河北坝上丰宁黄土剖面记录的230 ka BP以来的环境演化<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2017.04.059

古地理学报 ›› 2017, Vol. 19 ›› Issue (4): 745-756. doi: 10.7605/gdlxb.2017.04.059

• 古今地理环境及人类文明 • 上一篇

河北坝上丰宁黄土剖面记录的230 ka BP以来的环境演化^*

毛欣^1,2, 刘林敬^1,2, 李长安³, 姜高磊^1,2, 张玉芬⁴, 赵红梅^1,2, 毕志伟^1,2

1 中国地质科学院水文地质环境地质研究所,河北石家庄050061;
2 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;
3 中国地质大学地球科学学院,湖北武汉 430074;
4 中国地质大学地球物理与空间信息学院,湖北武汉 430074

收稿日期:2017-01-16 修回日期:2017-04-24 出版日期:2017-08-01 发布日期:2017-08-07
通讯作者: 刘林敬,男,1982年生,中国地质科学院水文地质环境地质研究所助理研究员,主要从事第四纪地质与环境演变方面的研究。E-mail: liulj206@126.com。
作者简介:毛欣,男,1989年生,中国地质科学院水文地质环境地质研究所研究实习员,主要从事第四纪环境演变方面的研究。E-mail: maoxin.iheg@hotmail.com。
基金资助:
*中国地质科学院基本科研业务费专项(编号: YWF201411)、国家自然科学基金项目(编号: 41602194)联合资助

Environmental evolution since 230 ka BP recorded by Fengning loess section in Bashang area of Hebei Province

Mao Xin^1,2, Liu Linjing^1,2, Li Changan³, Jiang Gaolei^1,2, Zhang Yufen⁴, Zhao Hongmei^1,2, Bi Zhiwei^1,2

1 Institute of Hydrogeology and Environmental Geology,Chinese Academy of Geological Sciences,Shijiazhuang 050061,Hebei;
2 Key Laboratory of Quaternary Chronology and Hydrological Environment Evolution, CAGS, Shijiazhuang 050061, Hebei;
3 School of Earth Sciences,China University of Geosciences,Wuhan 430074,Hubei;
4 Institute of Geophysics & Geomatics,China University of Geosciences,Wuhan 430074,Hubei

Received:2017-01-16 Revised:2017-04-24 Online:2017-08-01 Published:2017-08-07
Contact: Liu Linjing,born in 1982,is a research associate of Institute of Hydrogeology and Environmental Geology,Chinese Academy of Geological Sciences. He is mainly engaged in researches on Quaternary geology and environmental evolution. E-mail: liulj206@126.com.
About author:Mao Xin,born in 1989,is a research assistant of Institute of Hydrogeology and Environmental Geology,Chinese Academy of Geological Sciences. He is mainly engaged in research on Quaternary environmental evolution. E-mail: maoxin.iheg@hotmail.com.
Supported by:
Co-funded by the Basic Research Program of Chinese Academy of Geological Sciences(No; YWF201411) and the National Natural Science Foundation of China(No.41602194)

摘要/Abstract

摘要： 河北坝上地区位于东亚季风气候边缘区,对气候变化响应敏感。丰宁黄土剖面为研究该区域长时间尺度的环境演化提供了理想材料。通过丰宁黄土剖面地球化学元素和磁化率分析,结合光释光测年结果,恢复了该地区230,ka BP以来的环境演化历史; 通过野外观察,识别出了S₁古土壤之下发育的风化淋滤黄土层,探讨了S₁古土壤发育时期的风化淋滤特征及其所揭示的气候变化问题。结果表明: (1)230,ka BP以来的磁化率记录可与深海氧同位素3—8阶段进行细节上的对比,表明丰宁黄土堆积区对全球气候变化有着积极的响应;(2)S₁古土壤发育时期,由于受到强降水的影响,土壤中元素受到强烈淋溶从而向下迁移到L₂黄土中,造成L₂上部地球化学记录与磁化率的差异;(3)从S₁古土壤顶部到钙结核层之间土壤属于酸性淋溶土,可能相当于现今中国北亚热带的黄棕壤,其剖面由土壤层、风化淋滤黄土层和CaCO₃淀积层构成;(4)S₁古土壤发育时期的温度和降水量与现今江苏泗洪和六合地区相当,表明当时研究区为亚热带气候。

