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).
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1 April 2008
Platanoid leaves from Cenomanian to Turonian Mikasa Formation, northern Japan and their mode of occurrence
Atsufumi Narita,
Toshihiro Yamada,
Midori Matsumoto
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Cenomanian-Turonian
early Eudicots
Ettingshausenia
Mikasa Formation
platanoid