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Record W194169721

The Middle Eocene Climatic Optimum (MECO) in the high northern latitudes: biotic and climatic consequences

2012· dissertation· en· W194169721 on OpenAlexaboutno aff
Marcel Polling

Bibliographic record

VenueUtrecht University Repository (Utrecht University) · 2012
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
Fundersnot available
KeywordsLatitudeGeographyBiotic componentGeologyPhysical geographyClimatologyPaleontologyAbiotic component
DOInot available

Abstract

fetched live from OpenAlex

The so-called ‘Middle Eocene Climatic Optimum’ (MECO, ~40 Ma) represents a ~500-750 kyr period of transient climate warming followed by marked cooling superimposed on the long-term middle and late Eocene cooling trend (~50-34 Ma). The MECO, with the onset calibrated against magnetosubchron C18n.2n was originally recognized in sediments from the Southern Ocean but later also identified in records from the equatorial Atlantic Ocean and the central Tethyan Realm. Based on dinoflagellate cysts and organic geochemistry, this study provides the first evidence of the influence of the MECO in the higher northern latitudes, thereby confirming that it indeed was a truly global event. The studied middle to upper Eocene sediments from the Labrador Sea (Ocean Drilling Program, ODP, Site 647, 53ºN) and Norwegian-Greenland Sea (ODP Site 913, 75ºN) show a relative abundance peak in typical low latitude organic-walled dinocyst species and a strong drop in productivity at the base of magnetosubchron C18n.2n that are related to the MECO. The MECO coincides with carbonate dissolution while the organic molecular paleothermometer TEX86 shows a concomitant brief (~150 kyr) warming in sea surface temperatures (SSTs) at ODP Site 647. Warming during the MECO thus allowed typical low latitude dinocyst species to bloom in the high northern latitudes. The strong productivity collapse during the MECO possibly results from shifting water masses. Alternatively, since the signal recovered seems to be transported from elsewhere, changes in the source area (e.g. decreased runoff) may have caused productivity to drop during the MECO. Furthermore, post-MECO cooling (~6ºC for Site 647) allowed several typical cold-water adapted dinocyst species to occur. While this biotic change is similar to that found in the Southern Ocean, the duration and amount of warming are very different. This is possibly related to carbonate dissolution that may have had a larger influence in the high northern latitudes and caused a large part of the MECO signal to be missing at the studied high northern latitude sites.

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 score0.010
Threshold uncertainty score0.020

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.001
Scholarly communication0.0010.000
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.019
GPT teacher head0.195
Teacher spread0.176 · 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

Citations1
Published2012
Admission routes1
Has abstractyes

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