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Late Cretaceous plesiosaur teeth from Axel Heiberg Island, Nunavut, Canada.

ABSTRACT. We report the discovery of Late Cretaceous plesiosaur teeth from non-marine strata on Axel Heiberg Island in the Canadian High Arctic. In comparison to other plesiosaur teeth, these specimens are most similar to the teeth of elasmosaurs: they have a smooth outer surface and crenulated inner surface, with crenulations that extend nearly to the tip of the tooth. Comparisons with elasmosaurid fossils elsewhere indicate that the Axel Heiberg teeth are from juveniles. The presence of a plesiosaur in non-marine strata on Axel Heiberg Island supports the suggestion that juvenile elasmosaurs frequently inhabited freshwater environments. The temporal distribution of the Axel Heiberg specimens and other occurrences from the High Arctic suggests that elasmosaurids may have expanded their range during a time of extreme climatic warmth.

Key words: Late Cretaceous, Axel Heiberg Island, elasmosaurids, paleoclimate, paleoenvironment

RESUME. On signale la decouverte de dents de plesiosaure du Cretace superieur d'une strate non marine a l'ile Axel Heiberg, dans l'Extreme-Arctique canadien. Comparativement aux autres dents de plesiosaures, ces specimens ressemblent beaucoup aux dents d'elasmosaures: leur surface exterieure est lisse et leur surface interieure est crenelee, les crenulations s'etendant presque jusqu'a la pointe de la dent. Apres avoir compare ces specimens aux fossiles d'elasmosaures trouves ailleurs, on a remarque que les dents trouvees a Axel Heiberg sont les dents de juveniles. La presence d'un plesiosaure dans une strate non marine de l'ile Axel Heiberg vient etayer la suggestion selon laquelle des elasmosaures juveniles evoluaient souvent dans les milieux dulcaquicoles. La repartition temporelle des specimens d'Axel Heiberg et d'autres occurrences de l'Extreme-Arctique laissent suggerer que les elasmosaures auraient pu etendre leur parcours au cours d'une periode d'extreme chaleur climatique.

Mots cles: Cretace superieur, ile Axel Heiberg, elasmosaures, paleoclimat, paleoenvironnement

Traduit pour la revue Arctic par Nicole Giguere.


Vertebrate fossils collected from sedimentary strata on Axel Heiberg Island in the Canadian High Arctic suggest a mean annual temperature greater than 14[degrees]C during the Late Cretaceous (Turonian-Coniacian) in the Arctic region (Tarduno et al., 1998). Oxygen isotope data from lower-latitude deep-sea sites have indicated a similar period of warmth (Huber et al., 2002; Wilson et al., 2002). Because of its high latitude location during the Late Cretaceous (approximately 71[degrees]N, Tarduno et al., 2002), the Axel Heiberg locality can provide special insight into how latitudinal temperature gradients of the warm Late Cretaceous Earth are reflected in the vertebrate fossil record. Here we report the discovery of two well-preserved plesiosaur teeth found in the uppermost part of the thin (3.0 m) sequence of shale and siltstone from which vertebrate fossils have been recovered. These fossils add further to our understanding of the ecology of the Axel Heiberg assemblage and the environment of deposition.

The Late Cretaceous Axel Heiberg vertebrate locality is near Expedition Fiord (present-day location: 79[degrees]23.5' N, 92[degrees]10.9' W). The fossil-bearing sediments were deposited atop the subaerial basalts of the Strand Fiord Formation and are overlain by marine shales of the Kanguk Formation. The fossils define a diverse freshwater assemblage of turtles, fishes, and champsosaurs (Tarduno et al., 1998). The ichthyofauna consists of lepisosteids, amiids, and teleosts (Friedman et al., 2003). With the exception of a few jaw elements, the fossil fish elements are disarticulated and therefore could have undergone transport. The presence of articulated champsosaur fossils in the sediments, however, suggests that transport was minor (Tarduno et al., 1998).

