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Record W4414568263 · doi:10.1016/j.pocean.2025.103578

Holocene oceanographic variability in the Subtropical Northeast Atlantic

2025· article· en· W4414568263 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.

fundA Canadian funder is recorded on the work.
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

VenueProgress In Oceanography · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
FundersInstituto Español de OceanografíaHorizon 2020 Framework ProgrammeUniversity of Toronto MississaugaMinisterio de Ciencia e InnovaciónEuropean Commission
KeywordsHoloceneUpwellingTeleconnectionOcean gyreWesterliesSubtropicsLast Glacial MaximumForaminiferaSeamount

Abstract

fetched live from OpenAlex

• Early Holocene featured weak stratification and possibly year-round upwelling. • Subsurface warming peaked and upwelling weakened during the Middle Holocene. • Late Holocene marked by SST cooling, weaker NASTG, and seasonal upwelling. • Proxies suggest changes in NEABW composition and corrosivity during the Holocene. • Precession and remote forcings shaped complex monsoon–gyre–upwelling interactions. Cabo Verde hosts unique, highly biodiverse marine ecosystems that thrive on volcanic seamounts and island slopes. These ecosystems are shaped by distinct oceanographic dynamics, influenced by the southeastern edge of the North Atlantic Subtropical Gyre (NASTG) and by seasonal upwelling. To explore regional oceanographic variability over time, this study investigates Holocene (last 11.7 ka) sediments using multi-proxy palaeoenvironmental reconstructions from a short core retrieved from ∼ 4,400 m water depth off Cabo Verde. During the Early Holocene, year-round upwelling, or an intensified Guinea Dome, may have inhibited the development of the strong summer stratification characteristic of the modern regional non-upwelling season. Despite humid conditions over the continent, sea surface temperatures (SSTs) remained relatively low during this subepoch, diverging from the present-day pattern in Northwest Africa, where the wet season is marked by weaker upwelling and higher SSTs. This oceanographic state was likely driven by precession-induced insolation changes associated with the precession minimum, which may have modified seasonal regional wind regimes and influenced broader atmospheric processes. Teleconnections related to transitional postglacial conditions and/or continental climate feedbacks, may also have played a role. The Middle Holocene, corresponding to the most humid conditions of this epoch in Northwest Africa, is characterized by reduced upwelling and an eastward expansion of the NASTG, inferred from warmer subsurface conditions at our study site. This interval also provides tentative evidence for enhanced input of North Atlantic Deep Water (NADW) into the Northeast Atlantic Bottom Water (NEABW). During the Late Holocene, intensified upwelling and a reduced influence of the NASTG, possibly due to a westward retraction of its eastern boundary, are suggested at our site, occurring under arid conditions in Northwest Africa. These results highlight that, despite the overall climatic stability of the Holocene, oceanographic conditions off Cabo Verde experienced significant changes in seasonal upper ocean stratification, upwelling, subtropical gyre influence, and deep-water structure. Such insights improve our understanding of regional climate-ocean interactions, helping to refine climate models and improve predictions of ecosystem responses in this sensitive marine region.

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 score0.009
Threshold uncertainty score0.504

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0020.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.003
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.001
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 head0.012
GPT teacher head0.259
Teacher spread0.247 · 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