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belemniten

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I found this in Rosenfeld (Germany). Its from the "Arietenkalk".

Think it could be a crinoid stem, but this would be very unusual for this location.

Please help me ;)

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post-19413-0-71121600-1457471670_thumb.jpg

Many greetings from Germany ! Have a great time with many fossils :)

Regards Sebastian

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100% crinoid stem.

Yes

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"There has been an alarming increase in the number of things I know nothing about." - Ashleigh Ellwood Brilliant

“Try to learn something about everything and everything about something.” - Thomas Henry Huxley

>Paleontology is an evolving science.

>May your wonders never cease!

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"but this would be very unusual for this location." Well then, it seems you have found a rarity, congrats!!!

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This would appear to be a crinoid, as stated.

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

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100% crinoid stem.

One could argue the percentage. Where's the lumen ? Appears to be a cast.

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One could argue the percentage. Where's the lumen ? Appears to be a cast.

The lumen is tiny in a lot of Pentacrinites/Isocrinus type crinoids. That looks like normal echinoderm calcite cleavage so maybe it's just filled in by a bit of diagenetic calcite growth.

edit: I've just looked at a few of mine from the Lower Lias and the lumens are completely invisible in them.

Edited by TqB
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Tarquin

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I agree.

The Arietenkalk Formation in Germany date back to the Jurassic.

" The Hettangian-Sinemurian boundary is marked by the hiatus. The Arietenkalk Formation (up to 25m) is characterized by fossil-rich limestone beds with intercalated clay layers. The base is defined by the "Kupferfelsbank",a limestone bed with locally abundent iron ooids and bored pebbles. Gryphaeid oysters,giant ammonites (Arietitidae),brachiopods and echinoderm clasts are the most important fossils in this formation (Geyer&Gwinner 1984). The Arietenkalk Formation is overlain by the Optususton Formation (up to 65m). The dark grey clays and marly clays often exhibit concretions of siderite and phosphorite; quartz sand and mica increase upwards. Several fossil-rich marl layers occure in the upper part of the succesion;cach marks the onset of a different ammonite fauna. Other common fossils include brachiopods,bivalves,ammonites and crinoids (Geyer&Gwinner 1984). "

The geology of Central Europe, Vol 2: Mesozoic and Cenozoic - Tom McCann

The lumen in this kind of crinoid columnals is tiny and when is infilled with recrystallized sediments is almost indistinguishable.

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Thanks guys for your help !

All posts are very helpful ! thanks

So i am lucky that i found an crinoid stem ;)

Many greetings from Germany ! Have a great time with many fossils :)

Regards Sebastian

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100.01 % :D

Crinoid stem as well!!! Nice find

Thanks !

Many greetings from Germany ! Have a great time with many fossils :)

Regards Sebastian

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For sure crinoid stems.

Congratulations, belemniten for your uncommon find...

Here in Portugal they are abundant on Jurassic layers.

Regards,

Guguita

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For sure crinoid stems.

Congratulations, belemniten for your uncommon find...

Here in Portugal they are abundant on Jurassic layers.

Regards,

Guguita

Thanks :)

Many greetings from Germany ! Have a great time with many fossils :)

Regards Sebastian

Belo.gif

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