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The Eifelian-aged Hangman Sandstone Formation of southwest England is a unit of the ‘Old Red Sandstone’ that has traditionally been considered relatively barren of trace fossils. Following recent investigations, we here show it to contain the mos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::141c3b281d9e4dbb86c42bf3e7be0af8
https://www.repository.cam.ac.uk/handle/1810/350609
https://www.repository.cam.ac.uk/handle/1810/350609
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 621:111579
The mid-Palaeozoic was a significant interval in the evolution of plants, during which their biogeomorphic influence on terrestrial landscapes increased dramatically. The products of plant-sediment interactions are well known from Carboniferous strat