Gilboa in Schoharie County, New York — The American Northeast (Mid-Atlantic)
The Gilboa Fossils
This exhibit is the only visible proof of the other, ancient world that lies hidden beneath the landscape.
380 million years ago, Gilboa was located on the shore of the inland Catskill Sea. This was a tropical world, situated about twenty degrees south of the equator. Tree-like plants (Eospermatopteris) grew near the shore competing with large shrubby plants and horsetails. Herbaceous lycopods thrived around ponds and along stream banks. Lungfish, ancestors of later amphibians, may have ventured onto shore from streams in search of food. Wind and rain were all that were heard, since this early world was devoid of insect sounds, birdsong, and animal cries.
Long periods of drought were followed by monsoon rains and flooding. Occasionally, severe storms buried much of the shore forest in sand, killing the plants. In time, the trees rotted. The molds of the stumps left in the sand were eventually filled with more sand, leaving us with the tree-stump fossils seen here today.
The colonization of land that occurred during the Devonian Period was one of the most profound series of events in the history of life
Left Hand Insets (top to bottom):
Samuel Lockwood (1819-1894 amateur naturalist and minister of the Reformed Church in Gilboa from 1852 to 1854, found a sandstone cast of a portion of a Devonian-age tree trunk in Schoharie Creek near Gilboa.
Lockwood's specimen was described and illustrated by McGill University paleontologist John W. Dawson in 1871. The name Caulopteris lockwoodi was given to the specimen by Dawson to honor Lockwood.
This was the first documented discovery of fossil tree stumps in North America.
In October 1869, the Schoharie Creek, swollen from torrential rain, flooded, destroying bridges, roads, businesses, and homes in the village of Gilboa. While blasting rock along the creek to use for repairs, workmen discovered some in situ (in life position) fossil tree stumps.
Daniel Mackey, a resident of Gilboa, wrote to State Paleontologist James Hall in January 1870, describing the discovery and subsequent removal of two stumps. Hall then visited the site to retrieve the stumps and secure additional material. Recognizing the uniqueness and importance of these fossils, he immediately
By the end of the 19th century, the population of New York City had increased so dramatically that existing water supplies were becoming exhausted. Tapping the Catskill watershed was perceived to be the solution to this most critical problem. The topographical features that had made the area of Gilboa so attractive to early settlers also made it desirable as a site for a reservoir The ensuing construction of the Gilboa dam and reservoir begun in 1917, revealed a bonanza of fossil tree stumps and other Devonian-age plant material.
Winifred Goldring (1888-1971) joined the staff of the New York State Museum in 1914. She was appointed State Paleontologist in 1939, the first woman to hold this kind of position. During the 1920s she undertook the problem of scientifically describing and illustrating Gilboa fossil material, "the most impressive display of the early land flora in the known world”
Goldring convinced the New York City Board of Water Supply to leave the fossils, now on this site, in Gilboa. Without her intervention these too would have been reposited elsewhere in established museums. It is for this reason that this exhibit is dedicated to her memory.
Right-Hand Insets(top to bottom):
In 1968, the New York State Power
One of the most interesting arthropods finds from Gilboa was that of a nearly complete spider spinneret. The Gilboa spinneret represents the earliest known evidence of silk production, and therefore, the earliest record of spiders. It is unclear to what use Devonian spiders put their silk. Modern spiders with this type of spinneret use silk for lining their burrows, constructing trip lines to trap prey and for making egg sacs. The Devonian spiders may have used their silk for egg sacs and burrows; they did not use it for catching prey because flying prey would not appear for several more million years.
Photo cation: Alterops fimbriunguis Spinneret of the oldest known spider. Greatly magnified (Courtesy of Dr. William A Shear)
Centipedes are small terrestrial arthropods whose fragile exoskeletons and mode of life do not normally make them likely candidates for fossilization. However, at Gilboa, more than 30 specimens have been recovered. These represent a type of small centipede that constitutes a new order of these animals, the Devonobiomorpha, based on their unique poison claws.
