Evidence map›Paper›PMID 32286283›Full record

ArticleNature communications2020

Sediment controls dynamic behavior of a Cordilleran Ice Stream at the Last Glacial Maximum.

Ellen A Cowan, Sarah D Zellers, Juliane Müller, Maureen H Walczak, Lindsay L Worthington, Beth E Caissie, Wesley A Clary, John M Jaeger, Sean P S Gulick, Jacob W Pratt and 2 more

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing papers in PubMed
0.9field-weighted citation impact, top 26% 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

2 citing papers in PubMed, 13 citations in OpenAlex.

  1. Ice and ocean constraints on early human migrations into North America along the Pacific coast.Proceedings of the National Academy of Sciences of the United States of America · 2023
    Article
  2. 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

12 authors at 9 institutions in 3 countries.

Ellen A CowanDepartment of Geological and Environmental Sciences, Appalachian State University, Box 32067, Boone, NC, 28608, USA. cowanea@appstate.edu.ORCID http://orcid.org/0000-0001-6512-5769
Sarah D ZellersSchool of Geoscience, Physics, and Safety, University of Central Missouri, Warrensburg, MO, 64093, USA.ORCID http://orcid.org/0000-0002-2975-4717
Juliane MüllerAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Alten Hafen 26, 27568, Bremerhaven, Germany.ORCID http://orcid.org/0000-0003-0724-4131
Maureen H WalczakCollege of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, 97331, USA.
Lindsay L WorthingtonDepartment of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM, 87131, USA.
Beth E CaissieDepartment of Geological and Atmospheric Sciences, Iowa State University, Ames, IA, 50011, USA.ORCID http://orcid.org/0000-0001-9587-1842
Wesley A ClaryDepartment of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM, 87131, USA.ORCID http://orcid.org/0000-0003-4923-3553
John M JaegerDepartment of Geological Sciences, University of Florida, Gainesville, FL, 32611, USA.ORCID http://orcid.org/0000-0003-0248-489X
Sean P S GulickInstitute for Geophysics & Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, 78758, USA.ORCID http://orcid.org/0000-0003-4740-9068
Jacob W PrattDepartment of Geological and Environmental Sciences, Appalachian State University, Box 32067, Boone, NC, 28608, USA.
Alan C MixCollege of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, 97331, USA.
Stewart J FallonResearch School of Earth Science, The Australian National University, Canberra, ACT, 2601, Australia.ORCID http://orcid.org/0000-0002-8064-5903
Appalachian State University · USOregon State University · USUniversity of New Mexico · USAlfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung · DEAustralian National University · AUIowa State University · USThe University of Texas at Austin · USUniversity of Central Missouri · USUniversity of Florida · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The uncertain response of marine terminating outlet glaciers to climate change at time scales beyond short-term observation limits models of future sea level rise. At temperate tidewater margins, abundant subglacial meltwater forms morainal banks (marine shoals) or ice-contact deltas that reduce water depth, stabilizing grounding lines and slowing or reversing glacial retreat. Here we present a radiocarbon-dated record from Integrated Ocean Drilling Program (IODP) Site U1421 that tracks the terminus of the largest Alaskan Cordilleran Ice Sheet outlet glacier during Last Glacial Maximum climate transitions. Sedimentation rates, ice-rafted debris, and microfossil and biogeochemical proxies, show repeated abrupt collapses and slow advances typical of the tidewater glacier cycle observed in modern systems. When global sea level rise exceeded the local rate of bank building, the cycle of readvances stopped leading to irreversible retreat. These results support theory that suggests sediment dynamics can control tidewater terminus position on an open shelf under temperate conditions delaying climate-driven retreat.

Identifiers

PMID32286283
PMCPMC7156478
OpenAlexW3015665307

What OpenQuestion holds

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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.