it was flat and dry with limestone
During the Devonian period, Earth experienced high levels of atmospheric oxygen which supported the development of the first forests. In the Carboniferous period, these forests led to high levels of carbon dioxide absorption, which decreased the greenhouse effect, leading to global cooling. These changes allowed the evolution of large, complex plant life such as ferns, lycopods, and seed plants.
Pangaea formed during the late Paleozoic era, specifically during the Carboniferous and Permian periods around 335 million years ago. It was a supercontinent that consisted of all the major landmasses on Earth.
The highest oxygen level in Earth's history occurred during the Carboniferous Period, approximately 300-360 million years ago. This period is often referred to as the "golden age of insects" due to the size and diversity of insect species during this time.
The Earth's climate during the late carboniferous period was very similar to the climate of today, but during the early part there were some differences. Atmospheric CO_2 was a little higher, and so was global temperature. See: http://www.geocraft.com/WVFossils/Carboniferous_climate.html - SHARLENE ROMERO-PANCAN
Coal-forming swamps covered the Earth during the Carboniferous period, approximately 360 to 300 million years ago. This period is known for abundant plant growth, particularly lycopods and tree ferns, which accumulated and were transformed into the coal deposits we see today.
They evolved from amphibians during the Carboniferous Period.
Hydrocarbons and coal were formed in what is known as the carboniferous era.
They were abundant on Earth during the Carboniferous.
During the Devonian period, Earth experienced high levels of atmospheric oxygen which supported the development of the first forests. In the Carboniferous period, these forests led to high levels of carbon dioxide absorption, which decreased the greenhouse effect, leading to global cooling. These changes allowed the evolution of large, complex plant life such as ferns, lycopods, and seed plants.
it looked hot and spicy
Pangaea formed during the late Paleozoic era, specifically during the Carboniferous and Permian periods around 335 million years ago. It was a supercontinent that consisted of all the major landmasses on Earth.
The highest oxygen level in Earth's history occurred during the Carboniferous Period, approximately 300-360 million years ago. This period is often referred to as the "golden age of insects" due to the size and diversity of insect species during this time.
The Carboniferous period, also known as the Coal Age, contributed to the formation of vast coal deposits that are still used today as a source of energy. Additionally, the period was characterized by the diversification of plant and animal species, leading to the development of new ecosystems and adaptations. The Carboniferous also played a significant role in shaping Earth's climate and geology.
The Earth's climate during the late carboniferous period was very similar to the climate of today, but during the early part there were some differences. Atmospheric CO_2 was a little higher, and so was global temperature. See: http://www.geocraft.com/WVFossils/Carboniferous_climate.html - SHARLENE ROMERO-PANCAN
Coal-forming swamps covered the Earth during the Carboniferous period, approximately 360 to 300 million years ago. This period is known for abundant plant growth, particularly lycopods and tree ferns, which accumulated and were transformed into the coal deposits we see today.
During the Tertiary Period, the surface of the earth looked much like it does today. It was quite warm with periods of cold much like today.
They first appeared during the late Carboniferous/ early Permian periods, Paleozoic