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Clay templates in Ediacaran vendotaeniaceans: Implications for the taphonomy of carbonaceous fossils
B. Becker-Kerber; A. Abd Elmola; A. Zhuravlev; C. Gaucher; M.G. Simões; G.M.E.M. Prado; J.A. Gámez Vintaned; C. Fontaine; L.M. Lino; D. Ferreira Sanchez; D. Galante; P.S.G. Paim; F. Callefo; G. Kerber; A. Meunier; A. El Albani
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Cover Image
Cover Image
Cover: Picture taken from an unmanned aerial vehicle (DJI Mavic 2 pro) of a large marble block (50 m diameter) within a 200 m-thick wildflysch-type deposit on Kalymnos (Greece). Coordinates of the drone and its elevation: UTM35 492698E, 4099923N, 20 m a.s.l. The Triassic olistostrome is most likely related to the closure of the Paleotethys. See “Paleogeographic position of the central Dodecanese Islands, southeastern Greece: The push-pull of Pelagonia” by Grasemann et al., p. 1506–1528.
Photo by: B. Grasemann.
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