JpGU-AGU Joint Meeting 2017

講演情報

[JJ] 口頭発表

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-CG50] [JJ] 沿岸海洋生態系──2.サンゴ礁・藻場・マングローブ

2017年5月24日(水) 13:45 〜 15:15 301A (国際会議場 3F)

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)、梅澤 有(長崎大学)、渡邉 敦(東京工業大学 環境・社会理工学院)、座長: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)、座長:渡邉 敦(東京工業大学)

14:10 〜 14:30

[ACG50-02] 海草藻場における炭素隔離・貯留過程の解析

★招待講演

*渡辺 謙太1清家 弘治2所 立樹1門谷 茂3桑江 朝比呂1 (1.港湾空港技術研究所、2.東京大学大気海洋研究所、3.北海道大学)

キーワード:海草藻場、炭素貯留、同位体分析、堆積物、有機炭素

Seagrass meadows are one of the most productive ecosystems and play an important role as carbon reservoirs, storing large amount of organic carbon in the sediments. Estuaries are considered to be a net source of atmospheric CO2 due to the mineralization of terrestrial carbon but recent studies demonstrated that seagrass meadows in estuaries can be sinks for atmospheric CO2. The flow of organic and inorganic carbon derived from multiple sources regulates these processes but the knowledge about these relationships is limited. In this study, we evaluated the flow of carbon derived from multiple sources in seagrass meadows using isotopic approaches and associated the flow with the processes of both atmospheric CO2 uptake and carbon storage in sediments. We estimated the contribution of atmospheric CO2 to assimilated seagrass carbon by a carbon-source mixing model using radiocarbon concentrations (Δ14C). The model indicated that the seagrass assimilated 0–40% of its inorganic carbon as atmospheric CO2. The stable isotopic signatures (δ13C and δ15N) of both particulate organic carbon (OC) and sedimentary OC suggested that the efficiency of OC storage in sediments would be dependent on OC derived from multiple sources. We will also present the historical changes in carbon storage using sediment core analyses.