File:Marinedrugs-18-00091-g002.webp
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editDescriptionMarinedrugs-18-00091-g002.webp |
English: Simplified vertical section of a deep hypersaline anoxic basins (DHAB). The transition from the overlying seawater to the brine is commonly referred to as the halocline or brine–seawater interface, which is characterized by gradients of temperature, salinity, pH, and dissolved oxygen (A); the main biogeochemical processes taking place within the halocline are shown in (B). From left to right, the manganese cycle, the sulfate reduction and sulfide oxidation cycle, the methanogenesis and aerobic (anaerobic) methane oxidation cycle, and the anammox and denitrification cycle that occur in the halocline are shown. DOC: Dissolved Organic Carbon. |
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Source | Fig. 2 at https://www.mdpi.com/1660-3397/18/2/91/htm Deep Hypersaline Anoxic Basins as Untapped Reservoir of Polyextremophilic Prokaryotes of Biotechnological Interest. In: MDPI Mar. Drugs 18(2), Special Issue Bioactive Molecules from Extreme Environments, 91; doi:10.3390/md18020091 | ||
Author | Stefano Varrella, Michael Tangherlini, Cinzia Corinaldesi | ||
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