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RaONS > . ere oO ads e+) => nae Y Yo RSE: Ke ea — NO FG GARY = Ka OP o S was m *\ SS 2 ase m re hs = re) a, = wn z LIBRARIES SMITHSONIAN INSTITUTION NOILNLILSNI NVINOSHLIN - = < = WY; = >" = w = z ” Zz ” NOILALILSNI LIBRARIES SMITHSONIA ” 2 if 2 a wl o a wo wu : : : : : ea (a es e = ig 4 = = Lo mo rs) ea re) = G 2 a3 z ait LIBRARIES SMITHSONIAN’ INSTITUTION NOILNLILSNI i z a z z 3) Sil 3) > 0) = rae a Ee ae th Br es = is o _ 2 o = Oo NOILNLILSNI SAIYVYEIT LIBRARIES w z= 2) = wee Yo = Hed S 2 ae WS = = i 4 2: Eo hee = z re) 5 SY t4j ro) NX. ba z = 2 “yy = NS = > = > ‘ = Se Z ” 2 7 2 SMITHSONIAN _INSTITUTION NOILOLILSNI NVINOSHLIV NOILALILSNI LIBRARIES xv Satuyvudil LIBRARIES SMITHSONIA SAIYVYRITLIBRARIES INSTITUTION NOILNLILSNI S3luvad!ly INSTITUTION LIBRARIES SMITHSONIAN INSTITUTION NOILONLILSNI NVINOSHLIV NN NYS NOILNLILSNI NVINOSHLIWS SAIYVYUEIT LIBRARIES es i wn < > Py NVINOSHLIWS SMITHSONIAN “ig NVINOSHLIWS IN SMITHSONIA RARITIES SMITHSONIAN SARIES SMITHSONIAN NALILSNI NLILSNI STITUS RARIES J - / TRANSACTIONS OF THE KENTUCKY ACADEMY OF SCIENCE Volume 30, 1969 EDITORIAL STAFF Editor WirtiAM F. WAGNER Associate Editors WitLt1AM DENNEN, Geology MarsHALL Gorpon, Chemistry L. A. Krumuouz, Botany and Microbiology RoBeRtT KuEHNE, Zoology Editorial Office Department of Chemistry University of Kentucky Lexington, Kentucky 40506 Published in 1969 by THe Kentucky ACADEMY OF SCIENCE CONTENTS TO VOLUME 30 No. 1-4 Influence of Artificial Destratification on Plankton Populations in Impoundments. ERNEST L. ROBINSON, WILLIAM H. IRWIN ONE) PANES M.S YMIONS cisc; deicceicesseisee-cessvettercdeavcnccceccnsosa i Note on the Life Cycle of Cathaemasia Reticulata (Wright) in the Eastern Belted Kingfisher. JOHN VINCENT ALIFF AND JAMES M. EDNEY ............... 20 Age and Growth of the Western Blacknose Dace Rhinichthys Atratulus Meleagris Agassiz, in Doe Run, Meade County, Kentucky. TE CORN ANIL GS BE Bd Io BF] Se aA 23 A Study on Plethodon Richmondi from Mason County, Kentucky with Notes on Its Distribution Within the State. Pee ben VV AU AG AGE, 02 kent cacssccentenotepcecsxsevcnessaceundonussuncentaeseus 38 Some Notes on the Growth, Development and Distribution of Ochrotomys Nuttalli (Harlan) in Kentucky. PRES PV ATTA CEE ooo Geis Seascccouecssedadussnsdbecadeacsusceuessseosebes 45 LENE ESTE AL. scecopeceagc Aes eae eee een Soe Soe ee A 53 The Fishes of West Kentucky. I. Fishes of Clark’s River Beige Lg AUN Ec) SES IG ice sachet ee nd caces tactirevsc de) sacs ose sane cds sate eeectee donk 54 The Fishes of West Kentucky II. The Fishes of Obion Creek. PAUL L. SMITH AND MORGAN E. SISK ...............cccccsseeees 60 An Anotated List of Known Species of Fresh-Water Ostracoda of Western Kentucky. Ryle ee NEG OE VEL YIN, COLE 1.005 ceosdtedscthn esse ectascegoastedanoeaatt 69 A Record of the Occurrence of the Exotic Land Planarian, Bipalium Kewense, in Calloway County, Kentucky. Re ean EE EV EY IN COMB aoe o oss .nsesoscducsscdccdeveccdedesecancstss 71 Parospirifer Acuminatus From the Brevispirifer Gregarius Zone at the Falls of the Ohio. JAMES E. CONKIN AND BARBARA M. CONKIN .............. Te CRB 0 75 LRT ANT OTRAS aa eo 78 LuBlase (PD) SUCCESS VESRES| pets 9 87 same 30 ke od ae ef V6 1969 Numbers 1-2 TRANSACTIONS of the KENTUCKY CADEMY of SCIENCE Official Organ Kentucky ACADEMY OF SCIENCE Ant ASO CONTENTS oM ‘Ay : NECA 1969 Influence of Artificial Destratification on Plankto ne Populations in Impoundments. lip RARIC? ERNEST L. ROBINSON, WILLIAM H. IRWIN AND JAMES M. SYMONS ........::.-csscsssossesescsssensecesonnsssveasenese 1 Note on the Life Cycle of Cathaemasia Reticulata (Wright) in the Eastern Belted Kingfisher. JOHN VINCENT ALIFF AND JAMES M. EDNEY .............. 20 Age and Growth of the Western Blacknose Dace Rhinichthys Atratulus Meleagris Agassiz, in Doe Run, Meade County, Kentucky. POON ATG ED CG. TAR TER s. ccscnecccedecsntooscestvacsovesecouetsusevetetsicvacedeanaas 23 A Study on Plethodon Richmondi from Mason County, Kentucky with Notes on Its Distribution Within the State. JAMES T. WALLAGE, .....cccccccsccessscssnsensessssesscrsavsnnereasessssecnssvens 38 Some Notes on the Growth, Development and Distribution of Ochrotomys Nuttalli (Harlan) in Kentucky. AMES) TL) WALLACE? iriiitessssncesscssncscsercvsessavcsssnspnsessonenneeereneers 45 The Kentucky Academy of Science Founded May 8, 1914 BOARD OF DIRECTORS Lloyd E. Alexander ........c0.....t0 1969 John M. Carpenter ........ rs a Le 8 | Margaret B. Heaslip .........0..t0 1969 William M. Clay ......ccsscc-s- ...to 1971 Sarl Mussang toes to 1970 Gordon Wilson ........... eee oh ROT 2 Grace Quinto .........ccsssscseseereeee tO 1970 L.A. Krambholz, v.c.2-seeee to 1972 EDITORIAL OFFICE William F. Wagner Editor Department of Chemistry University of Kentucky Lexington, Kentucky, 40506 Associate Editors: Botany and Microbiology: L. A. Krumholz, University of Louisville Chemistry: Marshall Gordon, Murray State University Geology: William Dennen, University of Kentucky Zoology: Robert Kuehne, University of Kentucky Membership in the Kentucky Academy of Science is open to interested persons upon nomi- nation, payments of dues, and election. Application forms for membership may be obtained from the Secretary. THE TRANSACTIONS are sent free to all members in good standing. Subscription rates for non-members are: domestic, $4.00 per volume; foreign, $4.00 per volume. The TRANSACTIONS are issued semi-annually. Four numbers comprise a volume. Correspondence concerning memberships or subscriptions should be addressed to the Secretary. Exchanges and correspondence relating to exchanges should be addressed to the Librarian, University of Louisville, who is the exchange agent for the Academy. Manuscripts and other material for publication should be addressed to the Editor. ———— Se INFLUENCE OF ARTIFICIAL DESTRATIFICATION ON PLANKTON POPULATIONS IN IMPOUNDMENTS ERNEST L. ROBINSON, WILLIAM H. IRWIN and JAMES M. SYMONS* Respectively, Research Aquatic Biologist, Aquatic Biologist, and In Charge, Im- poundment Behavior Studies, Cincinnati Water Research Laboratory, Federal Water Pollution Control Administration, U.S. Department of the Interior. INTRODUCTION Recently, much attention has been given to the influence of thermal stratification on water quality in reservoirs and the possible improvement of reservoir water quality by artificial destratification. During the past sev- eral years, the authors have investigated water quality in three northern Kentucky fishing lakes to determine the effectiveness of controlling water quality by artificial destratification. Previous papers on this subject by Irwin et al. (1966), Symons, Irwin and Robeck (1967), Irwin et al. (1967), and Symons et al. (1967); have mainly discussed the influence of mixing on chemical water quality. The purpose of this paper is to show the phytoplankton populations that existed during destratification. Enumerations of plankters were made of total and generic groups existing before and after mixing. These data were compared to physical and chemical data collected at the same time, to determine if the plankton populations were modified by chemical and physical conditions. Finally, the results of both years’ studies were compared to determine any similarities or differences. LAKES STUDIED, EQUIPMENT AND ANALYTICAL METHODS USED The control lake, Bullock Pen Lake, was not mixed, but was used to show the general trend of water quality characteristics for lakes in the area studied. Test Lake I, Boltz Lake, was artificially destratified by mechanical pumping continuously for 36 days from August 6 to September 10, 1965, and by diffused-air for four periods totaling 14.4 days between June 3 and August 23, 1966. Test Lake II, Falmouth Lake, studied only in 1966, was destratified by the diffused-air system for five periods totaling 28.5 days between May 16 and September 13, 1966. The morphological characteristics of the study lakes during the 1965 and 1966 experiments, and the mechanical pump used for destratification have been described previously (Irwin et al., 1966; Symons, Irwin and Robeck, 1967). The diffused-air system has also been described previously (Irwin et al., 1967; Symons et al., 1967). Both mixing devices were placed at or near the deepest portions of the lakes studied. * Current title and location, Chief, Surface Water Protection, Water Supply and Sea Resources Program, National Center for Urban & Industrial Health, U.S. Public Health Service, U.S. Dept. Health, Education & Welfare, Cincinnati, Ohio. 2 E. L. Robinson, W. H. Irwin, and J. M. Symons Water samples were taken at various depths and times in the deep- water areas to determine the influence of destratification on water quality. Details of sampling techniques and methods of field and laboratory an- alyses for physical and chemical constituents of the study lakes have been described previously (Symons et al., 1967). One-liter water samples were collected from Bullock Pen Lake to study the influence of artificial destrati- fication on plankton populations at the surface and at depths of 5, 15, 30, and 43 ft., respectively; at the surface and at depths of 5, 15, 30, 45, and 60 ft., respectively, from Boltz Lake; and at the surface and at depths of 5, 15, 30, and 40 ft., respectively, from Falmouth Lake. Samples were preserved with 0.16% thimerosal and 1% Lugol’s solution. One gram of sodium borate was added for each gram of thimerosal to keep the thim- erosal in solution. This preservative, reported by William (1963), aided preservation and precipitation of organisms for microscopic identification. Samples were examined in a Sedwick-Rafter cell with a 20-power objective and 10-power oculars. The “strip counting” method was used; calibration, dilution factors, and the number of plankters per ml were computed. All recognizable plankters were identified to genus and enumerated. Each single-cell organism was counted as one and organisms grouped in colonies were counted as one. Filamentous colonies were listed as units of 100 microns in length and only whole zooplankters were enumerated. No special effort was made to identify the plankters to species. Diatoms were identified only from wet mounts and single cells of less than 4 microns were not enumerated. Some samples contained such low numbers of plank- ters that concentration was necessary. Aliquots of 200 and 500 ml, de- pending upon the concentration of plankters, were filtered through mem- brane filter discs (0.4 microns). Discs were placed in 250-ml beakers and gently rinsed with distilled water. The rinse water was used to make a slurry that was diluted to a desired volume. The discs were examined under 430 X magnification to establish that the organisms had been removed by this technique. The concentrated organisms were then examined in a Sedgwick-Rafter cell. RESULTS Total Plankton Population Plankton populations occurring in the three study lakes during 1965 and 1966 and the average plankton count throughout the total depth of each lake were computed for comparison. The plankton numbers/ml at the 5-ft. depth were assumed to represent the organisms in the O- to 5-ft. layer, the 15-ft. count was assumed to represent the organisms in the 5- to 15-ft. water layer, and so forth. The plankton counts/ml at the various depths were multiplied by the water volume of the layers they represented and the arithmetic sum for the entire lake was divided by the total volume of the lake to obtain the number of plankters/ac ft. throughout the lake. Influence of Artificial Destratification 3 The plankton totals at the 5-ft. depth were compared (see Figure 1, diagrams 2 and 3) to show similarity of the mixed to the unmixed lake during 1965 and 1966. The diagrams were not designed to show magni- tude but were designed to indicate the times variations occurred. The graphs were plotted quantitatively above and below the abscissa to mag- nify variations for easier recognition. Diagrams 1 and 2 show some simi- larity of plankton in the control lake and Test Lake I in 1965 during the months before mixing. The plankton numbers declined sharply when the artificial destratification began and continued to decline during pumping MAY SEPTEMBER | OCTOBER TUNE JULY ANGUST TEST LAKE I 1965 CONTROL LAKE 1965 TEST LAKE II 1966 Figure 1. Diagrams showing comparisons in total plankton at the 5-ft depths in the Test Lakes with the Control Lake. Brackets indicate stirring periods. 4 E. L. Robinson, W. H. Irwin, and J. M. Symons in Test Lake I. The plankton numbers also declined in the unmixed lake at this time, though less rapidly than in Test Lake I. Diagram 4 shows that the total plankton numbers decreased sharply during mixings 2, 3, and 4, and rose when the mixings stopped, in Test Lake I, 1966. During the first mixing, the plankton numbers did not decrease, but their rate of increase was retarded. A somewhat different growth pattern occurred in Test Lake II during 1966, as shown in Dia- gram 5. The total plankton numbers increased during mixings 1, 2, and 5. Small declines were recorded during mixings 3 and 4. Plankton Distribution With Depth The plankton concentration varied with depth in all three lakes. The unmixed lake, as an example, is shown in Table I. As the summer season progressed the plankton concentration was highest in the lower layers. This lake was sufficiently clear to support plankton populations through- out its total depth. Table II demonstrates that, in 1966, in Test Lake I during mixings 2, 3, and 4, the plankton numbers declined at all levels. This shows that the surface algae were not transported to the lower layers in the lake during mixing. Test Lake II behaved slightly differently from Test Lake I, probably because of an increased phosphorus concentration near the sur- face. In this case, although the data from all depths showed similar trends, the plankton numbers in the 5-ft. samples were consistently and significantly higher than those taken at the other depths. Occurrence of Plankton Categories The green and blue-green algal counts at the 5-ft. depth in the un- mixed lake were similar during 1965 and 1966, as shown in Figure 2, diagrams 1, 2, 3, and 4. In Test Lake I in 1966 the decline in the blue- green algal counts was greater than that in the green algal counts following mixings 2, 3, and 4 (Figure 2, diagram 8). The blue-green algae decrease was more pronounced in 1966 than in 1965 (Diagrams 5 and 7). Table 1. Total Plankton Concentrations At Various Depths In Unmixed Lake 1966 Total Plankton Count/acre-foot (109 omitted after each value) 0-5 ft 5-15 ft 15-30 ft 30-44 ft Date Layer Layer Layer Layer June 3 3.1 1.4 1.1 0.9 June 16 1.5 1.1 5.3 7.3 June 29 4.1 9.5 3.4 4.3 July 18 2.4 Dp) 2.3 8.7 Aug. 5 0.4 0.9 eo 5.8 Sept. 3 1.3 1.3 1.8 3.6 Oct. 5 0.5 0.2 1.1 1.0 Influence of Artificial Destratification 5 Table 2. Total Plankton Concentrations At Various Depths In Test Lake-I 1966 Total Plankton Counts/acre-foot (1019 omitted after each value) 0-5 ft 5-15 ft 15-30 ft 30-40 ft 45-62 ft Date Layer Layer Layer Layer Layer May 23 1.4 0.6 0.7 ileeé 0.7 June 7 (A-1) 2.0 2.4 1.1 3.6 0.8 June 21 (B-2) 87.0 45.0 6.4 14.0 15.0 June 25 (A-2) 8.1 5.5 3.7 3.7 1.3 July 18 (B-3) 140.0 51.0 51.0 27.0 36.0 July 20 (A-3) 5.9 7.7 9.6 6.1 14.0 Aug. 17 (B-4) 19.0 21.0 33.0 9.0 3.7 Aug. 23 (A-4) 0.9 2.0 1.3 1.2 2.4 Sept. 16 3.4 3.0 2.8 2.9 3.1 October 5 0.8 1.9 ei, 2.5 1.5 Note: B-2 means before mixing 2; A-2 means after mixing 2, and so forth. In Test Lake II a different pattern was evidenced, as shown in Figure 2, diagrams 9 and 10. During mixings 1 and 2, the counts of both green and blue-green algae increased, the green algal increase being the greater. During mixings 3 and 4, a slight increase in green algae numbers occurred, while the blue-greens declined. Finally, both categories of algae decreased during mixing 5. Figure 2, diagrams 9 and 10, indicate that artificial destratification is more detrimental to blue-green than green algae. Composition of Standing Crop The counts from all samples were separated into five categories: green algae, blue-green algae, diatoms, zooplankton, and pigmented flagellates. The percentage of the total plankton numbers throughout the lake was then calculated for each category. For representation, the zooplankton and the pigmented flagellates were added to form one category, as shown in Figures 3 and 5. Figures 3 and 5 also show that, in the unmixed lake, the blue- green algae predominated during the months of July, August, and Sep- tember. Figure 4 shows that, when mixing began in Test Lake I in early August 1965, the general upward trend of the blue-green algae stopped and reversed, and green aglae predominated during the remainder of that season. The percentage of zooplankton and pigmented flagellates rose sharply during the mixing period. Figure 6 shows that in Test Lake I in 1966, mixings 2, 3, and 4 resulted in a sharp decrease in the percentage of blue-green algae. Diatoms in- creased during mixing 2, and the combined zooplankton and pigmented flagellates increased during mixing 3. A different situation developed in Test Lake II in 1966, as shown in Figure 7. During mixings 2, 3, and 4, there was a reduction in the per- centage of blue-green algae, though not as pronounced as in Test Lake I in 1966. During mixing 5, the percentage of blue-green algae increased, 6 E. L. Robinson, W. H. Irwin, and J. M. Symons | MAY JUNE JULY AUGUST SEPTEMBER jOCTOBER BLUE GREENS ~ . CONTROL LAKE 1965 1966 3. CONTROL LAKE -GREENS 1965 4. CONTROL LAKE 1966 5. TSE LO I 6. TEST LAKE I 1965 GREENS BLUE GREENS 1966 8. TEST LAKE I GREENS 1966 9. TEST LAKE II 1966 BLUE GREENS 10. TEST LAKE II GREENS Figure 2. Diagrams showing the comparisons of Blue Green and Green Algae counts in the three study lakes. Brackets indicate stirring periods. probably because blue-green algae tend strongly to predominate in Sep- tember in this geographical location. Also, Figure 7 shows a rather high percentage of the combined zooplankton and pigmented flagellates category. The environment in Test Lake II differed somewhat from Test Lake I, sup- porting a wider variety of organisms. Changes in plankton composition during artificial destratification have also been noted by Bernhardt (1967) and Cooley et al., (1967). Influence of Artificial Destratification 7 100 UNMIXED LAKE 80 ” = z Fe w u < = sol ° < << re ° ‘ Oz 677 = ! =a Ww zo re | < = ” <69 4 N O @a@aAna x 7 20 N N | | N 4 i | Oh Is st N NUH 2 6/3 |6/16|6/29|7/13 8/5 9/ 10/3}10/27; DATE, 1966 Figure 5. Composition of plankton standing crop in unmixed lake in 1966. of the water during early summer in Test Lake II permitted plankton to grow in wider variety. Predominant Organisms During the two years of study, 81 genera of algae were identified from the three lakes. Fifty-six genera were identified from the unmixed lake, 33 of them found in both years. Sixty-three genera were found in Test Lake I, 30 of them in both years. Forty-eight genera were found in Uo (= T Uns ESSERE Ele en ee T T ra} imsreo oor A TT M.2 M-3 M4 TEST LAKE-I 80 r DIFFUSED-AIR | PUMPING x m < | 60 F 0 t i | il | | | | li | 5/23| 6/7)6/21|6/25|7/13|7/20 8/17|8/23 9/16| 10/5 PERCENT OF TOTAL COUNTS END OF MIXING-I GREEN ALGAE | sid BLUE-GREEN ALGAE Bere se ZOO PLANKTON & PIGMENTED FLAGELLATES LS] DIATOMS DATE, 1966 Figure 6. Composition of plankton standing crop in Test Lake | in 1966. Influence of Artificial Destratification 9 100 a rae Tl aes | 1 I 1 1 1 1 1 1 1 ! M-2 M-3 M-4 M-5 TEST LAKE-II 80 DIFFUSED -AIR KEY ra UXINGEI PUMPING = = 5/16-5/19 fl h 5 5/20-5/23 = ° | E Uv —_ z 60 < su e oO oO 2 wz 63 az < Ce ° 9G Zo - 40 <2 ode z | zo zaZz w A ee ee el U w “4 FOF = | ~ 2 £00 a © os ONa | i | } < 20 | d \ | | Ni | Hove | ] } ; | N | N | AN E NP SIAMIAN il | 0 N ~ H N ! N S bs HN 5/13|5/20| 6/8 ,6/15|6/30| 7/8 |7/25| 8/3, , 1 9/8|9/15|10/6, DATE, 1966 Figure 7. Composition of plankton standing crop in Test Lake II in 1966. Test Lake II. Thirty-five genera were common to all three lakes. All of the plankton genera identified during this study are presented in Table IV. The total number of samples from each study lake and the number of times that a given organism occurred in any sample are presented to show which of the algal genera appeared most frequently. Some data on the occurrence of zooplankton genera are also given in these tables. Table 3. Number of Plankton Genera in the Standing Crop on Various Dates in 1966 in the Three Study Lakes Unmixed Lake Test Lake I Test Lake II Number of Number of Number of Date Genera Date Genera Date Genera 5/18 25 5/28 18 5/20 Q7 6/3 18 6/7 7 6/8 16 6/16 21 6/21 25 6/15*-2 O7/ 6/29 29 6/25*-2 25 6/30 17 7/18 383 7/18 36 7/8*-3 94 7/20*-3 41 7/25 23 8/5 Wl 8/3*-4 28 8/17 30 8/23*-4 80 9/2 33 9/8 82 9/16 38 9/15*-5 35 10/8 36 10/5 81 10/6 30 10/27 33 *92 indicates the mixing 2 ended. Mixing 2 started on the previous date. The same code is used for the other mixings. 10 E. L. Robinson, W. H. Irwin, and J. M. Symons Table 4. Number of Times Plankton Appeared in Samples. al oO SS ars Be SS am am n =~ ~ Sane eo = ex oe Pai nc er CHES eS) ove.) See GENERA 5a @82 ne on Be GENERA Se SE oa ee 74 Green Algae ot EY ea ph mirc wo ey RERE CE Non-Filamentous Ah fea SO ie LN et Cd 84 SN Lee BH = a = a pen rain 4 An aw YS YS et aL aw aw awry aw avd aN AN at 3 3 ° ° ri 2 2 8 v 2 v © LS a =] a a te Ankistrodesmus = 3 Blue-Green Botryococcus = 1 - - Algae Chlorobotrys 1 - = = = Anabaena (100) 12 Bo fo il Chlorella 5 6 5 10 9 Single Cells 9 - 10 - - Chlorogonium 6 2 1 - - Anacystis 14 8 - 10 9 Chlorococcum - 4 - 10 4 Aphanizomenon 14 4 12 7 5 Chodatella - 1 - - 4 Coelosphaerium = 6 - 2 - Chroococcus - 1 - 1 - Cylindrospernum 1 - 7 10 Closterium 3 4 9 6 10 Gomphos phaeria 9 4 - - - Coelastrum 19 6 19 9 7 Oscillatoria 13 8 1l 7 8 Cosmarium 3 7 2 5 1 Phormidium - 2 1 5 Crucigenia = = = 2 l reeset i 2 L ll 7 1 agellates Been aeece - 1 = = = Ceratium 8 6 10 7 6 Eurastrum - 2 - 2) = Chrysococcus 4 5 3 BLE Franceia - 1 - - 3 Cryptomonas 4 4 - 2 10 leocystis 1 2 1 8 4 Dinobryon - - - - Be vinvide - 1 5 : 1 Euglena 5 6 4 6 1l Hormidium - - 1 - - Euglenopsis 1 - - - - Lagerheimia - - - - 1 Glenodinium - - 5 7 Oocystis 17 8 19 10 10 Golenkinia - - 6 - - Pamella - 2 4 4 - Gymnosinium 1 = > 2 3 Pandorina - - - - 2 Lepocinclis - - - - 1 Pediastrum 3 1 2 1 = Mallomonas 4 3 6 2 4 Planktosphaeria - 1 - = = Peridinium 5 6 1 1 5 Pleodorina 1 - - - - Phacus - 1 1 5 6 Scenedesmus 7 7 5 8 Trachelmonas 17 8 1l 7 ll Selenastrum - - - 1 Diatoms Sphaerocystis 17 2 6 - Ze Achnanthes - 1 - 4 7 Staurastrum 8 2 12 7 2 Asterionella 5 7 8 9 1 Sticococcus - - - 2 - Cyclotella 1 3 1 2 4 Tetraedron = 3 - - - Cymbella - 2 = 2 2 Green Algae Fragillaria 2 3 = 6 6 Filamentous Gomphonema - - - 2 3 Cladophora ‘. 1 - 1 - Melosira = 6 = 3 5 Hormidium 1 - - - Navicula 1 2 3 2 Microspora 1 - - 1 - Nitzschia 2 5 1 4 Oedogonium - - - - 1 Pennularia - 1 = = 1 Spyrogyra - - 1 - Rhopalodia 2 1 - - = Stigeoclonium - 1 - - - Stauroneis 2 3 1 1 2 Tribonema 1 1 = 2 - Synedra). 2) Jus) 235 ee eee Ulothrix = L = - - Zooplankton Green Algae Crustaceans Flagellates Copepods 4 3 4 5 2 Chlamydomonas 23 8 21 10 11 Cladocerans 3 1 2 7 2 Coccomonas - 3 - 2 2 Rotifers Gonium - 1 - 2 4 Sp. 5 - - - 2 Phacotus 9 2 10 6 9 Keratella 5 2 4 7 3 Ciliophorans sp. 6 - 6 4 4 Rhyzopods sp. 1 2 1 5 5 Actinopods sp. - 2 = = Codenella - - - < Nematodes sp. - 1 - - 1 The predominant plankton, based on the numbers of organisms in the unmixed lake were as follows: green algae—Ankistrodesmus, Chlamydom- onas, and Chlorella; blue-green algae—Anabaena, Anacystis, Aphanizom- enon, and Oscillatoria; diatom—Asterionella, Nitzschia, Melosira, and Syn- edra; pigmented flagellates—Ceratium, Chrysococcus, Glenodinium, and Trachelmonas. The predominant genera of algae at the time of optimum growth in Test Lake I during 1966 were: green algae—Chlorella and Chlamydomonas (their numbers were higher in the upper layers); blue-green algae—An- Influence of Artificial Destratification 11 abaena and Anacystis. Pigmented flagellates appeared for a short period, the most abundant being Chrysococcus, Euglena and Ceratium. Few zoop- lanktonic forms were found in Test Lake I during 1966. In Test Lake II in 1966, the greatest number of genera was among the green algae but the largest populations were blue-greens. At the mid- summer optimum, the most abundant genera of the blue-green algae were Anabaena, Anacystis, Cylindrospermum and Oscillatoria. Phormidium suc- ceeded ni the period following the midsummer optimum, and was dom- inant the remainder of the season. Pigmented flagellates increased as temperatures rose, the predominant genera being Chlamydomonas. Also, appreciable numbers of Glenodiuium and Trachelmonas were present. Relationship to Water Quality The diagrams in Figures 8 and 9 show the relationship of the phytop- lankton populations to some important chemical water quality parameters in Test Lakes I and II during 1966. The data in these diagrams were plotted quantitatively as were data in previous charts. These diagrams are arranged to show the changes in the total number of phytoplankton in the entire lake with time, together with changes in the average concentra- tion of some of the chemical constituents. The average chemical concen- trations were calculated by weighting the individual concentrations from the samples at various depths according to the volume of the water layer at the sampling depth. In this way, a weighted vertical average chemical constituent concentration was obtained. The use of total plankton numbers and weighted vertical averages has its disadvantages because the bulk of the algae and the bulk of a given chemical constituent may be vertically separated in a lake, thus having little, if any, relationship to, or influence on, each other. Diagram 2 of Figure 8 shows an increasing trend in organic nitrogen concentrations during mixings 2, 3, and 4, and abrupt declines following mixings 3 and 4 in Test Lake I. The nitrate nitrogen decreased as plankton pulses increased, and increased despite pulses during mixings (diagram 3). The ammonia nitrogen concentration shows no relationship to plankton pulses, and increased in the two test lakes during the last half of the summer as shown in diagram 4 in Figures 8 and 9. The total hydrolyzable phosphorus concentration and the plankton numbers appear unrelated in Test Lake I (diagram 5, Figure 8). The addition of phosphorus as fertilizer in Test Lake II during 1966 is reflected in increased plankton and phosphorus measurements, as discussed by Gerloff and Skoog (1957). Concentrations of carbon dioxide, DO, and plankton show similarities in both lakes (diagrams 6 and 7) and an increase in carbon dioxide during mixings 1, 3, 4, and 5 in Test Lake II (Figure 9). Mixing 2 occurred as a large plankton pulse was developing (Figure 9). The growing algae used much of the CO,. The oxygen demanding processes decreased the DO concentration that occurred throughout the summer season, even when plankton numbers were largest and contributing oxygen. 12 E. L. Robinson, W. H. Irwin, and J. M. Symons Heat Budget, Alkalinity and Hardness Mixing increased the heat content of each lake an average of about 17 percent (Irwin et al., 1967). The surface layer budget decreased while deeper layers (normally cold) increased their heat budget. The heat, uniform in the mixed lakes, was transferred to the deeper waters. Associ- ated with the increased heat budget was a decrease in total plankton num- bers for each test lake, with a greater decrease in blue-green than green JUL TEST LAKE I 1966 q SEPTEMBER OCTOBER 2. ORGANIC N 3. NITRATE N 4. AMMONIA N 5. PHOSPHORUS 10. HARDNESS Figure 8. Diagroms showing the variations of physical and chemical parameters from Boltz Lake and their relationships to the total plankton populations. Bars at the top of the columns indicate stirring periods. Influence of Artificial Destratification 13 TEST LAKE IL 1966 MAY JUNE JULY AUGUST SEPTEMBER OCTOBER y — Tt 1. TOTAL PLANKTON 2. ORGANIC N 3. NITRATE N 4. AMMONIA N Figure 9. Diagrams showing the variation of physical and chemical parameters from Falmouth Lake and their relationships to the total plankton populations. Bars at the top of the columns indicate stirring periods. algae numbers. Following the summer pulse the plankton numbers of the control lake decreased, though this was slight compared to commensurate reductions in the test lakes. Populations decreased when the total heat budget was at its maximum in the two test lakes (Figures 8 and 9). The abundance of blue-green algae is consistent with reports that blue- greens favor hard waters (Prescott, 1951). Alkalinity and hardness results are also listed in Figures 8 and 9 for the two test lakes. 14 E. L. Robinson, W. H. Irwin, and J. M. Symons Temperature and Turbulence Blue-greens predominated when the temperature was the highest in all three lakes. The predominant genera found were similar to those re- ported by Cole (1957) in a Southern Kentucky stratified artificial im- poundment. The effect of temperature on genera was clearly observed from data of the unstirred lake, which showed blue-greens to be predom- inant in upper waters where temperature was above 15°C, and greens predominant in the lower waters where temperatures were less than 15°C. Green algae, however, never were found in quantities sufficient to cause conspicuous blooms. The effect of increased temperature on green and blue-green algae was demonstrated in laboratory experiments (Venkataraman and Yanagita, 1964) in which a species of Chlorella was killed exponentially when heated for short periods, but the blue-green Anacystis was able to withstand longer periods of heating. While the waters studied in nature during this experi- ment did not reach temperatures as high as those in the aforementioned experiment, there may be some correlation. Chu (1942) reported that temperature within normal limits had little effect on the plantonic forms he studied; he stated further that chemical DISCUSSION Environmental factors important to plankton production are variable, and natural growth patterns must be compared with those in controlled laboratory experiments to explain the controlling factors and their func- tions in the algae environment. Influence of Stratification and Light Plankter numbers in the stratified control lake were greatest in the deeper layers. Water of this lake was clear, and its light penetration greater than in the Test Lakes, effecting increased algal growth. Light intensity was not as great at the lower depths as at the surface; also the plankton may have been stimulated by chemicals concentrated in the stratified layers. These findings concur with those of Juday and Schomer (1935) who demonstrated that excessive light inhibits algae growth. The effect of excessive light intensity on plankton growth is a photo-oxidative destruction of chloroplast enzymes (Steeman-Neilsen and Hansen, 1959; Steeman- Neilsen and Jorgensen, 1962). Light intensity also affects the uptake of phosphorus and influences the ratio of phosphorus to sulfur within the algal cells during metabolism (Kylin, 1964). Variances in light intensity may also bring about different requirements for iron and manganese by algae (Gerloff and Skoog, 1957). The complex interrelationship of temperature and light affects carbon dioxide assimilation, thus affecting growth (Krauss, 1956). Influence of Artificial Destratification 15 composition of growth medium under suitable conditions of illumination is probably of greatest importance to plankton growth. Powell et al., (1965) conducted experiments to assay the effect of turbulent flow on the growth of algae in a closed system. The experiments were arranged to provide the alternating periods of light and darkness reportedly necessary for optimum growth. The experimenters concluded that turbulence alone can be ex- pected to produce favorable light and dark cycles for only a small per- centage of algae in a flowing solution. This may account for the failure of blue-green algae to produce blooms in the mixed waters. Influence of Mixing Mixing alters the length of time organisms remain in contact with salts, gases and other chemicals in solution. In spite of the mixing of phos- phorus throughout the test lakes, the number of plankters decreased throughout the whole lake in all layers. Many other environmental changes undoubtedly influenced the changes in plankton populations that occurred during mixing. Single species may have been affected in many ways, even increased, but over-all the algal numbers decreased. Mixing of waters may move plankters from phototrophic levels to areas of reduced light, altering the time of plankter exposure to illumination and thereby retarding growth (Krauss, 1956). Nitrogen, Phosphorus and Trace Nutrients The nitrogen contents in the three study lakes were consistent with amounts found in nature. Some increase in ammonia-, nitrite-, nitrate-, and organic-nitrogen concentrations occurred in Test Lake I during 1966 following each stirring, and some decrease occurred in all but the organic- nitrogen concentration at Test Lake II during the same summer. The organic-nitrogen increase may have been due to extra-cellular substances released by some algae as they lysed or were broken apart by stirring. Growth conditions could have been such that toxins were formed in some species and released into the surrounding waters, thus limiting other species (Tucker, 1956; Nalewajko, 1966; Scott, 1964). Algae are inhibited when the concentration of nitrogen and phosphorus exceeds 20 mg/l (Chu, 1942), a concentration that was never reached in the three lakes studied. Deficiencies in growth occur when the nitrogen concentra- tion is below 0.2 mg/l and when phosphorus is below 0.05 mg/l (Chu, 1943). These levels also did not occur in the study lakes; thus it is un- likely that these two chemicals were limiting the whole plankton crop. Large populations of diatoms require higher concentrations of nitrogen and phosphorus than are generally found in nature, which may explain the scarcity of diatoms in the three lakes studied. Also, some diatoms seem to require a growth factor which affects the phosphorus dependency (Chu, 1943). The diatom population increased as the phosphorus concentration increased at Test Lake II in 1966. Iron, manganese and sulfides were 16 E. L. Robinson, W. H. Irwin, and J. M. Symons found in the study likes in quantities that probably were not limiting (Rodhe, 1948). Gerloff and Skoog (1957) concluded from laboratory studies that available nitrogen is the most important limiting factor in algal growth. This may not always be the case because algal growth in natural waters must depend upon depth, location, time of year, rates of absorption, rates of water replacement, temperature and other conditions. SUMMARY Based on the data presented herein, the following conclusions are drawn: 1. The total plankton numbers declined during most mixings, both in 1965 and 1966. 2. Except for a somewhat higher surface concentration in Test Lake II, Falmouth Lake, the plankton densities were similar at all depths in all three study lakes. 3. During most mixings the blue-green algal populations declined more than the green algal populations. 4. During artificial destratification the number of plankton species remained the same or increased slightly in both test lakes. 5. In some cases a change in the total plankton population in the lakes was reflected in a change in the average concentration with depth of NH.-N, NO;-N, Organic-N, total and soluble acid hydrolyzable phos- phorus, and carbon dioxide. The average concentration with depth of DO was not related to the total plankton population in the lakes. CONCLUSIONS Although insufficient experimentation has been done up until now (1968) to determine whether the changes in plankton population re- ported in this paper would occur in all lakes that were artificially destrati- fied, the influence on plankton appears promising enough to warrant fur- ther consideration. In addition to the favorable influence on plankton pop- ulation, artificial destratification improves water quality by adding DO and oxidizing any reduced material present. This engineering technique for water quality control should be given serious consideration if up- grading of water quality in a lake or reservoir is desired. ACKNOWLEDGMENTS The authors wish to thank Lawrence Kamphake, George Holtzer, and Richard Shibiya for the laboratory chemical analyses and Glenn R. Gruber for help with the field work. In addition, the cooperation of the personnel of the State of Kentucky Department of Fish and Wildlife Resources is gratefully acknowledged. Influence of Artificial Destratification 17 Literature Cited Bernhardt, H. 1967. Aeration of Wahnbach Reservoir without changing the temperature profile. Jour. AWWA, 59 (8) :943-964. Cole, G. A. 1957. Studies on Kentucky Knobs Lake. III. Some qualitative aspects of the net plankton. Trans. Kentucky Acad. Sci. 18 (4) :88-101. Cooley, P., J. A. Steel and J. E. Ridley, 1967. Discussion of impoundment destratification by mechanical pumping. J. San. Div., Am. Soc. Civ. Engrs. 93(SA-4) :139-141. Chu, S. P. 1942. The influence of the mineral composition of the medium on the growth of plankton algae. I. Methods and culture media. J. Ecology 30(2) :284-325. Chu, S. P. 1943. The influence of the mineral composition of the medium on the growth of plankton algae. IJ. The influence of the concentra- tion of inorganic nitrogen and phosphate phosphorus. J. Ecology 31(2):109-148. Gerloff, G. and F. Skoog. 1957. Nitrogen as a limiting factor for the growth of Microcystis aeruginosa in southern Wisconsin lakes. J. Ecology 38 (4) :556-561. Irwin, W. H., J. M. Symons, and G. G. Robeck. 1966. Impoundment destratification by mechanical pumping. J. San. Eng. Div., Am. Soc. Civ. Engrs., 92(SA-6) :21-40. Irwin, W. H., J. M. Symons and G. G. Robeck. Water quality in reservoirs and modifications from destratification. In press, Proc. Reservoir Fishery Resources Symposium, Southern Division, Am. Fish. Soc., U. Georgia, Athens, Georgia, April 5-7, 1967. Juday, C. 1934. The depth distribution of some aquatic plants. J. Ecology 15 (322320, Juday, C. and H. A. Schomer. 1935. The utilization of solar radiation by algae at different depths in lakes. Biol. Bull. 61:75-81. Krauss, R. W. 1956. Photosynthesis in the algae. Ind. and Engr. Chem. 48:1449. Kylin, A. 1964. The influence of phosphate nutrition on growth and sulphur metabolism of Scenedesmus. Physiol. Plant. 17:384-402. Nalewajko, C. 1966. Photosynthesis and excretion in various planktonic algae. Limnol. Oceanog. 11 (1):1-10. Powell, C. K., J. B. Chaddock and J. R. Dixon. 1965. The motion of algae in turbulent flow. Biotech. Bioneg. 7:295-308. Prescott, G. W. 1951. Algae of the western Great Lakes area. Cranbrook Inst. Sci. Bull. 31:4-33. Rodhe, W. 1948. Environmental requirements of fresh-water plankton algae. Almquist and Wiksells Boktryckeri A. B. Uppsala, Sweden. Scutt, J. E. 1964. Autoinhibiter production by Chlorella vulgaris. Ann. J. Bot. 51:581-584. 18 E. L. Robinson, W. H. Irwin, and J. M. Symons Steemann-Nielsen, E. and V. K. Hansen. 1959. Light adaptation in marine phytoplankton populations and its interrelation with temperature. Physiol. Plant. 12:353. Steemann-Nielsen, E. and E. G. Jorgensen. 1962. The adaptation to dif- ferent light intensities in Chlorella vulgaris and the time dependence on transfer to a new light intensity. Physiol. Plant. 15:505. Symons, J. M., W. H. Irwin and G. G. Robeck, 1967. Impoundment water quality changes caused by mixing. J. San Engr. Div., Am. Soc. Civ. Engrs. 93(SA2). Symons, J. M., W. H. Irwin, E. L. Robinson and G. G. Robeck. 1967. Im- poundment destratification for raw water quality control using either mechanical or diffused-air-pumping. J. AWWA, 59 (10) :1268-1291. Tucker, A. 1957. The relation of phytoplankton periodicity to the nature of the physico-chemical environment with special reference to phos- phorus. Am. Midland Naturalist 57 (2) :300-370. Venkataraman, G. S. and T. Yanagita. 1964. Photosynthetic activity as a measure of viability in microalgae. J. Gen. Appl. Microbiol. 10;69-76. Williams, L. G. 1963. Plankton population dynamics. National Water Qual- ity Network Supplement 2, PHS Publ. No. 663, Government Printing Office, Washington, D. C. Received September 12, 1968; Accepted June 10, 1969. NOTE ON THE LIFE CYCLE OF CATHAEMASIA RETICULATA (WRIGHT) IN THE EASTERN BELTED KINGFISHER JOHN VINCENT ALIFF and JAMES M. EDNEY Department of Zoology Lexington, Kentucky 40506 Cathaemasia reticulata, a trematode related to both the fasciolids and echinostomes, was described as Distomum reticulata by Wright (1879) from an eastern belted kingfisher, Megaceryle alcyon, near Toronto, Canada. Harwood (1936) referred the species to the genus Cathaemasia, created by Looss (1899) after examination of specimens from a kingfisher collected at Reelfoot Lake, Tennessee. C. reticulata has been collected from Iowa, Mich- igan, Kentucky and Tennessee, by us. Travassos (1916) described Pulchrosoma pulchrosoma from a Brazilian kingfisher, Streptoceryle torquata. Manter (1949) after examination of three specimens of C. reticulata from a belted kingfisher collected near Lin- coln, Nebraska, proposed the synonomy of Cathaemasia and Pulchrosoma. However, Van Den Broek (1963) has suggested that the comparative geographic and taxonomic isolation of hosts, as well as the different habitat of Cathaemasia within the host is sufficient to justify the genus Pulchrosoma, the Old World Cathaemasia being intestinal parasites of storks and the American species inhabiting the air sacs of kingfishers. Two adult trematodes, subsequently identified as C. reticulata were recovered from a male belted kingfisher collected from North Elkhom Creek, Russell Cave Road, near Lexington, Kentucky, on October 15, 1967. Subsequent collection of another eastern belted kingfisher from North Elkhorn Creek, November 16, 1967, near Frankfort, Kentucky, yielded five adult C. reticulata. The specimens of C. reticulata were recovered within the posterior abdominal air sacs lying next to the intestine of the bird. Harwood (1936) and Zeliff (1942) suggested that the correct loca- tion of C. reticulata is the intestine and that adults obtained within the air sacs had migrated there through shot holes. These birds were thoroughly examined and no shot holes were found in the intestine. After the adult C. reticulata were discovered, conspicuous spots along the mesentery were noted and examined microscopically. These spots proved to be numerous egg plaques consisting of as few as 7 to as many as 30 eggs within the gelatinous appearing mass. Subsequent examination of the trachea of the second bird yielded 68 trematode eggs. The two worms obtained from the first bird resembled those collected by Harwood (1936) in being about 10 mm long and 3.5 mm wide. The second bird yielded five larger worms, being on the average of 28 mm in length and 16 mm in width (Figure 1). Eggs were recovered from the plaques as well as a greater number from the adult worms. The amber colored eggs, from the first bird, have the following average measurements: 118.9 u length (a range of 105-124), 75.2 u width (a range of 68-82), John Vincent Aliff and James M. Edney 20 ca*geee* eae @D OS—Oral sucker, , OV—ovary, T1—anterior testis, T2—posterior testis, and G—gut. Line drawing of Cathaemasia reticulata adult showing: Figure 1: VS—Ventral sucker Life Cycle of Cathaemasia Reticulata 21 and 27.2 u opercular width (a range of 25.3-30.5). These measurements compare closely to those given by Harwood (1936), 110 u x 70 u and Zeliff (1942) 120 u x 75 u. The eggs from the second bird measured 122 u x 84 u. Eggs from one of Edney’s larger specimens in the U.S. National Museum measured 126 u x 92 u, the difference probably depen- dent on worm size. Eggs were removed from refrigeration on October 26 and allowed to embryonate at room temperature. The hatching period has been found to be about 32 days. The first notable development was noticed after 14 days, when the polygonal outlines of ciliated epidermal plates becaz2 evident. This event was followed by the appearance of an eye spot. at 17 days. (See Figure 2), and the appearance of flame cells at 18 days. All observa- tions were made on unstained live eggs. The taxonomic position of C. reticulata may be solved in the future when data on the morphology of the miracidium and other larval stages become available through this work. We would like to acknowledge the aid provided by the Kentucky De- partment of Fish and Wildlife Resources for the privilege of scientific ~' Figure 2: Photomicrograph of the developing miracidium of Cathaemasia reticulata showing eyespot. 22 John Vincent Aliff and James M. Edney collection, and the staff of the Frankfort National Fish Hatchery for their aid in collection of possible intermediate hosts. Summer research work was supported by a grant from the Thomas Hunt Morgan School of Biological Sciences and by a grant from the Kentucky Research Foundation. Literature Cited Broek, E. Van Den. 1963. Considerations of the taxonomy of the Genus Cathaemasia Looss, 1899. (Trematoda, Cathaemasiidae) Archives Neerlandaises de Zoologie Tome XV, 4: 472-490. Harwood, Paul D. 1936. Notes on Tennessee Helminths III. Two trema- todes from a Kingfisher. J. Tenn. Acad. Sci. 11: 251-256. Looss, A. 1899. Weithere Beitrage zur Kenntis der Trematoden Fauna Aegyptens. Zool. Jahrb. System 12: 521-784. Monter, H. W. 1949. The trematode Cathaemasia pulchrosoma (Travassos | 1916) N comb. from the body cavity of a kingfisher in Nebraska. J. Parasitol. 35: 221. Travassos, L. 1951. O genera Pulchrosoma Travassos 1916 e sua situacao no sistema de trematodeos. Archquivos de Zoologia do Estado de Sao Paulo 7,: 465-492. Zeliff, C. Courson, 1942. Observations on Cathaemasia reticulata a trema- tode from the Belted Kingfisher. Am. Naturalist V. LXXV, No. 760, 508-512. Accepted July 9, 1969. AGE AND GROWTH OF THE WESTERN BLACKNOSE DACE RHINICHTHYS ATRATULUS MELEAGRIS AGASSIZ, IN DOE RUN, MEADE COUNTY, KENTUCKY? 2 DONALD C. TARTER Biology Department, Kentucky Southern College Louisville, Kentucky 40222 INTRODUCTION The age and growth of fishes of the different year classes reflect, to a large extent, the well-being of the population and its ability to maintain itself under the extant environmental conditions. Two methods applicable to a study of the age and growth of the western blacknose dace, Rhinichthys atratulus meleagris Agassiz, in Doe Run are the scale method (Van Oosten, 1929) and the length frequencies as displayed by the individuals of the population (Van Oosten, 1938). These methods are particularly useful in studies of short-lived fishes where the lengths of the different year classes, particularly the juveniles, are easily separated and can readily be identified by examination of the scales. In the present study, age and growth of the western blacknose dace were based on 3,358 specimens collected from the upper 3.1 miles of Doe Run. Length frequencies, verified by the scale method, were used in aging the fish. In addition, length-weight relationship, coefficient of condition, pattern of scale development, and growth in length and weight were de- termined. I am sincerely grateful to Dr. Louis A. Krumholz for advice and en- couragement throughout this study and for criticism and suggestions in the preparation of this manuscript: DESCRIPTION OF THE STUDY AREA A detailed description of Doe Run (Minckley, 1963) has been sum- marized by Krumholz (1967) as a large torrent spring that rises near Ekron, in eastern Meade County, Kentucky. The stream flows north-north- east for about 3.5 miles and empties into Doe Valley Lake, a recent im- poundment of more than 500 acres and about 4 miles long. As it leaves the lake, Doe Run flows over the floodplain of the Ohio River for about 2 miles and empties into the Ohio River 3.5 miles east of Brandenburg, Kentucky, and about 36 miles downstream from Louisville (Figure 1). 1This paper is part of a doctoral dissertation submitted to the Graduate School, University of Louisville, in partial fulfillment of the requirements for the degree of Doctor of Philosophy, June 1968. It was supported in part by the U.S. Atomic Energy Commission, under Contract No. AT-(40-1)-3540 with the Uni- versity of Louisville, Louis A. Krumholz, Principal Investigator. 2 Contribution No. 119 (New Series) from the Department of Biology, Uni- versity of Louisville, Louisville, Kentucky 40208. 9A Donald C. Tarter 0 0 VALLEY oe INSERT A Dem! BRECKINRIDGE COUNTY ’ HARDIN Buffalo COUNTY INSERT 8 As, ing Seurce Siivil Figure 1.—Doe Run, Meade County, Kentucky, showing locations of collecting stations, stream miles, extent of Doe Valley Lake, and other features. The broken line through Doe Valley Lake shows the course of the stream prior to impoundment (after Krumholz, 1965). MATERIALS AND METHODS Each fish to be weighed was placed in cheesecloth to remove the excess preservative and was immediately weighed to the nearest milligram on a Mettler electric, single-pan balance. Total and standard lengths, to the nearest millimeter, were determined with a divider and the reading taken from a steel ruler. Both lengths were measured by the methods described by Hubbs and Lagler (1958). Total length is used consistently in this study. A conversion factor based on 274 dace of all sizes can be expressed as follows: Western Blacknose Dace 95 T.L. Sant 1.23 Length frequencies, verified by the scale method, were used to de- termine the age groups of 3,358 western blacknose dace collected from three stations in Doe Run. Data for the monthly collections were arranged in 2-mm length groups and the percentage frequency of each group was determined. The scales were removed by forceps from the left side of the body about midway between the dorsal fin and lateral line. Four or five scales were mounted in water under a cover slip and the number of annuli counted with the aid of magnification from a conventional scale reader. The most important characteristics used to recognize the annuli were crowding of circuli and the “cutting over” of circuli near the lateral margin of the scale (Lagler, 1956). The relationship between total length and weight was calculated from data on 3,358 western blacknose dace from three stations in Doe Run. There were no consistent differences in length and weight when each sta- tion was determined separately. For ease in presentation, those data were placed in 3-mm length groups and plotted on the average millimeter in- terval. A curve was constructed comparing empirical averages with cal- culated values. The following length-weight equation, in logarithmic form, was solved by the method of least squares: Log W = loga+nlogL where W = weight in grams, L = total length in millimeters, and log a and n = constants. As a part of the study of the length-weight relationship, K, the coeffici- ent of condition, the physical condition of a fish, was calculated for 3,358 dace (sexes combined), and 743 dace (sexes separate), using the follow- ing equation: W x 108 L3 where W = weight in grams, L = total length in millimeters. K= Standard length usually is used in this equation since the caudal fin contributes very little to the total weight, but for consistency in length measurements, I used total length. Growth curves based on 3,358 dace, were constructed for each age group, from monthly averages in length, to obtain the absolute growth rate. Growth curves also were constructed from computed lengths and weights for comparison with computed increments of length and weight for each age group. The percentage increase for length and weight of each age group was calculated. A series of smaller dace was preserved in 10 percent formalin for studying the pattern of scale development. 26 Donald C. Tarter AGE AND GROWTH Age Groups Length frequencies were used to distinguish the age groups of dace collected monthly from three stations in Doe Run (Figure 2). Histograms constructed for each station were quite useful in separating the younger age groups, but the overlap between the older age groups limited their usefulness. Age groups were designated by Roman numerals to indicate the age in years of fish. A fish which belonged to Age Group II had two annuli. There was very little overlap between Age Group 0 and Age Group I in the length-frequency distribution, but it increased between the older age groups. The number of annuli on the scales of fish in the areas of overlap was helpful in separating the older age groups. Three complete age groups, O, I, and IJ, were represented in the population, and there were a few individuals belonging to Age Group III. Length-Weight Relationship and Coefficient of Condition The length-weight relationship of the western blacknose dace in Doe Run was expressed by the following equation: Weal where W = weight in grams, L = total length in millimeters, and a and n = constants. The values for a and n were computed mathematically by the method of least squares. The equation was fitted to the average total lengths and weights between 28 and 88 mm in Figure 3, A and B, respectively. The length-weight equation is: Wea 28 Ona e eee There was a high coefficient of correlation (r = .90) between total length and weight of dace collected from Doe Run. In Figure 3, the circles represent empirical length-weight averages and the curve was plotted from the total lengths and calculated weights using the length-weight equation in Table 1. The calculated weights agreed quite well with the empirical weights and provided additional evidence that the length-weight equation can be used to determine the weight of a dace in Doe Run if only its length is known. The curve showed a gradual rise with increasing total lengths of dace, indicating that the weight in- creased proportionately faster than the total length of dace. A thorough review of the length-weight relationship in fishes was reported by Beck- man (1948). Calculations of the coefficient of condition (K), based on the cube law, are: WSK K Li Western Blacknose Dace OF. 10- December 342 Fish O- Roe > eo 1 =- io= November gre 598 Fish O- SO ) Io- October 527 Fish Oo- 10- September er 287 Fish ae O- SSS Oe -_ POs August < 176 Fish ° o- Dolan ie ae Pes ] o 10- July e ne 516 Fish be O- — —_— u 20- June 10- 460 Fish @® O- = AS pe! Ss ee eae =! 10- May 28 Fish ia o- Q el 0) eal) [4 0 j 8 at ee eee oe es a 10- March 107 Fish o- Sessa | oe nee Hess Ss 10- February | pm m 84 Fish o- come 1i0- January ar eel n 142 Fish Or | \ Pe-lejses ! .e) 20 40 60 80 100 120 Total Length, Millimeters Figure 2.—Length frequencies at monthly intervals of western blacknose dace from three stations in Doe Run, Meade County, Kentucky. 98 Donald C. Tarter Improvement in the condition of the fish is represented by an increase in the value of K (Van Oosten, 1938). The results, calculated from empirical length-weight data on the dace (Table 1) indicate that longer fish are relatively heavier bodied, since the Grams Weight, Total Length, Millimeters Figure 3.—Length-weight relationship of western blacknose dace from three stations in Doe Run, Meade County, Kentucky. Western Blacknose Dace 29 TABLE 1. Length-weight relationship and coefficient of condition (K) of western black- nose dace, based on empirical and calculated weights of 3,358 individuals, arranged in 3-mm length groups, from three stations in Doe Run, Meade County, Kentucky. Average Average Calculated Total Length Weight Weight K (mm) (g) (g) 8 0.003 0.003 S59 10 0.007 0.006 0.70 13 0.01 0.01 0.46 16 0.02 0.03 0.49 iy) 0.05 0.05 0.58 22 0.07 0.08 0.66 25 0.11 OsL2 0.70 28 0.16 0.17 0-73 31 0.22 0.24 0.74 34 0.29 0.33 0.74 37 0.38 0.43 0.75 40 0.49 0.55 0.77 43 0.60 0.70 0.76 46 0.74 0.87 0.76 49 0.89 1.09 0.76 52 1.09 1.11 0.78 539 7.29 33 0.78 58 1.58 1.58 0.81 61 1.82 1.86 0.80 64 205 2.18 0.82 67 2.48 2693 0.83 70 2.88 292 0.84 73 3.28 3.34 0.84 76 3.73 3.81 0.85 79 4.28 4.32 0.87 82 4.76 4.88 0.86 85 5.42 5.48 0.88 88 6.08 6.14 0.89 91 7.02 6.85 O9s 94 93 Tot 0.96 97 8.54 8.43 0.94 100 oT) 9.30 0.98 103 10.54 10.34 0.97 106 11.69 as 74 0.98 109 2761 12.43 0.98 ie? 14.17 135352 POL 115 16.08 14.74 1.06 118 17.26 16.04 1.05 124 18.21 sof 0.96 i —————————— 30 Donald C. Tarter slope of the logarithmic length-weight equation is greater than 3.0. The value of K increased with age since fish tend to gain proportionately more in weight than in length (Figure 3) as they grow older (Rounsefell and Everhart, 1953). An attempt was made to determine if any sexual differences in the coefficient of condition were present during the different seasons (Figure 4). Generally, both sexes showed similar fluctuations in condition in all seasons except winter. The mean coefficient of condition for both sexes started to increase in the middle of spring and reached its highest value just priod to spawning. Condition declined after spawning and was some- what constant in summer. Females showed a sudden rise in condition in early fall. Males sharply declined in condition in early winter but gradually increased from then until spring. The decline in condition of males in winter and early spring may be correlated with the high percentage of empty stomachs (Tarter, in press). The good condition of females in winter, early fall, and early spring may be correlated with the low percentages of empty stomachs at various stations during those seasons. Females had a higher mean coefficient of condition (1.22) than males (1.04), and the combined average of both sexes was 1.13 (based on 743 sexed specimens) ; the range was 0.94 to 1.57. The average coefficient of condition based on 3,358 specimens from Doe Run (sexes combined) was 0.82; the range was 0.46 to 1.06. The lower coefficient of condition was to be expected from the larger number of specimens since many of them were small. 1.60 8 1.40 = i< te} (S) 5 1.20 Females & All Fish oo /_-Males = 1.00 °o oO Dec Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Figure 4.—Mean coefficient of condition of both sexes of western blacknose dace col- lected at all seasons from three stations in Doe Run, Meade County, Kentucky. Pattern of Scale Development The pattern and sequence of scale development in western blacknose dace follows the pattern common to other minnows. No scales were found Western Blacknose Dace 31 on any dace less than 19 mm total length. There were a few cycloid scales along the lateral line area on the caudal peduncle of dace 19 mm long. As the fish increased in length, scale development proceeded gradually anteriorly from the caudal peduncle along the lateral line area with more scale rows developing below the lateral line than above it. By the time the fish reached a length of 21 mm, the scale pattern had developed beyond the origin of the dorsal fin, and had reached the area of the pec- toral fins at a total length of 23 mm. Western blacknose dace in Doe Run are completely scaled at a total length of 26 to 27 mm. Growth in Length and Weight Total Length The greatest absolute growth occurred during the first two years of life, with a gradual decline in the third year, in western blacknose dace collected from Doe Run (Figure 5). A preliminary study, based on 743 dace, indicated that only a small difference existed between the growth rates of males and females. Females were only slightly larger than males, therefore all the growth curves were based on combined data from both sexes. Growth rate was slightly faster the first year, and slowest in the Length, Millimeters Total Average Year of Life Figure 5.—Average calculated total length at the end of each year of life (solid line), and average yearly increment of growth (broken line) of western blacknose dace in Doe Run, Meade County, Kentucky. 32 Donald C. Tarter third year (Table 2). If the average length at the end of the third year. of life (104 mm) is taken as 100 percent, it is obvious that 45 percent and 85 percent of the total length was completed by the end of the first and second years of life, respectively. The total length at the end df each year of life and also the annual increments of length are shown graphically in Figure 5. The percentage increases in total length for the second and third years of life are listed in Table 2. TABLE 2. Average calculated total lengths in millimeters, annual increments of length, and annual percentage increase in total lengths of western blacknose dace in Doe Run, Meade County, Kentucky. Year of Life il ve 3 Total Length 47 88 104 Increment of length 47 41 16 Percentage of increase —_ 87 18 The average total length for each month of life for each age group is shown graphically in Figure 6. Young-of-the-year dace were collected in June and averaged 10 mm in total length. The smallest dace fry collected was 8 mm total length. The growth rate of dace was quite rapid during the summer and early fall of the first year of life, and they averaged be- tween 32 and 39 mm total length from September through November. Growth during winter was limited and dace of Age Group 0 averaged only about 38 mm long in early spring. Age Group I also grew rapidly in summer and averaged between 70 and 75 mm in fall. Inadequate sampling of dace in winter, due to high discharge in Doe Run, no doubt accounted for the somewhat erratic values during that season. Growth gradually in- creased again in spring. The growth rate of Age Group II was much slower in summer than the younger age groups. Dace in that age group reached a fairly constant level of growth in late summer and fall. The decline in growth in spring, especially in May, probably was due to inadequate sampling of fish because of secretive habits of spawning dace. A few fish (Age Group III) lived on into the fourth year of life but inadequate num- bers of specimens prevented any interpretation of growth. Weight The absolute growth curve of weight increased very slowly during the first year of life (Figure 7), quite the antithesis of length. The curve of Western Blacknose Dace 33 ee ee 120 ° 100 = 457 Specimens E = 80 = > iJ = 758 Specimens _ 60 \~] ° - o 40 = 2131 Specimens < 20 Jun Jul Aug Sep Oct Nov Dec Jan Feb Mar Apr May Figure 6.—Average total lengths of age groups based on measurements of 3,358 western blacknose dace from Stations |, II, and III, Doe Run, Meade County, Kentucky. weight rose sharply in the second and third years of life. The increment curve increased rapidly during the second year and declined only slightly during the third year of life. The average calculated weight (from length- weight equation), annual increments of weight, and annual percentage increase in weight are listed in Table 3. The percentage increase of weight during the second and third years of life was about 6 and 4 times greater, respectively, than the percentage increase in length during that same period. If the average weight at the end of the third year of life (10.6 grams) is taken as 100 percent, it is apparent that only 9 percent of the growth in weight was completed by the end of the first year and that an additional 50 percent was completed at the end of the second year of life. During the third year of life in Doe Run an additional 41 percent of the weight is added. 34 Donald C. Tarter ) 2 3 Year of Life Figure 7.—Average calculated weight at the end of each year of life (solid line) and average yearly increment of growth (broken line) of western blacknose dace in Doe Run, Meade County, Kentucky. TABLE 3. Average calculated weights in grams corresponding to the average calculated total lengths in Table 2, annual increments of weight, and annual percentage increases in weight of western blacknose dace in Doe Run, Meade County, Kentucky. Deena Year of Life i 2 3 Calculated weight 1.0 6.1 10.6 Increment of weight iLs{@) Deal: 4.5 Percentage of increase -- 510 74 Western Blacknose Dace 35 The percentages of length and weight indicated that 45 percent of the total length is reached by the end of the first year of life, but that nearly two years are necessary to reach an equivalent percentage of weight. GENERAL CONCLUSIONS AND DISCUSSION Length-frequency analysis is based on the assumption that the lengths of fish of one age group show variation in a normal distribution (Rounse- fell and Everhart, 1953). Fish of successive ages are clustered about suc- cessive lengths so that when data are plotted from a sample of the pop- ulation, the different age groups can be recognized (Lagler, 1956). The longevity of the western blacknose dace in Doe Run usually is three years, with some individuals living into the fourth year of life. It is doubtful that any dace completed four years of life in Doe Run. Traver (1929) and Noble (1964) reported that there were two age groups and three age groups, respectively, in blacknose dace populations they studied. Kuehn (1949) found five age groups and four age groups in females and males, respectively, in the longnose dace from rivers in southeastern Minnesota. The relative relationship between lengths and weights of fishes can be expressed in numerical terms (degree of well-being, plumpness, rel- ative robustness) using the coefficient of condition, K (Hile, 1936; Lagler, 1956). The values of the coefficient of condition are used to indicate the suitability of an environment by comparing fish from a specific area with a general average for an entire region (Rounsefell and Everhart, 1953). Hile (1936) presented a thorough review of the coefficient of condition in fishes, and indicated that the weight of a fish may be considered a func- tion of its length. If specific gravity and form were constant throughout the life of a fish, the relationship could be expressed by the cube law (W = cL?, where W = weight, L = length, and c = constant). Wide variation exists in nature for the value of c, which is not constant for a species or population. Noble (1964) reported the coefficient of condition (sexes combined) of backnose dace in Iowa to range from about 1.4 to 1.9, but no data were given for December, January, or February. No averages for sexes separate or combined were given for comparison. Males were more robust at one station and females at another station in his study. The direct proportion method for aging fish has been in use for many years (Van Oosten, 1929), and assumes a direct proportion between the growth of the scale and growth of the body throughout the life of the fish. Since it is well known that newly hatched fishes do not have scales, it was suggested by Fraser (1916) that a correction factor must be intro- duced as an addendum to the direct proportion method. The length of the body prior to development of the scales must be subtracted from the actual total length since it was present before any scales were formed. Such a correction factor is determined by actual measurements from specimens at 36 Donald C. Tarter hand or by extrapolating the regression line obtained when scale length is plotted against body length. The longest male and female dace collected from Doe Run were 121 mm (Station III) and 128 mm total length (Station Il), respectively, both in their fourth year of life. The longest blacknose dace previously re- ported in the literature, so far as I could determine, was by Moore et al. (1934), who reported an individual of 97 mm total length but did not report the sex. Kuehn (1949) reported that the largest longnose dace in his study was a 124-mm female, and that males never exceeded 96 mm total length. Traver (1929) indicated that the largest blacknose dace taken from Cascadilla Creek, New York, was 63 mm but did not indicate whether the measurement was in total length or standard length. The heaviest male and female dace collected from Doe Run weighed 17.2 grams (Station III) and 20.9 grams (Station II), respectively. The stage of development of the eggs in the female was no doubt partly re- sponsible for the greater weight. The constancy of water temperature, abundance of food on a yearly basis, and a long growing season at this latitude were important factors in Doe Run which influenced the fast rate of growth and produced larger blacknose dace than any reported in the literature. Literature Cited Beckman, W. C. 1948. The length-weight relationship, factors for conver- sion between standard and total lengths, and coefficients of condition for seven Michigan fishes. Trans. Am. Fish. Soc., 75:237-256. Fraser, C. 1916. Growth of the spring salmon. Trans. Pac. Fish. Soc., 2:29-39. Hile, R. 1936. Age and growth of the cisco, Leucichthys artedi (LeSueur), in the lakes of the northeastern highlands, Wisconsin. Bull. U. S. Bur. Fish., 48(19) :211-317. Hubbs, C. L., and K. F. Lagler, 1964. Fishes of the Great Lakes region. (revised ed.). Univ. Mich. Press, Ann Arbor, Mich. 213 pp. Krumholz, L. A. 1965. A radioecological study of the biota of Doe Run, Meade County, Kentucky. USAEC Doc. No. TID-22815. Microfiche. ————— . 1967. Accumulation of radioactive fallout materials in the biota of Doe Run, Meade County, Kentucky. 1959-63. In Radioecological Concentration Processes. Pergamon Press, New York. Pp. 791-818. Kuehn, J. H. 1949. A study of a population of longnose dace Rhinichthys c. cataractae. Proc. Minn. Acad. Sci. 17:81-87. Lagler, K. F. 1956. Freshwater fishery biology, W. C. Brown Co. Dubuque, Iowa. 421 pp. Minckley, W. L. 1963. The ecology of a spring stream: Doe Run, Meade County, Kentucky. Wildl. Monogr., 11:1-124. Western Blacknose Dace 37 Moore, E., J. R. Greeley, C. W. Greene, H. M. Faigenbaum, F. R. Nevin, and H. K. Townes. 1934. A problem in trout stream management. Trans. Am. Fish. Soc. 64:68-80. Noble, R. L. 1964. Life history and ecology of western blacknose dace, Rhinichthys atratulus meleagris Agassiz, Boone County, Iowa. Unpub- lished master’s thesis, lowa State University, Ames, Iowa. 76 pp. Rounsefell, G. A., and W. H. Everhart. 1953. Fishery Science. John Wiley and Sons, Inc., New York. 444 pp. Tarter, D. C. 1969. Food Habits of the Western Blacknose Dace Rhinichthys atratulus meleagris Agassiz, in Doe Run, Meade County, Kentucky. Am. Midl. Nat. (In press). Traver, J. R. 1929. The habits of the black-nosed dace, Rhinichthys atronasus (Mitchill). J. Elisha Mitchell Sci. Soc., 45(1):101-125. Van Oosten, J. 1929. Life history of the lake herring (Leucichthys artedi LeSueur) of Lake Huron as revealed by its scales, with a critique of the scale method. Bull. U.S. Bur. Fish., 44, 1928 (1929) :265-428. ————— . 1938. The age and growth of the Lake Erie sheepshead, Aplodin- otus grunniens Rafinesque. Pap. Mich. Acad. Sci., Arts, Lett., 23 (1937 ) :651-668. Received December 31, 1968; Accepted July 9, 1969. A STUDY ON PLETHODON RICHMONDI FROM MASON COUNTY, KENTUCKY, WITH NOTES ON ITS DISTRIBUTION WITHIN THE STATE JAMES T. WALLACE* Department of Biology, Eastern Kentucky University Richmond, Kentucky 40475 The Ravine salamander, Plethodon richmondi, thought for many years to be an aberrant form of Plethodon cinereus, was first described by Net- ting and Mittleman, 1938. Since then, few papers concerning P. richmondi in Kentucky have been published. The species is recorded in the literature from 13 counties in Kentucky. These literature records are as follows: Adams (1940, unpublished thesis), Breathitt, Floyd, Harlan, Knott, Law- ernce, Pike and Perry Counties; Dury and Gessing (1940), Kenton, Camp- bell, Harlan and Carter Counties; Schmidt (1953), Carter and Fayette Counties; Welter and Barbour (1940), Carter and Rowan Counties; Bar- bour (1953), Harlan County; and Wallace and Barbour (1957), Mason County. The zoological collection of the University of Kentucky contains speci- mens from all of the above named counties with the addition of 18 others. These are Bath, Bell, Boyd, Bracken, Clark, Harrison, Jefferson, Jessamine, Leslie, Madison, Montgomery, Nicholas, Pendleton, Powell, Robertson, Rockcastle, Scott and Wolfe counties. The distribution of these published and unpublished records is shown in Figure 1. Over a four year period from 1953-1956, a total of 230 specimens were collected from 13 localities in Mason County, in northern Kentucky. In general, the area is steeply sloping, well drained, and possessed of numerous outcroppings of limestone. A number of the specimens were found to be unsatisfactory for the study of certain variables; however, as much data as possible was taken. METHODS The following items of data were taken: a) Snout-vent length (s.v.)—From the tip of the snout to the posterior end of the vent; b) Tail length (t.I.)—Posterior end of the vent to the posterior tip of the tail; c) Costal grooves (c.g.)—The groove in close approximation to the axilla of the forearm was counted as number one. The two branches of the * Present address: Department of Histology, School of Dental Medicine, University of Pittsburgh, Pittsburgh, Pa. 15213. Study on Plethodon Richmondi 39 Ss oe aA F Be Ki (ac \ S Bago S ( (Ra @. Piukg wr % igh @: 3; sere CON GURE VW 40 James T. Wallace Y pattern, sometimes present just anterior to the hind legs, were counted separately as two grooves; d) Vomerine teeth (v.t.)—Counted via use of stereoscopic scope. e) Sex determination—Adult males were recognized by the presence of cloacal papillae. The females lack these papillae. Juvenile specimens were cut open and examined for the presence of darkening testes in the males or slightly swollen ovaries in the females or the presence of eggs. REPRODUCTION Wallace and Barbour (1957) described the eggs and newly hatched young of Plethodon richmondi found in the care of two adults of the species. The author has not found the eggs of this species in nature since that time. However, females having ovarian eggs were collected in March, April and November. Of the 94 females captured in March, 68 specimens (71.4%) contained ovarian eggs. These ranged from 0.5 mm to 3.0 mm in diameter. Twenty-three of the 35 females (60.7%) captured in April contained eggs of the same range diameter as in March. None of the three females taken in July contained developing eggs. Three of the five females collected in November were gravid. The eggs, however, ranged from only 0.5m to 1.0mm in diameter. This would indicate that laying had probably taken place in May or early June as suggested by the size of eggs found in the specimens collected in March and April. In all, 137 females were taken, of which 94 (68.6%) were gravid. The snout-vent length of the gravid females was similar in most cases. In March, the average snout-vent length of the gravid females was 51.6 mm; in April, 53.1mm; and in November, 47.6mm. The smallest female with developing eggs was 35 mm snout-vent with a tail of 61 mm. This specimen was taken on March 2, 1956, and was probably beginning its breeding cycle for the first time. The average number of eggs per female for each month ranged from 7.9 to 8.7 eggs per gravid female (Tables 1 and 2). TABLE 1. Egg diameter as related to month of collection. EGG SIZE MARCH APRIL JULY NOVEMBER IN MM. 0.5 t aL - 1 1.0 20 2 - 2 IAG} alah 6 a 2 2.0 23 12 = 2 2e5 ik 2 # m 3.0 6 2 - a 355) ot — - - Study on Plethodon Richmondi 4] TABLE 2. Comparative collecion and reproduction data. MONTH NO. NO. NO. % FEMALES AVG. NO. AVG. SIZE MALES FEMALES FEMALES WITH EGGS EGGS PER FEMALES WITH EGGS FEMALE WITH EGGS * MM. MARCH 60 oh 68 Talo! 8.7 51.6 APRIL 2h 35 23 65.7 7.9 Does JULY I 3 = = z i NOVEMBER 1 5 3 60 8.3 47.6 ANALYSIS Costal groove counts were made on 221 specimens. Table 3 concerns the number of costal grooves associated with animals of different snout- vent lengths. Five specimens had costal groove counts of 18, 27 had 19, 4 had 22, and 1 had 23 costal grooves. It is easily seen from Table 3 that 19-21 costal grooves is the most common. On 83 males and 135 female specimens, costal groove counts, counts of the number of vomerine teeth in each half of the upper jaw, and a measure of the snout-vent length was taken. Tail length and total length were measurable on 48 of the 83 males, and 107 of the 135 females, in addition to the above measures listed for the larger group. Tables 4, 5, and 6 contain the statistical values calculated from the raw data. T-tests of the difference between means and F-tests of the ratios between variances and of the ratios between the coefficients of variation squared were performed. Those values which were found to be statis- tically significant at P = 0.05 are indicated by asterisks and those sig- nificant at P = 0.01 by double asterisks. TABLE 3. Costal groove count as related to snout-vent length. S.V. LENGTH IN MM. TOTAL NUMBER OF COSTAL GROOVES 18 19 20 aul 22 23 30 1 4 6 3 o a ho 3 10 41 2h 2 - 50 1 12 73 36 1 ak 60 - 1 1 - iL - SPECIMENS PER GROOVE SERIES 5 27 TOA fy 463 4 1 42 James T. Wallace TABLE 4. Comparative statistics as related to sex and morphological character involved. COSTAL -VOMERINE VOMERINE SNOUT*VENT TAIL TOTAL GROOVES TEETH TEETH LENGTH LENGTH M F R-M L-M R-F L-F M F M F M F N 83 135 83 83 135 135 83 135 48 107 48 107 2 20.19 20:18 5.08 5.14 5.33 5.41 48.22 50.77 43.64 48.W6 91.35 99.43 8 0.76 0.79 1.07 1.12 1.19 1.14 4.50 5.51 8.40 8017.64 12.02 12.73 5. 