nvans ~~ JOURNAL
OF THE
KENTUCKY
ACADEMY OF
SCIENCE
Official Publication of the Academy
SMITASOT “ee
Volume 62
Number 1
Spring 2001
The Kentucky Academy of Science
Founded 8 May 1914
GOVERNING BOARD
EXECUTIVE COMMITTEE
2001
President: Ron Rosen, Department of Biology, Berea College, Berea, KY 40404
President Elect: Jerry W. Warner, Department of Biological Sciences, Northern Kentucky University,
Highland Heights, KY 41099
Vice President: Robert Barney, Community Research Service, Kentucky State University, Frankfort, KY
40601
Past President: Blaine R. Ferrell, Department of Biology, Western Kentucky University, Bowling Green,
KY42101
Secretary: Stephanie Dew, Department of Biology, Centre College, Danville, KY 40422
Treasurer: Kenneth Crawford, Department of Biology, Western Kentucky University, Bowling Green,
KY 42103
Executive Secretary (ex officio): Donald Frazier, Science Outreach Center, University of Kentucky, Lex-
ington, KY 40536-0078
Editor, JOURNAL (ex officio): John W. Thieret, Department of Biological Sciences, Northern Kentucky
University, Highland Heights, KY 41099; (859) 572-6390
Editor, NEWSLETTER (ex officio): Brent Summers, Department of Biology, Campbellsville University,
Campbellsville, KY 42718-2799
Chair, Junior Academy of Science (ex officio): Elizabeth K. Sutton, Department of Chemistry, Campbellsville
University, Campbellsville, KY 42718
Program Director (ex officio): Robert O. Creek, Department of Biological Sciences, Eastern Kentucky
University, Richmond, KY 40475 .
Editor, JKAS Webpage (ex officio): Claire Rinehart, Department of Biology, Western Kentucky University,
Bowling Green, KY 42103
COMMITTEE ON PUBLICATIONS
Editor and John W. Thieret, Department of Biological Sciences, Northern Kentucky University,
Chair: Highland Heights, KY 41099
Associate Editor: James O. Luken, Department of Biological Sciences, Northern Kentucky University,
Highland Heights, KY 41099
Index Editor: Varley Wiedeman, Department of Biology, University of Louisville, Louisville, KY
40292
Abstract Editor: Robert Barney, Community Research Service, Kentucky State University, Frankfort,
KY 40601
Editorial Board: John P. Harley, Department of Biological Sciences, Eastern Kentucky University,
Richmond, KY 40475
Marcus T. McEllistrem, Department of Physics and Astronomy, University of
Kentucky, Lexington, KY 40506-0055
J.G. Rodriguez, Department of Entomology, University of Kentucky, Lexington, KY
40546-0091
John D. Sedlacek, Community Research Service, Kentucky State University,
Frankfort, KY 40601
Gordon K. Weddle, Department of Biology, Campbellsville University, Campbellsville,
KY 42718-2799
All manuscripts and correspondence concerning manuscripts should be addressed to the Editor.
The JOURNAL is indexed in BIOSIS, Cambridge Scientific Abstracts, and in State Academies of Science Abstracts.
Membership in the Academy is open to interested persons upon nomination, payment of dues, and election. Application
forms for membership may be obtained from the Secretary. The JOURNAL is sent free to all members in good standing.
Annual dues are $25.00 for Active Members; $15.00 for Student Members; $35.00 for Family; $350.00 for Life Mem-
bers. Subscription rates for nonmembers are: $50.00 domestic; $60.00 foreign. Back issues are $30.00 per volume.
The JOURNAL is issued semiannually in spring and fall. Two numbers comprise a volume.
Correspondence concerning memberships or subscriptions should be addressed to the Executive Secretary.
This paper meets the requirements of ANSI/NISO Z39.48-992 (Permanence of Paper).
INSTITUTIONAL AFFILIATES
Fellow
University of Kentucky University of Louisville
Sustaining Member
Eastern Kentucky University Northern Kentucky University
Morehead State University Western Kentucky University
Murray State University
Member
Bellarmine College Cumberland College
Berea College Somerset Community College
Campbellsville University Southeast Community College
Centre College
Associate Member
Georgetown College Midway College
Jefferson Community College | Owensboro Community College
Kentucky State University Spalding University
Kentucky Wesleyan College Thomas More College
Maysville Community College Transylvania University
INDUSTRIAL AFFILIATES
Associate Patron
Ashland Oil, Inc.
Member
Corhart Refractories Corporation
MPD, Inc.
X
Associate Member
All-Rite Pest Control
Wood Hudson Cancer Research Laboratory, Inc.
OT EOE
JOURNAL OF THE KENTUCKY ACADEMY OF SCIENCE
ISSN 1098-7096
Continuation of
Transactions of the Kentucky Academy of Science
Volume 62
spring 2001
Number 1
J. Ky. Acad. Sci. 62(1):1-17. 2001.
The genus Trifolium (Fabaceae) in Kentucky
Michael A. Vincent
W. S. Turrell Herbarium, Department of Botany, Miami University, Oxford, Ohio 45056
ABSTRACT
The scope and range of the genus Trifolium (Fabaceae) were examined for Kentucky. Review of literature
and 910 herbarium specimens from 35 herbaria revealed 11 species of clover as part of the state’s flora: T.
arvense, T. aureum, T. campestre, T. dubium, T. hybridum, T. incarnatum, T. pratense, T. reflexum, T. repens,
T. resupinatum, and T. stoloniferum. Four species are rejected as a part of the flora: T. alexandrinum, T.
ambiguum, T. hirtum, and T. medium. Descriptions, illustrations, and distribution maps are provided for
each species accepted.
INTRODUCTION
The genus Trifolium (true clovers) is a near-
ly cosmopolitan member of the papilionoid
Fabaceae (Leguminosae) that contains 240 to
250 species (Zohary and Heller 1984), though
this number, rising as new species are de-
scribed, may be closer to 300 (Gillett and
Cochrane 1973). In the Old World, Trifolium
is native to the Mediterranean region in south-
ern Europe, Asia Minor, the Midele East, and
northern Africa, extending into northern Eu-
rope and east to northwestern China; in Afri-
ca, the genus occurs through eastern regions
to South Africa. In the New World, there is a
wide diversity of species in western North
America, with fewer species native to eastern
portions, Central America, and South Ameri-
ca. According to Zohary and Heller (1984), the
genus may be subdivided into eight sections,
six of which (Paramesus, Mistyllus, Vesicaria,
Chronosemium, Trifolium, and Trichocephal-
um) are native entirely to the eastern hemi-
sphere; Lotoidea is native to both the eastern
and western hemispheres; Involucrarium is
endemic to the western hemisphere. The
word “clover” is probably derived from the
Dutch “klafer” or the Anglo-Saxon “cloefer,”
meaning “club,” a reference to the three-part-
ed leaf that supposedly resemble the three-
lobed club of Hercules (Evans 1957; Haragan
1991).
North America is home to ca. 95 species of
Trifolium, 65 native, 30 introduced. These
numbers are higher than those of Isely (1998),
since he was not aware of some of the less
frequently encountered introduced species.
Kartesz (1999) lists 96 species for North
America. Of the native North American spe-
cies, 43 belong in section Lotoidea; of these,
six are found east of the Mississippi River; the
remaining 37, mainly in the Rocky Mountains
and along the Pacific coast. The native species
in section Involucrarium are all found in west-
ern North America. The introduced species,
representing all sections of the genus except
Paramesus, have been imported mainly for ag-
ricultural purposes, though some introduc-
tions appear to have been inadvertent (Isely
1998).
Clover species have been widely cultivated
as forage crops for hundreds, if not thousands
of years, and are of great economic impor-
tance (Duke 1981). In North America, most
of the species cultivated are perennials, among
the most commonly grown of which are T.
2 Journal of the Kentucky Academy of Science 62(1)
praten ed clover), T. repens (white, Dutch,
or Ll. » clover), and T. hybridum (Alsike
clov: \nnual species sometimes cultivated
inclide LT. inearnatum (crimson clover), T. hir-
rose clover), and T. alexandrinum (ber-
cin clover). Clovers are used as forage crops,
as sources of nectar for honey production
Pellett n.d.), for erosion control, and as nitro-
gen sources for crop fields and pastures. Men-
ke and Hillenmeyer (1886) considered “clo-
ver” (species not specified) to be the most im-
port mt crop then grown in Kentucky.
There is a considerable body of folklore as-
sociated with the clovers (Evans 1957). Four-
leaf clovers have long ee considered a
source of good luck and with having the ability
to protect against witchcraft (RDA 1986).
Four-leaf clovers are actually leaves with mu-
tations resulting in the prolife ration of leaflets,
with leaflet numbers ranging anywhere from
the more commonly seen 4 to 24 or more
(Ford and Claydon 1996; Jaranowski and Bro-
da 1978) or rarely a single leaflet (Atwood
1938). The multifoliolate condition is relativ ely
common throughout Trifolium. Also of inter-
est to many are the leaf marking patterns on
the leaves of many Clover species. These can
range from the more commonly encountered
V-shape -d pattern, or chevron, to various types
of dark to light, colored or white patterns
(Corkill 1971; Ganders et al. 1980). These
marks, although attractive, are very variable
within a species; they can be inherited to dif-
fering degrees, may sometimes vary according
to growing conditions, and provide no infor-
mation of taxonomic value.
During the last 200 years, beginning with
M’Murtrie’s Florula Louisvillensis (1819),
many reports have been published on the flora
of Kentucky. In those reports, various ac-
counts of the clovers have appeared. The ear-
liest report of Trifolium in the state was of T.
arvense, T. pratense, and T. repens (M°’Murtrie
1819). In the 20th century, McFarland (1942)
reported 9 species, and Braun (1943) reported
5. Wharton and Barbour (1971) mentioned
only 1, Meijer (1992) listed 9, and Browne and
Athey ( 1992) and Medley (1993) accepted 11.
Most rece tly, Kartesz (1999) recognized 10
species as part of the Kentucky flora.
The purpose of this paper is to determine
which species of Trifolium are documented for
Kentucky and to clarify the known distribution
for each species in the state.
MATERIALS AND METHODS
| examined 910 herbarium specimens from
the following herbaria (acronyms from Holm-
1990): APSC, BEREA, BH, BRIT,
CM, DAO, DHL; EKY,-F-GA
GH, KNK, KY, LLO, LSU, MDKY, MICH:
MO, MU, NCU, NY, OKL, OSH, PH, SIU,
US, VDB, WIS, WKU, and WVA. In addition,
specimens were studied from the herbaria of
Cumberland College in Wilmington, Kentucky
(cumb), the Kentucky Agricultural Experi-
ment Station in Lexington (kes), and the clo-
ver herbarium of the Department of Agricul-
ture, University of Kentucky, Lexington (uk).
Distributional data were gathered from her-
barium records only; no undocumented re-
ports are included in distribution maps. Un-
fortunately, specimens in the Athey Herbari-
um (MEM) were unavailable. Distribution re-
cords from books, papers, and theses were not
included, and data in other published sources
may not coincide with those presented here
(e.g., Browne and Athey 1992).
gren et al.
CAN, CINC,
RESULTS
Eleven species of Trifolium are documented
by herbarium specimens for Kentucky. Of
these, nine are introduced and two are native
to the state. Three clover species reported for
Kentucky in literature could not be docu-
mented by specimens and are excluded from
the flora. For 13 of the 120 Kentucky counties
(Adair, Boyd, Cumberland, Hancock, Hender-
son, Ow sley, Robertson, Scott, Simpson, Tay-
lor, Union, W. ayne, and Webster), I saw no clo-
ver specimens at all.
TAXONOMIC TREATMENT
Trifolium L., Sp. Pl. 764. 1753.
Annual, biennial, or perennial, glabrous to
pubescent herbs with a taproot or fibrous
roots. Stems simple to much-branched from
the base and above. Leaves alternate, pal-
mately trifoliolate to 5-7 foliolate; leaflets
toothed; stipules adnate to the petiole. Inflo-
rescences umbelliform, racemose, or capitate,
axillary or terminal, long-peduncled to sessile,
leafy or not; involucre absent or of small to
large free to fused bracts; flowers pedicellate
The genus Trifolium (Fabaceae) in Kentucky—Vincent
to nearly sessile, with or without bracts; calyx
tubular to campanulate, 5-lobed, lobes nearly
equal in length or the lower one longer, each
lobe entire to toothed; petals free to basally
fused, white, pink, red, purple, or yellow, per-
sisting in fruit, the petals clawed and often
fused with the staminal column, the upper
(banner) broad, oblong to obovate, the lateral
pair (wings) narrow, usually longer than the
lower pair (keel), which are fused into a boat-
shaped structure; stamens diadelphous, fila-
ments dilated below the uniform anthers: ova-
ry sessile or stalked, style curved upward, stig-
ma capitate to curved, ovules 1-12; fruit a
straight legume enclosed by the persistent ca-
lyx and corolla, dehiscent or indehiscent, seeds
1—3(9), globular to reniform.
KEY TO SPECIES OF TRIFOLIUM IN
KENTUCKY
1. Plants perennial, stoloniferous, rooting at the
nodes; inflorescences held on axillary, upright
stems, with or without a pair of bract-like leaves;
petals white to pinkish; flowers reflexing with age.
2. Peduncles 1-2, arising from upright axillary
stems with a pair of bract-like leaves; calyx 4-7
mm long, teeth subulate, twice as long as tube
a as rere cic Mite ah 11. T. stoloniferum
2. Peduncles 1, arising from leaf axil on stolon,
without bract-like leaves: calyx 3-5 mm long,
teeth triangular-lanceolate, lower about same
lemethtasyitibers warksn. Wh) 2) aplalt. ase 9. T. repens
1. Plants erect or decumbent, not rooting at the
nodes.
3. Petals yellow; banner petal obovate, straight or
downcurved; fruit with an obvious stalk inside
calyx; petioles mostly shorter than leaflets.
4. Terminal leaflet sessile or nearly so; stipules
nearly as long as to longer than the petiole;
fruits 2 times the length of the style; seed
OVOIG! sists bh eR Sr eee eee
2. T. aureum
4. Terminal leaflet stalked; stipules about half
as long as the petiole; fruits 3-6 times the
length of the style; seeds ellipsoid.
5. Inflorescences 5-7 mm wide: flowers 2.5—
3.5 mm long; terminal leaflet stalk about
RminnMlon cme este yen? 4. T. dubium
5. Inflorescences 7-12 mm wide: flowers
3.5-7 mm long; terminal leaflet stalk 1-3
mm long
MS RHA eae 3. T. campestre
3. Petals white, pink, red, or purple; banner petal
oblong, upcurved; fruit not stalked or minutely
so; petioles mostly longer than leaflets.
(ow)
6. Flowers sessile or nearly so, erect to
spreading in fruit, in dense globose to
elongate heads.
7. Petals lavender to white: flowers re-
supinate; calyx with a more densely
pubescent region dorsally, becoming
inflated in fruit, with obvious reticulat-
ing veins
7. Petals pink, red, or white; flowers not
resupinate; calyx glabrous or with
evenly distributed pubescence, not be-
10. T. resupinatum
coming inflated in fruit, veins not ob-
viously reticulating.
8. Flowers 10-20 mm long; corolla
much longer than the calyx; leaflets
broadly ovate to obovate; stipules
broad, ovate.
9. Perennial; heads sessile or nearly
so, globose to ovoid; stipules
abruptly narrowed into an awn-
hikemtipg 5p teen eee eosin. |
S Seaets, 2 - Meter to gee 7. T. pratense
9. Annual; heads stalked, elongate-
ovoid to cylindrical; stipules
broadly rounded at the tip
4 Bee Ebates 6. T. incarnatum
8. Flowers 5-7 mm long; corolla
scarcely longer than to shorter than
the calyx; leaflets narrowly oblong
to linear-lanceolate; stipules nar-
rowly ovate to oblong .. 1. T. arvense
6. Flowers with pedicels, sharply reflexed in
fruit, in umbels.
10. Annual or biennial: flowers 8-14 mm
long; inflorescences 2-4 cm wide:
pedicels 4-12 mm long; calyx 6-9
mm long, teeth 2-3 times the length
of the tube; leaflets 14.5 x 0.5-2
cm; stipules broadly ovate, leaflike
SERRA CAR ang: 8. T. reflexum
10. Perennial; flowers 7-10 mm long, in-
florescences 1-2.5 cm wide; pedicels
1-5 mm long; calyx 34 mm long,
teeth 1-2 times the length of the
tube; leaflets 1-3.5 X 1-2 cm; stip-
ules narrowly obovate to lanceolate,
not leaflike ......... 5. T hybridum
1. Trifolium arvense L., Sp. Pl. 2: 769. 1753.
Rabbit-foot clover. (Figure 1)
Annual, upright, 5-40 cm tall. Stems often
much-branched, with short appressed to
spreading hairs. Leaves petiolate below to
nearly sessile above, longest petioles to 15
mm, shorter than the leaflets. Stipules ovate
to oblong, tips long attenuate, longer than the
4 Journal of the Kentucky Academy of Science 62(1)
Trifolium arvense L.
Figure 1. Documented county-dis-
tribution in Kentucky; plant (from Besette and Chapman
1992). Bar = 10 mm.
associated petioles. Leaflets 5-20 x 2-4 mm,
sessile or nearly so, linear to narrowly lance-
olate, base cuneate, apex acute to mucronate
and slightly serrate. Inflorescence 8-30 X 8—
10 mm, racemose, densely ovoid or cylindrical,
on peduncles 5—30 mm, or nearly sessile: flow-
ers 10-150, sessile. Calyx long- hairy, often sil-
very to pinkish or purplish, none 1.5-2 mm,
teeth subulate, nearly equal, 2.5-5 mm, plu-
mose. Corolla white to pinkish, slightly shorter
than the calyx lobes, 4 mm, the ste indard nar-
row, oblong, obtuse. Fruit ovoid, 1.3°> mm.
Seed 1, pi ale yellow, 0.9-1.3 mm. 2n = 14, 16,
28. Flowering in Kentucky in June—July, fruit-
ing August-September.
Native to Europe, northern Africa, and
western Asia, rabbit-foot clover is naturalized
in many areas of the world and throughout
much of North America. Zohary and Heller
(1984) recognized two varieties, which differ
somewhat in habit and pubescence density.
This species was first reported for Kentuc
by M’Murtrie (1819). The earliest Kentucky
eae I saw was from 1835, Fayette Coun-
(Short s.n., CINC, KY).
” Trifolium arvense is sometimes cultivated as
a winter annual (Henson and Hollowell 1960).
It is adapted to infertile, dry, often sandy soil
such as that found on roadsides, where is
makes an attractive, silvery-pink display when
in flower, and rose to buff when in fruit.
This species is sometimes also called hare’s
foot (M’Murtrie 1819), stone clover, old-field
clover, and pussies (Delorit and Gunn 1986;
Small 1933).
2. Trifolium aureum Pollich, Hist. Pl. Palat.
2: 344. 1777. Hop clover. (Figure 2)
(Tf. agrarium L., a confused name [Dandy
1958])
Annual or biennial, upright, 20-60 cm tall.
Stems often much-branched, with short ap-
pressed hairs. Leaves petiolate below to short-
petiolate above, longest petioles to 12 mm,
shorter than the leaflets. Stipules oblong-lan-
ceolate, tips narrowly long-triangular, as long
as or longer than the associated petioles, ad-
nate to the petiole for half their length or
more. Leaflets 15-25 < 6-8 mm, sessile or
essentially so, oblanceolate to one or ellip-
tic, base cuneate, apex obtuse to emarginate
and mucronate, serrate in the upper half. In-
florescence 10-25 X 12-14 mm, racemose,
densely ovoid or cylindrical, with a flat top in
age, on peduncles 10-50 mm; flowers 10—
40(80). short-pedicellate. Calyx glabrous, tube
1 mm, teeth narrowly triangular to subulate,
lower teeth 2-3 times the length of the upper,
1.2-1.5 mm. Corolla bright yellow, turning
brown with age, 5-S mm, the aaaneed broadly
obovate, obtuse-emar ginate, strongly parallel-
veined, especially in age. Fruit oblong, 3-3.5
mm, stalked. Seed 1, pale yellow green to yel-
low brown, 1—-1.2 mm. 2n = 14, 16. Flowering
in Kentucky in June-July, fruiting August—
September.
Native to Europe, hop clover is introduced
in eastern and northern North America;
The genus Trifolium (Fabaceae) in Kentucky—Vincent 5
George Washington is known to have ordered
seed of this species from Europe in 1786 (Pie-
ters 1920). Zohary and Heller (1984) recog-
nized two subspecies, which differ mainly in
the leaf apices and style position. The earliest
Kentucky collection I saw was from 1903,
Boone County (Davis s.n., kes).
Trifolium aureum has also been called large
hop clover, yellow clover, and palmate hop-
clover (Gillett and Cochrane 1973; Gleason
and Cronquist 1991; Knight 1985b). It is
sometimes cultivated (Knight 1985b).
3. Trifolium campestre Schreb. in Sturm,
Deutsch. Fl. Abt. 1, Band 4, Heft 16, t. 253.
1804. Low hop clover. (Figure 3)
(T. procumbens L., a confused name [Dan-
dy 1958])
Annual, upright to ascending (rarely pros-
trate), 5-40 cm tall. Stems often much-
branched, with short appressed hairs to nearly
glabrous. Leaves pinnate, long-petiolate below
to short-petiolate above, longest petioles to 1.5
times as long as the leaflets. Stipules ovate,
tips acute to somewhat attenuate, shorter than
the associated petioles. Leaflets 4-16 x 4-8
mm, oblong-obovate, base cuneate, apex trun-
cate to emarginate, slightly serrate in the up-
per half, the terminal leaflet on a 1-3 mm long
stalk, lateral leaflets nearly sessile. Inflores-
cence 7-15 X 7-10 mm, racemose, densely
globose to ovoid or cylindrical, on peduncles
as long as or shorter than subtending leaves;
flowers (10)20—40(50), short-pedicellate. Calyx
glabrous to slightly pubescent, tube 0.5-1 mm,
teeth narrowly triangular to subtlate, lower
teeth 2-3 times the length of the upper, 0.6—
1.3 mm, each tooth often tipped with 1-2 stiff
hairs. Corolla pale to bright yellow, 3.5-6 mm,
the standard obovate, with a slightly toothed
margin, emarginate, more or less enveloping
the wing and keel petals, strongly parallel-
veined, especially in age. Fruit oblong, stalked,
2-2.5 mm. Seed 1, shiny yellow, 1-1.5 mm. 2n
= 14. Flowering in Kentucky in April-June,
fruiting June—August.
Native to Europe and widely introduced
elsewhere, Trifoliwm campestre is widely dis-
tributed in North America, often being found
along roadsides, in lawns, and in other dis-
turbed places. Haragan (1991) considers this
species a weed in Kentucky. The earliest Ken-
tucky collection I saw was from 1882, Jessa-
Trifolium aureum Pollich. Documented coun-
Figure 2.
ty-distribution in Kentucky; plant (from Cost 1901 [right
figure] and Hegi 1923 [left figures]). Bar = 20 mm (whole
plant), 10 mm (branch), 2 mm (flower).
mine County (Peter s.n., KY). This species is
also called hop clover, pinnate hop clover, and
small hop clover (Gillett 1985; Gleason and
Cronquist 1991; Knight 1985b).
Low hop clover and especially least hop clo-
ver (the next species) are often confused with
Medicago lupulina L. (black medic), a com-
monly encountered annual or biennial, pros-
trate to ascending species. It differs from
these clovers by its usually obviously toothed
stipules, deciduous corolla, and reniform,
shiny black fruits.
A. Trifolium dubium Sibth., Fl. Oxon. 231.
1794. Least hop clover. (Figure 4)
Annual, upright, 5-40 cm tall. Stems simple
or branched, glabrous to slightly hairy. Leaves
6 Journal of the Kentucky Academy of Science 62(1)
Documented
Schreb.
county-distribution in Kentucky; plant (from Cost 1901
and Hegi 1923 [lower right and left
figures}). Bar = 15 mm (whole plant),
2 mm
Figure 3. Trifolium campestre
[upper right figure
10 mm (branch),
flower).
pinnate, petiolate below to nearly sessile
above, longest petioles to 15 mm, mostly
shorter than the leaflets. Stipules ovate, tips
acute, slightly adnate to and shorter than the
associated petioles, 3-5 mm. Leaflets 5-15
4-7 mm, terminal stalked, lateral nearly ses-
sile, obovate, base cuneate, apex rounded to
slightly emarginate and slightly serrate. Inflo-
rescence 5-10 X 6—S mm, racemose, loosely
ovoid to obovoid, on peduncles much longer
than associated leaves; flowers 3-20, pedicels
short, reflexing dramatically with age. Calyx
rane. 0.5-0.8 mm, teeth subulate,
lower about twice as long as upper. Corolla
pale yellow, 3-4 mm, the standard narrow, ob-
long, obtuse. Fruit ovoid, nearly sessile, 1.5-2
mm. Seed 1 (rarely 2), shiny tan to dark
glabrous,
Figure 4. Trifolium dubium Sibth. Documented county-
distribution in Kentucky; plant (from Cost 1901 [upper
figures] and Hegi 1923 figure]). Bar = 20 mm
(whole plant), LO mm (branch), 4 mm (flower).
[lower
brown, 1-1.5 mm. 2n = 16; 28. Flowering in
Kentucky in May—June, fruiting July-August.
Least hop clover is native to . Europe and is
now introduced throughout the world. It is
widely distributed in North America. It is
sometimes cultivated as a pasture plant (De-
lorit and Gunn 1986). Trifolium dubium was
reported as new to Kentucky by McFarland
(1942). Mohlenbrock et al. (1966) again re-
ine the species, but I could not locate the
specimen cited in that paper. The species was
also reported for Henry County in an unpub-
lished thesis (Gentry 1963), but again the
voucher could not be located. Medley (1993)
accepted only reports from Lyon, Trigg, and
The genus Trifolium (Fabaceae) in Kentucky—Vincent
Rockcastle counties. The earliest Kentucky
collection I saw was from 1855, without local-
ity (C.W. Short s.n., PH).
Trifolium dubium is also called little hop
clover (Gillett and Cochrane 1973; Gleason
and Cronquist 1991), small hop clover (De-
lorit and Gunn 1986; Isely 1998) and sham-
rock (Small 1933). It is often confused with T.
campestre, but can be distinguished from it by
the smaller inflorescences with fewer flowers:
its standard is not striate or only faintly so,
whereas that of T. campestre is strongly striate.
It is also commonly confused with Medicago
lupulina L. (black medic), but can be distin-
guished as described in the entry for T. cam-
pestre; more records for little hop clover iden-
tified as black medic may lurk in herbaria. Tri-
folium dubium is thought by some to be the
“shamrock” of Irish folklore, but others claim
that the shamrock may be one of several spe-
cies of Trifolium, Medicago, or Oxalis (Colgan
1896; Everett 1971; Nelson 1991).
5. Trifolium hybridum L., Sp. Pl. 2: 766.
1753. Alsike clover. (Figure 5)
Perennial, upright to ascending, 15-60(80)
cm tall. Stems often much-branched, nearly
glabrous, often somewhat fleshy. Leaves peti-
olate, longest petioles to 80 (sometimes even
100) mm, longer than the leaflets, gradually
reduced upward. Stipules obovate to lanceo-
late, tips long attenuate, 10-30 cm, adnate to
petioles for about one-third their length. Leaf-
lets 10-35 X 10-20 mm, sessile or nearly so,
ovate to elliptical or fermi! base cuneate,
apex rounded to slightly emar ginate, serrate.
Inflorescence 10-25 mm roads globose,
short-racemose to nearly onbelllare. on pe-
duncles 20-80 mm; flowers 20-80; pedicels 1—
5 mm, reflexing ih age. Calyx glabrous ex-
cept in the U-shaped sinuses, tube 1-2 mm,
teeth subulate, nearly equal, as long as or lon-
ger than the tube. Corolla white and pink, 6-
11 mm, the standard ovate-oblong, obtuse,
sometimes emarginate. Fruit oblong, 3-4 mm.
Seeds 2-4, mottled yellow brown, red brown,
to nearly black, 1-1.3 mm. 2n = 16. Flowering
in Kentucky in May-July, fruiting July-Sep-
tember.
Alsike clover is native to Europe, probably
in the Mediterranean region. It is introduced
throughout temperate regions worldwide, and
is often cultivated. The species, also called Al-
Figure 5. Trifolium hybridum L. Documented county-
distribution in Kentucky; plant (from Hermann 1966). Bar
= 20 mm (whole plant), 5 mm (flower), 1.5 mm (calyx).
satian clover and Swedish clover (Delorit and
Gunn 1986; Small 1933), was apparently first
cultivated in Sweden, and first cultivated in
England about 1832 (Taylor 1975). It was first
brought to the United States about 1839 (Tay-
lor 1975). The earliest Kentucky collection I
saw was from 1895, Rockcastle ‘County (n.C.,
CINC).
Trifolium hybridum may cause dermatitis in
sensitive humans (Hardin and Arena 1974).
Alsike clover is said to cause photosensitivity
and biliary fibrosis in horses (Fisher 1995),
though the connection between these diseases
and the clover is not conclusive (Nation 1989).
Trifolium nigrescens Viv. (ball clover, a
8 Journal of the Kentucky Academy of Science 62(1)
Medite:ranean species) is found with increas-
ing frequency in southeastern United States
(Isely 1990, 1998), and has been documented
from: iumerous sites in Tennessee. It is pos-
sible that this species will be encountered in
the southern tier of Kentucky counties, espe-
cially since it can be cultivated in the state
Taylor and Sigafus 1984). Ball clover is an an-
nual, prostrate to ascending, glabrous to gla-
brescent species, which can be distinguished
from Alsike clover by its habit, as well as by
\-shaped sinuses be ‘tween the calyx lobes ( U-
sh aped in T: hybridum), white to cream or yel-
low-white (rarely pale pinkish) corolla (gen-
erally deep pink in T. hybridum), and stipule s
with sharply recurved, black to dark maroon,
subulate tips (straight, green tips in T. hybri-
dum).
6. Trifolium incarnatum L., Sp. Pl. 2: 769.
1753. Crimson clover. (Figure 6)
Annual, upright, 20-90 cm tall, hairy
throughout. Stems simple to sparingly
branched below. Leaves long-petiolate below
to nearly sessile above, longest petioles 4-5
times the le ngth of the leafle tS. Stipules broad-
ly ovate to oblong, sheathing the stem at the
base, white to pale | green with dark green to
red purple veins Below: tips toothed and
rimmed with dark red purple or green. Leaf-
lets 10-30(40) X 10-20(30) mm, sessile or
nearly so, broadly ovate-obovate to orbicular,
base broadly cuneate, apex obtuse to emargin-
ate. Inflorescence 20-60 X 10-20 mm, spi-
cate, densely cylindrical, peduncles 10-60
mm; flowers many, sessile or nearly so. Calyx
long-hairy, ae 3-5 mm, teeth subulate, near-
ly equal, 1 2 times as long as the tube. Corolla
crimson, te white or pink, longer than the
calyx lobes, 10-17 mm, the standard linear-
oblong to elliptical, acute. Fruit sessile, ob-
long, 3-4 mm. Seed 1, buff to brown, 1.9-2.3
mm. 2n = 14. Flowering in Kentucky in
April-May, fruiting June-July.
Crimson clover (also called Italian clover
(Small 1933] and many other common names
[Knight 1985a; Nourse 1894]), is native to
southern and western Europe and widely nat-
uralized in other areas. The species has been
cultivated since the 1700s in Europe and was
introduced into the United States in 1818
(Knight 1985a). Crimson clover is used exten-
sively as a ground cover in crop rotations, for
Trifolium incarnatum L. Documented county-
distribution in Kentucky; plant (from Hegi 1923). Bar =
40 mm (whole plant), 10 mm (flower), 5 mm (calyx).
Figure 6.
green manure, and as a nitrogen-fixing plant
in fields (Taylor and Sigafus 1984); it is also
used an annual hay crop (Nourse 1894). It is
occasionally cultivated in Kentucky (Garman
1902: Taylor 1986: Taylor and Sigafus 1984).
The “Males! Kentucky collection I saw was
from 1934, Jefferson County (Bishop & Bish-
op s.n., DHL).
7. Trifolium pratense L., Sp. Pl. 2: 768. 1753.
Red clover. (Figure 7)
Perennial, ascending to upright, 20-60(100)
em tall. Stems much-branched, with ap-
pressed to spreading hairs or glabrous. Leaves
long-petiolate below to nearly sessile above,
longest petioles 3-4 times the length of the
leaflets. Stipules ovate to lanceolate, 10-30
The genus Trifolium (Fabaceae) in Kentucky—Vincent 9
Figure 7. Trifolium pratense L. Documented county-dis-
tribution in Kentucky; plant (from Besette and Chapman
1992). Bar = 20 mm.
mm, adnate to the petioles for most of their
length, the lower portion pale with dark green
to red veins tips long mucronate. Leaflets 10-
30(50) < 7-15(25) mm, sessile or nearly so,
ovate to elliptic or obovate, base broadly cu-
neate, apex rounded, rarely slightly emargin-
ate, essentially entire. Inflorescence single or
in pairs, 10-30 < 10-30 mm, head-like, glo-
bose, dense, sessile or on peduncles to about
4 mm, subtended by a pair of bract-like leaves;
flowers 40-150, sessile. Calyx hairy, tube 2.5—
4 mm, teeth subulate, lowest about as long as
the tube, others nearly equal and much short-
er than the lowest. Corolla red purple to white
or pinkish, longer than the calyx lobes, 11-18
mm, the standard oblong-oblanceolate, emar-
inate. Fruit ovoid-oblong, 2-3 mm. Seed
1(2), tan to brown, 1.5-2 mm. 2n = 14, 28,
56. Flowering in Kentucky in April—October,
fruiting June—November.
Trifolium pratense is morphologically very
variable, and many binomials have been
coined for the various forms; Zohary and Hell-
er (1984) recognized six varieties of the spe-
cies. Red clover (also called purple clover
[Small 1933]) is the grown in more areas of
the world than any other species of Trifolium
(Taylor 1975). It is native to southeastern Eu-
rope and Asia Minor (Smith et al. 1985). Tri-
folium pratense has been in cultivation since
the 3rd and 4th centuries, probably beginning
in Spain, from where it spread to Holland and
Lombardy, then to Germany. This species was
introduced into England about 1645, from
where it was brought to the New World by
1663 (Taylor and Quesenberry 1996). It is a
very important forage crop but may also cause
bloating in animals overeating its young
growth; a diet high in red clover may cause
infertility in sheep (Taylor and Quesenberry
1996).
Red clover has been cultivated in Kentucky
since at least 1803 (Fergus 1931; Taylor et al.
1997a), and is probably naturalized in every
county; Fergus (1931) indicated that red clo-
ver was cultivated in every county in Ken-
tucky. M’Murtrie (1819) reported red clover
in the Louisville area as early as 1819. The
earliest Kentucky collection I saw was from
1892, Fayette County (Terrill s.n., kes). Tri-
folium pratense has been described as a “ubi-
quitist,” which may occur in practically any
plant community (Merkenschlager 1934). Red
clover has been used in revegetation of strip
mine coal spoil fields in western Kentucky
(Powell et al. 1980). It is the state flower of
Vermont.
Red clover may be used for tea or as an
ingredient in herbal cough syrup (Coon 1980;
Gibbons 1962), to flavor vinegar (Coon 1980),
and as a salve to treat eye and skin diseases
(RDA 1984). There are even claims that red
clover can be used in cancer treatments (Duke
1985; Ritchason 1995). The young growth can
be cooked as a vegetable (Coon 1980). Dried
flower heads have been powdered and used in
breads during times of famine (Millspaugh
1974).
Trifolium medium (zigzag clover) is a similar
perennial species sometimes cultivated in
Kentucky (see Excluded Species). It differs
10 Journal of the Kentucky
Figure S.
tribution in Kentucky; plant (from Isely 1951).
Trifolium reflecum L. Documented county-dis-
Bar = 20
mm (whole plant), 3 mm (flower).
from T. pratense by its peduncled inflores-
cences, narrowly elliptical leaflets, and rhizo-
matous nature. Trifolium hirtum (rose clover),
an annual species resembling red clover, has
been reported from nearby states and is oc-
casionally cultivated in Ke ntucky (see Exclud-
ed Species).
8. Trifolium reflexum L., Sp. Pl. 2: 766. 1753.
Buffalo clover. (Figure 8)
Annual to biennial, ascending-upright, 20-
50 cm tall. Stems simple to branched from the
base, densely pubescent to glabrous. Leaves
petiolate, gradually reduced “upward, longest
petioles 3-4 times the le ngths of the eaters
Stipules broadly ovate, leaflike, tips long acu-
minate, entire to serrate. Leaflets 10—30(45)
6—20(25) mm, sessile or nearly so, ovate to ob-
ovate, base cuneate, apex acute broadly
Academy of Science 62(1)
rounded, serrate. Inflorescence 20—35(40) mm
wide, umbellate, nearly spherical in flower, on
peduncle s 20-60(S0) mm; flowers 10-40; ped-
icels 4S mm, reflexing dramatically and elon-
gating to 7-12(15) mm in fruit. Calyx hairy to
glabrous, tube 1-1.5 mm, teeth linear, nearly
equal, 3-7 mm, with broad, U-shaped sinuses
between. Corolla deep pink to white, longer
than the calyx lobes, 8-14 mm, the standard
oblong to e lliptic, obtuse, often slightly emar-
ginate. Fruit ote to oblong, 3-5 mm, slightly
stalked. Seeds (1)2-4, pale hast 1-1.5 mm.
2n = 16. Flowering in Ke sntucky in May, fruit-
ing June.
Buffalo clover is native to eastern North
America from Virginia and the Carolinas south
into Florida, west to central Texas, north to
eastern Kansas, Nebraska, and Iowa, and east
to Ohio; there is also an old record from east-
ern Pennsylvania. The earliest Kentucky col-
lection I saw was from 1835, Fayette County
(Short s.n., GH); the most recent collection
was from 1990, Trigg County (Chester et al.
90-210, APSC). This species is becoming very
rare in Kentucky (Taylor and Campbell 1989)
and is listed as endangered in the state
(KSNPC 1996): four extant “occurrences” are
recorded by the Kentucky State Nature Pre-
serves Commission (D.L. White, KSNPC,
pers. comm., 19 Jan 2000).
According to Taylor et al. (1994), buffalo
clover is autogamously self pollinated. Some
authors have recognized two varieties, based
on pubescence differents but this character
is variable and probably clinal in nature, with
the more glabrous forms in the northeastern
part of the range of the species. Glabrous and
pubescent forms may grow intermingled in
some mid-south populations, with the most
densely pubescent populations occurring in
the deep south and the western portion of the
range. The species was rediscovered in Ohio
in 1990 at a site that had burned the previous
fall (Vincent 1991), but there have been no
further fires, and it has not reappeared there
since. Populations of this species often reap-
pear in sites after a burn, heavy logging, or
some equally severe disturbance. (pers. obs.).
Trifolium virginicum Small ex Small & Vail
(Kate’s Micha ein clover) is a similar species
found on exposed shale barrens from south-
western Pennsylvania south through West Vir-
ginia to the Shenandoah alley of Virginia
The genus Trifolium (Fabaceae) in Kentucky—Vincent 1]
Figure 9. Trifolium repens L. Documented county-dis-
tribution in Kentucky; plant (from Besette and Chapman
1992). Bar = 20 mm (whole plant), 15 mm (inflores-
cence).
(Linscott 1994). It is a perennial species, with
a rosette of leaves with narrowly elliptical leaf
lets: the corolla is white. If suitable habitat
were found in eastern Kentucky, this species
might be found there.
9. Trifolium repens L., Sp. Pl. 2: 767. 1753.
White clover. (Figure 9)
Perennial, stoloniferous to rhizomatous,
rooting at the nodes, 10-30 cm tall. Stems
much-branched, glabrous to sparsely hairy.
Leaves petiolate, petioles 10-200 mm. Stip-
ules thin and membranous, whitish to brown-
ish, often with darker reddish to greenish
veins, ovate-lanceolate, fused into a tube, tips
short-attenuate, 8-15 mm. Leaflets 6-30
10-25 mm, sessile or nearly so, broadly elliptic
to ovate, base broadly cuneate, apex obtuse to
emarginate or obcordate, serrate. Inflores-
cence 15-35 mm broad, umbellate to short-
racemose, nearly globose, on peduncles as
long as or longer than the associated leaves,
arising from leaf axils on the stolons; flowers
20-50(100); pedicels reflexing dramatically
with age. Calyx glabrous, often whitish with a
purplish to green apex, tube 1.8—3 mm, teeth
triangular-lanceolate, unequal, upper shorter
than the tube, lower about as long as tube,
sinus sharply V-shaped. Corolla white to pink-
ish, 7-12 mm, the standard elliptic-obovate,
obtuse. Fruit linear-oblong, 3-5 mm. Seeds 3-
4, yellowish tan to brown, 0.9-1.5 mm. 2n =
16, 28, 32, 48, 64. Flowering in Kentucky in
March—November, fruiting June—November.
White clover (also called Dutch clover and
Ladino clover) may very well be the most im-
portant temperate pasture plant (Baker and
Williams 1987). It was introduced so early and
was so widely grown in North America that it
was known to Native Americans as “White
man’s foot grass” (Strickland 1801); its culti-
vation may have begun in the early 1700s, and
it was widespread by the middle of that cen-
tury (Isely 1998). Piper (1924) considered
white clover “the most important perennial
pasture plant in North America.” The species
is widely grown in Kentucky (Rice et al. 1982)
and was the earliest clover species cultivated
in the state (Carrier and Bort 1916).
M’Murtrie (1819) reported this species from
the Louisville area. The earliest known Ken-
tucky collection I saw was from 1890, Fayette
County (Garman s.n., kes). The species is un-
doubtedly to be found in every Kentucky
county.
Trifolium repens is extremely morphologi-
cally plastic, and varies greatly in size of both
leaves and flowers depending upon environ-
mental conditions (Gillett and Cochrane
1973). Zohary and Heller (1984) recognized
nine intergrading varieties. Most North Amer-
ican specimens appear to be T. repens var. re-
pens. A recent monograph on the species COvV-
ers in great detail many aspects of its taxono-
my, morphology, and cultivation (Baker and
Williams 1987).
12
White clover may have some medicinal
uses, although human ingestion of powdered
fresh heads resulted in “a sensation of
fullness and congestion of the salivary glands
with pain, and mump-like pain ... fol-
lowed by copious flow of saliva” (Millspaugh
1974).
\ similar species is T. calcaricum Collins &
Wieboldt, which differs from white clover in
its terminal inflorescences. It is native to the
cedar glades of central Tennessee and south-
western Virginia (Collins and Wieboldt 1992).
If similar cedar glade habitat exists in south-
eastern Rentals it is possible that this spe-
cies could be found in the state: it is found in
Lee County, Virginia, within 10 miles of the
Kentuc ky state line.
10. Trifolium resupinatum L., Sp. Pl. 2: 771
1753. Persian clover. (Figure 10)
Annual, procumbent to ascending or up-
right, 10-60 cm tall. Stems often much-
branched, glabrous or nearly so. Leaves peti-
olate Belon to nearly sessile above, longest
petioles to 4-5 times the length of the lee ths
Stipules lanceolate to lanceolate-ov ate, tubular
at the base, tips long attenuate, shorter than
the associated petioles. Leaflets 5-20(30) x 2—
4 mm, sessile or nearly so, obovate, elliptic to
lanceolate, or rhombic, serrate, base cuneate,
apex rounded to acute. Inflorescence 8—15
mm broad, capitate, densely hemispherical, on
peduncles 20-50 mm; flowers 6-20, short-pet-
iolate to sessile. Calyx glabrous except for a
dorsal band of hairs, w hitish to pale green with
a dark basal band, tube 1.5—2 mm, teeth su-
bulate, unequal, shorter than the tube, often
dark green; calyx becoming inflated and en-
closing the fruit at maturity, the veins obvi-
ously reticulating. Corolla resupinate, lavender
to pink or rarely white, 4-9 mm, the standard
oblong, emarginate. Fruiting head globose,
looking star-like. Fruit ovoid- lenticular, 1.7-
2.3 mm. Seed 1, yellow to tan or purple
brown, 1.2-2 mm. 2n = 14, 16, 32. Flowering
in Kentucky in May-June, fruiting June-July.
The resupinate (inverted, with ine standard
below and the keel above) corolla and inflated
fruiting calyx makes T. resupinatum easy to
distinguish ‘from other clovers. The presence
of Persian clover in Kentucky was first report-
ed by McFarland (1942), whose report was ac-
ce pted by Browne and Athey ( 1992) and Med-
2 Journal of the Kentucky Academy of Science 62(1)
Trifolium resupinatum L.
Figure 10. Trifolium resupinatum L. Documented coun-
ty-distribution in Kentucky; plant (from Hegi 1923). Bar
= 20 mm (whole plant), 3 mm (flower and fruiting calyx).
ley (1993). It may be cultivated in the state as
a winter annual (Taylor and Sigafus 1984). I
located only one Kentucky collection, from
1915, Metcalfe County (Salmon s.n., kes). A
report by Browne and Athey (1992) for the
Shawnee Hills was rejected by Medley (1993),
and I was unable to locate a specimen to verify
the report. Widespread in much of the south-
eastern United States (Isely 1990), this species
was recently documented from Ohio (Vincent
and Cusick 1998). It is reported from “scat-
tered stations” in northeastern U.S. by Glea-
son and Cronquist (1991).
Ll. Trifolium stoloniferum Muhl. ex A.
