Chapter 11 - COSEE Florida
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Transcript Chapter 11 - COSEE Florida
CHAPTER 11
The Coastal Ocean
Overview
Coastal waters support
about 95% of total biomass
in ocean
Most commercial fish
caught within 320 km (200
m) from shore
Important also for shipping,
oil and gas production, and
recreation
Many pollutants found here
– that’s a problem!
http://www.safmc.net/Portals/0/shrimp%20trawler2.jpg
Ocean ownership
1609 sea is free to all (mare liberum = free)
Assumed fish resources are inexhaustible
1702 territorial sea under coastal nation’s
sovereignty (3 nautical miles from shore)
Distance of cannon shot
United Nations and ocean
laws
1958-1982 United Nations Law of the Sea
Conferences
National sovereignty extends 12 nautical miles
Exclusive Economic Zone (EEZ) 200 nautical miles
(370 km) from land (mineral and fishing resources)
Right of free passage for ships
Open ocean mining regulated by International
Seabed Authority
○ This has changed, still very contentious
United Nations arbitrates disputes
EEZ of the U.S.--about 30% more
than land area of entire U.S.
Fig. 11.1
Characteristics of coastal
waters
Adjacent to land (to edge of continental
shelf)
Influenced by river runoff, wind, tides
Salinity variable
Freshwater runoff
Winds
Mixing by tides
Characteristics of coastal
waters
Temperature variable
Low-latitudes: restricted circulation, very
warm
High-latitudes: sea ice
Mid-latitudes
○ Seasonal changes
○ Prevailing winds
Types of coastal waters
Estuary
Partially enclosed coastal area with ocean
water and freshwater (runoff) mixing; mouths
of rivers, bays, etc.
Lagoon
Shallow coastal water separated from ocean by
barrier island
Marginal sea
Relatively large semi-isolated body of water
Estuaries - Origin of estuaries
Rising sea level “drowns” what
was once land
Coastal plain estuary
Former river valley now flooded with
seawater
Fjord
Former glaciated valley now flooded
with seawater
Bar-built estuary
Lagoon separated from ocean by sand
bar or barrier island
Tectonic estuary
Faulted or folded down-dropped area
now flooded with ocean
Estuaries - Classification of estuaries
4 types - Based on mixing of freshwater and saltwater
Vertically mixed
Slightly stratified
Highly stratified
Salt wedge
Shallow, low volume
Salinity uniform
Deeper than previous
Upper layer less salty; lower layer more salty
Estuarine circulation
Deep, relatively strong halocline
Deep, high volume
Strong halocline
Typical at mouths of deep, high volume rivers
Figure 11.8
Severely effected by human activity, freshwater wedge can be traceable far out to sea
Chesapeake Bay Estuary
Anoxic conditions below pycnocline in summer
Runoff of sewage and fertilizer cause algae bloom
when these organisms die, increased decomposition causes anoxic
conditions
Decrease in oxygen levels in water
Major kills of commercially important marine animals
Lagoons
Water isolated by barrier islands
3 main zones:
○ Freshwater zone
○ Transition zone of brackish water
○ Saltwater zone
Hypersaline in arid regions
Indian River Lagoon
Well-mixed due to winds
and shallow depths
Seasonal changes in
salinity, temperature,
dissolved oxygen
Most biologically diverse
estuary in north
america…over 4,000
species of plants and
animals
Threats: habitat
destruction, stormwater
runoff, and invasive exotic
species
Sebastian Inlet
http://www.indianriverlagoon.org/docs/irlmap.html
Marginal seas
Mostly from tectonic events
Ocean crust between continents,
e.g., Mediterranean Sea
Behind volcanic island arcs, e.g.,
Caribbean Sea
Shallower than ocean
Connected to ocean
