According to newly published research by Chapin Professor of Geology J.
Mark Erickson and St. Lawrence alumnus Scott J. Carpenter, fossilized
fish bones may help scientists to reconstruct the temperatures of 65
million years ago.
A paper co-authored by Erickson; Carpenter, of the University of Iowa,
Iowa City; and F.D. "Bud" Holland Jr., professor emeritus, department
of geology and geological engineering, University of North Dakota,
Grand Forks, ND, was published in the May 1 issue of Nature.
It 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
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
"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.
Erickson notes, "Although no students are directly involved in this
work, the study of the Fox Hills Formation and its paleoenvironmental
conditions has been a long standing research interest of mine and many
St. Lawrence people have been, and are currently, involved in it. My aim
has been to clarify issues of paleogeography, habitat, invertebrate,
botanical and vertebrate paleontology and paleoceanography of the
Western Interior Seaway close to the K-T boundary when the dinosaurs
and many other organisms became extinct. We continue to work out the
difficult stratigraphy of the central North Dakota region as well, so
that we can determine the timing of events relative to the 'Extinction
Event' more clearly.
"The paper published in Nature describes some of the paleoecological
relationships that advance our understanding of the oceanographic
and paleoclimate setting of the younger part of the formation," Erickson says.
Dan Peppe '03 and Tim Bouchard '03, who were St. Lawrence Fellows last
summer, are wrapping up research on these upper Fox Hills rocks as well."
Posted: May 1, 2003