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Hydrothermal vents and the supply of nutrient metals for the origin and early evolution of life

Lead Research Organisation: University of St Andrews
Department Name: Earth and Environmental Sciences

Abstract

The origin, survival, and early evolution of life on the Earth, and if exists, on Enceladus must require transition metals (e.g., Ni, Mo, Cu etc.). Weathering of continental crust followed by riverine transport, which is the main source of metals in the present Earth, was/is limited on the Early earth/present-day Enceladus. Instead, hydrothermal vents (HTVs) and/or weathering of the sub-oceanic rocks are proposed to be the main source of metal on these planetary bodies, however, the metal concentrations in these vents are highly speculative and unconstrained. Furthermore, the existing models that tried to quantify the metal contents in the early ocean on Earth and Enceladus are theoretical and lack the consideration of critical parameters (e.g., organic ligands) that influence metal solubility. The proposed research aims to quantify the metal contents in HTVs and in the ocean on the early earth and Enceladus by performing hydrothermal experiments followed by thermodynamic and mass-balance (Box) modelling. Together these methods would replicate the interaction between early Earth Crust/Enceladus core with corresponding ocean water at various pressures (P) and temperatures (T) and the mixing of HTV fluids with ocean water. Experiments will be performed using novel set-up comprising hydrothermal reactor and syringe pump, which will allow performing multiple experiments in controlled T, P, and redox conditions. The modelling will be done using computer-based software. The proposed research will finally be able to constrain if obtained metal concentrations (in vents and ocean) are sufficient to trigger biologic pathways required for the origin and early evolution of life in these planetary bodies. The results are therefore critical for future space exploration targeting the existence of extra-terrestrial life. With the expertise of the researcher and the host, available facilities at the host institution, the project can be finished within proposed time (24 months).

Publications

10 25 50
 
Description Did hydrothermal vents push the frontiers of habitability on the early Earth?
Amount £1,371,900 (GBP)
Funding ID NE/V010824/1 
Organisation Natural Environment Research Council 
Sector Public
Country United Kingdom
Start 03/2021 
End 03/2025
 
Description Phosphate reduction thermodynamics 
Organisation Rensselaer Polytechnic Institute
Country United States 
Sector Academic/University 
PI Contribution We performed new phosphate reduction experiments in the laboratory and derived reduction yields over a range of temperatures and compositions.
Collaborator Contribution The collaborator performed thermodynamic modelling to demonstrate that our experimental findings are consistent with theoretical predictions. In addition, he provided feedback on the interpretation of the experimental results.
Impact Baidya, A.S., Pasek, M.A. and Stüeken, E.E., 2024. Moderate and high-temperature metamorphic conditions produced diverse phosphorous species for the origin of life. Communications Earth & Environment, 5(1), p.491.
Start Year 2022
 
Description Rare Earth Element systematics 
Organisation Gottfried Wilhelm Leibniz Universität Hannover
Country Germany 
Sector Academic/University 
PI Contribution I performed nitrogen, carbon and sulfur isotope analyses on stromatolite samples to asses the response of these proxies to changing environmental conditions.
Collaborator Contribution The collaborator provided analyses of Rare Earth Elements of carbonates to assess relative contributions of hydrothermal fluids and continental runoff, as well as local redox conditions.
Impact Stu¨eken, E.E., Viehmann, S. and Hohl, S.V., 2023. Exploring the effects of residence time on the utility of stable isotopes and S/C ratios as proxies for ocean connectivity. ACS Earth and Space Chemistry, 7(7), pp.1337-1349. Stüeken, E.E., Viehmann, S. and Hohl, S.V., 2022. Contrasting nutrient availability between marine and brackish waters in the late Mesoproterozoic: Evidence from the Paranoá Group, Brazil. Geobiology, 20(2), pp.159-174.
Start Year 2021