Rapidly changing climatic conditions for wine grape growing in the Okanagan Valley region of British Columbia, Canada

2016 ◽  
Vol 556 ◽  
pp. 169-178 ◽  
Author(s):  
Sierra Rayne ◽  
Kaya Forest
Keyword(s):  
British Columbia ◽  
Climatic Conditions ◽  
Wine Grape ◽  
Okanagan Valley

Monitoring of Drosophila suzukii (Diptera: Drosophilidae) in Okanagan Valley vineyards, British Columbia, Canada, and assessment of damage to table and wine grapes (Vitaceae)

2020 ◽  
Vol 152 (4) ◽  
pp. 415-431
Author(s):  
Susanna Acheampong ◽  
Etienne Lord ◽  
D. Thomas Lowery
Keyword(s):  
British Columbia ◽  
Weather Conditions ◽  
Wine Grape ◽  
Drosophila Suzukii ◽  
Wine Grapes ◽  
Apple Cider ◽  
Table Grapes ◽  
Soft Fruit ◽  
Grape Cultivars ◽  
Okanagan Valley

AbstractSpotted-wing drosophila, Drosophila suzukii, (Matsumura) (Diptera: Drosophilidae), has become a serious pest of soft fruit in the Okanagan Valley of British Columbia, Canada since its detection in 2009. The study was conducted to determine the distribution of D. suzukii and damage levels in grapes. Apple cider vinegar-baited traps placed in table and wine grape (Vitis vinifera Linnaeus; Vitaceae) vineyards during 2011–2013 demonstrated that D. suzukii was numerous in all sites, with earliest emergence and highest numbers recorded in 2013. Drosophila suzukii were reared from intact and damaged table grapes and damaged wine grapes collected from the field, but not from intact wine grapes. Drosophila suzukii were reared in low numbers in 2011 from intact fruit of 11 wine grape cultivars exposed artificially in the laboratory. Susceptibility of intact wine grapes under laboratory conditions in 2011 when sour rot was widespread might relate in part to undetected infections of berries due to weather conditions. Identification of Drosophila Fallén species revealed that D. suzukii comprised a small portion of the total. Our results demonstrate that healthy wine grapes in the Okanagan Valley of British Columbia are largely undamaged by D. suzukii, while certain table grape cultivars should be protected from attack.

Bionomics of the Pear Psylla, Psylla pyricola Foerster in Pear Orchards of the Kootenay Valley of British Columbia, 1960

1962 ◽  
Vol 94 (8) ◽  
pp. 845-849 ◽  
Author(s):  
W. H. A. Wilde
Keyword(s):  
British Columbia ◽  
Climatic Conditions ◽  
Biological Study ◽  
Pear Psylla ◽  
Biological Aspects ◽  
Economic Pest ◽  
Okanagan Valley

Of the fruits grown in the Kootenay Valley of British Columbia, pears are third in importance; in the more arid Okanagan Valley 300 miles to the wrest they are second. During 1959 the pear psylla, Psylla pyricola Foerster, caused severe losses for fruit growers in the Okanagan Valley. The damage was much greater than had occurred during the previous 17 years. It became clear that the insect was a major economic pest, and that it was not being adequately controlled by the recommended insecticides. Obviously, more information was needed on the biological aspects of the situation. The roie of climatic conditions was particularly in question. In 1960 a start was made on a biological study of the pear psylla at Creston in the Kootenay Valley. This paper deals with observations thnf were made there.

Utility of compost and wood mill waste amendments to mitigate severe replant stress of sweet cherry in the Okanagan Valley of British Columbia

2019 ◽  
pp. 421-428
Author(s):  
T.A. Forge ◽  
D. Neilsen ◽  
G.H. Neilsen ◽  
P. Munro ◽  
T.T. Watson ◽  
...  
Keyword(s):  
British Columbia ◽  
Sweet Cherry ◽  
Mill Waste ◽  
Okanagan Valley

scholarly journals Native insectary plants support populations of predatory arthropods for Australian vineyards

2019 ◽  
Vol 15 ◽  
pp. 01004 ◽  
Author(s):  
M. Retallack ◽  
L. Thomson ◽  
M. Keller
Keyword(s):  
Biological Control ◽  
Functional Groups ◽  
Native Plants ◽  
South Australia ◽  
Diversity Indices ◽  
Climatic Conditions ◽  
Suitable Habitat ◽  
Wine Grape ◽  
Pest Incidence ◽  
Predatory Arthropods

