Evidence map›Paper›PMID 41993777›Full record

ArticleCommunications earth & environment2026

High-enthalpy Larderello geothermal system, Italy, powered by thousands of cubic kilometres of mid-crustal magma.

Matteo Lupi, Douglas Stumpp, Iván Cabrera-Pérez, Konstantinos Michailos, Gilberto Saccorotti, Marco Bonini, Federico Farina, Elliot Amir Jiwani-Brown, Riccardo Lanari, Samuele Papeschi and 8 more

Abstract read
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In one paragraph

Article in Communications earth & environment, 2026. 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

18 authors.

Matteo LupiDepartment of Earth Sciences, University of Geneva, Geneva, Switzerland.ORCID 0000-0002-2351-6371
Douglas StumppDepartment of Earth Sciences, University of Geneva, Geneva, Switzerland.ORCID 0009-0003-9972-3646
Iván Cabrera-PérezDepartment of Earth Sciences, University of Geneva, Geneva, Switzerland.
Konstantinos MichailosDepartment of Earth Sciences, University of Geneva, Geneva, Switzerland.ORCID 0000-0003-3011-6939
Gilberto SaccorottiIstituto Nazionale di Geofisica e Vulcanologia, Pisa, Italy.ORCID 0000-0003-2915-1446
Marco BoniniInstitute of Geosciences and Earth Resources, National Research Council of Italy (CNR), Florence, Italy.ORCID 0000-0003-4818-8076
Federico FarinaDepartment of Earth Sciences "A. Desio", Università degli Studi di Milano, Milano, Italy.ORCID 0000-0002-7112-7047
Elliot Amir Jiwani-BrownDepartment of Earth Sciences, University of Geneva, Geneva, Switzerland.
Riccardo LanariInstitute of Geosciences and Earth Resources, National Research Council of Italy (CNR), Florence, Italy.
Samuele PapeschiInstitute of Geosciences and Earth Resources, National Research Council of Italy (CNR), Florence, Italy.ORCID 0000-0002-5774-7119
Geneviève SavardDepartment of Earth Sciences, University of Geneva, Geneva, Switzerland.ORCID 0000-0001-5464-3384
Juan PorrasDepartment of Earth Sciences, University of Geneva, Geneva, Switzerland.
Julien SfalcinInvert SA, Canton Vaud, Switzerland.
Francisco Muñoz-BurbanoDepartment of Earth Sciences, University of Geneva, Geneva, Switzerland.
Riccardo MinettoInstitut Terre et Environnement de Strasbourg, Université de Strasbourg/CNRS, Strasbourg, France.ORCID 0000-0002-6797-5190
Chiara Del VentisetteDepartment of Earth Science, University of Florence, Florence, Italy.
Davide PiccininiIstituto Nazionale di Geofisica e Vulcanologia, Pisa, Italy.
Domenico MontanariInstitute of Geosciences and Earth Resources, National Research Council of Italy (CNR), Florence, Italy.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Thousands of cubic kilometers of magma lie in the upper crust below supervolcanoes such as Yellowstone (USA), Toba (Indonesia), and Taupo (New Zealand). Most of these systems are identified because of surface geomorphology and eruptive deposits. Recognizing such volcanoes without surface evidence is challenging, causing large magmatic reservoirs to go unnoticed. The Tuscan Magmatic Province, Italy, features only sparse Quaternary volcanic activity, but subsurface data indicate the presence of supercritical fluids at shallow depths. Here we show that more than 5'000 km

Indexed as

SeismologyTectonicsVolcanology

Identifiers

PMID41993777
PMCPMC13079101

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.