New York City had been
growing rapidly throughout the nineteenth century and with its growth
came a growing thirst for safe fresh drinking water. The City and
the State Legislature looked north to the streams and valleys of the
Catskill mountains. In 1905 the legislature enacted a proposal for
the damming of the Esopus and Schoharie Creeks to create reservoirs
and a system of aqueducts to conduct water to the City. On the
Schoharie, the gorge at Gilboa was selected for a reservoir site with
the dam running right through the village of Gilboa, requiring that
the whole town be razed. Three churches, two boarding houses, many
stores, business and homes – some 430 structures were torn down or
burned. Seven cemeteries and family burial plots were relocated. In
1917 land acquisitions began and by 1920 excavations for the dam
commenced.
GILBOA SETTLEMENT
COTTON MILL 1840-1869, TANNERY
CHURCH & CEMETERY STOOD ON NYSHM at Schoharie Dam (now obscured by dam reconstruction)
GROUND NOW COVERED BY RESERVOIR
OF NEW YORK CITY WATER SUPPLY
STATE EDUCATION
DEPT. 1949
As the steam shovels began
their work to dig footings, and as crews began blasting out rock
from creek-side quarries for the dam, workers began to discover fossil
tree stumps.
Some seventy years before,
Samuel Lockwood, a local pastor and amateur naturalist had first
discovered pieces of fossilized tree trunks, and foliage as well as
some distinctive bulbous tree stumps in a quarry along the Schoharie
Creek. They had been identified as a species of fern-trees from the
Devonian age. They had been located at the edge of a shallow inland
sea and buried in a slurry of storm-borne sand.
The New York State Museum
was called and a team was rapidly assembled to rescue any significant
fossils that emerged before they were covered by the construction of
the dam or the waters of the reservoir. Beyond the team's important
discoveries, the State Museum's project was significant for other
reasons as well. First, it was one of the earliest “salvage
paleontology projects” and secondly it was one of the first major
paleontology projects headed by a woman.
Winifred Goldring was an
extremely bright young woman, graduating from Albany's Milne School
as class valedictorian in 1905 and graduating with honors from
Wellesley College four years later. She began her college years
focusing on classical languages but two required “science”
courses (geology and “geography”) set her on a totally different
path. As a girl she had collected fossils in the Helderberg
Mountains; and her father must have sparked in her an early interest
in botany. Frederick Goldering was trained as a master gardener at
Kew gardens in Great Britain, and had come to America to manage the
exotic orchid collection of Erastus Corning
a wealthy businessman and politician in Albany. Later Goldring ran a
successful florist/greenhouse business from his home in Slingerlands,
N.Y. In 1912 Winifred earned her AM degree at Wellesley and took
additional courses in geography, paleontology and paleobotany at
Harvard, Colombia and John Hopkins University.
In 1914 she was hired by
John Mason Clarke, the New York State Museum's third director as a
“Special Temporary Expert in Paleontology” to create fossil
invertebrate exhibits for the State Museum. Hired to “fill the
cases” she worked, instead on creating interpretive exhibits that
would educate the public, beginning with exhibits entitled “What is
a Fossil?” and “What is a Formation?”
She would go on to create
full-sized dioramas that would depict a Devonian Forest and the pot
hole deposition site of the Cohoes mastodon bones. Eventually her
museum work would lead her into science publications for the general
public. The Handbook of Paleontology for Beginners and Amateurs,
first published in 1933 went through several publications and was
widely used as a college introductory text. The Guide to
the Geology of John Boyd Thatcher Park
was also published in 1933, and was republished in 1997!
In
1915 she was hired as an assistant paleontologist. Clarke had begun
an ambitious review of the literature and of the State's extensive
collections of both catalogued and as yet un-studied fossil crinoids
(sea lilies), but the project had languished as Clarke was occupied
with other museum business. In 1916 he asked Winifred to take over
the study. Early on he had been impressed by her scholarship and work
ethic, praising her as a “particularly hardy seeker after the
truth.” After seven years of comprehensive study she published a
670 page monograph that systematized the ancient crinoids into twenty
five families, sixty genera and one hundred and fifty five species,
firmly establishing her reputation as a first rank paleontologist.
When
fossils began emerging from the excavations and quarry sites at
Gilboa in 1920, Clarke and his team began collecting. But again,
the press of business at the museum prevented him from devoting
adequate attention to overseeing the project. In 1921 he turned over
the Gilboa fossil project to Winifred Goldring and her colleague
Rudolf Reudemann.
They would work the site until 1926 when rising
reservoir waters would prevent further work. In 1924 Goldring
published a synopsis
of
their work to date at Gilboa in the New York State Museum Bulletin
#251. Over forty tree stumps had been found from three successive
forests, each having been buried by storm driven sands. In the same
layers, but not attached to the stumps were found considerable
amounts of fossilized vegetative matter – (apparently) seeds, spore
cases,branches and palm-like fronds.
Based on this evidence Goldring
concluded the stumps were a new genus of “seed ferns” she named
Eospermatoperis (ie.
“dawn of the seed fern”). This designation would stand for
eight decades. The publication of this report and subsequent journal
articles would make Gilboa and Winifred Goldring world famous.
