kS / X THE VIRGINIA JOURNAL OF SCIENCE EDITOR Werner Wieland Biological Sciences Department University of Mary Washington Fredericksburg, VA 22401 Phone: (540)654-1426 BUSINESS MANAGER James H. Martin Dept, of Biology - PRC J. S. Reynolds Comm, Coll. P.O. Box 85622 Richmond, VA 23285-5622 Phone: (804)523-5593 ©Copyright, 2005 by the Virginia Academy of Science. The Virginia Journal of Science (ISSN:0042-658X) is published four times a year (Spring, Summer, Fall , Winter) by the Virginia Academy of Science, 2500 W. Broad Street, Richmond, Virginia 23220-2054. The pages are electronically mastered in the Parham Road Campus Biology Department of J. Sargeant Reynolds Community College. The Virginia Academy of Science and the Editors of the Virginia Journal of Science assume no responsibility for statements or opinions advanced by contributors. Subscription rates for 2005: $35.00 per year, U.S.A.; $35.00 per year, other countries. All foreign remittances must be made in U.S. dollars. Most back issues are available. Prices vary from $5.00 to $25.00 per issue postpaid. Contact the Business Manager for the price of a specific issue. Changes of address, including both old and new zip codes, should be sent promptly to the following address: R. Gerald Bass, Executive Officer, Virginia Academy of Science, 2500 W. Broad Street, Richmond, Virginia 23220-2054. All correspondence relating to remittance, subscriptions, missing issues and other business affairs should be addressed to the Business Manager. For instructions to authors, see inside of back cover. VIRGINIA JOURNAL OF SCIENCE OFFICIAL PUBLICATION OF THE VIRGINIA ACADEMY OF SCIENCE Vol. 56 No. 2 SUMMER, 2005 TABLE OF CONTENTS PAGE ARTICLES Phytoplankton Development Within Tidal Freshwater Regions of Two Virginia Rivers, U.S.A. Harold G. Marshall and Lubomira Burchardt The Small Mammals of Isle of Wight County, Virginia, as Revealed by Pitfall Trapping. Robert K. Rose Bats Of Sky dusky Hollow, Bland County, Virginia. Virgil Brack, Jr., Richard J. Reynolds, Wil Omdorff, Joe Zokaites, and Carol Zokaites JEFFRESS RESEARCH GRANT AWARDS ^wthsoaTT^^ I . , . i' I I MH^X.i^’ pa' ■■ ,/■! •?i^P“'^ r ‘ (.■il'''>’' ' ' "£€4" '‘Jlya?i^'itr>': «!ij ■«■'.■ % m r. ■4 : f," . r. r ' , • i _ V 4 ^ .^«,a ■}« ' ' ;i ' 'I. 3 ■ I 1 V*’ 1 ■• JiiAfS -V ; .».,' ;f; ■5i<^ *« ." ■ '-.: - ■>" . {4(‘' -- ■ '. ‘ '7.''„v-irvV- -•' .. ■ ®‘ IJ-I *“■ ' . '•■■'■•» ■■■ -♦■I ? r, , <»'f^^j5' !,E- ■ '('■'^ I „ -.f > ' I,:' . . / ' ■V').: " : - ’-v ’‘i- P A At ' M ' Virginia Journal of Science Volume 56, Number 2 Summer 2005 Phytoplankton Development Within Tidal Freshwater Regions of Two Virginia Rivers, U.S.A. 1 2 Harold G. Marshall and Lubomira Burchardt ^Department of Biological Sciences, Old Dominion University, Norfolk, VA, 23529-0266, U.S.A., Department of Hydrobiology, Collegium Biologicum, Adam Mickiewicz University, 61-614 Poznan, Poland ABSTRACT Phytoplankton composition and the range of seasonal patterns of abundance are presented for the tidal freshwater regions in two Virginia rivers based on data accumulated monthly from 1986 through 1999. Diatoms dominated the flora during spring, summer, and fall, whereas, other taxonomic categories were more representative when the river flow rates decreased, allowing for a more stable water system and increased residency time within this tidal region during summer and early fall. This summer/fall period was associated with increased water temperatures, higher productivity rates and chlorophyll lev¬ els, increased total phytoplankton abundance and species diversity. The major components of the summer flora were autotrophic picoplankton, chlo- rophytes, and cyanobacteria. Mean, maximum, and minimum monthly abun¬ dance figures are given for the different phytoplankton categories, and total phytoplankton biomass and abundance, over this 13 -year period. Although one station showed considerable influx of oligohaline water into its tidal freshwater region during sampling, no significant relationships were associ¬ ated with phytoplankton biomass or productivity to these changing salinities. Key words: Phytoplankton, Virginia, Rappahannock, Pamunkey, tidal freshwater INTRODUCTION Marshall and Burchardt, 1998, have described the tidal freshwater region as a unique component of a river system. It is daily influenced by tidal action, yet, the location of this region in a river will move upstream or downstream, depending upon daily or seasonal changes in the occuirence and duration of rainfall, or due to various hydrodynamic events that would influence tidal amplification and flow within the river. The tidal freshwater is defined as the region within a river possessing daily tidal movements bordered upstream by freshwater (<0.5 ppt) lacking a tidal response, and downstream by tidal waters of greater salinity. This is the tidal oligohaline region that is characterized by salinities 0.5 to 5.0 ppt. The algae entering the tidal fresh region upstream are dominated by chlorophytes, diatoms, and cyanobacteria in contrast to downstream flora (e.g. in oligohaline and mesohaline regions) where estuarine diatoms and dinoflagellates are the dominant taxa (Haertel et al., 1969; Forester, 1973; Jackson et al., 1987; Marshall and Alden, 1990). The tidal freshwater region may also contain a small percentage of estuarine species. These are introduced from sub-pycnocline waters advancing upstream during periods of low river discharge and when tidal 68 VIRGINIA JOURNAL OF SCIENCE movement advances farther upstream into normally tidal freshwater regions (Marshall and Burchardt, 1998). Farrell, 1994 and Schmidt, 1994, have associated increased diatom abundance with increased river discharge common during spring months. Marshall and Burchardt ,1998, reported peak diatom development occurred in the tidal freshwater James River (Virginia) during periods of increased river discharge, with chlorophytes, cyanobacteria, autotrophic picoplankton, and euglenophytes having greater abundance during summer and periods of more stable water conditions. This study reports on the phytoplankton populations and water quality of tidal freshwater stations in the Pamunkey River and Rappahannock River, both located in southeast Virginia, U.S.A. The Rappahannock River (ca. 341 km in length) is a major tributary of the Chesapeake Bay located in the eastern coastal plain of Virginia. The river flows southeasterly through predominantly forest, crop-land, and pasture before entering Chesapeake Bay. The Pamunkey River (ca. 96 km long), is also located in Virginia, just south of the Rappahannock River, flowing southeasterly through mostly forest and land used in agriculture, or for raising live stock. The river terminates at its confluence with the Mattoponi River, forming the York River that continues parallel to the Rappahannock River before entering the Chesapeake Bay. The climate in this region is moderate with an average annual temperature ca. 14‘^C and average rainfall ca. 106-1 16 cm. Previous phytoplankton studies in the Pamunkey/York and Rappahannock rivers include those by Marshall and Alden, 1 990; Marshall and Affronti, 1 992; Marshall and Nesius, 1993; and Marshall and Burchardt, 2004. Their results identify the charac¬ teristic species composition and abundance in these rivers. Spring, summer, and fall productivity and abundance maxima were described in relation to dominant flora, with the autotrophic picoplankters being a major component and contributor to productivity during summer (Marshall and Nesius, 1993). Downstream studies in the York River section are mainly in the lower reach of the river where summer dinoflagellate blooms are common (Mackieman, 1968;Zubkoffetal., 1979). Relationships of phytoplankton distribution and stratification to tidal cycles in the York River are discussed by Haas etal., 1981 and Ducklow, 1982. The objectives of this study are to identify the seasonal developmental patterns of the phytoplankton composition within the tidal freshwater regions of two rivers. Using a long-term data base the annual biomass patterns are described to indicate the range of population fluctuation that may occur within these systems. Additional charac¬ teristics and environmental relationships between the phytoplankton community and several physical and chemical factors associated with these rivers are also presented. METHODS Monthly water samples were taken at the tidal freshwater stations in the Rappahan- nock River (TF3.3, 38“ 01’ 07” N; 16° 54’ 30"W) and the Pamunkey River (TF4.2, 37“ 34’ 47"N; 11° 01’ 19"W) from July 1986 through December 1999 (13.5 years) (Figure 1 .). The mean depths at these stations were ca.6.8 m and ca.8.9 m respectively for TF3.3 and TF4.2. At each station a vertical series of five 3 liter water samples were taken from the upper third of the water column and placed in a carboy, mixed, and a 500 mL sample drawn off and fixed with Lugofs solution. These samples were analyzed using a modified Utermohl technique following a series of settling and PHYTOPLANKTON DEVELOPMENT 69 FIGURE 1 . Sampling stations: Station TF3.3 (38° 01 ’ 07” N; 76° 54’ 30” W) located in the Rappahannodc River and Station TF4.2 (37° 34’ 47”N; 77° 01’ 19” W) in the Pamunkey River, Virginia. siphoning steps over time to produce ca. 40 mL concentrate of the original sample for subsequent microscopic analysis (Marshall and Alden, 1990). Identification and cell abundance for each sample were based on a minimum microscope cell count of 200, using a minimum of 10 random fields examined at 315X and 500X, plus including other species observed by scanning the entire counting chamber at 125X. An additional 24 samples from 1998-1999 at these stations were examined for further species identification. The autotrophic picoplankton cells were identified using epifluores- cence microscopy as described in Marshall, 1995. Also determined were produc¬ tivity rates, beginning in July 1989, using protocols described by