Eaton, Man. Bot. 468. 1818. Running buffalo
clover. (Figure 11)
Perennial, stoloniferous, upright flowering
branches 10—40 cm tall. Prostrate stems often
The genus Trifolium (Fabaceae) in Kentucky—Vincent 13
Trifolium stoloniferum
Muhl. ex A.Eaton
Figure 11.
little branched, glabrous or nearly so, rooting
at the nodes, forming extensive clones. Leaves
from stolons long-petiolate, those on the up-
right flowering stems in a pair, petioles as long
as the leaflets or shorter. Stipules of stolons
broadly lanceolate, membranous, tips attenu-
ate, shorter than the associated petioles; those
of the upright stems leaf-like, ovate-oblong,
broadly triangular to attenuate, slightly to
much-serrate. Leaflets 10-40 < 8-35 mm,
serrate, on petiolules about 1 mm, obovate to
obcordate, base broadly cuneate, apex round-
ed to emarginate. Inflorescence 15-30 mm
wide, umbellate, spherical, on peduncles 10-
30 mm; flowers 25-45; pedicels 2-8 mm, re-
flexing dramatically in age. Calyx glabrous or
nearly so, tube 1.5-2.5 mm, teeth subulate,
nearly equal, about twice the length of the
tube. Corolla white, sometimes pinkish with
age, 8-14 mm, the standard obovate to ob-
Trifolium stoloniferum Muhl. ex A. Eaton. Documented county-distribution in Kentucky; plant (drawn by
Ethel Hickey 1995, used with permission). Bar = 20 mm.
long, rounded to emarginate. Fruit oblong,
2.5-3 mm. Seeds 1-2, yellow to brown, 1.3-2
mm. 2n = 16, 32. Flowering in Kentucky in
April-May, fruiting May-June.
In spite of the use of the citation “Muhl.,
Cat. Pl. Amer. Sept. 67. 1813.” for this name
(Browne and Athey 1992; Medley 1993; Zo-
hary and Heller 1984), the authorship should
be given as “Muhl. ex A. Eaton” since Muhl-
enberg’s (1813) publication of the name was a
“nomen nudum” as stated by Merrill and Hu
(1949) and Brooks (1983).
Running buffalo clover once ranged widely
over middle east-central North America from
present-day West Virginia west to Kansas, and
from Arkansas north to north-central Ohio
(Brooks 1983). Its predominant range was
montane West Virginia and the Ohio River
drainage in Ohio and south to central Ken-
tucky. It was once found in great stands in
14 Journal of the Kentucky
Kentuck: (Campbell et al. 1988) and Ohio
(Cusick 1989). This species, once thought ex-
tinct as rediscovered in 1983 by B: urtgis
(1985). and was listed in 1987 by the US Fish
and \Vildlife Service as an endangered species
\nonymous 1987) under the federal Endan-
gered Species Act. It was thought to be ve ry
rare in Kentucky (Taylor and C ‘ampbell 1989),
and is listed as a threatened species in the
state (KSNPC 1996): 69 extant “occurrences”
are recorded in the state by the KSNPC (D.L.
White, KNSPC, pers. comm. 19 Jan 2000).
The earliest Kentucky collection I saw was
from 1834, Fayette County (Peter s.n., MICH,
NY): the most recent is from 1995, Madison
County (Vincent et al. 6959, MU).
Taylor et al. (1994) stated that running buf-
falo clover is an outcrossing species that sets
fewer seeds if selfing, Bal that seed set in
selfed plants was still high enough to maintain
the species in the wild. They At: suggested
that habitat loss and competition may comely
ute more to the decline of the species than
inbreeding. Hickey et al. (1991) found that ge-
netic diversity was low among many popula-
tions of the species, based on “alllorsc me band-
ing patterns, and that many populations might
actually represent clones. Crawford et zal
(1998), however, in a study using RAPDs,
found that most populations were not single
clones, and that even the smallest populations
contained unique § genetic information.
Running apelin clover is sometimes con-
fused aie T. repens, from which it differs by
the bract-like pair of leaves below the inflo-
rescence on the upright stems, and by the
overall larger size of the former. Another sim-
ilar species is T. calcaricum, which is discussed
under the treatment of T. repens.
EXCLUDED SPECIES
Trifolium alexandrinum L. Berseem clover
This species was reported from cultivation
by Garman (1902) and more recently by Tay-
lor and Sigafus (1984). Its presence in Ken-
tucky outside of cultivation was rejected by
There is a Fayette County
Medle 2y
specimen
(1993),
(Garman s.n.,
kes),
but it is from
cultivation. I saw no specimen of this clover
from other than cultivation.
Trifolium ambiguum L. Kura clover
Kura clover
and is a very hardy rhizomatous perennial
can be cultivated in Kentucky
Academy of Science 62(1)
(Taylor 199la; Taylor et al. 1997b). Isely
(1998) and Kartesz (1999) reported T. ambig-
uum as an escape in Ohio, but the reports
were based on cultivated material; it is not yet
documented that the species will escape in
North America. All Kentucky collections I ex-
amined were of cultivated material.
Trifolium hirtum L. Rose clover
Rose clover was reported for Kentucky by
Isely (1990, 1998) and was provisionally ac-
cepte 4 by Medley (1993). Kartesz (1999) ac-
cepted the species as part of the state flora.
The only Kentucky specimens identified by Is-
ely as T. hirtum were at NCU. Of those, all
were T. pratense except one, a cultivated spec-
imen of rose clover from Jefferson County
(Gunn J150, NCU). If this species becomes
widely cultivated, and since it is possible to
grow it in Kentucky (Taylor and Sigafus 1984),
it could very well become established in the
state.
Trifolium medium L. Zigzag clover
~ ©
Zigzag clover was reported for Kentucky by
Garman (1902) and Linney (1880). I saw no
non-cultivated Kentucky specimens of this
species, although it is known to be cultivated
in the state (Tay lor 1991b). Medley (1993) re-
jected the occurrence of this species in Ken-
tucky. Gleason and Cronquist (1991) reported
that T. medium occasionally escapes from cul-
tivation in northeastern North America. I have
seen specimens from escaped populations in
North Carolina, Massachusetts, Maine, and
eastern Canada.
Other clover species which are known only
from cultivation in Kentucky include T. vesi-
culosum Savi (arrowleaf clover) and T. subter-
ranean L. (sub clover) (Taylor and Sigafus
1984). In addition, Dr. Norman Taylor has cul-
tivated many other species in greenhouses and
field plots in Lexington.
ACKNOWLEDGMENTS
I thank the curators of the herbaria for al-
lowing me access to specimens for this study.
I am very grateful to Dr. Ralph Jones, Dr.
Norman daylon Dr. John W. Thieret, and Dr.
Ralph Thompson for sharing information
about Kentucky clovers with me.
The genus Trifoliwm (Fabaceae) in Kentucky—Vincent 15
LITERATURE CITED
Anonymous. 1987. Endangered and threatened wildlife
and plants: determination of endangered status for Tri-
folium stoloniferum (running buffalo clover). Fed. Reg-
ister 52(108):21478—21480.
Atwood, S. S. 1938. A “one-leaved” white clover. J. Hered.
29:2.39-240.
Baker, M., and W. M. Williams. 1987. White Clover. CAB
Intemational, Wallingford, Oxon, U.K.
Bartgis, R. L. 1985. Rediscovery of Trifolium stoloniferum
Muhl. ex A. Eaton. Rhodora 87:425—429.
Bessette, A. E., and W. K. Chapman. 1992. Plants and
Flowers: 1,761 Illustrations for Artists and Designers.
Dover, New York, NY.
Braun, E. L. 1943. An annotated catalog of spermato-
phytes of Kentucky. J.S. Swift, Cincinnati, OH.
Brooks, R. E. 1983. Trifolium stoloniferum, running buf-
falo clover: description, distribution, and current status.
Rhodora 85:343-354.
Browne, E. T., and R. Athey. 1992. Vascular plants of Ken-
tucky: an annotated checklist. Univ. Press of Kentucky,
Lexington, KY.
Campbell, J. J. N., M. Evans, M. E. Medley, and N. L.
Taylor. 1988. Buffalo clovers in Kentucky (Trifolium sto-
loniferum and T. reflexum): historical records, presettle-
ment environment, rediscovery, endangered status, cul-
tivation and chromosome number. Rhodora 90:399-—
A418.
Carrier, L., and K. S. Bort. 1916. The history of Kentucky
bluegrass and white clover in the United States. Agron.
]. 8:256-266.
Colgan, N. 1896. The shamrock in literature: a critical
chronology. J. Roy. Soc. Antiquaries Ireland 26:211-
226, 349-361.
Collins, J. L., and T. F. Wieboldt. 1992. Trifolium calcar-
icum (Fabaceae), a new clover from limestone barrens
of eastern United States. Castanea 57:282-286.
Coon, N. 1980. Using wild and wayside plants. Dover,
New York, NY. Republication of a work first published
in 1957.
Corkill, L. 1971. Leaf markings in white clover. J. Hered.
62:307—310.
Cost, H. 1901. Flore descriptive et illustrée de la France.
Vol. 1. Klinckseick, Paris, France.
Crawford, D. J., E. J. Esselman, J. L. Windus, and C. S.
Pabin. 1998. Genetic variation in Running buffalo clo-
ver (Trifolium stoloniferum: Fabaceae) using Random
amplified polymorphic DNA markers (RAPDs). Ann.
Missouri Bot. Gard. 85:81—89.
Cusick, A. W. 1989. Trifolium stoloniferum (Fabaceae) in
Ohio: history, habitats, decline and rediscovery. Sida 13:
467-480.
Dandy, J. E. 1958. List of British vascular plants. British
Museum, London, U.K.
Delorit, R. J., and C. R. Gunn. 1986. Seeds of continental
United States legumes (Fabaceae). Agronomy Publica-
tions, River Falls, MN.
Duke, J. A. 1981. Handbook of legumes of world econom-
ic importance. Plenum Press, New York, NY.
Duke, J. A. 1985. CRC Handbook of medicinal herbs.
CRC Press, Boca Raton, FL.
Evans, G. 1957. The clover tradition in Wales. J. Agric.
Soc. College Wales 38:30-35.
Everett, T. H. 1971. Some facts and fallacies about the
shamrock. Gard. J. 21:24—26.
Fergus, E. N. 1931. Adaptability of red clovers from dif-
ferent regions, to Kentucky. Kentucky Agric. Exp. Sta.
Bull. 318:21 7-246.
Fisher, C. 1995. Horse care: perilous pasture plants. Rural
Heritage 20:44—45.
Ford, J. L., and R. B. Claydon. 1996. Inheritance of mul-
tifoliate leaves in white clover. Spec. Publ. Agron. Soc.
New Zealand. 11:167—170.
Ganders, F. R., A. J. F. Griffiths, and K. Carey. 1980. Nat-
ural selection for spotted leaves: parallel morph ratio
variation in three species of annual plants. Canad. J.
Bot. 58:689-693.
Garman, H. 1902. Kentucky forage plants—the clovers
and their allies. Kentucky Agric. Exp. Sta. Bull. 98:3-
46.
Gentry, J. L. 1963. The vascular plants of Henry County,
Kentucky. Master's thesis. Univ. Kentucky, Lexington,
KY.
Gibbons, E. 1962. Stalking the wild asparagus. McKay,
New York, NY.
Gillett, J. M. 1985. Taxonomy and morphology. Pages 7—
69 in N. L. Taylor (ed). Clover science and technology.
Agron. Monogr. 25.
Gillett, J. M., and T. S. Cochrane. 1973. Preliminary re-
ports on the flora of Wisconsin. No. 63. The genus Tri-
folium—the clovers. Trans. Wisconsin Acad. Sci., Arts,
Lett. 61:59-74.
Gleason, H. A., and A. Cronquist. 1991. Manual of vas-
cular plants of northeastern United States and adjacent
Canada. 2nd ed. New York Botanical Garden, Bronx,
NY.
Haragan, P. D. 1991. Weeds of Kentucky and adjacent
states. Univ. Press of Kentucky, Lexington, KY.
Hardin, J. W., and J. M. Arena. 1974. Human poisoning
from native and cultivated plants. 2nd ed. Duke Univ.
Press, Durham, NC.
Hegi, G. 1923. Illustrierte Flora von Mittel-Europa. Vol.
4(3). A. Pichler Witwe & Sohn, Vienna, Austria.
Henson, P. R., and E. A. Hollowell. 1960. Winter annual
legumes for the south. USDA Farm. Bull. 2146:1-24.
Hermann, F. J. 1966. Notes on western range forbs: Cru-
ciferae through Compositae. USDA Forest Serv. Agric.
Handb. 293.
Hickey, R. J., M. A. Vincent, and S. I. Guttman. 1991.
Genetic variation in running buffalo clover (Trifolium
stoloniferum, Fabaceae). Conservation Biol. 5:309-316.
Holmgren, P. K., N. H. Holmgren, and L. C. Barnett.
1990. Index Herbariorum. Part 1: The Herbaria of the
World. 8th ed. Regnum Veg. 120.
Isely, D. 1951. The Leguminosae of the north-central
16 Journal of the Kentucky Academy of Science 62(1)
United States: I. Loteae and Trifolieae. Lowa State Coll.
J. Sci. 25:439-482.
Isely, 1. 1990. Vascular flora of the southeastern United
States. Vol. 3, part 2. Leguminosae (Fabaceae). Univ.
orth Carolina Press, Chapel Hill, NC.
Isely, D. 1998. Native and naturalized Leguminosae (Fa-
baceae) of the United States (exclusive of Alaska and
Hawaii). Monte L. Bean Life Science Museum, Brigh-
am Young Univ., Provo, UT.
Jaranowski, J. K., and Z. Broda. 1978. Leaf mutants in
diploid red clover (Trifolium pratense L.). Theor. Appl.
Genet. 53:97—103.
Kartesz, J]. T. 1999. A synonymized checklist and atlas with
biological attributes for the vascular flora of the United
States, Canada, and Greenland. Ist ed. In J. T. Kartesz,
and C. A. Meacham. Synthesis of the North American
flora, version 1.0. North Carolina Botanical Garden,
Chapel Hill, NC.
[KSNPC] Kentucky State Nature Preserves Commission.
1996. Rare and extirpated plants and animals of Ken-
tucky. Trans. Kentucky Acad. Sci. 57:69-91.
Knight, W. E. 1985a. Crimson clover. Pages 491-502 in
N. L. Taylor (ed). Clover science and technology.
Agron. Monogr. 25.
Knight, W. E. 1985b. Miscellaneous annual clovers. Pages
547-562 in N. L. Taylor (ed). Clover science and tech-
nology. Agron. Monogr. 25.
Linney, W. M. 1880. Report on the timbers of Boyle and
Mercer counties [Kentucky]. Yeoman Press, Frankfort,
KY.
Linscott, T. M. 1994. Morphological and genetic diversity
of Trifolium virginicum populations using quantitative
and allozyme studies. Master's thesis. Miami Univ., Ox-
ford, OH.
McFarland, F. T. 1942. A catologue of the vascular plants
of Kentucky. Castanea 7:77—108.
M’Murtrie, H. 1819. Sketches of Louisville and its envi-
rons: included, among a great variety of miscellaneous
matter, a Florula Louisvillensis. $. Penn, Louisville, KY.
Medley, M. E. 1993. An annotated catalog of the known
or reported vascular flora of Kentucky. Ph.D. disserta-
tion. Univ. Louisville, Louisville, KY.
Meijer, W. 1992. Herbaceous flora of Kentucky. 2nd ed.
Univ. Kentucky, Lexington, KY.
Menke, A. E., and H. F. Hillenmeyer. 1586, Clover. Ken-
tucky Agric. Exp. Sta. Bull. 6:1-7.
Merkenschlager, F. 1934. Migration and distribution of
red clover in Europe. Herbage Rev. 1934:88—92.
Merrill, E. D., and S.-Y. Hu. 1949. Works and publications
of Henry Muhlenberg, with special attention to unre-
corded or incorrectly recorded binomials. Bartonia 25:
1-66.
Millspaugh, C. F. 1974. American medicinal plants. Do-
ver, New York, NY. Republication of a work first pub-
lished in 1892.
Mohlenbrock, R. H., D. R. Windler, and D. O'Dell. 1966.
New and otherwise interesting plant collection reports
from Kentucky. Castanea 31:296-301.
Muhlenberg, H. 1813. Catalogus plantarum Americae
septentrionalis. W. Hamilton, Lancaster, PA.
Nation, P. N. 1989. Alsike clover poisoning: a review. Can-
ad. Vet. J. 30:410-415,
Nelson, E. C, 1991. Shamrock: botany and history of an
Irish myth. Boethius Press, Aberystwyth, Wales.
Nourse, D, O. 1894. Crimson clover (Trifolium incarna-
tum). Virginia Agric. Mech. Coll., Agric. Exp. Sta. Bull.
44, n.s. 3:113-117.
Pellett, F. C. n.d. Useful honey plants. American Bee
Journal, Hamilton, IL.
Pieters, A. J. 1920. The hop clovers. USDA Office of For-
age Crop Investigations. 2 pp. (mimeo)
Piper, C. V. 1924. Forage plants and their culture. Rev.
ed. Maemillan, New York, NY.
Powell, J. L., R. I. Barnhisel, and G. W. Akin. 1980. Rec-
lamation of surface-mined coal spoils in western Ken-
tucky. Agron. J. 72:597-600.
[RDA] Reader's Digest Association. 1984. Magie and
medicine of plants. Reader's Digest Association, Pleas-
antville, NY.
Rice, H. B., M. Rasnake, N. L. Taylor, and R. E. Sigafus.
1982. Growing white clover in Kentucky. Univ. Ken-
tucky Coop. Exten. Serv. AGR-93.
Ritchason, J. 1995. The little herb encyclopedia, 3rd ed.
Woodland Health Books, Pleasant Grove, UT.
Small, J. K. 1933. Manual of the southeastern flora. Pub-
lished by the author, New York, NY.
Smith, R. R., N. L. Taylor, and S. R. Bowley. 1985. Red
clover. Pages 457-470 in N. L. Taylor (ed). Clover sci-
ence and technology. Agron. Monogr, 25.
Strickland, W. 1801. Observations on the agriculture of
the United States of America. W. Bulmer, London, U.K.
Taylor, N. L. 1975. Red clover and Alsike clover. Pages
148-158 in M. E. Heath, D. S. Metcalfe, and R. E.
Barnes (eds). Forages. lowa State Univ. Press, Ames,
IA.
Taylor, N. L. 1986. Registration of KY C-1 crimson clover
germplasm. Crop Sci. 26:838.
Taylor, N. L. 199la. Registration of KY-1 kura clover
germplasm. Crop Sci. 31:237.
Taylor, N. L. 1991b. Registration of KY M-2 zigzag clover
germplasm. Crop Sci. 31:1395-1396.
Taylor, N. L., and J. N. N. Campbell. 1989. Native Ken-
tucky clovers: buffalo clovers. Univ. Kentucky Coop.
Exten. Serv. AGR-142.
Taylor, N. L., J. M. Gillett, J. J. N. Campbell, and S. Ber-
ger. 1994. Crossing and morphological relationships
among native clovers of eastern North America. Crop
Sci. 34: 1097-1100.
Taylor, N. L., J. C. Henning, and G. D. Lacefield. 1997a.
Growing red clover in Kentucky. Univ. Kentucky Coop.
Exten. Serv. AGR-33.
Taylor, N. L., D. Henry, and J. Vandevender. 1997b. Kura
clover for Kentucky. Univ. Kentucky Coop. Exten. Serv.
AGR-141.
Taylor, N. L., and K. H. Quesenberry. 1996. Red clover
science. Kluwer, Boston, MA.
~
{
The genus Trifolium (Fabaceae) in Kentucky—Vincent 1
Taylor, N. L., and R. E. Sigafus. 1984. Some winter annual Wharton, M. E., and R. W. Barbour. 1971. A guide to the
clovers Kentucky 1980-1983. Kentucky Agric. Exper. wildflowers and ferns of Kentucky. Univ. Press of Ken-
Sta. Prog. Rep. 277. tucky, Lexington, KY.
Vincent, M. A. 1991. Trifolium reflexum L. (buffalo clover: | Zohary, M., and D. Heller. 1984. The genus Trifolium.
Leguminosae) in Ohio, its history and present status. Israel Academy of Sciences and Humanities, Jerusalem,
Michigan Bot. 30:65-68. Israel.
Vincent, M. A., and A. W. Cusick. 1998. New records of
alien species in the Ohio vascular flora. Ohio J. Sci. 98:
10-17.
J. Ky.
Acad 62(1):18—-25. 2001.
The Role of Light in Regulating Dandelion (Taraxacum officinale;
Asteraceae) Inflorescence Height
David Lowell Robinson
Department of Biology, Bellarmine University, Louisville, Kentucky 40205
ABSTRACT
This research examined the ecophysiological basis for extension of the stalks (scapes) supporting the
inflorescences (heads) of the common turfgrass weed, dandelion (Taraxacum officinale Weber). In turf, a
statistically significant positive correlation was observed between turfgrass height and height of dandelion
heads occurring in it. Dandelion heads tended to extend to the top of the turfgrass canopy only, whereas
seedheads extended, on average, an additional 11 em above that. Excised scape segments taken from scapes
at the pre-flowering stage elongated significantly less in the light than in the dark; those taken after flowering
elongated the same in the light as in the dark and significantly more than the illuminated pre-flowering
scapes segments. In a whole-plant study, pre-flowering scapes grown in a far-red enriched microenvironment
elongated significantly more than scapes grown in other light microenvironments. Scape elongation after
flowering, however, was not statistically different in any treatment. Pre-flowering scape elongation in dan-
delion, therefore, appears to be a phytochrome-mediated response, whereas elongation after flowering is
not. These results suggest that dandelion scape elongation may be physiologically linked to the height of the
turfgrass canopy.
INTRODUCTION
Dandelion (Taraxacum officinale Weber)
possesses numerous weedy characteristics that
make it one of the most common invasive
plants of turf in urban areas (Longyear 1918).
It is adapted to a wide range of environments,
is a long-lived species, reproduces vegetatively
from its taproot, and has few natural enemies
(Crutchfield and Potter 1995: Mitich 1989:
Roberts 1936). Dandelion is also a prodigious
seed producer: up to 60,000 seed m? per sea-
son (Roberts 1936). Taraxacum species can set
seed apomictically, thus ensuring high seed
production even under conditions unfavorable
for fertilization, such as extreme temperatures,
water stress, or lack of pollinators (Munn
1919). Seed dispersal over long distances is as-
sisted by the parachute-like pappus attached
to each seed.
Another characteristic contributing to the
weedy nature of this species concerns the
grow th habit of its reproductive stalk (scape).
Dandelion inflorescences (heads) often do not
extend far enough above the soil surface to be
cut by turforass. mowers. Prior to flowering,
dandelion scapes grow straight upwards, but
immediately after ‘flowering elongation slows
noticeably and the uppermost portion of the
scape can become diagravitropic (Clifford and
Oxlade 1989). As a result, dandelion heads, for
the majority of the time it takes for the seed
to mature, are kept low to the ground and be-
low the lawnmower blade (Longyear 1918).
During seed maturation the scape rapidly
elongates upwards again, lifting the seedhead
far lsat e the canopy and into a better position
for dispersal of seed by wind (Chao 1947;
Longyear 1918). Growth during the pre- oes
ering and pre-shattering (post-flowering) stag-
es may be partially controller by hormones
(Clifford et al. 1985: Clifford and Oxlade 1989:
Oxlade and Clifford 1981).
My research concerns the ecophysiological
mechanisms controlling elongation of dande-
lion scapes. There have been numerous re-
ports on how radiant energy controls the way
plants develop and interact with one another
(Ballare et al. 1992; Briggs 1996; Holt 1995;
Koornneef and Kendrick 1994: Schmitt and
Wulff 1993). One of the most important plant
molecules involved in the detection of light is
phytochrome. Numerous plant photomorpho-
genic responses are mediated by phyto-
chrome, including those regulating plant
height, branching, leaf shape, photoperiodic
Gar ering, photosynthate allocation, and seed
germination (Ballare et al. 1988; Ballare et al.
1990; Ballare et al. 1992; Novoplansky 1991;
Sanchez 1971; Schmitt and Wulff 1993; Smith
1982: Vierstra 1993).
Phytochrome is a family of photoreceptor
Dandelion Inflorescence Height—Robinson 19
molecules containing a photoreversible pig-
ment that can absorb either red (maximal at
666 nm) or far-red (maximal at 730 nm) light.
Plants grown completely in the dark synthe-
size the form of phytochrome (designated P,)
that absorbs red light. Following an exposure
to red light the P, pigment converts to a form
(designated P,,) that absorbs far-red light. Af-
ter an exposure to far-red light the P,, can con-
vert back to P, in a cyclical process. One of
the ways that red:far-red ratios are modified in
nature is by the presence of neighboring plant
foliage (Ballare et al. 1988; Holmes and Smith
1975; Smith 1994). This is due to the prefer-
ential absorption of red light (vs. far-red) by
chlorophyll. If a plant is growing by itself in
uninterrupted sunlight, the microenvironment
will contain more red light than far-red, and
there will be relatively more P,, in the plant,
while a plant growing in a dense vegetative
canopy will be exposed to more far-red light
than red and contain relatively more P,. The
physiologically active form of phytochrome is
P,,. When present, it induces the synthesis of
a cascade of gene products involved in the
photomorphogenic traits mentioned above
(Smith 1994; Vierstra 1993). Generally, high
levels of P;, inhibit elongation of plant cells
and tissues. The magnitude of phytochrome-
mediated responses is often a function of the
P,.: P, ratio at any given time.
In plants, exposure to lowered red:far-red
ratios typically induces an increase in apical
elongation (height) at the expense of lateral
growth (Ballare et al. 1987, 1990; Schmitt and
Wulff 1993; Smith 1982), and is the reason
that plants growing beneath a plant canopy are
generally taller than in an open field (Holmes
and Smith 1975; Solangaarachchi and Harper
1987). Even plants similar in height can have
this influence on one another at distances up
to 30 cm (Smith et al. 1990). The ecological
consequence of this “neighbor effect” is that
plants detect the presence of other plants in
their vicinity before those plants become com-
petitors for sunlight or pollinators (Ballare et
al. 1988, 1991; Holt 1995).
The objectives of my study were to examine
the role of light in regulating dandelion scape
elongation, and to describe the developmental
changes in light sensitivity of the scape during
the transition from flowering to seed dispersal.
MATERIALS AND METHODS
Field Observation
Naturally occurring variation in dandelion
scape height was evaluated in Louisville, Ken-
tucky, in April-May 1996 and April 1997. Six-
ty-six randomly selected turfgrass sites were
surveyed in 1996; 81 sites in 1997. Survey sites
were from public and residential turfgrass ar-
eas that were in full sunlight and had not been
recently mowed. Measurements taken at each
site were height of open inflorescence (from
soil level to the bottom of receptacle), height
of shattering seedhead (from soil level to bot-
tom of receptacle), and turfgrass canopy
height. In both cases, the head was pulled ver-
tically taut while measuring heights. Best-fit
regression analysis was performed with these
data (Jandel Scientific 1995).
Excised-Scape Study
Dandelion scapes at either the pre-flower-
ing or pre-shattering (post-flowering) stages
were collected in May 1996 from a single, uni-
form turfgrass location on the Bellarmine Uni-
versity campus (Louisville, Kentucky), excised
into 1 cm segments, and floated in 100 x 15
mm petri dishes containing a 20 ml sucrose
solution (10 g I) and 30 uM _ 3-indoleacetic
acid, as described by Chao (1947). It has been
determined that indoleacetic acid is necessary
to prevent the scape segments from splitting.
Only the upper 4 cm of each scape were used
for sampling, and segments were evenly dis-
tributed into different treatments (dishes).
Dishes containing the scape segments were
immediately placed onto a glass shelf in an en-
vironmental growth chamber and allowed to
grow for 3 days at constant illumination and
constant temperature (26°C). Sixteen 160-W
fluorescent bulbs provided illumination from
above, and two 100-W clear incandescent
bulbs provided illumination from below. The
photosynthetic photon flux density (PPFD)
provided from above was 874 mol m~°s"';
the PPFD from below was 42 pmol m~?s"!,
both measured by a LI-1800 spectroradiome-
ter (LI-COR Inc).
Transparent, colored cellophane filters cut
to the size of the dishes were placed on the
bottom to filter the light coming from the in-
candescent bulbs placed below. Filters trans-
mitted clear, blue, red, or far-red light. Far-
20 Journal of the Kentucky Academy of Science 62(1)
red filters were achieved by overlapping blue
with red filters. The thickness of the colored
filters was adjusted so that each had an equiv-
alent amount of light passing through. Their
ectral qualities are described in the next sec-
ion. Two experimental controls were used:
one in which the bottom light was blocked
with paper and another in which the dish was
completely wrapped in aluminum foil. Each
experiment consisted of 12 dishes of excised
dandelion segments: six from scapes collected
prior to flowering, and six from scapes col-
lected prior to shattering. Each dish held 14
scape segments taken from 14 different plants.
The segments in each dish were illuminated
the same from above but were treated with
one of the five different light treatments from
below, while the sixth dish received no light at
all. Three days after the start of the experi-
ment the ler vgth of each segment was mea-
sured and av eraged. There were five replicat-
ed experiments fitecks) ), and results were sub-
jected to two-way analysis of variance (Jandel
Scientific 1995).
Whole-Plant Study
Dandelion seeds used in this study were
collected in May 1995 from a single popula-
tion in Afton, Minnesota. The peed: were
planted into 216 cm® plastic containers filled
with potting soil (Metro-Mix 510) and grown
in the environmental growth chamber with an
alternating 14-hr light period (26°C) and 10-
hr dark period (20°C). The same growth
chamber as described above was used except
that six incandescent bulbs (100 W) were used
in addition to the fluorescent ones and no il-
lumination was provided from below. This
generated a PPFD of 950 pmol m~?s~!. After
2 wk, plants were thinned to three plants per
container. Seven weeks after sowing, the
plants were vernalized by placing them in a
5°C coldroom and illuminated with fluores-
cent lights. After 4 mo, the plants were taken
out and acclimated.
After acclimation at room temperature for
| day, single pots were placed individually into
the Gatton of single transparent plastic cylin-
ders (10-cm daneian! Two windows were cut
into the cylinders just above soil level so leaves
could be pulled out through the windows and
held horizontal. This was to prevent photosyn-
thesis from being affected by the light treat-
ments and to prevent the foliage from inter-
fering with the light microenvironment around
the scape. Transparent colored cellophane
(described above) was wrapped around the
cylinders above the windows extending 7 cm
above the soil. Blue, red, and far-red filters
were used. As done previously, the thickness
of the colored filters was adjusted so that there
was an equivalent amount of light passing
through each. As experimental controls, clear
plastic was wrapped around one cylinder in
the same fashion, and opaque black plastic was
wrapped around another. The transmission
spectra for the filters were determined with
the spectroradiometer. Spectral quality (R: FR)
of the different filters was calculated as de-
scribed by Smith (1994). The R:FR_ ratios
were: clear = 1.54, opaque = 1.43, red = 1.48,
far-red 1.37, and blue = 1.36. Although
these values are higher than those reported by
other researchers (because most of the radiant
energy was emitted from fluorescent light
bulbs) they are within the range of values
known to induce phytochrome-mediated re-
sponses (Holmes and Smith 1975; Smith 1994;
Weller and Reid 1993). Each replication
(block), of which there were six in all, consisted
of five cylinders representing these five light
treatments.
Cylinders were placed at least 30 cm apart
in the growth chamber. The long- -day condi-
tions in the chamber induced the plants to
flower. Height of the first six dandelion scapes
to emerge fr om each pot was monitored daily,
from ANS first day of flowering until seedhead
opening. Heights were measured from soil
level to bottom of receptacle. Two-way analy-
sis of variance was used to test for significance
(Jandel Scientific 1995).
RESULTS
Field Observation
To illustrate the relationship between dan-
delion scape height and height of the sur-
rounding canopy, observations were made in
dozens of different public and residential turf
grass communities in Louisville in spring 1996
and 1997. Similar results were observed in
both years (Figure 1). The height of the turf-
grass canopies ranged from 2 to 35 cm; the
height of the dandelion heads growing in them
ranged from 3 to 32 cm. Generally, the heads
Dandelion Inflorescence Height—Robinson 21
Seedhead -——_~_
O Oo
©
Spring 1996
Kn. Inflorescence
Scape Height (cm)
Scape Height (cm)
Turf Height (cm)
Figure 1. The relationship between turfgrass canopy
height and dandelion scape height at various turfgrass sites
in Louisville, Kentucky, during spring 1996 (upper) and
1997 (lower). In 1996 (n = 66), inflorescence (head)
height was described by Y = 3.884 + 0.737X (° = 0.70),
and seedhead height was described by Y = 13.429 +
0.912X (12 = 0.65). In 1997 (n = 81) inflorescence (head)
height was described by Y = 2.683 + 0.717X (x2 = 0.86),
and seedhead height was described by Y = 10.716 +
0.953X (x2 = 0.75).
extended only to the top of the turfgrass can-
opies. Linear regression analysis revealed a
statistically significant (P < 0.001) correlation
between head height and turf height with r
values of 0.70 for 1996 and 0.86 for 1997. In
1996, average head height was the same as the
average canopy height, whereas in 1997 the
average head was | cm shorter than the can-
opy. Regression analysis indicated that heads
were slightly taller than the surrounding turf
at canopy heights below 15 cm in 1996 (9 cm
in 1997). Above that height, dandelion heads
tended to be slightly shorter than the canopy.
In the tallest turfgrass communities, the dan-
delion heads averaged 5 cm (1996) and 7 cm
(1997) below the canopy.
Seedhead heights, measured at the same lo-
cations, ranged from 10 to 54 cm and were
significantly taller than the height of the
neighboring turfgrass (on average, 12 cm taller
in 1996 and 10 cm taller in 1997). Seedhead
height was significantly correlated (P < 0.001)
with the height of the turf canopy with r° val-
ues of 0.65 for 1996 and 0.75 for 1997. In
1996, the slopes for the head and seedhead
regression lines were not statistically different
from one another, whereas in 1997 they were
(P < 0.001).
In this field study, the positive correlation
of dandelion scape elongation with height of
the neighboring turf canopy suggests that dan-
delions adjust their scape growth to the veg-
etative growth of the turfgrass species sur-
rounding it. Since head and seedhead heights
were measured at the same time and at the
same place, the changes in growth of dande-
lion scapes prior to flowering versus their
growth after flowering were probably due to
physiological shifts within the scapes them-
selves and not to changes in the environment.
The other experiments described in this paper
were designed to explore the possibility that
this regulation of growth is phytochrome me-
diated. Since scapes at the flowering and seed-
head stages appeared to respond to the mi-
croenvironment differently, the effect of light
at these two developmental stages was also ex-
amined.
Excised-Scape Study
Pre-flowering scape segments (that were il-
luminated) elongated an average of 38%,
whereas segments from older scapes, carrying
heads that were about to shatter, elongated an
average of 50% (Table 1). This difference was
statistically significant (P < 0.001) and indi-
cates that scape growth, in response to light,
shifts as it progresses from one developmental
stage to another. The only statistical difference
in elongation among the pre-flowering scape
segment treatments was for those kept in
complete darkness. This experimental control
elongated significantly more (15%) than pre-
flowering scape segments grown in light. In
the dark, however, the pre-flowering scape
segments elongated as much as the pre-shat-
tering segments kept in either the light or the
dark. No significant differences were observed
for pre-shatter scape elongation in any of the
22 Journal of the Kentucky Academy of Science 62(1)
Table |. Length of pre-flower and pre-shatter dandelion
scapt sments after 3 d treatment with supplemental
light. Scapes were collected in May 1996 in Louisville,
K ky and excised into 10 mm lengths before treat-
it. Average of 5 replications, 14 segments per repli-
cation (n = 70 segments per treatment). Means followed
by the same letter, within a column, are not significantly
different (P < 0.05) according to the Student-Newman-
Keuls test.
a Pre-flower scape Pre-shatter scape
segment length segment haneti
Filter color mim) * SE mm) = SE
Clear 13.8 + 0.09 b 14.9 + 0.05 a
Barrier 13.7 + 0.06 b 14.6 + 0.05 a
Blue 13.7 + 0.07 b 15.1 = 0.05 a
Red 14.1 + 0.06 b 15.2 + 0.05 a
Far-Red 13.7 = 0.04 b 152 = 0:05" a
Wrapped 15.9 + 0.02 a 15.0 = 0.05 a
treatments. All pre-shatter scape segments
grew the same whether they were placed in
the dark, in the light, or were supplemented
with specific wavelengths of light from be-
neath. This experiment demonstrates that
scapes have the same growth potential before
flowering as they do aftenw ards, but that this
potential is not realized prior to flowering be-
cause of light sensitivity at that stage.
Whole-Plant Study
The flowering head heights in the two con-
trol treatments (clear atl opaque) were not
significantly different from one another and
averaged 10.6 cm above soil level, which was
3.6 cm above the top of the filters (Table 2).
The blue and red treatments were not statis-
tically different from the clear and opaque
treatments. Plants treated with far-red light,
however, produced heads that were 23% taller
than any of the other treatments or controls
(significant at P < 0.05). This differential re-
sponse for far-red light, versus red light, in-
dicates that phytochrome may have a role in
regulating head elongation.
It took an ave rage of 7.5 days for heads to
develop into shattering see »dheads. There were
no statistical differences for this time frame
among the treatments. During this period the
scapes elongated another 6 cm, on average,
representing an increase of 52% (Table 2). As
with the heads, there were no significant dif-
ferences in seedhead scape height in the clear,
opaque, blue or red treatments. Elongation of
the far-red treated scapes, however, was sta-
tistically greater. When head height was sub-
tracted from seedhead height, no significant
differences were apparent, indicating that
post-flowering elongation may not be strongly
influenced ee the light microenvironment.
These results support the field observation
that dandelion seedheads extend a fairly uni-
form distance above the turfgrass canopy re-
gardless of their height at flowering (Figure 1).
It also supports the explant study showing that
seedhead scape tissue was less sensitive to
light than scape tissue at the flowering stage
(Table 1).
Another photomorphogenic response that
occurred in this study involved the time it took
for the plants to flower. It took 13.2 days, from
the time the blue-treated plants were placed
in the growth chamber, to the time they pro-
duced six heads (Table 3). The far-red treat-
ment completed blooming after only 9.5 days,
significantly faster (P < 0.05) than the blue-
meried plants. Accelerated flowering rates are
associated with plants pursuing a shade-avoid-
ance strategy, which is generally phytochrome
mediated (Smith 1994).
DISCUSSION
Like many weedy-plant species, dandelions
show large amounts of phenotypic plasticity
Table 2. Head and seedhead elongation in dandelion plants treated with supplemental light. Prior to treatment, plants
were induced to flower under enviornmentally controlled conditions. Average of 6 replications, 6 scapes per replication
(n = 36 scapes per treatment). Means followed by the same letter, within a column, are not significantly different (P
< 0.05) according to the Student-Newman-Keuls test.
Filter color Head height (em) + SE
Seedhead height (em) = SE
Difference (em) = SE
Clear 10.1 + 0.46 b
Opaque 11.1 + 0.79 b
Blue 10.5 = 0.62 b
Red 11.0 + 0.48 b
Far-Red 13.1 = 0.64 a
16.0 1.47 b 5iGr == allo
16.9 + 0.82 b 5.8 + 0.62 a
15.0 = 1.00 be 45+ 0.8la
Vip E2S ih 6.2 + 140a
19.8 + 1.22; 6.7, eS ra
Dandelion Inflorescence Height—Robinson 93
Table 3. Time it took for the first 6 heads to emerge in
dandelion plants treated with supplemental light. Prior to
treatment, plants were induced to flower under enviorn-
mentally controlled conditions. Average of 6 replications,
6 scapes per replication (n = 36 segments per treatment).
Means followed by the same letter, within a column, are
not significantly different (P < 0.05) according to the Stu-
dent-Newman-Keuls test.
Filter color Days to 6th head + SE
Clear 10.3 = 1.41 ab
Opaque 12.3 + 0.49 ab
Blue 13.2 + 1.08 a
Red 10.3 + 0.92 ab
Far-Red 9.5 + 0.76 b
(Clifford and Oxlade 1996). These ecological
adaptations are exhibited in their reproductive
biology. Dandelion heads require light in or-
der to open, and they must open if they are
to set seed (Longyear 1918; Roberts 1936; Ta-
naka et al. 1987). This means that heads ex-
tending to the top of the turfgrass canopy
maximize their potential for setting seed.
However, the farther above the canopy dan-
delion heads extend the greater their risk of
being separated from the plant by mowing. Af-
ter flowering, the tight control of scape elon-
gation may not be as important because ex-
tension of the seedhead above the canopy sur-
face enhances seed dispersal by wind. This
shift in elongation strategy can occur rapidly
as both Longyear (1918) and Roberts (1936)
observed that dandelions producewiable seed
long before seedheads actually shatter.
This research illustrates that control of dan-
delion scape growth is due to an interaction
between the physiological status of the plant
and the surrounding microenvironment. In
the field, dandelion plants produce heads that
just reach the top of the turfgrass canopy. This
linkage of dandelion head height to the height
of the surrounding turf is maintained in com-
munities ranging from only 2 cm in height up
to more than 17 times that. The laboratory
studies demonstrate that control over scape
elongation is mediated by phytochrome. The
far-red treatment (with a red:far-red ratio of
1.37) caused scapes to grow significantly taller
than light treatments with higher red: far-red
ratios, like clear (1.54), red (1.48), and opaque
(1.43). Due to the asymptotic relationship be-
tween red:far-red ratios and the amount of P,,
in plant tissues (relative to P,,,,;), small changes
in the quality of light have been found to elicit
major physiological changes in plants (Smith
1994). Previous researchers have shown that
phytochrome-mediated responses are corre-
lated to relative amount of far-red light up to
red:far-red values of 2.00 (Holmes and Smith
1975: Smith 1994; Weller and Reid 1993).
We have measured the red:far-red ratios in
natural turfgrass canopy microenvironments to
be 1.06, compared to 1.14 in full sun. As dan-
delion scapes form and elongate, the lower
red: far-red ratio caused by the preferential
absorption of red light by turf foliage may en-
courage elongation due to predominance of P,
phytochrome, the form which does not inhibit
elongation. When the inflorescence bud ap-
proaches the top of the canopy, however, the
red:far-red ratio may be high enough (due to
predominance of the P,, form of phytochrome)
to discourage any further scape elongation
and, at the same time, induce head opening.
The photomorphogenic control of scape
elongation by phytochrome appears to be de-
velopmentally controlled. Whereas all three of
these studies indicate that dandelion scapes,
up to the time of flowering, are sensitive to
light, no evidence was found that scape growth
after flowering was affected by light. Thus,
major physiological changes must be occurring
in this tissue in a relatively short period of
time: 7.5 days in this growth-chamber study
vs. 9 or 10 days in the field (Longyear 1918).
Scape elongation rates between the flowering
and shattering stages in the clear-plastic treat-
ment of the whole-plant study averaged more
than 8 mm d“!. This growth is rapid enough
to carry the head above the turfgrass canopy
at a faster rate than the canopy height itself
increases. Chao (1947) reported that the ma-
jority of this scape growth occurred in the up-
per third of the scape and involved increases
in epidermal cell length, fresh weight, and
non-protein nitrogen content, as well as de-
creases in dry weight, and protein nitrogen
content.
An important source of light perception
might reside in the dandelion head itself. Ta-
naka et al. (1987) showed that some type of
photoreceptor must occur in the dandelion
head as its opening is dependent on sunlight.
Since the majority of the scape growth is due
to cell elongation in the upper third of the
24 Journal of the Kentucky Academy of Science 62(1)
scape (Chao 1947; Oxlade and Clifford 1981)
it is possible that a growth regulator (like gib-
bey //in, auxin, or ethylene) is synthesized in
the cad and moves down to that region (Clif-
ci and Oxlade 1989: Clifford et al. 1985) to
sodulate tissue growth. This would explain
he discrepancy he tween the excised-scape ex-
periment and the whole-plant experiment.
Some factor important to the phytochrome re-
sponse in dandelion scapes may not have been
present in the excised segments,
This research has implications for turfgrass
managers interested in reducing the propaga-
tion of dandelion by seed. Since the majority
of dandelion seed production and dissemina-
tion is in the spring (Gray et al. 1973), the
simple act of keeping turf taller during the
preceding winter months might force dande-
lion heads to elongate enough in the spring so
that a larger percentage of them could be
mowed before they set seed. The same sce-
nario might be applied during the second flush
of flowering that occurs in the autumn. This
paper sets the groundwork for studies of these
types of management strategies.
ACKNOWLEDGMENTS
The cooperation of Edie Greer and Karan
Kaul at the Atwood Research Facility, Ken-
tucky State University, is much appreciated.
Thanks also go to students Scott Farmer, Mik-
ki Jo eather and Anton Clemmons for their
work on the dandelion project. Joann Lau and
Snake Jones provided helpful suggestions.
This research was funded by the Bellarmine
University Faculty Summer Stipend Program.
LITERATURE CITED
Ballare, C. L., R. A. Sanchez, A. L. Scopel, J. J. Casal,
and C. M. Ghersa. 1987.
plants by phytochrome perception of spectral changes
in reflected sunlight. Pl. Cell Environm. 10:551—557.
Ballare, C. L., R. A. Sanchez, A. L. Scopel, and C. M.
Ghersa. 1988. Morphological responses of Datura ferox
L. seedlings to the presence of neighbors. Oecologia 76:
288-293.
Ballare, C. L., A. L. Scopel, and R. A. Sanchez. 1990. Far-
red radiation reflected from adjacent leaves: An early
Early detection of neighbour
signal of competition in plant canopies. Science 247:
329-332.
Ballare, C. L., A. L. Scopel, and R. A. Sanchez. 1991.
Photocontrol of stem elongation in plant neighbour-
hoods: effects of photon fluence rate under natural con-
ditions of radiation. Pl. Cell Environm. 14:57-65.
