Lichens as Nesting Material for Northern Flying Squirrels in the Northern Rocky Mountains

1994 ◽  
Vol 75 (3) ◽  
pp. 663-673 ◽  
Author(s):  
G. D. Hayward ◽  
R. Rosentreter
2008 ◽  
Vol 86 (8) ◽  
pp. 851-862 ◽  
Author(s):  
S. A. Dubay ◽  
G. D. Hayward ◽  
C. Martínez del Rio

Many small mammals consume lichen and fungi, but southern red-backed voles ( Clethrionomys gapperi (Vigors, 1830)) and northern flying squirrels ( Glaucomys sabrinus (Shaw, 1801)) exhibit strong mycophagy compared with other North American taxa. We analyzed nutrient content of lichen and fungi and observed feeding preferences of voles and flying squirrels to understand the foraging behavior of these mammals and their strategy for surviving on relatively low-quality diets dominated by lichen and fungi. We analyzed nutrient characteristics of 10 hypogeous (fruiting belowground) fungi and four arboreal lichens eaten by red-backed voles and northern flying squirrels in the Rocky Mountains. Hypogeous fungi contained higher nitrogen, lipid, neutral detergent fiber, acid detergent fiber, ash, potassium, and phosphorous concentrations than arboreal lichens, but lichens were higher in calcium. To assess diet preferences, 10 pairwise feeding trials using four hypogeous fungi and two arboreal lichens were conducted with voles and seven trials using three hypogeous fungi and two lichens were conducted with squirrels. In general, squirrels and voles preferred hypogeous fungi over arboreal lichens. We then calculated dry matter and nitrogen digestibilities for flying squirrels and red-backed voles fed diets of arboreal lichen and hypogeous fungi. Overall mean dry matter digestibilities were ≥70% for all diets. For hypogeous fungi, nitrogen digestibility was 12.3% and 24.9% for squirrels and voles, respectively, suggesting that most nitrogen was indigestible. Animals maintained positive nitrogen balance when fed fungi but were unable to maintain positive nitrogen balance when fed lichens. Maintenance nitrogen requirements for flying squirrels were lower than predicted. Low requirements may allow for increased consumption of lichen in winter, but lichen diets must be supplemented with a source of nitrogen because animals were unable to maintain nitrogen balance when fed lichen alone. Consumption of numerous fungi and lichen taxa is necessary to sustain these animals year-round.


Author(s):  
Michael L. Zientek ◽  
Pamela D. Derkey ◽  
Robert J. Miller ◽  
J. Douglas Causey ◽  
Arthur A. Bookstrom ◽  
...  

Author(s):  
Edward A. Mankinen ◽  
Thomas G. Hildenbrand ◽  
Michael L. Zientek ◽  
Stephen E. Box ◽  
Arthur A. Bookstrom ◽  
...  

The Holocene ◽  
2019 ◽  
Vol 30 (3) ◽  
pp. 479-484
Author(s):  
Daniel P Maxbauer ◽  
Mark D Shapley ◽  
Christoph E Geiss ◽  
Emi Ito

We present two hypotheses regarding the evolution of Holocene climate in the Northern Rocky Mountains that stem from a previously unpublished environmental magnetic record from Jones Lake, Montana. First, we link two distinct intervals of fining magnetic grain size (documented by an increasing ratio of anhysteretic to isothermal remanent magnetization) to the authigenic production of magnetic minerals in Jones Lake bottom waters. We propose that authigenesis in Jones Lake is limited by rates of groundwater recharge and ultimately regional hydroclimate. Second, at ~8.3 ka, magnetic grain size increases sharply, accompanied by a drop in concentration of magnetic minerals, suggesting a rapid termination of magnetic mineral authigenesis that is coeval with widespread effects of the 8.2 ka event in the North Atlantic. This association suggests a hydroclimatic response to the 8.2 ka event in the Northern Rockies that to our knowledge is not well documented. These preliminary hypotheses present compelling new ideas that we hope will both highlight the sensitivity of magnetic properties to record climate variability and attract more work by future research into aridity, hydrochemical response, and climate dynamics in the Northern Rockies.


1977 ◽  
Vol 18 (79) ◽  
pp. 325-328 ◽  
Author(s):  
W. L. Graf

AbstractEvidence from aerial photographs, maps, and field checks indicates that 319 glaciers lie in cirques of the Rocky Mountains, south of the United States-Canadian border. On a subcontinental scale, the distribution of glaciers is highly clustered, with larger and denser clusters located in the northern Rocky Mountains. Lesser concentrations of small glaciers occur in the southern Rocky Mountains. The total area of glaciers in the Rocky Mountains of the U.S.A. is 78.9 km2.


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