Lecture 10: Deep sea vents Flashcards

1
Q

Deep sea shrimp (Rimicaris exoculata) and bacteria

A

= ectosymbiotic associations with bacteria

  • farming on the back
  • shed ectoskeleton and then eat skeleton
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2
Q

how do vents ‘die’

A

if local hydrothermal activity ceases or an eruption occurs

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3
Q

Tubeworms when vents ‘die’

A

tubeworm larvae must be able to colonise new vents which may be 10-100km away

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4
Q

lab study tubeworm colonisation

A
  • 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)
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5
Q

ocean currents aid in tubeworm colonisation post vent death

A
  • 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
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6
Q

larvae ___ contain symbionts

A

dont contain

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7
Q

how are symbionts re-acquired to tubeworm larvae

A
  • dont enter through mouth and gut, actually enter via the skin
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8
Q

slow spreading vents, geothermal sites are __ apart

A

further

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9
Q

deep sea shrimps: found where and movement between geothermal sites

A
  • slow spreading sites (100km + apart)
  • dispersale via larvae
  • Larvae have eyes and feed on photosynthetic derived material
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10
Q

cold seeps found in what conditions and whats found there

A

low temps and high pressures

  • methane is found as methane hydrates
  • CC a concern as heating = release methane
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11
Q

Hesiocaeca methanicola (type of worm) and cold seeps

A

burrow through methane hydrates, presumably feeding on bacteria as they are not thought to contain symbionts

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12
Q

Lamellibrachia luymesi (tube worm) from a cold seep

A
  • 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
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13
Q

difference to tube worms at cold seeps and hot water vents

A
  • 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
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14
Q

cold seep surface =

A

abundant bacterial mats on the seep surface

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15
Q

sulphur flow in cold seeps

A
  • 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
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16
Q

nitrogen fixation in cold seeps

A
  • bac & Archaea also fix nitrogen
17
Q

the challenges of small and organisms stuck together =

A
  • microbes as a ‘species’ incorrect they swap genes
  • microbes form intimate associations with other microbes
    to allow complex metabolic interactions to occur
  • Spatial heterogeneity (diverse in character) is high
  • only scratched the surface on whats known