Importance of the
Ocean Environment
Marine Ecology Notes
Area
Saltwater covers about 71% of
the earth’s surface
Life
 There are 250,000 known species
of marine plants and animals, many
are food for other organisms, like
us.
Temperature
 Solar heat is distributed by ocean currents &
as ocean water evaporates.
 The oceans are major players in the earth’s
climate & are a gigantic reservoir for carbon
dioxide; therefore they help regulate the
temp. of the troposphere.
Zones of the Marine
Environment
Two major zones that break
up into smaller zones –
coastal and the open sea
Coastal Zone
Varies greatly during high
and low tide
Intertidal or Beach
Zone
Broken up into five areas
Lower Shoreface
The deepest part of the beach;
farther into the water, before
the breaker bar that forms
waves
Upper Shoreface
Shallow zone where the waves
begin to form
Forebeach
Contains the swash zone –
place where the waves crash.
Backbeach
Only under water during high tide
Fore-Island Dunes
Sand dunes; doesn't flood often,
except during hurricanes, etc.
Constantly changing due to the wind
Estuary
Where fresh water and salt
water meet
Definition
 An estuary is a coastal body of
water, partly surrounded by land,
with access to the open ocean and
a large supply of fresh water from
a river
Characteristics
Water Levels
Water levels rise and fall with the tides
Salinity
 Salinity fluctuates with tidal cycles,
the time of year, & precipitation.
The organisms that live here must
be able to tolerate these conditions
Fertility of Estuaries
 Estuaries are the most fertile
ecosystems in the world
 Greater productivity than either the
adjacent ocean or the fresh water
upriver
Reasons for High Fertility
 Nutrients are transported from the land into
rivers that flow into the estuary
 Tidal action circulates nutrients and helps
remove wastes
 A high level of light due to shallow water
 Many plants provide an extensive
photosynthetic carpet
The Shoreline
Between High and
Low Tides
Characteristics
Abundant levels of light,
nutrients, and oxygen
Difficulties
 Sandy beach – Life must deal with a shifting
environment that threatens to engulf them & no
protection against wave action. Most animals
bury into the sand. They move with the tides,
so they’re always underwater & don’t dry out.
Difficulties (Continued)
 Rocky shore – high wave action at high tide;
drying out & temperature changes during low.
Animals have a way of sealing in moisture like
a shell & find a way to cling to the rocks so they
don’t get washed away with waves.
The Open Ocean
Pelagic
 The open ocean environment;
divided into neritic (open ocean
from the shoreline to a depth of
200m) and oceanic provinces
(depths > 200m).
Euphotic Zone
Lots of light.
From 0 - 200
meters.
Photosynthesis
takes place
here.
Bathyal Zone
The dimly lit
part of ocean.
From 200 -
1500 meters.
Benthic
The ocean floor or bottom
Benthic Characteristics
 The ocean floor consists of sediments
(mostly sand and mud)
 Many marine animals, like worms and
clams, burrow
 Bacteria are common & can go down 500
meters below ocean floor. The Benthic
environment extends from the shore to
the deep.
Sea Grass Beds
Flowering plants that have adapted to
complete submersion in salty water.
Location of sea grass
 Found in shallow water to depths of
10 meters where they can
photosynthesize. Sea grasses are
found in quiet, temperate, tropical,
and subtropical waters; not in polar
waters.
Eel, turtle, and manatee grass.
Examples
Ecological Importance
 Reduce surface erosion, provide
food, & provide habitats for many
marine organisms.
 Animals that eat sea grass are
manatees, green turtles, parrotfish,
sturgeon fish, and sea urchins.
Abyssal Zone
 Completely dark.
Extends to a depth
of 4000 to 6000
meters (2.5 to 3.7
miles). Water here
is very cold & has
little dissolved
oxygen.
Kelp
 The largest of the brown algae, many reach
lengths of 60 meters (200 feet). Common in
cooler water & are found along rocky coasts.
Provide habitat for many animals like
tubeworms, sponges, clams, fish, & mammals.
Some animals eat the kelp.
Characteristics
 Built from layers of calcium carbonate,
coral reefs are found in warm, shallow sea
water. The living portions must grow in
shallow waters where light hits. They are
the most diverse of all marine ecosystems.
Coral Reefs
Examples
 Many coral reefs are made of red coralline
algae that photosynthesize.
 Others have zooxanthellae (symbiotic algae)
that live and photosynthesize in their tissues.
 Not all corals have zooxanthellae, but only
those with it build reefs.
 Coral animals also capture food at night with
stinging tentacles that paralyze zooplankton
and small animals that drift nearby.