0.08 0.06 0.12 0.12 0.10 0.10 0.49 0.47 1.21 0.74 1.73 1.23 cv «3.74 3.92 21.10 21.71 22.33 21.20 9.34 10.85 19.24 15.76 13.15 12.80 TABLE 5. Calculated t values for selected mean and variance comparisons. P = 0.05 (*); P= 0.01 (**). COSTAL VOMERINE VOMERINE SNOUT-VENT TAIL TOTAL, GROOVES TEETH TEETH LENGTH LENGTH LENGTH M-F (R,M)-(R,F) (L,M)-(L, F) M-F M-F M-F t. 0.094 1.564 1.709 3.550% 4 .660%* 891% M-(R-L) F-(R-L) te 0.353 0.560 TABLE 6. Calculated F values for selected mean and yariance comparisons. P = 0.05 (*); P=0.01 (**). COSTAL VOMERINE VOMERINE SNOUT-VENT TATL TOTAL GROOVES TEETH TEETH LENGTH LENGTH § LENGTH M-F (R,M)-(R,F) (L,M)-(L, F) M-F M-F M-F Fo 1.09 1.23 1.06 1.50* 1.21 1.08 M-(R-L) F-(R-L) Fo 1.08 1.07 No statistical differences were found between the mean costal groove counts of the separate sexes. No statistical differences were found in the mean number of vomerine teeth either between sides within the sexes or within sides between sexes. Th mean snout-vent lengths between the sexes and the variance ratios were statistically significant at P = 0.01, df.co, t, (table value) = 2.575 and P = 0.05, d.f. (females 100, males 80), t, = 1.42, respectively. Both the tail length and total length means were statistically significant between the sexes at P= 0.01, df.co, t, = 2.575; however, neither the variance ratio between the sexes for the tail length or total length was statistically significant at P = 0.05. Study on Plethodon Richmondi 43 None of the ratios of (C.V.)? between sexes were significant at the P = 0.05 level. Neither, in the case of the vomerine teeth, were the (C.V.)? ratios between sides within sexes statistically significant at P = 0.05. The coefficients of variation are rather high for all variables except the number of costal grooves. Such high values are usually indicative of either an insufficient sized sample or an extremely variable biological system. The latter appears to be the most probable considering the size of the sample involved. The coefficient of variation is used as a means of relating the measure of absolute variation, the standard deviation, to a measure of absolute size, the mean. The use of this statistic depends on the assumption that varia- tion is relative to absolute size in the biological sense. F-tests were made of the values of ratios between coefficients of varia- tion squared since the squaring process allows a test of the variance di- vided by the mean squared of the samples. The statistical treatment of the data suggests that both sexes are under similar developmental regulation as indicated by the general lack of static- tical differences between the variance measurements of the two sexes. The greater absolute size of the females, however, is statistically different from that of the males, thus, defining this parameter as a populational sexual dimorphism, rather than as a response to widely different biological mech- anisms within the species. Literature Cited Adams, William, Jr. 1940. Some amphibia of Eastern Kentucky. Unpub- lished Thesis. George Peabody College for Teachers, Nashville, Ten- nessee. Barbour, Roger W. 1953. The amphibians of Big Black Mountain, Harlan County, Kentucky. Copeia 1953:84-89. Duellman, William E. 1954. The salamander Plethodon richmondi in South- western Ohio. Copeia 1954:40-45. Dury, Ralph and William Gessing, Jr. 1940. Additions to the herpetofauna of Kentucky. Herpetologica 2:31-32. Netting, M. Graham and M. B. Mittleman 1938. Description of P. rich- mondi, a new salamander from West Virginia and Ohio. Ann. Car- negie Museum 27:287-293. Schmidt, Karl P. 1953. A check list of North American amphibians and reptiles. Amer. Soc. Ichth. and Herp., Univ. Chicago Press, Chicago, 6th ed., 280 pp. Simpson, George G., Ann Roe, and Richard C. Lewontin 1960. Quantitative Zoology. Harcourt, Brace and Company, New York, 440 pp. Wallace, James T. and Roger W. Barbour 1957. Observations on the eggs and young of Plethodon richmondi. Copeia 1957:48. 44 James T. Wallace Welter, Wilfred and Roger W. Barbour 1940. Additions to the herpeto- fauna of Northeastern Kentucky. Copeia 1940:132-133. Wood, John T. 1945. Plethodon richmondi in Green County, Ohio. Copeia 1945:49. ACKNOWLEDGEMENTS: The author wishes to thank Dr. Roger W. Barbour, Department of Zoology, University of Kentucky, for the loan of some of the specimens used in this study. Accepted July 10, 1969. SOME NOTES ON THE GROWTH, DEVELOPMENT AND DISTRIBUTION OF OCHROTOMYS NUTTALLI (HARLAN) IN KENTUCKY JAMES T. WALLACE* Department of Biology Eastern Kentucky University Richmond, Kentucky 40475 Ochrotomys nuttalli (Harlan), the golden mouse, occupies primarily the southeastern quadrant of the United States from southern Virginia west throughout Kentucky, southern Illinois, southeastern Missouri, eastern Oklahoma, eastern Texas and southeast to Florida. Although widely dis- tributed, the golden mouse has not been extensively studied in Kentucky; therefore, the presentation of additional data concerning this species is particularly relevant. Goodpaster and Hoffmeister (1954) produced a comprehensive study of the life history of the golden mouse in Kentucky, while Barbour (1942, 1951), has added important details about nests and habitat of the species within the state. No other literature references concerning the golden mouse in Kentucky are known to the author. Primarily among the publica- tions concerning Ochrotomys in other states are studies of its home range (Dunaway, 1955); ectoparasites (Layne, 1958); response to different small mammal traps (Sealander and James, 1958); response to flooding (Mc- Carley, 1959); ecology, behavior and population dynamics (McCarley, 1958); spermatozoa (Hirth, 1960); growth and development (Layne, 1960); distribution (Brown, 1963); hematology (Gough and Kilgore, 1964); nests (Packard and Garner, 1954); and litter size (Blus, 1966). Although the above publications treat, in detail, many of the important aspects of the biology of Ochrotomys, the golden mouse has not been suf- ficiently studied within enough portions of its range for an adequate an- alysis of its geographic variation; therefore, the following data will sup- plement the slowly growing literature concerning this species. The author has had the opportunity to study the litters of several golden mice collected within the state; however, the data presented here consist of only the most complete and consecutive records kept on any of the litters. Fragmentary data collected on other litters support, in general, the following description of the growth and development of this single litter of three males. An adult female was captured near Colossal Cave, Mammoth Cave National Park (MCNP), Edmonson County, Kentucky, April 23, 1961 and had been retained in isolation 34 days before the birth of young oc- curred at 12:20 P.M., May 27, 1961. The young were not disturbed for weighing until 9:15 P.M. of the same day at which time a single member * Present address: Department of Histology, School of Dental Medicine, University of Pittsburgh, Pittsburgh, Pa. 15213. 46 James T. Wallace was found to weigh 2.56 grams. By way of comparison, three young of a Madison County female, captured on July 18, 1961, weighed 1.75, 1.76, and 1.66 grams, respectively, at one day post-natal on July 27, 1961. Positive righting reactions were immediately noticeable at birth and nursing began within minutes after parturition. The milk obtained during nursing was easily visible in the swelled stomach through the ventral abdominal wall. The eyes were closed. On the second day following birth, the tail showed a slight bicoloration being darker dorsally. Ventrally the caudal vein was prominent and easily visible through the light ochrous fur. The whiskers were five millimeters in length. Squeaking of the litter mates was frequent. Nursing was vigor- ous, but the young could remain attached to the nipples during only a few inches of travel when the female left the nest. In general, the body fur showed dorsal darkening. Changes in body weight, crown rump length, tail, ear, hind foot and whisker length were recorded periodically. These data appear in the ac- companying tables, and will be discussed later. Four days after birth, righting reactions were more rapid, upright wobbling about a point occurred and a tenacious attachment to the nipples of the mother was demonstrable. Development of the ventral abdominal fur resulted in a pale opaque pelage which almost obscured the stomach when viewed ventrally. Increased darkening of the ochrous dorsal tail fur occurred while the ventral tail pelage became slate colored. The pinnae of ears remained folded closed and became cinnamon colored on the anterior apical edges and posterior-dorsal portions. Six days post-partem, the litter mates were agile and ran about blindly upon release, demonstrated a distinct clinging reaction, and hung on the finger of the author in an inverted position when it was presented to them. Distinct openings were visible at the ear locations. The ventral abdominal pelage lengthened as a short pale fur while the lateral areas became light brown. At eight days, the eyes remained closed and the young, attached to the nipples, accompanied the female when she journied from the nest. Body fur extended posteriorly over and covered the base of the tail. Squeaking became decidedly more frequent. The dorsal pelage took on the dark ochorous color of the adults and the white ventral fur appeared distinctly dense. Nine days after birth, the scrotal sac of the males began to enlarge and the eyes remained closed. Eye opening occurred on the 12th day; however, considerable squint- ing was noticeable. Marked difference in mobility was observed and the young tended to jump on the hand or any object held near by. The well furred ears were sensitive to being touched and became folded against the head when disturbed. The ventral abdominal fur showed a yellowish tinge. Fifteen days after birth, squeaking gave way to chattering, nursing was Growth, Development & Distribution of Ochrotomys Nuttalli 47 reduced to infrequent periods, the ears were shaped as in adults, sitting occurred upon release, and the eyes ceased to be overly sensitive to the light. Full weaning had occurred by 24 days of age with no nursing being observed. DISTRIBUTION The distribution of Ochrotomys nuttalli (Harlan) in Kentucky has not been adequately established; however, from the pattern of the distribu- tion records available to date, it appears that the animal occupies pri- marily the eastern, southern and western portions of the state. Excluded are the central Inner Bluegrass area and the non-mountainous portions of the Outer Bluegrass region both of which are within the confines of the Knobs. Osgood (1909) reported the golden mouse from Lincoln County, Ken- tucky; Welter and Sollberger (1939) and Barbour (1942) reported speci- mens from Rowan County. Specimens from Harlan County were reported by Barbour (1951), and Barbour (personal communication) reported the collection of Ochrotomys in Hickman, Breathitt, Madison, and Bullitt County. Goodpaster and Hoffmeister (1954) reporter golden mice from Lewis, Carter, and Edmonson County. The author has collected Ochrotomys in Barren, Hickman, Hopkins, Christian, Madison and Edmonson County and has reliably sighted the species in Hart County. The following data pertain to specimens collected by the author: BARREN COUNTY, Kentucky, 0.4: mi. ENE Little Hope Church, 0.1 mi. NW Sand Cave, Mammoth Cave National Park (MCNP), 22 April 1961, elevation 910’, adult female, total length 187 mm, tail 84.5, hind foot 18.5, and ear (from notch) 19.5, with 3 fully furred young, eyes open, attached to nipples, from nest 12’ high in cedar tree; CHRISTIAN COUNTY, Ken- tucky, 1 mi. NNW of park lodge, Pennyrile State Forest, 3 July, 1961, elevation 450’, adult male (187-88-20-18), testes 10 mm by 15 mm long (scrotal), 26.1 gms, honeysuckle (Lonicera) covered fence row, also, adult scared from a nest 7’ high in a honeysuckle covered pine tree, Pennyrile State Forest 9 mi. S Dawson Springs, 1 July, 1961, several empty nests were found.in the area; EDMONSON COUNTY, Kentucky, 0.7 mi. S. Mammoth Cave Church, near Colossal Cave, MCNP, Flint Ridge, 23 April, 1961, elevation 620’, adult female with three young, darkly pigmented, eyes not open, nest 7’ above ground and 24 way out limb of cedar tree of 30-35’ height, HART COUNTY, Kentucky, specimen sighted by the author as it climbed about in a tree after leaving the nest (date unrecorded); HICKMAN COUNTY, Kentucky, 1.2 mi. S. Beulah, route 307, Murphey’s Pond Swamp, honeysuckle growth contained a nest with three subadult males, 5 November, 1966; HOPKINS COUNTY, Kentucky, 1.37 mi. NW junction Ky. 109 and U.S. 62, 1 July, 1961, elevation 460’, adult male (160-74-18-17), testes 5 x 8 (scrotal), 18.0 grams, captured within a 48 James T. Wallace 3’ stand of annuals growing in boggy soil near the outlet from a 4-H camp lake. A dead tree with numerous cavities was located about 18’ from the trap site. MADISON COUNTY, Kentucky, 1.2 mi. S. Bighill (town) on U.S. route 421, 18 July, 1961, elevation 900’, adult female, numerous empty nests located in honeysuckle and green-brier; 19 November, 1966, old and newly constructed nests, 3 females were snap-trapped, (184-86- 19.5-20, 170-74-18-18, 185-86-18.5-19), two others disturbed from nest in greenbrier (Smilax); 20 November, 1966, one male captured as it leaped from its nest in the greenbrier; 25 November, 1966, 3 females, 6 males, captured in live traps during one night. GROWTH RATES The geometric growth rates of a selected number of variables were determined in order that an approximation could be made of the stages of development represented by specimens captured in the field. Table 1 contains the means (x) of the weights, length of hind foot, tail, ear, whiskers, and total length of young O. nuttalli over various continuous intervals of time. The natural logs of the measures were used in the calculation of the geometric growth rates over each time period via the formula _ log. Yi - log, Yo K 2 t, - ty The values of Kg (Table 2) demonstrate the sharp increase in the geometrical growth rate of the variables during the first few days of post- natal development followed by a generally gradual decrease in rate as the mice continue development. Neither the arithmetic, natural log nor geometric rate of growth adequately explains the nature of the growth pattern by itself; however, if the Kg values for each time period are in- spected in Table 2 it will be noted that the growth rate is not truly ex- ponential. The geometric growth rates for all variables decrease gradually from about the sixth day post-natal to adulthood. Plots of these rates appear in Figures 1 and 2. Body weight did not attain adult values until some time later than did the other variable considered. Therefore, it is specifically clear that whisker, ear, tail, hind foot and total length dimen- sions rapidly approach maximum (i.e. adult) expected size whereas the weight factor continues at a more gradual but decreasing rate toward adult values. Literature Cited Barbour, R. W. 1942. Nests and habitat of the golden mouse in eastern Kentucky. Jour. Mamm. 23:90-91. Barbour, R. W. 1951. The Mammals of Big Black Mountain, Harlan County, Kentucky Jour. Mamm. 32:100-110. Growth, Development & Distribution of Ochrotomys Nuttalli 49 TABLE 1. Body weights (gms.) and measures (mm.) relative to time in days. (*) Values based on a single individual from a litter of three, while the others are the means (x) of three values. tS ea Ww WwW WW 18 TOTAL LENGTH 68.0* TH 84.6 105.6 118.0 126.3 127.6 129.0 135.0 14h .0 TATL LENGHT 19.0* 25.0 30.6 43.6 51.0 57-3 58.0 60.6 62.3 65.6 HIND FOOT LENGTH 7.0* 11.6 13.2 16.3 LSS 19.0 19.0 19.3 19.3 19.3 EAR WHISKER LENGTH LENGTH 45% 4 0% Bod) 8.3 6.3 9.6 10.0 14.3 12.0 (a3 13.8 21.6 14.6 2h..6 15.5 25.6 16.3 26.6 16.3 28.3 t=t n to 2 WEIGHT (gms. ) 2.56% 3.2h* h 86% 5.91 6.88 8.78 9.59 11.43 12.54 13.64 14.34 19.52 TABLE 2. Kg, geometric growth rates, of selected body dimensions (mm.) and the body weight (gms.) (*) Values based on single individual from a litter of three, while the others are based on the means (x) of three values. paeren 18 TOTAL LENGTH .06215 -04706 .05543 03701 -01699 .00341 00364 .01515 .00358 TAIL LENGTH - 13722 . 10106 -08851 05225 02912 - oooh -OL46L 00922 00286 HIND FOOT LENGTH 225255 .06460 05274 .02367 -02056 .00000 .00522 .00000 - 00000 EAR LENGTH .10033 .06790 Sali za .06077 -03494. .01878 .01994 .O1677 - 00000 WHISKER LENGTH 36498 -O7275 .09962 06348 .05549 04335 01328 -01277 00344 WEIGHT (gms .) .11778* -20278* .09780 -07598 .06096 02941 04328 .03168 02715 .01672 01722 50 James T. Wallace 2 a git 003.004915 7 © TOTAL LENGTH ost b 6 9 98 x) it sere 003 (o) 904015,202, : © TAIL or (a) 9 er oO Le) ° ) ro 3° 2 Le) ¥ 05 000 000 HIND FOOT 2 1°} 24 92' ou o 9° i) a 8g [o} o\t o 1 9 19\"5 % > 6 BODY WEIGHT Oo 5 10 15 20 25 30 35 40 45 50 AGE IN DAYS Figure 1. Log values of linear dimensions (mm.) and weights (gms.) as related to age in days. Kg values are indicated between each pair of points. Blus, L. J. 1966. Relationship between litter, size and latitude in the golden mouse. Jour. Mamm. 47:546-547. Brown, L. N. 1963. Notes on the distribution of Peromyscus nuttalli flammeus and Peromyscus maniculatus ozarkiarum. Jour. Mamm. 44: 424-425, Dunaway, P. B. 1955. Late fall home ranges of three golden mice, Peromy- scus nuttalli. Jour. Mamm. 36:297-298. Goodpaster, W. W. and D. F. Hoffmeister. 1954. Life History of the golden mouse, Peromyscus nuttalli in Kentucky. Jour. Mamm. 35:16-27. Gough, B. J. and S. S. Kilgore. 1964. A comparative hematological study of Peromyscus in Louisiana and Colorado. Jour. Mamm. 45:421-428. Growth, Development & Distribution of Ochrotomys Nuttalli 51 Hirth, H. F. 1960. The spermatozoa of some North American bats and rodents. Jour. Morph. 106:77-83. Layne, J. N. 1958. Records of fleas (Siphonaptera) from Illinois mammals. Nat. Hist. Misc. No. 162 (1-7). McCarley, H. 1958. Ecology, behavior and population dynamics of Peromy- scus nuttalli in eastern Texas. Texas Jour. Sci., 10:147-171. McCarley, H. 1959. The effect of flooding on a marked population of Peromyscus. Jour. Mamm. 40:57-63. WHISKERS ao bh ANANDwO .003 where ° EAR LENGTH Oo 5S 10 '% 20 25 30 35 40 45 50 AGE IN DAYS Figure 2. Log values of linear dimensions (mm.) as related to age in days. Kg values are indicated between each pair of points. 52 James T. Wallace Osgood, W. H. 1909. Review of the mice of the American genus Peromyscus. North Amer. Fauna No. 28. Washington. 285 pp. Packard, R. L. and H. Garner. 1964. Arboreal nests of the golden mouse in eastern Texas. Jour. Mamm. 45:369-374. Sealander, J. A. and D. James. 1958. Relative efficiency of different small mammal traps. Jour. Mamm. 39:215-223. Welter, W. A. and D. E. Sollberger. 1939. Notes on the mammals of Rowan and adjacent counties in eastern Kentucky. Jour. Mamm. 20:77-81. ACKNOWLEDGEMENTS: The author wishes to thank Dr. Roger W. Barbour, Department of Zoology, University of Kentucky, for supplying information helpful in the completion of this paper. Accepted July 10, 1969. ry ivgn we iy Ri rT] an Ly | ip A Sea aih ei INSTRUCTIONS FOR CONTRIBUTORS The TRANSACTIONS OF THE KENTUCKY ACADEMY OF SCIENCE is a medium of publication for original investigations in science. Also as the official organ of the Kentucky Academy of Science, news and announcements of interest to the member- ship are published therein. These include programs of meetings, titles, abstracts of papers presented at meetings, and condensations of reports by the Academy’s officers and committees, Papers may be submitted at any time to the editor. Each manuscript will be reviewed by one or more editors before it is accepted for publication, and an at- tempt will be made to publish papers in the order of their acceptance. 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Galley proofs must be returned promptly. Blanks for reprint orders will be supplied with the galley proof. Yol. 30, No. 34 K3K37 1969 Coden: TKASAT TRANSACTIONS of the KENTUCKY CADEMY of SCIENCE Official] Organ Kenrucky ACADEMY OF SCIENCE ¥ CONTENTS The Fishes of West Kentucky. I. Fishes of Clark’s River MORGAN E. SISK The Fishes of West Kentucky II. The Fishes of Obion Creek. PAUL L. SMITH AND MORGAN E. SISK An Anotated List of Known Species of Fresh-Water Ostracoda of Western Kentucky. MARGARET EVELYN COLE A Record of the Occurrence of the Exotic Land Planarian, Bipalium Kewense, in Calloway County, Kentucky. MARGARET EVELYN COLE Parospirifer Acuminatus From the Brevispirifer Gregarius Zone at the Falls of the Ohio. JAMES E. CONKIN AND BARBARA M. CONKIN yn ACADEMY AFFAIRS ............... wien ~s o) Index to Volume 30 SB RARIES The Kentucky Academy of Science Founded May 8, 1914 OFFICERS 1968-69 President: Orville Richardson, Kentucky Wesleyan College President-Elect: Lloyd Alexander, Kentucky State College Vice-President: Karl Hussung, Murray State University Secretary: Robert S. Larance, Eastern Kentucky University Treasurer: C. B. Hamann, Asbury College Representative to A.A.A.S. Council: Mary Wharton, Georgetown College © OFFICERS 1969-70 President: Lloyd Alexander, Kentucky State College President-Elect: Karl Hussung, Murray State University Vice-President: Marvin Russell, Western Kentucky University Secretary: Robert S. Larance, Eastern Kentucky University Treasurer: C. B. Hamann, Asbury College Representative to A.A.A.S. Council: Mary Wharton, Georgetown College BOARD OF DIRECTORS Lloyd E. Alexander ...........000: to 1969 William M. Clay. ......ccccosessses to 1971 Margaret B. Heaslip ............... to 1969 Gordon Wilson: :..:.ceee to 1972 Roarl Eirias csiecesnstessecnaes to 1970 L.A. Krumbholz:...tecsueees to 1972 Grace Quinte c.isisstdascatecccrasssssns to 1970 Sanford L. Jones: {.cceseres to 1973 John M. Carpenter ............000 to 1971 Ellis V. Brown. ...:..-s.vsseesers to 1978 EDITORIAL OFFICE William F. Wagner Editor Department of Chemistry University of Kentucky Lexington, Kentucky, 40506 Associate Editors: Botany and Microbiology: L. A. Krumholz, University of Louisville Chemistry: Marshall Gordon, Murray State University Geology: William Dennen, University of Kentucky Zoology: Robert Kuehne, University of Kentucky Membership in the Kentucky Academy of Science is open to interested persons upon nomi- nation, payments of dues, and election. Application forms for membership may be obtained from the Secretary. THE TRANSACTIONS are sent free to all members in good standing. Subscription rates for non-members are: domestic, $4.00 per volume; foreign, $4.00 per volume. The TRANSACTIONS are issued semi-annually. Four numbers comprise a volume. Correspondence concerning memberships or subscriptions should be addressed to the Secretary. Exchanges and correspondence relating to exchanges should be addressed to the Librarian, University of Louisville, who is the exchange agent for the Academy. Manuscripts and other material for publication should be addressed to the Editor. EDITORIAL On November 3-5, 1969, your editor had the privilege of attending a workshop for editors of academy journals at Battelle Institute, which was sponsored by the Ohio Academy of Science and supported by the National Science Foundation. It was perhaps comforting to learn that most of the editors are plagued with essentially the same problems that we have, but at the same time disturbing that we do have the problems. The main concerns expressed at the workshop were: the rising costs of publications, accompanied by insufficient income to support publication at the desired rate, and the ability of the journals to attract a sufficient number of high quality manuscripts. The workshop brought into focus several questions which have occurred to me during my initial year as editor. Many of these questions will need considerable discussion by the members of the Academy and hard work on the part of many to achieve the goals after the questions are answered. What should be the goals of the Transactions of the Kentucky Academy of Science? Briefly, should they be to publish sound material, quickly, at a reasonable price, and make it widely available, at least through secondary sources? Our journal is abstracted by Chemical Abstracts and Biological Abstracts and starting with Volume 31, will be indexed in Science Citation Index. We do have wide circulation through these media. Considering finances: The Transactions should be a budgeted item in the Academy and should have a more substantial and consistent source of income. Can this best be accomplished by increasing our membership, selling more subscriptions (to whom?), more institutional support (schools and industries), selling advertising space (low yield for the effort), raising dues, increasing subscription rate, initiating page charges to authors who have financial support for publication, and using cheaper methods of print- ing (e.g. offset from authors’ manuscripts)? Concerning editorial policy: Should the editors personally solicit good papers? Should publication be limited to members? Should subject matter of manuscripts have special or limited relation to Kentucky or members of the Academy? Should we encourage some controversial articles, include a section for member viewpoints, or a regular editorial page (including guest editorials)? Does our journal’s title accurately reflect its contents—should it be renamed (as many Academies have done)? Is the format too stodgy and unappealing? If it were changed, would it attract a wider circulation? During the coming months, these questions and others need to be answered. Your editors and officers of the Academy welcome your com- ments and suggestions. Will you help increase the significance of our efforts? Write to us—we might publish it as an editorial! William F. Wagner THE FISHES OF WEST KENTUCKY. I. FISHES OF CLARK’S RIVER* MORGAN E. SISK Department of Biological Science Murray State University, Murray, Kentucky 42071 Introduction The piscine fauna of West Kentucky has never been adequately sampled; few literature references to fishes from this part of Kentucky have come to my attention. Woolman (1892) made four collections from the area and these were later included in Evermann’s catalogue (1918). Sporadic records appear in recent works (Gibbs, 1961; Collette, 1962; et. al.) but these represent specimens collected or examined for taxonomic revisions and not comprehensive studies of this area. This paper represents the first portion of a faunal survey encompassing the inland streams, lakes and springs of the eight western counties. The study will culminate in a species list, distribution records and keys to the species of Western Kentucky fishies. Rapid changes in topography are occurring throughout West Kentucky that will probably result in alteration of the present biota. Species com- position of streams change with habitat changes. The present trend of flood control measures, agriculture practices and non-agrarian land use are contributing to these changes. It is therefore desirable to have available a complete record of existing species in West Kentucky as reference material for future studies concerned with the effects of habitat changes on the fauna. Description of Clark’s River The Clark’s River System drains about 550 square miles of the Jackson Purchase region in West Kentucky and Tennessee. The river consists of two major branches, the Middle and West Forks, both arising from springs and intermittent streams. The Middle Fork lies to the east of a third and minor fork, East Fork, a victim of misnomer as yet uncorrected. Middle Fork arises in the northern part of Henry County, Tennessee and drains 45.5 square miles of the county before flowing in a northerly direction for 55 miles through Calloway, Marshall and McCracken counties in Kentucky. West Fork arises near Lynn Grove, Calloway County and flows northward for 31 miles through Marshall, Graves and McCracken counties to its juncture with Middle Fork at Oaks in McCracken County. From Oaks the stream continues in a northerly direction to its confluence with the Tennessee River near Paducah (Anonymous, 1959 and 1960). The drainage lies in a physiographic region known as the Mississippi Embayment (Braun, 1943). It is typical coastal plain with clays, sands and gravels of Tertiary and Cretaceous origin (McFarlan, 1958). Topo- * Research support by grants from the Murray State University Foundation and the Society of the Sigma Xi. The Fishes of West Kentucky—I 55 graphically the area is a low, undulating plain and ranges in elevation from 300 to 640 feet above sea level (Anonymous, 1959 and 1960). Vegetation consists of broadleaf deciduous trees, primarily oak-ash-maple and oak- hickory associations, lichens and herbaceous plants other than grasses (Espenshade, 1964). The entire area slopes toward the north. Over much of its course, Clark’s River is sluggish with steep, muddy banks. The stream bed in Kentucky is 20-150 feet wide and is composed of soft mud, sand, gravel and rocks. The water is clear in the upper reaches but tends to darken in the lower extremities due to an increased content of organic matter. Average stream gradients are as follows: Middle Fork, 55 miles at 3.9 feet per mile; East Fork, 9 miles at 8.3 feet per mile; West Fork, 31 miles at 4.1 feet per mile (Manthey, 1965; personal communication). Description of Stations This paper includes only collections from the Kentucky portion of Clark’s River. A total of 24 collections from 23 stations were made. Stations are listed with data by collection number assigned by the collector. 1. Calloway County, Middle Fork 6 miles south of Murray and 0.5 miles east of Highway 641, near Tobacco. 6 May 1965. 2. Calloway County, Farley Branch of Middle Fork, 2 miles south of Murray on Highway 641. 8 May 1965. 3. Calloway County, Middle Fork 1.5 miles east of Dexter. 10 May 1965. 4. Calloway County, Middle Fork 4 miles north and 2 miles east of Murray. 10 May 1965. 5. Calloway County, Middle Fork .5 miles east of Murray on Highway 94. 10 May 1965. 6. Calloway County, West Fork, .75 miles west and 1.5 miles south of Stella. 16 May 1965. 7. Calloway County, West Fork, .75 miles west and 2.5 miles north of Stella. 16 May 1965. 8. Calloway County, Spring fed slough near West Fork, .75 miles west and 4 miles north of Stella. 16 May 1965. 9. Calloway County, West Fork .25 miles west of Backusburg on Highway 464. 16 May 1965. 10. Calloway County, East Fork at Martins Chapel 6 miles southwest of Murray. 18 May 1965. 11. Marshall County, Middle Fork 1.8 miles east of Hardin on Highway 80. 14 July 1965. 12. Marshall County, Middle Fork 7.0 miles east of Benton on Highway 408. 14 July 1965. 13. Marshall County, Middle Fork .5 miles north of Benton on Highway 641. 14 July 1965. 14. McCracken County, Clark’s River at its mouth near Paducah. 14 July 1965. 15. Marshall County, Wades Creek .5 miles south of Hardin on Highway 641. 14 July 1965. 16. Marshall County, West Fork 1.5 miles west of Brewers on Highway 58 and 80. 11 August 1965. 56 Morgan E. Sisk 17. Graves County, West Fork .5 miles west of Kaler. 11 August 1965. 18. Marshall County, Hales Spring 1.0 miles west of Brewers on Highway 58 and 80. 12 August 1965. 19. Calloway County, Rockhouse Creek 1.5 miles north of Almo Heights on Highway 641. 12 August 1965. 20. Calloway County, Middle Fork 1.0 miles east of Almo Heights. 13 August 1965. 21. Calloway County, Whiteoak Creek, 6 miles south of Murray and .8 miles east of Toabacco. 22 July 1965. 22. Same station as number 14. 30 October 1965. 23. Marshall County, Middle Fork 3 miles southeast of Draffenville near Scale crossing. 3 November 1965. 24. Calloway County, Middle Fork .5 miles southeast of Murray at R.R. bridge near Highway 121. 5 November 1965. List of Species In the following list, the scientific name is followed by the common name, station numbers and pertinent notes. All specimens are at present in the Murray State University Collection of Fishes. The nomenclature and arrangement of taxa is that of Moore (1957). Polyodontidae 1. Polyodon spathula (Walbaum). Paddlefish. Station 14. Sight record. Lepisosteidae bo Lepisosteus osseus (Linnaeus). Longnose gar. Station 24. Natives report this as a common species. Six caught in gill nets at this station. 3. L. platostomus Rafinesque. Shortnose gar. Station 14. Sight record. Amiidae 4. Amia calva Linnaeus. Bowfin. Station 17. Sight record. Apparently rare in stream. Clupeidae 5. Dorosoma cepedianum (Le Sueur). Gizzard shad. Stations 22 and 24. 6. Signalosa petenensis (Gimther). Threadfin shad. Station 22. Esocidae 7. Esox americanus Gmelin. Grass pickerel. Stations 3, 11, 12, 19 and 20. Common in the Middle Fork. 8. E. niger Le Sueur. Chain pickerel. Station 24. Catostomidae 9. Ictiobus cyprinellus (Valenciennes). Bigmouth Buffalo. Station 14. Sight record. 10. Carpiodes carpio (Rafinesque). River carpsucker. Station 22-24. 11. Moxostoma aureolum (Le Sueur). Shorthead redhorse. Station 1. One specimen. 12. M. erythrurum (Rafinesque). Golden redhorse. Stations 9, 23 and 24. 13. 14, 15. 16. is 18. 19. 20. 21. 22. 23. 24, 25. 26. 27. 28. 29. 30. 31. 32. 33. 34, 30. 36. 37. 38. 39. The Fishes of West Kentucky—I 57 Minytrema malanops (Rafinesque). Spotted sucker. Stations 5, 22-24. Erimyzon oblongus (Mitchill). Creek chubsucker. Stations 3-5, 7, 10, 16, 18, and 20. pean nigricans (Le Sueur). Northern hogsucker. Stations 2, 7, 9 and 11. Cyprinidae Cyprinus carpio Linnaeus. Carp. Stations 5, 22 and 23. Much more common than records indicate. Carassius auratus (Linnaeus). Goldfish. Station 5. Notemigonus crysoleucas (Mitchill). Golden shiner. Stations 4, 4, 10, 13, 17, and 20. Semotilus atromaculatus (Mitchill). Creek chub. Stations 2, 5-7, 9, 10, 15, 16, 18, 20, and 21. Very common in the upper reaches of both forks. Opsopoeodus emiliae Hay. Pugnose minnow. Stations 1, 3, and 10. Notropis boops Gilbert. Bigeye shiner. Stations 1, 10, 16, 19, and 21. N. umbratilis (Girard). Redfin shiner. Stations 1, 5, 8-10, 19, 21. This species and the next one are common throughout the drainage. N. atherinoides Rafinesque. Emerald shiner. Stations 3, 10-12, 14, 16, 17, and 19. N. blennius (Girard). River shiner. Station 12. One specimen. N. volucellus (Cope). Mimic shiner. Station 17. One specimen. N. spilopterus (Cope). Spotfin shiner. Station 16. One specimen. Pimephales notatus (Rafinesque). Bluntmose minnow. Stations 1-3, 5-7, 9-11, 16, and 20. Campostoma anomalum (Rafinesque). Stoneroller. Stations 1-3, 6, 7, 9, Miele 6 and 2: Ictaluridae Ictalurus punctatus (Rafinesque). Channel catfish. Station 22. I. furcatus (Le Sueur). Blue catfish. Station 14. Sight record. I. natalis (Le Sueur). Yellow bullhead. Stations 5, 20, 21. I. melas (Rafinesque). Black bullhead. Station 14. Sight record. Pylodictis olivaris (Rafinesque). Flathead catfish. Station 22. Sight record. Anguillidae Anguilla rostrata (Le Sueur). American eel. Station 22. Cyprinodontidae Fundulus notatus (Rafinesque). Blackstrip topminnow. Station 16. F. olivaceus (Storer). Blackspotted topminnow. Stations 1-3, 5-7, 11, 13, 16, 17, 19-21. Poeciliidae Gambusia affinis (Baird and Girard). Mosquitofish. Stations 8 and 13. Much more abundant than collections indicate. Aphredoderidae Aphredoderus sayanus (Gilliams). Pirate perch. Stations 17, 19-21. Atherinidae Labidesthes sicculus (Cope). Brook silverside. Station 14. 58 Morgan E. Sisk Serranidae 40. Roccus chrysops (Rafinesque). White bass. Stations 17 and 22. Centrarchidae 41. Micropterus punctulatus (Rafinesque). Spotted bass. Stations 1, 2, 4, 9, 1a eta arand ob: 42. M. salmoides (Lacepede). Largemouth bass. Stations 1, 2, 4, 5, 9, 11, 14, and 19. 43. Chaenobryttus gulosus (Cuvier). Warmouth. Station 5. One specimen. 44. Lepomis cyanellus Rafinesque. Green sunfish. Stations 4-7, 10, 12, 16, 17, 20, and 21. 45. L. megalotis (Rafinesque). Longear sunfish. Stations 1, 2, 5, 6, 9-14, 16-19. 46. L. macrochirus Rafinesque. Bluegill. Stations 1, 5, 10, 13, 14, 17, 20, 21, and 24. 47. L. humilis (Girard). Orangespotted sunfish. Stations 3-5, 11-13, 19 and 20. 48. Pomoxis nigromaculatus Le Sueur. Black crappie. Station 18. One specimen. 49. P. annularis Rafinesque. White crappie. Stations 9, 13, and 24. 50. Elassoma zonatum Jordan. Banded pygmy sunfish. Station 17. Percidae 51. Stizostedion canadense (Smith). Sauger. Station 22. Sixteen individuals netted; one kept for record, remainder released. 52. Percina maculata (Girard). Blackside darter. Stations 1, 9, 16, and 19. 53. P. caprodes (Rafinesque). Logperch. Station 7. Ten collected, one kept for reccrd. 54. Etheostoma nigrum Rafinesque. Johnny darter. Stations 1 and 7. This is the subspecies nigrum. 55. E. chlorosomum (Hay). Bluntnose darter. Stations 10 and 20. 56. E. sp. Unnamed species, close to E. simoterum (Cope). Stations 1, 2, 6, 7, 9, 16, 18, 19, and 21. 57. E. rufilineatum (Cope). Redlined darter. Stations 9 and 16. 58. E. gracile (Girard). Slough darter. Staticns 1-3, 7, 8, 16, 18, 19-21. 59. E. squamiceps Jordan. Spottail darter. Stations 2, 3, 4, 5, 11, 12. 60. E. flabellare Rafinesque. Fantail darter. Stations 7, 19, 16, 18, and 21. Sciaenidae 61. Aplodinotus grunniens Rafinesque. Fresh-water drum. Station 14. Sight record. LITERATURE CITED Anonymous. 1959. Workplan for watershed protection and flood prevention. West Fork of Clark’s River watershed. S.C.S., U.S. Dept. Agr. State Office, Lexington, Kentucky. --—-——— . 1960. Workplan for watershed protection and flood prevention. Middle Fork of Clark’s River watershed. S.C.S., Dept. Agr. State Office, Lexington, Kentucky. The Fishes of West Kentucky—I 59 Braun, E. Lucy. 1943. An annotated catalog of spermatophytes of Ken- tucky. John S. Swift Co., Cincinnati. 161 pp. Collette, Bruce C. 1962. The swamp darters of the subgenus Hololepis (Pisces: Percidae). Tulane studies in Zool., 9(4): 115-211. Espenshade, E. B., ed. 1964. Goode’s world atlas. Rand McNally, Chicago. Everman, Barton W. 1918. Fishes of Kentucky and Tennessee: a dis- tributional catalogue of the known species. Bull. Bureau Fish., XXXV, no. 858:295-368. Gibbs, R. H. 1961. Cyprinid fishes of the subgenus Cyprinella of Notropis. IV. The Notropis galacturus-camurus complex. Amer. Mid. Nat., 66 (2); 337-354. Manthey, John. 1965. Personal communication. Data supplied by the Tennessee Valley Authority, Paris, Tennessee. McFarlan, A. C. 1958. Behind the scenery in Kentucky. Ky. Geol. Survey Spec. Pub. 10. U. of Ky., Lexington. Moore, George A. 1957. In: Vertebrates of the United States. McGraw- Hill Book Co., N. Y.: 33-210. Woolman, A. J. 1892. Report of an examination of the rivers of Kentucky, with list of fishes obtained. Bull. U. S. Fish. Comm., Vol. 10(1890): 249-292. Accepted August 1, 1969. THE FISHES OF WEST KENTUCKY. Il. THE FISHES OF OBION CREEK* PAUL L. SMITH and MORGAN E. SISK** Department of Biological Sciences, Murray State University, Murray, Kentucky 42071 INTRODUCTION Currently, little information is available in the literature concerning the combined effect of upstream flood control impoundments and stream channel diversion on the species composition of a drainage system. This is a survey to establish the species of fishes present in the Obion Creek drainage system before flood control measures are taken. Obion Creek rises in Graves County near Cuba, Kentucky, and flows some 42 miles in a westerly direction to its confluence with the Mississippi River near Hickman, Kentucky. The major tributaries are Brush, Little Joe, Cane and Bowles creeks. Murphey’s Pond, a ponded, swamped area of several hundred acres, lies in the Obion Creek flood plain, and is located on the north side of Obion Creek, just east of Kentucky Highway No. 307. The Obion Creek watershed comprises an area of 206,108 acres in Graves, Hickman, Carlisle and Fulton counties, Kentucky. It extends in an east-west direction for a distance of approximately 35 miles from the upper extremity to its confluence with the Mississippi River. The average width, measured in a general north-south direction, is ten miles. The area is low, rather undulating plain ranging in elevation from 300-500 feet above sea level, with local relief of less than 50 feet. Physiographically the region is in its youth; the stream dissection having little affected its rather level upland. Geologically, the watershed lies in the Gulf Embayment, a coastal plain region with areas of outcrop of unconsolidated or semil-consolidated clays, sands and gravels, which are of Tertiary age. The entire region, is covered with Pleistocene loess, ranging in depth from a few inches in the upper part of the watershed to several feet along the Mississippi River. Upland soils are deep, moderately well drained to well drained silt loams that are derived from loess, with the principal soil series being Memphis, Loring, Granada and Lexington. Valley soils are well drained to imperfectly drained silt loams that are of mixed origin and loess with Collins, Falaya and Waverly being the principle soil series. In 1957, there were 122,186 acres of cropland; 27,388 acres of pasture; 40,387 acres of woodland; 6,924 acres of idle land; and 7,223 acres in miscellaneous use in the Obion Creek watershed. The above watershed * Research supported by grants from the Murray State University Foundation and the Society of the Sigma Xi. ** To whom correspondence should be addressed. The Fishes of West Kentucky—II 61 description was taken in part from the Obion Creek Watershed Work Plan (Dec., 1957). Obion Creek is a spring fed stream with an average gradient of four feet per mile. It flows over a two to four foot layer of mud, forming an alternating series of deep, sluggish pools and swift, well-defined rif_les. The channel is bordered by deciduous, hardwood forests composed primarily _ of oak-ash-maple and oak-hickory associations. The well-defined channel, which never exceeds fifty feet in width, contains much debris from previous logging operations in the bordering forests. During heavy rains, these logging wastes impede the flow of water causing overflow flooding in the lower portions of the watershed. Waters of the stream carry an extremely heavy silt load due to sheet erosion which occurs throughout the watershed, excepting the floodplain, at an estimated rate of five tons per acre per year (Watershed Work Plan). The U. S. Army Corps of Engineers working in conjunction with the Obion Creek Watershed Conservancy have organized a two-part plan to prevent both the yearly flooding of the watershed and the severe erosive conditions. The Corps of Engineers’ plan includes the diversion of Obion Creek from a point approximately 8.2 miles above its mouth, westerly to the Mississippi River; and realignment and enlargement of the channel beginning at this point and extending possibly as far east as the railroad bridge near Pryorsburg, Kentucky (Watershed Work Plan). The Obion Creek Watershed Conservancy and Corps of Engineers plan to construct fourteen floodwater retarding structures having an aggregate capacity of 1,629 acre feet of sediment storage and 5,444 acre feet of fiood retention storage, controlling runoff from a 42 square mile area of the headwaters of Obion, Little Joe, Thompson Branch, Bowles, Cane, Bryon, Barnes and Little Cypress creeks (Watershed Work Plan). The only published collection of fishes from Obion Creek is that of Woolman (1892) who sampled the creek during the summer of 1890. His species list, included in Evermann’s catalogue (1918), records thirty species taken during two days of collecting. Obion Creek is an Order V stream according to the Horton system of classification, which is based on stream branching (Kuehne, 1962). Accord- ing to this system, extreme hardwater streams are ranked as first order. Union of two such streams forms the second order. When any streams of equal order join, they form a next higher order, but if two streams of unequal order unite, the order is not increased (Kuehne, ibid.). The number of species increased with stream order in Obion Creek as is shown below. Stream Order Number of Species I 5 II 9 III ui IV 26 62 Paul L. Smith and Morgan E. Sisk MATERIALS AND METHODS Gill nets, rotenone and seines were used in making collections. The one-inch mesh gill nets were set in brushy areas of the channel and in sloughs that could not be seined. When used in the creek, the nets were stretched completely across the channel. Large seines were used in sloughs that were free of obstructions. Smaller seins were used to sample the channels of all streams. The most practical seine proved to be a small habitat seine (4’ x 3’) of mosquito-net mesh. Powdered 1% rotenone was used on two occasions in small sloughs that were not connected to flowing water. Specimens were killed and fixed in 10% formalin and preserved in 70% alcohol. Collections are presently in the Murray State University Vertebrate Collections. Collecting stations generally were located near highways or railroads. A total of 39 collections from 25 stations were taken from parts of the entire drainage system. Stations are listed below by collection number. 1. 14:VI:1966; Obion Creek, 3 miles south of Arlington, Kentucky, U. S. 51, Hickman County. 2. 15:VI:1966; Slough near Obion Creek, 4 miles southeast of Columbus, Kentucky, Ky. 58, Hickman County. 3. 15:VI:1966; Obion Creek, 4 miles southeast of Columbus, Kentucky, Ky. 58, Hickman County. 4, 20:VI:1966; Slough near Obion Creek, 4 miles east of Arlington, Kentucky, Carlisle County. 5. 20:6:1966; Spring near Obion Creek, 4 miles east of Arlington, Kentucky, Carlisle County. 6. 20:VI:1966; Obion Creek, 4 miles east of Arlington, Kentucky, Carlisle, County. 7. 28:VI:1966; Obion Creek, 6 miles east of Arlington, Kentucky, Carlisle County. 8. 18:VII:1966; Little Joe Creek, 3 miles south of Kentucky 80 on Kenucky 307, Hickman County. 9. 22:VII:1966; Obion Creek, .5 miles west of U. S. 51 under Illinois Central Railroad trestle, Hickman County. 10. 27:VII:1966; Same station as number 9. 11. 10:VIII:1966; Hollingsworth Creek, 4 miles south of Columbus, Kentucky, Ky. 123, Hickman County. 12. 10:VIII:1966; Obion Creek, .5 miles northwest of Oakton, Kentucky, Ky. 123, Hickman County. 13. 10:VIII:1966; Whayne Branch, 2 miles south of Oakton, Hickman County. 14. 10:VIII:1966; Cane Creek, 3 miles north of Oakton, Hickman County. 15. 10:VIII:1966; Brush Creek, 5 miles south of Arlington, Kentucky, U. S. 51, Hickman County. 16. 11:VIII:1966;Same station as number 14. 17. 16:VIII:1966; Obion Creek, 4 miles north of Hickman, Kentucky, Fulton County. 18. 16:VIII:1966; Prehistoric canal, 1 mile north of Hickman-Fulton county line, Hickman County. 19. 20. 21. 22. 23. 24. 25. 26. 27. 28. 29. 30. 3l. 32. 33. 34. 35. 36. 37. 38. 39. The Fishes of West Kentucky—II 63 16:VIII:1966; Slough 1 mile south of Obion Creek under Illincis Central Railroad between Arlington and Clinton, Hickman County. 18: VIII:1966; Cane Creek, 4 miles southwest of Pryorsburg, Kentucky, Kentucky 58, Graves County. 18:VIII:1966; Obion Creek, 2 miles northeast of Watts’ Station, Kentucky 339, Graves County. 18:VIII:1966; Brush Creek, 2 miles southwest of Wingo, Kentucky, Kentucky 45, Graves County. 18:VIII:1966; Obion Creek, Pryorsburg, Kentucky, Kentucky 45, Graves County. 23:1X:1967; Same station as number 12. 23:IX:1967; Obion Creek, 2 miles north of confluence with Bayou De Chein Creek, Fulton County. 23:IX:1967; Same station as number 18. 23:1X:1967; Same station as number 12. 6: VIII: 1967; Same station as number 1. 9:X:1967; Same station as number 15. 30:11I:1968; Hurricane Creek, 1 mile south of Arlington, Kentucky, near the Illinois Central Railroad, Carlisle County. 30:III:1968; Same station as number 9. 17:IV: 1967; Same station as number 15. 17:VIII:1966; Murphey’s Pond, 1 mile south of Beulah, Kentucky, Hickman County. 30:III:1968; Bowles Creek, .5 miles east of G.M. & O. Railroad on Kentucky 80, Hickman County. 30:III:1968; Unnamed intermittent creek .25 miles south of Zion Church, Kentucky 123, Hickman County. 30:III:1968; Same station as number 11. 15:IV:1967; Hopewell Creek, 3 miles east of Arlington, Kentucky, on Ken- tucky 80, Carlisle County. 15:IV:1967; Guess Creek, 5 miles east of Arlington, Kentucky, Kentucky 80, Carlisle County. 16:IV:1967; Same station as number 1. RESULTS This survey resulted in the following list of 17 families represented by 57 species. The scientific name is followed by the common name and collection locales. The nomenclature and arrangement of taxa is that of Moore (1968). LIST OF SPECIES Amiidae Amia calva Linnaeus. Bowfin. Stations 19, 33, and 89. Common in the sloughs near Obion Creek but rare in the streams. Lepisosteidae Lepisosteus platostcmus Rafinesque. Shortnose gar. Stations 17, 19 and 28. Common in both streams and sloughs. 64 1 12. Paul L. Smith and Morgan E. Sisk Clupeidae Dorosoma cepedianum (LeSueur). Gizzard shad. Stations 1, 2, 6, 7, 9, 17, 21, 23, 25 and 33. Common throughout the system. Esocidae Esox americanus Gmelin. Grass pickerel. Stations 1, 2, 4, 5, 7, 15, 19, 24, 31 and 33. Common throughout the system. Hiodontidae Hiodon alosoides (Rafinesque). Goldeye. Station 7. One specimen collected in deep, swift water of Obion Creek. Catostomidae Ictiobus cyprinellus (Valenciennes). Bigmouth buffalo. Stations 14, 19 and 33. Common in large sloughs and in deep waters of streams. Ictiobus bubalus (Rafinesque). Smallmouth buffalo. Sight record. Com- mercial fishermen take this species from the backwaters of Obion Creek. They may move upstream during periods of flooding. Carpiodes carpio (Rafinesque). River carpsucker. Station 39. One specimen, apparently rare in the system. Moxostoma erythrurum (Rafinesque). Golden redhorse. Station 7. Six immature specimens collected, uncommon in system. . Moxostoma aureolum (LeSueur). Shorthead redhorse. Station 39. One specimen collected. Erimyzon oblongus (Mitchill). Creek chubsucker. Stations 1, 6, 12, 15, 22, 23 and 30. Common throughout system. Minytrema melanops (Rafinesque). Spotted sucker. Station 33. Three very large specimens were taken from Murphey’s Pond. Apparently absent from the streams in the drainage. Cyprinidae Cyprinus carpio Linnaeus. Carp. Stations 1, 4, 9, 18, 19, 22, 24, 26 and 39. Common except in intermittant creeks. Notemigonus crysoleucas (Mitchill). Golden shiner. Stations 1, 2, 4, 7, 11, 21, 24, 26, 30 and 34. Common throughout drainage but not in large numbers. Semotilus atromaculatus (Mitchill). Creek chub. Stations 15, 22, 23, 30, 32 and 38. Common in small streams but rare in sloughs and large streams. . Opsopoeodus emiliae Hay. Pugnose minnow. Station 1. Five specimens taken from a slough. . Phenacobius mirabilis (Girard). Suckermouth minnow. Stations 7 and 22. Not common, collected in streams only. . Notropis umbratilis (Girard). Redfin shiner. Several specimens taken by junior author and class near Station 23 on 10:V1968. Notropis atherinoides Rafinesque. Emerald shiner. Stations 1, 5, 6, 9, 12, 19, 21, 27 and 28. Common in large streams. . Notropis rubellus (Agassiz). Rosyface shiner. Stations 9 and 23. One specimen from each station. 21. 22. 23. 24, 25. 26. 27. 28. 29. 30. 3l. 32. 33. 34. 35. 36. 37. 38. The Fishes of West Kentucky—II 65 Notropis whipplei (Girard). Steelcolor shiner. Stations 6 and 7. Collected from large streams only. Notropis lutrensis (Baird and Girard). Red shiner. Stations 6 and 9. From swift water only. Notropis volucellus (Cope). Mimic shiner. Stations 7 and 23. Streams only. Hybognathus nuchalis Agassiz. Silvery minnow. Stations 6, 7, 8, 9, 12, 14, 15, 18, 26 and 27. Common in streams throughout the system. Hybognathus hayi Jordan. Cypress minnow. Stations 1, 18 and 29. Occurs beth in streams and sloughs but is not as common as H. nuchalis. Pimephales promelas Rafinesque. Fathead minnow. Station 11. Uncommon. Ictaluridae Ictalurus punctatus (Rafinesque). Channel catfish. Station 9. This species is common in Obion Creek; the most important food and game fish in the drainage system. Ictalurus natalis (LeSueur). Yellow bullhead. Stations 18, 22, 23, 24, 25, 26, 32 and 33. Common in streams and sloughs. Ictalurus melas (Rafinesque). Black bullhead. Stations 1, 5, 6, 11, 22, 24 and 33. Common. Pylodictis olivaris (Rafinesque). Flathead catfish. Sight record. This species occurs in deep pools in Obion Creek and is taken occasionally by local fishermen. Noturus gyrinus (Mitchill). Tadpole madtom. Stations 6, 7, 9, 12, 24 and 27. Occur in the larger streams and sloughs. Noturus miurus (Jordan). Brindled madtom. Stations 6 and 7. Collected from shallow, swift water of Obion Creek. Anguillidae Anguilla rostrata (LeSueur). American eel. Sight record. Often taken by sport fishermen according to natives. Cyprinodontidae Fundulus notatus (Rafinesque). Blackstripe topminnow. Stations 2, 8 and 24. Not common in any area of the drainage system. Fundulus olivaceous (Storer). Blackspotted topminnow. Stations 1, 2, 6, 7, 12, 15, 17, 18, 19, 22, 23, 24, 26, 29, 30, 32, 33 and 37. Common in all streams and sloughs. Poeciliidae Gambusia affinis (Gaird and Girard). Mosquitofish. Stations 1, 2, 4, 6, 7, 8, 11, 13, 17, 18, 22, 23, 24, 26, 30, 31, 32, and 33. Common throughout drainage. Aphredoderidae Aphredoderus sayanus (Gilliams). Pirate perch. Stations 1, 2, 4, 5, 9, 12, 18, 24, 26, 29, 32 and 33. Common. Serranidae Roccus chrysops (Rafinesque). White bass. Station 39. White bass seem to migrate up Obion Creek from the Mississippi River each spring. 66 39. 40. Al. 42. 43. 44, 45. 46. 47. 48. 49. 50. dl. 52. 53. 54. 50. 56. 57. Paul L. Smith and Morgan E. Sisk Centrarchidae Micropterus salmoides (Lacepede). Largemouth bass. Stations 1, 7, 9, 17, 21, 24, 33 and 39. Common but individuals do not attain large size. Chaenobryttus gulosus (Cuvier). Warmouth. Stations 1, 2, 18, 19, 21, 24, 31 and 33. Common in sloughs. Lepomis cyanellus Rafinesque. Green sunfish. Stations 1, 7, 8, 11, 12, 13, 15, 18, 20, 22, 23, 24, 29, 30, 32, 34, 35, 36 and 37. Occurs abundantly in streams and sloughs; the most wide spread species of the drainage system. Lepomis symmetricus Forbes. Bantam sunfish. Station 2. One specimen collected from a slough. Lepomis megalotis (Rafinesque). Longear sunfish. Station 17. One specimen from Obion Creek. Lepomis humilis (Girard). Orangespotted sunfish. Stations 1, 2, 7, 17, 24 and 33. Common in both streams and sloughs. Lepomis macrochirus Rafinesque. Bluegill sunfish. Stations 1, 7, 8, 15, 17, 19, 22, 23, 24, 33 and 37. Common throughout the drainage. Pomoxis nigromaculatus LeSueur. Black crappie. Stations 1 and 39. Not as common as white crappie. Pom xis annularis Rafinesque. White crappie. Stations 1, 2, 6, 7, 18, 21, 24, 25 and 33. Very common. Centrarchus macropterus (Lacepede). Flier. Stations 1, 2, 4, 21, 24, 25, 26 and 27. Very common. Elassomatidae Elassoma zonatum Jordan. Banded pygmy sunfish. Stations 12, 18, 31 and 33. Common in sluggish waters. Percidae Percina cymatotaenia (Gilbert and Meek). Bluestripe darter. Stations 7 and 9. Collected in riffles two to three feet deep. Percina maculata (Girard). Blackside darter. Stations 6 and 12. Collected in deep diffles of Obion Creek. Percina uranidea (Jordan and Gilbert). Stargazing darter. Stations 7 and 9. Collected in riffles of Obion Creek. Etheostoma chlorosomum (Hay). Bluntnose darter. Stations 12, 17, 19, 24 and 25. Collected in sluggish areas of Obion Creek. Etheostoma histrio Jordan and Gilbert. Harlequin darter. Station 12. Three specimens were collectd from a turbid riffle over a scft mud bottom. The stream at the collecting site is about 35 feet wide and passes through an oak-hickory hardwood forest. The habitat and discontinuous distribution of this species has been discussed by Tsai (1968). Etheostoma asprigene (Forbes). Mud darter. Stations 12, 18, 24, 25, 26 and 27. Common in the larger streams. Etheostoma gracile (Girard). Slough darter. Stations 1, 4, 6, 7, 9, 12, 13, 17, 18, 19, 22, 24, 26, 31, 32, 33 and 34. The most common darter in both streams and sloughs. Sciaenidae Aplodinotus grunniens Rafinesque. Freshwater drum. Stations 10 and 26. Fishermen take this species with hock and line occasionally. Apparently common in Obion Creek but difficult to collect. The Fishes of West Kentucky—Il 67 CONCLUSIONS Habitats of Obion Creek have undergone changes in the past eighty years and so has the composition of its fishes. When the drainage system was sampled by Woolman in 1890, the major portion of the watershed was covered by hardwood forests and the waters were clear. Subsequent to the conversion of forests to farmland, the silt load in the stream began to increase. Percina caprodes, Labidesthes sicculus and Micropterus dolomieui were collected by Woolman but were not encountered during this survey. These species are not highly silt tolerant and were presumably eliminated from the drainage system by the increased siltation. One can only speculate to what extent these changes affected the number of species in the system because Woolman’s collections were too incomplete to offer any comparison. The proposed flood and silt control measures will create another drastic alteration of habitats. Some species, such as Etheostoma histrio, E. asprigene, and the percids, which were collected only from channel riffes near the mouth, may be eliminated from the drainage system. The diversion ditch above the mouth of the stream will destroy that area of Obion Creek where these fishes have been collected. The habitats of the ditch will differ from this area of the stream, which presently is bordered by forests, since it will then bisect existing croplands. Riffles will thus be eliminated with the leveling of the bed of the ditch. It is doubtful that E. histrio and E. asprigene will find suitable habitats under these condi- tions. However, most of the species in the system are not restricted to this particular type of habitat and may not be drastically affected. There- fore, the number of species totally eliminated from the drainage will possibly remain small. A study by Cross (1950) in Oklahoma indicates that the number of piscine species may increase following flood control measures. The same condition may obtain where Obion Creek is concerned. Much of the silt will be removed from the water by the sediment retention structures, al- lowing species with a lower silt tolerance to occupy the streams, whereas few, if any, species will be adversely affected by the silt removal. Possibly some of the fishes that were eliminated by siltation will be able to re-invade from the Mississippi River. There is little reason to doubt that the piscine fauna of Obion Creek will be altered following man-made changes in the stream system, but the extent of these changes can only be determined by future collections of fishes. Therefore, a continual survey must be maintained after com- pletion of the watershed project to record these changes. LITERATURE CITED Cross, Frank B. 1950. Effects of sewage and a headwaters impoundment on the fishes of Stillwater Creek in Payne County, Oklahoma. Amer. Mid. Nat., vol. 43:128-145. 68 Paul L. Smith and Morgan E. Sisk Everman, Barton W. 1918. The fishes of Kentucky and Tennessee: A distributional catalogue of the Bureau of Fisheries. Vol. 35:295-368. Kuehne, Robert A. 1963. A classification of streams, illustrated by fish distribution in an Eastern Kentucky creek. Ecol., vol. 43:608-614. Moore, George A. 1968. IN: Vertebrates of the United States. Second edition. McGraw-Hill, Inc., New York, N. Y. Watershed Work Plan for Obion Creek, Dec. 1957. Woolman, Albert J. 1982. Report of the examination of the rivers of Kentucky with lists of the fishes obtained. Bull. U. S. Fish Comm., X, 1890(1892) :249-288. Accepted August 1, 1969. AN ANNOTATED LIST OF KNOWN SPECIES OF FRESH-WATER OSTRACODA OF WESTERN KENTUCKY MARGARET EVELYN COLE Murray State University, Murray, Kentucky 42071 To my knowledge there has been no major taxonomic study of the Ostracoda in Kentucky reported in the literature. Gerald A. Cole sum- marized the knowledge of the group in Kentucky and added records from Jefferson County in 1959. Scattered collections have been taken from eight counties of western Kentucky since 1960 by students of Murray State University and by me, adding new distribution records. A systematic list of ostracod species known to occur in western Kentucky is as follows: Stenocypris major (Baird, 1859) Apstein, 1907 One female was collected from Hematite Lake, Trigg County in July. Cyprinotus incongruens (Ramdohr, 1808) Turner, 1895 One female was taken from Empire Lake, Trigg County in November. Cypricercus reticulatus (Zaddach, 1844) Hoff, 1942 Pepulations of this species were collected from Murphey’s Pond, Hickman County in February, March, and April. Others were taken from a roadside ditch near Dog Creek in Calloway County in March. A few males were present in the Calloway County population, and males of this species are generally rare. Cypridopsis aculeata (Costa, 1847) G. W. Muller, 1900 A number of females of this species were collected from Hematite Lake, Trigg County in February, July, and December. Cypridcpsis helvetica Kaufmann, 1892 This species was taken from a woodland pond at the Conservation Center, Land Between the Lakes, Lyon County and from Empire Lake, Trigg County in November. Cypridopsis obesa G. S. Brady and Robertson, 1869 Three females of this species were collected from Empire Lake, Trigg County in November. Cypridopsis vidua (O. F. Muller, 1776) Brady, 1868 Females of this common species were taken from a tributary of Blood River, from quarry ponds and pasture ponds in Calloway County, from a pasture pond in Henderson County, frcm a sinkhole pond in Marshall County, and from Murphey’s Pond in Hickman County. Potamocypris pallida Alm, 1914 One female was collected from a spring-fed branch in Mammoth Cave National Park, Edmonson County in December. Cyclocypris forbesi Sharpe, 1897 Individuals of this species were taken frem Hematite Lake, Trigg County in February and December and from Murphey’s Pond, Hickman County in February, April, and November. * Supported by Murray State University Institutional Studies and Research Fund. 70 Margaret Evelyn Cole Cypria obesa Sharpe, 1897 Two individuals of this species were collected from Murphey’s Pond, Hickman County in April and one from a sinkhole pond in Marshall County in May. Cypria turneri Hoff, 1942 Representatives of this species were taken from Hematite Lake, Trigg County in December and February; from a sinkhole pond in Marshall County in May; and from Murphey’s Pond, Hickman County in March, April, and November. Physocypria globula Furtos, 1933 In Calloway County, individuals of this species were collected from a pasture pond in October and from a quarry pond in March; in Hematite Lake, Trigg County they were collected in July; in a sinkhole pond of Marshall County they were collected in May; and in Murphey’s Pond, Hickman County they were collected in March, April, and November. Candona crogmaniana Turner, 1894 In November, representatives of this species were collected from the Conservation Center woodland pond, Lyon County; from Empire Lake, Trigg County; and from Murphey’s Pond, Hickman County. Candona elliptica Furtos, 1933 Individuals of this species were found in the Conservation Center woodland pond, Lyon County and Empire Lake, Trigg County in November. Candona simpsoni Sharpe, 1897 A population of this species was located in Murphey’s Pond, Hickman County in April. Candona truncata Furtos, 1933 One female was collected from Hematite Lake, Trigg County in February. The sixteen species reported here are members of the family Cypridae. Systematic collecting in all types of aquatic habitats should reveal other representatives of this family as well as the Cytheridae and Darwinulidae. The future investigator would probably discover a few new species as well as extend the range of known species. Ostracods are detritus feeders and herbivores, and they serve as food for bottom-feeding carnivores such as rhabdocoels, oligochaetes, and midge larvae. Some of the swimming ostracods are consumed by fish. Therefore the ostracods desrve to be investigated as an important component of the microfauna of aquatic situations. Ostracods also should receive more attention as ideal research organisms, since many species can be reared in the laboratory under controlled con- ditions; and due to their small size, they require very little space. LITERATURE CITED Cole, G. A. 1959. A summary of our knowledge of Kentucky crustaceans. Trans. Ky. Acad. Sci. 20 (3-4):66-81. Received July 16, 1969. Accepted August 1, 1969. A RECORD OF THE OCCURRENCE OF THE EXOTIC LAND PLANARIAN, BIPALIUM KEWENSE, IN CALLOWAY COUNTY, KENTUCKY MARAGET EVELYN COLE* Murray State University, Murray, Kentucky 42071 In October, 1967, a small population of the land planarian, Bipalium kewense, was discovered on North 16th Street in Murray, Kentucky. The animals were established under concrete blocks next to a storage house. They were collected and examined taxonomically. Serial section slides were prepared by Robert W. Hackney, graduate student; and the slides remain in his possession. A preserved specimen is in the Invertebrate Museum of MSU. According to Hyman (1943, 1954), this tropical land planarian occurs in greenhouses in the United States and has become established outdoors in the Gulf States and up the Atlantic coast into North Carolina. The closely-related species, B. adventitium, is established outdoors in California (Hyman, 1943) and in the Northeastern United States (Klots, 1960). Apparently the exotic land planarians are extending their range in the United States. LITERATURE CITED Hyman, L. H. 1943. Endemic and exotic land planarians in the United States. Amer. Mus. Novitates 1241: 1-23; 25 figs. Hyman, L. H. 1954. Some land planarians of the United States and Europe. Amer. Mus. Novitates 1667: 1-21. Klots, A. B. 1960. A terrestrial flatworm well established outdoors in the Northeastern United States. Syst. Zool. 9 (1): 33-34. Received July 16, 1969. Accepted August 1, 1969. * Supported by Murray State University Institutional Studies and Research Fund. PARASPIRIFER ACUMINATUS FROM THE BREVISPIRIFER GREGARIUS ZONE AT THE FALLS OF THE OHIO JAMES E. CONKIN Department of Geology, University of Louisville, Louisville, Kentucky and BARBARA M. CONKIN Jefferson Community College, Louisville, Kentucky INTRODUCTION During a study of Middle Devonian bone bed stratigraphy of the Jefferson County, Kentucky-southern Indiana area (Conkin and Conkin, 1969), an occurrence of the stratigraphically important brachipod, Para- spirifer acuminatus, was noted 0.1 foot above the base of the Brevispirifer gregarius Zone of the Jeffersonville Limestone (immediately above the Amphipora Subzone of the Coral Zone) at the Falls of the Ohio, Clark County, Indiana (Figs. 1, 2); this paper concerns itself with this singular occurrence and presents some stratigraphic and ecological information regarding P. acuminatus. Stratigraphy As noted by Perkins (1963, p. 1350), the guide fossil, Paraspirifer acuminatus, does not occur in the lower part of the P. acuminatus Zone (of old terminology). P. acuminatus is, however, universally present in the upper part of the P. acuminatus Zone (old terminology) in its out-crop area in northwestern Kentucky, southern Indiana, and central Ohio. Perkins (1963, p. 1350) used the term bryozoan-brachiopod zone for the lower part of the P. acuminatus Zone (without the P. acuminatus guide fossil); our findings (Conkin, et al., In Press) are in agreement with Perkins on this point, for extensive study of this lower part of the P. acuminatus Zone (bryozoan-brachiopod zone of Perkins) in northwestern Kentucky and southern Indiana has never revealed the presence of P. acuminatus. It is therefore rather startling to find P. acuminatus near the base of the underlying Brevispirifer gregarius Zone. Measured Section The following section (Fig. 2), with notation as to the occurrence of Paraspirifer acuminatus in the lowest part of the Brevispirifer gregarius Zone, was measured at the Falls of the Ohio immediately west of the whirlpool as marked on the map (Fig. 1). Paraspirifer Acuminatus 73 — 1000 Ft. Figure 1. Map showing location of the collecting site of Paraspirifer acuminatus at the Falls of the Ohio. Systematic Description Paraspirifer Wedekind in Salomon, 1926 Paraspirifer acuminatus (Conrad), 1839 Figs. 3, 4 Description.—Paraspirifer acuminatus is represented by a fragment of the pedicle valve which is bilobed, with a prominent median sinus, be- coming wider and deeper anteriorly; shell is large with the surface plicated; some of the plications bifurcate anteriorly; concentric delicate striae are obsecured by silicification, as is the usual case in the species. Horizon.—The singular, fragmentary specimen of Paraspirifer acuminatus PARTIAL THICKNESS BRACH | 0- POD ZONE BONE BED <€- SMOOTH LAYER LIMESTONE LJ me O N ic) =) FE <= a (aa <— => —) a= Ww) © aa) (ad =) = JEFFERSONVILLE PARASPIRI FER ACUMINATUS PARTIAL THICKNESS Figure 2. Measured section at the Falls of the Ohio, Clark County, Indiana. Paraspirifer Acuminatus 75 was found in place in the lower 0.1 foot of the Brevispirifer gregarious Zone = the Mollerina greenei Zone of Conkin, et al. (In Press). Remarks.—This single specimen is fragmentary (Figs. 4A, 4B), but sufficient detail is preserved for confident assignment of the specimen to Paraspirifer acuminatus. Detailed comparisons were made between the present specimen and well preserved specimens of P. acuminatus from the P. acuminatus Zone of the Jeffersonville Limestone in Jefferson County, Kentucky and Clark County, Indiana as well as the upper part of the H Zone (P. acuminatus Zone) of the Columbus Limestone in the Columbus, Ohio area. The present specimen is a portion of the pedicle valve which Figure 3. Outlines of disarticulated pedicle and brachial valves and complete specimens of Paraspirifer acuminatus. Magnification is approximately XI. A—Outline of “spoonlike” brachial valve; B—Outline of the less convex posterior two-thirds of the pedicle valve after fragmenta- tion (which broke off the anterior one-third of the valve); C—Outline of complete pedicle valye showing the anterior one-third of the valve which is subject to breakage and separation from the posterior two-thirds of the valve; D—Ouitline of the posterior view of a complete shell, oriented so that the upper valve is the pedicle and the lower valve is the brachial valve; E—Outline of the anterior view of a complete shell, oriented so that the upper valve is the brachial and the lower valve is pedicle valve. 