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CHEN Hao, HE Lei, YE Siyuan, HAN Zongzhu, YUAN Hongming, Edward A. Laws. 2022. Differentiation of sedimentary environment and its carbon sequestration rate since the Late Pleistocene in the Luanhe River Delta, northern Bohai Bay[J]. Geology in China, 49(5): 1555-1570. doi: 10.12029/gc20220513
Citation: CHEN Hao, HE Lei, YE Siyuan, HAN Zongzhu, YUAN Hongming, Edward A. Laws. 2022. Differentiation of sedimentary environment and its carbon sequestration rate since the Late Pleistocene in the Luanhe River Delta, northern Bohai Bay[J]. Geology in China, 49(5): 1555-1570. doi: 10.12029/gc20220513
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Differentiation of sedimentary environment and its carbon sequestration rate since the Late Pleistocene in the Luanhe River Delta, northern Bohai Bay

  • 1. School of Marine Geosciences, Ocean University of China, Qingdao 266003, Shandong, China;

  • 2. Key Laboratory of Coastal Wetland Biogeology, China Geological Survey, Qingdao Institute of Marine Geology, Qingdao 266071, Shandong, China;

  • 3. Qingdao National Laboratory of Marine Science and Technology, Laboratory of Marine Geological Process and Environmental Function, Qingdao 266061, Shandong, China;

  • 4. School of coast and environment, Louisiana State University, Baton Rouge 70803-4110, USA

More Information
  • Corresponding author: YE Siyuan  
Received Date:  13 March 2020
Revised Date:  21 May 2020
    Abstract
  • This paper is the result of marine and environmental geological survey engineering.
    [Objective] Carry out the differentiation of the sedimentary environments since the Late Pleistocene in the Luanhe River Delta, northern Bohai Bay, calculate and analyze the magnitude and controlling factors of the carbon sequestration rate (CSR), and further evaluate the regional carbon storage capacity. [Methods] In this paper, the reconstruction of the paleo- sedimentary environment since the Late Pleistocene was carried out on the core of hole BXZK03, and the parameters including particle size, age (AMS14C and OSL), water content, organic carbon, total carbon and other nutrients contents were sampled and analyzed. [Results] Since the Late Pleistocene, the strata were divided from bottom to top into five sedimentary environmental units, including flood plain, sand ridge, shallow sea, barrier sand bar (delta front), and lagoon. The CSRs were in the order of barrier sand bar 51.47 g/(m2 · a)> beach sand ridge 32.59 g / (m2 · a)> shallow sea 7.82 g/(m2 · a)> lagoon 4.66g / (m2 · a). Correlation analysis showed that there was a significant (P <0.01) linear correlation between total carbon, organic carbon and each nutrient element. Variance analysis suggested that CSRs were likely controlled by the deposition rate and carbon concentration, respectively. [Conclusions] Although the organic carbon concentrations of sediments in Luanhe River Delta were relatively low, there were relatively high organic CSRs due to an elevated deposition rate during Holocene. Therefore the Holocene sediment has a remarkable carbon storage capacity.
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