Evidence map›Paper›PMID 26693204›Full record

ArticleGlobal biogeochemical cycles2015

Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia.

Birgit Wild, Jörg Schnecker, Anna Knoltsch, Mounir Takriti, Maria Mooshammer, Norman Gentsch, Robert Mikutta, Ricardo J Eloy Alves, Antje Gittel, Nikolay Lashchinskiy and 1 more

Open access · hybridAbstract read
In one paragraph

Article in Global biogeochemical cycles, 2015. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.

0numbers the graph read from it
0cells of the map it votes in
9citing papers in PubMed
5.4field-weighted citation impact, top 4% of its field
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

9 citing papers in PubMed, 132 citations in OpenAlex.

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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

11 authors at 4 institutions in 6 countries.

Birgit WildDepartment of Microbiology and Ecosystem Science, University of Vienna Vienna, Austria ; Austrian Polar Research Institute Vienna, Austria ; Department of Earth Sciences, University of Gothenburg Gothenburg, Sweden.
Jörg SchneckerDepartment of Microbiology and Ecosystem Science, University of Vienna Vienna, Austria ; Austrian Polar Research Institute Vienna, Austria.
Anna KnoltschDepartment of Microbiology and Ecosystem Science, University of Vienna Vienna, Austria ; Austrian Polar Research Institute Vienna, Austria.
Mounir TakritiDepartment of Microbiology and Ecosystem Science, University of Vienna Vienna, Austria ; Austrian Polar Research Institute Vienna, Austria.
Maria MooshammerDepartment of Microbiology and Ecosystem Science, University of Vienna Vienna, Austria.
Norman GentschInstitute of Soil Science, Leibniz Universität Hannover Hannover, Germany.
Robert MikuttaInstitute of Soil Science, Leibniz Universität Hannover Hannover, Germany.
Ricardo J Eloy AlvesAustrian Polar Research Institute Vienna, Austria ; Department of Ecogenomics and Systems Biology, University of Vienna Vienna, Austria.
Antje GittelDepartment of Biology, Centre for Geobiology, University of Bergen Bergen, Norway ; Department of Bioscience, Center for Geomicrobiology Aarhus, Denmark.
Nikolay LashchinskiyCentral Siberian Botanical Garden, Siberian Branch of Russian Academy of Sciences Novosibirsk, Russia.
Andreas RichterDepartment of Microbiology and Ecosystem Science, University of Vienna Vienna, Austria ; Austrian Polar Research Institute Vienna, Austria.
University of Vienna · ATLeibniz University Hannover · DEAarhus University · DKCentral Siberian Botanical Garden · RU

Funding

Austrian Science Fund FWF I 370
6 · The paper itself

Abstract

Soil N availability is constrained by the breakdown of N-containing polymers such as proteins to oligopeptides and amino acids that can be taken up by plants and microorganisms. Excess N is released from microbial cells as ammonium (N mineralization), which in turn can serve as substrate for nitrification. According to stoichiometric theory, N mineralization and nitrification are expected to increase in relation to protein depolymerization with decreasing N limitation, and thus from higher to lower latitudes and from topsoils to subsoils. To test these hypotheses, we compared gross rates of protein depolymerization, N mineralization and nitrification (determined using KEY POINTS: We compared soil N dynamics of seven ecosystems along a latitudinal transectShifts in N dynamics suggest a decrease in microbial N limitation with depthWe found no decrease in microbial N limitation from arctic to temperate zones.

Indexed as

boreal forestpermafrostprotein depolymerizationtundra

Identifiers

PMID26693204
PMCPMC4676305
OpenAlexW2127854785

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

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.