Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)

The virtually unfolded sedimentary cover of the Cordilleras Central and Oriental in the eastern Dominican Republic (eastern Hispaniola, tropical North Atlantic) largely consists of Pliocene to Early Pleistocene mixed siliciclastics and carbonates. These deposits have been grouped into two laterally...

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Autores: Braga Alarcón, Juan Carlos, Díaz de Neira Sánchez, José Alberto, Lasseur, E., Mediato Arribas, José Francisco, Aguirre, Julio, Abad, Manuel, Hernáiz Huerta, Pedro Pablo, Monthel, J., Pérez Valera, Fernando, Lopera Caballero, Eusebio
Tipo de recurso: artículo
Fecha de publicación:2012
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/276850
Acceso en línea:http://hdl.handle.net/10261/276850
https://doi.org/10.1016/j.sedgeo.2012.04.007
Access Level:acceso abierto
Palabra clave:mixed carbonate–siliciclastic shelf
coral reef
Pliocene
Early Pleistocene
La Española
República Dominicana
Cordillera Central
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spelling Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)Braga Alarcón, Juan CarlosDíaz de Neira Sánchez, José AlbertoLasseur, E.Mediato Arribas, José FranciscoAguirre, JulioAbad, ManuelHernáiz Huerta, Pedro PabloMonthel, J.Pérez Valera, FernandoLopera Caballero, Eusebiomixed carbonate–siliciclastic shelfcoral reefPlioceneEarly PleistoceneLa EspañolaRepública DominicanaCordillera CentralThe virtually unfolded sedimentary cover of the Cordilleras Central and Oriental in the eastern Dominican Republic (eastern Hispaniola, tropical North Atlantic) largely consists of Pliocene to Early Pleistocene mixed siliciclastics and carbonates. These deposits have been grouped into two laterally interfingering mapping units, the Yanigua and Los Haitises formations. The former (mainly siliciclastics) comprises marl, marly limestone, and minor conglomerate, sandstone, lignite, and carbonaceous clay and crops out closest to the basement. The Los Haitises Formation mainly consists of limestone and intercalating beds of marly limestone and marl. Lithological mapping at the 1:50,000 scale and facies analysis of twelve measured sections and of additional fourteen outcrops suggest that these deposits mainly formed on a shallow-water marine platform fringing the precursor reliefs of the Cordillera Oriental and the southeastern end of the Cordillera Central. Only a limited proportion of sediment formed in floodplains and marshes. Marl and marly limestone dominated the inner platform sediments. Terrigenous mud decreased away from the emergent basement and carbonate sedimentation dominated the more external platform. Corals, molluscs, echinoids, foraminifers, bryozoans, coralline algae, and Halimeda are the main components with varying amounts of carbonate mud. The platform was generally a low-energy environment with seagrass patches. In the inner platform, corals grew as isolated colonies or as small patch reefs dominated by Porites in marly and bioclastic substrates. Branching corals (Stylophora and Acropora) grew in extensive carpets in more distal areas. At least in the last stage of its development (Early Pleistocene), the platform was rimmed by a reef barrier similar to the Holocene Caribbean barrier reefs, with Acropora gr. palmata, A. cervicornis, Porites, Montastrea, Siderastrea, and Diploria as the main reef buildersDepartamento de Estratigrafía y Paleontología, Universidad de Granada, EspañaUnidad de Tres Cantos, Instituto Geológico y Minero de España, EspañaCentre Scientifique et Technique, Bureau de Recherches Géologiques et Minières, FranciaINYPSA, EspañaDepartamento de Geodinámica y Paleontología, Universidad de Huelva, EspañaElsevierEuropean Commission202220222012info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501http://hdl.handle.net/10261/276850https://doi.org/10.1016/j.sedgeo.2012.04.007reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE#Programs Sysmin I y IIhttps://reader.elsevier.com/reader/sd/pii/S0037073812001133?token=00E3DBB345F193E6A639F91B18F3619A4A030DF3104C732CB9DAC51AA56DCFFAEDC8236A3207F986A1E09CDBBA51777Ainfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/2768502026-05-22T06:33:51Z
dc.title.none.fl_str_mv Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)
title Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)
spellingShingle Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)
Braga Alarcón, Juan Carlos
mixed carbonate–siliciclastic shelf
coral reef
Pliocene
Early Pleistocene
La Española
República Dominicana
Cordillera Central
title_short Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)
title_full Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)
title_fullStr Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)
title_full_unstemmed Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)
title_sort Pliocene–Lower Pleistocene shallow-water mixed siliciclastics and carbonates (Yanigua and Los Haitises formations) in eastern Hispaniola (Dominican Republic)
dc.creator.none.fl_str_mv Braga Alarcón, Juan Carlos
Díaz de Neira Sánchez, José Alberto
Lasseur, E.
