JpGU-AGU Joint Meeting 2020

講演情報

[J] 口頭発表

セッション記号 A (大気水圏科学) » A-CG 大気海洋・環境科学複合領域・一般

[A-CG56] 沿岸海洋生態系─2.サンゴ礁・藻場・マングローブ

コンビーナ:梅澤 有(東京農工大学)、宮島 利宏(東京大学 大気海洋研究所 海洋地球システム研究系 生元素動態分野)、渡邉 敦(笹川平和財団 海洋政策研究所)、樋口 富彦(東京大学大気海洋研究所)

[ACG56-05] ツバルサンゴ年輪黒色バンドに記録された人為汚染による季節強還元(Anoxic)環境形成史

*中村 修子1,2,3茅根 創1高橋 嘉夫1砂村 倫成1細井 豪1,4山野 博哉5 (1.東京大学 大学院理学系研究科 地球惑星科学専攻、2.慶應大学 理工学部、3.笹川平和財団 海洋政策研究所、4.電通、5.国立環境研究所 生物・生態系環境研究センター)

キーワード:ツバル環礁、サンゴ年輪、黒色バンド、強還元(無酸素) 環境、人為汚染、硫化鉄

Atoll islands are small, low-lying and highly vulnerable to sea level rise (SLR). Because these islands are fully composed of the skeletons from coral reef creatures, the healthy coral ecosystem plays a pivotal role in island resilience against SLR. The environmental deterioration of reefs caused by increases in the human population has been recently reported, but the timing and process are unknown. We investigated the annual black bands in a coral boring core from Fongafale Island, the capital of Tuvalu, which is a symbolic atoll country that is being submerged due to SLR. The iron redox state and microbial gene segments in the coral skeleton might be new environmental indicators that reveal the linkage between anthropogenic activity and coral reef ecosystems. Our findings provide the first demonstration that iron sulfide has formed concentrated black layers since 1991 under the seasonal anoxic conditions inside coral annual bands. Since the 1990s, increasing domestic waste-induced eutrophication has promoted seasonal algae proliferation, resulting in sulfate reduction by anaerobic bacteria. With the recent climate variability, these anthropogenic effects have induced the mass mortality of branching corals, deteriorated the coral reef ecosystem and deprived the resilience of the island against SLR.