日本語
 
Help Privacy Policy ポリシー/免責事項
  詳細検索ブラウズ

アイテム詳細

登録内容を編集ファイル形式で保存
 
 
ダウンロード電子メール
  Oxygen isotope ratios of sedimentary biogenic silica reflect the European transcontinental climate gradient

Tyler, J. J., Leng, M. J., Sloane, H. J., Sachse, D., & Gleixner, G. (2008). Oxygen isotope ratios of sedimentary biogenic silica reflect the European transcontinental climate gradient. Journal of Quaternary Science, 23(4), 341-350. doi:10.1002/jqs.1172.

Item is

基本情報

表示: 非表示:
資料種別: 学術論文

ファイル

表示: ファイル
非表示: ファイル
:
BGC1123.pdf (出版社版), 222KB
 
ファイルのパーマリンク:
-
ファイル名:
BGC1123.pdf
説明:
-
OA-Status:
閲覧制限:
制限付き (Max Planck Institute for Biogeochemistry, MJBK; )
MIMEタイプ / チェックサム:
application/octet-stream
技術的なメタデータ:
著作権日付:
-
著作権情報:
-
CCライセンス:
-

関連URL

表示:

作成者

表示:
非表示:
 作成者:
Tyler, J. J., 著者
Leng, M. J., 著者
Sloane, H. J., 著者
Sachse, D., 著者
Gleixner, G.1, 著者           
所属:
1Molecular Biogeochemistry Group, Dr. G. Gleixner, Department Biogeochemical Processes, Prof. E.-D. Schulze, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497773              

内容説明

表示:
非表示:
キーワード: Oxygen isotopes Diatoms Biogenic silica Palaeoclimate Lakes Hydrogen isotopes N-alkanes Biomarkers Diatom silica Meteoric precipitation Lake-sediments Marine diatoms N-alkanes Record Delta-o-18 Water Fractionation Temperature
 要旨: Oxygen isotope ratios of biogenic silica offer considerable potential in tracing past climate change using both marine and lacustrine sediment records. Despite recent improvements and standardisation in preparatory and analytical methods, evidence for a systematic relationship between climate parameters and the oxygen isotope composition of sedimentary diatom silica (delta O-18(silica)) is contradictory. In particular, observed differences between the delta O-18(silica) of living and sedimentary diatom silica in both lake and marine environments question the validity of applying isotope fractionation models derived from living diatoms to reconstructing climate from sediment records. In order to address this issue, oxygen isotope ratios of biogenic silica (delta O-18(silica)) are examined from a suite of lake surface sediment samples which span a large climatic gradient across western Europe. delta O-18(silica) values are strongly correlated with air temperature and the isotope composition of precipitation (delta O-18(p)). When evaporation of lake waters is accounted for, the time-averaged surface sediment data suggest a fractionation of similar to 35 parts per thousand between water and biogenic silica. However, the effect of temperature appears less marked than that observed between contemporary diatoms and lake water over short timescales, suggesting that diagenetic processes may lead to a reduction in the temperature sensitivity of sediment delta O-18(silica) records. Comparison of delta O-18(silica) data with delta D analysed from n-alkanes of aquatic origin (n-C17, n-C21 and n-C23) demonstrates that the slope of the regional delta O-18:delta D water line is preserved within the sediment record, offering exciting potential for palaeoclimate research. (c) Natural Environment Research Council (NERC) copyright 2008. Reproduced with the permission of NERC. Published by John Wiley & Sons, Ltd. [References: 44]

資料詳細

表示:
非表示:
言語:
 日付: 2008
 出版の状態: 出版
 ページ: -
 出版情報: -
 目次: -
 査読: -
 識別子(DOI, ISBNなど): DOI: 10.1002/jqs.1172
その他: BGC1123
 学位: -

関連イベント

表示:

訴訟

表示:

Project information

表示:

出版物 1

表示:
非表示:
出版物名: Journal of Quaternary Science
種別: 学術雑誌
 著者・編者:
所属:
出版社, 出版地: Chichester : John Wiley & Sons, Ltd.
ページ: - 巻号: 23 (4) 通巻号: - 開始・終了ページ: 341 - 350 識別子(ISBN, ISSN, DOIなど): CoNE: https://pure.mpg.de/cone/journals/resource/954925500137
ISSN: 0267-8179