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  • Research progress on the mechanism of sedimentary carbon sink in delta-shelf systems
    FAN Daidu, ZHANG Qiaowen, WU Yijing, SU Jianfeng, WEI Bingbing, NI Sha

    The sediment source-to-sink system serves as a critical link connecting active carbon pools (e.g., atmosphere, biosphere, hydrosphere) with the stable lithospheric carbon pool, playing a core buffering role in the global carbon cycle. As the core area of marine sedimentary carbon sinks, delta-shelf regions account for over 80% of the global marine sedimentary organic carbon flux while occupying less than 8% of the global ocean area. The processes and mechanisms of carbon burial in these regions are crucial for global carbon balance. This paper systematically reviews the source composition and sedimentary flux characteristics of terrestrial organic carbon in delta-shelf sedimentary systems, focuses on elaborating organic carbon source-to-sink tracing technologies, remineralization processes and their dominant mechanisms, analyzes the impacts of human activities on sedimentary carbon sinks, and discusses marine negative emission and carbon sequestration enhancement schemes based on sediment management. Studies show that the heterogeneity of terrestrial organic carbon, physicochemical conditions of the sedimentary environment, and human disturbance collectively regulate the migration, transformation, and burial efficiency of organic carbon. Currently, the potential of sedimentary carbon sinks has not been fully exploited; thus, it is urgent to promote the integration of sedimentary carbon sinks into the global climate governance system through methodological innovation, mechanism deepening, and technological development, so as to provide scientific support and feasible paths for achieving the temperature control goals of the Paris Agreement.

  • Deep-water sedimentary processes and organic carbon burial effects
    SU Ming, MA Wenbin, LUO Kunwen, GAO Ya, OU Hejie

    Deep-water sedimentary processes are key drivers that shape seafloor topography and actively participate in marine material cycles, thereby playing a crucial role in the formation of depositional systems and material cycling along continental margins and within deep-sea basins. The transport and transformation of carbon elements and carbon-containing substances are essential for sustaining organic life and maintaining climate stability. As an important end-member reservoir in this cycle, deep-sea sediments act as efficient sinks for atmospheric greenhouse gases, exerting significant regulatory effects on climate evolution over geological timescales. This study aims to elucidate the coupling mechanisms between distinctive deep-water sedimentary processes and organic carbon burial, providing a theoretical basis for establishing the “Shelf edge-slope-deep sea basin organic matter continuous transport system” and the “Deep-water organic carbon burial pyramid model”. By comprehensively analyzing representative deep-water organic carbon burial systems in global ocean basins, this research demonstrates that turbidity currents and bottom currents are the main dynamic mechanisms enabling the continuous transport of deep-water organic matter. The (micro)biological carbon pump, turbidity current carbon pump, bottom current carbon pump, and deep stratigraphic carbon pump together form the core framework for deep-water sedimentary carbon burial. Furthermore, the factors influencing deep-water organic carbon burial outcomes exhibit hierarchical characteristics. However, current research on deep-water organic carbon burial is still in its early stages, with limited case studies and mechanistic understanding, underscoring the urgent need to strengthen research on carbon burial processes in deep-water environments.

  • Distribution, sources and burial flux of black carbon in marine sediments
    WANG Jialun, YU Zenghui, HU Limin, BAI Yazhi, YU Wenxiu, CHONG Weini, ZHOU Jiawen, RAN Xue, BAI Jinming

    Black carbon (BC), a refractory organic carbon, is produced during the incomplete combustion of biomass and fossil fuels. Globally, an estimated 3%-10% of the annual BC production ultimately buried in marine sediments. As a critical component of the inert carbon pool, its spatiotemporal distribution and source-to-sink processes are essential for understanding global carbon cycling and climate evolution. Based on published BC data from nearly 1 000 marine sediment samples worldwide, this study reveals that BC contents vary widely, from 0.02 to 9.72 mg/g, with averaging 1.06 mg/g and accounting for an average of 15.1% of total sedimentary organic carbon. Spatial patterns are controlled by sediment grain size, organic carbon content, and depositional environments while temporal variations reflect the combined influence of climate change and human activities. Current knowledge of marine sedimentary BC sources predominantly assumes terrestrial dominance, with riverine transport, atmospheric deposition, and coastal erosion as primary input pathways. However, emerging evidence indicates that BC sinking fluxes in mid- to deep-ocean layers substantially exceed known terrestrial supply. This raises the possibility of potential unidentified sources. In addition, BC degradation and recycling processes within the marine systems remain poorly understood. Future research must prioritize source-to-sink dynamics in key areas (e.g., deep-sea environment) by integrating geochemical and organic molecular isotopic techniques to resolve BC cycling mechanisms and address current budget imbalances.

