Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades

Autores
Benavente, Cecilia Andrea; Bohacs, Kevin M.
Año de publicación
2024
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The lake-basin- type model classified the stratigraphic record of ancient lake sys-tems according to rates of potential accommodation relative to sediment + watersupply. The model convolved all modes and paths of water supply (direct fall,surficial, subsurface) with amounts and types of sediment supply (clastic, bio-genic, chemical) into a single basin-filling volume term (sediment + water); itsmajor strength was its widespread applicability. This was supported by subsequentinvestigations confirming the utility of this approach, but it also revealed someimportant limitations due to simplifications in the original model. The modelhas been expanded here to address all inland waters (lakes, ponds, wetlands, pla-yas) as well as adding two major subdivisions of the sediment + water term: (1)water supply paths and (2) the volume of water supply relative to sediment sup-ply. Water supply flow paths in the subsurface are subdivided into ‘throughflow’,‘recharge’ and ‘discharge’. Each of these groundwater hydrology states can be de-fined quite precisely by the ratio of net outflow to inflow, from persistently opento consistently closed. These paths can be deciphered using stable carbonate andoxygen isotope composition of primary lacustrine limestones, detailed sedimen-tology, stratigraphy, palaeontology and mineralogy. Distinguishing water supplypaths provides additional insights into playa systems and the occurrence andcharacter of evaporites and carbonates. The volume ratio of water to sedimentsupply most directly influences the water depths of lakes, ponds and wetlands,which affect water body hydrodynamics and ecosystem behaviour as well as thedetails of stratal stacking and depositional sequences. It helps fine-tune estimatesof the distribution of sediment texture, bedding, composition and organic mattercontent. The aim of this contribution is to address questions about the funda-mental types of inland water bodies and to explain the new lake-basin subtypesand provide examples that illustrate their potential to enable higher-resolution,robust analysis of inland water systems and their stratigraphic records.
Fil: Benavente, Cecilia Andrea. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Bohacs, Kevin M.. No especifíca;
Materia
CARBONATES
COAL
EVAPORITES
KEROGENITE
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
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oai:ri.conicet.gov.ar:11336/263866

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spelling Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgradesBenavente, Cecilia AndreaBohacs, Kevin M.CARBONATESCOALEVAPORITESKEROGENITEhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The lake-basin- type model classified the stratigraphic record of ancient lake sys-tems according to rates of potential accommodation relative to sediment + watersupply. The model convolved all modes and paths of water supply (direct fall,surficial, subsurface) with amounts and types of sediment supply (clastic, bio-genic, chemical) into a single basin-filling volume term (sediment + water); itsmajor strength was its widespread applicability. This was supported by subsequentinvestigations confirming the utility of this approach, but it also revealed someimportant limitations due to simplifications in the original model. The modelhas been expanded here to address all inland waters (lakes, ponds, wetlands, pla-yas) as well as adding two major subdivisions of the sediment + water term: (1)water supply paths and (2) the volume of water supply relative to sediment sup-ply. Water supply flow paths in the subsurface are subdivided into ‘throughflow’,‘recharge’ and ‘discharge’. Each of these groundwater hydrology states can be de-fined quite precisely by the ratio of net outflow to inflow, from persistently opento consistently closed. These paths can be deciphered using stable carbonate andoxygen isotope composition of primary lacustrine limestones, detailed sedimen-tology, stratigraphy, palaeontology and mineralogy. Distinguishing water supplypaths provides additional insights into playa systems and the occurrence andcharacter of evaporites and carbonates. The volume ratio of water to sedimentsupply most directly influences the water depths of lakes, ponds and wetlands,which affect water body hydrodynamics and ecosystem behaviour as well as thedetails of stratal stacking and depositional sequences. It helps fine-tune estimatesof the distribution of sediment texture, bedding, composition and organic mattercontent. The aim of this contribution is to address questions about the funda-mental types of inland water bodies and to explain the new lake-basin subtypesand provide examples that illustrate their potential to enable higher-resolution,robust analysis of inland water systems and their stratigraphic records.Fil: Benavente, Cecilia Andrea. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Bohacs, Kevin M.. No especifíca;Wiley2024-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/263866Benavente, Cecilia Andrea; Bohacs, Kevin M.; Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades; Wiley; The Depositional Record; 10; 5; 5-2024; 748-7922055-4877CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/full/10.1002/dep2.280info:eu-repo/semantics/altIdentifier/doi/10.1002/dep2.280info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:33:33Zoai:ri.conicet.gov.ar:11336/263866instacron: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 10:33:33.704CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades
title Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades
spellingShingle Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades
Benavente, Cecilia Andrea
CARBONATES
COAL
EVAPORITES
KEROGENITE
title_short Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades
title_full Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades
title_fullStr Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades
title_full_unstemmed Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades
title_sort Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades
dc.creator.none.fl_str_mv Benavente, Cecilia Andrea
Bohacs, Kevin M.
