2005
DOI: 10.1007/bf02732907
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The transition of a freshwater karst aquifer to an anoxic marine system

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Cited by 16 publications
(2 citation statements)
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“…Some distinctive biofilms are not directly associated with vents. For example, the walls of the sinkhole in the deepest part of the anoxic layer hosts grey finger-like Bacterial mats similar to those observed in Jewfish Sink [19]. Other parts of the anoxic layer contain long thin filamentous mats with a white coating.…”
Section: Hospital Hole: the Ecosystemmentioning
confidence: 74%
“…Some distinctive biofilms are not directly associated with vents. For example, the walls of the sinkhole in the deepest part of the anoxic layer hosts grey finger-like Bacterial mats similar to those observed in Jewfish Sink [19]. Other parts of the anoxic layer contain long thin filamentous mats with a white coating.…”
Section: Hospital Hole: the Ecosystemmentioning
confidence: 74%
“…Yakushev and Neretin, 1997) both of which can co-occur at very low but non-zero DO. In coastal karst environment in which seawater intrusion occurs, on the other hand, increased NO2 associated with decreased DO has been previously associated with the presence of deep karst conduits favouring the recirculation of seawater over large timescales (Garman and Garey, 2005). In such cases, nitrite levels are higher at the transition zone between low oxygen deep karst and surface karst waters (Garman and Garey, 2005).…”
Section: 52mentioning
confidence: 98%