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The article discusses the discovery of a fossil within Canada's Devon Island that provides a link in the evolution of pinniped ancestry. It was discovered by undergraduate researcher Elizabeth Ross while traveling with a palaeontology filed crew. The crew was headed by Canadian Museum of Nature palaeobiologist Natalia Rybczynski, who provides quotes.

The Back River Project is an approved gold mine in Nunavut, Canada owned by Sabina Gold & Silver Corp. Sabina developed a comprehensive community engagement program during the environmental assessment phase of the Project to share information, receive and address local feedback and concerns, and develop productive relationships in support of Project advancement. This paper outlines Sabina's engagement program, successes and challenges encountered from the perspective of a mineral developer, and insights obtained for effective community engagement in a Canadian Arctic context. The program has been commended by observers and is consistent with best practice models. Sabina's experiences revealed the importance of engaging early and often using a context-specific approach; comprehensive record-keeping and reporting; the meaningful incorporation of community perspectives and Traditional Knowledge; and focusing on long-term relationships, partnerships, and local benefits. Effective community engagement subsequently played a key role in Sabina securing major licenses and permits for Project advancement. [ABSTRACT FROM AUTHOR]

When faced with a species that is seldom encountered or discussed, can local or indigenous people piece together their accumulated experience to make inferences about the ecology of that species? In this paper the Greenland shark acts as a model to study how the Inuit of southern Baffin Island are able to produce ecological knowledge. We examine experiential information, reflections, variations in knowledge, and sense-making related to the Greenland Shark, and present a knowledge co-production process based on heuristic reasoning. The process of knowledge co-production has similarities to fuzzy logic, and highlights the adaptability and versatility of indigenous knowledge systems to generate new understandings about the species and its role in the Arctic marine environment. Interactions between the Inuit and researchers can provide a forum to facilitate knowledge co-production, and can be used as a strategy to engage the Indigenous and traditional peoples in resource management and conservation. [ABSTRACT FROM AUTHOR]

This paper provides ethnographic and historical evidence for the existence, in time and space, of a network of well-established trails connecting most Inuit settlements and significant places across the Canadian Arctic. The geographic and environmental knowledge relating to trails (and place names associated with the trails) has been orally transmitted through many generations of Inuit. I use historical documents, ethnographic research, and new geographic tools such as GPS, GIS and Google Earth, to show the geographic extent of the network and its historical continuity. I particularly draw on a trip following Inuit along a traditional trail connecting the communities of Iglulik and Naujaat (Repulse Bay). Inuit have made systematic use of the Arctic environment as a whole and trails are, and have been, significant channels of communication and exchange across the Arctic. There are some types of oral history and knowledge that can be accurately transmitted through generations, and I propose that some aspects of Inuit culture are better understood in terms of moving as a way of living. [ABSTRACT FROM AUTHOR]

Brucella serostatus was evaluated in 3189 muskoxen sampled between 1989 and 2016 from various locations of the Canadian Arctic archipelago and mainland, near the communities of Sachs Harbour and Ulukhaktok, Northwest Territories, and Cambridge Bay and Kugluktuk, Nunavut. Brucella antibodies were found only in muskoxen sampled around Cambridge Bay, both on southern Victoria Island and on the adjacent mainland (Kent Peninsula). Consistent with participatory epidemiology data documented from local harvesters describing increased Brucella-like syndromes (swollen joints and lameness) and a decreased proportion of juveniles, the apparent Brucella seroprevalence in the sampled muskoxen of the Cambridge Bay area increased from 0.9% (95% CI 0.3–2.1) in the period of 1989–2001 to 5.6% (95% CI 3.3–8.9) in 2010–2016. The zoonotic bacteria Brucella suis biovar 4 was also cultured from tissues of muskoxen sampled on Victoria Island near Ulukhaktok in 1996 (n = 1) and Cambridge Bay in 1998, 2014, and 2016 (n = 3). Overall, our data demonstrate that B. suis biovar 4 is found in muskoxen that are harvested for food and by guided hunts on Victoria Island and Kent Peninsula, adding an important public health dimension to this study. Robust participatory epidemiology data on muskox health and diseases greatly enhanced the interpretation of our Cambridge Bay data and, combined with the serological and microbiological data, provide compelling evidence that the prevalence of B. suis biovar 4 has increased in this area since the late 1990s. This study enhances the available knowledge on Brucella exposure and infection in muskoxen and provides an example of how scientific knowledge and local knowledge can work together to better understand disease status in wildlife. [ABSTRACT FROM AUTHOR]

