Japan Geoscience Union Meeting 2019

Presentation information

[J] Oral

B (Biogeosciences ) » B-BC Biogeochemistry

[B-BC03] Interrelation between Life, Water, Mineral, and Atmosphere

Tue. May 28, 2019 3:30 PM - 5:00 PM 201A (2F)

convener:Takeshi Kakegawa(Graduate School of Science, Tohoku University), Tadashi Yokoyama(Graduate School of Integrated Arts and Sciences, Hiroshima University), Keisuke Fukushi(Institute of Nature & Environmental Technology, Kanazawa University), Fumito Shiraishi(Department of Earth and Planetary Systems Science, Graduate School of Science, Hiroshima University), Chairperson:Takeshi Kakegawa, Fumito Shiraishi(Hiroshima Univ.)

3:30 PM - 3:45 PM

[BBC03-07] Secular variation of multiple sulfur isotopic compositions of sulfate and sulfide during long term incubation of Desulfovibrio desulfuricans

*Fumihiro Matsuura1, Hiroko Makita2, Ken Takai3, Yuichiro Ueno1,3 (1.Tokyo Institute of Technology, 2.Tokyo University of Marine Science and Technology, 3.Japan Agency for Marine-Earth Science & Technology (JAMSTEC))

Keywords:sulfate reducing bacteria, sulfur isotope fractionation, long term incubation

Incubation experiments of sulfate reducing microbes have been carried out since 1950s to quantify sulfur isotope fractionation. Sulfur isotope fractionation models are constructed from the results of these experiments. These models are applicable only when steady state is accomplished in the cells; thus, most of incubation experiments targeted cells exponential growth phase. We aimed to quantify the isotope fractionation in stationary to death phase of the cells and carried out two series of incubation experiment of sulfate reducing bacteria, Desulfovibrio desulfuricans (DSM-642), until c.a. 2000 hours. In addition, we used glucose as electron donor to make cell specific sulfate reduction rate low. Cells grew linearly rather than exponentially until cell concentration became c.a. 2×107 cells/mL in the early stage of incubation. Calculated sulfur isotope fractionation increased from 13.5±3.7‰ at the earliest stage of linear growth phase to 70.5±21.0‰ at the middle of linear growth phase. The cell specific sulfate reduction rate was 1.0±0.3 fmol/cell/day when sulfur isotope fractionation became 70.5±21.0‰, consistent with the results of a previous study. In the stationary to death phase, sulfide concentration started decreasing on the contrary to our expectation. Besides, δ34Ssulfide value increased concomitant with the decrease of Δ33S’sulfide value. The δ34S’sulfide and Δ33S’sulfide have good linear correlation, and that indicate a sulfide originated reaction in a closed system with a unique fractionation factor dominates sulfur cycle during stationary to death phase. The calculated enrichment factors of the reaction in the two series experiments are 10.5‰ and 30‰. These enrichment factors are large compared to those of biotic or abiotic sulfide oxidation experiments of previous studies. We checked the reaction occur without cells and infer that the reaction is caused from sulfide oxidation by oxidants containing in the medium or sulfurization of organic matter containing in the medium.