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    孢粉证据揭示MIS5a以来福建东北沿海地区人类活动、海平面及气候变化

    于俊杰 彭博 兰佑 武彬 王继龙 丁大林 劳金秀 李帅丽 戴璐

    于俊杰, 彭博, 兰佑, 武彬, 王继龙, 丁大林, 劳金秀, 李帅丽, 戴璐, 2021. 孢粉证据揭示MIS5a以来福建东北沿海地区人类活动、海平面及气候变化. 地球科学, 46(1): 281-292. doi: 10.3799/dqkx.2019.264
    引用本文: 于俊杰, 彭博, 兰佑, 武彬, 王继龙, 丁大林, 劳金秀, 李帅丽, 戴璐, 2021. 孢粉证据揭示MIS5a以来福建东北沿海地区人类活动、海平面及气候变化. 地球科学, 46(1): 281-292. doi: 10.3799/dqkx.2019.264
    Yu Junjie, Peng Bo, Lan You, Wu Bin, Wang Jilong, Ding Dalin, Lao Jinxiu, Li Shuaili, Dai Lu, 2021. Palynological Record Revealed Anthropogenic Deforestation, Sea Level and Climate Changes since Marine Isotope Stage 5a in the Northeastern Coast of Fujian Province. Earth Science, 46(1): 281-292. doi: 10.3799/dqkx.2019.264
    Citation: Yu Junjie, Peng Bo, Lan You, Wu Bin, Wang Jilong, Ding Dalin, Lao Jinxiu, Li Shuaili, Dai Lu, 2021. Palynological Record Revealed Anthropogenic Deforestation, Sea Level and Climate Changes since Marine Isotope Stage 5a in the Northeastern Coast of Fujian Province. Earth Science, 46(1): 281-292. doi: 10.3799/dqkx.2019.264

    孢粉证据揭示MIS5a以来福建东北沿海地区人类活动、海平面及气候变化

    doi: 10.3799/dqkx.2019.264
    基金项目: 

    中国地质调查局“宁德海岸带陆海统筹综合地质调查”项目 DD20189505

    详细信息
      作者简介:

      于俊杰(1983-), 男, 高级工程师, 主要从事海岸带与第四纪地质调查、研究工作.ORCID:0000-0002-8493-178X.E-mail:25320701@qq.com

      通讯作者:

      戴璐, ORCID:0000-0002-5883-9752.E-mail:dailu@nbu.edu.cn

    • 中图分类号: P532

    Palynological Record Revealed Anthropogenic Deforestation, Sea Level and Climate Changes since Marine Isotope Stage 5a in the Northeastern Coast of Fujian Province

    • 摘要: 通过获取了位于福建省宁德市海岸带的两个钻孔,并使用孢粉分析的方法来重建古环境.光释光和放射性碳十四测年结果表明,钻孔中最老的沉积物来自于深海氧同位素(MIS5a)阶段.孢粉组合中,海相沟鞭藻出现在MIS5a,MIS3早期和早、中全新世阶段,反映了这些时段的海侵事件.MIS5a以来,孢粉组合受控于常绿栎(Quercus)和松属(Pinus),指示了周边地区一直被亚热带阔叶林和松林所覆盖,表现了偏暖的亚热带气候.因此,孢粉证据揭示了末次盛冰期时该地区不存在大幅度的降温.芒萁属孢子和草本花粉的剧增指示了晚全新世以来宁德地区人类活动对天然植被的破坏.

       

    • 图  1  中国东部植被区划(a)以及钻孔位置(b)

      图a中:Ⅰ.温带草原; Ⅱ.温带落叶阔叶林; ⅢA.北亚热常绿-落叶阔叶混交林; ⅢB.中亚热带常绿阔叶林; ⅢC.南亚热带常绿阔叶林; ⅣA.北热带季雨林和热带雨林; ⅣB.南热带季雨林和热带雨林; 下部3个钻孔表示图 5中所引用的钻孔的位置; 区划图数据吴征镒(1980); 图a中的红框表示图b中所显示的福建省宁德市的地理位置

      Fig.  1.  Vegetation regionalization in eastern China (a) and location of sample sites (b)

      图  2  NDGK2孔与NDQK5孔中孢粉和藻类的浓度及地层对比

      底部数字单位为粒/克

      Fig.  2.  Stratigraphy and concentration of pollen, concentricystes and marine dinocysts of cores NDGK2, NDQK5

