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DEPARTMENT OF AGRICULTURE DIVISION 01' lUOUKIICAI, SUKVEY NORTH AMERICAN FAUNA ISTo. 19 [Actual (kite ol pulilication, Octoljer (5, 1900] RESULTS OF A BIOLOillCAL 11EC0XX01S.SANCE OF THE YUKON RIVER REGION General Account of the Region Annotated List of Mammals I5y Wilfred 11. Osgood Annotated List of Birds By Louis B. Bishop, M. U. Pruimnil inirter tho direction of Dr. C. HART MBRRIAM CHIEF OF DIVISION OF BIOLOGICAL SURVEY WASHINGTON GOVERNMENT PRINTING OFFICE 1 \) U 0 V* Jj-"" LETTER OE TRANSMEFTAL. u. s. dei'ailtment of agriculture, Washington, D. C, Ju/i/ ':JS, 1900. Sir: I have the honor to transmit for publication, as No. 19 of North American Fauna, a report entitled ' Results of a Biological Reconnois- sanco of the Yukon River Region,' by Wilfred H. Osgood and Louis B. Bishop. Under instructions dated May 11, 1899, Wilfred H. Osgood, an assistant in the Biological Survey, proceeded to Skagway, Alaska, and thence over White Pass to the headwaters of the Yukon and down the entire length of the Yukon River to St. Michael. He was accom- panied by Dr. Louis B. Bishop, of New Haven, as volunteer assistant; Dr. Bishop has prepared the report on the birds observed during the trip. These are the first investigations of the kind undertaken on the Upper Yukon, and the results herewith presented will be found to contain many important facts concerning the distribution of mammals, birds, and trees in this region. Respectfully, Hon. James Wilson, Secretary of Ayrieultare. C. Hart Merriam, Chief., Biological Survey. CONTENTS. Page. General account of the region, 1 )y Wilfred H. Osgood 7 Itinerary 7 Faunal districts 8 Lynn Canal district 8 White Pass district 9 Canadian Yukon district — Lake subdivision 10 River subdivision 12 Hudsonian Yukon district 13 Alaska Tundra district 15 Summary of faunal districts 16 Previous work 18 New species - 19 Mammals of the Yukon region, by Wilfred H. e divided for convenience into five dis- tricts: (1) The Lynn Canal district, (2) the White Pass district, (3) the Canadian Yukon district, (i) the Hudsonian Yukon district, and (5) the Alaska Tundra district. These districts are limited in a general way by their respective life zones, but they^ are not of equal extent or importance, and the names applied to them are used not to specially designate restricted parts of zones alread}' recognized, but purel}^ as a matter of convenience. They are longitudinal districts — that is, they are very much longer than wide, and each is merely a nar- row tract covered by our route through some larger fauna! region. Lynn Ccmul dlst/'ict. — Skagway and the country bordering Lynn Canal are in the northern part of that faunal area which Nelson has called the 'Sitkan district' and which has often been included in the Northwest Coast district. The trees and shrubs are much the same as those at Juneau, Wrangell, and other points farther south, but the vege- tation is not quite so dense and luxuriant. The shores of Lynn Canal are steep, rocky, and comparatively sparsely timbered, but in some places, as at Haines, low, swampy ground and heavy saturated forests are found. At Skagway, poplars {Populus treviulmdes and Pojndus OCT., 1900.] FAUNAL DISTRICTS. 9 hahamifera) are very common; they share the river bottom with wil- lows and extend well up the steep canj^on sides, where the}' occupy larj^e areas adjacent to the pines, tirs, and spruces. Skaj^way is surrounded I)}' high mountains, and its fauna is limited chietly by altitude. Glacier Station, 1-1 miles distant, and about 1,900 feet higher, is near the }>oundary between the Lynn Canal and White Pass districts. The station is situated on the side of a wooded gulch through which a fork of Skagwaj' River flows. The immediate vicinity is similar to the country aljout Skagway, but shows the influence of the Hudsonian zone of the White Pass district, which begins only a short distance beyond. On either side of the gulch are glaciated granite clift's supporting an irregularly distributed vegetation, chiefly groves of poplars and dense thickets of alders, while in the bottom of the gulch conifers are the prevailing trees. The most common trees and shrubs are lodgepole pines [Pinus 'laurrayanri)^ alpine firs {Ahiea las'wcariKt)^ tidewater spruces [Picea sitc/umsis), poplars or aspens {Popuhos tvemnloides and Populics halsamiferd)^ alders {Ahius sinuata), dwarf birches {Betula glandulosa)^ currants {Pibes laxijlorxim), and huckleberries ( Yacchiium ovalifoUum). The black crowberry {Empe- truni nigrum) and several other heather-like plants occur in the gulch but are more common higher up. Along the trickling streams are man}' ferns and mosses, as well as occasional patches of the lichen known as 'reindeer moss.' Among the mammals of this region are the Streator shrew {Soi'ex ]). str'eatori), the Bangs white-footed mouse {Peromyscus 07'eas), the Dawson red-backed mouse {Evokmiys dawsoni)^ the long-tailed vole {Mlcrotus mord^ix)^ and the red squirrel {Sciurus h. petulans). Characteristic birds are the sooty song sparrow {Melo- spiza m. rufina), the Townsend fox sparrow {Passerella i. tmvnsendl)^ the Oregon snowbird {Junco h. oregonus), and the varied thrush {IFcs- pet'ocicJda ncBvia). White Pass district. — The summits of the mountains that rise directl}' east of Skagwa}' are covered with glaciers and perpetual snow, which feed numerous streams that flow down between mass- ive walls of granite. The sides of the wider canyons have been smoothed and scored hy glaciation, and the smaller and more recent ones are but jagged rock-bound chasms. These unfavorable conditions cause a rapid change in the character of the plant and animal life, and from Glacier to the summit of White Pass the zones are Hudsonian and Arctic-alpine. A few hundred feet abovfe Glacier the trees become smaller and more scattered, and at Summit only the alpine juniper {JxLnip>eru^'< nana)., the bearl^erry {Arctostaphylos uvaimsi), and depau- perate alpine hemlocks {Tsuga mertensiana) occur. Heathers and mosses prevail and large areas of reindeer moss arc conspicuous. For some distance on the summit of White Pass (Plate II, fig. 1) the elevation and phj^siograph}' are nuich the same; the country- is slightly 10 NORTH AMERICAN FAUNA. [no 19. rolling and consists entirol}'^ of granite rock, alxnit wliicli cling many mosses and heathers, while small alpine junipers and hemlocks struggle for existence in favorable places. The breeding birds found with these Hudsonian plants were ptarmigan {Lagojim riqjestris and L. leucuru-s)^ pipits {Anthus 2)e'H8ilva7iicus)^ rosy finches {Leucosticte t. littoraUs)^ and golden -crowned sparrows {Zonotrichiacoronata). Char- acteristic manmials noted were pikas {Oehotona collctris)^ hoary mar- mots {Arctomys caUgatus)^ and mountain goats {Oreamnos m.ontmnis). Canadian Yukon district. — Lake subdivision: On the north side of the divide the hemlocks are soon replaced by pines and spruces, and in the vicinity of Shallow Lake the boundary of the interior fauna and flora is reached. The change is complete at Log Cabin, British Colum- bia, nine miles from the head of Lake Bennett, where the characteristic features of the Canadian zone are again established and the general aspect of the country is very different. The most abundant tree is the white spruce {Picea canadensis)^ and among shrubs seen for the first time the buffalo berry {LepciTgyrmi canadensis) is very common. Birds marking a change of fauna are the slate-colored junco {Jwico hyeinalis)., the Alaska jay {Perisoreus canadensis fumifi'ons)., the inter- mediate sparrow [Zonotrichia I. gamheli)., and the l)lack-poll warbler {Devdroica st7'iata). A new chipmunk {Entamias caniceps) is very conspicuous. At the head of Lake Bennett another change occurs; the country becomes more arid and rocky and there is a tinge of Hudsonian. Lake Bennett is a long, narrow sheet of water inclosed by high granite clifl's, the sides of which are often so steep as to l)e unfavorable for plant and animal life, and whose summits are doubtless similar to White Pass in fauna and flora. Cold winds sweep down the lake much of the time, and cool shadows envelop the east side most of the fore- noon and the west side most of the afternoon, so that opportunity for warmth by direct sunlight is limited. Hence there is quite a strong Hudsonian element about the lake. Among the plants^ collected here are the pale dwarf laurel {Kalmia glauca)^ the Greek valerian {Polemmiitim Immile)^ the forget-me-not {Myosotls sylvatica alpestrL-i), the alpine juniper {Juniperus )uma), the bush cranberry {Vihurmim pauciflormii).^ the dwarf birch {Betula glandidosd)^ the bearberry {Arctostaphylos uvaursi)^ the buffalo berry {Lepargyrwa canadensis), the shadbush {Amekmchie?' alnifolia), the Labrador tea (Ledum grcen- Jandicuiiii), and the black crowberiy {Enijxti'um nigrum). Where trickling streams come down to the lake alder thickets abound, and along terraces of rock clumps of pines and spruces as well as poplars find suppoit. Among Hudsonian mammals were found pikas {Oeho- tona collar is), hoary marmots {Arctoviys caligatus), and Dall sheep 'Identified by F. V. Coville, chief botanist, U. S. Department of Agriculture. North American Fauna, No. 19. Plate II. Fig. 1.— Summit of White Pass. Fig. 2.— Canadian Police Station at caribou Crossing. OCT., 1900.] FAUNAL DISTKICTS. 11 {Oms dalll). Although the lake widens slightly at its lower end, its outlet is a narrow stream about 3 miles long, called Caribou Cross- ing- (Plate II, fig. 2), on the north side of which is an open, grassy swamp })ordered ]jy willow thickets. This low country, though very limited and not extending to the next lake, affords a breeding place for a few mammals and birds not found about Bennett. Lake Tagish, which receives the waters of Bennett through Caribou Crossing, is like Bennett in character, though not so closely walled, and is characterized by practically the same plants and animals. The surrounding mountains are covered with dense forests, which in many places are almost impenetrable. Connected with Lake Tagish by a short, narrow stream, known as Six-Mile River, is Lake Marsh, a long shallow lake on each side of which extends low country, with rolling hills farther back. The valley widens here quite appreciably, and the open country is like that at Caribou Crossing. On the east side are sedgy l^ogs surrounded by willow thickets, and in many places a wide margin of beautiful green sedge meets the edge of the water. Rocky shores are found at some points on the northwest side, but in general the country is low and moist, in marked contrast to that about Bennett and Tagish. The mountain animals of those lakes are of course absent, and the bird life i.s also somewhat different. Fifty-Mile River, into which the Yukon waters proceed from Lake Marsh, is rather narrow, and for a short distance at White Horse Rap- ids very swift. Its banks are chiefly abrupt bluffs of sandy clay (from 50 to 100 feet high) but at Miles Canyon it is confined between walls of basalt. Below the rapids the stream widens somewhat and the higli banks become less frequent, often being replaced l^y low ones thickly grown with willows. The timber is somewhat scattered, and on the rolling hills back from the river bare granite spaces may be frequently seen. At the head of Fifty-Mile River, we first met with birch trees {Bettda 2)a2)yrifera f)^ and from that time on they were seen daily. They do not grow to large size — trees more than 8 inches in diame- ter were seldom seen. Several small streams flow into Fifty-Mile River, which favor the growth of thickets of alders along their )>anks and large clumps of willows about their mouths. The little l)oreal sagebrush {Artemisia Jrigida) grows abundantly on the warm exposed slopes that occasionally alternate with the sandy 1)luffs. Lodgepole pines are also abundant and f requentl}' occupy large areas to the exclu- sion of all other trees. Spruce and poplar, however, are still the strong- est elements in the forest. From Fifty-Mile River we enter Lake Lebarge, the last and largest of the lakes. All abovit its clear, cold waters are low granite moun- tains (Plate III, fig. 1). Occasionally patches of heavy spruce forest are found near the Avater, l)ut in man}^ places clift's rise al)ruptly from 12 NORTH AMERICAN FAUNA. [no. 19. the water's edg-e, and the timber i,s very sparsely sprinkled over them. The rocks found here and a few in Thirty-Mile River are the last we saw showing signs of glaciation. Lake Lcbarge is quite different from Lake Marsh, and is more similar to Lakes Tagish and Bennett, though all the Hudsonian elements of these are not present. River subdivision : This area includes the section from the foot of Lake Lebarge to the mouth of the Pell v River at Fort Selkirk. There is very little variety in the character of the country between these points. Thirty -Mile River, which proceeds from Lake Lebarge, is a swift, narrow stream, and at low water is barely navigalile for small steamers. A conspicuous feature of its banks, which are cut abruptly like those of Fiftv-Mile River, is a narrow ribbon-like stratum of vol- canic ash about 6 inches below the surface that may be seen wherever the bank is exposed. On the mountains a short distance from the river the forest of spruce is heavier and purer than an}" previousl}' noted. The poplars and willows are more confined to the brink of the river, and the birches are scattered. Thirt3"-Mile River is simply that por- tion of the Yukon between Lake Lebarge and the mouth of the Hoota- linqua orTeslin River. The stream is greatly augmented b}^ the waters of the Hootalinqua, and from this point on to Fort Selkirk is known as the Lewes River. Below the Hootalinqua it cuts through the Semenow Hills, for the most part abrupt, rock}', and rather barren mountains from 2,000 to 3,000 feet high. Near their bases and at the water's edge are forested areas, but the exposed hillsides are covered with boreal sagebrush {A7'temisiafngida)^ with here and there a pros- trate juniper or a small clump of spruces. The river now widens rapidly, receiving in succession the waters of the Big Salmon, the Little Salmon, and the Nordenskiold. The rolling hills are sometimes a mile or several miles from the river bank, with low willow swamps intervening. Islands varying from 1 to 100 acres in extent and covered with luxuriant vegetation are abundant. The distribution of trees on the small, regular-shaped islands is very uniform, this different kinds being grouped in concentric belts. Alders generally form the outer margin; next come the willows; next the poplars, rising somewhat higher; and finally the dark-green spruces, which occupy the central area. The whole effect is quite picturesque. On the larger islands the spruces are larger, and usually predominate to such an extent that almost everything else should be classed as under- growth (including trees and shrubs belonging to the genera Alnus, Salix, Pojndus^ Lepargyrcm^ Cornus^ Vihurnwn, jRosa, Zedmn, Yac- dnium^ Hihes^ and others). Lodgepole pines still occur, though unlike the spruces they nowhere form continuous forest and disappear entirely a short distance beyond Fort Selkirk. The Canadian Yukon district as a whole is very well marked. Char- acteristic mammals are the gray-headed chipmunk {Eutamias caniceps), North American Fauna, t!:. 