Coral Reef Waters
 The waters where coral reefs are
found are often poor in nutrients.
Yet, other factors are favorable
such as temperature, sunlight year
round, and zooxanthellae.
Growth
Coral reefs grow slowly; as one
dies, another organism grows
on it.
Types of Coral Reefs
Fringing Reef
The most common type of coral
reef. It is directly attached to
the shore of a volcanic island or
continent.
Fringing Reef Bora Bora NASA JPL Satellite: Space Shuttle Sensor: SIR-C/X-SAR
Atoll
 A circular reef that surrounds a
central lagoon of quiet water.
 An atoll forms on top of the cone of
a submerged volcanic island.
 More than 300 atolls are found in the
Pacific and Indian Oceans.
View of Midway Atoll from Space Shuttle
Atolls in The Maldives Landsat 7
Barrier Reef
 A lagoon of open water separates
the land from the barrier reef.
 The largest barrier reef is the Great
Barrier Reef off the coast of
Australia.
 The second largest is off the coast
of Belize.
Provides a Habitat
Provides a habitat for a wide
variety of marine organisms.
Ecological Importance
of Coral Reefs
Coastline Protection
Protects coasts from shoreline
erosion.
Benefits for Humans
Provides humans with seafood,
pharmaceuticals, and
recreational/tourism dollars
Coral Reef Risks
 Of the 109 countries with large reefs,
90 are damaging them, and 27% of
the coral reefs are at high risk,
especially off the coast of
Southeastern Asia.
 In the western Atlantic, 30-50% of
all coral species are either rare or
endangered.
Coral Reef Risks Con’t
 Silt washing from downstream has
smothered the reefs
 High salinity from fresh water diversion,
over-fishing, boat groundings, fishing
with dynamite or cyanide, hurricane
damage, disease, coral bleaching, land
reclamation, tourism, and the mining of
coral for building materials.
©1997-2001 Jeffrey N. Jeffords
This bottle still shows a slightly burned
fuse from its use to blow up the coral.
Protection of
 300 coral reefs in 65 countries are
protected as reserves or parks, and
another 600 have been
recommended for protection.
 The good news is coral reefs can
often recover from damage.
Pollution and
Human Impact
Massive Oil Slicks in Bahrain
African Proverb
 “Water may flow in a thousand
channels, but it all returns to the
sea.”
 The oceans are the ultimate sink
for much of the waste matter we
produce.
Differences of Opinion
 Oceans dilute, disperse, and degrade large
amounts of raw sewage, sewage sludge, oil,
and some types of industrial waste, especially
in deep-water areas.
 Marine life has proved to be more resilient
than some scientists expected, some suggest it
is safer to dump sludge & other hazardous
wastes into the deep ocean than to bury them
on land or burn them.
Differences of Opinion
Other scientists disagree, pointing
out that we know less about the
deep ocean than we do about
space. They say that dumping
waste in the ocean would delay
urgently needed pollution prevention
and promote further degradation of
this vital part of the earth’s life-
support system.
Oil Spills
 When a tanker accident happens, it gets lots
of publicity.
 But, more oil is released by normal operation
of offshore wells, washing tankers & from
pipeline or storage tank leaks.
 One estimate says that oil companies spill,
leak, or waste per year an amount of oil
equal to that shipped by 1000 huge Exxon
Valdez tankers.
Floating Oil
 Oil coats the feathers of birds (especially
diving birds) and the fur of marine
animals, destroying the animals’ natural
insulation and buoyancy
 Many drown or die of exposure from loss
of body heat.
Other Information
 Oil is broken down by bacteria over time;
slower in cold waters.
 Heavy oil components can smother bottom-
dwelling organisms such as crabs, oysters,
mussels, and clams, or make them unfit to eat.
 Oil spills have killed coral reefs. A recent study
showed that diesel oil becomes more toxic to
marine life with the passage of time.
Clean Up
Mechanical Methods
 Floating booms contain the oil spill or keep it
from reaching sensitive areas
 Skimmer boats are used to vacuum up some of
the oil into collection barges
 Absorbent pads or large feather-filled pillows
are used to soak up oil on beaches or in waters
that are too shallow for skimmer boats
Chemical Methods
 Coagulating agents cause floating oil to clump
together for easier pickup or sink to the
bottom, where it usually does less harm.
 Dispersing agents break up oil slicks. However,
these can also damage some types of
organisms.
 Fire can also burn off floating oil, but crude oil
is hard to ignite.

Marine Ecology Notes.ppt

  • 1.
