Petalodus is by far the most interesting genus of vertebrate fossil to be reasonably found in Parks Township. In 2019, four different teeth were recovered from the local limestone layer. The genus is currently only known from its teeth. No fossilized body or jaws of Petalodus have been found worldwide. Any current reconstructions of the creature are based on relative genus found within its class, the Chondrichthyes.
Specimens from Parks Township
|Catalog ID||Specimen Name||Crown Height||Crown Width|
* – Measured based on symmetry. One side broken/obscured.
** – Unable to measure, both sides broken.
*** – From top of distal crown tongue.
Petalodus Tooth Anatomy
Below you will find three views of a Petalodus Tooth. Shown here are Lingual, Lateral and Labial views. Lingual is the side of the tooth that faces inwards towards the tongue. Labial is the side that faces the outside of the mouth. The crown is convex as it faces outside of the mouth.
The teeth of the genus are considered homodont, therefore all teeth are of the same morphology. While teeth towards the back appear flatter, the ones toward the front are thought to be taller. The side profile is said to be sigmoid, or more simply, an S shape.
Named Petalodus Species
There are 16 named species in the current online Paleobiological database online, however there are more than 30 in existence (Harper 2016). The vast majority of named species were designated in the 1800’s. Only 1 or 2 (Harper 2016) species have been named in the 1900’s.
|Petalodus||arcuatus||1870 (St. John)|
|Petalodus||curtus||1870 (Newberry and Worthen)|
|Petalodus||hybridus||1875 (St. John and Worthen)|
|Petalodus||linguifer||1866 (Newberry and Worthen)|
|Petalodus||proximus||1875 (St. John and Worthen)|
Petalodus Holotype Photographs
We are currently collecting holotype photographs. A type of a species is a specimen. A type of a genus is a species. The most prominent of several variations of types is the holotype. Following this, there are several more defined named type variants. In searching for holotypes of Petalodus, these situations arise and need situated.
|Holotype||The representative specimen in which to define the species. Typically these are the specimen in which the species was first defined.|
|Paratype||When the holotype is defined alongside other specimens in the same description, these specimens are Paratypes.|
|Allotype||Used to designate a specimen of the opposite sex of the holotype specimen. This specimen is from the group of paratypes. Also used if the specimen shows features not visible on the holotype.|
|Neotype||If the Holotype is lost or destroyed or not specified in the original description of a species, then a neotype specimen may be selected.|
|Syntype||One of many specimens originally described when a holotype isn’t selected. Typically it is best practice to later define a best in class specimen, which is called the Lectotype.|
|Lectotype||Specimen that is selected to serve as the single type specimen from a set of Syntypes.|
|Paralectotype||Once a Lectotype is defined, the remaining syntypes are redesignated as paralectotypes.|
|Hapantotype||When the type species specimen is two or more that represent different stages of life. A juvenile and adult for instance of a related specimen.|
|Iconotype||If a new species is designed from an illustration of a specimen, then the illustration is the iconotype.|
Described by Leidy in 1856, P. allegheniensis is often described as a junior synonym to P. ohioensis. Safford and later Hay in 1929 both listed it as such.
This specimen was collected at the head of inclined plane No. 3 of the old Portage Railroad, in Blair County, Pennsylvania. This locality correlates with the Brush Creek Limestone, which is located within the Glenshaw Formation.
Described by Safford in 1853, the holotype of Petalodus ohioensis resides in the Yale Peabody Museum in Connecticut. The catalog number is YPM 2861. It comes from Yale University as they publish their digital collection catalog online. The tooth that was photographed is a cast of the original. I believe the original is currently lost.
This species was described in 1836 originally by Louis Agassiz, a Swiss geologist and biologist. The holotype is specimen MHNN-FOS 171, currently in the collections of the Muséum d’histoire naturelle de Neuchâtel in Switzerland. SM E 4291 is listed as a holotype, and identified as P. acuminatus, however it is the holotype of P. rhombus. Eventually, P. rhombus was synonymized with P. acuminatus.
