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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. Corbicula

Agrensis

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.,is

much more

inequilateral.

Descriptions of

new

PalaeozoicFossils from Illinois

and

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-hemispherical

below

the

summit

ofthefirstradials,

rounded on

the

under

side,height about two-thirds thebreadth. Base saucer-shaped, ornearlyfourtimes as

wide

as high, pentagonalinoutline, the sidesbeing nearlystraight or slightlyconcave, sutures anchylosed;

columnar

facet large,itsbreadthequallingabouthalfthat ofthebase, concave,

margined by

aslightly raised

somewhat

undulated rim,

and

perforated

by

a large central opening. First radial plateslarge, sub- quadrangularingeneraloutline, but havingthe superior lateral angles trun- cated for the reception of the anal

and

interradialpieces, wideningalittle fromthebase

upwards

; facetforthe reception of the second radial pieces

[June,

(2)

NATURAL SCIENCES OF PHILADELPHIA. ]29

prominent, nearone-third aswideastheplate,

and

extending

down between

one-third

and

one-halfitslength. Secondradial pieces small, extending out nearlyhorizontallyfromthefirst;

round

below,

and

presentinga pentagonal outline, as seenfrom the

under

side, supporting

on

their superior (outer) slopingsides, the

two

firstdivisions ofthearms. Firstanal piece rather large foraspecies ofthisgenus,apparently pentagonal,

and

extending

down between

thefirstradials,nearlyasdeepasthe articulatingfacetssupportingthesecond radial pieces. (Otherparts

unknown.)

The

suturesseparatingthefirstradial platesfrom eachother,

and

from the base, are rather distinctly canaliculated, inconsequenceofthe bevelingofthe edgesof theplates.

The

surfaceisfinelygranulose,

and ornamented by

small obscurely subnodosecostae,of

which

there are

two on

thebase passing

around

nearthemargin. Threesimilarcostae

ornament

thefirst radial plates,being arranged parallel to the basal

and

lateral margins, but

becoming

nearlyor quite obsoleteabovethemiddle.

Named

in

honor

ofProf. Richard

Owen,

ofthe Geological

Survey

ofIndiana.

Localityandposition. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. Charles

Wachsmuth.

Platycrinusscobina.

Body

rather small,cup-shapedorsubturbinatebelow the

summit

ofthefirstradial pieces. Base basin-shaped, about twice aswide as high,

and

rather

more

thanequalling one-third the heightof the

body

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 little

upwards

fromthe base, presentingasubangularoutline, the superior lateral angles being truncated forthe reception ofthe anal

and

interradial pieces; facet for the reception of thesecondradial piecenot protuberant, concave,ratherlessthanone-thirdthe breadthofthe

upper

side of thefirstradial plates,

and

extending

down

about one-fifththeir length. Secondradial pieces small, triangular,

and

supporting

on

their superior sloping sidesthefirstdivisions ofthearms. After dividing

on

thesecondradial pieces, the

arms

divide again

on

thesecondpieceabove,

beyond which

theyarelong,slender,

and

apparentlysimple. After thesecond bifurcation, theyareeachatfirst

composed

ofa singleseries of

wedge-shaped

pieces,but gradually pass intoa doublealternating series of pieces, eachof

which

isaboutaslongas wide.

The

surface ofthe basal

and

firstradial platesis

ornamented

with

numerous

small, rathersharplyelevated, irregularlyarrangednodes, or coarse granules, so as topresenta rasp-likeappearance.

The

suturesare closelyanchylosedin the base,

and

well defined

between

thefirstradialplates.

Initssurface

markings

thisspeciesis

much

like P. Wortheniof Hall,but it differsinhavinga distinctlyprotuberant, instead of a flat or concave base,

and

inhaving butfour

arms

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. Base

much

depressed, largely

and

deeply excavated below, with a

narrow prominent

marginal rim,

which

is notched at the sutures,

and somewhat

undulated. First radial plates broaderthanhigh, widening moderately

upwards and

presenting a subquadrangular outline, but really hexagonal, in consequence of the truncation of the superior lateral angles for the reception of the interradial

and

anal plates; sinus in the

summit

of each, for the reception of the second radials, deep, semi- circular,

and

equalling about half the breadth of the

upper

side; surface ofeach

ornamented by

a very prominent, sharply elevated carina,

which

passesacrossnear the lowerside,

and

is

waved

or oftenbroken

up

intoisola- ted prominences. Second radial pieces triangular, wider than long,

and

1861.]

