Foraminifera from the Upper Cretaceous of northern James Ross Island (Antarctica): a preliminary report
The Cretaceous biostratigraphy of the James Ross Island region is generally based on palynomorphs and macrofossils (bivalves, ammonites). During geological mapping of the northern James Ross Island a number of samples from Upper Cretaceous lithologies were gathered to test the presence of foraminife...
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ftmasarykunivojs:oai:ojs.journals.muni.cz:article/12808 2023-05-15T13:46:41+02:00 Foraminifera from the Upper Cretaceous of northern James Ross Island (Antarctica): a preliminary report Hradecká, Lenka Vodrážka, Radek Nývlt, Daniel 2011-06-01 application/pdf http://journals.muni.cz/CPR/article/view/12808 eng eng Masaryk Univerzity http://journals.muni.cz/CPR/article/view/12808/11121 http://journals.muni.cz/CPR/article/view/12808 Copyright (c) 2020 Czech Polar Reports https://creativecommons.org/licenses/by-nc-nd/4.0 CC-BY-NC-ND Czech Polar Reports; Vol 1 No 2 (2011); 88-95 Czech Polar Reports; Vol. 1 No. 2 (2011); 88-95 1805-0697 1805-0689 James Ross Basin Upper Cretaceous Kotick Point Whisky Bay Santa Marta Hidden Lake Formations Foraminifera biostratigraphy lithology info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2011 ftmasarykunivojs 2022-06-26T10:16:32Z The Cretaceous biostratigraphy of the James Ross Island region is generally based on palynomorphs and macrofossils (bivalves, ammonites). During geological mapping of the northern James Ross Island a number of samples from Upper Cretaceous lithologies were gathered to test the presence of foraminifers as a possible tool for stratigraphic evaluation of Upper Cretaceous strata. Limited number of samples did not provide foraminiferal content large enough to give relevant information for biostratigraphic conclusions. Samples from older sediments of Whisky Bay and Kotick Point formations (Albian – Turonian) were either not fossiliferous or contained scarce specimens of agglutinated foraminifers. Foraminiferal assemblages from younger sediments of Hidden Lake and Santa Marta formations (Coniacian – Campanian) contained species with both agglutinated and calcareous types of tests. Many of studied marine sediments were barren of foraminifers, probably due to late diagenetic secondary decalcification. Taxonomy of low-diversified assemblages was carried out and a biostratigraphical and palaeobiogeographical significance discussed. Article in Journal/Newspaper Antarc* Antarctica James Ross Island Ross Island Masaryk University Journals Ross Island Hidden Lake ENVELOPE(63.048,63.048,-67.687,-67.687) Whisky Bay ENVELOPE(-58.134,-58.134,-63.889,-63.889) Kotick ENVELOPE(-58.325,-58.325,-63.989,-63.989) Kotick Point ENVELOPE(-58.367,-58.367,-64.000,-64.000) |
institution |
Open Polar |
collection |
Masaryk University Journals |
op_collection_id |
ftmasarykunivojs |
language |
English |
topic |
James Ross Basin Upper Cretaceous Kotick Point Whisky Bay Santa Marta Hidden Lake Formations Foraminifera biostratigraphy lithology |
spellingShingle |
James Ross Basin Upper Cretaceous Kotick Point Whisky Bay Santa Marta Hidden Lake Formations Foraminifera biostratigraphy lithology Hradecká, Lenka Vodrážka, Radek Nývlt, Daniel Foraminifera from the Upper Cretaceous of northern James Ross Island (Antarctica): a preliminary report |
topic_facet |
James Ross Basin Upper Cretaceous Kotick Point Whisky Bay Santa Marta Hidden Lake Formations Foraminifera biostratigraphy lithology |
description |
The Cretaceous biostratigraphy of the James Ross Island region is generally based on palynomorphs and macrofossils (bivalves, ammonites). During geological mapping of the northern James Ross Island a number of samples from Upper Cretaceous lithologies were gathered to test the presence of foraminifers as a possible tool for stratigraphic evaluation of Upper Cretaceous strata. Limited number of samples did not provide foraminiferal content large enough to give relevant information for biostratigraphic conclusions. Samples from older sediments of Whisky Bay and Kotick Point formations (Albian – Turonian) were either not fossiliferous or contained scarce specimens of agglutinated foraminifers. Foraminiferal assemblages from younger sediments of Hidden Lake and Santa Marta formations (Coniacian – Campanian) contained species with both agglutinated and calcareous types of tests. Many of studied marine sediments were barren of foraminifers, probably due to late diagenetic secondary decalcification. Taxonomy of low-diversified assemblages was carried out and a biostratigraphical and palaeobiogeographical significance discussed. |
format |
Article in Journal/Newspaper |
author |
Hradecká, Lenka Vodrážka, Radek Nývlt, Daniel |
author_facet |
Hradecká, Lenka Vodrážka, Radek Nývlt, Daniel |
author_sort |
Hradecká, Lenka |
title |
Foraminifera from the Upper Cretaceous of northern James Ross Island (Antarctica): a preliminary report |
title_short |
Foraminifera from the Upper Cretaceous of northern James Ross Island (Antarctica): a preliminary report |
title_full |
Foraminifera from the Upper Cretaceous of northern James Ross Island (Antarctica): a preliminary report |
title_fullStr |
Foraminifera from the Upper Cretaceous of northern James Ross Island (Antarctica): a preliminary report |
title_full_unstemmed |
Foraminifera from the Upper Cretaceous of northern James Ross Island (Antarctica): a preliminary report |
title_sort |
foraminifera from the upper cretaceous of northern james ross island (antarctica): a preliminary report |
publisher |
Masaryk Univerzity |
publishDate |
2011 |
url |
http://journals.muni.cz/CPR/article/view/12808 |
long_lat |
ENVELOPE(63.048,63.048,-67.687,-67.687) ENVELOPE(-58.134,-58.134,-63.889,-63.889) ENVELOPE(-58.325,-58.325,-63.989,-63.989) ENVELOPE(-58.367,-58.367,-64.000,-64.000) |
geographic |
Ross Island Hidden Lake Whisky Bay Kotick Kotick Point |
geographic_facet |
Ross Island Hidden Lake Whisky Bay Kotick Kotick Point |
genre |
Antarc* Antarctica James Ross Island Ross Island |
genre_facet |
Antarc* Antarctica James Ross Island Ross Island |
op_source |
Czech Polar Reports; Vol 1 No 2 (2011); 88-95 Czech Polar Reports; Vol. 1 No. 2 (2011); 88-95 1805-0697 1805-0689 |
op_relation |
http://journals.muni.cz/CPR/article/view/12808/11121 http://journals.muni.cz/CPR/article/view/12808 |
op_rights |
Copyright (c) 2020 Czech Polar Reports https://creativecommons.org/licenses/by-nc-nd/4.0 |
op_rightsnorm |
CC-BY-NC-ND |
_version_ |
1766245066676895744 |