Evidence map›Paper›PMID 35767617›Full record

ArticleScience advances2022

Exceptionally stable preindustrial sea level inferred from the western Mediterranean Sea.

Bogdan P Onac, Jerry X Mitrovica, Joaquín Ginés, Yemane Asmerom, Victor J Polyak, Paola Tuccimei, Erica L Ashe, Joan J Fornós, Mark J Hoggard, Sophie Coulson and 3 more

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Science advances, 2022. 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

13 authors.

Bogdan P OnacKarst Research Group, School of Geosciences, University of South Florida, 4202 E Fowler Ave., NES 107, Tampa, FL 33620, USA.ORCID 0000-0003-2332-6858
Jerry X MitrovicaDepartment of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA.
Joaquín GinésEarth Sciences Research Group, Universitat de les Illes Balears, Ctra. Valldemossa km 7.5, 07122 Palma (Mallorca), Spain.ORCID 0000-0003-4608-8709
Yemane AsmeromDepartment of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131, USA.ORCID 0000-0003-3440-1294
Victor J PolyakDepartment of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131, USA.ORCID 0000-0002-2010-1066
Paola TuccimeiDipartimento di Scienze, Università "Roma Tre," Largo San Leonardo Murialdo 1, 00146 Roma, Italy.
Erica L AsheDepartment of Earth and Planetary Sciences, Rutgers University, Piscataway, NJ 08854, USA.ORCID 0000-0002-7445-6321
Joan J FornósEarth Sciences Research Group, Universitat de les Illes Balears, Ctra. Valldemossa km 7.5, 07122 Palma (Mallorca), Spain.ORCID 0000-0002-3131-1085
Mark J HoggardDepartment of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA.ORCID 0000-0003-4310-3862
Sophie CoulsonFluid Dynamics and Solid Mechanics Group, Los Alamos National Laboratory, Los Alamos, NM 87545, USA.
Angel GinésEarth Sciences Research Group, Universitat de les Illes Balears, Ctra. Valldemossa km 7.5, 07122 Palma (Mallorca), Spain.ORCID 0000-0003-3309-8297
Michele SoligoDipartimento di Scienze, Università "Roma Tre," Largo San Leonardo Murialdo 1, 00146 Roma, Italy.
Igor M VillaInstitut für Geologie, Universität Bern, Baltzerstrasse 1-3, 3012 Bern, Switzerland.ORCID 0000-0002-8070-8142

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

An accurate record of preindustrial (pre-1900 CE) sea level is necessary to contextualize modern global mean sea level (GMSL) rise with respect to natural variability. Precisely dated phreatic overgrowths on speleothems (POS) provide detailed rates of Late Holocene sea-level rise in Mallorca. Statistical analysis indicates that sea level rose locally by 0.12 to 0.31 m (95% confidence) from 3.26 to 2.84 thousand years (ka) ago (2σ) and remained within 0.08 m (95% confidence) of preindustrial levels from 2.84 ka to 1900 CE. This sea-level history is consistent with glacial isostatic adjustment models adopting relatively weak upper mantle viscosities of ~10

Identifiers

PMID35767617
PMCPMC9242593

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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.