karbonische

Karbonische is a term that refers to the Carboniferous period of geological history. This period, spanning from approximately 359 to 299 million years ago, is a subdivision of the geologic timescale. It follows the Devonian period and precedes the Permian period. The Carboniferous is renowned for its vast coal deposits, which were formed from the accumulated plant matter of the era's extensive forests. These forests, dominated by giant horsetails, clubmosses, and ferns, thrived in warm, humid climates, often in vast swampy regions.

Life during the Carboniferous saw significant developments. On land, insects grew to enormous sizes, including dragonflies with wingspans of up to two feet. Amphibians were abundant and diverse, and the first reptiles evolved, a crucial step in the colonization of drier environments. Marine life continued to flourish, with ammonites and various invertebrates populating the oceans. The period is often divided into two sub-periods: the Mississippian and the Pennsylvanian. The Mississippian is characterized by extensive marine limestone deposits, while the Pennsylvanian is known for its coal swamps and the formation of the supercontinent Pangaea began during this time. The environmental conditions of the Carboniferous, particularly its high oxygen levels and widespread plant life, had a profound impact on the subsequent evolution of life on Earth.