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Hokkaido University Collection of Scholarly and Academic Papers >
Graduate School of Science / Faculty of Science >
Peer-reviewed Journal Articles, etc >
Geochemical and Microstructural Signals in Giant Clam Tridacna maxima Recorded Typhoon Events at Okinotori Island, Japan
| Title: | Geochemical and Microstructural Signals in Giant Clam Tridacna maxima Recorded Typhoon Events at Okinotori Island, Japan |
| Authors: | Komagoe, Taro Browse this author | | Watanabe, Tsuyoshi Browse this author →KAKEN DB | | Shirai, Kotaro Browse this author →KAKEN DB | | Yamazaki, Atsuko Browse this author | | Uematu, Mitsuo Browse this author |
| Keywords: | giant clam | | typhoon | | sclerochronology | | oxygen isotope ratio | | trace elements |
| Issue Date: | May-2018 |
| Publisher: | American Geophysical Union |
| Journal Title: | Journal of geophysical research biogeosciences |
| Volume: | 123 |
| Issue: | 5 |
| Start Page: | 1460 |
| End Page: | 1474 |
| Publisher DOI: | 10.1029/2017JG004082 |
| Abstract: | To validate the usability of the giant clam shell as a recorder of short-term environmental changes such as typhoons, we collected a live Tridacna maxima from Okinotori Island, Japan, on 15 June 2006. Growth increment thickness, stable isotope ratio (O-18(shell), C-13(shell)), and the barium/calcium ratio (Ba/Ca) in the T.maxima shell sample were measured and compared to Okinotori Island instrumental environmental data. In the outer layer of the shell sample, there were 3656 growth increments per year, as estimated by the O-18(shell) profile compared with sea surface temperature. The growth increments in the specimen were formed daily, and thus, we can determine the date of the sampling points of O-18(shell), C-13(shell) and the Ba/Ca ratio by counting growth increments. After typhoon approach, there is a decrease in increment thickness and some disturbed growth increments. The positive peaks in the shell Ba/Ca ratio and O-18(shell) corresponded to lower sea surface temperature caused by typhoons. These results indicated that the microstructural and geochemical record in Tridacna maxima shells could be useful for detecting past typhoon events. |
| Rights: | Copyright 2018 American Geophysical Union |
| Type: | article |
| URI: | http://hdl.handle.net/2115/71789 |
| Appears in Collections: | 理学院・理学研究院 (Graduate School of Science / Faculty of Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)
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Submitter: 渡邊 剛
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