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Journal articles on the topic 'Davis Strait'

Author: Grafiati

Published: 4 June 2025

Last updated: 1 August 2025

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1

Murillo, Francisco Javier, Ellen Kenchington, Gabrielle Tompkins, et al. "Sponge assemblages and predicted archetypes in the eastern Canadian Arctic." Marine Ecology Progress Series 597 (June 11, 2018): 115–35. https://doi.org/10.3354/meps12589.

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Little information exists on the environmental requirements of sponges from the Canadian Arctic, increasing the necessity to establish baseline distribution data on sponge assemblages to predict their susceptibility to climate change. Here we describe the sponge taxa of Hudson Strait, Ungava Bay, Western Davis Strait and Western Baffin Bay collected by Canadian research vessel trawl surveys. A total of 2026 sponge specimens were examined, and 93 different taxa were identified with 79% identified to species, of which 2 are new to science, 1 recorded for the first time in the North Atlantic, 16

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2

Clarke, D. B., B. I. Cameron, G. K. Muecke, and J. L. Bates. "Early Tertiary basalts from the Labrador Sea floor and Davis Strait region." Canadian Journal of Earth Sciences 26, no. 5 (1989): 956–68. http://dx.doi.org/10.1139/e89-077.

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Fine- to medium-grained, phyric and aphyric basalt samples from ODP Leg 105, site 647A, in the Labrador Sea show little evidence of alteration. Chemically, these rocks are low-potassium (0.01–0.09 wt.% K2O), olivine- to quartz-normative tholeiites that compare closely with the very depleted terrestrial Paleocene volcanic rocks in the Davis Strait region of Baffin Island and West Greenland. However, differences exist in the Sr–Nd isotope systematics of the two suites; the Labrador Sea samples have ε Nd values (+9.3) indicative of a more depleted source, and are higher in 87Sr/86Sr (0.7040), rel

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3

Curry, B., C. M. Lee, and B. Petrie. "Volume, Freshwater, and Heat Fluxes through Davis Strait, 2004–05*." Journal of Physical Oceanography 41, no. 3 (2011): 429–36. http://dx.doi.org/10.1175/2010jpo4536.1.

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Abstract Davis Strait volume [−2.3 ± 0.7 Sv (1 Sv ≡ 106 m3 s−1); negative sign indicates southward transport], freshwater (−116 ± 41 mSv), and heat (20 ± 9 TW) fluxes estimated from objectively mapped 2004–05 moored array data do not differ significantly from values based on a 1987–90 array but are distributed differently across the strait. The 2004–05 array provided the first year-long measurements in the upper 100 m and over the shelves. The upper 100 m accounts for 39% (−0.9 Sv) of the net volume and 59% (−69 mSv) of the net freshwater fluxes. Shelf contributions are small: 0.4 Sv (volume),

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4

Larsen, Lotte Melchior, and Marie-Claude Williamson. "Depleted and ultradepleted basalt and picrite in the Davis Strait: Paleocene volcanism associated with a transform continental margin." Geological Magazine 157, no. 12 (2020): 1983–2003. http://dx.doi.org/10.1017/s0016756820000175.

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AbstractVolcanic rocks from the Davis Strait were studied to elucidate the tectonomagmatic processes during rifting and the start of seafloor spreading, and the formation of the Ungava transform zone between Canada and Greenland. The rocks are from the wells Hekja O-71, Gjoa G-37, Nukik-2 and Hellefisk-1, and from dredges on the northern Davis Strait High. Ages range from Danian to Thanetian (dinocyst palynozones P2 to P5, 62.5–57.2 Ma). The rocks are predominantly basaltic, but include picrites on the Davis Strait High. Calculated mantle potential temperatures for the Davis Strait High are c.

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5

Cuny, Jérôme, Peter B. Rhines, and Ron Kwok. "Davis Strait volume, freshwater and heat fluxes." Deep Sea Research Part I: Oceanographic Research Papers 52, no. 3 (2005): 519–42. http://dx.doi.org/10.1016/j.dsr.2004.10.006.

