Evidence map›Paper›PMID 33093492›Full record

ArticleScientific reports2020

The fast-acting "pulse" of Heinrich Stadial 3 in a mid-latitude boreal ecosystem.

Federica Badino, Roberta Pini, Paolo Bertuletti, Cesare Ravazzi, Barbara Delmonte, Giovanni Monegato, Paula Reimer, Francesca Vallé, Simona Arrighi, Eugenio Bortolini and 9 more

Open access · goldAbstract read
In one paragraph

Article in Scientific reports, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
0.8field-weighted citation impact, top 27% of its field
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

1 citing paper in PubMed, 11 citations in OpenAlex.

  1. 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

19 authors at 8 institutions in 3 countries.

Federica BadinoDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy. federica.badino@unibo.it.
Roberta PiniResearch Group on Vegetation, Climate and Human Stratigraphy, Laboratory of Palynology and Palaeoecology, CNR-Institute of Environmental Geology and Geoengineering (IGAG), 20126, Milan, Italy.
Paolo BertulettiResearch Group on Vegetation, Climate and Human Stratigraphy, Laboratory of Palynology and Palaeoecology, CNR-Institute of Environmental Geology and Geoengineering (IGAG), 20126, Milan, Italy.
Cesare RavazziResearch Group on Vegetation, Climate and Human Stratigraphy, Laboratory of Palynology and Palaeoecology, CNR-Institute of Environmental Geology and Geoengineering (IGAG), 20126, Milan, Italy.
Barbara DelmonteDepartment of Environmental and Earth Sciences, University of Milano-Bicocca, 20126, Milan, Italy.
Giovanni MonegatoCNR-Institute of Geosciences and Earth Resources (IGG), 35131, Padua, Italy.
Paula ReimerSchool of Natural and Built Environment, Queen's University Belfast, Belfast, BT7 1NN, UK.
Francesca ValléDepartment of Environmental and Earth Sciences, University of Milano-Bicocca, 20126, Milan, Italy.
Simona ArrighiDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy.
Eugenio BortoliniDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy.
Carla FigusDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy.
Federico LugliDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy.
Valter MaggiDepartment of Environmental and Earth Sciences, University of Milano-Bicocca, 20126, Milan, Italy.
Giulia MarcianiDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy.
Davide MargaritoraDepartment of Environmental and Earth Sciences, University of Milano-Bicocca, 20126, Milan, Italy.
Gregorio OxiliaDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy.
Matteo RomandiniDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy.
Sara SilvestriniDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy.
Stefano BenazziDepartment of Cultural Heritage, University of Bologna, 48121, Ravenna, Italy.
University of Bologna · ITUniversity of Milano-Bicocca · ITInstitute of Environmental Geology and Geoengineering · ITInstitute of Geosciences and Earth Resources · ITMax Planck Institute for Evolutionary Anthropology · DEQueen's University Belfast · GBUniversity of Ferrara · ITUniversity of Siena · IT

Funding

European Research Council 724046-SUCCESS
6 · The paper itself

Abstract

A 3800 year-long radiocarbon-dated and highly-resolved palaeoecological record from Lake Fimon (N-Italy) served to investigate the effects of potential teleconnections between North Atlantic and mid-to-low latitudes at the transition from Marine Isotope Stage (MIS) 3 to 2. Boreal ecosystems documented in the Fimon record reacted in a sensitive way to millennial and sub-millennial scale Northern Hemisphere atmospheric circulation patterns. The high median time-resolution of 58 years allows the identification of five abrupt event-boundaries (i.e., main forest expansion and decline excursions) synchronous with the sharp stadial/interstadial (GS/GI) transitions within dating uncertainties. During Heinrich Stadial 3 (HS 3) we reconstruct more open and dry conditions, compared to the other GS, with a dominant regional scale fire signal. Linkages between local fires and climate-driven fuel changes resulted in high-magnitude fire peaks close to GI/GS boundaries, even exacerbated by local peatland conditions. Finally, palaeoecological data from the HS 3 interval unveiled an internal variability suggesting a peak between 30,425 and 29,772 cal BP (2σ error) which matches more depleted δ

Identifiers

PMID33093492
PMCPMC7581741
OpenAlexW3094495930

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

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.