Abstract
Two formations on Curaçao contain abundant volcaniclastic materials within a carbonate rock, the Neogene Seroe Domi formation, and the quaternary lower coral terrace. These two formations have clasts of Curaçao lava formation of various sizes and degrees of diagenetic alteration. This study hypothesizes that the alteration of clasts of the Curaçao lava formation liberates Mg ions into diagenetic fluids that contribute to: (1) the dolomitization of the Seroe Domi formation and/or (2) microbial precipitation of magnesium-rich carbonate mineral phases. Textural, petrographic, mineralogic, and elemental data indicate that the unaltered material of the lower terrace contains Mg-rich mineral phases that are missing in the older, altered Seroe Domi rocks. These results suggest that carbonate rocks with mafic detrital materials are possible environments for Mg enrichment that may lead to the formation of Mg-rich carbonate mineral phases.
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Acknowledgements
The author would like to thank the various undergraduate students that helped collect and catalog samples, and Dr. John P Harris who was extremely helpful in various phases of sample preparation and analysis. In addition, the two anonymous reviewers provided meaningful feedback, without which this manuscript would not have been possible.
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Sumrall, J.B. Petrogenic history of volcaniclastic carbonates from Curaçao, Netherlands Antilles. Carbonates Evaporites 34, 1627–1638 (2019). https://doi.org/10.1007/s13146-019-00511-5
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DOI: https://doi.org/10.1007/s13146-019-00511-5