Continental marging off Southeastern Alaska, the Queen Charlotte Islands, and Northern Vancouver Island

1989 ◽  
Vol 67 (6) ◽  
pp. 1386-1393 ◽  
Author(s):  
Guillermo R. Giannico ◽  
David W. Nagorsen

From multivariate analyses of 25 cranial measurements, we assessed geographic and sexual variation in three island and two mainland samples of Pacific coast marten (Marten americana) from the caurina subspecies group. Three morphological groups were evident: the first from Queen Charlotte Islands, the second from Alexander Archipelago and Alaska Panhandle, and the third from Vancouver Island and the southern British Columbia coast. We concluded that the subspecies M. a. nesophila should be restricted to the Queen Charlotte Islands; Vancouver Island and southern British Columbia coastal marten are aligned with M. a. caurina. Alaskan marten showed some affinities with the americana subspecies group. The strong differentiation of M. a. nesophila is concordant with the isolation and unique selection regime of the Queen Charlotte Islands. Sexual dimorphism was most pronounced in island samples; possible explanations for this trend are discussed.


1953 ◽  
Vol 10 (3) ◽  
pp. 125-145 ◽  
Author(s):  
G. L. Pickard ◽  
D. C. McLeod

Grand monthly means of daily observations of surface sea-water temperature and salinity from twelve light stations along the British Columbia coast during the 13 years 1935 to 1948 have been analysed. In general the temperatures reach a minimum of 45°F. ± 1° (7.2 °C. ± 0.5°) in January and February. The maximum varies from 50° to 64°F. (10° to 18 °C.) in August. The warmest waters occur in bays protected from wind action, and the coldest waters occur in regions of turbulent mixing due to wind or strong currents. The salinity along the mainland coast is a minimum in early summer, associated with the maximum run-off from melting snow. Along the west coast of Vancouver Island the minimum occurs in mid-winter, associated with maximum precipitation which is not stored as snow in this region. At the southern and northern tip of the Queen Charlotte Islands there is little or no variation of salinity because there is no land drainage of consequence in the vicinity.In passes between Georgia Strait and the sea where the waters are mixed to homogeneity by strong tidal currents the annual variation of temperature and salinity is reduced, and in some cases entirely suppressed.On the west coast of Vancouver Island it is shown that the annual cycle is affected by the dominant winds and upwelling of deep ocean waters.


1999 ◽  
Vol 36 (8) ◽  
pp. 1371-1413 ◽  
Author(s):  
Susan M DeBari ◽  
Robert G Anderson ◽  
James K Mortensen

The Westcoast Crystalline Complex (WCC), Island Intrusions, and Bonanza Group of Vancouver Island, Canada, form three different crustal levels of the Early to Middle Jurassic Bonanza island arc. Differential uplift has exposed the plutonic roots and the volcanic carapace of the arc for a strike length of ~500 km, and for another 250 km on the Queen Charlotte Islands. At deeper crustal levels within the arc, influx of mantle-derived magmas was accompanied by metamorphism and melting of Wrangellian basement rocks, yielding the heterogeneous WCC. Upward mobilization and hybridization of magmas to shallower levels in the crust resulted in the batholiths of the Island Intrusions and the lavas and pyroclastic rocks of the Bonanza Group. New U-Pb crystallization ages for plutonic rocks of the arc span an age range of 190.3 ± 1.0 to 168.6 ± 5.3 Ma. Ages of the WCC and western Island Intrusions are indistinguishable and overlap with published fossil and isotopic ages for the Bonanza Group. Younger Middle Jurassic ages for the eastern Island Intrusions overlap with those for plutonic rocks in the southern Coast Belt and Queen Charlotte Islands. All plutonic and volcanic rocks within the arc have overlapping geochemical signatures, supporting their comagmatic origin. All are light rare earth element-enriched with abundances 10-50× chondrites. The most mafic noncumulate gabbroic rocks have compositions typical of island arc basalts, with intermediate values of Al2O3 (16-17 wt.%) and high MgO (7-9 wt.%). More differentiated rocks follow a calc-alkaline trend with concomitant increase in Al2O3 (18-20 wt.%). Their geochemistry indicates varying degrees of mixing with melts of mafic Wrangellian basement.


1981 ◽  
Vol 61 (2) ◽  
pp. 365-381 ◽  
Author(s):  
LONNIE W. AARSSEN

This paper provides a summary of biological data on Hypochoeris radicata L. (spotted cat’s-ear). This weed is naturalized in Canada on both the west and east coasts but is common only on Vancouver Island, the Queen Charlotte Islands, and the adjacent mainland of British Columbia. It is adapted to a wide range of habitats such as lawns, fields and along roadsides. The species is commonly mistaken for dandelion (Taraxacum officinale Weber), fall hawkbit (Leontodon autumnalis L.) or Hypochoeris glabra L. due to the close resemblance of their bright yellow flowers. This last species is the only other member of the genus occurring in Canada and it hybridizes readily in nature with H. radicata. Several herbicides can be used to control H. radicata.


