econ nie fee we pee oenemenr eee Toten ren ; BIN DING LisT Dre 14 ) AALS Digitized by the Internet Archive in 2009 with funding from Ontario Council of University Libraries http://www.archive.org/details/proceedingscalif06cali rm Fon i A PROCEEDINGS OF THE CALIFORNIA ACADEMY OF SCIENCES FOURTH SERIES VoL. VI 1916 7, SAN FRANCISCO PUBLISHED BY THE ACADEMY 1916 . ( PAG My, Cy AW, % sy A -, \ : 4. COMMITTEE ON PUBLICATION GEORGE C. EDWARDS, Chairman C. E. GrRuNsky BARTON WARREN EVERMANN, Editor CONTENTS OF VOLUME VI. Prates 1-17. PAGE Tt Sah el Ca cxes eee emce nae was esses cseasscscesenectnsshccusenscuseisensecasnsoreccveessheonnsnsesesnntocce i Gora Cera Se eee eae ae rests cco ant steceeemnnncesesonccedsstvacesedabaracesveseseSssonce iii Eocene of the Lower Cowlitz River Valley, Washington.................-..-.-- 1 By Charles E. Weaver. (Published May 6, 1916) The Post-Eocene Formations of Western Washington...............20-.-00-- 19 By Charles E. Weaver. (Published May 6, 1916) The Oligocene of Kitsap County, Washington...........--.-scccsssscseecssssesnseneeeee 41 By Charles E. Weaver. (Published May 6, 1916) The Pacific Coast Races of the Bewick Wren..............--sss:ssssssssssscsssesneene 53 By Harry S. Swarth. (Published May 8, 1916) Monograph of the North American Species of Orthotylus (Hemip- MET!) pcos dacesstasahawes esaas cad Sue se hes 8 coca acess aes besa cecnestevnsa code tvaastactcneactbtcanececennssnstsd 87 By Edward P. Van Duzee. (Published May 8, 1916) A, Catalogueand Host List:of the Amopl uta essence concoct asessccecnetcecnteeces 129 By G. F. Ferris. (Published May 12, 1916) Four Species of Salamanders new to the State of California, with a Description of Plethodon elongatus, a New Species, and Notes ontother: Sallammean ders izccesa 5 ssc ses ae saa ata cance tance eetcaseeantanee 215 By John Van Denburgh. (Published May 12, 1916) Report of the President of the Academy for the Year 1916..............-...... 223 By C. E. Grunsky. (Published June 23, 1917) Report of the Director of the Museum for the Year 1916... 229 By Barton Warren Evermann. (Published June 23, 1917) EET cen aa as cages rao SSeS ca 295 July 6, 1918 — 7 PROCEEDINGS OF THE CALIFORNIA ACADEMY OF SCIENCES FourTH SERIES VoL. VIE Nos I pp, 1=17, pli al. May 6, 1916 I EOCENE OF LOWER COWLITZ RIVER VALLEY, WASHINGTON BY CHARLES E. WEAVER Assistant Professor of Geology, University of Washington, Seattle INTRODUCTION The purpose of this paper is to place upon record the re- sults of geologic and faunal studies made by the writer during the past three years in portions of the lower Cowlitz River Val- ley. The area under investigation is of special interest because of the large number of exposures of Eocene strata and the ex- ceptidnally well preserved faunas contained within them. Surface outcrops of Tertiary formations in western Wash- ington are largely obscured because of the heavy overburden of Pleistocene deposits. In King and Pierce counties much de- tailed work has been done so that the lithology and structure of the Eocene rocks is fairly well known.’ The strata in this region are, however, almost entirely of estuarine origin, ren- dering it impossible to make satisfactory correlations with the Eocene of other parts of the Pacific Coast. Isolated outliers of Eocene rocks occur in many localities such as Crescent Bay 1Willis, Bailey, and Smith, Geo. O., Tacoma Folio, U. S. Geol. Surv. 1899, May 6, 1916 2 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. along the Strait of Juan de Fuca, the low hills about Tenino and Centralia in Chehalis County and the exposures on Coal Creek north of Columbia River in Cowlitz County. At these localities only fragmentary sections of the Eocene column of Washington can be studied. The region under discussion in this paper contains the most complete fossiliferous marine sec- tion occurring within the western portion of the state. REVIEW OF LITERATURE One of the earliest important scientific references to the geologic conditions in this region is to be found in the report by Dr. Ralph Arnold’ on “The Tertiary and Quaternary Pec- tens of California.” He described Pecten landesi from this area. The following quotation is well worth noting: “P. landesi is found quite abundantly in a dark greenish sandstone bed that outcrops about 100 yards west of the junction of Still- water and Olequah creeks (U.S. Nat. Mus. locality 4019) one- fourth mile southwest of Little Falls, Lewis County, Wash. It is also found in a similar matrix in the bed of Olequah Creek (U. S. Nat. Mus. locality 4024), one mile north of the first locality. It is associated in this formation with a characteristic Eocene fauna, among which are the following species: V eneri- cardia planicosta Lamarck, Thracia dilleri Dall, Crassatellites sp., Meretrix sp., Ostrea sp., Pteria (cf.) limula Conrad, Car- dium 2 sp., Barbatia sp., Glycimeris sp., Corbula sp., Callista sp., Turritella (cf.) uvasana Conrad, Fusus 4 sp., Ocinebra sp., Ranella sp., Calyptrophorus sp., Lunatia sp., Turbinella (?) sp., Murex 2 sp., Conus sp., Cassis sp., Tritonium sp., Dentalium (cf.) cooperi Gabb, and Nautilus sp. This horizon is probably upper Eocene, possibly above the Tejon.”” Dr. Ar- nold’s suggestion that this horizon is very high in the Eocene seems to be well in accord with more recent studies. The Geology and Paleontology of this area is discussed in a paper by the writer® published in 1912. A large fauna was noted as occurring along the banks of Cowlitz River about one *Arnold, Ralph, The Tertiary and Quaternary Pectens of California. Professional Paper 47, U. S. Geol. Surv., p. 52, 1906. 3Weaver, C. E., “A Preliminary Report on the Tertiary Palaeontology of Western Washington,”’ Bull. 15, Wash. Geol. Surv., pp. 12-15, 1912. Vor. VI] WEAVER—EOCENE OF LOWER COWLITZ VALLEY 3 and one-half miles east of the town of Vader in Lewis County. Many new species of mollusks were described and the fauna as a whole was referred to the Cowlitz formation which was re- garded as of Eocene age and possibly older than the Tejon. A suggestion was, however, made that future studies might show that it was identical with the Tejon. A further discussion of this region is to be found in a report by Arnold and Hannibal* on “The Marine Tertiary Strati- graphy of the North Pacific Coast of America.” In this paper the Tejon is divided into three formations: the Che- halis, Olequah and Arago formations. They are referred to as the Tejon Series. The Chehalis and Olequah formations are present in the region involved in this report. The Arago is absent. On the basis of fossil floras colder climatic condi- tions obtained during the deposition of the Chehalis formation than during that of the Olequah. During the last year an important paper appeared by Dr. Roy E. Dickerson’ entitled the “Fauna of the Type Tejon: Its Relation to the Cowlitz Phase of the Tejon Group of Washing- ton.” Collections were made and studied from certain locali- ties along the Cowlitz River and a number of new species were described. A total of 95 species are listed from Washington and 55 of these are found within the Tejon of California. The paper gives the results of studies at the type Tejon locality in southern California and makes correlations with the Cowlitz phase of the Tejon in Washington. He states ‘“The Cowlitz phase of the Tejon of Washington appears to represent the same faunal facies as the fauna of the type Tejon, i. e., the Rimella simplex zone is present in both localities.” GEOGRAPHY OF AREA UNDER INVESTIGATION ‘The region involved in this study is situated in southern Lewis County and extends from the town of Winlock southerly for a distance of fifteen miles to the town of Castle Rock. From east to west the area averages five miles in width. Just east *Arnold, Ralph, and Hannibal, Harold, The Marine Tertiary Stratigraphy of the North Pacific Coast of America, Proc. Am. Phil. Soc., vol. 52, pp. 566-571, 1913. 5Dickerson, R. E., ‘‘Fauna of the Type Tejon: Its Relation to the Cowlitz Phase of ereh eeicn Group of Washington.” Cal. Acad. Sci. Proc., 4th series, vol. 5, pp. 51, 3 4 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4tH Ser. of the town of Vader (formerly known as Little Falls and So- penah) the Cowlitz River swings from its east-west course and assumes a due north-south direction. One mile south of Vader, Stillwater Creek enters Cowlitz River and about one- fourth mile south of the town, Olequah Creek joins Stillwater Creek. From this point Olequah Creek extends almost due north to Winlock. The Northern Pacific Railway between Portland and Seattle follows the valley of this creek. The drainage of the entire area is southerly to the Colum- bia and the hills on either side rise gradually into a rolling tim- bered country. Eocene strata away from the banks of the creeks are not exposed but are covered with gravels and sands formerly deposited by Cowlitz River. STRATIGRAPHY In the examination of this region a transit survey was made of Stillwater and Olequah creeks and the position of all fossil localities as well as observations taken upon strikes and dips definitely located. These data have been plotted upon the map accompanying this report. Between the towns of Castle Rock and Olequah only four exposures of Eocene strata are known to occur. They consist of dark gray, sandy shales with intercallated basaltic flows. Two miles north of Castle Rock and 2,000 feet south of the Northern Pacific Railway bridge over Toutle River, there is an exposure in the railway cut composed of bedded tuffaceous materials together with sedimentary deposits of worked over basalt. These beds have a strike of N. 75° E. and a dip of 5° N. W. They are overlaid with Pleistocene deposits com- posed of sand and gravel intermixed with angular fragments of basalt, which appear to have been derived by rapid erosion from nearby bluffs of Eocene basalt. From this point northerly for a distance of two miles the only exposures along the railway consist of Pleistocene grav- els and sands. One and two-thirds miles north of the Toutle River bridge Eocene rock outcrops occur for a distance of 450 feet. The bluffs at this point are about 60 feet high and con- Vor. VI] WEAVER—EOCENE OF LOWER COWLITZ VALLEY 5 sist of thinly bedded, fine-grained, dark brown shale contain- ing a few narrow bands of sandstone. The total thickness of the sediments at this point is about 75 feet. They are overlaid with 35 feet of black basalt showing well defined columnar jointing. Both the sedimentaries and lavas have a strike of N. 80° E. and a dip of 10° to the N. W. About one-half mile south of the railway bridge across Cow- litz River there is a third exposure of Eocene basalt but no sedimentary rocks. The lower portion of the bluff is made up of agglomeratic materials consisting of a heterogeneous mass of angular fragments of badly weathered, dense and vesicular basalt having a thickness of 20 feet. Above this is a flow of fine grained, dense, black basalt exhibiting a tendency to col- umnar structure. The approximate strike of these flows is nearly east and west with a low dip to the north. The eroded surface of this outcrop is overlaid with Pleistocene sands and gravels. One-half mile north of the previously mentioned outcrop, and along the south bank of Cowlitz River at the railway bridge, basalts and sedimentary rocks again appear. At the south end of the bridge and along the river there is a quarry composed of basalt exhibiting pronounced columnar structure. Lying conformably below the basalts are dark shales and brown sandstones, which in places contain narrow carbonaceous bands. They are about 60 feet in thickness with a strike of N. 35° W. and a dip of 10° to the N. E. From this point northward to the town of Olequah no recognizable exposures of the Eocene occur. At one of the above mentioned localities a single speci- men of Turritella uvasana Conrad was collected, but aside from this, the only fossils occurring are a few plant fragments and wood. From observations taken upon strike and dip there appears to be a continuous low dipping series of sedimentary beds with intercallated basaltic flows extending from Castle Rock to Olequah. However, it is possible that there may be folding and faulting in the intervening covered areas. If the strata are continuously dipping northward they possess a thick- ness of at least 6000 feet. From Olequah northward to Win- lock, where the strata are better exposed, a stratigraphic sec- 6 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. tion can be made. The sediments in the area between Castle Rock and Olequah are stratigraphically below those outcrop- ping between Olequah and Winlock. Section between Olequah and Winlock:—Strata of Eocene age outcrop in the banks of Olequah and Stillwater creeks and also along the railway track at many places between Olequah and Winlock. They consist predominately of massive, sandy, clay shales together with grayish brown sandstones contain- ing carbonaceous seams. These materials are of marine, brack- ish and fresh water origin. With the exception of the basal portion of this section, basaltic flows are absent. The basal part involves certain sandstones and basalts outcropping at the town of Olequah. The upper portion of the section is two miles south of the town of Winlock. The actual contact of the upper limit of the Tejon and the overlying Oligocene has not been definitely determined. Four hundred feet south of the last Oligocene outcrop in the banks of Olequah Creek are Eocene shales containing a marine Tejon fauna. It is impos- sible to sav whether the two formations are conformable or not. The strata have approximately the same strike, but the dip of the Oligocene is only 2° to the northeast, while that of the Tejon is 27° in the same direction. It is possible that the two formations are conformable but that in the interval of 400 feet between them the dip flattens out. The lower portion of this section as exposed along Still- water Creek to the southwest of Vader and as far south as Ole- quah is of marine origin. Stratigraphically above, these strata grade into those of brackish water origin and finally into those containing a freshwater fauna. Still higher up in the section they pass back to a brackish water condition and finally to marine. The entire upper portion of the section is a marine deposit. The total thickness of the Eocene section, as meas- ured from Olequah to Winlock, is approximately 4970 feet. The following stratigraphic section shows approximately the variations in the lithologic character of the sediments from the base to the top, including a part of the overlying Oligocene. Vor. VI] WEAVER—EOCENE OF LOWER COWLITZ VALLEY Tor oF SECTION Banded sandstone and shale as exposed at the town of Winlock and in the banks of Olequah Creek to the west and northwest of town. The fauna occurring at Locality No. 229 is charac- fEOMISM EPO RREIS TZ ODE User cto citi siefeceite erafsielejats slaisievs.stelers/s sities sie Massive clay shale grading in places into sandy shale as exposed along the banks of Olequah Creek south of Winlock and also in the bank of Cowlitz River in Section 5, Township 11 North, Range 2 West, at fossil Locality No. 239 (locally known as the Graeco Ranch). This is the base of the Oligocene in this TES IOM MIA yer eee rice e eco stad ake oesee ter eealsragedotece lakes cot avereuskels Top of Eocene section. Chiefly sandy shale grading into massive clay shale of a dark brownish gray color. 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VI] WEAVER—EOCENE OF LOWER COWLITZ VALLEY 15 The above listed faunas are typically Tejon. The Cowlitz phase of the Tejon as represented at Locality No. 1 on the Cowlitz River one and one-half miles east of Vader was in a previous paper by the writer regarded as older than the Tejon, and more closely related to it than to the Martinez of California. Since the publication of that report more extensive collections have been made, as well as more detailed stratigraphic studies. The faunal evidence now points directly to its Tejon age. Dr. Dickerson® believes it is to be correlated with the type Tejon of Grapevine Canyon in southern California. He considers it to represent the middle division of the Tejon or Rimella sim- plex zone. Arnold and Hannibal‘ in their report on “The Marine Ter- tiary Stratigraphy of the North Pacific Coast of America” consider two divisions of the Tejon to be present in the Ole- quah Creek region. The lower division or Chehalis formation is described as occurring at “the bluffs along Cowlitz River below the mouth of Drew Creek, one and one-half miles east of Olequah.” It is apparent that they must have meant Vader rather than Olequah, as Cowlitz River is less than one-half mile east of Olequah, and the only rock exposures in that region are deposits of Pleistocene gravels and sands. Their faunal local- ity, No. 113, is probably the same as Locality No. 1, la, 232 and 233 of this report and California Academy of Sciences Localities Nos. 182 and 183, as referred to in Dr. Dickerson’s report. Detailed stratigraphic measurements made with a transit show that the strata occurring at the above mentioned localities are stratigraphically higher than the strata exposed along Olequah Creek from a point two miles north of Vader southward to Olequah. The type locality of the Olequah for- mation as described by Arnold and Hannibal “extends from the Erwing ranch a little over two miles above Little Falls south- ward down Olequah Creek to Olequah, a distance of about five and one-half miles.” In this area, where both the Chehalis and Olequah forma- tions are described as occurring by Arnold and Hannibal, strat- igraphic evidence shows their lower division or Chehalis for- ®Dickerson, Dr. R. E., ‘‘Fauna of the Type Tejon: Its Relation to the Cowlitz Phase of the Tejon Group of Washington.’”’ Cal. Acad. Sci. Proc., 4th series, vol. 5, pp. 39-51. fOp:> Git: 16 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH Ser. mation to rest upon their upper or Olequah formation. Their evidence for two divisions here seems to have been based in part upon the evidence of fossil floras. An examination of the faunas obtained at various intervals from the base of sec- tion at Olequah to near the top at Winlock shows very little difference in their composition. It is true that near the middle of the section brackish and fresh water beds appear, but the marine faunas below and above are very similar. A compari- son of the faunas occurring in the Eocene strata of the Cowlitz River area with those which have been listed and described from the type Tejon in southern California leads the writer to the same conclusions as have been stated by Dr. Dickerson, namely, that the Tejon of the Cowlitz River area is the equiva- lent of the middle zone in California as represented in the Mount Diablo region. CONDITIONS OF DEPOSITION The Eocene of western Washington is widely distributed. It extends well up into the western portions of the Cascade Mountains and may even possibly connect beneath a thick cov- ering of Miocene lavas with the Eocene deposits on the east- ern slopes of the mountains. The Eocene deposits involved within the western slopes of the Cascades are almost entirely of brackish or fresh water origin. No marine strata are known to be interbedded. In the Puget Sound Basin, brackish water deposits predominate, but in southwestern Washington great thicknesses of marine deposits are interbedded. During the upper Eocene the larger part of southwestern Washington and a portion of the Puget Sound Basin appear to have been an embayment of the ocean. The present site of the western slopes of the Cascade Mountains seems to have been in part occupied by large estuaries. During Tejon time diastrophic movements were differentially acting upon the entire western portion of the state, causing fluctuations in the depth of water in the embayments and estuaries and a shifting of the shorelines. These oscillations are recorded in the interbedded character of the marine and brackish water sediments. The eastern shore- line of the southwestern Washington embayment appears to have existed at times along the present site of the Northern Vor. VI] WEAVER—EOCENE OF LOWER COWLITZ VALLEY 17 Pacific Railway line from Centralia ta Portland. An interpre- tation of the stratigraphic section shows that this shore line was alternately shifting east and west as the sea floor was be- ing differentially elevated and depressed. The effect of those diastrophic movements as recorded within the area involved in this paper may be seen in the passage from marine to brackish and fresh water and thence back again to marine. The marine faunas as listed above indicate tropical climatic conditions and an environment ranging from shallow water to moderately deep water. CONCLUSIONS Within the area studied between Winlock and Olequah there are about 4000 feet of shales and shaly sandstones of upper Eocene age. Beneath these, between Olequah and Castle Rock, there are possibly 6000 feet of unmeasured upper Eocene sandstones and shales, together with numerous intercallated layers of basaltic lavas. Overlying the Eocene in the vicinity of Winlock and at the Graeco ranch on Cowlitz River are marine deposits of Oligocene age. A section of the Eocene measured between Olequah and Winlock consists of a lower division of marine beds at least 400 feet in thickness. This is overlaid by 550 feet of brackish water strata and that in turn with 300 feet of freshwater beds. Above the freshwater beds are 520 feet of brackish water strata. Above these are marine beds having a thickness of 2410 feet. These strata are all fos- siliferous and appear to be most closely related to the middle Tejon as described in the Mount Diablo region of central California. The basement upon which the Tejon in this area rests, as in the case of most of western Washington, is unknown. The fauna of the upper portion of the Cowlitz section bears a close relation to the overlying Molopophorus lincolnensis zone of the lower Oligocene as represented to the north in the vicinity of Lincoln Creek, in Thurston County. PROCEEDINGS OF THE CALIFORNIA ACADEMY OF SCIENCES FourtTH SERIES Vot. VI, No. 2, pp. 19-40. May 6, 1916 II THE POST-EOCENE FORMATIONS OF WESTERN WASHINGTON BY CuHartes E. WEAVER Assistant Professor of Geology, University of Washington, Seattle INTRODUCTION Marine deposits of post-Tejon age form a considerable part of the formations exposed at the surface in western Wash- ington. They have been folded and eroded, and, in some areas, are deeply buried beneath sand and gravel of glacial and flu- viatile origin. As a result, outcrops are usually found in the form of low cliffs along the banks of rivers and creeks or along the sea cliffs of the Sound or ocean. Certain portions of these Oligocene-Miocene formations yield fairly abundant marine invertebrate faunas. Upon a faunal basis five separate divi- sions of the post-Tejon portion of the Tertiary can be recog- nized. Marine deposits of Pliocene age with the exception of a very sinall area on the western side of the Olympic Peninsula are unknown within the state. The uppermost division or upper Miocene is separated from the lower four divisions by a well-marked unconformity. The pre-Pleistocene formations of the southwestern portion of the state are somewhat ob- May 6, 1916 20 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. scured by clays, sands and gravels of fiuviatile origin. In many areas the Tertiary rocks themselves have been so deeply weath- ered that very little information can be obtained concerning their lithologie character and structure. All parts of western Washington are clothed with a dense growth of forest and underbrush, which conceals many exposures of Tertiary rocks which are not covered with Pleistocene sands and gravels. LITERATURE Numerous references to the occurrence of Tertiary strata may be found in papers dealing with the geology of western Washington. The majority of these papers invoive investiga- tions of economic products such as coal and contribute little to the purely scientific phases of Tertiary geology. Only the more important literature is here reviewed. James D. Dana referred to Tertiary strata in the report on the geology of the United States Exploring Expedition under Wilkes? as occurring to the north of Columbia River and along the shores of Puget Sound and the Strait of Juan de Fuca. Collections were made from the south side of Columbia River at the town of Astoria. This fauna was iden- tified by Conrad, who regarded it as Miocene. Marine Neocene deposits are mentioned by Dr. Bailey Willis as occurring near Seattle immediately north of the northern limits of the Tacoma quadrangle.” ‘These deposits are not described. The first detailed description of the occurrence of Oligo- cene-Miocene strata within the state is to be found in a report by Dr. Ralph Arnold* on a “Geological Reconnaissance of the Coast of the Olympic Peninsula, Washington.” Oligocene- Miocene deposits are described as occurring along the north- ern border of the Olympic Peninsula. Pliocene deposits are mentioned as being present on the west coast of the peninsula near the mouth of Queniult River. The Miocene deposits are composed of conglomerates, sandstones and shales which at- 1Dana, J. D., in U. S. Exploring Expedition, under command of Charles Wilkes, U. S. _N., Philadelphia, vol. 10, 1838-1842. Willis, Bailey, Tacoma Folio, No. 54, U. S. Geological Survey, 1896. 3Arnold, Ralph, Bulletin Geological Society of America, vol. 17, pp. 451-468, September, 1906. Vor. VI] WEAVER—POST-EOCENE OF WESTERN WASHINGTON 21 tain a thickness of 15,000 feet and have been folded into an- ticlines and synclines. Upon the basis of faunal evidence he states that the fossils of the formation indicate that the basal portion of the series is Oligocene in age, while the upper part is certainly Miocene. Since the separation of the two members will necessarily have to be made on paleontological grounds and will require a more detailed study of the material in hand than time has yet permitted, the term “Oligocene-Miocene series” will be used temporarily to designate the age of the beds. Arnold applied the term to this formation and recog- nized five faunal zones within it. Further mention is made concerning the occurrence of Oli- gocene and Miocene fossils at Restoration and Beans points, just west of Seattle, by Dr. Ralph Arnold* and Dr. W. H. Dall.® A paper published in 1908 by A. B. Reagan® and entitled “Some Notes on the Olympic Peninsula,” describes the Ter- tiary rocks occurring in certain localities along the north and west sides of the Olympic Peninsula. Several new species of mollusks are described and figured. In 1911, the writer, in a preliminary paper on the Ter- tiary of western Washington, described in a general way the distribution of the Miocene formations within the state. The following subdivisions were made: Lincoln formation of Oli- gocene age; Blakeley, Wahkiakum and Chehalis formations of Lower Miocene age, and the Montesano of Upper Miocene. Since the appearance of that paper, more detailed field work has been done by the writer. As a result, a large portion of the Chehalis formation is now included within the Wahkia- kum and Montesano formations, and another division inter- mediate between the Lincoln and Blakeley is introduced, namely, the Porter.’ The area along the western border of the Olympics represented upon the map accompanying the report as undifferentiated Lower Miocene, is of probable Jurassic age and is now referred to as the Hoh formation. ‘Arnold, Ralph, Professional Paper No. 47, U. S. G. S., “The Tertiary and Quat- ernary Pectens of California,’ Washington, 1905, ‘Dall, W. H., Professional Paper No. 59, U. S. G. S., “The Miocene of Astoria and Coos Bay, Oregon,’’ Washington, 1906. "Reagan, A. B., “Some Notes on the Olympic Peninsula,” Kansas Acad. Sci. Geological Papers, pp. 131-238, 1908. "Weaver, C. E., ‘‘A Preliminary Report on the Tertiary Palaeontology of Western Washington,” Bulletin No. 13, Washington Geological Survey, 1911. 