豫西渑池盆地湖泊沉积特征与古环境

doi:10.13249/j.cnki.sgs.2011.08.922

地理科学 ›› 2011, Vol. 31 ›› Issue (8): 922-928.doi: 10.13249/j.cnki.sgs.2011.08.922

豫西渑池盆地湖泊沉积特征与古环境

翟秋敏¹, 郭志永^1,2, 沈娟¹

1. 河南大学资源与环境研究所, 河南开封 475004;
2. 南京大学地理与海洋科学学院, 江苏南京 210093

收稿日期:2010-10-12 修回日期:2011-02-18 出版日期:1997-08-20 发布日期:1997-08-20
基金资助:
国家自然科学基金(40601105,40325007)、河南大学资源与环境研究所项目(HD-ZHS-01)资助。

Sedimentary Characteristics of Lacustrine Sediment Profile and Paleoenvironment in Mianchi Basin, Western Henan Province

ZHAI Qiu-min¹, GUO Zhi-yong^1,2, SHEN Juan¹

1. Institute of Natural Resources and Environmental Science, Henan University, Kaifeng, Henan 475004, China;
2. School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing, Jiangsu 210093, China

Received:2010-10-12 Revised:2011-02-18 Online:1997-08-20 Published:1997-08-20

摘要/Abstract

摘要： 对渑池盆地池底村古湖泊沉积剖面进行连续采样,在粒度组成和有机碳含量分析的基础上,结合¹⁴C年代测定(校正为日历年龄),重建了盆地区末次冰盛期以来的气候环境演化进程:19543~9240cal.aB.P.,气候比较干燥,古湖泊尚未形成;9240~8039cal.aB.P.,气候由干冷向暖湿化方向转变,古湖泊开始形成;8039~3473cal.aB.P.期间,气候温暖湿润,湖泊水位最高;3439~2931cal.aB.P.期间,气候波动剧烈,总体上气候较前一段干旱,湖泊水位下降;2931~2423cal.aB.P.期间,气候干旱,古湖泊干涸。盆地区的人类文化演进对气候环境变化的响应十分明显,二者之间存在一定的耦合关系。

Abstract: In this paper, continuous sampling, grain size and total organic content(TOC) analysis have been done with the paleolacustrine sediment profile in Chidi Village, Mianchi Basin, combining with ¹⁴C dating and calibrating, the paleoenvironment in Mianchi Basin since the Last Glacial Maximum was reconstructed as follow: (1) During 19 543-9 240 cal. a B.P., the climate was dry and the lake was not formed; (2) During 9 240- 8 039 cal.a B.P., the climate turned to be warmer and humid, paleolake started to form;(3) During 8 039- 3 473 cal.aB.P., it was warm and humid in Lake Basin, and water level of the paleolake was the highest;(4) During 3 439-2 931 cal.a B.P., the climate change violently, in the whole period it was less warm and humid than before, water level of the paleolake decreased.(5) During 2 931-2 423 cal.a B.P., it was a dry and cold period with lower temperature and less precipitation, the paleolake gradually dried up. The evolution of human cultural in Mianchi Basin responded to climate change obviously, and was in correlation with the environment change.

中图分类号:

X144

翟秋敏, 郭志永, 沈娟. 豫西渑池盆地湖泊沉积特征与古环境[J]. 地理科学, 2011, 31(8): 922-928.

ZHAI Qiu-min, GUO Zhi-yong, SHEN Juan. Sedimentary Characteristics of Lacustrine Sediment Profile and Paleoenvironment in Mianchi Basin, Western Henan Province[J]. SCIENTIA GEOGRAPHICA SINICA, 2011, 31(8): 922-928.