(3)

130 PROCEEDINGS OF THE ACADEMY OF

nearly entirely received within the sinus, in the

upper margin

ofthe first radial pieces. Firstanal

and

first interradial plates of apparently ahout the

same

size, theformer connecting with a range of smallplates above,

which

form the

under margin

ofthe lateral analopening.

The

arms, afterthefirstdivision

on

the second radial plates, divideagain on the second piece, above

which

the

two

inner branchesbifurcateagain

on

thesecond piece, thus

making

six

arms

in each ray seen in the

specimen under

description.

Above

thelastdivisionthe

arms

are slender, very gradu- allytapering,

and

each

composed

ofadouble seriesofsmallalternating pieces, (excepting near the points of bifurcation,)

and

support

on

theirinner side ratherclosely setrangesof tentacles.

The column

isalittlecompressed,

and composed

of rather thin pieces,with

prominent

crenulated margins near the base.

Locality

and

position. Burlington, Iowa. Burlington Limestone. Collec- tion ofCharles

Wachsmuth.

Genus FORBESIOCRINUS, Koninck and Le Hon.

Fokbesiockinds Moxeoensis.

Body

below the free

arms

apparentlyskort- turbinate, or subglobose,

composed

of nearly smooth, rather thick plates, connected

by

linear sutures. Base small,

and

nearly hidden

by

thecolumn.

Subradialplates ofmoderatesize, four of

them

pentagonal,

and

one

on

the anal side apparently hexagonal, with

unequal

sides. First radials about twice as wide as high, hexagonal in form,

and

nearlytwice as large asthe subradials. Second, third

and

fourth radials, in

two

ofthe rays, (and the fifth

and

sixth in another,)all nearlyofthe

same

length,hexagonal inform

and

abouttwice aswide as long. Last

primary

radial pieces ofnearly the

same

size as the others,

and

supporting

on

their superior sloping sides the secondaryradials.

Of

the

numerous

interradials,the first is about thesizeof the subradial pieces, hexagonal in form,

and

supports

two

smaller pieces inthesecond range.

Above

these four or five occurinthenextrange, inoneinterradial space,

which

isasfar

up

asthey can be counted in the

specimen examined, though

it isevidentfrom the breadthofthe interradial spaces, thatthey

must

increaseatthe

same

rateforseveralranges above. (Analplates

unknown.)

The column

is

rounded and

comparatively thick at its junction with the base, from

which

ittapersgradually towardsthe lower extremity.

Near

the baseitis

composed

ofextremelythin, equalsegments, connected

by

minutely crenulatedsutures. Farther

down

itgradually passesinto a series of alter- natelythicker

and

thinnerpieces.

After the first division of the rays

on

thelast

primary

radial pieces, the

arms

divide several times,

and

appear to give off lateral branches, but our specimenisnotina condition toenableustodetermine

how many

pieces in- tervene

between

the points of division, nordo they

show whether

ornotthere are

any

interaxillary pieces.

The

specimenbeforeuspresents the peculiar

and anomalous

appearanceof

having

asmallfalse

arm

arising directlyfrom the

summit

of the

upper

trun- catedsideofthelargest subradial piece. It

seems

eventobe inserted into a sinusinthe

upper

sideofthe subradial, yet

we can

scarcely believeitisany- thing but oneofthe smallerdivisions of thearms,accidentally

broken

off

and

placedinthat position.

As

nearas

we

can determine from a description alone, this species appears tobe

somewhat

closely relatedto F.exculptus, (Onychocrinusexsculptus,

Lyon

and

Cassiday,

Am.

Jour. Sci.vol.29,N. S.page 78,)butdiffersinhavingless

produced

basal pieces, while the

upper

angles of the subradials are obtuse instead of "quite sharp." Italso

seems

to

have two

or three

more primary

radial pieces inone ray than occurin

any

ofthose ofthespecies described

by

Lyon and

Cassiday.

Again

itssurfaceappears tobe

smooth

instead ofgranu-

[Juue,

(4)

NATURAL SCIENCES OF PHILADELPHIA. 13l

lose,

and we have

notbeenable to see

any

indications of the small patelloid pieces between theradial

and arm

pieces asin F. exscu'ptus.

Locality

and

position. River Bluff, near the south lineof

Monroe

County,

Illinois.

