Metabolic Diversity
Spend more time talking about phototrophs, anoxygenic and oxygenic
phototrophs, chemolithotrophs and anaerobic respiration.
Phototrophs - eukaryotic and prokaryotic microorganisms.
Chlorophyll - heterocyclic compound with a Mg atom in the
middle. Chlorophyll a is the common chlorophyll of higher
plants. It absorbs red (680 nm) and blue (430 nm) light wavelengths
and reflects green - Why plants are green! Other chlorophylls
have different absorption spectra - absorb different wavelengths of
light.
Bacteriochlorophyll - analogous to higher plants chlorophyll
but have a absorption maximum in the neighborhood of 700
nm and greater. Different phototrophs with different
bacteriochlorophylls can coexist since they are not competing for the
same light wavelengths - increase biodiversity.
Bacteriochlorophyll located in (1) invaginations of the cytoplasmic
membrane, (2) the cytoplasmic membrane, or (3) the cytoplasmic
membrane and chlorosomes. Recall in eukaryotic phototrophs the
chlorophyll is found in the thylakoid membranes inside the
chloroplasts. In these membranes there are special chlorophyll
molecules called reaction centers associated with other
light-harvesting chlorophyll molecules whose purpose is to harvest
quanta of light and transfer their energy to the reaction center.
Purple bacteria
Invagination of cytoplasmic membrane called chromatophores.
Contains reaction center, light-harvesting I and light-harvesting
II components plus bc1 complex which is common to
the respiratory electron transport chain. The function of
light harvesting I and II also referred to as
B870 and B800-850 respectively, is to channel absorbed
light energy to the reaction center.
Electron flow ( Figure 13.10) - Light harvesting antennae
bacteriochlorophyll a molecules funnel their energy to the
reaction center bacteriochlorophyll a molecules - the
special pair. The special pair becomes excited and is
converted to a good electron donor with sufficiently low
Eo' (-1000 mVolts) to reduce a very electronegative
acceptor molecule - bacteriopheophytin. Solar energy has now
been converted to chemical energy.
Bacteriopheophytin reduces quinones in the reaction center
which reduce quinones in the quinone pool before the electrons flow
to Cyt bc1 to iron sulfur proteins, through Cyt c2 back to P870 of
the reaction center.
How does this drive ATP synthesis?
The quinones move electrons down the electron transport chain
but also move protons from inside the cell to outside the cytoplasmic
membrane thus establishing a PMF which can be used to drive
ATP synthesis via photophosphorylation - cyclic
photophosphorylation since the electrons flow in a circular
fashion.
How are reducing equivalents (NADPH) generated? NADPH is used to
reduce CO2 to organic carbon used by the cell-
auxotrophy!
Need a source of electrons since in cyclic
photophosphorylation there is no net gain or loss of electrons
from the transporters. The ultimate souce of electrons for the
reduction of NADP+ is a reduced inorganic molecule like
H2S, elemenal sulfur, thiosulfate, H2 or
organic acids like butyrate or malate.
Two ways to reduce NADP+ to NADPH.
Direct reduction if the reducing agent has a redox potential
more negative than NADP+. H2 has a redox
potential of -420 mVolts and NADP+ is -320 mVolts.
Reverse electron flow - reduced compounds that have a more
positive redox potential than NADP+. The membrane
potential is used to push electrons from the quinone pool
to NADP+ - where the quinones have a more positive redox potential
than NADP+.
Anoxygenic phototrophs - by definition these are organisms
that obtain their energy from the sun by converting solar energy to
chemical energy and do not produce oxygen during
photosynthesis as higher plants and some eukaryotic and prokaryotic
microorganisms do.
Compare Figure 13.9 with 13.13
We have been talking about energy but what about carbon? How do
autotrophs obtain their carbon if not from organic sources?
Calvin cycle or reductive pentose cycle (see 13.18)
Ribulose bisphosphate carboxylase is the enzyme responsible
for the first reaction in the cycle involving CO2 and ribulose
bisphosphate - a 5 carbon sugar. The product is 2 molecules of
phosphoglyceric acid.
Phosphoglycerate is phosphorylated and reduced by NADPH to
3-phosphoglyceraldehyde.
Steps:
6 molecules of ribulose bisphosphate accepts 6
molecules of CO2 for a total of 36 carbons among
12 3-carbon molecules (phosphoglyceric acid). These 12
molecules are than rearranged to make 6 5-carbon molecules
(ribulose bisphosphate) and 1 6-carbon (hexose) molecule. A
total of 12 NADPHs and 18 ATPs are used during the
reduction of 6 CO2s to hexose.
Chemolithotrophs - obtain their energy from the oxidation of
reduced inorganic molecules. ATP generated from oxidation of
inorganic molecules like chemoorganotrophs (aerobic respiration
process) and reducing power (NAD(P)H) is generated either directly if
the inorganic molecule has a redox potential sufficiently low or by
reverse electron transport reactions. Recall the greater the
difference between the redox potentials of two reactions, the greater
the amount of energy released.
Hydrogen oxidizing bacteria - most are facultative
chemolithotrophs capable of growing either chemoorganotrophically or
chemolithotrophically.
Chemolithotrophic growth - hydrogenase enzyme oxidizes
H2 and the electrons are transfered to quinones in the electron
transport chain ultimately moving to oxygen as the terminal electron
acceptor. A PMF is generated by the movement of the electrons
and ATP is made via membrane bound ATPases.
Reducing equivalents in the form of NADPH
some species reduce NADP+ directly
most species use the reverse electron transport mechanism discussed
earlier
Carbon fixation - use the Calvin cycle but organic
carbon will repress the synthesis of key enzymes of the Calvin
cycle.
