128 PROCEEDINGS OF THE ACADEMY OP
laterali,
tumidula
; striisregularibus distantibus; epidermideflavescentein- duta; valvis solidiusculis, intus albis,umbonibus
prominentibus, erosis, cardinecrasso, tridentato.Long.11;lat. 10;diam. 6mill.
Hab.
'(Collect. Prime.)14. Corbicula vio1acea Prime. C.testa ovato-transversa, subaequilate-
rali, obliqua, extremitatibus aequaliter obtusa, transversim irregulariter striata;epidermidesqualide virescente vestita;
umbonibus
magnis, obliquis,erosis,intusprofundeviolacea;cardine angustotridentato.
Long. 15; lat.13; diam.8mill.
Hab.
? (Collect.Jay
etPrime.) 15. CorbiculaAgrensis
Prime.CyrenaAgrensis Kurr., in litt.
C. testa ovato-transversa, aequilaterali, laevigata, depressiuscula,extremi- tatibusrotundata;epidermideviridi-olivaceainduta; sulcis regularibus, dis- tantibus;intus pallide violacea;
umbonibus
tumidis, erosis;cardineangusto, dentibuscardinalibuscrassis, lateralibus aequalibus, tenuiter serrulatis.Long. 9;lat. 8; diam.5mill.
Hub.
Agra, India. (Collect. Prime.)16. Corbicula
inaequilateralis
Prime. C. testa ovatotransversa, depressiuscula, tenui, inaequilaterali; extremitatibus rotundata;umbonibus
prominentibus, approximatis, antice obliquatis, violaceo subradiatis; sulcis regularibus,intus pallide violacea;epidermidepallide virescenteinduta;car- dine angusto;dentibuscardinalibuscrassis, lateralibus inaequalibus.Long.16;lat. 12;diam.8 mill.
Hab.
Africa. (Collect. Prime.)17.
Sphaerium Vermontana
Prime. S. testa ovato-trigona, tumida, inaequilaterali,, striisregularibus, epidermideviridi-fiavescente vestita;um-
bonibus tumidis;cardine arcuato; dentibuslateralibus crassis. ,Long. 11;lat.10; diam. 7mill.
Hab. Vermont,
N. America. (Collect. Prime.)Thisspecies,
though somewhat
allied toSph.striatinum
Lam.,ismuch more
inequilateral.Descriptions of
new
PalaeozoicFossils from Illinoisand
Iowa.BY
F. B.MEEK AND
A. H.WORTHEN,
OftheIllinoisStateGeologicalSurvey.
ECHINODERMATA.
CRINOIDEA.
Genus PLATYCRINUS,
Miller, 1821.Platycrinus Oweni.
Body
rather large, cup-shaped, or sub-hemisphericalbelow
thesummit
ofthefirstradials,rounded on
theunder
side,height about two-thirds thebreadth. Base saucer-shaped, ornearlyfourtimes aswide
as high, pentagonalinoutline, the sidesbeing nearlystraight or slightlyconcave, sutures anchylosed;columnar
facet large,itsbreadthequallingabouthalfthat ofthebase, concave,margined by
aslightly raisedsomewhat
undulated rim,and
perforatedby
a large central opening. First radial plateslarge, sub- quadrangularingeneraloutline, but havingthe superior lateral angles trun- cated for the reception of the analand
interradialpieces, wideningalittle fromthebaseupwards
; facetforthe reception of the second radial pieces[June,
NATURAL SCIENCES OF PHILADELPHIA. ]29
prominent, nearone-third aswideastheplate,
and
extendingdown between
one-thirdand
one-halfitslength. Secondradial pieces small, extending out nearlyhorizontallyfromthefirst;round
below,and
presentinga pentagonal outline, as seenfrom theunder
side, supportingon
their superior (outer) slopingsides, thetwo
firstdivisions ofthearms. Firstanal piece rather large foraspecies ofthisgenus,apparently pentagonal,and
extendingdown between
thefirstradials,nearlyasdeepasthe articulatingfacetssupportingthesecond radial pieces. (Otherpartsunknown.)
The
suturesseparatingthefirstradial platesfrom eachother,and
from the base, are rather distinctly canaliculated, inconsequenceofthe bevelingofthe edgesof theplates.The
surfaceisfinelygranulose,and ornamented by
small obscurely subnodosecostae,ofwhich
there aretwo on
thebase passingaround
nearthemargin. Threesimilarcostaeornament
thefirst radial plates,being arranged parallel to the basaland
lateral margins, butbecoming
nearlyor quite obsoleteabovethemiddle.Named
inhonor
ofProf. RichardOwen,
ofthe GeologicalSurvey
ofIndiana.Localityandposition. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. Charles
Wachsmuth.
Platycrinusscobina.
Body
rather small,cup-shapedorsubturbinatebelow thesummit
ofthefirstradial pieces. Base basin-shaped, about twice aswide as high,and
rathermore
thanequalling one-third the heightof thebody
to the top of the first radials; pentahedral in outline, with slightly concave sides,columnar
facet lessthanone-thirdthebreadthofthe base. First radial plates slightlybroader than high, widening a littleupwards
fromthe base, presentingasubangularoutline, the superior lateral angles being truncated forthe reception ofthe analand
interradial pieces; facet for the reception of thesecondradial piecenot protuberant, concave,ratherlessthanone-thirdthe breadthoftheupper
side of thefirstradial plates,and
extendingdown
about one-fifththeir length. Secondradial pieces small, triangular,and
supportingon
their superior sloping sidesthefirstdivisions ofthearms. After dividingon
thesecondradial pieces, thearms
divide againon
thesecondpieceabove,beyond which
theyarelong,slender,and
apparentlysimple. After thesecond bifurcation, theyareeachatfirstcomposed
ofa singleseries ofwedge-shaped
pieces,but gradually pass intoa doublealternating series of pieces, eachofwhich
isaboutaslongas wide.The
surface ofthe basaland
firstradial platesisornamented
withnumerous
small, rathersharplyelevated, irregularlyarrangednodes, or coarse granules, so as topresenta rasp-likeappearance.The
suturesare closelyanchylosedin the base,and
well definedbetween
thefirstradialplates.Initssurface
markings
thisspeciesismuch
like P. Wortheniof Hall,but it differsinhavinga distinctlyprotuberant, instead of a flat or concave base,and
inhaving butfourarms
toeachray, instead ofeight or nine.Locality
and
position. Burlington, Iowa. Burlington Limestone. Mr.Charles
Wachsmuth's
collection.Platyckinus (Pledeocrinus) asper.