13 Plate Fig. 1.— Cliffs on East Side of Lake Lebarge. Fig. 2.— Yukon River, 50 Miles below Fort Selkirk. OCT., 1900.] FAUNAL DISTRICTS. 13 the Bennett grouiul s(|uiiTel {Speriiwpldlwi em^et'rai}le>ere(jrin(i)^ the pileolated warl:»ler ( Wdsonla jyiiAiilla plleolatcib)^ and the mountain bluebird {Slalia arctica). Of these, CJwrdeiles is perhaps the most noteworthy, as it is decidedly a southern genus. It is very common, and was seen nightly from Caribou Crossing to Rink Rapids, but after we had passed that point it disappeared. Its range in this region as observed by us is probably accurate and corresponds with the limits of the district. Among trees, the lodgepole pine {Pinus 7mMrrayana) is common throughout the district, but does not extend beyond it. Iludsoniojii Yidion district. — This district, as here considered, includes till of the Yukon region from Fort Selkirk to the limit of trees. The Lewes River is joined at Fort Selkirk by the Pelly, after which the increased volume of water flows on between heavily forested slopes and jutting cliffs (Plate III, fig. 2), which replace the sandy banks of the upper river. From the mouth of the Selw}^! northward the topography of the river banks is but slightly different. The num- ber of poplars in the forest is much increased; the spruces are corre- spondingly decreased not only in number but also in size; while the birches about hold their own, and the pines are not present at all, having disappeared between Fort Selkirk and the mouth of the Sehv3^n River. As we approach Dawson spruces become dwarfed and entirely subordinate to the poplars, which crowd their l)ushy tops together for miles and miles. The spruces are in the gulches and in small clumps elsewhere, and a few are scattered about, their dark-green spike tops showing off well against the billowy mass of the lighter foliage of poplar and birch. The undergrowth remains much the same, and deep moss covers the ground and rocks. In damp sandy places along shore and on islands occasionally overflowed a bright-green scouring rush {E(pdsetum) grows so abundantly as to be a characteristic plant. The alpine juniper {Juniperus nana) is found occasionally on hill- sides not too thickly grown with poplars, and on the more open hill- sides the landscape is brightened liy masses of fireweed ( ChamcBnerion angusti folium), for even here forest fires are not a novelty. Two more large rivers, the White and the Stewart, empty into the Yukon in this vicinity. About the mouths of these and other tributaries is more or less low country covered with willows. Islands become 14 NORTH AMERICAN FAUNA. [no. 19. still iiioru nunici'ous iind larger, and have a forest growth that is more uniform in character than that of the river banks. High clifis over- hanging the I'iver arc of frequent occurrence. From Dawson to the Alaska boundary and thence to Circle the country is about the same. For a long distance in the vicinity of the boundary a range of high mountains is visiljle to the northward on the right bank of the river. The low, rolling hills which border the upper river do not quite reach Circle, l)ut are replaced by a broad, flat country known as the ' Yidvon Flats,' which extends from near Circle to Fort Hamlin, a distance of about 200 miles. Through the ' Flats ' the course of the river breaks up into a great man}^ channels, and the islands still further increase in size and number. These are composed of sand and silt, in which poplars thrive better than spruces, though the latter are by no means eliminated. A wild rose {Rosa cmnaniohieaf) is the most abundant shrubby plant, and on the ground below it the Equisetuvi is rampant. The larger islands are identical in character with the mainland, and on them the spruces form quite a heavy forest, with deep moss beneath. At Fort Hamlin the river narrows again and flows l)etween rolling wooded hills, which are similar to many farther up the river. Small streams enter the main river frequently, and the timl^er is much the same; poplars, alders, and birches cover the hills in dense thickets, through which spruces are sprinkled. Alders arc more numerous than before. The hills var}- in height from 600 to 3,000 feet, and the highest have a distinct timberline at about 2,000 feet. At the mouth of the Tanana the hills become smaller and the river very much wider. Here, at Fort Gibbon, Dr. Bishop found the larch {LariM aiaericana) quite alnmdant. This Avas the only point at which it was seen by an}^ of our party. The Lower Yukon beyond the Tanana is very uniform in character. The banks are low and rolling and overgrown with willows and alders; farther back are higher hills covered with poplars and birch; occasion- ally the summits of a few hills higher than the rest are devoid of trees. On the sandy islands the willow thickets are impenetrable, and where a cut bank exposes a section of tliem their slender perpendicu- lar trunks stand so closely as to present a solid front like a thick hedge or canebrake. Thus it continues until the limit of timber is reached at Andraefski, 90 miles above the mouth of the Yukon. This district as a whole is characterized l)v absence of southern plants and animals. Among migratory birds a few have their center of abundance farther south, but all the mammals are northern forms, and nearly all belong to genera of circumpolar distribution.^ Plant life, though quite luxuriant, is made up of only a small number of hardy species. Characteristic mammals are the Fort Yukon ground ^ The only exceptions are Synaptomys, Fiber, and Erethizon. OCT., 1900.] FAUNAL DISTRICTS. 15 squirrel {^Sperino^Jdlus osgoodi)^ Dawson red-backed mouse {Eootomys dawsoni), yellow-cheeked vole {Microtus xanthognathus), Yukon lem- ming {Lemm.usyuJione7isis)^ Dall varjang hare {Lejms americanus dall'i)^ and tundra weasel {Putorms arcticui). Of the birds, the most char- acteristic are the duck hawk {Falco peregrinus anatum)^ pigeon hawk {Falco coluijiharius)^ Alaska longspur [Calcarius lajpjponicus alascensis)^ hoary redpoll {AcantJds Iwrnemannl exlllpes)^ fox sparrow {Passerella illaca)^ Bohemian waxwing {ArnjJelis gai'mdtis)^ and wheatear {Saxicola mnanthe). Alaska Tundra district. — The Yukon from Andraefski to the coast of Norton Sound is bounded on ])oth sides by typical tundra. The country is low and gently undulating, and its surface a short distance away appears to be thickly carpeted with grass. That this is not the real condition a short walk ashore soon demonstrates; but the delusion is so complete that were it not for the presence of the great river one might fancy himself looking out over the undulating plains at the eastern base of the Rocky Mountains in the western United States. The flora of the tundra, though devoid of trees deserving of the name, is found on careful examination to ])e quite varied. Besides the numerous mosses and heathers and many small berry-bearing plants are dwarf willows, birches, and alders. The alders attain the greatest size, but are usually found in isolated clumps in favorable spots, where they often grow from 6 to 8 feet high. The ground is frozen a few inches below the surface, and the heavy, spongelike cover- ing of vegetation is kept constantly saturated. Occasional high bluffs on the coast in exposed situations are bleak and bare, but besides these there is scarcely a spot not covered Avith low, matted vegetation. Numerous small ponds are irregularly distributed over the tundra, and around them the vegetation is ranker than elsewhere. Broken lava borders the shores of St. Michael Island, and small moss-covered heaps of it, which form practically the only solid footing on the island, are scattered about over the tundra. Characteristic mammals at St. Michael are the Hall Island fox ( Vul^yes hallensis), Nelson vole {Microtus ojMrarius), tundra red-backed mouse {Evotoinys dawsoni alascensis), Nelson pied lenmiing {Dicro- stmiyx nelsoni), Alaska lemming {Leminus alascensis)., and Alaska Arctic hare {Zejms otJuis). Land birds known to breed are the hoary redpoll [AcantMs Iwrnemanni exiUpes)^ common redpoll (Acanthis linaria), Alaska longspur {Calcarius lajjponicus alasccmsis)., western tree spar- row {Sjnzella inonticola ochracea)., golden-crowned sparrow {Zonotrickia coronata)., and Siberian yellow wagtail {Budytes Jlavus lev cost?' iat us). Common tundra plants^ are Cassiopea tetragona., Andromeda x>oli folia., Vaccinium, vitisidcea., Mairania alp>ina.. Ledum palustre, Artemisia ^Nelson, Report upon Natural History Collections in Alaska, 30, 1887. 16 NORTH AMERICAN FAUNA. [no 19- arctica^ Riihun cJutmiam'xynis^ Iii(l>iis (irctlGus^ Betida nana, Alnus sinuata. CIt<( nuvcii^tux jn'ocairiheus, and Tnsnlago frigida. SUSEVIAKY OF FAUXAI. DISTRICTS. All the country horo, consitlorcd is in the boreal zones, the Tundra district and a small part of the White Pass district belon«^ing- to the Arctic subdivison, and the Yukon Valley principally to the Hud- sonian, thoutj;-h it has also a well-marked Canadian section. Birds are comparatively rare in all the interior region, and it is difficult to determine the exact range of many species. Some were seen but once or twice; others appeared sporadically at rather long intervals; while still others that are known from the region were not seen at all; so it is hardly safe, in making generalizations, to ridy too much on the ranges obserxed b}- us. The distribution of trees and shrubby plants and of man}' of the manmials, however, could be determined with much greater accuracy and constitute reliable guides in fixing the limits of the districts. These districts are in general the same as those recognized by Nelson, but with more definite and somewhat modified limits. Names slightly different from those he used are adopted here in order to agree with the commonly accepted names of the primary zones of North America. Thus the part of his 'Alas- kan-Canadian' district here considered is called the 'Hudsonian Yukon ' district, since it lies entirely within the transcontinental Hud- sonian zone. Owing to fluviatile conditions, the boundaries of the Yukon districts doubtless do not agree in latitude with those which might be made away from the rivers. The zones which we successivel}^ traversed in going from Skagway to St. Michael via White Pass and the Yukon are: (1) Canadian; (2) Hudsonian; (3) Arctic- Alpine; (4) Canadian; (5) Hudsonian, and (6) Arctic. The Lynn Canal district is in the Canadian zone, but it has some slight peculiarities such as are to be expected in a coast district. Though it does not have the Hudsonian animals of the northern coast, it lacks several of the typical Canadian forms of the coast farther south. ^ It is really near the northern limit of the Canadian zone on ^The coast of Alaska south of the peninsula, or what has been known as the 'Sit- kan district,' may be easily divided into two districts corresponding to the Canadian and Hudsonian zones. Lynn Canal is situated near the boundary between these districts. Among Canadian mammals which have their center of abundance in the restricted Sitkan district on the coaat south of Lynn Canal are: OdocoUeus sitkensis, Sciurus vancouverensis, Peromyscus ^nacrorhinus, Erotomys urangdi, Microtus maatii'us, Synaptomys wrangeli, Zapus mltator, and Myotis alascerms. Among the Hudsonian forms found on the coast only north of Lynn Canal are: Eangifer sp.. Oris dalli, Sciunts hndsonicus, Spermophihtx r. plmufi, Zapus h. alascensis, Ochotonn coUaris, and Myotis hiclfugm. Among trees which find their northern limit in the vicinity of Lynn Canal are: Thuja plkaia, Ahies lasiocarpa, and Phnis murrayana. The northern district from Lynn Canal to Kadiak is so similar to the great interior Hudsonian region that it hardly merits recognition as a distmct district, but it certainly should not be included in the Sitkan district. OCT., 1900.] SUMMAKY OF FAUNAL DISTRICTS. l7 the Pacific coast. The occurrence at Skagway of iiiummals of the interior, such as Mlwotus m'ordax,^ Evotomys dmcwnl, and Peromyscua or^eas, seems to show an approach to the condition farther north where the coast and interior forms are practically the same. The Canadian zone of the Lynn Canal district gives way to the Hudsonian and Arctic-Alpine in the White Pass district. The character of this dis- trict is essentially the same as that of other mountain regions in western North America. This is well indicated by the fact that its mammals include the hoary marmot {Arctomys caligatm), the Alaska pika {Ochotona coUaris), and the mountain goat {Oreamnos mo7itanm)^ and its birds the ptarmigan {Lagopiis Imourus and Z. rupestris), the pipit (Anthuspensilvamcits), and the rosy finch (Leucostccte t. littoraUH). The Canadian Yukon district from Bennett to Fort Selkirk merely represents the extent to which our route entered the extreme northern part of the Canadian zone; that is, its limits are those of the section that our route made across the end of a narrow tongue which extends northward from the great areas occupied by the Canadian zone farther south. Owing to its being so near the border of the Hudsonian zone, its character is not purely Canadian, but the presence of such forms as chipmunks {Eutamias) and white-footed mice {Peromyscus) among manmials, night hawks {CJiordeiles) among birds, and lodgepole pines {Plnus murrayana) among trees, makes it evident that the Canadian element is very strong. The Hudsonian Yukon district represents the complete section which the Yukon River makes through the great northern forest belt of the Hudsonian zone. This belt corresponds to the Alaskan-Canadian district outlined by jTelson. It is bounded on the south by the Canadian zone and the extreme northern limit of southern forms, and on the north by the treeless tundra. On the west it probably reaches and includes the coast from Kadiak to Lynn Canal; on the east its limits are unknown. The Alaska Tundra district defines itself. Its character is the combined result of latitude and rigorous coast clunate. Our experience in this treeless district was limited to St. Michael Island and the ninety miles between Andraefski and the mouth of the Yukon. The animals of this region are not all abso- lutely confined to it, many of them ranging some distance into the forest belt. Small mammals, such as the Nelson vole {Mlcrotm ope- rarim), occupy so-called ' islands '—local spots oft'ering what are prac- tically tundra conditions— as far within the forest belt as Circle. 