• 中文核心期刊
  • 中国科技核心期刊
  • 中国科学引文数据库核心期刊
ZHANG Zongyan, LIU Xiang, LI Xiang, ZHANG Jianyu, KE Xue, XU Yadong. 2020: The Late Oligocene-Early Pleistocene sporopollen assemblages and paleovegetation succession of core ZkA01 in Hetou town, Leizhou Peninsula of Guangdong Province. Geological Bulletin of China, 39(6): 880-892. DOI: 10.12097/gbc.dztb-39-6-880
Citation: ZHANG Zongyan, LIU Xiang, LI Xiang, ZHANG Jianyu, KE Xue, XU Yadong. 2020: The Late Oligocene-Early Pleistocene sporopollen assemblages and paleovegetation succession of core ZkA01 in Hetou town, Leizhou Peninsula of Guangdong Province. Geological Bulletin of China, 39(6): 880-892. DOI: 10.12097/gbc.dztb-39-6-880

The Late Oligocene-Early Pleistocene sporopollen assemblages and paleovegetation succession of core ZkA01 in Hetou town, Leizhou Peninsula of Guangdong Province

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  • Received Date: October 20, 2019
  • Revised Date: May 21, 2020
  • Available Online: August 15, 2023
  • The data of Cenozoic sporopollen fossils obtained from ZKA01 drill hole in Leizhou Peninsula of Guangdong Province were systematically analyzed.Through the analysis of spore-pollen data, 8 sporopollen assemblages can be recognized from this drill hole.In the late Oligocene, the vegetation types in this area reflected the obvious vertical distribution of vegetation; coniferous forests were distributed in the surrounding mountains, and deciduous broad-leaved and evergreen broad-leaved mixed forests grew in the plain.In the early and middle Miocene, the vegetation types in this area evolved from deciduous broad-leaved and evergreen broad-leaved mixed forests into evergreen broad-leaved forests and tropical rainforests.In the late Miocene, the vegetation types in this area evolved into coniferous forests in mountain areas and deciduous broad-leaved and evergreen broad-leaved mixed forests in plain areas.During the Pliocene-Early Pleistocene period, the vegetation types in this area were deciduous broad-leaved and evergreen broad-leaved mixed forests, and the temperature changes fluctuated significantly.The climate change characteristics of Late Oligocene to Early Pleistocene period were reflected by spore-pollen assemblages, which had good comparability with the trend of global climate change.

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