Keokuk

Limestoneofthe

Lower

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 are

some

differ- ences inthe

number and

arrangementoftheanal

and

interradial plates. It alsodiffersinhavingits

column

almostexactly cylindricalforadistance of at least four inches below the base, while that of F. Agassizi,isdescribedas

"rapidlytaperingbelowthe

summit." We

suspectit

may

provetobeadis- tinctspeciesfromthat described

by

Prof.Hall, but as it agreeswithhisdes- cription

and diagram

in

most

ofitscharacters, excepting the points ofdiffer- ence

we have

mentioned,

we

merelycall attention to it as a varietyofthat species, until

we

can

have

an opportunityto

compare

better

examples

of it with authentic specimensor figures ofProf. Hall's species. Should it prove tobedistinct, itcan takethe

name

giganteus,

which would

be veryappropri-

ate, sinceitisthelargestspecies of thatgenus

known,

the length of its

body

tothe

commencement

ofitsfree

arms

being near3-30inches,

and

itsbreadth apparently about the same. Its

arms

are proportionally short,

and

bifurcate frequently.

Localityandposition. Burlington, Iowa. Burlington Limestone.

Genus ACTINOCRINUS,

Miller, 1821.

Actinocrinusdodecadactylus.

Body

rather small, subglobose;

summit and

calyx below the

arms

of nearly the

same

size; breadthalittlegreaterthan

the-height;

composed

of slightly convex,

smooth

or subgranulose plates,

which

areconnected

by

moderatelydistinctsutures. Base small,

much

de- pressedor subdiscoidal, obtuselyhexagonalin outline,withthree otherobtuse retreatinganglesatthesutures. First radial plates wider thanlong, three of

them

regularlyhexagonal,

and two

heptagonal. Secondradial pieces

much

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

the

two

superior sides each about equalling the base. In the

two

posterior rays, the third radial pieces each support on one of their superior sloping sides a large brachial piece,

and on

the otherasecondaryradial ofnear the

same

size,which,initsturn, supports

two

brachial pieces,

making

three

arms

toeach oftheserays;whileinallthe others,

two

brachial pieces rest directly

upon

the thirdradial, thus

making

only twelve

arms

inthewholeseries.

The

firstanal plateisaboutaswideas thefirstradials,buta littlelonger, being longer than wide, instead ofthe re- verse. It isregularlyheptagonal,

and

supports

on

eachsuperiorlateralslop- ingside,asmaller heptagonalpiece; while

an

elongated, coffin-shaped piece rests

upon

its short superiortruncatedside,

between

the

two

latter,

and

ex- tends up, flankedoneither side

by

thefirstbrachials, toits connection with the

summit. Each

oftheinterradial spacesisfilled

by

a single ovate, octago- nalpiece, aboutas large asthe second

and

third radial pieces takentogether.

The

vaultis

composed

ofrather large,

somewhat

regularlyarrangedplates

which

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 very

narrow and

apparently

1861.]

(5)

132 PROCEEDINGS OF THE ACADEMY OF

cylindrical from the base to the top of the third radial plates,above

which

the secondaryradial

and

brachial piecescurve abruptly outwardstothe base of thearms, so astoform withthe ventricose

summit

a

much expanded

vis- ceral cavity, entirelyabovethe basal

and primary

radial plates. Baseun-

known

; firstradials

unknown,

excepting from

some

remaining portions of their

upper

ends,

which show

that theyare comparativelylarge. Second radialsverysmall, alittlewider thanlong, (those seen)irregularlypentagonal in form, oneofthe sidesbeing

much

shorterthan the others. Thirdradials aslongasthefirst,

and

nearlyone-third wider, (the only

two

visible inour specimen,)hexagonal in form,

and

each supporting

on

its superior sloping sides

two

secondaryradialsofaboutits

own

size.

Each

oftheseis

surmounted by

a

somewhat

largersecond secondaryradial,

which

initsturn supports

two

firstbrachial pieces, eachof

which

issucceeded

by

a second, from

which

the free

arms

aregivenoff.

The two

series of secondary radials,

and

the

fmr

series of brachial pieces in each ray, connect laterally, so as to leave

no room

forinteraxillary

and

interbrachial pieces. Interradial plates

two

or three, thefirstbeing aboutthe

same

sizeasthesecondradials,

and

hexagonal orheptagonalinform.

Above

thisthere areoneor

two

smallpieces, of variable size

and

form,over

which

the secondaryradials,

and

thelateral seriesofbra- chial pieces of the rays

on

eachside, connectallthe

way up

tothefreearms, insuch a

manner

astoleave

no

spacesforinterradialsabovethose just descri- bed. (Analplates

unknown.)

Dome

hemispherical,

composed

ofpentagonal, hexagonal,

and

heptagonal plates ofnearly uniform size, each of

which

is provided witha spine-like tubercle. Proboscis central or nearly so.