关键词: 黄土, 古地壤, 磁化率, 元素地球化学, 古气候, 河北坝上

Abstract: Bashang area of Hebei Province,located in the peripheral region of the East Asian Monsoon,is sensitive to climate change. The Fengning loess section provides ideal materials for studying long-time environmental changes in this region. Combined with OSL dating results,elemental concentrations and magnetic susceptibility were determined to obtain the record of environmental evolution since 230 ka BP. Based on identification of weathering and leaching loess under S₁ in the field,we also discussed weathering features in S₁ paleosol and the relevant climate change. The results showed that:(1)Magnetic susceptibility record of the Fengning loess section coincided with marine isotope stage 3-8 perfectly,that indicated that the study area had given a sensitive response to globe palaeoclimatic changes since 230 ka BP;(2)Due to the impact of heavy rainfall in the period of S₁ paleosol development, elements were strongly leached and migrated downward to L₂ loess,resulting in the difference between geochemical records and magnetic susceptibility in the upper of L₂ loess;(3)The Layer from S₁ paleosol to calcrete belongs to acidic leached soil type that can be equivalent to yellow-brown soil developed at modern northern subtropics, and is consist of soil layer,weathered and leached loess layer and CaCO₃ illuvium; (4)The temperature and precipitation in the period of S₁ paleosol development were quite similar to those in Sihong area and Liuhe area of Jiangsu Province,that indicated that the climate of the study area was subtropical during the forming period of S₁ paleosol.

Key words: loess, paleosol, magnetic susceptibility, geochemistry of element, palaeoclimate, Bashang area of Hebei Province

中图分类号:

P532
P595

毛欣, 刘林敬, 李长安, 姜高磊, 张玉芬, 赵红梅, 毕志伟. 河北坝上丰宁黄土剖面记录的230 ka BP以来的环境演化^*[J]. 古地理学报, 2017, 19(4): 745-756.

Mao Xin, Liu Linjing, Li Changan, Jiang Gaolei, Zhang Yufen, Zhao Hongmei, Bi Zhiwei. Environmental evolution since 230 ka BP recorded by Fengning loess section in Bashang area of Hebei Province[J]. JOPC, 2017, 19(4): 745-756.

