Professor Sophie L Nixon, University of Manchester, was awarded funding in the UKCCSRC’s Flexible Funding 2023 call to look at “Microbial Impacts of CCS: Potential Benefits and Problems During Geological CO2 Storage”.
Carbon capture and storage (CCS) is considered crucial to the delivery of global 2050 Net Zero emissions targets, which are now a legal obligation for the UK. In order for CCS to succeed, CO2 must be permanently stored in deep (>800m) geological formations, namely saline aquifers and depleted oil and gas reservoirs, with target storage times in excess of 10,000 years (Alcalde, Flude et al. 2018).
It is well established that conventional oil and gas reservoirs can have significant issues with problematic microbial activity within the subsurface, leading to reservoir souring, biofouling at the injection well and also microbially-influenced corrosion (MIC) (Bodtker, Thorstenson et al. 2008, Johnson, Folwell et al. 2017, Skovhus, Eckert et al. 2017, Vigneron, Alsop et al. 2017). Therefore, in sites where there is already a significant, and costly, microbial presence, it would be remiss of the industry to not take into account the potential impacts of the subsurface microbiology once these depleted oil and gas reservoirs are repurposed for long-term CO2 storage.
However, the metabolic reactions driven by CO2 fixation in subsurface communities are not well understood, and could feasibly result in a net gain or loss of CO2, production of methane, and microbially induced corrosion (Tyne, Barry et al. 2021, Tyne, Barry et al. 2023). This microbial activity could compromise the capacity, integrity and long-term safety of CO2 storage sites. Alternatively, microbially-enhanced CO2 sequestration could enhance the mineralization of CO2 within the subsurface, improve the overall success of CCS operations and uncover novel ways to convert waste CO2 into useful products (Matter, Stute et al. 2016, Trias, Menez et al. 2017, Bachleitner, Ata et al. 2023).
In this study, we aimed to take a first look at the response of a mature oil-field derived microbial community to a CO2 saturated environment (Dutta, Smith et al. 2020). By utilising 16S rRNA gene sequencing, we were able to determine how the microbial community changed over the 12-month incubation period, and identify the proliferation of any potential problematic or beneficial microbial processes that could indicate potential shifts within the microbiome of depleted oil and gas reservoirs when utilised for subsurface CO2 storage.
The results from this study demonstrate that mature oilfield communities can persist under CO2 storage conditions (i.e. saturated CO2 seawater and a CO2 gas headspace), and that heterotrophic microbial processes, including sulfide production, were observed within a 12-month incubation period in the presence of readily utilisable hydrocarbons (i.e. VFAs).
The enrichment of heterotrophic taxa within the CO2 enrichments demonstrates that hydrocarbon degradation, and sulfide production were able to occur under high concentrations of CO2 and a reduced pH, and were supported by a reduction in available concentrations of VFAs (acetate, propionate and butyrate) throughout the 12-month incubation period.
Desulfallas-Sporotomaculum was the most abundant sulfate-reducing genus within the Test 6 (CO2+VFA) enrichments after 12-months of incubation, and is a known anaerobic, spore-forming, sulfate-reducing genus which can be moderately thermophilic and is known to utilise short and long chain fatty acids (Watanabe, Kojima et al. 2018). It can therefore be surmised that Desulfallas-Sporotomaculum species were able to utilise the available fatty acids within the enrichment medium as electron donors and facilitate dissimilatory sulfate-reducing processes. This is further supported by the low relative abundance of Desulfallas-Sporotomaculum within the Test 1 (CO2) enrichments, where there was no additional readily metabolisable hydrocarbon added to the saline media prior to incubation.
By the end of the study, the Test 1 (CO2) and Test 6 (CO2+VFA) enrichments were dominated by hydrocarbon degrading genera, such as Parvibaculum, Marinobacter, Marinobacterium and Breoghania. All of these genera have previously been isolated from hydrocarbon associated marine environments, and are known to have the capacity to degrade hydrocarbon compounds (Gallego, Vila et al. 2010, Lai, Wang et al. 2011, Rosario-Passapera, Keddis et al. 2012, Bae, Jung et al. 2018, Scheffer, Hubert et al. 2021).


Genus-level microbial community composition of the CO2 saturated enrichments monthly (T0-T6) and then after 12-months of incubation (T7) using 16S rRNA gene sequencing.
Therefore, the results from this study demonstrate that microbial activity can persist under saturated CO2 conditions, and that evidence of potentially problematic microbial activity (e.g. hydrogen sulfide production) can occur in hydrocarbon saturated environments that are utilised for CCS operations.
Ongoing research will encompass the use of groundwater and formation fluid samples from industrially relevant CO2 storage sites of interest to profile the baseline microbial community and associated functional potential, and also identify the subsequent response to saturated CO2 environments.
Read more on Sophie’s Flexible Funding 2023 project page.
Principal Investigator: Prof. Sophie Nixon (Chair of Environmental Microbiology and Biotechnology)
Researcher Co-Investigator: Leanne Walker (Research Associate in Subsurface Microbiology (CCS))
Research Institution: The University of Manchester
Industrial Sponsor: ExxonMobil
References
Alcalde, J., S. Flude, M. Wilkinson, G. Johnson, K. Edlmann, C. E. Bond, V. Scott, S. M. V. Gilfillan, X. Ogaya and R. S. Haszeldine (2018). “Estimating geological CO2 storage security to deliver on climate mitigation.” Nature Communications 9(1): 2201.
Bachleitner, S., Ö. Ata and D. Mattanovich (2023). “The potential of CO(2)-based production cycles in biotechnology to fight the climate crisis.” Nat Commun 14(1): 6978.