      图  3  NDGK2钻孔主要花粉类型百分比图

      花粉百分比基于总花粉数量,孢子百分比基于花粉和孢子总数, 底部数字单位为%; 在Quercus中,D代表落叶,E代表常绿; 阴影表示高海平面阶段

      Fig.  3.  Percentage of major pollen taxa of core NDGK2

      图  4  NDQK5钻孔主要花粉类型百分比图

      花粉百分比基于总花粉数量,孢子百分比基于花粉和孢子总数; 底部数字单位为%; 在Quercus中,D代表落叶,E代表常绿; 阴影表示高海平面阶段

      Fig.  4.  Percentage of major pollen taxa of core NDQK5

      图  5  南海北部3个钻孔松属花粉百分比与区域海平面重建的对比

      MD05-2906孔数来自Dai et al.(2015); MD05-2904孔数据来自常琳等(2013); STD235孔数据来自Yu et al.(2017); 海平面数据来自Geyh et al.(1979)Hanebuth et al.(2011)

      Fig.  5.  Comparison between Pinus pollen percentages of three cores in the northern South China Sea and reconstruction of regional sea-level

      图  6  全球平均相对海平面重建及福建沿海地区高海平面时段

      黑色棒和虚线框长度对应于下部年代,分别指示了本研究和他人研究揭示的高海平面时段(王绍鸿等,1994; 马明明等,2016).全球平均相对海平面重建结果修改自文献Rohling et al.(2014)

      Fig.  6.  Reconstruction of global sea-level and high sea-level intervals in coasts of Fujian Province

      表  1  NDGK2和NDQK5钻孔的AMS 14C测年结果

      Table  1.   AMS 14C and OSL dating samples and ages

      样品号 深度(m) 样品 AMS 14C年代(a B.P.) 树轮校正后的年代范围2σ(95.4%)(a B.P.)
      NDGK2 14C-1 8.00 植物残体 580±20 641~589
      NDGK2 14C-2 14.70 4 580±20 5 323~5 284
      NDGK2 14C-3 20.90 碳化植物残体 2 230±20 2 270~2 155
      NDGK2 14C-4 24.90 片状贝壳碎片 8 195±25 9 258~9 032
      NDGK2 14C-5 25.75 贝壳碎屑 8 225±25 9 290~9 090
      NDGK2 14C-5-2 25.75 植物残体 7 995±25 8 999~8 770
      NDGK2 14C-6 31.85 碳化植物残体 14 450±35 17 811~17 450
      NDGK2 14C-7 33.10 碳化植物残体 36 320±230 41 485~40 408
      NDGK2 14C-8 35.10 碳化植物残体 > 43 320 超过测试范围
      NDGK2 14C-9 39.00 碳化植物残体 33 960±180 38 885~38 001
      NDQK5 14C-1 7.35 6 560±25 7 508~7 426
      NDQK5 14C-2 12.47 7 330±35 8 200~8 024
      NDQK5 14C-3 13.40 7 365±25 8 220~8 154
      NDQK5 14C-4 18.90 双壳 8 120±35 9 134~8 993
      NDQK5 14C-5 22.90 泥炭 22 280±70 26 852~26 206
      NDQK5 14C-6 23.60 碳化植物残片 29 660±120 34 061~33 586
      NDQK5 14C-7 30.10 碳化植物残体 41 500±300 45 541~44 376
      NDQK5 14C-8 34.35 炭化木块 > 43 320 超过测试范围
      NDQK5 14C-9 36.70 炭化植物根茎 > 43 320 超过测试范围
      下载: 导出CSV

      表  2  NDGK2和NDQK5钻孔的光释光测年结果

      Table  2.   NDGK2 and NDQK514C OSL dating results of the borehole

      样品编号 深度(m) Th (10-6) error (10-6) U (10-6) error (10-6) 年龄(ka) 误差(ka) 粒径(µm)
      NDGK2-OSL-2 41.20~41.30 3.85 2.61 3.16 3.54 92.2 7.4 38~63
      NDGK2-OSL-3 46.90~47.00 0.15 0.15 0.15 0.15 38~63
      NDGK2-OSL-4 48.90~49.00 1.05 1.40 1.44 1.95 64.8 6.3 38~63
      NDGK2-OSL-5 53.30~53.40 0.06 0.06 0.06 0.06 92.2 6.9 38~63
      NDGK2-OSL-6 54.45~54.55 11.90 11.40 10.30 18.30 67.0 8.2 38~63
      NDQK5-OSL-2 32.90~33.00 1.05 1.40 1.44 1.95 64.5 4.7 38~63
      NDQK5-OSL-3 42.90~43.00 11.90 11.40 10.30 18.30 7.4 2.9 38~63
      NDQK5-OSL-4 46.90~47.00 11.90 11.40 10.30 18.30 36.8 0.7 38~63
      下载: 导出CSV
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    • 收稿日期:  2019-10-21
    • 刊出日期:  2021-01-15

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