Molecular complexity and diversity of persistent soil organic matter
dc.contributor.author | Jones, AR | en_AU |
dc.contributor.author | Dalal, RC | en_AU |
dc.contributor.author | Gupta, VVSR | en_AU |
dc.contributor.author | Schmidt, S | en_AU |
dc.contributor.author | Allen, DE | en_AU |
dc.contributor.author | Jacobsen, GE | en_AU |
dc.contributor.author | Bird, MI | en_AU |
dc.contributor.author | Grandy, AS | en_AU |
dc.contributor.author | Sanderman, J | en_AU |
dc.date.accessioned | 2023-12-21T23:30:06Z | en_AU |
dc.date.available | 2023-12-21T23:30:06Z | en_AU |
dc.date.issued | 2023-09 | en_AU |
dc.date.statistics | 2023-06-23 | en_AU |
dc.description.abstract | Managing and increasing organic matter in soil requires greater understanding of the mechanisms driving its persistence through resistance to microbial decomposition. Conflicting evidence exists for whether persistent soil organic matter (SOM) is molecularly complex and diverse. As such, this study used a novel application of graph networks with pyrolysis-gas chromatography-mass spectrometry to quantify the complexity and diversity of persistent SOM, defined as SOM that persists through time (soil radiocarbon age) and soil depth. We analyzed soils from the Cooloola giant podzol chronosequence across a large gradient of soil depths (0–15 m) and SOM radiocarbon ages (modern to 19,000 years BP). We found that the most persistent SOM on this gradient was highly aromatic and had the lowest molecular complexity and diversity. By contrast, fresh surface SOM had higher molecular complexity and diversity, with high contributions of plant-derived lignins and polysaccharides. These findings indicate that persisting SOM declines in molecular complexity and diversity over geological timescales and soil depths, with aromatic SOM compounds persisting longer with mineral association. © 2023 Elsevier Ltd | en_AU |
dc.description.sponsorship | We thank the DES Soil and Chemistry Centre at Ecosciences Precinct, Brisbane, for their support, CSIRO National Soil Archive, Canberra, for use of their samples, and Alexander Burridge for producing illustrations. We are grateful to Jan Skjemstad, Rob Fitzpatrick, Fred Oudyn, and Klaus Kaiser for insightful discussions on the topic matter and Thomas Orton for statistical assistance. This works was supported by CSIRO and AINSE postgraduate research scholarships (PGRA ALNSTU11910) to Andrew Jones, and ANSTO research grants #11007 and #11853 for radiocarbon dating. We acknowledge the financial support from the Australian Government for the Centre for Accelerator Science at ANSTO through the National Collaborative Research Infrastructure Strategy (NCRIS). | en_AU |
dc.identifier.articlenumber | 109061 | en_AU |
dc.identifier.citation | Jones, A. R., Dalal, R. C., Gupta, V. V. S. R., Schmidt, S., Allen, D. E., Jacobsen, G. E., Bird, M., Grandy, A. S., & Sanderman, J. (2023). Molecular complexity and diversity of persistent soil organic matter. Soil Biology and Biochemistry, 184, 109061. doi:10.1016/j.soilbio.2023.109061 | en_AU |
dc.identifier.issn | 0038-0717 | en_AU |
dc.identifier.journaltitle | Soil Biology and Biochemistry | en_AU |
dc.identifier.uri | https://apo.ansto.gov.au/handle/10238/15298 | en_AU |
dc.identifier.volume | 184 | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | Elseiver B. V. | en_AU |
dc.relation.uri | https://doi.org/https://doi.org/10.1016/j.soilbio.2023.109061 | en_AU |
dc.subject | Soils | en_AU |
dc.subject | Organic matter | en_AU |
dc.subject | Decomposition | en_AU |
dc.subject | Gas chromatography | en_AU |
dc.subject | Mass spectroscopy | en_AU |
dc.subject | Lignin | en_AU |
dc.subject | Minerals | en_AU |
dc.title | Molecular complexity and diversity of persistent soil organic matter | en_AU |
dc.type | Journal Article | en_AU |
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