76 James E. Conkin and Barbara M. Conkin Figure 4—Stereopair of a fragment of Paraspirifer acuminatus from the Brevispirifer gregarius Zone at the Falls of the Ohio; X1.5. is the usual valve encountered when P. acuminatus is found disarticulated; in fact, the great predominance of specimens of P. acuminatus in the P. acuminatus Zone in the Falls of the Ohio area, are found as fragments of the pedicle valve (Fig. 3B). The brachial valve (Fig. 3A) is very rarely seen except when the shells of P. acuminatus are not disarticulated (Figs. 3D, 3E). Pedicle valves are almost always broken, but generally only approximately the anterior one-third of the shell is broken off; the remaining two-thirds (Fig. 3B) is flatter and much less convex than the complete pedicle valve (Fig. 3C). The more convex (“spoonlike”) brachial valve (Fig. 3A) was more liable to have been caught by currents and carried away, fragmented by impact of the waves in shallow water, and reduced to “coquinoid” particles. Deposition. —This specimen of Paraspirifer acuminatus is deposited in the U.S. National Museum, Washington, D.C., No. 165849 in Paleozoic Catalog No. 34. SUMMARY A fragmentary specimen of the pedicle valve of Paraspirifer acuminatus was found in place in the lowermost part of the Brevispirifer gregarius Zone = the Moellerina greenei Zone at the Falls of the Ohio, Clark County, Indiana. A detailed measured section of the Brevispirifer gregarius Zone at the Falls of the Ohio is presented with the occurrence of the Paraspirifer acuminatus specimen noted in its lowest 0.1 foot which directly overlies the Amphipora Subzone of the Jeffersonville Coral Zone. Paraspirifer Acuminatus iy The predominance of incomplete pedicle valves of Paraspirifer acum- inatus in the P. acuminatus Zone itself is believed to be a result of dis- articulation of the pedicle and brachial valves and subsequent fragmentation of the pedicle valve. After fragmentation, the pedicle valve was reduced to a rather low convex residual portion which was more stable in currents. The more convex “spoonlike” brachial valve was quite liable to be carried away and fragmented by wave action. LITERATURE CITED Conkin, J. E. and Conkin, B. M., 1969. Middle Devonian bone beds of Jefferson County, Kentucky and southern Indiana. Abstract, S. E. Sec., Geol. Soc. America, p. 14. —————————— , In Press. Middle Devonian Moellerina greenei Zone and suppression of the genus Weikkoella Summerson, 1958. Micropaleon- tology. Perkins, R. D., 1963. Petrology of the Jeffersonville Limestone (Middle Devonian) of southeastern Indiana. Bull. Geol. Soc. America 74: 1335-1354. Received: July 10, 1969. Accepted: October 17, 1969. ACADEMY AFFAIRS THE FIFTY-FIFTH ANNUAL MEETING OF THE KENTUCKY ACADEMY OF SCIENCE, MURRAY STATE UNIVERSITY, MURRAY, OCTOBER 24-25, 1969 HOST: DR. WALTER E. BLACKBURN, Dean, School of Arts and Sciences Minutes The annual business meeting of the Kentucky Academy of Science was called to order by President Orville Richardson on Friday night, October 24, 1969, immediately following the banquet in the Dining Room of the Holiday Inn, Murray, Kentucky. Minutes of the Fall Meeting, 1968, were distributed to members by the secretary, R. Larance. A mction was made and seconded to approve the minutes. The motion passed. The president at this time expressed appreciation and thanks to Murray State University for inviting the Academy to its campus for the 1969 Fall Meeting. The host, Dr. Walter Blackburn, and the entire planning committee received a special thanks. The treasurer, C. B. Hamann, distributed the financial report for KAS. A motion was made and seconded that the report be approved. The motion passed. (This report is filed in the KAS Secretary’s Book. ) President Richardson called upon the Auditing Committee for its report. C. B. Hamann, representing H. Howell, chairman of this committee, presented this report. A motion was made and seconded that the report be approved. Motion passed. (This report is filed in the KAS Secretary’s Book. ) M. Taylor, Director of the Junior Academy of Science, presented his report. Copies of the year’s activities were made available to members present. He expressed a desire and need for help wih the Junior Acadmy, particularly from the extreme Western and Eastern sections of the state. The central sector of Kentucky is most active in the Junior Academy. The President expressed thanks and appreciation for Dr. Taylor’s concern with the Junior Academy. William Wagner, Editor of the Transactions, presented a report o the members. Dr. Wagner stated that the Academy had caught up with its publications and that Volume 30, numbers 3 and 4 should be published in December. He stated that all concerned should try to better the Transactions by submitting high quality papers. After some announcements, the President recessed the meeting until the scheduled 10:00 a.m. Annual Business Meeting on Saturday morning. After greeting the members of the Academy President Richardson, representing the Executive Committee, stated that the Committee had received requests for two new sections of the Academy. These are for the establishment of a “Sociclogy” section and a section called “Physiology, Bio-Physics, and Pharmacology.” A motion was made by P. Sears, seconded by R. Barbour, that each section be established as reccmmended by the Executive Committee. The motion was approved without any opposition. (The Sociology section met for organizational purposes at this 1969 Fall Meeting of the Academy; the President of the Academy appointed Dr. F. Zechman as Chairman and Dr. J. Engelberg as Secretary of the Physiolcgy, Bio-Physics, and Pharmacology Section. They are to get this section together for next year.) The secretary, R. Larance, was called upon to give a report on the Constitution of the Academy. He stated that the Executive Committee recognized a need for certain constitutional revisions within the present Constitution, which was last revised in 1951. After pointing out several parts of the Constitution which should receive attention and perhaps changes, he stated that the Executive Committee Academy Affairs 79 strongly recommended to the in-coming president the appointment of a committee to study and make changes in the Constitution. President Richardson commented upon the action the Executive Committee had taken in connection with the role of KAS in KEP (Kentuckians for Environ- mental Planning.) The President had appointed a committee, Man and His Environment, to study and make recommendations to the Academy at the Fall Meeting, 1969, as to KAS’s role and activity with KEP. The Committee had not met; thus, no report. With this information Dr. R. Barbour made a motion that “KAS affiliate itself with KEP.” The motion was seconded and passed. Con- siderable discussion followed as to who would represent the KAS and the duties of the representatives. With this in mind Dr. B. Branson made a motion that the Executive Committee cf KAS act as an advisory committee to the representative to KEP. The motion was amended to read as above plus “the Executive Committee would appoint a delegate and an alternate delegate (today—10/25/69).” The motion and amendment passed. Dr. R. Barbour, University of Kentucky, and Dr. B. Branson, Eastern Kentucky University, were appointed delegate and alternate respectively. It was announced by the president that the next Annual Fall Meeting would be held at Gecrgetown College, Georgetown, Kentucky, and that in 1971 Eastern Kentucky University, Richmond, Kentucky, would host the meetings. In 1972 Transylvania College will act as host to the meeting in Lexington, Kentucky. Immediately, the Academy received invitations to meet in 1973 at Morehead State University and from Centre College to meet there in 1974. G. Wilson, Jr. was recognized by the President to make comments upon the functicn of the Board of the Academy. He stated that as it is now the Board of Directors do not meet and are not functioning. He stated that the Board should work to stimulate local and state industry in supporting the activities of the Academy. J. Engelberg commented upon the disadvantages of receiving large financial sums from industries and the advantages of support from small industries. He stated that it may be to the Academy’s advantage to receive small amounts of money from a large number of industries rather than large amounts from a few. There may be danger of becoming committed to large donors, he stated. He also commented upon advantages of having a secretary as we now have rather than an Executive Secretary. Dr. B. Branson was recognized to state that he thought the Academy should receive any amount of money, large or small, from anyone or from any industry or institution. Dr. Branson also was in favor of the Academy having an Executive Secretary. The Nominating Committee reported the following officers for the Academy and with no additional nominations from the floor, they were elected by ac- clamation. PEE SH CTI er aecdeescauchs. cccscctadessssesencoaenadossuctencssncacenencese-cesseatateacstentodaatzoctt catecceer eeeeeeeeee to 1969 Tiloyd iB. Alexander. icc tcccccocssiscacatsosacdassestobaccnesoonceedtcccessaneresst ete aa tea eeeeeeen to 1969 PROGRAM Friday, October Twenty-Fourth 12:45-4:00 p.m. Optional Field Trips: Land-Between-the-Lakes Recreation Area or Calvert City Chemical 1:00-6:00 p.m. Registration 6:00 p.m. Social Hour, Holiday Inn 7:00 p.m. Banquet, Holiday Inn Welcome: Dr. Harry Sparks President, Murray State University Feature Address: Dr. Donald Caplenor Dean, College of Arts and Sciences, Tennessee Technological University Topic: “What is the Way to Effective Conservation” Saturday, October Twenty-Fifth 8:00 a.m. Sectional Meetings 10:00-10:45 a.m. Annual Business Meeting 11:00 a.m. Sectional Meetings 12:00 Noon Informal Luncheon Assembly 8:40 9:00 9:20 9:40 11:00 11:20 11:40 8:30 ANTHROPOLOGY SECTION Richard Furlow, Chairman Frederic Hicks, Secretary Initiation Rite Theory: The Maori Case—A Consideration of Alternatives. Michael F. Conway, Western Kentucky University. The Management of Tension Persuant to Witchcraft Accusation: A Comparative Study. Allen C. Turner, University of Kentucky. A Paramount Chief as an Agent of Change. Steve Davis, University of Kentucky. The Growth of Negro Landownership in a Rural Louisiana Parish. Jules W. Delambre, University of Kentucky. Preservation of Prehistoric Human Remains in Kentucky. Louise Robbins, University of Kentucky. Observation and Analysis of Human Remains from an Archaic Burial in Trigg County, Kentucky. John E. Keller, University of Kentucky. Election of Officers BOTANY AND MICROBIOLOGY SECTION Charles J. Isbell, Chairman Harold E. Eversmeyer, Secretary Effects of Cycocel and B-Nine on Certain Mitrogenous Fractions in Barley Seedlings. Kinser, Linda and Frank Toman, Western Kentucky University. 8:45 9:00 9:15 9:30 9:45 11:00 11:15 8:30 8:45 9:00 9:15 9:30 9:45 11:00 11:15 11:30 8:00 8:15 8:30 8:45 Academy Affairs 83 The Flora of Kentucky as an Object for Field Study and the Teaching of Botany. Willem Meijer, University of Kentucky. Studies in Lichen Enzymology. Seibert, Sr. M. Angelice, Ohio State University. The use of Computers in Taxonomy. Marion J. Fuller, Murray State University. Flowering Cycle of the Commen Dandelion. Eugene M. McGehee and Elmer Gray, Western Kentucky University. Relative Concentration of Fermentation Products in Corn Silage Contain- ing Various Levels of Urea. Shirley, J. E., L. D. Brown, J. D. Skean, W. H. Stroube, and L. Mutter, Western Kentucky University. Relic Species in the Red River Gorge. Mary Wharton, Georgetown College. Business Meeting and Election of Officers. CHEMISTRY SECTION K. Grant Taylor, Chairman Gordon Wilson, Jr., Secretary Stoichiometry, Physical Properties and Bonding in Scandium Hydride. W. G. Bos and C. Dean Parks, University of Louisville. Thermochromism in Simple Anhydrides. Jerry Hendon, Annette Gordon and Marshall Gordon, Murray State University. The Determination of Stability Constants for Iron (III) and Vanadium (V) with Beta-Isopropyltropolone by the Extractive Method. B. E. McClellan, Murray State University, David Bright, University of Maryland and Oscar Menis, National Bureau of Standards. Synthesis and Characterization of tris—( Malononitriledithiolato ) metalates. T. H. Crawford, University of Louisville and H. B. Gray, California Institute of Technology. Mechanism of the Base Catalyzed Synthesis of Azobenzenes. Ellis V. Brown and William Kipp, University of Kentucky. Election of Officers and Coffee Break. Selective Deprotonation of Imidazoles. John L. Wong, University of Louisville. Some Electrophilic Reactions of Carbenoids. K. G. Taylor, W. E. Hobbs, M. Clark and M. Saquet, University of Louisville. The Separation of Acetone from Water by Salting Out and its Use in Solvent Extraction. Charles E. Matkovich and Gary E. Christian. GEOLOGY-GEOGRAPHY SECTION Preston McGrain, Chairman Dennis L. Spetz, Secretary Election of Officers. Paleozoic Oil Possibilities in the Jackson Purchase, Western Kentucky. Howard Schwalb, Kentucky Geological Survey. Paraspirifer acuminatus in the Brevispirifer gregarius Zone at the Falls of Ohio. James E. Conkin, University of Louisville and Barbara M. Conkin, Jefferson Community College. Plant Fossils from the St. Louis Formation in Kentucky. Ruth G. Browne, Louisville and Albert L. Bryant, Geologist, Louisville Gas and Electric Company. 84 8:15 Academy Affairs The Stratigraphic Position of the Renfro Member of the Borden Forma- tion (Mississippian) in East-Central and Northeast Kentucky. John C. Philley, Morehead State University. Subsurface Geology of Kentucky Cryptoexplosion Structures. C. Ronald Seegar, Western Kentucky University. Subsurface Geology and Ground-Water Resources of the Jackson Purchase Region, Kentucky. Robert W. Davis, United States Geological Survey. Recognition of Upper Mississippian Time-Stratigraphic Units in South- central Kentucky. E. R. Pohl, Horse Cave, Kentucky. Urbanization in Kentucky: Patterns and Trends. William A. Withington, University of Kentucky. Development of Railroads in the Purchase Area of Western Kentucky. Stanford Hendrickson, Murray State University. Geography of Homer. Kguis Hicks, Murray State University. The Populaticn Distribution on the Ethiopian Plateau. S. Reza Ahsan, Western Kentucky University. PHYSICS SECTION Fletcher Gabbard, Chairman George K. Miner, Secretary Optical Properties of Antimony Trisulfide. G. R. Morris and J. M. Kline, Murray State University. Beam Foil Spectroscopy at Murray State University. Lewis M. Beyer, ~Murray State University. Optical Processing of Ultrasonic Fields...W. Richard Klein, Murray State University. nh wea ae A New Method for Investigating the Surface Reflection of Low aces Electrons. M. W. Russell, A. D. Sanders, J. D. Burd and I. E. Collier, Western Kentucky University. Electron Reflection Coefficient of Polycrystalline Tungsten from 0.4 to 10 eV. I. E. Collier and M. W. Russell, Western Kentucky University. Nuclear Structure of the Argon Isotopes. B. D. Kern, University of Kentucky. The Nuclear Energy Levels of 194Pt. Donald Benson, Bresica College. Mossbauer Measurements on Single Crystal Potassium Ferrocyanide Trihydrate vs. Orientation. H. E. Groskreutz, Thomas More College. Report on the Middlebury Confers .on the Teaching of Physics in Liberal Arts Colleges. G. K. Miner, Thomas More College. Improved Lecture and Laboratory Apparatus. J. G. Black, Eastern Kentucky University. PSYCHOLOGY SECTION Rex Knowles, Chairman Harry Robe, Secretary The role of the Hippocampus in Discrete Trial Inhibitory Behavior. Thomas B. Posey, Murray State University. Abstract and Concrete Response Bias on the Similarities Subtest of the WAIS as a Function of Sex. Thomas B. Posey, Murray State University; Richard Alumbaugh, Central Washington State College; Charles G. Halcomb, and David Taylor, Texas Tech University. 8:45 9:00 9:15 9:30 11:00 11:15 9:00 9:20 Note: 9:00 Note: 8:00 8:15 8:25 8:40 8:55 9:10 9:25 9:40 9:50 Academy Affairs 85 The Role of Intra-maze Cues in Choice of “place” versus “response” strategics by Rats Solving a T Maze. Sterling Hall, Centre College. Political Affiliations of High School Seniors and their Parents. Sam Floyd and Gene Weis, Bellarmine-Ursuline College. The Effects of Occupation and Social Environment on Female Perception of Males. L. M. Faindaca, D. S. O’Leary, and E. A. Ross Jr., Bellarmine- Ursuline College. Synchronization of Non-24-hour light-dark Cycles Affecting Reproduction in Animals. Frederick M. Brown, Centre College. Program: New Programs offered in Conjunction with Psychology in Colleges and Universities in Kentucky. Rex Knowles, Chairman. Election of Officers. SCIENCE EDUCATION SECTION Frank Howard, Chairman Morris Taylor, Secretary General Business Meeting and Election of Officers. Discussion of Science Education in Kentucky. Other Portion of Program to be Arranged. SOCIOLOGY SECTION C. D. Bryant, Appointed Chairman Organizational Meeting and Election of Officers. This is an organizational meeting for Sociology, which is to become a new section of the Kentucky Academy of Science. ZOOLOGY SECTION John C. Williams, Chairman Election of Officers. Preliminary Report: Effects of Stripmining on the Fish Fauna of Leather- wood and Bear Branch Creeks, Breathitt County, Kentucky. Branson, Branley A. and Donald L. Batch, Eastern Kentucky University. Fishes of the Spring River Drainage; Missouri, Kansas and Oklahoma: Origin and Affinities. Branson, Branley A., Eastern Kentucky University. Advances in Faunal Research*on Kentucky Lepidoptera. Covell, Charles V., Jr., University of Louisville. A Statistical Study of the Human Sex Ratio. Loyd, Robert C. and Elmer Gray, Western Kentucky University. A Preliminary Investigation of the Incidence of Acanthocephalans in Freshwater Fish from two Similar Streams in Rowan County, Kentucky. Smith, Langston D., Morehead State University. A Comparison of the In Vitro Viability of Mouse Ova from Hormone- Treated Mice with Ova from Spontaneous Ovulations. Spears, James R., Morehead State University. Waterfowl Marking for Visual Identification. Rudersdorf, Ward J., Eastern Kentucky University. Some Studies of the Feather Tracts of Developing Japanese Quail (Coturnix c. japonica). Hamon, J. Hill, Transylvania College. 86 11:00 11:15 11:30 11:45 12:00 Academy Affairs Preliminary Studies of the Effects of Lipase and Temperature on the Rate of Maceration in Some Birds. Whisler, James R. and J. Hill Hamon, Transylvania College. Survey of Plecoptera as they Relate to Stream Classification in Tight Hollow and Mill Creeks, Wolfe County, Kentucky. Batch, Donald L. and Branley A. Branson, Eastern Kentucky University. Does the Arterial Pulse Wave Transport Blood? Engelberg, Joseph, University of Kentucky. Body Weight and Blood Volume Relationships in Parasitized and Non- Parasitized Tobacco Hornworm Larvae. Dahlman, Douglas L., University of Kentucky. Sex Hormones and their Effects when Reversed in One-Day Old Chicks. Meek, Baron and James W. Snyder, Eastern Kentucky University. INDEX TO VOLUME 30 ACADEMY AFFAIRS, 78 Aliff, J. V., 20 Bipalium Kewense, 71 Brevispirifer Gregarius Zone, 72 Cathaemasia Reticulata, 20 Clark’s River, fishes, 54 Cole, M. E., 69, 71 Conkin, B. M., 72 Conkin, J. E., 72 Destrafication in Impoundments, 1 Eastern Belted Kingfisher, 20 Editorial, 53 Edney, J. M., 20 Falls of the Ohio, 72 Fishes of West Kentucky, Clarks River, 54 Obion Creek, 60 Irwin, W. H., 1 Land Planarian, 71 Obion Creek, fishes, 60 Ochrotomy Nuttalli (Harlan) in Kentucky, 45 Ostracoda, Western Kentucky, 69 Paraspirifer Acuminatus, 72 Plankton Populations, 1 Plethodon Richmondi, 38 Rhinichthys Atratulus Meleagris Agassiz, 23 Robinson, E. L., 1 Sisk, M. E., 54, 60 Smith, P. L., 60 Symons, J. M., 1 Tarter, D. C., 23 Wallace, J. T., 38, 45 Western Blacknose Dace, 23 =e ea vei eh Ble Ss. INSTRUCTIONS FOR CONTRIBUTIONS The TRANSACTIONS OF THE KENTUCKY ACADEMY OF SCIENCE is a medium of publication for original investigations in science. Also as the official organ of the Kentucky Academy of Science, news and announcements of interest to the member- ship are published therein. These include programs of meetings, titles of papers presented at meetings, and condensations of reports by the Academy’s officers and committees. Papers may be submitted at any time to the editor. 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The author is responsible for correcting the galley proof. Extensive alterations from the origical are expensive and must be avoided or paid for by the author. Galley proofs must be returned promptly. Blanks for reprint orders will be supplied with the galley proof. ie i % TRANSACTIONS OF THE KENTUCKY ACADEMY OF SCIENCE Volume 31, 1970 EDITORIAL STAFF Editor WILLIAM F. WAGNER Associate Editors WILLIAM DENNEN, Geology MarsHALL Gorpon, Chemistry LL. A. KrumuHowz, Botany and Microbiology RosBerT KuEHNE, Zoology Editorial Office Department of Chemistry University of Kentucky Lexington, Kentucky 40506 Published in 1970 by THE Kentucky ACADEMY OF SCIENCE CONTENTS TO VOLUME 31 Nos. 1-4 Upper Mississippian Deposits of South Central Kentucky— A Project Report HEV, PO ERD i doc eccckedboreendecesdivecssscnisencevuesetetesers-cvesee ee 1 The History of Anthropology Departments in Kentucky Universities LOUISE M. ROBBINS, Editor’ «.....):c..6.0ci.s-00-0-;2ee soe 16 I. Anthropology at Transylvania CARA E. RICHARDS and L. A. BROWN 2.2.2.8 19 II. Anthropology at the University of Kentucky Lexington Campus FRANK J. HSSHNED ....0:cccccccscseseotecoecerescscenesereneteeeeememee 22 III. The Growth of Anthropology at the University of Louisville FREDERIG HICKS) .5.2...c:cs::chescce.ieccscces sen ee eee 28 An Annotated Check List of the Dragonflies and Damselflies (Odonata) of Kentucky PATRICIA LILES RESNER Some Mechanisms With Which Crotalus horridus horridus Responds to Stimuli A Lets) WEED IR. josesecsescssecdeeledeceed caste eet 45 The Corn Snake, Elaphe Guttata Guttata (Linnaeus) in Kentucky JOSEPH: A COWLIEINS » o.é.c.2.225.c52 Stenace states see eee 49 An Annotated List of Fishes From the Upper Salt River, Kentucky R. D. HOYT, S. E. NEFF and L. A. KRUMHOLZ .................. 51 Record of Occurence of a Trypanosome Infection in the Prairie Vole Microtus Orchogaster, in Jefferson County, Kentucky WILLIAM T. McGEACHIN, FRED H. WHITAKER, and FRANK WitQUIGK: [Rey 2s... cccuceasct re saeneeeeeeeeeeere .. 64 Continued on next page Kentucky Algae GARY E. DILLARD and STEPHEN B. CRIDER ................... 66 List of Amphibians and Reptiles from Tight Hollow in East- Central Kentucky BRANLEY A. BRANSON, DONALD L. BATCH, ERIE OU NICE: SIM) ig NOOB 2s loeescusaeounesss-bedanaeconsaceseesoteaseesowees 73 Records for and Annotations on Some Valley Millipeds (Diplopoda) from Northern Kentucky ..............ccccccssccceseeeeseeees 79 Spiders (Arachnida: Araneida) from Northern Kentucky, with Notes on Phalangids and Some Other Localities BRANLEY A. BRANSON and DONALD L. BATCH ............ 84 Pilot Experiments Involving X-ray Induced Mutants in the Dumpy and Yellow Regions of Scute—19i Chromosomes in Drosophila Melanogaster SAU AG Elen @ ON ETAE YOUR YG ie areca socease a. cca sce casuacdaesseaticvsusesecessee 99 A Search for Trypanosoma cruzi in Kentucky Opossums IKON PANTER Eh Soee sci sccncotus muaria sent dass Sesceuaansnfaey candace arsagaseen 104 PAG MD EEL ey NEO ANE ENS aeac oe csh ananassae hes aseceatcestsousbever vesuscnedeedsdecnerene se 105 Mae XALOMN OLUTIIO LO LO dreh ene an cc ieee Lu Mn CU AED hhc a A ee VS i j ING NG 7 Vol. 31, Nos. 1-2 1970 Coden: TKASAT TRANSACTIONS of the KENTUCKY ACADEMY ot SCIENCE Official Organ KentTucky ACADEMY OF SCIENCE CONTENTS Upper Mississippian Deposits of South Central Kentucky— A Project Report mpm RO EDO pO ees ey eee EL iduea ee wanewec 1 The History of Anthropology Departments in Kentucky Universities Perse My ROBB INSS BGitor -2.c20.<2 csscccsscoeciesoleevevecacastensscetee 16 I. Anthropology at Transylvania CARA E. RICHARDS and L. A. BROWN ................ 19 II. Anthropology at the University of Kentucky Lexington Campus PEE ea Cd epee EN ocala ee Use naucaet kay satandeebedouendh Ganboonaces 22 Ill. The Growth of Anthropology at the University of Louisville USES BAD I Da RU LGah o UG, Co i pal ear ae le le Rae A Ao 28 An Annotated Check List of the Dragonflies and Damselflies (Odonata) of Kentucky Berend E NAG LING) es Le Peis ER EL INIUERS sik oes ceg sssaveticubenccesedeeneosabonsederssones 32 Some Mechanisms With Which Crotalus horridus horridus Responds to Stimuli Py ED ec, 45 The Corn Snake, Elaphe Guttata Guttata GRRE NZ in Kentucky RBH T) CORDING (2... ROT H1970-~- . 49 NLIBRARIE The Kentucky Academy of Science Founded May 8, 1914 OFFICERS 1969-70 President: Lloyd Alexander, Kentucky State College President-Elect: Karl Hussung, Murray State University Vice-President: Marvin Russell, Western Kentucky University Secretary: Robert S. Larance, Eastern Kentucky University Treasurer: C. B. Hamann, Asbury College Representative to A.A.A.S. Council: Mary Wharton, Georgetown College BOARD OF DIRECTORS Rear) Einascuin yt 2 sscpeatecsiscsdeeoodks to 1970 Gordon Wilson ........... sasusvencens tO LOE Grace Ouro. cos.ccnssaverseseeees to 1970 L. A. Krumbolz: 2.0223 to 1972 John M. Carpenter ............00000 to 1971 Sanford’ Li: Jones <;..2225ee to 1978 William M. Clay. i.ccscseccsccacesne to 1971 Ellis .V.. Brown iste to 1973 EDITORIAL OFFICE William F. Wagner Editor Department of Chemistry University of Kentucky Lexington, Kentucky, 40506 Associate Editors: Botany and Microbiology: L. A. Krumholz, University of Louisville Chemistry: Marshall Gordon, Murray State University Geology: William Dennen, University of Kentucky Zoology: Robert Kuehne, University of Kentucky Transactions indexed in Science Citation Index —— Membership in the Kentucky Academy of Science is open to interested persons upon nomi- nation, payments of dues, and election. Application forms for membership may be obtained from the Secretary. THE TRANSACTIONS are sent free to all members in good standing. Subscription rates for non-members are: domestic, $4.00 per volume; foreign, $4.00 per volume. The TRANSACTIONS are issued semi-annually. Four numbers comprise a volume. Correspondence concerning memberships or subscriptions should be addressed to the Secretary. Exchanges and correspondence relating to exchanges should be addressed to the Librarian, University of Louisville, who is the exchange agent for the Academy. Manuscripts and other material for publication should be addressed to the Editor. UPPER MISSISSIPPIAN DEPOSITS OF SOUTH-CENTRAL KENTUCKY A PROJECT REPORT E. R. POHL Box 527, Horse Cave, Ky. 42749 Introduction A critical review of the Upper Mississippian sequence in south-central Kentucky was initiated about five years ago. The endeavor consists of con- tinuous channeling of these beds. Insoluble residues and polished, vertically overlapping study surfaces are produced for the carbonates. Thinsections are prepared at vertical intervals averaging no greater than 15 centimeters, and multiple slides are produced wherever necessary for biostratigraphical and sedimentological purposes. The practice is to sample measured field sections of artificial exposures of greatest possible continuous thicknesses, geographically closely spaced (Fig. 1). The purpose is to accumulate maxi- mum source data for the interpretation of the depositional and biological history of one small area of the earth’s surface during a selected interval of time. The data, therefore, includes some information not available from continuous core material alone, by providing unlimited selected-horizon collections and the opportunity to study and record lateral variations. Results, to date, comprise just over two thousand mounted micro- sections, with appropriate reserve samples, and nine excellently preserved, free-form microfaunules. The latter, composed mostly of foraminifers and ostracods, are stratigraphically distributed as follows: Salem 2, St. Louis 2, Ste. Genevieve 2, Fraileys 1, Glen Dean 1, and Tar Springs 1. An estimated 80 percent of the foraminiferan species are undescribed and some of the genera are new to eastern North America, to the Mississippian, and to the Paleozoic. Systematic paleontologic study of the most prolific of the faunules, the Fraileys (Pohl, Browne and Chaplin 1968), has been delayed until new techniques were devised and refined for thinsectioning specimens in the 100 to 300 micron size-range. This method will be reported in detail later. A co-worker, R. G. Browne, has a paper in advanced preparation on the more unusual foraminifer genera. J. W. Baxter is participating in a study of the stratigraphic value of the dasycladacean genus Koninckopora and other calceareous algae. Thanks are due A. C. McFarlan, Alan Horowitz, Garland Dever and J. W. Baxter, who have read this manuscript and have offered valuable suggestions. Discussion Pre-Salem Deposits. No attempt is made to unravel the intricate and involved correlation efforts, applicable to the local column, of numerous workers studying the stratigraphic units near the base of the Upper Mis- sissippian. Significant efforts in the Illinois Basin have extended over the past 100 years. An excellent summary of the history of the current unit bo E. R. Pohl 1 2 Jackson Oo 25 50 75 100 MILES Legend F sj Outcrop of Mississippian ~~] Post-Borden Epeiric Ry pest Bord ah Post-Paleozoic Embayment. . % — Standard Collections. 2 — Comparison or Preliminary lOWAs, Collections. Wos Columbus 1 e A < ° x Springfield \Cincinnati °* Frankfort 4 SS J> / Cae \ WARREN Jy * ee 1 be Se OOS Zs ZRZ~\ LONE EN Fig. 1. Area of this Study of Upper Mississippian Epeiric Sediments and approximate Location of Collecting Sites. Outcrop Outline is diagramatic and does not include Out- liers or Inliers. names, Borden, Ramp Creek, Harrodsburg, and Warsaw, is given by Line- back 1966: 33-34. His findings are followed here and are supported at the present stage of this study. In south-central Kentucky deposits equivalent in position with the Ramp Creek Member of the Ullin Formation (Lineback 1966) of Indiana and southern Illinois form the base of the Upper Mississippian (Fig. 2). The change from the predominantly terrigenous Borden to the predominantly biogenous Ullin rocks is not sharply defined. There appears to have been no interruption in deposition as the regional process of infilling of the deep- water depressions and troughs of the Borden marine-delta front progressed to the end of Harrodsburg time. A striking feature of the lower part of these beds, their massive lenticular nature, is shown in recent artificial cuts in central Kentucky, particularly along the Blue Grass Parkway east of Elizabethtown, and at natural exposures near Great Falls, Tennessee. Up- ward the bedding becomes less and less inclined, and less lenticular; as- suming horizontal sheet-like bedding toward the top. The Harrodsburg Limestone was redefined recently for Kentucky to ex- clude the Ramp Creek Member from the Upper Mississippian and to in- clude all other beds to the base ‘of the Salem in one unit (Sable, Kepferle and Peterson 1966). Lineback (1966) has since included the Ramp Creek Upper Mississippian Deposits 3 beds in the Ullin Formation which is, thus, again equivalent to the original Harrodsburg definition (Hopkins and Siebenthal 1896). Salem Deposits. The Salem equivanent beds of the area differ from those above in the presence of much terrigenous carbonaceous material, frank pyritization of great quantities of fossil fragments, and quantities of quartzose silt. It is not at all clear, at present, that the range of Globoendo- thyra baileyi (Hall) coincides with the boundaries of beds of Salem age. It is, certainly, most common here; but the genus extends upward through- out the Mississippian, and has representatives in beds of Harrodsburg lithology. Until more definitive work is forthcoming on this group of foraminifers, its occasional occurrence should not, alone, be depended on to identify Salem deposits. Salem—St. Louis Contact. The cooperative geologic mapping program, involving the federal and state agencies, was undertaken early in the 1960's. Under this project, the field exposures, the subsurface and the relationships of the Upper Mississippian deposits in south-central Kentucky have under- gone massive investigation. However, despite the common effort and the unprecedented opportunity for consultation, the varying backgrounds of the many mappers has led to a multiplicity of concepts of what constitutes the limits of formational units and their fundamental internal attributes. Some confusion and conflict inevitably found its way into the published quad- rangle maps on matters of complex stratgraphic relationships. Widely varying and sometimes conflicting criteria have been used to define the Salem—St. Louis contact of the study area: 1—at the top of the highest coarse bioclastic limestone of the Salem sequence (Myers 1964, S. Moore 1963a, Nelson 1963); 2—gradational and/or intertongueing (Haynes 1963, 1962, F. Moore 1968, Ketner 1962, Cattermole 1966, Haynes 1965, 1964a, Peterson 1966, Kepferle 1967); 3—at the topmost sandy limestone of the Salem (Cattermole 1966); 4—no definitive criteria (Miller and S. Moore 1967, Kepferle 1966, Gildersleeve 1962, Haynes 1962, Miller and S. Moore 1967); 5—with local 3 to 6 foot blue-grey limestone at the base of the St. Louis (Cattermole 1965); 6—a 5 to 15 foot basal unit, in the St. Louis, of banded, shaley limestone with lens and banded chert and a “probable facies of the above”, a fine grained detrital limestone with calcite and silt matrix (S. Moore and Miller 1965); 7a—Salem-like bed 15 to 25 feet above base of St. Louis (S. Moore 1968), or a variant of this, 7b—a 3 to 5 foot bed of dark grey fossiliferous limestone 45 to 55 feet above the base of the St. Louis (S. Moore 1968); 9—St. Louis crossbedding and stylolites less prominent than below (Ketner 1962); 10—a 3 foot shale at the base of the St. Louis (Miller 1969); and 11—“Amoeboid” chert and conglomerate or breccia near the base of the St. Louis (Kepferle 1967). In consequence of this diversity of opinion there are probebly as much as fifty feet of deposits in various parts of the study area whose affinities to the Salem or St. Louis are in question. In this study, support is given categories 1 and 3 above thus excluding from the Salem any evaporitic facies and emphasizing the importance of the non-silty character of the St. Louis deposits. E. R. 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R. Pohl St. Louis Deposits. Beds of St. Louis age in the lower two-thirds of the formation are rapidly variable laterally; no attempt has been made pre- viously to formally subdivide these deposits. They comprise mostly inter- tidal, supratidal and evaporitic accumulations with relatively thin, less restricted marine facies at irregular intervals. Mappers responsble for the geology of the central and southern parts of the study area fail to mention the dominant evaporitic facies of the main body of the Lower St. Louis, even though it was well known to the north and west (Kepferle 1966). This feature is well shown along U. S. Highway 31E just north of the Green River Bridge, and at a number of minor exposures elsewhere in the area. The generally covered nature of this interval and of the dominantly dolomitic beds overlying them is the probable cause of this failure. The upper one- third of the St. Louis beds of the area comprise an open shelf facies. The various carbonate rock types here give the earliest evidence in the Upper Mississippian of recurrent events of a rhythmic and cyclic character. St. Louis—Ste. Genevieve Contact. The determination of the contact between the St. Louis and Ste. Genevieve Formations has long been highly controversial among workers throughout the Illinois Basin. It is no less so in the present area of study. Field criteria have been developed according to varying concepts, as shown here: 1—no definitive criteria (Miller and Moore 1967, Richards 1964, F. Moore 1966, Haynes 1966, 1962); 2—at the top of bedded fossiliferous, or blocky, chert 2 to 10 feet thick (S. Moore 1963, Haynes 1965); 3—Lithostrotionoids in uppermost beds of St. Louis (Miller 1969); 4—white, oolitic fossiliferous limestone in the upper part of the St. Louis (Haynes 1964a); 5-10 to 15 feet, or an indefinite thickness, below (Lost River) chert (S. Moore and Haynes 1967, Shawe 1963, Gilder- sleeve 1963, Cattermole 1966, Miller 1969); 6—above highest residual ball chert below tan, blocky chert and at topographic break in slope (Rainey 1965). Not mentioned in the above list is an informal field criterion often used where fresh exposures are encountered at this interval, such as in quarrying operations. This is called the “color break” in which the St. Louis beds have been identified by their darker, or bluer, color. Needless to say, this guide is without validity, as it represents only a shift in the character of the carbonate matrix. The faunal ranges of certain biocriteria previously considered diagnostic of beds of Ste. Genevieve age have been extended downward. There have been earlier reports that Platycrinites penicillus (M. & W.) and Pugnoides ottumwa (White) were present beneath the base of the Ste. Genevieve (McFarlan 1943, Bom 1943). This study shows that both taxa occur 65 feet beneath the Lost River Chert Bed (Swann 1963), well below the top of beds previously assigned to the St. Louis (see Gildersleeve 1963), at the abandoned McLellan Quarry in the southwest corner of the Bristow Quadrangle, GQ-216. Attention to various microfaunal elements, particularly foraminifers and algae, has added additional historical criteria which appear to be of greater Upper Mississippian Deposits 7 help in determining affinities of deposits than do such selected taxa of the macrofauna. Depositional Energy Zones and the Sequence Model. The late St. Louis, Ste. Genevieve and early Girkin deposits of the area have been depicted as a helter-skelter disposition of widely varying carbonate types, both horizontally and vertically (Klemic 1963a, Miller and S. Moore 1967, Haynes 1964b, 1966, and others). These beds are here interpreted as an extremely well organized expression of rhythmic and cyclic deposition with- in a well-defined model. This study’s findings are not new, and reference is made to a single, earlier application of this concept to beds in the late part of the Ste. Genevieve and early part of the Girkin at the western edge of the present study ara (Sandberg and Bowles 1965). However, their sug- gested organization was not pursued and there is some confusion in the two separate sequences they offered for successive parts of the column. A model involving large amounts of clastics, deep-water environments, and basin infilling would be required for deposits earlier than the St. Louis, and is not attempted here. Neither is enough presently known about the St. Louis evaporitic facies, with its irregular and frequent alternation of structureless microspars, biomicrites, and minutely comminuted skeletal calcarenites, to indicate any sequential organization. It is noteworthy that these limestones, of very high purity, are associated with salt casts, algal pisolites, algal felts, and indistinct biscuits, oncoliths and stromatoliths: and that the gypsum, although vuggy, is banded and bedded. Serpulids are frequent. The relatively great topographic irregularity of the Borden epeiric sea floor, amounting to 200 to 800 feet as calculated by Swann, Lineback and Frund (1965), was mostly eliminated by the accumulation of Ullin and Salem deposits, resulting in a monotonous, shallow-water shelf. The earliest true blanket sediments to appear in the Upper Mississippian of east-central North America were of late St. Louis time. In such sediments lateral ex- tents were on the order of hundreds of miles and bottom slopes measured feet, or fractions of feet, per mile—the result of wave base activity in the lesser depths and of marine currents in areas farther down slope. It is in these sediments that cyclicity is most frequently evident and most amenable to interpretation. It is, also, the type of sediment, when composed almost exclusively of carbonates, that affords little field evidence of nonsequence and none of hiatal values. The use of a depositional model for clear-water, shallow marine car- bonate sediments (Irwin 1965, Armstrong 1967) offers a solution to events of transgression-regression, which should be reflected in sediment character as workable criteria. Such use would appear to avoid the confusion at- tending the determination of the Salem—St. Louis—Ste. Genevieve—Girkin boundaries. In the study area—one of essentially uninterrupted carbonates— the “formation” or mapping unit has been arbitrary, at best. Incidents of greatest stratigraphic significance include the appearance to an otherwise autochthonous sequence of patently terrigeonus material. This 8 E. R. Pohl occurs in the form of thin and abrupt clay-shales (near the top of the St. Louis as later defined, at several horizons within the Fredonia, Karnak and Paoli, and at the position of the Sample and the Elwren); and disseminated quartzose silt- and sand-grains (especially at the top of the Salem, in the top beds of the St. Louis and of the Fredonia, and at the positions of the Spar Mt., Bethel, Sample, and Elwren= ? Cypress). Occurrences of dolo- stones, algal stromatolites and oncolites, and of bedded cherts are also periodic (see Fig 2). In the local depositional model these all find a proper and rational role in the sequence (Table 1). Table 1. Shallow, Clear-water depositional Model for Upper Mississippian carbonate Sequence of south-central Kentucky. Modified from Irwin 1965, and Folk 1959. ENERGY ZONES Shoreward ————>- <——— Seaward Areally Extensive. MODERATE-LOW ENERGY. Areally Extensive. Areally Restricted. HIGH ENERGY. GENERALLY LOW ENERGY. BEYOND ALL BUT STORM-WAVE ACTIVITY. SEDIMENT MOSTLY POORLY SORTED DETRITUS FROM ZONE Y PLUS LITTLE-WORN INDIGENOUS SKELETAL MATERIAL. HIGHLY OXYGENATED, SUBJECT TO VIOLENT, STORM-BORN WAVE & TIDE ZONE. SEDIMENT} FLOODING ACTIVITY. SEDIMENT MOSTLY WELL SORTED, SKEL-]| BASICALLY CHEMOGENIC. ETAL DETRITUS, BASICALLY BIOGENIC. DEPOSITIONAL ZONES & COMMON SEDIMENT TYPES MATRIX MOSTLY CALCISILTITIC. MATURE OO"MICRITE", BIOCALCISILTITE. OOSPARUDITE, |FINE-GRAINED MATURE-OOLITH | CALCARENITE, CRINOIDAL LIMESTONE, SULFIDE |OOSPARITE, BIO-| FINE-GRAINED —_ $$ FACIES SPARUDITE. OOSPARITE & OOMICRITE, SPICULAR BIO- MICRITE, COAT- ED-GRAIN SPAR- ITE, MATALGA, CHALKY DOL-|BEDDED GYP- OMITE, GHOST |SUM, FLUORI DOLOSTONE, |MICROSPARITE. DOLOMITIZED |SALT CASTS. BIOMICRITE, DOLOMICRITE, ALGAL- ASSOC- IATED DOLO- MITE. THIN-WALLED OSTRACOD ONCOLITES. DISSEMINATED QUARTZOSE SILT THIN, BARREN. CLAY-SHALES. BEDDED CHERT+>LENTICULAR CHERT (OFTEN The Horse Cave Limestone: a new stratigraphic member of the St. Louis Formation. I am convinced of the need to establish a new unit for beds adjacent to the St. Louis—Ste. Genevieve boundary. These beds, until now, usually referred to the basal Ste. Genevieve simply because of the customary presence of Platycrinites penicillus, are assigned to the upper- most part of the St. Louis Formation. The evidence for this assignment includes lithologic, sequential, and paleontologic evidence. These beds are designated as the Horse Cave Member of the St. Louis Formation. The Upper Mississippian Deposits 9 type locality is the Hart Stone Company Quarry, one mile east of the town of Horse Cave, Hart County, Kentucky. Here, 38 feet of ledges near the base of the 1969 excavations comprise the new unit, the lower contact being at 625 feet A.T. on the south quarry face (Fig. 3). Other excellent exposures of this interval occur at: highway cuts on both north and south banks of Green River along Interstate Highway 65, 2.4 miles west-southwest of Munfordville; at the Pace Quarry, 5.5 miles north-northwest of Glasgow; at the abandoned McLellan Quarry, 4 miles east-northeast of Bowling Green, where the base is 50 feet above the quarry floor and the top is at 93 feet; and at the Hoover Quarry, 2 miles northeast of Park City. These shallow water shelf deposits constitute a completed depositional cycle, beginning just above a dolostone at the top of the preceding unnamed unit in the St. Louis, and ending with ghost dolostone, dolomicrite and microsparite. The Horse Cave Member has remarkably uniform characteristics over the area of exposure from central Indiana, via the Pennyrile into western Kentucky (see also McGrain 1969). Complete series of thinsections are available for this interval at five localities. Ten more such series are in various stages of completion, and will allow comparisons for more than 400 miles of extent, west to the type areas of the St. Louis and the Ste. Genevieve Formations. Such series are parts of the standard and com- parative collections. The member terminates throughout its occurrence with stromatolite-associated dolostone and bedded and disseminated ter- rigenous material. Its upper limit marks the viable extinction, although perhaps not the final occurrence in this part of the world, of the foraminifer genus Eoendothyranopsis Reitlinger 1966, and the dasyclad algal genus Koninckopora Lee 1912 emend. Wood 1942. Three species of the latter are present in the study area. Both taxa may occur as contaminants later than the St. Louis. In view of their awesome proliferation, and their abundance in loosely-bound sediment, it would be surprising not to find contamnation in later deposits. Calcarenites and lithoclast-containing beds later than the St. Louis should be particularly suspect if remains of these forms seem to be present. Eoendothyranopsis is not found outside of the confines of the St. Louis Formation, as here defined for south-central Kentucky; although it is reported elsewhere in beds ranging in age from Upper Tournaisian (?=Keokuk) through the Meramecan Series (Reitlinger 1966, Mamet 1968a & b). Ste. Genevieve Deposits. Upward there are present, generally well de- limited, representations of various membrs into which the column is presently subdivided elsewhere. Each has its distinctive characteristics. The local Ste. Genevieve Formation consists of the Fredonia Limestone (type in western Kentucky), Spar Mt. Member, Karnak Limestone, Joppa Lime- stone and the Aux Vases equivalent (types in southern Illinois and Mis- souri). Although their differentiation as units is clear, relationships to the ideal depositional model have not, as yet, been determined. Significant time limitation is indicated for the distinctive colonial coral 10 E. R. Pohl DEPOSITIONAL ZONES (after IRWIN 1965) x|_Y. IT REGRESSIVE- ~ = i =< > UPPER 6 INCHES. “COLOR BREAK” AT BASE, ORGANISM-REWORKED, SPICULAR BIOMICRITE WITH SOME RHOMB REPLACEMENT OF MATRIX, GRADING ABOVE TO GALCAR- ENITIC, PACKED BIOSPARITE. IRREGULAR OOSPARITE ——-—-—— KONINCKOPORA INCLUSIONS. SCRAGGLY BLACK CHERT IN LOWER ! FOOT. MEDIUM GREY, UNPACKED, UNSORTED ALGAL-LEACHED BRYO-ECHINO-BRACHIO BIOSPARUDITE, WITH UP TO 60% CALCISILTITE MATRIX IN PARTS AND UP TO 15% MATURE OOLITHS IN OTHER PARTS. SOME LITHOCLASTS AND VERY LARGE ECHINOID SPINES. SOME DISSEMINATED RHOMBS AND QUARTZ SAND IN UPPER 6 INCHES. FINE GRAINED, COATED-GRAIN SPARITE, MATURE OOLITHS INCREASING FROM l!0% BELOW TO 80% | | | I | ! I 1 ! I | I | | ABOVE, ALONG WITH SOME INCREASE IN COARSENESS OF SKELETAL — FOENDOTHY RANOPS/S ELEVATION= 624.9 aT. » WELL-SORTED, LAMINATED AND MILLIMETER-VARVED, FINE AND MEDIUM GRAINED BIOCALCARENITE WITH SPAR MATRIX, AND BIOPELSPARITE. MUCH SCRAGGLY AND LENTICULAR, FORAM-BEARING GHERT BELOW; SPICULAR CHERT LENTIGLES AND STRINGERS ABOVE. POHL 69 QUARRY FLOOR 1969 Fig. 3. Measured Section of Type Locality of Horse Caye Member of St. Louis Formation. Hart Stone Co. Quarry, 1,926,150 ft. E. 308,300 ft. N., Ky. Coord. Syst., S. Zone; Horse Cave Quadrangle, Kentucky. Upper Mississippian Deposits ll -Siphondendron genevievensis Easton (Lithostrotion harmodites of the literature). It has been found only in beds at the position of the Joppa Limestone, which in this area ranges in thickness from six to 12 feet. This fossil is widely distributed geographically and is, therefore, an excellent marker. Elsewhere this form has been reported from beds above and below those equivalent to the Joppa, but such occurrences lack authentica- tion (see Malott 1952, Swann 1963). Ste. Genevieve—Girkin Contact. No unified opinion is as yet available for the characteristics of the beds at this horizon. Several widely various criteria have been developed: 1—no definitive criteria (Miller and S. Moore 1967); 2—limestone and breccia in the upper beds of a _ three-part depositional cycle (Sandberg and Bowles 1965); 3—at or above the last occurrence of Platycrinites and/or Siphonodendron genevievensis Easton (F. Moore 1965, Haynes 1962, S. Moore and Haynes 1967, Shawe 1963, Rainey 1964, Klemic 1963a, Rainey 1965); 4—above last oolite with Platycrinites (Haynes 1964a); 5—at the top of distinctive lithology (which, in the present study, is identified with the Aux Vases) (Haynes 1965); 6—above beds with Platycrinites and below “lowest geode-bearing” bed of Girkin (Klemic 1963b); 7—Siphonodendron in upper 60 feet of the Ste. Genevieve (Richards 1964, Haynes 1966); 8—cherts and quartz clusters in lower part of the Girkin (Haynes 1966); and 9—below beds with Lithodrumus veryi Greene (and Talarocrinus) (F. Moore 1965, Gilder- sleeve 1963, Rainey 1963). Pre-Elwren Girkin Deposits. The limestone sequence, locally, continues, with only very minor amounts of terrigenous contamination through beds identified with the Paoli Limestone, Mooretown = Bethel sandy Limestone, the Beaver Bend Limestone, the Sample Member, and the Reelsville Limestone. Type localities for these beds are in southern and central Indiana except for the Sample, originally described in Kentucky. All of these horizons are identified on the basis of stratigraphic position, lithology, and gross paleontology. Details of study have begun, and comparative type- locality thinsections are in preparation. The fasciculate coral, Lithodrumus veryi Greene (Campophyllum gasperense Butts), appears to have a remarkably short range and can nearly always be disclosed in the pertinent part of exposures. Locally, it is restricted to beds equivalent to the Beaver Bend Limestone, and is especially abundant in its upper one-third. Elwren—Beech Creek Deposits. The term Elwren is used here as a matter of convenience and as a facies term. Nowhere in the study area does this interval present any true sandstone such as makes up the probably equivalent Cypress in the latter’s type locality in Illinois. The Elwren, however, in its type area in central Indiana is made up in large part of shales, and there are also some associated limestones (Malott 1952: 25). These characteristics are more descriptive of the local pertinent interval. No paleontological criteria are presently conclusive for the local Elwren and Beech Creek deposits. It is now known that the productid brachiopod 12 E. R. Pohl Inflatia inflata (McChesney) appears as early as mid-Fredonia. It is then periodically and commonly present throughout the sequence to its heyday in the uppermost Girkin beds. In the study area it takes on features of a favorable-facies explosion in biostrome accumulations and thanatocoenoses. Contrarily, it is uncommon in central Indiana. Another brachiopod, Martina contracta (M. & W.), often referred to as a diagnostic feature of the Beech Creek and which is extremely abundant in its type area in Indiana (Malott: 14), is rare or wanting in most comparable deposits in southern Kentucky. Two foraminifer genera, Climacammina Brady 1873 and Neoarchaediscus Maclay 1956 are notably abundant in the middle beds of the type-area Beech Creek and in comparable beds near Slade, Ken- tucky. In spite of similarities in lithology, strata occupying the same position in southern Kentucky are nearly lacking in these forms, except for localized swarms of Neoarchaediscus, other Asteroarchaediscins and the incertae alga Girvanella. The local Beech Creek basal beds are oosparitic in character and the higher beds follow the pattern displayed in a typical cyclic sequence of the area model. Post-Girkin Deposits. With the introduction to this area of quantities of coarse terrigenous clastics in Fraileys-Big Clifty time, less difficulty is en- countered in correlating mid- and late Chester shale-sandstone-limestone alternations with similar beds at the originally described localities, up through the Vienna Limestone. Detailed investigation of the Leitchfield Shale of the area has not been undertaken so far. The Upper Mississippian Limestone Sequence. Deposits of the entire Upper Mississippian limestone sequence, from the Ullin to the Beech Creek, are lithologically and constituently dissimilar to those of the com- parable type localities, in some cases. Thus, it may be desireable to apply new, local member names and descriptions, where a particular succession of events of a rhythmic or cyclic nature, over a significant areal extent, justifies such treatment. It would be even more desireable to evaluate the carbonate units, so far described, in a basin-wide framework, and to develop a uniform model for depositional environment and process con- tinuity. Summary Mississippian deposits upward from the base of the Ullin Formation are discussed for south-central Kentucky. A depositional model for the car- bonates is developed. Physical and biological criteria for units and contacts are compared. A new stratigraphic unit, the Horse Cave Member of the St. Louis Formation is proposed, described, and criteria for its identification and limits are offered. The foraminifer genus Eoendothyranopsis is identified with the St. Louis Formation, and the extinction, locally, of the algal genus Koninckopora is shown to occur toward the end of this unit. Aims are out- lined for a continuing study of basin-wide depositional environments within a suitable model. Upper Mississippian Deposits 13 Literature Cited Armstrong, A. K., 1967. Biostratigraphy and Carbonate Facies of the Mississippian Arroyo Penasco Formation, North-Central New Mexico. N. Mex. Inst. Min. & Tech., Mem. 20: 1-80. Born, K., 1943 in McFarlan, A. C., 1943. Geology of Kentucky. Univ. Ky.: 78. Cattermole, J. M., 1965. Geology of the East Fork Quadrangle, Kentucky. U. S. Geol. Surv. GQ-413. Cattermole, J. M., 1966. Geologic Map of the Sulphur Well Quadrangle, Metcalfe and Green Counties, Kentucky. U. S. Geol. Surv. GQ-555. Folk, R. L., 1959. Practical petrogaphic classification of limestones. Bull. Am. Assoc. Petrol. Geol., vol. 43: 1-38. Gildersleeve, B., 1962. Geology of the Polkville Quadrangle, Kentucky. U. S. Geol. Surv. GQ-194. Gildersleeve, B., 1963. Geology of the Bristow Quadrangle, Kentucky. U. S. Geol. Surv. GQ-216. Haynes, D. D., 1962. Geology of the Park City Quadrangle, Kentucky. U. S. Geol. Surv. GQ-183. Haynes, D. D., 1963. Geology of the Lucas Quadrangle, Kentucky. U. S. Geol. Surv. GQ-251. Haynes, D. D., 1964a. Geology of the Glasgow North Quadrangle, Ken- tucky. U. S. Geol. Surv. GQ-339. Haynes, D. D., 1964b. Geology of the Mammoth Cave Quadrangle, Ken- tucky. U. S. Geol. Surv. GQ-351. Haynes, D. D., 1965. Geology of the Hiseville Quadrangle, Kentucky. U.S. Geol. Surv. GQ-401. Haynes, D. D., 1966. Geology of the Horse Cave Quadrangle, Barren and Hart Counties, Kentucky. U. S. Geol. Surv. GQ-558. Hopkins, T. C. and C. E. Siebenthal, 1896. The Bedford Oolitic Lime- stone of Indiana. Indiana Dept. of Geol, Ann. Rept. 21: 289. Irwin, M. L., 1965. General Theory of Epeiric Clear Water Sedimentation. Bull. A. A. Petrol. Geol. 49 (4): 445-459. Kepferle, R. C., 1966. Geology of the Elizabethtown Quadrangle, Hardin and Larue Counties, Kentucky. U. S. Geol. Surv. GQ-559. Kepferle, R. C., 1967. Geology of the Vine Grove Quadrangle, Hardin and Meade Counties, Kentucky. U. S. Geol. Surv. GQ-645. Ketner, K. B., 1962. Geology of the Scottsville Quadrangle, Kentucky. U. S. Geol. Surv. GQ-184. Klemic, H., 1963a. Geology of the Rhoda Quadrangle, Kentucky. U. S. Geol. Surv. GQ-219. Klemic, H., 1963b. Geology of the South Union Quadrangle, Kentucky. U. S. Geol. Surv. GQ-275. Lineback, J. A., 1966. Deep-Water Sediments Adjacent to the Borden Siltstone (Mississippian) Delta in Southern Illinois. Ill. Geol. Surv., Cir. 401:29-35. 14 Ey RaPont Malott, C. A., 1952. Stratigraphy of the Ste. Genevieve and Chester Formations of Southern Indiana. Edwards Letter Shop, Ann Arbor, Mich.: 8, 9, 34, 58, 98. Mamet, B. L., 1968. Foraminifera, Etherington Formation (Carboniferous), Alberta, Canada. Bull. Can. Petrol. Geol. 16 (2): 167-179. Mamet, B. L. and D. Mason, 1968. Foraminiferal Zonation of the Lower Carboniferous Conner Lakes Section, British Columbia. Bull. Can. Petrol. Geol. 16 (2): 147-166. McFarlan, A. C., 1943. Geology of Kentucky. Univ. Ky., 77. McGrain, P., 1969. Extension of Lost River Chert Across Parts of Kentucky. Bull. A. A. Petrol. Geol. 53 (7): 1506-7. Miller, R. C. and S. L. Moore, 1967. Geology of the Center Quadrangle, South-central Kentucky. U. S. Geol. Surv. GQ-693. Miller, R. C., 1969. Geology of the Canmer Quadrangle, Hart County, Ken- tucky. U. S. Geol. Surv. GQ-816. Moore, F. B., 1965. Geology of the Millerstown Quadrangle, Kentucky. U. S. Geol. Surv. GQ-417. Moore, F. B., 1966. Geologic Map of the Tonieville Quadrangle, Larue and Hardin Counties, Kentucky. U. S. Geol. Surv. GQ-560. Moore, F. B., 1968. Geology of the Hodgenville Quadrangle, Larue and Nelson Counties, Kentucky. U. S. Geol. Surv. GQ-749. Moore, S. L., 1963a. Geology of the Allen Springs Quadrangle, Kentucky. U. S. Geol. Surv. GQ-285. Moore, S. L., 1963b. Geology of the Drake Quadrangle, Kentucky. U. S. Geol. Surv. GQ-277. Moore, S. L., 1968. Geology of the Exie Quadrangle, Green County, Kentucky. U. S. Geol. Surv. GQ-752. Moore, S. L. and D. D. Haynes, 1967. Geologic Map of the Park Quad- rangle, South-central Kentucky. U. S. Geol. Survey. GQ-634. Moore, S. L. and R. C. Miller, 1965. Geology of the Glasgow South Quadrangle, Barren County, Kentucky. U. S. Geol. Surv. GQ-416. Myers, W. B., 1964. Geology of the Petroleum Quadrangle, Kentucky- Tennessee. U. S. Geol. Surv. GQ-352. Nelson, W. H., 1963. Geology of the Meador Quadrangle, Kentucky. U. S. Geol. Surv. GQ-288. Peterson, W. L., 1966. Geology of the Nelsonville Quadrangle, Kentucky. U. S. Geol. Surv. GQ-564. Pohl, E. R., R. G. Browne and J. R. Chaplin, 1968. Foraminifera of the Fraileys Member (Upper Mississippian) of Central Kentucky. J. Pal., 42, (2): 581-2. Rainey, H. C., 1963. Geology of the Hadley Quadrangle, Kentucky. U. S. Geol. Surv. GQ-237. Rainey, H. C., 1964. Geology of the Rockfield Quadrangle, Kentucky. U. S. Geol. Surv. GQ-309. Rainey, H. C., 1965. Geology of the Auburn Quadrangle, Kentucky. U. S. Geol. Surv. GQ-415. Upper Mississippian Deposits 15 Reitlinger, E. A., 1966. Some Classification Questions and the Evolute Endothyrins and Primitive Fusilins. Vopros’ Mikropaleontologii, Acad. Nauk SSSR, Issue 10: 39-70. Richards, P. W., 1964. Geology of the Smiths Grove Quadrangle, Ken- tucky. U. S. Geol. Surv. GQ-357. Sable, E. G., R. C. Kepferle and W. L. Peterson, 1966. Harrodsburg Limestone in Kentucky. U. S. Geol. Surv., G. S. Bull. 1224-I: I1-112. Sandberg, C. A. and C. G. Bowles, 1965. Geology of the Cub Run Quadrangle, Kentucky. U. S. Geol. Surv. GQ-386. Shawe, F. R., 1963. Geology of the Bowling Green North Quadrangle, Kentucky. U. S. Geol. Surv. GQ-234. Swann, D. H., 1963. Classification of Genevievian and Chesterian (Late Mississippian) Rocks of Illinois. Ill. Geol. Surv., RI 216: 73. Swann, D. H., J. A. Lineback and E. Frund, 1965. The Borden Siltstone (Mississippian) Delta in Southwestern Illinois. Ill. Geol. Surv., Cir. 386. Swinchatt, J. P., 1969. Algal Boring: A Possible Depth Indicator in Carbonate Rocks and Sediments. Bull. Geol. Soc. Am., v 80: 1391. Received: July 8, 1969. Accepted: October 14, 1969. THE HISTORY OF ANTHROPOLOGY DEPARTMENTS IN KENTUCKY UNIVERSITIES LOUISE M. ROBBINS, Editor Department of Anthropology University of Kentucky Lexington, Kentucky 40506 The early teaching of anthropologically-oriented courses was long sporadic in the leading institutions of higher learning in Kentucky. The material presented tended to be a reflection of the special interest of the presiding instructor and pertained in a general fashion to the discipline he represented, whether it be history, sociology, psychology, etc. Few of the early instructors had formal training in anthropology, and they were less likely to convey the particular emphasis given to the study of man than would be given by the professional anthropologist. It was comparable to reading a novel with some major informative chapters omitted, to take those early courses. In recent years, an increasing institutionalization of anthropology departments occurred in several Kentucky universities. Professionally trained personnel has been hired to design and teach the curriculum of the newly-formed departments. So much time and energy was directed toward the development of adequate study programs in anthropology that the professional anthropologist had little time for interaction with his col- leagues at other schools in the state. In an effort to decrease this isolation, several interested anthropologists suggested that application be made to the Kentucky Academy of Science in 1967 for the establishment of an Anthropology Section in the Academy. The application was accepted, and the Anthropology Section met formally for the first time the following year with Henry F. Dobyns of the University of Kentucky serving as Chairman, and Louise M. Robbins of the same institution acting as Secretary. Since the first session was of historical note for the profession in Ken- tucky, it was deemed appropriate that the papers presented should emphasize the historical development of the discipline in the state. Few anthropology departments, and other academic departments, for that mat- ter, make an effort to record their historical development, and as a result contribute nothing to the history of science, especially in the United States. One of the few anthropology departments that has published even a short history of itself is the one in the London School of Economics and Political Science, University of London.1 The papers reproduced here record the history of anthropolgy depart- ments in three Kentucky universities. Anthropological beginnings at other schools were discussed in the Anthropology Section meeting, since the subject is also taught at’ Eastern Kentucky State University, Western Kentucky State Vevey and in several of the Community Colleges of History of Anthropology Departments iy the University of Kentucky system. It is notable that each contributor as- sesses the development of a department in terms of the emphasis placed upon anthropology in his or her school at a given period of time. Con- sequently, the course programs of the different departments are not replications of each other, which is at it should be if the discipline as a whole is to continue growing. The authors of these three histories are eminently qualified by their key roles in departmental development to write their sketches. Dr. Cara E. Richards, the first professional anthropologist at Transylvania University, received her doctorate from Cornell University in 1957. Her research interests center around the ethnohistory of the American Indians, particularly the Iroquois,” the effects of cultural change in Peru,* and the study of inter-ethnic relationst and urban social patterns® in complex societies. Dr. Frank J. Essene, former Head of the University of Kentucky anthro- pology department, received his Ph. D. from the University of California at Berkeley in 1947. His research has dealt mainly with the ethnology of American Indians with special emphasis on California® and the Navajo of the American Southwest.? Dr. Frederic N. Hicks received his doctorate from the University of California at Los Angeles in 1963. He is considered a Latin Americanist among anthropologists since his interest and research are in cultural changes in contemporary Latin America.’ In keeping with his areal specialization, he taught for a year at the National University of Paraguay as a Fulbright Lecturer, stimulating anthropological research there.? He also specializes in ecological anthropology.!° References 1. Firth, Raymond, “A Brief History (1913-1963),” Programme of Courses, The London School of Economics and Political Science, Department of Anthropology. London, 1967-8. pp. 1-7. 2. Richards, Cara E., “Matriarchy or Mistake: The Role of Iroquois Women through Time,” in Cultural Stability and Cultural Change. Proceedings of the 1957 Annual Spring Meeting of the American Ethnological Society, pp. 36-45. 3. Stycos, J. Mayone and Cara E. Richards, “Fuentes de la Migracion a la Gran Lima,” in H. F. Dobyns y M. C. Vazquez, (eds.) Migracion e Integracion en el Peru. Lima: Editorial Estudios Andinos, 1963, pp. 37-44. 4, Richards, Cara E., “Cooperation Between Anthropologist and Medical Personnel,’ Human Organization, 19:2 (Summer 1960) 64-67; “Modern Residence Patterns Among the Navajo,” El Palacio, (Spring- Summer 1963) 25-33. 5. Richards, Cara E., “City Taverns,” Human Organization, 22:4 (Winter 1963-64) 260-268; C. E. Richards & H. F. Dobyns, “Topography and 18 10. Louise M. Robbins Culture: The Case of the Changing Cage,” Human Organization, 16:1 (Spring 1957) 16-20. Frank J. Essene, W. Goldschmidt & E. M. Foster, “War Stories from Two Enemy Tribes,” Journal of American Folklore, 52 (1939) 141- 154. F. J. Essene, Culture Element Distributions: 21, Round Valley. Univ. of Calif. Anthropological Records, 8:1, 1942. F. J. Essene and G. A. Hillery, “Navajo Population: An Analysis of the 1960 Census,” Southwestern Journal of Anthropology, 19:3 (1963) 297-313. Frederick Hicks, “Politics, Power, and the Role of the Village Priest in Paraguay,” Journal of Inter-American Studies, 9:2 (April 1967) 273-282. Frederick Hicks y Egidio Picchioni, “Algunos aspectos de la in- dustrialization en una comunidad paraguaya,” Revista del Ateneo Paraguayo, Suplemento Antropoldgico, 2:1 (Dic. 1966) 31-54. Frederick Hicks, “La Etnobotanica y el Estudio de la Ecologia Cul- tural,” Revista del Ateneo Paraguayo, Suplemento Antropodgico, 1:1 (Set. 1955) 15-25. I. ANTHROPOLOGY AT TRANSYLVANIA CARA E. RICHARDS & L. A. BROWN Transylyania University Lexington, Kentucky 40508 In the late 1700’s interest in American Indians was not limited to antiquarians, missionaries or other precursors of modern anthropologists. The subject was of considerable importance to military men and. business men—especially those involved in fur trade and land speculation. It was also a topic of considerable interest to the average layman. In Kentucky, which for some years after the founding of Transylvania University remained frontier territory, interest in Indians was far from academic. Perhaps for this reason no courses in Indian lore or antiquites were offered during the earliest period of Transylvania’s growth. Following the pattern of most institutions of higher learning at the time, attention at Transylvania was focused on classical subjects. A typical curriculum of the early part of the 19th century (1824) offered Greek, Latin, Grammar, Logic, Rhetoric, Declamation and Ethics along with Mathematics, History, Chemistry, Astronomy and in the Senior year Forensics and Political Economy. Professors at Transylvania University on the other hand had diverse interests, and the limited course offerings did not prevent individuals from pursuing those interests outside the University, nor did it interfere with their publishing articles that today might be thought appropriate for inclusion in an anthropological journal. Constantine Samuel Rafinesque was one of the more prolific early Transylvania professors who became involved in what would today be anthropological research. He was a naturalist with broad interests that included archeology, physical anthropology (he theorized about evolution), ethnology and linguistics. Rafinesque’s first article of record, published after he joined the Transylvania faculty, on what today would be considered an anthro- pological topic was “On a remarkable ancient monument near Lexington.” This appeared in a Lexington magazine in December of the same year he came to Transylvania, 1819.1 He followed this up with two other archeological articles in the same journal in May and August of 1820. In 1824 Rafinesque published several articles in the Cincinnati Literary Gazette. Most were on archeological topics, but two were ethnological. One dealt with “Nazahual, the Nabijos and Comanchees,”? and the other was a “Biography of the American Solomon.”? One was on a linguistic topic. An exhaustive bibliography of Rafinesque’s works published in Fitzpatrick’s biography of Rafinesque lists scores of such publications.® From descriptions of Rafinesque’s character, it is probably safe to assume he did not confine his opinions on these subjects to his publications but discussed them at length with students, colleagues, and anyone else who would listen. Anthropology at Transylvania therefore probably dates at least from the appearance of Rafinesque on the faculty in 1819. 20 Cara E. Richards and L. A. Brown Rafinesque was not the only Transylvanian interested in anthro- pological matters. A museum, of which the present one is the lineal descendant, was started by Regent J. B. Bowman about 1866 or 1867. Housed in the old Henry Clay home of Ashland for several years, it then moved to Morrison Hall and finally to the present science building when it was built in 1908. The first active curator was Professor Alexander Win- chell who divided his time between the University of Michigan and Ken- tucky University (which was the name of Transylvania between 1865 and 1908). The acquisition of Indian relics by the museum is first mentioned in the University records in 1870 when some were given to the college by Daniel Boothe. Gifts and purchases continued actively at least until the turn of the century. Unfortunately when the museum collections were moved from the first floor of the Science building to the attic in 1933 or 1934, essential records were misplaced. When (and if) the Ledger of Ac- quisitions and the record books of Professor Winchell and his successors are located, more detailed information will be available. In 1969 there was a fairly extensive collection of Indian artifacts in the museum that was uncatalogued and not on display. The first formal course offering of Anthropology appears much later in Transylvania’s history. Robert Peter’s history of the school during the period from the founding in 1780 up to 1865 makes no mention of any offerings in anthropology.® There is also no mention of an anthropology course in Peter’s history of the medical department which covers the period from 1799 to 1857.7 A sampling at five year intervals of the catalogues of Kentucky University does not reveal any offerings in anthro- pology either. The first mention of a course offered after 1908 when Transylvania resumed its present name is in the 1925-26 catalogue. It states: “Sociology 431, Anthropology (not offered in 1926-27).” The 1926-27 catalogue describes an anthropology offering as follows: Sociology 431. Cultural anthropology. A brief survey of physical an- thropology is followed by a study of the social and mental life of pri- mitive men, his economic and industrial activities, his science, magic, and religion, his ethics, social organization, and culture. Prerequisite, Sociology 260 and six additional hours. First semester, three hours. This course was listed through 1935-36, when 21 students enrolled. The 1936-37 catalogue did not list an anthropology course, but one reap- peared with the same description in the 1937-38 catalog. Anthropology apparently dropped out of the curriculum in the wartime academic year 1941-42. Records indicate that 39 students took a course in anthropology in the Spring quarter of 1950-51. A five quarter-hour course reappeared in the biennial catalogue for 1953-55, listed as “Sociology”. Beginning with the Fall quarter of 1954-55, the five credit hour anthropology course taught as “Sociology 226” was taught by Arnold Foster, an Assistant Professor of Sociology. From then on a course has been offered regularly, although sometimes in alternate years. In 1955-56 anthropology became “Sociology 126.” Arnold Foster taught “Sociology 126” until the Winter quarter of Anthropology of Transylvania 21 1964-65 when the course assumed its present designation, “Sociology 242”. Bruce H. Mayhew, a temporary appointment from the University of Kentucky, taught it that quarter. The following year Dr. Joyce Query taught the course and the year after that Mr. Joseph Mouledous. Since the Fall quarter of 1967, “Sociology 242” has been taught by Dr. Cara E. Richards, the first professionally trained anthropologist employed by Transylvania, at least in recent years.8 Since the academic year 1954-55, the number of students enrolled has varied from eleven in 1954 to approxi- mately 60 each in 1968 and 1969. A second course in anthropology was added in the Spring quarter of 1968. This “Sociology 341” course for four credits is labeled “Advanced Anthropology”. It provides students with an examination of current theoretical and research interests with emphasis on the relevance of anthropological concepts and data to modern world and national prob- lems. Through the Board of Curators, the university has expressed an interest in strengthening the fields of Sociology and Anthropology. In the light of this interest, a third course offering in anthropology—“Development of Man’—was added to the university curriculum beginning in the Fall Quarter of 1969. At the same time, the university instituted an “Inter- Cultural Studies” major which includes anthropology among its require- ments. Literature Cited 1. Rafinesque, Constantine, S., 1819, “On a remarkable ancient monument near Lexington,” Western Review and Miscellaneous Magazine, 1:313- 314. 2. Rafinesque, Constantine S., 1824b, “On Nazahual, the Navajos and Comanchees,’ Cincinnati Literary Gazette, 1:26 (26 June) 202. 3. Rafinesque, Constantine S., 1824a, “Biography of an American Solomon,” Cincinnati Literary Gazette, 1:22 (29 May) 170. 4. Rafinesque, Constantine, S., 1824c, “On the Panis Language and Dialects,” Cincinnati Literary Gazette, 2:7 (14 August) 50-51. 5. Fitzpatrick, T. J., 1911. Rafinesque, a Sketch of His Life with Biblio- graphy. Des Moines: History Department of Iowa. 6. Peter, Robert, 1896. History of Transylvania University. Louisville: John P. Morton. 7. Peter, Robert, 1905. History of the Medical Department of Transylvania University. Louisville: J. P. Morton. 8. See editor’s introduction. Her most recent publication is a theoretical article: “Presumed Behavior: Modification of the Ideal-Real Dichotomy,” American Anthropologist, 71:6 (December 1969) 1115-1117. Received: November 25, 1969 Il. ANTHROPOLOGY AT THE UNIVERSITY OF KENTUCKY LEXINGTON CAMPUS FRANK J. ESSENE UNIVERSITY OF KENTUCKY Lexington, Kentucky 40506 The Department of Anthropology and Archaeology was officially estab- lished at the University of Kentucky in 1926. The date is amazingly early and the name of the department oddly redundant. At that time only a few of the larger universities in the United States had independent departments of anthropology. Those that offered anthropology automatically included archaeology as a subdivision of anthropology. The early date and odd title reflect the drive and to a degree the backgrounds of the two men who founded the department, William S. Webb and William D. Funkhouser. Webb was a physicist and Funkhouser a zoologist but both were zealous collectors of arrowheads, among other things. In addition, Webb had once been an employee of the Bureau of Indian Affairs working on the Seminole Reservation in what was then Indian Territory but is now the state of Oklahoma. To over-simplify only slightly, the word “anthro- pology” meant to Webb and Funkhouser the study of living Indians and the word “archaeology” had to do with collecting Indian artifacts, primarily arrowpoints. William S. Webb was a powerful figure on the University of Kentucky campus. He served for many years as Head of the Department of Physics and one of his well-earned nicknames was “Bull neck”. William D. Funk- houser similarly headed the Department of Zoology, for a long period of time. He was also the first Dean of the Graduate School, and for a time Chairman of the Southeastern Athletic Conference. Both were native Ken- tuckians with impeccable lines of ancestors. Together they could apply enough force not only to create a new department but to shape its course for many years to come. The subsequent history of anthropology at the University of Kentucky fits neatly into successive 10 year time spans. Each decade had a different color and emphasis. To a large extent, U.S. anthropology in general went through much the same stages as this department, but over a much longer period of time. It should delight some scientists to recognize that ontogeny once again recapitulates phylogeny. The Age Of Innocence (1926-1935) The first decade of anthropology at the University of Kentucky was a period of Simon-pure amateurism. Webb and Funkhouser were paid their salaries and had their primary duties in the Departments of Physics and Zoology respectively. Webb also had an unpaid co-appointment as Pro- fessor and Head of the Department of Anthropology. Funkhouser was co- appointed Professor of Anthropology, also without salary for these ad- Anthropology at the University of Kentucky 23 ditional duties. Funkouser developed and taught a number of highly idiosyncratic anthropology courses while Webb was the administrator. They used week-ends and vacation periods to excavate Indian sites, often en- listing students and friends as “voluntary” laborers. Sometimes, they even paid a local: individual to plow upper surfaces of mounds and _ haul away quantities of dirt. Descriptions of excavations and artifacts recovered were published. In 1928, their first full-length monograph, Ancient Life in Kentucky appeared as Vol. 34 in the Kentucky State Geological Survey series. In 1929, they started the University of Kentucky series entitled Reports in Archaeology and Anthropology. In the last year of the department’s first decade, the first degree in Anthropology was granted by the University of Kentucky. Strangely enough, it was a Master’s degree but more predictably the thesis dealt with Kentucky Archaeology. The Epoch Of Creeping Professionalism (1936-1945) The Great Depression was at its midway point when policies aimed at reducing unemployment gave a big boost to anthropology. The U. S. government began providing funds to employ men on relief rolls, pre- ferably in projects not competing in any way with private industry. Dig- ging up the remains of dead Indians competed with no industry and Ken- tucky, along with several other states, was soon the scene of large scale excavations. William S. Webb was soon in over-all charge of such projects not only in Kentucky but also throughout the Tennessee valley. His pro- ject supervisors and higher-level technicians did not have to come from relief rolls but were mostly young professionally-trained anthropologists. Webb learned a good deal of anthropology from these young professionals. The ones he liked best he moved from field projects to work with excavated materials brought to the Lexington campus. The next step was to give regular staff appointments to these young men, when possible including regular university salaries. In this manner, Charles E. Snow and William G. Haag were added to the university staff. Anthropology first was assigned space on campus during this decade, enough for Museum display rooms, offices, storage, and research areas. The University Library had moved into a new building and its old building was grabbed by Webb and Funkhouser in a typical power play. This building remained the center of many anthropological activities till it was demolished in 1967. Symptomatic of Webb’s increasing sophistication were two changes in title. The Department of Anthropology lost its useless last two words “and Archaeology.” The University of Kentucky series was similarly changed to Reports in Anthropology. The only degrees granted were three B.A.’s in Anthropology in 1941 and 1942. World War II activities then forced a virtual end to all anthro- pological activities. 