Ecology and Virulence o f Legionnaire's Disease Bacteri a in Aquatic Habitats Near Mt . St . Helen s by David L . Tiso n Ramon J . Seidle r Water Resources Research Institut e Oregon State Universit y Corvallis, Orego n WRRI-84 September 1983 ECOLOGY AND VIRULENCE OF LEGIONNAIR E ' S DISEASE BACTERI A IN AQUATIC HABITATS NEAR MT . ST . HELEN S by David L . Tison and Ramon J . Seidle r Department of Microbiology, Oregon State Universit y Final Technical Completion Repor t for Project No . A-060-OR E to United States Department of the Interio r Washington, D .C . 2024 0 Project Sponsored by : Water Resources Research Institut e Oregon State Universit y Corvallis, Oregon 9733 1 The research upon which this report is based was financed in part by th e U .S . Department of the Interior, Washington, D .C . (Project No . A-060-ORE) , as authorized by the Water Research and Development Act of 1978, P .L . 95-467 . Contents of this publication do not necessarily reflect the views an d policies of the U .S . Department of the Interior, nor does mention of trad e names or commercial products constitute their endorsement or recommendatio n for use by the United States Government . WRRI-84 September 1983 ABSTRACT Illnesses among researchers exposed to lakes and streams i n the Mt . St . Helens blast zone after the 18 May 1980 eruptio n prompted us to determine the occurrence and potential virulenc e of Legionella (Legionnaire's disease bacteria) in aquati c habitats near Mt . St . Helens during the summers of 198 . 1 and 1982 . Concentrations of L . pneumophila, L . nnicdadei, L . g©rmanii, L . dumoffii, and L . bozemanii, determined by microscopic count s using direct immunofluorescent staining, ranged from <l0 4 to 10' cells/L in lakes and rivers outside of the Mt . St . Helens blas t zone while the numbers of Legionella in aquatic habitats insid e the blast zone were from 10 5 to 10 7 cells/L . Legionella number s were consistently highest in N . Coldwater and Spirit lakes, whic h received water from hydrothermal seeps . Legionella pneumophil a serogroups 4 and 6 were isolated from N . Coldwater Lake in 198 1 and from S . Coldwater Creek in 1982, indicating that th e potentially virulent strains of Legionella persist in aquati c habitats in the blast zone of Mt . St . Helens . FOREWORD The Water Resources Research Institute, located on the Orego n State University campus, serves the State of Oregon . Th e Institute fosters, encourages and facilitates water resource s research and education involving all aspects of the quality an d quantity of water available for beneficial use . The Institute administers and coordinates statewide and regional programs o f multidisciplinary research in water and related land resources . The Institute provides a necessary communications an d coordination link between the agencies of local, state an d federal government, as well as the private sector, and the broa d research community at universities in the state on matters o f water-related research . The Institute also coordinates th e inter-disciplinary program of graduate education in wate r resources at Oregon State University . It is Institute policy to make available the results o f significant water-related research conducted in Oregon' s universities and colleges . The Institute neither endorses no r rejects the findings of the authors of such research . It doe s recommend careful consideration of the accumulated facts by thos e concerned with the solution of water-related problems . ACKNOWLEDGEMENT S We thank Cliff Dahm (Oregon State University) and Jim Bedel l (U .S . Forest Service) for assistance in coordinating sampl e collection and for helpful discussions . The U .S .. Forest Servic e is thanked for providing helicopter time . Financial support wa s provided by the Oregon State University Department of Laborator y Animal Resources and the U .S . Department of the Interior, Offic e of Water Policy, through the Water Resources Research Institut e at Oregon State University . 11 TABLE OF CONTENTS Pag e INTRODUCTION 1 MATERIALS AND METHODS 3 RESULTS 7 DISCUSSION 9 REFERENCES 11 LIST OF FIGURES Page Figure 1 . Mt . St . Helens and vicinity, showing river s and lakes affected by May 18, 1980 eruption 4 Figure 2 . Diagrammatic representation of a sample are a in the S . Coldwater Creek drainage area Figure 3 . 