Evidence map›Paper›PMID 37379389›Full record

ArticleScience advances2023

Tracking carbon from subduction to outgassing along the Aleutian-Alaska Volcanic Arc.

Taryn Lopez, Tobias P Fischer, Terry Plank, Alberto Malinverno, Andrea L Rizzo, Daniel J Rasmussen, Elizabeth Cottrell, Cynthia Werner, Christoph Kern, Deborah Bergfeld and 3 more

Abstract read
In one paragraph

Article in Science advances, 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
–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

1 citing paper in PubMed.

  1. Review
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

13 authors.

Taryn LopezGeophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA.ORCID 0000-0001-6831-4573
Tobias P FischerUniversity of New Mexico, Albuquerque, NM, USA.ORCID 0000-0002-3467-0649
Terry PlankLamont Doherty Earth Observatory, Columbia University, Palisades, NY, USA.ORCID 0000-0002-1665-0484
Alberto MalinvernoLamont Doherty Earth Observatory, Columbia University, Palisades, NY, USA.ORCID 0000-0003-4442-9055
Andrea L RizzoIstituto Nazionale di Geofisica e Vulcanologia, Sezione di Milano, Milano, Italy.ORCID 0000-0003-2225-3781
Daniel J RasmussenLamont Doherty Earth Observatory, Columbia University, Palisades, NY, USA.ORCID 0000-0003-0137-6715
Elizabeth CottrellDepartment of Mineral Sciences, National Museum of Natural History Smithsonian Institution, Washington, DC, USA.ORCID 0000-0002-9402-9394
Cynthia WernerU.S. Geological Survey Contractor, New Plymouth, New Zealand.ORCID 0000-0003-3311-6694
Christoph KernCascades Volcano Observatory, U.S. Geological Survey, Vancouver, WA, USA.ORCID 0000-0002-8920-5701
Deborah BergfeldCalifornia Volcano Observatory, U.S. Geological Survey, Moffett Field, CA, USA.ORCID 0000-0003-4570-7627
Tehnuka IlankoUniversity of Waikato, Hamilton, New Zealand.ORCID 0000-0001-6535-1117
Janine L AndrysU.S. Geological Survey Contractor, New Plymouth, New Zealand.ORCID 0000-0001-5695-2375
Katherine A KelleyGraduate School of Oceanography, University of Rhode Island, Narragansett, RI, USA.ORCID 0000-0002-7516-2683

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Subduction transports volatiles between Earth's mantle, crust, and atmosphere, ultimately creating a habitable Earth. We use isotopes to track carbon from subduction to outgassing along the Aleutian-Alaska Arc. We find substantial along-strike variations in the isotopic composition of volcanic gases, explained by different recycling efficiencies of subducting carbon to the atmosphere via arc volcanism and modulated by subduction character. Fast and cool subduction facilitates recycling of ~43 to 61% sediment-derived organic carbon to the atmosphere through degassing of central Aleutian volcanoes, while slow and warm subduction favors forearc sediment removal, leading to recycling of ~6 to 9% altered oceanic crust carbon to the atmosphere through degassing of western Aleutian volcanoes. These results indicate that less carbon is returned to the deep mantle than previously thought and that subducting organic carbon is not a reliable atmospheric carbon sink over subduction time scales.

Identifiers

PMID37379389
PMCPMC12488040

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Registered trials

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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.