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Regional variability in peatland burning at mid-to high-latitudes during the Holocene

2023· article· en· W4323922746 on OpenAlex
Thomas G. Sim, Graeme T. Swindles, Paul J. Morris, Andy J. Baird, Angela Gallego‐Sala, Yuwan Wang, Maarten Blaauw, Philip Camill, Michelle Garneau, Mark Hardiman, Julie Loisel, Minna Väliranta, L. Anderson, Karina Apolinarska, Femke Augustijns, Liene Auniņa, Joannie Beaulne, Přemysl Bobek, Werner Borken, Nils Broothaerts, Qiaoyu Cui, Marissa A. Davies, Ana Ejarque, Michelle Farrell, Ingo Feeser, Angelica Feurdean, Richard E. Fewster, Sarah A. Finkelstein, Marie‐José Gaillard, Mariusz Gałka, Liam Heffernan, Renske Hoevers, Miriam C. Jones, Teemu Juselius‐Rajamäki, Edgar Karofeld, Klaus‐Holger Knorr, Atte Korhola, Dmitri Kupriyanov, Malin E. Kylander, Terri Lacourse, Mariusz Lamentowicz, Martin Lavoie, Geoffrey Lemdahl, Dominika Łuców, Gabriel Magnan, Alekss Maksims, Claudia A. Mansilla, Katarzyna Marcisz, Elena Marinova, Paul Mathijssen, Dmitri Mauquoy, Yuri Mazei, Natalia Mazei, Julia McCarroll, Robert McCulloch, Alice M. Milner, Yannick Miras, Fraser Mitchell, Елена Новенко, Nicolas Pelletier, Matthew Peros, Sanna Piilo, Louis‐Martin Pilote, Guillaume Primeau, Damien Rius, Vincent Robin, Mylène Robitaille, Thomas P. Roland, Eleonor E. Ryberg, A. Britta K. Sannel, Karsten Schittek, Gabriel Servera-Vives, William Shotyk, Michał Słowiński, Normunds Stivriņš, Ward Swinnen, Gareth Thompson, Alexei V. Tiunov, Andrey N. Tsyganov, Eeva‐Stiina Tuittila, Gert Verstraeten, Tuomo Wallenius, J. C. Webb, Debra A. Willard, Zicheng Yu, Claudio Zaccone, Hui Zhang

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

VenueQuaternary Science Reviews · 2023
Typearticle
Languageen
FieldEnvironmental Science
TopicPeatlands and Wetlands Ecology
Canadian institutionsUniversité du Québec à MontréalUniversity of TorontoCarleton University
FundersNatural Environment Research CouncilU.S. Geological SurveyAgencia Nacional de Investigación y DesarrolloRussian Science FoundationFondo Nacional de Desarrollo Científico y TecnológicoLatvijas UniversitateAkademie der NaturwissenschaftenNarodowe Centrum NaukiChinese Academy of SciencesDeutsche ForschungsgemeinschaftLeverhulme TrustBayerisches Hochschulzentrum für LateinamerikaSchweizerischer Nationalfonds zur Förderung der Wissenschaftlichen ForschungAcademy of FinlandQuaternary Research AssociationSociety for Research on AdolescenceGerman Academic Exchange Service LondonDeutscher Akademischer AustauschdienstPast Global ChangesWestfälische Wilhelms-Universität MünsterRussian Science Support FoundationEesti TeadusagentuurNational Science Foundation
KeywordsPeatHolocenePhysical geographyClimate changeFire regimeCharcoalEnvironmental scienceBorealGeologyEcologyGeographyEcosystemOceanographyArchaeologyPaleontology

Abstract

fetched live from OpenAlex

Northern peatlands store globally-important amounts of carbon in the form of partly decomposed plant detritus. Drying associated with climate and land-use change may lead to increased fire frequency and severity in peatlands and the rapid loss of carbon to the atmosphere. However, our understanding of the patterns and drivers of peatland burning on an appropriate decadal to millennial timescale relies heavily on individual site-based reconstructions. For the first time, we synthesise peatland macrocharcoal records from across North America, Europe, and Patagonia to reveal regional variation in peatland burning during the Holocene. We used an existing database of proximal sedimentary charcoal to represent regional burning trends in the wider landscape for each region. Long-term trends in peatland burning appear to be largely climate driven, with human activities likely having an increasing influence in the late Holocene. Warmer conditions during the Holocene Thermal Maximum (∼9–6 cal. ka BP) were associated with greater peatland burning in North America's Atlantic coast, southern Scandinavia and the Baltics, and Patagonia. Since the Little Ice Age, peatland burning has declined across North America and in some areas of Europe. This decline is mirrored by a decrease in wider landscape burning in some, but not all sub-regions, linked to fire-suppression policies, and landscape fragmentation caused by agricultural expansion. Peatlands demonstrate lower susceptibility to burning than the wider landscape in several instances, probably because of autogenic processes that maintain high levels of near-surface wetness even during drought. Nonetheless, widespread drying and degradation of peatlands, particularly in Europe, has likely increased their vulnerability to burning in recent centuries. Consequently, peatland restoration efforts are important to mitigate the risk of peatland fire under a changing climate. Finally, we make recommendations for future research to improve our understanding of the controls on peatland fires.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.005
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.017
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0050.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.002

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.026
GPT teacher head0.278
Teacher spread0.251 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it