“…Kenrick & Crane, ; Steemans et al, ; Salamon et al , ). Their increased abundance through the Silurian correlates with a marked decrease of the sheet‐braided style fluvial architecture, characterized by relatively thin and wide sediment bodies interpreted as channels much shallower and wider than the latter dominant meandering and braided streams (Cotter, ; Long, ; Fuller, ; Davies & Gibling, ; Davies et al, ; Bridgland, Bennett, McVicar‐Wright, & Scrivener, , but see Santos, Almeida, Godinho, Marconato, & Mountney, , Ielpi & Rainbird, , Ielpi, and Ganti, Whittaker, Lamb, & Fischer, for alternative views). Accordingly, the frequency of preserved meandering river deposits seems to increase from the Silurian to the present, in parallel to the adaptive evolution of land plants to new environments (Davies et al, ; Fuller, ; Gibling & Davies, ; Gibling et al, ; McMahon & Davies, ).…”