^r6U
HARVARD UNIVERSITY
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Library of the
Museum of
Comparative Zoology
3-t\/A - Prov o
Brigham Young University
Scienc Bulletin
THE PEREGRINE FALCON IN UTAH,
EMPHASIZING ECOLOGY AND
COMPETITION WITH THE
PRAIRIE FALCON
MUS. COMP. ZOOl-
L/BRARY
SEP 24 1973
HARVARD
byUNJVERSlTY
Richard D. Porter and Clayton M. White
in collaboration with
Robert J. Erwin
BIOLOGICAL SERIES— VOLUME XVIII, NUMBER 1
JUNE 1973/ISSN 0068-1024
BRIGHAM YOUNG UNIVERSITY SCIENCE BULLETIN
BIOLOGICAL SERIES
Editor: Stanley L. Welsh, Department of Botany,
Brigham Young University, Provo, Utah
Acting Editor: Vernon J. Tipton, Zoology
Members of the Editorial Board:
Ferron L. Andersen, Zoology
Joseph R. Murdock, Botany
WiLMER W. Tanner, Zoology
Ex officio Members:
A. Lester Allen, Dean, College of Biological and Agricultural
Sciences
Ernest L. Olson, Director, Brigham Young University Press
The Brigham Young University Science Bulletin, Biological Series, publishes
acceptable papers, particularly large manuscripts, on all phases of biology.
Separate numbers and back volumes can be purchased from University Press
Marketing, Brigham Young University, Provo, Utah 84602. All remittances should
be made payable to Brigham Young University.
Orders and materials for library exchange should be directed to the Division
of Gifts and Exchange, Brigham Young University Library, Provo, Utah 84602.
Brigham Young University
Science Bulletin
THE PEREGRINE FALCON IN UTAH,
EMPHASIZING ECOLOGY AND
COMPETITION WITH THE
PRAIRIE FALCON
by
Richard D. Porter and Clayton M. White
in collaboration with
Robert J. Erwin
BIOLOGICAL SERIES— VOLUME XVIII, NUMBER 1
JUNE 1973/ISSN 0068-1024
Frontispiece. Male (tierce!) Peregrine Falcon on rock in front of eyrie (Table 1, site 7); it is clutching a young
American Avocet ( Recurvirostra amcricuna), that was fed to tlie young falcons, c. New York Times Co., 1971.
Photo by R. D. Porter, 1952.
TABLE OF CONTENTS
ABSTRACT 1
INTRODUCTION 1
GEOGRAPHIC DISTRIBUTION IN UTAH 2
Historic Records 2
Specimen Records 2
Nesting Records 2
Postnesting Season and Winter Records 9
DENSITY DISTRIBUTION OF PEREGRINE EYRIES IN UTAH 12
TOPOGRAPHY. CLIMATE, AND PLANT COVER IN UTAH 13
ECOLOGICAL DISTRIBUTION OF UTAH PEREGRINES 14
Climate 14
Altitude '. 15
Habitat Niche 15
Nesting Sites 19
Cliff Orientation 19
Rock T)pe, Cliff Size, and Eyrie Height 19
Hunting Sites 21
Food Niche 28
NESTING BEHAVIOR IN UTAH 32
History of Nesting at a Wasatch Mountain Eyrie 32
Egg Laying 38
Incubation 41
PEREGRINE DECLINE IN UTAH 41
Climatic Change Hypothesis for Peregrine Decline 42
Pesticide Hypothesis for Peregrine Decline 44
Pesticide Syndrome in Utah Peregrines 44
Residues of Pesticides in Peregrine Prey Species 46
Mosquitocide Usage in Utah 46
Disease Hypothesis for Peregrine Decline 47
Human Activity Factors in the Decline of the Peregrine 47
FACTORS INFLUENCING PEREGRINE DISTRIBUTION AND ABUNDANCE IN UTAH 48
Water, Food, and Nesting Sites as Limiting Factors 49
Interspecific Competition during Nesting Season 50
Some Factors Modifying Competition and Success 51
Competition with the Prairie Falcon for Food 52
Competition with the Prairie Falcon for Eyrie Sites 55
Directional Exposure Preferences 55
Height Preference for Cliffs and Eyrie Sites 56
Eyrie Type Preferences 56
Size Preference for Nesting Area 58
Aggressive Interactions between Peregrines and Prairie Falcons 59
Date of Egg Laying as a Competitive Factor 61
Reproductive Potential as a Competitive Factor 62
PLEISTOCENE AND PREHISTORIC PEREGRINE AND PRAIRIE FALCON DISTRIBUTIONAL
RELATIONSHIPS 62
Pleistocene Distributional Records 62
Post- Pleistocene Distributional Records 63
Lake Bonneville and Peregrine Distribution in Utah 63
SUMMARY AND CONCLUSIONS 65
Addendum 70
ACKNOWLEDGMENTS 70
APPENDIX —ADDITIONAL HISTORY OF DDT USAGE AS A MOSQUITOCIDE IN UTAH 70
LITERATURE CITED 71
THE PEREGRINE FALCON IN UTAH, EMPHASIZING
ECOLOGY AND COMPETITION WITH THE PRAIRIE FALCON
by
Richard D. Porter^ and Clayton M. White^
in collaboration with Robert J. Erwin^
ABSTRACT
This study was undertaken to record the
known history of the Peregrine Falcon ( Faico
peregrinus) in Utah as we have been able to
construct it from both the hterature and from
our original research that extends over about a
30-year period in the state. The present total
population of the peregrine in Utah is possibly
only 10 percent of what it has been in historic
times. In an effort to find explanations for the
decline, we have explored hypotheses of ch-
matic changes, impact of pesticides, disease,
and human disturbances. We conclude that
pesticide contamination and climatic changes
mav have been the major reasons for their de-
cline in Utah.
A general background of the geographical
and ecological distribution of the species in
Utah is provided as are also details of its nest-
ing behavior from some Wasatch Mountain
eyries. Our data suggest that its nesting density
along the Wasatch Mountains was about the
same order of magnitude as nesting densities
in other regions of North America that are gen-
erally considered more favorable to the pere-
grine.
We have considered some of the environ-
mental factors that may limit the species in Utah
and especially its relationship with a congener,
the Prairie Falcon {Falco mexicanus). We con-
clude that the peregrine may live jointly with
the Prairie Falcon with a minimum of intra-
specific competition. We present evidence which
suggests that the peregrine has been in Utah
since the late Pleistocene and that it has had a
long history of sympatric existence with the
Prairie Falcon.
INTRODUCTION
Breeding populations of the Peregrine Falcon
(Falco peregrinus) have declined sharply over
much of its historic range in North America and
Europe during the last two decades. Although
this decline has been well documented for many
areas (Hickey, 1969), little has been published
on the status, past or present, of the species in
the Great Basin, especially as a breeding bird in
Utah, an area encompassing 84,916 sq miles
(219,932 km-).
We wish, therefore, to place on record our
obscr\'ations of the peregrine in Utah from data
collected over the past .30 years. In presenting
these data, it is our purpose to : ( 1 ) describe
the ecological distribution of the species in the
state, (2) delineate the ecological factors which
may have Hmited its distribution and breeding
success there, (3) describe its food and habitat
niches, (4) discuss its competition with related
species, especially the Prairie Falcon (Falco
mexicanus), and (5) compare its present levels
of population with those formerly known,
since peregrines in Utah have not been immune
to the decline that afflicted its populations else-
where. Because the known active eyries of this
species in the state are now only about 10 per-
cent of those known to have been present earlier
in the century, another of our objectives is to
(6) discuss and evaluate the factors which may
have led to the near extirpation of this species
in the state.
^Present address: Bureau i>f Sport KiOieries and Wildlife. Inteniiountain Forest and Range Experiment Station, Federal Building, Rm B2,
West First North, Provo, Utah 84t)()l
^Department of 7,ooIogv. Brigham Young University. Provo, Utah 84(i02
'892 East 3250 North, Ogden, Utah H+404-
Bricham Young Univehsity Science Bulletin
GEOGRAPHIC DISTRIBUTION
Historic Records
The percgriiu' was not mentioned in the or-
nithological literature for Utah until 1871, when
it was reported by Allen (1872) to prey on
waterfowl about the marshes of the Great Salt
Lake near Ogden. He found it to be common
there in September. The next to mention the
presence of the species was Henshaw (1874),
who with Yarrow, collected 600 specimens of
birds representing 165 species on a trip from Salt
Lake City to St. George between July and De-
cember 1872. The peregrine was considered by
Henshaw to be a rather common resident in
Utah and to nest in the state. Henshaw's later
account (1875) mentions only an observation
of this species by Allen (1872) in the vicinity
of Ogden, thus opening to question the source
of his data supporting the status of the species
in Utah.
The lack of observations by Allen (1872)
of the Prairie Falcon in the Great Salt Lake Val-
ley and the complete absence of this species in
his account of the birds encountered in Kan-
sas, Colorado, Wyoming, and Utah is difficult
to understand, since the peregrine apparently
was noted at all but two of Allen's collecting
localities and a specimen (young bird) was ob-
tained by him (ibid.) at Fairplay (South Park),
Colorado Territory. Did Allen ( ibid. ) overlook
the Prairie Falcon or did he consider all large
falcons to be peregrines? Nevertheless, his ob-
servations of the peregrine along the Great Salt
Lake marshes probably were accurate, as the
species has been seen there many times since
then. Although Ridgway ( 1S74, 1877) found
the Prairie Falcon to be common in the rocky
canyons of the Wasatch Mountains and a rare
breeder along cliffs of canyons and valleys in
Salt Lake Cit)' and neighborhood in 1869, he
apparently made no observations of the pere-
grine in Utah. Several earlier naturalists and
explorers (Fremont, 1845; Stansbury, 1852;
Baird, 1852; and Remy and Brenchley, 1861)
also failed to mention the presence of the pere-
grine in Utah.
Specimen Records
Specimens from both the arctic tundra pop-
ulation (F. ;;. timdriu.s) and the more southern
population ( F. p. amitttm) have been taken
in Utah during the winter months. A specimen
of the tumhius race, identified b)' C. M. White
(CMW), was found shot and wounded by R.
Vem Bullough on 15 December 1956, near
Famiington Ba\-, Davis County. (For a dis-
cussion of peregrine systematics, see White,
1968b.)
A male specimen of unknown racial affinity
was collected by Wolfe ( 1928 ) near St. George,
Washington County, on 5 February 1926. John
Hutchings (Bee and Hutchings, 1942) collected
a specimen of anattan (sensii lata; western sub-
group) (CMW) near Pelican Point, Lake Moun-
tains, Utah County (date not given, Woodbury,
Cottam and Sugden, unpubl. ms, indicate speci-
men was taken alive, 2 August 1935). Five
specimens (Twomey, 1942)— a male, molting into
adult plumage; an adult female, collection date
not given; and three males, collected on 23
April and 5 and 23 August in 1935 at the Ash-
ley Creek marshes, Uintah County— were as-
signed to the race anatinn {scnsu lato; western
subgroup) (CMW).
Woodbury et al. (unpubl. ms) record the
following additional specimens by countv: Box
Elder, at Bear River marshes, specimens taken
1 Julv and 6 September 1914; 14 September
1915; '2<S July and 28 September 1916 (U.S.
Biol. Surv.); 18 August and 7 September 1927
(Phil. Acad. Sci.); all aimtum (sensu lato;
western subgroup) (CMW). Davis, Jordan Fur
Farm, W of Bountiful, 5 January 1939 (Univ.
Utah Coll.; UU) anatum (sensu /afo).SaIt Lake,
near Salt Lake Cit>-, 4 September 1947 (UU).
Iron, near Cedar City, 12 May 1936 (Chicago
Field Mus.; LBB), anatum (sensu lato; western
subgroup) (CMW). Uintah, Ashley Creek
marshes, a young male in 1937 (Carnegie Mus.).
Washington, Zion Canvon (Zion National Park),
16 July 1939 (Zion Park Museum) anatum
(sensu lato; u-estern subgroup) (CMW).
Additional specimens of F. p. anatum (sensu
lato; western subgroup) have been examined
by C. M. White for Emerv Count)', two speci-
mens, July; and Salt Lake Countv, two speci-
mens, Januar)' and November.
Nesting Records
Historically, the peregrine is known to have
nested in 13 counties of Utah and is suspected
of nesting in at least three others. Figure 1 shows
the pattern of known and suspected breeding
distribution in Utah, and Table 1 gives their
known histories in the state.
The first recorded eyrie for the state was an
observation by Johnson (1899), who in May
1898, found three \oung peregrines in a shallow
cave under an overhanging rock of an 80-foot
(24 m) cliff [Land Rock] in Lake Mountains,
west of Utah Lake, Utah Count)', and five eggs
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
m
UTAH
Fig. 1. Pattern of known and suspected breeding distribution of the Peregrine Falcon in Utah. Letters for the
regions and numbers correspond to those on Table 1. The hne running nearly vertically through the center
of the state separates the Great Basin from the Colorado River Basin. The west face of the Wasatch Moun-
tains bisects area A and is encompassed within the northern and southern boundary of the area. Lightly
stippled area between regions A and B delimits the Great Salt Lake Desert, although there are also other
areas of salt flats at the southwest edge of the Great Salt Lake that are not classified within the confines
of the desert.
Bricham Young University Science Bulletin
Table 1. Peregrine eyries in Utah. Eyrie site numbers and letters for regional areas correspond with those
given in Figure 1.
Site
No.
First Located and Subsequent History
Last Known to be Active
Date
Observer
Date
Observer
1
2'
3
4
9
10
11
12
13
1898
1940
1939-42
1935
ca. 1926-27
1939-42
1954
1956
1940s
1939-42
1939-42
1943
ca. 1900-20?
1939-42
1943
1939
1939-42
1950
1955
1939-42
1939-42
1940s
1951
14
ca. 1900-20
1926-27
1939-42
1940s
15
1930
16
1943
1940s
17
1930s
1940s
1950s
1967
18
1930s
1939-46?
19
1930-32
20
1946-?
A — Great Basin Region — Surrounding Utah and Great
Salt lakes, and North Central Utah
H. C. Johnson (1899)
R. G. Bee (field notes)
Nelson (1969)°
Bee and Hutchings (1942)
L. R. Wolfe (in letter)
Nelson (1969)°
Porter et al. (unpubl. ms)
C. M. White
Morlan Nelson (pers. comm., 1971)
Boyd Shaeffer ( pers. coinin. )
Nelson (1969)°
Nelson (1969)°
R, D. & R. L. Porter
R. J. Erwin, J. F. Poorman
(unpubl. data)
Trcganza ( in Woodbury et al.,
unpubl. ms)
Nelson (1969)°
R. D. Porter & R. ]. Erwin
(unpubl. data)
Morlan Nelson (pers. comm., 1971)
Nelson (1969)°
C. Wilson (pers. comm.)
Lorin Carsey (pers. comm.), one
young female taken for falconry
Nelson (1969)°
Nelson (1969)°
Boyd Shaeffer (pers. comm.)
reported eyrie to have been
found and photographed in
tlie 1930's by a different party
R. D. Porter and Jack Hagan
(unpubl. data), birds seen,
eyrie not located
Treganza ( in Woodbury et al.,
unpubl. ms)
L. R. Wolfe ( in field notes
of R. G. Bee), seen carrying
food toward cliffs, and
Wolfe (1928)
Morlan Nelson (pers. comm., 1971)
Boyd Shaeffer (pers. comm.),
took young from eyrie
Dr. Harold Austin (pers. comm.)
R. D. & R. L. Porter, and R.
J. Erwin (unpubl. data)
Boyd Shaeffer (pers. comm.)
Clyde Ward ( pers. comm. )
Boyd Shaeffer (pers. comm.)
C. 'M. White (unpubl. data)
Del Diamond (pers. comm.)
Clyde Ward (pers. comm.)
Morlan Nelson ( pers. comm. )
Clyde Ward (pers. comm.)
Boyd Shaeffer (pers. comm.)
Marcus Nelson?
Early H. G. Johnson (field notes
1900s of R. G. Bee)
1940 R. G. Bee (field notes)
Nelson (1969)
1957-58 C. M. White (unpubl.
data)
1953 R. J. Erwin (unpubl.
data)
1969 C. M. White (unpubl.
data), single bird
1956 C. M. White (unpubl.
data )
1952 R. J. Erwin (unpubl.
data)
1968? Clyde Ward
19.54 Clyde Ward
1969 H.' Austin and L. Wakefield
one adult seen.
1930-32 Clyde Ward (pers. comm.)
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
Table 1 ( Continued )
21 (SNV)= ca. 1926-27
22 (SNV)
1939-4S
23'
1942
24
1942
25 ca.
1939
26
1969
27 (SNV)
1960
28
1961
29 (SNV)
1916 &
1936
30 (SNV)
1958
1959
31 (SNV)
1953
32
1958
33 (SNV)
1958-59
34
1937
35 (SNV)
1935-?
1965-66
36 (SNV)
1961
37
1936
38
1939
39 (SNV) 1963
40 (SNV) ca. 1926
L. R. Wolfe ( ill field notes of
R. G. Bee)
Morlan Nelson ( pers. comm., 1971)
1970 C. M. White (unpubl.
data)
B — Great Basin Region — Great Salt Lake Desert
1959-60 C. M. White and Gary D.
Lloyd (unpubl. data)
H. Webster (letter, 1961)
H. Webster (letter, 1961)
C — Central Utah, eastern edge Great Basin, western
Colorado River Basin (Plateau)
Gunther and Nelson ( in Woodbury
et al., unpubl. ms.)
C. M. White (unpubl. data) 1969
G. G. Musser, A. D. Stock, and
C. M. White (unpubl. data)
White and Lloyd (1962) 1964
D — Colorado Plateau and Navajo Country
Woodbury and Russell (1945) 1961
edge
R. J. Erwin (unpubl. data) 1962
R. D. Porter (unpubl. data)
Behle (1960)
G. L. Richards (pers. comm.),
saw fledged young
C. M. White (pers. comm. from
M. Hopkins, unpubl. data)
E — Uinta Basin and Upper Colorado River Basin
Twomey (1942) 1961
Twomey (1942)
E. Peck, W. Pingree, and J.
Gaskill (pers. comm.)
F — Southwestern Utah, edge Great Basin; and Virgin River Valley
C. M. White (unpubl.
data)
C. M. White and G. D.
Lloyd (unpubl. data)
C. M. White and G. D.
Lloyd (unpubl. data),
pair seen in area
G. D. Lloyd (unpubl. data),
adult in general area
G. L. Richards (pers. comm.),
at nearby locahty
C. M. White and G. Worthen
(unpubl. data)
W. S. Long ( breeding female
collected )
Grater (1947)
Wauer and Carter (1965)
Wolfe (1928)
1961 G. M. White (unpubl.
data)
1962 C. M. White and G. D.
Lloyd (unpubl. data),
an adult in area
1964 Wauer and Garter (1965)
1966 C. M. White (unpubl.
data), lone adult seen
JMay be an alternate site for number 1: located only 2 or 3 miles (3.2 or 4.8 km) from site number 1, but nearly 40 years later.
-SNV, (suspected, but not verified) adults were observed at these localities, but eyrie sites not actually located; although adult birds
have been >cen one nr nir>re time^, m the authors' opinions, the sites need further verification. The validity of these sites is probable.
■The eyrie proper is about 0-5 mile (0.8 km) into Nevada.
"These sites are the ones referred to by Nelson (1969); their locations were commimicated to us in a letter from Nelson dated 25
April 1969.
on the same ledge on 30 March 1899 (Figs. 1-5;
Table 1, site 1). While circling Utah Lake, John-
son (ibid) noted Long-billed Curlew (Ntimenius
americamts) , snipes (Capella gallinago), bitterns
(Botaurus lentigino.nis), and a goodly number
of ducks of various species which probably
served as a food supply for the peregrines.
Bee and Hutchings (1942) report finding a
nest containing four fresh eggs on a ledge over-
looking Utah Lake, (5 miles south of the Land
Rock site) near Pelican Point in the Lake Moun-
tains, 20 May 1935 (Fig. 1, Table 1, site 3).
Thev collected the adults to verify identification.
Local residents report that peregrines had been
observed nesting there for many years ( ibid. ) . A
visit to the sites on 22 April 1950 by R. D. Por-
ter and R. J. Erwin revealed no indications of
recent occupancy. In recent years lime mining
Bhicham Young Univehsity Science Bulletin
Fig. 2. Land Rock, west side of Utah Lake; location
of first known peregrine eyrie site in Utah. It is
a marginal site, which in some recent years has
been occupied by Prairie Falcons. Note scrubby
nature of vegetation in foreground. Photo by Kim
Despain, 197L
operations have destroyed the Pehcan Point site
(Fig. 6) and Prairie Falcons have occasionally
occupied the Land Rock site.
Nelson ( 1969 ) located 9 or 10 eyries ( in
letter, 25 April 1969, Nelson gave 9 eyrie loca-
tions) in the area surrounding the Utah and
Great Salt lakes during the period 1939-1942.
This area included parts of Box Elder, Weber,
Davis, Salt Lake, Utah, and Tooele counties.
Treganza (in letter, 5 January 1930; Woodbury
et al., unpubl. ms) found the species breeding
on the cliffs fronting the lake from Brigham to
Ogden [at least four eyries overlooked the Bear
River Marshes in the 18 miles from Ogden to
Brigham City (Woodbury, pers. comm., in White,
1969b)]. Although he located nests, he was
unable to negotiate the cliffs; one was over 1,000
feet (305 m) high (Fig. 7). Females were col-
lected off the nests, but precise nesting data
were not obtained.
Gunther and Nelson (Woodbury et al., un-
publ. ms) noted the species nesting at a site
in the Great Basin Desert of west central Utah
during the nesting season (vear not given). Gun-
ther (Woodbury et al., unpubl. ms) saw the
species at a large reservoir in Wasatch County
in the summer of 1938.
Fig. 3. Utah Lake and adjacent habitat as presently seen from atop the Land Rock eyrie site; marshes former-
ly were more extensive than today and came closer to the eyrie. Photo by Kim Despain, 197L
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
Fig. 4. A view of Land Rock eyrie showing nature of terrain and vegetation. Photo by Kim Despain, 1971.
Grater ( 1947 ) recorded peregrines at Angel's
Landing in Zion Canyon, Washington County,
from March to August 1939, where adults fre-
quently were seen carrying food to a high ledge
on the face of the peak. On 16 July 1939 (the
more precise dates from Woodbury et al., un-
publ. ms ) a young female, only a few weeks old,
was accidentally killed in the canyon (Figs. 1
Fig. 5. A different view of the Land Rock eyrie show-
ing terrain. Flat area formerly contained some
marsh habitat. Photo by Kim Despain, 1971.
and 8, Table 1, site 38). Wauer and Carter
( 1965 ) reported this site to be active as late as
19&4.
In the Uinta Basin, Twome)' ( 1942) re-
ported an inaccessible eyrie about 40 feet
(12.2 m) up on a deep shelf of a cliff, east of
the Green River, near Venial ( Fig. 1; Table 1,
site 34), Uintah Count)'. Actions of the adults
indicated that young were in the nest and im-
mature birds were seen at the Ashley Creek
marshes in early August and in the vicinity of
Jensen from August through September. G. L.
Richards ( pers. comm. ) saw a pair in the marsh-
es in 1961, the most recent evidence of activity
at this eyrie.
In southern Utah, single falcons were seen at
Kanab, Kane County, on 28 April 1935, and 6
April 1947, and two were recorded along Kanab
Creek on 20 May 1947 (Behle, Bushman, and
Greenhalgh, 1958). Behle (1960) also noted the
species near the Colorado River at Dewey on
21 May 1953 (Fig. 1; Table 1, site 31), and in
Glen Can\'on on 6 August 1958. Peregrines were
seen several times in July and August at Navajo
Mountain, San Juan County, by Woodbury and
Russell ( 1945) in 1936, and by C. M. White and
G. D. Lloyd (unpubl. data) in 1960 and 1961
(Fig. 1; table 1, site 29). White and Lloyd
(1962) reported on the predation of young
peregrines which had not yet fledged from an
eyrie in the Colorado River Basin (Figs. 1, 9,
and 10; Table 1, site 28).
Bricham Young University Science Bulletin
Fig. 6. Pelican Point eyrie site (Table 1, site 3, Fig. 1) showing lime mining operation, which in recent years
destroyed the nesting cliff. Photo by Kim Despain, 1971.
^-\/'-
JS^w"-*^^
Fig. 7. Treganza noted a pair of peregrines nesting on the distant 1,000 ft. (305 m) cliff in the early 1900s,
but he was unable to reach the eyrie site (Woodbur)' ct al. unpubl. ms). Photo by R. J. Erwin, 1971.
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
■mm.- '■ ■ I ' -^ '"''J\A
A:
■4-J^
it^
.a#tr-
:^
Fig. 8. Angel's Landing, Zion Canyon. Cliff in center where Grater (1947) saw peregrines nesting high on face
of peak (Fig. 1, Table 1, site 38). Photo by Grant, 1 September 1929, Courtesy U. S. National Park Service.
Postnesting Season and Winter Records
The species is present in the state through-
out the year (Woodbury, Cottam, and Sugden,
1949). Postbrceding adults, immatures, migrants,
and wintering falcons congregate near marshes
where a plentiful supply of food is available,
especially near the marshes of the Great Salt
Lake (Woodbury, Cottam, and Sugden, unpubl.
ins). At the Bear River marshes, for example,
records extend back to 1915, when Alexander
Wetmore found the peregrine to be a regular
and frequent visitor after mid-July (ibid.). The
Christmas bird censuses taken loy Vanez T. Wil-
son et al. (in Bird Lore 42, 1940; Audubon
Magazine 43-48, 1941-1946; and Audubon Field
Notes 1-24, 1947-1970) at the Bear River Migra-
tor\ Waterfowl Refuge, indicate that the spe-
cies wintered there in small numbers until the
early 1960s (Fig. 11). The greatest number of
peregrines seen during the seven- to eight-hour
censuses was seven, in 1940. The Christmas bird
counts at the Bear River marshes were exception-
ally consistent from one vear to the next begin-
ning in 19.39 through 1960 as regards the number
of participants. th(> area covered, and the party
hours afield. .Vdditionallv, V. T. Wilson directed
and participated each year until 1960, after
which other observers were involved and a
greater area was covered, although the number
of party hours afield remained essentially the
same.
Tlie racial affinity of specimens taken at
the Bear River marshes between 1 July and 28
September (anatum, sensu lato; western sub-
group), suggest that most of the postbreeding
and fall peregrines in these marshes were from
local eyries. The steady decline in the numbers
of peregrines recorded at the Bear River marshes
during thi' Christmas bird counts (ibid.) from
1939 to the early 1960s (Fig. 11) closely cor-
responded with the decline in the number of ac-
tive eyries in the area surrounding the marshes.
This correspondence suggests that most pere-
grines wintering in the marshes of Great Salt
Lake probably were from local breeding popu-
lations, although they also mav have been from
some other sharply declining population of the
anatum race. It is probable that only a small
percentage of these wintering birds were from
the arctic populations (F. p. twidrius), because
arctic birds normally winter farther south, and
because the arctic populations were not known
10
Bricham Young University Science Bulletin
to have declined between 1939 and the late
1960s.
Peregrines also have been reported on Christ-
mas bird counts both at Ogden and Salt Lake
Cit)' over the past 30 years. In addition, they
have been recorded at Parowan, Iron County,
on 27 December 1963 (Audubon Field Notes
18; 1964) and at St. George, Washington County,
on 1 January 1969 (Audubon Field Notes 23;
1969). Cliristmas bird count data for the areas
other than the Bear River marshes are either
too spotty or are too heterogeneous in their
method of collection to be evaluated statistically.
The peregrine was recorded at Clear Lake
State Waterfowl Management Area by R. Wil-
liams on 16 September 1939, and by Gunther
Mi:^^'^5«^-»i
Fig. 9. Peregrine cliff in desert of Colorado Plateau,
reported by White and Lloyd (1962) (Fig. I,
Table 1, site 28). Distance from the rock at point
A to the eyrie ledge at point B is 70 ft (21.3 m).
Poplar trees (Popidus fremotitii), along a water
course in foreground (C) are 40-50 ft (12.2-
15.2 m) in height. Photo by J. B. Piatt, May 1971.
and Nelson on 24 October, 10 November, and
4 December 1941 (Woodbury et al., unpubl.
ms), indicating that the species winters at
other marshes as well as at those near the Great
Salt Lake. Members of arctic populations (F. p.
tundrius) apparently utilize Utah's marshes both
as stopping places during migration and, spar-
ingly, as wintering grounds. This is suggested
by Lincoln's ( 1933 ) report of a peregrine banded
as a juvenile at King's Point, Yukon Territory,
within the geographic range of tundrius on 30
July 1924; by its recovery at Duchesne, Du-
chesne Countv', Utah, on 20 February 1925;
and by the collection in December of the pre-
viously mentioned specimen of tundrius from
Famiington Bay.
Late summer sightings, which could repre-
sent either resident birds or early migrants, have
been recorded from several other areas. Twomey
(1942) reported peregrines at Hill Creek, 40
miles (64.4 km) south of Ouray, Uintah Coun-
ty, on 5 August [1935?], at Strawberr)' Reser-
voir, Wasatch County, on 17 August [1935?], and
Bchle ( 1960) recorded the species at Glen Can-
von near Wahweep Creek, Mile 17, on 6
August 1958 and at 10,500 feet (3,200 m) on
the north slope of Mt. Ellen, Henry Mountains,
on 8 September 1957. Finally, a subadult was
seen near Park City, Wasatch County, in late
August 1959 (M. Nelson and F. Welch, pers.
comm. ) .
Fig. 10. Two-day-old young and an addled egg on
nesting ledge at desert eyrie in Colorado Plateau
(site 28) shown in Figure 9. Photo by G. D. Lloyd
and C. M. White, 10 June 196L
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
11
y=.38l+(-.OI4X)
Fig. 11. Linear regression analysis of the number of Peregrine Falcons recorded per party hour, during Christ-
mas bird counts at the Bear River Migratory Waterfowl Refuge between 1939 and 1970. Each circle
represents the observations for one Christmas bird count. Downward trend is statistically significant (p<0.01).
This analysis suggests that the peregrine had essentially disappeared as a wintering bird in the Bear
River marshes by 1965.
12
BnicnAM Young University Science Bulletin
DENSITY DISTRIBUTION OF PEREGRINE EYRIES IN UTAH
Utah's desert climate should seem to be a
significant barrier to the nesting of the pere-
grine, yet we have compiled a list of about 40
eyries in the state (Table 1), which appear to
have been active at one time or another. On
the basis of density, if all 40 eyries were active
simultaneously, there would be about 2,123 sq
miles (5,499 km-) per eyrie site. If the 11 sus-
pected but unverified eyries (SNV, Table 1)
are excluded, the density would be reduced to
one eyrie site for every 2,928 sq miles (7,584
km=).
Density of peregrine nesting sites in Utah
appears to be directly related to the availability
of food and suitable cliffs for nesting. The im-
portance of these two factors to the distribution
and density of the peregrine in the state will be
discussed separately in a later section. Eyrie
sites usually were situated near marshes, lakes,
or rivers, where there was a plentiful supply of
prey species. Where the nesting habitat was ex-
tensive, such as in the area of the Great Salt
Lake ( Fig. 1, Table 1 ), eyrie sites were clustered
around the marshes in a pattern conforming to
the availability of nesting sites (Fig. 12). Else-
where in the state, where suitable habitat is
greatly restricted, each eyrie site usually was
located many miles from its closest known neigh-
bor (Fig. 1).
The density of peregrine eyries in Utah, ex-
clusive of the area surrounding the Great Salt
Lake (4,500 mi-; 11,655 km-), is one site per
4,232 sq miles ( 10,962 km-), if the 19 additional-
ly known and suspected eyries were all active
simultaneously. If the 10 suspected eyries in the
remainder of the state are excluded, the aver-
age area per nest site would be 8,935 sq miles
(23,142 km-). There were 20 known eyries in
the area surrounding the Utah and Great Salt
lakes (Fig. 1, Table 1, e}rie sites, 1-20). This is
exclusive of eyrie site 22 (Table 1) which is
outside of the region. One other probable eyrie
is suggested by the presence of adults on each
of several visits by L. R. Wolfe ( field notes of
R. G. Bee) to one other site (site 21, Table 1).
If all 20 known eyries were active concurrently,
there would have been one eyrie site for about
every 225 sq miles (583 km-) in an area cover-
ing about 4,500 scj miles (11,655 km-), sur-
rounding and including the Utah and Great Salt
lakes (Fig. 1, Table 1).
The average distance between 13 eyries ( sites
5, 7-10, 12-19, Table 1) located along 130 linear
miles (209 km) of the west face of the Wasatch
Mountains from the south end of Utah Lake to
the north end of the Great Salt Lake was 10.0
linear miles ( 16.1 km). The closest eyries to each
other were about 2 miles ( 3.2 km ) apart and the
Fig. 12. Looking east from the peregrine's hunting habitat at a large Utah marsh toward its nesting habitat
along the escarpment of the Wasateh Mountains. Two pairs of peregrines ami tliree pairs of frairie FiJcons
nested on the portion of the ejiffs seen in tlie distanee and both species utilized tlie marshes. Photo by R. J.
Erwin, August 1971.
Biological Sehies, Vol. 18, No. 1 PEREcniNE Falcon in Utah
13
farthest were 20 miles (32.2 km) apart. How-
ever, since cliffs make up only about 25 miles
(40 km) of the 130 linear miles, including side
canyons (estimated from U. S. Geological Sur-
vey topographic maps), peregrine eyries, on the
average, were only about two miles (3 km)
apart on the cliff sections of the mountain. Sev-
eral additional eyries near the western edge of
Utah Lake and the eastern and southern edges
of the Great Salt Lake were not included because
they did not fall in a direct line with the 13
eyries mentioned above.
It is possible that populations of the pere-
grine were substantially greater prior to arrival
of the first white settlers than historically, con-
sidering the apparent abundance of food that
was available in nearby marshes, the number of
cliffs which appear to be suitable (but which
lia\'e not been known to harbor peregrines ) , and
the probable lack of human disturbance.
Population densities of the magnitude of
those occurring around the Great Salt Lake
seeminglv did not differ greatly from some of
those present in other regions of North America
where the environment is considered more con-
genial to the peregrine. For instance, Herbert
and Herbert (1965) recorded nine eyries along
55 miles (88.5 km) of the Hudson River (eight
on the west side) for an average of 6.1 miles
(9.8 km) per eyrie. Berger and Mueller (1969)
found 14 eyries along a 198.4-mile (319 km)
stretch of upper Mississippi River for an average
of 14.2 miles (22.8 km) between eyries.
White and Cade ( 1971 ) recorded a peregrine
density along the Colville River in 1967-1969 to
be one pair per 8.3 miles (13.4 km) above
Umiat Mountain and one pair per 3.7 miles
(6.0 km) below Umiat Mountain, giving an
overall average of 6.03 river miles (9.7 km) be-
tvveen eyries. The distance between active eyries
ranged from 0.4 miles (0.64 km) to 27 miles
( 4.3.4 km ) . There were 32 nesting pairs of pere-
grines along 183 miles (294 km) of the Colville
River in Alaska in 1952, 40 pairs in 1959, and
27 pairs in 1967, for an average distance in miles
between eyries of 5.7, 4.6, and 6.8 (9.2, 7.4, and
10.9 km), respectively (Cade, I960; White and
Cade, 1971).
The average distance between 19 eyries along
172 miles (277 km) of the Yukon River in Alas-
ka was 9.3 miles (15 km) (range, 2.75-31 mi;
4.4-49.9 km) in 1951 and 10.1 miles (16.3 km)
(range, 2-31; 3.2-49.9 km) in 1966 (Cade, White,
and Haugh, 1968). Cade, White, and Haugh
(1968) believed that the peregrine probably
was never more common along the Yukon than
in 1966.
For the Aleutian Islands, White, Emison, and
Williamson ( 1971 ) found the average distance
between peregrines defending territories to be
about 5.8 miles (9.3 km) (range, 0.81-21 mi;
1.3-34 km) for Amchitka Island, similar densi-
ties on Rat and Semisopochnoi islands, and
ec|ual or perhaps greater densities on Kiska
Island (M. Nelson, pers. comm., 1971).
On the other hand, no locality in Utah had
populations approaching the densities found in
several other regions. Hickey (1942), for exam-
ple, in a local area of the eastern United States,
reported five pairs of peregrines on 7 miles
(11.3 km) of escaqiment. In Great Britain, Rat-
cliff e ( 1962 ) found three pairs residing along
a linear distance of 1,000 yards (914 m) of sea
chff, and 15 pairs along a 17-mile (27.4 km)
distance. The highest densities known are for
the Queen Charlotte Islands, where five to eight
pairs of falcons utilized a linear distance of a
mile (1.61 km) of sea cliff (Beebe, 1960).
Hickey (1942) listed 19 pairs of peregrines
in an area of about 10,000 sq miles ( 25,900 km^ )
around New York City, for an average of one
pair for evers' 526 sq miles (1,362 km-). Cade
( 1960 ) estimated a probable density of 200 and
300 sq miles (518 and 777 km') per pair in
the Colville and Yukon river systems, respec-
tively, and one known pair per 2,000 sq
miles (5,180 km-) in the Yukon countr\'. Bond
( 1946 ) considered the peregrine to be common
along the western coast of the United States
and Baja, Mexico, where there was an average
of less than 2,000 sq miles (5,180 km=) per
known pair. Judging from the data presented
above, the peregrine was relatively common in
the area of the Great Salt Lake and uncommon
elsewhere in Utah.
TOPOGRAPHY, CLIMATE, AND PLANT COVER IN UTAH
Utah is in a region of generally high inland
plateaus and mountains which have been dis-
sected by numerous canyons and dotted with
manv lakes and inland valle\s. A chain of moun-
tains and high plateaus beginning at the comer
of Wyoming and extending southwest\vard ap-
proximately two-thirds of the length of Utah
separate the major part of the state into the
Colorado and Great Basin drainage areas (see
Fig. 1 ) . The elevation of this central mountain
14
BniGHAM YouNO Univeksity Science Bulletin
chain ranges from 9.000 to 12,000 feet (2,743-
3,658 m). Tlie Wasatch Mountains make up the
northern third of the central cliain ( to the south-
em end of Utah Lake) and high plateaus the
remainder.
Nearly all of Utah west of the central moun-
tain chain lies in the Great Basin and contains
the entire drainage of ancient Lake Bonneville,
of which Utah, Sevier, and Great Salt lakes are
remnants. The Great Salt Lake, which is about
83 miles (134 km) long by 51 miles (82 km)
wide, has fluctuated in area from 2,400 sq miles
(6,216 km-) in 1870 to 950 sq miles (2,461 km-)
in 1961 (Nelson, 1969). It contains high concen-
trations of salts (about 25 percent) comprising
principally sodium chloride and sodium sul-
fate. Utah Lake, which is about 23 miles (37
km) long and 15 miles (24 km) wide, is fresh
water. Water comprises nearly three percent of
Utah's area due mainly to these lakes. The low-
lands on the floor of the basin range from
4,200 to 5,550 feet (1,280-1,692 m) in elevaHon.
Just west of the Great Salt Lake lies the Great
Salt Lake Desert, one of the most formidable
deserts in North America. In its greatest length
and width it exceeds 150 by 60 miles (240 by
97 km) (see Fig. 1).
Tlie eastern half of the state is in part of the
Colorado Plateau or Colorado River Basin. The
Colorado River Basin is bordered on the north
by the high Uinta Mountains, some peaks of
which exceed 13,000 feet (3,962 m), and con-
tains the Uinta Basin immediately south of the
mountains and the eanvonlands farther south.
It is dissected from north to south by the Green
and Colorado rivers. The basin floor ranges in
elevation from about 4,300 feet to 6,000 feet
(1,311-1,829 m). The Virgin River Basin, in
southwestern Utah, is about 2.250 feet (686 m)
in elevation.
Because Utah lies in the rain shadow of the
high coastal ranges, it is one of the drier regions
in North America, with an average of onlv 4
to 10 inches ( 10.2-25.4 cm ) of annual precipita-
tion in the desert lowlands. The precipitation
generally increases with an increase in altitude
and may reach 30 to 50 inches (76.2-127.0 cm)
annually in the higher mountains. Daily and
seasonal temperatures in Utah vary widely. The
summer maximum may exceed 100°F. The rela-
tive humidity is extremely low and the evapora-
tion rate is high.
The desert lowlands are dotted with salt
desert shrubs consisting chiefly of greasewood
(Sarcobatus vermiculatus) and shadscale (Atrt-
plex confertifolia) in areas below 5,.500 feet
( 1,676 m) in elevation, and sagebrush (Artemisia
tridentata) in areas higher than 5,500 feet (1,676
m) throughout much of the Colorado Plateau
and the Great Basin. This low scrubby vegeta-
tion ranges from several inches to several feet
in height. Desert scrub, consisting predominantly
of mesquite (Prosopis glandtiliflora) , creosote
bush ( Larrea divaricata ) , and black brush
( Coleogtjne Tamosissima ) , occurs in the southern
desert of southwestern Utah.
The more arid foothills in the Great Basin
and Colorado Plateau, which receive 10 to 15
inches (25.4-38.1 cm) of rainfall annually, are
covered with pinon-junipcr forests (Pinus and
Jimipems). 10 to 30 feet (3.0-9.1 m) in height.
Foothills receiving 16 to 20 inches (40.6-50.8
em) of rainfall are covered with a variety of
scrubbv trees and bushes called chaparral, con-
sisting of oak (Qiiercus), maple (Acer), service-
berry (Amelancliier), mountain mahogany (Cer-
cocarpus), mountain laurel (Ceanothus), and
manzanita (Arctostaphtjlos). Above the foot-
hills lie montane forests of spruce (Picea), fir
(Abies), and aspen (Populus tremnloides) . The
aforementioned data on relationships between
precipitation and vegetation are modified from
Woodbury and Cottam (1962).
Utah's numerous mountain ranges, its ex-
tensive plateaus, and its high cliffs and mesas
supply a plentitude of suitable nesting sites
for birds of prey. The low scrubby vegetation
of its foothills and desert lowlands provides the
extensive hunting areas preferred by the larger
falcons.
ECOLOGICAL DISTRIBUTION OF UTAH PEREGRINES
Climate
The peregrine, as represented by a cosmo-
politan assortment of geographically variable
races, has adapted to a wide variety of environ-
mental conditions. This is true also for the ana-
tum race, which ranges from the tree line of
the North American Arctic south sparingly into
northern Mexico and the southern tip of Baja
California. In Utah, the peregrine has been
known to nest in the Great Salt Lake Desert,
one of the more arid regions known to be in-
habited by this cosmopolitan species. At Wen-
dover, for example, the monthly rainfall for the
critical breeding period of March through July
averaged onlv 0.44 inches (1.12 cm) over a 49-
vear period; the mean monthlv temperature
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
15
ranged from 42° F (6°C) in March to 79°F
(26°C) in July (U. S. Dept. of Commerce,
1965). Bond ( 1946) tells of peregrines nesting in
the hot, arid climates along the lower Colorado
River in California, in northeastern California,
and eastern Oregon.
Climate along the Wasatch Mountains of
Utah, where the peregrine historically attained
its maximum density in the state, is more mod-
erate. Here (Salt Lake City) the monthly rain-
fall for March through July averaged 1.03 inches
(2.62 cm) over a 32-year period; the monthly
temperature ranged from 40°F (4.4°C) in March
to 77°F (25°C) in July (U. S. Dept. of Com-
merce, 1965).
Figures 13-15 delineate some of the climatic
extremes associated with nesting peregrines in
Utah. The hythergraphs given in Figure 13
are composites of the mean monthly extremes
of daily temperature (for record period) and
the mean monthly precipitation for weather sta-
tions near 18 known peregrine eyries distrib-
uted throughout Utah. Tlie breeding period,
March through August, is indicated also. Tlie
composite hythergraphs are constructed the
same as those given by Twomey (1936) and
Linsdale ( 1937 ) , except that these authors used
mean nionthlv averages of daily temperature
rather than extremes (data from U. S. Dept. of
Commerce, 1965).
In Figure 14 we have plotted the monthly
a\'erage of the daily minimum temperature
against the monthly average of the daily maxi-
mum relative humidit>' (from readings taken at
three-hour intervals, 1965 through 1969) and the
monthly average of the daily maximum tempera-
tures against the monthly average of the daily
minimum relative humidity for Salt Lake City
( U. S. Dept. of Commerce, Local Climatol. Data
1965-1969).
Figure 15 gives a composite of the mean
number of days per month that the precipitation
was equal to or exceeded 0.1 inch (0.25 cm)
and the mean number of davs per month in
which the temperature was equal to or exceeded
90°F (.32.2°C), averaged for the 18 stations util-
ized in Figure 13 (data from U. S. Dept. of
Commerce, 1965, [for record period]).
We used the extremes of climate since they,
more than means, are likelv to influence the
general distribution of a species. According to
Odum (19.59:116-117):
. . . temperature exerts a more severe limiting effect
on organLsm.s when moishire conditions are extreme,
that is, either very high or very low, tlian wlien such
conditions are moderate. Likewise, moisture plays a
more critical role in the extremes of temperature.
It is at the environmental extremes that the
evolutionary processes for a species are most
pronounced in regards to the development of
new limits of tolerance. By comparing the cli-
matic extremes at the periphery of the ecologi-
cal range of a species, such as the peregrine in
Utah, one may gain an insight into the climatic
factors which may hmit its range.
Altitude
For western North America, Bond's data
( 1946 ) indicate that the peregrine rarely nests
above 5,000 feet (1,524 m) in elevation, with
a few nesting up to 10,000 feet (3,048 m) in
California. However, many of the 18 eyries
cited by Enderson (1965) for Colorado were
above 5,280 feet (1,610 m), while the majority
of them were above 6,000 feet (1,829 m) (En-
derson, pers. comm.), with one eyrie in a high
mountain region of Colorado, situated at an
elevation of 12,000 feet (3,658 m) (Thomas D.
Ray, pers. comm.). It may be that the habitat
requirements of the peregrine are best satisfied
in Colorado at these higher elevations. The
paucity of eyries known to Bond ( 1946 ) to be at
the higher elevations may be due, in part, to the
difficulties encountered in reaching and search-
ing the cliffs.
Nelson (1969) reported that peregrines in
Utah nest at elevations up to tree line, between
6,000 and 7,000 feet (1,829 and 2,134 m). The
only eyrie in Utah exceeding 6,000 feet (1,829
m), that is known to us, is at an elevation of
6,700 feet (2,042 m) (Table 1, site 36), but two
are at 6,000 feet (Fig. 1, Table 1, sites 22 and
37), and the elevations of four others approach
6,000 feet (Fig. 1, Table 1, sites 26, 28, 35, 38).
One suspected eyrie site, however, is at an ele-
vation of 8,500 feet (2,591 m) (Fig. 1, Table 1,
site 29) and another is at 9,750 feet (2,972 m)
(Fig. 1, Table 1, site 27), suggesting the possi-
bility that if higher areas were searched, others
would be found. The mean elevation of pere-
grine eyries in Utah is about 5,000 feet (1,524
m) (Table 2). They ranged from 3,360 to
6,750 feet (1,024-2,057 m), with a prepon-
derance of eyries (89 percent) between 4,000
and 6,000 feet (1,219 and 1,829 m) in eleva-
tion, and with nearly 50 percent of them at
elevations between 4,500 and 4,999 feet (1,372
and 1,524 m). A frequency distribution of the
elevations of Utah eyries is given in Table 2.
Habitat Niche
The habitat niche of the peregrine may be
divided into two parts: (1) the cliff or substrate
upon wliich it lays its eggs and rears its young
16
Bhicium YdUNC University Science Bulletin
100-
2C>-
10- -
Maximum
oV
0
■M-
4-
M
NIMUM
I I I I I I I I
2 3 0 12
Inches of Precipitation
Fig. 13. Composite hythcrj^raph for 18 stations situated near known peregrine eyries in Utah. Mean total
monthly precipitation is represented in inches and mean monthlv extremes of temperature (daily ma.\i-
mum and minimum, for record period) are represented in degrees F; they were constnicted the same
as those given by Twomev (1936) and Linsdale (1937), except that these authors used mean monthly
temperatures (U.S. Dept. Commerce, 1965). The diagonalK lined area depicts the climatic conditions for
the egg-laying and incubation period (March-May); the stippled area represents the hatching and nestling
period (May and June); the vertically lined area shows the fledging period (June-August).
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
17
IOOt
SO-
SO'
UJ
S60-
Q
-50-
LlI
a:
<40-
Ixl
a.
^30'
20--
10- -
0'
MIN TEMP : MAX REL HUM
■'• K.
MAX TEMP-. MIN REL HUM
1 I I I I I I I
0 10 20 30 40 50 60 70
Percent of Humidity
-I
80 90 100
I'ig. 14. Climographs for Salt Lake City. Utah. Daily maximum temperatures (averaged monthly for years
1965-1969), represented in degrees F are plotted against the mean daily minimum relative humidity for the
same period; and the mean daily minimum temperatures for the same period are plotted against the mean
daily maximum relative humidity. Humidit)- vahies were average from the maximum and minimum readings,
taken at .3-hour intervals for 196.5 through 1969 (U.S. Dept. Commerce, Local Climatological Data). Num-
bers beside points designate month.s of the year.
18
Bhigham Young University Science Bulletin
3a
25-
20
o
o
<
Q
10-
N=I8
Mean-
EXTREMES
/
/
/
-r-
^^
\
•4-
Mar Apr May Jun
MONTHS
Jul
Aug
30
25
20
15
\0
O
Al
i^^--^^
N=I8
Mean
Extremes a;:^'
—(I
^•~.
I
0^
,<i- —
Mar Apr May Jun
MONTHS
Jul
Aug
•0
Fig. 15. Composite graph for 18 stations near peregrine eyries in Utah depicting the mean number of days
per month in which precipitation was 0.1 inch (0.25 cm) or more and the average number of days per month
in which the temperature was 90°F (32.2°C) or higher. (For record period, U.S. Dept. of Commerce,
1965.) Values were averaged (dashed hues) for tlie same 18 eyrie sites u.sed in Fig. 13; extreme values
are represented by sohd triangles.
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
19
Table 2. Frequency distribution of peregrine eyrie site
elevations in Utah.
Elevation
(500-ft. inter\als)
n
Percent
Elevation
( intervals in meters )
3000-3499
1
3.2
914.4-1066.7
3500-3999
0
0.0
1066.8-1219.1
4000-4499
3
9.7
1219.2-1371.5
4500-4999
15
48.4
1371.6-1523.9
5000-5499
6
19.4
1524.0-1676.3
5500-5999
4
12.9
1676.4-1828.7
6000-6499
1
3.2
1828.8-1981.1
6500-6999
1
3.2
1981.2-2133.3
Totals:
31
100.0
xelev. 4987 ft (1520 m)
Range 3360-6750 ft ( 1024-2057
m)
and around which its reproductive activities take
place (nesting sites), and (2) the surrounding
environs or territor)' where it obtains its food
(hunting sites).
Nesting Sites
Most peregrine eyries in Utah were situated
on a high ledge on the face of a cliff, but one
female peregrine was reported to have laid her
eggs in 1946 (Boyd Shaeffer, pers. comm.) on
one of the dikes (elevated roadways) that sep-
arated two impoundment lakes at Ogden Bay
State Waterfowl Management Area (Table 1,
site 20). Additionally, an ornithologist (verbal
report, to J. H. Enderson at AOU meeting, 1964 )
reported seeing an adult peregrine carry food
to a \oung, nonflving falcon on the Monnon
Temple in'Salt Lake City in 1962, although we
can find no corroborative evidence that falcons
ever nested there.
CHff OrientaHon
The ledges on which most Utah peregrines
nest are in extensive mountain ranges which lie
in a north-south direction. The escarpments of
these mountains provide east- and west-facing
cliffs, while their side canyons provide both
north- and south-facing cliffs (Fig. 12). As il-
lustrated in Figure 16, most peregrine eyries in
the state were found in east- and north-facing
cliffs. .Although the escarpment along the Wa-
satch Mountains provided cliffs which faced all
directions (Fig. 12), 10 of 12 eyries, for which
data are available, were at sites facing north-
ward (five evries) and eastward (five eyries);
three of the 12 faced slightly westward (NNW
and NW), four faced southward (ESE and SE),
one faced directlv west, and one faced directly
south. This suggests a directional orientation
by the peregrine to the sun's exposure. Cliffs
facing north or east should provide the eyrie
better protection from the hot afternoon sun than
would those facing south or west.
These findings tend to corroborate those
of Nelson (1969), who has documented the
death of nestling Golden Eagles {Aquila chrysae-
tos) due to direct exposure to the hot rays of
the sun. He considers tlie peregrine to be more
sensitive to the extremes of temperature and to
the direct rays of the sun than the Prairie Fal-
con. He has pointed out that the later nesting
of the peregrine, compared to that of the Golden
Eagle and Prairie Falcon makes the peregrine's
young more vulnerable to heat and sun than are
the young of either of the other t^vo species.
McGahan (1968) found a preference by the
Golden Eagle in Montana for southern exposures.
He suggested that nest site preference was in-
fluenced by the direction of the sun and noted
that exposure should be important when tem-
peratures are below freezing as well as during
the warmer months of June and July.
In Alaska, Cade ( 1960) found that peregrines
nesting along the Yukon River preferred cliffs
facing an easterly direction and that this orienta-
tion had some relation to the sun. He noted
no such correlation, however, for eyries along
the Colvillc River and hypothesized that the
Yukon eyries faced eastward because of strong
prevailing summer \vinds, whereas the lack of
special orientation along the Colville was due to
the absence of such winds.
On the other hand, in Great Britain, where
the climate is more moderate, Ratcliffe (1962)
found that suitable cliffs faced all directions
and that British peregrines are indifferent to di-
rectional facing. He argues further that more
intensive ice action on shaded north and east
slopes have resulted in more extensive develop-
ment of cliffs or crag ranges on these slopes.
Hence, he concludes that cliff exposure is
unlikely to influence the deliberate choice of a
nesting cliff or site.
Our data and those of Cade's (1960) suggest
that sun and wind exposure in the harsh ex-
tremes of climate such as those in the desert
and in the Arctic may, indeed, elicit a deliberate
choice of nesting sites. In Great Britain peregrine
eyries probably are not subjected to such harsh
extremes of climate, and thus, peregrines have
less need for making deliberate choices there.
Rock Type, Cliff Size, and Eyrie Height
The physical characterisHcs of the cliff play
an important role in their use by the peregrine
as a nesting site. The geological formation, in-
volving type of rock and height of cliff, con-
tributes to the suitability of the cliff as a nest-
ing site. Tliirty peregrine eyries in Utah were
20
N
BnicHAM Young University Science Bulletin
,\
W'^j:!:) 00 o^ cx;
0
2
t)
0
B
^^
99^MRIE £^^^/p^
O
^P\ f^ V.
lV<^ 3.,.
^%t'
vP
■^. 1^^
C^
O
^ 3ia\x/>^^
Cv.
^/S^"^^'^93B3a ^^K^
I
b.
£
\
&/\
A
Fig. 16. Directional facings of Peregrine Falcon and Prairie Falcon eyries in Utah, both in areas of sympatry and
in areas of allopatry. The values in the outer ring are for the peregrine; those in the inner ring are for the
Prairie Falcon. The directional relationships shown here were statistically significant at /; <0.01 (X" test;
calculated .\= value, 7.37, 1 df) for the Prairie Falcon and p<0.05 (X=test; calculated X= value, 4.48, 1 df)
for the Peregrine Falcon.
situated on cliffs composed principally of four
types of rocks: limestone, nine e\'rics; sandstone,
nine eyries; quartzite, six eyries; and volcanic
rock, three eyries. One additional eyrie each
was located on volcanic agglomerate, granite,
and metamorphic gneiss.
According to Hickey (1942), the height of
the cliff is involved in the species' fidclit) at the
eyrie site over many generations of occupancy,
and this concept is supported h\- Ratcliffe ( 1962,
1969) in Great Britain; iMsclu-r (1967) has dis-
cussed the concept for eyries elsewhere in Eu-
rope. Hickey (1942), on the basis of height and
c()ntinuit\' of use, classified cliffs in the eastern
United States into three classes. Bond (1946)
believes Hieke\"s (op. eit. ) classification to bi' an
oversimplification in the western United States.
Peregrines in Utah selected a wide variety
of e\ rie sites. .-Mthough the histor\- of occupancy
of indi\'iduai eyries in Utah is largely unknown,
there is some evidence to support Hickey's
( op. cit. ) hypothesis, at least in regards to height.
I']\rie sites on the low, marginal cliffs were the
first to be abandoned in Utah, whereas several
Biological .Series, Vol. 18, No. 1 Pereghine Falcon in Utah
21
that were situated high up, on massive cliffs
that were difficult to climb, have the longest
histories of occupancy.
A frequenc\' distribution of heights of cliffs
which supported nesting peregrines in Utah are
gi\'en in Table 3. These cliffs ranged from 40
to 400 feet (12.2-122 m) in height. The mean
height of 21 such cliffs in Utah was 178 feet
(.54.3 m). An additional cliff, first noted by
Treganza earlv in this centur)' and reported by
\\'oodburA- et al., (unpubl. ms), was in excess
of 1,000 feet (304.8 m) in height (Figs. 1 and
7; Table 1, site 8). We excluded it from our cal-
culations so as to not disturb unduly the more
normal range of heights (see footnote. Table 3).
For 14 evries the distance from the base of
the cliff to the evrie site averaged 105.5 feet
(32.2 m) and ranged from 28 to 330 feet
(8.5-100.6 m). These measurements do not
include the talus slope and mountain side. If
these distances were included, the values given
above would be considerably higher for most
sites, especially those on the escaq^mcnt of the
Wasatch Mountains. Ratcliffe (1962) has dis-
cussed the importance of the steep slopes as a
relevant factor in attracting peregrines to the
cliff.
From the brink of the cliff to the eyrie
sites below, the distance averaged 68.6 feet
( 20.9 m ) and ranged from 12 to 250 feet ( 3.7-
76.2 m ) for 13 e\ries.
The values given here for cliff heights aver-
age somewhat higher than those reported by
Cade (1960) for "the Yukon River in Alaska,
and by White and Cade (1971) for the Colville
River. Distances from the base of cliffs to the
nest sites in Utah, however, averaged nearly
twice those reported by Cade ( 1960) in the Arc-
tic.
Hunting Sites
Marshes apparently play an important role
in the breeding ecology of the peregrine in
Utah (Figs. 12, 17, and 18), because nearly all
peregrine eyries are situated near them. We
measured the distances from each of 20 known
eyrie sites in the Great Salt Lake and Utah
Lake valleys to the closest nonflowing surface
water, to the closest marsh 320 acres (130 ha)
or larger, and to the closest marsh with no re-
gard to size. The surface areas of the closest
nonflowing water and the size of the closest
marsh were also determined. Measurements were
taken from U.S. Geological Survey topographic
maps which were constructed from aerial photo-
graphs taken between 1945 and 1956; they are
summarized in Table 4.
Of the 4,.500 sq miles (11,655 km=) sur-
rounding and including these two lakes, marshes
covered about 100 sq miles (259 km-), while
open water comprised about 1,443 sq miles
(3,737 km=). With exclusion of the Utah and
Great Salt lakes, with their surface areas of
about 138 sq miles and 1,661 sq miles (358
km- and 4,302 km-), respectively, the surface
area of water would be 80 sq miles (207 k-m").
If the three large impoundment lakes (surface
area, about 55 mi"; 142 km-) at the Bear River
Table 3. Frequency distribution of heights of cliffs containing Peregrine
Utah and the vertical distances of eyrie sites above bases of the cliffs.
Falcon and Prairie Falcon eyries in
Distance
CLIFFS
EYRIES
Distance
in
Peregrine
Prairie
Peregrine
Prairie
in
Feet
n Percent
n
Percent
n
Percent
n
Percent
meters
0-24
0 0.0
1
2.3
0
0.0
10
19.6
0.0-7.5
25-49
1 4.5
11
25.0
3
21.4
19
37.3
7.6-15.1
50-74
1 4.5
10
22.7
3
21.4
8
15.6
15.2-22.8
75-99
4 18.2
8
18^2
3
21.4
7
13.7
22.9-30.4
100-124
4 18.2
5
11.4
0
0.0
2
3.9
30.5-37.9
125-149
1 4.5
0
0.0
1
7.1
0
0.0
38.0-45.6
150-199
3 13.6
3
6.8
0
14.3
2
3.9
45.7-60.9
200-249
1 4.5
2
4.5
0
0.0
1
2.0
61.0-76.1
250-299
1 4.5
1
2.3
1
7.1
1
2.0
76.2-91.3
300-349
2 9.1
2
4.5
1
7.1
0
0.0
91.4-106.6
350-399
1 4.5
0
0.0
0
0.0
0
0.0
106.7-121.8
400-449
2 9.1
0
0.0
0
0.0
0
0.0
121.9-137.0
450-499
0 0.0
0
0.0
0
0.0
1
2.0
137.1-152.3
500 >
1 4.5
1
2.3
n
0.0
0
0.0
152.4>
Totals:
22 99.7
44
100.0
14
99.8
51
100.0
X
178.0 ft"
101.7 ft
105.5 ft
64.2 ft
(54.3 m)
(31.0 m)
(32.
,2 m)
(19.6 m)
Range:
40--400 ft
7-500 ft
28-330 ft
2,
.5-450 ft
(12.2-121.9)
(2.]
1-152.4 m)
(8.,5-100.6 m)
(0.76-1.37.2 m)
•Excludes one ground nestcr and one eyrie on a 1.000 ft ( ^On m) cliff.
22
Bricham Young University Science Bulletin
I
\
Fig. 17. Saltgrass (Distichlis stricta) marsh at Ogden Bay Refuge, Black-necked stilts (Himantopus mexicantis),
a prey species of the peregrine, in the foreground. Photo by R. D. Porter, 1953.
Fig. 18. View to the west toward Promontory Mountains from Ogden Bay Waterfowl Management Area.
Marshes in foreground are typical of those adjacent to Great Salt Lake from which peregrines and prai-
ries nesting along the Wasatch escarpment and adjacent mountains obtained their major food source. Photo
1)V R. J. Erwin, August 1972.
Biological Series, Vol. 18, No. 1 Pehecrine Falcon in Utah
23
Table 4. Distances from peregrine e)rie sites in the Great Salt Lake Valley and Great Basin De.sert to open,
nonflowing water and marsh liiinting areas and the size of these areas in relation to distance (measured
from U.S. Geological Sursey topographic maps which were constructed from aerial photographs taken be-
tween 1946 and 1956). Values in parentheses represent metric equivalence in kilometers or hectares.
MARSHES
SURFACE WATER'
Mi. to
Mi. to
Number of
Mi. to
closest
Acres in
Mi. to
closest
acres in
closest
marsh >
closest
closest
water >
closest
Area & Sta- marsh
320 acres
marsh
water
320 acres
water
tistic ( km )
(130 ha)
(ha)
(km)
(130 ha)
(ha)
Wasatch Mountains
( Utah & Great Salt
Lake valleys)
n 19
19
17=
19
19
14'
x±SD 3.3 ±2.6
7.6±5.1
17.5 ±20.6
2.5+2.0
5.2±4.3
59.6 ±344
(5.3 ±4.2)
(12.2±8,2)
(7.1±8.3)
(4.0 ±3.2)
(8.4±6.9)
(24.1 ±13.9)
Range 0.19-9.7
0.19-18.6
3.7-82.6
0.10-6.7
0.10-13.6
1.2-188.8
(0.31-15.6)
(0.31-29.9)
(1.5-33.4)
(0.16-10.8)
(0.16-21.9)
(0.49-76.4)
Desert, Great Basin
n 3
3
3
3
2*
3
x±SD 1.3 + 1.3
1.3 + 1.3
7,302 ±10,396
1.7 + 2.0
4.0
406 ±701
(2.1±2.1)
(2.1±2.1)
(2,955 ±4,207)
(2.7 ±3.2)
(64)
(164 + 284)
Range 0.19-2.8
0.19-2.8
640-19,281=
0.19-4.0
4.0-4.0
1.0-1,216
(0.31-4.5)
(0.31-4.5)
(259-7,803)
(0.31-64)
(6.4-6.4)
(0.40-492)
'nonflowing waters; lakes and ponds, -excludes Iwo large marshes, one 5,598 acres {2,2G() hal, the other 1,114 acres (-lol ha),
^closest water to five eyries was either Utah Lake or Great Salt Lake; hence, they were excluded. Mata for one desert eyrie, which was
nearly 100 miles (Ifil km) from large bod,y of water, was excluded. ^Nelson (19(36) gives 4,700 acres (1.000 ha) for Clear Lake Water-
fowl Management .\rea, but topographic maps show an additional 14,5-Sl acres (5,901 ha), contiguous with the management area, and a
total of 53,000 acres (21.449 ha) are shown within about 20 miles radius of the Clear Lake e.vrie,
Refuge were also excluded, the amount of sur-
face w'ater would be reduced to 25 sq miles
(65 km-). If both surface waters, exclusive of
the Utah and Great Salt lakes, and marshes were
divided equall\- by the 20 known peregrine
eyries for the area, each pair of birds at these
evries would use prey species from 4.0 sq miles
('10.4 km-) of water.'S.O sq miles (13.0 km=) of
marsh, and 9.0 sq miles (23.3 km-) of the two
combined. Nelson ( 1966), on the other hand, re-
ports that there are 234 sq miles (606 km=) of
managed marshlands surrounding the Great Salt
Lake (see Fig. 19), to which may be added
several sq miles of unmanaged marshes con-
trolled bv duck clubs. The disparitv between
Nelson's measurements and ours probablv is due
to the fact that we used onlv marsh areas as
shown on topographic maps and excluded mud
flats and water, whereas Nelson's measurements
probabU' include all lands and water within the
Waterfowl Management Areas.
Marshes were the dominant features near
three eyries in the Great Basin desert (Figs.
1 and 20, Table 1, sites 4, 23, and 25), and
Twome\- (1942) reported the use of the Ashley
Greek marshes by peregrines nesting in Uintah
Gount)-. The desert eyrie in the Colorado Plateau
reported by White and Lloyd (1962) was by
a river (Fig. 9). Figure 21 gives an aerial view
of a river site in the desert of northern Arizona,
tspical of those in parts of Utah, and Figures
22 and 23 show marshes near eyrie sites in the
Great Salt Lake Desert.
Peregrines nesting along the Wasatch es-
carpment traveled long distances to obtain shore
and marsh birds, which made up the bulk of
the food items found in their nests (Table 4),
and the marshes where they hunted were rather
extensive. In general, the Great Basin desert
eyries were closer to marshes and to open
water than were the Wasatch escarpment eyries
( Table 4 ) . One marsh supporting an eyrie in the
Great Salt Lake Desert is onlv about a square
mile (2.6 km-) in extent, and is only about a
mile (1.6 km) from the eyrie (Fig. 20). It is
about the same size as the Ashley Creek marsh
(Stewart Lake Waterfowl Management Area,
Nelson, 1966) near the eyrie found by Twomey
( 1942 ) . The marsh at one other e^'ric in the
Great Salt Lake Desert covers about 2^4 square
miles (5.8 km-) and is less than a mile from the
e\rie site. An additional eyrie site (Woodbury
et al., unpubl. ms) was 2.8 miles (4.5 km) from
a marsh that covered over 30 square miles
(78 km-') (Table 4). The surface area of fresh
water at two of the desert sites is only a few
acres in extent (Fig. 23), whereas that at the
additional site was about 2 square miles (5.2
km-) in extent.
Of the 40 eyries and suspected eyries in
Utah for which we have data, three were along
rivers with marshes, streams, or lakes; five were
24
Bricham Young Universiti- Science Bulletin
GRANTSVlLLfc
Fig. 19. Distrihiition of maiuigcd marshlands concciitratnl aniviiul tlu- Cr^at Salt Lake region. Photo by per-
mission of Utah Oivisioii of Wildlife Resources, in Nelson, 1960.
Biological Series, Vol. 18, No. 1 Pehegrine Falcon in Utah
25
^^j"-*'
Fig. 20. View across a marshy area adjacent to an eyrie in the Great Basin at the edge of the Great Salt
Lake Desert. R. D. Porter is standing in foreground ;ind is about 1 mile (1.6 km) east of the eyrie shown
in Figure 44. Photo by R. J. Erwin, August 1972.
Fig. 21. Aerial view of a river eyrie site in the desert of northern Arizona typical of those in southeastern
Utah. View looking NNE. Peregrines nested on the canyon wall on the right hand side of tile photo.
Photo by G. D. Lloyd, 1960.
26
Bricham Young University Science Bulletin
along major rivers; 25 were near marshes with
lakes and streams; five were along streams only;
and there was one each near a marsh and a lake
only. All but two of the 21 eyries near the Great
Salt Lake were adjacent to a stream, which usual-
ly comprised the closest source of water. The
smaller passerine birds associated with the
streamside vegetation provided the peregrines
with a source of food which frequently was
within the immediate area of the eyrie.
The marshes originate from desert springs,
from the overflow of rivers and creeks, from
deltas at the junctions of rivers and lakes, and
in more recent times, from artificial damming
of streams or from the fomiation of ponds re-
sulting from the drilling of wells. Bulrush (Scir-
pus sp. ), saltgrass {Distichlis stricta) (Figs. 17
and 18), and cattail (Tijpha sp. ) (Fig. 12) are
the principal plants in these marshes.
The marshes supply food for peregrines dur-
ing all seasons of the year, but are especially im-
portant during nesting season. The presence of
an abundant food supply in the marshes at Og-
den Ba\' undoubtedly was the major ecological
factor responsible for the groundnesting of a
peregrine there. Several easily accessible eyries
that were mentioned by Beebe (1960) in the
Queen Charlotte Islands mav have been due to
an abundant source of pre)' and to the absence
of mammalian predators.
The combination of marshes adjacent to suit-
able cliffs for nesting may be considered an
"ecological magnet" (Hiekey, 1941) for the pere-
grine in Utah, especially along the Wasatch es-
carpment, where extensive marshes border the
Utah and the Great Salt lakes. Here, marshes
are formed at the deltas of three major rivers
that flow into the lake (Fig. 19). Typical of
M
i^' '>-%'^
Fig. 22. Eyrie site near the eastern limits of the Great Salt Lake Desert. The eyrie, when first located by
Porter in the early 19.5()s, was on a small cliff in the left foreground which does not show in this photo be-
cause it was removed to make a road bed. The peregrines were last .seen using the cliffs near the top right
of the photo. Prairie l'"alc()iis also used the same eyrie that was last used by the peregrines at least three
years after the peregrines were last seen there. Photo by K. J. Krwin, August 1971.
Biological Sebies, Vol. 18, No. 1 Peregrine Falcon in Utah
27
their vegetation is that at the delta of the Weber
River (Ogden Bay), which, from salt flats to
river channels, consists mainly of glasswort
(Salicornia sp. ), saltgrass, alkali bulrush (S.
pahi(losus). hardstem bulrush (S. acutiis), cat-
tail (T. latifoJia and T. angustifolia) , and sago
pondwecd (Potamogeton pectinatus) (Nelson,
1954). For a more comprehensive description
of plant ecology in Utah marshes, see Nelson's
( 1954 ) studies of a marsh near the Great Salt
Lake ( Ogden Bay ) and Bolen's ( 1964 ) discus-
sion of a spring fed marsh in the Great Salt Lake
Desert (Fish Springs).
Numerous remains of nine species of water-
birds, including grebes, ducks, rails, avocet,
gulls, and terns, from anthropological sites at the
northwest side of the Great Salt Lake, some
dating back at least 8,350 years (Hai^per and
Alder, in press ) , suggest that marshes were pres-
ent in the Great Salt Lake valley long before
the arrival of the white man. Some of the early
hunters and explorers to enter the valley re-
ported the presence of numerous waterfowl and
shorebirds. Father Escalante, who visited Utah
Lake in 1776, wrote that the lake "abounds in
man\' kinds of fish and in geese and waterfowl"
(Harris, 1909). Osborne Russell, a trapper, saw
"miriads of Swans, Geese Brants, and Ducks
which kept up a continuous hum day and night
. . ." at Bear River marshes on 2 April 1842
(Haines, 1955). Fremont (1845), who visited the
Bear River Delta on 3 September 1843, men-
tioned the thunderous noise made by multitudes
of waterfowl in the marshes and described the
area as being covered with rushes and canes.
Captain Stansbury (1852) made similar observa-
tions on 22 October 1849 from a vantage point
on the east side of Promontory Point. He re-
corded that ". . . thousands of acres, as far as the
eye could reach, were covered with them [water-
fowl]. . . ." Fremont (1845) reported that "the
stillness of the night [8 September 1843] was en-
livened by millions of waterfowl," this time at
the mouth of the Weber River near Little Moun-
tain; and on 9 September he reported that the
shallow delta of the river was "absolutely cov-
ered with flocks of screaming plover." Stansbury
( 1852 ) noted innumerable flocks of ducks, geese,
white swan, and long-legged plover around the
shallows at the mouth of the Jordan River on
4 April 1850. It is probable that the "plover"
were mostly American Avocet {Recurvirostra
americana). Black-necked Stilt (Himantopus
viexicarms). and Willet {Catoptrophorus semi-
pahnattis) .
Vegetation at the river sites was comprised
mostly of cottonwoods {PopuJus fremontii in the
Lower Sonoran desert areas; P. angustifolia in
the Upper Sonoran areas) and willows (Salix
exigua was most frequently present, with S.
hitea, S. gooddingi, and S. caudata occasionally
present also). Other plant species known to oc-
Fig. 2.3. View from hilLsiile below eyrie in Figure 22, Brackish marsh can be seen in the midgroiind, and salt
flats from the Great Salt Lake can be seen in the background. Photo by R. J. Erwin. August 1971.
28
Brigham Young University Science Bulletin
cur with the cottonvvoods and willows include:
squawbush (RIius trilohata), wildrose {Rosa
sp. ), tamarix (Tamarix ramosissimu) , Joshua tree
(Clistoyucca hrevifolia), box elder (Acer ne-
gundo ) , ash ( Fraxinus sp. ) , baccharis ( Baccharis
emonji), hackberrv (Celtis douglasii), and even
scrub oak {(^)uercus gambelii). Tlie presence or
absence of the latter species is dependent upon
altitude, latitude, and local ecological conditions.
Food Niche
Little has been published on the diet of the
peregrine in the intermountain region. Wet-
more's ( 1933:49-50) account of the hunting tac-
tics of the peregrine on the Bear River marshes
has been quoted elsewhere ( Bent, 1938 ) . It is re-
peated here because it gives a remarkedly vivid
picture of the peregrine in its native haunts
along marshes of the Great Salt Lake earlier in
the present century.
The birds [falcx)ns] at rest perched in low willows, or
on logs or bits of drift, where tliey had clear view of
the teeming bird life about them. Wlien hungry, they
dashed across the open flats at high speed, striking
ruthlessly at any birds that appeared, from small s;md-
pipers to large ducks.
Their appearance in the air was always the signal
for chattering cries of akirm from blackbirds and avo-
cets that put all tlieir bird neighbors on the watch.
These warnings had little effect, however, as the duck
hawk, killing practically at will, was truly despot of
this realm.
I have seen this falc-on dash through closely massed
flocks of flying sandpipers, striking out two or three
with as mimy thrusts of the claws, allowing each bird
to drop and then wheeling swiftly to seize the falling
prey in mid-air before it reached the ground. Again, I
liave seen one in a stoop, swift almost ;is light, knock
a redhead duck to the ground, where it landed with
a broken wing and other injuries.
On one occasion a pair of duck hawks harried a help-
less nighthawk, stooping at it playfully until one in
passing gave it a f[uick squeeze with one foot. It
then ;Ul()wed the nighthawk to fall, when it was seized
by the other duck h;uvk. Tlicn the pair flew away,
and the one with the booty at intervals dropped it, so
that it could be seized in air by its mate.
Food items found in several Utah eyries are
summarized in Tables 5 and 6. We collected 107
individual prev items representing 20 species
of birds and at least one species of mammal from
two eyries along the escarpment of the Wasatch
Mountains between 1943 and 1957. The Ameri-
can Avocet was represented in the greatest num-
bers ( Fig. 24 ) . It, the Mourning Dove ( Zenai-
I"ig. 24. Avoccl at nest. This species was the most important food species found in the eyries of the pere-
grine in the valley of tin; Great Salt Lake and also the most fre(iuent shorebird species in the eyries of the
Prairie Falcon in the same localit)-. I'hoto by R. J. Erwin, 8 Jiuie 19.59.
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utaii
29
Table 5. Prey species in Peregrine Falcon and Prairie Falcon eyries in areas of sympatry along the escarpment
of Utah's Wasatch Mountains', facim' the marshes v( the Great Salt Lake.
Prey species
Weight class
in grams"
Duck sp. (yng. )'
Killdeer
( Charadrius lociferous )
Willet
( Catotrophorus semipalmatus )
Greater Yellow-legs
( Totanus melanoleucus)
Long-liillcd Dowitcher
( Limnodromus scolopaceus)
Sanderling
(Crocethia alba)
American Avocet
( Rccurvirostra americana )
Black-necked Stilt
( Himantopus rncxicnnus )
Wilson's Phalarope
( Stcganopus tricolor )
Franklin's Gull
( Lurus pipixcan )
Shorebird and Gull
Subtotal
California Quail
( Lophortijx californiciis)
Ring-necked Pheasant
{Phasianus colchicus)
Gallinaceous
Bird Subtotal
Mourning Dove
(Zetuiidura macroura)
Rock Dove
{Coluniba livia)
Dove
Subtotal
Red-shafted Flicker
(Colaptcs cafer)
Western Kingbird
(Tijranrws vcrticalis)
Homed Lark
(Eremophila alpestris)
Scrub Jay
(Aphelocoma coeridescens)
Robin
(Tiirdui- migratoriiis)
Bohemian WiLwving
(Bombi/cilla garrula)
House sparrow
(Passer domcsticus)
Western Meadowhvrk
(Sturnclla ncglecta)
Redwinged Blackbird
(Agelaius phocniceus)
Brewer's Blackbird
( Euphagus cijanoccphalus )
Unidentified blackbird
Green-tailed Towhee
(Chlorura chlorura)
Rufous-side Towhee
( Pipilo en/throphthalmus)
Passerine
Subtotal
Big brown bat
(Eptcsicus fuscus)
Unidentified bat
150
106
203
165
86
63
281
152
58
295
198
807
115
318
137
42
29
77
82
56
26
89
54
68
61
30
.37
n
Peregrine
Percent of
total
Falcon
Percent of
biomass
3
2
2.80
1.87
2.75
1.29
10
9.35
12.38
3
2.80
3.02
2
1.87
1.05
Prairie Falcon
n Percent of Percent of
total biomass
22
20.56
1
0.93
6
5.61
1
0.93
50
43.92
13
12.15
5
4.67
18
16.82
8
7.48
0.93
1.87
1.87
9
8.41
4
3.74
3
2.80
5
2
4.67
1.87
37.10
0.93
2.12
1.80
59.69
9.12
9.70
18.82
6.69
0.47
0.99
0.68
4.89
1.32
1.24
1.86
0.37
28
26.16
11.82
18
1
0.93
0.11
10
2
1.87
0.12
9
18
1
1
2
40
2.63
11.84
6.58
1.32
7.89
21
27.63
1
1.32
2
2.63
3
3.95
2
2.63
1
1.32
3
3.95
1
1.32
1
1.32
1
1.32
9.21
11.84
23.67
1.32
1.32
2.63
52.63
2.60
8.26
8.79
0.55
14.60
32.20
1.71
13.97
15.68
1.99
2.75
4.74
1.19
0.36
0.25
4.97
2.03
13.87
0,59
0.53
0.64
23.24
30
Bricham Young Univebsity Science Bulletin
Table 5 (Continued)
Uintah groiintl squirrel
{Cilelius trrmatus)
250
_
_
_
2
2.63
4.33
Rock siniirrel
696
_
_
_
2
2.63
12.04
(Citellus variegatus)
Unidentified ground
400
_
_
_
1
1.32
3.46
squirrel (Citellus sp)
Meadow mouse
60
_
_
_
1
1.32
0.52
( Microtus sp )
Mammal
3
2.80
0.23
6
7.90
20.35
Subtotal
Totals
107
99.98
20 species
100.00
76
100.01
21 species
100.00
'Mo.':t prey itcni^ for both species origmated Irom the Peregrine Falcon and Prairie Falcon eyries at site 7 (Table 1, Fig. 1); hence, ior
the most part, they represent prey species from n common resource.
'Weights of all avian species, with exception of tlie common pigeon, were obtained from Porter, Bushman, and Behle (impubl. ms);
the value for the common pigeon w.is obtained from Roxie I.ayboume. of the U. S. Bureau of Sport Fishencs and Wildlife; weights of
mammalian species were estimated from those given by Hall I194C). Those of xmidentified bats, ground squirrels, and young ducks were esti-
mated by the authors.
^Weight of the young ducks is estimated; voimg pintails iAnas titutti) not vet feathered were in the peregrine e\Tie on 13 and 14
June 19+7.
dura macruura), Willct (Fig. 25), Western Mead-
owlark ( Sturnella neglecta ) , Red-shafted Flicker
{Colaptes cafcr), Wilson's Phalarope {Stegano-
piis tricolor). Rock Dove {Columha livia), and
two species of blackbirds (Agelaius phoenicetts
and Euphagus cijanocephalus) made up nearly
79 percent of the food items at the eyries. How-
ever, in both total biomass (59.7 percent) and
in numbers (4.3.9 percent), the shorebirds com-
prised the largest segment of the diet, of which
the avocet (37.5 percent biomass) (also see
White, 1963) and Willct (12.4 percent biomass)
were by far the most frequent. Tliis is probably
a reflection of the availabilit)' of shorebirds in
the Great Salt Lake marshes.
Aside from being common, both avocet and
Willet ma\' have some conspicuous behavior that
makes them easv to capture and that accounts
for the numbers taken b\' the falcons. Tinbcrgen
( 1940 ) has shown that various behavioral pecu-
liarities of certain passerine birds enhance their
vulnerability to predation, and F. and J. Craig-
head (1956), based on the study of the food
remains at 20 peregrine eyries, have suggested
that the flash patterns of meadowlarks, redwings,
and the Blue |a\ {Cijanocitta cristata) and the
eonspieuous Hight of flickers ma\' increase the
vuliKTability of these species to predation by the
peregrine. This hypothesis may be applicable to
the Willet and avocet, both of which have con-
spicuous flash patteiTis.
Mourning l^oves and Rock Doves were im-
portant columbiforme items ( hS.S percent of bio-
mass and 16.8 percent of total items). Passer-
ines, woodpeckers, and bats were represented
in smaller numbers and biomass (Table 5).
The use of bats for food by peregrines has
been reported from Texas by Stager ( 1941 ), and
desert nesting Shaheen Falcons ( Falco pelegri-
nokles hahtjloniciis) of the Middle East, which
are either peregrines or are very closeh' related
to them (Vaurie, 1961; White, 1968b; Brown
and Amadon, 1968), reportedly hunt bats at
dusk (Dementiev, 1951 and 1957). In Indonesia,
Mees (1949) reports that wintering tundra fal-
cons seem to be specialized for feeding on bats.
He saw one falcon kill seven bats one after an-
other. Fischer ( 1968 ) reports that the subspecies
of peregrine (F. ;}. ernesti) indigenous to Indo-
nesia also hunts bats.
Fig. 25. Willet {Catoptrophortis scvtipahiatus) on nest.
The Willet was an important prey species in pere-
grine cvries of the CJreat Salt Lake Valley. This
species is inconspicuous while on nest but in fUght
it, like the stilt and avocet, shows a striking flash
pattern. Photo by R. J. Erwin 19.59.
Biological Series, Vol. 18, No. 1 Pehecrine Falcon in Utah
31
Table 6. Prey species in two Peregrine Falcon eyries in Utah's desert (sites 4 and 28, Table 1, Figs. 1, 9, and
22).* C = Colorado Plateau, GB = Great Basin.
Weight
class
in grains
No.
Percent
of
total
Percent
ot
biomass
Chukar {Alectoris graeca) (C)'"
American Coot (Fulica americana) (GB)°"
Mourning Dove {Zeimidura macroura) (C, GB)
Common Nightliawk (Chordeiles minor ) (GB)°°
Ash-throated Flycatcher {Myiarchus cincra'icens) (C)""
Sav s Phoebe ( Sayrnis saya ) ( C ) ° °
Horned Lark { Eremophila alpcslris) (C, GB)""
Pinon Jay {Gijmnorhinus cyanocephala) (C)°°
Western Meadowlark (Sturnella ncglccta) (GB)
Yellow-headed Blackbird ( Xanthocephahis
xanthocephalus) (C)"
Redwinged Blackbird {Agelaiits phocniceus) (C, GB)
Lark Sparrow (Chondestes grammacus) (GB)""
Unidentified Passerines (C)
Passerine Subtotal
Desert Totals
520
1
5.26
26.52
365
1
5.26
18.60
115
2
10.53
11.73
62
1
5.26
3.16
29
2
10.53
2.96
21
1
5.26
1.07
29
3
15.79
4.44
116
1
5.26
5.92
89
1
5.26
4.54
92
3
15.79
14.07
54
2
10.53
5.51
29
1
5.26
1.48
14
73.68
39.99
19
99.99
100.00
'Sro fonttinte for Table 5
•'Not recorded in Wasatch Moiinlain eyries (see Table 5).
Eyries adjacent to the Great Salt Lake con-
tained no full-grown waterfowl despite the abun-
dance of waterfowl in the adjacent marshes, al-
though the peregrine has been observed eating
or pursuing full-grown ducks of several species
during the breeding season. These include the
Gad\\all ( Anas strepera ) ( observed 5 May 1938,
field notes of R. G. Bee), a teal (H. Austin,
pers. comm.), a teal on 10 April 1948 at Ogden
Bay (Porter), and the Redhead {Aijthya ameri-
cana) (Wetmore, 19.33). Calvin Wilson (pers.
comm.) has watched peregrines from an eyrie
in the Wasatch Mountains eating Ruddy Duck
(Oxytira janmicensis) , Cinnamon Teal {Anas cij-
anoptera). Pintail (Anas acuta), and American
Coot {Fulica americana) on dikes of a nearby
marsh. R. J. Erwin (unpubl. data) flushed a
peregrine from the side of a highway in Grand
County in April 1958, where it had just cap-
tured an adult Mallard {Anas platjtrhynchos).
Cade, White, and Haugh ( 1968), on the other
hand, found that waterfowl constituted nearly
50 percent (biomass) of the food items in the
eyries of the Alaskan taiga peregrine (F. p.
anatum, sensu lata). Utah peregrines are smaller,
however, than those of interior Alaska. The
absence of ducks in the Wasatch Mountain ey-
ries mav possibly be explained on the basis of
the weight of the prev item in relation to the
distance that peregrines must earn,' it to their
evries. A full-grown duck may be too heavy for
peregrines to carry the several miles from the
Great Salt Lake marshes to eyries along the
Wasatch escarpment.
Shorcbirds were not present in two desert
eyries. One e\rie was located near a marsh in
12 species
the Great Basin and the other near a river in
the desert of the Colorado Plateau. The avail-
ability of a variety of marsh and shorcbirds to
the peregrines at the desert eyries in the Great
Basin (Table 6) accounts for the presence of the
coot. The coot in the Great Basin desert eyrie
probably came from a pond (desert spring)
which was only about 1,200 yards ( 1,097 m )
from the eyrie site. Since its weight (400 g) is
about the same as that of a duck, it is possible
that its absence from the Wasatch Mountain
eyries may have been for the same reason that
ducks were missing from these eyries. The small
sample-size of food items probably accounts
for the absence of shorcbirds in this desert eyrie.
At a Wasatch Mountain eyrie, observed by
R. D. Porter (site 7, Table 1) for the first two
weeks after hatching, only one, and at most,
two, prey items were found each day in the
nest; these usually consisted of Redwinged Black-
birds, Mourning Doves, Willets, and meadow-
larks. But as the nesting season progressed,
a greater number of species and items were
brought to the nest. On 28 June 1952, for ex-
ample, about three weeks after hatching of
the young falcons, the female returned with a
young Willet at 11:00, a robin-sized bird at 11:50,
and an unidentified item at 17:20. The male re-
turned with a young avocet at 15:20 and a leg
of a young avocet at 15:45. The next day the
male brought a Wilson's Phalarope to the nest
and the female an avocet. Other items found
in the nt^t on 29 June were Scrub Jay ( Aphelo-
coma coerulescens) , unidentified blackbird, big
brown bat {Eptesicus fuscus) and one adult and
one immature Wilson's Phalarope. Of the shore-
32
Brigham Young UNrvERsiTY Science Bulletin
birds brought to the young at this eyrie (site 7,
Table 1) during the years it was observed, 33
percent were partially fledged young of the sea-
son. Peregrines nesting along the face of the
Wasatch Mountains traveled several miles to
obtain the marsh and shorebirds (Table 4);
other species were obtainable much closer to the
eyries.
Despite the peregrine's reported antipathy to
capturing food on or near the ground (Bond,
1936a), mammalian prey species such as the
brush rabbit (Sijlvilagus bachmani) (Bond,
1936c), rats [Rattus sp.) (White, et al, 1973),
and certain gallinaceous birds (ptamiigan,
Lagopus sp.) '(Cade, I960; White and Cade,
1971 ) also are taken for food occasionally. Bond
( 1946 ) reported that peregrines commonly
brought Horned Larks to their small young.
The Homed Lark, which is essentially a ground-
dwelling species, is one of the most abundant
birds in Utah's salt desert scrub vegetation. It
was present in peregrine evries in both the
Colorado Basin and Great Basin deserts of Utah
(Table 6).
Much of the desert lowlands and foothills
of Utah are vegetated with desert scnib and with
pigm\' conifer forests, respcctivelv, yet the pere-
grine was not known to nest far from water in
those areas where the Homed Lark of necessity
would have been an important item in its diet.
Javs (ApliclocoDia and Gymnorliinus), king-
birds {Tyranmis), Ash-throated Flvcatcher
[Miiiarclius cinerascens). Lesser Nighthawks,
Red-shafted Flickers, Robins, Mourning Doves,
and Black-throated Cra\' Warbler (Dcndroica
nigrescens). some of which are kTiown to be used
as prev bv the peregrine, are available in the pig-
mv forests, vet the peregrine nests in these areas
only when water or marshes are nearby.
A more intensive study of the peregrine's
food habits in Utah during nesting season un-
doubtedh' would have revealed a much wider
variety of prey species, especially the smaller
passerines. In terms of biomass, however, the
smaller species of birds probably would not have
altered appreciably the percentages of each
categor)' of birds.
The abundance of doves in Utah eyries is
not surprising, despite the availability of marsh
and shorebirds, since the domestic pigeon has
been found to be a favorite prey species of the
peregrine, not only in the eastern United States,
but also in many other areas of the peregrine's
cosmopolitan distribution (Hickey and Ander-
son, 1969).
The Utah peregrines utilize a wide variety
of prev species (at least 29 species, see Tables
5 and 6) during the nesting season, and in this
respect their diet is more comparable to that of
populations elsewhere in North America than to
tliat of populations in the Queen Charlotte Is-
lands, where Beebe (1960) found them limited
mosth' to one and not more than four prey spe-
cies during the nesring season. On Amchitka in
the Aleutian Islands, White, Emison, and Wil-
liamson ( 1973, in press ) list 32 species in the
peregrine's diet, most of which were found in
the nests, and comprised principally marine
birds, waterfowl, gulls, and shorebirds. Shore-
birds were represented frequenth' in the eyries
of peregrines along the Colville River of Alaska
(White and Cade, 1971). Cade, White, and
Haugh ( 1968) reported 49 prev species in eyries
located in the taiga zone of the Arctic, and Cade
(1960) found 21 species in nests located in the
tundra zone.
NESTING BEHAVIOR IN UTAH
History of Nesting at a Wasatch Mountain Eyrie
Eyrie sites of the Peregrine and Prairie Fal-
con at a chff on the escarpment of the Wasatch
Mountains (Table 1, site 7; Fig. 26) were ob-
served by R. D. Porter, R. J. Erwin, and others
from 1943 through 1952, exclusive of two war
years, 1944 and 1945. We obtained data at this
cliff on interspecific competition between the
two species and on productivity, incubation peri-
ods, and rcproduetive failure for the peregrine,
all of wliieh will be discussed under s(>parate
headings.
The cliffs were composed of quartzite and
faced westerly along the west-facing escarpment
of the mountains and southerK- along a south-
facing edge of a side canyon. Peregrines were
first noted there on 3 April 1943, the year the
cliff was first under our observations, by R. J.
Erwin and J. F. Poorman, and again that year
by J. F. Poorman and R. L. Porter on 15 April.
A nest containing three eggs was found on 26
,\pril. Prairie Falcons were also first noted at
this cliff in 1943. A summary of the reproductive
history of the peregrines at this site is given in
Table 7. The phvsical characteristics of the var-
ious peregrine and Prairie Falcon sites utilized
during the period of studv are given in Table 8.
The photographs represented by Figures 27-39
were taken in 1947, 1948, and 1952.
In 1949 the peregrines defended a nesting
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
33
Fig. 26. A cliff along the escarpment of the Wasatch Mountains which contained eyries of both the Peregrine Fal-
con and tlie Prairie Falcon (Table 1. site 7). The Peregrine Falcons used site A-3 in 194.3, 1952, and 1953;
site B in 1946 and 1947; and site C in 1948 and 1951. The Prairie Falcons used site 2 in 1948; site A-3,
1949; and site 1, to the north (not shown in photograph) of site A-3, in 1943 and 1950. Sites B and C
faced south, sites 1, 2, and A-3 faced west. Photo by R. J. Envin, 1972.
ledge, which contained two nest scrapes, but
apparently laid no eggs. They defended several
sites on the cliff in 1950 but with less tenacity
than usual. Although they made 20 to 25 scrapes
along several hundred feet of ledge, no eggs
were found. Between 4 March and early June
the cliffs were searched for an eyrie 10 times
without success. The behavior of the birds sug-
gested the presence of a nest at numerous places
along the cliff. However, each new section of
chff was defended with nearly equal spirit.
In 1952, the two young at site A (Fig. 26
and Tables 7 and 8) were measured and
weighed from date of hatching until 13 August.
They were removed from the nest on 5 July.
R. J. Erwin banded three young peregrines at
the 194.3 site in 1953. He obtained no informa-
tion on egg number or occurrence of Prairie
Falcons.
A new female peregrine nested at alternate
site A in 1952. She still had some immature
,0^'
•t
V
Fig. 27. Five-egg clutch of Peregrine Falcon (eyrie
site 7-B, Table 1, 1947). Note the wood rat {Neo-
toma sp. ) scat on ledge and about the eggs. Photo
by R. D. Porter.
34
Brigham Young University Science Bulletin
Fig. 28. Female peregrine entering eyrie. Photo by R. D. Porter and R. J. Erwin, 1948.
Fig. 29. Female peregrine settling down over nestling.s which are only a few days old (Table 1, site 7, alt.
.site C). Photo by R. D. Porter and R. J. Erwin. 1948.
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
35
Fig. 30. Female peregrine brooding young. Note addled egg. Photo by R. D. Porter and R. J. Erwin,
1948.
Fig. 31. Female peregrine with young, in defensive attitude. Photo by R. D. Porter and R. J. Erwin, 1948.
36
Bricham Young University Science Bulletin
».
Fig. 32. Female peregrine feeding young. Photo by R. D. Porter and R. J. Erwin, 1948.
\^1\ V
u^
«
t-''
Fig. 33. Female peregrine feeding young which were nearly 3 week.s old (eyrie site 7, alt. site B, Table 1).
Photo by R. D. Porter, 1947.
Biological Series, Vol. 18, No. 1 Peregrine F.alcon in Utah
37
A -
Fig. 34. Young peregrines at approximately 4 weeks of age (eyrie site 7, alt. site C). Photo by R. D. Porter
and R. J. Erwin, 1948.
Fig. 3.5. Young peregrines about 6 weeks of age, nearly old enough to fledge (eyrie site 7, alt. site C). Photo
bv R. D. Porter, 1947.
38
Bhicham Young University Science Bulletin
Table 7. Reproductive history of the peregrines at a Wasatch
Figs. 26-29).
Mountain eyrie ( site 7, see Tables 1 and 8, and
Alternate
EGGS
NESTLINGS
Probable
Incubation
Other
site
Dates
date of
period
Dates
dates of
Year
location
recorded
No.
1st egg
(in days)
No.
hatched
record
Misc. Data
1943
A
26 April
3
-
^37 (3rd egg)
3'
unknown
31 May
1946
B
-
-
-
unknown
4
unknown
26 June
Young nearly
fledged, two taken
1947
B
26 April
17 May
3
5?
21-22 April
35-37 (3rd egg)
3
unknown
31 May
Downy young
1948
C
16 April
19 April
27 May
3
4
5
11-12 April
42-44 (3rd egg)
39-41 (4th egg)
4
28-29 May
29 May
29 June
5 July
17 July
5 eggs, 1 pipped
27 May; 4 young -|-
1 addled egg, 29 May
4 young, 2 taken'
young fledged'
young full grown'
1951 C
2 May
3 May
13 May
19 May
3
3
2
0
unknown
0
-^
1952 A
29 April
1 May
27 May
V
V
3
29 April
37 (cggl)
0'
2
4 June
5 June, 07:00 5 June
2 eggs pipping
1 hatclied, 1°
nearly hatched
31 May
3
-
2
7 June
both hatched
1 June
3
-
1953 A
- -
-
-
unknown
3
-
^Three young were about ready for flight when two were taken for falconry s-iinetime in early July. -29 June: 4 young, 2 males,
2 females; females taken for falconry; oldest male, tail half grown, flew from nest. 5 July: I young male, still on nest ledge, flew at
approach of observer, first male to leave nest on rock above nest. \7 July: females taken from nest about full grown. ^Marked with a
numeral 1 in India ink. ^Two eggs pipping, one with small bole (egg 1), other barely dented, young peeping inside both eggs, loudest
in egg marked with numeral 1 ; marked egg weighed 47 g, other pipped egg, 50 g, and impipped egg, 48 g. ^Shell around abdomen and
legs; it probably hatched on 6 June; third egg addled.
feathers (see Figs. 36-38), and was undergoing
a molt as evidenced bv the fact that on 28 June
the upper surface of the wings had just begun
to molt into the adult plumage. The molt on the
back (capital and spinal feather tracts) and the
lower breast (ventral tracts) was nearly com-
plete, while that of the primaries and rectrices
had only begun. The capital tracts of the head
were only partially molted. While the female
was in flight, it was noted that at least one pri-
mary was missing on each wing as well as at
least one retrix on each side of the tail.