The specimen appears as a little more than half of the full tooth. The center of the crown consists of a piece of enamel that is adhered to the matrix. A cutting edge impression can be seen on the holotype.
P. rhombus is a legacy species that has been replaced with P. acuminatus. The holotype of P. rhombus is specimen SM E 4291 housed in the Sedgwick Museum of Earth Sciences at the University of Cambridge. As part of the BG3D Type Fossils project, the specimen photo is the best I’ll likely get. It was later designated as a junior synonym of P. acuminatus. McCoy original described this specimen as Petalodus rhombus in 1848, a new species.
First described in 1870 from a specimen in Illinois. The original plate illustration from his description is shown below. I am still searching for the holotype of this species, which is likely what is illustrated below.
TEETH of moderate size, thin and light in crown and root; crown broadly arched, twice as wide as high, concavo-convex laterally and vertically ; superior margin serrated or roughened by the termini of the calcigerous tubes ; anterior face of crown without imbricating enamel folds, half as high as posterior face; posterior face elliptical in outline, basal enamel folds 5-6, broad and strong ; root relatively short and thin, on posterior face two-thirds the height of the crown, in breadth two-thirds that of the crown, sides nearly straight, bottom arched and somewhat three-lobed, strongly beveled off so as to form a blunt edge on the anterior and longer side.J. S. Newberry, A.H. Worthen, Geological Survey of Illinois, Vol 4 Geology and Paleontology, Section 1 Descriptions of Vertebrates, 1870.
In general aspect this tooth resembles most P. linguifer, N. and W., from the Chester limestone, but it is thinner, and has a much shorter root, of which the lower edge is characteristically beveled. There is no other species for which it is likely to be mistaken.
Formation and locality : Keokuk limestone; Otter creek, Jersey county, Illinois.
The tooth this species was described from was said to be 2.5 inches across. I believe an inch from Dublin in 1883 is probably the same as an inch in the United States today. It was named a new species by Davis based on the large size.
The described specimen was given an identification number and I am currently attempting to obtain current specimen photography.
The tooth described by Sir Richard Owen in 1840 was provided by Sir Philip Egerton. Owen goes on to describe the tooth as having a thin layer of dense enamel, with a smooth shining surface. The holotype does exist, along with a neotype. They are NHMUK PV P613 (Holotype) and NHMUK PV P75414 in the Natural History Museum, London. We currently do not have the photos, so for now the illustrations will do.
One important fact to note is that the illustration is mirrored from the actual specimen. The specimen consists of only 30-40% of the original crown.
Described in 1875 by St. John and Worthen, this specimen came from the collection of Sir William Cornelius Van Horne. Van Horne once served as president of the Canadian Railroad Company, and later was knighted. The specimen was originally considered to be P. linguifer, and P. curtus. The authors state that the tooth may be an intermediate evolution piece stuck between the two species. It was under this assumption and it’s uniqueness that it should be named as a new species. The fossil collection of Sir William was eventually transferred to the University of Chicago. We are still searching for the specimens.
The holotype from this species comes from the University of Kansas Biodiversity Institute, Division of Vertebrate Paleontology. This specimen was first described by Halsey W. Miller (Jr) in 1957. The specimen catalog ID is KUVP 6672. It appears to have been glued back together in several places. Photos as described in the original appear to have the same silhouette.
The described specimen was originally found in October 1956, by John Mark Jewett. It was the first Petalodus tooth ever recorded as found in the Pennsylvanian rocks of Kansas. It was found in what was called the Plattsmouth limestone, Oread formation, Virgilian, upper Pennsylvanian, in a quarry in northwestern Franklin County, Kansas. The anterior crown face height was measured at 25mm while the width is 40mm. The posterior crown face height was measured at 35mm.
Miller argued that the tooth’s morphometric distinctions and its occurrence in an area geographically separated from other species warranted a name of a new species. Miller was aware that teeth from different parts of the jaw could indeed be different, but held that it would be for certain until someone finds a Petalodus jaw with embedded teeth.
