Pteranodon
"Pteranodon" was the first pterosaur found outside of Europe. Its fossils first were found by Othniel Charles Marsh in 1870, in the Late Cretaceous Smoky Hill Chalk deposits of western Kansas. These chalk beds were deposited at the bottom of what was once the Western Interior Seaway, a large shallow sea over what now is the midsection of the North American continent. These first specimens, YPM 1160 and YPM 1161, consisted of partial wing bones, as well as a tooth from the prehistoric fish "Xiphactinus", which Marsh mistakenly believed to belong to this new pterosaur (all known pterosaurs up to that point had teeth). In 1871, Marsh named the find ""Pterodactylus oweni"", assigning it to the well-known (but much smaller) European genus "Pterodactylus". Marsh also collected more wing bones of the large pterosaur in 1871. Realizing that the name he had chosen had already been used for Harry Seeley's European pterosaur species "Pterodactylus oweni" in 1864, Marsh re-named his giant North American pterosaur Pterodactylus occidentalis, meaning "Western wing finger," in his 1872 description of the new specimen. He also named two additional species, based on size differences: Pterodactylus ingens (the largest specimen so far), and Pterodactylus velox (the smallest).
Palaeochenoides
Only a single species, Palaeochenoides mioceanus, is known to date. The first fossil assigned to it – a distal right femur piece – was found near the source of the Stono River in Charleston County, South Carolina (United States). At first it was believed to be from the Early Miocene Hawthorne Formation – its specific name, seemingly referring to the "Miocene ocean" as presumed habitat but actually a simple spelling error for "miocaenus", "from the Miocene", that was never corrected and hence became valid – alludes to this. But in fact no Hawthorne Formation rocks were known in the Charleston region when the fossil was found, and consequently modern authors consider a Chattian (Late Oligocene) age more likely and suggest the fossil came from the Cooper or Chandler Bridge Formation. Specimen MCZ 2514, a distal left tarsometatarsus fragment from the Ashley River, was more tentatively assigned to "P. mioceanus" later on; it was also erroneously believed to be from the Hawthorne Formation.