white gyrfalcon ×
saker The gyrfalcon is a member of the
hierofalcon complex. In this group, ample evidence indicates
hybridisation and
incomplete lineage sorting, which confounds analyses of
DNA sequence data to a massive extent. The
radiation of the entire living diversity of hierofalcons took place around the
Eemian Stage at the start of the
Late Pleistocene. It represents lineages that expanded into the
Holarctic and
adapted to local conditions; this is in contrast to less northerly populations of northeastern
Africa (where the radiation probably originated) that evolved into the
saker falcon. Previous beliefs held that gyrfalcons hybridized with sakers in the
Altai Mountains, and this
gene flow contributed to the genetic lineage of the
Altai falcon. of unknown origin, theoretically any allele combination might be present. For instance, a mating of a pair of captive gyrfalcons is documented to have produced a
clutch of four young: one white, one silver, one brown, and one black. Molecular work suggests plumage color is associated with the
melanocortin 1 receptor gene (
MC1R), where a nonsynonymous point substitution was perfectly associated with the white/melanic polymorphism. but none of these are consistent and thus no living subspecies are currently accepted. The Icelandic population described as
F. r. islandus is perhaps the most distinct. The predominantly white Arctic forms are
parapatric and seamlessly grade into the
subarctic populations. The Icelandic types are presumed to have less
gene flow with their neighbors; they show less variation in plumage colors. Comprehensive
phylogeographic studies to determine the proper status of the Icelandic population have yet to be performed. A population genetic study, however, identified the
Iceland population as genetically unique relative to other sampled populations in both eastern and western Greenland,
Canada,
Alaska, and Norway. Further, within Greenland, differing levels of gene flow between western and eastern sampling locations were identified, with apparent asymmetric dispersal in western Greenland from north to south. This dispersal bias is in agreement with the distribution of plumage colour variants with white gyrfalcons in much higher proportion in north Greenland. Although further work is required to determine the ecological factors contributing to these distributions relative to plumage differences, a study using demographic data suggested that plumage color distribution in Greenland may be influenced by nesting chronology with white individuals and pairs laying eggs earlier in the breeding season and producing more offspring.
Swarth's gyrfalcon A
paleosubspecies,
Falco rusticolus swarthi, existed during the
Late Pleistocene (125,000 to 13,000 years ago). Fossils found in Little Box Elder Cave (
Converse County, Wyoming), Dark Canyon Cave (
Eddy County, New Mexico), and
McKittrick, California were initially described as
Falco swarthi ("Swarth falcon" or more properly "Swarth's gyrfalcon") on account of their distinct size. They have meanwhile proven to be largely inseparable from those of living gyrfalcons, except for being somewhat larger. Swarth's gyrfalcon was on the upper end of the present gyrfalcon's size range, with some stronger females even surpassing it. It seems to have had some adaptations to the temperate
semiarid climate that predominated in its range during the
last ice age. Ecologically more similar to current Siberian populations (which are generally composed of smaller birds) or to the
prairie falcon, this temperate
steppe population must have preyed on landbirds and mammals rather than the sea and landbirds which make up much of the American gyrfalcon's diet today. ==Ecology==