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应用生态学报 ›› 2026, Vol. 37 ›› Issue (9): 3041-3052.doi: 10.13287/j.1001-9332.202609.053

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滤食性双壳贝类养殖区沉积有机碳的再矿化与埋藏:机制与争议

曹英昆1,5, 刘建霞1,5, 马福堂1,5, 刘梦瑶1,5, 张继红2, 杨斌3, 李丽4, 潘哲1,5*   

  1. 1河北农业大学海洋学院, 河北秦皇岛 066000;
    2中国水产科学研究院黄海水产研究所, 山东青岛 266071;
    3江苏海洋大学, 自然资源部滨海盐沼湿地生态与资源重点实验室/江苏省海洋生物技术重点实验室, 江苏连云港 222005;
    4中国海洋大学, 山东青岛 266000;
    5河北省水产营养调控与疾病防控重点实验室, 河北秦皇岛 066000
  • 收稿日期:2026-05-31 接受日期:2026-08-12 出版日期:2026-09-18 发布日期:2026-10-12
  • 通讯作者: *E-mail: lfpanzhe@163.com
  • 作者简介:曹英昆, 女, 1986年生, 博士研究生, 讲师。主要从事水域生态学研究。E-mail: yingkun-cao@163.com
  • 基金资助:
    国家自然科学基金项目(32503188)、河北省自然科学基金优秀青年基金项目(C2023204161)和河北省高等学校科学研究项目(QN2026778)

Remineralization and burial of sedimentary organic carbon in filter-feeding bivalve aquaculture areas: Mechanisms and controversies.

CAO Yingkun1,5, LIU Jianxia1,5, MA Futang1,5, LIU Mengyao1,5, ZHANG Jihong2, YANG Bin3, LI Li4, PAN Zhe1,5*   

  1. 1Ocean College of Hebei Agricultural University, Qinhuangdao 066000, Hebei, China;
    2Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, Shandong, China;
    3Key Laboratory of Coastal Salt Marsh Ecosystems and Resources, Ministry of Natural Resources/Jiangsu Key Laboratory of Marine Biotechnology, Jiangsu Ocean University, Lianyungang 222005, Jiangsu, China;
    4Ocean University of China, Qingdao 266000, Shandong, China;
    5Hebei Key Laboratory of Aquatic Nutrition Regulation and Disease Control, Qinhuangdao 066000, Hebei, China
  • Received:2026-05-31 Accepted:2026-08-12 Online:2026-09-18 Published:2026-10-12

摘要: 滤食性双壳贝类养殖通过滤食、选择性摄食和生物沉积作用,增强颗粒有机碳(POC)向海底输送,并改变沉积有机碳(SOC)的来源、通量和反应性。然而,养殖诱导的新增有机碳具有“高输入-高反应性-高不确定性”特征,进入沉积物后,一部分经微生物再矿化或再悬浮与横向输送重新进入水体,另一部分则通过快速掩埋、矿物保护和微生物再加工等过程获得稳定化并形成长期埋藏。POC沉降增强能否形成净沉积碳汇,取决于新增有机碳在再矿化释放、物理输出、阶段性保存和长期埋藏之间的分配。当前争议的核心在于,POC沉降增加或海底表层SOC累积能否说明双壳贝类养殖对沉积碳汇有贡献:仅以沉降量或SOC增量判断可能高估其增汇效应,而仅强调再矿化损失则可能低估。本文围绕SOC的“输入-再矿化-稳定化与埋藏”,综述滤食性双壳贝类养殖条件下SOC的转化过程及其控制机制,厘清其形成长期SOC埋藏增量从而构成净沉积碳汇的条件。未来应加强各过程及时间尺度的同步观测与耦合核算,明确不同双壳贝种类、养殖模式和环境条件下SOC的埋藏效率及其影响因素,建立双壳贝类养殖沉积碳汇判定框架。

关键词: 滤食性双壳贝类养殖, 沉积有机碳, 生物沉积, 再矿化, 长期埋藏, 碳汇判定

Abstract: Filter-feeding bivalve aquaculture enhances the transport of particulate organic carbon (POC) to the seafloor through filtration, selective feeding, and biodeposition, thereby altering the sources, fluxes, and reactivity of sedimentary organic carbon (SOC). However, aquaculture-induced organic carbon inputs are characterized by “high input, high reactivity, and high uncertainty”. After entering the sediment, a fraction is returned to the water column through microbial remineralization, resuspension, and lateral transport, whereas another fraction is stabilized through rapid burial, mineral protection, and microbial reworking, which is ultimately retained through long-term burial. Whether enhanced POC sedimentation results in a net sedimentary carbon sink therefore depends on the partitioning of newly added organic carbon among remineralization, physical export, transient preservation, and long-term burial. The current debate centers on whether increased POC sedimentation or SOC accumulation in surface sediments can demonstrate a contribution of bivalve aquaculture to sedimentary carbon sequestration. Assessments based solely on sedimentation fluxes or SOC increments may overestimate the carbon-sink effect, whereas an exclusive emphasis on remineralization losses may underestimate the contribution of stabilization and long-term burial. Following the process sequence of “input-remineralization-stabilization and burial”, we synthesized the transformation processes and controlling mechanisms of SOC in filter-feeding bivalve aquaculture systems and clarified the conditions under which aquaculture-induced organic carbon inputs could generate a long-term positive increment in SOC burial and thereby constitute a net sedimentary carbon sink. Future studies should strengthen synchronous observations and coupled accounting of these processes across relevant timescales, quantify SOC burial efficiency and its influencing factors among different bivalve species, farming practices, and environmental conditions, and establish a framework for assessing sedimentary carbon sinks in bivalve aquaculture.

Key words: filter-feeding bivalve aquaculture, sedimentary organic carbon, biodeposition, remineralization, long-term burial, carbon-sink assessment