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Download Article (PDF) Open Geosci. 2019; 11:1061–1070 Research Article Rediat Abate, Changping Chen, Junrong Liang, Lin Sun, Xuesong Li, Bangqin Huang, and Yahui Gao* Decadal variations of total organic carbon production in the inner-shelf of the South China Sea and East China Sea https://doi.org/10.1515/geo-2019-0082 Received Apr 20, 2019; accepted Nov 25, 2019 1 Introduction Abstract: Organic carbon content is one of the major prox- In coastal and marine systems, the deposition of organic ies of aquatic primary production and implication of envi- matter and the ratio of TOC:TN is mainly influenced by ronmental changes. However, there is a scarcity of infor- both the supply of organic matter from overlaying water mation regarding the decadal variation of organic carbon mass, settlement velocity of organic matter onto sea floor production in inner-shelf of South China Sea (SCS) and and diagenetic process that acting on the organic matter East China Sea (ECS). To bridge this gap of information after settlement/deposition [1]. The relationship between two sediment cores were collected from the inner shelf of Total Organic Carbon (TOC) content (wt%) and Total Nitro- SCS (Leizhou Peninsula) and ECS. Then, Total Organic Car- gen (TN) content (wt%) has been used as an indicator of bon (TOC), Total Inorganic Carbon (TIC) and Total Nitro- marine Organic Matter (OM) productivity as well terrestrial gen (TN) content were examined. The TOC content in the OM input for more than half a century [2]. High TOC:TN Leizhou Peninsula averaged 0.56% and varied from 0.35% (molar weight), values greater than 20, are characteristic to 0.81%. At decadal time scale, the TOC content of Leizhou of terrestrial vegetation due to carbon-rich (and nitrogen- Peninsula erratically increased in the last century, and it poor) biochemical classes (i.e., lignin and cellulose) [3]. distinctly peaked after 1990’s. This is related to increased Whereas, marine algae typically have TOC:TN ratios be- primary production due to the increased input of anthro- tween 4 and 8, due to their cell content is rich in proteins pogenic nutrients and rainfall level. The TOC content of and lack cellulose [3]. the inner shelf of ECS averaged 0.5% and varied narrowly The East China Sea and South China Seas are being from 0.46% to 0.53%. The TOC:TN ratio of ECS averaged among the largest marginal western Pacific seas located 5.65 and varied from 4.42 to 7.85, indicating there is high de- in South East Asia; they are more prone to human pertur- gree of organic matter degradations. The TN:TP ratios were bations and climate changes. Furthermore, the impact of below 10 for the periods before late-1990’s, indicating that disturbances highly aggravated because they are found in there had been a potential nitrogen limitation in the inner one of the most densely populated areas of the world with shelf of ECS. Generally, this study showed that the TOC and TIC of ECS and SCS inner-shelf had undergone substantial changes in the last century. China; Key Laboratory of the Ministry of Education for Coastal and Keywords: anthropogenic impact, climate change, Wetland Ecosystem, College of Environment & Ecology, Xiamen decadal variation, diatoms, environment, inner shelf, phy- University, Xiamen 361102, China; College of Natural Science, Arba toplankton production, organic matter production Minch University, Arba Minch PO Box 21, Ethiopia Changping Chen, Junrong Liang: School of Life Sciences and State Key Laboratory of Marine Environmental Science, Xiamen Univer- sity, Xiamen 361102, China; Key Laboratory of the Ministry of Educa- *Corresponding Author: Yahui Gao: School of Life Sciences and tion for Coastal and Wetland Ecosystem, College of Environment & State Key Laboratory of Marine Environmental Science, Xiamen Ecology, Xiamen University, Xiamen 361102, China University, Xiamen 361102, China; Key Laboratory of the Ministry of Lin Sun, Xuesong Li: School of Life Sciences and State Key Labora- Education for Coastal and Wetland Ecosystem, College of Environ- tory of Marine Environmental Science, Xiamen University, Xiamen ment & Ecology, Xiamen University, Xiamen 361102, China; Email: 361102, China [email protected] Bangqin Huang: Key Laboratory of the Ministry of Education for Rediat Abate: School of Life Sciences and State Key Laboratory of Coastal and Wetland Ecosystem, College of Environment & Ecology, Marine Environmental Science, Xiamen University, Xiamen 361102, Xiamen University, Xiamen 361102, China Open Access. © 2019 R. Abate et al., published by De Gruyter. This work is licensed under the Creative Commons Attribution 4.0 License 1062 Ë R. Abate et al. fast economic growth and urbanization. As consequent of so, recent data showed evident environmental contami- this, high nutrient inputs especially nitrogen from agricul- nation and degradation along the coast [18]. Particularly, tural and aquaculture activities [4–6] and construction of rapid expansion and booming of