The plumage condition of this bird indicates
that she probably was no more than three years
of age. Records of breeding peregrines while
still in their immature plumage are not common.
Beebe (1960) noted no instances of mated pairs
in immature plumage, or even in plumage show-
ing traces of immaturity, in a rather large
sample of pairs along the northwest Pacific
Coast. However, Herbert and Herbert (1965)
pointed out two instances of immatiux'-plum-
aged females occupying an eyrie, neither of
which was found to lay eggs. Hickcy (1942)
reported on three immature, one-vi-ar-old fe-
males that failed to lay eggs and a fourth that
brooded a clutch of t\vo eggs, making a total
of only one first-year f(-male out of .34 falcons
over a two-year-period in New York. A report
by Herbert of two females believed by him to
be two-vear-old birds, both of which laid only
two eggs in different )ears, also was mentioned
by Hickcy ( 1942). White and J. R. Haugh (pers.
ol)ser. ) found one female, out of 17 pairs breed-
ing on the Yukon River in 1966, that was essen-
tially still in the streaked brown immature plum-
age. Therefore, it was thought to be but one
year old. She laid Uvo fertile eggs, one of which
hatched.
Egg Laying
At the alternate site A eyrie (Table 1, site
7) egg la\ing began between 12 and 29 April
( 1943-1952) as estimated by counting back from
known dates certain eggs were laid (Table 7).
Published records for the state range from about
22 March (counting back from 30 March as
given by Johnson, 1899) to the second or third
week in NIa\- (counting back from 20 Ma\' given
by Bee and Hutchings, 1942). The first' egg of
a three-egg clutch found by White and Lloyd
(Table 1, site 28) was probably laid around 6
Ma\', as indicated by the date of hatching. At
the aforementioned e\rie in the Wasatch Moun-
tains (Table 1, site 7), 3.8 (\ggs (range .3-5) on
the average were laid per year during the five
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
39
..v;-^
Fig. 36. A view of female peregrine with unmolted immature plumage. Her two young are about 3 weeks old
(eyrie site 7, alt. site A). Photo by R. D. Porter, 1952.
Fig. 37. Same female as in Fig. 36. This bird is c(;rtainly not more than three years old because of the amount of
immature plumage retained. Note tiiat most of the tail, secondary wing feathers, and greater wing coverts
are immature feathers. Photo by R. D. Porter, 1952.
40
Bhigham Young University Science Bulletin
Table 8. Physical characteristics of eyrie sites at a cliff in the Wasatch Mountains (Table 1, site 7, see Figs.
26-39) used by botli peregrines (Pe) and Prairie Falcons (Pr). Values in parentheses represent metric equiva-
lents.
Approx. dist.
Dist. Eyrie
Dia.
in ft (in)
Species'
Cliff
Eyrie
Ledge
Ledge
below
Nest
nest
Depth
from
and
height.
height,
length.
width.
overhang.
area
scrape.
.soil,
Alt.
site A
year
ft
ft
Direct
inches
inches
inches
ft=
inches
inches
site
to site
used
(m)
(m)
facing
(m)
(m)
(m)
(m=)
(m)
(m)
A-3=
0
Pe 1943
110
85
W
72
62
20
7.42
6.9
2
1952
(34)
(26)
(1.8)
(1.6)
(0.,51)
(0.69)
(0.18)
(0.051)
1953
Pr 1949
B
320
Pe 1946
135
90
S
120
60
18
6.45
-
-
(98)
1947
(41)
(27)
(3.0)
(1.5)
(0.46)
(0.60)
C
350
Pe 1948
135
90
S
156
48
35
6.55
6.4
(107)
1951
(41)
(27)
(4.0)
(1.2)
(0.89)
(0.61)
(0.16)
-
1'
300
Pr 1943
110
(91)
1950
(34)
-
w
-
-
-
-
-
2'
55
Pr 1948
110
95
w
61
90
21
21.8
-
2
(17)
(34)
(29)
(1.5)
(2.3)
(0.53)
(2.0)
-
(0.051)
M^rairie Falmiis wrie not reinrded in 1**47. 1952. and lOji, were seen, bul no nest was found in 1951.
'All values were obtained by direct measurements at eyrie sites; all other values given in the table, except cliff and ej-rie heights,
distances between e>Tie sites, are approximations from photographs, using a peregrine's egg or the adult peregrine as a unit of measurement.
^Exact e>xie site was not reached.
years that eggs were found (see Fig. 27), and
2.4 of the eggs (range 0-4) on the average
hatched. The eyrie produced a total of 19 young
during the seven years it was known to have
been active, for an average of 2.7 young per
year. Although the number of fledged young
was not ascertained, no )Oung were known to
have died in the nest. Eight young, however,
were removed for falconr>' when nearly fledged.
These values approach those for the peregrine
Fig. .38. A close-up of same female as in Fig. 36. Photo by R. D. Porter, 1952.
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
41
in eastern North America, where Hickey (1942)
found the average clutch size to be 3.72 and
the average number of downy young to be 3.0.
For western North America, Bond (1946) re-
ported an average clutch size of 3.7 and Cade
( 1960 ) recorded an average of 2.7 eggs per
clutch in northern Alaska and 3.1 eggs per clutch
in other locations in the Arctic.
Incubation
The eggs are laid usually at two-day inter-
vals, and occasionallv at three ( Cade, 1960; Her-
bert and Herbert, 1965; Dcmandt in Fischer,
1967). On the Hudson River, incubation gener-
ally began on the fifth day with the laying of
the third egg and averaged 32-33 days from time
of commencement until the hatching of the
last egg (Herbert and Herbert, op. cit. ). The
incubation period is detennined best by check-
ing the time between the last egg laid and the
last \oung hatched (Nice, 1954), providing
that all eggs hatch. Although the incubation
period in the peregrine is said to be 28-29
days (Witherby, et al, 1939; Dementiev, 1951;
Herbert and Herbert, 1965), there is still some
unccrtainb." regarding its exact length, as sug-
gested also by Nelson ( 1972), who believes it to
be closer to 32 to 34 days in F. p. pealei. If the
incubation period for the fifth egg is 28 to 29
davs, and not more than two days elapse be-
tween the laving of each egg, the period be-
tween la\'ing of the fourth egg and the hatching
of the fifth egg would be 30 to 31 days; be-
tween the la\ing of the third egg and the hatch-
ing of the fiftii, .32 to 33 days; between the
second and the fifth, 34 to 35 days; and between
the first and the fifth egg, 36 to 37 days. In
four-egg clutches, the intervals between the lay-
ing and hatching of the third and fourth egg
would be 30 to 31 days; between the second and
the fourth egg, 32 to 33 days; and between the
first and fourth egg, 34 to 35 days. For three-egg
clutches, the intervals between the laving of the
second and third eggs would be 30 to 31 days;
and between first and third eggs, 32 to .33 days.
If, as reported b\' Nelson (ibid.), the incubation
period is 32 to .34 days, 4 to 6 additional days
must be added to each of the above values.
At the Wasatch Mountain eyrie (Tables 1
and 7, site 7), the incubation period in 1947 and
1952 was close to that given by Nelson ( op. cit. )
for pealei. In 1948, however, it seemed to have
lasted abnormally long. The period from laying
to hatching was about 40 days (39 to 41) for
the fourth egg and at least 42 days (42 to 44)
for the third egg, which is about 10 days longer
than that expected using the 28 to 29 day period.
This could be explained if the first clutch was
destroyed within a day or so after the fifth egg
was laid and if the first egg of a new clutch
was laid a day or two later. This would increase
the observed incubation period by about 10
davs. This phenomenon has been reported in
captive American Kestrels {Falco sparverius)
(Porter and Wiemeyer, 1972).
In 19.52, the period between the laying and
hatching of marked egg number one was about
37 days. It likely was laid the day it was first
found or the day before. Unfortunately, the
period of 36 to 37 days corresponds closely to
the expected incubation period for the first egg
of a five-egg clutch, if the incubation period is
28 to 29 days, as well as that expected for the
first egg of a three-egg clutch if the incubation
period is 32 to .34 days.
Tlie 32- to 34-day period seems to fit our data
better than does the 28- to 29-day period. Addi-
tional observations are needed to resolve this
problem.
Two da\'s elapsed between the pipping of
the first egg to hatch and the fourth egg to
hatch (a fifth egg did not hatch) in 1948.
Only one day elapsed between pipping and
hatching of egg number one in 1952 and the
same was probably true of the second egg as
well. This appears to agree with Hall's (1955)
observation in 1943 on the Sun Life peregrines,
which hatched two eggs on each of t\vo succes-
sive days. Porter and Wiemeyer (1972) reported
a two-dav interval between the hatching of the
first and the last egg of five-egg clutches of
captive kestrels. The kestrels frequently began
incubation wath the laying of the fourth egg.
Unlike the peregrines of the lower latitudes,
those in the Arctic reportedly initiate incubation
with tlie la\ing of the first egg (Cade, 1960;
Dementiev, ■ 1951). Cade (1960) reported as
much as a week's difference between the ages
of the youngest and oldest nestlings in four-egg
clutches in the Arctic.
PEREGRINE DECLINE IN UTAH
The peregrine in Utah, as elsewhere in the
United States and in Europe (Hickev, 1969),
declined precipitously in the past two decades.
To our knowledge, only two or three of the 29
eyries known to occur in Utah over the past
several decades are still active. Nelson (1969)
42
Bhigham Young University Science Bulletin
reported that before 1942, 50 percent of the
"9 or 10" (9, Nelson, pers. comm. 1969, see
Table 1) eyries located by him between 1939
and 1942 around the Great Salt Lake were taken
over bv Prairie Falcons, and by 1948 onlv three
or four of them were left. White (1963), how-
ever, noted that five of these eyries (Table 1,
sites 4, 7, 8, 10, and 13) were still active as late
as 1952, and two additional eyries (sites 17 and
18) are known to have been active in 1952 (C.
Ward, pers. comm.), indicating that some of
them were overlooked b\' Nelson (1969) or else
previously unoccupied eyries were reactivated
later. However, White's (1969b) report of the
occupancN' by peregrines in 19.54 of an eyrie
which earlier in the ccnturv' ( 1927) was used by
Prairie Falcons (Wolfe, 1929) suggests that the
reverse situation also may have taken place.
The usurpation of peregrine eyries by Prairie
Falcons nia\' not have been permanent, as sug-
gested bv our observations of the two species
utilizing one another's eyries in Utah. Nelson
(1969) indicates that he was unaware of the
utilization of alternate nesting sites by the pere-
grine between 1939 and 1942, which increases
the possibility that some of the peregrine loca-
tions believed to have been taken over by Prairie
Falcons at that time were still being utilized by
peregrines nesting at alternate eyries.
By 19.56, onlv four of the 20 known eyries
along the Wasatch Front were active. No young
have been known to fledge from an\' of these
eyries since then (White, 1963), although one
adult was seen at each of two eyries in 1969
(Table 1, sites 8 and 18), and a third is report-
edly still active. Onh' two or three eyries were
believed to have been active by 1969 in the
entire state, which represents only about 10
percent of the total known to occur earlier. On
the other hand, there are vast areas in Utah
with seemingl)' appropriate ecological condi-
tions that have remained virtuallv unexplored
for falcons. It is possible that 10 or more eyries
exist in these areas. It is interesting to note that
the eyries in the more remote parts of Utah
remained active nearly a decade longer than did
those in the more populous and more intensive-
ly c>iltivat(>d areas.
Climatic Change Hypothesis for
Peregrine Decline
Nelson (1969) has hypothesized that the re-
duction in numbers of active eyries in Utah
was caused by a combination of rising average
temperature and drasticalK' reduced precipita-
tion, starting about 1870. He suggested that these
changes resulted in the dr\ing up of small lakes
and ponds and the lowering of the surface
water areas of larger lakes, causing a critical
reduction in the habitat for the prey species of
the peregrine in Utah and in other areas of the
northwestern United States. According to Nelson
(ibid.) b\' 1961 the drought gave way to more
moderate conditions resulting in habitat changes
more suitable to the peregrine.
Besides the drought conditions reported by
Nelson (1969), river waters were diverted for
irrigation and the vegetation adjacent to the
marshes was overgrazed by livestock (Behle,
1958). By 1910, thousands of once productive
acres of heavily vegetated marshlands along
the shores of the Great Salt Lake, with their
smaller lakes, ponds, and channels of frt^h water,
became mud flats with stagnant pools of alkaline
water. Ultimately these changes caused the
death of thousands of ducks, shorebirds, and
marshbirds due to botulism (Wehnore, 1915,
1918; Behle, 1958). It was not until after the
completion of the Bear River Migraton' Water-
fowl Refuge between 1932 and 1935 and tlie
Ogden Bav and Fannington Bay refuges in about
1941 that these marshes regained much of their
former vitality and productivity.
Some changes took place as late as the early
19.50s in the marshes fm-ther removed from the
lake. Weller, Wingfield, and Low (1958), for
example, recorded a drastic change in the size
of the Knudson Marsh, four miles west of Brig-
ham City, Utah, between 1950 and 1955. They
attributed the changes to a deepening of the
water channel entering Bear River Refuge, an
increased demand for irrigation waters, a below
average rainfall between 1952 and 1954, and
overgrazing bv cattle. The change in size of the
Knudson Marsh resulted in a decline of one-
third in the number of species and two-thirds
in the number of birds nesting there.
Bv 1960, the total acreage of marshland in
Utah was reduced bv nearly 50 percent ( Smith,
1961) of the 1,174,400 acres (475,279 ha) known
to exist originally (Low, 1966). Smith (1961)
reported the existence in 1960 of 600,000
acres (242,820 ha) of wetland habitat in Utah
of variable value to wildlife. Of this acreage,
83,000 (33,590 ha) were owned bv the U.S.
Fish and Wildlife Service and 60,()00 (24,282
ha) were owned and operated by the State Fish
and Game Department. The remaining acreage
was in private ownership, either as managed
clubs or as unmanaged natural wetlands. Un-
fortunately, the effects of these environmental
changes on the peregrine were never docu-
mented adeHjuatelv.
Morlan Nelson (Hickey, 1969: 96) has sug-
gested that in 1965 there was only enough
Biological Series, Vol. 18. No. 1 Peregrine F.alcon in Utah
43
habitat left in tlie Bear River marshes to sup-
port one pair ot peregrines. This would seem to
he an underestimation, since we know of several
evrie sites in the western United States where
peregrines have bred successfully adjacent to
marshes much smaller and much less productive
than are the Bear River marshes.
In discussing the decline of the peregrine in
Utah. Nelson (1969) indicated that the pere-
grines nesting in 1939 at the Ul site (site 11,
Table 1 ) adjacent to the Bear River Migratorv
Bird Refuge did not return to nest by 1941 be-
cause the drought dried up their hunting sites.
So that we might critically assess Nelson's im-
plication, we measured the extent of the marshes
and open waters within a fi\e-mile ( 18 km ) radi-
us (if tlu' Ul e\ rie, using U. S. Geological Sur-
\e\' topographic maps (aerialh- photographed,
1953-19.56). The resulting measurements tend
to weaken Nelson's argument, since there were
still 16.6 sq miles (43 km-) of marsh and 5.8
sq miles ( 15 km- ) of open water within the
five-mile radius. Moreover, the Bear River Ref-
uge, with its extensive marshes, was only seven
miles away. However, this is based on the as-
sumption that these marshes did not increase
appreciabh' in size between 1941 and 1956. We
cannot comment on the latter premise because
we have no infomiation on the extent of these
marshes for the earlv 1940s.
Since we consider the cliff at the Ul site
to be marginal in terms of accessibility to
humans and predators, we believe that human
disturbance may have been the major factor
causing the abandonment of this evrie, although
habitat change and competition with the Prairie
Falcon probablv played a subordinate role.
Further evidence which tends to weaken
Nelson's climatic change h\pothesis was ob-
tained from Noland F. Nelson, manager of the
Ogden Bay State Waterfowl Management Area.
Nelson spent man\ hours at the Bear River and
Ogden Bav marshes prior to the completion of
the refuges. He noted that there was not a
dearth of shorebirds and marshbirds at these
marshes before the dikes were constructed (N.
F. Nelson, pers. comm., 1971) and that the de-
velopment of the Ogden Bav area increased the
numbers of nesting and migrant shorebirds
(Nelson, 1954). Nevertheless, he does believe
that the shorebird populations at Ogden Bay
have declined in the past several years (N. F.
Nelson, pers. comm., 1971).
Furthermore, it is of interest to note that
Noland Nelson observed fewer peregrines at
Ogden Bay in the 1950s than in the i940s. He
saw them there occasionallv in the 1940s (Nel-
son, 1954), but rarely after the early 1950s (N.
F. Nelson, pers. com., 1971). The occasional ob-
servation of peregrines at Ogden Bay during
the 1940s is about all one would expect, con-
sidering that these marshes were supporting at
most only three pairs of active eyries during
these years. These observations correspond with
the reduction of breeding pairs along the Wa-
satch escarpment between 1940 and the 1950s.
The Great Salt Lake has been subject to
major cyclic fluctuations in size twice historical-
ly, and perhaps many times in the past several
thousand vears. Early historical evidence indi-
cates that in 1850, when the Great Salt Lake
was first sur\'eyed bv Captain Howard Stans-
bury, it was much reduced in size compared to
earlier and later reports. James Clvman, who
with a parts' of trappers first circumnavigated
the Great Salt Lake in a bullboat in 1826, wrote
the following in his journal on 1 June as he
passed through the Great Salt Lake Valley in
1846 on a trip east from California.
proceeded ne.irlv ea,st to the point of a liigh mountain
[Oquirrh Mountains] that Bound.s the Southern part of
the greate salt lake I observed that this lake like all
the rest of this wide spread Sterility ha.s nearly wasted
away one half of its surface since 1825 [1826] when
I floated around it in mv Bull Boate and we crossed a
large Bay of this lake with our horses which is now
dry . . . (Koms. 19.51:36).
Four \ears later when the lake was sur-
veyed bv Stansbur\' (1852), it covered 1,750 sq
miles (4,433 km-) '(Powell, 1879). By 1S69, the
lake had increased in size to 2,166 sq miles
(5,610 knr) (ibid.), and bv 1870 to 2,400 sq
miles (6.216 km-) (Bue, 1963 in Nelson, 1969).
By 1961, the Great Salt Lake had receded to an
unprecedented low (950 mi-; 2,461 km-) fol-
lowing several decades of drought (ibid.), and
b\' 1971 it had risen about seven feet (2.1 m)
above its historic low, with a surface area of
1,461 s(i miles (3,784 km') (U.S. Geol. Survey,
1971). Powell (1879) considered the lake to be
at its highest level in 1869, which exceeded a
level to which it had long been subjected, and
that its old mean area was 1,820 s(( miles (4,714
km-). A drawing of the lake in 18.50 by
Stansbury (Powell, 1879) is a near duplicate
of the size and shape of th(> lake shown on U.S.
Geological Sur\'ey topographic maps constructed
from photographs taken in 1953. Anthropologi-
cal studies in Utah b\' Antevs (1948) and Har-
per and Alder (in press) and the studies of
Blackwelder (1948) suggest that the lake prob-
ably was subjected to fluctuations in size many
times prior to written history; this will be taken
up in more detail imder a separate heading.
Despite these periods of drought and their
corresponding changes in aquatic habitat, the
44
BmciiAM YouNo University Science Bulletin
peregrine persisted until the late 1950s. Although
the relationsiiip between the changes in climate
and coneoiiiitant ilnetuations in tlie size of the
lake and the effects of these changes on peregrine
populations of the area may never be fully un-
derstood, it is clear that never before had these
populations been so adversely influenced by the
actixities of man as in the past century.
Data from Utah Lake also do not seem to
fully support Nelson's (1969) hypothesis. Data
on the fluctuations of water surface and com-
promise le\els have been plotted for the period
1883 to 1960 (from several sources, including
Bureau of Reclamation and Utah State Fish and
Game). The lake oscillated around the compro-
mise level (4,488.95 ft; 1,. 368.2.3 m) between a
plus and minus five feet (1.5 m) through 1925.
Between 192.5 and 19.30, the lake remained
around the minus five-foot (1.5 m) level, and
starting in 1930 the lake level gradually lowered
to its lowest level, slighth below minus 10 feet
(.3.0 m), in 19.34 and 1935. There was a slow
regain, remaining near the minus five-foot ( 1.5
m) level through the mid-1940s, until it reached
above the compromise le\el in 19.52. However,
the lake has remained below the compromise
level since then. At its lowest level ( 1934-35)
about .37 percent of the surface area was lost
(data through D.A. White from the Utah Lake
Research Shition). PresumabK many marshes
around the i-dgc- of the lake dried up during
this low period^ thereby reducing shorebird and
water bird habitat. However, this may not be
a totally satisfacton' index to the availability of
marshes. Man\- areas fomierly covered by water
l)ut appareiitl>- dr\ during the low water years,
such as Provo Bay, were fed b\ springs and
doubtless maintained some habitat for the prime
avian pre\ species. Some of these areas were
situated opposite acti\-e peregrine eyries. Thus,
tlie impact of tlie drought \ears on peregrines
is difficult to evaluate. Even so, it is clear that
it was not until well after the drought years
and after the 19.50s that some of the eyries
around Utah Lake became inacti\e (Table 1,
sites 17 and 18, for example).
As mentioned earlier, tlie nunilxT n) pere-
grines wintering in the marshes adjacent to
the Great Salt Lak(> declined steadilv from 1939
(;><0.01, linear regression analysis), the vear
Nelson ( U)69) located his first e\ ries in Utah,
until the early 1960s when tlie species disap-
peared as a resident in tlie iiiaishes (Fig. 1 \). The
decline correlated closely in tiiiu- with the aban-
dcmment of local eyries. The desertion of some
e\ries during the early 194()s and perhaps earlier
in the centun' is explainable on the ba.sis of Nel-
son's (ibid. ) cliniatie change hypothesis. How-
ever, the magnitude of the decline which fol-
lowed later in the decade and on into the late
195()s is not, since management methods by then
iiad brought about stabilit\ to the marshes and a
concomitant increased population of prey spe-
cies. If climate had been the sole cause of the
decline in Utah, one should have expected the
reactivation of e\ries b\- the early 1950s fol-
lowing the development of the migratory water-
fowl lefuges in Utah, yet this did not happen.
( Additionalh', a reported increase in nesting
peregrines since 19.39 in Arizona at the expense
of tlie Prairie Falcon is still unexplained [Phil-
lips, Marshall and Monson, 19641.)
We do not ciuestion thi' \alidity of Nelson's
(op. cit. ) climatic change hypothesis for Idaho
and elsewhere in the Northwest, where peregrine
food producing marshes and waters disappeared.
We do believe, however, that the more penna-
nent nature of the Great Salt Lake marshc^s great-
l\- lessened the impact of these climatic changes
in Utah, resulting in the abandonment of a few
marginal e\ries (Table 1, sites 11 and 25) that
were situated near smaller and less pemianent
marshes or that were located on small, relative-
l\ accessible cliffs. Howe\'er, the number of
e\ries, if anv, that disappeared prior to Nel-
son's (1969) 19.39-1948 observations in Utah is
not known. Furthermore, a 10-year reversal of
the prolonged drought of the preceding half
centurv \\'hich purporti'dl\ caused the peregrine
decline has not \et resulted in an appreciable
recolonization of old e\ lie sites or the estab-
lishment of new sites.
Nelson ( op. cit. ) also suggested that Utah's
peregrines ina\- have made altitudinal adjust-
ments during periods of drought to compensate
for the changes in climate. Our data show no in-
ilication whatever of shifts in the species nesting
populations from lower tn higher elevations
(see Table 2). On!\ one known eyrie (site 36,
Table 1) and two suspected e\ ries (sites 27 and
29, Table 1) in I'tah weii' above 6.000 feet
(1,829 m) in elexatioii. Two oi these were
known earlier in the eentun (early 1900s and
middle 19.3()s). whereas the third is of more re-
cent iibseixation in an area that was not investi-
(fated l)i(ili)L;ieall\ earlier in the eentur\'.
Pesticide Ilvpothesis for Peregrine Decline
Pesticide Si/;u/ro(»ic in Utah Fere<irines
Because climatic change did not appear to
be the complete answer to the peregrine decline
in Utah, we hav<- investigated th(> possibility
tli.it pesticides max ha\-e been iinohed during
the later stages oi the decline.
Biological Series, Vol. 18, No. 1 Pehegiune Falcon in Utah
45
Abnomial boha\ior and increased reproduc-
tive failure were recorded at several Utah e\rii's
durins; tlie period follo\vin<j; World War II
(Table 1).
As mentioned earlier, the birds at site 7 in
the Wasatch Mountains either failed to lay in
1949 and 1950 or if they laid, their eggs were
destroyed and the adults showed little inclina-
tion to defend their nests during these years. In
1951 the eyrie contained three eggs, but they
disappeared one b\" one over a 17-da\' period,
and in 1952 the nesting female at the e\'rie was
a ni'w one ( see Table 7 ) .
A pair of peregrines at an eyrie which was
located several miles away (Table 1, site 13),
reacted similarK' when they were first observed
on 20 Ma\ 1951. An adult male and immature
female dived at us onh- halflieartedly once or
twice, otherwise they circled, screamed, or just
perched. A third falcon which flew by at this
time elicited no response from either bird. A
pair was seen there again on 1 June 1952 by
R. J. Erwin. Although they apparently had no
eggs. the\' responded more nomially to human
intrusion than the\- had the previous year.
The occurrence of immature females at these
two evries suggests the possibilit)' of a break-
down in the nonnal ratios of adult to immature
peregrines during the early 19.50s. The two
aforementioned eyries were visited again by us
in 1961, but no falcons were seen.
One of the four eggs in a Great Basin
desert evrie (Table 1, site 4) was partially caved
in on one side and contained a small hole about
one-fourth inch ( 0.64 cm ) in diameter when the
nest was first located on 13 May 1954. The male
was not seen at this time, but the female dis-
played little if an\' of the expected aggressive-
ness toward our intrusion (Porter, et al., unpubl.
ms). When the evrie was next visited on 24
June, only one voungster was present, and both
adults screamed incessantlv at the observer. The
e\rie was still active in 1954 (White). It was
last observed to be active in 1957 or 1958 by a
local falconer, who trapped the adults after a
complete clutch of eggs was said to have dis-
appeared.
White and Lloyd (1962) found two freshly
killed peregrines, about 28 days old, at an eyrie
in the dissert of the Colorado Plateau (Table
1, site 28, Figs. 9 and 10). The two young were
located near their nest, 70 feet (21 m) from the
top of a 4(X)-foot (122 m) vertical cliff com-
posed of smooth Navajo sandst(jne on 7 July
1961. The back, portions of the thoracic organs,
and parts of the neck and wings of each had
been eaten. Thev attributed the death of the
two \oung to predation bv a Ringtail (Bassaris-
cus astiitus), because of the presence of fresh
Ringtail scats along the ledge and because of the
nature of the wounds on the young.
When next \'isited on 6 Jul)- 1962, the adults
screamed, using the "wailing" call described
by Hagar (in B^ent, 1938). The female then left
the area, while the male flew back and forth
but remained silent. The following year both
adults were present, but they remained perched
and made no noise. Only one adult was seen
in May 1964 and none in May of 1965.
Later, White re-examined the Noung pere-
grines, which had been preserved (Univ. Utah
collection) and could find no chewed off feath-
ers so characteristic of fox-killed peregrines and
other mammalian predation observed subse-
quent!) by him in the Arctic. Furthermore, the
feathers appear to have been plucked from the
young as though bv a bird, suggesting that their
death may have been the ri'sult of predation by
the parent birds or an avian predator rather than
a mammalian predator. As suggested by Morlan
Nelson (pers. comm., 1971), the deaths of these
two \'oung could have been caused by Great
Homed Owls ( BuJ)o vir^inianus), or some raptor
other than the adult peregrines. (See Fischer
1967, for a more complete assessment of owl
and other avian predation on peregrines. )
The phenomenon of egg breakage and egg
disappearance ma\ not be restricted to the pere-
grine. A Prairie Falcon e\rie north of the Bear
River marshes obser\'ed b\- R. D. Porter, R. L.
Porter, and Jack Hagan on 6 May 1951 con-
tained a single egg which was slightl)' cracked
on the small end. Tlie female was not seen on
the nest, nor did she react defensively towards
her nest. Tlic egg was absent on our next visit
to the nest on 13 Ma^•. Moreover, many of the
Prairie Falcon CN'ries that were present around
the Great Salt Lake were abandoned during
the past two decades, while those farther re-
moved from the marshes, occupied by pairs
living mostly on rodent diets, have persisted.
The pattern of reproductive failure described
here is similar to, and synchronous with, that
associated with the drastic declines which af-
flicted the peregrine elsewhere in the United
States, in Great Britain, and in northern Europe
(Hickev, 1969) beginning early in the 1950s.
The pattern of reproductive failure in Great
Britain, where the documentation is the most com-
plet(\ was characterized b\- a marked increase in
the number of eggs that were broken in the
nests, in the number of eggs that disappeared,
and in the number of eggs eaten by the parent
birds. This pattern was followed by the disap-
pearance of one or both of the adult birds and
finallv b\- the complete abandonment of the
46
BKTciHAM VouNO Univkhsity Sciknck Bulletin
eyries (Ratcliffe, 1958, 1963, 1965, 19671), 1969).
It was determined later that the eggshells of the
peregrine in both Great Britain ( Ratcliffe, 1967a,
1970), and in tlie United States (Hickey and
Anderson, 1968) liad experienced a marked de-
crease in thickness starting about 1947. Ratcliffe
(1967a, 1970), who was the first to recognize
and document this phenomenon, attributed egg-
sliell thinning to the chlorinated h\drocarbons.
These r<>productive abnormalities Iiave been
duplicated experimentalK' in the American Kes-
trel (Porter and Wi<'me\ cr, 1969), the Mallard
(Heath, Spann, and Kreitzer, 1969), and Black
Duck (Ana.s- ruhripes) (Longcore, Samson, and
Whittendale. 1971) b\' giving them low dietaiy
levels of organochlorine pesticides. The mode
of action of these chemicals on avian reproduc-
tion has been investigated (Peakall, 1969, 1970,
1971; Bitman, Cecil, and Fries, 1970), and the
effects of DDT on the structiue and chemistry
of the eggshell are now being studied ( McFar-
land, Garrett, and Nowell, 1971; Longcore et al.,
1971).
Experimental studies which indicate that
DDT dekns oxidation in the Bengalese Finch
(Loncluira striata) (Jefferies, 1967) and also
in American Kestiels ( Porter and Wiemeyer, un-
publ. data), suggest that this phenomenon may
have occurred in wild peregrines as well. The
la\'ing date of th(> first egg in 1952 at eyrie
number 7 (Tables 1 and 7) (29 April) was two
and one-half weeks later than in 1948 (approxi-
mately 11-12 April), and a week later than in
1947 (about 21-22 April). However, this may be
a reflection of the change in females that was
known to lunc taken place at the e\rie in 1952,
or of an adjiistment to ;i change in weather,
rather than to a pesticide-induced delav in ovu-
lation.
Direct mortalit\ of adult birds due to DDE-
poisoning cannot be discfuuited as a factor in the
decline of the peregrine, since Porter and Wie-
mever (1972) have demonstrated that dietary
le\'els of onlv 2.S ppm (wet weight basis) /;,//-
DDE were letlial to S p(ic(>nt ol male cap-
tive American Kestrels after one xcar on dosage.
The effects were most pionounced duiing molt
and immediatelv follow ing nesting seasoTi— a pe-
riod when the fat ev'ele of the kestrel was at its
lowest point. Thev ha\'e also shown (Porter and
Wieme\-er, in preparation ) that kestrels dosed at
both low (0.28 ppm dieldrin; 1.4 ppm DDT)
and high (0.84 ppm dieldrin; 4.7 ppm DDT)
(wet weight basis) dosage levels of DDT and
dieldrin in combination are more susceptibli- to
death following stress of weather than are non-
dosed kestrels.
Residues of Pesticides in Peregrine Prey Species
We will now consider the quantity of or-
ganochlorin(> pesticides in the tissues of some
of the peregrine's pre\' species in Utah, since
many of the principal pre\' of the peregrine are
known to contain high levels of these chemicals.
Cade, White, and Haugh (1968), and Ender-
son and Berger (1968), for instance, determined
that DDT, DDD, DDE, and dieldrin were
present in greater (|uantities in the tissues of
migrant sandpipers than in an\- other of the
peregrine's pre\' species in the .Arctic. Somc^ con-
tained DDE in their tissues in cjuantities of suf-
ficient magnitude* to be cause for concern (see
Porter and Wiemeyer, 1969. and Wiemc\cr and
Porter, 1970). ■
DDE is considered to be the most inimical
to avian reproduction of the metabolites of DDT.
Relatively high DDE residues were present in
the eggs and in tissues of Short-billed Dowitch-
ers {Limnodromus griscits), Killdeer (Cltarad-
rius vociferus), American .\\'ocets and Rlaek-
neeked Stilts in California (Keith and Hunt.
1966). Surprisingly liigh residues of /),//-DDE
( expressed in average and extreme ppm. wet
weight basis ) were found in the eggs ot Black-
necked Stilts (4.92, range 1.0-13.7), American
Avoccts (4.43, 1.5-12.0)', and Franklin's (inlls
(0.92, 0.5-2 2) collected at the Bear River marsh-
es in 1968 (unpubl. data, Dc>nver Wildlife Re-
search Center). The whole bodv tissues ol two
Lesser Yellowlegs (Totaiius flavipes) contained
(m the average 10.95 (range 5.1-16.8) ppm /).//-
DDE (wet weight basis); four Long-billed
Dowitchers {Liinnodromus scoloj)a(cus), 13.25
(0.7-49.20); one avoeet, 3.4; nine Whit(>-faced
Ibis (Plegadis chihi), 2.55 (0.1-6.5); and three
Marbled Godwits (Limosa fedoa), 6.04 (0.1.5-
17.8). Dieldrin in the tissues of these birds
ranged from 0.1-0.86 ppm in the ibis, 0.2 ppm
in the Lesser Yellowlegs, 0.0.5-0.50 ppm in
the godwits, and 0.6.8 ppm in the avoeet. Many
of the DDE values are greater than the 2.8
ppm (wet basis) of l^DE that caused eggshell
thinning ( Wiemc^-er and Porter, 1970) and
adult mortality (Porter and Wiem(>yer, 1972)
in .American Kestrels. Residues of PCB's were
found in foui- of the dowitchers and two of the
\(41owle^s. The\ axeraged 3.75 ppin (1. -5-10.0)
and 4.5 ppm (3.0-6.0), respectively.
Mosiiuilocidc I'sagc in Vlali
The chemical DDT was used as a mos(|uito-
eide in the marshes along the Great Salt Lake
as eari\ as 1947 in Weber (Ogden Ba\- State
Waterfowl Managemc-nt .Area) (Benge and
Fronk. 1970) and Box Elder eountic-s ( K. L.
Josephson. pers. eonnn., 1971 ) and on an experi-
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Ut^vh
47
mental basis in Salt Lake County (Salt Lake
City Mosquito Abatement District) in 1945
(Graham and Rees, 1958). This chemical was
used at Ogden Bay until 1961, at which time
the use of parathion was initiated (Benge and
Fronk, op. cit. ). Davis County probably began
the use of DDT in 1951 or 1952, since mosquito
control was initiated there in 1951 (Stewart,
1954; Nielson, 1962). The quantities of DDT
used in the early \'ears probably were not great,
since it was applied bv means of foggers and
hand-operated sprayers. However, beginning in
1949, DDT was applied to the extensive marshes
bordering the Great Salt Lake by means of air-
craft (for additional history of mosquitocide
usage in Utah, sec Appendix. The utiliza-
tion of DDT increased with the use of air-
planes as a vehicle for application. It is inter-
esting to note that reproductive failure in the
peregrine was most pronounced in the vcars
coincident with, and immediately following, the
initiation of aerial spraying, although this may
be an unrelated coincidence.
Between 1947 and 1961 many thousands of
pounds of DDT were deposited on agricultural
crops, and more importantly, directly on the
marshes and waters in the Great Salt Lake Valley
where nesting peregrines obtained much of their
food. The quantities applied by mosquito abate-
ment districts were greatest along the marshes
of the Great Salt Lake, where no peregrine
eyries are known to have been active after 1957,
and least in Utah County, where several pere-
grine eyries apparently remained active until
the late 1960s.
Data on the (juantities of organochlorine in-
secticides used for agricultural purposes in the
area surrounding the Utah and Great Salt lakes
were unavailable to us, but chlorinated hydro-
carbon pesticides probably were used in large
quantities, judging from a recent surv'ey of
pesticides in Utah (VVarnick, 1971). However,
they were applied to farm crops, farm animals,
and buildings, and not directly on the marshes
where the peregrine obtained its food. Unfor-
tunatelw little is known regarding the move-
ments of these chemicals from agricultural lands
to the marshes.
We have no direct evidence linking these
chemicals with the sharp reduction in active
peregrine e\ries along the Wasatch Mountains
during the critical years between 1945, when
the chemicals were first used, and 1957, when
the species was last known to breed in the area.
Nor do we know the extent of the environmen-
tal contamination at that time bv other chemicals
such as the polvchlorinated biphenyls (PCBs).
We do not know the effects of PCBs on raptor
reproduction, although some PCBs (1245) in
small dietary concentrations do not seem to
affect reproduction in Mallards, Pheasants (Pha-
siantis colcliicus) (Heath et al., 1972), and Ring
Doves (Streptopelia risoria) (Peakall, 1971) in
the same way as does DDE.
We can only speculate regarding the resi-
dues of chlorinated hydrocarbons present in the
tissues of either the peregrine or its prey species
during the period of its decline in Utah. Most
of the peregrine's prey species were migratory in
nature. Thus, part of the insecticide residues
acquired by them were from areas other than
Utah and the Great Salt Lake valleys. We are
unable, therefore, to establish an absolute cause
and effect relationship between the quantities of
chlorinated hydrocarbons used and the decline
of the peregrine in Utah, although one is sug-
gested by the experimental, ecological, and be-
havioral evidence which we have presented.
Disease Hypothesis for Peregrine Decline
White (1963) referred to 27 cases of botu-
lism (Clostridium botuJinum) in peregrines that
were found in the Great Salt Lake marshes be-
tween 1943 and 1958. Ralph B. Williams (pers.
comm., 1972) also found several affected pere-
grines on marshes around Utah Lake in the
mid-1940s. The disease was most prevalent be-
tween late July and early October, and it ap-
peared to affect adults more than young, and
females more than males. Botulism undoubted-
ly has taken its toll of peregrines during the
past several decades and perhaps, sporadically,
for many hundreds of years. Its effects, histori-
cally, on the local peregrine population cannot
be assessed because the fluctuations in numbers
of active peregrine eyries in Utah are not known.
We cannot evaluate the effects of botulism tox-
ins combined with those of pesticides, since
knowledge of the effects of pesticides on the
susceptibilit)' of birds to various diseases and
the interactions of botulism toxins with the
chlorinated hydrocarbons arc poorly understood.
However, any mortality of adult birds due to
disease during periods of reproductive failure
would tend to accelerate the decline.
Human Activity Factors in the
Decline of the Peregrine
A number of human activities, besides the
agricultural practices already mentioned, may
have adversely affected the peregrine in Utah,
particularly in combination with the inimical
effects of organochlorine pesticides, botulism
poisoning, and changes in the climate. (See an
48
Bricham Young University Science Bulletin
earlier analysis by White (1969b) of tlit- effect
of human pressures. )
The impact of nest robbing, which started
earlier in the centurv with egg collecting and
later in the centur\-, starting about 1939, with
the utilization of the nestlings for falconry, are
difficult to evaluate, although there is no evi-
dence that these activities per se were respon-
sible for the sharp increase in abandoned eyries
in the state. Some peregrine eyries in Europe
were robbed of their young for many hundreds
of years without apparent harmful effects ( Fi-
scher, 1967; Ratcliffe, 1969).
Photography at eyrie sites also may have
caused some birds to abandon their eyries, al-
though to our knowledge onl\' one nest in Utah
(Table 1, site 7) was harassed in this way and
the eyrie site was known to have been active
subsequently.
The reported collection of an adult falcon
from the Pelican Point eyrie (Table 1, site 3)
in 1935 (Bee and Hatchings, 1942) apparently
had little impact on this eyrie, since it was still
occupied as late as 1939 (notes of R. G. Bee).
The removal of the adults from evrie site 4
(Table 1) in 1957 or 195S b\ a falconer probably
hastened the abandonment of that eyrie by only
a few years, since what seems to us to have been
the pesticide syndrome was already in strong
evidence there.
The cliff at Pelican Point (site 3. Table 1,
Fig. 6) became a limestone quarr\' in recent
years and the evrie site was destroyed, as was
an eyrie site in southwestern Utah (site 37,
Table 1). Lower portions of the cliff near one
of the most inaccessible peregrine e\ries in the
state (Table 1, site 8) were blasted away dur-
ing tlie 1960s. .Some of the earlier observations
of peregrines in Utah were near this site. A bird
was noted there in 1969 ( C. M. White), but not
in 1971 (R. J. Erwin).
A recreation area, establislicd after 196(S, is
situated below one eyrie in east-central Utah
(Table 1, site 2S). When the e\rie was visited
in Mav 1971, several motore\cle clubs were us-
ing the area as a point of rendezvous and all
day and night the roar of motorcycles echoed
through the can\()n. Although fresh excreta
was seen along a ledge nnming adjacent to the
old e\rie site, no falcons were seen in two da\s
of observations. This eyrie had shown evidence
of the pesticide syndrome as early as 1961, how-
ever. The extent of the damage to the above
site is not known.
Depredation oi the species 1)\ hunters is a
mortality factor which is frequently overlooked.
Utah's marshes, which in the past were fre-
(juented b\ peregrines in the fall and winter,
have been used by increasingly greater numbers
of waterfowl hunters in recent years. This is es-
pecialK true of areas around the Great Salt
Lake since the establishment of state and federal
waterfowl refuges between 1930 and the early
1940s. Often hunters kill raptors and other birds
indiscriminatelv. This could be a contributory
factor to the peregrine decline, since peregrines
fre(iuenting the marshes during hunting season
probably were from local eyries. However, the
significance of depredation by hunters is diffi-
cult to assess since the peregrine is noted for
its abilitN' to withstand this type of persecution
and destructive treatment bv man (Ferguson-
Lei's, 1957; Cadc>, White, andHaugh, 196S; Rat-
cliffe, 1962, 1969).
In the past two decades, the construction of
human dwellings on the high foothills of the
Wasatch Mountains below certain eyrie sites
may have had an adverse affect on these eyries
(sec White, 1969b), and the effects of the activi-
ties at a nearby rifle range on one such eyrie
also ari' unknown. Oni' can only spcx'ulate what
the construction of homes near eyrie sites will do
to these sites, since there is already a precedent
set for peregrines nesting above railroad tracks,
on bridges, and in heavilv populated urban
centers (Hicke), 1942; Olivier, 19.5.3). The ex-
tent to which some individuals of the species
persist, despite the presence of human popula-
tions near their e\ries, is illustrated b\' the pere-
grines at one e\ rie that tolerati-d for o\-er a
centurv the acti\'ities of a \ illage of two hundred
peopli' at tlie base of the cliff th;it housed the
falcon evrie (TTiekey. 1942).
To sum up, pollution, shooting, nest site
and hiibitat destruction, human disturbance, and
climatic changes ha\i' contributed singlv and
jointK' to the near demise of the peregrine in
Utah. Of these, ]Dollution ;md climatic change
appear to have played the dominant roles.
FACTORS INFLUENCING PEREGRINE DISTRIBUTION AND ABUNDANCE IN UTAH
To more lull\ understand tlu' various fac-
tors involved in I lie distribution of tin- peregrine
in Utah prior to its catastrophic decline, we ha\('
.ttteniptcd to examine the impact on tlu' species
of \arinus ecological factors, both past and
present.
Biological Series, Vol. 18, No. 1 Peheghine F.alcon in Ut.\ii
49
Water, Food, and Nesting Sites as
Limiting Factors
Bond (1946) lias reported that in the west-
ern United States tlie peregrine seldom nested
more than one half mile (0.8 km) from
uater in which to bathe. Exceptions to Bond's
( ibid. ) observations are icw. Gabrielson and
Jewett (1940), for example, tell of a pair that
nested in Oregon on an isolated rock far from
water ( 11 mi.; 17.7 km., Bond, 1946), and Tliom-
as Ra\' (pers. comm. ) located an active eyrie
far from water in arid western New Mexico.
The peregrine's affinit)' for free water prob-
ably is associated more uith its needs to bathe
and to obtain food than \\ith its needs to drink.
Bartholomew and Cade (1963) point ont that
the larger predator^' birds obtain adecjuate quan-
tities of water from their food under most cir-
cumstances. They cited instances of several fal-
cons, including the peregrine, maintaining
weight for man\ months without free uater.
Beebe (1960) concluded that because 11
of 1.3 young peregrines taken from nests in the
Pacific Northwest and raised in Denver died
of deh\ dration, humidit\' rather than nearness of
free water was perhaps a critical factor in brood
success in areas of the West other than the
Northwest Pacific coast. Since these nestlings
died despite ha\'ing been supplied with drink-
ing water, Beebe (ibid.) Inpothesized that pere-
grines were more or less restricted to nesting
sites near water because of high humidit\' rather
than the presence of free water.
An important cjuestion appears to be whether
or not the young mentioned by Beebe were ac-
climatized to tht' cool, humid climate of the
Northwest before being transferred to the arid
intcmiountain area. Nelson (pers. comm., 1971)
has suggested that these birds may have died
of malnutrition rather than dehydration. He
raised and trained one of them and encountered
no difficult\- uith deln dration. Other nestling
peregrines from British Columbia and the Aleu-
tian Islands, similarly transferred to Utah, have
not been affected in this manner. Nestlings
taken from Utah evries have not appeared to
suffer greatl)' from delndration nor has there
been any evidence of moisture loss among young
peregrines cared for in the nest ])\' their parents.
This affinity for high humidit\-, if it exists,
mav be an inherited physiological characteristic
of the pealei race, which is less pronounced in
the peregrine populations of the arid Intennoun-
tain \\'est (see also. White. 196Sb, for further
documentation of this problem). Furthemiore,
other populations of falcons, such as those of
the Shaheen, exist and breed in the deserts of
the Middle East under the harshest conditions
known (Bartholomew and Cade, 1963).
Food availability appears to be a major cri-
terion influencing the distribution and abun-
dance of the peregrine in arid regions of the
West. Density and distribution of peregrine
populations in Utah appear to correlate best
with the abundance of the food supply. Pere-
grine populations are most dense in the area
surrounding the Utah and Great Salt lakes
where the preferred prey species, particularly
shorebirds and marshbirds, are most abundant.
Here, the marshes have historically supplied
food for 10 to 20 eyries during a single nesting
period. Hunting areas for isolated pairs of pere-
grines elsewhere in the state were supplied by
smaller, less extensive marshes or by narrow
tongues of streamside vegetation. Usually, iso-
lated pairs survived and reproduced where ade-
quate food was available.
Food availability apparcnth' is an important
factor in the distribution and abundance of the
peregrine in more humid and mesic regions as
well as in arid regions. Beebe (1960) has at-
tributed an unusually high breeding density of
peregrines in British Columbia to the extremely
high concentrations of four or five species of
colonial seabirds occurring there. These small
pelagic birds apparcnth' were especially suited
as pre\' species for the peregrine.
Ratcliffe (1962) considered the geographic
variation of food supph' as the most obvious
factor associated with population density of
the peregrine in Great Britain. He has correlated
size of territory and density' of peregrine popula-
tions in Britain with the nature of the food
supply.
The same factor generally appeared to be
operative in Utah, although peregrine density
in the Great Salt Lake Valley of Utah probably
was not limited by the size of the prey popula-
tions. However, the species may be limited by
the distance (up to 17 mi, 27.4 km; Table 4)
it must fly to reach the marshes where it obtains
its preferred prey species.
Peregrines ma\- select easily accessible nest-
ing sites in areas containing an abundance of
suitable prey species, as occurs in the Queen
Charlotte Islands (Beebe, 1960). Such sites are
seldom utilized in areas containing less favorable
food supplies. This is illustrated in Utah by the
occurrence of the ground-nesting peregrines at
Ogdcn Ba\'.
Hick(>\- (1942, 1969) considered the cliff on
which per(>grines nest as the dominant feature of
their ecological niche. He considered extremely
high cliffs as "ecological magnets" which at-
tract peregrines regardless of nesting success.
50
Brigham Young Univkhsity Science Bulletin
Cade (1960), on the other hand, has argued
that the ability of the pair to breed effectively
is a result of a strong pair bond, and that the
strength of the bond is a more important con-
sideration than the size of the cliff. He argued
that the pair bond would be dissolved and that
the evrie would become inacti\e indefinitely if
both the male and female disappeared from the
eyrie. Ratcliffe (Hickey, 1969), in support of
Hickey (1942, 1969), has cited examples of
several eyrie sites which were consistently reoc-
cupied following the deaths of both adults. This
also has been noted in the Arctic b\- White ( un-
publ. data). (See Fischer, 1967 for additional
documentation. )
In Utah, selection of e\rie sites by pere-
grines is associated with the avai]abilit\' of suit-
able sites near a readily available supply of
preferred prey species. The preferred prey spe-
cies usually are closely associated with a marsh
or stream. These two factors combined, then,
constitute the most important aspect of the pere-
grine's nesting econonn in the state.
Interspecific Competition During
Nesting Season
Cade (1960) has discussed competition be-
tween the jieregrine and the Cvrfaleon (Falco
riisticohis). White and C:ade (1971) have dis-
cussed competition among several species of
raptorial birds in the Arctic, and White (1968b)
has discussed this problem as concerns peregrine
distriliution and its relation to large congeners
over broad distributional areas. These papers
give a valuable basis for the evaluation of the
competition between the peregrine and other
raptors whose range and habitat in Utah are
svmpatrie. In our discussion of interspecific
competition, we prefer the more restricted defi-
nition of the tenn "interspecific competition"
as given b\' Birch (1957) and as discussed by
Cade (1960). Tliat is, competition results when
more than one species re(|uires a resource that
is in short supply.
Competition for food and/or nesting sites
between the peregrine and other species of rap-
tors, particularls' the Prairie Falcon and the
Golden Eagle, ma\' be factors contributing to the
relati\'e paucity of peregrines in the arid Inter-
mountain West.
Where relati\-el\- abundant, the Colden EagU-
ma\' be a eoinpetiti\e factor limiting the density
of the peregrine in the more arid regions of
Utah. Bond (1946) has watched the peregrine
strike at Golden Eagles and R. J. Erwin and J.
F. Poonnan (impubl. notes) have made a simi-
lar observation in Utah. Dixon (19.37) tells of
one instance when a pair nt Golden Eagles in
California usurped a cliff that had been occupied
by peregrines for years. Tlie eagles persistently
outfought the peregrines, forcing them to leave.
Cade ( 1960 ) found that the peregrine was quick-
er and more persistent in its attacks on Golden
Eagles than on any other raptor discussed. Rat-
cliffe (1962, 196.3)' reported that in man\- dis-
tricts in Scotland, where there is a surplus of
suitable cliffs, the densit\' of Golden Eagles is
high while the densities of the peregrine and
the Common Raven (Corviis corax) are low. In
these situations apparently the eagle replaced
the peregrine as the chief nesting predator in the
Scottish Highlands.
In Utah, peregrines and eagles were found
nesting concurrentK' on the same set of cliffs
only once. The eagles nested one mile ( 1.6 km)
(Morlan Nelson, pers. comm., 1971) from ac-
tive peregrine and Prairie Falcon eyries (see
Nelson, 1969), but on the opposite side of the
mountain (north). Tlu- eagles apparentK' foraged
northwardh , while the peregrines foraged south-
wardly. No aggression was noted between the
eagles and the falcons (Nelson, pers. comm.). A
cliff formerly occupied b\ peregrines in Utah
(site 15, Table 1) contained an active Golden
Eagle's nest in the spring of 1971, and the pres-
ence of two old eagle nests ( R. J. Erwin) sug-
gests a long period of occupancy bv the eagles.
The cliff also had been occupied b\' as man\- as
tliree pairs of Prairie Falcons simultaneously
during some oi the intervening \'ears (Nelson,
pers. cdinm., 1971).
The food habits of the eagle and peregrine
are sufficicnth' diverse in Utah so as to negate
a strong competition for food. Additionally, the
eagle seems to attain its greatest abundance in
the more arid regions of the state, wIktc it more
liki'K' would compete with the Prairie Falcon
for nesting sites than with the peregrine, al-
though the abundance of eagles in the deserts
of Utah may be one of the reasons whv the
piTegriiu' seldom occurs there. This latter postu-
lation, liowevi'r, appears unlikeK' because of an
absence of the ft)od niche preferred b\' the
peregrine.
The Common HaNcn lias lieen shown bv
White and C^ade (1971) to compete rather ex-
tensiveh with G\ rfaleons for nest sites in the
Arctic, though it seems to ha\e only limited
competiti\e effect on Arctic peregrines using
the same cliffs. In Utah, where the raven is com-
mon, onK three cliffs with peregrines were
known to house ravens. Like the situation in the
.Arctic. ra\('ns probably had "no" effect on Utah
peregrines, although Porter observed peregrines
at site number 4 pursuing ravens on 8 .April
19.51 |{;i\(iis ina\. howe\('r. h.ivc a considerable
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
51
modihing effect on Prairie FaIcon.s, a.s wall be
discussed in a later section. ( See also Ratcliffe,
1962, for a c-onsideration of raven-peregrine in-
teraction in Great Britain. )
The Prairie Falcon ( Fig. .39 ) , on the other
hand, is more closeh' related plu'logenetically,
is more similar in size, and is more equivalent
in ecological function to the peregrine, than is
cither the eagle or raven. Hence, it likely would
be a more serious competitor of the peregrine
and it probabK would be a more important
factor limiting peregrine populations in areas
of sympatr\'.
The Prairie Falcon is a true desert falcon.
It undoubtedly evolved in the arid West, and
therefore is probabK- better adapted than is the
peregrine for Utah's arid environment. The Pere-
grine Falcon is separated from the Prairie Falcon
and the Cyrfalcon at the subgeneric level. The
two species are of similar size, although the
peregrine is somewhat heavier than the I-'rairie
Falcon (Sei' Table 9 and Webster, in Beebe and
Webster, 1964).
The peregrine, which is nearh' cosmopolitan
in its geographic distribution, has a breeding
range which completely overlaps that of the
Prairie Falcon geographicallv but not ecologi-
callv. The Prairie Falcon breeds from central
British Columbia, southern Alberta, southern
.Saskatchewan, and North Dakota, south t(j Baja
California, and northern Mexico (Sec AOU
Checklist of N. Am. Birds, 1957). The pere-
grine is most abundant north of its zone of svm-
patry with the Prairie Falcon.
According to Bond (1946), the Prairie Fal-
con ma\' be quite common up to 6,000 or 7,000
feet (1,829 or 2,1.34 m) in suitable localities and
at elevations where trained Prairie Falcons, with
their much greater surface to weight ratio, clear-
ly outflv trained peregrines, which are their su-
periors at sea level. Morlan Nelson (pers. comm.
1971), who has tested Bond's (1946) hypothesis
on several occasions with captive falcons, con-
siders that it is more a matter of individual varia-
tion within both species than it is a factor of
elevation.
Actual contact between the two species oc-
curs where their ecological niches overlap. To
our knowledge, there is no locality in Utah
where peregrines nest which is not also inhabited
bv Prairie Falcons, but not the reverse. The
peregrine's proclivity to nest near water or
marshes where both its food and nesting re-
quirements are met is not shared by the more
euryecious Prairie Falcon which may fulfill these
requirements both near water and in the desert
many miles from water.
As discussed previously, the several pere-
grine e\ries found in the deserts of Utah were
situated within easy access of marshes, desert
springs, ponds, streams, or rivers. Perhaps this
reflects the differences in hunting methods and
food habits of the two species, as well as the
proclivitv of the peregrine to bathe in water as
discussed by Bond (1946) and Cade (1960).
Both species can be dust bathers in captivity
(Nelson, pers. comm.), although the Prairie
Falcon is less dependent on water than is the
Peregrine Falcon.
Some Factors Modifying Competition
and Success
Before examining the kinds of competition
that may affect Utah peregrines, a general dis-
cussion is in order. There are many ways that
falcons can exploit their respective environments.
Their success, that is, the total number of
young that become breeding adults in the next
generation, depends upon the effectiveness of
this exploitation.
Frequently ecologists use the terms "gen-
eralist" and "specialist" to describe a species in
terms of the manner in which it utilizes certain
resources. Most frequently this pertains to the
manner in which the food or habitat niche is
exploited, or to the modes of hunting certain
species of prey.
Although the specialist has a narrower habi-
tat tolerance, it usually compensates b\' being
more competitive (see, for example. Cade,
Table 9. Weights ( in gram,s ) of Peregrine Falcons and Prairie Falcons from various North American populations.
Species
and
MALES
FEMALES
Population
n
X
range
n
X
range
PEREGRINE FALCONS
(White. 1968a & b)
F. p. tundrius'
F. p. anatumr
PRAIRIE FALCONS'
(Enderson, 1964)
12
5
15
610.9
678.0
554.0
550-647
67.5-682
500-635
19
5
31
952.0
1,038.0
863.0
825-1,094
870-1,201
760-975
'Weights are from adult birds.
-From population in western United States.
52
Bhk;ham Young Univebsity Science Bulletin
1960). When the optimal requirements for the
speciahst are present, it tends to eapitahze on
or "monopoHze" the resources or conditions
to receive maximum benefit, often to the ex-
clusion of the generalist or other specialists. It
is the existence of a specific or optimal set of
conditions that allows the specialist to be suc-
cessful. The generalist might also successfully
exploit the precise conditions. However, because
of competition with the specialist, it may alter
the manner in which it uses the conditions by
partitioning the resource, or it mav be forced
into suboptimal conditions because of the domi-
nance of the specialist. In the absence of the
specialist, the generalist obtains even greater
benefit by the use of the specific combination
of resources or conditions that the specialist
would have used.
The generalist tends to be more widespread
geographicail\' and often more common than
the specialist. Moreover, when two closely re-
lated species with similar ecological niches oc-
cupy the same geographic area, one tends to
assume the role of the "specialist" and the other
th(> role of the "generalist," depending upon
their individual needs. G\'rfalcons, for instance,
are specialists on the Arctic Slope of .'\laska,
where thev have specific nesting requirements
and where thev specialize on ptannigan for food,
while the sympatric peregrine is the generalist,
having rather broad reciuirements for nesting
and feeding (White and Cade, 1971). The
G\ rfaleon seemingK has the adxantage and ap-
pears to outcompcte the peregrine for certain
resources. However, because the peregrine is a
generalist, it has less precise requirements and
therefore is able to occur over a much broader
geographic range in Alaska, such as the taiga
regions. Then, too, it is probabK more numer-
ous when considering its entire range.
Even though the j^eregrine is probably a
generalist o\er much of its cosmopolitan range,
it becomes a specialist in the Aleutian Islands,
where it has a narrower food niche consisting
mostK of marine birds of tlie famih' Alcididae
and of the order Procellariiformes. Thus, the
role of the species is modified In the conditions
in a given localih'.
Prairie Falcons ha\'e been thought of as spe-
cialists liecause the\' are al)le to exploit \('ry
arid climates where a limited number of food
species are present. They often occur where
other large falcons arc unable to survive. Be-
cause they are able to concentrate on the prey
species most a\ailable, Prairie I-'aleons mav have
a ratlier highK specialized food niche, especial-
ly in the more arid regions w^here a limited
number of food species occur. Their abilit\ to
"specialize" on what is a\ailable enables them
to live successfulh' in a wide variety of eco-
logical situations.
If one considers the Prairie Falcon's entire
geographic and ecological range, it is narrowly
selective in its exploitation of the climatic condi-
tions a\'ailablc to it (i.e. a near obligate of xeric
conditions), but it is broadh' selective in its ex-
ploitation of food and n(-sting sites. Additionally,
where the geographic ranges of the two species
o\'i'rlap, Prairie Falcons are much more common
than art" peregrines. Because of the Prairie Fal-
con's seemingly narrow climatic tolerance dur-
ing the breeding season, climate ma\' be a major
factor limiting its geographic distribution.
Peregrines, imlike prairies, are broadl\- selec-
tive in their exploitation of climatic conditions
over their entire geographic range. However,
tlie\' are narrowly selective in their exploitation
of food and nesting sites in the arid West where
the\- must compete with the s\mpatric Prairie
Falcon. Moreover, the\' are much less common
than are Prairie Falcons, where the ranges of the
two species are svmpatric. Their specialized
food rcHiuiremi'nts (generallv "water-t\ pe " birds)
and restrictive methods of capturing pre\ (not
prone to capture prey on the ground), are the
major factors limiting the expansion of their
geographic and ecological ranges in Utah and
probabK else\\here in the arid West.
The presence of surface water in the arid
West ma\' dramatically alter the environment.
For certain species it may even act as a limiting
factor. Water creates a food niche which ap-
parenth is optimal for the peregrine, providing
an abundance of aquatic birds in these local-
ized areas. Hence, the peregrine does better in
the presence of surface water. This is especially
evident at the margin of the species' ecological
range in the arid parts of Utah. With the pres-
ence of these "oases" of acjuatic habitat in an
otherwise unexploitable enxironment, the pere-
grine assumes the role of specialist: and, where
the peregrine and piairie occur together in Utah,
the prairie seemingK' assumes the role of the
"generalist." The broad spectnmi of food, habi-
tat, and nesting sites which the prairie selects
overlajis and surpasses the reciuirements of the
peregrine. The requirements of the peregrine are
more limited and restrictive, \ I't it may do bet-
ter competitiwlv than its congener when the
optimal conditions pre\ail.
(Competition \\ itli the Prairie I'alcon for Food
Where the two species occur together along
the escarpment of the Wasatch Mountains and
adjacent to the Croat Salt Lake, their food ap-
Biological Series, Vol. 18, No. 1 Peheghine F.\lcon in Utah
53
pears to be quite similar (Table 5), although
there are some marked differences. In this re-
gion of joint occupancy, the Prairie Falcon uti-
lizes a much wider \arictA' of vertebrate species
than docs the peregrine. As illustrated in Table 5,
the Prairie Falcon is more prone to feed on ro-
dents and on ground-dwelling birds, such as
([uail, pheasants, meadowlarks, and passerine
l)irds in general, and is less inclined to feed on
pigeons, doves, and flickers than is the pere-
grine (also see Bond, 1936a, b, and c).
Prairie Falcons also feed on reptiles. For in-
stance, at one Prairie Falcon eyrie in the Great
Basin, not far from a peregrine e)ric, adults
were observed carrying large whiptail lizards
( Cnemidophorits sp. ) to the eyrie.
The Prairie Falcon exploits a different food
resource in thi- allopatric parts of its geographic
range than in those that are sxmpatric with the
peregrine. A case in point is the high plateau
countr\- of Utah NNW of the Uinta Mountains
( 6,800' feet ele\ation; 2,073 m ) where only the
Prairie Falcon occurs, although one would expect
peregrines also to occup)' the habitat. Food
items taken from several nests between 1961
and 1964 in this region of allopatry consisted
of 61 percent mammals, about 90 percent of
which was the Uintah Ground Squirrel ( CifeUus
armatus), although another species of ground
squirrel, a chipmunk {Eiitamias sp. ), and a vole
(Slicrottis sp. ) also occurred. Birds made up
the remaining .39 percent, with Mourning Doves
being the principal avian food, though the Brew-
er's Blackbird (Euphaniis aianoccpJwhis). Flick-
ers ( Colaptcs sp. ), Horned Larks, Starling (Sfi/r-
ntis vidp^aris). and the Mountain Bluebird {Sialia
cttrrticoidcs) also occurred. Thus, about 75 per-
cent of the total food uas made up of t\\'o spe-
cies, one mammal and one bird. In this case, and
those cited bv Enderson (1964), with an ab-
sence of peregrines in both localities, the Prairie
Falcon tended to fill the role of a "specialist" in
food habits; and to a large extent the species
was mammi\-orous (mammal-eating). (See
Bond, 1936b). The avivorous (bird-eating)
peregrine, on the other hand, consumes few
mammals and fewer, if any, reptiles.
Ground-nesting birds and rodents are im-
portant items in the diet of the Prairie Falcon in
areas other than Utah. For example, Enderson
(1964) found remains of the ground-nesting
Horned Lark and of the Richardson's ground
sc|uirr(>l (Cifelhis richardsonii) most often, and
sometimi's exclusi\el\-, in the nests of Prairie
Falcons in eastern W\oming and Golorado. Og-
den (1971) considered the Townsend's ground
sfiuirrel (CiteUus fotcnsei-tdi) to be the most
important food species, followed by Homed
Larks, Meadowlarks, and whiptail lizards in
Prairie Falcon eyries along the Snake River of
southwestern Idaho. The antelope ground
squirrel (Citcllits Icucurus) was also present, but
in smaller numbers.
The Horned Lark was also a staple item in the
winter diet of Prairie Falcons in Utah and in the
prairies of Wyoming, Colorado, and New Mex-
ico, where it influences the falcon's seasonal
movements and distribution (Enderson, 1964).
An overlap in the food niches of the pere-
grine and Prairie Falcon is evident in the area
along the Wasatch Mountains (Table 5). In
terms of biomass, aquatic birds comprised the
largest categoPi' of prey species in the Wasatch
Mountain eyries of both species, but the\- were
much more predominant in the eyries of the
peregrine than in those of the Prairie Falcon.
The a\ocet was the major aquatic species in
the e\ ries of both falcons (see Frontispiece and
Fig. 39). The importance of the avocet as a
pre\ species of the Prairie Falcon was apparent
also at two e\ries in the Great Basin, northwest
of Great Salt Lake, where the adult Prairie
Falcons brought avocets and Antelope Ground
Squirrels to their young almost exclusively in
1962 (C. M. White, unpubl. data) and commonly
in 1969 (P'att, 1971). This, however, was in the
apparent absence of competition with the pere-
grine.
The presence of the avocet in the diets of
lioth species is probabK- a reflection of the local
abundance of this shorebird and the ease with
uhich it may be captured. The avocet likely
did not represent a resource in short supph' and
undoubtedh' was an important item in the diet
of the peregrine long before the first white
settlers arrived in the western United States.
In 1S71 Allen (1872) found it \-ery abundant
along the shores of Great Salt Lake, where he
noted flocks containing several thousand indi-
viduals from 1 September to 8 October, and a
quarter of a century earlier (4 April 1850),
Stansbury (1852) observed innumerable flocks
of long-legged ]ilo\ers, many of which probably
were avocets, Willets, and stilts. The avocet
predated uhite man in the Great Salt Lake
area 1)\ man\' thousands of years, as evidenced
b\' its presence among the bird remains dating
l^aek nearh- 8,500 \ears B.P. in the early strata
of Hogup Gave, just north of the Great Salt
Lake (Harper and Alder, in press).
Tlie White-faced Ibis was an additional
marshbird upon which both species of falcons
apparenth preyed. Wcller 't al. (1958) indi-
cated that the peregrine killed White-faced Ibis
in the Knudson marshes near Brigham Gity,
54
BnicnAM YouNO Univfusitv Science Bulletin
and R. D. Porter (unpuhl. data) ohscrvt-d a
Prairie Falcon feeding on an ibis at the Bear
River marshes on 5 June 1951. Since the ihis
was not found in the evries of either species,
it was prol)ahl\- too heavy for the falcons to
carry to their eyries. The weight of an adult
female ibis as determined by Porter et al.
(unpubl. ms) is 517 grams, whereas the weights
of two adult female avocets average 281
grams.
In Prairie Falcon eyries along the Wasatch
Mountains, shorebirds, passerines, rodents, and
gallinaceous birds were nearlv equally repre-
sented; whereas in the e\ries of the peregrine,
shorebirds predominated and gallinaceous birds
and rodents were absent (Table 5). The ducks
present in the eyri(«i of the Prairie Falcon (Table
5) were about half grown and probably inca-
pable ot (light. Hence, the\ probabK were either
captured on the water or on the ground and
were sufficiently light in weight that thev could
be carried hv the falcons.
We have no data for comparison of the food
habits of the peregrines nesting in the desert
(Table 6) with those of desert-nesting Prairie
Falcons in the same region. A comparison of
this kind is needed to fulh' evaluate the compe-
tition for food by the two species. Cade (1960)
found that the overlap in food species of the
peregrine and Gvrfalcon were least in the areas
of contact and greatest in areas where ranges
were not s\mpatric. A comparison of this kind
between the peregrine and Prairie Falcon would
be difficult to make, since in Utah the Prairie
Falcon occurs in the same geographic area as
the peregrine. Nevertheless, one would expect
,«
^
F"ig. 39. Prairie Falcon feeding its voung a downy avocct (peregrine site 7, alt. prairie site 2, see Fig. 26).
Photo l>v W. 1. Erwin and' IL I). Porter, 1948.'
liroLoc-.iCAL Sf.hies, Vol. 18, No. 1 Pehegrine Falcon in Utah
55
less latluT than more overlap in food habits in
areas of allopatry than in areas of contact. The
isolated jieregrine's evrie in Oregon, which was
situated far from water (Gabrielson and Jcwett,
1940), contained birds usually preyed upon by
Prairie Falcons, and an adult peregrine at an
eyrie in Zion Canyon was observed by Grater to
carrv a squirrel into a crag (Woodbury et al.,
unpubl. nis).
In Utah, then, the Prairie Falcon has a wider
versatility in taking prey species than does the
peregrine, which would seem to lessen the com-
petition between the two species for food.
Hence the role played by the Prairie Falcon in
Utah is similar to that of the peregrine in the
.\rctic (Cade, I960; White and Cade, 1971), and
that played bv the peregrine in Utah is similar
to that of the Gvrfalcon in the Arctic.
According to White and Cade (1971), there is
no evidence to suggest that density of breeding
peregrines is influenced in anv way by availa-
bilits- of food in the Colville valley of Alaska.
This generally is not applicable to the peregrine
in Utah, but in the region surrounding the
Great Salt Lake it is difficult to surmise how the
density of tlic peregrine could have been limited
b\- availabilit\ of food, considering the super-
alDundance of prey species in the Great Salt Lake
marshes. Nevertheless, extensive distances from
(•\rie sites (Table 4) to hunting sites in the
marsh mav have limited their density.
Competition with the Prairie Falcon for
Eyrie Sites
Directional Exposure Preferences
In Utah the peregrine's preference for cliffs
\\ith northerh^ or easterly exposures (Fig. 16)
would tend to lessen the competition for nest-
ing sites between it and the Prairie Falcon if the
Prairie Falcon had a preference for south-facing
cliffs similar to that reported for Colorado and
Wyoming by Enderson (1964). We investigated
this hypothesis by examining the directional fac-
ing of the 49 evrie sites of the Prairie Falcon in
Utah for which we had available data. As shown
in Figure 16, 69.4 percent of these evries faced
south and west and 30.6 percent faced north and
east. This relationship was statistically signifi-
cant at ;)<0.0I (X' test; calculated X- vahu07.37,
1 df). Conversely. 70.4 percent of 27 )ieregrine
evries in Utah faced north and east and 29.6 per-
cent faced south and west, and this relationship
was significant at /><0.05 (X- test; calculated X'
value, 4.48; 1 df).
When the two species nested in close juxta-
position on the same set of cliffs, as at site 7 in
the Wasatch Mountains, the Prairie Falcon
seemingly selected the sites more exposed to the
afternoon sun (west-facing sites) than did the
peregrine (see Histor)' of Nesting at a Wasatch
Mountain Evrie, Table 7 and Fig. 26). As a gen-
eral iTilc, the Prairie Falcon eyries on the escarp-
ment of the Wasatch Mountains were situated
directly on the west face, whereas those of the
peregrine, as discussed previously, usually were
on cliffs in the side canyons with northerly or
easterly exposures. For example, three of the
Prairie Falcon eyries were situated on west-fac-
ing cliffs (see Figs. 26 and 39-42). At each of
these sites, peregrines had been seen in the side
canyons, although not always concurrently with
the nesting of the Prairie Falcon (sites 7, 8, and
16, Table 1). In 1943, a Prairie Falcon nested in
one of the canyons (near peregrine site 16, Table
1), but at a west-facing site in an easily accessi-
ble Red-tailed Hawk's nest.
Morlan Nelson (pers. comm., 1971) noted a
similar orientation between the evries of the two
species at the Ul site in northern Utah (site 11,
Table 1), where he observed the two species in
aerial combat (Nelson, 1969). The peregrine eyrie
was on a ledge facing east and the Prairie Fal-
con evrie was in a pothole (cave-like recess) in
the side of the wt^st-facing cliff, less than half a
mile away (1,320 ft; 402 m; Nelson, pers. comm.,
1971). Potholes probably provide greater pro-
tection from the hot afternoon ra\s of the sun
than do exposed ledges.
These data suggest that both species may se-
lect eyrie sites on the basis of directional expo-
sure to the sun, and that such a preference by
these two species tends to lessen competition be-
tween them for eyrie sites. Nevertheless, this
jihenomenon needs further investigation, both
in Utah and elsewhere, since some studies sug-
gest that the Prairie Falcon in some parts of its
range selects evrie sites on the basis of availabil-
ity of suitable cliffs rather than directional fac-
ing. For example, Leedy (1972) investigated the
directional facing of 49 Prairie Falcon eyries in
Montana during 1970 and 1971 and compared
them u'ith the directional facing of the available
cliffs. He found that 72 percent of the eyries
faced south (33 percent) or east (39 percent), 8
percent faced north, and 20 ]iercent faced west.
Of the 45 available cliffs in Leedy 's study area,
71 percent faced south (31 ]icrcent) or east (40
percent), 7 percent faced north, and 22 percent
faced west— a near duplication of the directional
facing of tlu> eyrie sites. Similarly, Tyler (1923)
reported that most Prairii' Falcon eyries exam-
ined by him in southem California had northern
exposures because in the region where he made
his observations the north ends of the ridges
56
BniGiiAM Young University Science Bulletin
broke off abniptl\' into cliffs that faced north.
Nevcrtliclcss, a few of his e\rics were on west-
facing cHffs; one was on an cast-facing cliff; and
none were on south-facing cliffs.
Height Preference for Cliffs and Eyrie Sites
The I'rairie Falcon in Utah ma\' use nesting
sites of a quality inferior to those normally used
bv the peregrine in Utah. Judging from Bond's
(1946) observations, this ina\' be typical of the
behavior of the two species wherever their geo-
graphic ranges overlap.
Three of nine Prairie Falcon eyries found in
Utah bv Porter and Erwin between 1950 and
1952 were at locations that were easily accessible
to both humans and mammalian predators. Two
were situated in potholes, one of which was lo-
cated onh' 30 inches (76.2 cm) from the base of
a small sandstone cliff and the other was onh-
36 inches (91.4 cm) from the base and 48 inches
(121.9 cm) from the top of an outcropping of
limestone. A third e\rie was located in 194.3 by
R. L. Porter and J. F. Poorman in an old Red-
tailed Hawk's nest that was situated on a small
pinnacle of rock which required no climbing to
reach. One found in 1958 bv F. Welch and G. L.
Richards was on a large rock about 15 feet (5 m)
above the ground and 6 feet (2 m) below the top
of the rock. It probablv could have been reached
by a good climber without the aid of a rope. In
southwestern Utah the Prairie Falcon has nested
in a stick nest in the top of a 20-foot (6 m ) juni-
per tree (Jtmipcnis sp. ) (^^'illiams and Matteson,
1948).
In Utah peregrine evries were a greater dis-
tance from the base of the cliffs, on the average,
than were those of the Prairie Falcon. They were
on higher cliffs, on the average, and the\' were
on relativelv more inaccessible ledges than were
the eyries of their congener (Table 3). Moreover,
the peregrine evries averaged a greater distance
below the brink of the cliff (x= 68.6 ft. 21 m;
range, 2.5-250 ft, S-76 ni; n = i;3) than did those
of the Prairie Falcon (x= 2.5.3 ft, 7.7 ni; range,
4-175 ft, 1-53 m; n = 41).
The average height of the Prairie Falcon e\-
ries in Utah (64 ft; 20 ni) was grc;iter than that
recorded by Enderson (1964) in Colorado and
Wyoming (.34.7 ft; 11.1 m), and less than that re-
ported bv Leedv (1972) in Montana (80 ft; 24.4
m). The average cliff height of 101.7 feet (31 m)
for the Prairie Falcon in Utah is nearly twice
that recorded b\' Enderson (1964) for this species
in Colorado and W\-oining, and iibout 25 feet
(7.6 m) less than that recorded In Leedy (1972)
in Montana. Table .3. which compares the heights
of cliffs and eyrie sites ot the Prairie l-'iileon \\'ith
those of the peregrine, illustrates the difference
in height preferences between the two species.
The more marginal sites, including those on
the smaller or more accessible cliffs at sites such
as 1, 3, 11, and 20 (Table 1), probablv were aban-
doned b\- the peregrine earlier in the century.
Both their sizes and locations made them mar-
ginal sites. Several investigators (Hickey, 1942;
Ratcliffe, 1962) have indicated that the marginal
sites were the Hrst to become inactive following
the advent of earlv settlers.
Eyrie Type Preferences
Till' Piairie Falcon uses a wider variety of
nesting situations than does the peregrine (see
Figs. .39-45). For example, nearly half (45.8 per-
cent) of 72 Prairie Falcon nesting sites in Utah
were in potholes and crevices (Figs. 42-44) in the
face of a cliff, whereas onlv a third of them (31.9
percent) were on an open ledge of a cliff (Fig.
39). An additional third of the e\ries were in the
Fig. 40. Tlic Prairie Falcon eyrie that was .situattii on
.111 old Common Haven'.s {Corvus corax) nest and
was later leelaiined by the raven. Note the ac-
cumulation of fecal material and detritus suggest-
ing that the e\rie Ii;ul been used by the falcons for
a long period of time (evrie site faces southwest).
Photo bv W. D. Porter, 1951.
Biological Series, Vol. 18, No. 1 Pehecbine Falcon in Utah
57
Fig. 41. Raven'.s nest built upon prairie eyrie (shown
in Fig. 40). Photo by R. D. Porter, 1951.
nests of other species of raptors and Common
Ravens, which suggests that these species ma}'
be beneficial to the Prairie Falcon b\' providing
additional nesting sites. Table 10 gives the kind
of nesting situations used bv Prairie Falcons in
Utah.
Sometimes these competitors may preempt
their old nests from the Prairie Falcon. An oc-
Table 10. Percentage use of various categories of eyrie
sites bv Prairie Falcons in Utah ( see photos by
Wolfe, '1928)'
Kind
of
Site
Usage
n
of eyrie types
Percent
Potholes=
26
36.1
Open cliff ledges
Crevices
23
7
31.9
9.7
Stick nests
Red-tailed Hawk's
on cliff face
16
7
22.2
9.7
Common Raven's
on cliff face'
Tree nests
Golden Eagle's
on cliff face
5
2
1
6.9
2.8
1.4
Unknown species
of hawk
Totals
1
72
1.4
99.9
'From unpuliHshed data of authors, ficldnotcs of R. G. Bw. A
B, Boyle, ana R. J. Envin, and from ornithological literature for
the stale.
^Five or 6,9 percent of the eyries were in old ravens' nests lo
(ated witliiii potholes.
'IncliidinB the five that were in old ravens' nests within pot
holes, a total of 10 or 13.8 percent were in old ravens' nests.
currence of this kind took place at an eyrie in
Weber County observed by Porter and Erwin.
The falcons were using an old raven's nest which
apparentlv had been occupied for many vears
bv falcons, since it was almost entirely buried
in excrement (Fig. 40). Without the old raven's
nest as a base, a falcon's eyrie would have been
impossible. When fir'st located on 5 June 1950,
five fully grown young were present in the nest.
The following year the eyrie contained three.
fresh eggs on 7 April. When it was next visited
on 8 Mav, a raven flushed from the eyrie site,
exposing six raven eggs in a newlv constructed
stick nest over the old prairie eyrie (Fig. 41). The
whereabouts of the previous tenants was not de-
termined.
Peregrines apparently were more restrictive
in the selection of their eyrie sites. They used
prcdominantlv open ledges or shelves which usu-
alh were under an overhung portion of the cliff
(See Figs. 26-38). Only two Utah eyries, to our
knowledge, were situated in potholes on the sides
of cliffs [sites 4 (alternate) and 23, Table 1 (See
Fig. 44]. We have no evidence of a beneficial
relationship between the peregrine and other
cliff-nesting species similar to that previously
discussed for the Prairie Falcon.
Both species of falcon apparently prefer to
nest under overhangs. Although our data on the
>--■< V
^5*^
Fig. 42. Prairie Falcon eyrie in crevice on face of west-
facing cliff. Peregrines nested up side canyon (site
8, Table 1 ) . Much of the wood in the crevice was
carried there by wood rats ( Neotoma sp. ) . Photo
bv R. D. Porter, 1951.
58
Bhicham Young Univehsitv Scmknt k Hi'i.letin
Fig. 43. .\ cliff used alternately i)y I'rairie Falcons anil ravens. Nesting site is situated in a pothole similar to that
shown in I'igure 4(1 Cliff is less than 2 miles ( 2.6 km ) from the peregrine eyrie shown in Figure 22, and
this cliff may also have hecn used historically hy peregrines. Photo hx l\. J. Erwin. August 1972.
Prairie Falcon arc incomplete in thi.s regard, all
but one of 36 Prairie Falcon eyries in Colorado
and Wvoming reported 1)\' Ender.son (1964) were
directh' ovcrhinm li\ a |iortioii of tiie clifl.
Size Preference for Nesting Area
The Prairie I'"alcon appears to he less selec-
tive than the peregrine in the size of its nesting
or egg-laying area. White (nnpnbl. data), for in-
stance, ohserved a Prairie I'alcon nesting in a
pothole that was appart>ntl\ too small for a large
family of \()inig because, Ix'fore the vonng had
fledged, all but one were forced from the c\rie
to an unlimelv death on the talus below (Figs.
45-46). This nest was used for fi\e consccutix'c
years. The female laid five eggs each vear and
each vear onl\ one \ onng fledged. The e\Tie was
then abandoned. We have also, however, seen
prairies successfulh' fledge large broods from
ledges e(|ual to or smaller than the site men-
tioned above.
The aforementioned Prairie Falcon e\rie in
Weber Coimt\ that was taken over b\' ravens
liad a total, nesting area of only about 310 sq
inches (2,000 cm'-) (measured from photographs).
A Prairie Falcon e\rie in Box Elder Comity,
found bv Erwin, was in a crevice in the face of
a cliff wiiich was onlv 20 inches (51 cm) wide at
the point whcr(> the eggs were laid. The crc\'ice
was over 80 inches in depth (ca. 200 cm) and
nearlx high enough for a man to stand in (mea-
sured from a photograph).
In the Wasatch Mountains, peregrines usual-
ly laid their eggs on wider ledges with a relative-
Iv more spacious nesting area (fref|uentl\' with
grass on them) than did the Prairie I'alcon. The
area and or volume available for nesting on open
ledges and \\ ithin potholes used as evrie sites in
Utah are gi\en in Tables 9 and 11. The average
available nesting area for peregrine e\ries in
Utah is uearK' tvvice that of prairie cvries (Table
II).
The wider variabilit\' in size and height of the
Prairie Falcon's nesting siti's would appear to be
advantageous to the Piairie Falcon in its eom|)e-
tition with the peregrine. If the better qualit\-
sites were alread\ utilized, one of lesser qualitv.
BiOLOcic.\L Series, Vol. 18, No. 1 Peregrine F.\lcon in Utah
59
Table 11. Size of area available for nesting at Prairie and Peregrine Falcon eyrie sites in Utah."
Types of sites
and
PRAIRIE FALCONS
PEREGRINE
FALCONS
units of measure
n
X
range
n
X
range
POTHOLE SITES
Avail, nest, area
sq feet
5
11.6
8.0 -18.8
-
—
— —
sq meters
5
1.1
0.74- 1.7
-
—
— —
N'olume of potholes
cubic feet
4
20.2
9.0 -43.7
-
—
— ■ —
cubic meters
4
0.6
0.3 - 1.2
-
—
— —
LEDGE AND POTHOLE
SITES, combined
sq feet
sq meters
8=
16.3
2.2 -38.8
7'
27.8
10.0-52.0
8'
1.5
0.2 - 3.6
7'
2.6
0.9- 4.8
kI R, J Envii
'Data were collected between 1943 and 1972 by R. D. Porter, C .M While
peregrine eyrie site 7.
^Two of the eyrie sites were alternate sites at site 7 (Table 1); one was used in common with peregrines.
^Data are from toiu different eyrie sites, including tliree alternate eyrie sites at site 7 (Table 1. figs. 2(i-VI
r.ilile 8 for nuiie detailed data on
and possibly not suitable for peregrines, could
be used, thus giving additional pairs of Prairie
Falcons the opportunity to nest. Prairie Falcons
nesting in the more arid desert areas of Utah
frequentlv use sites which probably would not
be used b\' the peregrine.
Aggressive Interactions between Peregrines
and Prairie Falcons
Nelson's (1969) reported decline in active
peregrine eyries around the Great Salt Lake
probably involved the use by Prairie Falcons of
abandoned peregrine evries (Nelson, pers. comm.,
1971), and as mentioned earlier, the peregrine
also is known to have occupied an eyrie which
earlier in the ccntur\ was used by Prairie Fal-
cons (see White, 1969b).
No direct competition between the two spe-
cies for nt>sting sitt^ was recorded during the
\ears that the earlier mentioned Wasatch Moun-
tain evries (Table 1, site 7) were under observa-
tion by Porter and Erwin, despite the fact
that the e\'rie sites were only about 300 feet (91
111) apart (Figs. 22 and 23), and that the pere-
grines frequenth- flew within 100 yards (91 m)
or so of the prairie's evrie. Neither of the eyries
were visible from the other (see Fig. 22). White
and Cade (1971) found peregrines and Gyrfal-
cons nesting on the same cliffs simultancousb
and succc>ssfully. They postulated that perhaps
peregrines and Gvrfalcons can coexist in close
ju.xtaposition if their nests are not visible to one
another and if their schedules or routes of going
to and from their nests to hunt are different.
Other instances of amicable interspecific co-
existence between the peregrine and the prairie
have been reported. Bond (1946), for example,
tells of the two species nesting peaceably on!\ a
few hundred feet apart. Pettingill and Whitney
(1965) noted the nesting of a pair of peregrines
and prairies 400 yards (366 m) apart in South
Dakota without apparent conflict. French (1951)
found the tvvo species nesting 200 )ards (183 m)
apart, but not in view of each other. He watched
the peregrines attack the prairies at least three
times, but only during one of several visits to the
eyrie. It is possible that his disturbance of the
prairies at their eyrie helped provoke the attack
by the peregrines. Lanner Falcons {Falco biara-
Fig. 44. Cliff in Great Basin desert (site 23, Table
1 ) . Peregrine eyrie was situated near the horse-
shoe-shaped depression, "pothole," at the center of
the cliff indicated by arrow. Photo by R. J. Erwin,
August 1972.
60
HiiiGHAM Young Univehsitv Science Bulletin
Fig. 45. Prairie Falcon cvrie in pothole on side of
sandstone cliff. Photo hv Gar\- D. Llovd and C. M.
White, 1958.
inicus) and peiegiint's in Sicily have been re-
ported b\' Mel).s (in Fischer, 1967) to nest only
50() meters apart w itli no apparent conflict chn-
ing the nesting period.
On the other hand. Nelson (1969) watched a
pair of Prairie Falcons in aerial comliat witli a
pair of peregrines in Utah near the nesting site
of the latter (Tal)le 1, site 11); the two pairs
nested about one-fourth mile (402 m) apart (Nel-
son, pers. conim., 1971). In discussing the aerial
battles between the two species. Nelson (1969),
indicated tliat the Prairie Falcons seemed to win
them. Later in the paragraph he writes, "The
battles were not definite and alwaws ended in
sort of a draw, with observers deciding that the
Prairie Falcons won." lie also noted that al-
though the Prairie Falcons iiad command of tlie
air, when the two species parted the\' returned
to their respective sites. Hence, he did not con-
sider the aggression to result in the abandon-
ment of cvrics b\- cither species. Webster (in
Bcebe and Webster. 1964) gives a vivid account
of an aerial attack in Colorado bv a female I'rai-
rie Falcon on a peregrine presumabb cariv ing
food to its \oimg in which the Prairie Falcon
roblied tlie peregrine of its pre\ . The Prairie
Falcon nested nearb\ , but the location of the
Fig. 46. Young Prairie Falcon in pothole eyrie illus-
trated in Fig. 43. Plioto bv Gary D. Lloyd and
C. M. White, 1958.
peregrine's e\rie was not ascertained b\ the ob-
si'i^ver.
Not all encounters between the two species
are won 1)\ Prairie Falcons. Ogdcn (1972)
sighted an adult female peregrine along the
Snake River of southwestern Idaho on .31 March
and 6 April 1972. Although unmated, she forced
a pair of Prairie Falcons to abandon their estab-
lished territor\ and clutch of eggs following
about two weeks of conflict between the two
species (Ogden, pers. comm., 1972). The female
peregrine remained and defended the cliff
through the remainder of the nesting season and
on several occasions she made reproductive over-
tiues toward male Prairie Falcons (ibid.). Richard
Fvfe (pers. comm., 1972) made an observation
similar to Ogden's on 11 April 1972 in Alberta,
C^anada. A pair of Prairie Falcons was well es-
tablished and the female was about to la\' eggs
in a "iiothole" e\rie on a high dirt river bank at
the time that the female peregrine arrived at
that cvrie on 1 1 April. The male pei-egrine pre-
ceded her arrival b\ a few day.s. Within a mat-
ter of hours on the da\- of her arrival, the pere-
grines had dri\-en the prairies awa\' and usurped
the i)()th()!c.
Despite these obser\ations of conflict, both
sjiecies are able to establish and hold an e\rie
site in close proximit\' to its congener. The near
e(|Malit\ in size and strength betweeti the two
Biological Series, \'ol. 18, No. I PERECniNE Falcon in Utah
61
species seems to recliKv their dominance over
each otlier. This is unlike the competition be-
tween the peregrine and the Gvrfalcon in the
.Arctic, \\here the larger and stronger Gyrfal-
eon, due to its earlier nesting and superioritv
to the peregrine in aerial combat, is able to es-
tablish and hold the most propitious nesting
sites (Cade, 1960).
Both peregrines and prairies mav use one
another's alternate nesting sites, the availabilitv
of which ma\' enable the two species to nest
in closer pro.\imit\' to each other than would
two pairs of peregrines or t\\-o pairs of Prairie
Falcons. Mebs (in Fischer, 1967) reported a
similar relationship between the Lanner Falcon,
a near ecological i'(|ui\'alent of the Prairie Fal-
con, and the peregrine in Sicih . A nesting cavity
(hole) under his observation for three years was
occupied in 1957 b\ lanners and in 1958 and
1959 b\' peregrines.
In some instances, tlu' Prairie Falcon ina\'
occupy sites which otherwise would be used bv
additional pairs of peregrines— as well as the
reverse— thus possibh' limiting each other's
breeding density.
Each species is known to maintain distances
between exries in j^arts of its geographic range
not occupied b\ the other species which are
much less than the distances between their
evries along the Wasatch escarpment. Few of
the distances, however, averaged less than the
distance between the alternate nesting sites used
b\ the peregrine and Prairie Falcon at site 7.
Hickev (1942), for example, mentions that
two pairs of peri'griius nested only a half mile
(805 m) apart in Canada, and Ratcliff (1962)
gives an instance in Great Britain of four pairs
breeding on a mile (1.6 km) stretch of cliff.
White and Cade (1971) found peregrines nesting
a quarter of a mile (1.40 km) apart in the Arctic,
but this was the exception, not the rule. Beebe
(1960) noted fi\e to eight pairs nesting on a
linear mile (1.6 km) of cliff in the Queen Char-
lotte Islands, the highest density known for the
peregrine.
The highest Prairie Falcon densit\", to our
knowledge, is along the Snake River in south-
western Idaho, where in 1971 Ogden (1971)
found 74 acti\e nest locations along a 53 mile
(85.3 km) stretch of river, for an average of 1.4
occupied areas per linear mile (1.6 km). The
e\Tie sites averaged less than one mile (1.6 km)
apart (one pair/3,771 ft; 1,149 m).
Date of Egg Laying as a Competitive Factor
We have observed in Utah that the Prairie
Falcon generalK' initiates egg la\ing earlier in
the spring than does the peregrine, and Nelson
(1969) also noted this relationship between the
two species. In Utah, peregrines have initiated
egg laxing as earh as 22 March and as late as
the second week in May. We have records of
Prairie Falcon clutches in the Great Salt Lake
area containing three eggs on 7 April, four
eggs on 10 .'^pril (R. L. Porter and J. F.
Poonnan, unpubl. notes), and five eggs on 22
April. Newly hatched young were present
on 13 May; \oung capable of flight were pres-
ent on 10 June. A nest in extreme northern
Utah found by Erwin in 1969 contained fully
fledged \oung on 1 June. Woodbury et al.
(unpubl. ms) recorded 51 sets of eggs from
Tooele, Salt Lake, and Utah counties collected
from 3 March to 15 June 1939. The average
date of collection for 16 of the clutches, for
\\-hich sufficient dates are available, was 20
April (range: 3 April-22 May). This did not,
however, represent the dates of the laying of
the first eggs. Wolfe (1928) records complete
clutches of Prairie Falcon eggs in Utah from
5 to 20 April. The average nesting date for 36
records in I'tah Count\' was 18 April (range:
3 March-15 June) (data from Bee and Hutch-
ings, 1942).
An earlier nesting date would give the
Prairie Falcon first choice of eyrie sites. We
have yer\' little precise information for Utah on
the arrival dates of either species at their eyrie
sites, although White has seen Prairie Falcons
at cliffs where e\rie sites were situated in
Februarx' and earh March and Porter has re-
corded them at a nesting cliff in the west desert
of Utah as early as 3 Februar\- (1953) (Porter,
Bushman and Behle, unpubl. ms). Wolfe (1928)
noted the first appearance' of Prairie Falcons in
the Salt Lake Valley about the middle of
March, and earlier farther south. He indicated
that in some of the warmer valleys many of the
falcons probabh' remain during the entire win-
ter. Morlan Nelson (pers. comm., 1971) has
seen this species at its desert eyries in Utah the
year around. He believes that only the young
leave the area of the nesting site (ibid.), although
Enderson (1964) recorded the earliest arrivals in
northern Colorado on 22 Februar}- in 1961 and
observed that most adults became associated
with the cliffs b\- mid-March.
Judging from the observation of adult male
peregrines at exries the year around in New
Mexico (T. Smylie, pers. comm., 1971), it is
(|uite possible that peregrines remain at or near
some of the Utah e\ries the year around, [>ar-
tieularly the desert sites. Paul Newey (pers.
comm., 1952) observed peregrines chasing his
l^igeons near the Wasatch Mountains during
62
BiucHAM Young Univehsity Scieni:k IUu.i.ktin
the last week in January 1950 and again on 18
Februar\ 1950. The falcons were probably
from a nearb\- eyrie. The nesting cliff was
climbed on 25 February b\' R. D. and R. L.
Porter, but no falcons were seen. Both pere-
grines and Prairie Falcons, howe\c'r, were seen
b\' 4 April.
Re|)roductive Potential as a Competitive Factor
The Prairie Falcon appears to have a greater
reproductive potential than does the peregrine.
This, however, among other things such as food
availabilit\- and winter niortalit\' of \oung, may
be a reflection of the greater vulnerability of
the Prairie Falcon's eggs and \oung to predation
due to its selection of evries at sites which are
more easily accessible to predators. The average
clutch size for the Prairie Falcon is 4.5 for .55
completed clutches in Wyoming and Colorado
(I'lnderson. 1964), 4..'3 for 20 nests in western
Montana (Leeds', 1972), 4.25 for 31 eyries along
the middle Snake River in Idaho (Ogden, 1971),
and 4.35 for the 65 clutches from the Utah
e\ries in the present stud\ . These are compared
with an average clutch size of 3.8 for peregrines
in Utah, 3.7 for peregrines elsewhere in the
United States (Hickey, 1942; Bond, 1946), and
2.9 for peregrines in northern Alaska (Cade,
1960).
PLEISTOCENE AND PREHISTORIC PEREGRINE AND
PRAIRIE FALCON DISTRIBUTIONAL RELATIONSHIPS
Although Nelson's (1969) climatic change
hypothesis probabh' is not the complete answer
to the recent reduction in active eyries in Utah,
it has a great deal of merit on a long-term basis.
Perhaps the peregrine's present distribution in
Utah can be elucidated best bv an examination
of tlu> possible distribution of the peregrine and
prairie falcon during prehistoric and Pleistocene
times.
