32
Oxygen • “Permanent” burial of organic matter on cratons • Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet • Requires liquid water on the surface of the planet

Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

Embed Size (px)

Citation preview

Page 1: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

Oxygen

• “Permanent” burial of organic matter on cratons

• Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

• Requires liquid water on the surface of the planet

Page 2: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 3: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 4: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

The evolution of nannomachines

The fundamental problem in origins of life - evolution of energy

transduction before information? Or vice versa?

Page 5: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

Transmission microscope picture of NPP1

Electron sources: Photosynthesis and respiration

Page 6: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

Model of bacterial reaction center in Ro. denitrificans (modified from Takamia, 1989)

IRFRR fluorescence transient

Page 7: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

Light utilization and carbon fixation – these bugs are photoheterotrophs (a “dual fuel” metabolic strategy}

Wavelength [nm]400 500 600 700 800 900Absorbance (a.u.), 875 nm EM (a.u.),

and quantum efficiency

0.0

0.2

0.4

0.6

0.8

1.0Absorbance

Emission at 875 nm x 4

QuantumEfficiency

Irradiance [μmol quanta m-2s-1]

0 200 400 600 800 1000 1200( 2) ( )mmol CO fixed mol BChla

-1 s-1

4

6

8

10

12

14

16

18

electrons RC

-1 s-1

0

10

20

30

40

50

60

CO2 fixedElectron transportrate

Page 8: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 9: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 10: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

PSII type Reaction Center

Page 11: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

The Mn cluster in PS II

Page 12: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 13: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 14: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

Frozen metabolic accidents

Page 15: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

1.2

PsaCPsbAAtpHPsbDPetBPsbFAtpBRbcLPsaBPsbLPetDAtpAPsaAPsbCPsbBPsaEPetGPsbKAtpIPsbEPetCPetHAtpCPetAPsaDPsbHAtpEPsbJPetFPsaMPsbWPsbNPsaLAtpDPsbOAtpGAtpFPsbPPsbX

mutation rate (substitution/site/OTU)

proteins in all chloroplasts

proteins in at least one but not all chloroplasts

proteins in nucleus only

PS genes retained in chloroplasts are very highly conserved

Page 16: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 17: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 18: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 19: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

34S sulfate 34S sulfide 33S

-50

-25

0

25

50

0 1 2 3 4 5

Age (Ga)

34S

-10

-5

0

5

10

33S

Page 20: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 21: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

NitrogenaseNitrogenase

Page 22: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

Chronically Crippled Nitrogenase

0

50

100

150

200

250

300

350

0 5 20 50

Oxygen concentration (% in air)

% nitrogenase activity from

control

Northern - nifH

Westerns-Fe-protein

Oxygen concentration (% in air)

0 5 20 50

Nitrogenase activity

0

50

100

150

200

250

300

350

0 5 20 50

Oxygen concentration (% in air)

% nitrogenase activity from

control

Northern - nifH

Westerns-Fe-protein

Oxygen concentration (% in air)

0 5 20 50

Nitrogenase activity

Page 23: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 24: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

Anabaena sp.

Page 25: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 26: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 27: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

H2 or C-mediated

Photosynthesis

O2

Mn4+

NO3-

N2

Fe3+

SO42-

CO2

H2O

Mn2+ NH4+ Fe2+ HS- CH4 H2 [CH2O]

+CO2

Respiration

O2-mediated

Mn -mediated

Fe-mediated

S-mediated

N-mediated

N2-fixation

Page 28: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 29: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

The rise in oxygen

• The last big biological innovation on Earth

• Led to the rise of metazoans – and the success of aerobic eukaryotes.

• Altered Earth’s chemistry forever

Page 30: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet
Page 31: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet

Holding Oxygen concentrations in check

• Feedbacks with N cycle

• C cycle (photorespiration)

• And (later) oxidation of organic matter (lignins)

Page 32: Oxygen “Permanent” burial of organic matter on cratons Continuous coupling of C/N/O (and S) redox reactions – never an equilibrium state for the planet