Coniacian ammonites from James Ross Island, Antarctica

The Cenomanian-Santonian biostratigraphy of the James Ross Basin, north-eastern Antarctic Peninsula is in need of comprehensive revision. This is being achieved by the systematic re-investigation of a series of key reference sections on the north-west coast of James Ross Island, with the first of th...

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Published in:Cretaceous Research
Main Authors: Kennedy, W, Crame, J, Bengtson, P, Thomson, M
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://doi.org/10.1016/j.cretres.2006.08.006
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:63c803a6-0b8b-4f50-9465-82f74b008f80 2024-10-06T13:42:32+00:00 Coniacian ammonites from James Ross Island, Antarctica Kennedy, W Crame, J Bengtson, P Thomson, M 2016-07-28 https://doi.org/10.1016/j.cretres.2006.08.006 https://ora.ox.ac.uk/objects/uuid:63c803a6-0b8b-4f50-9465-82f74b008f80 eng eng doi:10.1016/j.cretres.2006.08.006 https://ora.ox.ac.uk/objects/uuid:63c803a6-0b8b-4f50-9465-82f74b008f80 https://doi.org/10.1016/j.cretres.2006.08.006 info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford https://doi.org/10.1016/j.cretres.2006.08.006 2024-09-06T07:47:35Z The Cenomanian-Santonian biostratigraphy of the James Ross Basin, north-eastern Antarctic Peninsula is in need of comprehensive revision. This is being achieved by the systematic re-investigation of a series of key reference sections on the north-west coast of James Ross Island, with the first of these being located in the vicinity of Brandy Bay. A new suite of 10 ammonite taxa from the uppermost Whisky Bay and Hidden Lake Formations at this locality has overwhelming Coniacian age affinities. It comprises representatives from the Tetragonitidae and Gaudryceratidae, together with the stratigraphically earliest representative of the Kossmaticeratidae and the three earliest Pachydiscidae species from the James Ross Basin. Some fragmentary specimens are assigned to the Collignoniceratidae, and various heteromorphs to the Nostoceratidae, Diplomoceratidae and Baculitidae. The one new taxon described herein is Gaudryceras (Gaudryceras) strictum sp. nov. This ammonite fauna represents an important precursor to the much more prolific assemblages that occur in the overlying Santa Marta and López de Bertodano formations (latest Coniacian-Maastrichtian). It shows some affinities to the Madagascan Coniacian ammonite fauna, and offers an opportunity for strengthening Late Cretaceous biostratigraphic correlations between the northern and southern hemispheres. © 2007 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica James Ross Island Ross Island ORA - Oxford University Research Archive Antarctic Antarctic Peninsula Brandy Bay ENVELOPE(-58.000,-58.000,-63.700,-63.700) Hidden Lake ENVELOPE(63.048,63.048,-67.687,-67.687) Ross Island Whisky Bay ENVELOPE(-58.134,-58.134,-63.889,-63.889) Cretaceous Research 28 3 509 531
institution Open Polar
collection ORA - Oxford University Research Archive
op_collection_id ftuloxford
language English
description The Cenomanian-Santonian biostratigraphy of the James Ross Basin, north-eastern Antarctic Peninsula is in need of comprehensive revision. This is being achieved by the systematic re-investigation of a series of key reference sections on the north-west coast of James Ross Island, with the first of these being located in the vicinity of Brandy Bay. A new suite of 10 ammonite taxa from the uppermost Whisky Bay and Hidden Lake Formations at this locality has overwhelming Coniacian age affinities. It comprises representatives from the Tetragonitidae and Gaudryceratidae, together with the stratigraphically earliest representative of the Kossmaticeratidae and the three earliest Pachydiscidae species from the James Ross Basin. Some fragmentary specimens are assigned to the Collignoniceratidae, and various heteromorphs to the Nostoceratidae, Diplomoceratidae and Baculitidae. The one new taxon described herein is Gaudryceras (Gaudryceras) strictum sp. nov. This ammonite fauna represents an important precursor to the much more prolific assemblages that occur in the overlying Santa Marta and López de Bertodano formations (latest Coniacian-Maastrichtian). It shows some affinities to the Madagascan Coniacian ammonite fauna, and offers an opportunity for strengthening Late Cretaceous biostratigraphic correlations between the northern and southern hemispheres. © 2007 Elsevier Ltd. All rights reserved.
format Article in Journal/Newspaper
author Kennedy, W
Crame, J
Bengtson, P
Thomson, M
spellingShingle Kennedy, W
Crame, J
Bengtson, P
Thomson, M
Coniacian ammonites from James Ross Island, Antarctica
author_facet Kennedy, W
Crame, J
Bengtson, P
Thomson, M
author_sort Kennedy, W
title Coniacian ammonites from James Ross Island, Antarctica
title_short Coniacian ammonites from James Ross Island, Antarctica
title_full Coniacian ammonites from James Ross Island, Antarctica
title_fullStr Coniacian ammonites from James Ross Island, Antarctica
title_full_unstemmed Coniacian ammonites from James Ross Island, Antarctica
title_sort coniacian ammonites from james ross island, antarctica
publishDate 2016
url https://doi.org/10.1016/j.cretres.2006.08.006
https://ora.ox.ac.uk/objects/uuid:63c803a6-0b8b-4f50-9465-82f74b008f80
long_lat ENVELOPE(-58.000,-58.000,-63.700,-63.700)
ENVELOPE(63.048,63.048,-67.687,-67.687)
ENVELOPE(-58.134,-58.134,-63.889,-63.889)
geographic Antarctic
Antarctic Peninsula
Brandy Bay
Hidden Lake
Ross Island
Whisky Bay
geographic_facet Antarctic
Antarctic Peninsula
Brandy Bay
Hidden Lake
Ross Island
Whisky Bay
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
James Ross Island
Ross Island
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
James Ross Island
Ross Island
op_relation doi:10.1016/j.cretres.2006.08.006
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https://doi.org/10.1016/j.cretres.2006.08.006
op_rights info:eu-repo/semantics/embargoedAccess
op_doi https://doi.org/10.1016/j.cretres.2006.08.006
container_title Cretaceous Research
container_volume 28
container_issue 3
container_start_page 509
op_container_end_page 531
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