Hurwitz, S., Peek, S., King, J., Pigati, J., Honke, J., Damby, D.E., and Stricker, C.A., 2020. Silicified wood from around Old Faithful Geyser, Yellowstone National Park: U.S. Geological Survey data release, https://doi.org/10.5066/P9LEQ5HC.
Summary
Radiocarbon dating of silicified wood was performed at the U.S. Geological Survey’s Radiocarbon Laboratory in Denver, Colorado. All samples were chemically treated using the standard acid-base-acid (ABA) procedure before being combusted online in the presence of excess high-purity oxygen. Water and other contaminant gases were removed using cryogenic separation techniques, and the resulting purified CO2 gas was measured manometrically and converted to graphite using an iron catalyst and hydrogen reduction (Vogel et al., 1984). Graphite targets were then submitted for accelerator mass spectrometry 14C analysis at the National Ocean Sciences Accelerator Mass Spectrometry facility in Woods Hole, Massachusetts. All 14C ages were calibrated [...]
Summary
Radiocarbon dating of silicified wood was performed at the U.S. Geological Survey’s Radiocarbon Laboratory in Denver, Colorado. All samples were chemically treated using the standard acid-base-acid (ABA) procedure before being combusted online in the presence of excess high-purity oxygen. Water and other contaminant gases were removed using cryogenic separation techniques, and the resulting purified CO2 gas was measured manometrically and converted to graphite using an iron catalyst and hydrogen reduction (Vogel et al., 1984). Graphite targets were then submitted for accelerator mass spectrometry 14C analysis at the National Ocean Sciences Accelerator Mass Spectrometry facility in Woods Hole, Massachusetts.
All 14C ages were calibrated using the IntCal13 dataset and CALIB 7.1html (Stuiver and Reimer, 1993; Reimer et al., 2013). Calibrated age ranges are presented in calibrated years before present (BP; 0 yr BP = 1950 A.D.), and uncertainties are given at the 95% (2sigma) confidence level.
Select sub-samples of silicified wood were excised with a stainless-steel razor blade and massed into 4 x 6 mm tin capsules (Costech Analytical, Inc, USA). Stable carbon isotope (δ13C) analysis was conducted by continuous flow-isotope ratio mass spectrometry at the U.S. Geological Survey’s Stable Isotope Laboratory in Denver, Colorado using a Carlo Erba NC1500 interfaced to a Micromass Optima mass spectrometer. Isotopic data are reported in per mil notation after normalization to VPDB with USGS 40 (δ13C = -26.39 ‰) and USGS 41A (δ13C = 36.55 ‰).
This research was conducted under Yellowstone Research Permit YELL-SCI-8030.
References
Johnson, C.A., Stricker, C.A., Gulbransen, C.A., and Emmons, M.P., 2017. Determination of δ13C, δ15N, or δ34S by isotope-ratio-monitoring mass spectrometry using an elemental analyzer: U.S. Geological Survey Techniques and Methods, book 5, chap. D4, 27 p., https://doi.org/10.3133/tm5D4.
Reimer, P.J., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronk Ramsey, C., Buck, C.E., Cheng, H., Edwards, R.L., Friedrich, M., Grootes, P.M., Guilderson, T.P., Haflidason, H., Hajdas, I., Hatte, C., Heaton, T.J., Hoffmann, D.L., Hogg, A.G., Hughen, K.A., Kaiser, K.F., Kromer, B., Manning, S.W., Niu, M., Reimer, R.W., Richards, D.A., Scott, E.M., Southon, J.R., Staff, R.A., Turney, C.S.M., and van der Plicht, J., 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0-50,000 years cal BP. Radiocarbon 55, 1869-1887.
Stuiver, M., and Reimer, P.J., 1993. Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon 35, 215-230.
Vogel, J.S., Southon, J.R., Nelson, D.E., and Brown, T.A., 1984. Performance of catalytically condensed carbon for use in accelerator mass spectrometry. Nuclear Instruments and Methods in Physics Research B 5, 289-293.
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Related External Resources
Type: Related Primary Publication
Enter Primary Related Publication: Hurwitz, S., King, J. C., Pederson, G. T., Martin, J. T., Damby, D. E., Manga, M., et al. (2020). Yellowstone's Old Faithful Geyser shut down by a severe thirteenth century drought. Geophysical Research Letters, 47, e2020GL089871. https://doi.org/10.1029/2020GL089871