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Evolution of calcite microcrystal morphology during experimental dissolution

Mohammed S. Hashim; Stephen E. Kaczmarek
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Extreme-flood-related peat blocks: An Anthropocene analogue to ancient coal-forming environments

Juan Pedro Rodríguez-López; Ana R. Soria; Carlos L. Liesa
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Contrasting facies patterns between river-dominated and symmetrical wave-dominated delta deposits

Brian J. Willis; Tao Sun; R. Bruce Ainsworth
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Depositional environments and salt-thickness variations in Urmia Lake (NW Iran): Insight from sediment-core studies

Ali Mohammadi; Razyeh Lak; Georg Schwamborn; Amaneh Kaveh Firouz; Attila Çiner; Javad Darvishi Khatouni
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Evolution of a complex early Permian coarse-grained shoreline along a rift basin margin

Antoine Dillinger; Annette D. George; Romain Vaucher
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    COVER EXPLANATION.—Gypsum–halite mounds from the hypersaline Urmia Lake. Mounds form in the dry season when salinity increases. Black cyanobacterial mats around the mounds contribute to their formation. See Mohammadi et al., this issue.

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