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6

Jørgensen, O. A., C. Hvingel, P. R. Møller, and M. A. Treble. "Identification and mapping of bottom fish assemblages in Davis Strait and southern Baffin Bay." Canadian Journal of Fisheries and Aquatic Sciences 62, no. 8 (2005): 1833–52. http://dx.doi.org/10.1139/f05-101.

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The bathymetry of Baffin Bay, with shallow sills both to the north and south, creates a relatively isolated body of deep polar water, unique among the Arctic Seas. During 263 trawl hauls completed during October 1999 and September to November 2001, 116 fish species were collected in Davis Strait and the southern Baffin Bay (61°44.1′ N73°52.8′ N, depths of 1451484 m). The abundance data for the 80 benthic species were used for analyses of the fish fauna diversity and fish assemblages. As a first step, seven assemblages were found by a standard type of cluster analysis. A Bayesian multinomial

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7

Vaughan, Richard. "Bowhead whaling in Davis Strait and Baffin Bay during the 18th and 19th Centuries." Polar Record 23, no. 144 (1986): 289–99. http://dx.doi.org/10.1017/s0032247400007117.

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ABSTRACTHistories of individual whale fisheries mainly undertaken by Europeans have yet to be written. This article provides an outline history of whaling in the Davis Strait area during the 18th and 19th centuries. Current knowledge is reviewed of whaling west of Greenland by ships from Danish, Dutch and German ports, and from English, American and Scottish ports. The land-based West Greenland whale fishery is also mentioned, and the activities of whalers from France and Spain. In spite of recent national whaling histories of the English, Dutch and Danish industries, quantitative data for the

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8

Mingxian, Wu. "The study of magnetic anomalies over Davis Strait." Chinese Journal of Oceanology and Limnology 4, no. 1 (1986): 56–67. http://dx.doi.org/10.1007/bf02850397.

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9

Dalebout, M. L., S. K. Hooker, and I. Christensen. "Genetic diversity and population structure among northern bottlenose whales, Hyperoodon ampullatus, in the western North Atlantic Ocean." Canadian Journal of Zoology 79, no. 3 (2001): 478–84. http://dx.doi.org/10.1139/z01-005.

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To assess population structure and genetic diversity among northern bottlenose whales (Hyperoodon ampullatus), we compared mitochondrial DNA control region sequences from three populations in the western North Atlantic Ocean. Skin-biopsy samples were collected from animals in the Gully off Nova Scotia, Canada, in 1996 and 1997 (n = 20), and teeth were obtained from whales taken in Davis Strait off northern Labrador (n = 20) and off northern Iceland (n = 5) between 1967 and 1971 by the historical Norwegian fishery. Only low levels of genetic diversity were found among the 45 animals sampled (th

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10

Tsubouchi, Takamasa, Sheldon Bacon, Yevgeny Aksenov, et al. "The Arctic Ocean Seasonal Cycles of Heat and Freshwater Fluxes: Observation-Based Inverse Estimates." Journal of Physical Oceanography 48, no. 9 (2018): 2029–55. http://dx.doi.org/10.1175/jpo-d-17-0239.1.

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AbstractThis paper presents the first estimate of the seasonal cycle of ocean and sea ice heat and freshwater (FW) fluxes around the Arctic Ocean boundary. The ocean transports are estimated primarily using 138 moored instruments deployed in September 2005–August 2006 across the four main Arctic gateways: Davis, Fram, and Bering Straits, and the Barents Sea Opening (BSO). Sea ice transports are estimated from a sea ice assimilation product. Monthly velocity fields are calculated with a box inverse model that enforces mass and salt conservation. The volume transports in the four gateways in the

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11

Hald, N., and J. G. Larsen. "Early Tertiary, low-potassium tholeiites from exploration wells on the West Greenland shelf." Rapport Grønlands Geologiske Undersøgelse 136 (December 31, 1987): 1–25. http://dx.doi.org/10.34194/rapggu.v136.8008.

