rsos172250_si_002.JPG (793.32 kB)
S2. Synsedimentary folding in the unit 15 near Arenicolites horizons. from Penetrative trace fossils from the late Ediacaran of Mongolia: early onset of the agronomic revolution
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posted on 2018-02-09, 12:14 authored by Tatsuo Oji, Stephen Q. Dornbos, Keigo Yada, Hitoshi Hasegawa, Sersmaa Gonchigdorj, Takafumi Mochizuki, Hideko Takayanagi, Yasufumi IryuSynsedimentary folding in the unit 15 near Arenicolites horizons, showing a ductile deformation of beds. This deformation also shows that the limestone beds were soft after deposition, allowing penetration of benthic organisms into the sediments.