Biostratigraphy and palaeoenvironment of the Agrio Formation (Lower Cretaceous), Mendoza Province, Neuquén Basin, Argentina

A bioestratigraphical and palaeoenvironmental study of the Agrio Formation, at the Cuesta del Chihuido section, southern Mendoza Province (35°45′S/69°34′W), Argentina, is presented. Thirty seven species of nannofossils, thirty four of foraminifers and six of ostracods have been recognized. Nannofoss...

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Publicado: 2006
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07160208_v33_n1_p47_Ballent
http://hdl.handle.net/20.500.12110/paper_07160208_v33_n1_p47_Ballent
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spelling paper:paper_07160208_v33_n1_p47_Ballent2023-06-08T15:42:52Z Biostratigraphy and palaeoenvironment of the Agrio Formation (Lower Cretaceous), Mendoza Province, Neuquén Basin, Argentina Agrio Formation Argentina Biostratigraphy Calcareous microfossils Lower Cretaceous Palaeoenvironment Biodiversity Eutrophication Geology Geomorphology Marine biology Sandstone Silt benthic foraminifera biostratigraphy Cretaceous microfossil nanofossil paleoenvironment Argentina Mendoza South America Epistomina Foraminifera Lagenidae Ostracoda Polymorphinidae Spirillinidae A bioestratigraphical and palaeoenvironmental study of the Agrio Formation, at the Cuesta del Chihuido section, southern Mendoza Province (35°45′S/69°34′W), Argentina, is presented. Thirty seven species of nannofossils, thirty four of foraminifers and six of ostracods have been recognized. Nannofossils association corresponding to Zones CC4A y CC4B indicates an Upper Valanginian-Upper Hauterivian age. At the base of the section, the presence of the benthonic foraminifer Epistomina loncochensis Ballent and radiolaria suggests eutrophic conditions of surface waters and oxygen depressed sea-bottom conditions. In the middle part of the section, diversity of lagenid foraminifers and nannofossils indicates a shelf and nearshore environment with clear and well-oxygenated waters. Abundant polymorphinids, spirillinids and involitinids towards the top of the section corroborate a general regressive tendency. Mudstones and silty-sandstone intercalations containing allochthonous adherent foraminifers and adult carapaces of cytheroid ostracods represent distal storm deposits. © 2006 Servicio Nacional de Geologí y Minería. 2006 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07160208_v33_n1_p47_Ballent http://hdl.handle.net/20.500.12110/paper_07160208_v33_n1_p47_Ballent
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Agrio Formation
Argentina
Biostratigraphy
Calcareous microfossils
Lower Cretaceous
Palaeoenvironment
Biodiversity
Eutrophication
Geology
Geomorphology
Marine biology
Sandstone
Silt
benthic foraminifera
biostratigraphy
Cretaceous
microfossil
nanofossil
paleoenvironment
Argentina
Mendoza
South America
Epistomina
Foraminifera
Lagenidae
Ostracoda
Polymorphinidae
Spirillinidae
spellingShingle Agrio Formation
Argentina
Biostratigraphy
Calcareous microfossils
Lower Cretaceous
Palaeoenvironment
Biodiversity
Eutrophication
Geology
Geomorphology
Marine biology
Sandstone
Silt
benthic foraminifera
biostratigraphy
Cretaceous
microfossil
nanofossil
paleoenvironment
Argentina
Mendoza
South America
Epistomina
Foraminifera
Lagenidae
Ostracoda
Polymorphinidae
Spirillinidae
Biostratigraphy and palaeoenvironment of the Agrio Formation (Lower Cretaceous), Mendoza Province, Neuquén Basin, Argentina
topic_facet Agrio Formation
Argentina
Biostratigraphy
Calcareous microfossils
Lower Cretaceous
Palaeoenvironment
Biodiversity
Eutrophication
Geology
Geomorphology
Marine biology
Sandstone
Silt
benthic foraminifera
biostratigraphy
Cretaceous
microfossil
nanofossil
paleoenvironment
Argentina
Mendoza
South America
Epistomina
Foraminifera
Lagenidae
Ostracoda
Polymorphinidae
Spirillinidae
description A bioestratigraphical and palaeoenvironmental study of the Agrio Formation, at the Cuesta del Chihuido section, southern Mendoza Province (35°45′S/69°34′W), Argentina, is presented. Thirty seven species of nannofossils, thirty four of foraminifers and six of ostracods have been recognized. Nannofossils association corresponding to Zones CC4A y CC4B indicates an Upper Valanginian-Upper Hauterivian age. At the base of the section, the presence of the benthonic foraminifer Epistomina loncochensis Ballent and radiolaria suggests eutrophic conditions of surface waters and oxygen depressed sea-bottom conditions. In the middle part of the section, diversity of lagenid foraminifers and nannofossils indicates a shelf and nearshore environment with clear and well-oxygenated waters. Abundant polymorphinids, spirillinids and involitinids towards the top of the section corroborate a general regressive tendency. Mudstones and silty-sandstone intercalations containing allochthonous adherent foraminifers and adult carapaces of cytheroid ostracods represent distal storm deposits. © 2006 Servicio Nacional de Geologí y Minería.
title Biostratigraphy and palaeoenvironment of the Agrio Formation (Lower Cretaceous), Mendoza Province, Neuquén Basin, Argentina
title_short Biostratigraphy and palaeoenvironment of the Agrio Formation (Lower Cretaceous), Mendoza Province, Neuquén Basin, Argentina
title_full Biostratigraphy and palaeoenvironment of the Agrio Formation (Lower Cretaceous), Mendoza Province, Neuquén Basin, Argentina
title_fullStr Biostratigraphy and palaeoenvironment of the Agrio Formation (Lower Cretaceous), Mendoza Province, Neuquén Basin, Argentina
title_full_unstemmed Biostratigraphy and palaeoenvironment of the Agrio Formation (Lower Cretaceous), Mendoza Province, Neuquén Basin, Argentina
title_sort biostratigraphy and palaeoenvironment of the agrio formation (lower cretaceous), mendoza province, neuquén basin, argentina
publishDate 2006
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07160208_v33_n1_p47_Ballent
http://hdl.handle.net/20.500.12110/paper_07160208_v33_n1_p47_Ballent
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