Microbial alteration of normal alkane δ13C and δD in sedimentary archives

Long-carbon chain normal alkanes (e.g. C25-C33) are produced by a wide range of terrestrial plants and commonly preserved in ancient sediments. These serve as a potential paleoclimate proxy because their hydrogen (δD) and carbon (δ13C) isotope values reflect the combined effect of plant-specific species effects and responses to environmental conditions. While these are commonly believed to remain unaltered at low burial temperatures (e.g. <150°C), there is still uncertainty around the role microbes play during the breakdown of these compounds in stored sediment and the potential risk for isotopic alteration. We analyzed two sets of identical samples to assess the role of microbial and other degradation process on the hydrogen and carbon isotope composition of these compounds. The first set of sediment samples were collected in the summer of 2011 from central Armenia, a region with continental climate, and allowed to sit in sealed bags at room temperature for three years. A second and identical set was collected in 2014 and frozen immediately. Stored samples showed high amounts of medium chain length n-alkanes (C19-C26), produced by microorganisms, which were absent from the samples that were collected in 2014 and frozen immediately after sampling. Along with the presence of medium chain length n-alkanes, the average chain length of n-alkanes from C25-C33 decreased significantly in all 2011 samples. Storage of the samples over three years resulted in altered δD and δ13C values of C29 and C31 n-alkanes. While δD values were heavier relative to the control by 4-25‰, δ13C values were mostly lighter (maximum change of -4.2‰ in C29 and -2.9‰ in C31). DNA analysis of the soil showed Rhodococcus and Aeromicrobium, genera that contain multiple coding regions for alkane degrading enzymes CYP153 and AlkB, increased by an order of magnitude during sample storage (from 0.7% to 7.5% of bacteria present). The proliferation of alkane degrading bacteria, combined with the large changes of long-chain n-alkane isotope values, suggest that bacteria may play a larger role than previously expected in altering the measured δD and δ13C values of long-chain n-alkanes during storage. This poses a potentially significant issue for all manner of samples that are not stored frozen, including a variety of sedimentary cores.