22 CALIFORNIA ACADEMY OF SCIENCES [Proc. 41H Ser. The most recent paper on the Tertiary of western Wash- ington is by Arnold and Hannibal* on the Marine Stratigraphy of the North Pacific Coast of America, published in 1913. A four-fold division of the Oligocene is recognized. The oldest is represented by the Sooke formation of southwestern Van- couver Island. This is followed by the San Lorenzo, Seattle and Twin River formations. Above this is the Monterey, which is thought to be in part Oligocene and possibly in part lower Miocene. The upper Miocene strata, which are de- scribed as occurring on the south and west portions of the Olympic Peninsula, are believed to be the equivalent of the Empire formation of Coos Bay, Oregon. GEOGRAPHIC DISTRIBUTION The Oligocene and Miocene deposits of western Wash- ington exist in three separate areas. The largest and most representative area occupies the northern half of the Puget Sound basin and the north border of the Olympic Peninsula. A second area embraces the western portion of the Chehalis and Willapa river valleys in the southwestern part of the state. A third area constitutes a belt ranging from five to fifteen miles in width and trending east and west along the north shore of Columbia River. Within the Puget Sound basin and along the northern portion of the Olympic Penin- sula, Miocene sediments are for the most part more or less heavily covered with deposits of glacial drift. They appear in the form of low sea cliffs along the shores of the entrance to the Bremerton Navy Yard, in the streets in the southern portions of the city of Seattle, and along the northern slopes of the Newcastle Hills. Along the north border of the Olym- pic Peninsula rock exposures appear almost continuously from Cape Flattery eastward to Port Crescent. Similar deposits occur within and along the shores of portions of the Quimper Peninsula south of Port Townsend. The Puget Sound Basin Oligocene and Miocene area is separated from that of south- western Washington by basalts and sedimentary rocks of Eo- ‘cene age. From the southern margin of the Olympic Moun- 8Arnold, Ralph, and Hannibal, Harold, “Marine Stratigraphy of the North Pacific Coast of America,” Proc. Amer. Philos. Soc., vol. 53, No. 212, November-December, 1913, Vor. VI] WEAVER—POST-EOCENE OF WESTERN WASHINGTON 23 tains in Chehalis County, Oligocene and Miocene formations extend southerly to the middle of Pacific County. Outlying residuals occur in western Thurston and Lewis counties. Sim- ilar deposits of post-Tejon age are present in Wahkiakum County and in the southwestern part of Pacific County. They have been cut by the Columbia River and their southern exten- sion forms a part of the well-known series of outcrops occurring at Astoria, Oregon. No marine deposits of Oligocene or Mio- cene age are known to occur within the Cascade Mountains or within the great basin area of eastern Washington. In these regions deposits of corresponding age are of igneous or freshwater origin. SEDIMENTATION From the standpoint of stratigraphy the post-Tejon sedi- ments occurring in the western part of the state are divided into two broad groups, separated by a well-marked uncon- formity. The older division includes deposits of Oligocene and lower Miocene age, while the younger involves sediments of upper Miocene and possibly lower Pliocene ages. During the Oligocene, embayments of the ocean were widely ex- tended over western Washington with the exception of the central and western portions of the Olympic Peninsula. Dur- ing the lower Miocene their extent became much smaller and by the opening of the upper Miocene they were almost en- tirely withdrawn. During the upper Miocene two small, shal- low basins of deposition were formed. One of these existed in the basin of Grays Harbor and the other near the junction of Bogachiel and Solduc rivers in southwestern Clallam County. During the Eocene epoch, southwestern Washington was occupied by an embayment of the ocean which seems to have extended as far north as the middle portion of the present Puget Sound basin. ‘This fact is indicated by the occurrence of narrow bands of marine strata interbedded with those of purely brackish water origin. On the eastern shores of this embayment were situated extensive estuaries in which over 10,000 feet of brackish water sediments were deposited and which now form extensive outcrops in King, Pierce and Lewis counties. Igneous activity was characteristic of the larger 24 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. portion of the Tejon epoch but had almost entirely ceased by the opening of the Oligocene epoch. Near the close of the Eocene or at the opening of the Oligocene minor crustal move- ments brought about an encroachment of the marine waters into the Puget Sound basin and also into the present site of the Strait of Juan de Fuca. In southwestern Washington the oldest deposits of post- Eocene age occur west of the city of Centralia in the valley of Chehalis River. They consist of indistinctly bedded, sandy, gray shales containing a marine invertebrate fauna which will be referred to in this report as the Molopophorus lincolnensis zone. The strata containing the fauna may be referred to as the Lincoln horizon. At the present time the strata at this locality are approximately 1,000 feet in thickness. Away from stream, railway or wagon road cuts, rock exposures are largely obscured by a veneer of sands, clays and gravels, rendering it difficult to determine the exact areal limits of these beds. Fossiliferous strata outcropping in the banks of Olequah Creek near the town of Winlock and in the banks of Cowlitz River, six miles east of Vader, at the Graeco Ranch, may have been contemporaneously deposited with those at Lincoln Creek. The same may be true of the shales on Porter Creek north of the town of Porter in Chehalis County. They are unknown to the southwest in Pacific and Wahkiakum counties, as well as along the Strait of Juan de [*uca. Toward the close of deposition of the Lincoln sediments the Oligocene seas expanded and occupied portions of the Strait of Juan de Fuca and the Puget Sound basin, as well as most of southwestern Washington. By the close of the Oli- gocene epoch these deposits had attained a maximum aggre- gate thickness of 15,000 feet. They consist predominately of shales and sandy shales within which local beds of conglom- erate and sandstone are occasionally interbedded. The thick- est and most complete section of the Oligocene is to be found in northern Clallam County along the northern border of the Olympic Peninsula. The section nieasured between Cape Flat- tery and Clallam Bay possesses a thickness of 13,300 feet. The basal beds are situated at the west end of Wyatch Slough and the upper about half way between Neah Bay and Clallam Bay. Vor. 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D1ADIIa9UDD “*pelu0g oignaanag vynpidadD at eth Ned umnoiyiond wnyoury “““peiu0d sdaauiad vjnptdasd TES cas Ned Pindosnys djjaqunjoy “suBseay $n71jup813 smiuoposkayD ee See leq tp4tpq snumoposkayD “oye s1ppradus snmoposkay) “(uedeay) tpjaifxou sntuoposkayD DDO (qqey)) DItajuarxa vapvalda}DD “"TOABOAA S1SUaUDI]DII SNUMoposkAyD po opsitt? rae (qqex)) DIDUAONS DaDAIGK]DD JOABINM SISUBUOJIUIYSDM DaDAdKOD daa ae PlOUly tMojuDJs DUO}S011]10D BAS Stead (qqexy) vsojyf vanadajoy JOABIM SISUINOJIZULYSDM DLADIJIIUDD peewee uBBeay 1794490309 wniu199Ng “"IOABAM SISUaUjOIUID WAY “IOABINM 1Y4D)9 SnIutdsKyoDAgT eats leq Pup1qgns vuoityjog ‘suBseay Hary2pd0q puojyjog “TTB esuasoor mnwu1IngGosay “Wed tunuwups unursonqgosay lates ovenoveis aloveis eelecsstnerseororetsiaere ds ‘u ‘nuaynduy nd ae eek leq sisuauosaso vurynduy vdaodOuaLsvo (U0) )—NOTONTHSVA\ NYALISAA\ NOI ATAV], IWNAVY Nola] -1s0g 39 WEAVER—POST-EOCENE OF WESTERN WASHINGTON Vor. VI] Tewece sees eepeerees ceeewepeeee ee). uUeseay yjDYSADU DIJaUDYy NOoURTU AOS ds ‘u ‘nyjauny “*** uBBeay SisuauDy1Dj9 D1iuDstg “sss 11eq mnjp2nsinbap wnyoyg "*"TOABIMA SISUIUIOIUN Sam1UK{OT “co ueseey ipidkjo san1ucjog BUY ORAS S 8 q Dsnnp9 sar1uKjog SAPO “*peluod vaxps sarucjog BORED “*"T]eq 40un1ps saotukjog Sat ons * (PINON) s4sImaz sartucjog TUCO ““peluog Dupospag 0190110 : " peIUOd StsuaUosa410 DIDNT “uosiapuy 1pjoudD DssDNy sensed sosiereiee JBACIM IMOSAIPUD DSSDN Syelecereneie pestuog vjDAnpur Duo1a1G01py ESSE Ted 19903 sndoydogojojy svatoelatessiniaxea acl TIWEd suqp2jns snsamorz “"**IQARIM DUDIUOITUIYSDA Snsnfima TT “"Teq wnjpjNI19G409 aAr01pam uinaursksy COD isp JOAeaMA SISuaDIAIhS UinaUut4cs) sielgisie “"*IQABIM SISHIULDIIDII SnI2q reese “*peluod sisuauosado snot : “IOABIM SISUaYI0ONKM SnItY : “IOABAM StSuastDYyayI SnIty aimee i (ploury) txo020y DyjMq siekerekee ofc Tl’ siSuasoor snuisny “*"*(pelu0d) snjuajndso? snuisng sletereisiansis (pjoury) sisuapsofunjs snuisn gy pre “IQABIM SISUIOUDSAIUOW SNUISNY Daisies Gl aereis\siee T9AVIM MMOSAIYIIp DIyIXT tei ote “‘uedeay Dupiuojsurysom Duany PELE ERORI.O ISOS uUBsedy 14JMUus DUNT Sidebar aan es (peiu0g) mnsodjag wnyopny op DABIM SISUIUOITULYSDAL WnIUOItdT is magnecen pe phere a Wed wMndafiana wnituondy ec] 8 3 > 8 c eS rs] z Q a9 q ix ag a ° ¢ 7353 Bo B lee] = leeelyee| & | we | 2 [eee] F [eislpeelyge| ees | yds ie) Le] 72 ef S eS S1osa ga. ) & ao oa Bao z EMege) g 5p PeaSiIPER| Bar| Sa0 Biehl oe eo 8 Bd Bo | 2 jags| 2 ose ote age PEE ° RE g 3 2. : » ° 3 5 sa B 2. a g (JU0))—NOLONIHSV\\ NUALSH\\ AOA ATAV], IWNAVY NoOfay-1s0og [Proc. 4TH Ser. CALIFORNIA ACADEMY OF SCIENCES 40 Anaad) oosce ocue concn inporee) nator darore Mentor! bitetuncl aesorml loon meniaed x x Kforce tenet ee aya frusuepsoy VOZOLOUd ee ee ee ee x x (a: teratas Pe(aia\eib eras viejnssTe\eietbiniehi*le. ccs SUT BOOS MB ATA OUST VaOVISNAO bY Sau RO Ce LEC a aN Wed Puntsojsp siacyjnua yy [0g en en ee leq Sypjuspr220 pipoyoAgadaT oie asaya flava; e,si| Ta ervia.eillevacaryie(eiflajavelniase!fl6:ctaie/e eff s,ainye-o%0! le(qiefa o1ell o(acsiarepe,hiciayacarate flasbjeye/e. ail slatat steal inceesetays K frcccetfeseeese sess saaawayy Sisuagiayno pynyoaqaua T VdGOdOIHOVad Vemren(e [niaeseg KM fecreetfeceeeeferseeafersee lessee feeeeefereee | gg feceeee[ereees[ereeesPereeePesteeeseeeeeeeeseesspuomay s1qqn8 yams VIVNUAGONIHO GeBdttol fenton banoun [ec (acnetial lvrentcd x ae ee) ed a x x KM frseesesseess es ppmm0g pypisnsup panty Vda0dO1VHdd) “UIRLLa Yl 1qMOIMaUu DIIAI1A44N T, "*IOABDM S1SUIKI]}IYDIQ 1I]911AAN T, esriaeses 2-1 sgeasseherdnibsencsnssac/ sie IOABIM StSUAdITAOG DII9I12AAN T, "*PpRIUOD SISUaNOTIAO 11]9]1AANT, ‘Wed vuninojsusysom Dyn2194N T, JBABIM, SISUIYIOOUKM SIAN [ ee adae oe qqer) Dsdaddad StAAn Ty, eines ciate espns he ce JOuLy Sisuaousadf SIAN T, Wed mous sidan yp scajerede Wed 209 staan y Il®q Stsuasoor stan 7 Syeda tol eliens epee pes Pploury sisuaurosayra sipy T, PSD ee aed (petuoDy) uinsojngors unury ee cohuseuenene thas Cis JOABAM SISUaUJOIUN DAnpIsdady Be ed eile otk scale Wed siskauosaso DAnpisgaay okelefetehereieeinunateleieie TaAran Sisuaujooury vjynoans: IneAraads Se arse an esee els Le led Stsuauosaso sapunydoag | re) > r] g 4 a lez DY 198 3 > 3s 8 ¢ Su] Be iS 28 to 5 > 2 3 < Bee) & [Eeplsee| & | oe | 2 (BBs! 2 leas lam] wer] ogg | 98s g BS YS |8egibag| ¥. om 9 IBSo)] & lBRa Sas |SEE| Sas] BRS 2 ae i) a3 ofB 5 Bry rt os is] oo O20 | ORD one oss 0 z -B 5 o AS & a5 o pe | a BO es es g 82, B |B | | 8d 8 5 ; Ss) (‘JU0D)—NOLONIHSVA\ NUALSTA\ NOX ATAVE, NAVY Nola] -1s0g PROCEEDINGS OF THE CALIFORNIA ACADEMY OF SCIENCES FourtTH SERIES Vou. VI, No. 3, pp. 41-52. May 6, 1916 III THE OLIGOCENE OF KITSAP COUNTY. WASHINGTON BY Cuar_tes E, WEAVER Assistant Professor of Geology, University of Washington, Seattle INTRODUCTION The purpose of this paper is to place upon record the re- sults obtained from geologic and paleontologic studies made in Kitsap County, Washington, along the north and south shores of the entrance to the Bremerton Navy Yard. Because of the isolated occurrence of pre-glacial outcrops, it seems desirable to select small areas of importance and to investi- gate the geology of them in as much detail as possible. The area involved in this study is located six miles west of Seattle and is of special importance because of the occurrence there of the most complete and representative section of the Oligo- cene within the Puget Sound basin. With the exception of the exposures along the south side of the Strait of Juan de Fuca, it is the most complete within the state. The surface rocks in the larger portion of the Puget Sound basin are composed of deposits of glacial drift. In a number of small and isolated areas the older pre-glacial bedrock for- mations project up through the drift. Such exposures are usually found in the form of low sea cliffs or in the canyons of certain streams. The region under investigation is one of such areas. May 6, 1916 42 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. PREVIOUS INVESTIGATIONS At various times during the last 10 years reference has been made in the literature on west coast Geology to the presence of Oligocene and Miocene fossils at Restoration and Beans points on the north shores of Richs Passage. In 1904 Dr. Ralph Arnold, in his paper on the Tertiary and Quaternary Pectens of California, refers to certain ‘‘shales near Beans Point, King County’,” which contain a fauna of probable Oligocene age. Note is made concerning the occurrence of Pecten peckhami Gabb at U.S. G. S. localities 4112a and 4113, between Beans and Restoration points, King County. Pecten clallamensis Arnold is noted at Beans Point and “is associ- ated with Terebratula, sp., Turritelia, sp., Marginella or Erato, sp., Natica or Lunatia, sp., Glycimeris, sp., and Astyris, sp.” In 1909, Dr. W. H. Dall’, in his paper on the Miocene of Astoria and Coos Bay, Oregon, mentions the occurrence of Oligocene strata at Port Blakeley and Restoration Point, op- posite Seattle. The following species are listed from these localities: Ampullina mississippiensis Conrad, Miopleiona in- durata Conrad, Turcicula washingtoniana Dall and Aturia an- gustata Conrad. In 1911, the writer® in a preliminary paper on the Tertiary Palaeontology of Western Washington described the occur- rence of lower Miocene strata and fossils in the Restoration Point and Blakeley Harbor area and provisionally referred to them as the Blakeley formation. These strata were recog- nized as a part of an extensive lower Miocene series involved in the north flank of a well-defined anticline trending from east to west across the Puget Sound basin. The most recent report involving a discussion of the Resto- ration Point area is to be found in a paper by Arnold and Han- nibal* on the Marine Stratigraphy of the North Pacific Coast of America, published in 1913. es llon oane SCAPHOPODA Dentalvum Conrad Daley acer evict Gano cick eae ee ae ses CEPHALOPODA Alursavangustata Contadun: acinar race Ecr ee eo rk) lane BRACHIOPODA IHemiupynisiastorionas Dally sic. cee ectopic ice: “ee Heueee HER HE H& * * een RH HH KKH E eS ERR REHR HH KER E CONDITIONS OF DEPOSITION At the close of the Tejon epoch the Eocene deposits were differentially uplifted. Early in the Oligocene new embay- ments were formed. The seas of the northern part of the 52 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. Puget Sound region were disconnected from those to the south in the Grays Harbor area. The shore line of the present site of the Puget Sound embayment appears to have existed some- where between Seattle and Tacoma and to have extended in an east to west direction from the present site of the Cascade Mountains to the present location of the Olympics. The pres- ent contact between the Eocene and Oligocene formations in the Bremerton Inlet, or Kitsap County, area is much farther north than the original southerly limits of the shore line. The strata have been tilted from their original horizontal position into a nearly vertical position and as a result those sediments which formerly extended to the south have been entirely re- moved by erosion. The lithologic character of the sediments and the faunas occurring within them indicate that they were deposited in shallow to moderately deep water. No products of direct volcanic origin were poured out in this region during the Oligocene epoch. This is in sharp contrast to the condi- tions of volcanic activity during the Tejon. CONCLUSIONS The area involved in this investigation is of special impor- tance because within it occurs one of the most complete sec- tions of Oligocene strata to be found in the state. There are approximately 8900 feet of conglomerates, shales and sand- stones which are entirely of marine origin and rest unconform- ably upon older Tejon basalts and sediments. The contact in this area between the Tejon and Oligocene is obscured by de- posits of glacial drift. The Oligocene strata form the north flank of an extensive east to west trending anticline, the axis of which has been deeply dissected by erosion. A marine fauna of 44 invertebrates is now known. The horizon repre- sented is upper Oligocene. The fauna is a unit from base to top of section and is termed the Acila gettysburgensis zone. PROCEEDINGS OF THE CALIFORNIA ACADEMY OF SCIENCES FourtTH SERIES Vox. VI, No. 4, pp. 53-85, pl. 2. May 8, 1916 IV THE PACIFIC COAST RACES OF THE BEWICK WREN! BY Harry S. SWARTH INTRODUCTION The material upon which these observations are based is mainly from the collection of the California Museum of Verte- brate Zoology. Besides the Museum collection proper there are on deposit in that institution the Grinnell, Morcom and Swarth collections. The total aggregation of skins of Thry- omanes bewicki in that Museum numbers 425 specimens. There was also available material in the Los Angeles Museum of History, Science and Art, including the collections of Messrs. Daggett, Law, Lamb, Richardson, and Willett, in all 109 specimens. To Messrs. Joseph Mailliard and John W. Mailliard the writer is under obligations for the loan of 52 skins, including splendid series of marinensis, and series of drymoecus and charienturus from regions not otherwise rep- resented. From Mr. A. B. Howell 11 skins were borrowed, illustrating special points. Altogether, a total of 597 examples of the Pacific coast forms of Thryomanes bewicki were ex- amined in the preparation of this paper. To the institutions 1Contribution from the University of California Museum of Vertebrate Zoology. May 8, 1916 54 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. and individuals above mentioned the writer is under deep ob- ligations for the use of this material. Next to the data obtained directly from this splendid series of specimens, the writer is inclined to give high place to the in- formational value of the field work incidental to its collection, in much of which he took an active part. The ideal material upon which to base conclusions as regards relationships and distribution consists of specimens in freshly acquired autumnal plumage, taken at the exact localities where the birds were born. As we have not usually any means of knowing the exact birthplace of a bird, the results of our studies must often depend upon assumptions based largely upon one’s knowledge of the species in general and its usual mode of life. Just here is where it would seem that experience and information acquired through extensive field work would be invaluable in aiding in an analysis of the facts presented by series of skins—facts often in apparent conflict. The man who works from the dried skin alone is handicapped more than he usually realizes. In working out the relationships and distribution of closely connected forms, a labor entailing the handling of large series, anomalous specimens are frequently encountered, calculated to lead one astray. Some knowledge of the country and climate, the physical surroundings of the species in gen- eral, will frequently give a clue to the explanation, while inti- mate acquaintance with the bird in life will enable one, to a certain extent, to imagine himself in the bird’s place and figure out what, under given conditions, is most apt to occur. The life history and habits of the species in general, the faunal complexion of its usual habitat, the nature and extent of vari- ation in the individual and in the race, are all factors of prime importance, and are all to be learned in the course of field work, some of them in no other way. It is not enough, be- cause a specimen bears a superficial resemblance to a race geo- graphically placed more or less remotely from where it was taken, to place the said specimen with such race. In the writer’s opinion, this has been done but too frequently in late years, resulting in extraordinary extensions of ranges of cer- tain subspecies without due justification. Familiarity with the birds in life should serve as a most excellent check to such hasty conclusions, Vor. VI) SWARTH—RACES OF BEWICK WREN 55 For many reasons the genus Tiryomanes as occurring in California is an attractive one to the student of geographical distribution. The birds exist in numbers where conditions are favorabie. As the species is not sharply delimited associ- ationally, conditions are more generally favorable than in many other groups of birds, and Thryomanes is consequently abun- dant and widely distributed throughout the state. The varia- bility of the group is notable, birds from different regions ex- hibiting to a marked degree the types of characteristics which we have learned to look for in animals of the various areas. Thus there are these several factors :—abundance, with conse- quent accumulation of extensive series of specimens; dis- regard of associational barriers effective in many other species, with resulting general distribution, this condition permitting careful scrutiny of conditions existing between many stations but slightly separated geographically, though of different faunal aspect; and variability, birds from different regions exhibiting peculiarities of color, etc.-—all combining to make this genus a profitable subject for careful examination. MANNER OF OCCURRENCE Wrens of the genus Thryomanes occur in fair abundance practically throughout the state of California. The genus in this state belongs pre-eminenily to the Upper Sonoran zone, but it also occurs commonly in places in Transition, as in the northern coast region, and sometimes in Lower Sonoran, as in parts of the San Diegan region and the San Joaquin Valley. It is not found, however, in the high Transition and Boreal of the Sierra Nevada and the southern Sierras, and it is notably absent from the arid Lower Sonoran of the Colorado and Mo- have deserts. This last was unexpected, as the species occurs commonly in regions of similar zonal character elsewhere. The above statements all apply to the breeding range of the bird. In seasons other than the nesting time there are exceptions, as noted beyond. In certain other variable groups, such as the Song Spar- rows (Melospiza melodia), Horned Larks (Otocoris al- pestris) and Bush-tits (Psaltriparus), associational requirements 56 CALIFORNIA ACADEMY OF SCIENCES {Proc. 47TH Ser. are of such a nature as to bar the species from large areas, but Thryomanes demands no such rigid conditions for its existence. The essential environmental requisite is underbrush, afford- ing shelter, and this is a condition so universally met with in California that there are few regions that do not answer. Just one of the California forms of this species has truly migratory habits, Thryomanes b. eremophilus. The others are practically resident wherever found. It is true that this fact is not generally recognized, and that there are records of sev- eral subspecies from points more or less remote from the breed- ing ground, but I am convinced that for the most part these records are not well founded. In the extensive series of skins here assembled, and in the field work incidental to the accumu- lation of the large proportion of them in which the writer took part, there has been no evidence evolved indicating regular migrations of these birds. As evidence to the contrary, the following facts may be adduced: Thryomanes b. calophonus is stated to remain in winter at the northern limit of its range (Oberholser, 1898, p. 441), which is also the northern extreme reached by the genus in North America. We do not find marinensis or spilurus wandering south in winter along the coast of southern California, any more than we do certain other forms of comparable distribution and faunal restriction, such as Pipilo maculatus falcifer, Zonotrichia leucophrys nut- talli, Junco oreganus pinosus, etc. In the extensive series of wrens assembled from southern California and from parts of the Mohave and Colorado deserts, numbering some hundreds of skins secured at all seasons of the year, there is none that can be considered as typical of Thryomanes b. drymoccus, to be taken as proof of a southward winter movement of this form. Thryomanes b. cremophilus appears to be truly migratory. Data are lacking to show whether or not the breeding ground is entirely deserted in winter, but the subspecies is known to occupy parts of the Colorado desert during the winter months, while it does not nest in that region. The birds found on the Colorado Desert during winter are apparently migrants from the desert mountains to the northward, and not from eastern Arizona, where this wren is a common resident. Though the Desert Wren has been found in winter to the eastern base Vor. VI) SWARTH—RACES OF BEWICK WREN 57 of the mountains separating the desert and coastal regions, there is no known instance of an individual of this subspecies having crossed the divide and invaded the Pacific slope. While I am convinced of the truth of the statements made above regarding the generally non-migratory habits of the Cal- ifornia wrens of the genus Thryomanes, excepting ere- mophilus, there do take place certain limited and irregular movements which are not to be considered as migrations. The late summer dispersal of birds in general, the ‘“‘scatter move- ment,” as it has been called, is common to many parts of the country, and may take individuals, mostly immatures, in any direction. The northward wandering of herons at the close of the breeding season is a well-known instance in point. In parts of California this movement takes the form of an invasion of high mountain regions by many low zone species from the ad- jacent valleys and foothills (see Grinnell, 1908, p. 22), and Thryomanes participates in this to a notable extent. In south- ern California during July and August, 7. b. charienturus is one of the most abundant birds in the higher mountains, at altitudes where it never breeds, occurring in numbers to the summits of the highest peaks. As early as the middle of Sep- tember this invading army has again withdrawn. Several specimens at hand from parts of the Sierra Nevada seem also, from dates and altitudes, to have been wanderers from lower elevations. This general movement is apt to carry occasional indi- viduals of any of the forms slightly beyond the usual faunal confines of their respective races, and there are several in- stances in the assemblage of skins examined where circum- stances seem to indicate a happening of this nature. The occurrence of T. b. charienturus in winter at stations in the western parts of the Mohave and Colorado deserts (as at Barstow, Victorville and Palm Springs), is easily ex- plained as due to continuous favorable avenues of approach from the normal breeding grounds in the foothills of the near- by mountains. Other species properly belonging to the San Diegan faunal region have been similarly found at the same places. 