Early Jurassic coral reef development outside Tethys: an example from western Argentina

Autores
Echevarría, Javier; Harguindeguy, Francisco Martín; Manceñido, Miguel Oscar; Carignano, Ana Paula; Damborenea, Susana Ester
Año de publicación
2024
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Coral-reefs suffered during the end-Triassic extinction event, being scarce during the Early Jurassic. This paper deals with an Early Pliensbachian reef from Puesto Araya, southern Mendoza, Argentina. Five sections were logged ensuring lateral and vertical coverage across the reef outcrop. All determinable associated faunal elements of the reef were recorded. The reef structure was generated by phaceloid and cerioid coralla, and at least two, most likely three, developmental phases were recognized. The first of these shows an early demise, the second a neat vertical succession. The third phase may show the main successional stages or, less likely, may represent a progradation of the previous phase. Phaceloid coralla dominate the colonization stage, and cerioid ones the domination stage; in the diversification stage cerioid morphologies prevail or else; both morphologies occur in similar proportion. All the structural guilds were identified in the Puesto Araya reef, particularly during the diversification stage. Suspension feeders dominate the trophic guilds, though deposit-feeders, herbivores, and carnivores were also present, and cerioid corals might have been zooxanthellate. Although developing some relief over the surrounding sea floor (a true bioherm), the coral growth was constratal. Unlike other coral-reefs, the microfossil assemblage is dominated by nodosarid foraminifers, being most diverse during the diversification stage of the third phase. This reefal structure shares many features with the Sinemurian coral-reefs from the East Pacific realm, but the dominance of cerioid coralla in later seral stages is a novelty of the Puesto Araya reef.
Fil: Echevarría, Javier. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Harguindeguy, Francisco Martín. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Manceñido, Miguel Oscar. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Carignano, Ana Paula. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Damborenea, Susana Ester. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Materia
SCLERACTINIA
EAST PACIFIC REALM
PLIENSBACHIAN
NEUQUÉN BASIN
BIOHERM
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/244248
Acceder
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network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Early Jurassic coral reef development outside Tethys: an example from western ArgentinaEchevarría, JavierHarguindeguy, Francisco MartínManceñido, Miguel OscarCarignano, Ana PaulaDamborenea, Susana EsterSCLERACTINIAEAST PACIFIC REALMPLIENSBACHIANNEUQUÉN BASINBIOHERMhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Coral-reefs suffered during the end-Triassic extinction event, being scarce during the Early Jurassic. This paper deals with an Early Pliensbachian reef from Puesto Araya, southern Mendoza, Argentina. Five sections were logged ensuring lateral and vertical coverage across the reef outcrop. All determinable associated faunal elements of the reef were recorded. The reef structure was generated by phaceloid and cerioid coralla, and at least two, most likely three, developmental phases were recognized. The first of these shows an early demise, the second a neat vertical succession. The third phase may show the main successional stages or, less likely, may represent a progradation of the previous phase. Phaceloid coralla dominate the colonization stage, and cerioid ones the domination stage; in the diversification stage cerioid morphologies prevail or else; both morphologies occur in similar proportion. All the structural guilds were identified in the Puesto Araya reef, particularly during the diversification stage. Suspension feeders dominate the trophic guilds, though deposit-feeders, herbivores, and carnivores were also present, and cerioid corals might have been zooxanthellate. Although developing some relief over the surrounding sea floor (a true bioherm), the coral growth was constratal. Unlike other coral-reefs, the microfossil assemblage is dominated by nodosarid foraminifers, being most diverse during the diversification stage of the third phase. This reefal structure shares many features with the Sinemurian coral-reefs from the East Pacific realm, but the dominance of cerioid coralla in later seral stages is a novelty of the Puesto Araya reef.Fil: Echevarría, Javier. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Harguindeguy, Francisco Martín. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Manceñido, Miguel Oscar. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Carignano, Ana Paula. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Damborenea, Susana Ester. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaScandinavian University Press2024-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/244248Echevarría, Javier; Harguindeguy, Francisco Martín; Manceñido, Miguel Oscar; Carignano, Ana Paula; Damborenea, Susana Ester; Early Jurassic coral reef development outside Tethys: an example from western Argentina; Scandinavian University Press; Lethaia; 2024; 5-2024; 1-270024-1164CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.18261/let.57.3.1info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:39:56Zoai:ri.conicet.gov.ar:11336/244248instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:39:56.384CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Early Jurassic coral reef development outside Tethys: an example from western Argentina
title Early Jurassic coral reef development outside Tethys: an example from western Argentina
spellingShingle Early Jurassic coral reef development outside Tethys: an example from western Argentina
Echevarría, Javier
SCLERACTINIA
EAST PACIFIC REALM
PLIENSBACHIAN
NEUQUÉN BASIN
