stratification
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Stratification. Stratification. Vertical layering – usually of plants. . Stratification. Vertical layering – usually of plants. Best seen in a forest. Stratification. Vertical layering – usually of plants. Best seen in a forest - PowerPoint PPT PresentationTRANSCRIPT
STRATIFICATION
STRATIFICATION Vertical layering – usually of plants.
STRATIFICATION Vertical layering – usually of plants. Best seen in a forest
STRATIFICATION Vertical layering – usually of plants. Best seen in a forest Animals can also form vertical layers in
the soil, and in lakes/sea Dragonfish
The deep sea dragonfish is a ferocious predator in spite o pf its small size. The
dragonfish has a long barbel attached to its chin. This barbel is tipped with a light-producing organ known as a photophore. These fishes
are sexually dimorphic (the males and females look different). Dragonfishes live in deep ocean waters at depths of up to
1500 m (5000 feet).
STRATIFICATION Vertical layering – usually of plants. Best seen in a forest Animals can also form vertical layers in
the soil, and in lakes/sea In tropical forests, the animals form
verticals layers through things like – monkeys staying in the canopy without ever going onto the ground.
STRATIFICATION Vertical layering – usually of plants. Best seen in a forest Animals can also form vertical layers in
the soil, and in lakes/sea In tropical forests, the animals form
verticals layers through things like – monkeys staying in the canopy without ever going onto the ground.
General layers in a NZ forest:
STRATIFICATION Vertical layering – usually of plants. Best seen in a forest Animals can also form vertical layers in the soil, and
in lakes/sea In tropical forests, the animals form verticals layers
through things like – monkeys staying in the canopy without ever going onto the ground.
General layers in a NZ forest:1. Canopy2. Sub-canopy3. Tree fern layer4. Shrub layer5. Forest floor layer6. Litter layer
USING YOUR HANDOUT Fill in the layers of stratification
AND SOIL LAYERS...1. Litter layer2. Topsoil layer3. Sub-soil layer4. Soil parent material
REASONS FOR LAYERS Dominant plants in canopy – filter
sunlight, cut down the wind, drop the temperature, and increase humidity.
There a different micro-climates which form at each level.
REASONS FOR LAYERS Dominant plants in canopy – filter
sunlight, cut down the wind, drop the temperature, and increase humidity.
There a different micro-climates which form at each level.
EG. Beech forests – uncomplete canopies. Can be uneven, with sub-canopy filling space
REASONS FOR LAYERS Dominant plants in canopy – filter
sunlight, cut down the wind, drop the temperature, and increase humidity.
There a different micro-climates which form at each level.
EG. Beech forests – uncomplete canopies. Can be uneven, with sub-canopy filling space
EG. In soil – leaf-litter animals are dark coloured and active.
REASONS FOR LAYERS Dominant plants in canopy – filter sunlight,
cut down the wind, drop the temperature, and increase humidity.
There a different micro-climates which form at each level.
EG. Beech forests – uncomplete canopies. Can be uneven, with sub-canopy filling space
EG. In soil – leaf-litter animals are dark coloured and active.
EG. Topsoil, animals aren’t so dark and are slower-moving, while sub-soil animals are usually large, sluggish (pun!) and pale.
ZONATION Bands of organisms may form in relation
to a gradient in a major environmental factor = zonation.
ZONATION Bands of organisms may form in relation
to a gradient in a major environmental factor = zonation.
As you move down a particular environment, vegetation and animals may change slowly/rapidly.
ZONATION Bands of organisms may form in relation
to a gradient in a major environmental factor = zonation.
As you move down a particular environment, vegetation and animals may change slowly/rapidly.
EG. Rocky shore = bands of organisms form due to exposure to the air (at low tide)
ROCKY SHORE ZONATION