Biogeochemical data of water, sediments, periphyton, and macroinvertebrates collected from springs in and near Grand Canyon National Park, Arizona (ver. 4.0, October 2022)
Dates
Publication Date
2019-12-09
Time Period
2016-04-20
Time Period
2021-03-02
Last Revision
2022-10-06
Citation
Fuller, C.C., Cain, D.J., Croteau, M.N., Barasch, D.A., Beisner, K.R., Stoliker, D.L., Schenk, E.R. and Campbell-Hay, K.M., 2019, Biogeochemical data of water, sediments, periphyton, and macroinvertebrates collected from springs in and near Grand Canyon National Park, Arizona (ver. 4.0, October 2022): U.S. Geological Survey data release, https://doi.org/10.5066/P9CR6GCW.
Summary
The U.S. Geological Survey is studying uranium and associated trace element bioaccumulation in aquatic invertebrates across a gradient of dissolved uranium concentrations in spring outflow pools and creeks in the Grand Canyon and adjacent watershed. This data release makes available data from sampling campaigns in April 2016, April 2017, and in April 2019. Data collected include: (1) major ion, trace element and dissolved organic carbon in surface waters of spring outflow pools and streams; (2) concentrations of uranium and other trace elements in bed sediment, periphyton, and larva of aquatic insect taxa; (3) uranium and iron extraction data from a subset of bed sediment samples, and (4) X-ray diffraction data for bed sediment samples [...]
Summary
The U.S. Geological Survey is studying uranium and associated trace element bioaccumulation in aquatic invertebrates across a gradient of dissolved uranium concentrations in spring outflow pools and creeks in the Grand Canyon and adjacent watershed. This data release makes available data from sampling campaigns in April 2016, April 2017, and in April 2019. Data collected include: (1) major ion, trace element and dissolved organic carbon in surface waters of spring outflow pools and streams; (2) concentrations of uranium and other trace elements in bed sediment, periphyton, and larva of aquatic insect taxa; (3) uranium and iron extraction data from a subset of bed sediment samples, and (4) X-ray diffraction data for bed sediment samples collected in 2019. This dataset includes samples from the corrected original data release (invertebrate data for 2016 were incorrectly reported as mass concentrations (mg/kg) in the original csv file), plus samples collected in 2019. NOTE: While previous versions are available from the author, all the records in previous versions can be found in version 4.0. Direct questions regarding data to the authors.
Click on title to download individual files attached to this item.
Fuller_et_al_ 2018_datarelease_V4.0.xml Original FGDC Metadata
View
145.97 KB
application/fgdc+xml
Horn 2.2.JPG
3.67 MB
image/jpeg
Sediment 2016.csv
2.35 KB
text/csv
Sediment 2017.csv
4.52 KB
text/csv
Periphyton 2016-2017.csv
2.78 KB
text/csv
2017_sediment_extraction.csv
516 Bytes
text/csv
2019_XRDdata.csv
57.27 KB
text/csv
Inverts 2016-2019_V4.0.csv
49.13 KB
text/csv
QAQC U.csv
6.83 KB
text/csv
revision_history_V4.0.txt
1.05 KB
text/plain
Sediment 2019_V4.0.csv
2.72 KB
text/csv
Water 2016-2019_V4.0.csv
5.13 KB
text/csv
Purpose
Processes controlling uranium (U) bioaccumulation and toxicity are poorly understood for aquatic macroinvertebrates, a large and diverse assemblage of species that is functionally vital to aquatic and riparian ecosystems. Conceptually, U exposure occurs from contact with contaminated water as well as from ingestion of contaminated food. Bioaccumulation and toxicity resulting from exposure are moderated by site-specific geochemical conditions and the ecological and physiological traits of the species. To complement laboratory studies aimed at developing a mechanistic model of U bioaccumulation for aquatic macroinvertebrates, field data are needed to constrain model parameters relevant to environmental conditions and taxa at sites in the Grand Canyon region. These data provide a description of the occurrence of U, and other trace elements associated with U-ore and to qualify their potential to contaminate aquatic food webs. Therefore, for this study, spring outflow pools and creeks are sampled because they are essential to aquatic and riparian ecosystems of the region. Site selection is guided by measurements of water chemistry from springs and associated runoff which have shown a range of U concentrations ranging from elevated levels in Horn Creek and Salt Creek situated below the South Rim of the Grand Canyon, and in Pigeon Spring in a tributary to Kanab Creek, to lower levels in nearby creeks. The contrast in dissolved U concentrations among sites provides a gradient in U exposure to examine responses in U bioaccumulation, as determined by body burdens of U in aquatic macroinvertebrates inhabiting the sites.
Revision 4.0 completed by Marie-Noële Croteau on October 5, 2022. To review the changes that were made, see “revision_history_V4.0.txt” in the attached files section.