bioenergetics and geomicrobiology

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Philippe Van Cappellen and Christina Smeaton Bioenergetics and Geomicrobiology (Are microbes better at thermodynamics than geochemists?) Cargèse Summer School 2018 0

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Page 1: Bioenergetics and Geomicrobiology

Philippe Van Cappellen and Christina Smeaton

Bioenergetics and Geomicrobiology(Are microbes better at thermodynamics than geochemists?)

Cargèse Summer School 2018

0

Page 2: Bioenergetics and Geomicrobiology

Geomicrobial Activity

• Cycling of carbon and nutrients (N, S, P, K, Si, Ca, Fe, …)

• Weathering, soil formation, soil fertility, water quality

• Organic matter decomposition, transformation and preservation

• Production greenhouse (CO2, CH4, N2O) and other reactive gases

• Biomineralization, bio(nano)materials

• Natural attenuation, bioremediation

• Biotechnology

• Green (bio)chemistry

...

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Page 3: Bioenergetics and Geomicrobiology

Geomicrobial Activity in the Subsurface

• Microbial ecosystems

• Ecological interactions

• competition, syntrophy,

• predation, energy flow

• Complex reaction networks

• biotic-abiotic

• Energy-limited environments

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Page 4: Bioenergetics and Geomicrobiology

Life = Redox Chemistry

electron

donor substrates

Cell synthesis

reactions

terminal

electron

acceptor

Energy generation - catabolismBiomass synthesis - anabolism

electrons electrons

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Page 5: Bioenergetics and Geomicrobiology

Example

Aerobic cell growth on citric acid: macrochemical reaction:

+1 -0.2 +4

Citric acid (C6H8O7): both electron donor for energy production

and for biomass synthesis.

YG = d/6a (mol C/mol C)Here:

Growth yield:new biomass produced

substrate utilizedYG =

aC6H8O7 + bO2 + cNH4+ dCH2O0.6N0.2 + eCO2 + fH+ + gH2O

new biomass

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Page 6: Bioenergetics and Geomicrobiology

Redox Zonation

http://www.awi.de/fileadmin/user_upload/Research/Research_Divisions/Geosciences/Marine_Geochemistry5

Page 7: Bioenergetics and Geomicrobiology

Redox Zonation � Thermodynamics

https://clu-in.org/techfocus/default.focus/sec/Bioremediation/cat/Aerobic_Bioremediation_(Direct)/

Redox zonation:

subsurface microbial communities optimize catabolic energy production

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Page 8: Bioenergetics and Geomicrobiology

Microbial Kinetics

Microbial growth: Monod kinetics

X:

µ:

biomass

specific growth rate

µmax:

S:

Ks:

maximum µlimiting (growth) limiting

half-saturation constant

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Page 9: Bioenergetics and Geomicrobiology

growth

rate

maximum growth rate

½ maximum

growth rate

Ks substrate concentration, [S]

Saturation Kinetics

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Page 10: Bioenergetics and Geomicrobiology

[S]

B

Growth Kinetics � Geochemical Kinetics

Michaelis-Menten kinetics

(substrate utilization):

Y: growth yield

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Page 11: Bioenergetics and Geomicrobiology

Example: Sulfate Reducers Growing on H2

Electron donor:

Catabolic reaction:

Electron acceptor:

X 4

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Page 12: Bioenergetics and Geomicrobiology

Catabolic Reactions & Thermodynamics

energy demanding reaction

energy yielding reaction

Catabolic reaction:

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Page 13: Bioenergetics and Geomicrobiology

Gibbs Energy of Reaction

standard state Gibbs energy (ai = 1)

Q: reaction quotient

a: activity

ν: stoichiometric coefficient

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Page 14: Bioenergetics and Geomicrobiology

Example: Sulfate Reducers Growing on H2

Aqueous solute:

Hydrogen ion:

Volatile species:

Pure solid: solvent:

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Page 15: Bioenergetics and Geomicrobiology

Life = Chemical Disequilibrium

degree of

disequilibrium

[0,1]

