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

参考文献(88)

An, X.H., 2016.Morphological Characteristics of Phytoliths from Representative Conifers in China.Palaeoworld, 25(1):116-127. doi: 10.1016/j.palwor.2016.01.002
Berger, A., Loutre, M.F., 1991.Insolation Values for the Climate of the Last 10 Million Years.Quaternary Science Reviews, 10(4):297-317. https://doi.org/10.1016/0277-3791(91)90033-q
Bond, G., Kromer, B., Evans, M.N., et al., 2001.Persistent Solar Influence on North Atlantic Climate during the Holocene.Science, 294(5549):2130-2136. https://doi.org/10.1126/science.1065680
Chen, F.H., Xu, Q.H., Chen, J.H., et al., 2015.East Asian Summer Monsoon Precipitation Variability since the Last Deglaciation.Scientific Reports, 5(1):11186. https://doi.org/10.1038/srep11186
Chen, F.H., Yu, Z.C., Yang, M.L., et al., 2008.Holocene Moisture Evolution in Arid Central Asia and Its Out-of-Phase Relationship with Asian Monsoon History.Quaternary Science Reviews, 27(3-4):351-364. https://doi.org/10.1016/j.quascirev.2007.10.017
Fan, J.W., Xiao, J.L., Wen, R.L., et al., 2016.Droughts in the East Asian Summer Monsoon Margin during the Last 6 kyrs:Link to the North Atlantic Cooling Events.Quaternary Science Reviews, 151:88-99. https://doi.org/10.13039/501100001809
Gao, G.Z., Jie, D.M., Wang, Y., et al., 2017.Phytolith Reference Study for Identifying Vegetation Changes in the Forest-Grassland Region of Northeast China.Boreas, 47(2):481-497. https://doi.org/10.1111/bor.12280
Ge, Q.S., Zheng, J.Y., Man, Z.M., et al., 2002.Reconstruction and Analysis on the Series of Winter-Half-Year Temperature Changes over the Past 2 000 Years in Eastern China.Earth Science Frontiers, 9(1):169-181 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY200201034.htm
Ge, Y., Jie, D.M., Guo, J.X., et al., 2010.Response of Phytoliths in Leymus Chinensis to the Simulation of Elevated Global CO₂ Concentrations in Songnen Grassland, China.Chinese Science Bulletin, 55(27):2735-2741 (in Chinese).
Grimm, E.C., 1991.Tilia and Tiliagraph.Illinois State Museum, Springfield.
Gu, Y.S., Li, C.A., Zhang, Z.J., 1997.Application of Phytolith Analysis in Study of Vermicular Red Earth in South China.Geological Science and Technology Information, 16(4):55-58 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZKQ704.009.htm
Gu, Y.S., Liu, H.M., Zeng, Z.X., et al., 2016.Environmental Change Documented by Pluvial Phytolith Records in the Past 26 ka on East Edge of Tengger Desert.Earth Science, 41(4):605-611 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201604005.htm
Guan, Y.X., 2011.A Research on the Land Use of the West of Liao River and Environmental Change in Qing Dynasty (Dissertation).Jilin University, Changchun (in Chinese with English abstract).
Guo, C., Ma, Y.Z., Hu, C.L., et al., 2014.Holocene Humidity Changes in Inland China Inferred from Lake Sediments.Progress in Geography, 33(6):786-798 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLKJ201406008.htm
Han, M.L., 2010.A Study on Settlements and Environment of Prehistoric Times in the West Liaohe River Valley.Acta Archaeologica Sinica, (1):1-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KGXB201001003.htm
Han, P., Liu, X.Q., 2017.The Climate Evolution Inferred from Chagan-Nuur in Middle-East Part of Inner Mongolia since the Last 7 000 Years.Quaternary Sciences, 37(6):1381-1390 (in Chinese with English abstract). http://www.dsjyj.com.cn/EN/Y2017/V37/I6/1381
Hu, J.M., Cui, H.T., Li, Y.Y., 2002.Reconstruction of the Evolution History of Man-Land System since the Holocene in the Xiliao River Basin.Scientia Geographica Sinica, 22(5):535-542 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLKX200205003.htm
Jia, X., Lee, H.F., Zhang, W.C., et al., 2016a.Human-Environment Interactions within the West Liao River Basin in Northeastern China during the Holocene Optimum.Quaternary International, 426:10-17. https://doi.org/10.13039/501100001809
Jia, X., Sun, Y.G., Wang, L., et al., 2016b.The Transition of Human Subsistence Strategies in Relation to Climate Change during the Bronze Age in the West Liao River Basin, Northeast China.The Holocene, 26(5):781-789. https://doi.org/10.1177/0959683615618262
Jiang, J.M., Wu, J.L., Shen, J., 2004.Lake Sediment Records of Climatic and Environmental Change in Angulinao Lake.Scientia Geographica Sinica, 24(3):346-351 (in Chinese with English abstract).
