Title: Aquatic Ecology Notes
1Aquatic Ecology Notes
2Chapter Overview Questions
- What are the basic types of aquatic life zones
and what factors influence the kinds of life they
contain? - What are the major types of freshwater life
zones, and how do human activities affect them?
3Chapter Overview Questions
- What do we know about aquatic biodiversity, and
what is its economic and ecological importance? - How are human activities affecting aquatic
biodiversity? - How can we manage and sustain the worlds marine
fisheries?
4Chapter Overview Questions (contd)
- How can we protect, sustain, and restore
wetlands? - How can we protect, sustain, and restore lakes,
rivers, and freshwater fisheries?
5Chapter Overview Questions
- Why is water so important, how much freshwater is
available to us, and how much of it are we using? - What causes freshwater shortages, and what can be
done about this problem? - What are the advantages and disadvantages of
withdrawing groundwater? - What are the advantages and disadvantages of
using dams and reservoirs to supply more water?
6Chapter Overview Questions (contd)
- What are the advantages and disadvantages of
transferring large amounts of water from one
place to another? - Can removing salt from seawater solve our water
supply problems? - How can we waste less water?
- How can we use the earths water more
sustainably? - What causes flooding, and what can we do about it?
7The Water Resource
8Importance
- Leonardo da Vinci said that Water is the driver
of nature. Without water, the other nutrient
cycles would not exist in their present forms,
and current forms of life on earth could not
exist.
9Hydrogen Bonds
10Attraction Between Molecules
- The strong forces of attraction between molecules
of water.
11Heat Capacity
- Water changes temp very slowly because it can
store heat. This protects living organisms from
the shock of abrupt temperature changes.
12Heat of Vaporization
- The temperature at which water turns to vapor.
13Universal Solvent
- Water can dissolve a wide variety of compounds.
This means it can easily become polluted by
water-soluble wastes.
14Expansion When Frozen
- Ice has a lower density than liquid water. Thus,
ice floats on water.
15Surface Water
- Examples streams, rivers, and lakes
- Source precipitation
- Watershed Ex. small streams ? larger streams ?
rivers ? sea
16Groundwater
- Aquifersporous rock w/ water flowing through
- Water Table the level of earths land crust to
which the aquifer is filled - Renewability the circulation rate of
groundwater is slow (300 to 4,600 years).
17WATERS IMPORTANCE, AVAILABILITY, AND RENEWAL
- Water keeps us alive, moderates climate, sculpts
the land, removes and dilutes wastes and
pollutants, and moves continually through the
hydrologic cycle. - Only about 0.02 of the earths water supply is
available to us as liquid freshwater.
18WATERS IMPORTANCE, AVAILABILITY, AND RENEWAL
- Comparison of population sizes and shares of the
worlds freshwater among the continents.
Figure 14-2
19WATERS IMPORTANCE, AVAILABILITY, AND RENEWAL
- Some precipitation infiltrates the ground and is
stored in soil and rock (groundwater). - Water that does not sink into the ground or
evaporate into the air runs off (surface runoff)
into bodies of water. - The land from which the surface water drains into
a body of water is called its watershed or
drainage basin.
20Hydrologic Cycle
21 Unconfined Aquifer Recharge Area
Evaporation and transpiration
Evaporation
Precipitation
Confined Recharge Area
Runoff
Flowing artesian well
Recharge Unconfined Aquifer
Stream Well requiring a pump
Water table
Infiltration
Lake
Infiltration
Unconfined aquifer
Less permeable material such as clay
Confined aquifer
Confining impermeable rock layer
Fig. 14-3, p. 308
22Water Usage
- Irrigation watering crops
- Industry coolant (power plant)
- Domestic and Municipal drinking, sewage,
bathwater, dishwater laundry
23WATERS IMPORTANCE, AVAILABILITY, AND RENEWAL
- We currently use more than half of the worlds
reliable runoff of surface water and could be
using 70-90 by 2025. - About 70 of the water we withdraw from rivers,
lakes, and aquifers is not returned to these
sources. - Irrigation is the biggest user of water (70),
followed by industries (20) and cities and
residences (10).
