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3 Stingrays: opportunities for discovery

Chondrichthyes, Myliobatiformes

Despite being an ecologically-important group of vertebrates in Aotearoa New Zealand and around the world, and being found relatively commonly as fossils, New Zealand fossil stingrays have received very little attention. Indeed, while there are examples of fossil sharks, fossil sawsharks, and fossil bony fish from New Zealand that have been identified as distinct species (see Giant moonfish buried three layers deep), the same level of description has never been reported for a fossil stingray from New Zealand. Which means that at the time of writing, there are many opportunities to contribute to the New Zealand fossil record by studying and describing stingrays.

Two images of a fossil tooth plate from an unidentified species of stingray. The fossil is yellow to light brown and has the specimen ID number for the fossil is OU22788. The upper image shows the side of the tooth plate that has the occlusal or food-grinding surface towards the top of the figure. The lower image shows the ridges on the ventral or underneath side of the fossil that would have anchored the tooth plate into the jaw.

Two views of a tooth plate from an unidentified species of stingray (specimen OU 22788). The upper view shows the side of the tooth plate with the occlusal surface (i.e. food-grinding surface) towards the top. The lower view shows the ridges on the ventral side (underneath side) that anchor the tooth plate into the jaw. Image credit: JH Robinson.

One of the challenges faced with describing ancient stingrays is that their skeletons are almost entirely constructed from cartilage which tends to break down before it can be preserved in the fossil record. Fortunately, stingrays have tooth plates that are constructed from mineralised tissues and which preserve very well as fossils. These tooth plates have a distinctive shape as they are narrow bars with a smooth occlusal surface on one side (surface for processing food), while on the opposite side there is a surface with ridges where the tooth is embedded into the jaw. Stingrays use their tooth plates to crush the carapaces of crabs and the shells of bivalves, their most common types of prey. Hence, the parts of the stingray skeleton that is most likely to preserve as a fossil is also likely to be informative about ancient diet.

There are many locations across New Zealand where fossil tooth plates have been found. For example, the University of Otago Geology Museum collections include stingray tooth plates from Cosy Dell and Brydone in Southland. This material is a great starting point for any paleontologist who aspires to fill in the major gap in the New Zealand fossil record by studying ancient stingrays.

—Written by Daniel B Thomas

Specimen number: OU 22788 Age: Approximately 26 million years old (Oligocene, Duntroonian stage)
Locality: Waimumu, Southland Rock Formation: Chatton Formation
Collected by: GSNZ fieldtrip attendee
Citation: Lee D, Lindqvist J, Beu A, Robinson J, Ayress M, Morgans H, Stein J. 2014. Geological setting and diverse fauna of a Late Oligocene rocky shore ecosystem, Cosy Dell, Southland. New Zealand Journal of Geology and Geophysics 57:195–208. doi.org/10.1080/00288306.2014.898666
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