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Strobel, Paul; Henning, Theresa; Bliedtner, Marcel; Mosher, Stella G; Rahimova, Humay; Haberzettl, Torsten; Kirsten, Kelly L; Lehndorff, Eva; Power, Mitchell J; Zech, Michael; Zech, Roland (2023): Coupled isotopes in Holocene sediments from the Vankervelsvlei peatland at the southern Cape coast of South Africa [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.956464, In: Strobel, P et al. (2023): Holocene fire dynamics and their climatic controls at Vankervelsvlei, southern Cape coast, South Africa [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.956477

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Published: 2023-03-13DOI registered: 2024-01-03

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Keyword(s):
charcoal; Paleoclimate; paleofire; Polycyclic aromatic hydrocarbons; precipitation; relative humidity; Stable isotopes
Related to:
Strobel, Paul; Bliedtner, Marcel; Carr, Andrew S; Struck, Julian; Du Plessis, Nadia; Glaser, Bruno; Meadows, Michael E; Quick, Lynne J; Zech, Michael; Zech, Roland; Haberzettl, Torsten (2022): Reconstructing Late Quaternary precipitation and its source on the southern Cape coast of South Africa: A multi-proxy paleoenvironmental record from Vankervelsvlei. Quaternary Science Reviews, 284, 107467, https://doi.org/10.1016/j.quascirev.2022.107467
Funding:
German Research Foundation (DFG), grant/award no. 434918595: Late Quaternary climate and environmental reconstruction based on lake and peat sediments from South Africa
Coverage:
Latitude: -34.013000 * Longitude: 22.904000
Minimum Elevation: 152.0 m * Maximum Elevation: 152.0 m
Event(s):
Vankervelsvlei * Latitude: -34.013000 * Longitude: 22.904000 * Elevation: 152.0 m * Recovery: 15 m * Location: South Africa * Method/Device: Piston corer, UWITEC (PCUWI) * Comment: Samples were taken in 2016.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
AGEAgeka BPStrobel, PaulAges model according to Strobel et al. (2022)Geocode – Median age
Sugar, δ18OSugar δ180‰ SMOWStrobel, PaulGas Chromatograph (GC), Agilent Technologies, 7890B; measured with 18O-pyrolysis reactor, Thermo Fisher Scientific; coupled with Interface, Thermo Fisher Scientific, ConFlo IVvs. VSMOW
Sugar, δ18O, standard deviationSugar δ18O std dev±Strobel, PaulGas Chromatograph (GC), Agilent Technologies, 7890B; measured with 18O-pyrolysis reactor, Thermo Fisher Scientific; coupled with Interface, Thermo Fisher Scientific, ConFlo IVvs. VSMOW
δ Deuterium, leaf waterδD leaf water‰ SMOWStrobel, PaulCalculated after Zech et al., (2013)vs. VSMOW
δ Deuterium, leaf water, standard deviationδD leaf water std dev±Strobel, PaulCalculated after Zech et al., (2013)vs. VSMOW
δ Deuterium, source waterδD source water‰ SMOWStrobel, PaulCalculated after Zech et al., (2013)vs. VSMOW
δ Deuterium, source water, standard deviationδD source water std dev±Strobel, PaulCalculated after Zech et al., (2013)vs. VSMOW
Humidity, relativeRH%Strobel, PaulCalculated after Zech et al., (2013)Reconstructed
Deuterium excessd xsStrobel, PaulCalculated after Zech et al., (2013)
10 Deuterium excess, standard deviationd xs std dev±Strobel, PaulCalculated after Zech et al., (2013)
11 Reference/sourceReferenceStrobel, Paul
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
640 data points

Data

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


Age [ka BP]

Sugar δ180 [‰ SMOW]

Sugar δ18O std dev [±]

δD leaf water [‰ SMOW]

δD leaf water std dev [±]

δD source water [‰ SMOW]

δD source water std dev [±]

RH [%]

