Evidence map›Paper›PMID 39454008›Full record

ArticleScience advances2024

Atmospheric particulates over the northwestern Pacific during the late Holocene: Volcanism, dust, and human perturbation.

Samuel K Marx, James Hooper, Tomohisa Irino, Nicola Stromsoe, Krystyna M Saunders, Osamu Seki, Anthony Dosseto, Andrea Johansen, Quan Hua, Florian Dux and 2 more

Abstract readHistorical Article
In one paragraph

Article in Science advances, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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

0 citing papers in PubMed.

No citing paper in PubMed yet.

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

12 authors.

Samuel K MarxEnvironmental Futures, School of Earth, Atmosphere and Life Sciences, The University of Wollongong, Wollongong, New South Wales, Australia.ORCID 0000-0003-2333-5260
James HooperEnvironmental Futures, School of Earth, Atmosphere and Life Sciences, The University of Wollongong, Wollongong, New South Wales, Australia.
Tomohisa IrinoEarth and Planetary Sciences, School of Science, Hokkaido University, Sapporo, Hokkaido, Japan.ORCID 0000-0001-6941-770X
Nicola StromsoeResearch Institute for the Environment and Livelihoods, Faculty of Science and Technology, Charles Darwin University, Casuarina, Northern Territory, Australia.ORCID 0000-0001-6042-6220
Krystyna M SaundersAustralian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights, New South Wales, Australia.ORCID 0000-0002-6800-2630
Osamu SekiInstitute of Low Temperature Science, Hokkaido University, Sapporo, Hokkaido, Japan.ORCID 0000-0001-6136-288X
Anthony DossetoEnvironmental Futures, School of Earth, Atmosphere and Life Sciences, The University of Wollongong, Wollongong, New South Wales, Australia.ORCID 0000-0002-3575-0106
Andrea JohansenEnvironmental Futures, School of Earth, Atmosphere and Life Sciences, The University of Wollongong, Wollongong, New South Wales, Australia.ORCID 0000-0003-4940-4324
Quan HuaAustralian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights, New South Wales, Australia.ORCID 0000-0003-0179-8539
Florian DuxEnvironmental Futures, School of Earth, Atmosphere and Life Sciences, The University of Wollongong, Wollongong, New South Wales, Australia.ORCID 0000-0002-3275-710X
Geraldine JacobsenAustralian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights, New South Wales, Australia.ORCID 0000-0002-9644-5877
Atun ZawadzkiAustralian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights, New South Wales, Australia.ORCID 0000-0002-1096-8109

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Mineral aerosols form a key component of Earth's dynamic biogeochemical systems, yet their composition and mass are variable in time. We reconstruct patterns in mineral aerosol flux from East Asia, the second largest global dust source, in a peat mire in northern Japan. Using geochemical fingerprinting, we show for the past ~3600 years that high but variable tephra flux dominated regional aerosol loads. A human signal was discernible as elevated pollutant metals, along with East Asian mainland dust, identifiable by its geochemical signature. After ~700 years before the present, dust flux increased as the westerly jet intensified and moved south, the summer monsoon strength reduced, and agriculture expanded. From the 20th century, dust flux increased by two times. Attributable largely to human activity, this demarks a major change in aerosol export to the northwestern Pacific with accompanying increases in fluxes for key micronutrients and increased pollution flux by 16 times.

Indexed as

AerosolsDustParticulate MatterVolcanic EruptionsAir PollutantsAtmosphereEnvironmental MonitoringHistory, AncientHumansPacific OceanAerosolsAir PollutantsDustParticulate Matter

Identifiers

PMID39454008
PMCPMC12680304

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.