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The Dead Zone:. Hypoxia in the Gulf of Mexico. What is the dead zone?. Condition that occurs in coastal waters where:. • Little or no oxygen is present • Little or no marine life can survive. The term for low oxygen is hypoxia . Hypoxia=<2 mg/l dissolved oxygen (DO).
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The Dead Zone: Hypoxia in the Gulf of Mexico
Condition that occurs in coastal waters where: • • Little or no oxygen is present • • Little or no marine life can survive
The term for low oxygen is hypoxia.Hypoxia=<2 mg/l dissolved oxygen (DO)
The term for no oxygen is anoxia. Anoxia =0 mg/l dissolved oxygen
Ireland • Scotland • Sweden • Norway • Finland • Spain • Germany • Japan • Hong Kong • Australia • New Zealand • United States • Canada • France • Italy • Greece • Turkey • Russia • Sea of Azov • Adriatic Sea • Aegean Sea • Mediterranean Sea
In the U.S., hypoxia occurs in coastal waters in New York, Maryland, North Carolina, Florida, Alabama, Texas and Louisiana.
In Louisiana, the dead zone occurs west of the Mississippi and Atchafalaya rivers
In Louisiana, hypoxia occurs from late spring until late summer.
The dead zone can affect: •Benthos •Fisheries •People
Benthos • Stressed or die • Decreased diversity • Degraded environment
Fisheries • Food base is reduced and/or lost • Habitat is reduced and/or lost • Recruitment is disrupted • Migratory patterns are disrupted • Species diversity is reduced • Mortality increases
People • Commercial fisheries • Recreational fisheries • Tourism • Economy
The dead zone decreases the ability of the Gulf to produce seafood. This affects the local economy.
Louisiana has one of the largest coastal dead zones in the world.
Since 1985, the dead zone has ranged in size from about 100 square miles in 1988 to over 8,500 square miles in 2002.
The size of the dead zone depends upon the conditions that cause it.
A combination of physical, chemical and biological factors create conditions for hypoxia in Louisiana.
Warm Temperatures Warm spring and summer temperatures heat the water surface.
O2 Calm seas decrease oxygen exchange at the surface.
Nutrients Warm fresh water and nutrients are delivered by the Mississippi River and float on the denser saltwater.
A stratified layer is formed with lighter, fresher, warmer water at the surface and heavier, saltier, cooler water near the bottom limiting oxygen mixing throughout the water column. Lighter Fresher Warmer Water Stratified Layer No O2 mixing Heavier Saltier Cooler Water
The Mississippi River drains 41% of the lower 48 United States. It carries water and sediment hundreds of miles to the Gulf of Mexico.
Excess nutrients from runoff are carried to the Gulf of Mexico.
Nutrients include compounds which contain: • Phosphorus • Nitrogen • Silica
Nutrients that are carried by the river come from a variety of sources.
Municipal & industrial runoff Atmosphere Fertilizers Cattle, pig and poultry farm runoff Wastewater treatment
Microscopic algae or phytoplankton use these nutrients to reproduce.
Excess nutrients enable plankton populations to explode, causing a plankton or algal bloom.
At the surface, plankton blooms occur when excess nutrients are present Plankton bloom
When plankton die, they sink to the bottom and decompose. During decomposition bacteria use up most or all of the available oxygen. Dead Plankton No O2 Decomposers
During decomposition, bacteria use up most or all of the oxygen causing the water column to become hypoxic or anoxic.
Mobile animals become stressed and leave Stationary animals become stressed and/or die
When little or no oxygen is present: • Mobileanimals leave. • Stationary animals become stressed or die.
Warm Temperatures Fresh River Water Nutrients O2 Plankton Bloom Lighter, Fresher, Warmer, Water Dead Plankton Stratified Layer No O2 Mixing Heavier, Saltier, Cooler, Water No O2 Decomposers
Human activities contribute to the causes of hypoxia
• Land use practices •Fertilizer use •Poor management practices
Changes in land use from Agriculture Industry Flood control Urban expansion Lead to: Loss of natural habitat
Change flood control practices • Use fertilizers more efficiently • Control discharges of nitrogen • Create and restore wetlands • Reduce nutrient loading • Manage the whole system