|Taxonomic Notes: This species is placed in Lithobates by some authors, following Frost et al., 2006. This has been a controversial decision, because such well-known species as Rana catesbeiana, with an enormous literature, are made more obscure to many. What is not controversial is that Lithobates is the sister taxon of Rana, so the argument is simply one of Linnean ranks. AmphibiaWeb recommends treating Lithobates as a subgenus of Rana, with species names to be written as Rana (Lithobates) catesbeiana, as an example. This option preserves the maximal amount of phylogenetic information and preserves a long-standing taxonomy.|
© 2010 Matthew Niemiller (1 of 44)
Can you confirm these amateur observations of Rana palustris?
Rana palustris LeConte, 1825
1. Historical versus Current Distribution. Pickerel frogs (Rana palustris) are distributed from Nova Scotia and New Brunswick, west through southern Québec and Ontario, to Michigan, Wisconsin, and extreme southeastern Minnesota. From southeast Minnesota south along the Mississippi Drainage (west to extreme southeast Kansas and eastern Oklahoma, but absent from interior prairies of Illinois) to the Gulf Coast in eastern Texas. Absent from most of the eastern Gulf Coastal Plain (except Conecuh County, Alabama, and Escambia County, Florida). In the eastern United States, they are generally distributed from New England south to South Carolina and Georgia, where they are apparently absent from the Atlantic Coastal Plain (Smith, 1961; Schaaf and Smith, 1971; Pace, 1974; Mount, 1975; Ashton and Ashton, 1988; Conant and Collins, 1991).
One subspecies, R. p. mansuetti, was applied to populations along the Atlantic Coastal Plain by Hardy (1964), who noted selection pressures of floodplain swamps probably affect phenotype. That subspecies was synonomized by Schaaf and Smith (1970), who noted that the phenotype was not geographically restricted.
The similarity to northern leopard frogs (R. pipiens, Schaaf and Smith, 1970; Pace, 1974; Hunter et al., 1992; Redmer and Mierzwa, 1994) has lead to erroneous records. Around the peripheries of their range, pickerel frog populations may be localized in suitable habitat, and special efforts may be needed to detect new localities or to relocate them at or near historical localities (Redmer, 1998b). For example, during surveys in Illinois, pickerel frogs were found in 10 (~59%) of 17 counties with previous historical records, but five new county records also were reported (Walley, 1991; Redmer and Mierzwa, 1994; Redmer and Ballard, 1995; Redmer et al., 1995; Redmer, 1998b; Petzing et al., 1998). They may be extirpated in the urban Chicago region and at a locality in extreme southern Illinois (Mierzwa, 1998a; Redmer, 1998b). Vogt (1981) reported only 15 active localities in Wisconsin, but Johnson (1984) identified 61 active localities (a 407% increase) in the state.
2. Historical versus Current Abundance. Unknown. It is unclear whether pickerel frogs have suffered range-wide decline, though their somewhat specialized habitat characteristics and intolerance of pollution may make them vulnerable to human activities (Redmer and Mierzwa, 1994; Harding, 1997). Because pickerel frogs are sometimes difficult to detect (Mossman et al., 1998; Redmer, 1998b), periodic species-specific surveys may be needed to monitor populations.
3. Life History Features.
i. Breeding migrations. Timing and length of breeding season follow a south–north cline. The reported breeding season ranges from December–May in the south (Mount, 1975; Garrett and Barker, 1987; Dundee and Rossman, 1989; Trauth et al., 1990; Hardy and Raymond, 1991), March–May in the middle of their range (Walker, 1946; Minton, 1972; Vogt, 1981; Johnson, 1984; Green and Pauley, 1987; Johnson, 1987; Shaffer, 1991; Redmer and Mierzwa, 1994; Redmer, 1998b), and May–June in the north (Hunter et al., 1992; Oldfield and Moriarty, 1994).
Immigration takes place after one or a combination of the following occurs: water temperatures reach 7–18 ˚C (Wright, 1914; Moore, 1939; Pope, 1944; Johnson, 1984; Hardy and Raymond, 1991), air reaches 10–26 ˚C (Wright, 1914; Pope, 1944; Johnson, 1984), or surface soil temperature reaches 7–12 ˚C (Hardy and Raymond, 1991). Weather conditions greatly affect emergence from caves where frogs winter (Resetarits, 1986). In southwestern Illinois, males and gravid females are found on roads as they move towards breeding ponds during late March and April (unpublished data).
ii. Breeding habitat. Breed in a variety of aquatic habitats adjacent to adult habitat, including woodland pools and ponds, stream overflow pools, farm ponds, sinkhole ponds, floodplain wetlands, marshes, and flooded quarries (Smith, 1961; DeGraaf and Rudis, 1983; Johnson, 1984; Resetarits, 1986; Adams and Lacki, 1993; Redmer and Mierzwa, 1994; Harding, 1997; Redmer, 1998b). Brown (D.R., 1984) reported oviposition in a cave pool in Indiana.
