Geologist/Collection Manager Albert D. Kollar
4400 Forbes Avenue
Pittsburgh, PA 15213-4080
Click here for full bio
MS Geology, University of Pittsburgh
BS Geology, Southhampton University
Click here for Curriculum Vitae (MS Word document)
Click here for PDF download of: Brezinski, D. K. and A. D. Kollar. 2008. Geology of the Carnegie Museum Dinosaur Quarry site of Diplodocus carnegii, Sheep Creek Wyoming. Annals of Carnegie Museum, Vol. 77, number 2, Pp. 243-252.
Regional Geology Education Collaborations through the Application of Museum Collections, Research, and Field Work
- Shady Side Middle School Earth Science, Fifth Grade
- Frick Science Academy, Fourth Grade
- Nine Mile Run Watershed Association of Frick Park
- Venture Outdoors
- Montour Trail Council
- Carboniferous brachiopod paleontology of the Redwal Limestone of Arizona
- Late Paleozoic reef–brachiopod ecology of Montana and New Mexico
- Geology of Carnegie's Dinosaurs, Sheep Creek, Wyoming, and Dinosaur National Monument, Jensen, Utah
- Paleoclimates of Late Paleozoic tetrapods of western Pennsylvania
- Paleoclimates of Pennsylvania Age eurypterid trackway of western Pennsylvania
- Section research and collecting continues to investigate late Devonian and Carboniferous climate change and its implication to biotic evolution and extinction. During this episode of global climate change from the late Devonian through the late Pennsylvanian or 65 million years of time, global climatic cooling and warming had a profound affect on Earth's paleoenvironments, sea level, extinctions, and evolution. Preliminary evidence (invertebrate fossils) collected from the Carboniferous reefs of the Bridger Range of Montana, New Mexico, and Oklahoma, suggests an apparent biotic recovery from the marine extinctions of the Late Devonian Ice House climate.
- Research on the geology of the classic Carnegie Museum Dinosaur Quarries in Sheep Creek, Wyoming and Earl Douglass (Dinosaur National Monument), Jensen, Utah continues.
Western Pennsylvania Discoveries
- The investigation continues of the rocks of the Pittsburgh region for evidence on late Pennsylvanian climate change and how it might affect tetrapod (vertebrate) evolution during the Carboniferous.
- A reinvestigation of the holotype euryterid trackway in Elk County, Pennsylvania is underway.