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Enregistrement W2809675081 · doi:10.1093/biosci/biy059

New Streams of Thought: Glacial Retreat Creates New Habitat for Salmon

2018· article· en· W2809675081 sur OpenAlexaboutno aff
Lesley Evans Ogden

Notice bibliographique

RevueBioScience · 2018
Typearticle
Langueen
DomaineEnvironmental Science
ThématiqueFish Ecology and Management Studies
Établissements canadiensnon disponible
Organismes subventionnairesnon disponible
Mots-clésSTREAMSGlacial periodHabitatGeographyFisheryEcologyGeologyComputer scienceBiologyPaleontology

Résumé

récupéré en direct d'OpenAlex

Glaciers cover 10 percent of our planet's land surface, but as our climate warms, many glaciers are shrinking. As glacial retreat proceeds northward along the Pacific coast of the continental United States, through Canada, to Alaska, it is creating new stream habitat for salmon that has not existed in millennia. When and how will this new stream rollout happen? Where will salmon be distributed in the future? These questions are the focus of a newly formed multidisciplinary working group led by Canadian and US researchers. The research collaboration is the brainchild of Kara Pitman, Jonathan Moore, and Matthew Sloat. Moore, an aquatic ecologist and conservation scientist who heads the Vancouver, British Columbia–based Simon Fraser University's Salmon Watersheds Laboratory, supervises Pitman, a PhD student. Sloat is director of science at the Wild Salmon Center, in Portland, Oregon. The new Glacial Retreat and Salmon Futures working group is part of the Salmon Science Network that Moore coleads, supported by the Gordon and Betty Moore Foundation (no relation to Jonathan Moore). After completing a master's degree in glacial studies, Pitman came to her doctoral work “excited about looking at how glacial retreat would have impacts on salmon and salmon habitat,” she says. She realized early on that a working group would need to include representatives of multiple scientific disciplines. The group's first in-person meeting, held in November 2017 in Vancouver, brought together 15 experts from the United States, Canada, and the United Kingdom to share expertise in fish biology, climate change, river ecosystems, hydrology, and glaciology. In addition, Swiss glaciologist Matthias Huss recently came on board. As the team's first step, Pitman is spearheading a research literature survey for a forthcoming review paper. A second focus digs deeply into the empirical data to better understand watershed and salmon changes on the glacier-fed Copper River in Alaska. Third, for watersheds from Oregon to Alaska, the team is using glacial-retreat and climate projection models to map out how streams and lakes emerge from under ice. “For the [roughly] 40,000 glaciers up and down the coast, [the team] will be predicting how those will march up the valleys,” says Moore. Salmon are better known for their homing instincts than for their colonization of new habitats. But salmon do not always return to their natal streams. Rates vary widely by species, but genetic studies indicate that as many as 15 percent of salmon stray to new territory for spawning. It is these errant salmon that exploit the novel streams that are opening up as glaciers retreat. In Glacier Bay, Alaska, working group member Alexander Milner, of Birmingham University, in England, has watched glacial retreat birth new streams since the late 1970s. Within just a few decades, for example, he witnessed Stonefly Creek—an icy stream initially devoid of fish—transform into a waterway that now supports thousands of pink, coho, and sockeye salmon. Milner's wider analysis of glaciers suggests that there are “tipping points of glacial cover where there is a switch in the community,” he says. The repercussions are complex. As glaciers retreat, the thermal shift increases local aquatic species diversity. At the same time, there is a loss of rare endemic species, such as cold stenothermic organisms that can only survive within narrow temperature limits. Researchers are only beginning to understand the complex ecological cascades that glacial retreat is stimulating. Climate-induced glacier loss also produces profound downstream effects on hydrology, sediment transport, and biogeochemical and contaminant fluxes. Chemicals locked up in ice for decades can be released as ice melts, releasing such legacy contaminants as black carbon, mercury, and persistent organic pollutants, including polychlorinated biphenyls (PCBs), polychlorinated dibenzo-p-dioxins and dibenzofurans (PCDD/Fs), and dichlorodiphenyl trichloroethane (DDT), into meltwaters. To understand how the multiplicity of physical, chemical, and biological changes will play out for salmon as glaciers retreat, the Glacial Retreat and Salmon Futures group has their work cut out for them, including maintaining an openness and sense of humor about dealing with communication challenges that come with team members working across many disciplines and in many locales. Going forward, what they learn will be critical for salmon conservation. In environmental assessments for proposed projects, “we envision things as they currently are,” says Pitman. For example, a mine approved for construction in a currently heavily glaciated area may not threaten salmon now, she explains, but it might threaten salmon futures. Like the habitats emerging and exploited by life as glaciers melt away, the diverse group is spawning new streams of thought.

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 distillée sur la base complète

Imitation des enseignants

Ni prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.

score de la tête « metaresearch » (Codex)0,000
score de la tête « metaresearch » (Gemma)0,000
Version: codex-gemma-dda1882f352aStatut de validation: machine_predicted_unvalidated
Catégories candidatesaucune
Catégories consensuellesaucune
DomaineSignal candidat: aucune · Signal consensuel: aucune
Devis d'étudeSignal candidat: Observationnel · Signal consensuel: aucune
GenreSignal candidat: Empirique · Signal consensuel: Empirique
Score de désaccord entre enseignants0,481
Score d'incertitude au seuil0,715

Scores Codex et Gemma par catégorie

CatégorieCodexGemma
Métarecherche0,0000,000
Méta-épidémiologie (sens strict)0,0000,000
Méta-épidémiologie (sens large)0,0000,000
Bibliométrie0,0000,000
Études des sciences et des technologies0,0000,001
Communication savante0,0000,000
Science ouverte0,0000,000
Intégrité de la recherche0,0000,000
Charge utile insuffisante (le modèle a refusé de juger)0,0010,000

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.

Tête enseignante Opus0,014
Tête enseignante GPT0,246
Écart entre enseignants0,232 · la distance entre les deux têtes enseignantes sur ce seul travail
Statut de validationscore_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 découle

Classification

machine, non validée

Prédiction automatique; un appel candidat d’une seule tête enseignante, pas un consensus.

Les modèles n’ont appliqué aucune catégorie : rien dans la taxonomie ne correspondait à ce travail.
Devis d'étudeObservationnel
Domainenon disponible
GenreEmpirique

Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».

En bref

Citations0
Publié2018
Routes d'admission1
Résumé présentoui

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