A Virus Disease and Introduced Parasites as Factors Controlling the European Spruce Sawfly, Diprion hercyniae (Htg.), in Central New Brunswick

1957 ◽  
Vol 89 (8) ◽  
pp. 371-378 ◽  
Author(s):  
F. T. Bird ◽  
D. E. Elgee
Keyword(s):  
Nova Scotia ◽  
New Brunswick ◽  
New Hampshire ◽  
Virus Disease ◽  
Spruce Forests ◽  
North Shore ◽  
The North ◽  
Gaspe Peninsula ◽  
Gaspé Peninsula ◽  
St Lawrence River

An outbreak of the European spruce sawfly, Diprion hercyniae (Htg.), was discovered in the Gaspé Peninsula in 1930. By 1938, heavy infestations had developed west of the Gaspé Peninsula in Quebec, throughout New Brunswick and northern Maine, and in parts of Vermont and New Hampshire. Moderate to light infestations occurred through all other parts of the spruce forests of this region and extended from Nova Scotia, to the north shore of the St. Lawrence River, and west to Ontario.

scholarly journals Une épidémie d’insectes, facteur de déboisement dans le Québec

2005 ◽  
Vol 2 (4) ◽  
pp. 233-240
Author(s):  
Gilles Roy
Keyword(s):  
Spruce Budworm ◽  
The Past ◽  
North Shore ◽  
The North ◽  
Forest Industries ◽  
Gaspe Peninsula ◽  
Gaspé Peninsula ◽  
St Lawrence River

Spruce budworm bas invaded the forest of Québec since 1939, especially the pines of the coniferous area. There are jour major infested regions : three are located on the North shore of the St. Lawrence river : in the Gatineau river bassin, in the Laurentians between the Lachute Area and lake St. John, and in the North Shore region behind Baie Comeau Sept-Iles. The fourth region starts behind Rimouski and spreads eastward, covering the whole Gaspé peninsula. In this last the authorities are quite concerned about this plague, which is becoming a serious menace to the forest industries. Various air-spays have been used during the past jour years in order to circumscribe the dammages, and more than 4,000,000 acres have been treated with DDT, first step toward the rehabilitation of the forest.

MITES, TICKS, AND FLEAS OF THE MICE ZAPUS HUDSONIUS AND NAPAEOZAPUS INSIGNIS FROM THE MARITIME PROVINCES AND GASPÉ PENINSULA, QUEBEC, CANADA

1982 ◽  
Vol 114 (11) ◽  
pp. 1031-1035 ◽  
Author(s):  
Gwilym S. Jones ◽  
Howard H. Thomas
Keyword(s):  
Nova Scotia ◽  
New Brunswick ◽  
Prince Edward Island ◽  
Maritime Provinces ◽  
Napaeozapus Insignis ◽  
Gaspe Peninsula ◽  
Gaspé Peninsula

AbstractMites, ticks, and fleas were removed from the fur of 110 specimens of Zapus hudsonius (Zimmermann) from Prince Edward Island, coastal New Brunswick, and northern Nova Scotia. The species which were most abundant and the only ones which occurred on these mice throughout the area were Dermacarus newyorkensis, Neotrombicula harperi, Androlaelaps fahrenholzi, and Ixodes muris. Also examined were 47 specimens of Napaeozapus insignis (Miller) from the above provinces plus Gaspé Peninsula, Quebec. Dermacarus newyorkensis and Neotrombicula harperi were the most abundant ectoparasites. Neotrombicula harperi was the only ectoparasite which occurred on N. insignis throughout the region.

Ticks from mammals from Prince Edward Island, New Brunswick, northern Nova Scotia, and Gaspé Peninsula, Quebec

1980 ◽  
Vol 58 (7) ◽  
pp. 1394-1397 ◽  
Author(s):  
Gwilym S. Jones ◽  
Howard H. Thomas
Keyword(s):  
Nova Scotia ◽  
New Brunswick ◽  
Small Mammals ◽  
Prince Edward Island ◽  
New Host ◽  
Tamias Striatus ◽  
Sorex Cinereus ◽  
Gaspe Peninsula ◽  
New Host Records ◽  
Gaspé Peninsula

Four species of ticks were recovered from small mammals collected in Prince Edward Island. New Brunswick, northern Nova Scotia, and the Gaspé Peninsula, Quebec. Included among these were the following new host records: Ixodes marxi ex Sorex cinereus, I. muris ex. Clethrionomys gapperi, and Haemaphysalis leporispalustris ex. Tamias striatus. New provincial records were Ixodes marxi, I. muris, and Haemaphysalis leporispalustris from Prince Edward Island and Ixodes muris from New Brunswick.