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Page 16: Bioenergetics and Geomicrobiology

Reaction

rate

−∆Gr+0−

Thermodynamically

inhibited

Thermodynamically

limited

No thermodynamic

limitation

Kinetics and Thermodynamics

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Page 17: Bioenergetics and Geomicrobiology

Thermodynamic Limitation

Example: Sulfate reducing bacteria growing on H2

Classical “Monod” kinetics:

With thermodynamic limitation:

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Page 18: Bioenergetics and Geomicrobiology

Thermodynamic Driving Force, FT

Model 1*: ∆Gmin

= m⋅ ∆GATP

*Jin Q. and Bethke C.M. (2003) Appl. Environ. Microbiol. 69, 2340-2348 #LaRowe D.E. et al. (2012) Geochim. Cosmochim. Acta 90, 96-109

where

Model 2#: F ⋅∆Ψ

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Page 19: Bioenergetics and Geomicrobiology

Thermodynamic Driving Force, FT

Model 1: Transition State Theory

FT

= 0

Model 2: Fermi-Dirac Statistics

where

Active bacteria:

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Page 20: Bioenergetics and Geomicrobiology

Cellular Energy Balance

Dissipation

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Catabolic energy production = growth + dissipation + maintenance

Page 21: Bioenergetics and Geomicrobiology

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Anabolic Energy Demand

Anabolism (ANA):

carbon source + nutrients (N, P, …) + energy � 1 C-mol biomass

Catabolism (CAT):

electron donor + electron acceptor � products + energy

Metabolic reaction (MET): MET = ANA + λcat•CAT

number of times the catabolic reaction must proceed

in order to build 1 C-mol biomass

λcat:

λcat is directly related to the growth yield!

Page 22: Bioenergetics and Geomicrobiology

75 studies, batch and chemostat

Thermodynamics � Growth Yields

21Smeaton C. and Van Cappellen P. (2018) GCA – under review.

Page 23: Bioenergetics and Geomicrobiology

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Example: Iron Reducers Growing on Acetate

Anabolic reaction (ANA):

acetate biomass

Catabolic reaction (CAT):

(at 35°C)

(at 35°C)

Page 24: Bioenergetics and Geomicrobiology

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Thermodynamics � Growth Yield

Page 25: Bioenergetics and Geomicrobiology

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Departure from Standard State Conditions

Page 26: Bioenergetics and Geomicrobiology

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Gibbs Energy Dynamic Yield Method (GEDYM)

Empirical relationship:

Obtain ∆Gmet and calculate:

Page 27: Bioenergetics and Geomicrobiology

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Gibbs Energy Dynamic Yield Method (GEDYM)

YOBS (C-mol biomass/C-mol ED)

YP

RE

D(C

-mo

lb

iom

ass

/C-m

ol

ED

)

Page 28: Bioenergetics and Geomicrobiology

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Experimental conditions: Caccavo et al. (1994) Geobacter sulfurreducens sp. nov., a hydrogen-

and acetate-oxidizing dissimilatory metal-reducing microorganism. Applied and Environmental

Microbiology 60, 3752-3759.

Experimental Data: Acetate/Fe(OH)3

Page 29: Bioenergetics and Geomicrobiology

Metabolic (Macrochemical) Reaction

Page 30: Bioenergetics and Geomicrobiology

Dynamic Growth Yields

Acetotrophic

Methanogenesis

(12°C, pH 7)

Page 31: Bioenergetics and Geomicrobiology

Pirt Equation:

where

substrate utilization rate

specific growth rate

growth yield

maintenance requirement (rate)

Growth and Maintenance

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biomass

Page 32: Bioenergetics and Geomicrobiology

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Bioenergetics and Reactive Transport

1. FT: thermodynamic limitation on catabolic reaction

2. λcat: coupling catabolism and anabolism

3. me: maintenance requirement

Page 33: Bioenergetics and Geomicrobiology

Source: http://www.jantoo.com/cartoon/12265265

The End

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