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Anthropogenic impacts on the
biogeochemistry of the aquatic environment
Mississippi - Atchafalaya River Basin and the Gulf of Mexico
Amir Hossain, Beatrice Brix da Costa, Gesche Reich, Kena Weise, Sarah Ahmed, Teresa Nobre
International Studies in Aquatic Tropical Ecology (ISATEC)
Anthropogenic impact on ecosystems
Mississippi river Delta
A swamp in the Atchafalaya Basin
Historical Background
• Link between agricultural alterations and
stream nutrient concentrations
• Reasons in the past: transformation of forest
into crop fields
→ erosion + sediment input into river stream
• Reasons today: input of fertilizer
→ land use directly linked to water quality
Nitrogen in the Mississippi - Atchafalaya River Basin
(Goolsby et al. 2000)
Biogeochemical consequences
High N input leads to:
• Increased productivity
→ algal blooms
→ change in phytoplankton community
→ microbial degradation of the biomass
→ oxygen depletion and bottom water hypoxia
Oxygen depletion and bottom water hypoxia
→ decreased nutrient cycling and bioturbation
→ shift in biogeochemical composition of sediments and overlaying waters
→ sulfate respiration dominant
Biogeochemical consequences
Strong seasonal stratification
Less fresh water discharge =
● Lower surface salinity
● Less low oxygen conditions
● Reduced suspended sediment loads
● Reduced nutrient flux
● Increased water clarity across the continental shelf
Hypoxia in the Gulf of Mexico
Higher temperatures will increase biological processes
Higher precipitation will lead to:
• increased runoff & erosion
• increased freshwater discharge
→ strengthen stratification and worsen hypoxia
Tropical storms etc. may create temporary mixing in water column
→ destratification and re-aeration
The Impact of Climate Change
• Develop and implement long-term, broad-scale, and persistent efforts to reduce substantial
nutrient loads
• Nominate water and resource managers to take actions and monitor
• Working together towards a mutually satisfying equilibrium of interest, including scientists, land
managers, agriculturists, as well as citizens
Solutions
Thank you for your attention!
Historical Background - Global
Literature
Goolsby, D.A., W.A. Battaglin, B.T. Aulenbach, R.P. Hooper. 2000. Nitrogen flux and sources in the Mississippi River Basin. Sci. Total Environ. 248:
75–86.
Goolsby, D.A., W.A. Battaglin, B.T. Aulenbach, R.P. Hooper. 2001. Nitrogen Input to the Gulf of Mexico. J. Environ. Qual. 30: 329–336.
Rabalais, N.N., R.E. Turner, W.J. Wiseman. 2001. Hypoxia in the Gulf of Mexico. J. Environ. Qual. 30: 320–329.
Steinberg, D.K., D.G. Martinson, D.P. Costa. 2012. Eutrophication-Driven Deoxygenation in the Coastal Ocean. 25: 56–67.
TURNER, R.E., N.N. RABALAIS. 2003. Linking Landscape and Water Quality in the Mississippi River Basin for 200 Years. Bioscience 53: 563.

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Mississippi and Atchafalaya river basin and the gulf of mexico

  • 1. Anthropogenic impacts on the biogeochemistry of the aquatic environment Mississippi - Atchafalaya River Basin and the Gulf of Mexico Amir Hossain, Beatrice Brix da Costa, Gesche Reich, Kena Weise, Sarah Ahmed, Teresa Nobre International Studies in Aquatic Tropical Ecology (ISATEC)
  • 3. Mississippi river Delta A swamp in the Atchafalaya Basin
  • 4. Historical Background • Link between agricultural alterations and stream nutrient concentrations • Reasons in the past: transformation of forest into crop fields → erosion + sediment input into river stream • Reasons today: input of fertilizer → land use directly linked to water quality
  • 5. Nitrogen in the Mississippi - Atchafalaya River Basin (Goolsby et al. 2000)
  • 6. Biogeochemical consequences High N input leads to: • Increased productivity → algal blooms → change in phytoplankton community → microbial degradation of the biomass → oxygen depletion and bottom water hypoxia
  • 7. Oxygen depletion and bottom water hypoxia → decreased nutrient cycling and bioturbation → shift in biogeochemical composition of sediments and overlaying waters → sulfate respiration dominant Biogeochemical consequences
  • 8. Strong seasonal stratification Less fresh water discharge = ● Lower surface salinity ● Less low oxygen conditions ● Reduced suspended sediment loads ● Reduced nutrient flux ● Increased water clarity across the continental shelf Hypoxia in the Gulf of Mexico
  • 9. Higher temperatures will increase biological processes Higher precipitation will lead to: • increased runoff & erosion • increased freshwater discharge → strengthen stratification and worsen hypoxia Tropical storms etc. may create temporary mixing in water column → destratification and re-aeration The Impact of Climate Change
  • 10. • Develop and implement long-term, broad-scale, and persistent efforts to reduce substantial nutrient loads • Nominate water and resource managers to take actions and monitor • Working together towards a mutually satisfying equilibrium of interest, including scientists, land managers, agriculturists, as well as citizens Solutions
  • 11. Thank you for your attention!
  • 13. Literature Goolsby, D.A., W.A. Battaglin, B.T. Aulenbach, R.P. Hooper. 2000. Nitrogen flux and sources in the Mississippi River Basin. Sci. Total Environ. 248: 75–86. Goolsby, D.A., W.A. Battaglin, B.T. Aulenbach, R.P. Hooper. 2001. Nitrogen Input to the Gulf of Mexico. J. Environ. Qual. 30: 329–336. Rabalais, N.N., R.E. Turner, W.J. Wiseman. 2001. Hypoxia in the Gulf of Mexico. J. Environ. Qual. 30: 320–329. Steinberg, D.K., D.G. Martinson, D.P. Costa. 2012. Eutrophication-Driven Deoxygenation in the Coastal Ocean. 25: 56–67. TURNER, R.E., N.N. RABALAIS. 2003. Linking Landscape and Water Quality in the Mississippi River Basin for 200 Years. Bioscience 53: 563.

