Japan Geoscience Union Meeting 2021

Presentation information

[E] Oral

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS02] Astrobiology

Thu. Jun 3, 2021 3:30 PM - 5:00 PM Ch.26 (Zoom Room 26)

convener:Hikaru Yabuta(Hiroshima University, Department of Earth and Planetary Systems Science), Seiji Sugita(Department of Earth and Planetary Science, Graduate School of Science Sciece, The University of Tokyo), Misato Fukagawa(National Astronomical Observatory of Japan), Fujishima Kosuke(Tokyo Institute of Technology, Earth-Life Science Institute), Chairperson:Fujishima Kosuke(Tokyo Institute of Technology, Earth-Life Science Institute), Misato Fukagawa(National Astronomical Observatory of Japan), Seiji Sugita(Department of Earth and Planetary Science, Graduate School of Science Sciece, The University of Tokyo), Hikaru Yabuta(Hiroshima University, Department of Earth and Planetary Systems Science)

3:45 PM - 4:00 PM

[MIS02-06] Abiotic synthesis of metal-sulfur clusters containing iron and molybdenum and evaluation of their catalytic functions

*Shunjiro Sodei1, Sebastian Adrian Sanden1, Daisuke Ishikawa1, Shawn E McGlynn2, Masahiko Hara1 (1.Tokyo Institute of Technology, 2.Earth-Life Science Institute, Tokyo Institute of Technology)

Keywords:Chemical evolution, Iron-sulfur cluster, Metalloprotein

The chemical evolution is a widely accepted theory describing the origin of life on Earth. However, the specific reaction pathways and catalysts of the chemical evolution are still controversial. Extant life uses metalloproteins with clusters consisting of metal and sulfur atoms as their active centers, as catalysts for a variety of biochemical reactions in metabolic systems [1]. Metal-sulfur clusters ligated by small compounds are predicted to have played a catalytic role in chemical evolution [2]. There are however only few reports of chemical reactions catalyzed by metal-sulfur clusters in the context of chemical evolution (e.g., [3]) and among the reactions reported, iron-sulfur clusters are predominantly used. It is unclear how metal-sulfur clusters containing metals other than iron could contribute to chemical evolution as catalysts. Herein, this study aims to experimentally evaluate the role of metal-sulfur clusters in chemical evolution processes on the early Earth. This study is focused on the iron-sulfur clusters and iron-molybdenum-sulfur clusters, which are the active centers of ferredoxin [4] and nitrogenase [5], respectively. We examined whether metal-sulfur clusters containing iron and molybdenum could be synthesized abiotically and whether they also exhibit a catalytic function.

Ferric chloride, ferrous chloride, ammonium tetrathiomolybdate, and sodium sulfide were used as metal and sulfur sources, and glutathione and 2-mercaptoethanol were used as ligands. Reacting these compounds yielded UV-visible absorption spectra akin to 4Fe4S clusters. These preliminary results suggests that metal-sulfur clusters containing iron and molybdenum might have been synthesized abiotically. The addition of anthraquinone-2-sulfonate, used here as a redox indicator, suggests that some of the mixed metal-sulfur clusters could be involved in redox reactions. It is currently investigated whether these cluster species could facilitate the reduction of organic compounds.

Reference
[1] J. Winkler & H. Gray, Chem. Rev. 114, 3369-3380 (2014)
[2] L. Belmonte & S. Mansy, Elements 12, 413-418 (2016)
[3] C.Bonfio, et al., Nat. Catal. 1, 616-623 (2018)
[4] P. Venkateswara Rao & R. Holm, Chem. Rev. 104, 527-559 (2004)
[5] C. Van Stappen, et al., Chem. Rev. 120, 5005-5081 (2020)