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