Widespread Distribution and Probable Origin of Resistance to Metalaxyl in Clonal Genotypes ofPhytophthora infestansin the United States and Western Canada

1996 ◽  
Vol 86 (7) ◽  
pp. 793 ◽  
Author(s):  
Stephen Goodwin
Plant Disease ◽  
2011 ◽  
Vol 95 (7) ◽  
pp. 873-873 ◽  
Author(s):  
L. M. Kawchuk ◽  
R. J. Howard ◽  
R. D. Peters ◽  
K. I. Al-Mughrabi

Late blight is caused by the oomycete Phytophthora infestans (Mont.) de Bary and is one of the most devastating diseases of potato and tomato. Late blight occurs in all major potato- and tomato-growing regions of Canada. Its incidence in North America increased during 2009 and 2010 (2). Foliar disease symptoms appeared earlier than usual (June rather than July) and coincided with the identification of several new P. infestans genotypes in the United States, each with unique characteristics. Prior to 2007, isolates collected from potato and tomato crops were mainly US8 or US11 genotypes (1). However, P. infestans populations in the United States have recently experienced a major genetic evolution, producing isolates with unique genotypes and epidemiological characteristics in Florida and throughout the northeastern states (2). Recent discoveries of tomato transplants with late blight for sale at Canadian retail outlets prompted an examination of the genotypes inadvertently being distributed and causing disease in commercial production areas in Canada. Analysis of isolates of P. infestans from across Canada in 2010 identified the US23 genotype for the first time from each of the four western provinces (Manitoba, Saskatchewan, Alberta, and British Columbia) but not from eastern Canada. Allozyme banding patterns at the glucose phosphate isomerase (Gpi) locus indicated a 100/100 profile consistent with US6 and US23 genotypes (4). Mating type assays confirmed the isolates to be A1 and in vivo metalaxyl sensitivity was observed. Restriction fragment length polymorphic analysis of 50 isolates from western Canada with the multilocus RG57 sequence and EcoRI produced the DNA pattern 1, 2, 5, 6, 10, 13, 14, 17, 20, 21, 24, 24a, 25 that was indicative of US23 (3). The recently described P. infestans genotype US23 appears to be more aggressive on tomato, and although isolates were recovered from both tomato and potato, disease symptoms were often more severe on tomato. Results indicate that movement and evolution of new P. infestans genotypes have contributed to the increased incidence of late blight and that movement of the pathogen on retail plantlets nationally and internationally may provide an additional early season source of inoculum. A major concern is that the introduced new A1 populations in western Canada have established a dichotomy with the endogenous A2 populations in eastern Canada, increasing the potential for sexual recombination producing oospores and additional genotypes should these populations merge. References: (1) Q. Chen et al. Am. J. Potato Res. 80:9, 2003. (2) K. Deahl. (Abstr.) Phytopathology 100(suppl.):S161, 2010. (3) S. B. Goodwin et al. Curr. Genet. 22:107, 1992. (4) S. B. Goodwin et al. Phytopathology 88:939, 2004.


1997 ◽  
Vol 129 (4) ◽  
pp. 733-743 ◽  
Author(s):  
Gordon Pritchard ◽  
Andrea Kortello

AbstractAlthough Amphiagrion abbreviatum (Selys) and Argia vivida Hagen often occur at the same geothermally heated springs in western Canada and the United States, they differ markedly in their abundance at any particular site. There is no relationship between crude data on water temperature, conductivity, or aquatic vegetation and the relative abundance of the two species, but there is a striking correlation with presence or absence of trees. The absence of A. abbreviatum from heavily treed areas is associated with the paucity of suitable daytime perching sites, and there may be competitive pressure exerted by A. vivida for the perching sites that are available. Argia vivida does not live at open sites because it requires trees for night-time roosts. Argia vivida roosted higher than A. abbreviatum in cages and held the body at a greater angle from the cage wall. The roosting posture of A. vivida is probably related to interception of solar radiation in the morning, and the body positions of both species possibly provide defence against predation.


