(Also, if you're interested in cave fossils, check out our recently finalized paleontological inventory for Carlsbad Caverns NP!)
IchthyosaursWe start out with the ichthyosaurs, which are known from the fewest reports so far. In fact, there is only one definite record of ichthyosaurs from an NPS unit: specimens from the Upper Triassic Nizina Limestone in Wrangell-St. Elias NP and Preserve. Ichthyosaurian fossils here were first noted by USGS geologist David Whistler in 1963, who collected a tooth-bearing jaw fragment. The site was relocated by Pat Druckenmiller and Mike Loso in 2017, who observed many additional pieces of bones (Rozell 2017). Otherwise, the only other thing to mention is the discovery of fossils pertaining to Ophthalmosaurus-like ichthyosaurs in the Redwater Member of the Jurassic Stump Formation near Dinosaur NM (Chure 1993).
PlesiosaursThe plesiosaur record of the NPS is currently limited to Upper Cretaceous rocks. By far the best record comes from the Tropic Shale of Glen Canyon NRA, which is notable for the diversity of short-necked plesiosaurs it has produced: the polycotylid plesiosaurs Dolichorhynchops tropicensis, Eopolycotylus rankini, and Trinacromerum ?bentonianum, and the late-surviving pliosaurid plesiosaur Brachauchenius lucasi (Albright et al. 2007a, 2007b; McKean 2012). Another polycotylid, Palmulasaurus quadratus, was also found in the vicinity (Albright et al. 2007a; originally named Palmula, which was preoccupied). D. tropicensis and E. rankini were named from specimens found in the recreation area. The D. tropicensis type has also been reported for its gastroliths (Schmeisser and Gillette 2009). In addition to the short-necked plesiosaurs, the recreation area has produced fossils of several other marine reptiles, including a few vertebrae of a juvenile long-necked plesiosaur (Schmeisser McKean 2013), a partial skull and vertebrae of a basal mosasauroid (Albright et al. 2012), and, as a bonus, specimens potentially representing the early protostegid marine turtle Desmatochelys (Albright et al. 2007a).
With GLCA staking a claim to short-necked plesiosaurs, Missouri National Recreational River specializes in long-necked plesiosaurs. Like our old friend MNRRA, Missouri National Recreational River is a partnership park, so most of the land within its boundaries is owned by other stakeholders. Two or three long-necked plesiosaur specimens have been documented in print from this park. The most recent is the easiest to deal with: an elasmosaur (UNSM 123606) found in the Graneros Shale at Ponca State Park (Matson et al. 2002), at the southeast end of Missouri National Recreational River (see also Pabian and Lawton 1984 and 1987 for more on the geology of this park). The others are a bit trickier, and may be the same thing. The better-documented is AMNH 1495, a.k.a. the holotype of Edward Drinker Cope's Elasmosaurus serpentinus, later renamed Hydralmosaurus and most recently considered indeterminate within Styxosaurus (Otero 2016). Cope's locality information reads, in total, "This fossil was discovered in the blue shale of Cretaceous No. 3, in a bluff in Nebraska, on the southwest side of the Missouri, between Sioux City, Iowa, and Yankton, Dakota" (Cope 1877:583). This is essentially a description of the eastern section of Missouri National Recreational River.