The teeth recovered from the Axel Heiberg Island locality closely resemble those of elasmosaurid plesiosaurs (Plesiosauroidea). The teeth are gently curved and culminate in a sharp apex (Fig. 1). The teeth are broken off from the root. The crowns, which are fully covered by enamel, measure 18.34 mm and 12.45 mm long, with maximum diameters of 3.61 mm and 3.12 mm, respectively. In both specimens, the crown has been beautifully preserved, displaying fine longitudinal striations that are most prominent on the lingual side. Fine longitudinal striations and slender shape are characteristic of elasmosaurid teeth; in contrast, absence or reduction of striations on the labial surface is a feature present in a range of plesiosaur taxa (e.g., Brown, 1981). The teeth are more slender than is usually the case in elasmosaurid plesiosaurs, but this could be a feature associated with their small size. Alternatively, they could be posterior teeth from a polycotylid plesiosaur. Slender recurved teeth are present in the Late Cretaceous genus Dolichorhynchops. In that genus, however, striations are confined to the lower two-thirds of the teeth (Carpenter, 1996), whereas in the Axel Heiberg specimens the striations extend nearly to the tip. Slender recurved teeth are also present in ornithocheirid pterosaurs, but in that group, the enamel surface is smooth, restricted to the apex of the tooth, and asymmetrically distributed (Averianov et al., 2003, 2005). Thus, on the basis of the general shape of the teeth, the extensive covering of enamel, and the distribution of striations on the enamel, we identify these teeth as Elasmosauridae gen. et sp. indet.


Two fossil adult elasmosaurs (NZGS CD425 and NZGS CD442) from New Zealand have been described as having teeth 35-40 mm long above the alveoli (Wiffen and Moisley, 1986). An adult elasmosaur from Cretaceous beds of Texas, measuring just under 6 m in total length, contained teeth with crowns up to 50.8 mm long and 9.5 mm in diameter (Schuler, 1950). The teeth collected from Axel Heiberg are noticeably smaller. A relatively complete juvenile elasmosaurid (MMM J. T. 86-100) from France contained teeth that are at maximum 54 mm long, including the root. The crown is described as comprising one-third of the total length (Bardet et al., 1999), indicating a crown length of 18 mm, which is comparable to the longer tooth from the Axel Heiberg vertebrate assemblage. Size estimates based on isolated teeth are inherently uncertain, but this comparison suggests the teeth recovered from Axel Heiberg Island were from a juvenile elasmosaurid no more that 3.9 m in total length.

While the majority of plesiosaur material is associated with marine shelf deposits, some specimens have been found associated with lagoonal (Forrest and Oliver, 2003), estuarine, or delta-margin environments (Cruickshank and Fordyce, 2002) and freshwater environments (Sato et al., 2005). Sedimentological evidence for the environment of deposition of the Axel Heiberg locality indicates that it was deposited in a lagoon or bay, but the evidence is equivocal as to the salinity of the water during deposition. While the occurrence of the plesiosaur suggests marine or brackish-water conditions, the associated fauna suggests a non-marine environment. Taxa found in association with plesiosaurs recovered from marine and near-shore lagoonal environments typically include a diverse assemblage of marine vertebrates. Mosasaurs (Kear, 2003) are typically found in association with plesiosaurs in Late Cretaceous vertebrate assemblages. Other marine vertebrates typically found in association with plesiosaurs include marine turtles (Whetstone, 1977; Kear, 2003) and various fishes, such as Enchodus, Coelodus, Oseroides, and Hoplopteryx (Ekrt et al., 2001). However, such taxa are absent in the Axel Heiberg assemblage. At this locality, the vertebrates found in association with the plesiosaur remains are all taxa that are typical of non-marine vertebrate assemblages. Thus the faunal evidence suggests that these teeth represent an additional non-marine occurrence of plesiosaurs.

Plesiosaur occurrences in non-marine settings are typically dominated by small individuals. In the Late Campanian Dinosaur Park Formation of Alberta, all the plesiosaur remains recovered are from individuals of small size, and one-third of the specimens show features indicative of juvenile individuals (Sato et al., 2005). The small size of the plesiosaur from the Axel Heiberg assemblage is consistent with the dominance of juveniles in non-marine environments.

