元古代泥球地球与非光合作用产生的过量氧气

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引用次数: 0

摘要

根据地球尺度的顶部模型,地球的轴线在27亿到9亿年前大约倾斜了18亿年。这导致了赤道地区的冻结和对泥球地球的认识,解释了彭古拉、休伦、斯图亚特、马里诺和冈瓦纳冰期以及地球上许多其他历史事件。氮、氧和水是由于高温高压下的核嬗变而形成的假说表明,光合作用产生了过量的氧气,氮和水通过一个开放系统从上地幔的岩浆库中释放到大气中,这一系统在海洋岛屿上造成了火山。在过去的4亿年里,大气中氧浓度的演变导致了生命的发展,这可以用岩浆库被阻塞时通过开放系统释放到平流层的氮来解释。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Proterozoic Slushball Earth and Generation of Excess Oxygen not achieved by Photosynthesis
According to the Earth-scale top model, the Earth’s axis was tilted approximately 1.8 billion years between 2.7 billion to 900 million years ago. This resulted in the freezing of the equatorial zone and the recognition of a Slushball Earth, explaining the Pongola, Huronian, Sturtian, Marinoan, and Gondwana -glaciations as well as numerous other historical events of the Earth. The hypothesis that nitrogen, oxygen, and water were formed due to nuclear transmutation at high temperatures and pressures, suggests that excess oxygen was produced during photosynthesis and nitrogen and water were expelled into the atmosphere from magma reservoirs in the upper mantle through an open system which caused volcanoes in ocean islands. The evolution of atmospheric oxygen concentration leading to the development of life over the past 400 million years, can be explained by the nitrogen released into the stratosphere through open systems while the magma reservoirs are blocked.
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