94 Frank J. Essene Poverty-Stricken Professionalism (1946-1955) The department’s third decade began with Webb still firmly in control as the Department Head and Funkhouser teaching his own peculiar brand of anthropology, but, Snow and Haag began to take over most of the classes. Frank J. Essene was hired in 1947, the last year that Funkhouser was teaching. Funkhouser died in 1948, which meant a loss to the depart- ment in campus power but a gain in professionalism. Haag resigned in 1948 and was replaced by Richard Woodbury who in turn was suceeded in 1952 by Raymond H. Thompson. Thompson also resigned at the end of the decade. Haag, Woodbury, and Thompson were archaeologists and their relatively short stays on campus resulted at least partially from conflicts with Webb over archaeological doctrine. Webb continued as department head till 1952 when Snow took over. Webb was 70 years old in 1952 but, far from retiring, he simply went into archaeology on a full-time basis. (1) (2) An adequate curriculum leading to the BA and MA degrees in Anthropology was developed near the beginning of the decade. Large lectures were the rule for beginning classes with advanced classes quite small and often conducted like seminars. Some 17 students received bachelor’s degrees in anthropology and 2 master’s degrees were granted. Despite the large enrollments and variety of courses, no more than 3 professors were teaching anthropology at any time. There were no graduate assistants and at best only one part-time secretary. In addition to normal duties the faculty sometimes taught off-campus, handled evening classes, and prepared and graded correspondence lessons. All these helped to eke out the low salaries characteristic of the time. The professionals had won, but with Webb’s retirement the department lost the last of its potent amateur boosters. Opportunistic Expansion (1956-1965) The year of 1956 witnessed many firsts in the department. It hired its first full-time secretary, appointed its first graduate assistant, obtained ap- proval for the first non-staff member to teach evening classes, and signed the first of many archaeological research contracts with the National Park Service. Douglas W. Schwartz was added to the staff in 1956 and proved to be something of a genius in obtaining contracts that in turn often paid for additional personnel.? Frank J. Essene was first Head and then Chair- man for the ten years. Four anthropologically-trained persons in other departments were given co-appointments in anthropology. Donald Hoch- strasser, Marion Pearsall, John Barrows, and Kenneth Harper each taught 1 or 2 anthropology courses per year. George P. Faust transferred from English to Anthropology in 1962 to bring the full time staff up to 4. Following this break through, Art Gallaher, Louise M. Robbins, Margaret Lantis, and Martha A. Rolingson were also added to the staff while Charles E. Snow transferred to the College of Medicine. The number Anthropology at the University of Kentucky 25 of graduate student assistants increased to 6 and a second secretary was hired. More courses were drawn up and all classes were offered more frequently. Only 16 Bachelor of Arts degrees were awarded in Anthropology, a decline of one from the previous period. Masters degrees increased to 14, on the other hand, indicating a new emphasis on graduate education. This trend also appeared in systematic attempts to obtain approval for starting a doctoral program. These efforts were not successful then but bore fruit early in the next period. The series published at Lexington, Reports in Anthropology, was dis- continued and a new series Studies in Anthropology was established by the University of Kentucky Press. Changes in both format and content were involved. Near the end of 1965, arrangements were made to move the entire editing and printing of Human Organization, the journal of the Society for Applied Authropology, to our campus under the editorship of _ Marion Pearsall. Florescence And Future (1966-1975) The first 4 years of the fifth decade are nearly complete. Henry F. Dobyns came to our department as professor and chairman in 1966. Wil- liam Y. Adams also joined the department that year. In 1967, the depart- ment lost Douglas W. Schwartz but added Albert Bacdayan. In 1968, Martha Rolingson resigned but Philip Drucker joined the staff. The number of graduate assistants increased each year. During the fall semester 1968, eleven graduate students in anthropology had assistantships and three were on fellowships. A third secretary worked for the department. A program leading to the Ph.D. in anthropology had been approved by the University administration. A complete revision of the curriculum was in process with many new courses, particularly on the graduate level, being added. An image of the department as a center for applied anthropology was growing in the profession, to which Human Organization, contributes since it is both edited and published on campus (4). In the 3 years 1966-1968, 14 Bachelor and 4 Masters degrees have been awarded. Within a few years, one or more Ph.D. degrees will be awarded annually. More new staff will be added particularly at the assistant professor level. Staff turn-over will probably increase and students are likely to become more peripatetic as specialized programs become more numerous throughout the country. Anthropology is expanding generally in the U. S. and Kentucky now has a good chance of becoming one of the major anthropological centers of the nation. Summary of The First 43 Years Anthropology at the University of Kentucky has developed from amateur collecting to full professionalism. An early stress on archaeo- 26 Frank J. Essene logy has been finally succeeded by an accent on applied anthropology. The degrees awarded in anthropology have been distributed as follows: Persons receiving only BA 43 Persons receiving BA and MA i Persons receiving only MA 14 TOTAL 64 Ten of these 64 persons have been awarded the Ph.D. in anthropology elsewhere and are employed as professional anthropologists. Another 6 are also working full-time in-anthropological positions. Fifteen of the 64 are now seeking higher degrees in anthropology at various universities. Three other former students got their first exposure to anthropology at the Uni- versity of Kentucky, received a degree here in another field, and then went on to a Ph.D. in anthropology at other institutions. Kentucky did get its professional anthropology staff from outside but has already more than paid its debt to the profession by training young converts. The development of anthropology in other universities and colleges within Kentucky is at least partially due to influences emanating from the Lexington campus. In a number of cases, former students from the University of Kentucky carried the message to those colleges. In other in- stances, direct assistance in starting anthropology programs has been provided. The net result is that the Commonwealth of Kentucky as a whole has passed many wealthier and more thickly populated states in its interest in anthropology. Annotated Bibliography 1. William G. Haag, “William Snyder Webb, 1882-1964’, Amreican Antiquity 30:4, pp. 470-473, April 1965. A sympathetic obituary stressing Webb's archaeological career and including practically all of Webb's archaeological publications. 2. Douglas W. Schwartz, “Conceptions of Kentucky Prehistory” Studies in Anthropology 6, pp. 1-133, University of Kentucky Press, Lexington, 1967. While other personalities are presented, Webb is the major character covered. Excellent photographs of Webb and his con- temporaries are included. Schwartz evaluates Webb solely on his work in archaeology. 3. Contractors with the U. S. National Park Service for surveying areas to be destroyed by construction projects or inundated by artificial reservoirs financed research that discovered many previously unknown | prehistoric sites in Kentucky, several of them subsequently excavat- ed in the National Park Service archeological salvage program. Supple- mented by other research, these contracts led to the publication of new knowledge of Commonwealth prehistory. See, Lee H. Hanson, Jr., The Hardin Village Site (Lexington: University of Kentucky Press), Martha Ann Rolingson and Douglas W. Schwartz, Late Paleo-Indian and Anthropology at the University of Kentucky Pail Early Archaic Manifestations in Western Kentucky (Lexington: Uni- versity of Kentucky Press), and Martha Ann Rolingson, Paleo-Indian Culture in Kentucky. (Lexington: University of Kentucky Press). 4. Frank J. Essene, “Geographical Distribution of AES Members” American Ethnological Society Newsletter 14, pp. 6-7, October, 1967. Kentucky ranked eleventh of the 50 states in AES members. In addition, Henry F. Dobyns and Essene in an unpublished manuscript show that Ken- tucky ranks well above the average state in several other -anthro- pological societies. Received: November 25, 1969. » Ill. THE GROWTH OF ANTHROPOLOGY AT THE UNIVERSITY OF LOUISVILLE FREDERIC HICKS University of Louisville Louisville, Kentucky 40208 While some anthropology has been taught at the University of Louis- ville since 1946, it was not until 1967 that an undergraduate major in the field was offered. Most of the history of anthropology at Louisville, there- fore, has taken place within the last few years. Anthropology has attracted attention on campus, however, from the time it was first taught in the late 40’s. Or perhaps the attention was at- tracted not by anthropopolgy itself, but by its leading exponent, Ray Birdwhistell. Birdwhistell, apparently the first man to teach anthropol- ogy at Louisville, came to the university in 1946 as a member of the Department of Sociology. His training at the University of Chicago, how- ever, had included a good deal of anthropology. After coming to Louisville, his interests developed still further in that direction, particularly in the field of personality and culture. These interests, Birdwhistell found, could be better satisfied in the Department of Psychology, and he transferred to that department. There, he set up the university's first curriculum in anthropology, and to ac- comodate this innovation, the department was re-named the Department of Psychology and Social Anthropology. This departmental designation was retained until 1967, and the curriculum designed by Birdwhistell remained essentially unchanged until 1965. That curriculum had some unusual features. The introductory course, on a sophomore level, was called “Personality and Culture”, and was re- quired of all psychology majors. “Introduction to Social Anthropology” was a two-semester, junior-level course. In addition, there was a course on “Culture and Mental Illness” and a graduate seminar in social anthropology. To many, the most unusual feature of all was Birdwhistell himself. Those who knew him while he was at Louisville describe him as a dynamic personality, an exciting but controversial lecturer, given, as one professor put it, to “making generalizations in class beyond what the data actually warranted’ —and often about his colleagues and students. Frequently em- broiled in controversy, often dressing in an unorthodox manner, Bird- whistell won a fame for his personality and classroom performances that spread beyond Louisville, and he was once caricatured in Al Capp’s “Lil Abner’. Some of his students were his devoted followers, others disliked him strongly, but he made anthropology, or more specifically “social anthropology”, a familiar word on campus. One of his major achievements was the organization, in 1955, of a conference on culture, Anthropology at the University of Louisville 29 psychology, and linguistics, which brought to Louisville such people as Margaret Mead, S. I. Hayakawa, George Trager and Jerome Frank. Birdwhistell left in 1956, and was replaced by Harold C. Yeager, who held a doctorate from Yale in sociology, but who also had a strong back- ground in social psychology and anthropology. He carried on Birdwhistell’s program, and for a time there was a second anthropologist: Raymond Wilkie, who had doctorates in both anthropopolgy and psychology. Wilkie left after two years, and until 1965, Yeager taught the university’s only “social anthropology” courses. In 1956, the first library building was constructed at the University of Louisville. Previously the university’s “highly selective” book collection was housed in several rooms of the administration building. In 1961, the board of trustees made available $200,000 to remedy deficiencies in library holdings, a good many of which were in anthropology. Largely through the efforts of Dr. Yeager, who was on the senate library committee at the time, complete or nearly-complete sets were obtained of the American Anthropologist, Southwestern Journal of Anthropology, American Antiquity, Africa, Oceania, and some other journals, plus the Human Relations Area Files on microcard. Books were also obtained in greater numbers, and by 1965, a promising start had been made toward building an adequate anthropology library. As might be expected, however, library holdings were best in personality and culture, and became progressively worse as one moved away from this field. In archaeology, for example, they were negligible. In the early 1960’s, the psychology department began to shift its emphasis away from social and clinical psychology and into experimental and laboratory work. The continued presence of “social anthropology” as an appendage of psychology seemed increasingly incongruous, and a decision was made to separate the two disciplines. Yeager set out to re- cruit a second anthropologist, seeking this time someone whose interests were near the anthropological mainstream, rather than an interdisciplinarian. I was hired, and Yeager and I were to form the nucleus of a new and independent department. Before I arrived in Louisville, however, Yeager took a leave of absence to head the local anti-poverty program. He decided to apply for a permanent position with this program, and to increase his chances, he resigned from the university. He did not obtain the anti-poverty position, and when the university re-hired him, it was in the department of sociology. This left me, with no previous departmental administrative experience, with the primary responsibility for building an anthropology department. In the fall of 1966, Edwin S. Segal joined the faculty. Segal, presently a Ph.D. candidate at Indiana University, is an Africanist. The following year, Joseph E. Granger was added. Granger is a Ph.D. candidate at the State University of New York at Buffalo, and his interests are in the archaeology of eastern North America (my own interest is in Latin America). With a faculty of three, we were now able to meet the uni- 30 Frederic Hicks versity requirements for independent departmental status, and in the fall of 1967, the Department of Anthropology was formally established. Library resources and equipment for teaching and research were still deficient, however, and in recent years, more attention has been paid to remedying these deficiencies. Library holdings in anthropology have increased greatly since the decision to establish an independent department. Wayne Yenawine, formerly head librarian at Syracuse University, assumed duties as head librarian at Louisville in 1965. Under his direction, the number of volumes in the university library has practically doubled, complete sets of the major anthropological monograph series and journals have been acquired when available, standing orders have been placed for the publications of all university presses, and a relatively large sum has been allocated each year for other anthropological acquisitions. Today, the major deficiencies are in older works which have not been reprinted. Necessary teaching aids and basic equipment for research have been acquired gradually. A start was made with a National Science Foundation grant for instructional scientific equipment and with university funds. An Archaeological Survey, with close ties to the anthropology department, but formally a part of the Graduate School, was established in 1968, and grants to the survey from federal and state sources, again supplemented by university funds, have made possible the acquisition of equipment for archaeological research. The Survey, under the direction of Joseph E. Granger, has carried out salvage excavations in each of the two summers since its formation. Another slow development has been the awakening of student interest in anthropology, which has been largely a problem of creating an awareness of the nature of anthropology’s subject matter. Despite the local fame which Birdwhistell enjoyed as a person, few people outside the uni- versity were aware of what he taught, so anthropology was still thought of as having something vaguely to do with “old bones”. Overcoming this problem has been.gradual, but encouragaing. Intro- ductory cultural anthropology is now required of majors in psychology and sociology, and majors in a number of other fields are being strongly urged to take it. By dealing with cultural and social anthropology in the first semester of the introductory sequence, leaving physical anthropology and prehistory until the second, we believe the student who takes only one semester of anthropology as an elective will be more likely to get a clearer picture of the field. Finally, an experimental course developed by Segal one summer, in which his course on African cultures was modified, in con- sultation with the directors of the Upward Bound program, to meet the needs of students enrolled in that program, was apparently responsible for the sharp increase in enrollment in that and other non-introductory courses. The department now has a faculty of three, and is hoping to add one or two more in the near future, in order to have a well-balanced under- Anthropology at the University of Louisville 31 graduate program. So long as the university remains relatively small, it is expected that efforts will continue to be toward improving the quality of undergraduate training, and toward providing further opportunities for the professional development of the faculty. Received: November 25, 1969 AN ANNOTATED CHECK LIST OF THE DRAGONFLIES AND DAMSELFLIES (ODONATA) OF KENTUCKY?! PATRICIA LILES RESENER Department of Biology University of Louisville Louisville, Kentucky 40208 Introduction There exist to date relatively few published studies of the Odonata fauna of Kentucky. These are either outdated, scant in detail, or limited in scope. Garman (1924) was the first extensive state list, and treated 66 species. With the combination of Perithemis domitia with P. tenera in Ris (1930), Garman’s total was reduced to 65. Other early works treating Ken- tucky Odonata were Williamson (1909) and Garman (1932). Cook (1947) gave dates and localities for species of the genus Somatochlora known from Kentucky; and in 1951 he added 35 species more to the state list of Odonata. Needham and Westfall (1955) added four more, and brought together much of the information on dragonflies known up to the time of publication. Their records included those known from Kentucky, as well as from nearby states. In 1967 Macklin and Cook added another 28 names to the species list for Kentucky; and Montgomery (1967) published another state list, but without locality or seasonal information. The total number of dragonflies and damselflies was 133 species at this point. The present list gives all known county records for each species, plus the earliest and latest collection dates for adults as compiled from both specimens in collections and published records. Furthermore, three species are added to the state record, bringing the total to 136. These are Neurocordulia molesta Walsh, Enallagma antennatum Say, and Tetra- goneuria spinigéra Selys. Their determinations have been verified by specialists. The first two were collected by the author; and the last was recorded by Dr. Jerry Macklin. In addition to the records published in the works cited above, data were taken from specimens in the insect collections of the University of Louisville and the University of Kentucky. Other material studied was either collected by the author or borrowed from private collections. Specimens were identified by the author with the help of various papers on damselflies, and of Needham and Westfall (1955), which is the authority for the nomenclature and classification of dragonflies used here. Some specimens were sent for determination or verification to doctors M. J. Westfall, Jr., University of Florida, and Oliver S. Flint, Jr., United States National Museum. 1 University of Louisville Contributions in Biology (New Series) No. 122. Dragonflies and Damselflies 33 Suborder ZYGOPTERA Family CALOPTERYGIDAE Calopheryx angustipennis Selys Breckinridge; Edmonson; Grayson; Marion. May—June. Calopteryx dimidiata Burmeister Garman (1924, p. 285) lists this species as occurring in Kentucky. Calopteryx maculata Beauvais Adair; Allen; Ballard; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Cumberland; Edmonson; Fayette; Fulton; Graves; Green; Greenup; Hart; Henderson; Jefferson; Kenton; Knott; Logan; Lyon; Marion; Meade; Metcalfe; Monroe; Muhlenberg; Ohio; Oldham; Pike; Powell; Pulaski; Rockcastle; Taylor; Todd; Trigg; Union; Warren; Wayne; Whitley. Apr. 25—Sept. Hetaerina americana Fabricius Adair; Allen; Anderson; Breckinridge; Bullitt; Butler; Carter; Casey; Christian; Cumberland; Edmonson; Fayette; Green; Jefferson; Madison; Marion; Metcalfe; Monroe; Nelson; Oldham; Pike; Pulaski; Rock- castle; Taylor; Warren; Wayne; Whitley. May—Oct. 5. Hetaerina titia Drury Adair; Barren; Breckinridge; Carter; Edmonson; Green; Hardin; Marion; Metcalfe; Rockcastle; Wayne. July 26—Nov. 2. Family LESTIDAE Archilestes grandis Rambur Fayette; Green. Sept. Lestes congener Hagen Breckinridge; Bullitt; Butler; Edmonson. Lestes disjunctus Walker Adair; Carter; Fayette; Fulton; Green; Hardin; Hart; Henderson; Jefferson; Metcalfe; Ohio; Oldham; Taylor; Warren. Apr. 16—July. Lestes dryas Kirby Bell. June. Lestes eurinus Say Oldham; Union; Wayne. May 26. Lestes forcipatus Rambur Barren; Breckinridge; Bullitt; Edmonson; Fayette; Green; Hardin; Hart; Jefferson; Ohio; Taylor; Union; Warren. Apr. 4—Aug. 29. Lestes inaequalis Walsh Green; Hardin; Hart; Jefferson; Marion. May 27—Aug. Lestes rectangularis Say Carter; Edmonson; Fayette; Green; Hart; Hopkins; Jefferson; Russell; Taylor; Wayne. May 20—Oct. 34 Patricia Liles Resener Lestes unguiculatus Hagen Breckinridge; Edmonson; Green; Ohio; Taylor; Union; Warren. June— Oct. Lestes vigilax Hagen Butler; Edmonson; Grayson; Green; Hart; Pike; Powell; Wayne; Whitley. July 15—Sept. Family COENAGRIONIDAE Argia apicalis Say Adair; Allen; Ballard; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Christian; Cumberland; Edmonson; Fayette; Fulton; Grayson; Green; Hardin; Hart; Henderson; Jefferson; Kenton; Lyon; Madison; Marion; McCreary; Meade; Metcalfe; Monroe; Muhlenberg; Ohio; Oldham; Powell; Pulaski; Taylor; Trigg; Union; Warren; Washington; Wayne; Whitley; Woodford. May 5—Oct. 10. Argia fumipennis Burmeister Garman (1924, p. 286) lists this species as occurring in Kentucky. Argia moesta Hagen Adair; Allen; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Cumberland; Edmonson; Fayette; Fulton; Grant; Green; Hardin; Har- rison; Hart; Henderson; Jefferson; Kenton; Lyon; Marion; McCreary; Mercer; Metcalfe; Monroe; Muhlenberg; Ohio; Oldham; Powell; Pulaski; Rockcastle; Russell; Taylor; Trigg; Union; Warren; Washing- ton; Wayne; Whitley. June 4—Sept. Argia sedula Hagen Adair; Allen; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Christian; Cumberland; Edmonson; Fulton; Grant; Green; Hardin; Harrison; Hart; Henderson; Logan; Lyon; Marion; McCreary; Mercer; Metcalfe; Monroe; Muhlenberg; Ohio; Powell; Pulaski; Russell; Taylor; Todd; Trigg; Union; Warren; Washington; Wayne; Whitley. June— Sept. Argia tibialis Rambur Adair; Allen; Barren; Breckinridge; Butler; Carter; Casey; Edmonson; Green; Harrison; Hart; Henderson; Jefferson; Marion; Mercer; Met- calfe; Monroe; Oldham; Pike; Todd; Union; Wayne. May—Aug. Argia translata Hagen Adair; Allen; Butler; Carter; Casey; Cumberland; Edmonson; Green; Marion; McCreary; Metcalfe; Monroe; Pulaski; Russell; Washington; Wayne; Whitley. June—Aug. Argia violacea Hagen Adair; Allen; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Christian; Cumberland; Edmonson; Fayette; Grayson; Green; Hardin; Harrison; Hart; Henderson; Jefferson; Jessamine; Kenton; Marion; Metcalfe; Monroe; Muhlenberg; Ohio; Oldham; Pike; Pulaski; Robert- Dragonflies and Damselflies 35 son; Rockcastle; Taylor; Warren; Washington; Wayne; Woodford. May 26—Sept. Amphiagrion saucium Burmeister Whitley. June. Anomalagrion hastatum Say Adair; Allen; Barren; Bullitt; Butler; Carter; Edmonson; Fayette; Green; Hardin; Hart; Letcher; Marion; Taylor; Trigg; Union; Warren. _ May 17—Oct. 5. Chromagrion conditum Hagen Hardin; McCreary. May—July. Enallagma antennatum Say Union. June 28. Enallagma aspersum Hagen Adair; Barren; Bullitt; Butler; Edmonson; Fayette; Green; Hart; Jefferson; Muhlenberg; Oldham; Taylor; Trigg. May 15—Aug. 6. Enallagma basidens Calvert Adair; Breckinridge; Bullitt; Butler; Casey; Fayette; Green; Hart; Henderson; Jefferson; Oldham; Pendleton; Taylor; Warren. May 15— Sept. 30. Enallagma carunculatum Morse Adair; Bullitt; Green. June—July. Enallagma civile Hagen Adair; Allen; Barren; Bell; Boyle; Breckinridge; Bullitt; Butler; Carter; Casey; Cumberland; Edmonson; Fayette; Fulton; Green; Hardin; Harrison; Hart; Henderson; Hopkins; Jefferson; Kenton; Letcher; Lyon; Marion; McCreary; Metcalfe; Monroe; Nicholas; Ohio; Oldham; Powell; Pulaski; Robertson; Taylor; Trigg; Union; Warren; Washington; Wayne. Apr. 4—Oct. 20. Enallagma divagans Selys Breckinridge; Hickman; Jefferson; McCreary; Mercer. May 28—July ulate Enallagma doubledayi Selys Taylor. June. Enallagma ebrium Hagen Hickman. Sept. 4. Enallagma exsulans Hagen Adair; Allen; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Cumberland; Edmonson; Fayette; Fulton; Grayson; Green; Hardin; Harrison; Hart; Henderson; Lyon; Marion; Metcalfe; Monroe; Ohio; Oldham; Pike; Powell; Pulaski; Robertson; Trigg; Union; Warren; Washington; Wayne. May—Sept. Enallagma genimatum Kell Breckinridge; Butler; Fayette; Taylor. June—Sept. 36 Patricia Liles Resener Enallagma signatum Hagen Adair; Barren; Bullitt; Butler; Carter; Christian; Cumberland; Edmon- son; Fayette; Green; Hardin; Hart; Henderson; Jefferson; Lyon; Marion; Metcalfe; Monroe; Ohio; Pulaski; Taylor; Trigg; Union; War- ren; Washington. May—Sept. 26. Enallagma vesperum Calvert Breckinridge; Green; Hardin. May—July. Ischnura kellicotti Williamson Bullitt; Fayette; Hardin; Taylor. June—Sept. Ischnura posita Hagen Adair; Allen; Ballard; Barren; Bell; Boyle; Breckinridge; Bullitt; Butler; Carter; Casey; Cumberland; Edmonson; Fayette; Fulton; Green; Hardin; Harrison; Hart; Henderson; Hopkins; Jefferson; Kenton; Lyon; Marion; McCreary; Metcalfe; Monroe; Ohio; Oldham; Powell; Pulaski; Robertson; Taylor; Trigg; Union; Warren; Washington; Wayne. May 1—Sept. Ischnura verticalis Say Adair; Allen; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Cumberland; Edmonson; . Fayette; Fulton; Green; Hardin; Harrison; Hart; Henderson; Hopkins; Jefferson; Jessamine; Kenton; Lyon; Marion; Metcalfe; Monroe; Muhlenberg; Ohio; Oldham; Powell; Pulaski; Robertson; Taylor; Trigg; Union; Warren; Washington; Wayne. Apr. 13—Oct. 12. Nehalennia irene Hagen Fayette. Suborder ANISOPTERA Family PETALURIDAE Tachopteryx thoreyi Hagen Fayette; Green; Jessamine; McCreary; Powell; Wayne; Whitley. June 4—Aug. 8. Family CORDULEGASTERIDAE Cordulegaster diastatops Selys Russell. May. Cordulegaster erroneus Hagen Green. Aug. Cordulegaster maculatus Selys Adair; Bell; Floyd; Letcher; McCreary; Whitley. May 28—June 19. Cordulegaster obliquus Say Harrison. May. Family GOMPHIDAE Progomphus obscurus Rambur Allen; Bell; Butler; Carter; Edmonson; Grayson; Green; Harrison; Dragonflies and Damselflies 37 Marion; Metcalfe; Pulaski; Robertson; Rockcastle; Todd; Trigg; War- ren. June—Aug. Hagenius brevistylus Selys Adair; Allen; Barren; Bell; Butler; Carter; Edmonson; Green; Harrison; Metcalfe; Oldham; Rockcastle; Trigg; Warren. June—Aug. Ophiogomphus aspersus Morse Green. June—July. Ophiogomphus rupinsulensis Walsh Breckinridge; Green; Harrison. May—June. Erpetogomphus designatus Hagen Butler; Cumberland; Edmonson; Grayson; Hart. July—Sept. Dromogomphus spinosus Selys Allen; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Cumberland; Fayette; Fulton; Green; Hardin; Harrison; Hart; Henderson; Letcher; Marion; McCreary; Metcalfe; Monroe; Pike; Pulaski; Russell; Taylor; Todd; Trigg; Warren; Washington; Wayne. June—Sept. Dromogomphus spoliatus Hagen Butler; Henderson; Warren. July—Aug. 4. Lanthus albistylus Hagen Bell; Letcher. June—July. Lanthus parvulus Selys Harrison. May. Gomphus (Arigomphus) lentulus Needham Union. July. Gomphus (Arigomphus) pallidus Rambur Fulton; Monroe; Pulaski; Trigg. June—July. Gomphus (Arigomphus) submedianus Williamson Union. July. Gomphus (Arigomphus) villosipes Selys Bullitt: Breckinridge; Edmonson; Fayette; Floyd; Green; Hardin; Hart; Metcalfe; Trigg. May 20—June 5. Gomphus (Gomphurus) crassus Hagen Green; Marion. July. Gomphus (Gomphurus) externus Hagen Bullitt; Green; Trigg. June—July. Gomphus (Gomphurus) fraternus Say Adair; Allen; Barren; Bell; Bullitt; Butler; Cumberland; Edmonson; Fayette; Green; Harrison; Letcher; Marion; Metcalfe; Pike; Rockcastle; Taylor; Trigg; Union; Warren; Washington. May 27—June 5. Gomphus (Gomphurus) hybridus Williamson Cumberland. May. Gomphus (Gomphurus) lineatifrons Calvert Adair; Allen; Barren; Butler; Casey; Edmonson; Green; Marion; Taylor; Warren; Washington; Whitley. May 17—July. 38 Patricia Liles Resener Gomphus (Gomphurus) vastus Walsh Bullitt; Cumberland: Edmonson; Green; Russell; Trigg. May—July. Gomphus (Gomphurus) ventricosus Walsh Grayson; Green. May—June. Gomphus descriptus Banks Letcher. May 29. Gomphus exilis Selys Bell; Bullitt; Casey; Fayette; Kenton; Letcher; Marion; Rockcastle; Washington. Gomphus graslinellus Walsh Bullitt; Fayette; Jefferson; Marion. May 24—June 5. Gomphus lividus Selys Adair; Allen; Barren; Bell; Breckinridge; Butler; Edmonson; Floyd; Grant; Grayson; Green; Hart; Henderson; Letcher; Marion; Metcalfe; Rockcastle; Taylor; Trigg; Union; Warren; Washington; Whitley. Apr. 17—July 5. Gomphus quadricolor Walsh Green. May 23—30. Gomphus (Hylogomphus) viridifrons Hine Green. Gomphus (Stylurus) amnicola Walsh Campbell; Robertson. July. Gomphus (Stylurus) laurae Williamson Casey; Green. Gomphus (Stylurus) notatus Rambur Bell; Breckinridge; Butler; Cumberland; Edmonson; Green; Harrison; Letcher; Marion; Mason; Monroe; Muhlenberg; Rockcastle; Russell. July 21-Sept. Gomphus (Stylurus) spiniceps Walsh Adair; Green; Harrison; Marion; Russell. Sept.—Oct. Family AESCHNIDAE Gomphaeschna furcillata Say Green; McCreary. June. Basiaeschna janata Say Barren; Bell; Bullitt; Butler; Casey; Edmonson; Green; Jefferson; Marion; Metcalfe; Robertson; Rockcastle; Trigg; Warren. May 10. Boyeria grafiana Williamson “Cave Branch, Kentucky.” Aug. Boyeria vinosa Say Allen; Bell; Breckinridge; Bullitt; Butler; Cumberland; Edmonson; Green; Harrison; Hart; Marion; Rockcastle; Russell; Taylor; Washing- ton; Wayne. July—Oct. Dragonflies and Damselflies 39 Anax junius Drury Allen; Barren; Bath; Bell; Bullitt; Edmonson; Fayette; Fulton; Green; Hart; Hopkins; Jefferson; Jessamine; Madison; Marion; Menifee; Oldham; Richmond; Rockcastle; Scott; Taylor; Trigg; Warren. Apr. 12—Oct. Anax longipes Hagen Green. June—Aug. Epiaeschna heros Fabricius Breathitt; Bullitt; Edmonson; Fayette; Green; Jackson; Jefferson; Met- calfe; Trigg. Apr. 21—Sept. Aeschna constricta Say Breckinridge. Sept. Aeschna mutata Hagen Green. May—June 16. Aeschna umbrosa Walker Adair; Green; Jefferson; Metcalfe; Trigg. Aug. 5—Oct. Aeschna verticalis Hagen Harrison. Sept. Family LIBELLULIDAE Didymops transversa Say Fayette; Jefferson; Oldham. Apr. 18—May 9. Macromia alleghaniensis Williamson Adair; Grayson; Green; Marion; Rockcastle. June 23—July. Macromia georgina Selys Butler. Macromia illinoiensis Walsh Adair; Allen; Bell; Butler; Carter; Cumberland; Edmonson; Green; Harrison; Hart; Henderson; Letcher; Marion; Metcalfe; Powell; Robertson; Rockcastle; Russell; Taylor; Todd; Trigg; Union; Warren; Washington; Wayne. May 5—Sept. Macromia taeniolata Rambur Adair; Butler; Cumberland; Edmonson; Gallatin; Green; Marion; Powell; Union; Warren; Washington. June—Aug. 12. Neurocordulia molesta Walsh Henderson. June 15. Neurocordulia obsoleta Say Bell; Cumberland. June—Aug. Neurocordulia yamaskanensis Provancher Adair; Green; Hart; Whitley. May 12—Aug. 10. Epicordulia princeps Hagen Barren; Bell; Breckinridge; Bullitt; Carter; Clinton; Edmonson; Fayette; 40 Patricia Liles Resener Fulton; Grayson; Green; Hardin; Harrison; Hart; Henderson; Hopkins; Letcher; Metcalfe; Monroe; Muhlenberg; Pike; Powell; Rockcastle; Taylor; Todd; Trigg; Union; Washington; Wayne. May—Aug. 4. Tetragoneuria cynosura Say Adair; Allen; Anderson; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Christian; Cumberland; Edmonson; Fayette; Floyd; Fulton; Grayson; Green; Hardin; Harrison; Hart; Henderson; Jefferson; Kenton; Letcher; Logan; Marion; McCreary; Meade; Metcalfe; Monroe; Muh- lenberg; Nelson; Ohio; Oldham; Pike; Pulaski; Robertson; Russell; Taylor; Todd; Trigg; Union; Warren; Washington; Whitley. Apr. 10— July 5. Tetragoneuria spinigera Selys Union. June. Helocordulia uhleri Selys Bell; Floyd; Letcher; McCreary. May 28—June. Somatochlora filosa Hagen Edmonson; Fulton; Union. June 27—July. Somatochlora linearis Hagen Breckinridge; Edmonson; Fayette; Green; Hart; Pulaski; Trigg; Union; Warren. June 19—Sept. 3. Somatochlora'provocans Calvert Green; Trigg. June 28. Somatochlora tenebrosa Say Edmonson; Floyd; Fulton; Green; Letcher; Pulaski; Trigg. June—July 30. Nannothemis bella Uhler Edmonson; Hardin; McCreary. May—June 9. Perithemis tenera Say Allen; Ballard; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Christian; Clinton; Cumberland; Edmonson; Fayette; Floyd; Fulton; Grayson; Green; Hardin; Harrison; Hart; Henderson; Hick- man; Hopkins; Jefferson; Letcher; Marion; McCreary; Metcalfe; Ohio; Oldham; Pike; Powell; Pulaski; Robertson; Russell; Taylor; Todd; Trigg; Warren; Wayne. May 22—Oct. 3. Celithemis elisa Hagen Adair; Allen; Breckinridge; Bullitt; Butler; Edmonson; Fayette; Gray- son; Green; Hart; Henderson; Jefferson; Marion; McCreary; Meade; Ohio; Oldham; Pulaski; Russell; Taylor; Union; Warren; Washington. Apr. 14—Aug. 24. Celithemis eponina Drury Adair; Allen; Breckinridge; Bullitt; Edmonson; Fayette; Fulton; Gray- son; Green; Hart; Hickman; Hopkins; Jefferson; Letcher; Marion; Meade; Metcalfe; Ohio; Russell; Shelby; Taylor; Trigg; Union; Warren; Washington. June—Aug. 22. Dragonflies and Damselflies 41 Celithemis fasciata Kirby Bullitt; Edmonson; Green; Hart; Metcalfe; Ohio; Taylor; Trigg; War- ren. June—Aug. Celithemis verna Pritchard Edmonson; Hart. May 14—July 26. Ladona deplanata Rambur Breckinridge; Edmonson; Hart. May 14—June 5. Libellula auripennis Burmeister Fulton. June. Libellula axilena Westwood Breckinrdige; Bullitt; Edmonson; Green; Hart; McCreary; Ohio; Union. June 26—Aug. 25. Libellula cyanea Fabricius Allen; Barren; Bell; Breckinrdige; Bullitt; Butler; Carter; Casey; Ed- monson; Fayette; Fulton; Green; Hardin; Harrison; Hart; Henderson; Jefferson; Marion; McCreary; Meade; Metcalfe; Ohio; Pike; Pulaski; Russell; Taylor; Todd; Trigg; Union; Warren; Wayne. May 3—Sept. Libellula flavida Rambur Whitley. June. | Libellula incesta Hagen Barren; Bell; Bullitt; Butler; Carter; Edmonson; Fayette; Green; Hardin; Harrison; Hart; Hickman; Ohio; Oldham; Pulaski; Taylor; Trigg; Union; Warren. Apr. 14—Sept. Libellula luctuosa Burmeister Allen; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Cumberland; Fayette; Floyd; Fulton; Green; Harrison; Hart; Hender- son; Hickman; Hopkins; Jefferson; Jessamine; Letcher; Marion; Mc- Creary; Metcalfe; Ohio; Pike; Taylor; Todd; Trigg; Union; Warren; Wayne. Apr. 14—Oct. 19. Libellula pulchella Drury Allen; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Cumberland; Edmonson; Fayette; Floyd; Fulton; Grayson; Green; Hardin; Harrison; Hart; Henderson; Hickman; Hopkins; Jefferson; Jessamine; Letcher; Lincoln; Marion; McCreary; Metcalfe; Ohio; Oldham; Pike; Powell; Pulaski; Robertson; Russell; Taylor; Todd; Trigg; Union; Warren; Wayne. Apr. 11—Sept. 25. Libellula semifasciata Burmeister Breckinridge; Cumberland; Edmonson; Fayette; Green; Hart; Jef- ferson; Marion; McCreary; Taylor; Trigg; Warren. Apr.—July 26. Libellula vibrans Fabricius Adair; Ballard; Breckinridge; Edmonson; Green; Hart; Marshall; Trigg; Union. June 26—Sept. 3. Plathemis lydia Drury Allen; Barren; Bell; Boyle; Breckinridge; Bullitt; Butler; Carter; Casey; 42 Patricia Liles Resener Cumberland; Edmonson; Fayette; Floyd; Fulton; Grayson; Green; Hardin; Harrison; Hart; Henderson; Hickman; Hopkins; Jefferson; Kenton; Letcher; Lincoln; Marion; McCreary; Metcalfe; Monroe; Ohio; Oldham; Pike; Powell; Pulaski; Robertson; Russell; Taylor; Todd; Trigg; Union; Warren; Wayne. Apr. 13—Sept. Leucorrhinia intacta Hagen Cumberland; McCreary; Pulaski; Russell. May. Erythrodiplax minuscula Rambur Union. June. Sympetrum ambiguum Rambur Bullitt; Carter; Edmonson; Fayette; Fulton; Green; Harrison; Hart; Jefferson; Ohio; Oldham; Rockcastle; Taylor; Trigg; Union; Warren; Washington. May 20—Oct. 16. Sympetrum danae Sulzer Montgomery (1967) lists this species as occurring in Kentucky. Sympetrum internum Montgomery Bell; Carter; Edmonson; Green; Hart; Ohio; Trigg; Union. Aug.—Oct. Sympetrum obtrusum Hagen Breckinridge; Edmonson; Hart; Ohio. Aug.—Oct. Sympetrum rubicundulum Say Bullitt; Edmonson; Fayette; Green; Harrison; Hart; Jefferson; Mc- Creary; Ohio; Taylor; Trigg. July—Oct. 29. Sympetrum semicinctum Say Carter; Harrison. Sept. Sympetrum vicinum Hagen Allen; Bell; Bullitt; Butler; Carter; Edmonson; Green; Hardin; Har- rison; Hart; Jefferson; Marion; McCreary; Ohio; Pulaski; Rockcastle; Taylor; Whitley. June—Oct. 27. Erythemis simplicicollis Say Allen; Barren; Bell; Breckinridge; Bullitt; Carter; Cumberland; Edmon- son; Fayette; Floyd; Fulton; Green; Harrison; Hart; Henderson; Hickman; Jefferson; Jessamine; Marion; Meade; Metcalfe; Oldham; Russell; Taylor; Todd; Trigg; Union; Warren; Washington. May 7— Sept. 10. Pachydiplax longipennis Burmeister Allen; Ballard; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Casey; Edmonson; Fayette; Floyd; Fulton; Green; Hardin; Harrison; Hart; Henderson; Hickman; Hopkins; Jefferson; Marion; McCreary; Meade; Metcalfe; Ohio; Oldham; Pike; Pulaski; Russell; Taylor; Todd; Trigg; Union; Warren. Apr. 12—Oct. 6. Tramea carolina Linnaeus Allen; Barren; Bell; Breckinridge; Bullitt; Butler; Carter; Christian; Edmonson; Fayette; Fulton; Green; Hardin; Harrison; Hart; Jefferson; Dragonflies and Damselflies 43 Letcher; Marion; McCreary; Metcalfe; Monroe; Ohio; Rockcastle; Russell; Taylor; Trigg; Union; Warren; Whitley. May 7—Sept. Tramea lacerata Hagen Allen; Barren; Bell; Breckinridge; Bullitt; Carter; Cumberland; Ed- monson; Fayette; Floyd; Green; Harrison; Hart; Hopkins; Marion; Meade; Mercer; Metcalfe; Russell; Taylor; Todd; Trigg; Union; Wash- ington; Warren; Wayne. May 4—Sept. _ Tramea onusta Hagen Carter; Edmonson; Fayette; Hart; Ohio; Pulaski; Trigg; Wayne. May 12-Aug. Pantala flavescens Fabricius Bullitt; Butler; Edmonson; Fulton; Green; Harrison; Hickman; Jef- ferson; Kenton; Marshall; Ohio; Pike; Pulaski; Taylor; Trigg; Union; Warren. June—Sept. 16. Pantala hymenea Say Breckinridge; Cumberland; Edmonson; Green; Harrison; Henderson; Jefferson; McCreary; Trigg; Wayne. June 5—Aug. Acknowledgements I wish to express my thanks to Dr. M. J. Westfall, Jr., and to Dr. O. S. Flint, Jr., for determining specimens; to Dr. Jerry Macklin, University of Kentucky, for making available his personal records; to Dr. P. H. Freytag for the use of material in the University of Kentucky Insect Collection; to Mr. Carl Cook, Center, Ky., for encouragement and assistance; to messrs. Keith Collins, Richard Henderson, and Leroy Henderson for the loan of material; and to Dr. Charles V. Covell, Jr., University of Louisville, for supervision of this project. I am also grateful to Dr. John A. Dillon, Jr., Dean of the Graduate School, University of Louisville, for providing fmancial support for this study. References Cook, C., 1947. Notes on the genus Somatochlora collected in Kentucky and Tennessee (Odonata; Cordulinae). Ent. News 58 (5): 127—131. , 1951. Some new dragonfly records for Kentucky (Odonata). Ent. News 62 (6): 181—188. Garman, H., 1924. Odonata from Kentucky. Ent. News 35 (8): 285—288. , 1932. The genus Archilestes in Kentucky (Odonata). Ent. News 43 (4): 85-92. Macklin, J. M. and C. Cook, 1967. New records of Kentucky Odonata. Proc. N. Central Branch Ent. Soc. Amer. 22: 120—121. 44 Patricia Liles Resener Montgomery, B. E., 1967. Geographical distribution of the Odonata of the North Central States. Proc. N. Central Branch Ent. Soc. Amer. 92: 121129; Needham, J. G. and M. J. Westfall, Jr., 1955. A manual of the dragon- flies of North America (Anisoptera). Los Angeles, Univ. of Calif. Press, xii + 615 pp., 342 figs. Ris, F., 1930. A revision of the libelluline genus Perithemis (Odonata). Univ. Mich. Mus. Zool. Publ. 21: 1—50. Williamson, E. B., 1909. The North American dragonflies (Odonata) of genus Macromia. Proc. U. S. Nat. Mus. 37 (1710): 369—398. Received: October 28, 1969. Accepted: January 7, 1970. SOME MECHANISMS WITH WHICH Crotalus horridus horridus RESPONDS TO STIMULI A. L. WHITT, JR. Department of Biology Eastern Kentucky University Richmond, Kentucky 40475 Introduction Although snakes in general have a fairly well-developed nervous sys- them, they do not have the accessory apparatus to react to their environ- ment quite as well as some of the other vertebrates. Snakes lack movable eyelids and have instead a transparent window, the “brille” which be- comes opaque before ecdysis and renders vision poor during this time; snakes lack an outer ear, middle ear, eustachian tubes or tympanium of any type; it is difficult to determine the mechanism of smell since both gustation and olfaction are so closely related, but both are located in Jacobson’s Orange; the flickering, two pronged tongue picks up chemical particles from the atmosphere around the animal and when retracted, the tongue tips insert into the openings of the pockets of Jacobson’s Organ. Beyond the above sense organs perhaps the most used and most valu- able sense organs possessed by two groups of nocturnal snakes, the Viperidae and Boidae, are the radiation or heat sensitive organs. Rattle- snakes and other members of these two groups posses special sensory pits on each side of the head. In the Viperidae they are con-shaped depressions located slightly below and midway between the nostrils and the eyes and have forward directed openings. These pits have been known as far back as the seventeenth century, but it was not until 1937 that Noble and Schmidt presented a satisfactory theory to account for the function of these pits. Their experiments with rattlesnakes with all major sensory organs other than these pits destroyed or blocked showed that these reptiles could still accurately locate and strike at objects with temperatures higher than that of the surrounding environment. It appears then, that even under noctural conditions these heat sensitive organs can accurately locate and enable the snake to strike at warm-blooded vertebrates whose body temperatures are warmer than the environment. Purpose This research was conducted to define the role that the various sen- sory mechanisms of Crotalus horridus horridus play in picking up external stimuli. 46 A. L. Whitt, Jr. Procedure The snake was placed in a 24x 12x12 inch cage which was mounted on foam rubber pads to cut down on substrate vibration. All test materials were lowered into an open cage on a piece of string to cut down noise and odors. Water at 3 to 4°C, 20-22°C, 37-40°C was introduced in cel- lulose tubing, and acetic acid or 40% formalin was placed on laboratory cotton for the same reason stated above. Sound reception was tested by striking the sides of the wooden cages with a solid object. Rest periods of at least one hour were given between each stimulus presented. Any re- sponse to the stimulus was recorded as positive and the absence of any response was recorded as negative. Experiment 1. No sense organs were blocked. When materials were lowered into the cage and moved back and forth in front of the snake, it would follow the object with movement of the head due to vision, smell, taste and/or pits. The response was positive to all three temperatures of the water, to the cotton soaked in 40% formalin or in acetic acid and to the test for sound receptions. Experiment 2. Two thicknesses of adhesive tape were placed over each eye to completely obstruct vision. After a brief period of readjustment during which the snake hit against the sides of the cage, he appeared well-oriented to the surroundings. Later, when removed for further taping, the snake experienced little difficulty in readjusting to the cage. Cellulose tubing with room temperature (20-20°C) water was lowered within three inches of the snake’s head with no response. When his head was touched, he responded by flicking out the tongue. One hour later when 37°C water was introduced in front of his head, the response was immediate. Again water at room temperature was used and there was no response. Ice water (4-5°C) lowered into the cage illicited the same response as the warmed water (37°C). The snake could not detect 37-40°C water when it was placed directly over the head and behind the eye level. Due to the position and direction of th pits it was necessary to bring the object, at least lateral to and in front of the eye level for detection by these heat sensitive organs. The snake reacted to 40% formalin at room temperature and actually followed it. Two hours later when acetic acid at room temperature was offered, he pulled away and would not move toward it. The reactions had to be gustatory and/or olfactory. There was also a positive reaction to substrate vibrations when the cage was tapped. Experiment 3. The pit (heat-sensitive organ) on the right side of the head was blocked. The snake was still blindfolded. A small piece of (pleistocene) clay was used with tape to hold the clay in the shallow pit. There was not response to water at room tem- Crotalus Horridus Horridus AT perature when lowered on the side of the occluded pit, nor on the open pit side. When 37°C water was lowered on the right side, there was no response but when the tubing was rotated past the midline in front of his head there was an immediate response. With cold water (4 to 5°C) there was no reaction on the occluded side but a positive response on the open pit side. The response to formalin and acetic acid were the same as in ex- periment one and two. Again there was a positive reaction to substrate vibration. Experiment 4. Both pits were occluded—still blindfolded. There were no responses to water at any of the three temperatures. The responses re- mained the same to acetic acid and 40% formalin as in preceding tests and again there was a positive reaction to substrate vibrations. Experiment 5. The tape was removed from the snake’s eyes but the pits remained occluded. The snake now responded positively to all tests: Water at 4°C, 20°C, 37°C, acetic acid, 40% formalin and substrate vibration. Summary There is no doubt that Crotallus horridus horridus uses its eyesight to good but restricted advantage in its life’s activities. Although the hearing apparatus is much modified, the purpose seems to be fuHilled quite well considering the amount of body in contact with its substrate environment. There is little doubt that the sense of taste and/or smell is well developed TABLE 1 Heat Sensitive Pits Olfactory and/or Auditory Gustatory Water Water Water 40% Acetic Substrate Room 387-40°C 3-5°C Formalin Acid Vibrations Temp. No sense organ blocked + + a a au ct Eyes covered = + aL ae at at —on —on — right right = ae + + on + on left left Eyes covered with both pits occluded =~ al a a at a Eyes uncovered with both pits oe = 2a a ae ae occluded + indicates response ( Postitive ) — indicates no response (Negative) 48 A. L. Whitt, Jr. in this snake and that it keeps in almost constant contact with its en- vironment with the tongue and Jacobsen’s Organ. However, the most used sensory structure may very well be the sensory pits. As long as ob- jects of differential temperatures were anterior to, and within 50 or so degrees lateral to the midsagittal line of the body they could be detected by the snake quite easily. See Table 1. Literature Cited Noble, G. K. and A. Schmidt 1937. Proc. Amer. Philo. Soc. 77:263 Received: July 30, 1969. Accepted: May 18, 1970. THE CORN SNAKE, ELAPHE GUTTATA GUTTATA (LINNAEUS) IN KENTUCKY JOSEPH T. COLLINS Museum of Natural History, University of Kansas Lawrence, Kansas 66044 Garman (1894) first mentioned the Corn snake in Kentucky when he placed it on his list of possibly occurring forms as Elaphis guttatus (= Elaphe guttata) and referred to it by the common name “fox snake.” No actual example of this species was found for 41 years after Garman’s work until Hibbard (1936) collected three Kentucky specimens of Elaphe g. guttata (only two specimens were preserved—MCNP 1907 and KU 19760). The first specimen (MCNP 1907) was collected at Taylor’s Coats Hollow, 8 mi NW Park City within the Mammoth Cave National Park con- fines, Edmonson County, on 10 September 1934. The second example (KU 19760) was found at Mammoth Cave Ridge, Edmonson County, on 30 April 1935. Chenoweth (1949) cited Hibbard’s records and reported another Corn snake (CU 5716) collected 2 mi W Park City on Preston’s Ridge within the Mammoth Cave National Park confines, Edmonson County, on 22 April 1948. These three specimens represent the only published examples of Elaphe g. guttata from Kentucky to date. I have discovered five additional Elaphe g guttata from various localities in Kentucky. These specimens, with the three just mentioned, are deposited in the following collections: Cornell University (CU), Illinois Natural History Survey (INHS), Joseph T. Collins collection (JTC), University of Kansas (KU), Mammoth Cave National Park collection (MCNP), Uni- versity of Kentucky (UK), and the University of Louisville (UL). The new records are: BARREN COUNTY: near Park City—no other data (UK R- 178). EDMONSON COUNTY: near junction Mammoth Cave Ferry road and old Route 70—collected by Arthur Graham on 25 May 1961 (MCNP 1823). HART COUNTY: 3 mi W Barren County line on U.S. Rt. 31-W— collected by Joseph T. Collins and Dennis R. Magee on 19 August 1958 (JTC 82). MENIFEE COUNTY: 8 mi S Frenchburg at junction of Ken- tucky Routes 77 and 715—collected by William Clay on 24 June 1954 (UL 6511). POWELL COUNTY: Natural Bridge State Park—collected by L. & M. Stannard on 12 August 1958 (INHS 8953). These eight specimens of Elaphe g. guttata are divided into two widely separated populations. Six of the snakes are from the Mammoth Cave Park area (Barren, Edmonson, and Hart Counties) while the remaining two specimens were collected in the Natural Bridge State Park region (Menifee and Powell Counties), approximately 140 miles airline to the northeast. This disjunct distributional pattern is consistent with evidence presented by Smith (1957) for southern animal species which invaded northward during the post-Wisconsin Climactic Optimum. Unless additional specimens are discovered in the hiatus separating the two isolated Kentucky colonies 50 Joseph T. Collins or the hiatus between these two colonies and the main range of this species to the south, the map of Conant (1958) depicting the Kentucky range of Elaphe g. guttata as isolated, disjunct populations is correct. I wish to thank Roger W. Barbour, William Clay, Carl H. Ernst, Edward Raney, Thane S. Robinson, and Philip W. Smith for the loan of specimens. For assistance in the field I am indebted to Corson J. Hirschfeld. Literature Cited Chenoweth, W. L. 1959. Elaphe guttata in south-central Kentucky. Herpeto- logica 5(2): 22. Conant, R. 1958. A field guide to reptiles and amphibians. Houghton- Mifflin Co., Boston. xv + 1-366 p. Garman, H. 1894. A preliminary list of the vertebrate animals of Ken- tucky. Bull. Essex Inst. 26(1-3): 1-63. Hibbard, C. W. 1936. The amphibians and reptiles of Mammoth Cave National Park proposed. Trans. Kansas Acad. Sci. 39: 277-281. Smith, P. W. 1957. An analysis of post-Wisconsin biogeography of the prairie peninsula region based on distributional phenomena among terrestrial vertebrate populations. Ecology 38(2): 205-218. Received: April 17, 1970. Accepted: May 18, 1970. INSTRUCTIONS FOR CONTRIBUTIONS The TRANSACTIONS OF THE KENTUCKY ACADEMY OF SCIENCE is a medium of publication for original investigations in science. Also as the official organ of the Kentucky Academy of Science, news and announcements of interest to the member- ship are published therein. 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WHITAKER, prema WN, OUI PRG choos ccs kescedstcnnceocnscenteaseescecsesnensoas 64 Kentucky Algae GARY E. DILLARD and STEPHEN B. CRIDER List of Amphibians and Reptiles from Tight Hollow in East- Central Kentucky BRANLEY A. BRANSON, DONALD L. BATCH, and CHARLES J. MOORE Records for and Annotations on Some Valley Millipeds (Diplopoda) from Northern Kentucky Spiders (Arachnida: Araneida) from Northern Kentucky, with Notes on Phalangids and Some Other Localities BRANLEY A. BRANSON and DONALD L. BATCH Pilot Experiments Involving X-ray Induced Mutants in the Dumpy and Yellow Regions of Scute—19i Chromosomes in Drosophila Melanogaster SARA H. COMLEY-FRYE A Search for Trypanosoma cruzi in Kentucky Opossums JOHN V. ALIFF ACADEMY AFFAIRS Index to Volume 31 The Kentucky Academy of Science Founded May 8, 1914 OFFICERS 1969-70 President: Lloyd Alexander, Kentucky State College President-Elect: Karl Hussing, Murray State University Vice-President: Marvin Russell, Western Kentucky University Secretary: Robert S. Larance, Eastern Kentucky University Treasurer: C. B. Hamann, Asbury College Representative to A.A.A.S. Council: Mary Wharton, Georgetown College OFFICERS 1970-71 President: Karl Hussung, Murray State University President-Elect: Louis Krumholz, University of Louisville Vice-President: Marvin Russell, Western Kentucky University Secretary: Robert S. Larance, Eastern Kentucky University Treasurer: C. B. Hamann, Asbury College Representative to A.A.A.S. Council: Branley Branson, Eastern Kentucky University BOARD OF DIRECTORS arly ussving (,,.sccecsteccocmtee to 1970 Gordon, Wilson :.i.2.eeeeee to 1972 Grace AO UTEO ss ccer url ateraseeut to 1970 Sanford .L,. Jones 725s to 1973 John M. Carpenter .............0000 to 1971 Ellis 'V. Brown (32 to 1973 William We Clay cnr eee oe to 1971 Donald. Batch ..).: 335 eee to 1974 Bg, Ae ern nie Ie. Sure seoctotes aes to 1972 J: Ball Hamon..02 ee to 1974 EDITORIAL OFFICE William F. Wagner, Editor Department of Chemistry University of Kentucky Lexington, Kentucky, 40506 Associate Editors: Botany and Microbiology: L. A. Krumholz, University of Louisville Chemistry: Marshall Gordon, Murray State University Geology: William Dennen, University of Kentucky Zoology: Robert Kuehne, University of Kentucky Transactions indexed in Science Citation Index Membership in the Kentucky Academy of Science is open to interested persons upon nomi- nation, payments of dues, and election. Application forms for membership may be obtained from the Secretary. THE TRANSACTIONS are sent free to all members in good standing. Subscription rates for non-members are: domestic, $4.00 per volume; foreign, $4.00 per volume. Tue TRANSACTIONS are issued semi-annually. Four numbers comprise a volume. Correspondence concerning memberships or subscriptions should be addressed to the Secretary. Exchanges and correspondence relating to exchanges should be addressed to the Librarian, University of Louisville, who is the exchange agent for the Academy. Manuscripts and other material for publication should be addressed to the Editor. AN ANNOTATED LIST OF FISHES FROM THE UPPER SALT RIVER, KENTUCKY? R. D. HOYT?, S. E. NEFF, and L. A. KRUMHOLZ Department of Biology and Water Resources Laboratory University of Louisville, Louisville, Kentucky INTRODUCTION The Salt River in central Kentucky has a drainage area of 2920 square miles. This area includes all or parts of 15 counties and makes up 7.2% of the total area of the Commonwealth. The main stem of the Salt River _ arises in Boyle County, Kentucky, in the southwestern part of the Inner Bluegrass region, flows north to near Lawrenceburg, turns west across the Outer Bluegrass region, and enters the Ohio River at West Point. It drains the northern and extreme eastern parts of the basin. The two main tribu- taries of the river, the Beech Fork and the Rolling Fork, drain the southern regions of the basin. Due to a history of floods on the river, three flood control impoundments are scheduled for construction on the Salt River and its two tributaries during the 1970’s. Since the impoundment of the river will create three sizable bodies of water (ca. 4000 acres each) and will cause changes in the flora and fauna and influence downstream water quality, an intensive pre-impoundment survey of the Salt River has been undertaken at the Water Resources Laboratory, University of Louisville, under the spon- sorship of the Office of Water Resources Research, U.S. Department of the Interior. Information gathered in this survey will permit an accurate appraisal of the various changes that will be brought about by impound- ment of portions of the river system. The first flood control reservoir is to be constructed on the main stem of the Salt River about 3 miles east cf Taylorsville, Spencer County, Kentucky. The proposed reservoir will have a surface area in flood of 7900 acres, and the seasonal surface area will be about 3600 acres. This body of water will provide an aquatic recreational area within easy access of an urban area of nearly a million people. In order to estimate the potential of this reservoir for recreational fishing, we conducted a preliminary survey of the fish fauna of the uper reaches of the Salt River. Collections were begun in the fall of 1968 and intensified during the spring and summer of 1969. 1 Contribution No. 126 (New Series) from the Department of Biology, University of Louisville, Louisville, Kentucky 40208. This study was supported by the Office of Water Resources Research, Department of the Interior, under Project No. B-005-KY with the University of Louisville. 2 Present address: Department of Biology, Western Kentucky University, Bowling Green, Kentucky 42101. 52 R. D. Hoyt, S. E. Neff, and L. A. Krumholz MATERIALS AND METHODS Fishes were collected using a 30-foot bag seine, minnow seines, and dip nets in conjunction with electroshocking apparatus (U.S. Army Signal Gen- erator, Model GN-51-B, 300 watt, 120-240 volts, 2.5 amps with 150 feet of line and electrodes) which provided effective sampling along 200 feet of stream at each sampling station. Specimens were fixed in formalin and preserved in 70% ethyl alcohol. All material is deposited in the University of Louisville Fish Collection, Louisville, Kentucky. A total of 6,722 fish was taken during the study; 50 species, referable to 11 families, and 3 hybrid sunfishes were repre- SHELBYVILLE ips > z-__—_. Ke ak / TAYLORSVILLE nf < F ok % eed an seen GY QL. Ma) Se" eservoir 6 @ 2 XS k A PAAR Be we: =O eM an x AV, ey Wy oo oO Ry: Qi) ae 0 “g = 2 RD Ae) roy v9 Y@ & G3) (PF LER 2 a OIG ® : > = | so . iy, ap unwSee nce oe ae Map 1. The ranges of Virginia valeriae valeriae (diagonal lines) and Virginia valeriae elegans (stippling) in Kentucky. Solid circles represent the localities of specimens examined. Academy of Sciences (CA), private collection of Joseph T. Collins (JTC), private collection of James C. List, Muncie, Indiana (JCL), Field Museum of Natural History, Chicago (FMNH), Mammoth Cave National Park, Kentucky (MCNP-—collection was destroyed in 1968), University of Ken- tucky (UK), University of Louisville (UL), United States National Museum (USNM), and the West Virginia Biological Survey, Huntington (WVBS). Methods: In our study, 91 specimens of Virginia valeriae were com- pared using 22 characters (characters 1 through 14 are those used by Blanchard, 1923). All measurements were taken in millimeters. Characters 15 through 22 were measured with dial calipers. The characters examined and measured were: 1. Keeling on anterior dorsal scales—dorsal scales were either keeled (though sometimes faintly) or not keeled on the anterior one-third of the body (snout-vent). 2. Keeling on posterior dorsal scales—dorsal scales were examined as in character 1, but recorded for the posterior one-third of the body (snout- vent). NOTE: Keeling on median dorsal scales tends to be so variable among both V. v. valeriae and V. v. elegans that it is of little value as a character. Care must be exercised in looking for keels because frequently the dorsal scales possess a light-colored median line that superficially re- sembles a keel. This median line, however, shows no elevation and is not a keel. 3. Number of dorsal scale rows—counted in an oblique line across the body. Counts were initiated on the first dorsal scale row as follows: neck (within one head length of the posterior margin of the parietals), mid-body (center of the snout-vent length), and pre-anal (within one head length anterior to the anus). 4. Number of ventral scales—the number of ventral scutes present, ex- 18 George R. Pisani and Joseph T. Collins cluding the anal plate, were counted by Dowling’s (1951) method. Blanchard (1923) did not employ this standardized counting technique, but we feel that the difference in number between his counts and ours would not be significant. 5. Number of subcaudal scales—were counted from the first sub- caudal scale contacting another subcaudal scale on the opposite side up to, but not including, the terminal spine. Tails lacking a terminal spine were not counted. 6. Anal plate—determination of whether the anal plate was single or divided. 7. Number of supraocular scales, left and right. 8. Presence or absence of loreal scale. 9. Number of supralabial and infralabial scales, left and right. 10. Number of parietal, prefrontal, and internasal scales. 11. Number of nasal scales, left and right—the nasal was judged to be single unless divided both above and below the nostril. 12. Number of postocular scales, left and right. 13. Presence or absence of apical scale pits. 14. Ratio of tail length to total length—tail length was measured from the posterior margin of the anal plate at midline to the tip of the terminal spine. Tails lacking a terminal spine were not measured. 15. Frontal scale length (FSL)—distance between the anterior and posterior apices of the frontal scale. 16. Frontal scale to rostral scale length (FRL)—distance from the anterior apex of the frontal scale to the most anterior portion of the rostral scale. 17. Head width—the greatest width of the head between the snout and the posterior edge of the parietal scales. 18. Distance from eye to eye (DEE)—the distance between the most convex portion of each eye. 19. Ratio of FSL plus FRL to head width. 20. Ratio of FSL plus FRL to DEE. 21. Ratio of FSL plus FRL to snout-vent length. 22. Ratio of FRL to FSL plus FRL. Characters of Virginia v. valeriae and V. v. elegans were examined to ascertain differences between these subspecies as well as sexual dimorphism within them. Most comparisons were made a priori by use of the Student’s t-Test (Sokal and Rohlf, 1969) on an Olivelli-Underwood 101 Programma electronic desk computer. Relative degree of anterior and posterior dorsal scale keeling (characters 1 and 2) was computed on the 101 Programma by treating presence of keels as a “success”, the total number of specimens examined as n, and comparing the ratios of “successes” to n’s via Olivetti- Underwood program 5.30 (Williams, 1969). All other ratios tested were transformed to arcsine values (from Rohlf and Sokal, 1969) prior to com- putation. Terminology used for the degrees of difference noted via the t-Test is as follows: significantly different (p <.05), very significantly different (p <.01), and highly significantly different (p <.001). The Smooth Earth Snake 19 ' Analysis of Character Variation Characters showing no significance: The two subspecies of Virginia valeriae found in Kentucky are alike in the following characters: Appearance of the anal plate (divided in all specimens), number of supraoculars one on each side of the head in all specimens), presence or absence of loreal scale (present in all specimens), number of supralabial and _ infralabial scales (generally 6 of each scale on each side of the head, rarely 5 or 7 - scales), number of parietal, prefrontal, and internasal scales (two of each in all specimens), number of nasal scales (generally two on each side of the head, rarely one left or one right, or both), and presence or absence of apical scale pits (absent in all specimens). The frontal scale length (FSL), frontal scale to rostral scale length (FRL), head width, and distance from eye to eye (DEE), and ratios in- volving these morphometric head characters also showed no diagnostic significance. Snout-vent lengths among specimens of both subspecies were homogeneous, a fact that permitted the above morphometric comparisons to be made without bias. Detailed examination of a sample of the Pen- nsylvanian subspecies, Virginia valeriae pulchra, showed that when body sizes (snout-vent) differed significantly, differences in apparent head dimensions also occurred. Virginia v. valeriae shows a greater tendency towards possession of three postocular scales than does V. v. elegans. The difference was of limited significance and would not be useful as a diagnostic character except pos- sibly for large samples. Characters showing significance: Difference in degree of keeling of dorsal scale rows ‘was highly significant; V. v. elegans has a greater tendency to exhibit keeled dorsal scales both anteriorly and posteriorly than V. v. valeriae. Other characters that showed either highly significant or very significant differences were (values given are range and mean for V. v. elegans fol- lowed by the same for V. v. valeriae): number of ventrals (males) 110-126 (117.3) and 112-118 (114.2), number of ventrals (females) 119-134 (124.7) and 114-127 (119.6) (see Figure 1); number of subcaudals (males) 33-44 (40.1) and 29-37 (33.9), number of subcaudals (females) 24-34 (31.0) and 24-29 (26.3) (see Figure 2); ratio of tail length to total length (males) 0.158-0.222 (0.196) and 0.123-0.218 (0.177), ratio of tail length to total length (females) 0.133-0.241 (0.158) and 0.123-0.187 (0.134) (see Figure 3). In all characters depicted in Figures 1, 2, and 3, males differed from females within subspecies to a highly significant degree. High significance also exists in the number of dorsal scale rows, with V. v. elegans typically having 17 rows from the neck to the pre-anal region while V. v. valeriae has 15 rows through the same area. Occasional specimens of V. v. elegans show a loss of one anterior dorsal scale row. Many specimens of Virginia valeriae have been examined by us from a number of states throughout its range. No differences between populations 20 George R. Pisani and Joseph T. Collins 140 9 elegans 130 . ff elegans 9 valeriae Us f valeriae (19) 110 100 Figure 1. Differences in number of ventral scales between Virginia valeriae valeriae and Virginia valeriae elegans. Vertical line = range and horizontal line = mean. Solid rectangle = +2 X standard error of mean. Number in parentheses is n of sample. of the subspecies of this snake in Kentucky and those populations in neigh- boring states were noted. For purposes of comparison, data from popula- tions in Maryland, Ohio, Tennessee, Virginia, and West Virginia were in- cluded with the data from the Kentucky specimens in some of our calcu- lations when the Kentucky sample size was too small to permit accurate computation. This larger sample size gave a more accurate representation of the range of variation to be expected in Kentucky. Anomalous specimens: Four specimens of Virginia v. elegans from western Kentucky, and one V. v. valeriae from southeastern Kentucky show anomalous dorsal scale row patterns of 16-17-15, 15-17-15, and 16-17-16- 17-15. Blanchard (1923) referred to such specimens from other states as examples of intergradation and used them as a basis for assigning Virginia elegans to a subspecific status of Virginia valeriae. Examination of variation in over 200 specimens of Virginia valeriae throughout its range indicates The Smooth Earth Snake 21 that these phena may not truly represent intergrades. A detailed examination of geographic variation in this genus is in progress as the doctoral thesis research of the senior author. Natural History Habitat: Data from field notes are available for only three specimens. Two specimens of Virginia v. valeriae (JTC 42 & 49) were found dead on a highway bordered by heavy forest in McCreary County in southeastern Kentucky. Suitable retreats were available in this area in the form of leaf litter interspersed with large, flat rocks. A single example of Virginia v. 50 45 f elegans 40 J valeriae 35 $ elegans (21) 30 i valeriae Figure 2. Differences in number of subcaudal scales between Virginia valeriae yaleriae and Virginia yaleriae elegans. Vertical line = range and horizontal line = mean. Solid rectangle = +2 X standard error of mean. Number in parentheses is n of sample. 22 George R. Pisani and Joseph T. Collins 9 elegans .240 f elegans .220 f valeriae .200 9 valeriae .180 .160 .140 .120 Figure 3. Differences in ratio of tail length to total length between Virginia yaleriae valeriae and Virginia yaleriae elegans. Vertical line = range and horizontal line = mean. All standard errors were less than .001. Number in parentheses is n of sample. elegans (JCL 636) was captured beneath a rock at the foot of a sandstone bluff in Livingston County in western Kentucky. These limited data preclude any attempt to determine whether these two subspecies exhibit distinct habitat preferences in Kentucky. Annual activity: Collection dates are available for 26 Virginia v. elegans. This subspecies was found during every month from March to September with the months of March through May yielding the most specimens. No significant data are available for V. v. valeriae in Kentucky. Breeding habits: No information about gestation period or breeding The Smooth Earth Snake 23 activity for either Kentucky subspecies is available. However, three female specimens of Virginia v. elegans were X-rayed to determine reproductive activity. The largest specimen (APS 321b) from Trigg County had a snout-vent length of 219 mm and contained six enlarged follicles. A second specimen (JCL 1862) from Ballard County had a snout-vent length of 200 mm and also contained six enlarged follicles. The third and smallest animal (APSU 321la) from Trigg County had a snout-vent length of 196 mm and contained four enlarged follicles. There is no way to determine from X rays whether any of these follicles had been ovulated. The size of the three females and their respective follicle number are within the range of variation for this snake when compared with specimens from throughout its range. In addition, records of brood sizes are available for two female Virginia v. elegans from Bullitt County. One specimen (UL 6486a) collected on 18 August 1950 and having a snout-vent length of 235 mm gave birth to five young (UL 6486b-f) measuring 96, 94, 92, 92, and 81 mm snout-vent, respectively. No date of birth was recorded. The second and larger snake (UL 6487a) measured 246 mm snout-vent, was collected on 21 June 1950, and gave birth on 21 September 1950 to a single young specimen (UL 6487b) which measured 96 mm snout-vent. Range The ranges of Virginia v. valeriae and V. v. elegans in Kentucky are shown (see Map 1). Most immediately apparent from the map is the lack of records from the northeastern quarter of the state and the hiatus between the ranges of the two subspecies. Collecting of additional specimens of this snake from both the northeastern quarter and the discovery of populations in the hiatus (if they occur there) would contribute much to a more accurate assessment of the distribution and variation of Virginia valeriae in Kentucky. No intergrading individuals or populations between Virginia v. valeriae and V. v. elegans are recognized from Kentucky. Analysis of variation of 22 meristic and morphometric characters of 91 specimens of this snake from Kentucky and five other states shows that five characters are very or highly significant in separating the two forms. They are: 1) degree of keeling of dorsal scale rows, 2) number of ventral scales, 3) number of subeaudal scales, 4) ratio of tail length to total length, and 5) number of dorsal scale rows. The natural history of Virginia valeriae in Kentucky is poorly known. Available information for V. v. elegans on annual activity, follicle number, brood number, and dates of birth are presented. Meager habitat data for both V. v. elegans and V. v. valeriae are given. Specimens Examined A total of 53 specimens of Virginia valeriae elegans were examined from the following localities: 24 George R. Pisani and Joseph T. Collins KENTUCKY: Ballard County: Blandville (JCL 1862). Bullitt County: Bernheim Forest (UL 6487a-b), Bernheim Forest, 5 mi S Shepherdsville on Ky. Rt. 61 (UL 6485, 6486a-f), 5 mi S Shepherdsville (UL 3346), 5 mi W Shepherdsville on Ky. Rt. 44 (UL 6488). Calloway County: near Murray (JCL 1273), New Concord (JCL 1492). Christian County: Pennyrile State Park (UK R-183). Edmonson County: Mammoth Cave .25 mi back of Park Hotel (USNM 79291), Mammoth Cave National Park grounds (MCNP 2060). Graves County: 5 mi SE Lowes (JCL 1566). Hardin County: Ft. Knox (JTC 373). Livingston County: 8.6 mi N Smithland (JCL 548-551, 1073, 1078-1081, 1484), 1.5 mi SE Smithland (JCL 636). Lyons County: Duncan’s Creek Cove (APSU 193). Meade County: near Otter Creek (UL 3400, 4645), Lapland, 4 mi W Battletown (UL 2900, 3019, 3087), 4 mi NW Battletown (UL 3111). Nelson County: 4 mi E Boston (UK R-1101). Trigg County: S Golden Pond (APSU 600), SW Golden Pond (APSU 861), in (former) Kentucky Woodlands Wildlife Refuge near Lyon County line (UL 4636), 1 mi NW Turkey Creek (APSU 32la-b), NNE Fenton near Lyon County line (APSU 475a-b). TENNESSEE: Stewart County: near Model (APSU 631, 819), SE Model (APSU 504), NW Dover (APSU 296a-b), Ft. Henry (APSU 584), S Fork Panther Creek (APSU 566), 3 mi SW Bumpus Mills (APSU 357). A total of 38 specimens of Virginia valeriae valeriae were examined from the following localities: KENTUCKY: Bell County: Middlesboro (CA 13309, 13670), Chenoa (UK R-4, R-173, R-209). McCreary County: no other data (JTC 331), W Cumberland Falls on Ky. Rt. 90 (JTC 42), E Monticello on Ky. Rt. 92 (JTC 49), near Cumberland Falls (JTC 320). Wayne County: Wolf Creek Lake (UL 2392, 2398). MARYLAND: Cecil County: Elk Neck (FMNH 44977). OHIO: Scioto County: Shawnee State Forest (JTC 52, 420a, 420b), Shawnee State Forest at North Shawnee sawmill (JTC 145). VIRGINIA: New Kent County: Lanexa (CM 13265-13266, 18163, 34504, 34519-34520, 35450, 36537, 37601, 37608, 40527). York County: Harwood’s Mill (CM 35451). WEST VIRGINIA: Hampshire County: near Romney (CM 23794). Hardy County: 5 mi S Moorefield (WVBS 1313). Kanawha County: Belle (WVBS 2293). Lincoln County: near Ranger (WVBS 2439). Mineral County: near Reese’s Mill (CM 13893), 3 mi SE Keyser (CM 9028), Gerstell Hollow (CM 13826). Wayne County: Wayne (WVBS 3785), 5 mi S Wayne (WVBS 2884), West Huntington (WVBS 2108). Acknowledgements For assistance in the field or for the loan of specimens we are indebted to Roger W. Barbour, Lois Bousman, William M. Clay, the late Doris M. Cochran, N. Bayard Green, Corson Jay Hirschfeld, George Iannarone, James C. List, Clarence J. McCoy, George T. McDuffie, Burt L. Monroe, Jr., David H. Snyder, and George R. Zug. The Smooth Earth Snake 25 Stephen R. Edwards instructed us in the use of the Programma 101. We are also grateful to William E. Duellman and students of the Uni- versity of Kansas herpetology division who read the manuscript and offered suggestions. Jane W. Collins assisted in typing the manuscript. Literature Cited Blanchard, F. N. 1923. The snakes of the genus Virginia. Papers Michigan Acad. Sci., Arts & Letters 3: 343-365. Collins, J. T. 1962. Notes on Virginia valeriae (Baird & Girard) in Kentucky. Herpetologica 18(2): 136-137. Dowling, H. G. 1951. A proposed standard system of counting ventrals in snakes. British Journ. Herp. 1(5): 97-98. Rohlf, F. J., and R. R. Sokal 1969. Statistical Tables. ix—253 pp. W. H. Freeman & Co., San Francisco. Sokal, R. R., and F. J. Rohlf 1969. Biometry. xxi—776 pp. W. H. Freeman & Co., San Francisco. Williams, J. B. 1969. Statistical analysis programs for the Olivetti-Under- wood 101 Programma. 