書誌事項
- タイトル別名
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- δ<13>^C vertical change of peat in the Ozegahara Wetland
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Carbon isotope composition of peats in wetlands has been widely studied to understand paleoenvironment. In this study carbon isotope ratio (^<13>C/^<12>C) of the holocellulose and lignin components of peat in the Ozegahara Wetland were measured separately. The δ^<13>C values of the untreated peat show a decrease with the sampling depth. The reason for the decrease has been proved that the lignin compornent having lower δ^<13>C value became more dominant with the increasing depth. Lignin is more preservative than holocellulose and it is considered that the δ^<13>C value of lignin gives more straightforward information of paleoenvironment. The change of the δ^<13>C value resembles that of the burial rate based on ^<14>C-age, which is corrected assuming that only holocellulose have decayed exponentially. It is likely that the growth of plants in the Ozegahara Wetland increased between 7000 to 2000 years before present.
収録刊行物
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- 名古屋大学加速器質量分析計業績報告書
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名古屋大学加速器質量分析計業績報告書 8 146-151, 1997-03
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
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詳細情報 詳細情報について
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- CRID
- 1390572174357872128
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- NII論文ID
- 110000476032
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- NII書誌ID
- AN10305282
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- HANDLE
- 2237/13341
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- IRDB
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用可