Evidence map›Paper›PMID 42603803›Full record

ArticleScientific reports2026

Annual-resolution evidence for aridity spikes at the onset of the Last Glacial Inception in an Eifel maar lake sediment.

Frank Sirocko, Frederik Krebsbach, Christian Forster, Frank Dreher, Martin Grosjean, Lucas Silva, Dana F C Riechelmann, Klemens Seelos, Ralf Schiebel

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Article in Scientific reports, 2026. 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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1 · What the graph read from it

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2 · The registry

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4 · The record

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5 · Who and what money

Authors and funding

9 authors.

Frank SirockoInstitute of Geosciences, Johannes Gutenberg-University Mainz, Mainz, Germany. sirocko@uni-mainz.de.
Frederik KrebsbachInstitute of Geosciences, Johannes Gutenberg-University Mainz, Mainz, Germany.
Christian ForsterInstitute of Geosciences, Johannes Gutenberg-University Mainz, Mainz, Germany.
Frank DreherInstitute of Geosciences, Johannes Gutenberg-University Mainz, Mainz, Germany.
Martin GrosjeanUniversity of Bern, Oeschger Centre for Climate Change Research & Institute of Geography, Bern, Switzerland.
Lucas SilvaClimate and Environmental Physics, University of Bern, Bern, Switzerland.
Dana F C RiechelmannInstitute of Geosciences, Johannes Gutenberg-University Mainz, Mainz, Germany.
Klemens SeelosInstitute of Geosciences, Johannes Gutenberg-University Mainz, Mainz, Germany.
Ralf SchiebelMax Planck Institute for Chemistry, Mainz, Germany.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

This study presents an annually laminated sediment record from the infilled maar lake at Hoher List in the Eifel volcanic field (Germany), documenting the "Last Glacial Inception" (LGI) at the end of the Eemian interglacial. The landscape of the late Eemian was dominated by a mixed forest containing Abies alba (silver fir). The collapse of this forest occurred within only a few years and was accompanied by frequent wildfires, aeolian dust deposition, a decline of all thermophilous tree species, and the disappearance of Abies, all indicating increasing aridity. The transition unfolded in three distinct phases. LEAP-I (Late Eemian Aridity Pulse I) lasted approximately 250 years and was followed by a 750-year recovery phase during which the interglacial forest returned. LEAP-II was characterized by comparable arid conditions but persisted for at least 750 years, followed by a 350-year phase of boreal forest development. The final transition to stadial conditions occurred during LEAP-III, marked by a pronounced lake-level decline, expansion of grassland, scattered birch and pine, and reduced summer temperatures, likely corresponding to North Atlantic cold event C25. The LGI lasted at least 2700 years, whereas individual aridification pulses developed within decades, indicating rapid aridification events superimposed on a long-term cooling trend.

Identifiers

PMID42603803
PMCPMC13477475

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