http://www.shinesforall.com/images/Caribbeanmap.gif
Caribbean Sea
On Caribbean plate defined by Greater and
Lesser Antilles – volcanic island arc
Relatively shallow marginal sea – deepest is
Cancun Trough at 7,686 m (25,220 ft)
Underlain by oceanic crust
http://woodshole.er.usgs.gov/project-pages/caribbean/images/PBATHY1.GIF
Mediterranean Sea
Remnant of Tethys Sea – when all the continents
were together
Deeper than usual marginal sea
Underlain by oceanic crust
Thick salt deposits – almost dried up about 6 million
years ago
Fig. 11.14a
Mediterranean circulation
Fig. 11.14b
High rates of evaporation
Mediterranean Intermediate Water very salty
Coastal Wetlands - Types of coastal wetlands
o
o
o
Ecosystems that are saturated with
water
o Swamps, tidal flats, coastal
marshes, bayous
Salt marsh
o Any latitude
Mangroves
o Low latitude
Characteristics of coastal
wetlands
Efficiently cleanse polluted water
Absorb water from coastal flooding during
storms
Protect shores from wave erosion
http://soundwaves.usgs.gov/2008/03/WetlandLG.jpg
Coastal Wetlands - Loss of coastal
wetlands
Half of U.S. coastal
wetlands lost to
development (housing,
industry, agriculture)
U.S. Office of Wetland
Protection, 1986
Minimize loss of
wetlands
Protect or restore
wetlands
http://www.on.ec.gc.ca/wildlife/factsheets/images/glfs-coast-stress.jpg
Marine pollution
Any harmful substance or energy put into the
oceans by humans
Harmful to living organisms
○ Standard laboratory bioassay – concentration of pollutant
that causes 50% mortality among test organisms
Hindrance to marine activities (e.g., fishing)
Reduction in quality of sea water
Waste disposal in ocean
Diluting pollutants with huge volume of
ocean water
Long-term effects not known
Debate about dumping wastes in ocean
None at all ??
Some, as long as properly disposed and
monitored ??
Main types of marine pollution
Petroleum
Nutrient excess
○ Sewage sludge
○ Fertilizer runoff
DDTs and PCBs
Mercury
Non-point-source pollution and trash
○ Drainage from roads, canals, etc.
Petroleum
Biodegradable
hydrocarbons
Recovery faster than
expected
○ Exxon Valdez oil spill,
1989
But many organisms
killed outright
Long-term
consequences
uncertain
○ Research is still
being done in this
area, some animal
populations have not
completely recovered
Fig. 11.16
BP Deepwater Horizon Oil Spill in Gulf
of Mexico
April 20, 2010
4.9 MILLION barrels of oil were leaked
What are future effects?
Cleaning oil spills
Natural processes
Volatilization
Photo oxidation
Emulsification
Biodegration by
pelagic organisms
Biodegration by
benthic organisms
Artificial processes
Oil dispersants
Isolate spill with
booms
Skimming or
absorbing surface oil
slick
Bioremediation by
“hydrocarboneating” bacteria
Preventing oil spills
Double
hulled oil tankers by 2015
1990 Oil Pollution Act
Burn
oil before it spreads
1999 M/V New Carissa
http://www.ec.gc.ca/EnviroZine/images/aerial.jpg
http://www.modelshipmaster.com/products/ocean_liners/tube.jpg
Sewage sludge
Semisolid
material after treatment
No dumping of sludge in ocean after
1981
Clean Water Act, 1972
HOWEVER - many exceptions/waivers
New York’s sewage sludge disposal
First, shallow water
sites
Then (1986), deeper
water site
Adverse effects on fish
1993 all sewage
disposed on land
Fig. 11.25
DDT and PCBs
Pesticide DDT and industrial chemicals PCBs
(polychlorinated biphenyls)
○ DDT – pesticide that was widely used
○ PCBs – used in transformers and other areas of
industry
Widespread in oceans
Persistent organic pollutants
Toxic
Long life dissolved in seawater
Accumulated in food chain
Bioaccumulation – it’s happening in us, also!
