Definition
The chemocline is the vertical chemical gradient or cline, which is produced in a mass of water having restricted circulation (e.g., meromictic lakes where water layers do not intermix). Local conditions of circulation provoke the formation of bottom anoxic waters – where only anaerobic organisms exist – overlain by oxygenated waters, where aerobic photosynthetic life flourishes. At the contact between these two zones, photosynthetic communities of anaerobic purple sulfur bacteria develop, taking advantage of both the sunlight from above and the hydrogen sulfide (H2S) produced below. In astrobiology, this zone of the chemocline is studied because it could be an analogue of Archean niches of life where limited oxygenated waters developed over an anoxic Archean ocean.
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Pinti, D.L. (2022). Chemocline. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_5157-3
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DOI: https://doi.org/10.1007/978-3-642-27833-4_5157-3
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Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-27833-4
Online ISBN: 978-3-642-27833-4
eBook Packages: Springer Reference Physics and AstronomyReference Module Physical and Materials ScienceReference Module Chemistry, Materials and Physics
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Chapter history
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Latest
Chemocline- Published:
- 16 November 2021
DOI: https://doi.org/10.1007/978-3-642-27833-4_5157-3
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Original
Chemocline- Published:
- 04 May 2015
DOI: https://doi.org/10.1007/978-3-642-27833-4_5157-2