Jin, Z.D., Shen, J., Wang, S.M., et al., 2002.The Medieval Warm Period in the Daihai Area.Journal of Lake Sciences, 14(3):209-216 (in Chinese with English abstract). doi: 10.18307/2002.0303
Li, Y.Y., Willis, K.J., Zhou, L.P., et al., 2006.The Impact of Ancient Civilization on the Northeastern Chinese Landscape:Palaeoecological Evidence from the Western Liaohe River Basin, Inner Mongolia.The Holocene, 16(8):1109-1121. doi: 10.1177/0959683606069403
Liu, H.Y., Xu, L.H., Cui, H.T., 2002.Holocene History of Desertification along the Woodland-Steppe Border in Northern China.Quaternary Research, 57(2):259-270. https://doi.org/10.1006/qres.2001.2310
Liu, L.J., Yang, Z.J., Wang, P.L., et al., 2017.Comparative Study of Pollen and Phytolith Records since the Middle Holocene from Pingliang Region of Loess Plateau.Acta Geoscientica Sinica, 38(3):393-402 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DQXB201703009.htm
Lu, H.Y., Wu, N.Q., Yang, X.D., et al., 2006.Phytoliths as Quantitative Indicators for the Reconstruction of Past Environmental Conditions in China Ⅰ:Phytolith-Based Transfer Functions.Quaternary Science Reviews, 25(9/10):945-959. https://doi.org/10.1016/j.quascirev.2005.07.014
Ma, L., Wu, J.L., 2009.Environmental Significance from Organic Carbon and Its Isotope of Angulinao Lake Sediment.Journal of Natural Resources, 24(6):1099-1104 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZRZX200906017.htm
Madella, M., Alexandre, A., Ball, T., 2005.International Code for Phytolith Nomenclature 1.0.Annals of Botany, 96(2):253-260. https://doi.org/10.1093/aob/mci172
Mao, X., Liu, L.J., Li, C.A., et al., 2017.Elemental Composition Features of Loess-Paleosol Profile in Fengning, Hebei Province.Earth Science, 42(10):1750-1759 (in Chinese with English abstract).
PAGES, 2009.Science Plan and Implementation Strategy.IGBP Report NO.57.IGBP Secretariat, Stockholm, 67.
Peng, Y., Xiao, J., Nakamura, T., et al., 2005.Holocene East Asian Monsoonal Precipitation Pattern Revealed by Grain-Size Distribution of Core Sediments of Daihai Lake in Inner Mongolia of North-Central China.Earth and Planetary Science Letters, 233(3-4):467-479. https://doi.org/10.1016/j.epsl.2005.02.022
Piperno, D.R., 2006.Phytoliths: A Comprehensive Guide for Archaeologists and Paleoecologists.Alta Mira Press, Lanham, MD, 238.
Qiu, W.L., Zhai, Q.M., Hu, H.B., et al., 1999.Holocene Water Level Changes of Angulinao Lake and Their Environmental Significance.Journal of Beijing Normal University (Natural Science), 35(4):542-548 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-BSDZ199904030.htm
Ran, X.B., Yu, Z.G., Zang, J.Y., et al., 2013.Advances in the Influence of Earth Surface Process and Human Activity on Silicon Output.Advances in Earth Science, 28(5):577-587 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkxjz201305010
Reimer, P.J., Bard, E., Bayliss, A., et al., 2013.IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0-50 000 Years cal BP.Radiocarbon, 55(4):1869-1887. https://doi.org/10.2458/azu_js_rc.55.16947
Sun, J.Z., Sheng, X.B., Liu, Y.X., 1999.A Study on the Human Activities and Ecological and Environmental Changes in the Bashang Area of Heibei Province.Advances in Environmental Science, 7(4):102-111 (in Chinese with English abstract).
