Net uptake of atmospheric CO sub(2) by coastal submerged aquatic vegetation
'Blue Carbon', which is carbon captured by marine living organisms, has recently been highlighted as a new option for climate change mitigation initiatives. In particular, coastal ecosystems have been recognized as significant carbon stocks because of their high burial rates and long-term...
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Veröffentlicht in: | Global change biology 2014-06, Vol.20 (6), p.1873-1884 |
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creator | Tokoro, Tatsuki Hosokawa, Shinya Miyoshi, Eiichi Tada, Kazufumi Watanabe, Kenta Montani, Shigeru Kayanne, Hajime Kuwae, Tomohiro |
description | 'Blue Carbon', which is carbon captured by marine living organisms, has recently been highlighted as a new option for climate change mitigation initiatives. In particular, coastal ecosystems have been recognized as significant carbon stocks because of their high burial rates and long-term sequestration of carbon. However, the direct contribution of Blue Carbon to the uptake of atmospheric CO sub(2) through air-sea gas exchange remains unclear. We performed in situ measurements of carbon flows, including air-sea CO sub(2) fluxes, dissolved inorganic carbon changes, net ecosystem production, and carbon burial rates in the boreal (Furen), temperate (Kurihama), and subtropical (Fukido) seagrass meadows of Japan from 2010 to 2013. In particular, the air-sea CO sub(2) flux was measured using three methods: the bulk formula method, the floating chamber method, and the eddy covariance method. Our empirical results show that submerged autotrophic vegetation in shallow coastal waters can be functionally a sink for atmospheric CO sub(2.) This finding is contrary to the conventional perception that most near-shore ecosystems are sources of atmospheric CO sub(2). The key factor determining whether or not coastal ecosystems directly decrease the concentration of atmospheric CO sub(2) may be net ecosystem production. This study thus identifies a new ecosystem function of coastal vegetated systems; they are direct sinks of atmospheric CO sub(2). |
doi_str_mv | 10.1111/gcb.12543 |
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In particular, coastal ecosystems have been recognized as significant carbon stocks because of their high burial rates and long-term sequestration of carbon. However, the direct contribution of Blue Carbon to the uptake of atmospheric CO sub(2) through air-sea gas exchange remains unclear. We performed in situ measurements of carbon flows, including air-sea CO sub(2) fluxes, dissolved inorganic carbon changes, net ecosystem production, and carbon burial rates in the boreal (Furen), temperate (Kurihama), and subtropical (Fukido) seagrass meadows of Japan from 2010 to 2013. In particular, the air-sea CO sub(2) flux was measured using three methods: the bulk formula method, the floating chamber method, and the eddy covariance method. Our empirical results show that submerged autotrophic vegetation in shallow coastal waters can be functionally a sink for atmospheric CO sub(2.) This finding is contrary to the conventional perception that most near-shore ecosystems are sources of atmospheric CO sub(2). The key factor determining whether or not coastal ecosystems directly decrease the concentration of atmospheric CO sub(2) may be net ecosystem production. 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In particular, coastal ecosystems have been recognized as significant carbon stocks because of their high burial rates and long-term sequestration of carbon. However, the direct contribution of Blue Carbon to the uptake of atmospheric CO sub(2) through air-sea gas exchange remains unclear. We performed in situ measurements of carbon flows, including air-sea CO sub(2) fluxes, dissolved inorganic carbon changes, net ecosystem production, and carbon burial rates in the boreal (Furen), temperate (Kurihama), and subtropical (Fukido) seagrass meadows of Japan from 2010 to 2013. In particular, the air-sea CO sub(2) flux was measured using three methods: the bulk formula method, the floating chamber method, and the eddy covariance method. Our empirical results show that submerged autotrophic vegetation in shallow coastal waters can be functionally a sink for atmospheric CO sub(2.) This finding is contrary to the conventional perception that most near-shore ecosystems are sources of atmospheric CO sub(2). The key factor determining whether or not coastal ecosystems directly decrease the concentration of atmospheric CO sub(2) may be net ecosystem production. 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source | Wiley Online Library Journals Frontfile Complete |
subjects | Marine |
title | Net uptake of atmospheric CO sub(2) by coastal submerged aquatic vegetation |
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