Lecture 10: Deep sea vents Flashcards
Deep sea shrimp (Rimicaris exoculata) and bacteria
= ectosymbiotic associations with bacteria
- farming on the back
- shed ectoskeleton and then eat skeleton
how do vents ‘die’
if local hydrothermal activity ceases or an eruption occurs
Tubeworms when vents ‘die’
tubeworm larvae must be able to colonise new vents which may be 10-100km away
lab study tubeworm colonisation
- larvae cultured at 2DC and 250 atmosphere (cold than vent, still = pressure)
- estimated survival of 38 days
- modelling studies show that larvae could colonise sites up to 100km away NOT FURTHER
- fast spreading vents (dont eat on the way)
ocean currents aid in tubeworm colonisation post vent death
- ocean currents constrain embryo dispersal along the ridge
- larvae are therefore transported along the ridge improving their chances of survival)
- drawn towards other active geothermal sites
larvae ___ contain symbionts
dont contain
how are symbionts re-acquired to tubeworm larvae
- dont enter through mouth and gut, actually enter via the skin
slow spreading vents, geothermal sites are __ apart
further
deep sea shrimps: found where and movement between geothermal sites
- slow spreading sites (100km + apart)
- dispersale via larvae
- Larvae have eyes and feed on photosynthetic derived material
cold seeps found in what conditions and whats found there
low temps and high pressures
- methane is found as methane hydrates
- CC a concern as heating = release methane
Hesiocaeca methanicola (type of worm) and cold seeps
burrow through methane hydrates, presumably feeding on bacteria as they are not thought to contain symbionts
Lamellibrachia luymesi (tube worm) from a cold seep
- 550m depth at gulf of mexico
- form association with microbes to use methane
- dye tubes with blue chitin stain to determine growth
- grow v v slowly, live 170-250 years
- longest lived animal on earth
difference to tube worms at cold seeps and hot water vents
- sulphide doesnt enter the water column, instead it is taken up through the ‘root’ of the worm
- despite low temps, v high flux of sulphide through the system
cold seep surface =
abundant bacterial mats on the seep surface
sulphur flow in cold seeps
- methane can provide energy for sulphate reduction, but
vestimentiferan tubeworms do not form symbioses with methane oxidising symbionts - Aggregates of bacteria are found within the cold
seeps.
–Anaerobic sulphate reducing Bacteria
–Anaerobic methane oxidising Archaea
—> Archaea produce elemental S which is then used by bacteria - sulphate must be recycled through the tubeworm root in order to provide sufficient sulphur for 200-250 years growth