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The Earth evolution as a thermal system
Author(s) -
Tang Chunan,
Li Sanzhong
Publication year - 2016
Publication title -
geological journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.721
H-Index - 54
eISSN - 1099-1034
pISSN - 0072-1050
DOI - 10.1002/gj.2748
Subject(s) - lithosphere , magmatism , geology , snowball earth , earth science , volcanism , crust , tectonics , earth (classical element) , extinction event , geophysics , paleontology , population , mathematical physics , biological dispersal , physics , demography , sociology , glacial period
Cooling and warming has occurred many times during the Earth's history. At times, the Earth has entirely frozen to form a ‘snowball’, while at others, it has become extremely hot, resulting in the mass extinction of species. However, despite 50 years of established plate tectonic theory, the reasons that these patterns and extremes of cooling and warming have occurred remain elusive. Here, we propose a new model of the evolution of the Earth's temperature that explains the planet's thermal cycles in terms of changes in the heat balance of the system. The expansion of the lithosphere and its associated uplift lead to the collapse of Earth's crust, and volcanism and magmatism are the global‐scale response. These shallow lithospheric processes can reach a critical state with a positive feedback loop, resulting in the formation of large igneous provinces, which remove huge heat from lavas by radiating into outer space. Endothermic phase changes during the de‐compressive melting also absorb large quantities of heat from the inner Earth and cool their surroundings. This process may terminate the warming cycle and initiate a new cooling cycle, possibly an ice age. Copyright © 2016 John Wiley & Sons, Ltd.