Monday, February 7, 2011

Unprepped Aulopora Coral Fossils


This blog posting highlights four fossil specimens of unprepared Aulopora coral found in the Silver Creek Limestone of Clark County, Indiana.  The first picture shows the most extensive colony that attached to a spirifer brachiopod.  It should make a nice display fossil once the sand abrasive cleaner has processed its surface. 

Earlier this year, I read about an Aulopora fossil on the Wooster College in Ohio blog in which the author talks about the protocorallite (the origin of the colony).  I am hoping to find origin points on some of these specimens.




Sunday, February 6, 2011

Devonian Megastrophia Brachiopod

One of the largest of the Devonian period brachiopods a person can find in the limestones of Clark County, Indiana.  This specimen appears to be from the Silver Creek layer.  One side of the specimen has broken off but the top and bottom sections of the brachiopod appear to be in place.  The fossil is a little over 5 cm wide.  A matting bryozoan was growing over part of the shell.  The engraver should be able to remove matrix on the bottom half of the fossil.

Dave at Views of the Mahantango fossil blog recently wrote about this genus found in the Silica Shale.




Saturday, February 5, 2011

Mineral in Fossil Analysis


A December 19, 2010 posting on this blog highlighted a mineral specimen that had grown out of Devonian period brachiopod fossil.  The question this fossil produced, was what mineral was it?  After researching minerals found in the county of that fossil, it appeared to be either gypsum or aragonite.  Thanks to blog reader Howard of Calgary, Canada, who provided a chemical test for helping decide which.

As part of the test I included two other specimens taken from Mississippian period road cuts about 25 miles south of Louisville, Kentucky.  I suspected both could be gypsum as well.

Small samples of three specimens were placed on a glass plate.  Diluted hydrochloric acid was then dripped on each sample until immersed.  The plate was then left for the liquid to evaporate.  The plate was then examined under 100x magnification using a microscope.

The first specimen had quite a bit of limestone in it.  The acid began fizzing right away once in contact.  It does not appear to be gypsum.  The first image is interesting it that gray beads appeared on part of the slide.



Specimen #2 ended up being the most visually appealing under the microscope.  It is gypsum seeing the crystal balls that formed around the perimeter of where the acid evaporated on the glass slide.













As for the fossil, after looking at its glass plate the mineral appears to be aragonite.  The sample fizzed when exposed to acid but no crystal ball formation after evaporation.




My blog posting has been sporadic as of late.  A bad case of the flu really disrupted my work flow which I still have not recovered from.