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  • The PC-C boundary interval represents one of the critical phases in the evolution of life. Any outside observer considering the approximately 4500-million-year history of our planet would likely choose the 150 Ma time interval between 650 and 500 Ma as one of the most dramatic periods in Earth history. This period connects the Proterozoic and Phanerozoic Eons with its boundary at 542 Ma. It includes the Ediacaran (ca 630-542 Ma) and the Cambrian (542-493 Ma) periods. The Ediacaran, in particular, is characterized by concurrent profound changes in global tectonics, possibly the largest climatic deviation from the steady-state mean global temperature since the Archean (popularized by the %22Snowball Earth%22 concep), the first evidence leading to the possibly %22explosive%22 (on a geological scale) but indisputably largest evolutionary radiation event of the biosphere, and a significant increase of free atmospheric and oceanic oxygen. The subsequent Cambrian time interval largely records the gradual establishment of a newly acquired ecologic stability, the beginning of the metazoan conquest of Earth's surface environment, and a profound rearrangement in the chemical composition of Earth's atmosphere and oceans.
  • The PC-C boundary interval represents one of the critical phases in the evolution of life. Any outside observer considering the approximately 4500-million-year history of our planet would likely choose the 150 Ma time interval between 650 and 500 Ma as one of the most dramatic periods in Earth history. This period connects the Proterozoic and Phanerozoic Eons with its boundary at 542 Ma. It includes the Ediacaran (ca 630-542 Ma) and the Cambrian (542-493 Ma) periods. The Ediacaran, in particular, is characterized by concurrent profound changes in global tectonics, possibly the largest climatic deviation from the steady-state mean global temperature since the Archean (popularized by the %22Snowball Earth%22 concep), the first evidence leading to the possibly %22explosive%22 (on a geological scale) but indisputably largest evolutionary radiation event of the biosphere, and a significant increase of free atmospheric and oceanic oxygen. The subsequent Cambrian time interval largely records the gradual establishment of a newly acquired ecologic stability, the beginning of the metazoan conquest of Earth's surface environment, and a profound rearrangement in the chemical composition of Earth's atmosphere and oceans. (en)
Title
  • The Precambrian-Cambrian biosphere (r)evolution: Insights from the Chinese Yangtze Platform
  • The Precambrian-Cambrian biosphere (r)evolution: Insights from the Chinese Yangtze Platform (en)
skos:prefLabel
  • The Precambrian-Cambrian biosphere (r)evolution: Insights from the Chinese Yangtze Platform
  • The Precambrian-Cambrian biosphere (r)evolution: Insights from the Chinese Yangtze Platform (en)
skos:notation
  • RIV/00216208:11310/12:10132471!RIV13-MSM-11310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I
http://linked.open...iv/cisloPeriodika
  • 1
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http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 160924
http://linked.open...ai/riv/idVysledku
  • RIV/00216208:11310/12:10132471
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Yangtze Craton; Precambrian; Cambrian; animal embryos; invertebrates (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [16AC08DB4B04]
http://linked.open...i/riv/nazevZdroje
  • Bulletin of Geosciences
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 87
http://linked.open...iv/tvurceVysledku
  • Fatka, Oldřich
  • Steiner, Michael
  • Weber, Bernd
  • Zhu, Maoyan
http://linked.open...ain/vavai/riv/wos
  • 000301056900006
issn
  • 1214-1119
number of pages
http://bibframe.org/vocab/doi
  • 10.3140/bull.geosci.1346
http://localhost/t...ganizacniJednotka
  • 11310
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