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GRASSLANDS GRASSLANDS, TUNDRA AND CHAPARRAL BIOMES GRASSLANDS  REGIONS WITH ENOUGH AVERAGE ANNUAL PRECIPITATION TO ALLOW GRASS (AND IN SOME AREAS, A FEW TREES) TO PROSPER BUT WITH PRECIPITATION SO ERRATIC THAT DROUGHT AND FIRE PREVENT LARGE STANDS OF TREES FROM GROWING GRASSLANDS  MOST GRASSLANDS ARE FOUND IN THE INTERIORS OF CONTINENTS  GRASSLANDS PERSIST BECAUSE OF A COMBINATION OF  SEASONAL DROUGHT  GRAZING BY LARGE HERBIVORES  PERIODIC FIRES GRASSLANDS  THESE 3 FACTORS KEEP LARGE TREES AND SHRUBS FROM GROWING  MANY GRASSES ARE PERENNIALS  STEMS GROW OUT FROM BOTTOM, ALLOWING PLANT TO GROW AFTER TOP IS EATEN TROPICAL GRASSLANDS  FOUND IN AREAS WITH HIGH AVERAGE TEMPERATURES  LOW TO MODERATE PRECIPITATION  PRLONGED DRY SEASON  OCCUR IN A WIDE BELT ON EITHER SIDE OF THE EQUATOR TROPICAL GRASSLANDS      SAVANNAS WARM TEMPEATURES YEAR ROUND TWO PRLONGED DRY SEASONS ABUNDANT RAIN THE REST OF THE YEAR LARGEST SAVANNAS IN CENTRAL AND SOUTHERN AFRICA  ALSO IN CENTRAL SOUTH AMERICA, AUSTRALIA AND S.E. ASIA SAVANNAS  PREDOMINANT VEGETATION:  AFRICAN SAVANNA- ACACIA TREE  AUSTRALIA SAVANNA-EUCALYPTUS TREE AFRICAN SAVANNAS  CONTAIN ENORMOUS HERDS OF GRAZING AND BROWSING HOOFED ANIMALS (WILDEBEESTS, GAZELLES, ZEBRAS, GIRAFFES, ANTELOPES)  HERBIVORES HAVE SPECIALIZED FEEDING HABITS THAT MINIMIZE COMPETITION AFRICAN SAVANNAS  GIRAFFES EAT LEAVES AND SHOOTS FROM THE TOPS OF TREES  ELEPHANTS EAT LEAVES AND BRANCHES LOWER DOWN  THOMPSON’S GAZELLES AND WILDEBEESTS PREFER SHORT GRASS  ZEBRAS GRAZE ON LONGER GRASS AND STEMS TEMPERATE GRASSLANDS  COVERS VAST EXPANSES OF PLAINS AND GENTLY ROLLING HILLS IN THE INTERIORS OF N. AND S. AMERICA, EUROPE AND ASIA.  NO TREES  SEASONAL EXTREMES OF HOT AND COLD  WINTERS BITTERLY COLD  SUMMERS ARE HOT AND DRY TEMPERATE GRASSLANDS  ANNUAL PRECIPITATION AVERAGES 10-39 INCHES  RECURRENT FIRES – PLANTS HAVE ADAPTED THE ABILITY TO GROW BACK RAPIDLY AFTER A FIRE  DEEP, FERTILE SOIL FROM GRASSES DYING AND DECOMPOSING TYPES OF TEMPERATE GRASSLANDS  TALL GRASS PRAIRIES & SHORT GRASS PRAIRIES OF THE MIDWESTERN AND WESTERN U.S. & CANADA  SOUTH AMERICAN PAMPAS  AFRICAN VELDT  STEPPS OF CENTRAL EUROPE AND ASIA POLAR GRASSLANDS ARCTIC TUNDRA – COVERS 10% OF EARTH’S SURFACE; OCCURS JUST SOUTH OF THE POLAR ICE CAP BITTERLY COLD, COVERED WITH ICE AND SNOW WINTERS ARE LONG AND DARK MOST PRECIPITATION FALLS AS SNOW TUNDRA PLANTS  GROW CLOSE TO GROUND  LEATHERY EVERGREEN LEAVES COATED BY WAXES THAT REDUCE HEAT LOSS  OTHER PLANTS SURVIVE AS ROOTS, STEMS, BULBS  SOME DEHYDRATE TO AVOID FROST DAMAGE(LICHENS) PERMAFROST  A PERENNIALLY FROZEN LAYER OF THE SOIL THAT FORMS WHEN THE WATER THERE FREEZES.  IN SUMMER SOIL IS WATERLOGGED, FORMING SHALLOW LAKES, MARSHES, BOGS, PONDS ANIMAL ADAPTATIONS  THICK FUR COATS  FEATHERS  COMPACT BODIES TO EXPOSE AS LITTLE SURFACE AS POSSIBLE  LIVING UNDERGROUND TUNDRA  DECOMPOSITION IS SLOW DUE TO THE COLD  PARTIALLY DECOMPOSED ORGANIC MATTER FORMS SOGGY PEAT BOGS ALPINE TUNDRA  OCCURS ABOVE THE LIMIT OF TREE GROWTH BUT BELOW THE PERMANENT SNOW LINE ON HIGH MOUNTAINS  NO PERMAFROST  MORE SUNLIGHT IMPACT OF HUMAN ACTIVITIES ON GRASSLANDS  CONVERTING SOME AREAS OF SAVANNA INTO CROPLAND  RELEASES LARGE AMOUNTS OF CO2 INTO ATMOSPHERE  OVERGRAZING BY LIVESTOCK – TURNS GRASSLANDS INTO DESERTS AND SEMIDESERT  CULTIVATING TEMPERATE GRASSLANDS CAN CAUSE SOIL EROSION  DRILLING IN THE ARCTIC TUNDRA CHAPARRAL  TEMPERATE SHRUBLAND  OCCURS ALONG COASTAL AREAS WITH A MEDITERRANEAN CLIMATE  LOCATED IN:  PARTS OF PACIFIC COAST OF N.A.  S. TEXAS AND N.E. MEXICO  COASTAL HILLS OF CHILE, S.W. AFRICA, S.W. AUSTRALIA & THE MED. CHAPARRAL  FIRES A YEARLY PROBLEM  CHAPARRAL IS ADAPTED TO AND MAINTAINED BY PERIODIC FIRES