Ballare, C. L., A. L. Scopel, R. A. Sanchez, and S. R.
Radosevich. 1992. Photomorphogenic processes in the
agricultural environment. Photochem. Photobiol. 56:
777-788.
Briggs, W. R. 1996. Light and the genesis of form in
plants. Pages 1-8 in W. R. Briggs, R. L. Heath and E.
M. Tobin (eds). Regulation of plant growth and devel-
opment by light. Current topics in plant physiology 17.
Ame : an Society of Plant Physiologists, Rockville, NY.
Chao, M. D. 1947. Growth of the dandelion scape. PI.
P a 22:393—406.
Clifford, P. E., D. M. A. Mousdale, S. J. Lynd, and E. L.
Oxlade. 1985. Differences in auxin level detected across
geostimulated dandelion peduncles: evidence support-
ing a role for auxin in geotropism, Ann. Bot. 55:293-
296.
Clifford, P. E., L. Oxlade. 1989. Ethylene produe-
tion, georesponse, and extension growth in dandelion
peduncles. Canad. J. Bot. 67:1927—1929.
Clifford, P. E., and E. L. Oxlade. 1996. Using dandelions
to demonstrate the concept of phenotypic plasticity.
Am. Biol. Teach. 60;:291-293.
Crutchfield, B. A., and D. A. Potter. 1995. Feeding by
japanese beetle and southern masked chafer grubs on
lawn weeds. Crop Sci. 35:1681—1684.
Gray, E., E. M. McGehez, and D. F. Carlisle. 1973. Sea-
sonal variation in flowering of common dandelion.
Weed Sci. 21:230-232.
Holmes, M. G., and H. Smith. 1975. The function of phy-
tochrome in plants growing in the natural environment.
Nature 254:512-514.
Holt, J. S. 1995. Plant responses to light: A potential tool
for weed management. Weed Sci. 43:474-482.
Koornneef, M., and R. E. Kendrick. 1994. Photomorpho-
genic mutants of higher plants. Pages 601-628 in R. E.
Kendrick and G. H. M. Kronenburg (eds). Photomor-
phogenesis in plants. Kluwer Academic Publishers,
Dordrecht, Netherlands.
and E.
Jandel Scientific. 1995. SigmaStat user’s manual, version
2.0. Jandel Scientific Corporation, San Rafael, CA.
Longyear, B. O. 1918. The dandelion in Colorado. Colo-
rado Agric. Exp. Sta. Tech. Bull. 236.
Mitich, L. W. 1989. Common dandelion—the lion’s tooth.
Weed Technol. 3:537-539.
Munn, M. T. 1919. Spraying lawns with iron sulfate to
eradicate dandelions. New York Agric. Exp. Sta. Ann.
Rep. 38:246-284.
Novoplansky, A. 1991. Developmental responses of por-
tulaca seedlings to conflicting spectral signals. Oecolo-
gia 88:138-140.
Oxlade, E. L., and P. E. Clifford. 1981. Experiments in
geotropism. J. Biol. Educ. 15:137-142.
Roberts, H. F. 1936. Seed reproduction in the dandelion.
Sci. Agric. 17:235-242.
Sanchez, R. 1971. Phytochrome involvement in the con-
trol of leaf shape of Taraxacum officinale L. Experientia
27:1234—1237.
Schmitt, J., and R. D. Wulff. 1993. Light spectral quality,
Dandelion Inflorescence Height—Robinson 95
phytochrome and plant competition. Trends Ecol. Evol.
8:47-51.
Smith, H. 1982. Light quality, photoreception, and plant
strategy. Ann. Rev. PI. Physiol. 33:481-518.
Smith, H. 1994. Sensing the light environment: the func-
tions of the phytochrome family. Pages 377-416 in R.E.
Kendrick and G.H.M. Kronenburg (eds). Photomor-
phogenesis in plants. Kluwer Academic Publishers,
Dordrecht, Netherlands.
Smith, H., J. J. Casal, and G. M. Jackson. 1990. Reflection
signals and the perception by phytochrome of the prox-
imity of neighboring vegetation. Pl. Cell Environm. 13:
T1303.
Solangaarachchi, S. M., and J. L. Harper. 1987. The effect
of canopy filtered light on the growth of white clove:
Trifolium repens. Oecologia 72:372-376.
Tanaka, O., H. Wada, T. Yokoyama, and H. Murakami
1987. Environmental factors controlling capitulum
opening and closing of dandelion, Taraxacum albidum.
Pl. Cell Physiol. 28:727—730.
Weller, J. L., and J. B. Reid. 1993. Photoperiodism and
photocontrol of stem elongation in two photomorpho-
genic mutants of Piswm sativum L. Planta 189:15-23.
Vierstra, R. D. 1993. Illuminating phytochrome functions.
Pl. Physiol. 103:679-684.
J. Ky. Acad. Sci 26-34. 2001.
Distri>ution and Status of Freshwater Mussels (Bivalvia: Unionoidea)
in the Cumberland River Basin Upstream from
Cumberland Falls, Kentucky
Ronald R. Cicerello and Ellis L.
Nature Preserves Commission, 801 Schenkel Lane,
Kentucky State
Laudermilk
Frankfort, Kentucky 40601
ABSTRACT
Freshwater mussels were sampled in the Cumberland River basin upstream from Cumberland Falls in
southeastern Kentucky in 1987-1999 to determine their distribution and status. A total of seven species was
found at 57 of 434 sampling sites compared to 11 taxa previously reported. Alasmidonta atropurpurea and
Anodontoides denigratus, USFWS-
and/or KSNPC-endangered species, are the most abundant taxa and
exclusively inhabit tributaries. Lampsilis ovata was introduced from below the falls and is extirpated from
the basin along with Toxolasma parvus and Villosa lienosa. We believe that records for Strophitus undulatus
are based on misidentified Alasmidonta atropurpurea and Anodontoides denigratus. The Marsh Creek fauna
is the richest and most abundant upstream from the falls, and it should be the focus of mussel conservation
efforts in the basin.
INTRODUCTION
Despite considerable interest in the fresh-
water mussels of Kentucky’s upper Cumber-
land River basin (e.g., Miller et al. 1984: Neel
and Allen 1964; Gelneter et al. 1989: Wilson
and Clark 1914), little has been published re-
garding the fauna upstream from Cumberland
Falls. Wilson and Clark (1914) and Neel and
Allen (1964) each sampled six sites, all but one
in the mainstem, and found a depauperate
fauna ee eight generally uncommon spe-
cies (Table 1). Recent examination of 14 Cum-
berland River tributaries revealed mussels
only in Marsh Creek and added Alasmidonta
atropurpurea to the fauna (Call and Parmalee
1981; Harker et al. 1979, 1980; Layzer and
Anderson 1992). Museum records for Toxolas-
ma parvus and Villosa lienosa increase the
fauna to 11 species, or ca. 15% of the taxa
known from the basin below Cumberland
Falls (Cicerello et al. 1991).
The basin above the falls has changed con-
siderably since the work of Wilson and Clark
(1914) and Neel and Allen (1964). Commu-
nities and infrastructure have expanded, and
surface and underground coal mines occur
throughout the watershed (Leist et al. 1982).
Development has degraded water quality and
aquatic communities throughout the basin and
downstream from Cumbedend Falls (Carter
and Jones 1969; Cicerello and Peale
1997: Harker al. 1979: KDOW 1996).
Nonetheless, ie area contains many of Ken-
et
tucky’s highest quality streams (KDOW 1997),
most of ach have not been thoroughly sam-
pled for mussels. We examined streams in the
upper Cumberland River basin of Kentucky
upstream from Cumberland Falls and muse-
um collections to determine the distribution
and status of the mussel fauna.
STUDY AREA
Located in the Appalachian Plateaus Phys-
iographic Province in southeastern Kentucky
and Tennessee, the study area encompasses
5120 km? of the upper Cumberland River ba-
sin in Kentucky extending from Cumberland
Falls es to the southent Virginia bor-
der (Figure 1). Cumberland Falls is a 17 m
high barrier to the upstream movement of
aquatic organisms that has receded ca. 72 km
from its hypothesized original location near
Burnside, Kentucky (McGrain 1966). The Big
South Fork Cumberland, Rockeastle, and
Laurel rivers and Buck Creek formerly dis-
charged into the river above the falls, but now
they enter between its hypothesized original
and present locations. The Cumberland River
is formed by the confluence of the Poor and
Clover forks; it meanders westerly 212 km to
the falls. Major tributaries are Marsh, Jellico,
Stinking, Straight, and Yellow creeks and
Clear and Martins forks. The headwaters of
Marsh and Jellico creeks and Clear Fork are
in Tennessee. Most streams have moderate to
high gradients, clear water, and alternating
Mussels collected from the Cumberland River system upstream from Cumberland Falls, following prevailing nomenclature.
Table 1.
1s
This study and
museum record
1987-1988*
1978-19809
1947-1949?
1910-1911!
A. pectorosa
A. pectorosa
Actinonaias pecterosa
Alasmidonta atropurpurea
A. viridis
A, atropurpurea
A. viridis
A. atropurpurea
Alasmidonta minor
A. denigratus
L. fasciola
A. ferussacianus
L. fasciola
Anodontoides ferussacianus
Freshwater Mussels—Cicerello and Laudermilk 7
L. fasciola
Lampsilis fasciola
Lampsilis ovata
L. cardium
L. ventricosa
L. o. ventricosa
Strophitis edentulus
Unio gibbosus
E. dilatata
E. dilatata
E. dilatatus
Elliptio dilatatus
Toxolasma parvus
Villosa lienosa
Neel and Allen (1964); ° Harker et al. (1979, 1980) and Call and Parmalee (1981); * Layzer and Anderson (1992).
1 Wilson and Clark (1914); 2
pools and riffles underlain with substrate:
ranging from exposed sandstone bedrock to
mixed sand and silt. Mean annual discharge
and 7-day 10-year low flow at Cumberland
Falls are 89.7 m?/s and 0.65 m/s, respectively;
major tributaries such as Jellico and Stinking
creeks have summer low flows of zero (Ruhl
and Martin 1991: USGS 1993). The watershed
is mountainous and land use is ca. 84% forest,
13% agriculture, 2.5% mining, and 0.5% ur
ban and developed areas (MSE 1975). Wil-
liamsburg, Barbourville, Pineville, Middles-
boro, and Harlan, the largest communities in
the basin, have a combined population of less
than 30,000. Although water quality is im-
proving, many streams continue to be impact-
ed by pollutants associated with coal mining,
domestic waste, highway construction, and
poor land use (Harker et al. 1980: KDOW
1996).
MATERIALS AND METHODS
We examined 434 upper Cumberland River
basin sites for mussels in 1987-1999. All hab-
itats at each site were sampled using a viewing
bucket or while snorkeling during low flow
when the water was clear. Mussel collections
at the Academy of Natural Sciences of Phila-
delphia (ANSP), Eastern Kentucky University
(EKU), Harvard University (MCZ), National
Museum of Natural History (NMNH), Ohio
State University Museum of Zoology (OSU),
and University of Michigan Museum of Zool-
ogy (UMMZ) were examined. Species ac-
counts are presented alphabetically following
scientific names in Gordon (1995) and Tur-
geon et al. (1998). Cumberlandian regional
endemics and Cumberland River endemics
(Gordon 1995; Gordon and Layzer 1989; Ort-
mann 1924) are indicated. Each annotation in-
cludes collection site numbers (Appendix A)
followed in parentheses by the number of
specimens collected (L = living specimen(s),
F = freshly dead, R = relic) during each sam-
pling visit. Results for sites visited more than
once are in chronological order. Terms used to
summarize distribution follow Smith (1965)
and include “generally distributed” (any suit-
able habitat should yield specimens with a rea-
sonably thorough search), “occasional” (suit-
able-appearing habitat may or may not yield
specimens even after prolonged search), and
28 Journal of the Kentucky Academy of Science 62(1)
Richland
55 Creek
Big Sy : Stinking
berland Indian Creek Poor Fork
P Creek
as ~
Patterson 33 57
ones 34 st ie? —
‘ ! eg . Clover Fork
7,
~— 3
PP 5
ST A 6
4 ‘4 4
4
42
4
a 3
ara
oO
; VA
( Lo ee eee
Marsh TN
Creek N
Y
Jellico Clear Fork 0 Ki
se
Creek 47-50
Figure 1. Freshwater mussel collection sites in the upper Cumberland River basin above Cumberland Falls, south-
eastern Kentucky, 1987-1999. Site numbers are referenced in Appendix A.
“sporadic” (encountering specimens cannot be
predicted at all).
SPECIES ACCOUNTS
A brief discussion of the historical and pre-
sent distribution and status of mussels report-
ed upstream from the falls follows. Only gen-
eralized distributional information is present-
ed for Corbicula fluminea.
Actinonaias pectorosa (Conrad). Pheas-
antshell. Cumberlandian regional endemic.
Sites: 1(0; 19L, 3R; 16L): 2(8L); 3(14F: 1L):
4(1L); 5(7L); 6(1R); 7(1R); 8(1R); 9(1R);
LO(UIF): 11(1L, 1R; 1L, 1R); 1301R; 0); 14(2 2/
2R; 0); 16(1R); 18(1F); 19(8L, 1R; 7L, 1F, 1B;
41, 3F): 20(8L, LF): 21(3L); 2201F): 23(1L);
46(1L). This is the most common species in
the upper Cumberland River and lower Marsh
Creek, where it is occasional to generally dis-
tributed; it is sporadic in Clear Fork. It inhab-
its sand among cobbles or boulders, and sand
and coal fines in bedrock fractures. It was not
collected by Wilson and Clark (1914), and
Neel and Allen (1964) found only one speci-
men (near Williamsburg) which “appeared to
be a recent immigrant.”
Alasmidonta atropurpurea (Rafinesque).
Cumberland elktoe. Cumberland River en-
demic. Sites: 19(5L, 3R: 0: 3L, 2R): 20(5L):
DAA ATs): p22( Qiks) 23 (Qa)! SACL earl)
26(2L); 27(2L); 28(4L); 29(4L, 5F); 31(8L,
OF): 32(2L, IR): 331, 1E): 34S
QF); 35(1L, 17F; 22L; several L; 5L; 42L);
36(0; 1L); 37(2L; 0); 38(1F); 39(1F); 40(1F);
47(0; 1L); 48(1L; 0; 0); 49(1L); 50(1L). Until
recently, this mussel was synonymized under
A. marginata (Call and Parmalee 1981; Clarke
1981). It historically inhabited the Cumber-
land River and its southern tributaries in Ken-
tucky and Tennessee, including the Big South
Fork of the Cumberland River, upstream from
the hypothesized original location of Cumber-
land Falls near Burnside, Pulaski County,
Kentucky (Gordon 1991; Gordon and Layzer
1993). It was not reported by Wilson and
Clark (1914) or Neel and Allen (1964), but, as
observed by Gordon (1991), historic records
for A. marginata from the Cumberland River
just above the falls, McCreary/Whitley coun-
ties (UMMZ 63954), and at Williamsburg,
Whitley County (Clarke 1981, MCZ 224076),
are A. atropurpurea. Downstream from the
present falls location, it occurred in the Laurel
River, Laurel County, (as Strophitus undula-
tus) (Neel and Allen 1964; UMMZ 172886),
Lynn Camp Creek, Whitley County (Clarke
1981), and in the Big South Fork of the Cum-
berland River above Burnside, Pulaski County
(as A. marginata) (Wilson and Clark 1914).
Wilson and Clark’s (1914) record for A. mar-
Freshwater Mussels—Cicerello and Laudermilk 29
ginata from the Cumberland River near Burn-
side could be this species. This endangered
mussel (KSNPC 1996; USFWS 1998) is spo-
radic in Laurel Fork of Clear Fork, and it is
generally distributed and common in Marsh
Creek, where it was discovered by Harker et
al. (1980) and Call and Parmalee (1981). It
also inhabits the Big South Fork of the Cum-
berland River, Kentucky and Tennessee, the
Rockcastle River, where it occurs sympatrical-
ly with A. marginata (contra Gordon 1991:
Gordon and Layzer 1993), and Rock Creek,
Kentucky (Cicerello et al. 1991; Gordon 1991,
EKU). It lives in sand and silt often among
cobbles and boulders in relatively shallow
pools and runs (Gordon and Layzer 1989).
Alasmidonta viridis (Rafinesque). Slipper-
shell mussel. Sites: 19(0; 0; IR); 22(1F);
93(1F); 27(1L); 28(4L); 330L); 47(1L; 1L);
48(0: 1R; 1R). Wilson and Clark (1914) col-
lected specimens from the Cumberland River
between the falls and Pineville and from the
Clear Fork. Neel and Allen (1964) did not find
this species and hypothesized that it was lost
to acid coal mine drainage. This species is oc-
casional in Marsh Creek, where it was discov-
ered by Harker et al. (1980) and Call and Par-
malee (1981), and it is sporadic in Laurel
Fork, a Clear Fork tributary. In both streams,
small numbers of this easily overlooked mussel
inhabit sand or mixed sand, gravel, and silt
near boulders.
Anodontoides denigratus (Lea). Cumber-
land papershell. Cumberland River endemic.
Sites: 18(1R); 23(1L); 25(1L); 30(3L); 31(2L,
3F); 32(1L, 1F); 33(1L, 1R); 34(2F, 2 3/2R;
HME) 3535L, LE, 2R; 21F; 1L, 4 1/2F; 40L;
73L, 3F); 36(9L; 6L); 37(15L, 3F; 1R); 38(1L,
3F); 39(4F); 40(5L, 1F); 41(3L); 51(15L);
52(8L, IR; 13L; 10L, 3F); 53(2L; 3L); 54(5L,
IF, 2R; 18L, 1F); 55(10L, 1F, 1/2R; 8L);
56(1R; 1L). This species was described by Lea
(1852) and has been confused with A. ferus-
sacianus and Strophitus undulatus. It is dis-
tinctive from the allopatric A. ferussacianus
according to Gordon (1995), who is redescrib-
ing it. It is restricted to the upper Cumberland
River on the Cumberland Plateau in Kentucky
and Tennessee upstream from the original lo-
cation of the falls (Gordon 1995). Historically,
A. denigratus was collected from the Cum-
berland River at Pineville and Orby, Bell
County (Ortmann 1918; Wilson and Clark
~
1914; UMMZ 105530) (as A. ferussacianus ).
and from the Clear Fork (UMMZ 66141) (as
S. undulatus). Downstream from the present
location of the falls, it is known from Lynn
Camp Creek, Whitley County (UMMZ
105533) (as A. ferussacianus), and from the
Laurel River, Laurel County (Neel and Allen
1964: UMMZ 172886) (as S. undulatus). Wil-
son and Clark’s (1914) record for A. ferussa-
cianus from the Clear Fork, Jellico, Tennes-
see, probably is this species (Gordon 1995).
This species inhabits Marsh, Moore, Pine, and
Rose creeks, Mills Fork, Billies Branch,
Demps Hollow, and Rockcastle River tributar-
ies in Kentucky (EKU, KSNPC), and Big
South Fork of the Cumberland River tributar-
ies in Tennessee (Gordon 1995). The best
population of this endangered mussel
(KSNPC 1996) is generally distributed in the
middle segment of Marsh Creek, where it
comprised 57% of 282 live mussels specimens
collected in 1994. Its habitat is identical to that
of A. atropurpurea, slowly flowing or still
ools and runs underlain with silt and sand. It
is locally abundant in Moore, Pine, and Rose
creeks, Mills Fork, Billies Branch, and Demps
Hollow, all first- and second-order streams in-
habited only by A. denigratus.
Elliptio dilatata (Rafinesque). Spike. Sites:
SF(1F); 11(0; 1R); 19(5L, 1R; 1R; 1F); 20(1L,
QF): 21(1L); 24(1R); 26(1L); 42(1R); 43(1R);
44(1R); 45(1 1/2R). Historically, the spike was
the most widely distributed and abundant spe-
cies above the falls. Wilson and Clark (1914)
collected specimens at all of their sampling
sites and found that it comprised about 90%
of the Clear Fork mussel population. In the
late 1940s, it was the predominant species in
the upper Cumberland (Neel and Allen 1964).
Call and Parmalee (1981) considered the spike
common in Marsh Creek, where Layzer and
Anderson (1992) also noted its presence. The
distribution and abundance of E. dilatata have
declined greatly throughout the basin. It is
sporadic in the Cumberland River, Jellico
Creek, and Clear Fork, where we found main-
ly relic specimens, and relatively common only
in lower Marsh Creek.
Lampsilis cardium Rafinesque. Plain pock-
etbook. Sites: 3(1F; 0); 11(1R; 0); 12(1F); 13(3
WIR BO) "14(O2 MEL) FSe/2R): SCE, awk):
16(1R); 19(0; 1L, 1F; 1L, 1F); 20(1L); 22(1R);
93(1L); 24(1R); 35(1L; 0; 0; 0; 1L); 45(2L, 3
30 Journal of the Kentucky
3/2R) The plain poc ‘ketbook is widely
distribute a ue sporadic in the Cumberl: ind
Ri rom the falls upstream to Harlan Coun-
bh : in Marsh Creek, where it was collected
lurker et al. (1980) and Call and Parmalee
S1). It is sporadic in the Clear Fork, Whit-
County. Marsh Creek supports the best
population above the falls, but only seven liv-
ing or freshly dead specimens were found at
21 s: umpling sites in 1994. It forme rly was very
abundant above and below the falls (Neel and
Allen 1964), where Wilson and Clark (1914)
failed to find specimens. The only ai we
found from above the falls that pre-date Neel
and Allen (1964) are an undated Bryant Walk-
er collection from the Cumberland River at
Williamsburg, Whitley County (MCZ 46747),
and collections made in 1941 and 1945 by
Clark from the Cumberland River at Molus,
Harlan County (MCZ 123966), and 5 miles
east of Pineville (UMMZ 165273), respective-
ly.
~ Lampsilis fasciola Rafinesque. Wavyrayed
lampmussel. Sites: 1(1/2R: 0: 0): 9(1R): 10
(1R): 11(1L, 2R; 1/2F): 12(2 F); 13 (4R; 1R);
14(1 2/2R; 2L): 16(2/2F): 17(1L): 19(0; 1F, IR:
2L); 20(1L); 22(1R); 46(1/2R); 48(0; 0; 2F);
S7(1F). Although L. fasciola was not collected
by Wilson and Clark (1914), Neel and Allen
(1964) reported that it was very abundant. Call
and Parmalee (1981) and Layzer and Ander-
son (1992) collected specimens from Marsh
Creek. Lampsilis fasciola is widely distributed
but sporadic in the Cumberland River, Poor
Fork, Marsh Creek, and Clear Fork, where it
inhabits sand and/or sand, pebbles, and gravel
often near cobbles or boulders in shallow
pools or runs.
Lampsilis ovata (Say). Pocketbook. Sites:
none. Wilson and Clark (1914) collected a few
dwarfed specimens from the Cumberland Riv-
er and re ported that L. ovata was transplanted
into the river above the falls, possibly by pearl
collectors (Neel and Allen 1964). This appar-
ent effort to develop a commercially valuable
stock failed. Now considered endangered in
Kentucky (KSNPC 1996), L. ovata apparently
has not been collected subsequently; it is con-
sidered extirpated from above the falls.
Strophitus undulatus (Say). Creeper. Sites:
none. Wilson and Clark (1914) reported spec-
imens from the Cumberland River at Pine-
ville, collected by their collaborator J. F. Boep-
dilatatus, and A. pectorosa.”
Academy of Science 62(1)
ple, and from the Clear Fork, Tennessee. Neel
and Allen (1964) listed it from the Cumber-
land River at Pineville and at Wallins (near
Harlan), but stated that “[iJn the present sur-
vey only 4 forms occurred above the falls: L
fasciola, L. ovata ventricosa (=L. cardium), E.
We did not find
S. undulatus and we were unable to locate
specimens from the area for re-examination.
Based on the following, we believe Wilson and
Clark's (1914) records for S. undulatus from
above the falls are actually A. denigratus. We
re-identified two specimens of S. undulae col-
lected by Hubbs from the Clear Fork, Whitley
County, (UMMZ 66141) as A. denigratus. Wil-
son and Clark (1914) and Nese and Allen
(1964) also reported S. undulatus from the
Rockcastle and Laurel rivers. Both S. undulatus
and A. denigratus inhabit the Rockcastle River
basin (KSNPC, MCZ), but we re-identified
Neel and Allen’s (1964) S. undulatus speci-
mens from the Laurel River at Lily (UMMZ
172886) as A. denigratus and A. atropurpured.
Wilson and Clark (1914) noted that their S.
undulatus specimens were “exceedingly vari-
able and presented many puzzling forms,” in-
dicating difficulty in making identifications. Fi-
nally, ae shell descriptions and the picture of
S. undulatus in Wilson and Clark (1914) and
Neel and Allen (1964) also could be inter-
preted as A. denigratus.
Toxolasma parvus (Barnes). Lilliput. Sites:
none. Known from only one specimen col-
lected by C. Goodrich from the Cumberland
River northwest of Pineville, Bell County
(UMMZ 99672). The lilliput can be over-
looked because of its small size, but it proba-
bly is extirpated.
‘Villosa lienosa (Conrad). Little spectacleca-
se. Sites: none. A specimen collected by H.D.
Athearn from the Cumberland River near
Barbourville, Knox County, (HDA 13857) in
1966 is the only record of this rare Kentucky
mussel (KSNPC 1996) from above the falls.
This record is interesting because Richland
Creek, a nearby tributary, lies in close prox-
imity to C ollins Fork, a Kentucky River trib-
utary that supports one of Kentucky's largest
V. lienosa populations (Cicerello pers. obs.).
Geological evidence and fish distribution pat-
terns identify this area as a stream capture
theater, with probable multiple faunal ex-
changes between the drainages during recent
Freshwater Mussels—Cicerello and Laudermilk 3]
geological times (Burr and Warren 1986:
Kuehne and Bailey 1961). Stream capture oc-
curs when natural erosion cuts across a head-
water drainage divide and a stream segment
and its biota are diverted from one basin into
another. Villosa lienosa is absent, extirpated,
or rare in the adjacent Tennessee, Cumber-
land (below the falls), and Big Sandy rivers
(Beetle 1973; Cicerello et al. 1991; Starnes
and Bogan 1988), and it is tempting to invoke
stream capture and transfer of its fish host
from the Kentucky River drainage as the
source of this highly localized record. How-
ever, even the most suggestive stream capture
evidence may lead to invalid conclusions, and
limited distributions may result from intro-
ductions rather than natural factors (Jenkins et
al. 1971). The origin of V. lienosa is unclear;
the species probably is extirpated.
INTRODUCED SPECIES
Corbicula fluminea (Miiller). Asian clam.
This introduced, exotic clam is the most com-
mon and widely distributed mussel above the
falls. It inhabits the mainstem from the falls
to near the headwaters of the Poor Fork, the
lower half of Marsh Creek, Jellico Creek near-
ly to the Tennessee border, Clear Fork up-
stream into Mud Creek and Laurel Fork, Big
Indian Creek including Mills Fork, lower
Stinking Creek, and Martins Fork upstream to
Martins Fork Lake. Densities exceed 100/m?
in Marsh Creek.
DISCUSSION
We found a total of seven species, all living
or freshly dead, at 57 of the 434 sites sampled
(Table 1). With the exception of Marsh Creek
and other streams inhabited by A. denigratus,
mussels generally are sporadic and restricted
to the mainstem Cumberland River and to the
Clear and Poor forks. Species richness is
greatest in Marsh Creek (7 species), Clear
Fork (6), and the mainstem Cumberland River
(4), and several streams support only one spe-
cies (e.g., Big Indian, Jellico, Patterson creeks,
and the Poor Fork). Lampsilis fasciola is the
most widely distributed native species, inhab-
iting the Cumberland River from the falls up-
stream ca. 216 river km into Poor Fork, Marsh
Creek, and Clear Fork.
Three species found mainly in tributaries
comprised ca. 92% (613/667) of the living or
freshly dead specimens encountered. Anodoi-
toides denigratus, the most abundant specic:
is restricted to Marsh Creek, Clear Fork, and
segments of Big Indian, Patterson, Richland,
and Stinking creeks. Alasmidonta atropurpu-
rea is found primarily in Marsh Creek, as is
A. pectorosa, which lives also in the Cumber-
land River from the falls to above Yellow
Creek. Elliptio dilatata and, to a lesser extent,
L. cardium and L. fasciola, formerly were the
dominant species in the mainstem Cumber-
land River (Neel and Allen 1964; Wilson and
Clark 1914). Their decline in abundance is a
result of persistent and varied water quality
problems (Charles 1966; Jillson 1927; KDOW
1996, 1998).
Eleven species have been reported above
the falls, but only as many as nine are native
to the area. Specimens previously reported as
S. undulatus probably were mis-identified A.
atropurpurea and A. denigratus. Lampsilis
ovata was introduced into the basin (Wilson
and Clark 1914). Toxolasma parvus and V.
lienosa each were collected only once from the
basin and are considered extirpated from
there.
Marsh Creek is the most important refuge
for mussels in the upper Cumberland River
basin. It is the most species-rich, and it sup-
ports the best populations of all mussels ex-
cept A. pectorosa. More than 70% (471/667)
of all living and freshly dead specimens we en-
countered were found in Marsh Creek. The
resence of Phoxinus cumberlandensis
(USFWS (1998) threatened species) and Eth-
eostoma nigrum susanae (KSNPC (1996)
threatened species), upper Cumberland River
basin endemic fishes, increase the importance
of Marsh Creek as an epicenter for recoloni-
zation of degraded streams throughout the ba-
sin.
We note several challenges to the protection
of the biological diversity and integrity of
Marsh Gres that also threaten other basin
streams. Marsh Creek has relatively good wa-
ter quality, but it is being impacted by silt
from farms and inactive coal strip mines
(KDOW 1996). A National Resources Conser-
vation Service (formerly the Soil Conservation
Service) proposal to remove the silt by chan-
nelizing upper Marsh Creek was rebuffed, but
this proposal could resurface despite recom-
mendations to identify and revegetate eroding
32 Journal of the Kentucky Academy of Science 62(1)
areas. | reviously mined areas also could be re-
mine (o obtain formerly inaccessible or un-
pro!able coal deposits. The development of
oi) sources in uplands along the stream pos-
renewed threat to the biota. A 1987 oil
oill killed hundreds of A. atropurpurea and
\. denigratus along an undetermined length
/! Marsh Creek (Cicerello pers. obs.). Finally,
a 1965 United States Army Corps of Engi-
neers proposal to construct a 24+ m high dam
on the Cumberland River 1.6 km upstream
from Cumberland Falls was revived in 1995
by local entities interested in hydroelectric
generation and recreation. This project would
embay the Cumberland River upstream into
lower Marsh Creek and adversely impact the
aquatic biota and water quality.
ACKNOWLEDGMENTS
Thanks to M. Evans, R. R. Hannan, M.
Mays, S. E. McMurray, B. Palmer-Ball Jr., M.
A. Patterson, D. Peak, M. Thomas, and B.
Winters (former or present KSNPC) and R.
G. Biggins (USFWS) for field assistance; H.
D. Athearn (HDA), A. J. Baldinger (MCZ), E.
Hartowicz, D. O’Foighil (UMMZ), and G. A.
Schuster (EKU) for access to their collections,
data, or specimens; and C. Moore (KDOW)
and J. Kiser for sharing the Pine Creek record.
Our work was supported in part by the Ken-
tucky Department for Surface Mining Recla-
mation and Enforcement, Frankfort, Ken-
tucky.
LITERATURE CITED
Beetle. D. 1973. A checklist of the land and freshwater
mollusks of Virginia. Sterkiana 49:21—35.
Burr, B. M., and M. L. Warren, Jr. 1986. A distributional
Kentucky State Nature Pre-
serves Comm. Sci. Tech. Ser. 4.
Call, S. M.,
extant populations of Alasmidonta atropurpurea (Raf-
atlas of Kentucky fishes.
inesque) (Bivalvia: Unionidae) in the upper Cumber-
land River basin. Bull. Am. Malacol. Union 1981:42—
43.
varter, J. P., and A. R. Jones. 1969. Inventory and classi-
fication of streams in the upper Cumberland River
drainage of Kentucky. Kentucky Dep. Fish Wildlife Re-
Bull. 52.
tharles, J. R. 1966. Effects of coal-washer wastes on bi-
~~
sources, Fish.
lan}
ological productivity in Martin’s Fork of upper Cum-
berland River. Kentucky Dep. Fish Wildlife Resources,
Fish. Bull. 27-B.
Jicerello, R. R., and E. L. Laudermilk. 1997.
decline in the fre aes unionid (Bivalvia: Unionidae
lant
Continuing
>)
and P. W. Parmalee. 1981. The discovery of
fauna in the Cumberland River downstream from Cum-
berland Falls, Kentucky. Trans. Kentucky Acad. Sci. 58:
55-59.
Cicerello, R. R., M. L.
1991. A distributional checklist of the freshwater union-
ids (Bivalvia: Unionoidea) of Kentucky. Am. Malacol.
Bull. 8:113-129.
Clarke, A. H. 1981. The tribe Alasmidontini
Anodontinae), Part I; Pegias, Alasmidonta,
dens. Smithson. Contrib. Zool. 326:1—101.
Gordon, M. E. 1991. Alasmidonta atropurpurea. Report
submitted to The Nature Conservancy, Arlington, VA.
Gordon, M. E. 1995. Anodontoides denigratus (Lea) (Biv-
alvia: Unionoida) from the upper Cumberland River
system. Report submitted to the U.S. Fish and Wildlife
Service, Asheville, NC
Gordon, M. E., and J. B. Layzer. 1989. Mussels (Bivalvia:
Unionoidea) of the Cumberland River: review of life
Warren Jr, and G. A. Schuster.
(Unionidae:
and Arci-
histories and ecological relationships. U.S. Fish and
Wildlife Service Biological Report 89(15).
Gordon, M. E., and J. B. Layzer. 1993. Glochidial host of
Alasmidonta atropurpurea (Bivalvia: Unionoidea,
Unionidae). Trans. Am. Microscop. Soc, 112:145-150.
Harker, D. F., Jr., S. M. Call, M. L. Warren, Jr., K. E.
Camburn, and P. Wigley. 1979. Aquatic biota and water
quality survey of the Appalachian Province, Eastern
Kentucky. Kentucky Nature Preserves Commission,
Tech. Rept., Frankfort, KY.
Harker, D. F., Jr., M. L. Warren, Jr., K. E. Cambum, S.
M. Call, G. J. Fallo, and P. Wigley. 1980. Aquatic biota
and water quality survey of the upper Cumberland Riy-
er basin. Kentucky Nature Preserves Commission,
Tech. Rept., Frankfort, KY.
Jenkins, R. E., E. A. Lachner, and F. J. Schwartz. 1971.
Fishes of central Appalachian drainages: their distri-
bution and dispersal. Pages 43-117 in P. C. Holt (ed).
The distributional history of the biota of the southern
Appalachians, Part II: vertebrates. Res. Div. Monogr.
4, Virginia Polytechnic Institute and State University,
Blacksburg, VA.
Jillson, W. R. 1927. Pollution of stream waters in Ken-
tucky. Kentucky Geological Survey, Frankfort, KY.
[KDOW] Kentucky Division of Water. 1996. 1996 Ken-
tucky report to congress on water quality. Kentucky Di-
vision of Water, Frankfort, KY.
[KDOW] Kentucky Division of Water. 1997. Guidelines
for developing a competitive nonpoint source project.
Kentucky Division of Water, Frankfort, KY.
[KDOW] Kentucky Division of Water. 1998. 303(d) list of
waters for Kentucky. Kentucky Division of Water,
Frankfort, KY.
[KSNPC] Kentucky State Nature Preserves Commission.
1996. Rare and extirpated plants and animals of Ken-
tucky. Trans. Kentucky Acad. Sci. 57:69-91.
Kuehne, R. A., and R. M. Bailey. 1961. Stream capture
and the distribution of the percid fish Etheostoma sag-
itta, with geologic and taxonomic considerations. Cop-
eia 1961:1—-5
Freshwater Mussels—Cicerello and Laudermilk
Layzer, J. B., and R. M. Anderson. 1992. Impacts of the
coal industry on rare and endangered aquatic organisms
of the upper Cumberland River basin. Final report sub-
mitted to Kentucky Dep. Fish Wildlife Resources,
Frankfort, KY and Tennessee Wildlife Resources Agen-
cy, Nashville, TN.
Lea, I. 1852. Descriptions of new species of the family
Unionidae. Trans. Am. Philos. Soc. 10:253-294.
Leist, D. W., F. Quinones, D. S. Mull, and M. Young.
1982. Hydrology of area 15, eastern coal province, Ken-
tucky and Tennessee. Water Resources Investigations
Open-File Report 81-809, Geological Survey, U.S. De-
partment of the Interior.
McGrain, P. 1966. Geology of the Cumberland Falls State
Park area. Kentucky Geological Survey Series X, Spec.
Pub. I. University of Kentucky, Lexington, KY.
[MSE] Mayes, Sudderth, and Etheredge, Incorporated.
1975. The river basin water quality management plan
for Kentucky—upper Cumberland River—303(e) plan.
Prepared for Division of Water, Frankfort, KY.
Miller, A. C., L. Rhodes, and R. Tippit. 1984. Changes in
the naiad fauna of the Cumberland River below Lake
Cumberland in central Kentucky. Nautilus 98:107—110.
Neel, J. K., and W. R. Allen. 1964. The mussel fauna of
the upper Cumberland basin before its impoundment.
Malacologia 1:427—459.
Ortmann, A. E. 1918. The nayads (freshwater mussels) of
the upper Tennessee drainage, with notes on synonymy
and distribution. Proc. Am. Philos. Soc. 57:521-626.
Ortmann, A. E. 1924. The naiad-fauna of the Duck River
in Tennessee. Am. Mid]. Naturalist 9:18—62.
Ruhl, K. J., and G. R. Martin. 1991. Low-flow character-
istics of Kentucky streams. Water Resources Investiga-
tions Report 91-4097. Geological Survey, U.S. Depart-
ment of the Interior.
Schuster, G. A., R. S. Butler, and D. H. Stansbery. 1989.
A survey of the unionids (Bivalvia: Unionidae) of Buck
Creek, Pulaski County, Kentucky. Trans. Kentucky
Acad. Sci. 50:79-85. %
Smith, P. W. 1965. A preliminary annotated list of the
lampreys and fishes of Illinois. Illinois Nat. Hist. Surv.
Biol. Notes 54:1—12.
Starnes, L. B., and A. E. Bogan. 1988. The mussels (Bi-
valvia: Unionidae) of Tennessee. Am. Malacol. Bull. 6:
19-37.
Turgeon, D. D., A. E. Bogan, E. V. Coan, W. K. Emerson,
W. G. Lyons, W. L. Pratt, C. F. E. Roper, A. Scheltema,
F. G. Thompson, and J. D. Williams. 1998. Common
and scientific names of aquatic invertebrates from the
United States and Canada: Mollusks. Am. Fish. Soc.
Spec. Publ. 16:1-277.
[USFWS] United States Fish and Wildlife Service. 1998.
Endangered and threatened wildlife and plants. De-
partment of the Interior, Washington, DC.
[USGS] United States Geological Survey. 1993. Water re-
sources data—Kentucky. Water year 1993. Data Report
KY-93-1, Louisville, KY.
Wilson, C. B., and H. W. Clark. 1914. The mussels of the
Cumberland River and its tributaries. United States
Fish Commission, U.S. Bureau of Fisheries Document
781:1-63.
APPENDIX A
Upper Cumberland River basin mussel col-
lection sites in southeastern Kentucky listed
by and within sub-basins from down- to up-
stream. Site numbers refer to numbers in Fig-
ure l.
CUMBERLAND RIVER MAINSTEM:
(1.) Just above Cumberland Falls. McCreary/
Whitley cos. 28 Apr, 10 Sep 1987; 14 Sep
1995. (2.) Between Cumberland Falls and
Ryans Branch. McCreary/Whitley cos. 30 Jul
1993. (3.) At Marsh Creek. McCreary/Whitley
Cos. 3 Jul, 10 Aug 1993. (4.) Between Buck
Shoals and Crow creeks. McCreary/Whitley
cos. 10 Aug 1993. (5.) At Summer Shoals.
Whitley Co. 29 Jul 1993. (6.) At Rough Shoals
Creek. Whitley Co. 27 Jul 1994. (7.) At Inter-
state 75. Whitley Co. 27 Jul 1994. (8.) KY 296
at Williamsburg. Whitley Co. 27 Jul 1994. (9.)
At Whetstone Creek. Whitley Co. 28 Jul 1994.
(10.) Ca. 1 km downstream from Big Indian
Creek. Knox Co. 30 Sep 1994. (11.) Ca. 1.9
km upstream from Stinking Creek. Knox Co.
14 Jul, 22 Sep 1993. (12.) At Pineville. Bell
Co. 5 Aug 1993. (13.) Ca. 1.6 km downstream
from KY 119. Bell Co. 2 Aug 1990; 29 Sep
1994. (14.) KY 1344 at Calvin. Bell Co. 10, 23
Sep 1993. (15.) At KY 987. Bell Co. 23 Sep
1993. (16.) At Minton Branch. Bell Co. 29 Jul
1994. (17.) At Fourmile Branch. Harlan Co. 8
Jun 1994. MARSH CREEK: (18.) Ca. 0.8 km
upstream from mouth. McCreary Co. 10 Aug
1994. (19.) Ca. 0.2 km downstream from
Brushy Creek. McCreary Co. 16 Aug 1989; 9,
18 Aug 1994. (20.) At Hens Nest Creek.
McCreary Co. 10 Aug 1994. (21.) Ca. 2.7 km
upstream from Hens Nest Creek. McCreary
Co. 11 Aug 1994. (22.) Ca. 3.3 km upstream
from Hens Nest Creek. McCreary Co. 11 Aug
1994. (23.) At trib. 3.6 km upstream from
Hens Nest Creek. McCreary Co. 10 Aug 1994.
(24.) At tributary ca. 1 km downstream from
KY 679. McCreary Co. 3 Aug 1994. (25.) At
KY 679. McCreary Co. 15 Aug 1989. (26.) At
tributary ca. 0.5 km downstream from KY 679.
McCreary Co. 3 Aug 1994. (27.) Ca. 0.4 km
upstream from KY 679. McCreary Co. 3 Aug
1994. (28.) Ca. 0.5 km downstream from Lau-
rel Creek. McCreary Co. 8 Aug 1994. (29.) Ca.
34 Journal of the Kentucky Academy of Science 62(1)
1 km downstream from Duck Run, McCreary
Co. 9 ‘ng 1994. (30.) Ca. 0.2 km downstream
fron: jaylor Branch. McCreary Co, 3 Aug
199-1. (31.) At KY 478. McCreary Co. 30 Aug
los7. (32.) Ca. 0.3 km upstream from KY 478.
McCreary Co. 11 Aug 1994. (33.) At Big
Branch. McCreary Co. 12 Aug 1994. -(34.)
Downstream from Kidd School Road Ford.
McCreary Co. 15 Aug 1989; 4 Aug 1994. (35.)
Ca. 0.3 km upstream from Kidd School Road
Ford. McCreary Co. 30 Aug 1987; 28 Apr
1993; 12 Jul 1994: 4, 17 Aug 1994. (36.) Ca.
0.5 km upstream from Kidd er Road
Ford. McCreary Co. 4, 17 Aug 1994. (37.) Ca.
0.7 km downstream from KY 1044. Morea
Co. 2, 12 Aug 1994. (38.) Ca. 0.2 km down-
stream from KY 1044. McCreary Co. 2 Aug
1994. (39.) At KY 1044. McCreary Co. 18 Jul
1989. (40.) Ca. 0.1 km upstream from KY
1044. McCreary Co. 2 Aug 1994. (41.) Ca. 0.2
km downstream from C eae Creek. McCreary
Co. 2 Aug 1994. JELLICO CREEK: (42.) Ca
4.4 km downstream from KY 92. Whitley Co.
6 Jul 1994. (43.) Ca. 2.0 km downstream from
KY 92. Whitley Co. 6 Jul 1994. (44.) Down-
stream from Shut-in Branch. McCreary Co. 12
May 1993. CLEAR FORK: (45.) At Tackett
Creek. Whitley Co. 7 Jul 1994. (46.) At Buck
Creek. Whitley Co. 7 Jul 1994. (47.) Laurel
Fork at TN border. Whitley Co. 27 Jul 1993;
21 Sep 1996. (48.) Laurel Fork ca. 0.4 km up-
stream from TN ce Whitley Co, 27 Jul
1993; 11 Jan 1994; 26 Sep 1996. (49.) Laurel
Fork ca. 0.7 km upstream from TN border,
Whitley Co, 27 Jul 1993. (50.) Laurel Fork ca.
0.9 km upstream from TN border. Whitley Co.
27 Jul 1993. (51.) Pine Creek at KY 190. Bell
Co. 28 ee 1999. PATTERSON CREEK:
(52.) Rose Creek ca. 0.2 km upstream from
sao: Creek. Whitley Co. 16 Jun, 15 Oct
1993; 22 May 1997. BIG INDIAN CREEK:
(53.) Demps Hollow ca. 1.3 km upstream
from Big Indian Creek. Knox Co. 21 Jul 1993,
20 May 1997. (54.) Mills Fork ca. 0.8 km up-
stream from Big Indian Creek. Knox Co, 21
Jul 1993, 21 May 1997. RICHLAND CREEK:
(55.) Billies Branch ca. 3.2 km upstream from
Richland Creek. Knox Co. 22 Jul 1993, 20
May 1997. STINKING CREEK: (56.) Moore
Creek ca. 10.5 km NW Pineville. Knox Co. 28
Jan 1993, 21 May 1997. POOR FORK: (57.)
0.6 km upstream from Middleton Branch.