Author(s):  
Arnold L. Rivera ◽  
Darren C. Day

Enbridge Inc. operates the world’s longest crude oil and refined liquids pipeline system. The company owns and operates Enbridge Pipelines Inc. (the Canadian portion of the Enbridge crude oil mainline) and a variety of affiliated pipelines in Canada and the United States. It also has approximately, a 12% interest in Enbridge Energy Partners, L.P. which owns the Lakehead Pipeline System in the United States. These pipeline systems have operated for over 50 years and now comprise approximately 15,000 kilometers (9,000 miles) of pipeline, delivering more than 2.2 million barrels per day of crude oil and refined liquids. The combination of the Enbridge System in Canada and the Lakehead System in the United States brings together the primary transporter of crude oil from Canada into the United States. It is also the only pipeline that transports crude oil from Western Canada to Eastern North America, serving all of the major refining centres in the province of Ontario as well as the Great Lakes region of the United States. The system consists of approximately 9000 kilometers (5,600 miles) of mainline pipe in Canada, and 5300 kilometers (3,300 miles) of mainline pipe in the United States. The Canadian portion of the pipeline system extends from Edmonton, Alberta as the primary initiating facility, across the Canadian prairies to the U.S. border near Gretna, Manitoba. It continues again from the U.S. border near Sarnia, Ontario, to Toronto, Ontario, and Montreal, Quebec, with lateral lines to Nanticoke, Ontario, and Niagara Falls, Ontario. The total length of the pipeline right-of-way is nearly 2300 kilometers (1,400 miles).


2018 ◽  
Vol 68 (2) ◽  
pp. 188-195 ◽  
Author(s):  
Ilan S Schwartz ◽  
Nathan P Wiederhold ◽  
Kimberly E Hanson ◽  
Thomas F Patterson ◽  
Lynne Sigler

1982 ◽  
Vol 60 (4) ◽  
pp. 364-368
Author(s):  
Orson K. Miller Jr. ◽  
W. Blain Askew

Calvatia defodiodis Lloyd (Disciseda defodiodis (Lloyd) Zeller) has been found to be conspecific with Gastrosporium simplex Matt. Previously known only from Europe, G. simplex is reported from western Canada and the United States. Distinctive features are the low warted surface of the spores, distinctive calcium deposits in the exoperidium, a gelatinized endoperidium, and a paracapillitium with clamp connections. Information on its known range in North America, microhabitats in which it grows, and its relationship to other Gasteromycetes is presented.


2016 ◽  
Vol 571 ◽  
pp. 342-354 ◽  
Author(s):  
Jesse M. Lepak ◽  
Mevin B. Hooten ◽  
Collin A. Eagles-Smith ◽  
Michael T. Tate ◽  
Michelle A. Lutz ◽  
...  

1978 ◽  
Vol 15 (8) ◽  
pp. 1250-1271 ◽  
Author(s):  
David W. Krause

Plesiadapiform primates have been recovered from seven Paleocene sites in western Canada: (1) Roche Percée (Ravenscrag Formation) — Carpodaptes cygneus, Plesiadapis churchilli, Ignacius frugivorus, Micromomys vossae, n. sp.; (2) Police Point (Ravenscrag Formation) — Carpodaptes cf. cygneus, Plesiadapis sp., Ignacius sp.; (3) Calgary site 2E (Porcupine Hills Formation) — Microsyopinae incertae sedis; (4) Cochrane site 11 (Porcupine Hills Formation) — Elphidotarsius russelli, n. sp., Pronothodectes? sp., Paromomys cf. depressidens, Picrodus silberlingi; (5) Erickson's Landing (Paskapoo Formation) — Plesiadapis rex; (6) Canyon Ski Quarry (Paskapoo Formation) — Carpodaptes cygneus; and (7) Swan Hills site 1 (Paskapoo Formation) — Carpodaptes cygneus, Plesiadapis sp.The primate evidence now available from western Canada permits biostratigraphic correlation with Paleocene sites in the western interior of the United States. The Roche Percée, Canyon Ski Quarry, and Swan Hills sites are accorded a late (but not latest) Tiffanian age. Police Point appears to be slightly older and is assigned to the middle Tiffanian, as is Erickson's Landing. A late Torrejonian age is tentatively given Cochrane site 11. The single primate tooth from Calgary site 2E provisionally suggests a Torrejonian age.The evidence from fossil mammals, primarily primates, suggests that the local faunas from sites in the Alberta Foothills (Cochrane and Calgary) are considerably older than those from the Plains (Erickson's Landing and Canyon Ski Quarry). This does not accord with earlier lithostratigraphic studies, which suggest the reverse should be the case.


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