Blue Jay, Vol.35, Issue 2

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FIRST RECORD OF THE STONECAT IN SASKATCHEWAN WATERS LEROY M. ROYER, Kelsey Institute of Applied Arts and Sciences, Saskatoon, Saskatchewan, and C. BLAINE ANDERSON, Box 310, Shaunavon, Saskatchewan Members of the catfish family (7c- The stonecat can be distinguish tal u ridae) are not common or from most other members of widespread in Saskatchewan waters. family Ictaluridae by the presence Three species, the black bullhead (7c- an aanate adipose fin (low ridgelj talurus melas), the brown bullhead (7. forward extension of the caudal nebulosus) and the tadpole madtom The much smaller tadpole mad (Noturus gyrinus) are reported by also has this feature. Other diagnq Scott and Crossman (1973) to occur in characters of the stonecat I the Souris River basin of southeastern premaxillary tooth patch with lad Saskatchewan. extensions (lacking in tadpole n tom), square caudal fin, and H In July, 1975, Mr. Anderson coloration strongly countershad collected several specimens of the dark above, yellow to white belt stonecat (Noturus flavus) while com¬ pleting a fish collection as part of the The three specimens of stonl course work for the Renewable collected from the Frenchman Rl Resources Technology Program at in 1975 measured 85, 113 and 1541 Kelsey Institute of Applied Arts and total length. One specimen is ini Sciences, Saskatoon. Tnis species was personal collection of Mr. Anderl collected in the Frenchman River a second is in the fish collection al (NEV4 33-4-17 W 3rd) from a pool of Saskatchewan Fisheries Laboratol slow moving water on the north side Saskatoon and the third is in the* of a high bank. Very little vegetative collection at Kelsey Institute, Sa growth was present in the river and at toon, Saskatchewan." tnis point and the bottom was com¬ posed mainly of mud and a few large stones. BROWN, C. J. D. 1971. Fishes of Monl| Previous distribution records for Big Sky Books, Montana State iFI this species in the prairie region of Bozeman, Montana. |l^ Canada indicate its presence only in the Red River as far north as Win¬ FEDORUK, A. N. 1971. Freshwater fish I nipeg, Manitoba and in the Milk Manitoba: Checklist and keys. Man If River (Missouri River drainage) of Dept. Mines, Res. and Envir. Manag southern Alberta. The Frenchman River in Saskatchewan is also part of SCOTT, W. B. and E. J. CROSSMAN. | the Missouri River system since it Freshwater fishes of Canada. Bull. lu flows into the Milk River in Montana. Fish. Res. Bd. Canada. Ottawa. .

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The Fauna from the Tyrannosaurus Rex Excavation, Frenchman Formation (Late Maastrichtian), Saskatchewan
The Fauna from the Tyrannosaurus rex Excavation, Frenchman Formation (Late Maastrichtian), Saskatchewan Tim T. Tokaryk 1 and Harold N. Bryant 2 Tokaryk, T.T. and Bryant, H.N. (2004): The fauna from the Tyrannosaurus rex excavation, Frenchman Formation (Late Maastrichtian), Saskatchewan; in Summary of Investigations 2004, Volume 1, Saskatchewan Geological Survey, Sask. Industry Resources, Misc. Rep. 2004-4.1, CD-ROM, Paper A-18, 12p. Abstract The quarry that contained the partial skeleton of the Tyrannosaurus rex, familiarly known as “Scotty,” has yielded a diverse faunal and floral assemblage. The site is located in the Frenchman River valley in southwestern Saskatchewan and dates from approximately 65 million years, at the end of the Cretaceous Period. The faunal assemblage from the quarry is reviewed and the floral assemblage is summarized. Together, these assemblages provide some insight into the biological community that lived in southwestern Saskatchewan during the latest Cretaceous. Keywords: Frenchman Formation, Maastrichtian, Late Cretaceous, southwestern Saskatchewan, Tyrannosaurus rex. 1. Introduction a) Geological Setting The Frenchman Formation, of latest Maastrichtian age, is extensively exposed in southwestern Saskatchewan (Figure 1; Fraser et al., 1935; Furnival, 1950). The lithostratigraphic units in the formation consist largely of fluvial sandstones and greenish grey to green claystones. Outcrops of the Frenchman Formation are widely distributed in the Frenchman River valley, southeast of Eastend. Chambery Coulee, on the north side of the valley, includes Royal Saskatchewan Museum (RSM) locality 72F07-0022 (precise locality data on file with the RSM), the site that contained the disarticulated skeleton of a Tyrannosaurus rex. McIver (2002) subdivided the stratigraphic sequence at this locality into “lower” and “upper” beds.