d xs []
10 
d xs std dev [±]
11 
Reference
-0.05331.550.47-26.94.43-68.27-10.4461.4-60.993.72
-0.03135.721.71-24.98.49-82.81-12.3345.9-90.2613.18
-0.01031.180.02-4.94.07-32.21-5.7674.5-36.202.30
0.01630.310.35-15.63.22-45.31-7.4672.3-40.412.85
0.04132.430.65-24.15.29-67.54-10.3459.4-64.745.01
0.06731.350.25-28.74.23-70.22-10.6961.2-61.282.15
0.09828.600.70-13.81.56-35.26-6.1580.0-25.815.45Strobel et al., 2022
0.23530.590.56-22.63.50-57.50-9.0467.5-49.534.46
0.25732.360.23-30.25.22-76.95-11.5756.4-70.452.47
0.28633.030.10-36.35.87-89.28-13.1750.6-81.491.06
0.32731.180.11-24.44.07-62.82-9.7364.2-55.781.31
0.36931.150.05-30.04.04-71.44-10.8561.3-61.131.35
0.41130.600.50-30.23.51-69.47-10.5963.4-57.234.00Strobel et al., 2022
0.58128.401.10-30.81.36-61.07-9.5071.8-41.338.62Strobel et al., 2022
1.21030.280.01-28.33.19-65.11-10.0365.7-52.891.01
1.22828.500.26-25.41.46-52.91-8.4474.3-36.593.62
1.25234.200.50-23.07.01-73.38-11.1053.0-76.963.88Strobel et al., 2022
1.29428.490.51-20.71.45-45.59-7.4976.8-31.864.04
1.33128.480.24-9.91.44-28.58-5.2882.5-20.952.26
1.38429.870.00-12.62.80-38.80-6.6175.6-34.160.80
1.47028.610.31-31.41.57-62.89-9.7470.6-43.493.82
1.54629.300.29-21.62.24-50.35-8.1173.1-38.792.86
1.62729.840.88-24.52.77-57.32-9.0269.4-45.856.76
1.71230.500.40-17.63.41-49.29-7.9770.4-43.863.27Strobel et al., 2022
1.80429.880.24-11.12.80-36.41-6.3076.4-32.672.54
1.88329.220.59-16.02.16-41.24-6.9376.4-32.585.01
1.96725.390.35-19.9-1.56-31.16-5.6289.5-7.834.04
2.04529.090.25-18.92.04-45.37-7.4675.3-34.622.19
2.21032.600.60-14.45.45-53.17-8.4863.8-56.394.96Strobel et al., 2022
2.28028.100.14-25.01.07-50.66-8.1576.1-33.253.18
2.71435.900.30-19.68.67-75.37-11.3648.0-86.372.48Strobel et al., 2022
2.85828.010.18-17.90.98-39.08-6.6580.2-25.393.30
3.38231.150.06-24.34.04-62.49-9.6964.3-55.410.83
3.51524.710.41-28.7-2.23-42.08-7.0487.5-11.554.35
3.65129.300.30-32.92.24-68.06-10.4167.2-50.106.15Strobel et al., 2022
3.76029.370.06-25.42.30-56.60-8.9270.8-43.101.57
3.87228.630.13-13.01.59-34.10-6.0080.3-25.221.16
3.98233.500.60-24.96.33-73.39-11.1054.7-73.6210.65Strobel et al., 2022
4.05526.971.66-37.5-0.03-65.43-10.0773.9-37.2513.13
4.13033.730.32-24.26.56-73.26-11.0954.2-74.653.82
4.19528.920.41-22.41.87-50.03-8.0774.2-36.753.26
4.31031.600.00-30.04.48-73.34-11.1059.6-64.491.10Strobel et al., 2022
4.38531.130.57-27.14.03-66.89-10.2662.9-58.145.33
4.44928.050.22-25.51.03-51.21-8.2276.0-33.382.20
4.51330.290.10-26.43.20-62.19-9.6566.6-51.091.09
4.58225.460.12-30.8-1.50-48.58-7.8883.4-19.263.61
4.64725.641.51-28.7-1.32-46.01-7.5583.8-18.5011.66
4.71230.080.94-44.33.00-89.25-13.1658.0-67.357.82
4.77932.700.20-29.25.55-76.71-11.5355.6-71.901.78Strobel et al., 2022
4.83226.910.61-28.7-0.09-51.37-8.2478.8-27.984.79
4.88525.302.00-32.7-1.66-50.90-8.1883.1-19.9915.47Strobel et al., 2022
4.94725.311.36-23.9-1.65-37.14-6.4087.7-11.2510.47
5.02830.340.25-33.03.25-72.66-11.0163.0-58.033.58
5.27930.800.50-22.73.70-58.58-9.1866.6-51.233.93Strobel et al., 2022
5.36227.350.23-23.90.35-45.82-7.5279.6-26.591.90
5.45031.091.00-15.53.98-48.42-7.8669.3-46.127.85
5.54328.700.10-23.31.66-50.60-8.1474.6-36.081.18Strobel et al., 2022
5.62130.181.30-13.13.10-40.86-6.8874.1-36.9510.43
5.71428.700.60-10.21.66-30.09-5.4881.5-22.985.12Strobel et al., 2022
5.79528.790.243.91.74-8.29-2.6588.6-9.492.42
5.96327.100.40-13.90.10-29.08-5.3585.9-14.683.73Strobel et al., 2022
6.05726.650.53-24.8-0.34-44.13-7.3081.9-22.134.11
6.16028.700.0012.31.665.14-0.9093.4-0.480.60Strobel et al., 2022
6.34830.580.56-23.33.49-58.59-9.1867.1-50.195.27
6.44128.820.61-33.91.77-67.69-10.3668.5-47.564.74
6.53229.100.20-10.42.04-31.98-5.7279.8-26.103.64Strobel et al., 2022
6.63427.930.65-17.90.91-38.76-6.6180.5-24.846.20
6.72928.100.50-20.61.07-43.77-7.2678.4-28.844.82Strobel et al., 2022
6.83427.950.40-41.20.92-75.37-11.3668.1-48.294.31