We provide a summary of two recent studies that investigated the role that three native insectary plants can play in promoting predatory arthropods, and thereby to enhance biological control of vineyard pests in Australia. Native plants are preferred as supplementary flora, as they are locally-adapted to Australia's climatic conditions. Stands of mature Bursaria spinosa, Leptospermum continentale and Rytidosperma ssp. located adjacent to, or in vineyards, in South Australia were sampled for arthropods in 2013/14. Grapevines were also sampled to explore relationships between each plant and associated arthropods using common diversity indices. Twenty seven thousand and ninety-one individual invertebrate specimens were collected, comprising 20 orders and 287 morphospecies. These were categorised into functional groups of predators, herbivores and other. Predatory arthropods dominated the diversity of morphospecies present on each plant. The richness of predator morphospecies across all plant types was nearly double the number found in association with grapevines. It may be possible to increase the functional diversity of predatory arthropods by more than 3x when either B. spinosa or L. continentale is present versus grapevines only, and increase the net number of predator morphospecies by around 27% when Rytidosperma ssp. are planted in combination with grapevines. The selected plants provide a suitable habitat to support diverse and functional populations of predatory arthropods. The opportunity to plant selected native insectary species could help wine grape growers save time and resources by producing fruit with lower pest incidence, while enhancing biodiversity associated with vineyards.

Evidence for "Caribooan Orogeny" in the Southern Okanagan Region of British Columbia

1972 ◽  
Vol 9 (12) ◽  
pp. 1693-1702
Author(s):  
John V. Ross ◽  
William C. Barnes
Keyword(s):  
British Columbia ◽  
Sedimentary Rocks ◽  
Late Paleozoic ◽  
Deformational History ◽  
Exposed Part ◽  
Strong Deformation ◽  
Paleozoic Rocks ◽  
Okanagan Valley

A sequence of non-metamorphosed, little deformed, fossiliferous, sedimentary rocks, near Keremeos, southern British Columbia, unconformably overlies rocks having a history similar to that of the Vaseaux Formation, the most westerly exposed part of the Shuswap Complex of the southern Okanagan Valley. Fossils from the younger sequence have a late Mississippian – early Pennsylvanian age.This part of the southern Okanagan region has a deformational history that is pre-mid-Carboniferous and likely related to the Caribooan orogeny. This is in contrast to Late Paleozoic rocks at northern Okanagan localities and elsewhere in British Columbia that have under-gone strong deformation of probably Mesozoic age.

Evaluating the efficacy of seasonal grazing and livestock exclusion as restoration tools for birds in riparian habitat of the Okanagan Valley, British Columbia, Canada

2017 ◽  
Vol 25 (5) ◽  
pp. 768-777 ◽  
Author(s):  
Timothy R. Forrester ◽  
David J. Green ◽  
René McKibbin ◽  
Christine A. Bishop
Keyword(s):  
British Columbia ◽  
Riparian Habitat ◽  
Seasonal Grazing ◽  
Okanagan Valley

K–Ar and Fission Track Geochronometry of an Eocene Thermal Event in the Kettle River (West Half) Map Area, Southern British Columbia

1975 ◽  
Vol 12 (5) ◽  
pp. 836-843 ◽  
Author(s):  
G. A. Medford
Keyword(s):  
British Columbia ◽  
Abrupt Change ◽  
Fission Track ◽  
Apatite Fission Track ◽  
Thermal Event ◽  
South Central ◽  
Early Tertiary ◽  
Okanagan Valley

The Okanagan and Similkameen plutonic complexes west of the Okanagan Valley of south-central British Columbia yield K–Ar dates that range from 185 to 133 m.y. East of the Okanagan Valley Shuswap gneisses into which the plutonics intrude, and which may be as old as pre-midCarboniferous in age yield K–Ar dates between 59.9 and 47.4 m.y. This abrupt change, which approximately coincides with the Okanagan Valley, is a consequence of an intense thermal event in the early Tertiary which has reset K–Ar dates in the gneisses at shallow depths. Comparison of K–Ar, sphene and apatite fission track dates demonstrates that the heating affected the plutons west of the Okanagan Valley and that cooling of the Shuswap gneisses occurred at a rate in excess of 25 °C. per million years. The scatter observed in the older K–Ar dates of the plutonic complexes could be caused by post-emplacement heating with variable partial argon loss rather than by separate magmatic events. Thus, only the oldesl K–Ar dates obtained from the plutons may be significant as minimum ages for emplacement.

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