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Der Name ist von der Kenora-Orogenese abgeleitet, die vor rd. Kenorland bestand im Wesentlichen aus dem Kanadischen Schild , d.

Also, there is speculation based on the rift margin spatial arrangements of Laurentia, that at some time during the breakup, the Slave and Superior cratons were not part of the supercontinent Kenorland, but, by then may have been two different Neoarchaean landmasses supercratons on opposite ends of a very large Kenorland.

This is based on how drifting assemblies of various constituent pieces should flow reasonably together toward the amalgamation of the new subsequent continent.

The Slave and Superior cratons now constitute the northwest and southeast portions of the Canadian Shield , respectively. The breakup of Kenorland was contemporary with the Huronian glaciation which persisted for up to 60 million years.

The banded iron formations BIF show their greatest extent at this period, thus indicating a massive increase in oxygen build-up from an estimated 0.

The rise in oxygen levels caused the virtual disappearance of the greenhouse gas methane oxidized into carbon dioxide and water. The simultaneous breakup of Kenorland generally increased continental rainfall everywhere, thus increasing erosion and further reducing the other greenhouse gas, carbon dioxide.

Despite the anoxia indicated by the BIF, photosynthesis continued, stabilizing climates at new levels during the second part of the Proterozoic Era.

North America. South America. Harold Williams, Paul F. Hoffman, John F. Lewry, James W. Monger und Toby Rivers: Anatomy of North America: thematic geologic portrayals of the continent.

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