Sun, Q.L., Xiao, J.L., 2006.Characteristics of the Holocene Optimum in the Monsoon/Arid Transition Belt Recorded by Core Sediments of Daihai Lake, North China.Quaternary Sciences, 26(5):781-790 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DSJJ200605013.htm
Wang, C., Fu, Y.S., Bi, J., 2005.A Preliminary Study on the Reasons of Degradation of Angulinuur Wetland.Journal of Hebei Forestry Science and Technology, (S1):5-6, 11 (in Chinese).
Wang, H.Y., Liu, H.Y., Zhu, J.L., et al., 2010.Holocene Environmental Changes as Recorded by Mineral Magnetism of Sediments from Anguli-Nuur Lake, Southeastern Inner Mongolia Plateau, China.Palaeogeography, Palaeoclimatology, Palaeoecology, 285(1-2):30-49. https://doi.org/10.1016/j.palaeo.2009.10.020
Wang, S.W., Cai, J.N., Zhu, J.H., et al., 2002.Studies on Climate Change in China.Climatic and Environmental Research, 7(2):137-145 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/jjdl201506018
Wang, S.W., Gong, D.Y., 2000.Enhancement of the Warming Trend in China.Geophysical Research Letters, 27(16):2581-2584. https://doi.org/10.1029/1999gl010825
Wang, W.M., Liu, J.L., Zhou, X.D., 2003.A Study on the Climate Index of Phytoliths in the Nanjing Homo Erectus Cave Deposits.Chinese Science Bulletin, 48(11):1205-1208 (in Chinese). http://d.wanfangdata.com.cn/Periodical/kxtb-e200318021
Wang, Y.J., Lu, H.Y., 1993.The Study of Phytolith and Its Application.China Ocean Press, Beijing (in Chinese with English abstract).
Wen, R.L., Xiao, J.L., Fan, J.W., et al., 2017.Pollen Evidence for a Mid-Holocene East Asian Summer Monsoon Maximum in Northern China.Quaternary Science Reviews, 176:29-35. https://doi.org/10.13039/501100001809
Wu, Y.H., Wang, S.M., Zhou, L.P., et al., 2007.Modern Reservoir Age for ¹⁴C Dating in Daihai Lake.Quaternary Sciences, 27(4):507-510 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ200704004.htm
Xia, Z.K., Deng, H., Wu, H.L., 2000.Geomorphologic Background of the Prehistoric Cultural Evolution in the Xar Moron River Basin, Inner Mongolia.Acta Geographica Sinica, 55(3):329-336 (in Chinese with English abstract).
Xiao, J.L., Chang, Z.G., Wen, R.L., et al., 2009.Holocene Weak Monsoon Intervals Indicated by Low Lake Levels at Hulun Lake in the Monsoonal Margin Region of Northeastern Inner Mongolia, China.The Holocene, 19(6):899-908. https://doi.org/10.1177/0959683609336574
Xiao, J.L., Wu, J.T., Si, B., et al., 2006.Holocene Climate Changes in the Monsoon/Arid Transition Reflected by Carbon Concentration in Daihai Lake of Inner Mongolia.The Holocene, 16(4):551-560. https://doi.org/10.1191/0959683606hl950rp
Xiao, J.L., Xu, Q.H., Nakamura, T., et al., 2004.Holocene Vegetation Variation in the Daihai Lake Region of North-Central China:A Direct Indication of the Asian Monsoon Climatic History.Quaternary Science Reviews, 23(14-15):1669-1679. https://doi.org/10.1016/j.quascirev.2004.01.005
Xiao, J.L., Si, B., Zhai, D.Y., et al., 2008.Hydrology of Daili Lake in Central-Eastern Inner Mongolia and Holocene East Asian Monsoon Variability.Journal of Paleolimnology, 40(1):519-528. doi: 10.1007/s10933-007-9179-x
