Sediment and pore water samples from all drill sites of International Ocean Discovery Program (IODP) Expedition 385 were analyzed quantitatively for aliphatic hydrocarbons, petroleum (C9–C44) hydrocarbons, and aromatic and polyaromatic compounds. All hydrocarbon classes showed concentration peaks in deep, hot sediments just above and below deeply buried sills (Sites U1545 and U1546), indicating that they were formed by thermal maturation of buried organic matter in the thermal aureole of sill intrusion and have, to a large extent, remained in situ. Plotting hydrocarbon concentrations against in situ temperature shows a pronounced increase in concentration between 65° and 80°C, the thermal limit of hydrocarbon-degrading microbial populations. A smaller hydrocarbon maximum is associated with surficial sediments: within the upper 4 m of the sediment column, the concentrations of total saturated hydrocarbons and of total petroleum hydrocarbons were almost always higher compared to the next sediment samples in downhole sequence, compatible with biogenic hydrocarbon input that reaches all drill sites in Guaymas Basin. The U-shaped hydrocarbon profiles suggest a biological filter that degrades surficial hydrocarbon input and deeply sourced hydrocarbons as soon as the temperature regime in gradually cooling, slowly accumulating sediments permits microbial activity.
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Microbial production and consumption of hydrocarbons in the global ocean
Seeps, spills and other oil pollution introduce hydrocarbons into the ocean. Marine cyanobacteria also produce hydrocarbons from fatty acids, but little is known about the size and turnover of this cyanobacterial hydrocarbon cycle. We report that cyanobacteria in an oligotrophic gyre mainly produce n-pentadecane and that microbial hydrocarbon production exhibits stratification and diel cycling in the sunlit surface ocean. Using chemical and isotopic tracing we find that pentadecane production mainly occurs in the lower euphotic zone. Using a multifaceted approach, we estimate that the global flux of cyanobacteria-produced pentadecane exceeds total oil input in the ocean by 100- to 500-fold. We show that rapid pentadecane consumption sustains a population of pentadecane-degrading bacteria, and possibly archaea. Our findings characterize a microbial hydrocarbon cycle in the open ocean that dwarfs oil input. We hypothesize that cyanobacterial hydrocarbon production selectively primes the ocean’s microbiome with long-chain alkanes whereas degradation of other petroleum hydrocarbons is controlled by factors including proximity to petroleum seepage.
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- Award ID(s):
- 1634478
- PAR ID:
- 10231175
- Date Published:
- Journal Name:
- Nature microbiology
- Volume:
- 6
- ISSN:
- 2058-5276
- Page Range / eLocation ID:
- 489–49
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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