Taphofacies and biofacies of the Vaca Muerta Formation in the southern mendoza sector of the neuquén basin: paleoecological, sedimentological and stratigraphic implications

Taphonomic and paleocological studies of fossil assemblages from the transgressive and highstand succession of the Vaca Muerta Formation (lower Tithonian to upper Valanginian) in Loncoche Creek, Rahue Creek and Cuesta del Chihuido, Mendoza province, was carried out. A range of paleoenvironments that...

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Autores principales: Kietzmann, D.A., Palma, R.M.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00027014_v46_n2_p321_Kietzmann
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spelling todo:paper_00027014_v46_n2_p321_Kietzmann2023-10-03T13:53:06Z Taphofacies and biofacies of the Vaca Muerta Formation in the southern mendoza sector of the neuquén basin: paleoecological, sedimentological and stratigraphic implications Kietzmann, D.A. Palma, R.M. Jurassic-cretaceous Outer ramp Taphofacies. Biofacies Vaca muerta formation ammonite biofacies biostratigraphy bioturbation bivalve brachiopod Cretaceous fossil assemblage gastropod highstand Jurassic oxygenation paleoecology paleoenvironment pavement sedimentation rate sedimentology species diversity substrate taphonomy Argentina Mendoza South America Ammonoidea Bivalvia Brachiopoda Discinisca Epistominidae Foraminifera Gastropoda Inoceramidae Mollusca Ostreidae Pectinidae Serpulidae Taphonomic and paleocological studies of fossil assemblages from the transgressive and highstand succession of the Vaca Muerta Formation (lower Tithonian to upper Valanginian) in Loncoche Creek, Rahue Creek and Cuesta del Chihuido, Mendoza province, was carried out. A range of paleoenvironments that include mid, outer and basin deposits of carbonate ramp have been determinated based on integrated studies of taphofacies, biofacies, lithofacies and microfacies. In the mid ramp zone were recognized the following taphofacies: two types of autoparabiostromes, as well as concentrations of bivalves, gastropods and serpulids. Meanwhile, biofacies included autobiostromes rich in grypheids and serpulids. In the outer ramp zone were recognized two types of parabiostromes, ammonite and aptychus pavements, bioclastic detritus, molluscs and brachiopods pavements, besides bioturbated nodular limestones and truncated ammonites. In this zone, biofacies are characterized by high diversity including: Lingularia-Discinisca, infaunal bivalves, epistominid foraminifers, filament bivalves, besides of pectinidae, oysters and inoceramid bivalves, hardgrounds and microbial mats. Taphofacies and biofacies data allow to estimate relative sea level changes, sedimentation rates, substrate consistency, oxygenation, nutrient levels and productivity. © Asociación Paleontológica Argentina. Fil:Kietzmann, D.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Palma, R.M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00027014_v46_n2_p321_Kietzmann
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Jurassic-cretaceous
Outer ramp
Taphofacies. Biofacies
Vaca muerta formation
ammonite
biofacies
biostratigraphy
bioturbation
bivalve
brachiopod
Cretaceous
fossil assemblage
gastropod
highstand
Jurassic
oxygenation
paleoecology
paleoenvironment
pavement
sedimentation rate
sedimentology
species diversity
substrate
taphonomy
Argentina
Mendoza
South America
Ammonoidea
Bivalvia
Brachiopoda
Discinisca
Epistominidae
Foraminifera
Gastropoda
Inoceramidae
Mollusca
Ostreidae
Pectinidae
Serpulidae
spellingShingle Jurassic-cretaceous
Outer ramp
Taphofacies. Biofacies
Vaca muerta formation
ammonite
biofacies
biostratigraphy
bioturbation
bivalve
brachiopod
Cretaceous
fossil assemblage
gastropod
highstand
Jurassic
oxygenation
paleoecology
paleoenvironment
pavement
sedimentation rate
sedimentology
species diversity
substrate
taphonomy
Argentina
Mendoza
South America
Ammonoidea
Bivalvia
Brachiopoda
Discinisca
Epistominidae
Foraminifera
Gastropoda
Inoceramidae
Mollusca
Ostreidae
Pectinidae
Serpulidae
Kietzmann, D.A.
Palma, R.M.
Taphofacies and biofacies of the Vaca Muerta Formation in the southern mendoza sector of the neuquén basin: paleoecological, sedimentological and stratigraphic implications
topic_facet Jurassic-cretaceous
Outer ramp
Taphofacies. Biofacies
Vaca muerta formation
ammonite
biofacies
biostratigraphy
bioturbation
bivalve
brachiopod
Cretaceous
fossil assemblage
gastropod
highstand
Jurassic
oxygenation
paleoecology
paleoenvironment
pavement
sedimentation rate
sedimentology
species diversity
substrate
taphonomy
Argentina
Mendoza
South America
Ammonoidea
Bivalvia
Brachiopoda
Discinisca
Epistominidae
Foraminifera
Gastropoda
Inoceramidae
Mollusca
Ostreidae
Pectinidae
Serpulidae
description Taphonomic and paleocological studies of fossil assemblages from the transgressive and highstand succession of the Vaca Muerta Formation (lower Tithonian to upper Valanginian) in Loncoche Creek, Rahue Creek and Cuesta del Chihuido, Mendoza province, was carried out. A range of paleoenvironments that include mid, outer and basin deposits of carbonate ramp have been determinated based on integrated studies of taphofacies, biofacies, lithofacies and microfacies. In the mid ramp zone were recognized the following taphofacies: two types of autoparabiostromes, as well as concentrations of bivalves, gastropods and serpulids. Meanwhile, biofacies included autobiostromes rich in grypheids and serpulids. In the outer ramp zone were recognized two types of parabiostromes, ammonite and aptychus pavements, bioclastic detritus, molluscs and brachiopods pavements, besides bioturbated nodular limestones and truncated ammonites. In this zone, biofacies are characterized by high diversity including: Lingularia-Discinisca, infaunal bivalves, epistominid foraminifers, filament bivalves, besides of pectinidae, oysters and inoceramid bivalves, hardgrounds and microbial mats. Taphofacies and biofacies data allow to estimate relative sea level changes, sedimentation rates, substrate consistency, oxygenation, nutrient levels and productivity. © Asociación Paleontológica Argentina.
format JOUR
author Kietzmann, D.A.
Palma, R.M.
author_facet Kietzmann, D.A.
Palma, R.M.
author_sort Kietzmann, D.A.
title Taphofacies and biofacies of the Vaca Muerta Formation in the southern mendoza sector of the neuquén basin: paleoecological, sedimentological and stratigraphic implications
title_short Taphofacies and biofacies of the Vaca Muerta Formation in the southern mendoza sector of the neuquén basin: paleoecological, sedimentological and stratigraphic implications
title_full Taphofacies and biofacies of the Vaca Muerta Formation in the southern mendoza sector of the neuquén basin: paleoecological, sedimentological and stratigraphic implications
title_fullStr Taphofacies and biofacies of the Vaca Muerta Formation in the southern mendoza sector of the neuquén basin: paleoecological, sedimentological and stratigraphic implications
title_full_unstemmed Taphofacies and biofacies of the Vaca Muerta Formation in the southern mendoza sector of the neuquén basin: paleoecological, sedimentological and stratigraphic implications
title_sort taphofacies and biofacies of the vaca muerta formation in the southern mendoza sector of the neuquén basin: paleoecological, sedimentological and stratigraphic implications
url http://hdl.handle.net/20.500.12110/paper_00027014_v46_n2_p321_Kietzmann
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