1984
DOI: 10.2307/3808476
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Home Ranges, Activity, and Habitat Use by Gray Foxes in an Oak-Hickory Forest

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Cited by 37 publications
(35 citation statements)
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“…Gray foxes seem to behave as habitat specialists in brushy habitats; this contrasts with most assessments of their habitat use indicating generalist habits and usage of both open and brushy habitats (Trani 1980;Haroldson and Fritzell 1984;Harrison 1997). 2.…”
Section: Discussionmentioning
confidence: 93%
“…Gray foxes seem to behave as habitat specialists in brushy habitats; this contrasts with most assessments of their habitat use indicating generalist habits and usage of both open and brushy habitats (Trani 1980;Haroldson and Fritzell 1984;Harrison 1997). 2.…”
Section: Discussionmentioning
confidence: 93%
“…It was found that TSs with the highest FO were the sites with the most dense vegetation cover, which is considered to be protective of daytime movements across the range of the gray fox (Haroldson and Fritzell 1984;Farias et al 2005;Sollmann et al 2013). Fritzell and Haroldson (1982), considering different locations, seasons and estimation methods, found that the density of the gray fox varied from 1.2 to 2.1 individuals per km², which is consistent with the density found in this study (1.73).…”
Section: Discussionmentioning
confidence: 99%
“…Indeed, given the limited ranges of the smaller mammals (<10 km 2 , Gehrt and Fritzell, 1997;Goheen and Swihart, 2005;Haroldson and Fritzell, 1984) we would not expect their diets to include food from regions with radically different geological ages, though the presence of migratory prey animals may have contributed to the 87 Sr/ 86 Sr values of the gray fox. It is possible that the isotopic composition of the human material reflects the homogenization of strontium values due to the heterogeneity of the mid-Hudson Valley geology.…”
Section: Establishing the Local Newburgh 87 Sr/ 86 Sr Signaturementioning
confidence: 96%
“…The predominant component is the Ordovician age Normanskill Formation, a shaley siltstone. The area also contains Gehrt and Fritzell, 1997;Goheen and Swihart, 2005;Haroldson and Fritzell, 1984) it is possible that they ranged into the nearby Cambro-Ordovician, Cambrian, Precambrian formations. The modern snails were selected such that they should be representative of the major geological units in the Newburgh area: Cronomer Hill formation (sample F5), the Poughquaq Formation (sample F6), Wappinger Group (sample F7), and Normanskill Formation (sample F8).…”
Section: Strontium Analyses and New York Geologymentioning
confidence: 99%