The Cretaceous saw an explosion of plesiosaurian diversity, and distributions extended to above the Arctic Circle. In the Southern Hemisphere, high-latitude occurrences of Cretaceous plesiosaurs have been reported from Seymour Island of the Antarctica Peninsula (Fostowicz-Frelik and Gazdzicki, 2000), New Zealand (Wiffen and Moisley, 1986; Cruickshank and Fordyce, 2002), Argentina (Gasparini et al., 2003), and Australia (Keat, 2003). In addition to the new Axel Heiberg occurrence, high-latitude occurrences of plesiosaurs in the Cretaceous of the Northern Hemisphere include reports of plesiosaurs from the Kanguk Formation of Ellesmere Island (Fig. 43.4 of Ricketts and McIntyre, 1986) and from Upper Cretaceous sediments on Banks Island (Jutard and Plauchut, 1973), Eglinton Island (Russell, 1988), and Melville Island (Tozer and Thorsteinsson, 1964) in the western Canadian Arctic (Fig. 2). The ages of some of the western Arctic occurrences are not yet well constrained, but it is possible that they are from sedimentary correlates of the Kanguk Formation (e.g., Jutard and Plauchut, 1973).


Seasonal migration of vertebrates has been discussed for some Cretaceous Arctic vertebrates (Russell, 1987). But the high-latitude distribution of plesiosaurs may also be a further reflection of the extreme Turonian-Coniacian climatic warmth, which is apparent from other vertebrates found in the Axel Heiberg assemblage (Freidman et al., 2003).


We thank J. Massare for helpful discussions, G. Kloc for his skillful fossil preparation, T. Whiteley for his photographic expertise, and K. Carpenter and two anonymous reviewers for their comments. This work was supported by the U.S. National Science Foundation, the National Geographic Society, and the Canadian Polar Continental Shelf Project.


AVERIANOV, A.O., LESCHINSKIY, S.V., SKUTSCHAS, P.P., and REZVYI, A.S. 2003. Pterosaur teeth from the Lower Cretaceous of Russia and Uzbekistan. Sovremennaa Gerpetologia 2:5-11.

AVERIANOV, A.O., MARTIN, T., and BAKIROV, A.A. 2005. Pterosaur and dinosaur remains from the Middle Jurassic Balabansai Svita in the northern Fergana Depression, Kyrgyzstan (Central Asia). Palaeontology 48:135-155.

BARDET, N., GODEFROIT, P., and SCIAU, J. 1999. A new elasmosaurid plesiosaur from the Lower Jurassic of southern France. Palaeontology 42:927-952.

BROWN, D.S. 1981. The English Upper Jurassic Plesiosauroidea (Reptilia) and a review of the phylogeny and classification of the Plesiosauria. Bulletin of the British Museum (Natural History), Geology Series 35:253-347.

CARPENTER, K. 1996. A review of short-necked plesiosaurs from the Cretaceous of the Western Interior, North America. Neues Jahrbuch fur Geologie und Palaontologie Abhandlungen 201:259-287.

CRUICKSHANK, A.R.I., and FORDYCE, R.E. 2002. A new marine reptile (Sauropterygia) from New Zealand: Further evidence for a Late Cretaceous austral radiation of cryptoclidid plesiosaurs. Palaeontology 45:557-575.

EKRT, B., KOSTAK, M., MAZUCH, M., VALICEK, J., VOIGT, S., and WIESE, F. 2001. Short note on new records of Late Turonian (Upper Cretaceous) marine reptile remains from the Upohlavy quarry (NW Bohemia, Czech Republic). Bulletin of the Czech Geological Survey 76:101-106.

FORREST, R., and OLIVER, N. 2003. Ichthyosaurs and plesiosaurs from the lower Spilsby Sandstone member (Upper Jurassic), North Lincolnshire. Proceedings of the Yorkshire Geological Society 54:269-275.

FOSTOWICZ-FRELIK, L., and GAZDZICKI, A. 2001. Anatomy and histology of plesiosaur bones from the Late Cretaceous of Seymour Island, Antarctica Peninsula. Palaeontological Results of the Polish Antarctic Expeditions; Part III. Palaeontologia Polonica 60:7-31.

FRIEDMAN, M., TARDUNO, J.A., and BRINKMAN, D.B. 2003. Fossil fishes from the high Canadian Arctic: Further palaeobiological evidence for extreme climatic warmth during the Late Cretaceous (Turonian-Coniacian). Cretaceous Research 24:615-632.

