The Cretaceous–Paleogene (K–Pg) transition saw mass extinctions in terrestrial and marine ecosystems.
Terrestrial vertebrate diversity patterns across the K–Pg boundary have been
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The Cretaceous–Paleogene (K–Pg) transition saw mass extinctions in terrestrial and marine ecosystems.
Terrestrial vertebrate diversity patterns across the K–Pg boundary have been
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Syesis: Vol. 8, Supplement 1: Vegetation and Environment of the Coastal Western Hemlock Zone in Strathcona Provincial Park, British Columbia, Canada
byThe Royal British Columbia MuseumAudiobook
The Permian Period: The History and Legacy of the Era with the Largest Mass Extinction Event
byCharles River EditorsEbook
PLANT FOSSIL ATLAS from (Pennsylvanian) CARBONIFEROUS AGE FOUND in Central Appalachian Coalfields
byThomas F. McloughlinAudiobook
The Silurian Period: The History of the Prehistoric Era When Life Formed on Land
byCharles River Editors