Where did the paleoequator pass during the Devonian Period?

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Devonian paleogeography — Devonian Period Distribution of landmasses, mountainous regions, shallow seas, and deep ocean basins during the early Devonian Period. Included in the paleogeographic reconstruction are the locations of the interval's subduction zones.

During the Devonian Period, there is general scientific agreement that the paleoequator crossed through the northern part of the supercontinent Laurussia, specifically passing through North America and China, which existed as a separate landmass at that time.12

While this is the consensus, it is important to note that paleomagnetic data for the period remains conflicting, and various specific positions for the paleoequator have been proposed by researchers. Because of these inconsistencies, modern efforts to reconstruct the geography of the Devonian often rely on analyzing the distribution of climate-sensitive rock types—such as evaporites, carbonates, and corals—rather than relying solely on paleomagnetic evidence.1