Oil in the Sea IV: Inputs, Fates, and Effects (2022)

Chapter: Appendix I: Table of Common Hydrocarbon Degraders

Previous Chapter: Appendix H: Omics Techniques
Suggested Citation: "Appendix I: Table of Common Hydrocarbon Degraders." National Academies of Sciences, Engineering, and Medicine. 2022. Oil in the Sea IV: Inputs, Fates, and Effects. Washington, DC: The National Academies Press. doi: 10.17226/26410.

Appendix I

Table of Common Hydrocarbon Degraders

TABLE I.1 Some Commonly Detected Marine Hydrocarbon-Degrading Bacteria (Aerobic Degraders Unless Otherwise Indicated)

Preferred Substrate(s) Organism Name Typical Marine Environment Comments Selected Citations
ALIPHATICS
Methane Methylomonas spp. Natural gas seeps Obligate methanotroph. Enriched in Deepwater Horizon plume during methane depletion Dubinsky et al., 2013
n-Alkanes C9–C32; iso-alkanes (e.g., isoprenoids); alkyl components of alkyl-cycloalkanes and alkyl aromatics Alcanivorax borkumensis Ubiquitous in marine ecosystems (water, sediment, coastal, deep sea); rare in pristine waters; DNA detected in polar areas but only isolated from more temperate environments Obligate hydrocarbonoclastic species; produces biosurfactants, forms emulsions; early responder; widespread; found in partnership with marine invertebrates; often early to bloom in response to oil Yakimov et al., 1998, 2007; Dutta and Harayama, 2001; Gregson et al., 2019; Joye and Kostka 2020; Van Landuyt et al., 2020
Methane and liquid alkanes Candidatus Macondimonas diazotrophica Oil-contaminated marine sediments worldwide Bloomed in Gulf of Mexico after Deepwater Horizon to 30% of total sediment microbes; N2 fixer Karthikeyan et al., 2019
Gaseous and liquid n-alkanes; cycloalkanes Order Oceanospirillales: Oceanospirillum Oceaniserpentilla Bermanella Cold marine waters Various genera dominant during Deepwater Horizon spill; genes for mono-aromatic and PAH degradation detected but expressed poorly Mason et al., 2012; Kleindienst et al., 2016; Hu et al., 2017
Alkanes Oleibacter spp. Temperate water; deep water (Mariana Trench) Only one species has been cultivated; others detected using ‘omics Lofthus et al., 2018; Liu et al., 2019; Schreiber et al., 2021
Alkanes Oleiphilus messinensis Sponge symbiont Obligate hydrocarbonoclastic species Golyshin et al., 2002; Yakimov et al., 2007
Alkanes Oleispira antarctica Cold water and high latitudes; sea ice Psychrophilic; may also degrade Corexit 9500A components Yakimov et al., 2003; Kube et al., 2013; Boccadoro et al., 2018; Lofthus et al., 2018; McFarlin et al., 2018
>C16 n-alkanes; Isoprenoids (e.g., squalane) n-Alkanes Alkanindiges illinoisensis Few reports in marine systems; Arctic beach, marine biofilms Obligate hydrocarbonoclastic species Røberg et al., 2011; Vergeynst et al., 2019a
Thalassolituus oleivorans Marine waters and sediments Obligate hydrocarbonoclastic species; particularly associated with cold oil biodegradation; degrades nC10nC32 but not pristane Yakimov et al., 2004 Brakstad et al. 2015b; Gregson et al., 2018; Shtratnikova et al., 2018
n-Alkanes Halomonas neptunia Halomonas titanicae Cold marine (deep sea and Antarctic surface water) Produces bio-emulsifier when growing on hydrocarbon Pepi et al., 2005; Van Landuyt et al., 2020
Suggested Citation: "Appendix I: Table of Common Hydrocarbon Degraders." National Academies of Sciences, Engineering, and Medicine. 2022. Oil in the Sea IV: Inputs, Fates, and Effects. Washington, DC: The National Academies Press. doi: 10.17226/26410.
Preferred Substrate(s) Organism Name Typical Marine Environment Comments Selected Citations
n-Alkanes Zhongshania spp. Cold marine water Early responder in cold seawater, possibly specializing in short- to medium-chain alkanes Ribicic et al., 2018; Murphy et al., 2021
n-Alkanes Paraperlucidibaca Cold marine water Metagenome detected in sub-Arctic marine sediments incubated with diesel or crude oil Murphy et al., 2021
n-Alkanes Desulfosarcina/Desulfococcus clade Marine seeps Anaerobic degradation via sulfate reduction Kleindienst et al., 2014
AROMATICS WITH OR WITHOUT ALIPHATICS
Aromatics including PAHs and PACs; also ethane, propane, butane Cycloclasticus spp. Global distribution Obligate hydrocarbonoclastic bacterial genus; associated with dilbit degradation by ‘omics Kasai et al., 2002; Yakimov et al., 2007; Brakstad et al. 2015b; Messina et al., 2016; Rubin-Blum et al., 2017; Gutierrez et al., 2018; Murphy et al., 2021; Schreiber et al., 2021
PAH and long-chain alkanes Marinobacter spp. Ubiquitous Form biofilms and produce emulsifiers; tolerates high salt concentrations Gauthier et al., 1992; Yakimov et al., 2007; Brakstad et al. 2015b Laio et al., 2015; Murphy et al., 2021
PAH and various alkanes Pseudoalteromonas Global distribution; versatile heterotroph Enriched in cold North Sea water microcosms with oil Chronopoulou et al., 2015
Short-chain alkanes (C2–C4), benzene, PAHs Colwellia spp. Global distribution, but certain strains are adapted to cold marine water and sea ice; also detected in deep sea sediments Associated with marine oil snow; possibly sensitive to hydrostatic pressure; may metabolize dispersant components Bælum et al. 2012; Redmond and Valentine, 2012; Dubinsky et al., 2013; Mason et al., 2014a,b; Brakstad et al., 2015b; Barbato and Scoma, 2020
PAH Dietzia spp. Arctic seafloor sediments; Antarctic sediments Predominant sequence in 16S marker gene survey; degrades phenanthrene and emulsifies diesel Dong et al., 2015; Ausuri et al., 2021

NOTE: A more comprehensive list of hydrocarbon-degrading prokaryotes, including from terrestrial and freshwater sources, has been prepared by Prince et al. (2018).

Suggested Citation: "Appendix I: Table of Common Hydrocarbon Degraders." National Academies of Sciences, Engineering, and Medicine. 2022. Oil in the Sea IV: Inputs, Fates, and Effects. Washington, DC: The National Academies Press. doi: 10.17226/26410.
Page 491
Suggested Citation: "Appendix I: Table of Common Hydrocarbon Degraders." National Academies of Sciences, Engineering, and Medicine. 2022. Oil in the Sea IV: Inputs, Fates, and Effects. Washington, DC: The National Academies Press. doi: 10.17226/26410.
Page 492
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