Oil spills

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Introduction

Electron micrograph of the Ebola Zaire virus. This was the first photo ever taken of the virus, on 10/13/1976. By Dr. F.A. Murphy, now at U.C. Davis, then at the CDC.

As the demand for crude oil as energy source is fast increasing, accidental and associated oil spills have been more and more frequent during the process of exploration, production, transportation and storage. On land, oil spills are usually localized and the impact is limited in a certain area. However, when oil spills happened in marine it may result in very serious ecological risks and long-term environmental disturbance (Patin 2004, 737-748). The primary source of oil input into seas is usually associated with transportation by tankers and pipelines.

Once the oil spill happened, the oil will experience a series of physical, chemical and biological change, the effect of which is overall defined as “weathering”. However, this process happened in a limited speed in the natural environment and need long time for the contaminated environment to recover. Various remediation methods have been proposed, among which the biological remediation has drawn increasing attention recently. There are two general approaches: to apply fertilizers or surfactants in order to promote the microbial degradation process, and to add naturally occurring adapted microbial hydrocarbon degraders seeding (Mulkinsphillips and Stewart 1974, 915-922). The rate of biodegradation in a remediation site is highly dependent on the characteristics of spilled oil, the localized physical chemical environment, as well as the indigenous microbe’s communities. In order to better use bioremediation, lots of research are being conducted, focusing on both the biotic and abiotic factors influencing the degradation rate.

Physical environment

Oil spill can happen everywhere, from arctic to tropical marine, from soil to water, and therefore the physical and chemical environment of oil spill can vary significantly from one to other. Many factors have been proved to influence microbial degradation of petroleum, including physical status of oil spill, temperature, oxygen, nutrients, soil type and characteristics, and vegetation etc.

Physical status of oil spill

Physical status of oil spill is the most important factor determines the environment the petroleum degraders live. The status of oil spill and those environmental factors will have complex interactions and exert mark influence on microbial communities. Generally, there are two kinds of oil spills: Oil spill in water and oil spill in soil. The biggest different between them is the degree of spread. In soil, hydrocarbon is absorbed by plant and soil particles, limiting its spreading. Oil on soil surface will receive relatively ample oxygen which is crucial for biodegradation. Some portion will go deeper into the soil, but still within limited depth. In that situation, when oxygen becomes limiting factor, aeration is needed in order to enhance the bioremediation (PRINCE 1993, 217-242).

In marine environment, there can be a lot of forms oil; each has its own typical environment. Most of the oil normally spreads, forming a thin slick on the top of water body. A large portion of the oil also forms emulsions or dissolve the water. Some heavy portion will settle into to the bottom. The oxygen can be relatively easily obtained in the slick oil spill, but the nutrient sometimes is limited; the dissolved oil or oil emulsion droplets usually have chance to obtain both oxygen and nutrient when they travel through water column; the environment in the sediments is low in oxygen although the nutrient may not be limited. The difference in these environmental factors can create big different in the petroleum degradation process, for example, it was found that the petroleum hydrocarbons would persist for longer periods in reduced sediments than would it do in aerated surface oil layers (Hamnrick, Delaune, and Patrick 1980, 365-369). In addition, the toxic concentration, which is mostly caused by aromatic hydrocarbons, in different biota will also vary within several orders of magnitude. The toxicity has been proven to be crucial factor for biodegradation of petroleum hydrocarbon.

Temperature

The influence of temperature on biodegradation are interactive with other factors, such as the quality of the hydrocarbon mixtures and the composition of the microbial community. First, the temperature affects the physical status of petroleum. Higher temperature will result in higher viscosity, the volatilization of toxic alkanes is reduced, and their water solubility increased, delaying the rate of biodegradations. The second effect is on microbial activity. Higher temperature usually resulted in better activity of enzymes and therefore increased rate of metabolism. Actually, biodegradation activity has been found in almost all environments with extreme temperatures. Biodegradation can occur at very low temperature, e.g. 5 ºC even in arctic zone (Mulkinsphillips and Stewart 1974, 915-922), and tropical area(Teralmoto et al. 2009, 3362-3370). In addition, temperature will affect other environmental parameters that might be crucial to petroleum biodegrading microbes, for example, the availability of liquid water. Atlas (Atlas, Horowitz, and Busdosh 1978, 585-590) found that the petroleum hydrocarbons from Prudhoe Bay crude oil in Arctic marine’s ice ecosystems were degraded extremely slowly mainly because of the unavailability of the liquid water rather than the temperature itself.