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Data on the Tertiary basalts in the Davis Strait region are reported from two exploration wells drilled by Arco and Mobil on the West Greenland shelf. Hellefisk 1 (67°53 'N, 56°44'W), situated only 60 km east of the mid-line in Davis Strait, penetrated the upper 690 m of a subaeriallava sequence continuous with the onshore volcanics of Disko and situated beneath 2.3 km of Paleocene to Quaternary sediments. The lavas are feldspar microporphyritic tholeiites and mostly unmetamorphosed despite the presence of laumontite and prehnite in the vesicular top zones. Nukik 2 (65°38'N, 54°46'W) penetrate

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12

Curry, B., C. M. Lee, B. Petrie, R. E. Moritz, and R. Kwok. "Multiyear Volume, Liquid Freshwater, and Sea Ice Transports through Davis Strait, 2004–10*." Journal of Physical Oceanography 44, no. 4 (2014): 1244–66. http://dx.doi.org/10.1175/jpo-d-13-0177.1.

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Abstract Davis Strait is a primary gateway for freshwater exchange between the Arctic and North Atlantic Oceans including freshwater contributions from west Greenland and Canadian Arctic Archipelago glacial melt. Data from six years (2004–10) of continuous measurements collected by a full-strait moored array and concurrent high-resolution Seaglider surveys are used to estimate volume and liquid freshwater transports through Davis Strait, with respective annual averages of −1.6 ± 0.5 Sverdrups (Sv; 1 Sv ≡ 106 m3 s−1) and −93 ± 6 mSv (negative sign indicates southward transport). Sea ice export

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13

Knudsen, C., U. Gregersen, T. F. Kokfelt, M. Olivarius, and T. B. Thomsen. "A mid-Cretaceous alkaline volcano in the Davis Strait." Canadian Journal of Earth Sciences 57, no. 1 (2020): 69–86. http://dx.doi.org/10.1139/cjes-2018-0307.

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The AT2-1 well in the Davis Strait between Canada and Greenland penetrated an approximately 1.2 km thick sequence of alkaline volcanic rocks with some intercalated sediments at depths between 3690 to 4850 m. These volcanic rocks can be mapped on 2D seismic data and constitute a cone-shaped 5 km × 10 km wide and >1.2 km high structural high named the Atammik Volcano. This sequence comprises two distinct parts, an upper part of phono-tephrite to basaltic trachy-andesite and a lower part of tephriphonolite and phonolite. Rock textures and structures testify to a volcanic origin, with the upper

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14

Piasecki, Stefan. "Neogene dinoflagellate cysts from Davis Strait, offshore West Greenland." Marine and Petroleum Geology 20, no. 9 (2003): 1075–88. http://dx.doi.org/10.1016/s0264-8172(02)00089-2.

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15

Heide-Jørgensen, M. P., H. Stern, and K. L. Laidre. "Dynamics of the sea ice edge in Davis Strait." Journal of Marine Systems 67, no. 1-2 (2007): 170–78. http://dx.doi.org/10.1016/j.jmarsys.2006.10.011.

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16

Bowen, W. D., R. A. Myers, and K. Hay. "Abundance Estimation of a Dispersed, Dynamic Population: Hooded Seals (Cystophora cristata) in the Northwest Atlantic." Canadian Journal of Fisheries and Aquatic Sciences 44, no. 2 (1987): 282–95. http://dx.doi.org/10.1139/f87-037.

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Pup production of hooded seals (Cystophora cristata) in the Northwest Atlantic was estimated by aerial survey. Simultaneous surveys and the collection of ground-truth data were conducted in March 1984 in both major whelping areas, namely the floe ice in the Davis Strait and off northeastern Newfoundland (the Front). Abundance estimates were obtained from both fixed-wing photographic and helicopter sighting surveys using a strip survey method for unequal-sized sampling units. These abundance estimates were corrected to account for pups which had left the ice and those pups which had yet to be b

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17

Andersen, Liselotte Wesley, Erik W. Born, Robert EA Stewart, Rune Dietz, DW Doidge, and Clement Lanthier. "A genetic comparison of West Greenland and Baffin Island (Canada) walruses: Management implications." NAMMCO Scientific Publications 9 (December 15, 2014): 33. http://dx.doi.org/10.7557/3.2610.