58 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. VARIATION There are but two distinguishable stages of plumage in this species (besides the natal down)—the juvenal and those of the first and subsequent winters. The juvenal differs from the later stages mainly in being mottled or spotted over much of the area that is subsequently uniformly colored. After loss of the juvenal plumage, in the first August and September, there are no further changes in appearance, immatures of the first winter being indistinguishable from adults; after the first vear there is but the one molt annually, at the end of the sum- mer. There are thus no seasonal changes in appearance other than those produced by the mechanical wear and tear upon the plumage, amounting to fading of colors proportionate to the nature and extent of exposure, and obliteration of finer mark- ings as the feather tips are worn away. There are no appreci- able sexual distinctions of color or markings, merely slight average differences in measurements, males averaging a trifle larger than females. It is seen that the wrens of this genus have a wide zonal range, and that where a change in life-zones acts as a check, it is, in this group as in most others, usually an absolute barrier to the species rather than an accompaniment of subspecific va- riation. It is also evident that environmental requirements are not rigid, the species being readily adaptive within rather wide limits. While the species as a whole is wide ranging, however, there is a strong tendency toward separation into different forms or races distinguished by peculiarities of color and proportions. Study of this variation demonstrates close ac- cordance of appearance with locality. Inthis groupof birds each faunal area represented tends to a remarkable degree to pro- duce its own peculiar type. So that it is seen that Thryomanes, wide ranging and with the faculty of thriving under varied climate and surroundings, exhibits to an extraordinary extent —perhaps as part of this same adaptability—variation of ap- pearance in accordance with every change in environment. It must be understood, of course, that the differences alluded to are not always conspicuous. There are frequently variations in proportions requiring careful measuring for de- tection, or slight differences in color which in scattered speci- Vor. VI) SWARTH—RACES OF BEWICK WREN 59 mens might be thought of no especial significance. With a series as extensive and representative as the one here assem- bled, however, these variations can be recognized as parts of a coordinated whole, and in the occasional instance where an in- sufficient specimen or two from some obscure locality exhibits an unexpected line of development, there is usually to be found at least a possible explanation of the occurrence. The extent and manner of variation illustrated in this series of birds can not be too strongly emphasized. For one thing there are enough specimens at hand to show a surprising range in characteristics from any one locality. Many stations are represented each by numerous specimens of freshly molted fall birds, undoubtedly individuals of the resident form of each respective place, as they appear prior to any wear and tear of the plumage. In every case there are individuals exhibit- ing wide variation in appearance, though extremes may be shown by but one or two specimens. ‘These differences can not be explained save as illustrating the amount of variation to be encountered among individuals at any one point. These variants are not of the same nature as the “inter- mediates” encountered near the line of meeting of two dif- ferent races. In the latter case, as is well illustrated from many such localities in the series here assembled, we find whole pop- ulations showing characters variously intermediate between two extremes. The occasional variants found elsewhere may crop up at any place, and in appearance do not necessarily incline towards any other subspecific type. It would almost seem as though the species as a whole was in a formative stage, showing occasional response to stimuli which we can- not at present understand. In this connection it is well to consider conditions in the juvenal plumage. In the several distinguishable Pacific coast forms of Thryomanes bewicki the color differences shown in the adults are accurately reflected in the juvenal plumage, young birds of the different recognizable subspecies exhibiting vari- ations of precisely the same nature as are seen in adults, usually in about the same degree. This, according to the general understanding of the significance of characters of the juvenal plumage, would argue great age and consequent deep-seated- ness of the color characters observed, which is hard to recon- 60 CALIFORNIA ACADEMY OF SCIENCES [Proc. 41H Ser. cile with the generally variable nature of the several subspecies as observed at this time. The above statements must not be understood as weighing against the validity of the several “subspecies” so far de- scribed from California, for in nearly every case where a name has been applied to a local race it covers an aggregation of characters fairly easily defined and recognized. In fact, the races of Thryomanes bewicki, as occurring on the mainland of the Pacific coast, may be taken as an ideal illustration of subspecific division as it is ap- plied in systematic ornithology. There are six recog- nized forms in this region—smarinensis, spilurus, drymoecus, charienturus and eremophilus in California, and calophonus in the coast region to the northward. In every case it is an easy matter to distinguish typical examples of the races. Typical specimens are not necessarily topotypes. The best manifesta- tion of a race may be found at some distance from the type locality; usually at about the center of the geographical area occupied. As departure is made from the habitat of one race toward that of another, in just such proportion is variation encountered among individuals of the races. Geographical continuity of range with corresponding intergradation of char- acters is usually taken as the test of subspecific, rather than specific, difference, but there are few instances among North American birds where these conditions are as ideally met with as among the Pacific coast forms of Thryomanes bewickt. A brief resumé of the course of variation in some of the most salient features of these races may be profitable. At the extreme northern limit of the species, on the mainland of southern British Columbia and Washington, is calophonus, of relatively large size and extremely dark coloration. On the adjacent Vancouver Island is a slightly paler colored, rather more reddish, form (included under the name calophonus), of practically the same size. Farther south, on the coast of northern California, southward to the Golden Gate, is marin- ensis, about like Vancouver Island calophonius in color but ap- preciably smaller. South of the Golden Gate is spilurus, oc- cupying the narrow coastal strip west of the Coast Ranges, south to about the southern end of Monterey Bay. This form is of a somewhat paler and brighter red than is marinensis, Vor. VIJ SWARTH—RACES OF BEWICK WREN 61 and of slightly greater size. South of spiluwrus is charienturus of the coast of southern California, a large sized, pale colored, and long tailed race. There are two inland races of Thryo- manes in California, drymoecus and eremophilus. Typical drymoecus of the Sacramento Valley is of distinctly reddish coloration, most nearly like, though paler than, marinensis and Spilurus, whose ranges it adjoins in places. Eremophilus is a desert race, exhibiting an extreme of pale coloration, and with relatively long tail. Of the insular forms, nesophilus of Santa Cruz and Santa Rosa islands, and cataline of Santa Catalina Island, are but slightly different from the geograph- ically adjacent charienturus. They are a trifle darker in color- ation, and show certain differences in proportions. Leuco- phrys, of San Clemente Island, is a short tailed race of dis- tinctly pale coloration. As regards the coastal races, from calophonus through ma- rinensis and spilurus to charienturus, the line of variation is continuous, to be traced from one to another without a break. In coloration, from the sooty calophonus to the pale charien- turus, intergradation is perfect. The intermediate stages are represented in marinensis and spilurus, the dividing lines be- tween these several races being impossible of exact definition. This gradual color change is nicely correlated with the cli- matic variation of the region, from the extremely humid Puget Sound district, with its somber hued calophonus, southward through lessening degrees of humidity accompanied by corre- sponding brightening of color in the birds. As regards size and proportions, variation is also continuous. Calophonus is of large size and with proportionately short tail. Southward, as far as the Golden Gate, as shown by marinensis of Hum- boldt and Marin counties, there is diminution in size. South of this point spilwrus shows slightly greater dimensions, and, as illustrated by specimens from many intermediate stations, there is steady increase in this regard southward through the range of charienturus. ‘Together with increased size south- ward from the Golden Gate there is correlated a proportion- ately greater length of tail. In calophonus, marinensis and spilurus, the tail is shorter than the wing. Specimens collected in the region of meeting of spilurus with charienturus have tail and wing of about equal length, while in typical charien- 62 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4rH Ser. turus the tail is usually decidedly the longer. Eremophilus, of the southern deserts, shows still greater extremes of pallid coloration and length of tail. Between eremophiius and cha- rienturus, where there is a wide gap in distribution except in one limited region, as noted beyond, there can not be traced the nicely graded series of changes found between the other California mainland forms; judging from the imperfectly rep- resentative material here assembled from the southern Sierra Nevada (where apparently the ranges of eremophilus and cha- rienturus closely adjoin), such a condition may be existent in this region. Further collecting here at the proper seasons is necessary to demonstrate this. Thus on the whole it is seen that the Pacific coast races of Thryomanes bewicki may be divided into two general groups, of pale colored, long tailed forms in the arid south- western region, and dark colored, short tailed forms in the humid northwestern coast region, with maximums of size at the extreme north and south. In every type of variation, con- necting chains of intermediates may be traced, corresponding as exactly in geographical position as in extent of variation. Drymoecus, as detailed beyond, occupies a central position, almost surrounded by the other mainland forms, and the char- acteristics of birds of this subspecies vary exactly as the con- fines of the several contiguous races are approached. The insular forms of Thryomanes bewicki do not exem- plify continuous variation such as seen on the mainland. Van- couver Island calophonus, in its comparatively paler browns, shows a departure from the mode that does not accord with the general manner of variation of the species in this region. San Clemente Island leucophrys, in its gray coloration, might be regarded as exhibiting results of the same nature as are shown in the comparatively gray Pipilo maculaius clemente of the same island. This theory is upset by the fact that on the closely adjacent Santa Catalina Island (lying directly between San Clemente and the mainland), where Pipilo m. clement@ also occurs, the representative form of Thryomanes, T. b. cataline, is distinguished from the mainland charienturus by slightly darker brown coloration. T. b. nesophilus of Santa Cruz and Santa Rosa islands is again differentiated from cha- rienturus by slightly darker, more rufescent, coloration. Vor. VI] SWARTH—RACES OF BEWICK WREN 63 In fact, in the insular forms of Thryomanes bewicki (as well as in other races of birds occurring upon the several isl- ands of the Santa Barbara group) it is at present impossible to detect generally uniform results of any factor or factors, either as to the occurrence or non-occurrence of species upon the different islands, or in the amount and nature of differen- tiation that has taken place. Possible criticism may be invited by the fact that in the present paper certain local races (subspecies) are pointed out and their characteristics described, but no names affixed. This applies particularly to the Vancouver Island form of calo- phonus, and to the wren of the southern boundary of the Great Basin region as distinguished from typical eremophilus of the Gila Basin. It is the writer’s opinion that the aggregations of individuals occupying these several areas are geographically separated from the typical forms whose names they bear. They are also probably to be distinguished, though with some dif- ficulty, by the average differences indicated; possibly they are local races in early stages of differentiation. The objections to formally affixing names in their cases are two in number: first, in the slightly distinguished races in question it is impos- sible to indicate more than obscure average distinctions; and second, the extreme variability shown in individuals of even the most strongly marked of the several described forms militates against the recognition of these apparent geographic variants even though they appear to be isolated. The peculiar char- acters of the Vancouver Island wren are perhaps to be ex- plained as solely a result of isolation. The Desert Wren of southeastern California, in its departure from typical ere- mophilus, shows a distinct approach to charienturus, and it may be that in its affinities, as it is geographically, it is inter- mediate between the two. 64 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. DIAGRAM SHOWING INTER-RELATIONSHIPS OF PACIFIC COAST RACES OF THRYOMANES BEWICKI. Island forms; Mainland forms; continuous varia- discontinuous variation. tion. Dark to light coloration, short tail to long tail. VANCOUVER ISLAND " CALOPHONUS" ———__ (Pale color) CALOPHONUS MARINENSIS DRYMOECUS SPILURUS NESOPHILUS an I ee eve CHARIENTURUS ‘ke A GRark goles CATALINAE : (Dark color; large bill and feet; long tail) LEUCOPHRYS (Pale color; short tail) DETAILED DISCUSSION OF CALIFORNIA RACES Thryomanes bewicki marinensis Grinnell. Type locality—Nicasio, Marin County, California. Range—The humid coast belt north of the Golden Gate, at least to Humboldt Bay; probably to the Oregon line. Specimens examined from the following localities: Hum- boldt County: Capetown, 1; Ferndale, 1. Mendocino County: Covelo, 7; Sherwood, 3; Willits, 1; Gualala, 3. Sonoma County: Guerneville, 5; Freestone, 2; Fulton, 1. Marin County: San Geronimo, 14; Nicasio, 3; Inverness, 8. Total, 49. Distinguishing characters—Similar to T. b. spilurus, of the coast region immediately south of San Francisco Bay, but dorsal coloration appreciably darker. Compared with calo- phonus as represented on Vancouver Island, marinensis is Plate 2 [SWARTH] PROC. CAL. ACAD. SCI., 4th Series, Vol. VI. “1yIu2aq Sounmoksy T JO satdadsqng 943 JO BrusOF LD ur uorNquysig gee ‘s€ayqoona] q saunmoksy J bi ‘2DUN DIDI “g sauDmok«y [ ‘snpiy dosau-q sounmoksy ‘a8uel Surpaeiq umouy JO @pisjno suoHne}s PIOWY -snprydouasa ‘q sounmokiy, @ ‘snpiydomasa gq saupmokay (e) ‘aSue1 Surpseiq uMOoUy JO ePIs]NO sUOHL}s P1OIVY “sninjuaiupys “gq sauvutokay T B ‘Snanpuaiivys “q saupumokayy Ey ‘Q8uUeI Suipseiq uMoUy JO apisIno suOHe}s psrox2yY ‘snI20mAup gq souDmoL4y T vr ‘sn2a0ufap “q saupmokiy yy, WF ssnanigs q saupmoksy 7 fe ‘sisuauipu -q soupmotiy TF ‘POUMUEXS 919A sustutoads YoIYM wor syuIOg i ag. Wirt x) 7) VINUOATIVS AO ALISHZAINA ADOTOOZ ALVUGALYAA AO W Vor. VI) SWARTH—RACES OF BEWICK WREN 65 closely similar in coloration; compared with calophonus as represented on the coast of Washington and Oregon, it is brighter and less sooty. In size and proportions, intermediate between calophonus and spilurus, though nearer the latter. Remarks—The wrens of the northern coast region of Cali- fornia present certain peculiarities of appearance which were commented upon, first by Oberholser (1898, p. 440), and later by Ridgway (1904, p. 565, footnote). The race marinensis was formally described by Grinnell (1910, p. 307) upon the basis of these same peculiarities. There have been available for comparison in the present connection, besides the series of the several California sub- species, 18 skins of calophonus from Vancouver Island, and 10 from the mainland of the Puget Sound region of Washington and Oregon. Inspection of these series develops several in- teresting points in regard to the wrens of the northwestern coast region in general. Judging from the material at hand it seems evident that calophonus does not occur in California, unless it is to be found on the coast of the extreme northwest- ern corner of the state, from which point there are at this time no specimens available. Furthermore, in the range of country at present ascribed to calophonus, there appear to be two distinct types existent, lumped under the one name, races which eventually may have to be separated in nomenclature. Specimens from the mainland of Washington and Oregon, which may be considered as typical of calophonus, present the extreme of dark coloration in this species. Vancouver Island birds are distinctly paler and more reddish, though of practi- cally the same size. Thus there is the dark colored mainland calophonus situated between the Vancouver Island (unnamed ) form to the northward, and wiarinensis to the southward, these latter two being paler colored and more reddish, and practi- cally alike in coloration. To put it a little differently: Beginning at the northern limit of the range of Thryomanes bewicki on the Pacific Coast, there is first, on Vancouver Island, a dark, reddish-colored bird of relatively large size. Immediately to the southward, on the mainland of the Puget Sound region, there is an ap- preciably darker, more sooty form (typical calophonus), of 66 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. approximately the same size. South of this, along the north- ern coast of California southward to the Golden Gate, is marin- ensis, paler colored again, practically the same color as the Vancouver Island bird, but smaller. Spilurus, from south of San Francisco Bay, is still paler but a trifle larger, gradually merging, both in color and size, into the larger and more pallid charienturus of southern California. The two birds at hand from the vicinity of Humboldt Bay are typical of marinensis. They are like the average of Marin County birds, and are correspondingly unlike calophonus of the mainland farther north. In the series from Marin and southern Mendocino counties there are several notably pale colored specimens. A female from San Geronimo (no. 2158, Mailliard coll.) is quite grayish above, and there are several juvenals from southern Mendocino County also aberrantly colored. Such a bird is mentioned by Ridgway (1904, p. 565, footnote), from Nicasio; so altogether, it evidently is not un- common to encounter such pale colored individuals at this point. This is at once suggestive of exactly similar condi- tions found prevailing among the bush-tits (Psaltriparus) of the region (see Swarth, 1914, pp. 513-515), and it would seem that in both instances the phenomena are to be explained in the same way. The conditions described as probably explanatory in the case of the bush-tit are as follows: “Marked restriction of territory appropriate to the humid coast races, ineffective bar- riers interposed against complementary forms of much greater numbers occupying adjacent territory, and continual encroach- ment of individuals (the radiating overflow) of the latter sub- species” (Swarth, Joc. cit.). The genus Thryomanes appears to offer a parallel instance, though to not so marked an ex- tent as in Psaltriparus. Aberrant individuals occur as men- tioned above, in a manner similar to that observed in the latter genus, but not so numerously. A series of juvenals from Marin County is appreciably less bright reddish above than is the case in young birds of spilurus from Palo Alto. Type locality—Near San Francisco or Monterey, Cali- fornia. Range—Coast region of central California (Santa Cruz faunal district) ; southern and eastern sides of San Francisco Bay, south to southern end of Monterey Bay. Restricted to the region west of the Coast Range. Specimens examined from the following localities: Contra Costa County: Martinez, 1. Alameda County: Berkeley, 3; Oakland, 7; Piedmont, 2; Alameda, 1; San Lorenzo, 1; Haywards, 2. San Mateo County: La Honda, 1; Woodside, 2; Pescadero, 2. Santa Clara County: Palo Alto, 24; Mil- pitas, 1. Monterey County: Pacific Grove, 3; Monterey, 1. Morales Distinguishing characters—Most nearly like T. b. marinen- sis, Whose range adjoins that of spilurus at the north, but of lighter brown coloration dorsally, and of slightly greater size. Compared with drymoecus it is brighter reddish above. From charienturus it differs in deeper red coloration, and in differ- ent proportions. In spilurus the tail is slightly shorter than the wing ; in charienturus the tail is longer than the wing. Remarks—Thryomanes bewicki spilurus, as here restricted, ranges over a limited area in the central coast region of Cali- fornia between San Francisco and Monterey bays. Geograph- ically it occupies a position between marinensis and charien- turus, and analysis of the characters of spilurus demonstrates that in this latter respect also it is a transitional step between the races to the northward and to the southward. Palo Alto specimens present the best manifestation of the characters of Spilurus of any of the series at hand. These birds are quite uniformly bright reddish above, the only exceptions being two or three individuals, rather duller colored, and apparently verging toward drymoecus. Birds from the east shore of San Francisco Bay (Berkeley, Oakland, etc.) present a certain peculiarity of coloration, for with hardly an exception they are extremely dark and sooty in appearance, as remarked by Oberholser (1898, p. 439). This is undoubtedly partly, but not altogether, due to smoke stain, the darkening effect of which has been noted in certain 68 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. other species at these points. I am inclined to class the birds of this region as representing an intergradient stage between typical spiluyus of the coast region and drymoecus of the inte- rior. The plumage, normally of a less bright rufescence than in the former, is still further modified by the action of the smoke, producing the extremely dark effects seen in the speci- mens at hand. Of the available skins from the east side of San Francisco Bay, practically all were secured at suburban points in the various towns, where they would be subject to the effects of the smoke of the communities. There is one speci- men in the series that forms a striking exception to the above remarks. This is no. 4284, coll. Mus. Vert. Zool., collected by Dr. J. G. Cooper, at Martinez, Contra Costa County, De- cember 15, 1863. This bird is bright, clear reddish above, closely similar to certain of the Palo Alto specimens, and even brighter colored than many from that point. It shows no sign of smoke stain. This latter fact may possibly be due to the fact of there being less smoke in the atmosphere in this general region at that early date. There are in the series four specimens from the vicinity of Monterey Bay, three from Pacific Grove and one from Monte- rey. This is too small a series to draw conclusions from, but one of these birds (coll. J. & J. W. Mailliard, no. 4691) dis- plays what appears to be a distinct trend toward the colora- tion of charienturus. Thryomanes bewicki dyymoecus Oberholser Type locality—Baird, Shasta County, California. Range—tThe central portion of California; the Sacramento Valley, and northward at least to the Oregon boundary ; north- east to the Warner Mountains, on the Nevada boundary; the west slope of the central Sierra Nevada, everywhere below Transition ; southward over about the northern half of the San Joaquin Valley. Specimens from the east slope of the Sierra Nevada at Carroll Creek, taken in September, may have been wanderers from the west side of the mountains, and not neces- sarily within the normal breeding range. Specimens examined from the following localities: Modoc County: Cedarville, 2; Sugar Hill, 1. Trinity County: Hel- Vor. VI] SWARTH—RACES OF BEWICK WREN 69 ena, 1. Siskiyou County: Callahan, 2. Shasta County: Baird, 1. Tehama County: Tehama, 5; Tuscan Springs, 1. Glenn County: Winslow, 1. Colusa County: Stony Ford, 2. Butte County: Chico, 3; Oroville, 2. Sutter County: West Butte, 2; Sutter, 5. Yolo County: Grand Island, 1; Rumsey, 3. Solano County: Vacaville, 11. Amador County: Carbondale, 2. Nevada County: Cherokee, 4; Montezuma Hill, 2. Placer County: Blue Canyon, 1. Inyo County: Carroll Creek (east slope of the Sierras), 4. Fresno County: Lane Bridge, 1. Madera County: Raymond, 2. Stanislaus County: Modesto, 7. Mendocino County: Mount Sanhe- drin, 1. Contra Costa County: Walnut Creek, 8; Mount Dia- blo, 6. Santa Clara County: Palo Alto, 1. Total number of specimens, 82. Distinguishing characters—Compared with charienturus, drymoecus has the upper surface darker and more rufescent. The tail is somewhat shorter, and in different proportion to the wing. In charienturus the tail is slightly longer than the wing, in drymoecus slightly shorter. Compared with spilurus, the upper surface of drymoecus is a duller and less rich brown. In the juvenal plumage the character of intensity of rufescence of the upper surface is also apparent, young of drymoecus be- ing less deeply colored than young of spilurus and marinensis on the one hand, and somewhat darker (though slightly so) than the young of charientwrus on the other. It is noteworthy in this regard that whereas in typical drymoecus (Sacramento Valley birds) the adults approach spilurus more nearly than they do charienturus, the juvenal plumage is but slightly dif- ferent from the same stage in charienturus. Remarks—Of the available material of this form, the greater part consists of summer adults in rather worn plumage, with a good proportion of juvenals. There is a lack of birds in fresh fall plumage. Thryomanes bewicki drymoecus is a composite race, and one probably not subject to exact definition. It differs from all the other California forms of Thryomanes in the nature of its geographical position, being centrally placed and apparently intergrading with each of the surrounding races at the va- rious points of contact. Consequently birds from different re- 70 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. gions exhibit a diversity of appearance that renders it difficult in the extreme to frame a satisfactory characterization of the race, and in places the dividing lines must be somewhat arbi- trarily drawn. Birds from the Sacramento Valley exhibit the best mani- festation of the characters of the subspecies. These characters consist of decidedly reddish dorsal surface (though not so rich a red as in marinensis and spilurus) and short tail, bear- ing a different relation to length of wing than is seen in charienturus and eremophilus. Thus in the last analysis the form drymoecus is seen to be an intergradient between the long-tailed, pale colored, southern and desert races, charientu- rus and eremophilus, and the short-tailed, richly colored, coastal subspecies, marinensis and spilurus. This is so markedly the case that while in the Sacramento Valley drymoecus may be considered a fairly well marked form, just as this center is departed from so is there encountered a variation of charac- ters tending toward whichever of the other subspecies is ap- proached. There is at hand one adult from Baird, Shasta County, California, the type locality of T. b. drymoecus. There are also available one from Trinity County and two from Siski- you County, all in the same general region in north central California. As indicated by this small series the birds from this part of the state seem to belong to the subspecies dry- moecus. Warner Mountain District. There are one adult and two in juvenal plumage from the Warner Mountains, in the ex- treme northeastern corner of California. The old bird is de- cidedly gray, as compared with Sacramento Valley specimens, but the two young ones are even more rufescent than are com- parable examples from the latter locality. The dull color of the adult is so noticeable as to suggest the possibility of the existence of a definable local race in this little known portion of the country, but in view of the manner of variation shown by drymoecus in others of the outlying parts of its range, I prefer at present to regard this specimen as another example of the variability of the form. In this connection it may be well to call attention to the possibility that the wren recorded from Camp Harney, southeastern Oregon, by Bendire (1877, Vor. VI) SWARTH—RACES OF BEWICK WREN 71 p. 113), and tentatively referred to eremophilus by Oberholser (1898, p. 429), may well be of the same race as the Warner Mountain bird. Sacramento Valley. Thirty-eight specimens from the fol- lowing counties: Tehama, Glenn, Butte, Colusa, Sutter, Yolo, Solano, and Amador. Of this series 25 are adults, the re- mainder in juvenal plumage. They were coilected during spring and summer, from early March until the mid- dle of July, hence the adults are all in rather worn plumage. Despite this wear, however, these specimens uni- formly exhibit to a marked extent the characteristic reddish dorsal surface of the subspecies. As indicated above Sacra- mento Valley birds may be regarded as typically representa- tive of the interior form, drymoecus. San Joaquin Valley. Birds from this valley are not so easily or satisfactorily disposed of. Both Oberholser (1898, p- 437) and Ridgway (1904, p. 563) have included this re- gion in the habitat of drymoecus, but the former author at least had no examples-from this valley, as shown by his list of the localities from which specimens were examined. The region is not satisfactorily represented in the series now avail- able, but there is at hand a series of seven skins from Modesto, Stanislaus County (Mailliard coll., nos. 6987, 6993, 7125, 7333, 7385, 7386, 7400), two specimens from Raymond, Ma- dera County (Mus. Vert. Zool., nos. 19,688, 19,689), and one from Lane Bridge, near Fresno (Mus. Vert. Zool., no. 19,687). All of these points are in the east central portion of the San Joaquin Valley. Of these the Modesto birds were collected in January, February, March, and May, the Lane Bridge and Raymond examples in April. Some of them are breeding birds, and the probabil- ities are that the January and February specimens are also examples of a resident form. At any rate peculiarities of appearance can hardly be explained on the ground that the birds are wandering examples of charienturus, for this more southern form would hardly be found represented by in- dividuals wintering so far north of their summer home. On the other hand, these San Joaquin Valley birds are too unlike Sacramento Valley drymoecus to be regarded as southward traveling visitants from that region. 