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J the St. Mary and Milk Rivers J 2010 J
1 J J Report to THE INTERNATIONAL JOINT COMMISSION J On J THE DIVISION OF THE WATERS OF J THE ST. MARY AND MILK RIVERS J 2010 J J J J J J 1 J J J J Cover Photos: Left Side: Norm Midtlyng (USGS) conducting streamflow measurement Milk River at Eastern Crossing using conventional mechanical current meter. Photograph by Aroscott Whiteman, USGS, Montana Water Science Center, Helena, Montana Right Side: Aroscott Whiteman (USGS) conducting streamflow measurement Milk River at Milk River (Town) using hydro-acoustic equipment, acoustic doppler current profiler (ADCP) . Photograph by Don Bischoff, USGS, Montana Water Science Center, Helena, Montana J J REPORT TO THE INTERNATIONAL JOINT COMMISSION ON THE DIVISION OF THE WATERS OF THE ST. MARY AND MILK RIVERS FOR THE YEAR 2010 J Submitted By Russell G. Boals Representing Canada And Dr. Randall G. Updike Representing the United States J J November 2011 International Joint Commission Ottawa, Ontario, and Washington, D.C. Commissioners: In compliance with the provisions of Article VI of the Boundary Waters Treaty of 1909 and Clause VIII( c) of your Order of October 4, .1921; directing the division of the waters of the St. Mary and Milk Rivers between the United States and Canada, we are transmitting herewith a report on the 1 operations during the irrigation season ended October 31, 2010. J Respectfully submitted, J J Russell G. Boals Field Representative for the Accredited Officer of Her Majesty 1 J rA-..t,~ 1 Dr. Randall G. Updike Accredited Officer of the United States J j J J 1 1 l 1 J J 1 1 J J This page intentionally left blank J 1 J 1 j J J SYNOPSIS During the 2010 irrigation season, the natural flow of the St.
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Fish Survey of the Saskatchewan Portion of the Missouri Drainage
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From David Forbes, Saskatchewan Watershed Authority To
1 Saskatbhewan Head office Victoria Place 11 1 Fairford Street East Moose Jaw, Canada S6H 7x9 (306) 694-3900 (306) 694-3944 Fax www.swa.ca August 30,2004 The Right Honourable Herb Gray Mr. Dennis L. Schornack Chairman, Canadian Section Chairman, United States Section International Joint Commission International Joint Commission 2ZndFloor, 234 Laurier Avenue West 1250 - 23d Street N.W., Suite 100 OTTAWA ON KlP6K6 WASHINGTON D.C. USA 20037 Dear Sirs: Re: Montana Request to Open 1921 Order of the St. Mary and Milk Rivers Attached is a paper that was prepared by Saskatchewan Watershed Authority as Saskatchewan’s position with respect to Montana’s request to open the I92 1 Order. As we have noted in previous correspondence and as outlined in the Watershed Authority presentation to you recently at Eastend, Saskatchewan, we are opposed to the opening of the Order. This paper provides background information on our position leading to a number of conclusions and observations. We appreciate having had the opportunity to provide input to the deliberations of the International Joint Commission on this apportionment issue and we would be pleased to try and provide any additional information the IJC might like to have to assist them. We continue to look forward to an early resolution of this matter. Sincerely, LLwDavid Forbes Minister Responsible for f ILE 1 008SER Saskatchewan Watershed Authority I 3-1-4-9 I Attachment cc: Honourable Len Taylor, Minister of Government Relations St. Mary and Milk River Systems International Joint Commission Public Consultation The Saskatchewan Perspective Regarding the International Joint Commission’s Consideration toward Opening of the 1921 Order Prepared by: Saskatchewan Watershed Authority August 2004 Table of Contents 1.0 INTRODUCTION........................................................................................................
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