_format pangaea
spellingShingle Investigation of Quaternary foraminifera in sediment core CRP-1 from the Ross Sea, Antarctica
Webb, Peter-Noel
Strong, C Percy
16 km ENE Cape Roberts; Cape Roberts Project; Core wireline system; CRP; CRP-1; CRP-1__Campaign; CWS; off Cape Roberts, Ross Sea, Antarctica; Sampling/drilling ice
Foraminifera are examined in twenty-six samples from a 44 metre succession of Quaternary glacial sediments recovered from the CRP-1 drillhole on Roberts Ridge, southwestern Ross Sea, Antarctica. In situ marine assemblages were documented in at least three of the six lithostratigraphic units, and it is likely that the remaining three interbedded diamicton units are also marine in origin. Peak foraminiferal diversities are documented in Unit 3.1 (73 species) and Unit 2.2 (32 species). Calcareous benthics dominate the assemblages, but may be accompanied by abundant occurrences of the planktonic Neogloboquadrina pachyderma. Low diversity agglutinated faunas appear in the uppermost strata of Units 4.1 and 2.2. A close relationship between lithofacics and foraminiferal biofacies points to marine environments that alternated between proximity to and distance from active glaciers and iceshelf fronts, with associated variations in salinity, sea-surface ice cover and the levels of rainout from debris-laden ice.
title Investigation of Quaternary foraminifera in sediment core CRP-1 from the Ross Sea, Antarctica
topic 16 km ENE Cape Roberts; Cape Roberts Project; Core wireline system; CRP; CRP-1; CRP-1__Campaign; CWS; off Cape Roberts, Ross Sea, Antarctica; Sampling/drilling ice
url https://doi.org/10.1594/PANGAEA.510745