Archean Paleo-climate: The first snowball?
Hector Javier Durand-Manterola

TL;DR
This paper explores the possibility that during the Archean Eon, Earth was a frozen 'snowball' planet, yet still supported life and sediment formation, challenging the traditional clement climate assumption.
Contribution
It presents an alternative 'snowball' Earth scenario supported by reinterpretation of geological evidence and a mathematical model questioning the inevitability of ice-albedo feedback.
Findings
Life could have existed in ocean depths beneath ice cover.
Sediments could form in isolated liquid water cavities.
The model suggests Earth defrosted at the end of the Proterozoic.
Abstract
The model accepted is one where during the Archean Eon the Earths climate was clement despite the weaker Sun. The observational evidence that supports this concept is: the emergence of life, the existence of evaporitic sediments and the presence of terrigenous sediments, all of which require liquid water and clement conditions. A theoretical argument used to support this idea is the so called ice-albedo feedback, which states that if the Earth was frozen, it would still be frozen.The aim of this document is to present an alternative scenario in which a frozen world, "snowball" style, with liquid water at the bottom of the sea, also allows for the emergence of life and evaporitic and terrigenous sedimentation. Archean climatic evidence, available at present, is discussed and can be reinterpreted to support the idea that, in Archean times, the surface of the Earth was frozen. Also, a…
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Taxonomy
TopicsPaleontology and Stratigraphy of Fossils · Astro and Planetary Science · Geology and Paleoclimatology Research
