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An understanding of the potential sources and transformations of OC throughout the linked terrestrial and marine components of S2S systems provides a rich foundation for interpreting stratigraphic...
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Continental slopes and the adjacent deep basins are the ultimate sink for glacigenic sediment that has been supplied to the glacimarine transfer zone, reworked, and advected to the more distal part of...
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One indirect depositional proxy of episodic advance-retreat events on the continental shelf is the isolated hummocks and ridges found in many fjords or inner continental shelves, which are interpreted...
View ArticleDeriving erodibility metrics for landscape evolution
Observations from contemporary glaciated systems, primarily through marine geophysics (swath bathymetry, seismic), geochronology, and advances in sedimentary provenance, have proven instrumental in...
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For any given sedimentary basin, the contributing rivers may drain different areas. These fluvial systems can range from the largest-scale extra-basinal rivers that are linked to bedrock catchment...
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Prior to the MIS 2 lowstand, the Mississippi, Western Louisiana, and Brazos deltas were abandoned by their fluvial sources. Bentley et al. (2016--in this Vialinin A volume) review late Quaternary...
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