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- W2020029275 abstract "Red algae occur in the sediments of the Lower Guajira shelf, Colombia, and two biofacies are differentiated, a relict, outer shelf, lower sea-level facies and a modern, high sea-level facies. The continued development of organogenic facies in the Guajira region demonstrates the persistence of climatic aridity over the past 12,500 years. The factors controlling the development of rhodophyte facies include temperature, rainfall, the influence of trade-winds, the morphology of the shelf, and ocean dynamics and the rhodophyte facies have, in part, taken the place of coral reefs, which cannot develop in this region. The sedimentation on the Guajira shelf has been significantly affected by glacio-eustasy. An idealized sequence can be recognized for the past 18,000 years." @default.
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- W2020029275 date "1992-02-01" @default.
- W2020029275 modified "2023-10-18" @default.
- W2020029275 title "Late quaternary carbonate sedimentation on the lower Guajira shelf, Colombia" @default.
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- W2020029275 doi "https://doi.org/10.1016/0025-3227(92)90090-5" @default.
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