5 A portion of the S . Coldwater Creek drainag e area illustrated in Figure 2 6 LIST OF TABLE S Table 1 . Numbers of cells per liter reacting wit h serogroup specific fluorescent antibod y conjugates to Legionella spp iv 7 INTRODUCTION The eruption of Mt . St . Helens on May 18, 1980 reshape d nearby pre-existing lakes and streams, created new lakes as a result of damming of drainages by debris flows, and produce d numerous hydrothermal seeps . Tremendous quantities of pyrolize .d organic matter from the destroyed forest and inorganic nutrient s from the ash and pyroclastics were added to previousl y oligotrophic sub-alpine lakes typical of those in the Cascad e Range in the Pacific Northwest U . S . These aquatic environment s progressed from oligotrophic to hypereutrophic in a matter o f days ; undisturbed, this progression would have taken centuries . Because of the proximity of academic research institutions t o these unique environments, characterization of the chemical an d biological properties of thes e ' habitats was initiated soon afte r the May 18, 1980 eruption (1, 7, 9) . Research personnel exposed to aquatic environments in the Mt . St . Helens blast zone reported illnesses with "flu-like" symptom s throughout the summer of 1980 and again early in the spring o f 1981 . The similarity of the reported symptoms to . the "Pontia c Fever" syndrome cause by Legionella'pneumophila and the nature o f the aquatic environments produced by the cataclysmic eruption o f Mt . St . Helens prompted us to initiate a study to determine th e density and distribution of Legionella spp. (the etiologic agent s of Legionnaires'• Disease and Pontiac Fever) in the blast zone o f Mt . St . Helens . MATERIALS AND METHOD S The degree of impact by the May 18, 1980 eruption on lake s and streams in the Mt . St . Helens blast zone is shown in Figur e 1 . Sites sampled included spirit Lake, North Coldwater an d Castle creeks, which are in the scorch zone, and Ryan Lake, whic h is in the blowdown zone . South Coldwater Creek and hydrotherma l seeps in the South Coldwater drainage area and sites outside o f the blast zone including McBride Lake, Silver Lake (not shown ) and the Muddy and North Toutle rivers were also sampled . Figure s 2 and 3 illustrate the nature of the South Coldwater Cree k drainage area . The physical, chemical and biological characteristics o f these sites have been described previously (1, 7, 9) . In general, lakes in the blast zone were high in dissolved organi c carbon (DOC), nitrogen-limited, and dominated by heterotrophi c and metal oxidizing bacteria with total direct microscopic count s ranging from 10 6 to 1Q 8 bacteria per ml (1, . .7, 9) . One-to-four ]n iters of water were colleeted, concemtr-ate ;d by membrane filtration (6), and examined microscopically usin g direct immnn, 0fluorescence (3) . Cells reacting with fluorescen t antibody conjugates (Biological Products Section, , .enters fo r Disease Control) specific for L . pneumophila ser®groups micdadei, L . gormanii, L . dumoffii, and L . bozemanii wer e quantitated . The virulence of presumptive Legionella was assessed by guinea pig innoculation (5) . L, Figure 1 . Mt . St . Helens and vicinity, showing rivers and lake s affected by May 18, 1980 eruption . 4 U CUO O)N a) r 4-) ( 4 ) S- O -o -0 (a a) 4-+-) CU 0 4• CU U i r a) L +) a ) a) ~ t 4-) 3 -N Cd 3'~ C -Cl a) 0 r C O•r b C)Cda) 4) 4-) • C C d N 0 S U +) W N = -4-) d- r Or C C •r N b RESULT S Concentrations of Legionella species from the most intensively sampled sites are presented in Table 1 . The numbers of Legionella spp . in Ryan and Castle Creek lakes are of the sam e order of magnitude as those found for L . pneumophila in a survey of a number of lakes and rivers in the southeastern United State s (4) . Concentrations of Legionella spp . in North Coldwater an d Spirit lakes were consistently high (10 6 to 107 cells/L) whe n compared to lakes outside of the blast zone (Table 1) . These data may be attributed to the high concentrations of DOC an d available metals in these lakes . Although the concentrations o f Legionella spp . were particularly high in North Coldwater an d Spirit lakes, the percentage of the total bacterial populatio n these bacteria comprised (0 .1% to 1%) was not unusual whe n compared to other aquatic habitats (4) . The enrichment of thes e aquatic environments with DOC from pyrolysis of the productiv e coniferous forest and inputs of inorganic nutrients from the as h and pyroclastics have enriched for not only Legionella but the total bacterial population as well . Legionella pneumophila serogroups 4 and 6 were isolated o n BCYE agar inoculated with the liver, spleen and peritoneal flui d at necropsy from animals inoculated with concentrated water fro m North Coldwater Lake collected on April 30, 1981 and from Sout h Coldwater Creek collected on June 15, 19 .82 .. 