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Until recently Atlantic walruses (Odobenus rosmarus rosmarus) have been subject to relatively intense exploitation in West Greenland. Animals in this stock have also been hunted in Nunavut/Canada. However, the demographic identity of these animals and their connection with walruses in neighbouring areas is poorly resolved, hampering the determination of sustainable harvest levels. It has been suggested that walruses in West Greenland are genetically linked with walruses at SE Baffin Island (Canada) where they are also hunted for subsistence purposes. To determine the relationship(s) between wa

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18

Hosseinpour, M., R. D. Müller, S. E. Williams, and J. M. Whittaker. "Full-fit reconstruction of the Labrador Sea and Baffin Bay." Solid Earth Discussions 5, no. 2 (2013): 917–62. http://dx.doi.org/10.5194/sed-5-917-2013.

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Abstract. Reconstructing the opening of the Labrador Sea and Baffin Bay between Greenland and North America remains controversial. Recent seismic data suggest that magnetic lineations along the margins of the Labrador Sea, originally interpreted as seafloor spreading anomalies, may lie within the crust of the continent–ocean transition. These data also suggest a more seaward extent of continental crust within the Greenland margin near the Davis Strait than assumed in previous full-fit reconstructions. Our study focuses on reconstructing the full-fit configuration of Greenland and North America

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19

Hosseinpour, M., R. D. Müller, S. E. Williams, and J. M. Whittaker. "Full-fit reconstruction of the Labrador Sea and Baffin Bay." Solid Earth 4, no. 2 (2013): 461–79. http://dx.doi.org/10.5194/se-4-461-2013.

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Abstract. Reconstructing the opening of the Labrador Sea and Baffin Bay between Greenland and North America remains controversial. Recent seismic data suggest that magnetic lineations along the margins of the Labrador Sea, originally interpreted as seafloor spreading anomalies, may lie within the crust of the continent–ocean transition. These data also suggest a more seaward extent of continental crust within the Greenland margin near Davis Strait than assumed in previous full-fit reconstructions. Our study focuses on reconstructing the full-fit configuration of Greenland and North America usi

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20

Heide-Jørgensen, Mads Peter, Kristin Laidre, Sabrina Fossette, Marianne H. Rasmussen, Nynne Hjort Nielsen, and Rikke G. Hansen. "Abundance of walruses in Eastern Baffin Bay and Davis Strait." NAMMCO Scientific Publications 9 (December 15, 2014): 159. http://dx.doi.org/10.7557/3.2606.

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Walruses (Odobenus rosmarus) are exploited for subsistence purposes in West Greenland. However, current information about the abundance of walruses subject to harvest in eastern Baffin Bay subject to harvest has been unavailable despite being critical for maintaining sustainable catch levels. Three visual aerial surveys were conducted in 2006 (21 March to 19 April 2006), 2008 (3 to 12 April) and 2012 (24 March to 14 April) to estimate the number of walruses on the wintering grounds in eastern Baffin Bay and Davis Strait. Data on the fraction of walruses that were submerged below a 2m detection

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21

Jauer, Christopher D., Gordon N. Oakey, and Qingmou Li. "Western Davis Strait, a volcanic transform margin with petroliferous features." Marine and Petroleum Geology 107 (September 2019): 59–80. http://dx.doi.org/10.1016/j.marpetgeo.2019.05.004.

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22

Berg, Vidar, Karl I. Ugland, Nils R. Hareide, Paul E. Aspholm, Anuschka Polder, and Janneche Utne Skaare. "Organochlorine contamination in deep-sea fish from the davis strait." Marine Environmental Research 44, no. 2 (1997): 135–48. http://dx.doi.org/10.1016/s0141-1136(96)00107-9.

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23

Clarke, D. Barrie, and Erin K. Beutel. "Davis Strait Paleocene picrites: Products of a plume or plates?" Earth-Science Reviews 206 (July 2020): 102770. http://dx.doi.org/10.1016/j.earscirev.2019.01.012.