http://www.gdlxb.cn/CN/Y2017/V19/I4/745

参考文献

1 陈骏,汪永进,陈旸,刘连文,季峻峰,鹿化煜. 2001. 中国黄土地层Rb和Sr地球化学特征及其古季风气候意义. 地质学报,75(2): 259-266. [Chen J,Wang Y J,Chen Y,Liu L W,Ji J F,Lu H Y. 2001. Rb and Sr geochemical characterization of the Chinese Loess and its implications for palaeomonsoon climate. Acta Geological Sinica,75(2): 259-266]
2 陈旸,陈骏,刘连文. 2001. 甘肃西峰晚第三纪红黏土的化学组成及化学风化特征. 地质力学学报,7(2): 167-175. [Chen Y,Chen J,Liu L W. 2001. Chemical composition and characterization of chemical weathering of late Tertiary red clay in Xifeng,Gansu Province. Journal of Geomechanics,7(2): 167-175]
3 陈一萌,曾宪光. 2009. 中国西北与华北地区末次冰期黄土气候记录的对比研究. 中国沙漠,29(6): 1075-1080. [Chen Y M,Zeng X G. 2009. Comparative study of climate changes recorded in loess strata both in Northwest China and Northern China during the last glacial period. Journal of Desert Research,29(6): 1075-1080]
4 陈忠,马海州,曹广超,周笃珺,张西营,姚远. 2007. 关于黄土碳酸盐与气候环境关系探讨. 云南地理环境研究,19(3): 7-10. [Chen Z,Ma H Z,Cao G C,Zhou D J,Zhang X Y,Yao Y. 2007. The discussion about the relationship between carbonate in loess and climate environment. Yunnan Geographic Environment Research,19(3): 7-10]
5 董红梅,赵景波,宋友桂. 2010. 长安少陵塬S 4 古土壤化学成分与环境变化. 地理科学,30(6): 904-909. [Dong H M,Zhao J B,Song Y J. 2010. Geochemical components and paleoenvironment implication for S 4 paleosol in Shaolingyuan,Chang'an County. Scientia Geographica Sinica,30(6): 904-909]
6 靳鹤龄,李明启,苏志珠,董光荣,赵晖,孙忠. 2007. 萨拉乌苏河流域地层沉积时代及其反映的气候变化. 地质学报,81(3): 307-315. [Jin H L,Li M Q,Su Z Z,Dong G R,Zhao H,Sun Z. 2007. Sedimentary age of strata in the Salawusu River Basin and climatic changing. Acta Geologica Sinica,81(3): 307-315]
7 李长安,张玉芬,熊德强,周耀,郭洁. 2013. “巫山黄土”常量元素地球化学特征. 地球科学(中国地质大学学报),38(5): 916-922. [Li C A,Zhang Y F,Xiong D Q,Zhou Y,Guo J. 2013. Major element compositions of the “Wushan Loess”. Earth Science—Journal of China University of Geosciences,38(5): 916-922]
8 李徐生,杨达源. 2002. 镇江下蜀黄土—古土壤序列磁化率特征与环境记录. 中国沙漠,22(1): 27-32. [Li X S,Yang D Y. 2002. Magnetic susceptibility features and environmental records of the Xiashu Loess in Zhejiang,Jiangsu Province. Journal of Desert Research,22(1): 27-32]
9 李徐生,杨达源,鹿化煜. 1999. 皖南风尘堆积序列氧化物地球化学特征与古气候记录. 海洋地质与第四纪地质,19(4): 75-82. [Li X S,Yang D Y,Lu H Y. 1999. Oxide-geochemistry features and paleoclimatic record of the aeolian-dust depositional sequence in southern Anhui. Marine Geology & Quaternary Geology,19(4): 75-82]
10 李志文,李保生,孙丽,温小浩,邱世藩,吕映霞. 2008. 影响中国黄土磁化率差异的多因素评述. 中国沙漠,28(2): 231-237. [Li Z W,Li B S,Sun L,Wen X H,Qiu S F,Lü Y X. 2008. Evaluation of multifactors that affect the susceptibility of China's Loess. Journal of Desert Research,28(2): 231-237]
11 刘东生. 1985. 黄土与环境. 北京: 科学出版社,7-12. [Liu D S. 1985. Loess and Environment. Beijing: Science Press,7-12]
12 刘秀铭,刘东生,夏敦胜,Hesse P,Jirl C,王冠. 2007. 中国与西伯利亚黄土磁化率古气候记录—氧化和还原条件下的两种成土模式分析. 中国科学(D辑: 地球科学),37(10): 1382-1391. [Liu X M,Liu D S,Xia D S,Hesse P,Jirl C,Wang G. 2007. Discussion on two models under oxidation and reduction conditions of paleoclimatic records of magentic susceptibility of Siberia and Chinese Loess. Science China: Earth Sciences,37(10): 1382-1391]
13 欧阳椿陶,李保生,欧先交,温小浩,曾兰华,杨艺,刘宇飞. 2007. 萨拉乌苏河流域末次间冰期古土壤化学风化与古气候. 地理学报,62(5): 518-528. [Ouyang C T,Li B S,Ou X J,Wen X H,Zeng L H,Yang Y,Liu Y F. 2007. Chemical weathering of the Milanggouwan paleosols in the Salawusu river valley and their paleoclimatic implication during the last interglacial period. Acta Geographica Sinica,62(5): 518-528]
