2011 NORTHEASTERN NATURALIST 18(4):521–526
Non-genetic Data Supporting Genetic Evidence for the
Eastern Wolf
L. David Mech*
Abstract - Two schools of thought dominate the molecular-genetics literature
on Canis spp. (wolves) in the western Great Lakes region of the US and Canada:
(1) they are hybrids between Canis lupus (Gray Wolf) and Canis latrans (Coyote),
or (2) they are hybrids between the Gray Wolf and Canis lycaon (Eastern Wolf). This
article presents 3 types of non-genetic evidence that bears on the controversy and concludes
that all 3 support the second interpretation.
Introduction
Wilson et al. (2000) presented molecular genetic evidence for a new interpretation
of the taxonomy of North American Canis species and proposed that
the Canis lupus L. (Gray Wolf) subspecies lycaon, is a separate species, similar
to Canis rufus Audubon and Bachman (Red Wolf), that should be named Canis
lycaon Schreber (Eastern Wolf). The study was based on analyses of 8 microsatellite
loci and mitochondrial DNA (mtDNA) control-region sequences from
wolves of southeastern Ontario from the 1960s. None showed Gray Wolf mtDNA,
and estimates were that mtDNA sequences from both the Eastern Wolf and Red
Wolf diverged from Canis latrans Say (Coyote) 150,000–300,000 years ago, as
compared to divergence from the Gray Wolf around 2 million years ago. Based
on this evidence, Wilson et al. (2000) suggested that both the Red Wolf and Eastern
Wolf evolved in North America along with the Coyote, as opposed to the
Gray Wolf, which evolved in the Old World. Wilson et al. (2000) also compared
their microsatellite allele frequencies with published frequencies of wolves and
Coyotes from other areas (Roy et al. 1994, 1996), and found both microsatellite
evidence and mtDNA evidence of Eastern Wolves as far west as Manitoba.
Previously, Lehman et al. (1991) and Wayne and Lehman (1992) had considered
the same mtDNA haplotypes as evidence of Gray Wolf x Coyote hybridization,
and the Wayne school continued to interpret them that way (Koblmuller et al.
2009, Leonard and Wayne 2008). Wilson et al. (2000) based their interpretation
on the fact that those haplotypes have not been found in extant non-hybridizing
Coyote populations and on other considerations. Wayne and Vila (2003:235, 236)
agreed that the Wilson et al. (2000) interpretation should be further tested.
Kyle et al. (2006) examined in detail whether the genetic data support the Eastern
Wolf as a distinct species and considered the alternate hypotheses that the Eastern Wolf
is a subspecies of the Gray Wolf or derived from hybridization between the Gray
Wolf and Coyote. Kyle et al. (2006) rejected the subspecies and hybrid hypotheses
*US Geological Survey, Northern Prairie Wildlife Research Center, 8711 37th Street, SE,
Jamestown, ND 58401-7317; mailing address - US Geological Survey, The Raptor Center,
1920 Fitch Avenue, University of Minnesota, St. Paul, MN 55108; mechx002@umn.
edu; david_mech@usgs.gov.
522 Northeastern Naturalist Vol. 18, No. 4
and accepted Eastern Wolf as a species, which other authors have also since accepted
(Fain et al. 2010, Murray and Waits 2007, Rutledge et al. 2009, Way et al. 2010,
Wheeldon 2009, Wheeldon and White 2009, Wheeldon et al. 2010).
Leonard and Wayne (2008) reported on divergent mtDNA haplotypes in historic
Great Lakes wolves and suggested they belonged to a distinct mtDNA lineage
referred to as the “Great Lakes wolf ” that originated from ancient hybridization
between Coyote females and male Gray Wolves. However, Wheeldon and White
(2009) showed that 2 of these haplotypes were similar to, or the same as, haplotypes
of the Eastern Wolf. Meanwhile, Koblmuller et al. (2009) interpreted genetic
data from Great Lakes wolves without distinguishing between Coyote and Eastern
Wolf lineages, instead referring only to Gray Wolf and Coyote lineages, but found
all 3 Eastern Wolf mtDNA haplotypes of Wilson et al. (2000) among both historical
and modern wolves of the western Great Lakes region. Furthermore, each school of
molecular genetics (the Wilson school and the Wayne school) mustered additional
genetic data and arguments in support of their interpretation. The most apparent
conflicting issue is the lack of consensus on whether the Coyote-like mtDNA sequences
in hybridized wolves are those of actual Coyotes or of the Eastern Wolf.
