FOSSIL MAMMALS FROM THE NEOGENE STRATA IN THE SINDA BASIN< EASTERN ZAIRE

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概要

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• Since 1989, a geological and paleontological expedition has been carried out in the Zairean part of the Western Rift Valley. During two field seasons, more than 600 fossil remains were collected in the Sinda basin, Gaty, Haut-Zaire, mainly as surface finds. This fossil collection contains 52 mammalian fossils which comprise the following taxa; ? Agriotherium, four proboscidean groups such as Prodeinotherium, ?Anancus, Mammuthus subplanifrons and Stegodon kaisensis, two Rhinocerotidae, i.e., ?Aceratherium and Brachypotherium, ?Sivatherium, Hippopotamus, and a bovid. The Sinda fauna is composed of both Miocene and Pliocene mammals and suggest that the strata including the fossils are of late Miocene to early Pliocene in age. This fauna resembles that from the Nkondo formation which is located in the Ugandan side of the Western Rift Valley. The composition of the fauna from the Sinda area may indicate a different paleoenvironment (probably more humid) in this area from that in contemporary East Africa. RESUME Depuis 1989, une expedition geologique et paleontologique est realisee dans la partie zairoise de la branche occidentale du Rift. Durant deux saisons, plus de 600 restes fossiles ont ete collectele basin de Sinda, Gaty, haut-za?re, principalement comme decouvertes de surface. Cette collection fossile contient 52 mammiferes fossiles qui comprennent les taxa suivant; ?Agriotherium, qutre groupes proboscidean tels que Prodeinotherium, ?Anancus, Mammuthus subplanifrons et Stegodon kaisensis, deux Rhinocerotidae par exemple, ?Aceratherium et Brachypotherium, ?Sivathrium, Hippopotamus, et un bovide. La faune de Sinda est composee des mammiferes du miocene et du pliocene et suggere que le strate inclus les fossils sont de l'age du miocene superieur au debut pliocene Cette faune ressemble celle de Nkondo formation qui est situee dans la partie ougandaise du Rift Occidental. La composition de la faune de l'aire de Sinda devra indique un paleoencironement different (probablement plus humide) dans cette aire de celui en l'est-aficain contemporain.

• 京都大学の論文

著者

• 久家 直之

  京都大・理

• 久家 直之

  横浜市旭区善部町50-29

• 久家 直之

  京都大学理学部地質学鉱物学教室

• 久家 直之

  綜合開発

• Kinya Yasui

  Department Of Anatomy 1 Dokkyo University School Of Medicine

• Hidemi ISHIDA

  Faculty of Human Sciences, Osaka University

• ISHIDA Hidemi

  Department of Human Nursing, University of Shiga Prefecture

• ISHIDA Hidemi

  Laboratory of Physical Anthropology, Graduate School of Science, Kyoto University

• Yutaka KUNIMATSU

  Laboratory of Physical Anthropology, Kyoto University

• Naoyuki KUGA

  Laboratory of Paleontology, Kyoto University

• Baluku BAJOPE

  Department of Biology, Centre de Recherche en Sciences Naturelles

• Hidemi ISHIDA

  Laboratory of Physical Anthropology, Kyoto University

• Yutaka Kunimatsu

  Laboratory Of Physical Anthropology Kyoto University

• Yasui Kinya

  Department Of Orai Anatomy 1 Kagoshima University Dental School

• Naoyuki Kuga

  Department Of Geology And Mineralogy Kyoto University

• Baluku Bajope

  Centre De Recherche En Sciences Naturelles

• Hidemi Ishida

  Laboratory Of Physical Anthropology Kyoto University

• Hidemi Ishida

  Laboratory Of Physical Anthropology Department Of Zoology Kyoto University

• Hidemi Ishida

  Department Of Human Nursing University Of Shiga Prefecture

• 石田 英実

  京都大学理学部自然人類学研究室

• KUNIMATSU Yutaka

  Laboratory of Physical Anthropology, Kyoto University

• KUGA Naoyuki

  Laboratory of Paleontology, Kyoto University

• BAJOPE Baluku

  Department of Biology, Centre de Recherche en Sciences Naturelles

• ISHIDA HIDEMI

  Department of Nursing, Seisen University, Hikone

• KUNIMATSU Yutaka

  Laboratory of Physical Anthropology, Department of Biology, Faculty of Science, Kyoto University

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