Though Goldring had the support and respect of most of her colleagues
at the State Museum, many people, including some of her co-workers
were uncomfortable with a young single woman doing geological field
work, and wished she would confine her work to the laboratory and the
museum. Though she participated regularly in professional meetings
and conferences, she was rarely invited on collecting expeditions out
of state and colleagues mentioned in letters the “limitations of
taking women into the field.” To many it simply didn't seem proper
for a woman to be seen clambering around rocky outcroppings or
picking through shattered bedrock at a quarry or examining the latest
discovery at the bottom of a hole at a construction site while
construction workers stood around watching. Certainly the fashions of
the first decades of the twentieth century were not conducive to such
activities, as the voluminous ankle length skirts of the first decade
gave way to the pencil thin dresses of the second decade. It would be
another twenty or twenty-five years before women commonly wore pants,
but Miss Goldring was not to be thwarted. She created her own outfit
with bloomers for fieldwork. When other critics and concerned
friends raised the issue of her personal safety when working alone
un-escorted in the field, around quarries and construction sites, she
answered them by learning to shoot a revolver, implying she would
work armed, if she was ever working alone and felt threatened.
Perhaps
more troubling for Winifred were issues of fair compensation and
opportunities for advancement, as a woman. In 1918 she resigned
briefly over issues of inadequate salary combined with the pressures
of completing her exhibit work and working on the crinoid project. In
1928 she considered applying for a position with the U.S. Geological
Survey but was dissuaded by colleagues who alerted her that the
survey directors were looking for a “he-man” paleobotanist. The
following year in a letter she discussed the issue of whether a woman
should go into the fields of geology and paleontology. She pointed
out that her salary of $2,300 was half that of the (male) clerks and
stenographers at the museum. Generally she encouraged girls to go
into other fields – botany and zoology instead of paleontology. Her
promotions came slowly but steadily as her dedication to her
profession and the quality of her work could not be denied. From
1920 to 1938 she worked as an Associate Paleontologist, during which
for three years she held the title of Paleo-botanist. From 1938 to
1939 she was the provisional State Paleontologist until she became
State Paleontologist in 1939, the first woman to hold such a position
in the United States, and the highest ranked woman in her profession
in the world. In 1949 she became the first women elected president of
the Paleontological Society and the following year, vice president of
the Geological Society of America.
In the 1930's Miss Goldring turned her attention to an unusual rock
formation a few miles west of Saratoga Springs. Discover in 1825, by
J. H. Steele, he described the site as having “great quantities calcareous concretions...mostly hemispherical. But many are globular
and vary in size from half an inch to two feet in diameter; they are
obviously composed of a series of successive layers nearly parallel
and perfectly concentric; these layers have a compact texture, and
are dark blue or near black in colour, and are united by layers of
lighter coloured calcareous substance....they are very thin and I have
counted more than a hundred [layers] in one series.” The advancing
glaciers had sheared off their upper portions leaving them looking
something like cabbages, halved and ready to be grated.
Lester Park Rd, south of Co. Rte 21, Saratoga
But
what were these things? Both Steele and William Mather, a geologist
reporting for the Geographic survey of 1843 he felt they were
inorganic concretions. In 1883 James Hall examined the area and
discovered within the fossils minute branching “canaliculi”. He
named them Cryptozoon
proliferium (ie.
Prolific hidden life). In 1906 H.M. Seeley confirmed they were
organisms but classified them with the sponges. In 1916 G. R. Wieland
first advanced arguments that they belonged to a group of algae.
Robert Ritchie, an amateur geologist bought the property that
contained much of the outcroppings. Uncovering much more of the
area, he opened it to the public as a park, Petrified Sea Gardens, in
1924. New York State acquired the rest, which became Lester State Park.
In
the 1930's Winifred Goldring joined the fray, and with characteristic
thoroughness studied the area, for several years. In a 70 page
report she concluded they were actually three reefs of ancient algae,
each dominated by a different species: Cryptozoon
proliferium, C. ruedemanni, or C. undulatum. She
described the environmental conditions that favored one or another
species. Goldrings conclusions would be supported by studies in
recent times by the discovery of living stromatolites found in reefs
in Australia and other places.
Miss
Goldring died in 1971. Her career spanned over 40 years and was
marked by significant professional achievements as she rose to the
top of her profession, in the face of sustained gender
discrimination. While her accomplishments are highlighted in a kiosk
type display near the Gilboa Museum which features several of Gilboa
tree fossils of the type she discovered and described, she is not
mentioned at the Lester Park site. In 1998 Governor George Pataki's
administration promoted a series of New York State Historical Markers
spotlighting the achievements of Women in New York State.3
Unfortunately she was not among those chosen. Hopefully in the future
she will be considered for a Marker, perhaps at the site of her home
in Slingerlands.
Marker of the Week -- You have to Wonder,
given the (ah) shall we say, spontaneous habits of cattle if you spend any time marching them back and forth over clay won't they tend to make their own "contributions" to the clay? Well, of course the bricks were fired....and maybe a little additional organic matter made them stronger.
At any rate, the good Doctor ended up with a handsome house.
Buckwheat Bridge Rd., North of Clermont