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Uranium-, thorium-, strontium-, carbon- and oxygen-isotope data used to evaluate a 300,000-year history of water-table fluctuations at Wind Cave, South Dakota, USA — scale, timing, and groundwater mixing in the Madison Aquifer

Dates

Publication Date
Start Date
2010
End Date
2017

Citation

Paces, J.B., 2020, Uranium-, thorium-, strontium-, carbon- and oxygen-isotope data used to evaluate a 300,000-year history of water-table fluctuations at Wind Cave, South Dakota, USA — scale, timing, and groundwater mixing in the Madison Aquifer: U.S. Geological Survey data release, https://doi.org/10.5066/P9136UKL.

Summary

Tables of U- and Th-isotopic data used to calculate uranium-series age estimates and initial 234U/238U activity ratios as well as 87Sr/86Sr, δ13C, and δ18O for samples of phreatic speleothems from Wind Cave National Park and U- and Sr-isotopic compositions of waters from the southern Black Hills of South Dakota, USA

Child Items (0)

Contacts

Point of Contact :
James B Paces
Originator :
James B Paces
Metadata Contact :
James B Paces
Publisher :
U.S. Geological Survey
Distributor :
U.S. Geological Survey - ScienceBase
SDC Data Owner :
Geosciences and Environmental Change Science Center
USGS Mission Area :
Core Science Systems

Attached Files

Click on title to download individual files attached to this item.

Isotopes_Wind_Cave metadata (v3).xml
“Wind Cave metadata”
Original FGDC Metadata

View
42.49 KB application/fgdc+xml
WindCave'19_DataRelease_2_waters.csv
“Wind Cave water data”
3.6 KB text/csv
WindCave'19_DataRelease_DataDictionary.csv
“Wind Cave data dictionary”
8.88 KB text/csv
WindCave'19_DataRelease_1_cc.csv
“Wind Cave calcite data”
17.76 KB text/csv

Purpose

Isotopes of U and Th from phreatic speleothems exposed in lower passageways at Wind Cave were used to better establish the history of water table fluctuations over the past million years. In addition, Sr-, U-, C-, and O-isotopes from dated calcite samples were obtained to evaluate potential shifts in paleo groundwater composition compared to modern groundwater compositions from different aquifers in the region. Results are used to understand processes contributing to water resources at Wind Cave National Park and the regional hydrogeologic responses to Plestocene climate shifts.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9136UKL

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