|AMNH 1495, from Otero (2016), clipped from Figure 1 (scale bar = 1 m). Is this the partial postcranium of a monster? CC-BY-4.0.|
Now we let the plot thicken. As Matson et al. (2002) noted, there is a second plesiosaur known from the Ponca State Park area, the "Ponca Monster" of 1873. It turns out there is a detailed description of the circumstances of its discovery in a history of Dixon County, Nebraska (Huse 1896). This specimen was found by a resident of Dixon County known familiarly as "Old Joe Brewer", who "was a man whose study was nature and whose unfaltering enthusiasm and expectation led him to see wonders in every hill and to expect valuable minerals in the rocks and slopes of every ravine. His land, which extended to the river a fearful array of bluffs and gorges, was in his belief the place where mound builders many ages ago had lived" (Huse 1896:94). (This seems about par for the course when your protagonist is known as "Old" anything.) The description of his discovery goes on for a page of text, so rather than quote the whole thing, let me summarize the highlights. In the spring of 1873, Mr. Brewer found the skeleton of a plesiosaur eroding at the base of the Missouri River bluff, and undertook to excavate it with his sons. None of them being versed in the art of fossil excavation, they did a great deal of damage to the bones, but they sold the specimen to outside parties who brought it to Sioux City and glued the pieces back together. It was exhibited in Sioux City, then brought to Chicago and sold to a museum. Huse (1896) reported that the specimen belonged to an animal 80 feet long, which would be the longest plesiosaur known by quite a bit, but of course these things shrink in the wash (and, I suppose, there could have been other things mixed in, either due to multiple plesiosaurs at the site or exhibitors wanting a more impressive display). The specimen was also mentioned obliquely in Todd (1908), from which we learn that "In the vicinity of Ponca Ferry it [Graneros Shale] is represented by about 65 feet of beds. Few fossils are found in this formation. Some bones of large reptiles, among them those of a plesiosaur, were obtained years ago from the Missouri River bank near Limekiln Ravine, about a mile above Ponca Ferry" (Todd 1908:2).
The general geography of the Ponca Monster fits Cope's report, which certainly reads like a third-hand description, and the type of specimen and the time are also consistent. What doesn't fit, however, is the stratigraphy: AMNH 1495 is usually reported as coming from the Niobrara or the Pierre Shale, but these formations are not found within Ponca State Park, and in fact their nearest outcrops are 45 km away (28 miles) (Matson et al. 2002). Meanwhile, the "Ponca Monster" as noted came from the significantly older Graneros Shale. This leaves us with two basic options: these are indeed two different specimens, or AMNH 1495 is the "Ponca Monster" and the stratigraphy has just been reported incorrectly, which could certainly have come about with a third-hand description. So, if anyone here reading this is familiar with AMNH 1495, and it strikes you that it looks like it was excavated by someone called "Old Joe Brewer" with crowbar and pickaxe, maybe we've got something. If nothing else, it would put the question of identifying Hydralmosaurus with Styxosaurus in a different light, given AMNH 1495 would be Cenomanian in age instead of Campanian.
Little Bighorn Battlefield NM has one of the more unusual records, to date primarily documented in internal NPS reports. This unit is partially over the Upper Cretaceous Bearpaw Formation, and during routine work in Custer National Cemetery in 1977, a worker came across unexpected bones: the partial skeleton of a polycotylid, identified as Dolichorhynchops osborni. This specimen, now catalogued as USNM PAL 419645, consists of the vertebrae, ribs, and limb girdles, and is complete enough that for a couple of decades it was exhibited at the Smithsonian with the addition of a skull and flippers (it was withdrawn during the recent redesign).
|The Little Bighorn NB specimen of Dolichorhynchops, plus head and flippers, as it was on display at the Smithsonian. Found on Wikimedia Commons, originally taken by Ryan Somma. CC-BY-2.0.|
The other records are not quite as impressive. Chaco Culture NHP (Varela et al. 2019) and Mesa Verde NP (Harrison et al. 2017) have yielded plesiosaur pieces-parts from the Cliff House Sandstone, and possible plesiosaur remains have been reported in a general way from localities in the Mowry Shale including at Dinosaur NM (Stewart et al. 1994). Finally, I included Yellowstone NP on the map because of a previous report of a plesiosaur specimen from the Telegraph Creek Formation (Santucci 1998). This specimen has since been reinterpreted as an indeterminate reptile per internal NPS reports (which doesn't rule out a plesiosaur identity, but doesn't rule out a lot of other things either).
MosasaursThe best park for mosasaurs in the NPS is Big Bend NP. Mosasaurs have been reported here since Maxwell et al. (1967) (San Vicente Member of the Boquillas Formation). Several taxa are present in the Ernst Member of the Boquillas Formation, representing basal mosasauroids, russelosaurines, and potentially mosasaurines (Bell et al. 2012; supersedes Bell 1995 and Bell and VonLoh 1998).
