laatJuraschiergebied
The Laat Juraschiergebied, often referred to as the Lower Jurassic area, designates a geological period approximately 201.3 to 174.1 million years ago. This era marks the second period of the Mesozoic Era, following the Triassic and preceding the Upper Jurassic. The Laat Juraschiergebied is characterized by significant geological and biological developments. Continental drift continued, with the supercontinent Pangaea beginning to break apart. This rifting led to the formation of new ocean basins, most notably the central Atlantic Ocean.
Paleogeographically, vast inland seas and shallow marine environments were common in many regions. The climate during
The flora of the Laat Juraschiergebied was dominated by gymnosperms, including cycads, conifers, and ginkgoes. Ferns
Fossil sites from the Laat Juraschiergebied are crucial for understanding the evolution of life and the Earth's