期刊文献+

长江三角洲地区全新世以来环境变迁对人类活动的影响 被引量:15

IMPACT OF ENVIRONMENTAL CHANGES ON HUMAN ACTIVITIES DURING THE HOLOCENE IN THE CHANGJIANG (YANGTZE)RIVER DELTA REGION
在线阅读 下载PDF
导出
摘要 对长江三角洲地区搜集的泥炭、贝壳砂堤、埋藏古树的测年数据 ,新石器时代考古遗址点的测年资料以及海拔高程等的分析表明 :新石器时代人类的生产和生活与生态环境变迁有密切关系 ,表现出人类活动对环境变迁的适应。马家浜时期气候潮湿 ,地面水域扩大 ,房屋大多以干栏式为主 ,而且遗址大多分布在山坡和湖汊岸边稍高的岗地、土墩上 ;崧泽文化期湖泊沼泽比较多 ,遗址多建于河湖间高爽处 ;良渚文化时期泥炭埋藏点的分布较马家浜与崧泽文化时期少 ,而且距离湖泊较远 ,表明当时地理环境有所好转 ,适宜人类生活的空间变得更为宽广 ,遗址的分布开始分散。对古遗址高程以及埋藏古树、泥炭14 C年龄数据统计分析结果表明 ,新石器时代人类居住高程与地面水域扩张和缩小状况相一致。同时 ,研究结果也表明影响人们居住地高低的因素较多 ,先人们的“择高而居”在某种程度上也只是部分地防止海水倒灌及台风和洪水灾害的侵害而采取的一种解决手段 ,而不是全部 。 Collection and analysis were performed on dating data of peat, shells, fossil trees and the dating data and altitude of the Neolithic sites in the Yangtze River delta. The research results indicate that there exists close correlation between human activities and the environmental changes, showing the human adaptation to the climatic changes. Climate during the Majiabang cultural period was humid and warm. The expansion of ground surface water led to the appearance of pole-supported houses. People chose higher positions to live in to avoid negative impacts from excessive precipitation and humid environmental conditions. This also occurred in the Songze cultural periods. The scarce distribution of the peat points during the Songze cultural period indicated a relatively cool and dry climate condition. This was profitable for shrinking of ground surface water area. The large area of exposed land provided enough space for human activities. Analysis performed on altitude of the Neolithic cultural sites and the ()^(14)C data of the buried paleo-trees and peat demonstrated that the height of human living places was in close relation to the expansion and shrinking of the ground surface water area. And at the same time, the driving factors impacting the height of the human living places were numerous and various. The living-high style was just a countermeasure partly for preventing the negative impacts such as typhoon, storm tide and flood disasters. Religious ceremony and superstitious activities and faiths served as part of the human′s living-high during the Neolithic cultural periods.
出处 《海洋地质与第四纪地质》 CAS CSCD 北大核心 2004年第4期9-15,共7页 Marine Geology & Quaternary Geology
基金 中国博士后基金 中国科学院王宽诚博士后教育基金 中国科学院知识创新工程重要方向项目 (KZCX3 SW 3 3 1) 中国科学院南京地理与湖泊研究所知识创新工程所长专项基金(SS2 2 0 0 0 7)
关键词 测年 全新世 人类活动 气候潮 高程 环境变迁 台风 地面水 湖泊 ^14C environment evolution the Neolithic culture human activities the Yangtze River delta
  • 相关文献

参考文献35

  • 1于世永,朱诚,史威.上海马桥地区全新世中晚期环境演变[J].海洋学报,1998,20(1):58-64. 被引量:20
  • 2施少华.中国全新世高温期环境与新石器时代古文化的发展[A].中国全新世大暖期气候与环境[C].北京:海洋出版社,1992.
  • 3张晓阳,蔡述明,孙顺才.全新世以来洞庭湖的演变[J].湖泊科学,1994,6(1):13-21. 被引量:47
  • 4Ovenden L. Peat accumulation in northern wetlands [J]. Quaternary Research, 1990, 33: 377-386.
  • 5钟金岳,张则友.我国沿海地区的埋藏泥炭及其形成的古地理[J].海洋与湖沼,1981(5):412-421. 被引量:7
  • 6Oertel G F, Kraft J C, Kearney M S, et al. A rational theory for barrier-lagoon development[A]. Quaternary Coasts of the United States: Marine and Lacustrine Systems[C]. Society of Economic Paleontologists and Mineralogists (SEPM Special Publication No. 48), 1992.77-87.
  • 7Jordan J W, Mason O K. A 5 000 year record of intertidal peat stratigraphy and sea level change from northwest Alaska [J].Quaternary International, 1999, 60: 37-47.
  • 8Miller N G,Futyma R P. Paleohydrological implication of Holocene peatland development in Northern Michigan[J]. Quaternary Research, 1987, 27:297 311.
  • 9孙顺才.太湖平原有全新世海侵吗?[J].海洋学报,1992,14(4):69-77. 被引量:11
  • 10刘苍字 吴立成 等.长江三角洲南部古沙堤(冈身)的沉积特征、成因及年代[J].海洋学报,1985,7(1):55-66.

二级参考文献157

共引文献400

同被引文献376

引证文献15

二级引证文献106

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部