'The case of Microtas mordax at the head of Lynn Canal is particularly interesting, since a closely related form, M. macruriis, has been found at Glacier Bay on the north side of the mouth of the canal and also at Juneau on the south side, and would therefore be expected at Skagway, which is halfway between. Assuming that 7namirus has been dispersed from tlie south northward on the coast, it seems that it did not reach Glacier Bay by way of the present mainland, otherwise it would be fomid at Skagway. M. mordax doubtless reached Skagway from the interior. 4494— No. 19 2 18 NOETH AMERICAN FAUNA. [no. 19. The fauna of the Yukon Ijasin as a whole is composed of two prin- cipal elements, one containing absolutely circumpolar forms, evidently derived from the north, the other containing- forms which have their center of abundance farther south. This is particularly true of the mammals. Among the genera Ijelonging to the north may be men- tioned Ilan(j>fei\ EvoioniyH, Lenniius, and Dlcrostonyx^ all of which are circumpolar in distri})ution; those from farther south are Mcei^^ Sciuropterus, Etttamias, Peromyscus^ Neotoma^ Fihe/\ and Synajytomys. With the exception of alpine species and a few wide-ranging forms, chiefly carnivores, the variations of which are not sufficiently known to be of use in defining faunal regions, no species of mammals are common to the Yukon region and the Sitkan coast district. From this it seems that all the southern forms which reach the Yukon region have been derived from the interior rather than from the coast. This is also true of the trees and to a great degree of the birds. But, on the other hand, some species of land l)irds are common to the lower Yukon and the Sitkan district while a large intervening area in the interior is uninhabited by them.^ SelasphoruH rufus, Dendrolca townsendi^ and Ilyloclchla aoimlascldw were found on both sides of White Pass, but only rarely and for a very short distance on the interior side. PREVIOUS WORK. Our knowledge of the natural history of the Yukon region has been derived chiefly from two sources — the members of the Kusso-Ameri- can Telegraph Expedition and the Signal Service officers formerly stationed at St. Michael. The first information was gathered l)y the scientific corps of the Telegraph Expedition of 1865 to 1868. Promi- nent among the members of this corps were Robert Kennicott, Wil- liam H. Dall, and J. T. Rothrock, all of whom secured valual)le speci- mens and information. The notes of Kennicott were not published, owing to his untimely death at Nulato, May 13, 1866, but numerous specimens, particularly from the vicinity of Fort Yukon, are now in the National Museum, a monument to his faithful pioneer work. Among the numerous papers on various subjects relating to Alaska published by Dail are lists of birds and mammals.'^ A list of plants including some records from Fort Yukon was published by Rothrock.^ ^ One of these species is the varied thrush (Hesperocichla nsevia) which was found in the Lynn Canal district, but not in any numbers in the Yukon Valley above Daw- son. Below Dawson it is quite common along the Yukon and undoubtedly breeds there. It is well known to range along the Pacific coast to Kadiak, and thence to the shores of Kotzebue Sound and up the Kowak River. Its absence on the Upper Yukon and its occurrence all along the coast make it extremely probable that in reaching the Yukon its course of migration is up the river from its mouth. ^ List of Birds of Alaska, by W. H. Dall and H. M. Bannister < Trans. Chicago Acad- emy of Sciences, I, pt. II, 267-310, 1869; also Alaska and its Resources, by W. H. Dall, Boston, Lee & Shepard, 1870. ^Sketch of the Flora of Alaska, by J. T. Rothrock < Annual Report Smithsonian Institution, 1867, 433-463. OCT., 1900.] NEW SPECIES. 19 In 1874, with the establishment of a meteorological station at St. Michael, work was begun by Lucien M. Turner. Ho collected about St. Michael and secured specimens from the fur traders and natives on the Yukon as far up as Fort Yukon. The results of his work were published in the Arctic Series of the Signal Service.^ Turner was relieved in 1877 by E. W. Nelson, who continued to collect specimens until 1881. His work was more extensive than that of Turner, but was carried out along the same lines. He made several trips up and down the coast from St. Michael, and also worked about the Yukon delta and up the river as far as Anvik. L. N. McQuesten, who conducted a trading post at Fort Reliance, furnished him with numerous specimens and much valuable information. The results of Nelson's work were also published in the Arctic Series of the Signal Service ^ and form by far the most valuable contribution to the natural history of Alaska jet made. In 1889 an important report ^ was pub- lished by Dr. George M. Dawson, covering the region of the sources of the Yukon and down as far as Fort Selkirk. This report contains detailed descriptions of the physical features of the upper river, notes on natural history, particularly on the distribution of trees, and a list of plants by John Macoun. NEW SPECIES. Nine new species and subspecies of mammals arc doscril^ed in the present report. They are as follows: Scluropterus yukonensis. Sciurus hudsonicus petalaris. Eutamias caniceps. SpcrmopMlus emj)etra j)lesitis. Neotoma saxamans. Fiber spatulatus. Lepus saliens. Lutreola mso^i ingens. Mustela amerlcana acluosa. In the collection of birds, three new forms were found. These have been described by Dr. Bishop * as follows : Canachites canadensis osgoodi. I Contopus richardsoni saturalH,'^. Sayornis saya yukonensis. \ ^ Contributions to the Natural History of Alaska, by L. M. Turner, Arctic Series, Signal Service, No. II, Washington, 1886. '^ Report upon Natural History Collections made in Alaska, by E. W. Nelson, Arctic Series, Signal Service, No. Ill, Washington, 1887. ^ Geological and Natural History Survey of Canada, Annual Report, HI (1887-88), Pt. I, 6 B-277 B, 1889; * Auk, XVII, 113-120, April, 1900. 20 NOKTH AMERICAN FAUNA. [no. 19. Besides the tibove, several new mammals whieh come within the scope of the present report have been recently described by Dr. Mer- riam.^ These are as follows: hfpermophilus osgoodi. Lemmus yukonensis. Lemmus alascensis. Dicrostonyx nelsoni. Ereihizon epixcmthun myops. Lepus americanus dalli. Lepus othus. Vulpes hallensis. Sorex personatus arclicus. Sorex tundrerms. In addition to these, three new forms recently described ))y Witmer Stone '~ should be mentioned: jyicrostonyx hudsonius alasceTisin ( equals D. nelnoni Merriam ) . Puturius rixosus eskimo. Lynx canadensis mollipilosus. 1 Proc. Wash. Acad. Sci., II, 13-30, March 14, 1900. '' Proc. Acad. Nat. Sci. Phila., March 24, 1900, 33-49. MAMMALS OF THE YUKON REGION. Bv Wilfred H. Osgood. INTRODUCTION. The following list, primarily based on collections made during the past year, includes all the known mammals of the Yukon region. Besides the species which belong strictly to the Yukon, are included those found in the Lynn Canal and White Pass districts and those known to occur at St. Michael. This makes a list containing the majority of the mammals known from Alaska, which is not, however, intended to be comprehensive, but should be considered as supplementary to the list published by Nelson in 1887. As may be seen from the itin- erary, our collections were made during a hasty trip from the coast of southeastern Alaska to the head waters of the Yukon and thence down the river to St. Michael. Good series of all the common small mam- mals were secured, but the larger and rarer species were not often obtained. It was not only difficult to secure specimens of the larger mammals, but it was hard to gain much accurate information in regard to them. Most of the miners we met had lieen in the country but a short time and their knowledge of animals was limited; natives were seldom met on the upper river and the few that were interviewed seemed disinclined to talk. The fur trade on the Yukon has dwindled to comparatively meager proportions. The Indians still bring a few furs to the traders every year and receive pittances of flour and tea in return; but the trade is apparently very small and were it not for the transportation business which has recently become so important, the large companies would doubtless find it difficult to maintain themselves. In identifying the recently collected specimens and studying their geographical distril)ution, it has been necessary to refer constantly to the specimens collected by Kennicott, Dall, Nelson, and Turner. Many of these, which are in the National Museum, were found to be in poor condition and required considerable renovating to make them compar- able with modern specimens. For the free use of these specimens I am indebted to Gerrit S. Miller, jr., assistant curator of manunals in the National Museum. I am also indebted to Outram Bangs for the use of specimens, and E. W. Nelson for much valuable informa- tion. The identifications of some of the mammals have been verified 21 22 NORTH AMERICAN FAUNA. [NO. 19. by spccialistj as follows: The species of Sorex by Dr. C. Hart Merriam; of Microtus by Vernon Bailey, and of Zapus by Edward A. Preble. All measurements are in millimeters. LIST OF SPECIES AND SUBSPECIES. 1. Rangifer montamis Seton-Thompyon. 2. Rangifer arcticus ( Richardson) . 3. Rangifer tarand us (Linnaeus). 4. Alces gigas Miller. 5. Ovis dalli Nelson. 6. Oreamnos montanus {Ord) . 7. Sciuropterus yukonensis sp. nov. 8. Sciurus hudsonicus Erxleben. 9. Sciurus hudsonicus jJetulana subsj). nov. 10. Eutamias caniceps sp. nov. 11. Spermophilus empetra 2)lesius subsp. nov. 12. Spermophilv^ osgoodi Merriam. 13. Arctomys caligatus Eschscholtz. 14. Castor cayiadensis Kuhl. 15. Mus decumanus Pallas. 16. Peromyscus oreas Bangs. 17. Peromyscus maniculatus arcticus (Mearns). 18. Neotoma saxarnans sp. nov. 19. Evotomys dawsoni Merriam. 20. Evotomys dawsoni alascensis (]Miller). 21. Microtus mordax CNLerrisun) . 22. Microtus drummondi ( Aud.and Bach. ) . 23. Microtus xantJiognathus (Leach). 24. Microtus ojyerarius (Nelson ) . 25. Fiber spatulatus sp. nov. 26. Synaptomys dalli Merriam. 27. Lemmus yukonensis Merriam. 28. Lemmus alascensis Merriam. 29. Dicrostonyx nelsoni Merriam. 30. Zapus hudsonius alascensis Merriam. 31. Erethizon epixantkus myops Merriam. 32. Ochotona collaris (Nelson) 33. Lepus saliens sp. nov: 34. Lepus americanus dalli Merriam. 35. Leptis othus Merriam. 36. Lynx canadensis mollipilosus Stone. 37. Canis occidcntalis Richardson. 38. f Vulpes fulvus (Desmarest). 39. Vulpes hallcnsis Merriam. 40. Ursus americanus Pallas. 41. Ursus horribilis alascensis Men-iam. 42. Lutra canadensis (Schreber) . 43. Lutreola vison ingens subsp. n( »\-. 44. Putorius arcticus Merriam. 45. Putorius cicognani alascensis (Mer- riam.) 46. Putorius nxosus eskimo Stone. 47. Mustela americana actuosa subsj). nov. 48. Mustela pennanti 'Erxleben. 49. Gulo luscus (Linnaeus). 50. Sorex personatus streatori Merriam. 51. Sorex 2Jerso7iatus arcticus Merriam. 52. Sorex obscurus Merriam. 53. Sorex tundrensis Merriam. 54. Myotis lucifugus (Le Conte). ANNOTATED LIST OF SPECIES. Rangifer montanus Seton-Thompson. Mountain Caril)oii. Rangifer montamis Seton-Thompson, Ottawa Naturalist, XIII, No. 5, (i, Aug. 11, 1899; Allen, Bull. Am. Mus. Nat. Hist., N. Y., XIII, 1-18, April 3, 1900. This large woodland caribou is reported as quite eouimon in northern British Columbia al^out the head waters of the Yukon and for an indefinite distance northward. It does not occur on the coast south of Cook Inlet, but is reported from many points immediately bej'ond the summit of the coast mountains. It prefers the higher ground in summer and is not found along river bottoms like the moose, for which reason few are killed by parties descending the river. Its fiesh is smoked and dried b}^ the Indians for winter food, and when so cured is preferred to all other meat of the country. The hides, like those of the moose, serve the natives for various articles of clothing and a"e utilized especialW for sleeping ro])es. OCT., 1900.] MAMMALS OF THE YUKON REGION. 