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The Subarctic Forest–Tundra: The Structure of a Biome in a Changing Climate

2001· article· en· W1953431167 on OpenAlexfundaboutno aff
Serge Payette, MARIE-JOSÉE FORTIN, Isabelle Gamache

Bibliographic record

VenueBioScience · 2001
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicTree-ring climate responses
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsSubarctic climateTundraBiomeTaigaEcologyGeographyEnvironmental sciencePhysical geographyForestryAgroforestryArcticEcosystemBiology

Abstract

fetched live from OpenAlex

The forest–tundra (FT) is a term coined byClements (1936) to describe the transition zone where the subalpine forest and alpine tundra communities meet. The term has been extended to include the high-latitude subarctic vegetation between the circumpolar boreal forest and the arctic tundra (Marr 1948, Hare 1959, Löve 1970, Hare and Ritchie 1972, Rowe 1972, Larsen 1980, Payette 1983). The vegetation mosaic of the FT is viewed as either an ecotone, a zonal subdivision, or a biome, depending on the scale of perception (Marr 1948, Hare 1959, Britton 1967, Rowe 1972, Nichols 1975, Payette 1983). The term ecotone is now gaining popularity, although the concept is an old one (Clements 1936), and it is now used to describe the structural and functional changes occurring at different spatial scales (Gosz 1993, Risser 1995). In the subarctic FT, forest communities are often confined to wind-protected, well-watered, and seepage sites, whereas upland, exposed, well-drained sites are occupied by treeless communities. Across a south–north gradient, the FT extends from the continuous-forest limit, that is, the limit of the area where all well-drained sites are colonized by forest, to the arctic tree line, that is, the northernmost position of arboreal growth. The contrasted structure of the subarctic FT is the inverted mirror image of the agro-forested landscape, in which forests are typically located on the exposed sites and low-stature agricultural fields are found on the bottomlands and riparian soils. Much like the agro-forested landscape, the subarctic FT is heavily fragmented, with strong edaphic and elevational gradients at the local and regional scales. The subarctic FT in North America covers a large area, mostly on the acidic, nutrient-poor soils of the Precambrian shelf across northern Canada, east and west of Hudson Bay (Figure 1). With its patchy vegetation pattern, the subarctic FT is certainly one major bioclimatic zone that exemplifies the ecotone concept. The subarctic FT is composed of climate-sensitive forests and trees at their northernmost ranges, which may explain why it has been used extensively in paleoecological and ecological studies for the evaluation of the environmental impact of climatic change (Lamb 1985, Ritchie 1987, Gajewski et al. 1993, Spear 1993).

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.033
Threshold uncertainty score0.067

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.004
Science and technology studies0.0010.002
Scholarly communication0.0020.002
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.015
GPT teacher head0.232
Teacher spread0.217 · 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 source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
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

Citations189
Published2001
Admission routes2
Has abstractyes

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