Reduction of equatorial land area and silicate weathering consumption of CO<sub>2</sub> with transformation from Pangea B to Pangea A in the Permian and the ultimate demise of the Late Paleozoic Ice Age

Kent, Dennis

Reduction of equatorial land area and silicate weathering consumption of CO₂ with transformation from Pangea B to Pangea A in the Permian and the ultimate demise of the Late Paleozoic Ice Age

Dennis V Kent, Rutgers University New Brunswick, EPS, New Brunswick, NJ, United States; Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, United States and Giovanni Muttoni, University of Milan, Department of Earth Sciences 'Ardito Desio', Milan, Italy

Reduction of equatorial land area and silicate weathering consumption of CO2 with transformation from Pangea B to Pangea A in the Permian and the ultimate demise of the Late Paleozoic Ice Age

Reduction of equatorial land area and silicate weathering consumption of CO₂ with transformation from Pangea B to Pangea A in the Permian and the ultimate demise of the Late Paleozoic Ice Age