Pleistocene Distributional Records
Botii tlu' peregrine and tlie Prairie Falcon
are known from late Pleistocene deposits in
western North America (Howard, 1962b; Miller,
1943). Hence, both species probabh' were pres-
ent in Utah during the late Pleistocene. White
and (>ade (1971) suggest that the peregrine
ma\- have originated in midlatitude regions of
Ein-asia, then spread northward into the Arctic,
and from there into North America (White
1968b). The Prairie Falcon apparently evolved
in situ in western North America.
Both species were ]iresent in the Los Angeles
area of California conlem]ioraneousl\' (Howard,
1962b) throughout much of the late Pleistocene
period covered by fossils found in the La Brea
Tar Pits. The fossils in tlicse pits are believed
to range from 5.()()() to 10,000 sears old (Berger
and Libln-, 1966; Ho, .Marcus, and Berger, 1969;
and Downs and .Miller, 1971).
Pit 16 contained fossils of three each of
both the peregrine and the Piairic I-'aleon. I'ossil
wood from two depths, 6'/2 and 12 feet (2-3. 7m),
in this pit has been dated back > 40,000 years
bv radiocarbon dating (Berger and Libbw 1966).
The occurrence of these two species together
in this and other pits (Howard, 1962b) suggests
a long association between the two species.
Since there is, however, a considerable \aria-
tion in the ages of the fossils from the various
pits and from the various depths of each pit, and
since the greatest depths have not alwax's yield-
ed the oldi'st fossils (pit 9, Berger and Libb)',
1966), the exact age of the peregrine fossils is
not known. In addition, Howard's (1962b) pub-
lished account of the fossils present in the vari-
ous pits does not indicate the depths from which
the fossils were obtained nor if the fossils of
the two species discussed here intermixed with-
in the same depth. Therefore, a more definitive
interpretation regarding the duration of a s\m-
patric association between the two species and
the age of their fossil remains must await car-
bon dating of the actual peregrine and Pniirie
Falcon fossils.
Additional speeiinens of tlie Prairie Falcon
from Pleistocene deposits are known from Smith
Creek Cave in Nevada (Howard, 1952), from
Rock\- Arro\() (Wetmore, 1932) and Howell's
Ridge C;ave (Howard, 1962a) in New Mexico,
from Lubbock Reservoir in Texas (Brodkorb,
1964), and from Nuevo Leon in Mexico (Miller,
194.3). Specimens of the peregrine also have been
found at Potter Creek Cave and at McKittrick
in California (Miller, 1911 and 1927). Shelter
Cave in New Mexico (Howard and Miller. 1933),
and at American Falls in Idaho (Brodkorb. 1963).
Vertebrate fossils from the late Pleistocene
American Falls bed B, wlu're this latter speci-
men apparently originated, have been dated as
having an age greater than 29,700 B. P. (ibid.).
Biological Series, Vol. LS, No. 1 Peregrine Falcon in Utah
63
Post-Pleistocene Distributional Records
The Prairif Falcon was distributed widely
durinc; prehistoric times. It is known from Ore-
gon (Miller, 1957; <S,000 B. P.), California
[(Howard, 1929; ^^l.OOO B. P.) and (DcMav,
1942; ^500 B. P.)], Arizona (Miller, 1932; 1,000
A. D.), and Utah [(Harper and Alder, in press;
^8,500 B. P.) and (Steward, 1937; remains not
dated, but probabh- very recent)]. The pere-
grine, on the other hand, has been found, to our
knowledge, only at prehistoric sites in California
(Howard, 1929;' ==^1,000 B. P.) and Utah (Stew-
ard, 19.37; remains not dated, but one of the two
specimens probably was very recent; the other
may haye been somewhat older; one apparently
was within strata containing artifacts of the
Promontor\' culture).
These records suggest that both species were
rather wideh' distributed geographically during
the late Pleistocene, and that the peregrine prob-
abh' was more common then than now; but fol-
lowing the Pleistocene period, the relative dis-
tribution and abundance of the two species
probabh were much the same as the\- have been
historically.
Lake Bonneville and Peregrine Distribution
in Utah
Ancient Lake Bonneville was formed during
the thrusts of the most recent Pleistocene gla-
ciers some 60,000 to 70,000 \ears ago (Black-
welder, 1948, and Autevs, 1948). At its greatest
height (the Bonneville level), this lake covered
19,750 sq miles (51,153 knv') of Utah's Great
Basin (Antevs, 1948) and had a shoreline of 2,550
miles (4,103 km) (Fenneman, 1931). After stand-
ing at the Bonneville level for a long period of
time, it is believed to have receded below the
present level of the Great Salt Lake ( Marsell
in Diirrant. 1952). Then, some 25,000 \'ears ago
during the Provo pluvial it rose to the Provo
level [Lake Provo, 13,000 mi= (.3.3,670 km^
area, Antevs (1948)]. It then receded (Antevs,
ibid.; Marsell, op. cit.) after which it again filled
back up to the Prove level (Marsell, op. cit.). In
the last 12,000 years it receded to the present
level (op. cit.).
A warmer interval of some 4,000 years began
about 5,550-4,000 years B. C. (Blackwelder,
1948). at which time the lake receded to a level
below that of the Great Salt Lake, with average
temperatures distinctly higher than those of the
present (Antevs, 1948; Blackwelder, 1948). Be-
ginning about 2, .500 years ago, a reduction in
mean temperatures and evaporation caused an
expansion of the lake to its historic levels (An-
tevs, 1948).
The present environmental conditions in the
Arctic ina\ be near optimal for the pere-
grine, judging from its recent distribution and
population density there. Climatic conditions in
Utah during the late Pleistocene glacial periods
probably were much less arid than at present and
consequently closer to those presently occurring
in the Arctic. According to Blackwelder (1948),
temperatures in the Great Basin during the cold-
est ages probably were 8-12° F below the long-
term average, and the rate of evaporation was
much slower than at present. The extent of the
ecological changes that took place in the south-
em part of the Great Basin during the latest
glacial age are revealed in the dung of extinct
ground sloths found in G\ psum Cave of south-
em Nevada (Laudermilk and Munz, 193.5). The
dung contained species of plants which now oc-
cur 3,000 feet (914 m) higher in the mountain
ranges some 20 miles (.32.2 km) awa\'.
Recent data collected by Harper and Alder
(in press) from an anthropological site in north-
ern Utah, although agreeing in the sequence of
events, indicate that the date of the actual onset
and termination of these jieriods ma\' be in er-
ror as might the extent of temperature change.
At Hogup Cave, which is located just north of
the Great Salt Lake, Harper and Alder (in press)
found that all but one of the plant species that
were present in the 14 feet of deposit dating
back 8,500 years presently occur within 40
miles (64 km) of the cave. During this period,
the upland areas were dominated by a xeric
desert shrub community, although the first 500
years were somewhat more mesic in nature.
They (ibid.) found that the lowlands had under-
gone a greater degree of change than had the
uplands, as suggested b\' both plant and animal
remains in the deposits. From about 7,800 B. P.
to 2,500 years B. P. (except for a brief period
about 6,000 years B. P.), the temperature in-
creased at least 1° C and the open water and
marshlands decreased. Then some 1,500 years
ago and continuing for about a milleniuin, there
was a relative increase in grasses on the uplands
[suggesting an increase in rainfall]. Haq^er and
Alder (ibid.) believe that the last .500 years were
more arid and that the climate around the cave
became as dry and inhospitable as at an\'time
during the past 8,.500 years.
Historically, with the utilization for irrigation
of the river waters which support the Great
Salt Lake and a general increase in mean tem-
peratures and decrease in precipitation during
the past several decades, as was discussed ear-
64
Bhigham Young Univehsitv Science Bulletin
lier, the Groat Salt Lake reached its minimum
level for historic times in about 1961. Since then
it now has risen about seven feet ( 2. 1 m ) above
its historic low.
The climate and ecological conditions pres-
ent during the past 8,500 years would not seem
to have been sufficienth' arid to have eliminated
c()ni]iletelv the peregrine as a breeding bird in
the area surrounding the Great Salt Lake. This
is especialK' so if one considers the apparent
extent of the aridity during the past 500 years
and the persistence of the peregrine as a breed-
ing bird in Utah despite the dr\' harsh climate of
the past half centur\-.
The occurrence of the Prairie Falcon at the
oldest level (at least 8,350 years B. P.). along
with numerous remains of nine species of water
birds, at a time when ecological conditions
probabh' were more optimal for the peregrine
than at j^resent, would suggest that the region
surrounding the Great Salt Lake was even at
that time an area of s\nipatr\" for these two
species. The presence of both species in Black
Rock Cave, south of Great Salt Lake (Steward,
1937), gives credence to this h\pothesis.
The date of the first occurrence of the pere-
grine in the intermountain area, of course, is not
known, but one can speculate that it ap]5eared
during one of the pluvial periods when the en-
vironmental conditions were most propitious
for its sur\ival and for its competition with the
Prairie Falcon tor food and ncstin<r sites.
It is probable that it \\as present in Utah dur-
ing the late Pleistocene, contemporaneoush'
\\ith its occurrence at Rancho La Brea. The
presence of this species among fossils at the
.Xmcrican Falls bed B, dating back at least
29,7(K) \t'ars, tends to confirm this supposition.
During the Bonneville and Provo pluvials.
Lakes Bonneville and Provo, with their extensixc
shorelines and numerous islands, must have pro-
vided innumerable nesting sites, an abundance
of pre\' species, and a near optimal climate for
the peregrine. Pleistocene rivers and smaller
lakes also must have provided correlative con-
ditions which ma\' account for e\ries in areas
outside of Bonneville Basin.
If the ])eregrine was present during the Bon-
neville and Pro\-o inlerpkn iais, it nia\ have en-
countered environmental conditions of even
greater aridity than at present. It would be of
interest to know if peregrine evries were main-
tained during these pi-riods of extrenie ariditv or
if, as suggested b\- Nelson (1969) for |iresent
conditions, altitudinal and latitudinal adjust-
ments were made. If the latter were true then
the evries became reactivated when the lake
gradually increased again to its maximum his-
toric level.
The overlap between the breeding distribu-
tion of the Prairie Falcon and peregrint' in the
intermountain area during the cooler, wetter plu-
vial period was probabh' dominated bv the pere-
grine, but as the climate slowh- ameliorated,
populations of the Prairie Falcon likely increased
in densit\' and gradualK- extended northward,
probably at the expense of the peregrine. As the
environmental conditions became more arid, the
peregrine eyries that were near lakes or streams
where sufficient food was available ma\' have
remained active. Those where the water disap-
peared probabh' either were taken over bv the
better adapted Prairie Falcon or else were de-
serted. Peregrines at the active e\ries may have
gradually adapted to the increasing aridity, but
thev would have been able to compete with the
Prairie Falcon onl\- at sites where water was
a\'ailable. This hypothesis seems to be supj^ortcd
bN' the geographical and ecological distribution
of the peregrine in Utah during historic times
(Fig. 1). For instance, of the 40 known and
suspected e\ries in Utah, 26 were located in or
near the Bonneville Basin. The greatest con-
cenh'ations of breeding pairs occurred near the
largest remaining bodies of water, jiarticularlv
in the area surrounding the Utah and Great Salt
lakes.
The e\ries in the harsh en\ironment of the
Great Salt Lake Desert were adjacent to small
expanses of marsh (Figs. 20 and 23). Most
astounding is that these evries existed at all,
considering the harsh nature of the einironment.
It is c\idence of the adaptabilit\ of the species
and of tlu' species' tenacit\- at its c\ric sites.
How long these e\ries would have remained ac-
ti\c in the absence of human interference is a
(jucstion that ma\' never be answered. The te-
nacit\ of peregrines at their e\rie sites as dis-
cuss('(l hx Cade (1960) and Hiekey (1942), and
the t( lulcncN' toward a genetic contiinu't\ in ey-
rie maintenance as proposed bv White (1969a)
(for a nioic complete discussion, see White,
196Sb) woultl suggest the possibilitx that some of
tlu> i-\ rie sites that were acti\c' during recent
times nia\' ha\'e had long histories of activity
sonu' perhaps, (>ven extended back into Lak(>
Honne\ille tim(>s. This possibilitx seems especial-
In' plausible when one considers the relative re-
ei'ne\' of some of the later pluvial periods. Thus,
tlie relationship between tlii' Prairie Falcon and
peregrine |in)babK extends back maTi\' thou-
sands ot years, which ma\ be a factor in the
relati\"i- compatibilitN of the two species.
Biological Sebies, Vor.. 18, No. 1 Peheghine Falcxjn in Utah
65
Data piivsentcd pre\iousl\' regarding the coii-
temporaneit\' of the two species at Rancho La
Brea; tlie occiirrenci' of the peri'grine in a lossil
bed at American Falls. Idalio, dating back to at
least 29,700 \ears B. P. (Brodkorb^ 1963); tiie
presence of both species at anthropological sites
just south of the Great Salt Lake (Steward. 1937;
Black Hock C^avc); and the climatic and environ-
mental evidences from Hogup Ca\e in northern
Utah ( Harper and Alder, in press ) tend to coi-
roborate this supposition. The lack of aggression
between them also suggests a long sympatric
relationship.
White and Cade (1971) believe that tradi-
tional use of an eyrie site will in the long run
reduce the total impact of intolerant behavior
and promote stability in the peregrine popula-
tions of the Arctic. If so, a long history of oc-
cupancN' at Utah evries probablv would have en-
hanced the peregrine's competitive position with
the Prairie Falcon and thus strengthened the
peregrine's hold on its oj^timal e\rie sites.
SUMMARY AND CONCLUSIONS
Utah's rugged topograph)' and ecological
variabilitv is conducive to its inhabitation by a
wide varietx' of raptorial species. This includes
the Peregrine Falcon, which now has \irtuallv
disappeared as a breeding bird in the state.
Although sparselv distributed throughout
Utah, the species apparentlv found conditions
especialh' suitalile for nesting in the environs of
the Great Salt Lake and Utali Lake valle\s,
where its nesting sites in the adjacent mountains
were within fhing distance of a plentitude of
preferred pre\' species which inhabited the
marshes and shorelines surroundin<? the two
lakes. Despite the aridity of the environment, the
20 eyries that occurred there, when and if thc\
all were active simultaneously, comprised a pop-
ulation comparable to some populations else-
where in North America where the environment
is considered to be uKjre congenial to the pere-
grine. On the average, there was one evrie site
for ever\" 225 stj miles (583 km-) in an area of
about 4,500 sq miles (11,655 km-) surrounding
the Utah and Great Salt lakes. The average dis-
tance between 13 evries along 130 linear miles
(209 km) of the Wasatch Mountains was 10.0
miles (16.1 km) (range. 2-20 mi; 3.2-32.2 km).
Elsewhere in the state, the species was more
sparseb' distributed, and then onlv at sites where
suitable nesting cliffs were adjacent to marshes
or rivers. OnK' nine additional eyries have been
verified for the remainder of the state [one pair
per 7.732 mi- (20,025 km-) in area, exclusive of
the aforementioned 4,500 mi'}, although 11
others are suggested bv the presence of adult
birds and /or voung during the nesting season.
If all 40 known and suspected evries are in-
cluded, there would be about one c\ rie for
every 2,12.3 s(i miles (.'^.499 km ). If 1 1 unverifii'd
evries are excluded, there woiild be about one
evrie for c\-erv 2.928 s(| miles (7.584 km'-') of the
state.
Peregrines have reproduced successfidh' in
the deserts of Utah's Great Basin and Colorado
Plateau under some of the harshest climatic
conditions to which the species is subjected. All
evries in Utah's deserts have been situated near
marshes, lakes, or rivers. Peregrine nesting sites
in the desert generallv were closer to extensive
marshes than were those along the Wasatch
escarpment. The average distance from evrie to
hunting sites in the marshes was onlv 1.3 miles
(2,1 km) (range, 0.19-2.8 mi; 0.31-4.5 km) for
three desert e\ries. For the nesting sites in the
region of the Utah and Great Salt lakes, the dis-
tances averaged 3.3 miles (5.3 km) (0.19-9.7 mi;
0.31-15.6 km). Marshes used bv peregrines at
the desert e\ rics usualK were less than 3 sq
miles (7,8 km-) in extent (Table 4).
Although the Peregrine Falcon has been
known to occur in LUah since the earh' 1870s.
most of our knowledge of its nesting distribution
and abtmdance dates back onlv three or four
decades. The status of the species in Utah prior
to the late 1930s is largely unknown. Its past
historv and present status in LTtah, therefore,
has been postulated on the basis of all records
available to us. both before and after 19.39. Data
are too sketchv for a thorough understanding of
the kinetics of local populations. E\ries that
siu"\'ived the longi'st arc those farthest from
areas of intensive agricultural practices and al-
so dense human populations. Those at the poor-
est qualit\' sites appeared to have been desert-
ed first. Abandonment of active e\ries first be-
came apiiarent in the 1940s. The known breed-
ing ]50]-)ulation in Utah was reduced bv the late
1960s to less than 10 percent of the pre-1940
estimates.
The several factors, in order of relative im-
portance, that may have contributed to these
changes are as follows: (1) the inimical effects
of DDT, its metabolites, and other chlorinated
66
Bricham Young University Science Bulletin
hydrocarboiis on percgiiiu' reproduction; (2) a
drying up of marshes which supported the pere-
grine's prey species, due to a decline in annual
precipitation; an increase in the average dail\'
temperatures; and the diverting of river waters
for irrigation purposes; (3) the killing of adult
and young falcons with firearms; (4) the death
of peregrines due to botulism toxins; (5) the
robbing of e\ries for their eggs or \oung; and
(6) the destruction of nesting cliffs for mining
and construction operations and general human
encroachment.
Reproductive failure t\pical of the pesticide
syndrome was recorded at three peregrine eyries
and one Prairie Falcon eyrie in Utah during the
period following the extensive use of DDT to
control mosquitoes and agricultural pests in Utah
and elsewhere. All of these factors combined
probably have contributed to the near extirpa-
tion of the peregrine in Utah, although the use
of organochlorine pesticides probabh' was the
most important contributory factor, especialh'
when combined with a prolonged drought which
occurred during the first half of the centur\'.
The average clutch size at one peregrine
eyrie site in Utah for five \ears betAveen 1943
and 1952 was 3.8, and an average of 2.4 voung
hatched during these vears; and for seven vears
between 1943 and 1953 a total of 19 voung were
produced for an average of 2.7 voung per vear.
This is in close agreement with figures recorded
at other e\rie sites in North America at an
erjuivalent latitude. The incubation period at
the aforementioned e\rie site was estimated to
exceed the 28 to 29 davs reported elsewhere bv
four or fi\-e da\s. An unusualK' long incubation
period of about 40 daws in 1948 was explained
on the basis of rencsting, if based on a 28- to
29-da\ incubation period.
Nestling peregrines in Utah were given a
wide variety of avian prev species. Pairs nest-
ing along the Wasatch Mountains (near thv
Great Salt Lake) fed their \oung mosth- shore-
aiid marshbirds, man\- of w hich were obtainable
onI\' from Great Salt Lake marshes up to 17
miles (27.4 km) distant. Avocets and Willets were
the species of shorebirds most used. Mourning
Doves, Rock Doves, Red-shafted Flickers, and
Western Meadowlarks were most used of the
nonatjuatic prey species. Rats, uhieh were the
only mammalian prey species present in ITtah
evries, represented less than one percent of the
diet. Passerine and gallinaeeous pre\- species
were of greater importance and a(|uatic pre\'
species of lesser importance in the desert e\ries.
The selection of eyrie sites hv peregrines in Utah
appears to be associated with the ;ivailabilitv of
suitable nesting sites adjacent to a marsh or
stream where prey species are available in ade-
(juate numbers. Tlie utilization of aijuatic prey
species as food for nestling peregrines in Utah
undoubtedl)- is a major factor in the species's
proclivit)- for nesting sites near water.
The Golden Eagle and Prairie Falcon are the
two species most likely to compete with the
peregrine for food and nesting sites. Direct com-
petition between the peregrine and Golden
Eagle for food probablv is minimal, since mam-
malian prey species contribute greath' to the
eagle's diet, and no direct evidence of compe-
tition between the two species for nesting sites
has been observed in Utah.
The Prairie Falcon, on the other hand, is a
probable competitor, which is expected because
both species belong to the same genus, both are
basically equivalent in ecological function, and
both are approximately ecjual in size and
strength. Although the habitat of the two species
overlaps, habitat separations are present. The
Prairie Falcon, for example, may nt>st in the des-
ert many miles from water. In the zone of con-
tact between the two species, its selectivit\' in
habitat and food encompasses and exceeds that
of the peregrine. The zone of contact between
the two species appears to be restricted onl\' bv
the paucit\- of suitable nesting habitat adjacent
to an adequate supply of food for the peregrine.
Where the\- occup\- the same habitat their
diets are somewhat different, thus mitigating
the possibility of strong competition for food, al-
though where they nested side bv side in the
Great Salt Lake Valley their food niches did
overlap considerabh-. Both species preved rather
extensivcK- on the same two |)re\' species, the
avocet and Willet, which probably was a re-
sponse to the abundance of these two shorebirds.
In general, the Prairie Falcon was much less
selective in its food requirements in the area
surrounding the Great Salt Lake than was the
peregrine in the same area, and it was more
prone to supph-ment its diet with rodents,
ground nesting birds, and reptiles. Thus, in this
respect, it ap(X'ared to have an adaptive ad-
vantage over the peregrine.
Competition between the two species for
food did not appear to ha\e been an important
factor in controlling their relative densities
along the escarpment of the Wasatch Mountains,
especialK when pojiulations of avocets, Willets,
and other s|X'cies of shorebirds were sufficiently
large to support them both.
We have no data regarding the food niches
of the IVairie Falcon in the zones of contact
between the two species at riviT sites in the
Biological Series, Vol. 18, No. 1 1'ereghine Falcon in Utah
67
desert. However, we would expect a greater
overlap in the avian prey of the food niches of
the two species in these areas due to the ehmina-
tion of a great portion of aquatic birds from the
diet of the peregrine (see Gabrielson and Jewett,
1940). Our data, however, suggest that the ex-
tensi\'e utilization of rodents, particulail\' ground
squirrels {Citcllus sp.), by the Prairie Fakvn in
the desert areas would tend to k'ssen the im-
pact of the competition between the two con-
geners for a\ian pre\ in those regions.
In regions of Utah where the populations of
the peregrine were greatest, pairs of Prairie Fal-
cons and peregrines ne'sted much closer together
than did pairs of peregrines or pairs of prairies.
Tlie two species sometimes e\'en used one
another's alternate nesting sites. When they nest-
ed close together, their nesting sites were not
known to be visible from one another. Although
thev were observed in aerial combat, neither
species appeared to be able to consistently dis-
lodge its congener from its nesting site.
Our data suggest that both species select
e\Tie sites on the basis of availabilit\', but when
given a clioice thev seemingly select them on the
basis of directional exposure to the sun. The
peregrine shows a preference for north- and
east-facing cliffs, and the Prairie Falcon shows
a preference for south- and west-facing cliffs.
This relationship between the two species needs
additional investigation to further test its valid-
itv in Utah and to test its applicability elsewhere
in the arid West.
The Prairie Falcon was less selective than
was the peregrine in its choice of nesting sites,
sometimes selecting sites which were seemingly
shunned hv the peregrine. The former species,
for example, utili/ed sites that were located on
smaller ledges with a smaller total nesting area,
as well as sites located on lower cliffs nearer
the base of the cliff or otherwise more easily ac-
cessible to humans and to maniinalian predators,
than did the latter species. Furthermore, ravens
which are common in Utah, seemingh' alter the
nesting habitat in a beneficial way for Prairie
Falcons b\ proxiding additional nests that are
frequenth" used b\' the falcons, whereas the pere-
grine apparently is little affected by the pres-
ence of ra\'ens.
The Prairie Falcons initiated egg laying ear-
lier in the season, thus giving them first choice
of nesting sites; and on the average they laid
larger clutches than did the peregrine.
Tlie Prairie Falcon is a true desert species. It
apparently evolved in the arid environment of
western Xortli .America, and as expected, in its
association with the peregrine it appears to be
the dominant competitor in the following ways:
(1) it has a greater reproductive potential than
does the peregrine, based on its larger clutch
size; (2) it is less selective than is the peregrine
in choice of nest sites and thereby has more
nesting situations to choose from; (3) it lays
earlier in the season than does the peregrine;
thus it mav have first choice of cliffs and evrie
sites; (4) it shows less selectivity in its choice of
prey species as food for its young; consequently
it has a wider range of species to choose from,
including birds, mammals, and reptiles; and (5)
because of its selection of prev species other
than birds, it is not as obligate to open water for
food, nor is it as obligate to open water for
liathing, and thus it may nest many miles from
water.
The Prairie Falcon, then, would appear to
have a marked adaptive advantage over the
peregrine, especially in marginal areas where
the peregrine's ecological tolerance is restricted
and wluTC the peregrine's preferred food and/
or nesting sites are in short supply. The Prairie
Falcon's adaptive advantage over the peregrine
ma\' contribute to the restriction of the pere-
grine to the more optimal aquatic habitats near
streams and marshes where food and nesting
sites are not in short supply, and where the
peregrine competes successfully with its con-
gener.
Some of the reasons the peregrine in Utah is
able to compete successfully with the Prairie
Falcon for food and quality nesting sites may be:
(1) the relative tolerance of the two species for
each other while nesting close together; (2) the
utilization of one another's alternate eyries,
coupled with the inabilitv of either species to
consistently gain a dominance over the other in
aerial combat, although recent observations by
Ogden (1972) and R. Fyfe (pers. comm.)
suggest that the peregrine may occup\- the
most propitious sites because it is capable of
forcing the Prairie Falcon from them; (3) the
possibk- partitioning of the mating cliff with
each species having distinct preferences for dif-
ferent t\|ies of nesting sites or a wide variability
in acceptable nesting situations. There is, for ex-
ample, tlu' peregrine's preference for open
ledges and the Prairie Falcon's acceptance of a
wide range of nesting situations, illustrated by
its use of potholes in the face of the cliff, open
ledges, and old stick nests of other raptorial
species. The pothole e\'ries probabK enhance
the survival prospects of voung reared on west-
facing cliffs and probably offer greater protec-
tion from predation than do the open ledges; (5)
a variation between the two species in the size
68
Bricham Young University Science Bulletin
of the nesting area and in the height of the chffs
and eyrie sites; (6) the presence, in abundance,
of the prey species preferred bv the peregrine in
areas of Utah wlieri' tlie peregrine was most
common, witli partial partitioning b\' the two
species of their food niches; and (7) tlie pere-
grine's fidehty to the cliff.
We have Inpotlu'si/ed tliat the peregrine
probably invaded the intennountain region dur-
ing a pluvial period of the Pleistocene, when the
environmental conditions favored the peregrine
in its competition with the Prairie Falcon. More-
over, tlie iincient Pleistocene Lakes Bonneville
and Provo undoubtedly presented the peregrine
with both an abundance of food and a suffi-
ciency of nesting sites. Fossil remains of pere-
grines from the La Brea Tar Pits dating back
40,000 \ears or more and from American Falls
in Idaho dating back nearly 30,000 years sup-
]5ort this hvpothesis.
There ma\' have been times during the cooler
pluviiil periods when the geographic ranges of
the two species were mutualh' cxclusi\e, at least
in some localities of Utah. During the drier inter-
pliuials, the Prairie Falcon probabh' took over
nesting sites no longer tenable to the peregrine.
However, the peregrine probabh' persisted at
those sites where the ecological conditions were
most propitious to its sur\iyal and where it
gradually adapted to the more arid condition of
the interpluvial. as is the present case. The pere-
grine is noted tor its fidelit\' to certain cliffs over
man\' generations of breeding birds. Traditional
occupanc\' ma\ not be the rule with the Prairie
Falcon. Finally, one would expect that the longer
the existence of a svmpatrie relationship between
two closeh' related congeners, the more exten-
sive would be the partitioning of their resotirces
and the greater the reduction in the conflict be-
tsveen them. The partitioning of the resources
between the peregrine and prairie seems to be
sufficientK di'fined to suggest that this phe-
nomenon lias been in operation for a consider-
able period of time. The low level of interspecif-
ic aggressiyeness as well as the paleontological
records suggest that the relationship between
the two species is probably of long standing.
Fluctuations in |ieregrine populations con-
comitant with fluetu;itions in height and length
of the shoreline of the I^leistocene lakes prob-
abh' luive ])een of natural occurrence down
through the ages. Peregrine populations possibh'
have been declining slowh in I'tah o\er the past
several centuries eoneurrent with a general
amelioration of climate and accompaining re-
duction in suitable habitat based on climatic
and biotic e\'idenee from Tlogup Cave dating
back 8,5(X) vears, while popuhitions of the Prai-
rie l^'alcon may have slowK expanded to fill the
\'oid as suggested by Nelson (1969).
Evidence that the southern extremit\' of the
peregrine's geographic range historicalh' shifted
northward along with an associated shift ;dti-
tndinalK' (Nelson, 1969) has not been demon-
strated for Utah. With the drastic decline in
the species' breeding populations that is pres-
ently taking place throughout North Amer-
ic;i, ;i Inpothesis of this kind is difficult to test.
A general cooling trend in Utah and elsewhere
in the Northwest which started about 1961, how-
ever, should result in more suitable ecological
conditions for the peregrine. The extent to which
old eyrie sites are recolonized should be a test
of the validitN' of Nelson's (1969) climatic change
liN'pothesis for the peregrine decline in the west-
ern United States.
The presence of the peregrine at desert sites
on the peripher^• of its ecological range as late
as 1959-60 in the Great Basin (Table 1, site 23)
and the earl\- 1960s in the Colorado Plateau
(Table 1, site 28) emphasizes the species's abilit\'
to adapt and its tenacity for survival.
The competitive roles of the peregrine and
the Prairie I'alcon appiu'i'ntK' change according
to locality, based on a\'ailability of food and
nesting sites, and on the behavior and ecology
of the rajitorial species with which thev must
compete. For example, in the Arctic the Pere-
grine Falcon is a gi'iieralist, both in terms of its
selection of nesting sites and in regards to troph-
ic relationships with its competitors (White and
Cade, 1971); there, this species utilizes a wide
variety of food, which is not a restricti\e aspect
of its econoniN in the Arctic, and a broad selec-
tion of nesting sites. Its chief competitors in the
Arctic are the Common Ra\'en, the Cxifalcon.
and th(> Rough-k'gged Ilauk (Biitco Ia<i0j)iis).
The C\ ifaleon, the peregrines most closeK' re-
lated competitor, on the other hand, is a special-
ist in tenns of nest site and food selection. The
raven and C\i-faleon have similar nesting recjuire-
ments, and since both are earh nesti'rs the\
have an earlier choice of evrie sites. Thus, when
the later-nesting peregrines and rough-legs ar-
ri\'e. the late anivals are more or less limitcxl to
the remaining sil(>s. Conse()uentI\'. the peregrine
utili/es "mar^inid " sites where it ma\' ha\'e to
compete with the rough-legs. Apparenth', how-
e\'er. the iK^regrine is capal)le of usurping the
I'oiigh-lcgs's nest. In addition, the two species
ma\' joint K' occu|)\' the same cliffs, thus lessen-
ing the competition between them. White ;md
Cade (1971) believe that .since ravens and pere-
<j;i'incs do not get along well together, the
Biological Series, Vol. 18, No. 1 Pehecuink F.alcon in Utah
69
earlier nesting raven max force the peregrine
into "marginal" and "submarginal" sites on those
occasions when peregrines tn' to nest too close
to the ra\ens. The\ believe that the same thing
applies when peregrines attempt to settle too
close to Gyrfalcons on the same cliff. The pere-
grine, nevertheless, does use "optimal" sites in
the Arctic when thev are available.
In the desert, however, the i^eregrine's role
is the reverse of its role in the Arctic. Here the
peregrine is forced into the roll' of a specialist
because the harsh arid environment produces
few of the pre\' species preferred by the pere-
grine and because the Prairie Falcon competes
more successfulh' for both the former's marginal
food niche and its marginal nesting niche. The
specialization in the peregrine's food require-
ments is apparent onh' when compared with that
of the Prairii- Falcon in the zones of contact be-
tween the two species. Here the utilization bv
the Prairie Falcon of rodents (especiallv ground
squirrels), reptiles, and birds (to a great extent
the same jirincipal shore birds used by pere-
grines) makes it a generalist in its food habits.
In areas of allopatiy, as in the deserts, the Prai-
rie Falcon often uses predominantlv one or two
species of rodents and /or birds and, therefore,
in thc^e regions, it is seemingly a specialist.
In its nesting site requirements, the Prairie
Falcon is a generalist when both allopatric and
svmpatric with peregrines. In its selection of
nesting sites, it seems to prefer sites which we
would consider to be marginal for the peregrine.
This more or less limits the peregrine to the
more optimal nesting sites and to the role of a
specialist. Distribution of free water, and its
concomitant supply of suitable prev species, is
the most important environmental factor dictat-
ing the distril)uti()n and abundance of the Pere-
grine Falcon in the arid \\'est. Con\ersel\-, lack
of free water and its associated supph' of suit-
able prev species is a limiting factor in the dis-
tribution and abundance of this species.
Climate, on the other hand, appears to be a
major factor restricting the geographic distribu-
tion of tin- Prairie Falcon as is its strong pio-
clivit\' to nest on cliffs, thus nearlv eliminating
the use of tree nests as evrie sites. In general,
however, the selection bv the Prairie Falcon of
a wide varietv of prev species, encompassing
three classes of vertebrates, its utilization of sev-
eral different t\pes of nesting situations, its rela-
tiveh' high reproductive potential, and its abilit\'
to exploit successfulh' the arid environments of
western North America points out the extent to
which this sjiecies has become adapted to its par-
ticular environment. With its versatilit\' in selec-
tion of prey species and nesting sites, but more
especially the former, the Prairie Falcon is
among the better adapted and more successful
of North American raptors.
Because of its extensive utilization of rodents
for food, its frequent occurrence in areas many
miles from water and man\- miles from civiliza-
tion, and its relatively nonmigratory nature, the
Prairie Falcon is much less likely to become a
permanent victim of the indiscriminate use of
the chlorinated hydrocarbons than is the pere-
grine.
The current precarious status of the Pere-
grine Falcon in Utah is probabh' a result both
of a change in climate and of the inimical effects
of man's activities. The future of the species in
Utah, as elsewhere, appears bleak. Many of the
factors responsible for its decline are still in evi-
dence. DDT and other harmful pesticides are
still being used in Utah. In 1969, for example,
7,593 pounds (3,440 kg) of DDT were used in
Utah for the control of noxious insects (in the
pesticide polic\' statement of the Utah State De-
partment of Natural Resources) and this was in-
creased to 11,.^8 pounds (5,140 kg) in 1970
(Work Unit A, Pesticides Applied— State of Utah,
Utah State Health Dept., 1970; Stephen L. War-
nick). The impact on raptors of polvchlorinated
biphen\ls and of the heav\- metals, such as mer-
eurv, lead, and cadmium, are still poorly un-
derstood, and other chemical hazards of un-
known kinds also ma\' be involved.
Although man is still encroaching on the ac-
tivities and habitat of the peregrine and on its
environment, with the construction of artificial
lakes such as those formed in Glen Can\on and
in the Flaming Gorge and with a general cool-
ing of the climate which is resulting in the re-
establishment of certain lakes and marshes, nest-
ing pairs of peregrines mav vet be attracted in-
to new and old areas, hopefully awa\' from the
harmful activities of man. Inimical environmen-
tal factor's must first be eliminated. The use of
management methods, such as construction of
manmade marshes near suitable nesting cliffs or
manmade evrie sites near suitable marshes, has
not vet been attempted. Management techniques
have worked well with other species, and mav
l^rove successful with the peregrine.
The few peregrine eyries still remaining ac-
tive, as well as the manv active Prairie Falcon
evries in the state, should be given the strictest
protection and or management. All peregrine
e\ries should be guarded zealouslv that future
generations ma\' have the pleasures which have
been ours; that is, to see, to stud\'. and to enjoy
this magnificent species alive in its native haunts.
70
limcaiAM VouNc Univehsitv Science Bulletin
AcldeiKlum
After the final inamiscript was in press, we
learned of two more localities used by pere-
grines. Ralph B. Williams (pers. comm.) told
us of an eyrie that the late Charles Springer of
Salt Lake City, an avid birder and falcon en-
thusiast, located sometime in the late 1930s and
early 1940s. The eyrie was west of the general
area of the Bear River marshes. From the de-
scription of the eyrie it appeared to be about
12 to 15 straight-line miles from eyrie number
9 ( Tabic 1 ) and within region A as outlined
on Figure 1. It was apparently inactive after
the early 1940s since that area was searched
for falcons in the mid-1940s. The second locality
occupied by a pair of territorial peregrines
would also be included in the area of region A
but to the cast of the boimdary lines, as shown
in Figure 1 . This locality was adjacent to several
pairs of Prairie Falcons, but the exact canyon
in which it was located could not be determined
from a map, as it was located in the lati' 1930s
and details are vague (Morlan Nelson, pers.
comm., 1973).
ACKNOWLEDGMENTS
Thanks and appreciation are extended to
Morlan W. Nelson for his critical review of an
early draft of the manuscript. His comments and
data are distributed liberalK- throughout the
publication. Roger L. Porter assisted in the col-
lection of data during the earlv vears of the
study; Lois G. Porter typed several drafts of the
manuscript; and Sanford D. Porter made the
diagrams and offered helpful suggestions at var-
ious stages of the writing.
Van T. Harris and Thomas D. Ray reviewed
the manuscript prior to final typing, and Chand-
ler Robbins, Charles Gish, and James Ruos
assisted in various wavs with the data from the
Bear River Refuge Christmas Bird Counts. James
Ruos critically reviewed some of the first sec-
tions of the manuscript. Harris, Robbins, Gish,
and Ruos are all of the U. S. Bureau of Sport
Fisheries and Wildlife; we thank "tliem for their
assistance.
There have been so manv people that have
helped in gathering data that it would be diffi-
cult to acknowledge all of them without missing
some, but they have all been given credit in the
bodv of the text. We owe a special thanks to all
of them.
We would like to dedicate this stud\' to the
late Gary D. Llovd, who was a constant com-
panion to White while working with raptors
tlu-ough the 1950s and earl\- 1960s, and who met
an untimcb' and premature death, along with
his wife, while thev were working in the falcon
countrv of east-central LUah.
APPENDI.X-ADDITIONAL HISTORY OF DDT USAGE
AS A MOSQUITOCIDE IN UTAH
According to Collett ( 1955), Salt Lake Coun-
t\- sprayed 310 acres (125 ha) by aiqjlane in
1949 and in 19.50, according to Smith (1951), both
Weber and Salt Lake City Mosquito Abate-
ment districts (MAD) hired planes for aerial
spray work, and the latter treated more than
1,300 acres (526 ha). From 1950 through 1953
the Salt Lake Cit\' district treated 10,680 acres
(4,322 ha) by aircraft (Collett, 1955) and Davis
(>ounty sprayed 3,000 acres (1,214 ha) by air-
craft in 1953 (Stewart, 1954). Aerial spraving
greatlv increased in 19.54, according to Graham
and Rees (19.58). In that year tlie Salt Lake
City district (Collett, 1955) aerialh- treated
12,128 acres (4,908 ha), of which 2,286 acrc^
(925 ha) were in cooperation with the Davis
County MAD. Insecticides used by the Salt
Lake City MAD in 19.54 were DDT in number
2 fuel oil, DDT and water emulsion, and hepta-
chlor emulsion in water; DDT was applied at
the rate of two gals per acre (19 l/ha), contain-
ing 0.4 lbs (181 g) of DDT; heptachlor was ap-
plied at the rate of 0.06 lbs/acre (67 g/ha) for
lai-vae and 0.08 lbs/acre (90 g/ha) for adults
(Collett, ibid.).
The Weber County MAD spra\ed over 10,000
acres (4,047 ha) by air in 1952 and 19,825
acres (8,023 ha) in 19.53. DDT was applied at
0.2 lbs/acre (224 g/ha) for 15,812 acres (6..399
ha) and at 0.4 lbs/acre (448 g/ha) for 1,793
acres (726 ha) in 1953, for a total of 3,880
lbs (1,760 kg) of DDT applied to 17,605 acres
(7,124 ha) of marsh and pasture lands (Fronk,
1954). In 1954 Weber County aerially treated
Biological Series, Vol. 18, No. 1 Peregrine Falcon in Utah
71
13,300 acres (5,382 ha) at 0.1 to 0.4 llxs of DDT
per acre (112-448 g/ha) (Fronk and Jenne,
1955), while Box Elder Count\' .similarly sprayed
5,000 acres (2,02,3 ha) (Josephson, 1955). '
An abatement district was not operative in
Utah Count\ nntil 1963, and the chemicals used
were Bavtex, parathion (both in pastures), and
DDT (where residues were considered to be no
problem) (Davis, 1964). DDT was not used
b\' the South Salt Lake Count\' district. Hepta-
chlor was used in this county starting with the
inception of the MAD in 1953 (Graham and
Rees, 19.58; Graham in letter). It was applied
at 0.04 lbs per acre (45 g/ha). Dieldrin was
used extensively in this district also at the same
concentrations as heptachlor. Other districts
then began using heptachlor, and by 1958 it
became as commonly used as DDT (Graham
and Rees, 1958). Malathion and parathion were
used in 1956, and parathion became the insecti-
cide preferred by the Salt Lake County MAD
in 1957 when resistance to heptachlor developed
in the mosquitoes (Graham and Rees, 1958).
B\' 1962 nearly all mosquito abatement districts
in Utah had abandoned the use of DDT because
pastures, milk, and food were becoming polluted
with residues, and by 1970, only Box Elder
Count)' was still using DDT.
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Brigham Young University
Mus. coMP. zoou Science Bulletin
NOV 51973
u'OTicOLOGICAL SURVEY OF THE
ALGAE OF
HUNTINGTON CANYON, UTAH
by
Lorin E. Squires
Samuel R. Rushforth
Carol J. Endsley
BIOLOGICAL SERIES — VOLUME XVIII, NUMBER 2
JUNE 1973/ISSN 0068-1024
BRIGHAM YOUNG UNIVERSITY SCIENCE BULLETIN
BIOLOGICAL SERIES
Editor: Stanley L. Welsh, Department of Botany,
Brigham Young University, Provo, Utah
Acting Editor: Vernon J. Tipton, Zoofogy
Members of the Editorial Board:
Ferron L. Andersen, Zoology
Joseph R. Murdock, Botany
WiLMER W. Tanner, Zoology
Ex officio Members:
A. Lester Allen, Dean, College of Biological and Agricultural
Sciences
Ernest L. Olson, Director, Brigham Yoimg University Press
The Brigham Young University Science Bulletin, Biological Series, publishes
acceptable papers, particularly large manuscripts, on all phases of biology.
Separate numbers and back volumes can be purchased from University Press
Marketing, Brigham Young University, Provo, Utah 84602. All remittances should
be made payable to Brigham Young University.
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of Gifts and Exchange, Brigham Young University Library, Provo, Utah 84602.
Brigham Young University
Science Bulletin
AN ECOLOGICAL SURVEY OF THE
ALGAE OF
HUNTINGTON CANYON, UTAH
by
Lorin E. Squires
Samuel R. Rushforth
Carol J. Endsley
BIOLOGICAL SERIES — VOLUME XVIII, NUMBER 2
JUNE 1973/ISSN 0068-1024
TABLE OF CONTENTS
ABSTRACT 1
INTRODUCTION 1
REVIEW OF SELECTED ALGAL STUDIES IN UTAH S
DESCRIPTION OF THE HUNTINGTON CANYON DRAINAGE 6
GEOLOGY 6
CLIMATE AND VEGETATION ZONES 12
DESCRIPTION AND USES OF HUNTINGTON CREEK 15
DESCRIPTION OF SAMPLING SITES 17
LAWRENCE ( SITE 1 ) 17
HIGHWAY 10 BRIDGE (SITE 2) 17
PLANT SITE ( SITE 3 ) 17
BEAR-RILDA CAMPGROUND (SITE 4) 19
TIE FORK POND (SITE 5) 20
STUART FIRE STATION (SITE 6) 20
BEAR CANYON ( SITE 7 ) 20
METHODS 22
PHYSICAL AND CHEMICAL MEASUREMENTS 22
Temperature 22
Turbidity 22
Water Chemistry 22
PHYTOPLANKTON 22
Net Plankton 22
Naimoplankton 24
PERIPHYTON 24
VISIBLE BENTHIC ALGAE 26
FLORISTIC SAMPLING 26
RESULTS AND DISCUSSION 26
LAWRENCE ( SITE 1 ) 26
HIGHWAY 10 BRIDGE (SITE 2) 31
PLANT SITE ( SITE 3 ) 33
BEAR-RILDA CAMPGROUND (SITE 4) 39
STUART FIRE STATION (SITE 6) 44
BEAR CANYON ( SITE 7 ) 50
TIE FORK POND (SITE 5) 51
ALGAL FLORA OF HUNTINGTON CANYON 55
ACKNOWLEDGMENTS 57
APPENDIX I— NET PLANKTON, NANNOPLANKTON, PERIPHYTON, AND VISIBLE BENTHIC ALGAL
TABLES 57
APPENDIX II— ALGAE COLLECTED FROM HUNTINGTON CANYON OCTOBER 1970— MARCH 1972 .... 84
LITERATURE CITED 86
AN ECOLOGICAL SURVEY OF THE ALGAE OF
HUNTINGTON CANYON, UTAH
by
Lorin E. Squires/ Samuel R. Rushforth/ and Carol J. Endsley'
ABSTRACT
A quantitative and ecological study of the
algae of Huntington Canyon, Emery County,
Utah, was conducted from March 1971 to April
1972. Net plankton, nannoplankton, periphyton,
and visible attached algae were studied. Cer-
tain physical and chemical parameters in the
waters of Huntington Creek and a small pond
along its course were also measured.
Huntington Creek contains a wide diversity
of genera and species of algae. Diatoms are the
main constituent of the flora of this stream
throughout the year. Hydrurus foetidus is preva-
lent in Huntington Creek from late winter to
early summer, and filamentous blue green algae
abound in the summer and fall. Cladophora
glomerata, Oedogonitim sp., and Cham vulgaris
are abundant in the creek beyond the mouth
of the canyon. Most plankton in Huntington
Creek originate on the substrate and in reser-
voirs on the left fork.
Huntington Creek is a cold, fast-flowing,
hard-water mountain stream, and the algal
flora of this creek is typical of such a habitat.
INTRODUCTION
In October 1970 a study of the algae of
Huntington Canyon, Emery County, Utah, was
initiated ( Fig. 1 ) . The need for this study stems
from the construction of a coal-fired power-
generating station and a 30,000 acre-foot reser-
voir by Utah Power and Light Company. The
generating station is located in lower Hunting-
ton Canyon approximately 12 miles northwest
of Huntington, Utah, on land formerly owned
by the Utah State Division of Wildlife Re-
sources and the Bureau of Land Management
(Fig. 2). The Peabodv Coal Company will sup-
ply coal for the generating station from a mine
2.5 miles southwest of the station, and the elec-
tricity will be transmitted south to the Four
Comers area and north to Camp Williams
(Draft Environmental Statement, 1971). When
completed, the station will consist of four gen-
erating units. The first unit will generate 430
megawatts of electricity and will be operational
in 1974. Thereafter, one unit will be completed
during each of three four-year periods. Upon
completion, the station will be capable of gen-
erating 2,000 megawatts of electricity.
The four generators will be cooled with
water taken from Huntington Creek. To insure
Fig. 1. Index map
area.
of the Huntington Canyon study
^Department of Botany and Range Science. Brigliain YounK University, Provo. t'l.ili ^f4(l02
Bricham Young University Science Bulletin
Fig. 2 Mouth of Huntington Canyon on tlio eastern edge of tlie Wasatch Plateau. The Utah Power and Light
Company Generating Station is located at the right center. Photographed Feb. 7, 1972.
that a continuous supply of water will be avail-
able, a new reservoir, called E'ectric Lake, will
be constructed on the right fork of Huntington
Creek approximately 20 miles upstream from
the generating station near the mouth of Bear
Canyon, Emery County, Utah (Fig. 3). The
reservoir will be approximatelv 4.5 miles long
and 215 feet deep at the dam (Fig. 4). It will
store water from the spring nmoff, which will
be released as needed during the summer and
fall months. A paved road will allow access to
the reser%oir, and public recreational facilities
will be provided.
Initial impact of this project on the environ-
ment of Huntington Canyon will result from
the following four factors : ( 1 ) the construction
Biological Sehies, Vol. 18, No. 2 Algae of Huntington Canyon, Utah
Fig. 3. Locality of the dam for Electric Lake on the Right Fork of Huntington Creek below Bear Canyon.
Photographed Nov. 16, 1970.
Bricham Young University Science Bulletin
Fig. 4. Upper drainage of the Right Fork ol Huntjiigtoii Creek. Flat Canyon is at the lower right and James
Canyon is at the left center. Photographed Nov. 16, 1970.
of the generating station itself, which neces-
.sitates extensive excavation and will infringe on
the winter deer range; (2) the scarring of the
mountainside during the construction of the
dam and the relocation of approximately 15
miles of road through heavily forested regions;
(3) the flooding of approximately 4.5 miles of
prime fishing stream on the right fork of Hun-
tington Creek, which currently serves as spawn-
ing grounds for brown and cuttliroat trout; and
(4) the destruction of watersheds along the
patli of the power lines.
Other less obvious effects may occur, espe-
cially in the aquatic environment, which often
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah
becomes a repository for chemical and physical
pollutants entering via effluents, drainage from
surrounding lands, and directly by rain and
snow. The silt load in the creek is an important
factor, especially during construction periods,
causing abrasion and erosion which can be
detrimental to the stream ecosystem. Also, the
release of reservoir water into Huntington Creek
may cause temporary or permanent temperature,
chemical, and/ or nutrient changes which will
affect the ecological balance of the biota of tlie
stream.
Because of the possible environmental effects
of this project, the Center for Health and En-
vironmental Studies at Brigham Young Univer-
sity, with primary funding from Utah Power
and Light Company, undertook a comprehensive
study of the aquatic environment of the Hun-
tington Canyon region in September 1970. The
initial goal of this study was to gather data on
physical, chemical, and biological parameters,
which may be used to determine future changes
in this ecosystem.
Algae are important in such an environmen-
tal impact study inasmuch as they are extremely
responsive to changes in the environment and
thus indicate changes and fluctuations that may
occur. For instance, Blum (1957) found a
marked change in the benthic algal flora as
pollution outfalls entered the Sahne River, Mich-
igan. Foerster and Corrin ( 1970 ) observed that
the presence or absence of certain algae enable
one to determine the condition of the water in
which they are normally found. Palmer ( 1961 )
stated that a knowledge of the algal population
of rivers both quantitatively and qualitatively
is important if one is to assess their true value in
the ecosystem. Pahner ( 1961) fmther stated that
"... it can be important to know the algal
population of a river before any major change is
made in the use of the stream. Also, we need
to know the algal population of rivers through-
out the year and not merely for the simimer
months."
This paper reports the initial algal studies
of Huntington Creek. Future comparative studies
will be made during and after construction and
operation of the power plant-reservoir complex.
The initial goal of this study was to obtain
an overall picture of the entire aquatic algal
flora rather than one specific part. Therefore,
sampling included water chemistry, quantitative
analysis of phytoplankton and attached algae,
and a floristic survey.
Plankton are interpreted in this study as all
organisms found in the open water (Kofoid,
1^)8), and only chlorophyll-bearing phytoplank-
ton (Welch, 1935) are considered in this paper.
Phytoplankton are divided into net plankton
(those forms large enough to be retained by a
67-//,m mesh plankton net) and nannoplankton
(those forms which can pass through the net).
Nannoplankton are of primary importance in this
study, since diatoms, the dominant algae in most
rivers (Rice, 1938), are included in this group.
Sampling of the attached algae included bo£h
microscopic periphyton, defined by Young
(1945) as that assemblage of microscopic or-
ganisms growing upon free surfaces of sub-
merged objects in water, and the visible at-
tached algae.
Floristic sampling was done to determine
the composition and distribution of the algae of
the canyon.
REVIEW OF SELECTED ALGAL STUDIES IN UTAH
Aquatic research in Utah has not been ex-
tensive, although it has included several ecologi-
cal and pollution studies. One significant con-
tribution was made by Clark (1958), who stud-
ied the phytoplankton of the Logan River in
the Bear River Range of the Wasatch Moun-
tains. Clark's results were valuable for com-
parison with those of the present study, since
the two streams are similar in size and certain
other characteristics. A companion study to that
conducted by Clark was completed by McCon-
nell (1959), who estimated the algal productiv-
ity of the Logan River from chlorophyll extracts
of the algae growing on the river bed.
Samuelson ( 1950) completed a study which
illustrated man's influence on the algal floras
in two mountain streams in the Wasatch Moun-
tain Range east of Salt Lake Valley, Utah. He
observed that hvestock grazing and recreation
severely damaged the aquatic ecosystem in
Emigration Canyon as compared to that of Red
Butte Canyon.
Another pollution study (Quinn, 1958) dem-
onstrated that organic wastes from the effluent
of a sugar beet factory were detrimental to the
algal flora of the Jordan River in Salt Lake
County, Utah.
Currently, an algal floristic and ecological
investigation is being conducted along the en-
tire length of the Provo River (Lawson, pers.
comm. ) . This study will establish the algal com-
munities in the river and their responses to
man's use of the drainage area.
More investigations have been conducted
Bricham Young University Science Bulletin
on insects than on algae in Utah streams. These
studies are valuable, since they often include
information on the algae in the ecosystem being
studied and give general information concerning
biological responses to environmental stresses.
One such study was conducted by Smith ( 1959 ) ,
who included algal samples in his macroinverte-
brate study of the Weber River in north central
Utah. His results showed that siltation from
watershed misuse, habitat destruction from
dredging, and stream bottom exposure resulting
from irrigation diversion were more destructive
to the aquatic biota than organic pollution.
An earlier study by Dustans ( 1951 ) on the
Provo River also discussed the effects of dredg-
ing on aquatic life. He mentioned reduced
photosynthesis, loss of marginal vegetation, and
the loss of diatoms, desmids, and filamentous al-
gae as primary contributing causes to the re-
duction of insect benthos in dredged stream
channels.
A pollution studv was conducted in central
Utah on the Price' River (Miller, 1959). Al-
though this river, like Huntington Creek, drains
the Wasatch Plateau, it is of little value for com-
parison with the present study, since the ex-
treme silt load in the Price River and organic
pollution contributed by towns through which
it passes severely restrict biological life. Mil-
ler found only rare and limited amounts of
Cladophora sp. and Chaetophora elegans in the
river and a noteworthy absence of aquatic vas-
cular plants.
Work has also been done on the plankton
of ponds, reservoirs, and lakes of Utah. These
studies include the following: Piranian's (1937)
report on the plankton of the Bear River Migra-
tory Waterfowl Refuge; Chatwin's (1956) study
of the vertical distribution of phytoplankton in
Deer Creek Reservoir, Wasatch County, Utah;
Pratt's ( 1957 ) investigation of plankton periodi-
city in Salem Lake, Salem, Utah; and Longley's
( 1969) discussion of the phytoplankton associa-
tions in Flaming Gorge Reservoir. The infor-
mation provided by these and similar studies
is valuable in understanding stream environ-
ments and communities, since lentic environ-
ments normally exert a definite strong influence
on the streams that drain them. Since several
reservoirs presently occur on the Huntington
Creek drainage, and a new one (Electric Lake)
is under construction as of 1972, their manage-
ment and algal populations need to be con-
sidered as factors affecting the physical and bio-
logical parameters of Huntington Creek itself.
Mention should also be made of some im-
portant taxonomic references concerning Utah
algae. The most significant contribution in this
regard was made by Dr. Seville Flowers who
published mimeographed keys to the common
algae of Utah (n.d., a) and to the blue green
algae of Utah, (n.d., b). Flowers has also re-
ported on the nonvascular plants of various re-
gions of the state ( 1959, 1960 ) . Two other taxo-
nomic studies are those by Norrington (1925)
and Coombs (1964) of the Wasatch and Uinta
Mountains, and the Western Uinta Mountains,
respectively.
DESCRIPTION OF THE HUNTINGTON CANYON DRAINAGE
Geology
Huntington Creek is one of many streams
that drain the Wasatch Plateau of central Utah.
This plateau is the northernmost of the plateaus
of Utah and is situated in the central part of the
state between 30 and 40 degrees north latitude
and 111 and 112 degrees west longitude. It
merges northward with the higher land of the
Uinta Basin and is separated from the Fish
Lake Plateau to the south by a 20-mile-vvide
erosional depression. The Wasatch Plateau,
which rises to elevations of 11,000 feet above
sea level and 5,000 to 6,000 feet above Castle
Valley on the east and Sanpete Valley on the
west (Spieker and Reeside, 1925), is essentially
a tableland 90 mik^ long and 20 to 30 miles
wide (Figs. 5-6). Strata in the plateau are
mostly Late Cretaceous and Early Tertiary in
age and lie flat or dip at moderate angles. Re-
sistant rocks alternate with those less resistant,
giving cliff, bench, and slope profiles much like
those of the Colorado Plateau (Spieker and
Billings, 1940). Castle Vallev on the east is of
erosional origin. The western edge of this valley
exhibits a sharp profile, since the eastern edge
of the Wasatch Plateau drops abruptly through
horizontal strata from one formation to another
( Fig. 2 ) . Sanpete and Sevier Valleys, west of
the plateau, arose from down folding and fault-
ing, with the western front of the plateau itself
being a great monoclinal flexure. Otlu^ faults
nnming through the plateau have created ir-
regularities in stratigraphy, and erosion has
carved canyon, cliffs, and gullies throughout the
area (Dutton, 1880).
The eastern slopes of the Wasatch Plateau
are dissected bv deep, rock\' gorgt»s with fast-
flowing streams similar to lower Huntington
Biological Series, Vol. 18. No. 2 Algae ok Huntington Canyon, Utah
Fie 5 North central portion of the Wasatch Plateau sliowing the Huntington Creek drainage. Left Fork of
Huntington Creek is at A, Right Fork of Huntington Creek is at B, Nuck Woodward Canyon is at C,
North Hughes Canyon is at D and Candland Mountain is at E. Photographed i-eb. 7, 197Z.
Creek The eastern face of the plateau consists of the eastern slopes of the plateau. The San
of sharp cUffs of Starpoint sandstone and rough Rafael River drains into the Green River, which
erosion of the uppermost layers of Mancos in turn feeds the Colorado River. Streams of
shale. From the mouth of Huntington Canyon, the western slope of the Wasatch Plateau dram
Castle Vallev extends eastward toward the San into the San Pitch and Sevier rivers.
Rafael River (Fig. 7), which collects the waters Spieker and Billings (1940) described the
of Huntington Creek and other drainage waters stratigraphy and thickness of each formation
Bricham Young Univehsity Science Bulletin
>
Fig. 6. Eastern edge of the Wasatch Plateau and Lower Huntington Canyon looking eastward toward the San
Rafael Swell. The Left Fork of Huntington Creek is at the lower right, the right fork is at the lower left
and Tie Fork Canyon is at A. Photographed Feb. 7, 1972.
of the Huntington Canyon section of the Wa-
.satch Plateau as follows:
Paleocene
Flagstaff limestone. Gray, tan, white
limestone, with minor amounts of shale
and sandstone; lacustrine 300-500'
Upper Cretaceous and Paleocene
North Horn formation. Buff, gray, red
sandstone, gray to variegated shale,
conglomerate, some limestone; flood-
plain and lacu,strine in origin
Upper Cretaceous
Price River formation.
Upper member: Gray sandstone and
conglomerate with minor amounts of
shale
2000'
600'
Castlegate sandstone member: Massive,
cliff-forming gray sandstone, coarse
grained to conglomeratic 300'
Blackhawk formation. Medium-tcnfine-
grained buff and gray sandstone, gray
shale, coal 1500'
Starpoint sandstone. Massive, cliff-
forming buff sandstone, medium-to-
fine grained; marine 450'
Mancos shale. Gray marine shale (only
uppermost pat^ exposed in area
described) 4000' -\-
The upper portion of the Huntington Creek
drainage (Fig. 8) is mostly North Horn sand-
stone and shale with glaciated cirques, moraines,
and widened valleys with outwash deposits of
Biological Series, Vol, 18, No, 2 Alcae of Huntington Canyon, I'taii
Fig, 7, Mouth of Huntington Canyon looking across Castle Valley toward the San Rafael Swell, Photographed
Feb, 7, 1972,
Pleistocene age (Spieker and Billings, 1940).
Most cirques occur in Joe's Valley Graben, a
vertically displaced fault block in the central
part of the plateau. This graben averages 2.5
miles wide and extends south for 60 miles from
the north central part of the plateau (Spieker
and Billings, 1940). Most glaciers issued east-
ward from the western edge of the plateau
into the graben valk'\-, often coalescing to form
large sheetlike moraines. Stream notches in many
of these moraines have been dammed in recent
years to foma storage reservoirs, such as Cleve-
land and Huntington reservoirs.
The left fork of Huntington Oeek drains the
northern part of tliis graben and the slopes that
rise from it. The headwaters gather from Spring,
Lake, Rolfson, and Staker canyons, flow across
the graben valle\ , and descend through a rocky
gorge approximatel)' 3,000 feet deep (Spieker
and Billings, IMO).'
The headwaters of the right fork of Hun-
tington Creek arise north of the termination of
Joe's Valley Graben, which ends at Cleveland
Reservoir. The right fork origmates in narrow
rocky canyons in the Price River sandstone but
flows early into Blackhawk sediments where
the stream channel widens into a broad U-
shaped valley (Fig. 9). This valley remains
prominent to Bear Canyon, where it narrows
again to a V-shaped mountain gorge (Fig. 10).
This flat-bottomed valley was created by lateral
erosive cutting by glaciers in this canyon.
10
Bricham Young University Science Bulletin
"Xfea.
Fig. 8. Geologic map of part of the Wasatcli Plateau, Utah (after Spieker and Billings, 1940).
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah
11
Fig. 9. Glacier cut U-shaped valley in the upper drainage of the Right Fork of Huntington Creek. Northern
end of Joe's Valley Graben is at the upper right. Photographed Nov. 19, 1970.
12
Bricham Young University' Science Bulletin
Fig. 10. Deep gorges of Huntington Canyon. Pole Canyon (A), Left Fork (B), Horse Creek Canyon (C), Tie
I^ork Canyon (D). Photographed Feb. 7, 1972.
Climate and Vegetation Zones
Tlie upper part of the drainage of Hunting-
ton Creek exists under semihumid montane con-
ditions, with 30 to 40 inches of precipitation
annually (Draft of Environmental Statement,
1971). A large snowpack accumulates in this
region in the winter, creating a high spring
runoff supphing ground water which feeds
local springs throughout the year. Aspen-snow-
berr\- ( Populus tremttloides-Stjinphoricarpos vac-
cinoides) associations are scattered throughout
this upper drainage with populations of sub-
alpine spruce ( Picea engelmannii ) on the north-
other slopes and in the open valleys (Figs. 11-
12). Wet meadows and willows are common
along gendy flowing streams and in pockets
formed from Pleistocene glaciation.
Lower Huntington Canyon exhibits a semi-
arid climate with approximately 12 inches of
precipitation amuially. Pinyon-juniper [Pinus
monopJiyUa-Junipcrus osteosperma) and sage
{Artemesia tridentata) communities are the
dominant vegetation types here, with cotton-
woods (Populus angustifolia) often hning the
streams in the canyon bottoms (Fig. 2).
em slopi^ and sagebrusli-grass communities on
Castle Valley is flat and arid with a few
scattered small towns. It provides some pasture
Biological Series, \'ol. 18, No. 2 Algae of Huntington Canyon, Utah
13
Fig. 11 . North Hughes Canyon looking northeast from the Right Fork of Huntington Creek toward the Book Cliffs
(in the background) showing spruce-aspen forest cover. Photographed Nov. 16, 1970.
14
Bricham Young University ScitNCE Bulletin
<t
■'h
^3
Fig. 12. Right Fork of Huntington Creek at James Canyon. Photographed Nov. 16, 1970.
Biological Series, Vol. 18. No. 2 Alc.\e of Huntington Canyon, Utah
15
land and crop land for alfalfa, com, and other
grains, utilizing irrigation water supplied from
streams draining the eastern slopes of the Wa-
satch Plateau. Much of the lower slopes of the
eastern face of the Wasatch Plateau and
the Castle Vallev floor are composed of Man-
cos shale deposits. Since these rocks are rich in
carbonates and other easily dissolved mineral
salts, the streams passing through them are
greatly influenced and become less desirable for
agricultural uses. Because of this, much of the
irrigation water used in Castle Valley is obtained
via canals from storage reservoirs and streams
further up the canyon where the water is of
higher quality.
Description and Uses of Huntington Creek
The present study is mainly concerned with
the right fork of Hunrington Creek and its main
course below the junction of the two forks, since
these will be influenced directly by the Utah
Power and Light Company project. As men-
tioned, the upper reaches of the right fork are
gentle and smooth flowing, becoming torrential
upon descent through deep canyon gorges. From
the headwaters of the right fork until it joins
the San Rafael River, Huntington Creek is ap-
proximately 50 miles long and drains approxi-
mately 320 square miles. The lengtii of the creek
sampled during this study extended from the
mouth of Bear Canyon downstream approxi-
mately 35 miles to the town of Lawrence on the
western edge of the San Rafael Swell.
The Huntington-Fairview Forest Highway
follows Huntington Creek and its right fork
rather closely and is paved from its junction
with Utah Highway 10 at Huntington to two
miles above the junction of the right and left
forks. Plans for the future in this area include
an all-weather road across the summit, linking
Huntington and Fairview (Draft of Environ-
mental Statement, 1971). Many campgrounds
and picnic areas presently occur along the creek,
and these facilities are well used, especially on
summer and fall weekends. The stream and
neighboring reservoirs are stocked and managed
by the Utah State Division of Wildlife Re-
sources and provide some of the best fishing in
eastern Utah. The upper reaches of the right
fork provide excellent spawning grounds for
German brown and cutthroat trout, and the
natural channel of the creek provides good hab-
itat for aquatic insects, which contribute to a
productive environment for fish. The upper val-
le\s are also used for summer grazing of cattle
and sheep.
Cleveland, Miller's Flat, Rolfson, and Him-
tington Reservoirs on the left fork of Hunting-
ton Creek are maintained and managed by the
Huntington-Cleveland Irrigation Company to
supply water to the communities and farms of
Castle Valley. These reservoirs achieve some
control of the spring runoff and allow a con-
stant flow to Castle Valley through the summer
and fall dry period. Most of the water released
by these reservoirs, as well as water from Hun-
tington Creek proper, is diverted from the creek
into a canal by a diversion dam located four
miles northwest of Huntington. This canal emp-
ties into North Huntington Reservoir northeast
of the town of Huntington. The water stored
there is used for agricultural purposes in Castle
Valley. Below this diversion dam the stream
flow is greatly reduced but increases slightly as
it gathers drainage waters from the surrounding
land and springs along its course. The water
in this lower portion of Huntington Creek is
greatly affected bv this drainage water and is
generally of low qualit\-.
Water discharge in Huntington Creek fluc-
tuates greatly with the seasons. Discharge mea-
surements have been made at two localities
along the creek. Utah Power and Light Com-
pany took readings at the site for Electric Lake
on the right fork just below the mouth of Bear
Canyon. Tlie U.S. Geological Survey took read-
ings at Station 9-318, located seven miles north-
west from the town of Huntington and one
mile upstream from Fish Creek. The average
yearly flow for the Electric Lake locality was
30.3 cubic feet per second for the period 1968
to 1971. The average monthly mean reached a
high over this same time period of 159.7 cfs at
spring flood in May and a low of 7.8 cfs in
January. Water flow near the mouth of the can-
yon (U.S.G.S. Station 9-318) showed a yearly
average of 100 cfs for the years 1966 to' 1971,
with the monthly mean being high in May at
309 cfs and low in January and February at
27 cfs. The six-\'ear high was in May 1969, when
the discharge was 552 cfs. The six-year low was
in Februan- 1966, when the water level dropped
to 18 cfs.
Observations of the creek throughout the
1971-72 study period supported the water flow
data. Heav)- spring runoff began in early April
1971, and reached a peak during May and early
June. A significant drop in water flow was
noted on Juno 29, 1971, followed by a gradual
decline during the summer and fall to winter
lows in Januarv- and February 1972. The summer
decline in the main creek was less severe than
that of the right fork because the natural drain-
age of the main fork was supplemented with
16
BiucHAM YouNC University Science Bulletin
Fig. 13. Index map of Huntington Canyon drainage.
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah
17
water from the reservoirs on the left fork. The but an early thaw opened a major part of the
river was completely frozen by December 1971, creek channel in February 1972.
DESCRIPTION OF SAMPLING SITES
Sampling sites were chosen to represent a
variet)- of different ecological niches along the
drainage. Seven sites were estabhshed for quan-
titative study, which were numbered beginning
downstream at Lawrence and proceeding up
Huntington Canyon to the mouth of Bear Can-
yon (Fig. 13). Tliis was also the general order
followed during sampling.
Lawrence (Site 1)
This site is located on Huntington Creek 4.7
miles southeast of Huntington, Emery County,
Utah, and 1.5 miles east of Lawrence, Emery
Countv', Utah. It is approximately nine miles
below the main diversion dam on Huntington
Creek and was established to monitor effects of
agricultural drainage and increased dissolved
minerals on the algal flora. The actual sampling
site was located in a pasture through which the
creek meandered near the intersection of Hun-
tington Creek and a road leading to the San
Rafael Swell (Fig. 14). The average width of
the creek at this locahty was 22 feet during the
spring flood and 15 feet during low water
periods. Average water depths during the same
periods were 22 and 13 inches, respectively.
This site included slow-flowing deep water and
lli-1
A-r
^;.A.wJ*Jft
Fig 14. Huntington Creek 47 niileb, southeast of Hun-
tington. I'tah. Locality of collecting site 1. Photo-
graphed April 28. 1972.
swifter-flowing shallow riffles, providing varied
algal habitats. A sharp, eroded bank character-
ized the west side of the stream, whereas the
east bank sloped gradually into a pasture. Popu-
lus angustifolia, Tamarix pentandra, Chrijsotham-
nus tmuseosus, and Artemesia tridentata oc-
curred along the banks throughout this area.
The stream bed here consisted mostly of silt and
sand, with small stones in the riffles, and the
water was generally of low quality. In talking
with the rancher who owns the land at this
locality, he mentioned that over the last few
years his cattle will no longer drink the water
from the creek unless they have no other source.
This is probably due to the diversion of the bet-
ter quality water upstream, and perhaps to the
addition of organic pollutants by Huntington
City.
Highway 10 Bridge (Site 2)
Tliis site is located four miles upstream
from Lawrence and is 0.3 mile northeast of Hun-
tington on Utah Highway 10 at the crossing of
the creek by the road. Samphng at this site in-
cluded water chemistry, visible attached algae,
and floristics. It was established to augment the
data collected at site 1 and was similar to it in
most respects. The bottom was silty in the slow
areas and rocky in tlie faster water. The aver-
age width was 35 feet in the spring and 16 feet
in the summer and winter, and the average
depth was 12 to 18 inches and 5 to 7 inches, re-
spectively, during the same periods. Streamside
vegetation was similar to that of site 1 except
that a large grove of cottonwoods created some
shading effect at this site.
Plant Site (Site 3)
This site is located approximately three miles
above the North Huntington Reservoir diversion
dam about three-fourtlis of a mile downstream
from the Utah Power and Light generating sta-
tion, at an altitude of 6,.300 feet above sea level.
It is approximately 0.3 mile below the entry
of Deer Creek, which drains the mountains west
of the generating station (Fig. 15). The river
at this location was basically deep and fast flow-
ing, although some swift riffles were present.
The average depth of the creek at this site was
three feet during the spring flood when it was
25 or more feet wide. In the low flow period.
18
Bitir.iiAM Yni'Nr: I'niversitv Scikncf. But.LETiN
Fig. 15. Utah Power and Light Company Generating Stntioii. Deer Creek (A), transmission lines (B), collect-
ing site 3 (C). Photographed Feb. 7, 1972.
Bioi.oGicAi. Series, Vol. 18, No. 2 Alg.\e or Huntincion Canyon, Utah
19
it was usually less than 1.5 feet deep and about
20 feet wide. The bottom was strewn with large
and small stones, and many large boulders pro-
truded from the water. This site often showed
siltation resulting from construction, and pollu-
tion from Deer Creek, which carried coal dust
and other pollutants originating from mines
above the generating station. The water here
was often turbid with suspended sediments, and
the bottom generally showed coal dust deposits.
Terrain surrounding this site included steep
banks on the west side of the stream with a
more gentle incline on the east. Terrestrial vege-
tation here was dominated by Pinus monophyUa,
Juniperus osteospermum, Arteinesia tridentata.
with Poptihis angustifolia abundant along the
stream channel. This site was established to
monitor the effects of construction and opera-
tion of the generating station on the algal flora
of the creek.
Bear-Rilda Campground (Site 4)
This site is located approximately two miles
above the generating station between Bear
Creek and Rilda Canyons at an elevation of
6,600 feet above sea level (Fig. 16).
The creek at this campground was character-
ized by a deep-flowing chamiel, a shallow rif-
fle, and a deep pool, thus providing a variety of
Fig 16 Huntington Canvon above Bear Creek Canyon (A) showing collecting site 4 (B). Photographed Feb. 7,
1972.
20
habitats. Tlio stream here was bordered by a
broad flood plain and averaged about 2 feet
deep and 55 feet wide at spring flood. During
low water the riffle area became exposed when
the current was limited to a narrow channel.
The average width during this period was 11
feet and the depth 1 foot. The pool at this site
collected sediment and exliibited a deep accumu-
lation of silt. The bottom over much of the rest
of the stream, especially in the riffle, was cov-
ered with small stones. Willows ( Salix sp. ) and
cottonwoods ( Populus angtistijolia ) were abun-
dant on the banks, and a large thicket of Rus-
sian Olive (Eleagnus angiistifolia) was present
( Fig. 17 ) . Leaves from these trees contributed
to the detritus in the stream during the fall
months, and the trees were responsible for some
shading throughout the year, particularly in the
spring and summer.
Tie Fork Pond (Site 5)
This site is a small shallow pond located at
the mouth of Tie Fork Canyon at 7,300 feet ele-
vation, six miles upstream from the generating
station (Fig. 18). Tliis pond is fed by drainage and
seepage from the surrounding hillsides and in
turn drains into Huntington Creek via a culvert.
This site was established to provide infonnation
concerning the composition and seasonal fluctua-
tions of algal populations characteristic of some
of the ponds and backwaters occurring along
the creek drainage. Heavy growths of Potomo-
geten, Cham, and filamentous algae dominated
the vegetation in this pond during the summer
Bbicham Young University .Science Bulletin
Fig. 17. Huntington Creek at collecting site 4. Photo-
graphed Feb. 7, 1972.
Fig. 18. Tie Fork Pond just west of the mouth of Tie
Fork Canyon. Photographed April 28, 1972.
months, and a thick accumulation of organic
mud from decomposition lined its bottom. The
water level here was high in the spring, became
quite low during the summer, and rose again
in the fall. It was completely frozen from No-
vember 1971 to March 1972.
Stuart Fire Station (Site 6)
This site is located on the right fork of Hun-
tington Creek 1.5 miles below Stuart Fire Sta-
tion at an elevation of 7,700 feet (Fig. 19). The
creek meandered through this portion of the
canyon and was less turbulent than downstream
(Fig. 20). The site included a riffle with small
stones and a deep-flowing channel with larger
rocks providing good habitat for the attachment
of visible bcnthic algae and diatoms. The right
fork at this site averaged 25 to .30 feet in width
and about 1 foot in depth throughout most of
the year. A steep mountain slope covered with
sage, grasses, and spruce rose from the south-
west bank, whereas the northeast bank was
lined with willows and gently rose a few feet to
the canyon floor. This was the highest eleva-
tion in the canyon that could be reached during
winter months.
Bear Canyon (Site 7)
This site is located on the right fork near
the mouth of Bear Canyon at the present junc-
tion of the Huntington-Fairview Forest High-
way with the Miller's Flat road (Fig. 21). The
elevation here is S,4(X) feet. This portion of the
Biological Series, Vol. 18, No. 2 .^lcae of Huntington Canyon, Utah
'■*«-#^?»igfe._^.
21
<^
^'
■X
■**-—.«.
'■J^-'^'' •'■''■ ijN-i ' ■
Jfe'^^?"
'•-'''V!^^'. , y-«^^;.-'i-'^^<.
^«V' „,*'?
Fig. 19. Right Fork of Huntington Creek. Nuck Woodward Canyon is at the right center of the photograph,
Stuart Fire Station is at A and collecting locality 6 is at B Photographed Nov. 16, 1970.
22
Bricham Young UNrvERSiTv Science Bulletin
creek averaged 20 feet wide and less than 2
feet deep throughout the study. The bottom
was sandy in slow areas and covered with small
stones in the riffles. A clay shelf along part of
the channel supported growths of benthic Chlo-
rophyta during much of the growing season.
Stream banks at this site were vertical and un-
dercut, rising approximately 10 feet above the
stream channel. The creek valley here is wide
with grass-covered low hills rising gently to
the mountains. This site is located at the tran-
sition zone between the broad U-shaped valleys
of the upper drainage and the deep gorges of
the lower canyons. It was added to the previous
six sites in June 1971 to sample the flora of the
upper drainage and for comparison with site 6.
From December to June, this site was inacces-
sible due to snow pack.
METHODS
Physical and Chemical Measurements
Physical and chemical sampling was initiated
on June 8, 1971, at sites 1, 3, 4, 5, and 6; and sites
2 and 7 on August 20, 1971. Measurements were
taken during each collecting trip until the study
was terminated in March 1972. However, site 7
became inaccessible after November 1971; and
site 5 was frozen from November to March of
the study period.
Temperature. Water temperature was recorded
at each sampling station in degrees centigrade.
Turbidity. Turbidity was measured using the
colorimeter in a Hach model DR-EL portable
water engineer's laboratory. Turbidity was ex-
pressed in Jackson turbidity units (JTU) as a
measure of the intensity of light scattered by
particles suspended in the water.
Water Chemistry. The pH was tested using a
Sargent-Welch pH meter. All other chemical
Fig. 20. View down the Right Fork of Huntington
Creek from collecting site 6. Photographed April
28, 1972.
tests were run following standard methods
(Amer. Public Health Assoc, 1971) using a
Hach Model DR-EL portable water engineer's
laboratory. Tests were run for the levels of dis-
solved oxygen, carbon dioxide, nitrate, ortho and
meta phosphate, silica, calcium and magnesium
hardness, alkalinity, and sulfate.
The amount of oxygen dissolved in the
water was tested in the field, since biochemical
and chemical oxygen demand can alter the dis-
solved oxygen content of a stored sample. All
other tests were completed in the laboratory
upon returning from the field.
Phytoplankton
Phytoplankton studies were divided into net
plankton and nannoplankton. Traditionally this
division is determined by the ability of nanno-
plankton to pass through the meshes of bolting
cloth No. 25, which has meshes measuring 0.04
to 0.05-mm square (Ward and Whipple, 1918).
This classification will be altered here so that
nannoplankton will include all diatoms regard-
less of size, and other algal forms too small to be
adequately sampled with a 0.067-mm mesh
plankton net.
Net Plankton. Net plankton were collected by
filtering 40 liters of water through a 67-/im mesh
plankton net. Tlie 4()-liter sample was collected
by scooping an 8-liter bucket of river water
from five randomh' chosen sections at each
sampling site. Tlie concentrated sample was
collected in a .30-ml vial attached to the net.
Care was taken to wash the net witli filtered
water to remove anv organisms that might cling
to it. The vials were transported to the labora-
tory where net plankton were examined and
enumerated. Since it was possible to count net
plankton soon after returning to the laboratory,
preservatives were not used on these algae.
Tlie 40-liter quantitative sample (Clark,
1958) is similar to the plankton pump method
described by Ward and Whipple (1918). This
method is superior to plankton net tows used
BiOLOCiCAi, Series, Vol. 18. No. 2 Algae of Huntington Canyon, Uiaii
23
Fig. 21. Right Fork of Huntington Canyon at junction with Bear Canyon (A). Collecting site 7 is at B, the
dam of Electric Lake is at C and North Hughes Canyon is at D. Photographed Nov. 16, 1970.
24
Brigham Young University Science Bulletin
by Kofoid (1908), Allen (1920), and others,
since a known volume of water is filtered and
the chance of error from an uncertain amount
of water passing through the plankton net is
eliminated.
Enumeration of net plankton was done using
a Sedgwick-Rafter counting cell. This counting
cell is commonly used for plankton studies (Ko-
foid, 1908; Allen, 1920), and many different
counting procedures have been adapted to it.
The counting method used for this study was
adapted from Weber ( 1970 ) . After thoroughly
mixing the 30-ml vial of concentrated river
water, a 1-ml aliquot was pipetted into the
Sedgwick-Rafter cell. The sample was counted
at 100 magnifications under the microscope. An
ocular micrometer was used to measure a width
of 1 mm on the slide, and two or more longi-
tudinal transects across the slide were made.
Algae encountered during these transects were
identified, and the number of occurrences of
each genus or species was recorded. From the
total, an average number of organisms per single
50-mm transect was calculated, and from this,
the number of organisms per liter of river water
was determined.
Occasionally, it was necessary- to modifv
these procedures slightly. During the summer
months the density of net plankton at site 5
(Tie Fork Pond) required dilution of the 30-ml
concentrate. In September and October the
sample size at Tie Fork Pond was reduced from
40 liters to 24 liters in order to reduce algal den-
sity in the sample. Because of low frequency and
low total number of organisms, samples taken
during the winter months were concentrated by
centrifugation to 5 or 10 ml to increase sensi-
tivity during counting.
Nannoplankton. Nannoplankton were collected
by obtaining 1 liter of river water from each of
four randomly chosen sections at each site. This
sample was placed in a gallon container and re-
turned to the laboratoiy. Two liters of this
sample were then suction filtered through a
membrane filter with a pore size of 1.2-,"m. This
filtering process removed all phvtoplankton and
much (>xtrancous suspended matter from the
water. The filters were cleaned using distilled
water, and the resulting suspension centrifuged.
The excess water was carefully decanted, and
the pellet was resuspended in 5 ml of standard
formalin-alcohol-acetic acid (FAA) to preserve
it or in 5 ml of distilled water, if counting was
done immediately.
Nannoplankton were counted using a Pal-
mer nannoplankton counting slide (Palmer and
Maloney, 1954). This slide is designed for use
with high power dr\' microscope objectives and
allows for higher magnification and resolution
necessary to identify and count nannoplankton
genera. All nannoplankton observations and
counts were made at 400x. An ocular micrometer
was used to measure a 0.25-mm width on the
Palmer slide, and the algae encountered in four
transects of this width were counted across the
diameter of the slide. From the four counts, an
average count per transect was then computed.
In most cases a new aliquot was used for each
count, and the samples were always thoroughly
mixed before the alicjuot was taken to maximize
the chances for uniform distribution of the sus-
pended organisms.
Furthermore, averaging the number of algae
c^ncounterc^d in four transects increased the
probability of obtaining an accurate representa-
tion of algae actually found in the river and
reduced abnormal values due to clumping. The
number of algae encountered in each transect
was tallic^d separately as a check on the preci-
sion of the counts, and, in most cases, relatively
little variation occurred between the four counts.
As mentioned previoush'. all diatoms were in-
cluded in these nannoplankton investigations,
as well as algal forms too small to be adequately
retained in the plankton net. Since the original
sample was taken directly from the river, net
plankton forms were encountered during nanno-
plankton enumeration. These were not included
in the nannoplankton computations, although
they did provide a check on net plankton studies.
Turbidity was a noteworthy problem during
nannoplankton investigations since most sus-
pended particles were retained by the filters.
Silt and sand particles, which were especially
prevalent during the spring lainoff, often ob-
scured the algal specimens and made it neces-
sary to dilute samples to 10 ml, 15 ml, or 20 ml.
In rare eases, higher dilutions were necessar)'.
Pemianc^nt diatom slides were made from the
nannoplankton samples from September 1971 to
March 1972 so that a permanent record of the
plankton flora would be available. Methods
have been described by Weber (1970) and
Patrick et al. (1954) to count diatoms and char-
acterize diatom floras from prepared slides. Such
studies may be undertaken at a future date, and
the slides are also valuable to compare with
future collections. All diatoms were mounted in
Pleurax (Hanna, 1949). This mounting medium
has a very high index of refraction (1.770) and
greatly facilitates resolution.
Periphyton
Sampling of the periphxton community has
received the attention of many workers in recent
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah
25
years, and many variations in sampling methods
have been attempted. Sladeckova (1962) sum-
marized techniques ajid materials developed in
periphyton work. Recent trends have been to
submerge artificial substrates at study sites to
obtain both a qualitative and quantitative con-
cept of periphyton communities from studying
the algae that become attached to these sub-
strates. Materials such as wood, slate, concrete,
asbestos, asbestos cement, various sheet metals,
plastics, celluloid, st\'rofoam, and glass have
been used. However, smooth glass is most wide-
ly used and has given accurate results. Patrick
et al. (1954) found that by using glass slides
for sampling periphyton they were able to
sample 75% to 85% of all species obtained by
other collections, and 95% of those species with
more than eight individuals per sample. Dor
( 1970 ) compared glass slides with basalt and
limestone substrates in Lake Tiberia in Israel
and found that production on slides was 73%
of that produced on natural substrates. Odum
(1957) found that succession of algae on glass
slides was similar to that on Sagittaria plants.
In general, Whitf ord and Schumacher ( 1963 )
found that colonization on glass slides was simi-
lar to that of rock substrates, although it was
somewhat different from colonization observed
on hving plants.
Under certain conditions, glass may be sur-
passed by styrofoam as a colonization substrate
for periphvton, especiallv diatoms. Holm and
Hellerman'(1963) found that at 16° and 25°C,
both substrates gave reprcsentarive colonies; but
at 3°C, diatom species diversity on the glass was
reduced as much as 40% while the sts'rofoam
continued to support a representative flora.
However, Dillard (1966) reported glass to have
higher diatom populations at both high and low
temperatures.
The means of attaching slides to the sub-
strate has also resulted in the development of
many devices. Butcher (1932), who did a pio-
neer river study using glass slides to sample
periphvton, used a frame attached to tlie river
bed to support his slides. Patrick ct al. (1954)
developed a special apparatus for holding slides
in the water which they called the Catherwood
diatometer. This apparatus consists of a plastic
rack with attached floats so that it can be sus-
pended at desired depths in the water. Slides
are placed vertically in the rack, which allows
diatoms to colonize the slides and concurrently
reduces silt deposition. Weber and Raschke
(1970) described a similar apparatiis with styro-
foam floats as a standard periphyton sampler
for pollution surveillance. In Huntington Creek
the current is extremely swift during runoff
and quite low in tlie summer and fall. In
addition, the stream and canyon are heavily
used by campers, picnickers, and fishermen; and
a periphyton sampling device such as described
above is impractical.
Consideration has also been given to the
length of time the slides should be left in the
water. Patrick et al. (1954) found two weeks to
be optimum, since by that time diatom diver-
sity had been established and longer periods
had been allowed for excessive silt and debris
deposition. Newcombe (1949), on the other
hand, suggested 25 days to be the optimum
time period. Patrick et al. (1954) found that
the accumulation of debris and other organisms
on the slides over a long time period made them
less favorable for diatom growth, and the more
adapted species actually crowded others out.
However, a longer time period allows dominant
species to become well established on tlie slides,
and this may actually be an advantage in aid-
ing an understanding of relationships between
periphyton and the periphyton-influenced plank-
ton assemblages.
Newcombe (1949) discussed the advantages
of vertical placement of the slides versus hori-
zontal placement, claiming the latter to be best
since production was higher and the results
were more reproducible. However, Hohn and
Hellerman ( 1963 ) reported no appreciable dif-
ference due to slide placement, and since silt
accumulation on horizontal slides presents a
problem, vertical placement is often used. Peri-
phvton slides in the present study were oriented
both horizontally and vertically, and no appre-
ciable difference in silt accumulation or diatom
populations was observed.
Periphyton sampling techniques used in the
present studv were similar to those used by
Whitford and Schumacher (1963). Clean 1" x
3" microscope slides were fastened to a length
of copper or stainless steel wire by means of
electrician's tape. The slides were then secured
in the river bv fastening the wire to submerged
sticks, large stones, or other convenient objects.
Generally, the slides were allowed to drift free-
Iv in the current. Four slides were placed in the
water at each site monthly and retrieved the fol-
lowing month. Both sides of the slides were
cleaned with distilled water in the laboratory,
and the attached algae were preserved in 10 ml
of FFA until counting could be done. Samples
were counted using a Palmer counting slide, and
procedures similar to those used in counting
nannoplankton were followed, except that all
algal forms encountered were identified and re-
corded.
26
Bricham Young University Science Bulletin
In computing the algal totals, an average
number of individuals per transect across the
Palmer slide was made from four individual
counts. Periphyton were computed in number
per cm-. This counting method was used because
it is the most precise commonly used method
(Sladeckova, 1962) and it correlated with the
nannoplankton procedures, thus allowing the
establishment of accurate relationships between
periphyton and plankton assemblages.
Difficult)' was often encountered due to ex-
cessive silt deposition on the slide, which ap-
parently was entrapped by mucilage secreted by
the algae. Dilutions beyond 10 ml were often
necessary for accurate counting, although dilu-
tions were kept as low as possible.
Data presented from periphyton studies were
obtained from counts on slides taken as much
as possible from one specific location at each
site. These data characterize the general peri-
phyton flora of the area but certainly are not
representative of every available ecological con-
dition. Slides submerged at site 1 were sus-
pended in slow, evenly flowing water. Those at
site 3 were in deep fast-flowing water. Shdes
from site 4 were in a deep hole where the water
was quiet and in a shallow riffle. Slides from
site 6 were in a shallow riffle, and slides from
the pond (site 5) were submerged just below
the water surface in still water.
Visible Benthic Algae
Visible benthic algae, including such forms
as Cladophora, Chara, and Hydrurus were
sampled following the methods of Blum (1957)
and Dillard (1966), combining quadrat and
line transect methods for studying plant com-
munities. Transects were chosen across the
stream at right angles to the current flow in
areas displaying average growth conditions. The
percent coverage of the substrate by each genus
encountered was estimated in alternating 10-cm
by 25-cm plots along this transect. Macroscopic
benthic algae were always most abundant in
riffles, and so one or more representative tran-
sects of a riffle were taken at each study site.
At sites 1 and 2 slow water also supported sig-
nificant algal growths. Transects were run in
these slow water areas as well as in riffles at
these sites, and the results were averaged to
give a figure representative of the site as a
whole.
From data gathered it was possible to calcu-
late cover, composition, and frequency of each
genus on the stream substrate. The frequency
percent for each genus was obtained by dividing
the total number of quadrats in the transect into
those quadrats in which each genus occurred.
The cover percent for each genus was deter-
mined by assigning coverage classes (Dauben-
mire, 1968) to the estimation of each genus re-
corded in the field and then averaging the mid-
points of these coverage classes. From the cover
percentage, the percent composition of the total
communitv represented bv each genus was de-
termined bv dividing the total cover into the
cover of each genus and multiplying by 100.
This method of estimating cover in each
quadrat gave more accurate information than
Blum's (1957) method of onlv recording the
presence or absence of a species beneath the
plots.
Where the water was deep and swift, this
sampling method was not applicable. Turbid
waters also hindered its use, altliough a glass jar
submerged in the water enhanced visibility.
Floristic Sampling
Samples were taken from rocks, twigs, sand,
and macroscopic vegetation at fourteen sites
along the creek. Seven of these sites corresponded
with the seven quantitative sites; and the other
sites represented ponds, backwaters and other
areas where algae were found growing. Floristic
sampling began in October 1970 and continued
throughout the study. Tlie algae in these samples
were identified to species in the laborator)-.
Samples of man\- filamentous algae were pre-
served in FAA solution, and pennanent diatom
slides were made.
RESULTS AND DISCUSSION
Each site in this study was chosen to repre-
sent a unique ecological habitat. Consequently,
each site was studied with the view in mind to
characterize the complete alga! communitv' and
ecological parameters found under each set of
conditions. The following discussion therefore
treats the algolog\' and ecology' of each site of
the studv area.
Lawrence (Site 1)
The algal flora at Lawrence is dominated by
macroscopic species including Cladophora
glomerata, Oedogonhim sp. and Chara vulgaris
and bv many diatom genera. Cladophora glom-
erata was first recorded from floristic samples
in April 1971. B\- Ma\- it was prevalent among
the rocks on the stream bottom (Fig. 22). The
BioLocicAi. Series, Vol. 18, No. 2 Alg.^e of Huntington Canyon, Utai
27
iignnl
Fig. 22. Cladophora glomerata attached to a stone at
site 2. This photograph was taken in the spring
when Cladophora began to be prominent in the flora,
and the alga is approximately one half as long as
it is at maturity. Photographed April 28, 1972.
first quantitative sample in June showed this
alga to cover 35% of the stream bottom in riffle
areas. The second sample in June showed a peak
development of C. glomerata when it covered
43% of the riffle substrate occurring as long deep
green streamers from the stones.
C. glomerata declined sharply through July
and hx the end of the month was represented
mostly by stubb)- basal portions of the plant.
These fragments have the ability to regenerate
(Fritsch, 1906), and many began to do so in
September, causing this species to reappear sig-
nificantly in the flora. However, the fall growth
consisted only of heavily encrusted compact
mats which lacked the long luxuriant streamers
charactt'ristic of spring growth.
Tliis cycle of Cladophora glomerata develop-
ment at Lawrence supports the assumption of
Blum (1956) that this alga is sensitive to
temperatures approaching 25°C and does very
poorl\- at higher temperatures. The water tem-
perature at this site on June 29, 1971 was 15°C
in earl\- morning and approached 25°C by late
afternoon. Temperatures through July, August
and early September likewise approached 25°C
for at least portions of the day.
Cladophora glomerata beds at Lawrence
provided excellent habitat for development of
other organisms. Consequently, they were often
full of insects and epiphytic algae. The peak of
biological activity of the stream could thus al-
most be said to parallel the peak of Cladophora
development.
Mats of Oedogonium sp. also formed long
green streamers intermingled with Cladophora
glomerata. This alga could be recognized since
the mats were generally formed nearer the water
surface and their color was yellow green as op-
posed to the deep green of Cladophora. The
pattern of development of this genus at Lav^'-
rence was similar to that of C. glomerata. Oedo-
gonium sp. appeared in April and reached a
peak of development in June. By July Oedo-
gonium sp. was not evident as a visible alga al-
though small filaments were found to colonize
glass slides throughout the year and were found
in the net plankton until November.
Mats of Chara vulgaris began developing in
(\arly summer when the water level declined
and the water temperature rose. By October C.
vulgaris dominated the aquatic vegetation cover-
ing 64% of the total substrate. C. vulgaris oc-
curred in greatest abundance in slow-flowing
water, where it reached 85% cover in October.
Riffles averaged only 54% Chara cover at the
same time. The water level was extremely low
during this period, and C. vulgaris mats literally
filled much of the creek channel. By November
the plants forming these large mats had begun
to die and decompose, and walking through
them stirred up a black organic ooze and large
amounts of entrapped silt. Visible films of epi-
ph\'tic diatoms covered the upper filaments of
C. vulgaris. These diatoms consisted mostly of
Achnanthes minutissima and Sijnedra ulna. Simi-
lar to the Cladophora glomerata mats, Chara
vulgaris beds were the site of a great deal of
biological activity.
In December and January extensive decom-
position of C. vulgaris occurred under the ice
cover and the stream bed became very murky
with silt and decomposition products. The water
was significantly influenced by decomposition
during this period. Due to high biological oxygen
demand, dissolved oxygen levels during Novem-
ber, December and January fell to 6, 3 and 8
ppm, respectively, from the usual average of
9-10 ppm. Carbon dioxide levels rose concur-
rently from averages of 2-4 ppm to 6, 24, and
16 ppm for the same three months. The higher
CO2 levels also lowered the pH slightly through
this period. It is interesting that a significant
amount of Chara vulgaris remained viable
through the winter months, indicating that suf-
ficient light penetrated the ice and snow to al-
low photosynthesis and also indicating that C.
vulgaris is quite resistant to low temperatures.
The ice broke in February 1972 due to an
early thaw, and the large mats of Chara had
28
Brigham Young Univehsity Science Bulletin
entrapped large amounts of silt. The bottom
was black and murky, and the water was ex-
tremely turbid from silt stirred up from the
substrate. With the rise of the spring flood in
March, turbidity became so intense that visibility
through the water was reduced to zero as higher
and faster water began scouring the stream
channel and washing silt deposits downstream.
During late summer and early fall, a pros-
trate, often encrusted alga became quite evi-
dent on smaller stones of the stream bottom.
This alga was very difficult to identify accu-
rately due to its growth form, but was suspected
to be Trotoderma viride since this alga was prev-
alent on periphyton slides collected in Septem-
ber. P. viride appears to prefer wann water,
since it first appeared in the summer then dis-
appeared as the waters cooled in the fall.
The vascular plant, Potomogeton sp. was in-
cluded in the sampling at Lawrence since it
was an important aquatic plant throughout
much of the growing season. Interestingly, few
epiphytic diatoms were found growing on living
Potomogeton sp. plants as contrasted to Oedo-
goniurn sp. and CladopJiora glomerata which
supported large popularions of attached diatoms.
Hynes (1970) indicated that some species of
aquatic plants such as Potomogeton pectinattis
support a poorlv developed periphyton assem-
blage while living, and apparently this holds
true for the Potomogeton at Lawrence.
Potomogeton sp. first appeared in early July
and bv late July constituted an important part
of the total flora. Small amounts remained pres-
ent throughout the winter and were still present
when the ice broke in February. Most Potomo-
geton plants lasting through the winter were re-
moved by scouring during spring high water.