Regarding the current wolf population in the Great Lakes region, from northeastern
Ontario west across Ontario, Michigan, Wisconsin, Minnesota, and at
least part of Manitoba, the disparate schools of thought are that those wolves are
either hybrids between Gray Wolf x Eastern Wolf (Wheeldon 2009, Wilson et
al. 2009) or Gray Wolf x Coyote (Koblmuller et al. 2009, Lehman et al. 1991).
The Gray Wolf has been on the US Endangered Species List since 1967 and is
protected by the Endangered Species Act of 1973. Although it has been delisted
a few times, legal issues have forced it back on the list. In addition, claims have
been made, based on genetic analyses, that the native Great Lakes wolves were
not restored (Leonard and Wayne 2008, but cf Mech 2009, Wheeldon and White
2009) and that the Great Lakes wolves are a “unique population or ecotype of
Gray Wolves” (Koblmuller et al. 2009, but cf Cronin and Mech 2009).
Therefore, it is important to try to determine the correct interpretation of the
Coyote-like mtDNA haplotypes by examining evidence other than the genetic
data. This article attempts to do that.
Discussion
There are 3 types of non-genetic evidence relevant to the question of whether
the Coyote-like mtDNA haplotypes in hybridized wolves are those of Coyotes
(the Wayne interpretation) or those of the Eastern or Red Wolf that putatively
evolved with Coyotes (the Wilson interpretation): (1) morphological data, (2)
reproductive information, and (3) behavior. Some of this evidence has been discussed
before, but is included here for the sake of completeness.
Phenotypically the Gray Wolf, the putative Eastern Wolf and the Red Wolf, and
the Coyote are similar, with body and skull sizes decreasing from the Gray Wolf
to the Coyote. There seems to be agreement that the Eastern Wolf (formerly C. l.
lycaon) and the Red Wolf appear intermediate to the Gray Wolf and the Coyote
(Kolenosky and Standfield 1975, Mech 1970). However, the picture is further confounded
by the fact that, in eastern North America, hybridization occurred between
2011 L.D. Mech 523
western Coyotes and the Eastern Wolf (Kays et al. 2009, Kolenosky and Standfield
1975, Kyle et al. 2006, Way et al. 2010, Wheeldon et al. 2010, Wilson et al. 2009).
The crux of distinguishing between the Wayne and Wilson interpretations is
determining whether Coyotes have ever hybridized with the Gray Wolf or whether
they even can (Mech 2010). Morphological evidence that would help distinguish
whether phenotypic wolves with Coyote-like mtDNA are Gray Wolves that have
hybridized with Coyotes or with Eastern Wolves would be (1) the existence of
Canis that generally appeared intermediate between Gray Wolves and Coyotes or
that generally appeared intermediate between Gray Wolves and Eastern Wolves,
or (2) skulls that appear similarly intermediate.
As for the former, Great Lakes (Minnesota, Wisconsin, Michigan) wolves look
like Gray Wolves both in appearance and size, although females in some areas are
up to 12% lighter weight, and males up to 15% lighter weight than Gray Wolves
(Mech and Paul 2008). Similarly, skulls of 1970–1976 Great Lakes wolves are similar
to those of the Gray Wolf (Nowak 2009), although a sample taken later possess
narrower rostra (Mech et al., in press). In both body mass and skull measurements,
the Great Lakes wolves are more similar to the Gray Wolf than to the Coyote, providing
evidence that they have resulted not from Gray Wolf x Coyote but rather
from Gray Wolf x Eastern Wolf. Furthermore, the only animals or skulls that have
been recorded that appeared to be a product of mating between Coyote and any
kind of wolf were those in eastern Canada, which according to the Wilson interpretation
would have resulted from matings between Coyotes and Eastern Wolves
(Kolenosky and Standfield 1975, Sears et al. 2003). Not only do these hybrids only
occur in eastern Canada and the northeastern US, but their sizes and skulls are intermediate
between Eastern Wolves and Coyotes, not between Gray Wolves and
Coyotes (Kolenosky and Standfield 1975:Fig. 5–2).
