Carbonate facies patterns in surface sediments of upwelling and non-upwelling shelf environments (Panama, East Pacific).

J.J.G. Reijmer, Th. Bauch, P. Schäfer

    Research output: Contribution to JournalArticleAcademicpeer-review

    Abstract

    In this study two carbonate environments are compared and contrasted; the Gulf of Panama and the Gulf of Chiriquí on the Pacific side of Panama. These two embayments are in close geographic proximity at latitudes between 7°N and 9°N. The Gulf of Panama and the Gulf of Chiriquí are characterized by contrasting oceanographic conditions with year-round stable non-upwelling conditions in the Gulf of Chiriquí and strong seasonal upwelling in the dry season (December to April) in the Gulf of Panama. The upwelling variations only have a limited influence on the amount of carbonate produced; however, they do have a major impact on the occurrence of specific carbonate producing biota. In addition, carbonate production and distribution is influenced in both gulfs by the occurrence of islands and by terrigenous input. Terrigenous material is found mainly in the smaller grain sizes (<63 to 250μm) that can be transported easily by currents and waves. Carbonate dominant sediments (carbonate sands and mixed carbonate-siliciclastic sands) mainly occur around the islands and are dominated by larger grain-sizes (>500μm). The Gulf of Panama and the Gulf of Chiriquí both show warm and temperate carbonate-producing biota, with carbonate producers from tropical (corals) to mixed tropical to cool-water (coralline red algae) and cold-water (balanids) environments. The Gulf of Chiriquí is characterized by oligotrophic to mesotrophic conditions resulting in a photozoan (coral) and/or rhodolith-facies in shallow-water areas surrounding the islands and a mollusc-dominated facies in deeper waters towards the shelf edge. Seasonal upwelling causes temporary eutrophic conditions in the Gulf of Panama, which results in a heterozoan facies around the islands dominated by balanids, echinoderms and molluscs. Thus a 'cool-water' carbonate fauna and eutrophic conditions can exist in the tropics within an area prone to seasonal upwelling. The distinct facies differences found on the Pacific shelf of Panama stress the importance of variations in oceanographic conditions, upwelling versus non-upwelling, in determining carbonate production and associated facies patterns in the tropics. © 2010 The Authors. Journal compilation © 2010 International Association of Sedimentologists.
    Original languageEnglish
    Pages (from-to)32-56
    Number of pages25
    JournalSedimentology
    Volume59
    Issue number1
    DOIs
    Publication statusPublished - 2012

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