Chapter 6 Aquatic Biodiversity
Chapter 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 saltwater life zones, and how do human activities affect them? What are the major types of freshwater life zones, and how do human activities affect them?
Updates Online The latest references for topics covered in this section can be found at the book companion website. Log in to the book’s e-resources page at www.thomsonedu.com to access InfoTrac articles.
InfoTrac: Down the bayou: a marine biologist, a community, and the resolve to preserve an ocean's bounty. Taylor Sisk. Earth Island Journal, Autumn 2006 v21 i3 p27(6). InfoTrac: A scourge of the '70s returns to Great Lakes. The Christian Science Monitor, March 30, 2006 p14. InfoTrac: The fate of the ocean. Julia Whitty. Mother Jones, March-April 2006 v31 i2 p32(15). National Oceanic and Atmospheric Administration: Fisheries Amazon Conservation Association: Amazon Rivers Project
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 colonies of polyps. Figure 6-1
Fig. 6-1a, p. 126
Fig. 6-1b, p. 126
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 organisms.
AQUATIC ENVIRONMENTS Saltwater and freshwater aquatic life zones
cover almost three-fourths of the earth’s surface
Figure 6-2
Ocean hemisphere
Land–ocean hemisphere
Fig. 6-2, p. 127
AQUATIC ENVIRONMENTS
Figure 6-3
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)
Necton: fish, turtles, whales. Benthos: bottom dwellers (barnacles, oysters). Decomposers: breakdown organic compounds (mostly bacteria).
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.
Euphotic zone (upper layer in deep water habitats): sunlight can penetrate.
SALTWATER LIFE ZONES The oceans that
occupy most of the earth’s surface provide many ecological and economic services.
Figure 6-4
Natural Capital Marine Ecosystems Economic Services
Ecological Services
Climate moderation
Food
CO2 absorption
Animal and pet feed
Nutrient cycling Waste treatment Reduced storm impact (mangroves, barrier islands, coastal wetlands) Habitats and nursery areas
Pharmaceuticals Harbors and transportation routes Coastal habitats for humans Recreation Employment
Genetic resources and biodiversity
Oil and natural gas
Scientific information
Building materials
Minerals
Fig. 6-4, p. 129
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. Subject to human disturbance.
The Coastal Zone
Figure 6-5
Euphotic Zone
Photosynthesis
Sun
Twilight
Estuarine Zone Continental shelf
Open Sea Sea level
Bathyal Zone
Abyssal Zone
Darkness
High tide Coastal Zone Low tide
Fig. 6-5, p. 130
Marine Ecosystems Scientists estimate
that marine systems provide $21 trillion in goods and services per year – 70% more than terrestrial ecosystems.
Figure 6-4
Fig. 6-6, p. 130
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.
Figure 6-7
Herring gulls
Peregrine falcon
Snowy Egret
Cordgrass Short-billed Dowitcher
Marsh Periwinkle Phytoplankton
Smelt
Soft-shelled clam
Zooplankton and small crustaceans
Clamworm Bacteria Producer to primary consumer
Primary to secondary consumer
Secondary to higher-level consumer
All consumers and producers to decomposers
Fig. 6-7a, p. 131
Fig. 6-7b, p. 131
Mangrove Forests (Stopped) Are found along
about 70% of gently sloping sandy and silty coastlines in tropical and subtropical regions.
Figure 6-8
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. Provide food, habitats and nursery sites for many aquatic species.
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. Intertidal Zone: area of shoreline between low and high 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 Figure 6-9
Rocky Shore Beach
Hermit crab
Sea star
Shore crab High tide Periwinkle
Sea urchin
Anemone
Mussel Low tide
Sculpin Barnacles Kelp
Sea lettuce
Monterey flatworm Nudibranch Fig. 6-9, p. 132
Barrier Beach Beach flea Peanut worm Blue crab
Tiger Beetle Clam
Dwarf Olive
High tide
Sandpiper Low tide
Silversides
White sand macoma
Sand dollar
Mole Shrimp
Ghost Shrimp
Moon snail Fig. 6-9, p. 132
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.