Missouri National Recreational River again takes second place, this time with its entry "Mosasaurus missouriensis from Niobrara State Park". The specimen was found in 1987 by Nebraska Game and Park Commission horticulturalists Jon Morgensen and Steve Brey in the Mobridge Member of the Pierre Shale, in a road cut following road construction (Bailey and Diffendal 1997) and measures an impressive 10 m long (33 ft) (Johnsgard et al. 2007). In this case, I'm not entirely satisfied whether the find was made within the area where Niobrara State Park and Missouri National Recreational River overlap, but if it wasn't, it was within about 30 m (100 ft) of the line. Unlike the retired Dolichorhynchops, this one is one display at the University of Nebraska State Museum in Lincoln, Nebraska, complete with unhealed bite marks on the jaw.
|Which you can see in this photo on the lower jaw.|
As with the plesiosaurs, most of the other reports are much more minor. Mosasaur bones are known from the Fox Hills Formation of Badlands NP (Landman et al. 2013), and there is an internal report of a possible mosasaur bone from the Severn Formation of Fort Washington Park. Pieces-parts of mosasaurs are known from the Cliff House Sandstone of Mesa Verde NP (Harrison et al. 2017) and the Cliff House Sandstone, Lewis Shale, and possibly the Pictured Cliffs Sandstone of Chaco Culture NHP (Varela et al. 2019); one of the Chaco Cliff House specimens has been identified to Prognathodon overtoni. Finally, as mentioned, the Glen Canyon record consists of a partial skull and vertebrae of a basal mosasauroid (Albright et al. 2012).
ReferencesAlbright, L. B. III, D. D. Gillette, and A. L. Titus. 2007a. Plesiosaurs from the Upper Cretaceous (Cenomanian-Turonian) Tropic Shale of southern Utah: Part 1, new records of the pliosaur Brachauchenius lucasi. Journal of Vertebrate Paleontology 27(1):31–40.
Albright, L. B., III, D. D. Gillette, and A. L. Titus. 2007b. Plesiosaurs from the Upper Cretaceous (Cenomanian-Turonian) Tropic Shale of southern Utah: Part 2, Polycotylidae. Journal of Vertebrate Paleontology 27(1):41–58.
Albright, L. B., III, A. L. Titus, H. S. Richardson, E. C. Clites, and T. A. Birthisel. 2012. A basal mosasauroid from the Early Turonian of Utah. Journal of Vertebrate Paleontology 32(Supplement):55.
Bailey, B. E., and R. F. Diffendal Jr. 1997. Vertebrate fossils and minerals. Pages 13–14 in Flowerday, C. A. and R. F. Diffendal Jr., editors. 1997. Geology of Niobrara State Park, Knox County, Nebraska, and adjacent areas, with a brief history of the park, Gavins Point Dam, and Lewis and Clark Lake. University of Nebraska – Lincoln, Conservation and Survey Division, Lincoln, Nebraska. Educational Circular 13.
Bell, G. L., Jr. 1995. Middle Turonian (Cretaceous) mosasauroids. National Park Service, Big Bend, Texas. Paleontological Research volume 2, Technical Report NPS/NRPO/NRTR-93/11.
Bell, G. L., Jr., and J. P. VonLoh. 1998. New records of Turonian mosasauroids from the western United States. Dakoterra 5:15–28.
Bell, G. L., Jr., K. R. Barnes, and M. J. Polcyn. 2012. Late Cretaceous mosasauroids of the Big Bend region of Texas. Earth and Environmental Science Transactions of the Royal Society of Edinburgh 103(3-4):571–581.
Chure, D. J. 1993. The first record of ichthyosaurs from Utah. Geology Studies 39:65–69.
Cope, E. D. 1877. Report on the geology of the region of the Judith River, Montana, and on vertebrate fossils obtained on or near the Missouri River. Bulletin of the United States Geological and Geographical Survey of the Territories 3:565–597.
Harrison, G. W. M., J. S. Tweet, V. L. Santucci, and G. L. San Miguel. 2017. Mesa Verde National Park: Paleontological resource inventory (non-sensitive version). Natural Resource Report NPS/MEVE/NRR—2017/1550. National Park Service, Fort Collins, Colorado.
