The first fossils of Geosternbergia was collected by American paleontologist George F. Sternberg in 1952 from the lower portion of the Niobrara Formation.
The fossils of the animal looked similar to those of the species Pteranodon longiceps, but the crests were set upright and in a slightly different position.
In 1958, Sternberg and paleontologist  Myrl V. Walker published a study about this peculiar find.
In 1966, American paleontologist John Christian Harksen assigned the specimens found as a new species of Pteranodon called P. sternbergi due to its distinct upright crest that set it apart from P. longiceps.
Halsey W. Miller however, concluded a revision of the different species of Pteranodon in 1971, and created three different subgenera.
One of which was Sternbergia, which consisted of the Pteranodon specimens with upright crests.
P. sternbergi was assigned to this subgenus along with another species called P. walkeri, but Miller then found out that the name Sternbergia had been preoccupied, so he changed it into Geosternbergia instead.

Paleontologists like S. Christopher Bennett consider Geosternbergia to be older than P. longiceps, and therefore the direct ancestor of that species.

The most complete example of the species, currently in the collections of the University of Alberta Laboratory for Vertebrate Paleontology as specimen number UALVP 24238, is a partially-articulated sub-adult fossil with a wingspan of about 4 metres (13 ft).
The skeleton is missing only parts of the skull and the ends of the wings and feet, was discovered in 1974 near Utica, Kansas.
The fossil was found by Richard C. Fox and Allen Lindoe in rocks belonging to the lower part of the Smoky Hill Chalk Member of the Niobrara Formation.
These rocks date to the late Coniacian or early Santonian stage, about 86 million years ago.
In 2010, a paper by Alexander W.A. Kellner argued that this specimen was different enough from G. sternbegi that it should be re-classified as its own genus and species, which he named Dawndraco kanzai.
This generic name combined the Dawn deity of the Iroquois with a Latin draco, "dragon".
The specific name refers to the Kanza tribe of Kansas.
Kellner thought that several features of the skeleton supported his hypothesis that D. kanzai was a unique species, most notably its unique snout, which does not strongly taper towards the tip as in female Pteranodon specimens, with the upper and lower margins running almost parallel instead.
Kellner thought this meant the specimen must have had a crest running along the length of the snout.
However, a re-examination of the fossil published in 2017 by Elizabeth Martin-Silverstone and colleagues argued that the differences in the snout were more likely due to male pteranodontids having longer, broader bills than the more complete female specimens Kellner used for comparison.
Martin-Silverstone concluded that "Dawndraco" was simply a male G. sternbergi with a very long bill with a gradual taper.

Geosternbergia fossils are known from the Niobrara and Sharon Springs Formations of the central United States.
Geosternbergia existed as a group for more than four million years during the late Coniacian - early Campanian stages of the Cretaceous period.
The genus is present in the lower the Niobrarra Formation except for the upper two; in 2003, Kenneth Carpenter surveyed the distribution and dating of fossils in this formation, demonstrating that Geosternbergia sternbergi existed there from 88-85 million years ago, while the species later named G. maiseyi existed between 81.5 and 80.5 million years ago.
The first fossils of Geosternbergia was collected by American paleontologist George F. Sternberg in 1952 from the lower portion of the Niobrara Formation. The fossils of the animal looked similar to those of the species Pteranodon longiceps, but the crests were set upright and in a slightly different position. In 1958, Sternberg and paleontologist  Myrl V. Walker published a study about this peculiar find. In 1966, American paleontologist John Christian Harksen assigned the specimens found as a new species of Pteranodon called P. sternbergi due to its distinct upright crest that set it apart from P. longiceps. Halsey W. Miller however, concluded a revision of the different species of Pteranodon in 1971, and created three different subgenera. One of which was Sternbergia, which consisted of the Pteranodon specimens with upright crests. P. sternbergi was assigned to this subgenus along with another species called P. walkeri, but Miller then found out that the name Sternbergia had been preoccupied, so he changed it into Geosternbergia instead.
Paleontologists like S. Christopher Bennett consider Geosternbergia to be older than P. longiceps, and therefore the direct ancestor of that species.
The most complete example of the species, currently in the collections of the University of Alberta Laboratory for Vertebrate Paleontology as specimen number UALVP 24238, is a partially-articulated sub-adult fossil with a wingspan of about 4 metres (13 ft). The skeleton is missing only parts of the skull and the ends of the wings and feet, was discovered in 1974 near Utica, Kansas. The fossil was found by Richard C. Fox and Allen Lindoe in rocks belonging to the lower part of the Smoky Hill Chalk Member of the Niobrara Formation. These rocks date to the late Coniacian or early Santonian stage, about 86 million years ago. In 2010, a paper by Alexander W.A. Kellner argued that this specimen was different enough from G. sternbegi that it should be re-classified as its own genus and species, which he named Dawndraco kanzai. This generic name combined the Dawn deity of the Iroquois with a Latin draco, "dragon". The specific name refers to the Kanza tribe of Kansas. Kellner thought that several features of the skeleton supported his hypothesis that D. kanzai was a unique species, most notably its unique snout, which does not strongly taper towards the tip as in female Pteranodon specimens, with the upper and lower margins running almost parallel instead. Kellner thought this meant the specimen must have had a crest running along the length of the snout. However, a re-examination of the fossil published in 2017 by Elizabeth Martin-Silverstone and colleagues argued that the differences in the snout were more likely due to male pteranodontids having longer, broader bills than the more complete female specimens Kellner used for comparison. Martin-Silverstone concluded that "Dawndraco" was simply a male G. sternbergi with a very long bill with a gradual taper.
Geosternbergia fossils are known from the Niobrara and Sharon Springs Formations of the central United States. Geosternbergia existed as a group for more than four million years during the late Coniacian - early Campanian stages of the Cretaceous period. The genus is present in the lower the Niobrarra Formation except for the upper two; in 2003, Kenneth Carpenter surveyed the distribution and dating of fossils in this formation, demonstrating that Geosternbergia sternbergi existed there from 88-85 million years ago, while the species later named G. maiseyi existed between 81.5 and 80.5 million years ago.
Geosternbergia