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Data Publisher for Earth & Environmental Science

Todd, Claire E; Stone, John O; Conway, Howard; Hall, Brenda L; Bromley, Gordon RM (2010): (Table 2) Surface exposure ages of samples near the head of Reedy Glacier [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.786185, In supplement to: Todd, CE et al. (2010): Late Quaternary evolution of Reedy Glacier, Antarctica. Quaternary Science Reviews, 29(11-12), 1328-1341, https://doi.org/10.1016/j.quascirev.2010.02.001

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Coverage:
Median Latitude: -86.084608 * Median Longitude: -127.611130 * South-bound Latitude: -86.327980 * West-bound Longitude: -131.223370 * North-bound Latitude: -86.010130 * East-bound Longitude: -125.706600
Minimum ELEVATION: 1516 m a.s.l. * Maximum ELEVATION: 1988 m a.s.l.
Event(s):
Reedy_Glacier * Latitude: -86.000000 * Longitude: -131.000000 * Elevation Start: 1200.0 m * Elevation End: 2000.0 m * Location: Antarctica * Method/Device: Ice measurement (ICEM)
Comment:
Be-10 concentrations are based on Be isotopic measurements normalized to pre-2007 values of the KNSTD standard series. Multiply by 1.106 for values compatible with post-2007 normalization. See Nishiizumi et al. (2007, doi:10.1016/j.nimb.2007.01.297). Simple exposure ages assume a steady production rate; altitude corrections per Lal (1991, doi:10.1016/0012-821X(91)90220-C) as implemented in the CRONUS calculator (http://hess.ess.washington.edu/math/). Standard deviation = external errors including all known analytical and production rate contributions propagated at the ±1sigma level. Internal errors do not include contributions to uncertainty in the final exposure ages common to all samples, such as production rate and scaling errors. External errors should be used when comparing these ages to ages obtained with other dating methods. Internal errors should be used to assess the consistency of exposure ages at a given site. Range of exposure ages returned by the four paleomagnetically corrected production rate scaling methods implemented in the CRONUS calculator. As noted before, these ranges are appropriate for external comparisons with other dating methods, and should not be used to assess the internal consistency of ages from a given site.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Area/localityAreaTodd, Claire E
2Sample IDSample IDTodd, Claire E
3Sample commentSample commentTodd, Claire E
4LATITUDELatitudeGeocode
5LONGITUDELongitudeGeocode
6ELEVATIONElevationm a.s.l.Geocode
7CorrectioncorrTodd, Claire Ethickness
8CorrectioncorrTodd, Claire Ehorizon
9Beryllium-1010Be109 atoms/gTodd, Claire E
10Beryllium-10, standard deviation10Be std dev±Todd, Claire E
11Exposure ageExp agekaTodd, Claire Eexposure age
12Exposure age, standard deviationExp age std dev±Todd, Claire E1 sigma
13Exposure age, standard deviationExp age std dev±Todd, Claire Einternal uncertainty
14Exposure ageExp agekaTodd, Claire Eminimum
15Exposure ageExp agekaTodd, Claire Emaximum
Size:
324 data points

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