Evidence map›Paper›PMID 30150388›Full record

ArticleProceedings of the National Academy of Sciences of the United States of America2018

Impact of climate change on the transition of Neanderthals to modern humans in Europe.

Michael Staubwasser, Virgil Drăgușin, Bogdan P Onac, Sergey Assonov, Vasile Ersek, Dirk L Hoffmann, Daniel Veres

Abstract readHistorical Article
In one paragraph

Article in Proceedings of the National Academy of Sciences of the United States of America, 2018. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 22 papers.

0numbers the graph read from it
0cells of the map it votes in
22citing 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

22 citing papers in PubMed.

  1. Article
  2. Article
  3. Article
  4. Article
  5. Article
  6. Article
  7. Review
  8. Article
  9. Article
  10. Neanderthal coexistence withScience advances · 2023
    Article
  11. Article
  12. Article
  13. Article
  14. Article
  15. Review
  16. Article
  17. Subarctic climate for the earliestScience advances · 2021
    Article
  18. Article
  19. The early Aurignacian dispersal of modern humans into westernmost Eurasia.Proceedings of the National Academy of Sciences of the United States of America · 2020
    Article
  20. 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

7 authors.

Michael StaubwasserInstitute of Geologie and Mineralogy, University of Cologne, 50674 Cologne, Germany; m.staubwasser@uni-koeln.de.
Virgil DrăgușinEmil Racoviţă Institute of Speleology, Romanian Academy, 010986 Bucharest, Romania.
Bogdan P OnacSchool of Geosciences, University of South Florida, Tampa, FL 33620.ORCID 0000-0003-2332-6858
Sergey AssonovInstitute of Geologie and Mineralogy, University of Cologne, 50674 Cologne, Germany.
Vasile ErsekDepartment of Geography and Environmental Sciences, Northumbria University, Newcastle upon Tyne NE1 8ST, United Kingdom.
Dirk L HoffmannDepartment of Human Evolution, Max Planck Institute for Evolutionary Anthropology, 04103 Leipzig, Germany.
Daniel VeresEmil Racoviţă Institute of Speleology, Romanian Academy, 400006 Cluj-Napoca, Romania.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Two speleothem stable isotope records from East-Central Europe demonstrate that Greenland Stadial 12 (GS12) and GS10-at 44.3-43.3 and 40.8-40.2 ka-were prominent intervals of cold and arid conditions. GS12, GS11, and GS10 are coeval with a regional pattern of culturally (near-)sterile layers within Europe's diachronous archeologic transition from Neanderthals to modern human Aurignacian. Sterile layers coeval with GS12 precede the Aurignacian throughout the middle and upper Danube region. In some records from the northern Iberian Peninsula, such layers are coeval with GS11 and separate the Châtelperronian from the Aurignacian. Sterile layers preceding the Aurignacian in the remaining Châtelperronian domain are coeval with GS10 and the previously reported 40.0- to 40.8-ka cal BP [calendar years before present (1950)] time range of Neanderthals' disappearance from most of Europe. This suggests that ecologic stress during stadial expansion of steppe landscape caused a diachronous pattern of depopulation of Neanderthals, which facilitated repopulation by modern humans who appear to have been better adapted to this environment. Consecutive depopulation-repopulation cycles during severe stadials of the middle pleniglacial may principally explain the repeated replacement of Europe's population and its genetic composition.

Indexed as

ArchaeologyClimate ChangeExtinction, BiologicalNeanderthalsAnimalsEuropeHistory, AncientHumansCentral EuropeMiddle—Upper Paleolithic transitionmillennial-scale climate cyclesspeleothemsstable isotopes

Identifiers

PMID30150388
PMCPMC6140518

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
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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.