Early Turonian (Late Cretaceous) age of the Tuskoola sandstone Pine River area, northeastern British Columbia

2002 ◽  
Vol 39 (12) ◽  
pp. 1783-1793 ◽  
Author(s):  
C R Stelck ◽  
W E Moore ◽  
S G Pemberton

The presence of Watinoceras reesidei Warren, Watinoceras coloradoense (Henderson), Watinoceras thompsonense Cobban, and Mytiloides mytiloides (Mantell) within the Tuskoola sandstone beds of the Vimy Member of the Kaskapau (Blackstone) Formation, places these strata within the lower Turonian stage of the Upper Cretaceous, within the Watinoceras reesidei Zone. International discoveries of Watinoceras in the United States, the Arctic, west Africa, northern Africa, Europe, and Asia, in the past fifty years has allowed the authors, while updating the stratigraphy and taxonomy, to refine correlation of the Tuskoola sandstone, a sandy facies of the "Second White Specks" horizon of Western Canada.


1984 ◽  
Vol 37 (3) ◽  
pp. 380-397 ◽  
Author(s):  
Alfred S. McLaren

This paper examines the evolution of the arctic submarine and the ever-increasing scientific and commercial potential which have accompanied this evolution over the past 340 years. It is a sporadic history of arctic submarine ideas, concepts and actual experiences with vessels at sea. It happens to be a history that is largely American, with important additions as a result of the experiences of the Germans, Soviets and the British, particularly during World War II. Finally, it is a history in which five early visionaries in particular stand out: Bishop John Wilkins of England; Jules Verne of France; Professor Anschutz-Kampfe of Germany; the submarine designer Simon Lake, of the United States — whose influence extended over four decades until well into the twentieth century; and Sir Hubert Wilkins of Australia.



1982 ◽  
Vol 60 (7) ◽  
pp. 1607-1611 ◽  
Author(s):  
Stuart A. Harris ◽  
Leslie Hubricht

Extensive collecting and dissecting of live material shows that eight species of Oxyloma occur in southern and western Canada. Oxyloma haydeni is the common species across the Prairies from northern Ontario to southern Alberta. Oxyloma kanabensis occurs west of Edmonton, east of the Continental Divide and north of Sundre, while O. nuttalliana occurs west of the Continental Divide in southern British Columbia. Oxyloma groenlandica is found in the Yukon Territory and in the intermontane valleys in interior British Columbia. Oxyloma hawkinsi occurs sparsely, centred in the Okanagan area, but also persists as a probable remnant of the Hypsithermal interval at Exshaw, Alberta. Oxyloma retusa and O. gouldi are confined to the southern portions of Ontario and Quebec.A new species, Oxyloma missoula, occurs in and adjacent to the areas occupied by the former Pluvial Lake Bonneville and Glacial Lake Missoula. All the species could have survived from before the last Wisconsinan ice advance since their distributions straddle the boundary of the glaciated area.



Zootaxa ◽  
2012 ◽  
Vol 3174 (1) ◽  
pp. 51 ◽  
Author(s):  
G. G.E. SCUDDER ◽  
MICHAEL D. SCHWARTZ

Two new species of stenodemine Miridae from western Canada and the United States are described. Trigonotylus exilis n.sp. from British Columbia to northern California and Utah, and T. setosus n. sp. from northern British Columbia, YukonTerritory, and adjacent northern Northwest Territories and Alaska are documented. A key to the species of Trigonotylusfrom this study region is provided to allow identification of the included fauna. Host plant species are identified. Lactic acid is proposed as an alternative to potash as a dissection medium for male genitalia.



Nordlit ◽  
2008 ◽  
Vol 12 (1) ◽  
pp. 69
Author(s):  
Tiffany Johnstone

In 1908, Agnes Deans Cameron, a schoolteacher, journalist andsuffragist from Victoria, British Columbia, traveled from Chicago to the Arctic with her niece, Jessie Cameron Brown. Cameron followed the original 1789 route of Alexander Mackenzie and was intent on being one of the first white women to explore and document this northern territory (Roy, "Primacy" 56). She wrote about her trip in the popular book The New North, which was published in New York in 1909 by Appleton. While The New North is written by a Canadian author about Canada, it is deliberately aimed at an American audience. Not only was the book published in the United States, but the narrative also begins and ends in Chicago and repeatedly depicts her Canadian surroundings according to American frontier motifs.