23 Eangifer arcticus (Richardson). Barren Ground Caribou. The barren ground caribou ranges over nearly all of extreme north- ern North America from northwestern Labrador to the Aleutian Islands. It was formerly abundant over this great territory, but is now quite rare. Even at the time of Nelson's work in 1877 it had become comparatively uncoumion, though it was once common all about Norton Sound and for some distance up the river. The south- ern and interior limits of its range are uncertain. During our stay in St. Michael, I saw half a dozen skins which had been secured near Andraefski, 90 miles above the mouth of the Yukon. There are specimens in the National Museum from Nushagak and Unalakleet, Alaska; and from Rampart House and La Pierre House, Northwest Territory. Rangifer tarandus (Linnfeus). Domesticated Reindeer. During the past few years, as is well known, an effort has been made to introduce domesticated reindeer from Siberia into Alaska. The animals as a rule have been carefully herded, but in a few cases they have had opportunities to stray away and run wild. The herd that had perhaps the best chance to stray was one which was brought from Lapland to Haines in 1898, and driven inland over the Dalton trail. A short time after it started several of the animals were seen in the forest near Haines, and one of them was killed. This was the only instance of the kind brought to my attention, but I have no douljt that reindeer have occasionally wandered from the care of the herders at other times and in other places. Alces gigas Miller. Alaska Moose. Aires ffigas Miller, Proc. Biol. Soc. Wash., XIII, 57-59, May 29, 1.S90. The Alaska moose, as has frequently been stated, is the largest of the deer family in North America. Its distribution along the Yukon extends from Lakes Atlin and Tagish at least to the mouth of the Tanana and prol)al)ly somewhat farther. Whymper^ says that it was 'never known as low as Nulato,' even in the time of its greatest abundance. It is evident, however, from the record of Nelson ^ at the Yukon delta, and that of Richardson ^ at the mouth of the Mackenzie, that it does occasionally leave its favorite woodlands of the interior and wander as far as the Arctic coast. At present it is still quite numerous, but is chiefly contined to the small streams tri])utary to the Yukon, According to reports which came to me it is abundant in the region al)out the upper waters of the Stewart, Pelly, and MacMillan rivers. Along- the great river itself numbers have been killed during ^ Travels in Alaska and on the Yukon, 245, 1869.' ^ Report upon Natural History Collections in Alaska, 2S7, 1887. ■' Fauna Boreali-Aiuericana, 233, 1829. 24 NORTH AMERICAN FAUNA. [no. 19. the recent iiiHux of pro.spectors. At the l)egiiining of the Klondike rush, it wjis not uncommon for a l)Jirty to secure one or two moose while descending the river, but such is rarely the case at present. Our party failed to see any, though w^e spent nearly three months in the region; duiing this time we heard of but two animals being killed, one near the foot of Lake Lebarge and another on upper Charlie Creek, a short distance above Circle; both were secured by Indians. We saw comparative!}^ few fresh tracks. In winter, moose meat is the staple diet of both Indians and whites and has readily sold in the mining camps at $1 to $2 per pound. Such a price, even in this country of high wages, has l)een a great incentive to hunting, and many a miner has left his claim to pursue the moose. The hides also are a source of prolit, particularly to the Indians, who tan them and make them into mittens and moccasins. What the Indians do not need they sell readily to miners and prospectors. It is dif- ficult to estimate the number of animals that have been killed, but it must be ver}^ large, for the demand has been steady and a comparatively large population has been supplied with meat. On one hunt, an ac- count of which has been given by Tappan Adney,^ 44 moose were killed in about one month, and a single party of Indians was credited with a total of 80 moose and 65 caribou in one Avinter. Ovis dalli (Nelson). Dall Mountain Sheep. Most of the specimens of the Dall sheep which have reached our museums were secured in the vicinity of Cook Inlet, but the animal occurs in nearly all the high mountains of Alaska, and in the north ranges to the Arctic coast. Since we were at a distance from the mountains during the greater part of our trip, I was unal)le to secure much information in regard to the distribution of the species. Sheep are said to occur about the West Arm of Lake Bennett, and Windy Arm of Lake Tagish. A prospector with whom I talked at Lake Tagish said he had seen and killed them at both of these places. Lake Bennett is not far from the type locality of 0. stonei, and it is possible that this species occurs there with O. dalli. Both white and gra}' sheep are reported, though all are said to be white in winter. I was told that white sheep were killed some years ago on the cliffs about Lake Lebarge, but I failed to find signs of them there. Prospectors at Fort Selkirk say that sheep are always to be found in the mountains along Pelly Kiver, particularly in the MacMillan Mountains ^ near the mouth ' Harper's Magazine, C, 495-507, March, 1900. ^ The sheep from the MacMillau INIouiitains are 8aid to he the ' black wlieep,' which name could hardly api:)ly to 0. dalli, hut i.s the name commonly given to 0. stoneL If Monc'i really does occur in these mountains the record is a very interesting one, and the locality nmch farther north than any from which thesjjecies hiia been previously recorded. OCT., 1900.] MAMMALS OF THE YUKON EEGION. 25 of MacMilliui liivor, and they were also reported from the head waters of the Stewart and from the Xanana Hills. Oreamnos montanus (Ord). Mountain Goat. Goats occur on the high granite clifl's which inclose the upper part of Lynn Canal; they arc also common on the mountains near White Pass and about the rock}' walls of Lake Bennett. 1 was told that they had been killed recentl}'^ at the upper end of Little Windy Arm on Lake Tagish, but I could obtain no relia])le report of their occurrence in the interior bej^ond this point. At Lake Lebarge they were very doul)tfully reported. Their range is known to extend north to White Pass in the coast mountains at least to Copper River/ ])ut does not reach far into the interior. Hunters from the mountains a1)out the upper waters of the Pelly and Stewart rivers asserted positively that none had been heard of in that region. The station agent at Glacicn-, near White Pass summit, told me that goats frequently appear on the cliffs within easy view of his house. He also showed me the hide of one that had been killed near there a short time before our arrival. I made one short trip into these mountains, but failed to see any goats. The character of the cliffs is ideal for them, but they had evidently gone farther hack to their summer feeding' grounds, as the abundant tracks and dung were a few weeks old. Sciuropterus yukonensis sp. nov. Yukon Flying Squirrel. Ti/2'i' from Camp DavidiJon, Yukon River, near Alasska-Canada boundary. No. Hf if) U. S. Nat. Mu.«. Collected Decemljer 8, 1890, by R. E. Carson. Characters. — Size largest of North American flying squirrels; tail exceedingly long; color rather dark, underparts suffused with fulvous; skull slightly characterized. Color. — Top of head, neck, and upperparts to base of tail pale cin- namon or between the wood brown and cinnamon of Ridgway; under- fui' ]>luish black, partially exposed on legs and membranes; underparts dull whitish, irregularl}^ suffused with cinnamon fawn; feet dusky above, lightly edged with creamy white, buffy white below; cheeks and sides of head ashy, lighth^ mixed with cinnamon; end of nose slightly paler than top of head, not light ashy as in S. sahrinus; black e^'c-ring prominent; tail light fawn below, with a light edging of dusky, becoming l)roader toward tip; tail above fawn heavily mixed with black, which predominates for terminal fifth. Sh///. — Size large, slightly larger than in S. alpfm(.s/ audital bulla? larger; width at postorbital constriction greater; molars heavier, particularly the mandibular series. 1 H. T. Allen, Science, YII, 57, 1886. 26 NORTH AMERICAN FAUNA. [no. 19. Measurements. — Total length 3^)5; tail 180; hind foot (measured dry) 41. Skull: Occipitouasal length 40; zygomatic breadth 35; postorbital con.striction 10. Remarks. — This species is distinguished from both 8. sdbrinus and S. al2)inu.s by its large size and very long tail, but it is also ver}^ dif- ferent from either in color. It is evidently a ver}" rare squirrel, as the type and one topotype are the only specimens known. A speci- men from Chilkoot Inlet which ma}" possil)ly be this species has been recorded l)y Dr. George M. Dawson.^ Camp Davidson is the north- ernmost point at which the genus Sciuropterus is known to occur. The type and one other specimen were secured by R. E. Carson, who was a member of the boundary survey part}^ of the l^. S. Coast and (leo- detic Survey under J. E. McGrath, in 1890. Dr. W. W. Kingsbury, also a member of the party, writes me as follows in regard to these specimens: I send you the following notes taken from my journal regarding two Flying Squir- rels which were captured l)y a member of our party while in Alaska, in 1890; their skins were sent to the National Museum at Washington. The female was caught Dec. 8th, 1890, and the male Dec. 9th, 1890. Both squirrels were caught in a trap known as the 'dead fall,' which was set by R. E. Carson for marten. The traps were set in the bed of a frozen stream, where it ran through a clump of spruce trees about one-fourth of a mile back from the Yukon river. This clump of trees is about 2J miles east of the International boundary line, and on the east bank of the Yukon river. We showed these skins to both McQuesten and Mayo, two traders who had been in that country over twenty years, and who said that they had seen Flying Squirrels along the Yukon river quite a number of times before, and had also seen them at Ft. Reliance and Ft. Yukon; but had not seen any of them for a number of }'ears before this date. We also showed the skins to an Indian, who said these squirrels would attac'k a man by flying in his face, and the Indians would not eat them because the squirrels ate dirt. During the winter and spring of that year, I hunted very carefully in the vic-inity where these squirrels were captured, but failed to find further ti-ace of them. The stomachs of both of these squirrels were empty. The traps in which they were caught were set for martens, and two or three had been caught, but none were caught in tl>ese traps after the squirrels were captured. Sciurus hudsonicus Erxleben. Hudson Bay Red Squirrel. All the red squirrels from the Yukon basin and northern Alaska, as far as can be determined at present, are referable to Sciurus kudsoni- cus ' proper,' although those from the Upper Yukon show considerable tendency toward 8. h. streatori. Most of the Yukon specimens are in summer pelage, while the few available specimens from eastern Canada and the vicinity of Hudson Bay are in winter pelage, so that close comparison is not possible. Specimens from various points along the Yukon from Bennett to Nulato have been examined. The ' Geol. and Nat. Hist. Survey of Canada, Annual Report, III (1887-88), pt. 1, 50 A, 1889. North American Fauna, No, 19. Plate IV. S ■•' ■■"it ,>. P':'%:W* S*.?^^. i'^ '' ''^4if ^ft£^^^^ ' !*4H b ^ ^|K^; Hhv^'' ^ ' '^' i n* ^*^ ^ "^ ^'^'^W^ F™1 1_ i. ■;■- IflHHHK^dl -IS^: Fig. 1.— Nests of Red Squirrels in Spruce Thicket. Fig. 2.— Burrows made by Red Squirrels in loose Scales stripped FROM Spruce Cones. OCT., 1900.] MAMMALS OF THE YUKON EEGION. 27 animal is exceedingly abundant in all the .spruce forest, and doubtless ranges northward to the limit of trees. Evidences of its activity are to be found all through the spruce forest. Its globular nests of grass, moss, bark, and refuse are com- mon (Plate IV, fig. 1), and are usually situated near the trunk of some slender spruce, 10 or 20 feet from the ground. Sometimes several will ))e found in the same tree, and a half dozen or more are very often to be seen at the same time. Little excavations in the moss show where the chickarees have been digging for roots; and spruce cones tucked away in these and other out-of-the-way places are fur- ther evidence of their sagacity. The ground is often strewn for some distance with the scales of spruce cones which they have stripped (Plate IV, fig. 2). Near Lake Marsh I found one such place 20 feet square which was covered 6 inches deep with scales. Sciurus hudsonicus petulans subsp. nov. Ti/pe from Glacier, White Pass, Alaska (altitude 1,870 feet). No. 97457, U. S. Nat. Mus., Biological Survey Collection, ? ad. Collected June 4, 1899, by W. H. Osgood. Original No., .370. Characiers. — Similar to aS'. hudsonicrts^ but larger and darker; central portion of tail darker and with slight mixture of black; submarginal black in tail wider; edging of tail much darker; underparts not pure white in summer. Similar to Sciurus Ji. streatori^ but more reddish; central portion of tail with much less admixture of black; subterminal black in tail much narrower. Somewhat similar to S. Vancouver ensis^ but paler and cranially different; lateral stripe much more prominent; submarginal and subterminal black in tail narrower; median dor.sal stripe less suffused; median dorsal hairs of tail with much less black. Color. — Summer pdage: Upperparts between the raw umber and Prout's brown of Ridgway; top of head slightly darker than back; lateral line prominent, intense black; forelegs and feet russet; under- parts lightly washed with fulvous; median dorsal portion of tail hazel, slightly mixed with black-tipped hairs; submarginal and subterminal l)lack in tail rather limited; edging of tail ochraceous; under surface of tail palei- than upper, the grayish roots of the hairs showing through. ^¥^nter 'pelage: Similar to the corresponding pelage of S. hudsonicus^ but considerably darker; median dorsal line more diffuse; tail darker and with greater admixture of black in central portion. Skull.