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
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