Basin-scale variability of microbial methanol uptake in the Atlantic Ocean

Sargeant, SL; Murrell, JC; Nightingale, PD; Dixon, JL. 2018 Basin-scale variability of microbial methanol uptake in the Atlantic Ocean. Biogeosciences. 10.5194/bg-2018-30 (Submitted)

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Official URL: https://www.biogeosciences-discuss.net/bg-2018-30/

Abstract/Summary

Methanol is a climate active gas and the most abundant oxygenated volatile organic compound (OVOC) in the atmosphere and seawater. Marine methylotrophs are aerobic bacteria that utilise methanol from seawater as a source of carbon (assimilation) and/or energy (dissimilation). A few spatially limited studies have previously reported methanol oxidation rates in seawater; however the basin-wide ubiquity of marine microbial methanol utilisation remains unknown. This study uniquely combines seawater 14C labelled methanol tracer studies with 16S rRNA pyrosequencing to investigate variability in microbial methanol dissimilation and known methanol utilising bacteria throughout a meridional transect of the Atlantic Ocean between 47° N to 39° S. Microbial methanol dissimilation varied between 0.05–1.68 nmol l−1 h−1 in the top 200 m of the Atlantic Ocean and showed significant variability between biogeochemical provinces. The highest rates of methanol dissimilation were found in the northern subtropical gyre (average 0.99 ± 0.41 nmol l−1 h−1), which were up to eight times greater than other Atlantic regions. Microbial methanol dissimilation rates displayed a significant inverse correlation with heterotrophic bacterial production (determined using 3H-leucine). Despite significant depth stratification of bacterial communities, methanol dissimilation rates showed much greater variability between oceanic provinces compared to depth. There were no significant differences in rates between samples collected under light and dark environmental conditions. The variability in the numbers of SAR11 (16S rRNA gene sequences) were estimated to explain approximately 50 % of the changes in microbial methanol dissimilation rates. We estimate that SAR11 cells in the Atlantic Ocean account for between 0.3–59 % of the rates of methanol dissimilation in Atlantic waters, compared to < 0.01–2.3 % for temperate coastal waters. These results make a substantial contribution to our current knowledge and understanding of the utilisation of methanol by marine microbial communities, but highlight the lack of understanding of in situ methanol production mechanisms.

Item Type: Publication - Article
Subjects: Data and Information
Ecology and Environment
Marine Sciences
Oceanography
Divisions: Plymouth Marine Laboratory > Science Areas > Cycling in the Sunlit Ocean
Plymouth Marine Laboratory > Science Areas > Marine Biochemistry and Observations
Depositing User: Jo Dixon
Date made live: 21 Mar 2018 12:37
Last Modified: 21 Mar 2018 12:37
URI: http://plymsea.ac.uk/id/eprint/7818

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