Journal of Tropical Oceanography ›› 2026, Vol. 45 ›› Issue (5): 162-177.doi: 10.11978/2025224CSTR: 32234.14.2025224

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Distribution characteristics of biomarker components and their environmental indications at Well NK-1 on Meiji Atoll, Nansha Islands*

ZHU Xiaowei1,2(), MO Ziyi1,2,3, MAO Shengyi4, TIAN Yuhang1,2,5, LUO Yun1,2, MIAO Li1,2, XU Weihai1,2, LI Gang1,2, YAN Wen1,2,3()   

  1. 1 South China Sea Institute of Oceanology, State Key Laboratory of Tropical Oceanography, Guangzhou 511458, China
    2 South China Sea Institute of Oceanology, Laboratory of Ocean and Marginal Sea Geology, Guangzhou 511458, China
    3 University of Chinese Academy of Sciences, Beijing 100049, China
    4 Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences, Key Laboratory of Gas Hydrate, Guangzhou 510640, China
    5 Hainan Key Laboratory of Marine Geological Resources and Environment, Haikou 570206, China
  • Received:2025-11-26 Revised:2026-01-14 Online:2026-09-10 Published:2026-10-13
  • Contact: YAN Wen. email: wyan@scsio.ac.cn
  • Supported by:
    National Key Research and Development Program of China(2021-06); National Natural Science Foundation of China(42373029); National Natural Science Foundation of China(42306076); National Natural Science Foundation of China(42176079); National Natural Science Foundation of China(42376079); General Program of Natural Science Foundation of Guangdong Province(2024A1515012382); General Program of Natural Science Foundation of Guangdong Province(2025A1515010958); Hainan Marine Geological Resources and Environment Key Laboratory Open Fund(24-HNHYDZZYHJKF047)

Abstract:

Coral reefs have developed extensively in the South China Sea, and their growth records preserve diverse information on marine climate and environmental changes, making them a crucial environmental archive. This study focuses on the Well NK-1 site on Meiji Atoll, systematically analyzing the composition and distribution of lipid biomarkers within coral reef carbonate rocks, with emphasis on the potential of short- and medium-chain C14-18 fatty acids for reconstructing paleoproductivity and their environmental implications. The results indicate that these fatty acids exhibit high resistance to diagenesis and degradation, and are closely correlated with terrestrial nutrient input, surface-water productivity, and sea-level changes, thus serving as reliable proxies for reconstructing the paleoproductivity records of reef-building corals. Furthermore, aliphatic hydrocarbon assemblages with petroleum hydrocarbon signatures were identified in the 45-65 m and 95-110 m stratigraphic intervals. Integrating the regional tectonic setting and chronological data of Meiji Reef, these assemblages are inferred to be products of natural hydrocarbon seepage events during the Middle-Late Pleistocene, potentially triggered by the oblique arc-continent collision in the Taiwan region of China. This study reveals the environmental recording capacity of coral reef areas in the South China Sea, showing that they can respond to paleoproductivity on a millennial scale, while also providing new geochemical evidence for abrupt natural hydrocarbon seepage events.

Key words: Meiji Atoll, biomarkers, productivity indicators, southern South China Sea

CLC Number: 

  • P734.43