Table 1. Evidence of wolves killing Coyotes in the Great Lakes region. No. = number of wolfkilled
Coyotes.
Location No. Source
Michigan 1+ B. Roell (Department of Natural Resources, South Marquette, MI, pers. comm.)
Wisconsin 3 R.P. Thiel (2006) and (Department of Natural Resources, Babcock, WI, pers.
comm.)
2 R. Schultz (Department of Natural Resources, Woodruff, WI, pers. comm.)
1 J. Evrard (Department of Natural Resources, Grantsburg, WI, pers. comm.)
Minnesota 1 M.E. Nelson (US Geological Survey, Eli, MN, pers. comm.)
1 L.D. Mech (unpubl. data)
2 Berg and Chesness 1978
Eastern 0A B. Patterson, (Ontanrio Ministry of Natural Resources, Petersborough, ON, Canada,
Ontario pers. comm.)
0 J.B. Theberge and M.T. Theberge (1998, 2004) and (University of Waterloo,
Waterloo, ON, Canada, pers. comm.)
0 G. Kolenosky (Ontanrio Ministry of Natural Resources, Petersborough, ON,
Canada, pers. comm.)
Quebec 0 M. Villemure (2003)
A“We had Coyote-like animals killed by wolves, but they were in ‘wolf’ packs and functioning
like wolves.”
524 Northeastern Naturalist Vol. 18, No. 4
It seems highly relevant that, although hybrids of Eastern Wolves and Coyotes
have been recorded for years in eastern Canada, no such phenotypic hybrid
between Gray Wolves and Coyotes has been found west of there. Neither has
genetic evidence of Coyotes been found in Gray Wolves from Montana, Wyoming,
or Manitoba (Carbyn 1982, Paquet 1992, Pilgrim et al. 1998), where no
one disputes that the wolves are Gray Wolves and have long been sympatric with
Coyotes. In Minnesota, Wisconsin, and Michigan alone, over 2000 wolves have
been examined (Beyer et al. 2009, Mech and Paul 2008, Nowak 2009, Wydeven
et al. 2009) with no one reporting an apparent Gray Wolf x Coyote hybrid. This
finding supports the Wilson interpretation.
The second line of relevant non-genetic evidence that might help distinguish
between the Wayne and Wilson interpretations would be reproductive experiments.
A wolf from eastern Canada (putative Eastern Wolf) has successfully bred
in captivity with a Coyote (Kolenosky 1971), but no one has attempted to mate
a Gray Wolf from the West with a Coyote. If such an experimental mating were
accomplished, it would lend some support to the Wayne interpretation.
The third type of non-genetic evidence relevant to the Wayne-Wilson difference
in interpretation is behavioral. If a Gray Wolf mated with a Coyote, there had to
be some tolerance between the 2 species. Here the record is clear. From Michigan
westward, Gray Wolves kill Coyotes (summary by Ballard et al. 2003, Berger and
Gese 2007), whereas I could find no record of wolves east of Michigan killing Coyotes,
despite considerable field work there on both species (Table 1).
In the Great Lakes area, the extant wolf population, considered Gray Wolf x
Coyote under the Wayne interpretation and Gray Wolf x Eastern Wolf under the
Wilson interpretation, does kill Coyotes (Table 1), although a few observations
of wolves and Coyotes tolerating each other have been made (Thiel 2006). On
balance, however, Great Lakes wolves kill Coyotes as do wolves farther west, a
fact that makes it unlikely that the 2 species would mate. This is further evidence
that the Coyote-like mtDNA sequences found in some Great Lakes wolves are
not derived from Coyotes, a finding that leaves the alternative—that they derive
from the Eastern Wolf—more plausible.
In summary, non-genetic evidence based on morphology, reproduction, and
interspecific relations all support the contention that Gray Wolf x Coyote hybridization
is rare to non-existent from approximately Michigan westward. This
finding then lends support to the Wilson (2000, 2009) hypothesis that the Coyotelike
genetics found in wolves of the Great Lakes region represent the Eastern
Wolf rather than the Coyote.
Acknowledgments
This study was supported by the US Geological Survey. I thank T. Wheeldon and S.R.
Fain for critiquing an earlier draft and making helpful suggestions for improving it.
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