The Forest Habitat of the University of Kansas Natural History ReservationFitch, Henry S. (Henry Sheldon)
History
The Forest Habitat of the University of Kansas Natural History Reservation
Fitch, Henry S. (Henry Sheldon)
Forest reserves -- Kansas; University of Kansas. Natural History Reservation
Produced by Chris Curnow, Tom Cosmas, Joseph Cooper and
the Online Distributed Proofreading Team at
https://www.pgdp.net
University of Kansas Publications
Museum of Natural History
Volume 10, No. 3, pp. 77-127, 2 pls., 7 figs. in text, 4 tables
December 31, 1956
The Forest Habitat of the University of
Kansas Natural History Reservation
BY
HENRY S. FITCH AND RONALD L. MCGREGOR
UNIVERSITY OF KANSAS
LAWRENCE
1956
UNIVERSITY OF KANSAS PUBLICATIONS, MUSEUM OF NATURAL HISTORY
Editors: E. Raymond Hall, Chairman, A. Byron Leonard,
Robert W. Wilson
Volume 10, No. 3, pp. 77-127, 2 pls., 7 figs. in text, 4 tables
Published December 31, 1956
UNIVERSITY OF KANSAS
Lawrence, Kansas
PRINTED BY
FERD VOILAND, JR., STATE PRINTER
TOPEKA, KANSAS
1956
26-3855
The Forest Habitat of the University of
Kansas Natural History Reservation
By
HENRY S. FITCH and RONALD L. MCGREGOR
Introduction
In northeastern Kansas, before it was disturbed by the arrival of
white settlers in the eighteen fifties, tall grass prairies and
deciduous forests were both represented. These two contrasting types
of vegetation overlapped widely in an interdigitating pattern which
was determined by distribution of moisture, soil types, slope exposure
and various biotic factors.
The early explorers who saw this region, and the settlers who came
later, left only incomplete descriptions, which were usually vague as
to the locality and the species of plants represented. As a result,
there is but little concrete information as to the precise boundaries
between the forests and grasslands, and opinions differ among
ecologists. No representative sample of either type remains.
It may be assumed that the plant communities existing one hundred
years ago and earlier were far more stable than those of the present
that have resulted from man's disruptive activities. This stability
was only relative, however. Within the last few thousand years since
the final withdrawal of the Wisconsinan ice sheet, fairly rapid and
continual change must have occurred, as a result of changing climate,
the sudden extinction of various large, dominant mammals, and finally
the impact of successive aboriginal cultures.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account