372 pp. Olivetti-Underwood Corp. Received February 18, 1971. Accepted March 5, 1971. CULTURE AND DISEASE: THE HOOKWORM CASE ALLEN C. TURNER Department of Anthropology, University of Kentucky, Lexington, Kentucky Introduction An increasing awareness of the complex inter-relationships between culture and biology, especially with regards to evolution, has resulted in an in- creased emphasis on medical anthropology (Alland 1966). Recognizing that relationship as a factor in primate evolution, Shultz states, “. . . disease is the most potent selective factor in anthropoids.” Focusing more specifically on parasitic disease as a mitigating factor in evolution, Lambrecht (1964:22 quoted by Alland 1966:43) says, “Exposure to and invasion by parasitic organisms may play an important part among many other intrinsic factors that guide the evolution of animal forms.” Lambrecht further suggests that more resistant primates (resistant to trypanosomes, the etiological agents of African sleeping sickness) were able to fill available ecological niches associated with ground-dwelling. This, he says, provides a clue as to why man developed in Africa as opposed to some other area of the world. Fruitful investigation of the relationships between culture and disease is dependent upon adequate analysis of the interaction complex. Alland (1966) has provided a framework within which disease and culture traits are related. He considers the following categories for study: The mutual adjustment between host and parasite. Cultural practices which indirectly affect health and fertility levels. Ethnomedicine. Introduction of new diseases through contact. Acculturation. UU 09 to The problem to which we address ourselves in this paper is the re- lationship between hookworm disease and culture and to that end we shall avail ourselves of Alland’s framework. Hookworm Disease and Culture 1. The Mutual Adjustment Between Host and Parasite Due to the specificity of environment it is clearly demonstrable in the case of most parasites, that both host and parasite evolved together. Such simultaneous evolution is not so prevalent in the Phylum Nematoda of which the hookworms are members. The Nematodes are, as a group, suc- cessful both free-living and as parasites (Dougherty 1951). There are two principle species of hookworm which rely upon man as their host. Ancylostoma duodenale is the more injurious to his host while Necatur americanus is the more frequently occurring. Although it was first discovered in America, Necatur is of African origin. Necatur, primarily Culture and Disease 27 a human parasite, finds pigs, apes and monkeys, similarly amiable. The mode of infestation is the penetration of the host’s skin by the larvae. Skin penetration generally occurs as a result of contact with infested soil. The life cycle of the hookworm involves penetration, migration through the blood system to the heart and lungs where it may cause pneumonia. While in the pulmonary capillaries they begin to burrow into the air spaces in the lungs and are carried by the ciliary movement of the epithelium to the throat. From the throat they are either expectorated or swallowed. If swal- lowed they proceed to the intestines and attach themselves to the wall and commence to lay eggs. The eggs are eliminated with the feces, develop into viable larvae and present themselves for contact by a suitable host (Chandler 1958:408-417). Morbidity resultant from infestation is due to iron deficiency anemia caused by blood loss (Foy and Kondi 1960) as well as reduced protein absorption (Banwell, et al. 1967). The general picture of hookworm disease is one of lassitude which is exemplified by the Erskine Caldwell characters. The victims of hookworm are caught in the sweep of a vicious circle. A typical picture is that of the victim who lacks industry, doesn’t work and therefore cannot afford to buy shoes for himself or his children who then go barefoot and contact hook- worm disease and spread it further. This cycle continues until at some point it is broken either by eradication of the larvae, the adult worm in the intestine, or by the provision of shoes or sanitation facilities. The goal of the parasite is not to kill its host but rather to provide itself with a suitable environment. To this end the parasite will debilitate its host as much as is compatible with their mutual life. Hookworms, like many other parasites have definite host preferences. In a survey taken in 1940, Keller found that rural whites are more suscep- tible than are rural. Negroes. It was found that whites were, on the aver- age, infested four times as frequently as Negroes with the highest propor- tion being found in Florida whites of whom 38.8 percent were infested. The lowest, on the other hand, were Mississippi Negroes, 1.3 percent of whom carried hookworm. These percentages do not reveal the total picture as the intensity of infestation, as determined by fecal egg count, was twice as high in whites as in Negroes. On this point it should be recalled that Necatur americanus is of African origin as are American Negroes. It would appear therefore, that the Negroid race, through prolonged contact with hookworms, evolved an adaptive mechanism which lessens the impact of the hookworm as a negative environmental factor. 2. Cultural Practices which Directly Affect Health Just as hookworm thrives in particular physical environments (es- pecially tropical) certain cultural practices lend themselves to producing a suitable environment for their growth. Chandler (1958:418-420) notes several of these cultural factors. The keeping of feces-eating animals such as hogs and dogs serves to sperad hookworm in the same areas where humans are likely to go. The eggs can be eaten by these animals and pass through their intestines unharmed. Cockroaches, on the other hand, seem to 28 Allen C. Turner destroy the eggs and were a significant factor in reducing the incidence and intensity of hookworm disease in mines in India. Chandler also makes note of the occupational factors which predispose to the disease. Agriculture and mining are the occupations most conducive to hookworm disease be- cause of the moist and warm medium. Tropical agriculture is especially significant. Jute and rice farming are less conducive to hookworm growth if the cultivation is of the flooded ground type. Dry soil farming such as grain farming is not favorable to hookworms nor is cotton farming as the soil is unfavorable in constitution. Defecation habits are another significant cultural factor. The provision of latrines which keep the feet off the ground can eliminate much of the disease as can the wearing of shoes. A particularly interesting relationship between disease and another cultural characteristic is that of the habitual chewing of coca leaves and the intensity of morbidity of hookworm disease. Buck, Sasaki, Hewitt, and MacRae (1968) demonstrated the potentiating effect of coca use and hookworm infestation on malnutrition and anemia among Peruvian peasants. The chart below demonstrates this effect. Table 1. Intensity of hookworm infestation and hemoglobin mean yalues among 41 pairs of coca chewers and controls Differ- Coca Chewers Controls ence Hookworm no. per cent mean no. per cent mean Eggs of total Hgb of total Hgb % in gm in gm Jo % Negative 11 26.8 10.6 17 41.5 12.4 1.8 Few 18 31.7 Wt 14 34.1 12.6 1.5 Moderate 15 36.6 9.6 7 17.1 11.2 1.6 Numerous 2 4.9 TUetl 3 7.3 10.8 3.1 Totals 41 100.0 10.4 Al 100.0 12.2 1.8 From this chart one can see that the morbidity of hookworm disease is especially acute in individuals with numerous worms and also chew coca. This is demonstrated by a difference in mean hemoglobin of 3.1 percent while in non-coca chewers who are heavily infested it is about the same as in coca users who have no hookworms. This relationship is also noted by Roche and Layrisse (1966) and further substantiated by Buck, Sasaki, and Anderson (1968). An explanation for this relationship between coca chew- ing and hookworm disease rests in the fact that coca provides a local analgesic effect in the stomach. In areas of chronic poverty where hunger is constant, coca can provide relief from the pains of hunger. At the same time it provides relief from the discomfort caused by the worms. With this added factor (the relief from pain) those individuals with more hook- worms chew more coca. Culture and Disease 29 3. Ethnomedicine Although it is not defined by users as a prescription for hookworm disease it is possible that the widespread use of betel nut indicates that it is considered salubrious. Although betel nut contains areceline, an an- thelmintic, the continuous spitting associated with betel nut use in Asia is probably a more significant factor in reducing the incidence and intensity of the disease in the Asian population. A more definite ethnomedical cor- relation occurs in the southern United States where hookworm disease is endemic. In that area, tobacco chewing was considered good for the health. Again, the virtue lies not in the substance being chewed but rather in the expectoration of the hookworm (Chandler 1958: 420). Relating specifically to the ethnoetiology of hookworm disease is the in- junction against fetching the cows before the dew dries and going barefoot in the rain (related by a rural Kentucky informant). Both of these pre- cautions are well based in fact as the hookworm larvae are viable only in moist soil and are readily susceptible to dessication. 4. Introduction of New Disease through Contact Payne, et al. (1956) conducted a survey in the Callejon de Huaylas valley of Peru for the purpose of designating the type and spread of pa- rasites. The survey accounted for nine groups of people in five villages and one plantation at altitudes ranging from 8,000 to 11,000 feet of elevation. It is interesting to note that of the nine groups studied only two had hook- worm—the prisoners in the Huaraz jail and the Huaraz police force. The disease was obviously brought into town by people who became prisoners. This was verified by unsuccessful attempts to incubate the hookworm eggs in local soil. They would incubate only outside the valley. Salem and Truelove (1964) expressed concern that the disease might spread from Pakistani immigrants througout the English mining camps. 5. Acculturation Alland (1966) uses this heading to treat the introduction of new di- sease as a by-product of acculturation of cuture contact. We shall use it to describe some of the problems encountered in attempts to eradicate the disease which originates from outside the affected culture. Foster (1962:50, 61-62, 129, 239-240) recounts some of the problems described by Phillips (1955) which obstructed the progress of the Rockefeller campaign against hookworm disease in Ceylon. First of all, the coolies were suspicious of capsular form medication. Even when convinced that the medicines were safe they were reluctant to take it as it prevented them from working for a few days—something they could not afford. They were also suspicious of the goals of the medicators as their offerings were free of charge. This objection was counterbalanced when it was explained that Mr. Rockefeller, the donor, had been ill with hookworm, was cured, and felt obligated to Allah to express his gratitude by curing all who had the disease. The Ceylon example points out well the need for cultural fit of any program designed to bring aid to a suffering people. 30 Allen C. Turner Evolutionary Consequences As was indicated above, hookworm disease is a vicious circle which is difficult to break due to cultural factors as well as characteristics inherent in the disease itself. The consequences of the disease go far deeper than personal discomfort and debilitation. Children who are victims may suffer from several years’ physical and mental retardation. Their capacity to learn is reduced. Delayed puberty severely impairs their ability to reproduce. Particularly acute are the effects of hookworm disease during pregnancy because of the increased demand for iron and protein. Hookworm disease causes a large number of stillbirths and is responsible for more serious complications of pregnancy than is syphilis (Chandler 1958:422-423). As population or biomass is the predominant success indicator in Dar- winian evolution it is evident that any disease which reduces reproductivity is evolutionarily significant. Likewise, the adaptive value of the differential resistance to infestation offered by the Negroid and Caucasoid races has evolutionary implications although modern medical practice largely oblite- rates these differences. This suggests that a profitable course for research in this area might focus on an investigation of early hookworm morbidity and mortality statistics to determine to what extent the antebellum whites were at a biological disadvantage to their chattels. References Cited Alland, A. Jr. 1966. “Medical anthropology and the study of biological and cultural adaptation,” American Anthropologist, 68, 1:40-50. Banwell, J. G., et al. 1967. “Hookworm infection and intestinal absorption amongst Africans in Uganda,” American Journal of Tropical Medicine and Hygiene, 16, 3:304-308. Buck, A.A., Sasaki, T. T., Hewitt, J. J. and MacRae, A. 1968. “Coca chew- ing and health: an epidemiological study among residents of a Peruvian village,’ American Journal of Epidemiology, 88:2, pp. 159- ae Buck, A. A., Sasaki, T. T., and Anderson, R. I. 1968. Health and Disease in Four Peruvian Villages: Contrasts in Epidemiology. Johns Hopkins Press, Baltimore. Chandler, A. C. 1958. Introduction to Parasitology. Wiley, New York. Dougherty, E. C. 1951. “Evolution of zooparasitic groups in the Phylum Nematoda, with special reference to host-distribution,” Journal of Parasitology, 37: 353-378. Foster, G. M. 1962. Traditional Cultures: and the Impact of Technological Change. Harper and Row, New York. Foy, H. and Kondi, A. 1960. “Hookworms in the aetiology of tropical iron deficiency anemia, Radioistotope studies,” Transactions of the Royal Society of Tropical Medicine and Hygiene. 54:419-433. Culture and Disease 31 Keller, A. D., Leathers, W. S. and Densen, P. M. 1940. The results of recent studies on hookworm in eight southern states,” American Journal of Tropical Medicine, 20:493-509. Lambrecht, F. L. 1964. “Aspects of evolution and ecology of tsetse flies and trypanosomiasis in prehistoric African environment,” Journal of African History V, No. 1:1-24. Payne, E. H., Gonzales Mugaburu, L., and Schleicher, E. M. 1956. “An in- testinal parasite survey in the High Cordilleras of Peru,” American Journal of Tropical Medicine and Hygiene, 5:4 (July) 696-698. Phillips, J. 1955. “The hookworm campaign in Ceylon,” In Howard M. Teaf, Jr., and Peter G. Granck, eds. Hands across frontiers: case studies in technical cooperation. Ithaca, N. Y.: Cornell University Press, pp. 265- 05. Roche, M. and Layrisse, M. 1966. “The nature and causes of hookworm anemia, American Journal of Tropical Medicine and Hygiene, 15:1032- 1102. Salem, S. N. and Truelove, S. C. 1964. “Hookworm disease in immigrants,” British Medical Journal, 1:1074-1077. Schultz, A. H. 1950. “The specialization of man and his place among the Catarrhine primates,” Cold Springs Harbor Symposium on Quantitative Biology 15:37-53. Received: March 2, 1971. Accepted: March 27, 1971 THE MAINTENANCE REQUIREMENT OF THE BROOK STICKLEBACK CULAEA INCONSTANS (KIRTLAND)! VINCENT H. RESH Department of Biology, University of Louisville, Louisville, Kentucky 40208 Detailed studies of members of the stickleback family, Gasterosteidae, both in the field and laboratory, have centered on physiological and be- havioral responses during reproduction, descriptive and analytic behavior, endocrinology, and neuroanatomy (Reisman and Cade, 1967). Reports of sticklebacks’ feeding habits indicate that their food source consists mainly of aquatic insects and crustaceans (Hynes, 1958). Most descriptions of aquarium care with these fish have entailed presenting an abundance of food and removing the excess after a designated period of time. This periodic feeding may be repeated daily, three times a week, or at longer intervals, depending on the study. While feeding behavior and responses to various diets have been de- scribed in detail, no report has been given of the maintenance requirement of gasterosteids. The maintenance requirement is the amount of food that a fish must eat to provide for routine metabolism and neither gain nor lose weight (Brown, 1946). This amount of food has been reported to vary with the size, age, and physiological state of the fish (Brown, 1957). The purpose of this paper is to report the maintenance requirement of sticklebacks of various sizes, under controlled conditions. In this study, 9 male and 11 female sticklebacks possessing 5 dorsal spines, ranging in size from 0.27 to 0.86 g and including first- and second- year fish, were used. These specimens were collected from Fish Creek, a slow-moving stream in Niagara County, New York. They were collected in early fall 1968 and were kept at 11.5 C for more than 2 weeks prior to be- ginning the study, the length of time necessary to assure temperature ac- climation (Armitage and Olund, 1967). Each fish was kept separately in a 300-ml Florence flask throughout the study. The fish were also given an adjustment period to these con- tainers and at no time showed undue signs of stress as a result of being confined. No mortalities occurred. Nylon netting with approximately 4 mm? mesh was placed over the flasks to prevent escape. The 20 flasks containing the sticklebacks were placed in a gravel- bottomed 10-gallon aquarium. A temperature of 11.5 C was maintained throughout the 10 days of the study by a thermostatically controlled re- frigeration system; daily variations never exceeded 0.5 C. Water was cir- culated through the aquarium by an underground filter. An air line placed in the center of a tin-coated copper cooling coil located at mid- 1 Contribution No. 14D (New Series) from the Department of Biology, University of Louisville, Louisville, Kentucky 40208. Maintenance Requirement of the Brook Sticklebrack 33 depth toward one end of the aquarium resulted in further circulation and aeration of the water. The purpose of this air line was to reduce formation of ice on the cooling coils when the system was operating at lower temperatures. A photoperiod of 12 hours was maintained, supplied by a 15-watt flourescent lamp, 5 cm above the water line and controlled by a time switch. Thawed, frozen brine shrimp, Artemia salina (Leach), served as the food source. Prior to the experiment, an average percentage dry weight of 10 samples of brine shrimp was determined. When the rations were weighed daily for each fish, a sample was set aside for dry weight determination. This dry weight determination remained within 95% confidence limits of the average percentage dry weight of the 10 samples. All amounts fed were then expressed as dry weight. The fish were weighed every 24 hours and fed immediately thereafter. The excess food and feces in each flask were filtered through a Buchner funnel and the preweighed filter paper and debris were dried in an oven for 20 hours at 80 C and placed in a desiccator until weighed. The dry weight of the food digested and absorbed was then determined by sub- tracting the dry weight of the uningested food and fecal material from the original amount fed. The fish were transferred to a beaker containing moist cotton and were weighed. This procedure took about 1 minute. For each day of the study, weight changes and amounts of food assimilated were recorded. The results of these measurements are shown in Figure 1. Using the normal equations, the slope of the curve of the maintenance requirements and body weights equaled —1.97. This indicates the mean of the relation of the factors analyzed. No significant differences were found between males and females in this relationship. The relationship between the maintenance requirement and the body weight of the brook stickleback is similar to that reported for the brown trout (Salmo trutta L.). At 11.5 C, the maintenance requirement of the trout decreased with increase in weight (Brown, 1946). Plaice (Pleuronectes platessa L..) also exhibited this decrease in maintenance requirement with increase in weight (Brown, 1957). However, studies of brown trout from 7.0 to 10.0 C showed no correlation between maintenance requirement and body weights (Pentelow, 1939). Johnson (1966) reported little difference between the maintenance re- quirements of large and small pike (Esox lucius L.). In that study, the maintenance requirement differed with season and temperature (Johnson, 1966). A relationship between the maintenance requirement and tempera- ture has also been reported for the brown trout and plaice (Brown, 1957). In the present study, both temperature and photoperiod were within the ranges which promote breeding behavior. Therefore, if seasonal variation of maintenance requirements does exist for the brook stickleback, the main- tenance requirements calculated possibly approach the maximum for the species. Although no estimates of maintenance requirements were made at 34 Vincent H. Resh g BRINE SHRIMP/g FISH/24 hr O 1 2 ° 3 4 5 6° 7 28° Momo WEIGHT OF FISH (g) Figure 1. Maintenance requirement for brook sticklebacks of different weights as indicated by weight of brine shrimp eaten during 24 hours. lower temperatures, observations of fish at temperatures approaching 0 C indicate that the maintenance requirement probably is lower at this temperature. This work was done at Niagara University, Lewiston, New York, under the direction of Dr. Bryan T. Britten. I thank Dr. Louis A. Krumholz, Water Resources Laboratory, University of Louisville, for reading and criticizing the manuscript. Literature Cited Armitage, K. B., and L. J. Olund. 1967. Salt tolerance of the brook stickle- back. Am. Midl. Nat. 68:274-277. Brown, M. E. 1946. The growth of the brown trout (Salmo trutta L.). II. The growth of two year old trout at a constant temperature of 11.5 C. J. Exp. Biol. 22:130-144. Maintenance Requirement of the Brook Sticklebrack 35 ———-———— 1957. The Physiology of Fishes. Academic Press, Inc., New York. Vol. 1, 447 pp. Hynes, H. B. N. 1958. The food of fresh-water sticklebacks (Gasterosteus aculeatus and Pygosteus pungitius), with a review of methods used in the study of foods of fishes. J. Anim. Ecol. 16:188-204. Johnson, L. 1966. Experimental determination of food consumption of pike, Esox lucius, for growth and maintenance. J. Fish. Res. Bd. Can. 23:1495-1505. Pentelow, F. T. K. 1939. The relation between growth and food consumption in the brown trout (Salmo trutta). J. Exp. Biol. 16:445-469. Reisman, H. M., and T. M. Cade. 1967. Physiological and behavioral aspects of reproduction in the brook stickleback, Culaea inconstans. Am. Midl. Nat. 77:257-295. Received: March 5, 1971. Accepted: April 4, 1971. ‘want i dere woos inl rch ; tay ahs tN i see ~ ede yee Bie, cea ni’ TP ey ges | ¥ Hoh it wealth a Petieh! fo BUMP es ee ay i leei u iaridenae) Slat Aare nq ov hai : ' =x — Ss —— a . a , ‘ { ie ; e \ : “ p an INSTRUCTIONS FOR CONTRIBUTIONS The TRANSACTIONS OF THE KENTUCKY ACADEMY OF SCIENCE is a medium of publication for original investigations in science. Also as the official organ of the Kentucky Academy of Science, news and announcements of interest to the member- ship are published therein. These include programs of meetings, titles of papers presented at meetings, and condensations of reports by the Academy’s officers and comnittees. Papers may be submitted at any time to the editor. 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The author is responsible for correcting the galley proof. Extensive alterations from the origical are expensive and must be avoided or paid for by the author. Galley proofs must be returned promptly. Blanks for reprint orders will be supplied with the galley proof. Sa (Madi (tig Bh eee A ‘ ‘ol. 32, Nos. 3, 4 1971 Coden: TKASAT TRANSACTIONS _ of the KENTUCKY \CADEMY of SCIENCE Official Organ Kentucky ACADEMY OF SCIENCE CONTENTS Trichinella Spiralis: Morphology of the First-Stage Migratory Larva a SET TE BUCO RITE 02s SS NSS ES Oe aa 87 Molecular Orbital Calculations. I. Off-diagonal Matrix Elements in Extended—Huckel Molecular Orbital Theory Pe NS SUCHIN Se eee coo ss acasadcnscctcholoccosddsicedecessoces 43 Mass Conservation and Multiple Stoichiometries Bem ERRS Dro cee ere Ge cos es cusculssusiau casos ia lanuivesecsuone 5k Radiation Effects on the Permeability of the Nuclear Membrane of Frog Erythrocytes to Sodium, Potassium, and Chlorine ESE SDSS il 21 ORR Sp 57 RESEARCH NOTES Effect of Nippostrongylus Brasiliensis (Nematoda) on Rabbit Body Weight Ieee ANU ER TCE NCc caccclacsvenscsaceuce 62 New Records of Zapus Hudsonius (Zimmerman) from Kentucky Siar Narte UA CEI cc oss sapocbs dave dossaecooosiesiees: 65 Monopetalonema Alcedinis (Rudolphi) (Nematoda Filariidae ) in the Eastern Belted Kingfisher pee ve AE: and HIUGH BY ENGLISH 2.c..:.-ccccssccecdoscgsseccesteccecas 70 ERNEST DEL FOSSE and FRED H. WHITTAKER Fundulus Notti in Kentucky ge SOME UTS UTS a 76 RALPH W. TAYLOR PE UAE se siicbsccesnseesendhh cas.easssccevoOoccenlelssoereces Minutes of 1971 Annual Meeting Program of 1971 Annual Meeting CORRESPONDENCE POR ema a emer eee eee e ease eeeeeaeeseeee PPP O Some eee es eee sees seeeeeeeeeseesussentesese The Kentucky Academy of Science Founded May 8, 1914 OFFICERS 1971-72 President: Louis Krumholz, University of Louisville President-Elect: Marvin Russell, Western Kentucky University Vice-President: Donald Batch, Eastern Kentucky University Secretary: Rudolph Prins, Western Kentucky University Treasurer: Wayne Hoffmun, Western Kentucky University Representative to A.A.A.S. Council: Branley Branson, Eastern Kentucky University BOARD OF DIRECTORS John M. Carpenter .............000 to 1971 Ellis V. Brown. .:s-neoe oe to 1973 Willian Me Glay-ccsccaccunsteaskont to 1971 Donald Batch ..4.043 ee to 1974 Lv Krom holes Aeon astaeeecans to 1972 J. Hill Hamon iio eee to 1974 Gordon WalsOm: tiscescascsescesvtenes to 1972 Thomas B. Calhoon ..........:...-. to 1975 Sanford. Eu; JOMeS sispscksuevessesandoce to 1973 Charles Kupchella ................-.++ to 1975 EDITORIAL OFFICE William F. Wagner, Editor Department of Chemistry University of Kentucky Lexington, Kentucky, 40506 Associate Editors: Biological Sciences: L. A. Krumholz, University of Louisville Chemistry: Marshall Gordon, Murray State University Geology: William Dennen, University of Kentucky Transactions indexed in Science Citation Index Membership in the Kentucky Academy of Science is open to interested persons upon nomi- nation, payments of dues, and election. Application forms for membership may be obtained from the Secretary. THE TRANSACTIONS are sent free to all members in good standing. Subscription rates for non-members are: domestic, $5.00 per volume; foreign, $6.00 per volume; back issues $6.00 per volume. Tue TRANSACTIONS are issued semi-annually. Four numbers comprise a volume. Correspondence concerning memberships or subscriptions should be addressed to the Secretary. Exchanges and correspondence relating to exchanges should be addressed to the Librarian, University of Louisville, who is the exchange agent for the Academy. Manuscripts and other material for publication should be addressed to the Editor. TRICHINELLA SPIRALIS: MORPHOLOGY OF THE FIRST-STAGE MIGRATORY LARVA JOHN P. HARLEY Department of Biological Sciences, Eastern Kentucky University, Richmond, Kentucky 40475 ABSTRACT Male ablino rats infected with Trichinella spiralis were killed at 5+ days postinoculation. Morphological observations were made on first- stage newly born larvae, larvae recovered from abdominal fluid, blood, muscle, lymph, lungs, liver, kidneys, and abdominal mesentery. These first-stage migratory larvae were studied in the living state and stained with Giemsa’s, Ehrlich’s hematoxylin, and eosin. The results indicate that the larva was spindle-shaped, unsegmented, and bilaterally sym- metrical. Both ends were bluntly rounded. The pseudocoelom was filled with fluid containing many very small granules. The outer body wall was composed of a prominent cuticle containing striae. A hypodermis and rudimentary muscle cells were seen associated with the cuticle. Underneath the cuticle was a fine granular material. A circumpharyngeal nerve ring, stomatostylet, pseudoesophageal bulb, and complete ali- mentary canal were present. Intracellular spheroid bodies were present only in the larvae recovered from abdominal fluid. INTRODUCTION Although generally established, there still remain certain developmental phases of the Trichinella spiralis (Owen, 1835) Railliet, 1895 life cycle that are not clear and have never been completely investigated. One such phase is the descriptive morphology of the first-stage migratory larva. This morphology has been covered only superficially by several workers (Staubli, 1909; Lamb, 1911; Hemmert-Halswick and Bugge, 1934; Dammin, 1941; Gould, 1945; Berntzen, 1965; and Khan, 1966). In summary, these workers reported that the larva’s anterior and posterior ends are bluntly rounded and a small terminal indentation representing a, stoma is present. Also present are an oral spear, a poorly differentiated esophageal bulb, and a nerve ring 26 ,» from the anterior tip. A clear hyaline homogeneous cap is on the anterior end and no loose sheath is present. Obviously, a more detailed description is definitely needed for this larval stage and is the basis for this report. MATERIALS AND METHODS In order to retain uniformity, Sprague-Dawley male ablino rats, weighing 150-170¢ (X = 159 + 11) and 42 + 2 days of age were infected with 3000 + 100 T. spiralis larvae and killed at 54 days postinoculation. First-stage migratory larvae were recovered from: females in the host’s small intestine, abdominal fluid, blood, muscle, lymph, lungs, liver, kidneys, and abdominal mesentery according to the methods of Harley and Gallicchio (1971 a, b). Live larvae from individual body sites were placed on albuminized microscope slides and examined. The pro- cedure of fixation, dehydration, and staining were as given by Berntzen (1965). 38 John P. Harley In addition, larvae were stained with Giemsa’s, Ehrlich’s hematoxylin, and eosin. Larvae were examined at 450X and 900X under phase and ordinary light. Line drawings were made with the aid of a microprojector and drawing tube. RESULTS Larvae recovered from lymph, lungs, liver, and kidneys showed similar morphological features except where noted below. Thus, in order to obtain an overall morphological description of the larva, line drawings (Figs. 1-4) are used for discussion purposes. From Fig. 1, the larva is spindle-shaped, unsegmented, and bilaterally sym- metrical (Fig. 1). When examined in the living state, the larva was opague and grayish. The anterior end is 5-6 u (excluding the blunt caps). Both ends are bluntly rounded. Internally, the body is not metamerically segmented. The pseudocoelom is filled with fluid containing many very small granules. The outer body wall is composed of a prominent cuticle marked by regularly arranged fine transverse grooves or striae. At times, and with some difficulty, hypodermis and/or musculature could be discerned beneath the cuticle. It ap- peared to be a syncytium. The circumpharyngeal nerve ring appears as a dense undulating bar lying at an angle of 10-15 degrees to the body. A space of approximately 1 » delineates the outer limits of the nerve ring from the apparent hypodermis and/or musculature. The nerve ring begins 20-28 » from the anterior tip (X = 26 + 2; N = 25) and is 1-2 « wide. No other nervous tissue could be discerned. In both temporary mounts and stained specimens, an oral stylet was positioned within the stoma and pseudobulb region of the esophagus. Thus, it should be correctly called a stomatostylet. The stomatostylet was seen to actively move in and out in temporary saline mounts and its position varied in stained specimens. The stomatostylet was attached to the base of the pseudobulb region of the esophagus (Fig. 2). The mouth or oral opening is terminal. The stoma (1-2 » long) leads to a slender pseudoesophageal bulb. At a point 10-11 / posterior, it merges with the esophagus. The latter continues past the circumpharyngeal nerve ring and then curves slightly toward the cuticle. Posterior to this esophageal curvature (40-42 u from the anterior tip), in the region where the stichosome eventually develops, is an esophageal enlargement. The esophagus then continues posteriorly where it joins the intestine. However, no esophageal-intestine valve could be seen. The terminal portion of the intestine curves slightly toward one side of the larva and ends at the anal opening. The hyaline cap, or nonnucleated cephalic space, is very prominent in the cephalic region and extends 3-4 » posteriorly. No cells were discernible in this region. Body cells were most dense around the nerve ring and less dense anteriad and posteriad. The exact cell types present in the larva could not be determined. In some of the larvae recovered from the blood, lungs, liver, kidneys, and muscle, a more highly developed muscular esophagus was present (Fig. 3). Intra- cellular spheroid bodies, 1-2 » in diameter, were present in the majority of larvae recovered from abdominal fluid. These were 5-8 » from the posterior tip of the larva (Fig. 4). These bodies were not seen in larvae recovered from any other body site. They appeared yellowish to reddish-brown under ordinary light and had a definite birefringence. Under dark-field illumination they appeared as bright spheroids. They did not stain with Giema’s, eosin, or Ehrlich’s hematoxylin and disappeared in both xylol and alcohol. The number present per larva ranged from 8 to 20 (X = 12; SE = 6; N = 250) and there was no apparent consistency in arrangement. ee S <2 ‘=F SUS 8 (7 OL aie > ae core) if §e SIONS ke aS eer cert 2) Lom Gee SL eee | ——== n = RACK a a ee AA Asso tas 5 Sie SCN ‘ “P. = zs > = ’ vet ’ .~ Wits, . vO ” Tes Cn hi ps 0 cath is) ©2506 C52 oe , Sis ST, stoma; GR, granules; STY, stomatostylet; ES, esophagus; NRV, ES E, esophageal enlargement; CUT, cuticle; BO C, body keletal muscle luid showing spheroid 3 z = wn > > Oo ~ YV 4 (4 OG nm oo z uw 3 8 | ee pe octet ES ee " arom Se ae xn a) SOOKE SCS iss a OER S¢ ows ed ioe = 2) Sean cae (sy ees) Ne een =*Cane wehe) © K Crease ie) CZES Lays days postinoculation showing the muscular esophagus (M ES) surrounding the Figs. 1-4. Line drawings of Trichinella spiralis first-stage migratory larvae. Fig. 1. Typical cavity; IN R, intestinal region; AN, anal opening. Fig. 2. Anterior region showing ex- tended stomatostylet and hyaline cap (H). Fig. 3. Larva recovered from s at 5+ esophageal lumen. Fig. 4. Posterior region of larva from abdominal f circumpharyngea! nerve ring; bodies (SPH). larva. OR, oral opening; 40 John P. Harley Within the hyaline cap and also near the anal opening, 2-6 dark granules were present in all of the larvae recovered from the different body sites. The granules were very transparent and exhibited no birefringence. They disappeared in both xylol and alcohol. Larvae in temporary saline mounts (from all body sites) were extremely active. They exhibited a pronounced whip-like thrashing movement. DISCUSSION The present morphological observations confirm reports by Staubli (1909), Lamb (1911), Dammin (1941), Gould (1945), Berntzen (1965), and Khan (1966) that the first-stage larva is: cylindrical, has bluntly rounded anterior and posterior ends, has a clear hyaline anterior cap, and has a small terminal indentation representing a stoma. Staubli (1909) and Dammin (1941) reported the presence of an oblique clear band that formed a line of demarcation between the anterior quarter and posterior three-quarters of the body. Lamb (1911) did not observe this clear band. Khan (1966) referred to this clear band as a nerve ring 26 y» from the anterior tip. This is in general agreement with the present study. However, following the terminology of Chitwood (1950), it should be correctly called a circumpharyngeal nerve ring. In contrast to Khan’s (1966) find- ings, the position of the circumpharyngeal nerve ring varied between 20 and 28 , from the anterior tip. Hoyberg (1907) reported that he observed a “boring apparatus” in newly born larvae, but his observation was refuted by Staubli (1909) and Hemmert-Halswick and Bugge (1934). Fulleborn (1923) and van Someren (1939) reported that a buccal stylet, about 7 » long by 1 » wide, was attached to the ventral wall at the base of the buccal capsule. They also stated that it was divided into blade and shaft portions and that the stylet could not be seen in living specimens. Khan (1966) reported that in living larvae an “oral spear” could be seen moving back and forth, but that in fixed and stained specimens, the structure was obscure. In the present study, an oral stylet 5-6 » wide could be seen in both living and stained larvae. It was within the stoma and pseudobulb region of the esophagus. According to Chitwood (1950) it should be correctly called a stomatostylet. Also, since the position of the stomatostylet varied in stained specimens and could be seen moving in and out in temporary mounts, it was apparent that the stomatostylet is actively protrusible. In the present study, several interesting morphological features of the first-stage larva were observed that, heretofore, have not been reported. Regularly arranged fine transverse striations are present on the cuticle. The body cavity (pseudocoelom) is filled with many very small granules. The stoma (1-2 » long) leads into a slender pseudoesophageal bulb which, 10-11 , posteriad, merges with the esophagus. The latter continues past the circumpharyngeal nerve ring and then curves slightly toward the cuticle. Posterior to this esophageal curvature (40-42 y from the anterior tip), in the region where the stichosome eventually develops, is an eso- phageal enlargement. The terminal portion of the intestine curves slightly toward one side of the larva and ends at the anal opening. From the preceding, it can be concluded that a complete alimentary canal is present. This is in contradiction with Khan’s (1966) findings. He reported that the Morphology of the First-Stage Migratory Larva Al larva possessed no alimentary canal and considered them similar to micro- filariae. The presence cf a muscular esophagus in some of the larvae agrees with Wu's (1955) findings. One of the interesting observations in this study was the presence of intracellular spheroid bodies in the posterior region of the larva. These were only seen in the majority of larvae recovered from abdominal fluid. They were not seen in larvae recovered from any other body site. These bodies have been discussed in a previous report (Harley and Gallicchio, 1970). Since it was observed that all first-stage migratory larvae (regardless of body site location) were extremely active, it can be assumed that the muscular and nervous systems are functional at this time. Finally, the size of the migratory larva was dependent upon the body site from which they were recovered and also the length of time following inoculation. This size variability has been reported and discussed in detail in another report (Harley and Gallicchio, 1971a). It can be concluded that the first-stage migratory larva of T. spiralis is morphologically fully developed at hatching except as to size and reproduc- tive structures. The larva seems to be typical of other nematodes (except the Filarioidea). LITERATURE CITED Berntzen, A. K. 1965. Comparative growth and development of Trichinella spiralis in Vitro and in Vivo, with a redescription of the life cycle. Exp. Parasit. 16:74-106. Chitwood, B. G. 1950. An Introduction to Nematology. Section I. Monumental Printing Co., Md., 105-107. Dammin, G. J. 1941. Trichinosis. Report of a case with demonstration of the larva in the arterial blood. New Eng. J. Med. 224:357-360. Fulleborn, F. 1923. Uber den “Mundstachel” den Trichotrachelidenlarven und Bemerkungen uber die jungsten Stadien von Trichocephalus trichiurus. Arch. Schiffs Tropen-Hyg., bes. Berucksicht. Path. Ther. 23:421-425. Gould, S. E. 1945. Trichinosis. Charles C. Thomas, Publishers, Springfield, IIl., 356 p. Harley, J. P., and V. Gallicchio. 1970. Trichinella spiralis: Intracellular spheroid bodies in “migratory” larva. Trans. Am. Micros. Soc. 89:497-498. Harley, J. P., and V. Gallicchio. 1971a. Growth of Trichinella spiralis larvae from birth to day 13 postinoculation in the male albino rat. J. Parasit. 57:781-786. Harley, J. P., and V. Gallicchio. 1971b. Trichinella spiralis: Migration of larvae in the rat. Exp. Parasit. 30:11-21. Hemmert-Halswick, A., and G. Bugge. 1934. Trichinen und Trichinose. Ergbn. allgem. Path. Path. Anat. 28:313-392. Hoyberg, H. M. 1907. Beitrag zur Biologie der Trichinen. Ztschr. Tiermed. 11:208-226. Khan, Z. A. 1966. The postembryonic development of Trichinella spiralis with special reference to ecdysis. J. Parasit. 52:248-259. Lamb, A. R. 1911. Concerning the presence of the embryos of Trichinella spiralis in the blood of patients suffering from trichiniasis. Am. J. Med. Sci. 142:395-402. 49 John P. Harley Owen, R. 1835. Description of a microscopic entozoon infesting the muscle of the human body. Trans. Zool. Soc. London 1:315-324. Railliet, A. 1896. Quelques rectifications a la nomenclature des parasites. Rec. Med. Vet. 3:157-161. Staubli, C. 1909. Trichinosis. J. F. Bergmann (Wiesbaden), 295 p. van Someren, V. D. 1939. On the presence of a buccal stylet in adult Trichinella and the mode of feeding of the adult. J. Helmin. 17:83-92. Wu, L. Y. 1955. The development of the stichosome and associated structures in Trichinella spiralis. Can. J. Zool. 33:404-446. Received: April, 1971. Accepted: May 28, 1971. MOLECULAR ORBITAL CALCULATIONS. |. OFF-DIAGONAL MATRIX ELEMENTS IN EXTENDED-HUCKEL MOLECULAR ORBITAL THEORY JOHN R. WASSON University of Kentucky Department of Chemistry Lexington, Kentucky 40506 ABSTRACT This work summarizes equations proposed for the calculation of off- diagonal matrix elements in extended-Hiickel molecular orbital theory and also considers a number of new ones. INTRODUCTION The bulk of literature! produced in recent years in which the results of semi-empirical molecular orbital (MO) calculations are employed to predict, correlate and/or rationalize experimental data testifies for the utility of such calculations. To the purist semi-empirical MO methods leave much to be desired. However, as Clementi? has noted, desirable levels of quan- tum mechanical rigor are frequently limited by the willingness of chemists to undertake such calculations and of institutions to provide the necessary digital computer systems. Also, the majority of chemists desire calculational procedures readily implemented on commonly available computational facilities and which do not significantly decrease the amount of time engaged in experimental work. In MO theory the wave function for the system of interest is generally assumed to be of the linear combination of atomic orbitals (LCAO) type, i.e. n Ye => Cy Pi t=] ! where ¢; represents a specified atomic orbital on a given atom and the coefficients, c,, give the contribution of atomic orbitals, ¢,, to molecular i molecular orbital, k. Employing the variation principle, the well-known secular equations n > Hi; = S;Elci; a0) 1A are obtained. In simple Hiickel theory, which has been of great use to organic chemists concerned with z-electron systems,* the assumption is made that the overlap integrals $,; = 0 for i ~j and S,; = 1 fori = j. Values of E, the energy levels of the system, are obtained from the secular determinant |H;; — SE] = 0 in which the matrix elements Hj; are represented by the parameter a (Coulomb integral = <¢,;|H|¢,;> where H is the Hamiltonian operator) for i = j and B (resonance integral = <¢;|H|¢;>) for i ~j when the neighboring atoms are interacting. In extended-Hiickel molecular orbital (EHMO) theory Coulomb integrals are obtained from valence state ionization energies and all orbital overlap integrals for interacting atoms are retained. EHMO theory, e.g., described by R. Hoffmann,** is conceptually simple, even if somewhat questionable on theoretical grounds, and calcula- 44 John R. Wasson tions are readily performed. EHMO calculations can be used to predict numerical values for experimental quantities, e.g., equilibrium bond lengths and electronic spectral transitions, and are equally applicable to both inorganic and organic ions and molecules. The geometry predictions of EHMO theory are very good except when the electronegativity difference4” (on the Pauling scale) between bonding atoms exceeds about 1.3. The major use of EHMO calculations in inorganic chemistry has been the elucidation of the electronic structure of transition metal complexes.5-6 Other applications to inorganic chemistry have included calculation of the preferred geometry? of IF; and Issleib and Grundler$’ have shown that EHMO calculations can assist in understanding the non-existence of certain compounds, e.g., PH-. Despite lack of complete theoretical rigor, EHMO methods are an important tool in modern chemistry. Considerations of the basis? of EHMO theory have resulted in the consensus!9 that the success of calculations in describing chemical systems arises from the fortuitous cancellation of a number of errors inherent in the technique. In order to increase the reliability of EHMO calculations a number of refinements to the method described above have been introduced.®6 The one parameter in EHMO theory which has received the most attention is the resonance integral, Hi; (i4j), which appears as an off-diagonal matrix element in the calculations and is used to describe the bonding of atoms in molecules. The purpose of this paper is to: (a) summarize the many existing formulas for the off- diagonal matrix elements and consider hitherto unreported ones and (b) to evaluate some of the general properties of H,; (i¢j) terms in EHMO calcu- lations. Subsequent papers in this series will address themselves to the success of various H,;(i+j) terms in yielding reasonable descriptions of the physical properties of chemical systems as well as questions concerning the electronic structure and existence of a number of inorganic ions. Summary and Discussion of Off-Diagonal Matrix Elements Table I lists nineteen formulas for off-diagonal terms in EHMO cal- culations. Hj; terms are taken to be proportional to the product of the overlap integral of interacting orbitals and mean values of the respective valence state ionization energies (VSIE’S), ice., H;; = KS,; (mean VSIE’s) where K is the proportionality constant. The mean of the VSIE’s H,, and H,; can be expressed arithmetically,!” i.e., (Hj, + H,,;)% geometrically,1? i.e., (H;; H,;)1/°, or given in terms of the harmonic or reciprocal!® mean, i.e. 2(H;; H;;)/(H, + H,;). Mulliken™ suggested the use of an arithmetic mean. Subsequently, Wolfsberg and Helmholz!? adopted his approach in their classic calculations for the permanganate ion. Ballhausen and Gray? and Yeranos!® chose geometric and harmonic mean values of H;, and H,;, respectively. The reasons for the choice of these various mean values of the VSIE’s to describe interatomic interactions are discussed in the original literature.11-15 In many applications of EHMO theory to inorganic compounds the value of K has been “judiciously varied” to obtain agreement with experiment. In Table I the commonly used values of K are included in the formulas used to evaluate H;; terms in EHMO theory. Cotton and Haas!8 examined the Molecular Orbital Calculations 45 effect of K variation on the calculation of the ligand field splitting parameter: 10Dq, for hexaammine transition metal complexes. They found it necessary to vary K considerably to obtain agreement with observed values of 10Dq. Hoffmann‘ investigated the calculated properties of ethane by varying K from 1.0 to 2.6 and chose 1.75 as a reasonable value of K for all ie work. On the basis of theoretical considerations Cusachs' introduced K — (2—|S,;)). His formula is not without its shortcomings!® but it does remove a degree of arbitrariness from the evaluation of Fey terms. More recently, Jug!” has suggested that K can be taken equal to 2/(1 + S;;?). K can then be unity for vanishing internuclear distance and two for infinite separation. To allow for variation of K, Gopalakrishanan and his co-workers introduced the empirical relation [ely = Jebel K = K — ————___—_ 2 lg se [Ele where K = 2.00 and H,; = H,;. They pointed out that their approximation gave the required order of 10 Dq for the complex ions Ti(H,0) ¢°+, TiF.?—, Cpki= and VE.2— Consideration of the various values of K and mean VSIE’s yields a num- Table | Off-Diagonal Matrix Elements* 1. Wolfsberg-Helmholz or Mulliken-Wolfsberg-Helmholz(12). General form: H,. = -K S.. (H.. + H..)/2 1j ij it JJ o-bonding: K = 1.6/7 mbonding: K = 2.00 2. Ballhausen-Gray (13) gl, S&S 2.00 S., Gl. lla. Le tj tj ii JJ 3. Hoffmann (4) Bl. , = 15/5 S., Ci, a lan) Y/2 ij ij ii alg 4. Cusachs (14) = -(2 - + He, (2 Is.5)) Si, Gh. H,,)/2 5. Yeranos (15) j cq *. a5 2.00 Sig l2 Gas Hy )/ Gy; Hla) 6. Gopalakrishnan — Sathyanarayana - Patel (16) Me 1/2 Hy, = ~[2.00 - lH, 5 = Blan 2 +H, Ab (Hi, Hy) 7. Jug (17) - Wolfsberg-—Helmholz 2 alse = -(2/(1 + Pag )) Sq (A, 3F A, ,)/2 46 John R. Wasson 8. Cusachs - Ballhausen - Gray Hs = -(2-|8,5|) Si (Hy, H. 4) 9. Cusachs - Yeranos H,. = -(2-|85. 1) S )] ij [2,; Hy 5) / yy +H, ij j 10. Cusachs - Gopalakrishnan et al. wits 2 ck ba apie: Hy = -[(2 Is, 51) lH, Bea lWicleag + 4,511 Si Cag H,5) ll. Cusachs - Gopalakrishnan - Wolfsberg -— Helmholz Hy, = ~L2-|8, 5) )- 1H; Hy 51/2 PR, + H, 51 85 (GER H, ,)/2 12. Cusachs - Gopalakrishnan - Yeranos H,, = “[@-|s,,))-]H,, - He, l/218Gy + Hy] 8, , (2G, Hs )/ (yy + Hy) 13. Gopalakrishnan - Wolfsberg - Helmholz = -[2- - + Hs, [2 lH, 5 H,,|/21H,, ~ He!) $4, y; H,5)/2 Py 14. Gopalakrishnan - Yeranos Hi = -[2-|H;, - H,, 1/2185 + Hy {] Sj [2(H, 5 Hy5)/ (yy + H,,)] 15. Jug - Ballhausen - Gray ee 2 1/2 ay = SAG) sr Siy )) Ss (Hy 5 Hs) 16. Jug - Yeranos ante 2 Hey = =(2/(1 + Si, )) Si, [2H, Hy 5/ Ay y + Hy) 17. Jug - Gopalakrishnan aye ek am 1/2 Hi, = =[K He He W2Gh + Hy [1] 8 Gre Hs) < 2 K = 2/(1 + 85, ) 18. Jug - Gopalakrishnan - Wolfsberg - Helmholz Hig = SES He W2tbo ge Hl S.; (yy + 45/2 a 2 K = 2/(1 + So ) 19. Jug - Gopalakrishnan - Yeranos Ho, = -[K- |B, , > AVE Hy 1] Sj (2H, Hy/G@,, + 4,1 K = 2/(1 + 845°) * In these expressions the VSIE's Hoy and He are taken as positive quantities. Molecular Orbital Calculations 47 ber of new possibilities for the calculation of off-diagonal matrix elements in EHMO theory. Coupled with previous Hj; terms a total of nineteen variations are obtained. These are listed in Table I. A computer program written in Fortran IV for calculating H,; terms by all of these methods is available from the author upon request. Calculated Results Table II presents H;; values for a number of heteropolar and homopolar o and z bonds. For C-H, C-C, and C-N bonds overiap integrals for Slater orbitals were evaluated using the computer program described by Offen- hartz.2° The Slater orbital exponents employed were the optimized values of Clementi and Raimondi.?!_ The appropriate VSIE’s were those of Hinze and Jaffe.2? For P(3p)—S(3p) orbital interactions Slater orbital exponents and VSIE’s were obtained from References 8 and 23. H,; terms for heteropolar bonds have nineteen different values whereas the off-diagonal matrix elements describing the interaction between the Table II H,,; (eV) for Various Bond Types* Method CHa CCg? Cex CNgt = CNge PSgt = PSxf 1 17.86 20.29 6.37 27.19 6.70 7.28 4.65 2 21.34 24.30 6.37 32.16 7.97 8.62 4.60 3 18.72 21.26 5.57 28.50 7.03 7.63 4.07 4 13.56 14.85 5.46 19.74 6.76 7.08 4.18 5 21.29 24.30 6.37 31.76 7.92 8.52 4.55 6 20.97 24.30 6.37 30.90 7.74 8.29 4,49 uf 13.93 15.14 5.89 20.09 7.30 7.63 4.47 8 13.53 14.85 5.46 19.49 6.71 6.99 4.14 9 13.50 14.85 5.46 19.25 6.67 6.91 4.09 10 13.16 14.85 5.46 18.23 6.48 6.67 3.96 11 13.19 14.85 5.46 18.46 6.52 6.74 4.01 12 13.13 14.85 5.46 18.00 6.43 6.59 3.91 13 21.03 24.30 6.37 31.29 7.79 8.39 4.48 14 20.92 24.30 6.37 30.52 7.68 8.20 4.37 15 13.89 15.14 5.89 19.84 7.25 7.55 4,42 16 13.86 15.14 5.89 19.60 7.20 7.46 4.37 ily 13.53 15.14 5.89 18.58 7.01 7.22 4.24 18 13.56 15.14 5.89 18.81 7.06 7.30 4.29 19 13.49 15.14 5.89 18.35 6.96 TAS 4.20 * The negative of the H,,; terms are tabulated for convenience. 4 C(sp?)—H(1s) g bond distance: 1.071A. b C(sp2)—C(sp2) ¢ bond distance: 1.353A. ¢ C(sp?-2,77)—C(sp?-2,77) a bond distance: 1.353A. 4C(sp)—N(sp) o bond distance: 1.150A. © C(sp-2,7)—N(sp-2,2) 2 bond distance: 1.150A. £P(3p)—S(3p) g and z bond distance: 1.90A. 48 John R. Wasson same types of orbitals on identical atoms show less variation. For the C(sp?)—C (sp?) o-bond in ethylene it is observed that methods 2,5-6,13, and 14 (Table I) give H,,; = 24.30 eV, methods 4,8,9,10,11 and 12 yield H;; = 14.85 eV and methods 7, and 15-19 give H,, = 15.14 eV while methods 1 and 3 provide H,,; terms of 20.29 and 21.26 eV, respectively. Similar behavior is exhibited for the C(sp?z)—C (sp?) a-bond of ethylene except that the Wolfberg-Helmholz method (eq. 1 in Table I) yields a value of H,; in agreement with those obtained using methods 2:5,6,13 and 14. Thus, in calculating H,; terms for similar interactions with identical atoms fewer off-diagonal matrix elements need to be considered. It is noted that methods for calculation of H,; terms which provide more negative values will lead to larger calculated force constants for molecules whereas the estimated internuclear distances will remain approximately the same. In order to provide a measure of the effectiveness of the various H;; terms (Table I) in estimating the physical properties of molecules the energy of the 7—7* transition of ethylene was evaluated using a model comprised of two 2p7 orbitals separated by the C-C internuclear distance in ethylene. The results of these calculations are given in Table HI. It is shown that methods employing arbitrary values of K, except Hoffmann’s formulation,# yield a better calculated value for the 7—~7x* transition energy than those employing H,; terms for which there is some, albeit dubious, justification for K. More detailed and inclusive calculations? might be expected to yield different numerical results but the observed trends should be the same. Table III a— 7 Electronic Transition of Ethylene Method AE(eV) z= x” % Deviation 1,2,5,6,13,14 6.93 8.8 3 6.20 18.4 4,8,9,10,11,12 4.96 34.7 7,15,16,17,18,19 6.89 9.3 Experiment (Ref. 24) 7.60 0 Table IV Carbonyl Group 7—7* Electronic Transition Method AE(eV )z—2* Method AE(eV) 2-7" il 9.56 ili 8.09 2 9.31 12 ene 3 8.43 13 9.03 4 8.54 14 8.60 5 9.08 15 8.80 6 8.81 16 8.67 ih 9.11 17 8.41 8 8.35 18 8.61 9 8.17 19 8.23 10 7.98 Experimental: 7.29 — 8.27 eV25 Molecular Orbital Calculations 49 Simple carbonyl compounds exhibit singlet-singlet z—zx* transitions in the region 150-170 nm.?° The average carbonyl bond length is 1.23A. The results of calculations similar to those given above for ethylene are listed in Table IV. Methods 9-12 and 19 yield results within the range of experi- mental data. Conclusions Nineteen formulations for the off-diagonal matrix elements in EHMO calculations have been assembled in Table I. The choice of the mean of the VSIE’s is somewhat a matter of personal choice but the value of K employed in obtaining H,; terms can be obtained by two formulas having some theoretical justification. Of these, the Jug approximation appears to be the better choice. In applying EHMO theory to the calculation of various properties of molecules it may be found that different formulas for Hj; terms give better values for particular properties, e.g., dipole moments, than others. REFERENCES 1. Recently a large number of books and reviews concerning the applications semi-empirical MO methods have appeared, e.g., R. L. Flurry, Jr., “Mole- - cular Orbital Theories of Bonding in Organic Molecules,’ Marcel Dekker, Inc., New York, 1968; M.J.S. Dewar, “The Molecular Orbital Theory of Organic Chemistry,’ McGraw-Hill Book Co., Inc., New York, 1969; P.O.’D. Offenhartz, “Atomic and Molecular Orbital Theory,” McGraw-Hill Book Co., Inc., New York, 1970; J. A. Pople and D. L. Beveridge, “Approximate Molecular Orbital Theory,” McGraw-Hill Co., Inc., New York, 1970. 2. E. Clementi, Chem. Revs., 68, 341 (1968). 3. A. Streitwieser, Jr., “Molecular Orbital Theory for Organic Chemists,” J. Wiley and Sons, Inc., New York, 1961; K. Higasi, H. Baba and A. Rembaum, “Quantum Organic Chemistry,” Interscience Publishers, New York, 1965; L. Salem, “The Molecular Orbital Theory of Conjugated Systems, “W. A. Benjamin, Inc., New York, 1966; H. Suzuki, “Electronic Absorption Spectra and Geometry of Organic Molecules,” Academic Press, New York, 1967. 4. (a) R. Hoffman, J. Chem. Phys., 39, 1397 (1963); ibid., 40, 2474 and 2745 (1964). 4. (b) L. C. Allen, in “Sigma Molecular Orbital Theory,” O. Sinanoglu and K. B. Wiberg, eds., Yale University Press, New Haven, Connecticut, 1970, 1 ZA 5. F. A. Cotton, Revs. Pure Appl. Chem., 16, 175 (1966); H. B. Gray, J. Chem. Educ., 41, 2 (1964); “Structural Chemistry and Molecular Biology,” A. Rich and N. Davidson, eds., W. H. Freeman and Co., San Francisco, 1969, p. 783; J. P. Dahl and C. J. Ballhausen, Adv. Quantum Chem., 4, 170 (1968). 6. C.J. Ballhausen and H. B. Gray, “Molecular Orbital Theory,” W. A. Benjamin, Inc., New York, 1964; W. A. Yeranos, Z. Naturforsch, 25a, 1937 (1970). 7. R. L. Oakland and G. H. Duffey, J. Chem. Phys. 46, 19 (1967). 8. K. Isslieb and W. Grundler, Theoret. Chim. Acta, 8, 70 (1967). 9. G. Blyholder and C. A. Coulson, Theoret. Chim. Acta, 10, 316 (1968). 10. P. W. Smith, R. Stoessiger and A. G. Wedd, ibid., 11, 81 (1968). 11. R.S. Mulliken, J. Chim. Phys., 46, 497, 675 (1959). 50 John R. Wasson 12. M. Wolfsberg and L. Helmholz, J. Chem. Phys., 20, 837 (1952). 13. C. J. Ballhausen and H. B. Gray, Inorg. Chem., 1, 111 (1962). 14. L. C. Cusachs, J. Chem. Phys., 43, S 157 (1965); ibid., 45, 2717 (1966). 15. W. A. Yeranos, ibid., 44, 2207 (1966). 16. J. Gopalakrishnan, D. N. Sathyanarayana and C. C. Patel, Indian J. Chem., 7, a (1969). 17. K. Jug, Theoret. Chim. Acta, 16, 95 (1970). 18. F. A. Cotton and T. E. Haas, Inorg. Chem., 3, 1004 (1964). 19. M. D. Newton, J. Chem. Phys., 45, 2716 (1966). 20. P. O’D. Offenhartz, J. Chem. Educ., 44, 604 (1967). 21. E. Clementi and D. L. Raimondi, J. Chem. Phys., 38, 2686 (1963). 22. J. Hinze and H. H. Jaffe, J. Amer. Chem. Soc., 84, 540 (1962). 23. R. Gleiter and R. Hoffmann, Tetrahedron, 24, 5899 (1968). 24. F. H. Watson, Jr., A. T. Armstrong and S. P. McGlynn, Theoret. Chim. Acta, 16, 75 (1970). 25. H. Suzuki, reference 3, p. 431. Received: May 1, 1970. Accepted: May 25, 1971. MASS CONSERVATION AND MULTIPLE STOICHIOMETRIES P. L. CORIO University of Kentucky Lexington, Kentucky 40506 Every stoichiometry is undetermined to the extent of an arbitrary multiplicative factor », + 0. This indeterminacy is unessential, since multi- plication of the stoichiometric coefficients by » does not alter their ratios and leaves the mass conservation principal intact.1 There are, however, chemical transformations that admit multiple stoichiometries, essentially dis- tinct in the sense that the several sets of stoichiometric coefficients are not related by mere factors of proportionality. The oxidation of t-butyl alcohol to acetic acid, acetone carbon dioxide, and water admits three essentially distinct stoichiometries: 5(GH,),COH + 100, > 2CH,COOH + 4(CH,;),CO + 4CO, + 9H,0, (1) 3(CH,),COH + 60, — 2CH,COOH + 2(CH,),CO + 2CO, + 5H,0, (II) Q(GH.)-COH + 60,—> CH,COOH + (CH,),CO + 38CO, + 5H,0, (III) It has been suggested (1) that mechanistic arguments may be adduced to eliminate all but one of a given set of multiple stoichiometries. This point of view is untenable; for although a given mechanism implies a definite stoichiometry, the mechanism of a chemical reaction is not invariant to changes in experimental conditions. If the experimental conditions are not specified, but reactants and products are known, the only limitations imposed upon ordinary chemical reactions are those implied by the mass conservation principle. Under these circumstances, all stoichiometries consistent with this principle are acceptable. The utility of mass conservation in writing chemical equations appears to have been appreciated first by Bottomley (2) in 1878, and re-emphasized more recently by Bennett (3). However, considerable confusion persists among some writers concerning multiple stoichiometries, conditions for their occurrence, and the number of independent stoichiometries. These matters are of general interest in elementary chemical theory and of some practical importance in quantitative investigations. The purpose of this paper is to present a simple mathematical discussion of mass conservation and multiple stoichiometries. The principle of mass conservation has an immediate physical significance for students, and the mathematics is entirely limited to linear algebraic equations. The discussion has the further advantage of generating nontrivial problems of an investiga- tive nature that relieve the monotony often associated with writing equations. Mass Conservation In Chemical Recations Consider a closed system containing p reactants Ry, Ro, .. . Re that com- bine to form z products P,, Ps, ..., Px. The transformation may be symbolically written 1 Multiplication by » may be interpreted as a change in the unit of mass or a change in the scale of performance. BD} P.. LCorie S,R, -- SoRs ate es ete SpRp = Sp41Py + SpiiPy + Sp+02P. +...t+ where the set S = (S,,Sx..., Spa) of p+ stoichiometric coefficients are to be chosen so that (IV) conforms to the mass conservation principle. The simplest realization of this principle occurs in the form of material balances on the atoms constituting reactants and products. These conditions determine a system of linear homogeneous equations for the p+z stoichio- metric coefficients (4). The rank of this system, defined as the nonvanishing determinant of highest order contained in the matrix of coefficients, will be denoted »; it is equal to the number of independent mass conservation conditions. To illustrate these remarks, consider the oxidation of t-butyl alcohol, written in the general form (IV): S, (CH, ),COH + S,0,—> S,CH,COOH + S,(CH,); 2CH,COOH + HO (IX) Every stoichiometry of (V) may be written in the form C,f; + Cof. + C;f,. The stoichiometries cited in the introduction are given by (1) Cie, —4. G.—9; (2)sC=C, =2"C,=5: (3) C= 1. C5=3, C3=5. Charge conservation provides an additional constraint in stoichiometric equations involving ionic species. Consider the reduction of permanganate ion by hydrogen peroxide in an acidic medium: S,Mn0O,— + S.H,0., + S3;H+ = SsMnt + + S;O0. + S;H.2O (X) Since p+z = 6, and » = 4 (including charge conservation) there are 6—4 = 2 linearly independent stoichiometries. From (X), one derives the linear system 48, + 2S, = 28; + Se, 28, +S, = 2g, a =i Sys —S, +S, = 28,, The last two equations give S;=S4, S3=3S,, so that the first two equations may be rewritten 54 PLES Cone 4S, + 2S. = 2S; + Se, 38, + 285 = 2S. Assigning, in turn, to S; and S, the values (1,0) and (0,1), one derives the fundamental set ff Solas (6) oF OES 1, & eee Every stoichiometry of (X) may be written in the form C,f, + Cofs. In particular C; = 5, C. = 8 give the result cited in most textbooks, namely, 2MnO,— + 5H.O, + 6H+ > 2Mn++ + 50, + 8H,O. (XI) Another independent stoichiometry is given by C, = 3, Cy = 4: 2MnO,— + H.O,. + 6H+ > 2Mn++ +4 30, + 4H,O (XII) The following (unbalanced) transformations are offered as additional examples of systems exhibiting multiple stoichiometries MnO,— + H,O,—> MnO, + O, + H,O +OH-, GH CO,-> HO > COMane (CH,).C = CHCH = CH, + 0,5 CH.O “ (CH,),cO 9 He™@nn W " q © CH,CH = CH(CH,).CH = CH, + MnO,- + H,O> HOOC(CH,),COOH + CO, + CH,COOH + MnO,, HO! D, > HO. - BDO DLO» Has Hbeabe Whether the various stoichiometries of a multiple set will yield the equation as written requires a separate investigation, which presents no real difficulty. The following example illustrates one possible procedure. S,CuO + S,Cu,0 + S3H. > S,Cu + S;H,O (XIII) Mass conservation requires 51 + 2S9 = S4, 5; + So = Ss, S3 = Ss, which yield the fundamental stoichiometries ee (aL OO) sen (OL OE TL) The most general stoichiometry is Cf Coto — (— C7 + 2G) 1G — ©, CG.) The equation XIII will appear as written provided that each component of Cif; + Cof, is positive. These conditions will be satisfied if m and n are positive rational numbers satisfying — C7 = 2C> — mC, — Ci Solving, one obtains mCuO + nCu,0 + mH.,O + (m+n)H, > (m+2n)Cu + (2m+n)H.,O Mass Conservation and Multiple Stoichiometries 55 Any two independent choices for the number pair (m,n) will yield two independent stoichiometries for the reaction as written, e.g.,m = n = I, Miele == 2. It might seem that a diophantine analysis could be useful in the study of stoichiometries (5). However, as only rational mathematical operations are employed in solving linear homogeneous systems of equations with rational coefficients an explicit diophantine analysis is not necessary.2 Application to Chemical Transformations The mass conservation principle may also be used to investigate the possibility of proposed chemical reactions. A proposed transformation will be forbidden by the mass conservation principle whenever the homogeneous equations for the stoichiometric co- efficients admit only the trivial solution S$; = S$; = .... = Spia = 0, and this will occur whenever » = p-+z, that is, whenever the number of inde- pendent mass conservation conditions is greater than or equal to the sum of the numbers of reactants and products. For example, C,H, — C,H;CHs is impossible, since p+7=v=2. However, CgHg+H, — C,H;CHs is consistent with mass conservation, since p+z=3, y=2. Similarly, CH;0H-+C,H;OH is impossible (y>p+7), whereas CH;0H — C,H;OH + H, + H.O is con- sistent with mass conservation (p+7>y). Problems of this type can be worked out by elementary students with modest mathematical backgrounds. In the conversion of benzene to toluene, mass conservation quickly yields the system 6x = Ty, 6x = 8y, with the obvious solution x=y=0. Similarly, the proposed conversion CH;0H— C,H;OH yields the system x=6y, 4x=6y, x=y, so that x=y=0. As a final illustration, consider the interconversion of methylbenzenes. Since y=2 (carbon and hydrogen conservation), any proposed intercon- version of methylbenzenes will be consistent with mass conservation pro- vided that p+2=3. Conclusions The preceding discussion may be concisely summarized as follows: A proposed stoichiometry is (1) unique, save for a performance factor, if p+a—v=1; (2) multiple, if p+2—y>1;, (3) impossible, if p+2—v=0. In the case of a multiple stoichiometry, the number of linearly inde- pendent stoichiometries is ¢=p+z—v. There exists, to be sure, a ¢-fold infinity of stoichiometries, but every one of these can be expressed in terms of the ¢ linearly independent stoichiometries obtained by the procedure described above. 2Tt should be noted that the remarks made concerning independent stoichio- metries in Example 1 of reference 5 are not correct. 56 P. L. Corio LITERATURE CITED R. B. Smith, J. Chem. Ed., 47, 281 (1970). . J. Bottomley, Chem. News, 37, 110 (1878). G. W. Bennett, J. Chem. Ed., 31, 324 (1954). M. Bocher, “Introduction to Higher Algebra,” Chapter IV. Macmillan, New York (1907). 5. R. Crocker, J. Chem. Ed., 45, 731 (1968). Received: August 1, 1971. Accepted: October 7, 1971. AO PO RADIATION EFFECTS ON THE PERMEABILITY OF THE NUCLEAR MEMBRANE OF FROG ERYTHROCYTES TO SODIUM, POTASSIUM, AND CHLORINE? GERTRUDE C. RIDGEL Biology Department Kentucky State College Frankfort, Kentucky 40601 ABSTRACT Electron probe microanalysis was used in an attempt to determine the effects of ionizing radiation on the permeability of the nuclear mem- brane of frog erythrocytes to sodium, potassium, and chlorine. The data suggest that sodium is gained and potassium is lost from the nucleus after the frogs were exposed to 1,000 R whole body irradiation. Within 2, hours there appears to be a restoration of the membrane which brings the sodium and potassium to control levels. No conclusion can be drawn as to changes in the permeability of the nuclear membrane to chlorine following irradiation. INTRODUCTION Creasey (1960) reported that thymus and spleen nuclei isolated from rats five minutes after being exposed to from 25 R to 1,000 R showed a loss of both sodium and potassium. However, there was considerable vari- ability in the levels of sodium and potassium in the nuclei obtained from both the control and experimental animals. In an attempt to obtain more standardized results, he isolated nuclei from normal rat spleen cells, irradiated a portion of the nuclear suspension, and retained another portion as a control. From these pooled nuclei he was able to show a loss of both potassium and sodium as a result of irradiation and these results showed that the loss of potassium from the irradiated spleen nuclei was not as great as the loss of sodium. He further concluded that the greatest losses of these elements were at the same order of radiation dose levels as that which inhibit nuclear phosphorylation. Jackson and Christensen (1964) published results of research which failed to show a loss of either sodium or potassium from in vitro or in vivo x-irradiated rat spleen nuclei. Their controls showed the same variability in sodium and potassium concentrations as reported by Creasey. When calf thymus nuclei were exposed to 100 R and 1,000 R of x-irradiation, there were no significant changes in the sodium and potassium levels in the nuclei nor in the medium surrounding the nuclei at the time of irradiation. Jackson and Christenson concluded that “under the conditions employed in these experiments, sodium and potassium binding by lymphoid cell nuclei is not a radiosensitive process.” Prior to the above investigations, Ting and Zirkle (1940) reported in- 1 This project was undertaken at Lawrence Radiation Laboratory, Bio- Medical Division, Livermore, California, in a College Teacher Summer Research Program in 1970 under the supervision of Dr. William Robison. 58 Gertrude C. Ridgel creases in the permeability of the cell membrane of human erythrocytes for potassium and sodium following in vitro irradiation. Also, Hevesy and Zerahn (1946), using yeast cells labeled with radioactive potassium, demon- strated a loss of potassium after irradiation. Sheppard and Beyl (1951) reported that after in vitro irradiation, the human erythrocytes lost potas- sium and gained sodium. Lessler (1959) gave evidence for a change in the geometry and the physiological nature of the membrane of amphibian erythrocytes following in vitro irradiation with doses as low as 100 R. Reviewing the methods and application of the electron probe micro- analyzer to biochemistry, Anderson (1967) cites as one example the ele- mental analysis of Amphiuma red blood cells conducted by Revel. This study was made on air-dried blood smears coated with a thin layer of carbon. Analysis of results, obtained from electron probe microanalysis, showed that the sodium and potassium concentrations in the red blood cells were some- what higher in the nucleus than in the cytoplasm. It was concluded that the excess of these cations in the nuclei “was related to the presence of large nondiffusible organic molecules acting as anions.” Scanning images of these elements further indicated the unequal distribution of these elements in the cell. In another illustration, Anderson showed that the results of elemental analysis, using the electron probe microanalyzer, may be greatly affected by the method of sample preparation. Data of the sodium concentrations in nuclei and cytoplasm from air-dried samples gave better results than the freeze-dried samples. This, however, was not the case in all elements analyzed. This experiment was designed to determine if ionizing radiation results in the loss of chlorine, potassium, and sodium from the nuclei of frog erythrocytes. MATERIALS AND METHODS Smears from blood collected by heart punctures of laboratory frogs, Rana pipiens or Rana clamitans, were either air-dried or freeze-dried and coated with a thin carbon film about 400 A° thick and stored in a vacuum desiccator. Experimental frogs received whole body radiation of 1,000 R from a 137Cs source, 20 minutes or 2 hours prior to their sacrifice for blood smears. The relative amounts of chlorine, sodium, and potassium in the nucleus and cytoplasm were analyzed using an Applied Research Labs Electron Microprobe. This machine was operated at a setting of 2,350 volts with the current to the tungsten filament of 7 kv. At the proper settings, the current to the sample was adjusted and maintained about 0.08 microamperes. RESULTS A. Comparison of the air-dried and freeze-dried technique of sample preparations. The data from electron microprobe analysis of the erythrocytes of two species of Rana are given in Table I. These data are in counts per minute representing the results of monitoring X-ray emissions from a particular element following electron bombardment of that element. Each count is the mean value of 10 different cells in which the nuclei and the cytoplasm were counted three times at a single site. All data were computer processed, using the statistical program Radiation Effects 59 Comparison of Air-Dried with Pen Technique of Sample Preparation A. Rana clamitans1 Air Dried Freeze Dried Element Analyzed Nucleus Cytoplasm N/C Nucleus Cytoplasm N/C K 470 321 0.683 1219 592 0.434 Na 7086 5690 0.802 7026 4288 0.610 Cl 3102 2869 0.925 4707 3011 0.640 B. Rana pipiens? kK 327 261 0.798 5107 2185 0.4278 Na 5364 4780 0.891 586 768 1.310 Clee ree ree ats 543 385 .709 1 Results obtained from a single animal. 