Body
small, rather deeply basin-shaped
belowthearms. Basemuch
depressed, largelyand
deeply excavated below, with anarrow prominent
marginal rim,which
is notched at the sutures,and somewhat
undulated. First radial plates broaderthanhigh, widening moderatelyupwards and
presenting a subquadrangular outline, but really hexagonal, in consequence of the truncation of the superior lateral angles for the reception of the interradialand
anal plates; sinus in thesummit
of each, for the reception of the second radials, deep, semi- circular,and
equalling about half the breadth of theupper
side; surface ofeachornamented by
a very prominent, sharply elevated carina,which
passesacrossnear the lowerside,and
iswaved
or oftenbrokenup
intoisola- ted prominences. Second radial pieces triangular, wider than long,and
1861.]
130 PROCEEDINGS OF THE ACADEMY OF
nearly entirely received within the sinus, in the
upper margin
ofthe first radial pieces. Firstanaland
first interradial plates of apparently ahout thesame
size, theformer connecting with a range of smallplates above,which
form theunder margin
ofthe lateral analopening.The
arms, afterthefirstdivisionon
the second radial plates, divideagain on the second piece, abovewhich
thetwo
inner branchesbifurcateagainon
thesecond piece, thusmaking
sixarms
in each ray seen in thespecimen under
description.Above
thelastdivisionthearms
are slender, very gradu- allytapering,and
eachcomposed
ofadouble seriesofsmallalternating pieces, (excepting near the points of bifurcation,)and
supporton
theirinner side ratherclosely setrangesof tentacles.The column
isalittlecompressed,and composed
of rather thin pieces,withprominent
crenulated margins near the base.Locality
and
position. Burlington, Iowa. Burlington Limestone. Collec- tion ofCharlesWachsmuth.
Genus FORBESIOCRINUS, Koninck and Le Hon.
Fokbesiockinds Moxeoensis.
Body
below the freearms
apparentlyskort- turbinate, or subglobose,composed
of nearly smooth, rather thick plates, connectedby
linear sutures. Base small,and
nearly hiddenby
thecolumn.Subradialplates ofmoderatesize, four of
them
pentagonal,and
oneon
the anal side apparently hexagonal, withunequal
sides. First radials about twice as wide as high, hexagonal in form,and
nearlytwice as large asthe subradials. Second, thirdand
fourth radials, intwo
ofthe rays, (and the fifthand
sixth in another,)all nearlyofthesame
length,hexagonal informand
abouttwice aswide as long. Lastprimary
radial pieces ofnearly thesame
size as the others,and
supportingon
their superior sloping sides the secondaryradials.Of
thenumerous
interradials,the first is about thesizeof the subradial pieces, hexagonal in form,and
supportstwo
smaller pieces inthesecond range.Above
these four or five occurinthenextrange, inoneinterradial space,which
isasfarup
asthey can be counted in thespecimen examined, though
it isevidentfrom the breadthofthe interradial spaces, thattheymust
increaseatthesame
rateforseveralranges above. (Analplatesunknown.)
The column
isrounded and
comparatively thick at its junction with the base, fromwhich
ittapersgradually towardsthe lower extremity.Near
the baseitiscomposed
ofextremelythin, equalsegments, connectedby
minutely crenulatedsutures. Fartherdown
itgradually passesinto a series of alter- natelythickerand
thinnerpieces.After the first division of the rays
on
thelastprimary
radial pieces, thearms
divide several times,and
appear to give off lateral branches, but our specimenisnotina condition toenableustodeterminehow many
pieces in- tervenebetween
the points of division, nordo theyshow whether
ornotthere areany
interaxillary pieces.The
specimenbeforeuspresents the peculiarand anomalous
appearanceofhaving
asmallfalsearm
arising directlyfrom thesummit
of theupper
trun- catedsideofthelargest subradial piece. Itseems
eventobe inserted into a sinusintheupper
sideofthe subradial, yetwe can
scarcely believeitisany- thing but oneofthe smallerdivisions of thearms,accidentallybroken
offand
placedinthat position.As
nearaswe
can determine from a description alone, this species appears tobesomewhat
closely relatedto F.exculptus, (Onychocrinusexsculptus,Lyon
and
Cassiday,Am.
Jour. Sci.vol.29,N. S.page 78,)butdiffersinhavinglessproduced
basal pieces, while theupper
angles of the subradials are obtuse instead of "quite sharp." Italsoseems
tohave two
or threemore primary
radial pieces inone ray than occurinany
ofthose ofthespecies describedby
Lyon and
Cassiday.Again
itssurfaceappears tobesmooth
instead ofgranu-[Juue,
NATURAL SCIENCES OF PHILADELPHIA. 13l
lose,
and we have
notbeenable to seeany
indications of the small patelloid pieces between theradialand arm
pieces asin F. exscu'ptus.Locality
and
position. River Bluff, near the south lineofMonroe
County,Illinois.
