1 / 83

Aquatic Biodiversity

Aquatic Biodiversity. Chapter 8. Core Case Study: Why Should We Care about Coral Reefs?. Biodiversity Important ecological and economic services Natural barriers protecting coasts from erosion Provide habitats Support fishing and tourism businesses Provide jobs Studied and enjoyed.

mare
Download Presentation

Aquatic Biodiversity

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Aquatic Biodiversity Chapter 8

  2. Core Case Study: Why Should We Care about Coral Reefs? • Biodiversity • Important ecological and economic services • Natural barriers protecting coasts from erosion • Provide habitats • Support fishing and tourism businesses • Provide jobs • Studied and enjoyed

  3. Human Activities Are Disrupting and Degrading Marine Systems • Major threats to marine systems • Coastal development • Overfishing • Runoff of nonpoint source pollution • Point source pollution

  4. Human Activities Are Disrupting and Degrading Marine Systems • Major threats to marine systems • Habitat destruction • Introduction of invasive species • Climate change from human activities • Pollution of coastal wetlands and estuaries

  5. Earth: The Watery Planet • 71% Earth covered by ocean • 2.2% covered by freshwater

  6. What are Earth’s Major Oceans? • Pacific • Largest, deepest • Atlantic • Second largest • Indian • Mainly in Southern Hemisphere • Arctic • Smallest, shallowest, ice-covered

  7. Average Ocean Depth

  8. Pelagic Intertidal Abyssal Benthic

  9. Most Aquatic Species Live in Top, Middle, or Bottom Layers of Water • Plankton • Phytoplankton • Zooplankton • Ultraplankton • Nekton • Benthos • Decomposers

  10. Measuring Primary Production • Satellites measure differences in sea surface color • Color = type of producer • Green color = chlorophyll pigments

  11. Eutrophication • Light Availability – depth, season, latitude • Little photosynthesis below 100m (330ft) • Phytoplankton productivity limited to photic zone

  12. Eutrophication • Nutrient Availability – “Natural fertilizer” • Upwelling - aids primary production by bringing nutrients to surface • Nitrogen and Phosphorous • Caused by winds blowing either parallel or offshore along a coastline • Brings up cold nutrient-rich water

  13. Eutrophication • Nutrient Availability – “Natural fertilizer” • Zooplankton (fecal pellets, death) – leads to future phytoplankton blooms • Need bacteria to decompose waste

  14. Phytoplankton: Season & Latitude

  15. Red Tide Impacts • Toxic to marine life: accumulates in clams, mussels, scallops, fish, mammals • Death to some species; biomagnification • Human poisoning after consumption (30 min.) • Symptoms: • Paralytic: paralysis, asthma, heartattack (rare) • Neurotoxic: tingling, paralysis, memory loss • Diarrhetic: cramps, vomiting, diarrhea

  16. Red Tide Impacts

  17. What is turbidity? • Measure of the degree to which the water looses its transparency • Due to the presence of suspended particulates

  18. What causes turbidity? • There are various parameters influencing the cloudiness of the water. Some of these are:  • Phytoplankton   • Sediments from erosion   • Resuspended sediments from the bottom (frequently stir up by bottom feeders like carp)  • Waste discharge  • Algae growth  • Urban runoff 

  19. What are the consequences of high turbidity? • Suspended particles absorb heat from the sunlight • Turbid waters become warmer • Reduce the concentration of oxygen in the water

  20. What is Dissolved Oxygen? • Amount of gaseous oxygen (O2) dissolved in an aqueous solution. • Oxygen gets into water by: • Diffusion from the surrounding air • Aeration (rapid movement) • Waste product of photosynthesis

  21. Environmental Impact • Should not exceed 110 % • Concentrations above this level can be harmful to aquatic life.

  22. Gas Bubble Disease • Fish in waters containing excessive dissolved gases • Bubbles block the flow of blood through blood vessels causing death • External bubbles (emphysema) • fins, skin and eyes

  23. Environmental Impact • As dissolved oxygen levels in water drop below 5.0 mg/l, aquatic life is put under stress. • The lower the concentration, the greater the stress. • Oxygen levels that remain below 1-2 mg/l for a few hours can result in large fish kills.

  24. Cultural Eutrophication Is Too Much of a Good Thing • Cultural eutrophication – increase in nitrates and phosphate containing effluents from various sources in urban and agricultural communities

  25. Eutrophication • Nutrients are food for algae, and water with high amounts of nutrients can produce algae in large quantities. • When these algae die, bacteria decompose them, and use up oxygen. • DO concentrations can drop too low for fish to breathe, leading to fish kills.

  26. Organic Wastes • Remains of any living or once-living organism • Leaves, grass clippings, dead plants or animals, animal droppings, and sewage • Decomposed by bacteria; these bacteria remove dissolved oxygen from the water when they breathe.

  27. Some Lakes Have More Nutrients Than Others • Oligotrophic lakes • Low levels of nutrients and low NPP • Eutrophic lakes • High levels of nutrients and high NPP • Mesotrophic lakes • Cultural eutrophication leads to hypereutrophic lakes

  28. The Effect of Nutrient Enrichment on a Lake

  29. Water Stands in Some Freshwater Systems and Flows in Others • Standing (lentic) bodies of freshwater • Lakes • Ponds • Inland wetlands • Flowing (lotic) systems of freshwater • Streams • Rivers

  30. Water Stands in Some Freshwater Systems and Flows in Others • Formation of lakes • Four zones based on depth and distance from shore • Littoral zone – top layer near the shore • Limnetic zone – open sunlit layer away from the shore; extends to depth penetrated by light • Profundal zone – deep open water; too dark for photosynthesis • Benthic zone – bottom of lake; mostly decomposers, detritus feeders and some fish

  31. Stratification by depth/distance from shore

  32. Stratification by temperature • Epilimnion • Hypolimnion

  33. Lake Rain and snow Glacier Rapids Waterfall Tributary Flood plain Oxbow lake Salt marsh Deposited sediment Delta Ocean Source Zone Transition Zone Water Sediment Floodplain Zone Stepped Art Fig. 8-17, p. 176

  34. Water Resources Chapter 13

  35. Earth’s water supply: 97.2% 2.15% 0.62% 0.02% 0.001% World ocean Frozen in glaciers and ice caps Groundwater and soil moisture Streams and lakes Water vapor in the atmosphere Hydrologic Cycle

  36. Hydrologic Cycle • Water moves between the ocean, atmosphere, and land.

  37. We Get Freshwater from Groundwater and Surface Water • Ground water: water that percolates downward through the Earth until it collects in an impenetrable layer of rock • Zone of saturation: depth where Earth is completely filled with water

  38. We Get Freshwater from Groundwater and Surface Water • Water table: top of groundwater zone • Aquifers: underground caverns and porous layers of sand, gravel, or bedrock through which groundwater flows • Natural recharge • Lateral recharge

  39. Natural Capital: Groundwater System: Unconfined and Confined Aquifer

  40. Water Tables Fall When Groundwater Is Withdrawn Faster Than It Is Replenished • India, China, and the United States • Three largest grain producers • Overpumping aquifers for irrigation of crops • Rate of pumping exceeds natural recharge • Deeper wells increase pollution • India and China • Small farmers drilling tubewells • Effect on water table

  41. Water Tables Fall When Groundwater Is Withdrawn Faster Than It Is Replenished • Saudi Arabia • As water-poor as it is oil-rich! • 70% of drinking water produced by removing salt from seawater • High evaporation rates • Large pools and fountains • Aquifer depletion and irrigation

  42. Natural Capital Degradation: Irrigation in Saudi Arabia Using an Aquifer

  43. Case Study: Aquifer Depletion in the United States • Ogallala aquifer: largest known aquifer • Runs from South Dakota to Texas • One-time deposit of liquid natural capital • Irrigates the Great Plains

  44. Dams and Reservoirs

  45. Is Building More Dams the Answer? • Dam: structure built across a river to control the river’s water flow • Reservoir: artificial lake formed when a river is dammed • 800,000 worldwide

  46. Advantages • Increase the reliable runoff available by 1/3 • Reduce flooding • Grow crops in arid regions • Hydroelectricity

  47. Disadvantages • Displaced 40-80 million people from their homes • Flooded agriculturally profitable regions the size of CA • Impaired ecological services of rivers • 1/5 loss of plant and animal species • High evaporation and seepage rates • Fill up with sediment within 50 years • 85% of US reservoirs by 2020

  48. Advantages and Disadvantages

  49. Case Study: The Colorado River Basin— An Overtapped Resource • Four Major problems • Colorado River basin has very dry lands • Modest flow of water for its size • Legal pacts allocated more water for human use than it can supply • Amount of water flowing to the mouth of the river has dropped

  50. Using Laws to Protect Drinking Water Quality • 1974: U.S. Safe Drinking Water Act • Sets maximum contaminant levels for any pollutants that affect human health • 5.6 million Americans drink water that does not meet EPA safety standards • Health scientists: call for strengthening the law • Banning all toxic lead in new plumbing • Current laws allow fixtures with up to 10% lead to be sold as “lead free”

More Related