2 Results from two animals. developed at the Laboratory for treating data obtained from the electron probe microanalyzer. It is clearly apparent from the data in Table I that the counts for potassium from freeze-dried preparations were much higher than those received from air- dried preparations. There is a significant difference in the nucleus to cytoplasm ratio, 0.434 from freeze-dried preparations compared with 0.683 from air-dried preparations, of blood obtained from a single animal of the Rana clamitans. Com- parable results are indicated from blood samples of the Rana pipiens. Counts for chlorine, like those of potassium, were higher in freeze-dried preparations but they were lower for sodium. Although there were considerable variations in the counts of cells on a single slide, and between the mean counts of the two species, the cytoplasmic to nucleic ratios were similar for potassium, but such similarities were not as evident for sodium and chlorine. Anderson (1967) reported data showing much higher counts for sodium and chlorine from slides of Amphiuma blood prepared from air-dried samples. His results do not agree with those obtained in this experiment, nor did they agree with other experiments conducted by Robinson and Davis (1970) who reported that the freeze-dried technique of sample preparation gave more accurate data than air-dried samples. Further analysis in this experiment employs the freeze-dried method of sample preparation. B. The Effects of Ionizing Radiation. Table II compares the results of two control animals with three that received whole body doses of 1,000 R. One experimental animal, sacrificed 20 minutes after radiation, showed data which seem to suggest that potassium was lost from the nucleus while sodium was taken up. This is reflected in the C/N value for potassium, 0.4278 and 0.45 from the controls and the C/N values of sodium 0.538 is significantly different from the 1.31 and 0.902 of the control animals. In those red blood cells collected from the animals sacrificed two hours after radiation, there is much similarity in their C/N values for the potassium and sodium. These values for potassium, 0.4177 and 0.404, and for the sodium, 0.80 and 1.131, do not deviate significantly from those of the controls. Comparing the C/N values for chlorine among the two controls with those of the experimental animals, there is no indication that ionizing radiation affects the membrane permeability of the nucleus to Cl ions. 60 Gertrude C. Ridgel Table II Comparison of Results from Control and Irradiated Frogs Control Animals (Rana pipiens) Frog X Nucleus (N) Cytoplasm (C) C/N K 5107 2185 0.4278 Na 586 768 1.310 Cl 543 385 0.709 Frog 8 K 4945 2250 0.45 Na 592 534 0.902 | 127 191 1.50 Experiment Animals (Rana pipiens) Frog H 20 minutes after 1,000 R Dose K 3344 1790 0.5353 Na 4675 2516 0.5398 Gl 1600 1180 0.73875 Frog I—120 minutes (2 hrs.) after 1,000 R Dose kK 4278 1787 0.4177 Na 1210 968 0.80 ‘Olt 1258 866 0.6884 Frog J—120 minutes (2 hrs.) after 1,000 R Dose kK 4712 1905 0.404 Na 1286 1455 Ali Cl 1270 1313 1.03 DISCUSSION Sufficient data have not been collected in this experiment to make definitive conclusions as to the effect of ionizing radiation on the perme- ability of the nuclear membrane of frog erythrocytes to chlorine, sodium, and potassium. However, these data seem to suggest that there is a change in the permeability to potassium and sodium. Similar conclusions could not be drawn for the activity of the membrane to chlorine. There was considerable variation in the counts of x-ray emission from electron bombardment of the elements in the nucleus and cytoplasm. Some of the variability in counts may have been due to the inexperience of the investigator in handling the instrumentation involved in electron probe microanalysis. Another factor may have been the method of preparation of the freeze-dried slides. Although care was exercised in preparing smears, there was observed some cells with smooth outline and others with fuzzy outline on the same slide. A comparison of the counts of the two types of cells is summarized in Table III. These results clearly demonstrate a difference in the counts depending upon the nature of cells. Further investigation is necessary to determine if this difference is due to technique Radiation Effects 61 Table III Comparison of Cell Types on Freeze-Dried Preparations Element Nuclear Cytoplasmic Nuclear Cytoplasmic Analyzed Count Count C/N Count Count C/N Smooth Cells Fuzzy Cells K 4712 1905 0.404 1595 1070 0.63 Na 1286 1455 eS 9149 5095 0.611 Cl 1270 1313 1.01 2931 2206 0.752 or to some other factor. However, variations in the “actual” or relative amounts of sodium and potassium were reported by Creasey (1960) and by Jackson and Christenson (1964) using other methods of analysis. If the trends indicated by this experiment are real, the initial effects following irradiation are a loss of potassium and a gain of sodium in the nuclei of frog erythrocytes. Apparently there is a repair mechanism in the membrane, for within two hours after irradiation, the levels of sodium and potassium in the nucleus return to the levels of those in the control. Lessler (1959) observed a similar reversibility in the permeability of the cellular membrane to the uptake of #2K,CO, at different intervals of time following in vitro irradiation of frog and Amphiuma erythocytes. This experiment demonstrates another technique, electron probe micro- analysis, that can be used in investigating radiation damage in cells. LITERATURE CITED 1. C. A. Anderson. 1967. An Introduction to the Election Probe Microanalysis and its Application to Biochemistry. Methods of Biochemical Analysis 15: 147-270. 2. W. A. Creasey. 1960. Changes in the Sodium and Potassium Contents of Cell Nuclei After Irradiation. Biochim Biophys. Acta. 38:181-182. 3. G. Hevesy and K. Zerahn. 1946. The Effect of Roentgen Rays and Ultraviolet Radiation on the Permeability of Yeast. Acta Radiol. 27:316-327. 4, K.L. Jackson and G. M. Christensen. 1964. Sodium and Potassium Binding in X-Irradiated Nuclei. Radiation Research. 27:434-444. : 5. Milton A. Lessler. 1959. Low-Level X-Ray Damage to Amphibian Erythro- cytes. Science 129:1551-1552. 6. William L. Robinson and David Davis. 1970. Determination of Concentration and Distribution in Rat Thyroid Follicles by Electron Microprobe Analysis. Review of prepublished materials and personal communications. 7. C. W. Sheppard and Gertrude E. Beyl. 1951. Cation Exchange in Mammalian Erythrocytes III. The Prolytic Effect of X-Rays on Human Cells. J. Gen. Physiology. 34:691-704. 8. T. P. Ting and R. E. Zirkle. 1940. The Kinetics of the Diffusion of Salts Into and Out of X-Irradiated Erythrocytes. J. Cellular Comp. Physiology. 16: 197-206. Received: October 7, 1971. Accepted: November 5, 1971. RESEARCH NOTES EFFECT OF NIPPOSTRONGYLUS BRASILIENSIS (Nematoda) ON RABBIT BODY WEIGHT JOHN P. HARLEY Department of Biological Sciences, Eastern Kentucky University, Richmond, Kentucky 40475 INTRODUCTION Previous investigations (Thorson, 1953; Harley, 1966; and Harley and Gallicchio, 1970) have shown that the rabbit is a highly refractory abnormal host to Nippostrongylus brasiliensis (Travassos, 1914). However, experi- mental evidence concerning weight gain of rabbits infected with this parasite has, heretofore, not been reported and is the basis for this report. MATERIALS AND METHODS The strain of N. brasiliensis used was obtained through the courtesy of Dr. Paul Weinstein, National Institutes of Health. Procedures for the maintenance of stock infections in rats and for inoculation of experimental rabbits were similar to those described by Haley (1966). Holtzman albino rats of both sexes were used to maintain the parasite. Young Dutch-belted rabbits (Oryctolagus cuniculus) were obtained from a local supplier and were 56 + 2 days of age (weighing 630-696 g; X = 660 + 48; N = 80) when inoculated. Purina Laboratory Chow and fresh water were provided ad lib. Twenty male and 20 female rabbits were inoculated individually with 50,000 + 2000 larvae. Controls consisted of 20 male and 20 female rabbits. All rabbits were weighed to the nearest gram on a Mikro-Doft balance on the day of inoculation and daily (at the same time each day) through day 15 postinoculation, at which time, the infection disappears (Harley and Gallicchio, 1970). Weight gain values were expressed as mean percentage gain in grams (the percentage increase in weight between the time of inoculation and day 15 post- inoculation). Student’s ¢ test (Snedecor, 1956) was employed in the statistical analysis of paired means. Differences between means were considered significant when P values were less than 0.05. Five control rats were included in the experiment and served to insure that larvae administered to experimental rabbits were infective and capable of develop- ing into adult worms. Controls were necropsied on the 8th day postinoculation and the gut examined for worms according to the method of Haley (1966). RESULTS AND DISCUSSION Recoveries of adult worms from control rats ranged from 62-91% (X = 80; SD = + 20; N = 5). It is apparent from these viability control data that infective larvae administered to experimental rabbits were capable of developing into a population of adult worms. There was a significant (P < 0.05) difference in weight gain between inocu- lated and uninoculated male rabbits (Table I, comparison I), female rabbits (comparison II), and combined weights of male and female rabbits (comparison III). There was no significant (P > 0.05) difference in weight gain between Research Notes 63 Table 1 Comparisons of weight gains of rabbits infected with Nippostrongylus brasiliensis and uninfected rabbits over a 15-day period postinoculation Weight Comparison Uninoc- (X % gain P no. Host sex Inoculated ulated ingrams) —+SD value | Males = 35 36 I <0.05 Males bi 72 52 Females - 84 89 II <0.05 Females Li 80 60 Males + females * 34 39 Ill <0.05 Males + females 76 56 Males = 85 86 IV >0.05 Females = 34 39 Males * a2. 52 Vv >0.20 Females 3 80 60 either inoculated male and female rabbits (comparison IV) or uninoculated male and female rabbits (comparison V). Thus, N. brasiliensis significantly (P < 0.05) influences the weight gain of both male and female rabbits equally, through day 15 postinoculation. The exact mechanism(s) responsible for the diminished weight gain in rabbits infected with N. brasiliensis is not known. Current research is underway to elucidate the mechanism(s) involved. Nevertheless, the following evidence is presented as a possible explanation for the diminished weight gain observed in this host—parasite relationship. Harley (1966) and Harley and Gallicchio (1970) have shown that rabbits with heavy infections of N. brasiliensis were manifestly ill; had hemorrhagic, congested, and edematous lungs; and verminous pneumonia was common. Inflam- mation was also demonstrated in the skin and lungs of infected rabbits. In the present study, similar results were obtained. In rats, Symons (1957, 1960a, 1960b, 1960c, 1960d) and Gallagher and Symons (1959) have shown that in the small intestine, there are debilitating changes in the concentrations of fats and electrolytes. Symons (1960c, 1960d) has also shown that the rate of absorption of d-glucose and protein digestion is greatly reduced. All of the above are possible contributors to undernourishment and may possibly be occurring in rabbits infected with N. brasiliensis. For, it was observed in this investigation that rabbits infected with N. brasiliensis had a drastic loss of appetite; superficially, explaining the diminished weight gains. REFERENCES Gallagher, C. H., and L. E. A. Symons. 1959. Biochemical studies on Nippo- strongylus muris infestation. Austral. J. Exper. Biol. Med. Sci. 37:421-432. Haley, A. J. 1966. Biology of the rat nematode Nippostrongylus brasiliensis 64 John P. Harley (Travassos, 1914). III. Characteristics of N. brasiliensis after 30-120 serial passages in the Syrian hamster. J. Parasit. 52:98-108. Harley, J. P. 1966. The effect of cortisone on the establishment of Nippostrongylus brasiliensis (Nematoda) in the rabbit. Unpublished Master’s Thesis, Kent State University, Kent, Ohio, 68 p. Harley, J. P., and V. Gallicchio. 1970. Effect of cortisone on the establishment of Nippostrongylus brasiliensis in the rabbit. J. Parasit. 56:271-276. Snedecor, C. W. Statistical Methods. 5th ed. Iowa State University Press, Ames, Towa, 534 p. Symons, L. E. A. 1957. Pathology of infestation of the rat with Nippostrongylus muris (Yokogama). I. Changes in the water content, dry weight and tissues of the small intestine. Austral J. Biol. Sci. 10:374-383. . 1960a. Pathology of infestation of the rat with Nippostrongylus muris (Yokogawa). II. Chemical constituents of the jejunum and dry weight of the mucosa. Austral. J. Biol. Sci. 13:163-170. . 1960b. Pathology of infestation of the rat with Nippostrongylus muris (Yokogawa). III. Jejunal fluxes in vivo of water, sodium and _ chloride. Austral. J. Biol. Sci. 13:171-179. . 1960c. Pathology of infestation of the rat with Nippostrongylus muris (Yokogama). IV. The absorption of glucose and histidine. Austral. J. Biol. Sci. 138:180-187. 1960d. Pathology of infestation of the rat with Nippostrongylus muris (Yokogama). V. Protein digestion. Austral. J. Biol. Sci. 13:578-588. Thorson, R. E. 1953. Infection of rabbits with a rat nematode, Nippostrongylus muris. J. Parasit. 39:575. Travassos, L. 1914. Trichostrongylideos brazileiros (3. nota previa). Brazil Medico. 28:325-327. Received: April 21, 1971. Accepted: May 28, 1971. NEW RECORDS OF ZAPUS HUDSONIUS (ZIMMERMAN) FROM KENTUCKY JAMES T. WALLACE Department of Anatomy, School of Dental Medicine, University of Pittsburgh, Pittsburgh, Pennsylvania 15213 The jumping mice (Genus Zapus) are distributed widely over North America from about latitude 35°N to the Arctic Circle (Walker, 1964). In spite of their wide distribution, Zapus are often poorly represented in mam- mal collections. Such has been the case for collections from Kentucky where the genus has seldom been captured. This is probably a result of their low population densities in the wild, their habit of hibernating for several months of the year in cold climates and little effort in the field by collectors. Krutzsch (1954) listed a specimen of Zapus in the United States National Museum, from Lyon County in western Kentucky, with no exact locality record. This represents the only published record of Zapus from Kentucky. Krutzsch (ibid.) designated the (USNM) specimen as Zapus hudsonius intermedius. He considered Zapus hudsonius americanus to be present in the eastern half of Kentucky, but based his speculation on geographic criteria without the benefit of specimens. More recently several specimens of Zapus have been collected from the eastern part of Kentucky as well as a single specimen from western Kentucky. In addition, three specimens col- lected in 1964 in Oldham County, Kentucky were received from the De- partment of Biology, University of Louisville. All of the Kentucky specimens with the exception of the one in the USNM will be discussed in this presentation. Collections (Table I) of Zapus have been made in Madison County, Table 1 Collection Sites in Madison, Daviess and Oldham Counties Madison—1) 84° 24’ 6”, 37° 42’ 30” longitude, el. 680’ 3 mi. N. Kirksville. 2) 84° 28’ 45” latitude, 37° 47’ 45” longitude, el. 560’, near mouth of Silver Creek at Kentucky River and 4 mi. SW Valley View. Preserved in formalin, author’s collection. Daviess—Home of Mr. Albert Powell on Carpenter Lake. No other details available. Study skin and skull, Dept. Zool., University of Kentucky. No. 4132. Oldham—1 mi. N and 3 mi. E. of La Grange. Study skins with skulls, Dept. Biol. mammal collection, Univ. Louisville, KRT #47, 50 and 51. 9STh# TN L9, ‘PO SG pesemed= 61 “Tr ce 86 SOL 76 ~~ ices tcees Osi O\Om es | S0iGGs. Cle Sol (W) 89TT Ayonquey “AyuNoD uosipey, ‘JaAny AxonJUeY 3e YaoI-D IsAjIG Jo yNou rvaNy soAIquia ou L9. ‘PO &% SUP ONe Oc a0, alice 0G =O 66 -[co 88 €6 OF Ter SG OF —O0e 4 = 3 = n “d 3 oo & ° Kets) Re 9 20 C ostracod ) = 1 0 1 2 3 “ 5 6 T 8 9 WEEKS Fig. 1 - Adult population density of Cyclops viridis and Cypris virens cultured separately under three temperature regimes. > 10 + 20 C Cyclops 4 se me! od 3 oO & ° Aa 2 ° 3 = 10) al: 2 3 4 5 6 if 8 9 10 WEEKS Fig. 2 - Adult population of Cyclops viridis and Cypris virens cultured together under three temperature regimes. colder temperatures than at the higher levels. Sprague (1963) found that isopod and amphipod reproduction was greater at colder temperatures, as was body size when compared to higher levels. My results confirmed those of both McLaren and Sprague. Monakov (1958), working with the effects of temperature on freshwater invertebrates, found that organisms at colder temperatures had a longer life span and greater population density than those at higher temperatures. My results were similar to those of Dewey and Cole (1962) and Monakov. Transactions of Kentucky Academy of Science, Vol. 33, 1972 5 10 C ostracod 4000 3500 3000 2500 2000 1500 I 1000 20 C ostracod od d wo u Oo 500 a ©) 35 C ostracod 2 70% 30 15 10 C Cyclops 20 C Cyclops 35_C Cyclops ) 1 2 z 4 5 6 T 8 9 WEEKS Fig. 3 - Net production of Cyclops viridis and Cypris virens cultured together under three temperature regimes. The total net production (immature stages) of both copepods and ostra- cods cultured together at 10 C was greater than production at either 20 or 35 C (Fig. 3). Similarly, Monakov (1958) found that total net production, as well as life span, was greater at the colder temperature than at the warmer ones. Population density and production of irradiated copepods and ostracods grown together was greatest at the cold emperature and least at the high temperature (Figs. 4, 5, 6). The copepods did not reproduce following irradiation of 24, 48, and 96 kR, however, further investigation showed re- production did occur between 8 and 16 kR (Heaslip, pers. comm.). Adult population densities of irradiated copepods and ostracods grown together were greatest at 10 C and somewhat lower at 20 C, as were life span dura- 6 Transactions of Kentucky Academy of Science, Vol. 33, 1972 tions; there were significant decreases in both density and life span of irradiated species at the high temperature (Figs. 4, 5, 6). There was no significant mortality of adult copepods immediately follow- ing exposure to 24, 48, and 96 kR of gamma rays. Ostracod mortality, although not greatly affected by 24 kR of gamma rays, showed a significant increase at 48 and 96 kR (Table 1). TABLE 1.—Number of adult Cyclops viridis and Cypris virens per culture preceding (A) and following (B) exposure to 0, 24, 48, and 96 kR of gamma rays Radiation Level Organism A B 0 kR Cyclops winidis: (0385 Ses sharks eee ee 90 90 CUPTIS. OUT CNS Core ieiecre obese eee oe 30 30 24 kR Cyclops: Gigs o.0.) WEEKS Fig. 5 - Mean net production of Cyclops viridis and Cypris virens cultured together under three temperature regimes following exposure to 0 or 48 kR. effect of irradiation of freshwater crustacea with shortening of life span and adult mortality being secondary. My results support these findings. Com- bined eftects of irradiation and temperature stress resulted in a decreased life span at 35 C and an increased life span at 10 C over the life span at 20 C for all levels of irradiation tested. With the exception of slight adult copepod mortality immediately fol- Transactions of Kentucky Academy of Science, Vol. 33, 1972 9 Ae + 96 kR a ~ 7 = : 35 30 ane (0) » di qd od ze 20 cq “d =| u o 15 [or Le] o & Lo} g 410 3 GS > WEEKS Fig. 6 - Mean net production of Cyclops viridis and ris virens cultured together under three temperature regimes following exposure to O or 96 kR gamma rays. lowing gamma ray exposure at 96 kR, the adult survival was the same at all levels of irradiation. The ostracod survival was decreased 7% after exposure to 24 kR; 23% after exposure to 48 kR, and 47% after exposure to 96 kR. Marshall (1965), working with adult daphnia populations, found that radiation exposure levels below LD 50 had little or no effect on adult 10 Transactions of Kentucky Academy of Science, Vol. 33, 1972 TABLE 2.—Adult population density of gamma irradiated Cyclops viridis and Cypris virens grown at three temperatures No. of Weeks 0 1 2 35 C Organism 24 48 96 Gyclops: viridis. .....5:.sc-ees 10; 105710 (UTI OUNENS ceessees wtewceteceese By Gyclops viridis. .........0ccs00+ 10 10 10 Gypris) Cinens) eee eee 4 4 4 Gy Clo psig ov ccsccscaccsst ates 10. 10% 10 (COP OES BURGOS. cccescscecese sce Be ee Cyclops tATAdiss esl .ckos.sccee-s8es i nem iat Waar (CUT OUS) DUNGLOS. coooeosasoctneepscaccece DT DN eo, Cyclops viridis: ....ccccc.iceucte-o0ss 3 oo (CUT DUS EUROS cppcapsoscncachos sco 1 1 il Gyclops Viridis. ....c.cc0c.sccccess00s OG; 0" 20 (COIS SEGHADS Gonsoeaseoceosssosacsnoes 1 J I Cyclops viridis .cccccccccccsecec-o00s OFF yOu a0 (GIP DUOS EGWAUS coosconnacencosesco0 YY @ Cyclops viridis. ......0ccc.sc0cs-000: OOO GPITS OINENS We eceeeete nee eee Huy @ Cyclops wintdis shee Oe Ow) (COP OUDS ELRADS. -roscecnacnecscousncc oO @O © “Cyclops viridis, .......<.0c.00-.s0005- OOOO CDCR BERZOS copeonconconcocedsacoss Oe ee OF) 20 C 24 48 96 LO 1010 Dy Le) LOe LORELe 5) Pomme 10." LOt0 4 4 4 LO LO VLG 3 fon ane GC) Gr esG 3: Soe 4 4 4 Pee 52) 2! (Deane, Pees O © OF (Oneae OF ORC 0 > OFe70 0 Oe Oy Om 20 10C 24 48 96 10 5 10 5 10 KH SOON OCWrFRNAWAWOFK 10 5 — i= = — SOONOCOWrFANAWAWORS OU 10 5 10 5 10 — SOON OCOWFRAKBNAWAWOR mortality and that net production of irradiated daphnia at 20 C was not appreciably affected by radiation exposure levels. Results of this study sup- port those of Marshall. TABLE 3.—Control adult population density of Cyclops viridis and Cypris virens grown together at three temperatures No. of Weeks Organism 24 0 Gyclops wiridis ...<:.kescsc<-s--0e-s 10 (COPURES CERADS cncectccsseos.cos200007 5 1 Guyclopsiinidisi. ee 10 CUpiiseOinens eee 5 2 Guclops windis\ se 10 Gupristvirense ee 4 3 Cyclops voinidisc. 7 ee 10 WOJDTUS BURBDS: ccccsssosnocceoousenocs 2 4 Cyclops onidis 2... 6 COpOOS CORRS. sococaseacccss0000300008 1 5 Cyclonsmuindis en ee 1 CUpTiSROITEN See ee 0 6 Cyclopsioinidisse.: sen 0 (GUPBTUS UTES. soo-aeecnonens69soee006 0 a Cyclonsoinidism ee ee 0 Cuprissvirensie 0 8 Cyclopsmimdisne ee 0 (GOFOTUS BHRERS. concscasnseronneseoanned 0 9 Cyclops vindis We: 0 (COPDTES DURES” ssassxcnccceecosssi0007 0 35 C 48 10 5 10 HH SeooqooooocoorrFanoc pi SOOCOCCOCOCCOFRFRONOK 24 10 5 10 5 10 5 10 4 10 3 10 2 10 2 8 1 6 1 5 1 20 C 48 10 “5 10 5 10 5 10 96 = = — = i — = BOR ORrONONDGDWORhRCUCDUSOCWO 10 tk SCRODRANAWOROUSCUWS UL 10C 48 10 5 10 5 10 — SCRODHANAWOPH MOUS UW 10 — SCR ODRANAWAFKOUC UW Transactions of Kentucky Academy of Science, Vol. 33, 1972 11 ACKNOWLEDGMENTS I am deeply grateful for assistance in preparation and review of this manu- script from Candi Samsel; also, Drs. B. C. Parker, J. Cairns, Jr., and M. B. Heaslip, and to Morehead State University at which the research for this paper was com- pleted. LITERATURE CITED Beyers, R. J. 1962. Relationship between temperature and the metabolism of ex- perimental ecosystems. Science 136 (3520) :980-982. Beyers, R. J. 1965. The pattern of photosynthesis and respiration in laboratory microecosystems. Proceedings of the International Biol. Programme: Sym- posium on Primary Productivity in Aquatic Environments, Pallanza, Italy, April, 1965. 18 (supple.):61-74 [Rec’d., 1966]. Calkins, J. 1963. Variation of radiation sensitivity of Paramecium aurelia as a func- tion of time of irradiation in the interdivision growth cycle. Nature 198( 4881): 704. Chernykh, S. I., and T. D. Panasyuk. 1964. Distribution of Daphnia magna under conditions of temperature, oxygen, and light gradients. Zool. Zh. 43(11): 1715-1716. Dewey, W. C., and A. Cole. 1962. Effects of heterogeneous populations on radia- tion survival curves. Nature 194( 4829 ) :660-662. Engel, D. W., and D. J. Fluke. 1962. The effect of water content and postirradia- tion storage on radiation sensitivity of brine shrimp cysts (eggs). Radiat. Res. 16(2):173-181. Failla, P. Mc. 162. Some effects of radiation on rotifers irradiated at different ages. Radiat. Res. 16(4):573. Fontaine, Y. A., and A. Aeberhardt. 1963. Experimental laboratory study of the radioactive contamination by cesium-144 of a complex fresh water community. Health Phys. 9(11):1047-1056. Eng. Summ. Ghys, R. 1963. Metabolic factors on radiosensitivity. In: Symposum on Radio- sensitivity Quebec, 1962. Laval Med. 34(1):69-79. Eng. Summ. Hrbackova-Esslova, M. 1966. The differences in the growth and reproduction at 8° C. and 20° C. of Daphnia publicara Forbes (Crustacea: Cladocera) popu- lations inhabiting midland ponds and high Tatra likes. Vest. Spolemosti Zool. 39(1):30-38. Marshall, J. S. 1961. The effects of continuous gamma radiation on the intrinsic rate of natural increase of Daphnia pulex, Diss. Abst. 22( 2) :682-683. Marshall, J. S. 1962. The effects of continuous gamma radiation on the intrinsic rate of natural increase of Daphnia pulex. Ecology 43(4) :598-607. McLaren, I. A. 1963. The effects of temperature on growth of zoo-plankton, and the adaptive value of the vertical migration. J. Fish. Res. Bd. Can. 20(3): 685-727. McLaren, I. A. 1965. Some relationships between temperature and egg size, body size, development rate and fecundity of the copepod Pseudocolnus. Limnol. Oceanogr. 10(4):528-583. Monakoy, A. V. 1958. Some data on the biology of development and reproduction of Acanthocyclops viridus (Jur), (Copepoda, Cyclopoida). Doklady Acad. Nauk. SSSR Biol. Sci. Sect. [trans.] 119(1/6):291-294. Needham, J. G., Galtsoff, P. S., Lutz, F. E., and Welch, P. S. 1937. Culture Methods for Invertebrate Animals. Comstock Publishing Company, Ithaca, New York. 510 p. Rees, G. H. 1960. Effects of gamma irradiation on two decapod crustaceans, Palamonetes pugio and Uca pugnax. In: Proceedings of the 57th Annual Meeting of the North Carolina Academy of Science, 1960. J. Elisha Mitchell Sci. Soc. 76(2):191. 12 Transactions of Kentucky Academy of Science, Vol. 33, 1972 Reyment, R. A. 1963. Effect of certain environments on the carapace of the fresh- water ostracod Cypridopsis vidua (Muller). Nature 197( 4856) :787-788. Sprague, J. B. 1963. Resistance of four freshwater crustaceans to lethal high tem- perature and low oxygen. J. Fish. Res. Bd. Can. 20(2):387-415. Stroganov, N. S., and M. M. Telitchenko. 1959. Chronic influence of small doses of radioactive substances on successive generations of Daphnia magna. Bull. Mosk. Obshch. Ispoyt. Prirody. Otd. Biol. 64(1):154-155. Referat, Zhur; Biol. 1960. Ward, H. B., and G. C. Whipple. 1918. Freshwater Biology. John Wiley Sons, Inc. New York. 680p. Yamaguchi, T. 1963. Time changes in Na, K, and Ca contents of Paramecium caudatum after gamma irradiation. Onnot. Zool. Japan. 36(2):55-56. Received: August 9, 1971. Accepted March 9, 1972. Transactions of Kentucky Academy of Science, Vol. 33, 1972 13 A SURVEY OF THE HELMINTHS OF THE MUSKRAT, ONDATRA Z. ZIBETHICA MILLER, 1912, IN MADISON COUNTY, KENTUCKY JOHN P. HARLEY Department of Biological Sciences, Eastern Kentucky University, Richmond, Kentucky 40475 ABSTRACT From 100 muskrats collected in Madison County, Kentucky, three species of cestodes: Taenia taeniaeformis, Hymenolepis evaginati, and Monoecocestus americanus; six species of nematodes: Trichuris opaca, Trichostrongylus calcartus, Trichinella spiralis, Capillaria ransomia, Long- istriata dalrymplei, and Ascaris lumbricoides; and eight species of trema- todes: Quinqueserialis quinqueserialis, Notocotylus urbanensis, Echin- ostoma revolutum, Nudacotyle novicia, Pseudodiscus zibethicus, Plagior- chis proximis, Echinoparyphium recurvatium, and Paragonimus kellicotti were identified. All of the reported helminths constitute new range- extensions and state records for parasites of the muskrat. Numerous helminthological surveys of the muskrat Ondatra z. zibethica Miller 1912, have been made in North America, and consequently the hel- minth fauna of muskrats is well known (Anderson and Beaudoin, 1966). Several reports have summarized the literature up to 1967 (Beckett and Gallicchio, 1967; Knight, 1951; Meyer and Reilly, 1950). However, prior to this report, no helminthological work has been done on Kentucky musk- rats. Therefore, the objective of this investigation was to determine the species of helminths parasitizing muskrats in Madison County, Kentucky. During the 1970-71 Kentucky trapping season, fur dealers and trappers supplied skinned carcasses from Madison County. In addition, ten animals were trapped by the author. A total of 100 muskrats (57 males and 43 females) made up the survey. As obtained, muskrats were data-tagged, frozen and stored at —10 C until autopsied. All of the helminths recovered at autopsy (with the exception of nema- todes) were immediately fixed in hot A.F.A. Mayer’s paracarmine and Dela- field’s hematoxylin were used to stain the cestodes and trematodes. Fast- green in 95% ethyl alcohol was used to counterstain the ventral glands of the monostomes and the cephalic spines of the echinostomes; they were distinguished after clearing. Nematodes were cleared in warm glycerine and mounted in glycerine jelly. Finally, all diaphragms were digested with pepsin-HC]l in order to search for Trichinella spiralis. Three species of cestodes, six species of nematodes and eight species of trematodes were identified (Table 1). A total of 26 muskrats had only one species of helminth each (regardless of species). Two or more species occurred in 74 of the muskrats. Trematodes occurred in 81 muskrats while nematodes and cestodes occurred in 47 and 12 muskrats, respectively. No Acanthocephala were found. Both sexes were approximately parasitized to the same extent. Quinqueserialis quinqueserialis and Notocotylus urbanen- sis were the most prevalent trematodes, Taenia taeniaeformis the most preva- lent cestode, and Trichuris opaca the most prevalent nematode recovered. Echinoparyphium recurvatium has been reported from Minnesota musk- rats (Penner, 1940), from Maine muskrats (Meyer and Reilly, 1950) and Transactions of Kentucky Academy of Science, Vol. 33, 1972 14 aUNSezUT [PUIG 9UI}SOJUT osI1eT duns] ][eUulsg useiydeiq aUu}So}UT [[PUIS 9USOUT os1e'T aUuT}Sa}U] [[eUIS aUl}Sa}UT [[PWIS ausoyU] [[BUIS ssun'y auI}so}UT [[PUIS eunsayy [BUS euT}sayUy [Pus OUI}SOJUT os1e'T eunsa}UT [[eusg QUI}SOJUT IS81e'T aUSoUT os1e'T UOT}BOOT o}IsSeieg Il VG 6G 0€ LE 67 IL peyefur SyBIYSNUL fo Toquunyy Ayonjuay ‘Ayuno> uosippy wos syosysnw QQ] wWosy pasado0re4 syyuIWjay yo saidads—| 479gVL (aes i (SI-1)6 (LI-F)L (111-06) IF (1I-1)P (F-1)Z CS ee Ono SO Mm Ont r OS Ql Ol > at CID ri 09 soysered fo Jequinu oseieAy suiseviydetp ul s}sk_ , . osuey SGLT ‘Shevuury saploouqun siimosy CE6L ‘sueUIYIC 1ajdwhyop vo1.4s1B8U0T CI6I ‘Se4ON pue rayxIeg DNWOSUDL DILDO TIdDD xa(GE8T UWeMO) syouds vyjauryou T, TI6I ‘Wosuey snzo1v9]09 snpisuo4soyois 7, GI6I ‘SeAON pue ioyIeg vondo sniniyotw J VGOLVWAN (G68T ‘S9I9S) snupoiawp snysas0da0u0 CI6I ‘SMerpuy pue JoyxIeg DJDUIZDAA sisdajouawA O8LT Yosieg swu1ofapiuan, pian, VGOLSHO SO6I “PIEM 4709N]0y SnunUOsDIDg (ELET “Ado}spury UoA) wnyvainga, wniydhisdouryoq GIGI “oye svwixoid svyos0isy) J (SGI6I ‘sey pue JoyIeg) sno1yjaqiz snosipopnasg 9QI6T “eyxIe_ DIDIA0U ajhzooppnN, (ZO8T ‘Yorysory) wngnjoaas pwosouyoq (PIBI 40D) sisuaunqun smjhjzoo0j0N (TI6I ‘UyYysneyT pue soyeg) sypwasanbuinb sypiiasanbuin(d VGOLVWNAYL satoeds Transactions of Kentucky Academy of Science, Vol. 33, 1972 15 from Ohio muskrats (Beckett and Gallicchio, 1967). This present report is thus the fourth record of E. recurvatum from North American muskrats. Paragonimus kellicotti has only been reported from the lungs of Michigan muskrats (Ameel, 1932). This present report constitutes the second report of this species from North American muskrats. Rausch et al. (1956) reported encysted Trichinella spiralis from one Alaskan muskrat and Beckett and Gallicchio (1967) from one Ohio muskrat. This present report thus constitutes the third report of this species from North American muskrats and also, the greatest incidence so far reported. Ascaris lumbricoides has only been reported from Illinois muskrats (Gil- ford, 1954). This present report constitutes the second report of this large nematode from North American muskrats. Since no previous helminthological reports have been reported for Ken- tucky, all of the herein reported helminths constitute new range-extension and state records for parasites of the muskrat. When compared to surveys in two neighboring states (Illinois: Arata, 1959; Gilford, 1954; and Ohio: Beckett and Gallicchio, 1967; Rausch, 1946), it would appear from the re- sults of this present survey that Kentucky muskrats are parasitized with an above average helminthic burden. This relatively high degree of parasitism cannot necessarily be attributed to the size of the muskrat population in Madison County, however, since the relative abundance of intermediate hosts, feeding habits, and other epidemiological factors are unknown. Never- theless, this work extends our knowledge of the helminthofauna of a state that, to date, has been virtually untouched by parasitologists. LITERATURE CITED Ameel, D. J. 1932. The muskrat a new host for Paragonimus. Science. 75:382. Anderson, D. R., and R. L. Beaudoin. 1966. Host habitat and age as factors in the prevalence of intestinal parasites of the muskrat. Bull. Wildl. Disease Assoc. 2:70-76. Arata, A. A. 1959. Ecology of muskrats in strip-mine ponds in southern Illinois. J. Wildl. Mgmt. 23:177-186. Beckett, J. V., and V. Gallicchio. 1967. A survey of helmints of the muskrat, Ondatra z. zibethica Miller, 1912, in Portage County, Ohio. J. Parasit. 53: 1169-1172. Gilford, J. H. 1954. A survey of helminths in Illinois. J. Parasit. 40:702-703. Knight, I. M. 1951. Disease and parasites of the muskrats (Ondatra zibethica) in British Columbia. Can. J. Zool. 29:184-215. Meyer, M. C., and J. R. Reilly. 1950. Parasites of muskrats in Maine. Am. Mid. Nat. 44:467-477. Penner, L. R. 1940. Morphological and biological studies on certain helminths of the muskrat. Ph.D. dissertation. Univ. of Minnesota, 275 p. Rausch, R. 1946. The parasites of Ohio muskrats. J. Wildl. Mgmt. 10:70. Rausch, R., B. B. Babero, R. V. Rausch, and E. L. Schiller. 1956. Studies on the helminth fauna of Alaska. XXVII. The occurrence of larvae of Trichinella spiralis in Alaskan mammals. J. Parasit. 42:259-271. Received: December 12, 1971. Accepted March 8, 1972. 16 Transactions of Kentucky Academy of Science, Vol. 33, 1972 SOME OBSERVATIONS ON BACTERIAL POPULATIONS IN WILGREEN LAKE, MADISON, KENTUCKY R. B. OTERO Department of Biological Sciences Eastern Kentucky University Richmond, Kentucky 40475 S. LEUNG Department of Geology Eastern Kentucky University Richmond, Kentucky 40475 INTRODUCTION Lake Wilgreen (Taylor Fork Lake), 5 miles south of Richmond, Madi- son County, Kentucky, and formed behind a 650-ft long by 75-ft high rolled-earth dam across Taylor Fork Creek, has a total area of 175 acres. The lake has a 9,000-acre watershed, 90% of which is in pasture (on which subdivisions are located) and 10% in woodland. The lake is approximately 6 years old (dam completed, August 1966). This study on the bacterial pollution of the lake was begun 19 September 1970, and terminated 26 May 1971. Experimental samplings were secured from the lake itself and from tributaries flowing into it (Fig. 1). The pur- pose of this study was to determine the extent of bacterial populations in the lake, and their sources. MATERIALS AND METHODS Collection of Samples A total of 10 samples was collected at each interval. The samples were ob- tained in sterile 250-ml screw-capped Erlenmeyer flasks. The surface samples were collected by inserting the closed flask approximately 1 inch below the sur- face and opening the flask. The flask was immediately closed and stored for later microbiological analysis. Water temperatures were recorded at the time of sam- pling. Deep samples were obtained with a Kemmerer deep-water sampler ( Wild- life Supply Co., 1200-ml capacity), and the water samples obtained were poured into sterile 250-ml screw-capped Erlenmeyer flasks. All samples were studied for bacterial content within 3-4 hr after the last sample was taken. Bacteriological Examination All samples were examined bacteriologically by the Millipore membrane filter method as follows: 1. Total coliform: A sterile membrane filter (porosity 0.454) was aseptically inserted into a Millipore filtering apparatus. The water sample (diluted according to type of sample collected) was poured into the apparatus and vacuum was ap- plied to start filtration. After filtration, the apparatus was rinsed with 50 ml of sterile phosphate buffer (34 g KH.PO, in 500 ml of distilled water, adjusted to pH 7.2. This stock buffer (1.25 ml was added to 1 liter of distilled water and autoclaved in various aliquots, 50 and 100 ml, at 15 lb pressure for 15 min). The filter was removed aseptically and transferred to a 47-mm diameter plastic Petri dish containing a sterile absorbent pad saturated with 2.0 ml of MF-endo broth Transactions of Kentucky Academy of Science, Vol. 33, 1972 17 (BBL). The Petri dish was placed in an incubator at 37 C for 24 hr. Colonies that formed on the filter membrane were counted directly in the Petri dish using an electric counter. Only dark or metallic-sheened colonies were counted. The maximum acceptable number for a lake such as Wilgreen in Kentucky is 1,000 organisms/100-ml sample (Proposed Standards for Water Quality, Kentucky Water Pollution Commission, 1971). 2. Fecal coliform: The sample was treated as above except the membrane filter was placed into a plastic Petri dish on an absorbent pad saturated with 2.0 ml of M-FC broth (BBL) and incubated in a plastic bag at 44.5 C. This tempera- ture was used to select only for fecal coliforms. Fecal coliform colonies appeared blue, while nonfecal coliform colonies were gray to cream colored. The maximum acceptable number for a lake such as Wilgreen in Kentucky is 200 organisms/100- ml sample. 3. Fecal streptococci: The sample was treated the same as in total coliform except that the membrane was inserted into a plastic Petri dish containing M-enterococcus agar (BBL). The plates were incubated for 48 hr at 37 C. Only the colonies that appeared red on the surface of the membrane filter were counted. The colonies appeared red because the indicator system triphenyltetrazolium chloride (TTC) was reduced by the organism. There is no maximum acceptable range for this group of microorganisms. 4. Pseudomonads: The membrane was placed in a Petri dish containing pseudosel agar (BBL) and incubated for 24-48 hr at 37 C. Pseudomonads ap- peared green on the surface of the membrane filter. 5. Salmonella and Shigella species: The membrane was inserted into 5 ml of selenite (BBL) broth after filtration of 100 ml undiluted sample and incubated for 16-18 hr at 37 C. Subcultures were made on the following plating media: (a) brilliant green agar (BBL); (b) Salmonella-Shigella agar (BBL); (c) eosin methylene blue agar (BBL); MacConkey agar (BBL); and bismuth sulfite agar (BBL). These plates were incubated for 24 hr and suspected colonies were sub- cultured on the following biochemical media: (a) triple sugar iron (BBL); (b) Simmon citrate agar (BBL); (c) SIM agar (BBL); and (d) lysine iron agar (BBL). If the reactions were questionable, typing sera for Salmonella and Shigella species were used. RESULTS AND DISCUSSION Samples were obtained from the following Stations (Fig. 1, Table 1): 6, near the dam site; 18 and 19, at upper and lower points near Caleast tributary; 34, opposite Caleast junction; 35, opposite Caleast junction near- est the dam; 8 and 7, at upper and lower points near Old Town Branch; 9, junction at Deacon Hill tributary; and 9A, upper end of Wilgreen Lake. The largest numbers of total and fecal coliforms were obtained from Old Town Branch, Stations 7 and 8 (Table 1). As expected, deep samples as well as temperate waters (10-20 C) showed the highest counts. For ex- ample, the station at the lower point on Old Town Branch-Wilgreen Lake junction (7) showed total coliform counts ranging from 11,000 (7 November 1970; 22 ft; 10 C) to 180,000 (21 November 1970; 23 ft; 10 C), whereas the upper Station (8) showed 4,000 (7 November 1070; 10 ft; 14 C) to 4,200,000 (7 November 1970; 20 ft; 10 C). Fecal counts had a wider range, from less than 100 per sample tested to 2,800, the latter occuring in Novem- ber at Station 8. Samples from Old Town Branch contained large numbers of total and fecal coliforms in both the surface and deep samples (Table 2). The total coliform ranged from 14,000 to 510,000, the latter in November. The fecal 18 Transactions of Kentucky Academy of Science, Vol. 33, 1972 > ° -O,oO ° nz=wuZz =) naw Nn maro wo2zs 258 5 4 Zz (3) 2 < =) x ra) 7) We. S r) ANCASTER [41 WOODS ESTATE 40 39 25 L DEACON HILLS SUBDIVISION est AEROFLOW DISPOSAL PLANT HAINES Zz Pre i — ro) [a4 =~ oe bo, y y S17 zy © 257 262 a DE, 2.5 1.9 205 (246) Dey 257 263 — 1.0 1.2 1.6 1.8 2, 2-pyridine- — 241¢ 253 259 265 — carboxaldehyde Di 2.6 3.0 BAD 205 (240) . (254) 259 265 = 2.8 ais) Ae D5 all 2-pyridine- 2174 — (259) 264 (270) sa carboxylic acid ead 3.8 4.1 Sul 216 wi (258) 263 (270) Sra 14 7.4 8.0 6.0 6-chloro-2-pyridine- 220e — — — 274 — carboxylic acid 1.3 0.87 218 — —- (2TTE) QT4 (280) 5.8 3.6 3.8 3.0 2,6-pyridinedi- (215)? — — (265 ) 269 (275) carboxylic acid 9.5 3.6 8.9 al | “306 220 (261) oe 269 (275) 9.2 Cail 2.6 Sav 2.9 (a) Solvent is methanol unless otherwise stated. Wavelengths enclosed in paren- theses indicate a shoulder rather than a band maximum. (b) Sadtler Standard Ultra Violet Spectra, Sadtler Research Laboratories, 3316 Spring Garden Street, Philadelphia, Pennsylvania, Spectrum No. 9. Slit 0.60 mm. (c) See reference b No. 9306. (d) See reference b No. 1090. (e) See reference b No. 16277. (£) See reference b No. 5542. eliminate any possible error from the above considerations, molar ab- sorptivities on compounds were compared only when all of the above considerations were constant. The structure of carboxylic acids in solutions are complicated by the fact that dimers, both linear and cyclic, as well as polymers, are possible. The following facts are well established: (a) carboxylic acids exist as dimers except in dilute solutions (3), (b) the stronger the carboxylic acid, the weaker are the hydrogen bonds formed between the acid molecules (10), and (c) in media with high dielectric constant, whose molecules 66 Transactions of Kentucky Academy of Science, Vol. 33, 1972 Table 2 The Ultraviolet Spectral Data® of 6-Substituted 2-Pyridinecarboxylic Acids in Methanol and Water oe ( nm ) emaxe Lo Compound Band 1 Band 2 6-methyl-2-pyridine- 218 — — — 272 carboxylic acid 18 11 204b — 260 — ote ll 13 2-pyridinecarboxylic 216 — (258) 263 (270) acid 14 7.4 8.0 6.0 204» — 260 (265) — 11 13 11 6-bromo-2-pyridine- 223 — — — 277 carboxylic acid 6.2 4.2 215» — — (267) 274 7.8 4.2, 5.1 2-chloro-2-pyridine- 218 — —— (271) QT4. carboxylic acid 5.8 8.6 3.8 216» — — (269 ) 274 ll 7.6 8.8 6-nitro-2-pyridine- 212 230 — — 272 carboxylic acid 12 5.6 3.3 205> (230) — — — 59 17 2,6-pyridinedi- 206 220 (261) — 269 carboxylic acid 9.2 Tet 2.6 3.7 (215)> — — (270) 273 12 9.3 9.6 6-acetamido-2-pyridine- 212 244 — — — carboxylic acid 34 21 206» 239 — — 285 17 8.6 5.9 6-methoxy-2-pyridine- 205 228 — — 287 carboxylic acid 5.1 6.0 6.1 — 223b — (281) 284 Ee, 5.7 6.0 6-amino-2-pyridine- 207 2492 — — — carboxylic acid 9.9 6.9 203» 240 — —— — 24 9.2 (a) See reference a Table 1. (b) Solvent is water. Transactions of Kentucky Academy of Science, Vol. 33, 1972 67 themselves have a marked tendency to form hydrogen bonds, the solvent molecules cause a disruption of the hydrogen bonds between solute mole-. cules (6). Thus for a weak acid (pyridinecarboxylic acid), in dilute solu- tions (10-°M) of solvents with high dielectric constant (¢«) and strong hydrogen bonding ability such as methanol (¢ = 32) and water (¢ = 78), monomers are present (5,11,12). Usually, 2-pyridinecarboxylic acid may be considered to have an elec- tronic structure similar to that. of 2-pyridinecarboxaldehyde since the acid carbonyl group, C=O, is isoelectronic with the aldehyde group. 2-Pyridine- carboxaldehyde has intense absorption bands at 265nm (emax 2100), 259nm (émax 2000), and 254nm (enax 2200). The spectrum of 2-pyridinecarboxylic acid has a shoulder at 270nm (ema, 6000), a peak at 263nm (e,,; 8000), and a shoulder at 258nm (¢,x 7400). Comparison of the intensities (Table 1) of the absorption bands indicate that they are increased in the acid reflecting differences in their electronic structures. We compared the spectra of 2-pyridinecarboxylic acid with a number of its derivatives. The ultraviolet spectral data in methanol and water of these compounds are shown in Table 2. The most probable three structures CHART I Ha oO uaa gl ie Na CODH Nee I Il Il for 2-pyridinecarboxylic acid are shown in Chart I. The planar structure (II) depends on the availability of electron density on the ring nitrogen. The ultraviolet spectra of I or III would not be expected to change in a systematic way with a change ofelectron density on the ring nitrogen. Thus structure II can be distinguished from structure I or III by changing the electron density on the ring nitrogen and observing these uv spectra. When studying electron density vs. substituent effect one approach is to consider Hammett (cp) relationships; however, the choice of o values must be theoretically resolved if possible. Substituents at the 6-position could affect the electron density on the ring nitrogen in the following ways: (a) resonance effects, (b) field effects, (c) inductive effects, and (d) steric effects. The resonance effect of 6-substituents on the electron density is not very large. Sigma, («), which measures mainly resonance effects, shows a poor correlation for ionization of 2-substituted pyridines in water; however, excellent correlation is found with the 4-substituted pyridines. Sigma induction, (o;), which measures inductive and field effects, gave good correlation with the 2-substituted pyridines. These results show that 68 Transactions of Kentucky Academy of Science, Vol. 33, 1972 substituents in the 4-position on a pyridine ring have the expected electrical effects, whereas substituents in the 2-position behave abnormally and do not show the type of electrical effect customarily exerted by an o-substituent. It is believed that the short range inductive effect on the nitrogen electron density accounts for the correlation of the 2-substituted pyridines (2). A substituent constant which measures inductive effects even more ef- ficiently than o; is o’: The o’ constants are almost the same as the a, constants; although, much of the field effect present in o; is eliminated in o’ (7). Thus if the electron density on the ring nitrogen is affecting the structure of 2-pyridinecarboxylic acid, a relationship between o’ and molar absorptivity should be found. Table 3 Low Energy Absorption Maxima (nm) and ¢,,,, Walues of These Pyridinecarboxylic Acids in Methanol and Water Methanol Water Compound max Fae ates repels 6-methyl-2-pyridine- 272 11 278 8.1 carboxylic acid 2-pyridinecarboxylic 263 8.0 260 13 acid 6-bromo-2-pyridine- 277 4.2 274 onl carboxylic acid 6-chloro-2-pyridine- 274 3.8 274 8.8 carboxylic acid 6-nitro-2-pyridine- 272 3.3 OT 12 carboxylic acid 2,6-pyridinedicar- 269 8.1 273 9.6 boxylic acid 6-acetamido-2-pyridine- 290 11 285 5.9 carboxylic acid 6-methoxy-2-pyridine- 287 6.1 284 6.0 carboxylic acid 6-amino-2-pyridine- 815 5.3 315 9.2 carboxylic acid Table 3 shows the Amax and emax Of the low energy band for these acids. We find that as the inductive effect of the substituent (o’) increases the enax decreases for the first five compounds in the Table (i.e., R=CHs, H, Br, Cl, NO,). Therefore, it is reasonable to assume that the ring nitrogen electron density is affecting ¢,,x. As the electron density on the ring.nitrogen is decreased, one would expect structure II to be less favor- able. This would result in decreased planarity of the molecule and low molar absorptivities. The acids with the large substituents would not be expected to follow this trend in molar absorptivities. Large groups sterically hinder the forma- Transactions of Kentucky Academy of Science, Vol. 33, 1972 69 tion of structure II. When considering this effect, we must envision rotation about all bonds in the substituent, since the rotations take place at a rapid rate. This is the case with the acetamido and methoxyl groups. The 2-pyridinedicarboxylic acid is different, although the steric problem is still present. Now either group can form structure II. It will be noted that this molar absorptivity falls between the chloro and nitro group. The o’ constant for the carboxyl substituent is 0.32, for the Br substituent is 0.45, and for the Cl substituent is 0.47. If the carboxyl group belongs in the above generalization then its molar absorptivity should be greater than the one for the bromo compound. Since it is not, steric interference to formation of the N-H interaction must be the dominant factor. The amino group has long been known to be abnormal in any kind of relation- ship between 6-substituents and electronic ability (2,8), thus, it is not surprising to see that it does not fit into this generalization. The substituent effects on structure I or III are not obvious. However, no meaningful relationship can be found between ¢,,,, and o constants in Table 3. Thus, in contrast to methanol, there is no systematic change in €max With substituent in water. Either structure I or III could be used to explain these results; however, since previous investigators have found that in water the zwitterion predominates, we feel our data support this view. In conclusion, our data agree with other evidence that in water, structure III is the predominate species. However, in methanol we find evidence that structure II is present; this does not agree with Stevenson and Sponer (12). The basis of the disagreement may lie in the method of obtaining the molar absorptivity of the cation of 2-pyridinecarboxylic acid (14). Nomenclature « represents the dielectric constant; emax represents the molar absorp- tivity, emax = A/lc; emax represents the wavelength (nm) of maximum absorption; g represents Hammett substituent constant; o; represents Taft (13) substituent constant; and o’ represents an inductive substituent constant (7). LITERATURE CITED 1. Cantwell, N. H. and Brown, E. V., J. Amer. Chem. Soc., 74, 5967 (1952). Charton, M., J. Amer. Chem. Soc., 86, 2033 (1964). 3. Coutts, R. T., “Pharmaceutical Chemistry,” Vol. II, L. G. Chatten, Ed., Marcel Dekker, New York, N.Y., 1969, p. 85. 4, Evans, R. F., Herington, E. F. G. and Kynaston, W., Trans. Faraday Soc., 49, 1284 (1953). 5. Green, R. W. and Tong, H. K., J. Amer. Chem. Soc., 78, 4896 ( (1956). 6. Harrow, B. and Mazur, A., “Textbook of Biochemistry,” 9th Ed., W. B. Saunders Co., Philadelphia, Penn., 1968, p. 63. 7. Kosower, E. M., “Physical Organic Chemistry,” Wiley, New York, N.Y., 1968, p. 49. Moser, R. J. and Brown, E. V., J. Org. Chem., 36, 454 (1971). 9. Moser, R. J. and Brown, E. V., J. Heterocycl. Chem., 8, 189 (1971). 10. Murty, T. S. S. R. and Pitzer, K. S., J. Phys. Chem. 73, 1426 (1969). bo & 70 elk, 12. 13. 14. Transactions of Kentucky Academy of Science, Vol. 33, 1972 Otsuji, Y., Koda, Y., Kubo, M., Furukawa, M. and Imoto, E., Nippon Kagaku Zasshi, 80, 1298 (1959); Chem. Abstr., 55, 6576 (1960). Stephenson, H. P. and Sponer, H., J. Amer. Chem. Soc., 79, 2050 (1957). Taft, R. W. and Lewis, I. C., J. Amer. Chem. Soc., 80, 2436 (1958). Thamer, B. J. and Voigt, A. F,, J. Phys. Chem. 56, 225 (1952). Received: August 25, 1972. Neeeated October 18, 1972. Transactions of Kentucky Academy of Science, Vol. 33, 1972 71 CAPTURE OF THE ALFALFA WEEVIL, HYPERA POSTICA (GYLLENHAL), IN ILLUMINATED STICKY TRAPS? GARY E. CRUM Department of Entomology, University of Kentucky, Lexington, Kentucky 40506 The capture of flying alfalfa weevils using light traps was proven largely ineffective by Whitmer (1968). The present study attempted to ascertain the effectiveness of ground-situated sticky traps in capturing crawling alfalfa weevil adults. Preliminary laboratory tests suggested light as a possible weevil attractant for use in such traps. MATERIALS AND METHODS Thirteen hollow 1-ft cubes were constructed of plywood, each with one vertical side missing for an opening through which weevils could enter. Stikem® (Michel and Pelton Co., Emeryville, Calif.) was spread inside the cubes to entangle any insect which entered. A light socket was installed in 7 of the 13 traps at the center of the side opposite the open side. The outside surface of each trap was covered with plastic for protection against the weather. Both types of traps were placed in each of 2 University of Kentucky alfalfa fields. An area approximately 2 ft square was cleared of plants before the open side of each trap. The traps were inspected weekly for entangled alfalfa weevils and for loss of Stikem. The tests ran from March 9 to November 23. The light sources utilized were incandescent bulbs which ranged in wattage from 7 to 25 watts. The majority of traps were installed with 25-watt white-frosted bulbs (Ken-Rad Lamp Dept., Owensboro, Ky.). RESULTS The total number of trap days (number of traps X number of days in the field) for the lighted and unlighted traps equalled 1,236 and 895, respectively. Nonoperative bulbs, electricity outages, and harvest opera- tions caused some minor interruptions over the test period. The total -number of adult alfalfa weevils caught in the lighted and unlighted traps was 202 and 54, respectively, or averages of 0.163 weevil and 0.060 weevil per trap day, respectively. A chi-square test upheld the significance (.01 level of this difference. The test period covered many trap days during which there was little or no weevil movement (e.g. March, July, and August). Peak response to the traps occurred during May and June. CONCLUSION The results seem to warrant using ground-situated sticky traps with lights installed for alfalfa weevil surveys. 1 The investigation reported in this paper (No. 72-7-96) is in connection with a project of the Kentucky Agricultural Experiment Station and is published with approval of the Director. 72, Transactions of Kentucky Academy of Science, Vol. 33, 1972 REFERENCE CITED Whitmer, G. L., 1968. Field observations of the migration and flight habits of the alfalfa weevil, Hypera postica (Gyllenhal), in Kentucky. Unpublished M.S. thesis. University of Kentucky, Lexington, Ky. 73 p. Received: July 2, 1972. Accepted: August 2, 1972. Transactions of Kentucky Academy of Science, Vol. 33, 1972 3 A PRELIMINARY LIST OF THE FISHES OF THE LAND BETWEEN THE LAKES, CUMBERLAND AND TENNESSEE RIVER DRAINAGES, KENTUCKY? BY VINCENT H. RESH, CLAUDE R. BAKER? AND WILLIAM M. CLAY Department of Biology, University of Louisville The National Recreation Area known as the Land Between the Lakes (LBL) is a narrow strip of hilly land about 5 to 8 miles wide and ap- proximately 40 miles long, between impounded portions of the Tennessee and Cumberland rivers in western Kentucky and Tennessee. It is bordered on the west by Kentucky Lake, on the north and east by Lake Barkley (and a navigation canal connecting the two lakes), and on the south by U. S. Highway 79 in Tennessee. Kentucky Lake was impounded in the Tennessee River by the Tennessee Valley Authority in 1944, and Lake Barkley in the Cumberland River by the U. S. Army Corps of Engineers in 1965. Both impoundments were formed for multiple-use land management, flood control, recreation, and as a source of hydroelectric power. These two impoundments are the site of important fisheries, both com- mercial and recreational. A large number of sport fisherman utilize the Land Between the Lakes as a center of activity. Students and sportsmen have been impressed with the diversity and abundance of fishes in this region, but no list of species was available. During three recent summers while conducting a course in aquatic biology, we made collections and began the preparation of a preliminary list of species for the entire area. Although the impoundments of the Tennessee and Cumberland rivers have greatly changed the available habitats, earlier species lists are of historical interest and may serve as a point of comparison. The first century of ichthyological exploration in Kentucky began with the work of Constantine Samuel Rafinesque in 1818, and was reviewed and summarized by Ever- mann (1918). In that paper, he omitted the summary of Woolman’s (1892) work, but included Woolman’s collection records (pp. 333-361) and the list of waters examined (pp. 299-304), and tabulated the distribution of the species according to principal stream systems. Although two of the river systems reported by Evermann are the lower Tennessee and Cumber- land river basins, respectively, the latter extended upstream to Cumberland Falls. Therefore, the list of 94 reported species included a number of high-gradient headwater forms, particularly minnows and darters which in historical time probably have not occurred near the Land Between the Lakes. In addition to Rafinesque’s records, most of which must be disregarded due to a lack of definitely known localities, only two collections were made near the LBL area. Both were made in 1890 by Woolman, who had studied under both Evermann and David Starr Jordan, and an assistant, Hiram W. Monical, a student at Indiana University. Rafinesque’s only specific designation of a locality within this area gives credit to another 1 Contribution No. 156 (New Series) from the Department of Biology, Uni- versity of Louisville, Louisville, Kentucky 40208. 2 Present address: University of Illinois, Dixon Springs Agricultural Center, Simpson, Illinois 62985. 74 Transactions of Kentucky Academy of Science, Vol. 33, 1972 man as the collector: “Semotilus (?)notatus Cumberland River and Little River, a branch of it. (Collector, Mr. Wilkins)” (Rafinesque 1820:86). On 26 July 1890, Woolman and Monical seined a sandbank in the Cumberland River 1.25 miles south of Kuttawa, Lyon County, Kentucky, “the only place in this part of the country where the river could be fished successfully with a small seine, the banks being generally precipitous and the water deep” (Woolman 1892:262), taking a total of 37 species, including 5 species of darters. The now uncommon lake sturgeon, Acipenser fulvescens Rafinesque (recorded as Acipenser rubincundus Lesueur), was noted to be “common; several specimens taken” (p. 262). Two days later, they seined a sand bar in the Tennessee River, about 3 miles upstream from Paducah, Kentucky, where they took 18 species, including 2 species of darters. Acipenser rubicundus was found to be “very common in quiet water” (Ibid.:268). Those collections of Woolman contained some species collected during the present study, but did not include others (Table 1). Because of nomenclatorial changes, some synonymies of species names used by Wool- man are indicated. We did not include all synonymies because all specimens were not available to us. The last major preimpoundment study of the fishes of this region was made by Dr. Carl L. Hubbs, to evaluate the changes in the ichthyofauna following the impoundment of the Tennessee River to form Kentucky Lake. The unpublished species list that resulted from that study was revised in 1943, and included 176 species. In studies on the fishes of western Ken- tucky, Sisk (1969a; 1969b) did not include collection records from the Tennessee or Cumberland rivers. The present list is from collections made in July 1969, 1970, and 1971 during field sessions of the National Science Foundation Summer Institute “The Science of Inland Waters.” The sites sampled within the Land Between the Lakes area were: Honker Bay and Pisgah Bay (Lyon Co.), and Energy Lake, Crooked Creek, Ferguson Springs, Shaw Branch, and Barnes Hollow Creek (Trigg Co.). Collections in Pisgah Bay were made in 1972 with sport fishing tackle. Additionally, we sampled three locations outside the recreation area, Beechy Creek, Donaldson Creek, and Little River (Trigg Co.), but within the Lake Barkley Drainage. Collecting gear consisted of an experimental gill net, a 12-volt Smith- Root Electroshocker, fry nets, seines, trotlines, hook and line, and combina- tions of these sampling techniques. A single specimen of hog sucker, Hypentelium nigricans (Lesueur), was taken by hand while the fish was floundering in shallow water. This list is not intended to be an exhaustive survey of the LBL region. A complete list will certainly include more members of the Cyprinidae, Percidae, and possibly the paddlefish, Polyodon spathula (Walbaum), which has been taken in this region by local fishermen. Evermann (1918) reported additional darters from this drainage. Our list of 53 species of fishes, referable to 18 families, gives the location, relative abundance, and method of capture, and follows the nomenclature of A List of Common and Scientific Names of Fishes from the U. S. and Canada (Third Edition, 1970), published by the American Fisheries Society. The common shiner, Notropis cornutus chrysocephalus is considered as a subspecific form ac- cording to Resh et al. (1971) and Miller (1968). Transactions of Kentucky Academy of Science, Vol. 33, 1972 15 We thank the following for their assistance in this study: the participants of the NSF summer institutes of 1969, 1970, 1971; Drs. Donald Distler, University of Wichita; Robert D. Hoyt, Western Kentucky University; Louis A. Krumholz and Stuart E. Neff, University of Louisville; Charles R. Liston, Michigan State University; and Mr. Edward Veasey of the Tennessee Valley Authority. The Tennessee Valley Authority extended permission to collect fishes in this area. LIST OF SPECIES Family LEPISOSTEIDAE Lepisosteus oculatus (Winchell), spotted gar One speciman collected in gill net in Honker Bay. Lepisosteus platostomus (Rafinesque ), shortnose gar Collected by hook and line in Pisgah Bay. Family AMIIDAE Amia calva L., bowfin One speciman collected by hook and line in Honker Bay. Family CLUPEIDAE Alosa chrysochloris (Rafinesque ), skipjack herring Abundant in both seine and gill net collections in Energy Lake and Honker Bay; collected by hook and line in Pisgah Bay. Dorosoma cepedianum (Lesueur), gizzard shad Abundant in seine, gill net, and fry net collections in Energy Lake and Honker Bay. Dorosoma petenense (Giinther), threadfin shad Abundant in seine, gill net, and fry net collections in Energy Lake and Honker Bay. Family ESOCIDAE Esox americanus vermiculatus Lesueur, grass pickerel Several specimens collected by seining and electrofishing in Crooked Creek and Shaw Branch. Esox niger Lesueur, chain pickerel A single speciman collected by seining in Beechy Creek. The specimen escaped. Family CYPRINIDAE Cyprinus carpio L., carp Common in seine collections in Energy Lake and Honker Bay. Notemigonus crysoleucas (Mitchill), golden shiner Rare. Collected by seining in Barnes Hollow Creek and Crooked Creek. Notropis atherinoides Rafinesque, emerald shiner Common in seine collections in Honker Bay. Notropis cornutus chrysocephalus (Rafinesque ), common shiner Common in seine and electrofishing collections in Barnes Hollow Creek and Creeked Creek. Notropis umbratilis (Girard ), redfin shiner Rare. Collected by seining and electrofishing in Creeked Creek and Beechy Creek. Campostoma anomalum (Rafinesque ), stoneroller Abundant in seine and electrofishing collections in Barnes Hollow Creek, Crooked Creek, and Shaw Branch. Semotilus atromaculatus (Mitchill), creek chub Abundant in seine and electrofishing collections in Barnes Hollow Creek and Crooked Creek. 76 Transactions of Kentucky Academy of Science, Vol. 33, 1972 Rhinichthys atratulus (Hermann), blacknose dace Abundant in seine and electrofishing collections in Barnes Hollow Creek and Crooked Creek. Pimephales notatus (Rafinesque ), bluntnose minnow Common in seine collections in Barnes Hollow Creek, Shaw Branch, and Honker Bay. Family CATOSTOMIDAE Carpiodes cyprinus (Lesueur ), quillback One specimen collected by seining in Barnes Hollow Creek. Ictiobus bubalus ( Rafinesque ), smallmouth buffalo One specimen collected by hand along the shore of Honker Bay. Moxostoma erythrurum (Rafinesque), golden redhorse Common in seine collections in Shaw Branch and Barnes Hollow Creek. Minytrema melanops (Rafinesque), spotted sucker Common in electrofishing collections in Energy Lake and Beechy Creek. Hypentelium nigricans (Lesueur), hog sucker One specimen collected by hand in Beechy Creek. Catostomus commersoni (Lacépéde), white sucker Common in electrofishing collections in Beechy Creek and Crooked Creek. Erimyzon oblongus (Mitchill), creek chubsucker Rare. Collected by seining and electrofishing in Barnes Hollow Creek and Crooked Creek. Family ICTALURIDAE Ictalurus punctatus (Rafinesque), channel catfish Common in hook and line and trotline collections in Energy Lake, Honker Bay, and Pisgah Bay. Ictalurus melas (Rafinesque), black bullhead Abundant in seine and hook and line collections in Barnes Hollow Creek, Beechy Creek, Energy Lake, and Honker Bay. Ictalurus natalis (Lesueur), yellow bullhead Common in hook and line, seine, and electrofishing collections in Donaldson Creek, Beechy Creek, Energy Lake, and Honker Bay; collected by hook and line in Pisgah Bay. Pylodictis olivaris (Rafinesque), flathead catfish Collected by hook and line in Honker Bay. Family AMBLYOPSIDAE Chologaster agassizi Putnam, spring cavefish Sighted in Ferguson Spring by William M. Clay. Family APHREDODERIDAE Aphredoderus sayanus (Gilliams), pirate perch Common in seine collections in Barnes Hollow Creek and Crooked Creek. Family CYPRINODONTIDAE Fundulus olivaceus (Storer), blackspotted topminnow Common in seine and electrofishing collections in Barnes Hollow Creek, Crooked Creek, and Ferguson Spring. Family POECILIIDAE Gambusia affinis (Baird and Girard ), mosquitofish Abundant in seine collections in Barnes Hollow Creek, Crooked Creek, and Beechy Creek. Family ATHERINIDAE Labidesthes sicculus (Cope), brook silverside Abundant in seine and electrofishing collections in Barnes Hollow Creek, Crooked Creek, Beechy Creek, and Honker Bay. Transactions of Kentucky Academy of Science, Vol. 33, 1972 (ws Family PERCICHTHYIDAE Morone mississippiensis Jordan and Eigenmann, yellow bass Abundant in gill net collections in Honker Bay; rare in seine collections in Barnes Hollow Creek. Morone chrysops (Rafinesque ), white bass Rare. Collected by gillnetting and seining in Honker Bay and hook and line in Pisgah Bay. Family CENTRARCHIDAE Micropterus dolomieui Lacépéde, smallmouth bass One specimen collected by hook and line in Honker Bay. Micropterus punctulatus (Rafinesque), spotted bass Common in hook and line, seining, and electrofishing collections in Beechy Creek, Little River, Honker Bay, Crooked Creek, and Pisgah Bay. Micropterus salmoides (Lacépéde), largemouth bass h Commonly collected by hook and line in Barnes Hollow Creek, Energy Lake, Honker Bay, and Pisgah Bay. Lepomis macrochirus Rafinesque, bluegill Abundant in gill net, seine, electrofishing, and hook and line collections in Barnes Hollow Creek, Beechy Creek, Little River, Energy Lake, and Honker Bay; collected by hook and line in Pisgah Bay. Lepomis cyanellus Rafinesque, green sunfish Common in seine and electrofishing collections in Barnes Hollow Creek, Beechy Creek, and Crooked Creek; collected by hook and line in Pisgah Bay. Lepomis megalotis (Rafinesque ), longear sunfish Abundant in hook and line, seine, and electrofishing collections in Barnes Hollow Creek, Crooked Creek, Energy Lake, Honker Bay, Shaw Branch, and Little River. Collected by hook and line in Pisgah Bay. Lepomis microlophus (Giinther ), redear sunfish Rare. Collected by seining in Little River. Lepomis humilis (Girard), orangespotted sunfish Rare. Collected by seining in Little River. Lepomis gulosus (Cuvier), warmouth Rare. Collected by hook and line in Honker Bay. Pomoxis annularis Rafinesque, white crappie Common in seine collections in Barnes Hollow Creek, Little River, Energy Lake and Honker Bay; collected by hook and line in Pisgah Bay. Pomoxis nigromaculatus (Lesueur ), black crappie Rare. Collected in Honker Bay by seining; collected in Beechy Creek and Little River by seining and electrofishing; collected in Pisgah Bay by hook and line. Family PERCIDAE Percina caprodes (Rafinesque ), logperch Rare. Collected in Little River by seining. Etheostoma caeruleum Storer, rainbow darter Rare. Collected in Little River by seining. Etheostoma spectabile (Agassiz), orangethroat darter Common in seine and electrofishing collections in Beechy Creek. Etheostoma squamiceps Jordan, spottail Garter Abundant in seine and electrofiishing collections in Beechy Creek and Crooked Creek. Stizostedion vitreum (Mitchill), walleye Collected by hook and line in Pisgah Bay. Family COTTIDAE Cottus carolinae (Gill), banded sculpin Abundant in electrofishing collections in Barnes Hollow Creek, Beechy Creek, and Donaldson Creek. 78 Transactions of Kentucky Academy of Science, Vol. 33, 1972 Table 1 Comparison of present day records with those records as listed in Woolman (1892) L. Barkley Cumberland R. Kentucky L. Tenn. River (Woolman, 1892 ) (Woolman, 1892) Acipenser fulvescens Rafinesque as A. rubicundus Lesueur Amia calva L. Lepisosteus oculatus (Winchell ) Lepisosteus osseus (L.) Lepisosteus platostomus Rafinesque Alosa chrysochloris (Rafinesque ) Dorosoma cepedianum (Lesueur ) Dorosoma petenense (Ginther ) Hiodon alosoides ( Rafinesque ) Esox americanus vermiculatus Lesueur Esox niger Lesueur Cyprinus carpio L. Notemigonus cryoleucas ( Mitchill ) X — os = Notropis atherinoides Rafinesque X Notropis cornutus chrysocephalus (Rafinesque) X Notropis megalops (Rafinesque) — Notropis jejunus (Forbes) — Notropis umbratilis (Girard ) X Notropis whipplei (Girard ) — Campostoma anomalum (Rafinesque ) D4 Hybognathus nuchalis Agassiz - Hybopsis storeriana ( Kirtland ) _ Semotilus atromaculatus (Mitchill ) Rhinichthys atratulus (Hermann ) Pimephales vigilax (Baird and Girard) as Cliola vigilax Baird and Girard Pimephales notatus (Rafinesque ) Opsopeodus emiliae (Hay ) Carpiodes cyprinus (Lesueur ) Carpiodes velifer Rafinesque as C. difformis Cope Ictiobus bubalus (Rafinesque ) Catostomus commersoni (Lacépéde ) Cycleptus elongatus ( Lesueur ) Hypentelium nigricans (Lesueur ) Erimyzon oblongus (Mitchill) Moxostoma duquesnei (Lesueur ) Moxostoma erythrurum (Rafinesque ) Minytrema melanops (Rafinesque ) X _ X A | amas | MM | | | A | | | Anes Ml Mel OK | | ~~ Pa ws rw | | | | | ms wml *K | 1 x1 | oil mw! | ms | Kw l aM I ml wx | | | rs Transactions of Kentucky Academy of Science, Vol. 33, 1972 79 Table 1—(continued) L. Barkley Ictalurus punctatus (Rafinesque ) Ictalurus melas (Rafinesque ) Ictalurus natalis (Lesueur ) Pylodictis olivaris (Rafinesque ) Chologaster agassizi Putnam Aphredoderus sayanus (Gilliams ) Fundulus olivaceus (Storer ) as Zygonectes notatus Rafinesque Fundulus catenatus ( Storer ) Gambusia affinis (Baird and Girard ) as Gambusia patreulis Baird and Girard Labidesthes sicculus (Cope) Moroneé mississippiensis Jordan and Figenmann Morone chrysops ( Rafinesque ) Micropterus dolomieui Lacépéde Micropterus salmoides (Lacépéde ) Micropterus punctulatus (Rafinesque ) Lepomis macrochirus Rafinesque as Lepomis pallidus (Mitchill ) Lepomis cyanellus ( Rafinesque ) Lepomis megalotis (Ginther ) Lepomis microlophus (Girard ) Lepomis humilis ( Girard ) Lepomis gulosus (Cuvier) Pomoxis annularis Rafinesque Pomoxis nigromaculatus (Lesueur ) Stizostedion vitreum (Mitchill) Percina caprodes ( Rafinesque ) as Etheostoma caprodes ( Rafinesque ) Percina maculata (Girard ) as Etheostoma aspro (Cope and Jordan) Etheostoma caeruleum Storer Etheostoma nigrum (Rafinesque ) Etheostoma pellucidum Baird Percina phoxocephala (Nelson) as Etheostoma phoxocephalum Nelson Etheostoma shumardi (Girard ) Etheostoma spectabile ( Agassiz ) Etheostoma squamiceps Jordan Aplodinotus grunniens Rafinesque Cottus carolinae (Gill) X Xx Xx x X | ~ KKM KM PA PM PS PS DM Dd Ar KM Cumberland R. Kentucky L. Tenn. River Woolman, 1892 ) rv Ps raioa xX PX | bia &) wm MX | | | pA PS nw Me | (Woolman, 1892) 80 Transactions of Kentucky Academy of Science, Vol. 33, 1972 LITERATURE CITED Evermann, B. W. 1918. The fishes of Kentucky and Tennessee: A distributional catalogue of the known species. Bull. Bur. Fish. 35:295-368. Miller, R. J. 1968. Speciation in the common shiner: An alternate view. Copeia 1968: 642-647. Rafinesque, C. S. 1820. Ichthyologica Ohioensis, or Natural History of Fishes Inhabiting the River Ohio and Its Tributary Streams. Lexington, Ky., 90 pp. Resh, V. H., R. D. Hoyt, and S. E. Neff. 1971. The status of the common shiner, Notropis cornutus chrysocephalus (Rafinesque) in Kentucky. Proc. 95th Ann. Conf. Southeast. Assoc. Game Fish Comm. Sisk, M. E. 1969a. The fishes of West Kentucky. 1. Fishes of Clark’s River. Trans. Ky. Acad. Sci. 30:54-59. Sisk, M. E. 1969b. The fishes of West Kentucky II. The fishes of Obion Creek. Trans. Ky. Acad. Sci. 30:60-68. Woolman, A. J. 1892. Report of an examination of the rivers of Kentucky, with lists of the fishes obtained. Bull. U.S. Fish Comm. 1890:249-288. Received: September 4, 1972. Accepted: October 2, 1972. Transactions of Kentucky Academy of Science, Vol. 33, 1972 81 ACADEMY AFFAIRS THE FIFTY-EIGHTH ANNUAL MEETING OF THE KENTUCKY ACADEMY OF SCIENCE, MOREHEAD STATE UNIVERSITY, MOREHEAD, KENTUCKY November 8 and 4, 1972 Host: Dr. John C. Philley Associate Professor of Geoscience Department of Geoscience Morehead State University MINUTES OF THE ANNUAL BUSINESS MEETING The annual business meeting was called to order at 11:10 am. (EST) in Room 129, Lappin Hall, Morehead State University, Morehead, Kentucky, on November 4, 1972, by President Louis A. Krumholz. About 70 members were present. Rudolph Prins, Secretary, moved that the minutes of the 1971 Annual Business Meeting as published in the Transactions Vol. 32 (3-4), 1971, be approved. Motion carried. Wayne Hoffman, Treasurer, submitted the following report for the period January 14, 1972 to October 25, 1972: Money Transferred from former Treasurer: $1,427.38 RECEIPTS: INST) SYST Gy DIVE Si see et ge ae ee Oe $1,290.00 TRVESOTHIDIS, Ce ecto uc en HES uco Soe Re acece BEREEE CE eR Coa eC Ree CeCe rE 281.50 Transaction Subscriptions ............c.seccccccssesssecssscssssecscccctecsenes 165.00 University of Louisville Purchase of Transaction ................ 150.00 Miscellaneous yi ee Pa Uh eta oi ME Ue ee ee 5.00 1,891.50 $3,318.88 DISBURSEMENTS: Melee tom AAAS betes. Utes ocd Meee hcl ake desea sa huneteocswedaseeat 194.54 ANTTRSAYSUIO NS fee ore aes cerca eee ror ere eee cee Cee eee eee 2,003.75 AE NIG eLen RE@ SESW este Yas eR coisa) sia eos Ale canes emetic ag, 86.76 (Supplies for officers of Academy ) (Evecienracloweens. ate tien, seh eotnl bokeh dee Ml uae, bee 14.00 “LETROVD) NUS, Seo A Re Se oe PP ee) ea 76.37 Samronesteaclemy: Of iKsAL Sc eihs choi .cih sec Seenect es. csee tee 150.00 NISC CMATICOUSION ates. cote eto FIG hk sew adl sx NN aie ok 120 2,526.62 $ 792.26 ashy G@itizens' National Barbi sis.25).)cess es eotkes eibiscsctodesdssstenrsitorsssceess $ 792.26 Savings Account—Lexington Federal Savings & Loam .........c:ccccccesseesseeeees 1,022.48 Thomas Hunt Morgan Fund—First Federal Savings & Loan ............:.000++- 157.37 AUG MNO SETS, Les. eh ehh wert, ARM cat do. tiene Boke. Sacuaat. $1,972.11 The report was accepted. Dr. Krumholz then announced, for information purposes, that the Executive Committee approved the transfer of Academy funds to a bank closer to the residence of the treasurer—in this case, from Lexington to Bowling Green. Gordon Wilson, 1972 Chairman of the Board of Directors, presented a report on activities of the board. He said the board has been inactive in 1972 except for reviewing some past objectives relative to the raising of money for the Academy. Attention then turned to reports from standing committees. 