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Larson 1991
Larson, R.L. (1991). Geological Consequences of Superplumes. Geology 19(10): 963-966.
Superplumes are suggested to have caused the period of constant normal magnetic polarity in mid-Cretaceous time (124-83 Ma) and, possibly, the period of constant reversed polarity in Pennsylvanian-Permian time (323-248 Ma). These times coincide with increases in world temperature, deposition of black shales, oil generation, and eustatic sea level in the mid-Cretaceous, and increased coal generation and gas accumulation in the Pennsylvanian-Permian, accompanied by an intracratonic Pennsylvanian transgression of epicontinental seas. These geologic anomalies are associated with episodes of increased world-wide ocean-crust production and mantle outgassing, especially of carbon and nutrients. These superplumes originated just above the core-mantle boundary, significantly increased convection in the outer core, and stopped the magnetic field reversal process for 41 m.y. in the Cretaceous and 75 m.y. in Pennsylvanian-Permian time.
BACKGROUND DATA FILES

Abstract
Abstract

Keywords
sea-level changes, climate, reversals, tectonics, field
Journal
Geology
http://www.gsajournals.org/gsaonline/?request=search-simple
Publisher
The Geological Society of America
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