24Salinity
25Niches
26What 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) - Necton fish, turtles, whales.
- Benthos bottom dwellers (barnacles, oysters).
- Decomposers breakdown organic compounds (mostly
bacteria).
27Phytoplankton
- Description small drifting plants
- Niche they are producers that support most
aquatic food chains - Example cyanobacteria many types of algae
28Zooplankton
- Description herbivores that feed on
phytoplankton or other zooplankton - Niche food stock for larger consumers
- Example krill small crustaceans
29Nekton
- Description larger, strong-swimming consumers
- Niche top consumers in the aquatic ecosystem
- Example fish, turtles, and whales
30Benthos
- Description bottom-dwelling creatures
- Niche primary consumers, decomposers
- Example barnacles, oysters, and lobsters
31Freshwater Ecosystems
32FRESHWATER LIFE ZONES
- Freshwater life zones include
- Standing (lentic) water such as lakes, ponds, and
inland wetlands. - Flowing (lotic) systems such as streams and
rivers.
Figure 6-14
33Flowing Water Ecosystems
- Because of different environmental conditions in
each zone, a river is a system of different
ecosystems.
34Natural Capital
Ecological Services of Rivers
- Deliver nutrients to sea to help sustain
coastal fisheries - Deposit silt that maintains deltas
- Purify water
- Renew and renourish wetlands
- Provide habitats for wildlife
Fig. 12-11, p. 267
35Freshwater Streams and RiversFrom the Mountains
to the Oceans
- Water flowing from mountains to the sea creates
different aquatic conditions and habitats.
Figure 6-17
36Headwater Stream Characteristics
- A narrow zone of cold, clear water that rushes
over waterfalls and rapids. Large amounts of
oxygen are present. Fish are also present. Ex.
trout.
37Downstream Characteristics
- Slower-moving water, less oxygen, warmer
temperatures, and lots of algae and
cyanobacteria.
38Energy Source
39Standing Water Ecosystems
40Life 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. - Euphotic zone (upper layer in deep water
habitats) sunlight can penetrate.
41Lakes 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
matter).
42Littoral Zone
- A shallow area near the shore, to the depth at
which rooted plants stop growing. Ex. frogs,
snails, insects, fish, cattails, and water lilies.
43Limnetic Zone
- Open, sunlit water that extends to the depth
penetrated by sunlight.
44Profundal Zone
- Deep, open water where it is too dark for
photosynthesis.
45Thermal Stratification
46Lakes Water-Filled Depressions
Figure 6-15
47Definition
- The temperature difference in deep lakes where
there are warm summers and cold winters.
48Lakes 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
bottom and nutrients from the bottom are brought
to the top.
49Causes
- During the summer, lakes become stratified into
different temperature layers that resist mixing
because summer sunlight warms surface waters,
making them less dense.
50Thermocline
- The middle layer that acts as a barrier to the
transfer of nutrients and dissolved oxygen.
51Fall Turnover
- As the temperatures begin to drop, the surface
layer becomes more dense, and it sinks to the
bottom. This mixing brings nutrients from the
bottom up to the surface and sends oxygen to the
bottom.
52Spring Turnover
- As top water warms and ice melts, it sinks
through and below the cooler, less dense water,
sending oxygen down and nutrients up.
53Freshwater Wetlands
54Freshwater 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.
Figure 6-18
55Freshwater 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.
- Provide economic resources and recreation.
56Marshes
- An area of temporarily flooded, often silty land
beside a river or lake.
57Swamps
- A lowland region permanently covered with water.
58Hardwood Bottomland Forest
- An area down by a river or stream where lots of
hardwoods, like oaks, grow.
59Prairie Potholes
- These are depressions that hold water out on the
prairie, especially up north in Canada. It is a
very good duck habitat.
60Peat Moss Bog
- A wet area that over time fills in (the last
stage of succession is peat moss). It can be
very deep. In Ireland, they burn this for wood.
61Importance of freshwater wetlands
- They filter purify water.
