Endeavour Segment Hydrothermal Biological Systems from the ... · at cracking front •Intense...
Transcript of Endeavour Segment Hydrothermal Biological Systems from the ... · at cracking front •Intense...
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Endeavour Segment
[email protected]; [email protected]
Hydrothermal BiologicalSystems from the Subseafloor
to the Water Column
James CowenDepartment of Oceanography
University of HawaiiSession #5, 1/11/05
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Outline• Geological/geochemistry background—Mike Mottl, Mon.• MOR Hydrothermal Habitats/biogeochem—JPC, Tues.
– Subseafloor– Seafloor– Hydrothermal plumes– MOR magmatic/tectonic events
• Molecular biology primer—Mike Rappe, Tues.• Ridge flanks subseafloor biosphere—JPC, Wed.• Serpentinization and mud volcanoes—MM, Wed.,• MOR hydrothermal microbiology—John Baross, Thurs.• Origin of life—John Baross, Friday
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Definitions
• Microbial groups by temperature tolerances– Psychrophiles: optimal growth at -10 to 20 oC– Mesophiles: optimal growth at 10-50 oC– Thermophiles: optimal growth at 40-70 oC– Hyperthermophiles: optimal growth at >80oC
• Redox reactions: In living organisms, chemical energy isstored in high-energy electrons that are transferred fromone atom to another in oxidation/reduction reactions.
NO3- + 2H+ + 2e- NO2
- + H2O H2 2H+ + 2e-
NO3- + H2 NO2
- + H2O
NO3- reduction
Half-cell rxtnsH2 oxidation
G1
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Karl 1995
G1
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Which potential metabolic processes isenergy-yielding?
– Methogenesis or methanotrophy?– CO2 + 4H2 CH4 + 2H2O– CH4 +2O2 CO2 +H2O
– Sulfur oxidation or reduction?– S(s) +1.5O2 + H2O SO4
2- + 2H+
– S(s) + H2 H2S
Depends on (i.e., Gibbs free energy of reaction, ΔGr)
– Temperature (<150oC for biotic reactions)– Pressure– Chemical composition of system (in solution and
solids)
G1
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Deep-Sea Hydrothermal Systems• Novel communities?
– MOR system 60,000 km, ~60 % hydrothermallyactive!
– Not counting ridge flanks, subduction zone back arcsystems, hotspot volcanism etc
• Key role in origins of life, early earth?– Hot, reducing conditions like early earth– UV protected; refuge from bombardment of
planetesimal bodies– Abundant source of electron donors (e.g. H2)– Presence of electron acceptors (e.g., seawater SO4
-2;Fe+3 from mineral hydrolysis)
G1
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• Analogue for extraterrestrial oceancovered bodies (e.g., Europa)– Probable liquid ocean (tidal heating)– Possible hydrothermal circulation (tidal
heating)– Planetary differentiation (partial melt of
rocky interior??—deep tidal heating)
(Nasa Galileo mission, 1997)
(R. Thomson)
G1
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prec.
leached
Neutrally-buoyant plume
Buo
yant
plu
me
G1
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Hydrothermal Vents
Subseafloor Ecosystems
G2
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MOR hydrothermalcirculation
1-3: Recharge zone•<2-150oC•e- acceptors: O2, NO3
-, SO4-2
•e- donors: Fe+2, org-CSW•Initial water-rock reactions
4-5: Reaction zone•High To (to 400oC), fresh rock at cracking front •Intense water-rock reaction•Volatile/metals leaching•Too extreme for active life
6: Upflow zone•Fluids at 350-400oC; low pH; high reduced metals/volatiles•No active life•Some entrained fluids (w/cells)
G2
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Discharge Zones1. Black Smokers
• 200-400oC (mixingdependent)
• No active microorganisms• Entrained microbes present• High concentrations of
reduced metals/volatiles• Reducing, low pH
2. Diffuse flow• 2 to ~150oC• Chemical disequilibria (High
To fluids + SW mixing)• Microbially dynamic
Active Subseafloor Biocommunity• Intense thermal/chemical
gradients• Tolerable To zones (<150oC)• Includes chimney walls
Rapid venting at 260-400oC
Slower ventingat 30-330oC
G2
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Kelley et al. 2002
G2
MOR subseafloorbiosphere
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Kelley et al. 2002
Abiogenic(degassing/fluid-rock rxtns)
Biogenic oxid-reduc rxtnsduring fluid-SWmixing
Chemical transformations in hydrothermal systemsG2
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Potential Microbial Metabolic Processes
FermentationOrganic compoundsOrganic compoundsOrganic compounds
S & sulfate reductionOrganic compoundsSo, SO42-Organic compounds
DenitrificationOrganic compoundsNO3-Organic compounds
Methane oxidation?SO42-CH4
MethanogenesisCO2CO2H2
S & sulfate reductionCO2So, SO42-H2
H2 oxidationCO2NO3-H2Anaerobic
Heterotrophicmetabolism
Organic compoundsO2Organic compounds
Methane (C-1)oxidation
CH4, CO2, COO2CH4 (and other C-1compounds
NitrificationCO2O2NH4+, NO2
-
Mn oxidationCO2O2Mn2+
Fe oxidationCO2O2Fe2+
S oxidationCO2O2HS-, So, S2O32-, S4O6
2-
H2 oxidationCO2O2H2Aerobic
Metabolic processC sourceElectron acceptorElectron (energy)donor
Conditions
G2
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e- donors
e- acceptors
Chemical systems
G2
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Amend and Shock 2001
‘H-O-N’ Chemical SystemG2
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‘H-O-S’ Chemical system
Amend and Shock 2001
G2
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370 reactions
>200 ‘species’ currently known
G2
