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The impact of vegetation on meandering rivers
The Palaeozoic evolution of land plants revolutionized river geomorphology. However, the
relationships between biotic forcing and channel dynamics are still debated and, as such …
relationships between biotic forcing and channel dynamics are still debated and, as such …
The role of discharge variability in the formation and preservation of alluvial sediment bodies
Extant, planform-based facies models for alluvial deposits are not fully fit for purpose,
because they over-emphasise plan form whereas there is little in the alluvial rock record that …
because they over-emphasise plan form whereas there is little in the alluvial rock record that …
[HTML][HTML] Resolving MISS conceptions and misconceptions: a geological approach to sedimentary surface textures generated by microbial and abiotic processes
The rock record contains a rich variety of sedimentary surface textures on siliciclastic
sandstone, siltstone and mudstone bedding planes. In recent years, an increasing number …
sandstone, siltstone and mudstone bedding planes. In recent years, an increasing number …
The environmental implications of upper Paleozoic plant-fossil assemblages with mixtures of wetland and drought-tolerant taxa in tropical Pangea
We evaluate the influences of elevation and climate on the spatio-temporal distribution of
wetland and dryland biomes during the Pennsylvanian and early Permian in tropical …
wetland and dryland biomes during the Pennsylvanian and early Permian in tropical …
Planform architecture, stratigraphic signature and morphodynamics of an exhumed Jurassic meander plain (Scalby Formation, Yorkshire, UK)
Modern fluvial meander plains exhibit complex planform transformations in response to
meander‐bend expansion, downstream migration and rotation. These transformations exert …
meander‐bend expansion, downstream migration and rotation. These transformations exert …
Uplands, lowlands, and climate: Taphonomic megabiases and the apparent rise of a xeromorphic, drought-tolerant flora during the Pennsylvanian-Permian transition
Abstract The Late Mississippian and Pennsylvanian have been referred to as the Coal Age
due to enormous paleotropical peat accumulations (coal beds). Numerous fossil floras have …
due to enormous paleotropical peat accumulations (coal beds). Numerous fossil floras have …
Coal-bearing fluvial cycles of the late Paleozoic tropics; astronomical control on sediment supply constrained by high-precision radioisotopic ages, Upper Silesian …
The late Paleozoic sedimentary record is well known for its mixed marine–terrestrial coal-
bearing sedimentary sequences, traditionally called cyclothems, and their hypothetical …
bearing sedimentary sequences, traditionally called cyclothems, and their hypothetical …
Considering river structure and stability in the light of evolution: feedbacks between riparian vegetation and hydrogeomorphology
River ecological functioning can be conceptualized according to a four‐dimensional
framework, based on the responses of aquatic and riparian communities to …
framework, based on the responses of aquatic and riparian communities to …
Palaeozoic co-evolution of rivers and vegetation: a synthesis of current knowledge
As vegetation evolved during the Palaeozoic Era, terrestrial landscapes were substantially
transformed, especially during the∼ 120 million year interval from the Devonian through the …
transformed, especially during the∼ 120 million year interval from the Devonian through the …
Formation and dynamics of vegetated fluvial landforms follow the biogeomorphological succession model in a channelized river
Feedback between hydrogeomorphological processes and riparian plants drives landscape
dynamics and vegetation succession in river corridors. We describe the consequences of …
dynamics and vegetation succession in river corridors. We describe the consequences of …