
NSF Org: |
EAR Division Of Earth Sciences |
Recipient: |
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Initial Amendment Date: | August 1, 2012 |
Latest Amendment Date: | July 14, 2014 |
Award Number: | 1151682 |
Award Instrument: | Standard Grant |
Program Manager: |
Enriqueta Barrera
EAR Division Of Earth Sciences GEO Directorate for Geosciences |
Start Date: | August 15, 2012 |
End Date: | July 31, 2018 (Estimated) |
Total Intended Award Amount: | $400,000.00 |
Total Awarded Amount to Date: | $423,632.00 |
Funds Obligated to Date: |
FY 2014 = $23,632.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
550 S COLLEGE AVE NEWARK DE US 19713-1324 (302)831-2136 |
Sponsor Congressional District: |
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Primary Place of Performance: |
DE US 19716-2553 |
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): |
EARTHSCOPE-OPERATIONS & MAINTE, Geobiology & Low-Temp Geochem, CLB-Career, EPSCoR Co-Funding |
Primary Program Source: |
01001415DB 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
Microbes are numerous, widespread, and metabolically-versatile organisms, impacting virtually every environment on Earth?s surface. Fe-oxidizing microorganisms (FeOM) have likely been oxidizing, or ?rusting,? the Earth for billions of years. In near-neutral pH environments, FeOM form iron oxyhydroxides, which adsorb metals, organics, and other nutrients, affecting element bioavailability, C cycling, and soil and water quality. Microbial Fe oxidation is predicted to accelerate Fe oxidation rates in low oxygen, Fe(II)-rich environments found in circumneutral aquifers and soils, where abiotic oxidation rates are slow. However, few neutrophilic FeOM species have been unambiguously shown to oxidize Fe; therefore we know little about the diversity, genetics, and biochemistry of FeOM that function at neutral pH.
My overall aim is to develop an integrated microbiological, biochemical, mineralogical and geochemical understanding of Fe microbial oxidation, in order to accurately describe modern and ancient Fe cycling on Earth. We first need to develop methods to recognize and quantify circumneutral microbial Fe oxidation and effects, so this project has the following research objectives: (1) Isolate and characterize novel FeOM from groundwater and thus expand the currently limited knowledge of FeOM diversity; (2) Discover candidates for key genes/proteins involved in Fe oxidation, to gain insight into bio(geo)chemical mechanisms and to give us the abilities to assay Fe-oxidation and recognize the genetic capability in (meta)genomes; (3) Characterize C metabolism and related genes in isolates, to understand how microbial Fe oxidizers can influence C cycling. This work will involve a combination of culturing and physiological characterization, differential gene/protein expression, qPCR, as well as sequencing and analysis of isolate genomes and environmental 16S rRNA and other genes. We will work in conjunction with the NSF Christina River Basin Critical Zone Observatory (CRB-CZO) in DE and PA, using CRB-CZO sites as a source of novel FeOM and as a testing ground for our new methods for detecting FeOM presence and activity.
The research themes will be integrated into educational activities that train students to think creatively and work across disciplines. Creativity and interdisciplinary scientific thought is vital to the innovation and problem-solving needed to advance our society and address environmental issues. Such skills take practice, so the main educational objectives are to (1) develop an inquiry-based undergraduate geomicrobiology class and (2) create a curriculum for a ?Microbes in the Wild!? science module for under-represented female middle school students in the Serviam Academy. I will also train a postdoctoral researcher and a PhD student over the course of the project. The research will be incorporated into continuing outreach programs, including school presentations, teacher workshops, the college?s annual Coast Day, Science Café, and other opportunities organized by the DE Sea Grant office.
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.
Microbes are numerous, widespread, and metabolically-versatile organisms, impacting virtually every environment on Earth?s surface. Iron-oxidizing microorganisms have likely been oxidizing, or ?rusting,? the Earth for billions of years. In near-neutral pH environments, they form iron oxyhydroxide minerals, which adsorb metals, organics, and other nutrients, affecting element bioavailability, carbon cycling, and soil and water quality. Iron-oxidizing microbes are predicted to be active in low oxygen, ferrous iron-rich environments found in near-neutral pH aquifers and soils, where abiotic oxidation rates are slow. However, few microorganisms have been unambiguously shown to oxidize iron at neutral pH (which is most common in the environment). Therefore we know little about the diversity, genetics, and biochemistry of iron-oxidizers that function at neutral pH.
