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Pedogenic carbonate forms in arid to semi-arid environments when infiltrating soil water evaporates and deposits solutes rather than leaching them through the soil profile. The amount and morphology of carbonate accumulation in soils, along with the overall degree of horizon and profile development, evolve over time (Brock & Buck 2009), reflecting relative age, and climate and/or geomorphic stability. The term “petrocalcic horizon” describes horizons in which carbonate accumulation has either completely engulfed and/or indurated the horizon, while “calcic horizon” reflects younger relative ages of less-extensive carbonate accumulation without complete horizon cementation (Soil Survey Staff, 2014).

WHAT CAN PETROCALCIC LAMINAE TELL US ABOUT SOIL PROCESSES AND PALEOENVIRONMENTS?