PREDATION BY INSECTS AND SPIDERS INHABITING COLONIAL WEBS OF HYPHANTRIA CUNEA

1972 ◽  
Vol 104 (8) ◽  
pp. 1197-1207 ◽  
Author(s):  
R. F. Morris
Keyword(s):  
Population Dynamics ◽  
Nova Scotia ◽  
North America ◽  
Population Density ◽  
New Brunswick ◽  
Numerical Response ◽  
Initial Number ◽  
Hyphantria Cunea ◽  
The North ◽  
The Mean

AbstractThe number of predators inhabiting nests of Hyphantria cunea Drury was recorded annually for 13 years in four areas in New Brunswick and two areas on the coast of Nova Scotia. The most common groups were the pentatomids and spiders, which sometimes reproduced within the nests, but the mean number per nest was low in relation to the number of H. cunea larvae in the colonies. The rate of predation on fifth-instar larvae was low. Small or timid predators appeared to prey largely on moribund larvae or small saprophagans during the principal defoliating instars of H. cunea.No relationship could be detected between the number of larvae reaching the fifth instar and the number of predators in the colony; nor could any functional or numerical response of the predators to either the initial number of larvae per colony or the population density of colonies be found. It is concluded that the influence of the nest-inhabiting predators is small and relatively stable, and may be treated as a constant in the development of models to explain the population dynamics of H. cunea.H. cunea is a pest in parts of Europe and Asia, where it has been accidentally introduced from North America. The introduction to other continents of the North American predator, Podisus maculiventiis (Say), is discussed briefly.

Seismicity and faulting in the Charlevoix zone of the St. Lawrence Valley

1984 ◽  
Vol 74 (2) ◽  
pp. 595-603
Author(s):  
F. M. Anglin
Keyword(s):  
Active Zone ◽  
Continuous Monitoring ◽  
North Shore ◽  
The North ◽  
Earthquake Zone ◽  
St Lawrence River

Abstract Continuous monitoring of the seismically active Charlevoix zone since late 1977 has delineated the boundaries of the earthquake zone under the north shore and has enabled an association to be made with surface mapped faults that strike along the St. Lawrence Valley and dip to the southeast. Within the active zone, aseismic volumes are found under parts of the St. Lawrence River and another elongated zone of activity is found to the southeast on unmapped faults dipping under the river. The previous suggestions that the activity is related to old rift faults, which have been later weakened by a meteor impact, would seem to be upheld.

Preliminary interpretation of the first refraction arrivals in Gaspé from shots in Labrador and Quebec

1969 ◽  
Vol 6 (4) ◽  
pp. 771-774 ◽  
Author(s):  
Douglas S. Rankin ◽  
Ravi Ravindra ◽  
David Zwicker
Keyword(s):  
Upper Mantle ◽  
Arrival Time ◽  
The South ◽  
North Shore ◽  
The North ◽  
A Value ◽  
South Shore ◽  
Compressional Velocity ◽  
St Lawrence River

Previous work in the Gulf of St. Lawrence has yielded an unusually high upper-mantle compressional velocity. In the Gaspé area a more recent determination has yielded a value of 8.75 ± 0.20 km/s for an unreversed profile. The arrival time at a station on the north shore of the St. Lawrence River suggests that there is no major difference in velocity and depth relative to the south shore.

Silurian Proporidae and Plasmoporidae (Anthozoa, Tabulata) from the Chaleurs Bay region, Canada

1990 ◽  
Vol 64 (2) ◽  
pp. 184-199 ◽  
Author(s):  
Graham A. Young ◽  
James P. A. Noble
Keyword(s):  
New Brunswick ◽  
Type Species ◽  
Facies Distribution ◽  
Patch Reefs ◽  
Holotype Specimen ◽  
Upper Silurian ◽  
Gaspe Peninsula ◽  
Open Shelf ◽  
Gaspé Peninsula

Six species belonging to the families Proporidae and Plasmoporidae occur in the Lower and Upper Silurian rocks of the Limestone Point and La Vieille Formations of northern New Brunswick and of the Anse à Pierre-Loiselle, La Vieille, and Gascons Formations of the Gaspé Peninsula of Québec. The three species ofProporaare widely distributed but show varying faunal affinities, while both species ofPlasmopora, Plasmopora loganiandPlasmopora corrugata, are new and are almost endemic. Revised concepts ofProporaandPlasmoporaare proposed. The holotype specimen for the type species ofCamptolithuswas examined and confirms the genus as distinct fromPropora, rather than a synonym as has been previously suggested.The facies distribution of these corals is variable. In general, the proporids, which mostly occur in facies indicating shallow carbonate banks and patch reefs, are more restricted in distribution than the plasmoporids, which occur in these facies and also in others representing a variety of open-shelf environments.

