
NSF Org: |
EAR Division Of Earth Sciences |
Recipient: |
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Initial Amendment Date: | March 8, 2019 |
Latest Amendment Date: | March 6, 2023 |
Award Number: | 1847684 |
Award Instrument: | Continuing Grant |
Program Manager: |
Margaret Fraiser
mfraiser@nsf.gov (703)292-0000 EAR Division Of Earth Sciences GEO Directorate for Geosciences |
Start Date: | March 15, 2019 |
End Date: | February 28, 2025 (Estimated) |
Total Intended Award Amount: | $557,226.00 |
Total Awarded Amount to Date: | $557,226.00 |
Funds Obligated to Date: |
FY 2022 = $119,147.00 FY 2023 = $104,023.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
601 S HOWES ST FORT COLLINS CO US 80521-2807 (970)491-6355 |
Sponsor Congressional District: |
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Primary Place of Performance: |
200 W. Lake Street Fort Collins CO US 80521-4593 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | Geobiology & Low-Temp Geochem |
Primary Program Source: |
01001920DB NSF RESEARCH & RELATED ACTIVIT 01002324DB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
Microbial communities in terrestrial environments catalyze myriad biogeochemical cycles with global implications. However, in many ecosystems the combination of biological and chemical complexity can preclude a true mechanistic understanding of how microorganisms interact, are affected by viruses, and exchange metabolites. These kinds of insights are critical for our ability to manipulate microbiomes for beneficial outcomes, and better predict how biogeochemical cycles might change under varying environmental conditions. Deep fractured shales host more constrained microbial consortia that are more amenable to interrogation, and offer opportunities for new scientific insights and development of tools that can be applied to increasingly complex systems. Indeed, the investigator has previously revealed that the cycling of methylamines--simple carbon and nitrogen compounds--is a conserved metabolic strategy that fuels methylotrophic methanogenesis in deep shale formations across the Appalachian Basin. Work outlined in this proposal will determine the extent of functional conservation across geographically distinct shales, and use an extensive library of deep biosphere microbial isolates to investigate microbial metabolic interdependencies that enable persistence of life in these extreme environments. The role of viruses in driving microbial community dynamics and metabolite cycling will also be investigated. Finally, novel tools and insights developed in the shale ecosystem will be applied to a more complex wetland system to further illuminate the extent of methylamine metabolism in terrestrial environments. This project will train a graduate student and offer opportunities to undergraduate researchers. The involvement of industrial partners will enable internship placements for graduate students, and contribute to curriculum materials aimed at informing students of diverse career opportunities in subsurface science. Given the level of public interest in hydraulic fracturing and deep biosphere topics, a series of outreach events at local organizations are also planned.
Genome-resolved metagenomic and metabolomic analyses, coupled with laboratory experimentation, has revealed that methylamine cycling in deep terrestrial shales is a conserved functional process across the Appalachian Basin that enables microbial communities to persist for many hundreds of days. Using multiomic approaches, this work will expand investigations into western US shale plays, and determine how functional traits are altered under varying salinity and temperature conditions. Genomic insights into metabolite exchange and methane isotope fractionation in these systems will be tested in the laboratory using environmental isolates and high-pressure incubation apparatus that enables in situ conditions (e.g., pressure, temperature, salinity) to be recreated. Novel analytical tools including high-pressure real-time NMR will be used to track the cycling of substrates at high temporal resolution. The ability of novel and abundant viral populations to mediate carbon and nitrogen cycling in the deep biosphere will also be investigated using a combination of bioinformatic tools and laboratory experimentation. Data resulting from these studies will offer unique insights into the functioning of microbial and viral populations, and the impact of microbial metabolism on poorly-resolved carbon and nitrogen cycles in the deep terrestrial subsurface.
This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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PROJECT OUTCOMES REPORT
Disclaimer
This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.
The deep terrestrial subsurface is the largest reservoir of microbial life on Earth and yet challenges in accessing this environment limits our understanding of how microorganisms live under extremes of temperature, pressure, and salinity. In this project, we used hydraulically fractured wells as portals into the deep biosphere, allowing us to collect microbial samples and better understand the diversity of these microbial populations and determine how they survive.
Our team collected water samples from these wells across North America, England, and China, and profiled the microbial communities using a DNA sequencing approach termed metagenomics. This approach involves the sequencing of all the microbial DNA within a given sample, and then reconstructing microbial genomes from the resulting sequencing data using computational pipelines. This incredibly powerful tool allows us to identify different microbial species and their metabolisms without ever having to grow those microbes in the lab, something which is extremely difficult for many of the bugs that live in the deep subsurface.
Our analyses revealed that different subsurface regions across the US host different microbiomes, with these differences likely influenced by variability in temperature and salinity deep underground. Using the microbial genomes that we had generated, we were able to determine how these communities survived at depths of up to 3-km underground. In many instances compounds produced by bacteria to tolerate the extremely saline conditions (termed ‘osmolytes’) could also be used as energy sources by other bacteria. Across all the environments we studied here, microorganisms capable of metabolizing different sulfur compounds were frequently dominant, as were members of the Archaea that generate methane from acetate, hydrogen, and methyl compounds. These subsurface microbiomes also contained large numbers of phage – or viruses that infect bacteria and archaea. Our analyses revealed an ongoing ‘arms race’ between bacteria and viruses in the subsurface; many of the bacteria used CRISPR defense systems that act like a bacterial immune system to protect themselves from viral infection. Over time in these deep biosphere ecosystems we were able to observe increasing bacterial use of CRISPR defenses in response to greater numbers of phage.
Finally, to make our extensive datasets more accessible to scientists, industry, and the general public, we developed an online tool that allows people to explore our data across three continents (https://geocentroid.shinyapps.io/MAP-FRAC-Database/). This interactive tool enables people to look at the distribution of specific microbial groups across our sample locations, and even infer the function of different microorganisms.
Over the project period, this award allowed for the training of a graduate student at Colorado State University who was the lead author on a series of high impact, peer-reviewed manuscripts. The project allowed the student to interact extensively with industry contacts and develop their professional network. Highlighting the translational importance of this work, the same researcher is now leveraging many of the approaches that were developed on this NSF project to understand how subsurface microbiomes might interact with geologic hydrogen production and storage.
Last Modified: 03/12/2025
Modified by: Michael James Wilkins
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