Evidence map›Paper›PMID 39772680›Full record

ArticleScience advances2025

Role of the stratosphere in the global mercury cycle.

Alfonso Saiz-Lopez, Carlos A Cuevas, A Ulises Acuña, Juan A Añel, Anoop S Mahajan, Laura de la Torre, Wuhu Feng, Juan Z Dávalos, Daniel Roca-Sanjuán, Douglas E Kinnison and 15 more

Abstract read
In one paragraph

Article in Science advances, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.

0numbers the graph read from it
0cells of the map it votes in
6citing 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

6 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

25 authors.

Alfonso Saiz-LopezDepartment of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, CSIC, 28006 Madrid, Spain.ORCID 0000-0002-0060-1581
Carlos A CuevasDepartment of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, CSIC, 28006 Madrid, Spain.ORCID 0000-0002-9251-5460
A Ulises AcuñaDepartment of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, CSIC, 28006 Madrid, Spain.
Juan A AñelDepartment of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, CSIC, 28006 Madrid, Spain.ORCID 0000-0003-2448-4647
Anoop S MahajanCentre for Climate Change Research, Indian Institute of Tropical Meteorology, Ministry of Earth Sciences, Pune 411008, India.ORCID 0000-0002-2909-5432
Laura de la TorreEnvironmental Physics Laboratory (EPhysLab), Centro de Investigación Mariña (CIM-UVIGO), Universidade de Vigo, 32004 Ourense, Spain.ORCID 0000-0001-5305-6946
Wuhu FengSchool of Chemistry, University of Leeds, Leeds, UK.ORCID 0000-0002-9907-9120
Juan Z DávalosDepartment of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, CSIC, 28006 Madrid, Spain.ORCID 0000-0002-5835-6371
Daniel Roca-SanjuánInstitut de Ciencia Molecular, Universitat de Valencia, 46071 Valencia, Spain.ORCID 0000-0001-6495-2770
Douglas E KinnisonNSF National Center for Atmospheric Research (NSF NCAR), Boulder, CO 80301, USA.ORCID 0000-0002-3418-0834
Javier Carmona-GarcíaDepartment of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, CSIC, 28006 Madrid, Spain.ORCID 0000-0001-5359-7240
Rafael P FernandezInstitute for Interdisciplinary Science (ICB), National Research Council (CONICET), FCEN-UNCuyo, Mendoza 5501, Argentina.ORCID 0000-0002-4114-5500
Qinyi LiDepartment of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, CSIC, 28006 Madrid, Spain.ORCID 0000-0002-5146-5831
Jeroen E SonkeGéosciences Environnement Toulouse, CNRS/OMP/Université de Toulouse, 31400 Toulouse, France.ORCID 0000-0001-7146-3035
Aryeh FeinbergDepartment of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, CSIC, 28006 Madrid, Spain.ORCID 0000-0001-5325-4731
Juan Carlos Gómez MartínInstituto de Astrofísica de Andalucía, CSIC, 18008 Granada, Spain.ORCID 0000-0001-7972-085X
Julián VillamayorDepartment of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, CSIC, 28006 Madrid, Spain.ORCID 0000-0002-8844-7389
Peng ZhangSchool of Atmospheric Sciences, Nanjing University, Nanjing, China.
Yanxu ZhangDepartment of Earth and Environmental Sciences, Tulane University, New Orleans, LA 70118, USA.ORCID 0000-0001-7770-3466
Christopher S Blaszczak-BoxeEarth, Equity, and Environment Department, Howard University, Washington, DC 20059, USA.
Oleg TravnikovDepartment of Environmental Sciences, Jožef Stefan Institute, Jamova cesta 39, 1000 Ljubljana, Slovenia.ORCID 0000-0002-4413-0777
Feiyue WangCentre for Earth Observation Science, and Department of Environment and Geography, University of Manitoba, Winnipeg, MB R3T 2N2, Canada.ORCID 0000-0001-5297-0859
Johannes BieserHelmholtz-Zentrum Geethacht, Institute of Coastal Research, Max-Planck-Strasse 1, 21502 Geesthacht, Germany.ORCID 0000-0003-2938-3124
Joseph S FranciscoDepartment of Earth and Environmental Science and Department of Chemistry, University of Pennsylvania, Philadelphia, PA 19104, USA.ORCID 0000-0002-5461-1486
John M C PlaneSchool of Chemistry, University of Leeds, Leeds, UK.ORCID 0000-0003-3648-6893

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Mercury (Hg) is a global pollutant with substantial risks to human and ecosystem health. By upward transport in tropical regions, mercury enters into the stratosphere, but the contribution of the stratosphere to global mercury dispersion and deposition remains unknown. We find that between 5 and 50% (passing through the 400-kelvin isentropic surface and tropopause, respectively) of the mercury mass deposited on Earth's surface is chemically processed in the lower stratosphere. Our results show the stratosphere as a unique chemical environment where elemental mercury is efficiently converted to long-lived oxidized species. Subsequent downward transport contributes substantially to the oxidized mercury burden in the troposphere. The results show that the stratosphere facilitates the global dispersion of large amounts of mercury from polluted source regions to Earth's remote environments. We find that stratospheric transport is as important as tropospheric transport in interhemispheric mercury dispersion. Future projections suggest that expected changes in atmospheric circulation will increase the transport of mercury into the stratosphere.

Identifiers

PMID39772680
PMCPMC11804340

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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.