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鄭先祐 (Ayo) 靜宜大學 生態學系

鄭先祐 (Ayo) 靜宜大學 生態學系. Ayo 台南站: http://mail.nutn.edu.tw/~hycheng/ Email add: Japalura@hotmail.com. Outline. Introduction Temperature, Atmospheric Circulation, and Precipitation Climate Diagrams Terrestrial Biomes Tropical rain forest Tropical dry forest Tropical savanna Desert

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鄭先祐 (Ayo) 靜宜大學 生態學系

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  1. 鄭先祐(Ayo) 靜宜大學 生態學系 Ayo 台南站:http://mail.nutn.edu.tw/~hycheng/ Email add:Japalura@hotmail.com

  2. Outline • Introduction • Temperature, Atmospheric Circulation, and Precipitation • Climate Diagrams • Terrestrial Biomes • Tropical rain forest • Tropical dry forest • Tropical savanna • Desert • Mediterranean woodland and shrubland • Temperate grassland • Temperate forest • Boreal forest • Tundra • Mountains: islands in the sky

  3. Introduction • Janzen(1960s-1980s)studied natural history of tropical dry forests in Costa Rica to aid restoration efforts. • Guanacaste tree (E. cyclocarpum) has no current dependable dispersers, thus trees produce massive numbers of fruits. • Last native dispersers went extinct 10,000 years ago. • Cattle and horses (exotics) now act as dispersers.

  4. Dispersers of Guanacaste Seeds

  5. Temperature, Atmospheric Circulation, and Precipitation • Spherical shape and tilt of earth’s axis cause uneven heating of earth’s surface. • Drives air circulation patterns and consequently precipitation patterns. • Warm, moist air rises. • Cools, condenses, and falls as rain. • Cooler, dry air falls back to surface. • Rainforests found near equator. • Major deserts found near 30o N / S.

  6. Solar-Driven Air Circulation

  7. Temperature, Atmospheric Circulation, and Precipitation • Coriolis effect causes apparent deflection of winds clockwise in the N hemisphere and counterclockwise in the S hemisphere.

  8. Climate Diagrams • Summarize climatic information using a standardized structure. • Temperature plotted on left vertical axis. • Precipitation plotted on right vertical axis. • 10o C equivalent to 20 mm precipitation. • Relative position of lines reflect water availability. • Adequate moisture for plant growth when precipitation above temperature.

  9. Climate Diagrams

  10. Soil : Foundation of Terrestrial Biomes • Soil is a complex mixture of living and non-living material. • Classification based on vertical layering (soil horizons). • Profile provides a snapshot of soil structure in a constant state of flux.

  11. Soil Horizons • O horizon: Organic Layer freshly fallen organic material - most superficial layer. • A horizon: Mixture of minerals, clay, silt and sand. • B horizon: Clay, humus, and other materials leached from A horizon - often contains plant roots. • C horizon: Weathered parent material.

  12. Soil Profile

  13. Terrestrial Biomes • Biomes are distinguished primarily by their predominant plants and are associated with particular climates. • Geographic and seasonal variations in temperature and precipitation are fundamental components.

  14. Tropical Rainforests • Most occur within 10o latitude of equator. • Little temperature variation between months. • Annual rainfall of 2,000 - 4,000 mm relatively evenly distributed. • Quickly leaches soil nutrients. • Mycorrhizae help gather nutrients. • Organisms add vertical dimension. • Harbor staple foods and medicines for world’s human populations - increasingly exploited.

  15. Tropical Rainforests

  16. Tropical Dry Forest • Usually located between 10o - 25o latitude. • Climate more seasonal than tropical rainforest. • Soils generally richer in nutrients, but vulnerable to erosion. • Shares many animal and plant species with tropical rainforests. • Heavily settled by humans with extensive clearing for agriculture.

  17. Tropical Dry Forest

  18. Tropical Savanna • Most occur north and south of tropical dry forests within 10o - 20o of the equator. • Climate alternates between wet / dry seasons. • Drought associated with dry season leads to lightning-caused wildfires. • Soils have low water permeability. • Saturated soils keeps trees out. • Landscape is more two-dimensional with increasing pressure to produce livestock.

  19. Tropical Savanna

  20. Desert • Major bands at 30o N and 30o S latitude. • Occupy about 20% of earth’s land surface. • Water loss usually exceeds precipitation. • Soil usually extremely low in organic matter. • Plant cover ranges from sparse to absent. • Animal abundance low, but biodiversity may be high. • Strong behavioral adaptations. • Human intrusion increasing.

  21. Desert

  22. Mediterranean Woodland and Shrubland • Occur in all continents except Antarctica. • Climate cool and moist in fall, winter, and spring, but can be hot and dry in summer. • Fragile soils with moderate fertility. • Trees and shrubs typically evergreen. • Fire-resistant plants due to fire regime. • Long history of human intrusion. • Cleared for agriculture.

  23. Mediterranean Woodland and Shrubland

  24. Temperate Grassland • Extremely widespread distribution. • Annual rainfall 300 - 1,000 mm. • Experience periodic droughts. • Soils tend extremely nutrient rich and deep. • Thoroughly dominated by herbaceous vegetation. • Large roaming ungulates. • Bison vs. cattle

  25. Temperate Grassland

  26. Temperate Forest (Old Growth) • Majority lie between 40o and 50o latitude. • Rainfall averages 650 - 3,000 mm. • Fertile soils • Long growing seasons dominated by deciduous plants. • Short growing seasons dominated by conifers. • Biomass production can be very high. • Many major human population centers.

  27. Temperate Forest (Old Growth)

  28. Boreal Forest (Taiga) • Confined to Northern Hemisphere. • Covers 11% of earth’s land area. • Thin, acidic soils low in fertility. • Generally dominated by evergreen conifers. • Relatively high animal density. • Historically, low levels of human intrusion.

  29. Boreal Forest (Taiga)

  30. Tundra • Covers most of lands north of Arctic Circle. • Climate typically cool and dry with short summers. • 200 - 600 mm precipitation. • Low decomposition rates. • Supports substantial numbers of native mammals. • Human intrusion historically low, but increasing as resources become scarce.

  31. Tundra

  32. Mountains: Islands in the Sky • Built by geological processes and thus concentrated in belts of geological activity. • Climate changes with elevation and latitude. • Soils are generally well-drained and thin. • Flora and fauna change with elevation. • Historically used as a source of raw materials for human settlements.

  33. Mountains: Islands in the Sky

  34. Review • Introduction • Temperature, Atmospheric Circulation, and Precipitation • Climate Diagrams • Soil Horizons • Terrestrial Biomes

  35. On the Net • Society for Ecological Restoration International • http://www.ser.org/ • Endangered Species Habitat Conservation Program • http://www.fws.gov/endangered/hcp/index.html • The world's biomes • http://www.ucmp.berkeley.edu/glossary/gloss5/biome/

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