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Late Quaternary strata and carbon burial records in the Yellow River delta, China

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Abstract

Sediment carbon sequestration plays an essential role in mitigating atmospheric CO2 increases and the subsequently global greenhouse effect. To clarify the late Quaternary strata and carbon burial records in Yellow River delta (YRD), detailed analysis of benthic foraminifera, total carbon (TC), organic carbon (Corg), sedimentary characteristics and moisture contents of sediments, was performed on core ZK3, 30.3 m in length and obtained from YRD in 2007. Eight depositional units (designated U1-U8 in ascending order) were identified. A comprehensive analysis method of historical geography and sedimentary geology was used to determine the precise depositional ages of the modern Yellow River delta (MYRD), from which pre-MYRD ages were deduced. The results indicates that the maximum burial rates of TC, inorganic carbon (IC) and Corg occurred in the delta front (U5), and the minimum in the shallow sea (U3). Remarkable high sedimentation rates in the MYRD are responsible for burial efficiency of carbon, with an average rate of Corg burial reaching 2087±251 g (m2 yr)−1, and that of IC reaching 13741±808 g (m2 yr)−1, which are much higher than those of other regions with high contents of Corg. Therefore, YRD has a significant burial efficiency for carbon sequestration.

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Authors and Affiliations

  1. College of Marine Geo-science, Ocean University of China, Qingdao, 266100, P.R. China

    Guangming Zhao & Guangxue Li

  2. The Key Laboratory of Coastal Wetlands Biogeosciences, China Geologic Survey, Qingdao, 266071, P.R. China

    Guangming Zhao, Siyuan Ye, Xigui Ding & Hongming Yuan

  3. The Key Laboratory of Marine Hydrocarbon Resource and Geology, Ministry of Land and Resources, Qingdao, 266071, P.R. China

    Guangming Zhao, Siyuan Ye, Xigui Ding & Hongming Yuan

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  1. Guangming Zhao
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  2. Siyuan Ye
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Correspondence to Siyuan Ye.

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Zhao, G., Ye, S., Li, G. et al. Late Quaternary strata and carbon burial records in the Yellow River delta, China. J. Ocean Univ. China 14, 446–456 (2015). https://doi.org/10.1007/s11802-015-2773-z

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  • DOI: https://doi.org/10.1007/s11802-015-2773-z

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