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(Kelley et al. 2002)
<1 to >20 m
Hydrothermal vent chimney
G2
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Chimney habitats
Kelley et al. 2002
G2
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Hydrothermal Vents
Seafloor Ecosystems—
–Bathed in warm vent fluids/SW,–Variable To, O2, H2S, etc. (e.g., tides, currents,discharge rates)
G1
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Macrofauna, endosymbiontsChemoautotrophic sulfur and methanotrophic symbionts
G1
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Surface colonization by H2S oxidizing bacterium (Acrobacter sp.) excreting elemental S as rigid irregular filaments
(Taylor et al. 1999)
Microbial matsG1
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Fe-encrusting, sheathed bacteria attachedto vestimentiferan worm tubes
Fe hydroxideassoc w/sheath
Fe hydroxide Assoc w/”slime”
Sheathed bacteria
(Juniper and Tebo 1995)
worm tubeouter surface
worm tubeouter surface
Microbial mats:
Fe-deposits often cemented by amorphous silica
G1
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Hydrothermal Plumes
Buoyant and Neutrally-buoyantPlumes
G3
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Neutrally-buoyant plume
Buo
yant
plu
me
G3
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High buoyancy hydrothermalplume rising into a crossflow
J.W. Lavelle, NOAA
G3
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Cowen
G3
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(Cowen and Baker, 1998)
2
2
4
2+
2+
222NH4
+ oxid
G3
Microbial processes:•Mostly aerobic (w/ O2)•Low To (<2oC)•Cells free living and•Particle-associated•Microbes likely opportunistic
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Plume from single source invariable currents
J.W. Lavelle, NOAA/Seattle
G3
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Plume from multiple sources in variable current - PipeOrgan and neighboring vents - animation
J.W.Lavelle, NOAA
G3
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Implications of studies of hydrothermalplumes
• MOR are 60,000 km long corridor of focuseddeep ocean productivity– Oasis for deep-water zooplankton– Highway for larval and microbial transport– Enhanced biodiversity
• Extraterrestrial search for life– Subsurface basement ecosystems difficult to access– Vent systems relatively small area
• But…the water column more diffuse, butexpanded detection zone
G3
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MOR Volcanic EruptionsEvent Detection and Response
(Chadwick et al. 1998)
Old flow New flow
G4
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Kelley et al. 2002
G4
Intrusive dike phase Extrusive
flow
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Response to MOR magmatic/tectoniceventsEvent Plume
(Summit and Baross 1998)
(Haymon et al. 1993)
Snowblowerventing
G4
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(Baker 1998)
Event Plume: 1996 Gorda Ridge
Massive, catastrophically expulsed volume of hydrothermalfluids—unique chemistry and microbiology, suggesting originsIn portions of subsurface different from those supplying chronic Hydrothermal discharge
10’s kms
1,000 m vertical
G4
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Heat from cooling lava
Heat from cooling dike
Pre-existing hotfluids releasedby diking or othermagmatic process(or major tectonic?)
•Not enough heat•Heat released too slow (EPs form rapidly)•Chemistry inconsistent w/ that of EPs (EP: low uniform 3He/heat; low Mn/heat)
•Presence of thermophiles in EPs
(Embley and Lupton 2004) (Summit and Baross 1998)
G4Event PlumeFormation
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Magmatic event: heat flux vs time
0 100
5 103
1 104
1.5 104
2 104
2.5 104
3 104
0
2 1016
4 1016
6 1016
8 1016
1 1017
0 0.5 1 1.5 2 2.5 3 3.5
Heat Flux (MW) 1993 CoAxial Floc
Heat Flux (MW) 1993 CoAxial Flow
Heat Inventory (J) 1998 AxialH
eat
Flu
x (
MW
)
Heat
Invento
ry (
J)
Years since eruption
G4
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Real time detection of seismicity associatedwith magmatic/tectonicevents
G4
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T-phase waves
(J. Cook 2004)
U.S. Navy’s Sound Surveillance System (SoSuS)
G4
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Post-eruption time-seriesvent fluid chemistry
(Huber et al. 2003)
Volatile-rich SW-dominated
G4
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(Huber et al. 2003)
Higher To Lower To
Time series rRNA community signaturesG4
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Implication of magmatic (tectonic too)events for Microbial Communities
• Changes to hydrothermal circulation– Intensity (e.g., higher/lower flux)– Subseafloor plumbing (e.g., new
cracks/fissures/vents; also demise of whole ventfields)
– Temporal/spatial variability in thermal / chemicalgradients and in microbial consortia
• Event plume formation– Heat and mass flux to ocean– Large-scale dispersion of subseafloor
microorganisms (long-term colonization/survival?)– Window into MOR subsurface biosphere
G4
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Summary• Deep-Sea Hydrothermal Systems
– Global corridor of high productivity and high microbialdiversity (both subseafloor and in water column)
– Diverse habitats• thermal / chemical / substrate gradients• Subseafloor, seafloor, water column
• Important implications for origin of life (stay tuned for Baross lecture-Friday)• Implications for search for life on liquid (esp.