Keokuk
LimestoneoftheLower
Carboniferousseries.ForbesiocrinusAgassizi, var. giganteus. Thislarge Crinoiddiffersfrom the typicalspecimenofF. Agassizi (Hall), in
having
four instead of three plates ineach secondary ray; (in three of therays seen)whilethere aresome
differ- ences inthenumber and
arrangementoftheanaland
interradial plates. It alsodiffersinhavingitscolumn
almostexactly cylindricalforadistance of at least four inches below the base, while that of F. Agassizi,isdescribedas"rapidlytaperingbelowthe
summit." We
suspectitmay
provetobeadis- tinctspeciesfromthat describedby
Prof.Hall, but as it agreeswithhisdes- criptionand diagram
inmost
ofitscharacters, excepting the points ofdiffer- encewe have
mentioned,we
merelycall attention to it as a varietyofthat species, untilwe
canhave
an opportunitytocompare
betterexamples
of it with authentic specimensor figures ofProf. Hall's species. Should it prove tobedistinct, itcan takethename
giganteus,which would
be veryappropri-ate, sinceitisthelargestspecies of thatgenus
known,
the length of itsbody
tothecommencement
ofitsfreearms
being near3-30inches,and
itsbreadth apparently about the same. Itsarms
are proportionally short,and
bifurcate frequently.Localityandposition. Burlington, Iowa. Burlington Limestone.
Genus ACTINOCRINUS,
Miller, 1821.Actinocrinusdodecadactylus.
Body
rather small, subglobose;summit and
calyx below thearms
of nearly thesame
size; breadthalittlegreaterthanthe-height;
composed
of slightly convex,smooth
or subgranulose plates,which
areconnectedby
moderatelydistinctsutures. Base small,much
de- pressedor subdiscoidal, obtuselyhexagonalin outline,withthree otherobtuse retreatinganglesatthesutures. First radial plates wider thanlong, three ofthem
regularlyhexagonal,and two
heptagonal. Secondradial piecesmuch
smaller than the first, about twice as wide as long,
and
allquadrangular.Third radialsalittlelargerthan thesecond, all regularlyhexagonal, the
two
lateral margins being very short,
and
thetwo
superior sides each about equalling the base. In thetwo
posterior rays, the third radial pieces each support on one of their superior sloping sides a large brachial piece,and on
the otherasecondaryradial ofnear thesame
size,which,initsturn, supportstwo
brachial pieces,making
threearms
toeach oftheserays;whileinallthe others,two
brachial pieces rest directlyupon
the thirdradial, thusmaking
only twelvearms
inthewholeseries.The
firstanal plateisaboutaswideas thefirstradials,buta littlelonger, being longer than wide, instead ofthe re- verse. It isregularlyheptagonal,and
supportson
eachsuperiorlateralslop- ingside,asmaller heptagonalpiece; whilean
elongated, coffin-shaped piece restsupon
its short superiortruncatedside,between
thetwo
latter,and
ex- tends up, flankedoneither sideby
thefirstbrachials, toits connection with thesummit. Each
oftheinterradial spacesisfilledby
a single ovate, octago- nalpiece, aboutas large asthe secondand
third radial pieces takentogether.The
vaultiscomposed
ofrather large,somewhat
regularlyarrangedplateswhich
are very nearly flat, the smaller onesallbeing ontheanalside; the proboscisissmall,and
locatednearertheanalthanthe dorsalside.Heighttobaseof proboscis, 0-50inch; breadth, -58inch; breadthof base, 0-23 inch.
Locality
and
position. Burlington, Iowa. Burlington Limestone.Actinocrinusptriformis, var. rudis. Actinocrinus pyriformis,
Shumard,
1855, Geol. Reportof Missouri,p. 192, pi.A, fig. 6,a, b.Body
exclusive ofthe proboscis piriform,being verynarrow and
apparently1861.]
132 PROCEEDINGS OF THE ACADEMY OF
cylindrical from the base to the top of the third radial plates,above
which
the secondaryradialand
brachial piecescurve abruptly outwardstothe base of thearms, so astoform withthe ventricosesummit
amuch expanded
vis- ceral cavity, entirelyabovethe basaland primary
radial plates. Baseun-known
; firstradialsunknown,
excepting fromsome
remaining portions of theirupper
ends,which show
that theyare comparativelylarge. Second radialsverysmall, alittlewider thanlong, (those seen)irregularlypentagonal in form, oneofthe sidesbeingmuch
shorterthan the others. Thirdradials aslongasthefirst,and
nearlyone-third wider, (the onlytwo
visible inour specimen,)hexagonal in form,and
each supportingon
its superior sloping sidestwo
secondaryradialsofaboutitsown
size.Each
oftheseissurmounted by
asomewhat
largersecond secondaryradial,which
initsturn supportstwo
firstbrachial pieces, eachof
which
issucceededby
a second, fromwhich
the freearms
aregivenoff.The two
series of secondary radials,and
thefmr
series of brachial pieces in each ray, connect laterally, so as to leave
no room
forinteraxillaryand
interbrachial pieces. Interradial platestwo
or three, thefirstbeing aboutthesame
sizeasthesecondradials,and
hexagonal orheptagonalinform.Above
thisthere areoneortwo
smallpieces, of variable sizeand
form,overwhich
the secondaryradials,and
thelateral seriesofbra- chial pieces of the rayson
eachside, connectalltheway up
tothefreearms, insuch amanner
astoleaveno
spacesforinterradialsabovethose just descri- bed. (Analplatesunknown.)
