The Carboniferous system, Permian System
and Triassic systems are seen in the western Himalayas.
In the Carboniferous, rainforest collapse led to a great loss of plant
and animal life.
They are known as fossils from the Carboniferous Epoch of the great Palaeozoic era 300,000,000 years ago.
They have been around virtually unchanged in general appearance since the Carboniferous period, more than 300 million years ago.
In the Early Carboniferous, northwest Africa had touched the southeastern coast of Euramerica,
creating the southern portion of the Appalachian Mountains, and the Meseta Mountains.
They are the remnants of a vastly more
numerous flora that populated much of the Earth during the Carboniferous Period(about 360 to 300 million years ago).
In the Early Carboniferous, northwest Africa had touched the southeastern coast of Euramerica,
creating the southern portion of the Appalachian Mountains, the Meseta Mountains and the Mauritanide Mountains.
I was particularly interested in moments of time that are examples of life changing the air, but also the air that can
influence how life will evolve, like Carboniferous air.
Western Kazakhstania collided with Baltica in the Late Carboniferous, closing the Ural Ocean between them and the western Proto-Tethys in them(Uralian orogeny),
causing the formation of not only the Ural Mountains but also the supercontinent of Laurasia.