46 PROCEEDINGS OF UNITED STATES NATIONAL MUSEUM.
I
was
unableto procure evenaspecimen oftliesalmon, butobtained enoughsmelts to forward,some
excellent specimensto Washington.Very
respectfully, yourobedientservant,JAMES
G.SWAK.
Prof.
Spencer
F.Baird,
United States Commissioner Fish andFisheries, Smithsonian Institution, Washington, D. C.
p. S.
—
I omittedto mention that thesurf-smelt arecommon
inallthesalt waterof
Paget
Sound, but Ihave not heard of an instancewhere they runup
fresh-water streamsto spawn,likethe easternsmelt.J. G. S.
1VOTE OIV
THE OCCUKREIVCE OF IPRODUCTUS GIGAIVTEUS
liV CAI..IFORi'VIA.
By
C. A.^WMITE.
Among
a smallcollectionoffossilssenttothe NationalMuseum by
Mr.Ludwig
Kumlien,oftheUnitedStatesFishCommission,fromthe valley ofMcCloud
Eiver, ShastaCounty,California,arethreeorfour largeex- am])lesof Productus,whichIam
unableto distinguish fromP.giganteus Martin sp.,the well-known typespecies ofthegenusasitis extensivelyknown
inEuropean
strata.They
arepreserved in a hard,dark-colored, argillaceous rock, which is partlymetamorphosed,and
they are, there- fore,somewhat
imperfect; butportionsofthem show
thecharacteristics of thespecies veryplainly.The
largest of theseCalifornian examples was,when
perfect, quite equal in size tothe largerEuroi>ean examples ofP:giganteus, havinghad
a transverse diameter nearthe hinge of not lessthan 140millimeters, or 5Jinches.A
smallcollectionoffossilswas
sentby
mailfromthesame
localityin 1877by
Mr. Livingston Stone, the speciesof which were recognized as of Carboniferous age,but P. giganteuswas
notamong
them, although thelater collections indicatethat they occurin thesame
strata. These associated forms of both collections are too imi)erfectlypreserved for specitic determination,but the generaFcnestella,Streptorhynchus, Spiri- gera Camarophoria, Allorisma,and
Eiiomphalus aremore
or less satis- factorily recognized.They
all together plainly indicate tho Carbonif- erous age of the strata from which they come, which factwas
also l)reviouslyknown
throughthe reports ofTraskand
Whitney.This, so tar as I
am
aware, is the first discovery of P. giganteus inAmerican
strata. Itis not alittle remarkable that it slioidd befotind inthe westernportion of the continentand
notin themiddle andeast- ernportions, where the Carboniferous system is sowell,developed,and
where
severalEuropean
speciesof Carboniferousbrachiopodaare recog- nized.PROCEEDINGS OF UNITED STATES NATIONAL MUSEUM. 47
Fig.1, on Plate ,represents one ofthe examples referredto, the principal portion oftliefigureshowinga naturalcast ofthe dorsalvalve, with the
nmbonal
portion of the ventralvalve. In this figure thefull length of the shellfromback to frontis not shown, butit is represented inthe acconiijanying diagram, Fig-. 2.Washington,
D.C,
December3, 1879.NOTE OX ACKOTHEIiE.
By
C. A.\%^HITE.
Among
thefossilscollectedfromPiimordialstrata atAntelopeSpring, Southern Utah,by
Mr. G. K. Gilbertand
Mr. E. E. Howell,who
were then connectedw^ith the exi^lorationsand
surveys west of the 100th meridian,were anumber
of examples of adiscinoid brachiopod. This form Idescribedand
figuied* under thename
of Acrotretaf subsidua, referring ittothat genusprovisional!}'. JSToue of theexamples werein a conditiontoshow
all the generic characters clearly, butcertain fea- tures in theseshells indicated their i^ossession of importantdifferences fromany
genus then establishedand
ledme
to suggest that they prob- ablyrepresented anew
generictype. Inthesame
year, 187G, Prof. G.Linnarsson, ofStockholm, Sweden, publishedt a
new
genericform from the Primordial rocks of Sweden, under thename
ofAcrothele^ which plainlyincludes Acrotreta? subsiduaWhite. ProfessorLinnarssondes cribedtwo Swedish
speciesunderthis genericname
(A. coriaceaand
A.granulata),
and
in 1870 he published a third species underthename
of A. intermedia,^but A. siibsidua is at present the onlyknown American
species. Itisnot unlikely,however,that
some
of theAmerican
species heretofore referred to])isci)ia willbefound tobelong to Acrothele.Washington,
D.C,
February1, 1880.DESCRIPTIOiV OF A NEW CKETACEOIS
PIIVIVAFROm TiEW MEXICO.
By
C. A.IVHITE.
Pinna stevensoni.
Shell large, elongate-triangular in marginal outline; valves moder- ately convex; the convexity being slight
and
nearly uniform poste- riorly,butmuch
greatertoward the front,whereitamounts
toan obtuse median angularityupon
each valve,and
wheie a transverse section of theshell has an approximatelyregular rhombic outline; upperborder*Expl. amiSiir.WestoftlielOOtli Merit!.,Vol.IV,p.34, pi.I, fig.3,a, b, c,audd.
tBihangtillk.Svenska Vet. Akad Handliugar,Baud3, No. 12, p. 20, pi.IV,figs.
44-52.
tSvcriges Geologiska Uudersokuiug; Ser. C. Afhaud. ock Upps. No. 35, p.25, pi.
iii, figs.40-44.