著者

沢田 順弘 中山 勝博 実吉 玄貴

出版者

島根大学

雑誌

島根大学地球資源環境学研究報告 (ISSN:13439774)

巻号頁・発行日

vol.20, pp.13-23, 2001-12-28

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The Miocene strata in the Nachola area,northern Kenya have yielded many hominoid fossils which are important for the study of hominid evolution.The Joint Japan-Kenya team has conducted palaeontological excavations at Nachola since 1982 and has collected abundant fossil fauna,especially of Nacholapithecus,a hominoid of the Kenyapithecus group.13;Nacholapithecus fossils were found at 15 sites in a thin horizon in the lowest part(15 Ma)of the Middle Miocene Aka Aiteputh Formation,scattered over an outcrop area of 13 km×3 km.The fossiliferous strata are covered by thick basalt lava flows.Clastic sedimentary rocks at representative fossil sites BG-K and BG-I are volcaniclastic and have been subdivided into at least 10 units,totaling about 13 m maximum thickness.Most of the clastic sediments are characteristically poorly sorted and are matrix supported with pyroclastic matrix and pumice(less than 2 cm in diameter).13;They were mainly derived from a lahar,except for some units formed by flood or pyroclastic flow.Pyroclastic materials include volcanic glass,anorthoclase and aegirine augite derived from phonolitic trachyte.The Nacholapithecus fossils are well preserved,and many of the skeletal parts are in connection,especially at the site BG-K.13;The hominoids seem to have been buried alive,similar to the situation that occurred on November13th,1985,at Amlero town,Colombia.Excavated fossils comprise many individuals of various age groups(infants to aged adults of both sexes)which may allow us to launch a new field of study,"palaeo-primate sociology",which will throw light on the population structure of Macholapithecus groups.

著者

中山 勝博 河村 善也

出版者

地学団体研究会

雑誌

地球科學 (ISSN:03666611)

巻号頁・発行日

vol.47, no.4, pp.289-300, 1993-07-25

被引用文献数

1

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The Plio-Pleistocene Osaka Group in the Nara Hills is composed mainly of fluvio-lacustrine sediments with 15 intercalations of volcanic ash. Of these volcanic ash layers, nine principal layers are described in detail on the basis of lithology and analyses of mineral assemblage and of glass shape and refractive index. The results of the observation and analyses indicate that four of them such as the Pumice-sand, Shimoumedani, Kurokamiyama II, and Takanohara volcanic ash layers are correlative with the Higashibata, Fugenji, Susudani I, and Zakuro volcanic ash layers in the adjacent Tanabe Hills respectively. Further, the Shimoumedani, Kurokamiyama II, and Takanohara volcanic ash layers are correlated with the Fukuda, Yellow IV, and Pink volcanic ash layers in the SennanSenpoku Hills respectively, where one of the stratotypes of the Osaka Group is exposed. The correlation indicates that the Osaka Group in the Nara Hills is assignable to the lower-most and lower parts of the standard sequence of the group.