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- W2899685593 endingPage "862" @default.
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- W2899685593 abstract "Abstract In contrast to soils forming at present, soils that developed in the past require deciphering the effects of concurrent sedimentary processes and pedogenesis under fluctuating environmental conditions for their study. As a consequence, the discontinuity of soil evolution at geological timescales and the palimpsest-like memory of palaeosoils are the two basic principles that define the originality of palaeopedology. System analysis is applied to palaeosoils and relict soils for grouping sedimentary and pedological features and related attributes into distinctive pedosedimentary facies that are described at relevant microscopic scales. Time series of pedosedimentary facies allow for establishing the hierarchy of soil-forming processes and sedimentary processes. They are interpreted as sequences of events reflecting the succession of environmental and climatic changes. In this chapter, we present the most common hierarchies of textural, ferruginous and calcitic features and the related pedosedimentary facies that are encountered in palaeosoils and relict soils, in a wide diversity of geographical contexts. We more particularly focus on the characteristics of distinctive types of soil disturbance that help to recognise the type of transition between successive events: internal reworking, short-distance displacement, secondary deposition as pedosediments, settling of allogenic materials on exposed soil surfaces and their integration into the underlying horizons or pedosedimentary layers. The reported case studies illustrate the occasional preservation of high-quality palaeoenvironmental records in conditions of rapid burial." @default.
- W2899685593 created "2018-11-16" @default.
- W2899685593 creator A5024735056 @default.
- W2899685593 creator A5055482116 @default.
- W2899685593 creator A5091612050 @default.
- W2899685593 date "2018-01-01" @default.
- W2899685593 modified "2023-10-16" @default.
- W2899685593 title "Palaeosoils and Relict Soils" @default.
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