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| Produced 
        by the Population Genetics and Evolution class, Furman University | ||||
|  | The 
          Devonian: Cladoselache |  | ||
| Cladoselache 
        are one of the most well-known early sharks, and they resemble the modern 
        mackerel shark (Martin 2003). They lived in the warmer waters over eastern 
        North America (Miller 2000) and their fossils were first found in the 
        Cleveland Shale. Many of the fossils that have been found are actually 
        whole, and some even include remnants of internal organs (Coates 2010). 
        These sharks grew to be about three feet long, and had several unique 
        characteristics. They had weaker jaws than modern sharks; however the 
        muscles used to close their jaws were very strong. Another interesting 
        feature is that they had large forked tails, which probably aided them 
        in swimming faster. This means that they were most likely preyed upon 
        by larger fish, such as Dunkleosteus (Miller 2000). However, 
        they were predators for other fish as well, as some smaller fish fossils 
        have been found within the stomachs of these sharks (Coates 2010). Cladoselache, 
        unlike most other sharks, were not covered in dermal denticles (Martin 
        2003). In fact, they are only known to have compound scales around their 
        head and fins, which is a very odd characteristic for sharks. Perhaps 
        even more unique, however, is the fact that Cladoselache do not 
        appear to have claspers, which is a male internal reproductive structure. 
        As a result, little is known to how they reproduced; but they clearly 
        managed to reproduce somehow (Coates 2010)! Page by Lindsay Gerzel |  | 
| Cladoselache. Image from: Martin 2003. | |
| Coates M. 2010. Cladoselache. AccessScience@McGraw-Hill. Accessed February 24, 2010 Martin RA.2003. Ancient Sharks: Cladoselache. Biology of Sharks and Rays. Accessed February 24, 2010. Miller DW. 2000. Cladoselache. Discovery Education. Accessed February 24, 2010. |