1969 ◽  
Vol 101 (1) ◽  
pp. 97-100 ◽  
Author(s):  
K. R. Depner

AbstractThe range of the face fly, Musca autumnalis De Geer, has extended from the site of its first North American occurrence in Nova Scotia in 1952 to the northern half of the United States from coast to coast and every province in Canada. The first recorded appearance in Western Canada was at Virden, Man., in 1964 and it has since become established in eastern Saskatchewan. Face flies moved from Washington and Idaho into British Columbia in 1966. In 1967 they spread to most areas of the southern half of British Columbia and into southwestern Alberta through the Crowsnest Pass. Moisture and shade in pastures influenced the numbers of face flies seen on cattle and resulted in higher numbers than under dry prairie conditions.



Author(s):  
Henrik Larsen

The chapter presents the dominant discourse in Danish foreign policy. The dominant discourse articulates the EU as essential and the key platform for Danish foreign policy, while NATO and the United States are also articulated as crucial if mainly in the field of security. The articulation of an activism that breaks with the strategic passivity in the past is the background for Denmark’s participation in conflicts in Syria and Iraq. The UN and in particular Nordic cooperation are not attributed the same value as the EU and NATO/the United States. However, particularly from the Foreign and Security Policy Strategy 2019–20, tendencies towards an even stronger Danish emphasis on the EU, multilateralism, international rules, and on issue areas such as security in the neighbourhood, immigration, the Arctic, and trade are identified. The chapter raises the question of whether the ensemble of these tendencies will challenge or reinforce the EU’s and NATO’s central roles.



2016 ◽  
Vol 58 (1) ◽  
pp. 159-180 ◽  
Author(s):  
Wyatt MacGaffey

AbstractThe past thirty years have seen, particularly in the United States, a transformation in the public image of “Kongo,” an ill-defined entity (a tribe, a kingdom, a culture, a region?) on the Atlantic coast of Central Africa. The efforts of R. F. Thompson, professor of art history at Yale, and A. Fu-kiau, himself Kongolese, have done much to popularize a “Kongo” characterized more by its romantic appeal than by historical or ethnographic verisimilitude. Elsewhere in the Americas, the reputation of “Kongo” has suffered by comparison with “Yoruba,” another historically emergent Atlantic identity, based in West Africa. These identities, and the supposed contrast between them, are products of an increasingly complex trans-Atlantic discourse.



2016 ◽  
Vol 66 (4) ◽  
pp. 609-626
Author(s):  
Stephen C. Hook ◽  
William A. Cobban

Abstract Lopha staufferi (Bergquist, 1944) is a medium-sized, ribbed, Late Cretaceous oyster with a slightly curved axis and a zigzag commissure; it appears suddenly and conspicuously in upper Cenomanian rocks in the Western Interior Basin of the United States. At maturity, the ribs on both valves thicken into steep flanks that allow the oyster to increase interior volume without increasing its exterior footprint on the seafloor. Lopha staufferi is the first (earliest) ribbed oyster in the Late Cretaceous of the Western Interior, but has no ancestor in the basin. It disappears from the rock record as suddenly as it appeared, leaving no direct descendent in the basin. In the southern part of the basin where it is well constrained, L. staufferi is restricted stratigraphically to the upper Cenomanian Metoicoceras mosbyense Zone (= Dunveganoceras conditum Zone in the north). Lopha staufferi has an unusual paleogeographic distribution, occurring in only two, widely scattered areas in the basin. It has been found at several localities near the western shoreline of the Late Cretaceous Seaway in west-central New Mexico and adjacent Arizona, and in localities 1,900 km (1,200 mi) to the northeast near the eastern shoreline in northeastern Minnesota, but nowhere in between. In west-central New Mexico and adjacent Arizona, L. staufferi is a guide fossil to the Twowells Tongue of the Dakota Sandstone.



1976 ◽  
Vol 108 (11) ◽  
pp. 1296-1296 ◽  
Author(s):  
A. M. Harper

Aphidius smithi Sharma and Subba Rao is the most important parasite of the pea aphid, Acyrthosiphum pisum (Harris), in North America. In 1958, it was imported into the United States from India to control the pea aphid and was subsequently released and recovered in most of continental United States except the Gulf Coast States and Texas (Halfhill et al. 1972). Mackauer and Finlayson (1967) reported that the parasite was present in Ontario, Quebec, and British Columbia and had been released but not recovered in Nova Scotia. A. smithi has never been released in western Canada nor been found on the Canadian prairies before 1970.



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