Photo Caption: Centipede Devenobis delta (refers to the Catskill delta) is among the oldest known centipedes Head and maxillipeds partially connected. Greatly magnified (Courtesy of Dr. Patricia M. Bonamo)
In 1987, three new genera and seven new species of the arachnid order Trigonotarbida were described. These extinct relatives of spiders have armored plates on their abdomens and lack silk-producing organs.
Photo Caption: Gilboarachne griersoni The arachnids are the most abundant animal found at Gilboa. Of the three new Trigonotarbid genera, Gilboarachne, commemorates Gilboa Greatly magnified (Courtesy of Dr. Patricia M. Bomano)
Fourteen whole or partial mite specimens were recovered in Gilboa. New genera and species include Protochthonius gilboa. Also, many specimens of a tiny, multilegged animal were found. These creatures are believed to be the precursors of the arthropleurids, a group of huge millipede-like arthropods, in excess of six feet in length, which inhabited coal swamps of the Carboniferous Period. These animals have no living descendants.
Photo Caption: Protochthonis gilboa A tiny mite. Greatly magnified. (Courtesy of Dr. Patricia Monamo)
Legend to center drawing:
1. Eospermatopteris. Trunk and stump of a tree fern.
2. Aneurophyton. Foliage and stems of a tree fern.
3. Lepidosigillaria. The "Naples Tree,” an arborescent lycopod.
4. Psilophyton. One of the earliest vascular land plants.
5. Protolepidopeudron. A herbaceous lycopod very similar to today's club mosses.
6. Ichthyostega. A Late Devonian amphibian- about 4 feet in length.
Precambrian - 543-4,600 million years ago
Origin of the earth, Single-celled life appears.
Cambrian - 489-543 million years ago<
Gilboa's ancient world, Colonization of land
Carboniferous - 280-162 million years ago
Earliest reptiles and insects Great coal-forming forests
Triassic - 190-245 million years ago
Earliest dinosaurs, Earliest mammals
Jurassic 144-190 million years ago
Dinosaurs, Earliest birds
Cretaceous 65-144 million years ago
Dinosaurs' climax, Flowering plants
Quaternary 2 million years ago Earliest humans
This exhibit is made possible by the Catskill Watershed Corporation working in partnership with the New York City Department of Environmental Protection and the Gilboa Historical Society
Thanks to Linda Van Aller Hernick, author of The Gilboa Fossils (Givetian Press), Kristen Van Houten Wyckoff, artist, Linda Trautman Stratigen Ellen Thom, and Gerald Stoner.
Erected by Catskill Watershed Corporation, Gilboa Historical Society.
Topics. This historical marker is listed in these topic lists: Horticulture & Forestry • Paleontology • Roads & Vehicles.
Location. 42° 23.869′ N, 74° 26.832′ W. Marker is in Gilboa, New York, in Schoharie County. Marker is on New York State Route 990V 0.1 miles west of Flat Creek Road (County Route 17), on the left when traveling east. Touch for map. Marker is in this post office area: Gilboa NY 12076, United States of America. Touch for directions.
Other nearby markers. At least 8 other markers are within 4 miles of this marker, measured as the crow flies. Schoharie County (here, next to this marker); Gilboa Settlement (approx. 0.4 miles away); a different marker also named Schoharie County (approx. 1.4 miles away); Cabin of John More (approx. 3˝ miles away); a different marker also named Schoharie County (approx. 3.6 miles away); Town of Conesville War Memorial (approx. 3.6 miles away); Manor House (approx. 3.7 miles away); Stone Bridge (approx. 3.7 miles away). Touch for a list and map of all markers in Gilboa.
Credits. This page was last revised on July 22, 2020. It was originally submitted on July 19, 2020, by Steve Stoessel of Niskayuna, New York. This page has been viewed 61 times since then and 5 times this year. Photos: 1, 2, 3, 4. submitted on July 19, 2020, by Steve Stoessel of Niskayuna, New York. • Bill Pfingsten was the editor who published this page.