University of Saskatchewan - Geology
Assistant Professor, Geological Sciences at University of Saskatchewan
Research
Joyce
McBeth
Saskatoon, Saskatchewan, Canada
I'm currently recruiting MSc students, and I have fully-funded positions for several students to begin in 2019. If you are interested in furthering your career in environmental geosciences with an MSc degree in mine waste remediation-related sciences, please get in touch to discuss the possibilities.
Further info here: https://research-groups.usask.ca/mcbeth/opportunities.php#EmployeeOpportunities
My scientific interests:
-redox transformations of metal(loids) in the environment
-relationships of microorganisms to these transformations
-using synchrotron methods to image and characterize the chemistry of contaminated sites and mine wastes
-environmental microbiology and the cycling of iron, sulfur, toxic metals, and other elements in environments such as mine-impacted environments, uranium mine tailings, oil sands tailings, wastewater, hydrocarbon contaminated sites, constructed wetland treatment systems, salt marshes, and marine sediments
-microbiology of steel corrosion
-microbial ecology of microbial mats
-fossilized microbes and microbial biosignatures in the rock record
-archaeaology and toxicology
Specialties:
Geomicrobiology
Biogeochemistry
Geochemistry
Soil and Groundwater Bioremediation
Microbiology
Bacteriology
Microbial Ecology
Use of synchrotron tools in geomicrobiology
Adjunct Professor, Geological Sciences
Joyce worked at University of Saskatchewan as a Adjunct Professor, Geological Sciences
Assistant Professor, Geological Sciences
As an Assistant Professor at USask, I teach and conduct research on microbial interactions with the geosphere. I am specifically interested in metal(loid) and hydrocarbon contaminant remediation, metal transformations mediated by microbes in mine wastes, and metal biosignatures in fossils. My projects included studies of uranium mine tailings and ores, oil sands tailings, groundwater treatment for elevated Mn and Fe, saline/freshwater gradient microbiology, and metals in trace fossils. I teach physical geology (1st year course), introductory geomicrobiology (3rd year course), and I've assisted with hard and soft rock field schools. I'm heavily involved in three open textbook projects for our first year physical geology course.
Postdoctoral Researcher
Investigating marine corrosion communities and the influence of iron-oxidizing bacteria on steel corrosion. Isolated GSB-2, the first example of a Zetaproterobacterium isolated in a near-shore environment.
Part-time postdoc
undergrad project supervision, lipid extraction and biosignature analyses
Field Geoscientist in Training
hydrocarbon contaminated site remediation, supervising tank pulls and installations, supervising contractors.
Staff Scientist - Earth & Environment
In my work at CLS, I conducting research on topics relating to sustainable mine waste studies - specifically metal(loid) contaminant remediation and metal transformations mediated by microbes in mine wastes. My projects included studies of uranium mine tailings and ores, oil sands tailings, groundwater treatment for elevated Mn and Fe, potash mine wastewater, and constructed wetland treatment systems.
PhD
Geological Sciences
Geomicrobiology
MSc
Geological Sciences
Geomicrobiology
BSc
Earth and Ocean Sciences
Geological Sciences
Journal of Archaeological Science: Reports
The Franklin Expedition (1845–1848) left in search of the Northwest Passage and ended tragically with the loss of all crew members. Mystery surrounds their ultimate fate, with particular speculation around the role of lead poisoning. Our unique study turns nails from crew member John Hartnell into a time machine to determine what happened to the Franklin Expedition crew members. Using micro-X-ray fluorescence mapping, stable isotopic measurements, and laser ablation inductively coupled plasma mass spectrometry, we navigate through the nails and temporally characterize lead, copper and zinc content in our subject during the early expedition. By circumventing external contamination on exposed nail surfaces, we challenge the theory that crew members were exposed to high levels of lead on the expedition. Our analyses suggest that lead exposure actually decreased over the course of the expedition and Hartnell's levels were within a healthy, normal range. Our study also finds, however, that Hartnell was severely zinc-deficient, possibly leading to immuno-suppression and ultimately, tuberculosis and death. The significant weight loss from his illness resulted in a flush of previously stored lead from his bones into his blood (and nail), but only in the last few weeks of life.