Marshall andNesius, 1 993. Biomass was determined from cell volume measurements made for the different species and transferred to cell carbon according to Smayda, 1978. The Margalef Diversity Index was used regarding species diversity. River water discharge rates were provided by the U.S. Geological Survey from locations near station TF3.3 (38°19’20" N, 77°3 r05"W), and station TF4.2 (37°46’03"N, 77''l9’57'’W). Surface water tem¬ peratures and Secchi readings were taken on station during each sampling period. Additional water quality data from these stations were provided by the Virginia 70 VIRGINIA JOURNAL OF SCIENCE Monthly Mean Discharge Rates Month FIGURE 2. Monthly mean discharge rates (1986-1999) for stations adjacent to stations TF3.3 in the Rappaliannock River and TF4.2 in the Pamunkey River Chesapeake Bay Monitoring Program. These included analysis of water taken on station for total nitrogen (TN), total phosphorus (TP), total suspended solids (TSS), and dissolved oxygen. Seasonal references are defined as winter including the months of December, January, and February, followed by the sequential 3-month periods for spring, summer, and fall. A Student T-test was used to determine distribution relation¬ ships of the phytoplankton and productivity to salinity differences noted during the sampling period at the Rappahannock River station TF3.3. RESULTS 2 2 The drainage area above the two sampling stations is 4,133 km and 1,739 km for the Rappahannock and Pamunkey Rivers respectively, with the monthly discharge pattern similar at both sites. Peak water flow at these stations was from winter through early summer (December-June), with decreased flow in mid-summer that continued into early fall (July-September), after which flow increased, from mid-fall into the winter months (Figure 2). The summer minimum and winter-spring maximum of the mean monthly rates of flow differed at the two stations, ranging from. 25.8 m^ sec’^ (912 sec’^) in July to 76.7 m^ sec'^ (2,71 1 ft^ sec’^) in March for the Rappahannock River, and from 12.4 m^ sec'^ (438 ft^ sec'^) in August to 52.7 m^ sec'^ (1,863 ft^ sec'^) in February in the Pamunkey River. The major annual influence to these seasonal flow patterns was the amount of rainfall within these two river watersheds. U.S. Geological Survey records of flow rates began in 1951 and are the basis for estimating average and extreme periods of monthly and annual mean flow. Those annual rates that were within the 25 to 75 percentile of this data set were considered average, or normal. If the annual rate falls below the 25 percentile it would be considered a “dry” year, whereas, flow rates above the 75 percentile would be classified as “wet” years. During the 13 years of this study, the annual flow into these rivers varied greatly. There were 5 “wet” and 5 “dry” years, and 3 years where the flow may be considered “normal”, PHYTOPLANKTON DEVELOPMENT 71 or “average”. As these differences in annual rainfall occur, they will have major influence on the horizontal range and dynamics associated with the tidal fresh and various downstream salinity regions of these rivers. Progressing into this study it became evident that salt-water intrusion frequently occurred at TF3.3 in the Rapppa- hannock River. Over the 13 year period, Station TF3.3 had freshwater status (<0.5 ppt) 40.6% of the collection dates, whereas, during 59.4% of the dates the salinity was >0.5 ppt. Tidal freshwater status was associated with periods of increased rainfall and coincided with the spring diatom bloom (e.g. January-May). Periods when salinity intrusion into this area was most common occurred during the summer and fall months (June-October). In contrast, station TF4.2 in the Pamunkey River had freshwater status on 97.7% of the collection dates. Overall, more water flowed through the Rappahan¬ nock station, and at a faster rate, than at the Pamunkey station. Both stations had similar surface water temperature patterns reaching highs of ca. 28 in July, with lowest mean monthly temperatures occurring in February at TF3.3 (3.6 ®C) and in January at TF4.2 (4.8 ®C). The dissolved oxygen concentrations were inversely related to the water temperature with lowest values during summer and highest in winter. The mean monthly range was from 6.5 in July to 12.2 mg L'* at TF3.3 in February, and 4.7 in August to 1 1.8 mg L"* in February at TF4.2. Monthly periods of peak total suspended solids (TSS) varied, with greatest loads during periods of high flow in spring (Figure 3). At station TF3.3, TSS were consistently higher than at TF4.2, ranging from 20.6 mg L‘* in late summer (August) to 51.2 mg L^, in late winter (February). The TSS at station TF4.2 ranged from monthly means of 13.5 (Sept.) to 1 8.9 mg L"* (Dec.), showing a rather stable pattern throughout the seasons. The TSS increased gradually from summer into fall, reaching highest concentrations from early winter through spring. Maximum records of 140 and 168 mg L'^ at TF3.3 occurred in January and May respectively. Mean monthly Secchi readings ranged from 0.3 1 m (February- April) to 0.64 m (September) at TF3.3, and from 0.51 m (January) to 0.82 m (September) at TF4.2. The annual monthly means for TF3.3 and TF4.2 were 0.45 m and 0.70 m respectively. These results indicated an association between increased water flow to higher TSS concentrations and reduced Secchi readings at TF3.3, in contrast to the reverse relationships during periods of reduced flow during summer. However, this relationship was less clear at TF4.2, where a lower and more consistent presence of TSS was recorded. More suspended solids were carried in the Rappahan¬ nock, with the mean and range of Secchi readings less than in the Pamunkey River. There were differences in the total nitrogen (TN) patterns at the two stations (Figure 3). At TF3.3, peak levels (monthly means) occurred in early spring (1.32 mg L'*, March), decreasing into the summer and fall months to a low of 0.73 mg L‘* (August) to increase through late fall and winter to the spring highs. Maximum levels occurred from mid-winter through mid-spring. The mean range at TF4.2 showed less variability, increasing from 0.69 mg L’’ (November) to 0.88 mg L"^ (June), resulting in the mean total nitrogen being higher at TF3.3 than at TF4.2. The mean monthly total phosphorus (TP) at TF3.3 ranged between 0.06 and 0. 12 mg L’* throughout the seasons, showing a decrease from late spring into summer, before rising again in winter (Figure 3). At TF4.2, the monthly means ranged from 0.06 mg L'* in the fall (October), to a spring (March) high of 0.12 mg L"l Maximum TP occurred during winter-spring at TF3.3 and in summer at TF4.2 (Figure 3). Both stations had pulses that occurred in early spring, mid-summer, and fall, with the highest monthly means at TF3.3. The mean 72 VIRGINIA JOURNAL OF SCIENCE TN:TP ratio ranged from 7.6 to 12.6 at TF3.3, and 8.2 to 13.8 at TF4.2, with the lowest ratios occurring May through July at TF3.3, and in July and August at TF4.2. Thus, there were general differences in the periods of maximum levels of nitrogen and phosphorus in these rivers. In the Rappahannock, the greatest TN concentrations occurred in spring and the lowest in late summer, corresponding to the high and low flow periods in this river. In the Pamunkey, the highest TN concentrations were in early summer, and least in late fall. TP maxima occurred in winter and summer respectively for the Rappahannock and Pamunkey. In the Pamunkey, this summer TP high coincided with high productivity, decreased river flow, and increased concentra¬ tions of cyanobacteria, picoplankton, and other algae. Chlorophyll a increased into summer from a winter low, with concentrations greater at TF3.3 than at TF4.2 (Figure 4). At TF3.3, the monthly mean ranged from 2.9pg L’' (January) to 13.9 pg L‘* (August). There was generally a late spring (May) develop¬ ment, a slight decrease in early summer, then highs from mid-summer through fall. At TF4.2, there was chlorophyll a increase during summer, with peaks in July and August (9.27, 8.37 pg L'*), to a January low (2.09 pg L”'). Also present were periods of maximum chlorophyll a concentrations from spring through fall at both stations. The mean productivity rates for both stations were lowest during mid-winter, then gradually increased to peaks during late spring, summer, and early fall, before declining into winter (Figure 5). The higher rates were consistently recorded at station TF3.3 and ranged from 12.2mgcm^h‘* (Dec.) to 156.9 mg cm^ h'^ (May). Increased productivity extended from April through August. At TF4.2, productivity ranged from 5.2 mg cm'’ h" ^ (Dec.) to highs of 43 . 1 and 46.3 mgcm^ h‘ ^ for July and August respectively. This pattern was similar to seasonal chlorophyll a concentration differences between the two river stations with highest mean rates of productivity during the summer months. A total of 268 phytoplankton taxa were identified at these two stations (Marshall and Burchardt, 2004). There were 208 and 232 phytoplankton taxa represented at the Rappahannock River and Pamunkey stations respectively. Sixty one percent of the taxa were present at both stations, with the general composition of the dominant species similar. The major difference in composition was the estuarine taxa at the Rappahan¬ nock station during periods (summer/early fall) of increased salinity and upstream advancement of tidal water from the oligohaline region. Collectively for both stations, there were 133 Bacillariophyceae, 63 Chlorophyceae, 31 Cyanobacteria (cyano- prokaryotes), 10 Dinophyceae, 11 Euglenophyceae, 6 Xanthophyceae, 5 Cryptophy- ceae, and 9 Chrysophyceae. The autotrophic picoplankton was identified as a separate and composite group from the above categories and consisted predominantly of single celled cyanobacteria. Figures 6 and 7 show the monthly maximum and minimum records, and means for the major phylogenetic categories. The two extremes indicated the past ranges recorded for these categories. Variability also occurred over this time period in taxon representation in each water sample analyzed, with maximum repre¬ sentation of taxa per water sample in the summer months and least in winter (e.g. at TF3.3 these totals were 73 and 26 taxa; and at TF4.2, 59 and 22 taxa). The Margalef Diversity Index maxima during this period ranged from 2.3 (January) to 4.0 (July) at TF4.2, with the mean monthly range from 1.6 (March) to 2.4 (August). The diversity maxima at TF3.3 ranged from 2.3 (January) to 4.0 (July), with monthly means from 1 .6 (March) to 2.4 (August). Diversity was lowest at both stations in late winter/early PHYTOPLANKTON DEVELOPMENT 73 . i _ ! ' 0500' . - - . . "yfmw - - \ imw/\ i 0403 i If \ Ijawi ' r- 015 1 GO, 1 I g i 0 iffiJ , T 7 \ ^ 1 \ \ 0.TO ■ o.m m i F « A i* J . i A $ O « £> FIGURE. 