Late Paleozoic tropical climate response to Gondwanan deglaciation
Late Paleozoic tropical climate response to Gondwanan deglaciation
Geology (Boulder) (September 2007) 35 (9): 771-774
- ancient ice ages
- arid environment
- biomes
- carbon dioxide
- Carboniferous
- climate change
- data processing
- deglaciation
- digital simulation
- general circulation models
- GENESIS model
- glacial extent
- Gondwana
- numerical models
- paleoatmosphere
- paleoclimatology
- paleoecology
- paleohydrology
- Paleozoic
- Pangaea
- Permian
- terrestrial environment
- theoretical models
- tropical environment
- upper Paleozoic
- vegetation
- BIOME4
Coupled climate-biome model simulations of the late Paleozoic were developed to determine the response of Pangean tropical climate to Gondwanan deglaciation. The model simulations predict substantial changes over equatorial Pangea including continental drying, a reversal of equatorial winds, warming, heavier delta (super 18) O values of meteoric precipitation, and the expansion of deserts and the contraction of forests. The magnitude of these tropical responses is sensitive to the extent of Gondwana continental ice and the deglacial rise in atmospheric pCO (sub 2) , boundary conditions that are not well known for the late Paleozoic. Nonetheless the model predictions are consistent with climatic and environmental trends determined from terrestrial proxy data, implying that the deglaciation of Gondwana was a transformational climate event in tropical Pangea.