Notice bibliographique
Résumé
11 DECEMBER 1919 * 8 DECEMBER 2004 DIGBY JOHNS McLAREN was born 11 December 1919 in Carrickfergus, County Antrim, Northern Ireland, and died 8 December 2004 in Ottawa, Ontario, Canada. He was predeceased in 2003 by his wife of sixty-one years, Phyllis Mary (Matkin), and is survived by their sons, Ian and Patrick, and their daughter, Alandra. Digby McLaren was a brilliant scientist and a visionary and inspiring leader within the Geological Survey of Canada, the Royal Society of Canada, and the Canadian, North American, and global geoscience communities. Digby attended St. Mary's School, Roxburghshire, Scotland, and Sedbergh School, Yorkshire, England, before entering Queen's College, Cambridge University, where he received a B.A. Natural Sciences, Part I, Geology, Mineralogy, Chemistry, in 1940. During World War II he served from 1940 to 1946 in the British army, Royal Artillery. For three and a half years he experienced the human misery and horrors of war as an artillery officer in the Middle East and in Italy, where he participated in the battle for Ortona. His first scientific paper, published in 1946 (in Italian), was on local geology in the Italian province of Perugia. In 1948 he received an M.A. Natural Sciences, Part II (First Class Honours), Geology, Paleontology, from Cambridge University. That year he joined the Paleontology section of the Geological Survey of Canada (GSC) in Ottawa, and began his studies of the Devonian rocks of western Canada. Digby McLaren was a remarkably gifted individual who had the good fortune to be in the right place at the right time. He arrived in Canada shortly after the unexpected 1947 discovery of a giant oil field in Upper Devonian (375-385 million years old) stromatoporoid-coral reefs at Leduc, near Edmonton, Alberta, an event that launched the amazing growth of Canada's oil and gas industry and sparked intense interest in the Devonian stratigraphy of western Canada. His initial research assignment in the GSC was to do the He began by studying the superbly exposed Upper Devonian strata in the nearby Rocky Mountains that are laterally equivalent to the Leduc reefs. Digby quickly mastered the intricacies of Upper Devonian regional and local reef-margin stratigraphy and the taxonomy of the Upper Devonian fossil brachiopods and corals that helped to elucidate many important aspects of the nature, origin, and evolution of the petroleum resource system. With encouragement and support from the GSC, he was able to fulfill the requirements for a Ph.D. in geology and paleontology at the University of Michigan by 1951. The scope of Digby's scientific experience expanded rapidly with his participation, in 1955, in Operation Franklin, a GSC aircraft-supported reconnaissance study of an immense area in Canada's western Arctic archipelago, and, in 1957, in Operation Mackenzie, a GSC helicopter-supported geological regional mapping project in the Mackenzie Mountains of the Northwest Territories. His research interests became focused on regional and global stratigraphic correlations and, in particular, on one of the global mysteries in the evolution of life on Earth-an abrupt mass extinction that occurred about 375 million years ago, between the Frasnian and Fammenian stages of the Upper Devonian. This extraordinary global event, marked by the abrupt disappearance of many species and families of organisms, including the obliteration of the Frasnian reef ecosystem that was responsible for the generation and entrapment of the petroleum at Leduc, was recognizable around the world. In his 1969 presidential address to the Paleontological Society, Digby's analysis of the available evidence led him to the conclusion that the most likely cause was an impact with a giant meteorite that disrupted the normal functioning of Earth's atmosphere, oceans, and biosphere. This bold hypothesis was controversial; it challenged prevailing ideas that favoured stable, gradual, non-catastrophic evolution of the Earth system. …
Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.
Comment cette classification a été obtenuedéplier
Prédiction machine sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Le volet Gemma est une étiquette directe du modèle pour chaque travail de la base, lue sur la notice réduite au titre. Le volet Codex est un classifieur appris des 10 348 étiquettes directes de Codex et calibré sur les taux pondérés de l'échantillon; les champs sans appui suffisant ne portent aucun appel Codex. Le mode candidate est l'union des deux volets; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont pas des étiquettes humaines.
Scores du classifieur distillé par catégorie (deux têtes)
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,001 | 0,005 |
| Méta-épidémiologie (sens strict) | 0,001 | 0,000 |
| Méta-épidémiologie (sens large) | 0,001 | 0,000 |
| Bibliométrie | 0,003 | 0,003 |
| Études des sciences et des technologies | 0,008 | 0,002 |
| Communication savante | 0,005 | 0,003 |
| Science ouverte | 0,002 | 0,005 |
| Intégrité de la recherche | 0,002 | 0,004 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,135 | 0,049 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule source (Gemma direct ou Codex distillé), pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».