地理学报 ›› 1987, Vol. 42 ›› Issue (4): 289-298.doi: 10.11821/xb198704001

• 论文 •    下一篇

中国东部第四纪自然环境演化及庐山“冰碛层”堆积时期的自然环境研究

黄培华1, 陆仲家1, 任振纪2, 朱凤冠3   

  1. 1. 中国科学技术大学
    2. 河北师范大学
    ;3. 国家海洋局第二海洋研究所
  • 出版日期:1987-10-15 发布日期:1987-10-15
  • 基金资助:
    中国科学院科学基金资助的课题

EVOLUTIONS OF QUATERNARY NATURAL ENVIRONMENT IN THE EASTERN CHINA AND NATURAL ENVIRONMENT OF "QUATERNARY GLACIATION" IN MT.LUSHAN

Huang Peihua1, Lu Zhongjia1, Ren Zhenji2, Zhu Fengguan3   

  1. 1. University of Science and Technology of China;
    2. Hebei Normal University;
    3. Second Inititute of Oceanography
  • Online:1987-10-15 Published:1987-10-15

摘要: 根据第四纪地层内孢粉组合和动物群等新资料恢复了我国东部各大区域第四纪各个时期的自然环境特征,其温暖期与干冷期的交替与深海沉积O18温度变化趋势大致对应。庐山三次“冰期冰碛层”内孢粉组合表明均为温暖湿润针阔叶混交林景观,而不是寒冷的冰川环境。

关键词: 动植物群, 自然环境变化, 庐山冰川问题

Abstract: Environmental evolutions in the eastern China have the hollowing characters: 1. Quaternary environmental changes are mainly controlled by global climatic variations. 2. The sensitive regions of environmental changes are between the middle part of Northeast China and the middle part of Central China. The environmental variations of the former were between the forest-tundra of cool temperate zone and the deciduous broadleaved forest of warm temperate zone, and those of the latter were between the broadleaved forest with grassland of warm temperate zone and the broadleaved evergreen forest of south subtropic zone. 3. The coldest and dry climate appeared about 18000-15000 years ago in Late-Pleistocene, When the annual average temperature decreased about 8℃ compared with that of today, and the natural environmental zones moved southward about 1000 km in Northeast China and North China. The hottest and wet climate appeared in middle Pleistocene, when the temperature increased 4℃ compared with that of to-day and natural environmental zones moved northward about 700 km in North China. 4. The general tendency of Quaternary environmental variations was to become dry and the continentality of climate was from strength to strength in the eastern China during Quaternary. 5. The natural environmental variations of the southern part of Central China and South China were smaller than those to the north of them, and the tempertural variations were about 3-5℃ 6. We found that the sporo-pollen assemblages in the "glacial boulder clay beds" of Mt. Lushan and Huangshan all belong to warm and wet forest environment, There fore, the problem of glaciation in Mt. Lushan and Huangshan is questionable.

Key words: Fauna and flora, Environmental variations, Environment of "Quaternary gliciations" in Mt. Lushan