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Anoxygenic Photosynthesis in the Archaean World

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Covers 2 lectures talking about the origin of photosynthesis - both oxygenic and anoxygenic. Only basic material/summary of lecture covered - no extra reading.

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Anoxygenic Photosynthesis in the Archaean World

The Archaean Environment (3.4 bya)

 Hydrothermal vents
 Stromatolites – gives clues on the
appearance of photosynthetic activity
(3.4 bya) – inferred by morphology, no
direct evidence to support any of the
possible origins (Olson and Blankenship,
2004) but stromatolites suggested
that photosynthetic organisms existed
 “redox gradients” – oxidising surface
at the top and an alkaline hot solution
at the bottom (more subject to
debate)
 Oxygenic photosynthesis had a large impact on the planet
- Great Oxidation Event: oxygen began to accumulate from ~2.7-2.2 bya (seen from
formation of iron oxides Fe2+  Fe 3+)
- No ozone prior – needed photochemistry and oxygen  for about ~450 million
years, ozone layer has been protecting organisms against UV

Photosynthesis

 In the 1770s – Joseph Priestly performed experiments showing that plants (sprig of
mint) released a gas that allowed combustion (inadvertently demonstrated that
plants released molecular oxygen – even though he was not aware of this)
 Jan Ingenhousz later demonstrated that sunlight was necessary for photosynthesis
and that only green parts of plant could release oxygen
 Photosynthesis leads to carbon assimilation, but it is a misnomer to say that is the
hydration of carbon – it is a light-driven redox reaction
 Van Niel recognised that some bacteria used hydrogen sulphide rather than oxygen
– concluded that photosynthesis depends on elctron donation and acceptor reactions
and that oxygen released during photosynthesis came from the oxidation of water

Oxygenic Photosynthesis
CO2 + 2H2O + Light Energy  (CH2O) + O2 + H2O
Anoxygenic Photosynthesis
2H2S + CO2 - 4e- -> CH2O + H2O + S2
2H2Org (Succinate) + CO2 – 4e- -> CH2O + H2O + Org (Fumarate)
2H2 + CO2 - 4e- -> CH2O + H2O
Van Niel Equation
2H2A + CO2 – 4e- and light -> CH2O + H2O + A2

, Experimental evidence that molecular oxygen came from water was provided by Hill
and Scarisbrick (1940) using isolated chloroplasts where A is an eelectron acceptor
or Hill oxidant
 Ruben et al., (1940) also demonstrated this using 18O enriched water
 Titration experiments also revealed that there were 2 light reactions (in oxygenic
photosynthesis)

Photosynthetic Energy Transformation

 Light reactions = electron and proton transfer
reactions
 Light independent reactions = biosynthesis of
carbohydrates from CO2
 In more primitive organisms (eg. oxygenic
cyanobacteria, prochlorophytes, anoxygenic
photosynthetic bacteria) lack organelles
- Light reactions occur in complex membrane
system (photosynthetic membrane)
that is made up of protein complexes,
electron carriers, lipid molecules
- Photosynthetic membrane is
surrounded by water and thought of
as a 2-D surface that defines a
closed space with inner and outer
water phase
- Protein complexes embedded creates
an asymmetrical arrangement which allows some energy released during electron
transport to create an electrochemical gradient of protons across the
photosynthetic membrane
 Light reaction convert energy into several forms
- First step is conversion of photon to an excited state of an antenna pigment
molecule located in the antenna system
- Antenna system consists of several pigment molecules – chlorophyll,
bacteriochlorophyll, carotenoids
- Antenna system anchored to proteins within photosynthetic membrane and serve a
specialised protein complex known as a reaction centre
 In oxygenic photosynthetic organisms – 2 different reaction centres (PSI and PSII)
work concurrently but in series
- PSII feeds electrons to PSI
- Electrons are transferred from PSII to PSI by intermediate carriers

, - Net reaction is the transfer of electrons fronm a water molecule to NADP+,
producing reduced NADP (NADPH)
- Energy stored in NADPH is then used for later reduction of carbon
- Addtionally, the movement of electrons also pumps hydrogen ions across the
membrane producing a electrochemical gradient which is used to generate ATP via
ATP-synthase
 In anoxygenic photosynthetic organisms, water is not used as the electron donor
- Electron flow is cyclic and driven by a single photosystem, producing a proton
electrochemical gradient used to provide energy for reduction of NAD+ by an
external H-atom or electron donor (eg. H2S or an organic acid) in a process known
as “reverse electron flow”
- Fixation of CO2 occurs via different pathways in different organisms




Reaction Centres

Oxygenic Organisms Anoxygenic Organisms
- Plants, algae, bacteria - Use light energy to extract electrons from
- Structure of PSII in molecules other than water
these organisms is very - Assumed to be ancient organisms
similar - Purple bacteria, green sulphur bacteria, green
gliding bacteria, gram positive bacteria


Type 1 Reaction Centres

 Iron-sulphur type reaction centres
 Electron from sulphide succinate, through
metabolic processes  MQ which eventually
excites a chlorophyll molecule to emit an
electron

Type 2 Reaction Centres

 Quinone type reaction centres
 Electron from chlorophyll passed onto quinone
then to ETC (ATP synthesised)
 Electron returns to original donor through
metabolism
 Primary distinguishing feature between two
types are the early electron acceptor cofactor
- FeS centres in type 1
- Pheophytin/quinone complexes in type 2

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Geüpload op
6 april 2016
Aantal pagina's
5
Geschreven in
2014/2015
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