0005The canopy ,the upper level of the trees in the rain forest, holds a plethora of climbing mammals of moderately large size, which may include monkeys, cats, civets, and porcupines. Smaller species, including such rodents as mice and small squirrels ,are not
as prevalent overall in high tropical canopies as they are in most habitats globally.
(5) Small mammals, being warm blooded, suffer hardship in the exposed and turbulent
environment of the uppermost trees. Because a small body has more surface area per unit
of weight than a large one of similar shape, it gains or loses heat more swiftly. Thus, in
the trees, where shelter from heat and cold may be scarce and conditions may fluctuate, a
small mammal may have trouble maintaining its body temperature.
(10) Small size makes it easy to scramble among twigs and branches in the canopy for
insects, flowers, or fruit, but small mammals are surpassed, in the competition for food,
by large ones that have their own tactics for browsing among food-rich twigs. The weight
of a gibbon (a small ape) hanging below a branch arches the terminal leaves down so that
fruit-bearing foliage drops toward the gibbon’s face. Walking or leaping species of a
(15) similar or even larger size access the outer twigs either by snapping off and retrieving the
whole branch or by clutching stiff branches with the feet or tail and plucking food with
their hands.
Small climbing animals may reach twigs readily, but it is harder for them than for large
climbing animals to cross the wide gaps from on tree crown to the next that typify the
(20) high canopy. A macaque or gibbon can hurl itself farther than a mouse can: it can achieve
a running start, and it can more effectively use a branch as a springboard, even bouncing
on a climb several times before jumping. The forward movement of a small animal is
seriously reduced by the air friction against the relatively large surface area of its body.
Finally, for the many small mammals that supplement their insect diet with fruits or seeds
(25) an inability to span open gaps between tree crowns may be problematic, since trees that
yield these foods can be sparse.
4. According to paragraph 2, which of the
following is true about the small mammals in
the rain forest?
(A) They have body shapes that are adapted to
life in the canopy.
(B) They prefer the temperature and climate of
the canopy to that of other environments.
(C) They have difficulty with the changing
conditions in the canopy.
(D) They use the trees of the canopy for shelter
from heat and cold.
Question 30
During most of their lives, surge glaciers behave like normal glaciers, traveling perhaps
only a couple of inches per day. However, at intervals of 10 to 100 years, these glaciers
move forward up to 100 times faster than usual. The surge often progresses along a glacier
line like a great wave, proceeding from one section to another. Subglacial streams of meltwater
(5) water pressure under the glacier might lift it off its bed, overcoming the friction between ice
and rock, thus freeing the glacier, which rapidly sliders downhill Surge glaciers also might
be influenced by the climate, volcanic heat, or earthquakes. However, many of these
glaciers exist in the same area as normal glaciers, often almost side by side.
(10) Some 800 years ago, Alaska’s Hubbard Glacier advanced toward the sea, retreated, and
advanced again 500 years later. Since 1895, this secentry-mile-long river of ice has been
flowing steadily toward the Gulf of Alaska at a rate of approximately 200 feet per year. In
June 1986, however, the glacier surged ahead as much as 47 feet a day. Meanwhile, a
western tributary, called Valerie Glacier, advanced up to 112 feet a day. Hubbard’s surge
(15) closed off Russell Fiord with a formidable ice dam, some 2,500 feet wide and up to 800
feet high, whose caged waters threatened the town of Yakutat to the south.
About 20 similar glaciers around the Gulf of Alaska are heading toward the sea. If
enough surge glaciers reach the ocean and raise sea levels, West Antarctic ice shelves could
rise off the seafloor and become adrift. A flood of ice would then surge into the Southern
(20) Sea. With the continued rise in sea level, more ice would plunge into the ocean, causing sea
levels to rise even highter, which in turn would release more ice and set in motion a vicious
cycle. The additional sea ice floating toward the tropics would increase Earth’s albedo and
lower global temperatures, perhaps enough to initiate a new ice age. This situation appears
to have occurred at the end of the last warm interglacial (the time between glacations),
(25) called the Sangamon, when sea ice cooled the ocean dramatically, spawning the beginning
of the Ice Age.
38.The term “vicious cycle” in lines 21-22 refers
to the
(A) movement pattern of surge glaciers
(B) effect surge glaciers could have on the
temperature of tropical areas
(C) effect that repeated rising sea levels might
have on glacial ice
(D) constant threat surge glaciers could pose to
the Gulf of Alaska