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The handful of studies that provide data on soil C stocks in buried horizons and estimate their spatial extent suggest that buried soils can contain significant regional OC reservoirs that are currently ignored in inventories and biogeochemical models.
However, biodegradable C in buried soils was less than that in the surface soils even though the buried soils usually had equal or larger quantities of total soil C and LF C. Our results suggest that the deposition of soil in depositional landscape positions in eroded landscapes constrained decomposition and mineralization of SOM.
Buried soils have well developed profiles and diagnostic features.
Buried soils of the Subatlantic period (Soil 2) are usually referred to as Luvisols.
Pedostratigraphy can be defined as the study of the stratigraphical and spatial relationships and implications of surface and buried soils.
These buried soils provide a record of changes in paleoecological and paleo-alluvial conditions spanning ~ 14 ky.
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The findings confirmed previously obtained results and indicated that the buried Soil 3 at the ZBS site could be developed under mixed forests dominated by spruce.
Buried soil horizons at Campitello Matese contain gibbsite, which suggests that these horizons weathered at the soil surface for relatively long periods before being buried by subsequent ash falls over the past 39 ka.
Evolution of the atmosphere is recorded by banded-iron formations (BIFs), paleosols (buried soil horizons), and red beds, whereas tillites (sedimentary rocks formed by the lithification of glacial till) provide clues to the climatic patterns that occurred during Precambrian glaciations.
The comparison of differences in properties of buried soil at specific times and historical data on cultures' functioning in these periods has allowed us to reveal the interrelation of nature and society processes development in South Kalmykia since the middle Holocene.
Horizons of an underlying buried soil may have become incorporated in the - now - Anthrosol.
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