| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9530360 | Geochimica et Cosmochimica Acta | 2005 | 19 Pages |
Abstract
The Permian was characterized by low sea levels, icehouse conditions, and southern hemisphere glaciation. Such conditions, analogous to the present ice age, and the similarities between Permian seawater and modern seawater, all suggest that general Phanerozoic supercycles, driven by mantle convection and global volcanicity, also control the major-ion chemistry of seawater.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Tim K. Lowenstein, Michael N. Timofeeff, Volodymyr M. Kovalevych, Juske Horita,