Sulfur oxidizing bacteria - These were some of the first
chemolithotrophs described by Winogradsky. Use reduced sulfur such as
H2S, So, and
S2O32-(thiosulfate).
ATP formation - Electrons enter the electron transport
chain at various points depending on the redox potential of the
source. Electrons flow to oxygen as the terminal electron acceptor
and generate a PMF which is used to drive ATP synthesis.
Reducing equivalents - NADPH is formed by the reverse electron
transport mechanism.
Carbon fixation - Calvin cycle
Note: they grow poorly on elemental sulfur or thiosulfate
since these compounds have a relatively high redox potential.
Note:H+ is generated which means that this is an acidifying
reaction - sulfuric acid is generated. Some sulfur-oxidizing bacteria
can live at pHs in the 1-2 range.
Iron-oxidizing bacteria - Ferrous iron, Fe+2, is oxidized to
ferric iron, Fe+3. Iron has an interesting chemistry about it:
Ferrous iron rapidly oxidizes to ferric iron in air at neutral pH -
stable in anoxic conditions. At acidic conditions, ferrous iron is
stable. Best known iron-oxidizing bacteria is Thiobacillus
ferroxidans. Found in acid polluted waters like coal mining
dumps.
Energy production - ATP formation
Very little difference between the redox potential of Fe+3/Fe+2 and
1/2O2/H2O compare +0.77 V at pH 3 for the former to +820 V for the
latter. The redox potential of Fe+3/Fe+2 is too positive to reduce
NAD+, FAD, and many of the electron transport chain.
Unique ecology allows these bacteria to take advantage of the
natural pH gradient in which they live. The live in acidic
environments such that the pH outside the cell might be 2 and inside
the cell the pH is around 6 - this difference is a preformed
PMF. To maintain a constant pH inside the cell, the oxidation
of Fe+2 to Fe+3 is a proton consuming reaction - 2Fe+3 +
1/2O2 +2H+ -----> 2Fe+3 +
H2O.
Carbon fixation - Calvin cycle as usual. Generate NADPH by the
reverse electron transport process using the PMF to drive electrons
uphill. Because of the very positive redox potential of Fe+3 / Fe+2
the reverse electron process requires a lot of energy, therefore
there is very little biomass generated by these organisms in the
habitat but there is lots of ferric iron precipitates.
There is some iron oxidation occuring near neutral pH specifically at
the oxic and anoxic interfaces in nature. Recall that at neutral pH
ferrous iron is rapidly oxidized to ferric iron in the presence of
oxygen.
Neat phenomenon - large deposits of ferric iron have been
found in ancient sediments which were originally thought to be the
result of abiotic oxidation of ferrous iron where the oxygen came
from oxygenic photosynthesis. Perhaps these deposits were formed by
anoxygenic phototrophs oxidizing ferric iron in anoxic
environments.
Ammonium and nitrite-oxidizing bacteria - referred to as the
nitrifying bacteria. They use ammonia and nitrite as their
energy source - electron source. Nitrosomonas oxidize ammonia
and Nitrobacter oxidize nitrite. These bacteria are widespread
in soils.
Growth yields from the oxidation of NH3 or
NO2- are very small since there is very little
energy available from the oxidation of these two compounds. The redox
potentials of ammonia to nitrite is 0 volts and nitrite to nitrate is
+0.43 Volts and therefore they donate electrons to the electron
transport chain at relatively high redox potential electron
carriers.
Carbon fixation - Calvin cycle
Summary - chemolithotrophs growing autotrophically require ATP
and NADH. NADH generated either by the direct reduction of
NAD+ by H2 for the hydrogen oxidizing bacteria
or the energy driven reverse electron flow for the other
chemolithotrophs.
ATP production - the chemolithotrophs contain cytochromes and
quinones like the chemoorganotrophs. With the exception of the
hydrogen oxidizing bacteria, the other chemolithotrophs cannot feed
electrons into the electron transport chain at NADH level but instead
at some intermediate level between NADH and oxygen.
Mixotrophy - chemolithotrophs that can grow on organic carbon
as heterotrophs.
Anaerobic respiration - uses an electron acceptor other than
oxygen - could be organic or inorganic in nature.
facultative aerobes - are aerobes that can use either oxygen
or another electron acceptor such as nitrate.
obligate anaerobes - are anaerobes unable to use oxygen.
Nitrate reduction and denitrification - nitrate as an electron
acceptor and reduced to nitrous oxide or dinitrogen gas. This process
is called denitrification which is detrimental to agriculture since
it represents a loss of nitrogen from the ecosystem.
Enzyme is nitrate reductase which is synthesized under anoxic
conditions only. Produces nitrite which is reduced using
nitrite reductase.
Nitrite may be reduced to ammonia or reduced to nitrous oxide or
dinitrogen gas. (See figure 13.29).
See figure 13.30 for comparison of nitrate reduction with
aerobic respiration. The point is less energy from nitrate reduction
than aerobic respiration.
Common denitrifiers include species of pseudomonads such as P.
fluorescens and P. aeruginosa.
Sulfate - reducing bacteria - sulfate is reduced to hydrogen
sulfide. An organic molecules including organic acids, fatty acids,
alcohols and H2 as an electron source = source of energy.
H2 produced during the oxidation of lactate diffuses out of the cell
and is subsequently oxidized by a hydrogenase leaving the protons
outside the cell and transporting the electrons to sulfate. This
generates the PMF which can be used to make ATP. There are other
types of sulfate reducing bacteria that we will not get into.
Methanogenesis - methane formers. These use carbon dioxide as
an electron acceptor