New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica

New petrographic and geochemical insights from inoceramid bivalve shells of lower Campanian (Marambio Group, James Ross Basin, Antarctica) show that they suffered significant palaeoenvironmental stress just before their disappearance in the southern high latitudes. Inoceramid data have mainly been d...

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Published in:Antarctic Science
Main Authors: Álvaro,Jimenez Berrocoso, Olivero, Eduardo Bernardo, Elorza, Javier
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press
Subjects:
Online Access:http://hdl.handle.net/11336/162483
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/162483 2023-10-09T21:45:35+02:00 New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica Álvaro,Jimenez Berrocoso Olivero, Eduardo Bernardo Elorza, Javier application/pdf http://hdl.handle.net/11336/162483 eng eng Cambridge University Press info:eu-repo/semantics/altIdentifier/doi/10.1017/S0954102006000411 info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/antarctic-science/article/abs/new-petrographic-and-geochemical-insights-on-diagenesis-and-palaeoenvironmental-stress-in-late-cretaceous-inoceramid-shells-from-the-james-ross-basin-antarctica/4A37DF2E7538E879E0F15C7E4B55CF21 http://hdl.handle.net/11336/162483 Álvaro,Jimenez Berrocoso; Olivero, Eduardo Bernardo; Elorza, Javier; New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica; Cambridge University Press; Antarctic Science; 18; 3; 12-2006; 357-376 0954-1020 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ CAMPANIAN CATHODOLUMINESCENCE GEOCHEMISTRY INOCERAMID EXTINCTION LOW MG CALCITE MICROSTRUCTURE SHELL GROWTH https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1017/S0954102006000411 2023-09-24T20:11:17Z New petrographic and geochemical insights from inoceramid bivalve shells of lower Campanian (Marambio Group, James Ross Basin, Antarctica) show that they suffered significant palaeoenvironmental stress just before their disappearance in the southern high latitudes. Inoceramid data have mainly been derived from shell fragments of the large form Antarcticeramus rabotensis Crame & Luther, collected at stratigraphical levels marking the early disappearance of inoceramids in the James Ross Basin (10 m.y. before the Cretaceous/Tertiary boundary in Antarctica). Cathodoluminescence studies and minor and trace element intra-shell variations in A. rabotensis shells, along with their whole shell geochemistry (major, minor, and trace elements, including REE), have revealed evidence of only weak diagenesis but significant palaeoenvironmental stress. The most relevant evidence of such adverse palaeoenvironmental conditions in A. rabotensis shells is reflected by marked growth interruptions in the normal shell layering, including the occurrence of a previously undetected inner aragonitic nacreous layer formed of alternating aragonitic and calcitic sublayers. The weak diagenesis produced characteristic geochemical intra-shell variations which have subsequently been detected in the inoceramid shell microstructure, specially in the inner aragonitic nacreous layer. Fil: Álvaro,Jimenez Berrocoso. Universidad del País Vasco; España Fil: Olivero, Eduardo Bernardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Elorza, Javier. Universidad del País Vasco; España Article in Journal/Newspaper Antarc* Antarctic Science Antarctica CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Austral Argentina Marambio ENVELOPE(-56.750,-56.750,-64.283,-64.283) Olivero ENVELOPE(-63.600,-63.600,-66.133,-66.133) Antarctic Science 18 3 357 376
institution Open Polar
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
op_collection_id ftconicet
language English
topic CAMPANIAN
CATHODOLUMINESCENCE
GEOCHEMISTRY
INOCERAMID EXTINCTION
LOW MG CALCITE MICROSTRUCTURE
SHELL GROWTH
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
spellingShingle CAMPANIAN
CATHODOLUMINESCENCE
GEOCHEMISTRY
INOCERAMID EXTINCTION
LOW MG CALCITE MICROSTRUCTURE
SHELL GROWTH
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Álvaro,Jimenez Berrocoso
Olivero, Eduardo Bernardo
Elorza, Javier
New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica
topic_facet CAMPANIAN
CATHODOLUMINESCENCE
GEOCHEMISTRY
INOCERAMID EXTINCTION
LOW MG CALCITE MICROSTRUCTURE
SHELL GROWTH
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description New petrographic and geochemical insights from inoceramid bivalve shells of lower Campanian (Marambio Group, James Ross Basin, Antarctica) show that they suffered significant palaeoenvironmental stress just before their disappearance in the southern high latitudes. Inoceramid data have mainly been derived from shell fragments of the large form Antarcticeramus rabotensis Crame & Luther, collected at stratigraphical levels marking the early disappearance of inoceramids in the James Ross Basin (10 m.y. before the Cretaceous/Tertiary boundary in Antarctica). Cathodoluminescence studies and minor and trace element intra-shell variations in A. rabotensis shells, along with their whole shell geochemistry (major, minor, and trace elements, including REE), have revealed evidence of only weak diagenesis but significant palaeoenvironmental stress. The most relevant evidence of such adverse palaeoenvironmental conditions in A. rabotensis shells is reflected by marked growth interruptions in the normal shell layering, including the occurrence of a previously undetected inner aragonitic nacreous layer formed of alternating aragonitic and calcitic sublayers. The weak diagenesis produced characteristic geochemical intra-shell variations which have subsequently been detected in the inoceramid shell microstructure, specially in the inner aragonitic nacreous layer. Fil: Álvaro,Jimenez Berrocoso. Universidad del País Vasco; España Fil: Olivero, Eduardo Bernardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Elorza, Javier. Universidad del País Vasco; España
format Article in Journal/Newspaper
author Álvaro,Jimenez Berrocoso
Olivero, Eduardo Bernardo
Elorza, Javier
author_facet Álvaro,Jimenez Berrocoso
Olivero, Eduardo Bernardo
Elorza, Javier
author_sort Álvaro,Jimenez Berrocoso
title New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica
title_short New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica
title_full New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica
title_fullStr New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica
title_full_unstemmed New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica
title_sort new petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in late cretaceous inoceramid shells from the james ross basin, antarctica
publisher Cambridge University Press
url http://hdl.handle.net/11336/162483
long_lat ENVELOPE(-56.750,-56.750,-64.283,-64.283)
ENVELOPE(-63.600,-63.600,-66.133,-66.133)
geographic Austral
Argentina
Marambio
Olivero
geographic_facet Austral
Argentina
Marambio
Olivero
genre Antarc*
Antarctic Science
Antarctica
genre_facet Antarc*
Antarctic Science
Antarctica
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1017/S0954102006000411
info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/antarctic-science/article/abs/new-petrographic-and-geochemical-insights-on-diagenesis-and-palaeoenvironmental-stress-in-late-cretaceous-inoceramid-shells-from-the-james-ross-basin-antarctica/4A37DF2E7538E879E0F15C7E4B55CF21
http://hdl.handle.net/11336/162483
Álvaro,Jimenez Berrocoso; Olivero, Eduardo Bernardo; Elorza, Javier; New petrographic and geochemical insights on diagenesis and palaeoenvironmental stress in Late Cretaceous inoceramid shells from the James Ross Basin, Antarctica; Cambridge University Press; Antarctic Science; 18; 3; 12-2006; 357-376
0954-1020
CONICET Digital
CONICET
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
op_doi https://doi.org/10.1017/S0954102006000411
container_title Antarctic Science
container_volume 18
container_issue 3
container_start_page 357
op_container_end_page 376
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