- Habitat for many animals and plants.
62Historical Aspects
- Developers and farmers want Congress to revise
the definition of wetlands. This would make
60-75 of all wetlands unavailable for
protection. The Audubon Society estimates that
wetlands provide water quality protection worth
1.6 billion per year, and they say if that
wetlands are destroyed, the U.S. would spend 7.7
billion to 31 billion per year in additional
flood-control costs.
63Estuaries
64Definition
- A partially enclosed area of coastal water where
sea water mixes with freshwater.
65Salt Marshes
- The ground here is saturated with water and there
is little oxygen, so decay takes place slowly.
It has a surface inlet and outlet, and contains
many invertebrates. It is also the breeding
ground for many ocean animals. Ex. crabs and
shellfish.
66Mangrove Forests
- These are along warm, tropical coasts where there
is too much silt for coral reefs to grow. It is
dominated by salt-tolerant trees called mangroves
(55 different species exist). It also helps to
protect the coastline from erosion and provides a
breeding nursery for some 2000 species of fish,
invertebrates, and plants.
67Importance of Estuaries
- Just one acre of estuary provides 75,000 worth
of free waste treatment, and has a value of about
83,000 when recreation and fish for food are
included. - Prime Kansas farmland has a top value of 1,200
and an annual production value of 600.
68The Everglades
- Southern Florida to the Keys
69Case Study Restoring the Florida Everglades
- The worlds largest ecological restoration
project involves trying to undo some of the
damage inflicted on the Everglades by human
activities. - 90 of parks wading birds have vanished.
- Other vertebrate populations down 75-95.
- Large volumes of water that once flowed through
the park have been diverted for crops and cities. - Runoff has caused noxious algal blooms.
70Problems
- As Miami develops, it encroaches on everglades.
Plus, it prompts people vs. wildlife. It is
freshwater and local areas are draining it.
71Restoring the Florida Everglades
- The project has been attempting to restore the
Everglades and Florida water supplies.
Figure 12-10
72Restoration
- Build huge aqueduct, or find other sources of
fresh water an protect it federally under
endangered species act, etc.
73Problems
74Too Much Water
- Problems include flooding, pollution of water
supply, and sewage seeping into the ground.
75TOO MUCH WATER
- Heavy rainfall, rapid snowmelt, removal of
vegetation, and destruction of wetlands cause
flooding. - Floodplains, which usually include highly
productive wetlands, help provide natural flood
and erosion control, maintain high water quality,
and recharge groundwater. - To minimize floods, rivers have been narrowed
with levees and walls, and dammed to store water.
76TOO MUCH WATER
- Comparison of St. Louis, Missouri under normal
conditions (1988) and after severe flooding
(1993).
Figure 14-22
77TOO MUCH WATER
- Human activities have contributed to flood deaths
and damages.
Figure 14-23
78 Forested Hillside
Oxygen released by vegetation
Diverse ecological habitat
Evapotranspiration
Trees reduce soil erosion from heavy rain and wind
Agricultural land
Steady river flow
Leaf litter improves soil fertility
Tree roots stabilize soil and aid water flow
Vegetation releases water slowly and reduces
flooding
Fig. 14-23a, p. 330
79 After Deforestation
Tree plantation
Evapotranspiration decreases
Roads destabilize hillsides
Ranching accelerates soil erosion by water and
wind
Winds remove fragile topsoil
Gullies and landslides
Agricultural land is flooded and silted up
Heavy rain leaches nutrients from soil and erodes
topsoil
Rapid runoff causes flooding
Silt from erosion blocks rivers and reservoirs
and causes flooding downstream
Fig. 14-23b, p. 330
80Too Little Water
81Examples
- Examples include drought and expanding deserts.
82Overdrawing Surface Water
- Lake levels drop, recreation use drops, fisheries
drop, and salinization occurs. Ex. Soviet Union
(Aral Sea) the inland sea drained the river that
fed into it. Now its a huge disaster (read pg.
322 in text).
