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Earliest record of dental pathogen discovered in a North American Eocene rabbit

LLucja Fostowicz-Frelik and Grzegorz J. Frelik
Earliest record of dental pathogen discovered in a North American Eocene rabbit
Palaios (December 2010) 25 (12): 818-822

Abstract

Mammalian teeth are made of extremely hard and durable calcified tissues, which make them superb candidates for fossilization. The enamel crown, the outermost layer in the erupted tooth, precludes most microorganisms from entering into the underlying dentine and cementum, supporting tissues that are more vulnerable to microbial destructive action. Here we report the discovery of a single tooth of the late Eocene (ca. 35 Ma) North American basal lagomorph Megalagus, clearly containing filamentous and occasionally branching microfossils. The remarkably preserved microfossils are most similar to actinomycetes, gram-positive Eubacteria. We argue that these microorganisms were growing during the animal's life and thus document the first known tooth infection in placental mammals. Our findings provide insight into the initial development of mammal-dental pathogen interactions.


ISSN: 0883-1351
Serial Title: Palaios
Serial Volume: 25
Serial Issue: 12
Title: Earliest record of dental pathogen discovered in a North American Eocene rabbit
Affiliation: Polish Academy of Sciences, Vertebrate Paleontology Department, Warsaw, Poland
Pages: 818-822
Published: 201012
Text Language: English
Publisher: Society for Sedimentary Geology, Tulsa, OK, United States
References: 27
Accession Number: 2011-006713
Categories: Vertebrate paleontology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 1 table
N45°45'00" - N46°34'60", W112°37'00" - W111°40'00"
Secondary Affiliation: University of Portsmouth, GBR, United Kingdom
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States. Reference includes data supplied by SEPM (Society for Sedimentary Geology), Tulsa, OK, United States
Update Code: 201104
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