Cited by 99Geological formations and processesGeochemistry and Elemental AnalysisPaleontology and Stratigraphy of Fossils

Recent dolomite in the Persian Gulf

WELLS, ALAN J.·1962·Nature

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Crossref · 10.1038/194274a0

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  • Holocene dolomites have been repeatedly observed in evaporitic environments worldwide.

    “In spite of their paucity, the Holocene dolomites have been repeatedly observed in evaporitic environments worldwide (Wells, 1962; Middelburg et al., 1990; Vasconcelos and McKenzie, 1997; Wright, 1999; van Lith et al., 2002; Wright and Wacey, 2005; Bontognali et al., 2010, 2012; Deng et al., 2010; Meister et al., 2011; Brauchli et al., 2016).”
  • Modern dolomite exists but is common only in certain environments: marginal, restricted, hypersaline regimes; nonmarine lakes; and zones of microbial sulfate reduction.

    “Modern dolomite does indeed exist but is common only in certain environments: (1) marginal, restricted, hypersaline regimes such as the Coorong lakes of South Australia (Alderman, 1959), supratidal lagoons on the island of Bonaire, Netherland Antilles (Deffeyes, Lucia, and Weyl, 1965), and the sabkhas of the Persian Gulf (Wells, 1962)”

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Authors
WELLS, A. J.
Affiliations
Shell (Netherlands) (NL)
Corresponding author
WELLS, ALAN J.
Venue
Nature
Published
1962-04
Volume
194
Issue
4825
Pages
274-275
ISSN
  • 0028-0836 (ISSN-L)
  • 1476-4687
OpenAlex
W2035766707
Cited by
99
References
0
Citations by year
2026: 3 · 2025: 1 · 2024: 2 · 2023: 2 · 2022: 1 · 2021: 5 · 2020: 5 · 2019: 2 · 2018: 2 · 2017: 3 · 2016: 6 · 2015: 2 · 2013: 3 · 2012: 2
FWCI
11.17
Type
journal article
Language
en
Open access
closed
Locations
Nature (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
carbonate sediments, Persian Gulf, Qatar, nearshore sediments, intertidal sediments, carbonate diagenesis

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