Evidence map›Paper›PMID 37976260›Full record

ArticleProceedings of the National Academy of Sciences of the United States of America2023

Industrial-era decline in Arctic methanesulfonic acid is offset by increased biogenic sulfate aerosol.

Ursula A Jongebloed, Andrew J Schauer, Jihong Cole-Dai, Carleigh G Larrick, William C Porter, Linia Tashmim, Shuting Zhai, Sara Salimi, Shana R Edouard, Lei Geng and 1 more

Open access · greenAbstract read
In one paragraph

Article in Proceedings of the National Academy of Sciences of the United States of America, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
1.5field-weighted citation impact, top 19% 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

1 citing paper in PubMed, 7 citations in OpenAlex.

  1. Climate warming increases global oceanic dimethyl sulfide emissions.Proceedings of the National Academy of Sciences of the United States of America · 2025
    Article
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 2 countries.

Ursula A JongebloedDepartment of Atmospheric Sciences, University of Washington, Seattle, WA 98195.ORCID 0000-0002-9482-4857
Andrew J SchauerDepartment of Earth and Space Sciences, University of Washington, Seattle, WA 98195.ORCID 0000-0002-5941-5396
Jihong Cole-DaiDepartment of Chemistry and Biochemistry, South Dakota State University, Brookings, SD 57007.ORCID 0000-0003-0921-5916
Carleigh G LarrickDepartment of Chemistry and Biochemistry, South Dakota State University, Brookings, SD 57007.
William C PorterDepartment of Environmental Science, University of California, Riverside, CA 92521.
Linia TashmimDepartment of Environmental Science, University of California, Riverside, CA 92521.ORCID 0009-0009-3236-8073
Shuting ZhaiDepartment of Atmospheric Sciences, University of Washington, Seattle, WA 98195.ORCID 0000-0003-1557-3672
Sara SalimiDepartment of Atmospheric Sciences, University of Washington, Seattle, WA 98195.
Shana R EdouardDepartment of Atmospheric Sciences, University of Washington, Seattle, WA 98195.
Lei GengDeep Space Exploration Laboratory, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, China 230052.ORCID 0000-0003-2175-2538
Becky AlexanderDepartment of Atmospheric Sciences, University of Washington, Seattle, WA 98195.
University of Washington · USSouth Dakota State University · USUniversity of California, Riverside · USUniversity of Science and Technology of China · CN

Funding

MOST | National Natural Science Foundation of China (NSFC) 41822605MOST | National Natural Science Foundation of China (NSFC) 41871051National Science Foundation (NSF) 2155192National Science Foundation (NSF) AGS 1702266National Science Foundation (NSF) PLR 0612461National Science Foundation (NSF) PLR 1904128National Science Foundation (NSF) PLR 1904142National Science Foundation (NSF) PLR 2230351National Science Foundation (NSF) PLR 629363
6 · The paper itself

Abstract

Marine phytoplankton are primary producers in ocean ecosystems and emit dimethyl sulfide (DMS) into the atmosphere. DMS emissions are the largest biological source of atmospheric sulfur and are one of the largest uncertainties in global climate modeling. DMS is oxidized to methanesulfonic acid (MSA), sulfur dioxide, and hydroperoxymethyl thioformate, all of which can be oxidized to sulfate. Ice core records of MSA are used to investigate past DMS emissions but rely on the implicit assumption that the relative yield of oxidation products from DMS remains constant. However, this assumption is uncertain because there are no long-term records that compare MSA to other DMS oxidation products. Here, we share the first long-term record of both MSA and DMS-derived biogenic sulfate concentration in Greenland ice core samples from 1200 to 2006 CE. While MSA declines on average by 0.2 µg S kg

Indexed as

dimethyl sulfideice corephytoplanktonprimary productivitysulfate

Identifiers

PMID37976260
PMCPMC10666112
OpenAlexW4388759847

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
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.