北極海のアラゴニット不飽和:海洋酸化と海氷の融解の影響
Michiyo Yamamoto-Kawai1, Fiona A McLaughlin, Eddy C Carmack
1Department of Fisheries and Oceans, Institute of Ocean Sciences, 9860 West Saanich Road, Sidney, British Columbia V8L 4B2, Canada. michiyo.kawai@dfo-mpo.gc.ca
まとめ
北極海の水域は,二酸化炭素排出量の増加と海氷の融解により,カルシウム炭酸に飽和していない状態になっています. この酸化は海洋生物を脅かし,北極の生態系全体に影響を与えています.
科学分野:
- 海洋学 海洋学とは
- マリン・バイオロジー マリン・バイオロジー
- 気候科学 気候科学
背景:
- 人為的な二酸化炭素排出量の増加は,海洋の酸化を推進しています.
- 北極の海氷の融解は,海洋の化学構造と循環パターンを変化させている.
研究 の 目的:
- 海洋酸化と海氷の融解がカナダ盆地におけるカルシウム炭酸塩飽和度状態に与える影響を調査する.
- これらの変化が北極の海洋生態系に及ぼす影響を評価する.
主な方法:
- カナダ盆地における地表水の化学分析.
- 海氷の面積とアラゴニトの飽和度状態の関係に関する評価.
主要な成果:
- カナダ流域の地表水は,2008年にアラゴニットに関して不飽和であることが判明しました.
- 広範囲にわたる海氷の融解が,この過飽和の主要な原因として特定されました.
- 海氷の退去は,飽和していない地下水の上流を大陸棚に増加させた.
結論:
- 海洋酸性化と海氷の融解は,北極海の飽和状態を低減しています.
- これらの変化は,石灰化プランクトンと無脊椎動物にとって重大な脅威となる.
- 北極の生態系の構成は,これらの進行中の環境変化によって変化する可能性が高い.
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