82 Transactions of Kentucky Academy of Science, Vol. 33, 1972 Rudolph Prins, reporting for Karl Hussung, Chairman of the Membership Committee, who was absent, referred the members to the October Newsletter in which membership was broken down into numbers, by sections. Total member- ship was 469. However, it was pointed out that approximately 70 of these were being dropped, as of November, for lack of payment of dues. Dr. Prins also explained that the membership has been separated by interest sections. Names of individuals in each section were sent to sectional Chairmen. Sectional Chairmen were urged to use the lists to promote membership in their respective sections. Closer communication will be maintained between the secretary and sectional officers to keep the officers abreast of changes of membership in their sections. Marvin Russell, chairman of the committee on Legislation, reported that his committee has been attempting to elevate the stature of the K.A.S. in the eyes of legislators, to enhance the influence of the Academy in legislative matters of concern to scientists in Kentucky. Dr. Russell also discussed how, at the request of the Executive Committee, he is attempting to develop a committee to deal with serious issues. When he assumes the Presidency of the K.A.S. he proposes to appoint an Ad Hoc Committee to deal with these issues, in turn coordinating with the Committee on Legislation and ultimately to filter outcomes of deliberations to the Resolutions Committee where issues could become resolutions. The role of the Resolutions Committee would thereby be expanded to include serious issues as well as the traditional “Thank You” resolutions. Donald Batch, chairman of the A.A.A.S. awards Committee, recommended two recipients this year. There were 6 applicants for the award which amounted to a total of $128.00 in 1972. 1. Joseph T. Collins, Museum of Natural History, University of Kansas, Lawrence, $78.00 to study “Head scutellation variation of Carphophis amoenus (worm snake) in Kentucky, as correlated with soil and physiography.” Ward Rudersdorf, Department of Biological Science, Eastern Kentucky University, $50.00 to study “Winter nesting of Mute Swans.” bo There being no dissenting comments, Dr. Krumholz accepted the Committee’s recommendation. William Wagner, Editor of the Transactions commented that Vol. 33 (3-4) was nearly completed and encouraged members who would be willing to referee papers to write to him. The Publications Committee has been discussing the feasibility of a monograph series but recommendations for Executive Committee action have not been formulated to date. Rudolph Prins reported for Emest O. Beal, Chairman of the Audit Com- mittee, who was absent. The Committee certified as accurate the financial records of the Treasurer, summarized above in the Treasurer’s report, and provided nine exhibits to verify the records. An especially thorough audit was made this year because, for the first time in many years, the financial records were passed on to a new Treasurer. The Committee also recommended that the books of the K.A.S. be closed and audited at least 30 days prior to each annual scheduled meeting of the K.A.S. The complete report of the audit committee will be permanently filed in the Secretary's Book. Dr. Krumholz accepted the report with thanks to the Committee. The K.A.S. representative to the A.A.A.S., Branley Branson, presented a report on some recent changes and near future potential changes in the re- organization of the Constitution of the A.A.A.S. These changes very likely will affect the K.A.S. in that the K.A.S. representative will not necessarily represent the K.A.S. directly to the A.A.A.S. Rather ,a regional representative (not neces- sarily the Kentucky representative ) will perform this duty. The number of members on the A.A.A.S. Council may be reduced from 540 to 100. Transactions of Kentucky Academy of Science, Vol. 33, 1972 83 The reorganizational process is complicated and final action has not been taken to date (may not until some time in 1973-1974). This report was therefore basically for information purposes and was accepted as such. Herbert Leopold reported on the affairs of the Junior Academy in the absence of the Director, William Martin. Information in the report included: 1. Total assets for 1971-1972 amounted to $797.19. Balance on hand as of October 31, 1972 amounted to $188.48. 2. A Fall Conference will be held at Western Ken- tucky University on November 11, 1972. 3. A Spring Symposium (rather than the traditional Fair) is being planned. 4. A concerted effort is underway to encourage greater numbers of High Schools to associate with the K.J.A.S. 5. Finally, a plea was made for money and ways and means to obtain donations on a regular basis. Since there was no old business, Dr. Krumholz next turned to new business and requested Jerry Howell of Morehead to report on matters dealing with a proposed list of rare or endangered species in Kentucky. Dr. Howell yielded the floor to Mr. William H. Casey of the Soil Conservation Service who, very briefly, provided the following report: There is a need to identify rare and endangered plant and animal species in Kentucky, to develop a list of these organisms, and to attempt to provide recom- mendations on how to protect these organisms and means by which to detect potentially endangered species. Mr. Glen Murray presented a paper to two sections in the morning outlining problems, needs, and possible ways to handle the problems and needs, and pledged the support of the Soil Conservation Service. The hope was expressed that the K.A.S. would consider forming a committee to begin to develop such a list. Dr. Krumholz stated that this item was to be placed on a near future agenda of an Executive Committee Meeting. Since a resolution concerning this matter was to be presented later (Resolution B), Dr. Krumholz referred to additional new items of business, thanking Mr. Casey for his report. Dr. Krumholz displayed a copy of the newly published brochure and en- couraged members to use these to promote membership in the academy. Dr. Krumholz then asked the membership for opinions regarding the question whether or not presentors of papers at the Annual Meetings should be members of the K.A.S. Charles Covell moved that: papers submitted for presenta- tion at Annual Meetings be restricted to members; in case of multiple author- ships, at least one must be a member. The motion was seconded by Branley Branson. Immediately, Thomas Coohill moved to amend the motion to state that: a member may be allowed to sponsor a non-member to present a paper. Dr. Krumholz ruled that Dr. Coohill’s amendment was to substantive and declared it out of order. After much discussion, the vote was taken and the main motion was carried by about a 5-vote margin. Dr. Coohill then resurrected his amendment, in the words presented above, as a motion. The motion carried. H. H. LaFuze, member of the Resolutions Committee, then presented five resolutions for consideration individually, in the absence of William Day, Chairman of the Committee. The resolutions are listed below in the order of consideration and in the form that they were all accepted by the members present. RESOLUTIONS Whereas, Morehead State University has so graciously served as the Host Institution for the Fifty-eighth Annual Meeting of the Kentucky Academy of Science; and Whereas, Dr. John C. Philley and other Morehead personnel have labored diligently to make this meeting a success; and Whereas, Morehead State University under the presidency of Dr. Adorn Doran is now celebrating its Golden Anniversary year; now 84 Transactions of Kentucky Academy of Science, Vol. 33, 1972 Therefore, be it resolved, that the Academy express its appreciation and offer its congratulations to Morehead State University and the above individuals, and that the Secretary be instructed to so inform them. Whereas, the Kentucky Academy of Science recognizes that there is nation- wide concern for the plight of many plant and animal species that are now rare or threatened with extinction; and Whereas, no list of rare or enuangered plant and animal species has been developed specifically for Kentucky; and Whereas, such a list, together with knowledge of the distribution and habitat requirements of the plants and animals on it, is essential to the protection and preservation of such species; and Whereas, the membership of the Kentucky Academy of Science is composed of scientists and other professional people who are eminently qualified to assess the status of the state’s flora and fauna; and Whereas, the Kentucky Academy of Science recognizes the need for co- ordinated effort by scientists, educational institutions, private foundations or museums, professional societies, governmental agencies, and other informed people to develop an action program for the protection and preservation of rare or endangered species; now Therefore, be it resolved, that the Kentucky Academy of Science will take appropriate action to: (1) Prepare a list of the state’s rare or endangered plant and animal species. (2) Describe the measures needed to preserve the habitat of these species. (3) Develop a monitoring program that will provide advance warning of actions or disturbances that might further endanger these species so necessary protective actions can be taken. Whereas, the Kentucky Academy of Science is a society founded to promote the interests of science; and Whereas, the education in science of our youth must therefore be a continuing concern to the Academy; and Whereas, the training of science teachers is a vital concern to the education of our youth; and Whereas, there has been no recent evaluation of the certification requirements of science teachers, particularly with respect to the new interdisciplinary courses now being taught; now Therefore, be it resolved, that The President of the Kentucky Academy of Science should appoint an ad hoc Committee on Science Teacher Certification. This committee should have suitable representation from Science related disciplines. The said committee should review present certification require- ments of all science teachers and, especially, the requirements to certify teachers of inderdisciplinary science courses. This committee should report its findings to the Academy during the fall meeting, 1973. At the same time, this committee should make recommendations for action, if any, to the Academy at that time. Whereas the Kentucky Academy of Science has a vital interest in the quality of public higher education in Kentucky, both undergraduate and post-graduate, not only in the sciences but in other disciplines, and Whereas the Council on Public Higher Education has been charged with the duty and power to set basic policy in public higher education in the Common- wealth, and Whereas the current membership of the Council reflects a disproportionately large representation of the professions, i.e., medicine and law, relative to other disciplines; now Transactions of Kentucky Academy of Science, Vol. 33, 1972 85 Therefore, be it resolved that the Kentucky Academy of Science urges the Governor, in making future appointments to the Council on Public Higher Education, to achieve a better balance in the representation of all academic fields. Whereas, the Kentucky Academy of Science recognizes the responsibility of its membership to provide expert counsel to the Commonwealth in matters pertaining to the identification of opportunities, needs, and the solution of state problems in the area of science and technology; and Whereas, the means to assist state government and the governor is presently limited by the lack of regularized communication between the Academy and the Kentucky Science and Technology Commission; and Whereas interaction of the scientific community and commissions of science and technology have proven their worth in other states; now Therefore, be it resolved that the Kentucky Academy of Science affirms the need for the Kentucky Science and Technology Commission and requests its chairman to arrange for periodic meetings with designated representatives of the Academy. Dr. Krumholz then yielded the floor to Gordon Wilson, Chairman of the Nominating Committee, who presented the slate of nominees for offices as follows: Donald Batch, Eastern Kentucky University, President-Elect Rex Knowles, Centre College, Vice President Rudolph Prins, Western Kentucky University, Secretary Wayne Hoffman, Western Kentucky University, Treasurer Charles Payne, Morehead State University, Board of Directors to 1976 (4-year term ) Morris Taylor, Eastern Kentucky University, Board of Directors to 1976 (4-year term) Branley Branson, A.A.A. representative for 1973 and 1974 (2-year term) Charles Covell moved to elect those nominees by acclamation. Motion carried and Dr. Kumholz ordered the Secretary to declare the nominees elected by acclamation. Responding to the President’s enquiry as to whether there was any further business to come before the Academy, Dr. Frank Six recommended: 1) that the Executive Committee consider means by which to extend the length of the annual meetings to afford more casual time and lattitude for participants to attend paper sessions. A straw vote showed that the majority of the members present favored the idea of longer meetings. 2) that the membership committee consider sending letters to Mathematics Department Heads in the State to enquire if there is any interest among Kentucky mathematicians to create a Mathematics Section in the Academy. Dr. Krumholz terminated his duties as the 1972 President of the K.A.S. by expressing appreciation to members and officers of the K.A.S. for the cooperation he received and for the opportunity to get better acquainted with the membership. The gavel was then turned over to the new K.A.S. President, Dr. Marvin Russell, Dean of the Ogden College of Science and Technology, Western Kentucky University. He accepted the challenge and responsibility of th office and resolved to work hard and effectively on programs that have been initiated recently and that hopefully will be implemented in the near future. Dr. Russell praised Dr. Krumholz for initiating many of the programs that are before the academy and for his concern over the future of the organization. Dr. Russell stated that he will visit around the State to talk with members in order to ascertain what, in fact, the goals and aims of the K.A.S. should be. Dr. Rex Knowles then moved for adjournment. The motion carried and the 1972 Annual Business Meeting adjourned at 12:50 (EST). Rudolph Prins, Secretary 86 Transactions of Kentucky Academy of Science, Vol. 33, 1972 PROGRAM Friday, November 3, 1972 P.M. 4:00- 7:00 REGISTRATION, Third Floor Lobby, Adron Doran University Center 4:00- 5:00 STANDING COMMITTEE MEETINGS, Lappin Hall —Membership Committee: Room 101B —Legislation Committee: Room 122 —Distribution of AAS Funds: Room 121 —Publications Committee: Room 126 —Nominations Committee: Room 105 5:15- 6:15 EXECUTIVE COMMITTEE & SECTION CHAIRMEN MEETING U. N. Room, Third Floor, Adron Doran University Center 4:00- 6:00 COFFEE HOUR Cornucopia Room, Lappin Hall, Room 128 7:00- 9:00 GOLDEN ANNIVERSARY BANQUET Ballroom, Adron Doran University Center —Presiding: Dr. Louis A. Krumholz, President Kentucky Academy of Science —Invocation: Dr. David R. Cutts, Morehead State University —Welcome: Dr. Adron Doran, President Morehead State University —Speaker: Dr. Justin W. Leonard, Department of Natural Resources, University of Michigan —Topic: “Man and His Environment” 9:30-11:30 HOSPITALITY HOUR, Holiday Inn 9:00 9:50 10:15 P.M. 1:30 8:15 8:30 8:45 9:00 SECTION MEETINGS (Times indicated are AM, except where noted ) November 4, 1972 ANTHROPOLOGY SECTION Room 121, Lappin Hall Cara Richards, Chairman Carla Lowenberg, Secretary Primitive Man and His Physical Environment: The Lesson from Lithics. Michael B. Collins Election of new officers Phenomenology of Nature and Empirical Anthropology. Edward J. Emery Panel Discussion on the FUTURE OF MAN/LAND RELATIONSHIPS. Joint session with Sociology - BOTANY AND MICROBIOLOGY SECTION Room 126, Lappin Hall Harold E. Eversmeyer, Chairman Joe E. Winstead, Secretary Election of Officers The Influence of Benzimidozole on the Growth of the Gametophyte of Dryopteris felix-mas. Joan Shade and James J. Dyar, Ballarmine College Factors Affecting the Radiosensitivity of Deciduous Tree Seed and Seed- lings. Margaret B. Heaslip, Morehead State University Arrangement of D-Stomates on the Leaf of Ilex crenata var. convexa. George W. Fedrick, Béllarmine College 9:15 9:30 9:45 10:00 10:15 10:30 Transactions of Kentucky Academy of Science, Vol. 33, 1972 87 Computer Simulation of D. Stomates on the Leaf of Ilex crenata var. convexa. Robert W. Korn, Bellarmine College A Computer Model for Monolayer Plant Tissues. Richard Spalding, Bellar- mine College BOTANY AND MICROBIOLOGY SECTION A Relict Hardwood Forest in Barren County, Kentucky. Chris K. Bougher and Joe E. Winstead, Western Kentucky University Species Diversity: Changes Along a Small Stream. Craig A. Zimmerman, Centre College of Kentucky A List of Exterminated, Rare and Endangered Plant Species of the Red River Gorge. Johnnie B. Varner, Harrison County High School A Proposal for Protecting Rare or Endangered Plants and Animals in Ken- tucky. Glen E. Murray, U. S. Soil Conservation Service CHEMISTRY SECTION Room 129, Lappin Hall Verne A. Simon, Chairman Howard Powell, Secretary Sectional business meeting and election of officers. Synthesis of some Derivatives of Naphto[1,2-C]-[1,2,5] Selenadiazole. David P. Moore and Walter T. Smith, Jr., Southeastern Christian College and The University of Kentucky. Ketone/Pyrolylborane—Condensations. Clifford D. Miller, Department of Chemistry, Eastern Kentucky University. Cis-trans Isomerization in the Phenylazopyridines. G. Richard Granneman and Ellis V. Brown, Department of Chemistry, University of Kentucky. The Synthesis of 5,7-Diisopropyl-8-Hydroxyquinoline and 5-sec-buty]-8- hydroxyquinoline in Acid Medium. James D. Searcy and Charles A. Payne, Department of Chemistry, Morehead State University. Coffee The Nuclear Magnetic Resonance Spectra of o-Hydroxymethylphenyl- phenylethanols. Sharad Draramshi and Victor Bandall, Department of Chemistry, Eastern Kentucky University. Thermal Analysis of Lanthanide Fluoro-£- diketonates. Henry E. Francis and William F. Wagner, Department of Chemistry, University of Kentucky. The Low Temperature Catalytic Oxidation of Carbon Monoxide. William G. Lloyd and Donald R. Rowe, Western Kentucky University. GEOGRAPHY SECTION East Room, Adron Doran University Center David Irwin, Chairman Wilfred Bladen, Secretary Election of Officers The Evolution of Small Population Centers Along the Chesapeake & Ohio Railroad and U.S. 60 in Northeastern Kentucky. Robert Gould, Morehead State University. Wheatley, Kentucky, A Microstudy in Settlement Geography. C. M. Dupier, Cumberland College. An Analysis of Land Values in Bowling Green, Kentucky. James Frymark, Lexington-Fayette County Planning Commission. A Rationale for The Revision of Mobile Home Ordinances for Lexington- Fayette County, Kentucky. T. P. Field, University of Kentucky. Applications of Aerial Photography in Studies of Industrial Sites in The Ohio-Tennessee Confluence Area. William Smith, Murray State University. The Development of The Computer Atlas of Kentucky. Phillip Phillips, University of Kentucky. 88 9:36 9:47 10:05 10:16 10:27 10:38 10:49 Transactions of Kentucky Academy of Science, Vol. 33, 1972 The Development of The Commercial Catfish Farming Industry in The Southeast. Gary C. Cox, Morehead State University. Coffee Break Computer Presentation of Geographic Data. The Use of SYMVU to Portray Innovation Adoption. Ronald Garst, University of Kentucky. Vertical Geography. Sanford Hendrickson, Murray State University. Modes of Transportation in A Middle Ganges City: The Case of Monghyr. S. Reza Ahsan, Western Kentucky University. Lusaka, Zambia: An Example of Primary Business District Eccentricity. John Snaden, Western Kentucky University. Recent Urban Evolution in Southeast Asia. W. A. Withington, University of Kentucky. GEOLOGY SECTION Room 113, Lappin Hall Howard Schwalb, Chairman John C. Philley, Secretary Election of Officers Origin, Distribution, and Physical and Chemical Properties of Unconsoli- dated Chert in Pike County, Illinois. James Cobb, Eastern Kentucky University. Variations in Quality and Constituents of the Mulford #9 Coal in the Western Kentucky Coal Field. Allen Williamson, Kentucky Geological Survey. A Study of the Heavy-Metals Content of the Kentucky River. Barry M. Faulkner, Eastern Kentucky University. A Preliminary Report on the Almont Graben, Gunison County, Colorado. S. Judson May, Eastern Kentucky University. What is Coal? Gilbert E. Smith, Kentucky Geological Survey. The Pre-Knox Sequence and its Relation to the Precambrian Subsurface Topography in Eastern Kentucky. Robert S. Goble, Eastern Kentucky University. Middle Devonian Stratigraphy and Bone Beds on the East side of the Cincinnati Arch in Kentucky. James E. Conkin, University of Louisville. Barbara M. Conkin, Jefferson Community College. Zelek Lipchinsky, Berea College. PHYSICS SECTION Room 105, Lappin Hall Louis M. Beyer, Chairman Jerry Faughn, Secretary Undergraduate Physics at Morehead State University. R. M. Brengelman, Morehead State University. Mossbauer Effect in Lead, Nickel, Zinc, and Calcium Ferrocyanides. L. Brun, L. Busse and Sr. M. C. Madden. Thomas More College. Computer Fit and Plotting of Mossbauer Data. R. Livingston, M. Stampe and D. Boyle. Thomas More College. A Velocity Stepper for Constant Velocity Mossbauer System. K. Muething and D. Boyle. Thomas More College. Computer Modeling in the Undergraduate Physics Laboratory. J. Lang. Thomas More College. The Orbital Motions of the Trojan Asteroids. D. Uckotter and J. Lang. Thomas More College. A Comparison of the Presentations of College Physical Science. D. Boyle. Thomas More College. EPR of the Vanadyl Ion in Solution. D. E. Munninghoff and G. K Miner. Thomas More College. 9:40 9:50 10:00 10:10 10:20 10:30 10:40 10:50 11:00 11:10 11:20 11:30 11:50 9:00 10:00 10:15 8:15 8:30 8:45 9:00 9:15 9:30 9:45 Transactions of Kentucky Academy of Science, Vol. 33, 1972 89 The Advanced Classical Physics Laboratory at Eastern Kentucky Univer- sity. J. S. Faughn. Eastern Kentucky University. Using the Computer in an Open Lab. C. D. Teague and J. C. Mahr. Eastern Kentucky University. Establishmen of a Graduate Student Referral Center. C. E. Laird. Eastern Kentucky University. A Humanistic Approach to Science. J. L. Roeder. Transylvania University. Study of Nuclear Levels Through Use of Isobaric Analog Resonances. F. D. Snyder and B. D. Kern. University of Kentucky. Lifetime Measurements in the Range From 5 to 100 Nanoseconds. F. D. McDaniel and F. D. Snyder. University of Kentucky. A New Technique for Measurement of Nuclear Excitation Energies. F. Gabbard. University of Kentucky. A Model for Thermoluminescence of Ruby. W. Scates and W. Buckman. Western Kentucky University. Thermoluminescence Response of Some Aluminum Oxide Crystals to UV Radiation. L. Wells and W. Buckman, Western Kentucky University. A Luminosity Discriminant for Red Giants and Supergiants. A. Waw- rukiewicz and S. Sharpless. Western Kentucky University. Foundational Problems in Physical Theory. J. B. Kizer. Scioto County, Ohio PA/VR Project. Report from the KAPT Educational Advisory Committee. T. M. George. Eastern Kentucky University. Business Meeting. L. M. Beyer. Murray State University. PHYSIOLOGY, BIOPHYSICS, PHARMACOLOGY Room 101A, Lappin Hall Bertram Peretz, Chairman H. A. Leopold, Secretary Special Lecture—Behavioral and EEG effects in the cat resulting from systemic and amygdaloid stimulation with d-amphetamine sulfate during a visual discrimination task. Richard L. Miller, Ph.D., Psychology Dept., Western Kentucky University. Coffee Break Sectional Business Meeting: (1) Consideration of Proposed Changes in the Format of this KAS Section (2) Election of Officers PSYCHOLOGY SECTION West Room Adron Doran University Center Edward S. Rosenbluh, Chairman Frederick M. Brown, Secretary Election of Officers for 1972-73. Behavioral Treatment of Test Anxiety. Bernard Segal (Read by Clarence Weathers), Murray State University. Establishment of a Conditioned Paced-Aversion in the Rat with a 24-Hour CS-US Interval. Frank Etscorn and Richard Miller, Western Kentucky University. The Organization Ability of the Learning-Disabled Child. Rex H. Knowles, Centre College. The Life Satisfaction of Non-Normal People. Paul Cameron, University of Louisville. Coffee Break. Assessment of Assertiveness: A Psychometric Approach. David V. Myers, J. Thomas Muehleman, and B. Thomas, Murray State University. 90 10:00 10:15 10:30 8:15 8:30 9:00 9:30 10:00 10:30 10:45 8:15 8:30 8:45 9:00 9:15 9:30 P.M. 1:30 8:00 8:15 8:30 8:45 9:00 9:30 Transactions of Kentucky Academy of Science, Vol. 33, 1972 The Effects of the Pyramid: Besides Sharpening Razors, What Implications for Behavior? Kay Hutton and Walter Tapp, Centre College. A Psychometric Look at Women’s Rights. Richard D. Kahoe, Georgetown College. Geophysics, Physiologic, and Psychologic Factors Present in Apparently Successful Instances of Telepathy. Frederick M. Brown, Walter Tapp, and Kay Hutton, Centre College. SCIENCE EDUCATION SECTION Room 122, Lappin Hall Doris K. Mouser, Chairman R. H. Barker, Secretary Election of Officers. Environmental Education Experiences. Shaw Blankenship, Title 111, Region 6. Science Support and Science Orientation of College Students in Kentucky. George Miller, University of Louisville. An Evaluation of Independent Study Projects in Physics. George Minor, Thomas More College. A Study of Content Development in Secondary Biology Classes. B. J. Stoess, Eastern Kentucky University. An Environmental Information Dissemination Program for Eastern Ken- tucky. Jerry F. Howell, Jr., Morehead State University. An Environmental Science Degree Program for Morehead State University. Jerry F. Howell, Jr., Morehead State University. SOCIOLOGY SECTION Room 101B, Lappin Hall Richard F. Armstrong, Chairman Amiya K. Mohanty, Secretary Election of Officers. Social Factors in Aspiration Level. James De Burger. University of Louisville. The Rat’s Short, Spectacular Career as a Social Problem: The Politics of Environmental Quality. Craig Taylor. Western Kentucky University. Self-Hatred Among Minorities. Hwa-bao Chang. Morehead State University. Alienation et al.: What Do They Mean? Joseph Donnermeyer. University of Kentucky. Man and His Social Environment. Panel Discussion. James Wittman, Western Kentucky University. Richard Reser, Morehead State University. Richard Armstrong, Eastern Kentucky University. Panel Discussion on the Future of Man/Land relationships. Joint session with Anthropology Section. To be held in Room 121, Lappin Hall. ZOOLOGY SECTION SESSION A. Room 130, Lappin Hall—J. Hill Hamon, presiding DDT-Dehydrochlorinase in DDT-Susceptible Housefles. Ben T. Feese, J. Gregory Cooper and Daniel S. Rush, Centre College. The Occurrence of Leucerutherus Micropteri in Kentucky Fishes. Azygiida: Trematoda. Sharon Patton, University of Kentucky. Early Swan Nesting. Ward Rudersdorf, Eastern Kentucky University. Clarification of Trichinella Spiralis (Nematoda) life cycle terminology. John P. Harley, Eastern Kentucky University. Coffee Break. Sectional Business Meeting. 10:00 10:15 10:30 8:00 8:15 8:30 8:45 9:00 9:30 10:00 10:15 10:30 Transactions of Kentucky Academy of Science, Vol. 33, 1972 91 A Proposal for Protecting Rare or Endangered Plants and Animals in Kentucky. Glen E. Murray, United States Soil Conservation Service. Cynipid Gall Anatomy and Distribution of the Causal Organism. David E. Murray, Morehead State University. Morphologic Alterations in Channel Catfish exposed to Methyl Mercuric Chloride. Chromic Dietary Administration. David E. Hinton, Charlotte Pool and Peter Thurman, University of Louisville. SESSION B. Room 224, Lappin Hall—Rodney Hays, presiding A Checklist of Adult Digenetic Trematodes from Kentucky Fishes. John V. Aliff, Georgia College, Milledgeville, Georgia. An Aerial View of Stripmining Damage Featuring Coal Mining in Kentucky and Kaolin Mining in Georgia. John V. Aliff, Georgia College. Status of two Endangered Butterfly Species in Southern Florida. Charles V. Covell, Jr., University of Louisville. The Mammals of Pulaski County, Kentucky. David J. Fassler, Somerset Community College. Coffee Break. Joint Sectional Business Meeting. A Proposal for Protecting Rare or Endangered Plants and Animals in Ken- tucky. Glen E. Murray, United States Soil Conservation Service. Dehydration and Kidney mucopolysaccharides in the Rat. Charles E. Kupchella and John Wilhelmus, Bellarmine College. Alteration in the absorption of 131I-L-Thyroxine from the small intestine of the Rat. Sanford L. Jones, Eastern Kentucky University. speak aN Naan ON snug aa 0 teat) "at oe hae Ronen bein wae freee a PAs mbieielee 53 an tind } ers pine: Sia Eo rane iagihe ne Contr ess iat igre 48% racer ay ‘sh: ffeil cll ah Aisghoh't yee tab A (Me 3 sia RS ah Ect ce dT yt ats ntiie dbo Racy if earl yahoo had? bey erly “We htt 2. - ue 5 aS), Ai § they ‘ ere or Mi i i, 4 td tj ay o Veet! , 5 ‘ a ’ ‘ rea =| 1 a mh La im INDEX TO VOLUME 33 ACADEMY AFFAIRS, 81 Acer Negundo L., Variation in Seed Germination, 43 Alfalfa Weevil, Capture of, 71 Aquatic Microecosystem, 1 Bacterial Populations, Wilgreen Lake, 18 Baker, C: R., 73 Barbour, R. W., 41 Batch, D. L., 33 Blankenship, S., 37 Branson, B. A., 33 Brown, E. V., 64 Butter, J. R., 41 Clear Creek, Fishes, 33 Clay, W. M., 73 Gross, J-.E.,.27 Crockett, D. R., 37 Crum, G. E.,, 71 Brust, C: H:, 41 Fassler, D., 36 Fishes: Clear Creek, Rockcastle River, 33 Land Between the Lakes, 73 Freshwater Mussel Fauna, 37 HarleyayjeoR 13 Helminths, of Muskrats, 13 Hoary Bat, Record of, 36 Hoyt, R. D., 27 Hypera Postica (Gyllenhal), 71 Johnson, V., 40 Leung, S., 18 Lin, C., 57 Moser, R. J., 64 Muskrats, Helminths of, 13 Ondatra Z. Zibethica Miller, 1912, 13 Otero, R. B., 18 Pyridinecarboxylic Acids, Spectra of, 64 Rana Pipiens, Eggs, Effect of Temperature and Photoperiod, 27 Resh, V. H., 73 Rockcastle River, Freshwater Mussel Fauna, 37 Samsel, Jr., G. L., 1 Spectra, 6-Substituted 2-Pyridinecarboxylic Acids, 64 Sperka, C. L., 40 Spermatozoa, Venus Mercenaria, 57 Thompson, Jr., M. P., 49 Triozocera (Strepsipteria: Mangeidae), New Record, 40 Turtles, Genus Kinosternon, Habitat, 41 Upper Lusk Creek, Summer Vertebrate Fauna, 49 Venus Mercenaria, Spermatozoa, 57 Vertebrate Fauna, List of, Upper Lusk Creek, 49 Wilgreen Lake, Bacterial Populations, 18 Williams, R. D., 43 Winstead, J. E., 43 CONTENTS TO VOLUME 33 Nos. 1-4 The Effects of Temperature and Radiation Stress on an Aquatic Microecosystem GENE) Li: SAMSEDL, JR.) jcicsccescecstsecessosssesccateqeerts eee it A Survey of the Helminths of the Muskrat, Ondatra Z. Zibethica Miller, 1912, in Madison County, Kentucky JOHN P. HARLEY 5.02. -.25i8.-:c0c.c.ectsdsscecevctesscaceess see ae eee 13 Some Observations on Bacterial Populations in Wilgreen Lake Madison, Kentucky R: BeOTERO and ‘SS; LEUNG. «........cccccccceeticse eee econ eee 18 The Effect of Combined Temperature and Photoperiod on Early Development rate of Rana Pipiens Eggs JEFFREY F. CROSS and ROBERT D. HOYT ..............0c:cccssescenness 27 Fishes of Clear Creek, Tributary to Rockcastle River, Kentucky BRANLEY A. BRANSON and DONALD L. BATCH .................... 33 An Additional Record of the Hoary Bat in Kentucky DA VID WBVASS STEER OE eccsccsvenceveceecceecccscucceuenees snot aeeeeeeee 36 Changes in the Freshwater Mussell Fauna of the Rockcastle River at Livingston, Kentucky SHAW BLANKENSHIP and DAVID R. CROCKETT .................. 37 A New Record of Triozocera (Strepsiptera: Mangeidae) from Kentucky VICTOR JOHNSON and CHRISTINA L. SPERKA ...........escseeeeee- 40 Habitat Perferences of Two Florida Turtles, Genus Kinosternon CARL H. ERNST, ROGER W. BARBOUR, and PAIMIEIS RS BUT Ree esr cec ea cocee ects cena cee eee Al Population Variation in Seed Germination and Stratification of Acer Negundo L. Ro D: WILETAMS ‘and JOE E. WINSTEAD... tre = eee 43 An Annotated List of the Summer Vertebrate Fauna of Upper Lusk Creek, Pope County, Illinois MARVIN, BEATE THOMPSON: [Ri --:.-52--:.--scerseeeeueeceeeeeeeenee reer 49 Electron Microscope Study of the Spermatozoa of the Hard-Shelled Clam Venus Mercenaria (Mollusca) by Negative Staining CHIECRIUNG ISIN 6 ccckcccccccssesedesveceseces cessed ok ieuetes een setae Reena 57 CONTENTS TO VOLUME 33—Continued Electronic Absorption Spectra of 6-Substituted 2-Pyridinecarboxylic Acids. On a Possible Cyclic Structure in Methanol RUSSELL J. MOSER and ELLIS V. BROWN ......0...0.....cecsceereeoeeee Capture of the Alfalfa Weevil, Hypera Postica (Gyllenhal), in Illuminated Sticky Traps GUAM RIE TS 1 Gr UNI DIR Soar Ae ae ma een a RO enn AOL area ter SD A Preliminary List of the Fishes of the Land Between the Lakes, Cumberland and Tennessee River Drainages, Kentucky VINCENT H. RESH, CLAUDE R. BAKER and TTT ANU TN bs (i By GRR SR eee Er nan eee eer ene pO em INVA WAU RUANUIAS) ces vo usa ce scce cate autos oceseveseceesabedesusceesonsetvecersesscedesbceceseces ‘oh irr bv amatcieg 9 Hustle é. ay we Oh hy pect on wast ert bay ie 1d > plbbanne'é a Sees ned VS Eas Peat) Mala ines eo a Laie 5 ; ini in j ee ae Tot Ati ey HRN Me Dat ehh Fa i VER oe Roe Sra ea fa wiih: a CAMA ; i Put: ne) See oud Wa " fn Atigtt: Ble ae Bio h i > BGM aibeh au wih sp Ritmo! hy aie ibd i ; ‘ te 4 ; ‘ Saiehig Sere i 4 { . { } re rif et an ans’ { hh j Sh ES 7) x 5 ‘ i eM, apt ba) j “ eo pu tot : ‘ } i *\ r i nf f ‘ aie h oe ij j eae: et \ ty M rh, f ‘ ? ra ae & ? i &? ie ? [ gt: i n ue 7 i A ; aa Wey f ; if 47 5 ee ’ VEE ES eta i ua ‘ j AY ; a he a f ie A y Y ES ea! y c q , i < ; ey ‘ sf my ie "| 1% A ‘ay Ait) oy the Ee ah te all Oye 1%) i BN coh aN f Wenate | ; 4 rad i io : Ps t " Niven is ee The ee a ee ee ee ee ge ee ae Pee ee Sx a eee INSTRUCTIONS FOR CONTRIBUTIONS The TRANSACTIONS OF THE KENTUCKY ACADEMY OF SCIENCE is a medium of _ publication for original investigations in science. Also as the official organ of the Kentucky Academy of Science, news and announcements of interest to the member- ship are published therein. These include programs of meetings, titles of papers presented at meetings, and condensations of reports by the Academy’s officers and committees. Papers may be submitted at any time to the editor. Each manuscript will be ‘reviewed by one or more editors before it is accepted for publication, and an at- tempt will be made to publish papers in the order of their acceptance. 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Blanks for reprint orders will be supplied with the galley proof. Vol. 34, Nos. 1, 2 1973 Coden: TKASAT ‘TRANSACTIONS «Kan oe of the KENTUCKY ACADEMY of SCIENCE Official Organ KENTUCKY ACADEMY OF SCIENCE CONTENTS _ Relation of Organic Activity to Early Diagnetic Changes in the Tyrone Limestone of Kentucky PETER W. WHALEY _ Fishes of Eagle Creek, Northern Kentucky NELSON D. HORSEMAN and BRANLEY A. BRANSON Preliminary Investigations of a Headwater Creek in Eastern Kentucky G. L. SAMSEL, JR., J. R. REED, and R. R. DAUB Effect of a Methoxyl Group on the Decarboxlyation of 2-Pyridinecarboxylic Acids ELLIS V. BROWN, RUSSELL J. MOSER and MANVENDRA B. SHAMBHU The Ultraviolet Spectra of Some 9-Anthracenecarboxaldehyde Hydrazones. Evidence for a Planar Structure in Methanol RUSSELL J. MOSSER and ELLIS V. BROWN Some Physical, Chemical, and Benthic Characteristics of War Fork, an Interrupted Stream in Jackson County, Kentucky NORMAN H. CRISP and CATHERINE B. CRISP Apophallus Venustus (Trematoda, Digenea): A New Metacercaria Record from New Hampshire NORMAN CRISP and JOHN P. HARLEY An additional Evening Bat from South Central Kentucky DAVID J. FASSLER The Kentucky Academy of Science Founded May 8, 1914 OFFICERS 1972-73 President: Marvin Russell, Western Kentucky University President-Elect: Donald Batch, Eastern Kentucky University Vice-President: Rex Knowles, Centre College Secretary: Rudolph Prins, Western Kentucky University Treasurer: Wayne Hoffman, Western Kentucky University Representative to A.A.A.S. Council: Branley Branson, Eastern Kentucky University BOARD OF DIRECTORS Sanford Es Jones ier to 1973 Thomas B. Calhoonsiagee ee to 1975 Bis) Vo Bea wik ncn aues keene to 1973 Charles Kupchella fa) x ie) uv ie) o ) ra) io e) N @) > ww Ve 8 Co eee CEPHALOPOD (STRAIGHT) pe aot G AX ANONSIXDOAR)) SS INIYVW MOTIVHS a Zw Q 5) R a C on (4 FOSSIL FRAGMENTS ia ow GMENTS) za > TETRADIUM (F TRILOBITE (HYPOSTOME) 4V1d 1VGIL Transactions of Kentucky Academy of Science, Vol. 34, 1973 3 Figure 2. Burrow Types A. oO Polished slab showing tidal flat spar-filled burrows (sb) in micrite (m). Slab cut perpendicular to bedding. Polished slab showing tidal flat spar-filled burrows (sb), and area of burrow collapse (c) in micrite (m). Slab cut parallel to bedding. Burrow mound on bedding surface, well developed mound to left of paper clip. Polished slab showing marine dolomitized burrows; (m) micrite, (db) do- lomitized burrow, (da) dolomitized area. Slab cut perpendicular to bedding. Polished slab showing more complete dolomitization with increase in the number of shallow marine burrows; (m) micrite, (db) dolomitized burrow, (da) dolomitized area. Slab cut perpendicular to bedding. 1. The formation of magnesia-rich solutions. 2. The magnesia-rich solutions must flow through the sediment. 3. The rate of production and flow of the magnesia-rich water must be sufficient to complete dolomitization within the available time. Murray (1964) states that excess carbonate ions must be available for the process of dolomitization to occur. He also states that during dolomiti- zation, dolomite crystals have a strong tendency to replace calcium carbonate 4 Transactions of Kentucky Academy of Science, Vol. 34, 1973 and do not tend to grow into void spaces. The distribution of dolomite and sparry calcite in the Tyrone Limestone suggests that these processes occurred there. Since a vertical sequence in one locality reveals fluctuating shallow marine and tidal flat conditions (Fig. 1), one may deduce from Walther’s Law that these environments were laterally contemporaneous. The magnesia- rich solutions were generated by evaporation of sea water on the tidal flats. As the magnesia-rich solutions moved through the tidal flat sediments into the shallow marine sediments, infrequent dolomite rhombs were formed in the tidal flat sediments. The ratio of carbonate ion to magnesia-rich solu- tion in the nonsediment-filled tidal flat burrows was not sufficient to permit formation of dolomite; rather, these voids were filled with sparry calcite. The disturbed sediment which filled the shallow marine burrows, being more porous than the surrounding undisturbed bedded micrite, formed preferential channels for the flow of magnesian solutions. The excess carbonate ions furnished by the burrow fill, and the increased availability of magnesian solutions resulted in these disturbed areas becoming localized centers of dolomitization. Upon complete dolomitization of the shallow marine burrows, this process extended into the adjoining undisturbed sedi- ments (Fig. 2 D, E). A bed of dolomite would thus develop in highly burrowed sediments subject to movements of magnesia-rich solutions for an extended time. Such local beds of dolomite are found in other locations in the Tyrone Limestone (Whaley, 1964). However, in this locality, a decrease of magnesia-rich solutions resulted in the incomplete dolomitization of the shallow marine sediments. The Tyrone Limestone provides an ancient example of environmentally controlled organic activity selectively controlling some early diagenetic changes in carbonate sediments. In addition, it provides an example of early dolomitization in the subtidal, rather than the supratidal environment. ACKNOWLEDGEMENTS In part, field expenses for this study were provided by the George W. Pirtle Fellowship, Department of Geology, University of Kentucky. REFERENCES Deffeyes, K. S., Lucia, F. J., and Weyl, P. D., 1965, Dolomitization of Recent and Plio-Pleistocene sediments by marine evaporite waters on Bonaire, Netherlands Antilles; In: Dolomitization and Limestone Diagenesis, Soc. Econ. Pale- ont. and Mineral. Spec. Publ. No. 18: 71-88. Howell, B. F., 1957, Vermes; In: Treatise on Marine Ecology and Paleontology, Geol. Soc. Am. Mem. 67, (2): 805-816. Laporte, L. F., 1967, Carbonate deposition near mean sea-level and resultant facies mosaic: Manlius Formation (Lower Devonian) of New York State: Am. Assoc. Petrol. Geol. Bull., 51: 73-101. Murray, R. C., 1964, Preservation of primary structures and fabrics in dolomite; In: Approaches to Paleontology, John. Wiley and Sons, New York, p. 388-403. Shinn, E. A., 1968, Burrowing in Recent lime sediments of Florida and the Bahamas: J. Paleont. 42,: 879-894. Whaley, P. W., 1964, A Petrographic study of the Tyrone Limestone, unpub. M. Sc. thesis, University of Kentucky, Lexington, Kentucky, 45 pp. Accepted: June 7, 1973. Transactions of Kentucky Academy of Science, Vol. 34, 1973 5 FISHES OF EAGLE CREEK, NORTHERN KENTUCKY NELSON D. HORSEMAN AND BRANLEY A. BRANSON Department of Biology, Eastern Kentucky University Richmond, Kentucky 40475 ABSTRACT Fifty-two species of fish were collected in Eagle Creek, Northern Kentucky, during the summer of 1972. The collections illustrated well-defined longitudinal succession and habitat preferences. Siltation from agriculture plays a significant role in limiting fishes in the drainage. Several characteristics of the streams are briefly analyzed with reference to proposed damming of the creek by the U.S. Army Corps of-Engineers. INTRODUCTION Eagle Creek is the last large tributary of the Kentucky River before the latter empties into the Ohio River. It rises on the Eden Shale and adjacent calcareous members of the Cincinnatian sequence (Upper Ordovician) (Jillson 1928) in northwestern Scott County. The three main headwater streams, East Fork, West Fork, and Little Eagle Creek, converge in northern Scott County to form Eagle Creek which in turn winds into Owen County, flowing primarily over Cincinnatian rocks but also over some underlying members of Chaplainian (Middle Ordovician) rocks near the Scott-Owen county line (Jillson 1928). Meandering northward through Owen and Grant Counties, Eagle Creek is bedded in Eden Shale (Jillson 1928). In north- western Grant County, at the hamlet of Folsom, Eagle Creek bends 90° to the west. This point represents the point at which Eagle Creek was pirated from its original northeasterly course toward the Ohio River into its present course to the Kentucky River, a mid-Pliocene piracy (Jillson 1949). In its westward flow, Eagle Creek forms the southern boundaries of Gallatin and Carroll counties separating them from Owen County. The creek flows westward over the Eden Shale depositing alluvium in its valley but exposing part of the Cynthiana group in its last miles (Shideler 1929). Eagle Creek lies in an area of rolling erosional hills on a wide floodplain yielding much rich bottomland which is intensively farmed. This tillage has led to moderately heavy siltation which seems to affect the fish fauna (discussed below). Several small towns and villages occur in the drainage, but the largest directly abutting the creek is Glencoe, population 650. Along the eastern perimeter of the basin in Grant County are two larger towns, Williamstown and Dry Ridge, with populations of approximately 2,000 and 1,000, respectively. None of the towns in the basin seems to present an immediate threat to the fauna of Eagle Creek, either from industry (lacking) or municipal sewage. Eagle Creek flows through Oak-Ash-Maple associations, nearly all of the creek being bounded by relatively densely wooded tracts which lend a great deal of shading and cooling to the water during summer. Bentgrass, Agrostis sp., grows in many of the shallow areas along the creek. This vegetation appears to be important cover for several species of fishes. Specimens were collected between 10 June and 17 November 1972, pri- marily by means of various-sized seines. The last station, because of its 6 Transactions of Kentucky Academy of Science, Vol. 34, 1973 greater depth, was also sampled with a 220-volt electric shocker, two one- inch gill nets, and a two-inch trammel net. Seining at each station covered stream lengths of 0.25 to 0.5 mile and was conducted intensively for about 2 hours with emphasis on sampling each type of habitat. The shocker was used for a similar length of time, primarily along the banks, around brush piles and other places of concealment. Gill nets were set for approximately 3 hours, and the trammel net was left out overnight. Five different water chemistry tests were made with a Hach DRL-1 field kit (Table 1) at each station according to methods outlined in Standard Methods for the Examination of Water and Wastewater (1971). Because of limitations of time and funds, no measurements were made of silt and s¢@imentation. For that reason our statements concerning siltation are to Be regarded as qualitative observations. The taxonomy used herein follows that of Moore (Blair, et al. 1968). All specimens were deposited in the Eastern Kentucky University collection. Table 1 Some chemical parameters (in parts per million) of Eagle Creek, Northern Kentucky Collecting Dissolved Calcium Total otation Oxygen Free CO, Hardness Hardness Alkalinity 1 9 15 85.5 1721 171 2 11 30 119 at 153.9 136.8 3 9 35 VyAl 188.1 188.1 h 13 15 136.8 188.1 188.1 5 8 20 136.8 171 153.9 6 8 15 136.8 205.2 153.9 U 8 30 136.8 171 171 8 11 15 153.9 188.1 153.9 9 9 20 136.8 15329 188.1 10 7 20 119.7 alas 188.1 i 8 20 119.7 188.1 153.9 12 "/ 20 136.8 188.1 153.9 13 6 20 136.8 171 153.9 wy 7 30 136.8 171 153.9 15 8 15 15309 188.1 188.1 16 6 30 136.8 171 153.9 Transactions of Kentucky Academy of Science, Vol. 34, 1973 74 ‘ ‘ é ’ ’ é : ’ ’ ‘ ‘ ‘ ‘ ‘ ‘ ’ ‘ ¢ ’ ‘ ’ ‘ ¢ é ‘ \¢ ‘ ’ ‘ é ‘ ? ale ’ ’ ’ ‘ ’ ’ TOPOGRAPHIC MAP INDEX re er aw eee ee ee TT Figure 1. The Eagle Creek Drainage Basin, Northern Kentucky, showing collecting stations. Topographic map quadrangles are indicated by the following numbers: 1—Patriot; 2— Verona; 3—Walton; 4—Vevay South; 5—Sanders; 6—Glencoe; 7—Elliston; 8—Williams- town; 9—Worthville; 10—New Liberty; 11—Owenton; 12—Lawrenceville; 13—Mason; 14—Monterey; 15—New Columbus; 16—Sadieville; 17—Breckinridge; 18—Stamping Ground; 19—Delaplain; 20—Leesburg. COLLECTING STATIONS Stream orders are assigned according to the modified Horton system as described by Kuehne (1962). Primary tributaries, whether intermittent or constantly running, are termed Order 1. The union of any two streams of equal order creates a stream of the next higher order, but no order change is associated with the junction of a stream of lower order (Kuehne 1962). For example, the union of two Order 1 streams creates an Order 2 stream. This type of classification is important to the fish ecologist in analyzing longitudinal distributions. The following are the sites from which our specimens were obtained during the summer and fall of 1972 (Fig. 1). 1. Little Eagle Creek, 2.5 miles southwest of Sadieville, Scott Co., near State Highway 32; Order 3. 10 June. 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East Fork of Eagle Creek, 3.6 miles southeast of Sadieville, Scott Co., on Davis-Turkeyfoot Road; Order 3. 10 June. 3. Eagle Creek, 0.75 mile north of Sadieville, Scott Co., on Hinton Road; at and upstream from the mouth of Elk Lick Branch; Order 4. 12 June. 4. Juncture of Little Eagle and Eagle Creeks, 2.5 miles northwest of Sadieville, Scott Co., Interstate Highway 75 bridge; Order 4. 12 June. 5. Eagle Creek, 2.6 miles southeast of Natlee, Owen-Scott Co. line; Order 4, 4 July. 6 aoe Creek, at and near its mouth on Eagle Creek, 2.3 miles north- northwest of Natlee, Owen Co., on State Highway 281; Order 4. 4 July. 7. Eagle Creek, 1.0 mile east of Lusby’s Mill, Owen Co., on Highway 1739; Order 5. 15 July. 8. Eagle Creek, 0.7 mile south of Needmore, Owen Co., Near Fortneroy Road; Order 5. 15 July and 15 October. 9. Eagle Creek, 2 miles northwest of Lawrenceville, Grant Co., on High- way 1993; Order 5. 5 August. 10. Eagle Creek, 2.2 miles south of Four Corners, Grant Co., on State High- way 22; Order 5. 5 August. 11. Eagle Creek, 2.0 miles south of Folsom, Grant Co., near Highway 1132; Order 5. 8 August. 12. Eagle Creek, 0.6 mile south of Glencoe, Gallatin-Owen Co. line, at U.S. Highway 127; Order 6. 12 August. 13. Eagle Creek, 1.3 miles east of Sparta, Gallatin-Owen Co. line, near State Highway 461; Order 6. 12 August. 14. Eagle Creek, 0.5 mile south of Sanders, Carroll-Owen Co. line, near State Highway 47; Order 6. 9 September. 15. Eagle Creek, 0.8 mile southeast of Eagle Station, Carroll-Owen Co. line; Order 6. 9 September, 15 October, and 17 November. 16. Mouth of Eagle Creek 1.0 mile south of Worthville, Carroll-Owen Co. line; Order 6. 23 September. DISCUSSION Of the fifty-two species collected: (Table 2), none was found at all 16 sites; all demonstrated some degree of habitat selectivity. Four species, Notropis ardens (Cope), Pimphales notatus (Rafinesque), Lepomis megalotis (Rafinesque), and Micropterus punctulatus (Rafinesque), exhibited a wide distribution and tolerance of habitats. Two minnows, Notropis ardens (Cope) and Pimephales notatus (Rafinesque) are the dominant forage species throughout most of the stream until replaced by such species as Notropis atherinoides Rafinesque, Notropis spilopterus (Cope) and Notropis buchanani as the stream becomes Order 6. Two centrachids, Lepomis megalotis and Micropterus punctulatus have a wide distribution, and although their num- bers were smaller they represented a significant portion of the biomass. Four species of darters of the genus Etheostoma, E. blennioide blennioides Rafinesque, E. flabellare Rafinesque, E. nigrum Rafinesque, and E. spectabile (Agassiz), were collected in the drainage. Each of these was found in the headwaters, with one, E. spectabile (Agassiz) being confined to the smallest tributary, Little Eagle Creek, indicating its preference for low-order streams. The remaining three species were collected in all areas that contained riffle habitats. Darters of the genus Percina were collected in Order 4 and larger segments but, unlike the Etheostoma, were collected in pools as well as Transactions of Kentucky Academy of Science, Vol. 34, 1973 1l rifles. This characteristic allows the Percina to replace the Etheostoma in high order streams which have no riffles. Kuehne (1962) stated that successional changes in fishes were strongly correlated with stream-order changes. Several examples of this phenomenon could be cited, but one noteworthy example, Notropis ardens, will suffice for our purposes here. This species is highly abundant in Eagle Creek stations until the stream becomes Order 6. Here, a sharp drop in abundance was noted and this trend continued as the stream became larger. Finally, the species was entirely replaced by several other cyprinids (e.g., Notropis atherinoides and Notropis buchanani). An increase in the diversity of species also has been recorded with increasing stream order (Kuehne 1962). In Eagle Creek, 17 species were found in Order 5, 22 species in Order 4, 25 species in Order 5, and 40 species in Order 6 stream segments. The amount of siltation present in Eagle Creek apparently has altered the fish fauna and will continue to do so. Rapid, dramatic alterations or exterminations of fish faunas by extreme siltation from such practices as strip mining or clearcut logging have been studies by several authors, in- cluding Branson and Batch (1971), Hall and Lantz (1969), and many others. However, virtually no work has been done on the subtle effects upon reproductive success and feeding habits caused by moderate but chronic siltation. This type of siltation seems to promote some species (e.g., Micropterus punctulatus, Lepomis megalotis and Phenacobius mirabilis (Girard) (Hubbs and Lagler 1958), while limiting others, (e.g., suckers and Lepomis macrochirus. Siltation may play a very significant role in impounded streams, some- thing which should be considered before impounding a stream such as Eagle Creek. At the present time a dam on Eagle Creek is in the planning stages by the U.S. Army Corps of Engineers. Silting usually begins to reduce the bottom fauna in the deeper portions of lakes within the first three to five years of impoundment (Ellis 1942). Likewise, density currents carrying heavy silt loads often flow through such impoundments to the detriment of the fish fauna (Ellis 1942). Silt loads may directly or indirectly affect organisms in lentic habitats by altering such chemical contents as dissolved oxygen and mineral salts (Ellis 1936). Alteration of physiography by impoundment can eliminate many habitats by reducing shallow areas along the shoreline (Ellis 1942). This, of course, could severely limit several species’ members in Eagle Creek if the proposed impoundment is constructed. A notable example is the spotted bass, a widely distributed and abundant species in the drainage. Most spotted bass were collected near the banks or from beneath cover such as undercut banks, roots, and brush. Such habitats are virtually eliminated by the steep banks and fluctuating depth of man-made lakes. At best, the gain in total poundage of harvestable fishes in man-made impoundments is a trade-off against the types previously present in the stream. Therefore, several important aspects related to Eagle Creek need to be considered. First is the possible complications due to siltation. Second is the high cost of the recommended impoundment project—$22.55 million— (U.S. Army Corps of Engineers 1973). These aspects are both related to the planned impoundment. The creek as it presently stands is, as demonstrated by this survey, a reservoir for a widely diverse population of fishes; and with the extensive 12 Transactions of Kentucky Academy of Science, Vol. 34, 1973 dammings already completed throughout the state on comparable sized bodies of water (e.g., Dix River, Middle Fork, etc.) the authors feel that Eagle Creek would best be left in its lotic state. ACKNOWLEDGEMENTS Special thanks are due several persons for their assistance in this project. First, thanks to W. H. Engelhardt, Norman Crisp, Glenn White and Bruce Bauer, all students at Eastern Kentucky University, for field assistance, and to Dr. William Martin who identified vegetation samples. Also, we are indebted to Professor William Adams, Department of Geography, Eastern Kentucky University, from whom we acquired the base map of the Eagle Creek drainage. LITERATURE CITED Blair, W. F., et al. 1968. Vertebrates of the United States. 2nd ed. McGraw-Hill Book Co., New York. G. A. Moore, Fishes: 22-165. Branson, B. A., and D. L. Batch. 1971. Effects of strip mining on small stream fishes in east central Kentucky. Proc. Biol. Soc. Wash. 84 (59): 507-518. Ellis, M. M. 1936. Erosion silt as a factor in aquatic environments. Ecology, 17 (1): 29-42. . 1942. Freshwater impoundments. Trans. Amer. Fish. Soc. 71: 80-93. Hall, J. D., and R. L. Lantz. 1969. Effects of logging on the habitat of coho salmon and cuttroat trout in coastal streams. H. R. McMillan Lectures in Fisheries, Symposium on Salmon and Trout in Streams, Univ. of Brit. Col. Vancouver, Canada. 355-375. Hubbs, C. L., and K. F. Lagler. 1958. Fishes of the Great Lakes region. Univ. Mich. Press, Ann Arbor. 213 p.. Jillson, W. R. 1928. Geology and mineral resources of Kentucky. Ky. Geol. Surv. Ser. VI, 17. Frankfort, Ky. 409 p. . 1949. The piracy of Eagle Creek. Ky. Geol. Surv. Misc. Publ. Frankfort, Ky. 31 p. Kuehne, R. A. 1962. A classification of streams illustrated by fish distribution in an Eastern Kentucky Creek. Ecology 43: 608-614. Shideler, W. H. 1929. Geologic map of Carroll County Kentucky. Ky. Geol. Surv. Frankfort, Ky. Taras, M. J. et al. (ed), 1971. Standard methods for the examination of water and wastewater. 13th ed. Amer. Pub. Health Assoc. Inc. Wash. D.C. 874 p. U.S. Army Corps of Engineers District, Louisville. 1973. Eagle Creek Lake Environmental Study Kentucky. Louisville, Ky. 20 p. Received: February 21, 1973. Accepted April 27, 1973. Transactions of Kentucky Academy of Science, Vol. 34, 1973 13 PRELIMINARY INVESTIGATIONS OF A HEADWATER CREEK IN EASTERN KENTUCKY G. L. SAMSEL, JR., J. R. REED, AND R. R. DAUB Department of Biology, Virginia Commonwealth University, Richmond, Virginia 23220 ABSTRACT Investigations of a headwater stream, Rich Creek, in south-central Lawrence County, Kentucky, were initiated to ascertain the feasibility of impounding this water for construction of an environmentally controlled recreational reservoir. In addition, baseline data were gathered to facilitate future studies on effects of sedimentation and erosion. Data collected on physical and chemical parameters, algae, fish, and bottom fauna, as well as primary productivity, indicated that Rich Creek was an undis- turbed, headwater stream. Floral and faunal composition and relative abundance indicated good water quality. Nutrient values and primary productivity were low, and in general all parameters analyzed were indicative of a moderate flow, clean, headwater stream which would provide good quality water for a recreational impoundment. INTRODUCTION Investigations of a headwater stream, Rich Creek, in south-central Lawrence County, Kentucky, were initiated to ascertain the feasibility of impounding this water for construction of an environmentally controlled recreational reservoir. The reservoir will be constructed by a private recreational land development firm, Wellman Corporation, Adams, Kentucky. In addition, baseline criteria were collected to facilitate future studies on the effects of sedimentation and erosion resulting from earthmoving opera- tions and dam construction. Rich Creek is a small intermittent headwater stream, 8.6 km in length with immediate drainage into Blaine Creek near the junction of Kentucky Rt. 32 and Rich Creek Road. Further drainage patterns include the Big Sandy and Ohio rivers. No published data are available on any streams in this area of eastern Kentucky. The stream originates, and for the most part, flows through undisturbed, nonagricultural forested area with only occasional pertubation by lumbering operations. In addition, the stream basin and immediate watershed are composed of sedimentary rock formations, low in nitrogen, phosphates, iron, chlorides, and sulfates (Daily 1938, Hopkins 1970). For these reasons, Rich Creek was chosen as a possible inflow source to impound for con- struction of a controlled, low-nutrient reservoir. Biological and chemical parameters of the stream were investigated on six occasions between June 1971 and August 1972. The preliminary nature of this study must be stressed. Further investigations are continuing in an effort to evaluate the effect of impoundment on a section of Rich Creek. MATERIALS AND METHODS Six sampling sites were selected along a 4.7-km stretch of stream, and periodic collections were made for algal identifications, chemical nutrients, 14 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Figure 1. Sampling stations on Rich Creek lmile impoundment Lawrence Co. Site Big Sandy R. productivity analysis, and physical measurements of light, temperature, and flow rate over a 14-month period. Fish and bottom fauna collections were made on three occasions. Sampling sites ranged from the stream’s origin through the proposed impoundment area and continued far enough down- stream below the damsite to encompass as many habitats as possible (Fig. 1). With the exception of two small ephemeral pool areas along the 4.7-km sampling area, shallow riffle areas dominated. All six sampling sites selected were along the riffle areas of Rich Creek. Site 6 at the head of the impound- ment area differed insignificantly from the other five. Incident radiation was measured with a Belfort pyrheliometer Model 68. Air and water temperatures were recorded with a standard mercury thermometer, +0.1 C accuracy. Flow rates were determined by using pulse injections of fluorescein dye over a 10-m section of stream and capture of inflow into large plastic bags stretched across the stream. Algae in net tows, from water edge collections, and on submerged debris were identified to genus often after concentration by filtration. Culturing of several epiphytic algae in streamwater enrichment media Transactions of Kentucky Academy of Science, Vol. 34, 1973 15 facilitated certain identifications. Bottom fauna samples were collected using the equal time-effort method of Cairns et al. (1968). Fish sampling em- ployed D-frame dipnets and 10-foot fine-mesh seines. Future investigations will concentrate more on fish and bottom fauna collections. Analysis of dissolved chemicals in the field were made with a Hach Model DREL Kit and accessories, replicate samples yielding values within +5%. Laboratory analyses using standard method procedures were also employed. Resuspended stream sediments were analyzed for chemical com- position using standard method procedures (Amer. Public Health Assoc. 1971). Total chorophyll per liter of stream water was determined by acetone extraction of particulate matter retained on millipore GS filters with 0.22p, pores. The acetone extracts were analyzed with a Bausch and Lomb Spectronic 20, using equations by SCOR/UNESCO cited by Strickland and Parsons (1968) and adjusting calculated concentrations to values equivalent to 10-cm path length tube determinations. Primary productivity of attached algae was also determined by the in situ carbon-14 method of Steeman Nielsen (1952) as modified by Goldman (1963) and Strickland and Parsons (1968). The primary productivity methods were modified to measure productivity of attached and macroscopic algae by expressing the productivity as milligrams of pigment of carbon per 100 mg of algal dry weight. All values for total chlorophyll and carbon fixation are means of duplicate samples, differing by less than 10%. Although six sampling sites were investigated along a 4.7-km stretch of Rich Creek, data on all para- meters measured varied less than 15% between individual stations. There- fore to simplify the tables, data have been averaged for all stations. EXPERIMENTAL RESULTS AND DISCUSSION Physical and Chemical Parameters The basin and immediate watershed area of Rich Creek consist of sedimentary rock formations, sandstone, limestone, and shale. The area is rich in coal and gas deposits. Ferric and ferrous minerals are found on the surface of many of the sedimentary formations. Siliceous minerals are plentiful with moderate amounts of chlorides and a notable lack of phos- phates in basin watershed formations (Hopkins 1970). Water temperatures ranged from 1.0 to 24.6 C during the sampling period. Radiation varied from levels below detection to 1.0 langley/min at approximately 10 cm depth where productivity measurements were made. Flow rates ranged from 1.0 m/sec during the spring rainy season to less than 0.1 m/sec during the drier summer periods. For the most part, Rich Creek never exceeded 2.3 in width and 25 cm in depth in the riffie areas and 4 m in width and 45 cm in depth in the two pool areas. Table 1 summarizes physical and chemical data for Rich Creek; the values are means of the six sampling stations. Note in particular the low total carbon values. Higher values were expected due to the coal, gas, and unmetamorphosized shale deposits of the area. Ammonia nitrogen values appear slightly high for an unperturbed nonagricultural area (Steinbeck 1966). Values for silica are indicative of the rich siliceous sedimentary formations through which Rich Creek flows. Other chemical nutrient 16 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Table | Some physical and chemical parameters of Rich Creek (mg/1 or as indicated; values means of sampling Stations 1-6) Parameter June 1971 Aug. 1971 Nov. 1972 Jan. 1972 Apr. 1972 Aug. 1972 NH), *-N 25 0.2 ‘2 0.35 0.06 0.4 Ortho PO) -P 0.01 0.0 -0 0.05 0.05 0) NO.”-N 0.30 0.15 4 3.0 2.0 0) NO, -N 0) 0) 0 0) 0.01 0) Total Alkalinity 20.0 ---- 18.0 10.0 22.0 30.0 Cat 20.0 — 10.0 12.0 10.0 30.0 Fett 0.2 0.1 0.2 0.5 0.15 0) Total Hardness 30.0 ---- ==-- 25.0 40.0 30.0 Si. 6.0 ===> 7.0 8.0 14.0 30.0 Cis TiO 5.0 7.0 8.0 9.0 13.0 F1- 0) a 0) 0) 0) 0) pH 6.80 —— 6.75 6.72 6.84 6.95 SO), 10.0 ==== 15.0 20.0 12.0 15.0 Turbidity (JTu)1 25.0 —— 30.0 ---- ---- 50 ‘Dissolved Oo 10.0 =se= 11.0 12.0 13.0 9.0 Total Organic C 9.0 — 7.5 oe 7.0 8.1 ly~y = Jackson Turbidity Units values, pH, and turbidity levels reflect the nutrient-poor geologic formation, nonagricultural area (Hynes 1960, Hopkins 1970). Results of resuspended sediment material were similar to the values found in Table 1 with the exception of slightly higher Fe++ and total C values. The major nutrients including ammonia nitrogen, phosphate phos- phorus, nitrate nitrogen, and sulfate varied less than 15% between bottom sediments and stream waters; higher values occurred in the sediments. Following combustion at 500 C, the sedimentary shale bottom sediment from the stream, dried previously at 100 C, lost less than 20% of its weight. Algal Genera, Chlorophyll, and Primary Productivity The algae in Rich Creek during the sampling period consisted pre- dominately of filamentous and macroscopic Chlorophyta (green algae), Ulothrix, Spirogyra, Stigeoclonium, and Cladophora, and planktonic and epiphytic Chrysophyta (diatoms) Navicula, Gomphonema, Nitzschia, and Cymbella (Table 2). Seasonal changes in algae distribution were observed with greatest species composition in the summer periods (Daily 1939, Round 1966). Diatoms were plentiful and diverse flourishing in the high Transactions of Kentucky Academy of Science, Vol. 34, 1973 17 Table 2 Algal genera in Rich Creek. Identification of several of these algae are tentative pending further study in cultures; D = Dominant (>40% of sample), 0 = Occasional (10-40% of sample), R = Rare (<10% of sample), — = Absent; quantitative data not collected in November 1971. Sampling Dates Genus: June 1971 Aug. 1971 WNov. 1971 Jan. 1972 Apr. 1972 Aug. 1972 Closteridium R R - ~ R 0 Chlamydomonas - R + = = = Ulothrix D D + D - D Spirogyra D D + (0) - D Stigeoclonium D D + = = D Cladophora D (0) + (6) = D Coelastrum - - ~ - - R Zygnema - R + = = = Oedogonium = - + = R = Cosmarium - - + - R Oscillatoria 0) - - = = R Gomphonema D D + D D D Navicula D D + 3) D D Fragilaria 0 0 7 - ) fe) Surirella - 0 + R - - Nitzschia D D as D 6) D Cymbella D D + (0) - D Pinnularia 0) (0) + - = ie Synedra - R = = = = silica waters of the stream (Williams 1964). For the most part, the algae present during sampling periods were indicative of slow to moderate flow, intermittent clean water streams (Palmer 1955, 1969). As the distribution of algae collected was fairly random and dispersed equally between the six sampling stations, Table 2 represents species composition of all sampling stations. Results of productivity analyses (Table 3) are means of the six sampling stations. Also, the results are expressed as averages of 24-hr diel experiments run for each sampling date indicated. Productivity measurements were employed on planktonic as well as attached and epiphytic algae. As Table 3 indicates, values for both chlorophyll extraction and carbon-14 fixation exemplify oligotrophic, low-nutrient, low-productivity waters (Odum 1956, Hutchinson 1957). No consistent correlation existed between chlorophyll and carbon fixation during our sampling period. However, seasonal variations Transactions of Kentucky Academy of Science, Vol. 34, 1973 18 (ace 9°6 eS) ae 3 Te ANG Ot: T'0 OT‘ Gal 9°0 1° 02 9°OT Tt Z£°0 S0°0 ZO" cL6L “ony el6t “4dy elét ‘uer 0° 6T Lt c°0 Site TL6T “AON soqeq Suttdwed 0°62 6°9 ele) 1° 6E (q4 Arp su QOT/D Su sesTe — peyoeyjy) uot IexTy 20470 €°g (74 Arp Bu OOT/JueusTd/3m -se3Te peyoeyiy) TTAydoz0TyD Whe cu/queustd sm -oeSTe ofTuczyueTq) TTAydozo Typ TE*O (des/m) e7ey ACTA 9°8T (D0) 21n4e 1edu9 i, O€* (UTW/*suUeT) UOTIeTpPeY TL6T Sune Jojowe reg ‘yydep wo ye sioyeM YyoeID Yyory jo AWAHONpoid Arewud pue {[Aydoropyo 9[qe}0e.4xe [v}0} ‘UOTeIpPeL ‘oInje1odUIe} Jo s}USWOINsvsU [eIp Udy Transactions of Kentucky Academy of Science, Vol. 34, 1973 19 Table 4 Macrobenthic Fauna in Rich Creek. D = Dominant (>40% of sample), R = Rare (<10% of sample), O = Occasional (10-40% of sample); quantitative data not collected in January 1972. Order June 1971 January 1972 August 1972 Ephemeroptera Baetidae D + D Ephemeridae (0) + (0) Heptageniidae (6) + (0) Plecoptera Peltoperlidae R + R Nemouridae 0 + (0) Perlidae D + D Odonata Coenagrionidae (0) => (@} Libellulidae D + D Diptera Chironomidae - - (0) Trichoptera Hydropsychidae (0) + (6) Limnephilidae D + D for both chlorophyll and carbon-14 fixation were observed. Also, typical patterns for productivity values were observed during diel measurements (Goldman 1966). Bottom Fauna The bottom fauna of Rich Creek was indicative of a moderate flowing headwater stream although extensive seasonal sampling was not done. There were eleven families collected and of these the mayflies (Ephemero- ptera), stoneflies (Plecoptera), dragonflies and damselflies (Odonata), and caddisflies (Trichoptera) were the most common (Table 4). Numbers of individual organisms of each family varied considerably during each sampling period from 27 individuals per square foot (caddisflies) to 3 per square foot (stoneflies). Chironomidae were present during one sampling period from Station 6 alongside a road culvent filled in with debris and straw. The low dissolved oxygen and rapid decomposition associated with this area may have induced the short-lived chironomid development. Total species composition of organisms did not change between the two summer sampling periods, June 1971 and August 1972. Table 4 represents total abundance of macrobenthic fauna collected from all six sampling sites. Investigations are continuing in an effort to classify the macrobenthic fauna to the species level. 20 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Fishes Like the bottom fauna, limited sampling was done, but the fishes collected were typical of cool, relatively small, headwater streams. Six species were found, of these the blacknose dace (Rhinichthys atratulus), and the southern redbelly dace (Phoxinus erythrogaster) were the most common. Also present but in fewer numbers were the creekchub (Semotilus atromaculatus) and the rosyside dace (Clinostomus funduloides). Two centrachids were present, the green sunfish (Lepomis cyanellus), and bluegill, (Lepomis macrochirus), the latter probably introduced. These fishes do not represent the total fish fauna of Rich Creek but only the extreme headwater area studied. Another typical headwater family, the Percidae containing the darters, was not present in the three collections made but future sampling should produce members of this group since the Big Sandy drainage contains several darters, especially of the genera Percina and Etheostoma (Holt 1971). Like the other parameters sampled in this study the fish fauna reflects the good water quality of Rich Creek. SUMMARY Preliminary data on physical and chemical parameters, algae, fish, and bottom fauna, and primary productivity indicate the undisturbed headwater nature of Rich Creek. Species composition and relative abundance indicated good water quality. Nutrient values for Rich Creek were, for. the most | part low, as was primary productivity. In general, all parameters analyzed were indicative of a moderate flow, clean, headwater stream that: would provide good quality water for a recreational impoundment. The baseline information gained from this study will be useful to later evaluate the effects of stream impoundment and reservoir construction and operation. REFERENCES American Public Health Association, American Water Works Association, and Water Pollution Control Federation. 1971. Standard Methods for the Examination of Waste and Waste Water, 13th Ed. Amer. Publ. Health Assoc., New York. 873 pp. Cairns, J., Albaugh, D. W., Busey, F., and Chanay, M. D. 1968. The sequential comparison index—a simplified method for non-biologists to estimate relative differences in biological diversity in stream pollution studies. J. Wtr. Poll. Cont. Fed. 60: 1607-1613. Daily, W. A. 1938. Distribution of the algae of Kentucky in relation to soil regions. Castanea 3: 32-35. Daily, W. A. 1939. A checklist of the algae of Kentucky. Castanea 4: 27-37. Goldman, C. R. 1963. The measurement of primary productivity and limiting factors in freshwater with 14C. In: Proc. Conf. Primary Prod. Measurement, Marine and Freshwater. Pp. 103-113. Hawaii, 1961, USA & CTIO 7633. Goldman, C. R. (ed.) 1966. Primary Productivity in Aquatic Environments. Mem. Ist. Ital. Idrobiol., 18 Suppl., Uni. of Calif. Press, Berkeley, 464 pp. Holt, Perry C. (ed.) 1971. The distributional history of the biota of the Southern Appaiachiazs. Research Division Monograph 4. Virginia Polytechnique In- stitute and State University, Blacksburg, Virginia, 36 pp. Hopkins, H. T. 1970. Occurrence of freshwater in the Lee formation in parts of Transactions of Kentucky Academy of Science, Vol. 34, 1973 21 Elliott, Johnson, Lawrence, Magoffin and Morgan counties eastern coal field region, Kentucky. USGS Bull. 1867, pp. 44. Hutchinson, G. E. 1957. A Treatise on Limnology. Vol. II. Introduction to lake biology and limnoplankton. New York, John Wiley & Sons, 1107 pp. Hynes, H. B. N. 1960. The Biology of Polluted Waters. Liverpool Univ. Press, Liverpool, 202 pp. Odum, H. T. 1956. Primary productivity in flowing waters. Limnol. Oceanogr., 1: 102-117. Palmer, C. M. 1955. Distribution of algae in Big Sandy River water near Catlettsburg, Kentucky. Report of Survey, Sept. 22-23, 1955, Biol. Sec., R. A. Taft San. Eng. Center, Cincinnati, Ohio, 7 pp. Palmer, C. M. 1969. A composite rating of algae tolerating organic pollution. J. Phycol. 5(1): 78-83. Round, F. E. 1966. The Biology of the Algae. St. Martins Press, New York, 269 pp. Steeman Nielsen, E. 1952. The use of radioactive carbon (14C) for measuring organic production in the sea. J. Con. Internatl. Explor. Mer. 18: 117-140. Steinbeck, J. T. 1966. An ecological investigation of the algal genera (and other biota) in waters polluted by mineral acid-drainage from coal mines in Vinton County, Ohio, 1956-1966. M.A. Thesis, Ohio State University. Strickland, J. P., and Parsons, J. R. 1968. A Practical Handbook of Seawater Analysis. Bull. Fish. Res. Can. No. 167. 