A. J. Robb III (2003), considers P. jewetti to be a junior synonym of P. ohioensis, but he cited the same precautions as Miller did. Miller was also keen to mention that many species of the genus has been erroneously given unique species names for the same reasons as Robb, but still named this a new species based on a combination of morphology and geography.
The type specimen, X-521, comes from the Prairie Research Institute Center for Paleontology at the University of Illinois. There are two other specimens, VPF-199 and VPF-201, at the Museum of Comparative Zoology at Harvard University. The first illustrated specimen below was described as a perfect specimen from Pope county.
In 1875 this was described along side P. hybridus. This tooth was compared to P. allegheniensis, however it’s uniqueness designed it as a new species as well. Dr. Leidy also apparently provided the two the original specimens of P. allegheniensis in which to compare this specimen to. So the duo had more to go on that simply illustrations. The following is part of their description.
These fragments exhibit a uniformity of characters which has led provisionally to their recognition as a distinct form. From Petalodus Alleghaniensis, Leidy, with which they are associated, they are distinguished by the regularly arched crest, the comparatively horizontal direction of the basal border of the concave face, relatively low convex face, and apparently short, broadly rounded base, which is produced downward in nearly the same vertical plane as the convex crown-face, comparatively slight antero-posterior diameter, and about two-thirds the lateral diameter of the crown.St. John and Worthen, 1875 Geological Survey of Illinois, Vol 6, Geology and Paleontology
Originally grouped with the genus Chomatodus, Agassiz wrote in his Recherhes sur les poissons fossiles 1833-1843) (Research of the fossil fish) that his Chomatodus acuminatus is now part of a new genus Petalodus from M. Owen. He said it now belongs to another family, other than that of Cestraciontes, because of it’s sharp teeth. Agassiz then listed species of the new genus, Petalodus. Afterwards, he named Hastingsiae (which is now corrected as Hastingsii), psittacinus, laevissimus, rectus, radicans, marginalis, and sagittatus.
Later in 1855, this species was finally illustrated in a book by Frederick McCoy, as a specimen in the Geological Museum of the University of Cambridge.
- Fossilworks – Taxon Page
- John A. Harper, Reflections on Petalodus, a Common Late Paleozoic “Shark”1 Tooth Found in Western Pennsylvania’s Rocks, Pennsylvania Geology V. 48 No 2, p. 3-11
- Robb, A. J., III, 2003, Notes on the occurrence of some petalodont shark fossils from the Upper Pennsylvanian rocks of northeastern Kansas: Transactions of the Kansas Academy of Science, v. 106, no. 1/2, p. 71–80 https://doi.org/10.1660/0022-8443(2003)106[0071:NOTOOS]2.0.CO;2
- 1957, Transactions of the Kansas Academy of Science, Vol. 60, No. 1, Petalodus jewetti, a New Species of Fossil Bradyodont Fish From Kansas, P. 82-85
- YPM 2861 Collections Page – Yale Peabody Museum of Natural History
- Google Books – The annals and magazine of natural history, zoology, botany and geology: incorporating the journal of botany, Volume 2, Taylor & Francis, 1848
- SM E 4291 – Fossil specimen : SM E 4291 – Holotype
- Worthen, A.H., Newbery, J.S., 1866, Geological Survey of Illinois, Vol 2, Paleontology.
- Knowles, V, 2010, William C. Van Horne: Railway Titan, Page 25
- 1840, R. Owen, Odontography; or, A treatise on the comparative anatomy of the teeth
- 1850-1855, A synopsis of the classification of the British Palæozoic rocks / by the Rev. Adam Sedgwick ; With a systematic description of the British Palæozoic fossils in the Geological museum of the University of Cambridge, by Frederick McCoy.
- Itano, Wayne. “Petalous Ohioensis, the Most Common Shark Tooth Found at McCoy, Colorado, and the Search for Its Lost Holotype: Part 1: History of Petalodus Ohioensis from Its Discovery to the Early Twentieth Century.” Trilobite Tales 38, no. 2 (2020): 22–26.
- Zangerl, R et al., 1993, Comparative microscopic dental anatomy in the Petalodontida (Chondrichthyes, Elasmobranchii), Page 16-23