hydrothermal vents Flashcards
what are hydrothermal vents?
naturally formed structures, occur on divergent plate boundaries, where tectonic plates are moving apart. The vents expel a fluid that was heated to extreme temperatures when seeping through the Earth’s crust from the ocean
depth
500-5000
light
none
pressure
increases with depth, with every 10 m of depth there is an additional 1 atm of pressure
temperature
Water coming out of the vents can be up to 400 C
But the water does not boil because of the great pressure
Waters surrounding the vents can be as low as 3-4oC
substrate
Chimneys – smokestacks that form as superheated
water is extruded
This water is very rich in minerals which precipitate
out in the much colder, oxygen-rich water to form
chimneys
Up to 55 m tall (Lost City)
Pillow lava – forms during slow extrusion of lava
the cycle of water in vent
Cold water seeps through cracks in seafloor
Water is heated by molten rock and chemically modified:
Oxygen is removed
Hydrogen sulfide and dissolved metals (e.g. iron, copper and zinc) are added
Heated water then rises up through crust
In cold, oxygen-rich water metal sulfides form and precipitate out
oxygen
absent from vent water but present in
surrounding water
H2S hydrogen suflide
present in vent water but absent from surrounding water
pH
of water coming out of vents can be as low
as 2.5 (but at ‘Lost City’ pH = 9-11)
salinity
remember that hydrothermal vents are one source of the salt in the ocean
Nutrients
iron from vents, others may sink from shallower waters
black smokers
Hottest of the vents
Mostly iron and sulfide which combine to make
black ‘smoke’
white smokers
Cooler water than black smokers
Barium, calcium & silicon
bio adaptations
No light means no photosynthesis
Chemosynthesis instead!
Chemical equations of photosynthesis and
chemosynthesis are very similar but the
source of energy differs (light versus hydrogen
sulfide)