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Fossil With A Fourfold Symmetry


Gen. et sp. indet.

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It is a central European glacial erratic boulder (Geschiebe) in a form of a calcitic fossil. It is somehow similar to tabulates, stromatoporoids, and rugosans found in the same sediments. I think it might be a part of one of these, or something different (rhodophyte, chaetetid, conularid) :) As you can see, the walls of the concave square cells are convex and sinous - but still not randomly. The other side of the rock is uninformative. The upper side of the specimen is ca. 11 mm long. Please help.

post-5671-0-75860400-1313067252_thumb.jpgpost-5671-0-42195100-1313067264_thumb.jpg

Edited by Gen. et sp. indet.
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Nobody???

ckmerlin, thanks for the try & the link

Pleasure hope the link was helpful

"A man who stares at a rock must have a lot on his mind... or nothing at all'

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