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Newark Supergroup Question


DVL

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Quick question for the experts:

I've found a number of marine fossils in Newark Supergroup locations- corals, crinoids, brachiopods, yet I've read that the formation is non-marine.  I'm told they could be glacial deposits.  I also recall that Coelacanths have been found which I assume were marine. Was the formation marine or not?  Or both?

 

Thanks in advance!

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The Newark Supergroup was not made up of marine deposits. 

 

The prevailing theory is that it was a lacustrine environment, with some alluvial fan deposits, and possibly some estuarine deposits as well. 

So - freshwater lakes,  some river entrances/exits, and some brackish water possibly.

Regards, 

 

 

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    Tim    -  VETERAN SHALE SPLITTER

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4 hours ago, Fossildude19 said:

The Newark Supergroup was not made up of marine deposits. 

 

The prevailing theory is that it was a lacustrine environment, with some alluvial fan deposits, and possibly some estuarine deposits as well. 

So - freshwater lakes,  some river entrances/exits, and some brackish water possibly.

Regards, 

 

 

Thanks!  Assume the stuff I'm finding is glacial then (or freshwater brachiopods maybe?).

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9 minutes ago, DVL said:

Thanks!  Assume the stuff I'm finding is glacial then (or freshwater brachiopods maybe?).

 

The only freshwater bivalves/shells known in the NSG are unionid clams, (Unio sp.) and darwinulid ostracods, (Darwinula sp. ) and the conchostrachans Cyzicus sp. and Estheria ovata.

The larger clams, Unio sp. are very rare. 

Regards,

  • I found this Informative 3

    Tim    -  VETERAN SHALE SPLITTER

   MOTM.png.61350469b02f439fd4d5d77c2c69da85.png      PaleoPartner.png.30c01982e09b0cc0b7d9d6a7a21f56c6.png.a600039856933851eeea617ca3f2d15f.png     Postmaster1.jpg.900efa599049929531fa81981f028e24.jpg    VFOTM.png.f1b09c78bf88298b009b0da14ef44cf0.png  VFOTM  --- APRIL - 2015  

__________________________________________________
"In every walk with nature one receives far more than he seeks."

John Muir ~ ~ ~ ~   ><))))( *>  About Me      

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