In the Hudson-James Bay system, grubbing and grazing by lesser snow geese have resulted in severe devegetation of coastal marshes. These changes likely represent an example of an alternative stable state; however, long-term datasets documenting whether revegetation is occurring are scarce. Here, we report results of a 10-year study investigating changes in the state of a degraded salt marsh system on the north coast of Akimiski Island, Nunavut. Four transects were intensively sampled in 1998 and 2008, two within the dense nesting and brood-rearing area of a snow geese colony, one on the colony edge, and one outside it; all of these sites were also used by broods of Canada geese. Key forage species ( Puccinellia phryganodes, Festuca rubra, Carex subspathacea) were less common near the colony center than elsewhere; biomass of Puccinellia also tended to be lower in more central areas. Forage species often increased in abundance between samplings, but the magnitude of changes was small. In contrast, non-forage species ( Salicornia, Spergularia, Glaux) often reached high abundance within the colony center; some ( Salicornia) decreased while others ( Spergularia) increased. We argue the degraded state was initiated by foraging damage from an exceptional stopover of 295,000 staging birds in 1972 and that the combined foraging pressure of relatively small numbers of nesting and migrant geese since then, coupled with soil changes, has been sufficient to maintain devegetated areas as a persistent alternative state. Whether or not this state is truly stable, further recovery is likely to be very slow. [ABSTRACT FROM AUTHOR]

The spatial (i.e. microhabitat) and temporal (i.e. seasonal) characteristics of diatom assemblages in adjacent High Arctic lakes were studied intensively June-August 2004. These baseline data are used to improve understanding of modern diatom community dynamics, as well to inform paleoenvironmental reconstructions. Diatoms were collected approximately weekly through the melt season from each principal benthic substrate (moss/macrophyte, rock scrapes, littoral sediment), plankton, and sediment traps, and were compared to the uppermost 0.5 cm of a surface core obtained from the deepest part of the lake where sediment cores are routinely collected. Water samples were collected concurrently with diatom samples to investigate species-environment relationships. The lakes share approximately half of their common taxa, the most abundant overall in both lakes being small Cyclotella species. Results of detrended correspondence analysis (DCA) indicate that the largest gradient in species turnover existed between benthic and planktonic communities in both lakes, and that sediment trap and the surface core top samples most closely resemble the planktonic assemblage, with an additional contribution from the lotic environment. Our results indicate clear micro-spatial controls on species assemblages and a degree of disconnection between the benthos and deep lake sediments that manifests as an under-representation of benthic taxa in deep lake surface sediments. These findings are particularly relevant in the context of interpreting the paleoenvironmental record and assessing ecosystem sensitivity to continued climate change. [ABSTRACT FROM AUTHOR]

Individuals breeding in seasonal environments are under strong selection to time reproduction to match offspring demand and the quality of the post-natal environment. Timing requires both the ability to accurately interpret the appropriate environmental cues, and the flexibility to respond to inter-annual variation in these cues. Determining which cues are linked to reproductive timing, what these cues are predicting and understanding the fitness consequences of variation in timing, is therefore of paramount interest to evolutionary and applied ecologists, especially in the face of global climate change. We investigated inter-annual relationships between climatic variation and the timing of reproduction in Canada’s largest breeding population of Arctic common eiders ( Somateria mollissima) in East Bay, Nunavut. Warmer spring temperatures predicted both earlier mean annual laying dates and the earlier ice-free conditions required by ducklings for post-natal growth. Warmer springs had higher variation in this temperature cue, and the population laying distribution became increasingly positively-skewed in warmer summers, potentially indicating that more low-quality females had the opportunity to commence laying in warmer years. Females that timed laying to match duckling hatching just prior to fully ice-free conditions obtained the highest duckling survival probability. Inter-annual data on repeated breeding attempts revealed that the individuals examined show a similar degree of laying flexibility in response to climatic variation; however, there was significant individual variation in the absolute timing of laying within an average year. This work sheds light on how reproductive timing is related to and influenced by variation in local climate and provides vital information on how climate-related variation in reproductive timing influence a fitness measure in an Arctic species. Results are especially relevant to future work in polar environments given that global climatic changes are predicted to be most intense at high latitudes. [ABSTRACT FROM AUTHOR]

