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

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• 作者：Juan C. Braga^a ; ^{jbraga@ugr.es} ; Alberto Dí ; az de Neira^b ; Eric Lasseur^c ; José ; Mediato^d ; ^b ; Julio Aguirre^a ; Manuel Abad^e ; Pedro P. Hernaiz-Huerta^d ; Jacques Monthel^c ; Fernando Pé ; rez-Valera^f ; Eusebio Lopera^g
• 关键词：Mixed carbonate&ndash ; siliciclastic shelf ; Coral reef ; Pliocene&ndash ; Early Pleistocene ; Hispaniola ; Eastern Dominican Republic
• 刊名：Sedimentary Geology
• 出版年：2012
• 期刊代码：81_00370738
• 类别：ear
• 出版时间：15 July, 2012
• 卷：265-266
• 期：Complete
• 页码：182-194
• 文件大小：3080 K

摘要

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.