Dome
hemispherical,composed
ofpentagonal, hexagonal,and
heptagonal plates ofnearly uniform size, each ofwhich
is provided witha spine-like tubercle. Proboscis central or nearly so.Arm
openings twenty. Surfacesmooth
orobscurely granulose; smallratherpointedtubercles are also seenon
the secondand
third radial plates, first interradials,and
firstsecondary radials.It ispossible thisCrinoid
may
bespecificallydistinctfrom A.pyriformis, ofShumard,
butitagreeswithitinsomany
respects thatwe
do not feel fully warrantedinregarding itas specifically distinct. Itsmost
important differ- encesare the sub-spiniferous character ofitsplates,and
the possession ofonlytwo
or three interradial plates, instead of six in eachinterradial space. It alsodiffersinhavingamore
ventricosedome,
while the inferior half of itsbody
ismore
abruptlycontractedbelow the arms.Locality
and
position. SaltLickPoint,Monroe
County,Illinois.Where
itoccursinbedsofthe
same
age astheChouteau
LimestoneofProf. Swallow.Actinocrinus
(Amphokacrinus
?)cofCAvcs.Body
small, subglobose,broader thanhigh, alittleoblique;summit
nearlyflat;under
siderounded and
dis- tinctlyconcave, sides rising vertically ornearlyso. Surfacesmooth
or sub- granulose. Basesmall, concave,and
entirelyincluded within the concavity oftheunder
side. First radial platescomparativelylarge, convex,and
curv- ing under, so as to form a part ofthe concavity below;two
ofthem
hept- agonal,and
threehexagonal. Secondradial pieces(wantingintwo
ofthe rays ofthe specimenbefore us,)widerthanlong,and
quadrangularinform inthe others.Third radial pieces smaller than the second, (in three of therays,) pent- agonalin form,
and
each supportingupon
its superiorsloping sides the firstbrachialpieces,
which
forma part ofthewalls of thebody. First interradial pieces, comparativelylarge, oraboutone-half thesizeofthefirstradial plates, nine-sided, the superior sloping sides ofeach supporting one side oftwo
of thebrachial pieces, whiletwo
very smallpiecesrestupon
the middle ofthesummit, and
connect withthevault above,and
with the brachial pieceson
eachside. Firstanalpiece alittlelargerthanthefirstradials, heptagonalin form,and
supportinginthenext rangethreepieces, thetwo
lateral ofwhich
are larger than the other,and
connect aboveon
their slopingsides, with brachial pieces,whilethemiddlepiecebetween
theseisirregularlyhexagonal,[June,
NATURAL SCIENCES OF PHILADELPHIA. 133
and
supports threevery smallpieces in the next range,which
connectwith theanalopening,and
thevault pieces above,and
withthe brachialson
each side.The
vaultismade up
of afew comparativelylarge pieces,the central oneofwhich
isalittlemore convex
than the others.The
anal opening is verysmall, lateral,orabouton
thesame
horizon as thearm
openings,and
surroundedby
onlyfiveplates,which
arenot protuberant. Thereare twelve smallarm
openings arrangedaround
themargin
ofthesummit,
three toeach ofthe posterior rays,and two
toeachoftheothers.The arms would
appear, fromthesmallsizeoftheopenings,and
the very small articulating surfaces for thereception of thefirst freearm
pieces, to be veryslenderand
fragile.(Column unknown.)
Heightofbody, C'31 inch., breadthfrom the anal totheanteriorside, 0*42 inch; breadthof base, 0*17 inch.
This is a very remarkable species,differing from
any
otherActinocrinusknown
tous, in theconcavityoftheunder
side,and
the incurved character ofits firstanal,and
first radial pieces. Itsunder
sidepresentsmuch
the ap- pearanceof Zeacrinus,though
in thenumber and arrangement
of the partscomposing
thewhole body
itwillbe seento possessallthe essential characters ofthe greatgenusActinocrinus as it isnow
understood.We
place itprovi- sionally inthe sub-genus Amphoracrinus,on
accountofthelateralposition of the anal opening, butwe
suspect it should bemade
the type ofa distinct sub-genus. It differs from Agaricocrinus, inhaving
comparativelymuch
larger firstradial pieces, as well as inthe general formofitsbody,
and
itsmuch
smaller arms,which
are also locatedaround
thesummit,
instead ofaround
thelowerpart of thebody.We
areunder
obligations to Mr. CharlesWachsmuth,
ofBurlington, Iowa, fortheuseoftheonlyspecimenwe have
seen.Locality
and
position. Burlington, Iowa. Burlington Limestone, of theLower
Carboniferousseries.Actinocrinus (Pradocrinus?)amplus.
Body
large, unshaped,composed
ofthin,smooth,orfinelygranuloseplates. Base comparativelysmall,
somewhat
spreading;columnar
facet large, orbetween
one-halfand
two-thirds aswide
asthe base,havingasmall marginalrim.Column
strong, round,and com-
posed ofthin segments near the body,where
it has a veryminute round
central cavity. Firstradial plates ratherlarge, alittlelongerthanwide,and
allapparently hexagonal, therebeing
no
distinctangleatthe middleofthose alternatingwiththe basal pieces. Second radial plates about two-thirds as large as thefirst,nearlyor quite aswideas long,and
all hexagonal. Third radialsalittlesmallerthan the second, hexagonaland
heptagonal in form,and
supporting ontheir superior sloping sides thetwo
first brachial pieces,which
are comparatively large,and
each succeededby
three or fourmuch
smallershort brachials, beforethe
arms
passintodoublealternatingrangesof smallpieces.The
firstanal plateisas large as the first radials,pentagonal in form,and
supportstwo
subhexagonalpieces inthenextrange,abovewhich
there aresome
twelveorthirteenother smallerpieces ofvariousforms.The
firstinterradial plates are alittlelargerthanthesecondradials,irregularyhex- agonal,
and
eachsurmounted by two
rathersmallpieces inthesecondrange,and
three in the next,overwhich
there are six orseven still smaller pieces,making
elevenortwelveineachinterradial space.After the division of the rays on the third
primary
pieces,thebrachials abovethefirstpaircurve nearly horizontally outwards, but are included so as toform apart ofthewalls ofthebody.Beyond
thefourth orfifthbrachial, thearms
consist of a doublerow
of smallalternatingpieces, ofwhich
there are eight or ten ranges,toa pointwhere
thefirstbifurcation ofthe freearms
takesplace.Beyond
thisdivision, thearms
continue to be strong, rounded,and
eachcomposed
ofa double seriesof short alternating pieces,though
thespecimen
1861.]
