Christopher Fuller
Christopher Fuller is a Emeritus Scientist for the USGS Water Resources Mission Area. His research characterizes processes and mechanisms of metal sorption reactions through field studies and lab experiments to better understand the metal transport and natural attenuation in mine contaminated systems and to better understand geochemical processes affecting bioavailability of metal contaminants to aquatic organisms.
Professional societies/affiliations/committees/editorial boards
American Geophysical Union
American Chemical Society
Geochemical Society
Professional Experience
Professional Studies/Experience
2019 - current: Scientist Emeritus
2018 - 2019: Research Hydrologist (Geochemistry), Hydrological-Ecological Interactions Branch, Earth Surface Processes Division, Water Mission Area, U.S. Geological Survey
1982 - 2017: Research Hydrologist (Geochemistry), National Research Program, Western Region, U.S. Geological Survey
1976 - 1982: Research Technician, Unversity of Southern California
Education and Certifications
Education
1976: BS Chemistry, SUNY Oswego
1982: MS Geology, emphasis in Marine Geochemistry, University of Southern California
Honors and Awards
Honors, awards, recognition, elected offices
May 1996: Editors Citation for Excellence in Manuscript Review for the Soil Science Society of America Journal
May 2003. STAR award for instrumental role in developing cooperative project with BLM at the Fry Canyon permeable reactive barrier demonstration site.
November 2006 Superior Service Award
October 2007. STAR award “Chris has done an outstanding job in age dating over 90 lake sediment cores collected from Great Salt Lake in a very short time frame to accommodate a Utah Water Science Center cooperator. This work was published in Applied Geochemistry.
June 2014 Superior Service Award
Science and Products
The approaching obsolescence of 137Cs dating of wetland soils in North America
Geochemistry of mercury and other constituents in subsurface sediment—Analyses from 2011 and 2012 coring campaigns, Cache Creek Settling Basin, Yolo County, California
Estimation and uncertainty of recent carbon accumulation and vertical accretion in drained and undrained forested peatlands of the southeastern USA
Sources and ages of fine-grained sediment to streams using fallout radionuclides in the Midwestern United States
Assessing the dietary bioavailability of metals associated with natural particles: Extending the use of the reverse labeling approach to zinc
Soil data for a thermokarst bog and the surrounding permafrost plateau forest, located at Bonanza Creek Long Term Ecological Research Site, Interior Alaska
Decadal and long-term boreal soil carbon and nitrogen sequestration rates across a variety of ecosystems
Soil data for a vegetation gradient located at Bonanza Creek Long Term Ecological Research Site, interior Alaska
Biogeochemical controls of uranium bioavailability from the dissolved phase in natural freshwaters
A millennial-scale record of Pb and Hg contamination in peatlands of the Sacramento-San Joaquin Delta of California, USA
Dietary uptake of Cu sorbed to hydrous iron oxide is linked to cellular toxicity and feeding inhibition in a benthic grazer
Recent rates of carbon accumulation in montane fens ofYosemite National Park, California, U.S.A.
Science and Products
- Science
- Data
- Multimedia
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Filter Total Items: 83
The approaching obsolescence of 137Cs dating of wetland soils in North America
The peak fallout in 1963 of the radionuclide 137Cs has been used to date lake, reservoir, continental shelf, and wetland sedimentary deposits. In wetlands such dating is used to project the ability of wetlands to keep pace with sea level rise and develop strategies for mitigating carbon pollution using biological carbon sequestration. Here we demonstrate that reliable 137Cs profiles are increasingAuthorsJudith Z. Drexler, Christopher C. Fuller, Stacey A. ArchfieldGeochemistry of mercury and other constituents in subsurface sediment—Analyses from 2011 and 2012 coring campaigns, Cache Creek Settling Basin, Yolo County, California
Cache Creek Settling Basin was constructed in 1937 to trap sediment from Cache Creek before delivery to the Yolo Bypass, a flood conveyance for the Sacramento River system that is tributary to the Sacramento–San Joaquin Delta. Sediment management options being considered by stakeholders in the Cache Creek Settling Basin include sediment excavation; however, that could expose sediments containing eAuthorsMichelle R. Arias, Charles N. Alpers, Mark C. Marvin-DiPasquale, Christopher C. Fuller, Jennifer L. Agee, Michelle Sneed, Andrew Y. Morita, Antonia SalasEstimation and uncertainty of recent carbon accumulation and vertical accretion in drained and undrained forested peatlands of the southeastern USA
The purpose of this study was to determine how drainage impacts carbon densities and recent rates (past 50 years) of vertical accretion and carbon accumulation in southeastern forested peatlands. We compared these parameters in drained maple-gum (MAPL), Atlantic white cedar (CDR), and pocosin (POC) communities in the Great Dismal Swamp National Wildlife Refuge (GDS) of Virginia/North Carolina andAuthorsJudith Z. Drexler, Christopher C. Fuller, James L. Orlando, Antonia Salas, Frederic C. Wurster, Jamie A. DubersteinSources and ages of fine-grained sediment to streams using fallout radionuclides in the Midwestern United States
