JpGU-AGU Joint Meeting 2017

Presentation information

[JJ] Oral

A (Atmospheric and Hydrospheric Sciences) » A-CG Complex & General

[A-CG50] [JJ] Coastal Ecosystems -- 2. Coral reefs, seagrass and macroalgal beds, and mangroves

Wed. May 24, 2017 1:45 PM - 3:15 PM 301A (International Conference Hall 3F)

convener:Toshihiro Miyajima(Marine Biogeochemistry Group, Division of Ocean-Earth System Science, Atmosphere and Ocean Research Institute, The University of Tokyo), Yu Umezawa(Nagasaki University), Atsushi Watanabe(School of Environment and Society、Tokyo Institute of Technology), Chairperson:Toshihiro Miyajima(Marine Biogeochemistry Group, Division of Ocean-Earth System Science, Atmosphere and Ocean Research Institute, The University of Tokyo), Chairperson:Atsushi Watanabe(Tokyo Institute of Technology)

2:10 PM - 2:30 PM

[ACG50-02] Carbon sequestration and storage in seagrass meadows

★Invited papers

*Kenta WATANABE1, Koji SEIKE2, Tatsuki TOKORO1, Shigeru MONTANI3, Tomohiro KUWAE1 (1.Port and Airport Research Institute, 2.Atmosphere and Ocean Research Institute, The University of Tokyo, 3.Hokkaido University)

Keywords:seagrass meadows, carbon storage, isotopic analyses, sediment, organic carbon

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.