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Brimhall, G. H. et al. Deformational mass transport and invasive processes in soil evolution.
These paleosols provide evidence for Holocene soil evolution.
After deglaciation (11 12 ka BP), soil evolution was progressive.
We detect evidence of increasing human disturbance (regressive soil evolution) for about the last 1 ka.
It is now certain that soil evolution will be strongly influenced by climate change.
A micromorphological index of soil evolution in highly calcareous arid and semiarid conditions is proposed.
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The results suggest a strong relationship between landscape evolution, soil development and hydraulic properties.
Dating of fluvial deposits is essential for a more quantitative understanding of landscape evolution and soil development in floodplain environments.
As a geomorphologist, her research is driven by an overarching interest in abiotic vs. biotic, lithologic, and climatic controls on bedrock to soil conversion and implications for soil development and landscape evolution.
Soil development and landscape evolution were studied in the basin-shaped Phobjikha Valley at 2900 3200 m a.s.l., to the west of the Black Mountain Range, West Central Bhutan.
Soil geomorphological studies consist of six principal components, including the development of chronosequences, soils as indicators of landscape stability, soils as indicators of climate change, soil development and drainage basin evolution, soils as indicators of erosion and deposition processes, and soils as indicators of Quaternary parent materials and stratigraphy.
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