F. Grasslands are, surprisingly <G>, dominated by grasses, which
can form a continuous or discontinuous cover. There can also be found
trees, shrubs, and forbs, too, depending on the area. I'll discuss
four subtypes.
1. The first two are tropical grasslands.
a. The first of these is savanna.
i. This is dominated by medium to tall grasses (up to 3-4 m!),
which form a continuous or discontinuous cover.
a. This grass is soft and green and humid soon after the
rainy summer season starts, affording high quality
forage for large herds of a few species of grazing
animals (e.g., zebras, wildebeests) and for herds of
domestic animals. Great numbers of them move into
savanna as summer begins. It grows to really impressive
heights by the end of the wet season, and it'll be
virtually continuous in good years and more
discontinuous in drier years.
b. Comes winter, the hot dry season, this grass gives a
dry, brown, coarse appearance, and it can be quite
dangerous to hike in, because of the silica deposited on
the blades of the grasses as they struggle to input
scarcer and scarcer soil water. Nasty stuff. The great
herds of animals migrate out of it then. It is very
prone to massive fires at this time.
ii. The peoples who have lived with this vegetation for
hundreds and thousands of years will often themselves set
it on fire just before the rainy season, to turn all that
dead biomass into ash fertilizer and to knock it down so
sun can reach the soil. This stimulates really rapid
growth of tender grass shoots, which is great for those
herds of wild animals or their own domestic herds of
cattle, horses, goats, and camels. There is some
speculation that savanna and many grasslands in fact may
not be strictly natural vegetation forms! The argument is
that people have been messing with fire for perhaps 100,000
years and, so, changing the balance between grass and
trees. Sometimes, when firing ceases or recurs less
frequently, you see tropical deciduous woodland moving back
in, filling the grassy spaces, so there might be something
to this.
iii. Interspersed with the grass is a grouped cover of smaller
tree-form plants, including acacias, palms, even giant
cacti. In drier or overburnt portions, this second cover is
in shrub form.
iv. There is also an understory of forbs, most evident in the
early rainy season.
v. Tropical savanna is associated with the drier portions of
the tropical wet and dry climate (the wetter portions of
that climate being occupied largely by tropical deciduous
woodland). That would be the Aw climate in the Köppen
system.
vi. Accordingly, you can expect to find savanna in such places
as southern central Brazil, northeast South America, Africa
well south of the Sahara, East Africa, and much of southern
Africa (the African savannas are the most extensive, and
people have lived there the longest), southern and central
India, interior Southeast Asia, and Australia some distance
around the tropical desert there.
b. Sudan, sometimes called tropical steppe.
i. This is a tropical grassland, dominated by a continuous or
discontinuous cover of short grasses, normally interspersed
with a very discontinuous layer of small shrubs. Both are
generally from 15 cm to 1 m in height, so this is a pretty
low-lying vegetation.
ii. In good years, the grass cover is quite lush, forming a
pretty continuous cover and attaining greater height; in
dry years, the grass cover becomes very sparse and short,
which brings the shrub component to visual dominance.
iii. This vegetation type is associated with BSh climates in the
Köppen system: The tropical semi-arid or the tropical
steppe climate. As such, it can be seen as a nearly
perfect transition from savanna to tropical desert. In
good years, it resembles the savanna; in bad, the desert.
iv. So, you can find it in a long, slender strip immediately
south of the Sahara (often called the Sahel). It is also
found in southern Africa inland from the Namib Desert, in
an area called the Kalahari Steppe (sometimes called a
"desert"). It's also found in northern Australia, just
north of the Australian desert but south of the
savannalands there.
v. The recurrent hazard here is drought. The drier a climate
is, the less predictable is its precipitation. So, if the
ITCZ doesn't quite get to this vegetation one year (or
several in a row), the sudan takes on a desert-like
appearance. Famine accompanies drought here. Sometimes we
see that human tendency to respond to low level, recurrent
hazards by setting society up for the rarer high-magnitude
event. In the Sahel, international agencies have sunk
boreholes to tap fossil water and give people a place to
get water for their animals even in drought. The problem
is that cows aren't all that stupid: They hang out around
the boreholes, and their hooves crush and pulverize the
soil, making it susceptible to wind erosion. Their
overgrazing kills the local grasses and shrubs. The result
is "desertification," the degradation of non-desert
vegetation into something resembling the desert. This, of
course, makes the landscape even less able to support the
human population, which becomes really apparent when the
rains fail and marginal farmers and animal herders lose
their few resources and starve by the dozens of thousands.