- — Similar to that of hudsonicus and its other subspecies; nasals longer and posteriorly more compressed than in S. vancd those from Cook Inlet are clearly referable to it. A more or less im- perfect specimen from Inverness, British Columbia, indicates a possi- ble interg-radation with Sciurns h. streatmn. There is ample material demonstrating ])y skulls as well as by color that it has no very close relationship to S. Vancouver ensis. My specimens oij)ettdmhs taken early in June are in new summer pelage or in old winter pelage just previous to or in process of change. The latter doubtless does not fairly represent the winter pelage; but in making comparison with eastern specimens, 1 have chosen those in a similar condition. About Lynn Canal and on the southwest side of White Pass I found these red squirrels abundant. Several at Glacier had become quite tame, and came every day to the cabin of one of the railroad hands to be fed. They have all the vivacious energy, curiosity, and vocal accomplishments of their Eastern cousins, and fully maintain their reputation for rollicking- good nature and fearlessness, Eutamias caniceps sp. nov. Gray -headed Chipmunk. Tyjw from Lake Leljarge, Northwest Territory, Canada. No. 99200, V. S. Nat. Mus., Biological Survey Collection, ? ad. Collected July 13, 1899, Ijy W. H. Osgood. Original No., 603. Characters. — Similar to^. hwealis^i but grayer, particularly the head, tail, and feet; postauricular spots more prominent; uuderparts pure white. C6lm\ — Summer or j)ostbreeding j^^^Za^e.' Sides bright ochraceous, extending from Hanks forward and stopping immediateh' below ears, but interrupted at shoulders by the extension of gray from arm; five black stripes on back very distinct and, except outer ones, entirely unmixed with ochraceous; outer pair of light stripes pure white, prominent, not continuous with postauricular spots ; inner light stripes bluish white mixed with ochraceous; top of head brownish gray; postauricular spots bluish white, connected with throat b}^ a continuous light stripe running below ear; light stripes on sides of head promi- nent, almost pure white; dark stripes rufous mixed with blackish, narrower and darker than in E. horealis; underparts pure w^hite; feet yellowish white. Worn j>ut these would often frisk about within a few feet of me as if entirely oblivious of ni}^ presence. Spermophilus empetra plesius subsp. nov. Bennett Ground Squirrel. Type from Bennett City, head of Lake Bennett, British Cohimbia. No. 98931, U. S. Nat. Mus., Biological Survey Collection, 9 ad. Collected June 19, 1899, by W. H. Osgood. Original No., 465. Characters. — Similar to S. emjpetra and S. kadlacenHia., but smaller; general color less fulvous; under side of tail always clear bright cinna- mon rufous; molar teeth relatively much larger than in kadtacensis,' skull small and light and otherwise slightly peculiar. Color. — Postbreeding j)elage: Above, mottled as in S. emjpetra^ but general colorless fulvous; upperparts, mixed black, white and yellow- ish gray extending forward to top of head, becoming narrower and slightly grayer between shoulders; top of head chestnut mixed with black; nose and forehead clear hazel; under side of bod}' cinnamon rufous paling to nearly white around chin and extending to sides of body, neck and cheeks, and botR sides of legs; under side of tail some- what deeper cinnamon rufous margined by yellowish white; subterminal black in tail less extensive than in empet7'a and kadlacensis; median part of upper side of tail grizzled black and yellowish, narrow sub- margin and subterminal zone black, the whole edged and overlaid with yellowish white. The hairs of the back in ,6'. j^^&si-us are of two kinds, some being of several colors arranged in zones and some pure black for their entire length. The former, which are most abundant, are dark sooty plumbeous at the base followed by a zone of light gray, 1 See Allen, Bull. Am. Mus. Nat. Hist., N. Y., Ill, 109, 1890. 30 , NOKTH AMKKU'AN FAUNA. [no. 19. then one of hhick, tlu'ii yeilowisli white, and Hiially a black ti}). In S. cmipetni, tlic arranoeiiHMit is ])iiU'tically tlie same, but the upper part of the li^'ht gray zone; blends into ful\'ous. As this is the widest zone, it gives a fulvous suti'usion to the entire u])perparts of the ani- mal. Injjlesius the black sul)inaroin of the tail never shows through on the under side. Wodi xprhuj j^tdaijc: Upperparts 3'ellowish gray; top of head, forehead, and nose cinnamon rufous; thighs with faint suggestions of rufous; shoulders and neck hoary; sides and under- parts grayish white washed with yellowish and flecked with ochrace- ous; feet pale buffy ochraceous; tail paler than in postbreeding pelage. Skull. — Similar to that of S. emjpetra from Unalaska, but smaller and lighter; nasals shorter and wider in proportion to their length; postpalatal notch extending fai'ther f(jrward, being almost on a plane with the last molar; molar teeth decidedly larger than those of kadiace7ims. Measureiiients. — Tjqje (from dry skin): Total length 845; tail verte- brae 93; hind foot 50. Skull of type: Basal length 45; zygomatic breadth 35', postorbital constriction 13; length of nasals IS; least width of nasals G; alveolar length of molar series 13. Refmarlxs. — The material representing SjjermojjJdlus eiiijpetnt is still very scanty and imperfect. Specimens from the Arctic coast are few in number and poor in quality, while from Hudson Bay one flat skin, unaccompanied by a skull, is all I am able to find. I have considered this (No. 13932, U.S.N.M.) to bo typical of emjjetra and have used it in making skin comparisons. Since it agrees fairly well wdth speci- mens of the ground squirrel which has been introduced on Unalaska, I have used the skulls of these for skull comparisons. Specimens from Bristol Bay and the Alaska peninsula are apparentl}' intermediate between efmxjetra and j)l&slus. jS. kadiacensis is apparently confined to Kadiak Island, as specimens from the mainland immediately opposite the island are cranially and dentally distinct. The southern members of the group, colu7nbianu» and erythroglutceus, also need not be con- sidered, as they are very difierent from erripefra and 2jlesl'm. K plexitis was first met with on the south side of White Pass near Glacier, where a small colony was found on a steep rocky slope above the canyon. They were active here in early June while patches of snow still lay on the ground. On the summit of White Pass another small colony was found, and at Lake Bennett they were very abundant. Here their burrows are to be found wherever the conformation of the rocks affords lodgment of sufficient soil. From Bennett on to Fort Selkirk they are exceedingly abundant. We saw them daily about all the lakes, and as we floated down Fifty-Mile and Thirty -Mile rivers, we often saw them bobbing in and out of their burrows or scurrying along their little trails which score the banks. From sunrise till late in the afternoon, their sharp clicking cries OCT., 1900.] MAMMALS OF THE YUKON KECIION. 31 rang' out ticross tlic ^vater, ,so that, if not to ])e seen, the}' at least reminded us of their presence nearly' all the time. When alarmed, they stand erect on their haunches near their l)urrows and violently utter their sharp, high-pitched dlehetij dick as long as the exciting cause is in sight, always emphasizing each cry ]jy vigorously slapping their short tails against the groiuid behind them. As a rule they were quite wary, and it was not possible to get within gunshot without some concealment and careful stalking. The limit of the range of the spe- cies along the river is near Fort Selkirk. The last specimen secured was caught near Rink Rapids, but I learned that (juite a colony of ground squirrels exists on the west bank of the river just boloAV Fort Selkirk. Spermophilus osgoodi Merriam. Fort Yukon Ground Squirrel. Hpcrmnph'dm ot^ijuodl Merriam, Prof. AVash. Acad. Sci., II, 18, March 14, 1900. From Fort Selkirk, near the limit of Spermo2)ldlwiple8ius in the inte- rior, nearl}" to Circle, we saw no signs of ground squirrels of an}' kind. Just before reaching Circle, however, we began to see unmistakable signs of them and were soon attracted to a small colony by their click- ing calls which reached our ears as we floated down in midstream. The call is executed in about the same time as that of S. pleHiux^ but its pitch is nuich lower and its effect on the ear is utterly different. It suggests the click of castanets. On going ashore we found their burrows and connecting paths scattered over (juite an area on the hill- side. The colony occupied the open hillside and a few ledges of loose rock, and even extended down into a thicket of alder and willow at the foot of the hill. The animals were very shy and became much excited at our approach. Their long tails were very noticeable in marked contrast to the short ones of 8. jpledus^ which we had been accustomed to seeing. Fifteen specimens were secured.^ At this time (Aug. 14) they were all very fat and in splendid postbreeding pelage; the entire underparts were rich ferruginous without a trace of any othei* color; the back was very dark, and the long tail was full and bushy . One specimen was pure glossy black with faint shadowy indications of vermiculation on the back. Among the specimens in the National Museum from Fort Yukon are several in this melanistic condition, showing that it is not uncommon. The range of this spe- cies on the Yukon begins a])out ^0 miles above Circle and extends at least to Fort Yukon and probably to the mouth of the Tanana. Arctomys caligatus Eschscholtz. Hoary Marmot. Six specimens of the hoary marmot were secured in the AVhite Pass region and about Lake Bennett, where it was common. It is confined * ThiH valuable series was unfortunately destroyed. 32 NORTH AMERICAN FAUNA. [no. 19. to rocky, mountainous parts of the Hudsonian zone, and consequently we did not meet with it during the latter part of our trip, and only heard of it through reports from the mountains at the headwaters of the White and Tanana rivers. As elsewhere, it is familiarly known as the 'whistler,' although occasionally rather inappropriately called 'ground hog.' Its long drawn whistle is peculiarly mournful, par- ticularly when it breaks the deathly silence of some rock}^ canyon. It loves to stretch at full length on top of a large rock and bask in the sun. I frequently found it quietly enjoying itself in this manner. Castor canadensis Kuhl. American Beaver. It hardly seems possible that half a million or more beaver skin.'j have been secured in the Territory of Alaska. The animal is now almost as rare there as it is in the United States, the inevitable result of continued pursuit by both whites and natives, which has so many parallels that it is useless to emphasize it here. At Fort Selkirk I saw several beaver skins taken on a small tributary of Stewart River, and at St. Michael I found a very few in the warehouses of the trad- ing companies. Beyond this I saw or heard nothing of them, Mus decumanus Pallas. Norway Rat. Large rats are exceedingly abundant at St. Michael. Their intro- duction must have been effected very recently, as they were unknown there at the time of Nelson's work. Unalaska has long been their northern limit on the Pacific coast. They find shelter about the wharves and lumber piles at St. Michael and also infest the l)uildings, particularly food warehouses. Their distribution will undoulitedly soon be extended all along the Yukon by means of the many steamers now plying between St. Michael and Dawson. Peromyscus oreas Bangs. Bangs White-footed Mouse. Peromyscus oreas Bangs, Proc. Biol. Soc. Wash., XII, 84, March 24, 1898. Long-tailed mice were taken at Skagway, Glacier, Summit, Bennett, Caribou Crossing, Fifty-Mile River, and Rink Rapids. In general they seemed to be more woodland loving than the short-tailed species, though at Bennett a number were taken among bare rocks at the very water's edge. I first noticed them here while walking along the shore at night. They were darting in and out among the rocks, chasing- each other as if playing a game of tag, and often four or five were in sight at once. jP. otvas from the type locality is somewhat intermedi- ate between my specimens and those which come from the coast of Puget Sound and southern British Columbia. Northern specimens are slightly larger, paler, and less ruddy brown than typical oreas. They are very similar in color to canade7isis and increase the prob- OCT., 1900.] MAMMALS OF THE YUKON KEGION. 