Editor's Notes

  1. As we learned during the last day anthropogenic activity has a major impact on material/element/nutrient fluxes and alters our ecosystem. This graphic gives you a great overview over the processes and the interconnection Not only our actual activities but also climate change will have a major impact on our aquatic system. Nutrient input will not only alter sediment chemistry but also lead to bloom and affect oxidation of the water column Environmental changes like sea level rise temperature and winds also will alter biological and physical processes, depending on area in the world. And will increase the latter named changes. In the following we want to present you our case study about the gulf of mexico/mississippi river area and show you what influence densely populated coast and human activities can have on the ecosystem and which outlook we have to expect and how we can change it
  2. A river-dominated delta system where the Mississippi River meets the Gulf of Mexico, in the southeastern United States. The 7th largest river delta in the world 70 million people live within the Mississippi basin One of the most productive farming regions in the world produces the majority of the corn, soy-bean and wheat in the US
  3. This slide just gives you a more detailed overview of how nutrient input in the Mississippi river was formerly influenced by human activity and how it developed until today. Soil erosion, due to extensive agricultural land use, lead to huge amounts of nitrogen release already back between 1830 and 1850 and in the beginning of the 20th century. Though the effects were rather minor in comparison what is happening today: you see that the use of nitrate fertilizer has a much larger impact on the water quality and changes in ecosystems (here reffered to diatom abundance at the coast) and that’s what we want to look at in more detail in the following slides
  4. - Slide shows the long-term patterns in nitrate concentrations in the lower Mississippi River at St Francisville - Concentrations of nitrate in Mississippi River and tributaries have increased by a factor of 2-5 since 1990 - correlation between streamflow and nitrogen concentrations (graph not in slide) → indicates that it comes from non-point sources (otherwise conc would decrease with increasing streamflow due to dilution) -The large year-to-year variation in flux is caused by variations in streamflow. → high N concentrations when streamflow high. -The Higher streamflow could influence nitrate N flux in two ways. -First, the volume of flow would be larger and more nitrate N transported. -Second, the higher precipitation would leach more accumulated nitrate N from soils in the basin.The combination of higher concentrations and higher streamflow in the 1980–1996 period would produce significant increases in nitrate N flux. - Principal sources of N: nitrate due to agricultural fertilizer used for crop production like corn, soybean, or sorghum and drainage system - study also showed that ¾ of nitrogen flux from Mississippi -Atchafalaya River Basin enters the Gulf via the Mississippi River channel -
  5. Higher nutrient availability leads to an exponential increase in phytoplankton population. Their decay and microbial decomposition lead to high oxygen consumption which depletes the seawater of dissolved oxygen and creates hypoxic zones. Changes in phytoplankton community can occur if a ratio of Si to N decreases which would favor non-siliceous forms of phytoplankton, such as dinoflagellates or cyanobacteria rather than diatoms.
  6. oxygen depletion and bottom water hypoxia Size of these areas closely related to N load (the same-sized hypoxic area is now formed with a lower nitrate load than historically ) New chemical composition depends length and severity of hypoxia *sulfate respiration normally dominant in the sediment now on sediment-water line Higher PH in bottom water lower PH on top
  7. Hypoxic waters here are distributed from shallow depths near shore to as deep as 60 m - but more typically between 5 and 30 m. There is higher stratification in the summer because there is less river outflow and less wind Winds lead to vertical mixing and creates upwelling of deeper oxygenated waters. Figure: distribution of hypoxic zones by frequency of occurrence
  8. Higher temperatures will increase biological processes (like photosynthesis and respiration) Primary production then maybe light limited or lack of nutrients Higher precipitation will lead to increased runoff, and ersion à higher P loss and increased flux of DIN (especially no3-) + increased freshwater discharge à higher nutrient discharge via mississipii in guld à strengthen stratification and worsen hypoxia Role of tropical storm and hurricanes may will help to create temporary mixing in water column and therefore destratify and re-aerate
  9. Cheap crude oil ~1950 → increased commercial production of fertilizers via haber bosch, which started at beginning of century Lead to an significant exponential increase in nutrient emission creation of reactive nitrogen, which has increased by over 20 times since the Industrial Revolution to a global production of 187 Tg N yr–1 in 2005, drives the changes in nitrogen loading in the last 100 years (Galloway