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ShareMay 5, 2003 — CANTON, N.Y. - Fossilized fish bones may help scientists to reconstruct the temperatures of 65 million years ago, according to a paper in this week's Nature, co-authored by colleagues representing three generations of researchers.
St. Lawrence University alumnus Scott J. Carpenter of the University of Iowa, Iowa City; Chapin Professor of Geology J. Mark Erickson, St. Lawrence University, Canton, NY; and F.D. "Bud" Holland Jr., professor emeritus, department of geology and geological engineering, University of North Dakota, Grand Forks, ND, co-authored the paper, which compared the carbon, oxygen and strontium isotope ratios of four fossils collected from the Fox Hills Formation of South Dakota. The relics were the calcium carbonate ear stones belonging to Vorhisia vulpes, a Late Cretaceous fish that spawned in brackish water before migrating to open marine waters of the Western Interior Seaway of North America. The fossils suggest that the seawater temperature in this region was an ambient 18 degrees, Centigrade. This is consistent with previous temperature estimates that have used different techniques. Sediments from the Western Interior yield exceptionally well-preserved fossils that serve as proxies for the rapid climate change that occurred 67-65 million years ago.
Carpenter, research scientist in the UI Center for Global and Regional Environmental Research and associate director of the Paul H. Nelson Stable Isotope Laboratory, says that the work provides another piece of the paleo-climate puzzle for the time period just prior to the end of the Cretaceous.
"This is the first published report of the life history of a Mesozoic age fish," Carpenter says. "This fish was thought to have lived in freshwater, but our analyses indicate that it never lived in freshwater."
The research is part of an ongoing collaboration to characterize the ecology and climate of North and South Dakota near the Cretaceous-Tertiary [K-T] Boundary.
"The preservation of fossils in the sediments from this area is unparalleled," Carpenter says. "Clam shells look like those collected on a beach today. This preservation is why these specimens can provide such detailed geochemical information."
The collaboration represents three generations of researchers. Holland was Erickson's dissertation advisor at the University of North Dakota. Erickson was Carpenter's advisor at St. Lawrence. Carpenter's undergraduate thesis and first publication, in 1988, was on the geochemistry of fossil-bearing concretions from the Fox Hills Formation of North Dakota.
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