3 Monthly concentrations for chlorophyll a, total phytoplankton abundance, and total phyto¬ plankton biomass at TF3.3 and TF4.2, 1986-1999, indicating mean (solid line), maximum (dotted line), and minimum (dot-dash line) records. spring when flow in the rivers was greatest, increasing into summer during periods of reduced flow rates. In presenting total phytoplankton abundance and total phytoplankton biomass, the mean monthly values, plus the cell maxima/minima amounts are indicated (Figure 4). The seasonal patterns of phytoplankton development show seasonal abundance peaks in mid-winter, spring, mid-summer and fall (Figure 4). The abundance figures do not include the picoplankton, however, the picoplankton biomass was included in the total phytoplankton biomass. The mean monthly range at TF3.3 was 6.8 x 10^ cells L'^ (February) to 35.5 x 10^ cells L'^ (July), with the highest cell concentrations as 108.8 X 10^ cells L“^ (July). At TF4.2, abundance ranged from 24.0 x 10^ cells L'^ (March) to 12.8 X 10^ cells L'^ (July), with the maximum of 35.9 x 10^ cells L’^ (January). The phytoplankton biomass mimics these patterns, but with greater biomass during spring and fall, followed by winter and summer at TF3.3. In contrast, at TF4.2 the summer biomass was greater than in the other seasons. At TF3.3 the phytoplankton biomass 74 VIRGINIA JOURNAL OF SCIENCE j OlHUJ 50.05. -laco. : G OQlCO 1 s I moo 1 QOO JFMAMi JASO NO FIGURE 4. Monthly concentrations of chlorophyll a, total phytoplankton abundance, and total phytoplank¬ ton biomass at TF3.3 and TF4.2, 1986-1999, indicating mean (solid line), maximum (dottedline), and minimum (dot-dash line) records. ranged from 279 to 979 x 10^ figcm^ (December, April), with the maximum of 4,902 X 1 0^ pgCm^ (October), and the least as 48 pgcm^ (November). Biomass peak records were associated with the diatoms. At TF4.2, the biomass ranged from 91 to 818 x 10^ n ^ It pgcm (December, July), with a maximum record of 3,694 10 pgcm in July. Since there were frequent salinity differences occurring in the tidal freshwater station (TF3.3) in the Rappahannock River, student T-tests were run to determine the degree of phytoplankton/salinity relationships present. The results indicated there were no significant differences between total phytoplankton biomass (p = 0.296), diatom biomass (p = 0.1 16), cyanobacteria biomass (p = 0.399), or productivity (p = 0.823), to salinity values <0.5 and those >0.5 ppt. at this location. PHYTOPLANKTON DEVELOPMENT 75 Mean Productivity Rates Month FIGURE 5. Mean monthly carbon productivity rates for stations TF3.3 and TF4.2 from July 1989 to December 1999. I . Bacillariophyceae: The diatoms had mean monthly concentration peaks occurring during win¬ ter/spring, summer, and fall at both stations, with greater abundance recorded in the Rappahannock River (Figure 6). Diatoms represented the seasonally dominant flora at both stations. Mean monthly minimum and maximum concentrations were 3.2 to I I. 4x lO^cellsL’^ (December, May) at TF3. 3, and 1.0to3.5x lO^cellsL”^ (December, July) at TF4.2. The recorded minimum and maximum concentrations over this period were 0.5 and 53.1 x 10^ cells L'^ at TF3.3 (October, January), and 0.007 to 28.2 x 10^ cells L'^ at TF4.2 (October, April). The diatoms had a diverse assemblage of taxa that included the major producer of the spring diatom pulse, Skeletonema potamos, and an abundance of planktonic centrics and benthic pennates. Most common were Aste- rionella formosa, Aulacoseira granulata, A. granulata v. angustissima, A. distans, A. varians, Cyclotella Meneghiniana, C. striata, Navicula crytocephala, N. radiosa, Nitzschia acicularis, Surirella ovata, and a variety of other pennates and centrics <20 microns in size. This composition and dominant freshwater taxa were similar in both rivers. However, the summer/fall flora at TF3.3 contained ample representations of estuarine species, specifically Skeletonema costatum. The mean abundance for the diatoms was moderate within their maximum and minimum concentrations. However, there existed considerable fluctuation in the year-to-year patterns that were influenced by flow through the system and the initiation time for diatom development to occur. The maxima depicted here also illustrates the range of the potential growth for this community. The historic maxima during spring, summer, and fall that occurred at both stations greatly exceeded the mean concentrations. 76 VIRGINIA JOURNAL OF SCIENCE \ . \ II ■ . /V . . * ^ « 10 :| 1 i 5 \ . A i i ? I j . ^ * I i f A u i ■$*. s o a i > FIGURE 6. Monthly concentrations for diatoms, cyanobacteria, and chlorophytes at stations TF3.3 and TF4.2, 1986-1999, indicating mean (solid line), maximum (dotted line), and minimum (dot-dash line) records. 2. Cyanobacteria: At both stations, the predominant development of the cyanobacteria (cyano- prokaryotes) occurred from mid-summer into mid-fall, then decreased in late fall and winter (Figure 6). Flowever, there were sporadic seasonal highs throughout the year with the mean monthly range from 1.2 to 22.2 x 10^ cells L” (April, July) at TF 3.3, and at TF4.2, from 0.2 to 6.3 x 10^ cells L”^ (December, July). Maxima at the two stations were 95.5 and 29.2 x 10^ cells L'^ respectively for TF3.3 and TF4.2, with both occurring in July. Several filamentous taxa were common during winter and early spring. These included Oscillatoria limnetica, O. granulata, O. irregua, O. pseudominima, Nodularia spumigena f litorea, and Lyngbya contorta. Noted through¬ out the year was Dactylococcopsis rhapidioides . This species, plus D. rhapidioides v. falciformis, O. granulata, O. angustissima. Microcystis aeruginosa, M. incerta, and Merismopedia marssonii were common representatives of the summer/early fall flora. The same tidal freshwater species occurred at both stations, with previous records of their abundance common in downstream oligohaline and mesohaline regions of these PHYTOPLANKTON DEVELOPMENT 77 60000 IVWW . ” tFX} Plsopiankton ■■ | 50000 TF4.2 Plc^cnkton ^ - - - .. .* *• i o 40000 / : 2 fimm / '•'* i * - - , - — ^ 1 T* 30000 - ’ « 40000 • ■« i s ; %.* \ % 20000 . i n 20000 . O 10000 i 1 A 0 : JFMAMJJASOND i Marth fFMAMJ JA50NC Month ) FIGURE 7. Monthly concentrations for dinoflagellates, cryptophytes, and autotrophic picoplankton at stations TF3.3 and TF4.2, 1986-1999, indicating mean (solid line), maximum (dotted line), and minimum (dot-dash line) records. rivers (Marshall and Nesius, 1993). The greatest development and diversity within this category occurred during the more stable, decreased flow periods of the year (summer, early fall), which also coincided with warmer water temperatures and a reduced sediment load. 3. Chlorophyceae The chlorophytes were among the most common taxa in the tidal freshwater region. They consisted of a diverse group of single cell, or small colonial forms in the Pamunkey (57 taxa) and Rappahannock Rivers (52 taxa). Seasonal maxima were greater at the Rappahannock River station, and developmental patterns also differed in the two rivers (Figure 6). At TF3.3, several seasonal peaks occurred in late spring, mid-summer, and early fall. The mean monthly range of cells varied frorri 0.5 to 2.7 X 10^ cells L‘^ (April, July), with a maximum of 19.6 x 10^ cells L‘^ in July. At TF4.2 lower concentrations prevailed, with the mean monthly abundance from 0.08 to 2.2 x 10^ cells L'^ (March, July), with a maximum of 1 1 .0 x 10^ cells L'^ for September. At TF4.2 there was a single development during summer, rather than several-peak periods 78 VIRGINIA JOURNAL OF SCIENCE present at TF3.3. Taxa most prevalent included a diverse group of Scenedesmus spp, Ankistrodesmus falcatus, A. falcatm v. fluviatile, Pediastrum duplex, plus several Crucigenia spp. and desmids. Scenedesmus quadricauda was recorded year round, but also common were S. bijuga, S. dimorphus, and S. acuminatus, with the filamentous Ulothrix variabilis also abundant. The development of these taxa favored the less turbulent conditions in the rivers between the spring rains and the fall-winter period. 4. Dinophyceae: Dinoflagellates were not abundant at these stations. Ten species common for this region were recorded and included the freshwater Peridinium cinctum, P. wisconsi- nense and Ceratium hirundinella, plus several taxa characteristic of the downstream estuarine waters, e.g. Heterocapsa rotundata, PI. triquetra, and Prorocentrum mini¬ mum (Marshall and Affronti 1992). There were differences in their abundance, presence, and seasonal patterns at the two stations (Figure 7). TF3.3 contained the higher mean concentrations, exhibiting abundance peaks in spring, summer, and late fall, with lowest concentrations during the winter months when freshwater status was more common. The range was from 0.03 to 0.25 x 1 0^ cells L'^ (February, April), with a maximum abundance of 3.3 x 10^ cells L’^ for April. At TF4.2 the cell maxima occurred in early summer, with a maximum count of 1.5 x 10^ cells L"’ in June, and monthly ranges from 0.004 to 0.14 x 10^ cells L'^ (September, June), with late winter and mid-spring lows prevailing. These taxa were absent in numerous samples through¬ out the year and most common at TF3.3. 