Introduction to the Special Issue commemorating the 30th anniversary of the Royal Tyrrell Museum of Palaeontology, with a summary of the museum’s early history and its research contributions
Notice bibliographique
Résumé
Located just west of Drumheller, in southern Alberta, Canada, the Royal Tyrrell Museum of Palaeontology (RTMP) is nestled among outcrops of the Upper Cretaceous Horseshoe Canyon Formation exposed along the Red Deer River valley (Fig. 1). Since it officially opened on 25 September 19851, the museum has become one of Alberta’s must-see tourist attractions, a significant contributor to the local economy, and earned an international reputation for the quality of its palaeontological collections and the research conducted by its scientists. The RTMP is unique within Canada in being the only government-supported museum dedicated to palaeontology, and it is one of the few such institutions in the world. Fig. 1. The Royal Tyrrell Museum of Palaeontology. (A) Front of museum and main entrance (circa 2010), looking westwards and with horizontal beds of the Upper Cretaceous Horseshoe Canyon Formation exposed in the walls of the Red Deer River valley in the distance. (B) Aerial photograph, oblique angle and looking to the north-northeast. The museum sits on top of the number 7 coal seam (sensu Gibson 1977) and at the base of the Horsethief Member of the Horseshoe Canyon Formation (D.A. Eberth, pers. comm., 2015). That stratigraphic position correlates with an age of about 71.5 Ma (i.e., late Campanian) and lies within the upper part of the Edmontosaurus regalis – Pachyrhinosaurus canadensis dinosaur assemblage zone (see Eberth et al. 2013, fig. 6). (C) The iconic “running theropod” logo that until recently graced the exterior of the museum, below a life-sized tyrannosaurid sculpture by Brian Cooley (one of many such sculptures by Cooley that have been featured at the museum since its opening in 1985) and with the education wing (opened in 2003 as the ATCO Tyrrell Learning Centre) in the background. (D) The Cretaceous Alberta life-sized diorama (opened in 2007), an example of a RTMP exhibit that relies heavily on discoveries and interpretations by museum researchers, in this case work done in the Albertosaurus bonebed and at other localities throughout the Horseshoe Canyon Formation. All photographs courtesy of the Royal Tyrrell Museum of Palaeontology. This Special Issue of the Canadian Journal of Earth Sciences presents a collection of papers commemorating the RTMP’s 30th or pearl anniversary. Our rationale for doing a 30th anniversary volume was two-fold. First, it is an opportunity to showcase the breadth of research conducted by current and former museum scientists as well as by some colleagues having a history of collaboration with the RTMP. The 13 invited papers included in this volume are a mix of review and original research papers, all thematically focused on the geology and palaeontology of Alberta. To varying degrees, each contribution is the result of work supported by the RTMP and relies on specimens housed in the museum’s collections. Second, the 30th anniversary is an opportunity to reflect on the RTMP’s history and its research program. As is typical for most institutions, the RTMP has done little to formally document its own history. This year likely will be the last major milestone for which the original generation of museum staff are still working and available to share their recollections about the museum, fieldwork, and research. Already, deaths and departures have winnowed away part of the original …
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 | 0,002 | 0,004 |
| Méta-épidémiologie (sens strict) | 0,001 | 0,001 |
| Méta-épidémiologie (sens large) | 0,001 | 0,001 |
| Bibliométrie | 0,003 | 0,002 |
| Études des sciences et des technologies | 0,002 | 0,001 |
| Communication savante | 0,006 | 0,003 |
| Science ouverte | 0,002 | 0,004 |
| Intégrité de la recherche | 0,002 | 0,003 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,157 | 0,076 |
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 ».