2022
DOI: 10.1111/1462-2920.16276
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Stromatolites: Linking the past to the future

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Cited by 4 publications
(3 citation statements)
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“…Microbialites are organo-sedimentary deposits formed by the metabolic activity of microbial communities that induce the precipitation of minerals and trapped sediments to form structures that can be amorphous, clotted (thrombolites) or layered (stromatolites) [ 13 ]. They are ubiquitous in the fossil record, dating back to the Archaean and Precambrian eras [ 14 17 ]. Extant microbialites occur in temperate (marine and freshwater) as well as extreme environments that include hypersaline lagoons [ 18 ].…”
Section: Introductionmentioning
confidence: 99%
“…Microbialites are organo-sedimentary deposits formed by the metabolic activity of microbial communities that induce the precipitation of minerals and trapped sediments to form structures that can be amorphous, clotted (thrombolites) or layered (stromatolites) [ 13 ]. They are ubiquitous in the fossil record, dating back to the Archaean and Precambrian eras [ 14 17 ]. Extant microbialites occur in temperate (marine and freshwater) as well as extreme environments that include hypersaline lagoons [ 18 ].…”
Section: Introductionmentioning
confidence: 99%
“…Microbialites are organo-sedimentary deposits formed by the metabolic activity of microbial communities that induce the precipitation of minerals and trapped sediments to form structures that can be amorphous, clotted (thrombolites), or layered (stromatolites) [13]. They are ubiquitous in the fossil record, dating back to the Archaean and Precambrian eras [14][15][16][17]. Extant microbialites occur in temperate (marine and freshwater) as well as extreme environments that include hypersaline lagoons [18].…”
Section: Introductionmentioning
confidence: 99%
“…1 They are ubiquitous in the fossil record, dating back to the Archaean and Precambrian eras and retain information about past physical, geochemical and biological processes in the course of evolution. [2][3][4][5] Extant microbialites occur in temperate (marine and freshwater) as well as extreme environments that include hypersaline lagoons. 6 They have been documented primarily from several sites in Western Australia, 7 the Bahamas, 8 South/Central America, 9 , North America, 10,11 and South Africa, 12,13 with diverse microbial community structures and metabolisms.…”
Section: Introductionmentioning
confidence: 99%