Platanoid leaves from Cenomanian to Turonian Mikasa Formation, northern Japan and their mode of occurrence

Atsufumi Narita; Toshihiro Yamada; Midori Matsumoto

doi:10.2517/1342-8144(2008)12[81:PLFCTT]2.0.CO;2

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Atsufumi Narita,¹ Toshihiro Yamada,^2,* Midori Matsumoto³

¹1Laboratory of Ecological and Systematic Botany, Graduate School of Agriculture, Hokkaido University
²2Division of Life Sciences, Graduate School of Natural Science and Technology, Kanazawa University,
³3Department of Earth Science, Graduate School of Science, Chiba University, Chiba, 263-8522, Japan

^** Author for correspondence

Abstract

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).

Citation Download Citation

Atsufumi Narita, Toshihiro Yamada, and Midori Matsumoto "Platanoid leaves from Cenomanian to Turonian Mikasa Formation, northern Japan and their mode of occurrence," Paleontological Research 12(1), 81-88, (1 April 2008). https://doi.org/10.2517/1342-8144(2008)12[81:PLFCTT]2.0.CO;2

Received: 23 February 2007; Accepted: 1 November 2007; Published: 1 April 2008

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