AQUATIC HABITATS AND

TERRESTRIAL BIOMES

Fig 50.17 shows the distribution of major aquatic biomes
More than 97% of earth's water is in oceans

Water in the Biosphere (modified from Wetzel 1983). Do NOT memorize.
Location

Volume (km 3 x 1000)

% of total

Renewal time
Oceans

1,370,000

97.61

3100 yrs
Polar ice, glaciers

29,000

2.08

16,000 yrs
Groundwater

4000

0.29

300 yrs
Freshwater lakes

125

0.009

1-100 yrs
Saline lakes

104

0.008

10-1000 yrs
Soil

67

0.005

280 days
Rivers

1.2

0.00009

12-20 days
Atmosphere

14

0.0009

9 days

Fresh Water

Lentic waters

Lakes exhibit thermal stratification (layering) - Fig. 50.15

thermocline
water most dense at 4
o C
turnover
Colder areas, dimictic
In Texas and other warm areas, only one mixing per year - monomictic

Lakes subdivided into three zones by light penetration - Fig. 50.18 - photic vs. aphotic zones

Littoral zone
Limnetic zone
Profundal zone
Benthic zone
Compensation point

Lakes Divided into Productivity Categories

Oligotrophic lakes - Fig. 50.19a
Mesotrophic lakes
Eutrophic lakes
- Fig. 50.19b

Lakes temporary
Go through succession
Oligotrophic > mesotrophic > eutrophic > marsh > land
Marshes
and swamps (freshwater wetlands) constitute intermediate zones
- Fig. 50.21a

Lotic waters - Rivers and streams - Fig. 50.19c

riffles, runs, and pools
erosion and deposition
rivers and streams much older and more permanent
Dams - Fig. 50.20

Marine Habitats - Fig. 50.17

Estuaries - Fig. 50.21b

Two major zones based on light penetration

photic
aphotic

Two major areas

pelagic
benthic

Major Kinds of Oceanic Habitats - Fig. 50.22

intertidal zone Tides - Fig. 50.23a
neritic zone
continental shelf
oceanic zone
abyssal zone
deep sea hydrothermal vents - Fig. 50.23c - a black smoker - Tubeworms - The movie

Coral Reefs - Fig. 50.23b - The Movie

Terrestrial biomes

Biomes are terrestrial communities occurring over wide areas

Recognized by characteristic appearance
Associated with characteristic climates
Classified by vegetation

Distribution - Fig. 50.24 of biomes is a result of: See Fig. 50.10 for a climograph

climate - primarily determined by temperature and precipitation
latitudes and altitudes
precipitation
soil

Tropical Dry Forests

Alternate wet and dry periods - also called seasonal rainforest
Many trees lose leaves in dry period.

Tropical Rain Forests

Richest biome in terms of number of species
Substantial rainfall throughout year
Competition great for sunlight; epiphytes and vines common

Savannas - Fig. 50.25b

Reduced rainfall with prolonged dry seasons
Open grassland with scattered shrubs and trees
Maintained by periodic fires - fire adapted
Large herbivores and their predators dominate

Deserts - Fig. 50.25c

Extremely low rainfall
All great deserts at or near 30 degrees
latitude N or S - Map
Other major deserts at continental interiors
Other deserts on leeward side of mountain ranges
Rain shadow effect: drier on leeward side of mountain
Both cold and hot deserts
Special adaptations by both plants and animals

Chaparral - Fig. 50.25d

Spiny evergreen shrubs
Climate dry in summer
Maintained by fire, needed for some seeds to germinate - fire adapted

Temperate Grasslands - Fig. 50.25e

Grasslands also called plains or prairies
Maintained by grazing (large herbivores) and periodic fires or become forest - fire adapted
Most grasslands in US now converted to agriculture

Temperate Deciduous Forests - Fig. 50.25f

Dominated by deciduous trees like oak, hickory, elm, maple, ash - lose leaves in winter
Moderate rainfall

Coniferous forests - also called boreal forests or taiga - Fig. 50.25g

Northern coniferous forests of Eurasia and North America
Long, cold dry winters
Largest terrestrial biome
Very short growning season
Now being logged at a treamendous rate

Temperate Rain Forests - Fig. 50.25g3

Cool weather, dense fog, high precipitation
On coastlines as in northwestern U.S.
Large evergreens, many epiphytes
Very important timber - little old growth left

Tundra - Fig. 50.25h

Bitter cold, high winds
Very low precipitation
Very short growing season
Permanent ice, permafrost, underlying surface
Arctic (far north) and high mountains.

Polar Ice

Ice caps at north (Arctic) and south (Antarctic) poles
No precipitation, fresh water scarce, life limited to coasts
Only bacteria, algae, small insects in Antarctic interior

Texas Ecoregions from Texas Parks and Wildlife