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Record W2276825175 · doi:10.14288/1.0096623

Plankton blooms of the British Columbia northern shelf : seasonal distributions and mechanisms influencing their formation

2010· article· en· W2276825175 on OpenAlexaboutno aff
Richard Ian Perry

Bibliographic record

VenuecIRcle (University of British Columbia) · 2010
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
Fundersnot available
KeywordsPlanktonOceanographyEnvironmental scienceClimatologyGeographyFisheryGeologyBiology

Abstract

fetched live from OpenAlex

The first description is presented of spatial and seasonal distributions of plankton blooms, and physical oceanographic conditions underlying their formation, on the British Columbia northern shelf. This region includes Queen Charlotte Strait and Sound, Hecate Strait, Dixon Entrance and their contiguous waters. Its biological oceanographic characteristics are virtually unknown, yet it has valuable petroleum and fishery resources. Samples were collected between March 1978 and August 1980 using a coastal oil tanker as a ship of opportunity. Fourteen cruises were conducted, concentrated during spring and summer. Samples for salinity, nutrients, phytoplankton composition and pigments were collected from the sea water intake system (depth 3 m) while underway. Zooplankton were collected with a Miller sampler towed from the stern; temperature profiles were obtained with an XBT system. Light penetration and vertical mixing characteristics were the principal physical properties leading to initiation of phytoplankton blooms in spring and summer. The spring (diatom) bloom was predicted by a critical - mixed depth model calculated from historical data. Summer blooms were predicted by a tidal front model, which compares tidal velocities with water depth. Bathymetry is the common feature of these two mechanisms, limiting the mixed depth in spring and maintaining tidal mixing in shallow regions during summer. The spring bloom progressed northward with increasing irradiance, occurring during February - March in the Strait of Georgia and during May in Dixon Entrance. However, it was predicted and observed earlier in Hecate Strait (April), where a shallow shelf limits the mixed depth, than in more southerly Queen Charlotte Sound. The bloom in Queen Charlotte Sound first developed along its southeastern coast, apparently due to runoff-related stratification. On the scale of sampling, zooplankton blooms in spring occurred in the same areas as phytoplankton. During summer, observations confirmed low biomass (flagellates) and well-mixed conditions in shallow western Hecate Strait, and high biomass (diatoms) and stratified conditions on its eastern side. However, mean mixed layer light intensities were similar, and near-surface nutrient concentrations low, on both sides of the strait. Phytoplankton on the shallow side were probably limited by rates of nutrient resupply, while the eastern side received nutrients from upwelling or sporadic mixing by storms. This may distinguish the effect of tidal mixing in shelf seas and straits, with advection of nutrients to the mixed region of straits reduced by the shallow bottom and adjacent land boundaries.

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)0.001
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: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.127
Threshold uncertainty score0.255

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.006
GPT teacher head0.156
Teacher spread0.151 · 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

Citations4
Published2010
Admission routes1
Has abstractyes

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