72 CALIFORNIA ACADEMY OF SCIENCES [Proc. 47H Ser. So, on the whole, the series may safely be considered as representing the form breeding in this same general region. In coloration the whole series is quite uniform and but slightly distinguished from charienturus, being more nearly like this race than like Sacramento Valley drymoecus. In measure- ments the birds stand about midway between the two forms, though rather nearer the latter (see table). All things consid- ered, I have regarded these birds as illustrating intergradation between typical drymoecus and charienturus, and as represent- ing about the extreme southern valley locality which the name drymoecus may be used to cover. Sierra Nevada. There are six spring birds from Nevada County. Two are from Montezuma Hill, taken March 30, and four from Cherokee, April 5 and 7. From these dates they may fairly be assumed to be representative of the breed- ing bird of the region. In coloration they closely approach Sacramento Valley drymoecus, though they are not quite so reddish; in measurements and proportions there is no dif- ference. There are at hand four immatures in fresh winter plum- age: a male, Blue Canyon, Placer County, October 21; two males and a female, Carroll Creek, east slope of Sierra Ne- vada in Inyo County, September 11 and 12; all collected at altitudes from 5000 to 7500 feet. A difficulty arises in the proper weighing of the characters of these birds, in that they were evidently late summer wanderers from lower altitudes, from just where, it is impossible to say. The Blue Canyon specimen (Mus. Vert. Zool., no. 23,295) is dark reddish above, widely different from autumnal charien- turus, but not so readily distinguished from fall specimens of marinensis. It is presumably typical of the fall plumage of drymoecus as occurring in the central Sierra Nevada. The three birds from Carroll Creek (Mus. Vert. Zool., nos. 20,858, 20,859, 20,866) are quite different in appearance. They are but slightly reddish above, and with a grayish cast not seen either in charienturus or in typical drymoecus. As to the pre- cise region occupied by these latter birds during the breeding season, that, of course, is problematical, for they might have wandered even from over the crest of the Sierras; but their appearance leads to the assumption that they represent an ex- Vor. VI] SWARTH—RACES OF BEWICK WREN 73 treme southern outpost of Sierran drymoecus, where that race abuts on eremophilus. The grayish cast of the dorsal surface may well be explained as evidence of intergradation between the two. From Walnut Creek and Mount Diablo, Contra Costa County, there is a series of two adults and 12 juvenals. The adults, June birds in excessively worn plumage, bear no re- semblance to the ruddy colored spilurus of the nearby coast region. The young birds, too, lack the clear reddish tone of Palo Alto juvenals, and are very similar to young birds from the Sacramento Valley. The series is unsatisfactory in the lack of fresh plumaged adults, but is apparently to be referred to drymoecus, though tending toward the coast form spilurus. Birds from the east shore of San Francisco Bay (Berkeley, Oakland, etc.), the nearest point in the range of spilurus, are themselves for the ‘most part not typical of that race, so that specimens from this whole general region may be regarded as illustrating intergradation between the coastal spilurus and drymoecus of the interior. The reference of the Walnut Creek and Mount Diablo birds to drymoecus is necessarily based al- most wholly upon the appearance of the juvenals. Fortunately there are certain characteristics at this stage, as shown by the large series from the Sacramento Valley, apparently justify- ing such procedure. There is one specimen at hand from a point outside of the general breeding range of drymoecus, which I feel obliged to refer to this form. This is an immature female (no. 5268, Grinnell coll.) taken at Palo Alto, California, September 27, 1902, and in complete first winter plumage. In color and pro- portions this bird appears to be unequivocally drymoecus. Without conceding any regular migratory habits to the form, it is quite possible for occasional individuals to stray during late summer and fall for as short a distance as is indicated by this capture. I believe this specimen to be such a wanderer from the breeding ground. The subspecies Thryomanes bewicki drymoecus has been denied recognition by the American Ornithologists’ Union Committee, and declared to be “not separable from Thryo- manes b. spilurus’ (1901, p. 314). Ata later date, in the third edition of the Check-List (1910, p. 339), the ascribed range 74 CALIFORNIA ACADEMY OF SCIENCES [Proc. 47H Ser. of drymoecus is included in that of T. b. charienturus. Con- ceding that drymoecus is not as sharply defined a race as cer- tain other forms of the species, still the disposition accorded it under this latter ruling is certainly unsatisfactory, and not tending to assist to an understanding of existing conditions. The wren of the Sacramento Valley is as widely different from charienturus of southern California as is the northern coast bird, to which it is more nearly related. If it is not deemed de- sirable to recognize these slightly differentiated forms in the Check-List, a better compromise would be effected by extend- ing the range of spilurus to include the Sacramento Valley and central Sierra Nevada, that of charienturus to extend through the San Joaquin Valley. Such treatment would be nearer the truth than is the present accepted arrangement ; but even so, there would be encountered the difficulties and dis- crepancies bound to arise in the attempt to define by rigid lines the many fluctuations encountered in the birds of these wide and varied regions. Thryomanes bewicki charienturus Oberholser Type locality—Nashoguero Valley, Lower California (near Mexican and United States boundary line). Range—Coast region of southern California, south from San Benito County and into northwestern Lower California. Breeds mainly on the coastal slope, but in winter is found eastward to the western edges of the Colorado and Mohave deserts, as at Palm Springs, Victorville and Barstow. Specimens examined from the following localities: San Benito County: Paicines, 13; Mulberry, 4. San Luis Obispo County: Paso Robles, 1. Santa Barbara County: Santa Barbara, 2; Lompoc, 4; Point Conception, 1; Santa Inez River, 1. Ventura County: Mount Pinos, 1; head of Piru Creek, 1. Tulare County: Cannell Meadow, 1; Monache Meadow, 1; Trout Creek, 7. Kern County: Weldon, 3; Onyx, 3; Isabella, 2; Bodfish, 2; Walker Pass, 3; Piute Moun- tains, 4. Los Angeles County: Pasadena, 91; San Fernando Valley, 19; Santa Monica Mountains, 3; Sierra Madre, 3; Monrovia, 1; San Gabriel Mountains, 6; San Francisquito Vor. VI] SWARTH—RACES OF BEWICK WREN 75 Canyon, 2; Los Angeles, 7; El Monte, 2. San Bernardino County: San Bernardino Mountains, 5; Cajon Wash, 1; Victorville, 5; Barstow, 1; Reche Canyon, 3. Riverside County: Riverside, 5; San Jacinto Mountains, 28; Vallevista, 4; Palm Springs, 6; San Gorgonio Pass, 1. Orange County: Santa Ana Canyon, 1. San Diego County: San Diego, 1; Witch Creek, 1; Cuyamaca Mountains, 2. Total, 252. Distinguishing characters—Coloration paler, less rufescent dorsally than in any other form of Thryomanes from the main- land of California, save eremophilus. In fresh fall plumage adults of charienturus average close to Saccardo’s umber, a color about intermediate between the richer, more rufous, raw umber of spilurus, and the grayer hair brown of eremo- philus. In measurements charienturus differs from eremo- philus in smaller size ; from spilurus, marinensis and drymoecus in different proportions, usually having tail longer than wing, whereas in the latter three forms the reverse is the case. Remarks—lIt is in the relative geographical positions ac- corded to charienturus and drymoecus that the results of my observations are most at variance with those of the writers who have previously studied the group. Both Oberholser (1898, p. 437) and Ridgway (1904, p. 563) define the habitat of drymoecus as inclusive of the entire San Joaquin Valley, and as extending westward to the coast in San Luis Obispo County. As already stated under drymoecus, birds from the central San Joaquin Valley are not typical of that form, being rather of the nature of intergrades toward charienturus. Still less are birds from the coast region of San Luis Obispo and Santa Barbara counties to be regarded as representative of drymoecus. Such divergence from the mode of charienturus as they exhibit appears to be an approach toward spilurus, whose territory they border. This, to my mind, is a satisfac- tory explanation of the slightly more reddish coloration of certain individuals, as well as of the variation in measure- ments. Seventeen skins from San Benito County, 13 from Paicines and four from Mulberry, most of them in fresh, unworn plum- age, afford excellent comparative material from an interme- diate locality, about at the meeting place of the ranges of 76 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH Ser. charienturus, spilurus and drymoecus. These birds in colora- tion are practically like southern California charienturus, being no more rufescent than are most specimens from that region, and less reddish than birds from the coast of Santa Barbara County. In measurements the San Benito County birds are shorter tailed than is typical charienturus, and thus approach Spilurus or else San Joaquin Valley drymoecus. There is very little difference in measurements between these latter two. There is at hand one skin from San Luis Obispo County and eight from the coast of Santa Barbara County. Some, but not all, of these birds are slightly darker and more rufescent above than charienturus from points farther south, but I be- lieve that all are to be referred to that form. It is probably the type of specimen such as [ have at hand from San Benito and Santa Barbara counties that formed the basis for the exten- sion of the range of drymoccus to these points, but I prefer to regard such birds as illustrating intergradation between charienturus and spilurus, over the intermediate territory which they occupy. They are with difficulty distinguished from typi- cal charienturus, and are certainly quite different in appearance from typical drymoecus of the Sacramento Valley. The excellent series of skins at hand from the coastal re- gion of Los Angeles, San Bernardino and Riverside counties, includes specimens in all stages and from all seasons, and, judging from these, it would seem that the race charienturus, as confined to southern California, is as well defined as any of the forms of the genus Thryomanes. Here, too, however, there is a certain amount of variation, usually in shade of ru- fescence dorsally, even in specimens in fresh fall plumage taken at practically the same points; differences that can hardly be explained on any grounds save that they represent the varia- bility existing among individuals of the one race. Segregation according to age or sex yields no uniform or satisfactory di- visions. In the series at hand there are six winter birds from points at the western edge of the Mohave Desert, five from Victor- ville and one from Barstow. These specimens have been re- corded as drymoecus (Mailliard and Grinnell, 1905, p. 101; Grinnell, 1901, p. 70), but I am unable to distinguish them Vor. VI) SWARTH—RACES OF BEWICK WREN 7f7/ from Pacific Slope charienturus, and believe that they are probably wanderers from the nearby San Bernardino Moun- tains. Midwinter specimens from Palm Springs, at the west- ern edge of the Colorado Desert, belong in a similar class, of winter visitants from the adjacent San Jacinto Mountains. There is available a series of 23 skins from the southern Sierra Nevada, in Tulare and Kern counties. Of these, 14 are juvenals, while the nine adults are in midsummer plumage, so frayed and faded as to be of little value for color compari- sons. It is evident, however, that this series is not to be re- ferred to drymoecus, and at present it seems best to include it under charienturus. Vhe young birds are decidedly less red- dish than juvenals of drymoecus, averaging closely similar to young charienturus. The variability shown among them tends toward grayish extremes, certain individuals being even paler colored than the average of eremophilus. The adults closely approach charienturus in similarly worn plumage, and in meas- urements and proportions also approximate this form. There are at hand, fortunately, three adults in fresh, unworn plumage, taken in December in the Piute Mountains, at the southern extremity of the Sierra Nevada. These birds are unequivocally charienturus, and I believe it is fair to assume that they represent the resident form of this region. Alto- gether the available material is sufficient to justify the state- ment that the wren of the extreme southern Sierra Nevada is not drymoecus. At first it seemed questionable as to whether or not the birds were representative of eremophilus, which breeds on the east slope of the Sierras a short distance to the northward. The juvenals, as noted above, tend toward an ex- treme of grayish coloration, while the faded adults have some- thing of the appearance of the Desert Wren. Also the pres- ence in the series of an undoubted example of eremophilus from the Piute Mountains in September tended to obscure the facts, but this bird in all probability was a migrant from the desert regions to the eastward. Fresh plumaged Thryomanes from the Sierra Nevada of Kern and southern Tulare counties are desirable, and it may be that such will exhibit characteristics intermediate between typical charienturus and cremophilus. 78 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. Thryomanes bewicki nesophilus Oberholser Type locality—Santa Cruz Island, California. Range—Santa Cruz and Santa Rosa islands, California. Specimens examined from the following locality: Santa Cruz Island, 19 (14 adults, 5 juvenals). Distinguishing characters—Most nearly like T. b. charien- turus of the adjacent mainland, from which it is but slightly differentiated. In coloration the dorsal surface and flanks are of a somewhat darker brown than is the mode in the mainland form. ‘Tail usually shorter than wing; in just one of the adults at hand is it the reverse. In charienturus the tail is generally longer than the wing. Remarks—The Santa Cruz Wren is apparently one of the most illy defined of any of the described forms of Thryomanes bewicki. The available series affords satisfactory material for comparison, containing four September specimens in newly acquired winter plumage, others taken in early spring, before becoming excessively worn, and some juvenals. Judging from these specimens this island form has become but slightly dif- ferentiated from the mainland race. I am able to appreciate the average slightly darker coloration of upper surface and flanks, but it is covered in the range of variation shown by mainland charienturus, occasional individuals of the latter be- ing quite as dark. The difference in proportions is perhaps the most tangible character, for the proportionately shorter tail of nesophilus is evident upon measurement. It is perhaps noteworthy that the slight differences serving to distinguish nesophilus from chari- enturus are steps in the direction of spilurus, the slightly more reddish dorsal coloration, darker flanks, and shorter tail, be- ing just the characteristics encountered in birds occupying the intermediate coastal region between the ranges of charienturus and spilurus. The mainland nearest to Santa Cruz Island forms part of this intermediate region. Thryomanes bewicki cataline Grinnell Type locality—Avalon, Santa Catalina Island, California. Range—Santa Catalina Island, California. Vor. VIJ SWARTH—RACES OF BEWICK WREN 79 Specimens examined from the following locality: Santa Catalina Island, 14. Distinguishing characters—Closely similar to the mainland form charienturus, but averaging slightly darker dorsally, and with somewhat heavier bill and feet. Remarks—tThe peculiarities of the Santa Catalina Island Wren had been already commented upon (Oberholser, 1898, p. 436) before Grinnell (1910, p. 308) affixed a name to the race. The differences distinguishing this form from charien- turus of the neighboring mainland, however, are but slight, barely sufficient to indicate average distinctions in series from the two regions. Of the skins at hand, 13 are adults, mostly in winter plumage, fresh and unworn. These show the color difference claimed for the race, as well as differences of pro- portions, and, admitting that these differential characters are not trenchant, still they exist, and their existence justifies the use of a separate name, especially in an insular form. Thryomanes bewicki leucophrys (Anthony ) Type locality—San Clemente Island, California. Range—San Clemente Island, California. Specimens examined from the following locality: San Clemente Island, 23. Distinguishing characters—In coloration leucophrys is not- iceably grayish as compared with the darker colored neighbor- ing races, cataline, nesophilus and charienturus. In its pale color leucophrys thus approaches eremophilus, but is easily dis- tinguishable by size and proportions; leucophrys has shorter wings and tail, and longer bill. It also has tail shorter than wing, while in eremophilus the reverse is true. The broader superciliary stripe of leucophrys is diagnostic. Remarks—The San Clemente Wren is a strongly marked form presenting various points of difference easily appreciated by the most casual observer. The generally pale coloration is apparent in the juvenal as in the adult plumage, and the broader and more conspicuous superciliary stripe is also a feature in the juvenal plumage. 80 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH Ser. The series available contains 10 adults and 13 juvenals. The adults are all spring and summer birds, more or less worn and faded, there being no fresh autumnal specimens in the lot. Fall birds are probably more rufescent. Thryomanes bewicki cremophilus Oberholser Type locality—Big Hatchet Mountains, Grant County, New Mexico. Range in California—The part of California known to be occupied by this form during the breeding season is limited to the higher mountains of the desert regions of the eastern part of the state in Inyo and Mono counties, and on the east slope of the Sierra Nevada from Lone Pine Creek an undetermined distance northward. In winter it occurs over the breadth of the Mohave and Colorado deserts, westward to the Piute Mountains and to Palm Springs. Specimens examined from the following localities: Cali- fornia. Inyo County: Inyo Mountains, 2; Kearsarge Pass, 1; Lone Pine Creek, 1; Little Cottonwood Creek, 1. Kern County: Piute Mountains, 1. Riverside County: Palm Springs, 1. Colorado River between Needles and Riverside Mountain, 9. Arizona: Fort Mohave, 3; Huachuca Moun- tains, 33; Chiricahua Mountains, 6; Fort Lowell, 13; Santa Cruz River near Tucson, 1. Total, 72. Distinguishing characters—Largest of the California forms of Thryomanes (see table). Tail longer than wing. Colora- tion pallid, the palest colored of the California subspecies of the genus. Remarks—The series here accumulated from different points in southeastern California presents certain peculiarities of appearance that suggest the possibility of these birds repre- senting a form recognizably distinct from typical eremophilus. In general the California birds appear to be slightly darker dorsally and on the flanks, and slightly smaller, with propor- tionately shorter tail. Also in the California birds the ground color of the black-barred central rectrices is usually brownish, where in specimens from Arizona it is more decidedly gray; in the California birds there is a tendency toward a dusky, un- WREN 81 SWARTH—RACES OF BEWICK Vor. 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In southeastern Arizona eremophilus is a common resi- dent of both the Upper and Lower Sonoran zones, being abundant in the Lower Sonoran river valleys. In eastern Cal- ifornia this wren appears to breed only in Upper Sonoran, mi- grating down into Lower Sonoran in the winter months. It is, I believe, the only California wren of this genus that has truly migratory habits. That individuals of the species should be found in the valley of the Colorado River, at the western boundary of Arizona, in winter only (Grinnell, 1914, p. 209), while the species is resident the year through in valleys of similar zonal character in the eastern part of the state, argues, it seems to me, that these sets of individuals represent two entirely sepa- rate aggregations, two distinct subspecies, if we wish to call them so. Furthermore, observations so far made as regards other species show that the valley of the Colorado does not serve as a winter home for birds from the colder country to the eastward. The transient winter population of this valley seems to come almost entirely from the Great Basin region to the northward, with its surrounding mountains, and it is fair to assume that these winter visiting wrens are also from that re- gion. The slight differential characters apparent, as enumer- ated above, appear to bear out this assumption. Personally I believe that there are at least two separate forms included under the term eremophilus as now used, one occurring in the Great Basin region of southern Nevada and eastern California, migrating over the Colorado and Mohave deserts in winter, the other represented by the resident bird of southeastern Arizona. Additional material is needed from California, in the nature of fresh autumnal and early spring specimens from breeding stations, more clearly to demonstrate the presence of differentiating characters. In the absence of such material, and bearing in mind the variability shown by the wrens of this genus where different subspecies meet, it seems advisable to refrain from formally affixing a name to the pos- sibly recognizable California race. It is significant in this con- nection to note that in proportion as California specimens of Vor. VI] SWARTH—RACES OF BEWICK WREN 8&3 eremophilus differ from the mode of that subspecies, so do they approach charienturus or drymoecus. There is a specimen of the Desert Wren at hand collected in the Piute Mountains, Kern County, September 6, 1903. As noted previously in this paper, under charienturus, examples of the latter race were taken in winter in the same mountain range; and circumstances make it appear that charienturus is the resident form. With little doubt eremophilus is but a migrant or winter visitant at this point. There is at hand an- other example of this subspecies from Palm Springs, Riverside County, taken December 30, 1903. The Desert Wren thus ranges in winter over the breadth of the Colorado Desert, and probably over the Mohave Desert as well, but it evidently is rare at the western borders of these tracts. Considerable win- ter collecting at points on the Mohave River, as at Victorville and Yermo, has failed to disclose its presence there, and the one specimen from Palm Springs is the only example recorded from the latter station. Apparently the bottom lands of the Colorado River form the main winter home of the species in this region. The series of skins from southeastern Arizona contains an excellent representation of both adults and juvenals, taken at all seasons of the year. The individuals of this series, al- though true in the main to the characteristics of the race, ex- hibit a certain amount of variation, apparently to be explained only as due to individual peculiarities. This is true of both adults and juvenals. As having bearing upon the extremes of variation encountered, mention might be made of the re- corded occurrence of drymoecus at Calabasas, southern Ari- zona (Oberholser, 1898, p. 438). In the series before me there is a single individual taken in the Chiricahua Mountains, Arizona, October 27, 1914 (no. 2538, coll. of J. E. Law), that might be considered as belonging in the same category. This last mentioned bird is short tailed and rather dark col- ored, being not unlike certain examples of drymoecus in ap- pearance, while it is even darker colored than selected speci- mens of chartenturus. While this specimen in certain respects thus bears a casual resemblance to some California birds rather than to typical eremophilus, I cannot believe that it belongs to the race drymoecus, in the sense that this is an individual 84 CALIFORNIA ACADEMY OF SCIENCES {Proc. 4TH Ser. that has actually traveled from central California to southeast- ern Arizona. Such action would be so remarkably at variance with all known conditions prevailing among the subspecies of Thryomanes of the central valley and coast regions of Cali- fornia that I do not for a moment consider that it is to be taken into account in explaining this circumstance. As affording additional evidence to the contrary, there is in my series a molting bird taken in the Huachuca Mountains, Arizona, August 17, 1902 (no. 3082, Swarth coll.). This specimen, covered with pin feathers, and with rectrices and remiges but partly grown, is assuming a dorsal coloration far more rufescent than the average of eremophilus, freshly molted birds being used in comparison, and it is closely simi- lar to the Chiricahua Mountain bird just described. Yet there can be but little doubt that this individual was in its summer home when captured, and that it is representative of an extreme of color variation occasionally reached in the subspecies eremophilus. LITERATURE CITED AMERICAN ORNITHOLOGISTS’ UNION CoMMITTEE, J. A. Allen, Chairman and Editor. 1901. Tenth supplement to the American Ornithologists’ Union Check-list of North American birds. Auk, 18, pp. 295-320. 1910. Check-list of North American birds. Ed. 3, re- vised (New York, American Ornithologists’ Union), 430 pp., 2 maps. BENDIRE, C. 1877. Notes on some of the birds found in southeastern Oregon, particularly in the vicinity of Camp Harney, from November, 1874, to January, 1877. Proc. Boston Soc. Nat. Hist., 19, pp. 109-149, GRINNELL, J. 1901. Midwinter birds at Barstow. Condor, 3, pp. 70-71. 1908. The biota of the San Bernardino Mountains. Univ. Calif. Publ. Zool., 5, pp. 1-170, pls. 1-24. Vor. VI) SWARTH—RACES OF BEWICK WREN &5 1910. Two heretofore unnamed wrens of the genus Thryomanes. Univ. Calif. Publ. Zool., 5, pp. 307-309. 