i. Egg deposition sites. Oviposition takes place more often in eutrophic zones than oligotrophic ones, but dissolved oxygen was high and water temperature was cool at breeding sites in Wisconsin (Johnson, 1984). Eggs are attached to dead or submerged vegetation at or near the water surface and are often concentrated in portions of the pool that receive greatest sunlight (Johnson, 1984; Harding, 1997; unpublished data).
ii. Clutch size. Unknown. Egg masses are spherical; while the inner most embryos develop in a more hypoxic environment than those in the outer egg mass, ciliated epithelia of the embryos are used to create convective ventilation (Burggren, 1985). Under natural conditions, larvae hatch within 10–24 d (Johnson, 1984; Harding, 1997). In the lab, eggs hatch in 6–8 d (unpublished data).
C. Larvae/Metamorphosis. Under natural conditions, larvae begin to metamorphose within 60–90 d after hatching (Johnson, 1984; Harding, 1997). In the lab, metamorphosis occurs from 75–90 d following hatching (unpublished data).
D. Juvenile Habitat. Specific data are not available, presumably similar to that of adults.
E. Adult Habitat. Often reported to prefer streams or ponds with cool, unpolluted water (Dickerson, 1906; Toner and St. Remy, 1941; DeGraaf and Rudis, 1983; Cook, 1984; Conant and Collins, 1991; Harding, 1997), but Johnson (1984) found no evidence to support this. Stream corridors may be important conduits for movements in forests (Gibbs, 1998a). Some coastal and floodplain populations are reported to occupy swamps (Smith, 1961; Hardy, 1964; Schaaf and Smith, 1970). The most cave-adapted North American anuran, they are often abundant in areas of karst topography (Smith, 1961; Schaaf and Smith, 1970; McDaniel and Gardner, 1977; Resetarits, 1986). Individuals occurred in a Missouri cave from July–March (Resetarits, 1986). They may also enter abandoned mines (Heath et al., 1986). Other habitats include wooded wetlands, bogs, and shrubby, open meadows (Dickerson, 1906; DeGraaf and Rudis, 1983; Johnson, 1984; Redmer and Mierzwa, 1994; Harding, 1997). They prefer the margins of aquatic habitats with dense herbaceous vegetation (Pope, 1944; DeGraaf and Rudis, 1983; Johnson, 1984; Redmer and Mierzwa, 1994). Rural land use proximal to occupied habitats may or may not influence occurrence, though adults may be less abundant where stream bank vegetation is mowed or grazed (Johnson, 1984) or absent from areas that are logged (Cook, 1984).
F. Home Range Size. Unknown.
G. Territories. Unknown.
H. Aestivation/Avoiding Dessication. True aestivation is unknown. Warm summer temperatures may cause individuals to become nocturnal (Harding, 1997). In Missouri, some individuals retreat to caves during summer (Resetarits, 1986). Critical thermal maxima and capacity for acclimation to changing thermal conditions have been reported (Moore, 1939; Brattstrom and Lawrence, 1962; Brattstrom, 1968).
I. Seasonal Migrations. Pickerel frogs migrate from breeding areas (pools or ponds) to summer habitat (stream sides) where individuals may remain sedentary during spring and summer until they return to hibernacula in the fall (Johnson, 1984).
J. Torpor (Hibernation). Overwinter in the mud bottoms of ponds (DeGraaf and Rudis, 1983; Green and Pauley, 1987; Harding, 1997), ravines (Wright, 1914; DeGraaf and Rudis, 1983), under mud, rock, or debris in spring seeps and pools (Johnson, 1984), and in or around the edges of pools in caves (Resetarits, 1986). In spring-fed habitats, individuals may remain active (Pope, 1944; Harding, 1997).
K. Interspecific Associations/Exclusions. Often reported to exclude northern leopard frogs (Manion and Cory, 1952; Johnson, 1984; Conant and Collins, 1991), but the reasons are unknown. It is believed that skin toxins (see "Anti-predator Mechanisms" below) may kill other anurans kept in the same collecting container (Behler and King, 1998). Because of their anti-predator effect, it has been suggested that toxic skin secretions may be an adaptive advantage that makes Pickerel frogs more abundant than northern leopard frogs where they are sympatric (Dunn, 1935). Experimental evidence indicates that larvae compete with those of American toads (Bufo americanus; Wilbur and Fauth, 1990), but this is not affected by reproductive phenology (Alford, 1989b).
