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Small quantities of a rare Ca‐deficient dolomite have been found coexisting in thin layers and alternating with the normal Ca‐rich variety in the Holocene sabkhas of southern Kuwait. The Ca‐poor dolomite has a molar composition of Ca46–49, whereas the Ca‐rich type is Ca51–56. The former type has been found only in two localities of the supratidal zone that are not subjected to tidal flooding today, and mostly within the fluctuating ground‐water table in these zones. The thin layers are either carbonate mud‐rich or pellet‐rich, and the amount of Ca‐poor dolomite is never more than 4 to 6 per cent by weight of the total carbonate fraction. The dolomites vary in size between 2 μm and 5 μm and exhibit characteristic rhombic crystal morphologies.

The complex of Pleistocene-Holocene sediments in the Al-Khiran area of Kuwait represents a petroleum basin analogue where organic-rich sediments in lagoons are closely associated with porous potential reservoir facies of oolitic beach ridges. The petrography, mineralogy, elemental and organic geochemistry of the carbonate-evaporite successions exposed along the southern coast of Kuwait have been analyzed. The physical and chemical conditions of the depositional environments and the diagenetic history of the sediments have been evaluated.Analysis of sediment grain-size distributions and parameters indicates that the coastal areas near their connection to the open Gulf and at the mouths of tidal creeks are dominated by coarse-grained, moderately-sorted carbonate beach sands, with low amounts of total organic matter (TOC ¼ 0.3 wt%). Landward, at the ends of the creeks, the concentration of ooids decreases, and silt-clayey sediments composed mainly of pellets and calcareous mud interbedded with algal mats are found. This low-energy setting reveals a higher TOC content (0.9 wt%) than the sediments deposited at the mouths of the tidal creeks, indicating petroleum source-rock potential for the tidal creek facies.Pleistocene oolitic limestones consist of elongate, cross-bedded, thinly-laminated ridges of carbonate sand, oriented parallel to the strong tidal currents. The sediments are composed entirely of well-sorted, coarse ooids (0.5 mm diameter). Study of the diagenetic processes and porosity in these rocks shows that they exhibit excellent reservoir potential as a result of prolonged exposure to freshwater leaching.Low amounts of trace metals, low organic-matter contents, and relatively high O/C atomic ratios of the organic matter in the bioturbated beach sediments and ridges, indicate that they were laid down under highly oxygenated open-marine conditions, where current and wave action contributed to the destruction of the organic matter. However, sediments deposited at the ends of the creeks show relatively higher tracemetal and higher TOC contents. The physical and chemical conditions in the creeks allow the preservation of amorphous algal marine-type organic matter, enhancing the source-rock potential of the sediments.