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Porcupine Densities Estimated from Winter Aerial Surveys in North Dakota, 1964–1965

William F. Jensen1*, Jack M. Samuelson1,2, and Robert W. Seabloom3

1North Dakota Game and Fish Department, 100 North Bismarck Expressway, Bismarck, North Dakota 58501, USA. 2Deceased. 3University of North Dakota (retired), Starcher Hall, Grand Forks, North Dakota 58202, USA. *Corresponding author.

Prairie Naturalist, Volume 55 (2023):N7–N10

Abstract
During the winter of 1964–1965, aerial counts of Erethizon dorsatum (Linnaeus) (North American Porcupine) were recorded while conducting deer surveys. In total, 443 North American Porcupines were observed on 5,722 km2, with an overall minimum density of ~0.1 individuals/km2. Densities appeared to be greatest in areas managed as national wildlife refuges and parks.

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Porcupine Densities Estimated from Winter Aerial Surveys in North Dakota, 1964–1965 William F. Jensen1*, Jack M. Samuelson1,2, and Robert W. Seabloom3 Abstract – During the winter of 1964–1965, aerial counts of Erethizon dorsatum (Linnaeus) (North American Porcupine) were recorded while conducting deer surveys. In total, 443 North American Porcupines were observed on 5,722 km2, with an overall minimum density of ~0.1 individuals/km2. Densities appeared to be greatest in areas managed as national wildlife refuges and parks. Limited information is available in the literature on Erethizon dorsatum (Linnaeus) (North American Porcupine) densities, particularly on the northern Great Plains. While recently archiving historical data sheets of winter aerial surveys for Odocoileus virginianus (Zimmermann) (White-tailed Deer) and Odocoileus hemionus (Rafinesque) (Mule Deer), conducted by the North Dakota Game and Fish Department, detailed observations on North American Porcupines were discovered. Although the primary purpose for these surveys was to observe and count deer, incidental notes and observations were made for other species. During the winter of 1963–1964, comments were made about the abundance of North American Porcupines observed, but the actual number sighted was not recorded. During the winter of 1964–1965, the number of North American Porcupines observed was dot tallied on datasheets. North American Porcupine observations were not regularly recorded in subsequent years. Herein we summarize the 1964–1965 incidental observations and provide minimum estimates of winter North American Porcupine densities by physiographic regions in North Dakota. All flights were conducted in a Super Cub piloted by Elmer Homelvig, with big game biologist Jack Samuelson serving as observer and recorder. Winter aerial survey conditions for deer require snow depth >15 cm and uniform coverage throughout the study area. Surveys were conducted through intense searches of various habitats from a fixed-wing, light aircraft at altitudes from 76 to 107 m, and at flight speeds preferably below 129 km/hour (McKenzie 1958). Snow conditions permitted a total of 55 survey units to be flown in 17 deer hunting units (DHUs) from 2 December 1964 to 17 February 1965. Survey units ranged in size from 21 to 299 km2. North American Porcupine observations were recorded on 36 (65%) of the 55 survey units. Surveys were subsumed into the Badlands, Slope, Missouri Coteau, and Drift Prairie physiographic regions (Figure 1). In total, 443 North American Porcupines were observed on the 5,722 km2 flown. The greatest overall densities were observed on the Drift Prairie, followed by Missouri Coteau, Slope, and Badlands, respectively (Table 1). North American Porcupine densities were greatest on survey areas that encompassed national wildlife refuges (NWR) (Upper Souris NWR: 0.98/km2; Des Lacs NWR: 0.44/km2), national parks (South Unit of Theodore Roosevelt National Park: 0.27/km2), and along major river systems (White Earth River: 0.71/km2, Missouri River: 0.47/km2). We caution that these were minimum counts and that sightability bias from an aerial survey was not ground-truthed and probably influenced these estimates. Estimated North American Porcupine densities in forested provinces and states generally range from 2 to 13/km2 (e.g., New Brunswick: 2.7/km2, Reek 1942; Michigan: 3.5/km2, Earle and Kramm 1982; New York: 4.7/km2, Shapiro 1949; 10.7/km2, Roze 1984; Oregon: 12.6/km2, Smith 1977). However, in Upper Michigan, when coexisting with Pekania pennanti (Erxleben) (Fisher), North American Porcupine densities were significantly lower and averaged 0.4/km2 (Earle and Kramm 1982). Density estimates for North American Porcupines in western grasslands and shrub habitats are limited. We are aware of only two estimates for North American Porcupine densities in western prairie states (Montana: 6/km2, Hendrick and Allard 1988; Wyoming: 3.4/km2, Band 1996). However, both those studies were based upon limited sample sizes. In Arizona, Taylor (1935) estimated densities ranging from 0.4 to 34 individuals/km2; those estimates were based upon the number of North