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24

Duyck, Elodie, Nicholas P. Foukal, and Eleanor Frajka-Williams. "Circulation of Baffin Bay and Hudson Bay waters on the Labrador shelf and into the subpolar North Atlantic." Ocean Science 21, no. 1 (2025): 241–60. https://doi.org/10.5194/os-21-241-2025.

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Abstract. In the coming decades increasing amounts of freshwater are predicted to enter the subpolar North Atlantic from Greenland and the Arctic. If this additional freshwater reaches the regions where deep convection occurs, it could potentially dampen ventilation and the formation of deep waters. In this study, we use a surface drifter dataset spanning the period 1990–2023 to investigate the pathways followed by waters originating from Davis Strait and Hudson Strait on the Labrador shelf and into the interior subpolar North Atlantic. Recent drifter deployments in the region allow for an imp

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Peace, Alexander Lewis, Gillian R. Foulger, Christian Schiffer, and Ken J. W. McCaffrey. "Evolution of Labrador Sea–Baffin Bay: Plate or Plume Processes?" Geoscience Canada 44, no. 3 (2017): 91–102. http://dx.doi.org/10.12789/geocanj.2017.44.120.

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Breakup between Greenland and Canada resulted in oceanic spreading in the Labrador Sea and Baffin Bay. These ocean basins are connected through the Davis Strait, a bathymetric high comprising primarily continental lithosphere, and the focus of the West Greenland Tertiary volcanic province. It has been suggested that a mantle plume facilitated this breakup and generated the associated magmatism. Plume-driven breakup predicts that the earliest, most extensive rifting, magmatism and initial seafloor spreading starts in the same locality, where the postulated plume impinged. Observations from the

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26

Koski, William A., and Ralph A. Davis. "Distribution and numbers of narwhals (Monodon monoceros) in Baffin Bay and Davis Strait." Meddelelser om Grønland. Bioscience 39 (April 22, 1994): 15–40. http://dx.doi.org/10.7146/mogbiosci.v39.142532.

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Aerial surveys were conducted over Baffin Bay during May-October 1978-79 and off West Greenland and over southern Baffin Bay, Davis Strait and Hudson Strait during March 1981-82. Narwhals (Monodon monoceros) were dispersed throughout the pack ice in northern Davis Strait and Baffin Bay during late winter and spring and moved into nearshore areas in and adjacent to Lancaster Sound during late June and July. Important summering areas were identified in Buchan Gulf, Eclipse Sound, Admiralty Inlet, Prince Regent Inlet and Peel Sound, and possibly in Smith Sound and Home Bay, but there was co

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27

Dalhoff, Finn, Lotte M. Larsen, Jon R. Ineson, et al. "Continental crust in the Davis Strait: new evidence from seabed sampling." Geological Survey of Denmark and Greenland (GEUS) Bulletin 10 (November 29, 2006): 33–36. http://dx.doi.org/10.34194/geusb.v10.4901.

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Although the structural framework of the subsurface offshore West Greenland has been well documented based on comprehensive seismic analysis (cf. Dalhoff et al. 2003), the stratigraphy of the region is less well known. The oldest documented sedimentary rocks drilled offshore West Greenland are Santonian sandstones reached at TD in the 6354/4-1 well (Fig. 1) although reworked palynomorphs of Carboniferous, Triassic and Jurassic (Kimmeridgian) age have been reported from a number of wells in the region. In order to obtain better constraints on the pre-Upper Cretaceous stratigraphy, a preliminary

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28

Heron, P. J., A. L. Peace, K. J. W. McCaffrey, et al. "Segmentation of Rifts Through Structural Inheritance: Creation of the Davis Strait." Tectonics 38, no. 7 (2019): 2411–30. http://dx.doi.org/10.1029/2019tc005578.

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29

Suckro, Sonja K., Karsten Gohl, Thomas Funck, et al. "The Davis Strait crust—a transform margin between two oceanic basins." Geophysical Journal International 193, no. 1 (2013): 78–97. http://dx.doi.org/10.1093/gji/ggs126.

