Lecture 5: Life in rocks Flashcards

1
Q

souring of oil wells

A

1926

  • known for many years that micro-organisms cause souring
  • microbial induced corrosion is a major problem
  • microbes produce acid to go through steel
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2
Q

microbes & fuel

A

microbes can degrade fuels

  • for clean up? –> possible ecosystem service
  • > can be a bad thing aeroplane fuel tanks
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3
Q

example of microbe that leads to oil souring

A

Archaeoglobus fulgidus

– chemoautotroph

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4
Q

problems with studying life in rocks

A
  • Access
  • – extremely limited
  • – many organisms are obligate piezophiles
  • contamination
  • identification
  • – many bacteria ‘shrink’ when starved of nutrients., can be tiny, hard to find
  • biology
  • – is an individual organism millions of years old or is there a slowly growing population at depth? / different time scale?
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5
Q

piezophiles

A

pressure lovers

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6
Q

problems faced by organisms living within rocks

A
  • extremes of heat and pressure
  • space (must be enough room for them to live)
  • nutrients and energy source
  • access –> how do they get there?
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7
Q

confined subsurface microbial communities in Cretaceous rock:

A

KRUMHOLZ ET AL 1997

  • drill into side of volcanoe
  • erupts, sterilises everything
  • angled borehole unsuccessful but vertical a little further away was
  • drill down 300m obtained rock cores
  • fluorescent dyes for contamination
  • foil w radioactive sulphate used
  • sample analysed
  • spikes in bio activity where sandstone and shale meet as where organic material is
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8
Q

drilling into rocks: what do you need

A

drilling fluid

  • contain contaminants, must use tracer to determine if recovered material is contaminated
  • tracers =
  • –fluorescent dyes
  • – fluorescent microspheres
  • – volatile perfluorocarbons
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9
Q

detection of biological activity in rock cores

A
  • rock cores are sectioned and overlaid with a foil containing radioactively labelled sulphate
  • biological activity reduces sulphate to sulphide (sulphates wash off)
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10
Q

why peaks in biological activity where sandstone and shale meet

A
  • shale rich in organic material but too compact for life

- sandstone larger pore size filled w water, but lack organic nutrients

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11
Q

shale and sandstone what happens to radioactive labelled sulphate foil

A

it is reduced to sulphide and acetate production (acetate is important substrate for microbial growth)

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12
Q

acetate and microbes

A

important substrate for growth

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13
Q

drilling bore holes expenses

A

deeper u go, more expensive it is. so how do we get around this?

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14
Q

alternatives to drilling multiple bore holes

A
  • drill one, let it fill w water, lower down substrate to certain depth
  • MULTILEVEL SAMPLER
  • measure the microbes grown on those substrates
  • measure conc of microbes at diff depths
  • 16S rRNA gene sequencing used
  • careful to not ruin rock stratification
  • KOVACIK ET AL 2006 used one
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15
Q

microbial activity in oil reservoirs:

A
  • sandstone, below = water saturated, top = oil water contact
  • water supplies nutrients
  • near oil-water contact, microbes skew oil material, as oil degraded
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16
Q

biodegradation ___ oil quality

A

reduces

  • undegraded oil reservoirs contain many short chain, light oils
  • biodegradation removes these (producing methane), leaving heavy oils & tars
  • specific organisms not known, but probs anaerobic (fermentative) methanogens with upper temp limit of 80DC
17
Q

what are the pressure limits on life? How do u measure this

A
  • organisms w air spaces i.e. lungs risk of crushing
  • microbes were introduced into a DIAMOND ANVIL CELL
  • formate oxidation was monitored (NMR) within the anvil at a range of pressures
18
Q

NMR use in measuring pressure

A
  • can be used to monitor the chemical state within the anvil
  • formic acid & bacteria
  • formic acid produces unique NMR signals
  • oxidation of the formate leads to these signal declining
  • formate oxidation continues even at ultra-high pressures (but rates decline at high pressure)
19
Q

pressure issue on life?

A

not really a problem unless you have air spaces

20
Q

nematode in deep mines of South africa

A
  • Halicephalobus mephisto
  • multicellular organism
  • isolated from water 900-3600m deep
  • C14 shows water is 3000-12000 years old
  • extensive efforts to show not contamination
  • not all subsurface life is single celled microbes
21
Q

nematode: Halicephalobus mephisto

A
  • nematode found in deep mines in South Africa
  • preferentially fed on borehole bacteria
  • low O2 environment
  • reproductive parthenogenetically
  • grow up to 41DC