1914. Anaccount of the mammals and birds of the lower Colorado Valley with especial reference to the distributional problems presented. Univ. Calif. Publ. Zool., 12, pp. 51-294, pls. 3-13, 9 text figs. MAILLIARD, J., with GRINNELL, J. 1905. Midwinter birds on the Mojave Desert. Condor, 7, pp. 71-77, 101-102. OBERHOLSER, H. C. 1898. A revision of the wrens of the genus Thryomanes Sclater. Proc. U. S. Nat. Mus., 21, pp. 421-450. Ripeway, R. 1904. The birds of North and Middle America. U. Sa Nat. Muss) Bull SO; ee, Fig. 1. Male genital hooks of the species of Orthotylus, as viewed from a point vertical to the plane of the hook. 1, Orthotylus insignis; 2, tibialis; 3, ferox; 4, viridicatus; 5, coagulatus ; 6, flavosparsus; 7, chlorionis; 8, fraternus; 9, uniformis; 10, translucens; 11, ovatus; 12, catulus; 13, languidus; 14, modestus; 15, dorsalis; 16, mar- ginatus; 17, molliculus; 18, affinis; 19, brunneus; 20, pullatus; 21, crucia- tus; 22, lateralis; 23, cuneatus. ‘PROCEEDINGS OF THE ’ CALIFORNIA ACADEMY OF SCIENCES FourtH SERIES Vor. VI; sNoni6, pp: 129-213. May 12, 1916 ; VI . A CATALOGUE AND HOST LIST OF THE ANOPLURA BY G. F. Ferris Of Stanford University » INTRODUCTION The Anoplura (sucking lice) have long been much neg- lected and much misunderstood, for as late as 1904 no critical, comparative study of the group had ever been made; and this in spite of the fact that the group had had a place in two monu- mental works upon parasitic insects, Insecta Epizoa of Giebel and Les Pediculines of Piaget. With the exception of a few forms of such peculiar nature that they were almost of neces- sity given generic rank, the species were for the most part lumped under the genus Hematopinus and all were regarded as forming a single family, the Pediculide. In 1904, Ender- lein, in a series of “Lausestudien” published in the Zoolog- ischer Anzeiger, broke up the all-inclusive genus Hematopinus into several genera and elevated this group, as well as certain other groups, to family rank. There has been some objection to this procedure, but on the whole it has been amply justified by time. The old classi- fication was based upon lack of knowledge and served only successfully to conceal a wealth of remarkably interesting bio- May 12, 1916 130 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. logical facts that the newer classificatiom has revealed and em- phasized. The remarkable degree to which these parasites are broken up into natural groups that are strictly confined to closely related groups of hosts, is now clearly evident, while previously it was barely hinted at. The problem of their dis- tribution is shown to be almost exclusively the problem of the genetic relationships of their hosts. In 1908 there appeared, as a part of Wytsman’s Genera Insectorum, a catalogue, compiled by Dalla Torre, based upon the work of Enderlein. This catalogue has proved of immense value, but the knowledge of the Anoplura has increased so rapidly since its publication that the additions and corrections have now attained a bulk almost rivaling the original cata- logue, and it therefore seems well that a new catalogue should be issued. These changes and additions may briefly be summarized. Since 1909 nine valid genera have been added to the list and approximately 60 species have been described (the previous catalogue listed 65, the present one lists 120). The position of numerous species then in doubt has since been cleared up and many of the question marks have been removed, this being the case especially with the North American species described by Osborn, almost all of which were then in doubt but have since been cleared up. More significant, perhaps, than the de- scription of new genera and species is the improved standard of work that has been established. The magnificent “Mono- graphie der Robbenlaiise” of Enderlein, in the report of the “Deutsche Siidpolar Expedition,” and the careful and critical work of Fahrenholz, Cummings, and Neumann, form a splen- did contrast to the superficial and often inaccurate work that formerly prevailed. The synonymy of many of the hosts and some of the para- site species is still badly tangled. The hosts have frequently been referred to only by their vernacular names and when the scientific names have been used they have sometimes been in- accurate, added to which the instability of mammal nomen- clature has not been conducive to clearness. The synonymy of the North American mammals has in part been worked out from the “List of North American Land Mammals in the United States National Museum’ (Miller, 1911), and, in ad- Vor. VI) FERRIS—ANOPLURA 131 dition, the authorities of the Museum of Vertebrate Zoology of the University of California have been extremely kind in helping to clear up numerous matters. The synonymy of the European mammals has been worked out from the “Catalogue of the Mammals of Europe” (Miller, 1912). The synonymy of the Primates has been taken from Elliot's “A Review of the Primates” (1912), but it is very probably still far from cor- rect. The synonymy of other species, when not obtainable elsewhere, has been reduced to the basis of Trouessart’s “‘Cata- logus Mammalium” (1899), although it has been necessary to do this only in the case of some of the older species. The host names given in the list of Anoplura are as nearly as can be determined the correct ones. In the host list the names in parentheses are regarded as synonyms, the others are correct as far as available information permits. An attempt has been made to list all the host names that have at any time been used. SYSTEMATIC POSITION OF THE ANOPLURA Anoplura Leach, Edinburgh Encyclopedia (1817) ; Ender- lein, Zool. Anz., vol. 28, pp. 121-147 (1904) ; Mjoberg, Ark. f. Zool., vol. 6, pt. 13 (1910); Cummings, An. Mag. Nat. Hist., ser. 8, vol. 15, pp. 256-259 (1915). Pediculine Burmeister, Handbuch d. Ent., vol. 2, p. 52 (1835). Siphunculata Meinert, Videnskabelige Meddelelser (1896) ; Cholodkovsky, Zool. Anz., vol. 27, p. 527 (1904). Pseudorhyncota Cholodkovsky, Zool. Anz., vol. 27, p. 125 (1903). Lipognatha Borner, Zool. Anz., vol. 27, p. 527 (1904). Ellipoptera Shipley, ibid., vol. 27, p. 261 (1904). The systematic position of the Anoplura has always been a matter of doubt and dispute. Because of their parasitic habits they were for a long time classed with the Mallophaga, but later under the influence of the “biting- or sucking-mouth- parts” fetish, the two groups were separated and the Anoplura were placed with the Hemiptera, of which they have for some time been regarded as a suborder most frequently known as Parasita. Their position here has quite generally been re- 132 CALIFORNIA ACADEMY OF SCIENCES [Proc. 47TH Ser. garded as rather definitely fixed, but within the last few years evidence has been found which indicates that a readjustment is again desirable. Handlirsch and Cholodkovsky have favored an arrange- ment which restores the Anoplura and Mallophaga to a posi- tion very similar to that which they originally held in relation to each other, and other authors have brought forward evi- dence in support of this view. As a result of a comparative study of the two groups Mjéberg has concluded that they are really quite closely related, the Anoplura being merely a further adaptation to a parasitic life, and with this view Kellogg and Cummings are inclined to agree. Enderlein alone, of recent authors, has contended for retaining the Anoplura as a sub- order of Hemiptera. The evidence is too voluminous to be reviewed here, but it indicates very strongly that the Ano- plura really have nothing to do with the Hemiptera and are related to the Mallophaga. It seems best to regard the Ano- plura as a distinct order and in the latest classification of the Insecta, that of Brues and Melander, this is done. However, the problem of their relationships is still an open question which can only be settled by much more careful comparative morphological studies. The classification within the order itself is extremely sim- ple; too little is known about the group for the classification to be otherwise. Four families, all of which apparently form quite natural groups, are recognized. Of these, one, Hzma- tomyzidz, contains a single remarkable species (with a possi- ble variety) which occurs upon elephants. Another small fam- ily, Echinophthiriidz, is limited in its occurrence to marine mammals, its peculiarities being ascribable to adaptation to the aquatic life of the hosts. The Pediculidz include the spe- cies found upon man, apes and monkeys, and the remainder of the species are contained in the family Heematopinide. Nearly as many species have been described since 1908 as had been described previous to that time, but in spite of this activity the study of the group has hardly begun. The host list, when compared with a list of the mammals of the world, is pitifully small, as is instanced by the fact that there are but four records of Anoplura from mammals of the South Ameri- Vor. VI] FERRIS—ANOPLURA 133 can region. It is certainly not unsafe to estimate that the number of known species is not more than one-fifth of those that actually exist. KEY To FAMILIES, SUBFAMILIES AND GENERA OF ANOPLURA. 1—Body thickly beset with more or less short, stout spines, or with spines and scales. Occurring exclusively on marine mammals. Family ECHINOPHTHIRIIDE...... Z Body with spines or hairs always in definite rows, never with scales. Occurring exclusively on land mam- mI. Song Seb acon poced oe FOC goo acon UU one Omer 4 2—Thorax and abdomen bearing delicate scales. Antenne four- or five-segmented. Subfamily ANTARCTOPHTHI- RUINED). G66 Ho. bid Bik © olbictos Od o.P O.0e aio PE OIDOIomir.c 3 Thorax and abdomen without scales. Antenne four- segmented. Subfamily EcHinopHTHIRIN#®..Genus Echinophthirius 3—Antenne four-segmented......... Genus Lepidophthirus Antenne five-segmented........ Genus Antarctophthirus 4—Head tubularly produced anteriorly; tibize without a thumb-like process opposing the claw. Family Ha#Ma- ToMYzID&. One genus, Hematomyzus, occuring on elephants. Head not so produced; tibize with thumb-like proc- ess opposine ithe Claws..2 ace eile +02 oe 2 oc eles 5 5—Eyes lacking. Family H@MATOPINIDE..........+-- 9 Eyes present, well pigmented. Occurring on man, apes and monkeys. Family PEDICULIDE............+++- 6 6—Antennz distinctly five-segmented, abdomen without pleural plates. Subfamily PEDICULINE............. 8 Antennz three-segmented or obscurely five-seg- mented, abdomen with pleural plates. Subfamily PEpt- CiNTEND.OD Pano boo Gaon s 010 00 oC eeu eo cetaro 7 7—Legs all with slender, pointed claws, abdomen with three pairs of pleural plates............ Genus Pedicinus Anterior legs with slenderer claw than the others, abdomen with two pairs of pleural plates............ SiS MOA amano onlin or oo Oo ......Genus Phthirpedicinus 134 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. 8—legs alliiofsame sizes. 2 .s aac eo. Genus Pediculus Anterior legs much smaller than others. ..Genus Phthirus O= Antenne) fivie-seommente di <\cte)ci).ar 0 = iaehetetssienmiceraiol= 11 Antenne three-segmented. Subfamily EuHa:MATOPI- NUN: Deg oh See lnc aaa aC Cea ae Met aati, lomtion ihc 10 10—Posterior legs with stalked, disk-shaped appendages on femurnsand' tibia? s.5,. 0.22.0 «25: Genus Euhematopinus Posterior legs without such appendages...........-. BSE air eR ES eee Genus Hematopinoides 11—Legs and claws all practically of equal size.......... Subfamily HA:MATOPININZE....... Genus Hematopinus Anterior legs smaller and with slenderer claw than the posterior pair, at least. Subfamily LivoGNaTHIN &..12 12—Anterior tarsi with two joints...... Genus Hybophthirus Anterior tarsi with but.one joint .2< 222 .r cise oe eee 13} 13—Anterior tarsi with a short, claw-like process in addi- tion tor theyclawies.. . .< sae 2 sacateeeree ee Genus Scipio Anteriontarsiimot SOs. 2:2 )/25 ue sereieare caer 14 14— Abdomen with well developed pleural plates.......... 18 Abdomen entirely without pleural plates............. 15 15—Abdomen with more than one row of hairs or spines OnveacheSeements 2 ..c/s sci pees: Genus Linognathus Abdomen with but one row of hairs on each segment. .16 16—Gonapods moderately long, behind each gonapod a stout, flat, spine-like process...... Genus Cervophthirius Gonapods very short, no flat, spine-like process behind GIGLI s Cetesches sttastis oc 0: >a tes ar Genus Hemodipsus (in part) 18—Anterior pair of legs equal to middle pair, both pairs very small, posterior pair large and stout............ PROTOS ape PT oho 15S. sis. 5's) agelOy shees uavorene ave Genus Enderleinellus Anterior legs smaller than either middle and poste- rior legs and with much smaller and more slender claw. 19 19—Second or third abdominal sternite with a chitinized plate or area near each lateral margin. Genus Fahrenholzia Second or third abdominal sternite without such PlBteS is cgi tes «© sinha Gloasia.e nto CR EE eons 20 20—Abdominal segments with but a single transverse row OF SPIMES Aa Aaae «4 < wuandie Solder sar eeeys oeeeweuemstete et ayeKs 21 Abdominal segments, at least in part, with two or more transversestows Of SPINES. ome einen 22 Vor. VI] FERRIS—ANOPLURA 135 21—Occiput deeply sunk into the thorax, rostrum sur- rounded by denticles, pleural plates quite large........ BINERSTENG CROTON OI cM CHIE RCE Genus Eulinognathus Occiput not deeply sunk into the thorax, rostrum not surrounded by denticles, pleural plates minute... . rat seh eves Genus Hemodipsus (in part) 22—Abdominal tergites and sternites with not more than EWOsTOWS! Ob hairsHOm SpImeSs crm says k-tcisti-s « «ose «6 5. 23 Abdominal tergites and sternites in part with three LOWS Otshaits Ol SPineSa oi) <--)noiie > Genus Hoplopleura 23—First antennal segment with a short, stout spine at the distal post axial angle or on the posterior margin..... Brahe ere eee ne Eee Genus Neohematopinus (in part) HirstrantennalseomentsnotisOmms ayes ace ose als ol 24 24—Posterior margin of second abdominal tergite of male distinctly emarginate with a group of spines at each end of this emargination...Genus Neohematopinus (in part) Posterior margin of second abdominal tergite of male MOtthussemarcinat@arcr serie acres asses see se 25 25—Abdomen with distinct, chitinized tergal and sternal plates imsbothysexesiicesrrshs secre per sie. elois Genus Polyplax Abdomen without distinct, chitinized tergal and sternal plates in the female and with these absent or ex- tremely reduced in size in the male. .Genus Linognathoides Family Pediculide Leach, Zool. Misc., Vol. 3, p. 64 (1817) ; Giebel, Insecta Epi- zoa, p. 21 (1874) ; Piaget, Les Ped., pp. 615-618 (1880) ; Enderlein, Zool. Anz., Vol. 28, p. 136 (1904) ; Dalla Torre, Gen. Ins., Anopl., p. 8 (1908). Antenne five- or three- (obscurely five-) segmented. Eyes present, distinctly pigmented. Legs fitted for climbing, the tibiz with a thumb-like process opposing the claw. No pre- tarsal sclerite between tibia and tarsus. Parasitic upon man, apes, and monkeys. Subfamily Pediculine Enderlein, Zool. Anz., Vol. 28, pp. 136, 138 (1904); Dalla Torre, Gen. Jns., Anopl., p. 8 (1908). Antenne distinctly five-segmented. No pleural plates. 136 CALIFORNIA ACADEMY OF SCIENCES [Proc. 47H Ser: Genus Pediculus Linnzus Linnzus, Systema Nature, ed. 10, p. 610 (1758); Denny, Mon. Anopl., pp. 12-13 (1842); Giebel, Ins. Epizoa, pp. 27-30 (1874) ; Piaget, Les Ped., pp. 619-623 (1880) ; En- derlein, Zool. Anz., Vol. 28, pp. 136, 138 (1904). Head short. Legs all of approximately the same size. Ab- domen elongated. Spiracles small. Abdominal segments without lateral projections, and with numerous small spines. Type of the genus P. capitis De Geer. 1—Pediculus mjébergi, new name. From Afteleus sp.? (traveling menagerie, Europe). 1910. Pediculus affinis (not of Burmeister), Mjéberg, Ark. f. Zool., Vol. 6, pt. 13, pp. 169-171, f. 85. 2—Pediculus capitis De Geer. From man. Also recorded from Ateleus ater (locality unknown) and from Cebus fa- tuellus and Cebus sp. (Rio de Janeiro, S. America). 1758. Pediculus humanus Linnzus, Syst. Nature, 10th ed., p. 610. 1778. Pediculus humanus var. I, Linnzus, ibid., 12th ed., Vol. 2, p. 1016. 1778. Pediculus humanus var. capitis De Geer, Mem. Hist. Ins., Vol. 7, p. 67; pl. 1, f. 6. 1817. Pediculus cervicalis Leach, Zool. Misc., Vol. 3, p. 66. 1818. Pedicuius capitis Nitzsch, Germar’s Mag., Vol. 3, p. 305. 1842. Pediculus capitis Denny, Mon. Anopl., pp. 13- LG pli 26, f. 2. 1874. Pediculus capitis Giebel, Ins. Epizoa, pp. 30-32; pl. 1, f. 1-2. 1880. Pediculus capitis Piaget, Les Ped., pp. 619-623; pi 50} f. 2: 1912. Pediculus capitis Fahrenholz, Jahresb. d. Nie- dersach. Zool. Ver., pp. 2-12:t. f. 1, 3, 7, pl. 3, f. 3-4. 3—Pediculus consobrinus Piaget. From Ateleus paniscus (Museum Leyden). 1880. Pediculus consobrinus Piaget, Les. Ped., pp. 626-628; pl. 51, f. 4. Vou. VI FERRIS—ANOPLURA 137 1908. Pediculus consobrinus Dalla Torre, Gen. Ins. Anopl., p. 8. 1911. Pediculus consobrinus Neumann, Arch. de Par., Vol. 14, pp. 412-413. Note: This species is very doubtfully distinct from Pediculus capitis. 4—Pediculus corporis De Geer. From man. 1758. Pediculus humanus Linneus, Syst. Nat., 10th ed p: 610: 1766. Pediculus Valine var. 2 Linneus, ibid., 12th ed.;, Vol. 2, p: 10L6: 1778. Pediculus Younus var. corporis De Geer, Mem. Hist, Ins... Vol. 7,,;p.1673pleit, £.. 7. 1818. Pediculus vestimenti Nitzsch, Germar’s Mag., Vol.3}=ps, 305: 1842. Pediculus vestimenti Denny, Mon. Anopl., pp. 16183: pl 26; fy 0. 1874. Pediculus vestimenti Giebel, Ins. Epizoa, pp. 27-30; ple Ito. 1880. Pediculus vestimenti Piaget, Les. Ped., pp. 623- 625; plantas: 1908. Pediculus corporis Dalla Torre, Gen. Ins., Anopl., p. 8. 1911. Pediculus capitis var. vestimenti Neumann, Arch. de Par., Vol. 14, pp. 411-412. 1912. Pediculus corporis Fahrenholz, 2-3-4th Jahresb. d. Niedersach. Zool. Ver., pp. 2-12; f. 2; pl. 3, f. 1-2. 5—Pediculus lobatus Fahrenholz. From Ateleus pan (Berlin Museum). 1913. Pediculus lobatus Fahrenholz (without descrip- tion), Zool. Anz., Vol. 41, p. 373. 6—Pediculus oblongus Fahrenholz. From Hylobates concolor and Hylobates syndactylus. , 1913. Pediculus oblongus Fahrenholz (without de- scription), Zool. Anz., Vol. 41, p. 373. 7—Pediculus schaffi Fahrenholz. From Pan sp.? 1910. Pediculus schaffi Fahrenholz, Zool. Anz., Vol. SONps TAR 138 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. Genus Phthirus Leach Phthirus Leach, Edinburgh Encycl., Vol. 9, p. 77 (1815) ; Zool. Misc., Vol. 3, p. 64 (1817) ; Enderlein, Zool. Anz., Vol. 28, pp. 136, 138 (1904) ; Dalla Torre, Gen. Ins., Anopl., p. 9 (1908). Phithirius Burmeister, Handbuch der Entomologie, Vol. 2, p. 1 (1835); Denny, Mon. Anopl., pp. 8-9 (1842) ; Giebel, Ins. Epizoa, pp. 23-27; pl. 1, f. 8 (1874); Piaget, Les Ped., pp. 628-630; pl. 51, f. 5 (1880). Anterior legs much smaller and with much slenderer claws than the others. Abdomen short and broad, the fifth to eighth segments with conical lateral processes. Spiracles large, those of the first three abdominal segments crowded close together. 1—Phthirus pubis Linneus. From man. 1758. Pediculus pubis Linnzus, Syst. Nature, ed. 10, p. 611. 1817. Phthirus inguinalis Leach, Edinburgh Encycl., Vol 9, p..77. 1818. Pediculus tabescentium Alt. De Phthiriasi. 1842. Phthirius inguinalis Denny, Mon. Anopl., pp. 9-11; pl. 26, £. 3. 1874. Phthirius inguinalis Giebel, Ins. Epizoa, pp. 23- Zola. fe Os 1880. Phthirius inguinalis Piaget, Les Ped., pp. 628- 630% pl. 51, £. 5d: 1904. Phthirus pubis Enderlein, Zool. Anz., Vol. 28, p. 130. 1908. Phthirus pubis Dalla Torre, Gen. Ins., Anopl., p. 9. Subfamily Pedicinine Enderlein, Zool. Anz., Vol. 28, pp. 136, 138 (1904) ; Dalla Torre, Gen. Ins., Anopl., p. 9 (1908); Fahrenholz, Jahresb. d. Niedersach. Zool. Ver., pp. 28-29 (1912). Antenne three-segmented or obscurely five-segmented. Head more or less elongated. Abdomen with a single row of many very small spines on each segment. Pleural plates pres- ent on certain abdominal segments. Vor. VI] FERRIS—ANOPLURA 139 Note: The synonymy of the species in this subfamily has been dealt with by Fahrenholz and, although it is still far from clear, his conclusions have been adopted here. Genus Pedicinus Gervais Gervais, Aptéres, Vol. 3, p. 301; pl. 48, f. 1 (1844) ; Giebel, Ins. Epizoa, pp. 32-33 (1874) ; Piaget, Les Ped., pp. 630-632 (1880) ; Dalla Torre, Gen. Ins., Anopl., p. 9 (1908) ; Fahren- holz, 2-3-4th Jahresb. d. Niedersach. Zool. Ver., pp. 12-16 (19142). All legs with slender, pointed claws of nearly the same size. Abdomen with three pairs of pleural plates. Type of the genus Pedicinus eurygaster Piaget. 1—Pedicinus breviceps Piaget. From Lasiopyga mona. Also from Cercopithecus, sp., and Pithecus albibarbatus. 1880. Pedicinus breviceps Piaget, Les Ped., pp. 632- GSSmiple 2 ital 1910. Pedicinus breviceps Mjoberg, Ark. f. Zool., Vol. 6, pt 135ip. 172: 1912. Pedicinus breviceps Fahrenholz, 2-3 - 4th Jahresb. d. Niedersach. Zool. Ver., p. 16, 28. 2—Pedicinus eurygaster (Burmeister). From Pithecus nemes- trinus and Pithecus fascicularis? 1838. Pediculus eurygaster Burmeister, Gen. Insecto- rum. 1880. Pedicinus eurygaster Piaget, Les Ped., p. 630; plysily te 6: 1908. Pedicinus eurygaster Dalla Torre, Gen. Ins., Anopl., p. 9. 1912. Pedicinus eurygaster Fahrenholz, 2-3 - 4th Jahresb. d. Niedersach. Zool. Ver., pp. 12-15, 28. 3—Pedicinus hamadryas Mjoberg. Type from Papio sp.? (Zool. Mus. Hamburg). 1910. Pedicinus hamadryas Mjoberg, Ark. f. Zool., Vol. 6, pt. 13, pp. 172-174, f. 86-87. 4—Pedicinus longiceps Piaget. Type from Pygathrix cristata? Also from Pithecus fascicularis? 140 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4tH Ser. 1880. Pedicinus longiceps Piaget, Les Ped., p. 632; ple, oljeh 7. 1908. Pedicinus longiceps Dalla Torre, Gen. Ins., Anopl., p. 9. 1912. Pedicinus longiceps Fahrenholz, 2-3 - 4th Jahresb. d. Niedersach. Zool. Ver., pp. 15, 28. _Padicouns paralleliceps Mjoberg. From Pithecus albibar- batus (Zool. Mus. Hamburg). 1910. Pedicinus paralleliceps Mjoberg, Ark. f. Zool., Vol. 6, pt. 13, pp. 174-176, f. 88. 6—Pedicinus rhesi Fahrenholz. From Pithecus rhesus. 1912. Pedicinus rhesi Fahrenholz, Zool. Anz., Vol. 39, p. 54. 1912. Pedicinus rhesi Vahrenholz, 2-3-4th Jahresb. d. Niedersach. Zool. Ver., pp. 15-22; pl. 1, f. 4, Siaipl.3, 1:0 Genus Phthirpedicinus Fahrenholz Fahrenholz, Zool. Anz., Vol. 39, pp. 54-55 (1912), 2-3-4th Jahresb. d. Niedersach. Zool. Ver., pp. 22-23. Anterior legs with slender, pointed claw, others with short, blunt claws. Abdomen with two pairs of pleural plates. Type of the genus Phthirpedicinus micropilosus Fahren- holz. 1—Phthirpedicinus micropilosus Fahrenholz. From Pithecus rhesus. 1912. Phthirpedicinus micropilosus Fahrenholz, Zool. Anz., Vol. 39) an:5 sare Capra | Auc bee ei eecc. oar Gapringe: A con metscn raced ores Gatnivora: .Girm.ccse nik. soon tie Gephalophinzy gerienas scsi on Cephalophusa ie. cet. een sss Cercopithecus = Pithecus Gérvocaprinze 2 acne cesses Gervicapralys-ee-ereees ss nek enya dae te sete se isters ceeys ss tessa s Genvusi ane seen eos a Chinchillidws eee ee oe Citellus eee meer acces Gricetinse ee wclslcloeaen co ststivie sic Gricetulus) Gece ereaeeicscaes Gynomys we sect cree cciessceie Dasyimiys: acetate ate srk DicnOStomysypes seein ie siete PDipodidee a wecite eres els ere Dipodomys!, caeeeseeccss cc Dipus 3: kcisaueeeeeae eae Domestic Tabbiteae- ccc. oc DryomyS: Saceoormocscer cee Duplictdentatasteersniceela-i.ee HOST LIST 195 Blephantidey nase see eee 204 188 Pilephas) ystyoscsce ators ee ate oe 204 202 ESP UIMIVIS: |, eve) ateresateveeetteeteehars 194, 195 202 EQUUS So: yoicre cic oeieroieerenyeate 204 194 Buitamiasa.ccce ete cca eeee 192 188 195 Ferrets is aviycracaeuninie aires 186 196 ENSSIDedia), Manners sateen 186 Gazellat Wairrgec asco Sees 202 199 Gazelle. ou Giodean see ceee ere 202 200 Geomyidze:) 2 oe 2 sryer we cuere siete 194 201 Geomys, soeeestansneee a coe 194 Gerbillinze) 4h aeeaicnioee 195 Gerbillus "sa: sche seek cee 195 204 Girafitdae. .. sadecutaaoatsberceterste 201 204 Glaucomys!.w)coshaeee see 192, 193 202 Goat SCI OC OS CIENT CAO Cac ee OOS 203 203 Hamadryasy fiz20n cieestamerene 200 a FVEHOSCIIEUS: caeies cose eee eer 192 eteromiyt dae. (..-cicieisrcheleyetetere are 193 188 Eiolochilusy sc acctenrceeenos 196 201 Hominid ic .).2nn6' mecca 200 201 ROMO’ Scat eee 200 201 Flylobatesy 1. c/ys-cmepctemret crates 200 186 Hylobatide ...........00000 200 203 | Hyracoidea .......-..02.000+ 204 203 Hyrax = Procavia 186 149 Inuus = Simia 199 InSectivora® ii.1./sieisrstyettele ere 186 202 202 Lagidiumimpesssodoe ce eee 198 Lagurus = Microtus 202 Wasiopy Sal sacasece enema. see 199 202 Dasiopyeidcen saci aisles cass see 199 201 Lemmus = Dicrostonyx 201 Wepus) ga. saivc cece seen 187 198 TeimnOtragisS) tee cies oie vielelereisls 203 188 Roxodontal (1-22 enaaceestee ee 204 196 194 Macacus = Pithecus 190 Marmotagyc eta: ccetoecnteentrs 190 Merionesis-$228 emcee oes 195 195 Microdipodops .............. 193 196 Micromiys! ot oe saceeses ent 194 198 Microtine: oermse oeeemeeerer 196 193 Microtus 2.i\claseceiewscieeicenrs 196 198 Mins ASS aec se seers 194 188 Mus = Epimys 194 Mauscardinidae sie creeps eticisiecs 194 187 IMustelidcemn-hcee ee aaeeeroee 186 Vor. VI) Myoxidz = Muscardinide Myoxus = Dryomys Nectomys = Holochilus Neotomay shu esse neese. 196, 197 INGSONYZOMIYS ewan eelas one: 197 @ctodontidepeaqay. vases: 198 Odobzenidawey. went amen 186 OWdoheniusway eee 186 @docoileus eens cents, 201 @nyvchomyst series eee on 197 @rycteropodidzey ce Noa. 198 Orycteropus! S-eeesceca ce nicn. 198 Onyctolactsi Syaqnes anise: 187 @taritdzeh rans aeetoe iste ents 187 @tomyliney Ayee eee sees 195 Otomysp esse ase vcsier eens 195 (OS Ghisinnrd ab Bone Moana ao en 203 Rachyuromiyss Wises seve 195 Paludicola = Arvicola ara eereaysraei kere ce neete oa a ota ee 200 Pedetes ails tient cenes kerio 198 iRedetidzemmmta isa edn ents 198 Rerssodactylayanaceec cn ene 204 IB EKOGIP US: sehen accent 193 Rerognathus! yl swenec ciate 193 IRGromySGuSerscuaee eee 197 Retaunistidcy ser cco canes 192 Bhachochoerus “i... s.a0ce-s6 200 FeNeNaACOmMysy nc neytectnsisctersietie 196 Bhocatenirascc eee 187 BhocanctosMene she sactee: 187 Bhocideriera cits reas 187 Rinnipedianaaccdacee aocse ee 186 Pithecitsem, camoronser petra is 199 onside nena snvytan et le 200 Potamochoerus) assess ces. 201 FERRIS—ANOPLURA 213 Brimatesiprercsicrs va cerhers 199 Rraboscidéaw ia scene 204 ES OCAV IAN eer a cteaarcicrcraarers 204 Brocavitdewesshiteee een 204 Pteromys = Glaucomys By a thtixce c)- erctaicte clad orclote els 199 VAM OEE Tees idle arc PN eee 201 Ra Di Eee daterahetetelcatarnaslar stators 188 Gal Om blaiinscesscccs snarsters sig tere 187 ARUP IGap Tayi eys)s c/s; s0ereal esas 203 RGD ICA FUME esta) ei -\jcheteley eects iets 203 SaccoOstomlusm sete sceect cee 195 Se alltiecn eee cat cares tvstiletarat tye 187 Seehunde ....... Win cevvarcarae 187 Suldeepeineac is ccdarascc te dsuenayse 200 SUSpe ara vase sce iis cyetatesvecetanions eve 201 Symphalaneus: Sachse seeeces es: 200 Mal prdze grees as wet seth eee 186 GD eunTAT ASH ertetanoenatcres tayaloneitetacrorehe 191 PRAUTOLEAGUS ceca. spals's mrarsiatcrene 203 MD TY ONOMYS! «cs cedcaea vines 198 Trachypithecus = Pygathrix Mragelaphinze! 537.85 tisccece 203 siubilidentatay <5 ).-.csscijyncetee 198 Wnknownhost . os... eos eces 204 Uncertain Muride .......... 198 Wncertain) Primates ......... 200 PGTAMCE Was leone aearetelore sta staraye 192 Xerospermophilus .......... 190 DCSE BIG, sey Nie EO ERS 192 PROCEEDINGS OF THE CALIFORNIA ACADEMY OF SCIENCES FourTH SERIES Vor. VIF _Noii7, pp: 2l5=221 May 12, 1916 Vil FOUR SPECIES OF SALAMANDERS NEW TO THE STATE OF CALIFORNIA, WITH A DESCRIPTION OF PLETHODON ELONGATUS, A NEW SPECIES, AND NOTES ON OTHER SALAMANDERS BY Joun Van DENBURGH Curator, Department of Herpetology In recent years the Academy has received specimens of four species of salamanders which seem never to have been collected previously in California. Three of these have been known from examples secured in Oregon or Washington; the fourth species appears never to have been described. In recording these facts opportunity is taken to publish certain other notes regarding California salamanders. 