water) / ice covered extraterrestrial body– Habitat (To, chemistry, substrates), metabolic diversity– Initial search strategies
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(Kelley et al. 2002)
G4
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(Lupton et al. 1998)
Tracking EPs bySeeding with floats (e.g., RAFOS)or AUVs*
*Autonomous underwater vehicle
recovery
launch
G4
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Standing Stock [mg C m-3]Production/(Consumption) [mg C m-2d-1]Flux [mg C m-2d-1] Cowen et al. 2004
G3Preliminary Mass Balance for OC Production
in Hydrothermal Plume
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• Analogue for extraterrestrial oceancovered bodies (e.g., Europa)– CO2 + 4H2 CH4 + 2H2O– 2CO2 + 6H2 (CH2O)n + CH4 + 3H2O
In extreme case of limited e- acceptors:– 2Fe(OH)3 + H2 2FeO +4H2O
However,– There is SOx and could be O2– Radiolytic O2:
• 40K ~ 0.012% total K(β-particles and γ-radiation + 2H2O 2H2 + O2)• 1010 moles O2 / yr on Europa107-109 kg biomass / yr (if plenty CO2)105-106 kg biomass / yr (if CO2 limited)
(R. Thomson)
Europa vent fluids too reducing and high pressure: reaction equilibrium to right
Earth’s oceanic production: 1013 kg C yr-1
Hydrothermal production: 107-108 kg C yr-1 (w/O2!)
(Gilmour and Sephton, 2004)
G1
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Pathways and sites for microbial biomass production inMOR hydrothermal system
Karl 1995
--Hypothetical location in hydrothermal system of biomass production
G2
B11
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Life: properties-oriented definition
Generational: changes inmineralogy due to change inenvironment and ion source.Individuals: water release /adsorption (clay minerals);outer resistant layers (e.g.,oxide or silicate layers)
Generational: Genetic adaptation,exchange of genetic material.Indivisual: homeostaticadaptation: movement, cellularshrinkage / spore formation innutrient-poor environment
Reaction to,compensation forand develop newabilities to respondto environmentalchanges
Adaptationtoenvironment
Crystals break due tocleavage; cleavage surfacemay contain “growth”information
Various mechanisms (binaryfission); genetic code preservedand duplicated
Multiplication ofinformation
Reproduction
Crystal growth withfavorable environ and ionsources; Local surfacereversibility can correctmistakes during silicate ormetal oxide minerals
Cell growth as long as nutrientsavailable / environ. conditionsfavorable; until reprod occurs;Self-organization, errorscorrected by enzymes
Increase in size ofsingle unit
Growth
Energy uptake via heat /light, elevation of e- tohigher energy bands;
Various types of biochemicalpathways including chemo- andphotosynth; energy stored asATP or GTP
Yield of energy byelectron transfer
Metabolism
Inorganic ParallelOrganic MechanismBasicRequirement
Property
Schultze-Makuch et al. 2002
G1
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Definition of Life: Inspired bysearch for extra-earth life
1. Bounded microenvironments inthermodynamic disequilibrium withexternal environment
2. Capable of transforming energy and theenvironment to maintain low entropy*state
3. Capable of information encoding andtransmission
Schultze-Makuch et al. 2002
G1
*Entropy: The tendency of a system, including the universe, toward increasing disorder and inertness
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(Haymon et al. 1993)
Snow blower vents, 9o N-East Pacific Rise
G4
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In situ Chemical Redox Analyzer
dissolved O2, H2S, MnII, FeII, S2O3
2-, S4O62-, Sx
2-, S0, aqueous species of FeIII and FeS
In situ VoltammetricElectrochemicalmeasurements
Volts (vs AgCl)-1.5 -1.0 -0.5
i (A)
-1e-6
0
1e-6
2e-6
time (sec)
0 30 60 90 120 150 180
co
nc
en
tratio
n (
µM
)
0
100
200
300
400
500
Free H2S
SAVS
FeS
A
B
FeSfree H
2S
SAVS
*
Brian Glazer
G3
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Thomson et al. 2004
G3