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):
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):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Name | Name | Aislabie, Jackie | of drift | ||
2 | Sample ID | Sample ID | Aislabie, Jackie | profile number | ||
3 | Soil properties | Soil prop | Aislabie, Jackie | weathering stage, see Campbell & Claridge (1975) | ||
4 | Soil properties | Soil prop | Aislabie, Jackie | salt stage, see Bockheim (1990) | ||
5 | Depth, relative | Depth rel | m | Aislabie, Jackie | depth to ice cement | |
6 | Depth, relative | Depth rel | m | Aislabie, Jackie | depth of staining | |
7 | Depth, relative | Depth rel | m | Aislabie, Jackie | depth of ghosts | |
8 | Depth, relative | Depth rel | m | Aislabie, Jackie | depth of visible salts | |
9 | Depth, relative | Depth rel | m | Aislabie, Jackie | depth of coherence | |
10 | Soil type | Soil type | Aislabie, Jackie | THo = Typic Haplorthel, TAo = Typic Anhyorthel, and TAt = Typic Anhyturbel | ||
11 | ELEVATION | Elevation | m a.s.l. | Geocode | ||
12 | Stage | Stage | Aislabie, Jackie |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
176 data points
Data
1 Name (of drift) | 2 Sample ID (profile number) | 3 Soil prop (weathering stage, see Campbel...) | 4 Soil prop (salt stage, see Bockheim (1990)) | 5 Depth rel [m] (depth to ice cement) | 6 Depth rel [m] (depth of staining) | 7 Depth rel [m] (depth of ghosts) | 8 Depth rel [m] (depth of visible salts) | 9 Depth rel [m] (depth of coherence) | 10 Soil type (THo = Typic Haplorthel, TAo =...) | 11 Elevation [m a.s.l.] | 12 Stage |
---|---|---|---|---|---|---|---|---|---|---|---|
Hatherton | LW01 | 1 | 1 | 0.46 | 0.00 | 0.00 | 0.01 | >0.46 | THo | 866 | Early Holocene |
Hatherton | LW02 | 1 | 1 | 0.51 | 0.00 | 0.00 | 0.01 | >0.51 | THo | 876 | Early Holocene |
Hatherton | LW03 | 1 | 1 | 0.50 | 0.00 | 0.00 | 0.01 | >0.50 | THo | 860 | Early Holocene |
Hatherton | LW04 | 1 | 1 | 0.35 | 0.00 | 0.00 | 0.01 | 0.35 | THo | 854 | Early Holocene |
Britannia | LW05 | 2 | 1 | 0.63 | 0.00 | 0.20 | 0.01 | >0.63 | THo | 980 | Late Wisconsin |
Britannia | LW12 | 2 | 1 | >0.76 | 0.08 | 0.05 | 0.09 | >0.76 | TAo | 971 | Late Wisconsin |
Britannia | LW13 | 2 | 1 | 0.49 | 0.09 | 0.26 | 0.01 | >0.49 | THo | 970 | Late Wisconsin |
Britannia | LW14 | 2 | 1 | >0.70 | 0.00 | 0.18 | 0.01 | 0.28 | TAt | 1038 | Late Wisconsin |
Danum | LW09 | 2.5 | 2 | >0.75 | 0.19 | 0.19 | 0.19 | >0.75 | TAo | 1204 | Marine isotope stage 6 |
Danum | LW10 | 2.5 | 2 | 0.76 | 0.16 | 0.24 | >0.75 | >0.76 | TAo | 1200 | Marine isotope stage 6 |
Danum | LW15 | 2.5 | 2 | 0.33 | 0.09 | 0.13 | 0.13 | >0.33 | THo | 1154 | Marine isotope stage 6 |
Danum | LW16 | 3 | 2 | 0.35 | >0.35 | 0.19 | 0.17 | >0.35 | THo | 1123 | Marine isotope stage 6 |
Isca | LW06 | 3 | 2 | 0.63 | 0.33 | 0.30 | 0.33 | >0.63 | THo | 1191 | Older than Danum |
Isca | LW07 | 3 | 2 | 0.68 | 0.30 | 0.37 | 0.30 | >0.68 | THo | 1187 | Older than Danum |
Isca | LW08 | 3 | 2 | 0.70 | 0.39 | 0.23 | 0.25 | >0.70 | THo | 1216 | Older than Danum |
Isca | LW11 | 2.8 | 2 | 0.40 | 0.12 | 0.18 | 0.12 | >0.40 | THo | 1224 | Older than Danum |