5. Cryptophyceae: Although represented by a modest number (5) of species, this was a ubiquitous group throughout the year. There were seasonal fluctuations of development at both stations, with greater abundance at TF3.3 (Figure?). Mean monthly concentrations ranged from 0.7 to 1.8 x 10^ cells L'^ and 0.3 to 1.2 x 10^ cells L"* at TF3.3 and TF4.2 respectively. Maximum records for these two stations were 9.4 and 3.4 x 10 cells L in July and November for TF3.3 and TF4.2. The cryptophytes have been noted as a common background population to other flora within Virginia tributaries (Marshall and Alden 1990). The species recorded were Cryptomonas erosa, C. marsonni, C. ovata, C reflexa, and Rhodomonas minuta. The major cryptomonad development was from early spring through mid-fall, and then decreased in early winter to a mid-winter low. 6. Autotrophic picoplankton: Ubiquitous throughout the year, this category consisted of mainly isolated single cells, or those in small doublets of cells. Cells in this category were less than 2.0 microns in size and did not include species reported in the other categories. They consisted of mainly cyanobacteria and less abundant chlorophytes, with other eucaryotes occasion¬ ally present, but not dominant. Maximum concentrations occurred during the summer months (July-September), but these high numbers frequently extended into early fall and were similar to patterns described in these rivers and Chesapeake Bay (Marshall and Affronti, 1992; Marshall, 1995). The mean monthly ranges for TF3.3 were from 8.3 to 367 X 10^ cells (March, August), and for TF4.2 from 2.2 to 128.2 x 10^ cells L'* (February, June), with maxima for these two stations at 870 and 537 x 10^ cells L'^ PHYTOPLANKTON DEVELOPMENT 79 (August, June) (Figure 7). The minimum counts were 0.31 and 0.18 x 10^ cells L’^ (December, March) at TF3.3 and TF4.3 respectively. The seasonal maxima occurred during the summer/fall months, being associated with warmer water temperatures and reduced river flow, in addition to being a major contributor to productivity during this period (Marshall and Nesius, 1993). 7. Other Phytoplankton Categories: Among other algal categories, there was a small variety of additional background taxa that included euglenophytes, xanthophytes, and chrysophytes. These groups were generally not abundant, with low species diversity in both rivers, and were more common during the summer/fall months. Representative xanthophytes were Cen~ tritractus belonophorus, Ophiocytium cochlerare, Tetraedriella spinigera, Tribonema minus, T. affine, and T. viride. The common euglenophytes were Euglena acus, Lepocinclis sp., Phacus caudatus, P. longicauda, Strombomonas asymmetrica, S. affinis, and Trachelomonas hispida. The chrysophytes were less abundant, but more diverse, and included Dinobryon cylindricum, D. sertularia, D. sociale, Synura uvella, Ochromonas minuscule, Chrysococcus ornatus, and Chromulina wislocchiana. These taxa were noted sporadically within the samples, lacking established periods of major development. DISCUSSION The tidal freshwater region of these rivers contained a diverse representation of phytoplankton taxa dominated in abundance and biomass by a diatom flora. High concentrations of the diatoms occurred during winter-spring, summer, and fall, with decreasing abundance in early winter. Although representative taxa from the other algal categories were present throughout the year, their development was most pronounced in summer and early fall. The patterns of development coincided with periods of high and low river flow. The maximum and minimum concentration records for the different algal categories provide a graphic illustration of the variability that may exist in their development. The major physical influence on water flow during these seasons was the period of the spring rains and increased flow within these rivers, which was followed by months of reduced flow and increased residence time for flora passing through the tidal regions of these rivers. Although the general phytoplankton compo¬ sition and the dominant species at these stations were similar and of mainly freshwater origin, there were differences in water quality and the abundance of the algal flora. For instance, station TF3.3 (Rappahannock River) represented waters with a more rapid rate of flow from a larger drainage system than TF4.2 (Pam unkey River), plus the total suspended sediment loads were greater, and mean Secchi readings were less at station TF3.3, in comparison to TF4.2. The total phosphorus values were somewhat similar, in what may be considered a nitrogen limiting system for both river stations (low TN:TP ratios predominated). The mean spring and fall chlorophyll pulses at TF3.3 corre¬ sponded to higher levels of TN and TP, with the summer chlorophyll highs associated with increased TP levels and a decrease in TN. These periods coincided with the spring diatom pulse, followed by increased abundance of cyanobacteria and chlorophytes during the summer, with a resurgence of diatom concentrations in fall. These were similar to patterns noted in the nearby James River (Marshall and Affronti, 1992; Marshall and Burchardt, 1998). Chlorophyll concentrations typically decreased with 80 VIRGINIA JOURNAL OF SCIENCE the lower temperatures of winter. At TF4.2, the greatest concentrations of chlorophyll were in summer, along with increased levels of both TN and TP. The mean TN:TP ratios increased during greater water flow within the rivers, when additional nitrogen input occurred, and followed by increased diatom development. The decreased flow of summer was associated with increased residency time, lower levels of TSS, deeper Secchi readings, increased picoplankton, increased productivity, greater species diver¬ sity, greater abundance of chlorophytes and dinoflagellates, plus higher chlorophyll concentrations. This was in contrast to the reverse status of these variables associated with the increased flow rates during the winter/spring months. In contrasting the flora at these stations, the Pamunkey River contained a greater diversity of diatoms, cyanobacteria, chlorophytes, chrysophytes, cryptophytes, and euglenophytes. Of the 268 taxa identified at these two stations, 232 (86.6%) were recorded in the Pamunkey River, with 208 (77.6%) in the Rappahannock River, and there were 61.9% of the taxa common to both stations. Differences in composition were mainly noted in three algal categories (diatoms, dinoflagellates, chlorophytes), with additional estuarine species recorded at TF3.3. There was greater phytoplankton abundance, productivity, and biomass in the Rappahannock River (TF3.3), which also contained higher TN and TP concentrations, with indications of less light availability than station TF4.2, as indicated by the more shallow Secchi depths recorded. SUMMARY The comparison of the tidal freshwater regions of two closely located river systems indicated both differences and similarities in the abundance, diversity, and develop¬ ment of the phytoplankton populations. These differences, which include the ranges of seasonal and annual development among the various phytoplankton taxa, were a product of the unique combination of conditions in the two rivers (e.g. water quality, light and nutrient availability, seasonal flow rates). These cumulative factors, and others, influenced the floral composition and its seasonal abundance, plus determine the initiation and duration of development among the algal assemblages. These conditions were further influenced by the amount, timing, and duration of river water flow annually, when wet and dry years of water occur within these rivers. Yet, there were similarities in algal composition and dominant species within these rivers, and in their seasonal development transitions that extend beyond local conditions and are characteristic of broader developmental patterns typically associated with phytoplank¬ ton in temperate regions. ACKNOWLEDGMENTS This study is a component of the Chesapeake Bay Monitoring Program supported by the Virginia Department of Environmental Quality and the U.S. Environmental Protection Agency. Special thanks are given to Dr. Kneeland Nesius of Old Dominion University for providing the results of the productivity analysis determined during the period of study. Both authors participated in the species identification and data analysis of this paper. LITERATURE CITED Ducklow, H. W. 1982. Chesapeake Bay nutrient and plankton dynamics. 1. Bacterial biomass and production during spring tidal destratification in the York River, Virginia, estuary. Limnology and Oceanography 27(4);65 1-659. PHYTOPLANKTON DEVELOPMENT 81 Farrell, I. 1994. Comparative analysis of the phytoplankton of fifteen lowland fluvial systems of the River Plate Basin (Argentina). Hydrobiologia 289: 109-1 17. Forester, J. W. 1973. The fate of freshwater algae entering an estuary. Pages 387-419 In L. Stevensen, and R. Colwell, R., eds. Estuarine Microbial Ecology, University of South Carolina Press, Columbia. Haas, L.W., S J. Jastings, and K.L. Webb. 1981. Phytoplankton response to a stratifi¬ cation mixing cycle in the York River during late summer. Pages 619-636 In J. Neilson and L. Cronin, eds. Estuaries and Nutrients, Humana Press, Clifton, N.J. Haertel, L., C. Osterberg, H. Curl, and P. Park. 1969. Nutrient and plankton ecology of the Columbia River estuary. Ecology 50: 962-978. Jackson, R., P.L. Williams, and 1. Joint. 1987. Freshwater phytoplankton in the low salinity region of the River Tamar Estuary. Estuarine, Coastal, and Shelf Science 25:299-311. Mackieman, G. B. 1968. Seasonal distribution of dinoflagellates in the lower York River, Virginia. M.A. Thesis, College of William and Mary, Williamsburg, Va., 104 pp. Marshall, H.G. 1995. Autotrophic picoplankton distribution and abundance in the Chesapeake Bay, U.S.A. Marine Nature 4:33-42. Marshall, H.G. and L.F. Affronti. 