The Sedimentary Structures and Depositional Mechanics of Certain Ordovician Turbidites, Cloridorme Formation, Gaspé Peninsula, Quebec

1975 ◽  
Vol 12 (11) ◽  
pp. 1934-1952 ◽  
Author(s):  
Keith Skipper ◽  
Gerard V. Middleton
Keyword(s):  
Large Scale ◽  
Fine Sand ◽  
Coarse Sand ◽  
Turbidity Currents ◽  
Upstream Migration ◽  
High Concentration ◽  
Sedimentary Structures ◽  
The North ◽  
Gaspe Peninsula ◽  
Gaspé Peninsula

Turbidites, belonging to the β1, member, Cloridorme Formation, are exposed on the north shore of the Gaspé Peninsula, Quebec. Their structural attitude is such that vertical sections through turbidite beds are exposed on the wave-cut platform and their strike is approximately parallel to the paleocurrent direction, as shown by sole marks on the bases of beds.Certain thick turbidite beds, in a distal position, display a sequence of sedimentary structures which differs from the sequence defined by Bouma. Three broad divisions are recognized: a basal division consists of either limestone or quartz granule to pebble conglomerate (0–4 cm thick) or coarse sand graywacke or calcareous wacke (0–15 cm thick). Basal divisions of calcareous wacke frequently display ripple-lamination, parallel lamination, or upstream-inclined laminae. Where the upstream inclined laminae form a single set, they occur below a sinuous profile (wavelength 40–80 cm, and amplitude 2–5 cm).A second division (0–330 cm thick) consists in most places of spindle- or globular-shaped calcareous nodules scattered in an argillaceous host. In some beds, streaking and lobing of light colored, carbonate bearing material is associated with these nodules. Internal hemi-ellipsoid structures, arranged en echelon and convex towards the base of the bed, are displayed from the second division. The upper division consists of fine grained siltstone and shale.The upstream-inclined laminae in the basal division of calcareous wacke beds are interpreted as being the result of the upstream migration of antidunes. The nodules within the second division developed as 'pseudo-nodules'. The hemi-ellipsoid structures resemble damped, large scale (macroturbulent) eddies associated with the flow of dense grain dispersions.Correlation of these beds has been achieved over a distance of 12 km. Basal divisions of granule and pebble conglomerate persist over this distance and show that coarse particles may be transported by turbidity currents over long distances. The sedimentary structures of the basal divisions of several calcareous wacke beds might be interpreted as the result of either an increase in flow regime downcurrent, or of nonpreservation of structures at up-current localities.The beds were probably deposited from turbidity currents composed largely of mud and fine sand, but containing a zone of coarse grains concentrated near the bed. The basal division was deposited from this lower zone and a period of traction formed rippled, flat, or antidune bed forms. Stratification in the basal division was preserved by the rapid deposition on top of sediment that settled en masse from the subsequent high concentration body of the current. The formation of a succession of 'quick' beds led to the sedimentation of the second division. The flows responsible for the sequence of structures observed and the downcurrent persistence of the beds probably approached closely a state of 'autosuspension'.

Control of Black Fly Larvae (Diptera: Simuliidae) in the Forests of Eastern Canada by Aircraft Spraying

1960 ◽  
Vol 92 (10) ◽  
pp. 745-754 ◽  
Author(s):  
A. S. West ◽  
A. W. A. Brown ◽  
D. G. Peterson
Keyword(s):  
Black Flies ◽  
Eastern Canada ◽  
Black Fly ◽  
North Shore ◽  
The North ◽  
Fly Larvae ◽  
And Control ◽  
St Lawrence River ◽  
Made In

The results reported in this paper are part of a study of the biology and control of black flies in the forests of Eastern Canada conducted on the north shore of the St. Lawrence River, near Baie Comeau, Quebec, during 1954, 1955, and 1956. Reference to this study is made in a review by Peterson and Wolfe (1958). The identification and biology of the black flies of this region has been reported on by Wolfe and Peterson (1959) who also describe the topography of the region. The important feature of this rugged area is an abundance of fast-flowing streams which provide highly suitable environments for the development of black-fly populations.

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