中-晚全新世以来安固里淖气候演变的植硅体记录

刘林敬; 李长安; 介冬梅; 张茹春; 王江永; 张玉芬; 毛欣; 姜高磊; 王盼丽

doi:10.3799/dqkx.2018.614

中-晚全新世以来安固里淖气候演变的植硅体记录

doi: 10.3799/dqkx.2018.614

刘林敬^1,2,3,,
李长安^1,4, ,,
介冬梅^5,6,
张茹春^7,8,
王江永⁵,
张玉芬¹,
毛欣^2,3,
姜高磊^2,3,
王盼丽^2,3

1.
中国地质大学地球科学学院, 湖北武汉 430074
2.
中国地质科学院水文地质环境地质研究所, 河北石家庄 050061
3.
中国地质科学院第四纪年代学与水文环境演变重点实验室, 河北石家庄 050061
4.
中国地质大学生物地质与环境地质国家重点实验室, 湖北武汉 430074
5.
东北师范大学地理科学学院, 吉林长春 130024
6.
东北师范大学植被生态科学教育部重点实验室, 吉林长春 130024
7.
河北省科学院地理科学研究所, 河北石家庄 050011
8.
河北省地理信息开发应用工程技术研究中心, 河北石家庄 050011

基金项目:

国家自然科学基金项目 41471164

国家自然科学基金项目 41602194

国家自然科学基金项目 41672355

详细信息

作者简介:
刘林敬(1982-), 男, 助理研究员, 主要从事第四纪地质与环境演变方面的研究

通讯作者:
李长安

中图分类号: P595
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- 被引次数: 0
出版历程
- 收稿日期: 2018-04-17
- 刊出日期: 2018-11-15

Paleoclimate Recorded by Phytolith in Anguli-Nuur Lake since Mid-Late Holocene

Liu Linjing^{1,2,3
,},
Li Chang'an^{1,4
, ,},
Jie Dongmei^5,6,
Zhang Ruchun^7,8,
Wang Jiangyong⁵,
Zhang Yufen¹,
Mao Xin^2,3,
Jiang Gaolei^2,3,
Wang Panli^2,3

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China
3.
Key Laboratory of Quaternary Chronology and Hydrological Environment Evolution, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China
4.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
5.
School of Geographical Sciences, Northeast Normal University, Changchun 130024, China
6.
Key Laboratory of Vegetation Ecology, Ministry of Education, Northeast Normal University, Changchun 130024, China
7.
Institute of Geographical Sciences, Hebei Academy of Sciences, Shijiazhuang 050011, China
8.
Hebei Engineering Research Center for Geographic Information Application, Shijiazhuang 050011, China

摘要

摘要: 河北坝上地区位于东亚季风边缘区和农牧交错带，季风强弱的变化深刻影响着该地区人类文明的发展.为了重建河北坝上地区中-晚全新世以来的气候演化过程，剖析气候变化与人类文明发展的关系，以坝上地区安固里淖湖为研究对象，通过对该湖沉积剖面植硅体的分析，并结合孢粉组合特征，恢复了安固里淖地区5 000 cal.a BP以来的气候演变历史.结果显示，在千年尺度上该区域气候总体呈冷干趋势，但在5 030~3 070 cal.a BP时期气候相对湿润，千年尺度上气候的变化主要受控于北半球太阳辐射量的变化.在百年尺度上安固里淖地区经历了7次冷干事件，分别发生于4 500 cal.a BP、4 100~3 800 cal.a BP、3 500 cal.a BP、3 000 cal.a BP、2 100 cal.a BP、1 100 cal.a BP和800~270 cal.a BP左右，这7次冷干事件对应于东亚季风减弱阶段，主要受到了北半球高纬气候和太阳活动的共同影响.该区人类文明的演化敏感响应于气候变化，气候温湿期以农业文明为主，气候冷干期以草原文明为主.
- 河北坝上 /
- 安固里淖 /
- 植硅体 /
- 孢粉 /
- 中-晚全新世 /
- 聚类分析 /
- 气候演变
Abstract: Bashang area of Hebei Province is located in the East Asian monsoon-margin region and the ecotone between agriculture and animal husbandry. East Asian monsoon variability significantly affects the development of human civilization within its area of influence. In order to reconstruct the climate changes in Bashang area and understand the interactions between past climate and human civilization, a continuous 120 cm sediment profile was recovered from Anguli-Nuur Lake based on phytolith and pollen analysis. The results show that the climate in this region was gradually becoming cold and dry during the last 5 000 years, which is related to the weakening of East Asian monsoon produced by gradual variations of solar radiation. However, the climate was relatively wet during the periods of 5 030-3 074 cal. a BP. On the centennial scale, Anguli-Nuur has experienced seven obvious cold and dry events, which occurred during ~4 500 cal. a BP, 4 100-3 800 cal. a BP, ~3 500 cal. a BP, ~3 000 cal. a BP, ~2 100 cal. a BP, ~1 100 cal. a BP and 800-270 cal. a BP. The cold and dry events are consistent with the weakening stage of East Asian monsoon that is probably affected by high latitude climate and the solar activities. In this region, the development of human civilization is sensitive to climate change. Agriculture civilization is relatively developed during warm and humid stage, and grassland civilization appears during cool and arid stage.
- Bashang area of Hebei Province /
- Anguli-Nuur Lake /
- phytolith /
- pollen /
- Mid-Late Holocene /
- cluster analysis /
- climatic evolution

