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Aislabie, Jackie; Bockheim, James G; McLeod, Malcolm; Hunter, David; Stevenson, Bryan; Barker, Gary M (2012): (Table I) Weathering stage and soil properties on drifts in the Lake Wellman area [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.806194, In supplement to: Aislabie, J et al. (2012): Microbial biomass and community structure changes along a soil development chronosequence near Lake Wellman, southern Victoria Land. Antarctic Science, 24(2), 154-164, https://doi.org/10.1017/S0954102011000873

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Coverage:
Latitude: -79.921170 * Longitude: 156.925190
Date/Time Start: 2007-12-03T00:00:00 * Date/Time End: 2007-12-21T00:00:00
Minimum ELEVATION: 854 m a.s.l. * Maximum ELEVATION: 1224 m a.s.l.
Event(s):
LakeWellman * Latitude: -79.921170 * Longitude: 156.925190 * Date/Time Start: 2007-12-03T00:00:00 * Date/Time End: 2007-12-21T00:00:00 * Location: Antarctica * Method/Device: Soil profile (SOIL)
Comment:
Depth of staining: thickness of the layers showing the strongest hues and chromas from oxidation of iron-bearing minerals and corresponds to the bottom of the Bw horizon; depth of coherence: thickness of consolidated soil from accumulation of weathering products such as salts and iron oxide; soil readily caves into the pit below the depth of coherence; depth of ghosts (pseudomorphs): depth to which highly weathered clasts can be observed in situ. This parameter varies with rock type as well as soil age; depth of visible salts: the maximum depth at which salts can be observed in a soil pit.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
NameNameAislabie, Jackieof drift
Sample IDSample IDAislabie, Jackieprofile number
Soil propertiesSoil propAislabie, Jackieweathering stage, see Campbell & Claridge (1975)
Soil propertiesSoil propAislabie, Jackiesalt stage, see Bockheim (1990)
Depth, relativeDepth relmAislabie, Jackiedepth to ice cement
Depth, relativeDepth relmAislabie, Jackiedepth of staining
Depth, relativeDepth relmAislabie, Jackiedepth of ghosts
Depth, relativeDepth relmAislabie, Jackiedepth of visible salts
Depth, relativeDepth relmAislabie, Jackiedepth of coherence
10 Soil typeSoil typeAislabie, JackieTHo = Typic Haplorthel, TAo = Typic Anhyorthel, and TAt = Typic Anhyturbel
11 ELEVATIONElevationm a.s.l.Geocode
12 StageStageAislabie, Jackie
Size:
176 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Name
(of drift)

Sample ID
(profile number)

Soil prop
(weathering stage, see Campbel...)

Soil prop
(salt stage, see Bockheim (1990))

Depth rel [m]
(depth to ice cement)

Depth rel [m]
(depth of staining)

Depth rel [m]
(depth of ghosts)

Depth rel [m]
(depth of visible salts)

Depth rel [m]
(depth of coherence)
10 
Soil type
(THo = Typic Haplorthel, TAo =...)
11 
Elevation [m a.s.l.]
12 
Stage
HathertonLW01110.460.000.000.01>0.46THo866Early Holocene
HathertonLW02110.510.000.000.01>0.51THo876Early Holocene
HathertonLW03110.500.000.000.01>0.50THo860Early Holocene
HathertonLW04110.350.000.000.010.35THo854Early Holocene
BritanniaLW05210.630.000.200.01>0.63THo980Late Wisconsin
BritanniaLW1221>0.760.080.050.09>0.76TAo971Late Wisconsin
BritanniaLW13210.490.090.260.01>0.49THo970Late Wisconsin
BritanniaLW1421>0.700.000.180.010.28TAt1038Late Wisconsin
DanumLW092.52>0.750.190.190.19>0.75TAo1204Marine isotope stage 6
DanumLW102.520.760.160.24>0.75>0.76TAo1200Marine isotope stage 6
DanumLW152.520.330.090.130.13>0.33THo1154Marine isotope stage 6
DanumLW16320.35>0.350.190.17>0.35THo1123Marine isotope stage 6
IscaLW06320.630.330.300.33>0.63THo1191Older than Danum
IscaLW07320.680.300.370.30>0.68THo1187Older than Danum
IscaLW08320.700.390.230.25>0.70THo1216Older than Danum
IscaLW112.820.400.120.180.12>0.40THo1224Older than Danum