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Leipe, Christian; Demske, Dieter; Tarasov, Pavel E (2013): (Supplement Table 5) Revised chronology of the A/C ratio record from Sumxi Co [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.808955, In supplement to: Leipe, C et al. (2014): A Holocene pollen record from the northwestern Himalayan lake Tso Moriri: Implications for palaeoclimatic and archaeological research. Quaternary International, 348, 93-112, https://doi.org/10.1016/j.quaint.2013.05.005

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Related to:
Danzeglocke, Uwe; Weninger, Bernhard; Jöris, Olaf (2013): CalPal-2007. Cologne Radiocarbon Calibration & Palaeoclimate Research Package [webpage]. https://www.calpal-online.de/
van Campo, Elise; Cour, P; Sixuan, Hang (1996): Holocene environmental changes in Bangong Co basin (Western Tibet). Part 2: The pollen record. Palaeogeography, Palaeoclimatology, Palaeoecology, 120(1-2), 49-63, https://doi.org/10.1016/0031-0182(95)00033-X
van Campo, Elise; Gasse, Françoise (1993): Pollen- and Diatom-Inferred Climatic and Hydrological Changes in Sumxi Co Basin (Western Tibet) since 13,000 yr B.P. Quaternary Research, 39(3), 300-313, https://doi.org/10.1006/qres.1993.1037
Weninger, Bernhard; Jöris, Olaf (2008): A 14C age calibration curve for the last 60 ka: the Greenland-Hulu U/Th timescale and its impact on understanding the Middle to Upper Paleolithic transition in Western Eurasia. Journal of Human Evolution, 55(5), 772-781, https://doi.org/10.1016/j.jhevol.2008.08.017
Coverage:
Latitude: 34.623000 * Longitude: 80.270000
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 10.40 m
Event(s):
Sumxi_Co * Latitude: 34.623000 * Longitude: 80.270000 * Elevation: 5058.0 m * Location: Himalaya
Comment:
Revised chronology of the A/C ratio record from Sumxi Co (Van Campo and Gasse, 1993) based on the digitised A/C ratio values and radiocarbon dates (14C BP) from Van Campo and Gasse (1993) and Van Campo et al. (1996) which were calibrated with CalPal-2007 online using the CalPal-2007-Hulu calibration curve (Weninger and Jöris, 2008; Weninger et al., 2013). For the radiocarbon dates given in Van Campo et al. (1996) we assigned a universal uncertainty range of 100 years.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
AGEAgeka BPGeocode
Age, standard deviationAge std dev±Tarasov, Pavel E
Calendar ageCal ageka BPTarasov, Pavel EAge, 14C recalibrated, this study0 = modern
Confidence intervalCITarasov, Pavel EAge, 14C recalibrated, this study68 %
RatioRatioTarasov, Pavel Edigitised from Van Campo & Gasse (1993) and Van Campo et al. (1996)A/C ratio, where A = Artemisia %, and C = Chenopodiaceae %
Size:
382 data points

Data

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


Depth sed [m]

Age [ka BP]

Age std dev [±]

Cal age [ka BP]

CI

Ratio
0.000.0000.0001.40
0.100.1250.10.1460.1191.60
0.200.3250.10.3450.1252.90
0.300.4500.10.4570.0990.70
0.400.5500.10.5720.0672.20
0.500.7000.10.6580.0791.80
0.600.8500.10.8000.0902.20
0.751.0250.10.9410.1141.80
1.001.3000.11.1980.0982.40
1.101.4000.11.3100.0961.10
1.201.5500.11.4610.0963.30
1.301.7000.11.6150.1211.50
1.401.8000.11.7270.1172.40
1.501.9500.11.9060.1232.30
1.602.0500.12.0360.1221.60
1.752.3000.12.3400.1541.40
1.852.4000.12.5100.1481.90
1.952.6000.12.6570.1422.00
2.102.7000.12.8400.0961.30
2.202.8000.12.9490.1242.30
2.302.9500.13.1200.1392.40
2.403.0750.13.2560.1271.50
2.503.2000.13.4340.1163.10
2.603.3500.13.6050.1191.50
2.703.5000.13.7850.1262.00
2.803.6000.13.9170.1440.80
2.853.6500.13.9920.1361.20
2.903.7750.14.1670.1540.40
3.003.9000.14.3280.1430.90
3.104.0500.14.5890.1580.70
3.204.1750.14.6930.1270.90
3.304.3000.14.8780.1610.80
3.404.4250.15.0800.1592.30
3.504.5500.15.2200.1671.10
3.604.7500.15.4670.1111.25
3.804.8000.15.5060.1222.80
3.904.9000.15.6520.1251.80
4.004.9500.15.7290.1141.90
4.105.0000.15.7620.1081.40
4.205.0500.15.7930.1050.70
4.305.1250.15.8730.1171.50
4.405.2000.15.9770.1482.60
4.505.2750.16.0690.1153.10
4.605.3750.16.1480.1162.50
4.705.4000.16.1640.1173.50
4.805.4500.16.2170.1252.10
4.905.5250.16.3220.0982.60
5.005.5750.16.3870.0902.00
5.105.7000.16.5100.1113.60
5.205.7500.16.5550.1084.80
5.305.8000.16.6100.1143.00
5.405.9000.16.7290.1282.30
5.505.9500.16.7990.1202.40
5.606.1000.16.9900.1401.50
5.706.1500.17.0410.1263.30
5.906.2250.17.1230.1213.90
6.006.3250.17.2370.1274.60
6.106.4250.17.3440.0834.80
6.206.4500.17.3650.0845.50
6.306.6500.17.5340.0735.90
6.406.8500.17.7130.0934.40
6.507.0500.17.8660.0959.40
6.607.3000.18.1380.1097.20
6.707.4500.18.2630.0934.20
6.907.8000.18.6410.1493.20
7.008.1500.19.1200.1394.10
7.158.3750.19.3500.1195.70
7.258.5000.19.4810.0814.20
7.308.7000.19.7470.1507.40
7.408.9500.110.0360.1505.00
7.509.1000.110.3020.1139.30
7.609.3000.110.4910.1439.40
7.709.4500.110.7920.2026.70
7.809.6500.110.9870.1646.50
7.909.8500.111.3520.14610.60
8.0010.0000.111.5490.2057.00
8.1010.1000.111.6920.2430.60
8.2010.2000.111.8880.2470.40
8.3010.3000.112.1370.2690.60
8.4010.4000.112.3080.2140.70
8.5010.5000.112.4060.2050.30
8.6010.6500.112.5690.1521.00
8.7510.8000.112.7920.0991.80
8.9010.9500.112.8960.1121.10
9.0011.1000.113.0060.1420.70
9.1011.2500.113.1460.1340.90
9.3011.4000.113.3040.1550.60
9.4011.5000.113.3990.1400.70
9.5011.7000.113.5830.1571.05
9.6011.7750.113.6700.1640.70
9.7011.8500.113.7660.1600.45
9.8012.0000.113.9890.2320.40
9.9012.1000.114.1300.2650.60
10.0012.2000.114.2660.2740.90
10.1012.3000.114.4590.3611.10
10.4012.6000.114.9490.3210.70