Image: Geology: "Quantifying controls on the occurrence of nonmarine fossils" Authors: Anik K. Regan Department of Geology, University of Georgia, Athens, Georgia 30602-2501, USA Department of Earth, Environment, and Society, University of St. Thomas, Saint Paul, Minnesota 55105-1096, USA Raymond R. Rogers Geology Department, Macalester College, Saint Paul, Minnesota 55105-1899, USA Steven M. Holland Department of Geology, University of Georgia, Athens, Georgia 30602-2501, USA Abstract: Although numerous studies have described differential preservation of nonmarine fossils in channel and floodplain facies, quantitative comparisons are lacking. We present measurements of the probability of occurrence of plant, mollusk, and vertebrate fossils in the Campanian Judith River Formation of north-central Montana, USA. The data reveal little difference in the probability of occurrence among higher taxa in channel and floodplain facies, except for plants, which have a higher probability in floodplain deposits. This surprising result supports more recent models in which many organisms are buried initially in floodplain deposits, but those deposits are subsequently exhumed by migrating rivers, and finally buried in those channels. Comparisons across systems tracts revealed intriguing patterns in which plants have a higher probability of occurrence in high-accommodation systems tracts in channel and floodplain deposits, and vertebrates have a higher probability of occurrence in channels of the low-accommodation systems tract. These results confirm that sequence-stratigraphic architecture should be considered in interpretations of the nonmarine fossil record. This probability of occurrence method has promise for many other comparisons of fossilization potential. Special Note: This article made the cover photo of Geology (Volume 50, Number 11, Cover Photo by Anik Regan) www.gsapubs.org | Volume 50 | Number 11 | GEOLOGY | Geological Society of America Type of News/Audience: Department News Alumni News Geology Volume 50, Number 11 Campanian (late Cretaceous) sediments of the Judith River Formation are beautifully exposed along the banks of the Missouri River in the Upper Missouri River Breaks National Monument of north-central Montana, USA. These cliffs reveal alternating layers of floodplain and channel deposits that host a plethora of plant, mollusk, and vertebrate fossils. Studying these deposits furthers our understanding of nonmarine sequence stratigraphy and enables us to better interpret the fossil record using a robust sequence stratigraphic framework. See ‘Quantifying controls on the occurrence of nonmarine fossils’ by Regan et al., p. 1287–1290. Photo by: Anik Regan Read More: Read the Full artical at Geology volume 50, Number 11