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(0 (Cl N Z t o 8 DISCUSSION The concentrations of Legionella spp . in hydrothermal seep s in the South Coldwater Creek drainage particularly emphasize th e enrichment potential of aquatic niches in this area . Therma l seeps eminating from the mud flow ranged in temperature from 7 50 C to ambient (18 0 C) . Dissolved organic carbon concentration s ranged from about 700 to 900 mg C/L in seeps having temperature s above 65 0 C while concentrations in thermal seeps wit h temperatures from 40 to 60 0 C were about 250 mg C/L (C . Dahm , pers . comm .) . Microbial communities similar to those in natura l thermal springs (2) and man-made thermal habitats (8) wer e observed . At temperatures above 40 0C these communities wer e comprised mainly of the cyanobacteria .Phormidium.sp ., and to a lesser extent, Oscillitoria sp ., and associate d non-photosynthetic bacteria . Concentrations of Legionella spp . ranged from 105 to 10 7 DFA positive cells per cm . It i s interesting to note that those lakes in the Mt . St . Helens blas t zone found to harbor the highest densities of Legionella, North Coldwater and Spirit, were the only lakes receiving waters fro m thermal seeps . These observations suggest that enriched therma l waters which foster microbial communities with hig h concentrations of biomass may act as source of Legionella wher e these bacteria may proliferate during favorable seasona l conditions in non-thermal waters such as Spirit and Nort h Coldwater lakes . 9 Legionella species were observed in rivers and lakes in th e Mt . St . Helens blast zone in concentrations similar to thos e found in other aquatic habitats outside of the blast zone excep t at hydrothermal seeps in the South Coldwater Creek drainage , North Coldwater Lake and Spirit Lake . The concentrations o f Legionella in those warmer waters were consistently one to tw o orders of magnitude higher than those found elsewhere . Virulent strains of L . pneumophila were isolated during both season s sampled ; however, illnesses among workers exposed to aquati c habitats in the Mt . St . Helens blast zone were not confirmed a s legionnellosis . The high concentrations of Legionella in water s in the blast zone (10 7 cells/L) are diluted significantly a s these waters flow to populated areas, as shown by the low number s found in the North Toutle River (10 4 cells/L) outside of th e blast zone . 10 REFERENCE S 1. Baross, J .A., C .N . Dahm, A .R . Ward, M .D . ',they, and J . R . Sedell . 1982 . Initial microbiological respons e in lakes to the Mt . St . Helens eruption . Nature . 296 : 49-52 . 2. Brock, T .D . 1978 . Thermophilic Microorganisms an d Life at High Temperatures . Springer-Verlag, New York . 3. Cherry, W .B ., B . Pittman, P .P . Harris, G .A . Hebert , B .M . Thomason, L . Thacker, and R .E . Weaver . 1978 . Detection of Legionnaires' disease bacteria by direc t immunofluorescent staining . J . Clin . Microbiol . 8 : 329-338 . 4. Fliermans, C .B ., W .B . Cherry, L .H . Orrison, S .J . Smith , D .L . Tison, and D .H . Pope . 1981 Ecological distributio n of Legionella pneumophila . Appl . Environm . Microbiol . 41 : 9-16 . 5. McDade, J .E . 1979 . Primary isolation using guinea pig s and embyonated eggs . In : G .L . Jones and G .A . Hebert, eds . "Legionnaires" the disease, the bacterium and methodology . U .S . Dept . of Health, Education and Welfare, Centers for Disease Control, Atlanta, Ga . 6. Orrison, L .H ., W .B . Cherry, C .B . Fliermans, S .B . Dees , L .K . McDougal and D .J . Dodd . 1981 . Characteristics of environmental isolates of Leqionella pneumophila . Appl . Environm . Microbial . 42 : 109-115 . 7. Staley, J .T ., L .G . Lehmicke, F .E . Palmer, R .W . Peet, and R .C . Wissmar . 1982 . Impact of Mt . St . Helens eruptio n on bacteriology of lakes in the blast zone . Appl . Environm . Microbial . 43 : 664-670 . 8. Tison, D .L ., D .H . Pope, W .B . Cherry and C .B . Fliermans . 1980 . Growth of Leqionella pneumophila in associatio n with blue-green algae (cyanobacteria) . Appl .. Environm . Microbial . 39 : 456-459 . 9. Wissman, R .C ., A .H . Devol, J .T . Staley, and J .R . Sedell . 1982 . Biological responses of lakes within the Moun t St . Helens blast zone . Science . 216 : 175-181 . "1I