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- The Devonian has been regarded as largely warm and equable, with a disastrous drop in temperatures in the Late Devonian leading to the Frasnian-Famennian "mass extinction".
- The climate of the Early Devonian is rather strongly zonal.
- In the Late Devonian, the southern "cool temperate" zone expands, with indications of glacial ice in parts of far western Gondwana (northern South America).
- However, the northern temperate zone appears to retreat before a subtropical zone which extends almost to 60° N.
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