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(1)

Chapter 7

(2)

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

(3)

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

(4)

AQUATIC ENVIRONMENTS

Saltwater (marine) and freshwater aquatic life

(5)

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

(6)

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.

(7)

Salt water life zones

1. 99.5% of earth’s habitable volume 2. 250,000 known species of marine

plants/animals

(8)

SALTWATER LIFE ZONES

The oceans that occupy

most of the earth’s

surface provide many ecological and

economic services.

(9)

Two major life zones

(10)

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.

(11)

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.

(12)

Mangrove Forests

Are found along

about 70% of gently sloping sandy and silty coastlines in tropical and subtropical regions.

(13)

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.

(14)

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.

(15)

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

(16)

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.

(17)

Threats to Coral

Reefs:

Increasing

Stresses

Biologically diverse

and productive coral reefs are

being stressed by human activities.

(18)

Threats to Coral Reefs

(19)

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

(20)

Vulnerable to damage because:

Grow slowly

Disrupted easily

Thrive only in clear, warm, fairly shallow

waters with high salinity

(21)

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.

(22)

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.

(23)

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.

(24)

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

(25)

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,

(26)

Effects of Plant Nutrients on Lakes:

Too Much of a Good Thing

Cultural eutrophication:

Human inputs of nutrients from the atmosphere and

(27)

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

(28)

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

(29)

Fall Overturn

Brings nutrients from bottom to surface and

brings DO from surface to bottom

Spring overturn – briefly nutrients and DO are

(30)

Characteristics of freshwater streams and rivers:

Surface water- precip that does not sink into

the ground or evaporate

Runoff- surface water that flows into streamsWatershed or drainage basin- the land area

that delivers runoff, sediment and dissolved substances to a stream

Harrisburg/Concord in Yadkin-PeeDee water

(31)

Freshwater Streams and Rivers:

From the Mountains to the Oceans

Water flowing from mountains to the sea creates

different aquatic conditions and habitats.

(32)

Fig. 6-17, p. 139 Source Zone

Rain and

snow Lake GlacierRapids

Waterfall

Tributary

(33)

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.

(34)

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.

(35)

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

(36)

Bad News

Everything that goes in a watershed ends up in

(37)

Good News

Aquatic life zones are constantly renewed

Water is purified naturally by hydrologic cycleNutrients cycle in and out

Populations can be replenished if given

References

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