Journal
FRONTIERS IN EARTH SCIENCE
Volume 10, Issue -, Pages -Publisher
FRONTIERS MEDIA SA
DOI: 10.3389/feart.2022.648337
Keywords
seafloor sediments; TOC; organic carbon isotope; TN; offshore of the Leizhou Peninsula
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Funding
- Special Talent Support Program of Guangdong Ocean University [R17001]
- Project of Enhancing School with Innovation of Guangdong Ocean University [GDOUQ18301]
- First-class special Funds of Guangdong Ocean University [231419029]
- Project of Marine geochemistry and climate change of Guangdong Ocean University [002026002004]
- Fund of Southern Marine Science and Engineering Guangdong Laboratory (Zhanjiang) [ZJW-2019-08]
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A study was conducted to analyze seafloor sediments from the offshore region surrounding the Leizhou Peninsula. The results showed lower organic carbon content compared to other offshore regions in China, indicating a dominant marine authigenic source. The abundance and distribution of organic matter were influenced by various factors.
A total of 43 seafloor surface sediment samples collected from the offshore region surrounding the Leizhou Peninsula were analyzed in terms of the total organic carbon content (TOC), total nitrogen (TN), organic carbon isotope (delta C-13(org)) and sediment grain size. Our results showed that the organic carbon content in the samples ranged from 0.12 to 0.79%, with an average of 0.42% which was lower compared with other offshore regions of China, whereas the delta C-13(org) was in the range of -22.47 parts per thousand to -19.18 parts per thousand. The total nitrogen content ranged from 0.011 to 0.100% which was also low. The combination of delta C-13(org) and TOC/TN ratio (5.1-14.3) suggested that the organic matter is dominant by marine authigenic source input, as marine sourced organic matter accounts for 71%, 82%, and 75% in the sediments from the offshore areas of the east side, west side and the south (Qiongzhou Strait) of the Leizhou Peninsula, respectively. The weak/poor correlations between the organic carbon and clay, silt content, the pH and Eh value suggested that organic matter abundance and distribution were influenced by the source input of organic matter, the seafloor sediments' redox status, and seawater's hydrodynamic condition.
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