File:Isotelus maximus fossil trilobite with healed bite mark (Flat Run Trilobite Lagerstatte, Arnheim Formation, Upper Ordovician; Flat Run Quarry, far-southwestern Highland County, southwestern Ohio, USA) 1 (15262673675).jpg
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DescriptionIsotelus maximus fossil trilobite with healed bite mark (Flat Run Trilobite Lagerstatte, Arnheim Formation, Upper Ordovician; Flat Run Quarry, far-southwestern Highland County, southwestern Ohio, USA) 1 (15262673675).jpg |
Isotelus maximus Locke, 1838 trilobite with healed bite mark from the Arnheim Formation (Upper Ordovician) of southwestern Ohio’s Flat Run Trilobite Lagerstätte (public display, Orton Geology Museum, Ohio State University, Columbus, Ohio, USA). Trilobites are important and common fossils in Paleozoic rocks, especially in the Cambrian. Much is known about their paleobiology, ontogeny, evolutionary patterns, etc. One of the less well known aspects of trilobitology is the significance of malformations, or deformities in the preserved exoskeleton. One category of trilobite malformation is healed bite marks, which can be seen here. This large outstretched specimen has a healed injury on the right side of the cephalon (head). The exoskeleton has partially regenerated and a small, anomalous genal spine has started growing. The regenerated exoskeleton indicates that the injury was not lethal - the bite mark is evidence of unsuccessful predation. This trilobite specimen, plus the large enrolled Isotelus specimen shown elsewhere in this photo album, have healed bite marks on their right sides. Published census information of bitten trilobites has shown that a statistically significant percentage of specimens have bite marks on their right sides. This is a great example of “handedness” (behavioral lateralization) in the fossil record. Note: Examination of this specimen by the trilobite research Danita Brandt has resulted in a re-interpretation of the malformation present on the right side. This may be a healed injury sustained during molting, rather than a healed predatory bite mark. Classification: Arthropoda, Trilobita, Polymerida, Asaphidae Stratigraphy & age: Flat Run Trilobite Lagerstätte, near-top Sunset Member, mid-Arnheim Formation, lower Richmondian Stage, upper Cincinnatian Series, upper Upper Ordovician Locality: Flat Run Trilobite Quarry, far-southern Clay Township, far-southwestern Highland County, just E of Sicily, E of Mt. Orab, southwestern Ohio, USA. Collected & prepared by Dan Cooper. Published references on bitten and malformed trilobites: Babcock & Robison (1989) - Nature 337: 695-696. Babcock (1993) - Journal of Paleontology 67: 217-229. Babcock (2007) - Role of malformations in elucidating trilobite paleobiology: a historical synthesis. in Fabulous fossils - 300 years of worldwide research on trilobites. New York State Museum Bulletin 507: 3-19. |
Date | |
Source | Isotelus maximus fossil trilobite with healed bite mark (Flat Run Trilobite Lagerstatte, Arnheim Formation, Upper Ordovician; Flat Run Quarry, far-southwestern Highland County, southwestern Ohio, USA) 1 |
Author | James St. John |
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This image was originally posted to Flickr by jsj1771 at https://www.flickr.com/photos/47445767@N05/15262673675. It was reviewed on 6 May 2015 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-2.0. |
6 May 2015
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Orientation | Normal |
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Horizontal resolution | 96 dpi |
Vertical resolution | 96 dpi |
Software used | Adobe Photoshop CS2 Macintosh |
File change date and time | 19:28, 16 September 2014 |
Color space | Uncalibrated |
Image width | 612 px |
Image height | 952 px |
Date and time of digitizing | 11:08, 14 August 2007 |
Date metadata was last modified | 15:28, 16 September 2014 |