Journal of Archaeological Science: Reports
The Franklin Expedition (1845–1848) left in search of the Northwest Passage and ended tragically with the loss of all crew members. Mystery surrounds their ultimate fate, with particular speculation around the role of lead poisoning. Our unique study turns nails from crew member John Hartnell into a time machine to determine what happened to the Franklin Expedition crew members. Using micro-X-ray fluorescence mapping, stable isotopic measurements, and laser ablation inductively coupled plasma mass spectrometry, we navigate through the nails and temporally characterize lead, copper and zinc content in our subject during the early expedition. By circumventing external contamination on exposed nail surfaces, we challenge the theory that crew members were exposed to high levels of lead on the expedition. Our analyses suggest that lead exposure actually decreased over the course of the expedition and Hartnell's levels were within a healthy, normal range. Our study also finds, however, that Hartnell was severely zinc-deficient, possibly leading to immuno-suppression and ultimately, tuberculosis and death. The significant weight loss from his illness resulted in a flush of previously stored lead from his bones into his blood (and nail), but only in the last few weeks of life.
Journal of Archaeological Science: Reports
The Franklin Expedition (1845–1848) left in search of the Northwest Passage and ended tragically with the loss of all crew members. Mystery surrounds their ultimate fate, with particular speculation around the role of lead poisoning. Our unique study turns nails from crew member John Hartnell into a time machine to determine what happened to the Franklin Expedition crew members. Using micro-X-ray fluorescence mapping, stable isotopic measurements, and laser ablation inductively coupled plasma mass spectrometry, we navigate through the nails and temporally characterize lead, copper and zinc content in our subject during the early expedition. By circumventing external contamination on exposed nail surfaces, we challenge the theory that crew members were exposed to high levels of lead on the expedition. Our analyses suggest that lead exposure actually decreased over the course of the expedition and Hartnell's levels were within a healthy, normal range. Our study also finds, however, that Hartnell was severely zinc-deficient, possibly leading to immuno-suppression and ultimately, tuberculosis and death. The significant weight loss from his illness resulted in a flush of previously stored lead from his bones into his blood (and nail), but only in the last few weeks of life.
Applied Geochemistry
Journal of Archaeological Science: Reports
The Franklin Expedition (1845–1848) left in search of the Northwest Passage and ended tragically with the loss of all crew members. Mystery surrounds their ultimate fate, with particular speculation around the role of lead poisoning. Our unique study turns nails from crew member John Hartnell into a time machine to determine what happened to the Franklin Expedition crew members. Using micro-X-ray fluorescence mapping, stable isotopic measurements, and laser ablation inductively coupled plasma mass spectrometry, we navigate through the nails and temporally characterize lead, copper and zinc content in our subject during the early expedition. By circumventing external contamination on exposed nail surfaces, we challenge the theory that crew members were exposed to high levels of lead on the expedition. Our analyses suggest that lead exposure actually decreased over the course of the expedition and Hartnell's levels were within a healthy, normal range. Our study also finds, however, that Hartnell was severely zinc-deficient, possibly leading to immuno-suppression and ultimately, tuberculosis and death. The significant weight loss from his illness resulted in a flush of previously stored lead from his bones into his blood (and nail), but only in the last few weeks of life.
Applied Geochemistry
Frontiers in Microbiology
This work indicates there is a successional pattern in the colonization of steel surfaces and iron oxidizing bacteria are early colonizers; over time the MIC community matures to include other members that may help accelerate corrosion. This work also shows there is a reservoir for Zetaproteobacteria in coastal sediment habitats, where they may influence the coastal iron cycle, and can rapidly colonize steel surfaces or other sources of Fe(II) when available.