Nutrients

Microorganisms require nitrogen and phosphorus for incorporation into biomass and therefore the availability of these nutrients are important for bioremediation. Still, the nutrient availability depends heavily on the physical status of oil spill, whether it is in soil or marine, whether it is in dissolved forms or slick. However, in most study, there seems not to be enough nutrients to carry out best degradation performance. Many researches have reported that the amendment of nutrient can significantly improve the degradation of petroleum pollutants both in water and soil (Xu and Obbard 2004, 861-867; Liang et al. 2011, 403-413; Tyagi, da Fonseca, and de Carvalho 2011, 231-241)

Oxygen

The major degradation pathways for petroleum hydrocarbons involves oxygenates and molecular oxygen, indicating the(Boufadel et al. 2010, 7418-7424) importance of oxygen for oil degradation microbes Template:340 Atlas,Ronald M. 1991. There is indeed anaerobe doing the degradation job, but the rate is significantly lower, for instance, within anoxic basins or sediments, the hypolimnion stratified lakes and benthic sediments, oxygen may severely limit biodegradation. Oxygen consumption by oil-degrading bacteria is high, even in some environment such as the water surface where oxygen is readily available right after the oil spill happens, oxygen may rapidly become limiting factor due to slow oxygen diffusion rates and its limited solubility in water. Since most of the degradation is aerobic processes, maintenance of aerobic conditions is important in the bioremediation. (Atlas 1991, 149-156)

Salinity and pressure

The influence of several other environmental factors on hydrocarbon biodegradation has been studied. Typically these factors are associated with the localized environment features such as saline lakes or deep seas where high hydrostatic pressure exists. Studies have shown that generally the biodegradation rate decrease as the salinity increase. The deep benthic zone in marine has been found to be one of those with least microbial activity, part of which is because of the higher pressure that has limited the microbial activity (Shin and Pardue 2001, 845-854).

Microbial communities

Microbial community composition

A very diverse group and microbes have been showed to have the ability to degrade petroleum hydrocarbons (Atlas 1981, 180-209), among which bacteria and fungi appear to be the prevalent hydrocarbon degraders in oil contaminated ecosystems.

Bacteria and archae

Many bacterial strains have been reported to have the ability to degrade recalcitrant compounds in petroleum. More than 20 genera of hydrocarbon degrading bacteria has been isolated including Alpha-, Beta- and Gammaproteobacteria; Gram positives; Flexibacter–Cytophaga–Bacteroides(Teralmoto et al. 2009, 3362-3370). On the other hand, fast development of molecular microbiological tool has enabled the identification of many un-culturable microbes and therefore extended the list of microbial species with petroleum hydrocarbon degrading abilities. Species of Pseudomonas, Mycobacterium, Haemophilus, Rhodococcus, Paenibacillus and Ralstonia, are some of the most extensively studied bacteria for their bioremediation capability Pseudomonas species is one of the most common species that have been isolated. The genetic information for hydrocarbon degradation has been found to occur on plasmids (Vila et al. 2010, no-362). Archae has also been found in oil comtanmated environment degrading petroleum hydrocarbons(Teralmoto et al. 2009, 3362-3370).

Fungi

Fungi, including yeast and filamentous fungi have also been found to have the ability to degrade petroleum carbon. Species reported include Candida, hodosporidium, Rhodotorula, Saccharomyces, Sporobolomyces, and Trichosporon etc. (Liu et al. 2009, 400-407)(Atlas 1981, 180-209).

Algae and cyanobacteria

Interestingly, the ability to oxidize petroleum hydrocarbons is widely distributed, not only among bacteria and fungi, but also among the cyanobacteria and algae. Oscillatoria spp., Microcoleus sp., Anabaena spp., Agmenellum sp., Cylindretheca sp.,Coccochloris sp., Ulva sp., Nostoc sp., Aphanocapsa sp., Chlorella spp., Dunaliella sp., Chlamydomonas sp., Amphora sp., Porphyridium sp., and Petalonia have all been found to be capable of oxidizing naphthalene(Sadaba and Sarinas 2010, 565-575).

Microbial processes

What microbial processes define this environment? Describe microbial processes that are important in this habitat, adding sections/subsections as needed. Look at other topics in MicrobeWiki. Are some of these processes already described? Create links where relevant.

Current Research

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References

[Sample reference] Takai, K., Sugai, A., Itoh, T., and Horikoshi, K. "Palaeococcus ferrophilus gen. nov., sp. nov., a barophilic, hyperthermophilic archaeon from a deep-sea hydrothermal vent chimney". International Journal of Systematic and Evolutionary Microbiology. 2000. Volume 50. p. 489-500.

Edited by <your name>, a student of Angela Kent at the University of Illinois at Urbana-Champaign.