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Fabrice Calmels

Researcher at Yukon College

Publications -  26
Citations -  2458

Fabrice Calmels is an academic researcher from Yukon College. The author has contributed to research in topics: Permafrost & Thermokarst. The author has an hindex of 12, co-authored 23 publications receiving 2001 citations. Previous affiliations of Fabrice Calmels include Laval University & Centre national de la recherche scientifique.

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Antibiotic resistance is ancient

TL;DR: Target metagenomic analyses of rigorously authenticated ancient DNA from 30,000-year-old Beringian permafrost sediments are reported and show conclusively that antibiotic resistance is a natural phenomenon that predates the modern selective pressure of clinical antibiotic use.
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Internal structure and conditions of permafrost mounds at Umiujaq in Nunavik, Canada, inferred from field investigation and electrical resistivity tomography

TL;DR: In this article, a systematic approach was used for the interpretation of the electrical resistivity tomography carried out on two permafrost mounds at Umiujaq in Nunavik, Canada, to assess their internal structure.
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Development and decay of a lithalsa in Northern Québec: A geomorphological history

TL;DR: In this article, the complete life cycle of a permafrost mound is reconstructed from its growth until its degradation, and the study site is a lithalsa, which is the subject of a long-term monitoring that includes geocryological observations, measurements of permfrost properties on cores, ground temperature measurements, and observations of landform changes.
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Segregated ice structures in various heaved permafrost landforms through CT Scan

TL;DR: In this article, the growth of segregated ice lenses in frost susceptible sediments in the discontinuous permafrost zone is the dominant mechanism for the formation of permaferost mounds, such as palsas, lithalsas and permafeur plateaus.
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Ice Segregation and Gas Distribution in Permafrost using Tomodensitometric Analysis

TL;DR: In this paper, the shape and spatial distribution of gaseous inclusions in the permafrost provide some clues on gas source and on the thermo-mechanics of ice segregation during aggradation.