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Platanoid leaves from Cenomanian to Turonian Mikasa Formation, northern Japan and their mode of occurrence
Authors
Matsumoto Midori
Narita Atsufumi
Yamada Toshihiro
Publication date
30 April 2008
Publisher
'The Paleontological Society of Japan'
Doi
Abstract
金沢大学理工研究域自然システム学系Ettingshausenia cuneifolia is reported from the Cenomanian to Turonian Mikasa Formation of central Hokkaido. These leaves occur exclusively in carbonaceous mudstone deposited in either lagoon or marsh. Based on their mode of occurrence, these remnants may have been trapped in the sediments without long prior transport (parautochthonous). © by the Palaeontological Society of Japan
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Last time updated on 06/05/2019