Methanol distribution and metabolic rate in the northwest Pacific Ocean in May/June 2021

doi:doi:10.1594/PANGAEA.952087

Methanol distribution and metabolic rate in the northwest Pacific Ocean in May/June 2021

We investigated the seawater methanol abundance, the dynamic of microbial methanol (MeOH) metabolism and the geochemical parameters in the northwest Pacific Ocean (NWPO) area. Seawater samples were collected during May-June 2021 aboard the R/V “Dongfanghong 3” in the northwest Pacific Ocean. Seawater was sampled using a Seabird 911 CTD-Niskin rosette system equipped with conductivity, temperature and depth sensors. Methanol samples were collected directly without filters and then stored at -80℃ for laboratory analysis. Methanol concentrations were determined by a modified commercial purge and trap system combined with Agilent GC-8890 gas chromatograph with a flame ionization detector. Microbial methanol assimilation and oxidation rates were determined by quantifying 14C-MeOH incorporation into biomass and oxidation to CO2 (Zhuang et al., 2018). Nutrients were measured using Seal Analytical Quaatro nutrient autoanalyzer except for ammonium which was analyzed by a fluorometric method on board (Ning et al., 2013). Chlorophyll-a was measured by fluorometric method (Parsons et al., 1984).

BibTex:

@dataset{Zhou_Zhen_and_Zhuang_Guang-Chao_and_Mao_Shi-Hai_and_Liu_Jiarui_and_Li_Xiao-Jun_and_Liu_Qiao_and_Song_Guo-Dong_and_Zhang_Hong-Hai_and_Chen_Zhaohui_and_Montgomery_Andrew_and_Joye_Samantha_B_and_Yang_Gui-Peng_2023,
    abstract = {We investigated the seawater methanol abundance, the dynamic of microbial methanol (MeOH) metabolism and the geochemical parameters in the northwest Pacific Ocean (NWPO) area. Seawater samples were collected during May-June 2021 aboard the R/V “Dongfanghong 3” in the northwest Pacific Ocean. Seawater was sampled using a Seabird 911 CTD-Niskin rosette system equipped with conductivity, temperature and depth sensors. Methanol samples were collected directly without filters and then stored at -80℃ for laboratory analysis. Methanol concentrations were determined by a modified commercial purge and trap system combined with Agilent GC-8890 gas chromatograph with a flame ionization detector. Microbial methanol assimilation and oxidation rates were determined by quantifying 14C-MeOH incorporation into biomass and oxidation to CO2 (Zhuang et al., 2018). Nutrients were measured using Seal Analytical Quaatro nutrient autoanalyzer except for ammonium which was analyzed by a fluorometric method on board (Ning et al., 2013). Chlorophyll-a was measured by fluorometric method (Parsons et al., 1984).},
    author = {Zhou, Zhen and Zhuang, Guang-Chao and Mao, Shi-Hai and Liu, Jiarui and Li, Xiao-Jun and Liu, Qiao and Song, Guo-Dong and Zhang, Hong-Hai and Chen, Zhaohui and Montgomery, Andrew and Joye, Samantha B and Yang, Gui-Peng},
    doi = {10.1594/PANGAEA.952087},
    institution = {PANGAEA (Lithosphere)},
    keyword = {'Northwest Pacific Ocean', 'air', 'methanol', 'microbial metabolism', 'sea exchange', 'source and sink'},
    title = {Methanol distribution and metabolic rate in the northwest Pacific Ocean in May/June 2021},
    url = {https://service.tib.eu/ldmservice/vdataset/png-doi-10-1594-pangaea-952087},
    year = {2023}
}