Hydrocarbonoclastic bacteria have two fundamental characteristics: (1) specific membrane-bound
dioxygenases and (2) mechanisms for optimizing contact with water-insoluble hydrocarbons. Microbial
biodegradation occurs wherever oil contamination occurs. However, biodegradation rates are slow and as a result there are severe toxic effects on marine life in the water and on the coast. The hydrocarbons contained in
petroleum have a different behavior in water depending on their chemical nature. This process is called
weathering, those with low molecular weight volatilize when they reach the surface. The rest is attacked by bacteria that are able to do this. These bacteria do not adhere to the oil and do not have a high
hydrophobicity of the cell surface. The next stage of degradation involves microorganisms with high cell surface hydrophobicity, which can adhere to residual high molecular weight hydrocarbons. Adhesion is due to hydrophobic fimbriae, fibrils, lipids and proteins of the
outer membrane and some small molecules of the cell surface, such as
gramicidin S and
prodigiosin. All petroleum products are derived from crude oil whose major constituents are hydrocarbons, that can be separated into four fractions:
saturated,
aromatic,
resin and
asphaltene fractions. The susceptibility of hydrocarbons to microbial degradation can be generally ranked as follows: linear alkanes branched alkanes > small aromatics > cyclic alkanes. Some compounds, such as the high molecular weight polycyclic aromatic hydrocarbons (
PAHs), may not be degraded at all, asphaltenes and resins are considered to be
recalcitrant to biodegradation.
Alkane degradation pathways Alkanes are readily biodegraded aerobically in the sea by several different pathways.
Terminal oxidation The degradation of medium-length ones by
Pseudomonas putida starts from the
alkane hydroxylase, this enzyme is made up of three components: the membrane-bound oxygenase component and two soluble components called
rubredoxin and rubredoxin reductase. From the oxidation of the
methyl group of n-alkanes by the alkane hydroxylase, n-
alkanols are released which are further oxidized by a membrane-bound
alcohol dehydrogenase in n-
alkanals. The n-alkanals are subsequently transformed into
fatty acids and then into
acyl CoA, respectively by the
aldehyde dehydrogenase and by the
acyl-CoA synthetase. CH3-R-CH3 -> CH3-R-CH2OH -> CH3-R-CHO -> CH3-R-COOH -> (CH2OH)-R-COOH CH3-R-CH2OH -> (CH2OH)-R-CH2OH -> (CH2OH)-R-CHO -> (CH2OH)-R-COOH (CH2OH)-R-COOH -> CHO-R-COOH -> HOOC-R-COOH
Subterminal oxidation This path leads to the release of
secondary alcohols. The n-alkanes are oxidized by monooxygenase to secondary alcohols, then to
ketones and finally to fatty acids. R1-(CH2)(CH2)-R2 -> R1-(CH2)(CHOH)-R2 -> R1-(CH2)(CO)-R2 -> R1-(CH2)O(CO)-R2 -> R1-COOH + R2-COOH
Cycloalkane degradation pathways Cycloalkanes are degraded by a co-oxidation mechanism, the process leading to the formation of a cyclic alcohol and a ketone. A monooxygenase introduces an oxygen into the cyclic ketone and the cyclic ring is cleaved. that codes for it. Toluene is degraded to alcohol to benzyl, to benzaldehyde and then to benzoate, which is further transformed into the intermediates of the
TCA cycle. •
F1 pathway:
P.putida is able to undertake this pathway, which consists in the introduction of two hydroxyl groups into toluene, forming cis-toluene dihydrodiol. This intermediate is then converted to 3-methylcatechol. •
KR1 pathway:
Pseudomonas mendocina KR1, is able to convert toluene into p-cresol, by the enzyme toluene 4-monooxygenase. Subsequently, p-hydroxybenzoate is formed through oxidation of the methyl side chain. •
PK01:
Pseudomonas pickettii PKO1 oxidizes toluene with the enzyme toluene 3-monooxygease to m-cresol, which is further oxidized to 3-methylcatechol by another monooxygenase. •
G4: The G4 pathway was observed in
Bukholderia cepacia G4, where toluene is converted into o-cresol by toluene 2-monooxygenase and subsequently another monooxygenase converts it to 3-methylcatechol.
Anaerobic degradation pathways Oil components that are trapped in marine sediments tend to persist in
anaerobic conditions. Some hydrocarbons can be oxidized under anaerobic conditions when
nitrate reduction, sulfate reduction, methane production, Fe3+ reduction or photosynthesis are coupled to hydrocarbon oxidation. Anaerobic bacterium strain HD-1 grows on in the presence of or tetradecane. In the absence of , tetradecane is degraded, and the major metabolic intermediate is 1-dodecene •
Biosurfactants: The contact between bacteria and hydrocarbons is fundamental because the first degradative step involves the use of oxygenase. Contact is favored by adhesion and
emulsifying mechanisms Bacteria that break down hydrocarbons often produce bioemulsifiers as
secondary metabolites. These can be divided into low molecular weight molecules which effectively lower surface and interfacial tensions, and high molecular weight polymers which bond firmly to surfaces. Some bioemulsifiers promote the growth of bacteria on hydrophobic substrates insoluble in water by increasing their bioavailability, increasing their surface, desorbing them from surfaces and increasing their solubility. Biosurfactants have an
amphiphilic nature, which allows the microorganisms that produce them to exploit hydrophobic substrates, allowing motility, avoiding competitors. The hydrophobic part usually comprises
saturated or
unsaturated fatty acids, fatty hydroxy acids or fatty
alcohols with a chain length between 8 and 18 carbon atoms. The hydrophilic components consist either of small
hydroxyl,
phosphate or
carboxylic groups, or of portions of
carbohydrates or
peptides. Biosurfactants are predominantly
anionic and
non-ionic compounds. •
Nutritional requirements for growth: The HCB also need large amounts of nitrogen and phosphorus. It has been estimated that 150 g of nitrogen and 30 g of phosphorus are required for 1 kg of oxidized hydrocarbon. •
pH and oxygen: Bacteria require a neutral pH, and in this the same oil can help neutralize environments that are too acidic for microbial growth. Oxygen is critical for aerobic degradation. == Ecology ==