Example:10.1021/acsami.1c06204 or Chem. Rev., 2007, 107, 2411-2502
Transformation of n-alkanes from plant to soil: a review Soil (IF5.841), Pub Date : 2021-11-25, DOI: 10.5194/soil-7-785-2021 Carrie L. Thomas, Boris Jansen, E. Emiel van Loon, Guido L. B. Wiesenberg
Despite the importance of soil organic matter (SOM) in
the global carbon cycle, there remain many open questions regarding its
formation and preservation. The study of individual organic compound classes
that make up SOM, such as lipid biomarkers including n-alkanes, can provide
insight into the cycling of bulk SOM. While studies of lipid biomarkers,
particularly n-alkanes, have increased in number in the past few decades,
only a limited number have focused on the transformation of these compounds
following deposition in soil archives. We performed a systematic review to
consolidate the available information on plant-derived n-alkanes and their
transformation from plant to soil. Our major findings were (1) a nearly
ubiquitous trend of decreased total concentration of n-alkanes either with
time in litterbag experiments or with depth in open plant–soil systems and (2) preferential degradation of odd-chain length and shorter chain length n-alkanes represented by a decrease in either carbon preference index (CPI) or odd-over-even predominance (OEP) with depth, indicating degradation of
the n-alkane signal or a shift in vegetation composition over time. The
review also highlighted a lack of data transparency and standardization
across studies of lipid biomarkers, making analysis and synthesis of
published data time-consuming and difficult. We recommend that the community
move towards more uniform and systematic reporting of biomarker data.
Furthermore, as the number of studies examining the complete
leaf–litter–soil continuum is very limited as well as unevenly distributed over geographical regions, climate zones, and soil types, future data collection should focus on underrepresented areas as well as quantifying the
transformation of n-alkanes through the complete continuum from plant to soil.