The Sporo-pollen Analysis and Paleoenvironment Change in Taohuajian Profile of Ruicheng County, Shanxi Province Since Late Mid-Holocene

Abstract

Abstract:

Based on the analyses of sporo-pollen，grain size and accelerator mass spectrometric （AMS）¹⁴C dating data from Taohuajian profile in Ruicheng County，Shanxi Province，this paper discusses the ancient cultural date and the paleoenvironmental change since Late Mid-Holocene. The study provides reliable quantitative data for the reconstruction of paleoenvironment in this area. The result shows that the climate is accord with its neighbouring areas, and the ancient cultural date belongs to the period of Miaodigou culture. Three sporo-pollen assemblage zones are established through the stratigraphical changes of the sporo-pollen: the 5,250-5,000 aBP interval is a mild-wet climate with the landscape of sparse prairie vegetation; the 5,000-4,800 aBP interval is a cool-dry climate with wilderness prairie vegetation; after 4,800 aBP there is a cool-wet climate with sparse prairie vegetation.

Key words: Taohuajian profile, AMS 14C dating, sporopollen analysis, paleoenvironmental change

CLC Number:

P534.63

NI Ai-Wu,TIAN Ming-Zhong,XUE Xin-Ming,WANG Jin-Ping. The Sporo-pollen Analysis and Paleoenvironment Change in Taohuajian Profile of Ruicheng County, Shanxi Province Since Late Mid-Holocene[J]. Geoscience, 2011, 25(2): 349-355.

References

[1]任来义，符俊辉，林桂芳，等.孢粉化石的信息函数与古环境分析
[J].西北大学学报：自然科学版，2001,31(6):506-508.

[2]张俊牌，童敏，王书兵，等.太白山芳香寺剖面孢粉记录的古气候重建
[J].地质力学学报，2001，7(4)：315-320.

[3]孙湘君，罗运利，陈怀成.中国第四纪深海孢粉研究进展
[J].科学通报，2003，48(15)：1613-1621.

[4]许清海，肖举乐，中村俊夫，等.孢粉资料定量重建全新世以来岱海盆地的古气候
[J].海洋地质与第四纪地质，2003，23(4)：99-108.

[5]鞠远江，刘耕年.孢粉记录揭示的4 000 aBP来乌鲁木齐河源区气候环境变化
[J].冰川冻土，2004，26(2)：166-170.

[6]张玉兰.孢粉分析在环境考古中的应用
[J].上海地质，2005(1):15-17.

[7]齐乌云，梁中合，高立兵，等.山东沭河上游史前文化人地关系研究
[J].第四纪研究,2006,26(4):580-588.

[8]谢远云，李长安，王秋良，等.江陵地区全新世早期人类活动的孢粉记录
[J].地理科学，2008(2)：276-281.

[9]吴才阳，张威，穆克华.长白山白河800年来气候环境变化
[J].科技信息，2009(16):465-467.

[10]史凯.苏州澄湖SC1孔晚更新世晚期以来的古环境演变研究
[J].现代地质，2010,24(2):214-220.

[11]靳桂云，刘东生.华北北部中全新世降温气候事件与古文化变迁
[J].科学通报,2001,46(20):1725-1730.

[12]夏正楷，陈福友，陈戈，等.我国北方泥河湾盆地新-旧石器文化过渡的环境背景
[J].中国科学：D辑,2001,31(5):393-400.

[13]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.

[14]Conserva M E, Byrne R. Late Holocene vegetation change in the Sierra Madre Oriental of Central Mexico
[J]. Quaternary Research , 2002,58 (2):122-129.

[15]薛新明.山西芮城寺里—坡头遗址勘察与清凉寺墓地的重要收获
[J].文物世界，2004(3):3-5.

[16]山西省考古研究所，运城市文物局，芮城县文物局.山西芮城清凉寺新石器时代墓地
[J].文物，2006(3):4-17.

[17]王晓毅，薛新明.有关清凉寺墓地的几个问题
[J].文物，2006(3):63-65.

[18]任明达，王乃樑.现代沉积环境概论
[M].北京:科学出版社,1981:11.

[19]贾鑫，王琳，董广辉，等.中全新世关中陕北陇东地区文化演变及环境驱动力
[J].兰州大学学报：自然科学版,2008,44(6):8-14.

[20]Huang Chunchang，Jia Yaofeng,Pang Jiangli，et al.Holocene colluviation and its implications for tracing huanginduced soil erosion and redeposition on the piedmont loess lands of the Qinling Mountains,northern China
[J].Geoderma,2006, 136:838-851.

[21]Huang Chunchang，Pang Jiangli,Chen Shue,et al. Holocene dust accumulation and the formation of polycyclic cinnamon soils(luvisols)in the China Loess Plateau
[J].Earth Surface Processes and Landforms,2003,28(12):1259-1270.

[22]张宏彦.渭水流域全新世环境变化的初步研究：环境考古研究(第二辑)
[M].北京:科学出版社,2000：145-151.

[23]许靖华.太阳、气候、饥荒与民族大迁徙
[J].中国科学:D辑,1998,28(4):366-384.