hydrothermal vent communities - masaryk university · hydrothermal vents 1. cold seawater sinks...
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Hydrothermal Vent Communities
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Hydrothermal Vents
1. Cold seawater sinks down through the crust.
2. O2 and K are removed from the seawater.
3. Ca, SO4, and Mg are removed from the fluid.
4. Na, Ca, and K from the crust enter the fluid.
5. Highest temperatures (350-400 oC), Cu, Zn, Fe, and H2S from the crust dissolve in the fluids.
6. Hot & acidic fluids with dissolved metals rise up through crust.
7. The hydrothermal fluids mix with cold, O2-rich seawater. Metals and sulfur combine to form metal-sulfide minerals: MnO2, FeO(OH), …
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www.pmel.noaa.gov/vents
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Black & White smokers
Metals & O2
Diffuse flow of water
Silica and Anhidrite
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Smoker chimney section
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Hydrothermal Vent Distribution
Pink, western Pacific; green, northeast Pacific; blue, East Pacific Rise; yellow, Azores; red, Mid-Atlantic Ridge; orange, Indian Ocean
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Hydrothermal vent age estimates
Age
• 20-100 years
• Decades
• <10 years
• < 6 months
Technique
• sulfide dating
• mollusk shells
• heat loss
• submersible observations
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Hydrothermal energy source
H2S + O2 SO4 ++ H+ + ATP
• Chemosynthetic (sulfur oxidizing)
• Thermophilic Bacteria (up to 120oC)
• Hot, anoxic, sulfide rich water mixes with Cold oxygenated water
• Hydrothermal Vents as origin of Life?
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Bacterial mat
www.divediscover.whoi.edu/i
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Bacteria from 120oC
http://mollie.berkeley.edu/~volkman/
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Vent biological communities
• BACTERIA (Bacteria and Archea)
• 400 morphological invertebrate species – New species every 2 weeks during 25 years!
• Evolutionary Origin – Derived from surrounding Deep Sea
– Derived from Shallow Water species
– Many evolutionary radiations at species level
– Many vent taxa originated at other organically enriched environments (cold seeps and whale bones)
• Vents as stable refugia from Global extinctions
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Cold Seeps
CH4 + O2 CO2 + H20 +ATP
CH4 CH3- + H+ +ATP
H2S + O2 SO4 ++ H+ + ATP
• Hydrocarbon reservoirs
• “methane bubbling”
• Continental shelves and Trenches
• 200 invertebrate species
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Whale skeletons & sunken logs
H2S + O2 SO4 ++ H+ + ATP
• Osteophiles
• Potential „stepping stones‟ for certain invertebrate vent species
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Invertebrate food sources Food chain based on sulfur-oxidizing bacteria • Symbiosis with Bacteria
– Vestimentiferan tube worms – Vent Mussels and vent clams
• Ingestion of Bacteria – Grazers (gastropod limpets and snails) – Filter Feeders (vent shrimp, polychaete worms,
amphipods, anemones)
• Predators – Ventfish, octopus
• Scavengers – Crabs
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Oceanic vent Biogeography
Atlantic vents
• Vent shrimp
Indian vents
• Vent shrimp
• Anemones
• Pacific vent species
East Pacific vents
• Vestimentiferan worms
• Alvinellid polychaetes
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http://web.uvic.ca/%7Everenat/364-13.jpg
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http://www.ifremer.fr/droep/Driftia.html
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www.divediscover.whoi.edu/i
Vent Mussels (Bathymodiolus )
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www.divediscover.whoi.edu/i
Vent Clams (Calyptogena)
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Vent Shrimp (Bresiliidae)
www.ifremer.fr/
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Alvinellid worms
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Vent limpets
http://web.uvic.ca/~abates/
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www.divediscover.whoi.edu/i
Vent Crabs
www.senckenberg.uni-frankfurt.de/
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Ventfish (Thermarces cerberus)
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www.divediscover.whoi.edu/i
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Periferic filter feeders
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Larval dispersal between vents Vent Plumes
www.pmel.noaa.gov/vents/PlumeStudies
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Tubeworm spawning
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Ocean Crust Age
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Mid Atlantic Ridge
http://faculty.washington.edu/lyn4/images/iceland.jpg
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East Pacific Rise
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Spreading rate and Plume incidence
www.pmel.noaa.gov/vents/PlumeStudies
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Fast and Slow spreading ridges
VanDover et al. 2002 (Science)
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White et al. 2002
Electromagnetic emissions by vents
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Light organs in vent organisms
www.deepsea.com/
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Jinks et al. 2003 (SCIENCE)
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Vent community regulation
EPR
Pacific
http://mollie.berkeley.edu/~volkman/
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Vent community regulation
Snake-Pit
Mid Atlantic Ridge
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Vent community regulation
Indian Ocean
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Vent community regulation
• Physical factors – Temperature
• Ecological factors – Competition
– Larval supply
– Predation
– Ecological cascading – Keystone predators
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http://www.pmel.noaa.gov/vents/nemo/index.html
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Lost City
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Chemical Reactions
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Olivine Density = 3.3 g/cm3 Serpentine Density = 3.3 g/cm3
40% Increase Volume
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Lost City
• Serpentinization – Olivine Serpentine (hydration)
– Exothermic reaction 260°C
– Basic fluids pH 9-10 (CaCo3 precipitate)
– Fluids contain high CH4 and H2
– 30.000 of Age
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