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Enigmatic carbonate isotope values in shark teeth: Evidence for environmental and dietary controls. Palaeogeography, Palaeoclimatology, Palaeoecology, 635, Article 111943
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Applying zinc isotopes to investigate the trophic positions of extinct marine vertebrates, including the megatooth shark Otodus megalodon, in ancient marine ecosystems [Abstract]. EGU General Assembly 2024, Vienna, Austria
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First-hand observations of rare piebaldism in the nurse shark, Ginglymostoma cirratum, near East Bahia Honda, Florida Keys, Florida. Florida Scientist, 86(1), 13–16
Revisiting body size trends and nursery areas of the Neogene megatooth shark, Otodus megalodon (Lamniformes: Otodontidae), reveals Bergmann’s rule possibly enhanced its gigantism in cooler waters. Historical Biology, 35(2), 208–217
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Tessellated calcified cartilage and placoid scales of the Neogene megatooth shark, Otodus megalodon (Lamniformes: Otodontidae), offer new insights into its biology and the evolution of regional endothermy and gigantism in the otodontid clade. Historical Biology, in press
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Endothermic physiology of extinct megatooth sharks. Proceedings of the National Academy of Sciences, 120(27), Article e2218153120
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Trophic position of Otodus megalodon and great white sharks through time revealed by zinc isotopes. Nature Communications, 13, Article 2980
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Cenozoic megatooth sharks occupied extremely high trophic positions. Science Advances, 8(25), Article eabl6529
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Body, jaw, and dentition lengths of macrophagous lamniform sharks, and body size evolution in Lamniformes with special reference to ‘off-the-scale’ gigantism of the megatooth shark, Otodus megalodon. Historical Biology, 33(11), 2543–2559
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Ontogenetic growth pattern of the extinct megatooth shark Otodus megalodon-implications for its reproductive biology, development, and life expectancy. Historical Biology, 33(12), 3254–3259
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Fossil fishes from a lag deposit within the Upper Cretaceous Mancos Shale in New Mexico, USA, with comments on correlative Turonian-Coniacian time-transgressive lags in the Western Interior Seaway of North America Cretaceous Research, 26, Article 104886
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Chondrichthyans from the Lower Clayton Limestone Unit of the Midway Group (Paleocene) near Malvern, Arkansas, USA, with comments on the K/Pg boundary. Paläontologische Zeitschrift, 94, 561–593
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Macroborings in Otodus megalodon and Otodus chubutensis Shark Teeth from the Submerged Shelf of Onslow Bay, North Carolina, USA: Implications for Processes of Lag Deposit Formation. Ichnos, 27(2), 122–141
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Lamniform and Carcharhiniform Sharks from the Pungo River and Yorktown Formations (Miocene–Pliocene) of the Submerged Continental Shelf, Onslow Bay, North Carolina, USA. Copeia, 106(2), 353–374
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Chondrichthyans from a lag deposit between the Shark River Formation (Middle Eocene) and Kirkwood Formation (Early Miocene), Monmouth county, New Jersey. Paludicola, 10(3), 149–183
Chondrichthyans from theTallahatta-Lisbon Formation Contact (Middle Eocene), Choctaw County, Silas, Alabama. Paludicola, 9(4), 183–209
Squalicorax Chips a Tooth: A Consequence of Feeding-Related Behavior from the Lowermost Navesink Formation (Late Cretaceous: Campanian-Maastrichtian) of Monmouth County, New Jersey, USA. Geosciences, 2(2), 109–129
Trace and Minor Element Chemistry of Modern Shark Teeth and Implications for Shark Tooth Geochronometry. In Wai, M., and Gong, X.G. (Eds), Strontium: Chemical Properties, Applications, and Health Effects, Nova Science Publishers, ISBN: 978–1–62257–631–9: 27–53
Chondrichthyans from the Lower Ferron Sandstone Member of the Mancos Shale (upper Cretaceous: Middle Turonian) of Emery and Carbon Counties, Utah, USA. Journal of Paleontology, 84(2), 248–266
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Large carcharhinoid-type shark vertebrae in the Upper Cretaceous of New Jersey: evidence for an anacoracid origin. Northeastern Geology and Environmental Science, 30 82), 118–129
Strontium isotopic signatures in the enameloid and dentine of upper Cretaceous shark teeth from western Alabama: paleoecologic and geochronologic implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 264(1–2), 188–194
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The paradox of large carcharhinoid-type shark vertebrae in the Upper Cretaceous of New Jersey [Abstract]. In Contributions to the Paleontology of New Jersey(II), E Rainforth, ed., Geological Association of New Jersey. Proceedings of the XXIV Annual Meeting: 69–84
Evidence for a shark-bitten turtle costal from the lowermost Navesink Formation (Campanian-Maastrichtian) Monmouth County, New Jersey. Northeastern Geology and Environmental Science, 28(2), 174–181
Chondrichthyans from the Arkadelphia Formation (Upper Cretaceous: upper Maastrichtian) of Hot Spring County, Arkansas. Journal of Paleontology, 80(4), 700–716
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Rostral morphology of the Late Cretaceous sawfish, Ischyrhiza mira, from the lower Navesink Formation (Campanian-Maastrichtian), Monmouth County, New Jersey. Northeastern Geology and Environmental Science, 27(1), 37–48
Chondrichthyans from the Fairpoint Member of the Fox Hills Formation (Maastrichtian), Meade County, South Dakota. Journal of Vertebrate Paleontology, 24(4), 780–793
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Reconstructing the Rostrum of the Sawfish, Ischyrhiza mira, from the lower Navesink Formation (Campanian-Maastrichtian), Monmouth County, New Jersey [Abstract]. GSA Conference 2003, Seattle Annual Meeting(November 2–5, 2003) Paper No. 221–19
A Survey of Non-tooth Chondrichthian Hard-parts from the Lower Navesink formation (Maastrichtian) in Monmouth County, New Jersey. Northeastern Geology and Environmental Science, 24(4), 282–292
Pathologic tooth deformities in modern and fossil chondrichthians: a consequence of feeding-related injury. Lethaia, 33(2), 103–118
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Mixing of Santonian and Campanian chondrichthyan and ammonite macrofossils along a transgressive lag deposit, Greene County, western Alabama. Southeastern Geology, 37(4), 205–216
Reworked Campanian and Maastrichtian macrofossils in a sequence bounding, transgressive lab deposit, Monmouth County, New Jersey. Northeastern Geology and Environmental Science, 18, 234–252