The Palaeozoic evolution of land plants revolutionized river geomorphology. However, the
relationships between biotic forcing and channel dynamics are still debated and, as such …

The Paleozoic emergence of terrestrial plants has been linked to a stepwise increase in
Earth's O 2 levels and a cooling of Earth's climate by drawdown of atmospheric CO 2 …

River management based solely on physical science has proven to be unsustainable and
unsuccessful, evidenced by the fact that the problems this approach intended to solve (eg …

Abstract The Late Paleozoic (Early Devonian to Middle Permian) was an interval of profound
changes in Earth-surface systems, reflected in dynamic interplay among the biosphere …

Recent robotic missions to Mars have offered new insights into the extent, diversity and
habitability of the Martian sedimentary rock record. Since the Curiosity rover landed in Gale …

We develop a conceptual framework for geo-evolutionary feedbacks which describes the
mutual interplay between landscape change and the evolution of traits of organisms residing …

Eco‐evolutionary dynamics, or eco‐evolution for short, are often thought to involve rapid
demography (ecology) and equally rapid heritable phenotypic changes (evolution) leading …

Anabranching rivers are characterized by multiple active channels. Vegetation, flow regime
and sediment retention are critical components for the formation, evolution and stability of …

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 …

The late Paleozoic sedimentary record is well known for its mixed marine–terrestrial coal-
bearing sedimentary sequences, traditionally called cyclothems, and their hypothetical …