They have sharp spines that create shade, reduce drying airflow, discourage herbivores and reflect sunlight.
They also secrete toxins into the soil to prevent interspecific completion.
They are dependent on water for germination;
They have short life spans;
They perform their entire life cycle from seed to flower to seed within a single growing season
They are generally small.
They are often nocturnal.
They have small surface areas.
They spend time in underground burrows where it is cold.
Animals include numerous birds, bats, small mammals, and insects.
Decomposition is rapid and soils are subject to heavy leaching.
Distinct seasonality where winter is absent and only two seasons are present.
The length of daylight is 12 hours and varies a little year-round
Large diversity of species.
Occur near the equator.
Annual rainfall exceeds 80 inches (200 cm) and is evenly distributed.
Plants are highly diverse.
Tree canopy is multilayered and continuous, allowing little light penetration.
Trees have buttressed trunks, shallow roots, and large, dark green leaves.
Occur in eastern North America, northeastern Asia, and western and central Europe.
Have a distinct winter, moderate climate, and a 140–200-day growing season during four to six frost-free months.
Temperature varies from –20°F to 85°F (–30°C to 30°C).
Precipitation averages 30–60 inches (75–150 cm) per year.
Fertile soil is enriched by decaying leaf litter.
Found in temperate regions with warm summers, cool winters, and enough rainfall to support forests.
Common in coastal areas with mild winters and heavy rainfall, or inland in drier climates or mountains.
These forests have cedar, cypress, fir, juniper, pine, redwood, and spruce.
These forests have two layers:
Overstory
Understory
Some forests have a shrub layer.
In winter, when food is scarce, many animals hibernate to conserve energy and build fat in summer.
Birds have feathers and many animals have thick fur to protect them from cold weather.
Some animals migrate to warmer climates during the winter months.
They grow near the coastline around islands and continents and are separated from the shore by narrow, shallow lagoons.
They are the most common type of reef.
These are also parallel to the coastline but are separated by deeper, wider lagoons.
At their shallowest point, they can reach the water’s surface, forming a “barrier” to navigation.
These are rings of coral that create protected lagoons and are usually located in the middle of the sea.
They usually form when islands, often the tops of underwater volcanoes, surrounded by fringing reefs, sink into the sea, or the sea level rises around them.
With the arrival of fall and cooler air temperatures, water at the surface of a lake begins to cool and becomes heavier.
During this time, strong fall winds move the surface water around, which promotes mixing with deeper water.