1999 ◽  
Vol 29 (4) ◽  
pp. 509-516 ◽  
Author(s):  
Mats Hannerz ◽  
Sally N Aitken ◽  
John N King ◽  
Sonya Budge

Fall and spring frost hardiness was determined from electrolytic leakage of artificially frozen needle segments in 22 full-sib families of western hemlock (Tsuga heterophylla (Raf.) Sarg.) from British Columbia and Washington State representing different levels of genetic gain, and of four provenance materials (stand progenies from the Queen Charlotte Islands, Vancouver Island, and Oregon Cascades, and seed-orchard progenies from the northern Oregon Coast Range). Samples for freeze testing were collected in a 5-year-old trial at Jordan River on southwestern Vancouver Island. Height and date of bud flush were recorded in the field. Genetic gain among the full-sib families was not correlated with fall frost hardiness, but high-yielding families displayed a lower spring frost hardiness and an earlier bud flush than low-yielding families. Both fall and spring frost hardiness increased and height growth decreased with the latitude of provenances. The highest growth, earliest bud flush and lowest fall and spring frost hardiness was demonstrated by the Oregon provenances, while the lowest growth, latest bud flush and highest hardiness was found for the Queen Charlotte Islands provenance.


1982 ◽  
Vol 60 (6) ◽  
pp. 1463-1469 ◽  
Author(s):  
Terry D. Beacham

Significant regional and annual variability in fecundity of coho salmon (Oncorhynchus kisutch) and chum salmon (O. keta) in British Columbia was detected during this investigation. A Kodiak Island (Alaska) coho salmon stock was more fecund than southern stocks in British Columbia and Washington. Fecundity ranged from 2450 to 2850 eggs per female at 53.6 cm postorbital–hypural length for Vancouver Island stocks to over 4400 eggs per female for a Kodiak Island stock at the same length. Chum stocks on Vancouver Island and the Queen Charlotte Islands generally had fecundities less than 3200 eggs per female at 58.8 cm postorbital–hypural length, whereas chum of equal lengths in mainland British Columbia stocks ranged from 3200 to 3450 eggs per female. Older chum and coho were usually more fecund than younger ones, but this difference could be accounted for by differences in mean length-at-age, fecundity being related to body size.


1969 ◽  
Vol 6 (3) ◽  
pp. 463-474 ◽  
Author(s):  
R. A. Stacey ◽  
L. E. Stephens

The survey area lies close to the continental margin and includes parts of the Insular Tectonic Belt and the Coast Mountains igneous and metamorphic complex, which are part of the Cordilleran (geological) Region. In an endeavor to clarify the structure of the Insular Tectonic Belt and the Coast Mountains complex, gravity measurements have been made using Worden or LaCoste and Romberg meters at 12–15 km intervals throughout the Queen Charlotte Islands, Vancouver Island, and the coastal areas of the British Columbia mainland. Measurements have been made at the same interval using a LaCoste and Romberg underwater gravity meter wherever the depth of water is less than 300 fathoms (< 540 m) along the fiords of the mainland coast and over the continental shelf. The observed gravity values have been reduced to Bouguer anomalies and terrain corrections have been calculated using either Bible's tables or a computer system based on the attraction of the rectangular prismatic block.The major features of gravity field are: (1) a positive Bouguer anomaly along the western edge of the area, which is associated with the change from continental to oceanic crust, and (2) a negative anomaly along the Coast Mountains, which is attributed to the thickening of the continental crust below these mountains. On the eastern side of the Queen Charlotte Islands, Hecate Strait, Queen Charlotte Sound, and Vancouver Island, the average Bouguer anomaly is approximately zero, with local anomalies superimposed on a fairly flat gravity field. Several of these local anomalies are related to density variations in the surface rocks.


1997 ◽  
Vol 75 (11) ◽  
pp. 1887-1896 ◽  
Author(s):  
Sandra C. Lindstrom ◽  
Jeanine L. Olsen ◽  
Wytze T. Stam

We used random amplified polymorphic DNA (RAPD) markers to examine the distribution of genotypes of Palmaria mollis (Setchell et Gardner) van der Meer et Bird, a red alga. We sampled populations along the Northeast Pacific coast from northern Washington to southwestern Alaska, an area extensively glaciated during the last ice age. Our objective was to determine whether the tracks of postglacial recolonization could be extracted from the extant pattern of genotype distribution in a species with limited dispersal capabilities. Thirty-eight individuals from 14 sites were sampled for RAPD markers using nine different random primers. As expected, individuals from the same population were more closely related to each other than to individuals from other populations. Relationships among populations, however, did not necessarily reflect geographic proximity. Rather, populations fell into groups corresponding approximately to outer and inner coastal sites: the northwestern end of Vancouver Island and the Queen Charlotte Islands formed one outer coast group, which associated with sites from Prince William Sound, the Alaska Peninsula, and Sitka, Alaska; the eastern side of Vancouver Island and Ketchikan, Alaska, represented one group of inner sites, which associated with sites near Juneau, Alaska and the eastern end of the Strait of Juan de Fuca. We conclude that this pattern does not represent a single postglacial recolonization event. Key words: biogeography, dispersal, genetic distance, Palmaria mollis, RAPDs, Rhodophyta.


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