scholarly journals Plastic ingestion by Arctic fauna: A review

Author(s):  
France Collard ◽  
Amalie Ask
Keyword(s):  
2021 ◽  
Vol 325 (2) ◽  
pp. 143-155
Author(s):  
N.E. Zhuravleva

The paper considers the species composition of the fauna of several cnidarian groups of the Kara Sea. The author presents a list of species of the studied groups and indicates the types of habitat for each species. The analysis was based on the literature data, the collections of the Zoological Institute of the Russian Academy of Sciences and material collected in the Kara Sea during the expedition to the R/V Professor Multanovsky in 2019. In total, 87 species of Hydrozoa, 3 species of Scyphozoa, 4 species of Staurozoa, and 5 species of the order Alcyonacea from the class Anthozoa were recorded for the fauna of the Kara Sea, based on the new material obtained by the author and published literature data. The report presents the biogeographic structure of the discussed cnidarian groups. According to the types of biogeographic ranges, the fauna of the above-mentioned cnidarian groups in the Kara Sea mostly consists of representatives of the Boreal-Arctic type of habitat (63%), the Boreal and Amphiboreal biogeographic groups each containing 12% of the total number of described species, and the Panoceanic and Arctic groups together accounting for only 9% and 4% of the fauna of the Kara Sea. Two species new for the Kara Sea, Neoturris pileata (Forsskål, 1775) and Neoturris pileata (Forsskål, 1775), are described. Neoturris pileata is an element of the warm-water Atlantic fauna that penetrated into the Kara Sea with waters of Atlantic genesis. Nausithoe werneri is an element of the cold-water Arctic fauna that penetrated into the Novaya Zemlya Trough of the Kara Sea from the north-western side from the St. Anna Trough, which was open to the Polar Basin.


2005 ◽  
Vol 64 (5) ◽  
pp. 468-477 ◽  
Author(s):  
Michael J. Bradley ◽  
Susan J. Kutz ◽  
Emily Jenkins ◽  
Todd M. O’Hara

1940 ◽  
Vol 179 (13) ◽  
pp. 231-232
Author(s):  
Cameron Shore
Keyword(s):  

1956 ◽  
Vol 37 (3) ◽  
pp. 375 ◽  
Author(s):  
H. T. Hammel
Keyword(s):  

1972 ◽  
Vol 2 (02) ◽  
pp. 119-134 ◽  
Author(s):  
David M. Hopkins ◽  
Robert W. Rowland ◽  
William W. Patton

Drift, evidently of Illinoian age, was deposited on St. Lawrence Island at the margin of an ice cap that covered the highlands of the Chukotka Peninsula of Siberia and spread far eastward on the continental shelf of northern Bering Sea. Underlying the drift on the northwestward part of the island are mollusk-bearing beds deposited during the Kotzebuan Transgression. A comparison of mollusk faunas from St. Lawrence Island, Chukotka Peninsula, and Kotzebue Sound suggests that the present northward flow through Bering and Anadyr Straits was reversed during the Kotzebuan Transgression. Cold arctic water penetrated southward and southwestward bringing an arctic fauna to the Gulf of Anadyr. Warmer Pacific water probably entered eastern Bering Sea, passed eastward and northeastward around eastern and northern St. Lawrence Island, and then became entrained in the southward currents that passed through Anadyr Strait.


2018 ◽  
Vol 4 (4) ◽  
pp. 669-690 ◽  
Author(s):  
Kathy L. Young ◽  
Laura Brown ◽  
Claude Labine

Information on arctic snow covers is relevant for climate and hydrology studies and investigations into the sustainability of both arctic fauna and flora. This study aims to (1) highlight the variability of snow cover at Polar Bear Pass (PBP) at a range of scales: point, local, and regional using both in situ snow cover measurements and remote sensing imagery products; and (2) consider how snow cover at PBP might change in the future. Terrain-based snow surveys documented the end-of-winter snowpacks over several seasons (2008–2010, 2012–2013), and snowmelt was measured daily at typical terrain types. MODIS products (snow cover) were used to document spatial snow cover variability across PBP and Bathurst and Cornwallis Islands. Due to limited data, no significant difference in snow cover duration can be identified at PBP over the period of record. Locally, end-of-winter snow cover does vary across a range of terrain types with snow depths and densities reflecting polar oasis sites. Aspect remains a defining factor in terms of snow cover variability at PBP. Northern areas of the Pass melt earlier. Regionally, PBP tends to melt out earlier than most of Bathurst Island. In the future, we surmise that snowpacks at PBP will be thinner and disappear earlier.


1940 ◽  
Vol 179 (20) ◽  
pp. 358-358
Author(s):  
William Harcourt-Bath
Keyword(s):  

2006 ◽  
Vol 86 (7) ◽  
pp. 760-786 ◽  
Author(s):  
Yu. I. Chernov ◽  
A. G. Tatarinov
Keyword(s):  

Polar Record ◽  
1974 ◽  
Vol 17 (108) ◽  
pp. 237-247 ◽  
Author(s):  
Kai Curry-Lindahl

In reviewing the conservation of Arctic fauna, it may be useful to describe what is meant, geographically and ecologically, by the word Arctic, as it is used here. Geographical boundaries are not often the same as ecological boundaries, and the Arctic Circle itself has no zoogeographical significance. Permanently ice-covered land and treeless lands with permanently frozen subsoil in the Northern Hemisphere would be included in any definition of the Arctic region, and in northern countries the timber line constitutes a satisfactory southern limit for the region in question. In mountains, it is altitude rather than latitude that gives an Arctic character to climate and landscape, as in the Urals, the mountain chain of Scandinavia (south to 59°N) and eastern Siberia, and the Rocky Mountains of North America.


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