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福建沿海全新世相对海平面变化:地质记录与“冰川-水均衡调整”(GIA)模拟对比

王龙 王张华 李翠玉

王龙,王张华,李翠玉. 福建沿海全新世相对海平面变化:地质记录与“冰川-水均衡调整”(GIA)模拟对比[J]. 海洋学报,2022,44(x):1–15 doi: 10.12284/hyxb2022065
引用本文: 王龙,王张华,李翠玉. 福建沿海全新世相对海平面变化:地质记录与“冰川-水均衡调整”(GIA)模拟对比[J]. 海洋学报,2022,44(x):1–15 doi: 10.12284/hyxb2022065
Long Wang,Zhanghua Wang,Cuiyu Li. Holocene relative Sea-level change of Fujian Coast, Southeastern China:Geological records and comparison with Glacio-hydro isostatic adjustment (GIA) modelling[J]. Haiyang Xuebao,2022, 44(x):1–15 doi: 10.12284/hyxb2022065
Citation: Long Wang,Zhanghua Wang,Cuiyu Li. Holocene relative Sea-level change of Fujian Coast, Southeastern China:Geological records and comparison with Glacio-hydro isostatic adjustment (GIA) modelling[J]. Haiyang Xuebao,2022, 44(x):1–15 doi: 10.12284/hyxb2022065

福建沿海全新世相对海平面变化:地质记录与“冰川-水均衡调整”(GIA)模拟对比

doi: 10.12284/hyxb2022065
基金项目: 国家留学基金委基金(CSC No.201806140081)
详细信息
    作者简介:

    王龙(1988-),男,博士研究生,陕西省宝鸡市人,主要从事全新世相对海平面变化方向研究。E-mail:arlenwang0109@gmail.com

    通讯作者:

    王张华,女,教授,博士生导师,主要从事河口三角洲地貌演化、晚第四纪海平面变化方向研究。E-mail:zhwang@geo.ecnu.edu.cn

Holocene relative Sea-level change of Fujian Coast, Southeastern China:Geological records and comparison with Glacio-hydro isostatic adjustment (GIA) modelling

  • 摘要: 重建高质量的全新世相对海平面变化曲线,可为海岸带人类社会科学预测及应对未来海平面上升风险,提供重要的地质历史依据和长时间尺度的数据参考。福建海岸带已发表了多条全新世相对海平面变化曲线,然而已有曲线反映的相对海平面变化历史,存在较大差异,甚至是矛盾结果。同时,相对海平面长期变化机制及影响因素也不明确。本研究收集、整理了福建沿海已发表的全新世相对海平面数据,对已有数据的年代、高程、指示意义等属性信息进行重新检查和校正,根据国际方法体系,建立了该区域一个标准化的全新世“相对海平面数据库”,共包括海平面数据183个。在此基础上,采用“变量误差–综合高斯(EIV-IGP)”统计学模型,提出了一条新的福建沿海全新世相对海平面变化曲线。并应用“冰川–水均衡调整”(GIA)理论,开展了相对海平面变化GIA模拟。最后,综合相对海平面变化地质记录及GIA模拟结果,得出以下结论:(1)福建沿海11.28~7.08 ka,相对海平面由–23.55±6.94 m快速连续上升至–1.51±1.80 m;7.08~4.08 ka,相对海平面由–1.51±1.80 m缓慢上升至约1.09±1.38 m;3.48 ka前后,相对海平面高于现代海平面约1.35±1.23 m。此后,波动下降并逐渐接近现代位置。(2)“冰川–水均衡调整”作用是福建全新世相对海平面变化的主要长期作用机制。11.28~7.00 ka,相对海平面变化主要受冰盖融水控制;7.00 ka以来,“水均衡调整”作用逐渐占据主导。(3)福建沿海中–晚全新世(6.75~0.16 ka)期间,存在高于现今海面位置的“高海平面”现象。不同于传统构造运动主导观点,研究认为GIA引起的“陆地掀斜”和“海洋虹吸”作用,可能是该区域“高海平面”现象产生的主要原因。(4)福建沿海全新世相对海平面变化,存在一定程度的空间差异。不同岸段之间的沉积物压实、差异性构造运动和潮差变化等非GIA因素,可能是这一现象产生的重要原因。
  • 图  1  研究区概况图

    a. 东亚板块边界分布;b. 福建海岸带全新世相对海平面数据空间分布及分区;c. 福建沿海已发表的全新世相对海平面变化曲线[11-19]

    Fig.  1  Map of the study area

    a. Locations of East Asia and the plate boundary;b. distribution of Holocene relative sea-level data along the Fujian coast and sub-zone;c. published Holocene relative sea-level curves from Fujian coast[11-19]

    图  2  福建沿海全新世“相对海平面数据库”数据统计

    Fig.  2  Statistics of Holocene relative sea-level database of Fujian coast

    图  3  福建沿海各亚区全新世相对海平面数据点及相对海平面变化曲线

    a. 宁德;b. 福州–平潭;c. 莆田–泉州;d. 厦门–漳州

    Fig.  3  Holocene relative sea level data and sea-level curve of each subzone on Fujian coast

    a. Ningde;b. Fuzhou-Pingtan;c. Putian-Quanzhou;d. Xiamen-Zhangzhou

    图  4  福建沿海全新世区域性相对海平面变化曲线与临近区域相对海平面曲线[87, 89]及全球冰融等效海平面曲线(IESL)[23, 30]对比

    Fig.  4  Comparison of Fujian regional Holocene relative sea-level curve with geological records[87, 89] from adjacent area and Global IESL curves[23, 30]

    图  5  福建沿海全新世相对海平面指示点(SLIP)数据与GIA模拟结果(理论RSL曲线、IESL曲线)对比

    a. 宁德;b. 福州-平潭;c. 莆田-泉州;d. 厦门-漳州

    Fig.  5  Comparison of SLIP with RSL curve and IESL curve at each subzone of Fujian coast

    a. Ningde; b. Fuzhou-Pingtan; c. Putian-Quanzhou;d. Xiamen-Zhangzhou

    表  1  福建海岸带全新世相对海平面标志物及其指示意义

    Tab.  1  Indicative meaning of Holocene sea level indicators on Fujian coast

    数据类型海平面标志物指示意义(IM)
    参考水位(RWL)指示范围(IR)
    指示点数据(SLIP)海滩岩(海滩型)(HAT+MLW)/2HAT-MLW
    贝壳堤(底部)(MSHW+MNHW)/2MSHW-MNHW
    牡蛎礁(MTL+MSLW)/2MTL-MSLW
    埋藏红树林(MSHW+MSLW)/2MSHW-MSLW
    盐沼泥炭(HAT+MNHW)/2HAT-MNHW
    潮滩淤泥(MSHW+MSLW)/2MSHW-MSLW
    潮间带沉积(上部)(MSHW+MTL)/2MSHW-MTL
    潮间带沉积(下部)(MTL+MSLW)/2MTL-MSLW
    陆地约束数据(TL)海滩岩(沙堤型)MTL>MTL
    贝壳堤MTL>MTL
    淡水泥炭MTL>MTL
    河湖相沉积MTL>MTL
    埋藏古树MTL>MTL
    海洋约束数据(ML)海相贝壳、牡蛎壳(原位)MTL<MTL
    河口砂坝MTL<MTL
    河口湾沉积MTL<MTL
    潮下带淤泥MTL<MTL
    浅海相及海相沉积MTL<MTL
    下载: 导出CSV
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  • 收稿日期:  2021-09-23
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