134 PROCEEDINGS OF THE ACADEMY OP
under
examinationisnotina condition toshow whether
ornottherewereany
otherhifurcations.They
allextend out nearlyhorizontallyatfirst,and
gradu- allycurve upwards. Restingupon
the inner sloping sides of each pair of firstbrachial pieces, thereisa rather large interaxillary piece, with three or fourmuch
smallerpiecesabove.The
vault is moderately convex,and composed
ofinnumerable minute
pieces,and
isprovided witha central, or sub-central proboscis. It appears tohave
continued out over the anusasfarastothe third or fourth ranges of smallalternatingarm
pieces.This species evidently belongs to the
same
group as thaton which
M.de
Vernuil proposedtoestablish thegenusPradocrinus,which
Prof.Koninck
thinks does notdifferfrom Ctenocrinus ofBronn.Locality
and
position. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. CharlesWachsmuth.
Actinocrinus Sillimani.
Body
of moderate size, distinctly stelliform, or pentalobate, asseen from belowor above, inconsequenceofthe deeplysinu- ouscharacter of the interradialand
anal spaces; rapidly spreading from the basetothe thirdradials, which, withthesecondaryand
tertiaryradials,and
brachial pieces, extend out horizontally.Summit
nearlyflatand
provided witha rathersmallsub-central proboscis. Basalpieces short, thickenedand
projectingdown
over thesummit
of the column, so as toforma distinctly trilobate rim, deeply indented at the sutures;columnar
facetconcave,and
ratherlessthanone-thirdthebreadthof the base. First radial plates about as large as theanalpieces,verythickand
prominent; wider thanhigh, three ofthem
heptagonal, (theangle at the middle of theunder
side beingvery obtuse,)and two
hexagonal.Second
radial pieces smaller than the first, thickand
prominent, wider thanhigh,and
hexagonalinform. Thirdradials about thesizeofthe second, wider than long, heptagonal or hexagonal,and
supportingon
eachsuperior sloping side asecondaryradial.Each
ofthelat- tersupportson
itsoutersideaseriesofbrachial pieces,and on
its innerside tertiaryradials,onthesecondofwhich
anotherbifurcationtakesplace,making
sixarms
toeachray, or thirty in the entire series.The
two. secondary,and
thefour tertiaryradials,aswell astwo
orthree of the brachial pieceson each side ofthem, arecoveredinaboveby
vault pieces.The
first anal plate ishexagonal,
and
nearlyas large as the first radial pieces. In thenext range above, itsupportstwo
smaller hexagonalpieces,which
in their turn support three pieces in thenextrange,the middle one ofwhich
is largerand
longer than theothers.On
eachside ofthislargermiddlepiece, there aretwo
other smallerpieces restingupon
thetwo
lateralpieces ofthethird range,and
con- necting withthe vaultabove,and
withthe brachial pieceson eachside.The
firstanalplateisregularlyhexagonal,
and
supportstwo
smallerpieces inthe secondrange, overwhich
there are three or fourstill smaller pieces connect- ingwiththe vaultabove.A marked
feature of this species is the prominence,and
veryprofound sculpturingofitsplates. Itsfirstradialand
firstanalpiecesriseintoelevated transverse nodes,which occupy
nearlytheir entire surface,and
projectbeyond
the base, so as to present a distinct six-lobed outline, asseenfrom below.From
theunder
side ofeachoftheseprominences, oneortwo
short ribscon- nect with thebase,whilesimilarribsconnectthem
with each otheron
each side.A
single, ratherprominent
ribalso passesfrom eachtoa smallernode on
each secondradial pieceabove.The two
second anal pieces,and
allthefirstinterradialsareprovidedinthe middle witharounded, rather small, veryprominent
subspiniferous node.The
third radial pieceshave
a centralprominence, connectingby
short carinae with thenode
onthesecondradialbelow,aswell aswith eachofthesecond- aryradials above.On
the latter pieces, these carinae bifurcate,and
extend along thetertiary radialand
lateralbrachial pieces,leaving deep depressions[June,
NATURAL SCIENCES OF PHILADELPHIA. 135
between.
The upper
analand
interradial plates areconvex, but do not gene- rallyriseinto distinctnodes.Named
inhonorof the venerable Prof. B. Silliman, Sr., ofNew Haven,
Connecticut,who
perhaps didmore
to createaninterest inscientificstudiesand
pursuits, atanearlyperiod in the history of thiscountry, thanany
other personnow
living.Locality
and
position. ClearCreek,Warren
County, Illinois. Burlington Limestone.Genus AGARICOCRINUS,
Troost.Agaricocrinusgracilis.
Body
small, truncato-subglobose exclusive ofthearms
;under
sideconcave, theconcavity extending outtothe middle of the secondradial,firstinterradial,and
second rangeof anal pieces, all ofwhich
are geniculated, orabruptly bentupwards,and
swollen, so asto formacircle ofhemispherical nodesaround
themarginsoftheconcaveunder
side.Anal and
interradial pieces rising verticallyfrom
the marginsof the con- cavitybelow.Dome
rather depressed,and
provided with a short, strong, sub-central spine.Anal
opening small,not protuberant,and
placed abouton
a levelwiththearm
openings,which
are located slightlyabove the middleof the entirebody, including thedome.