Fallout radionuclides, 7Be and 210Pbex, sampled in bed sediment for 99 watersheds in the Midwestern region of the United States and in 15 samples of suspended sediment from 3 of these watersheds were used to partition upland from channel sources and to estimate the age or the time since the surface-derived portion of sediment was on the land surface (0–∼1 year). Channel sources dominate: 78 of theAuthorsAllen C. Gellis, Christopher C. Fuller, Peter C. Van MetreAssessing the dietary bioavailability of metals associated with natural particles: Extending the use of the reverse labeling approach to zinc
We extend the use of a novel tracing technique to quantify the bioavailability of zinc (Zn) associated with natural particles using snails enriched with a less common Zn stable isotope. Lymnaea stagnalis is a model species that has relatively fast Zn uptake rates from the dissolved phase, enabling their rapid enrichment in 67Zn during the initial phase of labeling. Isotopically enriched snails werAuthorsMarie-Noële Croteau, Daniel J. Cain, Christopher C. FullerSoil data for a thermokarst bog and the surrounding permafrost plateau forest, located at Bonanza Creek Long Term Ecological Research Site, Interior Alaska
Peatlands play an important role in boreal ecosystems, storing a large amount of soil organic carbon. In northern ecosystems, collapse-scar bogs (also known as thermokarst bogs) often form as the result of ground subsidence following permafrost thaw. To examine how ecosystem carbon balance changes with the loss of permafrost, we measured carbon and nitrogen storage within a thermokarst bog and theAuthorsKristen L. Manies, Christopher C. Fuller, Miriam C. Jones, Mark P. Waldrop, John P. McGeehinDecadal and long-term boreal soil carbon and nitrogen sequestration rates across a variety of ecosystems
Boreal soils play a critical role in the global carbon (C) cycle; therefore, it is important to understand the mechanisms that control soil C accumulation and loss for this region. Examining C & nitrogen (N) accumulation rates over decades to centuries may provide additional understanding of the dominant mechanisms for their storage, which can be masked by seasonal and interannual variability whenAuthorsKristen L. Manies, Jennifer W. Harden, Christopher C. Fuller, Merritt TuretskySoil data for a vegetation gradient located at Bonanza Creek Long Term Ecological Research Site, interior Alaska
Boreal soils play an important role in the global carbon cycle owing to the large amount of carbon stored within this northern region. To understand how carbon and nitrogen storage varied among different ecosystems, a vegetation gradient was established in the Bonanza Creek Long Term Ecological Research (LTER) site, located in interior Alaska. The ecosystems represented are a black spruce (Picea mAuthorsKristen L. Manies, Jennifer W. Harden, Christopher C. Fuller, Xiaomei Xu, John P. McGeehinBiogeochemical controls of uranium bioavailability from the dissolved phase in natural freshwaters
To gain insights into the risks associated with uranium (U) mining and processing, we investigated the biogeochemical controls of U bioavailability in the model freshwater speciesLymnaea stagnalis (Gastropoda). Bioavailability of dissolved U(VI) was characterized in controlled laboratory experiments over a range of water hardness, pH, and in the presence of complexing ligands in the form of dissolAuthorsMarie-Noële Croteau, Christopher C. Fuller, Daniel J. Cain, Kate M. Campbell, George R. AikenA millennial-scale record of Pb and Hg contamination in peatlands of the Sacramento-San Joaquin Delta of California, USA
In this paper, we provide the first record of millennial patterns of Pb and Hg concentrations on the west coast of the United States. Peat cores were collected from two micro-tidal marshes in the Sacramento-San Joaquin Delta of California. Core samples were analyzed for Pb, Hg, and Ti concentrations and dated using radiocarbon, 210Pb, and 137Cs. Pre-anthropogenic concentrations of Pb and Hg in peaAuthorsJudith Z. Drexler, Charles N. Alpers, Leonid A. Neymark, James B. Paces, Howard E. Taylor, Christopher C. FullerDietary uptake of Cu sorbed to hydrous iron oxide is linked to cellular toxicity and feeding inhibition in a benthic grazer
Whereas feeding inhibition caused by exposure to contaminants has been extensively documented, the underlying mechanism(s) are less well understood. For this study, the behavior of several key feeding processes, including ingestion rate and assimilation efficiency, that affect the dietary uptake of Cu were evaluated in the benthic grazer Lymnaea stagnalis following 4–5 h exposures to Cu adsorbed tAuthorsDaniel J. Cain, Marie-Noële Croteau, Christopher C. Fuller, Amy H. RingwoodRecent rates of carbon accumulation in montane fens ofYosemite National Park, California, U.S.A.
Little is known about recent rates of carbon storage in montane peatlands, particularly in the western United States. Here we report on recent rates of carbon accumulation (past 50 to 100 years) in montane groundwater-fed peatlands (fens) of Yosemite National Park in central California, U.S.A. Peat cores were collected at three sites ranging in elevation from 2070 to 2500 m. Core sections were anaAuthorsJudith Z. Drexler, Christopher C. Fuller, James L. Orlando, Peggy E. Moore