1992. Seasonal phytoplankton development within three rivers in the lower Chesapeake Bay region. Virginia Journal of Science 43:15-23. Marshall, H.G. and R.W. Alden. 1990. A comparison of phytoplankton assemblages and environmental relationships in three estuarine rivers of the lower Chesapeake Bay. Estuaries 13(3):287-300. Marshall, H.G. and L. Burchardt. 1998. Phytoplankton composition within the tidal freshwater region of the James River, Virginia. Proceedings of the Biological Society of Washington 1 1 1(3):720-730. Marshall, H.G. and L. Burchardt. 2004. Phytoplankton composition within the tidal freshwater-oligohaline regions of the Rappahannock and Pamunkey Rivers in Virginia. Castanea 69(4):272-283. Marshall, H.G. and K.K. Nesius. 1993. Seasonal relationships between phytoplankton composition, abundance, and primary productivity in the three tidal rivers of the lower Chesapeake Bay. J. Elisha Mitchell Scientific Society 109(3): 141-151. Schmidt, A. 1 994. Main characteristics for the phytoplankton of the southern Hungar¬ ian section of the River Danube. Hydrobiologia 289:97-108. Smayda, T. 1978. From phytoplankters to biomass. Pages 273-279 In Soumia, A., ed. Phytoplankton Manual, United Nations Educational, Scientific and Cultural Organization, Paris. Zubkoff, P., J.C. Munday, R.G. Rhodes, and J.E. Warinner. 1979. Mesoscale features of summer (1975-1977) dinoflagellate blooms in the York River, Virginia (Chesapeake Bay estuary). Pages 279-286 In D.L. Taylor and H. H. Seliger, eds. Toxic Dinoflagellate Blooms. Elsevier, Inc., N.Y. 82 S’'. VIRGINIA JOURNAL OF SCIENCE i - J / - V -*• •■’^ t : : ti. .».• j •■'>'/; 'i? ( M _ 'V^i'v.y ._,L 39 . r .;.. ’ I ■ -I - *■■*;? ■•■ ■■ t * «' t WsllSiWflaJ.i^ ‘I' -1 ,j»i.i;t>''i '■•■" ' **-t' '■J!^''iVi'Wj9t5Sf'' ^‘-"t' '-j ■ i-V- ■ ■ -- ■-' • i‘-- ' <■ ^KvniL . V^. “ ■ ,: sJr^aifU ,vQ J. I < * \* ■' ^ L* > ' ' A::?^-^-.^' ■’■ > ' ’:' •. .■- -".di'CcttW '^f«»il)i>ti.'' I -ttCHfe^' ■ ? •' ..'^S'-W . ''jiv siiyTlHf 4!«tii*irjiai^4iil^^. ' .';'>r. f- ' '. .', ■- ’• H ' ’ ^I^^D^lll^S^(^l««■ v’, ..^^• ■ f (^^■4:•-';^.^i*J;^|i^■- |(; («■'*:, ■ ,.i: v: <• i,..* L.-.< ..jr|* J>jii{r;.M; , .w‘' V ’0:>/n Wlaiwaalwi.i^ j ; / : , -1 - a. rij .‘M .Kv. '" ■■ ■■ " '0 - i' n.if.4Rrifefa>Tj»ty“rtftfc^ ■,tj9ffi-iaS§BI 1^* ato.r Wt»R# 1^ . .r:.-^- 1?. ^ *v. .f.- r, .. KvJKfirtJtt ' ••r.i »w • ^ " vr .1 v*» ^ ■ fi- * •w n/AVi';'" t « ii:^) . . :< v'‘f-.V. " . ■-. I *.■•- - *)•' l" ^,V-’ ««r ^ ^ i ■ t \ . .ViVf i> ’. ''‘A»..,Jt.^r,jvr.iv. ■ ■ >■ I I r. ■.r‘;!^.iTrL II& . . " ' IBf’ '. Iff',,. e.' ■ • ;.;. ■'"i ... ■•:■ , ■... ''-. ,1 ■ ' :l. '{H- .r.|) r;.rtl.%jU.,‘r7?iK>?'‘''s •4 Virginia Journal of Science Volume 56 Number 2 Summer 2005 The Small Mammals of Isle of Wight County, Virginia, as Revealed by Pitfall Trapping, Robert K. Rose, Department of Biological Sciences, Old Dominion University, Norfolk, Virginia 23529-0266 ABSTRACT In a study conducted in mid-winter, pitfall traps were used to assess the small mammal communities on 14 grids set in open habitats in Isle of Wight County in eastern Virginia. In all, 136 shrews of three species and 103 rodents of five species were trapped. Least shrews (n=l 10) comprised 46 percent of small mammals and 80 percent of shrews. Eastern harvest mice (n=62) were the most common rodents. Reproduction was detected only in pine voles and southern bog lemmings. The majority of small mammals of the region were trapped during this month-long study. INTRODUCTION As part of a study to determine the western extent of populations of the then federally threatened Dismal Swamp southeastern shrew, Sorex longirostris fisheri, I conducted a survey of small mammals in Isle of Wight County, located just west of the City of Suffolk and lying approximately 40 km west of the Great Dismal Swamp National Wildlife Refuge in eastern Virginia. Using a standard protocol to study the Dismal Swamp southeastern shrew, an assistant and I established 14 study grids at different locations throughout the county. Trapping between 6 January and 6 February 1 992, we collected 239 small mammals of eight species. This report relates the details of the types of small mammals, and their associations, in a coastal plain county in eastern Virginia. MATERIALS AND METHODS The southeastern shrew, the species of particular interest, is known to achieve greatest numbers in early successional habitats, such as oldfields, recently clearcut forests, and sites that are infrequently mowed (Rose et al. 1990). Powerline rights of way provide excellent habitat for such small mammals because they are mowed at 3-5 year intervals to prevent excessive growth of shrubs and trees, thereby continually setting back biological succession and promoting the persistence of perennial grasses and other herbaceous plants. Furthermore, because powerlines cross roadways, these habitats are easily reached, an additional benefit. Several high-voltage powerlines form a network across Isle of Wight County (Figure 1), many radiating from the Surry Nuclear power plant located on the south side of the James River. Thus, wherever county roads crossed the 30 m wide powerlines, I examined the vegetative stage of the habitat and usually was able to establish one or two study grids nearby. The trapping grids were placed on sites with vegetation that is typical of early succession in the region. Grasses, mostly in the genera Andropogon, Pdnicum, and Uniola, dominated the vegetation of most grids, but sedges {Car ex spp.) and even softrushes {Juncus spp.) were present on wetter places. Many grids had American cane {Arundinaria gigantea) and other woody elements, such as brambles {Rubus spp.), Japanese honeysuckle (Lonicera japonica), and tree seedlings, especially .of sweet gum 84 VIRGINIA JOURNAL OF SCIENCE FIGURE 1. Map of Isle of Wight County, Virginia, showing the state roads and powerlines relevant to this study. The study grids were placed near where powerlines crossed the state roads, at locations listed in Table 1. {Liquidambar styraciflud). The soils varied greatly among the 14 sites with grids, from sandy loams to silty clays, and occasional patches of black or peaty loams. The standard trapping protocol for our shrew studies used a 5 X 5 grid with 12.5 m intervals, covering an area of 0.25 ha. Near each coordinate, we dug a 1 5 cm diameter hole, deep enough to accommodate a 15 X 23 cm #10 tin can. When partly filled with water or formalin solution, these serve as efficient pitfall traps, a common method to ISLE OF WIGHT COUNTY SMALL MAMMALS 85 secure some species of small mammals, especially southeastern shrews, that are resistant to being trapped by live or snap traps. These pitfall traps were unbaited, because early studies demonstrated that baiting did not increase their efficiency (Hudson and Solf 1959). Once in place, we tended these traps twice a week to remove the bodies of small mammals that had fallen into the traps and drowned. (Drowning is considered to be a more humane method of kill-trapping than other methods, and we sought Sorex shrews whose body lengths we could measure). We trapped each grid for three weeks, and then removed all pitfalls from the ground. Earlier studies (Everton 1985) had indicated that little additional information is learned on the small mammals of a site if trapping continued beyond three weeks. Catch rates for pitfall traps tend to be very low, often on the order of 1 -2 captures per 1 00 nights that a trap is in the ground. Animals were frozen until they could be measured, weighed, and examined for reproductive status. At necropsy, each animal was weighed and then measured for total length and lengths of tail, ear, and hind foot. Each animal was examined for evidence of past or current reproduction (for females) or for current reproductive competency for males (the presence of convolutions in the cauda epididymides of the testes). All cataloged specimens were donated as skeletal material to the Mammal Division of the Smithsonian Institution in Washington, D. C. Because the field study was conducted in the dead of winter, I did not expect to see evidence of reproduction in most species. RESULTS In all, 239 small mammals of eight species were collected from the 14 grids in this study (Table 1). The number of specimens per grid ranged from 3-5 1 and the number of species per grid ranged from 2~6. Least shrews {Cryptotis parva) and eastern harvest mice {Reithrodontomys humuUs) were taken on 13 of 14 grids, whereas the white¬ footed mouse {Peromyscus leucopus) and pine vole (Microtus pinetorum) were least common, from one and two grids, respectively. The short-tailed shrew {Blarina brevicauda), from seven grids, and southeastern shrew (Sorex iongirostris), from six grids, also shared locations with least shrews on three grids. The microtine rodents, meadow voles (Microtus pennsylvanicus) and southern bog lemmings (Synaptomys cooperi), were present on seven and eight grids, respectively, and co-occurred on four grids. The 239 small mammals collected in this study were taken in 3,750 trap-nights (one trap in place for one night equals one trap-night), for an overall capture rate of 3 .25 small mammals per 100 trap-nights. The catch rates among grids ranged from 0.57 to 9.75/1 00 trap-nights (Table 1), indicating great variation in the densities of populations in the small mammal communities from location to location. There were no obvious vegetation or soil patterns that would account for this range of variation in small mammal abundance among the 14 grids. Information on the number of specimens, their standard measurements, and other details is presented in Table 2 for the six species with sufficient specim'ens to permit calculations of standard statistics. Sex ratios of all species did not differ significantly from 1:1, nor was there statistically significant sexual size dimorphism. The mean number of species taken per grid was 4.07 and the mean number of individuals per grid was 17.07, but there was no significant correlation between the number of species and TABLE 1. Results of pitfall trapping on 14 study grids in Isle of Wight County, Virginia. Grids were placed where state highways or other state roads intersected with high-voltage powerlines. Two grids were placed near state road 600, and three grids each were placed near state roads 621 and 626. “# sites” denotes to the number of sites yielding individuals of that species, “total N” refers to the total individuals of that species collected during the study, and “t-n” equals trap nights. 