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Direct correlation of radiolarian <Emphasis Type="Italic">Kilinora spiralis</Emphasis> Zone with the Late Jurassic ammonite faunal succession in the Kurisaka Formation,Kurosegawa Terrane,SW Japan
Authors:Keisuke Ishida  Yasuyuki Tsujino  Takeshi Kozai  Tadashi Sato  Francis Hirsch
Institution:1.Laboratory of Geology, Institute of SAS, Faculty of Science,University of Tokushima,Tokushima,Japan;2.Tokushima Prefectural Museum, Bunka-no-Mori Park,Tokushima,Japan;3.Laboratory of Geosciences,Naruto University of Education,Naruto,Japan;4.Fukada Geological Institute,Bunkyo-Ku, Tokyo,Japan
Abstract:The last appearance datum of the radiolarian Kilinora spiralis is recorded above the first appearance datum of the ammonite Ataxioceras (A.) kurisakense in the Todoro Section of the Kurisaka Formation, Southern Kurosegawa Terrane, Shikoku, SW Japan. The constraint by ammonite age prolongs the range of the Kilinora spiralis Zone, a remarkable Jurassic radiolarian zone in Japan-NW Pacific region, into the lower Kimmeridgian. The direct correlation of the Kilinora spiralis zone with the Late Jurassic ammonite faunal succession in the Kurisaka Formation will provide a clue to the still pending chronological difference between European and North American radiolarian zones.
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