38 ability that the latter has a transcontinental range. Their skulls arc large]- and have fuller braincases than those of either oreaa or cana- densis. Peromyscus maniculatus arcticus (Mearns). Arctic White-footed Mouse. Ileupcroinyti Ifucupus ardicu-'i biennis, Bull. Xixi. Mus. Nat. Hist., N. Y., II, 285, Feb., 1890. A short-tailed white-footed mouse was found to be very common from Lake Marsh to Lake Lebarge. Thirty specimens were secured, most of them about the crevices of low ledges of rock along the lake shores. The name arcticus is onh^ tentatively used for these speci- mens, as its applicability can not be positively known until a series of Lal^rador specimens is obtained. My specimens do not differ from topotypes of arcticus^ and these in turn, as stated by Bangs, ^ do not differ in color and size from t3q:)ical maniculatus. The description of the skull of the Great Whale River specimen examined b}^ Bangs, how- ever, does not agree well with the characters of the skulls of arcticus, so it seems advisable to recognize arcticus as a subspecies of manicu- latus. It is probable that more material will amply justify this treat- ment of the western form. Neotoma saxamans sp. nov. Northern Bushy -tailed Rat. Typ<; from Be-nuett City, head of Lake Bennett, British Columbia. No. 98923, U. S. Nat. Mus., Biological Survey Collection, $ ad. Collected June 19, 1899, by W. H. Osgood. Original No., 462. (See Plate V, fig. 4. ) Characters. — Similar to Neotoma cinerea drummondi., but somewhat darker: underparts pure white; skull strongly characterized. Color. — (Type:) Above, grayish fawn mixed with black, becoming brighter on sides, Avhere the quantity of black is much diminished; underparts and feet pure white; eyelids intense black with a limited sooty area about them; nose and anterior cheeks ashy; tail slaty above, white below. Skidl. — Similar to that of W. drumm/mdi (Plate V, fig. 3^) but with interorbital space narrower; nasals narrower and more attenuate pos- teriorly; maxillary arm of zygoma lighter; sphenopalatine vacuities open; ventral surface of occipital with a high trenchant median ridge; front of incisors very pale. Measurements. — Type (from dry skin): Total length 452; tail verte- brae 192; hind foot 46. Skull of type: Basal length 52; zygomatic breadth 20; interorbital width 5; length of nasals 23. Reniarks. — Neotoma saxamans differs from N. cinerea^ N occiden- lAm. NaturaHst, XXXII, 496, July, 1898. '^Neotoma c. columbiann Elliot does not differ eranially from N. cmerea, and there- fore need not be considered in this connection. ^No. 75907, IT. S. Nat. Mus., from Jasper House, Alberta. 4494— No. 19 3 34 NORTH AMERICAN FAUNA. [no. 19. tdlls^ and iV. drumimmdl chiefly in its long attenuate nasals, open sphenopalatine vacuities, and pale incisors. The only specimens secured were caught in a slide of large granite ])owlders at the head of Lake Bennett. It was ascertained to occur, however, from White Pass to the Semenow Hills. In the cliffs above Glacier on the coast side of White Pass I found signs of Neotoina^ and once one peeped out of a crevice at me while I was busily engaged stalking a hoary marmot. It also occurs sparingly in the cliffs about Lake Lebarge and in the Semenow Hills, where the last evidences of its presence were seen. This distribution makes it the northernmost species of the genus. One night about 10.30, as I was returning to camp at Bennett, I saw one of these rats frisking about in the rocks. It was still quite light, and I immediately stopped and stood motionless while he darted in and out of the rocks. His movements were utterly noiseless and so quick that my eye could scarcely follow them. For some time his little whiskered nose appeared and disappeared at various openings in the rocks about ten feet away. Each time he would look steadily at me for a moment or two and then silently vanish. Gradually his curiosity overcame his caution, and in decreasing circles he came nearer and nearer until he bobbed out right before me and then cautiously approached until he could sniff at the toe of my shoe. A slight grat- ing of my gun barrel against a rock caused him to vanish like a flash, and this time he did not reappear. Evotomys dawsoni Merriam. Dawson Bed-backed Mouse. Red-lxicked mice are by far the most abundant maumials in the Yukon region. Although but one specimen was taken at Bennett, and none between there and Fifty-Mile River, in spite of considerable trapping, aside from this they were found all along our route from Skagway to Fort Yukon. The following are the most important localities at which specimens were secured: Skagway, Glacier, Ben- nett, W^hite Horse Rapids, Lake Lebarge, Rink Rapids, Fort Selkirk, Dawson, Char.lie Creek, and Circle. From a study of this series, which numbers over 100 specimens, it appears that all l)elong to one species, E. daivsoni. Its range probabl}^ reaches northward almost if not quite to the limit of trees. Specimens were trapped in all sorts of localities; along cold streams, under logs, in heavy moss, in Microtu^ runways, and among rocks. They abound on the large islands, where the}'^ were generally caught in dry, brushy places, in the dead leaves which cover the ground. We occasionally saw them during the day, and often heard them rust- ling the dead leaves on the ground about us as we lay in our blankets at night. They are the vermin of the miner's larder, and are always to be found about log cabins. ocT.,1900.] MAMMALS OF THE YUKON REGION". 55 Evotomys dawsoni alascensis (Miller). Tundra Red-backed Mouse. Bvotomys alascensis Miller, Proc. Acad. Nat. Sci. Phila., 1898, 364-367. The Evoto-inys found at St. Michael has heretofore been compared only with the Asiatic E. Tutilus. Its closest relationship is really with E. dawsoni^ with which its range is doubtless continuous. On com- paring the series secured at St. Michael with those in the same condi- tion of pelage from Rink Rapids,^ Northwest Territory, I am unable to find even the slightest difference in color or size. The skull of alascensis is slightly characterized by small, narrow molar series, and by nasals which have their posterior end truncate. The palate and audital bullse are not peculiar. The tail is often thick and bristly in winter pelage and in immature specimens of both dmmoni and alascen- sis. From this it appears that alascensis may be only a slightly marked subspecies. The favorite habitat of these mice about St. Michael is in the heaps of broken lava scattered about over the tundra. The}^ are very rarely taken in the Miarotus runways. They are common in the warehouses, which they seem to enter more readily than other mice of the tundra. Microtus mordax (Merriam). liong-tailed Vole. Specimens of this vole were taken at Skagway, Glacier, Bennett, Lake Marsh, Lake Lebarge, Rink Rapids, and near Charlie Village. Specimens from near the coast are almost exactly like those of the inte- rior and all are quite typical of the species. They were found in various environments, but the general habitat of the species was dry places rather than moist. At Glacier and Bennett they were secured on dry, rocky hillsides; at Lake Marsh two specimens were taken in the crev- ises of some granite rocks; at Lake Lebarge they were taken in the kitchen of a log cabin; at Rink Rapids, in an open, sandy place; and near Charlie Village, on the side of a cut bank, where they had made burrows and runways among the exposed roots of trees. Charlie Village is by far the northernmost locality from which the species has been recorded. Microtus drummondi (Aud. and Bach.). Drummond Vole. This is the most common meadow vole of the Yukon region. At Caribou Crossing and Lake Marsh its runways form interminable labyrinths in the level, open stretches of sedge at the margin of the water. It occurs in nearly all moist, grassy places from Caribou Crossing to Fort Yukon. From there it undoubtedly ranges farther on, at least to Nulato, where Dali took several specimens. It is most active during the day, as I easily learned by visiting traps night and ^ No good series of specimens is available from any point nearer Finlayson Eiver, the type locality of E. dawsoni, than Rink Rapids. This series is therefore used to represent the species. 36 NORTH AMERICAN FAUNA. [no. 19. morning. Near f'ort Yukon I found its runways on recently depos- ited silt sparsely j^rown uj) to Equlsetwm. Its burrows in this soft material were very mimerous, and at the entrance to each a little heap of earth in small globular lumps, as if carried in the mouth, was always to be seen. Microtus xanthognathus (Leach). Yellow-cheeked Vole. This tine species was met with only once. A small colony was found on a little stream near Charlie Village, occupying an old log ]am, part of which had become embedded in a matrix of sand and mud and overgrown with weeds. Burrows perforated this structure in numer- ous places, and well-beaten, open runways connected various openings about the protruding logs. The little animals were quite active during the daytime, and as I walked over the logs I occasionally saw one flash from one opening under a log to another and heard sharp little squeaks sounding all about beneath me. A liberal number of traps placed about yielded nine specimens, chiefly immature. The colony was apparently confined to the log jam, as traps set in suitable places but a few yards away secured only M. d/rummnondi. Four specimens of this vole collected l)y Kobert Kennicott are in the National Museum, one from the mouth of the Porcupine and three from the Yukon, 200 miles southwest of that point. Microtus operarius (Nelson). Nelson Vole. This vole was taken on a small stream about -10 miles above Circle, and a few more were secured between that point and Fort Yukon. It doubtless ranges from there to the coast. Forty-nine specimens were taken at St. Michael. These represent all stages of growth and several phases of color and seem to offer pretty conclusive proof that but one species of Microtm occurs at St. Michael. It was found in all moist parts of the tundra, being particularly numerous along the banks of the small ponds in the tall grass and rank, weedy growths. Fiber spatulatus^ sp. nov. Northwest Muskrat. Tijpe from Lake Marsh, Northwest Territory, Canada. No. 98567, U. 8. Nat. Mus., Biological Survey Collection, 9 yg. ad. Collected July 3, 1899, by AV. H. Osgood. Original No., 552. (See Plate VI, fig. 4.) Characters. — Similar in general to Fiber zibethicus; size small; color rather dark; skull small; molar teeth very small; nasals short and much expanded anteriorl3^ Col(yr. — Similar to Fiber zibethicus^ but apparently less suffused with fulvous. Shull. — Similar to that of Fiber zibethicus (Plate VI, tig. 3''), but smaller; jugals more slender, and but slightly produced dorsally ; audital bullae smaller; molar teeth decidedly smaller; nasals much shortened and ^ Simtulatus, spatulate, in allusion to the shape of the nasals. ^No. 76259, U. S, Nat. Mus., from Wilmington, Mass. North American Fauna, No. 19, Plate V. Skulls of Sciurus and Neotoma. (x u.) 1. Sciunis vancouverensis. 2. Sciunis kudsonicus petiUans. 3. Neotoma cinerea drummondi. 4. Neotoma saxamans. OCT., 1900.] MAMMALS OF THE YUKON REGION". 37 widely expanded anteriorl}^, rapidl^^ becoming- eonipressed posteriorly; angular process of mandible short, blunt, and upturned; condyle narrow and somewhat rounded. Memm^ements. — Tj'pe (from dry skin): Total length 4:95; tail verte- brne 170; hind foot 73. Skull of type: Basal length 57; zygomatic breadth 38; leng^th of nasals 21; alveolar length of molar series 14. Reiiim'Ji's. — Specimens of this species from Ugashik, Fort Kenai, Nushagak, and Nulato, in Alaska, have been examined. Besides these, I find two specimens from Alberta which seem to be referable to it, one from South Edmonton and one from Henry House. These all agree in having very small molar teeth and short, spatulate nasals, characters which are amply sufficient to distinguish the species from all other forms in the genus. The specimens secured by Nelson at St. Michael can not now be found, l)ut they doubtless show the same characters. Fiher osoyooseoisis has larger teeth and a much longer rostrum than spatalatus, so need not be further compared with it. From these facts it appears that Fiher .^patulatux is the form occupying all of northwest America, and is derived from a form east of the Rocky Mountains rather than from a western one. Muskrats occur sparingly all along the Yukon, where they find par- ticularly favorable environment about the many small swamp-invested ponds a short distance from the river banks. At St. Michael a few are still found about the open ponds on the tundra. Synaptomys dalli Merriam. Dall Lemming Mouse. Lemming nnce were taken at the foot of Lake Lebarge, at Rink Rapids, and near the mouth of the Chandindu River. At Lake L('])arge they were found in the long grass at the edge of a small pond; at other localities in cold, boggy places near small streams. The external characters of B. daUl have been unknown up to the present time, but, as was to be expected, they are in accordance with the gen- eral type so uniform throughout this genus. The color of the upper- parts is chiefly raw umber mixed with black; the lower parts are uni- form bluish white, and the feet and tail are dusky. The ears are of medium size and partially hidden by long hairs growing from the aiiterior base; a conspii-uous l)luish-white side gland is present in the males. The skull of the type of dalll is not fully mature and does not agree in all particulars with my specimens from the Upper Yukon. In these the skull is somewhat larger and heavier and the nasals ore a trifle longer and more noticeably constricted posteriori}". Lemmus yukonensis Merriam. Yukon Lemming. ic»imus 7/w^-o?ie?iS('s Merriam, Proc. Wash. Acad. Sci., II, 27, March 14, 1900. This lemming was found at only two localities — Rink Rapids, where five specimens were secured, and Charlie Creek, where five more were 38. NORTH AMERICAN FAUNA. [no. 19. taken. Considerable careful trappino- was clone at various points between these two places, but no other specimens were secured. At Rink Rapids they were caught about old logs and among dry leaves in places usually frequented by red-backed mice. At Charlie Creek one was caught in a M'wrotus runway and several were secured on the side of a cut bank. On one occasion one was seen running about under a brush heap in midday. Lemmus alascensis Merriam. Alaska Lemming. Lcmmui^ aluscensia Merriam, Proc. Wash. Acad. Sci., II, 26-27, March 14, 1900. All efforts to secure this species at St. Michael proved fruitless. I kept large numbers of traps out for more than two weeks and set them in all conceivable locations about the tundra, but failed to catch any lemmings. Dicrostonyx nelsoni Merriam. Nelson Pied Lemming. Dicrostonyx nelsoni Memam, Proc. Wash. Acad. Sci., II, 25-26, March 1-1, 1900. Dicrostonyx hudsonius alascensis Stone, Proc. Acad. Nat. Sci. Phila., March 24, 1900, 37-38. No specimens of this species were taken. Nelson says of it: Specimens were brought me by the fur traders from above Fort Yukon and from Nulato, Anvik, and Kotlik, along the course of the Yukon, and also from the Kaviak Peninsula and about Kotzebue Sound. A few were taken near St. Michael, but they were not numerous there. They are more plentiful about Bering Straits than any other district visited by me, if the number of their skins among the native children can be taken as a guide. Zapus hudsonius alascensis Merriam. Alaska Jumping Mouse. Three typical specimens of this jumping mouse were taken in a" sedgy swamp near the foot of Lake Lebarge. Similar swamps exist near the Yukon, at least as far as Fort Yukon, but I was unable to do any trapping in them. No specimens were taken elsewhere. Erethizon epixanthus myops Merriam. Alaska Porcupine. Erethizon epixantlius myojjs Merriam, Proc. Wash. Acad. Sci., II, 27-28, March 14, 1900. Porcupines are quite common in all the forest region of Alaska. I noticed signs of them at man}^ places along the Yukon. They were abundant about Glacier, in the White Pass region, and 1 shot one there one evening as it swayed back and forth in the top of a slender alder. It was eating the leaf buds which were just bursting. Ochotona coUaris (Nelson). Alaska Pika. Two specimens of an ashy gray Ochotona were taken, one at the summit of White Pass, another at the head of Lake Bennett. The species was apparently quite rare at these localities and it was only with considerable difficulty that these individuals were secured. Both are very pale, ashy gray, with pure white underparts, no traces of OCT., 1900.] MAMMALS OF THK YUKON REGHON. 89 fulvou.s, and vevy indistinct collars. They are in the early spring or left-over winter pelage, and agree quite well with specimens in the same pelage collected in the Chigmit Mountains, near Bristol Bay, by C. L. McKay. The type and topotypes of O. collaris are in the summer or post-breeding pelage and present quite a different appearance. The species apparently occurs in the high mountains throughout Alaska. It was reported to me from the MacMillan Mountains, the Upper Stewart River, the Upper White, and the Upper Tanana. Fragments of a skull were found in an owl pellet picked up by Dr. Bishop near Windy Arm, Lake Tagish. The present record from White Pass is the most southern one. There is suitable country for it farther south, and it will be interesting to trace its range in this direction. Lepus saliens sp. nov. Type from Caribou Crossing, between Lake Bennett and Lake Tagish, Northwest Territory, Canada. No. 98956, U. S. Nat. Mus., Biological Survey Collection, $ ad. Collected June 26, 1899, by W. H. Osgood. Original No., 504. Characters. — Similar to Lepus hairdi, but more yellowish and less ruddy; dorsal hairs with plumbeous roots; feet nearly white in sum- mer; similar to Z. coluiinihieiisis^ but with greater amount of black in dorsal region; feet much lighter; skull similar in general to that of Lepus a. dalli; audital bulla? very large. Color. — Type in wm'n spinng pelage: Upperparts mixed black and yellowish buff, with patches of plumbeous under -fur exposed in places; black hairs predominating on rump and middle of back, forming an ill-defined dorsal stripe; outer edge of thighs, outer side of forelegs and pectoral band buff; ears and head, except sides of nose, buff with black hairs sprinkled through; sides of nose gray; ears margined with white; hairs of fore and hind feet plumbeous at base, rufous in cen- tral part, and broadly white at tips; general appearance of feet white, lightl}^ mixed with rufous; underparts, except pectoral band, white. Skull. — Similar to that of dalli but somewhat larger; teeth heavier; nasals long, heavy, and very broad anteriorly; audital bullae very large; palate short; malars rather wide, deeply channeled anteriorly; postorbital and antorbital processes of f rentals well developed. Measurements. — Type (measured from dry skin): Total length 395; hind foot 134; ear from crown 74. Skull of type: Occipitonasal length 77; greatest zygomatic breadth 38; length of nasals 33; great- est width of nasals 17; alveolar length of molar series 16. Remarks. — The exact relation in which this species stands to ameri- canus^ hairdi.^ and columhiensis is difficult to determine at present. Its light feet point to relationship with haird% while its dark under color 1 Rhoads, Proc. Acad. Nat. Sci. Phila., 1895, 242-243. 40 NORTH AMERICAN FAUNA. [no. 19. and oenoral l)uliy appearance are more like eolumhlensh. Its skull is quite distinctive, the large audital bulke and broad nasals being- unequaled in the group. It seems probable that it is a northern form of hah'di not related to columhum^if^^ which is nearer to vxixhrixj- toni. There are no specimens availal)le to show whether or not it has any connection with dalli^ which is the form found on the Lower Yukon. But two specimens were secured — the type, which I shot in a Lejxirgyrcea thicket at Caril)Ou Crossing, and one very young female which Dr. Bishop took in a willow bog near Bennett City. It seems to have been a decidedly 'off year' for rabbits, for these two were the only ones we saw on our entire tY\\), though numerous signs of their former abundance were seen daily. Lepus americanus dalli Merriam. Dall Varjnng Hare. Le2yus americanus daUl Merriam, Proc. Wash. Acad. Sd., II, 29-30, March 14, 1900. This rabbit is doubtless abundant at certain times all along the Lower Yukon, but we heard very little of it. It is subject to epidem- ics and frequently becomes locally extinct, which probably accounts for its scarcity last year. Lepus othus Merriam. Alaska Arctic Hare. Lepufi otJi'iis Merriam, Proc. Wash. Acad. Sci., II, 28, March 14, 1900. Signs of Arctic hares were occasionally noticed about St. Michael, but we did not sec any of the animals. The Eskimos were hunting continually, and brought numbers of ducks and geese to the village to sell, but they brought no rabbits during our stay. Lynx canadensis mollipilosus Stone. Arctic Lynx. Lynx canadensis molKpilosm Stone, Proc. Acad. Nat. Sci. Phila., March 24, 1900, 48-49. The Canada lynx is not as common in the interior of Alaska as might be expected. I saw no signs of it and could obtain only very scanty information as to its occurrence. The police sergeant in charge of the station at the foot of Lake Lebarge told me that the tracks of but one had been seen in that vicinity during the previous winter. Lynxn skin robes are in common use in the country, but the majorit}^ of them are imported. This I learned from a trader at Circle, who had scA'cral for sale that came from eastern and southern Canada. Lynx skulls from the following localities arc in the National Museum: Tanana River, Russian Mission, Nulato, Andraefski, and mountains near Unalakleet. Canis occidentalis Richardson. Wolf. The country along the Yukon is not well suited for wolves, and they are seldom seen there. A prospector showed me the skin of a large gray one from the upper waters of the MacMillan river — the only one I saw on the trip. OCT., 1900] MAMMALS OF THE YUKON REGION. 41 Vulpes fulvus (Desmarest) 'i Red Fox. Occasional reports of foxes were received all along our route, l)ut no specimens were secured. Owing to their natural sagacity, foxes are doubtless able to hold their own against trappers better than most other fur- bearing animals. Their skins are quite common among traders and natives. Vulpes hallensis Merriam. Hall Island Fox. Vulpes hallensis Merriam, Proc. Wash. Acad. Sci., II, 1.5-16, March 14, 1900. White fox skins are common among the natives and traders at St. Michael, and could be bought at from $1 to $4 each, according to quality. During our stay there one of the animals was seen on the island, which indicates that they are still far from extermination. TJrsus americanus Pallas. Black Bear. Black and l)rown bears are common all along the Yukon. We found them conunon on the upper river, and Nelson records them as far down as Anvik. We saw tracks very frequently, but owing to the thick forest and underbrush, and the fact that we made no special hunts for them, the animals themselves were rarely observed. A young adult female in glossy black pelage was killed at Glacier by A. G. Maddren, and several others were seen during our stay there. I was told at Lake Lebarge and at White Horse Rapids that brown l)ears were seen very frequently. At Fort Selkirk I saw skins brought from the Pell}^ River. Near Charlie Village I saw the skin of a large brown bear that had been killed there shortly before our arrival. One afternoon while sitting in the boat preparing specimens, about 20 miles above Circle, I saw a good-sized black })ear walking deliberately across an open space on a hillside a short distance away. We gave chase, but did not see it again. At the mouth of the Tatondu River I saw numerous tracks, and on the border of a stagnant pool found evidences that bruin had been enjoying a mud bath. Moss uprooted hy })ears in digging for roots was noticed at several places. TJrsus horribilis alascensis Merriam. Alaska Grizzly Bear. Very little accurate information is obtainable in regard to the grizzly in the Yukon region. It doubtless occurs sparingly all along the river, but miners and prospectors report any large bear as a grizzly, and without doubt often mistake the brown bear for it. There are a num- ber of its skulls from Norton Sound in the Biological Survej^ collection. Lutra canadensis (Schreber). American Otter. The fate of the otter in Alaska is much the same as that of the bea- ver. There are doubtless a few on some of the smaller streams of the interior and about the Yukon delta, l)ut they are now quite rare in comparison with their former u1)uiidance. 42 NORTH AMERICAN FAUNA. [no. 19. Lutreola vison ingens sul)sp. nov. Alaskji Mink. Type (skull) from Fort Yukon, Alanka. No. G530, U. S. Nat. Mu.s., $ ad., old. Collected by Robert Kennicott. (See Plate VI, fig. 2.) Characters. — Size largest of North American mink; similar to L. v. energumenos^ but lighter in color and very much larger; skull and teeth v^ery large and heavy. Color. — Similar in general to Lutreola v. energumeno^., but palci-. Skull. — Very large, angular, and ridged; rostrum very wide; brain- case relatively sliallow and very wide; zygomata heavy; audital ])ulhe large and relatively wide; dentition heavy. (Compare with skull of Lutreola v. en^rgunienos, Plate VI, fig. 1.^) Measurements. — No. 13880, U. S. National Museum, St. Michael, Alaska (from dry skin): Total length 720; tail vertebras 180; hind foot 75. Skull of type: Occipitonasal length 69; zygomatic breadth 47; mastoid breadth 41; ])readth across postorbital processes 23; length of audital bulla 17. Average of five adults: Occipitonasal length 44.5; mastoid breadth 39.5; breadth across postorbital processes 21; length of audital bulla 17.5. LteinavTis. — The large size of the Alaska mink has been noted by various authors,^ but each has dismissed the subject by concluding that it is the natural result of the animal's northern range, and the form has remained unnamed, while less marked forms from other local- ities have been recognized. The largest mink previous!}^ described is L. V. en^ergumenos, which is very much smaller than rngen.^ and also averages much darker. The minks of the Yukon region are caught mostly on the tributarj^ streams, and, as stated by Nelson, are very abundant in the area between the deltas of the Yukon and the Kuskokwim. Along the Yukon itself our party did not see any, and very few signs of them were observed. Their skins were seldom seen among the Indians and Eskimos. They were reported, however, from the Porcupine, Koyu- kuk, Tanana, and various other streams tributary to the Yukon, and without doubt occur in suitable places all over Alaska. Putorius arcticus Merriam. Tundra Weasel. Puioriuii arcticus Merriam, N. Am. Fauna No. 11, 15, June, 1896. Putorius cicognani richardsoni Merriam, L c, 11-12 (part). Three immature specimens of this weasel were taken at St. Michael. They were caught in traps baited with sandpipers and set among the lava rocks along the shore. Several specimens which were also secured at St. Michael by Nelson and Turner are in the National Museum. Besides these I find specimens from Nulato, Fort Yukon, and Fort Reliance, which gives the species a more extensive range in the interior than it has been supposed to have. Most of these specimens are ^ No. 5537, Bangs collection, from Sumas, B. C. ■' See Allen, Bull. U. S. Geol. and Geog. Survey Terr., II, 327-328, 1876. North American Fauna, No, 19 Plate VI Skulls of Lutreola and Fiber. (Natural size.) 1. Liitrrold Tifion encrfinmriui>< 2. Lutreola rhon i)Hjni.<. 3. Fiber zibethicus. 4. Fiber spatidatns. ocT.,l'.ioo.] MAMMALS OF THE YUKON KEGION. 43 imperfect, but enough skulls are now at band to sbow conclusively that all tbe Yukon specimens heretofore identilied as rlcliardsoni are really practically identical witb P. arctlcus from Point Barrow. Putorius cicognani alascensis (Merriam). Juneau Weasel. A single immature specimen taken %) miles l)elow Fort Selkirk is referred to tbis form. Its skull is ratber large and indicates a possible intergradation with P. arcticus; otherwise it agrees with alascensi-H. Putorius rixosus eskimo Stone. Alaska Least Weasel. Putor'ms rixosux eskimo Stone, Proc. Acad. Nat. Sei. Phila., Marcli 24, 1900, 44-45. No specimens of this rare weasel were obtained. There are three imperfect specimens in tbe National Museum, two from St. Michael and one from Fort Reliance, Besides these tbe only ones recorded are the type and four topotypes from Point Barrow, Alaska, and tbe specimen mentioned by Stone (loc. cit.) from Bethel, Kuskokwim River, Alaska. Mustela americana actuosa subsp. nov. Alaska Marten. Type (skull) from Fort Yukon, Alaska. No. 6043, U. S. Nat. Mus., $ ad., old. Collected by Robert Kennicott. (See Plate VII, fig. 2. ) Characters. — Similar to 3£ hrumalis, but larger; cranial and dental characters distinctive. 