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Continental landmasses, Laurentia, Baltica, and Avalonia, collided to form Euramerica, leading to a major mountain building event, the Acadian orogeny which contributed to building the Appalachians and the Caledonide mountains.
The western margin of Laurentia/Euramerica was passive until the late Devonian when the Antler orogeny began, marking the beginning of subduction along the Cordilleran mobile belt that has continued to today.
Climate became much warmer after the Ordovician glaciation, which allowed reefs to make a come back during middle paleozoic. These reefs deposited on the passive margins of Laurentia in between mountain building events. However, another ice age and mass extinction came at the end of the Devonian period, which once again devastated the reefs.
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0:00 Mid Paleozoic Geology Summary
1:29 Paleogeography
2:51 Acadian Orogeny
5:28 Appalachian & Caledonian Mountains
6:03 Antler Orogeny
8:04 Warming, Drying, & Reefs
11:44 Paleozoic Deposition Pattern
13:09 Ice Age & Extinction
14:43 Related videos & references
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