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摘要:
Although the paleoclimate of the marine Cretaceous has been well studied, the paleoclimate of the non-marine is still not well understood. The Songliao Basin was one of the largest non-marine rift basins during Cretaceous. The Well-preserved Cretaceous lacustrine deposits in this basin provide a unique opportunity to study terrestrial paleoenvironments and paleoclimate during the Late Cretaceous. Here, the microfossils from the Late Turonian Qingshankou Formation of the Songliao Basin were used to investigate the paleoenvironments and paleoclimate of east Asia. There are two spore and pollen assemblages recognized: a Cedripites-Cyathidites-Classopollis assemblage from Upper Member 1, and a Cedripites-Cyathidites-Classopollis assemblage from Lower Member 2 of the Qingshankou Formation, respectively. Besides, relatively abundant ostracods have been identified. In the Songliao Basin, the climate was relatively warm and wet during Late Turonian, with good source rock deposited in the Songliao lake.
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篇名 Late Turonian Microfossils and Paleoclimate in the Songliao Basin, NE China
来源期刊 地质学期刊(英文) 学科 地球科学
关键词 Cretaceous Songliao Basin SPORE and Pollen PALEOCLIMATE
年,卷(期) 2019,(10) 所属期刊栏目
研究方向 页码范围 605-608
页数 4页 分类号 P5
字数 语种
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Cretaceous
Songliao
Basin
SPORE
and
Pollen
PALEOCLIMATE
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研究分支
研究去脉
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地质学期刊(英文)
月刊
2161-7570
武汉市江夏区汤逊湖北路38号光谷总部空间
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585
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0
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