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30

Mallory, Mark L., Gregory J. Roberston, and Alissa Moenting. "Marine plastic debris in northern fulmars from Davis Strait, Nunavut, Canada." Marine Pollution Bulletin 52, no. 7 (2006): 813–15. http://dx.doi.org/10.1016/j.marpolbul.2006.04.005.

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31

Peacock, Elizabeth, Mitchell K. Taylor, Jeffrey Laake, and Ian Stirling. "Population ecology of polar bears in Davis Strait, Canada and Greenland." Journal of Wildlife Management 77, no. 3 (2013): 463–76. http://dx.doi.org/10.1002/jwmg.489.

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32

Hudon, Christiane. "Distribution of Shrimp and Fish By-Catch Assemblages in the Canadian Eastern Arctic in Relation to Water Circulation." Canadian Journal of Fisheries and Aquatic Sciences 47, no. 9 (1990): 1710–23. http://dx.doi.org/10.1139/f90-196.

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In the Canadian eastern Arctic, the catches of common species of decapods and fish in bottom trawls reveal a continuum of increasing species richness and abundance in an easterly direction through Hudson Strait. Species richness is greatest in Ungava Bay, where Arctic and Labrador Sea components of the fauna coexist. Over the study area, species could be divided in three associations corresponding to the origin of the predominant water masses: Arctic cod, cottids, zoarcids, and liparids predominate in the Arctic waters of western and central Hudson Strait; Greenland halibut, roughhead grenadie

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33

Richard, Pierre R. "Abundance and Distribution of Narwhals (Monodon monoceros) in Northern Hudson Bay." Canadian Journal of Fisheries and Aquatic Sciences 48, no. 2 (1991): 276–83. http://dx.doi.org/10.1139/f91-038.

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Aerial surveys for narwhals (Monodon monoceros) were conducted in August 1981, in July 1982, 1983, and 1984, and in March 1983 in the Repulse Bay area between Roes Welcome Sound and Lyon Inlet, north of Southampton Island. About 1300 narwhals were estimated to occupy waters between northern Roes Welcome Sound and Lyon Inlet in July 1982, 1983, and 1984. Narwhals were found throughout the study area but were more concentrated in three areas: northern Roes Welcome Sound, southern Frozen Strait, and, in 1984, Lyon Inlet. Only four narwhals were observed during August 1981 reconnaissance surveys o

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34

Christensen, S. "On Yield and Revenue of Varying Shrimp Stock in the Davis Strait." Journal of Northwest Atlantic Fishery Science 19 (September 1996): 127–34. http://dx.doi.org/10.2960/j.v19.a11.

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Azetsu-Scott, Kumiko, Brian Petrie, Philip Yeats, and Craig Lee. "Composition and fluxes of freshwater through Davis Strait using multiple chemical tracers." Journal of Geophysical Research: Oceans 117, no. C12 (2012): n/a. http://dx.doi.org/10.1029/2012jc008172.

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CHRISTENSEN, STEEN, and NIELS VESTERGAARD. "A Bioeconomic Analysis of the Greenland Shrimp Fishery in the Davis Strait." Marine Resource Economics 8, no. 4 (1993): 345–65. http://dx.doi.org/10.1086/mre.8.4.42731366.

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Wadhams, Peter, Alfred S. McLaren, and Ruth Weintraub. "Ice thickness distribution in Davis Strait in February from submarine sonar profiles." Journal of Geophysical Research 90, no. C1 (1985): 1069. http://dx.doi.org/10.1029/jc090ic01p01069.

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Punshon, Stephen, Kumiko Azetsu-Scott, and Craig M. Lee. "On the distribution of dissolved methane in Davis Strait, North Atlantic Ocean." Marine Chemistry 161 (April 2014): 20–25. http://dx.doi.org/10.1016/j.marchem.2014.02.004.

