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...
| Autores: | , , , , , , , , , |
|---|---|
| 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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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 |
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info:eu-repo/semantics/openAccess |
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openAccess |
| dc.publisher.none.fl_str_mv |
Elsevier |
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Elsevier |
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reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
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Consejo Superior de Investigaciones Científicas (CSIC) |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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1869420637513056256 |
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15,811543 |