Periodic Reporting for period 1 - DeepSeep (Deep Serpentinization, H2, and high-pressure abiotic CH4)
Periodo di rendicontazione: 2021-06-01 al 2022-11-30
More than 90% of the total Earth's carbon is stored at depth. However, our understanding on how this carbon is recycled and affects life on out planet remains largely unconstrained. Among the most important carbon-bearing molecules, methane (CH4) is important because it has a much higher global warming potential with respect to carbon dioxide (CO2). However, the cycling of deep methane inside the Earth has received, surprisingly, little attention. DeepSeep focus on the production and cycling of deep methane produced through the process called "serpentinization", whereby the most abundant rocks on Earth – mantle rocks – react with water to produce a new mineral called serpentine. This process is special because it produces another fundamental fluid phase called molecular hydrogen, or dihydrogen (H2), which is nowadays central in green energy strategies. When serpentinization produces dihydrogen, carbon is converted to methane. The resulting geological fluids, rich in dihydrogen and methane, are among the least explored fluids of deep Earth processes, even though they may have disproportionate effects of global carbon cycling and may have played a key role in the emergence of life on our planet and potentially elsewhere.
DeepSeep aims at identifying the processes, chemical features, and fluxes of dihydrogen and methane produced through the process of serpentinization in the deep Earth today and in deep time, and how these fluids may have contributed to deep subsurface biosphere processes on Earth and potentially beyond.
DeepSeep aims at identifying the processes, chemical features, and fluxes of dihydrogen and methane produced through the process of serpentinization in the deep Earth today and in deep time, and how these fluids may have contributed to deep subsurface biosphere processes on Earth and potentially beyond.
The first 18 month of DeepSeep research have fully respected the proposed planning and milestones.
WP1: Three key field campaigns were done in Corsica and Vermont. Minor field activities were also done. Owing to COVID restrictions, some major field campaigns are postponed to 2023. The field work done so far has provided geological constraints and samples for laboratory analyses. More than 500 kilograms fo rocks have been collected so far for laboratory analyses. Additional samples have been obtained from international collaborators. The collected field data have allowed identifying a number of CH4 production and migration sites.
WP2: Sample characterization and the setup of the DeepSeep laboratory have been the main and most time-consuming activities during the first reporting period. The team has characterized more than 150 samples at the microscale (purchased optical and electron microscopes). Fluid inclusion characterization has already provided a large dataset on more than 80 samples from different localities. The presence of CH4 and H2 is confirmed in most of them. The setup of instrumentation and analytical protocols for fluid extraction and analysis were successfully concluded in November 2022. We plan substantial data collection for 2023.
WP3: Great step forward have been done on the compilation of the proposed numerical code for simultaneous thermodynamic and carbon isotope calculations (ThermotopesC_DEW). We also established a new collaboration aimed at establishing isotope fractionation factors for the main carbon-bearing fluid species at high-pressure conditions. These data will be integrate in the software to improve the internal consistency of the code.
Dissemination: the dissemination of DeepSeep results has started and already includes 5 papers published in international journals, including two papers in Nature Communications. Two manuscripts are currently under review. Five other manuscripts are in preparation. Two abstracts have been presented at international conferences during the first reporting period.
WP1: Three key field campaigns were done in Corsica and Vermont. Minor field activities were also done. Owing to COVID restrictions, some major field campaigns are postponed to 2023. The field work done so far has provided geological constraints and samples for laboratory analyses. More than 500 kilograms fo rocks have been collected so far for laboratory analyses. Additional samples have been obtained from international collaborators. The collected field data have allowed identifying a number of CH4 production and migration sites.
WP2: Sample characterization and the setup of the DeepSeep laboratory have been the main and most time-consuming activities during the first reporting period. The team has characterized more than 150 samples at the microscale (purchased optical and electron microscopes). Fluid inclusion characterization has already provided a large dataset on more than 80 samples from different localities. The presence of CH4 and H2 is confirmed in most of them. The setup of instrumentation and analytical protocols for fluid extraction and analysis were successfully concluded in November 2022. We plan substantial data collection for 2023.
WP3: Great step forward have been done on the compilation of the proposed numerical code for simultaneous thermodynamic and carbon isotope calculations (ThermotopesC_DEW). We also established a new collaboration aimed at establishing isotope fractionation factors for the main carbon-bearing fluid species at high-pressure conditions. These data will be integrate in the software to improve the internal consistency of the code.
Dissemination: the dissemination of DeepSeep results has started and already includes 5 papers published in international journals, including two papers in Nature Communications. Two manuscripts are currently under review. Five other manuscripts are in preparation. Two abstracts have been presented at international conferences during the first reporting period.
The results obtained during the first reporting period have provided substantial achievements. Three successful field campaign have allowed identifying ideal case studies demonstrating the global (time and space) significance of the target processes. The sample characterization performed so far could confirm fundamental high-risk/high-gain research hypotheses, such as the widespread occurrence of deep serpentinization, and the systematic presence of dihydrogen and methane in these rocks. The second reporting period will mark a fundamental step towards another fundamental objective, which is the chemical characterization of deep methane. The setup of the analytical protocols for this key objective of the project have already started during the first reporting period.