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(this will be filled in with additional sample and interpretive data)
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Table 3 from Burkett et al. (2016). Radiocarbon samples from an exposure in a cutbank along Slippery Creek. The exposure exhibits alluvial gravels capped by silt and a 10-15 cm thick organic-ric soil. The soil is overlain by a thin debris flow deposit. The entire sequence is faulted - illustrated by the folded/faulted buried soil and the scarp extending across the bouldery debris flow surface to the northeast. A single block sample was collected from the buried soil and subsamples of the individual organic fractions were collected and dated independently.
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Sample Name*
CAMS Lab Number†
14C Age (BP)§
Calibrated age
(cal BP)#
Sample material**
Sampled Unit
Submitted sample mass (mg)InterpretationEastingNorthing
Elevation (msl)
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MMRB01-A1661843130 ± 1403685 - 2960seeds? (a)buried soil4.3Inherited charred material59359670100421197
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MMRB01-B166185>ModernNAvery fine roots (b)buried soil13.49Modern roots59359670100421197
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MMRB01-C166186630 ± 70684 – 525
wood/twigs/old roots
buried soil2.8
Recent plant growth at time of debris flow
59359670100421197
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MMRB01-D ˠ1661873065 ± 253359 – 3210charcoal (c)buried soil13.1Inherited charcoal59359670100421197
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MMRB01-F1661883140 ± 603480 – 3182charcoal (c)buried soil11.7Inherited charcoal59359670100421197
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Note: Samples were picked from a block soil sample at the University of Kentucky and the sent to Lawrence Livermore National Laboratories Center for Accelerator Mass Spectrometry (LLNL CAMS) for AAA pretreatment.
* Site name codes: MMRB = Mt. McKinley Restraining Bend; 01 = block sample #1; A-F = organic fractions separated from the block sample.
†AMS analysis performed at LLNL CAMS.
§The quoted age is in radiocarbon years using the Libby half-life of 5568 years and following the conventions of Stuiver and Polach (1977). Sample preparation backgrounds have been subtracted, based on measurements of radiocarbon-dead standards pretreated in parallel with samples.
#Ages calibrated with Oxcal v4.2 (Bronk Ramsey, 2009a) using the IntCal 13 calibration curve (Reimer et al., 2013), with ages quoted at 2σ errors.
ˠ Sample was large enough to take a sample specific aliquot for 13C analysis
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** (a) black, charcoal-like spheres – possibly seeds. (b) collection of fine roots penetrating the buried soil horizon. (c) inherited charcoal preserved within the soil
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Unpublished radiocarbon data from a block sample collected from buried peaty soil exposed in a natural exposure near the Chedotlothna Glacier. 15-20 cm of fibrous, organic rich silt with silty sand laminae accumulated on top of a cobble-boulder glacial till. soil buried by ~1m of poorly sorted silt to coarse sand sheets that appear to blanket many of the surfaces in the area. These samples were delayed for a very long time at the lab, and samples 170562 and 170563 were run as duplicates, but reported miscommunication in the lab leads to some uncertainty about what these ages represent.
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Sample Name
CAMS Lab Number
d13Cfraction Modern±D14C±
14C Age (BP)§
±
Calibrated age
(cal BP)#
Sample material**
Sampled Unit
Submitted sample mass (mg)InterpretationEastingNorthing
Elevation (msl)
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MMRB hz.4*168499-32.570.74440.0026-255.62.6237030
woody macrofossils
buried soil25.485530566982875898
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MMRB hz.4 †168500-32.570.8810.0032-1193.2102030
woody macrofossils
buried soil25.485530566982875898
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MMRB hz.3*168501-28.670.94720.0027-52.82.743525
woody macrofossils
buried soil105.495530566982875898
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MMRB hz.3 dup
168502-28.670.95280.0025-47.22.539025
woody macrofossils
buried soil105.495530566982875898
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MMRB hz.2168503-280.95710.0036-42.93.635036
woody macrofossils
buried soil20.445530566982875898
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MMRB hz.1 *168505-27.190.98250.0025-17.52.514025
woody macrofossils
buried soil114.75530566982875898
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MMRB hz.1 dup
168506-27.190.97410.0028-25.92.821025
woody macrofossils
buried soil114.75530566982875898
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mmrb hz.1170562-27.190.95230.0034-47.73.439530
woody macrofossils
buried soil114.75530566982875898
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mmrb hz.1170563-27.190.95990.0029-40.12.933025
woody macrofossils
buried soil114.75530566982875898
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5530566982875898
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1) d13C values are the assumed values according to Stuiver and Polach (Radiocarbon, v. 19, p.355, 1977) when given without decimal places. Values measured for the material itself are given with a single decimal place. Samples with an (*) were large enough, and as requested, to take a sample specific split for IRMS d13C analysis.
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2) The quoted age is in radiocarbon years using the Libby half life of 5568 years and following the conventions of Stuiver and Polach (ibid.).
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3) Radiocarbon concentration is given as fraction Modern, D14C, and conventional radiocarbon age.
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4) Sample preparation backgrounds have been subtracted, based on measurements of samples of 14C-free coal. Backgrounds were scaled relative to sample size.
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5) Note, CAMS# 168500 (†) had a significantly smaller %C (~11%) relative to all of the other samples (35-60%)
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6) Assumed value of -28±2 for CAMS 168503 based on sample specific IRMS results.
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