GASPARINI, Z., SALGADO, L., and CASADIO, S. 2003. Maastrichtian plesiosaurs from northern Patagonia. Cretaceous Research 24:277-303.

HUBER, B.T., NORRIS, R.D., and MACLEOD, K.G. 2002. Deepsea paleotemperature record of extreme warmth during the Late Cretaceous. Geology 30:123-126.

JUTARD, G., and PLAUCHUT, B.P. 1973. Cretaceous and Tertiary stratigraphy northern Banks Island. In: Aitken, J.D., and Glass, D.J., eds. Proceedings of the Symposium on the Canadian Arctic. Saskatoon: Geological Association of Canada. 203-219.

KEAR, B.P. 2003. Cretaceous marine reptiles of Australia: A review of taxonomy and distribution. Cretaceous Research 24:277-303.

RICKETTS, B.D., and McINTYRE, D.J. 1986. The Eureka Sound Group of eastern Axel Heiberg Island: New data on the Eurekan Orogeny. Geological Survey of Canada Paper 86-1B:405-410.

RUSSELL, D.A. 1988. A checklist of North American marine Cretaceous vertebrates including freshwater fishes. Occasional Paper of the Tyrrell Museum of Palaeontology 4.62 p.

______. 1990. Mesozoic vertebrates in Arctic Canada. In: Harington, C.R., ed. Canada's missing dimension: Science and history in the Canadian Arctic Islands. Ottawa: Canadian Museum of Nature. 81-90.

SATO, T., EBERTH, D.A., NICHOLLS, E.L., and MANABE, M. 2005. Plesiosaur remains from non-marine to paralic sediments. In: Currie, P.J., and Koppelhaus, E.B., eds. Dinosaur Provincial Park: A spectacular ancient ecosystem revealed. Bloomington, Indiana: Indiana University Press. 249-276.

SCHULER, E. 1950. A new elasmosaur from the Eagle Ford Shale of Texas: The elasmosaur and its environment. Fondren Science Series 1. 32 p.

TARDUNO, J.A., and SMIRNOV, A.V. 2001. Stability of the Earth with respect to the spin axis for the last 130 million years. Earth and Planetary Science Letters 184:549-553.

TARDUNO, J.A., BRINKMAN, D.B., RENNE, P.R., COTTRELL, R.D., SCHER, H., and CASTILLO, P. 1998. Evidence for extreme climatic warmth from Late Cretaceous Arctic vertebrates. Science 282:2241-2244.

TARDUNO, J.A., COTTRELL, R.D., and SMIRNOV, A.V. 2002. The Cretaceous Superchron geodynamo: Observations near the tangent cylinder. Proceedings of the National Academy of Sciences of the United States of America 99:14020-14025.

TOZER, E.T., and THORSTEINSSON, R. 1964. Western Queen Elizabeth Islands, Arctic Archipelago. Geological Survey of Canada Memoir 332. 242 p.

WHETSTONE, K.N. 1977. Plesiosaur from Coon Creek Formation (Cretaceous) of Tennessee. Journal of Paleontology 51: 424-425.

WIFFEN, J., and MOISLEY, W.L. 1986. Late Cretaceous reptiles (Families Elasmosauridae and Pliosauridae) from the Mangahouanga Stream, North Island, New Zealand. New Zealand Journal of Geology and Geophysics 29:205-252.

WILSON, P.A., NORRIS, R.D., and COOPER, M.J. 2002. Testing the Cretaceous greenhouse hypothesis using glassy foraminiferal calcite from core of the Turonian tropics on Demerara Rise. Geology 30:607-610.


(Received 20 April 2005; accepted in revised form 20 July 2005)

(1) Department of Earth and Environmental Sciences, University of Rochester, Rochester, New York 14627, U.S.A.

(2) Corresponding author:

(3) Royal Tyrrell Museum of Paleontology, Box 7500, Drumheller, Alberta T0J 0Y0, Canada
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Author:Vandermark, Deborah; Tarduno, John A.; Brinkman, Donald B.
Geographic Code:1CANA
Date:Mar 1, 2006
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