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Otodus obliquus aff. Otodus subserratus
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| Otodus
obliquus teeth are found quite often on Sheppey, however teeth with serrations
are extremely rare. In the words of a good friend of mine, "as
rare as hens teeth". There is some debate as to whether
these serrations are due to the shark being of extreme age, or that of
an evolutionary development towards later forms is taking place. I hope
that someone can put me right on this issue. The examples that I am able
to exhibit on this page were found almost at opposite ends of the section.
One was found at Paddies Point at the far westerly end, which is the youngest
part of the section, where division D of the London clay moves into division
E. The other was found at Warden Point, towards the easterly end of the
section, much earlier in division D. The tooth could have come from the
top of the cliff which would place it nearer in time to the Paddies Point
specimen, but there could be as much as 3 million years between them |
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| This
image represents a typical Otodus tooth, and is figured here for comparison
with the serrated examples. |
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| This
tooth was found by Don Pople of the Medway Mineral and Lapidary
Society at Warden Point while scanning the deposits on the beach
for Shark's teeth. It is a unique specimen, and is wonderfully preserved.
Note the serrations on the lateral cusps. |
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Details
showing the serrations clearly
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This specimen was found near to Paddies point and may be slightly pathalogical, but the serrations are clearly evident either side of the blade. Collection of Jim Craig |
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Details
of the serrations.
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| An
unusual Otodus tooth found by Frederic Migom in slumped clay at Hensbrook
while on a field trip with me on Saturday 2nd. of June. The tooth is
not serrated but displays some characteristics similar to the teeth
above. Probably derived from a very old shark, the multiple side cusps
are very distinctive |
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