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About The Chemistry Of St. Clair Ferns...


Rockpervert

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I've been wracking my brains trying to think what it is about the chemistry of these rocks that causes the classic white colouration of St. Clair plant matter, but come up resoundingly empty-handed.

Any suggestions...? :blink:

Thanks

Gethin

Certifiably one trilobite short of a Silurian picnic...

http://fossil-world.lefora.com/

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  • 3 weeks later...

The white colored minerals in fern fossils at St. Clair, PA are primarily pyrophyllite (Al2Si4O10(OH)2) with minor kaolinite (Al2Si2O5(OH)4). The pyrophyllite probably formed under low temperature metamorphic conditions (about 275 degrees Celsius, or 525F). The coal at St. Clair is anthracite, which forms at temperatures greater than ca. 250oC. The ferns died during the Pennsylvanian age (about 310 million years ago) and were buried under up to 8 km of sediments and rock. During burial, the area was heated to 250 to 300 degrees C, allowing pyrophyllite to form. Few coals were buried as deeply or exposed to as high temperatures as those in eastern Pennsylvania, so the presence of pyrophyllite is unusual. Pyrophyllite does occur occasionally in other coal beds around the world but not in such striking fossil remains.

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Great information, grand8228; thank you! (And welcome to the Forum)

"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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