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During the Phanerozoic (the last ~0.5 billion years), the Earth has experienced massive changes in climate, spanning the extensive glaciations of the Permo-Carboniferous (~300 million years ago), to the mid-Cretaceous super-greenhouse (~100 million y
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d49acaa6155481cc39267ea4d6221e26
https://doi.org/10.5194/egusphere-egu23-9574
https://doi.org/10.5194/egusphere-egu23-9574
Mammals have dominated the Earth for the last ~55 Myr. Mammals have shown remarkable adaptation and resilience to climate change. However, it is unknown how long the Earth will be able to continue to sustain mammalian life. Estimates suggest the ulti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3da878446a535900f4a68e5663d1ef93
https://doi.org/10.5194/egusphere-egu23-5383
https://doi.org/10.5194/egusphere-egu23-5383
The severe “Snowball Earth” glaciations proposed to have existed during the Cryogenian period (720 to 635 million years ago) coincided with the breakup of one supercontinent (Rodinia) and assembly of another (Pannotia). The presence of extensive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e6f520e4ee195c498cc90f08e705d3b
https://doi.org/10.5194/egusphere-egu21-1354
https://doi.org/10.5194/egusphere-egu21-1354
Autor:
Chris Scotese, Rob Van der Voo
Publikováno v:
Geology. 10:487
Autor:
Rob Van der Voo, Chris Scotese
Publikováno v:
Geology. 9:583
Middle to Late Devonian paleomagnetic data from cratonic North America and Europe indicate that a 2,000-km sinistral displacement occurred between these two continents during Carboniferous time. Because the Lewisian basement of northwest Scotland and
Autor:
Rob Van der Voo, Chris Scotese
Publikováno v:
Geology. 10:606