Bioaccumulation and biomagnification
Bioaccumulation – organisms
concentrate pollutant from seawater
Biomagnification – organisms gain more
pollutant by eating other organisms
DDT
Decline in bird
populations and thin
eggshells
Long Island osprey
California brown pelican
DDT banned in U.S. in
1972
Some marine bird
populations rebounded
Mercury and Minamata disease
Methyl mercury toxic to most living organisms
Chemical plants, Minamata Bay, Japan,
released mercury in 1938
By 1950 first reported ecological changes
By 1953 humans poisoned
Neurological disorder – numbness, muscle
weakness, paralysis, coma, congenital defects
Bioaccumulation and biomagnification
Safe levels of
mercury determined
by
Rate of fish
consumption by people
Mercury concentration
in fish consumed
Minimum ingestion
rate of mercury to
cause damages
Non-point-source pollution and
trash
Not from underwater pipelines
Hard to regulate
For example, from storm drains
Pesticides and fertilizers
Road oil
Trash
Trash from dumping
Some trash can be legally
dumped far from shore
Biodegradable (e.g., food) or
Sinkable (e.g., glass, metal)
Some trash cannot be
dumped
Plastic
○ Lightweight (floats)
○ Not easily biodegradable
○ Plastic can incorporate
pollutants, such as DDT and
PCBs
http://www.sciencepunk.com/v5/gallery/greenpeace_table.JPG
It is up to us!
Don’t throw trash out your car
window
Don’t leave trash on the beach
Don’t throw trash off the side of
your boat
Don’t use fertilizers irresponsibly
Don’t just dump things down the drain
without reading about proper disposal
Get onto people you know that do
this!
○ Think of your kids and grandkids!
Problems with Contaminants in
Oceans
Research into immunosuppression and
reproductive problems in many species
Chemicals that are banned in US and
other countries are still used in
others – it is 1 ocean, doesn’t matter
where it is dumped
○ It will effect us all!
All drains lead to the ocean!
Fig. 11.32a,b
Misconceptions –What have we learned that
make the following statements false?
Science and technology can solve all of our problems.
The Earth can absorb and neutralize any amount of waste
and pollution over time.
Dilution is the solution to the problem.
Microorganisms are not important to human survival.
Local people cannot improve their environments; it is out
of their hands.
If we run out of oil and gas we will just find more.
Earth is both an endless supply of resources and a
limitless sink for the waste products of our society.
Ocean Literacy Principles
1.d - Sea level is the average height of the ocean relative to the
land, taking into account the differences caused by tides. Sea
level changes as plate tectonics cause the volume of ocean
basins and the height of the land to change. It changes as ice
caps on land melt or grow. It also changes as sea water expands
and contracts when ocean water warms and cools.
1.h - Although the ocean is large, it is finite and resources are
limited.
5.f - Ocean habitats are defined by environmental factors. Due
to interactions of abiotic factors such as salinity, temperature,
oxygen, pH, light, nutrients, pressure, substrate and circulation,
ocean life is not evenly distributed temporally or spatially, i.e.,
it is “patchy”. Some regions of the ocean support more diverse
and abundant life than anywhere on Earth, while much of the
ocean is considered a desert.
5.i - Estuaries provide important and productive nursery areas
for many marine and aquatic species.
Sunshine State Standards
SC.6.E.6.1 - Describe and give examples of ways in which Earth's surface is built up and torn down
by physical and chemical weathering, erosion, and deposition.
SC.6.E.6.2 - Recognize that there are a variety of different landforms on Earth's surface such as
coastlines, dunes, rivers, mountains, glaciers, deltas, and lakes and relate these landforms as they
apply to Florida.
SC.912.E.6.6 - Analyze past, present, and potential future consequences to the environment
resulting from various energy production technologies.
SC.912.L.17.2 - Explain the general distribution of life in aquatic systems as a function of
chemistry, geography, light, depth, salinity, and temperature.
SC.912.L.17.3 - Discuss how various oceanic and freshwater processes, such as currents, tides, and
waves, affect the abundance of aquatic organisms.
SC.912.L.17.8 - Recognize the consequences of the losses of biodiversity due to catastrophic
events, climate changes, human activity, and the introduction of invasive, nonnative species.
SC.912.L.17.11 - Evaluate the costs and benefits of renewable and nonrenewable resources, such as
water, energy, fossil fuels, wildlife, and forests.
SC.912.L.17.13 - Discuss the need for adequate monitoring of environmental parameters when
making policy decisions.
SC.912.L.17.16 - Discuss the large-scale environmental impacts resulting from human activity,
including waste spills, oil spills, runoff, greenhouse gases, ozone depletion, and surface and
groundwater pollution.
SC.912.L.17.20 - Predict the impact of individuals on environmental systems and examine how
human lifestyles affect sustainability.