Conservation Status Map
<img src="http://www.natureserve.org/explorer/servlet/GetMapGif?CA.BC=__&CA.MB=__&CA.NB=__&CA.NT=S3&CA.NS=__&CA.NU=SNR&CA.ON=__&CA.PE=__&CA.QC=__&CA.YT=S1&US.AK=S4&US.CA=S2&US.CT=__&US.DE=__&US.ID=__&US.ME=__&US.MD=__&US.MA=__&US.NN=SNR&US.NH=__&US.NJ=__&US.NY=__&US.NC=__&US.OH=__&US.OR=S4&US.PA=__&US.RI=__&US.SD=__&US.TX=S2&US.VT=__&US.VA=__&US.WA=__" alt="Conservation Status Map" style="width: 475px; height: auto;" />
Global Range
H - >2,500,000 square km (greater than 1,000,000 square miles) - H - The breeding range encompasses arctic North America and eastern Russia. In winter, brant occur along the Pacific coast from Alaska to Baja California and mainland Mexico, along the Atlantic coast from Massachusetts to North Carolina (mainly New Jersey to North Carolina), and from the British Isles to the Mediterranean area and south to coastal China.<br><br>BREEDS: arctic North America and Russia: Prince Patrick and Melville islands in the western Canadian high arctic and the Beaufort Sea islands to the coastal plain of Canada and Alaska, with small colonies on the north side of the Chukotka Peninsula in Russia and on Wrangel Island (Derksen and Ward 1993). In western North America, about 80% of the total black brant population nests in four major colonies on the Yukon-Kuskokwim delta in western Alaska (Derkson and Ward 1993). WINTERS: in North America, along the Pacific coast from Alaska to Baja California and mainland Mexico, along Atlantic from Massachusetts to North Carolina (mainly New Jersey to North Carolina); from British Isles to Mediterranean area, south to coastal China; occasional in Hawaii. A major shift in the winter distribution in western North America occurred during the 1950s and 1960s, with increased numbers using lagoons along the Mexican mainland and much decreased numbers wintering in California; since the mid-1960s, more than 80% of the counted winter population has occurred in Mexico (Derksen and Ward 1993). In the 1980s, an average of several thousand wintered in the Izembek Lagoon area of the Alaska Peninsula (Derksen and Ward 1993). Kasegaluk Lagoon on the Chukchi Sea in northwestern Alaska is an important migration stop during southward migration; as much as 49% of the entire Pacific flyway population may use the lagoon (Johnson 1993). Izembek Lagoon on the Alaska Peninsula is a critically important stop in spring and late summer, hosting at least the majority of the eastern Pacific population (Johnson and Herter 1989); nearly the entire black brant population spends as long as nine weeks there before departing for wintering areas to the south (Derksen and Ward 1993). Important summer molting areas occur on Alaska's north slope and Wrangel Island (Derksen and Ward 1993).
Global Range Description
>2,500,000 square km (greater than 1,000,000 square miles)
ELEMENT_GLOBAL.2.103759