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Ecology Lecture 2: Life on Land - Soil and Terrestrial Biomes - Prof. Brent Blair, Study notes of Ecology and Environment

A lecture outline for a university ecology course (biol 250) focusing on life on land. Topics include the importance of light and soil, soil horizons, soil texture, and terrestrial biomes. The lecture discusses various biomes such as tropical rainforests, tropical seasonal forests, deserts, mediterranean shrublands, temperate forests, temperate grasslands, and tundra.

Typology: Study notes

Pre 2010

Uploaded on 08/18/2009

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Today’s Outline
Ecology (BIOL 250)
Lecture 2: Life on Land
Announcements
The light resource
The soil Resour ce
Soil horizons
Soil profile
Importance of light an d soil
Terrestrial Biomes
Light Availability
Light Availability
Soil : Foundation of Terrestrial
Biomes
Soil is a complex mixture of living and non-
living material.
Classification based on vertical layering (soil
horizons), texture and chemical properties.
Profile provides a snapshot of soil structure in a
constant state of flux.
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.
Soil Profile vs Soil Ho rizons
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Download Ecology Lecture 2: Life on Land - Soil and Terrestrial Biomes - Prof. Brent Blair and more Study notes Ecology and Environment in PDF only on Docsity!

Today’s Outline Ecology (BIOL 250) Lecture 2: Life on Land Announcements The light resource The soil Resource Soil horizons Soil profile Importance of light and soil Terrestrial Biomes

Light Availability

Light Availability Soil : Foundation of Terrestrial

Biomes

Soil is a complex mixture of living and non- living material. Classification based on vertical layering (soil horizons), texture and chemical properties. Profile provides a snapshot of soil structure in a constant state of flux.

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. Soil Profile vs Soil Horizons

Soil Texture

Soil Texture: The proportion of different sized soil particles. Gravel: Particles greater than 2.0 mm. Sand: Particles between .05 - 2.0 mm  Silt: Particles between .002 - .05 mm  Clay: Particles less than .002mm

But why are soil types, light,

(& rainfall) important?

Predicts what the land may be used for (i.e., human uses the land may have) Influences what type of vegetation will be present Influences the quantity and diversity of vegetation

TERRESTRIAL BIOMES

Biomes - Areas sharing similar climate, topographic and soil conditions, and roughly comparable communities. Temperature and precipitation are among the most important determinants in biome distribution. Most terrestrial biomes are identified by the dominant plants of their communities.

Biomes

Climate Diagrams Tropical Rainforests

Location within 10o^ latitude of equator Little temperature variation between months. Annual rainfall of 2,000 - 4,000 mm relatively evenly distributed. Harbor staple foods and medicines for world’s human populations - increasingly exploited.

Temperate Forest

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. Eastern half of US was covered with broad leaf deciduous forest when European settlers arrived. Much of that was harvested a century ago for timber. Now large areas have re-grown and are again approaching old-growth status.

Temperate Forest

Temperate Grassland

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

Tundra

Covers most of lands north of Arctic Circle  Very short growing season, with cold harsh winters.  200 - 600 mm precipitation.  Low decomposition rates.  Supports substantial numbers of native mammals.  Human intrusion historically low, but increasing as resources become scarce.  Typically frozen! But…

Dispersers of Guanacaste Seeds

Janzen studied natural history of tropical dry forests in Costa Rica to aid restoration efforts. Guanacaste tree ( E. cyclocarpum ) has no current dependable dispersers Last native dispersers went extinct 10,000 years ago.

  • Cattle and horses (exotics) now act as dispersers.