Arm

openings twenty. Surface

smooth

orobscurely granulose; smallratherpointedtubercles are also seen

on

the second

and

third radial plates, first interradials,

and

firstsecondary radials.

It ispossible thisCrinoid

may

bespecificallydistinctfrom A.pyriformis, of

Shumard,

butitagreeswithitinso

many

respects that

we

do not feel fully warrantedinregarding itas specifically distinct. Its

most

important differ- encesare the sub-spiniferous character ofitsplates,

and

the possession ofonly

two

or three interradial plates, instead of six in eachinterradial space. It alsodiffersinhavinga

more

ventricose

dome,

while the inferior half of its

body

is

more

abruptlycontractedbelow the arms.

Locality

and

position. SaltLickPoint,

Monroe

County,Illinois.

Where

it

occursinbedsofthe

same

age asthe

Chouteau

LimestoneofProf. Swallow.

Actinocrinus

(Amphokacrinus

?)cofCAvcs.

Body

small, subglobose,broader thanhigh, alittleoblique;

summit

nearlyflat;

under

side

rounded and

dis- tinctlyconcave, sides rising vertically ornearlyso. Surface

smooth

or sub- granulose. Basesmall, concave,

and

entirelyincluded within the concavity ofthe

under

side. First radial platescomparativelylarge, convex,

and

curv- ing under, so as to form a part ofthe concavity below;

two

of

them

hept- agonal,

and

threehexagonal. Secondradial pieces(wantingin

two

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 supporting

upon

its superiorsloping sides the first

brachialpieces,

which

forma part ofthewalls of thebody. First interradial pieces, comparativelylarge, oraboutone-half thesizeofthefirstradial plates, nine-sided, the superior sloping sides ofeach supporting one side of

two

of thebrachial pieces, while

two

very smallpiecesrest

upon

the middle ofthe

summit, and

connect withthevault above,

and

with the brachial pieces

on

eachside. Firstanalpiece alittlelargerthanthefirstradials, heptagonalin form,

and

supportinginthenext rangethreepieces, the

two

lateral of

which

are larger than the other,

and

connect above

on

their slopingsides, with brachial pieces,whilethemiddlepiece

between

theseisirregularlyhexagonal,

[June,

(6)

NATURAL SCIENCES OF PHILADELPHIA. 133

and

supports threevery smallpieces in the next range,

which

connectwith theanalopening,

and

thevault pieces above,

and

withthe brachials

on

each side.

The

vaultis

made up

of afew comparativelylarge pieces,the central oneof

which

isalittle

more convex

than the others.

The

anal opening is verysmall, lateral,orabout

on

the

same

horizon as the

arm

openings,

and

surrounded

by

onlyfiveplates,

which

arenot protuberant. Thereare twelve small

arm

openings arranged

around

the

margin

ofthe

summit,

three toeach ofthe posterior rays,

and two

toeachoftheothers.

The arms would

appear, fromthesmallsizeoftheopenings,

and

the very small articulating surfaces for thereception of thefirst free

arm

pieces, to be veryslender

and

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

otherActinocrinus

known

tous, in theconcavityofthe

under

side,

and

the incurved character ofits firstanal,

and

first radial pieces. Its

under

sidepresents

much

the ap- pearanceof Zeacrinus,

though

in the

number and arrangement

of the parts

composing

the

whole body

itwillbe seento possessallthe essential characters ofthe greatgenusActinocrinus as it is

now

understood.

We

place itprovi- sionally inthe sub-genus Amphoracrinus,

on

accountofthelateralposition of the anal opening, but

we

suspect it should be

made

the type ofa distinct sub-genus. It differs from Agaricocrinus, in

having

comparatively

much

larger firstradial pieces, as well as inthe general formofitsbody,

and

its

much

smaller arms,

which

are also located

around

the

summit,

instead of

around

thelowerpart of thebody.

We

are

under

obligations to Mr. Charles

Wachsmuth,

ofBurlington, Iowa, fortheuseoftheonlyspecimen

we have

seen.

Locality

and

position. Burlington, Iowa. Burlington Limestone, of the

Lower

Carboniferousseries.

Actinocrinus (Pradocrinus?)amplus.

Body

large, unshaped,

composed

of

thin,smooth,orfinelygranuloseplates. Base comparativelysmall,

somewhat

spreading;

columnar

facet large, or

between

one-half

and

two-thirds as

wide

asthe base,havingasmall marginalrim.