Net plankton pulses showed a definite cor-
relation with the appearance and development
of Oedogonium sp. and Cladophora glomerata
(Fig. 2.3). C. glomerata fragments were a major
component of net plankton samples during late
spring and early summer but disappeared in
Julv and August. Oedogonium sp. appeared in
the net samples in Mav, reached a peak in June
when it was also most abundant as a visible
benthic form, and fell off shaq^ly in July. Total
net plankton occurrence followed much the same
curve as Cladopliora glomerata and Oedogo-
nium sp., being highest in the spring and ver)'
low throughout the summer and fall. Net plank-
ton at Lawrence increased significantly in Feb-
ruary and March 1972 because of the growth
of Vlothrix tenerrima on the substrate during
winter months. Periphyton slides retrieved in
December and March likewise had populations
of U. tenerrima growing on them. Blum (1957)
noted a similar winter growth of Ulothrix
through tlie late winter months in the Saline
River , Michigan.
Although the Lawrence site is located low
on the creek drainage, few true planktonic al-
gae were collected. Clark ( 1958 ) likewise found
the lower Logan River, Utah, to be low in
true phytoplankton. Kofoid (1903) and Whit-
ford and Schumacher (1963) discussed the de-
velopment of euplankton in rivers and con-
cluded that the water in a stream must be sev-
eral weeks old before a true river plankton will
develop. Thus, the water in Huntington Creek
probably takes much less time than this to pass
from its origin into the San Rafael River.
Infonnarion on diatom populations in this
study came from periphyton and nannoplankton
investigarions. A strong vernal increase in peri-
phyton was evident in April and early May fol-
lowed by a summer low and a general increase
from September through December. Winter lows
occurred from January to March and fewer
total organisms were present during this time
than in the summer. This yearly trend was basi-
cally fomied by the genera Navicula, Sijnedra,
Diatoma, Cymbella and Surirella (Fig 24).
Gomphonema likewise followed this general
trend except for a significant increase in Sep-
tember and October. This September-October
Gomphonema pulse was caused by rapid in-
crease of G. gracile. G. olivaceum, on the other
hand, was more important in the fall and espe-
cially in the winter.
Nitzscliia (mostly N. palea) was an impor-
tant component of the periphyton in early June
(30% of the total periphyton). It decreased
through the summer until October, when a sig-
nificant pulse occurred. It then declined again
through the winter months. Whitford and Schu-
macher ( 1963 ) classified periphyton into late
spring-early fall species and early spring-late fall
species. This classification followed their obser-
vation that diatoms appearing in late spring
usually also showed a high colonization rate in
early fall and, likewise, early spring diatoms
also were present in large numbers in the late
fall. The data on Nitzschia palea from Lawrence
indicate that this taxon is a late spring-early fall
form.
Se\eral diatoms reached theii' peak of de-
velopment during summer months. Tliese in-
cluded Cocconeis (mostly C. pediculus in June
and C. placentula in August), Achnanthcs ininu-
tissima, Ct/cloteUa meneghiniana and Pleurosig-
ma delicatulum. Cocconeis constituted approxi-
mately 22'/( of tlic periphyton from June to Au-
gust. Cocconeis placentida was an especially
important epiph\'te throughout most of the sum-
BiOL<;ciCAi, Series, Vol. 18. No. 2 Alo.-ve of Huntington Canyon, Utah
29
Total Net Plankton: 1 = 50 algae I
Selected Genera
1 = 25 algae I
Nov. Jan. Mar.
Cladophora
Oedogonium
Oscillatoria
Ulothrix
Fig. 23. Seasonal distribution of selected net plankton at Lawrence (site 1).
30
BmciiAM Ydi'Mc University Science Bulletin
Total Periphyton: 1 = 10 algae
m
Selected Genera: 1=5 algae ml
May June Aug. Oct. Dec.
Navlcula
Nitzschla
Coccone/s
Fig. 24. Seasonal distribution of selected periphvtoii at I.jiwrenre (site 1).
Biological Series, Vol. 18. No. 2 Alg.ae of Huntington Canyon, Utah
31
mer, and it was not uncommon to collect a fila-
mentous green alga covered with hundreds of
specimens of this species. Pleurosigma delicatu-
lum was most prevalent in July-
During the August-October period, Achnan-
thes minutissinui comprised about 36% of the
periphyton. However, this species was absent
from the periphyton in October, indicating that
colonization decreased sharply during that
period.
Cyclotella meneghiniana was the only cen-
tric diatom prevalent in Huntington Creek. It
showed a peak of development in the summer
from July to September with a maximum in
August.
Nannoplankton in Huntington Creek at Law-
rence were high throughout most of the year.
The higher nutrient levels in the creek here, and
the availability of filamentous green algae as a
substrate for diatom growth contributed to the
continuously high levels. Some diatom genera,
such as Gyrosigma, Cocconeis, Cyclotella, and
Achnanthes appeared in high numbers in the
nannoplankton beginning in July 1971 when
spring and fall genera such as Navicula, SuTirel-
la, and Synedra became quite low ( Fig. 25 ) .
These latter genera increased again greatly in
late fall when most of the dominant summer
genera declined in numbers. A low point for the
season in total nannoplankton was reached in
October. However, a large pulse occurred in
November composed mostly of Synedra ulna,
which comprised 41? of the total nannoplankton.
Synedra also actively colonized glass slides dur-
ing this month, and it grew so profusely on
d\ing Chara vulgaris mats that a brown film
was visible on each Chara plant.
From Januarv to March 1972 a scouring of
the stream channel occurred as the early run-
off waters riled the silt and decomposition prod-
ucts built up during the fall and earlv winter
season. This scouring process also scoured many
of the prevalent winter and spring diatoms from
the substrate and from among accumulated
plant material, causing extremelv high numbers
of these diatoms to occur in the nannoplankton.
Thus, nannoplankton in Februars and March
exceeded 2 million cells per liter. Important
genera during this period included Synedra,
Cymhella, Surirella and Navicula. Nannoplank-
ton levels were also high in April and May 1971,
which was probably caused by renewed coloni-
zation following spring scouring.
The flora at LawTcnce differed significantly
from that of the sites in Huntington Canyon, es-
pecially in the growth of Oedogonium sp., Cla-
dophora glomerata. and Chara vulgaris, and the
absence of Hydrurtis foetidus on the stream bed.
The general plankton pattern at this site was
similar to that of other sites consisting mostly of
diatoms. However, the diatom communities here
were much different in structure from those
of other sites since Cocconeis ( mostly C. placen-
tula), Cyclotella meneghiniana, Pleurosigma deli-
catulum, and Gyrosigma spencerii were present
in much greater numbers, while Cymbella spp.
were greatly reduced.
To summarize seasonal community variations
at Lawrence, Cladophora glomerata and Oedo-
gonium sp. dominated the flora in late spring
and early summer, with diatoms such as Navi-
cula, Cymbella, Synedra, and Surirella occurring
in high numbers on stones and macroscopic al-
gae. Chara vulgaris dominated the stream bot-
tom from summer through fall and occurred
with Protoderma viride, Cocconeis spp., Achruin-
thes minutissima, and Cyclotella meneghiniana.
Late summer and early fall allowed maximum
development of Gomphonema gracile and Nitzs-
chia (mostly N. palea), while the late fall en-
vironment stimulated another general diatom
pulse. Net and nannoplankton assemblages
were derived largely from cells and filament
fragments released from the substrate, and true
planktonic algae were rare in the flora.
Highway 10 Bridge (Site 2)
Water chemistry and visible attached algal
data from this site correlated closely with that
from Lawrence and consequently differed from
data collected upstream in the canyon. The
water at sites 1 and 2 had significantly higher
levels of nitrates, phosphates, alkalinity, and es-
pecially hardness, silica, and sulfate than the
water at site 3, which is the first site located in
Huntington Canyon (Table 1).
The same table illustrates that the levels of
these chemicals in the water at Lawrence are
generally higher than at Highway 10. This is
because as the creek leaves the canyon it passes
through strata and soils which are extremely
rich in carbonates. In addition, the creek here
drains both fanning and grazing lands which are
responsible for the addition of nitrates and phos-
phates, and passes near Huntington City which
Table 1 . Chemical Data for Huntington Creek, De-
cember 17, 1971.
Site 1
Site 2
Site 3
Nitrate nig/1
0.6
0.33
0.3
Pbosphatc nig/I
0.16
0.06
0.08
Alkalinity mg/l
410
370
240
Total harHness mg/I
2000
1300
250
(
CaCO,
■Silica mg/l SiO'
16
18
2.7
.Sulfate mg/l
2700
1300
28
Brioiiam Young University Science Bulletin
Total Nannoplankton: 1=100 olgoe ml
Selected Genero: l:=25 olgae ml
Apr. June July Sept. Nov. Jon.
Nitzschla
'Occoneis
Fip. i'l, Seasoiml distrihutiim of •^^lp(to<l iiHiuinplniik ton at T.awrenrp (site 1).
Biological Series, Vol. 18. No. 2 Algae of Huntington Canyon, Utah
33
likely also adds nutrients. Due to the removal
of water for irrigation and storage above these
tsvo localities, the creek is generally low at
sites 1 and 2 and thus the addition of these
nutrients has a profound effect on water quahty.
The algal community at site 2 was very simi-
lar to that of site 1 in many aspects, and both
resemble that reported by Blum ( 1957 ) for the
Saline River, Michigan, and appear to be typi-
cal of highly calcareous streams in general.
CladopJwra glotiwrata at Highway 10 demon-
strated a late spring-early summer development.
This species was prevalent here throughout May
and June 1971, covering 25% of the riffle sub-
strate in early June and 57% by late June. By
July, C. glomerata had apparently stopped
growing, but mats of it were still evident at-
tached to stones and streaming in the current.
Chara vulgaris appeared in July 1971 and
became prevalent in August. This alga was
found mostly in slower water rather than in
riffles, indicating that the replacement of Clado-
phora by Chara in the flora was not a result of
direct competition but rather represented sea-
sonal change. Transects to measure visible ben-
thic algae were run in both riffles and slow
water at this site, and the results were aver-
aged to characterize overall trends. However,
a comparison of the data summarized from each
area (Table 2) illustrates some interesting habi-
tat preferences for these two species. Cladophora
glomerata prefers riffles with fast water and a
ston\' substrate, whereas Chara vulgaris prefers
slow water and a silty substrate.
Chara persisted through the fall and into
the winter under the ice cover. However, it did
not form the extensive mats which were present
at Lawrence since the creek channel was much
shallower here and the water faster. As the
water level fell late in the season, much of the
Chara on the creek margins dried from t^xpo-
sure. When the ice melted in February 1972,
Chara was completely gone from the riffles but
still covered 13% of the stream bed in slower
areas. However, during the high runoff in March
Table 2. July-November 1971 averages of the fre-
quency, percent cover and percent composition for
Cladophora and Chara in a riffle and in a slow
water area at Highway 10 (Site 2).
Riffle
Slow water
Cladophora glomerata
Frequency
Cover
Composition
Chara vulgaris
Frequency
Cover
Composition
76.3
7.3
62.5
25.3
4.4
36.5
42.4
3.7
15.1
86.4
42.0
84.1
most of it was displaced and washed down-
stream by high turbulent water.
From floristic sampling at Highway 10 sev-
eral trends in population became apparent. In
early June and again in October 1971, Vaucheria
gemiiiata was found intermingled among Clado-
phora filaments and was covered with epiphytic
diatoms. Diatoms most abundant in the creek in
May and June were Ct/mbella parva, Amphi-
pleura pellucida, Diatoma vulgare, Diatoma
tenue and Stjnedra ulna. In late June Nitzschia
spp. and Cocconeis placentula entered the flora
in significant numbers. Diatoms decreased gener-
ally during the summer months, and the stones
became covered with an encrusting cyanophyte
and Protoderma viride. This crust disappeared in
October. In September 1971 large amounts of
Spirogtjra sp. were found here as well as species
of Oscillatoria and Ltjngbya. In October Amphi-
pleura pellucida showed an increase which was
followed in November by an increase in Sijned-
ra ulna and Achnanthes minutissima. The Janu-
ar\' sample showed these three diatoms to still
be important in the flora.
Although floristic trends at this site were
similar to those at Lawrence, the total abun-
dance of algae at Highway 10 was considerably
lower. This likelv resulted from the influence of
faster and shallower water here, fewer nutrients
present in the water and the shade of the bridge
and nearby cottonwood trees reducing the
amount of sunlight available for photosynthesis.
Plant Site (Site 3)
The plant site was the first site located on
Huntington Creek in Huntington Canyon prop-
er, and its algal flora was similar in many re-
spects to that of other creek sites in the canyon.
The dominant genera at this localit)' were Hyd-
rurus, Oscillatoria, other Oscillatoriaceae, Navi-
cula, Gomphonema, CijmheUo, Synedra, Nitzs-
chia and Achnanthes.
Immediately after the ice broke in Febru-
ary 1972, Hy drums foetidus covered 24% of the
stony substrates of this site. It consisted of light
brown filaments on stones with scattered patches
becoming dark brown. However, it lacked the
luxuriant growth evident for this species further
upstream. By March 1972 all H. foetidus had
disappeared except for a few isolated clumps.
However, in May and early June of the previous
year during the high point of the spring flood,
some specimens of this species were observed
growing on large rocks close to the water sur-
face or partly exposed.
Net plankton totals for //. foetidus at the
plant site showed that this May-June period was
34
BmcHAM Young University Science Bulletin
the peak of production for this species in Hun-
tington Creek upstream from the plant site
(Fig. 26). Most specimens observed in the net
plankton were damaged, indicating that they
undoubtedly originated some distance upstream
from where they were collected. H. foetidus
showed a definite downward trend in produc-
tivity as the water temperature increased to-
ward 12°C which Zhadin (1961) indicated as
the critical temperature for this alga.
Filamentous blue green algae were also espe-
cially important in the net plankton from the
spring through the summer and into the fall.
These algae in Huntington Creek consisted of
Schizothrix JTagUe, OsciUatoria spp. and other
genera of the family Oscillatoriaceae. They usu-
ally occurred mixed with diatoms, silt and debris
as encrustations on stones and other solid sub-
strate on tlie creek bottom. Single filaments or
clumps of filaments were released into the
creek current and were second only to diatoms
as a contributor to the total plankton of lower
Huntington Creek in the spring and summer.
Periphyton data indicate that blue green al-
gae were most active in colonizing the substrate
from late June to October. Floristic samples
taken each month revealed that the greatest
abundance and diversity of filamentous blue
green algae occurred in the summer and early
fall. By September a considerable accumulation
of blue green algae, diatoms and sediment had
accumulated on the stony substrate of the creek.
In October 1971 a definite resistant blue green
algal encrustation had developed beneath this
accumulation, and in November it was easily
scraped free. Periphyton data indicate that no
cyanophyte colonization occurred during No-
vember, which suggests that the onset of winter
made conditions unsuitable for these algae.
Net plankton data for the fall months cor-
relate very well with periphyton results. In
September small clumps of blue green algae
began appearing in the net plankton in signifi-
cant numbers and by November they comprised
70f of all net plankton indicating that these al-
gae were being readily released from the sub-
strate. Colonization began again during the
January-March 1971 period when an active
growth of OsciUatoria amphibia and O. agardhii
was noted both under the ice and in open water
after the thaw. Tliis recolonization trend was
mostly determined from floristic samples taken
one to two mik^ above and Ix-low the plant
site where OsciUatoria spp. were especially abim-
dant.
Green algae occurred onl\- sporadically on
periphyton sampling slides at the plant site.
However, net plankton data and visual obser-
vation indicated that some species of Chloro-
phyta were present on the stream bottom. Ulo-
thrix tenuissima was most significant in June
1971 and again in March 1972. Oedogonium sp.
occurred throughout most of the summer, and
Cladophora glomerata appeared in early sum-
mer and again in early fall. This suggests that
the approximate temperature preferences for
these algae are: Ulotlirix tenuissima around
10°C; Cladophora glomerata close to 15°C; and
Oedogonium sp. 15°C and higher.
Spirogijra sp., Zijgnema sp., and Mougeotia
sp., filaments occurred in the net plankton in
low amounts in the summer and early fall. These
filaments probably originated from quiet side
waters or ponds upstream from the plant site.
A few true planktonic algae were noted in
the net plankton during the summer months.
The most significant of these were Pandorina
morum which occurred from late June to Oc-
tober and Ceratiiim hirundinella which was col-
lected from August to November ( Fig. 26 ) . The
source of these algae was likely from lentic en-
vironments which drain into Huntington Creek
above the plant site. Cleveland, Miller's Flat,
Rolfson, and Huntington reservoirs on the up-
per drainage of the left fork of Huntington
Creek were the probable sources of these eu-
plankters. In addition, these algae may have
originated in part from pools, ponds and quiet
waters along the creek. The cycle of develop-
ment of Pandorina morum in Tie Fork Pond
substantiates this assumption since this alga was
prevalent in the pond from July to October,
reaching a peak in number in September. This
trend correlated with the highest number in the
river, both at the plant site and upstream at
site 4. Floristic samples taken from Cleveland
and Miller's Flat reservoirs in Julv showed Pan-
dorina morum to be present there also, but the
presence of this alga in right fork plankton
samples discourages the conclusion that these
reservoirs are its only source into the creek.
Ceratium hirundinella is suspected to origi-
nate almost entirely in the reservoirs on the left
fork of Huntington Creek. Tliis species has been
reported as a dominant summer plankter from
other reservoirs in Utah (Chatwin, 1956; Long-
lev, 1969) with large pulses generally occurring
in August and September, which were the
months of maximum Ceratium hirundinella
abundance in Huntington Creek. These were
also the months of m;iximum water release from
the storage reservoirs on the left fork to provide
irrigation water for Castle Valley. Many C. hir-
undinella cells in the plankton were broken,
suggesting that they had been transported
downstream from the reservoirs.
l^KM.iicirM, Skhiks, \'()i.. 18. \'(). 2 Ai.cak ok Hunting ii-n' C)\n\()N, Uiaii
Total Net Plonkton: 1 = 100 olgae
35
Selected Genera: 1=50 algae I
Apr. June July Sept. Nov. Jan. Mar.
Hydrurus
Osclllatoria
Fig. 26. Seasonal distribution of selected net plankton at the plant site (site 3).
36
Bricham Young University Science Bulletin
Nannoplankton samples taken during the
summer of 1971 contained three other true
planktonic algae, Dinobrijon cijlindricum and the
diatoms Asterionella formosa and Fragihria cro-
tonensis. These algae were likely also released
into the creek from the storage reservoirs. Long-
ley ( 1969 ) reported Dinobryon to be the domi-
nant phytoplankter in Flaming Gorge Reservoir,
Utah, during June and July. Daily ( 1938 ) in-
dicated that Dinobryon was present in Lake
Michigan during most months of the year but
that it demonstrated a strong peak of develop-
ment in July and a lesser peak in November.
Pratt ( 1957 ) likewise found a similar cycle in
Salem Lake, Utah County, Utah, where Dino-
bryon showed a summer pulse from late June
to mid September and another pulse from mid-
October to mid-November. Dinobryon cyUndri-
cum was present in Huntington Creek from
early June through November, with July and
October being peak months. Maximum develop-
ment of this alga in Huntington Creek corre-
lated with water release from the left fork reser-
voirs.
Asterionella formosa appears to prefer colder
water conditions thim Dinobryon. Longley
( 1969 ) indicated this species to be important in
Flaming Gorge Reservoir from September to
May, and Pratt ( 1957 ) found very high amounts
in November and December. Pratt also reported
a small pulse in August only on the bottom of
the pond where the temperature was approxi-
mately 14°C. The cycle of Asterionella formosa
in Huntington Creek was intimately associated
with the management of waters of the left fork
reservoirs. These reservoirs are either complete-
ly drained or kept at very low levels during
late fall and early winter months and are sub-
sequently filled with runoff waters during the
late winter and early spring. Consequently, no
opportunity exists for the release of euplank-
ton from these reservoirs during this period, ex-
plaining why very few euplanktonic species,
especially A. formosa, were found in the creek
during these months. When these reservoirs are
filled in the spring, the overflow enters Hun-
tington Creek carrying with it any plankton
which may have developed in tlie reservoir over
the winter. This was the probable source of A.
formosa in the plankton of Huntington Creek,
since this diatom was highest in the creek in June
1971 (59,490 coloni(>s per liter on June 8, and
30,250 colonies per liter on June 29). It declined
gradually through the summer and then in-
creased slightly in October. Tliis trend was un-
doubtedly directly txirrelated with the tempera-
ture curve in the reservoirs.
Clark (pers. comm. ) studied a similar situa-
tion in Idaho where Henry's Lake drains into
the north fork of the Snake River. Blooms of
Asterionella formosa occurred in Henry's Lake
in June and October 1971, and this alga was
found in the river plankton for 35 miles below
this lake during the time of the bloom. A. for-
mosa density was 815,200 colonies per liter at
the Lake's outlet and decreased to 32,600 colo-
nies per liter 35 miles downstream from the lake
due to the effects of the river current.
A similar reduction in colony number would
be expected in Huntington Creek from the reser-
voirs on the left fork downstream to the plant
site, which represents a distance of approxi-
mately 18 miles. Onlv moderate currents are suf-
ficient to cause such a reduction (Allen, 1920)
and turbulent cunents can often cause extreme
reduction in euplankton. For instance, Galstoff
( 1924 ) reported a 40% reduction in plankton
during an eight-hour passage of the water of
tlie Mississippi River through the Rock Island
Rapids.
Many of the Asterionelln formosa colonies
collected in the plankton at the plant site were
fragmented, which Brinley (1950) cited as an
evidence that they originated in a lentic environ-
ment and were not natural stream inhabitors.
Fragilaria crotonensis was another euplank-
tonic diatom present in the nannoplankton at
site 3. Clark (per. comm.) mentioned that Fra-
gilaria crotonensis was abundant in Island Park
Reservoir, Idaho, in October 1971. Likewise,
Daily (1938) indicated this species as a domi-
nant fonn from October to December in Lake
Michigan, and Longley (1969) observed the
same trend in Flaming Gorge, Utah. Fragilaria
crotonensis was prevalent at the plant site
from September to November, with a large peak
in October when its density reached 80,620
colonies per liter. The source of these algae was
likely the reservoirs on the left fork.
Other diatoms in the creek were produced
largely on the substrate and subsequently re-
leased into the current. Thus, understanding
trends in periphyton is essential to understand-
ing algal trends in the stream as a whole. Peri-
phyton data demonstrated a rather smooth
seasonal colonization curve of diatom develop-
ment on the substrate. A gradual increase in
colonization rate occurred through the spring
and earl\ summer until July, after which a de-
cline occurred until December. Dominant genera
included Navicttla, Ct/mbella. Gomphonema,
Synedra, Nitzschia, and Achnanthes.
As shown by Table 3, the importance of
these genera on the substrate correlated rather
closely with their importance in the nannoplank-
ton.
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah
37
Table 3. Percent occurrence of selected genera of periphyton and nannoplankton at plant site (Site 3).
5/13
1971
6/29
1971
7/30
1971
8/20
1971
10/8
1971
11/15
1971
12/17
1971
2/19
1972
Navicula
Periphyton
Nanno
Cymbella
Periphyton
Nanno
Gomphonema
Periphyton
Nanno
Synedra
Periphyton
Nanno
Nitzschia
Periphyton
Nanno
Achnanthes
Periph3rton
Nanno
Hannaea
Periphyton
Nanno
Diatoma
Periphyton
Nanno
Other Diatoms
Periphyton
Nanno
Nondiatoms
Periphyton
Nanno
26.4
14.7
11.2
17.3
18.0
22.4
26.8
22.7
26.6
14.1
14.0
20.7
15.9
13.3
9.9
13.9
30.5
19.9
44.2
36.1
10.9
26.2
15.9
24.3
13.1
15.4
19.5
18.7
30.4
17.7
26.0
24.6
22.0
32.2
11.7
6.2
3.1
8.7
2.6
10.1
2.7
5.0
7.3
6.7
9.1
3.1
36.2
20.8
14.0
8.9
5.2
3.1
1.5
1.2
3.5
1.9
4.5
8.5
11.8
7.6
8.4
7.7
7.5
8.2
16.5
6.9
14.3
6.2
18.6
32.7
20.3
36.9
26.4
28.7
38.7
20.3
25.3
10.5
16.7
5.0
2.8
11.7
6.2
57.1
12.3
13.7
12.6
6.2
5.8
5.0
2.2
4.1
7.2
3.9
4.4
.6
.5
2.0
4.1
.3
.3
.1
1.1
.3
1.1
1.9
.5
1.1
.4
2.1
1.1
1.7
1.4
2.5
8.0
1.1
5.1
22.1
5.7
9.6
1.1
3.2
4.1
12.0
.8
8.0
1.4
6.3
3.3
22.2
4.5
4.4
.8
3.9
.9
.3
2.7
2.0
2.1
6.0
5.8
A comparison of the total number of algae
colonizing periphyton sampling slides with the
total nannoplankton at the plant site for the
studv period is illuminating (Fig. 27). General-
ly speaking, the nannoplankton were dependent
upon the periphyton and the peaks and lows for
the two corresponded. However, through the
summer, especially in July, the production of
periphyton was high due to a heavy colonization
of Achnanthes (mostly A. minutissima) and
Navicula spp. This summer periphyton increase
was followed by an early fall nannoplankton in-
crease. Tliis nannoplankton pulse was caused
by such genera as Navicula, Cymbella, Gompho-
nema, Synedra, Nitzschia, and Achnanthes (Fig.
28). Tliese genera had developed on the creek
bottom throughout the spring and early summer
and apparently were released into the stream in
O
O
o
lOOO
750
§ 500
i
z
<
a.
o
z
z
<
z
250
PERIPHYTON
NANNOPLANKTON
I60
I20
80
40
O
O
O
5
z
z
O
t—
>-
I
APRIL JUNE JULY SEPT NOV JAN MAR
Fig. 27. Density and seasonal distribution of nannoplankton and periphyton at the plant site (site 3).
38
Brigham Young University Science Bulletin
Total Nannoplankton: 1 = 100 algae ml
Selected Genera: 1 = 50 algae ml
Apr. June July Sept. Nov. Jan.
Mar.
Navicula
Cymbella
Gomphonema
Nitzschia
Fig. 28. Seasonal distnbiition of splortpcf niiiiiiopl;iiiktoti at the plant sito (site i).
Biological Series, Vol. 18. No. 2 Alg.-\e of Huntington Canyon. Utah
39
the late summer due to certain enviromnental
stimuli. This conclusion is supported by de-
creased colonization rates during the nanno-
plankton pulse.
Nitzschia spp. (especially N. palea) were im-
portant in the nannoplankton throughout the
study period but demonstrated a peak of occur-
rence from August to October. The yearly high
occurred in August, one month later than the
Nitzschia high at Lawrence and one month ear-
lier than the Nitzschia peak from localities fur-
ther up the canyon.
Cocconeis placentula and Achnanthes minu-
tissima were predominately summer diatoms at
site 3, and Hannaea arcus was a late spring-
early summer species. Diatoma vulgare and
Gomphonema olivaceum have been reported by
Blum ( 1957 ) to be important winter colonizers
of bare areas. He found Diatoma vulgare most
abundant in early winter in the SaUne River,
Michigan, and Gomphonema olivaceum most
abundant in late winter and early spring. Peri-
phyton data from the plant site show Diatoma
vulgare to have been most active in colonization
in November 1971. D. vulgare also occurred in
high numbers in the plankton during the fall
and winter months. Gomphonema olivaceum be-
came most important in the periphyton in Janu-
ary-March 1972. The cells and mucilaginous
stalks on which they grow formed an extensive
diatom "ooze" on the entire creek substrate dur-
ing these months. Nannoplankton data from the
spring of 1971 and the winter of 1972 indicate
that Gomphonema spp. were important in the
flora throughout the winter and spring.
In summary, the algal flora at site 3 was
predominately composed of Htjdrurus foetidus
in the spring, filamentous blue green algae in
the summer and diatoms throughout the entire
year. Filamentous algae contributed to the net
plankton of the river and diatoms comprised
nearly the entire nannoplankton. The plankton
at site 3 was also influenced by blooms occur-
ring in Miller's Flat and Cleveland Reservoir
on the headwaters of the left fork of Huntington
Creek. Planktonic algae originating from these
reservoirs included Panclorina morum, Asterio-
nella jormosa and Dinohrijon cijlindricum in the
late spring and summer and Ceratium hirundi-
nclla and Fragilaria crotonensis in the fall.
Bear-Rilda Campground (Site 4)
The campground locality is located three
miles upstream from site 3 and exhibited a simi-
lar flora. However, certain noteworthy variations
between the two floras occurred. These differ-
ences are attributed to different ecological con-
ditions at site 4 and the effects of construction
and pollution from Deer Creek on site 3.
The creek at site 4 was high from April
to early June 1971 with a definite dechne in
water level in late June. Hydrtis foetidus ap-
peared here in May on stones in a broad shallow
riffle and increased to cover 25% of the sub-
strate in early June. By June 29, 1971, this spe-
cies had disappeared from the visible benthic
algae at site 4, but was still prevalent in the net
plankton indicating that it was carried down-
stream from higher elevations where it persisted
later in the season. A light film of H. foetidus
appeared on the substrate in February but dis-
appeared in March 1972. High water and prob-
able abrasion from ice breakup upstream con-
tributed to the disappearance of this alga at
sites 3 and 4 during this period.
The summer and early fall diatom ooze and
blue green algal encrustation noted at the plant
site were even more apparent at site 4 where
the water was shallower, creating more exten-
sive riffles. Algal and sediment buildup began
in July and continued through October, when an
extensive blue green algal crust was evident
under the diatom ooze. In November this crust
began flaking off.
It is possible that Protoderma viride or an-
other encrusting green alga was a member of
this community. However, filamentous blue
green algae were definitely the predominant
constituents since large amounts of blue green
algae were found in the net plankton when the
crust began to break up (Fig. 29). Also floristic
samples from the campground and further up-
stream at the junction of the two forks of Hun-
tington Creek showed large amounts of Schizo-
thrix fragile and other filamentous Cyanophyta.
The presence of these algae in Huntington
Creek correlates with the findings of Clark
( 1958 ) in the Logan River, Utah, where a blue
green encrusting mat was also found on the
substrate under the diatom ooze. A new build-
up on the substrate was noted in January and
February 1972, but it consisted mostly of di-
atoms. Filamentous blue green algae were pres-
ent at that time but not in sufficient quantities
to create an encrusted mat. During spring flood,
the high water and abrasion from its increased
silt load usually scoured the stones of much of
their periphyton.
By July, turbulence in the riffle had de-
creased significantly and many scattered mats
of Oscillatoria cf. tenuis, together with trapped
sediments, occurred on the stream bottom.
These were small mats covering only 6.4% of the
substrate in shallow water although they oc-
40
Brigham Young University Science Bulletin
Total Net Plankton: 1=100 algae I
Selected Genera:
Apr. June July Sept.
=50 algae I
Nov. Jan.
Mar.
Ulothrix
Fig. 29. Season<il di.stribntion of selected net plankton at the rampground (site 4).
Biological Series, Vol. 18. No. 2 Alc.ae of Huntington Canyon, Utah
41
curred in 77% of the plots observed in transects
across the creek. The mats were gone in August
but were evident to a lesser extent again in Sep-
tember.
Similar to other sites along the creek, net
plankton assemblages at site 4 were directly
influenced by the benthic algae. Oscillatoria cf.
agardhi filaments were most abundant in the
net plankton in the spring, although they oc-
curred throughout the year. In September and
November many small clumps of filamentous
Cyanophyta were collected in the net plankton
because of the aforementioned breakup of the
blue green algal encrustation. Ulothrix sp. oc-
curred mostly in May and June, Cladophora
glomerata from June through August, and Oedo-
gonium sp. from May through October. Spiro-
gijra sp., Mougeotia sp., and Zi/gnerna sp. oc-
curred through the summer months, and Stigeo-
clonium stagnatile appeared in the fall.
The same true planktonic algae occurred in
tlie creek at the campground localitv as at the
plant site (Fig. .30). Tliese included Ceratium
hirundinella in August and September 1971,
Pandorina morum in June through October,
Dinobrt/on cylindricum from June to November,
Asterionella formosa from June to December,
with highest numbers in June, and FragiJaria
CTotonensis from October to December, with
highest occurrence in November. Tliese trends
were similar to those at the plant site.
Periphyton colonization trends were similar
to those of the plant site. A general increase in
periph>'ton was noted through the spring of 1971
until Jul\', followed by a decline to November
1971. Periphyton data were compiled from slides
placed both in a pool and in riffles in order
to compare colonization in the two habitats.
Both areas showed a general decrease in most
genera collected on slides on June 29, 1971, al-
though Achnanthes mimttissima increased great-
ly. This species increased from 2,928 cells per
cm- on June 8, to 2.3,.532 cells per cm- on June
29, for slides in the riffle, and from 27,298 cells
per cm* on June 8, to 12.3,650 cells per cm- on
June 29, for slides in the pool (Table 4). From
late June to August. Achnanthes (mostly A.
minutissima) was the highest contributor to the
Table 4. Percent composition of Achnanthes on glass
slides at the campground, .lune 8-September 16,
1971.
6/8 6/29 7/30 8/20
9/15
Slides in riffle 3.2 28.1 54.6 43.2 (NS)*
Slides in pool 12.8 75.8 75.3 14.9 16.0
*NS — No slide was collected from the riffle in
September.
benthic diatom flora in terms of number of cells
produced.
Most other diatoms in the periphyton fol-
lowed the general trend of the total for this
site discussed above. The most important genera
were Navicula, CAjmbella, Gomphonema, Nitzs-
chia, and Sijnedra. Stjnedra (mostly S. ulna) dif-
fered somewhat by nearly disappearing during
the wanner months. Diatoma vulgare showed
good growth in November as it did at the plant
site, but Gomphonema olivaceum did not show
the expected late winter increase. However,
nannoplankton data for G. olivaceum showed
this species to increase in February and May,
which correlated with the conclusion drawn from
site 3 that this genus is a late winter and early
spring form.
Hannaea arcus was definitely a late spring
diatom, and Cocconeis placentula a summer di-
atom, as indicated by the periphyton and sub-
stantiated by nannoplankton data. Certain true
plankters were occasionally found on the peri-
phyton sampling slides. These algae became
entrapped there as they floated downstream
and fell out of the water column.
A comparison of data from slides placed in
the pool and the riffle reveals certain differen-
ces in colonization in the two habitats. The total
number of periphyton and the number of indi-
viduals of most genera were much higher in the
pool. The only exception to this was Cocconeis
placentula, which showed a comparable colon-
ization rate in the riffle to that in the pool. The
reason for the high colonization rate in the pool
was undoubtedly due to reduced removal of
periphyton by the stream current while concur-
rently allowing sufficient water flow for ade-
quate nutrient and gas exchange for rapid algal
metabolism.
Periphvton composition percentages for the
period May through August 1971 show certain
significant differences between the diatoms of
the pool and the diatoms of the faster water.
The riffle had a higher composition percentage
of Gomphonema (mostlv G. olivaceum) , Sijnedra
(mostly S. ulna), Ctjinhella spp., Nitzschia
(mostly N. palea). Cocconeis (mostly C. pla-
centula), Ulothrix sp., and Hijdrurus foetidus
than the pool. Converselv, the pool had a higher
percentage of Navicula spp., Achnanthes minu-
tissima, Diatoma vulgare and Surirella (mostly
S. ovata).
From comparing periphyton data with nan-
noplankton data at site 4 ( Fig. 31 ) , it is evident
that high periphyton production in June 1971
caused the high nannoplankton levels of the
same period and slightly later. The turbulence
of high water during this period probably
42
Bait;ii\M Yoi'Nt: I'Nniusnv Sciknck Bvi.i.ktin
Total Nonnoplonkton: 1=100 algae ml
Selected Genera: 1=50 algae ml
Apr. June July Sept. Nov. Jan.
Mar.
Fragllaria
Cymbella
Asterlonella
Ceratoneis
Fig. ^0. Sccison.il ilistiilnitian itf sclcrtrd niinnopl.iiiklnn ill tho cnnipgrniintl fsito 4).
Biological Series, \'ol. 18. No. 2 Alc.-ve of Huntington Canyon, Utah
43
lOOO
o
o
o
s
Z3
Z
z
o
z
<
a.
o
z
z
<
z
750
500
250
PERIPHYTON
NANNOPLANKTON
APRIL JUNE JULY SEPT NOV
Fig. 31. Densitj' of nannoplankton and periphyton at the campground (site 4).
300
O
225 8
5
150 iJ
to
5
z
75
X
JAN
MAR
scoured many diatoms from the substrate into
the current. Periph\ton production continued
to rise in Julv 1971, when nannoplankton levels
dropped, probably because fewer diatoms were
removed from the substrate by the current dur-
ing this period. Tliese periphytic diatoms were
subsequently released into the current during
earh" fall when plankton levels increased again.
The November nannoplankton increase and sub-
sequent relativeh' high winter levels were prob-
ably due to new colonization, since periphyton
levels also rose during this period.
The nannoplankton cycle for site 4 basically
followed the trend described for site 3. High
diatom levels were evident from April to late
June, followed by a summer low, and a high
pulse in September (Fig. 32). The decline in
plankton in October and subsequent rise in No-
vember followed a trend similar to that observed
at Lawrence, Stuart Station, and Bear Canyon,
although the plant site did not exhibit the No-
vember increase. The plant site also had much
lower plankton levels on June 29, 1971, than the
campground. Turbidity in Huntington Creek
lOOO
750
O
z
o
z
<
I
a.
o
z
z
<.
z
-J CO
500
250
PLANT SITE
CAMPGROUND
APRIL JUNE JULY SEPT NOV JAN
Fig. 32. Seasonal densities of nannoplankton at the plant site (site 3) and the campground (site 4).
MAR
44
BrICHAM IfoUNG UNrvERSITY SCIENCE BULLETIN
at the plant site was 40 JTU on June 29 com-
pared to 15 JTU at site 4. Likewise, on July 5,
1971 turbidity was 25 JTU for site 3 and 11 JTU
for site 4 ( Wingett, per. com. ) . The higher tur-
bidity levels were attributed to excavation at
the generating station approximately one mile
upstream from site 3. Abrasion caused by the
extra silt load in the water may have depleted
the source of nannoplankton at this site by re-
ducing periphyton populations prior to the June
29 collection, thus accounting for the lower
nannoplankton levels here during this period.
The lower nannoplankton levels in Novem-
ber 1971 are attributed to pollution from Deer
Creek. This creek flows east from a coal mine
across the Utah Power and Light Co. generating
station to Huntington Creek. During much of
the year its flow was restricted, but during cer-
tain periods it flowed freely, carrj'ing an ex-
tremely heavy load of coal dust and mining
wastes. In October and November the black,
soupy water from Deer Creek clouded the clear
waters of Huntington Creek and caused heavy
coal dust sedimentation on the creek bottom.
The effect of this water was probably the main
reason for the low November counts here.
In summary, the flora at site 4 was similar to
the flora at site 3 in containing large numbers of
diatoms both on the substrate and in the nanno-
plankton. High periphyton production in late
spring contributed to corresponding high nanno-
plankton levels. Production decreased during
late summer and increased again in winter.
Nannoplankton levels at site 4 fluctuated greatly
and differed somewhat from those of site 3.
These differences were apparently caused by ex-
cavation above site 3, and pollution from Deer
Creek. Encrustations of filamentous Cyanophyta
were more abundant at site 4 than site 3 in late
summer and visible mats of Oscillatoria sp. oc-
curred at the campground. Hydrunts foetidns
grew more profusely at the campgroimd in the
spring and greatly influenced the net plankton
during this period. Both sites were influenced
by euplankton from reservoirs on the upper
drainage of the left fork.
Stuart Fire Station (Site 6)
The Stuart Fire Station locality' is located
on the right fork of Huntington Creek approxi-
mately 8 miles below the proposed site for the
dam creating Electric Lake. Tliis site had con-
siderably less water volume and lacked the in-
fluence of reservoirs and artificial flow regu-
lation noted for the left and main Forks of Hun-
tington Creek. However, physical and chemical
conditions of the water at site 6 were similar
to conditions downstream except for slightly
higher silica and alkalinity levels.
Seasonal fluctuations in the algal flora at
Stuart Station differed in many respects from
those at other sites. This was probably due in
large part to the higher altitude and consequent
lower temperature and shorter growing season
and to the shading effect from the steep walls
in this part of the canyon.
Hijdrurus foetidus was much more prevalent
at Stuart Station than lower in the canyon. It
was abundant here as early as March in 1971,
although the creek was mostly frozen over. It
remained present throughout the spring and by
June it reached a peak of development forming
a prevalent dark covering on most of the stones
and rocks of the stream bottom. The quadrat
method for estimation of cover and frequency
showed this alga to cover 30% of the total sub-
strate and be present in 100% of the plots on
June 8, 1971. Visual estimation on the same date
of several sites further up the canyon showed H.
foetidus to be even more abundant there than at
Stuart Station. By June 29, this species had de-
clined significantly and soon after disappeared.
H. foetidus reappeared in December 1971 and
became abundant in Februar)' 1972 after the ice
had melted. This alga usually exhibited more
luxuriant growth on larger rocks than on small
stones, and it was common to find rich brown
filaments trailing in profusion from these rocks.
The spring net plankton here was greatly influ-
enced bv broken Hi/drums filaments, and the
peak in net plankton occurred in early June
concurrent to the peak of Hi/drurus production
on the substrate (Fig. 33).
Filamentous blue green algae formed an im-
portant part of the algal communitA' at Stuart
Station. They occurred in all floristic samples
and net plankton samples from this site, often
occurring in abundance. Maximum development
of these algae occurred on the substrate from
July to October 1971, when filaments of Lyng-
hija spp., Pliormidium spp., Oscillatoria spp.,
and Schizothrix fragile formed extensive en-
cnisting mats. These filaments were dense and
intertwined, and heavily laden with silt par-
ticles, diatom mucilage and frustules, and thick
deposits of calcium carbonate, which made the
exact characterization of this communit)' diffi-
cult. However, Oscillatoria agardfiii was abun-
dant in August and Schizothrix fragile and
Li/nghi/a acniginco-cocrulea were abundant in
October. Fragments of these blue green algae
appeared in high numbers in the net plankton
from October to November (Fig. 33) similar to
sites 3 and 4. Oscillatoria cf. tenuis also ap-
peared in October as bright blue green filamen-
1^1(11 cK.KM- Si Mils, \()i . US. \i). 2 Aix;\K oi' Huntincion Canyon, I'taii
45
Total Net Plankton: 1 = 50 algae I
Selected Genera: 1=25 algae I
Apr. June July Sept. Nov. Jan. Mar.
Oscillatoriaceae
Mougeotia
Splrogyra
Hydrurus
Fig. 55. Soasiirinl rlistrilnition of sclfcti'ci net plankton at Stuart Station (site 6).
46
BniGHAM Young UwivEnsiTi' Science Bulletin
tous entanglements similar to those observed at
the campground in July.
O. agardhii was also abundant in the flora
during the winter months. It was prevalent on
periphyton slides in November and February
and from floristic data it appeared to be wide-
spread on the substrate throughout the Novem-
ber-Feb ruar)' period. The high levels of Os-
cillatoria spp. in the 1971 spring net plankton
were probably the result of a similar coloniza-
tion during the winter of 1970-71.
Although this blue green algal community at
Stuart Station was ver>' important on the sub-
strate, it was of little significance on the peri-
phyton slides placed in the creek to monitor
substrate colonization. Blum ( 1957 ) reported a
similar situation in the Saline River, Michigan,
where a cnistose Schizothrix-Phormidium com-
munity occurred on the river bottom. He found
that even after a year's period, sterile rocks
placed in the river failed to develop a commu-
nits' stnicturt^ comparable to the mature Schizo-
thrix-Phormidium crust evident in the river. He
concluded that a mature crust required a year
or more to develop, and that the Schizothrix-
Phormidium communit\' was a permanent mem-
ber of the algal flora in tlie Saline River. A simi-
lar situation occurs in Huntington Creek. The
basic blue green algal community persists at
Stuart Station throughout the year and develops
extensively during summer and fall months.
Cladophora pjomerata likewise chd not ac-
tive^lv colonize microscope slides at Stuart Sta-
tion, although it occurred abundantly on the sub-
strate and significantK' influenced the net plank-
ton in the spring and fall. This species covered
6f of the substrate in September and 10.5% of
the substrate in October 1971. It occurred more
on large rocks than on small stones and was
covered with epiphvtic Cocconeis placentula,
Gomphonema olivaceum, and other diatoms. It
was much reduced in November, exhibiting a
stubby growth form, but existed through the
winter and became heavilv encrusted with cal-
cium carbonate and sediment.
In December C. glomerata was intertwined
with many filaments of UlotJirix zonata and V.
aequalis. lUothrix was otherwise most evident in
Mav and Jun(> at this localit\'.
Oedogonium sp. was rare at Stuart Station,
although it occurred throughout the summer.
Stiaeoclonium attenuatum and S. stagnatile oc-
cuiTcd here inostK' in the fall months. Mougeo-
tia sp.. Spirogijra sp., and Zijgnema sp. were of
unique importance in the summer net plankton
at Stuart Station and were the algae responsible
for the steadv, relatively high net plankton rates
through this period as contrasted to the lower
summer rates at other sites on Huntington Creek.
These species occurred mostly from late June to
October, but Spirogtjra sp. was found from early
June to Februar\'. Mougeotia sp. showed a signif-
icant increase in July when it comprised 62% of
the net plank-ton, and was the main contributor
to the general increase in net plankton during
that month (Fig. 33). The creek upstream from
Stuart Station contains many regions with slow
water and meandering stream channels, as well
as springs, pools, and quiet backwaters. These
areas supported luxuriant growths of conjugate
algae and were undoubtedly the source of these
algae in the net plankton at Stuart Station. Al-
gae in these ponds and backwaters probably
only entered the creek during runoff from late
summer rain storms, but those growing in pools
and side waters of the creek itself were con-
stantly released into the channel.
Diatom colonization of the creek substrate
at Stuart Station showed peak development in
May and November 1971. with lesser peaks in
late June 1971 and Febmar\' 1972. The Novem-
ber-March diatom density was much greater at
Stuart Station than that of any period at sites
3 and 4 (Fig. 34), suggesting that the aquatic
habitat here was more conducive to diatom
production than lower in the canyon. The low
colonization rate in early June was likely in
part a result of the extensive Hydrurus foetidus
development during that period. Summer diatom
production was low here as it was at sites 3 and
4, although the summer low began in July.
Many diatom genera on the substrate con-
tributed to the total periphvton trends for the
study period (Fig. .3.5). Certain genera such as
CijmheUa (mostly C. ventricosa and C. parva),
Synedra (mosth' S. uJrtc), and Diatoma (mostly
D. vulgare) demonstrated high numbers on the
slides collected on June 29, 1971. These genera
were responsible in large part for the general
periphyton increase of that period. CymheUa
spp. were especially abundant in June. Floristic
samples taken on June 15, at Stuart Station and
select(>d sites downstream demonstrated extreme-
Iv high numbers of CymheUa. Diatoma vulgare
was also an important colonizer during this
period.
The fall and winter Diatoma vulgare-Gom-
phomnna olivaceum increase was much the same
at Stuart Station as at sites 3 and 4 down can-
v(m. However, increased D. vulgare colonization
began in October rather than in November, and
G. olivaceum colonization began increasing in
November rather than later in the winter. D.
vulgare began forming long prominent zigzag
colonies in October which became a dominant
part of the periphvton flora in November and
Biological Series, Vol. 18, No. 2
400
300
Algae of Huntington Canyon, Utah
47
O
o o
h
o
200
lOO
stuart station
Campground
APRIL
JUNE
JULY
SEPT
NOV
JAN
MAR
Fig. 34. Density of periphj-ton at the campground (site 4) and Stuart Station (site 6).
continued dominant through the winter until
February 1972. G. olivaceum demonstrated a
high colonization rate throughout the November-
early May period.
Nitzschia, as a whole, demonstrated spring
and fall highs and a simimer low, thus following
the general diatom trend. However, N. acicularis
occurred mostly in the summer and early fall,
when it was found in both the periphyton and
nannoplanlcton from late June to November.
Cocconeis placenttila also occurred in greater
abundance during the summer and early fall
months. It began colonizing in July and reached
a peak in August and September, after which
it decreased significantly.
Butcher (1932) described an Ulvella-Coc-
coneis community which was abimdant in En-
glish calcareous rivers during summer months.
An alga similar to Ulvella, but identified as
Protoderma viride (after Prescott, 1962) was
found colonizing glass slides at Stuart Station
on September 15, 1971. Protoderma is a green
alga exhibiting a prostate, often encrusted
growth habit. In Huntington Canyon it becomes
400
O
O
O
300
:^
^ 200
z
o
< lOO
O
z
z
<
z
. . . .. PFRIPHYTON
NANNOPLANKTON
\
\ \/ \ / '- /
\
\ \' ^ / \ '/
. \
\ 1 \ / \ ' ^ 1
\ ' \ / \ \ ' \ //
1 \ / \ i * '/
\ / \ * '/
\ \
\ \
\ \
\ \
\ \
\ / \ V
\
400
O
300 O
o
200\
s.
z
lOOg
t—
>-
I
APRIL
JUNE
JULY
SEPT
NOV
JAN
MAR
Fig. 35. Density of nannoplankton and periph>'ton at Stuart Station (site 6).
48
BiuGHAM Young University Science Bulletin
crusted with calcium carbonate and silt parti-
cles, making it difficult to identify except when
on periphyton slides. This same species was
found abundantly on shdes at Lawrence in Sep-
tember and October 1971 and was an important
alga in the benthic community there. It was
likely also an important constituent of the crusts
evident at sites 3 and 4 during this same early
fall period, although accurate identification was
difficult and Protoderma was absent on glass
slides at these sites.
Four periphyton slides were retrieved from
site 6 in September, and Protoderma viride was
prevalent in three of the four, covering an esti-
mated 10% to 2D% of the surface of each slide.
In October P. viride was found on only one of
three slides and had decreased in importance
on that slide. Tliis alga therefore exhibited a
short colonization period here and was probably
not as effective in colonizing bare surfaces
rapidly as some diatoms, such as Cocconeis and
Achnanthes.
Visual observation of the stream bottom
throughout the summer indicated that Proto-
derma viride was more prevalent than our data
suggest. Such prostate, often encrusted forms
are rare in the plankton (Butcher, 1932), thus
eliminating plankton data as a means of moni-
toring their production on the stream bed.
Hence. Protoderma viride did not appear in
nannoplankton counts from Stuart Station. This
represents a weakness in subsampling and illus-
trates that total numbers of individuals in a
flora as determined onlv by one sampling method
may not always convey a true picture of the
flora as a whole. Protoderma viride mats were
few in number on the periphyton slides although
each covered a considerable area, making it
important in terms of total cover although in-
significant in total number of cells when com-
pared to diatoms on the same slide.
Achnanthes minutissima and Cocconeis pla-
centuhi illustrate a similar problem of sampling.
Table 5 compares the total number of Achnan-
thes minutissima and Cocconeis phirentula
cells per cm= and their relative abundance on
periphyton slides for the summer and early fall
of 1971.
Table 5. Density in cells/cm^ and relative abundance
of Achnanthes and Cocconeis in the periphyton of
Site 6 July-October 1971.
GENUS
7/30
8/20
9/15
8/10
Achnanthes
Density
Composition
Cocconeis
Density
Composition
29,500
61.2%
2,750
5%
37,290
5.3.1%
7,900
11.2%
32,989
61.2%
3,851
7.1%
5,1+8
8.0%
762
1.2%
These data show both of these genera to be
abundant in the summer flora at Stuart Station,
although Achnanthes minutissima appears to be
much more important. However, cells of this spe-
cies are small and occur on branched mucilagi-
nous stalks, often with many cells appressed
together. Cocconeis placenttila, on the other
hand, is larger and grows adnate to the sub-
strate. The microscope slides from this site in
September were visually examined prior to clean-
ing, and C. placentula appeared as one continu-
ous sheet of cells covering tlie substrate. It thus
appeared to be more important as a substrate
cover than A. minutissima, which was present
in higher numbers. Therefore, care must be used
in sampling, and, whenever possible, subjective
description should accompany numerical charac-
terization describing a total flora as it occurs in
place.
Nannoplankton at Stuart Station were rela-
tively constant throughout the year except for
lows in Mav, August, and October 1971, and
March 1972 (Fig. .36). The high winter and
spring nannoplankton levels here were supported
by similar high production on the substrate. As
periphvton production declined in July and Au-
gust, the number of nannoplankton also dropped.
In September a large number of Nitzschia spp.
and Navicula spp. released from the substrate
caused an increase in the number of nanno-
plankton. An October low occurred at site 6
as it did at site 4.
Generally speaking, nannoplankton levels
showed much less fluctuation at Stuart Station
than at sites 3 and 4 (Fig. 37), whereas peri-
phvton levels fluctuated more (Fig. .34). Nanno-
plankton levels were also generalh' lower at site
6 than at sites 3 and 4 (Fig. 37). Tliis was due
to the collection of diatoms in the plankton as
the current carried them downstream, thus giv-
ing higher levels lower in the drainage. How-
ever, many fluctuations and occasional lack of
correspondence between nannoplankton and
peripln ton data suggest that manv factors along
the stream affect these levels. For instance, many
algae, especially nondiatom species, are de-
stroyed as they travel dowoistream. The abun-
dance of filamentous conjugales at Stuart Sta-
tion and their paucitv at sites 3 and 4 illustrate
this fact. Likewise, localized habitat differences
are also extremely important in creating differ-
ences between floras of different parts of the
stream. Ilannaea arcus, for instance, was im-
portant at the plant site and campground, but
was almost nonexistent at site 6. A noteworthy
lack of euplankton was also evident at Stuart
Station.
Successive collections of nannoplankton from
Biological Series, Vol. IS Nd. 2 Aicvk. of HuNTiN't;TON Canyon, Uiam
49
Total Nannoplankton: 1 = 50 algae m
Selected Genera: 1 = 25 algae ml
Apr. June July Sept. Nov. Jan. Mar.
Diatoma
Fig. .36. Seasonal dislriliulioii of selertpd iiaiiMiipl.inktoii at Stiiail Station Csite 6).
50
Brigham Young University Science Bulletin
900
6 75
450
225
STUART STATION
CAMPGROUND
APRIL
JUNE
JULY
SEPT
NOV
JAN
MAR
Fig. 37. Density of narmoplankton at the campground (site 4) and Stuart Station (site 6)
Stuart Station were made on February 19 and
23, 1971. The results of tliese two samples are
summarized in Table 6. Tlie close correlation of
these two counts supports the reliability of the
sampling techniques used and also indicates rela-
tively stable conditions in the creek during this
four-day period.
In summary, the flora at Stuart Station dem-
onstrated many species of diatoms on the sub-
strate throughout the year with an Achiianthes-
Cocconeis-Protoderma community prevalent in
summer and early fall. Filamentous blue green
algae were important here throughout the year,
Table 6. Nannoplaiiltton totals for February 19 and
February 23, 1972, from Stuart Station.
February 19, 1972 February- 23, 1972
No. Percent No. Percent
Per Compo- Per Compo-
Liter sition Liter sition
Navicula
capitata
14,595
4.5
8,340
2.3
Navicula
Iripunclala
13,900
4.3
18,070
5.0
Other
Navicula
37,530
11.3
56,990
15.7
Cymbella
115,370
35.2
125,100
34.4
Gomphonema
33,350
10.2
38,225
10.5
Synedra
23,630
7.2
22,935
6.3
Nitzschia
47,955
14.7
47,260
13.0
Achnanthes
24,325
7.1
21,545
6.5
Diatoma
yulgare
4,170
1.3
9,730
2.7
Diatoma
hiemale
1,390
.4
1,390
.4
Gyrosigma
695
.2
695
.2
Surirella
2,085
.6
4,170
1.1
Cocconeis
4,170
1.3
3,475
1.0
Other
diatoms
4,170
1.3
5,500
1.5
especially in the summer-fall period. Hi/drurus
foetidus was abundant in spring and CAadoplwra
glomerata was quite prevalent in fall. The dom-
inant diatoms were Navicula, Cymbella, Gom-
phonema, Nitzschia, Achnanthes, Stjnedra, Coc-
coneis, Diatoma and Surirella.
Bear Canyon (Site 7)
Sampling at Bear Canyon was conducted
from July to November 1971. The stream gradi-
ent at this site was not steep and the stream ran
clear, usuallv with lower water flow than at
Stuart Station 9 miles downstream. Creen and
blue green algae were significant in the flora at
Bear Canyon. Ulothrix tenuissima was highest
in the net plankton in June, indicating that it
was an active stream bottom colonizer during
late spring. Oedogonium sp. and Cladophora
glomerata were prevalent throughout the sum-
mer in the plankton, and Oedogonium sp. was
also abundant on tlie substrate. Long streamers
of this alga were found on stones and a sub-
merged clay shelf in September and October.
In September Oedogonium sp. covered 12.3* of
the substrate and occurred with 79% frequency,
and in October it covered 7.2% of the substrate
and occurred in 86% of the plots studied. In Oc-
tober Spirogijra sp. filaments were intermingled
with the Oedogonium sp. strands. In November
the decrease in abundance of Oedogonium sp.
was accompanied by the initiation of growth of
Hijdrurus foetidus on the substrate. Much of the
creek bottom at Bear Canyon and upstream
was sandy and provided little habitat for the at-
tachment of benthic algae, and consequently.
Biological Series, Vol. 18, No.
Algae of Huntington Canyon, Utah
51
the total amount of attached algae was low in
these areas.
The seasonal cycle of Htjdrurtis foetidtis at
Bear Canyon probably was much the same as
at Stuart Station. It appeared in the late fall
and was Ukelv present throughout the winter,
since it was prevalent in the early spring when
the ice broke. Because of the high altitude and
consequent lower temperature of the water here,
H. foetidus persisted longer into the summer
than at sites lower in the drainage. Thus, this
species was abundant in tlie net plankton as late
as June 29, and still present in the July 30, 1971,
sample.
Growth of CladopJiora glomerata was not ex-
tensive at Bear Canyon, and when found, it
was covered with numerous epiphytic diatoms
such as Cocconeis placentula and Gomphonema
olivaceum. Filaments of several conjugate algae
were retrieved in net samples during the sum-
mer and early fall months. These algae largely
originated in protected environments upstream
from Bear Canyon where luxuriant mats of
Spirogi/ra sp. were observed in October. Spiro-
gijra sp. was more prevalent in these samples
in the fall while Moiigeotia sp. and Ztjgnema
sp. occurred mostly during the summer.
Closterium spp. (mostly C. moniJiferum) were
important in the creek at Bear Canyon. In July
their density in the net plankton was 67.5 cells
per liter and in August thev were present at 42
cells per liter. CAostcrium production in the
creek occurred in the substrate in protected
areas, among mats of filamentous algae and in
partially submerged streamside vegetation. These
same habitats were also the site of production
for Trachelomonas robusta, which appeared in
the creek in August, September, and November.
Nannoplankton samples were taken during
the August-November period. Tlie total numbers
varied somewhat from the figures obtained at
Stuart Station and in general were more stable
and quite consistently high (Table 7).
One reason for the stability in nannoplank-
ton levels at Bear Canyon was a large occur-
rence of Nitzschia palea and Gomplwnema oli-
vaceum in September, even though most other
genera decreased in numbers during this period.
A similar Nitzschia sp. pulse contributed to the
Stuart Station nannoplankton in September, but
the numbers of most other genera increased as
Table 7. Nannoplankton totals in cells per liter for
Stiiart Station and Bear Canyon for August-No-
vember 1971.
Aug.
Sept.
Oct.
Nov.
Stuart Station
Bear Canyon
116,741
215,576
310,271
218,223
66,435
112,295
282,768
265,056
well, thus producing a large pulse. This Sep-
tember increase at Stuart Station was followed
by a yearly low in October, which also occurred
at sites 1, 4, and Bear Canyon. A November
nannoplankton pulse was noted at Bear Canyon
as well as at other sites, caused by a general in-
crease in the numbers of most diatom genera.
A second reason for the plankton stability
in the upper drainage of Huntington Creek is
attributed to the terrestrial environment. The
terrain upstream from Bear Canyon consists of
large grassy valleys and rolhng mountains. Con-
sequently, late summer storms have less effect
on the right fork here than in the canyon im-
mediately above Stuart Station where the moun-
tain sides are steep and easily eroded during
storms, thus raising the water level rapidly and
increasing the silt load in the creek. This in-
creased silt load and high water is Hkely respon-
sible for scouring diatoms from the substrate
and thereby altering nannoplankton counts.
Tie Fork Pond (Site 5)
The lentic environment of Tie Fork Pond
provided a habitat uniquely different from that
of the swift flowing Huntington Creek, and thus
the flora here contained many algae which did
not occur in the creek. In addition, the cycles
of occurrence of some genera common to both
environments were very different.
Physical and chemical properties of the
water in Tie Fork Pond differed in several im-
portant aspects from that of the neighboring por-
tion of Huntington Creek. Silica fluctuated from
levels below to levels above those found in the
creek waters. Hardness was usually greater in
the pond, with magnesium hardness being much
higher and calcium hardness being somewhat
lower than in the creek. Total alkalinity in the
pond was higher and carbonate alkalinity was
usually present along with bicarbonate alkalinity.
Turbidity was also higher in the pond because
of abundant planktonic algal growth, and water
temperature was usually 5-I0°C higher since
the small pond was easily and rapidly warmed
by the sun.
The pond was completely frozen during the
winter. On March 11, 1972, it had begun to
thaw, but neither visible benthic algae nor
plankton were evident. A nannoplankton sample
taken from the pond yielded only a few diatom
fnistules which appeared to be left from the
previous year.
In April 1971, the pond was completely
thawed, and the remains of the previous year's
Chara mat were evident on the bottom. Fila-
mentous algae such as Oedogonium sp., Spiro-
52
Bricham Young University Science Bulletin
gtjra sp., and Microspora sp. were already float-
ing on the surface of the pond, indicating that
spring colonization is rapid. The plankton dur-
ing this month were predominately diatoms in-
cluding Navicula, Cijmhella, Gomphonema,
Sijnedra, Nitzschia, Achnanthes and Cocconeis.
Filamentous algae developed throughout the
summer ( Fig. 38 ) . By June a new growth of
Chara vulgaris was evident on the bottom and
Spirogyra spp. filaments were abundant through-
out the pond. Mougeotia spp. and Zt/gnetna sp.
mats were abundant near the south shore of the
pond wh(>re a culvert drained under the high-
way into the creek. In July Potomogeton sp. was
abundant in the pond and the Potomogeton-
Cfiara association completely covered the bot-
tom. Mougeotia (mostly M. gemiflexa) develop-
ment reached a climax during this month and
thoroughly saturated the water when it fonned
bright green fluffy "clouds" throughout the pond.
Tliis summer development of Mougeotia corre-
lated closely with its appearance in the net
plankton of the creek throughout the canyon,
indicating that the same developmental cycle
occurred in other habitats supporting Mougeotia
growth. Spirogi/ra spp. development occurred
mostlv in late summer and early fall in the pond,
similar to other locahties.
By August the water level in Tie Fork Pond
had fallen considerably and very little free
water above the Chara-Potomogeton cover was
present. Consequently, the filamentous green al-
gae declined considerably and generally became
restricted to narrow channels near the culvert.
Conditions in September were much the same
except that a new bloom of Mougeotia (mostly
M. gentiflexa) and Spirogt/ra sp. occurred in the
limited free water in the pond. The late summer
environment of August and September allowed
the rapid development of Oscillatoria limosa and
O. tenuis and, to a lesser extent, Lynghtja major
and L. aerugineo-coerulea.
The water level rose again in October and
by November, a 1-inch layer of ice covered the
pond. Extensive decomposition of the summer
acjuatic vegetation began beneath the ice, mak-
ing the water black and putrid.
Tie Fork Pond supported a large population
of diatoms throughout the studv, although sev-
eral genera, such as Gomphonema. Si/nedra,
Achnanthes, and Cymhella, declined in the sum-
mer months. Other genera, such as Nitzschia
(including N. palea, N. sigmoiclea, and N. linea-
ris), Epithemia (mostly E. gihha), Fragilaria
crotonensis, and F. virescens, were ver\' abun-
dant in the summer (Fig. 39). Nitzschia spp.
fluctuated throughout the study period from
.\pril to October. Epithemia (including E. gihha.
E. turgida, and E. argus) showed a maximum of
159,750 cells per liter occurring in July.
Fragilaria crotonensis and F. virescens oc-
curred throughout the summer. F. crotonensis
occurred in highest numbers in late June and
F. virescens in July. The bloom of F. crotonen-
sis was apparently much earlier here than in
the reservoirs on the left fork of Huntington
Creek, where the bloom occurred in October.
Tlie many nondiatom species present in the
nannoplankton and the large number of net
plankton during the summer in Tie Fork Pond
are characteristic of fresh water lentic environ-
ments. True plankters in the nannoplankton here
included: Trachelomonas robusta, which in-
creased in density throughout the summer to a
peak in October; Scenedesmus (mostly S. bi-
juga), which was most abundant in July ( 113,125
colonies per liter) but persisted in the flora un-
til October; N ephrocijtium hinatum, which ap-
peared in high numbers in July, declined in
August and September, and was essentially gone
by October; the desmid Sphaerozosma sp., which
composed 25% of the flora in August and Sep-
tember, appearing mostly as single cells rather
than in its typical colonial form; Cosmarium sp.,
which occurred throughout the season and
pulsed slightly in July and August; and Stauras-
trum sp., which occurred from June 29 to Oc-
tober 8, being highest in July and August. These
last two genera were of minor importance in
relation to the entire flora, never comprising
more than 37c of the total nannoplankton.
True plankters in the net plankton included:
Pandorina morum. which increased from July to
a maximum densitA' in September of 400 colonies
per liter; Euglerui spp., which were prevalent
throughout the season, occurring in greatest
numbers in August and September when they
reached 2,750 cells per liter; Chisterium (mostly
C. monilifcntm), which appeared occasionally
after May; planktonic Chroococcales (Cyano-
phyta) which occurred from July to October;
and species in Pyrrhoph\ta (mostly Peridinium
cinctum). which appeared in low numbers in
July, August, and October. Most of these algae
were not significant in numbers. Desmids, for
instance, were generally rare in Tie Fork Pond
and throughout the drainage since they are
more adapted to softwater and acid habitats
(Prescott, 1962) than to calcareous waters such
as those of Huntington Canyon.
Many euplanktonic algae were also found on
periphvton slides. Most of these probabU' settled
out of the water onto the slides and became a
part of the community developing there. For in-
stance, Scenedesmus was quite prevalent on the
slides throughout the summer. Butcher (1932)
Bi(M/^o:r\L Series. \<>i IS. No. 2 Ai.caf, ok Huntinoion C\nv(in, Utah
53
Total Net Plankton
1=2500 algae I
Selected Genera
1 = 2000 algae I
Apr. June July Sept.
Euglena
Mougeotia
Qscillatoria
Splrogyra
Fig. 38. Seasonal ilistribulioii of selerteil not plankton at Tic Fork Pond (site 5).
54
BniGiiAM VouNC. Univehsitv Science Bulletin
Total Nannoplonkton
1 = 100 olgae ml
Selected Genera
1=25 algae ml
Apr. June July Sept.
E pit he mi a
Scenedesmus
Fragilaria
Fifj. ^t. Sensorial distiibutioii of solciti-d iiiiiiiiopl.nikloii ^it Tii- Fork I'micl I site 5).
Biological Series, Vol, 18, No, 2 Alcae of Huntington Canyon, Utah
55
discussed Scenedesmus and other algae such as
Pediastrum and Ctjclotella that are cosmopohtan
in distribution and usually found on the bottom
of ponds, ditches, and slovv-flovving streams
where they live and reproduce until they are
disturbed and become a part of the plankton.
Production of diatoms on glass shdes in Tie
Fork Pond was generally less than in Hunting-
ton Creek, but since no current continually
washed the diatoms downstream, numbers in the
plankton of the two habitats were comparable.
Trends similar to those observed in Tie Fork
Pond occurred in other ponds throughout the
Huntington Canyon drainage. One such pond is
located adjacent to site 2. This pond maintained
an extensive mat of Cham vulgaris throughout
the year, with continual production and decom-
position adding to the 2 feet of black organic
mud on the bottom.
A pond located about 2 miles east of the
plant site was filled with moss rather than Chara.
In May this pond contained Microspora sp.
much as Tie Fork Pond and a bloom of Fragil-
aria virescens which continued through early
June. Microspora sp., Mougeotia sp. and Spiro-
gyra sp. were abundant here in the early spring,
and Oscillatoria limosa and O. tenuis became
abundant in late June. Epithemia gibba was
present from May to July and Navicula sp. and
Nitzschia sp. were abundant in early summer.
Green algae declined generally through the sum-
mer, while filamentous blue green algae, es-
pecially Oscillatoria tenuis and O. limosa, in-
Fig. 40. Shallow pond adjacent to the Right Fork of
Huntington Creek, These small ponds represent one
source of euplanktonic algae in the flora of Hun-
tington Creek, Photographed April 28, 1972,
creased greatly. Desmids were more abundant
in this pond than in any other habitat sampled
in Huntington Canyon. The dominant desmid
was Closterium rnoniliferum, common from July
to October.
A similar mossy pond is located one mile
above Stuart Station (Fig. 40). The spring flora
of this pond included Vaucheria geminata, Mou-
geotia parvula, and Ulothrix tenuissima. In June,
Spirogyra dubia occurred and Vaucheria gemiw-
ata disappeared. Draparnaldia plumosa was abun-
dant in June, as were Chlamydomonas sp., Clos-
terium moniliferum, C. erhenbergii, and C. ros-
tratum. Tliese desmids, along with Cosmarium
sp., were also collected throughout the summer
in floristic samples. Mougeotia genuflexa
bloomed in July and Spirogyra dubia and Oedo-
gonium sp. bloomed in August. Euglena (includ-
ing E. acus) was often present in the Spirogyra
mats. Epithemia sp. (mostly E. gibba) was pres-
ent throughout the season in this pond and was
most prevalent in August. Filamentous algae
became rare by October except for Oedogonium
sp. Spirogyra dubia became prevalent again in
November and was accompanied by a bloom of
Synedra (mostly S, ulna).
The third pond is adjacent to the Bear Can-
yon sampling site. Its flora consisted of Spiro-
gyra sp., abundant throughout most of the sea-
son except for July, Nitzschia sp. and Cymbella
sp. in June, and Zygnema sp. in July and Au-
gust. Epithemia gibba was also abundant in Au-
gust, as were several species that were also
found in Tie Fork Pond, including Oscillatoria
limosa, O. tenuis, and desmids. Staurastrum
eustephanum, especially, was common here in
July-September.
In September and October Amphipleura pel-
lucida appeared abundantly in this pond, and
Epithemia gibba continued abundant. Early fall
filamentous algae included Spirogyra sp., Zyg-
nema sp.. Mougeotia sp., and Vaucheria gemi-
nata. Tolypothrix larmta was prevalent in Sep-
tember and Oscillatoria tenuis became abundant
in October. Chara vulgaris was present in this
pond during the summer and fall season but did
not form the extensive mats found in Tie Fork
Pond.
Algal Flora of Huntington Canyon
Huntington Creek is a cold, clear, fast-flow-
ing, calcareous stream, which supports a diverse
algal flora adapted to these conditions. Diatoms
are the most abundant algae present, occiuring
throughout the year on the substrate and in the
plankton. Tlie dominant genera are Navicula,
Ci/mbella, Gomphonema, Nitzschia, Synedra,
Achnanthes, and Diatoma. Diatoms show maxi-
56
BniGHAM Young University Science Bulletin
mum production on the substrate in late spring
and early summer and in late fall and early
winter.
Benthic diatoms are the main contributors
to the nannoplankton, and the composition and
seasonal fluctuations of the nannoplankton are
largely determined by similar fluctuations on
the substrate. Water level fluctuations, water
temperature changes, and mechanical distur-
bances also appear to be factors influencing
nannoplankton levels.
Pcriphyton colonization is higher in the right
fork of Huntington Creek than lower in the can-
yon, and nannoplankton amounts increase as
the water moves downstream. However, the in-
crease is not entirely cumulative since destruc-
tion of cells occurs in the turbulent water.
True planktonic algae, including Asterionella
formosa. Frapilana crotonensis, Dinohnjon cijl-
inclricum, Pandorina morum, and Cerathim hir-
undinella occur in the plankton of Huntington
Creek. These algae are thought to originate in
reservoirs on the upper drainage of the left fork
of Huntington Creek, and their occurrence in
the creek basically correlates with algal cycles
in these reservoirs.
Filamentous algae are also important con-
stituents of the Huntington Creek algal flora.
Hydrurus foetidus grows profusely from late
winter to early summer, especially in the upper
reaches of the canyon, forming thick mucilagi-
neous growths on stones and rocks on the stream
bed. Blue green algae are present on the creek
substrate throughout the year, but show high-
est production during summer and fall when
encrusted communities form on the stony sub-
strate. Other filamentous algae present in the
canyon include Ulothrix tenuissima, U. zonata,
and Stigeoclonium stagnatile, which occur most-
ly in the spring, and Mougeotia spp., Spirogyra
spp., Zt/gnerna spp., and Vaucheria geminata,
which grow in backwaters, pools, and ponds
along the creek through the summer and fall.
Fragments from these filamentous algae are
an important source of net plankton. Hydrurus
foetidus fragments are prevalent in the plankton
in the spring, and filaments of blue green algae
occur in large quantities during October and
November. Most filamentous green algae occur
during the summer months, and they are most
prevalent in the right fork where protected areas
along the stream channel allow for their de-
velopment (Fig. 41). Most of these filamentous
algae are quickly destroyed as they are carried
downstream by the current.
Cladophora glomerata and Oedogonium sp.
also occur in significant numbers in Huntington
Creek. C. glomerata is most abundant in the
lower reaches of the right fork during the fall,
and Oedogonium sp. is most abundant in the
upper right fork during the same period. These
genera are likewise prevalent in tlie lower Hun-
tington Creek as it flows through Castle Valley,
where they form long streamers from the stones
during late spring and early summer.
Chara vulgaris occurs in lower Huntington
Creek from July to December, forming large
mats and sometimes filling large sections of the
stream channel.
Diatoms important in the flora of the lower
Huntington Creek include Navicula, Nitzschia,
Diatoina, Gomphonema, Synedra, Surirella,
Cymhella, Cocconeis, Achnanthes, and Cyclo-
tella.
Ponds in the drainage support abundant sum-
mer algal floras. Filamentous algae, desmids,
and such motile genera as Chlamydomoixas, Eu-
glena, and Trachelomonas are common constitu-
ents of these floras.
Fig. 41. A small tributary of Huntington Creek (A)
with profuse growths of Microspora willeana and
Cladophora glnmrrata. Photograj)he<i April 28. 1972.
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah
ACKNOWLEDGMENTS
57
This investigation was supported in part by
Biomedieal Sciences Support Grant FR-5 505
RR0711-03 from the General Research Support
Branch, Division of Research Resources, Bureau
of Health Professions Education and Manpower
Training, National Institutes of Health. Support
was also received from a Brigham Young Uni-
versity research grant, from a grant by Utah
Power and Light Company to the Brigham
Young University Center for Health and En-
vironmental Studies, and from National Science
Foundation Undergraduate Research Participa-
tion Grant GY-9052.
APPENDIX I
NET PLANKTON, NANOPLANKTON, PERIPHYTON, AND
N'ISIBLE BENTHIC ALGAL TABLES
Table 8. Number of organisms per liter and relative abundance of net plankton at Lawrence (Site 1)
Algae
4/15
.5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
Chroococcales
18.5
3.8
2.9
—
—
—
_
—
—
—
—
12.1%
—
—
5.9'^
14.1%
—
—
—
—
—
—
Oscilhltoria
23.0
3.9
7.5
—
—
1.9
—
_
4.5
4.1
3.8
1.5.0
59.71
—
2.5%
1.4%
—
—
9.2"^
—
—
59.2<?
16.3%
2.9%
3.2%
Oth.T Oscillii-
—
—
—
3.0
1.9
20.0
.6
.5
2.5
—
toriaceat^
—
—
—
—
—
—
14.8",
2.3.6T
87.3%
7.8%
2.07,.
1.9%
—
Chlamydomonas
—
—
4.3.0
—
—
—
1.9
—
—
—
-
-
-
—
—
28.1%
—
—
—
9.2%
—
—
—
—
—
—
Pandoriuu
—
—
—
55.5
—
—
.6
—
—
—
—
—
—
morum
—
—
—
10.5'/-;
—
—
3.0%
—
—
—
—
—
—
Pcdiwitrum
—
—
_
1.5.0
—
_
—
—
—
—
—
—
—
—
_
_
2.8%
—
—
—
—
—
—
—
—
—
Ulothrix
_
7,7
—
—
—
_
14.4
109.7
246.0
—
—
5.0%
—
—
—
—
—
—
—
■57.4%
84.7%
51.7%
Sti^t'ociuuium
—
—
—
—
_
—
—
—
—
.6
—
—
—
—
—
_
_
—
—
—
—
—
7.8'v
—
—
—
OfUo^iitiium
7.7
49.0
423.0
25.5
22.5
2.5
.6
—
1.9
4.1
5.0
.36.0
—
5.8%
32.0%
80.3%
69.4%
35.3%,
12.3%
7.8%
—
25.0%
16.3%.
3.9%
7.6%
('tuditjtfiora
15.5
86.0
18.5
18.0
3.8
—
—
1.7
—
—
—
5.5
36.0
^hnnnata
40.3'-;
64.9';i:
12.1%
3.4<f„
10.2%
—
—
21.5%
—
—
—
4.2%
7.6%
Spirii^yra
_
_
_
_
_
.6
—
—
3.0
15.0
—
—
—
—
—
—
—
7.8%
—
-
—
2.3':!
3.2%
Xy^nctna
^
—
_
_
—
1.5
—
—
—
—
_
_
—
—
—
—
—
—
6.0%
—
—
C.lostcrium
7.7
3.8
3.8
—
—
—
—
—
—
—
—
—
5.8'7<
—
.7%
10.2%
—
—
—
—
—
—
—
—
Cositiariurii
—
_
—
—
—
7.5
—
—
—
—
—
—
—
—
—
—
—
—
11.7%
—
—
—
—
—
—
—
Stiiurii^tntnt
—
—
_
.6
1.3
—
—
—
—
—
—
—
—
—
—
—
3.1%
15.8%
—
—
—
—
—
I'lilirotatiiiiitit
—
—
—
_
—
—
.6
—
—
—
—
—
—
—
—
—
—
—
—
7.8%
—
—
—
—
—
Eufflejia
31.0
12.4
3.8
.3.8
_
—
.6
1.7
—
.5
—
—
—
2.3.4%
8.1%
.7%
10.2%
—
—
7.8%
7.4%
—
2.0%
—
—
riutcus
—
—
—
—
—
—
1.3
—
—
—
—
—
—
—
—
—
—
—
—
5.4%
—
—
—
—
Ceratium
—
_
_
—
—
.30.0
6.7
—
—
—
—
—
—
hirundinetta
—
—
_
47.1%
3.3.0%
—
—
—
—
—
—
Vaurhrria
—
—
_
.6
—
—
—
—
22.5
—
—
_
—
7.8%
—
—
—
—
4.7%
Hydrurus
_
—
—
_
—
—
—
—
105.0
fnftidus
—
—
—
—
—
—
—
—
—
—
—
—
22.0%
Total .Mgae
.38.5
1.32.4
153.0
526.5
36.8
6.3.8
20.1
7.9
23.0
7.6
2.5.1
129.5
475.5
58 BiiicHAM YouNO Univkhsity Science Bulletin
Table 9. Number of organisms per liter and relative abundance of nannoplankton at Lawrence (Site 1)
Algae
4/15
5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
Cyctotella
1.042
4,180
46.200
79,250
25,716
15,567
11,620
5,560
22,240
48,6.50
27,800
—
—
.4%
2.9%
11.8%
36.4%,
13.9%
18.6%
2.97„
2.0%
2.8%
2.5%
1.2%,
Diatiyma
4,010
4,170
4.170
1,042
—
—
_
—
—
—
—
58,380
69,500
tenui'
1.1%
1.3%
1.6%
.7%
—
—
—
—
—
—
—
2.9%
3.0%
Diatoma
1,390
8,060
5,550
696
—
—
—
—
—
695
11,120
—
13,900
vulnare
A%
2.4%,
2.1%
.5%
—
—
—
—
—
.2%
1.4%
—
.6%
Fratiilaria
798
.2%
—
—
—
—
—
—
—
—
—
—
—
—
Sftridion
798
.2%
6.344
-
-
-
-
-
-
-
-
-
-
-
-
Sytiedra cf.
12,2.30
9,720
5.560
6,670
pulchella
I.77o
3.7%
3.7%,
3.9%
—
—
—
—
1.6%
—
—
—
—
Synedra cf.
30,126
20,570
9,312
11.120
4,180
348
1,668
20,961
160,015
41,700
278,000
497,000
291,900
ulna
8.3%
6.1%
3.6%,
7.9%
1.1%
.2%
.9%
25.1%
41.2%
14.8%
35.2%
24.5%
12.7%
Achruinthes
6,344
_
1,390
696
8,360
35,500
44,.500
13,900
29,190
20,850
48,920
136,220
97.300
1.7%
—
.5%,
.5%
2.1%
16. ,3%
24.0%,
16.6%
7.2%
7.4%
6.2%
6.7%.
4.2%
Cncconeis
798
—
—
4,338
5,560
52,500
9,035
5,837
23,240
11,676
44,480
136,220
194.600
.2%
—
—
3.1%
1.4%,
24.1%
4.9%
7.0%
5.7%
4.1%
5.6%
6.7%
S.4%
RhdicosphtTiia
_
1,390
—
—
—
—
—
—
—
1,390
5,560
_
—
—
.4%
—
—
—
—
—
—
—
.5%
.7%
—
—
Amphtprora
_
_
348
696
348
_
—
696
2,780
695
—
—
—
—
—
.1%
.5%
.1%
—
—
.S%
.7%
.2%
—
—
—
C'.yrosinma-
1,.589
2,780
4,448
4.448
89,250
4,170
1,.390
2,780
7,505
4,726
11,120
29,19U
13.900
Phxirosi^ma
.4%
.8%
1.7%,
3.1%
22.8%,
1.9%
.8%
.3..3%
1.9%
1.7%
1.4%
1.4%,,
.6%
Navicula cf.
1.5,888
11,120
3,0.57
1,042
10,700
2,085
—
—
—
—
—
—
83,400
tripunctata
4.4%
3.3%
1.2%
.7%,
2.7'7„
1.0%
—
—
—
—
—
—
3.6%
Other
88,959139,000
97,300
36,488
40,387
15,919
12,075
6,5.50
50.040
65,886
111,200
369,740
333,600
Naviclua
24.3%
41.7%
37.1%
25.8%
10.4%,
7.3%
6.5%
7.8%
12.4%
2.3.3%
14.1%
18.3%
14.5%
Piuuularia
—
—
—
—
—
—
—
—
—
—
—
9,730
.5%
77,840
—
CioniphotnTna
68,805
7,060
26,062
7,.506
I
27,800
gracil e
—
—
—
—
—
—
.37.1%
8.3%
6.4%
2.7%
—
3.8%
1.2%r
Gomphonema
23,543
6,670
1,390
3,480
11,275
1,668
4,865
2,780
348
7,.505
71,160
194,600
542,100
olivaceum
6..5%
2.0%,
.5%,
2.5%
2.9%
.8%
2.6%,
3.3%
.1%
2.7%
9.0%,
9.6%
23.5%
Cymbt'lla
109,611
1,.390
2,367
2,088
8,360
3,750
1,668
—
3,335
2,085
33,360
68,180
180,700
30.0%
.4%
1.0%
1..5%
2.1%,
1.7%
.9%
—
.8%,
.7%
4.2%,
3.4%
7.8%,
Epithrmia
—
-
-
-
-
-
-
-
-
-
-
—
13,900
.6%,
S'itzschia
2,780
6,950
3,480
696
1,390
1,668
2,085
I
z
I
acicularis
—
—
1.1%
4.9%,
.9%
.3%
.8%
2.0%
.5%
—
—
—
—
Nitzschia
—
—
—
—
—
1,042
1,168
1,042
4,170
—
—
_
55,600
deriticula
—
—
—
—
—
.5%,
.6%
1.2%„
1.0%
—
—
—
2.4%
Other
46,760
94,.520
104.2.50
41,800
163,000
18,632
10, .508
2,780
65,330
92,296
115,640
291,900
305,800
Nitzschia
12.8%.
28.3%,
40.9%
29.5%
41.7%
8.6%
5.7%
3.4%
16.2%
32.7%
14.6%
14.4%
13.3%,
Surirrtla
22,874
31,690
13,900
3,480
_
_
1,390
348
12,510
20,015
37,800
107,030
55,600
6.3%
9.5%
5.3%
2.5<!t
—
—
.8%
.4%.
3.1%
7.1'v
4.8%
5.3%
2.4%
Other
4,168
—
—
11,120
Pen n ales
1.2%
—
—
7.8%
—
—
—
—
—
—
—
—
—
Scenedcsmus
-
-
-
-
-
.348
.2%
215,908
-
-
-
-
-
-
-
Tot.il \Iv:,M
364,000 333,590
261,024
139.224
391,100
184,178
81,969
404,900
282,586
790,600 2024,680
2307,400
Bioi.oGicAi. Sehies, Vol. 18. No. 2 Algae of Huntington Canyon, Utah
59
Table 10. Number of organisms per cm^ and relative abundance of periphyton on glass slides at Lawrence (Site 1)
Algae
5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
CyclotcUa
810
—
304
2,045
20,900
6,075
6,281
1,523
2,574
304
288
.3%
—
.7%
10.0%,
21.67c
5.77c
3.2%,
1.2%
.6%,
3.7%
1.17c
Diatoma
9,320
204
102
—
1,020
52
206
1,235
48,392
536
1.9<t
.7%
.2%
—
1.17c
.1%
.1%
.9%
11.07c
—
2.1%
Frafiilaria
404
_
206
309
.1%
—
—
—
—
.27c
.1%
—
—
—
—
Sytiedra ct.
29.3,211
7,1.57
10,000
—
_
_
—
—
pulchclla
60.9'-f
24. 9-^^
21.8%
—
—
—
—
—
—
—
—
Synedra cf.
18,800
1,132
849
479
1.624
2,368
7,619
49,999
115,833
2,317
4,5.30
ulna
3.9T^
3.9%
1.97,,
2.4%
1.77c
2.27c
3.8%
38.27
26.37c
27.8%.
17.67c
Achruinthes
19,411
204
3,090
68
26,000
51,996
—
27,594
62,292
309
412
4.0'7f
."%
6.7%,
.3%
26.97c
49.0%,
—
21.17c
14.17o
13.0%
1.6%
Cocconeis
—
—
10.400
3,889
22,100
5,910
5,354
2,183
5,150
1,081
535
—
—
22.7%
19.0%
22.9%
5.6%
2.6%
1.7%
1.27c
3.77c
2.17c
Amphiprora
2,030
—
102
—
—
—
103
—
2,059
—
—
.4%
—
.2%
—
—
—
.17c
—
.5%
—
—
Gyrosigma-
38,822
808
204
4,727
_
_
618
288
515
—
700
Pleurosigma
8.1<J
2.9'^r
.47c
23.0%
—
—
.37c
.2%
.1%
—
2.7%
Savirula
69,610
6,152
3,218
5,309
8,108
4,223
16,268
17,009
56,115
927
6,177
U.-S'^J
21.47,
7.0%,
26.0%
8.4%
4.0%
8.27c
13.0%
12.7%,
11.1%
24.07c
Gontpfwnt^ia
—
—
_
_
_
—
17,297
—
—
309
—
gracih'
—
—
—
—
—
—
8.7%
—
—
3.77c
—
Com phonttna
4,040
1,886
1,320
34
2,1.30
25,6.38
2,368
10,996
41,185
1.236
5,231
olivaceum
.87c
6.6'^c
2.9%
.27c
2.2%,
24.0%
1.2%
8.47.
9.3%
15.37c
20.47c
CymbeUa
810
2,216
2,150
625
—
247
1,441
1,.3.59
2,574
309
1,770
.2'v,
7.7%
4.7%
3.0%,
—
.27c
.7%
1.07c
.6%
3.77c
6.97c
Sitz-schia
_
8,186
4,422
2,238
4,060
4,716
133,851
15,650
80,311
1,081
3,583
—
28..5<-f
9.6'5
11.0%
4.2%,
4.57,
67.4%
12.07c
18.2%
13.07c
13.97c
Surirdla
14,127
486
304
34
—
_
_
2,347
14,930
463
1,2.35
2.9%
1.8%
.7%
.2%
—
—
—
1.8%
3.4%
5.6%
4.87c
Other
1,210
304
2,250
138
—
—
—
—
—
—
124
Pennales
.3%
1.17c
4.9%
.7%
—
—
—
—
—
—
.5%
Chroococcales
4,860
_
_
—
408
—
—
—
—
_
—
1.0<5
—
—
—
.4%
—
—
—
—
—
—
Oscillatoria
3,240
—
812
410
_
_
_
124
515
_
288
.7%
—
1.87o
2.0%
—
—
—
.1%
.1%
—
1.17c
Other Oscillator-
—
—
—
—
9, .300
—
—
—
—
—
—
iaceae
—
—
—
—
9.6%
—
—
—
—
—
—
Ulothnx
-
-
-
-
-
-
-
-
3,604
.8%
-
288
1.17c
Proloderma
I
I
3,192
3,706
—
—
—
—
—
3.07,
1.9%
—
—
—
—
Stigeocloniuvi
-
-
-
-
-
-
-
-
3,089
.7%
1,544
-
—
Oedogonium
2,040
150
812
1,071
2,.578
412
—
—
—
—
4.4%
.77c
.8%
1.0%
1.3%
.3%
.3%
—
—
Cladophora
—
—
849
—
204
_
618
—
515
—
—
—
—
1.9%
—
.2%
—
.37
—
.1%
—
—
Other Filamen-
—
—
2,040
_
1,220
—
—
—
—
—
—
tous Chlorophyta —
—
4.4%
—
1..3%
—
—
—
—
—
—
C:lostrrium
—
—
612
.50
—
—
—
—
—
—
—
—
—
1.4%,
.2%
—
—
—
—
—
—
—
Cosmarium
-
-
-
-
-
52
.1%
—
—
—
—
—
Euglena
1,210
406
175
—
—
_
_
—
.3%
—
.97
.97
—
—
—
—
—
—
—
Total Algae
481,915
28,735
4.5,474
20,372
97,886
105,746
198,617
1.30,719
441,197
8,341
25,697
60 BRir.iiAM YouNC University Science Bulletin
Table 11. Number of organisms per liter and relative abundance of net plankton at plant site (Site 3)
Algae
4/15
1971
5/13
1971
6/8
1971
6/29
1971
7/30
1971
8/20
1971
9/15
1971
10/8
1971
11/15
1971
12/17
1971
1/20
1972
2/19
1972
3/11
1972
Chroococcales
-
15.5
3.0%
3.9
1.0%
—
11.2
4.2%
165.0
17.6%
3.5
1.0%
2.3
1.5%
—
—
—
—
—
Oscitlatoria
Other Oscilla-
toriaceae
69.5
40.7%
233.0
45.4%
-
3.8
1.4%
45.0
18.8%
18.2
1.9%
11.2
1.2%
15.8
4.4%
64.7
17.9%
10.5
6.9%.
47.0
30.7%
120.0
22.9%
367.0
70.0%
3.1
20.7%
5.7
38.0%
5.2
14.0%,
7.6
20.5%,
5.5
7.1%
4.3
5.5%
17.5
8.2%
9.8
4.6%
Anabaena
-
-
-
-
-
-
—
1.8
1 l%i
—
—
—
—
—
Chlamyd(ym(>nas
-
-
-
-
-
-
1.8
.5%,
78.7
21.7%
1.8
1.1%.
10.5
6.9%
-
-
-
-
-
Pandorina
moTum
-
-
-
15.0
5.6%
67.5
28.0%
78.0
8.3%
-
-
-
-
-
Other Volvo-
—
—
—
—
—
3.8
—
—
—
—
—
—
—
caceae
—
—
—
—
—
.4%
—
—
—
—
—
—
—
Ulothrix
—
—
96.0
25.3%.
30.0
11.3%.
3.8
1.6%
7.5
.8%
—
3.5
2.3%
—
—
1.5
4.0%
3.8
4.8%
11.0
5.2%
StigeocUinium ________ 22.5 — 2.6 _ 1.3
________ 4.3% _ 7.07o — .6%
Oedogonium — — 3.9 .37.5 _ 3.8 54.2 28.0 _ _ 1.0 .6 2.5
_ — 1.0% 14.1% — .4% 15.0%, 18.3% — _ 2.7% .8%, 1.2%
Cladophora — — 7.7 44.9 1.5.0 18.0 _ 9.3 7.5 .6 — 1.3 1.3
Rlomerala — — 2.0% 16.9% 6.3% 1.9%, — 6.1% 1.4%, 4.0% _ 1.6% .6%
M(mgeotia — — — — 7.5 — — 1.8 — — — — —
_ _ _ _ 3.1% — — 1.1% _____
Spirogyra _____ 11.2 7.0 11.0 3.8 3.1 _ .6 2.5
_ — — — — 1.2% 1.9% 7.2% .7% 20.7% — .8%, 1.2%
Zygnema _ _ _ _ 15.0 _ _ 3.0 — 1.9 .5 — —
— — — — 6.3% _ — 2.0% _ 12.7%, 1.3% _ —
Other Filamen- 23.2 15.5 11.6 — — 3.8 7.0 _ — .6 6.1 — —
tousChloro- 13.6%, 3.0%, 3.1% _ _ .4% 1.9% _ _ 4.0% 16.4%, _ _
phyta
ClosteHum _ _ _ _ 22.5 3.8 1.8 1.8 — — 1.0 .6 1.3
— — — — 9.4%, .4% .5% 1.1% — — 2.7% .8% .6%
Cosmarium — — — — 3.8 — — — — — — — —
Staurastrum _ _ 7.7 — 22.5 93.7 — 1.8 — — — — —
— — 2.0% — 9.4% 9.9% — 1.170 — _ — — —
Euglena _____ 3.8 _ 1.8 _ _ _ _ _
— — — — — .4%, _ 1.1%, _____
Ceratium hir- _____ 17.4 127.7 7.0 7.5 — — — —
undindla _____ 5.0% 35.3%, 4.6%, 1.4%, _ _ _ _
Other Pyrrho- — _ 3.9 _ _ _ _ 8.7 _ _ _ _ _
phyta _ _ 1.0% _ _ _ _ 5g<5[, _ _ _
Hydmms 78.0 248.0 244.0 135.0 25.5 _ — _ _ _ 11.6 62.0 165.0
foetidus 45.7%, 48.4% 64.0'"^ .50.7% 10.7%, _____ 31.3% 80.1% 77.5%
Total Algae 170.7 512.0 378.8 266.2 239.3 939.2 362.2 151.6 528.3 15.0 37.1 78.7 212.2
BiOLOGiCAi, Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah 61
Table 12. Number of organisms per liter and relative abundance of nannoplankton at plant site (Site 3)
Algae
4/15
5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
Cyclotella
2,780
—
3,127
2,780
—
—
—
695
_
_
—
—
—
.4%
—
.9%
.5%
—
—
—
.8%
—
—
—
AsttTionella
—
—
59,490
30,250
13,344
6,115
3,335
6,096
—
—
—
—
—
—
—
8.7%
9.6%
3.9%
1.0%
.4%
1.2%
—
—
—
—
—
Hannaea
1,390
47,260
13,066
1.042
—
—
695
—
_
1,668
2,780
3,892
arms
—
.5%
6.9%
4.1%.
.3%-
—
—
.1%
—
—
1.2%,
1.1%,
1.3%
Diatoma
—
1,390
2,780
695
—
—
—
—
—
—
—
—
973
hifmalf
—
.5%
.4%
.2%
—
—
—
—
—
—
—
—
.3%
Diatoma
—
—
—
—
—
—
_
18.348
6,960
21,545
8,757
tillUC
—
—
—
—
—
—
—
—
—
20. 27^
4.9%
8.5%.
2.970
Diatoma
3,475
4,170
2,780
3,475
7.086
10,286
11,120
13,100
1,737
1.668
4,450
2,780
1,946
vul^are
.5%
1.4%
.4%
.9%
2.1%
1.7%
1.2%
2.5%
1.1%
1.8%,
3.2%
1.17c
.6%
Fra^ilaria
1,390
—
1,390
2,780
80,620
3,474
1.390
1,042
695
973
—
—
—
.5%
—
.2%
.3%
15.4%
2.2%.
1.5%
.7%
..3%
.3%
Mi^ndioti
—
_
—
695
1,042
1,390
—
—
—
—
—
—
—
—
—
—
.2%
.3%.
.2%
—
—
—
—
—
—
—
Synedra
90,350
26,130
28,910
9,730
4,170
11,125
25,020
44,480
11,812
6.950
1.5,985
20,850
25,298
14.1%
8.9%
4.27^
3.1%
1.2%
1.9%
2.8%
8.5%
7.6%
7.77-
11.37-
8.2%
8.3%,
Achtuinthes
3,475
8,340
19,460
19,460
42,600
75,500
29,745
30,580
3,474
6,533
6,255
11,120
18,487
.5%
2.8%
2.7%
6.2%
12.3%
12.69fc
3.2%
5.8%
2.2%,
7.2%
4.47c
4.4%
6.1%
Cocconeis
—
2,780
—
—
5,004
14,400
2,780
4,170
1,737
695
1,042
695
1,946
—
.9%
—
—
1.4%
2.4%
.3%
.8%
1.1%
.8%
.77c
.37c
.6%,
Amphipleura
—
—
—
_
—
—
695
2,085
—
347
—
—
973
—
—
—
—
—
—
.1%,
.4%
—
.4%,
—
—
.37.,
Navirula cf.
