Early Cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from El Jagüelito Formation (Sierra Grande, Río Negro, Argentina)

Massive grey limestone blocks containing a fairly diverse but poorly preserved archaeocyath fauna were recovered from a meta-conglomerate bed in the El Jagüelito Formation (Sierra Grande area, Eastern North Patagonian Massif, Río Negro, Argentina). This is the first documented reference of the prese...

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Main Authors: GONZÁLEZ, P.D., TORTELLO, M.F., DAMBORENEA, S.E.
Format: Article in Journal/Newspaper
Language:English
Published: Universitat de Barcelona 2011
Subjects:
Online Access:http://revistes.ub.edu/index.php/GEOACTA/article/view/105.000001650
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spelling ftubarceojs:oai:revistes.ub.edu:article/2089 2023-05-15T13:32:26+02:00 Early Cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from El Jagüelito Formation (Sierra Grande, Río Negro, Argentina) GONZÁLEZ, P.D. TORTELLO, M.F. DAMBORENEA, S.E. 2011-07-14 application/pdf http://revistes.ub.edu/index.php/GEOACTA/article/view/105.000001650 eng eng Universitat de Barcelona http://revistes.ub.edu/index.php/GEOACTA/article/view/105.000001650/4347 http://revistes.ub.edu/index.php/GEOACTA/article/view/105.000001650 Geologica Acta; Vol. 9 No 2 (2011); 159-173 Geologica Acta; Vol. 9 No. 2 (2011); 159-173 Geologica Acta; Vol. 9 Núm. 2 (2011); 159-173 1696-5728 1695-6133 Archaeocyatha Early Cambrian El Jagüelito Formation Low-grade metamorphism North Patagonian Massif Argentina info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2011 ftubarceojs 2022-12-26T13:37:05Z Massive grey limestone blocks containing a fairly diverse but poorly preserved archaeocyath fauna were recovered from a meta-conglomerate bed in the El Jagüelito Formation (Sierra Grande area, Eastern North Patagonian Massif, Río Negro, Argentina). This is the first documented reference of the presence of archaeocyaths in continental Argentina. Seven different taxa were identified, preliminary described and figured. Recrystallization of the skeletons due to regional low-grade metamorphism and deformation of the unit does not allow observation of key detailed features and prevents identification to genera and species. Nevertheless, the specimens studied show general affinities with archaeocyathan assemblages from the Australia-Antarctica palaeobiogeographic province and indicate a middle Early Cambrian (Atdabanian-Botomian) maximum age for the deposition of the El Jagüelito Formation protoliths. The similarities between the North Patagonian Early Paleozoic El Jagüelito Formation and those rocks from Antarctica suggest a geologic and biologic common history of these regions on the same southwest margin of Gondwana during that time. Article in Journal/Newspaper Antarc* Antarctica Revistes Científiques de la Universitat de Barcelona Argentina
institution Open Polar
collection Revistes Científiques de la Universitat de Barcelona
op_collection_id ftubarceojs
language English
topic Archaeocyatha
Early Cambrian
El Jagüelito Formation
Low-grade metamorphism
North Patagonian Massif
Argentina
spellingShingle Archaeocyatha
Early Cambrian
El Jagüelito Formation
Low-grade metamorphism
North Patagonian Massif
Argentina
GONZÁLEZ, P.D.
TORTELLO, M.F.
DAMBORENEA, S.E.
Early Cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from El Jagüelito Formation (Sierra Grande, Río Negro, Argentina)
topic_facet Archaeocyatha
Early Cambrian
El Jagüelito Formation
Low-grade metamorphism
North Patagonian Massif
Argentina
description Massive grey limestone blocks containing a fairly diverse but poorly preserved archaeocyath fauna were recovered from a meta-conglomerate bed in the El Jagüelito Formation (Sierra Grande area, Eastern North Patagonian Massif, Río Negro, Argentina). This is the first documented reference of the presence of archaeocyaths in continental Argentina. Seven different taxa were identified, preliminary described and figured. Recrystallization of the skeletons due to regional low-grade metamorphism and deformation of the unit does not allow observation of key detailed features and prevents identification to genera and species. Nevertheless, the specimens studied show general affinities with archaeocyathan assemblages from the Australia-Antarctica palaeobiogeographic province and indicate a middle Early Cambrian (Atdabanian-Botomian) maximum age for the deposition of the El Jagüelito Formation protoliths. The similarities between the North Patagonian Early Paleozoic El Jagüelito Formation and those rocks from Antarctica suggest a geologic and biologic common history of these regions on the same southwest margin of Gondwana during that time.
format Article in Journal/Newspaper
author GONZÁLEZ, P.D.
TORTELLO, M.F.
DAMBORENEA, S.E.
author_facet GONZÁLEZ, P.D.
TORTELLO, M.F.
DAMBORENEA, S.E.
author_sort GONZÁLEZ, P.D.
title Early Cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from El Jagüelito Formation (Sierra Grande, Río Negro, Argentina)
title_short Early Cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from El Jagüelito Formation (Sierra Grande, Río Negro, Argentina)
title_full Early Cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from El Jagüelito Formation (Sierra Grande, Río Negro, Argentina)
title_fullStr Early Cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from El Jagüelito Formation (Sierra Grande, Río Negro, Argentina)
title_full_unstemmed Early Cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from El Jagüelito Formation (Sierra Grande, Río Negro, Argentina)
title_sort early cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from el jagüelito formation (sierra grande, río negro, argentina)
publisher Universitat de Barcelona
publishDate 2011
url http://revistes.ub.edu/index.php/GEOACTA/article/view/105.000001650
geographic Argentina
geographic_facet Argentina
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Geologica Acta; Vol. 9 No 2 (2011); 159-173
Geologica Acta; Vol. 9 No. 2 (2011); 159-173
Geologica Acta; Vol. 9 Núm. 2 (2011); 159-173
1696-5728
1695-6133
op_relation http://revistes.ub.edu/index.php/GEOACTA/article/view/105.000001650/4347
http://revistes.ub.edu/index.php/GEOACTA/article/view/105.000001650
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