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Wilson, Robert W., Knud Erik S. Klint, Jeroen A. M. Van Gool, Kenneth J. W. McCaffrey, Robert E. Holdsworth, and James A. Chalmers. "Faults and fractures in central West Greenland: onshore expression of continental break-up and sea-floor spreading in the Labrador – Baffin Bay Sea." Geological Survey of Denmark and Greenland (GEUS) Bulletin 11 (December 5, 2006): 185–204. http://dx.doi.org/10.34194/geusb.v11.4931.

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The complex Ungava fault zone lies in the Davis Strait and separates failed spreading centres in the Labrador Sea and Baffin Bay. This study focuses on coastal exposures east of the fault-bound Sisimiut basin, where the onshore expressions of these fault systems and the influence of pre-existing basement are examined. Regional lineament studies identify five main systems: N–S, NNE–SSW, ENE–WSW, ESE–WNW and NNW–SSE. Field studies reveal that strike-slip movements predominate, and are consistent with a ~NNE–SSW-oriented sinistral wrench system. Extensional faults trending N–S and ENE–WSW (baseme

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40

Maliuha, Е., and R. Gavriluk. "Interannual variability of ice cover across Davis Strait and the Labrador Sea for the period from 1979 to 2023." Ukrainian hydrometeorological journal, no. 32 (December 27, 2023): 80–94. http://dx.doi.org/10.31481/uhmj.32.2023.06.

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In conditions of rapid development of trade and transport communications, the issue of navigation through ice regime zones became of greater importance. In particular, reduction of the area of ice cover in the Canadian Arctic because of global warming opens up favourable prospects for further development of maritime shipping in this zone. Considering that the routes through the Northwest Passage are the shortest ones of all the routes connecting the Atlantic and Pacific oceans, it is clear that all aspects of this topic are of great importance and relevance. This especially applies to the aspe

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41

Gaston, Anthony J., and Michael S. W. Bradstreet. "Intercolony differences in the summer diet of Thick-billed Murres in the eastern Canadian Arctic." Canadian Journal of Zoology 71, no. 9 (1993): 1831–40. http://dx.doi.org/10.1139/z93-261.

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The diet of Thick-billed Murres collected near six colonies in the eastern Canadian Arctic comprised invertebrates (84% of 23 462 items) and fish (16%). Adult diets differed significantly among colonies, both within the Low Arctic (Hudson Strait), between Low and High Arctic (Lancaster Sound – Baffin Bay), and between Low-Arctic colonies and a colony close to the High/Low Arctic boundary (Davis Strait). Murres from the High Arctic took more invertebrates, fewer fish, and a smaller number of species overall than those from the Low Arctic. Diets were more diverse in the Low Arctic than in the Hi

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42

Parkinson, Claire L. "Recent sea-ice advances in Baffin Bay/Davis Strait and retreats in the Bellingshausen Sea." Annals of Glaciology 21 (1995): 348–52. http://dx.doi.org/10.3189/s0260305500016050.

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Recently reported decreases in the summertime ice coverage of the Bellingshausen Sea over the period 1988–91 have been mentioned in the popular press with some loss of the larger spatial and temporal context in which they occurred. Experience over the past two decades with the continually lengthening satellite record has frequently revealed prominent increases or decreases in regional or even hemispheric sea-ice coverage which last for a several-year period and are then reversed. Also, in almost any several-year period in the short satellite record available, at least one region could be highl

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Parkinson, Claire L. "Recent sea-ice advances in Baffin Bay/Davis Strait and retreats in the Bellingshausen Sea." Annals of Glaciology 21 (1995): 348–52. http://dx.doi.org/10.1017/s0260305500016050.

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Recently reported decreases in the summertime ice coverage of the Bellingshausen Sea over the period 1988–91 have been mentioned in the popular press with some loss of the larger spatial and temporal context in which they occurred. Experience over the past two decades with the continually lengthening satellite record has frequently revealed prominent increases or decreases in regional or even hemispheric sea-ice coverage which last for a several-year period and are then reversed. Also, in almost any several-year period in the short satellite record available, at least one region could be highl

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Herle, Anita. "Woven histories, dancing lives: Torres Strait Islander identity, culture and history - Davis, Richard." Journal of the Royal Anthropological Institute 12, no. 1 (2006): 226–28. http://dx.doi.org/10.1111/j.1467-9655.2006.00289_8.x.

