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埋没泥炭土の有機物組成
https://doi.org/10.18999/sumrua.2.18
https://doi.org/10.18999/sumrua.2.18b0bae93e-a0d2-4cd3-9014-cc1e883117e3
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
KJ00000187487.pdf (482.6 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2010-04-23 | |||||
| タイトル | ||||||
| タイトル | 埋没泥炭土の有機物組成 | |||||
| 言語 | ja | |||||
| その他のタイトル | ||||||
| その他のタイトル | Radio-carbon dationg and analysis of phenolic and lipid compounds of peat profiles at Tsukude in central Japan | |||||
| 言語 | en | |||||
| 著者 |
筒木, 潔
× 筒木, 潔× Tsutsuki, Kiyoshi× 白石, 祐彰× Shiraishi, Hiroaki× 鍬塚, 昭三× Kuwatsuka, Shozo |
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| アクセス権 | ||||||
| アクセス権 | open access | |||||
| アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
| 権利 | ||||||
| 言語 | ja | |||||
| 権利情報 | 名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会 | |||||
| 権利 | ||||||
| 言語 | ja | |||||
| 権利情報 | 本文データは学協会の許諾に基づきCiNiiから複製したものである | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | A histosol profile at Tsukude in central Japan has the age of ca. 32,000 yBP and records a history of Holocene and Pleistcene periods in the composition of organic and inorganic components in it. We have determined C and N contents and compositions of phenolic and lipid compounds along with ^<14>C-ages of important layers, and considered the implication of the change in their compositions with age in relation to the climatic changes and the topographic changes around the wet land. The ratio of C/N and compositions of phenolic and lipid compounds were very stable in peat layers formed during the last glaciation maximum (20,000-30,000yBP). During the age of post-glacial warming and frequent volcanic explosions, the C/N ratio increased and the contents of phenolic and lipid compounds decreased, while the phenolic acid/aldehyde ratio increased, indicating that decomposition and humification of peaty material was enhanced in this age. A reverse trend was also observed between the yield of phenolic compounds and the ratio of phenolic acid/aldehyde ratio. Long chain fatty acids with chain length from 16 to 30 were detected in the peat, where the yield of montanic acid (C28) was largest. The shorter the chain length, the more unstable the fatty acids were. Yields and ratios of fatty acids seemed to reflect the environmental conditions in which each peat layers were formed. | |||||
| 言語 | en | |||||
| 出版者 | ||||||
| 出版者 | 名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会 | |||||
| 言語 | ja | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| 資源タイプ | ||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
| 資源タイプ | departmental bulletin paper | |||||
| 出版タイプ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
| ID登録 | ||||||
| ID登録 | 10.18999/sumrua.2.18 | |||||
| ID登録タイプ | JaLC | |||||
| 関連情報 | ||||||
| 関連タイプ | isVersionOf | |||||
| 識別子タイプ | URI | |||||
| 関連識別子 | http://ci.nii.ac.jp/naid/110000475756/ | |||||
| 書誌情報 |
ja : 名古屋大学加速器質量分析計業績報告書 巻 2, p. 18-25, 発行日 1991-03 |
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| フォーマット | ||||||
| 値 | application/pdf | |||||
| 著者版フラグ | ||||||
| 値 | publisher | |||||
