2018
DOI: 10.1007/s10123-018-0008-z
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Great Salt Lake microbiology: a historical perspective

Abstract: Over geologic time, the water in the Bonneville basin has risen and  fallen, most dramatically as freshwater Lake Bonneville lost enormous volume 15,000–13,000 years ago and became the modern day Great Salt Lake. It is likely that paleo-humans lived along the shores of this body of water as it shrunk to the present margins, and native peoples inhabited the surrounding desert and wetlands in recent times. Nineteenth century Euro-American explorers and pioneers described the geology, geography, and flora and fau… Show more

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Cited by 51 publications
(53 citation statements)
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“…This paper provides an introduction to the basic morphology of these unique structures and how local environmental conditions, as well as periods of exposure and erosion, contribute to growth location, grouping, shape, size, orientation, and internal structure. Several other research groups are exploring other important aspects including mineral precipitation mechanisms Pace et al, 2016), biogeochemistry/microbiology (Lindsay et al, 2016;Baxter, 2018), and possible age of formation and paleoenvironmental record (Newell et al, 2017;Vennin et al, 2019).…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…This paper provides an introduction to the basic morphology of these unique structures and how local environmental conditions, as well as periods of exposure and erosion, contribute to growth location, grouping, shape, size, orientation, and internal structure. Several other research groups are exploring other important aspects including mineral precipitation mechanisms Pace et al, 2016), biogeochemistry/microbiology (Lindsay et al, 2016;Baxter, 2018), and possible age of formation and paleoenvironmental record (Newell et al, 2017;Vennin et al, 2019).…”
Section: Introductionmentioning
confidence: 99%
“…Locations of photographs from subsequent figures are shown; lake bathymetry is fromBaskin and Allen (2005) andBaskin and Turner (2006). The inset graph shows elevation of GSL through recorded history,1847-2018 (USGS, 2019.…”
mentioning
confidence: 99%
“…Microbial mats and microbialites are common in GSL (e.g. Baskin et al, ; Baskin et al, ; Baskin et al, ; Baxter, ; Bouton, Vennin, Boulle, et al, ; Chidsey et al, ; Newell et al, ; Vanden Berg, ) and likely play an important role in calcium sequestration. Characteristic of these benthic organosedimentary systems is the copious production of extracellular polymeric substances (EPS), which bind cations, notably Ca 2+ (Braissant et al, ), depleting the ambient water of this cation (Dupraz & Visscher, ).…”
Section: Can We Predict the Amount Of Carbonates Formed In A Sedimentmentioning
confidence: 99%
“…Recent renewed interest in the GSL has focused on constraining mechanisms of microbial carbonate deposition (e.g. Baskin, Driscoll, & Wright, ; Baskin, Driscoll, & Wright, ; Baskin, Wright, Driscoll, Graham, & Hepner, ; Baxter, ; Bouton, Vennin, Boulle, et al, ; Bouton, Vennin, Mulder, et al, ; Chidsey, Vanden Berg, & Eby, ; Della Porta, ; Lindsay et al, ; Newell, Jensen, Frantz, & Vanden Berg, ; Pace et al, ; Vanden Berg, ; Vennin et al, ), as analogue to those that partly make up the Cretaceous presalt reservoirs (Abelha & Petersohn, ).…”
Section: Introductionmentioning
confidence: 99%
“…Hypersaline lakes are considered extreme environments for microbial life. A variety of salt lakes have been surveyed for bacterial diversity such as Chaka Lake in China, Chott El Jerid Lake in Tunisia, Meyghan Lake in Iran, Keke Lake in China, and Great Salt Lake in the United States [ 5 , 13 16 ]. In addition, groups of novel halophilic or halotolerant bacteria in salt lakes have been described using culture-dependent methods: Actinopolyspora lacussalsi sp.…”
Section: Introductionmentioning
confidence: 99%