6^>/^r/r.— (Topotype, No. (M16, U.S.N.M., ere- grina were each found at a single place, while still others, as Junco hyemalis and Merula viigratoria., were regularly distributed along the river. The Pacific coast forms probably all reach the Yukon over the Alaska coast range. These disappear as one goes north, Hylo- cichla aonalasclikm extending through Lake Bennett, Wilsonia 2^- X>^^eo- lata to Lake Marsh, Dendroica townsendi to Lake Lebarge, Myadestes townsendi to Dawson, and Tachycineta thalassina to Circle. Last and most important in number of species, abundance of individuals, and regularity of distribution are birds which breed in the Yukon Valley and spend the winter in the western United States, as Zono- trichia I. ganibeli^ Spizella s. arizonce, and the small Ammodramus s. alaudinus of the Yukon lakes, and those which probably enter by the mouth of the Yukon, as the large Ammodrarmis s. alaudinus, found below Alaska boundary, and Seiurus n. notabilis^ first met near Dawson. In coloring, Yukon birds, especially in juvenile plumage, show a strong tendency to replace the buff-ochraceous markings of Eastern forms by white, cream color, and gray. Canachites c. osgoodi, Parim h. evura, and Hylocichla u. alma are good examples of this characteristic. I take this opportunity to express \nj hearty thanks to Dr. Merriam for the privilege of visiting Alaska as a member of the Biological Sur- vey party, of writing this report, and of using the collection of the Biological Survey in its preparation; also to Mr. Osgood and Mr. Oberholser of the Biological Survey for aid in determining species. I am also greatly indebted to Mr, Robert Ridgway and Dr. Charles W. Richmond for the opportunity of studying the collection of the OCT., 1900.] CLASSIFIED LISTS OF SPECIES. 51 United States National Museum and for much valuable assistance; to Dr. J. A. Allen and Mr. F. M. Chapman for the hours which I spent with the birds in the American Museum of Natural History; to Mr, William Brewster for the courtesy of allowing me to compare my speciniens with those in his valuable collection, and to Mr. Walter Deane for much help in this study. CLASSIFIED LISTS OP SPECIES. NEW SUB8PECIE,S. Canachites canadensis osgoodi. Contopus richardsoni saturatus. Sayornis saya yukonensis. SPECIES NOT HITHERTO RECORDED FROM WESTERN NORTH AMERICA. Haliseetus albicilla. SPECIES NOT HITHERTO RECORDED FROM SOUTHEASTERN ALASKA. ^chmophorus occidentalis. Xema sabinii. Lagopus leucurus. Picoides americanus alascensis. Contopus richardsoni saturatus. Empidonax hammondi. Junco hyemalis connectens. Sitta canadensis. Merula migratoria. SPECIES NOT HITHERTO RECORDED FROM UNALASKA. Larus Philadelphia. Tringa maculata. Tringa acuminata. Loxia curvirostra minor. Larus Philadelphia Tringa acuminata. SPECIES NOT HITHERTO RECORDED FROM THE PRIBILOF ISLANDS. ? Arenaria melanocephala. SPECIES NOT HITHERTO RECORDED FROM ST. MICHAEL. Calidris arenaria. SPECIES NOT HITHERTO RECORDED FROM THE YUKON ABOVE FORT YUKON. Tringa bairdi. Symphemia semipalmata inornata. Buteo borealis calurus. Falco sparverius. ? Megascops asio kennicotti. ? Dryobates villosus hyloscopus. Contopus l)orealis. Contopus richardsoni saturatus. Empidonax trailli alnorum. Empidonax hammondi. Spinus pinus. Spizella socialis arizonse. Passerella iliaca. Helminthophila peregrina. Dendroica townsendi. AVilsonia pusilla pileolata. Sitta canadensis. Hylocichla aonalaschkie. Hylocichla aonalaschkte pallasi. Saxicola oenanthe. Colymbus holboelli. Colymbus auritus. Gavia im])er. Gavia arctica. LIST OF SPECIES KNOWN FROM THE YUKON BASIN. Gavia lumme. Stercorarius pomarinus. ' Stercorarius parasiticus.^ Stercorarius longieaudus.' ^ Known only from Fort Yukon or below. 52 NORTH AMERICAN FAUNA. [NO. 19. Rissa tridactyla pollit-aris.' Larus barrovianuw.' Larus argentatuH sinithsonianus. Larus vegae.^ Larus braehyrhynchus. Larus Philadelphia. Xema sabinii.^ Sterna caspia.' Sterna j^aradissea. Sterna aleutica.' HydrocheUdon nigra surinamensis.' Phalacrocorax pelagicus robustus.^ Merganser aaiericanus. Merganser serrator.' Anas boschas. Mareca americana. Nettion carolinensis. Querquedula discors.' Spatula clypeata. Dafila acuta. Aythya vallisneria.^ Aythya marila. Aythya affinis. Clangula clangula americana. Clangula islandica. Charitonetta albeola. Harelda hyemalis. Histrionicus histrionicus. Arctonetta fischeri.^ Somateria v-nigra.^ Somateria spectabilis.^ Oidemia americana.^ Oidemia deglandi. Oidemia perspicillata. Chen hyperborea. ' Anser albifrons gambeli.^ Branta canadensis hutchinsi. Branta canadensis minima. Branta nigricans. ' Philacte canagica. ' Olor columbianus. ' Olor buccinator.' Grus canadensis. Fulica americana. "^ Crymophilus fulicarius.' Phalaropus lobatus. Gallinago delicata. Macrorhamphus scolopaceus.' Tringa canutus. ' Tringa couesi.' Tringa maculata. Tringa bairdi. Tringa ininutilla. Tringa al])ina paciiica. Ereunetes occidentalis. ' Calidris arenaria.' Limosa lapponica baueri.' Limosa haemastica.' Totanus flavipes. Helodromas solitarius cinnamomeus. Heteractitis incanus. ' Bartramia lopgicauda. ' Synij)hemia semipalmata inornata.^ Tryngitcs subruficollis ' Actitis macularia. Numenius hudsonicus. Numenius liorealis.' Squatarola squatarola. Charadrius dominicus. Charadrius dominicus fulvus.' ^gfalitis semipalmata. Arenaria interpres.^ Arenaria melanocephala. ' Canachites canadensis osgoodi. Bonasa umbellus umbelloides. Lagopus lagopus. Lagopus rupestris. Pedioecetes phasianellus columbianus. Circus hudsonius. Accipiter velox. Accipiter atricapillus. Buteo borealis calurus.^ Buteo swainsoni.' Archibuteo lagopus.' Halifeetus leucocephalus alascanus. Falco rusticolus gyrfalco. Falco peregrinus anatum. Falco columbarius. Falco columbarius richardsoni.^ Falco sparverius.^ Pandion haliaetus carolinensis.' Asio accipitrinus.' Scotiaptex cinerea. Scotiaptex cinerea lapponica.' Nyi'tala tengmalmi richardsoni. ?Megascops asio kennicotti.^ Bubo virginianus pallescens. Nyctea nyctea.' Surnia ulula caparoch. Ceryle alcyon. Dryobates villosus leucomelas. ?Dryobates villosus hyloscopus.'' ' Known only from Fort Yukon or below. ^ Known only above Fort Yukon. OCT., 1900. J CLASSIFIED LISTS OF SPECIES. 53 Dryobates pubescens nelsoni. Picoides arcticus. Picoides americanus alascensis. Colai^te.s auratus luteus. Chord eiles virgin ianus.'^ Selasphorus rufiis.^ Sayornis saya yukonensis.^ Contopus borealin. Contopus richardsoni satnratus.* Empidonax trailli.' P^m])idonax trailli alnoruni.^ Empidonax hanimondi.'-' Otocoris alpestris leucoltema. Pica pica hudsonica. Perisoreus canadensis fumifrons. Corvus corax principalis. Scolecophagus carolinus. Pinicola enucleator alascensis. Pyrrhula cassini.^ Loxia leucoptera. Acanthis hornemanni exilipes. Acanthis linaria. Spinus pinus.^ Passerina nivalis. Calcarius lapponicus alascensis. Calcarius pictus.^ Ammodramus sandwichensis alaudinus. Zonotrichia leucophrys gambeli. Zonotrichia coronata. Spizella monticola ochracea. Spizella socialis arizonae.'^ Junco hyemalis. Melospiza lincolni. Passerella iliaca. Petrochelidon lunifrons. Ilirundo erythrogastra iinalaschkensis. Tachycineta bicolor. Tachycineta thalassina.^ Clivicola riparia. Ampelis garrulus. Lanius borealis. Helminthophila celata. Helminthophila peregrina.^ Dendroica sestiva rubiginosa. Dendroica coronata hooveri. Dendroica striata. Dendroica townsendi.^ Seiurus aurocapillus.' Seiurus noveboracensis notabilis. Wilsonia pusilla. Wilsonia pusilla pileolata.'^ Budytes flavus leucostriatus.' Anthus pensilvanicus. Cinclus mexicanus. Sitta canadensis.^ Parus atricapilhis septentrionalis. Parus cinctus alascensis.' Parus hudsonicus evura. Phyllopseustes borealis.' Regulus calendula. Myadestes townsendi.'^ Hylocichla alicise. Hylocichla ustulata almse. Hylocichla aonalaschkee.^ Hylocichla aonalaschkse pallasi.'' Merula migratoria. Hesperocichla na3\aa. Saxicola oenanthe. Sialia arctica.* SPECIES WHOSE OCCURRENCE ON THE YUKON IS DOUBTFUL. Chaulelasmus streperus. Eniconetta stelleri. Branta canadensis. Macrorhamphus griseus. Aquila chrysaetos. Nucifraga columbiana. Loxia curvirostra minor. Motacilla ocularis. ' Known only from Fort Yukon or below. ^ Known only above Fort Yukon. 54 NORTH AMERICAN FAUNA. (NO. ly. SPECIES AND SUBSPECIES OCCURRING IN THE YUKON UASIN AND HAVING THEIR CENTER OF ABUNDANCE DURING THE BREEDING SEASON IN ALASKA AND BERING SEA. Rissa tridactyla poUicaris.' Larus barrovianus.' Lams vegpc'.* Larus brachyrhynchus. Sterna aleutica.' Phalacrocorax pelagicus rol)ustus.' Arctonetta fischeri.^ Somateria v-nigra.' Chen hyperborea.^ Branta canadensis minima. Branta nigricans.^ Philacte canagica.' Grus canadensis.^ Macrorhampus scolopaceus. Tringa couesi.^ Ereunetes occidentalis. Heteractitis incanus. Canachites canadensis osgoodi. Haliteetus leucocephalus alascanus. ? Megascops asio kennicotti. Picoides americanus alascensis. Sayornis saya yukonensis. Contopus richardsoni saturatus. Perisoreus canadensis fumifrons. Pinicola enucleator alascensis. Leucosticte tephrocotis littoralis. Calcarius lapponicus alascensis. Hirundo erythrogastra unalaschkensis. Dendroica testiva rubiginosa. Dendroica coronata hooveri. Parus cinctus alascensis. Parus hudsonicns evura. Hylocichla ustulata almae. Hesperocichla ntevia. Arenaria melanocephala. Of these 35 forms, 1 is a subspecies of can Asiatic bird, 5 are chiefly confined to Bering Sea, 2 range in winter to the western Pacific, 7 are resident subspecies of northern North American birds, and the remaining 20 pass in winter to the western United States or beyond. EASTERN NORTH AMERICAN SPECIES FOUND IN THE YUKON BASIN. Limosa hjemastica. Numenius borealis. Accipiter atricapillus. Falco span^erius. Colaptes auratus luteus. Chordeiles virgiuianus. Empidonax trailli alnorum. Junco hyemalis. Passerella iliaca. Helminthophila celata. Helminthophila peregrina. Dendroica striata. Seiurus aurocapillus. Wilsonia pusilla. Hylocichla alicipe. Hylocichla aonalaschkpe pallasi. Merula migratoria. WESTERN NORTH AMERICAN SPECIES FOUND IN THE YUKON BASIN. Anser albifrons gambeli. Branta canadensis hutchinsi. Olor buccinator. Symphemia semipalmata inornata. Bonasa umbellus umbelloides. Pedioecetes phasianellus columbianus. Buteo borealis calurus. Buteo swainsoni. Falco columbarius richardsoni. Bubo virginianus pallescens. ? Dryobates villosus hyloscopus. Picoides americanus alascensis. Selasphorus rufus. Empidonax trailli. Empidonax hammondi. Otocoris alpestris leucoljema. Pica pica hudsonica. Calcarius pictus. Ammodramus sandwichensis alaudinus. Zonotrichia leucophrys gambeli. Spizella monticola ochracea. Spizella socialis arizonse. Seiurus noveboracensis notabilis. Cinclus mexicanus. Parus atricapillus septentrionalis. Myadestes townsendi. Sialia arctica. ' Reported only from the Yukon Delta. * Known only as migrant*. OCT., 1900. classifip:d lists of species. 55 AMERICAN I'AC'IFIC COAST Sl'ECIES FOUND IN THE YUKON U.V.SIN. Helodromas solitarius cinnamouieiis. Tachycineta thalassina. Zonotric'hia coronata. Dendroica townsendi. Wilsonia pusilla pileolata. Hvlocichla aonalasclikfc. ASIATIC .VNIJ PACIFIC SPECIES FOUND I.N THE YUKON BASIN. Limosa lapponica baueri.^ Charadrius dominicus fulvus.' Archibuteo lagopus. Scotiaptex cinerea lapponica. ' Pyrrhula cassini. Budytes flavus leucostriatus.' Phyllopseustes borealis.' MIGRATORY SPECIES NOT COMMON TO NORTHERN NORTH AMERICA FOUND DURIN.19 entered Lake Lcbar^^e on the evening- of Jul}^ ly, when a tioek of at least a hundi-fd Hew hig-h overhead from the direetion of the hike. Al)out 8 p. ni. and at 10 p. m. of the ,sanie evening, and on the next morning, we ,saAV what we took to T)e tht^. same floek. The birds were probably taking a morning and evening flight, such as E. S. Bryant has noticed in the case of the white-Avinged scoters breeding at Devils Lake, North Dakota; and I believe that with both species these flights are taken chiefly to exercise the wing muscles. We saw no females on any of the lakes, nor could we find them on the shore, though they were undoubtedly nesting in the vicinitv- We observed several on Thirty -Mile River July 18 and two near the Little Salmon July 20. Near Whale Island, at St. Michael, we saw a number September 8, and two scoters, probably young of this species, September 21. I think there were a few with the American scoters I saw at Unalaska October 5. 43. Chen hyperborea. Lesser Snow Goose. 1 saw five snow geese at the Aphoon mouth August 28, and a large flock at St. Michael September 11. 44. Anser albifrons gambeli. American White-fronted Goose. A single white-fronted goose was seen by Osgood among a number of other birds killed by natives about the Yukon Delta August 29. 45. Branta canadensis hutchinsi. Hutchins Goose. Although Maddren was informed that a goose with four young was seen near White Horse Rapids about July 11, and although the sergeant in charge of the police station of Lower Lebarge told us that thousands of geese and ducks passed there in the spring, and that he had counted twenty -four distinct species, and had killed both Hutchins and cackling geese, we did not see a goose of any species until we were in the neighborhood of Charlie Village, August 10. There we saw a flock of about twenty of the Branta canaderwis group, and Osgood shot two hutchmd and saw many more near Fort Yukon August 21. Brown geese, apparently chiefly this subspecies, were common on the Yukon flats and on the lower river, especially the Yukon Delta. A Hutchins goose was brought to the steamer Robert Kerr by an Eskimo August 26, and I found the bird common at the Aphoon mouth August 27-28. Prospectors on the Kerr told me that geese bred abundantly at the head waters of the Porcupine and the marshes at the source of Birch Creek. During September this species was common about St. Michael in small flocks, but very shy; Osgood took one September 23. {Philacte canagica. Emperor Goose. Dr. Romig told me they were couniion on the tundra along the Kuskokwim.] OCT., 1900] . BIRDS OF THE YUKON REGION. 65 \^