Column

strong, round,

and com-

posed ofthin segments near the body,

where

it has a very

minute 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, hexagonal

and

heptagonal in form,

and

supporting ontheir superior sloping sides the

two

first brachial pieces,

which

are comparatively large,

and

each succeeded

by

three or four

much

smallershort brachials, beforethe

arms

passintodoublealternatingrangesof smallpieces.

The

firstanal plateisas large as the first radials,pentagonal in form,

and

supports

two

subhexagonalpieces inthenextrange,above

which

there are

some

twelveorthirteenother smallerpieces ofvariousforms.

The

firstinterradial plates are alittlelargerthanthesecondradials,irregularyhex- agonal,

and

each

surmounted by two

rathersmallpieces inthesecondrange,

and

three in the next,over

which

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, the

arms

consist of a double

row

of smallalternatingpieces, of

which

there are eight or ten ranges,toa point

where

thefirstbifurcation ofthe free

arms

takesplace.

Beyond

thisdivision, the

arms

continue to be strong, rounded,

and

each

composed

ofa double seriesof short alternating pieces,

though

the

specimen

1861.]

(7)

134 PROCEEDINGS OF THE ACADEMY OP

under

examinationisnotina condition to

show whether

ornottherewere

any

otherhifurcations.

They

allextend out nearlyhorizontallyatfirst,

and

gradu- allycurve upwards. Resting

upon

the inner sloping sides of each pair of firstbrachial pieces, thereisa rather large interaxillary piece, with three or four

much

smallerpiecesabove.

The

vault is moderately convex,

and composed

of

innumerable minute

pieces,

and

isprovided witha central, or sub-central proboscis. It appears to

have

continued out over the anusasfarastothe third or fourth ranges of smallalternating

arm

pieces.

This species evidently belongs to the

same

group as that

on which

M.

de

Vernuil proposedtoestablish thegenusPradocrinus,

which

Prof.

Koninck

thinks does notdifferfrom Ctenocrinus ofBronn.

Locality

and

position. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. Charles

Wachsmuth.

Actinocrinus Sillimani.

Body

of moderate size, distinctly stelliform, or pentalobate, asseen from belowor above, inconsequenceofthe deeplysinu- ouscharacter of the interradial

and

anal spaces; rapidly spreading from the basetothe thirdradials, which, withthesecondary

and

tertiaryradials,

and

brachial pieces, extend out horizontally.

Summit

nearlyflat

and

provided witha rathersmallsub-central proboscis. Basalpieces short, thickened

and

projecting

down

over the

summit

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,verythick

and

prominent; wider thanhigh, three of

them

heptagonal, (theangle at the middle of the

under

side beingvery obtuse,)

and two

hexagonal.

Second

radial pieces smaller than the first, thick

and

prominent, wider thanhigh,

and

hexagonalinform. Thirdradials about thesizeofthe second, wider than long, heptagonal or hexagonal,

and

supporting

on

eachsuperior sloping side asecondaryradial.

Each

ofthelat- tersupports

on

itsoutersideaseriesofbrachial pieces,

and on

its innerside tertiaryradials,onthesecondof

which

anotherbifurcationtakesplace,

making

six

arms

toeachray, or thirty in the entire series.

The

two. secondary,

and

thefour tertiaryradials,aswell as

two

orthree of the brachial pieceson each side ofthem, arecoveredinabove

by

vault pieces.

The

first anal plate is

hexagonal,

and

nearlyas large as the first radial pieces. In thenext range above, itsupports

two

smaller hexagonalpieces,

which

in their turn support three pieces in thenextrange,the middle one of

which

is larger

and

longer than theothers.

On

eachside ofthislargermiddlepiece, there are

two

other smallerpieces resting

upon

the

two

lateralpieces ofthethird range,

and

con- necting withthe vaultabove,

and

withthe brachial pieceson eachside.

The

firstanalplateisregularlyhexagonal,

and

supports

two

smallerpieces inthe secondrange, over

which

there are three or fourstill smaller pieces connect- ingwiththe vaultabove.

A marked

feature of this species is the prominence,

and

veryprofound sculpturingofitsplates. Itsfirstradial

and

firstanalpiecesriseintoelevated transverse nodes,

which occupy

nearlytheir entire surface,

and

project

beyond

the base, so as to present a distinct six-lobed outline, asseenfrom below.

From

the

under

side ofeachoftheseprominences, oneor

two

short ribscon- nect with thebase,whilesimilarribsconnect

them

with each other

on

each side.

