Evidence map›Paper›PMID 40572046›Full record

ArticleEcology letters2025

Drying Spring Accelerates Transitions Toward Pyrogenic Vegetation in Eastern Boreal North America.

A A Ali, D M Gaboriau, J A Lesven, M P Girardin, C C Remy, D Arseneault, G de Lafontaine, V Danneyrolles, H Asselin, F Gennaretti and 7 more

Abstract read
In one paragraph

Article in Ecology letters, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing 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

2 citing papers in PubMed.

  1. Article
  2. 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

17 authors.

A A AliInstitut Des Sciences de L'évolution, Université de Montpellier (UMR 5554), Montpellier, France.ORCID https://orcid.org/0000-0002-6927-6633
D M GaboriauInstitut de Recherche Sur les Forêts, Université du Québec en Abitibi-Témiscamingue, Rouyn-Noranda, Quebec, Canada.
J A LesvenInstitut de Recherche Sur les Forêts, Université du Québec en Abitibi-Témiscamingue, Rouyn-Noranda, Quebec, Canada.
M P GirardinNatural Resources Canada, Canadian Forest Service, Laurentian Forestry Centre, Quebec City, Quebec, Canada.
C C RemyLaboratoire Chrono-Environnement, UMR 6249 CNRS, Université Marie et Louis Pasteur, Besançon Cedex, France.
D ArseneaultDépartement de Biologie, Chimie et Géographie, Université du Québec à Rimouski, Rimouski, Quebec, Canada.
G de LafontaineDépartement de Biologie, Chimie et Géographie, Université du Québec à Rimouski, Rimouski, Quebec, Canada.
V DanneyrollesInstitut de Recherche Sur les Forêts, Université du Québec en Abitibi-Témiscamingue, Rouyn-Noranda, Quebec, Canada.
H AsselinÉcole D'études Autochtones, Université du Québec en Abitibi-Témiscamingue, Rouyn-Noranda, Quebec, Canada.
F GennarettiInstitut de Recherche Sur les Forêts, Université du Québec en Abitibi-Témiscamingue, Rouyn-Noranda, Quebec, Canada.
E BoucherGroupe de Recherche en Écologie de la MRC-Abitibi (GREMA), Institut de Recherche Sur les Forêts, Université du Québec en Abitibi-Témiscamingue, Amos, Quebec, Canada.
P GrondinMinistère des Ressources naturelles et des Forêts, Direction de la recherche forestière, Québec, Quebec, Canada.
M GarneauCentre de Recherche Geotop Research Centre, Université du Québec à Montréal (UQAM), Montreal, Quebec, Canada.
G MagnanCentre de Recherche Geotop Research Centre, Université du Québec à Montréal (UQAM), Montreal, Quebec, Canada.
B FréchetteCentre de Recherche Geotop Research Centre, Université du Québec à Montréal (UQAM), Montreal, Quebec, Canada.
S GauthierNatural Resources Canada, Canadian Forest Service, Laurentian Forestry Centre, Quebec City, Quebec, Canada.
Y BergeronInstitut de Recherche Sur les Forêts, Université du Québec en Abitibi-Témiscamingue, Rouyn-Noranda, Quebec, Canada.

Funding

IRL Forêts Froides (CNRS, INEE)Natural Sciences and Engineering Research Council of Canada
6 · The paper itself

Abstract

The ongoing climate change increases vegetation flammability in the boreal forests of eastern North America, leading to more intense and severe wildfires. Using palaeoecological data-including charcoal, pollen, chironomids and testate amoebae-and climate model simulations of vapour pressure deficit (VPD) and available soil water (ASW), we analysed fire dynamics over the past 8000 years in boreal eastern North America. Over the last 4000 years, and particularly in the last 250 years, increasing spring drought has led to fewer, but more severe fires. This shift in the fire regime has favoured the spread of fire-adapted conifer species, particularly jack pine (Pinus banksiana), across the landscape. We infer that the predicted increase in VPD and decrease in ASW triggered by climate change will alter the fire regime and amplify the transition toward more pyrogenic vegetation within the boreal forest of eastern North America, with ecological and socio-economic consequences.

Indexed as

Climate ChangeDroughtsFiresForestsTreesWildfiresClimate ModelsNorth AmericaPinusSeasonsSoilTaigaVapor PressureSoilboreal forestclimate changefire regimepaleoecologyPicea marianaPinus banksiana

Identifiers

PMID40572046
PMCPMC12202849

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.