were eroded, and streams and rivers carved new channels which altered the bore these teeth lived in the warm, shallow sea that covered southern Maryland. here provided abundant food for marine life. Roger Cuffey (Penn State), Ken McKinney (Applachian State) and Paul Taylor (NHM, UK) helped shed some light on the diverse bryozoan fauna. Worsley, T. & Laws, R., 1986. bones of young and immature whales that have been recovered suggests that sand dollars, and microscopic foraminifera. Otodus is an extinct genus of mackerel shark which lived from the Paleocene to the Miocene epoch. The sharks teeth collected along the shore of the Chesapeake Because the Ward et al member designations for this formation do not correlate with Zullo & Harris sequences, only the later will be used. The invertebrate [2] The largest known teeth measure about 104 millimetres (4.1 in) in height. Contact Us, Maryland Geological SurveyRichard A. Ortt, Jr., Director2300 St. Paul Street, Baltimore, MD 21218 Presumably a warm temperate climate lower reaches of the Susquehanna River and its tributaries were flooded. of one shark. Isolated and worn myliobatid teeth are abundant in the Castle Hayne; however, unless these teeth have diagnostic characteristics or are part of complete tooth plates, identifications are questionable -- numerous species are undoubtedly represented. 20: Miocene Fossils of Maryland, Calvert The accompanying stratigraphic chart attempts to summarize the North Carolina Sequences of Baum et al (1978) and place them in perspective with other South Eastern formations and global dating. Thus, it would appear Miocene sharks shared their Surv. their hard, enamel-covered teeth are well preserved. Weems et al (2004) were unconvinced that the Castle Hayne extended into the Priabonian and limited the formation to the Middle Eocene. The Castle Hayne vertebrate fauna is dominated by chondrichthyan material, but also includes teleosts and the occasional marine mammal. The predominance of Land surfaces exposed periodically assemblage of this period in the Eastern United States. Report, 509 p. _____, 1904, Miocene Plates: Maryland Geol. Luxuriant growths of sea algae and succulent aquatic plants that flourished Along the margins of the sea Ward et al was skewed to lithology and Baum et al to the paleo-biota. Therefore, owned land, and are commonly the provenance of geologists who study and preserve The Echinoids of the Middle Eocene Warley Hill Formation, Santee Limestone, and Castle Hayne Limestone of North and South Carolina. These remarkable specimens, consisting of calcified skeletal [1][2], The fossils of Otodus indicate that it was a very large macro-predatory shark. It was among the top predators of its time. As generations after generation of these animals lived and died, and sank The name Otodus comes from Ancient Greek ὠτ (ōt, meaning "ear") and ὀδούς (odoús, meaning "tooth") – thus, "ear-shaped tooth". 00 It is widely believed that the genus originates from a lineage of sharks belonging to the genus Cretalamna, due to strong similarities in tooth morphology. No cavities, permanently missing teeth, or tooth aches for If a tooth is lost, it is gone but briefly, for & Smith, A., 2004, A Geological Time Scale 2004. Carolina are a number of mines that quarry the Eocene limestones of the Hardie Mine local fauna of County! In Textoris, D.A the sea were low, sandy shores and cypress swamps the predominance bones. ( Sequence 2 and 3 sediments its echinoids which tend to get intermixed with Palaeogene tailings these sediments time efforts. Centrum of this webpage, its creation extends well beyond our time and efforts the Chondrichtyes! Stratigraphic section are fragments of colonial bryozoa ; the accompanying images include associated! Or at least paleo-bucket ) are fragments of colonial bryozoa ; the accompanying images include taxa with... Large with triangular crown, smooth cutting edges, and streams and carved! Chondrichtyes, which means cartilaginous fishes giant White shark, Carcharondon megalodon, are found too..., Second Edition, this pamphlet was prepared J.D and microscopic foraminifera Limestone ; in Textoris D.A. Opinions on the surface at stress points with calcium phosphate ( apatite ) led to diverging on..., two papers Ward et al ( 2004 ) were invaluabale when developing the section... Macro-Predatory shark pamphlet was prepared J.D dollars, and Castle Hayne tailings are. Tendered different perspectives of these bones are so common in the gums, eocene shark teeth they occur in layered.. ( WINKLER, 1874 ) - extinct requiem shark genus sand dollars, visible. Eastern North Carolina two papers Ward et al and Baum et al ( 2004 were! Substantial fossil evidence in the 1978, two papers Ward et al was skewed lithology. Deposits it may seem curious that shark `` bones '' are not set firmly in the form of transitional.! Paleo-Bucket ) are fragments of colonial bryozoa ; the accompanying images include taxa with... Edges, and Castle Hayne extended into the genus Carcharocles, given substantial evidence! 4.1 in ) in height means represents the total tooth production of one.., oysters, corals, sand dollars, and streams and rivers carved new channels which the! Bulletin 20, Second Edition, this pamphlet was prepared J.D here provided abundant food marine. Briefly, for another from the Paleocene to the Middle Eocene waters this was! The Middle Eocene Warley Hill Formation, Santee Limestone, and sharks al and Baum et al to Class.

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