1,390
1,390
695
—
—
_
—
—
_
4,4,50
1,390
973
capitata
—
.5%.
.5%
.2%
—
—
—
—
—
—
3.2%
.57c
.37c
Navicuta cf.
—
—
—
695
4,170
10,286
44,505
15,290
1,737
—
—
—
—
rhyncocephala
—
—
—
.2%
1.2%
1.7%,
4.9%.
2.9%
1.1%
—
—
—
—
Navicuta cf.
—
_
—
18,070
13,344
32,500
43,085
13,900
15,287
—
5.560
13,205
18,487
tripunctata
—
—
—
5.7%
3.9%.
5.4%
4.7%
2.5%
9.8%.
—
3.97-
5.2%
6.1%
Other
104,250
41,700
115,650
35,305
59,826
93,144
120,930
45,035
15,287
12,093
1.5.568
20,8.50
35,028
.Voficii/a
16.2%
14.2%
15.8%
11.2%.
17.3%
15.6%
13.47o
8.7%
9.8%
1.3.3%,
11.17c
8.27c
11.57c
StauToneis
—
—
—
—
—
348
695
_
—
—
—
—
—
—
—
—
—
—
.3%
.37c
—
GomphoniTna
139,000
94,520
116.760
19,460
.30,024
60,500
65,330
26,400
10.425
2,780
15.985
.52,820
75,894
21.6%
32.2%
17.0%
6.2%
8.7%
10.1%
7.2%
5.0%
6.7%
3.1%
11.. 3%
20.8%
24.87c
Cymbclta
205.520
58,380
150.120
113,980
90,375
145,500
216,505
80,620
29.187
15,985
25.993
62,5.50
6.5,191
32.0%
19.9%
21.9%
36.1%
26.2%
24.3%
23.8%
15.4%
18.7%
17.7%
18.4%
24.6%
21.3%
Nitzschia
—
—
—
695
5,004
2,084
2,362
2,362
—
—
—
—
—
acicularis
—
—
_
.2%
1.4%.
.4%.
.3%
.4%
—
—
—
—
—
Other
86,175
46,980
129,550
44,420
.59.175
119,416
328,038
136,220
60.462
22,935
34,333
42,395
44,758
Nitzschia
13.4%
16.5%
18.9%
14.1%
17.2%.
19.9%
36.1%
26.0
38.7%
25.3%
24.37c
16.77c
14.67c
SurircUa
10.425
4,170
1,.390
695
1,042
2,780
9,7.30
3,335
1.737
347
696
—
1,946
1.6%
1.4%
.2%
.2%
.3%
.5%
1.0%
.6%
1.1%
.4%
.57c
—
.6%
Other
—
1,390
7,230
3,335
1,042
—
695
—
—
—
696
695
—
Pennales
—
.9%
1.1%
1.1%>
.3%
—
.1%
—
—
—
.5%
.6%
—
Dinnbrynn
—
—
1,390
1,390
3,127
8,900
695
20,016
—
—
—
—
—
—
—
.2%
.4%
.9%
1.5%,
.1%
3.8%
—
—
—
—
—
Total Algae
642,670 292,730
686,940
317,501
344,544
598,096
907,350
52.5,004
1.56.356
90,766
141,031
255,065
305,522
62
BmcHAM Young University Science Bulletin
Table 13. Number of organisms per cm^ and relative abundance of periphyton on glass slides at plant site (Site 3)
Algae
5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
Cyclotetla
-
-
-
-
204
.2%
-
62
.2%,,
—
—
-
-
Asterionella
~_
445
850
202
612
62
—
.5%
1.0%
.1%
.6%
—
.2%c
—
—
—
—
Hannaea
154
445
1.740
496
_
_
—
371
—
154
309
arcus
.6%
.5%
2.0%,
.3%,
—
—
—
1.1%
—
.3%
1.6%
Diatoma hitinale
-
51
.1%
-
-
204
.2%
-
-
—
—
—
—
Diatoma tiiiue
z
I
2,625
1,081
—
—
—
—
—
—
—
—
—
5.1%,
5.7%
Diatoma vulgare
_
51
406
598
847
1,544
474
2,.595
407
309
154
—
.1%
.5%
.4%,
.9%
3.2%
1.4%
8.0%
5.1%
.6%,
.8%
Fratiilnria
—
—
—
—
—
—
350
247
—
_
154
CTotujicnsis
—
—
—
—
—
—
1.1%
.7%
—
—
.8%,
Meridian
—
51
.1%
2.062
-
—
—
—
-
-
-
-
-
Synedra
3,855
4.530
2,393
3,420
762
1,503
3,830
678
3,861
1.081
14.0%
2.5%
5.2%,
1.5%
3.5%,
1.6%,
4.5%
11.8%,
8.4%,
7.5%,
5.7%,
Achnanthcs
1,.390
3.960
10.300
94,100
13,340
15,589
2,060
1,606
325
2.008
618
5.07o
4.8%,
11.7%,
57.1%,
13.7%
32.3%,
6.29t
5.0%.
4.1%,
3.9%
3.3%
Cocconeis
103
—
—
596
305
1,174
144
—
—
—
—
.4%
—
—
.4%,
.3%.
2.4%
.4%.
—
—
—
—
Amphipleura
—
—
64
52
206
864
154
—
—
—
—
.1%.
.1%
.6%
2.7%.
—
—
.8%,
Navicula cf.
—
1,167
4,530
.5,335
6,997
556
2,471
1.831
407
1,390
463
tripunctata
—
2.0%
5.2%,
3.2%.
7.2%
1.2%
7.5%
5.7%
5.1%
2.7%.
2.4%c
Other Savicula
7.258
5,255
5,136
24,265
18.973
.3,913
6,322
2.707
868
3,707
772
26.4<7<
6.4%,
5.9%r
14.8%.
19.6%^
8.1%
19.1%
8..3%
10.8%
7.2%
4.1%,,
Gomphonema
6,067
14.415
10,300
5,050
2.501
3,027
885
2.348
732
18.688
7.877
22.0%
17.5%,
11.7%
3.1%.
2.6%
6.3%,
2.7%
7.. 3%,
9.1%
36.2^
41.5%,
Cymbctia
8,408
35,382
38,755
18,000
15.400
8,175
4,324
6.301
2.441
13.437
2.317
30.5%.
43.0%c
44.2%
10.9%t.
15.9%
17.0%
13.1%
19.5%,
30.4%o
26.0%
12.2%o
Nitzschia
—
_
_
920
406
206
—
—
acicularis
—
—
—
.6%
.4%
.4%
—
—
—
—
—
Other Nilzschia
—
17,649
6,062
9,240
32.094
12,397
12,335
9.267
1.627
5.406
3.861
—
21.4%,
6.9%,
6.2%
32.7%.
25.7%
36.9%.
28.7%
20.3%,
10.5%b
20.3%,,
Surirclla
201
303
536
503
204
154
144
371
68
.7%
.4%
.67o
.3%
.2%,
.3%
.4%
1.1%
.8%
—
—
Other I'ennales
—
294
2.183
_
_
52
62
—
—
—
—
—
.3%
2.5%
—
—
.1%
.2%
—
—
_
—
Dinohryoii
—
203
_
—
—
—
62
—
.2%
—
—
—
—
.2%
—
—
_
_
Osciltatoria
—
—
2.040
1.056
_
412
—
—
203
154
—
—
2.3%
.6%
—
.2%
—
—
2.5%
—
.8%
Other
93
—
_
1.151
1,877
103
1,853
—
203
Oscillatortaceae
.3%
—
—
.7%
1.9%
.9%
5.67o
—
2.5%
—
—
Anabacna
—
_
_
95
64
—
—
—
—
.17o
.1%
—
—
_
_
_
_
Ulothnx
_
_
—
95
103
—
—
—
.1%
—
.2%
—
—
—
—
—
Stigeoclonium
—
—
—
—
—
_
_
—
68
—
—
—
—
—
—
—
—
—
_
.8%,
—
_
Oedogonium
—
—
—
—
—
52
—
—
_
_
_
—
—
—
—
—
.1%
—
—
—
—
—
Other Filamentous
738
_
_
144
_
Chlorophyta
—
—
—
.4%
—
—
.4%,
_
_
—
—
Ctostmum
—
—
85
—
64
_
—
—
.1%,
—
.1%
EugltTia
-
51
1%
—
-
-
-
-
-
-
-
-
HydntrlM foetidus
51
247
95
z
—
.1%
.3%
.1%C
—
—
—
—
—
—
—
Total Algae
27.529
82.285
87.700
164.928
97,576
48,271
33,463
32.338
8,027
51..585
18.995
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah
63
Table 14. Number of organisms per liter and relative abundance of net plankton at campground (Site 4)
Algae
4/15
5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
Chroococcales
—
—
—
—
97.5
22.5
8.7
—
—
—
—
—
13.5%
1.2%
10.8%
—
—
—
—
—
Oscillatoria
93.0
123
3.9
7.5
3.8
15.0
30.0
7.7
33.7
4.5
3.1
2.5
7.5
60.0%
21.2%
.8%
2.4%,
2.9%,
2.1%
1.6%
9.6%
5.8%
14.6%,
9.5%,
4.4%
14.5%
Other Oscilla-
7.7
54.0
_
_
_
30.0
385.0
5.2
502.5
21.9
10.3
1.9
3.8
toriaceae
5.0%
9.3%
—
—
—
4.1%,
19.9%
6.5%
87.0%
69.9%,
31.4%
3.3%
7.2%
Anabaeria
—
7.7
1.3%
—
—
—
—
—
—
—
—
-
-
-
Chlamydomonas
I
15.0
I
I
1.8
I
I
~
I
I
—
—
—
—
11.5%,
—
—
2.2%
—
—
—
—
—
Pandorina
—
—
—
—
11.4
45.0
232.5
3.5
morum
—
—
—
—
8.6%
6.2%
11.9%
4.4%,
—
—
—
—
—
Other \'olvo-
—
—
—
—
—
3.8
—
3.5
—
_
_
—
_
caceae
—
—
—
—
—
.5%
—
4.4%,
—
—
—
—
—
Ulothrix
—
46.5
161.0
7.5
7.5
3.8
_
2.6
3.8
—
1.0
2.5
—
—
8.0%
32.0%.
4.0%
5.8%
.5%
—
3.2%
.6%
—
3.1%
4.4%
—
Stigeoctonium
—
—
—
—
_
—
_
_
22.5
3.9
1.5
—
2.5
—
—
—
—
—
—
—
—
3.9%
12.6%
4.6%
—
4.8%
Oedogonium
—
15.5
3.9
11.2
3.8
—
127.5
20.3
—
—
.5
—
—
—
2.7%
.8%
6.0%
2.9%
—
6.5%,
25.3%
—
—
1.5%
—
—
CtadophoTQ
—
—
11.6
15.0
15.0
15.0
_
4.4
_
.6
1.0
.6
_
glomerata
—
—
2.3%
8.0%
11.5%
2.1%
—
5.4%
—
1.9%
.3.1%
1.1%
—
Mougeotia
—
—
—
—
—
7.5
—
.9
—
—
—
—
—
—
—
—
—
—
1.0%
—
1.1%
—
—
—
—
—
Spirogyra
—
—
7.7%
—
—
—
—
7.7
_
_
—
.6
—
—
—
1.5%>
—
—
—
—
9.6%,
—
—
—
1.1%
—
Zygnema
—
_
_
—
33.0
3.8
—
.9
—
1.0
—
—
—
—
25.3%,
.5%
—
1.1%
—
—
.3.1%
—
—
Other Filamen-
7.7
—
3.9
_
—
—
—
—
—
—
2.0
.6
—
tous Chlorophyt
:a 5.0%
—
.8%
—
—
—
—
—
—
—
6.1%
1.170
—
Closterium
—
23.0
—
—
26.2
3.8
7.5
2.6
3.8
—
—
.6
.6
—
4.0%
—
—
20.2%
.5%
.4%
3.2%
.64%
—
—
1.1%
1.2%
Staurastrum
—
_
—
—
—
72.0
7.5
—
3.8
—
—
—
—
—
—
9.9%
.4%
—
.64%
—
—
—
—
Euglena
-
—
—
-
-
3.8
.5%
423.0
-
.9
1.1%
7.0
-
-
-
-
-
Ceratium hir-
I
I
I
I
I
1110.0
7.5
I
I
undinella
—
—
—
—
—
.58.4%
57.6%,
8.7%
1.3%
—
—
—
—
Other
—
7.5
Pyrrophyta
—
—
—
—
—
—
.4%
—
—
—
—
—
—
Hydrurus
46.5
310.0
309.0
146.8
15.0
12.4
48.0
37.5
foetidus
30.0%
53.5%,
62.0%
78.. 3%
11.5%
—
—
—
—
—
.37.8%
84.7%,
72.37o
Vaucheria
-
-
-
-
-
-
-
2.6
3.2%
80.3
-
-
-
-
-
Total Algae
154.9
579.7
501.0
188.0
130.7
724.0
1930.0
578.2
30.9
32.8
57.3
51.9
64 Bbicham Young University Science Bulletin
Table 15. Number of organisms per liter and relative abundance of nannoplankton at campground (Site 4)
Algae
4/15
5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
Cyclolella
4,170
—
1,668
—
—
_
1,042
—
—
—
_
_
—
.5%
—
.7%
—
—
—
.4%
—
—
—
Asterionella
—
—
46,425
88,9,50
13,200
2,357
1,390
2,085
2,085
1,042
—
—
—
—
—
9.0%
11.6%
6.1%.
1.0%
.2%.
.8%
.4%
.4%
—
—
—
llannaea
6,960
16,680
27,105
27,800
2,.362
348
695
—
1,390
3,058
1,390
4,170
3,475
arms
6.1'S
2.1%
5.3%
3.6%
1.1%
.2%,
.1%
—
.3%
1.1%
1.1%
1.0%
1.9%
Diatoma
2,432
_
4,170
3,335
_
—
—
—
—
—
696
—
1,390
hiifjialf
2.1%
—
.8%
.4%,
—
—
—
—
—
—
.5%
—
.8%
Diattrma
1,390
—
_
_
_
—
—
—
348
4,170
5,560
teiiue
—
_
.3%,
—
—
—
—
—
—
—
.3%
1.0%
3.1%.
Dialoma
5,912
12,510
2,085
8,895
2,780
1,668
15,845
3,335
20,016
4,865
4,450
9,730
4,865
vulnare
3.1%
1.6%
.4%
1.2%
1.3%
.7%
1.7%,
1.2%
4.3%
1.8%
3. .5%
2.3%
2.7%
Frti^lUiria
—
—
2,780
695
_
696
695
104,805
10,285
8,340
1,042
1,390
695
—
—
.5%
.1%
—
.31%
.1%
37.7%
2.2%
3.1%.
.8%
.3%
.4%
\feridion
_
12,510
6,9.50
2,780
—
—
—
—
—
347
—
1,390
—
—
1.6%
1.4%.
.4%
—
—
—
—
—
.1%
—
.3%
—
Synedra
6,602
46.702
11,675
22,795
7,200
5,560
20,8.50
9,730
20,8.50
10,703
17,653
33,360
8,340
5.8%
6.0%
2.3%
3.0%
3.3%
2.. 5%
2..5%
3.5%
4.5%
4.0%
13.7%.
7.8%
4.6%,
Achnanthes
1,740
.37,5.30
22,240
61,150
18,725
26,000
49,6.50
9,730
43,090
22,935
6,960
18,070
15,290
1..5%
4.8%
4.3%
8.0%
8.6%
11.5%
5.4%.
3.. 5%
9.2%
8.5%
5.4%
4.2%
8.5%
Cocconeis
1,390
—
695
1,390
696
6,255
6,096
_
2,780
3,0.58
1,668
2,780
695
1.2%
—
.1%
.2%
.3%
2.8%
.7%
—
.6%
1.1%
1..3%.
.7%
.4%
Rhoicos-
—
1,042
1,390
695
—
—
—
—
—
—
—
—
—
phfTiio
—
.1%
.2%
.1%
—
—
—
—
—
—
—
—
—
Amphipli-ura
—
—
—
—
_
—
—
_
695
695
—
1,390
—
—
—
—
—
—
—
—
—
.1%
.2%
—
.3%
—
Cyrosi^ma
-
-
-
-
-
-
-
695
.3%
-
-
—
1,390
.3%
-
Navicula cf.
695
1,042
I
695
I
I
695
2,085
8,340
2,085
capitata
.6%
.1%
—
.1%
—
—
—
.3%
—
—
1.6%
2.0%
1.2%
Navicula cf.
—
—
2,780
2,085
—
3,052
45,035
1,390
5,560
1,042
—
—
4,865
rhyncocephala
—
—
.5%
..3%
—
1.4%.
4.9%.
.5%
1.2%
.4%
—
—
2.7%
Navicula cf.
—
—
—
18,070
10,007
7,225
56,155
7„505
19,460
9,313
,5,838
18,070
13,205
tripunctata
—
—
—
2,4%
4.6%
3.2%.
6.1%.
2.7%
4.2%
3.4%
4.5%
4.2%.
7.3%
Other
11,468 141,760
67,550
94,290
36,585
33,323
107.010
11,120
72,280
59,353
10,842
52,820
15,985
Navicula
lo.n
18.2'-,
13.0%
12.4%
16.8%
14.4%
11.5%
4.0%.
15., 5%.
22.0%
8.5%
12.4%
8.9%
Pinnularia
-
1,042
.1%,
-
-
-
-
-
-
-
347
.1%
-
-
-
Staurnncis
-
-
-
-
-
-
-
695
.1%
53,375
-
-
695
.4%
20,155
CiomphnjttTiia
13,553
194,7.37
79,785
69,500
16,675
23,2,59
54,210
10,285
21,545
17,653
76,4.50
11.9%
25.0%
15.5%
9.1%
7.6%
10.. 3%.
5.8%.
3.7%
11.3%
8.0%
13.7%
17.9%
11.2%
Cymbclla
.38,920 159,.584
11.5,925
230,740
73,250
73,250
215,4.50
33,915
90,350
64,218
31,970
102,860
46,565
34.2%
20.5%
22.5%.
30.2%
.33.6%
32.4%
32.2%
12.2%
19.4%
23.7%
24.8%
24.1%,
25.9%
Epithcniia
-
1,042
.1%
-
-
-
-
-
-
-
-
-
-
—
Nitzschia
6,115
1,390
2,780
3,052
6,096
2,362
2,780
1,390
acicularis
—
—
1.2%.
.2%
.7%
1.4%
.7%
3.5%
.6%
—
—
.3%
—
Other
20.880
133,440
85,345
102,960
26,2.50
30,250
337,770
43,590
113,980
56,990
23,908
86,180
34,055
Nilzschia
18.4%
17.1%
16.6%
13. .5%
12.6%
13.. 3%.
36.47n
13.0%
24.5%
21.1%
18.5%.
20.2%
18.9%
Surirella
348
9,172
2,780
4,170
1,390
348
9,730
1,390
4,170
1,390
2,363
2,780
2,085
.3%
1.2%
..5%
.6%
.2%.
.2%,
1.1%
.5%
.9%
.5%
1.8%.
.7%,
1.2%
Other
5,210
4,170
5,560
16,000
_
1,042
—
—
_
_
_
—
—
Pennaies
4.6%
.6%
1.1%.
2.1%
—
.5%
—
—
—
—
—
—
—
Dinobryon
—
—
15,290
1,390
6,255
6,5.50
—
35,305
2,085
—
—
—
—
—
—
3.0%,
.2%
2.9%
2.9%
—
12.7%
.4%
—
—
—
—
Total Algae
116,110 772.963
514,150
763,795
218,145
225,903
926,677
277,937
465,925
270,283
128,866
426,730
180,005
Biol<)(;k:ai. Series, Vol. 18. No. 2 Ai.c.^E of Huntincton C.\nyon, Utah
65
Table 16. Number of organisms per cm- and relative abundance ol periphyton on glas.s slides in a pool at campground
(Site 4)
Algae
5/13
1971
6/8
1971
6/29
1971
7/.30
1971
8/20
1971
9/15
1971
10/8
1971
11/15
1971
Cyclotella
—
—
—
—
—
52
.2%
62
.5%
—
Astcrioncllu
—
—
85
.1%
1,020
.4%
102
.4%
103
.5%
—
—
Ihmnaeu
anus
1,020
2.0*
5,459
2.6%
648
.4%
304
.1%
—
—
206
.6%
Diittomu liUiHulf
z
607
.3%
242
.2%
—
—
Di(tti)m(t tcnuc
—
—
—
—
—
—
—
—
Diut(,inia vuli^are
810
1.6?
1,213
.6%
909
.5%
1,522
.6%
—
206
1.0%
762
6.4%
1,441
3.9%
Frit^ilarid crotunensis
—
—
I
—
—
62
.5%
3,532
9.5%
Mcrkliuii
—
—
—
—
102
.4%
—
—
—
Si/iicdro
2,677
5.2*
7,919
3.7%
85
.1%
.304
.1%
—
154
.7%
762
6.4%
1,544
4.2%
Achuanthc\
2,677
5.2%
27,298
12.8%
123,650
76.0%
196,100
75.3%
3,685
14.9%
,3,398
16.0%
412
3.5%
4,602
12.4%
Cocconeis
243
.5%
—
648
.4%
102
.1%
1,020
4.1%
1,853
8.7%
268
2.3%
31
.1%
Navicula cf.
ciii)it(it<i
102
.2%
2,426
1.2%
—
—
—
—
Navicula cf.
rhyncoccplwla
—
—
85
.1%
890
..3%
304
1.2%
968
4.6%
—
—
Navicula cf.
tripttnctatd
—
—
3,006
1.6%
3,583
1.4%
890
3.6%
1,133
5.. 3%
618
5.2%
1,1.33
3.5%
Other Navintla
21,210
41.0?
20,606
9.7%
4,674
2.9%
10,684
4.1%
3,690
15.0%
2,255
10.6%
2,821
23.8%
4,221
11.4%
Gomphonema
4,633
9.0%
.30,861
14.. 5%
3,583
2.2%
.3,152
1.2%
2,224
9.0%
350
1.6%
1,235
10.4%
1,205
3.2%
Cymhclla
14,9.32
29.0%
70,784
33.3%
19,770
12.0%
29,948
11.5%
2,224
9.0%
2,265
10.6%
2,327
19.7%
9,915
26.6%
Nitz-schiti acicularis
—
—
—
890
..3%
102
.4%
—
—
—
Other Nitz-schia
3,033
5.9%
40,0.32
18.8%
2,887
1.8%
10,600
4.1%
3,920
15.9%
8,2.37
38.7%
2,327
19.7%
7,279
19.6%
Surinlla
152
.3%
607
.3%
85
.1%
I
304
1.2%
52
.2%
62
.5%
103
..3%
Other Fennales
102
.2%
3,642
1.7%
648
.4%
I
—
—
—
31
.1%
Dinohryoii
—
—
—
—
102
.4%
I
—
Oscillataria
—
—
536
..3%
1,190
.5%
406
1.6%
154
.7%
206
.6%
Other Oscillatoriaceae
—
—
—
—
5,644
22.9%
—
62
.5%
1,514
4.1%
Ulolhrix
—
1,213
.6%
—
102
.1%
—
52
.2%
62
.5%
31
.1%
Stificocloniuni
—
—
—
102
—
—
—
31
(Table 16 continued on p. 66)
—
318
—
—
.4%
—
102
318
812
.1%
.4-?
2.2%
324
1,719
1,590
406
,5«
1.9^
2.0*
1.1%
318
—
—
A'i
—
g6 Brigiiam Young University Science Bulletin
— — — .1% — - - .1%
0«/(>gonii/;N — — — — — 52 — —
CAadophora — — 536 — — — — 72
— — .,3% _ _ _ _ .2%
Closterium _ _ _ 204 — — — 31
— - — .1% — — — .1%
Euglena 51 — — — — — — —
Hi/drunis — — 536 — — — — —
— — .3% — — — - -
Total Algae 51,642 212,667 162,613 260,697 24,719 21,284 11,842 37,128
Table 17. Number of organisms per cm- and relative abundance of periphvton on glass slides in a riffle at campground
(Site 4)
Algae 5/13 6/8 6/29 7/30 8/20 2/19 3/11
1971 1971 1971 1971 1971 1972 1972
Cyclotetia
Astcriimclla
Haniuicu
arcus
Diatonid hii'nuilr
Didtinnti triiuc — — —
Diittiiimi inlfiiirc 486 708 636
.7% .8% .8*
Fnigiliiria croloncnsis — — —
Meridion
Si/ncdrii
Achnantltes
Cocconeis
Wivictda cf.
rhyncocc'phala
Navicula cf.
tripunctata
Other Navicula
Gomplwnrmd
C.ymbella
iVi ( r.SY'/i ia acicu la ris
Other \itzschia
Surirt'lla
6,075
—
12.7%
—
103
154
.2%
.9%
3,295
1,287
6.9%
7.9%
204
206
1.54
,2%
.5%
.9%
—
51
—
.3%
—
102
—
—
—
103
—
—
.1%
—
—
—
.2%
-
7,113
4,040
1,272
—
204
7,928
1,493
11.0%
4.. 5%
1.6%
-
.2%
16..5%
9.2%
1,.375
2,928
23,532
20,400
43,200
2,780
1,184
2.1?
3.2%
28.1%
54.6%
43.2%
5.8%
7.3%
81
—
—
3,248
1,624
103
—
.1%
—
—
8.7%
1.6%
.2%
-
—
—
318
204
1,020
—
—
—
—
.4%
.5%
1.0%
-
—
—
1,617
6,678
406
3,040
1,.544
—
—
1.8%
8.0%
1.1%
3.0%
3.5%
-
7,923
5,982
10,.540
2,028
10,276
4,015
1,184
12.1%
6.6%
12.5%
6..5%
10.3%
8.4%
7..3%
15,131
24,015
2,226
2,670
2,670
2,574
1,287
23..3%
26.6%
2.7%
7.1%
2.7%
5.4%
7.9%
24,099
33,963
18,762
3,490
16.510
5,554
5,714
.37.2%
.37.6%
22.4%
9..3%
16. .5%
11.1%
35.0%
—
—
—
406
812
—
—
—
—
—
1.1%
.9%
—
-
8,080
13,820
12,720
1,886
17,503
8,546
3,088
12.5%
15.3%
1,5.2%
5.0%
17.4%
17.8%
18.9%
—
102
—
—
204
(Table
17 continued
103
on p. 67 )
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah 67
—
.1%
—
—
.2%
—
.8%
Other Pennales
81
.5%
943
1.0%
1,908
2.3%
204
.5%
—
2,162
4.5%
I
Dinobryon
—
102
.1%
I
—
—
—
Chroococcales
—
—
I
612
1.6%
—
—
—
Oscillatoria
81
.5%
1,272
1.6%
I
406
.4%
103
.2%
—
Other Oscillatoriaceae
z
—
—
—
2,228
2.2%
103
.2%
—
Ulothrix
81
.5«
—
—
—
I
51
.3,%
Clostcrium
—
—
—
204
.5%
—
—
—
Hy drums
—
20.3
.2%
1,272
1.6%
—
2,986
6.2%
566
3.5%
Total Algae
64,855
90,346
83,680
36,976
99,901
47,980
16,316
68 Bbigham Young University Science Bulletin
Table 18. Number of organisms per liter and relative abundance of net plankton at Tie Fork Pond (Site 5)
Algae
4/15
1971
5/13
1971
6/8
1971
6/29
1971
7/30
1971
8/20
1971
9/15
1971
10/8
1971
Chroococcales
—
—
12.4
1.3?
I
540.0
4.1%
876.0
8..3?
250.0
.8?
288.0
5.0%
Lynghya
—
—
19.0
2.0%
10.5
.4%
36.0
.3%
195.0
1.8%
300.0
.9%
45.0
.8%
Oscillatoria
86.0
15.6*
39.0
9.0?
291.0
30.3?
25.5
.9%
90.0
.7%
2,100.0
20.0%
2,000.0
6..3?
275.0
4.8%
Anabaena
—
.39.0
9.0?
15.5
1.6%
4.5
.2%
45.0
.4%
200.0
.6%
Cidothrix
—
—
—
—
—
—
150.0
.5?
—
Chlamydomona.1
—
—
—
—
330.0
2.5%
186.0
1.7%
2,750.0
8.7%
87.5
1.5%
Pandorina
—
7.7
1.8%
—
—
246.0
1.9%
276.0
2.5%
400.0
1.3?
70.0
1.5%
Other Volvocaceae
—
—
—
—
—
—
—
37.5
.7%
Gloeocystis
—
—
—
—
—
—
—
38.0
.7%
Oedogonium
—
85.0
19.6%
127.0
13.2?
—
156.0
1.2%
780.0
7.4?
250.0
.8?
137.5
2.4%
Cladofihora
—
—
7.7
.8%
10.5
.4?
81.0
.6?
22.5
.2%
700.0
2.2%
200.0
3.5%
Ankistrodesmus
I
46.7
10.8%
I
—
—
—
Mougeotia
93.0
16.9?
—
193.0
20.1%
1,335.0
45.3*
11,250.0
86.4?
4,710.0
44.8?
15,555.0
49.0?
4,275.0
73.8%
Spirogyra
46.5
8.5?
7.7
1.8?
147.0
15.3%
1,345.5
45.7%
66.0
.5?
255.0
2.4%
6,750.0
21. .3%
100.0
1.7%
Zygnema
I
.39.0
9.0%
43.5
4.5%
120.0
4.1%
30.0
.2%
705.0
6.7%
450.0
1.4%
—
Other Filamentous
Chlorophyta
Closterium
185.0
33.6%
69.5
16.0?
7.7
1.8?
61.5
6.4%
23.0
2.4?
100.5
3.4%
120.0
.9%
7.5
.1%
37.5
.3%
50.0
.2%
12.5
.2%
Euglena
1.39.5
25.4?
85.0
19.6%
7.7
.8%
4.5
.2?
45.0
.3%
315.0
2.9%
1,850.0
5.8%
187.5
3.2%
Pyrrophyta
—
I
I
I
30.0
.2%
7.5
.1%
I
12.5
.2%
Ophiocytium
—
7.7
1.8%
—
I
—
—
I
25.0
.4?
Vaucheria
—
—
12.4
1.3?
—
—
—
—
—
Total Algae
550.0
434.0
960.7
2,946.0
13,020.0
10,518.0
31,655.0
5,791.0
Bi()L()C:k:ai, Sehies, \'oi.. 18. No. 2 .^i.fi.vE of IIuntincton Canyon, Utah 69
Table 19. Number of organisms per liter and relative abundance of nannoplankton at Tie Fork Pond (Site 5)
Algae
4/15
5/13
6/8
6/29
7/30
8/20
9/15
10/8
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1972
Cyclotella
—
—
7,645
3.8%
—
—
—
—
—
—
Astcrioiiclla
_
_
2,780
2,088
5,004
—
—
1.3%
1.3%
.6%
—
—
—
—
Didtomd
—
3,476
9,035
1,042
12,525
348
2,780
348
1,043
—
1.3%
4.3%
.7%
1.5%
.2%
.7%
.2%
16.7%
Fraiiiluriu
—
—
7,228
40,310
23,775
4,875
2,780
2,363
—
crotoiiciisi.s
—
—
3.5%
25.5%
2.8%
2.4%
.7%
1.5%
—
Fni'^ihiriti
5,143
—
1,390
4,448
85,950
4,444
9,730
6,533
—
viresccus
6.2%
—
.7%
2.8%
10.5%
2.3%
2.5%
4.1%
—
Meridicit
—
4,170
1.6%
—
—
—
—
—
—
—
Si/ui'itra
4,448
16,680
26,828
6.255
13,.350
348
5,560
5,8.38
1,043
5.4%
6.4%
12.9%
4.0%
1.6%
.2%
1.4%
3.7%
16.7%
Achiiantlics
5,143
7,.505
17,.375
2,088
4,170
1,042
4,170
1,390
—
6.2«
2.9%
8.3%
1.3%
.5%
.5%
1.1%
.9%
—
Cocconcis
13,733
1,589
—
—
1,042
4,875
1,.390
348
—
16.6%
.6%
-
—
.1%
2.5%
.4%
.2%
—
Aniphipli-urti
—
—
3,475
1,390
—
—
2,085
348
—
—
—
1.7%
.8%
—
—
.5%
.2%
—
CyrosijJitui
—
696
—
348
—
—
1,390
1,043
1,043
—
.3%
—
.2%
—
—
.4%
.7%
16.7%
Navicula
19,734
34,611
9.175
6,185
19,852
4,170
9,035
12,510
2,085
23.8%
13.0%
4.4%
3.9%
2.4%
2.1%
2.3%
7.9%
33.4%
PinnuUirid
2,084
—
695
1,042
2,084
348
695
3,475
—
2.5%
—
.3%
.7%
.2%
.2%
.2%
2.2%
—
Sttmroiieis
2,084
1,589
—
1,390
3,127
348
695
1,043
—
2.5%
.6%
—
.8%
.4%
.2%
.2%
.2%
.7%
GoinpliDnema
348
69,500
1,042
2.432
7,086
—
1,390
3,085
—
.4%
26.1%
.5%
1.5%
.8%
—
.4%
2.0%
—
Ci/inhelt<i
2,084
67,275
3,058
4,686
5,004
1,042
2,362
4,865
—
2.5%
25.2%
1.5%
3.0%
.6%
.5%
.6%
3.1%
—
Epitliemid
1,390
696
696
5,837
159,750
37,585
82,010
7,228
—
1.7%
..3%
.3%
3.7%
19.. 5%
19.2%
20.7%
4.6%
—
Sitzachid dciculdris
4,868
—
13,900
696
2,084
—
8,895
2,780
—
5.9%
—
6.7%
.4%
.3%
—
2.2%
1.8%
—
Other Mtz-schia
12,507
45,035
39,968
25,397
85,950
6,550
36,695
24,603
1,043
15.2%
16.9%
19.1%
16.0%
10.5%
3.4%
9.3%
15.6%
16.7%
Surircllu
—
3,335
—
348
1,042
—
—
348
—
—
1.3%
—
.2%
.1%
—
—
.2%
—
Other Pennales
—
10,.575
696
696
—
—
—
—
—
—
4.1%
.3%
,4%
—
—
-
—
—
Chrooeoeeales
—
—
2,710
41,282
91,160
—
22,795
—
—
—
—
1..3%
26.1%
11.1%
-
5.7%
—
—
Aiidbucna
—
—
695
—
8,340
1,042
—
—
—
—
—
.3%
—
1.0%
.5%
—
—
—
Aiikislrodcsmus
—
—
2,362
—
—
5,140
6,950
—
—
—
—
1.1%
—
—
2.6%
1.8%
—
—
ClofilcriDpsis
20,475
—
—
—
—
—
—
—
—
10.5%
—
-
—
S'cplirocijtium
—
84,000
11,120
34,750
695
—
10.2%
5.7%
8.8%
.4%
—
(Table 19 continued on p. 70)
70
Scenedesmus
1,390
1.7%
Cosmarium
1,042
1.3«
Closterium rostrata
—
Euustnim
—
Spluierozosma
—
Stuurii.stnun
—
Other desmids
—
Fhacus
—
Truchc'lomonas
6,533
i.m
Vcruiininm
—
DiiKthryon
—
Total Algat-
82,513
Bricham Young Univehsiti' Science Bulletin
266,732
—
2,362
113,125
23,620
29,745
11,398
—
—
1.5«
13.8«
12.1*
7.5*
7.2%
—
—
2,780
9,225
5,987
2,085
1,043
—
—
\.m
lA'i
3.1!f
..5*
.7?
—
—
—
—
1,390
.6%
—
—
—
348
16,725
I
.2%
—
2.0?
—
—
—
—
—
—
57,075
49,.5O0
101,470
5,838
—
—
—
6.8%
25.4'l
25.6*
3.7*
—
—
5,560
4,170
1,390
—
348
—
—
3.5%
.5*
.7?
—
.2%
—
—
—
—
4,444
—
3,475
—
—
—
—
2.3*
—
2.2*
—
—
—
—
-
2,780
.7*
-
—
6,533
5,004
5,175
23,6.30
41,978
3.1%
—
m
2.7*
6.0*
26.7*
—
—
—
—
—
—
14,873
—
—
—
—
—
—
9.4*
—
50,735
—
—
—
695
—
—
24.3?
-
-
—
.2*
—
—
108,369
158,562
820,619
195,258
396,562
157,793
6,257
Biological Series, Vol. 18, No. 2 Al(;.\e of Huntington Canyon, Ut.vii
71
Table 20. Number ot organisms per cm^ and relative abundance of periphyton on glass slides at Tie Fork Poud
(Site 5)
Algae
5/13
1971
6/8
1971
6/29
1971
7/30
1971
8/20
1971
9/15
1971
10/8
1971
11/15
1971
Cyclotella
—
51
.2%
I
I
612
1.0%
52
.1%
—
I
A\tcriitncUii
—
1,964
6.1%
—
—
I
I
—
—
Didtdinii Icriue
—
363
1.1%
—
—
—
15,8.56
36.0%
412
l.,5%
793
20.8%
Other Diatoina
—
—
102
.6%
I
102
.2%
—
—
—
Franilaria crotnncnses
—
707
2.3%
699
3.8%
151
.8%
—
103
.2%
—
206
5.4%
Fragilaria virescens
2,420
3.7%
607
1.8%
204
1.1%
6.56
3.4%
1,280
2.2%
9,267
21.1%
1,380
5.0%
165
4.3%
Meridian
—
—
—
—
—
—
—
26
.7%
Syticdra
4,213
6.4%
4,751
14.9%
1,319
7.1%
254
1.3%
406
.7%
865
2.0%
3,098
11.2%
124
3.. 3%
Hannaea amis
—
—
I
I
z
52
.1%
—
Achnimthes
2,992
4.5%
6,308
19.7%
1,624
8.7%
51
..3%
304
.5%
247
.6%
62
.2%
206
5.4%
Cocconeis
242
.4%
—
102
.6%
850
4.4%
612
1.0%
206
.5%
62
.2%
—
Rhoicosphcnia
—
—
—
—
I
103
.2%
Aniphiplfurct
—
.505
1.6%
102
.6%
—
I
—
144
.5%
—
Gyrosigma
1,133
1.7%
51
.2%
—
—
—
247
.6%
474
1.7%
—
Navicula cf. tripunctata
—
1,108
3.5%
608
3.3%
243
1.3%
102
.2%
1,2.36
2.8%
144
.5%
51
1..3%
Other Navicula
27,652
41.9%
3,375
10.6%
1.330
7.0%
451
2.3%
597
1.1%
103
.2%
2,059
7.5%
258
6.8%
Pinnularia
3,420
5.2%
243
.7%
—
102
.5%
204
.4%
247
.6%
350
1..3%
—
Stauroneis
—
—
102
.6%
—
102
.2%
3.50
.8%
144
.5%
—
Comphoncma
324
.5%
445
1.4%
204
1.1%
406
2.1%
486
.8%
1,544
3.5%
268
1.0%
51
1..3%
Cymhella
972
1.5%
1,108
3..5%
1,105
6.0%
306
1.6%
—
556
l.,3%
762
2.8%
165
4.3%
Epitlwmia
890
1..3%
607
1.9%
486
2.6%
1,224
6.. 3%
3,220
5.6%
206
.5%
1,442
5.2%
26
.7%
Sitzschia
6,308
9.6%
4,893
15.. 3%
1,976
10.6%
1,.581
8.1?
3,248
5.6%
6,837
15..3%
12,293
44.5%
1,416
.37.1%
Surirella
161
.2?
—
—
I
—
52
.1%
.556
2.0%
—
Ophiocytium
242
.4%
—
.304
1.7%
—
—
—
—
Diniihrijon
—
2,730
8..5%
204
1.1%
z
—
62
.2%
—
Chroococcales
242
A'i
102
.3%
1,.376
7.4%
2,011
10.. 3%
7,745
1.3.4%
247
.6%
762
2.8%
—
Lyngbya
—
—
243
1.3%
5,4.50
0.4%
(Table
62 -
.2% -
20 continued on p. 72)
72 BmcHAM Young University Science Bulletin
Oscillatoria
Other Oscillatoriaceae
Anabaena
Calothrix
Chlamydomonas
Pandorina
Other Volvocaceae
Oedogonium
Cladophora
Rhizoclonium
Characium
Pediastrum
Ankistrodesmus
Nephrocytium
Scenedesmus
Mougeotia
Spirogyra
Zygnema
Other Fihimentous
Chlorophyta
Closterium
Cosmarium
Micrasterias
Pleurotaenium
Sphaerozosma
Staurustrtim
Euglena
Phacus
Trachelomonas
Total Algae 66,011 31,953 18,573 19,458 57,778 43,961 27,601 3,816
9,300
—
204
102
—
515
272
—
14.1%
—
1.1%
.5%
—
1.2%
1.0%
—
—
—
—
—
102
52
—
—
—
—
—
—
.2%
.1%
—
—
—
505
204
1,020
304
52
474
—
—
1.6%
1.1%
5.2%
.5%
406
.1%
1.7%
—
—
102
510
.8%
1,624
313
—
—
—
.3%
—
2.6%
2.8%
.7%
—
—
—
—
—
1,.326
486
—
—
26
—
—
—
6.8%
.8%
—
—
.7%
81
—
—
204
—
—
—
.1%
—
—
1.0%
—
—
—
—
648
363
2,960
—
1,280
154
247
226
1.0%
1.1%
15.9%
—
2.2%
.4%
.9%
6.1%
—
—
102
—
—
412
—
51
—
—
.6%
204
—
—
.9%
—
1.3%
242
—
1.1%
408
812
—
—
—
—
.4%
—
2.2%
4.2%
—
—
—
—
—
—
102
.306
—
—
—
—
—
—
1.1%
1.6%
—
—
—
—
—
152
304
—
—
—
206
—
—
.5%
1.7%
—
—
—
.7%
—
—
—
—
969
1,624
—
—
26
—
—
—
5.0%
2.8%
—
—
.7%
648
—
102
2,428
15,600
154
206
—
1.0?
—
.6%
12.4%
27.0%
.4%
.8%
—
—
505
—
1,323
972
247
618
—
—
1.6%
—
6.8%
1.7%
.6%
2.2%
—
—
—
304
102
204
103
268
—
—
—
1.7%
304
.5%
.4%
.2%
1.0%
—
1,698
—
1.7%
1,020
153
—
247
—
—
2.6%
—
5.5%
.8%
—
.6%
—
—
161
—
102
51
—
—
62
—
.2%
—
1.1%
..3%
—
—
.2%
—
161
102
—
1,267
306
52
—
—
.2%
.3%
51
.2%
—
6.5%
..5%
.1%
—
—
—
—
—
—
3,040
52
62
.2%
144
—
—
—
—
—
5.3%
.1%
.5%
—
81
203
102
—
—
—
—
.1%
.6%
.6%
—
—
—
—
890
51
—
204
3,730
2,470
247
1..3%
.2%
—
1.0%
6.5%
5.5%
.9%
—
—
304
152
1,210
515
62
—
—
1.7%
.8%
2.1%
1.2%
.2%
890
—
—
—
2,420
247
206
1.3%
—
—
—
4.2%
.6%
.8%
66,011
31,953
18,573
19,458
57,778
43,961
27,601
Biological Series, Vol. 18. No. 2 Algae of Huntington Canyon, Utah 73
Table 21. Number of organisms per liter and relative abundance of net plankton at Stuart Station (Site 6)
.^lga<.
4/15
5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
Chroococcales
-
-
-
-
-
-
-
1.8
4.3%
-
-
-
-
-
Os<^ll<itoria
69,5
93.0
46.5
11.2
3.8
7.5
1.2
3.7
16.2
13.0
3.1
23.0
45.0
34.7%
32.9%
9.77o
9.1%.
1.8%
7.1%
3.9%
8.9%
21.0%,
25.07-,
9.8%
14.. 3%
15.9%
Other Oscilla-
23.0
—
—
—
11.2
.3.8
8.7
14.2
55.3
19.8
4.1
2.3
6.3
tonaccae
11.5%
-
—
—
.5.. 5%
3.6%
28.1%
34.0%
71.8%,
38.2%
13.0%
1.4%
2.2%
AnabaiTia
—
—
—
3.8
—
—
1.2
—
—
—
.5
—
—
—
—
—
3.0%
—
—
3.9%
—
—
—
1.6%
—
—
Chlamydomonas
—
—
3.9
—
3.8
—
—
.6
—
—
—
—
—
—
.8%
—
1.8%
—
—
1.4%
—
—
—
—
—
Pandorina
—
—
—
—
7.5
_
—
.6
_
_
—
—
—
moruin
—
—
—
—
3.7%
—
—
1.4%
—
—
—
—
—
Sephrocytium
_
_
_
—
—
—
—
.6
—
—
_
_
_
—
—
—
—
—
—
—
1.4%
—
—
—
—
—
Ulothrix
—
15.5
31.0
.3.8
—
—
—
—
—
_
1.3
—
—
5.4%
6.5%
3.0%
—
—
—
—
—
—
—
.8%
—
Stigeoclonium
—
—
—
—
—
7.7
—
.6
1.2
1.3
.5
—
—
—
—
—
—
—
7.3%
—
1.4%
1.6%
2.5%,
1.6^,
—
—
Oedogonium
—
_
23.0
7.5
.3.8
—
3.7
3.0
.6
—
—
1.7
1.3
—
—
4.8%
6.1%
1.8%
—
11.9%
7.2%
.8%
—
—
1.1%
.4%
Cladophora
—
7.7
—
—
—
11.2
—
3.5
2.5
5.1
.5
.6
—
—
2.7%
—
—
—
10.7",
—
8.4%
3.2%
9.8%,
1.6%
.4%
—
Mougeotia
—
—
—
3.8
127.0
3.8
8.7
3.7
—
—
—
—
_
—
—
—
3.0%,
61.7%
3.6%
28.1%
8.9%
—
—
—
—
—
Sinrogyra
_
_
3.9
—
7.5
15.0
.3.7
1.1
.6
.6
_
.6
_
—
—
.8%
—
3.7%,
14.3%
11,9%
2.6%
.8%
1.2%
—
.4%
—
Zygnema
—
—
_
—
3.8
.30.0
—
1.1
—
—
1.0
—
1.3
—
—
—
—
1.8%
28.6%
—
2.6%
—
—
3.2%
—
.4%
Clostcrium
—
—
3.9
3.8
37.8
22.5
—
2.5
.6
—
—
—
—
—
—
.8%
3.0%
18.4%
21.4%
—
6.0%
.8%
—
—
—
—
Cosniarium
—
—
—
—
—
—
1.2
3.9%
—
—
—
—
—
—
Euglena
.3.8
1.2
_
—
—
—
—
—
3.6%
—
2.9%
—
—
—
—
—
Ccratium
—
—
—
—
—
—
2.5
.6
—
—
—
—
hirundincUa
—
—
—
—
—
—
8.1%
1.4%,
—
—
—
—
—
HydrUTUs
108.0
170.0
368.0
90.0
—
—
—
—
—
12.1
21.9
131.0
229.0
foctidus
53.9%
59.4%
76.6%
72.8%
—
—
—
—
—
23.3%,
69.3%
81.5%
81.0%
Vaucheria
-
-
-
-
-
-
-
3.0
7.2%
41.8
-
-
-
-
-
Total Algae
200.5
286.2
480.6
123.9
206.2
10.5.3
.30.9
77.0
51.9
31.6
160.5
282.9
74
Bricham Young University Science Bulletin
Table 22. Number of organisms per liter and relative abundance of nannoplankton at Stuart Station (Site 6)
Algae
4/15
1971
5/13
1971
6/8
1971
6/29
1971
7/30
1971
8/20
1971
9/15
1971
10/8
1971
11/15
1971
12/17
1971
1/20
1972
2/19
1972
3/11
1972
Cyclotella
-
-
-
-
-
-
-
-
-
347
.1%
348
.1%
—
z
Hannat-a arcus
-
696
.7%
-
348
.1%
348
.1%
—
I
z
I
695
.2%
348
.1%
—
Piatffma
1,390
.4%
—
2,085
.7%
1,042
.4%
—
I
—
—
—
—
—
1,390
.4%
—
Diatonta
vul^arc
2,780
.8%
348
.3%
3,048
1.0%
4,338
1.5%
3,480
1.3%
1,000
.9%
3,752
1.2%
7,645
11.5%
22,935
8.1%
.30,858
9.27o
9,7.30
3.4%
4,170
1.3%
2,085
1.6%
Fragilaria
—
1,390
1.4%
695
.2%
I
348
.1%
—
277
.4%
—
—
—
Meridion
—
—
.5,7.55
1.9%
—
—
500
.4%,
I
—
—
—
—
—
Syncdra
20,8.50
6.2%
41.700
41.7%
3,048
1.0%
7,922
2.7%
1,044
.4%
500
.4%
12.092
3.9%
11,538
17.4%
30,587
10.8%.
35,445
10.6%
2.5,715
9.1%
23,6.30
7.2%
13,205
9.9%
Achnanthes
10,286
:3.17r
4,170
4.2%
11,125
3.6%
9,312
3.2'5
14,875
.5. .5%
9,000
7.7%.
13,482
4.3%.
972
1.5%
12,510
4.4%
21,128
6., 3%
16,680
5.9%
24,325
7.4%
5,560
4.2%
VocconeiH
696
.2%
—
—
696
.2%
12,800
4.7%.
1.200
1.0%
7,922
2.6%
389
.6%
4.865
1.7'r,
2,085
.6%
3,057
1.1%
4,170
1..3%
1,390
1.0%
Hhoicosphenia
—
—
—
—
348
.1%
—
—
I
696
.2%
I
I
—
—
Amphipleura
-
348
.3%
-
-
-
-
-
-
-
-
348
.1%
—
—
Gyrosigma
6,115
1.8%
348
.3%
-
-
1,044
.4%
-
-
-
-
695
.2%
695
.2%
695
.5%
Savicula cf.
capitate
—
—
—
1.042
.4%
3,480
1.3%
4,500
3.8%,
14,456
4.7%
2,362
3.6%
9,035
3.2%
7,923
2.4%
15.290
5.4%
14,595
4.5%
3,475
2.6%
Navicula cf.
rhyncocephala
—
—
—
348
I
2,610
2.2%
14,177
4.6%
972
1..5%
4,445
1.6'-,
—
—
—
—
Navicula cf.
tripunctata
12,510
3.7%
—
10,008
3.2%
9,312
3.2%
12,800
4.7%
10.332
8.8%.
19,460
6..3%
4,865
7..3%
14,177
.5.0%
15,290
4.6%
12.075
4.3%
1.3,900
4.3%
8,340
6.3%
Other
Navicula
155,682
46.2%
25,020
25.0%
40,656
13.1%
24.115
8.4%
37,555
13.8%
21,888
18.8%
42,395
13.6%
3,752
6.6%
24,602
8.77r
49,345
14.8%
47.538
16.9%
37,530
11.3%
12,510
9.3%
Pinnularia
-
1,042
1.1*^.
-
-
-
-
-
-
-
-
—
—
—
StauToncis
-
-
-
-
250
.2%
348
.1%
-
-
-
-
-
-
Gomphonema
31,135
9.2%
696
.T7.
131,633
42..5%
19,460
6.8%
15.425
5.7'7r
8.694
7.4%
28,495
9.2%
3,752
5.6%.
34.375
12.2%
46.148
13.8%
39.615
14.1%
33,350
10.2%
21,545
16.1%
Cytnhella
7,505
2.2%
3,057
3.1%
60,743
19.6%
189,040
65.6%
100,075
36.8%
23,760
20.3%
28,772
9.3%,
10,702
16.1%
61.437
21.7%
66,720
20.0%
59.770
21.2%
115,370
35.2%
43,090
32.3%
Epithemia
-
-
-
—
—
—
348
.1%
—
—
—
—
—
—
Nitzxchia
acicularis
-
-
-
1,042
.4%
4.5,.500
16.7%
1,697
1.5%
8,310
2.7%
3,197
4.8%
2,362
.8%
-
-
-
-
Other
Nitzschia
47,815
14.2%
20,850
20.8%.
35.723
11.. 5%
15,985
5.5%,
21,525
8.0%
28,620
24.4%
111,120
35.8%
14,456
21.8%
52,820
18.7%
52,820
15.8%
47,955
17.0%
47,955
14.7%
19,460
14.6%
Surirella
37,530
11.1%
—
3.753
1.2%
—
—
1,200
1.0%
5.142
1.7%
696
1.0%
7,922
2.8%
4,448
1.3%,
3.057
1.1%
2,085
.6%
2,085
1.6%
Other
Fennales
—
—
1,668
.5%
4,450
1.5%,
348
.1%
I
I
I
—
—
—
4,170
1.3%
Oinohrypn
—
348
.3%
I
348
.1%
348
.1%
250
.2%
—
—
—
—
Anabaena
2,780
.8%
-
-
—
-
-
-
—
—
—
—
—
—
Trachelomonas
-
-
-
-
-
-
277
.4%
65,852
-
-
-
-
-
Total Algae
337,074 100,013
309,940
288,800
271,343
116,001
310,271
282,768
333,947
281.526
327,335
133,440
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah 75
Table 2.3. Number of organisms per cm^ and relative abundance of periphyton on glass slides at Stuart Station
(Site 6)
Algae
5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
Cyclotclla
—
—
—
—
—
52
—
—
-
-
—
—
—
—
—
.\%
—
—
—
—
Hannaea arcus
—
51
—
—
—
—
—
—
—
—
—
.1%
—
—
—
—
—
—
—
—
Diatmna
5,459
705
19,000
204
203
103
3,357
20,593
16,062
1,338
1.7%
1.7%
9.4%
.4%
.3%
.2%
5.2%
6.8%:
7.27.
4.07o
Fragilaria
_
_
—
—
—
52
—
—
1,082
—
crotoncnscs
—
—
—
—
—
.1%
—
—
.57o
—
\tendion
—
404
204
_
—
—
—
—
—
—
—
1.0%
.170
—
—
—
—
—
—
—
Synedra
27,901
825
11,980
—
51
412
5.704
18,945
23,630
1,647
8.7<!!-
2.0%
6.1%
—
.1%
.8%
8.9%,
6.2%.
10.6%
4.9%
Achnanthes
6,066
1,928
16,500
29,500
.37,290
32,989
5,148
125,615
25,947
4.221
1.9%
4.7%,
8.1%
60.9%
5.3.1%
61.2%
8.07o
41.37,
11.6%
12.. 57,
Cocconeis
241
—
102
2.7.50
7,900
3,851
762
1,853
1,082
—
.1%
—
.1%
.5.7%
11.2%.
7.1%
1.27,
.6%
.5%
—
Savictila cf.
—
—
—
204
—
824
4,119
1,082
206
capitata
—
—
—
—
..3%
—
l.,3%
1.47,
.57.
.67c
Savicuta cf.
—
—
_
204
—
1,133
—
—
—
—
rhyiicocfphala
—
—
—
.2%
—
2.1%
—
—
—
—
\at'icula cf.
—
1,320
1,115
1,380
3,.501
4,5.30
2,471
309
tripunctata
—
—
—
2.7%
1.67,.
2.6%
5.5%.
1.5%,
1.17,
.97c
Other Naticula
42,410
7,122
18,604
7,950
4,304
.3,274
11,594
28,006
22,085
3,295
13.2'-,
17.. 5%
9.2%
16.4%
5.9%
6.0%,
18.07,
7.8%
9.97,
9.7%
Gomphortcma
129,764
13,647
12.680
486
742
1,894
8,442
.3.5,213
46,488
1,493
40.2%.
33.5%
6.3%
1.0%,
1.1%
3.5%,
13.27o
11.6%
20.97,
4.47c
Cymbetla
77,153
8,694
111,200
3,590
1,601
1,071
5,004
28,624
60,697
13,436
23.9%
21.3%
54.8%
7.47o
2.37,,
2.0%
7.8%
9.47o
27.3%,
40.0%,
Nitzschia
—
—
—
304
1,218
206
1,235
—
—
—
acicularis
—
—
—
.6%
1.7-;;
.4%
1.9%
—
—
—
Other \itzschia
21,593
6,924
7,600
1,320
.5,274
7,195
17,154
32,372
12,047
3,552
6.7%
17.0%
3.7%
2.7%
7.5%
13.37r
26.87c
10.67f
5.4%
10.57o
Surirella
1,213
202
1,518
102
153
154
679
2,0.59
1,699
257
.4%
.5%
.7%
.2%.
.27»
.37o
1.1%
.77,
.87o
.87,
Other Pennales
51
2,550
102
102
52
144
—
—
—
—
.1%
1.2%
.2%
.27o
.1%
.27,,
—
—
—
Chroococcales
2,729
—
—
—
406
—
—
—
—
—
.8%
—
—
—
.6%
—
—
—
—
—
Oscitlatoria
1,213
—
_
406
509
103
350
2,059
1,082
154
.4%
—
—
.8%
.7%
.2%
.6%
.7%
.5%
..5%
Other
—
_
—
—
9,188
—
144
—
—
—
Oscillatoriaceae
—
—
—
—
13.1%
—
.27,
—
—
—
Utolhrix
972
—
406
102
_
—
—
—
1.54
—
.3%
—
.2%
.2%
—
—
—
—
.1%
—
Closterium
—
_
204
102
102
—
62
—
—
—
—
—
.1%
.2%
.2%
—
.17o
—
—
—
Euglena
241
.1%
5,459
-
-
-
—
—
—
—
—
—
Hy drums
202
406
I
7,722
3,964
1.7%
.5%
.2%.
—
—
—
—
—
3.. 5%
11.77o
Total Algae
322,414
40,755
202,954
48,442
70,362
53,921
64,105
303,988
223,3.30
33,872
76 Bricham Young University Science Bulletin
Table 24. Number of organisms per liter and relative abundance of net plankton at Bear Canyon (Site 7)
Algae
6/29
7/30
8/20
9/15
10/8
11/15
1971
1971
1971
1071
1971
1971
Chroococcales
—
—
3.7
—
—
—
—
—
6.6%
—
—
Oscillatoria
15.0
.30.0
3.0
10.0
6.2
28.7
3.3%
14.4%
3.9%
17.9%
20.9%
25.6%
Other Oscillatoriaceae
4.5
22.5
—
8.7
1.2
35.0
1.0%
10.8%
—
15.5%
4.1%
31.2%
Rivularia
15.0
—
—
—
—
—
3.3%
—
—
-
—
—
Chlamydomoruis
—
25.5
12.2%
—
2.5
4.5%
—
—
Pandorina morum
—
—
-
1.2
—
—
—
—
—
2.1%
—
—
Scenedesmus
—
1.2
—
—
—
—
—
2.1%
—
—
Ulothrix
90.0
11.2
3.0
—
—
5.0
19.9%
5.4%
3.9%
—
—
4.5%
Cylindrocapsa
—
I
10.5
13.7%
—
Stigeoclonium
—
—
z
I
—
1.7
1.5%
Oedogoixium
4.5
18.0
4.5
10.0
15.5
37.5
1.0%
8.6%
5.9%
17.9%
52.4%
33.4%
Cladophora
I
15.0
7.2%
7.5
9.8%
10.0
17.9%
.6
.5%
Mougeotia
4.5
1.0%
7.5
3.6%
—
2.5
4.5%
—
Spirogyra
—
—
I
5.0
8.9%
—
—
Zygnema
—
3.8
3.0
—
3.7
1.2
—
1.8%
3.9%
—
12.5%
1.1%
Closterium
4.5
67.5
42.0
1.2
.6
2.5
1.0%
.32.4%
54.9%
2.1%
2.1%
2.2%
Pleurotaeriium
—
—
—
—
.6
—
—
—
—
—
2.1%
—
Euglena
—
—
3.0
3.9%
—
.6
2.1%
—
Other Euglenophyta
—
—
I
—
1.2
4.1%
—
Hydmrus foetidus
31.5.0
69.5%
7.5
3.6%
—
—
I
Total Algae
453.0
208.5
76.5
56.0
29.6
112.2
Biological Series, Vol. 18, No. 2 Alcae of Huntington Canyon, Utah
77
Table 25. Number of organisms per liter and relative abundance of nannoplankton at Bear Canyon (Site 7)
Algae
8/20
1971
9/15
1971
10/8
1971
11/15
1971
Diatoma vulgare
Meridian
Synedra
Achnanthes
Coccimeis
Rhoicosjihenia
Naviculci cf
capituta
Navicula cf
rhyncoceplwla
Navicula cf
tripunctata
Other Navicula
Stauroueis
Gomphonema
Cymbt'lla
Epithemia
Nitzschia
acicidaris
Other Nitzschia
Surircllu
Trachclomonax
Total Algae
1,390
2,085
554
1,390
.6%
1.0%
.5%
.5%
348
—
—
2,085
.2%
—
—
.8%
1,042
4,170
3,890
12,787
.5%
1.9%
3.5%
4.8%
20,125
21,127
23,907
19,460
9.3*
9.7%
21.3%
7.3%
13,200
5,142
3,335
6,245
6.1%
2.4%
3.0%
2.3%
696
—
554
—
.3%
—
.5%
—
—
1,390
—
348
—
.6%
—
.1%
5,150
4,445
2,500
6,950
2.4%
2.0%
2.2%
2.6%
20,475
12,510
5,837
7,500
9.5%
5.7%
5.5%
2.8%
39,125
29,190
13,065
37,807
18.1%
13.4%
11.4%
14.2%
696
—
—
—
.3%
—
—
—
12,075
25,020
4,725
23,630
5.6%
11.5%
4.2%
8.8%
69,250
45,452
33,637
78,535
32.1%
20.8%
30.0%
29.4%
348
—
—
—
.2%
—
—
—
1,668
4,170
—
3,475
.8%
1.9%
—
1.3%
28,250
57,267
19,460
59,770
1.3.1%
26.3%
17.3%
22.4%
1,042
1,390
831
2,711
.5%
.6%
.7%
1.0%
696
4,865
—
4,448
.3%
2.2%
—
1.7%
215,576
218,223
112,295
267,141
78 Bhigham Younc Univfj\sity Science Bulletin
Table 26. Frf(|iicn(.v, percent cover, and pcrcenl composition of the visiljlc hcnlhu ilora at 6 localities in llinitington
Creek, June 1971 -March 1972
6/8
6/29
7/30
8/20
9/15
10/8
11/15
2/19
.3/11
1971
1971
1971
1971
1971
1971
1971
1972
1972
Lawrence
Total Frecjiiency
91
100
100
100
100
100
98
95
—
Total C'over
51
81
65.7
89.1
60.6
H6.9
73.8
17.7
—
Cladoplwra
Frequency
91
77
37
33
20
15
24
5
—
Cover
34
43
4.3
6.6
1.6
4,5
3.6
.13
—
Composition
67
53
6.0
8.0
2.6
5.0
4.8
1
—
Ot'(/()g(HliIiH^
Frequency
68
100
—
—
—
—
—
—
Cover
17
38
—
—
—
—
—
—
—
Composition
33
47
—
—
—
—
—
—
—
Chiira
Frequency
—
—
70
50
82
85
88
90
—
Cover
—
—
37.4
38.3
48.0
63.6
61.0
15.5
—
Composition
—
—
57
43
79.3
73
82.6
87
—
Protodcniui
Frequency
—
—
—
28
12
—
—
—
—
Cover
—
—
—
2.2
1.8
—
—
—
—
Composition
—
—
—
2.0
3.0
—
—
-
-
r<)f()»i()<;<(()ii
Fretpiency
—
—
70
57
49
40
41
34
—
Cover
—
—
24
42
9.2
18.8
9.2
2.1
—
Composition
—
—
37
47
15.1
22
12.5
12
—
Highway 10
Total Frecjuency
100
81
100
100
100
93
94
73
—
Total Cover
25
57
1.5.6
18.9
22.7
26.6
29.3
11
—
Cladophora
Frecpiency
100
81
97
59
25
48
61
20
—
Cover
25
57
13.4
2.5
1.4
2.5
5,8
,5
—
Composition
100
100
86
13.0
6.0
9.0
19.9
5
—
Clidra
Fretjuency
—
—
21
49
46
71
51
64
—
Cover
—
—
2.2
16.4
20.5
24.1
22.8
10,5
—
Composition
—
—
14.0
87
90.0
91.0
77.8
95
—
Polomogeton sp.
_
Frequency
—
—
—
—
11
—
14
—
—
Cover
—
—
—
—
.8
—
.7
—
—
Composition
—
—
—
—
4.0
—
2.4
—
—
Plant Site
Total Frtxpiency
—
—
—
—
—
—
—
89
10
Total ("over
—
—
—
—
—
—
—
24
1
I ly drums
Frecjuency
—
—
—
—
—
—
—
89
10
Cover
—
—
—
—
—
—
—
24
1
Composition
—
—
—
—
—
—
—
100
100
C^ampground
Total Fretpiency
75
—
—
77
—
—
—
.30
—
Total Clover
25
—
—
6.4
—
—
—
1,5
—
Oscillutoria
Fre<piency
—
—
—
77
—
—
—
—
—
Cover
—
—
—
6.)
—
—
—
—
—
Composition
—
—
-
1(H)
—
—
/ T" i_i _ r»/
—
.1 '70\
(Table 26 contiinied
HioLociKVM. Skiues, \'ou. 18, No. 2 Ai.cAE or Huntincton Canyon, Utah
79
llijdnirus
Frequency
Cover
75
25
—
Composition
100
—
Stuart Station
Total Friijut-ncy
100
22
Totiil Cover
30
.55
Hi/dnirtts
Fr«iuency
Cover
100
30
18
.45
Composition
100
82.0
Cladophora
Frequency
Cover
—
4
.1
Composition
—
18.0
Oscillutoria
Freijuency
—
—
Cover
—
—
Composition
—
—
Bear Canyon
Total Frefjuency
—
—
Total Cover
—
—
Oedogouiiim
Frequency
Cover
I
I
Composition
—
—
Hydrurus
Frixjuency
Cover
—
—
Composition
—
—
—
—
—
30
—
—
—
—
1.5
—
—
—
100
68
83
74
83
88
6.7
10.6
1.8
14
25
83
88
—
—
—
14
25
—
—
—
100
100
61
83
74
6.21
10.5
1.8
—
94.0
99
100
—
18
4.5
.44
.11
—
—
6.0
1.0
—
—
79
86
88
_
12.3
7.2
4.4
—
79
86
88
12.3
7.2
3.7
—
100
100
84
—
30
16
80
Brigham Young UNivERsrri- Science Bulletin
Table 27. Physical and chemical data from Huntington Canyon. Water temperature (°C).
Site
4/15
5/13
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
Lawrence
9
10.5
13
15
16
23
13
9
3
-1
0
0
4
Highway 10
nd
nd
nd
12
14
20
13
9
3
-1
0
0
3
Plant Site
5
4
8
10
12
18
13
8
1.5
0
.2
1
3
Campground
5
4
8
9
11
17
13
7
1.5
0
1
1
3
Tie Fork
15
14.5
13
20
22
23
16
13
nd
nd
nd
nd
2
Stuart Station
8.8
8
6
12
15
17
13
7
.5
0
1
1.5
3
Bear Canyon
nd
5
6
U
15
18
14
11
3
nd
nd
nd
nd
nd = no data available
Table 28. Physical and chemical data from Huntington Canyon. Turbidity (JTU).
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
3/11
1971
1971
1971
1071
1971
1971
1971
1971
1972
1972
1972
nd
58
10
7
40
5
15
30
80
140
170
nd
nd
nd
5
10
5
10
10
65
65
140
12*
40
0
15
20
13
65
5
15
5
20
20*
15
0
5
9
13
12
15
0
0
0
nd
nd
18
35
40
3
nd
nd
nd
nd
75
6*
0
0
20
22
1
5
15
5
0
5
nd
5
5
10
15
1
2
nd
nd
nd
nd
Lawrence
Highway 10
Plant Site
Campground
Tie Fork
Stuart Station
Bear Canyon
nd = no data available
♦Data recorded during corresponding time periods by Dr. Robert Wingett, Center for Health and Environmental
Studies, Brigham Young University.
Table 29. Physical and chemical data from Huntington Canyon. pH.
Site
6/8
1971
6/29
1971
7/30
1971
8/20
1971
9/15
1971
10/8
1971
11/15
1971
12/17
1971
1/20
1972
2/19
1972
3/11
1972
Lawrence
Highway 10
Plant Site
Campground
Tie Fork
Stuart Station
Bear Canyon
8.85
8.1
8.0
8.1
8.2
8.3
8.1
7.65
7.8
8.. 35
7.9
nd
nd
nd
7.7
8.3
8.3
8.0
8.0
7.8
8.4
7.9
8.2*
7.6
8.2
8.4
8.4
8.3
8.1
8.2
8.2
8.6
8.1
8.45
7.6
8.4
8.35
8.3
8.5
8.2
8.35
8.2
8.4
8.1
8.30
7.8
8.8
8.6
8.8
8.9
nd
nd
nd
nd
7.4
8.30
7.0
8.4
8.2
8.25
8.3
8.2
8.1
8.1
8.5
7.9
8.3*
8.4*
8.4*
8.65
8.25
8.2
8.2
nd
nd
nd
nd
nd = no data available
•Data recorded during corresponding time periods by Dr. Robert Wingett, Center for Health and Environmental
Studies, Brigham Young University.
liioi.i.cK Ai. Si nil s. \iii,. IS, No. 2 Ai.<:ak. <>i- IK'ntincion C^xnvon. I'taii 81
Table 30. Physical and chemical data fmm Huntington Canyon. Dissolved oxygen (mg/1).
Site 6/8 6/29 7/30 8/20 9/15 10/8 U/1.5 12/17 1/20 2/19 3/11
1971 1971 1971 1971 1971 1971 1971 1971 1972 1972 1972
Lawrence 9 5 9 9 10 8 6 .3 8 911
Highway 10
Plant Site
Campground
Tie Fork
Stuart Station
Bear Canyon 11* 7* 9* 8* 8 10 7 nd nd nd nd
nd = no data available
*Data recorded during corresponding time periods by Dr. Robert Wingett, Center for Health and Environmental
Studies. Brigham Yoinig University.
Table 31. Physical and chemical data from Huntington Canyon. Dissolved carbon dioxide (mg/1).
nd
nd
nd
9
10
8
10
4
6
9
11
10*
9
9*
9*
9
8
9
7
.5
9
11
11
10
9*
10*
9
7
7
9
8
10
11
8
5
nd
10
14
8
nd
nd
nd
nd
5
11
9
9*
9*
8
8
8
7
5
9
9
Site 6/8 6/29 7/30 8/20 9/15 10/8 11/15 12/17 1/20 2/19 3/11
1971 1971 1971 1971 1971 1971 1971 1971 1972 1972 1972
Lawrence
Highway 10
Plant Site
Campgroimd
Tie Fork
Stuart Station
Bear Canyon
2
4
12.8
12
4
2
6
24
16
18
8
nd
nd
nd
12
4
0
4
14
20
6
4
0*
1
4.8
8
0
0
2
6
6
2
2
1.4
2
6
12
1
2
2
5
6
2
2
0
0
0
0
0
2
nd
nd
nd
nd
24
2
3
3.6
4
2
2
2
6
4
2
2
nd
0*
nd
0
1
2
2
nd
nd
nd
nd
nd = no data available
*Data recorded during corresponding time periods by Dr. Robert Wingett, Center for Health and Environmental
Studies, Brigham Vonng University.
Table -32. Physical and chemical data from Huntington Canyon. Phosphate (mg/1)
Site
6/8
6/29
8/20
12/17
1/20
2/19
.3/11
1971
1971
1971
1971
1972
1972
1972
Lawrence
1.43
.10
.24
.16
.72
..30
.15
Highwav 10
nd
nd
.31
.06
.20
..32
.15
Plant Site
nd
.15
.07
.08
.18
.22
.11
Campgrotuid
4.0
..35
..57
.07
.04
.13
.05
Tie Fork
7..5
nd
nd
nd
nd
nd
.15
Stuart Station
1.31
.25
.04
.02
.04
.18
.03
Bear Canyon
nd
nd
.08
nd
nd
nd
nd
nd = n<i data .i\ ailable
1.0
..30
1..5
..57
.68
.60
.49
.60
.45
.49
.18
nd
nd
lul
.05
.07
.06
.24
..33
..32
.42
.20
.10*
.40
.0:5
.03
.08
.04
.22
.;30
.24
..34
.14
.10
.:)0
.0.3
.03
.02
.0.5
.20
..30
.26
..35
.17
.40
ml
.02
ncl
.06
.04
n<l
nd
nd
nd
.11
.40
.20
.10*
.07
.03
.04
.26
.31
.27
..35
.27
nil
.10*
.40*
.03
.06
.10
.37
nd
nd
nd
nd
82 BiiK.iiA.M Vou.NG Univehsity Scienck Bulletin
Table 33. Physical and chemical data I'rom Huntington Canyon. Nitrate nitrogen (mg/1).
Site 6/8 6/29 7/,30 8/20 9/1.5 10/8 11/15 12/17 1/20 2/19 .3/11
1971 1971 1971 1971 1971 1971 1971 1971 1972 1972 1972
Lawrence
Highway 10
Plant Site
Canipgronnd
Tie Fork
Stnart Station
Bear Canyon
nd = no data available
*Data recorded during corresponding time periods by Dr. Robert Wingett, Center for Health and Environmenta
Studies, Brigham Young University.
Table 34. Physical and chemical data from Huntington Canyon. Sulfate (mg/1).
Site
Lawrence nd 13,50* .3000 2.500 2600 22,50 26(K) 2700 17.50 1200 625
Highway 10 nd nd nd nd 1.300 1.500 16,50 1,300 1300 .3,50 190
Plant Site
Campground
Tie Fork
Stuart Station
Bear Canyon nd 2* nd 4* 5 5 6 nd nd nd nd
nd = no data available
*Data recorded during corresponding time periods by Dr. Robert Wingett, Center for Health and Environmental
Studies, Brigham Young University.
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
12
8*
17
7
10
8
36
28
20
15
.30
11
3*
5
7
10
10
25
22
18
10
20
nd
nd
7
nd
22
57
nd
nd
nd
nd
75
10
6*
8*
6
12
11
20
20
20
11
15
Table 35. Physical
and chemical dat.
a from
Hnntiii
gton Canyon. C
alclum
and magnesium
hariluf'
ss (mg/1 CaCOs).
Site
6/8
1971
6/29
1971
7/.30
1971
8/20
1971
9/15
1971
10/8
1971
11/15
1971
12/17
1971
1/20
1972
2/19
1972
3/11
1972
Lawrence
Ca Hardness
nd
760
770
660
580
11.50
9.50
10,50
6,50
7(K)
.300
Ml^ ] lardness
nd
2.50
6480
460
870
850
WO
9,50
6,50
1000
200
Total
nd
1010
7250
1120
14.50
1900
18.50
20t)0
1.300
17(H)
.500
Highway 10
Ca Hardness
nd
■id
ml
540
640
1100
7.50
800
7(K)
300
250
Mg Hardness
nil
nd
ml
160
180
400
550
,500
4.50
.3(K)
200
Total
nd
ml
ml
7(K)
820
1.500
1 500
13(X)
11,50
6(M)
450
Plant Site
Ca Hardness
11.5*
120
120
120
100
120
1,50
140
170
140
140
Mg Hardness
45*
55
60
40
60
60
80
110
40
UK)
no
Total
160*
175
180
160
160
180
2.30
2,50
210
240
250
Campground
Ca Hardness
120*
120
115
110
UO
120
160
140
1.50
1.50
140
Mg Hardness
35*
.50
45
40
70
60
80
110
60
90
90
Total
155*
170
160
1,50
180
180
240
250
210
240
230
Tie Fork
Ca Hardness
ml
55
60
60
60
70
ml
nd
nd
ml
2.30
Mg Hardness
ml
185
2,50
260
220
310
ml
ml
nd
ml
170
Total
mi
240
310
.320
280
.380
ml
ml
( Lihlc
nd
3.5 cm
ml
itinui'il
400
on p. 83)
Bi<)[.()(a<:Ai, Si;iui-.s, \i)i.. hS, \(i.
Alcae ok Humingion Canyon, Utah
83
Stuart Station
Ca Hardness
Mg Hardness
Total
Bear Caiivon
()a Hardness
Mg Hardness
Total
100*
135
130
140
130
140
140
140
150
130
110
50*
40
45
100
60
70
60
70
50
100
100
150*
175
175
240
190
210
200
210
200
230
210
nd
80*
110*
120
120
105
130
nd
nd
nd
nd
nd
50*
35*
120
60
55
60
nd
nd
nd
nd
nd
130*
145*
240
180
160
190
nd
nd
nd
nd
nd = no data available
*Data recorded dnring corresponding time periods by Dr. Robert Wingett, Center for Health and Environmental
Studies, Brigham Young University.
Table 36. Physical and chemical data from Huntington Canyon. Bicarbonate alkalinity (mg/1 CaCOs).
Site
6/29
7/30
8/20
9/15
10/8
11/1.5
12/17
1/20
2/19
3/11
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
Lawrence
315
330
290
300
330
380
410
300
330
250
High way 10
nd
nd
280
320
340
360
370
340
270
2.50
Plant Site
175
170
160
170
200
210
240
200
220
220
Campground
175
160
160
170
200
210
2.30
220
230
220
Tie Fork
2.50-'
270''
280''
250^
3.50
nd
nd
nd
nd
.380
Stuart Station
165
170
180
190
210
210
220
210
210
200
Bear Canyon
nd
nd
170
1.30
170
160
nd
nd
nd
nd
nd = no data available
■'Number includes 75 mg/1 of carbonate alkalinity
''Number includes .30 mg/1 of carbonate alkalinity
^'Number includes 20 mg/1 of (!arbonate alkalinity
Table 37. Physical and chemical data from Huntington Canyon. Silica (mg/1 SiOa)
Site
6/8
6/29
7/30
8/20
9/15
10/8
11/15
12/17
1/20
2/19
.3/11
1971
1971
1971
1971
1971
1971
1971
1971
1972
1972
1972
Lawrence
7.3
8.75
8.75
9.0
9.3
10.5
13.0
16.0
14.5
17.0
10.0
Highway 10
nd
nd
nd
10.5
14.5
12.5
18.0
18.0
16.0
12.0
9.0
Pl.int Site
3.9*
3.5
3.4
.3.2
4.2
4..35
6.75
7.5
8.3
8.0
7.5
Campground
1.9
4.0*
.31
.3.6
3.8
4.. 35
6.5
4.0
8.3
8.0
7.3
Tie Fork
6.2
nd
1.7
7.5
2.4
5.0
nd
nd
nd
nd
16.5
Stuart Station
4.1
3.5
6.13
6.4
5.6
6.25
6.5
8.5
7.5
8.5
8.0
Bear Canyon
nd
3.5*
7.2*
5.75
5.2
6.65
6.6
nd
nd
nd
nd
nd = no data available
♦Data recorded during corresponding time periods by Dr. Robert Wingett, Center for Health and Environmental
Studies, Brigham Young University.
84
Biiif:HAM Young U.NivERsiTi' Science Bulletin
APPENDIX II
ALGAE COLLECTED FROM HUNTINGTON
CANYON OCTOBER 1970 - MARCH 1972
Division Ghlorophyta
A. Class Chlorophyceae
1. Order Volvocales
a) Family Chlamydomonadaceae
Carteria klebsii (Dang.) Dill
Chlamydomonas sp.
b) Family Volvocaceae
Pandorina morum (Muell.) Bory
Volvox terlius A. Meyer
Order Tetrasporales
a) Family Gloeocystaceae
Gloeocystis sp.
Order Chlorcoccales
a) Family Chlorococcaceae
Characium ambiguum Hermann
C. obtusum A. Braun
b) Family Oocystaceae
Ankistrodesmus falcatus (Corda) Ralfs
Closteriopsis longissima var. tropica West
and West
Nephrocytium lunatum W. West
Oocystis gigas Archer
c) Family Dictyosphaeriaceae
Botryococcus sudeticus Lemmermann
d) Family Scenedesmaceae
Scenedesmus bijuga (Turp.) Lagerheim
S. denliculatus Lager.
S. quadricauda (Turp.) de Brebisson
e) Family Hydrodictyaceae
Pediastrum telras (Ehr.) Ralfs
Order Ulotrichales
a) Family Ulotrichaceae
Stichococcus sublilis (Kutz.) Klercker
Ulothriz aequalis Kutz.
U. lenerrima Kutz.
U. tenuissima Kutz.
U. zonata (Weber & Mohr) Kutz.
b) Family Microsporaceae
Microspora willeana Lagerheim
c) Family Cylindrocapsaceae
Cylindrocapsa conjerta W. West
Order Chaetophorales
a) Family Chaetophoraceae
Draparnaldia plumosa (Vauch.) C. A.
Agardh
Protoderma viride Kutz.
Sligeoclonium attenuatum (Hazen)
Collins
5. stagnatile (Hazen) Collins
b) Family Aphanochaetaceae
Aphanochaete repens A. Braun
c) Family Coleochaetaceae
Coleochaete irregularis Pringsheim
Order Oedogoniales
a) Family Oedogoniaceae
Oedogonium spp.
Order Cladophorales
a) Family Cladophoraceae
Cladophora fracla (Dillw.) Kutz.
C. glomerala (L.) Kutz.
Rhizoclonium hicroglyphicum (C. A.
Kutz.
Order Zygnematales
a) Family Zygnemataceae
Mougeotia capucinn (Bory) C. A.
Agardh
M. genufleia (Dillw.) C. A. Agardh
M. parvula Hassall
Spirogyra decimina (Muell.) Kutz.
S. dubia Kutz.
S. porticalis (Muell.) Cleve
S. spp.
Zygnema insigne (Hass.) Kutz.
Z. spp.
b) Family Desmidiaceae
Closteriuni acerosum (Schr.) Ehr.
C. dianae Ehr.
C. ehrenbergii Menegh.
C. lanceolatum Kg.
C. motiilifrruni Ehr.
C. rostratum Ehr.
C. spp.
Cosmarium margaritiferum Menegh.
C. ochthodes Nord.
C. ovale Ralfs
C. quinarium Lund
C. tinctum Ralfs
C. spp.
Euastrum sp.
Micrasterias sp.
Pleurotaenium ehrenbergii Ralfs
P. sp.
Sphaerozosma filiforme Rabh.
Stauraslrum eustephanum (Ehr.) Ralfs
lS. gracile Ralfs
5. mutica Breb.
B. Class Charophyceae
1 . Order Charales
a) Family Characeae
Chara vulgaris Linnaeus
IL Division Euglenophyta
A. Class Euglenophyceae
1 . Order Euglenales
a) Family Euglenaceae
Euglena acus Ehrenberg
E. gracilis Klebs
£. minuta Prescott
E. sp.
Eutreptia sp.
Phacus acuminatus Stokes
P. pyrum (Ehrb.) Stein
P. sp.
Trachelomonas robusta Swirenko
IIL Division Pyrrhophyla
A. Class Dinophyceae
I. Order Peridiniales
a) Family Peridiniaceae
Peridinium cinctum (Muell.) Ehrenberg
b) Family Ceratiaceae
Ceratium hirundinella (Muell.) Dujardin
IV. Division Chrysophyta
A. Class Xanthophyceae
1 . Order Heterococcales
a) Family Characiopsidaceae
Characiopsis acuta (A. Braun) Borzi
C. longipes (Rabh.) Borzi
b) Family Chlorotlieciaceae
Ophiocytium sp.
2. Order Tribonematales
Ag.) a) Family Tribonemataceae
Tribonema bombycinum (C. A. Ag.)
Derbes & Solier
3. Order Vaucheriales
a) Family Vaucheriaceae
Vaucheria geminata (Vauch.) De Candolle
Biological Series, Vol. 18, No. 2 Algae of Huntington Canyon, Utah
85
B. Class Chrysophyceae
1. Order Chromulinales
a) Family Hydniraceae
Hydrurus foetidus (Vill.) Trev.
2. Order Ochromonadales
a) Family Dinobryaceae
Dinobryon cylindricum Imhof
C. Class Bacillariophyceae
1. Order Centrales
a) Family Coscinodiscaceae
Cyclotella meneghiniana Kutz.
2. Order Peimales
a) Family Fragilariaceae
Asterionella formosa Hassall
Diatoma anceps var. linearis M. Perag.
D. hiemale var. mesodon (Ehr.) Grunow
D. tenue var. etongatum Lyngb.
D. vulgare Bory
D. vulgare var. breve Grunow
Fragilaria construens var. binodus (Ehr.)
Grunow
F. construens var. venter (Ehr.) Grunow
F. crotonensis Kitton
F. leptostauron (Ehr.) Hust.
F. pinnata var. lancettula (Schum.) Hust.
F. virescens Ralfs
Hannaea arcus (Ehr.) Patrick
Hannaea arcus var. amphioxys (Rabh.)
Patrick
Meridian circulare var. constrictum
(Ralfs) v. Heur.
Synedra acus Kutz.
5. affinis Kutz.
S. delicatissima W. Sm.
S. pulchella Ralfs
S. pulchella var. lanceolata O'Meara
S. radians Kutz.
S. ulna (Nitz.) Ehr.
S. ulna var. ozyrhynchus (Kutz.) v. Heur.
S. ulna var. subequalis (Grun.) v. Heur.
Tabellaria feneslrata (Lyngb.) Kutz.
b) Family Eunotiaceae
Eunotia curvata (Kutz.) Lagerst
c) Family Achnanthaceae
Achnanthes defleia Reim.
A. hauckiana Grunow
A. lanceolata (Breb.) Grunow
A. lanceolata var. dubia Grunow
A. lanceolata var. haynaldii (Istv.-
Scaarsch.) CI.
A. linearis fo. curta H. L. Sm.
A. minutissima Kutz.
Cocconeis disculus (Schum.) Cleve
C. pediculus Ehr.
C. placentula var. euglypta (Ehr.)
Cleve
C. placentula var. lineata (Ehr.) v.
Heur.
C. rugosa Sov.
Rhoicosphenia curvata (Kutz.) Grunow
d) Family Naviculaceae
Amphipleura pellucida Kutz.
Amphiprora alata (Ehr.) Kutz.
Anomoeoneis vitrea (Grun.) Reim.
Caloneis ventricosa (Ehr.) Meist.
Diploneis pseudovalis Hust.
Gyrosigma acuminatum (Kutz.) Rabh.
G. spenceri (Quek.) Griff. & Henfr.
Mastogloia smithii Thwaites
Navicula bicephala Hust.
N. capitata Ehr.
N. cryptocephala Kutz.
N . cuspidata var. major Meist.
N. elginensis (Greg.) Ralfs
N. elginensis var. rostrata (A. mayer)
Patrick
A', exigua Greg.
A', lanceolata (Ag.) Kutz.
N. minima Grun.
N . odiosa Wallace
N. pelliculosa (Breb.) Hilse
A', peregrina (Ehr.) Kutz.
A', pseudoreinhardtii Patrick
A', papula Kutz.
A', radiosa Kutz.
A', radiosa var. tenella (Breb.) Grunow
A', rhyncocephala Kutz.
A', secreta var. apiculata Patrick
A', tripunctata var. schizonemoides (v.
Heur.) Patrick
Neidium affine var. longiceps (Greg.)
Cleve
N. binode (Ehr.) Hust.
Pinnularia brebissonii (Kutz.) Rabh.
P. viridis var. minor Cleve
Pleurosigma delicatulum W. Sm.
Stauroneis anceps Ehr.
S. phoenicenteron (Nitz.) Ehr.
S. phoenicenteron fo. gracilis (Ehr.) Hust.
S. smithii Grunow
e) Family Gomphonemataceae
Gomphonema acuminatum Ehr.
G. constrictum Ehr.
C. gracile Ehr.
G. intricatum Kutz.
G. olivaceum (Lyngb.) Kutz.
f) Family Cjonbellaceae
Amphora ovalis Kutz.
Cymbella amphicephala Naeg.
C cuspidata Kutz.
C. cymbiformis Agardli
C. gracilis (Ehr.) Kutz.
C. parva (W. Sm.) Wolle
C. ventricosa Kutz.
g) Family Epitliemiaceae
Denticula elegans Kutz.
Epithemia argus Kutz.
E. turgida var. westermanni Ehr.
Rhopalodia gibba (Ehr.) O. Muell.
h) Family Nitzschiaceae
Nitzschia acicularis (Kutz.) W. Sm.
A', angularis var. affinis Grun.
A', communis Rabh.
N. dissipata (Kutz.) Grun.
A', frustulum var. perpusilla (Rabh.)
Grunow
A', hungarica Grun.
A', linearis W. Sm.
A', palea (Kutz.) W. Sm.
A', sigmoidea (Ehr.) W. Sm.
A', vermicularis (Kutz.) Hantz.
i) Family Surirellaceae
Cymatopleura elliptica (Breb.) W. Sm.
C. solea (Breb.) W. Sm.
Surirella angustata Kutz.
S. baileyi Lewis
S. ovalis Breb.
5. ovaia Kutz.
V. Division Cyanophyta
A. Class Myxophyceae
1 . Order Chroococcales
a) Family Chroococcaceae
Chroococcus limneticus Lemm.
C. minutus (Kutz.) Nag.
Gloeocapsa sp.
Gomphosphaeria aponina Kutz.
Merismopedia elegans A. Br.
M. glauca (Ehr.) Nag.
M. tenuissima Lemm.
2. Order Chamaesiphonales
a) Family Chamaesiphonaceae
Chamaesiphon sp.
86
Bhk;ham Young University Science Bulletin
3. Order Oscillatoriales
a) Family Oscillatoriaceae
Lyngbya aerugineo-coerulea (Kutz.)
Gomont
L. aestuarii (Mert.) Leib.
L. major Meneg.
L. martensiana Meneg.
L. spp.
Oscillatoria agardhii Gomont
O. amphibia Ag
O. limosa Ag.
O. tenuis Ag.
O. spp.
Phormidium sp.
Schizothrii fragilis (Kutz.) Gomont
Spirulina major Kutz.
S. princeps (West & West) G. S. West
4. Order Nostocales
a) Family Nostocaceae
Anabaena circinalis Rabh.
A. spp.
Nostoc paludosum Kutz,
A', piscinale Kutz.
b) Family Scv-tonemataceae
Tolypothrix lanata Wartm.
c) Family Rivulariaceae
Calothrix sp.
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Blum, John L. 1956. The ecolog>- of river algae.
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Bbinley, F. J. 1950. Plankton populations of certain
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Butcher, R. W. 1932. Studies in the ecology of
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Chatvvin, S. L. 1956. The vertical distribution of
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Clark, W. J. 1958. The phytoplankton of the Logan
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Coombs, Robert. 1964. A floristic and ecological sur-
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Utah. Salt Lake City.
Daily, William A. 1938 A quantitative studv of the
phytoplankton of Lake Michigan collected in the
vicinity of Evanston, Illinois. Butler Univ. Bot.
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Daubenmire. R. 1968. Plant communities. Harper
and Row, New York. 300 pp.
Dillard. Gary E. 1966. A floristic and ecological
study of benthic algae in two North Carolina
streams. Ph.D. Tliesis. North Carolina State Univ.,
Raleigh, North Carolina.
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in I^ake Tiberias as measured bv the glass-slide
method. Israel J. of Bot.. 19:1-15.
Dustans. William A. 1951. A comparative study of
dredged and undredged portions of the Provo River.
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Dutton, C. E. 1880. Report on the geology of the
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Gov't Printing Office, Washington D. C. 307 pp.
Flowers. Seville. 1959. Vegetation of Glen Canyon.
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Glen Canyon. Univ. Utah Anthropological Papers,
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Longley, Glenn J. 1969. Plankton associations in
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Whitford, L. a. and G. J. Schumacher. 1963. Com-
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^•^NA - ^(ro^o)
Brigham Young University
MuacoNH-zoou Science Bulletin
LIBRARY
NOV 510/3 **Hte«-^
u'nBRKding ecology of raptors
in the eastern great basin
OF UTAH
by
Dwight G. Smith
and
Joseph R. Murphy
BIOLOGICAL SERIES — VOLUME XVIII, NUMBER 3
JUNE 1973/ISSN 0068-1024
BRIGHAM YOUNG UNIVERSITY SCIENCE BULLETIN
BIOLOGICAL SERIES
Editor: Stanley L. Welsh, Department of Botany,
Brigham Young University, Provo, Utah
Acting Editor: Vernon J. Tipton, Zoology
Members of the Editorial Board:
Ferron L. Andersen, Zoology
Joseph R. Murdock, Botany
WiLMER W. Tanner, Zoology
Ex officio Members:
A. Lester Allen, Dean, College of Biological and Agricultural
Sciences
Ernest L. Olson, Director, Brigham Young University Press
The Brigham Young University Science Bulletin, Biological Series, publishes
acceptable papers, particularly large manuscripts, on all phases of biology.
Separate numbers and back volumes can be purchased from University Press
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Orders and materials for library exchange should be directed to the Division
of Gifts and Exchange, Brigham Young University Library, Provo, Utah 84602.
I
Brigham Young University
Science Bulletin
BREEDING ECOLOGY OF RAPTORS
IN THE EASTERN GREAT BASIN
OF UTAH
by
Dwight G. Smith
and
Joseph R. Murphy
BIOLOGICAL SERIES — VOLUME XVIII, NUMBER 3
JUNE 1973/ISSN 0068-1024
TABLE (W CONTENTS
ABSTRACT 1
INTRODUCTION 1
REVIEW OF LITERATURE 2
STUDY AREA 3
Location and Topography 3
Climate 3
Vegetation 3
Faunal Elements 5
Human Utilization 5
METHODS 6
RESULTS 7
Basic Population Data 7
Population Composition and Density 7
Seasonal Activity Timetables 9
Nest Site Requirements 13
Productivity 23
Territoriality 29
Hunting Activity Patterns and Habitat 43
Predation 45
DISCUSSION AND CONCLUSIONS 54
Populations 54
Nest Site 55
Productivity 58
Territoriality 62
Predation 64
The Ferruginous Hawk 67
The Long-eared Owl 68
Effect of the Investigator 69
SUMMARY 70
ACKNOWLEDGMENTS 71
APPENDIX — WEIGHTS OF PREY SPECIES USED LN THE BIOMASS CALCULATIONS 71
LITERATURE CITED 72
BREEDING ECOLOGY OF RAPTORS IN THE
EASTERN GREAT BASIN OF UTAH
by
Dwight G. Smith' and Joseph R. Murphy-
ABSTRACT
A comparative study of the breeding ecology
of 12 raptor species was conducted in the east-
em Great Basin from 1967-1970. The project
was designed to deteiTnine the composition and
densities, habitat selection, territoriahty and
predatory habits of raptorial birds in a semi-
arid en\iromnent. All topics were analyzed com-
parativeh', relating the requirements and activi-
ties of the 12 raptor species.
Average vearly population densities of all
species approximated 0.5 pairs per square mile,
but much of the available habitat was not util-
ized. Predominant raptors were the Ferruginous
Hawk and Great Horned Owl. Other important
raptors included the Golden Eagle, Red-tailed
Ha\\'k and Raven.
The breeding activities of the collective rap-
tor populations occurred over a period of eight
months. Great Homed Owls and Golden Eagles
\\ere the first raptors to initiate nesting activi-
ties, usually in late January and early February.
The raptor breeding season tenninated with the
fledging of the young Cooper's Hawks and Bur-
rowing Owls in late August.
The fecundity of the raptor populations
varied between years. Specific causes of mortal-
ity of eggs and voung included nest desertion
and destruction, predation, apparent egg infer-
tility, and accidents, most of which could be
directly attributed to some fonn of human inter-
ference.
The observed home ranges of the raptor
species were a function of their body size and
breeding status.
The food of the raptors included at least 55
different prev species, but most relied heavily
on only one or two species. A correlation be-
tween raptor size and mean prey weight was
evident. No examples of raptor predation on
game or domestic livestock were found.
INTRODUCTION
Raptorial birds generally occupy the top
levels of their food webs and as such exert
considerable influence on local mammal and
avian prev populations. Shelford ( 1963) classifies
them as major permeant influents and sug-
gests that the raptor populations of the Great
Basin desert fulfill roles equivalent to such
inannnalian predators as the bobcat ( Li/nx
Tufiis), coyote (Canis latram). kit fox (Vtilpes
uiacrotis), and badger {Taxklca taxtis). Their
declining numbers and economic relationships
warrant additional interest, and studies of total
raptor populations are needed as a means by
wliich we ma\' elucidate their responses to
changing pressures and environmental condi-
tions. Although their large size and predatory
habits render them conspicuous, their extensive
territorial recjuirements present difficulties to
raptor ecologists desiring to obtain data on rep-
resentative populations. Hence, there have been
few previous attempts to study collective rap-
tor populations in detail.
The objective of this study is tc; provide
quantitative data on the breeding ecology of
central Utah raptors. Aspects of the study which
are emphasized include raptor populations and
their distribution, yearly productivit)', territo-
riality, and predation. All topics are treated
comparatively, relating the requirements and ac-
tivities of the 12 raptor species. The species
studied include four buteonids, the Golden
Eagle (Aqtiila chrysaetos), Red-tailed Hawk
(Buteo jnmaicensis) , Fernaginous Hawk (Buteo
recalls), and Swainson's Hawk (Buteo swain-
'I)ep.trtnipnt nt Biology. Sonlliciii Coniiciticiil Slalo ('oIIckc New Iliivon. < oiinot lu ill Oft'jl')
-DepiTrtlilcnl of Zoology. lirit'.Ii.im Voiiii^ t,^iivci\ily. I'rovii. lll.ili 84()0i
HiuciiAM VouNc University Sf:iENCE Bulletin
sonii); two falcons, tlic Prairit> Falcon (Falco
incxicantis) , and Sparrow Hawk (Falco spar-
vcrius); three owls, the Great Horned Owl
(Bubo virginkiniis). Short-eared Owl (Asia
fltiiniiicus), and Burrowing Owl [Speotyto cuni-
ciihiria); the Marsh Hawk (Cirnis cijaneus),
Cooper's Hawk {Accipiter coopcrii), and Raven
(Corviis corax).