14 邱维理,李容全,朱楠,白鸿页. 2005. 河北省丰宁地区全新世风沙活动及其对古文化的影响. 第四纪研究,25(6): 67-78. [Qiu W L,Li R Q,Zhu N,Bai H Y. 2005. Aeolian sand activities at Fenning,Hebei Province during Holocene and their influence on ancient culture. Quaternary Sciences,62(5): 518-528]
15 武春林,朱诚,鹿化煜,马春梅,朱光耀. 2006. 南京地区下蜀黄土磁性地层年代与古环境变化. 地层学杂志,30(2): 116-123. [Wu C L,Zhu C,Lu H Y,Ma C M,Zhu G Y. 2006. Magnetostratigraphical dating of the Xiashu loess in Nanjing area and its paleoenvironmental interpretation. Journal of Stratigraphy,30(2): 116-123]
16 翟秋敏,郭志永. 2011. 坝上高原安固里淖全新世湖泊沉积与环境. 北京: 科学出版社,1-120. [Zhai Q M,Guo Z Y. 2011. Holocene Sediment and Environment of Angulinao Lake in Bashang Plateau. Beijing: Science Press,1-120]
17 张玉芬,李长安,熊德强,周耀,孙习林. 2013. “巫山黄土”氧化物地球化学特征与古气候记录. 中国地质,40(1): 352-360. [Zhang Y F,Li C A,Xiong D Q,Zhou Y,Sun X L. 2013. Oxide geochemical characteristics and paleoclimate records of “Wushan loess”. Geology in China,40(1): 352-360]
18 张玉芬,邵磊,熊德强. 2014. “巫山黄土”元素地球化学特征及成因和物源意义. 沉积学报,32(1): 78-84. [Zhang Y F,Shao L,Xiong D Q. 2014. Elemental compositions of the “Wushan Loess”: Implications for origin and sediment source. Acta Sedimentologica Sinica,32(1): 78-84]
19 赵景波. 1995. 古土壤CaCO 3 淀积层与大气降水入渗形式研究. 地理科学,15(4): 344-350. [Zhao J B. 1995. A study on the CaCO 3 illuvial horizons of paleosols and permeated pattern for rain water. Scientia Geographica Sinica,15(4): 344-350]
20 赵景波. 2000. 风化淋滤带地质新理论:CaCO 3 淀积深度理论. 沉积学报,18(1): 29-35. [Zhao J B. 2000. A new geological theory about eluvial zone:Theory illuvial on depth of CaCO 3 . Acta Sedimentologica Sinica,18(1): 29-35]
21 赵景波,顾静,杜娟. 2008. 关中平原第5层古土壤发育时的气候与土壤水环境研究. 中国科学(D辑: 地球科学),38(3): 364-374. [Zhao J B,Gu J,Du J. 2008. Research in climate and soil moisture during development of S 5 paleosol in Guanzhong Plain. Science China: Earth Sciences,38(3): 364-374]
22 赵景波,邢闪,董红梅,齐子云. 2011. 西安蓝田杨家湾黄土中第一层古土壤(S 1 )元素含量与环境. 第四纪研究,31(3): 514-521. [Zhao J B,Xing S,Dong H M,Qi Z Y. 2011. The element contents of S 1 paleosol in Yangjiawan,Lantian,Xi'an and the environmental implication. Quaternary Sciences,31(3): 514-521]
23 赵景波,罗小庆,刘瑞,陈宝群,岳应利. 2015. 关中平原黄土中第1层古土壤发育时的土壤水分研究. 地质学报,89(12): 2389-2399. [Zhao J B,Luo X Q,Liu R,Chen B Q,Yue Y L. 2015. Research in soil moisture during development of S 1 paleosol in Guanzhong Plain. Acta Geologica Sinica,89(12): 2389-2399]
24 An Z S. 2000. The history and variability of the East Asian paleomonsoon climate. Quaternary Science Reviews,19: 171-187.
25 An Z S,Liu T,Lu Y,Porter S C,Kukla G,Wu X,Hua Y. 1990. The long-term paleomonsoon variation recorded by the loess-paleosol sequence in Central China. Quaternary International,7-8: 91-95.
26 Chen J,An Z,Head J. 1999. Variation of Rb/Sr ratios in the loess-paleosol sequences of Central China during the last 130 000 years and their implications for monsoon paleoclimatology. Quaternary Research,51: 215-219.
27 Chen Y Y,Li X S,Han Z Y,Yang S Y,Wang Y B,Yang D Y. 2008. Chemical weathering intensity and element migration features of the Xiashu loess profile in Zhenjiang,Jiangsu Province. Journal of Geographical Sciences,18: 341-352.
28 Fang X M,Shi Z T,Yang S J,Yan M D,Li J J,Jiang P A. 2002. Loess in the Tian Shan and its implications for the development of the Gurbantunggut desert and drying of Northern Xinjiang. Chinese Science Bulletin,47: 1381-1387.
