サンゴ化石の地球化学記録から復元される氷期/間氷期の大気海洋変動 (特集 サンゴ骨格の地球化学)
デジタルデータあり(科学技術振興機構)
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J-STAGE
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- 資料種別
- 記事
- 著者・編者
- 浅海 竜司
- シリーズタイトル
- 著者標目
- 並列タイトル等
- Glacial and Interglacial Paleoclimate Variability Reconstructed from Geochemical Records in Fossil Corals : A Review
- タイトル(掲載誌)
- 地球化学 = Geochemistry
- 巻号年月日等(掲載誌)
- 59(4):2025
- 掲載巻
- 59
- 掲載号
- 4
- 掲載ページ
- 129-147
- 掲載年月日(W3CDTF)
- 2025
- ISSN(掲載誌)
- 0386-4073
- ISSN-L(掲載誌)
- 0386-4073
- 出版事項(掲載誌)
- 東京 : 日本地球化学会
- 出版地(国名コード)
- JP
- 本文の言語コード
- jpn
- NDLC
- 対象利用者
- 一般
- 所蔵機関
- 国立国会図書館
- 請求記号
- Z15-645
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館雑誌記事索引
- 書誌ID(NDLBibID)
- 034508686
- 整理区分コード
- 632
- 要約等
- <p>The interaction of tropical and subtropical sea-surface waters with the atmosphere on seasonal, interannual, and decadal timescales is one of the sources of climate changes. Understanding the Quaternary history of climate and ocean variability requires knowledge of how the ocean-atmosphere system operated in the past. Hermatypic scleractinian corals, especially <i>Porites</i> sp., are one of the best archives for extending the short and rather sparse instrumental record of sea-surface observations at monthly resolution. Coupled determinations of Sr/Ca ratio and oxygen isotope composition in fossil corals can yield high-resolution time series of sea-surface temperature and salinity with precise chronology, reconstructing seasonal-to-decadal climatic variability associated with the monsoon, the El Niño/Southern Oscillation, and the Pacific Decadal Oscillation during the Quaternary. This paper is a review of coral paleoclimatology, highlighting selected studies on coral-based climate reconstructions of surface ocean conditions during the Holocene, the last deglaciation, and the last interglacial. Although potential biases in paleoclimate reconstructions caused by diagenetic alteration, inter-colony offset, the past seawater chemistry, and errors of thermometers should be handled carefully, future works on skeletal geochemistry in corals with advanced analytical and statistical methods will provide a paleo-observational constraint on climate model simulations of ocean-atmosphere variability for the past.</p>
- DOI
- 10.14934/chikyukagaku.59.129
- オンライン閲覧公開範囲
- インターネット公開
- 連携機関・データベース
- 科学技術振興機構 : J-STAGE
- 要約等
- <p>The interaction of tropical and subtropical sea-surface waters with the atmosphere on seasonal, interannual, and decadal timescales is one of the sources of climate changes. Understanding the Quaternary history of climate and ocean variability requires knowledge of how the ocean-atmosphere system operated in the past. Hermatypic scleractinian corals, especially <i>Porites</i> sp., are one of the best archives for extending the short and rather sparse instrumental record of sea-surface observations at monthly resolution. Coupled determinations of Sr/Ca ratio and oxygen isotope composition in fossil corals can yield high-resolution time series of sea-surface temperature and salinity with precise chronology, reconstructing seasonal-to-decadal climatic variability associated with the monsoon, the El Niño/Southern Oscillation, and the Pacific Decadal Oscillation during the Quaternary. This paper is a review of coral paleoclimatology, highlighting selected studies on coral-based climate reconstructions of surface ocean conditions during the Holocene, the last deglaciation, and the last interglacial. Although potential biases in paleoclimate reconstructions caused by diagenetic alteration, inter-colony offset, the past seawater chemistry, and errors of thermometers should be handled carefully, future works on skeletal geochemistry in corals with advanced analytical and statistical methods will provide a paleo-observational constraint on climate model simulations of ocean-atmosphere variability for the past.</p>
- DOI
- 10.14934/chikyukagaku.59.129
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- Japan Link Center雑誌記事索引データベース
- 書誌ID(NDLBibID)
- 034508686