Sample Number* |
Lab Number† |
δ13C‡ | 14C Age (yr B.P.)§ |
Calibrated Years B.P.‖ | Comments |
---|---|---|---|---|---|
047 | 136442 | −25 | 4395±30 | 4870–5045 | Faulted Holocene sediments |
051 | 136443 | −25 | 3970±30 | 4300–4520 | Faulted and tilted Holocene sediments |
072 | 136444 | −25 | 1745±35 | 1550–1770 | Faulted Holocene sediments |
074 | 136445 | −25 | 2670±40 | 2740–2850 | Faulted Holocene sediments |
075 | 136446 | −25 | 1045±30 | 920–1050 | Holocene sediments (unfaulted?) |
076 | 136447 | −25 | 4165±35 | 4580–4830 | Faulted Holocene sediments |
080 | 136448 | −25 | 4450±35 | 4890–5290 | Faulted Holocene sediments |
*Sample locations are shown in Figure S3.
†Analyses from the Center for Accelerator Mass Spectrometry (CAMS), Lawrence Livermore National Laboratory, Livermore, California.
‡Δ13C assumed to be −25/00.
§Conventional radiocarbon age, expressed as years before 1950. Calculations assume a Libby half-life (5568 yr). Uncertainties are one standard deviation counting errors.
‖Dendrochronologically calibrated calendar-age ranges using the atmospheric decadal dataset of Reimer et al., 2009, two-sigma uncertainty, rounded to nearest decade. Calibration accomplished using CALIB, version 6 (Stuiver and Reimer, 1993) Rev. 6. (see Data and Resources section). B.P. is defined as before 1950.
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