Abstract
A temporary and drastic decrease in 34S/32S ratio of whole rock sulfide has been recognized at the suspected Permian/Triassic (P/Tr) boundary at Tenjinmaru in the Chichibu Terrane in eastern Shikoku, Japan, which is characterized by the occurrence of a carbonaceous black mudstone. The observed isotopic profile in the P/Tr section is in striking contrast in mode of 34S/32S excursion to that at the K/T boundary at Kawaruppu in eastern Hokkaido, Japan, and adds to significant geochemical constraint to the current arguments on the palaeoenvironmental changes during the time of terminal Permian mass extinction. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 59-65 |
| Number of pages | 7 |
| Journal | Annual Report - University of Tsukuba, Institute of Geoscience |
| Volume | 19 |
| Publication status | Published - Jan 1 1993 |
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All Science Journal Classification (ASJC) codes
- Environmental Science(all)
- Earth and Planetary Sciences(all)
Cite this
Sulfur isotopic data from the Permian/Triassic boundary at Tenjinmaru in the Chichibu Terrane in eastern Shikoku, Japan. / Kajiwara, Y.; Yamakita, S.; Kobayashi, D.; Imai, A.
In: Annual Report - University of Tsukuba, Institute of Geoscience, Vol. 19, 01.01.1993, p. 59-65.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Sulfur isotopic data from the Permian/Triassic boundary at Tenjinmaru in the Chichibu Terrane in eastern Shikoku, Japan
AU - Kajiwara, Y.
AU - Yamakita, S.
AU - Kobayashi, D.
AU - Imai, A.
PY - 1993/1/1
Y1 - 1993/1/1
N2 - A temporary and drastic decrease in 34S/32S ratio of whole rock sulfide has been recognized at the suspected Permian/Triassic (P/Tr) boundary at Tenjinmaru in the Chichibu Terrane in eastern Shikoku, Japan, which is characterized by the occurrence of a carbonaceous black mudstone. The observed isotopic profile in the P/Tr section is in striking contrast in mode of 34S/32S excursion to that at the K/T boundary at Kawaruppu in eastern Hokkaido, Japan, and adds to significant geochemical constraint to the current arguments on the palaeoenvironmental changes during the time of terminal Permian mass extinction. -from Authors
AB - A temporary and drastic decrease in 34S/32S ratio of whole rock sulfide has been recognized at the suspected Permian/Triassic (P/Tr) boundary at Tenjinmaru in the Chichibu Terrane in eastern Shikoku, Japan, which is characterized by the occurrence of a carbonaceous black mudstone. The observed isotopic profile in the P/Tr section is in striking contrast in mode of 34S/32S excursion to that at the K/T boundary at Kawaruppu in eastern Hokkaido, Japan, and adds to significant geochemical constraint to the current arguments on the palaeoenvironmental changes during the time of terminal Permian mass extinction. -from Authors
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UR - http://www.scopus.com/inward/citedby.url?scp=0027844338&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0027844338
VL - 19
SP - 59
EP - 65
JO - Annual Report - University of Tsukuba, Institute of Geoscience
JF - Annual Report - University of Tsukuba, Institute of Geoscience
ER -