| 松嫩平原晚第三纪—更新世孢粉组合及古植被与古气候的研究 |
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| 引用本文： | 夏玉梅,汪佩芳.松嫩平原晚第三纪—更新世孢粉组合及古植被与古气候的研究[J].地理学报,1987(2). |
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| 作者姓名： | 夏玉梅 汪佩芳 |
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| 作者单位： | 中国科学院长春地理研究所
(夏玉梅)，中国科学院长春地理研究所(汪佩芳) |
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| 基金项目： | 中国科学院基金课题的研究成果之一 |
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| 摘 要： | 本文通过大庆、乾安、长春、哈尔滨等地所揭示孢粉资料,试将松嫩平原晚第三纪到更新世时期划出13个孢粉带。根据孢粉组合系列变化和磁性地层测定,论述古植被与古气候演化过程,为研究东北平原第四纪自然环境变迁提供科学依据。
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| 关 键 词： | 松嫩平原 孢粉组合 晚第三纪 更新世 |
THE PALEOBOTANY AND PALEOOLIMATE IN THE SONGNEN PLAIN: A STUDY ON THE LATE TERTIARY-PLEISTOCENE SPORE POLLEN ASSEMBLAGES |
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| Xia Yumei Wang Peifang.THE PALEOBOTANY AND PALEOOLIMATE IN THE SONGNEN PLAIN: A STUDY ON THE LATE TERTIARY-PLEISTOCENE SPORE POLLEN ASSEMBLAGES[J].Acta Geographica Sinica,1987(2). |
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| Authors: | Xia Yumei Wang Peifang |
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| Abstract: | On the basis of the dating of the spore-pollen analysis from drilling cores and outcrop sections of Qianan, Daging, Fuyu, Harbin, Changchun, Longjiang in the Songnen Plain, the period of the late Tertiary-Pleistocene was divided into 13 spore-pollen assemblages. During the late Tertiary tree pollen dominated and during the Pleistocene herb pollen dominated.
According to the charesteristics of spore pollen assemblages and paleomagnetics and 14C dating, the succession of the paleibotany and paleoclimate in the region is as follows:
(1) In the early epoch of the late Tertiary, the Pinus, Tsuga, Ulmus, Carya represented a mixed evergreen conifer-broad leaf deciduous forest, which belong to warm and humid climate. At the end of the late Tertiary, Pinus and Picea with a number of broad-leaf species formed a mixed temperate conifer-broad leaf forest with steppe type vegetation occurring in part; the climate had changed from warm and wet to mild and dry.
(2) In the Pleistocene period, the vegetation in the region was dominated by temperate park steppe, meadow-steppe and steppe. In addition, the dark coniferous forest was distributed in isolated islands. During late Pleistocene epoch, the periglacial vegetation was distributed extensively, as the Climate of this period got drier and cooler. |
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| Keywords: | : Songnen plain Spore-pollen assemblages Late Tertiary Pleistocene |
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