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Cheng, Zhongjing; Weng, Chengyu; Steinke, Stephan; Mohtadi, Mahyar (2019): (Table S1) Radiocarbon ages and calendar ages of sediment cores GeoB16602-3 and GeoB16602-4. PANGAEA,, In supplement to: Cheng, Z et al. (2018): Anthropogenic modification of vegetated landscapes in southern China from 6,000 years ago. Nature Geoscience, 11, 939-943,

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Median Latitude: 18.951750 * Median Longitude: 113.710667 * South-bound Latitude: 18.951667 * West-bound Longitude: 113.710667 * North-bound Latitude: 18.951833 * East-bound Longitude: 113.710667
Date/Time Start: 2012-05-29T05:18:00 * Date/Time End: 2012-05-29T06:26:00
Minimum DEPTH, sediment/rock: 0.005 m * Maximum DEPTH, sediment/rock: 5.620 m
GeoB16602-3 * Latitude: 18.951833 * Longitude: 113.710667 * Date/Time: 2012-05-29T05:18:00 * Elevation: -955.0 m * Campaign: SO221 (INVERS) * Basis: Sonne * Method/Device: MultiCorer (MUC) * Comment: 10/10
GeoB16602-4 * Latitude: 18.951667 * Longitude: 113.710667 * Date/Time: 2012-05-29T06:26:00 * Elevation: -955.0 m * Campaign: SO221 (INVERS) * Basis: Sonne * Method/Device: Gravity corer (GC) * Comment: 9.7m
a: Measured at the Keck Carbon Cycle Accelerator Mass Spectrometry Facility (UCIAMS), Earth System Science Department, University of California, Irvine, United States of America.
b: All raw radiocarbon dates were converted to 2Sigma calendar ages with the CALIB 7.1 software using the MARINE13 calibration dataset without a further adjustment for a regional 14C reservoir age (ΔR, deviation from the average global reservoirage of 400 years).
c: 2Sigma enclosing 95.4% of probability distribution.
d: The sample contains excess 14C from post AD 1950 atmospheric thermonuclear weapons tests.
129 data points

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