Evidence map›Paper›PMID 32747679›Full record

ArticleScientific reports2020

Rapid microbial diversification of dissolved organic matter in oceanic surface waters leads to carbon sequestration.

Philipp F Hach, Hannah K Marchant, Andreas Krupke, Thomas Riedel, Dimitri V Meier, Gaute Lavik, Moritz Holtappels, Thorsten Dittmar, Marcel M M Kuypers

Open access · goldAbstract read
In one paragraph

Article in Scientific reports, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 15 papers.

0numbers the graph read from it
0cells of the map it votes in
15citing papers in PubMed
4.3field-weighted citation impact, top 5% 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

15 citing papers in PubMed, 61 citations in OpenAlex.

  1. Decoupled timescales of organic carbon and phosphorus recycling in the global ocean.Proceedings of the National Academy of Sciences of the United States of America · 2026
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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

9 authors at 4 institutions in 1 country.

Philipp F HachMax Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359, Bremen, Germany.
Hannah K MarchantMax Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359, Bremen, Germany.
Andreas KrupkeMax Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359, Bremen, Germany.
Thomas RiedelIWW Water Centre, Moritzstr. 26, 45476, Mülheim an der Ruhr, Germany.
Dimitri V MeierMax Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359, Bremen, Germany.
Gaute LavikMax Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359, Bremen, Germany.
Moritz HoltappelsMax Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359, Bremen, Germany.
Thorsten DittmarResearch Group for Marine Geochemistry (ICBM-MPI Bridging Group), at the Institute for Chemistry and Biology of the Marine Environment (ICBM), University of Oldenburg, Carl-von-Ossietzky-Str. 9-11, 26129, Oldenburg, Germany.
Marcel M M KuypersMax Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359, Bremen, Germany. mkuypers@mpi-bremen.de.
Max Planck Institute for Marine Microbiology · DEAlfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung · DECarl von Ossietzky Universität Oldenburg · DEIWW Water Centre · DE

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The pool of dissolved organic matter (DOM) in the deep ocean represents one of the largest carbon sinks on the planet. In recent years, studies have shown that most of this pool is recalcitrant, because individual compounds are present at low concentrations and because certain compounds seem resistant to microbial degradation. The formation of the diverse and recalcitrant deep ocean DOM pool has been attributed to repeated and successive processing of DOM by microorganisms over time scales of weeks to years. Little is known however, about the transformation and cycling that labile DOM undergoes in the first hours upon its release from phytoplankton. Here we provide direct experimental evidence showing that within hours of labile DOM release, its breakdown and recombination with ambient DOM leads to the formation of a diverse array of new molecules in oligotrophic North Atlantic surface waters. Furthermore, our results reveal a preferential breakdown of N and P containing molecules versus those containing only carbon. Hence, we show the preferential breakdown and molecular diversification are the crucial first steps in the eventual formation of carbon rich DOM that is resistant to microbial remineralization.

Identifiers

PMID32747679
PMCPMC7400608
OpenAlexW3046575927

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.