Sojo, V;
Ohno, A;
McGlynn, SE;
Yamada, YMA;
Nakamura, R;
(2019)
Microfluidic Reactors for Carbon Fixation under Ambient-Pressure Alkaline-Hydrothermal-Vent Conditions.
Life
, 9
(1)
10.3390/life9010016.
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Abstract
The alkaline-hydrothermal-vent theory for the origin of life predicts the spontaneous reduction of CO₂, dissolved in acidic ocean waters, with H₂ from the alkaline vent effluent. This reaction would be catalyzed by Fe(Ni)S clusters precipitated at the interface, which effectively separate the two fluids into an electrochemical cell. Using microfluidic reactors, we set out to test this concept. We produced thin, long Fe(Ni)S precipitates of less than 10 µm thickness. Mixing simplified analogs of the acidic-ocean and alkaline-vent fluids, we then tested for the reduction of CO₂. We were unable to detect reduced carbon products under a number of conditions. As all of our reactions were performed at atmospheric pressure, the lack of reduced carbon products may simply be attributable to the low concentration of hydrogen in our system, suggesting that high-pressure reactors may be a necessity.
Type: | Article |
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Title: | Microfluidic Reactors for Carbon Fixation under Ambient-Pressure Alkaline-Hydrothermal-Vent Conditions |
Open access status: | An open access version is available from UCL Discovery |
DOI: | 10.3390/life9010016 |
Publisher version: | https://doi.org/10.3390/life9010016 |
Language: | English |
Additional information: | © 2019 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/ licenses/by/4.0/). |
Keywords: | abiogenesis, carbon fixation, electrochemistry, hydrothermal vents, origin of life, reduction |
URI: | https://discovery.ucl.ac.uk/id/eprint/10067885 |
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