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件数:113件
[2012]
21.[] Changes in depth-transect redox conditions spanning the end-Permian mass extinction and their impact on the marine extinction: Evidence from biomarkers and sulfur isotopes..[Glob. Planet. Change,94-95,(2012),20-32]Kaiho, K., Oba M., Fukuda, Y., Ito, K., Ariyoshi, S., Gorjan, P., Riu, Y., Takahashi, S., Chen, Z-Q., Tong, J., Yamakita, S.
22.[] Significant changes in land vegetation and oceanic redox across the Cretaceous/Paleogene boundary..[Palaeogeogr., Palaeoclimatol., Palaeoecol.,369,(2012),41-42]Mizukami, T., Kaiho, K., Oba, M.
23.[] Carbon and sulfur isotope geochemistry of the Hirnantian (end-Ordovician) Wangjiawan (Riverside) section, South China: global correlation and environmental event interpretation..[Palaeogeogr., Palaeoclimatol., Palaeoecol.,337-338,(2012),14-22]Gorjan, P., Kaiho, K., Fike, D. A., Xu, C
[2011]
24.[] 現代地球科学入門シリーズ15、地球と生命:地球環境と生物圏進化.[共立出版,(2011)]掛川 武・海保邦夫
25.[] The Guadalupian-Lopingian boundary (Permian) in a pelagic sequence from Panthalassa recognized by integrated conodont and radiolarian biostratigraphy..[Micropaleontology,78,(2011),84-95]Nishikane, Y., Kaiho, K., Takahashi, S., Henderson, C.M., Suzuki, N. and Kanno M.
26.[] Short-term anoxia coinciding with rotaliporid extinctions during the Cenomanian–Turonian transition in the middle-neritic eastern North Atlantic inferred from organic compounds..[Geology,39,(2011),519-522]Oba, M., Kaiho, K., Okabe , T., Lamolda, M.A., Wright, J.D.
[2010]
27.[] A smooth negative shift of organic-carbon isotope ratios at an end-Permian mass extinction horizon in central pelagic Panthalassa.[Palaeogeography, Palaeoclimatology, Palaeoecology,292,(2010),532-539]Satoshi Takahashi, Kunio Kaiho, Masahiro Oba, Takeshi Kakegawa
28.[] An abrupt decrease in atmospheric oxygen by massive release of hydrogen sulfide during the End-Permian mass extinction..[Journal of Earth Science,21,(2010),141-142]Kaiho, K., Oba M., Takahashi S, Fukuda, Y., Koga, S., Chen, Z.Q., Yamakita, S.
[2009]
29.[] Response of ocean bottom dwellers exposed to underwater shock waves..[Shock Waves,(2009)]Hosseini, S. H. R., Kaiho, K., Takayama, K.
30.[] Possible causes for a negative shift in the stable carbon isotope ratio before, during and after the end-Permian mass extinction in Meishan, South China..[Australian Journal of Earth Sciences,56,(2009),799-808]Kaiho, K., Chen, Z.Q., Sawada K.
31.[] ペルム紀末大量絶滅事変:北部北上帯で確認されたペルム紀/三畳紀境界層の意義.[岩手の地学,39,(2009),1-11]高橋聡・山北聡・鈴木紀毅・海保邦夫・永広昌之
32.[] Panthalassic oceanic anoxia at the end of the Early Triassic: a cause of delay in the recovery of life after the end-Permian mass extinction,.[Palaeogeography, Palaeoclimatology, Palaeoecology,274,(2009),185-195]Takahashi, S., Oba, M., Kaiho, K., Yamakita, S.
33.[] Benzohopanes and diaromatic 8(14)-secohopanoids in some Late Permian carbonates..[Geochemical Journal,(2009)]Oba, M., Nakamura, M., Fukuda, Y., Katabuchi, M., Takahashi, S., Haikawa, M. and Kaiho, K.
34.[] High organic carbon content and a decrease in radiolarians at the end of the Permian in a newly discovered continuous pelagic section: a coincidence?,.[Palaeogeogr., Palaeoclimatol., Palaeoecol.,271,(2009),1-12]Takahashi, S., Yamakita, S., Suzuki, N., Kaiho, K., Ehiro, M.
[2008]
35.[] Hypervelocity impact of asteroid/comet on the oceanic crust of the earth.[International Journal of Impact Engineering,35,(2008),1770-1777]Saito, T., Kaiho K., Abe A., Katayama, M., Takayama, K.
36.[] ペルム紀末大量絶滅時の硫化水素大量放出事変.[Res. Org. Geochem.,23/24,(2008),5-11]海保邦夫
37.[] Timing and magnitude of early Aptian extreme warming: Unraveling primary δ18O variation in indurated pelagic carbonates at Deep Sea Drilling Project Site 463, central Pacific Ocean..[Palaeogeogr., Palaeoclimatol., Palaeoecol.,260(3-4),(2008),463-476]Ando, A., Kaiho, K., Kawahata, H., Kakegawa, T.
38.[] A carbon-isotopic study of an end-Permian mass-extinction horizon, Bulla, northern Italy: a negative δ13C shift prior to the marine extinction..[Terra Nova,20,(2008),253-258]Gorjan, P. Kaiho, K., Chen, Z.Q.
[2007]
39.[] Effects of sulfate aerosols induced by a large asteroid impact on ultra-violet radiation in the atmosphere.[Geophysical Research Letters,34,(2007),L23805-]Ishida, H., Kaiho, K., Asano S.
40.[] Paleoredox, biotic and sulfur-isotopic changes associated with the end-Permian mass extinction in the western Tethys.[Chemical Geology,244,(2007),483-492]Gorjan, P., Kaiho, K., Kakegawa, T., Niitsuma, S., Chen, Z.Q., Kajiwara, Y., Nicora, A.
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