REVIEW OF LITERATURE
netaili'd studies on eiilleeti\e raptor popula-
tions in North America have been conducted
ill Michigan and W\i»ming (Craighead and
Craighead, 1956), the' Alaskan tundra ( Pitelka,
Toni'ich and Treichel, 1955a, 19551)), and the
Tule Lake region of northern California (Dixon
and Bond, 1937; Bond, 1939). In other popula-
tion studies Mathisen and Mathisen (1968) ex-
plored tin- species and seasonal abundance of
raptors in Nebraska, and Baunigartner and
Bauingartner (1944) examined the food habits
and population fluctuations of hawks and owls
in Oklahoma. Recenth' Hicke\' ( 1969) has sum-
marized much information on the general status
and broad trends of cuiTcnt raptor populations,
but his work centers around the Peregrine Fal-
c(.n (Fiiico peregrinufi) . Other comparative
studies have dealt with the ecology of Great
I'orned Owls and Rcd-tailcd Hawks. The more
informative of these have been conducted in
Wisconsin (Orians and Kuhlman, 1956), New
York (Hagar, 1957), and Minni'sota (LeDuc,
1970). Brown (1966, 1970) has provided much
inlormation on African raptor populations, par-
tieularlv with respect to their niclu' allocation.
Other associative studies have focused on
a ]-)articular aspect of raptor ecology, most coni-
niDiih predation. Specific comparative food
habits studies on hawks and owls have been con-
ducted bv Fisher (1895), Errington (1932c,
1933), Mendall (1944), and Craighead and
Craighead (1956); on hawks by McAtce (1935),
Errington and Breckinridge (1938), Hamerstrom
;iii(l Ilamcistroin ( 1951), and Storer (1966); and
on owls bv Cahn and Kemp (1930), Wilson
(1938), Fitch (1947). Kirkpatrick and Conway
(1947), Pear.son and Pearson (1947), Marti
(1969a), and Earhait and Johnson (1970).
Life history studies of most of the raptors
have been conducted in a varietN' of habitats,
and many of them have been summarized in
the works of Rent (1937, 19.38) and Brown and
Amadon (1968). The following arc among the
more noteworthv of a large amount of published
literature on various phases of the nesting ecol-
ogy of the raptors studied in this report, to-
gether with the rcjgions in which they were
studied:
Golden Eagle. C-'ameron (1905), McGahan
(1967, 1968), Montana; Finley (1906), Dixon
(19.37), Carnie (1954), California; Arnold
(1954), North America; Wellein and Ray
(1964), Boeker and Ray (1971), Rocky Moun-
tains; Sandeman (1957), Watson (1957), Brown
and Watson (1964), Lockic (1964), Brown
(1969), Scotland.
Great Homed Old. Dixon (1914), Fitch
(1940), California; Errington (19.32b, 1938),
Iowa; Swenk (1937), Missouri Vallev; Baum-
gartner (1938, 1939), Iowa and New York; Er-
rington, Hamerstrom and Hamerstrom ( 1940),
north central United States; Houston (1971),
Saskatchewan.
Ferruginous Hank. Cameron (1914), Mon-
tana; Bowles and Decker (1931), Angell (1968),
Washington; Salt (19.39), Canada.
Red-tailed Hawk. English (1934), Michigan;
Fitch, Swenson and Tillotson (1946). California;
Austing (1964), North America; Luttich, et al.,
(1970), Luttich, Keith and Stephenson (1971),
Canada; Scidensticker (1970), Montana.
Swainson's Hawk. Cameron (1908, 1913),
Montana; Bowles and Decker (1934), Wash-
ington.
Prairie Falcon. Decker and Bowles (19.30),
Washington; Fowler (1931), California; Bailey
and Niedraeh (1933). Webster (1944), Ender-
son (1964), Colorado; Edwards (1968), Alberta.
Marsh Hawk. Breckinridge (1935), Minne-
sota; Errington and Breckinridge (1936), north-
central United States; Hammond and Henry
(1949), North D;ikota; Hamerstrom (1969),
Wisconsin. i
Cooper'.s Hawk. McDowell (1941), Schrivcr
(1969), Pennsylvania; Meng (1959), New York
and Pennsylvania.
S})arrow Hawk. Sherman (1913), Iowa; i
Rocst (1957), Oregon; Endcrs(m (1960), II- '
linois; Heintzelman (1964), Heintzelman and
Nagv (1968), Pennsylvania; Wilkmghbv and
Cade (1964), New York.
Short-eared Owl. Kitchin (1919), Washing-
ton; Sinder and Hope (19.38), Toronto; Lockic
BiOLor.iCAi, Sf.hies, \'ol. 18, No. 3 BuEEniNC. Ecology of Utah Raptohs
(1955), Scotland; Johnson (1956), California;
BorrtTO (1962), Colombia; Short and Drcw-
(1962), Michigan; Munyer (1966), Illinois.
BurroiL'ing Old. Rhoades (1892), Florida;
Errington and Bennett (1935), Scott (1940),
Iowa; Grant (1965), Minnesota; Coulombc
(1971). Thomsen (1971), California.
Raven. Oberholser (1918), North America;
Harlow (1922), Pennsylvania; Bowles and
Decker (1930), Washington; Nelson (1934),
Oregon; Cushing (1941), California; Parslow
(1967), Holyoak and Ratcliffe (1968), Great
Britain and Ireland; Ratcliffe (1962), England.
Literature pertaining to raptors of the Great
Basin includes egg-collecting notes (Wolf,
1928); population studies of wintering eagles
(Edwards, 1969); nesting studies of the Golden
Eagle, Great Horned Owl, and Ferruginous
Hawk (Murphy, et al., 1969); raptor population
trends ( White, 1969a ) ; and notes on interactions
between Red-tailed Hawks and Great Homed
Owls (Smith, 1970).
STUDY AREA
Location and Topography
This study was conducted in an 80-square-
niile section of the eastern edge of the Great
Basin Desert in north central Utah. It included
parts of Utah and Tooele Counties, in Town-
ships 7 and 8 South, Range 3 West, Salt Lake
base and Meridian (Fig. 1). The area chosen
is a representative portion of the habitat of
this part of the Great Basin. Its coverage is
thought to be sufficient to enable the compila-
tion of an accurate record of the raptor species
populations.
The topography is characterized bv broad,
flat, alkaline valle\s separated b\- high ridges
and hills. Its major ph\siographic featines, from
east to west, include Cedar Valley, the Thorpe
and Topliff Hills of the Tintic Range, and Rush
Valley. Valley elevations range from 4800 ft in
Cedar Valley to 5300 ft in Rush Valle\ . Maxi-
mum elevations were 6190 ft in the Thorpe Hills
and 6453 ft in the Topliff Hills.
A major feature of the hills was tht- numer-
ous sandstone and limestone cliffs and rock
outcroppings resulting from the erosion of a
series of Paleozoic strata ranging in age from
the Lower Cambrian to Upper Pennsylvanian
(Bullock, 1959; Bissell, et al., 1959) (Fig. 2).
A second striking feature of the hills is the pres-
ence of several large quarries, originally mined
for clay, calcite, or limestone, but long since
abandoned. These cjuarries are characterized by
steep, sheer walls occasionalK' reaching over
200 feet in height.
Climate
The general climatic conditions of this por-
tion of the Great Basin have been characterizi'd
by Fautin (1946) and Shelford (1963). The
mean annual precipitation is 16 inches at the
extreme northern edge of the study area and
12 inches over the majority of the rest of the
area. Slight local variations occur, with the high-
er elevations receiving larger amounts ( Feltis,
1967). Although the area receives some snow-
fall, most of the moisture falls from March
through May and July through August. Ex-
posure particularly alters the pattern with re-
spect to snowfall accumulation and persistence,
and north facing slopes may have from 3 to 12
inches of snow for over a month after southern
exposures are bare.
Approximate annual temperatures range from
-30°C to 65°C. Wide seasonal and daily varia-
tions occur, amounting to as much as 30°C or
more during the summer months. July is the
hottest month of the year, averaging 23°C. Sub-
zero temperatures can be expected for short
periods from December through mid-March.
High winds are a common feature of the
early spring months and rnay result in locally
heavy dust stonns. These become less severe but
may persist throughout all months of the year.
Water flow is ephemeral and no permanent
streams, seeps, ponds, or impoundments are
present within the study area.
Vegetation
Two distinct vegetational associations occur,
the northern desert shrub and the dwarf conifer
communit\-. The desert shrub community is
present over lower elevations of most of the
valley floors and consists of various shrubs and
grasses (Fig. 3). Several of these, becoming lo-
cally dominant and fonning large, continuous
stands, include, in order of their importance,
l)ig sagebrush (Artemisia tridentata ), rabbit-
i)rush (Cliri/sothamnu.s nau.scosu.s) , shadscale
(Alriplex confeitifolia). i^reast'wood {Sarcoha-
ttis vermiculatus) , winterfat (Eurotia hiiuita),
HiuciiAM Voi'SG Univeivsity Science Bulletin
Fig. 1. Location, topograpliv .iiul wgetation of flic shulv area.
Hi(n.(H;K:\i. Skhiks. Vol. 18, No. 3 Bueedinc Kcologv ok Utah IIaptoivs
;l#^-
Fig. 2. \i(\\ of a portion of the Thorpe Hills, showing tho> nnmeroiis
anil the seattered nature of the Pinyon-Juniper community.
limestone and sandstone cliff lines
Russian thistle (Salsola kali) ami hoisobriisli
{Tctnuhjmia ghibnita). Both Indian liccgiass
(On/zopsis hijmenoides) and cheat gias.s {Bro-
mus tectorum) arc present throughout most of
the shrub stages, with the latter apparently in-
creasing its coverage ( Christensen and Hutchin-
son. 1965).
The better drained slopes and hills support
the pigm^' conifer forest or woodland biome
(Kendeigh, 1961 j. Tiiis is characterized by the
uniform physiognomy of its principal species, the
two most important being Utah juniper {Juni-
pertis osteospcrma) and pinyon pine (Pimi.i
mdnoplu/Ua). The trees average approximately
10-1.3 ft in height and occur in stands varying
in densit\- from 10 to 100 trees per acre ( Smith,
1968). Important shrubs of the underston' in-
clude matchweed (Gutierrczia sarothrac) and
Ephedra {Ephedra sp. ). Other components pres-
ent in lesser amounts include cliffrose (Cowania
mcxicana) and mountain mahogany (Cercocar-
ptts ledif alius).
Faunal Elements
Fautin (1946) listed a total of i286 animals
known to occur in the northern desert shrub
communit\', including 28 mammals, 45 birds
(exchisi\'e of the raptors and aquatic species),
10 reptiles and 203 insects. Most of these also
occur within the pinvon-juniper community
which to dat(^ has recei\ed no in-depth study
in this area. Hardy ( 1945 ) did record 79 bird
species of the pigmy conifers and noted that 14
species were summer residents.
The major mammalian herbivores include the
mule deer (Odocoilciis hemiomts), black-tailed
jackrabbit (Lepus califoruicus), Townsend's
ground squiiTcl {Spermo])hilus townsendi), an-
telope ground squirrel [Ammospermophilus
leucunis), desert cottontail {Sylvilagus audu-
houi), and desert wood rat {Dipodomys sp. ),
pocket mouse (Perognathus sp.), and several
miuids and cricetids. Carnivores other than rap-
tors include the mountain lion (Felts concolor),
coyote (Canis latrans), kit fox (Vulpes macro-
tis), bobcat {Lynx mfiis), and badger {Taxidea
taxus). Two of the more common summer bird
species include the Honied Lark {Eremophila al-
f)cstris) and Mourning Dove {Zenaidura ma-
croura). Common reptile species include the
gopher snake {Pituophis melanoleucus), striped
racer {Coluber taeniatus), collared lizard
(Crotaphytus collaris), and Uinta lizard {Uta
stamburiana) .
Human Utilization
Two small settlements are present immedi-
ately northeast of the study area and portions of
the adjacent land are dry-fanned, but the most
important human activities include livestock
raising and hunting. Most of the valleys and
lower elevations are seasonally utilized for sheep
HiuciiAM VouNG Univeksity Science Bulletin
range and are heavily overgrazed. In addition,
the direct infkicncc of Hvestock interests has
resulted in the initiation of predator control
programs and govennnent trappers periodically
remove coyotes, bobcats, and kit foxes.
Recreational hunting activities assume major
proportions. Almost all parts of the area are
accessible by graded dirt roads, and large num-
bers of deer hunters in season and rabbit hunters
throughout the year utiUze the area for sport.
ii'-?«'»gT;s.'«.:
Fig. .3. Sagebrush ami IniiR-hgrass comiiiuiiit\ iif Cedar X'allev.
METHODS
The stud\' was conducted from December
1966 until August 1970. Most of the field work
took placi' duiing the four breeding seasons but
observations were recorded during every month
of the year. Intensive field work began in De-
cember of each \ ear and continued through
August. During this time at least weekK' or bi-
weekly \isits were made, but often the observa-
tion periods were more frequent. Throughout
the four breeding seasons the longest interval of
time between successive visits was 13 days in
April 1970,
Field data cards were designed and printed,
and copies of that portion of the study area
mapped by the U,S. Geological .Survey were
Xeroxed. All observations on raptor nests, ac-
tivities, and locations were recorded on them
and supplemt^nted by tape recorded notes.
The major task of the observer during each
breeding season involved the location of all
raptor nests. These were found by systematically
searching all potential nest sites; that is, all cliff
lines, rock outcioppings, and wooded areas were
methodicalh' examined. Discovered nests were
plotted on an area survey map, then gaps in
the distribution wen- intensively reexamined
lor missed nests or signs of raptor activit\' sev-
eral times dmintr the breedini: season. Addi-
tional techniques were employed to discover
nests; these included observations of behavioral
patterns (particularK displays and tiTritorial
postures), the mapping of old nests, and the
utilization of a fixed wing monoplane for aerial
surve\s. The latter proved to be of limited use,
due prinuuilv to its miniminn speed and altitude
re(|nirenu'nts, but was useful in checking the oc-
cupane\' of nests of the previous years.
Instances in which apparently nonnesting
pairs or individuals were occupying an area
necessitated numerous additional and time-con-
Biological Stints, \ol. 18, \i
BiittDJNc; Ecology of Utah Haitous
suming checks to ensure the accuracy of their
status. Apparent transients required similar ef-
forts.
Certain raptor species required proportion-
all\' greater efforts than others in locating their
nests. This proved to be particularly true of the
Great Homed Owl and Short-cared Owl. Their
secluded nest sites and nocturnal habits re-
quired several earlv morning and late evening
visits in an effort to locate hooting males. Baum-
gartner (1939) and Errington (1932b) employed
this method successfully in other habitats, but
the extreme ruggedness of most of the study
area terrain allowed only partial success. How-
ever, both owl species were observed occasion-
ally during these two time periods, particularly
on overcast davs or on rainy or snowv days. In
contrast, Burrouing Owls were easily located
because of their great diurnal activit\', more ac-
cessible nesting sites, and the habit of one or
both of the adults of roosting atop or alongside
the burrow. Onl\ t\\'o of the diurnal raptors, the
Marsh Hawk and Sparrow Hawk, presented
problems with respect to the location of their
nests. Both species are conspicuous during their
daily acti\'ities but verv secretive relative to the
actual location of their nests. These were most
easily found by continuous observation of the
adult pairs, one of which would eventually re-
turn to the nest site. Three of the Marsh Hawk
nests were found only after the increased de-
velopment of the \oung had rendered their loca-
tion conspicuous.
The tendencN' of raptors to reoccupy their
nest sites and territories (to be discussed in
detail later) greatly facilitated the task of lo-
cating nests during the last three years of study.
Data used to compute the raptor activity
timetables is based primariK' on the more readily
accessible nests. In addition, the necessary time
period between field observation days promotes
a possible time error of two days. Tlie presence
of the investigators may have accelerated some
events in the nesting cycle, with the fledging
period being particularly vulnerable to change.
Raptor territories and food habits were de-
termined during the nesting seasons of 1969 and
1970. Territories were plotted by observations
of pair activities from blinds and by plotting
sight locations. The points of maximum distance
from the nest site were then connected and the
encompassed area determined with a compen-
sating polar planimeter. The determined terri-
tory has been described as maximum territory
(Odum and Kunezler, 1955) or home range
(Craighead and Craighead, 1956). Food habits
of all raptors were determined by weekly tabu-
lations of prey items and analyses of pellets
gathered from the nest site. Again the more ac-
cessible nests were checked most frequently.
After the prey had been identified and counted
it was removed from the nest. An exception was
to leave fresh prey for the young, after marking
it for identification. Pellet contents were identi-
fied by comparison with specimens of the Brig-
ham Young University Life Sciences Museum
collection, following techniques described by
Errington (1930, 1932a), Glading, Tillotson and
Sellech (1943), and Moon (1949). Dr. V. A.
Nelson, entomologist. Southern Connecticut
State College, New Haven, Connecticut, assisted
in the identification of some insect remains.
All statistical analyses followed programs for
the Epic Model .3000 computer except regres-
sion, which was determined using Fortran pro-
grams. Numerical data within the text is normal-
ly presented as mean data, followed by the stan-
dard error, sample number, and range. The "t"
test, anah'sis of variance and chi-square tests
were used to compare data, and linear regression
analysis was used to test the significance of
correlated variables. The level of significance is
0.05 unless otherwise noted. All analytical meth-
ods are discussed by Goldstein ( 1964 ) and
Simpson, Roe, and Lewontin ( 1960 ) .
RESULTS
Basic Population Data
The study area supported a total of .354 in-
dividuals of 12 raptor species during the four
years of study. This included 141 nesting pairs,
20 nonnesting pairs and 32 individuals. The
species breakdown was as follows: Golden
Eagle, 17 pairs; Great Homed Owl, 31; Fer-
ruginous Hawk, 40; Red-tailed Hawk, 26; Swain-
son's Hawk, 5; Prairie Falcon, 3; Marsh Hawk,
5; Cooper's Hawk, I; Sparrow Hawk, 10; Short-
eared Owl, 1; Burrowing Owl, 6; Raven, 16.
Population Composition and Density
Annual species populations are presented in
Tables \-4. Both the total nesting population
and the number of nesting species varied from
year to year. The collective raptor population
consisted of 8 species in 1967 and 1968, 9 in
8
Biuf:ii,\M VouNC I'nivehs
nv S(:ii-.N( K
Bulletin
Table 1 . Summarv
of raptor
nesting populations. 1967.
No.
No. of
No.
No.
No. re-
No. successful
No. of nests
No. sq.
Species
of
nesting
single
nesting
nesting
nesting
incomplete
miles per
pairs
pairs
birds
failures
attempts
attempts
histories
pair
Golden Eagle
4
3
1
1
0
_
0
20
Great Horned Owl
5
4
1
0
-
-
0
16
Ferniijinous Hawk
8
8
2
3
0
-
0
10
Red-tailed Hawk
5
4
0
0
0
-
0
16
Swainson's Hawk
1
1
0
0
-
-
0
80
Prairie Kalcon
0
-
1
-
-
-
-
-
Marsh Hawk
0
_
1
_
_
_
_
_
Cooper's Hawk
1
1
0
?
?
-
1
80
Sparrow Hawk
4
3
1
1
0
_
1
20
S lort-eared Owl
0
_
2
_
_
_
_
_
Burrowing Owl
0
-
1
-
-
-
-
_
Raven
4
4
0
0
-
-
0
20
Totals
32
28
10
5
0
-
2
-
Table 2. Summary
of raptor
nesting populati
ons, 1968.
No.
No. of
No.
No.
No. re-
No. successful
No. of nests
No. sq.
Species
of
nesting
single
nesting
nesting
lencsting
incomplete
miles per
pairs
pairs
birds
failures
attempts
.lUeiupts
histories
pair
Golden Eagle
4
4
2
0
0
0
20
Great Horned Owl
10
9
5
0
0
2
8
Ferruginous Hawk
10
9
2
0
0
0
8
Red-tailed Hawk
i
7
3
2
1
1
11
Swainson's Hawk
1
1
0
-
0
0
80
Prairie Falcon
1
1
1
0
0
0
80
Marsh Hawk
0
-
-
-
_
-
-
Cooper's Hawk
0
-
-
-
-
-
-
Sparrow Hawk
3
3
1
0
0
0
27
S lort-earcd Owl
0
-
-
-
0
-
-
Burrowing Owl
0
-
-
-
-
-
-
Raven
4
4
0
0
-
-
0
20
Totals
40
38
6
14
2
1
3
-
Table 3. Summary of raptor nesting populations, 1969.
Species
No.
of
pairs
No. of
nesting
pairs
No.
single
birds
No.
nesting
failures
No. re- No. successful No. of nests No. sq.
nesting nesting incomplete miles per
attempts attempts histories pair
Golden Eagle .54121
Great Horned Owl S 8 1 2 0
Ferruginous Hawk 13 12 1 2 0
Bed-tailed Hawk 7 6 12 1
Swainson's Hawk 2 2 12 0
Piairic I'aleon 0 - 1 — -
Marsh Hawk 2 2 0 10
(.'ooper's Hawk 0 - 0 - -
Sparrow Hawk 2 2 2 10
Short-eared Owl 0 - 1 - -
Burrowing Owl 3 3 0 10
Raven 4 4 110
Totals 46 43 10 14 2
0
16
10
6
11
40
40
40
27
20
1969, and 11 in 1970. Only 7 of the 12 species
nested in all four study \ears. Of the more
sporadic nesters, 3, the Prairie Falcon, Marsh
Hawk and Burrowing Owl, nested during two
of the four years (not necessarily consecutively )
and 2, the Short-eared Owl and Cooper's Hawk,
nested in only one of the four \(\irs. .Ml, how-
ever, were represented bv either nonnesting
pairs or individuals during one or more of their
nonbreeding \ears, and are therefore considered
to be a minor but nonnal element of the raptor
breeding population of this area.
The minimum and maximum sizes of the
total raptor population varied from 74 to 102
iiidi\icluals and from 32 to 46 pairs. Individuals
coiniiioiiK comprised from 9 to 13 percent of
Bioi.or.icAi, SiiiiiEs, Vol. IS, No. .3 Hui i dino Ecology ok I'nii H.^i'tou.s
Table 4. Summary of raptor nesting populations, 1970.
No.
No. of
No,
No.
No. re-
No. successful
No. of nests
No. sq.
Specie.s
of
nesting
single
nesting
nesting
nesting
incomplete
miles per
pairs
pairs
birds
failures
attempts
attempts
histories
pair
Golden Eagle
4
3
0
0
_
_
0
20
Crt-at Horned Owl
8
6
19
3
1
1
0
10
Kemiginous Hawk
9
y
2
2
0
-
0
9
Ked-lailed Hawk
(
4
0
1
0
(1
0
11
SwainsDiis Hawk
1
1
1
0
-
-
0
80
Prairiu Falcon
2
2
0
1
0
-
0
40
Marsh Hawk
3
2
1
1
1
0
1
27
Cooper's Hawk
0
-
1
-
-
-
-
-
Sparrow Hawk
1
1
1
0
-
-
-
80
Short-eared Owl
1
1
0
1
0
-
0
80
Burrowing Owl
.3
3
0
1
0
_
0
27
Raven
4
■-)
0
0
-
-
0
20
Totals
43
32
24
10
2
1
1
-
the total population. Raptor populations in-
creased from 1967 (32 pairs, 10 individuals) to
1969 (46 pairs, 10 individuals) and then de-
clined slightly in 1970 (43 pairs, 6 individuals).
The peak number of nesting raptor species did
not coincide with the peak raptor populations
but rather occurred one year later. The yearly
variation in populations was due in part to some
shifting of raptor nesting sites onto the study
area from previous nesting sites and territories
immediatelv adjacent to the study area. Other
possible reasons will be discussed later.
Five species, the Golden Eagle, Great Horned
Owl, Ferruginous Hawk, Red-tailed Hawk and
Raven comprised over 81 percent of the average
vearlv raptor populations. Of these, the Fernigi-
nous Hawk was consistently the numerically
dominant raptor, averaging approximatel\' 25
percent of the annual breeding population. The
next most numerous species were, in order of
their abundance, the Great Homed Owl (which
approximated over 19 percent). Red-tailed
Hawk, Golden Eagle, and Raven. Of the re-
maining raptors. Sparrow Hawks were almost
twice as abundant as Swainson's Hawks, Marsh
Hawks, and Burrowing Owls, while the Cooper's
Hawk and Short-eared Owl were relatively rare
breeding elements. Although a conspicuous
pemianent resident, the Prairie Falcon rarely
achieved breeding status and comprised less
than t\\'0 percent of the average yearly breed-
ing population. The relative percent composition
of the large raptors varied only slightly and
each species maintained its proportional abun-
dance during the four study years. Thus the
population increase from 1967 to 1969 reflected
a similar increase in the number of pairs of
each, with the notable exception of the Raven
population, whicli remained stal)le. The limited
populations of the smaller raptors prevent clear-
cut evaluations. Both the Marsh Hawk and Bur-
rowing Owl populations became established dur-
ing the last two study years, but the Sparrow
Hawk population declined.
Yearly population densities averaged 0.5 pairs
per square mile (range 0.4-0.58), based on the
80-square-mile study area. However, approxi-
mately one-half of the area was apparently not
utilized for any purposes by the nesting rap-
tors. This was particularly true of the lower
\'alley elevations which were situated far from
potential nesting sites. If this area were elimi-
nated from the determinations, then the raptor
nesting densities would be increased to 1.0 pairs
per square mile (range 0.8-1.16).
Seasonal Activity Timetables
Winter Populations. Central Utah supports a
large and varied winter raptor population. Im-
portant permanent year-round residents winter-
ing in the area include Golden Eagles, Ravens,
Great Homed Owls, and Prairie Falcons. Gold-
en Eagles and Ravens occur singly or in small
groups of two to five individuals. Some Golden
Eagles may form hunting contacts and share
communal roosts with Bald Eagles {Haliaetus
leucocephahis). Estimated average yearly win-
ter populations of each were 13 Golden Eagles
and 9 Ravens. In contrast. Great Horned Owls
and Prairie Falcons were less common. A few
Great Homed Owls were flushed in the vicinity
of their nesting site of the previous year and a
single Prairie Falcon was obsei-ved every year,
occupying a large winter territory in Cedar Val-
ley. It was occasionally obser\'ed hunting among
flocks of Homed Larks and Dickcissels (Spiza
americana).
Large influxes of Bald Eagles and Rough-
legged Hawks {Buteo lagopus) began arriving
in the valleys in late November and December.
These conspicuous winter residents rosted com-
10
Biur.iiAM YouNC Uni\ i-.nsirv Scmknc:!-. Bi'i.i.etin
munallv in canyons and lightlv wooded areas
near settlements. Dnriiig the daylight hours the\'
ranged widely to hunt in the \allevs, returning
to a communal roost shortly before dark ( Ed-
wards, 1969). Estimated populations of each in
the study area were 30 Bald Eagles and 18
Rough-legged Hawks.
Winter live trapping studies revealed 5 Long-
eared Owls ( Asio ottis ) , and a number of Short-
eared Owls. The latter were frequently observed
(up to 8 individuals per group) ranging out-
ward from their diurnal communal roosting
sites during the late evening hours.
An average of 25 Marsh Hawks, 2 Shai^p-
shinned Hawks (Acripitcr striatus), 3 Red-tailed
Hawks, 1 Ferruginous Hawk, and 1 Screech Owl
(Ottis asio) were present in the \'alleys during
the winter months. The Marsh Hawk popula-
tions indicated a major influx of this species into
the area during the winter, but the status of the
wintering Red-tailed Hawks and Ferruginous
Hawks was uncertain. Two of tlie Red-tailed
Hawks wintered in the yieinit\' of a previously
used Red-tailed I lawk nesting site and ma\ have
been permanent residents.
The populations of these winter residents
fluctuated and appeared to be related to climatic
changes, particularly temperature. Their num-
bers declined sharply in late JanuaiT and earl\'
February, and they left the area by mid-March,
a transition coinciding with the arrival and
rapid buildup of the breeding populations.
Transients. Known transients, including Red-
tailed, Swainson's, and Cooper's Hawks were ob-
served from late Februan" to carK' Maw Large
numbers of transient Sparrow Hawks were ob-
served between early April and mid-Ma\-, simul-
taneously with the arri\al of tlie breetliiiu
population of Sparrow Hawks. A single Osprev
{Pdiuliiin liali(ictus) was observed roosting in a
dead cottonwood in Cedar Valley on 29 April
in the late e\-ening and presumabh' roosted
overnight. The niajorit\' of the transients re-
mained onK one or two da\s in the area, par-
ticularh' those observed later in the breeding
season.
Activitij timetables. The \cdv\v aeti\'it\- tiTne-
tables of the raptor populations are presented
in Tables .5-8. The breeding activities of the
populations occurred over a period of eight
months and avi'raged 202.7 da\s a year (range
163-22S da\s). Ho\\e\er. the in(li\idual species
activities occupied only a portion of this period.
.\lthough slight yearly variations in the timing
and duration of the events of the nesting c\cle
were evident, the chronological sequene(> of
each raptor species reniaincxl essentialh un-
changed with respect to the total raptor popu-
lations.
Golden Eagles and Great Horned Owls were
the first raptors to initiate their nesting activity.
Golden Eagles were observed occupying their
territories as early as 20 Januars', and courtship
displa\s were observed from this time onward.
Their nests were constnicted or rebuilt in Febru-
ary and early March and decorated with green-
ery. A Great Horned Owl was recorded on its
nest site of the previous year on 2 December
and pair fonnation had occurred as early as 10
January in some years. Average egg deposition
dates for both species ranged from mid-February
to earl\' March, with Golden Eagles generally
preceding Great Honied Owls b\- one or two
weeks.
Red-tailed and Fenaiginous Hawks were the
first of the migrator\- raptors to arri\'e in the
study area each year. The first Red-tailed Hawks
were observed in the vicinit\' of previous nesting
sites during the first week in Febniar)' and were
paired within one or two weeks, .^t this time
pairs would react aggressively when the nest
site was approached, screaming and soaring in
increasingly higher circles overhead. Onl\' three
pairs were observed constructing nests, but the
process was a mutual activit\', with both mem-
bers of a pair transporting juniper branches to
the nest site. Eggs were usually deposited in
late March and earlv April. Tlu' first Ferrugi-
nous Hawks were obsened from two to five
weeks later, usually during the first week in
March but as earl\ as 25 February. Eggs were
usualK deposited in mid-.\pril. As with Red-
tailed Hawks, nests were constructed rapidly
In- both members of a pair until finished, usual-
K within one to three da\s. Both species were
higliK secretive during nest eonstniction and
if intirrupted would fre(iuentl\' stop building
activities and begin another nest at a new site.
FiMruginous Hawks exhibited a greater tenden-
e\ to abandon newly constructed nests ( 12 oc-
eurrenc(\s) than Red-tailed Hawks (5 occur-
rences ) .
Swainson's Hawks were the last of the Buteos
to nest, appearing in the- \alle\s in earlx and
inid-.\pril and beginning their nesting between
two and three weeks later.
Of the medium and small sized raptors, the
Ra\-ens were the first to begin nesting, usually
from late Februarv- to mid-Mareh. Fairs of Prai-
rie Falcons and Marsh Hawks were observed
in late March and early April. The Prairie Fal-
cons were \er\ aggressive at this time both
toward humans and other raptors, particularly
(ireat Horned (a\]s. which if flusliefi were at-
Biological Stiuii.s, \'ol. KS, \i
Biu:i;i)iNo Kcoi.oGV ok Utah IlAnoiw
11
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Biological Sf.hiks. Vol. IS, No. 3 Bkeedino Ecology oi' Ut.mi Uai'toiis
13
tacked, although no actual contacts were ob-
served. The 1969 egg deposition dates of the
Marsh Hawk were computed, using the results
from the 1970 data for this species. Individual
Short-eared Owls were observed in the vicinity
of their nesting territon' in the first week in
March, and activit)' dates computed from the
data of Bent (1938) and Craighead and Craig-
head ( 1956 ) indicate that egg deposition oc-
curred within three weeks. Sparrow Hawks
were observed as early as 10 April, perched on
conspicuous locations in the vicinity of their
future nesting sites. Pair bonding had occurred
by 27 April and egg deposition from two to
three weeks later. By late April Burrowing Owls
were seen roosting beside the entrance to their
nest holes and protested vigorously when in-
vestigated. Their activity' timetables were com-
puted from the date of fledging on the basis
of data given by Bent (1938).
Only egg dates are available for the Cooper's
Hawk, but backdating 31 days (average from
Craighead and Craighead, 1956) suggests that
in this area their territories are selected by mid-
April.
The breeding raptor populations were well
established by April and Mav, which were the
months of ma.\inium activity. By late May and
early June nests of the Great Horned Owl were
terminated with the fledging of the voung. By
the end of June and the first week of July,
Red-tailed Hawks, Ferruginous Hawks, Golden
Eagles, Ravens, Prairie Falcons, and Marsh
Hawks had all completed their nesring activities,
and Swainson's Hawks, Burrowdng Owls, and
Sparrow Hawks had finished their nesting ef-
forts bv late July and earlv August.
The newly fledged young of most species
remained within the nesting tcnitor\- for a period
after fledging and were frequently seen in fam-
ily hunting groups. Defense of the young by
adults was particularly strong during this time
period but gradually lessened. Within three to
five weeks the young had drifted out of the
nesting area and into other parts of the valley.
The migratory species began moving out of
the area in late August and early September.
Their replacement by the first elements of the
wintering population was not as sudden as the
spring transition, and the interim raptor popu-
lations consisted only of pemianent residents
which were consequently comparatively low in
number.
Nest Site Requirements
Spatial Disirihution. Figures 4-7 show the
\early distribution of raptor nests (all species)
on the study area and clearly indicate that the
nests were unevenly distributed. The majority
of sites were present at middle and higher ele-
vations and consistently distributed along the
periphery of the central mountains or within the
woodland. Only Burrowing Owl, Marsh Hawk,
and Fenuginous Hawk (one nest) nest sites
were present in the valleys, below the fringes
of the Pinyon-Juniper woodland.
Nest Site. The nest site selections of the 12
raptor species are summarized in Table 9. The
raptors nesting on the study area utilized a wide
variety of sites, but some species exhibited a
narrower range of selection than others. Actual
sites chosen by one or more species included
cliffs, quarries, abandoned mining structures,
trees, burrows, or the ground.
Almost 35 percent of the nesting sites se-
lected were located in cliffs. The choice of cliff
sites by five of the raptor species appears to be
related to several factors, including the physiog-
raphy of the cliff, its vertical height, aspect,
position, altitude, and height above the valley
floor. Excluding the rock walls of quarries, which
are actually artificial structures, the maximum
height of cliffs within the study area did not
exceed 150 feet, and the great majority averaged
less than 50 feet. Two distinct types, sandstone
and limestone, are present. Limestone cliffs,
because of their distinctive weathering patterns
which result in numerous crevices and ledges,
provided greater numbers of suitable nesting
sites and were heavilv utilized bv the raptors.
The position of the cliff refers to its remoteness.
Cliff sites which overlooked the valleys were
preferred over similar cliffs located in the in-
terior of the hills. Sites were frequently chosen
in the first large cliff (over 20 feet high) above
the valley floor. This was particularly evident in
locations where several cliff lines were available
at increasingly higher elevations in stairstep
fashion.
Several abandoned quarries within the study
area were utilized for nesting sites by at least
six of the raptor species. The amount of use
was related to the size and ruggedness of the
quarr\- walls and was apparently independent
of the amount of human disturbance. The larg-
est quarries were utilized simultaneously by
two or three raptor species ever\' year.
Trees were also a common nesting site (34.6
percent) on the study area. The; majorit)' were
located in junipers, the predominant tiees in the
area, but a few were constmcted in pinyon,
cliffrose, and cottonwood. Nests in jimipers and
cliffrose were most frequently constructed in
the tops of the trees, approximately 11 feet
14
BiuGiiAM Young University ScitNCE Bulletin
1
2
3
4
5
6
7
8
9
10
11
12
\_J nesting pairs
I I non-nesting pairs
/\ individuals
Golden Eagle
Great Horned Owl
Ferruginous Hawk
Red-tailed Hawk
Swainson's Hawk
Prairie Falcon
Marsh Hawk
Cooper's Hawk
Sparrow Hawk
Short-eared Owl
Burrowing Owl
Raven
Fig. 4. Distribution of the raptor breeding population in 1967.
Biological Series, \'ni, 18. No. 3 Bueeding Ecology of Ut..\h H.m'iohs
15
1 Golden Eagle
2 Great Horned Owl
3 Ferruginous Hawk
4 Red-tailed Hawk
5 Swainson's Hawk
6 Prairie Falcon
7 Marsh Hawk
8 Cooper's Hawk
9 Sparrow Hawk
10 Short-eared Owl
11 Burrowing Owl
12 Raven
\_) nesting pairs
I I non-nesting pairs
/\ individuals
Fig. 5. Distrihution of the raptor breeding populatinn in 1968.
16
Bnir.HAM Young Univfksity Science Bulletin
®
1 Golden Eagle
2 Great Horned Owl
3 Ferruginous Hawk
4 Red-tailed Hawk
5 Swainson's Hawk
6 Prairie Falcon
7 Marsh Hawk
8 Cooper's Hawk
9 Sparrow Hawk
10 Short-eared Owl
11 Burrowing Owl
12 Raven
\^ nesting pairs
I I non-nesting pairs
/\ individuals
Fig. 6. Dislritiiitimi of the raptor breeding population in 1969.
Biological Sehils, \'ol. 18, No.
Bueedinc Ecology of Utah Uaptoiis
17
r.
1 Golden Eagle
2 Great Horned Owl
3 Ferruginous Hawk
4 Red-tailed Hawk
5 Swainson's Hawk
6 Prairie Falcon
7 Marsh Hawk
8 Cooper's Hawk
9 Sparrow Hawk
10 Short-eared Owl
11 Burrowing Owl
12 Raven
\_J nesting pairs
I I non-nesting pairs
/\ Individuals
Fig. 7. Distrihufion of the niptor breeding population in 1970.
18
BiuciiAM YnvNc Un'ivkhsity .St:iEVf:E Bulletin
Table 9. Summary of nesting site selections of raptors on the study area, 1967-1970.
Quarrv
Site'
Structure
Site
Tree
Site
Pinyon
Juniper
Cliffrose
Cottonwood
Species
No.
%
No.
%
No.
•I
\n.
%
No.
%
No.
%
Colden Eagle
4
2.8
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
Great Horned Owl
7
5.0
0
0.0
0
0,0
4
2.8
0
0.0
0
0.0
Ferruginous Hawk
0
0.0
0
0.0
0
0.0
24
17.0
1
0.7
0
0.0
Ked-tailed I lawk
•2,
1.4
0
0.(1
.!
2.1
7
.5.0
1
0.0
1
0.7
Swainson's Hawk
(1
0.0
0
0 0
0
0.0
5
3.5
0
0.0
0
0.0
Prairie Falcon
1
0.7
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
Marsh Hawk
0
0.0
0
0.0
0
0,0
0
0.0
0
0.0
0
0.0
Cooper's Hawk
0
0.0
0
0.0
0
0,0
1
0.7
0
0.0
0
0.0
Sparrow Hawk
5
3.5
2
1.4
0
0.0
O
1.4
0
0.0
0
0.0
Short-eared Owl
0
0.0
0
0.0
0
(1,0
0
0.0
0
0.0
0
0.0
Burrowing Owl
0
0.0
(1
0.0
(1
(1,0
(1
0.0
0
0.0
0
00
Haven
1
0.7
0
DO
0
0,(1
0
0.0
0
0.0
0
0.0
Totals
20
14.1
2
1.4
3
2.1
43
30.4
0
0.7
1
0.7
Ciround Site
chlf
Site
Sagebi
■ush
Shadscale
Greasewood
5-25
25-75
75-150
Species
No
%
No.
%
No.
%
No.
%
No.
3
No.
%
Colden Eagle
0
0.0
0
0.0
0
0.0
0
0.0
9
6.4
1
0.7
Great Horned Owl
0
0.0
0
0.0
0
0.0
3
2.1
13
9.2
0
0.0
Ferruginous Hawk
s
5.7
3
2.1
0
0.(1
0
0.0
0
0.0
0
0.0
Red-tailed Hawk
0
0.0
0
0.(1
0
0.0
-T
1.4
5
3.5
i
0.7
Swaiiisoo's Hawk
0
0.0
0
0,(1
0
0.(1
0
0.0
0
0.0
0
0.0
Prairie Falcon
0
0.0
0
0.(i
0
0,(1
(1
0.0
0
1.4
0
0.0
Marsh Hawk
2
1.4
2
1.4
0
0.0
0
0.0
0
0.0
0
0.0
Cooper's H;iwk
0
0.0
0
0,0
0
0.0
0
0.0
0
0.0
0
0.0
Sparrow Hawk
0
0.0
(1
0,0
0
0.0
0
0.0
0
0.0
0
0.0
Short-cared Owl
1
0.7
0
0.0
0
(1,(1
0
0.0
0
0.0
0
0.0
Burrowing Owl
0
0.0
1
0.7
5
3.5
0
0.0
0
0.0
0
0.0
Haven
0
0.0
0
0.0
0
0.0
3
2.1
7
5.0
3
2.1
Totals
11
7.8
6
4.2
5
3.5
8
5.6
36
25.5
5
3.5
above ground, which is the average height of
the pigmy woodland trees of this area.
The majority of the nests had western ex-
posures ( 33 percent ) , but 27 percent faced
south and 25 percent east, while only 15 percent
faced north. Tree nest exposure, determined b}'
the inclination of the slope, is included in the
above (sec Table 10). With reference to alti-
tude, 25 percent of the nests were situated be-
tween 48(X)-5200 feet, 63 percent between 5200-
.5800 feel and II percent l)et\\een 5800-6400
feet. The data of Table 11 indicate that several
of the raptor species exhibited a vertical strati-
fication of nesting sites.
Nests of the Golden Eagle were built on
cliffs, rock outcroppings, and in (|uarries. None
were constructed in trees, but ground nests and
artificial structures were utilized in areas im-
mediatelv adjacent to the stud\' area. Occupied
e\ries averaged 5690 ±: 62.0 feet (range 5380-
6170 feet). No apparent exposure preference
was exhibited. All pairs maintained from one to
I'.ililr 1(1. .Suiniii.irv of exposures of occupiod nests, I9'iT- 1^)7(1.
North West
South
East
Species No. % No. %
No. %
No.
%
Golden Eagle
C»reat Horned Owl
Ferruginous Hawk
Red-tailed Hawk
Swainson's Hawk
Prairie Falcon
Marsh Hawk
Gooper's Hawk
Sparrow Ihiwk
Short-eared Owl
Burrowing Owl
Raven
Totals
4
1
3
4
0
1
0
0
4
0
0
4
21
2.8
0.7
2.1
2.8
0.0
0.7
0.0
0.0
2.8
0.0
0.0
2.8
14.7
4
15
10
6
0
2
0
1
1
0
0
8
47
2.8
106
7.1
4.3
0.0
1.1
0.0
0.7
0.7
0.0
0.0
5.7
33.3
3
8
15
6
1
0
0
0
3
0
0
2
38
2.1
.5.7
10.6
4.3
0.7
0.0
0.0
0.0
2.1
0.0
0.0
1.4
26.9
3
2.1
3
2.1
8
5.7
5
3.5
4
2.8
0
0.0
4
2.8
0
0.0
1
0.7
1
0.7
6
4.3
0
0.0
35
24.7
Bioi.or.K At. Sfkiks, \
'OL.
18. No,
. :^
BMiiiiniNc 1'
^COl.OG^
;■ (IF
Ut..\h
Raftohs
19
Table 11. Summary
of ;
iiltitudinal distribution of
raptor
nests, 1967-1970.
4800
5000
5200
5400
5600
5800
6000
6200
5000
5200
5400
5600
5800
6000
6200
6400
Species
No.
. %
No.
%
No.
%
No.
%
No.
%
No.
%
No.
%
No.
%
Golden Eagle
0
0.0
0
0.0
1
0.7
4
2.8
6
4.3
0
0.0
3
2.1
0
0.0
Great Homed Owl
0
0.0
0
0.0
5
4.0
9
6.4
10
7.0
1
0.7
0
0.0
2
0.1
Ferruginous Hawk
1
0.7
8
5.7
17
12.1
16
11.3
0
0.0
0
0.0
0
0.0
0
0.0
Red-tailed Hawk
1
0.7
2
0.1
10
7.0
5
4.0
0
0.0
3
2.1
0
0.0
0
o.n
Swainson's Hawk
0
0.0
4
2.8
1
0.7
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
Prairie Falcon
0
0.0
0
0.0
1
0.7
0
0.0
2
0.1
0
0.0
0
0.0
0
0.0
Marsh Hawk
4
2.8
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
Cooper's Hawk
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
1
0.7
0
0.0
0
0.0
Sparrow Hawk
0
0.0
0
0.0
6
4.3
0
0.0
3
2.1
0
0.0
0
0.0
0
0.0
Short-eared Owl
1
0.7
0
0.0
0
0.0
0
0.0
0
0.0
0
0.(1
0
0,0
0
0.0
Burrowing Oul
6
4.3
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
0
0.0
Raven
0
0.0
0
0.0
0
0.0
3
2.1
1
0.7
1
0.7
7
5.0
2
0.1
Totals
13
9.2
14
8.6
41
29.5
37
26.6
22
14.2
6
4.2
10
7.1
4
0.2
five alternate nests, and one or more of tliese
would also be decorated at the onset of the
breeding season.
Great Horned Owls selected chffs, trees, and
quarries for breeding sites. Quarries were a fre-
quently utilized site (almost 26 percent of all
Great Homed Owl nests were in quarries), and
each year at least one pair nested in the niches,
ledges, or cracks of an abandoned quarry. None
of the pairs showed any attempt at nest con-
struction but instead occupied old nests of
Ravens, Red-tailed Hawks, Ferruginous Hawks,
or deposited the eggs directly on the dirt or rock
floor of a crevice or ledge. Tree nests were found
only in junipers within the study area, but the
owls did use old Rod-tailed Hawk nests situated
in tall cottonwoods in canyons located outside
and to the north of the study area. Nests aver-
aged 5640 ± 5.3.7 feet (range 5340-6320 feet)
in altitude. Over 55 percent of the nests faced
west and almost 30 percent had southern ex-
posures, while less than 1 percent faced north.
Nests were selected in cliffs wliich ranged from
21 to 65 feet in height, but sheer size of cliff
appeared to be less important than seclusion,
and crevices were more frequently occupied
than ledges.
Ferruginous Hawks were selective in their
choice of nesting sites. Nests were constructed in
junipers, cliffrose, on low ledges ( less than five
feet high) or directlv on the groimd (Fig. 8).
The most common nesting site was in a low tree
or shrub, either on the peripher\- of the wood-
land or in ver\' lightK' wooded areas of the foot-
hills. The average altitude of all Ferruginous
Hawk nests was 5290 ± 2.5 feet (range 4990-
5500 feet). Low foothills and knolls appeared to
offer the best sit(>s and were heavily utilized. In
contrast, no nests were located in steep-sided
canyons, cliffs, or heavily wooded areas, al-
though such sites were equally available in these
same localities.
Red-tailed Hawks exhibited a wide choice of
nesting sites somewhat paralleling that of the
Great Horned Owl. Their most common nest
sites were in junipers, but other localities in-
cluded cliffs, quarries, pinyons, and cottonwoods
(Fig. 9). Nests averaged 5380 ± 52.4 feet, but
had a wide altitudinal amplitude (range 4880-
5880 feet). Unlike Ferruginous Hawks, Red-
tailed Hawks constructed their nests in a variety
of habitats. Tree nests were most commonh'
built on the periphery of the woodland or in
lightly wooded areas but a few were also con-
structed in the center of dense woodlands and
in steep-wallcd canyons. Cliff sites were usually
in large rugged cliff lines but again some varia-
tion occurred and some nests were consti-ucted
on cliffs only 10-15 feet high. Red-tailed Hawks
were frequently usurped from their nesting sites
by the earlier nesting Great Horned Owls; they
then chose secondary, more exposed nesting
sites a short distance away.
The choice of nesting sites by the Swainson's
Hawks showed considerable overlap with Fer-
ruginous Hawks. Their nests were without ex-
ception constructed in low junipers and averaged
5130 ± 30.4 feet in elevation (range 5080-
5240 feet). As with Ferruginous Hawks, their
most common nesting site was on a low foothill
or knoll or at the edge of a juniper woodland.
Nesting sites of the Prairie Falcon averaged
5.590 ±: 88.3 feet (range .5.380-5760 feet). Of the
three nests on the study area, two were located
in (luarries and one in a limestone cliff crevice.
One quarry site was also located in a crevice
but the second was located in an unused Gold-
en Eagle nest. Heights of the nests above the
cliff base ranged from 13-78 feet. In 1970 a pair
20
Bricham Young University Science Bulletin
Fig. 8. Ferruginous Hawk ground nest in central Cedar Valley-
hatched egg. May, 1968.
Till' nest contains two chicks and one un-
Fig. 9. Hed-tailed H:nvk nest in juniper tree, Skull
Vallev. Tooele Co.. I'tah. Two vouiig visible al
top of tiest. May 1972.
of Prairie Falcons prevented a pair of Great
Homed Owls from successfully completing their
nesting attempt and then took over the aban-
doned nest site ( Fig. 10 ) .
The four Marsh Hawk nests were situated
in Cedar Valley and averaged 4930 ± 27.6 feet
in elevation (range 4870-4990 feet). All nests
were located in thick sag(>bmsh and rabbitbrush.
Although all were ground nests, their location
within the extensive sagebrush growth rendered
them relatively inaccessible.
Tlic only nesting of the Cooper's Hawk on
the study area was in a juniper at an elevation
of 6020 feet. The site was located deep within
a dense juniper stand atop a ridge between two
adjacent peaks, and overlooked Rush Valley.
The nest was small and hidden within the mid-
dle branches of the tree.
Sparrow Hawks nested in junipers, quarries
and abandoned mining structures. Nests aver-
aged 5460 • 49.7 feet in elevation (range 5.350-
5670 fe(!t). Quarr)' sites were actually small
crevices in the \-ertical walls which ranged from
<S-32 feet abo\'c the (juany floor. The scrape of
these nests was most often simply a hollowed
out portion of the dirt floor. Both tree nests
w(>re sitiiatetl in small crevices within the tree
tmnks. Both types of nesting sites were also used
BioLcx;icAL Seiues, \'()l. 18, No. 3 Bheeuing Ecology of Utah IUptoks
21
Fig. 10. Cliff nesting site of Prairir Falcons and Great Homed Oivls in the western Thorpe Hills.
l)V Starlings (Stunii.s vulgaris) nesting in the
same localities.
The onh' Short-eared Owl nest on the study
area was located at an elevation of 4S90 feet.
The nest site was placed at the base of a large
clump of sagebmsh and was partially sheltered
and hidden b\' its branches. A few twigs had
been arranged on the nest floor and down was
placed among them; otherwise, no nest con-
struction was attempted.
Nests of the Burrowing Owl averaged 4920
± 1.6 feet in elevation (range 4920-49.30 feet).
The three nests of the 1969 season and two of
the 1970 season were grouped together, fomiing
small colonies which were located in a stand of
grea.sewood, in dry sand and soil ( Fisj. 11).
The remaining nest was located in the bank of
a dr)' reservoir. All were within unused burrows
of kit foxes, badgers, or Townsend's ground
squirrels.
With feu' exceptions Raven nests were lo-
cated in the most remote, inaccessible regions
of the study area. Their average elevation was
5950 *- 65.5 feet (range 5590-6;32() feet). All
were well constructed, compact, and set far
back into a protective crevice. All had an over-
hanging ledge or rockshelf which prevented
direct exposure of the nest (Fig. 12).
Reoccupation of Nests and Nesting Localities.
Most of the regularly nesting raptor species
showed a strong tendency to reoccupv their ter-
ritories and often their exact nesting sites of the
previous year. This was particularly true of
crevice-nesting raptors, and it is probable that
these partially protected sites are used for an
indefinite number of breeding seasons. Table 12
summarizes the reoccupation data. Unfortunately
it was not possible to mark individuals, hence
it is impossible to detemiine if the same pairs
were present each vear. However, many pairs
and individuals of pairs exhibited distinctive
color or plumage patterns and behavioral char-
acteristics and could be identified on this basis.
Most of the large raptors selected different
nest sites within the same territory each vear.
This was particularly true of the Fermginous
Hawk which selected a different nest site 75
percent of the time, but also remained within
the same locality for suc-eessive years 77 percent
of the time. Similarly, pairs of Golden Eagles,
Great Homed Owls, Red-tailed Hawks, and
Svvainson's Hawks showed strong attachments to
22
Hkigiiam Young Univeksity Sciknce Bulletin
, , «««C*»/.
'»
^%^.
■4i
» ■-*'
'»•„♦
Fig. 11. Burrowing Ov
moiincl.
nesting site in northeastern Cedar Valley, July 1970. Both adults are on the
a particular area and were often found there
even during years in which tliey did not nest.
Long term consecutive occupation of a nest site
was more rare. One pair each of Great Homed
Owls (nesting in a cliff site) and Ferruginous
Hawks (nesting in a tree site) occupied their
same respective nest sites for all four vears of this
study. Another Great Horned Old pair liad oc-
cupied their nest site for the fourth consecutive
year but were displaced by a Prairie Falcon pair.
Several pairs of Golden Eagles, Great Homed
Owls, Fcrrusinous Hawks, and Red-tailed Hawks
reoccupied the same nesting site for three con-
secutive years, and every large raptor occupied
at least one nesting site for two consecutive
years. Most commonh-, those species which
nested in a different site selected a new site
veiy near that of the previous Near. For example,
a pair of Golden Eagles selected three sites in
the same (juarr\- for three a>nsecutive vears,
each but 3() feet from the previous years site.
The same phiMiomenon was observed in Fer-
ruginous, Ri'd-tailed, and Swainson's Hawks.
The amount of shifting appeared to be related
to the dei^ri'c of disturbance as well as the
success of the pre\'ious year's nest, but pairs
would often tolerate considerable disturbance
and ri'main within the same nesting localitv.
Of the medimn and small raptors, thi' Raven
showed the greatest population stabilitv'. The
Fig. 12. Raven nest located in \v<'ll-[>rotected crevice.
Biological Sehies, \'ol. 18, No. 3 BiiEiiiiiNC Ecology of Utah IIaptohs
23
Tablf 12. Siimman,' of reoccupation of nesting sites and territories.
No. years occupation of a
L nest site
No.
years
territorial occupatior
[•
I
2
3
4
1
2
3
4 Total no.
Species
No.
%
No.
%
No.
%
No.
%
No.
%
No.
%
No.
%
No.
% of
sites
Golden Eagle
5
55.6
.7
22.3
2
22.2
0
0.0
0
0.0
0
0.0
2
40.0
3
60.0
9
Great Horned Owl
6
40.0
7
46.7
1
6.7
1
6.7
0
0.0
4
400
3
30.0
3
30.0
15
Ferruginons Hawk
18
75.0
2
8.3
3
12.5
1
4.2
1
1 . 1
0
1,5.4
4
30.S
6
46.2
24
Red-tailed H.iuk
8
57.1
5
35.7
1
7.1
0
0.0
0
0.0
1
14.3
1
14.3
5
71.4
14
Swainson'-. Hawk
1
.33..3
■T
68.7
0
0.0
0
0.0
1
50.0
0
0.0
0
0.0
1
.50.0
3
Prairie Falcon
3
1(10.0
0
0.0
(1
0.0
0
0.(1
1
.33.0
2
67.0
0
0.0
0
0.0
3
Marsh Hawk
5
1 00.0
(1
0.0
0
0.0
0
oo
1
1 00.0
2
67.0
0
0.0
0
0.0
5
Cooper's Hawk
1
100.0
0
0.0
0
0.0
n
0,0
1
lOOO
0
0(1
0
0.0
0
0.0
1
Sparrow Hawk
4
66.7
1
16.7
1
16.7
0
0,0
0
0.0
1
25 0
3
75.0
0
0.0
6
Short-cared Owl
I
100.0
0
0.0
0
0.0
0
0 (1
1
100.0
0
0.0
0
0-0
0
0.0
1
Burrowing Owl
6
UHi.O
(1
0,0
0
0.0
0
0,(1
2
50.0
2
.50.0
0
0.0
(1
0,0
6
Raven
0
33.3
1
16.7
2
33.3
1
16,7
0
0.0
0
0.0
0
0.0
4
100.0
6
Totals
60
71.75
20
17.9
10
8.2
3
2.3
8
36.7
14
23.2
13
15.8
22
29.7
93
'Tulais iniluilo nc:>tiTig and nonnesting pans
four pairs of Ravens on the stuch' area occupied
their respecti\e territories for four consecutive
years and selected but six different nesting sites.
Sparrow Hawks also tended to reoccupv the
same territories, but their fluctuating popula-
tions altered their reoccupation frequencies.
None of the Burrowing Owl or Marsh Hawk
pairs reoccupied their exact nesting sites of the
pre\ious \ ear, but all returned and nested with-
in the same locality. The Prairie Falcons chose
three different sites in three different nesting at-
tempts, two of which were located within the
same torriton'.
Productivitv
Clutch Size. The summan' of clutch size fre-
quencies from 1967-1970 is presented in Table
13. Golden Eagle clutches on the study area
averaged 2.07 ± 0.07 eggs ( 14 clutches, range
2-3). Differences between the mean clutch size
of each of tlie four study years was not signifi-
cant. Total fecundit)- averaged 6.75 ± 0.96
eggs a year.
Great Homed Owl clutches averaged 2.82
± 0.15 eggs (22 clutches, range 1-4). Clutches
of 1968 and 1969 were significantly larger than
clutches of 1967 and 1970 (t--= 2.53; 2.63, re-
spectively) but not significantly different from
one another (t= 1.26). In addition, clutches of
1967-1970 were also not significantly different
(t= 1.15). Total vearh' fecundit)- averaged
15.5 ± 3.3 eggs.
Clutches of the Fenuginous Hawks aver-
aged 3.23 ±: 0.12 eggs (34 clutches, range 2-4).
Clutches of 1968 and 1969 were significantly
larger than clutches of 1967 and 1970 (t= 2.56;
2.75, respectively) but not significantly different
from one another (t= 0.05). Again, clutches of
1967 and 1970 were not significantly different
(t= 1.35). Total yearly fecundity- averaged 28.3
± 5.6 eggs.
Red-tailed Hawk clutches averaged 2.89 ±
0.13 eggs ( 19 clutches, range 2-4). Although
clutch size showed an increasing trend through-
out the tour study \ears, none of the possible
differences betwen yearh' clutch sizes was sig-
nificant. Total yearly productivity averaged 13.8
± 1.43 eggs a year.
Table 1.3. Summar)' of frequency distribution of raptor tlutch sizes from 1967-1970.
No.
eggs in
clutch
Species
1
3
3
4
5
6
7
Golden Eagle
0
13
1
0
0
0
0
Great Horned Owl
1
5
13
3
0
0
0
Ferruginous Hawk
0
5
13
16
0
0
0
Red-tailed Hauk
0
4
13
2
0
0
0
Swainson's Hawk
0
-1
1
0
0
0
0
Prairie Falcon
0
0
0
0
1
0
0
Marsh Hauk
()
0
1
0
0
0
1
Cooper's Hawk
0
0
1
0
0
0
0
Sparrow Hawk
0
0
0
3
3
1
2
Short-eared Owl
0
0
0
0
0
0
1
Burrowing Owl
?
?
?
?
?
p
p
Raven
0
0
1
3
4
2
4
Totals
1
31
44
27
8
3
9
24
BiiK.iivM YouNC Univihshv Sciknck Buli.ktin
Clutches of the Svvainson's Hawk averaged
2.2 ± 0.17 eggs (.5 clutches, range 2-3). There
were no significant variations in clutch size be-
tween any of the foin- study years. Total yearly
fecundity averaged 2.7.5 ± 0.6 eggs, rating low-
est of the large raptors on the study area.
(Comparisons of the average clutch sizes of
the large raptors indicate that the mean clutch
size of Ferruginous Hawks was significantly
larger than the Golden Eagle (t= 8.23), Great
Horned Owl (t= 2.11), and Swainson's Hawk
(t= 4.76) average clutches but did not differ
significantly from average Red-tailed Hawk
clutch size (t= 1.01). Red-tailed Hawk clutches
averaged significantly larger tlum those of Gold-
en Eagle (t— .5.72) and Swainson's Hawk
(t= 3.2) but did not differ significantly from
Ferniginous Hawk or Great Homed Owl (t =
4.47 for both) and Swainson's Hawk clutches
(t=2.63). Golden Eagle and Swainson's Hawk
clutches did not differ significantly from one
another (t= 0.678).
Of the smaller raptors, onlv Sparrow Hawks,
Marsh Hawks, and Ravens had sufficient clutch
size data for analysis.
Sparrow Hawk clutches averaged 5.22 ±
0.38 eggs ( 9 clutches, range 4-7 ) . No significant
differ<>nces between \earl\' clutch sizes were
found. Total yearly productivity averaged 10.0
± 2.18 eggs.
Clutches of the Marsh Hawk averaged 5.0
±1.4 eggs (2 clutches, range 3-7). No compari-
sons were possible.
Raven clutches on the study area averaged
5.35 ± 0.,34 eggs ( 14 clutches, range 3-7). There
were no significant differences between yearly
clutch size. Total productivity averaged 18.8
± 1.9 eggs.
No significant differences were found be-
tween th(> average clutch sizes of the Marsh
Hawk, Sparrow Hawk, and Raven but all were
significantly larger than the clutches of the
large raptors on th(> study area.
Ilatchahilitij. In 1967 the ov(>rall hatching
success of the efforts of all nesting raptors on
the study area was 82.5 ± 7.6 percent, the high-
(>st of the foiu- study years. In 1968 the overall
hatching success was 77.4 ± 5.7 percent, but in
contrast the lowest hatching success occurred
during the 1969 season (75.6 ± 9.2 percent).
In 1970 the overall hatching success was slightly
higher at 82.0 ' 4.7 percent. There were no
significant variations in yearly overall hatching
success between any of the four study years.
The overall hatching success of the five large
raptor species when calculated separately
showed no significant differences between years.
with the hatching percentages being as follows:
1967, 84.7 ± 8.7 percent; 1968, 75.9 ± 7.6
percent; 1969, 76.7 ± 10.24 percent; 1970, 84.2
± 7.1 percent.
From 1967-1970 Golden Eagle nesting ef-
forts hatched 70.8 it 14.9 percent of all eggs for
an average of 1.2 young per nest per year. How-
ever, the breeding seasons of 1967 and 1970
were highly successful, hatching 100 percent of
all eggs produced for an average of 2.0 young
per nest; whereas the combined results of 1968
and 1969 revealed a two-year hatching success
of less than 42 percent and an average of but
0.88 young per nest.
The average hatching success of Great
Horned Owls from 1967-1970 was 89.4 ± 3.6
percent for an average of 2.5 young per nest
per year. Great Horned Owl hatching efforts
were most successful in 1967 ( 100 percent
hatched, average of 2.0 young per nest) and
least successful in 1969 (80 percent hatched) al-
though the efforts of 1969 actualh- resulted in a
greater number of young (2.5) produced per
nesting effort.
The average hatching success of Fermginous
Hawks on the study area from 1967-1970 was
65.2 ± 5.2 percent for an average of 2.3 young
produced per nest per \'car. Ferruginous Hawk
nesting success was lowest in 1967 (5.3.3 percent
hatched, 1.3 young per nest) but highest in 1969
(81.8 percent hatched, 3.0 \()ung per nest). The
hatching success was comparati\el\- low during
all four breeding seasons, and a total of .35
eggs produced no young.
Red-tailed Hawk nesting efforts successfully
hatched 76.7 :^-: .3.9 percent of all eggs produced
from 1967-1970 for an average of 2.3 \'oung
per nest per year. As with Ferruginous Hawks,
Red-tailed Hawk hatching success was highest
in 1969 (88.9 percent hatched, 2.5 young per
nest) but lowest in 1970 (69.2 percent hatched,
2.2 )'oung per nest).
Swainson's Hawks had the highest hatching
success of an\- raptor on the study area, success-
fully hatching all eggs produced each year.
Swainson's Hawks averaged 2.2 yoimg per nest
per year but hatched 2.5 young per nest in 1969,
their most jiroductive \-ear.
The Prairie Falcon nest for which the initial
clutch size was known hatched all five eggs.
Hatching success is unknown for the Cooper's
Hawks and liunowing Owls (the latter because
of the inaecessibilitN' ot the nests). The only
Short-eared Owl nest on the study area hatched
six young from a clutch of seven eggs (85.7
percent). The two Marsh Hawk nests for which
clutch size data are available hatchcxl 70 percent
Biological .Seiuiss, \'ol. 18, No. 3 Bheedinc Ect)Loc;v oi- Utah HArrons
25
of the eggs for an average of 3.5 young per nest,
but the figures are misleading inasmuch as one
nest successfulh' liatchcd all seven eggs of the
clutch whereas the other nest failed to produce
any young.
Sparrow Hawk hatchabilits' is known for
1968-1970. During this time their hatching suc-
cess averaged 94.1 ± 4.9 percent for an average
of 4.7 young per nest. Their hatching success
was greatest in 1969 and 1970 ( 100 percent
hatched in both \ears).
From 1967-1970, Ravens successfully hatched
70.5 ± 7.6 percent of all eggs produced for an
average of 3.64 young per nest. Raven hatching
success was highest in 1970 (85 percent hatched,
5.0 \oung per nest) but lowest in 1969, when
less than 46 percent of the total eggs produced
hatched young for an average of 2.2 young per
nest.
Comparisons of hatching success between the
different raptor species reveals that Swainson's
Hawks had a significantly greater degree of
overall success than Ferruginous Hawks (t^
6.70) and Red-tailed Hawks" (t:= 5.85) but did
not differ significanth' from the other large rap-
tors. Great Horned Owls had the second highest
overall hatching success, significantly higher
than Feniiginous Hawks (t=r: 3.S3) but did not
var\' significanth- from that of the other larger
raptors.
Fled<iino Success. The overall fledging suc-
cess of all raptors on the study area was highest
in 1970 (61.6 ± 8.5 percent) and lowest in 1969
(53.4 ± 6.1 percent), with the 1967 and 1968
breeding seasons showing intemiediate success
(60.2 ± 7.4; 59.7 ± 6.8"percent, respectively).
There were no significant differences in fledging
success between any of the study years. Data
involving only the large raptor species of the
study area revealed a similar overall fledging
success, with 1970 again being the most success-
ful breeding season (77.8 ± 10.6 percent),
1969 the least successful (57.7 ± 7.8 percent),
and 1967 and 1968 again having intermediate
degrees of success (61.3 ± 8.9; 62.9 ± 9.1 per-
cc^nt, respectively). Again there were no signifi-
cant differences in fledging success among am-
of four study years.
From 1967-1970, Golden Eagle nests on the
stud\- area successfully fledged .S5.2 ± 13.4
percent of their original clutches for an average
of 1.0 young fledged per nest. Fledging rates
were highest in 1967 and 1970, when combined
data indicate a survival rate of 75.0 percent and
1..33 young fledged per nest, and lowest in 1968
and i969,\vhich had a combined fledging aver-
age of 35.4 percent and 0.75 young per nest.
The overall fledging success of Great Homed
Owls from 1967-1970 was 75.6 ± 7.2 percent
for an average of 2.0 young fledged per nest.
The yearly fledging range varied from 100 per-
cent (2.0 young per nest) in 1967 to a low of
70 percent in both the 1968 and 1969 breeding
seasons ( 1.75 young per nest; 2.33 young per
nest, respectively). Great Homed Owls success-
fully fledged the highest percentage of young
each year among the large raptors on the study
area, but Fermginous Hawks fledged a similar
overall average of 2.0 young per nest.
Ferruginous Hawks on the study area suc-
cessfully fledged an overall average of 56.2 ±
5.3 percent for an average of 2.0 young per nest
per year. Fen-uginous Hawks were most success-
ful in 1969 and fledged an average of 2.67 young
per nest during this season, the highest number
fledged per nest by any of the large raptors dur-
ing any study year. In contrast, their relative
fledging success during the other three study
years was but 50.6 percent for an average of
1.63 young fledged per nest for each of the
three years.
From 1967-1970 the average fledging suc-
cess of Red-tailed Hawks was 58.9 ± 4.6 per-
cent for an average of 1.74 NOimg fledged per
nest. As with the Ferruginous Hawks, Red-tailed
Hawks had their greatest fledging success in
1969 (72.2 percent) and also produced the great-
est number of young per nest (2.17 fledged per
nest) during this breeding season.
Swainson's Hawks had the second highest
fledging success on the study area, averaging
72.5 ± 13.4 percent during the four study years.
Although their average clutch size was highest
in 1969, they fledged but 1.0 young per nest this
vear, the lowest of the four study years.
Of the medium and small raptors, Prairie
Falcons in 1970 fledged but 20 percent of their
clutch of fi\'e eggs while Short-eared Owls
fledged none of six young.
Burrowing Owls fledged an average of 10
\-oung per xcar in 1969 and 1970, for an average
of 3.33 \-oung per nest per year.
From 196S-1970 the average fledging success
of Sparrow Hawks on the study area was 59.1
± 8.8 percent for an average of 2.83 young
fledged per nest. Sparrow Hawk fledging suc-
cess was highest in 1970 (80 percent, 4.0 young
per nest) but low in 1968 and 1969; the com-
bined data for these two \ears indicates a fledg-
ing success of 48.7 percent for an average of 2.6
voung fledged per nest per year.
The overall fledging success of Ravens on
the study area was 47.4 ± 3.3 percent for an
average of 2.57 young per nest. Raven fledging
26
BmcnAM Young Uni\ khsity Science Bulletin
success was consistently low, but was higher in
1967 (57.1 peiccmt, 3.0 \oung per nest) than
during the remaining study years.
Mortaliti/. The hatching and fledging per-
centages presented in Tables 14-17 are based on
the total number of eggs produced. The mor-
tality percentages of each of these stages can
therefore be detemiined by subtracting the rep-
resented figures from 100 percent. Specific
causes of the loss of eggs or young were often
difficult or impossible to determine, but im-
portant causes included nest desertion or de-
struction, human interference, predation and
apparent egg infertility (sec Table 18).
Nest desertion was observed in evciy raptor
species except the Raven and Cooper's Hawk,
with 24.1 percent of the established nests even-
tualK' being deserted before the fledging of the
young. The majority were deserted before eggs
had been deposited, and all species showed an
increasing tendencv to tolerate disturbance after
the young had hatched. Human interference,
including the presence of the investigators, was
the probable cause of the greatest number of
desertions, but many raptor pairs tolerated a
considerable amount of disturbance and yet
retained their nests (see Smith and Wilson
[1971]for a discussion of individual and species
differences in toleration of disturbance).
Red-tailed Hawks and Great Homed Owls
exhibited a tendencv to desert their nests (33.3
and 25.9 percent respectively). Both select very
similar nesting sites and often utilize the same
site in alternate years. In 1968 and again in
1969 a Great Horned Owl flushed from its nest
was attacked by a pair of Red-tailed Hawks
nesting in close pro.ximitv. In both cases the
Red-tailed Hawk nests (both containing full
Table 14. Summaiy of productivity of raptor nesting populations, 1967.
Species
No.
tomplete
clutclies
.•\v.
clutch
size
Range of
clutch
size
Total
no. of
eggs
producea
No.
young
hatched
Perecnt
young
hatched
No.
young
fledged
Percent
young
fledged
Golden Eagle
3
2.0
_
6
4
66.7
2
33.3
Great Horned Owl
4
2.0
1-3
8
8
100.0
s
100,0
Ferruginous Hawk
6
2.5
2-4
15
8
53.3
7
46.7
Red-tailed Hawk
4
2.5
2-3
10
7
70.0
6
60.0
Swainson's Hawk
1
2.0
-
2
2
100.0
1
50.0
Prairie Falcon
0
-
-
-
-
-
-
-
Marsh Hawk
9
-
-
-
-
-
-
-
Cooper's Hawk
1
3.0
-
?
?
?
?
?
Sparrow Hawk
2
4.5
4-5
9
?
?
?
?
Short-eared Owl
0
-
-
-
-
-
-
-
Burrowing Owl
0
—
-
-
-
-
-
-
Raven
4
5.2
4-7
21
15
71.4
12
57.1
Totals
34
-
-
71
44
-
36
-
Tabk- 15. Summary i
if produci
livity of
raptor nesting
p ipulations
, 1968.
Species
No-
romplete
clutches
.\v.
clutch
size
Range of
clutch
size
Total
no. of
produced
No.
young
hatched
Perecnt
young
hatched
No.
young
fledged
Percent
young
fledged
Golden Eagle
4
2.0
-
8
4
50.8
3
37.5
Great Horned Owl
8
3.0
2-4
24
21
87.5
15
62.5
F'erruginous Hawk
9
3.7
3-4
33
21
63.6
19
57.6
Red-tailed Hawk
5
2.8
2-3
14
11
78.6
8
57.1
Swainson's Hawk
1
2.0
-
2
2
100.0
2
100.0
Prairie Falcon
1
?
p
?
0
-
-
-
Marsh Hawk
0
-
-
-
-
-
-
-
Cooper's Hawk
0
-
-
-
-
-
-
-
Sparrow Hawk
3
5.7
4-7
17
14
82.4
9
52.9
S lort-eared Ow 1
0
_
-
-
-
—
-
-
Burrowing Owl
0
_
—
-
-
-
-
-
Raven
4
5.0
3-6
20
16
80.0
10
50.0
Totals
35
-
-
118
89
-
66
-
Biological Series, \'ol. 18, No. 3 ISheeuinc; Ecology ■•h- Uiaii Kai'i'oh.s
27
Table 16. Summary of productivity of raptor nesting populations, 1969.
Species
No.
toniplete
clutclies
Av.
clutch
size
Range of
clutch
size
Total
no. of
eggs
produced
No.
yoiuig
hatched
Perecnt
young
hatched
No.
young
fledged
Percent
young
fledged
Golden Eagle
Great Horned Owl
Ferriiginou.s Hawk
Red-tailed Hauk
Swainson'.s Hawk
Prairie Falcon
Marsh Hawk
Gooper's Hawk
Sparrow Hawk
Short-eared Owl
Burrowing Owl
Raven
Totals
4
6
12
6
2
0
2
0
2
0
3
4
41
2.2
3.3
3.7
3.0
2.5
4.5
5.5
2-3
9
3
3-4
20
16
3-4
44
36
2-4
18
16
2-3
5
5
4-5
?
■3
9
4-7
22
10
_
127
95
33.3
3
80.0
14
81.8
32
88.9
13
100.0
2
?
5
100.0
4
?
8
45.5
9
—
90
33.3
70.0
81.8
72.2
40.0
44.4
p
40.9
Table 17. Summary of productivity of raptor nesting population.s, 1970.
Species
No
complete
clutches
Av.
clutch
size
Golden Eagle 3
Great Horned Owl 4
Ferruginous Hawk 7
Red-tailed Hawk 4
Swainson's Hawk 1
Prairie Falcon 1
-Marsh Hawk 2
Gooper's Hawk 0
Sparrow Hawk 1
Short-eared Owl 1
Burrowing Owl 3
Raven 2
Totals 29
2.0
2.5
3.0
3.3
2.0
5.0
5.0
5.0
7.0
6.0
Total
Range of no. of
clutch eggs
size produced
2-3
2-4
3-4
5-7
6
10
21
13
2
5
10
5
7
p
12
91
No
young
hatched
6
9
13
9
2
3
young
hatched
100.0
90.0
61.9
69.2
100.0
60.0
70.0
100.0
85.7
p
85.0
No
>oung
fledged
6
7
10
6
2
1
5
4
0
12
5
58
Percent
young
fledged
100.0
70.0
47.6
46.2
100.0
20.0
50.0
80.0
0.0
?
41.7
clutches) uere subsequenth' abandoned as was
the Great Horned Owl nest of 1968 (Smith.
1970). Their most commonly chosen siti's, i.e.,
quarries, are in highh vulnerable situations
which inxite human presence and interference.
Twice in 1968 Red-tailed Hawks built nests in
quarr\' sites which were almost daily subject to
human disturbances. In both cases the nests
were subsequentl)' abandoned before eggs were
deposited. In 1970 a Great Horned Owl occu-
pied its quarr\' nest of the former three seasons.
Later interaction with a Prairie Falcon appar-
enth' caused it to abandon this crevice site be-
fore egg deposition took place. This Great
Horned Owl pair successfully renested only 42
feet from their original site which was then
occupied ( unsuccessfulh' ) 1)V the Prairie Falcon
pair. Nest desertion frequently led to renesting
attempts by Red-tailed Hawks, particularK if
nests had been deserted before egg deposition
occurred. None, however, were successful dur-
ing the four-year study.
Golden Eagles also frequently deserted their
nests, with 25.9 percent of all nesting attempts
temiinated b\ desertion. As with Great Homed
Owls and Red-tailed Hawks, the most frequent
cause of nest desertion was some form of human
interference. Two pairs each deserted their
nests in two of the three years in which they at-
tempted to nest. Egg collecting and photogra-
pliv activities were observed around these nests
before their desertion. A renesting attempt oc-
curred in 1969 but was unsuccessful.
Ferruginous Hawks deserted nests 22.2 per-
cent of the time. Several of the pairs would
tolerate no activity around the nest, particularly
during the time period immediately after egg
deposition had been completed; these birds de-
DiiiciiANt Young Universitv Science Bulletin
Tabic 18. Summar)' of causes of mortality, 1967-1970.
Total no.
Successful nests"
Unsuccessful nests
\cst (iestniction
Nest destruction
'•KR''
t-gg
losses
[uvenile losses
Egg not Eggs
E^s™.
faff
Species
prodviced
Infertile
Other
All causes
laid
laid
Young
Young
Golden Eagle.s
27
2( 2)
K 1)
i( 1)
1
3( 7)
0
0
0
1( 2)
Great Horned Owl
62
2(
2)
2( 3)
4( 4)
5
K 3)
K 3)
1
0
1( 3)
Fermftinou.s Ilauk
11.3
8(
9)
5( 6)
5( 6)
2
6(18)
0
0
1( 2)
K 4)
Red-tailed Hawk
.55
0
5( 7)
4( 4)
4
2( 5)
1( 3)
0
0
K 3)
Swainson's Hawk
11
0
K 1)
0
0
0
1( 3)
0
0
0
Prairie Falcon
5
K
1)
K 1)
K 1)
2
0
0
0
0
0
Mar.sh Hawk
■p
■?
p
1( 2)
0
1( 3)
0
0
0
0
Cooper's Hawk
.3
■?
?
v
?
?
■p
p
■p
p
Sparrow Hawk
40
0
0
3( 5)
1
1( 3)
0
0
0
1( 5)
Short-eared Owl
7
1(
1)
0
0
0
0
1( 6)
0
0
0
Burrowing Owl
?
?
?
'J
2
p
p
a
p
■>
Haven
75
4(
5)
7(18)
11(16)
0
0
0
0
0
0
Totals
398
18(:
20)
22(37)
.30(39)
17
14(39)
4(15)
1
1( 2)
5( 17)
•Numbers in uiliimns i
efpr l^ nuiiil>ri
of iicsts. nmntwrs in parpiilli
icMs following refer
til mini
tier of eggs or young.
serted their sites immediately after the nesting
tree had been chmbed or ground site ehc-eked.
However, none of tht; nests were abandoned
after the adults had hatched young.
In 1969 one Swainson's Hawk nest with
three young aged 1.5 weeks was deserted. Only
one of the pair was seen in the nest vicinity.
Three days later several pieces of the remains
of a Swainson's Hawk were found beneath the
roost of a pair of Golden Eagles which main-
tained a territorv in the same area. Evidently
this predation caused the termination of the
Swainson's Hawk's nesting aetixitics.
Prairie Falcons abandoned two ot three
nesting sites because of human activities. In ad-
dition, Marsh Hawks, Sparrow Hawks, Short-
eared Owls, and Burrowing Owls also deserted
one or more of their nests because of human
presence or interference. Marsh Hawks deserted
a nest containing three eggs which, when
checked, were infertile. Prairie I'aleons aban-
doned one nest due to aggress on eonhicts willi
Great Horned Owls (pre\ionsl\ disci:ssed) and
deserted anotlier nest located in a <|uarry whicli
was frequently visited b\ hunters and campers.
Sparrow Hawks abandoned two nests because
of similar activities. Apparentlv our investiga-
tions were the cause of th<> nest desertion b\'
Burrowing Owls and the Short-(uued Owl.
Nest destruction occurred in 4.9 percent ot
the 141 initiated nests. Causes of nest destruc-
tion included human interference and accidents.
Human interference in this case refers to the
destruction of the young and/or adults. An ex-
posed quarr\' site was occupied in 196S by a
pair of Great Horned Owls. lDespil<' distur-
bances they persisted in their attention to the
nest and succeeded in hatching three young,
but both the ni'st and \()ung were su])se(iiientlv
destroyed. In 1969 the same site was occupied
by a Red-tailed Hawk pair which also succeeded
in hatching thre(> voung. Again the nest was
destroyed before the young fledged. Another
Great Horned Owl nest occupied in 1969 was
destroyed before egg deposition. The body of
one of the adults was found beneath the nesting
tree, minus its feet and several tail feathers.
Two Ferruginous Hawk nests were similarly
destroyed. One containing two eggs was located
alongside a well-traveled road. The female was
later found shot, the eggs broken and the nest
destroyed (Weston and Ellis, 1968). The second
nest was located in a favorite rabbit hunting
locale and produced four \()ung. Shortly before
the young would have fledged, the nest was
found destroyed, with three shotgun shells King
beneath the nesting tree. One Sparrow Hawk
nest was also destroNcd. This nest was located
among the ruins of an abandoned mining
structure and had been deliberatcK- exposed.
An accident destroyed a Golden Eagle nest
in 1967, the onl\' observed instance of the nat-
ural destruction of a raptor nest. The nest had
been positioned in a loose shale quarry wall
which collapsed, killing both voung ( Murph\-
et al., 1969).
Based on tlie successful nests (i.e., those
wliich fledged at least one young) 6.5 percent
ot ail eggs produc(Hl by all raptors species
were apparenth' infertile and another 11.4 per-
cent were lost before hatching. Eggs which
did not hatch after a suitable time period were
judged infertile; how^ever, additional eggs may
have been infertile but were destroyed prior to
our cheeking them. Ferruginous Hawks had the
highest apparent percentage of infertile eggs
(10.1 percent) of an\' raptor species. Seven
Ferruginous Hawk nests contained one infertile
egg each and one contained bvo. Most com-
monly, one of a clutch of three or four eggs
Biological Seuies, X'ol. IS, Ni
Bheedinc Ecolocv ■ >!■• Utah Kaitohs
29
was infertile. Both Golden Eagles and Great
Horned Owls also produced infertile eggs. In
1968 a Golden Eagle pair produced a clutch of
two eggs. One egg disappeared early during
the incubation period, but the adult continued
to incubate the remaining egg. After 49 days
the egg had not hatched and was subsequenth'
abandoned. Raven nests also appeared to pro-
duce a high number of infertile eggs on the
studv area, with 6.7 percent of their total eggs
judged to be infertile.
Reasons for other egg losses are mostly un-
known, but the eggs usually disappeared during
incn])ation. Howe\er, one case is interesting. In
196S a Red-tailed Hawk pair produced a clutch
of two eggs. During the incubation period one
member of the pair was found destroyed (pre-
sumabh' shot). One egg disappeared but the
remaining adult rcmated with a new individual
and successfully incubated and then fledged
a )'Oung from the remaining egg.
Losses of young are also combined because
of lack of knowledge of specific causes. Juvenile
mortalit\' occurred most commonly in Raven
nests, but Golden Eagle, Great Horned Owl,
Ferruginous Hawk, and Red-tailed Hawk juve-
niles also occasionalb' disappeared.
Little infomiation was obtained on post-
fledging mortality, although this is the period
during which the majority of deaths among
first-year birds occurs (Hickey, 1949; Lack,
1954; Sprunt, 1963). In previous studies on
raptor mortalit\' in this area, Ellis, Smith, and
Murphy (1969) recorded a high percentage of
juveniles among birds which had been illegally
shot b\- hunters and suggested that juveniles are
particularly \'ulernable to tliis fonn of destnic-
tion.
Territoriality
The definition and concept of a territory has
been much discussed in the literature (Noble,
1939; Nice, 1941, 194.3; Odum and Kuenzlcr,
1955). Within the study area, however, the
minimal amount of intraspecific home range
overlap coupled with the ver\- few instances of
observed territorial defense suggests that the
most applicable concept is the "maximum home
range" category- as described by Odum and
Kuenzler (1955). Using this method, the ex-
treme positions and movements (jf raptors arc
plotted and connected and the area contained
within is the derived liome rantje. The home
ranges plotted in 1969 and 1970 were deter-
mined from a minimum of 25 obser\ations per
pair.
Home Range Estahlislitnetit ami Defense.
Home range establishment dates of all raptor
species from 1967-1970 have been previously pre-
sented in Tables 5-8. At the beginning of the
raptor breeding season, the permanent residents
selected their future nesting sites and confined
their activities within a restricted area. During
this period Golden Eagles were often observed
in such conspicuous activities as soaring, court-
ship display, and occupying a prominent perch.
Great Horned Owls were frequently active in
the early evening hours making short flights
from one perch to another. Both individuals
and pairs were observed hooting from the
cover of one perch, then making a short flight
to a new perch and hooting again. No intra-
specific or interspecific actions were observed
during this period, although on a few occasions
a Golden Eagle of one nesting pair flew within
sight of the nesting locale of a neighboring pair,
maintaining a good distance from the actual
nest site. Indeed, the pairs at times seemed to
be keeping watch on their neighbor's nest while
establishing their own territorial rights, much
in the manner described by Di.xon (1937). No
Golden Eagle and Great Homed Owl interac-
tions occurred, although pairs nested in close
proximity in 1968, 1969", and 1970. There is little
or no overlap in their respective activity pat-
terns and they do not usually come in contact
with one another. Unlike other large raptors.
Golden Eagles did not attack flushed Great
Homed Owls e\'en when owls were flushed
within 50 feet of active Golden Eagle nests.
Returning migratory pairs rapidly occupied
their territories and assumed territorial estab-
lishment acti\'ities. Ferruginous, Red-tailed, and
Swainson's Hawks were highly aggressive at
this time. In several locales Ferruginous Hawk
pairs nested in close proximity. Their morning
and evening soaring flights frequently provoked
interaction, and at times members of three pairs
would be observed soaring but short distances
from one another. Usually the act of soaring
kept the pairs distant, but occasionally one
would apparently venture too close and provoke
a response. One or both members of a pair
would posture and chase one or both members
of another pair simultaneously, although no
actual contact was ever observed. In one ex-
ample of interspecific contact, a Ferruginous
Hawk pair attacked a Great Horned Owl \\'hich
had landed some 30 feet from its cliff nest. The
Hawks dov(> at it in turn several times, each
time coining to within 3-9 feet of its head but
a\oiding contact. The owl in turn met each at-
tack by raising its wings in defense posture
and vigorously clapping its beak. The hawks
persisted until the owl flew into a nearby cliff
crevice, whereupon the hawks resumed their
30
Bbioiiam Young Univehsity Science Bulletin
soaring. In this case the Ferruginous Hawks
had arrived in the area and occupied their terri-
tory of the previous year in the moniing and
were activel)- defending it in the late afternoon
of the same day.
Hed-tailed Hawk pairs defended their terri-
tories against Great Horned Owls, Ferruginous
Hawks, and Golden Eagles but no intraspecific
conflicts were observed. Red-tailed Hawks al-
ways attacked flushed Great Horned Owls and
on at least three occasions struck from above
with open talons, although never visibly injuring
them. The owls made no attempt to defend
themselves during such attacks but instead flew
to the nearest cover. On one occasion a Red-
tailed Hawk pair attacked and drove a Golden
Eagle out of their territory. Tlie eagle was per-
sistently attacked from above when approxi-
mately 1 1/5 miles from the Red-tailed Hawk
nesting site and rapidh' flew out of the area,
followed for a distance by the red-tails. Red-
tailed Hawks also threatened Ravens, but onlv if
close to the nest site. The Ravens maintained
a cautious distance from soaring Red-tailed
Hawks and usuallv onlv a swoop in their direc-
tion sufficed to chase them away.
Encounters between Swainson's Hawks and
FerRiginous Hawks often occurred and are dis-
cussed by Murphy, et. al., (1969).
Prairie Falcons quickly and aggressively re-
acted to the presence of anv raptors within
their nesting vicinitv during this period. How-
ever, Ravens were tolerated surprisingly close
to the nesting vicinity, and in 1970 a pair of
Ravens nested within 75 feet of an active Prairie
Falcon e\rie. Both sites, however, were out of
sight of one another and hidden within recesses
in cliffs.
Ver\' little information was obtained on ag-
gression and territorial reactions of the medium-
and small-sized raptors during this period. Gen-
erally their nests were widely spaced and showed
no overlap, with the exception of the Burrowing
Owls. A Sparrow Hawk pair was observed at-
tacking a Red-tailed Hawk flying about 50
feet above its nest site, but reacted passively
to the presence of Ravens and Golden Eagles.
Burrowing Owls vigorously protested distur-
bances from investigators but allowed Marsh
Hawks to fly within their home ranges. Marsh
Hawks were similarly tolerant of the Burrowing
Owls and on two occasions nested within the
home range of Short-eared Owls.
As the breeding season progressed, the
raptors generally became less aggressixe toward
one another and fewer aggression contacts were
observed. At times much tolerance was shown
toward other raptor species flying over the nest
site, while on other occasions they would be
attacked and driven away. Definite vertical ter-
ritoiy limits appear to be present and were
easily observed during the reactions of a pair
to the presence of investigators. On several oc-
casions a second and sometimes a third pair
were observed soaring above a nesting pair
which were themselves attacking the investi-
gators. At these times the intruding pairs re-
mained unchallenged as long as they maintained
their higher altitudes. However, in one such
instance a Ferruginous Hawk pair from a near-
by nest flew over a Red-tailed Hawk nest at low
altitude; the intruders were immediately attacked
b\' the nesting pair, which suceessfulh' drove
them awav after one grappled with one of the
Ferruginous Hawks.
Home Range Coverage. The home ranges de-
termined during the breeding seasons of 1969
and 1970 are plotted in Fig. 13-21. Generally
the specific size and shape of the raptor home
ranges appeared to be a function of their size
and breeding status ( i.e., nesting pair, nonnest-
ing pair, or individual), the topography of the
surrounding locale, and apparently the breeding
population densities. Home ranges of nesting
raptor pairs were usually larger than home
ranges of nonnesting pairs and both maintained
larger home ranges than individuals of the
same species. Almost all of the raptors nesting
in the foothills had home ranges extending far
into the desert but only short distances into the
interior of the hills. Their nests, therefore, were
usuall)' located at the edge of the home range.
Average home ranges of all raptors except
Swainson's Hawks, Sparrow Hawks, and Bur-
rowing Owls were larger in 1970, correlating
with the overall decreased raptor population
densities. None, however, were significantly
larger than the average home ranges of 1969.
Additional home range information of the raptor
species is presented as follows (only home
ranges which were entirely within the study
area limits are included in the following data).
The iiome ranges of nesting Golden Eagle
pairs averaged 9.05 ± 1.1 sq miles in 1969 (3
pairs, range 6.6 — 11.8 sq miles) and 8.98 ±
0.6 s(i miles in 1970 (3 pairs, range 7.91 - 10.3
sq miles). Maximum diameters of the home
rani^es a\ c-ra,y;ed 4.09 -± 0.4 miles in 1969 (range
3.08 - 4.99 miles) and 3.85 ± 0.4 miles in
1970 (range 3.25 — 4.8 miles). Golden Eagles
possessed the largest home ranges of any raptor
nesting within the stud\' area and appeared to
be little aifeeted 1)\ topograpliic barriers. They
also appear to eoiisistenti\ utili/.e a sizeable
Biological Stuiiis, \'ol. 18, No. 3 Bueeding Ecology ok I'taii Haptous
31
Kig. 13. Home ranges ot Cioldfn Eagles (1) and .Swainson's Hawks (5) in 1969.
32
Bi<i(.ii\M Young Uninkhsitv Sciknce Bulletin
Fig. 14. Home raiims of Great Horned Owls (2) in 1969.
Biological Sehils, \ ol. hS, No. 3 Bueeding Ecology of Utah IUptobs
33
FiiT. 15. Home ranges of FerniKiiioiis Hawks (3) iti 1069.
34
Bhicham Young Univkiisity Science Bulletin
Kig. 10. Home ranges cil licd-lailcd Hawks (4) in I9()9.
Biological Seiuks, \'i>l. ly, Xo. 3 Biu;t;i)iNG Ecology of Utah Hai'tohs
35
Fig. 17. Home ranges of Prairie Falcons (6), Marsh Hawks (7), Sparrow Hawks (9), Short-eared Owls
(10), Burrowing Owls (11) and Ravens (12) in 1969.
36
BnioHAM Young Univkhsity Science Bulletin
Fig. 18. Home ranges of Golden Kagle.s (1), Red-t.nled Hawks (4) and Swainson's Hawks (5) in 1970.
Bk)looic;al Suuts, \'oi.. 18, \ii. 3 Bukkding Ec:olo(::y of Uiaii IUptohs
37
Fig. 19. Home raiip's of Great Iliirncd Owls (2) in 1970.
38
Bnir.nA%r Young University Scienck Bulletin
Kij;. 20 lloiiu' rallies 1)1 Kcrniniiioiis Hauks (3) in l!)7(l.
BiOLOciCAi, Skmies, \'oi.. 1,S, No. ,5 Bhkkding I'a:olo(;y ok Utah liAPioi
39
Fig. 21. Home ranges of Prairie Falcons (6), Marsli Ilauks (7). .Sparrow Hawks (<)), .Short-eared Owls
(10). Burrowing Owls (11) ami Ravens (12) in I970.
40
Bricham Young University Science Bulletin
portion of their home range, in contrast to
many of the smaller raptor species on the
study area. In 1969 an individual Golden Eagle
occupying a home range in the southeast por-
tion of tlie stiul\' area maintained a home range
of 2.48 s(i miles with a maximum diameter of
2.33 miles, although it was far removed from
the home ranges of the nesting Golden Eagle
pairs.
Home ranges of Great Horned Owl pairs
averaged 1.88 ± 0.1 sq miles in 1969 and 2.16
=t 0.2 sq miles in 1970 (7 pairs in 1969 and
1970 each, range 1.62 — 2.22 sq miles and 1.36
— 2.7 sq miles, respectively). Maximum diame-
ters of home ranges in 1969 averaged 1.87 ±
0.1 miles (range 1.3 — 2.53 miles) and 2.1 ±
0.3 miles in 1970 (range 1.89 — 2.8 miles).
Great Horned Owls ranged widely into the des-
erts from their nesting sites in the foothills and
maintained large home ranges. Their home
ranges appeared to he restricted by the topogra-
phy of the nesting locale, and pairs from two
nests only 0.46 miles apart but on opposite sides
of the Thorpe Hills showed no home range
ox'crlap although both nesting sites were active
during all four breeding seasons. Instead, the
pairs hunted in opposite valleys and were never
observed near the tops of the intervening ridges.
In other areas, however, slight overlaps in ad-
jacent home ranges were observed between
three pairs in 1969 and two pairs in 1970. In
1970 two nonnesting Great Horned Owl pairs
maintained home ranges of 1.64 d= 0.2 sq
miles, significantly smaller than the average
home ranges of the five nesting pairs (t =
3.2). The observed home range of an individual
on the study area in 1969 was about 1.04 sq
miles with the maximum diameter of 1.72 miles,
relatively smaller than the home ranges main-
tained by either nesting pairs or nonnesting
pairs.
The home ranges of Ferruginous Hawk pairs
averaged 2.04 ± 0.2 s(j miles in 1969 (9 pairs,
range 1.36 — 3.02 sq miles) and 2.52 ± 0.2
sq miles in 1970 (5 pairs, range 1.76 — 3.10
sq miles). Maximum diameters a\eraged 2.0S6
± 0.1 miles (range 1.51 — 2.61 miles) in 1969
and 2.02 ± 0.1 miles in 1970 (range 1.75 -
2.6 miles). As with Great Horn(>d Owls their
shapes and boundaries were in large part de-
termined by topography, and all observed home
ranges extended widely into th(< valleys but
only short distances into the hills in which the
nesting site was located. Five adjacent home
ranges overlapped in 1969 and three in 1970,
although in no case was the degree of overlap
extensive. In 1970 a nonnesting pair possessed
a home range of 1.76 sq miles, the smallest home
range of any Ferruginous Hawk pair of that
year and significantly smaller than the average
home ranges of the 1970 nesting pairs (t =
3.0.3, at the 0.001 level of probability). Home
ranges of individuals tm the study area in 1969
and" 1970 averaged 1.51 ± 0.07 sq miles (3 indi-
viduals, range 1.36 — 1.66 sq miles) and were
significantly smaller (t = 3.7) than the home
ranges of 1969 and 1970 pairs.
In 1969 the home ranges of four Red-tailed
Hawk pairs averaged 2.19 ± 0.2 sq miles
(range 1.48 — 2.78) and had average maximum
diameters of 2.21 ± 0.13 miles (range 1.79
— 2.48 miles). In 1970 the home ranges of
four Red-tailed Hawk pairs averaged 2.805 ±
0.3 sq miles (range 2.16 — 3.74 sq miles) and
had average maximum diameters of 2.25 ± 0.09
miles (range 2.07 — 2.52 miles). Home ranges
of Red-tailed Hawks were larger than the home
ranges of other Butco and Great Horned Owl
pairs but smaller than Golden Eagle home
ranges. In 1969 home range overlaps occurred
between four adjacent Red-tailed Hawk pairs
and in 1970 between two adjacent pairs. As
with other large raptors, the home ranges of
Red-tailed Hawks ranged widely into the des-
erts but very little into the hills. The average
home ranges of two nonnesting pairs in 1970
were 2.59 :h 0.3 sc] miles, significantly less than
the average home ranges of nesting pairs (t
= 3.95). The home range of an individual
present on the stud\ area in 1969 was 0.92 sq
miles, also significantly smaller (t — 5.4) than
the average home ranges of the 1969 Red-tailed
Hawk pairs.
