No: Cenozoic. (Tertiary).
Pangaea was formed during the late Paleozoic era, specifically in the Permian period, around 300 million years ago. It was a supercontinent that included almost all of Earth's landmasses.
The formation of Gondwana and Laurasia occurred during the Paleozoic era, specifically during the late Precambrian and early Paleozoic periods. Gondwana and Laurasia eventually merged to form the supercontinent Pangaea during the late Paleozoic era.
Coal beds formed during the Carboniferous Period, approximately 300 to 360 million years ago. This period was characterized by extensive forests being buried and compressed over time, eventually transforming into coal deposits.
Pangaea, the supercontinent, was formed during the late Paleozoic and early Mesozoic eras, specifically around 300-200 million years ago. It existed during the late Paleozoic and early Mesozoic eras before breaking apart into the continents we recognize today.
The supercontinent that formed at the end of the Paleozoic era is known as Pangaea. Pangaea began to break apart during the Mesozoic era, ultimately leading to the formation of the continents as we know them today.
There are so many facts about the Paleozoic era. This was the time when the explosion of different forms of life. New species of organisms were formed during this era which started over 500 million years ago.
Several such ranges were formed during that era, on several continents.
Most of our limestone formed during the Paleozoic era, approximately 500 to 250 million years ago. Coal formation occurred mainly during the Carboniferous period within the Paleozoic era, around 360 to 300 million years ago.
The one mass of land known as Pangaea was formed In the Era Paleozoic, along with mountains, and land breathing animals.
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
Limestone deposits suggest that they were formed in a marine environment, typically in shallow, warm, and calm waters where the accumulation of calcium carbonate skeletons and shells of marine organisms was prevalent. The presence of fossils within limestone can indicate the past biodiversity and environmental conditions of the area where the deposits formed. Additionally, the purity and composition of the limestone can provide clues about the depositional processes and the source of the materials.