2. The second two subtypes of the grassland biome are temperate ones.
a. The first of these is tall-grass prairie.
i. This consists of a variety of medium and taller grass
species (1-2 m in height).
ii. These normally form a continuous, even a dense cover,
though in dry years, you'll see a discontinuous cover
dominated by the shorter of the local grass species.
iii. There is a second layer of smaller forbs, which are very
evident in the early spring before the taller grasses shade
them out. There is a lovely wildflower display at this
time.
iv. You will also see riparian or "gallery forests," too --
trees and shrubs and many forbs growing along the banks of
rivers flowing through the prairie. In late summer, these
look like green snakes crossing the light green or beige
grasslands.
v. You occasionally see a tree or small grove of trees around
a spring or seep, too. Otherwise, the prairie is utterly
treeless.
vi. This prairie is associated with the moister sides of the
BSk climate, Köppen's cold semi-arid climate. You can
also find it on the drier side of the humid subtropical and
humid continental climates and the west coast marine
climate. This is a transition from the lusher vegetation of
these climates to the steppes and deserts beyond. In fact,
there is a lot of evidence that human firing may, in fact,
have created this prairie or extended its coverage beyond
any natural distribution. When fires are suppressed,
succession results in the replacement of prairie by
temperate broadleaf deciduous and mixed forest!
vii. American prairie extends from eastern Kansas, Arkansas,
eastern Oklahoma, Missouri, eastern Nebraska, and the
eastern Dakotas, into southern Saskatchewan. The South
American prairie is the pampas of Argentina, while in
eastern Europe, we have the Hungarian puszta.
viii. Not surprisingly, the great natural hazard here is prairie
fire. It does renew the prairie by cleaning debris off the
ground, killing a lot of disease organisms, and creating
fertilizer. So, again, mimicking nature, Native Americans
and other human occupants of such grasslands have regularly
torched them.
b. Steppe or shortgrass prairie.
i. This grassland is dominated by short to medium grass
species (15 cm to maybe a meter in height).
ii. They usually form a discontinuous cover, ranging from
pretty continuous in good years (which also favors the
taller of the local species of grass) to discontinuous in
dry years (which favors the shorter of the local grasses).
iii. Low shrubs are usually present also, forming a very
discontinuous cover, which is more apparent and visually
dominant during dry years. In this, the steppe strongly
resemles the sudan.
iv. Steppe is associated with the temperate steppe or temperate
semi-arid climate (the BSk climate in the Köppen
system discussed in lecture 20).
v. It is transitional from prairie to temperate desert in
character, sometimes looking more desert-like and other
times looking more like lush prairie.
vi. You can find it on the American Great Plains (eastern
Colorado; western Kansas, Nebraska, and the Dakotas;
Wyoming; Montana; southern Alberta; northern Texas; and
western Oklahoma); the northern Basin and Range (southern
Idaho and northern Nevada, parts of eastern Washington and
Oregon; parts of the Great Central Valley of California);
the Russian and Ukrainian steppes, extending into
Transcaucasia, southernmost Siberia, and parts of N. China;
parts of Turkey and Iran; central Spain; southeastern and
southwestern Australia just south of the Australian desert.
Well, that takes care of the world's biomes. In this lecture, we reviewed
four vegetation formations dominated by grasses. There were two tropical
grasslands, namely, savanna and sudan, associated with the drier tropical wet
and dry climate and the tropical semi-arid climate, respectively. There were
also two temperate grasslands, prairie and steppe. Both are associated with
the temperate semi-arid climate, but the former also extends into the drier
parts of the humid subtropical (Cfa), west coast marine (Cfb), and humid
continental (Dfa and Dfb, especially).
So, in all, this week we reviewed three major groups of biomes: those
dominated by trees, those dominated by shrubs, and those dominated by grasses.
Throughout the biosphere section, we've looked at the biosphere, including the
environment of organisms. The environment (both the physical environment and
the biotic environment of other organisms) provides the selective forces
operating to shape various kinds of life in various situations. These
different kinds of life can be classified according to their evolutionary
relations (genetic classifications). They can also be classed according to the
structures and functions imposed on each by the selective forces in their
environment, hence, the life form and functional classifications. The
assemblages of living things can be further classed into biomes, by the plant
life forms dominant in a particular association. Biomes and their subtypes
are sent to reflect broadly the climatic (and sometimes soil) conditions
of their environments, so that's why I related each to one of the Köppen
climatic categories.
Document and © maintained by Dr.
Rodrigue
First placed on web: 11/06/00
Last revised: 07/02/07