Abstract
Previously described "sporelike fossils" in a black silty shale in the Devonian Montebello sandstone, N. of Harrisburg, Pennsylvania, were re-studied and found to be flattened chamosite ooelites. The environment in which the ooelites formed was marine, slightly reducing, having a small clastic influx, and with currents strong enough to agitate sand grains.
This content is PDF only. Please click on the PDF icon to access.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
