ホロセンの半ばの熱帯西太平洋の温度と表面海水バランス
1M. K. Gagan, L. K. Ayliffe, J. A. Cali, G. E. Mortimer, M. T. McCulloch, Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia. D. Hopley, Sir George Fisher Centre, James Cook University, Townsvil.
まとめ
5350年前のサンゴ礁のデータは,熱帯海面が1°C暖かく,0.5‰が酸素-18 (18O) で濃縮されていることを示しています. この温暖化により蒸発が増加し,地球規模の気候パターンに潜在的に影響し,古気候記録を調和させました.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- マリン・ジオケミストリー (海洋地化学)
背景:
- 珊瑚の骨格記録は,過去の海洋状態の代理を提供している.
- 過去の海洋温度と同位体組成を理解することは,気候モデリングに不可欠です.
研究 の 目的:
- 約5350年前の熱帯海の表面状態を再現するために.
- 海洋温度と酸素同位体 (18O/16O) 濃縮の関係について調査する.
主な方法:
- 温度再構築のためのグレートバリアリーフのサンゴの骨格性ストロンチウム/カルシウム (Sr/Ca) 比率の分析.
- 珊瑚の骨格における酸素同位体 (18O/16O) の比率を測定し,海水の組成を決定する.
主要な成果:
- 熱帯海の表面温度は,現代の値より約1°C高かった.
- 海水は18Oで0.5ミリ濃度で濃縮され,蒸発が増加したことを示した.
- この18O濃縮は,熱帯外の気候に影響を及ぼし,氷河期とホロセンの18O/16Oシフトを減少させたのかもしれない.
結論:
- ホロセンの半ばの温暖化により,海洋の蒸発が増加し,18O濃縮に至った.
- この同位体異常は,過去の気候動態と脱氷の理解に意味を持つ可能性があります.
- 珊瑚の Sr/Ca と,フォラミニフェラル酸素同位体温度履歴の不一致を調和させる.
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