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Record W2906072433 · doi:10.1111/1365-2745.13123

Black spruce (<i>Picea mariana</i>) colonization of subarctic snowpatches in response to warmer climate

2018· article· en· W2906072433 on OpenAlexafffundabout
Alexandre Truchon‐Savard, Mélanie Jean, Serge Payette

Bibliographic record

VenueJournal of Ecology · 2018
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsUniversité LavalCenter for Northern StudiesNatural Sciences and Engineering Research Council of Canada
FundersFonds de recherche du Québec – Nature et technologiesAboriginal Affairs and Northern Development CanadaNatural Sciences and Engineering Research Council of Canada
KeywordsSubarctic climateBlack spruceTundraTaigaAfforestationTree lineShrubGrowing seasonSnowEcologyDeciduousMossBetula pubescensClimate changeScots pinePicea abiesSnowmeltColonizationEnvironmental scienceGeographyArcticBiologyBotanyPinus <genus>

Abstract

fetched live from OpenAlex

Abstract Snowpatches are disjunct arctic ecosystems scattered across the subarctic, particularly on wind‐protected lee slopes, where a thick snow cover accumulates during the winter. These snow‐rich treeless ecosystems are affected by delayed snowmelt, causing shorter growing seasons. Snow‐tolerant plants occupy the centre of subarctic snowpatches, whereas black spruce trees grow at the margins. Snowpatches have shown sporadic expansion and shrinkage phases from tree establishment and mortality linked to climatic trends. Field surveys in the subarctic of eastern Canada are showing an afforestation process occurring in snowpatches. The origin and nature of this afforestation were investigated based on the hypothesis that tree colonization and growth were closely associated with recent changes in climate. Snowpatches were categorized into three types based on border trees: forested, semi‐forested and tundra‐like. In eight randomly selected snowpatches of each type, snowpatch borders and areas covered by deciduous shrubs or trees were mapped and chionophilous plants and frost‐associated soil disturbances were recorded. Radial (tree‐ring) and vertical growth were measured on stems to evaluate the impact of climate and local factors on snowpatch black spruce populations. Two waves of spruce colonization occurred in all forested and semi‐forested snowpatches in the 1960s and in the 1980s to present. Spruce establishment was more frequent and abundant in recent years, near the forest margins and on moss and barren seedbeds. Expanding shrub (dwarf birch) cover inhibited spruce seedling establishment. Tree establishment and growth were positively correlated with growing season temperature and negatively correlated with annual maximum snow depth. More recently established spruce seedlings exhibited faster vertical growth than those established in the 20th century. Synthesis . Due to warmer conditions and earlier snowmelt in eastern Canada, black spruce trees and dwarf birch shrubs are racing through subarctic snowpatches. This afforestation could change biodiversity in the subarctic and affect watershed dynamics through a change in snowmelt pattern. Subarctic snowpatches are climate‐sensitive ecosystems of the forest–tundra landscape, forming ideal biotopes for snow‐tolerant, arctic–alpine species. Further tree encroachment in snowpatches in this century is potentially a threat to plant diversity, especially chionophilous species that have no corridors to migrate towards arctic ecosystems.

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)0.001
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 score0.097
Threshold uncertainty score0.996

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0050.000

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 head0.025
GPT teacher head0.260
Teacher spread0.235 · 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

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".

Quick stats

Citations5
Published2018
Admission routes3
Has abstractyes

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