A

single, rather

prominent

ribalso passesfrom eachtoa smaller

node on

each secondradial pieceabove.

The two

second anal pieces,

and

allthefirstinterradialsareprovidedinthe middle witharounded, rather small, very

prominent

subspiniferous node.

The

third radial pieces

have

a centralprominence, connecting

by

short carinae with the

node

onthesecondradialbelow,aswell aswith eachofthesecond- aryradials above.

On

the latter pieces, these carinae bifurcate,

and

extend along thetertiary radial

and

lateralbrachial pieces,leaving deep depressions

[June,

(8)

NATURAL SCIENCES OF PHILADELPHIA. 135

between.

The upper

anal

and

interradial plates areconvex, but do not gene- rallyriseinto distinctnodes.

Named

inhonorof the venerable Prof. B. Silliman, Sr., of

New Haven,

Connecticut,

who

perhaps did

more

to createaninterest inscientificstudies

and

pursuits, atanearlyperiod in the history of thiscountry, than

any

other person

now

living.

Locality

and

position. ClearCreek,

Warren

County, Illinois. Burlington Limestone.

Genus AGARICOCRINUS,

Troost.

Agaricocrinusgracilis.

Body

small, truncato-subglobose exclusive ofthe

arms

;

under

sideconcave, theconcavity extending outtothe middle of the secondradial,firstinterradial,

and

second rangeof anal pieces, all of

which

are geniculated, orabruptly bentupwards,

and

swollen, so asto formacircle ofhemispherical nodes

around

themarginsoftheconcave

under

side.

Anal and

interradial pieces rising vertically

from

the marginsof the con- cavitybelow.

Dome

rather depressed,

and

provided with a short, strong, sub-central spine.

Anal

opening small,not protuberant,

and

placed about

on

a levelwiththe

arm

openings,

which

are located slightlyabove the middleof the entirebody, including the

dome.

Basesmall, concave, nearly or quite hidden

by

the column. First radial platesflat,includedwithin the concavityofthe

under

side,about as wide as long,

and

apparentlyallhexagonal. Second radials slightly largerthan the

first,

and

quadrangularinform. Third radial pieces shorter

and

widerthan thesecond,

and

each provided with

an

obtuse mesial ridge,

which

connects withthe

prominence

ofthesecondradialsbelow; sub-heptagonal in outline, thesuperioranglebeingrathersalient,

and

the slopes

on

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

supporting

two

smaller elongated pieces in thenext range above. Firstanalplate small,

and

included within the con- cavity of the

under

side; supportingin the next rangethree largerpieces, the middle oneof

which

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, the

arms

are each at first

composed

of a single nodosebrachial piece, but almost immediately passintoadoubleseriesofshort alternating pieces,

which

supporta closelysetrangeoftentacles

on

eachside within.

As

they

do

not bifurcate again, there arebut

two arms

toeachray, or tenintheentireseries.

Near

thebasethe

column

israther slender,round,

and composed

of alternately thicker

and

thinnerplates, withavery small

round

central perforation.

The

surfaceisfinely

and

regularlygranulose

where

well preserved, but generally appearstobe smooth.

Locality

and

position. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. Charles

Wachsmuth.

Platycrinus Mui/n-BRAcniATus.

Body

below the

summit

of thefirstradial pieces depressed,basin-shaped. Basediscoid,pentagonal in outline,

moder-

atelyconcave below,

and

not prominent

enough

to be seen in a side view;

columnar

facetaboutone-third as wideasthe base. First radial plateslarge, broader thanhigh,

and

wideningrather rapidly

upwards

fromthebase; facet

forthe reception ofthe secondradial piecesprominent, extending

down

appa-

rently below the middle of the plate. Second radial pieces small, trian- gular,widerthanlong,

and

extendingobliquely outwards

and upwards

from the firstradials.

After dividingon the secondradials, the

arms

bifurcateagain

on

thesecond piece,

and

the

two

innerdivisions,

which

are largerthan theothers, bifurcate again onthesecondpiece,above

which two

ofthe sub-divisions in

some

ofthe

1861.]

(9)

136 PROCEEDINGS OF THE ACADEMY OF

rays again divide once more,

making

seven rays to

some

ofthe

arms and

eightto others.

The arms

are rounded, very graduallytapering,

and

each

composed

of adoubleseries of alternatingpieces, supportingtentacleswithin.

The

suturesseparating thefirstradials, as well as those

between them and

the base, are rather distinctlygrooved, as well as those

between

the succeeding pieces,

up

tothelast bifurcation ofthefreearms.

