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Deep Sea 016b

Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

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Page 1: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Deep Sea

016b

Page 2: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high
Page 3: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

100m

dysphotic

aphotic

photic

Page 4: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Deep Ocean Characteristics

• Cold• Still• Stable• Dark• Essentially no productivity• Sparse Life• Extremely high pressure• Little food

Page 5: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Deep sea orgs are dependant upon surface production from:

Dead phytoplankton, zooplankton, fish, mammals

Fecal pellets and crustacean molts

Macrophyte detritus

Animal migrations

Page 6: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Potential food source for deep sea organisms

Page 7: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Scavengers can feed on carcass in less than 6 months

Whale Fall; i.e., marine snow

Page 8: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Factors affecting organic material reaching the sea floor:

Storms

Seasonal variation

Page 9: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high
Page 10: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

100m

dysphotic

aphotic

photic

Page 11: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high
Page 12: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

• Ballard & Grassle (1977)- Alvin to Galapagos • Sulfur-rich vents 660 oF, but quickly cool to 73 oF• Thermophilic bacteria associated with vent

communities

Page 13: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Hydrothermal vents found at mid-ocean ridge spreading centers.

Page 14: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Active hydrothermal vents were first discovered at Loihi in the late 1980's

Page 15: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Loihi

• 15 mi S.E. of Kilauea

• 3,178 ft below sea level

• Will reach sea level in ~10,000 yrs

Page 16: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high
Page 17: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Loihi

Page 18: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

1. Cold seawater sinks into cracks deep into ocean floor

2. Water heated by magma rises and leaches out minerals from surrounding rocks

3. The water emerges from vents and precipitates out minerals

Page 19: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

magma

Bottom current

Seawater seepage

basalt

660oF

FeS, FeS2, CuFeS2

H2SFe, Mg

magma

Bottom current

Seawater seepage

basalt

660oF

FeS, FeS2, CuFeS2

H2SFe, Mg

Page 20: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high
Page 21: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high
Page 22: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Tube worms- pogonophoransOther orgs: • Calyptogena- large white clam• Large crabs• Sea anemones• Shrimp

Page 23: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Support communities with high biomass, but low diversity

Primary producers are chemosynthetic bacteria

90% endemism

Communities are small (25-60m in diameter)

Page 24: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Chemosynthesis:Oxygen + hydrogen sulfide + water + carbon dioxidesugar + sulfuric acid

602 + 6H2S + 6H20 + 6C02 C6H12O6 + 6H2S04

                                                        

      

Page 25: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Photosynthesis:6H2O + 6CO2 + nutrients + light energy C6H12O6 + 6O2

Chemosynthesis:

602 + 6H2S + 6H20 + 6C02 C6H12O6 + 6H2S04

Page 26: Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high

Inquiry

1. Where are hydrothermal vents located?

2. How do they form?3. Why doesn’t the vent water boil?4. Describe the chemosynthetic

bacteria's relationship with the vent and other animals living near the vent.