Journal of Archaeological Science: Reports
The Franklin Expedition (1845–1848) left in search of the Northwest Passage and ended tragically with the loss of all crew members. Mystery surrounds their ultimate fate, with particular speculation around the role of lead poisoning. Our unique study turns nails from crew member John Hartnell into a time machine to determine what happened to the Franklin Expedition crew members. Using micro-X-ray fluorescence mapping, stable isotopic measurements, and laser ablation inductively coupled plasma mass spectrometry, we navigate through the nails and temporally characterize lead, copper and zinc content in our subject during the early expedition. By circumventing external contamination on exposed nail surfaces, we challenge the theory that crew members were exposed to high levels of lead on the expedition. Our analyses suggest that lead exposure actually decreased over the course of the expedition and Hartnell's levels were within a healthy, normal range. Our study also finds, however, that Hartnell was severely zinc-deficient, possibly leading to immuno-suppression and ultimately, tuberculosis and death. The significant weight loss from his illness resulted in a flush of previously stored lead from his bones into his blood (and nail), but only in the last few weeks of life.
Applied Geochemistry
Frontiers in Microbiology
This work indicates there is a successional pattern in the colonization of steel surfaces and iron oxidizing bacteria are early colonizers; over time the MIC community matures to include other members that may help accelerate corrosion. This work also shows there is a reservoir for Zetaproteobacteria in coastal sediment habitats, where they may influence the coastal iron cycle, and can rapidly colonize steel surfaces or other sources of Fe(II) when available.
Environmental Science and Technology 44 (11): 156-162.
In this manuscript we describe experiments we did using gamma camera imaging and the short-lived isotope Tc-99m (T 1/2 = 6.5 hrs) to investigate movement of pM concentrations of Tc through columns of sediment from the Oak Ridge Field Research Center Field Site.
Journal of Archaeological Science: Reports
The Franklin Expedition (1845–1848) left in search of the Northwest Passage and ended tragically with the loss of all crew members. Mystery surrounds their ultimate fate, with particular speculation around the role of lead poisoning. Our unique study turns nails from crew member John Hartnell into a time machine to determine what happened to the Franklin Expedition crew members. Using micro-X-ray fluorescence mapping, stable isotopic measurements, and laser ablation inductively coupled plasma mass spectrometry, we navigate through the nails and temporally characterize lead, copper and zinc content in our subject during the early expedition. By circumventing external contamination on exposed nail surfaces, we challenge the theory that crew members were exposed to high levels of lead on the expedition. Our analyses suggest that lead exposure actually decreased over the course of the expedition and Hartnell's levels were within a healthy, normal range. Our study also finds, however, that Hartnell was severely zinc-deficient, possibly leading to immuno-suppression and ultimately, tuberculosis and death. The significant weight loss from his illness resulted in a flush of previously stored lead from his bones into his blood (and nail), but only in the last few weeks of life.
Applied Geochemistry
Frontiers in Microbiology
This work indicates there is a successional pattern in the colonization of steel surfaces and iron oxidizing bacteria are early colonizers; over time the MIC community matures to include other members that may help accelerate corrosion. This work also shows there is a reservoir for Zetaproteobacteria in coastal sediment habitats, where they may influence the coastal iron cycle, and can rapidly colonize steel surfaces or other sources of Fe(II) when available.
Environmental Science and Technology 44 (11): 156-162.
In this manuscript we describe experiments we did using gamma camera imaging and the short-lived isotope Tc-99m (T 1/2 = 6.5 hrs) to investigate movement of pM concentrations of Tc through columns of sediment from the Oak Ridge Field Research Center Field Site.
Geomicrobiology Journal 23: 1-9.
In this manuscript we summarize results from Tc spiked progressive sediment microcosm experiments. We examining the redox and coordination environment of Tc in parallel samples analyzed using EXAFS. The sediment used in these experiments was from the Oak Ridge National Lab Field Research Center Site.
Journal of Archaeological Science: Reports
The Franklin Expedition (1845–1848) left in search of the Northwest Passage and ended tragically with the loss of all crew members. Mystery surrounds their ultimate fate, with particular speculation around the role of lead poisoning. Our unique study turns nails from crew member John Hartnell into a time machine to determine what happened to the Franklin Expedition crew members. Using micro-X-ray fluorescence mapping, stable isotopic measurements, and laser ablation inductively coupled plasma mass spectrometry, we navigate through the nails and temporally characterize lead, copper and zinc content in our subject during the early expedition. By circumventing external contamination on exposed nail surfaces, we challenge the theory that crew members were exposed to high levels of lead on the expedition. Our analyses suggest that lead exposure actually decreased over the course of the expedition and Hartnell's levels were within a healthy, normal range. Our study also finds, however, that Hartnell was severely zinc-deficient, possibly leading to immuno-suppression and ultimately, tuberculosis and death. The significant weight loss from his illness resulted in a flush of previously stored lead from his bones into his blood (and nail), but only in the last few weeks of life.
