Earth & Ediacaran - Unionpedia, the concept map
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Difference between Earth and Ediacaran
Earth vs. Ediacaran
Earth is the third planet from the Sun and the only astronomical object known to harbor life. The Ediacaran is a geological period of the Neoproterozoic Era that spans 96 million years from the end of the Cryogenian Period at 635 Mya to the beginning of the Cambrian Period at 538.8 Mya.
Similarities between Earth and Ediacaran
Earth and Ediacaran have 10 things in common (in Unionpedia): Cambrian explosion, Fossil, Geologic time scale, Ice age, Neoproterozoic, Paleontology, Pannotia, Proceedings of the National Academy of Sciences of the United States of America, Snowball Earth, Tidal acceleration.
Cambrian explosion
The Cambrian explosion (also known as Cambrian radiation or Cambrian diversification) is an interval of time approximately in the Cambrian period of the early Paleozoic when a sudden radiation of complex life occurred, and practically all major animal phyla started appearing in the fossil record.
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Fossil
A fossil (from Classical Latin) is any preserved remains, impression, or trace of any once-living thing from a past geological age.
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Geologic time scale
The geologic time scale or geological time scale (GTS) is a representation of time based on the rock record of Earth.
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Ice age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers.
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Neoproterozoic
The Neoproterozoic Era is the unit of geologic time from 1 billion to 538.8 million years ago.
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Paleontology
Paleontology, also spelled palaeontology or palæontology, is the scientific study of life that existed prior to the start of the Holocene epoch (roughly 11,700 years before present).
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Pannotia
Pannotia (from Greek: pan-, "all", -nótos, "south"; meaning "all southern land"), also known as the Vendian supercontinent, Greater Gondwana, and the Pan-African supercontinent, was a relatively short-lived Neoproterozoic supercontinent that formed at the end of the Precambrian during the Pan-African orogeny (650–500 Ma), during the Cryogenian period and broke apart 560 Ma with the opening of the Iapetus Ocean, in the late Ediacaran and early Cambrian.
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Proceedings of the National Academy of Sciences of the United States of America
Proceedings of the National Academy of Sciences of the United States of America (often abbreviated PNAS or PNAS USA) is a peer-reviewed multidisciplinary scientific journal.
Earth and Proceedings of the National Academy of Sciences of the United States of America · Ediacaran and Proceedings of the National Academy of Sciences of the United States of America · See more »
Snowball Earth
The Snowball Earth is a geohistorical hypothesis that proposes during one or more of Earth's icehouse climates, the planet's surface became nearly entirely frozen with no liquid oceanic or surface water exposed to the atmosphere.
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Tidal acceleration
Tidal acceleration is an effect of the tidal forces between an orbiting natural satellite (e.g. the Moon) and the primary planet that it orbits (e.g. Earth).
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The list above answers the following questions
- What Earth and Ediacaran have in common
- What are the similarities between Earth and Ediacaran
Earth and Ediacaran Comparison
Earth has 577 relations, while Ediacaran has 128. As they have in common 10, the Jaccard index is 1.42% = 10 / (577 + 128).
References
This article shows the relationship between Earth and Ediacaran. To access each article from which the information was extracted, please visit: