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24 Cards in this Set
- Front
- Back
Depth Zones in the Ocean
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Sublittoral, Bathyal, Abysmal, Hadal, Trenches |
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Deep Sea physical environment
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Deep sea is the largest habitat. Temperature, very cold. Warmer in Mediterranean and red sea + hydrothermal vents with higher temperatures. Pressure is extremely high. Light is dark Completely inhabitable to us. |
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Food availability
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Nutrient Poor. Dependent on outside energy sources. Falling debris, fecal pellets, carasses
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Osedax
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Bone eating worms. Close relative to hydrothermal vents |
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Predictability
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Little or no seasonal variation in temperature. Infrequent disturbances - bioturbation, benthic storms, whale falls |
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Deep Sea Expeditions
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Dredged 4km around Britain Challenger expedition - circumnavigated the earth and dredged upto 5.5 km depth 1960s development of modern equipment and submersibles |
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Deep Sea Biodiversity
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Difficult to sample. Most diverse is mid deep level not the lowest for benthic invertebrates. Patchy distribution of species - richness can vary substantially. Low latitudes are more rich in species
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Low Latitude Biodiversity
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Many species have evolutionized to lost swim bladder and eyes |
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Megafauna
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Large moving or seaside7.2km depth Lost swim bladders and negatively buoyant |
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Macrofauna
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Polychaetes, small crustaceans, mollusks |
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Meiofauna
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Nematodes, copepods, ostracods, flatworms |
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Deep sea diversity causes hypothesis
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1. Stability-time hypothesis 2. Biological Disturbances 3. Patchy food resources 4. Large Area 5. Source sink hypothesis |
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Stability Time Hypothesis
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Biological Disturbances |
Predation by megafauna reduces competition among macrofauna, coexistence, Macrofauna in turn crops meiofauna
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Patchy food resources
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Food falls are generally patchy and can support high species diversity |
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Large Area
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Large are should be able to support many species |
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Source sink hypothesis
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Abundance goes up as you go deeper down. The deeper areas are sustained by the up top areas
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Vent Fauna
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Benthopelagic Different vent sites differ in fauna compositions |
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Vent Fauna Feeding
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Basic energy source - chemautotrophic bacteria receive energy by oxidizing reduced suphur and other compounds. Microbial production on some vents 2-3 times Macrofauna have evolved symbiotic relationships with bacteria. |
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Cold Seeps
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Area were hydrocarbon, methane, hydrogen sulphide, and other fluids seep out of the ocean floor. Common in gulf of Mexico. A concern is that when the ocean is getting warmer, then these will melt and methane will be released into the ocean |
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Anthropogenic Impacts on the Deep Sea
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Disposal, Exploitation, Ocean Acidification/Climate Change |
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Disposal |
Sewage, Chemicals, CO2 |
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Exploitations
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Mining, Fossil Fuels |
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Climate
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Warming temp, acidification, hypoxia |