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Worm or something else ?


TUMNI GREEN

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This doesn't look like a situation where one would expect to find trace fossils.

I would suspect that possibly it may be where someone extracted a fossil in the past .

Can you give us anymore supporting  information ?

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Haven't had any experience with chalk yet. It must be a little different than average limestone.

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56 minutes ago, Rockwood said:

Haven't had any experience with chalk yet. It must be a little different than average limestone.

Just purer calcium carbonate, so usually more brittle and powdery. Also reacts with vinegar vigorously.

 

Is there a possibility this could be an ammonite aptychus?

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58 minutes ago, WhodamanHD said:

Just purer calcium carbonate, so usually more brittle and powdery.

I've seen traces in limey sandstone, but not purer calcium carbonate than that. Is the coccolith origin what makes the difference ? Or is it just my perception ?

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This form seems to be barely differentiated from the matrix. An in-filled burrow makes sense.

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This is an in-filled burrow trace fossil, probably made by a crustacean. Note the semi parallel scratch marks that start and stop and meander slightly. These are not the more regular and parallel features expected from coral, polychaete worm tubes or an aptychus.

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Can we have the location, geological settings of the find, dimensions and a few more clear pictures from different angles of the specimen ?

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Quite a nice burrow piece. :)

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On ‎18‎/‎04‎/‎2018 at 10:57 AM, Rockwood said:

Haven't had any experience with chalk yet. It must be a little different than average limestone.

Here is an algae in chalk : goniolina hexagona

post-2385-0-48896400-1464377778.jpg

 

 

And it's back size.

 P3231932.JPG.a5b25c04c2fd9fc75cc1ed859815440c.JPG

 

 

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12 minutes ago, fifbrindacier said:

Here is an algae in chalk

I'm taking this to mean that chalk has a slightly different preservation potential than other marine limestones.

I'm allotting a couple days of spring vacation in Denver for a bit of exploring over in Kansas. ;)  

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