Appletons' Popular Science Monthly, December 1898: Volume LIV, No. 2, December 1898Various
Science
Appletons' Popular Science Monthly, December 1898: Volume LIV, No. 2, December 1898
Various
Science -- Periodicals; Technology -- Periodicals
On the whole, then, before the coming on of the Glacial epoch, we may
be pretty sure that plants and animals on the one hand had learned
organically and automatically to recognize the existence of the year
and to adapt themselves to it; and that men or the progenitors of
men on the other hand had also learned to correlate the recurrent
seasons of food supply with the movements of the sun, though nothing
equivalent to winter and summer as we know them to-day existed as
yet on any part of our planet. I say advisedly "on any part of our
planet," because even near the pole itself remains of a subtropical
vegetation in Tertiary times have been amply indicated. Nevertheless,
in all parts of the world then, as in the tropics now, we may gather
that plants and animals ran through annual cycles--that the year, as
I have put it, was organically recognized. Trees had their time to
sprout, to bud, to flower, to fruit, to seed, to shed their leaves
(in the evergreen way); birds had their time to nest and hatch out
their young; insects had their fixed periods for laying, for larval
life, for assuming the chrysalis form, for becoming winged beetles or
bees or butterflies. In one word, the year is a terrestrial reality,
not merely an astronomical fact, in the tropics now; it was a
terrestrial reality over the whole planet in the Tertiary period. But
it was hardly more marked, apparently, into distinct seasons than it
is marked to-day in the equatorial region. Rainfall and drought must
have had more to do in determining the annual cycles than winter and
summer.
From all this it must result that the conception of the year as an
epoch at all (save for advanced astronomy) is almost or entirely
due to that tilt of the earth's axis which causes the seasons--dry
or wet, cold or hot. Without the seasons, in one form or other, we
might have been ages longer in discovering the fact that the earth
moved round the sun, and that some three hundred and sixty-five days
(I omit those important fractions) were needed for its revolution.
Certainly, without the seasons, at least to the extent that they
occur in the tropics, plant and animal life could hardly have assumed
its fixed annual cycles, nor could early men have caught at the idea
of the year at all as a period of time, a unit of measurement.
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