The Cambrian impact hypothesis

dc.creatorZhang, Weijia
dc.date2008-09-01
dc.date.accessioned2026-07-07T10:01:38Z
dc.date.available2026-07-07T10:01:38Z
dc.descriptionAfter a thorough research on the circumstantial changes and the great evolution of life in the Cambrian period, the author propounds such a hypothesis: During the Late Precambrian, about 500-600Ma, a celestial body impacted the Earth. The high temperature ended the great glaciation, facilitated the communication of biological information. The rapid change of Earth environment enkindled the genesis-control system, and released the HSP-90 variations. After the impact, benefited from the protection of the new ozone layer and the energy supplement of the aerobic respiration, those survived underground life exploded. They generated carapaces and complex metabolism to adjust to the new circumstance of high temperature and high pressure. This article uses a large amount of analyses and calculations, and illustrates that this hypothesis fits well with most of the important incidences in astronomic and geologic discoveries.
dc.description15 pages, 4 figures, 4 tables. Supported by National Innovative Test Program
dc.identifierhttps://arxiv.org/abs/0809.0179
dc.identifierhttp://arxiv.org/abs/0809.0179
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/168692
dc.subjectGeneral Physics
dc.titleThe Cambrian impact hypothesis
dc.typetext

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