参考文献

[1] Finney B P,Johnson T C. Sedimentation in Lake Malawi(East Africa)during the past 10 000 years: a continuous paleoclimatic record from the southern tropics[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,1991,85(3-4):351-366.
[2] 王苏民,李建仁.湖泊沉积——研究历史气候的有效手段[J].科学通报,1991,36(1):54~56.
[3] 朱江玲,刘鸿雁,王红亚.河北坝上地区湖泊沉积物记录的中全新世干旱气候[J].地理科学,2007,27(3): 380~384
[4] 贾铁飞,戴雪荣,张卫国,等.全新世巢湖沉积记录及其环境变化意义[J].地理科学,2006,26(6):706~711
[5] 翟秋敏,李容全,郭志永.坝上高原安固里淖粒度年纹层与环境变化[J].地理科学, 2002,22(3):331~335
[6] Gerard Bond,Bernd Kromer.Persistent solar influence on North Atlantic climate during the Holocene[J].Science,2001, 294:2130-2136.
[7] Porter S C,An Z S.Correlation between climate events in the North Atlantic and China during the last glaciation[J]. Nature,1995,375:305-308.
[8] 鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义[J].中国科学(D),1998,28(3):278~283.
[9] 李志忠,凌智永,陈秀玲.新疆伊犁河谷晚全新世风沙沉积粒度旋回与气候变化[J].地理科学,2010,30(1):613~619
[10] 罗建育,陈镇东.台湾高原湖泊沉积记录指示的近4 000 a气候与环境变化[J].中国科学(D辑),1997,27 (4) :366~372.
[11] Chen Jing-an,Wan Guo-jiang,Tang De-gui.Recent climate changes recorded by sediment grain sizes and isotopes in Erhai Lake[J].Progress in Natural Science,2003,10 (3) :253-259.
[12] 孙千里,周杰,肖举乐.岱海沉积物粒度特征及其古环境意义[J].海洋地质与第四纪地质,2001,21(1): 93~95.
[13] 何华春,丁海燕,张振克.淮河中下游洪泽湖湖泊沉积物粒度特征及其沉积环境意义[J].地理科学,2005,25(5):590~596.
[14] 王心源,吴立,张广胜,等.安徽巢湖全新世湖泊沉积物磁化率与粒度组合的变化特征及其环境意义[J].地理科学,2008,28(4):548~553
[15] 苏秉琦.关于仰韶文化的若干问题[J].考古学报,1965,30(1):28~36.
[16] 夏鼐.考古研究所河南省调查团.河南渑池的史前遗址[J].科学通报,1951,2(9):933~936.
[17] 渑池县志编撰委员会.渑池县志[M].上海:汉语大辞典出版社,1991:64~72.
[18] Bronk Ramsey C.Bayesian analysis of radiocarbon dates[J].Radiocarbon,2009,51(1):337-360.
[19] Reimer P J, Baillie M G L,Bard E,et al.IntCal09 and Marine09 radiocarbon age calibration curves, 0-50 000 years cal B.P.Radiocarbon,2009, 51(4):1111-1150.
[20] Irino T,Tada R. Quantification of aeolian dust (Kosa) contribution to the Japan Sea sediments and its variation during the last 200 ky[J]. Geochemical Journal,2000,34(1):59-93.
[21] 長島佳菜,多田隆治,松井裕之.過去14万年間のアジアモンスーン·偏西風変動-日本海堆積物中の黄砂粒径·含有量からの復元[J].第四紀研究,2004,43 (2):85~97.
[22] 成都地质学院陕北队编.沉积岩(物)粒度分析及其应用[M].北京:地质出版社,1978:2~3.
[23] 翟秋敏,邱维理,李容全,等.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[J].古地理学报,2000,2(2):84~91.
[24] Bertrand P E,Lallier-Verges.Past sedimentary organic matter accumulation and degradation controlled by productivity[J].Nature,1993, 364:786-788.
[25] Sifeddine P,Bertrand E,Lallier-Verges, et al. Lacustrine Organic Fluxes and Palaeoclimatic Variations During the Last 15Ka:Lacdu Bouchet (Massif central,France)[J].Quaternary Science Reviews,1996,15:203-212.
[26] Meyer P A,Horie S.An organic carbon isotopic record of glacial-postglacial change in atmospheric pCO₂ in the sediments of Lake Biwa, Japan[J].Palaeogeography, Palaeoclimatology,Palaeoecology,1993,105(3-4):171-178.
[27] 董广辉,夏正楷,刘德成.河南孟津地区中全新世环境变化及其对人类活动的影响[J].北京大学学报(自然科学版),2006,42(2):238~243.
[28] 孙雄伟,夏正楷.河南洛阳寺河南剖面中全新世以来的孢粉分析及环境变化[J].北京大学学报(自然科学版),2005,41(2):289~294.
[29] Weiss H,Courty M-A,Wetterstrom W,et al.The genesis and collapse of third millennium North Mesopotamian civilization[J].Science, 1993, 261(20):995-100.
[30] Hodell D A,Brenner M Curtis,Jason H,et al.Solar forcing of drought frequency in the maya lowlands[J].Science, 2001,292:1367-1370.
[31] Haug G H,Gunther D.P eterson L C,et al.Climate and the collapse of maya civilization[J].Science,2003,299:1731-1735.
[32] Hodell D A,Crutis J H,Brenner M.Possible role of climate in the collapse of Classic Maya civilization[J].Nature,1995, 375:391-394.
[33] 周昆叔.周原黄土及其与文化层的关系[J].第四纪研究,1995, (2):174~179.
[34] 庞奖励,黄春长.关中地区新石器文化发展与环境演变藕合关系研究[J].地理科学,2003,23(4):448~453.
[35] 施少华.中国全新世高温期中的气候突变事件及其对人类的影响[J].海洋地质与第四纪地质,1993,3(4):65~73.
[36] 吴文祥,刘东生.4 000 a B.P.降温事件与中国古代文明的诞生[J].第四纪研究,2001,21(5):443~451.