BIOHERM
title_short Early Jurassic coral reef development outside Tethys: an example from western Argentina
title_full Early Jurassic coral reef development outside Tethys: an example from western Argentina
title_fullStr Early Jurassic coral reef development outside Tethys: an example from western Argentina
title_full_unstemmed Early Jurassic coral reef development outside Tethys: an example from western Argentina
title_sort Early Jurassic coral reef development outside Tethys: an example from western Argentina
dc.creator.none.fl_str_mv Echevarría, Javier
Harguindeguy, Francisco Martín
Manceñido, Miguel Oscar
Carignano, Ana Paula
Damborenea, Susana Ester
author Echevarría, Javier
author_facet Echevarría, Javier
Harguindeguy, Francisco Martín
Manceñido, Miguel Oscar
Carignano, Ana Paula
Damborenea, Susana Ester
author_role author
author2 Harguindeguy, Francisco Martín
Manceñido, Miguel Oscar
Carignano, Ana Paula
Damborenea, Susana Ester
author2_role author
author
author
author
dc.subject.none.fl_str_mv SCLERACTINIA
EAST PACIFIC REALM
PLIENSBACHIAN
NEUQUÉN BASIN
BIOHERM
topic SCLERACTINIA
EAST PACIFIC REALM
PLIENSBACHIAN
NEUQUÉN BASIN
BIOHERM
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Coral-reefs suffered during the end-Triassic extinction event, being scarce during the Early Jurassic. This paper deals with an Early Pliensbachian reef from Puesto Araya, southern Mendoza, Argentina. Five sections were logged ensuring lateral and vertical coverage across the reef outcrop. All determinable associated faunal elements of the reef were recorded. The reef structure was generated by phaceloid and cerioid coralla, and at least two, most likely three, developmental phases were recognized. The first of these shows an early demise, the second a neat vertical succession. The third phase may show the main successional stages or, less likely, may represent a progradation of the previous phase. Phaceloid coralla dominate the colonization stage, and cerioid ones the domination stage; in the diversification stage cerioid morphologies prevail or else; both morphologies occur in similar proportion. All the structural guilds were identified in the Puesto Araya reef, particularly during the diversification stage. Suspension feeders dominate the trophic guilds, though deposit-feeders, herbivores, and carnivores were also present, and cerioid corals might have been zooxanthellate. Although developing some relief over the surrounding sea floor (a true bioherm), the coral growth was constratal. Unlike other coral-reefs, the microfossil assemblage is dominated by nodosarid foraminifers, being most diverse during the diversification stage of the third phase. This reefal structure shares many features with the Sinemurian coral-reefs from the East Pacific realm, but the dominance of cerioid coralla in later seral stages is a novelty of the Puesto Araya reef.
Fil: Echevarría, Javier. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Harguindeguy, Francisco Martín. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Manceñido, Miguel Oscar. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Carignano, Ana Paula. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Damborenea, Susana Ester. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
description Coral-reefs suffered during the end-Triassic extinction event, being scarce during the Early Jurassic. This paper deals with an Early Pliensbachian reef from Puesto Araya, southern Mendoza, Argentina. Five sections were logged ensuring lateral and vertical coverage across the reef outcrop. All determinable associated faunal elements of the reef were recorded. The reef structure was generated by phaceloid and cerioid coralla, and at least two, most likely three, developmental phases were recognized. The first of these shows an early demise, the second a neat vertical succession. The third phase may show the main successional stages or, less likely, may represent a progradation of the previous phase. Phaceloid coralla dominate the colonization stage, and cerioid ones the domination stage; in the diversification stage cerioid morphologies prevail or else; both morphologies occur in similar proportion. All the structural guilds were identified in the Puesto Araya reef, particularly during the diversification stage. Suspension feeders dominate the trophic guilds, though deposit-feeders, herbivores, and carnivores were also present, and cerioid corals might have been zooxanthellate. Although developing some relief over the surrounding sea floor (a true bioherm), the coral growth was constratal. Unlike other coral-reefs, the microfossil assemblage is dominated by nodosarid foraminifers, being most diverse during the diversification stage of the third phase. This reefal structure shares many features with the Sinemurian coral-reefs from the East Pacific realm, but the dominance of cerioid coralla in later seral stages is a novelty of the Puesto Araya reef.
publishDate 2024
dc.date.none.fl_str_mv 2024-05
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/244248
Echevarría, Javier; Harguindeguy, Francisco Martín; Manceñido, Miguel Oscar; Carignano, Ana Paula; Damborenea, Susana Ester; Early Jurassic coral reef development outside Tethys: an example from western Argentina; Scandinavian University Press; Lethaia; 2024; 5-2024; 1-27
0024-1164
CONICET Digital
CONICET
url http://hdl.handle.net/11336/244248
identifier_str_mv Echevarría, Javier; Harguindeguy, Francisco Martín; Manceñido, Miguel Oscar; Carignano, Ana Paula; Damborenea, Susana Ester; Early Jurassic coral reef development outside Tethys: an example from western Argentina; Scandinavian University Press; Lethaia; 2024; 5-2024; 1-27
0024-1164
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.18261/let.57.3.1
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Scandinavian University Press
publisher.none.fl_str_mv Scandinavian University Press
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432

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