Corrigendum: Loess Plateau storage of Northeastern Tibetan Plateau-derived Yellow River sediment
نویسندگان
چکیده
The original version of this Article contained errors in the Supplementary Information files: Zircon U-Pb age results for sample 23, shown in Supplementary Fig. 3, are incorrect, and missing from Supplementary Data 1, while several identification labels relating to Yellow River Lanzhou terraces samples are missing from Supplementary Data 2. Supplementary Data 1 and 2 have now been updated to provide the missing information, while the corrected version of Supplementary Fig. 3 appears below. DOI: 10.1038/ncomms10831 OPEN
منابع مشابه
Loess Plateau storage of Northeastern Tibetan Plateau-derived Yellow River sediment
Marine accumulations of terrigenous sediment are widely assumed to accurately record climatic- and tectonic-controlled mountain denudation and play an important role in understanding late Cenozoic mountain uplift and global cooling. Underpinning this is the assumption that the majority of sediment eroded from hinterland orogenic belts is transported to and ultimately stored in marine basins wit...
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Reply: this statement was indeed based on the observed data at two gauge stations: one located at the outlet of Chinese loess plateau and named Huayuankou station; another was located at the estuary of yellow river and named Lijin station (Figure 1 and 9 in MS). In 1950s condition, we estimated that soil erosion mobilized, in total, ca. 8.21 ± 3.44 Tg C yr-1 which consistent with the observatio...
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