Swainson's Hawk pairs possessed the small-
est home ranges of any of the large raptors on
the study area and averaged 1.83 ± 0.23 sq
miles in 1969 (2 pairs, range 1.6 — 2.06 sq
miles) and 1.18 s(j miles in 1970 (1 pair). The
average maxinmm diameter of the 1969 home
ranges was 2.09 miles ±0.1 miles (range 1.94
- 2.23 miles) and that of the 1970 home ranges
1.51 miles. As Swainson's Hawks were few and
widely spaced, no overlap of home ranges oc-
curred. Indi\iduals (one each year) were pres-
ent in both 1969 and 1970 and maintained aver-
age home ranges of but 0.87 ± 0.03 sq miles,
significantly smaller (t = 3.51) than the aver-
age home ranges of the pairs.
The home ranges of two Prairie Falcon
pairs in 1970 aviTaged 2.35 ± 0.12 sq miles
(range 2.18 — 2..52 sc} miles) with average
maximum diameters of 2.09 ± 0.05 miles (range
2.01 — 2.17 miles). Prairie Falcons maintained
the largest home range of any of the medium-
Biological Sehies, \()L. 18, No. 3 Bueedinc Ecology ok Utah IUftohs
41
and small-sized raptors but they were also larger
than the average lionie ranges of the Swain-
son's Hawks nesting in 1970. Craighead and
Craighead (1956) found similar large Prairie
Falcon home ranges ni-ar Moose, Wyoming.
Possible reasons for the maintenance of such
large territories b\ a medium-sized raptor are
presented by Schoener (1968). In 1969 an in-
dividual Prairie Falcon maintained a narrow
home range of 1.64 sq miles with a maximum
diameter of 2.59 miles.
The home ranges of two Marsh Hawk pairs
in 1969 averaged 1.62 ± 0.3 sq miles (range
1..58 ~ 1.66 s(| miles) and had average maxi-
mum diameters of 1.83 ± 0.09 miles (range
1.7 — 1.95 miles). In 1970 the home ranges
of three pairs a\eraged 1.74 ± 0.15 sq miles
(range 1.38 — 2.02 sq miles) and had maxi-
mum home range diameters averaging 1.97 ±
0.13 miles (range 1.58 — 2.62 miles). Marsh
Hawk home ranges were entirely within the
Cedar \'allev area east of the Thorpe and Top-
liff Hills.
Sparrow Hawk home ranges averaged 0.31
± 0.08 sq miles in 1969 (4 pairs, range 0.18
— 0.56 sq miles) and 0.26 sq miles in 1970.
Maximum diameters of the ranges averaged
0.743 ± 0.003 miles ( range 0.63 ~ 0.81 miles )
in 1969 and 0.62 miles in 1970. None of the
wideh' spaced Sparrow Hawk nests overlapped.
In 1970 an individual maintained a home range
of 0.16 sq miles with a maximum diameter of
0.58 miles.
In 1969 the a\erage home ranges of three
Burrowing Owl pairs was 0.36 ± 0.11 sq miles
(range 0.16 — 0.62 sq miles). In 1970 the aver-
age home range of three Burrowing Owl pairs
was 0.28 ± 0.04 sq miles ( range 0.20 — 0.36 sq
miles). The avera,u;e maximum diameters of
the 1969 home ranges was 0.71 ± 0.09 miles
(range 0.53 — 0.91 miles) and of the 1970 home
ranges was 0.593 zt 0.05 miles ( range 0.51-0.72
miles). All Burrowing Owl home ranges were
located east of the Thorpe and Topliff Hills and
confined to the valley floor, primaril)- within
the greasewood communities. The home ranges
of the three adjacent pairs of 1969 and two ad-
jacent pairs of 1970 overlapped considerably.
The only Short-eared Owl pair on the study
area occupied in 1970 a home range of 1.48 sq
miles, with a maximum diameter of 1.76 miles.
In 1969 an individual Short-eared Owl had oc-
cupied the same territory but had maintained a
home range of only 0.66 s(j miles with a maxi-
mum diameter of 1.21 miles. In both cases the
home range extended o\cr the vallev floor and
did not enter the foothills or hills.
In 1969 two Raven pairs possessed home
ranges averaging 2.31 ±: 0.32 sq miles (range 1.86
— 2.76 sq miles ) with average maximum diame-
ters of 2.22 ± 0.15 miles (range 2.07 — 2.53
miles). In 1970 two Raven pairs maintained
home ranges of 2.74 =t 0.17 sq miles (range 2.5
— 2.98 sq miles) with average maximum di-
ameters of 2.12 ± 0.26 miles (range 1.76 —
2.48 miles). Raven pairs maintained larger home
ranges than all of the other raptor species ex-
cept Red-tailed Hawks and Golden Eagles.
They also appeared to be little influenced by
topography and possessed widely ranging terri-
tories.
Intraspecific and Interspecific Associatioi^.
Nesting and home range associations between
raptor species are examined as follows through
( 1 ) an analysis of observed hostile interactions
between species, (2) the degree of overlap of
intra- and interspecific home ranges, and (.3)
measurements of distances to nearest neighbors
of all raptor species.
A catalog of obsei'ved hostile interactions is
presented in Table 19. All forms of interactions,
including stooping, pursuits, fights, and displays
are combined. Most of the observed interac-
tions concerned territorial disputes or nest de-
fense or displacement activities caused by the
presence of the investigator; this has been pre-
vioush' discussed in other sections of this paper.
The two most aggressive species appear to be
the Ferruginous and Red-tailed Hawk, and one
is tempted to suggest that their aggressiveness
directly results in their high nesting populations
and positions of dominance. Undoubtedlv their
high populations and competition for similar nest-
ing sites produce some conflicts both within the
species populations and between these and other
raptor species with similar habitat requirements,
such as Swainson's Hawks. The similar habitat
requirements of Red-tailed Hawks and Great
Horned Owls almost certainl\- produces the
same' degrees of hostile interactions. Unfor-
tunately, many of the observed interactions were
prompted by disturbance caused by the investi-
gators. This is particularly true of the previ-
ously discussed attacks on Great Horned Owls
by Red-tailed Hawks, Ferruginous Hawks, and
Prairie Falcons, and it is probable that this noc-
turnal species has little or no contact with these
hawks in its normal activity patterns, although
both Cameron (1914) and Weigand (1967)
observed Ferruginous Hawks attacking Great
Horned Owls.
Few interactions of any kind were observed
ix'tween an\ of the medium- and small-sized
raptors. Their small populations and wide dis-
42
BiucnAM VouNo University Science Bulletin
Table 19. Catalog of interspecific and intraspecific interactions observed on the study area from 1967-1970.
1
3
o
n3
Ul
"s
be
Species Attacking
13
es p
£S
OX
■l1
O
.2 c
U O
l|
UK
ll
o
ll
1
>
Golden Eagle
0
0
1
3
0
1
0
0
0
0
0
0
Great Horned Owl
0
0
4
12
0
4
0
0
0
0
0
2
FernigiiioMS Hawk
0
0
5
6
4
0
0
0
0
0
0
0
Red-tailed Hawk
0
0
6
2
0
0
0
0
2
0
0
0
Swainson'.s Hawk
2
0
12
0
0
0
0
0
0
0
0
0
Prairie Falcon
0
0
0
0
0
0
0
0
0
0
0
0
Marsh Hawk
0
0
0
0
0
1
0
0
0
0
0
0
Cooper's Hawk
0
0
0
0
0
0
0
0
0
0
0
0
Sparrow Hawk
2
0
0
0
0
0
0
0
0
0
0
0
Short-cared Owl
1
0
0
0
0
0
0
0
0
0
0
0
Burrowing Owl
0
0
0
0
0
0
0
0
0
0
0
0
Raven
3
0
0
3
0
1
0
0
1
0
0
2
Totals
8
0
28
26
4
7
0
0
3
0
0
4
persal account for at least part of this lack (par-
ticularly intraspecific contacts), but their dif-
fering habitat requirements also prevent much
interspecific contact with the large raptor
species. However, this is not true of the Prairie
Falcon, which ranks third in aggressiveness on
the basis of observed aggression contacts. In
this case, however, Prairie Falcons are a raptor
with habitat requirements similar to those of
the larger species.
Information on intraspecific and interspecific
overlap of home ranges is useful in estimating
the degree of association of the various raptor
species and is detemiined from the pooled data
of the home range determinations of 1969 and
1970. The large Golden Eagle home ranges
overlapped to some extent with ever)- nesting
raptor species. Golden Eagle home ranges over-
lapped with almost one-half of the nesting Great
Horned Owl pairs in amounts ranging from
6-100 percent overlap; with 45 percent of the
Ferruginous Hawk home ranges in amounts
varving from 6-100 percent; with one-third of
the Red-tailed Hawk home ranges in amounts
varying from 5-90 percent; with 2.5 percent of
the Swainson's Hawks in amounts varying from
lS-65 percent and with most of the small- and
medium-si'/ed raptors in amounts varying from
slight (as with the Burrowing Owls) to consid-
erable, (ireat Horned Owl home ranges showed
very similar overlaps with the majority of the
raptors but did not overlap with home ranges
of tlie Short-eared Owl and Bunowing Owl,
supporting Errington's supposition (1938) that
they will tolerate no other owls within their
home range.
Overlap between adjacent Great Homed Owl
pairs was present in 32 percent of the popula-
tion but in \er\ slight (2-5 percent) amounts.
Ferruginous Hawk home ranges also over-
lapped with the majority of the raptor species
in amounts varying from appro.ximatcly 2-100
percent. In 1969 and again in 1970, three close
nesting Ferruginous Hawk pairs in the extreme
southeast portion of the study area overlapped
approximately 5-10 percent of their adjacent
boundaries, but in vers' slight amounts. The
majoritx' of the medium- and small-sized raptors
had home ranges overlapped by the large rap-
tors as discussed previously. No intraspecific
overlap between adjacent ranges of Sparrow
Hawks, Marsli Hawks or Ravens occurred, but
most were widely spaced. Marsh Hawk home
ranges did o\'erlap with Short-eared Owl home
ranges (approximately 24 percent), Burrowing
Owl home ranges (6-85 percent), and Raven
home ranges (35 percent), but did not overlap
with Sparrow Hawk or Prairie Falcon home
ranges. With one exception all Burrowing Owl
home ranges overlapped, both with adjacent
pairs and extensively within all members of the
small colony.
The distances to nearest neighbors should in-
dicate to some extent the degree of tolerance
disphui'd bi'tween adjacent pairs of the same
species and that existing between different rap-
tor species. In the following, results from all
four stud\' years are pooled. Golden Eagle
nests were spaced an avi-rage of 2.18 :+: 0.23
miles apart ( 14 nests, range 1.28 — 3.6 miles).
The nearest nests were separated by the high
ridges of the intervening Thorpe Hills and the
pairs tended to hunt in opposite valleys. Dis-
tances between (Golden I'agle and Great Homed
Biolocic:al StiuES, \'i)l. 18, No. 3 Bkei-dinc 1''.(:()i.()gv ■ii" Utah Raptohs
43
Owl nests avfiagod only 0.695 ± O.IS miles
(range 0.05 — 1.52 miles), but distances be-
tween Golden Eagles and the large Butco
hawks on the study area averaged 1.54 ± 0.22
miles to Ferruginous Hawk nests (range 0.55
- 2.51 miles); 1.52 ± 0.13 miles to Red-tailed
Hawk nest sites ( range 0.83 — 2.65 miles ) ; and
2.32 ± 0.994 miles ( range 0.73 — 3.91 miles ) to
Swainson's Hawk nesting sites. Despite their
ver\ similar nesting requirements, distances be-
tween Golden Eagle and Ra\en nests averaged
1.37 ± 0.21 miles (range 0.06 — 3.0 miles).
Distances between adjacent Great Horned Owl
pairs averaged 1.19 ± 0.21 miles (range 0.64
— 3.5 miles). The maximum distances were ob-
served between nests across areas which lacked
suitable nesting cliffs and had verv little cover.
Great Horned Owl nests were often in relatively
close proximit\' to nests of most of the diurnal
Buteos, averaging 0.766 ± 0.16 miles to Ferru-
ginous Hawk nest sites (range 0.21 — 1.7
miles); 0.8S6 ± 0.17 miles to Red-tailed Hawk
nests (range 0.004 — 1.4S miles); and 0.677
± 0.09 miles to Raven nests. As with the Gold-
en Eagle nests. Great Horned Owls nested far
from Swainson's Hawk nesting sites, averaging
2.2 - 0.16 miles distant (range 1.85 — 2.69
miles ) .
Distances between adjacent Ferruginous
Hawk nests averaged 1.55 ±0.1 miles (range
0.81 — 3.39 miles). Ferruginous Hawks aver-
aged 0.826 ± 0.13 miles (range 0.39-2.06 miles)
from Red-tailed Hawk nest sites and 0.788 ±
0.13 miles (range 0.29—1.06 miles) from Swain-
son's Hawk nests. In contrast, distances to nests
of the Riuen averaged 1.3 ± 0.22 miles ( range
0.46 — 2.44 miles). Distances between adjacent
Red-tailed Hawk nests averaged 2.05 ± 0.18
miles (range 1.27 — 4.2 miles) and were the
most widely spaced of the large raptors except
for those of the Swainson's Hawk and Raven
nesting sites, averaging 1.17 ± 0.07 miles to
the former (range 0.95 — 1.35 miles) and 1.08
*: 0.12 miles to the latter (range 0.55 — 1.84
miles).
Me;isurements of distances between the
medium- and small-sized raptors proved to be
unre;ilistie because of their small populations
and wide range of habitat reejuirements. The
majority were ver\ distant from any of the
larg(> raptor nesting sites, but exceptions were
noted. Frairie Falcon pairs nested within 0.013
miles (within the same eliffiine) of an active
Great Horned Owl nest, and Ravens in 1968
nested but 0.28 miles from a (iolden Eagle nest,
witli ,ill nests successluli\ ficdging at le;ist one
\i)ung.
Adjacent Marsh Hawk nests averaged 2.39
± 0.57 miles apart (range 1.12 — 3.65 miles).
Most of the Marsh Hawk, Burrowing Owl, and
Short-eared Owl nesting sites were in close
proximiti} (i.e., less than one-half mile apart);
this is undoubtedly a result of their similar habi-
tat requirements. Nests of the Burrowing Owl
colony averaged but 0.042 ±: 0.01 miles apart
(range 0.015 — 0.08 miles) and were the most
closely spaced of anv intr;ispecific nests on the
study area.
In summary, intraspecific nests maintained
minimum average distances apart, with the
noted exception of the Burrowing Owl; but in-
terspecific nesting site distances varied greatly,
primarily because of apparent tolerance differ-
ences among species and the influence of ac-
tivity patterns which will be discussed later,
all of which combined to reveal the habitat as
a mosaic of distinct home ranges centering
around the nesting sites.
Hunting Activity Patterns and Habitat
The hunting activity periods of the raptors
are presented in Fig. 22 and 23. These were
derixed from observations of birds from blinds
and from notes on the specific activity of rap-
tors when sighted. The area contained within
the lines represents the relative degree of ac-
tivity, and the thin lines which may or may not be
presi'ut represent additional but limited activ-
ity. Although it is a well-known fact that
raptors will hunt at any time if hungry or when
in need of prey for their young, they do exhibit
definite hunting periods. The activity patterns
of all of the diurnal raptors fall into a pattern
of separate morning and afternoon or early eve-
ning hunting periods, and all showed a lull or
midafternoon period of inactivity. Among the
large raptors, Ferruginous Hawks were the
first to initiiite hunting activities in the day,
and their most intensive hunting periods oc-
curred from first litijlit, 0545 lirs to sunrise (ap-
proximately 0600 hrs) and between 1745 hrs
and 2045 !ns in the late afternoon and evening
until shortly after sunset. Ferruginous Hawks
typic;illy hunted over mixed sagebrush-grass-
land areas but were also observed hunting in
th(> sagebrush-Tt'fra(/(y;/i/« areas near the nests.
Both Red-tailed Hawks and CJolden Eagles
initiated their hunting activities in the mid-
mornimr at approximately 0830 hrs and both
sp(>cies terminated their morning hunt near
1200 hrs. Golden Eagles ranged over a wide
area and have bc^'u observed hunting in a
variety of habitats, liut Red-tailed Hawks most
frecjuently hunted in sagebrush stands. Although
44
BmaiiAM Young University Science Bulletin
golden eagle
great horned owl
swainson's hawk -
RED-TAILED HAWK -
FERRUGINOUS HAWK "
6
LIGHT
9 12 3
NOON
Fig. 22. Hunting activity patterns of the large raptors on the study area.
9
DARK
PRAIRIE FALCON
MARSH HAWK
COOPER'S HAWK
SPARROW HAWK-
burrowing owl-
Fig. 23. Iluiiliiig activity ])al(crns of medium- and s[uall-si/cd raptors.
lU'cl-tailc'c! Hawks also ranged widely, one pair
lumted over a small sagebrnsh stand less
than 0.0.3 miles from their nestiijg site. Both
species had similar intensive hunting periods,
from approximately 1445 to 1830 hrs, but Red-
tailed Hawks tended to hunt throughout a
greater portion of the dav than any other large
raptor species. The morning hunting periods
of the Swainson's Hawk began well after that
of the Ferruginous Hawk had terminated, and
their afternoon hunting periods were completed
before Ferniginous Hawks began to hunt.
.Swainson's Hawks also tended to hunt in the im-
mediate n(\sting \ieinitv in habitats similar to
tliose in whieli Ferruginous Hawks predomi-
nantly hunted.
.\il of the small raptors nesting (ju the study
arc. initiated tlieir hunting periods very early
in tlie morning and generally before sunrise.
Marsli Hawks were partieularh active at this
time hut continued until well into the morning
hours. .Sparrow Hawks were the last of the
small raptors to b(\gin lumting, initiating their
morning limit at approximately 0745 hrs. Spar-
Biological Seiues, \'ol. 18, No.
BlUCKIMNG KCOLOGV OF UlAIl l{ArTOH,>,
45
row Hawks probably hunted during more hours
of the dav than anv other raptors on the stud\-
area, although still exhibiting peak late morning
(1045-1200 hrs) and late afternoon periods.
Thev hunted o\'er a wide variety of habitats in-
cluding pinvon-juniper, winterfat, and mixed
grassland areas. Prairie Falcons exhibited simi-
lar hunting habitat preferences. On the other
hand, both Marsh Ha\yks and Ravens appar-
ently preferred to hunt o\er sagebnish or mixed
grassland-rabbitbrush stands.
All of the nocturnal raptors on the study
area showed some tendency to hunt during
da\liglit hours. Great Horned Owls and Short-
eared Owls began hunting periods in the late
e\'ening liours after sunset but before darkness.
Both showed essentially two periods of in-
tensive hunting, one beginning at approximateh-
2030-2045 hrs and continuing until 2400 hrs,
and the other beginning in the earh' morning
hours from 0430 to shortly after first light. On
two occasions Great Horned Owls were ob-
served in the late afternoon from appro.ximately
1645 hrs until darkness. In both instances the
day was overcast and snowy. Similar observa-
tions of diurnal hunting by Great Horned Owls
have been noted jjy Fitch (1940) and \'aughn
( 1954 ) . Burrowing Owls arc \er>- alert and ac-
tive during the daylight hours, and their peak
aeti\it\' p(>riods are from approximately 0430 to
0645 hrs and from 1740 to 2330 hrs. They were
also observed hunting, although infrequently,
as late as 0850 hrs in the morning, and may
occasionally hunt at any time of the day.
Predation
The prey of 9 species of raptors was ex-
amined in 1969, and of 11 in 1970. A total
of 2111 prey individuals of 55 prey species were
identified and tabulated (Tables 20-39). The
prey of the collective raptor population in-
cluded 75.2 percent mammals ( 1588 prey indi-
viduals of 17 mammal species), 8.5 percent rep-
tiles (27 individuals of 7 species) and 15 per-
cent invertebrates (316 individuals of 8 families).
Minor but not significant variations in prey
species and frecjuencv occurred l^etween the
two \ears.
Golden Eagles utilized a total of only ten
prey species, including five mammal and five
avian species. Mammals were much more fre-
quently preyed upon (96.5 percent of the total
prey) and comprised the bulk of the prey bio-
mass (99.4 percent), whereas birds comprised
0.6 percent of the prey biomass and averaged
only 3.3 percent of the individuals taken. Lago-
Tahle 20. Food habits of Golden Eagles in 1969.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass
Lepus californicus
155
74.5
356,500
88.6
St/hilafius sp.
43
20.8
43,000
10.7
Ainin()S))crmophihis leucurus
3
1.4
435
0.1
Pero<i,nathns formosus
1
0.5
19
Tr."
Zenaidtini macroura
1
0.5
153
Tr.
Chanciest es i^ra m macus
1
0.5
30
Tr.
Bufco snainsoni
2
1.0
988
0.5
Asia flaninieiis
1
0.5
340
Tr.
Totals
207
99.7
401,465
99.9
"Present in trace nmoiints only.
Table 21. Food habits of Golden Eadcs in 1970.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass
Lepus californicus
68
57.1
156,400
80.5
Sijlvilafius sp.
35
29.4
35,000
18.0
Anu>i()S))erniophiltis leucurus
9
7.6
1,305
0.7
Mustclii frenala
2
1.7
356
0.2
Zeiiaidura macroura
1
0.8
153
0.1
Otocoris alpestris
3
2.5
56
Tr."
Buteo sicainsoni
1
0.8
988
0.5
Totals
119
99.9
194,258
100.0
'Present in trace amounts only.
46
BiiiciiAM VouNf. University Science Bulletin
'HiWe 22. Food habits of Croat Ilonu.l Owls in 1969.
No.
%
Species
Indv.
Indv.
Leptis californicus
165
58.9
Siilvil(iii,us auduboni
32
11.4
Neotoma Icpidii
6
2.1
Per()L:,milIius parvus
2
0,7
Dipadditii/s ruirrops
8
2.9
Dipodoniiia urdii
11
3.9
Microtiis sp.
5
1.8
Pertinuisciis numictduftis
7
2.5
CijanocvpJudus ciiinwrcpludus
3
1.1
Zcnaidum macroura
5
1.8
Phalaenopfdtis mttUdUi
1
0.4
Scorpionida
35
12.5
Totals
280
100.0
.Xppro.v.
%
Biomass
Biomass
379,500
91.4
32,000
7.7
1,.302
0.3
.30
Tr."
520
0.1
748
0.2
190
Tr.
119
Tr.
50
Tr.
765
0.2
62
Tr.
30
Tr.
415,316
100.0
'Present iti time niiKninls only.
Table 23. Food habits of Great Homed Owls in 1970.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass
Lepus californicus
83
49.1
190,900
89.6
Si/hnhiiius sp .
19
11.2
19,900
8.9
Neotoma lipida
1
0,6
217
0.1
Dipodoniifs ordii
24
14.2
1,632
0.8
Dipitdoitnjs microps
3
1,8
195
0,1
Pcntmiiscus iiianirtddlus
12
7.1
204
0.1
Microdipodops mc<s.accphalus
2
1.2
48
Tr.
Onijchointis leuco^cistcr
3
1.8
114
Tr.
Zcnaidura macroura
4
2.4
612
0.3
Otocoris alpestris
1
0.6
28
Tr.
Pica pica
1
0.6
173
Tr.
Scorpionida
16
9.5
14
Tr.
TotaLs
169
100.1
214,037
99.9
niorph.s were tlic predominate food item of
'ioldi'ii I'las^les on the stiuh' area and con,sti-
Inted o\fr 95 percent of tlu' pre\' in 1969 and
SO percent of I he pre\ in 1970, contrihutinij;
98.9 percent ol llie pre\ hioniass eaeli yt'ar. The
next mo.st important food item wa.s tlie Antelope
(ironnd Scinirrel, which averaged 4.5 percent of
the food items and 0.4 percent of the volumetric
diet lor tlie two N'car.s. Foiu' of tlie total of tt'ii
pre\ species taken h\ (Golden Eagles during tlie
two vears were hiixfs, hut none contributed sig-
nificinti\ to the ditt. 'iWo of the bird species
weic raptors (Short-eared ( )\\ 1 and .Swainson's
Hawk) and are examples of the (Golden I'^agU's
ability to prey on other avian predators. Dixon
(1937), Arnold (1954), Carnic (1954), Mc-
Cahan (1968), and others iiave reported simi-
lar examples ot (Jolden Eagle pretlation on
other raptors.
Great Horned Owls on the study area uti-
lized a total of 16 prev species, including 10
mammal, 5 bird, and 1 iin'crtebratc species.
M.immals eonstitutt'd S.5,6 percent of the prey
individuals and 99.7 percent of the total prey
biomass, while birds comprised 3.5 percent of
the pre\ items but onl\' 0.3 percent of the prey
biomass, Imcrtebrates accounted lor 11 per-
ernt ol the pre\' individuals but contributed
minor amiiuiits of prev biomass, Eauomoiphs
were the most lre([iientl\ taken pre\ item, a\er-
aging 65,3 perci'ut ol the total prev individuals
iccDrded; the\ contributed 98.9 percent of the
total pi('\ biomass during U}69 and 1970. Two
species ol Kangaroo liats were the lU'xt most
lre(|uentl\ recorded prey, a\'eraging o\er 11
percent (il the total prey items but contributing
laiK 0.6 penent ot the total prey biomass. Al-
thouiih CDiitribntinu ciiiK' minor amounts to the
Biological Series, \'ol. 18, No. 3 BnEEniNO Ecology ;)f Utah 11.\ptohs
47
Table 24. Food habits of Ferruginous Hawks in 1969.
Species
No.
Indv.
%
Indv.
Approx.
Biomass
%
Biomass
Lepus califonucus
St/Ivihiius sp.
AmmospcniiopJiilus Icucurus
105
6
IS
57.7
3.3
9.9
241,500
6,000
2,610
95.0
2.4
1.0
Spcrmoj)Iiihis touusendi
2
1.1
382
0.2
Pc'roiJ.n(ithiis jxirvus
1
0.5
15
Tr.
Dipodomys ordii
Dipodomijs microps
Onycliointjs Icucofiaster
Peroiiti/sctis numicidatus
25
2
1
4
13.7
1.1
0.5
2.2
1,700
130
38
68
0.6
Tr.
Tr.
Tr.
Otucoris alpcstiis
9
4.9
252
0.1
Calamospiza mehnocorys
Zcnaidiira macrouro
3
1
1,6
0.5
150
153
Tr.
Tr.
Pooccctcs iiramineus
2
1.1
100
Tr.
Pituoplii.s mchinolcticus
2
1.1
744
0.3
Cncinidophorus tif^ris
1
0.5
24
Tr.
Totals
182
99.7
253,866
99.6
'Present in Iiace amounts only.
Table 25. Food habits of Ferruginous Hawks
1970.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass
Lepus californictis
97
56.4
223,100
93.0
Si/hihiiius sp.
13
7.6
13,000
5.4
Amospcrmophihis Icucurus
8
4.7
1,160
0.5
Peroij.nalhus parvus
3
1.7
45
Tr.
Dipodomys ordii
17
9.9
1,156
0.5
Dipodomys microps
6
3.5
390
0.2
Pcromyscus maniculatus
9
5.2
153
Tr.
Otocoris alpestris
14
8.1
392
0.2
Pooccctcs gramincus
1
0.6
30
Tr.
Oreoscoptes montamis
1
0.6
33
Tr.
Pituophis mehmolcucus
3
1.7
372
0.2
TotaLs
172
100.0
239,831
100.0
'Present in trace amounts only.
T.ible 26. Food habits of Red-tailed Hawks in 1969.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass"
Lepus calijornicus
Ill
58.4
255,300
92.5
Si/lvihii^us sp.
17
8.9
17,000
6.2
S))cnu()p}iilus tonnscndi
4
2.1
764
0.3
Eutamicis minimus
2
1.0
146
Tr.
Peromyscus uuniictddttis
13
6.8
221
Tr.
Microtus sp.
22
11.6
836
0.3
Olocoris alpestris
6
3.2
168
Tr.
Sialia currucoidcs
1
0.5
45
Tr.
CyamKcphalus cyamxcphalus
7
3.7
350
Tr.
Sturnis vtdf^aris
3
1.6
252
Tr.
Pituophis mclanolcucus
1
0.5
372
0.1
^tastic(}j>his tacniatus
3
1.6
507
0.2
Totals
190
99.9
275,961
99.6
'l*ir>«pnt in irare amounts only.
48
HniniiAM Young IInivkhsity Science Bulletin
total l)i()mas.s of Great Horned Owl prey, at
least one species of scorpion was taken quite
frecjuently during all four study years (see
Murphw et al., 1969). Although scoqiions were
not taken by all Great Horned Owl pairs, they
showed up consistently and almost exclusively
in tlie n(-st site pellets of a pair nesting in the
west Thorpe Hills area, serving to indicate the
possibilities of error when analyzing food habits
of raptor pairs. Interestingly, the female of
this pair had an irregular left eye and it is
tempting to speculate that there was a possible
connection. Errington, Hamerstrom, and Hamer-
strom ( 1940 ) suggested that predation on ar-
thropods is most characteristic of recently
fledged owls, but as previouslv noted, the
scorpions were found every year that this fe-
male was present. One Black-billed Magpie
was taken by a pair of Great Homed Owls
nesting in pinyon-juniper. Magpies were com-
mon around the towns and cultivated areas of
the northeast portion of Cedar Valley and fre-
quenth' nested in cottonwoods and elms in
those areas. They did not nest within the study
area, probabK' I)ecause of a combination of un-
suitable habitat and possible predation.
Ferruginous Hawks within the study area
utilized a total of 17 prey species, including 9
mammal, 6 avian, and 2 reptile species. Mam-
mals comprised S9.5 percent of the prey indi-
viduals and 99.4 percent of the total prey
biomass. In contrast, birds comprised only 8.7
percent of the total prey items and 0.2 percent
of the total prey biomass, while reptiles in-
eluded 1.7 percent of the total prey individuals
and 0..3 percent of the total prey biomass. Lago-
Table 27. Food habit.s of Red-tailed Hawk.s in 1970.
No.
%
Appro.x.
%
Species
Indv.
Indv.
Biomass
Biomass"
Leptis californicus.
71
50.7
163,300
90.0
Sijlviliii:,us- sp.
15
10.7
15,000
8.2
Spennopltihis townsencU
1
0.7
191
0.1
Amiiiospcrmophihis leucums
9
6.4
1,304
0.7
Peromi/scus mdnicultifiis
26
1S.6
442
0.2
Mir rot Its sp.
1
0.7
38
Tr.
Thomomi/s holtac
2
1.6
340
0.2
Otecoris alpcstris
3
2.1
84
Tr.
Tt/ranniis verticalis
1
0.7
36
Tr.
Stiirnis vuli^aiis
9
6.4
756
0.4
PHitophis nichinoleiicits
1
0.7
372
0.2
Crot(ip]ii/lus coUaris
1
0.7
30
Tr.
Totals
140
100.0
181,893
100.0
'I'rt-'i.i'nl in Iraie iinnninls onlv-
Table 28. Food habits of Swainson's Hawks in 1969,
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass"
Lepiis californicus
42
51.2
96,600
95.0
St/lvihif^us sp.
4
4.9
4,000
3.9
Perotni/sctis nianiculatus
7
8.5
119
0.1
Mirrotits .v/).
3
3.7
114
0.1
Spcrniophiltis lounsendi
1
1.2
191
0.2
Calamospiza melanoconjs
3
3.7
99
0.1
Lanius ludoviciamis
1
1.2
52
0.1
Orcoscoptes iiwntanus
1
1.2
45
Tr.
Sai/ortiis sat/o
2
2.4
56
0.1
Zonotrichia leucophnjs
1
1.2
30
Tr.
Pituophis mehinoleucHS
1
1.2
372
0.4
Locustidae
15
18.3
95
Tr.
Carabidae
1
1.2
0.23
Tr.
Totals
82
99.9
101,688
100.0
•Prc-icril irt irate nnioiints unlv.
Bioloc;ic:al Skiues, Vol. 18, No. 3 Ukkicdinc; E(X)i,<)f:v oi- Vt.\u Hai-tohs
49
Table 29. Food habits of Swainson's Hawks in 1970.
No.
%
Species
Indv.
Indv.
Leptis californicus
15
19.0
St/IvihiiS.tis audohoni
9
11.4
Pcronujscits maniculatus
2
2.5
Micwtus sp.
1
1.3
Otocoris (dpestiis
11
13.9
Unident. Pa.s.serincs
8
10.1
Lociistidac
17
21.5
Carabidac
5
6.3
Tcncbrionidac
2
2.5
Grvllidat-
9
11.4
Totals
79
99.9
Appro.x.
%
Biomass
Biomass*
34,500
78.2
9,000
20.4
34
0.1
38
0.1
308
0.7
240
0.5
11
Tr.
1
Tr.
1
Tr.
4
Tr.
44,137
100.0
'Piesent III tiace aniounts only.
Table .30. Food habits of Prairie Falcons in 1970.
Species
No.
Indv.
Amiuospermiipliilus leuciirtis
5
Peromijscus maniculatus
Lepus californicus (juv. )
Otocoris alpcstris
Oberholscria chlorura
Pooecetcs L:,rami)icus
1
2
7
1
1
Sturnis vuli^aris
Sturnella neglecta
Locustidao
3
1
5
Totals
26
Indv.
19.2
3.8
7.7
26.9
3.8
3.8
11.5
3.8
19.2
99.7
Appro.\.
Biomass
725.0
17.0
2,300.0
196.0
30.0
27.0
84.0
145.0
3.2
3,527.2
Biomass*
20.6
0.5
65.2
5.6
0.9
0.7
2.4
4.1
Tr.
100.0
aiiioiiiits tmly.
Table .31. Food habits of Marsh Hawks in 1969.
No.
%
Appro.x.
%
Species
Indv.
Indv.
Biomass
Biomass*
Lepus californicus (juv.)
12
31.6
1,200.0
50.1
Spennophilus tounsendi
5
13.2
755.0
31.5
Pcroini/scus maniculatus
7
18.4
119.0
5.0
Reifhrodontomi/s Megalotis
2
5.3
24.0
1.0
Otocoris alpcstris
4
10.5
112.0
4.7
Zenaidura macroura
1
2.6
153.0
6.4
Pooecetes gramineus
1
2.6
30.0
1.0
Carabidae
6
15.8
1.4
1.3
Totals
38
100.0
2,394.4
101.0
* Present in Ii.lie ^iindiints imlv.
iiioiphs attain were the mo.st frequent prev
item, averas^ing 62.5 percent of the total prey
and contributing 97.4 percent of tlie prey bio-
mass in each of the two years. Tlie next most
frequently taken pre\- items were, in order of
their aNcrage vearh' freqiiencv; Ords kangaroo
rat, C(;nstituting 11.8 percent of the total prey
but only 0.5 percent of the prey biomass; the
antelope ground sfjuirrel. which averaged 7.3
percent of the total prev individuals and 0.25
percent of the prey biomass; and the Homed
Lark, which averaged 6.5 percent of the total
prey and 0.15 percent of the prey biomass. The
two kangaroo rat species and pocket mouse
reflect cssentiallv crepuscular hunting activity
patterns of the Ferruginous Hawk as discussed
earlier. Ferruginous Hawks also infrequently
pre\'ed on gopher snakes.
50
BniGiiAM '^'ouNG University Science Bulletin
Mammals wen- also the major prey of Red-
tailed Hawks, coinprisinu; S9.1 pcreent of the
prey individuals and 99.4 percent of the total
prey biomass, while birds constituted 9.1 per-
cent and 0.2 percent, and reptiles accounted for
1.8 percent and 0.3 percent of the total prey
items and total pr('\- biomass, respectively. The
major items of importance were again the lago-
morphs, which accounted for 64.4 percent of the
prev items and 98.5 percent of the total prey
ijiomass. In addition. Red-tailed Hawks preyed
on 6 other mammal species, 5 avian, and 3
reptile species. Other mammal species of im-
portance included tlu' deer mouse, which com-
prised 12.7 percent of its total diet; meadow
mice, comprising 6.2 percent; and the antelope
ground sciuirrel, which constituted 3.2 percent.
Starlings and Finvon Javs were the most fre-
((ueiitlv taken avian pre\ species. Starlings were
first recorded in Utah in 1949 in and around
url)an areas (Behle, 1954). Since that time they
ha\e spread widely throughout the state and
Table 32. Food habits of Marsh Hawks in 1970.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Bioma.ss°
Lepus californicus
5
13.5
5,000.0
86.9
Peroiui/scus maniculatus
15
40.5
255.0
4.4
SpeimopJiiliis tounscncU
1
2.7
191.0
3.3
Otocoiis (iIjK'stris
7
18.9
196.0
3.4
Pooecetcs ^raminetis
3
8.1
81.0
1.4
Demiestidae
5
13.5
1.2
Tr.
CrofopJuilus collaris
1
2.7
30.0
0.5
Totals
37
99.9
5,754.2
99.9
tit in hiifo anioiiiii'i
Table .33. i'ood liabits of Sparrow Hauks in 1969.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass*
Microtus sp.
5
6.5
190.0
17.6
Peromiisciis nuiniciilatiis
18
23.4
306.0
28.3
Otocoris alpestris
6
7.8
168.0
15.6
Sialia currucoide.s
2
2.6
90.0
8.3
Passer domcsticus
2
2.6
50.0
4.6
Sftirnis viiliiuris
3
3.9
252.0
23.3
Uta st(insl)uriami
1
1.3
4.0
0.4
Aranae
2
2.6
0.8
Tr.
Locustidae
29
37.6
18.3
1.7
Curculionidae
7
9.1
0.7
Tr.
Uniden. Colcoptcra
2
2.6
0.6
Tr.
Totals
77
100.0
1,080.4
99.8
'Pirst-nt in li.irc nnioimts imly.
Tal)le 34. Food habits of Sparrow Hawks in 1970.
Species
No.
Indv.
%
Indv.
Approx.
Biomass
%
Biomass*
Peronu/sciis maniculatus
7
21.2
119.0
30.4
Passer clomesticus
3
9.1
75.0
19.2
^Itirnis vulgaris
2
6.1
168.0
42.9
Uta stansl>uriana
3
9.1
12.0
3.1
Pltrynosonia plat i/ rhinos
1
3.0
9.0
2.3
Locustidae
13
39.4
8.2
2.1
Curculionidae
4
12.1
0.4
Tr.
Totals
33
100.0
391.6
100.0
'Present in trace amounts onlv.
Biological Sehies. \'ol. 18, No. .3 Bkeedinc Ecology ok Ut.\h K.-vptobs
51
Table 35. Food habits of Short-eared Owls in 1970.
No.
%
Appro.x.
%
Species
Indv.
Indv.
Biomass
Biomass
Dipodomifs ordii
7
20.0
476
37.4
Reithrodoiitomys tnei:.(ilotis
2
5.7
24
1.9
Peromt/sciis maniadatus
19
54.3
323
25.9
Pcroi:.nathu.s parvus
.3
8.6
45
3.5
Unidentifk'cl pa.s.scrine
1
2.9
30
2.4
Sturnis vulgaris
1
2.9
84
6.6
StttrncIIa ncjjccta
2
5.7
290
22.6
Totals
35
100.1
1,272
100.3
Table 36. Food habits of Burrowing
Owls in 1969.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass"
Dipodomtjs ordii
11
12.4
748.0
73.1
Peroi:.nathtis formosits
1
1.1
19.0
1.9
Microtus sp.
2
2.2
76.0
7.4
Phalaenoptilus mittali
1
1.1
62.0
6.0
Otocoris alpcsfris
3
3.3
84.0
8.2
Vta staushuriana
1
1.1
4.0
0.3
Locustidae
29
32.6
18.3
1.9
Scarabidae
19
21.3
5.7
0.6
Silphidac
11
12.4
3.3
0.3
Carabidae
7
7.9
1.6
0.2
Teiu'brionidae
2
2.2
1.1
0.1
.■\iaiiae
2
2.2
0.8
Tr.
Totals
89
99.8
1,023.8
100.0
* Pi (-sent in liiice .immmts only.
Table 37. Food habits of Burrowing Owls in 1970.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass
D'.jxidoiiu/s ordii
4
5.5
272.0
61.9
Pcromt/sctis iiuinicu
hit us
2
2.7
34.0
7.7
Reithrodontomys megalotis
1
1.4
12.0
2.7
Otocoris alpestris
2
2.7
56.0
12.7
Passer doniesticus
1
1.4
25.0
5.7
I'td staml)tiriarm
3
4.2
12.0
2.7
Locu.stidac
34
46.6
21.4
4.9
Silphidac
13
17.8
3,9
0.9
Caial)idae
8
11.0
1.8
0.4
Scarabidae
5
6.8
1.5
0.3
Totals
73
100.1
439.6
99.9
are perhaps the iiKJSt eoinnion nestini^ species
on the stiuK' area in such areas as quarries and
abandoned niiiiiiiL!; structures, where they are
oceasionalK' prcNctl on 1)\' raptors. Red-tailed
Hawks also infrecjuently preved on snakes, the
two species recorded from this stndv being tlu'
gopher snake and striped racer.
Swainson's Hawks on the stndy area utilized
a total of 1.5 pre\' species ineluding 5 ruamiiial.
5 a\ian, 1 reptile, and 4 invertebrate species. The
relati\e composition of the Swainson's Hawk
diet is as follows: mammals, 51.9 percent of the
total pre\' individuals and 99.1 percent of the
total pre\' biomass; birds, 16.9 and 0.8 percent;
reptiles, 0.6 and 0,2 percent; invertebrates, .30.6
and less tlian 0.1 percent. Swainson's Hawks
were the only large raptors studied in which the
average frecjuencv of lagomorjih prev was less
52
BmoiiAM VouNG University Science Bulletin
than lialf of tlic total diet. Lagomorphs thus
constituted 56.1 pcrct'ot of the diet in 1969 hut
onlv 30.4 percent in 1970. However, in both
years the higonioiphs, hv \irtne of tlieir large
body size, comprised almost 99 percent of the
total prey biomas.s. The second most numerous
prey items were Locustid insects which com-
prised an average 19.9 percent of the yearly
diet, although contributing comparatively small
amounts of the total biomass. Other insects
taken included carabids, tenebrionids, and
gryllids. Deer mice were taken iiifrequentlv, as
were meadow mice. Horned Larks were the
most frequently taken avian species and consti-
tuted almost 7 percent of the total prev taken.
Information on the food habits of the Prairie
Falcon was obtained only during the 1970
breeding season. Prairie Falcon prey consisted
of nine species, including three mammal, five
avian and one insect species. Birds were the
most frequently taken prey and comprised 49.8
percent of the prey individuals Ijut only 4.1
percent of the total prey biomass. Mammals
comprised 30.7 percent of the prey individuals
and contributed a prev biomass of 86.3 percent,
while invertebrates accounted for 19.2 percent
of the prev individuals but for little or no bio-
mass. The two most freeiuentlv taken prey
species were the Honied Lark (26.9 percent of
the total prey individuals) and antelope ground
squirrel (19.2 percent), but juvenile black-
tailed jackrabbits comprised over 65 percent of
the prey biomass, even though taken only one-
sixth as often.
Tile food of Marsh Hawks included 10 prey
species, of which there were 4 mammals, 3
birds, 1 reptile, and 2 invertebrate species.
Marsh Hawks preyed most fretjuently on mam-
mals (62.5 percent of the prey items) which
also contributed the bulk of the prey biomass
(91.9 percent). Of the other major prey groups,
birds were taken 21.4 percent of the time and
comprised 8.5 percent of the prev biomass, rep-
tiles 14.7 and 0.7 percent and invertebrates 1.4
and 0.3 percent, respectively. The most im-
portant prev of the Marsh Hawks included
black-tailed jaekral)liits and the deer mouse.
The majorit) of rabbits taken were immatures,
Table 38. Food habits of Ravens in 1969.
No.
%
."Vpprox.
%
Species
Indv.
Indv.
Bioma.ss
Biomass"
Leptis calif orniciis ( juv )
19
3L1
19,000.0
95.6
Peromijscus manicidatus
12
19.7
204.0
1.0
Microtus sp.
3
4.9
114.0
0.6
Neotonia Icpida
1
1.6
217.0
1.1
Spizella passcrina
1
1.6
38.0
0.2
Passer domesticus
3
4.9
75.0
0.4
Oreoscoptes monfunus
1
1.6
45.0
0.2
Masticoph is taeniattis
1
1.6
169.0
0.9
Dermestidae
9
14.8
0.9
Tr.
Silphidae
6
9.8
1.8
Tr.
Curculionidae
2
3.3
0.2
Tr.
Unident. Coleoptera
3
4.9
0.9
Tr.
Totals
61
99.8
19,864.8
100.0
'Pi<"ioiit in ttiiro nninunts milv.
Table 39. Food iiabits of Ravens in 1970.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biomass"
Si/Ivihii:,us sp.
6
16.7
6,000.0
90.7
Pcroniijsctis iimniculatiis
13
.36.1
221.0
3.3
Otocoris alpestris
4
11.1
112.0
1.7
Sttirnis vul'j,(iris
1
2.8
84.0
1.3
Maslirophis lacnialus
1
2.8
169.0
2.6
Sccl()}>or()us grasciosus
2
5.6
26.0
0.4
Unident. Coleoptera
9
25.0
2.7
Tr.
Totals
36
100.1
6,614.7
100.0
•I*resent in Irace amounLs only.
Biol()gic:al Sehiks. N'ol. 18, No. 3 Bhkkding Ecology of IItah Haptohs
53
juveniles, or carrion but they comprised 22.6
percent of the total prey biomass. Deer mice
were taken more frecjuently, yet, by contrast,
Townsends ground scjuirrels comprised only
8 percent of the prey items but 17.4 percent
of the total prey biomass. Horned Larks and
Mourning Doves were also taken occasionally.
Sparrow Hawks on the study area utilized a
total of 12 species, which included 2 mammal,
4 birds, 2 reptiles, and 4 invertebrates. The
relatixe composition of the prey frequency and
biomass of the major prey groups of the Spar-
row Hawk is as follows: maiumals, 25.6 percent
and .3S.2 percent; birds, 16.1 and 57.0 percent;
reptiles, 6.7 and 2.9 percent; and invertebrates,
51.7 and 1.9 percent. Locustids were the most
important ia\ertebrate prey species, averaging
38.5 percent of the yearly diet. The more im-
portant vertebrate prey species included the
deer mouse, which comprised 22. .3 percent of
the total pre\' items and 29.5 percent of the
total prey biomass, and Starlings, which con-
tributed the bulk of the prey biomass (.33.3
percent), although taken infrequently. Of the
a\ian prey species, English Sparrows, Starlings,
and Western Bluebirds reflect the habitat se-
lection of Sparrow Hawks, being the most com-
mon nesting birds in and around the abandoned
mines, (juarries, and mining structures. The oc-
currence of Western Bluebirds as prey is inter-
esting, because the disappearance of a bluebird
and the subsecjuent failure of its nesting efforts
coincided with the appearance of this species in
tlie prey of a Sparrow Hawk pair. The blue-
birds had selected a nesting site within the
wooden walls of a luining cabin only 80 feet
from tlie Sparrow Hawk nest and were incu-
l)ating a clutch of five eggs when checked the
day before the disappearance. Two days later
the remains of a bluebird were found among
the pre\- items in the Sparrow Hawk pair's
lust. Powers (1966) cites possible examples
of Sparrow Hawk predation on bluebirds in
Montana, and Drinkwater (1953) recorded a
ease of Sparrow Hawks capturing young blue-
birds by nest robbing.
Information on Short-eared Owl food habits
was obtained only in 1970 and is derived from
the analysis of 19 pellets gathered from the un-
successful nest site. Pellet anahsis \ielded a
total of 7 prey species and 35 individuals, but
onl\' mammals and birds were present. Mam-
mals contributed SS.6 percent of the prey indi-
viduals and 68.2 percent of the prev biomass,
while birds comprised 11.5 percent and 31.8
percent, respecti\'ely. The two most important
prey species were Orel's kangaroo rat and the
deer mouse. D(>er iTiiee were taken almost three
times as often as any other prey species and
contributed 26.4 percent of the total prey bio-
mass. Ord's kangaroo rat was the ne.xt most
fre(|uently taken prey and comprised 37.4 per-
c(>nt of the prey biomass. Western Meadowlarks
contributed 22.8 percent of the total prey bio-
mass.
Burrowing Owl prev included a total of 15
species of which there were 5 mammal, 3 avian,
1 reptile, and 6 invertebrate species. Burrowing
Owls preyed most frequently on invertebrates,
which comprised 80.4 percent of the prey indi-
\iduals but only 4.8 percent of the total prey
biomass, the lowest of all the major animal groups
except the reptiles. Mammals contributed 80.4
percent of the total prey biomass and almost 13
percent of the prey individuals taken, while
birds comprised 4.3 percent of the prey items
and 16.3 percent of the prey biomass. Locustids
were taken more frequently than any other
species, averaging 39.6 percent of the prey indi-
viduals but only 3.4 percent of the total prey
l)iomass. In contrast, Ord's kangaroo rat com-
prised only 9 percent of the yearly prey items
but contributed 67.5 percent of the total prey
biomass. Burrowing Owls lined the entrance
of their burrows with chewed up prey remains
and manure, a fact also recorded bv Stoner
(1932, 1933), Bent (1938), and Scott (1940).
Ha\'ens on the study area utilized a total of
16 prey species which included 5 mammal, 5
avian, 2 reptile, and 4 invertebrate species. The
majority of their food habits were determined
from castings and prev remains at the nest, and
there is the possibility that some of the prey
brought to the nestlings may have been carrion.
Mammals comprised 55.1 percent of the prey
individuals and 96.2 percent of the total prey
biomass. Birds comprised 11 percent of the
prey individuals but only 1.9 percent of the
total prey biomass, as did reptiles. Inverte-
brates, entirely insects in this case, accounted
for 28.9 percent of the prey individuals but con-
tributed only minor amounts to the total prey
biomass. Lagomorphs constituted the princi-
pal prey and averaged 23.9 percent of the
yearly prey individuals and 93.2 percent of the
total prey biomass. Although birds were taken
infrefjuentlv. Homed Larks and English Spar-
rows were the most common avian prey species.
Dermestids and unidentified beetles were the
most frefiu(>ntly taken invertebrates. In 1970
the deer mouse was the most commonly recorded
prey species, but no black-tailed jackrabbits
were found— in contrast to 1969. Almost two-
tiiirds of the jackrabbits were immatures or
juveniles, and there is the possibility that some
were taken as carrion.
54
BniGHAM Young University Science Bulletin
DISCUSSION AND CONCLUSIONS
Populations
The average yearly raptor population sup-
ported by this area of the Great Basin is ap-
parently low. Craighead and Craighead (1956)
recorded yearly populations of 140 raptors (9
species, 64 pairs, 12 individuals) during a two-
year study of a 36-square-mile Michigan wood-
lot habitat, and a population of 91 raptors ( 10
species, 45 pairs, 1 individual) in a 12-s([uare-
mile study area near Moose, Wyoming, r(>pre-
senting average densities of 1.8 and 3.8 raptor
pairs per square mile in Michigan and Wyo-
ming, respectively. These are almost four and
ten times the avi-rage densities of raptor pairs
recorded from this study. Additional compari-
sons are available from studies of particular
species.
Golden Eagles nesting on the study area
average 20 square miles per pair. Compara-
tively, Dixon (1937) recorded densities of ap-
proxiinateh' 36 square miles per pair in Southern
California, and Arnold ( 1954 ) found similar
pair densities in Colorado. In other studies
Lockie (1964) found Golden Eagle densities
of one pair per 27.1 square miles in the Scottish
Iliglilands and McGahan (196S) reported one
pair per 66.3 sejuare miles in Montana. Watson
(1957) found relatively high breeding densities
of one pair per 9 square miles in another Scot-
tish study, but in a later study covering a wider
portion of the same area Brown and Watson
( 1964 ) found Golden Eagle pair densities rang-
ing from approximately 20 to 34 square miles
per pair.
Great Horned Owl densities averaged one
pair per 10 square miles in central Utah. Studies
in other habitats have reported much higher
densities. I5aunigartner (19.39) estimated pop-
ulations of one pair per 0.5 scjuare miles of
riparian habitat near Lawrence, Kansas, and one
pair to 3 or 4 sciuare miles near Ithaca, New
York. Fitch (1947) estimated a very high popu-
lation density of one pair per 0.25 square miles
in California chaparral. In other studies Erring-
ton, Hamerstrom, and Hamerstrom (1940)
found one pair per 2 scjuare miles near Prairie
du Sac, Wisconsin; Orians and Kuhlman (1956)
recorded average densities of one pair per 5
square miles, also in Wisconsin; and Ilagar
(1957) reported Great Horned Owl densities of
one pair per 4.4 scjuare miles in central New
York. Cniighead and Craighead (1956) found
average densities of one pair per 5.8 square
miles in Michigan and one pair per 3 square
miles of stud\ area in northern \\'voming.
Densities of Ferruginous Hawks on the study
area averaged one pair per 8 stjuare miles. Data
on population studies from other areas are lack-
ing.
Red-tailed Hawks averaged approximately
one pair per 13 scjuare miles on the study area.
Comparisons with other areas indicates these
densities to be exceptionally low. Fitch, Swen-
son, and Tillotson (1946) reported densities
of one pair per 0.5 square miles in Madera Coun-
ty, California, and Orians and Kuhlman (1956)
found densities of one pair per 2.2 and 2.8
square miles in Wisconsin. In other studies
Hager (1957) reported densities of one pair
per 2.2 s(juare miles in central New York; Le-
Duc (1970) found one pair per 1.62 square
miles in southeast Minnesota; and Luttich,
Keith, and Stephenson ( 1971 ) reported one pair
per 2.7 sfjuare miles near Rochester, Alberta.
Craighead and Craighead (1956), however, re-
corded a similar low densit>' of one pair per
12.9 square miles in Michigan but found high
densities of one pair per 1 square mile in Wy-
oming.
Comparable infonuation on the population
densities of the majority of the rest of the
raptors nesting on the study area is lacking, but
Craighead and Craighead (1956) found greater
densities of Swainson's Hawks, Prairie Falcons,
Marsh Hawks, Short-eared Owls, and Ravens
than were present in the central Utah area.
The relativelv low raptor population densi-
ties encountered in this study may be due to a
number of factors. As previously noted, ap-
proximately (me-half of the area ( i.e., much of
the inter\ening vallev floors) is not used by
any of the breeding raptors for any purpose. If
these areas are eliminated, then the relative rap-
tor population densities become more efjuitable
witli tliose of other geographic areas. In addi-
tion, tiie raptor population studies presented in
tlie literature are often representative only of a
specific or confined area, which was chosen be-
cause of its high concentration of raptors (see
Craighi'ad and Craighead 1956, p. 5; Orians
and Kuhlman 1956, p. .382), thus artificially
eliminating the bare or dead areas. Hence, the
raptor dat;i ma\- or may not be representative
of the entire area to which they are referred.
Tile Utah area regularly supports from 9 to
11 raptor species, fully as many as was found
by Craiglu'ad and Craighead (1956) in both
Micliigan and Wyoming. In addition, a broad
overlap of raptor species occurred between these
;ire;is, with fiv(^ of the ITtah stud\- area species
BiOLOCicAi, Seiues, \'ol. 18, No. 3 Bkkkding Ecology of Utah Hai'tohs
55
also present in Micliit!;an and seven in Wyoming.
The majority of the raptors on the stndy area
show a wide geographic range and exhibit con-
siderable adaptability to various habitats. That
this is not a major cause of the observed den-
sity \'ariations is also shown bv the much higher
densities of the same species in man\' areas of
their range as already noted, with the single
exception of the Golden Eagle. However, lack
of suitable cover and habitat has apparently
limited the populations of the smaller raptors,
particularly the Sparrow Hawk and Cooper's
Hawk. The latter species, although known to
nest occasionally in the pinyon-juniper com-
munity (Wolf, 1928; Bee and Hutchings, 1942),
is probabh outside of its optimum habitat. It
would appear however, that the relatively low
populations of most of the raptors in the study
area cannot be attributed to habitat factors
alone.
The lower producti\'ity of this Great Basin
Desert biome should limit the raptor popula-
tions to some extent, even though mammalian
predator control programs havt' resulted in
higher populations of lagomorphs and rodents,
the chief food source of the raptors. Additional
evidence supporting this possibility is derived
from the observed fluctuations of raptor popu-
lations in response to lagomoqih population
fluctuations, a subject which will ])e discussed
in detail later. Two important raptor species
on the stud\' area, the Golden Eagle and Ferni-
ginous Hawk, were not part of the raptor popu-
lation composition of the areas studied by
Craighead and Craighead (1956). Their size,
liome range requirements, and apparent intoler-
ance of other raptor species almost certainly
influenced the density of small raptors, par-
ticularly in view of the previously noted Golden
Eagle predation on Short-eared Owls and
Swainson's Hawks. Ferruginous Hawks appar-
ently have restricted habitat requirements and
did not nest in the riparian cottonuood com-
munities in canyons to the north and east of the
study area. Here nesting Red-tailed Hawks
maintained densities on the order of one pair
per 0.5 - 2.0 sq miles, approximately similar to
those densities reported from other parts of their
range, and furtlier indicative of the possible ef-
fects of the large and aggressive Golden Eagles
and Ferruginous Hawks.
Population Fhictuations. Variations in yearly
raptor populations were evident during the
four-year stud\'. Raptor populations were high-
est in 1969, averaging 37.8 percent above the
1967 raptor populaticm levels, while 196S and
1970 populations were intermediate. In addi-
tion, a high proportion of pairs of the 1969 pop-
ulation attempted to nest (93.4 percent), com-
pared to 87.5 percent of the 1967 population,
95.0 percent of the 1968 population, and 74.4
percent of the 1970 raptor population. These
population variations were due primarily to
yearly fluctuations of several of the large raptor
species, specifically the Great Horned Owl,
Red-tailed Hawk, Ferruginous Hawk, and
Swainson's Hawk and were apparently inde-
pendent of the relatively stable populations of
the medium- and small-sized raptors.
The tendency of pairs to reoccupy nesting
sites and territories has the effect of stabilizing
the raptor population. This tendency is ap-
parently prevalent in almost all raptor species.
Craighead and Craighead (1956) reported that
almost 75 percent of the raptor pairs in the
Michigan and Wyoming study areas reoccupied
their same nesting vicinity. Elsewhere, Luttich,
Keith, and Stephenson ( 1971 ) reported that
only 12.4 percent of their Red-tailed Hawk
pairs built a new nest during the four-year
study near Rochester, Alberta, and both Hagar
(1957) and Orians and Kuhlman (1956) ob-
served numerous instances of Great Horned
Owls and Red-tailed Hawks reoccupying their
nesting sites or territories of the previous year.
Cade ( 1960), and more recently. White (1969b)
have expressed the opinion that a traditional or
"genetic" linkage may be responsible for the
almost continuous occupanev of certain cliffs
or locales by Peregrine Falcons ( Falco pere-
grintis) in Alaska, and Herbert and Herbert
( 1965 ) have suggested the same of falcons in
the New York City region. Conceivably, such
a tradition may apply to other raptor species
equally as well, and nesting locales may be re-
used continuously for long periods of time. Nest
decay and disintegration in this area of the
Great Basin is remarkably slow, and nesting
sites which were photographed in 1941-1944 by
Robert G. Bee (Unpubl. notes, BYU Life Sci-
vnccs Museum) were still present and in some
cases in use by the same species in 1967-1970,
suggesting a similar trend towards long tenn oc-
cupancy of a particular site.
Nest Site
Coiiijxirisoius with Other Geographic Areas.
The 12 raptor species nesting on the study area
show a wide variation in nesting selection
throughout their geographic range. In this por-
tion of the Great Basin the majority of Golden
l]agle iK-sts are located in cliffs ( 100 percent
in the study area) but Murphy, et al., (1969)
recorded a few built on artificial structures or
56
UnicHAM VouNG University Science Bulletin
dirccth' on the groiiiul, and Bcc and Uutchings
(1942) reported Golden Eagles nesting in juni-
pers and Douglas fir. In southern California,
Dixon (1937) found Golden Eagles nesting al-
most exclusively in cliffs, oaks, or eucal)ptus
trees. Carnie (1954) also found Golden Eagles
nesting in both cliffs and trees in the coastal
ranges of California. Elsewhere, Wellein and
Ray (1964) reported that in Colorado, New
Mexico, and Wyoming 87 percent of their Gold-
en Eagle nests were in cliffs, 11 percent in trees,
and 1.3 percent wi-re on the ground. In Sas-
katchewan, Whitfield et al. (1969) noted that
all Golden Eagle uests were constructed in
cliffs. In Scotland, Watson (1957) found 70
percent of the Golden Eagles nesting in cliffs
and 30 percent in trees, but Gordon ( 1955) indi-
cates that the majority of nests in the central
Highlands are in trees, and in cliffs in the
Hebrides.
In this area 59.3 percent of the Great Horned
Owl nests were in cliffs, 25.9 percent in quarries,
and 14.8 percent in junipers, but in the eastern
portion of their range most nest in trees. Orians
and Kuhlman (1956), LeDuc (1970), and others
have recorded all (heat Horned Owls nesting
in trees. In studies from the western portion
of the range, Dixon (1914) found Great Horned
Owls in California utilizing cliff sites and Fitch
(1947) reported a ground site in Madera Coun-
ty, California. In Utah, Sugden ( 1929) reported a
Great Horned Owl nesting in the ruins of Indian
cliff dwellings, and Bee and Ilutchiugs (1942)
found nests in junipers, ccjttonwoods, quarries,
and directly on the ground.
On the studv area. Ferruginous Hawks nested
in trees, primarily jimipers, (69.4 percent) and
on the ground. Cameron (1914) in Montana
and Bowles (1931) in Washington have de-
scribed ground nests of the Ferruginous Hawk
and Jacot (19.34) found a bulky nest in a 34-
foot c-edar. Bent (19.37) reported Ferruginous
Hawks nesting in swamp oaks in North Da-
kota. In Canada, Godfrey ( 1966 ) describes
nesting sites in trees, ledges, river cutbanks,
and on hillsides. Augell ( U)68) observed a Fer-
ruginous Hawk nest built on a slight cliff ledge
in Franklin County, Washington. In central
Utah, Bee and Hutchiugs (1942) found Ferni-
ginoiLS Hawks nesting predominatelv in junipers
but noted that they also nest in tall trees and
cliff ledges.
The nesting site selections of Hed-tailed
Hawks show wide variations throughout their
range. On the study area 54.5 percent of their
nests were constructed in tr<'es, 36.4 percent in
cliffs, and 9.1 percent in (|uarries. In other parts
of the state. Wolf (1928) reported them nesting
in trees and cliffs and Hardy (1939) describes
a Red-tailed Hawk nest constructed on a pinna-
cle ill the Book Cliffs of central Utah. Else-
where tlu-oughout most of their range, they most
commonly nest in trees. In California, Fitch,
Swenson, and Tillotson (1946) recorded all 18
pairs oi their Red-tailed Hawks nesting in trees,
as did Orians and Kuhlman (1956) in Wiscon-
sin; Hagar (1957) in central New York; Free-
meyer (1966) in Lyon County, Kansas; Tyler
and Saetveit (1969) in South Dakota and Iowa;
and LeDuc (1970) in southeast Minnesota.
However, they will evidently nest in any avail-
able site, and Dixon and Bond (1937) found
eight pairs nesting in the Petroglyph Cliff area
in northeastern California.
All Swainsons Hawk nests on the study
area were constructed in low junipers in the
foothills. Wolf (1928) and Bee and Hutchings
( 1942) also found this to be the same site
preference for their Swainsons Hawk nests. In
Montana, Cameron (1913) found Swainson's
Hawks nesting in a variety of low trees, but
primarilv in ash and cottonwoods.
Two of the three Prairie Falcon nests on
tlie study area were located in quarries and the
third was located in a limestone cliff crevice.
Cliff nesting appears to be the rule for this
species throughout its range, and no exceptions
seem to have been recorded. Burrowing Owls
similarly show few deviations from the typical
burrow nest site. Both Marsh Hauks and Short-
cared Owls are more commonly found nesting
around water. Bent (19.37) describes a number
of nests located in marshes and swamps in
Massachusetts, North Dakota, and New Jersey.
Bent also notes that J. W. Sugden wrote him
of a Marsh Hawk nest site in a dry wheat field
at least four miles from water in Salt Lake
County, Utah.
All of the Sparrow Hawks on the study area
nested in holes and crevices of structures, quar-
ries, or junipers. Hole nesting is apparentlv
mandatory for this .species and the majorit\' of
sites reported in the literature are of this type,
although the cavity may take the fonii of a
nesting box ( Heintzelman, 1964).
Ra\-ens on the stud\- area nested in high re-
mote cliffs, but Bee and Hutchings (1942)
also found their nests in mining structures and
tri'es. Elscnvherc. Ra\'eiis hav(> shown e(|ual if
not greater adaptai)ilit\-. In Washington, Bowles
and l^ceker (19.30) found Ravens nesting in
clilf potlioles, aband(;ned houses, on telephone
poles and oil derricks, and among the beams
of a railroad trestle. Rent (1946) recorded 13
Biological Skuii:.s, \'t)L. 18, No.
BiitEDiNG Hi:()Loi;v of Utah Rai'tors
57
of 17 nests in cliffs or ledges, and the remain-
ing 4 in conifers var\ing from 45-85 feet. In
the north they nest in cliffs or ledges, often
in close proximity to Peregrine Falcons and
Rough-leggetl Hawks (Fay and Cade, 1959;
Cade, 1960). In England they commonly nest
in high cliffs or in both deciduous and conifer
trees "^(Holyoak and Ratcliffe, 196S).
Differentiation amonp, Species' Nest Sites.
The revieu' of the literature presented above
suggests that these raptor species show a wide
range of nesting site selection throughout the
\arious portions of their geographic range. Yet
in areas where they nest together, such as here
in central Utah, both similarities and subtle
differences may be present. The similarities
observed are, of course, to some degree a func-
tion of the uniformity of the habitat. For the
larger raptor species, and many of the smaller
raptors also, the foothills and hills lying between
large expanses of surrounding desert provide
the most attractive of the potential nesting sites,
offering at once a combination of remoteness,
inaccessibility, and surveillance of possible ap-
proaches. All of the raptors except the Marsh
Hawks and Burrowing Owls nested most often
in junipers or cliffs, which simph represent the
predominant form of available nesting sites.
.Some species, however, selected a narrower
range of nesting sites than did others.
Both Ferruginous Hawks and Swainson's
Hawks apparenth required a restricted form of
nesting habitat. Both nested exclusively on the
low foothills surrounding the perimeters of the
\'allevs and in low junipers which were either
isolated or situated on the fringes of the pinyon-
juniper woodland. Ferruginous Hawks particu-
larly seemed to prefer isolated knolls and tended
to nest at higher elevations than Swainsons
Hawks. Three such knolls present in the south-
eastern corner of the studv area were each con-
tinuously occupied by a bre("ding pair of Fer-
ruginous Hawks during the four study years.
Observations of nesting sites in adjacent locales
reinforce this conclusion.
In contrast, Creat Homed Owls and Red-
tailed Hawks showed a much wider selection
of nesting sites. Both commonly nested in cliffs,
quarries, or trees but these sites tended to be
more remote than those of the Swainson's Hawk
and Ferruginous Hawk. Both appeared to pre-
fer nesting sites in long cliff lines or within
canyons over the more exposed tree sites, in
contrast to the Ferruginous Hawks and Swain-
son's Hawks, neither of which nested in can-
vons or on high cliffs. However, tree sites
were occasionalK used, and Great Homed Owls
sometimes nested in abandoned Ft^rruginous
Hawk juniper nests, such exposed sites utilized
only if they were removed from active Ferru-
ginous Hawk nests and territories. Although
Great Horned Owls did on occasion nest in rela-
tively close proximity to active Ferruginous
Hawk nests (average distance of 0.766 ± 0.16
miles, minimum of 0.21 miles), these close nests
were always within cliff crevices and relatively
unexposed. Neither Great Homed Owls nor
Red-tailed Hawks nested in thick pinyon-juniper
woodlands, preferring instead to nest in semi-
isolated junipers or within 50-70 feet of the edge
of the woodland. On the other hand, some
differences between the two species were ap-
parent. Great Homed Owls tended to nest at
slightly higher elevations than Red-tailed Hawks
and preferred to nest within crevices or caves,
whereas Red-tailed Hawks usually nested on
cliff ledges.
Golden Eagle nesting sites overlapped con-
sideiablv with those of Prairie Falcons and Rav-
ens and, to a lesser extent, with Great Horned
Owls. Both Golden Eagles and Prairie Falcons
always chose cliff or quarry nesting sites, which
may reflect their need for high cliffs; a pair of
Falcons nesting in 1970 utilized a Golden Eagle
quarr\' nest \\'hich had been constructed the
previous vear.
Of the remaining raptors, the Cooper's Hawk
showed virtually no overlap in its choice of nest-
ing sites. No other raptor nested within thick
pinvon-juniper woodlands and at such high ele-
\-ations. In contrast. Short-cared Owls and
Marsh Hawks both exhibited similar choices in
nesting sites with both nesting in rabbitbrush-
sagebrush stands on the desert floor. Burrowing
Owls similarly nested on the valley floor, but
achieved a measure of isolation owing to their
utilization of buiTOws for nests.
Sparrow Hawk nesting sites overlapped with
none of the medium- and small-sized raptor
species on the study area. Sparrow Hawks most
commonly nested in and around human struc-
tures. They did not nest directly on the valley
floors except at higher elevations and in juniper
cover.
Statistical comparisons of the average nest-
ing elevations of the raptor species reinforce
the above statements. Analysis of variance tests
indicate that the average nesting elevations of
the five large raptor species differed significantly
(p<0.01, "F" = 19.1). Paired "t" tests reveal
that all possible differences are significant ex-
cept between the CJreat Horned Owls and
Golden Eagles. However, although these two
species show much overlap in nest site elcva-
58
Biiir.iiAM YdUNG University Science Bulletin
tion, it has already been sliown that they prefer
different sites.
Siniihir analysis of variance tests of the five
medium- and small-sized raptor species for which
sufficient comparative data is available also
show significant differences in their average
nesting elevations but only at p<0.05 levels
("F" = 12.2). Most of the lesser variation is
attributable to die essentially similar nesting
site elevations of Marsh Hawks, Short-eared
Owls, and Burrowing Owls as discussed pre-
viously; and paired "t" tests between those species
most likely to be competitive revealed signifi-
cant differences in nesting elevations between
all medium- and small-sized raptors, with the
three exceptions noted. The other three species,
i.e., Prairie Falcon, Cooper's Hawk and Raven,
nested in sites similar to those of the large rap-
tor species (cliffs and/or at high altitudes).
Comparisons lietween these and the cliff-nesting
Red-tailed Hawks, Great Horned Owls, and
Golden Eagles reveal that there was no signifi-
cant difference in average nesting elevation be-
tween Prairie Falcons and Golden Eagles, but
Ravens and Cooper's Hawks nested at signifi-
canth- iiigher eknation than Golden Eagles,
Great Horned Owls, and Ri^d-tailed Hawks.
Populations and Breeding Habitat Require-
ments. Although Ferruginous Hawks were the
predominant raptor species on the study area,
their abundance was confined to certain locali-
ties which can be readil\- described topographi-
cally and, to an extent, by the physiognomy of
the surrounding vegetation. In areas where the
optimum conditions were absent, their numbers
dwindled rapitlly and tliey were replaced by
the Red-tailed Hawk. Red-tailed Hawks in turn
were apparently incapable of displacing Ferru-
ginous Hawks from the foothill rdgions, although
thev were present in immediately adjacent lo-
cales if a suitably different nest site (i.e., a
cliff or steep-sided canyon) was available. This
situation is strikingh- evident in areas where
the two species nest in close proximity (<1.0
miles apart).
Woodbury and Cottam (1962) liave de-
scribed the various ecological habitats of Utah,
and it miglit Ik' useful to examine the presence
and relative populations of the raptor species
within those habitats occurring in the study area
and surrounding localities. The applicable habi-
tat tvpes of Woodbury and Cottam include tiie
following: pigmy conifers, present o\er all of
the high<-r, better drained portions of tlie study
area and adjacent locales; desert scrul), present
over the lower elevations of Cedar and Rush
valleys; canvonlieads, present in tlic liiglier
mountain ranges immediately north and south
of the study area; and cultivated valleys, not
one of Woodbury and Cottam's original habitat
tvpes, but nevertheless present over a large por-
tion of Cedar N'allev northeast of the study area.
Six of the raptor species nested within the
pinyon-juniper habitat, but all spent some if
not most of their limiting activity periods in the
adjacent desert areas. Of these tlie Cooper's
Hawk appears to belong most exclusively within
the woodland, nesting in relatively dense stands
and hunting primarily in the lightly wooded
areas or o\er small hill-top meadows. In con-
trast, lioth the Swainson's Hawk and Ferru-
ginous Hawk are the least exclusive members,
nesting on its fringes, or as in the case of the
Ferruginous Hawk, in the transitional area be-
tween pigmy conifers and desert scrub. Ferru-
ginous Hawks constructed almost one-third of
their nests within the desert scrub commimity,
well beyond the limits of the woodland, and
thev achieve their maximum populations in such
localities.
Raptors associated with the desert scrub
community in tiie study area include Marsh
Hawks, Short-eared Owls, and Burrowing Owls.
These species all nested on the valley floors at
essentially the same altitude and appeared to
be restricted to tiiis community. However, all
other raptors except the Cooper's Hawk hunted
within tiiis community.
The predominant raptors nesting in canyons
included Great Horned Owls and Red-tailed
Hawks (Fig. 24). Canyons apparently pre-
cluded Ferruginous Hawks and Swainson's
Hawks in some way, as neither attempted to
nest within this habitat type, either on the
study area or in adjacent locales. Large can-
yons to the northeast supported dense popula-
tions of nesting Red-tailed Hawks, with nesting
pairs a\eraging 0.5 linear miles apart in years
of maximum populations.
The cultivated land northeast of the study
area also differed in raptor spi'cies composition
and relative populations. Here Sparrow Hawks
and Magpies were the most common raptorial
forms, with both utilizing the windrows of eot-
tonwoods for nesting sites. Red-tailed Hawks
and Great Honu'd Owls infre(]uentl\' nested
here also; such nests were usualh' disrupted or
destro\('d by humans before completion of the
e\ele.
Productivity
C.lulcli Size Comparisons. Comparisons with
other populations indicate slight variations in
a\-eiage eluteh size of most of the study area
Biological iliauEs, \'ol. IS, No. 3 Bul'.edinc; Ecology oi' Utah ll,-\rTons
59
P
1
Fig. 24. Great Horned Owl nest in West Canvon, March 1969. The nest was constructed the previous
year bv Red-tailed Hawks.
raptors, but the majority are in.significant. Con-
sequentlv, a few comparisons should suffice.
Yearly Golden Eagle clutches on the study
area averaged 2.07 ± 0.07 eggs. In a series of
studies in Cahfornia Dixon ( 1937 ) reported av-
erage clutches of 2.0 eggs, Hanna (19.30) found
an average clutch size of 1.7 eggs, and Slevin
(1929) found an average clutch size of 1.95
eggs for 21 clutches. In Scotland Gordon (1927)
reported an average clutch size of 1.91 eggs
per clutch for 82 clutches. Jollie (1943) found
1.8 eggs per clutch for five clutches in Colorado,
and more recently McGahan ( 1968 ) recorded
an average clutch size of 2.1 eggs for 20 nests
in Montana.
Great Homed Owl clutches on the study
area averaged 2.82 ± 0.15 eggs. Surprisingly,
only a few studies are available for comparison.
Craighead and Craighead (1956) reported aver-
age clutch sizes of 1.9 eggs in Michigan and
2.2 eggs in Wyoming. Wolhuter ( 1969 ) reported
an average clutch size of 1.9 eggs for nine nests
near Lawrence, Kansas, and Tyler and Saetveit
( 1969 ) reported average clutches of 2.0 eggs
for three nests in South Dakota and Iowa. In-
terestingly, all are significantly lower than the av-
erage Great Horned Gwl clutches of this area(t
= 5.43 for the Kansas comparison, t := 5.54 for
the South Dakota and Iowa comparison, and t
= 4.49 for the Wyoming area comparison).
Insufficient comparative data is available
on the average clutch size for Ferruginous
Hawks.
Red-tailed Hawk clutches on the study area
averaged 2.89 ± 0.13 eggs. In Michigan, Craig-
head and Craighead (1956) recorded average
clutches of 2.0 eggs, but in Wyoming an average
of 2.3 eggs per clutch was found. Elsewhere,
Freemeyer (1966) found an average clutch size
of 1.9 eggs for 21 nests in Kansas; LeDuc ( 1970)
foimd an average of 2.3 eggs per clutch for
three nests in Minnesota; and Luttich, Keith,
and Stephenson ( 1971 ) reported an overall av-
erage of 2.0 ± 0.1 eggs per clutch in Saskatche-
wan. Paired "t" tests indicate that the average
clutch sizes recorded from this study are signifi-
cantly larger than the overall average clutches
of each of the other areas noted above.
Swainson's Hawk clutches on the study area
averaged 2.2 ± 0.17 eggs. In the only other
60
Bricham Young University Science Bulletin
informative study available Cameron (1913)
found an average cluteh size of 2.6 ± 0.67
eggs in Montana, significantly higher than those
from this area.
The single Prairie Falcon clutch contained
5.0 eggs. Craighead and Craighead (1956) re-
ported average Prairie Falcon clutches of 5.0
eggs in Wyoming, but Enderson (1964) found
an average clutch size of 4.5 eggs for 55 nests
from the intemiountain area.
Marsh Hawk clutches on the study area
average 5.0 ^t 1.4 eggs. Elsewhere, Hammond
and Henry (1949) in a three-year study in
North Dakota found a range of 4.87 ± 0.806 to
5.25 ± 0.774 eggs per clutch for 60 clutches,
while Craighead and Craighead (1956) found
average clutches of 4.35 eggs per clutch in
Michigan, and Sealey (1967) reported an aver-
age clutch size of 4.18 eggs for 21 nests in Al-
berta and Saskatcliewan.
The single Short-cared Owl clutch contained
7 eggs. In other areas Goelitz (1918) reported
an average clutch size of 7.3 eggs for four nests
in Saskatchewan, but Kitchin (1919) found an
average clutch size of only 3.5 eggs for seven
nests in western Washington. At the northern
edge of the range, Pitelka, Tomich, and Treichel
(1955a, 1955b) reported an average clutch size
of 6.8 eggs for 22 clutches.
Sparrow Hawk clutches in tlie study area
averaged 5.22 ± 0.38 eggs. In Michigan and
Wyoming their average clutch sizes were 4.4
eggs (Craighead and Craighead, 1956). Rocst
(1957) indicates an average clutch size of 5.1
eggs irt Oregon, and Heintzelman and Nagy
(1968) found an average clutch size of 4.23
eggs for 13 nests in Pennsylvania. In experi-
mental propagation studies, Willoughby and
Cade ( 1964 ) reported an average clutch size of
3.66 eggs for 12 clutches.
Raven clutches on the study ari-a averaged
5.36 ± 0.34 eggs. Comparatively, Craighead
and Craighead ( 1956 ) found mean clutch sizes
of three nesting pairs in Wyoming to average
5.7 eggs. In England, Hatcliffe (1962) reported
an average clutch size of 4.6 eggs for 139 nests.
Hatchin<i Success. From 1967-1970, 14 nest-
ing efforts of Colden Eagles produci'ti 1.2 young
per nest for an overall hatching success of 70.8
± 14.9 percent. Comparatively, Wellein and
Ray (1964) reported 1.59 voung iiatched per
nest for 23 nests in the southern l^ockies, and
McGahan (1968) found an average of 1.59
young per nest hatched in Montana. In central
Saskatchewan, Whitfield et al, (1969) found
an average of 1.8 young per nest from six
nests.
(Jreat Horned Owls on the study area
hatched an average of 2.5 young per nest per
year. Elsewhere, Craighead and Craighead
(1956) reported a two-year average of 1.42
young per nest in Michigan and 2.0 young per
nest hatched in Wyoming. Orians and Kuhlman
(1956) reported an average of 1.4 young per
nest in Wisconsin while Hagar (1957) found
average broods of 1.9 young per nest during
his two-year study in central New York. More
recently, Marti (in Adolphson and Jonkel, 1969)
reported an average of 2.4 young per nest for
13 nests in Colorado; Dunstan (in Adolphson
and Jonkel, 1969) found 1.9 young in 11 nests
in South Dakota; and Adolphson and Jonkel re-
ported 1.96 young per nest for 21 nests, also in
South Dakota.
Ferruginous Hawk nests on the study area
averaged 65.2 ± 5.2 percent hatching success for
an average of 2.3 young per nest. In the onlv
comparative study Adolphson and Jonkel (1969)
reported 2.66 young fledged from three nests,
but the hatching success is not given.
Red-tailed Hawks on the study area hatched
76.7 ± 3.9 percent of all eggs produced for an
average of 2.3 young per nest per year. Else-
where, Craighead and Craighead (1956) found
an average of 1.3 young hatched per n(>st in
Michigan and 2.1 young hatclied per nest in
Wyoming. Hagar ( 1957 ) reported an average
brood size of 1.9 young per nest in New York
and Luttich, Keith and Stephenson ( 1971 )
found an overall hatching rate of 1.9 young
per nest of 75 nests in ,'\lberta.
Swainson's Hawks on the study area averaged
2.2 young hatched per nest per year. Compara-
tively, Craigliead and Craighead (1956) reported
an a\'eragc of 1.25 young hatched from four
clutches in Wyoming.
The Prairie Falcon nest on the study area
hatched 3 of 5 eggs. Elsewhere, Craigliead and
Craighead ( 19.56 ) ft)und all five eggs of a nest
in Wyoming hatched, but more recently Ender-
son (1964) found onlv 1.9 voung hatched per
nest studied.
The two Marsh Hawk nests hatched an av-
erage 3.5 young per nest. Coniparati\'e!v, Ham-
mond and Henry (1949) reported an axeragc
iiatching rate of 4.07 young piT nest for 60
nests in North Dakota, Craighead and Craig-
head (1956) found a very low hatching rate of
1.4 young per nest for 13 nests in Michigan,
and Sealey (1967) found an average of 1.55
young hatched per nest for II nests in Alberta
and Saskatchewan.
From 1968-1970 Sparrow Hawks on tlie study
arc;i hatclii'd an a\'erage of 4.7 young per nest.
Biological Sehies, \'ol. 18, No. 3 BiiELniNc: Ecology of Utah ri.\PTORs
61
In other areas, Craighead and Craighead (1956)
found an average of 2.5 young hatched per nest
in Mieliigan and 4.3 young hatched in Wyo-
ming. In another study, Ileiiitzehnan and Nagy
(196S) reported 3.29 young hatched per nest
for 13 nests in central Penns)'lvania.
Ravens produced an average of 3.64 young
per nest on the study area. In their study,
Craighead and Craighead (1956) reported an
average of 5.0 young hatched per nest for
three nests in Wyoming.
Fledging Rates. During the four-year study.
Golden Eagle nests fledged an average of 1.0
young per nest. Elsewhere, ^Vellein and Ray
( 1964 ) recorded an a%'erage of 1.32 birds fledged
per nest from 23 nests in the southern Rockies,
and McGahan (1968) found an average of 1.37
young fledged per nest from 45 successful nest-
ings in Montana. In a series of studies in Scot-
land, Watson (1957) found an average of 0.8
yoimg fledged per nest over a twelve-^ear
study period, Sandeman (1957) recorded 1.4
young fledged from 19 successful nests, and
Brown and Watson (1964) reported 1.3 young
per nest from 19 successful nests. Recently,
Dunstan (in Adolphson and Jonkel, 1969) found
an average of 1.67 Noung fledged per nest from
21 nests in South Dakota.
From 1967-1970 Great Horned Owl nests
fledged an average of 2.0 young per nest for
27 nesting efforts. Comparatively, Craighead
and Craighead (1956) found an average of
0.55 young fledged per nest in Michigan and
2.0 fledged per nest in \\'yoming; Orians and
Kuhlman (1956) reported an average of 1.87
voung fledged per nest in Wisconsin; and Hagar
( 1957) recorded an average of 1.7 young fledged
in New York. Recently, Wolhuter ( 1969 ) found
an average of 1.5 young fledged per nest in
Kansas.
Ferruginous Hawks fledging rates averaged
2.0 voung per nest. In comparison, Dunstan
(in Adolphson and Jonkel, 1969) reported an
average of 2.66 \<)ung fledged per nest for three
nests in South Dakota.
Red-tailed Hawks fledged an average of 1.74
voung per nest on the study area. Compara-
tively, tliis is higher than Craighead and Craig-
head (1956); Fitch, Swenson, and Tillotson
(1946); LeDuc (1970); and Luttich, Keith and
Stephenson ( 1971 ) ; but this is lower than the
overall average of 1.9 xoung fledged per nest
reported by Orians and Kuhlman (1956) and
Hagar (1957). Ellis in Florida and Dunstan in
South Dakota (in Adolphson and Jonkel, 1969)
found an average of 1.2 young and 2.5 young
fledged per nest, respectively, for each of the
two areas, with the latter data obtained from
20 nests. Jonkel (in Adolphson and Jonkel,
1969 ) reported an average of 0.52 young fledged
per nest for 31 nests, also in South Dakota.
Swainson's Hawks on the study area fledged
an average of 1.4 young per nest. Craighead
and Craighead (1956) found only 0.4 young
fledged per nest for five nests in Wyoming.
Recently, Adolphson (1969) found an average
of 2.0 young fledged per nest in South Dakota.
The Prairie Falcon nest fledged only one of
three young. In Colorado, Enderson (1964) re-
corded an average of 1.2 \oung fledged per
pair and Sealey (1967) reported an average
of 2.5 young fledged per nest in southern Al-
berta.
The four Marsh Hawk nests of 1969-1970
fledged an a\'erage of 2.5 young per nest. Else-
where, Hammond and Henr)' (1949) reported
an average of 2.1 young per nest fledged in
North Dakota, and Craighead and Craighead
(1956) found a very low fledging rate of 0.17
young per nest in Michigan for 13 nests.
From 1968-1970 Sparrow Hawks on the
study area fledged an average of 2.83 young per
nest. Comparatively, Craighead and Craighead
( 1956 ) found an average fledged rate of 3.4
young per nest in Michigan and 3.8 young per
nest in W\'oming.
The six nests of the Burrowing Owl on the
study area fledged an average of 3.33 young
per nest. In comparison, Grant (1965) esti-
mated a rate of 3.83 voung fledged per nest
in Minnesota.
Ravens fledged onl\' 2.57 voung per nest
on the study area. Craighead and Craighead
( 1956 ) found an average of 3.3 voung fledged
per nest in Wyoming.
Si/nopsis of Mortoliti/ and Populiifion Trends.
As is evident from the comparison of the rela-
tive hatching success and mortality data with
other studies, no significant differences exist
and most of the variations existing are within the
ranges reported from this study. The same holds
true also for the majority of the causes of mor-
tality, with nest desertion, egg infertility, and
human interference being the principal causes
of the obser\'ed mortality of eggs and voung.
There was no evidence of any mortality of voung
or eggs attributable to mammalian predation,
even though ground nests of Ferruginous Hawks,
Red-tailed Hawks, and Golden Eagles (the lat-
ter outside the study area l)ut within the same
habitat type) were directly accessible, and sev-
eral carnivores, including coyotes, bobcats, kit
foxes and mountain lions were present in the
study area. Angell (196S) reported a Ferru-
R2
limtMiAM VouNG Univehsity .S(:ienc;k Bulletin
ginous Hawk pair successfully defending their
brood against an intruding coyote, which sug-
gests that these raptors are little troui)led l)\
such mammals. A\ian predation could be an
important factor, but it was actualh' only ob-
ser\-ed in the two cases of Golden Eagle preda-
tion on otlier raptors, as previously mentioned.
Territoriality
Co))i])iirisoii.s iiith Other Areas. Compara-
tive information on home range size is available
from a tew published sources.
Golden Kagles on the study area maintained
average home ranges of 9.02 sq miles. This is
almost equivalent to the 9.0 sq miles of territory
reported by Watson (1957) for five pairs in
Scotland; however. Brown and Watson (1964)
found average Golden Eagle home ranges \ary-
ing from 20 to 34 sq miles.
Great Horned Owls on the study area main-
tained a\-erage home ranges of 2.02 sq miles.
Comparaliveiy, Miller (1930) observed that
Great Horned Owls maintained an irregular
shaped territory, with the largest diameter of no
more than one-half mile, while Baumgartner
(1938) found Great Horned Owl territories to
haw a diameter of 0.5 miles. Craighead and
Craighead (1956) found h)ur pairs near Moose,
Wyoming, to ha\e an average home range of
0.82 ± 0.15 s(| miles, or roughly half that of
the owls in central Utah.
Red-tailed Hawk home ranges on the study
are, I a\eraged 2.5 s([ miles. Fitch, Swenson, and
Tillotson (1946) reported that 6 Red-tai'ed
Hawk territories in Ga!ih)rnia chaparral ranged
from onh 0.125 — 0.313 sq miles, but it is
possible tliat peripheral areas were not included
in their d-ti'rminations. Craighead and Craig-
head ( 1956 ) reported somewhat larger home
ranges of six pairs in Michigan, which averaged
1.45 ± 0.21 s(| miles. In Wvoming, they found
eight pairs ha\ing average home ranges of 0.731
-+: O.ll S(( miles.
There is no apparent comparative data for
the home ranges of Ferruginous Hawks and
Short-eared Owls.
Swainson's Hawk home ranges on the stud\
area axcrageil 1.51 s(i miles per pair. (Craighead
and Craighead (19.56) reported an a\(Mage of
0.95 ± 0.55 for five pairs.
Prairie Falcons on the stud\ area a\eraged
2.35 s<i miles in iiome range size. This is much
smaller than the 9.96 s(( miles Craighead and
Craighead (1956) reported for a pair in Wy-
oming.
Marsh Hawks on the stud\' area n^aii taii;ed
average home ranges of .68 S(| miles. In Mi iii
gan, Craiglieatl and Craighead (1956) reported
tlie home ranges of 11 Marsh Hawk pairs as
0.974 ' 0.17 s(i miles.
Burrow iug Owls on the studv area averaged
0.32 s(i miles in their home range coverages.
CJrant (1965) reported territorial sizes of 0.025
and 0.019 s(| miles for two pairs in Minnesota
and snggi'sted that pairs in colonies maintained
liome ranges of 0.016 to 0.028 s([ miles.
Sparrow Hawk home ranges of the study
area a\iiaged 0.29 sfj miles. Comparatively,
Craighead and Craighead (1956) reported aver-
age home ranges of 0.504 it 0.15 scj miles for
five pairs in Michigan and 0.78 ± 0.14 sq
miles for 11 pairs in Wyoming.
Ra\'ens on the studv area possessed average
home ranges of 2.53 sq miles. Comparative data
from Moose, ^^'yoming, indicates that average
home ranges of three Raven pairs were 3.62 ±
0.4 s(| miles (Craighead and Craighead, 1956).
Home Raiii^e Characteristics. Characteris-
tically, the home ranges of raptors on the study
area extended well out into the desert, which
serves as their principal hunting area. Some of
the study area, however, was imused; that is, it
contained no portions of an\' raptor home ranges.
Such imused areas were t\pically far from any
potential nesting sites and apparently undesir-
able in terms of food resources. Undoubtedly,
raptors which ha\e to travel less to provide suf-
ficient food for their young are more efficient
in their reproductive efforts, and it is probable
that these peripheral areas are seldom, if ever,
utilized.
The rugged topography of the study area
plued an importai t role in preventing more
frecpient intraspecific coiitaets and actually al-
lowed two raptor populations to e.xist, one on
each side of the centralK" located hills.
Intraspecific and interspecific home range
o\er!aps and distances between active nests ap-
peared to be a function of several factors, in-
ehuling tolerance antl population densities, spe-
cific nesting site selection, and actixity patterns.
Intraspecific home ranges only slightly over-
lapped, if at all (except in the Burrowing Owl
case), and never o\erlapped in the \'icinit\' of
the nest sit(\ Inti-rspecific home range o\'erlap
was more common. Thus, home ranges of
CJolden I'^agles, CJreat HonKxl (h\ls, l'\'rruginous
Hawks, Swainson's Hawks, and Ra\ens all over-
lapped to some extent in amounts pre\iously
noted. Within this large raptor group, however,
home range o\'erlaps between members of the
same gemis, e.g., Biiteo. were less extensive than
l)etw(X'n relativeU' u^ related raptors. Hence
hntli t^dldei Kag'e aid Havei home ranges
BioLor.icAi. Sehien, N'ol. IS. No. .'3 Bueedinc Kcoi.ogv :w Ut.mi R.\ptoks
6.3
showed \irtuallv 100 per cent o\'erlap with some
pairs of Ferruginous Hawks and Red-tailed
Hawks, and in one year with Swainson's Hawks
also. However, the actual nest site of each of
these diurnal raptors w as relatively far removed
from nest sites of other species, and their flight
patterns indicated a form of altitudinal terri-
toriality which pemiitted movement to their
more commonly utilized hunting areas.
Home range overlaps between Great Horned
Owls and other raptors were common and often
extensive. In addition, their average distances
to nearest interspecific neighbors were the low-
est of any of the large raptors on the study area.
That this is a reflection of their acti\ity patterns
is indicated by the aggressiveness with which
other raptors react to their presence when
flushed. Ob\iously then, Great Horned Owls
are able to take advantage of a large portion
of the total habitat available compared to the
diurnal Buteos because of the direct absence
of interspecific territorial competition, although
their populations are smaller than those of the
Ferruginous Hawk.
Most of the smaller raptore on the study area
nested within the home ranges of one or more
of the larger raptors and occasionally, as pre-
viously noted, were pre\ ed upon by them. Home
ranges of these smaller raptors seldom over-
lapped between two species of comparable size,
e.g., the Sparrow Hawk and Burrowing Owl,
but much variation occurred in other cases. Bur-
rowing Owls displaced the greatest interspecific
tolerances, but their differing activity patterns
contributed to the allowance of their observed
home range overlaps with Marsh Hawks. Simi-
larly, the close nesting and high degree of over-
lap between Marsh Hawk and Short-eared
Owl home ranges can also be attril)uted to dif-
fering activity patterns which pre\ented direct
confrontation between the two species. Marsh
Hawk pairs were generally tolerant of intra-
specific and interspecific home range overlaps.
Raven pairs, however, tolerated little intraspe-
cific home range overlap even though their large
home ranges overlapped considerably with other
species.
Relationship of Speciei' Home Raniie Sizes.
With few exceptions there is an e\ident rela-
tionship between raptor weight and territorial
size, with the Sparrow Hawks maintaining the
smallest and Golden Eagles the largest observed
home ranges. Schoener (1968) has shown a
strong relationship between territorial size and
body weight iov a number of herl)i\'orous and
predatory bird species. The determination of a
similar regression of bodv weight to territorial
size in the raptors results in a positive slope of
0.0022 ± 0.0004, significantly larger than zero
(t = 9.36) at the 0.001 level (Fig. 25). This
suggests that their larger bodv weights require
higher energy budgets, which in turn necessi-
tate larger home ranges to provide adequate food
supply. The slightly smaller home ranges of the
Ferruginous Hawks and Swainson's Hawks (com-
pared to those raptors of similar size, such as
the Great Horned Owl and Red-tailed Hawk)
may reflect their nesting site preferences which
place them nearer to their prey source in
the \'alleys. On the other hand, the relatively
large home ranges of the Prairie Falcons do not
appear to be explicable, except perhaps in
terms of the wide-ranging food procurement of
tills raptor.
Relationship between Home Range Sizes
and Raptor Population Densities. Home ranges
of the Great Horned Owl, Red-tailed Hawk, and
Swainson's Hawk on the study area are, on the
whole, much larger than those recorded in
studies from other regions, suggesting that these
desert-nesting raptors range more widely for
food. The increased home range sizes may also
reflect the nature of the habitat, which provides
nesting sites in the hills and foothills and there-
by promotes the location of nests on the perime-
ter of the home range. Another aspect of the
relatively larger territories may relate to the
low population densities of these central Utah
raptor populations. The 1970 home ranges of
Great Horned Owls, Ferruginous Hawks, Red-
tailed Hawks, Marsh Hawks and Ravens were
larger than the comparable home ranges of the
denser 1939 populations of these species, but the
1500
Raptor weight in gms.
Kif^. 2,5. Hflationship between raptor weight and terri-
torial size. Niimlier.s refer to raptor .species as
previously noted.
64
HiuciiAM Young Univeusiiy Science Bulletin
diffcrcnci's arc not statistically significant and
tiic correlation cannot he made until additional
data arc acciinuilatcd. Other studies ha\i' shown
such a relationship hetween territory size and
population density, with territories becoming
larger as popidation densities decrease (Craig-
liead and Craighead, 1956; Krebs, 1970; South-
ern, 1970). However, the already large home
ranges on the study area suggest that any addi-
tional increase in size over those recorded might
be negated by the reduced efficiency of food
procurement, although we have no way of dem-
onstrating this at present.