Harlan Co. 24 May 1994.
J. Ky. Acad. Sci. 62(1):35-38. 2001.
Morphometric Variation of Cotton Mice (Peromyscus gossypinus) anc.
White-footed Mice (P. leucopus) in Kentucky
Nell A. Bekiares' and George A. Feldhamer
Department of Zoology, Mail Code 6501, Souther Illinois University, Carbondale, Illinois 62901-6501
ABSTRACT
We captured 151 white-footed mice (Peromycus leucopus) and 38 cotton mice (P. gossypinus) in Ballard
and Carlisle counties, Kentucky, during 3600 trap nights. There were significant differences between the
two species in body mass, hind foot length, condylobasal length, and length of the nasal bone for both adult
males and females. Morphological characteristics often used to differentiate the two species were not always
sufficient to do so accurately. Large white-footed mice may be misidentified as cotton mice.
INTRODUCTION
Cotton mice occur in southeastern United
States from eastern Texas and Oklahoma east
to Florida and north to Virginia (Jones and
Birney 1988). With regard to body size, the
largest of the three commonly recognized sub-
species, Peromyscus gossypinus megacephalus
(Rhoads 1894), is found at the northern pe-
riphery of the range. Cotton mice are uncom-
mon in Kentucky, Missouri (Hall 1981), and
the southernmost five counties of Illinois
(Feldhamer et al. 1998: Hoffmeister 1989).
The preferred habitat of cotton mice, “coin-
cident with the location of rivers, streams, and
other lowland areas” (McCarley 1963:787), in-
cludes swampy woodlands, bottomlands, low-
land forests, and sites near swamps, sloughs,
oxbow lakes, and areas with high water tables
(Goodpaster and Hoffmeister 1952; Laerm
and Boone 1994; Linzey et ak 1976; H.
McCarley 1954a, 1954b, 1963; W.H. Mc-
Carley 1964; Pournelle 1952). Woody debris is
used extensively (McCay 2000).
Cotton mice are sympatric throughout
much of their range with white-footed mice
(P. leucopus). The two species presumably di-
verged recently (Hooper 1968) and can be dif-
ficult to distinguish in the field. The purpose
of our study was to compare morphometric
characteristics of cotton mice from western
Kentucky, where the species is considered to
be threatened, with sympatric white-footed
mice.
! Present address: 7 East Lakeshore Drive #23, Cincin-
nati, OH 45237.
35
METHODS
Live trapping occurred from August 1998
through April 1999. Twelve sites were selected
in Ballard and Carlisle counties, Kentucky
(Bekiares 2000). Two Sherman live traps were
set at each station, with stations established 10
m apart along a 500-m transect. Traps were
set at two sites each week and checked be-
tween 0600 and 1000. Traps were set close to
fallen logs, brush piles, stumps, pond edges,
tree trunks, and on floating debris whenever
possible to optimize trap success for P. gos-
sypinus. Traps were baited with cracked corn
and sunflower seeds and were set for three
consecutive nights at each site, for a total of
300 trap nights per site. During summer, traps
exposed to sunlight were covered with leaves
to decrease the amount of heat absorbed by
the trap prior to checking. During cold tem-
peratures, traps contained polyester fiberfill
bedding material.
The sex, age class (juvenile or adult, deter-
mined by pelage color), and wet body mass
(nearest g) of captured animals were recorded.
Tchednels were then checked for a previous
capture mark. If the animal was new, a hind
foot measurement (mm) was taken. New cap-
tures were marked with a green permanent
marker along the ventral surface (Schmid
1998). Marks could be observed for the du-
ration of the three trap nights at each site.
Because P. leucopus and P. gossypinus are
morphologically similar and difficult to distin-
guish in the field, initial size criteria of Hoff-
pent (1977, 1989) were used to separate
the species. Individuals with hind foot length
=22 mm or body mass =26 ¢ were tentativ ely
identified as PB. gossypinus. These animals
36 Journal of the Kentucky Academy of Science 62(1)
were © thanized using cervical dislocation,
placed on ice, and returned to the laboratory.
Allovyme analyses (Bekiares 2000) were used
to confirm species identification of animals
ollected. Other rodents, birds, and reptiles of
ion-interest were released at the capture site.
For animals removed from the field, stan-
dard external measurements (in mm) were
made prior to dissection: total body length, a
length, ear length, and hind foot length. In
addition, wet body mass (g) was re ae da
second time using a triple- beam balance.
Measurements (mm) of cleaned skulls includ-
ed condylobasal length, length of the nasal
bone, and le ngth of Te maxillary toothrow.
The computer program Statview was used
to compute unpaired t-tests for comparisons
of means, Z-tests for comparisons of propor-
tions, and general descriptive statistics. Statis-
tical tests were considered significant at a =
0.01.
RESULTS
During 3600 trap nights we captured 197
fadividueales 151 white-footed mice, 38 cotton
mice, three rice rats (Oryzomys palustris), one
Eastern chipmunk (Tamias striatus), and four
leopard frogs (Rana sphenocephala). Seven of
the P. leucopus were believed to be P. gossy-
pinus upon capture and were removed from
the field.
Only data from adults were used in mor-
phological analyses because of the differences
in juvenile sizes. Another consideration is that
females collected in late summer and autumn
may be pregnant. We collected only six preg-
nant females and chose to remove them from
analyses. As expected, adult P. leucopus were
significantly smaller than P. gossypinus for
four of the eight measurements examined. For
males, P. leucopus were significantly smaller
than P gossypinus in body mass, hind foot
length, con lobasal length, and nasal length
(Table 1 Female P leucopus were eaiilier:
than ee P. gossypinus for the same four
measurements.
DISCUSSION
Most of the mean values for morphological
characteristics of white-footed mice in our
study represent a biased sample. Only those P.
leucopus tentatively identified as P. gossypinus
in the field were used for all measurements
and represented the largest individuals. Only
the hind foot and body mass measurements
represent an unbiased sample because data
were obtained on all animals captured in the
field, not just those presumed to be P. gossy-
pinus. We expect that the other four charac-
teristics measured (total length, tail length, ear
length, and maxillary toothrow length) also
would be significantly smaller in an unbiased
sample of P le UCOPUS.
Cotton mice in this study were significantly
larger than six specimens reported from
Horseshoe Lake Conservation Area, Alexan-
der County, Illinois (Feldhamer et al. 1998).
It is possible that the Ilinois specimens were
large P. leucopus misidentified as P. gossypi-
nus. More likely, we suspect they may have
been hybrids between the two species. Bar-
bour and Davis (1974) suggested hybrid cot-
ton mice occurred in Kentucky. Other inves-
tigators have also noted hybridization between
the two species (Lovecky et al. 1979: Mc-
Carley 1954b; St. Romain 1976; although see
Bradshaw 1968), with hybrids exhibiting inter-
mediate-sized mor hological characters.
Boone (1995) analyzed morphometric data
for cotton mice from throughout their range.
Using only adults, we compared his data to
our data from Kentucky. For all morphological
traits considered in both studies, Kentucky
specimens, from the periphery of the range,
were significantly larger (P < 0.01; see Beki-
ares 2000). This is consistent with the clinal
size relationship noted by Boone (1995) for
cotton mice throughout their range.
Hoffmeister (1977, 1989) created a scatter-
gram based on morphological characters to
distinguish between cotton mice and white-
footed mice. He used hind foot length X nasal
bone length on the x-axis, and condylobasal
length X maxillary toothrow length on the y-
axis. Measurements of cotton mice group to
the right of a line running approximately
through (0, 134) and (275, 0). In our study,
specimens “on the line” were white-footed
mice, based on allozyme data (Bekiares 2000).
Use of morphological measurements may
need to be more conservative for differenti-
ating white-footed mice and cotton mice on
the periphery of their range in Kentucky, Il-
linois, and Missouri. That is, “questionable”
specimens on or near the right side of the de-
Cotton Mice and White-footed Mice—Bekiares and Feldhamer
Table 1. Differences (t-test; * = P < 0.01) in mean values of morphological characteristics between specimens o
adult Peromyscus gossypinus and P. leucopus from Ballard and Carlisle counties, Kentucky, — collected between Augus
1998 and April 1999. Variation is reported as standard error.
Characteristic P. gossypinus
Male body mass (g) 30.97 + 1.20
n= 17
Female body mass (g) 33.18 + 1.04
n = 2)
Male total length 170.82 + 3.61
n= 17
Female total length WOSy = lll
n= 21
Male tail length TA 47 + 2.53
m= i
Female tail length 77.90 = 1.03
n = 21
Male hind foot length WOT 22 O27
m = If
Female hind foot length 92.81 = 0.20
n= 21
Male ear length 18.76 = 0.31
n= 17
Female ear length 18.86 = 0.51
n= 21
Male condylobasal length 98.05 = 0.27
n=17
Female condylobasal length 98.39 + 0.14
n= 21
Male nasal length 11.41 + 0.21
n= 17
Female nasal length 11.22 + 0.16
n = 21]
Male maxillary toothrow 3.94 + 0.08
n= 17
Female maxillary toothrow 3.98 + 0.06
n= 21
P. leucopus T., value
22.95 + 0.45 7.65*
n= 057
24.69 + 1.01 = 5 (a2
im = 3
159.00 + 5.21 1.49
n=4
174.00 += 7.77 1.42
n=3
66.25 + 206 1.52
n= 4
82.67 += 5.04 —1.48
ne
17.62 + 0.27 8.98*
n = 68
18.01 = 0.33 —9.34*
n = 30
18.00 + 0.41 1.14
n=4
17.00 + 3.06 1.09
n=3
25.56 + 0.59 4.00*
n=4
927.03 + 0.55 3.34%
n=3
9.61 + 0.28 3.99*
n=4
10.03 = 0.21 2.75
n=3
3.77 = 0.19 0.93
n=4
3.73 + 0.02 1.62
n=3
I
marcation line of Hoffmeister (1977, 1989)
should be considered P. leucopus,
ACKNOWLEDGMENTS
We thank D. Kevin Davie of the SIUC
Morris Library GIS lab, and Valerie Barko and
Dr. J. Scheibe for assistance in the field. This
paper represents a portion of a thesis submit-
ted by N. Bekiares for the degree of Master
of Science in the Zoology Department at
Southern Illinois University at Carbondale.
LITERATURE CITED
Barbour, R. W., and W. H. Davis. 1974. Mammals of Ken-
tucky. Univ. Kentucky Press, Lexington, KY.
Bekiares, N. 2000. Morphometric and allozyme variation
in the cotton mouse (Peromyscus gossypinus) in south-
em Illinois, southwestern Kentucky, and southeastern
Missouri. M.S. Thesis. Southern Illinois Univ., Carbon-
dale, IL.
Boone, J. L. 1995. Morphological and genetic variation in
the cotton mouse (Peromyscus gossypinus ): implications
for population genetics, systematics, and conservation.
Ph.D. Dissertation. Univ. Georgia, Athens, GA.
Bradshaw, W. N. 1968. Progeny from experimental mating
tests with mice of the Peromyscus leucopus species
group. J. Mammal. 49:475-480.
Feldhamer, G. A., J. C. Whittaker, and E. M. Charles.
1998. Recent records of the cotton mouse (Peromyscus
gossypinus) in Illinois. Am. Midl. Naturalist 139:17S—
180.
Goodpaster, W. W., and D. F. Hoffmeister. 1952. Notes
on the mammals of western Tennessee. J. Mammal. 33:
362-371.
Hall, E. R. 1981. The mammals of North America, 2nd
ed. John Wiley and Sons, New York, NY. [2:601—-1175}
Hoffmeister, D. F. 1977. Status of the cotton mouse, Per-
omyscus gossypinus, in southern Illinois. Am. Midl.
Naturalist 97:222—224.
Hoffmeister, D. F. 1989. Mammals of Illinois. Univ. Illi-
nois Press, Urbana, IL.
38 Journal of the Kentucky Academy of Science 62(1)
Hooper. |. T. 1968. Classification. Pages 27-74 in J. A.
Kins d). Biology of Peromyscus (Rodentia). Spec.
Publ. Am. Soc. Mammal. 2.
Jones, J. K., Jr, and E. C. Bimey. 1988. Handbook of the
unmals of the north-central states. Univ. Minnesota
Press, Minneapolis, MN.
iaverm, J., and J. L. Boone. 1994, Mensural discrimination
of four species of Peromyscus (Rodentia: Muridae) in
the southeasterm United States. Brimleyana 21:107—
123.
Linzey, A. V., D. W. Linzey, and S. E. Perkins, Jr. 1976.
The Peromyscus leucopus group in Alabama, J. Alabama
Acad. Sci. 47:109-113.
Lovecky, D. V., D. Q. Estep, and D. A. Dewsbury. 1979.
Copulatory behaviour of cotton mice (Peromyscus gos-
sypinus) and their reciprocal hybrids with white-footed
mice (P. leucopus). Anim. Behay, 27:371-375.
McCarley, H. 1954a. The ecological distribution of the
Peromyscus leucopus species group in eastern Texas.
McCarley, H. 1954b. Natural hybridization in the Pero-
myscus leucopus species group of mice. Evolution 8:
314-323.
McCarley, H. 1963. Distributional relationships of sym-
patric populations of Peromyscus leucopus and Pero-
myscus gossypinus. Ecology 44:784-788.
McCarley, W. H. 1964. Ethological isolation in the ceno-
species Peromyscus leucopus. Evolution 18:331—342.
McCay, T. S$. 2000. Use of woody debris by cotton mice
(Peromyscus gossypinus) in a southeastern pine forest.
J. Mammal. $1:527-535.
Pournelle, G. H. 1952. Reproduction and early post-natal
development of the cotton mouse, Peromyscus gossy-
pinus gossypinus. J. Mammal. 33:1-20.
Rhoads, S$. N. 1894. Descriptions of four new species and
two new subspecies of white-footed mouse from the
United States and British Columbia. Proc. Acad. Nat.
Sci. Philadelphia 46:253-261.
Schmid, $. 1998. The impact of patch characteristics on
small mammal fauna: Peromyscus leucopus and associ-
ated species in previously cut forest patches. Ph.D. Dis-
sertation. Southern Illinois Univ., Carbondale, IL.
St. Romain, P. A. 1976. Variation in the cotton mouse
(Peromyscus gossypinus) in Louisiana. Southwest. Nat-
uralist 52:290-300.
J. Ky. Acad. Sci. 62(1):39-51. 2001.
Woody Plants of Six Northern Kentucky Counties
Ross C. Clark
Department of Biological Sciences, Eastern Kentucky University, Richmond, Kentucky 40475
and
Ryan M. Bauer
Department of Computer Information Science, Eastern Kentucky University, Richmond, Kentucky 40475
ABSTRACT
Our field work and herbarium surveys have documented the woody flora of Bracken, Fleming, Harrison,
Mason, Nicholas, and Robertson counties, Kentucky. The presently known woody flora consists of 172 taxa;
11% of the woody flora is exotic. We report Thuja orientalis L. for the first time as an introduced member
of Kentucky's flora. There is a significant discontinuity of distribution between the northern Bluegrass and
Knobs regions. Arundinaria gigantea is a much rarer plant in northern Kentucky than conventional wisdom
indicates. We include an annotated listing of woody plant taxa and a discussion of the state of natural habitats
and potential impact of weedy woody species.
INTRODUCTION
Narratives related to the natural features of
Kentucky have typically attested to an abun-
dance and variety of natural resources. A re-
cent, statewide assessment of biodiversity in
Kentucky (Taylor 1995) convincingly argues
that plant diversity in the state is substantial.
However, in spite of recent attempts to esti-
mate vascular plant diversity in Kentucky
(Browne and Athey 1992; Medley 1993), suf-
ficient information is not yet available for an
accurate estimate of which vascular plant taxa
actually occur in the state. Contributing rea-
sons for this situation include repeated anec-
dotal and unvouchered reports of occurrences
and a general paucity of vouchered collections
in institutional herbaria (Jones et al. 1995).
However, the situation we find ourselves in
is beside the point. The point is, too little is
known about the flora of Kentucky, land use
trends are continually shrinking and modifying
native habitats, and we are at risk of losing
elements of the flora before we discover the
full extent of its diversity and distribution.
There is an urgent need for more thorough
documentation of the flora of Kentucky.
SCOPE AND JUSTIFICATION OF
THIS STUDY
Our study was undertaken to document the
occurrence of woody plants that are native,
naturalized, or spreading from cultivation in
39
six counties of northern Kentucky: Bracken,
Fleming, Harrison, Mason, Nicholas, and
Robertson. Our goal was to document the
woody plant diversity in these counties at
greater than the 90% level.
One of the reasons this region was selected
for study is because it is not well known bo-
tanically. Guetig (1993) compiled a summary
of all floristic work previously done in Ken-
tucky. His summary indicated that none of the
counties included in the present study has
ever been the subject of an organized effort
to document the flora. Also, we felt that thor-
ough vouchering of the woody plants of these
counties would make subsequent field work to
voucher the herbaceous vascular plants easier.
(The logistics of field collecting are simpler
when one is not continually searching for all
sizes of plants.) In addition, woody plants were
selected as the focus of our study because they
are keystone organisms in forest and savanna
ecosystems and have considerable economic
significance. We felt that documenting the oc-
currence of this portion of the flora would be
a connection to Kentucky's heritage that peo-
ple would be more likely to appreciate. Final-
ly, most of this area of the state is typified by
an advanced state of habitat elimination and
modification. Consequently, we concluded
that, if efforts to document the flora were de-
layed much longer, significant elements of the
woody flora could possibly be lost entirely.
40 Journal of the Kentucky
THE STUDY AREA
A’ of the counties lie within the drainage
of Licking River, except for the northern
Mason and Bracken counties,
hich are drained by creeks downcutting di-
‘ctly to the Ohio River. The six county study
totals almost 1700 mi2 (438,000 ha).
which is almost 4.3% of the land area of Ken-
tucky (Anonymous 2000a).
Elevations within the study area range from
about 500 ft. (152 m) above mean sea level
near Meldahl Dam on the Ohio River in
northwestern Bracken County, to about 1200
ft. (370 m) above sea level in extreme eastern
Fleming County. The maximal elevation at-
tained in the Bluegrass part of our study area
is about 1000 ft. (305 m), in extreme south-
western Harrison, near Leesburg (U.S. Geo-
logical Survey 1976, 1978).
All of the study area except eastern Fleming
tions of
ea
County lies within the Bluegrass Region of
Kentucky. The Bluegrass is atdertain by Or-
dovician strata. Main geologic formations in-
clude Lexington Limestone where exposed by
downcutting of main tributaries of the w estern
and northern Licking River, with Garrard Silt-
stone and the Clays Ferry Formation com-
prising most of the rolling uplands of the west-
em part of the study area. Proceeding east-
ward from the former exposures, one encoun-
ters relatively narrow outcropping belts of the
(Ordovician) Bull Fork Formation, Drakes
Formation, and Crab Orchard Formation
(both of these Silurian and marking the tran-
sition between Knobs and Bluegrass), and fi-
nally, Devonian and Mississippian strata of the
extreme western edge of the Mississippian
Plateau. (McDowell et al. 1981) Only extreme
eastern Fleming County is within the physio-
graphic province known as The Knobs, char-
een’ (sequentially as one goes eastward)
by outcropping Silurian, Devonian, and Mis-
sissippian rocks. The Knobs are interpreted as
the dissected remnant of the Mississippian
(Interior Low Plateau) Province, known pa-
rochially in Kentucky as the Pennyrile Plateau
(Fenneman 1938: Karan and Mather 1977).
Except over heavily organic Ohio shale in the
Knobs, most upland sails of our study region
have an alkaline pH.
Estimates of the original vegetation in this
region vary and are stall debated, possibly be-
Academy of Science 62(1)
cause originally there was a complex mosaic
from hich fire has now been systematically
excluded for 200 years. It may have included
a preponderance of ash-oak-prairie savanna in
the Inner Bluegrass and various facies of oak-
chestnut and mixed mesophytic on the Knobs
(Braun 1950; Bryant 1987; Campbell 1980;
Kiichler 1964; Martin et al. 1978).
MATERIALS AND METHODS
Prior to field collecting, each county was
surveyed to determine areas which might yield
more habitat diversity. Because of the relative
lack of geologic div ersity in most of the study
area, this surve y relied on physiographic maps
and county road maps (Anonymous 1997;
Puetz n.d.; U.S. Geological Survey 1976,
1978). By this method, we were able to iden-
tify circumstances with a high likelihood of
giving us efficient and repeated coverage of
major habitats within each county.
About two field collecting days were spent
in each county. Field work began on 7 Jun
1999 and ended 20 Jul 1999. Specimens were
collected wherever we found them first, from
roadsides and ruderal habitats to reasonably
intact habitats. Specimens were temporarily
held in wet newspaper within large polyeth-
ylene bags and later accessioned by collector,
pressed, dried, labeled, and determined to tax-
on. The senior author determined the taxa of
most specimens without consulting additional
sources, except to verify nomenclatural au-
thorship. The field work required 2441 miles
of travel, an average of about 3 miles (4.8 km)
for each taxon Bollecred!
Nomenclature in this report is generally ac-
cording to Gleason and Cronquist (1991),
which also was a source consulted for deter-
mination of some groups. The International
Plant Name Index (Anonymous 2000b) and
Rehder (1940) were consulted in a few cases,
and we used Fernald (1950) as an aid to the
determination specimens of specimens of Cra-
taegus and Rubus.
Following processing and determination of
our field Bollesnons herbarium collections at
EKY, UKY, MDKY, and KNK were surveyed
to see if additional taxa had been vouchered
in these counties by other collectors. These
surveys yielded a few (<1%) additional re-
cords. Travel to herbaria required 3 additional
work days and about 500 miles (800 km) of
Woody Plants—Clark and Bauer Al
Table 1.
Bracken Fleming
Area!? 495! 351!
Total number of taxa 109 140
Number of native taxa 92, 124
Number of non-native taxa 15 16
% Non-native
Human density/mi? !
‘in sq. mi.
? Source: Anonymous 2000.
additional travel. See Table 1 for statistical flo-
ristic data.
RESULTS
The field effort resulted in more than 760
collections from the study area. Our subse-
quent regional herbarium survey yielded a few
additional records. Overall, this study resulted
in the documentation of 172 woody taxa from
the six-county area. Fleming County, with 140
documented taxa, has the most diverse woody
flora. Robertson County, with 97 documented
taxa, has the least diverse woody flora (Table
1). Information from the Internet is cited here
in accordance with the standard proposed by
Walker (1995).
ANNOTATED VOUCHERS OF THE
WOODY FLORA
Below is a list of vouchers for the woody
plants of the six-county study area, followed
by citations of voucher specimens and a short
comment on the pattern of occurrence. To
save space, names of counties of origin of
voucher specimens (Bracken, Fléming, Har-
rison, Mason, Nicholas, Robertson) are abbre-
viated to first letter in parentheses after
voucher numbers. When only a number is list-
ed, it is the accession number of the senior
author and the specimen has been deposited
in EKY. Vouchers from other Kentucky work-
ers are more completely cited. Nomenclature
generally follows Gleason and Cronquist
(1991), but in the final analysis reflects the
judgment of the senior author. Abbreviations
for herbaria are from Holmgren and Holm-
gren (2000).
Little (1971, 1977) included some addition-
al distributional data for a few taxa within our
study area. Presumably, the vouchers on which
some of his data are based are in herbaria not
consulted during this study. Therefore, his
Comparative woody plant diversity data for six northern Kentucky counties.
Harrison Mason Nicholas Robertson Totals
309! QA)} 196! 100! 1692!
110 100 96 97 2,
95 82 78 §3 142
15 18 18 14 19
13.6 18.0 18.9 14.4 11
52.6 40 34.3 22.2,
vouchers are not referenced here. We conser-
vatively estimate that the specimens collected
during our study constitute more than 95% of
the data now extant for woody plants in this
six-county area of Kentucky.
PINOPHYTA
Cupressaceae
Juniperus virginiana L.—24915 (B), 25273
(a), Daley (aD), Dele TOM ie Wiallse! (i)
25038 (R). Common throughout. This is ap-
parently the only gymnosperm native in the
Bluegrass.
Thuja orientalis L.—25057 (R). Mature off-
spring from nearby cultivated plants are es-
tablished in a fencerow. Introduced; This is
apparently the first report of plants of this
taxon escaping in Kentucky (Brown and
Athey 1992; Medley 1993).
Pinaceae
Pinus echinata Miller—25244 (F). Occasional,
Knobs.
Pinus rigida Miller—25227 (F). Frequent,
Knobs.
Pinus virginiana Miller—25275 (F). Common,
Knobs.
ANTHOPHYTA
Aceraceae
Acer negundo L.—24869 (B), 25282 (F),
94628 (H), 24788 (M), 25147 (N), 25011
(R). Common throughout.
Acer nigrum Michaux f—24957 (B), 25322
(F), 24611 (H), 24799 (M), 25091 (N),
25024 (R). Mesic woods, usually on north-
and east-facing slopes or in alluvium along
streams.
Acer rubrum L.—25310 (F). Frequent in var-
ious habitats, Knobs.
42 Journal of the Kentucky Academy of Science 62(1)
Acer saccharinum L.—24956 (B), 25342 (F),
94606 (H), 24770 (M), 25136 (N), 24964
(i). Frequent; low ground along streams
nd terraces.
er saccharum Marshall—24901 (B), 25232
F), 24651 (H), 24796 (M). 25128 (N).
25020 (R). Frequent; various upland habi-
tats.
Anacardiaceae
Rhus aromatica L.—25327 (F), 24613 (H).
Xeric blufftops; rare.
Rhus copallina L.—25277 (F), 24648 (H),
25077 (R). Disturbed rights-of-way; rare.
Rhus glabra L.—24912 (B), 25271 (F), 24644
(H), 24831 (M), 25123 (N), 25029 (R). Var-
ious habitats, most common in fencerows.
Rhus typhina L.—24832 (B), 24774 (M). Me-
sic woods and low ground; infrequent; con-
fined to habitats near the Ohio River.
Toxicodendron radicans (L.) Kuntze—24946
(B), 25281(F), 24597 (H), 24756 (M), 25151
(N), 25079 (R).Various habitats; common.
Toxicodendron pubescens Miller—24874 (B),
24707 (H). Xeric woods: rare.
Annonaceae
Asimina triloba (L.) Dunal—24889 (B), 25313
(F), 24646 (H), 24758 (M), 25139 (N),
24990 (R). Various mesic and alluvial habi-
tats; frequent.
Apocynaceae
Vinca minor L.—25218 (F), 25047 (H), 24802
(M), 25047 (R). Introduced: ruderal habi-
tats and dump sites; infrequent.
Araliaceae
Aralia spinosa L.—25286 (F). Mesic and al-
luvial habitats: Knobs.
Hedera helix L.—24850 (B).
dump site; rare.
Introduced:
Berberidaceae
Berberis thunbergii DC.—24867 (B), 25048
(H), 25094 (N), 25048 (R). Introduced. Var-
ious disturbed and degraded habitats; infre-
quent.
Betulaceae
Alnus serrulata (Aiton) Willd.—Thieret s.n..
30 Jan 1983 (KNK) (B), 25235 (F), 24807
(M). Streambanks and low, open ground; in-
frequent; apparently absent from Bluegrass.
Betula nigra L.—25338 (F). Alluvial woods,
rare; Knobs.
Carpinus caroliniana Walter—24924 (B),
25307 (F), 24701 (H), 24754 (M), 25095
(N), 24991 (R). Various habitats, usually
mesic: frequent to occasional.
Corylus americana Walter—24879 (B), 25289
(F), 24694 (H), 25025 (R). Bluffs and mesic
habitats; infrequent.
Ostrya virginiana (Miller) K. Koch—24909
(B), 25203 (F), 24617 (HA). 24746 etre:
25096 (N): common.
Bignoniaceae
Bignonia capreolata L.—25324 (F), 24619
(H), 25025 (R). South- and west-facing
bluffs along major streams; rare, but locally
common.
Campsis radicans (L.) Seemann—24897 (B),
25241 (F), 24653 (H), 24798 (M), 25146
(N), 25015 (R). Most habitats; common.
Catalpa bignonioides Walter—24837 (M),
25132 (N). Low woods, rare. In spite of its
common name (southern catalpa), this spe-
cies appears to be native along the Ohio
River in the study area. However, both this
species and the following one are cultivated
and can be expected to produce adventive
plants.
Catalpa speciosa Warder—24586 (H). An ap-
parent escape from cultivation; Cynthiana.
Caesalpiniaceae
Cercis canadensis L.—24903 (B), 25255 (F),
24681 (H), 24767 (M), 25170 (N), 25039
(R). Various habitats; common throughout.
Gleditsia triacanthos L—24917 (B), 25207
(F), 24661 (H),. 24755 (M), 325145 CK
25002 (R). Various habitats; common
throughout.
Gymnocladus dioica (L.) K. Koch—24836 (B),
24332 (F), 24624 (H), 24721 (M), 25160
(N), 25073 (R). Disturbed habitats and me-
sic woods; infrequent.
Caprifoliaceae
Lonicera japonica Thaunberg—24098 (B),
25314 (F), 25052 (Hl), 253580 (Mi)s aailian
(N), 25054 (R). Introduced; most habitats;
common.
Lonicera maackii (Rupr.) Herder—24940 (B),
Woody Plants—Clark and Bauer AS
95251 (F), 24632 (H), 24772 (M), 25166
(N), 24976 (R). Introduced; most habitats;
common in counties bordering the Ohio
River. In our opinion, this is one of the po-
tentially most ecologically disastrous terres-
trial plants ever introduced into eastern
North America. It eliminates or severely in-
hibits the reproduction of most native East-
ern Deciduous Forest plants.
Sambucus canadensis L.—24833 (B), 25252
(F), 24695 (H), 24778 (M), 25174 (N),
24969 (R). Stream corridors, low ground,
and mesic woods; common.
Symphoricarpos orbiculatus Moench—24885
(B), 25215 (F), 24664 (H), 24810 (M),
95116 (N), 25033 (R). Various habitats; fre-
quent.
Viburnum acerifolium L.—25309 (F). Decid-
uous woods; Knobs.
Viburnum prunifolium L.—24937 (B), 25221
(Eee 5051 (Eee 24747, (MD) 251020) (IN),
25058 (R). Upland woods, blufftops, fence-
rows, and disturbed habitats; frequent.
Viburnum rufidulum Raf—24894 (B), 25336
(F), 24682 (H), 24764 (M), 25124 (N),
25036 (R). Upland woods and disturbed
habitats; frequent.
Celastraceae
Celastrus scandens 1..—24914 (B), 25315 (F),
24671 (H), 24829 (M), 25140 (N), 25037
(R). Upland and mesic woods and disturbed
habitats; common.
Celastrus orbiculatus Thunberg—25339 (F),
25104 (N). Introduced; ruderal habitats and
rights-of-way. Presently uncommon in the
study area and often confused with plants
of the preceding taxon. In our area, this spe-
cies may have the potential of eclipsing
most other introduced woody plants in its
eventual negative ecological impact.
Euonymus alatus (Thunberg) Siebold—25193
(N). Introduced; fencerow; rare, but with
the potential of becoming much more com-
mon.
Euonymus atropurpureus Jacquin—24873
(B), 25206 (F), 24670 (H), 24750 (M),
25153 (N), 24992 (R). Upland woods and
disturbed habitats, common in fencerows;
frequent.
Euonymus fortunei (Turez.) Hand.-Maz.—
24852 (B); 25049 (H), 24777 (M), 25109
(N), 25049 (R). Introduced; old dump sites
and also establishing adventively (spread |
birds). Not yet common in the study area
but soon will be. When fully established.
supplants the entire herbaceous stratum of
deciduous forest.
Clusiaceae
Hypericum stragulum Adams and Robson
(= Ascyrum hypericoides var. multicaule of
some authors)—25276 (F). Other woody
hypericums in Kentucky apparently are ab-
sent from the study area; Knobs only.
Cornaceae
Cornus amomum Miller var. schuetzeana
(Meyer) Rickett—24839 (B), 25234 (F),
24809 (M). During this study, located only
on the banks of the Ohio River and in Big
Run Swamp, Fleming County.
Cornus drummondii C.A. Meyer—24878 (B),
25329 (F), 24643 (H), 25100 (N), 25001(R).
Xeric woods, disturbed habitats, and fence-
rows; common.
Cornus florida L.—24890 (B), 25292 (F),
24703 (H), 24739 (M), 25090 (N), 25023
(R). Mesic woods and bluffs; widespread
but nowhere common; being decimated by
fungal pathogens (Harlow et al. 1996).
Nyssa sylvatica Marshall—25299 (F), 24636
(H), 24830 (M), 25068 (R). Mesic woods;
occasional to rare in study area, except for
Knobs of Fleming County.
Nyssa sylvatica Marshall var. biflora (Walter)
Sargent—25226 (F). Rare; Big Run Swamp.
Ebenaceae
Diospyros virginiana L.—24921 (B), 25262
(F), 24600 (H), 24732 (M), 25129 (N),
25006 (R). Frequent in fencerows; also
widespread but not common in mesic
woods.
Elaeagnaceae
Elaeagnus umbellata Thunberg—25250 (F),
94702, (H), 24791 (M), 25107 (N), 24972
(R). Introduced; disturbed habitats: infre-
quent.
Ericaceae
Gaylussacia baccata (Wangenh.) K. Koch—
Meijer, Setser, and Meade 1150 = MDKY
#4630 (F). Xeric woods, infrequent; Knobs.
44 Journal of the Kentucky Academy of Science 62(1)
Kalmia latifolia L.—25
rare: Knobs.
Oxydendrum arboreum (L.) DC.—25303 (F).
| pland woods; Knobs.
345 (F). Upland woods,
95344 (F).
land Wane fifequcnt ‘Kuobs only.
Vaccinium pallidum Aiton—25270 (F). Same
habitats and localities as Gaylussacia bac-
cata.
Vaccinium stamineum L.—25266 (F
woods, frequent; Knobs only.
Up-
Upland
Fabaceae
Amorpha fruticosa L.—24841 (B), 24808 (M).
In our study area, apparently confined to
the banks of the Ohio River.
Lespedeza bicolor Turez.—25205 (F), 25186
(N). Introduced; escaping from plantings in
state-managed wildlife management areas.
94920 (B), 25295
(F). 24633 (Hi 24781. (M), 25172. (N).
25080 (R). Very common in varied habitats
and disturbed areas.
Fagaceae
Castanea mollissima Blume—W. Meijer, 15
Sep 1974, UKY #35813 (F). Introduced.
Fagus grandifolia Ehrhart—24854 (B), 25230
(F), 25089 (N), 25013 (R). Ravines and me-
sic slopes; rare in Bluegrass, common only
in Knobs.
Quercus alba L.—24899 (B), 25311 (F),
94660 (H), 24713 (M), 25110 (N), 25004
(R). Mesic woods; common throughout.
Quercus bicolor Willd.—25201 (F). Upland
swamp, rare; Knobs.
Quercus coccinea Muenchh.—24856 (B),
25265 (F). Extremely rare in Bluegrass; we
discovered a population of only two mature
trees in a pasture fencerow in Bracken
County and noted no reproduction. Very
common in xeric and submesic woods in the
Knobs.
Quercus imbricaria Michaux—24934 (B);
25229 (F): 24588 (H), 24820 (M), 25177
(N), 24966 (R). Widespread but rare
throughout our study area.
Quercus macrocarpa Michaux—25320 (F),
24623 (H), 24823 (M), 25162 (N), 25056
(R). Frequent in the south but progressively
more rare northward in the area we studied.
Quercus montana Willd. (
some authors )—25287 (F). Xeric south- and
=Q. prinus L. of
west-facing slopes and ridges; frequent in
Knobs. The type of Q. prinus in the Lin-
naean herbarium may be of the lowland
chestnut oak (=Q. michauxii Nuttall) in-
stead of the upland chestnut oak, and the
two names have been confused in the lit-
erature for many years (Hardin 1979). Since
QO. michauxii and QO. montana, respectively,
are unambiguous names, it is better to use
them instead.
Quercus muhlenbergii Engelm.—24880 (B),
95195 (F), 24656 (H), 24757 (M), 25143
(N), 25041 (R). Upland habitats throughout;
frequent.
Quercus palustris Muenchh.—24947 (B),
95258 (F), 24698 (H), 24789 (M), 25106
(N). Frequent only along the Ohio River
and in Fleming County upland swamps;
otherwise sporadic and occasionally escap-
ing from cultivation.
Quercus rubra L.—24906 (B), 25288 (F),
24696 (H), 25102 (N), 24986 (R). Mesic up-
lands, usually on east- and north-facing
slopes; occasional to rare.
Quercus shumardii Buckley—24870 (B),
95294 (F), 24631) (Bl) °24734( Miao
(N), 25012 (R). Various habitats; common.
Quercus stellata Wangenh.—24871 (B), 25264
(F), 24666 (H), 24825 (M), 24977 (R). Up-
land woods and fencerows; occasional.
Quercus velutina Lamarck—24910 (B), 25278
(F). 24649 (EH), 247116 (Mi) 2a:
25069 (R). Upland woods; frequent.
Quercus Xwilldenowiana Zabel—24692 (H).
A hybrid, found in a fencerow, between Q.
velutina Lam. and Q. falcata Michaux. We
were unable to find the latter parent in the
vicinity; however, considering the advanced
state of habitat loss, it easily could have for-
merly occurred nearby.
Grossulariaceae
Ribes missouriense Nuttall ex Torrey and
Gray—25357 (N). Canebrake, rare.
Hamamelidaceae
Hamamelis virginiana L.—25294 (F). Various
wooded habitats; Knobs.
Liquidambar styraciflua L.—25259 (F). Vari-
ous wooded habitats; Knobs. Plants of this
taxon we noted along the Ohio River ap-
peared to have been planted.
Woody Plants—Clark and Bauer £5
Hippocastanaceae
Aesculus flava Aiton—24835 (B); 25223 (F);
24814 (M). Confined to ravines and north-
facing slopes along the Ohio River and its
direct tributaries; also in mesic woods of
Knobs.
Aesculus glabra Willd.—24855 (B), 25196 (F),
94614 (H), 24722 (M), 25173 (N), 25021
(R). Wooded slopes, disturbed habitats, and
fencerows; common.
Hydrangeaceae
Hydrangea arborescens L.—24927 (B), 25291
(F), 24720 (M), 25176 (N), 25061 (R). Nor-
mally confined to mesic east- and north-fac-
ing bluffs along major streams; infrequent.
Philadelphus coronarius L.—25243 (F). Intro-
duced; established and spreading on old
roadcut; rare. Most other adventive popu-
lations of this genus in Kentucky probably
should be referred to this taxon.
Juglandaceae
Carya cordiformis (Wangenh.) K. Koch—
94887 (B), 25202 (F), 24649 (H), 24763
(M), 25142 (N), 25031 (R). Most wooded
habitats; the most common hickory in our
study area.
Carya glabra (Miller) Sweet—24891 (UB).
25269 (F), 24676 (H), W. Meijer, 13 Jun
1969, UK #33801 (M); 25017 (R). Upland
woods; infrequent to rare.
Carya laciniosa (Michaux f.) Loud—24898
(B), 25328 (F), 24668 (H), 24712 (M),
25125 (N), 25014 (R). Various wooded hab-
itats; frequent.
Carya ovata (Miller) K. Koch—24892 (B),
94635 (H), 25125 (N), Thieret 52747 in
KNK (R). Infrequent to rare; most common
near the border between Bluegrass and
Knobs in Fleming County. Plants of this tax-
on in our region do not fit well the recent
description given by Stone (1997). The ap-
parent reason is that, throughout most of
central Kentucky, introgression may be oc-
curring between plants of this taxon and the
following one.
Carya tomentosa (Poiret) Nuttall—24883 (B),
95222 (F), 24640 (H), 24824 (M), 25087
(N), 24989 (R). Upland woods and woods
remnants; frequent to occasional.
Carya ovata X Carya tomentosa—24733 (M).
As mentioned above, introgression between
these two taxa is common in our region.
producing various degrees of intermediacy.
This is a collection that appeared to us to
be truly intermediate, so we cite it as an
unnamed hybrid.
Carya pallida (Ashe) Engler and Graebner—
24860 (B), 25112 (N), 25062 (R). Upland
woods and woods margins; infrequent.
Juglans nigra L.—24896 (B), 25280 (F),
24677 (H), 24730 (M), 25148 (N), 24923
(R). Various habitats; common. We did not
observe any specimens of J. cinerea L.., liv-
ing or dead, in the study area.
Lauraceae
Lindera benzoin (L.) Blume—24876 (B),
25293 (F), 24650 (H), 24762 (M), 25088
(N), 25019 (R). Various disturbed, degrad-
ed, and intact habitats; one of the most
common shrubs in this area of Kentucky.
Sassafras albidum (Nuttall) Nees—22419 (B),
25285 (F), 24647 (H), 24718 (M), 25114
(N), 25027 (R). Various habitats; common.
Magnoliaceae
Liriodendron tulipifera L.—24853 (B), 25305
(F), 24627 (H), 24717 (M), 25018 (R). Me-
sic woods; rare in Bluegrass, progressively
more common eastward.
Malvaceae
Hibiscus syriaca L.—24761 (M). Introduced;
escaped along roadside; rare, but to be ex-
pected more commonly in the future.
Menispermaceae
Menispermum canadense L.—24877 (B),
95246 (F), 24592 (H), 24760 (M), 25164
(N), 24998 (R). Various habitats, more fre-
quent in highly disturbed situations, such as
fencerows and rights-of-way; common.
Mimosaceae
Albizia julibrissin Durazzini—25216 (F). In-
troduced; possibly persistent after cultiva-
tion, or possibly an escape.
Moraceae
Broussonetia papyrifera (L.) Ventenat—24719
(M). Introduced; an escape into highly dis-
turbed habitat.
Maclura pomifera (Raf.) C.K. Schneider—
24859 (B), 25337 (F), 24684 (H), 24768
46 Journal of the Kentucky Academy of Science 62(1)
(M). 25156 (N), 25076 (R). Various dis-
turbed habitats; common.
Morus alba L.—24948 (B), 25319 (F), 24669
H), 24818 (M), 25182 (N), 25078 (R). In-
troduced; roadsides and other disturbed
habitats; occasional.
Vlorus rubra L.—24904 (B), 25290 (F), 24679
(H), 24779 (M), 25161 (N), 25008 (R). Me-
sic slopes and alluvial terraces; infrequent,
but more common eastward.
Oleaceae
Chionanthus virginica L.—25300 (F). Upland
woods; occasional: Knobs.
Fraxinus americana L.—24902 (B), 25296 (F),
24667 (H), 2481] (M), 25171 (N), 25007
(R). Woodlands and woodland remnants;
common.
Fraxinus pennsylvanica Marshall—24949 (B),
25204 5B)" 2AbS6CH). 24723" (MI) 25137
(N), 25060 (R). Alluvial terraces and stream
margins; Common.
Fraxinus quadrangulata Michaux—24938 (B),
25325 (F), 24618 (H), 25141 (N), 24983
(R). Various wooded habitats but most com-
mon on south- and west-facing xeric wood-
lands and stream bluffs: frequent.
Ligustrum sinense Louriero—24851 (B),
24602 (H), 24804 (M). Introduced; escaped
to waste places, highly disturbed habitats
and alluvial woods. Most common near the
Ohio River.
Ligustrum vulgare L.—24951 (B), 24785 (M),
25190 (N). Introduced; escaped to highly
disturbed habitats. Most common in the
Ohio River corridor.
Platanaceae
Platanus occidentalis L.—24941 (B), 25253
(F), 24630 (H), 24787 (M), 25149 (N),
25044 (R). Most common in low ground,
but also in other situations; frequent.
Poaceae
Arundinaria gigantea (Walter) Chapman
25355 (N). Wooded ravine; extremely rare.
Ranunculaceae
Clematis virginiana L.—24954 (B), 25257 (F),
24700 (H), 24742 (M), 25175 (N), 25070
(R). Low ground along streams and wood-
land margins; infrequent.
Rhamnaceae
Rhamnus caroliniana Walter—25197 (F),
24743 (M). Deciduous woods and disturbed
rights-of-way. Very rare in Bluegrass, infre-
quent in Knobs.
Rhamnus lanceolata Pursh—25200 (F), 24693
(H). Only two populations noted: one on a
wooded alluvial terrace (Bluegrass), the oth-
er in highly disturbed upland habitat (Blue-
grass-Knobs border).
Rosaceae
Amelanchier arborea (Michaux f.) Fernald—
25297 (F). Deciduous woods, occasional:
Knobs.
Crataegus calpodendron (Ehrh.) Medikus—
24863 (B), Meijer, Setser, and Meade 1190
= MDKY #1190 (F), 24594 (H), 25097 (N),
25063 (R). Upland roadsides, blufftops, and
woodland margins; infrequent.
Crataegus coccinea L.—25211 (F), 24612 (H),
25121 (N). Woodland margins and dis-
turbed habitats; infrequent.
Crataegus crus-galli L—25238 (B), 24685
(F), 24812 (M), 25126 (N). Upland dis-
turbed sites and woodland margins; infre-
quent.
Crataegus flabellata (Bosc) K. Koch—25208
(F), 24590 (H), 25113 (M), 25064 (R). Up-
land disturbed sites and woodland margins;
infrequent.
Crataegus mollis (Torrey and Gray) Scheele—
24863 (B), 24678 (H), 24817 (M), 25158
(N). Mainly in fencerows and on blufftops;
infrequent.
Crataegus pruinosa (Wendland) K. Koch—
24862 (B). Disturbed woodland; rare.
Malus angustifolia (Aiton) Michaux—25341
(F), 25118 (N). Only two populations noted:
open field (Bluegrass); low woods along
creek (Knobs). Rare.
Malus coronaria (L.) Miller—24932 (B),
25247 (F), 24683 (H), 24815 (M). Upland
woodland margins and fencerows; rare.
