Evidence map›Paper›PMID 32214119›Full record

ArticleScientific reports2020

Smoothed millennial-scale palaeoclimatic reference data as unconventional comparison targets: Application to European loess records.

Christian Zeeden, Igor Obreht, Daniel Veres, Stefanie Kaboth-Bahr, Jan Hošek, Slobodan B Marković, Janina Bösken, Frank Lehmkuhl, Christian Rolf, Ulrich Hambach

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Article in Scientific reports, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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0citing papers in PubMed
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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

10 authors.

Christian ZeedenLIAG, Leibniz Institute for Applied Geophysics, Hannover, Germany. christian.zeeden@leibniz-liag.de.
Igor ObrehtOrganic Geochemistry Group, MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Bremen, Germany.
Daniel VeresRomanian Academy, Institute of Speleology, Cluj-Napoca, Romania.
Stefanie Kaboth-BahrInstitute of Earth Sciences, Ruprecht-Karls-Universität Heidelberg, Heidelberg, Germany.
Jan HošekCzech Geological Survey, Prague, Czech Republic.
Slobodan B MarkovićChair of Physical Geography, Faculty of Sciences, University of Novi Sad, Novi Sad, Serbia.
Janina BöskenDepartment of Geography, RWTH Aachen University, Aachen, Germany.
Frank LehmkuhlDepartment of Geography, RWTH Aachen University, Aachen, Germany.
Christian RolfLIAG, Leibniz Institute for Applied Geophysics, Hannover, Germany.
Ulrich HambachBayCEER & Chair of Geomorphology, University of Bayreuth, Bayreuth, Germany.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Millennial-scale palaeoclimate variability has been documented in various terrestrial and marine palaeoclimate proxy records throughout the Northern Hemisphere for the last glacial cycle. Its clear expression and rapid shifts between different states of climate (Greenland Interstadials and Stadials) represents a correlation tool beyond the resolution of e.g. luminescence dating, especially relevant for terrestrial deposits. Usually, comparison of terrestrial proxy datasets and the Greenland ice cores indicates a complex expression of millennial-scale climate variability as recorded in terrestrial geoarchives including loess. Loess is the most widespread terrestrial geoarchive of the Quaternary and especially widespread over Eurasia. However, loess often records a smoothed representation of millennial-scale variability without all fidelity when compared to the Greenland data, this being a relevant limiting feature in integrating loess with other palaeoclimate records. To better understand the loess proxy-response to millennial-scale climate variability, we simulate a proxy signal smoothing by natural processes through application of low-pass filters of δ

Identifiers

PMID32214119
PMCPMC7096450

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