Final answer:
The late Paleocene torrid age was caused by a lack of land along the equator, less reflection from surfaces no longer covered in snow, large outpourings of volcanic activity that contributed greenhouse gases, and a change in density differentiation. These factors led to an increase in global temperatures.
Step-by-step explanation:
The late Paleocene torrid age was caused by a combination of the following:
- A lack of land along the equator
- Less reflection from surfaces no longer covered in snow
- Large outpourings of volcanic activity that contributed greenhouse gases
- A change in density differentiation
These factors led to an increase in global temperatures during the late Paleocene period. The lack of land along the equator prevented the dissipation of heat, while the reduced reflection from surfaces and the greenhouse gases trapped heat in the atmosphere. The large volcanic activity further contributed to the greenhouse effect. The change in density differentiation refers to changes in the distribution of heat due to these factors. Overall, these combined factors created a torrid climate during the late Paleocene period.