land and marine aqua- dams [7, 8] were reported in ECS and SCS. These ultimately culture, increasing of agricultural crop production by us- resulted in changes of Chlorophyll a concentrations [9], ing excessive artificial fertilizer, industrialization and un- nutrient levels [10], sediment supply to coastal zones and treated sewage disposal are among the main causes of the water discharges [8], eutrophication and hypoxia [11], red problems [19]. The detail description of ECS and SCS has tide frequency [12], primary production [13] and probably been explored [20, 21] (Figure 1). organic matter content as well. However, there are lim- ited scientific research reports on the decadal changes of the organic matter content in the inner shelf of ECS and 2.2 Sediment process and dating SCS. Thus, this research was aimed to bridge this gap of knowledge by setting two main objectives: 1) To analyze To assess recent decadal changes of sediment organic mat- the decadal variation of total organic carbon content and ter; two sediment cores were collected from the inner-shelf total nitrogen in the inner shelf of ECS and SCS and 2) To ex- of ECS and SCS. The first sediment core was collected from amine the decadal change of the ratio of total organic car- the inner-shelf of northwestern SCS (Leizhou, Zhanjiang) bon to total nitrogen content of the inner shelf of ESC and Peninsula coast at 20∘85.7650 N and 111∘18.168330E, from SCS. For this purpose, two sediment core samples were col- about 38m water depth, in 2012. Leizhou Peninsula is sur- lected from the inner-shelf of ECS and SCS followed by the rounded by Hainan Island from south next to Qiongzhou analysis of total organic carbon and total nitrogen content Strait, the coast of China from north and SCS from south, of the sediments; then the data were correlated with cli- and is drained by two large rivers, mainly the Red River mate change and anthropogenic impact variables. from the southwest and Pearl River from the northeast. The second sediment core was collected from inner-shelf ECS near to Yangtze River Estuary (YRE) at N 28∘26.15910and E 122∘11.07450, from 43m water depth, in 2011. The sediment 2 Material and methods samples were collected by gravity corer onboard the R/V Dongfanghong II. The sediment core showed gray to black 2.1 Study area color. After collection, the sediment sample slabs were ex- truded and sliced at 2 cm intervals and approximately 0.5 The East China Sea (ECS) is the largest continental cm of the outer rim of each sediment slab was trimmed marginal sea in the Western North Pacific [14, 15] and is off to minimize contamination between layers. Sediment one of the most developed shelf areas in the world. The dating was made by the α-spectrometry 210Pb (via 210Po) wide and shallow continental shelf favors primary produc- method [14, 22]. The detail of processing of the sediments tion through frequent replenishment of nutrients to the eu- and dating the chronologies has been reported [20, 21]. photic zone from a deeper layer [16]. The study site was lo- cated in the inner-shelf area of ECS, which is characterized by the distribution of fine-grained sediments manifested 2.3 Analyses of TOC, TN, Sulphur and by the dispersal of a plume from the Yangtze [17]. An im- Phosphorus mense amount of terrigenous and anthropogenic material flows into ECS from different river basins, and as a result, In the laboratory, 1 g of sediment subsamples were pre- it supports high biological production [16] (Figure 1). The treated; dried for 48 hours at 65∘C and finely ground. To South China Sea is one of the largest continental marginal measure the TOC, pre-treated samples were transferred seas of the Pacific Ocean, found in the western North Pa- into glass vials and acidified with 1M of HCl at room tem- cific surrounded by lands and islands which provide an perature for 12h to remove carbonates [23]. Then, the sam- ample amount of terrigenous material. The surface circu- ples re-dried and finely ground. Separate unacidified sam- lation is governed by East Asia monsoon systems which ples were used to measure TN, TC and total sulphur (TS). drive the cyclonic gyre during winter and anticyclonic gyre To measure the TC, TOC, TN and TS contents, approxi- in summer. Consequently, there is strong seasonality in pri- mately 25 mg of samples were weighed, foiled by tin cap- mary productivity and the organic material reaching the sules and loaded into CHNS elemental analyser (Vario EL sea floor. Although this area is regarded as one of the less- III, ElementarAnalysensysteme GmbH), with analysis ac- developed coastal areas of China until the last decade or curacy of ≤ 0.3% absolute (5mg benzene sulfonic acid) Decadal variations of total organic carbon production in the inner-shelf Ë 1063 Figure 1: Location of the study site of the East China Sea and the South China Sea, and description of the legend depicted on the bottom of the right side and ≤ 0.5% absolute (3mg benzoic acid).
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