A history of land mammals in the western hemisphereScott, William Berryman
History
A history of land mammals in the western hemisphere
Scott, William Berryman
Mammals; Mammals, Fossil
II. ARCTOGÆIC REALM. { 1. _Malagasy Region._—Madagascar.
{ 2. _Ethiopian Region._—Africa south of the
{ Sahara Desert.
{ 3. _Oriental Region._—Southern peninsulas of
{ Asia, Malay Archipelago.
{ 4. _Holarctic Region._—N. Africa, Europe, Asia,
{ (except southern part), boreal N. America.
{ 5. _Sonoran Region._—Remainder of N. America
{ (except lowlands of Mexico).
North America, as is expressed by this scheme, is zoölogically composite;
the northern half, including nearly all of Canada, belongs to the vast
Holarctic Region, which also comprises Europe, Africa north of the
Sahara and Asia north of the Himalaya Mountains. The remainder of the
continent, exclusive of the Mexican coastal lowlands, is set off as the
Sonoran Region. Inasmuch as we have here to do with broadly continuous
land-areas, not demarcated by great physical features, and as the genera
and species of mammals differ greatly in regard to their ability to
withstand a wide range of climatic variations, it is not to be expected
that the boundaries between the regions which make up North America
should be very sharply drawn. It is not surprising, therefore, to find
a transition zone, extending all across the continent, in which the
Holarctic and Sonoran faunas mingle, or that Central America should,
in considerable measure, be transitional to South America, though
zoölogically a part of the latter.
[Illustration: FIG. 53.—Zoölogical Divisions of North America. (After
Merriam.)]
Dr. Merriam’s arrangement, which deals only with North America
without reference to the Old World, divides the land into a series of
transcontinental zones, which he calls the Arctic, Boreal, Upper and
Lower Sonoran and Tropical. These zones have very irregular and sinuous
boundaries, which follow lines of equal temperature (isothermal lines)
during the breeding season, May, June and July, the tortuous boundaries
being conditioned by topographical features, which deflect the isothermal
lines.
[Illustration: FIG. 54.—Polar Bear (_Thalarctus maritimus_).—By
permission of the N.Y. Zoölog. Soc.]
The Arctic zone is part of a circumpolar area, which is very much the
same in North America, Asia and Europe; and in any of these continents
the fauna differs much more from that of the contiguous zone to the south
than from the Arctic fauna of another continent. There are some local
differences, but the characteristic mammals of this Arctic zone are the
Polar Bear, Arctic Fox, Musk Ox, Barren-ground Caribou, Lemming, Arctic
Hare, and a marmot. Most, if not all, of these forms are of Old World
origin.
[Illustration: FIG. 55.—Musk Ox (_Ovibos wardi_) female; the males have
much larger horns.—By permission of the N.Y. Zoölog. Soc.]
Public-domain text, read in full here on John Shaqi.
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