The common kestrel was
formally described in 1758 by the Swedish naturalist
Carl Linnaeus in the
tenth edition of his
Systema Naturae under the current
binomial name Falco tinnunculus. Linnaeus specified the
type location as Europe but restricted this to Sweden in 1761. The genus name is
Late Latin from
falx,
falcis, a
sickle, referencing the claws of the bird. The species name
tinnunculus is
Latin for "kestrel" from "tinnulus", "shrill". The Latin name
tinnunculus had been used by the Swiss naturalist
Conrad Gessner in 1555. The word "kestrel" is derived from the French crécerelle which is diminutive for crécelle, which also referred to a bell used by lepers. The word is earlier spelt 'c/kastrel', and is evidenced from the 15th century. The kestrel was once used to drive and keep away pigeons. roughly 2.5–2
mya, probably starting in tropical East Africa, as indicated by
mtDNA cytochrome b sequence data analysis and considerations of
biogeography. The
rock kestrel (
F. rupicolus), previously considered a subspecies, is now treated as a distinct species. Most differ little, and mainly in accordance with
Bergmann's and
Gloger's rules. Tropical African forms have less grey in the male plumage. •
F. t. tinnunculus Linnaeus, 1758 –
temperate areas of Europe, North Africa, the
Middle East, and Asia north of the
Hindu Kush-
Himalaya mountain ranges to the NW
Sea of Okhotsk region. Northern Asian populations
migrate south in winter, apparently not crossing the Himalayas but diverting to the west. •
F. t. perpallidus (
Clark, AH, 1907) – northeast Siberia to northeast China and
Korea Peninsula •
F. t. interstinctus McClelland, 1840 – breeds
East Asia from
Tibet to
Korea and
Japan, south into
Indochina. Winters to the south of its breeding range, from northeastern
India to the
Philippines (where it is localized, e.g. from
Mindanao only two records exist). Has dark heavily marked birds and has a foxed red phase but not reliably identified in the field. •
F. t. objurgatus (
Baker, ECS, 1929) –
Western,
Nilgiris and
Eastern Ghats of India;
Sri Lanka. Heavily marked, has rufous thighs with dark grey head in males. •
F. t. canariensis (
Koenig, 1890) –
Madeira and western
Canary Islands •
F. t. dacotiae Hartert, EJO, 1913 – eastern Canary Islands:
Fuerteventura,
Lanzarote,
Chinijo Archipelago. •
F. t. neglectus Schlegel, 1873 – northern
Cape Verde Islands •
F. t. alexandri Bourne, 1955 – southwestern Cape Verde Islands. •
F. t. rupicolaeformis (
Brehm, CL, 1855) –
Arabian Peninsula except in the desert and across the
Red Sea into Africa •
F. t. archerii (Hartert, EJO &
Neumann, 1932) –
Somalia, coastal
Kenya, and
Socotra •
F. t. rufescens Swainson, 1837 –
Sahel east to
Ethiopia, southwards around
Congo Basin to south
Tanzania and northeast
Angola. The common kestrels of Europe living during cold periods of the
Quaternary glaciation differed slightly in size from the current population; they are sometimes referred to as the
paleosubspecies F. t. atavus (
see also Bergmann's rule). The remains of these birds, which presumably were the direct ancestors of the living
F. t. tinnunculus (and perhaps other subspecies), are found throughout the then-unglaciated parts of Europe, from the
Late Pliocene (
ELMA Villanyian/
ICS Piacenzian,
MN16) about 3
million years ago to the
Middle Pleistocene Saalian glaciation which ended about 130,000 years ago, when they finally gave way to birds indistinguishable from those living today. Some of the
voles the Ice Age common kestrels ate—such as
European pine voles (
Microtus subterraneus)—were indistinguishable from those alive today. Other prey species of that time
evolved more rapidly (like
M. malei, the presumed ancestor of today's
tundra vole M. oeconomus), while yet again others seem to have gone entirely
extinct without leaving any living descendants—for example
Pliomys lenki, which apparently fell victim to the
Weichselian glaciation about 100,000 years ago. == Description ==