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D. Magyar* and K. Manninger Department of Plant Pathology, Plant Protection Institute
of Hungarian Academy of Science, Herman Ottó u. 15, H-1022, Budapest,
Hungary. * Correspondence author: Email: magyard@freemail.hu Accepted for publication: 29 October 2004 Citation: Cereal Rusts and Powdery Mildews Bulletin [www.crpmb.org/] 2004/1029magyar Note: This paper was presented at the International Cereal Rusts and Powdery Mildews Conference, John Innes Centre, Norwich, UK, 22-27 August 2004 Abstract Introduction The importance of aeromycological monitoring of plant
pathogenic spores has been recognised after the great epidemics in North
America caused by rusts in 1920' (Stakman & Christensen, 1946). Thereafter
other trajectories have been revealed, e.g. in India (Nagarajan & Singh,
1976) between Paraguay and Argentina (Waller, 1979), from Angola to Brazil
(Bowden et al., 1971), across the Tasman Sea from Australia to
New Zealand (Viljanen-Rollinson & Cromey, 2002). Our knowledge about
airborne spore pathway between South and Central Europe is insufficient
(Brown & Hovmøller, 2002). The aim is our study to complete information
of rust spore aeromycolgy in this critical geographical area. Materials and Methods Hirst-type air samplers (Hirst, 1952) were used to register
the daily concentration of airborne spores. The samples were located
in a traditional vineyard in Umbria country of Central Italy, in 1994,
1995 and 1996, between May and July. (in Brufa between 27 May and 13
June 1994; in Brufa between 05 June and 03 July 1995; in Brufa between
13 June and 24 June 1996; in Casalina between 13 June and 27 June
1991; in Ormelle between 03 June and 23 June 1996; in Torgiano between
24 May and 05 July 1993). The spore trap were placed in an instrumented
tower at height of 30 m above ground level. For microscopical work we
used 400X object lens of DIALUX 20 microscope. Two longitudinal transverses
along the length of the silicone-coated slide were scanned to determine
spore concentration of the air samples, concentration was expressed in
spore/m3. The measured meteorological factors were: wind speed [m/s],
wind direction, atmospheric pressure [Pa], minimum, maximum and mean temperatures
- [Co], precipitation [mm], rainfall intensity [mm/s], duration of precipitation
[min], cloud cover [%], relative humidity [%], presence of fog and mist,
dew point [Co], evaporation [mm], number of sun hours [min]. The Spearman's
Correlation Analysis was applied to clear the relations between changes
of daily airborne spore concentration and the meteorological factors. Results Hyaline uredospores of Cronartium / Melampsora/ Melampsoridium spp. were frequent in air samples. Concentration increased by solar radiation, minimum temperature, dew point, evaporation and long drought periods. Large amounts of spores were measured when the number of sun hours appeared to be high on the 2nd and 3rd day before capturing (Sd-2, Sd-3). Precipitation on the 3rd and 4th day before observation (Pd-3, Pd-4) caused high concentration. Wind gusts (50-80 km/h) and air currents from North-East in Brufa, and from South in Torgiano had strong positive effects. Spore concentration has been reduced by cloud cover. High relative humidity on the 1st and 2nd day before observation (RHd-1, RHd-2) decreased counts. Uredospore counts of Puccinia spp. correlated positively with temperature, number of sun hours, evaporation and solar radiation. High relative humidity, RHd-1, RHd-2, fog, number of rainy days, duration of precipitation had negative effect on the spore concentration. Rainstorms with strong winds removed the airspora efficiently. The presence of airborne sand particles showed positive correlation with the uredospore counts. Puccinia teliospores were observed rarely in the
monitored period. Sudden change of wind direction and wind gusts caused
spore release. Phragmidium teliospore were detected only once
when wind blown from South-East. The results of statistical analysis are
summarized in Table 1. Discussion As many author noticed, wind is probably the most important factor in the spore release of Uredinales (Carter et al., 1970; Hirst, 1961; Smith, 1966; Sache, 2000). Wind gusts are effective as well (Sache, 2000). However, spore free winds should reduce spore concentration by dilution or blow-off (Hamilton, 1959). Vourinen and Helander (1995) observed the positive effect of wind speed and temperature on the spore dissemination of Melampsoridium betulinum (Fries) Kleb. Our results suggest, that previously deposited teliospores of Puccinia, or large teliospores of Phragmidium should become airborne by excessive winds. In our results relative humidity has been proved more effective than precipitation. In saturated air deposition rate of spores increased because they are heavier (Weinhold, 1955) and larger (Madelin & Johnson, 1992). Wetted surfaces acts as natural spore traps as well, thereby reducing the number of airborne spores. The positive effect of temperature and light intensity (Smith, 1966: P. graminis Pers var. tritici Eriks. & E. Henn.) should correlate with favourable wind dissemination. Dry liberation by rain droplets (the so called 'tap and puff' mechanism) mentioned as well as splash dispersal of spores (Geagea et al., 1999; P. recondita f.sp. tritici C.O. Johnson; P. striiformis Westend, Nutman et al., 1960; Bock, 1962; Hemileia vastatrix Berk. & Br., Hirst, 1961; P. graminis Pers, Carter et al., 1970; Tranzschelia discolor (Fckl.) Tranz. & Litv.). In our results there were no direct positive effects of rain. Washing- off the spores from the air in longer rains (Hamilton, 1959; Puccinia spp.) or in intensive rainstorms (Sache, 2000) has been proved again. Acknowledgemets The authors are grateful to professor Giuseppe Frenguelli, Emma Bricchi and Emma Tedeschini from the University of Perugia. This work was supported by a grant from the Hungarian Grant Committee (MÖB). References Bock KR, 1962. Dispersal of uredospores of Hemileia vastatrix under field conditions. Transactions of the British Mycological Society 45, 63-74. Bowden J, Gregory PH, Johnson CG, 1971.Possible wind transport
of coffee leaf Brown JKM, Hovmøller MS, 2002. Aerial dispersal of pathogens on the global and continental scales and its impact on plant disease. Science 297, 537-541. Carter MV, Moller WJ, Pady SM, 1970. Factors affecting uredospore production and dispersal in Tranzschelielia discolor. Australian Journal of Agricultural Research 21, 905-914. Geagea L, Huber L, Sache I, 1999. Dry-dispersal and rain-splash of brown (Puccinia recondita f.sp. tritici) and yelow (P. striiformis) rust spores from infected wheat leaves exposed to simulated raindrops. Plant Pathology 48, 472-482. Hamilton ED, 1959. Studies on the air spora. Acta Allergologica 13, 143-175. Hirst JM, 1952. An automatic volumetric spore trap. Annals of Applied Biology 39, 257-265. Hirst JM, 1961. The aerobiology of Puccinia graminis uredospores. Transactions of the British Mycological Society. 44, 138-139. Madelin TM, Johnson HE, 1992. Fungal and actinomycete spore aerosols measured at different humidities with an aerodynamic particle sizer. Journal of Applied Bacteriology 72, 400-409. Nagarajan S, Singh H, 1976. Preliminary studies on forecesting wheat stem rust appearance. Agricultural Meteorology 17, 281-289. Nutman FJ, Roberts FM and Bock KR, 1960. Method of uredospore dispersal of the coffee leaf-rust fungus, Hemileia vastatrix. Transactions of the British Mycological Society 43, 509-515. Sache I, 2000. Short-distance dispersal of wheat rust spores by wind and rain. Agronomie 20, 757-767. Smith RS, 1966. The liberation of cereal stem rust uredospores
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