Huse, W. 1896. History of Dixon County, Nebraska: its pioneers, settlement, growth and development, and its present condition—its villages, townships, enterprises and leading citizens, together with portraits and biographical sketches of some of its prominent men, incidents of pioneer life, etc. Press of the Daily News, Norfolk, Nebraska.
Landman, N. H., Z. Remin, M. P. Garb, and J. A. Chamberlain, Jr. 2013. Cephalopods from the Badlands National Park area, South Dakota: reassessment of the position of the Cretaceous/Paleogene boundary. Cretaceous Research 42:1–27.
Matson, S. D., M. R. Voorhies, R. G. Corner, R. M. Joeckel, and B. Vrana. 2002. A new long-necked plesiosaur specimen from the Graneros Shale (Cretaceous, Cenomanian), Ponca State Park, Nebraska. Program and Proceedings - Nebraska Academy of Sciences 112:54–55.
Maxwell, R. A., J. T. Lonsdale, R. T. Hazzard, and J. A. Wilson. 1967. Geology of Big Bend National Park, Brewster County, Texas [enormous file!]. University of Texas Bureau of Economic Geology Publication 6711.
McKean, R. S. 2012. A new species of polycotylid plesiosaur (Reptilia: Sauropterygia) from the Lower Turonian of Utah: extending the stratigraphic range of Dolichorhynchops. Cretaceous Research 34:184–199.
Otero, R. A. 2016. Taxonomic reassessment of Hydralmosaurus as Styxosaurus: new insights on the elasmosaurid neck evolution throughout the Cretaceous. PeerJ 4:e1777. doi:10.7717/peerj.1777.
Pabian, R. K., and D. R. Lawton. 1984. Geology of Ponca State Park, Nebraska. University of Nebraska – Lincoln, Conservation and Survey Division, Lincoln, Nebraska. Educational Circular 6.
Pabian, R. K., and D. R. Lawton. 1987. Late Cretaceous strata exposed at Ponca State Park, Dixon County, Nebraska. Pages 7–12 in D. L. Biggs, editor. North-central section of the Geological Society of America. Geological Society of America, Boulder, Colorado. Centennial Field Guide 3.
Robinson Roberts, L. N., and M. A. Kirschbaum. 1995. Paleogeography and the Late Cretaceous of the Western Interior of middle North America; coal distribution and sediment accumulation. U.S. Geological Survey, Reston, Virginia. Professional Paper 1561.
Rozell, N. 2017. Prehistoric reptile one mile above McCarthy. The Field.
Santucci, V. L. 1998. The Yellowstone paleontological survey. Yellowstone Center for Resources, National Park Service, Yellowstone National Park, Wyoming. YCR-NR-91-1.
Schmeisser, R. L., and D. D. Gillette. 2009. Unusual occurrence of gastroliths in a polycotylid plesiosaur from the Upper Cretaceous Tropic Shale, southern Utah. Palaios 24(7):453-459.
Schmeisser McKean, R. L. 2013. First occurrence of a long-necked plesiosaur from the Tropic Shale (Cenomanian-Turonian), southern Utah. Abstracts with Programs – Geological Society of America 45(7):845.
Sloan, R. E. 1964. The Cretaceous System in Minnesota. Minnesota Geological Survey, St. Paul, Minnesota. Report of Investigations 5.
Stewart, J. D., S. A. Bilbey, D. J. Chure, and S. K. Madsen. 1994. Vertebrate fauna of the Mowry Shale (Cenomanian) in northeastern Utah. Journal of Vertebrate Paleontology 14(supplement to 3):47A.
Todd, J. E. 1908. Description of the Elk Point Quadrangle. U.S. Geological Survey, Washington, D.C. Folio of the Geologic Atlas 156.
Varela, P. J., V. L. Santucci, and J. S. Tweet. 2019. Chaco Culture National Historical Park: Paleontological resources inventory (non-sensitive version). Natural Resource Report NPS/CHCU/NRR—2019/1915. National Park Service, Fort Collins, Colorado.