387 pp. Williams, L. G. 1964. Possible relationships between plankton-diatom species numbers and water-quality estimates. Ecology 45(4): 809-823. aD Transactions of Kentucky Academy of Science, Vol. 34, 1973 EFFECT OF A METHOXYL GROUP ON THE DECARBOXLYATION OF 2-PYRIDINECARBOXYLIC ACIDS ELLIS V. BROWN, RUSSELL J. MOSER AND MANVENDRA B. SHAMBHU Contribution from the Department of Chemistry, University of Kentucky, Lexington, Kentucky 40506 ABSTRACT The rates of decarboxylation of 4-methoxy-2-pyridinecarboxylic acid and 3- methoxy-2-pyridinecarboxylic acid in 3-nitrotoluene were measured and compared with the kinetic data from 6-methoxy-2-pyridinecarbovylic and 5-methoxy-2- pyridinecarboxylic acids in 3-nitrotoluene. The AG}5o9, AStoo9, and AHt ao were then determined. An examination of the AGt for these acids indicates that ab- normally large and small values for AG} were observed in the case of 6-methoxy- and 3-methoxy-2-pyridinecarboxylic acids respectively. These apparent dis- crepancies were satisfactorily explained on the basis of the large steric effects exerted by the methoxyl groups in the ortho positions. It has been shown recently that one mechanism can not be used to explain the decarboxylation of both 5- and 6-methoxy-2-pyridinecarboxylic acids.6 The 5-methoxy-2-pyridinecarboxylic acid appears to have a zwit- terionic transition state,® while the exact nature of the transition state for 6-methoxy-2-pyridinecarboxylic acid is not known.*? To gain insight into the mechanism of decarboxylation of 6-methoxy-2-pyridinecarboxylic acid and the nature of steric effects on the decarboxylation of 2-pyridinecarboxylic acid, we have made the following assumptions: (a) the transition state of the 4-methoxy-2-pyridinecarboxylic acid should be similar to the transition state of 6-methoxy-2-pyridinecarboxylic acid but should lack the steric effect present in the latter? and (b) the transition state of 3-methoxy-2-pyridine- carboxylic acid should be similar to that of 5-methoxy-2-pyridinecarboxylic acid; however, an ortho steric effect may be present in the former which is not present in the latter. In this report we present the rate data and com- plete set of activation parameters for 3- and 4-methoxy-2-pyridinecarboxylic acids. Experimental The 3- and 4-methoxy-2-pyridinecarboxylic acids were synthesized and their rates of decarboxylation were determined in 3-nitrotoluene. The ap- paratus,* method,? and preparation of these compounds? have been described previously. Results and Discussion The rate data and complete set of activation parameters for 3- and 4- methoxy-2-pyridinecarboxylic acids and other pertinent compounds are shown in Table 1 and 2 respectively. It can be seen (Table 1) that 4- methoxy-2-pyridinecarboxylic acid required a temperature of only ca 160° to yield a rate of decarboxylation similar to that of 6-methoxy-2-pyridine- carboxylic acid at ca 220°. Also it can be seen that 3-methoxy-2-pyridine- carboxylic acid yielded a rate constant at ca 100° that was similar to a rate constant at ca 202° for 5-methoxy-2-pyridinecarboxylic acid and ca 220° for 6-methoxy-2-pyridinecarboxylic acid. Clearly the temperature required to Transactions of Kentucky Academy of Science, Vol. 34, 1973 23 Table 1 Apparent First-Order Rate Constants for the Decarboxylation of Methoxy-2-pyridinecarboxylic Acids in 3-Nitrotoluene? Rate Constant Coefficient Standard Acid Temp. °C x 104 sec Variation Deviation 6-methoxy-2- 200.04 0.33 = ee, pyridinecarboxylic 204.5 0.47 3.91 -009 acid> 3 210.6 1.23 3.95 -012 AI a5 2.03 1.01 -005 218.2 2.60 0.89 -003 224.8 4.85 0.37 -002 5-methoxy-2- 189.6 0.95 0.39 001 pyridinecarboxylic 194.9, 1.58 0.24 -001 acid® 200.0 2.67 ---- ---- 200.2 2.89 1.05 -005 204.2 3.95 0.76 -004 210.0 6.78 1.43 -009 4-methoxy—2- 150.4 1.02 0.30 001 pyridinecarboxylic 154.9 1.68 1.05 005 acid 160.3 3.24 1.56 -009 164.4 4.45 1.07 -006 169.6, 7.63 2.15 014 200.0 310. ---- -_-— 3-methoxy-2- 91.5 1.60 0.63 -003 pyridinecarboxylic 95.2 Tei2 2.03 -010 acid 100.9 3.14 1.45 -009 104.6 4.57 0.66 004 110.4, 8.18 1.74 .008 200.0 3840 ---- -_—- 2-pyridinecarboxylic 158.5 0.57 Sippel -006 acidb 163.6 1.22 4.31 016 169.8 1.92 1.21 007 175.5 2.96 aks7/s} -008 179.5, 4.49 1.14 -008 200.0 26.5 ---- === The concentration of the reaction mixture is ca. 0,015 M in all cases, R. J. Moser and E. V. Brown, J. Org. Chem., 36, 454 (1971). R, J. Moser and E. V. Brown, ibid., 37, 3938 (1972). Calculated from other rate constants. aowp decarboxylate 3- and 4-methoxy-2-pyridinecarboxylic acids is much lower than the temperature required to decarboxylate 5- and 6-methoxy-2-pyridine- carbovylic acids. An examination of the data in Table 2 indicates that the methoxyl group has a pronounced effect on the free energy of activation (AG{) for the decarboxylation depending upon its position on the pyridine nucleus. The difference between the largest and the smallest AG} is 8.8 kcal. In contrast, the methyl group is known to have only a slight effect on the decarbovyla- tion,® the difference in this series being 1.68 kcal. Obviously the methoxyl group can alter the rate of the reaction much more effectively due to its larger electronic and steric effects. As compared to the unsubstituted acid, a relatively large AG{ value is exhibited by 5-methoxy-2-pyridinecarboxylic acid (Table 2). The de- stabilization of the transition state by the electron-donating methoxyl group at the 5-position (by resonance) must be responsible for this increase.® Transactions of Kentucky Academy of Science, Vol. 34, 1973 24 “(TL6T) €00% 9€_‘*PFGF ‘umorg “A “a pue nyqueys “a “W, “(ZL6T) SE6€ “ZE S*PFGE ‘umozg “A “A pue TesoW “Cf “UY, “(TL6T) ¥Sy “9€ ‘*WeyD “S320 *f ‘uMoag “A “a pure TESOW “LC “A, “OOT * [(H UT JO enTeA eBer0Ae) + (A UT JO UOFIeTASp pzepueds) } :SMOTTOF SB pezeTNoTeo SF 31 +3987 so UOFIETNOTeD Oy} UF AFF eaenbs 4seaT 9Yy} 1OZ SNTeA 34} ST STUL, ra-*°"a = HAV, OT’ ileal 0° o+ 9°SE G°9€ L°ee ApoB SOR Lared —jeveuTpTrzhd-Z TELS 7°T 9°OT- T°9¢ T°Sé 30°62 PpRoe JFTAKoq -ie aut pTrAd -7—Axoyjeu-¢ 70° €S°0 0° c+ 6° LE 8°8e ae cf poe oF TAxoq —1e oUF pTsAd -7—-Kkxoyjou-4 €0° T?°O0 O° et+ 0°c? 0°eV 6°SE pero? DFTAKOg -1e deur pFazkd -7—-Axoy.ou—-G LT° 0°? 9° 6c+ 8°TS 6°¢S B°LE Boner oT TAKOq -ie.0uTprazhd -z-Ax0yjeou-9 uoTIepTASd Baoan aan apou/Sep/Te9 eToM/Tedy eToW/Teoy sTou/Teoy 5° 002 002 40e 002 pzepuels JUSTIFZJ09 {SV {HV a 4V PPOV B Fc a a ee aUANJOJOIIN-E Ul sploy orAxoqueoourpriAd-Z-Axoy}oJ JO UONe[Axoqieoaq] OY} JOF srojourVIeT UORBAHOY TOpIO Sih quoreddy Z PAqOL Transactions of Kentucky Academy of Science, Vol. 34, 1973 95 a“ RAP Ee Be Mit on —— Re 6 N om NeTG O 0 H~ The methoxyl group in the 4-position causes a decrease in AG} as compared to the unsubstituted acid. The slight electron-withdrawing inductive effect of this group from the meta position is capable of accounting for this decrease. The methoxyl group in the 6-position is also meta to the develop- ing negative charge. Instead of a decrease in AG} (as predicted by the electron-withdrawing inductive effect), a large increase is actually observed. As the methoxyl group in the 6-position lies close to the reaction site, its steric effects cannot be neglected and in fact must overwhelm the small electronic effect. The most likely role of the methoxy] group in the 6-position is to shift the equilibrium between I and II (Scheme 1) to the left by effectively blocking the ring nitrogen. If this explanation were valid, the methoxyl group in 3-position is expected to shift this equilibrium in the opposite direction and lower the AG} for the series. This large decrease in AG} cannot be explained by the small inductive effect of the methoxy group (co = 0.2) alone. A large range of AS} is also shown by the methoxy-2- pyridinecarboxylic acids. This range probably indicates that the transition states for decarboxylation involve different degrees of orientation. This also reflects that different mechanisms could be involved as postulated.* In con- clusion, the data prsented herein indicate that steric effects can cause great variations in the activation energies for the decarboxylation and can be more effective than the electronic effects. REFERENCES fe KG, pe Pederson, J. Amer. Chem. Soc., 51, 2098 (1929). 2. L. W. Clark, J. Phys. Chem., 66, 125 (1962). Sen Ji Moser and E. V. Brown, J. Org. Chem., 36, 454 (1971). 4, E. V. Brown and M. B. Shambhu, ibid., 36, 2002 (1971). 5. N.H. Cantwell and E. V. Brown, J. Amer. Chem. Soc., 74, 5967 (1952). 6. R. J. Moser and E. V. Brown, J. Org. Chem., 37, 3938 (1972). Received: August 21, 1972. Accepted, February 9, 1973. 26 Transactions of Kentucky Academy of Science, Vol. 34, 1973 THE ULTRAVIOLET SPECTRA OF SOME 9-ANTHRACENECARBOXALDEHYDE HYDRAZONES. EVIDENCE FOR A PLANAR STRUCTURE IN METHANOL.? RUSSELL J. MOSER? AND ELLIS V. BROWN Department of Chemistry, University of Kentucky Lexington, Kentucky 40506 ABSTRACT The ultraviolet spectra of seven 9-anthracenecarboxaldehyde hydrazones have been studied and compared with 9-anthracenecarboxaldehyde, 9-anthracenecarbox- ylic acid, and other 9-substituted anthracenes. The hydrazone spectra resembled that of 9-anthracenecarboxaldehyde and not that of 9-anthracenecarboxylic acid. The large degree of interaction of ring and substituent 7-electrons in these hydra- zones is attributed to a decrease in the steric effects which are present in the carboxylic acid. Consideration of molecular models suggests that the peri-hydrogen atoms in anthracene might exhibit a steric effect. As the 9-substitutent is forced out of the plane of the aromatic ring, the conjugation is decreased, and hence, the resonance stabilization energy is diminished. The con- formation of the substituted molecule thus depends on the relative magni- tudes of the resonance stabilization energy and the interaction energy. The long wavelength 7 — z°* transition of some substituted benzene, 1- and 2-naphthalene, and 9-anthracene molecules are shown in Table 1. From an examination of the ),,,x of each compound it can be seen that as the number of peri-hydrogens increases, A(Amaxzp — Amaxa) increases. This can be attributed to the larger steric effect of the hydroxyl group as compared to the hydrogen atom attached to the carboxyl group. The data in Table 1 give more evidence that it is the peri-hydrogen that causes the change in planarity. The A,,,x of 2-naphthoic acid is 332nm while the Ayax for 1,2,3,4-tetrahydro-l-carbazolyl 2-naphthoate is 331nm. As the —OH or —OR group of the acid function is moved away from the H-8 atom, steric hindrance is decreased. These molecules are able to assume the same conformation. Table 1 lists the data for the 2,4-dinitrophenyl hydrazones of these aldehydes. If one compares A(Amaxp - Amaxa) With values for A(Amaxc — Amaxp), the former increase in value while the latter decrease fram benzene through napthalene to anthracene. This indicates that the group attached to N-1 (see Figure 1) is far enough away from H-8 that little steric hindrance takes place here. The conformation of some other 9-substituted anthracenes has been studied.? It was found that the angle theta (@) between the plane of the substituent and that of the aromatic ues Ne (1) 18 H(8) H ee H H ane H CD OUD OLY 27 Transactions of Kentucky Academy of Science, Vol. 34, 1973 *ZEEZT “ON B BDUSTeTeI veg (f) "ZIEZ ‘ON B edUeTeZeA Bas (T) “GO8ST ‘ON B edUeTezeA Beg (Y) ‘€OZT ‘ON B BdUeZezeI vag (3) “III eTqQeL Peg (3) ‘II eTqeL PeS (9) *6€7Z “ON & DOUEZeZeI Beg (P) “/T@ST ‘ON B eDUeZezZeI Bag (2) *898 ‘ON @ odUeTazeI veg (q) *7GZ “ON wnajoeds ‘eptueaTAsuusg ‘efydpepettud *30043g uepiep dutads gTE¢ ‘seTr1oZeAOgGe] YOLvesey TeTIpes ‘erq0edg JeTOTAeIATA pxrepueig AeTIApes (F) --- cOSE < --- --- Tee Z€€ aueTeyrydeu-z 87- Ose < G+ 86€ --- ave ausdeIYQUe-6 6£ y lst 07+ pele --- 5262 aueTeyjydeu-T ZZ < OSE < ie q842 === 26L2 guezueq (9) 2euozeapéy (a) (V) PPV (arey = OXBIY) 9 qtAueydorzpurq-y‘z (vVxeuy — FXelly) 7 apAyepTexoqie9 19480 oT TAxoqae9 SuTy xXBUuL ‘wu UIST “yy ‘spunoduiop oneutory sUuI0g 10F (WU) BUIxeyy UOndIosqy L 21991 Transactions of Kentucky Academy of Science, Vol. 34, 1973 28 (¢) 2euozerpsy [9S°0] [7S°0] [9€°0] [6T°0] [6°€] [9°¢€] -T4£4nq-u-T p-N‘ N-epAy 86E (78E) (S9€) CvE aS ase GZ 877 ~opTexoqivoous0Pi1yjue-¢ (7) euozerpfsy [€8°0l Ef (0))| [29°0] [TS°0] [07°0] [o's] [e°s] {T4doid-os}t-Tp-N*‘ N-epéy 804 T6€ €8E 69€ Z9E --- €SZ LyZ —opTexoqieoouslPIYyIUe-6 (€) euozerpséy [8Z°o] [09°0] [s€°0] [67°0] [¥T°0] [7°9] [6°S] qTAdoid-u-T p-Nn ‘ N-epsy L6E (€L€) (8S€) (ZS€) (TVE) ~—— GZ Lz -—oplTexoqieoeue leary Ue-6 (7) 2euozerpfsy [Ss7°0] [os *0] [97°0] [ze°o] [7z°0] [gt°o] [y's] [6°S] -TAy J euTp-N‘ N-epsy €07 €8e TLE (9S€) (77) (€€€) 797 7GZ —opTexoqieooueleIYIWUe-~6 [S9°0] [z9°0] [T7°0] (/2107(0)1 TAT {G)Pe)| 86E =<—- ZLE LSE --= 8ZE 19Z (867) se2 — ll@eyal (1) epAyepTexoqieo oa --- --- --- — --- ‘797 €EZ quele1yjUe-§ Pe) q Z pueg T pueg [ I x xeul 0 pay punoduo) ‘jouryeWy Ul spunoduioD payepy pue opAyepyexoqivoousoviyjuy-G JO sonjeA a pue (WU) eUIxey, ~“oNdIosqy c FGOL 29 Transactions of Kentucky Academy of Science, Vol. 34, 1973 ‘uoT3e1 STY UF peATesqo Jou sem 1epTNoys to yeod e ey seqeotpuy vsoeds yueTq y (2) “Toueyjom UT “*/9T9 “ON wWNnajZDedg ‘efueATASuUeg ‘etydzopettrud *Jo019S§ ueprey BSutads otT¢E¢ “saTiojzeiogey yoieasey eT pes ‘e1rqzo0eds JFSTOFA P1ITN prepuejs AeTapes (q) "CE = JUBJSUOD DFAIOeTETE *wnuyXeW pueq e ueYy. 1z9yIeA t9pTnoys eB seOTpuy seseyjueied uz paesoToue syQSueTeaeM ‘peqeqs eSTM19Y4IO SSeTUN TOURYIeM ST JUeATOS (ke) Se ee ee ee ee ee (g) euTuT [yy*o] [sv°o] [9¢'o] [ev] -auept [Ay emp Ary ue-¢ 86 T6€ (ZL€) a See “== 67 Ered ~(TAzer4dT Ay 3 ou, N)-N (LZ) 2uozezpsy [06‘0] [98'o] {[98'o] [s°¢€] -TATTEEP-N ‘N-opsy 00% L8€ TLE o> S25 “— Z9Z --- —opTPxXoqieoeusleiryjUe-¢ (9) 9u0zerpkyTAQnqg [ss°o] [0S°0] [o€:'o] {[z°y] [s'4] -OST-TP-N‘ N-epsy 007 (78€) (79€) --- --- --- €SZ Lvz —opTexoqievous0PryqUe-~6 i a ee ee Ge BEBE T pueg xXeu we 3 [,.0T ] xeul Xe punoduog a 30 Transactions of Kentucky Academy of Science, Vol. 34, 1973 portion of the molecule for 9-nitroanthracene, 9-acetylanthracene, and 9- formylanthracene was 65° > © > 15°, © = 49°, and @ = 27° respectively. After correlation of this with dipole moment and ir stretching frequency measurements, they concluded that the probability of a planar conformation decreases as the size of the substituent increases. Steric reasons have been invoked to explain the polarization spectra of 9-substituted anthracenes.* Here are reported the spectra of some N,N-disubstituted hydrazones of 9-anthracenecarboxaldehyde to determine if planarity is sacrificed by the added N-substituent. EXPERIMENTAL The preparation and purity of these compounds have been described previously. A solvent blank of the exact composition as that containing the compound was used for each measurement. Measurements of absorbance were made on a Cary 15 recording spectrophotometer with 10 mm Beckman silica clls. RESULTS AND DISCUSSION The ultraviolet spectral data of 9-anthracenecarboxaldehyde (1) 9- anthracenecarboxyaldehyde-N,N-dimethylhydrazone (2), 9-anthracenecar- boxaldehyde-N,N-di-n-propylhydrazone (3), 9-anthracenecarboxaldehyde-N, N-di-iso-propylhydrazone (4), 9-anthracenecarboxaldehyde-N,N-di-n-butyl- hydrazone (5), 9-anthracenecarboxaldehyde-N,N-di-iso-butylhydrazone (6), 9-anthracenecarboxaldehyde-N,N-diallylhydrazone (7), and N-(N’-methyl- pyrazyl)-9-anthrylmethylideneimine (8) in methanol have been determined. The Amax and enax Of all the observable peaks in a given band are given in Table 2. The ena, of each given peak must be examined to find the Amax of a band. All of the compounds in Table 2 have their long wavelength absorption maximum around 400 nm in methanol (i.e., 1-398 nm; 2—383 nm; 3—397 nm; 4—408 nm; 5—398 nm; 6—400nm; 7—400; 8—391 nm). The ultraviolet spectral data of anthracene (9), 9-anthracenecarboxylic acid (10), 9-nitroanthracene (11), 9-bromoanthracene (12), and 9-methylanthracene (13) are shown in Table 3. All of these compounds have their long wave- length absorption maximum around 355 nm in methanol (i.e., 9-355 nm; 10—364 nm; 11—347 nm; 12—368 nm; 13—347 nm). Compounds 9, 12, and 13 all have similar A,,,x for the long wavelength absorption (i.e., 355 nm, 347 nm, and 368 nm, respectively) (Table 3). The amount of conjugation has not increased, and the substituents have not perturbed the molecular orbitals. In the case of 10 and 11 the situation is different. Conjugation of the substituent with the ring is possible. However, since the absorption maximum is in the same region as for 9, 12 and 13, we must conclude that conjugation is not important. This verifies earlier observations +678, 9-Anthracenecarboxaldehyde (1), whose angle @ is only 27°, has a low energy band similar to the hydrazones (i.e., 398 nm). It must be concluded that these hydrazones have an angle ® similar in size to the 9-anthracenecarboxaldehyde. The two absorption areas in these anthracene derivatives can be related to steric interaction of the peri-hydrogen (see Figure 1). In all three cases, C-11 is bonded to an anthryl group and is doubly bonded to either oxygen or nitrogen; however, on the other single bond there is either a hydrogen or hydroxyl group. The interaction of the peri-hydrogen (H-1) with the hydrogen or hydroxyl group is of major importance in determining @. The 31 Transactions of Kentucky Academy of Science, Vol. 34, 1973 °G9v8 “ON °Z 2T9UPL 7G] VvoUeLVjJe1 99S (P) “069 ‘ON ‘*Z eTGEL $4 eoUeTezeA vag (3) ‘H6E “ON °Z BTGPL 6G eoUeTezeI veg (2) “6Z6ST ‘ON ‘2 eTGeL ‘4 eoUeTeyer veg (5) *Z eTqeL ‘9 sduUetezoa veg (q) "0S89 ‘ON ‘*Z eTqGeL *q eoUerezea eag (9) *Z eTGeL *B sdUeTeyet veg (fF) [ss*o] [sz‘o] [v¥t*°o] [980°0] [sz] [st] Ee sm su Lye TEE QTE 40€ SS¢ (692) «= (ET) ecco se vt Od Hohe rth ai oher | a 88 89€ OSE Zee Ooze See €SZ (847) Kai) Ue se tra aewen dae teG-O)-2 192,01. U2r- ol [st] Cet] cs = ae Lye Zee (9TE) aos TSZ (292) (IT) ,SuecezyzUPOIITU-6§ ieee Ole Eo6-O)>% Tte"o] =-fze"ol -- .P21*0] [9T] 98€ H9E 9%€ 8ZE CTE a "SZ aS ss fos‘o] [9z*ol {[tt‘o] [940°0] [orl =f -6] (OT) pFoe IF TAxXoqie9 = =o 77 67 YT 00€ esc, (942) SoS e eee PesOle (ALO eco fee of = lctsol = [97050] [oz] ES OLE SSE BEE 2z€ 60€ 967 OS 5.q7* (6) euecezyjUe Z pueg T pueg Ptqnat aw >= xPuL Ns punodwmo9 joury eI UL spunodwioy po}epay pue ousovIyUW jo sonjeA 2 pue (UU) eUXeyy yUOndIOsqy € 1901 32 Transactions of Kentucky Academy of Science, Vol. 34, 1973 size of the secondary amine attached to N-1 is not of great significance, since it is far enough away from H-8, that only minor steric effects are present. ACKNOWLEDGEMENT This study was carried out under Contract No. 12-12-100-10311(73) with the Agricultural Research Service, U. S. Department of Agriculture, administered by the Eastern Marketing Research and Nutrition Division, 600 East Mermaid Lane, Philadelphia, Pennsylvania 19118. Nomenclature €amx = A/lc where emax represents the maximum molar absorptivity; max Tepresents the wavelength (nm) of maximum absorption. LITERATURE CITED 1. Presented in part at the National Meeting of the American Chemical Society, Washington, D. C., September 1971. 2. Present address: Department of Pediatrics, Albert B. Chandler Medical Center, University of Kentucky, Lexington, Kentucky. Le Fevre, R. J. W., Radom, L., Ritchie, G. L. D., J. Chem. Soc., B, 775 (1968). Kozlov, I. N., Sarzhevskii, A. M., and Khomick, M. I., Zh. Prikl. Spektrosk., 9, 666 (1968); Chem. Abstr., 73, 52591 h (1969). Yang, K. W. and Brown, E. V., Anal. Lett., 5, 293 (1972). Norman R. O. C. and Ralph P. D., J. Chem. Soc., 2221 (1961). Trotter, J., Acta Cryst., 12, 237 (1959). -Suzuki, H., “Electronic Absorption Spectra and the Geometry of Organic Molecules,” Academic Press, New York, N. Y., 1967, p. 446-449. Received: February 2, 1973. Accepted May 25, 1973. So rect ee) Transactions of Kentucky Academy of Science, Vol. 34, 1973 33 SOME PHYSICAL, CHEMICAL, AND BENTHIC CHARACTERISTICS OF WAR FORK, AN INTERRUPTED STREAM IN JACKSON COUNTY, KENTUCKY NORMAN H. CRISP AND CATHERINE B. CRISP Department of Biological Sciences, Eastern Kentucky University, Richmond, Kentucky 40475 This paper presents the results of an investigation of the physical, chemical; and benthic characteristics of War Fork Creek in Jackson County, Kentucky. War Fork is atypical in that sections of it are interrupted on nonlimestone terraces. The presence and position of these interruptions are dependent on rainfall and watershed discharge. Only a few publications treat interrupted streams, particularly with reference to limnological effects of such interruptions. This investigation was conducted to determine if interruptions in flow had any effect on the streams physical and chemical parameters, and if rapid desiccation and reinundation of interrupted stream beds had an adverse effect on the density and diversity of benthic organisms. __ A preliminary survey for general morphometry and for location of col- lection sites was started in May 1971 and continued until June 1971. Selected physical-chemical parameters were measured and benthic samples collected on 4 July, 17 July, and 1 August 1971. The section of the stream selected for study lies between 37°27'10” and 37°28’30” N latitude and 83°55/37” and 83° 54’ 47” W longitude in northeastern Jackson County, and is a fourth order stream according to Kuehne’s (1962) classification. Description of War Fork In his work on the McKee Quadrangle, Gordon Weir (pers. comm.) found several formations of two geological periods within the area covered by our study. In the uppermost section of the study area, War Fork flows over the Breathitt Formation (Upper Pennsylvanian), a heterogenous unit composed mostly of gray shale with lenses of light-brown sandstone (Figs. 1 and 2). The middle and upper-lower sections are floored with ledge forming, dark green sandstone and green shale. This sandstone capped shale is the Pennington Formation of Mississippian age. The extreme lower section of the area is floored by light to medium gray Newman limestone also of Mississippian age, a highly cavernous, weathering limestone with many sinks. War Fork itself, near Station 1 (Fig. 1), is about 5 feet wide with alternating riffles and pools, and this pattern persists throughout the length of the stream, although the width increases to about 15 feet in the lower sections. In general, stream width is very nearly equal to channel and/or floodplain width. Floodplains are poorly developed or absent. The stream is well shaded by the canopy of mixed hardwoods in the lower section and hardwoods and hemlocks in the upper sections. The elevation of War Fork at Station 1 is about 890 feet msl., falling to about 830 feet at Station 7; an average gradient of 30 feet per mile. A longitudinal profile (Fig. 2) discloses two areas of high gradient separated 34 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Figure 1. Map of Study Area and Stations ( BS } U == INTERRUPTFD FLOW U é / Site —— PERMANENT FLOW \ ‘ is ,@3 ¢ ‘ ? 1/2MILE by an area of relatively low gradient. Streams flowing on limestone sur- faces often have rapidly changing gradients in different sections (Neel, 1951. However, the locations of rapid gradient changes on War Fork are not associated with limestone, but occur close to the points where two out- crops meet. Differences in erosional rates of the two outcrops probably account for this fact. During periods of low flow, War Fork sinks into the Pennington Formation at two different points. The sites of these sinks were under the roots of large trees. Dr. Harry P. Hoge of the Eastern Kentucky University Geology Department (pers. comm.) suggested that since the Pennington Formation thinly overlays the Newman limestone at these points, the root systems of the trees probably have extended into the Newman Formation and caused fractures and fissures in the Pennington. This would allow the stream water to enter the limestone and form solution channels. Transactions of Kentucky Academy of Science, Vol. 34, 1973 35 Figure 2. Longitudinal Profile of the Study Area Breathitt Feet Pennington Miles Six stations were established at the beginning of the study and a seventh one added when dye-flows indicated the discharge of subterranean water. Station 1 was located at the junction of Steer Fork and War Fork. The stream is a series of riffles and pools with the bottom composed of rubble in the riffles and coarse sand, gravel, and some rubble in the pools. Station 2 was established at the site of an interruption about 1 mile below Station 1. This is not an interruption in the sense of that found in karst topography, but an infiltration of the stream into a series of alluyial deposits at the base of large trees. The site of the interruption is not fixed, but varies in location depending on discharge. Station 3 was at the junction of Hughes Fork with War Fork. The stream bed consists of shales with scattered rubble and gravel. During periods of low flow, the stream disappears into an alluvium deposit at the base of a large tree. Station 4 was added after the results of adding dye at Stations 2 and 3 indicated that some or all of this water was reentering the surface drainage at that point. Station 4 was a large pool with a bottom composed of large rubble and some silt. Station 5 was established at the source of a spring directly across from a recreation area. The spring runs about 30 feet before entering War Fork and is entirely riffles with the bottom composed of rubble and fine sand. Station 6 was about 100 feet below the point where the spring-fed stream from Station 5 entered War Fork. It is a shallow riffle area at the end of a large pool. The bottom is composed of small rubble with a few large rocks generally dispersed. Station 7 was not a fixed location but rather the point at which War Fork sank. Whether it was a pool or a riffle habitat depended upon water level at the time of sampling. The bottom material varied somewhat but at all times large amounts of small rubble grading into coarse sands were present. 36 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Methods and Materials Discharge and velocity measurements were not taken, but relative in- tensities were noted at Station 7. The lowest intensity observed was on July 17, medium intensity on July 4, and the greatest intensity on August 1. Temperature measurements were taken with a standard laboratory mercury thermometer. Turbidity measurements were determined by the use of a Hellige turbidimeter. Measurements of pH were taken on wide- range pH paper. Half values were interpolated using degree of color de- velopment as a basis for decision. Determinations of dissolved oxygen, calcium hardness, total hardness, alkalinity, and free carbon dioxide were made following the procedures outlined by Hach Chemical Company, Ames, Iowa. Oxygen saturation values were computed from a nomogram given by Reid (1961). Benthic samples were made by allowing 10 minutes of hand collecting on rocks and bottom debris at each station after the method of Macan (1958). Identification was made by standard keys, such as Edmonson (1959), Pennak (1953), and Ross (1953). Results and Discussion Character of Ground Water Flow. On July 4 an attempt was made to determine whether water, which disappeared at stations 2 and 3, reentered the stream in the middle portion of the study area through an underground spring. Flourescent yellow dye (0.5 Ib in 1 gallon of water) was placed in the stream just above the interruption at Stations 2 and 3. About 45 minutes after it was placed in the stream, the dye was observed spreading over the bottom at the location which was then established as Station 4. Temperature. The major factor in warming stream water is direct solar radiation. However, temperature is affected by altitude, aspect, cover, and type of source (Reid, 1961).. War Fork has a well-developed stream side canopy that for the most part excludes a great deal of incoming radiation. Minckley (1963) found that flow-through time in Doe Run had an effect on water temperature. Time of flow is decreased with increased discharge. With the exception of Station 5, all stations had the lowest temperature on August 1 when the discharge of the stream was greatest (Table 1). Thermal stratification is not usually a characteristic of a lotic environ- ment, but does sometimes occur. Neel (1951), in his investigation of a limestone stream, found that the location of underwater springs could be detected by marked differences in temperature readings. He concluded that since the ground water seasonally is colder than surface water, these areas of low temperature would be the result of incoming spring water. Thermal stratification was observed at one point on War Fork. Dye placed at the interruptions of Stations 2 and 3 was observed spreading across the bottom of a pool at the entrance to Turkey Foot recreation area. Temperature readings on July 17 were 20° C at the surface and 18° C at the bottom (20 inches). It should be noted that the subsurface water at Station 4 was considerably cooler than the surface water at Stations 2 and 3 where it originated (Table 1). It is possible that during its underground passage, the water received cold groundwater seepage, or lost heat to the cooler rocks, or a combination of both. On August 1, when there were no interruptions of War Fork, stratification was not observed. The water was Transactions of Kentucky Academy of Science, Vol. 34, 1973 ot Table 1 Physical-Chemical Parameters of War Fork. Temperature in °C. Free COg, Dissolved Oxygen, Calcium Hardness, Total Hardness, Total Alkalinity, and Turbidity Measured in ppm. Collecting Dates Station 1 7/4 AY 8/1 Temperature 21.0 20) IKS)= 0) pH Tai) 6.5 7.0 co, 3350 4.0. 2.0 De 70. 8.2 8.4 8.9 Per Cent Saturation 90.0 96.0 95.0 Calcium Hardness 20.0 ZZaAo 12.0 Total Hardness 28.0 38.0 20.0 Alkalinity (Total) DIO} 1250 4.0 Turbidity 8.5 720 20.0 Station 2 Temperature 2250 23.0 19.0 pH 6.5 TO 6.5 co, 265 2.0 Pas Da Os 9.4 8.8 oil Per Cent Saturation 105.0 100.0 7a@ Calcium Hardness 24.0 22.0 20.0 Total Hardness 30.0 30510 2250 Alkalinity (Total) IL{}56) 18.0 20.0 Turbidity 15.5 9.5 280 extremely turbulent and probably resulted in complete mixing of the sub- surface and surface water. Longitudinal gradation of temperature that characterize many streams was not observed in War Fork. The lower portions of the study area were, as a rule, cooler than the upper area. Since canopy over the stream was roughly equal over the entire area, some factor other than thermal radiation 38 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Table 1 (continued) Collecting Dates Station 3 7/4 7/17 Temperature 23.0 23.0 pH 6.5 6.5 co, 6.0 4.0 D.O. 6.0 6.2 Per Cent Saturation 70.0 70.0 Calcium Hardness 28.0 44.0 Total Hardness 44.0 50.0 Alkalinity (Total) 36.0 38.0 Turbidity 2.0 8.5 Station 4 Temperature 20.0 PH 6.5 co, 6.0 D.O. 9.8 Per Cent Saturation 105.0 Calcium Hardness 56.0 Total Hardness 60.0 Alkalinity (Total) Bae (0) Turbidity 9.3 8/1 19.0 6.5 1.0 9.5 100.0 16.0 24.0 20.0 14.5 18.0 7.0 7.0 8.7 92.0 40.0 40.0 28.0 7.5 must be considered. The most probable explanation is that subsurface water was entering the stream but not detected. Turbidity. Turbidity was measured at each station during each sampling period (Table 1) and was usually greatest during periods of high discharge. Two exceptions were Station 4 on July 17 and Station 5 on all occasions. A high value at Station 4 was probably the result of physical disturbance of the sediments prior to collecting. Station 5 showed no correlation between discharge and turbidity and fluctuated up and down for no apparent reason. Dissolved Oxygen. In streams, especially small mountain streams, photosyn- thesis plays a minor part in supplying dissolved oxygen. The most im- Transactions of Kentucky Academy of Science, Vol. 34, 1973 39 Table 1 (continued) Collecting Dates Station 5 7/4 WAY 8/1 Temperature 17.0 17.5 W7/5D) pH 7.0 6.5 720 co, 8.5 1350 5.0 D.O. 159 7.4 ORS Per Cent Saturation 82.0 75.0 110.0 Calcium Hardness 32.0 42.0 34.0 Total Hardness 43.0 44.0 36.0 Alkalinity (Total) 30.0 40.0 22.0 Turbidity 16.0 955 7.5 Station 6 Temperature LOR 20.0 18.0 pH 7.0 7.0 6.5 co, U5> Uc 4.0 D.O. 7.8 WO 256 Per Cent Saturation 80.0 86.0 100.0 Calcium Hardness 24.0 32.0 30.0 Total Hardness 40.0 38.0 30.0 Alkalinity (Total) 37.0 36.0 24.0 Turbidity 5.0 6.0 a2 portant factor is probably physical aeration. Due to the nature of War Fork morphology, circulation was probably very effective in supplying oxygen. Dissolved oxygen was relatively high at all stations. The lowest value was recorded from Station 3 when it was a nearly stagnant pool and the highest value was recorded from Station 5 during a period of high runoff. Station 5 had high concentrations of oxygen at all times. At any time of the year oxygen present in ground water differs insignificantly from that of the stream (Neel, 1951). A small t-test at the .05 level of significance revealed that the difference between the mean oxygen: concentration at Station 5 and the rest of the stream was not significant. 40 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Table 1 (continued) Station 7 Temperature ZORS 21.0 19.0 pH SoS) 7.0 6.5 co, ilo (@) 3510 2.0 D.O. 9.7 8.0 Saat Per Cent Saturation 105.0 90.0 97.0 Calcium Hardness 38.0 46.0 26.0 Total Hardness 40.0 50.0 32.0 Alkalinity (Total) 35.0 40.0 . 30.0 Turbidity 16.0 a0 BiG) Oxygen Saturation. Oxygen saturation values varied greatly between stations and at the same station on different sampling dates (Table 1). The amount of physical aeration apparently did not affect the saturation values. The main factor was the water temperature at the collecting site. Free Carbon Dioxide, Hydrogen Ion Concentration, and Alkalinity. There was little variation in the free carbon dioxide in the areas not grossly affected by subsurface water. Some subterranean waters are rich in carbon dioxide collected during passage through the soil. Station 5, which repre- sented only subterranean flow, typically had the highest free carbon dioxide concentration. Station 4 showed increase in concentration over Station 2 and Station 3, from which it obtained some of its water. Water at Station 6, which was primarily the result of influx of ground water above the station, also had a high free carbon dioxide content (Table 1). Hydrogen ion concentration changed little during the study, or from station to station. All readings were either 6.5 or 7.0 (Table 1). There was no apparent inverse relation between pH and free carbon dioxide as stated by Reid (1961). Alkalinity was low, as expected from a stream not flowing over limestone (Table 1). No phenolphthalein alkalinity was observed at any time. Total alkalinity (bromocresol green-methyl red) was present as bicarbonate alkalinity. Highest measurements were recorded from samples taken July 17, the collection period of lowest flow. These results are congruent with findings of Foster (1942), i.e., that the greatest concentrations of dissolved material are present during periods of low flow when most of the water represents runoff from ground water. Calcium and Total Hardness. Calcium hardness and total hardness were similar at all stations. Highest readings were recorded from Stations 4 and 5 and were highest during periods of low flow. Due to the close similarity of calcium and total hardness, the significance of the differences in the two means was tested using a small-scale t-test showing significance at the .01 Transactions of Kentucky Academy of Science, Vol. 34, 1973 41 Table 2 Distribution of Benthic Organisms from War Fork, Jackson County, Kentucky, Collected on July 4, July 17 and August 1, 1971. Taxa Station Total Plecoptera Acroneuria 3 1 - 10 al 2 ALg/ Tsoperla 3 = - - - - 3 Trichoptera Hydropsyche 3 - - - 3 Glossosoma 9 - - aL 6 2 18 9 Neophyiax 4 - - 2 Drusinus - - 3 aL i 1 6 Ephemeroptera Stenonema 6 al ib 7 3 3 21 Ephemerelia - - - - 1 = 1 Iron - - 2 - - 4 6 Odonata Aeschna 1 - - - - - al Coleoptera Psephenus 7 3 1 6 5 al 23 Diptera Chironomidae 1 - - 6 - - 7 TOTAL 38 9 7 38 33 22 level. The difference in the two values probably was due to small amounts of dolomite along with limestone (Hem, 1959). Benthos. The benthic organisms collected from War Fork were all Insecta, representing 6 orders and 13 genera (Table 2). With the exception of the Odonata and Diptera, all orders were represented at every station. Many of the benthic organisms commonly collected in the region surrounding the study area were not encountered at the collection sites. War Fork could be classified as an oligotrophic stream by using the calcium content of the water as an index of productivity (Reid, 1961). In an oligo- trophic stream, one typically finds many species with extremely low popula- tion densities. Unless extensive sampling is conducted in oligotrophic 42 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Table 3 Total Abundance and Distribution of Benthic Organisms from War Fork, Jackson County, Kentucky, Based on Habitat Preference (C=Characteristic; E=Exclusive). Taxa Riffle Pool Plecoptera Acroneuria T5a(G) 2 Isoperla 3 (BE) 0 Trichoptera Hydropsyche 10 2 Glossosoma 16 (C) 2 Neophylax 15 (E) fe) Drusinus 2 4 Ephemeroptera Stenonema ily (2) 4 Ephemerella 1 (E) () Iron 4 2 Odonata Aeschna 1 (E) (0) Coleoptera Psephenus A (@)) 2 Diptera Chironomidae 7 ) streams many species may be overlooked (Patrick, 1970). Since only a total of 30 minutes of sampling was used at each collecting station, some of the benthic organisms of low density which probably inhabit War Fork were not collected. Stehr and Branson (1938) felt that stream communities fall into two major groups, those of riffles and pools. These divisions can be further divided into rocky riffles, sandy riffles, rock-bottom pools, and sand-bottom pools. War Fork has few pools or rifles that could be classified as solely sandy or rocky. Only the broad category of riffles or pools was used for comparisons (Table 3). Organisms from Stations 1, 5, and 6 were always from a riffle community and organisms from Station 3 were always from a pool community. Organisms from Stations 2 and 7 were placed in either a riffle or pool community, depending on the character of stream flow when they were collected. It was impossible to recognize two distinct communities, because the pools had no exclusive or characteristic genera. Transactions of Kentucky Academy of Science, Vol. 34, 1973 43 The low number of organisms collected from the pools was probably due to the fact that the sections of the stream where the pools occurred was subject to periodic loss of water due to stream interruptions. However, Larimore, Childers, and Heckrotte (1959) indicated that many organisms are able to withstand periods of drought by burrowing into the moist sub- strate, aestivating, or retreating with the receding water. Repopulation of the previously dried sections of the stream bed should have been accomplished by normal stream drift. Variable water level is a factor that brings about an increase in drift (Minshall and Winger, 1968). Since water level was extremely variable on War Fork, sufficient drift should have been present to repopulate sections as they were reinundated. It was impossible, due to the nature of the study, to know how long a previously dry area had been reinundated when samples were taken. If reinundation had occurred just prior to sampling, the effect of stream drift would have been decreased. LITERATURE CITED Edmonson, W. T. (ed.) 1959. Ward and Whipple’s Fresh-Water Biology. John Wiley and Sons, Inc., New York. 1,248 pp. Foster, M. D. 1942. The chemistry of ground water. In, Hydrology, Physics of the Earth. McGraw-Hill Book Co., New York. 646-655 pp. Freund, J. E. 1970. Statistics, a First Course. Prentice-Hall, Inc., Englewood Cliffs, New Jersey. 340 pp. Hach Chemical Co. Water and Sewage Analysis Methods Manual. Ames, Iowa. 52 pp. Hem, J. C. 1959. Study and interpretations of the chemical characteristics of natural water. U.S. Geol. Surv., Water Supply Pap. 1473: 1-269. Kuehne, R. A. 1962. A classification of streams, illustrated by fish distribution in an eastern Kentucky creek. Ecology 48: 139-149. Larimore, R. W., W. F. Childers, and C. Heckrotte. 1959. Destruction and re- establishment of stream fish and invertebrates affected by drought. Trans. Amer. Fish. Soc. 88: 261-285. Macan, T. T. 1958. Methods of sampling the bottom fauna in stony streams. Mitt. int. Ver. Limnol. 8: 1-21. Minckley, W. L. 1963. The ecology of a spring stream Doe Run, Meade County, Kentucky. Wildl. Monogr. No. 11: 1-124. Minshall, G. W., and P. V. Winger. 1968. The effect of reduction in stream flow on the invertebrate drift. Ecology 49: 580-582. Neel, J. K. 1951. Interrelations of certain physical and chemical features in a headwater limestone stream. Ecology 32: 368-392. Patrick, R. 1970. Benthic stream communities. Amer. Sci. 58: 546-549. Pennak, R. W. 1953. Fresh-Water Invertebrates of the United States. Ronald Press, New York. 769 pp. Reid, G. K. 1961. Ecology of Inland Waters and Estuaries. Van Nostrand Rein- hold Co., New York. 375 pp. Ross, H. H. 1953. The caddisflies, or Trichoptera, of Illinois. Bull. Ill. Nat. Hist. Surv. 23: 1-326. Stehr, W. C. and J. W. Branson. 1938. An ecological study of an intermittent stream. Ecology 19: 294-310. Received: March 23, 1973. Accepted June 5, 1973. 44 Transactions of Kentucky Academy of Science, Vol. 34, 1973 APOPHALLUS VENUSTUS (TREMATODA, DIGENEA): A NEW METACERCARIA RECORD FROM NEW HAMPSHIRE NORMAN CRISP AND JOHN P. HARLEY Department of Biological Sciences, Eastern Kentucky, University, Richmond, Kentucky 40475 ABSTRACT Yellow perch (Perca flavescens) from Kidder Brook, New London, New Hamp- shire, were infected with the metacercaria of the heterophyid trematode Apophallus venustus. This is the first report of this metacercaria from New Hampshire; thus, extending its geographic range in North America. Apophallus venustus (Ransom, 1920) metacercariae have been reported only from the lower Ottaway Valley of Quebec (Cameron 1945). Adults have been reported from Georgia (Babero and Shepperson 1958), Wash- ington, D.C. (Cameron 1945), and Quebec (Cameron 1945). The first intermediate host of this heterophyid trematode is the snail Goniobasis liviscens; the second intermediate hosts are 13 species of fishes in nine families; and the definitive host, mammals and migratory piscivorous birds. All of the above are widely distributed in eastern North America (Cameron 1937a, 1937b). As a result, A. venustus should have an equally wide geo- graphic range. Recently, the authors had the opportunity to examine yellow perch (Perca flavescens) from New Hampshire for this parasite. Fish were collected by seining Kidder Brook, New London, New Hampshire, and preserved in 10% formalin. Later, the dorsal musculature was removed and digested according to the method of Weller (1943). After digestion was completed, the remaining muscle fiber was examined under a dissecting microscope for metacercarial cysts. After recovery, the cysts were opened and the meta- cercaria identified according to the criteria of Ransom (1920) and Cameron (1936). Thirteen yellow perch, ranging from 97 to 119 mm, were examined and all were found to be infested with A. venustus metacercaria. However, the number of cysts per fish was low, ranging from 1 to 4 (X = 3.7). Only one metacercaria was found per cyst, unlike other species which may have up to nine per cyst (Sinclair 1972). There was no apparent relationship between standard length and the number of cysts per fish. This report thus extends the geographical distribution of the metacercaria of A. venustus in North America and is the first report of the metacercaria being found in the United States. Like A. brevis as reported by Sinclair (1972), A. venustus probably has a fairly widespread but extremely diffuse distribution throughout the United States and Canada and is limited to the continent of North America. The authors acknowledge the assistance of Dr. Norm Sinclair, George Mason University, Fairfax, Virginia, for species conformation. LITERATURE CITED Babero, B. B., and J. R. Shepperson. 1958. Some helminths of raccoons in Georgia. J. Parasit. 44(5): 519. Transactions of Kentucky Academy of Science, Vol. 34, 1973 45 Cameron, T. W. M. 1936. Studies on the Heterophyid trematode, Apophallus venustus (Ransom, 1920) in Canada. Part I. Morphology and taxonomy. Can. J. Res., D, 14: 59-69. 1937a. Studies on the heterophyid trematode, Apophallus venustus (Ransom, 1920) in Canada. Part II. Life history and bionomics. Can. J. Res. D, 15: 38-51. 1937b. Studies on the heterophyid trematore, Apophallus venustus (Random, 1920) in Canada. Part III. Further hosts. Can. J. Res. D, 15: 275. __;, «1945. Fish carried parasites in Canada. Can. J. Comp. Med. 9: 245-311. Ransom, B. H. 1920. Synopsis of the trematode family Heterophyidae with description of a new genus and five new species. Proc. U.S. Natl. Mus., Wash- ington, pp. 527-573. Sinclair, N. R. 1972. Studies on the heterophyid trematode Apophallus brevis, the “sand-grain grub” of yellow perch (Perca flavescens). II. The metacercaria: position, structure, and composition of the cyst; hosts; geographical distribu- tion and variation. Can. J. Zool. 50: 577-584. Weller, T. H. 1943. Development of the larvae of Trichinella spiralis in roller tube tissue culture. Am. J. Path. 19: 503-515. Received: December 6, 1972. Accepted April 18, 1973. 46 Transactions of Kentucky Academy of Science, Vol. 34, 1973 AN ADDITIONAL EVENING BAT FROM SOUTH CENTRAL KENTUCKY DAVID J. FASSLER University of Kentucky, Somerset Community College, Somerset, Kentucky 42501 In July 1818, Constantine S. Rafinesque undertook a journey to Kentucky in search of fish, snakes, rats, and bats. Sometime during that trip to “.. . the lower parts of the Ohio, the Wabash, Green River, Barrens, Prairies, . . .” he took a Nycticeius (Vespertilio) humeralis from an unidentified type locality in Kentucky (Amer. Monthly Mag., 3(6) :445-447, 1818 and Jour. Phys. Chim. Hist. Nat. et Arts, Paris, 88:417, 1819). Since that time, few additional specimens of this species have been caught in the state. Bailey (Amer. Midl. Nat., 14:441-462, 1933), Barbour (J. Mamm., 44:122-123, 1963), and Davis (Bull. Natl. Speleolog. Soc., 26:82-83, 1964) collected a few individuals of this species from western Kentucky during the fall migrations and swarming activities. Hamilton (J. Mamm., 11:306- 311, 1930 and pers. comm.) collected a single specimen at Quicksand, Breathitt County, Kentucky about 22 June 1925 which is the only specimen from the Cumberland Plateau previously collected. Humphrey and Cope (J. Mamm., 49:329, 1968) published reports of three fall migrants, previously banded at separate nursery colonies in southern Indiana, being recaptured in Kentucky. The banded specimens were recaptured during the month of August in Webster, Wayne, and Henry counties. On 19 April 1972, an adult male evening bat was shot as it flew at tree top height above a pond in a wooded area 2 miles SSE of Jugornot, Pulaski County, Kentucky. The animal flew a slow, deliberate path in a westerly direction and was easily shot. It appeared 10 minutes before sunset. The testes were small (1 x 2 mm) and undescended. This specimen represents only the second record from the Cumberland. Plateau. Further collecting in the early spring may produce a number of additional specimens, including females migrating to Indiana nursery colonies. The specimen is in the collection of the author. Positive identification was made by Dr. Roger W. Barbour. Received November 14, 1972. Accepted December 5, 1972. The TRANSACTIONS OF THE KENTUCKY ACADEMY OF SCIENCE is a medium of publication for original investigations in science. Also as the official organ of the _ Kentucky Academy of Science, news and announcements of interest to the member- _ ship are published therein. These include programs of meetings, titles of papers _ presented at meetings, and condensations of reports by the Academy’s officers and committees. § a ‘ INSTRUCTIONS FOR CONTRIBUTIONS | ; 4 Papers may be submitted at any time to the editor. 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The author is responsible for correcting the galley proof. Extensive alterations _ from the origical are expensive and must be avoided or paid for by the author. _ Galley proofs must be returned promptly. Blanks for reprint orders will be supplied a with the galley proof. Ae De Terie ae Ra Vol. 34, Nos. 3, 4 1973 Coden: TKASAT TRANSACTIONS of the KENTUCKY ACADEMY of SCIENCE Official Organ KentTucky ACADEMY OF SCIENCE CONTENTS The Occurence of F’ fae Leeches (Hirudinea: Rhynchobdellida: Piscicolidae) on Kentucky River Drainage Fishes GLENN E. WHITE and NORMAN H. CRISP Six Additions to the Known Piscine Fauna of Kentucky MORGAN E. SISK Distributional Records for the Crayfishes Cambarellus Puer, C. Shufeldtii, Procambarus Gracilis, P. Viaeviridis, Orconectes Lancifer, O. Bisectus, and O. Rusticus LAWRENCE M. PAGE and BROOKS M. BURR Helminth Parasites of the White Sucker, Catostomus Commersoni, from Lake Wilgreen in Kentucky GLENN E. WHITE and JOHN P, HARLEY Intestinal Parasites from Two Species of Catfishes (Ictaluridae) from Wilgreen Lake in Kentucky BRUCE H. BAUER and JOHN P. HARLEY Sexual Dimorphism in Kentucky Queen Snakes (Regina Septemvittata) Based on Scute Counts BRANLEY A. BRANSON and EDD C. BAKER Citellina Triradiata Hall, 1916, from the Woodchuck in Kentucky JOHN P. HARLEY, M. PETE THOMPSON, and DAVID AUBREY The Kentucky Academy of Science — Founded May 8, 1914 OFFICERS 1972-73 President: Donald Batch, Eastern Kentucky University President-Elect: Ellis V. Brown, University of Kentucky Vice-President: Frederick M. Brown, Centre College Secretary: Rudolph Prins, Western Kentucky University Treasurer: Wayne Hoffman, Western Kentucky University Representatives to A.A.A.S, Council: Branley Branson, Eastern Kentucky University John M. Carpenier, University of Kentucky BOARD OF DIRECTORS Wonald Bate wy: wee e, to 1974 Charles Payne®....5) eee to 1976 7: dll Beamon pe eee to 1974 Morris Taylor: 2:.237 3 i Soaaiahe to 1976 Thomas B. Calhoon .............. to 1975 John C. Philley’-33 oe to 1977 Charles Kupchella .......0.00.0.... to 1975 Fletcher Gabbard ..............--.- to 1977 EDITORIAL OFFICE Effective Jan. 1974 Through Dec. 1973 Louis A. Krumholz, Editor William F. Wagner, Editor Varley E. Wiedeman, Associate Editor Department of Chemistry Department of Biology University of Kentucky University of Louisville Lexington, Kentucky, 40506 Louisville, Kentucky 40208 Section Editors: Chemistry: Gordon Wilson, Western Kentucky University Geology: William Dennen, University of Kentucky Transactions indexed in Science Citation Index Membership in the Kentucky Academy of Science is open to interested persons upon nomi- nation, payments of dues, and election. Application forms for membership may be obtained from the Secretary. THE TRANSACTIONS are sent free to all members in good standing. Subscription rates for non-members are: domestic, $5.00 per volume; foreign, $6.00 per volume; back issues $6.00 per volume. THE TRANSACTIONS are issued semi-annually. Four numbers comprise a volume. Correspondence concerning memberships or subscriptions should be addressed to the Secretary. Exchanges and correspondence relating to exchangee should be addressed to the Librarian, University of Louisville, who is the exchange agent for the Academy. Manuscripts and other material for publication should be addressed to the Editor. Transactions of Kentucky Academy of Science, Vol. 34, 1973 47 THE OCCURRENCE OF FOUR LEECHES (HIRUDINEA:RHY NCHOBDELLIDA:PISCICOLIDAE) ON KENTUCKY RIVER DRAINAGE FISHES GLENN E. WHITE AND NORMAN H. CRISP Department of Biological Sciences Eastern Kentucky University Richmond, Kentucky 40475 ABSTRACT This is the first report of piscicolid leeches from Kentucky waters. Four species, Cystobranchus verrilli Meyer, Illinobdella moorei (Meyer), Piscicola punctata (Verrill), and Pisciolaria reducta Meyer are reported along with their hosts, dates, and locations of collection. INTRODUCTION During the course of research work on the Kentucky River drainage, the authors collected 4 species of fish leeches. While no piscicolid leeches have been reported from Kentucky previously, the leeches herein reported have been recovered from fishes in states surrounding Kentucky. Meyer (1940) reported Cystobranchus verrilli from several fishes in Illinois, Hoffman (1962) reported it from Lepomis macrochirus Rafinesque in West Vir- ginia, and Mathers (1948) reported it from Ictalurus punctatus (Rafinesque) in Iowa. Illinobdella moorei has been reported from many fishes in Illinois and Iowa by Meyer (1946), from Lepomis (-Chaenobryttus) (Gill) and Micropterus Lacépéde in Tennessee by Bangham and Venard (1942), and from Ictalurus melas (Rafinesque) and I. punctata in Iowa by Mathers (1948). Piscicola punctata has been reported from Micropterus punctulatus (Rafinesque) in Ohio by Bangham (1933), from Micropterus salmoides (Lacépéde) in Tennessee by Venard (1940), from several fishes in Illinois by Meyer (1940), and from Percina caprodes (Rafinesque) in Iowa by Mullin (1926). Piscicolaria reducta has been reported from Percina (-Hadro- pterus) phoxocephala (Nelson) in Illinois by Meyer (1940). METHODS The specimens were secured from fishes the authors and other workers captured by seine and gill net and were placed in 10% formalin and later transferred to 70% alcohol. Our identifications, made with the aid of keys of Hoffman (1970) and Pennak (1953), were confirmed by Dr. C. K. Mathers of Northern Illinois University. The location of collections were determined from the United States Corps of Engineers Navigation Charts, 1968. RESULTS Table I shows the hosts, date and location of collections of the leeches. Esox masquinongy Mitchill is a new host record for Cystobranchus verrilli. Notropis atherinoides Rafinesque and Percina caprodes are new host rec- ords for Piscicolaria reducta. Our records of these leeches from Kentucky waters considerably extend their known geographic ranges and constitute the first reports for piscicolid leeches in Kentucky. 48 Transactions of Kentucky Academy of Science, Vol. 34, 1973 The authors are grateful for assistance provided by Drs. D. L. Batch and B. A. Branson and to Bruce Bauer and Nelson Horseman, all from Eastern Kentucky University. TABLE 1 Leeches, their hosts. dates, and locations of collection. CYSTOBRANCHUS VERRILLI Esox masquinongy, 6 April 1973, Kentucky River, Mile 220.0. ILLINOBDELLA MOOREI Lepomis sp., 8 August 1972, Eagle Creek, Carroll County. Ictalurus natalis (Lesueur), 14 April 1973, Hell-for-Certain Creek, Leslie County. Micropterus punctulatus, 21 April 19738, Eagle Creek, Carroll County. PISCICOLA PUNCTATA catostomus commersoni (Lacépéde), 10 February 1973, Kentucky River, mile 170.5. PISCIOLARIA REDUCTA Notropis atherinoides, 7 June 1972, Kentucky River, mile 249. Percina caprodes, 7 June 1972, Kentucky River, mile 249. LITERATURE CITED Bangham, R. V. 1933. Parasites of the spotted bass, Micropterus pseudalplites Hubbs, and summary of parasites of small mouth and largemouth black bass from Ohio streams. Trans. Am. Fish. Soc., 63:220-228. , and C. E. Venard. 1942. Studies on parasites of Reelfoot Lake fish. IV. Distribution studies and checklist of parasites. J. Tenn. Acad. Sci., 17(1): 22-38. Hoffman, G. L. 1962. Unpublished research. . 1970. Parasites of North American Freshwater Fishes. Univ. Cal. Press, Los Angeles. 486pp. Mathers, C. K. 1948. The leeches of the Okoboji region. Thesis, Univ. Iowa, Iowa City. 56pp. Meyer, M. C. 1940. A revision of the leeches (Piscicolidae) living on freshwater fishes of North America. Trans. Am. Micr. Soc., 59(3):354-876. . 1946. Further notes on the leeches (Piscicolidae) living on freshwater fishes of North America. Trans. Am. Micr. Soc., 65(3) :237-249. Mullin, C. A. 1926. Study of the leeches of the Okoboji Lake region. Ph.D. thesis, Univ. Iowa. Pennak, R. W. 1953. Fresh-water Invertebrates of the United States. The Ronald Press Co., N. Y. 769pp. United States Army Corps of Engineers, 1968. Kentucky River Navigational Charts. Louisville. Venard, C. E. 1940. Studies on parasites of Reelfoot Lake fish. I. Parasites of the large-mouth black bass, Huro salmoides (Lacépéde). J. Tenn. Acad. Sci., 15(1):48-68. Received: 19 June, 1973. Accepted: 8 September, 1973. Transactions of Kentucky Academy of Science, Vol. 34, 1973 49 SIX ADDITIONS TO THE KNOWN PISCINE FAUNA OF KENTUCKY MORGAN E. SISK Hunter Hancock Biological Station Department of Biological Sciences Murray State University, Murray, Kentucky 42071 ABSTRACT Six species of fishes not previously reported from Kentucky are listed. They are Umbra limi (Kirtland), Notropis maculatus (Hay), Fundulus chrysotus Hol- brook, Menidia audens Hay, Etheostoma fusiforme (Girard), and E. proeliare (Hay). Collecting sites and brief habitat descriptions are included. Several species of Gulf Coastal Plain fishes long have been suspected to occur in western Kentucky waters. One of these, Fundulus notti (Agassiz), recently was reported from the Obion Creek drainage by Branson (1971). Additional species may be represented in past collections but have not been reported in the literature. The purpose of this paper is to confirm the presence of six additional species in the Commonwealth. On 6 October 1973, a series of 14 Fundulus chrysotus Holbrook, 15 F. notti, and 2 specimens of Etheostoma fusiforme (Girard) were taken from Open Pond, Fulton County. Subsequent collecting on 14 October 1973, yielded an additional 14 F. chrysotus, 4 F. notti, and 2 E. fusiforme. The f -hes were taken in shallow water (5-50 cm) heavily choked with Poly- gonum sp. Open Pond is a shallow, ponded slough 16 km west of Hickman and 6 km north of the Kentucky-Tennessee state line. The slough appears subject to periodic flooding and has been reported dry on occasion. Reinvasion of fishes following periods of drought probably occurs from the south through Reelfoot Lake and Running Slough (old Bayou de Chein) during flood periods. Waters of Open Pond vary in depth from 1 cm to 1 m. Vegetation in and around the pond consists of Lemna minor, Azolla caroliniana, Spiro- dela polyrhiza, Myriophyllum sp., Polygonum sp., Ludwigia sp., Cepha- lanthus occidentalis, and Salix sp. On 12 October 1973, 7 specimens of Notropis maculatus (Hay) and 3 Etheostoma fusiforme were collected from Pond Slough, Fulton County. The collecting site is 4 km northeast of Open Pond and 2 km southwest of Fish Pond. The slough is 1.7 km long and averages about 10 m in width. Maximum water depth at time of collection was 1.2 m and aquatic vegetation was lacking. Banks were precipitous and brushy. Bottom materials consisted of silt, muck, and detritus. Hamby Pond, Fulton County, was seined on 20 October 1973, and pro- duced 4 specimens of Menidia audens Hay, 18 specimens of Etheostoma proeliare (Hay), and 14 specimens of N. maculatus. Hamby Pond is a permanent body of water 8 km southwest of Hickman, supporting a stand of large bald cypress, which extend into the water in places. E. proeliare was collected from shallow waters around the submerged boles of these trees. The specimens of M. audens came from open waters of the lake near its outflow. N. maculatus (3 specimens) was also taken from Running Slough, into which Hamby Pond flows during flood seasons. An 50 Transactions of Kentucky Academy of Science, Vol. 34, 1973 additional series of 13 E. proeliare was collected from Running Slouth 3 km west of Hickman. Umbra limi (Kirtland) was taken on 20 October 1973 from an unnamed slough adjacent to Running Slough 1.6 km south of Ledford. The fishes were seined from the only water remaining in the slough, two small pools no larger than 3 x 5 m and about 30 cm deep. Lemna minor and Spirodela polyrhiza covered the surface and a water temperature of 28 C was recorded. Two hundred twenty-six specimens were collected in no more than eight seine hauls. Thirty-four of these fishes were preserved for record and the remainder w -e transported to nearby Hamby Pond and released. The report of these six species of fishes from Kentucky fills a void in the distributional pattern of the species in the middle Mississippi River basin and appears to represent the northernmost range limits of N. maculatus, F. chrysotus, and M. audens (Moore 1968). Because the habitat requirements of these fishes are limited in Kentucky, it becomes obligatory that they be placed on the list of rare and endangered species in the state. I wish to acknowledge Ted Crowell, Paul Fielder, Ralph Jackson, Roger Jones, Fred Lieb, and David Webb, students of Biology at Murray State University, for their assistance in the field. The United States Army Corps of Engineers provided funds needed to support the survey of waters in Fulton County. LITERATURE CITED Branson, Branley A. 1971. Fundulus notti in Kentucky. Trans. Ky. Acad, Sci., 32 (3-4) :76. Moore, George A. 1968. Fishes. In. Vertebrates of the United States. McGraw- Hill, Inc., N.Y. 616pp. Received: 3 November, 1973. Accepted: 12 November, 1973. Transactions of Kentucky Academy of Science, Vol. 34, 1973 51 DISTRIBUTIONAL RECORDS FOR THE CRAYFISHES CAMBARELLUS PUER, C. SHUFELDTI!I, PROCAMBARUS GRACILIS, P. VIAEVIRIDIS, ORCONECTES LANCIFER, O. BISECTUS, AND O. RUSTICUS LAWRENCE M. PAGE AND BROOKS M. BURR Illinois Natural History Survey, Urbana, Ill. 61801 ABSTRACT The first records for Cambarellus puer and Procambarus viaeviridis in Mlinois, for Procambarus gracilis in Indiana, for Cambarellus shufeldtii in Kentucky, and for Cambarellus puer and Orconectes rusticus in Missouri are reported. Range ex- tensions for Orconectes lancifer and Orconectes bisectus are also reported. Although distributional reports on crayfishes have been written for Illinois (Forbes 1876, Rietz 1912, Brown 1955), Indiana (Hay 1896, Eberly 1955), Kentucky (Rhoades 1944), and Missouri (Steele 1902, Williams 1954), the amount of crayfish collecting done in these states has not been extensive, and the species lists are incomplete. Absent from the Illinois list are Cambarellus puer and Procambarus viaeviridis, from the Indiana list is Procambarus gracilis, from the Kentucky list is Cambarellus shufeldtii, and from the Missouri list are Cambarellus puer and Orconectes rusticus. The first records for these species in these states and range extensions for Orconectes bisectus and Orconectes lancifer are reported below. Cambarellus puer Hobbs.—Previously recorded only as far north as west- ern Tennessee (Hobbs 1972), three populations of C. puer were recently found in Coastal Plain swamps of southern Illinois and Missouri. Specimens were collected at Heron Pond, 1 mile NW Forman, Johnson County, Illinois, on 30 March 1973, at Grantsburg Swamp, 0.5 mile E Grantsburg, Johnson County, Illinois, on 19 May 1973, and at Mingo National Wildlife Refuge, Stoddard County, Missouri, on 25 October 1973. Cambarellus shufeldtii (Faxon).—Although known from both southern Illinois and Tennessee, C. shufeldtii has never been recorded from Kentucky. One male C. shufeldtii was collected at Mitchell Lake, 1 mile W Oscar, Ballard County, Kentucky, on 22 September 1973. Mitchell Lake is one of a series of cypress oxbows paralleling the Ohio River in Ballard and McCracken counties, Kentucky, and C. shufeldtii probably will be found throughout this oxbow area. Procambarus gracilis (Bundy).—Both Hay (1896) and Eberly (1955) stated that, although not yet found in Indiana, the range of P. gracilis prob- ably extends into the northwestern portion of the state. In the Chicago Museum of Natural History is one small male P. gracilis with the following collecting data: Kankakee River, S. Illinoi, Lake County, Indiana, Alfred C. Weed, 9 May 1922; this specimen represents the first known Indiana record of P. gracilis. Procambarus viaeviridis (Faxon).—The distribution of P. viaeviridis was given by Hobbs (1972) as including localities in Alabama, Arkansas, Lou- isiana, Mississippi, and Tennessee. Three populations recently were dis- covered in swamp habitats on the Coastal Plain of southern Illinois. Speci- mens were collected at the same Illinois localities and dates as Cambarellus puer and at a swampy roadside ditch (Bay Creek drainage), 2 miles SE Dixon Springs, Pope County, on 19 May 1973. 52 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Orconectes lancifer (Hagen).—A series of eight O. lancifer was collected at Horseshoe Lake, 1.5 miles S Olive Branch, Alexander County, Illinois, on 20 June 1973. This is the northernmost locality for O. lancifer and only the second Illinois record; the first was one female collected in the mid-19th century at Cairo, Illinois, by Robert Kennicott (Faxon 1914). Orconectes bisectus Rhoades.—Known previously only from the Crooked Creek drainage in Crittenden County, Kentucky (Rhoades 1944, Prins and Fitzpatrick 1965, Hobbs 1972), O. bisectus was found in Camp Creek, 2 miles S Weston, Crittenden County, Kentucky, on 2 August 1973. Camp Creek is the first stream system east of Crooked Creek; O. bisectus could not be found in streams west of Crooked Creek. Orconectes rusticus (Girard).—Steele (1902) listed several Missouri localities south of the Missouri River for O. rusticus; however, all apparently were based on misidentifications of other species, and recent publications (Williams 1954, Hobbs 1972) have not listed O. rusticus among the Missouri crayfish fauna. O. rusticus is the predominant crayfish in riffle habitats in the Salt and Fabius river systems of northeastern Missouri and was collected at 11 different localities between July and September 1973. ACKNOWLEDGMENTS We are indebted to Horton H. Hobbs, Jr., United States National Museum, for verifying our identifications of Cambarellus puer, Procambarus viaeviridis, and Orconectes rusticus, and to John A. Boyd, Matthew K. Butcher, Lloyd R. Davis, Ernest L. List, Philip W. Smith, and Donald W. Webb for aid in collecting specimens. LITERATURE CITED Brown, P. L. 1955. The biology of the crayfishes of central and southeastern Illinois. Unpubl. Doctoral Dissertation, Univ. Ill. 158p. Eberly, W. R. 1955. Summary of the distribution of Indiana crayfishes, including new state and county records. Proc. Ind. Acad. Sci. 64:281-283. Faxon, W. 1914. Notes on the crayfishes in the United States National Museum of Comparative Zoology, with descriptions of new species and subspecies to which is appended a catalogue of the known species and subspecies. Mem. Mus. Comp. Zool. Harvard Coll. 40( 8) :351-427. Forbes, S. A. 1876. List of Illinois Crustacea, with descriptions of new species. Ill. Mus. Nat. Hist. Bull. 1(1):3-25. Hay, W. P. 1896. The crawfishes of the state of Indiana. 20th Ann. Rept. Dept. Geol. Nat. Res. Ind. pp. 476-506. Hobbs, H. H., Jr. 1972. Crayfishes (Astacidae) of North and Middle America. Environ. Prot. Agency Biota of Freshwater Ecosystems Ident. Manual 9:1-1738. Prins, R., and J. F. Fitzpatrick, Jr. 1965. The first-form male of Orconectes bisectus Rhoades, a poorly known Kentucky crawfish. Amer. Midl. Nat. 74(1):141-147. Rhoades, R. 1944. The crayfishes of Kentucky, with notes on variation, distribu- tion, and descriptions of new species and subspecies. Amer. Midl. Nat. 31:111-149. Rietz, N. M. 1912. Ecological relations of the crawfishes of Illinois. Unpubl. Baccalaureate Thesis, Univ. Ill. 87 p. Steele, M. 1902. The crayfish of Missouri. Univ. Cincinnati Bull. 10:1-54. Williams, A. B. 1954. Speciation and distribution of the crayfishes of the Ozark Plateaus and Ouachita Provinces. Univ. Kansas Sci. Bull. 36(12):803-918. Received: 7 November, 1973. Accepted: 15 November, 1973. Transactions of Kentucky Academy of Science, Vol. 34, 1973 53 HELMINTH PARASITES OF THE WHITE SUCKER, CATOSTOMUS COMMERSONI, FROM LAKE WILGREEN IN KENTUCKY GLENN E. WHITE AND JOHN P. HARLEY Department of Biological Sciences Eastern Kentucky University Richmond, Kentucky 40475 ABSTRACT The following helminths were recovered from 51 white suckers Catostomus commersoni from Lake Wilgreen, Madison County, Kentucky: Acanthocephala Acanthocephalus jacksoni, Trematoda Clinostomum marginatus and Neascus sp., and oo Glaridacris catostomi. A. jacksoni and G. catostomi are new state records. To date, Harley and Keefe (1970) reported 15 helminths from 4 species of sunfishes and Bauer and Harley (1974) reported 2 cestodes from 2 species of catfishes in Lake Wilgreen, Madison County, Kentucky. As part of a continuing study of the fish parasites from that lake, this report includes the parasites of the white sucker, Catostomus commersoni (Lacépéde). Fifty-one C. commersoni were collected in the spring of 1973. The fish were autopsied and the parasites fixed, stained, and identified according to the procedure of Harley and Keefe (1970). Of the 51 fish examined, 37 were infested with at least 1 parasite, a 73 percent rate of infestation. The following helminths were recovered with the percentage of fish infested and mean intensity of infestation given, respectively: Acanthocephalus jacksoni (58%, 17), Trematoda Clinostomum marginatum (7%, 3) and Neascus sp. (11%, 59), and Cestoidea Glaridacris catostomi (37%, 3). No nematodes, leeches, or crustaceans were found. The acanthocephalan, A. jacksoni (Bullock 1962) was the most abundant helminth parasitizing the white sucker in Lake Wilgreen. The larvae of this worm are reported to occur in the isopod Asellus and the amphipod Gam- marus (Hoffman 1967). This was consistent with the authors’ findings in that isopods were observed to constitute a large part of the white sucker’s diet in the study area. The recovered trematodes belonged to the subclass Digenea. The white sucker was the intermediate host for 2 immature forms: C. marginatum (Ruldolphi 1819) and Neascus sp. (Hughes 1927). The adults of these flukes are reported to occur in piscivorous birds (Hoffman 1967). Neascus sp. was the most abundant. The second most abundant worm parasitizing the white sucker was the caryophyllaeid cestode Glaridacris catostomi (Cooper 1920). Finally, this report constitutes new state records for A. jacksoni and G. catostomi. Acknowledgements are due Dr. John S. Mackiewicz (State University of New York at Albany) and Professor W. L. Bullock (University of New Hampshire) for parasite confirmation. 54 Transactions of Kentucky Academy of Science, Vol. 34, 1973 LITERATURE CITED Bauer, B. H. and J. P. Harley. 1974. Intestinal parasites from two species of cat- fishes (Icataluridae from Lake Wilgreen in Kentucky. Trans. Ky. Acad. Sci. (In Press). Bullock, W. L. 1962. A new species of Acanthocephalus from New England fishes, with observations on variability. J. Parasit., 48 (3):442-451. Cooper, A. R. 1920. Glaridacris catostomi gen. nov., sp. nov., a cestodarian para- site. Trans. Am. Microsc. Soc., 89 (1) :5-24. Harley, J. P. and T. L. Keefe. 1970. Helminth parasites of four species of sun- fishes (Centrarchidae ) from Lake Wilgreen in Kentucky. Trans. Ky. Acad. Sci. 32:71-T74. Hoffman, G. L. 1967. Parasites of North American Freshwater Fishes. Univ. of Calif. Press, Berkeley, 486 pp. Hughes, R. C. 1927. Studies on the Trematoda family Strigeidae (Holostomidae). No. 8. A new metacerearia, Neascus ambloplitis, sp. nov., representing a new larval group. Trans. Am. Microsc. Soc., 46 (4) :248-267. Ruldolphi, C. A. 1819. Entozoorum Synopsis cui Accedunt Mantissa Duplex et Indices Locupletissimi, Berolini. 811 pp. Received: 7 August, 1973. Accepted: 16 October, 1973. Transactions of Kentucky Academy of Science, Vol. 34, 1973 55 INTESTINAL PARASITES FROM TWO SPECIES OF CATFISHES (ICTALURIDAE) FROM WILGREEN LAKE IN KENTUCKY BRUCE H. BAUER AND JOHN P. HARLEY Department of Biological Sciences Eastern Kentucky University Richmond, Kentucky 40475 The helminth parasites of Kentucky fishes have, overall, been grossly neglected compared with data from other states (Harley and Keefe 1970). The only studies in Kentucky are: (a) Cable (1935) who described a new species of trematode (Cercaria kentuckiensis); (b) Tarter (1969) who listed 2 helminths of the western blacknose dace; (c) Harley and Keefe (1970) who listed 15 helminths from 4 species of sunfishes; (d) Aliff (1973) who, in a very comprehensive survey, listed 28 digenetic trematodes from 92 species of Kentucky fishes; and (e) White (1973) who listed 4 ecto- and 11 endoparasites of the white sucker. This present study was undertaken to contribute further to the study of Kentucky fish parasites; specifically those of the channel catfish Ictalurus punctatus (Rafinesque) and the black bullhead Ictalurus melas (Rafinesque) in Wilgreen Lake, Madison County, Kentucky. Five I. punctatus and 10 I. melas were collected between 5 April and 29 April, 1973. The fish were autopsied and the parasites fixed, stained, and identified according to the procedures of Harley and Keefe (1970). The parasite load classification of: light (1-10 parasites/host), medium (10-50) parasites/host), and heavy (more than 50 parasites/host) was from Dechtiar (1972). Both species of fishes examined harbored parasites. Of the 15 specimens examined, 14 were infested with at least 1 species of parasite. All the J. punctatus examined were infested; 1 with a heavy infestation and 4 with moderate infestations. Nine of the I. melas examined had light infestations and 1 had no parasites. Two cestode species were found. Corallobothrium fimbriatum Essex was found in both I. melas and I. punctatus and was the most prevalent parasite. Immature adults of Proteocephalus perplexus LaRue were found in I. melas. The above cestodes were the only parasites found; nevertheless, they represent new state and range extension records. Finally, it should be noted that the specimens of C. fimbriatum in the channel catfish were fully developed, segmented adults. This is contrary to the findings of van Cleave and Mueller (Sneed 1961), in which they re- ported that C. fimbriatum (in I. punctatus) in the spring and summer were small and unsegmented, suggesting that this fish was an unsuitable host for the parasite. However, based on our evidence obtained the channel catfish is a suitable host for C. fimbriatum in Kentucky. The authors gratefully acknowledge the assistance of Dr. Branley A. Branson. LITERATURE CITED Aliff, John V. 1973. Digenetic trematodes from Kentucky fishes. Doctoral Dis- sertation, University of Kentucky. 128 p. 56 Transactions of Kentucky Academy of Science, Vol. 34, 1973 Cable, R. M. 1935. Cercaria kentuckiensis n. sp., first representative of the Vivax group known to occur in the United States. J. Parasit., 21:441. Dechtiar, A. O. 1972. Parasites of the fish from Lake of the Woods, Ontario. J. Fish. Res. Bd. Can. 29:275-283. Harley, John P. and T. L. Keefe. 1970. Helminth parasites of four species of sunfishes. Trans. Ky. Acad. Sci. 32:71-74. Sneed, K. E. 1961. A description of anomalous and a typically developed tape- worms (Proteocephalidae: Corallobothrium) from catfishes (Ictalurus). J. Parasit. 47:809-812. Tarter, Donald C. 1969. Some parasites of the western blacknose dace Rhinichthys atratulus meleagris Agassiz, in Doe Run, Meade County, Kentucky. Trans. Amer. Microsc. Soc. 88:425-430. White, Glenn E. 1973. Helminth fauna of the common white sucker, Catostomus commersoni (Lacépéde) (Pisces: Catostomidae) in the Kentucky River drainage system, with a note on the leeches and parasitic crustaceans re- covered. Master of Science Thesis, Eastern Kentucky University, Richmond, Kentucky. 49 p. Received: 27 August, 1973. Accepted: 11 September, 1973. Transactions of Kentucky Academy of Science, Vol. 34, 1973 57 SEXUAL DIMORPHISM IN KENTUCKY QUEEN SNAKES (REGINA SEPTEMVITTATA) BASED ON SCUTE COUNTS BRANLEY A. BRANSON AND EDD C. BAKER Department of Biological Sciences Eastern Kentucky University Richmond, Kentucky 40475 Regina septemvittata (Say) is the most common water snake in east- central Kentucky. Wood and Duellman (1950) in Ohio snakes, reported overlapping sexual dimorphism with regard to ventral and caudal scute counts, two-thirds of their specimens possessing counts that fell well within the area of overlap. Our observations on 126 queen snakes, collected from 3 creeks in Madi- son County, Kentucky, during June, July, and August 1969, demonstrated a marked difference in caudal scute counts, hence complete sexual dimorphism in that scute count (Table 1, Fig. 1, 2). Ventral scute counts, with con- Table 1 Ventral and Caudal Scute Counts in 126 Regina septemvittata. x—mean; s=standard deviation; s,—standard error. 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