HTML全文

图 1 安固里淖地理位置及采样点

Fig. 1. Location of the Anguli-Nuur Lake and the sampling site

下载: 全尺寸图片幻灯片

图 2 安固里淖剖面深度、岩性及年代序列

Fig. 2. Lithology and depth-age model of the Anguli-Nuur Lake profile

下载: 全尺寸图片幻灯片

图 3 安固里淖剖面中典型的植硅体形态

a.帽型；b.鞍型；c.哑铃型；d.齿型(d1.二齿型；d2.弱齿型、d3.多齿型)；e1、e2、e3、k.尖型(毛状细胞)；f.棒型(f1.扁棒型；f2.细长棒型；f3.光滑棒型；f4.突起棒型；f5.刺棒型；)；g1、g3.芦苇扇型；g2.其他扇型；h1、h2.方型；h3.不规则块状；i.不规则扁平状；j.特殊型

Fig. 3. Typical phytolith in Anguli-Nuur Lake profile

下载: 全尺寸图片幻灯片

图 4 安固里淖剖面植硅体、孢粉百分含量以及温暖指数曲线变化

孢粉数据来自阳小兰等(2017)；横坐标起始刻度为0

Fig. 4. Phytolith and pollen percentage composition diagram (%), warmth index in the Anguli-Nuur Lake profile

下载: 全尺寸图片幻灯片

图 5 安固里淖与周边古气候记录、65°N太阳辐射、亚洲季风模式、太阳活动及北大西洋极端冷事件的对比

a.亚洲季风模式据Chen et al.(2008)；b.东亚季风边缘区干旱指数据郭超等(2014)；c.65°N太阳辐射据Berger and Loutre(1991)；d.公海磁化率据Chen et al.(2015)；e.达里湖木本花粉含量据Wen et al.(2017)；f.岱海木本花粉含量据Xiao et al.(2004)；g.安固里淖温暖指数；h.安固里淖蒿藜比(A/C)；i.大气残留Δ¹⁴C据Reimer et al.(2013)；j.北大西洋磁铁矿锈斑颗粒含量据Bond et al.(2001)

Fig. 5. Correlations of Anguli-Nuur and the surrounding paleoclimate records, July insolation at 65°N, Asian monsoon model, solar activity and extreme cold events in the North Atlantic

下载: 全尺寸图片幻灯片

表 1 安固里淖剖面AMS ¹⁴C测年结果

Table 1. Results of AMS ¹⁴C dating in the Anguli-Nuur Lake profile

测年物质	深度(cm)	AMS ¹⁴C年龄(a BP)	树轮校正中值年龄 (cal. a BP, 2σ)	碳库效应校正年龄 (cal. a BP)
有机质	18	2080±30	2060	60
有机质	56	2450±30	2670	670
有机质	82	3010±30	3310	1310
有机质	120	6130±40	7030	5030

下载: 导出CSV

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