In this project, we showed that neutrophilic (neutral pH-loving) iron-oxidizers are widespread, occurring in novel environments such as a stratified estuary and coastal aquifer, in addition to the well-known environments of streams and iron-rich hydrothermal vents. We isolated new neutrophilic iron-oxidizers, and demonstrated Fe oxidation ability for existing isolates, which expanded the diversity of known FeOB. Freshwater FeOB are famous for making distinctive mineralized filaments like twisted stalks, similar to the first known FeOB Gallionella ferruginea. Our two new stalk-forming isolates are related to G. ferruginea, but form a new genus Ferriphaselus (?iron bean?) within the family Gallionellaceae. We also isolated two new coastal marine FeOB, Mariprofundus aestuarium and M. ferrinatatus, the first pelagic marine FeOB, from the Cheseapeake Bay. All of these new isolates gave us the opportunity to investigate the genomes for genes involved in Fe oxidation. When comparing all available marine and terrestrial neutrophilic iron-oxidizer genomes, we found one specific gene in common ? cyc2. These sequences are distantly related to one from an acidophilic iron-oxidizer, Acidithiobacillus ferrooxidans, in which Cyc2 has been shown to oxidize iron, suggesting that the neutrophiles? Cyc2 may also oxidize Fe. Our protein structure modelling predicts that this is an unusual structure consisting of a fused cytochrome-porin, which would make it an outer membrane cytochrome. This overall structure is similar to the known iron-reducing porin-cytochrome complex MtrCAB, which also has an iron-oxidizing homolog, MtoAB; however, Cyc2 is distinct in its simpler structure, with one heme-binding motif fused to a smaller porin, suggesting a distinct role in iron transformations.
To investigate the function of the neutrophilic iron-oxidizer cyc2, we first studied its expression in different iron-oxidizing environments. If Cyc2 is an Fe oxidase, we would expect high expression of cyc2 in such environments. We analyzed metatranscriptomes from two ecosystems dominated by Fe-oxidizing bacteria: the Loihi Seamount (Hawaii) hydrothermal vent Fe microbial mat and an Fe-rich alluvial aquifer in Rifle, Colorado (reanalysis of Jewell et al., 2016 dataset). In both environments, the putative Fe oxidase gene cyc2 was highly expressed in situ, often as the highest expressed gene. Furthermore, the cyc2 gene increased in expression in Loihi iron microbial mat incubations after Fe(II) amendment, with corresponding increases in expression of carbon fixation and central metabolism genes. Our re-analysis of the Rifle aquifer dataset shows that the cyc2 gene was expressed at much higher levels than mtoA, by two orders of magnitude. Thus, while both putative Fe oxidases were expressed when Fe oxidation was stimulated, cyc2 was clearly preferentially expressed. Our results support a Cyc2-based Fe oxidation pathway and demonstrate its significance in both marine and terrestrial Fe-mineralizing environments. Initial studies on heterologously-expressed Cyc2 provide additional evidence of function. In all, the work to date suggests that cyc2 could be a broadly-distributed genetic marker for Fe oxidation.
This project provided training for four undergraduates, four graduate students, and four postdocs, including seven female trainees, in geomicrobiological techniques, including culturing, biochemistry, and bioinformatics. Four theses were produced, and the PI earned tenure. We used research project sites and data in a problem-based learning Geomicrobiology class for undergraduates and early graduate students. We also developed a Microbes in the Wild outreach curriculum at the Serviam Academy in Wilmington, DE. This workshop introduce 5th to 8th grade girls to geo/environmental microbiology using a combination of culturing, microscopy, DNA extractions, and other hands on activities. Other outreach included science communication education at Havre de Grace high school, public outreach at our annual marine science festival Coast Day and a 4H camp, public community-oriented presentations, and school tours of our Biotechnology institute.
Last Modified: 07/10/2019
Modified by: Clara Chan
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