Terrestrial biomes of the world Lecture Topics:
Biome concept Biome classification, distribution Biome climate patterns (Walters Diagrams) Biome survey/distinctive ecological
characteristics
Introduction to biome concept Classification systems
Holdridge’s Life Zone system Whittaker’s classification scheme based on annual
precipitation, temperature (nine biomes recognized)--simpler for purposes here of describing basic biomes
Walter climate diagram: generic
Effective growing season (temperature above 0 ºC)
Ecosystem water-limited if temperature line (red) exceeds precipitation line (blue)
White zone denotes frozen conditions, inhospitable for life
Temperate forest physical environment Found at temperate latitudes, typically 40-60º latitude Climate highly seasonal:
Cool winter & warm summer, plentiful precipitation all year Cold makes water unavailabledeciduous foliage (leaf
drop), brilliant fall colors (depending on species) Spring flush of leavesabundant herbivores
(caterpillars,etc.) and migratory birds that feed on them Vernal herbs flower in spring, where forest floor warms up
before trees leaf-out (e.g., sweet white violet) Different subtypes of biome
Northern hardwoods—e.g., sugar maple, yellow birch Southern hardwoods—oaks, sweet gum, tulip poplar, &
evergreens (magnolias, live oak, and pines). Southern pinewoods on poor, sandy soils; fire important
Examples of temperate seasonal forest
Louisiana examples: Bottomland hardwoods, upland mixed-mesophytic (coniferous & deciduous) forest
Temperate rainforest characteristics
Found at temperate latitudes, typically 40-60º (Northwestern U.S., S. Chile, E. Australia, New Zealand)
Climate moderately seasonal: Mild winter (below freezing) versus warm to hot summer, Abundant winter rain Summer fog
Plants dominated by giant needle-leaved trees (in U.S.: redwoods, western hemlock, douglas fir, western cedar) Ancient, formerly widespread forest type Why giant trees? Year-round growing season, abundant
moisture, strong potential evapotranspiration all contribute
Physical environment of temperate grassland/desert biome
Typically 25-50º N, S of equator Climate characterized by high rate evaporation (often warm
temperatures), & periodic severe (summer) droughts Rainfall 25-70 cm annually, too little to support forest Often subject to fire—e.g., prairie , longleaf pine (essentially
prairie with scattered pine trees) Steppes are cold deserts, dominated by shrubs & grassland
Plants—1º productivity proportional to rainfall Grasses dominate (because they’re competitive over trees where
fire, grazing predominate) High degree spatial heterogeneity in plants, due to topography,
soils, fire history, animal activity (e.g., prairie dogs, bison)
Physical environment & plants of woodland/shrubland biome
Location (30-40º N, S of equator) Mediterranean region, coastal California, Chile,
southern S. Africa, south-western Australia Climate “Mediterranean” (mild, wet winter; hot, dry
summer = drought) Plants
Fire adapted, dense evergreen shrubs Often deeply rooted, to get at scarce (summer) water Sclerophyllous (waxy, drought-resistant) leaves Aromatic compounds that dissuade insect herbivores
Physical characteristics of deserts Evaporation exceeds precipitation (rainfall <30 cm) 20-30º N & S Latitude (subtrop. high pressure zone) Plants adapted to drought (= xerophytes)
Small leaves dissipate heat, large edge:area ratio Water-storage mechanisms (e.g., many cacti) Conserve H2O (e.g., CAM photosynthesis, waxy cuticle)
Protected against herbivores—spines, aromatic compounds Diverse life-forms of desert plants:
Succulents (e.g., saguaro & barrel cactus) store water Ephemerals (annuals) grow rapidly, seed after a rain Phreatophytes (e.g., mesquite, palo verde) deeply rooted Opportunistic perennials (ocotillo) flush leaves, flower after
rain
Boreal (northern coniferous) biome Climate & setting
Found typically from 50-70º N. Latitude (taiga), south in mts. Cold winter, cool-warm summer, 3-5 mo. growing season
Taiga (russian for “land of little sticks”) forms continuous stretches of boreal forest, dominated by trees in species of spruce (Picea), fir (Abies); also known as “spruce-moose” biome Diversity of trees low (1-2 spp./site) Conifers dominate (tolerate cold, photosynthesize whenever
it’s warm enough, conical shape sheds snow with minimal branch breakage)
Tundra physical environment & plants Climate & setting
Too cold, windy for trees; short growing season (50-60 days in arctic, up to 180 days in alpine zones at higher elevation)
Precipitation generally < 25 cm annually (cold air holds little moisture), “locked up” as snow (unavailable to plants)
Only in N. hemisphere, north. edge of all northern continents Plants—grassland & mixed shrubland (some dwarf trees)
Often low to ground = warmest microclimate, out of wind (e.g., cushion plants)
Lichens often important ground (& rock) cover, important in creating soils by breaking down rocks; alders (Alnus) can be an important nitrogen-fixer
Northern bogs characteristic of the wettest spots—dominated by carnivorous plants (animal source of N)
Climate & setting Tropical rainforest Near equator Climate continuously favorable for intense biological
activity (abundant rainfall, >400 cm, & high temperatures) Biological interactions (ecologically, evolutionarily) impt. Biological diversity staggering (latitudinal diversity gradient)
Diverse plant life forms: trees, shrubs, epiphytes, epiphylls, vines, lianas (woody), ferns, tree ferns Layering of plants prominent: ground layer, shrubs, sub-
canopy, continuous canopy, & “emergents” (up to 60 m tall) Some plant adaptations:
Buttresses to help prop up often shallow-rooted trees (why?) Oval, waxy leaves with drip-tips (why?) Nutrient scavenging & extremely tight nutrient cycling
Tropical seasonal forest/savanna Tropical seasonal forest occurs at higher latitudes than
rainforest (10-20º N, S) Rainfall less than rainforests (240-400 cm), highly seasonal
3-6 month dry season, often with no rainfall Dry forests have almost as diverse plant and animal
communities as rainforests Trees typically drought-deciduous (facultative) Ant-acacia mutualism is characteristic of dry forests of
Central America Biome highly threatened by human activities, because of its
potential for agriculture, grazing
Top Related