Synonyms
Bituminous rock; Organic-rich shale; Sapropelites
Definition
Black shales are organic carbon-rich sediments or sedimentary rocks. Black shales are important source rocks of fossil fuels (petroleum and natural gas) (Tissot and Welte 1984) and in some cases host economically viable metal accumulations (Vine and Tourtelot 1970). Sapropels are a geologically young analogue of black shales and offer high-resolution archives to decipher the interplay of paleoclimate and paleoceanography with biogeochemical and biological conditions in marine black shale depositional environments of the more distant geological past (Emeis and Weissert 2009).
Characteristics
Black shales and sapropels represent paleoenvironmental conditions that caused an unusually efficient transfer of mainly marine nonliving biomass into the geosphere and thus have been a key regulation on the global carbon cycle throughout Earth history. The sequestration of organic carbon in the geosphere is a small sink in the...
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References
Emeis K-C, Weissert H (2009) Tethyan–Mediterranean organic carbon-rich sediments from Mesozoic black shales to sapropels. Sedimentology 56:247–266
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Rossignol-Strick M, Nesteroff V, Olive P, Vergnaud-Grazzini C (1982) After the deluge; Mediterranean stagnation and sapropel formation. Nature 295:105–110
Schlanger SO, Jenkyns HC (1976) Cretaceous anoxic events: causes and consequences. Geologie en Mijnbouw 55:179–184
Tissot BP, Welte DH (1984) Petroleum formation and occurrence. Springer-Verlag, Berlin/Heidelberg/New York/Tokyo
Vine JD, Tourtelot EB (1970) Geochemistry of black shale deposits – a summary report. Econ Geol 65:253–272
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Emeis, KC. (2018). Black Shales and Sapropels. In: White, W.M. (eds) Encyclopedia of Geochemistry. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-39312-4_146
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DOI: https://doi.org/10.1007/978-3-319-39312-4_146
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