Malus sylvestris (L.) Miller (=M. pumila of
some authors)—25318 (F), 24765 (M),
25152 (N), 24974 (R). Introduced; fence-
rows and other ruderal habitats; infrequent.
Physocarpus opulifolius (L.) Maxim.—G.F.
Buddell Il #2206, in KNK (B).
Prunus americana Marshall—24857 (B),
25245 (F), 24589 (H), 24714 (M), 25144
Woody Plants—Clark and Bauer AT
(N), 24984 (R). Forest remnants, disturbed
woods, and fencerows; frequent.
Prunus cerasus L.—25219 (F). Introduced;
adventive, adjacent to road right-of-way.
Prunus mahaleb L.—24935 (B), 24690 (H),
94745 (M), 25133 (N), 25034 (R). Intro-
duced; roadcuts and rights-of-way; infre-
quent.
Prunus mexicana S. Watson—24905 (B),
24639 (H), 24715 (M), 25122 (N), 24981
(R). Forest remnants, disturbed woods, and
fencerows; frequent.
Prunus munsoniana Wight and Hedrick—
25214 (F). Ridgetop in deciduous woods,
Mississippian Plateau (Knobs); rare.
Prunus persica (L.) Batsch—25213 (F), 24687
(H), 24806 (M), 25178 (N), 24963 (R). In-
troduced; fencerows and other ruderal hab-
itats; infrequent.
Prunus serotina Ehrhart—24919 (B); 25304
(F), 24637 (H), 24775 (M), 25169 (N),
95042 (R). Most habitats; common.
Pyrus calleryana Decne.—24884 (B), 25209
(1B), DANS) (TEDL BAS (MD), SHI UN)
25059 (R). Introduced; roadsides, margins
of blufftop woods; infrequent.
Rosa carolina L.—24858 (B), 25274 (F),
24659 (H), 24735 (M), 25099 (N), 25009
(R). Upland deciduous woods and glades;
frequent.
Rosa multiflora Thunberg—24916 (B), 25283
(F), 24658 (H), 24786 (M), 25159 (N),
95035 (R). Introduced; most habitats, com-
mon. At present, the worst woody weed in
our study area. ‘
Rosa setigera Michaux—24895 (B), 24591
(H), 24741 (M), 25092 (N), 25075 (R).
Fencerows, low rights-of-way; common.
Rosa virginiana Miller—24680 (H). This is ap-
parently the first report of this species from
the Bluegrass (Browne and Athey 1992).
However, because Medley (1993) rejected
the notion that the species occurs in Ken-
tucky, this collection actually may represent
the first verified occurrence of the species
in the state. Fencerow; rare.
Rosa wichuraiana Crepin—24953 (B), 24601
(H), 24822 (M). Introduced; roadsides and
fencerows; infrequent, but undercollected.
Rubus allegheniensis T.C. Porter—25308 (F).
Various habitats, Knobs.
Rubus argutus Link—24881 (B), 25346 (F),
94675 (H), 24803 (M), 25150 (N), 2499
(R). Various habitats; common.
Rubus flagellaris Willd. (incl. R. ensleni
Tratt. )—24634 (H), 24995 (R). Deciduous
woods; infrequent, but undercollected.
Rubus occidentalis L—24866 (B), 25248 (F),
94674 (H), 24784 (M), 25165 (N), 24994
(R). Upland and lowland woods and various
disturbed habitats; frequent.
Rubus. trivialis Michaux—25331 (F), 25083
(R). Fencerows; rare.
Spiraea tomentosa L.—Meijer, Setser, and
Meade #1223, in MDKY (F). Wooded up-
land swamp.
Rubiaceae
Cephalanthus occidentalis L.—24944 (B),
25236 (F). Margin of Ohio River backwater;
upland swamp; rare.
Rutaceae
Ptelea trifoliata L.—25321 (F), 24607 (H),
25185 (N). Bluffs along major streams;
common in habitat but absent elsewhere.
Zanthoxylum americanum Miller—24931 (B),
95198 (F), 24641 (H), 24737 (M), 25085
(N), 25000 (R). Xeric bluffs and slopes, usu-
ally south- or west-facing; common in hab-
itat, absent elsewhere.
Salicaceae
Populus alba L.—24865 (B), 25194 (F), 24626
(H), 24725 (M), 25098 (N), 25065 (R). In-
troduced; spreading from cultivation at old
home sites, fencerows, and ruderal habitats;
occasional.
Populus deltoides Bartr. ex Marshall—24840
(B), 25340 (F), 24686 (H), 24795 (M),
24973 (R). Low ground; occasional to rare,
nowhere common.
Populus grandidentata Michaux—25242 (F).
Old roadcut; rare. Apparently absent from
Bluegrass area.
Salix alba L.—25108 (N). Introduced; estab-
lished along Brushy Creek.
Salix caroliniana Michaux—24848 (B). Back-
water of Ohio River, apparently absent from
other parts of study area.
Salix discolor Muhl—J. Campbell, 16 May
1992, UKY (F).
Salix exigua Nuttall—24846 (B), 25240 (F),
24706: (H), 24797 (M), 25135 (N), 24971
(R). Open stream corridors; common.
48 Journal of the
Salix nigra Marshall—24942 (B), ee i (F),
94705 (H), 24821 (M), 25135 (N), 34971
(R). Open stream corridors; Regen al.
Salix sericea Marshall—25261 (F). Open, up-
‘and swamp; rare.
Simar¢ yubaceae
Ailanthus altissima (Miller) Swingle—24955
(B), 25212 (F), 24604 (H), 24780 (M),
25130 (N), 25082 (R). Introduced: dis-
turbed habitats (mature trees; seedlings are
found in almost all habitats). Occasional,
but obviously accelerating in its rate of nat-
uralization.
Smilacaceae
Smilax glauca Walter—24861 (B), 25267 (F),
24645 (H), 25101 (N). South-and west-fac-
ing wooded slopes, fencerows; infrequent.
Smilax hispida Muhl.—24958 (B), 25279 (F),
24652 (H), 24759 (M), 25119 (N), 25071
(R). Most habitats; common.
Smilax rotundifolia L.—25302 (F).
habitats; Knobs.
Staphylea trifoli 24930 (B), 25323 (F),
24608 (H), 24740 (M), 25086 (N), 25066
(R). Mesic woods; frequent.
Various
Tiliaceae
Tilia americana L. var. americana—24S888 (B),
22S) 2465. CEl)s 24749 (Ni) ss 2bl 7
(N), 24987 (R). Mesic woods; frequent.
Ulmaceae
Celtis occidentalis L—24907 (B), 25301 (F),
24672 (H), 24773 (M), 25168 (N), 24999
(R). Various habitats, less frequent in the
Knobs; one of the most common trees in
this part of Kentucky.
Celtis tenuifolia Nuttall (= C. occidentalis var.
georgiana of some authors)—25330 (F),
3.4599 (H), 24965 (R). Upland xeric habi-
tats, fencerows; infrequent.
Ulmus americana L.—24960 (B), 25256 (F),
24663 (H), 24805 (M), 25157 (N), 25043
(R). Various upland and low habitats; com-
mon.
Ulmus pumila L.—24843 (B), 24792 (M). In-
troduced; adventive in counties bordering
the Ohio River.
Ulmus rubra Muhl.
24691 (H),
—24900 (B), 25249 (F),
24766 (M), 25192 (N). Mesic
Kentucky
Academy of Science 62(1)
wooded and disturbed slopes, stream bluffs;
frequent.
Ulmus thomasii Sargent—24616 (H). Wooded
stream bluff; rare.
Viscaceae
Phoradendron serotinum (Raf.) Johnst.—
Thompson and Thompson #89-150, in KNK
3), Thompson and McLaughlin #88-3217,
in MDKY me 24620 (on Ulmus thomasii,
see above)(H), Thompson #88-3223, in
KNK (M), ee and Denton #89-
3015, in MDKY (R). Less frequently en-
countered northward.
Vitaceae
Ampelopsis cordata Michaux—24849 (B),
25046 (H), 24727 (M), 25046 (R). Stream-
banks, low open ground, and fencerows;
sometimes frequent but rare or absent in
Knobs.
Parthenocissus quinquefolius (L.) Planchon—
94922 (B), 25316 (F), 24673 (H), 24752
(M), 25163 (N), 25016 (R). Most habitats;
common.
Vitis aestivalis Michaux—24911 (B), 25317
(F), 25053 (H), 24997 (R). Roadsides and
dry woods; common in Knobs, rare in Blue-
grass.
Vitis riparia Michaux—24794 (M). Low
ground along Ohio River; rare or absent
elsewhere.
DISCUSSION
Habitats
Before embarking on this study, we were
aware that most of the study region had a long
history of intensive post- -settlement land use.
However, we were frankly surprised at the
present extent of its effects. Most natural hab-
itats in this region have been completely de-
stroyed or degraded beyond recognition. Even
though one does not encounter extensive row
crops in this part of the Bluegrass, most of the
uplands in this rolling country have been com-
pletely cleared, or only remnant, highly dis-
turbed, young-aged woodlots remain. Down-
slope from uplands, where steeper terrain of-
ten militates against row cropping, land is
most often relegated to pasture. Cattle (and,
we suspect, very high populations of white-tail
deer, Odocoileus virginianus) range through
forested slopes and small creek bottoms,
Woody Plants—Clark and Bauer 49
fenced off only from dwellings and roadways.
As a result, most of the native herbaceous for-
est flora has been eliminated, woody plants do
not regenerate naturally, and exotic species
(such as Lonicera maackii and Rosa multiflo-
ra) are favored over natives. Oak regeneration
has practically been eliminated in most of this
part of the northern Bluegrass; scarlet oak
(Quercus coccinea) probably will disappear
from this part of the Bluegrass within the near
future.
In situations such as this, highway rights-of-
way and fencerows sometimes act as refugia
for elements of the flora. However, in this part
of Kentucky, this limited habitat is under fre-
quent assault from the heavy application of
herbicides along public roadways. Typically,
this results in the elimination of most herba-
ceous and seedling woody dicots, not only
along the roadway but as far as the sprayer can
reach into the forest, and the invasion and her-
baceous stratum dominance of species such as
Festuca spp. and Phalaris arundinacea are en-
couraged. In other words, herbicide spraying
is eliminating one of the very few habitats re-
maining in the Bluegrass for native plants. It
is a purposeful, all-out assault by the State on
its native plants.
As a result of these land-use patterns and
prolonged exclusion of fire as an environmen-
tal factor, habitats of high quality in our study
area were few and far between. In our opin-
ion, the remnant site we encountered (other
than Quiet Trails Nature Preserve [Harrison
Co.], within which we did not collect) with
highest natural value was within Clay Wildlife
Management Area in Nicholas County. In our
opinion, portions of Clay Wildlife Manage-
ment Area should be managed as a atrial
area to protect what has been lost elsewhere
in the region. In addition, we recommend that
all remaining forested steep bluffs encoun-
tered along the Licking River and its major
tributaries should receive protection. Without
these remnant habitats, a significant percent-
age of the native woody species in this region
would vanish entirely.
Distribution Patterns
We feel our study area is large enough to
indicate some possible geographic distribu-
tional patterns of woody plant occurrence but
too small to produce definitive evidence.
However, four distributional patterns perti-
nent to the woody flora have emerged within
the study area as a result of the evidence we
compiled. These distributional categories are
(1) an apparent distributional discontinuity be-
tween the northern Bluegrass and northern
Knobs; (2) plants whose distribution seems re-
lated to the Ohio River corridor: (3) notewor-
thy rarities; and (4) significant weeds.
Category 1. Within the area we studied, it
is apparent that there is a sharp distributional
divide between the Bluegrass and Knobs. The
following species occur in the Knobs but ap-
pear to be entirely missing from the Bluegrass.
Plants present in the rani and absent from
the Bluegrass (during this study) include all
species of Ericaceae (eit species), Acer rub-
rum, Amelanchier arborea, Aralia spinosa,
Betula nigra, Chionanthus virginica, Hama-
melis virginiana, Liquidambar styraciflua, Hy-
pericum stragulum, Nyssa sylvatica var. biflo-
ra, Pinus (three species), Populus grandiden-
tata, Prunus munsoniana, Quercus montana,
Rosa palustris, Rubus allegheniensis, Salix ser-
icea, Smilax rotundifolia, and Viburnum ac-
erifolium. This means that more than 19% of
native woody plant taxa occurring in the
Knobs apparently do not occur in the adjacent
northern Bluegrass. This is a significant dis-
continuity; reasons for it are hypothetical. One
possible explanation could relate to edaphic
factors, which affect mycorrhizae; the latter
are known to be favored by acid soil. Members
of Ericaceae and Pinaceae will grow if planted
in the northern Bluegrass, but perhaps ger-
mination and establishment are selected
against in Bluegrass soils. Also, it is well
known to nurserymen that some species un-
dergo mineral deficiency stress in dry alkaline
soils; Acer rubrum is one of those species. We
hypothesize that the combination of periodic
drought, conditions unfavorable to mycorrhi-
zae, Ane fire may have been major factors that
prevented the establishment of seed sources
in the Bluegrass, without which sustaining
populations of some plants could not persist.
One additional word about this distributional
discontinuity is that, if one were to include the
Cumberland Plateau (not far to the east of the
study area), the floristic discontinuity becomes
much more striking (includes Ilex spp., Mag-
nolia spp., etc.). This issue might be a fruitful
possibility for autecological investigations.
50
Category 2. A second recognizable group
of woody plants is composed ae those that are
either confined to the Ohio River corridor or
are tound only in the Knobs and Ohio River
corridor. As we define it here, the Ohio River
eorridor includes the Ohio River bottom-
lands, adjacent bluffs, and small streams
draining directly into the Ohio River. Plants
appar ently confined closely to the Olin River
in our study area include Amorpha fruticosa,
Physocarpus opulifolius, Rhus typhina, and
Salix caroliniana. Those associated with the
Ohio River and the Knobs but not found in
the Bluegrass interior include Aesculus flava,
Alnus serrulata, and Cornus amomum var.
schuetzeana. This physiographic feature (i.e.,
the river corridor) may actually serve as a mi-
gration pathway for some species around the
apparent barrier of the northern Kentucky
Bluegrass region.
Category Plants that are rare in the
study area include those that are confined to
particular habitats, as well as those that are in
an attenuated portion of their ranges. Plants
we would single out in this category include
several plants confined to steep or gladelike
bluffs (Bignonia capreolata, Rhus aromatica,
Ulmus thomasii); those near the edges of their
ranges (Malus angustifolia, Nyssa sylvatica
var. biflora, Prunus munsoniana, Quercus coc-
cinea, Rhamnus lanceolata, Rosa virginiana,
and Ulmus thomasii). ;
Perhaps the most surprising rare taxon we
encountered is Arundinaria gigantea. A few
early informal accounts waxed eloquent on the
extensive canebrakes in Kentucky, and these
accounts seem to have been repeated endless-
ly by later writers. Perhaps it was true at one
time. However, at the present time in our
study area, Arundinaria is among the rarest of
woody plants. We extensively but fruitlessly
searched for it and even offered rewards for
its discovery. Eventually, Dr. Wendell King-
solver of Nicholas County took the senior au-
thor to a single population on his land. Ac-
cording to him, cane in the northern Bluegrass
was once widespread but now has been re-
duced to a few small, isolated populations
along main stem of the Licking River by a
combination of gr azing by cattle and long-time
use of the stems for “jig poles,” or throw-away,
temporary fishing poles. Kingsolver a
o
comm.) stated chat protection of the small (<
Journal of the Kentucky Academy of Science 62(1)
ha) canebrake on his land from cattle grazing
and pole collecting has allowed it to increase
considerably in area, and ramets have been
used to re-establish cane in another location
where an extensive canebrake was completely
extirpated.
Category 4. On the whole, we determined
that 11% of the woody plant taxa of this region
is not native. (See Table 1.) Many of these
plants are not especially noticeable weeds at
the present time. One of them (Thuja orien-
talis) is reported herein for the first time as an
escape in Kentucky. Others (not included in
our statistics) are plants whose native ranges
are becoming obscured because they are both
native and escaped from cultivation (e.g., Jug-
lans nigra, Liriodendron tulipifera, Maclura
pomifera, and Quercus palustris).
However, there are some significant exotic
weeds and, based on the senior author's per-
sonal experience, few of these have reached
their zeniths. The impact of most of these will
increase with time, but some are more ag-
gressive invaders than others. Non-native ex-
otics escaped in our study area include the fol-
lowing (those marked with an asterisk were
vouchered from a minimum of five counties):
Ailanthus altissima,* Albizia julibrissin, Ber-
beris thunbergii, Broussonetia papyrifera, Ce-
lastrus orbiculatus, Elaeagnus umbellata,* Eu-
onymus alatus, Ewonymus fortunei,* Hedera
helix, Hibiscus syriaca, Lespedeza bicolor, Li-
gustrum SNCS, Ligustrum vulgare, Lonicera
japonica,* © Lonicera maackii,* Malus sylves-
tris, Morus alba,* Philadelphus coronarius,
Populus alba,* Prunus cerasus, Prunus ma-
haleb,* Prunus persica,* Pyrus calleryana,*
Rosa multiflora,* Rosa wichuraiana, Salix
alba, Ulmus pumila, and Vinca minor. From
our field observations, Lonicera japonica and
Rosa multiflora have the greatest negative eco-
logical impact at present. However, Ailanthus
altissima, Celastrus orbiculatus, Ewonymus
fortunei, and Lonicera maackii are showing
signs of rapid establishment and have the po-
tential for very significant negative impacts
within a few years. One omission readers may
note is Paulownia tomentosa (Thunb.) Steu-
del; though it appears not to be established in
the study area yet, doubtless that will happen
soon.
Woody Plants—Clark and Bauer 51
ACKNOWLEDGEMENTS
We are grateful to the Eastern Kentucky
University Research Committee for its finan-
cial support of this project; to Brenda Clark
and Adrienne Scott for their forbearance and
support; to herbarium curators who made
specimens in their care available for exami-
nation; and to Dr. Robert Kingsolver for help-
ing the senior author make contact with Dr.
Wendell Kingsolver, who granted access to the
Nicholas County Arundinaria population.
LITERATURE CITED
Anonymous. 1997. Kentucky atlas & gazetteer. Delorme,
Yarmouth, ME.
Anonymous. 2000a. “Kentucky Atlas & Gazetteer: Ken-
tucky Counties.” http://www.uky.edu/KentuckyAtlas/
kentucky-counties.html (25 May 2000).
Anonymous. 2000b. “International Plant Name Index.”
http://www.ipni.org/ (28 Dec 2000).
Braun, E. L. 1950. Deciduous forests of eastern North
America. Hafner Publishing Company, New York, NY.
Browne, E. T., and R. Athey. 1992. Vascular plants of Ken-
tucky: An annotated checklist. Univ. Press Kentucky,
Lexington, KY.
Bryant, W. S. 1987. Actual and potential vegetation of the
bluegrass region. Pages 17-19 in J. M. Baskin, C. C.
Baskin, and R. L. Jones (eds). The vegetation and flora
of Kentucky. Kentucky Native Plant Society, Richmond,
KY.
Campbell, J. J. N. 1980. Present and presettlement forest
conditions in the inner Bluegrass of Kentucky. Ph.D.
Dissertation. Univ. Kentucky, Lexington, KY.
Fenneman, N. M. 1938. Physiography of eastern United
States. McGraw-Hill, New York, NY.
Gleason, H. A., and A. Cronquist. 1991. Manual of vas-
cular plants of northeastern United States and adjacent
Canada, 2nd ed. New York Botanical Garden, Bronx,
NY.
Guetig, R. G. 1993. The vascular flora of Estill County,
Kentucky. M.S. thesis, Eastern Kentucky Univ., Rich-
mond, KY.
Hardin, J. W. 1979. Quercus prinus L.—nomen ambig-
uum. Taxon 28:355-357,
Harlow, W. M., E. S. Harrar, J. W. Hardin, and F. M.
White. 1996. Textbook of dendrology. 8th ed. McGraw
Hill, New York, NY.
Holmgren, P. K., and N. H. Holmgren. 2000. “Index her-
bariorum.” [8th edition, updated 28 Mar 2000] http:/,
www.nybg.org/bsci/ih/ih.html (25 Dee 2000).
Jones, R. L., D. A. Eakin, and R. C. Clark. 1995. Index
herbariorum kentuckiensis HI. Trans. Kentucky Acad.
Sci. 56:138-140.
Karan, P. P., and C. Mather (eds). 1977. Atlas of Kentucky.
Univ. Press Kentucky, Lexington, KY.
Kiichler, A. W. 1964. Potential natural vegetation of the
conterminous United States. Am. Geogr. Soc. Spec.
Publ. 36. [includes map]
Little, E. L., Jr. 1971. Atlas of United States trees, Vol. 1.
Conifers and important hardwoods. U.S.D.A. Mise.
Publ. 1146. U.S. Gov. Printing Office, Washington, DC.
Little, E. L., jr. 1977. Atlas of United States trees, vol. 4,
minor eastem hardwoods. U.S.D.A. Misc. Publ. 1342.
U.S. Gov. Printing Office, Washington, DC.
McDowell, R. C., G. J. Grabowski, Jr., and S. L. Moore.
1981. Geologic map of Kentucky. U.S. Geological Sur-
vey, in cooperation with Kentucky Geological Survey.
Publisher not listed (presumably U.S.G.S.), Reston, VA.
Martin, W. H., W. S. Bryant, M. E. Wharton, and J. B.
Varner. 1979. The blue ash-oak savanna-woodland, a
remnant of presettlement vegetation in the Inner Blue-
grass of Kentucky. Castanea 45:149-165.
Medley, M. E. 1993. An annotated catalog of the known
or reported vascular flora of Kentucky. Ph.D. Disser-
tation. Univ. Louisville, Louisville, KY.
Puetz, C. J. Kentucky County Maps. Thomas Publications,
Lyndon Station, WI. In press.
Rehder, A. 1940. Manual of cultivated trees and shrubs.
Macmillan Co., New York, NY.
Stone, D. E. 1997. Juglandaceae. Pages 416-428 in Flora
of North America Editorial Committee (ed). Flora of
North America north of Mexico, Vol. 3. Oxford Univ.
Press, New York, NY.
Taylor, D. J. (ed). 1995. Kentucky Alive! A report of the
Kentucky Biodiversity Task Force. Commonwealth of
Kentucky, Frankfort, KY.
U.S. Geological Survey (ed). 1976. Louisville, Ky.; Ind.;
Ohio 1:250,000 quadrangle, revised 1969. U.S. Geolog-
ical Survey, Reston, VA.
U.S. Geological Survey (ed). 1978. Huntington, W.Va.;
Ky.; Ohio 1:250,000 quadrangle, revised 1977. U.S.
Geological Survey, Reston, VA.
Walker, J. R. 1995. “The Columbia guide to online style.”
Version 1.3. http://www.cas.usf.edu/english/Avalker/
mila.html (25 May 2000).
Wunderlin, R. P. 1997. Moraceae, Morus. Pages 390-392
in Flora of North America Editorial Committee (ed).
Flora of North America north of Mexico, Vol. 3. Oxford
Univ. Press, New York, NY.
J. Ky. Acad. S 2(1):52-59. 2001.
Effects of Fish on Zooplankton Community Structure in Chaney Lake,
a Temporary Karst Wetland in Warren County, Kentucky
Nicole Vessels and Jeffrey D. Jack'
Department of Biology, Western Kentucky University, Bowling Green, Ke ntucky 42101-3576
ABSTRACT
Lake is an ephemeral karst lake in southern Kentucky (USA).
Chaney often contains fish that can enter the lake through the underlying Lost River drainage system. The
Chaney Unlike most ephemeral lakes,
effects of introduction of golden shiners (Notemigonus crysoleucas) on zooplankton in Chaney were examined
for a 2-week period in June and July 1997. Twelve fish were transplanted from an isolated region of the lake
into each of three enclosures in an area of the lake where no fish had been observed. Three additional
enclosures served as fish-free controls. Zooplankton samples and water chemistry and nutrient data were
taken every 4 days. Water chemistry and nutrient data showed no significant differences in the measured
parameters between enclosures with fish and those without fish. Bosmina and Acanthocyclops showed de-
creases in population growth rates in the presence of fish. The fish had no effect on the growth rates of the
smaller zooplankton present such as the rotifers. Vertebrate predation in systems like Chaney Lake may pose
significant ecological challenges for organisms adapted to temporary habitats.
INTRODUCTION
Fish can be important determinants of zoo-
plankton abundance, species structure, and
productivity in aquatic systems. Since the early
work of Hrbacek et al. (1961) there have been
numerous studies fede the impacts of
fish on zooplankton communities. Removal of
zooplanktivorous fish from lakes has been
shown to increase the densities of herbivorous
zooplankton with concomitant effects on the
phytoplankton (Carpenter et al. 1985, 1987;
Vanni et al. 1990). This work has prompted
research in the use of fish in “biomanipula-
tion” to aid managers in controlling water
quality in lakes (Shapiro and Wright 1984).
There has been less research eouduered on
the effects of fish on zooplankton in wetland
or forested lake communities, although fish
have been shown to have significant effects on
zooplankton in shallow, eutrophic, lakes that
may be similar in many respects to wetlands
(Hanson and Butler 1990). In a study of semi-
permanent Minnesota wetlands, Hanson and
Riggs (1995) found that densities, biomasses,
and taxa richness of zooplankton were signifi-
cantly lower in wetlands that contained fish as
opposed to similar ponds which did not con-
tain any fish. In a study of another Minnesota
' Current address: Department of Biology, University of
Louisville, Louisville, KY 40292: to whom correspondence
should be sent.
prairie lake, a fish kill resulted in shift in zoo-
plankton species composition from Bosmina
and Chydorus to the larger Daphnia galeata
and D. pulex (Hanson anal Butler 1994).
Wetland areas may provide more refuges to
zooplankton from fish predation than the open
water column of a lake.In a pond-enclosure
experiment where the density of vegetation
was controlled, perch did not consume as
much zooplankton biomass when vegetation
was present in the enclosures as when vege-
tation was absent (Diehl 1992). In their study
of a coastal marsh along Lake Erie, Kreiger
and Klarer (1991) found that some copepods
and cladocerans were more abundant near the
sediments or near macrophytes than in the
open-water column, which is consistent with
earlier work suggesting that vegetation can
provide an important refuge for zooplanktors
from fish predation (Timms and Moss 1984).
While such biotic interactions between fish
and zooplankton are important in structuring
planktonic communities in permanent aquatic
systems, in most temporary or ephemeral
pond systems zooplankton are not subject to
fish predation, although other vertebrates such
as amphibians may have strong effects on z00-
plankton assemblz ages (Wilbur 1997). Indeed,
taxa such as the large branchiopod Crustacea
are thought to be successful in temporary sys-
tems because fish are often excluded from
these habitats (Kerfoot and Lynch 1987). Or-
ganisms inhabiting ephemeral water bodies
Fish and Zooplankton Community Structure—Vessels and Jack 53
typically have life histories and ecological
strategies that are synchronized to the hydrol-
ogy of their habitat (reviewed in Wiggins et al.
1980) and that do not necessarily give these
organisms any advantage in responding to pre-
dation from fish. In most transient water hab-
itats, the threat of fish predation would be ex-
ceedingly small; in some ephemeral karst
lakes, however, fish predation may be an im-
portant force structuring the zooplankton
community.
Karst geology is characterized by extensive
caves, sinkholes, sinking streams, and springs.
Because of the many conduits leading into the
subsurface in well-developed karst landscapes,
surface water may be directed rapidly into the
groundwater areas through a sinkhole, may
rise again at a spring, and then sink into the
subsurface again as a sinking stream. These
points of exit and entrance of water are called
estavelles. In many karst landscapes, standing
surface water is uncommon, but variations in
local geology can produce ephemeral karst
lakes and wetlands such as Chaney Lake in
south-central Kentucky. Chaney Lake is a 68-
hectare state nature preserve located about 10
km south of Bowling Green in Warren County,
Kentucky. The lake area is a shallow depres-
sion that is connected by fissures (estavelles)
in the subsurface rock to the Lost River Cave
system, which has a drainage basin of about
933 km?. The lake is formed because of the
Lost River Chert formation, which overlays
the limestone under the lake and prevents the
rapid return of water to the subsurface except
where estavelles are located. When the capac-
ity of the Lost River Cave system is exceeded
during periods of high precipitation, ground-
water enters Chaney Lake via the estavelles
and also through one intermittent surface
stream on the south edge of the preserve. As
the water levels in the Lost River drop, water
may leave the lake through the estavelles as
well, leaving large numbers of smaller, isolated
pools behind. The lake usually holds water
from December through August, although
from May on most of that water is in small
pools (Jack, personal observation).
Historically, karst wetlands such as Chaney
Lake were very important aquatic habitats in
western Kentucky because they provided an
important source of standing water in a terrain
that had little surface water. Chaney Lake and
another nearby karst lake, Rich Pond,
huge numbers of migrating birds in the spri:<
and may be an important foraging area for a
variety of waterfowl on their spring migrations
(Mason, personal communication). Chaney
Lake contains a variety of zooplankton species,
including common ephemeral pond taxa such
as the fairy shrimp Streptocephalus. However,
the same estavelles that deliver water to sup-
port these communities can also serve as con-
duits for vertebrates such as the spring fish,
Chologaster agassizi, to enter the lake. If fish
can enter Chaney Lake, they may have a
strong impact on zooplankton densities and
community structure.
In early June 1997, a population of golden
shiners (Notemigonus crysoleucas), which may
have entered Chaney Lake via estavelles, was
found in an isolated pool in the northeast cor-
ner of Chaney Lake. These fish were trans-
planted to experimental enclosures in another
section of the lake to assess the effect of fish
on the zooplankton communities in Chaney.
We hypothesized that the fish would select the
largest zooplankton species in the water col-
umn and, in turn, would cause a decrease in
population growth rates of these larger spe-
cies. We expected that the smaller zooplank-
ton species such as rotifers would have no sig-
nificant response to the fish or that they would
increase in numbers if they are released from
competition for resources with, or predation
from, the larger macrozooplankton (see Gil-
bert 1988; Jack and Gilbert 1997).
MATERIALS AND METHODS
The study was conducted from 19 Jun 1999
to 1 Jul 1997 in a marsh area in the south-
eastern portion of Chaney (see Kelley et al
2000). This area was chosen as the study site
because no fish had been observed there and
it was unlikely to dry during the period
planned for the experiment. The dominant
vegetation in the marsh was buttonbush (Ce-
phalanthus occidentalis), aquatic plants such
as Polygonum sp. and a liverwort in the genus
Riccia. The higher ground around the marsh
area is ringed by tree species such as swamp
white oak (Quercus bicolor), red maple (Acer
rubrum) and sycamore (Platanus occidentalis ).
Large trees are not present in the marsh itself,
perhaps because this part of Chaney consis-
54 Journal of the Kentucky Academy of Science 62(1)
tently holds water for most of the year (>7
months in 1995-1998).
Six |-m* enclosures were constructed using
P\C piping for frames and plastic for the
des. The enclosures were then placed in the
marsh, enclosing the water column and the as-
sociated zooplankton. They were anchored
into the sediment of the marsh and were open
at the top and at the bottom. Three enclosures
were randomly selected to hold 12 fish each,
with the other three serving as controls. The
fish were caught by sweeping a net in the pool
containing the fish and moving the fish into
the appropriate enclosures in the marsh.
These stocking densities were about % the es-
timated density of the fish in the original pool.
This was determined by visually assessing the
numbers of fish in the source pool and then
taking transects through the pool to determine
average depth and emclen which were then
used to estimate pool volume. Invertebrate
and water chemistry samples were taken on
the first day of the experiment and every 4
days afterward in each of the six enclosures
for the duration of the project. Depth, turbid-
ity, specific conductivity, temperature, pH, dis-
solved oxy gen, and percent dissolved oxygen
were Peed using a YSI 6250 multiprobe.
One-liter nutrient grab samples were also tak-
en in acid-washed bottles to measure nitrates,
ammonia, and soluble reactive phosphorous
using a Hach DREL 6000 water analysis kit.
Nitrate was measured by the Cadmium Re-
duction method: ammonia was determined us-
ing the Nessler method; and soluble reactive
phosphorus was measured using the Hach
Phosver 3 method. Invertebrate sampling was
conducted using a 7-cm-diameter coring de-
vice. Two 5-liter core samples were taken from
each enclosure on each sampling date and fil-
tered through a 20-4~m mesh sieve. The ma-
terial collected was then washed into a con-
tainer and preserved in 90% ethanol.
All samples were counted in the laboratory
by using an Olympus SZH 10 dissecting mi-
croscope. The samples were counted in their
entirety and the dominant taxa (>95% of nu-
merical abundance) were identified down to
the lowest practicable taxon (usually genus).
Population growth rates were calculated for
the domaaanit taxa from the first and last ex-
perimental dates using the equation, r =
InN,-InN,t', where r is equal to the popu-
lation growth rate, N, is equal to the final sam-
pling date, No represents the beginning sam-
pling date, and t stands for the total number
of days in the experiment (Jack and G ilbert
1993). A Student's t-test was used to compare
growth rates in the fish and fishless enclosures.
A repeated measures ANOVA was calculated
using SYSTAT version 7.0 to assess changes in
the physical parameters in the enclosures.
RESULTS
The data met the assumptions of ANOVA
so transformation was not needed before the
data could be analyzed. Water chemistry and
nutrient analysis data indicated no significant
differences (P > 0.07) in measured parame-
ters between treatments over time. The aver-
age temperature for all enclosures was 23.4 +
0.84°C and the pH in the enclosures averaged
5.93 + 0.57 (all data are presented as mean
+ (standard errors). Turbidities were ee
variable in all enclosures (39.4 + 23.2 and
40.0 + 24.3 for fish and non-fish espera
and were higher after storm events. Dissolved
oxygen levels ranged from just under 1 mg li-
ter! to 3.3 mg liter~! but there were no dif-
ferences in oxygen levels between treatments.
Average nitrate, ammonia and soluble reactive
phosphorus concentrations were not different
between treatments (P > 0.15; Figure 1).
The fish added to the enclosures had an ini-
tial average size (mouth to base of caudal fin)
of 1.95 + 0.21 cm; the average length at the
end of the experiment was 2.46 + 0.06 cm.
The macrozooplankton assemblage in the
marsh was dominated (>90%) by Bosmina sp.
and Acanthocyclops sp., with smaller numbers
of Cer ‘iodaphnia sp., Daphnia sp., and at least
two species of ostracods. The ostracods were
similar in size and were grouped together for
the purposes of the analysis. One isopod (Cae-
cidotea sp.), one amphipod (Hyalella azteca),
and at least one water mite (Hydracrina) spe-
cies occurred in the samples. The latter three
groups were considered to be accidentals in
the plankton and were not included in the
analysis. The microzooplankton assemblage
was primarily composed of rotifers, with Mon-
ostyla sp., Euchlanis sp. and Ascomorpha sp.
as the numerical dominants (>78%). There
were also one species each of Branchinous,
Keratella, and Lecane, and two species of Po-
lyarthra species present in some samples. We
Fish and Zooplankton Community Structure—Vessels and Jack
On
Ot
Nutrients
@ Fish
0.4
0.3
0.2
0.1
0
=
OD
S|
Ammonia
Figure 1.
@ No Fish
Nitrate SRP
Ending concentrations of ammonia, nitrate, and soluble reactive phosphorous (SRP) in fish and fishless
enclosures in Chaney Lake, Warren County, Kentucky (19 Jun 1999-1 Jul 1997). Bars show means and standard errors.
did not find any identifiable protists in our
samples, but our filtering and fixation proce-
dure may have prevented adequate sampling
and recognition of these small organisms.
The presence of fish in the enclosures neg-
atively affected the larger invertebrate taxa but
showed no effect on the smaller taxa. The fish
negatively affected the Bosmina sp. and the
Anthocyclops sp. growth rates (P < 0.006; Fig-
ure 2). Ending mean densities of Bosmina
were significantly higher in the fish- less enclo-
sures (43 individuals liter~') compared to the
fish enclosures (5.3 individuals liter~!). Acan-
thocyclops sp. growth rates and ending mean
densities were significantly higher in enclo-
sures without fish (33 individuals liter~') than
in enclosures with fish (7.3 individuals liter~').
Ostracods as a group had a positive population
growth rate when the fish were present and a
negative growth rate without fish, but there
was no significant difference between the two
treatments (P = 0.07).
The presence of fish had no significant ef-
fect (P > 0.07) on the population growth rates
of the three dominant rotifer species-
Ascomorpha, Euchlanis, and Monostyla (Fig-
ure 3); however the densities of both Euch-
lanis and Ascomorpha decreased over time in
all of the enclosures. Density of Monostyla sp.
increased nearly 10 times over the same time
period in all enclosures.
DISCUSSION
Our results confirmed that fish predation
can affect aquatic invertebrate community
structure in Chaney Lake.
Physical factors and nutrients assayed were
not significantly different, so these factors
probably did not contribute to the response of
the zooplankton to fish. In enclosure experi-
ments the effects of fish are sometimes the
result of indirect mechanisms. Ammonia ex-
creted by fish, for example, may enhance algal
growth or the fish may feed on the algae, com-
peting with the zooplankton. The golden shin-
ers, however, are zooplanktivorous at this size
(R. Hoyt, pers. comm.), and we found no dif-
ferences in nutrient concentrations between
the two treatments. The population growth
rates we reported for our organisms were
somewhat low compared to the instantaneous
growth rates of related taxa in other ephem-
eral systems (Taylor et al. 1989), but this may
be a reflection of a more constrained resource
base in Chaney Lake.
Our data support the conclusion that fish
predation in the enclosures was driving the
suppression of large zooplankton in our study.
~p
56 Journal of the Kentucky Academy of Science 62(1)
Crustaceans
@ Fish
Bosmina
th rates day’
Sa
je) = NO
Population grow
Sy. i
Oo N
Figure 2.
Warren County, Kentucky (19 Jun 1999-1 Jul 1997).
Bosmina are not typically considered very vul-
nerable to fish predation because of their
small size es: to other crustaceans, and
many cyclopoids have well-developed escape
responses that they may use to avoid fish pre-
dation. As the largest common zooplankton
prey in the Boece however, one would
expect that visually foraging fish would focus
on Bosmina and the Acanthoc ylops. The os-
tracods were not significantly affected even
though their mean size in the enclosures was
comparable to that of Bosmina (0.65 vs. 0.44
mm, respectively). Ostracods are often found
in association with vegetation or in benthic ar-
eas, where the golden shiners are unlikely to
forage Secesecilly on them. The ostracods
present in our samples may not have been
common in the plankton but may have been
captured when the corer displaced them from
the vegetation or the bottom.
Schneider and Frost (1996) found that in
some cases the suppression of Daphnia in
temporary ponds was associated with an in-
crease in rotifer densities and taxon diversity.
We did not see the increase in rotifer densities
that we expected would occur once the ma-
Acanthocyclops
™ No Fish
Ostracods
Taxa
Population growth rates of the dominant crustacean species in fish and fishless enclosures in Chaney Lake,
Bars show means and standard errors.
crozooplankton numbers were reduced; in-
creases and decreases in rotifer numbers oc-
curred across all enclosures regardless of
treatment (see Results). This may indicate that
the larger zooplankton are not significant
predators on or competitors with the rotifers
during this period in Chaney or that the roti-
fers were being more strongly limited by re-
source levels or other physiochemical factors
in the lake. Previous research has indicated
that small cladocerans like Bosmina are gen-
erally not effective predators on rotifers (re-
viewed in Gilbert 1988). The high densities of
cyclopoid copepods in our study were also
lower than those reported by Schneider and
Frost (1996) in their study systems, so the im-
pact of these crustaceans on the rotifers may
have been too low to elicit a “release re-
sponse” when the cyclopoid densities were re-
duced. The general increases and decreases in
rotifer densities could also be the result of an
unidentified “enclosure effect” affecting the
rotifers. However, since this effect was ex-
pressed across all of the enclosures indepen-
dently of treatment it should not affect our
Fish and Zooplankton Community Structure—Vessels and Jack 57
Rotifers
0.75
0.5
Population Growth Rates Day”
mg Fish
wo No Fish
ot
oa
me
Taxa
Figure 3. Population growth rates of the dominant rotifer species in fish and fishless enclosures in Chaney Lake,
Warren County, Kentucky (19 Jun 1999-1 Jul 1997). Bars show means and standard errors.
interpretation of the fish effects in these en-
closures.
The introduction of fish can have a pro-
found impact on a system like Chaney. Early
in the year, the entire Chaney basin is full, but
as the year progresses it often dries to nu-
merous smaller and disconnected ponds. If
fish like the golden minnows are trapped in
these pools, they could conceivably remove all
of the large zooplankton from a particular
pool. Many of the rotifers and crustaceans in
these small pools appear to have multiple gen-
erations before they produce diapause eggs. If
fish are introduced to a pool and severely re-
duce macrozooplankton densities, this could
constrain the next year s recruitment in that
pool. These pools may be colonized by zoo-
plankton from other areas during periods of
high water or there may be diapause eggs
from previous years that could hatch, but that
would be dependent on the vagaries of water
level and on the natural histories of the organ-
isms involved. If there are localized ecotypes
adapted for the particular conditions in a pool
or a closely associated group of pools, any
unique genetic information in that popula-
tion’s gene pool may be lost as a result of fish
predation. This information would probably
not be replaced by colonists from other areas.
The path by which the fish enter Chaney
may also be important. It is clear that fish may
enter Chaney by the estavelles, but it may also
be possible that they could enter the lake via
overland flow during flood events. The area
around Chaney contains at least one farm
pond that may become connected to the lake
during very high rainfall events. This would
greatly expand the pool of potential fish colo-
nists as fish that would be unable to survive in
or travel through the Lost River system could
enter Chaney in this manner. Very high den-
sities of fish could be introduced this way; they
could have an impact on the waterfowl and
other vertebrate groups (e.g., amphibians) that
use Chaney as breeding or feeding ground.
Previous studies have already documented
that waterfowl and fish are competitors for in-
vertebrate prey in other wetlands (Hanson and
58 Journal of the Kentucky Academy of Science 62(1)
Riggs 1995), and that the presence of fish may
reduce the prey available to birds that rely on
Chaney as a foraging area during their spring
migrations.
SUMMARY
Hydrology has long been identified as an
import: int ‘factor impacting organisms in
ephemeral lakes and pools. In C ff aney, how-
ever, fish may be present in even anal pools
with short duration since they may colonize
the lake during the high flood period when the
whole basin is inundated.
Our data indicate that fish predation has sig-
nificant effects on zooplankton community
structure in Chaney Lake, but the impact of
these effects on ecosystem level processes
such as nutrient cycling and microbial activity
remains unexplored. Temporary habitats like
Chaney provide tremendous natural laborato-
ries for inv estigating ecological processes at a
number of different scales. In karst terrenes
in particular, these lakes probably have land-
scape-level effects on water quality and trans-
port as well as local importance as centers for
aquatic biological production and biodiversity.
With many Bi these lakes threatened by de-
velopment it is crucial that we continue to
study these unique systems so that better
management and preservation strategies can
be devised to preserve the ecological integrity
of these remarkable habitats.
ACKNOWLEDGEMENTS
We gratefully acknowledge the assistance of
the following mndivicale Randall Kelley
helped in che: field; Joyce Bender and Debra
White of the Kentucky State Nature Preserves
Commission gave logistical assistance; Wayne
Mason provided information about the birds
at Chaney; Robert Hoyt identified the fish;
and Doug McElroy, Michael Stokes, and Da-
vid Jenkins made useful comments on earlier
versions of this paper. This work was support-
ed by a grant from the Kentucky State Nature
Preserves Commission to JD] and by support
from the Western Kentucky University Un-
dergraduate Honors Program to NV.
LITERATURE CITED
Carpenter S. R., J. F. Kitchell, and J. R. Hodgson. 1985.
Cascading trophic interactions and lake productivity.
Bioscience 35:634-639.
Carpenter S. R, J. F. Kitchell, J. R. Hodgson, P. A. Coch-
ran, J. J. Elser, M. M. Elser, D. M. Lodge, D. Kretch-
mer, X. He, N. VanEnde. 1987. Regulation of
lake primary productivity by food web structure. Ecol-
ogy 68: 1863-15876.
Diehl S. 1992. Fish predation and benthic community
and C.
structure: the role of omnivory and habitat complexity.
Ecology 73:1646-1661.
Gilbert, J. J. 1988. Suppression of rotifer populations by
Daphnia: A review of the evidence, the mechanisms
and the effects on zooplankton community structure.
Limnol & Oceanogr. 33:1286-1303.
Hanson, M. A., and M. B. Bulter. 1990, Early responses
of plankton and turbidity to biomanipulation in a shal-
low prairie lake. Hydrobiologia 200/201:317—327.
., and M. B. Bulter.
plankton, turbidity and macrophytes to biomanipulation
Canad. J. Fish. Aquatic Sci.
Hanson, M. A 1994. Responses of
in a shallow prairie lake.
51:1180-1188.
Hanson, M. A., and M. R. Riggs. 1995. Potential effects
of fish predation on wetland invertebrates: a compari-
son of wetlands with and without fathead minnows.
Wetlands 15:167—175.
Hrbacek J., M. Dvorkova, V. Korniekk, and L. Prochaz-
kova. 1961. Demonstration of the effect of fish stock of
the species composition of zooplankton and the inten-
sity of metabolism of the whole plankton association.
Verh. Int. Vereinigung Theor. Angew. Limnol. 14: 192—
195.
Jack, J. D., and J. J. Gilbert. 1993. Susceptibilities of dif-
ferent-sized ciliates to suppression by small and large
cladocerans. Freshwater Biol. 29:19—29.
Jack, J. D., and J. J. Gilbert. 1997. Effects of metazoan
predators on ciliates in freshwater plankton communi-
ties. J. Eukary. Microbiol. 44:194-199.