Functiom of the Home Ranges. The classic
concept of the function of territorial behavior
suggests that it is a method of population regu-
lation in birds and other vertebrates (Howard,
1920; Wynne-Edwards, 1955, 1962). All raptors
residing on the study area maintained definite
home ranges and largely confined their activities
within them. Pairs reoccupying their territories
of the previous breeding season maintained simi-
lar home ranges from year to year (within the
noted size changes previously discussed) if the
same nest site was reoccupied, but modified
their boundaries somewhat if a new nest site was
chosen, with the new territorial shape confonii-
ing to the pattern of radiation away from the
iK'w nesting site. In a few cases, the new home
ranges differed grcatl\- in shape and specific
boundaries compared with the previous breed-
ing season, perhaps due to the replacement of
one or both members of a pair. Southern ( 1970 )
found tliat Tawnv Owl territories changed \er\'
little from year to year, even with changes in
nesting sites. This may reflect the differences
between the nonmigratory Tawny Owls, which
maintain year-round territories, versus the mi-
gratory species nesting on the Utah study area,
wliicli each year must return and reclaim their
territories.
Thus, although all raptors on th<> study area
were in a sense territorial, it is questionable as
to wliether territoriality limited or regulated
their populations. Brown (1969) has suggested
types of territorial behavior which acting as a
functiem of population densities would not be
limiting at low densities (i.e., all raptors would
be able to breed), but they would tend to be
limiting at high population levels because some
pairs would be excluded from Ijreeding. Un-
forttmately, none of his categories exactly fits
the territorial behavior of the raptor population
within the present study area which, as we have
already shown, depends primarily on tiie relative
food supply as a breeding stimulus.
Territoriality certainly regulated the indi-
\id\ial species popidations and probablv also the
combined Butco species populations in regions
of tlie studs' area with di-nse raptor populations,
but of course it would not be operative in the re-
gions of low population density. In addition,
evidence of old nests was present in many re-
gions of the study area which remained unused
by the raptors during this study. This tends to
preclude the possibilitv that territory was a
major limiting factor in regulating breeding
populations, except locally, and suggests instead
that the raptor population of this area may be
undergoing a long-tenn overall decline caused
l)v an as vet unidentified factor or factors.
Predation
Comparison.'i iiith Other Areas. Raptors are
considerably opportunistic in their predatory
hal)its and take a variety of prey throughout
different parts of their range. For this reason,
and because literature on food habits of the
various species of raptors is plentiful, compari-
sons will be limited only to the major food items.
All of the large raptors in this area relied
heavily, indeed almost completely, on tlu' lago-
moiphs for their chief food source. Although
the frequency of lagomorphs to total prey
items in the diet varied somewhat between the
five large raptor species, their relative contribu-
tion to tlic total prey l)iomass was consistently
above 90 percent for each species, with the re-
maining prey species contributing only minor
amounts to the total prey biomass and common-
ly to the total prey frequency .
Elsewhere, the studies of Gloyd (1925), Mc-
Atee (1935), Woodgerd (1952), Arnold (1954),
Carnie (1954), McGahan (1968), Whitfield et
al. (1969), and Packard et a). (1969) have
shown a similar predominance of lagomorphs
(Lepus and Sijh:Hiii!,us sp. ) ranging from 28 to
96 perc(Mit in Colden Eagle diets. Other impor-
tant prey items from these studies included
ground si|iiirrels (principally Sj)crmophihis),
wliicli constituted over 26 percent of tlic prey
taken by California Golden Eagles in Carnie's
(1954) study, and a variety of avian species
wliieh gcMicrally constituted less than 15 percent
of the total prey items. Murie (1944) reported
an Alaskan population which fed prim;u-ily on
ground squirrels (CiteUus unduhitus). A number
of European studies ha\-e reported high(M- avian
prev bcqueneiis ( Hagaii, 1952; Lockie and
Stephen. 19.39; Uttendorfer, 19.39); Watson, 1957;
iJrown and Watson, 1964), and the latter re-
ported that Red Grouse and Ptarmigan ( Lago-
pus s\). ) comprised 60 percent ol the total mim-
BiOLOciCAi, Seiuks, Vol. IS, No. 3 Bheedinc Et:oi.or.Y of Utah Rm-fobs
65
bt-r of prey iti-ins of a Scottish Golden Eagle
population.
Errington (1932c), Ellington, Hanierstrom
and Hamerstrom (1940), Alcorn (1942), Baum-
gartner and Baumgartner (1944), Fitch (1947),
brians and Kuhlman (1956), Crawford (1968),
Seidensticker (1968), and Marti (1969a) also
found lagomorphs to be the principal volumetric
contribution to the Great Horned Owl diets
within their respective study areas, but found
most other prey species more important in temis
of frequency. Thus, Fitch (1940) found wood-
rats (Neotoma fuscipes) and Jerusalem Crickets
(Stenapclmatus) being taken most commonlv;
Brodic and Maser (1967), Crawford (1968),
Seidensticker (1970). and Marti (1969a) found
murids taken most frequently; and Baumgart-
ner and Baumgartner (1944) reported cotton
rats (Sigmodon hispidus) as the most frequently
taken prev item on their study area. In other
areas lagt)morphs were absent or negligible con-
stituents of Great Horned Owl diets. Burns
(1952) reported a Florida Great Horned Owl
family preying primarily on American coots
(Fulica americana), and Bond (1940) found
harvest mice (Reithrodontomt/s mcg.aIotis) to
be the principal constituent of the diet of a Ne-
vada population.
Red-tailed Hawk diets similarlv show wide
variations throughout their range, and lago-
morphs are often unimportant constituents.
Fisher (1895) and McAtee (1935) found murids
to be the principal food item of their food habits
studies, and Errington (1932c) and Errington
and Breckinridge (193S) reportctl almost e([ual
numbers of mice and ground squirrels. Later stud-
ies ha\e also revealed the importance of ground
squiiTels, which comprised the majority of prey
items of studies in Wyoming ( Craighead and
Craighead, 1956), California (Fitch. Swenson,
and Tillotson, 1946), and Canada ( Meslow and
Keith, 1966). Recently, Luttich et al. (1970)
have shown the Richardson's ground s<{uirrt'l
(Spermophilits ricJiardsonii) to be- the most im-
portant constituent of the total prey biomass of
Alberta Red-tailed Hawk populations. In con-
trast to the heavy utilization of inamiiials noted
from the above studies, Orians and Kuhlman
( 1956) foimd their Wisconsin population preying
consistentl)' upon birds, of which pheasants
(Phdiiauits colchinus) were tlie most iiiipoitant
item. However. Hardv (1939) found the most
important pre\ of a Red-tailed Hawk nest in
central Utah to consist of lagoin(n[)]is and blow-
snakes.
In Montana, Cameron (1914) found Fer-
ruginous Hawks to !)(■ feeding primarilv on
prairie dogs ( Ct/nomt/s sp. ) and meadow mice,
but Fisher (1895) and Angell (1968) reported
that lagomorphs comprised the greater propor-
tion of prey items from their studies, followed
by ground squirrels. Both Cameron (1914)
and Angell (1968) noted that birds were taken
most fretjuently during the first weeks after the
young had hatched, an observation in agree-
ment with the present study.
Food habits of Swainson's Hawks apparently
vary greatly. Cameron (1913), Munro (1929),
Fisher (1S95), and White (1966) have all re-
ported large numbers of insects taken by this
species, but their principal volumetric prey items
are apparenth' ground squirrels (Craighead
and Craighead, 1956). In Utah, Stanford (1929)
reported a pair feeding on field mice and crick-
ets.
Prairie Falcons on the Utah study area
preyed most fre(]uently upon Horned Larks and
ground squirrels, but juvenile lagomorphs con-
tributed much of their total prey biomass. Else-
where, the studies of Fowler (1931), McAtee
(1935), Bond (1939), Enderson (1964), and
Edwards ( 1968 ) reported similar prey prefer-
ence's, with the exception of the lagomorphs. In
other studies, T\ler (1923) reported the virtu-
ally complete utilization of birds by a Cali-
fornia population, while Craighead and Craig-
head (1956) found both meadow mice and
ground scjnirrels to be taken twice as often as
avian prey.
Marsh Hawks on the study area preyed pri-
marily upon deer mice, although birds were
also taken and juvenile lagomorphs were im-
portant constituents of the total prey biomass.
McAtee (1935) found birds, particularly Song
Sparrows (Melo.spiza sp.), to be the most fre-
(|uent species in the stomachs he examined, fol-
lowed by meadow mice and lagomorphs. Breck-
inridge (1935) and Errington and Breckinridge
(1936) also reported a predominance of avian
prey but found that gnnmd squirrels and cotton-
tails comprised the larger portion of the total
prey biomass. In contrast, Craighead and Craig-
head ( 1956 ) reported meadow mice occurring
most frequently in Michigan, followed by birds,
\\itii rabbits and ground s((uirrels each com-
prising relatively nnnor amoxnits of the total
prey biomass.
Short-eared Owls on the study area utilized
prim:uily white-footed deer mice, followed by
kangaroo rats. Elsewhere, Short-eared Owls
seem to exhibit a distinct preference for small
mannnais, paiticularK deer mice and meadow
nnce, and Errington (1932e), Snyder and Hope
(1938), Fischer (1947), Kirkpatrick and Con-
66
IJmciiAM Young Univehsitv Sciknck Bulletin
way (1947), Johnston (1956), Short and Drew
(1962), and Munyer (1966) all recorded high
incidences of these two prey species. In addi-
tion, all of the above studies also recorded large
numbers of birds taken as prey.
Sparrow Hawks on the study area took a
wide variety of prey, but invertebrates were
their main dietary item, particularly grasshop-
pers; deer mice were next in importance. Heint-
zelman (1964) has summarized much of tlie in-
formation on North American Sparrow Hawk
predation and indicates that murid rodents and
grasshoppers are the most common components
of the Sparrow Hawk diet.
Invertebrates, particularly grasshoppers, com-
prised the majority of the prey taken by Bur-
rowing Owls on the study area. Scott (1940)
reported Burrowing Owl populations in Iowa
to be preying primarily on locustids and scara-
bids and noted that vertebrates were rarely
taken, in agreement with the findings of Bourdo
and Hesterberg (1950) in Michigan. Grant
(1965) and Marti (1969a), however, while not-
ing a similar heavy utilization of invertebrates,
also found that murids formed a conspicuous
portion of the total prey biomass.
Suqjrisingly, lagomoiphs were an important
element of the Raven diet in central Utah, but
an unknown percentage was undoubtedly car-
rion. Deer mice were next in importance and
were the most fre<iuently taken prey species.
Nelson (1934) also found a heavy utilization of
lagomorphs (51 percent of the total prey taken),
followed by invertebrates, chiefly insects.
Prey Species Taken Versus AvailaJnlitij. Many
of these central Utah raptors show similarities
in their food habits, particularly when compared
within their rilative size classes. Raptors have
been shown to respond to temporarily super-
abundant foods, but are also considerably op-
portunistic and will apparently take whatever
is available and most easily and efficiently
caught. Comparisons between the total number
of available prey species (potentials derived
from Fautin, 1946) reveal that the collective rap-
tor population utilized much of its potential
prey base. Thus 60.7 percent ( 17 of the 28
species listed by Fautin ) of the mammal species,
51.1 percent (2.3 of a potential 45) of tlie birds,
70 percent of the reptiles (7 of 10 species), and
11.9 percent of the available invertebrate fami-
lies (8 of 67 plus families) were utilized by
one or another raptor species.
However, the food habits studies were des-
ignated primarily to ascertain major predation
trends and, although sufficient, are not exhaus-
tive. Hence, these raptors almost certainly will
take more prey species than revealed by this
study, although this would occur only rarely. In-
stead, only a few species were heavily utilized
and these tended to be the most common ani-
mals on the study area.
Lagomorphs, primarily the black-tailed jack-
rabbit, were the most heavily utilized vertebrate
prev species and were recorded as prey more
frecjuentlv than any other vertebrate species.
As such, and in some fonn, they were the major
prev of 7 of the 11 species of raptors studied,
including the 5 large raptor species. Only the
smaller raptors excluded this species from their
diet. Black-tailed jackrabbits were also the
single most abundant and conspicuous medium-
sized mammal on the study area. All of the
raptors showed great efficiency in procuring
the \()ung of this species, and as many as nine
immature jackrabbits were recorded in a Golden
Eagle nest at one time.
Other mammals of particular importance as
prev iucludetl the anti'lope ground sf^uirrel, two
kangaroo rat species, and the deer mouse. Ante-
lope ground sciuirrels were a common food item of
the large raptors and most of the medium-sized
raptors, but failed to appear in the diets of the
smaller raptors. They were the most frequent
mammalian prey of the Prairie Falcon. Kanga-
roo rats were a very common minor penneant
influent and were significant elements of the
diets of all of the owl species nesting on the
study area and also the crepuscular Ferruginous
Hawk. Both Ord"s kangaroo rat and the chisel-
toothed kan:i;ar(io rat were taken b\' Great
Horned Owls and Ferruginous Hawks, but
only the former was taken by Burrowing Owls
aiul Sliort-eared Owls, whose home ranges were
restricted to the \allev floor. Deer mice were
distributed in all the stud\ area habitats and
were fre(|uentlv taken by four raptors, including
the Red-tailed Hawk, and less fre(juently by
Tuost of the otliiT raptor species.
Horned Larks were the most prevalent avian
species on the study area and were tlie only
bird spi'cies of major importance as prey. They
were recorded among the prey of 10 raptor
species, being excluded only from the Short-
eared OuTs diet.
Locustids were the onlv inxertebrates taken
in large numhiTS and were included in the diet
of four raptor species. They were of particular
importance to both Burrowing Owls and Spar-
row Hawks. Interestingly Fautin (1946) found
Orthoptcraus nuieh less common than at least
eiglit otlicr major insect orders, which suggests
lliat these represent a lower limit of efficient
prey size available to the raptors on tlu' studv
BiOLor.ic:Ai. Series. \'()i.. 18, No. 3 BuEEDiNt; Ecology of Uiaii HAProns
67
area ( although not iicces.sariK' representing the
smallest prey which might be taken).
Relationship betiveen Raptors and Their
Preij. In examining the food habits of raptors,
the frequency percentage of prev items can be
considered to reflect the prey species which the
raptors are expending time and energy to ob-
tain, whereas the biomass percentages essentially
reveal what prey species sustain the raptors.
Logically, raptors will be most efficient if they
can expend their energies on the largest prey
species which they are able to safely capture
and kill, thereby achieving a maximization of
the ratio between the food biomass necessarv
for their daily energy budget and their energy-
expending hunting time. An analysis of the
raptor-prey size relationships on the study area
reveals this to be the case (Fig. 26), and a
gradual increase in mean prey weight was found
to correspond with an increase in average raptor
species weight. The regression of the two vari-
ables results in a positive slope of 0.601 ±
0.221, significantly larger than zero at the 0.001
level (t ^ 4.92). There were no significant vari-
ations in mean prey weight between raptors of
approximately the same weight. This is evident
in comparisons of mean prey weights of the Ruteo
hawks and Great Horned Owl and points up
the fact that these species must bv directly com-
peting for the same food.
In summary, the predatoiy habits of these
raptors reflect pre\ a\aiiabilitv and a size dif-
i 1000
Fig. 26. Relationship between raptor weiglit and mean
weight of prey .species taken. N'umhers refer to
raptor species and follow standard te.\t numbers.
The number 1.3 refers to the Long-eared Owl, in-
cluded in this correlation analysis.
ferential selection correlating with the raptor's
body weight. Although apparently no available
prey species was too small to serve potentially
as a food source, several of the largest mammals
were not utilized, including the mule deer, bad-
ger, coyote and kit fox. These species are ap-
parently larger than the maximum prey weight
wliich can safely and efficiently be obtained and
are thus safe from avian predation, although
infrequent accounts of Golden Eagles attacking
or killing mule deer (Craighead and Craighead,
1956), bighorn sheep lambs (Kennedy, 1948),
pronghorn antelope (Lehti, 1947), and white-
tailed deer ( Willard, 1916 ) have been recorded.
With one exception, no examples of raptor
predation on game or domestic species were
found during this stud\-, despite the fact that
the valleys served for sheep range and lambing
during the spring months. McGahan (1968)
also reported a conspicuous lack of predation on
domestic sheep and lambs in Montana. Ravens
on the study area, however, sometimes lined
their nests with slieep wool, probably taken
from carrion.
The Ferruginous Hawk
Ferruginous Hawks were the predominant
raptors on the study area and also the domi-
nant Buteos. In this respect, they appear to dis-
place the Red-tailed Hawk and Swainson's Hawk
and limit the respective populations of these
species within the study area habitats. Allen
(1874) also recorded Ferruginous Hawks as
the most numerous raptor in Montana with the
exception of the Sparrow Hawk, and recently
Gra)son (in Adolphson and Jonkcl, 1969) re-
ported that Ferruginous Hawks were di.splacing
Red-tailed Hawks and occupying their former
ni'sting territories in the Texas panhandle. The
same possibilit)- exists in the Utah area also, as
evidenced by the fact that Behle ( 1944 ) reported
Swainson's Hawks to In- the most common
hawks of the central I'tah valleys.
Yet the Ferruginous Hawk's dominance and
indeed its presence is highly limited by its nar-
row breeding habitat recjuirements, as previously
discussed. In faxorable areas it consistently pro-
duces significantly larger clutches than any of
the other large raptors on the study area and
also succeeds in fledging more young per nest.
In these areas it is apparently limited only by
its minimmn interspecific (nearest neighbor)
nesting site distances. But it tends to be en-
tirely absent from unfavorable habitats, which
stands in marked contrast to the relatively ver-
satile Great Horned Owl, Red-tailed Hawk,
Raven, and e\'eii Ciolden Eagle, which may on
68
limciiAM Young Univeksity Science Bulletin
occasion disphu' a surprisingly wide choice of
nesting sites. Its absence from less favorable
areas is conspicuous and can be predicted on
the basis of the vegetational and topographic
features of the habitat. Thus, neither steep-
sided canyons nor the interiors of piuNon-juniper
woodlands were utilized. Neither of these habi-
tats support the high lagomorph populations
which constitute the chief prey of the Ferru-
ginous Hawks. Consequently, these habitats
may have been avoided because they would
necessitate longer flight times to and from the
more favorable sagebrush and grassland hunt-
ing areas, and additional time would have to be
.spent in food procurement. Instead, the Ferru-
ginous Hawk pairs choose to nest within very
short distances of their food supply, thereby
lessening the problem of procuring adequate
food for their large l^roods.
This suggests that Ferruginous Hawks are
dominant in numbers because they find suitable
habitats within th(> limits of the study area
which allow a maximization of their productiv-
ity. Undoubtedh', their status as the largest of
the North American Buteos is also contributory.
The Long-eared Owl
The status of the Long-eared Owl in this area
of the Great Basin is uncertain. Although Hen-
shaw (1875) and Bee and Hutchings (1942) re-
corded this species nesting in pinyon-juniper,
only one nest was fomid in this habitat type
during the present study. It was located in an
old Ferruginous Hawk nest constructed in the
top of a juniper and within a dense pinyon-
juniper stand in southwestern Rush \'alley ( Fig.
27). The nest was approximately 2.5 ft x 3.0 ft
and almost flat. On 3 Ma)' it contained three
newly hatched young and three eggs and on
26 May fi\e nearly full grown young were
present and sul)se(|ui'ntly banded.
Fifteen p(>ll(ts and several prey remains were
removed from tlie nest and analyzed. The re-
sults are presented in Table 40. Mammals com-
prised 90.4 percent of tlie total prey taken and
93.3 percent of the total prey bioniass. The two
principal species \\ere, in order of their im-
portance, Old's kangaroo rat and the dei'r mouse.
The mean prey weight taken by this species
was 40.S gms, or only 4.5 gms higher than the
in(\ui prey weight taken by the closely related
species, the Short-eared Owl. This is, however,
three and four times larger than the mean prey
weight taken by Sparrow Hawks and Burrowing
Owls on the study area, although a wide over-
lap within the variety of prey taken by these
four raptors is evident.
The absence of Long-eared Owl nests on the
study area invites comment, as does their ap-
parent scarcity in the pinyon-juniper community.
.'\s pre\i()usly discussed. Long-eared Owls com-
prised a sizeable portion of the wintering owl
populations and were trapped almost three times
as often as Great Horned Owls. Yet they were
virtually absent from the same area during the
breeding season. Although both Long-eared
Owls and Great Horned Owls prey on some
similar species, their prey selection differential
is great; hence, their rare breeding status can-
not be attributed to severe competition with the
larger owl. However, the combination of breed-
ing habitat recjuirements and potential preda-
tion offers another possibility. Long-eared
Owls do not construct their own nests but rather
utilize abandoned nests of a wide variety of
avian and mammal species, and in other parts of
their range, sciuirrel nests and Cooper's Hawk
nests are frequently utilized ( Bent, 1938; Arm-
strong, 1958; Re)nolds, 1970). In addition,
these nests are nonnallv placed in dense conifer
stands ( Randle and Austing, 1952). In the
pinyon-juniper habitat, however, the only nests
a\ailable are those of the Ferruginous Hawk,
Red-tailed Hawk, and Swainson's Hawk. All
of these are constructed in the tops of junipers
and are direeth exposed to potential predators
from aljove. I'^irthermore, probably all ot the
large raptors wliieli nest in this area are capable
of killing Long-eared Owls, and in other areas
Golden Fagles ( McGahan, 196S), Great Horned
Owls ( l'",rringt()n, Hamerstroiii, and Hamer-
Table 40. Food liahils of Long-eared Owls
1970.
No.
%
Approx.
%
Species
Indv.
Indv.
Biomass
Biuma.ss
Dipo(lonu/s
ordii
10
45.5
680
75.7
Pcronu/scus
inanictihitus
7
31.8
119
13.3
Microlus sp.
2
9.1
24
2.7
Pero<inathu.s
parvus
1
4.5
15
1.6
Unident. Passerine
2
9.1
60
6.7
Totals
22
100.0
898
100.0
BiOLOGiCAi, Series, Vol. 18, No. 3 Bueedinc Ecology of Utah Raptors
69
Fig. 27. Juniper tree nest containing; a brood of five voung Long-eared Owls in Rush V'allev. 30 May,
1969.
Strom, 1940), and Red-tailed Hawks (Collins,
1962) have been recorded as preying upon this
species. B. F. Harrison (personal communica-
tion) cites a specific example wherein a Long-
eared Owl was flushed from a similar juniper
nest (in this same area) containing eight well-
developed eggs. When rechecked about two
hours later, both eggs and adults had disap-
peared. The rapidity of their disappearance and
the absence of remains of either the eggs or
adults suggests that the predator was probably
a hawk or Raven.
The above considerations suggest that Long-
eared (>wls recjuire well-concealed nesting sites
in dense cover or thickets, all of which are lack-
ing in the pinxon-juniper commimity. Hence,
their breetling suec(\ss is rendered uncertain be-
cause of the high le\e]s of exposinc of the only
available nesting sites.
Effect of the Investigator
The effect of the investigations and the pres-
ence of the investigators are difficult to evaluate
except where such presence clearly led directly
to the destruction of the raptor's nests, eggs or
young, or resulted in adult mortality. The effect
of the investigators on raptor nesting activities
was often deleterioiLS. Despite the fact that nest
visits were kept short, particularly in cold weath-
er, adverse effects occurred. Most commonly
these effects took the fonn of nest abandonment,
with loss of eggs and yoiuig occurring less fre-
(juently. There is some indication, however,
that the birds adjusted somewhat to the investi-
gators after the first breeding season, and several
of the pairs which had abandoned their nests
in 1967 tolerated similar nest visits during the
subscciuent breeding seasons and nested success-
fully. However, some— particularly two Golden
Eagle pairs— never became tolerant of human
presence and activities.
The aggressiveness of the adults toward the
investigatois varied greatly, both among species
and among pairs of a species and even within the
members of a pair. Generally Golden Eagles
and Swainson's Hawks rapidly departed and
did not reappear during nest visits, but Ferru-
ginous Hawks and Red-tailed Hawks always
pressed attacks if young were in the nest, al-
though terminating them before actual contact
was made. Great Horned Owls were probably
BiiioiiAM Young University Science Bulletin
the most dangerous raptors in the study area.
Several females made det(>rmhied attaeks, and
three made actual eontact, two knocking one
of the authors out of the nesting tree, and the
tiiird lacerating the scalp and forehead of a
colleague ( Bruce Arnell, personal communica-
tion). Of the medium-sized and small-sized rap-
tors, Prairie Falcons were the most aggressive
and Ravens and Sparrow Hawks the most vocal.
None, however, made serious threats or dc-
tennined attacks against the investigators.
In summary, the activities of the investiga-
tion did apparentlv provoke the nesting raptor
species to some extent and apparently resulted
in mortality in e.xtre'me cases. The effect of this
mortality on the total population and popula-
tion trends is tmknown, but it is certainly not
as drastic as the sum total of untoward human
actix'ities directed against the nesting raptors,
which must contribute to the overall low raptor
densit\' of this area. Only additional evidence
will permit definite conclusions, however.
SUMMARY
A studv of the breeding ecologv of raptorial
birds was conducted in central Utah from 1967
to 1970. The objectives of the study were to
provide four years of (juantitative data on the
breeding raptor populations and their distribu-
tion, their habitat utilization, vearlv productivity
and success, territorialits , and predation.
The study area supported a total of 354 indi-
viduals of 12 raptor species during the four study
years. The vearlv raptor population varied
from 8 to 11 raptor species and from 32 to 46
pairs. Individuals commonly comprised from
9 to 13 percent of the yearly raptor population,
and a varying percentage of pairs did not at-
tempt to nest. Ferruginous Hawks were the
predominant raptor species and comprised
some 19 percent of the total yearly raptor popu-
lation. Other important raptors included the
CJolden Fagle, Red-tailed Hawk, and Raven.
Yearly population densities averaged 0.5
pairs per square mile, much lower than raptor
populations found in Michigan and Wyoming
((Iraigliead and Craigliiad, 1956). However,
much of the area was not utilized, and if such
areas were eliminated from the calculations, the
raptor population densities would be increased.
The breeding activities of the collective rap-
tor population occurred ovi'r a period of eight
months. Raptor species exhibited a definite
breeding sequence relative to one another, and
each species initiates! its nesting activities at
slightly different time periods, although some
overlap occurred between early and late nesters
of different species. Cireat Horned Owls and
Colden Eagles were the first raptors to initiate
nesting activities, usuall\- in late January or earh
February. Red-tailed Hawks were the first of
tlie migratory raptors to return and begin nest-
ing and were closely followed by Ferruginous
Hawks. Swainson's Hawks were the last of the
large raptors to begin nesting, usuailv in lati'
May or June, and at approximately the same
time Cooper's Hawks and Burrowing Owls ini-
tiated tluMr nesting activities.
The raptors exhibited a wide range of nest
site selection within the limits imposed by the
study area ]ial)itat. The large raptors nested
primarily in cliffs (including ([uarries) or juni-
pers; but many of the medium- and small-sized
raptor species, such as the Marsh Hawk, Short-
eared Owl, and Burrowing Owl were ground
nesters. Obserxations indicated that several of
the raptor species exhibited a vertical stratifi-
cation of nesting sites. Territories and, less com-
monly, nesting sites were usually reoccupied by
a pair of the sanie species.
The fecundity of the collective raptor popu-
lation varied between years. Specific causes of
mortality of eggs and young included nest de-
sertion and destruction, predation, apparent egg
infertilit\-, and accidents. Human interference
was the probable cause of most of the observed
nest desertion and destruction. Approximately
6.5 percent of all eggs produced were apparent-
ly infertile, of which the majority were from
Ferruginous Hawk nests.
The observed home ranges of the raptor
species were a function of their relative size
and breeding status. Thus, nesting pairs main-
tained larger home ranges than nonnesting pairs,
wliieh in turn held larger home ranges than in-
dividuals Tlie sizes and shapes of the liome
ranges confonned generally to the topography
of the nesting Idcale and usualK' ranged widely
into the surrounding desert. Distanci'S bi'tween
nearest neighbors of closely related species of
similar weight were greater than between rela-
ti\(l\ unrelated species. An exception occurs
bi'twcen species witli iliffering acti\itv pat-
terns, such as tlu' nocturnal owls and the diurnal
hawks. ( )verlapping of home ranges was seldom
substantial between pairs of the same species,
but it was somewhat more frecjuent between
pairs of diftereiit species.
Biological Seiues. \'oi,. IS, \o. 3 Bukkdinc Ecology of Utah Raptobs
71
Kach of the raptor species maintained defi-
nite luinting activity periods. The ob\ious dif-
ferential occurred between the diumal hawks,
eagles and ravens, and the nocturnal owls; but
at least one species, the Ferruginous Hawk, ex-
hibited a crepuscular hunting activity timetable.
The food of the raptors on the study area
included at least 55 different prey species, but
most relied hea\'ily on only 1 or 2 species. The
principal prey of the majority of the large rap-
tors was the black-tailed jackrabbit, which also
figured prominently in the diets of some of the
medium-sized raptors. Other prey species of im-
portance to one or more raptor species included
the antelope ground scjuirrel, two kangaroo rat
species, the white-footed deer mouse, and the
Horned Lark. Tlie smaller raptors also took
large numbers of invertebrates, principally or-
thopterans. Gencrallv the raptors preyed heavily
upon the most aliundant potential prey species,
and a correlation of predator-prey size was
found, indicating that the various raptor species
preyed most heavily upon the largest prey
species which they could most efficiently cap-
ture and kill. No examples of raptor predation
on game or domestic livestock were found dur-
ing the study period.
ACKNOWLEDGMENTS
We wish to express our sincere appreciation
to Dr. C. Lynn Hayward, Dr. Herbert H. Frost,
and Dr. Glen Moore for reading and criticizing
an earlier version of this manuscript. Grateful
acknowledgment is also expressed to many
others who contributed to the successful com-
pletion of this work, including Dr. Clyde C. Ed-
wards for his assistance in the field from 1967-
1970; David H. Ellis, Franz J. Camenzind, and
J. Bradford Weston for field assistance from
1967-1968; W. Bruce Arnell for field assistance
from 1969-1970; and Charles R. Wilson for field
assistance from 1969-1970.
Miss Nancv Lee Balan typed and edited the
final manuscript.
We express gratitude to the Southern Con-
necticut State College Computer Center for its
services and to the Brigham Young University
Department of Zoology for furnishing equip-
ment and transportation.
Tliis stud\ was supported in part by a Na-
tion;il Defense Education Act Fellowship and
in part bv a research grant from the National
Audubon Societv.
APPENDIX-WEIGHTS OF PREY SPECIES USED IN THE BIOMASS CALCULATIONS.
Species
MAMMALS
Lepus californicus
Si/Ivilagus sp.
Spermopliilus tDunsendi
Ammospermophihis leuctirus
Eutcnnius minimus
TfioDuimyv hotlac
Perognathus parvus
Peroiinuthtis formosus
Dipodomtjs microps
Dipodomi/s ordii
Microdipodops meii.acephalus
Ontjchomijs leucogaster
Reithrodentomi/s mcii.(dofis
Peromiiscus mitniculalus
Neotoma lepida
Micruttts sp.
Mustehi frenata
BIRDS
Btiteo sitditisoui
Appro.v. wt.
in gms.
Source
2300
Haskell and Reynolds (1947)
1000
Seidenstickcr (196S)
191
Cornish and Mrosovsky (1965)
145
This study
78
This study
170
This study
15
This study
19
This study
65
This study
68
Desha (1967)
24
This study
38
Marti (Unpubl IBP data)
12
Marti (Unpubl IBP data)
17
Bee (1947)
217
Marti (Unpubl IBP data)
38
Bee (1947)
178
Marti (Unpubl IBP data)
988
Craighead and Craighead (1956)
72
Brigham ^■ouNc University Science Bulletin
Zetiaklura macroura
Ask) flammeus
Chordeiles minor
Phdlacnoptilus nuttallii
TijTdnnns verticelis
Sai/ornis saija
Olocoris cdpestris
Pica pk;a
Ctjanocephalus ct/anocephalus
Oreoscoptes montamis
Sialki curnicokles
Larius hidovickimis
Passer domesticus
Oherholseria chlorura
Calanwspiza mchnocorijs
Poecetes graminetts
SpizcUa hreiceri
Zo not rich ia leiicoph n/s
Stiirnis vulgaris
Sturnella neglecta
REPTILES
Crotaphytus collaris
Ufa sfanshuriana
Sceloporus graciostis
Phrynosoma platyrhinos
Cncmidophorus tigris
Masticof)his tacniatus
Pituophis melanoleucus
INVERTEBRATES
Curahidae
Scarabidae
Sdphidae
Curcidionidae
Tcnchrionidae
Locustidae
Aranae
Scorpionidae
153
Hiitt and Hall (19.38)
340
Craiglicad and Craifjhead (
75
Thi.s .study
62
Thi.s studs'
36
This stud)
28
This study
28
Bohlc (1943)
173
SeidcnstickcT (1968)
108
Foole (1938)
45
This study
45
Marti (Unpubl IBP data)
52
Esten (1931)
25
Poole (1938)
30
This study
33
Marti (Unpubl IBP data)
27
Poolc (1938)
30
This study
30
Baldwin and Kendeigh ( 1938
84
Poole (1938)
145
Poole (1938)
30
This study
4
This study
13
This study
9
This study
24
This study
169
This study
372
This study
0.23
Marti (Unpubl IBP data)
0.3
Marti (UnpuhllBPdata)
0.3
Marti (Unpubl IBP data)
0.1
Marti (Unpubl IBP data)
0.55
Marti (Unpubl IBP data)
0.6.3
This study
0.4
Marti (Unpubl IBP data)
1.45
This study
1956)
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C)'. ' r^Acifo
Brigham Young University
Science Bulletin
MUS. COM^. ZOOL.
LtfiNARY -J!lo1r-Bo'feat
HOV 51973
HARVARD EFFECTS OF A NUCLEAR
uNiv^ONATION ON ARTHROPODS
AT THE NEVADA TEST SITE
by
Dorald M. Allred
BIOLOGICAL SERIES — VOLUME XVIII, NUMBER 4
JULY 1973/ISSN 0068-1024
BRIGHAM YOUNG UNIVERSITY SCIENCE BULLETIN
BIOLOGICAL SERIES
Editor: Stanley L. Welsh, Department of Botany,
Brigham Young University, Provo, Utah
Acting Editor: Vernon J. Tipton, Zoology
Members of the Editorial Board:
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Joseph R. Murdock, Botany
WiLMER W. Tanner, Zoology
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Brigham Young University
Science Bulletin
EFFECTS OF A NUCLEAR
DETONATION ON ARTHROPODS
AT THE NEVADA TEST SITE
by
Dorald M. Allred
BIOLOGICAL SERIES — VOLUME XVIII, NUMBER 4
JULY 1973/ISSN 0068-1024
TABLE OF CONTENTS
INTRODUCTION 1
METHODS 1
RESULTS 7
BEETLES 7
Araeoschizus sulcicoHis 7
Centrioptera muricata 7
Conibiosoma elongatum 8
Edrotes orhiis 8
Eleodcs armata 8
E. grandicollis 8
E. hispilabris 9
E. longipilosa 9
E. nigrina 9
Eupsophylus castaneus 9
Euschides htctatus 9
Eusatttis agnatus 9
Metoponium convexicoUe 9
Pelecijphorus pantex 9
P. semilaevis 9
Triorophus laevis 9
Trogloderus castatus 10
Changes within Sectors 10
Grid vs. Transect Extrapolation 11
Crater Occupants 12
ANTS 12
Aphaenogaster megommattis 12
Crematogaster coarctata 12
Iridomijrmex pniinosum 12
Mijrmecocijstus mexicanus 12
M. mimicus 12
Pheidole bicarinata 13
Pogonormjrmex calif ornicus 13
P. nigosus 13
Veromessor lariversi 14
V. smithi 14
Changes within Sectors 14
Grid vs. Transect E.xtrapolation 15
ORTHOPTERANS 15
Arenivaga erratica 15
Cetithophilus fossor 15
C. kimellipes 15
Litaneutria minor 15
Stenopelmatus fuscus 15
Changes within Sectors 15
SCORPIONS 16
Hadrurus spadix 16
Vaejovi^ becki 16
V. boreius 16
V. confusus 16
Changes within Sectors 16
Crater Occupants 16
Grid vs. Transect Extrapolation 16
SOLPUGIDS 16
Bronchia potens 16
Eremobates scopulatus IV
Eremorhax pulcher 17
Hemerotrecha calif ornica 17
H. proxima 17
H. scrrata 17
Changes within Sectors 17
Crater Occupants 17
Grid vs. Transect Extrapolation 17
SPIDERS 17
Calilena restricta 17
Gtuijilwsa hirsutipes 17
Iliipliidrassu.s- cuiiii 17
Ilirptjllus hcspcwlus 17
Loxosceles unicolor 18
Megamijrmecion naturalisticum 18
Ncuuntigraphis chamherlini 18
Orthonops gcrtschi 18
Physocijclus tanneri 18
Pailochorus utahensbi 18
St/.spira cclectica 18
Changes within Sectors 18
Grid vs. Transect E.xtrapolation 19
SUMMARY 19
LITERATURE CITED 20
EFFECTS OF A NUCLEAR DETONATION ON
ARTHROPODS AT THE NEVADA TEST SITE'
by
Dorald M. Allred^
INTRODUCTION
Allred, Beck, and Jorgensen (1963b, 1964)
and Jorgensen, Allred, and Beck (1963) dis-
cussed the effects of the nuclear detonation
"Sedan" on vegetation and rodents at the Ne-
vada Test Site. My report discusses the effects
of that same detonation on arthropods.
Project Sedan, a phase of the Plowshare pro-
gram for peaceful uses of nuclear energy, was
detonated underground at a depth of 194m on
July 6, 1962. The thermonuclear device of 100
short kilotons created a crater 98m deep and
.390m in diameter (Fig. 1). Intense radioactive
fallout was generally confined within an area
of 6.5km by 9.7km. Ecological studies, which
utilized the techniques described by Allred,
Beck, and Jorgensen ( 1963 ) for trapping ground-
dwelling arthropods, were made before and af-
ter the detonation.
METHODS
Can pit-traps were placed at intervals be-
tween 305m (1000 ft) and 2743m (9000 ft)
from ground zero (GZ = the center of the
nuclear detonation) as shown by the circles on
Fig. 2. One year after the detonation, pit cans
were also arranged in three grids as shown on
Fig. 2. Each grid consisted of four transects
3m apart, each transect with five cans 6m apart.
Cans along the main transect, which was
2438m long, were open for the capture of ani-
mals from June 17 through July 5, 1962 (pre-
test). Arthropods were removed from the cans
at two-day intervals prior to the detonation. Be-
ginning on August 25 after the detonation, which
was as soon as safety conditions allowed entry
into the area, the cans were opened and left
until September 2.3, 1962 (posttest). During
this latter time, collections were also made at
two-day intervals, except for three periods when
strong winds created sufficient movement of
radioactive dust to create a safety hazard. Dur-
ing this period, entry into the area was not al-
lowed, and collection intervals of five to seven
days were used. A year later, from 20 to 30
June, and 15 to 25 August 1963, cans were
opened and visited at two-day intervals.
Pit cans on the three grids which were es-
tablished in 1963 were also open from 20 to
30 June and 15 to 25 August 1963, and visited
every second day.
Jorgensen, Allred, and Beck (1963:51) des-
ignated two pretest and three posttest zones
(Fig. 2). On the basis of their analysis of
vegetation before the detonation and subse-
quent effects of the blast (Ibid: 54), I desig-
nated nine sectors for analysis of the arthropod
populations (Fig. 2). The major vegetative
types according to sectors are shown in Table 1.
For purposes of comparative populations be-
tween the 2438m transect and the grids, I
grouped those sectors of similar vegetative
types and damage with the specific area of the
grid. The grid closest to GZ (lOt) is compared
to the section of the transect within sectors 1
to 3, the second grid (lOu) with sectors 4 to
6, and the grid farthest from GZ (lOw) with
sectors 7 to 9.
In order to extrapolate population indices
from other areas of similar vegetative types of
the test site to those expected in the nine sec-
tors of the Sedan experiment, relative popula-
tion factors were determined for four major
types which correspond to the zones and vege-
tative analysis as designated by Jorgensen, All-
red, and Beck (1963:51, 54), and the nine sec-
tors as used in my report (Table 2). These are
■BYUAEC Report C00-78(i fin
denier for Health and Environmental Studies, Brigham Youni; Univ,, Provo, Utah 84h02.
Bhioham Young Univkhsitv Scienck Bulletin
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Brigham Young Uniyehsity Science Bulletin
TABLE 1. Principal vegetative types and conditions in nine sectors before and after the detonation of Sedan.
Sector
Feet
from
GZ
Pretest
Posttest
1
2
3
4
5
6
7
8
9
0-1500
1500-2500
2500-3500
3500-4500
4500-5500
5500-6500
6500-7500
7500-8500
8500-9500
Salsola-Grass
Sahola-Grass-Hymenoclea
Hijmenoclca-Grmjia-Grass
Coleogtjnc-Grm/ia-GjTass
Coleog,ijiic-Gr(itii(i
Coleogijnc-Graijia
Coleogyne-Grayia
Coleogtjne-Grayia-Lycium
Coleogyne-Grayia
Covered with soil
Covered with soil
ditto
Vegetation destroyed; partly covered
with soil
Vegetation damaged; layer of dust
No change; layer of dust
No change; layer of dust
No change; layer of dust
No change; layer of dust
TABLE 2. Relative abundance factors"
1959-1963.
of arthropods in four vegetative types at the Nevada Test Site,
Plant Commvmity""'
Group and species
Gr Ly Co Gr Ly Co Gr Ly
Sa (dis) (dis) (undis)
Tenebrionid Beetles
Araeoshiztis sulcicoUis
1
48
56
46
Centrioptera imiricata
1
39
25
5
Conibiosoma cloi}gatum
1
39
25
7
Edrotes orbus
3
8
5
1
Eleodes aniiata
1
7
6
5
E. grandicoUis
1.4
8
4
1
E. his p Hal iris
12
34
17
1
E. longipilosa
0
0
0
1
E. nigrina
0
0
0
0
Eupso])hyhis castaneus
0
2
1
4
Euschides btctatufi
0
1.3
1.3
1
Eusattus agnattts
1
2.6
0
0
Metoponium eonvexicoltc
1
2.5
1.3
2
Pelecyphonis pantex
1
3
1.6
3
P. semilaevin
0
1.5
1
2
Triorophus laevis
1
32
18
5
Trogloderus costatus
4
18
9
1
Ants
Aphaenogaster megommatus
0
2
1
2
Crematogaster eoarctata
1
1
1
1
Iridomynnex pruinosum
1
2
7
9
Mynnecoeystus mexicanus
1
9
8
12
M. mimints
1
2
2
2
Pheidole bicarinata
1
2
1
1
Pogonoimjrmex californiciis
1
1.5
1
1
P. rugosus
1
121
86
129
Veromessor lariversi
7
4
3
1
V. smithi
0
0
1
2
(Jrthopterans
Arenivaga erratica
0
1
2
3
Ceuthophibis fossor
1
1.5
1
1
C. lamcUipes
1
1
1
2
Litaneiitria vunor
1
1.5
4
6
Stenopelmatus fuscus
1
5
4
5
Biological Series, Vol. 18, No. 4 Effects of Nuclear Detonation on Arthropods
Table 2 (Continued)
Scorpions
Hadriirus spadix
Vaejovis hecki
V. horeus
V. conftisus
Solpugids
Bronchia potens
Eremohates scopulatus
Eremorhax pulcher
Hemerotrecha californica
H. proximo
H. serrata
Spiders
Calilcna rcsfricta
Gnaphosa hirsiitipes
Haplodrassus eunis
Herpt/Uus hesperolus
Loxoscclcs itnicoJor
Megoimjnnecion naturolis-
ticitm
Neoonagrophis chamberlini
Orthonops gertschi
Physoctjchis tanneri
Psilochoriis utahensis
Syspiro eclectica
*.Mi numbers are i-elated to the factor of "1" which represents the least abundant, "0" indicates not found Factors are not compar-
able between species.
••Sa = Salsola; Gr Ly (dis) = Grayia-Lycium disturbed, Co Gr Ly (dis) = Coleogyne-Grayia-Lycium disturbed; Co Gr Ly (undis)
= Coleogyne-Grayia-Lycium undisturbed.
1
3
3
4
1
2
2
2
0
.5
.3
.5
1
3
2
3
0
.5
2
3
1
1.5
1
1.5
1
1
.5
.5
0
3
3
5
0
2
1
2
1
1
1
1
0
3
2
3
1
4
6
9
1
5
9
14
1
3
5
7
0
0
0
0
0
0
1
2
1
1.5
2
2.5
0
1
1
1.5
0
0
0
0
1
1
1
1
0
.5
1
1
(1) Salsola. (2) disturbed Grayia-Lycium, (3)
disturbed Coleogyne-Grayia-Lycium, and (4)
undisturbed Coleogyne-Grayia-Lycium (Table
2).
Similar factors were determined for the
seasonal occurrence and abundance of each
species of arthropod in other areas of the test
site not affected by the Sedan experiment so as
to determine the expected species and their
populations during the different sampling peri-
ods in the environs of project Sedan (Table 3).
Factors of adjustment were used to standardize
sectors and grids, as well as other areas and
seasonal collecting at the test site, to the number
of stations and collections. Five equations were
used as follows.
For pretest and posttest populations of each
sector and vegetative type,
FN, = N,: X Ts
where
PNa = number of animals collected adjusted
to the number of collecting attempts,
Nc = actual number of specimens collected,
and
Ts = adjustment factor of the number of
traps in a given sector or vegetative type, as
determined by the greatest number of traps
used in any of the vegetative areas or sectors,
divided by the number of traps in the specific
sector or vegetative type considered.
Seasonal adjustment factors were determined
by Sp = Ph
Pi.
where
Sf = the seasonal adjustment factor,
Ph = the greatest population collected in
one of the four months, June through Septem-
ber, over the whole test site, and
P,, = the lowest population as above.
The base factor for determining the expected
population of a given species for a specific
vegetative type and month was calculated as
Bp =^ PNa
SJuf + SJyp
where
Bp =r the base factor,
PNa = as explained above,
SJup = the seasonal adjustment factor for
June, and
SJyp = the seasonal adjustment factor for
July.
6
Brigham Young Univebsiti- Science Bulletin
The posttest expected population was de- period considered,
fomiined by If the period considered was more than one
Fx = Bf X Sf month, then tlie etjuation should read:
where Px = Bk x (Sif + Sjf)
Px = the expected population for a given where
period, Sik = the first seasonal adjustment factor,
Bf ^ the base factor as explained above, and
and Slf = the second seasonal adjustment factor,
Sf ^= the seasonal adjustment factor for the and so on.
TABLE 3. Relative abundance factors" of arthropods related to above-ground activity during four months
at the Nevada Test Site, 1959-1963.
Month
Group and species
June
July
Aug.
Sept.
Tenebrionid Beetles
Araeoshiziis sulcicollis
1.6
1
2.2
3
Centrioptera nniricata
37
22
4
1
Conibiosoma elonp^atiim
1
2
1
1
Echofes orbtts
1
2
10
9
Eleodes armata
1
1.2
3.2
8.8
E. grandicoUis
1
2
7
8.5
E. hispiUiljris
3
1
1.4
1.4
E. loriiiipilosa
0
1
1
0
E. nigrina
0
0
3
0
Eupsopliyhis ca.staneus
18
1
0
0
Euschides luctatus
0
0
0
3
Eusattus agnatus
0
0
2
0
Metoponitim convexicolle
1.5
1
1
1.5
Pelectjphorus pantex
0
1 '
76
30
P. semilaevls
0
1
20
10
Triorophus laevis
17
7 .
2.4
1
Trogloderus costatus
1.4
1
3.6
1.2
Ants
Aphaenogaster megommatus
1
122
133
0
Crematogaster coarctata
8
, 17
21
1
Iridomtjrmex pruinusum
27
14
3
1
Mtjrmecociistus niexicanus
1
1
2
2
M. mimicus
1
2
2
1
Pheidole bicarinata
6
7
3
1
Pogonomtjrmex califoniicus
.3
5
3
1
P. rugosus
1.5
1
2
1.5
Veromessor lariversi
6
10
1
0
V. smithi
1
0
0
0
Orthopterans
Arenivaga erratica
15
1
3
0
Ceuthophilus fossor
79
34
1
2
C. lamellipes
0
1
5
6
Litaneutria minor
3
4
3
Slenopehnatus fu.scus
4
7
5
Scorpions
Hadrurus spadix
1
2
1
Vaejovis becki
2
2
2
V. horeus
1
2
2
V. confusus
3
2
2
SolpuRids
Bronchia potens
7
11
0
Biological Serifs, Vol. 18, No. 4 Effects of Nuclear Detonation on Arthropods
Table .3 ( Continued )
Eremohates scopulafus
2
1
0
0
Eremorhax pulcher
1
1
0
0
Hemerotrecha californica
65
20
2
1
H. proxima
0
0
0
0
H. serrata
1
5
6
2
Spiders
Calilemi restricta
3
4
1
1
Gnaphosa hirsittipes
14
11
1
7
Haplodrassus ctmis
1
0
1
2
HerpijUus Iiesperohis
2
1
0
4
Loxosceles unicolor
5
9
7
1
Megamiirmecion naturalistictim
3
3
2
1
Neoancti^raphis chamherlini
1
1
1
2
Orthonops p,ertschi
7
6
0
1
Pht/soctjchis tanneri
0
0
1
0
Psihchonis titahensis
5
5
4
1
Syspira eclectica
5
6
4
1
'All numbers are related to the factor of "1" which
represen
,ts the least abundant. "
0" indicates not found.
Factors are not com-
parable between si)ecies.
RESULTS
Beetles
Araeoschizus sulcicoUis. Beetles of this spe-
cies were present in all sectors except number
8 before the detonation, and most densely con-
centrated in sectors 5, 6, 7, and 2, respectively
(Table 4). One and two months after the deto-
nation, populations were 86 percent below
the e.vpected normal, and somewhat evenly dis-
tributed between all sectors except number 8,
where none were found. In June 1963, popula-
tions were 62 percent below the expected nor-
mal and occurred in only four sectors, including
number 8, but none were closer to GZ than
1067m. In August 1963, populations were 93
percent below the expected normal and were
found only in sector 8.
Ecologically, significant differences in popu-
lation occurred from the expected normal in all
sectors except numbers 1 and 2. The pretest
population in sector 2 was considerably higher
than the nomi, whereas the posttest population
was not significantly different. In sectors 3 to
9, pretest and posttest populations were signifi-
cantly lower than the expected norm.
Centrioptera muricata. Beetles of this species
were present in only four sectors before the det-
onation and were most densely concentrated in
sectors 7 and 8 ( Table 5 ) . One and two months
TABLE 4. Effects of a nuclear detonation on populations of beetles of the species Araeoschizus sulcicoUis.
No.
specimens
Pre-
test
Posttest
Aug.-Sept.
1962
J'
ine 1963
Aug.
1963
Sector
Actual
Expected
Actual
Expected
Actual
Expected
1
3
o
0
0
2
0
3
2
11
o
•
0
7
0
9
3
4
1
8
0
2
0
3
4
1
4
2
5
1
0
1
5
28
5
56
6
17
0
24
6
18
4
36
0
11
0
15
7
14
4
28
7
8
0
12
8
0
0
0
2
0
5
0
9
7
2
14
0
4
0
6 .
Total
86
20
144
20
52
5
73
"Colleclion attempts not made.
8 Bricham Young Univehsiti- Science Bulletin
TABLE 5. Effects of a nuclear detonation on populations of beetles of the species Centrioptera muricata.
No.
specimens
Pre-
test
Posttest
Aug.-Sept. 1962
June 1963
Aug.
1963
Sector
Actual
Expected
Actual
Expected
Actual
Expected
3
6
7
8
1
4
9
9
0
0
2
0
0
0
1
1
0
0
0
0
1
3
6
6
0
0
0
0
0
0
1
1
Total
23
2
2
0
16
0
2
after the detonation, populations were not re-
duced from the e.xpected. None were found in
sectors 3 and 6 immediately after the detona-
tion, and in 1963 none were found in any sector.
Ecologically, pretest populations were not
significantly different from the e.xpected nonn
in any sector except numbers 3 and 4, where
they were lower. Similarly, posttest populations
were also significantly lower than the norm in
these two sectors, whereas in other sectors pop-
ulations were as expected.
Conibiosoma elon<^(itum. One specimen was
taken in sector 9 before the detonation; none
were taken after. Elsewhere on the test site
beetles of this species were relatively abundant
in Coleogtjne and Grciyia-Lijcitim, but not in
Salsola. Seasonally they were common from
June to September.
Edrotes orhtis. Animals of this species were
present only in sector 6 before the detonation.
One and two months after the detonation they
were densely concentrated in sectors 3, 4, and
5, whereas none were foimd in sector 6. Post-
test populations occuned in six of the sectors.
One and two montiis after the detonation, the
population actually increased over the expected
by 64 percent. In June 1963 the population
showed an increase of 300 percent, whereas in
August 1963 a decrease of 100 percent from the
expected occurred.
Ecologically, pretest populations were not
significantly different from the expected nonn,
except in sector 3 where they were lower. Post-
test populations were significantly higher than
expected in sectors 3, 4, and 5.
Eleodes armata. Beetles of this species were
present in all sectors except numbers 1 and 8
prior to the detonation (Table 6). Greatest
concentrations were in sectors 7, 6, and 5, re-
spectively. One and two months after the det-
onation they were not found in sectors 2, 3, and
6, but were still most densely concentrated in
st'ctors 5, 6, and 7. Populations immediately
after the di'tonation were dimiiiislied by 74 per-
cent. In June 1963, beetles were found only
in tiiree sectors, and their populations were 66
percent iiiglier than expected. In August 1963,
the population iiad diminished from the ex-
pected norm by SO percent.
Ecologically, these beetles were significantly
more abundant in sectors 5, 6, and 7 before the
detonation tlian was expected.
Eleodes grandicoUis. Beetles were found
only in sectors 1 and 4 before tlie detonation.
One and two montlis after the detonation l)eetles
were present in sectors 3, 4, 5, and 7, l)ut not
TABLE 6. Effects of a nuclear detonation on populalioiis of hcitlt's ol the species Eleodes armata.
No.
specimens
Pre-
test
Posttest
Aug.-Sept
. 1962
June 1963
Aug.
1963
Sector
Actual
Expected
Actual
Ex
pected
Actual
Expected
2
4
D
e
1
0
0
1
3
4
0
2
0
0
0
1
4
2
1
1
2
0
0
0
5
12
4
7
0
1
0
2
6
14
0
8
0
1
0
2
7
19
2
10
2
1
2
3
9
7
2
4
0
0
0
1
Total
62
9
32
5
3
2
10
'Collertion allcmpts not made.
Biological Series, Vol. 18, No. 4 Effects of Nuclear Detonation on Arthropods
in sector 1 as previously found. A decrease of
30 percent from the expected population oc-
curred. In June 1963, no beetles were found,
and in August 1963, tlie population was 75
percent lower than the expected norm.
Ecologically, pretest populations were not
significantly different from the expected in any
sector, except number 3. Likewise, the post-
test population in sector 3 was the only one
that differed significantly from the expected
norm.
Eleodes hispilabris. Beetles of this species
were found only in sectors 1 to 5 before the
detonation, and only in sectors 1, 2, 3, 6, and
7 after detonation. In no sector were they
densely concentrated. One and two months af-
ter the detonation the population had diminished
from the expected norm bv 34 percent. In June
1963, the population was the same as expected,
and in August 1963, it had increased over the
norm by 50 percent.
Ecologically, pretest populations in sectors
1 to 4 were significantlv higher than expected,
and posttest populations in sectors 2, 3, 4, and
6 were significantlv lower than the norm.
Eleodes longipilosa. One specimen was taken
in sector 3 after the detonation in June 1963. In
other areas of the test site, these beetles were
taken in similar vegetative types in May, July,
and August, but only in small numbers.
Eleodes nigrina. Two specimens were taken
in sectors 3 and 4 in August and September
1962, immediatel) after the detonation, but
none at any other time. In other areas of the
test site these beetles were taken only in the
Pinvon-Juniper conimunitv, mainly in .August.
Their occurrence in the disturbed Grat/io-Li/citim
and Coleogyne near the Sedan crater was unex-
pected.
Eitpsophijlus castoneus. Eight beetles of
this species were taken in sectors 3, 4, and 5
after the detonation in June 1963. None were
taken at other times. In other areas of the test
site these beetles were most common in vege-
tati\e types other than those near the Sedan
crater and, seasonally, were most abundant in
Mav and June.
Euschides Itictcitus. Two specimens were
taken in sector 4 immediately after the detona-
tion in .August and September 1962. None were
found at other times. In other areas of the test
site these beetles were relatively common in
vegetative types similar to those which surround
the Sedan crater, but the\' were essentially ab-
sent between May and September.
Eusattus agnattis. Thirteen beetles of this
species were taken in sectors 1 to 4 in August
1963; none were taken at other times. In other
areas of the test site these beetles were most
abundant in the same vegetative types that
surround the Sedan crater, but they were ab-
sent from June to September.
Metoponium convexicoUe. Four specimens
were found in sectors 3, 5, 6, and 9 after the
detonation in June 1963. None were found at
other times. In other areas of the test site
these beetles were most abundant in the same
vegetative types as in the Sedan environs, but
their populations were at a minimum in August,
with an increase in September.
Pelecyphoms pantex. None were found
prior to the detonation or in June 1963. Im-
mediatclv after the detonation in August and
September 1962, 46 specimens were found in
sectors 3 to 7. In August 1963, 1.30 beetles
were found in all sectors except number 1. In
other areas of the test site these beetles were
relatively abundant in the same vegetative types
as occur around the Sedan crater. Seasonally
in other areas, thcv were most abundant in
August and September and essentially absent
at other times. This explains their absence in
June and July before the detonation, as well as
in June 1963.
Felecijphorus semUaevis. Beetles of this
species were not found in the Sedan area prior
to the detonation. After the detonation in Au-
gust and September 1962, three specimens were
found in sectors 4, 5, and 7. None were found
in June 1963, but in August 1963, 16 beetles
were found in sectors 1 to 7 and in 9. In other
areas of the test site these beetles were common
in the same vegetative types that surround the
Sedan crater. Seasonally, however, they oc-
curred almost exclusixelv in August and Sep-
temlier. This explains their absence in June
and Jul\' in the Sedan area.
Triorophus laevis. Before the detonation
these beetles were present in everv sector ex-
cept numbers 7 and 8 (Table 7). They were
most densely concentrated in sector 6. One and
two months after the detonation tliey were
found only in sectors 3, 4, 5, and 7, and most
denseiv concentrated in sectors 3 and 4. At
tliat time the population was 1000 percent
greater than the expected norm. In June 1963,
these beetles were found onlv in sectors 5 to
S, and their population was 29 percent less than
the expected norm. In August 1963, beetles were
not found in any sector.
Ecologically, pretest populations were signif-
10
BlUGHAM VoUNG UNIVERSITY SCIENCE BULLETIN
TABLE 7. I
Effects of a nil
clear detonation
oil popiil;i
itioiis of bee
ties
of the species '
iriorophus I
aevis.
No.
specimens
Pre-
test
Posttest
Aug.-SepI
:. 1962
J'
jne
1963
Aug.
1963
Sector
Actual
Expected
Actual
Expected
Actual
Expected
1
1
o
o
0
1
0
0
2
4
«
0
0
3
0
0
3
1
20
0
0
1
0
0
4
2
15
0
0
1
0
0
5
1
5
0
5
1
0
0
6
11
0
2
4
8
0
1
7
0
4
0
4
0
0
0
8
0
0
0
2
0
0
0
9
9
0
1
0
6
0
1
Total
29
44
3
15
21
0
2
•Collection attempts not made.
icantlv lower in sectors 3 and 4 and higher in
sector 6 than was expected. After the deto-
nation, the only significant difference was a de-
crease in the population below that expected in
sector 3.
Trogloderus costatus. Beetles of this species
were present only in sectors 1 and 2 before
tiic detonation. {)ne and two months after the
detonation they were found only in sectors 3,
4, and 5. In that period their populations were
only 23 percent less than the e.xpected norm.
In June 1963, the populations were 100 percent
above the norm and, in August 1963, 307 per-
cent above the expected.
lilcologicallv, these beetles had a lower pre-
test population in sectors 3 and 4 than expected,
but after the detonation their populations in
sectors 1 to 4 were significantly iiigher.
Changes trithin Sectors. Some significant
differences occurred between the population
trends in different sectors during the posttest
recover)' time. Populations generally and con-
sistently were less than tlie expected normal but
for few exceptions. In August 1963, the popu-
lation in sector 2 was 13 percent above the
expected, whereas in sector 8 it was 400 per-
cent higher. At other posttest times in tiiese
two sectors the populations were considerabh'
less than the expected normal. However, sectors
3 and 4 had posttest population increases dur-
ing eaeli sampling date except one, June 1963.
when the population was only 7 percent less than
e.xpected. At other times the population was
from 125 percent to 291 percent above the ex-
pected nonnal. As indicated by analysis of
the vegetation, sector 3 was in tlie fringe area
where tiie plants were desl roved and or cov-
ered bv a shallow layer of soil throw-out. Si-ctor
4 was typified by a removal of most of the
vegetation by flying debris, with a small amount
of throw-out deposition. Pretest populations
in sectors 1 and 2 were moderate and in sectors
5 and 9 generally were high. Except for sec-
tor 8, pretest populations of sectors 3 and 4
were lowest of all sectors. The hypothesis is
presented that the unexpected increase in post-
test populations in sectors 3 and 4 may have
been due to piiysical transport by the force
of the detonation of beetles from sectors 1 and
2 to sectors 3 and 4. Furthermore, as a result
of reverse air movement immediately after the
detonation, some beetles may have been car-
ried back towards sectors 3 and 4 from the
more outh ing sectors where populations were
higiiest. Because of the tough protective exo-
skeleton and nature of these beetles, one may
assume that thev were able to withstand the
shock and buffeting. This hypothesis is sup-
ported by a change of species distribution in
tile sectors. In sector 3 in August and Sep-
tember 1963, four species were present that
were not taken in this sector before the deto-
nation. Two of tiiese were present before the
test in sectors 1 and 2, one was present in
sector 4, and tiie other was not found prior
to tlie test. In sector 4, six species were found
posttest tliat were apparently not there pre-
test. Two of these were present in adjacent
sectors hi^fore tiie detonation, l)ut tiie other
four were not found prior to tiie detonation.
Complete or ncariv complete elimination of
tile population occurred in five of tiic sectors
at some period after detonation. A reduction
of 100 percent occurred in August and Septem-
i)er 1962 in sectors 2 and 8, and June and .Au-
gust 1963 in sector 9. Ninet\-foiir percent re-
diution was noti'd in sector 6 in August
Biological Series, Vol. 18, No. 4 Effects of Nucle.^r Detonation on Arthropods
11
and Soptcmber 1962, and 96 percent in sector
5 in August 1963.
Total populations of all species of tenebrio-
nid beetles were 5S percent lower than the e.K-
pected normal in August and September 1962,
61 percent lower in June 1963, and 58 percent
lower in August 1963.
Beetles of eight species were found both
before and after the detonation. Six other
species were found after the test that apparently
were not present before (Table 8). Seasonally
and ecologically, four of these should have been
present before the detonation, whereas the other
two were not expected. However, five of the
species were expected to be present after the
test, but one species found after was unexpected.
Heretofore Eleodes nigrina was found only in
the Pinyon-Juniper community, and its occur-
rence in the Grmjia-Lijchim and Coleogyne com-
munities was unforseen.
Species stabilization in the sectors was great-
ly upset during the postshot periods of August
and September 1962 and June 1963 (Table''9).
By August 1963, the numbers of kinds of spe-
cies had become somewhat stabilized, but in
lower numbers than during the predetonation
time.
Conibiosoma elongatum was taken before
the detonation in sector 9 but not after in any
sector. This species was taken from June to
September in similar \egetative types in other
areas of the test site; so its disappearance was
unexpected.
Grid vs. Transect Extrapolation. Results be-
tween the main transect stations and the grids
could not be correlated relative to the numbers
of beetles captured. On the basis of adjustment
to the number of can traps used in each grid
and the respective sectors of the main transect,
considerable differences were noted. In June
1963, the transect cans caught 190 percent and
55 percent more beetles, respectively, than did
the grid cans in regions 1 and 3. At the same
time in region 2, the transect cans caught 9
percent less than did the grid cans.
In August 1963, the grid cans consistently
caught more beetles than did the transect cans—
20 percent, 57 percent, and 37 percent more in
regions 1, 2, and 3, respectively.
In Julv and August 1963, when the grids
and transect were utilized simultaneously,
beetles of 19 species were collected. Six of these
were found only in those cans arranged as a
grid, whereas 13 were captured in cans on the
TABLE 8. Species of tenebrionid beetles found after but not prior to a nuclear detonation.
Species
Eleodes nigrina
Eup.mphyhis castaneus
Euschides luctatus
Metoponium convcxicoUe
Pelcciiphoriis pantex
Pelecijphorus semilaevis
Sector
where
Presence
found
Date
Expected
4
Aug.-Sept. 1962
no
3,4,5
June 1963
yes
4
Aug.-Sept. 1962
yes
3,5,6,9
June 1963
yes
2 to 9
Aug.-Sept. 1962
Aug. 1963
yes
1 to 7,9
Aug.-Sept. 1962
Aug. 1963
yes
TABLE
9.
Number
of
speci
ies of tenebrionid
beetles found in
speci
ific
sectors pretest
and
posttest
Sedan.
Sector
Posttest
Pretest
Aug.-Sept.
1962
June 1963
Aug. 1963
1
2
3
4
5
6
7
8
9
5
5
5
5
4
5
3
1
3
6
10
7
2
8
0
3
3
2
4
5
6
3
3
2
1
3
4
3
3
3
3
3
2
2
'Collettion attempts not made.
12
Bmgham Young Uniyersity Science Bulletin
main transect and on tlie grid. None were
taken on the transect that were not also taken
on the grids.
Crater Occupants. Minimal populations of
beetles of five species were found in the bottom
of the Sedan crater in July and August 1963,
one year after the detonation. These were
Centrioptera muricata, Chilometopon abnorme,
Coelocnemus sulcata. Eleodes armata, and
Eleodes hispilahris. Three of these were previ-
ously taken in the environs of the Sedan crater.
Coelocnemus sulcata was not reported from the
test site heretofore, whereas C. abnorme was re-
ported previously from other areas of the site.
Centrioptera muricata was taken before the test
on transect F in sector 2, approximately 488m
from the lip of the resulting crater. Eleodes
armata was taken before the detonation within
488m of the crater and E. hispilabris within 183m
of the crater.
Ants
Aphaenogaster meg,ommatiis. Ants of this
species were not found prior to or immediately
after the test, but a single specimen was taken
in June 1963 in sector 7. The usual habitat of
this species is not the vegetative types that oc-
cur in the environs of the Sedan crater but
is commonly the Larrea-Frameria commimity.
Seasonally these ants were most active above
ground in July and August, and only one speci-
men was taken elsewhere on the test site in
June.
Crematogaster coarctata. Two ants of this
species were taken in sectors 3 and 9 prior to
the test, and only one was taken on the grid
in sector 2 in August 1963. This species was not
commonly found elsewhere at the test site in
the vegetative types peculiar to the Sedan crater
environs, although seasonally it was abundant
from June to August in other areas.
Iridomyrmex pruinosum. Animals of this
species were present in small numbers in sectors
1, 2, 5, 8, and 9 prior to the test. After the test
in June 1963, three specimens were found in
sector 7. Elsewhere on the test site this species
was common in the same vegetative types as
those which surround the Sedan crater. Sea-
sonalh' it was most common in Jime and July,
but rapidly diminished in above-ground activity
in August.
Myrmecocystus mexicanus. Ants of this
species were present in sectors 4 to 9 prior to
the detonation (Table 10). One and two months
after the detonation none were found in any
sector except 4 and 9. In June 1963, ants were
found in sectors 5 to 7. In sector 6, 175 percent
more ants were found than expected. In Au-
gust 1963, ants were found in sectors 3, 7, and
8; none were expected in sector 3. In other sec-
tors, except 7, fewer animals were found than
expected. An increase of 175 percent occurred
in sector 7. Considering all sectors at the period
of one and two months after the detonation,
populations were 94 percent less than expected;
in June 1963, 42 percent more; and in .\ugust
1933, 55 percent less.
Ecolo'jjieallv, pretest and posttest popula-
tions were significantly lower than expected
in all sectors except numbers 1 and 2.
Mt/rmecocystus mimicus. Ants were present
in sectors 2, 5, 7, 8, and 9 before the detonation
(Table 11). One and two months after the
test, specimens were found only in sector 9.
In Juni- 1963, ants were present in sectors 5, 7,
and 8, and in sectors 5 and 7 in August 1963.
In sector S in June 1963 twice as many ants
were present as expected, and in August 1963
in sector 5, A'A times more ants were present
than expected. One and two months after the
detonation, populations in all sectors had di-
minished from the expected by 84 percent. In
TABLE 10. Effects of a nuclear detonation on popui.itions oi ants ot the species Mijrmrcpcij.stua tiwxicauus.
No.
specimens
Pre-
test
Posttest
Aug.-Sept.
1962
June 1963
Aug.
1963
Sector
Actual Expected
Actual
E.X
pected
Actual
Expected
3
0
0
0
0
0
1
0
4
2
1
4
0
2
0
2
5
9
0
17
4
5
0
9
6
7
0
12
11
4
0
7
7
5
0
8
2
3
11
4
8
2
0
2
0
1
2
2
9
7
2
12
0
4
0
7
Total
32
55
17
19
14
31
Biological Series, Vol. 18. No. 4 Effects of Nuclear Detonation on Arthropods
13
TABLE 11. Effects of a nuclear detonation on populations of ants of the species Myrmecocystus mimicus.
No.
specimens
Pre-
test
Posttest
Aug.-Sept.
1962
June 1963
Aug.
1963
Sector
Actual Expected
Actual
E.xpected
Actual
Expected
2
1
o
•
0
3
0
1
5
4
0
4
1
1
9
2
7
18
0
16
2
5
4
11
S
5
0
5
2
1
0
3
9
7
5
6
0
2
0
4
Total
35
5
31
5
12
13
21
'('ollection attempts not niade.
June 1963 the population wa.s 58 percent lower,
and in August 1963, 38 percent lower than ex-
pected.
Ecologically, pretest and posttest popula-
tions were not significantly different from the
expected nonn, except in sector 7, where the
population before the test was higher than e.x-
pected.
Pheidole hicarinata. Before the detonation,
ants were found in all sectors except number 9
(Table 12). None were found one and two
months later. In June 1963, ants were found
only in sectors 4 and 5 and none were found
in any sector in August 1963. A 100 percent
reduction from the e.xpected occurred one and
two months after the detonation, whereas the
populations in June 1963 were 75 percent lower,
and in August, 100 percent lower than expected.
Ecologically, the only significant deviation
from the expected norm was in sector 2 before
the detonation, when populations were higher
than expected.
Pogonomyrmex californicus. Ants of this spe-
cies were found in everv sector except number
9 before the detonation (Table 13). One and
two months after the detonation they were
found in sectors 4, 5, 6, and 9. In June 1963,
they were foimd in all sectors except numbers
7 and 8, but in August 1963, only in sectors
1 to 5. One and two months after the detona-
tion the population was only 23 percent less
than expected, in June 1963 it was 46 percent
less, and in August 1963 it had diminished by
76 percent.
Ecologicall}', populations in most sectors be-
fore the test were significantly different from
the e.xpected norm. In sectors 1, 2, and 9
they were lower than expected, whereas in sec-
tors 3 and 5 they were higher. After the det-
onation, populations in all sectors except 5 and
6 were lower than the expected norm, whereas
in sector 5 the population was higher. No sig-
nificant change from the expected occurred in
sector 6.
Pogonoinijrmex rtigosus. Only one specimen
of tiiis species was found before the detonation
in sector 9. One and two months after the deto-
nation, two specimens were found in sector 9.
None were found in June and August 1963. In
other areas of the test site ants of this species
T.^BLE 12. Effects of a nuclear detonation on populations of ants of the species Pheidole hicarinata.
No.
specimens
Pre-
test
Posttest
Aug.-Sept
. 1962
J'
ane 1963
Aug.
1963
Sector
Actual
Expected
Actual
Expected
Actual
Ex
pected
1
1
o
o
0
1
0
0
2
7
o
e
0
3
0
1
3
2
0
1
0
1
0
0
4
1
0
0
1
1
0
0
5
5
0
1
2
2
0
1
6
4
0
1
0
2
0
1
7
2
0
1
0
1
0
0
8
2
0
1
0
1
0
0
Total
24
0
5
3
12
0
3
"Collection attempts not made.
14
Bricham Young University Science Bulletin
TABLE 13. Effects of a nuclear detonation on populations of ants of the species Pogononnjrmex californicus.
No.
specimens
Pre-
test
Posttest
Aug.-Sept. 1962
J>
uie 1963
Aug.
1963
Sector
Actual
Expected
Actual
Expected
Actual
Expected
1
4
0
e
1
3
3
3
2
3
e
s
3
1
1
1
3
40
0
22
5
13
3
17
4
14
6
9
1
5
1
7
5
28
25
18
6
10
4
14
6
7
14
4
4
3
0
3
7
5
0
4
0
3
0
3
8
5
0
4
0
3
0
3
9
0
2
0
2
0
0
0
Total
106
47
61
22
41
12
51
•Collection attempts not made.
were most abundant in the Coleogijne and
Grayia-Lijchim communities, where seasonally
their above-ground activity was greatest from
June to September.
Veromessor lariversi. Seven ants of this spe-
cies were found in sector 5 before the detona-
tion. None were found after the tests e.xccpt
on the grid in sector 2, where two specimens
were taken in June 1963. In other areas of the
test site, ants of this species were inhabitants
principally of Piinon-Junipcr areas and were
most active in June and July.
Veromessor smithi. Five ants of this species
were found onlv in June 1963 after the deto-
nation in sectors 5 and 6, and on the grid of
sector 8. In other sections of the test site these
ants were taken infrequentlv in few numbers
only in the Coleogyne community in June.
Changes within Sectors. In August and Sep-
tember, 1962, populations in all sectors were
consistently less than the expected nomial, ex-
cept in sector 6 where they were the same as
expected. In June 1963, all populations were
less than the expected normal, except in sector
6 where they were 200 percent higher. All pop-
ulations in August 196.3 were less than the ex-
pected nonn.
Pretest populations were lowest in sectors
1 and 2 and higliest in sectors 3 and 5.
No significant changes in species composi-
tion occurred in the sectors by August and
September immediately after the test. How-
ever, in sector 9 one species was found after the
detonation that was not taken prior to the test.
Most changes were noted in June 1963, when
three species were found in sectors 5, 6, and
7 that had not been found there previously.
Similarly, two species were found in August
1963, in sectors 2 and 3. Eight species were
found before the detonation, only four in Au-
gust and September immediately after the det-
onation, seven in June 1963, and only four in
August 1963 (Table 14). One species, Vero-
messor lariversi, taken in sector 5 before the
detonation, was never taken subsequently, and
TABLE 14. Number of species of ants found in specific sectt>rs pretest and posttest Sedan.
Sector
Pretest
Posttest
Aug.-Sept. 1962
June 1963
Aug. 1963
1
2
3
4
5
6
7
8
9
3
4
3
3
6
3
4
5
5
0
2
1
1
0
0
4
1
1
1
2
5
2
4
1
1
1
2
2
1
2
0
2
1
0
*Colle«"ti<)n attempts not ni.idc.
Biological Sekies, Vol. 18, No. 4 Effects of Nuclear Detonation on Ahthropods
15
two species, Aphaenogaster megommatus and
Veromessor sniithi in sectors 5 and 7, taken in
June 1963, were not found at any other time.
Complete or nearly complete elimination of
the population occurred in eight of the sectors
at some period after the detonation. A reduc-
tion of 100 percent occurred in August and
September 1962 in sectors 1, 2, 3, 7, and 8,
and in August 1963 in sectors 6 and 9. Ninety
percent reduction was noted in sector 4 in Au-
gust 1963. In June 1963, populations in general
were not reduced as drastically as at other times.
In fact, in sector 6 in June 1963, a 200 percent
increase in population occurred when compared
to the expected norm. Similarly, the popula-
tion in sector 6 in August and September 1962
was the same as anticipated.
Total populations of all species of ants were
64 percent lower in August and September
1962 than the expected normal, only 30 percent
lower in June 1963, but 69 percent lower in
August 1963.
Grid vs. Transect Extrapolation. One speci-
men of Mynnecoct/stus mexicanus was taken on
the grid in sector 8 in June 1963 and one on
the grid in sector 4 in August 1963, although
beetles of this species were not taken on the main
transect in that sector. Similarly, other species
taken on the grids but not on the corresponding
transect in 1963 are Crematogastcr coarctata
and M. mimicus in sector 2 in August, Pheidolc
hicarinata in sector 2 in June, and Veromessor
smithi in sector 8 in June. None were found
on the transect that were not also taken on the
corresponding grid.
Orthopterans
The few specimens of this group collected
in June and August 1963 have not as yet been
identified to species. Consequently, effects of
the detonation on these insects are discussed
only for the immediate posttcst period of Au-
gust and September 1962.
Arenivaga erratica. Roaches of this species
were found in all sectors except 5, 8, and 9 be-
fore the detonation. After the test, the specimens
which were found onlv in sectors 3, 4, 5, and
9 represented a 450 percent increase above the
number expected. In other areas of the test
site roaches of this species were abundant in
the same vegetative tvpes as those which occur
in the environs of the Sedan crater. Seasonally,
however, populations of these roaches were at
low levels during August and September.
Ceuthophihis jossor. Crickets of this species
were found in sectors 1 to 7 (except 6) before
the detonation. After the test they were found
only in sector 9 in small numbers. In other areas
of the test site these insects were most common
in the same vegetative types that occur around
the Sedan crater. Seasonally they were most
abundant from March through July, and in few
numbers in August and September. This sea-
sonal variation likely accounts for the few
numbers found immediately after the detona-
tion in the Sedan area.
Ceuthophihis lameUipes. These crickets were
found in all sectors except numbers 2 and 7
before the detonation. Afterward, they were
found in all sectors except number 6. Their
numbers after the test were diminished by 97
percent from the expected normal. In other
areas of the test site these crickets were most
abundant in the same vegetative types that oc-
cur in the environs of the Sedan crater. Season-
ally they were most abundant from August to
November. Consequently, such few numbers
after the detonation seem significant.
Litaneutria minor. Three praying mantids
were found only in sectors 1, 5, and 6 before
the detonation; none were found after. In other
parts of the test site these insects were most
abundant in Coleogyne, which also occurs in the
area of the Sedan crater. Seasonally they were
relatively abundant during August and Septem-
ber. Their apparent absence after the test likely
was due to normal low populations in this par-
ticular area.
Stenopelmatus fuscus. Before the detona-
tion, Jerusalem crickets were found only in sec-
tors 1 to 5. After the test they were taken in
sectors 3 to 9, except 7 and 8. In all sectors
except 3 and 5 the numbers found were greater
than expected. Considering all sectors, popula-
tions increased by 36 percent over the expected.
In other areas of the test site these crickets
were most abundant in Graijia-Lijcium and
Pinyon-Juniper areas. Tlieir populations were
low in other vegetative types. Seasonally they
were most abundant from May to August and
in October. Consequently, their high popu-
lations in the environs of the Sedan crater in
August and September were expected.
Changes within Sectors. In August and
September 1962, populations in all sectors ex-
cept number 7 were considerably less than the
expected normal. In sector 7 an increase in
numbers occurred. Considering all species and
all sectors, a 93 percent reduction in popula-
tion occurred after the detonation.
Before the detonation, species distribution
was about equal between all sectors except num-
16
Bricham Young Univehsity Science Bulletin
bers 8 and 9, which had only one species
present. After the detonation, numbers of spe-
cies were concentrated in sectors 3, 4, 5, and
9. Three of the four species in sector 9 after
the test were found no closer than sectors 5
and 7 prior to the test.
Scorpions
Hadriiius spadix. Scorpions of this species
were found in few numbers and only in
sectors 1, 4, and 5 before the detonation. In
August and September 1962 (after the test)
they were found in greater nimibcrs than ex-
pected and only in sectors 3 and 5. In June
and August 1963, they were found in few num-
bers in sector 7. In no sector did the numbers
deviate significantly from the expected, either
before or after the detonation. In other areas
of the test site these scorpions were most abun-
dant in the Artemisia and Mixed plant associ-
ations, types which were not common in the
environs of the Sedan crater. Seasonally over
the test site these animals were active from
April to October, predominantly in July.
Vaejovis becki. Before the detonation these
scorpions were found in sectors 3 to 9, except
4. After the test in August and September
1962, the scorpions were found only in sectors
3, 4, 5, and 7. In June 1963, they were found
only in sector 7, and in August 1963, only in
sector 8. In no sector did the numbers found
deviate significantly from the expected, either
before or after the detonation. In other areas
of the test site these scorpions were abundant
in the same vegetative types that occur in the
environs of the Sedan crater. Seasonally they
were collected from March to September, pre-
dominantly from June to August.
Vaejovis boreus. Scorpions of this species
were not found in the Sedan area prior to the
detonation. In August and September 1962 they
were found in sectors 3, 4, and 5, but none were
found in June or August 1963. The numbers
present in the sectors did not deviate signifi-
cantly from the expected, either before or after
the detonation. In other areas of the test site
these scorpions were not abundant in the Grat/ia-
Ltjcium community and were not found at all
in the Coleoi^ijne and Salsola communities. Sea-
sonallv tliey were taken from June to Septem-
ber, and predominantly from JuK- to September.
Vaejovis confusus. Before the detonation
these scoipions were found in all sectors except
numbers 6 and 8. In August and September
1962 they were found in sectors 3, 4, 5, and
7. In that latter period, populations had in-
creased bv 438 percent above the expected. In
June 1963, scorpions were found in sectors 2 to
7 (except number 6), and in August 1963 only
in sectors 1, 2, 5, and 9. Significant differences
from the expected occurred in sectors 1 and
2 before the detonation and in sectors 3, 4, 5,
and 7 after the detonation, when more scorpions
were found than expected. In other areas of the
test site, scorpions of this species were moder-
ately abundant in the similar vegetative types
that occur in the environs of the Sedan crater.
Seasonally, specimens were taken from March
to November, predominantly from June to Au-
gust.
Changes iiithin Sectors. Significant differ-
ences occurred in populations in sectors 6, 8,
and 9 in August and September 1962, when
numbers were reduced by 100 percent. Simi-
lar reductions occurred in sectors 1, 6, 8, and
9 in June 1963 and in sectors 3, 4, 6, and 7 in
August 1963. Significant changes occurred in
sectors 3, 4, 5, and 7 in August and September
1962, with increases of 575 percent, 950 per-
cent, 350 percent, and 125 percent, respectively.
Only one significant increase occurred in June
1963— sector 7 with 166 percent. No increases
were noted in August 1963. Considering all sec-
tors, populations in August and September 1962
increased 160 percent but decreased liy 50 per-
cent and 72 percent in June and August 1963,
respectivelv, from the expected nomial.
Species composition in the sectors before
the test vaiied from one to three. In August
and September 1962, sectors 3 and 5 contained
all four species, but in June and August 1963, no
sector contained more than one species, except
sector 7, which had three in June.
Crater Occupants. One specimen of Had-
ruriis spadix was found in the bottom of the
crater in July 1963.
Grid vs. Transect Extrapolation. Scorpions
of lladrunts spadix were found on the grids in
sector 2 in August, sector 4 in June and August,
and sector 8 in June, but not on the correspond-
ing parts of the main transect. Those belonging
to Vaejovis becki were found on the grids in
sectors 2 and 4 in August, but not on the tran-
sect. Scorpions of V. confusus were taken on
the grids in sector S in Jime and sectors 4 and
8 in August, but not on the corresponding
transect.
Solpugids
Ihunchia potens. These solpugids were
found in few numbers and only in sector 8 be-
fore the detonation. None were found after.
BiOLOCiCAL Series, Vol. 18, No. 4 Effects of Nucxear Detonation on AnTHROPODS
17
In otlier areas of the test site, these organisms
were found in the Coleogijne and Graijia-Lijc'mm
communities in relative abundance from June
to September, predominantly in June and July.
Their seasonal limitations likely explain their
absence in August and September, but not their
absence in June 1963.
Eremohates scopulatus. These specimens were
found only in sector 1 before the test; none
were foimd after. In other areas of the test site
these animals were present in the similar vege-
tative types that occur in the area of the Sedan
crater, found predominantly in May, but also
present in June and July. This seasonal limita-
tion likelv explains their absence in June and
August after the test.
Eremorhax piilcher. This solpugid was found
only in sector 4 prior to the detonation; none
were found after except on the grid in sector
2. In other areas of the test site this new spe-
cies, described bv Muma in 1963, was taken in
few numbers in the Grayia-Lycium and Sahola
communities in June and July.
Hemerotrecha californica. Solpugids of this
species were foimd before the detonation in sec-
tors 2, 3, 5, 6, and 7. None were found after
the test. In other parts of the test site these
animals were most abundant in the Coleogyne
and Grayia-Lycium communities, but none were
found in Sahola. Seasonally they were taken
from April to September, predominantly in June.
Their absence in the sectors in June 1963 was
unexpected.
Hemerotrecha proximo. This species de-
scribed as new by Muma (1963) was repre-
sented by specimens found in sector 8 after the
test, but only in August and September, 1962.
In other areas of the test site the few speci-
mens of this species that were taken were pre-
dominantly in the Grayia-Lycium community
in October. Their occurrence in sector 8 was
expected, but not so early in the season.
Hemerotrecha scrrata. A single specimen
was found in sector 2 before the test, but none
after. In other areas of the test site these sol-
pugids were commonly found in the same vege-
tative t\pes that occur in the environs of the
Sedan crater. Seasonally they were found from
June to September, predominantly in July and
August.
Changes within Sectors. The almost com-
plete absence of solpugids in any of the sectors
after the detonation is indicative of the tre-
mendous influence of the detonation on sol-
pugids, although seasonal differences must be
considered as somewhat influential also on their
occurrence.
Crater Occupants. Specimens of two spe-
cies taken from the crater in August 1963 were
not found on the main transect, but one of the
species was taken on the grids in sectors 2
and 4. One specimen each of Eremohates zinni
and Therobates cameronensis was found in the
crater in August 1963. In other areas of the
test site E. zinni was the most abundant in the
Grayia-Lycium community and was also found
in Sahola; none was taken in Coleogyne. Sea-
sonally this species was found only in July and
August. Therobates cameronensis was found
in moderate abundance in Coleogyne and
Grayia-Lycium but not in Sahola. It occurred
from May to July.
Grid vs. Transect Extrapolation. Only one
species of solpugids was taken on the grids but
not on the main transect— Eremohates zinni, taken
in sectors 2 and 4 in August 1963. A specimen
of Eremorhax piilcher was taken from the grid
in sector 2 in August 1963, but not on the cor-
responding parts of the transect.
Spiders
Calilena restricta. A single specimen was
taken in sector 6 before the test. None were
taken after. In other areas of the test site these
spiders were only moderately abundant in the
Grayia-Lycium community. They were active
from February to December, predominantly
from June to November.
Gnaphosa hirsutipes. Only three spiders of
this species were taken before the test, all in
sector 7. None were taken after. In other areas
of the test site these spiders were relatively
abundant in the same vegetative types that oc-
cur in the environs of the Sedan crater. They
were active from Febraary to November, pre-
dominantly in June and July.
Haplodrassus eunis. Three specimens of this
spider were taken in sectors 2 and 3 before the
detonation. None were found after. In other
areas of the test site these spiders were com-
mon in undisturbed vegetation of the types
that occur in the environs of the Sedan crater.
Tiiey were active all months of the year, but
in predominant numbers only in the nonsum-
mer months of October to April.
Herpyllus hesperolus. A single spider of
this species was taken in sector 8 before the
test, and one specimen was taken after the
detonation in sector 7 and in August 1963. One
specimen was taken on the grid in sector 2
18
BuicuAM Young University Science Bulletin
in June 1963. In other areas of the test site
these spiders were rehitively abundant in un-
disturbed vegetation of the types which occur
in the area of the Sedan crater. Seasonally they
were active the year around, but predominantly
in April. Few were taken from June to August.
Loxosceles ttnicolor. Spiders of this species
were not found prior to the detonation. After
the test, a single specimen was found in sector
8 in June, and two in sectors 2 and 7 in August
1963. These spiders were not found in other
areas of the test site in the same vegetative
types that occur near the Sedan crater. Thev
were found predominantly in the Mixed type of
vegetation from April to September, predomi-
nantly in July and August.
Me<iamyrmecion naturalisticum. Spiders of
this species were found before the test in sec-
tors 2 and 7. None were found after. In other
areas of the test site these spiders were most
common in the Coleogyne community from April
to September, predominantly in June and July.
Neoanaiiraphis chamberlini. Spiders of this
species were taken before the test in all sectors
except number 9. The only ones found after the
test were taken in sectors 2, 6, and 8
in June, and in sector 4 in August 1963.
In other areas of the test site these spiders
were common in the Coleogyne, Grayia-Lychtm,
and Salsola communities. They were active
from February to October, predominantly from
June to October.
Orthonops gertschi. These spiders were
found before the test in sectors 5, 7, and 9. None
were found after. In other areas of the test
site spiders of this species were not abundant
in the vegetati\e tvpes common to the Sedan
area. They were acti\e from March to Sep-
tember, predominantly from April to July.
Physocyclus tanneri. Only one specimen of
tliis species was taken before the test, in sector
6. None were found after. In other areas of
the test site these spiders were not abundant
and were found onlv in August.
Psilocliorus utahensis. Spiders of this spe-
cies were the most abundant ones represented
in the Sedan area. They were found before the
test in all sectors, predominantly in sectors 6
and 7 (Table 15). One and two months after
the detonation they were not found at all. In
June 1963, they were found in all sectors except
numbers 1 and 2, and in August 1963, they were
found on the grids in sectors 2 and 8. Considering
all sectors, their 100 percent reduction in numbers
from the expected norm in August and Sep-
tember 1962 and in August 1963 is significant.
Likewise, in June 1963 their populations were
reduced b\' 50 percent. In other areas of the
test site these spiders were predominant in the
same vegetative types that occur around the
Sedan crater. Seasonally they were active all
vear, predominantly from June to August. Eco-
logicalh', before the test, in all sectors popula-
tions of this spider were higher than expected.
After the detonation, populations were not gen-
erally different from the expected.
Syspira eclectica. Spiders of this species were
found before the test only in sectors 8 and 9.
None were found after. In other areas of the
test site, these spiders were not common in the
same vegetative types that occur around the
Sedan crater. They were active from April to
November, predominantly from May to August.
Changes tcithin Sectors. Significant differ-
ences from the expected occurred in August and
TABLE 15. E
ffects of ;i
I nuclear deton
ation
on populations of s
piders of the species
Psilochon
ts utahensis.
No
. specimens
Pre-
test
Posttest
Aug.-Sept.
1962
J
une
1963
Aug.
1963
Sector
Actual
Expected
Actual
Expected
Actual
Expected
1
8
a
e
0
4
0
2
2
4
e
»
0
2
0
1
3
7
0
3
1
4
0
2
4
8
0
3
0
4
0
2
5
7
0
3
4
4
0
2
6
21
0
9
4
10
0
7
7
19
0
8
5
9
0
6
8
7
0
3
/
4
0
2
9
7
0
3
2
4
0
2
Total
90
0
32
23
36
0
26
*Collcclion allcnipts n»l made.
BioLOGicAi, Series, Vol. 18, No. 4 Effects of Nuclear Detonation on Arthhopods
19
September 1962 in sectors 6 and 7, where a 100
percent reduction in population occurred. In
June 1963, reductions of 100 percent occurred
in sectors 1 and 4, whereas in sectors 5, 6, and
8 populations were much higher than expected.
In August 1963, 100 percent reductions from
the expected occurred in all sectors except 2
and 7, where the actual numbers were equal
to the expected. Considering all sectors, popu-
lations in August and September 1962 decreased
by 100 percent, increased 33 percent in June
1963, then decreased by 80 percent in August
1963 from the expected normal.
Species composition in the sectors before
the test varied from 2 to 5. In June 1963, sec-
tors 3, 5, 7, and 9 each contained only one
species, whereas sectors 6 and 8 each contained
two. In August 1963, sector 7 contained two
species.
Grid vs. Transect Extrapolation. Spiders of
Herpyllus hesperolus were not found on the
main transect in sector 2 in June, but were
found on the corresponding grid. Those of
Loxosceles unicolor were not found on the tran-
sect in sector 2 in August, but were found
on the grid. Spiders of 'Neoanagraphis chainher-
lini were not found on the transect in sectors
2, 4, and 8 in June and August, but were found
on the grids. Psilochorus utahensis was not
found on the transect in sectors 2 and 8 in Au-
gust and sector 4 in June, but was found on
the corresponding grids.
SUMMARY
Fifty-three arthropod species were studied
in an area affected by an underground nuclear
detonation. These were represented by 10 spe-
cies of ants, 17 beetles, 5 orthopterans, 4
scorpions, 6 solpugids, and 11 spiders (Table
16). Relative populations were dctcnnined prior
to the detonation and at three periods after the
detonation— (1) one and two months after (Au-
gust and September 1962), (2) 11 months after
(June 1963), and (3) 13 months after (August
1963). One and two months after the detona-
tion, the number of species was reduced from
the expected b\' 48 percent, by 52 percent
after 11 months, and by 66 percent after 13
months. Greatest reduction of specimens oc-
curred with spiders, followed by ants and bee-
tles. Fewest changes occurred in the number of
scorpions.
Populations of each group changed signifi-
cantly in each period. Reductions from 30 per-
cent to 100 percent occurred in all groups in all
periods after the detonation except for the scor-
pions one and two months after, when an in-
crease of 160 percent was noted. After 11
months spiders had increased 33 percent ( Table
17).
Within specific sectors, populations did not
vary significantly from the expected except in
a few instances. In August and September 1962,
immediately after the detonation, populations
of arthropods in sectors 3, 4, and 5 were much
higher than expected. This represented the
area from approximately 65m to 140m from
ground zero. The increase may have been
due primarily to the physical transport and
initial survival of those arthropods living closer
TABLE 16. Effects of a nuclear detonation on species occurrence of arthropods in the disturbed area.
No.
Species
Category
Ants
Beetles
Orthoptera
Scorpions
Solpugids
Spiders
Total
Total no. involved
10
17
5
4
6
11
53
Pretest
Expected
Present
10
8
14
9
5
5
4
3
5
4
10
10
48
39
Posttest Aug.-Sept. 1962
Expected
Present
9
4
16
12
5
4
4
4
3
1
11
0
48
25
Posttest June 1963
Expected
Present
10
7
11
8
4
o
4
3
5
0
10
3
44
21
Posttest Aug. 1963
Expected
Present
9
3
15
8
5
0
4
2
2
0
9
2
44
15
•Ilata nut available.
20
BnicHAM Young University Science Bulletin
to ground zero than 65ni. Similarly, slight in-
creases were noted in sectors 7 and 9, but these
likely were not significant. In June 1963 in
sector 5 and in August 1963 in sector 3, slight
increases in populations were noted. These may
have been due to seasonal differences correlated
with vegetative type, and are also not consid-
ered significant.
TABLE 17. Population trends of arthropods affected by a nuclear detonation.
Group
Percent change from expected normal
Aug.-Sept. 1962
June 1963
Aug. 1963
Ants
Beetles
Orthoptera
Scorpions
Solpugids
Spiders
- 64
- 58
- 93
+160
- 90
-100
- 30
- 61
O
- 50
-100
-f 33
- 69
- 58
o
- 72
-100
- 80
'Data not available.
LITERATURE CITED
Allbed, D. M. and D E. Beck. 1967. Spiders of tlie
Nevada Tost Site. Great Basin Natur., 27( 1 ): 11-2.5.
Allred, D. M., D. E. Beck, and C. D. Jorcensen.
1963-a. Biotic communities of the Nevada Test
Site. Brigham Young Univ. Sci. Bull. Biol. Ser.,
l(2):l-52.
Allred, D. M., D E. Beck, and C. D. Jorcensen.
1963-1). Close-in effects of an underground nuclear
detonation on small mammals and selected inver-
tebrates. (Preliminary Report) Operation Sedan,
PNE-226 (P), Project 62.87, Office Tech. Services,
Oept. Commerce, Washington, D.C.
Allred, D. M., D E. Beck, and C. D. Jorcensen.
1964. Close-in effects of an underground nuclear
detonation on small mammals and selected inver-
tebrates. (Final Report) Project Sedan, PNE 226F,
Project 62.87, Office Tech. Services, Dept. Com-
merce, Washington, D.C.
Barnum, a. H. 1964. Orthoptera of the Nevada Test
Site. Brigham Young Univ. Sci. Bull. Biol. Ser.,
4(3):1-134.
Cole, A. C. 1966. Ants of the Nevada Test Site.
Brigham Y'oung Univ. Sci. Bull. Biol. Ser., 7(3):
1-27.
Certsch, W. J., and D. M. Allred. 1965. Scorpi-
ons of the Nevada Test Site. Brigham Young Univ.
Sci. Bull. Biol. Ser., 6(4):1-15.
Jorcensen, C. D., D. M. Allred, and D E. Beck.
1963. Some effects of an underground nuclear
detonation on biotic communities at the Nevada
Test Site. Proceedings Utah Acad. Sci. Arts and
Letters, 40(1):49-61.
.\IuMA, M. H. 1963. Solpugida of the Nevada Test
Site. Brigham Young Univ. Sci. Bull. Biol. Ser.,
3(2); 1-13.
Tanner, V. M.. and W. A. Packham. 196.5. Tene-
brionidae beetles of the Nevada Test Site. Brig-
ham Young Univ. Sci. Bull. Biol, Ser., 6(1): 1-44.
DATE DUE
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