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Imprinty

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Hello! 

Found this on my grandparents farm in southern Missouri. Any ideas what it is? 

Thanks! Btw, love this helpful forum. Thank you!

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Orthocone Cephalopod. :) 

orthocone_nautiloid.jpg

Great find. 

Regards,

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Definitely orthoconic cephalopod orthocone. Nice find ! :)

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" We are not separate and independent entities, but like links in a chain, and we could not by any means be what we are without those who went before us and showed us the way. "

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Cool cephalopod :)

 

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Every single fossil you see is a miracle set in stone, and should be treated as such.

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Because this was found in southern Missouri just out on the ground and not buried. And it's split down the middle and very smooth on too... Is there a possibly this was used by a native Indian tribe as a tool of some sort? Are these fossils normally found in southern Missouri and are they commonly split? Thanks!

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18 minutes ago, Imprinty said:

Because this was found in southern Missouri just out on the ground and not buried. And it's split down the middle and very smooth on too... Is there a possibly this was used by a native Indian tribe as a tool of some sort? Are these fossils normally found in southern Missouri and are they commonly split? Thanks!

Hi Imprinty!

 

I really like your orthocone nautiloid - it's a lot bigger than the ones I find up here in the Toronto area!  I've found a few embedded in rocks and a few that were just lying around in between creek-bed rocks - the fact that it was just lying around may just mean that it became separated from the rock that it was within due to exposure to the elements - it doesn't necessarily mean that it was used by somebody at some point (I think).

 

As for why it looks split - could the split be where the siphuncle once existed in the living animal?  The siphuncle wasn't always located in the centre of the phragmocone (shell).

 

Let's see what others have to say...

 

Thanks for sharing your find, and enjoy your fossil!
 

Monica

Edited by Monica
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The way your fossil looks is common. The split down the middle often occurs because of aggressive erosion like what can occur in the bed or bank of a waterway. The initial exposure may have been parallel to the flow and material in the water wore one side away before it was washed out. It is also common to find fossils completely free of the matrix. When the minerals that formed the fossil are harder than the matrix a very well preserved fossil can be found completely loose and floods can spread them over areas with no apparent streambed.

 

The siphuncle of a nautiloid is generally central compared to ammonoids but can be somewhat out of center to different degrees.  Ammonoids always have a siphuncle near the ventral margin. I suppose there could be exceptions to both of these norms but they are a good general rule for telling them apart.

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