Kelley, R., and J. D. Jack. 2000. A survey of physical pa-
rameters and nutrient concentrations of an ephemeral
karst lake in the Lost River Groundwater Basin, Ken-
tucky. Aquatic Ecol. 34:77-89.
Kerfoot, W. C., and M. Lynch. 1987. Branchiopod com-
munities: associations with planktivorous fish in time
and space. Pages 367-378 in W. C. Kerfoot and A. Sih
(eds). Predation: direct and indirect impacts on aquatic
communities. Univ. Press of New England, Hanover,
NH.
Krieger K. A., and D. M. Klarer. 1991. Zooplankton dy-
namics in a Great Lakes coastal marsh. Great Lakes
Res. 17:255-269.
Schneider, D. W., and T. W. Frost. 1996. Habitat duration
and community structure in temporary ponds. North
Am. Benthol. Soc. 15:64—86.
Shapiro J., and D. J. Wright. 1984. Lake restoration by
biomanipulation: Round Lake, Minnesota, the first 2
years. Freshwater Biol. 14:371-383.
Taylor, B. E., D. L. and R. A. Estes. 1989. Zoo-
plankton production in a Carolina Bay. Pages 425-435
in R. R. Sharitz and J. W. Gibbons (eds). Freshwater
Mahoney,
Fish and Zooplankton Community Structure—Vessels and Jack 59
wetlands and wildlife. US Department of Energy Sym-
posium Series 61.
Timms, R. M., and B. Moss. 1984. Prevention of growth
of potentially dense phytoplankton populations by zoo-
plankton grazing, in the presence of zooplanktivorous
fish, in a shallow wetland ecosystem. Limnol. Oceanogr.
29:472-486.
Vanni M. J., C. Leucke, J. F. Kitchell, and J. J. Magnuson.
1990. Food web effects on phytoplankton in Lake Men-
dota, Wisconsin, USA: effects of massive fish mortality.
Hydrobiologia 200/201:329-336.
Wiggins, G. B., R. J. MacKay, and I. M. Smith. 1980.
Evolutionary and ecological strategies of animals in an-
nual temporary pools. Arch. Hydrobiol Suppl. 58:97—
206.
Wilbur, H. M. 1997. Experimental ecology of food webs:
complex systems in temporary ponds. Ecology 78:2279—
2302.
J. Ky. Acad. Sci. 62(1):60-69. 2001.
A Historiography of Archaeological Research in the Mammoth Cave
Area of Kentucky: 1824-2000
Kenneth C. Carstens
Department of Geosciences, Murray State University, Murray, Kentucky 42071
ABSTRACT
Archaeological interest in the Mammoth Cave
area of Kentucky has been ongoing since the early 19th
century, primarily because of the unique preservation offered at the underground cave sites. In this paper
[| examine almost 200 years of archaeological research conducted in the area. The paper loosely adheres to
historical divisions first presented by Schwartz and later by Willey and Sablof.
INTRODUCTION
Examination of the history of archaeological
study in the Mammoth Cave region of Scie
central Kentucky reflects par allel deve ‘lopment
with the growth of archaeology in North
America (Guinane 1967: Willey
1993), but it also demonstrates why additional
intensive and systematic archaeological study
should to be conducted in this very “significant
archaeological region. In this paper I “provide
an historical overview of archaeological re-
search that has taken place in and around
Mammoth Cave National Park. The paper
loosely adheres to historical divisions first pre-
sented by Schwartz (1967) and expanded by
Willey and Sabloff (1993).
The Speculative Period: Pre-1915
One of the earliest archaeological records
pertaining to the central Kentucky karst area
was written in 1824 by Constantine Samuel
Rafinesque (1824). Rafinesque was deeply in-
terested in prehistoric remains of the Ohio
Valley (Stout and Lewis 1995:83-90). Accord-
ing to Col. Bennett Young (1910:18), Rafin-
esque claimed to have located 148 ancient
sites (settlements) and 505 monuments in a
41-county area of Kentucky, speculating as
with other early 19th century naturalists about
the origin of these “natural” curiosities. Raf-
ine sque’s entry for the central Kentucky karst
lists “shell mounds along Green River and
mummies in caves.”
Following Rafinesque’s initial inquiry into
Kentucky's prehistory, there appears to be an
absence of related literature about the antiq-
uities of the area. This is not to say that inter-
est in antiquities had died; it had not. Accord-
ing to Col. Bennett Young (1910), increased
‘and Sabloff
60
farming activity and, in general, disruption of
the land due to population growth, caused an
escalation in destruction and looting of pre-
historic sites. By 1870, the collecting, selling,
and smuggling of antiquities in Kentucky was
a major profession. Although the Mammoth
Cave area is known mostly for its large cave
system, the archaeological contents of the area
offered a variety of artifacts and desiccated
human remains for collecting and selling.
Finds, such as Fawn Hoof in 1813, Scudder’s
Mummy in 1814, Little Al in 1875, and Lost
John in 1935, helped make the Mammoth
Cave area famous (Meloy 1968). During the
mid-19th and early 20th centuries, many in-
dividuals explored nearby cave systems looking
for mummies and Indian relics to sell (see
Young 1910). Unfortunately, this dilettantish
pastime stopped only in those caves that came
under the pr otection of the National Park Ser-
vice (NPS) after 1940 (e.g., Salts, Mammoth,
Longs, Bedquilt, and Lee caves); even then,
infrequent looting of caves within the National
Park still occurred.
The earliest historic date known from inside
Salts Cave is 1809 (Watson et al. 1969:7).
Dates and names upon various signature rocks
in Mammoth and Salts caves indicate that the
majority of historic caving dates “from the last
quarter or so of the 19th century to the first
quarter of the 20th century” (Watson et al.
1969:7: see also Watson 1974:21-23). The veg-
etal antiquities (e.g., textile bags, cordage, san-
dals) that could be found within the dry caves
were not preserved normally in surface or
“open” sites. Hence, those items were espe-
cially sought for collecting, smuggling, and
looting. As an example of smuggling, in 1874
or 1875 Louis Vial and some friends explored
Archaeological Research in the Mammoth Cave Area—Carstens 61
extensively in Salts Cave using a “new side en-
trance known only to themselves” (Watson et
al. 1969:7). During one of those cave trips
they found the * ‘Salts Cave Mummy,” nick-
named incorrectly “Little Alice” (Robbins
1971, 1974; K. Tankersley et al. 1994; Watson
et al. 1969:7). More recent examinations by
the late Louise Robbins (1971:200—206) iden-
tified the sex and age of this individual to be
those of a 9-year-old male.
During the 1890s, men such as F. W. Put-
nam of the Peabody Museum, as well as local
Kentuckians such as Colonel Bennett Young,
T. F. Hazen, and W. D. Cutliff, made extensive
collections and/or purchased prehistoric ma-
terial from Salts and Mammoth caves. Young
(1910:300, 305) stated:
In 1893 Mr. Theodore F. Hazen ... opened a new
entrance into Salts Cave . . . [and] obtained many in-
teresting relics ... about the present entrance [Salts
Sink], numerous spalls, flakes of flint, pestles, axes,
awls, and other implements have been found .. .
Young went on to describe many artifacts
taken from within Salts and Mammoth caves,
such as cords of bark, hemp, cattail leaves, and
grass; basketwork; half-burmed cane torches:
corn cobs (probably modern); an aboriginal
ladder; wooden digging implements; cups,
Aches bowls, and water bottles made from
gourds and squash rinds; tobacco leaves and
seed pods (also probably modern); and many
chert implements. The large collection of an-
tiquities Young acquired was sold to the Mu-
seum of the American Indian, Heye Founda-
tion, New York (Schwartz 195S8e; Watson
1974:167). Later, John M. Nelson, who was a
cave guide from 1894 to 1907, extensively col-
lected antiquities both from the caves and
from surrounding surface sites (Carey 1942;
Schwartz 1958f:3; Watson et al. 1969; Watson
1974). With the exception of the John M. Nel-
son collection, the other large private collec-
tions were either given or sold to the Ameri-
can Museum of Natural History, the Smith-
sonian Institution, or the Peabody Museum of
Archaeology and Ethnology. It was the Mam-
moth Cave Estates collection, donated to the
American Museum of Natural History in 1913,
that prompted Nels C. Nelson (no relation to
John M. Nelson) to engage in the “only sci-
entific archaeological investigations’ ’ (Schwartz
1958d) of the Mammoth Cave area up to that
time and usher in the Classificatory Period of
archaeological work (Schwartz 1967; Wille
and Sabloff 1993).
The Speculative Period focused initiall,
upon discovery, with only meager attempts to
offer explanations of deriv Aeon of the discov-
ered sites. Once they were discovered and
made known, the sites were vandalized and
exploited for private purposes. Whether pots,
“arrowheads,” or “mummies,” the market for
trafficking in North American antiquities had
begun. But it was from the seeds of site de-
struction that the first museum acquisitions
were made, ushering in professional archaeo-
logical work of the Classificatory Period.
The Classificatory Period: 1916-1960
Nels C. Nelson worked in Mammoth Cave
National Park during May and November
1916 as an archaeological representative of the
American Museum of Natural History. His
1917 report described the materials found
during his surface and cave reconnaissances
and excavations in the Mammoth Cave area.
Specifically, Nelson described and compared
his surface finds from the Mammoth Cave and
Eaton Valley fields to similar bifacial chipped
stone materials then being found in the
French Paleolithic (Nelson 1917:16—19, 1923).
In total, Nelson examined, through excavation
and/or other study, six of nine cave sites, six
of seven open-surface sites, and one of four
rockshelters (Nelson 1917:11).The latter num-
ber refers to the category of site types he re-
ported for the Mammoth Cave area. Douglas
W. Schwartz (1958d:1—2) stated that Neleons
main contribution was to “scientifically docu-
ment the presence in the caves of some classes
of material previously only reported by ama-
teurs.” Nelson also drew substantial conclu-
sions from his materials, despite the lack of
published reports concerning antiquities of
the area and the role of plant domestication
(he found large quantities of charred sunflow-
er seeds in his Mammoth Cave vestibule ex-
cavations) in the central Kentucky region. He
concluded that the Flint-Mammoth Cave sys-
tem had an economic importance to the N Na-
tive Americans, e.g., the quarrying of flint
(e.g., from Flint Alley in Mammoth Cave,
which has since been questioned [Munson et
al. 1989: Prentice 1993]); Nelson was not
aware that the Native Americans also exploit-
62 Journal of the Kentucky Academy of Science 62(1)
ed the caves for minerals (e.g., mirabilite, gyp-
sum, s.tin spar, and selenite; see Munson et
al. 1989: K. Tankersley 1996).
‘lson’s archaeological excavations inside
th vestibule of Mammoth Cave is his major
ork in the Mammoth Cave area. Although
this excavation was exploratory, it was ex-
tremely extensive and thorough. Nelson sank
a series of 10 test trenches that revealed mid-
den in two places. One was near the west wall
of the entrance; the other, some 40 feet from
the first, extended 50 feet back over the entire
entrance area. Although Nelson’s notes are at
times ambiguous, he demonstrated a strong
concern for the temporal and spatial location
of artifacts excavated (personal observation in
April 1975 of Nelson’s catalog record on file
with the American Museum of Natural His-
tory, New York).
Nelson excavated almost all of the vestibule
entrance, but the number of artifacts found
was few. Douglas W. Schwartz (1958d) ex-
plained that ANG was probably the result of ex-
tensive looting that had occurred earlier
throughout the 19th century. It also may be
the result of Nelson’s recovery me sthods (no
screens were used) and/or extensive subsur-
face alterations resulting from cave commer-
cialization or previous saltpeter mining oper-
ations during the War of 1812 (Meloy 1968).
Any of these reasons may explain the paucity
of artifacts recovered from the Mammoth
Cave vestibule. Nelson did find and recognize
evidence of prehistoric diet in the form of an-
imal bone, sunflower seeds, and freshwater
molluses (Nelson 1917; Watson 1974:212). He
also found prehistoric tools such as bone awls,
bone flakers, antler points, tubes, stone pro-
jectile points, scrapers, ground stone imple-
ments, and items for personal adornment.
Most important, Nelson (1917:69) concluded
that two different cultures could be distin-
guished within his vestibule excavations. The
lowed or more “primitive” group was identified
yi Nelson as as archeologists would define
2 decades later (e.¢., Bitehie 1933) as the Ar-
chaic culture ie 1960a:133).
Only one other reference to Mammoth
Cave area prehistory appeared in print during
the first 2 decades of the 20th century. This
was a fleeting mention of a series of rockshel-
ter sites near what is now the western bound-
ary of Mammoth Cave National Park. The ref-
erence was made by C. B. Moore who visited
the Indian Hill rockshelter complex in 1915
(Moore 1916). Fortunately, shallow water con-
ditions on Green River forced Moore to ter-
minate his plunderous Green River expedition
near Indian Hill as his boat, The Gopher, was
too large to continue the journey upstream. In
1935, a newly discovered desiccated burial
within Mammoth Cave, known to the cave
guides as “Lost John,” brought additional ar-
Gree ological publicity to the area (Pond 1935,
1937). Mienae Pond and George Neumann’s
analysis of Lost John ( (Neumann 1938) consti-
tuted the only professional archaeological in-
quiry in the Mammoth Cave area between N.
C. Nelson’s 1916 work and the formation *
Mammoth Cave National Park (MCNP) i
1940 although several additional references te
caves and rockshelter sites in and around the
present boundary of the park appeared in
print intermittently (e.g., Fowke 1922; Funk-
houser and Webb 1932). With the final acqui-
sition of lands by the federal government on
25 Apr 1940, it ‘became a federal offense to
remove materials from cave interiors within
MCNP.
During the formation of MCNP, the Mam-
moth Cave National Park Association pur-
chased, from John M. Nelson, a collection of
prehistoric, historic, and geological specimens
that were subsequently donated to MCNP on
15 Jan 1942 (Carey 1942: 1). Henry A. Carey,
then of the Archaeology Department at the
University of Kentucky, was placed in charge
of cataloging the park’s new acquisitions. He
was Seeuiel by a new NPS employee, Jesse D.
Jennings (Carey 1942). Unfortunately, the ma-
jority of the : 25,000 specimens in the John M.
Nelson collection was without provenience.
Items in the collection had been bought from
the local area with no note made as to the
exact collecting location. Furthermore, Nelson
kept only “mental notes” for his more unusual
specimens. From the John M. Nelson collec-
tion, Henry Carey concluded (1) that the
MCNP area was utilized for an extensive pe-
riod of time by aboriginal peoples; (2) that a
typological sequence could be worked out for
the area by using the collection but extreme
caution should be used in drawing definitive
conclusions due to the lack of controlled lo-
cational data; and (3) that scientific archaeo-
logical excavations inside the caves and at se-
Archaeological Research in the Mammoth Cave Area—Carstens 63
lected surface sites should be started imme-
diately. Unfortunately, due to the start of
World War II, the Mammoth Cave collections
heralded for study by Carey were not exam-
ined again until 1957 when Douglas W.
Schwartz, from the University of Kentucky, ex-
amined the John M. Nelson materials and at-
tempted to relocate some of the surface sites
from which John Nelson had made his collec-
tions (Schwartz 1958f). Schwartz also brought
systematization to the study of Native Ameri-
can sites in MCNP and visited several major
museums in the East to study collections ac-
quired from the Mammoth Cave area at the
turn of the century (Schwartz 1958a—h). These
activities culminated in a series of valuable de-
scriptive reports (Schwartz 1958a—h) and oth-
er interpretive and popular accounts about the
archaeology of the area (Schwartz 1960a;
1965).
The Classificatory Period brought a logical,
scientific inquiry to the archaeology of the
Mammoth Cave area. With the first work of
Nelson in 1916, to the discovery of a desic-
cated individual (Lost John) in 1935, to the
systematic reporting of archaeological sites
above ground and below by Douglas Schwartz
during the late 1950s/early 1960s, the archae-
ology of the Mammoth Cave area yielded,
ever so slowly, evidence of very significant in-
formation about prehistoric cultural adapta-
tions and cultural processes. These later stud-
ies served as the foundation for investigations
by Patty Jo Watson, the Cave Research Foun-
dation, the National Park Service, and the II-
linois State Museum (Watson et ar 1969) dur-
ing the next period of archaeological devel-
opment.
The Explanatory/Interdisciplinary Period:
1960 to the Present
In 1942, Henry Carey emphasized the need
for further surface investigations and excava-
tions in MCNP, but little was accomplished
until the recent research efforts by Patty Jo
Watson and her associates (Brown 1977; Car-
stens 1974, 1975, 1976 1980; Carstens and
Watson 1996; Marquardt 1972a, 1972b, 1974;
Marquardt and Watson 1976, 1983; Robbins
1971; Wagner 1976; Watson et al. 1969; Wat-
son 1974). Whether you call it explanatory ar-
chaeology, processual archaeology, or even
post-processual archaeology, the post-1960 era
of interdisciplinary archaeological researc): in
the central Kentucky karst began to answer
many questions about the area’s prehistory anc
the avenues of cultural change and adaptation
through time and space.
Watson's archaeological work in MCNP be-
gan in 1962 when, in conjunction with the
Cave Research Foundation, the Illinois State
Museum, and MCNP, she initiated an archae-
ological reconnaissance of the large caves
within the Flint Mammoth Cave system (Car-
stens and Watson 1996: Watson et al. 1969:v).
Watson’s initial work was carried out primarily
in Salts Cave, but later research expanded into
other caves (e.g., Mammoth, Lee, and Bluff),
and to archaeological surface reconnaissance
(Carstens 1974, 1980). Watson’s reason for
studying the cultural materials from within the
caves was that data derived from those mate-
rials were highly relevant to the discovery of
dietary practices during the early agricultural
Late Archaic-Early Woodland period. Wat-
son’s research was expanded in April 1969 to
include, “excavation in Salts Cave Vestibule, a
search for and testing of possible surface sites
near Salts Sink, and recording of prehistoric
remains in other caves within the Park” (Wat-
son et al. 1969:v). Between 1973 and 1980,
Watson and her colleagues initiated compara-
tive studies at caves outside the park (e.g., Wy-
andotte Cave, Indiana, and Wolf River or Jag-
uar Cave, Tennessee) (Crothers 1986; Munson
and Munson 1990; Robbins et al. 1981; K.
Tankersley et al. 1994; S. Tankersley 1993).
She also obtained a more complete radiocar-
bon sequence from Salts and Mammoth caves,
excavated and floated a stratigraphic column
from Salts Cave vestibule; obtained pollen and
parasitological analyses from human paleofecal
specimens found within the cave, and took
pollen core samples from nearby sinkhole
ponds.
Aided in her research by scientists from
many different fields of study, Watson was able
to approach the archaeological problems of
the MCNP in a scientifically integrated man-
ner, a methodological approach she had
learned as a University of Chicago graduate
participating in Robert Braidwood’s_interdis-
ciplinary studies of agricultural origins in the
Near East. This approach led to some answers
and to many new questions, particularly with
respect to environmental changes and their
64 Journal of the Kentucky Academy of Science 62(1)
possible effects on the prehistoric inhabitants
of the study area. Watson and her colleagues
(e.c. Munson et al. 1989: K. Tankersley 1996:
K. Tankersley et al. 1985) documented that
historic people using the cave were mining
cave for minerals (e.g., mirabilite, gypsum,
selenite, and satin spar) and were simply ex-
ploring the cave system. She noted similar pat-
terns of cultural ‘eae s in portions of other
caves located inside (Lee and Bluff) and out-
side the park boundaries (e.g., Wyandotte Cave
in Indiana, and Big Bone and Jaguar caves in
Tennessee: Crothers 1986; Munson and Mun-
son 1990; Watson 1986:109-116).Although
Lee, Bluff, Wyandotte, and Jaguar caves are
not comp: arable in size to either Salts or Mam-
moth Cave, the data collected by Watson and
her colleagues clearly indicate that cave min-
ing and exploration were widespread activities
in this karstic region that probably began dur-
ing the Late Archaic (Crothers et al. n.d.;
Munson et al. 1989: Watson 1986; Watson
1974:221-232: Watson and Kennedy 1991).
The 50+ radiocarbon dates now available for
the Mammoth Cave archaeological project
clearly demonstrate the widespread prehistor-
ic use of caves over a very important and sim-
ilar time horizon (Kennedy 1990, 1996): that
of early agriculture in the ‘Late Archaic- Early
Woodland period (ca. 4000 to 2000 B.P.).
Watson's research between 1962 and 1980
in the Mammoth Cave region is unique for
two reasons: (1) it is the er time such sci-
entifically integrated archaeological deep-cave
research i been attempted in the eastern
U.S.; and (2) it provides an aspect of prehis-
toric ae process that was extremely im-
portant (i.e., the domestication of native
plants, evidence for which was not then being
found in “open” surface sites in the eastern
U.S.). Watson’s research continues in the
Mammoth Cave region.
As a part of the Watson research team be-
tween 1973 and 1975, my job was to docu-
ment the culture history evident in a sample
of 83 surface sites in and around MCNP., ex-
amining the techno-economies of several of
those sites diachronically and presenting a cul-
es historical context within which the sur-
face dwellers of the central Kentucky karst ex-
plored and exploited the large caves (Carstens
1980).
Between 1977 and 1987, MCNP witnessed
only intermittent archaeological research on
the park’s surface archaeology. Most of the
work accomplished included small, unrelated
cultural resource management surveys (e.g.,
Beditz 1979, 1981: Carstens 1977, 1978). Be-
tween 1981 and 1989, few archaeological pro-
jects were conducted on the surface of MCNP.
Exceptions are the work of Philip J. DiBlasi,
who investigated the 1920s homestead of
Floyd Collins (DiBlasi 1957a), a famous local
cave explorer, and George Crothers, who doc-
umented material left in Sand Cave where
Collins died in 1925 (Crothers 1981, 1983).
DiBlasi (1987b, 1996), working with the Cave
Rese on Foundation, also found in Salts Cave
a series of prehistoric pictographs and glyphs
previously undocumented. Other studies con-
cerning the human use of the cave system, and
of the people who were using the cave, fo-
cused on determining the exact nature of pre-
historic mineral procurement (K. Tankersley
1996), forensic examinations of the historic
findspots of mummies (K. Tankersley et al.
1994: S. Tankersley 1993), and a new and ex-
citing search for pathogenic microorganisms in
prehistoric and historic human feces and bodi-
ly fluids (Ruppert 1994; S. Tankersley 1993).
The most systematic undertaking to inven-
tory a representative sample of the park for
both historic and prehistoric cultural resources
was directed by NPS archeologist Guy Pren-
tice (1993). Although much of Prentice’s pre-
history is a summary of Nelson (1917),
Schwartz (1958a-g), Carstens (1980), and
Watson and Carstens’ (1982) site inventories,
Prentice adds new prehistoric and _ historic
sites to the overall resource inventory of the
park. As a result, Prentice (1994, 1996) was
able to offer a settlement synopsis of MCNP
for his doctoral dissertation that includes a hy-
pothetical seasonal round between the Big
Bend shell mound area and the Mammoth
Cave area.
In 1993, the Science and Resource Man-
agement Division at MCNP began a long-
term cultural resource inventory of all artifacts
(historic and prehistoric) within the main cave
in Mammoth Cave. This project is co-spon-
sored by the NPS and Earthwatch; the field
work for this project has been directed by Ken
Tankersley, Mary Kennedy, George Crothers,
Christine Hensley, and Bob Ward (Kennedy
1993: Crothers and Ward 1995). Using an
Archaeological Research in the Mammoth Cave Area—Carstens
65
Table 1. Archaeological Research in the Area of Mammoth Cave National Park, 1824 to the Present (not an exhaustive
list).
Speculative-pre-1915
Classificatory
1916-1970
Explanatory-Interdisciplinary
1971 to the present
Rafinesque (1824), Young (1910)
Carey (1942); Fowke (1922): Funkhouser and Webb (1932); Hanson
(1960); Meloy (1968); Moore (1916): Nelson (1917, 1923); Neumann
(1938); Pond (1935, 1938): Schwartz (1958a—h: 1960a, 1960b, 1965,
1967); Schwartz and Hanson (1961); Schwartz and Sloan (1958, 1960a,
1960b); Schwartz, Sloan, and Hanson (1960).
Beditz (1979, 1981): Carstens 1974, 1975, 1976, 1977, 1978. 1980): Car-
stens and Watson (1996): Crothers (1981, 1983): Grothers et al. n.d.:
Crothers and Ward (1995); DiBlasi (1987a, 1987b, 1996): Duffield
(1974); Hensley (1995, 1996); Kennedy (1990, 1993, 1996); Kennedy and
Watson (1997); Marquardt (1974); Molnar and Ward (1974); Munson et
al. (1989); Prentice (1993, 1994, 1996): Robbins (1971, 1974, 1980):
Robbins et al. (1981); Ruppert (1994); Schoenwetter (1974); K. Tank-
ersley et al. (1994); S. Tankersley (1993); Wagner (1976); Watson (1974,
1986, 1992); Watson et al. (1969); Watson and Carstens (1975, 1982):
Watson and Kennedy (1993).
Electronic Distance Measurement (EDM)
system, the Earthwatch team records the exact
location of every artifact noted within the sur-
veyed areas of the cave system. This makes it
possible to prepare density plots of aboriginal
activity within the cave system and to deter-
mine prehistoric use areas within the cave de-
spite 200 years of historic cave use and cave
disturbance to the aboriginal materials in
Mammoth Cave.
In 1992, Patty Jo Watson, Mary Kennedy,
Kristen Gremillion, and Kristin Sobolik began
a new study in Mammoth and Salts caves. This
new arena emphasized the collection of hu-
man paleofecal samples for radiocarbon dat-
ing, parasitological analysis, macro- and mi-
croethnobotanical studies, and _ biochemical
(hormonal) analysis. These studies would al-
low prehistoric fecal specimens to be sexed
and thereby enable a better understanding
about specific individuals who explored and
mined prehistoric Mammoth Cave (Watson
1992; Watson and Kennedy 1993).
In 1994, Christine Hensley and Tom Sus-
senbach, while working for the NPS in MCNP,
conducted excavations at the stairway rock-
shelter (Hensley 1995, 1996). The three radio-
carbon samples from Hensley’s excavations of
Feature 1 consistently place the site’s occu-
pation in the Early Woodland period, ca. 2170
to 2570 B.P., a date range quite comparable
to the majority of aboriginal use of Mammoth
and Salts caves (Hensley 1995:24, Table’ 1;
Kennedy 1990, 1996). Further, Paul Gardner
identified more than 5000 seeds of domestic,
semi-domestic, and wild chenopodium from
the nackeineliver occupation floor (Hensley
1995, 1996). Similar contractual ar chaeological
studies continue today through the supervision
of Bob Ward, cultural resource specialist at
MCNP and the assistance of Darlene Appel-
gate, archaeologist at Western Kentucky Uni-
versity (Appelgate pers. comm. 1 July 2000).
Analytically, the Explanatory/Interdisciplin-
ary (post-1960) era of archaeological research
has answered many questions about the Na-
tive Americans who explored and exploited
the environment and resources above and be-
low ground in the central Kentucky karst. Ini-
tial studies by Watson and her colleagues in
the early 1960s through 1980s focused upon
time-space and environmental reconstruction
sequences, then turned to more processual is-
sues while unraveling the prehistory of the
Mammoth Cave area. That work inspired oth-
er archeologists in Tennessee and Indiana to
test several of Watson’s observations and con-
clusions about the prehistory of Mammoth
Cave specifically, and prehistoric cultural pro-
cesses in general, finding that prehistoric ab-
original mining and exploration was a wide-
spread cultural phenomenon; it was not lim-
ited solely to MCNP or only to the Late Ar-
chaic-Early Woodland transition (e. g.,
Faulkner 1986). Furthermore, not only had
Watson and her associates confirmed and ex-
panded N. C. Nelson's initial observations
about the importance of plant cultivation in
the Mammoth Cave area, but they also went
far beyond, examining human paleofeces for
66 Journal of the Kentucky Academy of Science 62(1)
parasites and micro-organisms and determin-
ing w) ther prehistoric caving activities were
cearricd out by both sexes, chereen helping to
and more accurately describe,
Cave prehistory.
envy nde rH we
\iammoth ¢
DISCUSSION
The history of archaeology in the Mammoth
Cave area closely parallels the growth and de-
velopment of f archae ‘ological trends in North
America. From the Speculative to ie Classi-
ficatory to the Explanatory and Interdisciplin-
ary pe sriods, archaeological inquiry in the cen-
tral Ke ntucky karst hee demonstrated that the
uncommon preservation characteristics of the
cave environment provides unique insight into
human behavior (prehistoric and historic) that
may be more accessible than from open “sur-
face” sites. Table 1 also reflects that, along
with an increase in the intensity of cave ar-
chaeological investigation, a greater sophisti-
cation began once “interdisciplinary research
was initiated at the park (post-1960). That
work was initiated by Patty Jo Watson and her
associates and colleagues.
Early turn-of-the-century interests in cave
archaeology, primarily atheoretical, prompted
work at surface sites in the Mammoth Cave
area and led to speculation about the origins
of prehistoric cultural materials, sometimes
comparing them to the better-understood Eu-
ropean record (e.g., Nelson 1917; Young
1910).Assessing significance of and attempting
to order archaeological sites from within the
park area, both Anode ground and below, and
assessing Mammoth Cave collections held out-
side chee park, were the foci of the Classifica-
tory Period between 1916 and 1970, culmi-
nating in the summaries of Douglas W.
Gahennts (195Sa—h, 1960a, 1960b, 1965).
More recent work by Watson and her col-
leagues brought a theoretical and interdisci-
plinary framework to the archaeology of the
pé ark often reflecting various Themis promi-
nent in the “New Archaeology.” Within the
last decade cave art studies (DiBlasi 1996)
have added a cognitive, or post-processualist
research slant to fhe efforts begun by Watson’s
group. However, additional Pacenrch is still
needed in the Mammoth Cave area, above
ground and below. Only the tip of the prover-
bial iceberg at Mammoth Cave has been stud-
ied, whereas artifacts from surface sites and
from within the caves continue to be damaged
or stolen in spite of the security efforts of the
NPS. New. insights and new energies are
needed today to carry on the fascinating study
of the aboriginal and Euro-American people
who explore A and exploited the Kentucky un-
derworld.
ACKNOWLEDGEMENTS
Earlier readings of a shorter version of this
paper were made during the 1970s by my doc-
toral committee at W ashington University, St.
Louis. For their comments I am truly thank-
ful. This paper also has benefitted from con-
structive comments made by Kenneth Sassa-
man at University of South Carolina and Patty
Jo Watson at W ‘ashington University, St. Louis.
I thank the officials at MCNP for their past
and continued support of our archaeological
research at the park and the Department of
Geosciences at Murray State University. My
wife, Nancy Son Carstens, read and com-
mented on earlier versions of this paper,
thereby greatly improving it; however, errors
and omissions in this paper remain mine
alone.
LITERATURE CITED
Beditz, L. 1979. Archaeological reconnaissance and test-
ing of alternative JCCCC sites in Mammoth Cave Na-
tional Park. Manuscript on file, National Park Service,
Southeast Archaeological Center, Tallahassee, FL.
Beditz, L. 1981. Mammoth Cave National Park, Mam-
moth Cave, Kentucky: bluffline survey of the Childress
Farm/Great Onyx Job Corps Civilian Conservation
Center property. Manuscript on file, National Park Ser-
vice Southeast Archaeological Center, Tallahassee, FL.
Brown, J. 1977. The Elmore site surface collection: a pa-
leo-archaic lithic assemblage. Senior honors Thesis. De-
partment of Anthropology, Washington Univ., St. Louis,
MO.
Carey, H. 1942. Report on John M. Nelson collection.
U.S. Department of the Interior, National Park Service,
Mammoth Cave National Park Library, Mammoth
Cave, KY.
Carstens, K. 1974. Archaeological surface reconnaissance
Cave National Park, Kentucky. Master's
Thesis. Department of Anthropology, Washington
Univ., St. Louis, MO.
Carstens, K. 1975. Surface archaeology in Mammoth Cave
National Park, Kentucky. Paper presented to the 40th
annual mee ting of the Socie ty for American Archaeol-
of Mammoth
ogy, Dallas, TX
Carstens, kK. 1976.
Kentucky karst: a preliminary temporal ordering of sev-
Recent investigations in the central
Archaeological Research in the Mammoth Cave Area—Carstens 67
eral surface sites in the Mammoth Cave area, Kentucky.
Paper presented to the 55th annual meeting of the Cen-
tral States Anthropological Society, St. Louis, MO.
Carstens, K. 1977. Three Springs Pumphouse: an assess-
ment of damage. Manuscript on file, Mammoth Cave
National Park, Mammoth Cave, KY.
Carstens, K. 1978. Mammoth Cave National Park: ar-
chaeological survey of proposed water lines and sewers.
Manuscript on file, Southeast Archaeological Center,
Tallahassee, FL.
Carstens, K. 1980. Archaeological investigations in the
central Kentucky karst. Doctoral Dissertation. Depart-
ment of Anthropology, Washington Univ., St. Louis,
MO.
Carstens, K., and P. J. Watson (eds). 1996. Of caves and
shell mounds. Univ. Alabama Press, Tuscaloosa, AL.
Crothers, G. 1981. Archaeological investigations in Sand
Cave, Kentucky. Proc. Eighth Int. Congr. Speleol. 1:
374-376.
Crothers, G. 1983. Archaeological investigations in Sand
Cave, Kentucky. Bull. Natl. Speleol. Soc. 45:19-33.
Crothers, G. 1986. Final report on the survey and assess-
ment of the prehistoric and historic archaeological re-
mains in Big Bone Cave, Van Buren County, Tennessee.
Department of Anthropology, Univ. Tennessee, Knox-
ville, TN.
Crothers, G., C. Faulkner, J. Simek, P. J. Watson, and P.
Willey. n.d. Woodland Cave Archaeology. Pages 1-27 in
D. Anderson and R. Mainfort (eds). The Early Wood-
land Southeast. Univ. Alabama Press, Tuscaloosa, AL.
In press.
Crothers, G., and R. Ward. 1995. The NPS/Earthwatch
cultural resource survey: discerning patterns of prehis-
toric activity in main cave despite 200 years of historic
use. Paper presented at the Fourth Annual Science
Conference, Mammoth Cave National Park, Mammoth
Cave, KY.
DiBlasi, P. 1987a. Archaeological monitoring of the water
pipeline at the Floyd Collins complex: Manuscript on
file, National Park Service, Southeast Archaeological
Center, Tallhasssee, FL.
DiBlasi, P. 1987b. Drawings found in Salts Cave. Cave
Res. Found. Newslett. 15(4):1—2.
DiBlasi, P. 1996. Prehistoric expressions from the central
Kentucky karst. Pages 40-47 in K. Carstens and P. J.
Watson (eds). Of caves and shell mounds. Univ. Ala-
bama Press, Tuscaloosa, AL.
Duffield, L. 1974. Nonhuman vertebrate remains from
Salts Cave vestibule. Pages 123-133 in P. J. Watson
(ed). Archaeology of the Mammoth Cave Area. Aca-
demic Press, New York, NY.
Faulkner, C. (ed). 1986. The prehistoric Native American
art of Mud Glyph Cave. Univ. Tennessee Press, Knox-
ville, TN.
Fowke, G. 1922. Archaeological investigations. Part I.
Cave explorations in the Ozark Region of central Mis-
souri. Part II. Cave explorations in other states. Bull.
Bur. Am. Ethnol. 76.
Funkhouser, W., and W. Webb. 1932. Archaeologica! sur
vey in Kentucky. Univ. Kentucky Rep. Anthropol. Ar
chaeol. 2.
Hanson, L. 1960. The analysis, distribution and seriation
of pottery from the Green River drainage as a basis for
an archaeological sequence of that area. Unpublished
manuscript, Office of State Archaeology, Univ. Ken-
tucky, Lexington, KY.
Hensley, C. 1995. Archaeological investigations at the
Stairway Rockshelter. Paper presented at the Fourth
Annual Science Conference, Mammoth Cave National
Park, Mammoth Cave, KY.
Hensley, C. 1996. The Stairway Shelter (15Ed303), Mam-
moth Cave National Park. Paper presented at the 13th
Annual Kentucky Heritage Council Archaeological
Conference, Frankfort, KY. 4
Kennedy, M. 1990. An analysis of the radiocarbon dates
from Salts and Mammoth caves, Mammoth Cave Na-
tional Park, Kentucky. Master's Thesis. Department of
Anthropology, Washington Univ., St. Louis, MO.
Kennedy, M. 1993. NPS and Earthwatch cultural resource
inventory of Mammoth Cave. Cave Res. Found. News-
lett. 21(4):15.
Kennedy, M. 1996. Radiocarbon dates from Salts and
Mammoth caves. Pages 48-81 in K. Carstens and P. IJ:
Watson (eds). Of caves and shell mounds. Univ. Ala-
bama Press, Tuscaloosa, AL.
Kennedy, M., and P. J. Watson. 1997. The chronology of
early agriculture and intensive mineral mining in the
Salts Cave and Mammoth Cave region, Mammoth Cave
National Park, Kentucky. Bull. Natl. Speleol. Soc. 59(1):
5-9.
Marquardt, W. 1972a. Recent investigations in a western
Kentucky shell mound. A research report read 4 May
1972 at the Annual Meeting, Society for American Ar-
chaeology, Miami Beach, FL.
Marquardt, W. 1972b. Research report on excavations at
the Carlston Annis Mound. Newslett. Southeast. Ar-
chaeol. Conf. 16(2):45.
Marquardt, W. 1974. A statistical analysis of constituents
in human paleofecal specimens from Mammoth Cave.
Pages 193-209 in P. J. Watson (ed). Archaeology of the
Mammoth Cave area. Academic Press, New York, NY.
Marquardt, W., and P. J. Watson. 1976. Excavation and
recovery of biological remains from two archaic shell
middens in western Kentucky. Paper presented in a
symposium, “The research potential of shell middens:
methodological and analytical considerations,” orga-
nized by Thomas Ryan. Southeastern Archaeological
Conference, Tuscaloosa, AL.
Marquardt, W., and P. J. Watson. 1983. The shell mound
archaic of western Kentucky. Pages 323-339 in J. L.
Phillips and J. A. Brown (eds). Archaic hunters and
gatherers in the American Midwest. Academic Press,
New York, NY.
Meloy, H. 1968. Mummies of Mammoth Cave. Micron,
Shelbyville, IN.
Molnar, S., and S. Ward. 1974. Dental remains from Salts
68 Journal of the Kentucky Academy of Science 62(1)
Cave vestibule. Pages 163-166 in P. J. Watson (ed). The
archaeology of the Mammoth Cave area. Academic
Py New York, NY.
Me |G
itucky: certain aboriginal sites on lower Ohio River.
\cad. Nat. Sci. Philadelphia, ser. 2, 16(3).
and C. Munson. 1990. The prehistoric and
1916. Some aboriginal sites on Green River,
VMiunson, P.,
early historic archaeology of Wyandotte Cave and other
caves in southern Indiana. Indiana Historical Society,
Prehistoric Research Series, Indianapolis, IN.
Munson, P., K. Tankersley, C. Munson, and P. J. Watson.
1989. Prehistoric selenite and satin spar mining in the
Mammoth Cave system, Kentucky. Midcontinental J.
Archaeol. 14(2):119-145.
Nelson, N.
Mammoth Cave and vicinity, Kentucky. Anthropol. Pa-
pers Am. Mus. Nat. Hist. 22(1).
Nelson, N. 1923. Kentucky: Mammoth Cave and vicinity.
Unpublished manuscript on file at the American Mu-
seum of Natural History, New York, NY.
Neumann, G. 1938. The human remains from Mammoth
Cave. Am. Antiq. 3:339-353.
1917. Contributions to the archaeology of
Pond, A. 1935. Report of preliminary survey of important
archaeological discovery at Mammoth Cave, Kentucky.
Wisconsin Archeol. 15:27—35.
Pond, A. 1937. Lost John of mummy ledge. Nat. Hist. 39:
176-184.
Prentice, G. 1993. Mammoth Cave National Park: over-
view and assessment. Vols. I, Il. Southeast Archaeolog-
ical Center, National Park Service, Tallahassee, FL.
Prentice, G. 1994. A settlement pattern analysis of pre-
historic sites in Mammoth Cave National Park, Ken-
tucky. Doctoral Dissertation. Department of Anthro-
pology, Univ. Florida, Gainesville, FL.
Prentice, G. 1996. Site distribution modeling for Mam-
moth Cave. Pages 12-32 in K. Carstens and P. J. Wat-
son (eds). Of caves and shell mounds. Univ. Alabama
Press, Tuscaloosa, AL.
Rafinesque, S. 1824. Ancient history, or annals of Ken-
tucky: introduction to the history and antiquities of the
state of Kentucky. Author, Frankfort, KY.
Ritchie, W. 1933. The Lamoka Lake site. Res. Trans. New
York State Archaeol. Assoc. Lewis H. Morgan Chapter
7(A4).
Robbins, L. 1971. A woodland “mummy” from Salts Cave,
Kentucky. Am. Antig. 36:200-206.
Robbins, L. 1974. Prehistoric people of the Mammoth
Cave area. Pages 137-162 in P. J. Watson (ed). Archae-
ology of the Mammoth Cave area. Academic Press,
New York, NY.
Robbins, L. 1980. Appendix V: Report on Blue Spring
Hollow Burial. Pages 473-477 in K. Carstens. Archae-
ological investigations in the central Kentucky karst.
Doctoral Dissertation. Department of Anthropology,
Washington Univ., St. Louis, MO.
Robbins, L., R. Wilson, and P. J. Watson. 1981. Paleon-
tology and archaeoology of Jaguar Cave, Tennessee.
Proc. VILIth Int. Congr. Speleol. 1:377—380.
Ruppert, L. 1994. Evidence for the endoparasite Giardia
lamblia in human paleofeces from Salts Cave, Mam-
moth Cave National Park, Kentucky. Master's thesis,
Department of Anthropology, Western Michigan Univ.,
Kalamazoo, MI.
Schoenwetter, J. 1974. Pollen analysis of human paleofe-
ces from upper Salts Cave. Pages 97—105 in P. J. Watson
(ed). Archaeology of the Mammoth Cave area. Academ-
ic Press, New York, NY.
Schwartz, D. 195S8a. Sandals and textiles from Mammoth
Cave National Park. Manuscript, Mammoth Cave Na-
tional Park Library, Mammoth Cave, KY.
Schwartz, D. 195S8b. Archaeological report on materials in
the John M. Nelson collection from Mammoth Cave
National Park. Manuscript, Mammoth Cave National
Park Library, Mammoth Cave, KY.
Schwartz, D. 1958c. An archaeological report on physical
remains from Mammoth Cave National Park. Manu-
script, Mammoth Cave National Park Library, Mam-
moth Cave, KY.
Schwartz, D. 1958d. Summary and evaluation of the 1916
American Museum archaeological work in Mammoth
Cave National Park. Manuscript, Mammoth Cave Na-
tional Park Library, Mammoth Cave, KY.
Schwartz, D. 1958e. Description and analysis of museum
materials from Mammoth Cave National Park. Manu-
script, Mammoth Cave National Park Library, Mam-
moth Cave, KY.
Schwartz, D. 1958f. Archaeological survey of Mammoth
Cave National Park. Manuscript, Mammoth Cave Na-
tional Park Library, Mammoth Cave, KY.
Schwartz, D. 1958g. Report on two radiocarbon dates
from Mammoth Cave, Kentucky. Manuscript, Mam-
moth Cave National Park Library, Mammoth Cave, KY.
Schwartz, D. 1958h. The archaeology of Mammoth Cave
National Park. Manuscript, Mammoth Cave National
Park Library, Mammoth Cave, KY.
Schwartz, D. 1960a. Prehistoric man in Mammoth Cave.
Sci. Am. 203:130—140.
Schwartz, D. 1960b. Archaeological survey of the Nolin
River reservoir. Manuscript, Museum of Anthropology,
Univ. Kentucky, Lexington, KY.
Schwartz, D. 1965. Prehistoric man in Mammoth Cave.
Eastern Natl. Park & Monument Assoc. Interpretive
Ser. 2.
Schwartz, D. 1967. Conceptions of Kentucky prehistory:
a case study in the history of archaeology. Stud. An-
thropol. Univ. Kentucky 6.
Schwartz, D., and L. Hanson. 1961. Archaeological exca-
vation in the Nolin Basin—1961. Manuscript, Office of
State Archaeology, Univ. Kentucky, Lexington, KY.
Schwartz, D., and T. Sloan. 1958. Excavation of the Rough
River site, Grayson County 12, Kentucky. Manuscript,
Office of State Archaeology, Univ. Kentucky, Lexington,
KY.
Schwartz, D., and T. Sloan. 1960a. Archaeological survey
of the Barren Reservoir. Manuscript, Office of State Ar-
chaeology, Univ. Kentucky, Lexington, KY.
Archaeological Research in the Mammoth Cave Area—Carstens 69
Schwartz, D., and T. Sloan. 1960b. Archaeological survey
of twenty-two small federal projects in Kentucky. Man-
uscript, Office of State Archaeology, Univ. Kentucky,
Lexington, KY.
Schwartz, D., T. Sloan, and L. Hanson. 1960. Test exca-
vations in the Nolin Basin—1960. Manuscript, Office of
State Archaeology, Univ. Kentucky, Lexington, KY.
Stout, C., and R. B. Lewis. 1995. Constantine Rafinesque
and the Canton site, a Mississippian town in Trigg
County, Kentucky. Southeast. Archaeol. 14(1):83-90.
Tankersley, K. 1996. Prehistoric mining in Mammoth
Cave. Pages 33-39 in K. Carstens and P. J. Watson
(eds). Of caves and shell mounds. Univ. Alabama Press,
Tuscaloosa, AL.