86 VIRGINIA JOURNAL OF SCIENCE 2^ 2 1 VO cj m ro Cv) O 7,000 bats of four species were found (Table 2). Most were M. lucifugus, and most were in Newberry-Bane (5 species) and Buddy Penley (4 species) caves. Only M. lucifugus and Pipistrellus subflavus (eastern pipistrelle) were found in Paul Penley and Coon caves. During winter, 12 caves were searched and 16,185 bats counted (Table 2); 89% {n = 14,479) were M. lucifugus. Newberry-Bane (6 species) and Buddy Penley (3 species) caves again contained the greatest number of bats. More bats were in Newberry-Bane (48% more than in autumn). Buddy Penley (197%), Paul Penley (107%) and Coon (285%) caves in winter than in autumn. About half the increase of bats in Newberry-Bane Cave and about a third of the increase in Buddy Penley Cave resulted from increases in areas surveyed in those caves. Paul Penley and Coon caves again had M. lucifugus and P. subflavus, and a single Myotis septentrionalis (northern myotis) was also found in Coon Cave. Munsey #1, Bane Spring, and Paul Penley caves had 100 - 1,000 bats. No bats were found in Munsey Twin #2. No endangered C. t. virginianus were found during autumn and winter cave surveys. Myotis sodalis was found only in Newberry-Bane Cave, with the exception of a single individual in Buddy Penley Cave on 23 November (Table 2). On 22 November, 26% of the population was in Lower Junction with 74% in Upper Junction. The temperature in both areas was >8.5°C. During winter, bats had changed location, abandoning Lower Junction entirely, and Upper Junction in large part, although temperatures in both areas had dropped (Table 3). Instead, 88% of the population was in a new area, the Bane Entrance Passage, at a temperature that was lower than either of the other two areas (Table 3). Like M sodalis, Myotis leibii (small-footed myotis) was found only in Newberry- Bane Cave (Table 2). In autumn, one individual was found in the Junction area (9°C), and in winter, seven M. leibii were found hibernating between the Bane Entrance Passage and the Junction area (5.7 - 6.8°C). No M. septentrionalis were found during the autumn survey, but 12 were found in winter, 9 in Newberry-Bane Cave, scattered throughout the survey area, most near 9°C. Autumn surveys located 9 Eptesicus fuscus (big brown bat) and winter surveys located 15 hibernating at a wide range of tempera¬ tures (1.2° - 13.3°C). The largest concentrations of M. lucifugus were found in Newberry-Bane and Buddy Penley caves during both autumn and winter (Table 2). Numbers of M. lucifugus in Newberry-Bane Cave increased by 45% {n = 1,725) between November and February, but bats were less concentrated in the North Subway. There were three times more bats in Buddy Penley Cave in winter than in autumn (Table 2), but about one-third were from an area not visited in autumn. Nevertheless, the number of bats TABLE 2. Bats found during autumn 1999 and winter 2000 visits to caves in the Sky dusky Hollow Cave System and nearby caves in the same karst system in Bland County, Virginia. Four caves were surveyed in autumn and 12 caves in winter; refers to sample size. 98 VIRGINIA JOURNAL OF SCIENCE I ^ Cl) lO ^ U- ' — I ^ in (N o o o© Os in ^ OS in r-- (N (N so os ^ (N OO (N os^ oo (N ^ ^ in so" (n" p o O so 00 oo in ^ oo p — ; in o in (N ^ p p (N p o in ^ ^ in o so so (N p o pinininpcNppp rdrdsd^cdoscnoo ^ ^ VO o in os U- r- o OO cn so in o CO in 00 (N OS SO r- so — < rt o o o OS o o o (N p r—< OO p p p p p OO p "O- in in '0- P rn rn oo ■O' o SO in Os os os oo in os os os Os in OO OS m OO o s; OS oo o (N Os Tt Tt m so (N 'xf in O so in m o rn Os . (U c ^ g ^ Z CQ D- b cd 3 C cd TO § OJ § ^ b S -S c ^ g ^ 3 ’> c« ^ S H H ^ CO CD (D (U 1> r-! w:i QO c« 3 (L> (— < )-H f— ( r-< C 8.0°C (Table 3). Spring staging and autumn swarming. — Trapping at the entrance to Buddy Penley Cave for 4 nights in April 2000 produced 101 bats of four species: 63 M lucifugus, 31 M septentrionalis, 6 P. subflavus, and 1 E. fuscus. Female M. lucifugus were six times more common than males, but there were nearly equal numbers of male and female M. septentrionalis. During autumn 200 1 , trapping on 4 nights at Newberry-Bane Cave, 885 bats of six species were processed: 27 M sodalis, 603 M lucifugus, 185 M septentrionalis, 6 M. leibii, 60 P. subflavus, and 4 E. fuscus. Proportions of M sodalis, M. lucifugus, and P. subflavus in the catch in autumn 200 1 were different than proportions observed in Newberry-Bane Cave during winter 2000 {X^ = 123.9; at P<0.001; df = 2). Myotis lucifugus was over represented in the winter survey and P. subflavus in the autumn survey. Myotis sodalis was similarly represented in samples from both seasons. In addition, M. septentrionalis was nearly absent from the winter survey (0.2%), exclud¬ ing it from the analysis, but it was common in autumn (20.9%). Catch of female M. sodalis, although small, was greater in mid-September than early September and early October, whereas captures of males, relative to females, increased through the samples (Figure la). Captures of female M. lucifugus remained relatively constant, but captures of males, relative to females, dropped dramatically over the autumn season (Figure lb). More male than female M. septentrionalis were caught early and late in the sample season and the absolute catch appeared to increase late in the season (Figure Ic). The pattern for P. subflavus similar to that of M. lucifugus (Figure Id). Myotis leibii were caught on 8 September (2 male and 2 female), 26 September (1 male), and 1 1 October (1 male). On 26 September, owQmdXQ E. fuscus was caught and on 1 1 October two males and one female were caught. Summer maternity colonies. — ^No large accumulation of guano that would indicate summer use was found during autumn and winter intra-cave surveys. There was a 100 VIRGINIA JOURNAL OF SCIENCE TABLE 3. Temperatures at which concentrations of three species of bats were found during autumn 1999 and winter 2000 surveys in caves of the Skydusky Hollow Cave System, Bland County, Virginia. Because not all bats were in areas of concentration, totals in this table do not necessarily match totals in Table 2. Species Survey Date Cave Location Bats Temp (“C) M. sodalis Autumn 22 Nov Newberry-Bane Lower Jet. 44 8.5 Upper Jet. 126 8.9 Winter 5 Feb Newberry-Bane Lower Jet 0 7.2 Upper Jet 29 8.7 Bane Ent. Passage 206 7.0 M. lucifugus Autumn 22 Nov Newberry-Bane N. Subway 3,778 9.0 -9.5 23 Nov Buddy Penley Pit 1 2,068 7.9 23 Nov Paul Penley Big Room 245 11.0 Whisper Hall 67 10.0 24 Nov Coon Main Passage 67 11.0 Big Room 245 11.0 Winter 17 Jan Coon Main Passage 28 9.1 Big Room 1,268 8.6 -9.7 19 Jan Bane Spring Front 383 7.4-8.3 Pit 59 9.8 3 Feb Newberry-Bane N. Subway 2,891 8.2-8.9 5 Feb Junction area 1,802 7.4 Junction area 255 8.7 4 Mar Buddy Penley Pit 1 4,280 6.3-6.5 Pit 375 7.4 Guano Climb 1,400 6.9 Attic 210 8.4 5 Mar Paul Penley Big Room 76 9.8 Whisper Hall 755 9.4 -9.8 P. subflavus Autumn 22 Nov Newberry-Bane all 31 9.0- 11.0 23 Nov Buddy Penley Entrance Passage 101 9.0 Paul Penley Whisper Hall 32 10.0 24 Nov Coon Main Passage 175 11.0 Big Room 90 11.0 Winter 17 Jan Coon Main Passage 451 7.4-8.2 Big Room 469 8.6 -9.7 19 Jan Bane Spring Front 41 7.4 -8.3 28 Jan Munsey #1 all 78 7.7 -8.4 3 - 4 Feb Newberry-Bane various 105 8.1 -9.3 5 Feb Junction area 29 7.4 4 Mar Buddy Penley all 160 6.5 - 7.4 5 Mar Paul Penley Whisper Hall 47 9.4- 10.2 BATS OF BLAND COUNTY VIRGINIA lOI (C) (d) FIGURE 1 . Captures of male (diamond) and female (closed circle) M. sodalis (a), M. lucifugus (b), M septentrionalis (c), and P. subjlavus (d) during autumn 2001 swarming. Note that numbers of bats are not to the same scale. moderate accumulation of guano in the Attic of Buddy Penley Cave. When visited on 3 1 May 2000, no bats were present and there was no new accumulation of guano. The temperature was about 10°C. DISCUSSION Spring staging and autumn swarming. — Proportions of species of bats captured in spring and autumn varied among populations hibernating in the same caves. The greatest disparity was seen with M septentrionalis, a species ofteiF caught at entrances to hibemacula in spring and autumn (Whitaker and Rissler 1992) but infrequently found during winter (Brack et al. 2003b, 2004). The change in capture of bats as autumn progressed indicated a social component in use of the cave. Although there were disproportionately large numbers of males of all species, M sodalis had the most dramatic shift in relative abundance of sexes during 102 VIRGINIA JOURNAL OF SCIENCE autumn. Male M. sodalis are more common during swarming than females because they congregate near hibemacula to mate with females that are arriving for hibernation; females terminate autumn activities and enter hibernation before males (Cope and Humphrey 1977; LaVal and LaVal 1980). Richter et al. (1993) found that small male M sodalis with insufficient fat reserves to survive the winter may remain active in hibemacula, possibly seeking an opportunity to copulate before dying. Male M lucifugus were much more abundant than females early in autumn, but numbers dropped precipitously over time, similar to patterns observed for this species at caves in Indiana (Humphrey and Cope 1976). Activity of P. subflavus declined earlier in autumn than for other species, perhaps signaling an earlier