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2.1 Dissolved Methane and Nitrous Oxide
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2.1 Dissolved Methane and Nitrous Oxide
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Journal Article
2.1 Dissolved Methane and Nitrous Oxide
2021
Overview
Despite its relatively low concentrations, short-lived CH4 in the atmosphere is approximately 25 times more effective on a per molecule basis than carbon dioxide (CO2) in trapping heat. [...]CH4 has a significant influence on global climate change, the oxidative capacity of the atmosphere, and the chemistry of the stratospheric ozone. Nitrous oxide (N2O) is a potent greenhouse gas in the atmosphere, and has a global warming potential of about 300 times that of carbon dioxide and a long atmospheric lifetime of 118 to 131 years (IPCC, 2013). [...]CH4 distribution is vertically uniform in the continental shelf zone in spring and winter. In the coastal seawaters of the YS, CH4 was observed to accumulate after MPn enrichment with high MPn-to-CH4-conversion efficiency (~60%). [...]several Vibrio isolates isolated from the coastal waters were found to produce CH4 while growing in culture using MPn as the sole phosphorus (P) source, thus indicating that Vibrio spp. are capable of cleaving MPn for P acquisition and might be the major contributors to MPn-dependent CH4 production ( Y e et al., 2020).