Tankersley, K., J. Bassett, and S. Frushour. 1985. A gourd
bowl from Salts Cave Kentucky. Tennessee Anthropol.
10:95-104.
Tankersley, K., S. Frushour, F. Nagy, and S. Tankersley.
1994. The archaeology of Mummy Valley, Salts Cave,
Mammoth Cave National Park, Kentucky. North Am.
Archaeol. 15(2):129-145.
Tankersley, S. 1993. Detection and recovery of anthro-
pogenic introduced pathogenic microorganisms in
Mammoth Cave, Mammoth Cave National Park, Ken-
tucky. Master's Thesis. Department of Anatomy, Wright
State Univ., Dayton, OH.
Wagner, G. 1976. An archeobotanical analysis of five sites
in the Mammoth Cave Area. Master's thesis, Depart-
ment of Anthropology, Washington Univ. St. Louis,
MO.
Watson, P. J. 1986. Prehistoric cavers of the eastern wood-
lands. Pages 109-116 in C. Faulkner (ed). The prehis-
toric Native American art of Mud Glyph Cave. Univ.
Tennessee Press, Knoxville, TN.
Watson, P. J. 1992. Pages 46-47 in Cave research archae-
ological project. Cave Res. Found. Annual Rep. 20.
Watson, P. J. (ed). 1974. Archaeology of the Mammoth
Cave area. Academic Press, New York, NY.
Watson, P. J., and K. Carstens. 1975. Archaeological re-
sources of Mammoth Cave National Park: a brief sum-
mary. Report prepared for the National Park Service,
Tallahassee, FL.
Watson, P. J., and K. Carstens. 1982. Archaeological sur-
vey and testing, Mammoth Cave National Park. An ar-
chaeological contract (#CX5000080976) between the
Cave Research Foundation and the National Park Ser-
vice. Southeast Archaeological Center, National Park
Service, Tallahassee, FL.
Watson, P. J., and M. Kennedy. 1991. The development
of horticulture in the eastern woodlands of North
American: women’s role. Pages 255-275 in J. Gero and
M. Conkey (eds). Engendering archaeology: women
and prehistory. Basil Blackwell, Oxford, England.
Watson, P. J., and M. Kennedy. 1993. Cave Research
Foundation archaeologial project, 1993. Cave Res.
Found. Annual Rep. 21:49—-50.
Watson, P. J., R. Yarnell, H. Meloy, W. Benninghoff, E.
Callen, A. Cockburn, H. Cutler, P. Parmalee, L. Pres-
cott, and W. White. 1969. The prehistory of Salts Cave,
Kentucky. Illinois State Mus. Rep. Invest. 16.
Willey, G., and J. Sabloff. 1993. A history of American
archaeology. W. H. Freeman & Co., San Francisco, CA.
Young, B. 1910. The prehistoric men of Kentucky. Publ.
Filson Club 25.
J. Ky.
Acad. Sci. 62(1):70-76. 2001.
Jsing Composts as Growth Media in Container Production
of Tomatoes
Brian D. Lacefield and Elmer Gray
Department of Agriculture, Western Kentucky University, Bowling Green, Kentucky 42101
ABSTRACT
During the 1996 and 1997 growing seasons, soil (S), brush composts (B), leaf composts (L), N-Viro Soil
(N), and 50:50 mixtures of these materials (S:B, S$:L, S:N, B:L, B:N, L
for their effects on seasonal distribution and total production for four tomato (Lycopersicon esculentum)
:N) by volume were compared
cultivars. Each growth medium was replicated in four containers (55 cm diameter, 38 em depth; ca. 64 liters
‘Celebrity’, Red Cherry’, and ‘Small Red Cherry.’
based upon weekly production of vine-ripened fruits by each plant from mid-July to mid-October. The growth
capacity). The cultivars were ‘Patio’, ‘Large Results were
media were similar in their effects on seasonal distribution and total fruit production. All growth media/
cultivar combinations gave continuous tomato production throughout the growing season. Cultivar differ-
ences were exhibited in both plant and fruit characteristics, permitting the container gardener to practice
individual preferences. Overall, the results support the practice of composting waste products for use in
container gardening.
INTRODUCTION
Sustainability of society is enhanced when
recurring Ww aste products are effectively sub-
stituted for diminishing natural resources. The
sustainable dimension of food production is
receiving public attention and tangible govern-
ment support (Hudson and Harsch 1991).
Composting is an age-old process for con-
verting organic residues into forms that are
more aesthetically acceptable and more avail-
able for plant utilization. Composting is re-
ceiving renewed support as a means of waste
disposal because the process reduces the vol-
ume of yard waste by a factor of five times or
more and results in a product suitable for gar-
den or landscape utilization (Fine 1989). In
1992. 85% of the 4.6 million tons of solid
waste produced in Kentucky were disposed in
landfills. The Environmental Protection Agen-
cy set a goal to reduce municipal solid waste
going into landfills by 25% (Environmental Al-
manac 1994). Since yard waste accounts for
ca. 18% of municipal solid waste, composting
is critical to efficient waste management.
Organic gardening is based upon the sub-
stitution of organic sources for inorganic
sources of nitrogen. Recent increases in de-
mand for organically grown food have expand-
ed markets for composted organic matter. Or-
ganic gardening varies in scale from individual
plant containers to full-sized family gardens
(Lindgren et al. 1990).
70
Urbanites have become increasingly in-
volved in gardening during recent years. They
utilize small plots or containers to provide on-
going supplies of fresh fruits and vegetable. In
Seletieann: gardening serves as a hobby that for
many people is a source of pleasure, pride,
and satisfaction. These benefits are not depen-
dent on garden size (Bartholomew 1981).
Tomato (Lycopersicon esculentum) is the
crop of choice by most urbanite gardeners.
Research has shown that tomato yields from
litter-enriched plots matured earlier and were
larger than those grown in commercially fer-
tilized plots (Brown et al. 1995).
The present study was part of an ongoing
program sponsored by the Department of Ag-
riculture, Western Kentucky University
(WKU), to convert local municipal waste into
forms usable in gardening and landscaping.
Our objectives were to compare different
waste composts for their effects on total and
seasonal distribution of production of diverse
tomato cultivars grown in containers.
MATERIALS AND PROCEDURES
Composts
Three locally available waste products were
evaluated. Brush- and leaf- -composts were pro-
duced from Bowling Green yard waste col-
lected in 1994. In a tree inventory of Bowling
Green, Martin (1994) identified a variety of
common deciduous trees including ash, elm,
Container Production of Tomatoes—Lacefield and Gray ral
Table 1. Nutritive value of composts used in container
production of tomatoes.
% Carbon:
“Nitrogen
Compost N P K Ratios
Brush (B) 0.99 0.08 0.48 30:1
Leaf (L) 0.88 0.04 0.42 Soul
N-Viro soil (N) 0.96 0.36 0.67 16:1
dogwood, maple, mulberry, oak, redbud, and
willow as well as numerous ornamental trees.
The sewage compost, known by the trade
name N-Viro Soil (Kovacik 1988), is prepared
by mixing treated sewage sludge with cement
kiln dust according to approved procedures.
The resulting moist mixture is aerated and
composted on an environmentally approved
site. The Pembroke silt loam soil, obtained
from the WKU farm, tested medium to high
in both phosphorus and potassium.
Containers
The study was based on container-culture to
permit greater experimental control of the
compost mixtures and to extend the applica-
bility of the results to container gardening.
Forty plastic barrel sections (58 cm diameter,
38 cm depth) were located in an unshaded
area. Containers were embedded in the soil to
reduce drying and were punctured in the bot-
tom to permit drainage. They were spaced 1.5
m apart in 5 rows and 8 columns. Each con-
tainer received ca. 64 liters of compost mix-
ture.
Growth Media
Soil and the three composts were usec
make 10 growth media; four consisted
100% each of soil (S), brush compost (B), lea’
compost (L), and N-Viro Soil (N), and six con-
sisted of 50:50 combinations by volume of the
soil compost materials (S:B, S:L, S:N, B:L,
B:N, L:N). All growth media were supple-
mented prior to transplanting with fertilizer at
the rate of 56.0, 24.5, and 46.5 kg/ha-t of N,
P, K, respectively. No additional fertilizer was
applied.
Cultivars
Four diverse tomato cultivars— Celebrity’,
‘Patio’", ‘Large Red Cherry’, and ‘Small Red
Cherry —were studied. ‘Celebrity’ is an inde-
terminate garden type that produces large
plants and large fruits. ‘Patio’ exhibits a com-
pact, determinate growth habit and is more
suitable for urban or “patio” production.
‘Large Red Cherry and ‘Small Red Cherry
are characterized by indeterminate growth
habit and smaller fruits.
Production
One plant, ca. 15 cm tall, was transplanted
in mid-May to each container. Vine-ripened
fruits were harvested twice a week beginning
in mid-July and continuing to mid-October.
Fruits from each plant were counted and
weighed. Data from the two harvests per week
were combined and reported as production on
a weekly basis. After the last regular harvest,
‘
Table 2. Season production of tomato fruits per plant in 1996, Bowling Green, KY.
Cultivar?
Growth
Media! C iP Mean® C P Mean
Number Weight (kg)
S 100 o2 76 13.3 497 9.14
B 64 68 66 9.55 6.96 8.26
L 92 58 75 15.34 3.6 9.47
N 87 By) 70 12.07 5.4 8.74
S-B 87 65 76 13.41 5.92 9.66
S-L 99 66 82 15.64 7.35 11.5
S-N 74 68 fall 10.3 6.52 S41
B-L 120 Bil 88 125 SUDIL 11.38
B-N 136 64 100 17.25 5.94 11.6
L-N 98 83 90 13.29 6.79 10.04
Mean® 95.7a 63.3b 79.4 13.74a 5.89b 9.82
Ԥ = soil, B = brush compost, L = leaf compost, N = N-Viro Soil:
>C = ‘Celebrity’, P = ‘Patio’.
3 Growth mixture means were not significantly different (P > 0.05); Cultivar fruit number and fruit weight means followed by the same letters are not
significantly different (P > 0.05).
72 Journal of the Kentucky Academy of Science 62(1)
Fruits/Plant
ane eh) Serer of eee ee
14 es * ‘Celebrity’
= +' iat | |
aes! |+'Patio' | |
12 f
e |
_2— ¥
10 } - \ —— {
| 4 o— ——— }
8 } = vA \ \
of / \
6 J ax . ;
4 | ° oe aT
Ts ae
2 es y rs ~} te
hae
0 a — = — ——
1 2 3 4 5 6 7 8 9 10 11 12
Week
Figure 1. Season distribution of number of fruits/plant for ‘Celebrity’ and ‘Patio’ tomatoes in 1996, Bowling Green,
Kentucky.
remaining green fruits were counted and In 1997, the addition of “Large Red Cherry
weighed.
Supplemental water
once or twice per week to prevent plant wilt-
ing. Support stakes placed in the periphery of
The containers were connected with loose-fit-
ting twine to provide plant support. Plants
were permitted to spread without any restric-
tive pruning.
Design and Analysis
The 10 growth media were replicated four
times in a randomized complete block design
(Steel and Torrie 1980). In 1996, ‘Celebrity’
and ‘Patio’ were studied, resulting in two rep-
lications of each cultivar per growth medium.
Fruit/Plant (kg.)
was applied usually
and ‘Small Red Cherry’ resulted in one repli-
cation for each cultivar per growth medium.
Data analyses were directed toward both sea-
sonal distribution and total production of
number and weight of fruits.
RESULTS
Compost Analysis
Nutritive values for the brush- and leaf-
composts were about equal for N (ca. 1%), P
(trace), and K (0.45%), whereas N-Viro Soil
had a similar level of N (ca. 1%) but higher
levels of P (0.56%) and K (0.67%) (Table 1).
Variance among the C:N ratios was the most
important difference in nutritive value of the
-©'Celebrity’
+ 'Patio'
‘ a)
Figure 2.
Kentucky.
Week
Season distribution of weight of fruits/plant for ‘Celebrity and ‘Patio’ tomatoes in 1996, Bowling Green,
Container Production of Tomatoes—Lacefield and Gray
Table 3. Season production of tomato fruits per plant in 1997, Bowling Green, KY.
Cultivar
Growth — ee See =
Mixture! (e 1p LRC SRC Mean® Cc P LRC SRC Mean
Number Weight (kg)
S 60 ol 525 940 394 5.15 2.42 8.18 4.0] 4.94
B dl 76 67 1082 319 7.19 3.2] 1.26 a2 4,22
L 9] 34 383 710 304 9.68 4.44 5.94 4 6.02
N 73 34 408 980 374 10.17 3.84 6.34 4.54 6.22
S-B 45 60 362 765 308 7.06 6.08 6.06 4.13 5.96
S-L 80 28 270 786 291 9.31 1.91 4.19 3.92 4.83
S-N 47 Al 320 1017 356 5.2 SD) De, 4,92 4.7
B-L 92 45 344 794 319 11.68 3.69 6.57 4.03 6.49
B-N 39 40 457 1077 403 4.69 3.76 7.79 5.86 Day
L-N 57 32 353 899 335 8.91 3.79 5.71 3.88 5.56
Mean? 64c 44Ac 349b 905a 340 7.95a 3.66b 5.72ab 4.45b 5.45
'S = Soil, B = Brush Compost, L = Leaf Compost, N = N-Viro Soil.
2 ¢ = ‘Celebrity’, P = ‘Patio’, LRC = ‘Large Red Cherry’, SRC = ‘Small Red Cherry’.
5 Growth mixture means were not significantly different (P > 0.05); Cultivar fruit number and fruit weight means followed by the same letters are not
significantly different (P > 0.05).
composts. Ratios of 30:1, as exhibited in the
brush- and leaf-composts, immobilize avail-
able N and result in N starvation of the plants.
The C:N ratio of 16:1 for the N-Viro Soil
should not create N deficiency in plant
growth. The recommended level of fertilizer
for tomato production was applied to all
growth mixture to compensate for nutrient
differences.
1996 Season Production
Number and weight of fruits per plant are
given in Table 2. ‘Celebrity plants produced
significantly more fruits (ca. 96) than did ‘Pa-
tio’ plants (ca. 63). Average fruit weight per
‘
plant was significantly greater for ‘Celebrity
(13.74 kg) than for “Patio’ (5.89 kg). Thus, ‘Ce-
lebrity’ plants produced significantly more and
heavier fruits than did ‘Patio’ plants during
1996. Although there was variability among
the number and weight of fruits produced on
the different growth media, yield differences
associated with growth media were not signif-
icant. Analyses comparing groups of means,
i.e., those mixtures including soil vs. those that
did not, failed to detect any significant differ-
ences. Also, comparisons of growth media
means at different harvest dates during the
season failed to reveal any consistent differ-
ences.
Fruits/Plant
(0)
-@'Celebrity’
+'Patio'
Figure 3.
Kentucky.
Week
Season distribution of number of fruits/plant for ‘Celebrity’ and ‘Patio’ tomatoes in 1997, Bowling Green,
74 Journal of the Kentucky Academy of Science 62(1)
Fruits/Plant
140, _——_—_ ———___——
a: @LRC’
|+'SRC’
120 7 +'SRC
+—
100 y ae
7
80 + ¥ ~
+ er ——+. +
60 # 7 * ~ 4
° a
40 s
2
+ ~ A
20 - \+ ~ ——— ss
es e . So
+
0 ~——--— + -—---- -— = ~
1 2 3 4 5 6 7 8 9 10 1 12
Week
Figure 4. Season distribution of numbers of fruits/plant for “Large Red Cherry’ (LRC) and ‘Small Red Cherry’ (SMC)
tomatoes in 1997, Bowling Green,
Kentucky.
Since the growth media means did not dif-
fer significantly, yields were combined for
each cultivar in determining season distribu-
tions (Figures 1, 2). Fruit ripening began in
mid-July and continued until frost acoured in
mid-October. Peak production for both num-
bers and weights of fruits occurred in late Au-
gust and poukaed into early September. ‘Ce-
lebrity’ produced more and heavier fruits per
plant: than did ‘Patio’ during the second half
of the season.
1997 Season Production
Number and weight of fruits per plant for
each of the four auley ars are presented in Ta-
Fruit/Plant (kg)
ble 3. Both the number and weight of fruits
per plants of “Celebrity and ‘Patio’ were lower
in 1997 than in 1996. For number of fruits per
plant, “Small Red Cherry’ was highest (905),
‘Large Red Cherry’ was intermediate (349),
and “Celebrity and ‘Patio’ were lowest (64 and
44. respectively). Growth mixtures had no sig-
nificant effect on number of fruits. For weight
of fruits per plant. ‘Celebrity was highest
(7.95 ke), ‘Large Red Cherry was intermedi-
ate (5 72 kg), and ‘Patio’ and “Small Red Cher-
ry were lowest (3.66 and 4.45 kg, respective-
ly). Differences among number or weight of
fruits were not influenced significantly by
growth mixtures when such comparisons were
© 'Celebrity’
2 ea ae en ae + 'Patio' [a
Figure 5.
Kentucky.
Week
Season distribution of weight of fruits/plant for ‘Celebrity’ and “Patio” tomatoes in 1997, Bowling Green,
Container Production of Tomatoes—Lacefield and Gray
5 Fruit/Plant (kg)
*LRC
_ [SRC]
Figure 6. Season distribution of weight of fruits/plant for “Large Red Cherry’ (LRC) and ‘Small Red Cherry’
tomatoes in 1997, Bowling Green, Kentucky.
based upon either total season or individual
harvest period yields.
Growth mixture yields were combined for
each cultivar in determining season distribu-
tions (Figures 3-6). Fruit ripening continued
from mid-July throughout mid-October. For
‘Celebrity and ‘Patio’ the 1997 season distri-
butions of both number and weight of fruits
per plant were similar to those in 1996 with
the exceptions that ‘Patio’ production peaked
earlier in 1997 than in 1996. “Large Red Cher-
ry and ‘Small Red Cherry’ produced an abun-
dance of fruits throughout 1997. Peak produc-
tion occurred at week 6 (end of August) for
‘Small Red Cherry’, but no single period of
maximum production was exhibited by ‘Large
Red Cherry. For weight of fruits per plant,
yields were rather consistent for ‘Small Red
Cherry throughout the season. whereas
weight of fruits per plant decreased during
early September for “Large Red Cherry.’
End of Season Production
Following the first frost each year the un-
ripened fruits on each plant were counted and
weighed. In 1996, ‘Celebrity and ‘Patio’ av-
eraged 12.8 and 22.6 fruits weighing 0.68 and
0.76 kg per plant, respectively. In 1997, “Ce-
lebrity’, ‘Patio’, “Large Red Cherry’, and ‘Small
Red Cherry averaged 13.4, 23.7, 60.8, and
185.6 fruits weighing 0.72, 0.78, 0.48, and 0.51
kg per plant, respectively.
Week
(SMC)
DISCUSSION AND SUMMARY
These results indicate that composted com-
mon waste products, either alone or in mix-
ture, are suitable for growing tomatoes in con-
tainers. Since compost materials vary in nutri-
tive value and C:N ratios, composted g growth
media need to be supplemented with a com-
plete fertilizer (N, P, K) for protection against
nutrient deficiencies.
Cultivar selection is an important consider-
ation in container production of tomatoes. Our
present results indicate that cultivar charac-
teristics such as plant shape, plant size, and
fruit number and weight are consistent wheth-
er grown in an open garden or in containers.
The four cultivars exhibited different qualities
for container gardening. All cultivars produced
throughout the season and supported unrip-
ened fruits at the time of frost, thereby pro-
viding a continuous supply of fruits. ‘Celebrity’
was highly productive of large fruits as desired
for some purposes. However, its large, open
plants could be unsightly and problematic in
the urban landscape. ‘Patio’ was intermediate
in productivity and fruit size. Its compact plant
size would be desirable in a “patio” setting.
‘Large Red Cherry’ produced large numbers
of Aredia sized fruits throughout - the season.
Its spreading, open plant shape could be a lim-
itation in an urban setting. “Small Red Cherry
was a prolific producer of small fruits through-
out the season. However, smallness in fruits
76 Journal of the Kentucky Academy of Science 62(1)
and the vine-like plant type could limit its util-
ity.
“These preliminary results provide encour-
ac ent for using municipal waste products
beneficial purposes. The finding that the
different composts alone and in mixtures were
equally effective in producing tomatoes sug-
gests that a variety of composted waste prod-
ucts may be used successfully in gardening.
LITERATURE CITED
Bartholomew, M. 1981. Square foot gardening. Rodale
Press, Emmaus, PA.
Brown, I. E., C. H. Gilliam, R. L. Shumack, D. W. Porch,
and I. O'Donald. 1995. Comparison of broiler litter and
commercial fertilizer on production of tomato. J. Veg.
Crop Prod. 1(1):53-62.
Environmental Almanac. 1994. A. Hammond (ed). World
Resource Institute, Houghton Mifflin, Boston, MA.
Fine, S. 1989. Composting nature's garbage. World Watch
2(1):5-6.
Hudson, W. J., and J. Harsch. 1991. The basic principles
of sustainable agriculture. Coop. States Res. Serv.,
U.S.D.A., Washington, DC.
Kovacik, T. L. 1988. Sludge kiln dust makes fertilizer. Wa-
ter Engin. & Managem. (December):1-2.
Lindgren, D. T., D. H. Steinegger, F. P. Baxendale, and
]. E. Watkins. 1990. Organic gardening in the backyard.
Univ. Nebraska Coop. Ext. Serv, 681-548.
Martin, J. A., 1994. Street trees for Bowling Green, Ken-
tucky, Street Tree Inventory Program of the Kentucky
Division of Forestry. Division of Forestry, Department
for Natural Resources, Frankfort, KY.
Steel, R. G. D., and J. H. Torrie. 1980. Principles and
procedures of statistics, Ind ed. McGraw-Hill, New
York, NY.
]. Ky. Acad. Sci. 62(1):77-78. 2001.
BOOK REVIEW
Gary E. Dillard. 1999. Common Freshwater
Algae of the United States: An Illustrated
Key to the Genera (Excluding the Dia-
toms). J. Cramer in der Gebr. Borntraeger
Verlagsbuchhandlung, Berlin. 173 pages; il-
lus. ISBN 3-443-50026-9. Price not indicat-
ed.
Professor Gary E. Dillard put together this
book after many years of teaching courses on
the biology of algae at Western Kentucky Uni-
versity. His students were required to identify
genus algae from field collections. He found
that students had difficulty using published
keys and descriptions because of their lack of
familiarity with the technical terms used in
these keys to describe algal morphology. He
set out to produce this “user friendly” manual,
which avoids as much as possible discipline
specific language. His goal has not been fully
accomplished; there is still much technical jar-
gon in the book. The beginning student is un-
likely to be familiar with terms such as lorica,
epicone, hypocone, dendroid colony, and oth-
ers found throughout this manual. A simple
glossary would have been a most useful addi-
tion. Yet, this is the first simplified key to
freshwater algae to be published since Pres-
cott’s How to Know the Freshwater Algae
(1978), which today is hard to obtain.
The book starts with a statement of purpose
and a definition of “algae” as representing a
heterogeneous assemblage of oxygenic photo-
autotrophs that lack tissue differentiation and
contain chlorophyll a. Based on this definition,
algae include prokaryotic groups (the cyano-
bacteria and chloroxybacteria) as well as a
wide variety of phylogenetically unrelated eu-
karyotic groups. In this section the traditional
and modern systems of classification are brief-
ly mentioned. Since the purpose of the book
is to act as a key to identify algae only to the
generic level, Dillard did not find it necessary
to place the genera into higher categories (di-
vision, classes, orders). By doing this he also
avoids discussing the recent dramatic and
sometimes confusing changes in algal classifi-
cation. This first section of the book calls -at-
tention to the extensive bibliography for those
readers interested in phylogenetic relation-
~l
~l
ships among the algae or in proceeding to spe
cies identification.
The next section, on algal habitats and col-
lection methods, describes how to obtain qual-
itative samples with, for example, plankton
nets or artificial substrates, for the purpose of
conducting a survey of algal forms. There is
no description of standard quantitative meth-
ods.
The rest of the book is divided into nine
sections where genera are grouped by artificial
characteristics such as presence of flagella. By
this system phylogenetically related taxa may
not cluster together. The sections are I: Char-
ales, plant-like genera; II: unicellular flagellat-
ed genera; III: unicellular, non-flagellated gen-
era; IV: colonial, flagellated genera; V: eolonmal
non-flagellated genera; VI: unbranched fila-
mentous genera; VII: branched filamentous
genera; VIII: pseudoparenchymatous genera;
and IX: coenocytic or sac-like genera. ‘Within
each section, the dichotomous keys to the gen-
era are easy to follow, and each genus is illus-
trated with a detailed drawing. This manual
excludes diatoms and many genera that occur
largely in soil or aerial habitats.
Although the title of the book indicates that
it deals with algae “of the United States,” most
genera of algae are cosmopolitan in distribu-
tion and the book can find users worldwide.
There is a growing global demand for identi-
fication of freshwater algae. This demand is no
longer restricted to academic circles and phy-
cology classes. Identification of algae is a skill
valued by drinking-water utilities whose op-
erators are eaneeened with the presence of
possible taste-, odor-, or toxin-producing spe-
cies in their source water. It is also valued by
environmental regulatory agencies that use al-
gae as water quality nmgicatore Recently the
U. S. Environmental Protection Agency (EPA)
has added algae to its ~ Candidate Contami-
nant List” (CCL). This will increase the de-
mand for the identification of algae. Like the
students enrolled in the author’s algae class,
most people needing to identify common
freshwater algae lack knowledge of the tech-
nical jargon. Many of them currently use “pic-
ture keys,” partic ularly color charts available
78 Journal of the Kentucky Academy of Science 62(1)
from t! EPA that even have species names timely. It will be useful to anyone needing to
(not +s! genera) often associated with a pic- identify common freshwater algae to genus.
ture. this commonly leads to misidentifica- Miriam So Kannan
tioos since the important diagnostic features Department of Biological Sciences
not learned when one does not follow a Northern Kentucky University
vritten key. The publication of this manual is Highland Heights, Kentucky 41099
]. Ky. Acad. Sci. 62(1):79-88. 2001.
Abstracts of Some Papers Presented at the 2000 Annual Meeting of the Kentu. 4
Academy of Science
AGRICULTURAL SCIENCES
Insecticides from wild tomato: phase I—breeding, tri-
chome counts, and selection of tomato accessions.
GEORGE F. ANTONIOUS, Department of Plant and
Soil Science, Kentucky State University, Frankfort, KY
40601.
Among the thousands of secondary metabolites that un-
derlie the characteristic properties of higher plants are a
diverse assemblage of potentially toxic allelochemicals. Al-
lelochemicals are those natural products that affect the
growth, health, behavior, or population biology of mem-
bers of other species. These compounds may impart a
selective advantage to plants by inhibiting, repulsing, and
even killing non-adapted organisms thar may feed upon
or compete with the producing plant. Production of toxic
chemical compounds is one method by which trichomes
(leaf-hairs) can impart resistance. In the present investi-
gation morphological and chemical characteristics of two
glandular trichomes (type IV and type VI) of six wild to-
mato accessions of Lycopersicon hirsutum ip hirsutum,
four accessions of L. hirsutum f. glabratum, two acces-
sions of L. pennellii, and density of type VI glandular tri-
chomes of the commercial tomato L. esculentum cv. Fab-
ulous, are reported. Densities of type IV and VI glandular
trichomes varied among the accessions tested. Trichome
counts on the leaf surface were correlated to three types
of trichome exudates. Two methyl ketones (2-tridecanone
and 2-dodecanone), two sesquiterpenes (zingiberene and
elemine) and total glycolipids (sugar esters) in glandular
trichomes have been quantified per unit leaf area. Iden-
tifying the constituents of glandular trichomes was
achieved using chemical methods.
Residues of pyrethrins and piperonyl butoxide in soil,
water and on potato leaves. GEORGE F\ANTONIOUS*
and GAYATRI A. PATEL, Department of Plant and Soil
Science, Kentucky State University, Frankfort, KY 40601;
JOHN C. SNYDER, Department of Horticulture, Uni-
versity of Kentucky, Lexington, KY 40546.
Residues of pyrethrin- I (Py-1) and pyrethrin-II (Py-II),
the major insecticidal components of the pyrethrum daisy
(Tanacetum cinerariifolium), as well as residues of pipe-
ronyl butoxide (PBO, a pyrethrum synergist), were deter-
mined in soil and on potato foliage grown under field con-
ditions. A pyrethrum formulation “Multi-Purpose Insec-
ticide” containing the three active ingredients was sprayed
twice at the rate of 6 Ibs per acre of formulated product
(5.4 and 27.2 g ALI. of pyrethrins and PBO, respectively)
on potato foliage during the growing season. In soil, three
management practices (yard waste compost, grass filter
strips, and a no mulch treatment) were used to study the
impact of surface soil characteristics on the amount of
pyrethrins and PBO retained in soil. Soil samples and po-
tato leaves were collected at different time intervals after
79
spraying. Samples were purified and concentrated usii
solid-phase extraction columns containing C,,-octadecy!
bonded silica. Residues were quantified by high-perfor-
mance liquid chromatograph equipped with a UV detec-
tor. Following the first spray, the initial deposits were 0.18,
0.40 and 0.99 g/g potato leaves for Py-I, Py-II, and PBO,
respectively. Py-I and PBO residues in soil were higher in
compost treatments compared to no mulch treatments.
Effects of nitrogen fertilization on monoculture and bi-
culture cover crops in vegetable production. G. R.
CLINE,* A. F. SILVERNAIL, and K. KAUL, Community
Research Service, Kentucky State University, Frankfort,
KY 40601.
A four year experiment examined how winter cover
crops were affected by plus (+N) or minus (—N)
inorganic nitrogen (N)
previous
fertilization of sweet com (Zea
mays L.) and by kill dates associated with vegetable tillage
methods. Hairy vetch (Vicia villosa Roth) yields and ni-
trogen contents remained relatively constant in all years
and were not affected by nitrogen treatments. In the +N
treatment, yields of winter rye (Secale cereale L.) and a
vetch/rye biculture normally exceeded vetch yields. Nitro-
gen contents of vetch and biculture cover crops were gen-
erally similar and were greater than those of rye. In con-
trast to rye, vetch and biculture cover crop nitrogen con-
tents were similar in +N and —N treatments. Delaying
cover crop kill dates by eight days for no-till vegetables
increased vetch yields but did not affect vetch nitrogen
contents. In the biculture treatment, vetch competed bet-
ter with rye as nitrogen availability decreased. Total yields
of the biculture cover crop were generally greater in the
+N than in the —N treatment.
Assessment of genetic diversity within pawpaw (Asimi-
na triloba) patches. SHERI B. CRABTREE,* TERA M.
BONNEY, SNAKE C. JONES, and KIRK W. POMPER,
Land Grant Program, Kentucky State University, Frank-
fort, KY 40601- 9335.
The pawpaw (Asimina triloba) is a native tree fruit
found in the southeastern and midwestern United States:
it has great potential as a new high-value crop in these
areas. Kentucky State University is the site of the USDA
National Clonal Germplasm Repository for Asimina spp..
and our long-term goal is to develop a sampling strategy
to assess levels of genetic diversity in pawpaw across its
native range. The objective of this study was to determine
the level of genetic similarity among trees in pawpaw
patches. Since pawpaws sucker profusely from the roots,
our hypothesis is that pawpaw patches are at least partially
clonal. Pawpaw leaf samples were collected from three
different patches in Franklin County, Kentucky, in May
1999. DNA was extracted from the leaves, then analyzed
using either the inter simple sequence repeat PCR (ISSR-
PCR) or the random amplified polymorphic DNA meth-
SO Journal of the Kentucky Academy of Science 62(1)
odology 1e ISSR-PCR primer (UBC 855) yielded poly-
morphic markers in a subset of samples from patch #1
and» }\ APD primer (OPA-11) yielded polymorphic mark-
ers . subset of samples from patch #2. The identifica-
ti { marker polymorphisms suggests that the pawpaw
‘ches are not completely clonal. Primer screening and
uch evaluation will continue.
Influence of Cry9C Bacillus thuringiensis transformed
corn kernels on two stored product moth pests in the lab-
oratory. JEROME R. FAULKNER,* ANTHONY M.
HANLEY, BRYAN D. PRICE, and JOHN D. SEDLA-
CEK, Land-Grant Program, Kentucky State University,
Frankfort, KY 40601.
The Indian meal moth (IMM) and Angoumois grain
moth (AGM) are global pests of stored grains. Growing
concern regarding increasing resistance development to
insecticides by insects, perceived risks associated with res-
idues in foods, the Food Quality Protection Act of 1996,
and Montreal Protocol have focused research efforts on
alternative methods of pest control. Relatively recent de-
velopments in pest management of corn utilize transgenic
plants (rDNA-modified) containing Bacillus thuringiensis
(Bt) toxin genes. Bt CrylA(b) or Cry9C delta-endotoxin is
present in various tissues of transformed corn plants. It
was found recently that corn kernels of some CrylA(b) Bt
isolines cause reduced IMM and AGM emergence and
egg production. Some Cry9C isolines have been examined
for survivorship and development of IMM. However, fe-
cundity of IMM and all life history parameters of AGM
need to be examined. Thus, the objective of this research
was to quantify the effects of Cry9C transformed corn
kernels on IMM and AGM life histories. Experiments
were conducted at 27 + 1°C and =60% RH using Star-
link® Bt corn kemels (AgrEvo), its non-Bt isoline, and
topically applied Bt to the non-Bt kernels. Fifty eggs were
placed in ventilated pint jars containing 170 g of cracked
or whole corn for IMM and AGM, respectively. Adult
emergence and fecundity were lower for both IMM and
AGM in the Cry9C corm kernels and Bt treated seeds than
controls. Results are consistent with those obtained for
IMM and AGM reared on CrylA(b) transformed grain.
Impact of CrylAb transformed corn kernels on Indian
meal moth and Angoumois grain moth populations in farm
storage. ANTHONY M. HANLEY,* JOHN D. SEDLA-
CEK, BRYAN D. PRICE, and MICHAEL R. TINSLEY,
Community Research Service, Kentucky State University,
Frankfort, KY 40601.
Increased concern by consumers regarding chemical
residues in food products, the development of resistance
by stored grain insect pests to organophosphorus insecti-
cides, the Food Quality Protection Act of 1996, and other
federal regulations and international accords such as the
Montreal Protocol, have generated a need to examine new
control methods to assist or replace existing control man-
agement tactics of stored product insects utilizing several
biopesticides. Bacillus thuringiensis (Bt) is available for
use in stored grain, Currently, Dipel® is the only product
registered for use in stored grain environments against
Indian meal moth (IMM). Transgenic crops with insect
resistant characteristics used against insect pests have
been successful. One such example is transgenic Bt corn.
This study examines the efficacy of CrylAb transformed
Dekalb corn on Indian meal moth and Angoumois grain
moth (AGM) populations in on-farm bin storage. One
hundred bushels of Dekalb 679BTY (Bt+) and Dekalb
679 (Bt—) were added tol6 bins located at the Kentucky
State University Agricultural Research Farm in Franklin
County, KY. One thousand IMM and AGM eggs were
added to the bins twice to ensure infestation. Tempera-
tures were recorded weekly and adult moths were quan-
tified biweekly using sticky traps. Data from the sixth week
of observation indicated that populations of IMM were
twice as large in Bt— bins as those containing the Bt+
corn kernels. All data will be compiled at the finish of the
field season and results will be discussed relative to on-
farm storage capability and farmer impact.
Use of conservation tillage and cover crops for sustain-
able vegetable production. H. J. HRUSKA,* G. R.
CLINE, A. F. SILVERNAIL, and K. KAUL, Community
Research Service, Kentucky State University, Frankfort,
KY 40601.
Research began in 1999 to examine sustainable pro-
duction of bell peppers (Capsicum annuum) using con-
servation tillage and legume winter cover crops. Tillage
treatments included conventional tillage, strip-tillage, and
no-tillage, and winter covers consisted of hairy vetch (Vi-
cia villosa), winter rye (Secale cereale), and a vetch/rye
biculture. Pepper yields following the rye winter cover
crop were significantly reduced if inorganic nitrogen fer-
tilizer was not supplied. However, following vetch, yields
of peppers receiving no additional nitrogen were similar
to yields obtained in treatments receiving the recom-
mended rate of inorganic nitrogen fertilizer. Thus, vetch
supplied sufficient nitrogen to peppers in terms of yields.
Pepper yields following the biculture cover crop were in-
termediate between those obtained following vetch and
rye. When weeds were controlled manually, pepper yields
following biculture cover crops were similar among the
three tillage treatments, indicating that no-tillage and
strip-tillage could be used successfully if weeds were con-
trolled. With no-tillage, yields were reduced without weed
control but the reduction was less if twice the amount of
residual cover crop surface mulch was used. Without man-
ual weed control, pepper yields obtained using strip-tillage
were reduced regardless of metolachlor herbicide appli-
cation. It was concluded that a vetch winter cover crop
could satisfy nitrogen requirements of peppers and that
effective chemical or mechanical weed control methods
need to developed to grow peppers successfully using no-
tillage or strip-tillage.
Pesticide movement under field conditions: an over-
view. CHRISTINE LEE* and GEORGE F. ANTO-
Abstracts, 2000 Annual Meeting
NIOUS, Community Research Service, Department of
Plant and Soil Science, Kentucky State University, F rank-
fort, KY 40601.
Different management practices for growing vegetable
crops on highly erodible land (10% slope) have been eval-
uated by the Water Quality Project at Kentucky State Uni-
versity. Studies were conducted to determine the influ-
ence of landscape features and soil amendments on pes-
ticide movement into runoff and infiltration water. Three
soil treatments on a Lowell silty loam soil (pH 6.7, 2%
organic matter) were used to reduce soil erosion and sur-
face water runoff. Pesticides infiltration into the vadose
zone were monitored using pressure-vacuum lysimeters (n
= 27). Twelve tipping bucket metering units were used
to collect runoff. In 1998, three soil treatments were com-
pared: black plastic (BP) mulch, living fescue mulch (tall
fescue), and no-mulch treatments (NM, rototilled bare
soil). In 1999, living fescue mulch 30 cm wide was planted
between every cropping row (pepper intercropped with
tomato each in a row) to create multiple barriers to runoff.
Turf was also planted every other cropping row and both
treatments were compared with NM treatments. In year
2000, yard waste compost was used as a soil amendment.
Residues of pyrethrins (Py-I and Py-II) and piperonyl bu-
toxide (PBO) were quantified in soil and runoff water fol-
lowing spraying of a pyrethrum formulation “Multi-
Purpose Insecticide” containing Py-I, Py-II and PBO. Ac-
cordingly, the impact of the different soil mulches on the
horizontal and vertical movement of clomazone, dacthal,
endosulfan, and pyrethrins was measured and evaluated
under field conditions.
Recent advances in thin-layer chromatography of pes-
ticides. IESSHA MOORE,* HUMERA TAGUI, and
GEORGE ANTONIOUS, Department of Plant and Soil
Science, Kentucky State University, Frankfort, KY 40601.
Potential hazards to human health, food, soil, water, and
wildlife may be created by residues from some long-lived
pesticides that build up in the food chain ‘and cause wide-
spread contamination by pesticides. Thin-layer chroma-
tography (TLC) can be used widely to detect and quantify
residues of pesticides in various kind of samples such as
food, drinking water, environmental matrixes (soil,
groundwater and wastewater), biological materials, and to
detect low concentrations of active ingredients of pesti-
cides in their commercial formulations. The objective of
this study was to separate and detect pesticides and relat-
ed compounds using TLC plates. Methods for residue
analysis of carbofuran, pirimiphos-methyl, pyrethrins, and
piperonyl butoxide have been developed by KSU/Envi-
ronmental Toxicology research group using selected mo-
bile phases on silica gel plates. Hexane-ethyl acetate (80:
20) and hexane-benzene-acetone (80:20:10) were used as
mobile systems for best resolution. Orthophosphoric-tan-
nic acid reagent in acetone was used as chromogenic spray
reagent for simultaneous detection of pyrethrins and pi-
peronyl butoxide in environmental samples. Critical fac-
tors of the TLC procedure and stepwise confirmation of
positive results leading to flexibility of the methox
presented.
Sustainable soil management practices and quality
potato grown on erodible lands. GAYATRI A. PATEL,*
GEORGE F. ANTONIOUS, and CHRISTINE LEE, De-
partment of Plant and Soil Science, Kentucky State Uni-
versity, Frankfort, KY 40601; JOHN C. SNYDER, De-
partment of Horticulture, University of Kentucky, Lexing-
ton, KY 40546.
Land productivity can decline when top soil is lost. In
Kentucky, limited resource farmers often produce vege-
table crops on highly erodible lands. The objectives of this
study were 1) to quantify the impact of three soil man-
agement practices (SMPs) on quantity of potato produced
on erodible land, 2) to evaluate the performance of py-
rethrin and azadirachtin insecticides on potato tuber qual-
ity, and 3) to assess the impact of yard waste compost on
the chemical composition (ascorbic acid, free sugars, and
phenol contents) of potato tubers. Potatoes (Solanum tub-
erosum L. cv. Kennebec) were grown in a silty loam soil
of 10% slope. Plots (n = 18) were 3.7 m wide and 22 m
long, universal soil loss equation (USLE) standard plots,
with metal borders of 20 cm above ground level. Two bo-
tanical insecticides, a multi-purpose insecticide (contain-
ing pyrethrin 0.2%) and Neemix 4EC (containing 0.25%
azadirachtin) were sprayed twice on potato foliage during
each of two growing seasons (1997 and 1999) at the rec-
ommended rates of 6 lbs and 2 gallons per acre, respec-
tively. The SMPs were living fescue strips (FS) inter-
cropped between every other potato row, soil mixed with
yard waste compost (COM) and no mulch (NM) treat-
ment (roto-tilled bare soil). The experimental design was
a 2X 3 X 3 factorial with main factors of two insecticides
and three SMPs replicated three times. Potato rows (ori-
ented on the contour of the slope) and the three SMPs
were used as barriers to runoff. Average potato yield was
lowest in NM and FS and highest in COM treatments.
Yield obtained from the bottom of the plots was greater
than that obtained from the top of plots. Tuber defects
(rot, scab, sun green, hollow heart, necrosis, and vascular
discoloration) were significantly different between the two
growing seasons. The two insecticidal treatments and the
three SMPs used did not have much influence on tuber
defects.
The influence of fertilizer rate and application method
on early growth and development of container grown paw-
paw (Asimina triloba) seedlings. KIRK W. POMPER,*
EDDIE B. REED, and SNAKE C. JONES, Land Grant
Program, Kentucky State University, Frankfort, KY 40601-
2350.
The pawpaw (Asimina triloba) is a native American tree
fruit with potential as a new fruit crop and as an orna-
mental plant. Development of fertilizer rates and appli-
cation methods to facilitate rapid container production of
seedlings would be desirable to nurseries. A factorial
greenhouse experiment was conducted with treatments
82 Journal of the Kentucky
that incliled four levels of slow release fertilizer (either
0.3.8 ~.6 or 23 g of Osmocote per cubic foot) and three
level. of liquid feed fertilizer (0, 250 or 500 ppm Peters
20) 20P-20K). Seeds were sown in rootrainers with Pro-
! rowing medium that contained the slow release fer-
er treatment levels. After seedlings reached 2-3 leaves,
edlings were fertigated at 0, 250 or 500 ppm Peters
20N-20P-20K. The treatments were arranged in a split
plot design in three replicated blocks, where the main plot
effect was liquid feed, and subplot effect was slow release
fertilizer. There were 20 replicate seedlings per experi-
mental treatment combination. After 8 weeks, plants were
destructively harvested. Both liquid and slow release fer-
tilizer main effects significantly influenced pawpaw seed-
ling growth characteristics; however, interactions between
the main effects were also significant for all growth pa-
rameters except leaf number. Overall, the seedlings sub-
jected to the highest rate in both fertilizer methods
showed the greatest total dry mass, about three fold great-
er than control plants.
Effect of several beetle-active Bacillus thuringiensis
products on life history attributes of lesser grain borer,
Rhyzopertha dominica. BRYAN D. PRICE,* JOHN D.
SEDLACEK. and ANTHONY M. HANLEY, Community
Research Service, Kentucky State University, Frankfort,
KY 40601.
The lesser grain borer (Rhyzopertha dominica) (LGB),
causes extensive damage to stored grains, especially
wheat, and is considered a primary insect colonizer, feed-
ing on intact kernels and developing entirely inside the
grain. Artificial wheat kernels (pellets) were prepared in
our laboratory by combining ground wheat, corn starch,
wheat gluten and water. Pelleting techniques are a con-
venient way to examine the effects of various pesticides
and other compounds on life history attributes of inter-
nally feeding insects. The kernels were used to bioassay
several Bt products, Novodor™, Raven® and Foil™,
against the LGB, and were composed of 51% corn meal,
26% cor starch, 9% wheat gluten and 14% water. The
appropriate amount of each Bt product was added at a
concentration of 500 ppm active ingredient. Ten kernels
of each treatment, including control, were placed in five
vials. Eight LGB adults were placed into each vial, then
placed randomly in a small plastic container. The adults
were removed from the kernels after seven days and adult
mortality quantified. Surviving adults were then trans-
ferred to another set of vials containing untreated kernels
to determine any effect on fecundity. Both sets of vials
were observed until all progeny emerged, then the num-
ber of progeny and development time were determined.
There was no significant difference in adult survivorship
among the different Bt products, but preliminary data in-
dicates emergence from Raven and Foil treatments were
significantly reduced from control. Also, development
times were longer with those treatments. Fecundity data
will also be presented.
Academy of Science 62(1)
Influence of CrylAaAbAc2A Bacillus thuringiensis del-
ta-endotoxin on a non-target parasitoid, Habrobracon he-
betor LOUIE RIVERS I,* ANTHONY M. HANLEY,
BRYAN D. PRICE, and JOUN D, SEDLACEK, Land
Grant Program, Kentucky State University, Frankfort, KY
40601.