Mediato Arribas, José Francisco
Aguirre, Julio
Abad, Manuel
Hernáiz Huerta, Pedro Pablo
Monthel, J.
Pérez Valera, Fernando
Lopera Caballero, Eusebio
author Braga Alarcón, Juan Carlos
author_facet Braga Alarcón, Juan Carlos
Díaz de Neira Sánchez, José Alberto
Lasseur, E.
Mediato Arribas, José Francisco
Aguirre, Julio
Abad, Manuel
Hernáiz Huerta, Pedro Pablo
Monthel, J.
Pérez Valera, Fernando
Lopera Caballero, Eusebio
author_role author
author2 Díaz de Neira Sánchez, José Alberto
Lasseur, E.
Mediato Arribas, José Francisco
Aguirre, Julio
Abad, Manuel
Hernáiz Huerta, Pedro Pablo
Monthel, J.
Pérez Valera, Fernando
Lopera Caballero, Eusebio
author2_role author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv European Commission
dc.subject.none.fl_str_mv mixed carbonate–siliciclastic shelf
coral reef
Pliocene
Early Pleistocene
La Española
República Dominicana
Cordillera Central
topic mixed carbonate–siliciclastic shelf
coral reef
Pliocene
Early Pleistocene
La Española
República Dominicana
Cordillera Central
description The virtually unfolded sedimentary cover of the Cordilleras Central and Oriental in the eastern Dominican Republic (eastern Hispaniola, tropical North Atlantic) largely consists of Pliocene to Early Pleistocene mixed siliciclastics and carbonates. These deposits have been grouped into two laterally interfingering mapping units, the Yanigua and Los Haitises formations. The former (mainly siliciclastics) comprises marl, marly limestone, and minor conglomerate, sandstone, lignite, and carbonaceous clay and crops out closest to the basement. The Los Haitises Formation mainly consists of limestone and intercalating beds of marly limestone and marl. Lithological mapping at the 1:50,000 scale and facies analysis of twelve measured sections and of additional fourteen outcrops suggest that these deposits mainly formed on a shallow-water marine platform fringing the precursor reliefs of the Cordillera Oriental and the southeastern end of the Cordillera Central. Only a limited proportion of sediment formed in floodplains and marshes. Marl and marly limestone dominated the inner platform sediments. Terrigenous mud decreased away from the emergent basement and carbonate sedimentation dominated the more external platform. Corals, molluscs, echinoids, foraminifers, bryozoans, coralline algae, and Halimeda are the main components with varying amounts of carbonate mud. The platform was generally a low-energy environment with seagrass patches. In the inner platform, corals grew as isolated colonies or as small patch reefs dominated by Porites in marly and bioclastic substrates. Branching corals (Stylophora and Acropora) grew in extensive carpets in more distal areas. At least in the last stage of its development (Early Pleistocene), the platform was rimmed by a reef barrier similar to the Holocene Caribbean barrier reefs, with Acropora gr. palmata, A. cervicornis, Porites, Montastrea, Siderastrea, and Diploria as the main reef builders
publishDate 2012
dc.date.none.fl_str_mv 2012
2022
2022
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/276850
https://doi.org/10.1016/j.sedgeo.2012.04.007
url http://hdl.handle.net/10261/276850
https://doi.org/10.1016/j.sedgeo.2012.04.007
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv #PLACEHOLDER_PARENT_METADATA_VALUE#
Programs Sysmin I y II
https://reader.elsevier.com/reader/sd/pii/S0037073812001133?token=00E3DBB345F193E6A639F91B18F3619A4A030DF3104C732CB9DAC51AA56DCFFAEDC8236A3207F986A1E09CDBBA51777A
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
instname_str Consejo Superior de Investigaciones Científicas (CSIC)
reponame_str DIGITAL.CSIC. Repositorio Institucional del CSIC
collection DIGITAL.CSIC. Repositorio Institucional del CSIC
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