The melting of the Paleozoic supercontinent, often referred to as Gondwana, is attributed to several factors, primarily tectonic activity and changes in climate. As continental plates shifted, volcanic activity increased, releasing greenhouse gases that raised global temperatures. Additionally, the breakup of the supercontinent altered ocean currents and climate patterns, further contributing to the melting of ice traps that had accumulated during the late Paleozoic era. This interplay of geological and climatic changes facilitated the transition from glacial to warmer conditions.
Dry sunny warm climate. Little rain, but they need watering daily.
seasonal
Trilobites, eurypterids, and blastoids are examples of Paleozoic invertebrates that became extinct by the end of the Paleozoic era. These marine creatures were once diverse and abundant but disappeared due to various environmental changes and extinction events at the end of the era.
Yes. If no animals survived from the Paleozoic into the mesozoic, then there would be no animals today.
in the Mesozoic and Paleozoic era
You need to be specific, the Paleozoic Era has different time period. But I would say the climate then was tropics and subtropical because of the organism that existed then and the rock time that was formed
Paleozoic - climate change Mesozoic - meteor
injurious climate
the climate change during the shifting of the plates that was causing the making of Pangea
Paleozoic
The Paleozoic supercontinent ice cap method is a hypothesis that suggests ice caps formed over the supercontinent of Pangaea during the Paleozoic era, leading to global cooling and glaciation. This theory is based on the positioning of landmasses in the Southern Hemisphere during this time, which could have facilitated the buildup of ice sheets and contributed to significant climate changes.
Mercury has no climate, since it has no atmosphere.
usally a tropical climate.
bad winter climate
Subarctic climate
it is a tropic climate