author Benavente, Cecilia Andrea
author_facet Benavente, Cecilia Andrea
Bohacs, Kevin M.
author_role author
author2 Bohacs, Kevin M.
author2_role author
dc.subject.none.fl_str_mv CARBONATES
COAL
EVAPORITES
KEROGENITE
topic CARBONATES
COAL
EVAPORITES
KEROGENITE
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The lake-basin- type model classified the stratigraphic record of ancient lake sys-tems according to rates of potential accommodation relative to sediment + watersupply. The model convolved all modes and paths of water supply (direct fall,surficial, subsurface) with amounts and types of sediment supply (clastic, bio-genic, chemical) into a single basin-filling volume term (sediment + water); itsmajor strength was its widespread applicability. This was supported by subsequentinvestigations confirming the utility of this approach, but it also revealed someimportant limitations due to simplifications in the original model. The modelhas been expanded here to address all inland waters (lakes, ponds, wetlands, pla-yas) as well as adding two major subdivisions of the sediment + water term: (1)water supply paths and (2) the volume of water supply relative to sediment sup-ply. Water supply flow paths in the subsurface are subdivided into ‘throughflow’,‘recharge’ and ‘discharge’. Each of these groundwater hydrology states can be de-fined quite precisely by the ratio of net outflow to inflow, from persistently opento consistently closed. These paths can be deciphered using stable carbonate andoxygen isotope composition of primary lacustrine limestones, detailed sedimen-tology, stratigraphy, palaeontology and mineralogy. Distinguishing water supplypaths provides additional insights into playa systems and the occurrence andcharacter of evaporites and carbonates. The volume ratio of water to sedimentsupply most directly influences the water depths of lakes, ponds and wetlands,which affect water body hydrodynamics and ecosystem behaviour as well as thedetails of stratal stacking and depositional sequences. It helps fine-tune estimatesof the distribution of sediment texture, bedding, composition and organic mattercontent. The aim of this contribution is to address questions about the funda-mental types of inland water bodies and to explain the new lake-basin subtypesand provide examples that illustrate their potential to enable higher-resolution,robust analysis of inland water systems and their stratigraphic records.
Fil: Benavente, Cecilia Andrea. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Bohacs, Kevin M.. No especifíca;
description The lake-basin- type model classified the stratigraphic record of ancient lake sys-tems according to rates of potential accommodation relative to sediment + watersupply. The model convolved all modes and paths of water supply (direct fall,surficial, subsurface) with amounts and types of sediment supply (clastic, bio-genic, chemical) into a single basin-filling volume term (sediment + water); itsmajor strength was its widespread applicability. This was supported by subsequentinvestigations confirming the utility of this approach, but it also revealed someimportant limitations due to simplifications in the original model. The modelhas been expanded here to address all inland waters (lakes, ponds, wetlands, pla-yas) as well as adding two major subdivisions of the sediment + water term: (1)water supply paths and (2) the volume of water supply relative to sediment sup-ply. Water supply flow paths in the subsurface are subdivided into ‘throughflow’,‘recharge’ and ‘discharge’. Each of these groundwater hydrology states can be de-fined quite precisely by the ratio of net outflow to inflow, from persistently opento consistently closed. These paths can be deciphered using stable carbonate andoxygen isotope composition of primary lacustrine limestones, detailed sedimen-tology, stratigraphy, palaeontology and mineralogy. Distinguishing water supplypaths provides additional insights into playa systems and the occurrence andcharacter of evaporites and carbonates. The volume ratio of water to sedimentsupply most directly influences the water depths of lakes, ponds and wetlands,which affect water body hydrodynamics and ecosystem behaviour as well as thedetails of stratal stacking and depositional sequences. It helps fine-tune estimatesof the distribution of sediment texture, bedding, composition and organic mattercontent. The aim of this contribution is to address questions about the funda-mental types of inland water bodies and to explain the new lake-basin subtypesand provide examples that illustrate their potential to enable higher-resolution,robust analysis of inland water systems and their stratigraphic records.
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/11336/263866
Benavente, Cecilia Andrea; Bohacs, Kevin M.; Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades; Wiley; The Depositional Record; 10; 5; 5-2024; 748-792
2055-4877
CONICET Digital
CONICET
url http://hdl.handle.net/11336/263866
identifier_str_mv Benavente, Cecilia Andrea; Bohacs, Kevin M.; Advances in Limnogeology: The lake‐basin‐type model revisited 25 years after…anomalies, conundrums and upgrades; Wiley; The Depositional Record; 10; 5; 5-2024; 748-792
2055-4877
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/full/10.1002/dep2.280
info:eu-repo/semantics/altIdentifier/doi/10.1002/dep2.280
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 Wiley
publisher.none.fl_str_mv Wiley
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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