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Anaerobic microsites have an unaccounted role in soil carbon stabilization

2017· article· en· 519 citations· W2768500565 on OpenAlex· 10.1038/s41467-017-01406-6

Why is this work in the frame?

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

Canadian funderA Canadian agency funded it. The work may carry no Canadian affiliation at all.

No Canadian affiliation. An affiliation-only frame — the usual design — would never have seen this work. It is one of the works that make the case for inverting the frame.

Machine scores (provisional)

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Opus teacher head0.019
GPT teacher head0.275
Teacher spread
0.256 · how far apart the two teachers sit on this one work
Validation status
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Abstract

Soils represent the largest carbon reservoir within terrestrial ecosystems. The mechanisms controlling the amount of carbon stored and its feedback to the climate system, however, remain poorly resolved. Global carbon models assume that carbon cycling in upland soils is entirely driven by aerobic respiration; the impact of anaerobic microsites prevalent even within well-drained soils is missed within this conception. Here, we show that anaerobic microsites are important regulators of soil carbon persistence, shifting microbial metabolism to less efficient anaerobic respiration, and selectively protecting otherwise bioavailable, reduced organic compounds such as lipids and waxes from decomposition. Further, shifting from anaerobic to aerobic conditions leads to a 10-fold increase in volume-specific mineralization rate, illustrating the sensitivity of anaerobically protected carbon to disturbance. The vulnerability of anaerobically protected carbon to future climate or land use change thus constitutes a yet unrecognized soil carbon-climate feedback that should be incorporated into terrestrial ecosystem models.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

The record

Venue
Nature Communications
Topic
Soil Carbon and Nitrogen Dynamics
Field
Agricultural and Biological Sciences
Canadian institutions
Funders
Pacific Northwest National LaboratoryNational Research Council CanadaWestern Economic Diversification CanadaBiological and Environmental ResearchNatural Sciences and Engineering Research Council of CanadaCanadian Institutes of Health ResearchOffice of ScienceUniversity of SaskatchewanCanadian Light SourceU.S. Department of Energy
Keywords
Environmental scienceCarbon cycleSoil carbonEcosystemAnaerobic exerciseMineralization (soil science)Soil respirationAnaerobic respirationSoil waterEcologyCarbon fibersEnvironmental chemistryChemistrySoil scienceBiology
Has abstract in OpenAlex
yes