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• W2334851636 abstract "More than a half century ago, time was popularized as one of the state factors of soil formation. The accompanying concept of the “chronosequence” significantly impacted research efforts to understand the role of time in soil genesis. Two difficulties have plagued chronosequence soils studies: (i) small data sets (limited by what is available in nature), and (ii) variability within the data sets (introduced by geographical variations in other soil-forming factors). This paper describes a theoretical approach to developing more accurate chronofunctions in transgressive estuarine pedogenetic systems by minimizing these obstacles; it is here called the chrono-continuum. The encroachment of the sea on upland soils during the most recent coastal transgression caused a dramatic shift in pedogenetic processes, which brought about a number of significant changes in physical, chemical, mineralogical, and biological soil properties. The slowly rising sea level (a few mm/yr) has permitted the establishment of tidal marsh vegetation. The subsequent vertical accretionary growth of marsh vegetation generally has kept pace with sea-level rise. The rate of sea-level rise during an interval of marsh soil formation can be determined by various dating techniques, which can be related to the elevation of the submerged land surface through a topographic survey. In this way it is possible to recreate the relationship between sea level and the land surface at any point in the history of the marsh. Thus, the continuum in space (along the topographic surface) can be translated into a continuum in time. This permits one to sample a large number of points along the landscape that represent different points in time (addressing the first difficulty), and this can be done within a relatively small geographic distance (addressing the second difficulty)." @default.
• W2334851636 created "2016-06-24" @default.
• W2334851636 creator A5043010462 @default.
• W2334851636 date "1997-01-01" @default.
• W2334851636 modified "2023-09-27" @default.
• W2334851636 title "The Chrono-continuum: An Approach to Modeling Pedogenesis in Marsh Soils Along Transgressive Coastlines1" @default.
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• W2334851636 doi "https://doi.org/10.1097/00010694-199701000-00002" @default.
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