日本地球惑星科学連合2016年大会

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

[A-CG15] 沿岸海洋生態系──2.サンゴ礁・海草藻場・マングローブ

2016年5月24日(火) 15:30 〜 17:00 203 (2F)

コンビーナ:*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(東京工業大学 大学院情報理工学研究科 情報環境学専攻)、梅澤 有(長崎大学)、座長:渡邉 敦(東京工業大学 大学院情報理工学研究科 情報環境学専攻)、梅澤 有(長崎大学)

16:15 〜 16:30

[ACG15-10] ツバル フォンガファレ島のサンゴ年輪に見られる混入物について

*中村 修子1荻原 成騎2細井 豪3茅根 創2山野 博哉4 (1.慶應大学 理工学部、2.東京大学大学院理学系研究科地球惑星科学専攻、3.(株)電通、4.国立環境研究所)

Because of their low altitudes, atoll islands in Tuvalu, the South Pacific is concerned for the earliest influence of the sea level rise and resultant submergence caused by global warming. However the local environmental change such as land development and water pollution with recent increasing population also damages the ecosystem and the sustainability of coral reef islands. To examine the time series of anthropogenic impacts on the coastal reefs, we analyzed the coral annual bands obtained in 2009 from the lagoon of Fongafale Island, the capital of Tuvalu.
The coral core fg01 from living colonies of Porites lutea (core length; 78 cm) shows growth interruption at 20cm under the top and the characteristic black bands were observed along annual bands above that break. We introduced the age axis to fg01 using the Δ14C– annual bands correction constructed with the other continuous coral annual bands (fh11, core length; 93 cm, 1940–2009) from Funafala Island on the same atoll. The core fg01 started the growth from 1940-50s and the discontinuous period was for 1970s–1990s, after that the coral has restarted its growth but the black bands pollution is conspicuous.
To identify this pollution we performed organic/ inorganic analysis and studied a microscopic inspection. We found high dense fibers of boring microbes; some kinds of algae and fungi in the black bands of coral skeleton. The propagation of microbes into the feeble coral skeleton and the construction of the black bands started from 1990s, which was coincident with increase of living drainage caused by densely population at Fongafale Island (Yamano et al.,2007, Fujita et al.,2013, 2014). Further the construction of the black annual bands suggests the seasonal propagation of microbes related to coastal environment.
On the other hand, in the process of the organic analysis using GC/MS we detected the higher concentration of petroleum hydrocarbons from the bottom of the coral core corresponded to 1940-50s annual bands than the upper part. The low CPI value (Carbon Preference Index; a rate of diagenesis) suggests this hydrocarbon was used as fuel for heavy equipments introduced during the World War II. Fongafale Island has the history that the US Army built a heavy bomber-runway for one month in 1943.
70yr coral annual bands from Fongafale Island recorded both the trace of the World War II and recent human impact in that skeleton.