L. Age/Size at Reproductive Maturity. Age at reproductive maturity is unknown. Size at maturity is sexually dimorphic, with females averaging larger than males (Walker, 1946; Smith, 1961; Johnson, 1984; Resetarits and Aldridge, 1988; Hardy and Raymond, 1991). Minton (2001) reports a size range of 43.0 to 56.5 mm (mean 52.0) for adult males and from 54 to 78 mm (mean 64.0) for adult females.
M. Longevity. Unknown.
N. Feeding Behavior. Detailed studies of diet are unknown. Adults are reported to feed on insects, spiders, and other invertebrates (Pope, 1944; Harding, 1997). Tadpoles feed on algae and detritus (Pope, 1944; Harding, 1997).
O. Predators. Few observations of natural predation have been reported. Applegate (1990) reported predation by bald eagles (Haliaeetus leucocephalus), and Beane (1990) reported two frogs from the stomach of a mink (Mustela vison). Captive bullfrogs (Rana catesbeiana) and green frogs (R. clamitans) will eat small adults (Pope, 1944). A number of other vertebrate species (such as snakes, birds, and raccoons) may prey on adults. Some observations and experiments suggest that this species is distasteful to some predators (see "Anti-predator Mechanisms" below). Humans use adults as fishing bait (Cook, 1984). Several fish species were listed as potential tadpole predators in a stream (Holomuzki, 1995). Predators in experimental studies of larvae included newts (Notophthalmus viridescens), dragonfly naiads (Anax sp.), and diving beetles (Dytiscus verticalis; Brodie and Formanowicz, 1983; Wilbur and Fauth, 1990). Various other aquatic predators may prey on tadpoles.
P. Anti-Predator Mechanisms. Adults may have skin secretions that are toxic or distasteful to predators (Dickerson, 1906; Schaaf and Smith, 1970), and the bright yellow-orange colors on the concealed surface of the hind legs may serve to warn predators (Wright and Wright, 1949). Published observations and experimental evidence both support (Wright, 1932; Pope, 1944; Wright and Wright, 1949; Formanowicz and Brodie, 1979) and question (Mulcare, 1965) whether skin secretions are toxic or distasteful to predators. A combination of defensive posture and distasteful skin secretions may make this species unpalatable to shrews (Formanowicz and Brodie, 1979). Defensive behaviors and postures may be used in response to snakes (Marchisin and Anderson, 1978). In streams, choice of oviposition sites may make tadpoles unavailable to predatory fishes (Holomuzki, 1995). Unpalatability, rapid growth/size, or behavior (reduced activity or use of fish inaccessible areas) have been suggested as anti-predator mechanisms of tadpoles (Formanowicz and Brodie, 1982; Brodie and Formanowicz, 1983; Holomuzki, 1995).
Q. Diseases. Little is known about natural disease and non predation-caused mortality. A "red-leg" bacterial infection was reported in a cave (Lee and Franz, 1973). Johnson (1984) speculated that disease may have caused declines in Wisconsin during the 1970s. Devillars and Exbryant (1992) listed this species as one affected by a residue of the toxic pesticide dichlorodiphenyl trichloroethane (DDT).
R. Parasites. Reported parasites include trematodes (Bosma, 1934; Kuntz, 1941; Rankin, 1945; Goodchild, 1948; Walton, 1949; Bouchard, 1951; Coggins and Sajdak, 1982; McAllister et al., 1995b), cestodes (McAllister et al., 1995b), nematodes (Walton, 1929; Harwood, 1930, 1932; Coggins and Sajdak, 1982; Rankin, 1945; Baker, 1978a; McAllister et al., 1995b), and mites (Loomis, 1956; Murphy, 1965; McAllister et al., 1995b). Parasitic and commensal protozoans have also been reported (Metcalf, 1923; Walton, 1963; McAllister et al., 1995b; McAllister and Trauth, 1996).
4. Conservation. Pickerel frogs are listed as Declining in Iowa (Christiansen, 1981), as Declining and a Species of Special Concern in Wisconsin (Casper, 1998; Mossman et al., 1998) and (due to restricted range) a Species of Special Concern in Minnesota (Oldfield and Moriarty, 1994; Lannoo, 1998d). Pickerel frogs may be extirpated in Kansas (Platt et al., 1974; Collins, 1993). Some authors report that they are common regionally (DeGraaf and Rudis, 1983; Green and Pauley, 1987; Johnson, 1987; Hunter et al., 1992), while others report that they are rare, uncommon, or localized (Minton, 1972; Pentecost and Vogt, 1976; Vogt, 1981; Christiansen and Bailey, 1991; Redmer and Mierzwa, 1994; Harding, 1997; Redmer, 1998b).
Literature references for Amphibian Declines: The Conservation Status of United States Species, edited by Michael Lannoo, are here.
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