全新世以来福建宁德地区环境演变及人类活动的孢粉记录

李帅丽, 王继龙, 彭博, 武彬, 于俊杰, 戴璐

李帅丽, 王继龙, 彭博, 武彬, 于俊杰, 戴璐. 全新世以来福建宁德地区环境演变及人类活动的孢粉记录[J]. 海洋地质与第四纪地质, 2021, 41(3): 170-181. DOI: 10.16562/j.cnki.0256-1492.2020102201
引用本文: 李帅丽, 王继龙, 彭博, 武彬, 于俊杰, 戴璐. 全新世以来福建宁德地区环境演变及人类活动的孢粉记录[J]. 海洋地质与第四纪地质, 2021, 41(3): 170-181. DOI: 10.16562/j.cnki.0256-1492.2020102201
LI Shuaili, WANG Jilong, PENG Bo, WU Bin, YU Junjie, DAI Lu. Palynological evidence for palaeoenviromental change and human activity in Ningde of Fujian Province during Holocene[J]. Marine Geology & Quaternary Geology, 2021, 41(3): 170-181. DOI: 10.16562/j.cnki.0256-1492.2020102201
Citation: LI Shuaili, WANG Jilong, PENG Bo, WU Bin, YU Junjie, DAI Lu. Palynological evidence for palaeoenviromental change and human activity in Ningde of Fujian Province during Holocene[J]. Marine Geology & Quaternary Geology, 2021, 41(3): 170-181. DOI: 10.16562/j.cnki.0256-1492.2020102201

全新世以来福建宁德地区环境演变及人类活动的孢粉记录

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:

    李帅丽(1993—),女,硕士研究生,人文地理学专业,E-mail:1811073011@nbu.edu.cn

    通讯作者:

    于俊杰(1983—),男,高级工程师,研究方向为海岸带与第四纪地质学,E-mail:25320701@qq.com

    戴璐(1981—),男,副教授,研究方向为第四纪孢粉学,E-mail:dailu@nbu.edu.cn

  • 中图分类号: P532

Palynological evidence for palaeoenviromental change and human activity in Ningde of Fujian Province during Holocene

  • 摘要: 分析了福建省宁德市东部海岸带地区NDQK2钻孔的42个孢粉样品。3个光释光和9个14C测年结果显示,钻孔沉积物年代跨越了末次冰消期晚期和全新世阶段。本文试图通过孢粉分析来重建宁德地区全新世以来的古环境演化,探讨古人类活动对天然植被演替的可能影响。本钻孔与该区域已发表的NDGK2和NDQK5孔的孢粉组合共同显示,深海氧同位素(MIS)5a阶段(约85 kaBP)至早全新世,周边陆地一直被亚热带常绿阔叶林和松林所覆盖,然而,约7770~4970 aBP期间以禾本科(Poaceae)为主的草本植物花粉和以芒萁属(Dicranopteris)为主的蕨类孢子含量剧增,孢粉组合与MIS5a以来的其他时段明显不同,类似于现代山地和海域表土孢粉组合。考虑到当地亚热带阔叶林被破坏后可形成以芒萁和禾本科为主的植被群落,我们认为宁德地区在7770~4970 aBP前就存在人类活动,并开始强烈影响森林组成,古人类砍伐树木导致分布于林缘与荒地的芒萁和禾本科等次生植被迅速扩张。基于东南沿海考古证据的时空分布对比,认为中、晚全新世本研究区周边古人类活动的出现可能与长江中下游古文明的迁移存在某种关联。
    Abstract: Analyzed by this paper are 42 pollen samples from the core of NDQK2, a 17.3 m long drilling core on the eastern coast of Ningde city, Fujian Province. Three optical stimulated luminescence (OSL) and nine AMS14C samples are dated. It is revealed that the core is made of with the deposits from Late Last Deglaciation and Holocene. Pollen are used as a major mean to reconstruct the Holocene palaeo-environment and to explore the possible impact of human activities on vegetation succession. Together with the published pollen data from adjacent cores of NDGK2 and NDQK5, it is found that subtropical evergreen broad-leaved forest and pine forest prevailed since marine isotope stage (MIS) 5a (~85 kaBP). However, Poaceae-dominated non-arboreal pollen component and Dicranopteris-dominated spores component increased sharply since 0.777~0.497 kaBP. The pollen assemblages are significantly different from other intervals of MIS5a, but similar to those in modern soils and marine sediments. If the expansion of Dicranopteris dichotoma and Poaceae plants is due to the destruction of subtropical broad-leaved forests by human activities, it suggests that human being had colonized in this region around 0.777~0.497 kaBP. The deforest by human being changed the natural forest composition, and resulted in the expansion of secondary plants such as Dicranopteris dichotoma and Poaceae distributed along the boarder of forest. The spatial and temporal distribution of archaeological evidence along southeast China indicates a possible link of human activities between the the study area and the migration of ancient culture from the lower Yangtze River during Mid-Late Holocene.
  • 图  1   研究区域位置图

