| OCR Text |
Show 223 represented by fossils The K-T at the boundary boundary. horizon appears to be sequence in the interval between 202 m positioned and 208 from fossil recognizable and/or other pollen) horizon of shocked concentration) are available, support paleontologic data pertinent information (for example, precise placement the North Horn Mountain section is not Partial financial prominent coal (for a quartz and/or anomalously high iridium a more 4.6. a above the base of the North m Horn Formation at North Horn Mountain. Until additional example, within of the K-T boundary in likely. Acknowledgments of this project was provided by Utah Mineral Leasing Funds and the Utah Historical Society. We thank the for their significant contributions to this project: Paul Ames, Jess R. Bushman, Dye, Deborah Fulkerson, Hans Billy J. Jerqen Hansen, following people Martha Hayden, Jerald Hinshaw, Fred Lohrengel, John Lyons, Fred E. May, Doug J. Nichols, Charles Officer, Earl T. Peterson, Raivo Puusemp, Steve Robison, Quintin Sahratian, Craig Sanders, C. D. Stephenson, Peter Toft, John E. Welsh, and Brad Wolverton. We thank Dennis Bramble, M. Forester, Janet Emily Bray, Elizabeth Brouwers, Gillette, David Gillette, the late Karl Hirsch, and Frederick M. Swain, for their valuable assistance in fossil identifications. However, assume full especially Richard responsibility for the accuracy of identifications thank John, Aleta, Seth, and Thea general support throughout the entire project. Difley we reported herein. We for field assistance and for |