1. Ambystoma macrodactylum Baird. Three specimens (Nos. 39656, 39657, 39658) collected by Dr. E. C. Van Dyke in July, 1915, near Fallen Leaf Lake, El Dorado County, California, add a species to the known fauna of the State. They seem to differ in no respect from others collected in Washington. May 12, 1916 216 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. 2. Chondrotus paroticus Baird. I have not been able to find any previous record of the oc- currence of this salamander in California. It is represented in our collection by a typical specimen (No. 29108) found by Mr. J. R. Slevin in wet earth under a stump near Requa, Del Norte County, California, May 22-26, 1911. 3. Autodax ferreus Cope. This salamander has been known only from the type speci- men (U. S. N. M. No. 6794) collected by Dr. Vollen at Fort Umpqua, Oregon. We have specimens from Elmira and Marshfield, Oregon, and from Bayne Island, British Columbia, as well as from Requa, Del Norte County; Alton, Trinidad, and Carlotta, Humboldt County; and Comptche, Mendocino County, California. Our two Requa examples (Nos. 29099 and 29102) were found by Mr. Slevin, May 22-26, 1911. They were taken from the rotten wood of a dead tree in which they were living some 20 feet above the ground. This species is related to Autodax lugubris, but is quite distinct. 4. Plethodon elongatus, new species. Diagnosis—Similar in general appearance to Plethodon vandykei and Plethodon intermedius, but somewhat stouter ; costal grooves 16; toes and fingers not webbed ; adpressed limbs separated by 6 or 7 costal interspaces; tail cylindro-conic, con- siderably compressed in distal third; paratoid not developed; a dorsal band as in P. intermedius, but obscured by the general duskiness of coloration; lower surfaces blackish brown, relieved with whitish dots. Type—Cal. Acad. Sci. No. 29096, Requa, Del Norte County, California, J. R. Slevin, May 22-26, 1911. Material—Four specimens (Nos. 29094, 29095, 29096 and 29101) from Requa, all collected at the same time. Description of the type—General form similar to P. inter- medius, but with body, iimbs and tail somewhat stouter; tail cylindro-conic, compressed laterally in posterior half, nearly equal to length of head and body, with strong vertical grooves Vor. VI) VAN DENBURGH—CALIFORNIA SALAMANDERS 217 nearly to tip; head somewhat depressed, about width of widest part of body; snout rounded from above and in profile; eyes moderate, separated anteriorly by about one and one-half times the length of the orbital slit; nostrils small, separated by about their distance from pupil; subnasal groove descending nearly to margin of lip; line of lip curved downward from below eye to end of snout; palatine teeth in two slightly curved series beginning just behind the internal nares, converging obliquely backward, and separated on the median line by a space greater than the diameter of the internal nares; parasphenoid teeth in one patch throughout, separated from the palatine teeth by an interval equal to distance from nostril to edge of lip; inter- nal nares small; tongue large, ovate, not emarginate, attached along median line but free laterally and, for a short distance, behind; neck a little narrower than body, no paratoid gland, gular fold continued up and then forward as a groove to eye; a groove along vertebral line from head to tail; costal grooves between limbs 16, not continued to midline either above or be- low; limbs a little stouter than in P. intermedius, and with shorter digits, anterior with four and posterior with five digits; digits rather short, with rounded ends, each with a small ter- minal pad, inner shortest, third longest, second finger longer than fourth, second toe shorter than fifth, third and fourth toes nearly equal, broadly palmate, but no web; adpressed limbs separated by about six costal folds. The coloration is similar to that of P. intermedius, but heav- ily clouded with black. The general color is blackish brown above and below; a broad, lighter brown, black-edged, dorsal band extending from snout to base of tail; lower surfaces sprinkled with small whitish dots, which become larger on the sides, gular region and chin. Measurements MM. SnoutstOramusy sy aasatac sia oie ae eRe tee cueladess Blala. @ austere 59 Bront/otianus, tovendiortailiectasc site nis. orc ace one ale tee 58 Wit thio fiheadiavs peeps aes ep sete beten ose caersse oh orerapeeloiaus 7.5 INOSERIRCOKOT Iter mete ceereroterearker eter Raweuncewolis ig, seve elcome tacene 125 SnOUtetOmOnbit wae: BS Genet cusanessretetsteneeha ec ists 6 aus.overeesats 3 Snouttorular foldl. se cto sche inalrede Pees oe! « Wels shale wie 11 Snoutrto toreslinibspcrcsd certs Parsee cna a gaiae ae at 218 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH Ser. Gular fold to anus it. Sa%0s 0 he's wis win a awioie Sane eles 38 Axilla MORO eine miisce 6 chet s eidveic.s ste'> mpue ania sueumyeras 30 Adpressed ‘limbs*separated ‘by... 2.1.5 she wes wom creiniers ot 11 Fore dlinib 4 Sctorek woe dara deka b wile alone eee eee 9 Edn) Witrtb W neater. eave sic dacs oe ae nb ne Cems tine 10.5 Heelto endioitongest toe... fists cu nies acleamomadte 5 BreadtinwOrstootsi sn Ghai. co a's, cnc etwisterdtenaustcielen oinliedsen eatetes 3.5 Variation—The three adult specimens are identical in struc- tural characters and coloration. No. 29101 is a young sala- mander measuring 28mm. from snout to anal opening, with a tail 14mm. long. It is like the three adults in the number of its costal folds and general coloration, except that the dorsal band is bright pink clouded on the head and along the mid- dorsal line with dark brown. This brightly colored band ex- tends from the snout, along the back, nearly half way down the tail. This specimen looks very much like P. intermedius, but the lower surfaces are darker. Remarks—While this new species is manifestly closely re- lated to Plethodon intermedius and P. vandykei, it can easily be distinguished from both by the greater number of its costal grooves and the greater space between its adpressed limbs. The number of costal grooves is 16 in all four specimens of the new species, while in Plethodon vandykei these grooves are 12 and 13, and in P. intermedius they are 13 or 14. Plethodon intermedius is of more slender build, with longer toes, more truncate snout, and less dusky coloration. The paratoid gland and webbed feet of P. vandyket are characters which should render its recognition easy. 5. Plethodon intermedius Baird. This salamander was originally described from one speci- men said to have been secured by John Xantus while stationed at Fort Tejon, California. So far as I know, with the ex- ception of the type of Plethodon crassulus, this species has never since been found in California, although it is common in western Oregon and Washington. I have felt that the type could not have been collected by Xantus near Fort Tejon, but must have been so recorded through some error. With this VoL. VI] VAN DENBURGH—CALIFORNIA SALAMANDERS 219 in mind I wrote to Dr. Stejneger to inquire whether the rec- ords of the National Museum would throw any light on the matter. He has very kindly investigated these records and writes that “there seems originally to have been some trouble with the series of entries to which these belong, as apparently by some mistake two collections were given the same numbers. The locality Ft. Tejon looks to me exceedingly dubious, though, of course, it does not mean only the immediate neigh- borhood of the old fort.” A copy of the old record is printed here under that of Plethodon croceater; see remarks under head of that species. Seventy specimens of Plethodon intermedius from Oregon and Washington show costal grooves as follows: Specimens Costal grooves Oe ar oie eh version aby sgh enaranes saey nash dor wise 69s 13-13 Sen Ne SIR: ERE WGA Re Oe ten ee 13-14 Festi Nae a An SY 14-14 70 6. Plethodon crassulus Cope. The question of the identity of this salamander was raised by the comparison of Plethodon intermedius and Plethodon elongatus. Plethodon crassulus was described in 1886 by Cope from one specimen in the U. S. National Museum, and was said to have been collected in California by Dr. J. G. Cooper. Cope says that “this species has a superficial resemblance to the P. oregonensis, but its manifold differences are easily per- ceived.” He also states that the form is quite robust, but his cuts show a salamander similar in size and proportions to P. intermedius, and his description fits that species in every detail, for some specimens of P. intermedius show the dorsal band very indistinctly. The type of P. crassulus is No. 9447 of the National Museum collection. In response to my request for information regarding it Dr. Stejneger has very kindly written me as follows: “The record of 9447 is dated November 20, 1877, is in an unknown hand, and is blank as far as name is concerned. Locality is given as California, collector as Dr. Cooper. You 220 CALIFORNIA ACADEMY OF SCIENCES . (Proc. 47H Ser. ask what I think of P. crassulus. I have given the question some thovght and I am of the opinion that it is a uniform color phase holding the same relation to P. intermedius (with which the type agrees structurally and not with P. oregonensis) as P. cinereus does to P. erythronoius.” P. crassulus may, therefore, be regarded as a synonym of P. intermedius. I think one is justified in doubting that the original specimen really was collected in California. 7. Plethodon croceater Cope. This salamander also was described from a single specimen said to have been sent to the National Museum by John Xantus from Fort Tejon, California. This specimen was No. 4701 of the National collection. It seems to have been lost, for Dr. Stejneger writes me that it has not been on the shelves in his time. As in the case of P. intermedius, “there seems orig- inally to have been some trouble with the series of entries to which these belong, as apparently by some mistake two collec- tions were given the same numbers. First there is an entry in an unknown hand in black ink and under there is an entry in Prof. Baird’s handwriting thus: “4701 Rana Chiloweyush Dr. C. B. Kennerly Heredea Fort Tejon —1— Xantus “4732 Scotophis gutatus | Micanopy, Fila. Dr. Bean - occidentalis Ft. Tejon Xantus “The ditto mark [under Scotophis] refers to the line above, which is Plethodon, and this Plethodon, No. 4731, is a Pletho- don cinereus from Detroit, Dr. Sager.” It is evident that the locality Ft. Tejon is “exceedingly du- bious.” Plethodon occidentalis is evidently a manuscript name for P. intermedius. Cope has recorded Plethodon croceater from Cape San Lucas, Lower California, and San Diego, California, both of which localities need confirmation. The former locality may have resulted from the association of the original specimen with John Xantus, who collected both at Cape San Lucas and Vor. VI] VAN DENBURGH—CALIFORNIA SALAMANDERS 221 Fort Tejon. The latter, probably refers to a specimen recorded by Mr. Lockington (Am. Nat. XIV, 1880, p. 295) as having been taken in Lower California 75 miles southeast of San Diego. I have seen a number of specimens from the Sierra Ne- vada. The ground color varies from light brown to nearly black, and the yellow spots vary greatly in size and arrange- ment. 8. Plethodon flavipunctatus Strauch. I have no doubt that this is the same species as Cope’s Pleth- odon croceater, with which the description agrees. 9. Triton ensatus Eschscholtz. Eschscholtz evidently had the species which Baird and Girard later described as Amblystoma tcnebrosum, and which Cope referred to his genus Chondrotus. Dicamptodon Strauch is an older term than Chondrotus. Those who prefer to re- move the species from the genus Ambystoma may use the name Dicamptodon ensatus (Eschscholtz). 4 PROCEEDINGS OF THE CALIFORNIA ACADEMY OF SCIENCES FourtH SERIES Vor. VI, Nos. 8 and 9, pp. 223-294, pls. 3-17. June 23, 1917 VIII REPORT OF THE PRESIDENT OF THE ACADEMY FOR THE YEAR 1916 BY C. E. Grunsky President of the Academy In view of the fact that the work of the California Academy of Sciences, its purposes and aims, were rather fully set forth in the various addresses delivered at the dedication of its Mu- seum Building in Golden Gate Park last September, this annual report will be brief and devoted in the main to a summarization ot such facts and events as seem worthy of special mention. No special effort has been put forth during the last year to swell the Academy’s membership list. The accession of new members has nevertheless a little more than offset the losses by death and resignation. The present membership in the Academy is 483, made up of: PAGO Sere tetera eee VAR Tce 2 sna cba 5 Honorary Membersics scree ool neo iedisineie walalahae ate 26 eifevMembersieer con eerie rem COE ee te tes cokes 83 Members) h receyotocic cc yals eee ee italaceizciaveige eaibeiee 369 During the year 1916 there was an accession of 33 new members, and the Academy lost by death 5, by resignation 11, and by being dropped for arrearages in dues 6; leaving a net gain in membership of 11. June 23, 1917 224 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH Srr. The losses by death were: Davise Mir TWoracesen-aseee ae Wife Member’. cc seees terests che July 12, 1916 Gutzkow, Mr. Frederick....... Life Member ................. May 7, 1916 Leszynsky, Mr. S.L............ Members: seuccca:atave ce boaeree March 8, 1916 Sclater, Dr. Philip Lutley..... Honorary Member ............ , 1916 Trask, Mrs. Blanche ......... Life Member ...:.......05-50- Nov. 11, 1916 The Academy carries on its list of patrons the following names : Alvord, William Bourn, William B. Crocker, Charles Crocker, William H. Hendrie, John W. Dunne, Peter F. Lick, James Grant, Joseph D. Hosmer, Mrs. Charlotte Morrison, Alexander F. Of these the last six are the surviving members. Two other public spirited citizens, Mr. Herbert Fleishhacker and Mr. A King Macomber, have recently very generously offered to in- stal large habitat groups in the Museum, whereby they will be- come patrons. LECTURES During the year 1916, 11 free lectures have been delivered at the stated meetings of the Academy, as follows: January 19. “Bird and Animal Life of the Yosemite Region.” Tracy I. Storer, Assistant Curator of Birds, Museum of Vertebrate Zoology, University of California. Marcu 15. “The Gulls in and about San Francisco.” Joseph Mailliard. ApriL 19. “Bird Life as seen through a Camera.” Dr. J. Rollin Slonaker, Professor of Physiology, Stanford University. May 17. “The Relation of our Salmon and Trout to Forest Con- servation.” N. B. Scofield, Expert in charge of the Department of Commercial Fisheries, California State Fish and Game Commission. June 21. “Game Conditions in Great Britain vs. Conditions in Cali- fornia.” Carl Westerfeld, California Fish and Game Commis- sioner. Jury 19. “Horticultural Quarantine.” Frederick Maskew, Chief Deputy Quarantine Officer of the California State Horticultural Commission. Avucust 16. “A Naturalist in the Bahama Islands.” Dr. Charles Lincoln Edwards, Director of the Los An- geles Zoological Park and Aquarium. SEPTEMBER 20. “The Fur Seals and other animals of the Pribilof Islands.” George A. Clark, Academic Secretary of Stanford University. Ocroser 18. “The Physiographic History of the Southern Sierra and Mojave Desert Regions.” Dr. John P. Buwalda, Instructor in Geography, Uni- versity of California. Vor. VI] GRUNSKY—PRESIDENT’S REPORT FOR 1916 225 NoveMBer 15. “Japanese Pearl Fisheries.” ' Prof. 'C. A. Kofoid, Department of Zoology, University of California. DeceMBeER 20. “The California Pocket Gopher as a Useful Animal.” Dr. Joseph Grinnell, Director of the Museum of Ver- tebrate Zoology, University of California. In addition, Sunday afternoon lectures are being delivered in the Museum building, since October. The list for 1916 em- braces the following : Ocrtoser 22. “Picturesque India.” ; Dr. Walter K. Fisher, Stanford University. Octoser 29. “To the Tip-top of the United States in Quest of the Golden Trout.” : Dr. Barton W. Evermann, Director of the Museum. November 5. “A Trip to the Southern Sierra Nevada and the Cafion of the Kern.” Dr. Roy E. Dickerson, Assistant Curator of Paleon- tology. Novemser 12. “The Argentine Ant; a Pest from South America.” Prof. C. A. Woodworth, Department of Agriculture, University of California. NovemBer 19. “Ups and Downs of the Pacific Coast.” Prof. R. S. Holway, Department of Geography, Uni- versity of California. NoveMBer 26. “Some Common California Mammals.” Dr. Joseph Grinnell, Director of the Museum of Ver- tebrate Zoology, University of ‘California. DeceMBER 3. “Injurious Insects.” Prof. E. A. Essig, Department of Agriculture, Uni- versity of California. Decemper 10. “Turtles of the Galapagos Islands.” Dr. John Van Denburgh, Curator of the Department of Herpetology, California Academy of Sciences. ACCESSIONS TO THE MUSEUM AND LIBRARY Among the notable donations with which the Academy’s col- lections of material and of books have been enriched during 1916, the following may be noted : Argentine Government, through Hon. Enrique M. Nelson, Commissioner- General, Panama-Pacific International Exposition: Thirty-nine speci- mens of mounted Argentine birds; eight mounted specimens of native mammals; 10 boxes of exhibits of native insects; 10 framed colored drawings of Argentine plants; one stereoscope and 37 slides; exhibit illustrating water filtration; specimens of Argentine plants. Branner, Dr. John C., Stanford University: 55 bound volumes. California Botanical Club, through Miss Alice Eastwood: A collection of 397 specimens of Mexican plants collected by Dr. Edward Palmer in 1910, purchased for $39.80 by the Club. Crocker, Mr. William H.: Three large folios, “Japanese Temples and their Treasures.” 226 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH Ser. Evermann, Dr. Barton W.: Ten manganese nodules dredged by the U. S. Fish Commission Steamer Albatross in the South Pacific during the Agassiz-Albatross South Pacific Expedition of 1899-1900, and a col- lection of garnets from St. George Island, Pribilof Group. Grant, Mr. J. D.: One buffalo skull from the Klamath River. Heyer, Mrs. H. C., San Francisco: Sixty-one specimens of Alaska birds, chiefly water birds. Kelly, Mr. James H., Tiburon, Cal.: Twenty-one numbers of the earlier publications of the Academy. Logan, Mr. Hugh B. Baker, Ore., through Mr. John W. Mailliard: One skin of the Mountain Coyote (Canis latrans lestes), male, from North Powder, Baker Co., Oregon, and one skin of the Pallid Barred Wildcat (Lynx fasciatus pallescens), male, from Salisbury, Baker Co., Oregon, both collected by the donor. Martin, Mr. Bruce: 627 insects collected in Colombia, South America, in- cluding some very interesting forms. Mailliard, Mr. John W.: Two specimens of the California Condor (Gym- nogyps californianus), collected in San Diego Co., California, by E. B. Towne. Merriam, Dr. C. Hart, Washington, D. C.: A collection of 486 specimens of Atlantic coast mosses, comprising 65 genera and 181 species, all new to the herbarium. Smith, Mr. L. E., Sisson, Cal.: One hundred and forty-nine bound volumes. Snodgrass, Mr. R. E.: Seventeen volumes and 13 pamphlets, concerning the Galapagos Islands. Tobin, Mr. J. S.: Cash donation, $250. U. S. Fisheries Steamer “Albatross”: Twenty-one bird skins; 181 jars, vials and bottles of specimens of fishes, sponges, molluscs, crustaceans, etc. PUBLICATIONS The Academy has published during 1916 the following papers in continuation of the Fourth Series of the Proceedings : Vol. V, No. 7, pp. 195-201 REPORT OF THE PRESIDENT OF THE ACADEMY FOR THE YEAR 1915 by C. E. Grunsky, President of the Academy. Vol. V, No. 8, pp. 202-223 REPORT OF THE DIRECTOR OF THE MUSEUM FOR THE YEAR 1915 by Barton Warren Evermann, Director of the Museum. Vol. VI, No. 1, pp. 1-17 Eocene oF Lower Cow itz River VALLEY, WASHINGTON by Charles E. Weaver. Vol. VI, No. 2, pp. 19-40 Tue Post-EocENE ForRMATIONS OF WESTERN WASHINGTON by Charles E. Weaver. Vol. VI, No. 3, pp. 41-52 Tue OLIGocENE oF Kitsap County, WASHINGTON by Charles E. Weaver. Vol. VI, No. 4, pp. 53-85 Tue Paciric Coast Races oF THE BEWICK WREN by Harry S. Swarth. Vol. VI, No. 5, pp. 87-128 MonocrapPH OF THE NorTH AMERICAN SPECIES OF ORTHOTYLUS (HEMIP- ) by Edward P. Van Duzee. Vor. VI) GRUNSK Y—PRESIDENT’S REPORT FOR 1916 227 Vol. VI, No. 6, pp. 129-213 A CATALOGUE AND Host List or THE ANOPLURA by G. F. Ferris. Vol. VI, No. 7, pp. 215-221 Four SPEcIES OF SALAMANDERS NEW TO THE STATE OF CALIFORNIA, WITH A DESCRIPTION OF PLETHODON ELONGATUS, A NEW SPECIES, AND NOTES ON OTHER SALAMANDERS. by John Van Denburgh. Title pages and Indices for Fourth Series, Proceedings, Vol- umes IV and V, have also been printed but have not yet been distributed. The notable event in the affairs of the Academy which marks the beginning of a new epoch in its history, was the dedication on September 22, 1916, of the new Museum building in Golden Gate Park, with a first view by members and their friends of the habitat groups of which, at that time, 11 principal groups and a number of lesser groups had been completed. The ex- ercises on that occasion have been made a matter of record and I desire at this time only to renew the assurance to those who have made so much accomplishment possible of the sincere ap- preciation by all members of the Academy of the generosity and good will which has found such happy expression in this build- ing and its contents. Of the 11 principal groups the three bird groups were made possible by special donations as follows: The Farallon Bird Group, by Mr. Wm. H. Crocker. The San Joaquin Valley Bird Group, by Mr. Jos. D. Grant. The Desert Bird Group, by Mr. Wm. B. Bourn. I may note in connection with the installation of habitat groups that the Academy no longer commands the services of Mr. John Rowley, under whose supervision the habitat groups have been installed. Mr. Rowley has gone to the Municipal Museum of Oakland. I cannot refrain from commending again the results of Mr. Rowley’s work. The groups which have been installed portray nature, and especially the various animals therein presented, with remarkable fidelity. The general arrangement and effect of each group is pleasing and all will bear the closest inspection. The fact that Mr. Rowley will be active in such close prox- imity to San Francisco as Oakland, prompts the hope that for special work as occasion arises his services will still be available. 228 CALIFORNIA ACADEMY OF SCIENCES [Proc. 47H Ser. The Academy has been fortunate in securing the services of Mr. E. P. Van Duzee as Curator in the Department of Ento- mology and as active Librarian. The proper housing of the Library and the attention which it is now receiving have added greatly to its usefulness. In the other departments of the Academy’s work there has been no material change. What has been done in these various departments will be set forth by the several curators and it would be but repetition to dwell upon their activities in this general statement of affairs. The Director of the Museum, Dr. Evermann, will report in some detail upon the Museum and research work which has been accomplished and of the cordial appreciation which the public is manifesting in the Academy’s work. In order to make possible what has thus far been done on and in the museum building, the Academy has had to live beyond its income for several years. It has been necessary to add to our indebtedness about $35,000. This is not a serious matter but is cited as an evidence of the efforts of your Trustees and Officers to make the collected scientific material available for examina- tion and study at the earliest possible date. The estimated assets of the Academy are about $1,400,000, mainly represented by the Market Street property, against which there are liabilities of about $336,000. The net annual income may be stated in round numbers at about $50,000. It is expected that of this amount about $10,000 per annum can during the next few years be held available for reducing our financial obligations. There is not yet any prospect for the enlargement of the museum building, which would only be possible by outside aid. The space which has thus far been made available is, of course, inadequate to meet prospective requirements. All friends of the Academy should, therefore, as opportunity offers, call the attention of those who are financially able, to the good work which an ample additional endowment would make possible. In closing, I desire to express on behalf of the officers of the Academy their appreciation of the interest manifested by the members, and desire also to extend my personal thanks to the officers and members for their cordial support and also to the employees who have so willingly made sacrifices in the interest of the Academy whenever called upon to do so. IX REPORT OF THE DIRECTOR OF THE MUSEUM FOR THE YEAR 1916 BY Barton WARREN EvERMANN Director of the Museum At the time of the last annual report of the Director of the Museum (February 16, 1916), the actual installation of the habitat groups of California mammals and birds was well under way. Besides the regular employees of the Division of Exhibits, who devoted all their time to the habitat groups, three extra temporary men were employed on that work for nearly a year. By the twenty-first of September the following groups had been completed : California Valley Elk, Black-tail Deer (summer group), Northern Mule Deer (winter group), Antelope, Desert Moun- tain Sheep, Mountain Lion, Black Bear, Leopard Seal, Cali- fornia Sea Lion, Steller’s Sea Lion, Raccoon and Striped Skunk, Coyote, Farallon Islands Bird Rookery, San Joaquin Valley Spring Bird Group, and Desert Bird Group. Oppor- tunity has been taken to reproduce in this report excellent photographic illustrations of a number of these habitat groups. In addition to these 15 groups the California Condor Group was complete with the exception of the birds, which will be se- cured later. Small groups of the California Valley Quail and the Western Meadowlark were also completed. It was felt that the time had arrived for the dedication of the Museum building and the opening of the Museum to the public. The formal dedicatory exercises were held on Friday afternoon, September 22, in the California mammal room of the Museum. Mr. C. E. Grunsky, the President of the Academy, pre- sided. The invocation was by the Right Reverend William Ford Nichols, bishop of California. Brief addresses were 1A report of the opening exercises was published in Science for October 27, 1916, pp. 598-603. 