Xiao, Z.C., 2014.The Archaeological Site and Social Development of Liaoxi Corridor in Liao Dynasty.Agricultural Archaeology, 4:89-93 (in Chinese). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-ZAIE201402006.htm
Yang, L.H., Wang, T., Zhou, J., et al., 2012.OSL Chronology and Possible Forcing Mechanisms of Dune Evolution in the Horqin Dunefield in Northern China since the Last Glacial Maximum.Quaternary Research, 78(2):185-196. https://doi.org/10.1016/j.yqres.2012.05.002
Yang, L.H., Zhou, J., Lai, Z.P., et al., 2010.Late Glacial and Holocene Dune Evolution in the Horqin Dunefield of Northeastern China Based on Luminescence Dating.Palaeogeography, Palaeoclimatology, Palaeoecology, 296(1-2):44-51. https://doi.org/10.1016/j.palaeo.2010.06.014
Yang, X.L., Zhang, R.C., Zhang, Z., et al., 2017.Environmental Change since 5 000 cal.a B.P.in the Anguli-Nuur Lake Area Based on Palynological and Geochemical Records.Quaternary Sciences, 37(1):130-142 (in Chinese with English abstract). http://www.dsjyj.com.cn/EN/Y2017/V37/I1/130
Yang, Z.R., Suo, X.F., 1996.Preliminary Study on Relations between Human Activities and Environment in Farming-Animal Husbandry Zigzag Zone of North China.Journal of Beijing Normal University (Natural Science), 32(3):415-420 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-BSDZ603.029.htm
Zhai, Q.M., 2001.Holocene Soluble Salt Sediments of Angulinao Lake and Its Environment.Journal of Palaeogeography, 3(1):91-96 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-GDLX200101010.htm
Zhai, Q.M., Guo, Z.Y., 2002.Geochemical Characters and Environmental Changes of Holocene Sediments of Angulinao Lake in Bashang Plateau.Journal of Palaeogeography, 4(4):55-60 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-GDLX200204006.htm
Zhai, Q.M., Qiu, W.L., Li, R.Q., et al., 2000.The Middle and Late Holocene Lacustrine Sediments and Its Climate Significance of Angulinao-Bojianghaizi Lakes, Inner Mongolia.Journal of Palaeogeography, 2(2):87-94 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GDLX200002009.htm
Zhang, P., Cheng, H., Edwards, R.L., et al., 2008.A Test of Climate, Sun, and Culture Relationships from an 1 810-Year Chinese Cave Record.Science, 322(5903):940-942. https://doi.org/10.1126/science.1163965
葛全胜, 郑景云, 满志敏, 等, 2002.过去2 000 a中国东部冬半年温度变化序列重建及初步分析.地学前缘, 9(1):169-181. doi: 10.3321/j.issn:1005-2321.2002.01.021
葛勇, 介冬梅, 郭继勋, 等, 2010.松嫩草原羊草植硅体对模拟全球CO₂浓度升高的响应研究.科学通报, 55(27):2735-2741. http://www.cqvip.com/QK/94252X/201027/35554051.html
顾延生, 李长安, 章泽军, 1997.植硅石分析在第四纪环境研究中的应用.地质科技情报, 16(4):55-58. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ704.009.htm
顾延生, 刘胡玫, 曾佐勋, 等, 2016.腾格里沙漠东缘26 ka来环境演化的植硅体记录.地球科学, 41(4):605-611. http://www.earth-science.net/WebPage/Article.aspx?id=3277
关亚新, 2011.清代辽西土地利用与生态环境变迁研究(博士学位论文).长春: 吉林大学.
郭超, 马玉贞, 胡彩莉, 等, 2014.中国内陆区湖泊沉积所反映的全新世干湿变化.地理科学进展, 33(6):786-798. http://d.old.wanfangdata.com.cn/Periodical/dlkxjz201406007
韩茂莉, 2010.史前时期西辽河流域聚落与环境研究.考古学报, (1):1-20. doi: 10.1016-S0001-8708(03)00047-1/
韩鹏, 刘兴起, 2017.内蒙古中东部查干淖尔湖流域7 000年以来的气候演变.第四纪研究, 37(6):1381-1390.
