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- W69451746 abstract "Paleosols which lack datable materials may be assigned to relative age sequences by evaluating the nature of soil materials and the degree of pedological organization. The chronological ordering of pedological episodes, which is important to reconstruction of paleoenvironments where sequences of soils and weathering zones occur, is based on strat-igraphic principles and practices. Episodic development in the pedo-sphere may be established by applying concepts of separate identity, lateral continuity, ascendancy and descendancy, weathering differen-tials, and pedogenic persistence to soil mantles. These concepts are used in the stratigraphic ordering of soils after proofs of existence have been established for independent (buried) soil layers. Although pedological features and soil fabrics provide a basis for identifying the presence of rock- and soil stratigraphic units in whole soil profiles, they also help establish the relative ages of juxtaposed soil materials. The nature of skeleton grains, especially those which are etched, embayed or inherited from previous cycles, are important to evaluations of soil process and stage of development. Organization of soil plasma into distinct fabrics can, when correlated with specific pedostratigraphic intervals, provide an additional means of establishing chronological sequences based on geographically disjunct paleosols. These methods are particularly useful in deeply weathered terrains, such as those associated with tropical and subtropical cratonic regions, where Quaternary soil–stratigraphic units overlie Tertiary weathering zones. Micromorphological techniques effectively differentiate pedo-genic episodes where younger soil-stratigraphic layers contain soil parent materials derived from pre-existing weathering mantles." @default.
- W69451746 created "2016-06-24" @default.
- W69451746 creator A5034215492 @default.
- W69451746 date "1984-01-01" @default.
- W69451746 modified "2023-09-23" @default.
- W69451746 title "Evaluation of Relative Pedostratigraphic Dating Methods, with Special Reference to Quaternary Successions Overlying Weathered Platform Materials" @default.
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- W69451746 doi "https://doi.org/10.1016/s0920-5446(08)70080-3" @default.
- W69451746 hasPublicationYear "1984" @default.
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