The

surface ofthefirstradial platesisratherconcave,

and between

thepro- jecting

margin

ofthe sinus above,

and

the marginal grooves; the concave space being

sometimes marked

by veryfainttraces ofsmallradiatingcorruga- tions.

Very

smalllongitudinalobscurestriaeor wrinkles,canalsobe seen

by

theaid ofamagnifier

on

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 sides

and

baseofits first radialplates. Its

body

isalso proportionallyhighertothe

summit

ofthefirst radials.

Locality

and

position. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. Charles

Wachsmuth.

Genus CYATHOCRINUS,

Miller. 1821.

Cyathocrinus

Wachsmuthi. Body

depressed, obconical, or subturbinate.

Baseofmoderatesize, low,

and

distinctlypentagonal, the angles formed

by

the extremities ofthe plates alittleincurved.

Columnar

facetcovering about one-thirdto one-fourth of each basal piece.

Column

obscurelypentagonal nearthe base, the angles being

rounded

; central perforation comparatively large

and

pentagonal. Subradialplatesfiveor sistimesas large as thebasal pieces,aboutaslongas wide, three of

them

hexagonal,

and two on

the anal sideheptagonal, allindented or incurvedat thesides

and

atthe

upper

angles.

First radials largerthan thesubradials,

unequal

insize,

and

widerthan long; allheptagonal,inconsequenceofthetruncationofthe superior lateral angles apparentlyforthe reception ofsmallinterradials,each havingtheangles

below

distinctlyindented,

and upper

side truncated,

and

moderately concaveforthe reception of thesucceedingplates. Secondradialsveryshort ornearlylinear,

and

abouttwo-thirds aswide as the first. Third radials generally a little

narrower,

and

longer than the second,

and

apparentlytriangular in form.

Sub-analpiececomparativelylarge,quadrangular,

and

indentedattheangles;

firsttrueanalplate largerthan the sub-analpiece,heptagonalin form, resting

upon

averyshort

upper

truncatedside ofoneofthe subradials,

and

connect- ing

on

eachsidewiththefirstradials; itsright inferior sloping side alsorest- ingagainst thesub-analpiece.

The arms

after dividing

on

the thirdradials, are strong

and rounded

ontheouterside; oneofthe divisions ineachofthe rays,exceptinganterior one, bifurcates again

on

the fourth piece. All the divisions

and

subdivisions are rounded, gradually tapering,

and composed

eachofasingle series of pieces as longas, or a little longer

than

wide,

and

giving off at intervals of

two

or three pieces alternately

on

opposite sides, rather strong jointedlateraldivisions,

which

extend obliquelyoutwards

and

bifurcateseveral times.

The

surface

seems

tobe merelyirregularlygranulose.

On examining

itclosely, however,traces ofvery smallradiating slightly raised linesareseen

on

thesubradial

and

radial plates, as well asextending

up

the

principal divisions of thearms.

We

take pleasureindedicatingthisspecies to Mr. Charles

Wachsmuth,

of Burlington, Iowa,to

whom we

areindebtedforthe use ofthe

specimen

de- scribed.

Locality

and

position. Burlington, Iowa. Burlington Limestone of the

Lower

Carboniferousseries.

Genus BTJRSACRINTJS,

N.G.

(0vp<raapurse; x/wvocalily, inallusion tothe purse-like form ofthetypical species, asseenwithits

arms

folded together.)

[June,

(10)

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

crinoid

upon which we

proposetofoundthisgenus, has

much

the ap- pearanceofanIchthyocrinus,with

which

genusit

seems

toagree, exceptingin

having

truesubradial plates,

and

but two, instead of three

primary

radial plates ineach ray; alsoin the possessionofa distinctanalplate.

Notwithstandingitsgeneralsimilarityto Ichthyocrinus, itsstructureis

more

nearlylikethat of Cyathocrinus,

from which

it differs

mainly

in

having

only two, instead of threeprimaryradial pieces ineachray,

and much

broader

and

flatterarms,

which

connectlaterally as inIchthyocrinus, so as toleave

no

in- terradial spaces.

Bursacrinus

Wachsmuthi. Body

below the

summit

ofthefirstradial plates rather broad turbinate, or rapidly

expanding

from below. Base

unknown.

Subradialplates ofmoderatesize, alittlewider thanlong,

and

allhexagonal, excepting one

on

the anal side,

which

is larger than theothers,

and

hept- agonalinform; theangles at themiddleofthe

under

side of each beingless salientthanthatabove. First radial platesabout one-third larger than the subradials,near twice as wide as high,

and

all pentagonal, the

upper

side beingtransversely truncated.

