Evidence map›Paper›PMID 31312015›Full record

ArticleScientific reports2019

Microbial and abiotic controls on mineral-associated organic matter in soil profiles along an ecosystem gradient.

Robert Mikutta, Stephanie Turner, Axel Schippers, Norman Gentsch, Sandra Meyer-Stüve, Leo M Condron, Duane A Peltzer, Sarah J Richardson, Andre Eger, Günter Hempel and 3 more

Abstract read
In one paragraph

Article in Scientific reports, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 13 papers.

0numbers the graph read from it
0cells of the map it votes in
13citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

13 citing papers in PubMed.

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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

13 authors.

Robert MikuttaSoil Science and Soil Protection, Martin Luther University Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120, Halle (Saale), Germany. robert.mikutta@landw.uni-halle.de.ORCID http://orcid.org/0000-0002-7186-6528
Stephanie TurnerBundesanstalt für Geowissenschaften und Rohstoffe, Stilleweg 2, 30655, Hannover, Germany.
Axel SchippersBundesanstalt für Geowissenschaften und Rohstoffe, Stilleweg 2, 30655, Hannover, Germany.
Norman GentschLeibniz Universität Hannover, Institut für Bodenkunde, Herrenhäuser Str. 2, 30419, Hannover, Germany.
Sandra Meyer-StüveLeibniz Universität Hannover, Institut für Bodenkunde, Herrenhäuser Str. 2, 30419, Hannover, Germany.
Leo M CondronAgriculture and Life Sciences, Lincoln University, PO Box 85084, Lincoln, 7647, Christchurch, New Zealand.
Duane A PeltzerLandcare Research, PO Box 40, Lincoln, 7640, Canterbury, New Zealand.
Sarah J RichardsonLandcare Research, PO Box 40, Lincoln, 7640, Canterbury, New Zealand.
Andre EgerLandcare Research, PO Box 40, Lincoln, 7640, Canterbury, New Zealand.
Günter HempelInstitute of Physics, Martin Luther University Halle-Wittenberg, Betty-Heimann-Str. 7, 06120, Halle (Saale), Germany.
Klaus KaiserSoil Science and Soil Protection, Martin Luther University Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120, Halle (Saale), Germany.ORCID http://orcid.org/0000-0001-7376-443X
Thimo KlotzbücherSoil Science and Soil Protection, Martin Luther University Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120, Halle (Saale), Germany.
Georg GuggenbergerLeibniz Universität Hannover, Institut für Bodenkunde, Herrenhäuser Str. 2, 30419, Hannover, Germany.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Formation of mineral-organic associations is a key process in the global carbon cycle. Recent concepts propose litter quality-controlled microbial assimilation and direct sorption processes as main factors in transferring carbon from plant litter into mineral-organic associations. We explored the pathways of the formation of mineral-associated organic matter (MOM) in soil profiles along a 120-ky ecosystem gradient that developed under humid climate from the retreating Franz Josef Glacier in New Zealand. We determined the stocks of particulate and mineral-associated carbon, the isotope signature and microbial decomposability of organic matter, and plant and microbial biomarkers (lignin phenols, amino sugars and acids) in MOM. Results revealed that litter quality had little effect on the accumulation of mineral-associated carbon and that plant-derived carbon bypassed microbial assimilation at all soil depths. Seemingly, MOM forms by sorption of microbial as well as plant-derived compounds to minerals. The MOM in carbon-saturated topsoil was characterized by the steady exchange of older for recent carbon, while subsoil MOM arises from retention of organic matter transported with percolating water. Overall, MOM formation is not monocausal but involves various mechanisms and processes, with reactive minerals being effective filters capable of erasing chemical differences in organic matter inputs.

Identifiers

PMID31312015
PMCPMC6635608

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.