Scientists offer recommendations to decrease hypoxia in the Gulf of Mexico. The Council for Agricultural Science and Technology (CAST), an international consortium of 38 scientific and professional societies, released a report Gulf of Mexico Hypoxia: Land and Sea Interactions in which a CAST task force of 6 scientists provides recommendations to help better understand all aspects of hypoxia in the Gulf of Mexico and other areas of the world, and to decrease the Gulf hypoxic zone. The task force chaired by Dr. John A. Downing, Department of Animal Ecology, Iowa State University, Ames, includes individuals with expertise in agricultural economics, agricultural engineering, agronomy, animal ecology, biogeochemistry, biological sciences, environmental research, limnology, marine science, oceanography, and soil science.
The Gulf of Mexico hypoxic zone, a bottom area with dissolved oxygen levels too low to sustain animal life, is the largest zone of human caused coastal hypoxia in the Western Hemisphere. Mid-summer coastal hypoxia in the northern Gulf was first recorded in the early 1970s. Persistent coastal hypoxia has been most widespread during the 1990s. Mid-summer surveys show the hypoxic zone has covered as much as 18,000 square kilometers (km2) (1993-1996), covering 12,400 km2 (4,800 square miles) in 1998: about the size of Connecticut.
Gulf hypoxia results from:
Nitrogen (N) is the principal nutrient yielding excess organic matter sedimentation to the Gulf hypoxic zone. Nitrogen export from the Mississippi River Basin has increased 2- to 7-fold over the last century. Silicon (Si) and phosphorus (P) also play a role, and the changing balance of N, Si, and P can affect marine food chains.
Advanced anthropogenic hypoxia elsewhere in the world has had serious impacts on fisheries. Short-term economic costs impact.
Commercial and recreational fisheries in the Gulf generate $2.8 billion annually. Signs consistent with impact on Gulf of Mexico fisheries are:
The majority of Mississippi River N originates from agricultural practice, while smaller fractions arise from human sewage, nonagricultural fertilizer use, and precipitation. Agriculture’s share of this lost nitrogen has a fertilizer value of about $410 million.
The Mississippi River Basin:
Nitrogen moves from agricultural land to surface waters by air, surface runoff, sediment transport, and subsurface drainage. Inexpensive management options can reduce N losses from agricultural lands, e.g., alterations of fertilizer application methods to decrease runoff losses, alterations of tillage regimes to decrease sediment bound nutrient transport, and fine-tuning application rates to decrease losses through subsurface drainage.
Decreasing agriculture’s contribution to Gulf of Mexico nutrients will require changes in crop and livestock management practices to reduce nutrient losses. Several benefits would accrue to agriculture and society:
Gulf of Mexico Hypoxia: Land and Sea Interactions, 44 pages, is available for $20.00 from CAST.
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