地質調査研究報告/Bulletin of the Geological Survey of Japan

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1 Hideaki Nagamori, Hiroaki Yoshikawa, Koji Hatakeyama, Masumi Terao and Tomotaka Tanabe (2005) Proboscidean footprint fossils from the Lower Pleistocene Okui Formation on the river bed of Chikuma River, Saku Basin, Nagano Prefecture, Central Japan. Bull. Geol. Surv. Japan, vol. 56(3/4), p , 6 figs. Abstract: Many proboscidean footprint fossils were found from the Lower Pleistocene Okui Formation in the Komoro Group at the Chikuma River in Tomi City, Nagano Prefecture. The stratigraphic horizon containing the trace fossils are situated about 2 meters above the Hakeyama Pumice Tuff (ca. 1.3 Ma). The trackmaker was most likely Stegodon aurorae (Matsumoto), based on the morphological characteristics of the footprints and proboscidean biostratigraphy of Japan. The palaeoenvironment of the horizon containing the footprints is considered to be formed at flood plain based on sedimentary facies and associated plant and molluskan fossils. Keywords: footprint fossil, Proboscidea, Stegodon aurorae, Nagano Prefecture, Tomi City, Komoro Group, Okui Formation, Early Pleistocene Fig. 1 Index map of the Nunoshita region, Tomi City with footprint fossils locality. (after the 1:25,000 scale topographical map of Ueda published by Geographical Survey Institute of Japan ),

2 Fig. 2 Outcrop of the upper Okui Formation containing footprint fossils and grid.

3 Fig. 3 Columnar section of the Upper Okui Formation on Nunoshita region, Tomi City. Refer to the Fig.1 for location.

4 Sedimentary column of footprint fossils production locality. Fig. 4

5 Fig. 5 A distribution map of footprint fossils.

6

7 Fig. 6 A : Cross section of the footprint fossil. B : Schematic cross section showing the lithofacies of the footprint.

8

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