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Mineral Wells Fossil Park


Geogrl13!

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Good afternoon friends,

 

I was wondering if someone could kindly explain why the two trilobites I found at Mineral Wells Fossil Park around Dallas Texas fossilized so differently?

The off white trilobite is extremely brittle and can easily crack, while the other was fossilized in stone. I just do not understand the fossilization process of the two.

 

Thank you :)

Mirna Villarreal

 

The fossils are around 300 million years old

image 2.JPG

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Hopefully someone familiar with the site can confirm but this is my take: as you may know, fossils are usually the biological material replaced by minerals. In one case, it seems you have it preserved in a calcium carbonate rock (calcite or limestone or chalk) and in the other case something else, maybe a silica of some sort. They probably come from different stratigraphies, hence the different preservation. If any pieces of the white one have fallen off and your willing to put the piece in vinegar, it would bubble (If it is indeed calcium carbonate). 

“...whilst this planet has gone cycling on according to the fixed law of gravity, from so simple a beginning endless forms most beautiful and most wonderful have been and are being evolved.” ~ Charles Darwin

Happy hunting,

Mason

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    Tim    -  VETERAN SHALE SPLITTER

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Whodaman has it right. Most fossils are a product of what minerals were present in the sediment and that is variable even at a single location but also at different times so it could be different at different stratigraphic levels. If two fossils erode out of a slope from different layers they could even be found right beside each other and still look very different. One may be limestone and the other phosphatized.

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On 1/26/2018 at 4:27 PM, Fossildude19 said:

I had been wondering about the fossil preservation for months and it all makes sense now. I am so thankful for you all taking the time to write back to me and I am happy to be on the forum.

Thank you ynot,BobWill,Fossildude19 and WhodamanHD.

:)

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It's hard to tell by the resolution of the photo, but it could be that the one on the bottom was preserved within a concretion (maybe ironstone/siderite), while the top one was in 'soft' shale, which would leave it less reinforced.

Context is critical.

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