Cheng, Zhongjing; Weng, Chengyu; Steinke, Stephan; Mohtadi, Mahyar (2019): Pollen percentages, Charcoal flux, Mg/Ca-based SST and Benthic foraminiferal δ18O records of site GeoB16602. PANGAEA, https://doi.org/10.1594/PANGAEA.897555, 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, https://doi.org/10.1038/s41561-018-0250-1
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Vegetation dynamics during previous warm interglacial periods shed light on the human impacts on natural ecosystems during the Holocene. However, reliable terrestrial records that span such periods are rare and provide little information on regional scale. Here we present a high-resolution marine pollen record from the northern South China Sea, which reveals that during five peak interglacial periods, Marine Isotope Stages 13a, 11c, 9c, 5e and 1 (the Holocene), the vegetation successions in southern China were similar. At the beginning of each interglacial period, tropical rainforest conifers, which include Dacrydium, Dacrycarpus and Podocarpus, and associated broadleaved taxa, such as Altingia, expanded quickly at the expense of the subtropical/temperate montane conifer Pinus. Near the end of the warm periods, Pinus recovered and the tropical taxa retreated. However, the Holocene displays subtle but significant differences in which the species turnover was interrupted and the rainforest conifers did not fully expanded. The Mg/Ca-based sea surface temperature record from the same site reveals that temperature was the major control of the rise and fall of the peak interglacial vegetation. However, exceptionally high charcoal fluxes during the Holocene suggest that human activities through land-use modifications completely, and possibly permanently, altered the natural vegetation trend five to six thousand years ago.
Median Latitude: 18.951143 * Median Longitude: 113.709333 * South-bound Latitude: 18.951000 * West-bound Longitude: 113.709000 * 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
Datasets listed in this publication series
- Cheng, Z; Weng, C; Steinke, S et al. (2019): (Table S1) Radiocarbon ages and calendar ages of sediment cores GeoB16602-3 and GeoB16602-4. https://doi.org/10.1594/PANGAEA.897550
- Cheng, Z; Weng, C; Steinke, S et al. (2019): Macrocharcoal flux of composite sediment core GeoB16602. https://doi.org/10.1594/PANGAEA.897544
- Cheng, Z; Weng, C; Steinke, S et al. (2019): Mg/Ca based SST record of composite sediment core GeoB16602. https://doi.org/10.1594/PANGAEA.897471
- Cheng, Z; Weng, C; Steinke, S et al. (2019): Pollen and spores of composite sediment core GeoB16602. https://doi.org/10.1594/PANGAEA.897546
- Cheng, Z; Weng, C; Steinke, S et al. (2019): δ¹⁸O benthic foraminifera curve of composite sediment core GeoB16602. https://doi.org/10.1594/PANGAEA.897508