Applied Geochemistry
Frontiers in Microbiology
This work indicates there is a successional pattern in the colonization of steel surfaces and iron oxidizing bacteria are early colonizers; over time the MIC community matures to include other members that may help accelerate corrosion. This work also shows there is a reservoir for Zetaproteobacteria in coastal sediment habitats, where they may influence the coastal iron cycle, and can rapidly colonize steel surfaces or other sources of Fe(II) when available.
Environmental Science and Technology 44 (11): 156-162.
In this manuscript we describe experiments we did using gamma camera imaging and the short-lived isotope Tc-99m (T 1/2 = 6.5 hrs) to investigate movement of pM concentrations of Tc through columns of sediment from the Oak Ridge Field Research Center Field Site.
Geomicrobiology Journal 23: 1-9.
In this manuscript we summarize results from Tc spiked progressive sediment microcosm experiments. We examining the redox and coordination environment of Tc in parallel samples analyzed using EXAFS. The sediment used in these experiments was from the Oak Ridge National Lab Field Research Center Site.
Environmental Science & Technology
Journal of Archaeological Science: Reports
The Franklin Expedition (1845–1848) left in search of the Northwest Passage and ended tragically with the loss of all crew members. Mystery surrounds their ultimate fate, with particular speculation around the role of lead poisoning. Our unique study turns nails from crew member John Hartnell into a time machine to determine what happened to the Franklin Expedition crew members. Using micro-X-ray fluorescence mapping, stable isotopic measurements, and laser ablation inductively coupled plasma mass spectrometry, we navigate through the nails and temporally characterize lead, copper and zinc content in our subject during the early expedition. By circumventing external contamination on exposed nail surfaces, we challenge the theory that crew members were exposed to high levels of lead on the expedition. Our analyses suggest that lead exposure actually decreased over the course of the expedition and Hartnell's levels were within a healthy, normal range. Our study also finds, however, that Hartnell was severely zinc-deficient, possibly leading to immuno-suppression and ultimately, tuberculosis and death. The significant weight loss from his illness resulted in a flush of previously stored lead from his bones into his blood (and nail), but only in the last few weeks of life.
Applied Geochemistry
Frontiers in Microbiology
This work indicates there is a successional pattern in the colonization of steel surfaces and iron oxidizing bacteria are early colonizers; over time the MIC community matures to include other members that may help accelerate corrosion. This work also shows there is a reservoir for Zetaproteobacteria in coastal sediment habitats, where they may influence the coastal iron cycle, and can rapidly colonize steel surfaces or other sources of Fe(II) when available.
Environmental Science and Technology 44 (11): 156-162.
In this manuscript we describe experiments we did using gamma camera imaging and the short-lived isotope Tc-99m (T 1/2 = 6.5 hrs) to investigate movement of pM concentrations of Tc through columns of sediment from the Oak Ridge Field Research Center Field Site.
Geomicrobiology Journal 23: 1-9.
In this manuscript we summarize results from Tc spiked progressive sediment microcosm experiments. We examining the redox and coordination environment of Tc in parallel samples analyzed using EXAFS. The sediment used in these experiments was from the Oak Ridge National Lab Field Research Center Site.
Environmental Science & Technology
Appl Env Microbio
I isolated a new marine iron-oxidizing bacterium, Mariprofundus sp Strain GSB2 that enhanced uniform corrosion from mild steel in laboratory microcosm experiments. These results have important implications for the role of FeOB in corrosion of steel in nearshore and estuarine environments. In addition, this work shows that the global distribution of Zetaproteobacteria is far greater than previously thought.
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