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Record W3016307049 · doi:10.1130/abs/2020nc-348157

HYDROCLIMATE CHANGE IN SOUTHWESTERN BRITISH COLUMBIA, CANADA REVEALED BY A 7000 YEAR LAKE SEDIMENT OXYGEN ISOTOPE RECORD

2020· article· en· W3016307049 on OpenAlexaboutno aff
Christopher Shea, Byron A. Steinman, Mark B. Abbott

Bibliographic record

VenueAbstracts with programs - Geological Society of America · 2020
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
Fundersnot available
Keywordsδ18OHoloceneAuthigenicGeologyIsotopes of oxygenCarbonateTephraMeteoric waterSedimentStable isotope ratioPrecipitationGlacial periodHydrology (agriculture)Physical geographyOceanographyGroundwaterGeochemistryGeomorphologyVolcanoChemistry

Abstract

fetched live from OpenAlex

Holocene climate variability in the Pacific Northwest has not been well characterized due to the scarcity of continuous, high-resolution records and inconsistencies in proxy sensitivity. Analyses of the oxygen isotopic composition of lake sediment carbonates contribute to this research by providing information on past changes in water isotope values (δ18O), which respond to a variety of climate variables including changes in the balance between precipitation and evaporation, lake level, and/or the isotopic composition of precipitation. Here we present a decadally resolved carbonate oxygen isotope record spanning the last ~7000 yr BP from Turquoise Lake (N50.83°, W121.69°, 807 m), a small, alkaline, semi-closed basin system located in southwestern British Columbia. Turquoise Lake surface water isotope values fall along the local evaporation line but are not substantially enriched relative to local meteoric water, indicating that water losses from the lake occur principally through overflow and groundwater outseepage. We measured the δ18O values of carbonates in three meters of sediment recovered from the depocenter of Turquoise Lake, in order to make inferences on climate change during the Holocene. We dated the Turquoise Lake record using 210Pb, 137Cs, 10 14C measurements, and one tephra layer and analyzed 374 samples of authigenic carbonate (the <63µm fraction) collected at 2 mm intervals. The Turquoise Lake δ18O record exhibits highly positive values at ~7000 years BP, indicating low lake levels and dry conditions at this time, consistent with a similar δ18O record from Castor Lake, WA. δ18O values over the remainder of the Holocene exhibit marked multi-century scale variability, indicating changes in hydroclimate that likely far exceed those observed historically. The Turquoise Lake δ18O results provide insight on the influence of Pacific ocean-atmosphere dynamics including the El Niño Southern Oscillation, Pacific Decadal Oscillation, and the Pacific North American Pattern on climate in the Pacific Northwest, and thus should improve our overall understanding of past hydroclimate changes in North America.

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)0.000
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 score0.104
Threshold uncertainty score0.997

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.000
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.001
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 head0.022
GPT teacher head0.222
Teacher spread0.199 · 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

Citations0
Published2020
Admission routes1
Has abstractyes

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