Cultural eutrophication is one of several environmental stressors that represents a significant ecological threat as the human population continues to grow and encroach on aquatic ecosystems. However, until recently, the environmental impacts of ancient human populations that had low population densities were thought to be largely insignificant relative to those of post-industrial urban society. Based on paleolimnological and archeological data, we have shown that Thule Inuit whalers living in small, nomadic communities were altering High Arctic pond ecology centuries before industrialization. Changes in diatom species assemblage and spectrally inferred aquatic primary production indicate a period of increased production in a pond (E-Knud) on Knud Peninsula, Ellesmere Island, which can be linked to the effects of the Thule from about 810–340 years ago. This site is near the northernmost region of past Thule occupation. Input of nutrients from bowhead whale carcasses, used by the Thule Inuit for sustenance and the construction of winter settlements, as well as other Thule activities (e.g., sealing, human waste, etc.), resulted in an increase in δ15N, which coincided with ecologically significant diatom abundance changes, including an increase in Amphora ovalis. Diatom and nutrient changes also coincided with increased primary aquatic production, as measured by spectrally inferred chlorophyll a concentration. In addition, we recorded relative increases in diatom taxa such as Craticula halophila and Achnanthidum minutissimum in the more recent sediments, which we attribute to recent climate warming, manifested by lower water levels and associated evapo-concentration. Specific conductivities recorded during three sampling years (2004, 2006, 2009) show a trend of increasing conductivity in pond E-Knud in response to declining water levels. Together these changes in diatom species abundance suggest that multiple environmental stressors, operating several centuries apart, have led to marked limnological changes in E-Knud pond. [ABSTRACT FROM AUTHOR]

Allochthonous nutrient subsidies play an important role in shaping biotic communities, particularly in naturally oligotrophic ecosystems such as those commonly found in the Canadian High Arctic. Seabirds have been identified as an important vector capable of transporting significant quantities of nutrients from marine to terrestrial environments. However, the influence of seabird-derived nutrients on water quality and ecosystem functioning of Arctic freshwater systems has been largely unexplored. Here, we sampled 24 ponds on Cape Vera, Devon Island (Nunavut, Arctic Canada), an area that is home to over 10,000 nesting pairs of northern fulmars ( Fulmarus glacialis), in order to explore the influence of seabirds on water quality and diatom ecology. Our data reveal distinctive water chemistry changes (e.g., high pH, nutrients) and diatom assemblages (e.g., very low diversity) related to varying degrees of bird influence. Using δ15N as a proxy of trophic level, we show that a small but significant portion of the variance in the diatom species data can be explained by seabird-derived nutrients. Although the generation of robust quantitative models predicting δ15N from fossil diatom data was limited by the overwhelming dominance of a few taxa, this study provides evidence that seabird-derived nutrients play a critical role in influencing the water quality of Arctic ponds. Interestingly, diatom assemblage composition does not respond in a simple fashion to seabird-derived nutrients, in contrast to diatom–nutrient relationships recorded in many temperate regions. [ABSTRACT FROM AUTHOR]

Many public land management agencies are committed to understanding and protecting recreation visitor experiences. Parks Canada is deeply committed to that objective for visitors to Canada’s National Parks. This 2004 study, informed by a 2003 qualitative study of visitor experiences and influences on those experiences at Auyuittuq National Park in Nunavut, worked to bring 50 potential elements of visitor experiences down to five articulated dimensions of the experience that is currently being received at this remote eastern arctic park. A hypothesized set of 17 influences on experiences, also reduced to just two factors with similar response patterns, and with some items that did not flow into the two factors, were used in a regression analysis to understand the relationship between experiences and factors of influence. A sample of 61.8% (84) of the total recreation visitor population 16 years of age or older was surveyed during deregistration after the trip. Knowledge about the dimensions of the experiences currently received and factors of influence on those experiences can be used to guide selection of indicators for describing objectives and prescribing monitoring protocol. [ABSTRACT FROM AUTHOR]

Studies the physical, chemical and biological characteristics of Meretta Lake in Cornwallis Island, Nunavut, between 1992 and 1999 to determine its rate of eutrophication. Media through which the lake has been receiving sewage since 1949; Decline in nutrient concentrations of the lake; Decrease in eutrophication of the lake during 1990s.

