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Some pitfalls in paleosol interpretation in carbonate sequences

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Abstract

In Quaternary carbonate units composed mostly of eolianites, paleosols are important stratigraphic markers that help differentiate episodes of carbonate deposition tied to glacio-eustatic sea level fluctuations. Paleosols used in this manner can be misinterpreted, and thus lead to errors in interpretation of the geologic record. Some possible pitfalls include: failure to differentiate between terra-rossa paleosols and calcarenite protosols; failure to recognize that separate paleosols may merge laterally into composite paleosols; failure to recognize that single paleosols may bifurcate in highly weathered bedrock; and failure to recognize soil-derived material that infills karst features. The Quaternary carbonates of the Bahamas are used to illustrate these pitfalls, which may occur in carbonates of any age.

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Authors and Affiliations

  1. Department of Geology, The College of Charleston, 29424, Charleston, SC

    James L. Carew

  2. Department of Geology and Geography, Mississippi State University, 39762, Mississippi State, MS

    John E. Mylroie

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  1. James L. Carew
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  2. John E. Mylroie
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Carew, J.L., Mylroie, J.E. Some pitfalls in paleosol interpretation in carbonate sequences. Carbonates Evaporites 6, 69–74 (1991). https://doi.org/10.1007/BF03175383

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