Exploring
Red Hill, Pennsylvania, and the First North American Tetrapod Discovery
Compared to other places we have
searched, the Red Hill site yielded few fossils harder to work for. Situated in
Clinton County, Pennsylvania, adjacent to the West Branch Susquehanna River, we
hammered and chiseled, carefully extracting sedimentary sections, for
relatively little evidence of late Devonian flora and fauna while light drizzle
glazed red mudstone with September temperatures in the low 50’s. My family’s
best find was a fish scale about three fourths of an inch diameter, almost
certainly an instance of the large Hyneria predator. Other members of New York
Paleontological Society found similar scales, pieces of plant stems, and a large
section of fish vertebrae along the impressive, red-toned highway cut. But the
scarcity of fossil finds
paled in comparison to the importance of the rock we worked upon.
By invitation from Douglas Rowe, who
stewards the site in conjunction with Ted Daeschler of The Academy of Natural
Sciences, Philadelphia, Curator of Vertebrate Zoology, the group traveled to
north-central Pennsylvania in 2009 to collect, then stay in nearby Renovo and
Hyner hotels for the night and resume collecting in the morning. The mood was
somber as the weather and arrival of the fall season coupled with this fairly
isolated region of Pennsylvania, but everyone seemed to feel pleased to be treated
the opportunity with legendary Doug Rowe. This site is restricted to invitation
only, and significant finds are released to Rowe and Daeschler, but Hyneria
scales, isolated vertebra, plant matter, and possibly other minor finds were
ours to keep.
Having finished collecting together
late in the afternoon the day of our arrival, we caravanned to Rowe’s local
museum, an enormous collection of fossils including some of the first North
American tetrapod finds at Red Hill. Douglas Rowe is credited with Ted
Daeschler for the very first North American tetrapod discovery in the early
1990’s at Red Hill. By synchronicity of interest and endeavor, Ted Daeschler
happened upon Rowe pursuing his hobby at about this time along the road cut
near Hyner and Renovo, deeply absorbed in both his authentic ability and the
significance of this exposure of the Catskill Formation. Rowe has since
received the 2007 Harrell L. Strimple Award for contributions to paleontology.
One of two species of tetrapods discovered here, Densignathus rowei, is named
after him.
Tetrapods are extremely rare finds
along the one kilometer Red Hill site; usually a shoulder piece or jaw is found
rather than complete skeleton. The predominantly red mudstone is a deep deposit
from a wide lowland river bed and flood plain of the Catskill Formation, which
emptied into the inland Catskill Sea having flowed north and west from
highlands. The tropical or sub-tropical climate produced a flourishing of plant
life, and remains often found in the much less frequent green sandstone present
along the cut suggests the ancient presence of ponds on the flood plain.
Red Hill is one instance conveniently
exposed by highway construction of a larger unit of like rivers forming the
Catskill Delta produced by erosion of the Acadian Orogeny—mountains that lay to
the south and east. Alluvial deposits extend from southeast New York, through
Pennsylvania, Maryland, West Virginia, and northwest Virginia. Marine deposits
associated are to the west into Ohio, and southward into Tennessee. The late
Devonian continent of Euramerica, 365-370 million years ago, was distinctly
characterized by the inland sea, and no doubt fish forming appendages to
venture upon land is the most important value we encounter from that time.
Matt Litton chisels sedimentary stone, eventually finding large fish scale (Hyneria) fossils a full inch across, 365-370 million years old.