[Thread Prev] | [Thread Next] | [Thread Index] | [Date Prev] | [Date Next] | [Date Index] |
For several years I have been coordinating study of fossils from the Pipe Creek Sinkhole site, an earliest Pliocene (latest Hemphillian) buried sinkhole deposit in Grant County, Indiana. We have found thousands of plant and animal fossils from this unconsolidated deposti (cf. Farlow et al., 2001, American Midland Naturalist 145: 367-278; Martin et al., 2002, Journal of Vertebrate Palentology 22: 137-151). Recently we've been looking at the preservation of vertebrate bone from this site. There is little or no filling of pore spaces in the bone, and the inorganic portion of the bone is only slightly modified chemically from Recent bone. In some of our thin sections of the bone, however, we see abundant hemispherical (often paired) whatzits (to use a technical term) about 80 microns in diameter attached to the bone. These objects are mineralized. I've wondered if these might be mineralized remnants of microbial colonies. Is there anybody on this list who knows about such things, and would be willing to look at SEM images thereof, and offer an opinion as to their identity? James O. Farlow Professor of Geology Indiana-Purdue University Fort Wayne
Partial index: