1926] Swarth: Birds and Mammals from the Atlin Region 57 an altitude of 2200 feet, compared with Telegraph Creek at 540 feet, and Hazelton at 973 feet, and this increase in elevation, together with the more northern location, has almost eliminated at Atlin certain Canadian Zone elements that are conspicuous at the more southern stations. The lowlands of the Atlin region, it seems to me, are Hud- sonian Zone, with but a slight infiltration of Canadian Zone species. There is no definable zone between the lowlands (2200 feet altitude) and the Alpine-Arctic mountain tops, with timber line between 3500 and 4000 feet. The same species of plants, mammals, and birds, with few exceptions, range from timber line downward in suitable places throughout the valleys. The converse of this, however, is not true, of birds at least, for all species of birds that occur in the lowlands do not range upward to timber line. Then, a further exception must be made of three species of birds, Dendragapus obscurus flemingt, Spizella monticola ochracea, and Lanius borealis, the former two occupying in abundance, the latter in small numbers, types of country that are found in some places immediately below timber line (see pl. 6, fig. 4). However, making due allowance for the more decidedly Hudsonian character of higher altitudes, the general tone of the valleys, too, is of the Hudsonian Zone. This is exemplified in the extensive stands of white spruce with such accompanying bird species as the Alaska hermit thrush, Hudsonian chickadee, Canada jay, goshawk, and spruce grouse, all occurring in abundance. In the upper Skeena Valley the Canadian Zone is dominant, as demonstrated by the presence of many elements over a vast expanse of country. In the upper Stikine Valley, while the Canadian Zone char- acterizes the region, there are fewer bird species represented and they occur over a relatively restricted area. In the lowlands of the Atlin region there is but the merest infiltration of Canadian Zone elements into prevailing Hudsonian Zone surroundings. Lakes and streams in the Atlin region all find their way into the Arctic drainage, and here, too, in coming from the south, one first finds a few real Arctic birds. Among such may be mentioned the pair of black-throated loons we saw, apparently in two minds as to nesting in the region, the northern phalarope, apparently breeding at Carcross, the gyrfaleon, and the northern shrike. Some comparisons can be made of the status of certain species of birds at Hazelton, Telegraph Creek, and Atlin. Bubo virginianus lago- phonus is abundant at Hazelton. We secured no horned owls at Tele- graph Creek, but at Atlin the breeding subspecies is the more northern form, B. v. subarcticus. Dryobates villosus monticola is abundant at