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Rasmussen, Jan Audun, and Emma Sheldon. "Microfossil biostratigraphy of the Palaeogene succession in the Davis Strait, offshore West Greenland." Marine and Petroleum Geology 20, no. 9 (2003): 1017–30. http://dx.doi.org/10.1016/s0264-8172(02)00114-9.

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Khan, R. A., E. M. Lee, and W. S. Whitty. "Blood protozoans of fish from the Davis Strait in the northwestern Atlantic Ocean." Canadian Journal of Zoology 69, no. 2 (1991): 410–13. http://dx.doi.org/10.1139/z91-064.

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A study was carried out to determine the occurrence and prevalence of blood protozoans in benthic marine fish from the Davis Strait, an area between Baffin Island and Greenland (61–70°N, 53–63°W) in the northwestern Atlantic Ocean. Parasites were seen in all 17 species offish examined; piroplasms were most prevalent (78% of 413), infecting all fish species. Prevalences of infection were substantially lower for trypanosomes (23%) and haemogregarines (4%), both of which infected only 10 and 6 of the fish species, respectively. Prevalences were greater in 5 of the fish species examined, Reinhardt

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Gregersen, Ulrik, and Torben Bidstrup. "Structures and hydrocarbon prospectivity in the northern Davis Strait area, offshore West Greenland." Petroleum Geoscience 14, no. 2 (2008): 151–66. http://dx.doi.org/10.1144/1354-079308-752.

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Grygier, Mark J. "Dendrogaster (Crustacea: Ascothoracida) parasitic in Alaskan and eastern Canadian Leptasterias (Asteroidea)." Canadian Journal of Zoology 64, no. 6 (1986): 1249–53. http://dx.doi.org/10.1139/z86-186.

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The ascothoracid parasite Dendrogaster is reported from four boreal localities in the Western Hemisphere. Dendrogaster elegans Wagin infests the sea star Leptasterias polaris in Bristol Bay, Alaska, and in the Gulf of St. Lawrence; the eastern specimens have a shorter brood sac middle piece. A lectotype is selected and described for D. arctica Korschelt from L. groenlandica in the eastern Bering Sea; Siberian specimens previously assigned to this species differ from the type in many details. Immature specimens of an unidentified Dendrogaster species have been found in L. floccosa from the Davi

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Holst, M., and I. Stirling. "A note on sightings of bowhead whales in the North Water Polynya, Northern Baffin Bay, May-June, 1998." J. Cetacean Res. Manage. 1, no. 2 (2023): 153–56. http://dx.doi.org/10.47536/jcrm.v1i2.462.

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As part of a multidisciplinary research cruise by icebreaker in the North Water Polynya in northern Baffin Bay, we conducted shipboard surveys of marine mammal distribution and abundance throughout the area from April to July 1998. Fourteen sightings of at least ten individual bowhead whales (Balaena mysticetus) were made during May and June. Five additional large baleen whales, whose identities were not confirmed, were also seen. As well as being an important feeding ground, the polynya may also serve as an overwintering site for bowhead whales of the Davis Strait/Baffin Bay stock.

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Bacon, Sheldon, Garabato Alberto Naveira, Yevgeny Aksenov, N.J. Brown, and Takamasa Tsubouchi. "Arctic Ocean Boundary Exchanges: A Review." Oceanography 35, no. 3–4 (2022): 94–102. https://doi.org/10.5670/oceanog.2022.133.

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The Arctic Ocean has long been—and to a large extent remains—a data-sparse region. Paucity of ocean and atmosphere measurements impacts the fidelity of atmospheric reanalyses, and ungauged rivers lead to uncertainties in measurement-based estimates of river runoff. However, there exists a data resource that can provide material help: sustained (long-term) ice and ocean measurements around the Arctic Ocean boundary. The Arctic Ocean is surrounded by land and connects to adjacent ocean basins via four main gateways: to the Pacific through Bering Strait, to the Atlantic through Davis

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