entry into hibernation. By contrast, activity of M. septentrional is seemed to rebound late in autumn, and perhaps is related to greater activity during winter (Whitaker and Rissler 1992). Winter hibernation. — Cave morphology strongly affects suitability for hibernation (Humphrey 1978) by affecting airflow and thus temperatures. Large complex systems offer more opportunities for the combination of characteristics needed to support hibernating bats. The Skydusky Hollow Cave System and its individual caves are complex and extensive (Zokaites 1995). Most species of bats make relatively charac¬ teristic and recognizable use of hibemacula, including temperature regimes and spatial associations (Brack et al. 2003b). In the caves of Skydusky Hollow, the locations within caves used by concentrations of bats often changed between seasons, similar to studies in Missouri (Myers 1964; Clawson et al. 1980) Hibernating M sodalis often form dense clusters in cool areas of hibemacula. Myotis sodalis did not use the traditional roost in the Bane Entrance Passage in autumn, but by winter had moved there, at 7°C, from the Upper and Lower Junction areas. About 1 2% of the population remained in Upper Junction at 8.7°C. These temperatures are not as cold as is often considered optimal for the species during mid-winter, i.e., 4 - 8°C, or perhaps more narrowly 3 - 6°C (USFWS 1 999). Further, cooler temperatures (6.3 - 6.5°C) were available at the bottom of Pit 1 in Buddy Penley Cave. Hall (1962) in the Midwest, Henshaw and Folk (1966) in Kentucky, and Humphrey (1978) in midwestem and eastern states, considered mid-winter temperatures used by M. sodalis to be 4 - 5°C, 2 - 3°C, and 4 - 8°C, respectively, but they did not provided supporting documentation. In contrast. Brack et al. (2003b) completed 25 years of studies in many of the caves addressed by Hall (1962) and Humphrey (1978) in Indiana, and they documented increasing populations of M. sodalis in these caves, hibernating in areas with mean mid-winter temperatures of 6 - 8°C. In Missouri, Myers (1964) found M sodalis hibernating at 4.4 - 16.7°C, but considered 7.8°C representative; mid-winter temperatures at clusters in three caves were 5.0 - 9.2°C (/7 = 6; X = 7. 1 ; SD = 1 .4). Also in Missouri, Clawson et al. (1980) found M. sodalis hibernating at 6 - 8°C in late January. Thus, temperatures used by M sodalis in Skydusky caves were similar to those reported in other studies. Myotis lucifugus uses many caves (Dalton 1987; Brack et al. 2003b) and small numbers often hibernate in warm areas, sometimes giving the impression that this species prefers the warmer temperatures that are available in caves for hibernation (Brack et al. 2003b, 2004). In Skydusky caves, the largest concentration ofM lucifugus {n = 4,280) hibernated at 6.5°C, at the bottom of Pit 1 in Buddy Penley in an area cooler than areas used by M sodalis. The remaining 6,300 M. lucifugus hibernated at BATS OF BLAND COUNTY VIRGINIA 103 temperatures similar to, or slightly less than, temperatures used by M sodalis. In a limestone mine in Ohio, M lucifugus similarly used cooler areas, which were also less thermally stable, than did M sodalis (Brack unpublished data). Pipistrellus subflavus is found hibernating in more caves than other species of bats, and it typically hibernates singly and dispersed at warm, stable temperatures (Hassell 1967; Brack et al. 2003b, 2004). As in other caves, P. subflavus hung singly or occasionally in pairs and used a stable, warm area, but the number of P. subflavus in Coon Cave was much greater than observed in most caves. The species arouses less frequently than other species (Brack and Twenty 1985; Twenty et al. 1985), which may offset the cost of hibernating at warmer temperatures. This species often collects beads of moisture on guard hairs, which increases the mass of individuals and it is an interesting question whether this water, suspended between the bat and its environment, may act as a heat sink, dampening fluctuations in air temperature. Little is known about M septentrionalis and M leibii during the season of hibernation. Myotis septentrionalis is readily caught at cave entrances in spring and autumn, providing indirect evidence of winter use (Whitaker and Rissler 1992), but is infrequently found in hibernation (Brack et al. 2003b). When found in winter, it is often deep in cracks or tight crevices in warm stable areas of the cave. Myotis leibii is believed to hibernate at cold temperatures (Best and Jennings 1997), an inference based on limited observation. Eptesicus fuscus, a common summer resident in western Virginia, was uncommon in these caves in winter. In natural hibemacula, it is considered a hearty species that hibernates near entrances where temperatures may get very cold (Brack and Twente 1985), and it moves among hibemacula during winter. However, E, fuscus commonly hibernates in walls of old brick houses (Whitaker and Gummer 1992), where tempera¬ tures are 3 - 20°C (X= 10°C). Intra-cave movements of bats during the season of hibernation are poorly docu¬ mented. Like Skydusky caves, Clawson et al. (1980) documented an increasing concentration of M sodalis in areas considered traditional hibemacula roosts between autumn and mid-winter. Similar to Skydusky, Hassell (1967) found that M sodalis hibernated in areas that got colder through the first half of the winter and warmer during the latter half of winter. Because M sodalis is listed as endangered, the occurrence of even a single individual has sometimes been used to identify a cave or mine as a hibemaculum. A single M sodalis was found in Buddy Penley Cave in autumn; none were present in winter. There are several similar occurrences in Indiana: (1) an individual M sodalis was in a cave one winter, and none were present the next (Brack et al. 2004), and (2) an M sodalis was netted at a cave entrance in autumn, but no M sodalis have been found during several winter surveys over a 25-year period (Brack et al. 2003b). In Ohio, a single M sodalis was caught at a mine portal, but four additional nights of sampling during two seasons did not produce additional M sodalis (Brack, unpublished data). These occurrences indicate that M sodalis, and likely oth^ species, visits caves and mines that are not used as hibemacula. Bats undoubtedly explore caves or parts of caves not suitable for hibernation, especially during the spring and autumn migration and transient periods. Although Hassell (1967) reported that M lucifugus occupied the same locations within caves throughout winter, we found that numbers and proportions of M lucifugus 104 VIRGINIA JOURNAL OF SCIENCE in specific regions of Newberry-Bane, Paul Penley, and Coon caves changed dramati¬ cally over the season of hibernation. It is probable there were also inter-cave move¬ ments; Whitaker and Rissler (1992) documented bats exiting and entering hibemacula throughout winter. The net result of these population shifts was to concentrate hibernating M. lucifugus in cooler areas of the cave. Similarly, there were large changes between autumn and winter in numbers and proportions of P. subflavus in parts of Coon Cave. It is probable that in addition to temperature, the social nature of bats affects the locations they used for hibernation. Raesly and Gates (1987) found that the presence of other bats, of all species, strongly influenced use of sites for hibernation. Summer maternity colonies. — ^No concentrations of bats were found in Skydusky caves during summer. The most likely candidate for summer use was C t. virginianus, although there are records of bachelor colonies of M. grisescens in Lee County Virginia (Webster et al. 1985). There was no large accumulation of guano indicative of past use, and there were no bats in the Attic of Buddy Penley Cave in late May, The Attic was cooler (10°C) than maternity roosts used by C t. virginianus in Kentucky (Lackie et al. 1994) and the closely related subspecies C. t. ingens (Ozark big-eared bat) in Oklahoma (Clark et al. 1996) at this time of year (12.8 - 16.3°C). Summary. ^ — ^The caves of Skydusky Hollow held >16,000 bats of 6 species in winter 2000, which is an important resource for the Commonwealth of Virginia and the region. Most (89%) were M lucifugus, although 9% were P. subflavus and 1% the federally endangered M sodalis. No endangered C. t. virginianus were found. Most bats were in two caves, Newberry-Bane (37%) and Buddy Penley (40%), including endangered M sodalis, although there was an unusually large concentration of P. subflavus (64% of this species and 6% of the total) in Coon Cave. Of the three most common species, the largest mid-winter concentration of M lucifugus was at the coldest temperature (6.3-6.5°C), M sodalis at a more moderate temperature (7.0°C), and P. subflavus at the warmest temperature (8.6-9.7°C). No concentration of bats used the caves during summer. Proportions of species captured in spring and autumn were not consistent with wintering populations, with the greatest disparity shown by M septentrionalis, a species often caught at hibemacula in spring and autumn but infrequently found in winter. Changes in proportions of males and females caught over autumn indicate a social function to autumn swarming. ACKNOWLEDGMENTS All authors contributed to field and reporting efforts. American Electric Power (AEP) and Virginia Department of Game and Inland Fisheries funded portions of these studies. Ron Poff (AEP) played a vital role in assuring completion of the studies. We thank landowners who allowed access to caves: Molly and Jerry Thompson, Robert Banes, Gene Harman, Billy Dilman, Joe Bane, Ellis Morehead, Bob Munsey. Many individuals participated in caving trips, and, without them, the surveys would not have been as safe or as successful: Bobby Zokaites, Joe Thompson, Steve Wells, Steve LePera, Brad Atkinson, Eileen O’Malley, Matt Burnett, Kirk Digby, Raymond Sira, Don Anderson, Walter Pirie, Michael Malsbum, Charlie Jones, and Terri Brown. The 1992 bat count was led by Ed Devine in Paul Penley, Jerry Redder in Buddy Penley, Barbara Graham in Bane Spring, Paul Kirchman in Spring Hollow, and Joe and Carol Zokaites and Jean Simonds in Newberry Bane. We thank Dean Metter and Gary Finni for inspiration. BATS OF BLAND COUNTY VIRGINIA 105 LITERATURE CITED Barbour, R. W. and W. H. Davis. 