By G. Wayne Clough, Secretary of the Smithsonian Institution
Wednesday, July 15: Weather, 62 degrees and sunny at 7 a.m.
A picture-perfect day for venturing into the field. We head first to the grocery store to obtain provisions for lunch and plenty of water, something that will be much needed in the dry climate and the heat of the day. Scott explains that we will visit three sites where teams are working to investigate the PETM and its consequences from different perspectives. He and his colleagues consider this area ideal for their work since the deep sedimentary deposits of the basin capture the stratigraphic profile of the time leading up to the PETM, the PETM itself and the years following it. The rock strata in this large basin slope inward at the sides and are relatively horizontal in the center, but regional uplift in the last few million years has once again loosed the power of erosion, carving deep gullies and valleys that expose PETM rocks and allow the researchers to find the fossils and other evidence they seek. Adding to the favorable geologic circumstances, much of the land is under the management of the U.S. Bureau of Land Management, which has been helpful to the research teams, and it is transected by a network of dirt roads maintained by an energy company that operates the many oil jacks that remove oil from the mature oil field in the region.

Scott Wing points out the red and gray strata
visible in the distant hills.
(Photo by Wayne Clough)
The drive to the research sites from Worland is about 15 miles. They are located to take maximum advantage of the exposures of the beds deposited during the time of the PETM. The relevant stratigraphy begins with the underlying gray, brown and tan deposits known as the Fort Union Formation, which formed during the Paleocene Epoch just before the time of the PETM. This was a period of relatively stable carbon dioxide levels in the atmosphere and a warm, moderate climate that allowed temperate and subtropical plants to grow as far north as Wyoming. The Paleocene was a time of rapid evolution among mammals, probably because the dinosaurs had gone extinct at its beginning. Many of these early mammals did not survive the PETM or began to decline in diversity at that time.