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Record W2799836629 · doi:10.3389/fmars.2018.00147

Rare Earth Element Distribution in the NE Atlantic: Evidence for Benthic Sources, Longevity of the Seawater Signal, and Biogeochemical Cycling

2018· article· en· W2799836629 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueFrontiers in Marine Science · 2018
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeochemistry and Elemental Analysis
Canadian institutionsnot available
FundersNatural Environment Research CouncilEuropean CommissionImperial College LondonHorizon 2020 Framework ProgrammeMarine Alliance for Science and Technology for Scotland
KeywordsSeawaterOceanographyGeologyWater columnWater massBiogeochemical cycleBenthic zoneTransectContinental shelfSeafloor spreadingAdvectionEcology

Abstract

fetched live from OpenAlex

Seawater rare earth element (REE) concentrations are increasingly applied to reconstruct\n\nwater mass histories by exploiting relative changes in the distinctive normalised patterns.\n\nHowever, the mechanisms by which water masses gain their patterns are yet to be\n\nfully explained. To examine this, we collected water samples along the Extended Ellett\n\nLine (EEL), an oceanographic transect between Iceland and Scotland, and measured\n\ndissolved REE by offline automated chromatography (SeaFAST) and ICP-MS. The\n\nproximity to two continental boundaries, the incipient spring bloom coincident with the\n\ntiming of the cruise, and the importance of deep water circulation in this climatically\n\nsensitive gateway region make it an ideal location to investigate sources of REE to\n\nseawater and the effects of vertical cycling and lateral advection on their distribution. The\n\ndeep waters have REE concentrations closest to typical North Atlantic seawater and are\n\ndominated by lateral advection. Comparison to published seawater REE concentrations\n\nof the same water masses in other locations provides a first measure of the temporal\n\nand spatial stability of the seawater REE signal. We demonstrate the REE pattern is\n\nreplicated for Iceland-Scotland OverflowWater (ISOW) in the Iceland Basin from adjacent\n\nstations sampled 16 years previously. A recently published Labrador Sea Water (LSW)\n\ndissolved REE signal is reproduced in the Rockall Trough but shows greater light and\n\nmid REE alteration in the Iceland Basin, possibly due to the dominant effect of ISOW\n\nand/or continental inputs. An obvious concentration gradient from seafloor sediments to\n\nthe overlying water column in the Rockall Trough, but not the Iceland Basin, highlights\n\nrelease of light and mid REE from resuspended sediments and pore waters, possibly\n\na seasonal effect associated with the timing of the spring bloom in each basin. The\n\nEEL dissolved oxygen minimum at the permanent pycnocline corresponds to positive\n\nheavy REE enrichment, indicating maximum rates of organic matter remineralisation\n\nand associated REE release. We tentatively suggest a bacterial role to account for the\n\nobserved heavy REE deviations. This study highlights the need for fully constrained\n\nREE sources and sinks, including the temporary nature of some sources, to achieve\n\na balanced budget of seawater REE.

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.

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)0.002
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.039
Threshold uncertainty score0.316

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0020.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.016
GPT teacher head0.233
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