Interest in biological control of stored grain pests has
increased with decreasing efficacy of organophosphorus
insecticides, perceived risks of toxic residues, the Food
Quality Protection Act of 1996, and the Montreal Proto-
col, Bacillus thuringiensis (Dipel® [CrylAaAbAc2A]) has
been found to be effective against the Indian meal moth
(IMM) in stored grains. Habrobracon hebetor is an effi-
cient parasitoid of IMM. However, no studies have been
conducted to determine whether or not Bt and H. hebetor
are compatible methods of control. Thus, the objective of
this research is to quantify the impact of Bt on several H.
hebetor life history attributes. Ten treated larvae were
placed into three 20 ml plastic vials per treatment with
three replicates. Two male and one female H. hebetor
adults were added to each vial and allowed to oviposit for
24 hours. then were removed. Number of progeny and
longevity were determined. Progeny were placed in vials
in the previous ratio and allowed to oviposit on ten ad-
ditional larvae for 24 hours. Parasitoids were moved to
vials of fresh larvae daily until female death. Total number
of progeny and their development time were determined.
All rearing and experiments were conducted in an envi-
ronmental chamber at 27°C, =60% relative humidity and
in total darkness. Progeny production and longevity of F,
and F, individuals were the same between treatments.
Thus, it appears as though Dipel does not have a negative
impact on the parasitoids. Longer term experiments con-
stituting multiple generations should be performed as
should behavioral assays.
Insect fauna of ear corn stored in cribs on small farms
in Kentucky. JOHN D. SEDLACEK,* BRYAN D.
PRICE, and ANTHONY M. HANLEY, Kentucky State
University, Frankfort, KY 40601.
Storing ear corn in corn cribs is practiced by many small
and limited resource farmers in the central Kentucky area.
Approximately 53% of all corn cribs in Kentucky are lo-
cated in this region and as much as 30% of the total com
acreage and 75% of those storing corn on-farm in individ-
ual counties store it in this manner. Ear corn is more sus-
ceptible to attack by insects and fungi for the duration of
storage because it is completely exposed. This past storage
season we sampled ear corm in 15 corn cribs on small
farms in Casey, Christian, Franklin, and Metcalfe coun-
ties. Thus far we have identified 18 species or species
groups of beetles and 3 species of moth pests. The major
species of beetles are maize weevil, foreign grain beetle,
flat grain beetle, and hairy fungus beetles. The major moth
species were Indian meal moth and Angoumois grain
moth. Large numbers of parasitoids in the families Bra-
conidae and Pteromalidae were also found. Results will be
Abstracts, 2000 Annual Meeting
discussed relative to bin stored corn pests and potential
effects of transgenic Bt hybrids in storage.
CELLULAR & MOLECULAR BIOLOGY
Transcription factor isoform-specific regulation of pi-
tuitary hormone gene expression. SCOTT E. DIA-
MOND* and AMY L. FERRY, Department of Physiology,
University of Kentucky College of Medicine, Lexington,
KY 40536-0298.
We do not yet fully understand the mechanisms by
which related transcription factor isoforms with identical
DNA sequence specificity mediate distinct transcription
responses. Pit-1 and Pit-1b direct proper development of
and hormone expression by the anterior pituitary, and
constitute such a pair of transcription factor isoforms.
While Pit-1 and Pit-1b share identical DNA binding do-
mains, they differ by the splice-mediated insertion of the
26 amino acid b-domain in the transactivation domain.
Pit-1 and Pit-1b regulate prolactin gene expression in op-
posite ways; Pit-1 activates the prolactin promoter, yet Pit-
1b represses basal prolactin promoter activity as well as
Ras signaling to the prolactin promoter. We have previ-
ously demonstrated that the amino acid sequence of the
b-domain dictates isoform-specific repression. Here, we
utilize epitope- and alanine-scanning mutagenesis experi-
ments to identify specific residues of the b-domain inser-
tion that dictate repression of prolactin gene expression.
We demonstrate by pharmacological and molecular ge-
netic methods that b-isoform repression requires the ac-
tion of a histone deacetylase complex. In addition, we uti-
lize a chromatin immunoprecipitation assay to show that
Pit-1b specifically alters the histone acetylation state of the
prolactin promoter. These findings provide significant in-
sights into the structural determinants and mechanism of
an important example of transcription factor isoform-spe-
cific regulation of gene expression.
GEOLOGY
Nature and origin of the Cane Run Bed, Lexington
Limestone, central Kentucky. H. LISA JEWELL* and
FRANK R. ETTENSOHN, Department of Geological
Sciences, University of Kentucky, Lexington, KY 40506-
0053.
Much of the Middle Ordovician Lexington Limestone
represents coarse, bioclastic deposition on a shallow-wa-
ter, carbonate ramp subject to frequent storm perturba-
tion. In fact, position of the Lexington area in a subtrop-
ical, trade-wind belt on the southeast margin of Laurentia
during Middle Ordovician time supports the predomi-
nance of storm or tempestite deposition in the Lexington
Limestone. In contrast to most of the Lexington Lime-
stone, however, the Cane Run Bed, which occurs in the
uppermost Grier Member, is composed of interbedded
fine-grained limestones and shales, which exhibit second-
ary, soft-sediment deformation. Moreover, the Cane Run
grades laterally into coarser grained limestones of the Tan-
glewood and Grier members, which at the approximately
equivalent horizon are also locally deformed. Mapp
distribution of the fine-grained Cane Run Bed show -
it was deposited in a paleobathymetric low between
structural trends that formed high areas during Lexingt
deposition. Hence, the fine-grained nature of the Can Rui
Bed reflects storm deposition in deeper water, distal en-
vironments, while coeval parts of the Tanglewood and
Grier represent storm deposition in shallower waters on
adjacent, uplifted structural highs. The prominent soft-
sediment deformation in the Can Run Bed and its equiv-
alents not only provides correlation among different li-
thologies and facies, but indicates the necessity of likely
seismic activity for deformation (seismites) on one of the
structures. Presence of probable seismites in proximity to
local structures suggests reactivation of those structures
and is additional support for the impact of Taconian far-
field forces in the area during the ongoing Taconic tec-
tophase to the east.
Possible modern analogues to bryozoan bioherms in the
Tanglewood and Grier members, Lexington Limestone,
central Kentucky. JASON R. LAMBERT,* FRANK R.
ETTENSOHN, and ANDREA L. HOLBROOK, Depart-
ment of Geological Sciences, University of Kentucky, Lex-
ington, KY 40506-0053.
In equivalent parts of the Middle Ordovician Grier and
Tanglewood members of the Lexington Limestone, just
below the Brannon Member, a horizon of bryozoan bio-
herms is known from three localities. The bioherms are
sitting on a hardground surface, surrounded by coarse,
crossbedded, fossil-fragment calcarenites. The bioherms
are no more than a meter high and at most a meter and
a half in breadth. Upper portions of the bioherms are
composed of massive, but intricately encrusting platy
bryozoans, whereas lower parts typically show branching
or ramose bryozoans arranged around the base of the
bioherm. On the east-facing, oceanward side of San Sal-
vador Island, Bahamas, we observed within the surf zone
and in deeper shoreface waters red-algae-coral patch reefs
with some characteristics similar to those of the bioherms.
Although the patch reefs were up to a few tens of meters
in breadth and up to five meters in height, they were also
attached to a hardground and surrounded by moving skel-
etal sands. Upper parts of the reefs in the surf zone, es-
pecially where facing out to sea, were composed of en-
crusting red algae. Lower parts of the reefs below the surf
zone, and those reefs in deeper shoreface waters, were
composed of branching corals. Water depth and exposure
to the surf zone apparently controls the morphology (en-
crusting vs. branching) and taxonomic makeup of various
reef parts. Although sizes are an order of magnitude dif-
ferent, comparison of the two occurrences suggests that
the Ordovician bioherms occurred within an ancient surf
zone and that the different morphology and taxonomic
makeup of bryozoans on different parts of the bioherms
may reflect a similar zonation by depth. Hence, somewhat
similar modern analogues allow us to fully understand the
84 Journal of the Kentucky Academy of Science 62(1)
nature a lepositional environments of an unusual, bio-
herma! izon in the Lexington Limestone.
‘tonic control of Sunbury (Kinderhookian) and Bor-
d Osagean) deposition in northeastern Kentucky.
£ I )
(ARLES E. MASON,* Department of Physical Scienc-
Morehead State University, Morehead, KY 4035),
RANK R. ETTENSOHN, Department of Geological
Sciences, University of Kentucky, Lexington, KY 40506.
Deposition of the Sunbury and Borden formations in
northeastern Kentucky occurred during the fourth and fi-
nal tectophase ( (Sunbury Cycle of Ettensohn, 1994) of the
Acadian Orogeny. This Sunbury Cycle began in the Kin-
derhookian with an unconformity at the base of the Sun-
bury Shale. This break in deposition was in response to
convergence of a newly placed load (Avalon microplate)
on the eastern craton margin (Virginia promontory). This
event was followed by deformational loading throughout
most of remaining early Kinderhookian time, which re-
sulted in rapid subsidence of the Appalachian forland ba-
(west). The Sunbury
Shale was deposited during this time. By middle Kinder-
sin and its migration cratonward
hookian time, the loading-type relaxation phase of the
Sunbury Cycle began with deposition of the Henley Bed
of the F
phase reflects a deepening of the foreland basin and a
concomitant eastward shift of bulge migration. During lat-
est Kinderhookian time, carbonate turbidites were depos-
Farmers Member of the Borden Formation. This
ited in the basin, probably derived from the eastwardly
migrating bulge to the west. The clastic turbidites com-
Farmers Member, deposited during early Os-
agean time, had an eastern source as did sediments com-
posing the Nancy and Cowbell members of the Borden
posing the F
Formation. These members document the progradational
infilling of the forland basin by a coarsening-upward clas-
tic sequence during the loading-type relaxation phase of
eae
the Sunbury Cycle. The topmost member of the Borden
Formation, the Nada Member (upper Osagean) records
the reduction and ultimate cutoff of silicilastic sediments
from the highlands to the east, related to eastward bulge
uplift and migration combined with a regional eustatic
lowstand. Sediment reduction is most reflected in the
glauconite-rich Floyds Knob Bed in the Nada and equiv-
alent units.
New observations on Brachiospongia digitata (Hexac-
tinellidae, Porifera) from the Middle Ordovician of Cen-
tral Kentucky. DANIEL J. PHELPS,* Kentucky Paleon-
tological Society, Lexington, KY 40503; RICHARD
TODD HENDRICKS, Bardstown, KY 40004.
Recent discoveries of Brachiospongia digitata from the
Curdsville Member of the Lexington Limestone (Middle
Ordovician, Trentonian), shed light on the ecology and
taxonomy of Brachiospongia. Brachiospongia specimens
are present in an exposure of the Curdsville Member in
outcrops adjacent to the Kentucky River Fault Zone. In-
dividuals range from 8 to 35 cm in diameter and occur as
complete or macerated specimens in fining-upward se-
quences ranging from calcarenites and calcisiltites to or-
ganic-rich, fissile, shales. The sponges are filled with lith-
ified sediment; some are compacted and distorted. In one
bed, the sponges are in life position, and relatively undis-
torted. In other beds, sponges are associated with depres-
sions adjacent to lithified and bored mounds on hardg-
round surfaces. In these lenses, virtually all Brachiospon-
gia, even the largest specimens, are overturned or other-
wise displaced from life position. This suggests transport
and mutilation of the sponges during storm events. Faunas
associated with the sponges include bryozoans, dendritic
graptolites, crinoids, a paracrinoid, and other echino-
derms. Trilobites, including articulated specimens of Cer-
aurus sp., have been found inside Brachiospongia, sug-
gesting that trilobites interacted with sponges, perhaps for
shelter. Some specimens of B. digitata display areas in
which the body of the sponge is broken away to reveal an
internal mold or an internal structure that is covered with
tubercles and a thin layer of black materials. These tu-
bercles are similar to those found on Brachiospongia tub-
erculata (James). These details suggest that B. tuberculata
specimens represent internal molds of B. digitata, and
that B. tuberculata is synonymous with B. digitata.
HEALTH SCIENCES
Unintentional influence on diet quality of taste panel-
ists. MARTHA A. MARLETTE* and SUSAN B. TEM-
PLETON, Human Nutrition Program, Kentucky State
University, Frankfort, KY 40601.
A taste panel to determine the acceptance of popular
African-American foods modified to improve nutrient con-
tent was conducted for 10 weeks. Thirty-one African
Americans, 58% female and 71% under age 30, served as
panelists; 24 hr food recalls were collected from them at
the initial training session and during the exit interview.
Intakes were analyzed using Nutritionist V™. The panel-
ists were given charts indicating the calories, total fat, sat-
urated fat, cholesterol and dietary fiber content of the
foods to be evaluated. Panelists reported the same num-
ber of food items on both recalls. However, the quality of
dietary intake had improved in several areas, based on
Recommended Daily Values (RDV) for a 2000 keal diet.
Energy intake decreased from 123% to 104% RDYV, total
fat decreased from 161% to 115% RDYV, saturated fat de-
creased from 172% to 121% RDV, cholesterol decreased
from 118% to 79% RDYV, and fiber increased from 65%
to 75% RDV. These results suggest that panelists became
more aware of foods they were consuming and made bet-
ter food choices, because they were given fact sheets that
indicated the importance of a low fat, low cholesterol and
high fiber levels provided by the modified recipes. This
new knowledge on the need to reduce dietary fat and cho-
lesterol apparently improved the food choices made by
the panelists. However, these data do not indicate if these
reported dietary changes would be sustained by them over
time as no formal nutrition education was provided.
Abstracts, 2000 Annual Meeting 85
Lead and copper in tapwater of eastern Kentucky
homes: a pilot study. JOHN G. SHIBER, Division of Bi-
ological Sciences & Related Technologies, Kentucky Com-
munity & Technical College System/KCTCS, Prestons-
burg Community College, Prestonsburg, KY 41653.
One hundred nine Prestonsburg Community College
students, representing six eastern Kentucky counties, col-
lected two samples each of tapwater from their homes for
lead and copper analysis. The first sample was taken from
their kitchen faucets (cold water tap), before anyone had
used it that day (B), and the second from the same faucet,
after the water had been used for a few hours (A). Sev-
enty-three percent of the samples originated from city wa-
ter supplies, 24% from private wells, and 3% from other
sources (private river, reservoir or mine). Lead concentra-
tions found in the (B) samples ranged from ND (Not De-
tectable) to 10.20 ppb (¥ = 0.78 ppb), and the (A) samples
from ND to 5.48 ppb (« = 0.60 ppb). Copper ranged in
the (B) samples from ND to 0.84 ppm (¢ = 0.25 ppm)
and in (A) samples from ND to 1.19 ppm (« = 0.06 ppm).
No samples exceeded the EPA lead or copper “action lev-
el” of 15.0 ppb and 1.3 ppm, respectively. Although no
direct correlation between type of water source and lead
concentrations was attempted, 30% of the well samples
had over 1 ppb of lead, while only 12% of the city water
samples did. Sixty-eight percent of the students whose wa-
ter source was from city supplies drink from the cold wa-
ter tap, and 44% of those whose water comes from private
wells do also. Overall, 61% of the students’ families drink
from the cold water tap, and 14% drink directly from the
hot water tap. Seventy-seven percent cook with water
from the hot water tap.
African American taste panelists accept nutritionally en-
hanced recipes for traditional foods. SUSAN B. TEM-
PLETON* and MARTHA A. MARLETTE, Human Nu-
trition Program, Kentucky State University, Frankfort, KY
40601.
African Americans face a disproportionate risk for hy-
pertension, stroke, heart disease, diabetes, and some can-
cers, conditions known to be influenced by dietary factors.
Analysis of the Continuing Survey of Food Intakes of In-
dividuals 1994-1994 and National Health and Nutrition
Examination Survey III (1988-1994) data revealed many
food items frequently consumed by African Americans
were high in fat, sugar, sodium, or cholesterol or low in
fiber. Our goal was to nutritionally enhance traditional rec-
ipes for six commonly consumed items and to test their
acceptability to African Americans using a multistage taste
panel. Nutritionist Five was used to analyze the nutrient
content of original and modified recipes. Blind ratings
were made on taste alone; for Informed ratings, food
items were identified as original or modified and the nu-
trient content of each was provided; for Informed-Blind
ratings, nutrition information was provided, but the ver-
sions were not identified. Fifty-eight percent of the 31
African-American panelists were female; 71% were 19-30
years old. Based on a 1 (low) to 7 (high) scale, mean ac-
ceptability ratings for original/modified food iten:
5.2/4.6 (Blind), 5.5/4.7 (Informed), and 5.6/5.1 (Info:
Blind) (P < 0.05). Although original items received hig!
ratings, over 50% of Informed panelists indicated th
were equally or more likely to consume the modified vei
sion. Modified item ratings improved with each tasting; at
the third tasting, Informed-Blind panelists could not dis-
tinguish the modified food item from the original 35% of
the time. Our findings suggest that these low fat/high fiber
alternatives are acceptable to African-American panelists.
PHYSICS & ASTRONOMY
Generating solutions in Hinstein-Maxwell gravity.
SHARMANTHIE FERNANDO, Department of Physics
and Geology, Northem Kentucky University, Highland
Heights, KY 41099.
Solutions to Einstein-Maxwell gravity with cylindrical
symmetry is generated. By taking the symmetries of the
metric, the Lagrangian is written as a 1 + 0 sigma model.
Then, SL(2,R) transformations are applied to the func-
tions in 1 + 0 dimensions to generate new solutions in 3
+ 1 dimensions. Well-known electrical and magnetically
charged static solutions are taken as seed metrics to gen-
erate new rotating charged solutions.
NASA Kentucky Space Grant Consortium and NOVA
Program opportunities for space-related research, tech-
nology, and education. KAREN HACKNEY,* RICHARD
HACKNEY, ROGER SCOTT, CHARLES McGRUDER,
SANDRA CLEMENTS, MICHAEL CARINI, RI-
CHARD GELDERMAN, TERRY WILSON, DON
COLLINS, KATHI MATTHEW, and MIKE MAY, Ken-
tucky Space Grant Consortium and NASA NOVA Pro-
grams, Department of Physics and Astronomy, Western
Kentucky University, Bowling Green, KY 42101.
NASA has partnerships with Kentucky and its univer-
sities for the purpose of involving faculty and students in
space-related research, technology, and education. We will
describe current opportunities in the Kentucky Space
Grant Consortium for undergraduate scholarships and
graduate fellowships for students in mentored, space-re-
lated projects. Funding opportunities for the development
of space-related research projects will be described. Ac-
tivities of the NOVA and Space Grant programs that sup-
port the teaching of space-science and related disciplines
will be outlined. Progress of existing projects and new op-
portunities will be discussed.
Digital dynamism for enlivening astronomy in the class-
room. RICHARD HACKNEY,* KAREN HACKNEY,
ROGER SCOTT, MICHAEL CARINII, RICHARD
GELDERMAN, and CHARLES McGRUDER, Depart-
ment of Physics and Astronomy, Western Kentucky Uni-
versity, Bowling Green, KY 42101.
Digital technology is resulting in a wealth of available,
inexpensive illustrative materials for enlivening astronomy
presentations in the classroom. NASA and other sources
provide animated views that dynamically illustrate the mo-
S6 Journal of the Kentucky Academy of Science 62(1)
tions and pliysical activity of objects in the universe. Stu-
dents « ain a sense of personal involvement with, and
the ir cdiacy of, activity in space through timely sharing
of « at observational material on the web. Instructors
ay adents can make and share direct observations of
momical objects such as the sun and moon using sim-
telescopes and relatively inexpensive digital cameras.
\Ve present an assortment of sources, examples, and
methods for using these resources to enliven the teaching
and learning of astronomy.
Demonstrating the Ptolemaic and Copernican systems.
ROGER SCOTT,* RICHARD HACKNEY, KAREN
HACKNEY, MIKE CARINII, RICHARD GELDER-
MAN, and CHARLES MecGRUDER III, Department of
Physics and Astronomy, Western Kentucky University,
Bowling Green, KY 42101.
Many astronomy courses include a historical perspec-
tive of how the modern concept of the Solar System was
developed, and the role that Galileo's observations of the
phases of Venus played. This presentation will discuss the
significance of Galileo's observations, and will illustrate a
simple way of demonstrating the phases of Venus in both
the geocentric Ptolemaic system and the heliocentric Co-
pernican system.
Gravitational lensing by black holes. BRIAN TALBERT
and SEAN ROBERTS, Department of Physics and Ge-
ology, Northern Kentucky University, Highland Heights,
KY 41099.
Lensing by charged black holes characterized by the
mass and charge is studied. As a first step, we have cal-
culated the deflection of light from a electrically charged
black hole with the assumption that the gravitational field
is weak and that the deflection angles of light rays are
small. This approximation will lead to three images if the
parameters in lensing such as the mass, the charge and
the distances satisfy certain restrictions. We have done the
calculations for a supermassive black hole and found the
magnification of the images. The support from the Ken-
tucky Space Grant Consortium is gratefully acknowledged.
PHYSIOLOGY & BIOCHEMISTRY
Evidence for dramatically increased bone turnover in
spontaneously hypertensive rats. D. L. DeMOSS, De-
partment of Biology, Morehead State University, More-
head, KY 40351; G. L. Wright, Department of Physiology,
Marshall University School of Medicine, Huntington, WV
25704.
Using the *H-tetracycline model, whole body skeletal
bone resorption was compared among male and female
spontaneously hypertensive and normotensive Wistar Kyo-
to and Sprague-Dawley rats. Immature animals undergo-
ing rapid skeletal growth and bone sculpting showed a
tendency for decreased indices of skeletal resorption in
females compared to males. By 24 weeks of age, the in-
dices of rate of resorption and extent of metabolically re-
active bone in male rats were decreased an average of
68% and 74%, respectively, compared to values obtained
at 8 weeks. By comparison, values for 24 week old females
decreased only 26% and 56%, respectively, resulting in
evidence of a significantly elevated level of resorptive ac-
tivity in mature females compared to males in each of the
three rat strains studied. Within sex comparisons of 24-
week-old animals indicated that bone resorptive activity
was similar between normotensive male and between nor-
motensive female groups. By comparison, the resorptive
activity of both male and fernale hypertensive rats was
significantly increased compared to normotensive con-
trols. This condition was exaggerated in female hyperten-
sive rats, which showed an approximate 78% and 41%
increase in indices of rate of resorption and extent of met-
abolically reactive bone compared to normotensive con-
trols. The results indicate a marked sexual dichotomy in
the decline of skeletal bone resorptive activity following
maturation and slowing of skeletal growth. They further
indicate a significant elevation of whole skeleton bone
turnover in male hypertensive rats and dramatically in-
creased bone turnover in female hypertensive rats.
PSYCHOLOGY
Effects of observer type on social facilitation. TIM
KRAEMER and BONNIE BOWERS, Centre College,
Danville, KY 40422.
This experiment, which concems the effects of observer
type on social facilitation for a learning task, was modeled
after the research of Henchy & Glass (1968, cf. Gore &
Taylor, 1973) and Gore & Taylor (1973). The present ex-
periment proposed that males’ and females’ response time
and accuracy of answers on a learning task would be
quicker and more accurate for students observed by a per-
ceived nonexpert on the task than those observed by a
perceived expert on the task. Forty Centre College stu-
dents, 25 males and 15 females with a mean age of 19.83,
completed the Zinbarg learning task on standard college
computers, while being observed by a perceived expert/
nonexpert or not being observed (control condition). The
hypothesis was partially supported, such that only females’
scores showed social facilitation in that their performance
was quicker and more accurate in the nonexpert condition
than in the expert condition.
SCIENCE EDUCATION
Fear of algebra. JOHN G. SHIBER, Division of Bio-
logical Sciences & Related Technologies, Kentucky Com-
munity & Technical College System/KCTCS, Prestons-
burg Community College, Prestonsburg, KY 41653.
Frequent comments by community college students, es-
pecially non-traditional students, about disliking and fear-
ing algebra, prompted a survey to learn the extent of the
problem, and if there were similar fears of biology, chem-
istry or physics. Three hundred seventy-seven community
college students (40% non-traditional) responded. Most
had taken algebra, and 53% disliked or feared it. Twenty-
six percent and 22%, respectively, feared chemistry and
Abstracts, 2000 Annual Meeting 87
physics. Non-traditionals were more prone to fear all. Bi-
ology was least feared. Six hundred sixty-seven Eastern
Kentucky high school seniors completed the survey for
comparison purposes. Only 14% feared algebra, but many
feared calculus, i.e., 40% who had taken it and 48% who
hadn't. Twenty-four percent feared chemistry and physics,
30% of females vs. 18% of males feared physics, and bi-
ology, again, was least feared. Students blamed their fears
of algebra and calculus on a lack of confidence, e.g., “can’t
understand it,” “too confusing,” “not good at math,” etc.
Suggestions for improving the courses, though, reflected
need for better instructional approaches, wanting teachers
to go slower, explain more in depth, and have more hands-
on and real-life applications. Many high school seniors
wanted more knowledgeable instructors who are interest-
ed in math and student learning. It is concluded that a
perceptual problem among students that labels math in
general, and algebra and calculus in particular, as too dif-
ficult for the average person, does indeed exist, and is
often perpetuated by teachers and counselors. A more
positive attitude about math when dealing with students,
and a more concerted effort by all educators to remedy
the problem, is urged.
Student survey on violence. JOHN G. SHIBER, Divi-
sion of Biological Sciences & Related Technologies, Ken-
tucky Community & Technical College System/KCTCS,
Prestonsburg Community College, Prestonsburg, KY
41653.
The wave of concern in recent years about school vio-
lence prompted a survey on the issue at Prestonsburg
Community College. Sixty-three percent of 307 students
responding have weapons in their homes; 59% have more
than one. Eighty-eight percent of them have rifles, 70%
handguns, and 43% large knives. The weapons are used
chiefly for hunting (33%), personal protection (25%), or
both (27%). Twenty-nine percent of the students have
children at home, 51% of whom are under 15 years of
age. Over half know where the weapons are kept, and 23%
could get them if they wanted. Of all students surveyed,
58% often watch movies with a lot of violence, and 50%
believe children under 18 should be admitted to “R-rated”
movies. Only 17% play video games that are violent in
nature. When very angry, 48% resort to some form of
violent behavior, e.g., slamming doors, throwing things,
screaming, hitting something (or someone), etc. Thirty-
three percent have been in serious physical fights, and
64% have witnessed them in school. According to many,
most school fights are over the opposite sex (36%) and
kids teasing or spreading rumors about each other (25%).
Twenty-six percent had seen students with weapons in
school, but few told an adult about it, for fear of reper-
cussions. While attributing teen violence to many factors,
students most frequently mentioned the lack of parental/
guardian supervision and guidance. Parents of violent
teens, said a majority, are partially, if not entirely to blame
for their offsprings’ behavior. Temporary suspension or
permanent expulsion, with some type of police involve-
ment, was most commonly suggested as a punishme
students bringing weapons to school.
ZOOLOGY & ENTOMOLOGY
Abiotic factors as predictors of terrestrial vertebrate
species richness in Kentucky. MATTHEW L. COLE* and
TERRY L. DERTING, Department of Biological Scienc-
es, Murray State University, Murray, KY 42071.
On a global scale, abiotic factors, particularly those as-
sociated with climate, have significant impacts on species
richness. Climate variables have been used successfully in
models that predict large-scale variation in species rich-
ness. We tested the utility of abiotic factors as predictors
of species richness at the regional level. Using regression
analysis, we developed models to predict the combined
richness of terrestrial vertebrate species in Kentucky and
the species richness of amphibians, breeding birds, mam-
mals, and reptiles. The abiotic variables used in our mod-
els were precipitation, temperature, elevation, topograph-
ic variation, and road density. The resulting models were
generally effective, accounting for ~50% or more of the
variation of species richness in the state. Temperature,
precipitation, and elevation were of primary importance
in all models. Temperature alone was the best predictor
of total species richness (1? = 0.56). Elevation and tem-
perature together were the best predictors of the species
richness of breeding birds (1? = 0.49), mammals (1? =
0.48), and reptiles (1? = 0.75). Abiotic variables were less
effective as predictors of the species richness of amphib-
ians, however. Elevation and precipitation yielded the best
predictive model but explained only 22% of the variation
in amphibian species richness. As with global models, abi-
otic factors accounted for a significant amount of regional
variation in species richness. Through future modeling ef-
forts we will determine the extent to which biotic factors
improve predictions of species richness in Kentucky.
Mate selection of male Poecilia reticulata. GREG DAR-
NELL* and ZACHARY McCARTY,* Department of Bi-
ology, Transylvania University, Lexington, KY 40508.
Our experiment hypothesized that when male guppies
(Poecilia reticulata) were given the chance to select a po-
tential mate, they would prefer the larger of two female
guppies. To run trials, a test tank was setup with three
clear partitions to divide the tank into three equally sized
chambers. Different sized females were placed in the out-
er chambers and a male was released in the middle. Trials
were run for 15 minutes and data were collected based
upon how much time the male spent in the vicinity of
each female. All guppies were measured after the com-
pletion of each trial and new guppies being used in the
following trial. Of the 16 males tested, 12 preferred the
large female, 3 preferred the smaller female, and 1
showed no preference. Using the sign test to analyze these
data, the null hypothesis stating that the male would be
indifferent and spend equal time with each female was
rejected with 95% confidence. Therefore, when presented
with the opportunity for mate choice, male guppies dis-
88 Journal of the Kentucky Academy of Science 62(1)
criminaied and chose the larger female guppy. This may
relate ‘ the increased fertility of the large females, which
pro a greater number of eggs than the smaller fe-
n
low pattern of fruiting in tropical trees affects territory
size of white-winged trumpeters. PETER T. SHER-
MAN,* Department of Biology, Transylvania University,
Lexington, KY, 40508; PERRI K. EASON, Department
of Biology, University of Louisville, Louisville, KY 40292.
We investigated determinants of territory size in white-
winged trumpeters (Psophia leucoptera), which are group-
living, frugivorous birds that defend large, permanent ter-
ritories in Amazonian rainforest. During a 7-month peri-
od, we measured changes in food density at a site in Manu
National Park, Peru, and conducted full-day focal samples
on individuals that allowed us to record daily food intake
of territorial birds. Both census and focal sample data sug-
gested that food availability on trumpeter territories varied
widely. To determine whether trumpeter territory size is
related to food density, we conducted fruit removals dur-
ing which we removed daily an amount of fruit from the
territory that was equivalent to the amount of fruit in-
gested daily by the focal group during a control period
that preceded the removal experiment. Trumpeter food
consumption did not change when fruit was removed dur-
ing periods of resource abundance, but, when experimen-
tal removals were conducted during times when food was
scarce, total caloric value of food consumed decreased sig-
nificantly. Our results suggest that food abundance on
trumpeter territories sometimes exceeds and sometimes is
close to or below the amount needed to meet the ener-
getic needs of the groups. Based on data collected, we
propose that territory size of trumpeter groups reflects
some minimum size needed to provide the group with a
baseline level of food intake during seasonal periods of
decreased food abundance.
Swamp rabbit habitat modeling using a geographic in-
formation system. ADAM SMITH* and TERRY DERT-
ING, Department of Biological Sciences, Murray State
University, Murray, KY 42071.
Using a geographic information system (GIS), we de-
veloped three models predicting the occurrence of swamp
rabbits (Sylvilagus aquaticus) in western Kentucky. The
models were compared to the existing Kentucky GAP
model. All models were successful in the prediction of
confirmed swamp rabbit observations, both of presence
(>80%) and absence (>90%), with only slight variation
among models. After selection of the best model based
on statistical performance and model construction criteria,
the best model was applied to geographic areas of Ken-
tucky contiguous to the species’ current Kentucky range
to investigate the possibility of swamp rabbit reintroduc-
tions. Only five areas for potential reintroduction were
identified, with two of marginal quality and the remaining
unsuitable for swamp rabbit reintroduction. Land own-
ership and protection status of all habitat determined to
be suitable by our best model was assessed; the vast ma-
jority of all land was in private ownership. Wildlife Man-
agement Areas protected the most swamp rabbit habitat
(~=8%), but most suitable habitat remains at risk. These
models can serve as a solid basis for future swamp rabbit
management considerations. Field validation and frequent
assessments and modifications of the models associated
with increased data availability and improved GIS tech-
nology are recommended.
Guidelines for Contributors to the Journal
. GENERAL
. Original research/review papers in science will be con-
sidered for publication in JKAS; at least the first author
must be a member of the Academy. Announcements,
news, and notes will be included as received.
. Acceptance of papers for publication in JKAS depends
on merit as evaluated by each of two or more review-
ers.
. Papers (in triplicate) may be submitted at any time to
the editor. Do not send a disk file.
John W. Thieret
Biological Sciences
Northern Kentucky University
Highland Heights, KY 41099
Phone: (859) 572-6390
FAX: (859) 572-5639
E-mail: thieretj}@nku.edu
List in the cover letter your telephone number, your
e-mail address, and the names, addresses, and tele-
phone numbers of two persons who are potential re-
vieWers.
. Format/style of papers must conform to these guide-
lines and also to practices in recent issues of JKAS,
which are, in effect, a style manual.
. Papers should be submitted in hard copy. Do not sta-
ple pages together.
. Indent the first line of each paragraph (but not the
first line of entries in the Literature Cited).
. FORMAT
Papers should be in 12-point type on white paper 8.5
x 11 inches, with margins at least 1 inch all around.
Double-space throughout the paper (i.e., one full line
of space between each two lines of text, literature cit-
ed, or tabular data). Do not justify right margins.
. Except for scientific names of genera and of infrage-
neric taxa, which should be typed in italics, the same
type (roman) should be used throughout (i.e., one type
size only; bold only for paper title).
. Sequence of sections in papers should, where appro-
priate, be as follows: title of paper, name/address of
author(s), abstract, body of paper, footnotes, table cap-
tions, figure captions (all the preceding on consecu-
tively numbered pages), tables, and figures.
. The running head (top right) should give name(s) of
author(s), a short version of paper title, and page num-
ber of total.
. The first page should include the running head and,
centered near the top of the sheet, the papers title
and the name and address of author(s). These should
be followed immediately by the abstract. (The first
page should look as much as possible like the first page
of articles in JKAS.)
. The abstract, not to exceed 200 words, should be con-
89
4.
A.
cise, descriptive, and complete in itself without r:
ence to the paper.
. The body of the paper should, where appropriate, in
clude the following sections: Introduction, Materials
and Methods, Results, Discussion, Summary, Acknowl-
edgments, and Literature Cited.
. No more than three levels of headings should be used:
level 1, in capitals, centered; level 2, in capitals/low-
ercase, flush left; level 3, in italics, a paragraph indent,
with initial capital only (except proper nouns and ad-
jectives), and followed by a period, the text then start-
ing after one blank space.
Personal communications (avoid if possible) should be
indicated in the text as follows: (name, affiliation, pers.
comm., date), e.g., (O.T. Mark, Wainwright College,
pers. comm., 5 Jun 1995).
STYLE
In text, spell out one-digit numbers unless they are
used with units of measure (four oranges, 4 cm) and
use numerals for larger numbers; do not begin any
sentence with a numeral.
. Use no footnotes except those for title page and tables.
Footnotes, identified by consecutive superscript num-
bers, should be entered on a separate sheet.
. Measurements should be in metric and Celsius units.
Define lesser-known symbols and give the meaning of
acronyms at first use. Express time of day in the 24-
hour system. Dates should be written day, month (ab-
breviated to three letters), year without intemal punc-
tuation. Units with multiple components should have
individual components separated by a virgule (e.g., g/
m? or g/m?/yr).
. Names of authors of binomials may be included but
only at the first mention of the binomial. Cultivar
names are not italicized but are enclosed in single
quotes.
. Useful guides for contributors to JKAS are the follow-
ing: Scientific style and format: the CBE manual for
authors, editors, and publishers, 6th ed., Cambridge
University Press, 1994; The Chicago manual of style,
14th ed., University of Chicago Press, 1993; The ACS
style guide, American Chemical Society, Washington,
DC, 1986; and AIP style manual, American Institute
of Physics, New York, 1990.
IN-TEXT CITATION OF LITERATURE
Cite publications in the text by author(s) and date—
e.g., (Readley 1994); multiple citations should be in
alphabetical order and separated by semi-colons—e.g..,
(Ashley 1987; Brown 1994; Foster 1975); multiple ci-
tations of works by one author(s) should be in chro-
nological order—e.g., (Jones 1978, 1983); publications
by one author(s) in the same year should be distin-
guished by a, b, c, ete—e.g., (Smith 1994a, 1994b).
For in-text references to works with one or two authors
90) Journal of the Kentucky Academy of Science 62(1)
use ‘s of both authors—e.g., (Jones and Williams
19 x works with three or more authors use name
( first author followed by et al—e.g., (Lee et al.
)
o not include any reference unless it has been pub-
lished or accepted for publication (“in press”; see be-
low).
5. LITERATURE CITED
A. List all authors of each entry. Do not abbreviate jour-
nal titles; abbreviations for these will be supplied by
the editor.
B. The first line of each reference should be typed flush
left; the remaining lines should be indented.
C. Examples of common types of references are given
below.
JOURNAL ARTICLE
Lacki, M.J. 1994. Metal concentrations in guano from a
gray bat summer roost. Transactions of the Kentucky
Academy of Science 55:124—126.
BOOK
Ware, M., and R.W. Tare. 1991. Plains life and love. Pi-
oneer Press, Crete, WY.
PART OF A BOOK
Kohn, J.R. 1993. Pinaceae. Pages 32-50 in J.F. Nadel
(ed). Flora of the Black Mountains. University of
Northwestern South Dakota Press, Utopia, SD.
WORK IN PRESS
Groves, S.J., 1.V. Woodland, and G.H. Tobosa. n.d. De-
serts of Trans-Pecos Texas. 2nd ed. Ocotillo Press,
Yucca City, TX.
6. ILLUSTRATIONS
FIGURES (LINE DRAWINGS, MAPS, GRAPHS, PHO-
TOGRAPHS)
Figures must be camera-ready, glossy, black-and-white
prints of high quality or laser prints of presentation qual-
ity. These should be designed to use available space ef-
fectively: a full page or part of one, or a full column or
part of one. They should be mounted on heavy white
board and covered with a protective sheet of paper; pho-
tographs to be grouped as a plate should have no space
between them. Dimensions of plates must observe page
proportions of the journal. Each illustration in a plate may
be numbered as a separate figure or the entire plate may
be treated as one figure. Include scale bars where appro-
priate. Lettering should be large enough to be legible after
reduction; use lowercase letters for sections of a figure.
Figure captions should be self-explanatory without refer-
ence to the text and should be entered on a page separate
from the text. Number figures in Arabic numerals. Statis-
tics presented in figures should be explained in the caption
(e.g., means are presented + SE, n = 7).
i)
TABLES
Each table and its caption must be double-spaced, num-
bered in Arabic numerals, and set on a sheet separate
from the text. The caption should begin with a title relat-
ing the table to the paper of which it is a part; it should
be informative of the table’s contents. Statistics presented
in the table should be explained in the caption (e.g.,
means are presented + SE, n = 7).
7. ETHICAL TREATMENT OF ANIMALS AS RE-
SEARCH SUBJECTS
If vertebrate or invertebrate animals are involved in a re-
search project, the author(s) should follow those guide-
lines for ethical treatment of animals appropriate for the
subjects, e.g., for mammals or for amphibians and reptiles.
Papers submitted to JKAS will be rejected if their content
violates either the letter or the spirit of the guidelines.
8. PROOFS
Authors are responsible for correcting proofs. Alterations
on proofs are expensive; costs will be assessed to authors.
Proofs must be returned to the editor within 3 days after
the author receives them; delay in return may result in
delay of publication.
9. REPRINTS
Forms for ordering reprints will be sent to the author
when the proofs are sent. They are to be returned directly
to Allen Press, not to the editor.
10. PAGE CHARGES
A page charge covering the partial cost of publication will
be assessed for all authors. However, acceptance or rejec-
tion of an individual manuscript is determined solely on
scientific merit. Individuals may contact the KAS office
(Kentucky Academy of Science, Science Outreach Center,
University of Kentucky, Lexington, KY 40536-0078) to re-
quest an application form for full or partial remission of
page charges. The application form is also posted on the
KAS website. Awards are limited to available funds.
11. ABSTRACTS FOR ANNUAL MEETINGS
Instructions on style of abstract preparation for papers
presented at annual meetings may be obtained from the
editor. Copies will be available also at each annual meet-
ing of the Academy.
NEWS
The Morehead Electronic Journal of Applications in Mathematics (MEJAM) is a new interdisciplinary
journal sponsored by Morehead State University, Morehead, Kentucky. The goal of MEJAM is to provide a
refereed outlet for undergraduate students in any discipline to publish quality papers and see the results quick-
ly. MEJAM accepts papers that are outside the realm of the typical undergraduate curriculum and that
emphasize the applications of mathematics while maintaining significant mathematical interest. Papers may
be historical, expository, or completely original in nature but must adhere to strict academic standards and
must emphasize some aspect of the applications of mathematics. Papers from all disciplines will be consid-
ered for publication. More information about the journal and instructions for submissions can be found on
the journal’s website at http://www.morehead-st.edu/ colleges/science/math/mejam/.
The Kentucky Academy of Science is seeking to complete its set of Transactions of the Kentucky
Academy of Science. Various issues prior to 1985 are needed. Anyone willing to donate back issues or to
sell them at a reasonable price should get in touch with the editor at thieretj}@nku.edu.
The 2001 annual meeting of the Kentucky Academy of Science will be held jointly with the Tennessee
Academy of Science on Thursday—Saturday, 29-30 November and 1 December 2001, at Middle Tennessee
State University (MTSU), Murfreesboro, Tennessee. There will be a reception and symposium at the Garden
Plaza Hotel in Murfreesboro on Thursday evening. Friday technical sessions will be help on the MTSU cam-
pus in the Keathley University Center and James Union Building. The annual awards banquet and president's
reception will be held Friday evening at the Garden Plaza Hotel. Technical sessions will conclude on Saturday
in the Keathley University Center.
PUBLICATIONS
The Sibley Guide to Birds from the National Audubon Society is now available. This 544-page work, written
and illustrated by David Allen Sibley, covers North America north of Mexico. Families and, in some cases,
genera are introduced with small figures for initial comparisons. Each group is followed by individual species
accounts including figures of the different forms and phases that may be exhibited by each species and also
of both perching and flying views. The book has ca. 6600 illustrations (paintings) and descriptions of 810
species and 350 regional populations; it is more a reference source than a field manual. The introductory
chapter briefly discusses classification and techniques of field ornithology. A second chapter discusses and
illustrates the topography of birds. Sibley concludes with an index to common and scientific names of species.
The book is a Chanticleer Press edition published in 2000 by Alfred A. Knopf, Inc.; ISBN 0-679-45122-6;
$35.00 (soft cover).
The National Audubon Society Field Guide to Wildflowers. Eastern Region is a revision of the first edition
of the work (1979); the revising author is John W. Thieret. This 879-page book has all new photographs of
638 species, two or three per page. The introductory pages discuss the arrangement of the color plates
(mostly by color and type of flower cluster), flower parts, inflorescence type, leaves, and plant classification
and names. For each included species the text gives a description, flowering times, habitat, range, and com-
ments. Relevant families are briefly discussed. The book concludes with an index to common and scientific
names of species. The book is a Chanticleer Press edition published by Alfred A. Knopf, Inc., in 2001; ISBN
0-376-40232-2. $19.95 (soft cover).
Wt
3 9088 01304 3419 .
CONTENTS
The Genus Trifolium (Fabaceae) in Kentucky. Michael A. Vincent ........ 1
The Role of Light in Regulating Dandelion (Taraxacum officinale;
Asteraceae) Inflorescence Height. David Lowell Robinson. ..................++ 18
Distribution and Status of Freshwater Mussels (Bivalvia: Unionoidea) in
the Cumberland River Basin Upstream from Cumberland Falls, Kentucky.
Ronald R. Cicerello and Ellis L. Laudermilk ...............ccscsecessesseseseseces 26
Morphometric Variation of Cotton Mice (Peromyscus gossypinus) and
White-footed Mice (P. leucopus) in Kentucky. Nell A. Bekiares and
George Ax. Feldhaime nh sisson: cncckavasaedasecaecensusccneddunsecvuabsessassnnndupapantantiieeae ao
Woody Plants of Six Northern Kentucky Counties. Ross C. Clark and
Reyaant Mi Bauer cies istesastcicdtecdsensgndascdesdaduasqrakanwivnis<cnanee@ahan patina 39
Effects of Fish on Zooplankton Community Structure in Chaney Lake, a
Temporary Karst Wetland in Warren County, Kentucky. Nicole Vessels and
Sefiveny Di Sache) sos lssencesans cicie cavewqhsn deve scdecessvsubaiace ceavewcon teense healt 52
A Historiography of Archaeological Research in the Mammoth Cave Area
of Kentucky: 1824-2000. Kenneth C. Carstens ...............c.secsescesereceeeces 60
Using Composts as Growth Media in Container Production of Tomatoes.
Brian D. Lacefield ‘and. Elmer Gray <..scscosesscccedeccostecsiuaseeuensscemsenpensnens 70
Book Review ss cccoicoeccin ci ie nain ecgenanteckedanhibetpaucdeetoues sacduainpechadd orgs ian 77
Abstracts of Some Papers Presented at the 2000 Annual Meeting of the
Kentucky Academy ‘of SCienCe® .isccasieccd caedae cases adeecanenceaseneweussneaensuunenaneeens 79
Guidelines for Contributors to the Journal ................0c...ecccececccccececceceees 89