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Posted

Found in Holmes County, Mississippi in an area heavily used by Native Americans. This area was identified as a trading post by an archeological excavation per MDOT. Can someone help identify this? 

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Posted

Can You show the edges and other side?

Also (in second picture lower left, third picture upper right) there is a strip that looks folded over on itself. Can You take a close up of this feature?

 

 

Posted

At first glance at the “bottom” (light gray area) my guess was palm. However the “fibers” in their arrangement do not resemble others I have found. 

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Posted

I am thinking roots, but am not sure.

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Posted

It does very much resemble palm roots.

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Posted

Teredino (shipworm bivalve) borings in wood?

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Posted

I think TqB has it. If palm roots, the "fibers" would be much more dense. Good call!

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Posted

Yup, looks like shipworm to me, too. 

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Posted

The diameter of the tubes / borings is under 1mm, so it's not enough for Teredo / Teredolites (~1cm). Maybe they are close to Trypanites .

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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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Posted
34 minutes ago, abyssunder said:

The diameter of the tubes / borings are under 1mm, so it's not enough for Teredo / Teredolites (~1cm). Maybe they are close to Trypanites .

 

That's more likely. The matrix doesn't look like wood anyway, just sediment.

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Posted

+ 1 for worm borings

Posted

That was my thought also. The matrix looks like a sedimentary rock, so it could be a good hardground for Trypanites isp. (worms).

 

" More recently it has been argued (Plewes, 1996; Palmer et al., 1997) that Trypanites is best confined to cylindrical borings that are much longer than wide (ratio usually greater than 20:1) in lithic substrates.
Smaller borings that gently expand into the substrate (cylindroclavate borings), and which are often encountered in both lithic and biogenic substrates as far back as the Cambrian, are more properly referred to Paleosabella Clarke, 1921. (...) "

 

excerpt from Cole, A.R., Palmer, T.J. 1999. Middle Jurassic worm borings, and a new giant ichnospecies of Trypanites from the Bajocian/Dinantian unconformity, southern England. Proceedings of the Geologists' Association. 10 (3): 203–209

 

 

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image from here

 

 

" 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. "

Thomas Mann

My Library

Posted

In the first picture there is either stratification or growth rings.

Either way it does not fit with worm boring.

 

 

Posted

I noticed the first pic too, looks more fibrous to me. My first thought was bryozoans of some sort, but I could be way off on that.

Posted
11 hours ago, ynot said:

In the first picture there is either stratification or growth rings.

Either way it does not fit with worm boring.

 

9 hours ago, Wrangellian said:

I noticed the first pic too, looks more fibrous to me. My first thought was bryozoans of some sort, but I could be way off on that.

 

I've changed my mind, that's true and does knock the borings idea. I think the fibres may be too narrow for bryozoan though there's certainly a resemblance. Possibly something spongy?

It's a really intriguing one, I'd like to see one or two more really clear photos and an age would help...

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Posted

The crystals in the rock look metamorphic to me. You don't suppose the fibrous texture is serpentine ? 

Posted
3 hours ago, Rockwood said:

The crystals in the rock look metamorphic to me. You don't suppose the fibrous texture is serpentine ? 

Serpentine is a regional metamorphic rock, so no it is not serpentine.

 

 

Posted
35 minutes ago, ynot said:

regional metamorphic rock

Could you elaborate ?

Posted
1 hour ago, Rockwood said:

Could you elaborate ?

Be happy to.

Serpentinite is a metamorphic rock that is mostly composed of serpentine group minerals. Serpentine group minerals antigorite, lizardite, and chrysotile are produced by the hydrous alteration of ultramafic rocks. These are igneous rocks that are composed of olivine and pyroxene (peridotite, pyroxenite).

And by regional I mean it covers large areas like marble or slate, which are also regional metamorphic rocks.

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Posted

Basalt flows often smother fossiliferous rocks. The fibers could not be transported that far during the process ?

Posted
2 minutes ago, Rockwood said:

Basalt flows often smother fossiliferous rocks. The fibers could not be transported that far during the process ?

For the "tubes" to be filled with igneous rock and then be altered to a (highly) metamorphic serpentine the matrix rock would have been altered also.

The whole scenario seems far fetched to Me.

 

 

 

 

Posted
24 minutes ago, ynot said:

For the "tubes" to be filled with igneous rock and then be altered to a (highly) metamorphic serpentine the matrix rock would have been altered also.

The whole scenario seems far fetched to Me.

 

 

I am confident that it comes as no surprise that I would come up with something like it. :)

Posted

+1 for fossil palm.

Posted
19 hours ago, Echinoid said:

+ 1 for worm borings

"Shipworms" are not worms like earthworms or so... Shipworms are a kind of bivalve that can bore through wood/stone. As the name suggests, they are often found in ships, and are dangerous as they destabilize the wood of the ship. Luckily most ships are made of metal now, so that is no longer really a problem. 

Max Derème

 

"I feel an echo of the lightning each time I find a fossil. [...] That is why I am a hunter: to feel that bolt of lightning every day."

   - Mary Anning >< Remarkable Creatures, Tracy Chevalier

 

Instagram: @world_of_fossils

Posted

Very nice finds. Although I agree with the others the matrix looks more like a sedimentary rock it did make me think of this inherited sample of petrified wood with borings from nearby Arkansas that looks somewhat similar to your specimen in both coloration and some of the longer linear boring arrangements--but there are some definite differences and has much different boring meanders. You can also actually see some of the individual growth rings of the wood in places in my sample. I wish I had some more details on where my piece came from and its age but I don't unfortunately.

 

I wish we could see clearer details of the matrix in yours and the borings/linear features. I wonder what yours would look like if it was polished up at all and if the matrix between the borings and a cross section thru it would show any hidden details about its composition.   

 

Thanks for showing us--very cool piece.  

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Regards, Chris

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