  • Progress and challenges of global continental shelves delineation beyond 200 nautical miles in the past three decades
    TANG Yong, YIN Jie, FANG Yinxia
    2026, 44(1):10-22. DOI:10.3969/j.issn.1001-909X.2026.01.001
    Abstract ( 12 ) HTML ( 12 ) PDF ( 3906KB ) ( 4 )   
  • Deep-sea mining at a crossroads: The new ISA Secretary-General assumes office and the profound implications for regulation development
    WU Guanghai, FU Quanyou, YAO Zichao, HAN Chenhua, GAO Farong
    2026, 44(1):23-29. DOI:10.3969/j.issn.1001-909X.2026.01.002
    Abstract ( 7 ) HTML ( 7 ) PDF ( 1003KB ) ( 3 )   
  • The icy sea as a canvas, life as a verse: A review of biogeochemistry in the Southern Ocean
    ZHAO Jun, HU Ji, ZHANG Haifeng, LI Dong, ZHU Changfeng, HAN Zhengbing, HU Chuanyu, PAN Jianming, ZHANG Haisheng
    2026, 44(1):30-47. DOI:10.3969/j.issn.1001-909X.2026.01.003
    Abstract ( 3 ) HTML ( 3 ) PDF ( 3929KB ) ( 3 )   
  • The United Nations “Ocean Decade”: Advancing a shared future for the ocean through global scientific collaboration
    WANG Yuntao, MAO Yangyang, WANG Zheng, JIANG Yue, KONG Mengle, WANG Pengbin, LIANG Yuyang
    2026, 44(1):48-65. DOI:10.3969/j.issn.1001-909X.2026.01.004
    Abstract ( 8 ) HTML ( 7 ) PDF ( 3369KB ) ( 6 )   
  • Identification and analysis of key issues in China’s marine protected areas from the perspective of land-sea differences
    ZENG Jiangning, LI Guodong, DONG Han
    2026, 44(1):66-73. DOI:10.3969/j.issn.1001-909X.2026.01.005
    Abstract ( 7 ) HTML ( 6 ) PDF ( 1225KB ) ( 3 )   
  • Review, problems and prospects of submarine cable and pipeline management policies in China
    HUANG Panyang, LAI Xianghua
    2026, 44(1):74-82. DOI:10.3969/j.issn.1001-909X.2026.01.006
    Abstract ( 7 ) HTML ( 6 ) PDF ( 1016KB ) ( 2 )   
  • Seasonal variability and its influencing factors of ocean bottom pressure in the Arabian Sea
    ZHANG Kun, ZHANG Tao, WU Binjie, ZHANG Deng, ZHENG Hua, DING Ruibin
    2026, 44(1):83-92. DOI:10.3969/j.issn.1001-909X.2026.01.007
    Abstract ( 3 ) HTML ( 3 ) PDF ( 4461KB ) ( 2 )   
  • Electrochemical sensors and their applications in marine environment detection: A panoramic view from coastal waters to deep-sea extremes
    HAN Chenhua, YAN Jiaojiao, DU Hao, ZHU Zhongmin, CHEN Jiawang, XU Chenlu, GAO Farong, ZHANG Chunfang, WU Guanghai
    2026, 44(1):93-108. DOI:10.3969/j.issn.1001-909X.2026.01.008
    Abstract ( 6 ) HTML ( 6 ) PDF ( 1831KB ) ( 3 )   
  • Applications of sapceborne synthetic aperture radar for ocean monitoring
    ZHU Ling, CHEN Peng, ZHENG Gang, YANG Jinsong, ZHU Haitian, REN Lin
    2026, 44(1):109-123. DOI:10.3969/j.issn.1001-909X.2026.01.009
    Abstract ( 4 ) HTML ( 4 ) PDF ( 3576KB ) ( 5 )   
  • Analysis of borehole CSEM response characteristics for seafloor massive sulfides
    GAO Yan, ZHOU Jianping, ZHU Zhongmin, TAO Chunhui
    2026, 44(1):124-135. DOI:10.3969/j.issn.1001-909X.2026.01.010
    Abstract ( 4 ) HTML ( 4 ) PDF ( 4038KB ) ( 0 )   
  • Study on water quality improvement strategies for small tropical lagoons under environmental capacity constraints: A case study of the Xiaohai Lagoon, Hainan
    XIANG Yunyun, FANG Xin, HOU Zonghao, YANG Hui, SUN Zhaochen, SU Binwei, ZHANG Yifei
    2026, 44(1):136-148. DOI:10.3969/j.issn.1001-909X.2026.01.011
    Abstract ( 10 ) HTML ( 10 ) PDF ( 4574KB ) ( 3 )   
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