The Mississippi River provides an opportunity to examine models of sediment transport in large alluviated floodplain systems. We test the idea that sources of sandy sediment in such settings are invariable on timescales <104 y because of storage and recycling in the floodplains. To reconstruct the development of the Mississippi sediment load over the past 2500 years we collected sediment from an abandoned point bar complex nearby at False River, Louisiana, USA. We also took annual samples from the lower reaches between 2015 and 2021 to assess changes on that timescale. Optically stimulated luminescence dating indicated that the point bar accreted between 2460 and 860 years ago. Detrital zircon U-Pb dating was used to assess sediment source ...
Understanding climatic influences on the rates and mechanisms of landscape erosion is an unresolved ...
Understanding climatic influences on the rates and mechanisms of landscape erosion is an unresolved ...
The Appalachian and Cordilleran orogenic belts of North America and their related sedimentary basins...
Data related to modern and Holocene sands from the lower Mississippi River. Published inClimate and ...
During Pleistocene glacial cycles, ice sheets advanced into the drainage basins of North America, wa...
The response of continental-scale drainage systems to short-term (i.e., millennial-scale) climate ch...
Analytical methods, regional geological summary, zircon age compilation, and statistical testing of ...
The lower Mississippi valley contains multiple large braid belts for which age control has been limi...
Floodplain development, land-use, and flooding on the lower Ohio River are investigated with a 3100-...
Accelerated soil erosion has become a pervasive feature on landscapes around the world and is recogn...
The preservation of conglomerates far from mountainous sources is commonly interpreted in terms of t...
The preservation of conglomerates far from mountainous sources is commonly interpreted in terms of t...
As climate is changing rapidly, there is an increasing need to understand how water and soil resourc...
The change from Pliocene to Pleistocene fluvial sedimentation in Nebraska is denoted by gravel with ...
Understanding climatic influences on the rates and mechanisms of landscape erosion is an unresolved ...
Understanding climatic influences on the rates and mechanisms of landscape erosion is an unresolved ...
Understanding climatic influences on the rates and mechanisms of landscape erosion is an unresolved ...
The Appalachian and Cordilleran orogenic belts of North America and their related sedimentary basins...
Data related to modern and Holocene sands from the lower Mississippi River. Published inClimate and ...
During Pleistocene glacial cycles, ice sheets advanced into the drainage basins of North America, wa...
The response of continental-scale drainage systems to short-term (i.e., millennial-scale) climate ch...
Analytical methods, regional geological summary, zircon age compilation, and statistical testing of ...
The lower Mississippi valley contains multiple large braid belts for which age control has been limi...
Floodplain development, land-use, and flooding on the lower Ohio River are investigated with a 3100-...
Accelerated soil erosion has become a pervasive feature on landscapes around the world and is recogn...
The preservation of conglomerates far from mountainous sources is commonly interpreted in terms of t...
The preservation of conglomerates far from mountainous sources is commonly interpreted in terms of t...
As climate is changing rapidly, there is an increasing need to understand how water and soil resourc...
The change from Pliocene to Pleistocene fluvial sedimentation in Nebraska is denoted by gravel with ...
Understanding climatic influences on the rates and mechanisms of landscape erosion is an unresolved ...
Understanding climatic influences on the rates and mechanisms of landscape erosion is an unresolved ...
Understanding climatic influences on the rates and mechanisms of landscape erosion is an unresolved ...
The Appalachian and Cordilleran orogenic belts of North America and their related sedimentary basins...