Japan Geoscience Union Meeting 2015

Presentation information

Oral

Symbol M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS30] Evolution of the Pelagic Realm

Tue. May 26, 2015 9:00 AM - 10:45 AM 304 (3F)

Convener:*Atsushi Matsuoka(Department of Geology, Faculty of Science, Niigata University), Toshiyuki Kurihara(Graduate School of Science and Technology, Niigata University), Yasuhiro Kato(Department of Systems Innovation, Graduate School of Engineering, University of Tokyo), Tetsuji Onoue(Earth and Environmental Sciences, Graduate School of Science and Technology, Kumamoto University), Katsunori Kimoto(Japan Agency for Marine-Earth Science and Technology), Tatsuo Nozaki(Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology), Hayato Ueda(Department of Geology, Niigata University), Kenta Kobayashi(Department of Geology, Faculty of Science, Niigata University), Takashi Hasegawa(Division of Global Environmental Science and Engineering, Graduate School of Natural Science and Technology, Kanazawa University), Chair:Hayato Ueda(Department of Geology, Niigata University), Satoshi Takahashi(Department of Earth and Planetary Science, University of Tokyo)

9:45 AM - 10:00 AM

[MIS30-04] Chemostratigraphy of the Middle Triassic bedded chert sequence in the Mino Belt, central Japan

*Katsuhito SODA1, Tetsuji ONOUE1 (1.Kumamoto Univ.)

Previous studies have proposed that the alterations of chert and shale beds in the bedded chert sequence of the Japanese Jurassic accretionary complex are paced by precession and eccentricity cycles, especially chert bed thickness variation is interpreted as productivity fluctuations. However, the cyclostratigraphic interpretations and the continuity of sequence between sections await further verification (Ogg, 2014). In this study, we focus on shale beds as geochemical proxies for stratigraphic correlation and paleoclimatological interpretation. Then we conducted geologic survey at Section M, CH2L, L, and B (Anisian and Ladinian based on detailed radiolarian biostratigraphy by Sugiyama, 1997), reconstructed the composite column using stratigraphic correlation of lithological associations between sections, and collected shale bed samples with bed by bed resolution for geochemical analysis (more than 500 samples). The reconstructed lithostratigraphy of the Middle Triassic bedded chert sequence consists of lower gray bedded chert, lower red bedded chert, upper gray bedded chert, and upper red bedded chert in ascending order (Ikeda et al., 2010). The elemental compositions in shale beds are determined by XRF analysis. In presentation, we will discuss about the geochemical characteristics of shale beds, the chemostratigraphy of the Middle Triassic bedded chert sequence, and their implications.