胡金明, 崔海亭, 李宜垠, 2002.西辽河流域全新世以来人地系统演变历史的重建.地理科学, 22(5):535-542. doi: 10.3969/j.issn.1000-0690.2002.05.004
姜加明, 吴敬禄, 沈吉, 2004.安固里淖沉积物记录的气候环境变迁.地理科学, 24(3):346-351. doi: 10.3969/j.issn.1000-0690.2004.03.015
金章东, 沈吉, 王苏民, 等, 2002.岱海的"中世纪暖期".湖泊科学, 14(3):209-216. doi: 10.3321/j.issn:1003-5427.2002.03.003
刘林敬, 杨振京, 王盼丽, 等, 2017.黄土高原平凉地区中全新世以来孢粉-植硅体记录对比研究.地球学报, 38(3):393-402. http://d.old.wanfangdata.com.cn/Periodical/dqxb201703009
马龙, 吴敬禄, 2009.安固里淖湖积物中总有机碳含量及其碳同位素的环境意义.自然资源学报, 24(6):1099-1104. doi: 10.3321/j.issn:1000-3037.2009.06.017
毛欣, 刘林敬, 李长安, 等, 2017.丰宁黄土-古土壤剖面常量元素地球化学特征.地球科学, 42(10):1750-1759. http://www.earth-science.net/WebPage/Article.aspx?id=3662
邱维理, 翟秋敏, 扈海波, 等, 1999.安固里淖全新世湖面变化及其环境意义.北京师范大学学报(自然科学版), 35(4):542-548. http://www.cnki.com.cn/Article/CJFDTOTAL-BSDZ199904030.htm
冉祥滨, 于志刚, 臧家业, 等, 2013.地表过程与人类活动对硅产出影响的研究进展.地球科学进展, 28(5):577-587. http://d.old.wanfangdata.com.cn/Periodical/dqkxjz201305010
孙建中, 盛学斌, 刘云霞, 1999.河北坝上地区人类活动与生态环境变化研究.环境科学进展, 7(4):102-111. http://cdmd.cnki.com.cn/Article/CDMD-10027-2006030004.htm
孙千里, 肖举乐, 2006.岱海沉积记录的季风/干旱过渡区全新世适宜期特征.第四纪研究, 26(5):781-790. doi: 10.3321/j.issn:1001-7410.2006.05.013
王超, 付芸生, 毕君, 2005.安固里淖湿地退化原因初探.河北林业科技, S1:5-6, 11. http://d.old.wanfangdata.com.cn/Periodical/heblykj2005z1003
王绍武, 蔡静宁, 朱锦红, 等, 2002.中国气候变化的研究.气候与环境研究, 7(2):137-145. http://d.old.wanfangdata.com.cn/Periodical/qhbhyjjz200601001
王伟铭, 刘金陵, 周晓丹, 2003.南京直立人洞穴沉积的植硅体气候指数研究.科学通报, 48(11):1205-1208. doi: 10.3321/j.issn:0023-074X.2003.11.018
王永吉, 吕厚远, 1993.植物硅酸体研究及应用.北京:海洋出版社.
吴艳宏, 王苏民, 周力平, 等, 2007.岱海¹⁴C测年的现代碳库效应研究.第四纪研究, 27(4):507-510. doi: 10.3321/j.issn:1001-7410.2007.04.005
夏正楷, 邓辉, 武弘麟, 2000.内蒙西拉木伦河流域考古文化演变的地貌背景分析.地理学报, 55(3):329-336. doi: 10.3321/j.issn:0375-5444.2000.03.009
肖忠纯, 2014.辽代辽西走廊的考古遗址与社会发展.农业考古, 4:89-93. http://d.old.wanfangdata.com.cn/Periodical/nykg201404015
阳小兰, 张茹春, 张振, 等, 2017.安固里淖湖近5 000年来环境变化的孢粉及地球化学沉积记录.第四纪研究, 37(1):130-142. http://d.wanfangdata.com.cn/Periodical/dsjyj201701012
杨志荣, 索秀芬, 1996.我国北方农牧交错带人类活动与环境的关系.北京师范大学学报(自然科学版), 32(3):415-420. doi: 10.3321/j.issn:0476-0301.1996.03.004
翟秋敏, 2001.全新世安固里淖易溶盐沉积与环境.古地理学报, 3(1):91-96. doi: 10.3969/j.issn.1671-1505.2001.01.011
翟秋敏, 郭志永, 2002.坝上高原安固里淖全新世沉积地球化学特征与环境变化.古地理学报, 4(4):55-60. doi: 10.3969/j.issn.1671-1505.2002.04.007
翟秋敏, 邱维理, 李容全, 等, 2000.内蒙古安固里淖-泊江海子全新世中晚期湖泊沉积及其气候意义.古地理学报, 2(2):87-94. http://d.wanfangdata.com.cn/Periodical_gdlxb200002010.aspx