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The Info List - Euramerica



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(i)

EURAMERICA (also known as LAURUSSIA (not to be confused with Laurasia ), the OLD RED CONTINENT or the OLD RED SANDSTONE CONTINENT) was a minor supercontinent created in the Devonian as the result of a collision between the Laurentian , Baltica , and Avalonia cratons ( Caledonian orogeny ), 433 million years ago. In the Late Carboniferous , tropical rainforests lay over the equator of Euramerica. A major, abrupt change in vegetation occurred when the climate aridified. The forest fragmented and the lycopsids which dominated these wetlands thinned out, being replaced by opportunistic ferns. There was also a great loss of amphibian diversity and simultaneously the drier climate spurred the diversification of reptiles.

CONTENTS

* 1 Extent * 2 Events by period * 3 See also * 4 References * 5 External links

EXTENT

Euramerica
Euramerica
in the Devonian

Euramerica
Euramerica
became a part of the major supercontinent Pangaea in the Permian . In the Jurassic , when Pangaea rifted into two continents , Gondwana and Laurasia
Laurasia
, Euramerica
Euramerica
was a part of Laurasia.

In the Cretaceous , Laurasia
Laurasia
split into the continents of North America and Eurasia . The Laurentian craton became a part of North America while Baltica became a part of Eurasia , and Avalonia was split between the two.

EVENTS BY PERIOD

* Carboniferous: Climate change devastated tropical rainforests, fragmen