Basesmall, concave, nearly or quite hidden
by
the column. First radial platesflat,includedwithin the concavityoftheunder
side,about as wide as long,and
apparentlyallhexagonal. Second radials slightly largerthan thefirst,
and
quadrangularinform. Third radial pieces shorterand
widerthan thesecond,and
each provided withan
obtuse mesial ridge,which
connects withtheprominence
ofthesecondradialsbelow; sub-heptagonal in outline, thesuperioranglebeingrathersalient,and
the slopeson
eachsidesupporting the first brachial pieces. First interradial pieces larger than the first or second radial plates, wider above the geniculation than below; irregu- larly octagonal in form,and
supportingtwo
smaller elongated pieces in thenext range above. Firstanalplate small,and
included within the con- cavity of theunder
side; supportingin the next rangethree largerpieces, the middle oneofwhich
issmallerthan the othertwo.Above
these fivesmaller pieces areseenin thenextrange,which
is as far asthey can be counted in the specimen examined. After the first division on thethird radial pieces, thearms
are each at firstcomposed
of a single nodosebrachial piece, but almost immediately passintoadoubleseriesofshort alternating pieces,which
supporta closelysetrangeoftentacleson
eachside within.As
theydo
not bifurcate again, there arebuttwo arms
toeachray, or tenintheentireseries.Near
thebasethecolumn
israther slender,round,and composed
of alternately thickerand
thinnerplates, withavery smallround
central perforation.The
surfaceisfinelyand
regularlygranulosewhere
well preserved, but generally appearstobe smooth.Locality
and
position. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. CharlesWachsmuth.
Platycrinus Mui/n-BRAcniATus.
Body
below thesummit
of thefirstradial pieces depressed,basin-shaped. Basediscoid,pentagonal in outline,moder-
atelyconcave below,and
not prominentenough
to be seen in a side view;columnar
facetaboutone-third as wideasthe base. First radial plateslarge, broader thanhigh,and
wideningrather rapidlyupwards
fromthebase; facetforthe reception ofthe secondradial piecesprominent, extending
down
appa-rently below the middle of the plate. Second radial pieces small, trian- gular,widerthanlong,
and
extendingobliquely outwardsand upwards
from the firstradials.After dividingon the secondradials, the
arms
bifurcateagainon
thesecond piece,and
thetwo
innerdivisions,which
are largerthan theothers, bifurcate again onthesecondpiece,abovewhich two
ofthe sub-divisions insome
ofthe1861.]
136 PROCEEDINGS OF THE ACADEMY OF
rays again divide once more,
making
seven rays tosome
ofthearms and
eightto others.The arms
are rounded, very graduallytapering,and
eachcomposed
of adoubleseries of alternatingpieces, supportingtentacleswithin.The
suturesseparating thefirstradials, as well as thosebetween them and
the base, are rather distinctlygrooved, as well as thosebetween
the succeeding pieces,up
tothelast bifurcation ofthefreearms.The
surface ofthefirstradial platesisratherconcave,and between
thepro- jectingmargin
ofthe sinus above,and
the marginal grooves; the concave space beingsometimes marked
by veryfainttraces ofsmallradiatingcorruga- tions.Very
smalllongitudinalobscurestriaeor wrinkles,canalsobe seenby
theaid ofamagnifieron
theouterside ofthe arms, abovethelastdivisions.ThisspeciesisalliedtoP. corrugatus of
Owen and Shumard,
butdiffersinthe style ofitssurfacemarkings, being in fact nearly entirely smooth. It also differsinhavinga distinctmarginal groove alongthe sidesand
baseofits first radialplates. Itsbody
isalso proportionallyhighertothesummit
ofthefirst radials.Locality
and
position. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. CharlesWachsmuth.
Genus CYATHOCRINUS,
Miller. 1821.Cyathocrinus
Wachsmuthi. Body
depressed, obconical, or subturbinate.Baseofmoderatesize, low,
and
distinctlypentagonal, the angles formedby
the extremities ofthe plates alittleincurved.Columnar
facetcovering about one-thirdto one-fourth of each basal piece.Column
obscurelypentagonal nearthe base, the angles beingrounded
; central perforation comparatively largeand
pentagonal. Subradialplatesfiveor sistimesas large as thebasal pieces,aboutaslongas wide, three ofthem
hexagonal,and two on
the anal sideheptagonal, allindented or incurvedat thesidesand
attheupper
angles.First radials largerthan thesubradials,
unequal
insize,and
widerthan long; allheptagonal,inconsequenceofthetruncationofthe superior lateral angles apparentlyforthe reception ofsmallinterradials,each havingtheanglesbelow
distinctlyindented,and upper
side truncated,and
moderately concaveforthe reception of thesucceedingplates. Secondradialsveryshort ornearlylinear,and
abouttwo-thirds aswide as the first. Third radials generally a littlenarrower,
and
longer than the second,and
apparentlytriangular in form.Sub-analpiececomparativelylarge,quadrangular,
and
indentedattheangles;firsttrueanalplate largerthan the sub-analpiece,heptagonalin form, resting
upon
averyshortupper
truncatedside ofoneofthe subradials,and
connect- ingon
eachsidewiththefirstradials; itsright inferior sloping side alsorest- ingagainst thesub-analpiece.The arms
after dividingon
the thirdradials, are strongand rounded
ontheouterside; oneofthe divisions ineachofthe rays,exceptinganterior one, bifurcates againon
the fourth piece. All the divisionsand
subdivisions are rounded, gradually tapering,and composed
eachofasingle series of pieces as longas, or a little longerthan
wide,and
giving off at intervals oftwo
or three pieces alternatelyon
opposite sides, rather strong jointedlateraldivisions,which
extend obliquelyoutwardsand
bifurcateseveral times.The
surfaceseems
tobe merelyirregularlygranulose.On examining
itclosely, however,traces ofvery smallradiating slightly raised linesareseenon
thesubradialand
radial plates, as well asextendingup
theprincipal divisions of thearms.