    Figure  1.   Location map of the studied area

    图  2   宁德月降水量与月均温趋势图(1981—2010年)

    气候数据来源于中国气象数据网(http://data.cma.cn)。

    Figure  2.   Monthly precipitation and temperature in Ningde(1981—2010)

    Climatic data are from China Meteorological Data Service Center(CMDC)(http://data.cma.cn).

    图  3   NDQK2钻孔的地层和年代

    Figure  3.   Stratigraphy and ages of core NDQK2

    图  4   NDQK2钻孔主要花粉类型百分比及沟鞭藻浓度图

    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。

    Figure  4.   Percentage of major pollen taxa and concentration of marine dinocysts in core NDQK2

    The percentage of pollen is based on the total number of pollen, and the percentage of spores is based on the total number of pollen and spores. The unit of the bottom number is %.

    图  5   宁德表土花粉百分比图谱

    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。

    Figure  5.   Pollen percentage of surface samples in Ningde

    The percentage of pollen is based on the total number of pollen, and the percentage of spores is based on the total number of pollen and spores. The unit of the bottom number is %.

    图  6   NDGK2、NDQK5和NDQK2孔中主要孢粉组的百分比对比图

    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%。NDGK2和NDQK5钻孔的孢粉数据来自文献[37]。

    Figure  6.   Comparison of percentages of pollen group in cores NDGK2, NDQK5 and NDQK2

    The percentage of pollen is based on the total number of pollen, and the percentage of spores is based on the total number of pollen and spores. The unit of the bottom number is %. Pollen data from cores NDGK2 and NDQK5 are derived from ref.[37].

    图  7   东南沿海11000~4300 aBP遗址时空分布图

    Figure  7.   Temporal and spatial distributions of archaeological sites between 11000 and 4300 aBP in the southeast coast of China

    表  1   钻孔和现代表土采样点点位及样品类型描述

    Table  1   Description of modern topsoil sampling points and sample types

    样品编号海拔/m纬度 (N)经度 (E)样品类型
    NDQK2钻孔−2.626°38′09.79″119°33′04.28″黏土
    1号823.526°38′24.61″119°30′14.12″苔藓
    12号57226°38′39.60″119°30′04.15″苔藓
    15号45626°38′32.02″119°30′45.29″苔藓
    64号−7.326°41′54.02″119°39′52.01″
    65号−8.626°42′00.79″119°42′21.89″泥质砂
    55号−52.626°37′34.89″119°44′24.37″泥质砂
    下载: 导出CSV

    表  2   NDQK2钻孔的OSL测年结果

    Table  2   OSL dated ages of core NDQK2

    实验室编号深度/mTh/ (μg/g)误差/10−6U (/μg/g)误差/10−6年龄/ka误差/ ka粒径/μm
    NDQK2-OSL-113.90~14.000.150.150.150.1511.40.938~63
    NDQK2-OSL-215.00~15.103.852.613.163.5411.70.938~63
    NDQK2-OSL-317.35~17.450.150.150.150.15  38~63
    下载: 导出CSV

