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2025· peer-review· en· W4410816642 on OpenAlexaffabout
G Todd Ventura

Bibliographic record

Venuenot available
Typepeer-review
Languageen
FieldNursing
TopicClinical Nutrition and Gastroenterology
Canadian institutionsSaint Mary's University
Fundersnot available
KeywordsGeography

Abstract

fetched live from OpenAlex

Abstract. The Scotian Slope in the North Atlantic Ocean extends ~500 km along the coast of Nova Scotia, Canada, descending from 400 m to 5 km water depth. With a maximum sediment thickness of ~24 km, large portions of the deeper basin are affected by salt tectonism, which has greatly impacted the basin stratigraphy and locally facilitated hydrocarbon seepage to the ocean seafloor. The surface sediments along the slope may therefore be home to microbial communities, which respond to complex geochemical drivers that not only include communication with the overlying water column, but also potential advection of deeper basinal fluids. Archaea are fundamental components of these communities, and their lipids act as important indicators of environmental conditions and microbial interactions within marine sediments. This study evaluates the spatial abundance and diversity of archaeal lipids preserved in shallow buried Scotian Slope sediments to better understand deep marine archaea community dynamics. Seventy-four sediment samples from 32 gravity and piston cores reaching a maximum depth of 9 meters below seafloor (mbsf) were collected during three survey cruises across a large region of the Scotian Slope. The survey area extends across ~40,000 km2, marking ~3° of latitudinal change over a water column depth that increases from ~1500 to 3500 m, of which one sampling site was a suspected cold seep environment. In total, 14 archaeal lipid classes comprising 42 unique compounds were detected. The lipid distributions reflect a high contribution of anaerobic methanotrophic (ANME) archaeal groups, such as ANME-1 to -3. Hierarchical cluster analysis (HCA) and principal components analysis (PCA) were used to show varying contributions of four lipid classes that included distinct assemblages of intact polar lipids (IPLs), which are largely sourced from living cells as well as core lipids (CLs), and their degradation products (CL-DPs) that collectively are sourced from different alteration stages following the death of the cell. From this, four stratigraphically distinct archaeal lipidomes, marking varying relative abundances of the lipid classes were observed in the upper 9 m of the surveyed slope sediments. One lipidome likely reflects archaeal communities impacted by a cold seep based on hydrocarbon head space gas analyses and high methane index and GDGT/Cren ratios. The other three lipidomes occur across overlapping sediment depth intervals in which the diversity and abundance of living, fossil, and degraded core lipids systematically change in what is likely depth. These changes likely mark systematic geochemically controlled, microbial community variations that are accompanying an increasing stockpile of diagenetic altered CLs. The three ambient sediment lipidomes appear to be highly conserved across the latitudinal extent of the study area marking a resolvable shallow sediment lipostratigraphy for the Scotian Slope.

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)0.002
metaresearch head score (Gemma)0.018
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Commentary · Consensus signal: Commentary
Teacher disagreement score0.244
Threshold uncertainty score0.816

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0020.018
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0010.001
Science and technology studies0.0020.002
Scholarly communication0.0030.003
Open science0.0030.002
Research integrity0.0160.015
Insufficient payload (model declined to judge)0.2440.174

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 head0.055
GPT teacher head0.389
Teacher spread0.335 · 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 designNot applicable
Domainnot available
GenreCommentary

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
Published2025
Admission routes2
Has abstractyes

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