Variation in body size of ringed seals (Pusa hispida hispida) across the circumpolar Arctic: evidence of morphs, ecotypes or simply extreme plasticity?

The ringed seal is a small phocid seal that has a northern circumpolar distribution. It has long been recognized that body size is variable in ringed seals, and it has been suggested that ecotypes that differ in size exist. This study explores patterns of body size (length and girth) and age-at-maturity across most of the Arctic subspecies’ range using morphometric data from 35 sites. Asymptotic lengths varied from 113 to 151 cm, with sites falling into five distinct size clusters (for each sex). Age-at-maturity ranged from 3.1 to 7.4 years, with sites that had early ages of sexual maturity generally having small length-at-maturity and small final body length. The sexes differed in length at some sites, but not in a consistent pattern of dimorphism. The largest ringed seals occurred in western Greenland and eastern Canada, and the smallest occurred in Alaska and the White Sea. Latitudinal trends occurred only within sites in the eastern Canadian Arctic. Girth (with length and season accounted for) was also highly variable but showed no notable spatial pattern; males tended to be more rotund than females. Genetic studies are needed, starting with the “giants” at Kangia (Greenland) and in northern Canada to determine whether they are genetically distinct ecotypes. Additional research is also needed to understand the ecological linkages that drive the significant regional size differences in ringed seals that were confirmed in this study, and also to understand their implications with respect to potential adaptation to climate change.

Nunamiut, the Tundra Dwellers

This article investigates the various senses and derivations of the term nuna in the Inuit-Yupik languages in order to reveal its origin in referring to the Arctic tundra. These languages arguably derive from that of the ancestors of the earliest inhabitants of the North American tundra, other inhabitants of the circumpolar Arctic today having only moved up at later times. Likely etymological correspondences in Eurasian languages of the far north support the original meaning of the word, whose connotations can be contrasted with those of English land, by which it is usually translated. They include reference to the unique vegetation of the Arctic tundra and to settlement and migratory movements across it in the past. The word has survived through millennia as far apart as mountainous East Greenland and the Aleutian Islands chain, where it has been adapted (as Unangan tanaX) to the archipelagic setting. It is suggested that the term nunamiut, literally “tundra dwellers,” can suitably be applied to speakers of all these languages still today.

Community composition of aquatic fungi across the thawing Arctic

Thermokarst activity at permafrost sites releases considerable amounts of ancient carbon to the atmosphere. A large part of this carbon is released via thermokarst ponds, and fungi could be an important organismal group enabling its recycling. However, our knowledge about aquatic fungi in thermokarstic systems is extremely limited. In this study, we collected samples from five permafrost sites distributed across circumpolar Arctic and representing different stages of permafrost integrity. Surface water samples were taken from the ponds and, additionally, for most of the ponds also the detritus and sediment samples were taken. All the samples were extracted for total DNA, which was then amplified for the fungal ITS2 region of the ribosomal genes. These amplicons were sequenced using PacBio technology. Water samples were also collected to analyze the chemical conditions in the ponds, including nutrient status and the quality and quantity of dissolved organic carbon. This dataset gives a unique overview of the impact of the thawing permafrost on fungal communities and their potential role on carbon recycling.

Sila qanuippa? (how's the weather?): Integrating Inuit Qaujimajatuqangit and environmental forecasting products to support travel safety around Pond Inlet, Nunavut in a changing climate

As Inuit hunters living in Pond Inlet, Nunavut, we (Natasha Simonee and Jayko Alooloo) travel extensively on land, water, and sea ice. Climate change, including changing sea ice and increasingly unpredictable weather patterns, has made it riskier and harder for us to travel and hunt safely. Inuit knowledge supporting safe travel is also changing and shared less between generations. We increasingly use online weather, marine, and ice products to develop locally relevant forecasts. This helps us to make decisions according to wind, waves, precipitation, visibility, sea ice conditions, and floe edge location. We apply our forecasts and share them with fellow community members to support safe travel. In this paper, we share the approach we developed from over a decade of systematically and critically assessing forecasting products such as: Windy.com; weather and marine forecasts; tide tables; C-CORE’s floe edge monitoring service; SmartICE; ZoomEarth; and time lapse cameras. We describe the strengths and challenges we face when accessing, interpreting, and applying each product throughout different seasons. Our analysis highlights a disconnect between available products and local needs. This disconnect can be overcome by service providers adjusting services to include: more seasonal and real-time information, non-technical language, familiar units of measurement, data size proportional to internet access cost and speed, and clear relationships between weather/marine/ice information and safe travel. Our findings have potential relevance in the Circumpolar Arctic and beyond, wherever people combine Indigenous weather forecasting methods and online information for decision-making. We encourage service providers to improve product relevance and accessibility.