    表  3   NDQK2钻孔的AMS14C测年结果

    Table  3   AMS14C dating ages of core NDQK2

    实验室编号深度/m测年材料测试年龄/aBP校正年龄 (2σ) /aBP平均值/aBP
    NDQK2 14C-12.2625±20610~554582
    NDQK2 14C-25.9贝壳465±20531~500515.5
    NDQK2 14C-37.1贝壳505±20543~510526.5
    Beta-5679757.3植物残体4430±305069~48754972
    Beta-5522077.6植物残体6950±307849~76897769
    NDQK2 14C-48.2贝壳7425±258326~81858255.5
    NDQK2 14C-4-28.2木炭7055±307955~78357895
    Beta-55220210.3植物残体7990±409006~87058855.5
    Beta-55220313.3植物残体7970±308993~87048848.5
    下载: 导出CSV

    表  4   NDQK2钻孔的孢粉和藻类类型及生态学划分[22]

    Table  4   Pollen and algae taxa and ecological groups in core NDQK2[22]

    类型主要成分主要属种
    孢粉热带、亚热带针叶林成分Podocarpus罗汉松属、Cupressaceae柏科、Keteleeria油杉属、Taxodiaceae杉科、Pinus松属
    高海拔针叶成分Abies冷杉属、Picea云杉属、Tsuga铁杉属
    热带、亚热带阔叶成分Quercus-evergreen常绿栎属、Castanopsis/Castanea栲属/栗属、Phyllanthus叶下珠属、Moraceae桑科、Myrica杨梅属、Acanthaceae爵床科、Theaceae山茶科、Rubiaceae茜草科、Sapindaceae无患子科、Hamamelidaceae金缕梅科、Liquidambar枫香树属、Verbenaceae马鞭草科、Ilex冬青属、Euphorbiaceae大戟科、Fagus水青冈属、Oleaceae木犀科、Rutaceae芸香科、Randia山黄皮属、Magnoliaceae木兰科
    温带落叶成分Quercus-decidious落叶栎属、Alnus桤木属、Ulmus榆属、Betula桦木属、Pterocarya枫杨属、Carpinus鹅耳枥属、Corylus榛属、Juglans胡桃属、Tilia椴属、Celtis朴属、Ericaceae杜鹃花科
    草本植物Artemisia蒿属、Chenopodiaceae藜科、Poaceae禾本科、Brassicaceae十字花科、Cyperaceae莎草科、Asteraceae菊科、Thalictrum唐松草属、Polygonaceae蓼科、Myriophyllum狐尾藻属、Typha香蒲属
    蕨类蕨类孢子Polypodiaceae水龙骨科、Dicranopteris芒萁属、Pteris凤尾蕨属、Selaginella卷柏属、Hicriopteris里白属
    藻类淡水藻类Concentricystes环纹藻、Pediastrum 盘星藻属
    沟鞭藻囊孢OperculodiniumSelenopemphixSpiniferitesTuberculodinium
    下载: 导出CSV

    表  5   我国东南沿海各期文化遗址信息

    Table  5   Information of cultural relics in various stages along the southeast coast of China

    遗址类型上山文化跨湖桥文化马家浜文化河姆渡文化壳丘头文化/富国墩文化崧泽文化昙石山文化/大帽山文化
    时间/kaBP11~88~77~67~56.5~5.56~5.35~4.3
    遗址数量/个18631117/2446/5
    纬度(N)29° 27′ 36″30° 8′ 39″30° 42′ 19″29° 57′ 45″25° 37′ 25″/24°26′28″31°8′46″26° 9′ 1″/23° 43′ 13″
      考古资料和数据来自于《中国文物地图集浙江分册》(国家文物局,2009)[38]、《中国文物地图集福建分册》(国家文物局,2007)[39]及《长江下游考古时代的环境研究》[40]
    下载: 导出CSV
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出版历程
  • 收稿日期:  2020-10-21
  • 修回日期:  2020-12-22
  • 网络出版日期:  2021-01-31
  • 刊出日期:  2021-06-27

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