2012
DOI: 10.1016/j.margeo.2012.02.009
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Characteristics, distribution and morphogenesis of subtidal microbial systems in Shark Bay, Australia

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Cited by 172 publications
(157 citation statements)
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“…δ 18 O and δ 13 C values of cap samples are not dissimilar to those characterizing the other subunits of the mushroom, suggesting that unusual evaporative regimes or unusual carbonate sources were not the key factor controlling its formation. The porous cerebroid-like morphology of the cap is similar to that of stromatolites and thrombolites that occur in the photic zone of marine embayments and lagoons (Jahnert and Collins, 2012;Bosak et al, 2013). The analogies with microbialites are even more evident at the microscopic scale.…”
Section: Model For Mushroom Speleothem Formationmentioning
confidence: 67%
See 1 more Smart Citation
“…δ 18 O and δ 13 C values of cap samples are not dissimilar to those characterizing the other subunits of the mushroom, suggesting that unusual evaporative regimes or unusual carbonate sources were not the key factor controlling its formation. The porous cerebroid-like morphology of the cap is similar to that of stromatolites and thrombolites that occur in the photic zone of marine embayments and lagoons (Jahnert and Collins, 2012;Bosak et al, 2013). The analogies with microbialites are even more evident at the microscopic scale.…”
Section: Model For Mushroom Speleothem Formationmentioning
confidence: 67%
“…Although these speleothems have been well-known by speleologists for decades, and Santa Catalina has been declared "National Monument" in 1996 (Watson et al, 1997;D'Angeli et al, 2015), the exact mechanism of their formation, as well as their petrography and mineralogy, remain virtually unstudied. Besides representing a yet uncharacterized type of speleothem, they are of utmost interest due to their uppermost unit (i.e., the mushroom cap), which is similar to stromatolitic and thrombolitic microbialites that form in the presence of microbial mats (Figures 1A,B; Jahnert and Collins, 2012;Bosak et al, 2013). Microbialites occur in a large variety of distinctive morphologies and are found in the geological record from the early Archean onwards (Grotzinger and Knoll, 1999).…”
Section: Introductionmentioning
confidence: 99%
“…This difference in grain-size has been noted in present-day marine coarse-grained carbonate stromato lites formed by stabilisation (trapping and binding) of previously mo bile grains by microbial mats (Logan, 1961;Monty, 1976;Dravis, 1983;Reid and Browne, 1991;Riding et al, 1991a;Reid et al, 1999). In these examples, grain-trapping is produced by erect filaments, mat ir regularities, and extracellular polymeric substances (EPS) secreted by cyanobacteria and other mat microbes (Logan, 1961;Playford and Cockbain, 1976;Dravis, 1983;Dill et al, 1986;Awramik and Riding, 1988;Riding et al, 1991a;Visscher et al, 1998;Reid et al, 2000;Decho et al, 2005;Dupraz et al, 2009;Browne, 2011;Bowlin et al, 2012;jahnert and Collins, 2012). Rare filaments in some mixed laminae of the Leza coarse-grained stromatolites (Fig.…”
Section: Grain-rich Laminaementioning
confidence: 93%
“…Fossilized stromatolites reefs found in Shark Bay, Western Australia have provided great insights into primitive microbial life, which can be comparable to some of living stromatolites that have been found in recent times e.g. hot springs of Yellowstone National Park (Jahnert and Collins, 2012;Berelson et al, 2011). Fossilized stromatolites are petrological structures that represent lithified forms of microbial life observed in rocks aged 3.6 billion years old.…”
Section: Predicted Social Behaviours In Primitive Microorganismsmentioning
confidence: 96%