1997
1964
83Case Study The Aral Sea Disaster
- Diverting water from the Aral Sea and its two
feeder rivers mostly for irrigation has created a
major ecological, economic, and health disaster. - About 85 of the wetlands have been eliminated
and roughly 50 of the local bird and mammal
species have disappeared. - Since 1961, the seas salinity has tripled and
the water has dropped by 22 meters most likely
causing 20 of the 24 native fish species to go
extinct.
84Aquifer Depletion
- This harms endangered species, and salt water can
seep in.
85Salinization of Irrigated Soil
- Water is poured onto soil and evaporates. Over
time, as this is repeated, nothing will grow
there anymore.
86U.S. Water Problems
87Surface Water Problems
- The polluted Mississippi River (non-source point
pollution) has too much phosphorus. - In the Eerie Canal, which connects the ocean to
the Great Lakes, lampreys came in and depleted
the fish. The zebra mollusk is also a problem in
the Great Lakes.
88Effects of Plant Nutrients on LakesToo Much of
a Good Thing
- Plant nutrients from a lakes environment affect
the types and numbers of organisms it can support.
Figure 6-16
89Effects of Plant Nutrients on LakesToo Much of
a Good Thing
- Plant nutrients from a lakes 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, organic material, and inorganic
nutrients wash into lakes causing excessive plant
growth.
90Effects of Plant Nutrients on LakesToo Much of
a Good Thing
- Cultural eutrophication
- Human inputs of nutrients from the atmosphere and
urban and agricultural areas can accelerate the
eutrophication process.
91Mono Lake
- (like the Dead Sea) This has a huge salt
concentration due to mans draining.
92Colorado River Basin
- These are dams reservoirs that feed from the
Colorado River all the way to San Diego, LA, Palm
Springs, Phoenix Mexico. So far has worked
because they havent withdrawn their full
allocations. See pg306.
93The Colorado River Basin
- The area drained by this basin is equal to more
than one-twelfth of the land area of the lower 48
states.
Figure 14-14
94 IDAHO
WYOMING
Dam
Aqueduct or canal
Salt Lake City
Upper Basin
Denver
Grand Junction
Lower Basin
UPPER BASIN
UTAH
Colorado River
NEVADA
Lake Powell
COLORADO
Grand Canyon
Glen Canyon Dam
Las Vegas
NEW MEXICO
Boulder City
CALIFORNIA
Los Angeles
ARIZONA
Albuquerque
LOWER BASIN
Palm Springs
0
100 mi.
Phoenix
San Diego
Yuma
0
150 km
Tucson
Mexicali
All-American Canal
MEXICO
Gulf of California
Fig. 14-14, p. 318
95Case Study The Colorado Basin an Overtapped
Resource
- The Colorado River has so many dams and
withdrawals that it often does not reach the
ocean. - 14 major dams and reservoirs, and canals.
- Water is mostly used in desert area of the U.S.
- Provides electricity from hydroelectric plants
for 30 million people (1/10th of the U.S.
population).
96Case Study The Colorado Basin an Overtapped
Resource
- Lake Powell, is the second largest reservoir in
the U.S. - It hosts one of the hydroelectric plants located
on the Colorado River.
Figure 14-15
97Groundwater Problems
- These include pollution, salt, and draining too
much.
98Other Effects of Groundwater Overpumping
- Sinkholes form when the roof of an underground
cavern collapses after being drained of
groundwater.
Figure 14-10
99Groundwater Depletion A Growing Problem
- Areas of greatest aquifer depletion from
groundwater overdraft in the continental U.S.
- The Ogallala, the worlds largest aquifer, is
most of the red area in the center (Midwest).
Figure 14-8
100Ogallala Aquifer
- This is the worlds largest known aquifer, and
fuels agricultural regions in the U.S. It
extends from South Dakota to Texas. Its
essentially a non-renewable aquifer from the last
ice age with an extremely slow recharge rate. In
some cases, water is pumped out 8 to 10 times
faster than it is renewed. Northern states will
still have ample supplies, but for the south its
getting thinner. It is estimated that ¼ of the
aquifer will be depleted by 2020.