29 Goldberg K,Humayun M. 2010. The applicability of the chemical index of alteration as a paleoclimatic indicator: An example from the Permian of the Paran�� basin,Brazil. Palaeogeography,Palaeoclimatology,Palaeoecology,293: 175-183.
30 Guo Z T,Ruddiman W F,Hao Q Z,Wu Q Z,Qiao Y S,Zhu R X,Peng S Z,Wei J J,Yuan B Y,Liu T S. 2002. Onset of Asian desertification by 220 Myr ago inferred from loess deposits in China. Nature,416: 159-163.
31 Lisiecki L E,Raymo M E. 2005. A Pliocene-Pleistocene stack of 57 globally distributed benthic 18 O records. Paleoceanography,20: 1-16.
32 Liu B,Jin H L,Sun L Y,Niu Q H,Xie S B,Li G H. 2014. Holocene moisture change revealed by the Rb/Sr ratio of aeolian deposits in the Southeastern Mu Us desert,China. Aeolian Research,13: 109-119.
33 Liu T S,Ding Z L. 1998. Chinese loess and the paleomonsoon. Annual Reviews of Earth and Planetary Sciences,26: 111-145.
34 Nesbitt H W. 1979. Mobility and fractionation of rare earth elements during weathering of a granodiorite. Nature,279: 206-210.
35 Nesbitt H W,Young G M. 1982. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature,299: 715-717.
36 Nesbitt H W,Markovics G,Price R C. 1980. Chemical processes affecting alkalis and alkaline earths during continental weathering. Geochimica Et Cosmochimica Acta,44: 1659-1666.
37 Schatz A K,Scholten T,Kühn P. 2015. Paleoclimate and weathering of the Tokaj(Hungary)loess-paleosol sequence. Palaeogeography,Palaeoclimatology,Palaeoecology,426: 170-182.
38 Si Y J,Li B S,Zhang D D,Wen X H,Wang F N,Du S H,Niu D F,Guo Y H. 2014. Climate fluctuation on a Kiloyear scale during the late last glacial in Mu Us desert,China: Evidence from Rb and Sr contents and ratios. Environmental Earth Sciences,72: 4521-4530.
39 Sun J. 2002. Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau. Earth & Planetary Science Letters,203: 845-859.
40 Sun Y,Clemens S C,An Z,Yu Z. 2006. Astronomical timescale and palaeoclimatic implication of stacked 3.6-Myr monsoon records from the Chinese Loess Plateau. Quaternary Science Reviews,25: 33-48.
41 Xiong S,Ding Z,Liu T. 2001. Climatic implications of loess deposits from the Beijing Region. Journal of Quaternary Science,16(6): 575-582.
42 Yang S Y,Li C X,Yang D Y,Li X S. 2004. Chemical weathering of the loess deposits in the Lower Changjiang valley,China,and paleoclimatic implications. Quaternary International,117: 27-34.
43 Zeng L,Lu H Y,Yi S W,Li Y X,Lü A Q,Zhang W C,Xu Z W,Wu H F,Feng H,Cui M C. 2016. New magnetostratigraphic and pedostratigraphic investigations of loess deposits in North-east China and their implications for regional environmental change during the Mid-Pleistocene climatic transition. Journal of Quaternary Science,31(1): 20-32.
44 Zhai Q,Guo Z,Li Y,Li R. 2006. Annually laminated lake sediments and environmental changes in Bashang Plateau,North China. Palaeogeography,Palaeoclimatology,Palaeoecology,241(1): 95-102.

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河北坝上丰宁黄土剖面记录的230 ka BP以来的环境演化^*

Environmental evolution since 230 ka BP recorded by Fengning loess section in Bashang area of Hebei Province

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河北坝上丰宁黄土剖面记录的230 ka BP以来的环境演化*

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河北坝上丰宁黄土剖面记录的230 ka BP以来的环境演化^*