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Zhuang, Guang-Chao; Heuer, Verena B; Lazar, Cassandre Sara; Goldhammer, Tobias; Wendt, Jenny; Samarkin, Vladimir A; Elvert, Marcus; Teske, Andreas P; Joye, Samantha B; Hinrichs, Kai-Uwe (2017): Late Lutetian Thermal Maximum - crossing a thermal threshold in Earth's climate system? PANGAEA, https://doi.org/10.1594/PANGAEA.883599, Supplement to: Zhuang, G-C et al. (2018): Relative importance of methylotrophic methanogenesis in sediments of the Western Mediterranean Sea. Geochimica et Cosmochimica Acta, 224, 171-186, https://doi.org/10.1016/j.gca.2017.12.024

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Abstract:
Microbial production of methane is an important terminal metabolic process during organic matter degradation in marine sediments. It is generally acknowledged that hydrogenotrophic and acetoclastic methanogenesis constitute the dominant pathways of methane production; the importance of methanogenesis from methylated compounds remains poorly understood. We conducted various biogeochemical and molecular genetic analyses to characterize substrate availability, rates of methanogenesis, and methanogen community composition, and further evaluated the contribution of different substrates and pathways for methane production in deltaic surface and subsurface sediments of the Western Mediterranean Sea. Major substrates representing three methanogenic pathways, including H2, acetate, and methanol, trimethylamine (TMA), and dimethylsulfide (DMS), were detected in the pore waters and sediments, and exhibited variability over depth and between sites. In accompanying incubation experiments, methanogenesis rates from various 14C labeled substrates varied as well, suggesting that environmental factors, such as sulfate concentration and organic matter quality, could significantly influence the relative importance of individual pathway. In particular, methylotrophic and hydrogenotrophic methanogenesis contributed to the presence of micromolar methane concentrations in the sulfate reduction zone, with methanogenesis from methanol accounting for up to 98% of the total methane production in the topmost surface sediment. In the sulfate-depleted zone, hydrogenotrophic methanogenesis was the dominant methanogenic pathway (67-98%), and enhanced methane production from acetate was observed in organic-rich sediment (up to 31%). Methyl coenzyme M reductase gene (mcrA) analysis revealed that the composition of methanogenic communities was generally consistent with the distribution of methanogenic activity from different substrates. This study provides the first quantitative assessment of methylotrophic methanogenesis in marine sediments and has important implications for marine methane cycling. The occurrence of methylotrophic methanogenesis in surface sediments could fuel the anaerobic oxidation of methane (AOM) in the shallow sulfate reduction zone. Release of methane produced from methylotrophic methanogenesis could be a source of methane efflux to the water column, thus influencing the benthic methane budgets.
Coverage:
Median Latitude: 41.067715 * Median Longitude: 2.799847 * South-bound Latitude: 35.133170 * West-bound Longitude: -2.533000 * North-bound Latitude: 43.316170 * East-bound Longitude: 4.869330
Date/Time Start: 2013-04-07T09:37:00 * Date/Time End: 2013-04-11T17:38:00
Size:
11 datasets

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Datasets listed in this publication series

  1. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): Geochemistry (CH4, δ¹³C CH4, H2, TMA, DMSPt) of sediment core GeoB17306-2. https://doi.org/10.1594/PANGAEA.883593
  2. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): Geochemistry (CH4, δ¹³C CH4, H2, TMA, DMSPt) of sediment core GeoB17308-4. https://doi.org/10.1594/PANGAEA.883594
  3. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): Geochemistry (CH4, δ¹³C CH4, H2, TMA, DMSPt, TOC) of sediment core GeoB17314-1. https://doi.org/10.1594/PANGAEA.883595
  4. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): Geochemistry of sediment core GeoB17306-2. https://doi.org/10.1594/PANGAEA.883590
  5. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): Geochemistry of sediment core GeoB17308-4. https://doi.org/10.1594/PANGAEA.883591
  6. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): Geochemistry of sediment core GeoB17314-1. https://doi.org/10.1594/PANGAEA.883592
  7. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): Methanogenesis rate of sediment core GeoB17306-2. https://doi.org/10.1594/PANGAEA.883596
  8. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): Methanogenesis rate of sediment core GeoB17308-4. https://doi.org/10.1594/PANGAEA.883597
  9. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): Methanogenesis rate of sediment core GeoB17314-1. https://doi.org/10.1594/PANGAEA.883598
  10. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): TOC content of sediment coreGeoB17306-2. https://doi.org/10.1594/PANGAEA.883588
  11. Zhuang, G-C; Heuer, VB; Lazar, CS et al. (2017): TOC content, stable carbon isotope signal, and C/N-ratios of sediment core GeoB17308-4. https://doi.org/10.1594/PANGAEA.883589