101Global Water Problems
102Impacts 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 worlds 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 or (sub)urban development.
103Core Case Study A Biological Roller Coaster Ride
in Lake Victoria
- Lake Victoria has lost their endemic fish species
to large introduced predatory fish.
Figure 12-1
104Core Case Study A Biological Roller Coaster Ride
in Lake Victoria
- Reasons for Lake Victorias loss of biodiversity
- Introduction of Nile perch.
- Lake experienced algal blooms from nutrient
runoff. - Invasion of water hyacinth has blocked sunlight
and deprived oxygen. - Nile perch is in decline because it has eaten its
own food supply.
105Stable Runoff
- As water runs off from rain, its supposed to get
into rivers, and finally off to the sea. But
when we dam rivers, less goes to the ocean,
meaning the brackish water (where the river hits
the ocean) becomes more salty. This is the
breeding ground for many fish and invertebrates.
This harms the ecology of the area.
106Drinking Water Problems
107Coliform Bacteria
- The W.H.O. recommends there be zero colonies of
bacteria per 100ml of drinking water and 200
colonies per 100ml of swimming water. The
average human excretes 2 billion organisms per
day (see how easily untreated sewage can
contaminate water?).
108Oxygen Demanding Wastes
- These are organic wastes that can be decomposed
by aerobic bacteria (causes lack of oxygen).
Fish die as a result of a lack of oxygen.
109Water-Soluble Inorganic Chemicals
- These include acids, salts, mercury, and lead.
They make water unfit to drink.
110Organic Material
- These include oil, gas, plastics, pesticides, and
detergents.
111Population Growth
- Problems include over-drawing fresh water,
pollution, and over-building so that water cant
seep into the ground.
112Sharing Water Resources
- There are water wars out west. California bought
the water from the Colorado River, but Arizona
wants it. Who owns it? The same thing is
happening in Texas. More water rights are sold
than the actual amount of water. How do you
share water? This is a problem all over the
world.
113Water Management
114Dams and Reservoirs
- Description A dammed stream that can capture
store water from rain melted snow. - Benefits Hydroelectric power provides water
to towns recreation controls floods downstream - Problems Reduces downstream flow prevents
water from reaching the sea (Colorado River)
devastates fish life reduces biodiversity.
115USING DAMS AND RESERVOIRS TO SUPPLY MORE WATER
- Large dams and reservoirs can produce cheap
electricity, reduce downstream flooding, and
provide year-round water for irrigating cropland,
but they also displace people and disrupt aquatic
systems.
116 Provides water for year-round irrigation of
cropland
Flooded land destroys forests or cropland and
displaces people
Large losses of water through evaporation
Provides water for drinking
Downstream cropland and estuaries are deprived of
nutrient-rich silt
Reservoir is useful for recreation and fishing
Risk of failure and devastating downstream
flooding
Can produce cheap electricity (hydropower)
Downstream flooding is reduced
Migration and spawning of some fish are disrupted
Fig. 14-13a, p. 317
117 Powerlines
Reservoir
Dam
Powerhouse
Intake
Turbine
Fig. 14-13b, p. 317
118Case Study Chinas Three Gorges Dam
- There is a debate over whether the advantages of
the worlds largest dam and reservoir will
outweigh its disadvantages. - The dam will be 2 kilometers long.
- The electric output will be that of 18 large
coal-burning or nuclear power plants. - It will facilitate ship travel reducing
transportation costs. - Dam will displace 1.2 million people.
- Dam is built over seismatic fault and already has
small cracks.
119Dam Removal
- Some dams are being removed for ecological
reasons and because they have outlived their
usefulness. - In 1998 the U.S. Army Corps of Engineers
announced that it would no longer build large
dams and diversion projects in the U.S. - The Federal Energy Regulatory Commission has
approved the removal of nearly 500 dams. - Removing dams can reestablish ecosystems, but can
also re-release toxicants into the environment.
120Water Diversion
- Description Damming a river to control where
the water flows - Benefits Keeps water where we want it- cities!
