Evidence map›Paper›PMID 34706120›Full record

ArticleGlobal change biology2022

Shifting stoichiometry: Long-term trends in stream-dissolved organic matter reveal altered C:N ratios due to history of atmospheric acid deposition.

Bianca M Rodríguez-Cardona, Adam S Wymore, Alba Argerich, Rebecca T Barnes, Susana Bernal, E N Jack Brookshire, Ashley A Coble, Walter K Dodds, Hannah M Fazekas, Ashley M Helton and 8 more

Open access · hybridAbstract read
In one paragraph

Article in Global change biology, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.

0numbers the graph read from it
0cells of the map it votes in
4citing papers in PubMed
3.5field-weighted citation impact, top 7% 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

4 citing papers in PubMed, 47 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

18 authors at 15 institutions in 5 countries.

Bianca M Rodríguez-CardonaDepartment of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire, USA.ORCID 0000-0002-4792-7351
Adam S WymoreDepartment of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire, USA.ORCID 0000-0002-6725-916X
Alba ArgerichSchool of Natural Resources, University of Missouri, Columbia, Missouri, USA.ORCID 0000-0001-6430-0449
Rebecca T BarnesEnvironmental Studies Program, Colorado College, Colorado Springs, Colorado, USA.ORCID 0000-0001-6385-1062
Susana BernalCentre d'Estudis Avançats de Blanes (CEAB-CSIC), Blanes, Spain.ORCID 0000-0002-6726-8840
E N Jack BrookshireDepartment of Land Resources and Environmental Sciences, Montana State University, Bozeman, Montana, USA.ORCID 0000-0002-0412-7696
Ashley A CobleNational Council for Air and Stream Improvement, Inc., Corvallis, Oregon, USA.ORCID 0000-0002-5821-5026
Walter K DoddsDivision of Biology, Kansas State University, Manhattan, Kansas, USA.ORCID 0000-0002-6666-8930
Hannah M FazekasDepartment of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire, USA.ORCID 0000-0001-5651-6100
Ashley M HeltonDepartment of Natural Resources and the Environment, and the Center for Environmental Sciences and Engineering, University of Connecticut, Storrs, Connecticut, USA.ORCID 0000-0001-6928-2104
Penny J JohnesSchool of Geographical Sciences, University of Bristol, Bristol, UK.ORCID 0000-0003-1605-6896
Sherri L JohnsonUSDA Forest Service, Pacific Northwest Research Station, Corvallis, Oregon, USA.ORCID 0000-0002-4223-3465
Jeremy B JonesInstitute of Arctic Biology & Department of Biology and Wildlife, University of Alaska Fairbanks, Fairbanks, Alaska, USA.ORCID 0000-0003-3540-1392
Sujay S KaushalDepartment of Geology, University of Maryland, College Park, Maryland, USA.
Pirkko KortelainenFinnish Environment Institute, Helsinki, Finland.ORCID 0000-0002-1448-0688
Carla López-LloredaDepartment of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire, USA.ORCID 0000-0002-7983-1741
Robert G M SpencerDepartment of Earth, Ocean and Atmospheric Sciences, Florida State University, Tallahassee, Florida, USA.ORCID 0000-0003-0777-0748
William H McDowellDepartment of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire, USA.ORCID 0000-0002-8739-9047
University of New Hampshire · USCentre d'Estudis Avançats de Blanes · ESColorado College · USFinnish Environment Institute · FIFlorida State University · USKansas State University · USMontana State University · USNational Council for Air and Stream Improvement · USPacific Northwest Research Station · USUniversité du Québec à Montréal · CAUniversity of Alaska Fairbanks · USUniversity of Bristol · GBUniversity of Connecticut · USUniversity of Maryland, College Park · USUniversity of Missouri · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Dissolved organic carbon (DOC) and nitrogen (DON) are important energy and nutrient sources for aquatic ecosystems. In many northern temperate, freshwater systems DOC has increased in the past 50 years. Less is known about how changes in DOC may vary across latitudes, and whether changes in DON track those of DOC. Here, we present long-term DOC and DON data from 74 streams distributed across seven sites in biomes ranging from the tropics to northern boreal forests with varying histories of atmospheric acid deposition. For each stream, we examined the temporal trends of DOC and DON concentrations and DOC:DON molar ratios. While some sites displayed consistent positive or negative trends in stream DOC and DON concentrations, changes in direction or magnitude were inconsistent at regional or local scales. DON trends did not always track those of DOC, though DOC:DON ratios increased over time for ~30% of streams. Our results indicate that the dissolved organic matter (DOM) pool is experiencing fundamental changes due to the recovery from atmospheric acid deposition. Changes in DOC:DON stoichiometry point to a shifting energy-nutrient balance in many aquatic ecosystems. Sustained changes in the character of DOM can have major implications for stream metabolism, biogeochemical processes, food webs, and drinking water quality (including disinfection by-products). Understanding regional and global variation in DOC and DON concentrations is important for developing realistic models and watershed management protocols to effectively target mitigation efforts aimed at bringing DOM flux and nutrient enrichment under control.

Indexed as

Dissolved Organic MatterRiversCarbonEcosystemNitrogenCarbonDissolved Organic MatterNitrogenatmospheric acid depositionC:N stoichiometrydissolved organic carbondissolved organic matterdissolved organic nitrogenlong-term trendsstreams

Identifiers

PMID34706120
PMCPMC9297910
OpenAlexW3210579479

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.