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Plant Ecology - Chapter 18 Biomes
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Terrestrial biomes Defined by the physiognomy of the predominant vegetation
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Boundaries? No sharp boundaries between biomes Intergrades
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Importance of climate Prevailing climate is most important factor in determining what kind of biome will develop Precipitation, temperature are most important
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Desert biomes <10 inches (<25.4 cm) of rain per year Cool Temperate Tropical
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Grassland biomes 10-30 inches (25.4-76.2 cm) of rain per year Tundra Temperate grassland Tropical savanna
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Forest biomes >30 inches (>76.2 cm) of rain per year Taiga or coniferous forest Temperate deciduous forest Tropical rain forest
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Climatograph
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Temperature, precipitation not sole determiners Overlap among different biomes on plot suggests that other factors also are important Seasonality of precipitation Temperature fluctuations around mean Soil composition (based on geology)
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Deserts Lands where evaporation exceeds rainfall High evaporation rate 7-50X precipitation
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Deserts Occur in 2 distinct belts between 15-35° N & S latitude Result primarily from worldwide circulation of air masses (dry over deserts) ~25% of world’s land mass
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True deserts <10 inches of rain per year Semi-deserts may have 2-3X that, but have high evaporation rates Low humidity results in very hot days, but cool or cold nights Life is keyed to rainfall events Infrequent, but usually heavy when they occur
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Desert life Plants are either drought evaders or drought resistors
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Evaders Plants survive dry periods as seeds, but germinate, grow, and reproduce after rainfall
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Resistors Plants develop deep roots to become independent of rainfall events (woody shrubs) or are succulents to store water in stems (cactus)
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Grasslands Tropical savannas - grasslands with scattered individuals trees Central S. Amer., Central & S. Africa
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Savannas 3 distinct seasons Cool-dry, hot-dry, warm-wet Frequent fires suppress trees, maintain grasses and forbs Herbaceous, low-growing annuals & perennials (dicots) Regrow from roots or seeds every year
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Temperate grasslands Similar to tropical savanna, but occur in cooler regions N. Amer. prairie (French for plains) Russian steppe Hungarian pusztas S. Amer. pampas African veldt
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Temperate grasslands At one time covered 42% of world land surface Much under cultivation today Excellent soils Rich topsoil layer
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Temperate grassland climate High rates of evaporation Periodic severe drought Rainfall ~25-75 cm/year Too light to support forest, but too heavy to encourage desert
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Temperate grassland grasses Sod-forming Kentucky bluegrass Bunch grasses Big, little bluestem
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Temperate grasslands Most require periodic fires for maintenance, renewal, elimination of incoming/invading woody growth
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Tundra Northernmost limits for plant growth, and at high altitudes Plants generally low-growing Mat or shrubby
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Arctic tundra Encircles north pole Brief warm summers with nearly 24 hrs of sun/day Presence of permafrost Water-logged soils - low evaporation Shrubs, sedges grasses, mosses, lichens
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Alpine tundra At high elevations at all latitudes Variable daylength, many of the same restrictions, plant species
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Tropical forests Equatorial, mean temp. ~25°C, 12 hrs sunlight per day Rainfall highly variable-determines type of tropical forest present
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Types of tropical forests Thorn forests - furthest from equator, prolonged dry season
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Tropical deciduous forest More rainfall nearer equator, distinct wet, dry seasons Lose leaves during dry seasons Types of tropical forests
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Tropical rain forest >250 cm of rain per year Perpetual midsummer conditions Uninterrupted plant growth Types of tropical forests
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Tropical rain forests Contain as many species of plants and animals as all other types of ecosystems combined 4 mi 2 area - 750 species of trees, 1500 species of flowering plants
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Tropical rain forests Typically stratified into 5 layers Each layer has characteristic plants, animals May reach height of 80 m
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Tropical rain forest soil Very poor - little or no topsoil Easily weathered Subsoil with iron-based clay - laterite Major problems with slash-and-burn agriculture
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Tropical rain forests today Deforestation
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Loss of forests at present rate will mean disappearance within next 15-25 years Major problems will result from climate change, loss of species of medicinal, economic importance
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Temperate deciduous forest Eastern N. Amer, N. Europe and east Moderate temps., moderate moisture levels 5-6-month growing season
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Temperate deciduous forest Dominated by broad-leaved deciduous trees Relatively nutrient-rich soil provides for good growth Typically have 4 layers present Ground, shrub, sapling, canopy Rich diversity of plant, animal life
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Taiga Boreal forest, coniferous forest Harsh winters with lots of snow
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Taiga Dominated by conifers - spruce, pine, fir, hemlock Best suited for short growing season because they are not deciduous Can carry out photosynthesis whenever temps. rise above freezing Needle shape, waxy cuticle conserve moisture
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Thin, acidic, develop slowly Pine needles break down slowly in cool climate Taiga soils
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Taiga animals Primarily seed, insect eaters, or those that feed on plants in or near water Squirrels, birds, elk, moose, deer, beaver, porcupine, grizzlies, wolves
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