We
take pleasureindedicatingthisspecies to Mr. CharlesWachsmuth,
of Burlington, Iowa,towhom we
areindebtedforthe use ofthespecimen
de- scribed.Locality
and
position. Burlington, Iowa. Burlington Limestone of theLower
Carboniferousseries.Genus BTJRSACRINTJS,
N.G.(0vp<raapurse; x/wvocalily, inallusion tothe purse-like form ofthetypical species, asseenwithits
arms
folded together.)[June,
NATURAL SCIENCES OP PHILADELPHIA. 137
Generic formula.
Basalplates, 5?
Subradialplates, 5; fourhexagonal
and
one pentagonal.Radialplates,
2X5.
Anal
plate, 1.Interradialplates, none.
Arms,
10, bifurcating.The
crinoidupon which we
proposetofoundthisgenus, hasmuch
the ap- pearanceofanIchthyocrinus,withwhich
genusitseems
toagree, exceptinginhaving
truesubradial plates,and
but two, instead of threeprimary
radial plates ineach ray; alsoin the possessionofa distinctanalplate.Notwithstandingitsgeneralsimilarityto Ichthyocrinus, itsstructureis
more
nearlylikethat of Cyathocrinus,from which
it differsmainly
inhaving
only two, instead of threeprimaryradial pieces ineachray,and much
broaderand
flatterarms,
which
connectlaterally as inIchthyocrinus, so as toleaveno
in- terradial spaces.Bursacrinus
Wachsmuthi. Body
below thesummit
ofthefirstradial plates rather broad turbinate, or rapidlyexpanding
from below. Baseunknown.
Subradialplates ofmoderatesize, alittlewider thanlong,
and
allhexagonal, excepting oneon
the anal side,which
is larger than theothers,and
hept- agonalinform; theangles at themiddleoftheunder
side of each beingless salientthanthatabove. First radial platesabout one-third larger than the subradials,near twice as wide as high,and
all pentagonal, theupper
side beingtransversely truncated.Second
radial pieces of thesame
sizeand
form asthefirst, but invertedso as tobring the truncated side below; supportingon
their superior sloping sidesthe firstdivisions ofthe arms,which
are broad,flat,
and
connectedlaterallywith each otherall around.Anal
piece rather small,longer thanwide, heptagonal, the angle at the middleofthesummit
beingmore
salient than the others; supportedupon
the short truncatedupper
side ofoneofthesubradials,and
connectingon
eachside with thefirstand
secondradialplates,and
the first of thebroad secondaryradial orarm
piecesabove.
Afterthefirstdivision
on
the second radials, thearms
bifurcate againon
thesixth oreighthpiece, abovewhich
oneisseen to bifurcate againon
the twelfth piece,which
isasfarasthey can betraced inthe only specimenseen,though
theyseem
tobelongand
probablybifurcateonceorofteneraboveBetween
thedivisionson
thesecondradial pieces,and
thenext bifurcation above, theyareverywide, flat,and composed
of short, slightlywedge-formed
pieces,which
aresquarely truncatedon
eachside.The
nextdivisionsabove these are a littlemore
than half as wide,and composed
of a single series of piecesbearing near thesame
proportions oflengthand
breadthasthose below.The
surfaceisfinelygranulose,though
there areno
traces of nodes, costse,or other prominenceson any
oftheplates.The
sutures aremerely
linear,and>not impressed.
We
take pleasurein dedicating this interesting species, (the typeof anew
genus,) to Mr. CharlesWachsmuth,
of Burlington, Iowa,who
discovered the only specimenwe have
seen.Positionandlocality. Burlington Limestone. Burlington, Iowa.
Genus POTERIOCRINUS,
Miller, 1821.Poteriocrinus? enormis.
Body
small, irregularlycup-shaped; sidessome- what
convex,expanding
from the base; breadth greater than theheight.Basesmall,spreading from the column, above
which
theplates areseenpre- senting small pentagonal faces. Subradial plates comparatively large,un-
equal, hexagonal in form,excepting oneon
the anal side,which
ismuch
larger than the others,
and
sub-heptagonal in outline. First radial plates1861.] 10
138 PROCEEDINGS OF THE ACADEMY OF
larger than the smaller subradials, longer thanwide,
and
irregularly sub- hexagonalorheptagonal; facet for the reception ofthe secondradials small, not protuberant outwards, shallowand
aboutone-third aswideas theplates.Arms
above thefirst radial piecesveryslender, cylindrical,and composed
of a singleseriesofsegments fromtwice to three or fourtimes aslongaswide.In
some
ofthe rays thefirstdivision takes placeon
thesecond, in otherson
thethird,and
inthe anterior ray on the fourth piece above thefirstradials, afterwhich
theybifurcate irregularly once, twice, or oftener,on
thesecond, third or fourth piece.The
firstanalplateis rather large,and
restsupon
theupper
truncatedside ofthe largest subradial plate, so as to project considera- bly above thefirst radials. Its left side curves inwards,and
its right con- nectswith anotherplate ofnearlyitsown
size restingupon
a sloping side of thefirstradial on theright.Above
theseareseenseveralotherplates,which
form togetherakindofslenderlateral trunk,or proboscis, rising likean arm on
arange with thetruearms.Some
littledistance above, itcurvesinwith itsupper
extremitybetween
the arms, leaving atitsbase,on
theleft,a cavity oropening, passing apparentlyintothebody between
itand
the firstarm on
that side.The
surfaceisfinelygranulose,and
the suturesindistinct.The column
is small, round,and composed
of nearly equal, rather short joints, near the base.A
verymarked
feature ofthisspecies,isitspeculiarity ofhaving apparently a slender proboscismuch
likean
arm, rising from the anal side,withan
openingbetween
its left sideand
one of thearms. Thisissoanomalous
a character, thatifwe
were sureitisnotdue
tosome
accident,we would have
regardedthe species asthe typeofanew
genus.Locality
and
position. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. Chs.Wachsmuth.
