Abstract
Information about bearded seal seasonal distribution in the Pacific Arctic is limited. Bearded seals (Erignathus barbatus Exleben, 1777) from coastal sites along the southern, eastern, and northern Chukotka Peninsula, Russian Federation, were observed most seasons during 1993 – 96, 1998 – 2000, 2002 – 05, and 2010 – 11. These observations provide spatial and temporal information about bearded seal seasonal distribution, movements, and relative numbers in the coastal zones. In winter, bearded seals aggregate on the young ice in the northern part of the Gulf of Anadyr. Numbers gradually increase during March. In springtime (April–May), bearded seals in the northern Gulf of Anadyr are relatively numerous around Nunligran (Cape Achen), but the number is highly variable across years. During spring bearded seals move eastward along the coast from the northern part of the Gulf of Anadyr towards the Bering Strait and then to the north, as the marginal ice edge zone retreats north. These movements to the east and north continue in ice-free water, and by August, the spring migration of bearded seals along the coast of the Chukotka Peninsula ends. In the summer months of August and September, few bearded seals are present in this coastal zone. The southward autumn migration of bearded seals is not evident near the coast, which suggests that it occurs farther from shore.
Highlights
The bearded seal (Erignathus barbatus) is the largest of the northern Pacific Ocean seals in the family Phocidae, first described by Gray in 1825
The primary purpose of this study is to examine the seasonal movements and relative abundance of bearded seals in the coastal waters surrounding the Chukotka Peninsula
Gulf of Anadyr: In the southern coastal waters of the Chukotka Peninsula (Gulf of Anadyr), the number of bearded seals increased from January to March
Summary
The bearded seal (Erignathus barbatus) is the largest of the northern Pacific Ocean seals in the family Phocidae, first described by Gray in 1825. These seals have a widespread circumpolar distribution and are associated with seasonal sea ice in the shallow Arctic seas (Heptner et al, 1976; Burns et al, 1981). They are common inhabitants of the coastal waters surrounding the Chukotka Peninsula, including areas of the Bering and Chukchi Seas. These animals will make and maintain breathing holes if necessary (Rutilevsky, 1939; Burns and Frost, 1979)
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