Figure 6-10
Ocean
Beach Intensive recreation, no building
Primary Dune
Trough
Secondary Dune
No direct No direct Limited passage passage recreation or building and walkways or building
Grasses or shrubs Taller shrubs
Back Dune Most suitable for development
Bay or Lagoon Intensive recreation
Bay shore No filling
Taller shrubs and trees
Fig. 6-10, p. 133
Threats to Coral Reefs: Increasing Stresses Biologically
diverse and productive coral reefs are being stressed by human activities. Figure 6-11
Gray reef shark Green sea turtle
Sea nettle
Fairy basslet Blue tangs Parrot fish
Sergeant major
Hard corals Algae
Brittle star Banded coral shrimp
Phytoplankton Symbiotic algae Zooplankton
Coney
Blackcap basslet
Sponges
Bacteria Producer to Primary to primary secondary consumer consumer
Secondary to higher-level consumer
Moray eel
All consumer and producers to decomposers
Fig. 6-11, p. 134
Natural Capital Degradation Coral Reefs
Ocean warming Soil erosion Algae growth from fertilizer runoff Mangrove destruction Bleaching Rising sea levels Increased UV exposure Damage from anchors Damage from fishing and diving Fig. 6-12, p. 135
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.
Very cold, little dissolved O2.
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. Figure 6-13
Natural Capital Degradation Marine Ecosystems
Half of coastal wetlands lost to agriculture and urban development Over one-third of mangrove forests lost to agriculture, development, and aquaculture shrimp farms Beaches eroding because of coastal development and rising sea level Ocean bottom habitats degraded by dredging and trawler fishing At least 20% of coral reefs severely damaged and 30– 50% more threatened Fig. 6-13, p. 136
FRESHWATER LIFE ZONES(STOPPED) 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
Natural Capital Freshwater Systems EcologicalNatural CapitalEconomic Services Services Climate moderation
Food
Nutrient cycling
Drinking water
Waste treatment
Irrigation water
Flood control
Hydroelectricity
Groundwater recharge
Transportation corridors
Habitats for many species
Recreation
Genetic resources and biodiversity Scientific information
Employment
Fig. 6-14, p. 136
Lakes: Water-Filled Depressions(STOPPED 6-7) 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).
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 bottom and nutrients from the bottom are brought to the top.
What causes this overturning?
Lake in Winter
Lake in Spring
Lake in Summer
Lakes: Water-Filled Depressions
Figure 6-15
Sunlight Green frog
Painted turtle
Blue-winged teal Muskrat
Pond snail Littoral zone Limnetic zone Diving beetle
Plankton
Profundal zone Benthic zone Yellow perch
Bloodworms
Northern pike Fig. 6-15, p. 137
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. Figure 6-16
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, organic material, and inorganic nutrients wash into lakes causing excessive plant growth.
Effects of Plant Nutrients on Lakes: Too Much of a Good Thing Cultural eutrophication:
Human inputs of nutrients from the atmosphere and urban and agricultural areas can accelerate the eutrophication process.
Freshwater Streams and Rivers: From the Mountains to the Oceans
Water flowing from mountains to the sea
creates different aquatic conditions and habitats. Figure 6-17
Rain and snow
Lake Glacier Rapids Waterfall Tributary Flood plain Oxbow lake Salt marsh Delta Deposited sediment Ocean Source Zone Transition Zone
Floodplain Zone
Water Sediment
Fig. 6-17, p. 139
Case Study: Dams, Wetlands, Hurricanes, and New Orleans Dams and levees have been built to control
water flows in New Orleans. Reduction in natural flow has destroyed natural wetlands.
Causes city to lie below sea-level (up to 3 meters). Global sea levels have risen almost 0.3 meters since 1900.
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. Figure 6-18
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. Provide economic resources and recreation.
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 or (sub)urban development.
Impacts of Human Activities on Freshwater Systems These wetlands
have been ditched and drained for cropland conversion.
Figure 6-19