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- W1986661784 abstract "Lamellae enriched with clay have been identified in profiles of the Otama series during the course of field mapping in Southland, New Zealand. Similar soils have been reported in a variety of landscapes from other parts of the world, but explanations of their genesis differ considerably and do not fully account for the properties of the Otama series. Macro- and micromorphological analysis of this soil indicates a complex history in which the lamellae have formed by clay migration, possibly under a seasonal freeze-thaw environment, as aeolian sediment was accumulating during the last glacial. A cumulative mechanism of this kind may account for similar features in other aeolian landscapes. Limited bioturbation of lamellae occurred during the accumulation phase. Since establishment of a stable land surface during the Holocene, weathering, gleying, clay illuviation and bioturbation processes have been dominant with morphological features of present A and B horizons being superimposed on the uppermost lamellae and interlamellae." @default.
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- W1986661784 date "1989-10-01" @default.
- W1986661784 modified "2023-09-25" @default.
- W1986661784 title "Genesis of a texturally banded soil in Southland, New Zealand" @default.
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- W1986661784 doi "https://doi.org/10.1016/0016-7061(89)90056-6" @default.
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