Bae, S. S., J. Jung, D. Chung and K. Baek (2018). “Marinobacterium aestuarii sp. nov., a benzene-degrading marine bacterium isolated from estuary sediment.” Int J Syst Evol Microbiol 68(2): 651-656.
Bodtker, G., T. Thorstenson, B. L. Lillebo, B. E. Thorbjornsen, R. H. Ulvoen, E. Sunde and T. Torsvik (2008). “The effect of long-term nitrate treatment on SRB activity, corrosion rate and bacterial community composition in offshore water injection systems.” J Ind Microbiol Biotechnol 35(12): 1625-1636.
Dutta, A., B. Smith, T. Goldman, L. Walker, M. Streets, B. Eden, R. Dirmeier and J. S. Bowman (2020). “Understanding Microbial Community Dynamics in Up-Flow Bioreactors to Improve Mitigation Strategies for Oil Souring.” Front Microbiol 11: 585943.
Gallego, S., J. Vila, J. María Nieto, M. Urdiain, R. Rosselló-Móra and M. Grifoll (2010). “Breoghania corrubedonensis gen. nov. sp. nov., a novel alphaproteobacterium isolated from a Galician beach (NW Spain) after the Prestige fuel oil spill, and emended description of the family Cohaesibacteraceae and the species Cohaesibacter gelatinilyticus.” Syst Appl Microbiol 33(6): 316-321.
Government, U. (2019, 26th June 2019). “The Climate Change Act 2008 (2050 Target Amendment) Order 2019 ” Retrieved 4th January 2024, 2024, from https://www.legislation.gov.uk/uksi/2019/1056/pdfs/uksi_20191056_en.pdf.
Johnson, R. J., B. D. Folwell, A. Wirekoh, M. Frenzel and T. L. Skovhus (2017). “Reservoir Souring – Latest developments for application and mitigation.” J Biotechnol 256: 57-67.
Lai, Q., L. Wang, Y. Liu, J. Yuan, F. Sun and Z. Shao (2011). “Parvibaculum indicum sp. nov., isolated from deep-sea water.” Int J Syst Evol Microbiol 61(Pt 2): 271-274.
Matter, J. M., M. Stute, S. Snæbjörnsdottir, E. H. Oelkers, S. R. Gislason, E. S. Aradottir, B. Sigfusson, I. Gunnarsson, H. Sigurdardottir, E. Gunnlaugsson, G. Axelsson, H. A. Alfredsson, D. Wolff-Boenisch, K. Mesfin, D. Fernandez de la Reguera Taya, J. Hall, K. Dideriksen and W. S. Broecker (2016). “Rapid carbon mineralization for permanent disposal of anthropogenic carbon dioxide emissions.” Science 352(6291): 1312-1314.
Rosario-Passapera, R., R. Keddis, R. Wong, R. A. Lutz, V. Starovoytov and C. Vetriani (2012). “Parvibaculum hydrocarboniclasticum sp. nov., a mesophilic, alkane-oxidizing alphaproteobacterium isolated from a deep-sea hydrothermal vent on the East Pacific Rise.” Int J Syst Evol Microbiol 62(Pt 12): 2921-2926.
Scheffer, G., C. R. J. Hubert, D. R. Enning, S. Lahme, J. Mand and J. R. de Rezende (2021). “Metagenomic Investigation of a Low Diversity, High Salinity Offshore Oil Reservoir.” Microorganisms 9(11).
Skovhus, T. L., R. B. Eckert and E. Rodrigues (2017). “Management and control of microbiologically influenced corrosion (MIC) in the oil and gas industry-Overview and a North Sea case study.” J Biotechnol 256: 31-45.
Trias, R., B. Menez, P. le Campion, Y. Zivanovic, L. Lecourt, A. Lecoeuvre, P. Schmitt-Kopplin, J. Uhl, S. R. Gislason, H. A. Alfreethsson, K. G. Mesfin, S. O. Snaebjornsdottir, E. S. Aradottir, I. Gunnarsson, J. M. Matter, M. Stute, E. H. Oelkers and E. Gerard (2017). “High reactivity of deep biota under anthropogenic CO(2) injection into basalt.” Nat Commun 8(1): 1063.
Tyne, R. L., P. H. Barry, M. Lawson, D. J. Byrne, O. Warr, H. Xie, D. J. Hillegonds, M. Formolo, Z. M. Summers, B. Skinner, J. M. Eiler and C. J. Ballentine (2021). “Rapid microbial methanogenesis during CO(2) storage in hydrocarbon reservoirs.” Nature 600(7890): 670-674.
Tyne, R. L., P. H. Barry, M. Lawson, K. G. Lloyd, D. Giovannelli, Z. M. Summers and C. J. Ballentine (2023). “Identifying and Understanding Microbial Methanogenesis in CO(2) Storage.” Environ Sci Technol 57(26): 9459-9473.
Vigneron, A., E. B. Alsop, B. P. Lomans, N. C. Kyrpides, I. M. Head and N. Tsesmetzis (2017). “Succession in the petroleum reservoir microbiome through an oil field production lifecycle.” ISME J 11(9): 2141-2154.
Watanabe, M., H. Kojima and M. Fukui (2018). “Review of Desulfotomaculum species and proposal of the genera Desulfallas gen. nov., Desulfofundulus gen. nov., Desulfofarcimen gen. nov. and Desulfohalotomaculum gen. nov.” Int J Syst Evol Microbiol 68(9): 2891-2899.

