Chapter 7
Core Case Study:
Why Should We Care About Coral
Reefs?
• Coral reefs form in
clear, warm coastal waters of the tropics and subtropics.
– Formed by massive
Core Case Study:
Why Should We Care About Coral
Reefs?
• Help moderate atmospheric temperature by
removing CO2 from the atmosphere.
• Act as natural barriers that help protect 14% of
the world’s coastlines from erosion by battering waves and storms.
• Provide habitats for a variety of marine
AQUATIC ENVIRONMENTS
• Saltwater (marine) and freshwater aquatic life
What Kinds of Organisms Live in
Aquatic Life Zones?
• Aquatic systems contain floating, drifting,
swimming, bottom-dwelling, and decomposer organisms.
– Plankton: important group of weakly swimming,
free-floating biota.
• Phytoplankton (plant), Zooplankton (animal), Ultraplankton
(photosynthetic bacteria)
– Nekton: fish, turtles, whales.
– Benthos: bottom dwellers (barnacles, oysters).
– Decomposers: breakdown organic compounds (mostly
Life in Layers
• Life in most aquatic systems is found in
surface, middle, and bottom layers.
• Temperature, access to sunlight for
photosynthesis, dissolved oxygen content, nutrient availability changes with depth.
Salt water life zones
1. 99.5% of earth’s habitable volume 2. 250,000 known species of marine
plants/animals
SALTWATER LIFE ZONES
• The oceans that occupy
most of the earth’s
surface provide many ecological and
economic services.
Two major life zones
The Coastal Zone:
Where Most of the Action Is
• The coastal zone: the warm, nutrient-rich,
shallow water that extends from the high-tide mark on land to the gently sloping, shallow edge of the continental shelf.
• The coastal zone makes up less than 10% of the
world’s ocean area but contains 90% of all marine species.
– Provides numerous ecological and economic services.
Estuaries and Coastal Wetlands:
Centers of Productivity
• Estuaries include river
mouths, inlets, bays,
sounds, salt marshes in temperate zones and mangrove forests in tropical zones.
Mangrove Forests
• Are found along
about 70% of gently sloping sandy and silty coastlines in tropical and subtropical regions.
Estuaries and Coastal Wetlands:
Centers of Productivity
• Estuaries and coastal marshes provide
ecological and economic services.
– Filter toxic pollutants, excess plant nutrients, sediments, and other pollutants.
– Reduce storm damage by absorbing waves and
storing excess water produced by storms and tsunamis.
Rocky and Sandy Shores:
Living with the Tides
• Organisms experiencing daily low and high tides
have evolved a number of ways to survive under harsh and changing conditions.
– Gravitational pull by moon and sun causes tides.
Rocky and Sandy Shores:
Living with the Tides
• Organisms in intertidal
zone develop
specialized niches to
deal with daily changes in:
– Temperature
– Salinity
– Wave action
Barrier Islands
• Low, narrow, sandy islands that form offshore
from a coastline.
• Primary and secondary dunes on gently sloping
sandy barrier beaches protect land from erosion by the sea.
Threats to Coral
Reefs:
Increasing
Stresses
• Biologically diverse
and productive coral reefs are
being stressed by human activities.
Threats to Coral Reefs
Ecological and Economic services of Coral
Reefs
• Remove CO2 from the atmosphere
• Help protect costline from erosion
• Support many species of marine like and
account for 1/10 of the world’s fish catch.
• Provide jobs and building materials for some
of the world’s poorest countries
Vulnerable to damage because:
• Grow slowly
• Disrupted easily
• Thrive only in clear, warm, fairly shallow
waters with high salinity
Biological Zones in the Open Sea:
Light Rules
• Euphotic zone: brightly lit surface layer.
– Nutrient levels low, dissolved O2 high, photosynthetic activity.
• Bathyal zone: dimly lit middle layer.
– No photosynthetic activity, zooplankton and fish live there and migrate to euphotic zone to feed at night.
• Abyssal zone: dark bottom layer.
Effects of Human Activities on Marine Systems: Red Alert
• Human activities are
destroying or
degrading many ecological and
economic services provided by the
world’s coastal areas.
FRESHWATER LIFE ZONES
• Freshwater life zones
include:
– Standing (lentic) water
such as lakes, ponds, and inland wetlands.
– Flowing (lotic) systems
such as streams and rivers.
Lakes: Water-Filled Depressions
• Lakes are large natural bodies of standing
freshwater formed from precipitation, runoff, and groundwater seepage consisting of:
– Littoral zone (near shore, shallow, with rooted
plants).
– Limnetic zone (open, offshore area, sunlit).
– Profundal zone (deep, open water, too dark for
photosynthesis).
– Benthic zone (bottom of lake, nourished by dead
Effects of Plant Nutrients on Lakes: Too Much of a Good Thing
• Plant nutrients from a lake’s environment affect
the types and numbers of organisms it can support.
– Oligotrophic (poorly nourished) lake: Usually newly
formed lake with small supply of plant nutrient input.
– Eutrophic (well nourished) lake: Over time, sediment,
Effects of Plant Nutrients on Lakes:
Too Much of a Good Thing
• Cultural eutrophication:
– Human inputs of nutrients from the atmosphere and
Lakes: Water-Filled Depressions
• During summer and winter in deep temperate
zone lakes the become stratified into temperature layers and will overturn.
– This equalizes the temperature at all depths. – Oxygen is brought from the surface to the lake
Seasonal Changes in Temperate Lakes
• Thermal stratification of deep lakes in
temperate areas
• Summer months: 3 layers
1. Epilimnion – upper layer, high DO
2. Thermocline- water temps change rapidly with depth, moderat DO
Fall Overturn
• Brings nutrients from bottom to surface and
brings DO from surface to bottom
• Spring overturn – briefly nutrients and DO are
Characteristics of freshwater streams and rivers:
• Surface water- precip that does not sink into
the ground or evaporate
• Runoff- surface water that flows into streams • Watershed or drainage basin- the land area
that delivers runoff, sediment and dissolved substances to a stream
• Harrisburg/Concord in Yadkin-PeeDee water
Freshwater Streams and Rivers:
From the Mountains to the Oceans
• Water flowing from mountains to the sea creates
different aquatic conditions and habitats.
Fig. 6-17, p. 139 Source Zone
Rain and
snow Lake GlacierRapids
Waterfall
Tributary
Freshwater Inland Wetlands:
Vital Sponges
• Inland wetlands
act like natural sponges that
absorb and store excess water from storms and
provide a variety of wildlife
habitats.
Freshwater Inland Wetlands:
Vital Sponges
Filter and degrade pollutants.
Reduce flooding and erosion by absorbing slowly
releasing overflows.
Help replenish stream flows during dry periods.
Help recharge ground aquifers.
Impacts of Human Activities on
Freshwater Systems
• Dams, cities, farmlands, and filled-in wetlands alter and degrade freshwater habitats.
– Dams, diversions and canals have fragmented about 40% of the
world’s 237 large rivers.
– Flood control levees and dikes alter and destroy aquatic
habitats.
– Cities and farmlands add pollutants and excess plant nutrients to
streams and rivers.
– Many inland wetlands have been drained or filled for agriculture
Bad News
• Everything that goes in a watershed ends up in
Good News
• Aquatic life zones are constantly renewed
• Water is purified naturally by hydrologic cycle • Nutrients cycle in and out
• Populations can be replenished if given