Mecistotrachelos is known from several fossil specimens excavated from the Solite
quarry from the
Cow Branch Formation on the
Virginia-
North Carolina border. Only two of these have been formally described in a scientific journal. The first fossil was found in 1994 and the second fossil eight years later by Nick Fraser, a
vertebrate paleontologist at the
Virginia Museum of Natural History. The first fossil, VMNH 3649, is the
holotype of the genus and is preserved completely articulated, although missing the tail, hindlimbs, and most of the
pelvic girdle. The second fossil, VMNH 3650, is sometimes considered a
paratype and is more complete, only missing part of the tail as well as the left hindlimb. The Solite quarry was once a large lake and surrounding wetland which formed in a rift basin when
Pangaea started to break up during the Late Triassic. The quarry's sediments were initially believed to have formed during the
Carnian stage of the Triassic, about 230 million years ago. The ancient lake held abundant populations of insects and the
tanystropheid reptile
Tanytrachelos. The fossils of the Solite quarry are often preserved as dark grey bones embedded in dark grey
mudstone, and are thus usually very difficult to observe and prepare. As a result, the
Mecistotrachelos specimens had to be
CT scanned to be properly described. This makes
Mecistotrachelos one of the first extinct animals to be described based almost entirely on CT scan data. == Description ==