230 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. made by the following: Mr. William H. Crocker, President of the Board of Trustees; Mr. C. E. Grunsky, President of the Academy; Mr. Edward Rainey, for the Mayor; Mr. George Haviland Barron, Curator of the Memorial Museum, San Francisco, for the Board of Park Commissioners; Dr. David Starr Jordan, Chancellor Emeritus, Stanford University; Dr. Barton Warren Evermann, Director of the Museum. Mr. Crocker spoke feelingly of his long connection with the Academy, as President of the Board of Trustees continuously since 1898, or 18 years. Before him his brother, Charles F. Crocker, had occupied the same position for a number of years and his father, Charles Crocker, was deeply interested in the Academy. As president of the Board of Trustees, Mr. Crocker formally dedicated the new Museum building to the advancement of the biological and physical sciences and the educational interests of the city of San Francisco and the state of California. He then turned the building over to the Academy. Speaking of the history and the aims and ambitions of the Academy, President Grunsky said, in part: Organized in 1853, the California Academy of Sciences has now for 63 years been conducted along broad lines for public service. Membership in the Academy at a nominal annual fee is open to all who are interested in the study or advancement of science. Its activities are directed mainly along educational lines in providing the material and opportunity for secur- ing information on matters pertaining to the natural sciences; and second, along lines of research and study in the various subdivisions of the natural sciences. There are those present today who will recall, and some who were active in, the activities of the Academy while it was quartered in a building at the southwest corner of California and Dupont streets, and there are many here who have enjoyed and who have profited by the natural history museum and its accessories maintained for many years prior to the great disaster of 1906 on Market between Fourth and Fifth streets. It would be needless to present at this time a review of the history of the Academy and of the work done by it. Those who desire will find much of interest and of value in the published records of the Academy’s Pro- ceedings. It would be futile to give a due meed of credit to those heretofore con- nected with the work of the Academy whose contributions have borne fruit, and whose achievement is expressed in some measure in the Museum plant now to be brought closer to the general public. It must suffice to say that at all times in the history of the Academy there was a group of Vor. VI] EVERMANN—DIRECTOR’S REPORT FOR 1916 231 enthusiastic scientific workers—with changing personnel—who stood ever ready to make, and did make, the sacrifices and put forth the personal effort which made the work of the Academy worth while. In the matter of publications, as in the case of its other activities, the Academy has had to accept the limitation upon its output made necessary by the lack of adequate funds. Much has been left undone which ought to be done. Time will not, however, permit me to take up this matter for full presentation. Let me call attention merely to one fact which will be patent to all who look carefully into the affairs of the Academy. The field in which the Academy is active is but imperfectly covered; nor can it be covered as it should be without adequate support from those of means who, in furthering the aims of the Academy, will not alone be benefiting our city and commonwealth, but will be contributing to the sum of human knowledge. . The building which has here been erected and is today being dedicated is located upon public ground. The Academy has invested in it $183,000. Yet this building, while it is an earnest of what the Academy is willing to do for the public, represents, in area occupied, only about one-third of that of the museum building which we hope some day in the near future will be completed on this site. To accomplish the incomplete work with which we desire you to become better acquainted, the Academy has taxed its resources as far as seemed wise and has made it possible to open to the public, housed in the first unit of its museum building, certain exhibits which will forecast what it is hoped may ultimately be adequately accomplished. There should be here assembled material from the Pacific Ocean and its shores representative of all the natural sciences, more complete than can be found elsewhere. It can be done and will be done, but not without outside aid. The resources of the Academy, chiefly the result of bequests and endowments that will be referred to later, are limited and our installations and facilities for housing material always obtainable in abundance must progress slowly unless the Academy can count on the generous assistance of those who have the means. We can not at this time announce when our building will be extended. More material for research and exhibition has already been collected than we can properly display. Some of the most striking habitat groups that should be at once installed must wait until more funds are provided and in some cases until the time has come when we can add to the building. It has been suggested that the Academy should extend its activities by assuming the management of an aquarium. I think I speak for every mem- ber when I say that the Academy is ready to do this. But even though there are those of our citizens who may be willing to erect and equip the necessary buildings the Academy is not so circumstanced that it can provide the funds for maintenance and operation. But its staff and its or- ganization including the services of its Director of the Museum, Dr. Ever- mann, an expert in matters relating to fishes and the fisheries, are ready to help and will help. San Francisco should have an aquarium filled with 252 CALIFORNIA ACADEMY OF SCIENCES [Proc. 47H Ser. the life of the Pacific Ocean and of the streams discharging into the ocean, second to no other aquarium in the world. The Academy has asked you to be present today at this dedication of the first unit of its museum building in order that you may become better acquainted with the Academy’s aims and purposes and as a reminder to the public that the Academy is here to benefit and serve the whole community. It is appropriate that at this time attention be called to the generous aid which the Academy has received in the past and to that which it is now receiving in its plans for an enlarged field of usefulness. It should be remembered that the Academy is in Golden Gate Park with the consent of the people of San Francisco, who have seen fit to increase the Academy’s opportunity for service by permitting the erection here of the necessary museum buildings. This consent was given in 1910 and ever since that time the plans have been under consideration and in execution which are today beginning to see fulfillment. By bequest of James Lick forty-one years ago, the Academy became the owner of the Market Street property between Fourth and Fifth streets on which for many years a museum of natural history was maintained. This property, now in use for business purposes, is the Academy’s present main source of income. The Lick bequest is now carried on the books as an asset of $802,000. In 1881 the Academy received from Mr. Charles Crocker an endowment of $20,000, the income from which is to be used in aid of scientific research. Mr. John W. Hendrie in 1899 bequeathed to the Academy the sum of $10,000, the income from which has been set apart for the publication of scientific papers. The late William Alvord bequeathed to the Academy the sum of $5,000, to be used in improving and adding to its herbarium. During the last decade, while husbanding its resources, and collecting the material which is now assembled in the building being dedicated today, the Academy affairs have necessarily received but little publicity and there has been but little opportunity for the public to become acquainted with its activities ; nevertheless, the Academy has been selected by many who have collected material of scientific value as the proper institution to preserve the same and make it available for the public. Attention will be called to only a few recent donations the announcement of which is appropriate on this occasion. Our generous public-spirited fellow citizen, William M. Fitzhugh, has, by purchase and additions thereto, preserved in its entirety the collection of Indian baskets, ornaments, implements and related material made in their lifetime by the late Professor and Mrs. T. S. C. Lowe, of Pasadena. This collection of exceptional interest and magnitude, which would other- wise have been scattered and would have lost value by piecemeal sale, is on display in the Academy Museum as a loan and merits your careful atten- tion. The most important gift which the Academy has recently received is that of the Henry Hemphill collection of marine, freshwater and land shells. This magnificent collection, the making of which engaged the attention of Vor. VI] EVERMANN—DIRECTOR’S REPORT FOR 1916 233 Mr. Hemphill during practically all the years of his long and useful life, and which contains between 60,000 and 70,000 specimens representing more than 12,000 species, has been donated to the Academy by Mrs. Charlotte Hosmer, daughter of Mr. Hemphill. The Academy feels grateful to Mrs. Hosmer for this most generous gift. The installation of the bird-habitat groups which are today being opened to your inspection and which will contribute much to the education and enjoyment of the public has been made possible by the liberality of three other San Franciscans as follows: Mr. Wm. H. Crocker has presented to the Academy the Farallon Islands bird group. Mr. J. D. Grant has presented to the Academy the San Joaquin Valley bird group. Mr. W. B. Bourn has presented to the Academy the Desert bird group. It is their wish, as it is the wish of every one in any way connected with Academy activities, that these exhibits, and the others, now to be opened to public view, may prove instructive and inspiring and a source of lasting enjoyment to all of those who care to avail themselves of the privilege, open to all, of visiting the museum. To these donors and to all who have contributed to the service value of the Academy, the Academy, through its President, expresses its sincere appreciation and gratitude. The Academy welcomes such aid in the accomplishment of its aims and will ever be ready to accept and manage any trust having in view the ad- vancement of science. Mr. Rainey, representing the Mayor, and Mr. Barron on be- half of the Board of Park Commissioners, spoke of the great benefit which the Museum of the California Academy of Sciences will be to the people of San Francisco. The location of the Museum in Golden Gate Park, the most beautiful “peo- ple’s playground” in the world, is a guarantee that it will be visited not only by our own people, but by all who come to San Francisco. Dr. Jordan spoke of the value to general education and to science of natural-history museums. He called attention to the eminent position already attained in the field of scientific re- search by the California Academy of Sciences, and the prom- inent place the Academy is destined to fill as a scientific educa- tional institution. In a reminiscent way, he told of his many years’ connection with the Academy, as President in 1896 and 1897, and again in 1900 to 1902, of his first visit to the Academy in 1879, and his pleasant meeting at that time with W. G. W. Harford and Dr. 234 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH Srp. Albert Kellogg the botanist and one of the founders of the Academy. Dr. Evermann spoke in part as follows: In the few minutes allotted to me I shall be able to speak briefly of only one or two of the museum’s activities and aims. The California Academy of Sciences is a scientific, educational institu- tion. As a scientific, educational institution, the Academy, through its museum, has two important functions. The first of these is that of scientific research, The museum must furnish men and materials and facilities for scientific investigation. Through its research collections and its field in- vestigations, it must study and solve its share of the multitude of scientific and economic problems which the physical and biological sciences present to us, particularly those presented by the zoology, botany and geology of western America and the broad Pacific. We must do our share in study- ing and investigating and making known the natural resources of our country. The Academy must contribute its share to the world’s contribu- tions to human knowledge. The second important function of the Academy is educational. The Academy must do what it can within its means to be of real service in an educational way, not only to the general public, but also to the public and private schools. One of the ways in which it is endeavoring to render educational service is by installing in this museum habitat groups of California mammals and birds and other exhibits that possess real educational value and which show the natural resources of the state. Scientific research requires money and men. Habitat groups such as we are able to show you today also cost money. The income of the Academy is limited; it is not sufficient to enable the museum to carry on the scientific work which it should do and also build up popular educational exhibits. We have been able to prepare the splendid exhibits which we have to show you today because of the generosity of a number of public-spirited citizens of San Francisco and by curtailing somewhat for the time being the scientific activities of the Academy. Without the help of these friends of the Academy the valuable and attractive exhibits we have now installed would have been fewer in number. Nor would there have been so many if we had not drawn upon the Academy’s funds for scientific research. We have planned for several additional large habitat groups. We even have the animals on hand for a number of them. I may mention the very interesting elephant seal, a remarkable species of large marine mammal now nearly extinct. We have the animals for the group, but need funds for installing them. We have also the animals for two or three deer groups, a gigantic tortoise group, and a large iguana group. We have planned also for 22 groups of small California mammals, a dozen small bird groups similar to the very beautiful California quail group which you will see in the bird hall, and an indefinite number of small portable habitat groups such as that of the western meadowlark, which may be seen in the Vor. VI) EVERMANN—DIRECTOR’S REPORT FOR i916 235 office upstairs. These we propose to loan to the public schools should they desire them. It is hoped that the necessary funds for these exhibits may be supplied by private donations, so that the net regular income of the Academy may be reserved chiefly for scientific research. The large groups cost from $3,000 to $4,000; the small groups about $500 each; and the portable educa- tional groups about $100 to $250 each. It is hoped that this opportunity to do something worth while may appeal to those who are interested in education and who have the means to help along in such excellent work. What a splendid thing it would be for San Francisco and the state if, among those present here today, there might be some so impressed with the opportunity to help in this good work that they would provide the means to enable the Academy to add a dozen or more groups to the excellent series so well begun. We have the expert taxider- mists and preparators to do the work; we need only the funds to meet the expense. In conclusion, may I be permitted to mention one other need of the museum, to which I have called attention on another occasion. It is my ambition that there shall be in this museum a Children’s Room —a room in which will be displayed natural history objects such as are particularly attractive to little children. There would be in this room brightly and curiously colored birds and butterflies, moths and beetles and other insects; curious animals of other groups; attractive minerals, grow- ing plants, and aquariums with interesting and instructive animal and plant life; colored transparencies of beautiful native flowers, all selected and arranged with reference to the telling of an interesting story, of teaching a definite lesson. And there will be in this children’s room a children’s reading room in which will be found a library of all the interesting and reliable nature books and helps to nature study. And there will be in charge of this children’s room a well-educated, kindly, sympathetic man or woman who knows animals and plants; who knows the specimens in the museum and the live things in the park about it; and who, above all, knows and loves children; a man or woman who can wisely direct the observation and the reading of the children so that they may correlate their reading with what they have seen in the museum or in the open, and thus increase rather than stifle their interest in, and love for, animate things, as our public schools almost invariably do. It will be arranged so that children of the different grades will come to this room at different hours, and receive the instruction and help and encouragement adapted to their respective needs. And all this will be done and done soon, I confidently believe. It will be done because it so evidently appeals to us all as being the right thing to do, the right sort of education and training to give our children. It will be done, because the beauty and worth of it all, for the little children’s sake, will appeal to some one who has prospered in this world; some one with a kindly heart, who loves children, and who wants to help them to become the men and women they should become; and some day that man 236 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH Ser. or woman will come forward—I wish it might be today—and, out of his abundance, endow a Children’s Room in this museum, and thus make it possible for the California Academy of Sciences to do this splendid work for the children of California, not only of today but for those of the years to come. At the close of the formal dedicatory exercises a private view of the exhibits thus far installed was afforded the museum’s guests, of whom nearly one thousand were present in response to the special invitation. MUSEUM HOURS The Museum has been open to the public every day since the formal opening, September 22, 1916. The hours for the public are from 10 A. M. to 4 P. M. on week days and from 10 A. M. to 5 P. M. on holidays, including Sundays. VISITORS AT THE MUSEUM Attendance at the Museum has been very satisfactory. The number of daily visitors has varied on week days from fewer than one hundred on rainy, stormy days to more than 2,200, and on Sundays from 1,600 to 10,000. Totals by months are as follows: September(Odays)) i... 2... sissies 16,448 ©ctOben: «Se heee. oo ncetiew soe eee 36,933 INO Ven bei 56 <.t eee. ois dete ce este eee tee 27,718 December senses ooneke eee eee 15,002 Jandary caged «4 4cs-eseane mage eeee 23,170 Totalito Bebruary 1, 191722222 fee. 3. 119,271 THE MUSEUM AND THE SCHOOLS One very gratifying feature is the interest which the public and private schools are taking in the Museum. A large number of teachers have brought their entire schools to the Museum. Whenever possible the Director has accompanied the school about the halls, explaining briefly to the children the various exhibits. When the time of the school would permit the chil- Vor. VI] EVERMANN—DIRECTOR’S REPORT FOR 1916 237 dren were taken into the auditorium where an illustrated talk or lesson on some one of the habitat groups or other exhibits was given them. These efforts to help the children to understand the exhibits, to show to the teachers and pupils that the exhibits in the Museum are available as illustrative materials for their regular school work, and to make the Museum of real educational value to them, are appreciated not only by the teachers but by the children as well. The Academy is glad to be of service to the schools in this and all other ways in its power. It is hoped that even closer affiliation may be brought about and that a definite system for school visits may be arranged in the near future. LECTURES The regular course of free popular lectures on scientific sub- jects has been maintained throughout the year. These have been given at 8 o’clock on the third Wednesday evening of each month. Soon after the formal opening of the Museum arrangements were made for a Sunday afternoon course of lectures. These have been given in the Auditorium of the Museum and have proved very popular, the attendance at each reaching in nearly every case the full capacity of the hall. Indeed, on a number of occasions, many people were turned away. The lectures and the subjects are fully set forth in President Grunsky’s report. Through the liberality of Messrs. Wm. H. Crocker, R. fs Taussig, and John W. Mailliard the Academy has recently se- cured a complete moving picture equipment, including an ex- cellent camera. It is the intention to secure a number of reels illustrative of wild animal life, particularly of the species shown in the Museum’s habitat groups. The success of the Sunday afternoon lecture course is due in large measure to the industry and resourcefulness of Messrs. Roy E. Dickerson, W. W. Sargeant, and Edward P. Van Duzee, to whom, as a committee, all lecture matters were as- signed by the Director. 238 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH Ser. EMPLOYEES The regular employees of the Museum during the year 1916 have been as follows: Director and Executive Curator, Dr. Barton Warren Ever- mann; Curator, Department of Botany, Miss Alice Eastwood ; Curator, Department of Entomology, E. P. Van Duzee; Cura- tor, Department of Herpetology, Dr. John Van Denburgh; Assistant Curator, Joseph R. Slevin; Acting Curator, Depart- ment of Mammals, John Rowley; Curator, Department of In- vertebrate Zoology, Dr. Walter K. Fisher; Chief, Department of Exhibits, John Rowley; Assistants, Arthur L. Bolton, Paul J. Fair, Joseph P. Herring, and Mrs. M. L. Pariser; Assistant Curator, Department of Invertebrate Paleontology, Dr. Roy E. Dickerson; Librarian, Dr. Joseph Grinnell; Assistant Librar- ian, E. P. Van Duzee; Secretary, W. W. Sargeant; Stenog- rapher and Typewriter, Miss Susie Peers; General Office As- sistant, Ignatius W. McGuire; General Museum Assistant, John I. Carlson; Janitor, James H. Chastain; Assistant, Wm. C. Lewis; Janitress, Mrs. Johanna E. Wilkens; Night Watch- man, Frank W. Yale; Day Watch, Patrick J. O’Brien. DEPARTMENT ACTIVITIES The installation of the research collections of the respective departments having been practically completed before the be- ginning of the calendar year 1916, the curators and their as- sistants have been able to devote most of their time to field work for the securing of new material and to the care and study of the collections. The condition,and activities of the various departments are set forth in detail in the reports of the respective curators and need be referred to here only briefly. Department of Botany.—The customary enthusiasm and de- voted industry have characterized the department of botany during the year. The mounting and labeling of specimens has engaged much of the time of the curator. In this work she has been materially assisted by the members of the Botanical Club, with whose help the herbarium has been put in excellent condi- tion. Among the members of the Club who have rendered especially valuable service should be mentioned Mrs. Marian L. Vor. VI] EVERMANN—DIRECTOR’S REPORT FOR 1916 239 Campbell, Mrs. G. Earle Kelly, Mrs. C. L. Pitcher, Mrs. Ernest Meiere, Miss Kate L. Stoney and Miss Lena Gibbs. Many additions to the herbarium have been made within the year, the most important being a collection of 486 specimens of mosses donated by Dr. C. Hart Merriam; 81 specimens received in exchange from the U. S. National Museum; 100 plants from the Alps presented by Mrs. Zelia Nuttall; and two collections presented by the Botanical Club. The Curator reports that the needed data for the proper labeling of the plants collected by the Academy’s Galapagos ex- pedition have at last been supplied by the collector and it is now possible to correlate the field numbers with those used in the published report. The Botanical Club, under the supervision of the curator continues to hold weekly meetings and to be active in promot- ing interest in botanical matters. The curator has maintained throughout the year in the vesti- bule of the Museum an exhibit of the flowers of the Park and country. This exhibit receives much attention from Museum visitors and is proving of great educational value. Department of Entomology—Mr. Edward P. Van Duzee, who entered upon his duties as Curator of Entomology on June first, has been indefatigable in enlarging the collections in his department, classifying, arranging, and labeling the specimens, and, in general, in making the rich material under his care available for study. During the year he made a number of short collecting trips which resulted in the addition of many valuable specimens. The total number of accessions to the department within the year is 4859. Certain collections of the department have been sent to specialists for identification and study. The most important of these are the Orthoptera of the Galapagos expedition, sent to Messrs. Hebard and Rehm of Chestnut Hill, Pa., and the Plusiini sent to Dr. F. Ottolengui of New York. Considerable time has been given by the curator to the deter- mination of specimens submitted by correspondents and others who understand that the Academy is only too glad to be of service in this way. The curator is putting through the press a synoptic catalogue of the Hemiptera of America north of Mexico, which will prove 240 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. one of the most voluminous and important contributions of the year to entomological literature. Department of Exhibits—The employees of this department were engaged during the entire year on the installation of habitat groups. As stated elsewhere in this report, 17 groups were completed by September 21. Since that date two other small groups have been partially completed. Certain other ex- hibits have been temporarily placed in the mammal hall. The principal of these are eight cases of commercial mollusks and crustaceans and a giant clam shell, received from the United States Bureau of Fisheries; eight cases of shells from the Hemphill collection, selected for their educational value and general interest; one case of the edible clams of the west coast of America, presented by Mr. and Mrs. T. S. Oldroyd; one case of minerals, one of fossil fishes, and one of California butter- flies. A very instructive exhibit contributed by the Standard Oil Company has been temporarily installed in the Bird hall. This exhibit, installed without expense to the Academy, is illus- trative of the oil industry and attracts much attention. All these exhibits which do not logically belong in the Mam- mal and Bird halls will be removed to appropriate exhibition rooms as soon as an additional wing is provided. Department of Herpetology.—The activities of this depart- ment have continued throughout the year with their usual efficiency. Commendable progress has been made in classify- ing and arranging the collections on the shelves in the stack rooms. This work involves the separation, identification, re- bottling, labeling, and card-cataloguing of the entire collection, a task now more than one-third done. During the year the collection was enlarged by the addition of 1536 specimens. Considerable field work was done by the assistant curator in Nevada, Utah and Idaho, resulting in valuable collections and a much more complete knowledge of the herpetological fauna of those states. The collections of this department now number 33,816 speci- mens, and are among the most extensive in America. The hope of the curator to make the department second to none in Vor. VII EVERMANN—DIRECTOR’S REPORT FOR 1916 24 America in completeness and value of material is an ambition which should receive the hearty support of the Academy. Within the year the department has contributed four papers setting forth results of studies by the curator and assistant curator of the collections of the Academy, two of which have been published. The other two will be printed soon. Other scientific papers are in course of preparation. Department of Invertebrate Paleontology.—Mr. F. M. An- derson, the curator of this department, was on leave during the entire year, engaged on special work for certain oil companies and the Southern Pacific Railroad. The assistant curator, -Dr. Roy E. Dickerson, has shown his accustomed energy and in- dustry in looking after the interests of his department. A large amount was accomplished in preparing, sorting, identifying, and classifying the material in various collections, and putting the general collections of the department in order. Although the budget allotment to the department was small several field expeditions were successfully conducted,—one to the Simi hills in Ventura and Los Angeles counties, one to the Marysville Buttes, one to the vicinity of Petaluma and Free- stone, and one in the area on the southern border of the Mohave Desert, where certain studies in historical geology were made in co-operation with Dr. L. F. Noble of the U. S. Geological Survey. The assistant curator has been active and productive in original research, and has within the year contributed a number of papers to paleontological literature. Department of Invertebrate Zoology.