書誌事項
- タイトル別名
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- Environments of Ocean and Primary Productivity during the Late Quaternary. Biomarkers as Tools for Reconstructing Paleoenvironments.
- コカンキョウ オ フクゲンスル シヒョウ トシテノ バイオマーカー タイヘイヨ
- 太平洋における深海底堆積物を例として
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We present analytical results of organic compounds in the deep sea sediments recovered from the Central Pacific and the western tropical Pacific and describe recent progresses in sedimentary biomolecules as tools for reconstructing paleoenviroments. Biomolecules derived from terrestrial higher plants such as C25-C35 n-alkanes, C24-C28 fatty alcohols, or C23-C34 fatty acids in the surface sediments from 175° E transect show high concentrations in the higher latitudes in the Northern Hemisphere. Relative abundances of these terrestrial biomarkers are markedly different between low (15°N-15°S) and high (48°N-19°N) latitudes. Such a difference could be interpreted in terms of different wind regimes between the two areas. Unsaturation degree of long-chain alkenones (Uk37) derived from haptophyte algae suggests that sea surface temperature in the western tropical Pacific during the last glacial maximum was nearly the same as that of the present. We also found that the alkenone abundances over the last 20 kyr are anti-correlated with sedimentary nitrogen isotopic ratios, suggesting that a production rate of alkenones by haptophyte algae is controlled by the nutritional state of the algae.
収録刊行物
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- 地学雑誌
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地学雑誌 107 (2), 189-202, 1998
公益社団法人 東京地学協会
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詳細情報 詳細情報について
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- CRID
- 1390001204230130688
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- NII論文ID
- 10002237496
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- NII書誌ID
- AN00322536
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- ISSN
- 18840884
- 0022135X
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- NDL書誌ID
- 4480488
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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
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可