American Porcupines killed per area, and thus preclude making comparisons. Ilse and Hellgren (2001) estimated porcupine densities in pinyon-juniper woodlands of Texas to be 1.9 individuals/km2. Overall, a recent study suggested that the range distribution of North American Porcupines has expanded in recent years in south-central United States and northern Mexico (Barnes and Hoffman 2023). Herein, we provided minimum density estimates for North American Porcupines in North Dakota, with an overall minimum winter density estimate of about 0.1 individuals/km2 in the early 1960s (Table 1). North Dakota is the least forested state in the union with <5% in forest cover (Seabloom 2020). More than 10% of the badlands is in shrub or forest canopy cover (Jensen 1988). Although the Badlands physiographic region appears to support the most and possibly some of the best forested habitat in the state for North American Porcupines, the observed overall density was the lowest. Cattle ranching and hunting are prominent land uses in the Badlands. Loggers, ranchers, and Canis familiaris Linnaeus (Dog) owners have a long history of killing North American Porcupines to protect trees, livestock, and Dogs (Bailey 1926, Roze 1989, Seabloom 2020). As a result, North American Porcupine densities may have been suppressed. Lower observed densities in the Badlands also likely were due to reduced ability to see individuals in thick stands of Juniperus scopulorum Sarg. (Rocky Mountain Juniper). National parks, wildlife refuges and heavily forested river bottoms may provide North American Porcupines with a level of security not found on private rangeland. Use of small fixed-wing planes to conduct low-altitude aerial surveys in open prairie terrain can provide a unique opportunity to determine winter population density estimates for North American Porcupines, particularly in areas without coniferous trees and shrubs. Future use of aerial surveys for North American Porcupines should include ground searches of survey areas to determine detection rates. Since the 1960s, dramatic changes in habitat have occurred across North Dakota. Tree rows and shelterbelts are being removed at an increasing rate, road access to the Badlands and other areas has increased with energy development, and predators of North American Porcupines such as Fishers and Puma concolor (Linnaeus) (Mountain Lions) have become established in some areas. As a result, current densities of North American Porcupines in North Dakota might now be lower than they were in the 1960s. Acknowledgements We thank the reviewers for helpful comments and suggestions. We thank C. Penner and A. Powers for assistance with figures and tables, respectively. Financial support for collection and analysis of these data was provided by the North Dakota Game and Fish Department, Federal Aid Project W-67-R. Literature Cited Bailey, V. 1926. A biological survey of North Dakota. North American Fauna 49:1–226. Band, A.L. 1996. Population characteristic and habitat use of porcupines in a partially burned landscape in northwestern Wyoming. Graduate Student Theses, Dissertations, and Professional Papers. 6531. University of Montana, Missoula, MT, USA. 54 pp. Barnes, E.F., and J.D Hoffman. 2023. Significant range expansions in eight species of North American mammals. Occasional Papers, Museum of Texas Tech University 385:1–29. Earle, R.D., and K.R. Kramm. 1982. Correlation between fisher and porcupine abundance in Upper Michigan. American Midland Naturalist 107:244–249. Hendrick, P., and H.F. Allard. 1988. Winter food habits of prairie porcupines in Montana. Prairie Naturalist 20:1–6 Ilse, L.M., and E.C. Hellgren. 2001. Demographic and behavioral characteristics of North American porcupines (Erethizon dorsatum) in pinyon-juniper woodlands of Texas. American Midland Naturalist 146:329–338. Jensen, W.F. 1988. Summer and fall ecology of mule deer in the North Dakota badlands. Ph.D. Dissertation. Dept. of Biology, University of North Dakota, Grand Forks, ND, USA. 220 pp. McKenzie, J.V. 1958. White-tailed deer census. Big Game Surveys and Investigations. PR Report W-37-R-5. Job 1. North Dakota Game and Fish Department, Bismarck, ND, USA. 10 pp. Reek, W.A. 1942. Notes on the Canada porcupine in the maritime provinces. Forestry Chronicle 18:182–187. Roze, U. 1984. Winter foraging by individual porcupines. Canadian Journal of Zoology 62:2425–2428. Roze, U. 1989. The North American porcupine. Smithsonian Institute Press, Washington, D.C. USA. 261 pp. Seabloom, R.W. 2020. The Mammals of North Dakota. North Dakota State University Press, Fargo, ND. 470 pp. Shapiro, J. 1949. Ecological and life history notes on the porcupine in the Adirondacks. Journal of Mammalogy 30:247–257. Smith, G.W. 1977. Population characteristics of the porcupine in northeastern Oregon. Journal of Mammalogy 58:674–676. Taylor, W.P. 1935. Ecology and life history of the porcupine (Erethizon epixanthum) as related to the forests of Arizona and southwestern United States. University of Arizona Biological Science Bulletin No. 3:1–177 pp.