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Record W21293902 · doi:10.1007/s10529-011-0549-0

Late Quaternary sediment records from the northernmost lake archive of the Yukon (Herschel Island, Western Canadian Arctic)

2010· article· en· W21293902 on OpenAlexaboutno aff
Josefine Lenz, Michael Fritz, Hugues Lantuit, Sebastian Wetterich, Lutz Schirrmeister, Wayne H. Pollard, Peter Frenzel, Stefan Lorenz

Bibliographic record

VenueBiotechnology Letters · 2010
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyQuaternaryArcticGlacial periodRadiocarbon datingHolocenePaleolimnologyPleistoceneOceanographyBeringiaLimnologyGlacial lakePermafrostPaleontologyPhysical geographyGeography

Abstract

fetched live from OpenAlex

In spring 2009, a 730 cm sediment core was recovered from the largest lake on Herschel Island (Yukon Territory, Canada). This is one of the first continuous paleo-records in the Western Canadian Arctic and the northernmost archive derived from lake sediments in the Yukon.Located 70 km east of the Yukon-Alaska border in the Southern Beaufort Sea and with a maximum elevation about 180 m, Herschel Island is presumably a terminal moraine representing the westernmost extension of the Wisconsin glaciation. Characterizing the paleoenvironment and determining the age of the maximum glacial extent are important outcomes for Quaternary research and for the settlement history of Canada. A multi-proxy approach was applied to analyse the lake sediments and pore water. A combination of biogeochemical parameters (TC, TOC, TN), grain size analysis, magnetic susceptibility, x-ray fluorescence and stable isotope determination (δ13C) as well as the hydrochemistry of pore water (pH and electrical conductivity) were used to yield information about the late Quaternary limnology of Lake Herschel. Age determinations by radiocarbon dating allowed to develop an age-depth model of the sediment core. Our results from various analyses of the sediment core point towards four distinguished stratigraphic and lithologic units. A sharp contact, probably related to mass movements in the vicinity of the lake, divides the uppermost two units. The most prominent feature of the core, however, relates to a drastic change in sedimentology indicating the transition from late Holocene to Pleistocene between the lowermost two units at a depth of 700 cm. Electrical conductivity was observed to increase steadily with depth, providing an indication about the water balance throughout the Holocene. The brackish water conditions in the lake seemed to have interestingly enabled liveable conditions for both marine and freshwater organisms at the same time (ostracodes, foraminifera, molluscs). The results from this core refl ect the catchment sedimentology but provide a highly detailed and unique record of the paleoenvironment of the coastal western Arctic to be compared with similar records from both the neighbouring Ocean and the more southern lake sediment records in the Yukon.

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: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.030
Threshold uncertainty score0.060

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.004
Science and technology studies0.0020.001
Scholarly communication0.0010.000
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.009
GPT teacher head0.196
Teacher spread0.187 · 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

Citations0
Published2010
Admission routes1
Has abstractyes

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