    Importance of the OceanEnvironment Marine Ecology Notes
  • 2.
    Area Saltwater covers about71% of the earth’s surface
  • 3.
    Life  There are250,000 known species of marine plants and animals, many are food for other organisms, like us.
  • 4.
    Temperature  Solar heatis distributed by ocean currents & as ocean water evaporates.  The oceans are major players in the earth’s climate & are a gigantic reservoir for carbon dioxide; therefore they help regulate the temp. of the troposphere.
  • 5.
    Zones of theMarine Environment Two major zones that break up into smaller zones – coastal and the open sea
  • 6.
    Coastal Zone Varies greatlyduring high and low tide
  • 7.
  • 8.
    Lower Shoreface The deepestpart of the beach; farther into the water, before the breaker bar that forms waves
  • 9.
    Upper Shoreface Shallow zonewhere the waves begin to form
  • 10.
    Forebeach Contains the swashzone – place where the waves crash.
  • 11.
  • 12.
    Fore-Island Dunes Sand dunes;doesn't flood often, except during hurricanes, etc. Constantly changing due to the wind
  • 13.
    Estuary Where fresh waterand salt water meet
  • 14.
    Definition  An estuaryis a coastal body of water, partly surrounded by land, with access to the open ocean and a large supply of fresh water from a river
  • 15.
  • 16.
    Water Levels Water levelsrise and fall with the tides
  • 17.
    Salinity  Salinity fluctuateswith tidal cycles, the time of year, & precipitation. The organisms that live here must be able to tolerate these conditions
  • 18.
    Fertility of Estuaries Estuaries are the most fertile ecosystems in the world  Greater productivity than either the adjacent ocean or the fresh water upriver
  • 19.
    Reasons for HighFertility  Nutrients are transported from the land into rivers that flow into the estuary  Tidal action circulates nutrients and helps remove wastes  A high level of light due to shallow water  Many plants provide an extensive photosynthetic carpet
  • 20.
  • 21.
    Characteristics Abundant levels oflight, nutrients, and oxygen
  • 22.
    Difficulties  Sandy beach– Life must deal with a shifting environment that threatens to engulf them & no protection against wave action. Most animals bury into the sand. They move with the tides, so they’re always underwater & don’t dry out.
  • 23.
    Difficulties (Continued)  Rockyshore – high wave action at high tide; drying out & temperature changes during low. Animals have a way of sealing in moisture like a shell & find a way to cling to the rocks so they don’t get washed away with waves.
  • 24.
  • 25.
    Pelagic  The openocean environment; divided into neritic (open ocean from the shoreline to a depth of 200m) and oceanic provinces (depths > 200m).
  • 26.
    Euphotic Zone Lots oflight. From 0 - 200 meters. Photosynthesis takes place here.
  • 27.
    Bathyal Zone The dimlylit part of ocean. From 200 - 1500 meters.
  • 28.
  • 29.
    Benthic Characteristics  Theocean floor consists of sediments (mostly sand and mud)  Many marine animals, like worms and clams, burrow  Bacteria are common & can go down 500 meters below ocean floor. The Benthic environment extends from the shore to the deep.
  • 30.
    Sea Grass Beds Floweringplants that have adapted to complete submersion in salty water.
  • 31.
    Location of seagrass  Found in shallow water to depths of 10 meters where they can photosynthesize. Sea grasses are found in quiet, temperate, tropical, and subtropical waters; not in polar waters. Eel, turtle, and manatee grass. Examples
  • 32.
    Ecological Importance  Reducesurface erosion, provide food, & provide habitats for many marine organisms.  Animals that eat sea grass are manatees, green turtles, parrotfish, sturgeon fish, and sea urchins.
  • 33.
    Abyssal Zone  Completelydark. Extends to a depth of 4000 to 6000 meters (2.5 to 3.7 miles). Water here is very cold & has little dissolved oxygen.
  • 34.
    Kelp  The largestof the brown algae, many reach lengths of 60 meters (200 feet). Common in cooler water & are found along rocky coasts. Provide habitat for many animals like tubeworms, sponges, clams, fish, & mammals. Some animals eat the kelp.
  • 35.
    Characteristics  Built fromlayers of calcium carbonate, coral reefs are found in warm, shallow sea water. The living portions must grow in shallow waters where light hits. They are the most diverse of all marine ecosystems. Coral Reefs
  • 36.
    Examples  Many coralreefs are made of red coralline algae that photosynthesize.  Others have zooxanthellae (symbiotic algae) that live and photosynthesize in their tissues.  Not all corals have zooxanthellae, but only those with it build reefs.  Coral animals also capture food at night with stinging tentacles that paralyze zooplankton and small animals that drift nearby.