- Problems Drains wetlands, destroys land
121Desalinization
- Description Removing salt from salt water
- Benefits Freshwater
- Problems Uses lots of energy costs 3-5Xs more
money what do we do with the salt?
122DESALTING SEAWATER, SEEDING CLOUDS, AND TOWING
ICEBERGS AND GIANT BAGGIES
- Removing salt from seawater by current methods is
expensive and produces large amounts of salty
wastewater that must be disposed of safely. - Distillation heating saltwater until it
evaporates, leaves behind water in solid form. - Reverse osmosis uses high pressure to force
saltwater through a membrane filter.
123DESALTING SEAWATER, SEEDING CLOUDS, AND TOWING
ICEBERGS AND GIANT BAGGIES
- Seeding clouds with tiny particles of chemicals
to increase rainfall towing icebergs or huge bags
filled with freshwater to dry coastal areas have
all been proposed but are unlikely to provide
significant amounts of freshwater.
124Harvesting Icebergs
- Description Towing massive icebergs to arid
coastal areas (S. California Saudi Arabia) - Benefits freshwater
- Problems Technology not available costs too
high raise temperatures around the earth.
125INCREASING WATER SUPPLIES BY WASTING LESS WATER
- Sixty percent of the worlds irrigation water is
currently wasted, but improved irrigation
techniques could cut this waste to 5-20. - Center-pivot, low pressure sprinklers sprays
water directly onto crop. - It allows 80 of water to reach crop.
- Has reduced depletion of Ogallala aquifer in
Texas High Plains by 30.
126 Drip irrigation
(efficiency 9095)
Gravity flow
(efficiency 60 and 80 with surge valves)
Center pivot
(efficiency 8095)
Water usually pumped from underground and sprayed
from mobile boom with sprinklers.
Above- or below-ground pipes or tubes deliver
water to individual plant roots.
Water usually comes from an aqueduct system or a
nearby river.
Fig. 14-18, p. 325
127Conservation
- Description Saving the water we have
- Methods recycling conserving at home
xeriscaping fix leaks - Benefits Saves money Saves Wildlife
- Problems bothersome to people lack of caring
laziness
128Fishing Problems Techniques
- The major decline in the worldwide catch of fish
since 1990 is because of over-fishing. - By-catch- fish or animals that were not meant to
be caught.
129Overfishing and Extinction Gone Fishing, Fish
Gone
- About 75 of the worlds commercially valuable
marine fish species are over fished or fished
near their sustainable limits. - Big fish are becoming scarce.
- Smaller fish are next.
- We throw away 30 of the fish we catch.
- We needlessly kill sea mammals and birds.
130Trawler fishing
Fish farming in cage
Spotter airplane
Sonar
Purse-seine fishing
Trawl flap
Trawl lines
Fish school
Trawl bag
Drift-net fishing
Long line fishing
Buoy
Float
Lines with hooks
Deep sea aquaculture cage
Fish caught by gills
Fig. 12-A, p. 255
131Purse Seines
132Purse Seines
- A large purse-like net is put into the ocean and
is then closed like a drawstring purse to trap
the fish. - Tuna is a fish typically caught in purse seines
- Dolphins are a by-catch of purse seines
133Long-line fishing
- Lines are put out that can be up to 80 miles long
w/ thousands of baited hooks on them. These are
left out free-floating for days and then the boat
comes back and picks them up. - Pilot whales, dolphins, sea turtles, and birds
are by-catch of this technique.
134Drift-net fishing
- Each net hangs as much as 50 feet below the
surface and up to 34 miles long. - Anything that comes into contact w/ these nearly
invisible nets are entangled. - This leads to overfishing
- Many unwanted fish and marine mammals, turtles
and seabirds are caught.
135HUMAN IMPACTS ON AQUATIC BIODIVERSITY
- Area of ocean before and after a trawler net,
acting like a giant plow, scraped it.
Figure 12-2
136Population Growth and Pollution
- Each year plastic items dumped from ships and
left as litter on beaches threaten marine life.
Figure 12-3