The “Cribrilina annulata" problem and new species of Juxtacribrilina (Bryozoa: Cheilostomata: Cribrilinidae) from the North Pacific

Originally described from Greenland, Juxtacribrilina annulata (Fabricius, 1780) (previously known as Cribrilina annulata) has long been regarded as having a circumpolar, Arctic-boreal distribution. The genus Juxtacribrilina Yang, Seo, Min, Grischenko & Gordon, 2018 accommodated J. annulata and three related North Pacific species formerly in Cribrilina Gray, 1848 that lack avicularia, have a reduced (hood-like, cap-like, or vestigial) ooecium closely associated with modified latero-oral spines to form an ooecial complex, and produce frontally or marginally positioned dwarf ovicellate zooids. While the recently described NW Pacific species J. mutabilis and J. flavomaris, which have a vestigial ooecium like a short, flattened spine, clearly differ from J. annulata, the differences between J. annulata and other Pacific populations remained unclear. Here we provide descriptions for five species from the North Pacific region. We identified a specimen from the Sea of Okhotsk as J. annulata. Among the other four species, J. ezoensis n. sp. has a trans-Pacific distribution (abundant at Akkeshi, Hokkaido, Japan; also detected in the Commander Islands and at Ketchikan, Southeast Alaska); J. pushkini n. sp. was found only at Ketchikan; J. dobrovolskii n. sp. was found only at Shikotan Island in the Lesser Kuril Chain; and J. tumida n. sp. was found only at Kodiak, Gulf of Alaska. These four species all differ from J. annulata in having one or two frontal pore chambers on the proximal gymnocyst of most zooids; in budding frontal dwarf ovicellate zooids from these chambers rather than from basal pore chambers; in producing dwarf zooids more abundantly; and in having ooecia that are somewhat to markedly more reduced (cap-like rather than hood-like) and more closely integrated with the modified latero-oral spines. Furthermore, in the Pacific species, the ooecium in basal zooids arises from the roof of the distal pore chamber of the maternal zooid; ovicellate zooids can thus also bud a distal autozooid and are often arranged in columnar series with other zooids. In J. annulata, the hood-like kenozooidal ooecium budded from the maternal zooid replaces the distal autozooid, and ovicellate zooids are thus usually not embedded in a columnar series.

Geopolitics, Indigenous Peoples, and the Polar Thaw: Sub- and Transnational Fault Lines of the Coming Arctic Cold War

This article examines the current geopolitical transformation of the Arctic region in response to the interplay of rising great power competition (GPC), the institutional empowerment of Arctic indigenous peoples in domestic and international governing bodies, and the continued polar thaw – issues traditionally discussed separately or in pairs, but not generally all together. It applies classical geopolitical theory to the warming Arctic, finding that the fundamental relationships of Heartland to Rimland, and the isolating buffer of what Mackinder called Lenaland, are in a state of flux, and the once-isolated island chains that dominate the physical geography of the circumpolar Arctic are gaining increasing salience to global security, and must not be overlooked. It examines the political geography of the Arctic and the fundamental importance of its indigenous human terrain, where a future Cold War will either be won or lost.

Fungal community composition along a gradient of permafrost thaw

Thermokarst activity at permafrost sites releases considerable amount of ancient carbon to the atmosphere. A large part of this carbon is released via thermokarst ponds, and fungi could be an important organismal group enabling its recycling. However, our knowledge about aquatic fungi growing in thermokarstic systems is extremely limited. In this study, we collected samples from five permafrost sites distributed across circumpolar Arctic and representing a gradient of permafrost integrity. Samples were taken from the ponds surface water, the detritus and the sediment at the bottom of the ponds. These samples were extracted for total DNA, which was then amplified using primers targeting the fungal ITS2 region of the ribosomal genes. These amplicons were sequenced using PacBio technology. Surface water samples were also collected to analyze the chemical conditions in the ponds, including nutrient status and the quality and quantity of dissolved organic carbon. This dataset gives a unique overview of the impact of the thawing permafrost on fungal communities and their potential role on carbon recycling.