Poteriockinussub-impressps.
Body
obconical. Base formingashallowcup
abouttwice aswide as high,expanding
moderately from thesummit
ofthecolumn
;composed
of plateswhich
are aboutashighas wide,and
pentagonal in form, the angleatthe
middleof theupper
side of each beingalittlein- dented. Firstradialssomewhat
smallerthan thesubradials, widerthanlong, pentagonal,orsome
ofthem
hexagonal,and
truncatedabove
forthereception ofthesecondradials. First anal or sub-anal plate, a little largerthan the basal pieces, pentagonal,and
restingbetween
theupper
sloping sides oftwo
of thesubradial pieces; second analpiece ofthesame
sizeasthefirst, hex- agonalin form,and
restingupon
theupper
truncatedside ofoneofthe sub-radials, whileitsleftsideconnectswith one of thefirstradials,
and
its right with oneside ofthefirstanalpiece,and
with a thirdhexagonalpiece restingupon
it. (Succeeding partsunknown.)
The column
is comparatively strongat its connection with thebase,nearwhich
itiscomposed
ofrather thinsegments, connectedby
crenulated sutures;itscentral perforationisofmoderatesize
and
pentagonal.The
surfaceseems
to be granulose,and
the subradialpiecesshow
a very slighttendencyto develope 9hort costcenear the sutures on eachside,and
below,as well assometimes
attheirconnection withthefirstradialsabove.The round
indentations atthe anglesofthe subradialand
firstradial plates, presenta rathermarked
character inthisspecies.Locality
and
position. Burlington, Iowa. Burlington Limestone. Mr.Charles
Wachsmuth's
collection*Poteriockinus tenuibrachiatfs.
Body
small, calyculate, or turbinatebelow thesummit
of thefirstradial plates. Base small,formingalow pentagonal saucer-shapedcup,composed
of small plates,showing
a pentagonal outline abovethecolumn. Subradialplates ratherlarge,aboutaswideas long,three hexagonal,and two
on the analside heptagonal,and
alittlelonger than the[June,
NATURAL SCIENCES OF PHILADELPHIA. 139
others. First radial plates
somewhat
largerthan thesuhradials, wider than longand
pentagonal in form; facet for the reception of the secondradials moderately prominent, alittle concave,and
from one-half to two-thirds the breadthofthe plate.Anal
plates three, thefirst(orsuhanalpiece)hexagonal,and
restingbetween
the upper sloping sides oftwo
of the subradial pieces, whileanotheron
theleft restsagainstthis,and upon
thesuperiortruncated side ofoneof thesubradials.A
third pieceis supportedon
theupper
trun- cated side of the subanal piece,and
projectsmore
thanhalf itslength above thefirst radialon
its right.The
succeedingprimary
radial piecesafterthefirst,are distinctly smaller,
and
alittlewider thanlong. Inallexcepting the anterior ray,where
the bifurcationtakesplaceon
thefifthplate,thefirstdivi- sion of thearms
takes placeon
the fourthprimary
radial.Above
this the arms,which
are very long, slenderand
rounded, divideagainon
thefourth piece, afterwhich
the divisions bifurcate three or four times,and become
veryattenuate.Each
divisioniscomposed
ofa singleseriesof pieces, usually abouttwice aslongaswide.The
proboscisconnectsdirectlywith the analplatesalreadydescribed,and
is
made up
ofhexagonalplates, along the sutures ofwhich, distinct vertical rangesofrather largeand
distinctpores are seen.The
entire surfaceisfinely granulose.The
suturesare linearand
not groovedor impressed. This spe- ciesissimilar to P. calyculatus of Hall,butmay
beat once distinguishedby
itssuturesnot being excavated,
and by
itsmuch more
slender arms,which
arecomposed
of elongate, instead of shortwedge-formed
pieces.Locality
and
position. Burlington, Iowa. Burlington Limestone. Collec- tionofMr. CharlesWachsmuth.
Poteriocrinus carinatus.
Body
small, basin-shaped or rather rapidly spreading below the arms. Base verysmall,having
the formofapentagonal star,the angles ofwhich
projectbut slightlybeyond
thecolumn.
Subradial pieces small, aboutaswideas long, four ofthem
hexagonal, (theform
ofthe oneon
theanalsideisnot distinctly visible in thespecimen examined
;)all ratherprominent,and
provided with avertical carinaneartheupper
angle.First radial pieces abouttwice as large as the subradials, aswide again as high,
and
pentagonalin form,theupper
sidebeingtruncated,and
longerthan
either ofthe others.Second
radials slightly larger thanthefirst,widerthan
high, quadrangular,and
alittleconstrictedaround
the middle.Thirdradials about thesizeof the first,pentagonal in form,
and
like the secondslightlyconstricted, theupper
angles being rathersalient.The
anal plates arenotallpreservedinthe specimenbefore us,though we
canseethat thefirstorsubanalpieceisofmoderate
size,pentagonal in form,and
extends sofardown between two
of the subradials, as to connect (apparently)by
a veryshortside, with theproduced
extremityofone of thebasal pieces. Its rightsuperior sloping side supports oneedge of a firstradial above,and
itevidently supported another piece
on
its superior truncated edge, while itconnects
on
theleftwith anotherrestingon
theupper
truncatedside ofone
ofthesubradials.Afterthefirstdivision of the third radials