Bibliographic record
Abstract
s 29 Late Quaternary chronology of the Arctic: a review of methods and applications 30 An interglacial polar bear and an early Weichselian glaciation at Poolepynten, western Svalbard 31 Identifying changes in Arctic Ocean sea ice conditions north of Greenland during the Holocene 32 Landform assemblage from the collapse of the Bjornoyrenna Ice Stream, Polar North Atlantic 33 Postglacial vegetation history of central Chukotka deduced from permafrost paleoenvironmental records of the El’gygytgyn Impact Crater 34 Rapid response of a major outlet glacier in Greenland, to climate variability over the last century 35 Postglacial Pleistocene of Russian arctic mainland – an overview 36 Sedimentology of the Oulujoki River basin during the Late-Weichselian and Holocene 38 Consequences of northern ice sheet size and melting history for the last interglacial climate 39 Tunnel valleys in the Barents Sea 40 Environmental changes on the northern slope of the Okhotsk Sea during Termination I – MIS 1 and Termination II – MIS 5e: comparison of foraminiferal and biogeochemical data 41 Late Weichselian glacial history of the southern Yermak Plateau Preliminary results of a marine acoustic and sedimentological study 42 Palynological characteristics of MIS 5 marine sediments from northern part of West Siberia 43 Postglacial environmental changes at the eastern Laptev Sea continental margin: evidence from benthic and planktic foraminiferal assemblages 44 Deglacial meltwater discharge, sea-ice cover history and (late) attainment of optimal Holocene conditions in the Baffin Bay and northern Labrador Sea 45 The distribution of late Quaternary glacial-marine deposit on the northernmost part of Novaya Zemlya shelf 46 New geophysical mapping of the Chukchi margin reveals widespread glacial erosion 47 Weichselian ice dammed lakes: New geochemical evidence for a rapidly deposited event-layer in the Eurasian Arctic Basin 48 Preliminary pollen results from the Muhos Core 1; a window to the past environments of northern Fennoscandia 49 The new «PLOT – Paleolimnological Transect» research project: reconstruction of the Late Quaternary climate gradients along Northern Eurasia from lake sediment records and potentials for deep drilling 50 Initial Results from Seafloor Characterization of Arctic and Antarctic Margins using Multibeam Backscatter 51 The last interglacial in the Arctic – warm or cold? 52 Sediments formed during Kazantsevo transgression (MIS 5) in the north of west Siberia 53
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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot 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.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.001 | 0.001 |
| Meta-epidemiology (narrow) | 0.001 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.002 | 0.004 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.002 | 0.001 |
| Open science | 0.000 | 0.001 |
| Research integrity | 0.000 | 0.001 |
| Insufficient payload (model declined to judge) | 0.003 | 0.001 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
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".