1969. Bats of America. University Press of Kentucky, Lexington. 286 pp. Best, T. L. and J. B. Jennings. 1997. Myotis leibii. Mammalian Species 547:1-6. Brack, V., Jr., R. K. Dunlap and S. A. Johnson. 2003a. Advantages of infrared thermometers for recording temperatures in caves. Bat Research News 44:62-63. Brack, V., Jr., S. A. Johnson and R. K. Dunlap. 2003b. Wintering populations of bats in Indiana, with emphasis on the endangered Indiana bat {Myotis sodalis). Pro¬ ceedings of the Indiana Academy of Science 1 12:61-74. Brack, V., Jr. and J. W. Twente. 1985. The duration of the period of hibernation in three species of vespertilionid bats I: field studies. Canadian Journal of Zoology 63:2952-2954. Brack, V., Jr., J. O. Whitaker, Jr. and S. Pruitt. 2004. Bats of Hoosier National Forest. Proceedings of the Indiana Academy of Science 1 13:76-86. Clark, B. K., B. S. Clark, D. M. Leslie, Jr. and M. S. Gregory. 1996. Characteristics of caves used by the endangered Ozark Big-eared bat. Wildlife Society Bulletin 24:8-14. Clawson, R. L., R. K. LaVal, M. L. LaVal and W. Caire. 1980. Clustering behavior of hibernating Myotis sodalis in Missouri. Journal of Mammalogy 61:245-253. Cope, J. B. and S. R. Humphrey. 1977. Spring and autumn swarming behavior in the Indiana bat, Myotis sodalis. Journal of Mammalogy 58:93-95. Dalton, V. M. 1987. Distribution, abundance, and status of bats hibernating in caves in Virginia. Virginia Journal of Science 38:369-379. Devine, E. 1995a. Buddy Penleys Cave. Pages 30-33 In C. Zokaites, ed. Under¬ ground in the Appalachians: A Guidebook for the 1995 National Speleological Society Convention. National Speleological Society Press, Huntsville, Alabama. Devine, E. 1995b. Paul Penleys Cave. Pages 35-39 In C. Zokaites, ed. Underground in the Appalachians: A Guidebook for the 1995 National Speleological Society Convention. National Speleological Society Press, Huntsville, Alabama. Fenton, M. B. 1969. Summer activity of Myotis lucifugus (Chiroptera: Vestertilioni- dae) at hibemacula in Ontario and Quebec. Canadian Journal of Zoology 47:597- 602. Hall, J. S. 1962. A life history and taxonomic study of the Indiana bat, Myotis sodalis. Reading Public Museum Publication 12:1-68. Hassell, M. D. 1967. Intra-cave activity of four species of bats hibernating in Kentucky. Ph.D. Dissert., Univ. Kentucky, Lexington. 62 pp. Henshaw, R. E. and G. E. Folk, Jr. 1966. Relation of thermoregulation to seasonally changing microclimate of two species of bats {Myotis lucifugus and M. sodalis). Physiological Zoology 39:223-236. Humphrey, S. R. 1978. Status, winter habitat, and management of the endangered Indiana bat, Myotis sodalis. Florida Scientist 41 :65-76. Humphrey, S. R. and J. B. Cope. 1976. Population ecology of the little brown bat, Myotis lucifugus, in Indiana and north-central Kentucky. American Society of Mammalogists Special Publications 4:1-81. Kurta, A., S. W. Murray and D. H. Miller. 2002. Roost selection and movements across the summer landscape. Pages 118-129/^ A. Kurta and J. Kennedy, eds. The 106 VIRGINIA JOURNAL OF SCIENCE Indiana Bat: Biology and Management of an Endangered Species. Bat Conserva¬ tion International, Austin, Texas. Lacki, M. J., M. D. Adam and L. G. Shoemaker. 1 994. Observations on seasonal cycle, population patterns and roost selection in summer colonies of Plecotus townsendii virginianus in Kentucky. American Midland Naturalist 131:34-42. LaVal, R. K. and M. L. LaVal. 1980. Ecological studies and management of Missouri bats, with emphasis on cave-dwelling species. Missouri Department of Conserva¬ tion Terrestrial Series 8:1-53. Myers, R. F. 1964. Ecology of three species of species of myotine bats in the Ozark Plateau. Ph.D. Dissert., Univ. Missouri, Columbia. 210 pp. Parsons, K. N., G. Jones, I. Davidson- Watts and F. Greenaway. 2003. Swarming of bats at underground sites in Britain — implications for conservation. Biological Conservation 1 1 1:63-70. Raesly, R. L. and J. E. Gates. 1987. Winter habitat selection by North American temperate cave bats, American Midland Naturalist 118:15-31. Richter, A. R., S. R. Humphrey, J. B. Cope and V. Brack, Jr. 1993. Modified cave entrances: thermal effect on body mass and resulting decline of endangered Indiana bats {Myotis sodalis). Conservation Biology 7:407-415. Thomas, D. W., M. B. Fenton and R. M. R. Barclay. 1979. Social behaviour of the little brown bat, Myotis lucifugus. I. Mating behaviour. Behavioural Ecology and Sociobiology 6:129-136. Twente, J. W., J. Twente and V. Brack, Jr. 1985. The duration of the period of hibernation of three species of vespertilionid bats II: laboratory studies. Canadian Journal of Zoology 63:2955-2961. USFWS (U.S. Fish and Wildlife Service). 1999. Agency draft Indiana bat {Myotis sodalis) revised recovery plan. Fort Snelling, Minnesota. 53 pp. Webster, W. D., J. F. Parbell and W. C. Biggs, Jr. 1985. Mammals of the Carolinas, Virginia, and Maryland. University of North Carolina Press, Chapel Hill. 255 pp. Whitaker, J. O., Jr. and S. L. Gummer. 1992. Hibernation of the big brown bat, Eptesiciis fuscus, in buildings. Journal of Mammalogy 73:3 12-316. Whitaker, J. O., Jr. and L. J. Rissler. 1992. Winter activity of bats at a mine entrance in Venuillion County, Indiana. American Midland Naturalist 127:52-59. Wright, W. 1995. Hydrology of the Sky dusky Hollow Cave System. Pages. 126-141 In C. Zokaites, ed. Underground in the Appalachians: A Guidebook for the 1995 National Speleological Society Convention. National Speleological Society Press, Huntsville, Alabama. Zokaites, C. 1995. Sky dusky Hollow Cave System. Pages 22-25 //? C. Zokaites, ed. Underground in the Appalachians: A Guidebook for the 1995 National Speleologi¬ cal Society Convention. National Speleological Society Press, Huntsville, Ala¬ bama. Zokaites, J. and C. Zokaites. 1995. Newberry-Banes Cave. Pages 34-35 In C. Zokaites, ed. Underground in the Appalachians: A Guidebook for the 1995 National Speleological Society Convention. National Speleological Society Press, Huntsville, Alabama. JEFFRESS AWARDS 107 JEFFRESS RESEARCH GRANT AWARDS The Allocations Committee of the Thomas F. and Kate Miller Jeffress Memorial Trust has announced the award of Jeffress Research Grants to the institutions listed below to support the research of the investigator whose name is given. The Jeffress Trust, established in 1981 under the will of Robert M. Jeffress, a business executive and philanthropist of Richmond, supports research in chemical, medical and other natural sciences through grants to non-profit research and educational institutions in the Commonwealth of Virginia. The Jeffress Research Grants being announced here have been awarded in 2003 . The Jeffress Memorial Trust is administered by Bank of America. Additional information about the program of the Trust may be obtained by writing to: Richard B. Brandt, Ph.D., Advisor, Thomas F. and Kate Miller Jeffress Memorial Trust, Bank of America, Private Bank, P. 0. Box 26688, Richmond, VA 23261-6688. An unofficial website is listed under Grants and Awards, www.vacadsci.org. William P. Anderson, Radford University. Collection of Water Level Data to Test New Methods for Estimating Recharge in Water-Table Aquifers. $10,000. (one year renewal). Todd D. Averett, The College of William and Mary. Neutron Spin Structure Studies Using High Density Polarized ^He Targets. $10,000. (one year renewal). Stephen F. Baron, Bridgewater College. Regulation ofExcellular Polyhydroxalkanoate Depolymerase Synthesis in Streptomyces spp.5A. $27,320. (one year). Deborah C. Bebout, The College of William and Mary. Investigation of Silica Sup¬ ported Copper Complexes as Biometrics of Micronuclear Monooxygenases. $10,000. (one year renewal). John J. Beck, Sweet Briar College. Structure-Activity Relationships of Aromatic Analogs of (Z)-Ligustilide: A Natural Product from Ligusticum Species. $10,000. (one year renewal). Matthew J. Beckman, Virginia Commonwealth University/Medical College of Vir¬ ginia. Arthritis and the Importance of Ets-2 in Urokinase-Plasminogen Activator Expression. $10,000. (one year renewal). Wade E. Bell, Virginia Military Institute. The Role of Calcium in Paramecium Chemoresponse: Elucidation of Mechanisms for Calcium Influx. $10,000. (one year renewal). Mark P. Birkenbach, Eastern Virginia Medical School. Characterization of Interleukin- 27 Function in Immune Response to Murine Cytomegalovirus (MCMV). $20,000. (one year). Robert A. Bloodgood, University of Virginia School of Medicine. Calciurn Regulation of Whole Cell Locomotion. $10,000. (one year renewal). Timothy Bos, Eastern Virginia Medical School. Regulation of Breast Cancer Gene Targets by the AP-1 Transcription Factor. $10,000. (one year renewal). Karen J. Brewer, Virginia Polytechnic Institute and State University.. Binding Metal Centers to Photochemically Active Metal Sites. $10,000. (one year renewal). Stephen G. Cessna, Eastern Mennonite University. Reactive Oxygen Production During Salinity Tolerance Responses in Tobacco Cells: Relationship to Cytosolic Ca^~ Fluxes. $10,000. (one year renewal). 108 VIRGINIA JOURNAL OF SCIENCE Jennifer A. Clevinger, James Madison University. Phylogenetic Analysis of [Sil- phium} and [Berandiera] (Asteraceae) Using DNA Sequence data. $10,000. (one year renewal). Stuart C. Clough, University of Richmond. The Preparation and Application of 5-chioro-5-ary!-2, 4-pentadienoates to the Regioselective Synthesis of Heterocy¬ cles and Carbocycles. $20,000. (one year). Gary G. Cote, Radford University. 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