WANG Ye, YAN Xiaodong. The Study Progress on the Earth’s Climate during the Neoproterozoic[J]. Climatic and Environmental Research, 2011, 16(3): 399-406. DOI: 10.3878/j.issn.1006-9585.2011.03.15
Citation:
WANG Ye, YAN Xiaodong. The Study Progress on the Earth’s Climate during the Neoproterozoic[J]. Climatic and Environmental Research, 2011, 16(3): 399-406. DOI: 10.3878/j.issn.1006-9585.2011.03.15
WANG Ye, YAN Xiaodong. The Study Progress on the Earth’s Climate during the Neoproterozoic[J]. Climatic and Environmental Research, 2011, 16(3): 399-406. DOI: 10.3878/j.issn.1006-9585.2011.03.15
Citation:
WANG Ye, YAN Xiaodong. The Study Progress on the Earth’s Climate during the Neoproterozoic[J]. Climatic and Environmental Research, 2011, 16(3): 399-406. DOI: 10.3878/j.issn.1006-9585.2011.03.15
The Study Progress on the Earth’s Climate during the Neoproterozoic
A strong global glaciation took place on the Earth in Neoproterozoic. The evidences and characteristics of the glaciation during the Neoproterozoic is reviewed first while the mechanism of the glaciation is discussed. Then the models of the “Snowball Earth” and the effects of the glaciation on early life growth are summarized. Finally, the future development trend of “Snowball Earth” is forecasted.
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