—In this department, which is as yet only in the formative stage, the work of the year has consisted almost exclusively in the making of collec- tions for the department. The curator spent a portion of the month of June at Monterey Bay and vicinity collecting desir- able material. In the same month some collecting was done in the vicinity of Point Conception. In co-operation with the Department of Biology of the Uni- versity of Southern California, two weeks were devoted to dredging about Santa Catalina Island. The collections of the department have also been enriched by a valuable series of west coast Gephyrean worms and a mis- 242 CALIFORNIA ACADEMY OF SCIENCES (Proc. 4TH SER. cellaneous lot of invertebrates from British Columbia and the coast of California secured from Mr. W. F. Thompson, a small collection of California echinoderms donated by the University of Southern California, a representative series of invertebrates collected in the vicinity of Hilo, Hawaii, by Miss Leslie Tul- loch, and a small lot of echinoderms from Boundary Bay, B. C., contributed by Prof. Frank W. Weymouth. Department of Mammalogy.—As in the previous year the acting curator and his assistants devoted their time to the in- stallation of habitat groups. Little or no time was given to enlarging the collections. As no catalogue of the specimens in this department had ever been prepared, a proper record book was ordered made, and the collection was catalogued by Mr. Rowley, assisted by Mr. Bolton and Mr. Fair. The total number of entries is 2300. Very few of the speci- mens in this department have been accurately identified. There is urgent need of a mammalogist competent to make the identi- fications and who can add to the collection so that it may be- come a fair representation of the California mammalian fauna. Department of Ornithology.—This department being tem- porarily without a curator, has done no field collecting in the past year. The only additions to the collections are a few specimens received from miscellaneous sources. Mr. L. M. Loomis has continued to make use of the Tubinares of the col- lection in connection with the preparation of a monograph upon that group of birds upon which he is engaged. Library.—Mr. Edward P. Van Duzee, who entered upon his duties as assistant librarian June first, came to us with long ex- perience in library work. He had been connected with the Grosvenor Library of Buffalo, N. Y., for 28 years, 10 years as assistant librarian and 18 years as librarian. Although Mr. Van Duzee’s primary duties are those of curator of Ento- mology, he nevertheless devotes a portion of his time to the library. With the assistance of Mr. Ignatius W. McGuire and Mr. John I. Carlson commendable progress has been made in classifying and arranging the books on the shelves. After ma- ture consideration it was the opinion of the assistant librarian that the Decimal classification would best meet our needs, and Vor. VI] EVERMANN—DIRECTOR’S REPORT FOR 1916 243 that system has been adopted. The miscellaneous books in the main library, numbering some 2650 volumes, have been prop- erly arranged and author and subject cards written by Mr. McGuire and call numbers engrossed by Mr. Carlson on the back of each book and on each card. The sets of periodicals and publications of learned societies have also been similarly arranged. San Diego meeting of the Western Society of Naturalists.— As one of the societies affiliated with the Pacific Division of the American Association for the Advancement of Science, which met at San Diego August 9 to 12, 1916, the Western Society of Naturalists held its annual meeting at the same time and place. The Academy was well represented at these meetings, as many as twenty of its members appearing on the various programs for the presentation of papers. Two of the three presidential addresses were given by members of the Academy, the first by Dr. W. W. Campbell, President of the Pacific Di- vision of the American Association for the Advancement of Science, whose subject was ‘“‘What we know about Comets,” the second by Dr. Barton Warren Evermann, President of the Western Society of Naturalists, his subject being “Modern Natural History Museums and their relation to Public Educz- tion.” The following members of the Museum staff were present and presented papers: Miss Alice Eastwood and Messrs. Dickerson, Evermann, Grinnell and Van Duzee. ACCESSIONS TO THE MUSEUM The accessions to the Museum during the year have been numerous, as set forth in the detailed list in the appendix to this report. Several important donations were received from exhibitors at the Panama-Pacific International Exposition, and many others from various and miscellaneous sources. The Academy feels very grateful to all those who have in this way contributed to its collections. RECOMMENDATIONS Addition to the Museum Building.—Attention is again called to the necessity for additional room for the proper housing of 244 CALIFORNIA ACADEMY OF SCIENCES [Proc. 47TH SER. the Academy’s collections and the proper display of exhibition materials already on hand or expected in the near future. At the request of the President of the Board of Trustees the architect has submitted tentative plans and estimates for certain additions to the Museum building, as follows: a. Closing in the Court in such a manner as to provide one floor for exhibits; estimated cost, $35,000; or b. Closing in the Court in such a manner as to provide two floors for exhibits ; estimated cost, $50,000; or c. A main hall for the contemplated East wing; estimated cost, $90,000. Any one of these plans would meet the present needs of the Museum fairly well. Taxidermists’ Laboratory.—The work of the Museum has been and is seriously handicapped because there is no suitable shop or laboratory in which the taxidermists and preparators can carry on their work. An item of $1500 was provided in the budget for 1916 for such a building, but it was found that this amount would not construct a building that would meet the approval of the Park Commissioners. The matter was therefore abandoned for the time being. By using one of the habitat group cases not yet needed for exhibits and by constructing a small shed or room on the roof, we were able to get along for the time being. This arrange- ment is necessarily merely temporary. 1500 af This is an average for the last four years of only 1450 specimens as against an average growth of over 4000 for each of the preceding seven years. The number received during the year 1911 was over 6100 specimens, but in 1914 and 1915 this was reduced to nearly 800. This reduction in the rate of growth is due to the reduction in the amount of money available for field work. The present rate of growth is quite inadequate to secure pre-eminence for our collection. If we are to do this the rate of growth must at least be restored to its former standard, and such restoration in the rate of growth means that there must again be made available larger sums of money to be devoted to this purpose. Now that the building in the Park has been completed, I hope that this may be done. Vor. VI] EVERMANN—DIRECTOR’S REPORT FOR 1916 255 DEPARTMENT OF INVERTEBRATE ZOOLOGY By Walter K. Fisher, Curator Since the Department of Invertebrate Zoology is in a formative stage the work for the year has emphasized the accumulation of a collection. Systematic collecting was conducted at three points along the California coast: 1. By the curator, at Monterey Bay and vicinity, during June. 2. By Mr. ‘Carl Hubbs, in the region of Point Conception, during June. 3. By several members of the Department of Biology, University of Southern California, during a two-weeks’ cruise of their dredging boat about Santa Catalina Island. These have resulted in the accumulation of a considerable amount of material, which is being sorted. In addition, the curator secured from Mr. W. F. Thompson of Stanford University a very valuable collection of west coast Gephyrean worms, as well as a miscellaneous collection of invertebrates taken in British Colum- bia and along the coast of California. A small collection of Southern California echinoderms was donated by the University of Southern California. A representative series of invertebrates was collected in the vicinity of Hilo, Hawaii, by Miss Leslie Tulloch, and after her untimely death was sent to the Academy by Miss Martha Tulloch. Prof. Frank W. Weymouth, of Stanford University, has contributed a small lot of echinoderms and crustacea from Boundary Bay, B. C. DEPARTMENT OF INVERTEBRATE PALEONTOLOGY By Roy E. Dickerson, Assistant Curator In accordance with your request of January, the assistant curator is pleased to report concerning the activities of the Department of Inverte- brate Paleontology for the current year. With a small appropriation for field work this year, the department has been able to accomplish much very desirable exploration and investigations in three different portions of California. Laboratory studies on the Oligocene of Washington and Cali- fornia, the Miocene of the Mexican Gulf ‘Coast, the Caribbean, Panama and Lower California, the Pleistocene and Pliocene of Sonoma County, the Martinez-Eocene of the Rock Creek Quadrangle in Southern California, the Eocene of Mexico have been completed or are in progress. Some ex- hibit material has been arranged and more is in course of preparation for exhibition in the Museum. CARE OF COLLECTIONS The paleontological collections are practically all numbered with locality number, and the types, cotypes and figured forms given catalogue numbers as well. The conchological collections are only partially numbered, but 256 CALIFORNIA ACADEMY OF SCIENCES [Proc. 4TH Ser. the Hemphill conchological catalogue is almost completed. Approximately one-half of the Henry Hemphill conchological collection is unpacked, num- bered and placed in drawer cases or exhibition cases. But little work has been attempted on the excellent collections of rocks and minerals obtained from the Exposition. RESEARCH During the first three weeks of June, the assistant curator investigated the Eocene and Cretaceous in the Simi Hills, which are 30 miles north- west of Los Angeles. Lower Eocene fossils of the Los Angeles basin ex- hibit the same peculiar facies as the Martinez fauna of the San Francisco basin. The abundance and variety of Turritellas, the Volutide, the Cyp- reid, and other tropical and semi-tropical forms, in comparison with the fauna of the San Francisco basin, are evidences yielded by these collections that apparently well-marked climatic zones existed during lower Eocene time, in marked contrast with the vague and indefinite climatic conditions of the Upper Eocene, Tejon, during which semi-tropical conditions existed far north of the Equator. Palms and other tropical or semi-tropical forms of the land flora occur in Washington while semi-tropical invertebrate shells are numerous in the Cowlitz phase of Washington. Both the Rimella simplex zone or middle Tejon, and the Siphonalia sutterensis zone of the uppermost Tejon, were recognized in the vicinity of the Simi Hills. About five miles north of Chatsworth Pass, Mr. R. G. Stoner discovered an interesting locality which yielded numerous species characteristic of the uppermost Eocene of California, the Siphonalia sutter- ensis zone. This zone typically occurs in the Marysville Buttes, Sacramento Valley, and also extends along the western border of the Sierra Nevada, the marine equivalent of the land-laid auriferous gravels. This is the first recognition in California of the Siphonalia sutterensis zone in the outer Coast Ranges. Presumably, in most places in the coast ranges, the upper- most Eocene was removed during the interval of emergence between the Eocene and Oligocene on the Pacific Coast. About 15 new species from the Martinez-Eocene and about 12 forms new to science were found in the Tejon Eocene in this area. The Marysville Buttes were visited in April by the assistant curator. Eight different collections were obtained from the uppermost Eocene of this region. Ten beautiful new species were found. Knoxville cretaceous fossils were discovered for the first time in this ancient volcano of the Sacramento Valley. The uppermost Cretaceous, Chico group, was dis- covered in four different localities and fair collections were obtained. No Horsetown or middle Cretaceous was found in this area; presumably an interval of erosion in this region represents Horsetown time, as these de- posits occur in great thicknesses 30 miles west of the site of the Marys- ville Buttes, or faulting has uplifted the lower Cretaceous—the Knoxville— and lowered the upper Cretaceous, the Chico, and concealed the middle or Horsetown member of this Mesozoic period. During three weeks in July, the assistant curator, aided by Mr. John B. Kerr, collected from seven different localities in the Merced formation, Vor. VI] EVERMANN—DIRECTOR’S REPORT FOR 1916 257 between the ocean and Petaluma and northwest in the vicinity of Freestone. The type locality of the Merced, a Pliocene formation, is located in a cliff section 314 miles north of Mussel rock, where about 5000 feet of sands and shales are exposed. These collections demonstrate the presence of Merced strata resting unconformably upon an old erosion surface cut in ancient Franciscan rock of probable Jurassic age. Sonoma tuff, a volcanic ash and pumice deposit, was found interbedded with Merced strata in the vicinity of Freestone and environs. This tuff occurs in very extensive de- posits east of Napa, and occurs at the base of the Orindan formation near Pinole. The Orindan formation which consists of lake deposits, landlaid deposits, and interbedded volcanics is an extensive formation of the Berkeley Hills. Probably it is the equivalent of the marine Merced. This correlation is further reinforced by the discovery that the Lawlor ranch beds of Sonoma Mountain, which consist of sands, gravels and clays of an intervolcanic period rest upon andesite and Sonoma tuff. These beds have yielded Neohipparion gidleyi Merriam. Neo-Hipparion also occurs in the Orindan strata, and the Etchegoin of the western border of the lower San Joaquin Valley. Three collections from an ancient lake deposit east of Petaluma were obtained. Apparently a portion of the Petaluma lake beds represents a period of time somewhat younger than any of the marine Miocene of San Pablo age, as brackish water fossils were found in two localities. These fossils are identical with forms which occur in a similar deposit in the upper portion of the San Pablo formation of the Carquinez Straits vicinity, a marine formation about 2000 feet thick. Here we have apparently a tran- sition from marine to brackish water and finally to fresh water conditions in this Miocene basin. In summary then: The region lying between Tomales Bay and the top of Sonoma Moun- tain is a block which has been but little disturbed by folding or faulting since the Pliocene. This wave-cut block has, however, been warped so that it tilts from the sea towards Sonoma and Petaluma valleys, is up- lifted near Freestone on the northwest to 1100 feet, but is only 500 feet in elevation 20 miles south on the shore of Tomales Bay. The formations involved are in order, the Franciscan group, Petaluma lake beds of upper Miocene age, Marine Merced Pliocene, Basalts, Ande- sites, interbedded tuffs and sandstones of inter-volcanic period of the Sonoma Mountain region, stream terraces and marine terraces of Pleisto- cene age. Marine Miocene may exist beneath Sonoma Mountain, as is indicated by oil sands and oil impregnated basalts at one locality east of Petaluma. Sonoma tuff is interbedded with the Merced formation at Freestone. The Merced formation is the correlative in a broad way of the Sonoma tuff, the Pinole tuff, the Orindan, and probably the upper portion of the Etchegoin-Jacalitos of the San Joaquin Valley. The Hayward fault on the west side of Sonoma Mountain exhibits many characters which are due to recent movements which produced earthquakes during recent historic time. 258 CALIFORNIA ACADEMY OF SCIENCES [Proc. 47H Ser. At the invitation of Dr. L. F. Noble of the U. S. Geological Survey, the assistant curator spent two weeks last December in an area on the south- ern border of the Mojave Desert, the north flanks of the San Gabriel Mountains. This region is in a zone of great faults. Here we find blocks of Tertiary sediments dropped in between great breaks in the earth’s crust. In these sediments both marine and land forms were found imbedded. From these fossils and stratigraphy as bases, the historical geology of this region is being worked out. Some relations of the land laid deposits of the Great Basin region with the marine of the Pacific Coast and Gulf of Cali- fornia are being solved in this field. The nature of recent faulting and its resultant topographic forms are wonderfully exemplified in this field. The results of this work will be published in collaboration with Dr. Noble, as a Professional Paper of the U. S. Geological Survey. PUBLICATIONS Dr. C. E. Weaver published three papers in the Academy Proceedings during the current year:—Eocene of Lower Cowlitz River Valley, Wash- ington; The Post-Eocene Formations of Western Washington; and The Oligocene of Kitsap County, Washington. The Stratigraphy and Fauna of the Tejon Eocene of California was published by the assistant curator in the University of California Publications. A paper entitled The Strati- graphic and Faunal Relations of the Martinez Formation to the Chico and Tejon of Southern California, by Mr. C. A. Waring and The Fauna of the San Fernando Formation of Northeastern Mexico by R. E. Dickerson and W. S. W. Kew have been accepted for publication. Papers entitled: Geology of a Portion of the McKittrick District, by Mr. G. ‘C. Gester, Ancient Panama Canals, Climatic Zones of Martinez-Eocene Time, Climatic Conditions During the Oligocene with Descriptions of New Species from ‘he Oligocene of Washington, by R. E. Dickerson, have been submitted to the committee on publication. A paper on the Geologic History of the Marysville Buttes is in course of preparation by the assistant curator. EXHIBITS The Standard Oil Company has installed an oil exhibit in the east wing of the building and is now adding to, and improving it. Two cases of fossils representative of the oil bearing rocks are installed in connection with this valuable exhibit. A portion of the Henry Hemphill conchological collection showing varia- tion is on exhibition in the main Museum hall. Typical shells from this collection are being arranged in the reference room. Fossil freshwater fishes from an Eocene lake in Wyoming, a collection of rocks and minerals from Washington, and a collection of the edible clams of California are also displayed in the main hall. DONATIONS During the year many donations of valuable specimens have been re- ceived by the Museum, which have been added to the research collections of this department, as set forth in detail in the Director’s report. Vor. VI) EVERMANN—DIRECTOR’S REPORT FOR 1916 259 LrpraARIAN’sS REPORT By Edward P. Van Duzee, Assistant Librarian Please allow me as assistant librarian to submit the following report on the work done in this department during the past fiscal year, together with a few suggestions for the coming year. My connection with the library began on June first, 1916. I then found that after the removal of the library to the new Academy building the books had been placed on the shelves. The periodicals, the publications of societies and the administrative and scientific reports of the Federal and of the state governments, had been segregated and arranged in proper order, but only partially collated. Some of the more important individual books had been sorted out and arranged on the shelves in the reading room and a start had been made toward classifying them after the Library of Congress system. After correspondence with neighboring libraries and consultation with yourself and the members of the Academy staff it was finally decided to follow the majority of similar institutions and adopt the Decimal ‘Classification as the one best suited to our needs. The first work done was the classification and arrangement of the miscellaneous books in the main library. The books so treated numbered 2650 volumes. Author and subject cards for these were written by Mr. Ignatius McGuire, and Mr. John Carleson engrossed the call number upon the back of each book and on each card. The sets of periodicals and publications of learned societies have also been classified and the cards for them made and en- grossed, and those in the English language and a considerable part of those in foreign languages have been collated. The catalogue cards have been alphabeted in two series, one including the author and title cards, the other the subject cards, so there is now a fairly useful catalogue of the books in the main library but including very few analyticals. Current accessions to the library are entered and acknowledged as soon as possible after their receipt. An accession register has been started but is not yet nearly com- plete. Mr. McGuire has made the entries in this register, which now num- ber 5401. The most important work in this department for the coming year will be the classification and cataloguing of the state and Federal government publications in the main library and of the books in the laboratories of the departments of Botany, Ornithology and Paleontology, the books pertain- ing to the other departments having been mostly attended to in connection with the work on the main library. The preparation of a card shelf-list and the completion of the accessioning are other important matters to claim attention during the coming year. I would like to suggest the desirability of having a moderate appropria- tion in this department, of perhaps $100, in the next fiscal year for the purchase of Library of Congress and American Library Association an- alytical catalogue cards for certain important sets of serial publications, a smaller sum for the construction of a wall case in the reading room suit- able for the shelving of current serials and new accessions, and not less than $200 for the binding of a few important books and serial sets. The 260 CALIFORNIA ACADEMY OF SCIENCES [Proc. 47H Sern. binding of serial publications in a scientific library is always an important and considerable item in the fixed charges of the institution and it is rarely advisable to postpone such expenditures too long or the binding of the ac- cumulated volumes may become a serious problem. DEPARTMENT OF ENTOMOLOGY By Edward P. Van Duzee, Curator I beg to submit the following report on the condition and work in the Department of Entomology for the current fiscal year, including a few suggestions for the ensuing year. My appointment as curator of this department took effect on June first, 1916, and on assuming the duties of the position I found the collections of the department unorganized and unarranged, although well cared for and in excellent condition. The first work done was the fumigation of the laboratory with hydrocyanic acid gas to kill museum pests introduced into the room with the Galapagos tortoises that had been temporarily stored there. Suitable book shelving was then erected, the books pertaining to the department were brought in from the main library, and the scientific apparatus and property of the department was unpacked and made avail- able for use. The collection of insects was found to be in almost perfect condition with practically no infestation by museum pests. There were about 200 trays well filled with mounted specimens and about 60 trays filled with unmounted material in boxes and papers. A portion of the mounted ma- terial had been properly labelled for locality and collector, but the larger part was without such labels. It has been my first duty to get this material labelled so it can be made available for study and exhibition. Many thousands of these labels have been printed and attached to the speci- mens and this work is now nearing completion, so the arrangement and classification of the collection can soon be begun. During the year 4859 specimens have been added to this department by gift or through collections made by myself, and these have all been mounted and properly labelled. Very little field work was done during the year. I spent one day at Los Bafios, two at or near Mt. Diablo and three in Lake County. On the last two trips I went as the guest of Mr. W. M. Giffard, so the total expense to the department for all trips was but $6.75. I also spent two days collecting about San Diego, a few hours at Man- hattan Beach, Los Angeles, and took several Sunday trips about the Bay district without expense to the department. The total accessions from these collecting trips number 1976 specimens. During the year two collections have been sent to specialists for study. The Orthoptera of the Galapagos Expedition were sent to Messrs. Hebard and Rehm and the Plusiini to Dr. Ottolengui. A portion of my time during the past year was devoted to the study and determination of insects for correspondents of the Academy and to the publication of a bibliographical and synonymic Catalogue of the Hemiptera VoL. V1J EVERMANN—DIRECTOR’S REPORT FOR 1016 261 of America north of Mexico. This catalogue will soon be issued as a volume of the semicentennial publications of the University of California. A collection of butterflies for temporary exhibition in the Mammal Hall of the Academy was prepared soon after the formal opening of the Academy building. This collection consists of 12 trays of showy exotic species and six trays of carefully determined and labelled ‘California species which it is hoped may be of interest to children taking nature work in the public schools and to those beginning a collection of local insects and wish- ing help in the determination of their captures. Looking ahead to another year the most urgent duty of the curator of this department will be the classification and arrangement of the North American material now in the collection so it will be available for scien- tific research. Of scarcely less importance is the accumulation of a more complete collection of the insects of California as a basis for the ecological and taxonomic study of our insect fauna. Another matter of importance in outlining the work of the coming year is the inauguration of a system of recording the material in the collection and for this purpose a card system of species-records and a book record for current lots as received and for type material seems the most practical and useful. The preparation of a permanent exhibit, especially of the insects of our own State, should not be neglected, and later when our material has been worked over and made more available the preparation of life history groups can be under- taken to good advantage. For the preparation of these exhibits and for the mounting and labelling of the accumulated material now on hand, some pro- vision should be made in the estimates for the coming year that will allow the employment of an assistant to the curator occasionally as circum- stances may require. I might add that much of this accumulated material is of great scientific interest and is indispensable for study, but in its present condition it is entirely unavailable for such purposes and practically inaccessible, and it is important that it be mounted and suitable cases pro- vided for its reception. Much of the work of this department in the past has been the accumulation of material, but it now seems desirable that this material be made available to our own students and to other specialists who may wish to undertake its study so the Academy may profit by their labors and acquire the types and paratypes of the new species. 262 CALIFORNIA ACADEMY OF SCIENCES FINANCIAL STATEMENTS REPORT OF THE TREASURER for the fiscal year ending March 31, 1917: April. 1; 1916, ‘Cash Balance... :.2.cc cc teense ces Receipts Duesy Get sues etenasm coe hie adeiea aie eee $ 1,539.75 Chas. Crocker Scientific Fund Endowment In- COME) . Haiti, SMviohietiontwm ess ais esonde aren ewan 1,065.74 James Lick Endowment Income................ 42,890.81 General Income Account...............2.0e00e0 20,165.03 John W. Hendrie Income....................-: 607.50 Billg 7 tPavab lessee rears boasts = aisletesafete cetera 631,300.00 W.. B; Bourn Donations... i.csss-. sen. easaoneas 1,014.02 Jos7.D: "Grant 2 Donations: .ecacdtensecic tex eeisceieles 832.78 Herbert Fleishhacker Donation................. 1,000.00 Jes. -Lobini Donation). oy. 9.2. eccesecececc cee ee 250.00 W.G. Wright Bundssaoscs cc vecace names eerscee cre 38.50 California Elle Expenses: :.<. cance. nee cee ean wer 125.00 Museum Appro. No. 32 Exhibits............... 1,077.86 Museum Appro. No. 6 Botany.................. AS Muséum 22 .cctaciaseekieie. co sieit oO 1) o ep) + oO cp) a << oO