豫西渑池盆地湖泊沉积特征与古环境

Sedimentary Characteristics of Lacustrine Sediment Profile and Paleoenvironment in Mianchi Basin, Western Henan Province

PDF (PC)

赞

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

推荐阅读 0

[1]	姚李忠, 王中华, 徐圣友. 山岳型酒店能源强度与碳排放特征研究[J]. 地理科学, 2020, 40(6): 965-972.
[2]	钟聪, 李小洁, 何园燕, 邱微文, 李杰, 张新英, 胡宝清. 广西土壤有机质空间变异特征及其影响因素研究[J]. 地理科学, 2020, 40(3): 478-485.
[3]	张向敏, 罗燊, 李星明, 李卓凡, 樊勇, 孙健武. 中国空气质量时空变化特征[J]. 地理科学, 2020, 40(2): 190-199.
[4]	王来健, 张绍良, 尹鹏程, 王腊春, 彭山桂. 采煤沉陷湖人工湿地对周边土地价格的溢出效应研究——以徐州市九里湖湿地为例[J]. 地理科学, 2017, 37(8): 1234-1242.
[5]	孙朋, 巩杰, 贾珍珍, 谢余初. 基于通径分析的酒金盆地绿洲化时空变化及影响因子研究[J]. 地理科学, 2016, 36(6): 902-909.
[6]	王莉雯, 卫亚星. 基于减小叶片水分影响的湿地芦苇氮浓度高光谱反演研究[J]. 地理科学, 2016, 36(1): 135-141.
[7]	陈利顶, 贾福岩, 汪亚峰. 黄土丘陵区坡面形态和植被组合的土壤侵蚀效应研究[J]. 地理科学, 2015, 35(9): 1176-1182.
[8]	张永领, 董玉龙, 张东. 在三门峡水库影响下黄河有机碳的输送特征[J]. 地理科学, 2015, 35(7): 912-918.
[9]	赵雪雁, 薛冰. 干旱区内陆河流域农户对水资源紧缺的感知及适应 ——以石羊河中下游为例[J]. 地理科学, 2015, 35(12): 1622-1630.
[10]	廖芳均, 赵东升. 南岭国家级自然保护区森林景观格局变化与动态模拟[J]. 地理科学, 2014, 34(9): 1099-1107.
[11]	郗敏, 孔范龙, 吕宪国, 姜明, 李悦. 三江平原沟渠系统水体和底泥的养分特征及效应[J]. 地理科学, 2014, 34(3): 358-364.
[12]	李枫, 吴立, 朱诚, 孙伟, 王晓翠, 孟华平, 刘辉, 齐士峥, 龚琪岚, 朱光耀, 周凤琴, 李溯源, 欧阳杰. 江汉平原12.76 cal. ka B.P.以来环境干湿变化的高分辨率研究[J]. 地理科学, 2012, 32(7): 878-884.
[13]	杜会石, 哈斯, 李明玉. 1977~2008年延吉市城市景观格局演变[J]. 地理科学, 2011, 31(5): 608-612.
[14]	刘德燕, 丁维新. 天然湿地土壤产甲烷菌及其影响因子研究进展[J]. 地理科学, 2011, 31(2): 136-142.
[15]	徐明星, 周生路, 王晓瑞, 吴绍华, 曹伟, 张红富. 长江三角洲典型区社会经济发展对土壤重金属累积的影响[J]. 地理科学, 2010, 30(6): 880-885.