  • 37.
    Coral Reef Waters The waters where coral reefs are found are often poor in nutrients. Yet, other factors are favorable such as temperature, sunlight year round, and zooxanthellae.
  • 38.
    Growth Coral reefs growslowly; as one dies, another organism grows on it.
  • 39.
  • 40.
    Fringing Reef The mostcommon type of coral reef. It is directly attached to the shore of a volcanic island or continent.
  • 42.
    Fringing Reef BoraBora NASA JPL Satellite: Space Shuttle Sensor: SIR-C/X-SAR
  • 43.
    Atoll  A circularreef that surrounds a central lagoon of quiet water.  An atoll forms on top of the cone of a submerged volcanic island.  More than 300 atolls are found in the Pacific and Indian Oceans.
  • 45.
    View of MidwayAtoll from Space Shuttle
  • 46.
    Atolls in TheMaldives Landsat 7
  • 47.
    Barrier Reef  Alagoon of open water separates the land from the barrier reef.  The largest barrier reef is the Great Barrier Reef off the coast of Australia.  The second largest is off the coast of Belize.
  • 50.
    Provides a Habitat Providesa habitat for a wide variety of marine organisms. Ecological Importance of Coral Reefs
  • 51.
  • 52.
    Benefits for Humans Provideshumans with seafood, pharmaceuticals, and recreational/tourism dollars
  • 53.
    Coral Reef Risks Of the 109 countries with large reefs, 90 are damaging them, and 27% of the coral reefs are at high risk, especially off the coast of Southeastern Asia.  In the western Atlantic, 30-50% of all coral species are either rare or endangered.
  • 54.
    Coral Reef RisksCon’t  Silt washing from downstream has smothered the reefs  High salinity from fresh water diversion, over-fishing, boat groundings, fishing with dynamite or cyanide, hurricane damage, disease, coral bleaching, land reclamation, tourism, and the mining of coral for building materials.
  • 55.
    ©1997-2001 Jeffrey N.Jeffords This bottle still shows a slightly burned fuse from its use to blow up the coral.
  • 56.
    Protection of  300coral reefs in 65 countries are protected as reserves or parks, and another 600 have been recommended for protection.  The good news is coral reefs can often recover from damage.
  • 57.
  • 58.
  • 59.
    African Proverb  “Watermay flow in a thousand channels, but it all returns to the sea.”  The oceans are the ultimate sink for much of the waste matter we produce.
  • 60.
    Differences of Opinion Oceans dilute, disperse, and degrade large amounts of raw sewage, sewage sludge, oil, and some types of industrial waste, especially in deep-water areas.  Marine life has proved to be more resilient than some scientists expected, some suggest it is safer to dump sludge & other hazardous wastes into the deep ocean than to bury them on land or burn them.
  • 61.
    Differences of Opinion Otherscientists disagree, pointing out that we know less about the deep ocean than we do about space. They say that dumping waste in the ocean would delay urgently needed pollution prevention and promote further degradation of this vital part of the earth’s life- support system.
  • 62.
    Oil Spills  Whena tanker accident happens, it gets lots of publicity.  But, more oil is released by normal operation of offshore wells, washing tankers & from pipeline or storage tank leaks.  One estimate says that oil companies spill, leak, or waste per year an amount of oil equal to that shipped by 1000 huge Exxon Valdez tankers.
  • 63.
    Floating Oil  Oilcoats the feathers of birds (especially diving birds) and the fur of marine animals, destroying the animals’ natural insulation and buoyancy  Many drown or die of exposure from loss of body heat.
  • 64.
    Other Information  Oilis broken down by bacteria over time; slower in cold waters.  Heavy oil components can smother bottom- dwelling organisms such as crabs, oysters, mussels, and clams, or make them unfit to eat.  Oil spills have killed coral reefs. A recent study showed that diesel oil becomes more toxic to marine life with the passage of time.
  • 65.
  • 66.
    Mechanical Methods  Floatingbooms contain the oil spill or keep it from reaching sensitive areas  Skimmer boats are used to vacuum up some of the oil into collection barges  Absorbent pads or large feather-filled pillows are used to soak up oil on beaches or in waters that are too shallow for skimmer boats
  • 67.
    Chemical Methods  Coagulatingagents cause floating oil to clump together for easier pickup or sink to the bottom, where it usually does less harm.  Dispersing agents break up oil slicks. However, these can also damage some types of organisms.  Fire can also burn off floating oil, but crude oil is hard to ignite.