A peat deposit on Ellesmere Island, Nunavut, Canada, allows a unique glimpse of the Early Pliocene terrestrial biota north of the Arctic Circle. The peat accumulated in a beaver pond surrounded by boreal larch forest near regional tree line in coastal hills close to the Arctic Ocean. The ecological affinities of the plant and beetle remains contained in the peat indicate that winter temperatures on Ellesmere Island were nearly 15?°C higher and summer temperatures 10?°C higher than they are today. Here we show that the mammalian remains buried in the peat represent mainly taxa of Eurasiatic zoogeographic and phyletic affinities, including the first North American occurrence of a meline badger (Arctomeles). This deposit contains direct evidence of the composition of an Early Pliocene (4-5 million years ago) arctic mammalian fauna during an active period of interchange between Asia and North America. [ABSTRACT FROM AUTHOR]

The high 3He/4He ratio of volcanic rocks thought to be derived from mantle plumes is taken as evidence for the existence of a mantle reservoir that has remained largely undegassed since the Earth's accretion. The helium isotope composition of this reservoir places constraints on the origin of volatiles within the Earth and on the evolution and structure of the Earth's mantle. Here we show that olivine phenocrysts in picritic basalts presumably derived from the proto-Iceland plume at Baffin Island, Canada, have the highest magmatic 3He/4He ratios yet recorded. A strong correlation between 3He/4He and 87Sr/86Sr, 143Nd/144Nd and trace element ratios demonstrate that the 3He-rich end-member is present in basalts that are derived from large-volume melts of depleted upper-mantle rocks. This reservoir is consistent with the recharging of depleted upper-mantle rocks by small volumes of primordial volatile-rich lower-mantle material at a thermal boundary layer between convectively isolated reservoirs. The highest 3He/4He basalts from Hawaii and Iceland plot on the observed mixing trend. This indicates that a 3He-recharged depleted mantle (HRDM) reservoir may be the principal source of high 3He/4He in mantle plumes, and may explain why the helium concentration of the 'plume' component in ocean island basalts is lower than that predicted for a two-layer, steady-state model of mantle structure. [ABSTRACT FROM AUTHOR]

The Big Lake shear zone (BLsz) is a 60 km long deep crustal structure adjacent to the northern segment of the Snowbird Tectonic zone (STZ: Nunavut, Canada) in a region characterized by intensely sheared high-pressure granulite-facies rocks. The units exposed here provide an exceptional record of the lower crust that preserves crucial evidence bearing on interpretation of superimposed Neoarchean and Paleoproterozoic tectono-metamorphic events. Deformation along the BLsz postdates 2650 Ma, the age of a mylonitized monzogranite, and predates 2190 Ma, the age of cross-cutting MacQuoid mafic dykes. Metamorphic assemblages and P–T modeling suggest crustal thickening in the Neoarchean with peak conditions of 800 °C and 14–15 kbar at ca. 2530 Ma. Mylonitic fabrics developed at ca. 2505 Ma (T ~ 800 °C, P < 13 kbar). P–T data on the metamorphosed Paleoproterozoic dykes suggest ca. 1900 Ma recrystallization and partial reactivation of the BLsz at 770 °C–13 kbar. In this work, we demonstrate that U–Pb geochronology and diffusion modeling in Neoarchean titanite can be used to resolve time–temperature paths for lower crustal rocks. Preservation of Nb and Ta zoning with sharp boundaries in titanite and diffusion models of geochemical tracers (e.g., Pb), are indicative of a scenario involving fast cooling (> 10 °C/Ma) and partial exhumation post-ca. 2505 Ma followed by re-burial at 1900 Ma, rather than slower isobaric cooling at depth. These results indicate that the long-term residence models proposed by several authors for domains in the central STZ are not applicable to the BLsz region, and are more compatible with a ca. 1.9 Ga collisional setting. [ABSTRACT FROM AUTHOR]

Objectives: In 2014-2015, over 400 social housing units were constructed in selected communities in Nunavik and Nunavut, two Inuit regions in northern Canada where housing shortages and poor quality housing are endemic and undermine population health. This paper presents results from a before-and-after study examining the effects of rehousing, i.e., relocating to a newly constructed or pre-existing social housing unit, on psychosocial health and asthma-related symptoms for Inuit adults., Methods: Baseline data were collected 1-6 months before, and follow-up data 15-18 months after rehousing. Of the 289 participants at baseline, 186 were rehoused. Of the 169 participants eligible at follow-up, 102 completed the study. Self-reported health measures included psychological distress, perceived stress in daily life, perceived control over one's life, and asthma-related symptoms. Data are analyzed using multilevel models for longitudinal data., Results: After adjusting for age, sex, and region of residence, participants reported significantly lower levels of psychological distress and perceived stress in daily life, and improved sense of control over their lives 15 to 18 months after rehousing. Participants were also significantly less likely to report asthma-related symptoms at follow-up., Conclusion: Significant positive health impacts are observed for adults who relocated to newly constructed or pre-existing social housing units. Increasing investments to redress the housing situation across Inuit Nunangat is required, not only to improve living conditions but also to improve the health and well-being of the population.