Second

radial pieces of the

same

size

and

form asthefirst, but invertedso as tobring the truncated side below; supporting

on

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 middleofthe

summit

being

more

salient than the others; supported

upon

the short truncated

upper

side ofoneofthesubradials,

and

connecting

on

eachside with thefirst

and

secondradialplates,

and

the first of thebroad secondaryradial or

arm

piecesabove.

Afterthefirstdivision

on

the second radials, the

arms

bifurcate again

on

thesixth oreighthpiece, above

which

oneisseen to bifurcate again

on

the twelfth piece,

which

isasfarasthey can betraced inthe only specimenseen,

though

they

seem

tobelong

and

probablybifurcateonceoroftenerabove

Between

thedivisions

on

thesecondradial pieces,

and

thenext bifurcation above, theyareverywide, flat,

and composed

of short, slightlywedge-

formed

pieces,

which

aresquarely truncated

on

eachside.

The

nextdivisionsabove these are a little

more

than half as wide,

and composed

of a single series of piecesbearing near the

same

proportions oflength

and

breadthasthose below.

The

surfaceisfinelygranulose,

though

there are

no

traces of nodes, costse,or other prominences

on any

oftheplates.

The

sutures are

merely

linear,and>

not impressed.

We

take pleasurein dedicating this interesting species, (the typeof a

new

genus,) to Mr. Charles

Wachsmuth,

of Burlington, Iowa,

who

discovered the only specimen

we have

seen.

Positionandlocality. Burlington Limestone. Burlington, Iowa.

Genus POTERIOCRINUS,

Miller, 1821.

Poteriocrinus? enormis.

Body

small, irregularlycup-shaped; sides

some- 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 one

on

the anal side,

which

is

much

larger than the others,

and

sub-heptagonal in outline. First radial plates

1861.] 10

(11)

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, shallow

and

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 place

on

thesecond, in others

on

thethird,

and

inthe anterior ray on the fourth piece above thefirstradials, after

which

theybifurcate irregularly once, twice, or oftener,

on

thesecond, third or fourth piece.

The

firstanalplateis rather large,

and

rests

upon

the

upper

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 ofnearlyits

own

size resting

upon

a sloping side of thefirstradial on theright.

Above

theseareseenseveralotherplates,

which

form togetherakindofslenderlateral trunk,or proboscis, rising like

an arm on

arange with thetruearms.

Some

littledistance above, itcurvesinwith its

upper

extremity

between

the arms, leaving atitsbase,

on

theleft,a cavity oropening, passing apparentlyintothe

body between

it

and

the first

arm 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

very

marked

feature ofthisspecies,isitspeculiarity ofhaving apparently a slender proboscis

much

like

an

arm, rising from the anal side,with

an

opening

between

its left side

and

one of thearms. Thisisso

anomalous

a character, thatif

we

were sureitisnot

due

to

some

accident,

we would have

regardedthe species asthe typeofa

new

genus.

Locality

and

position. Burlington, Iowa. Burlington Limestone. Collec- tion ofMr. Chs.

Wachsmuth.

Poteriockinussub-impressps.

Body

obconical. Base formingashallow

cup

abouttwice aswide as high,

expanding

moderately from the

summit

ofthe

column

;

composed

of plates

which

are aboutashighas wide,

and

pentagonal in form, the angleat

the

middleof the

upper

side of each beingalittlein- dented. Firstradials

somewhat

smallerthan thesubradials, widerthanlong, pentagonal,or

some

of

them

hexagonal,

and

truncated

above

forthereception ofthesecondradials. First anal or sub-anal plate, a little largerthan the basal pieces, pentagonal,

and

resting

between

the

upper

sloping sides of

two

of thesubradial pieces; second analpiece ofthe

same

sizeasthefirst, hex- agonalin form,

and

resting

upon

the

upper

truncatedside ofoneofthe sub-

radials, whileitsleftsideconnectswith one of thefirstradials,

and

its right with oneside ofthefirstanalpiece,

and

with a thirdhexagonalpiece resting

upon

it. (Succeeding parts

unknown.)

The column

is comparatively strongat its connection with thebase,near

which

itis

composed

ofrather thinsegments, connected

by

crenulated sutures;

itscentral perforationisofmoderatesize

and

pentagonal.

The

surface

seems

to be granulose,

and

the subradialpieces

show

a very slighttendencyto develope 9hort costcenear the sutures on eachside,

and

below,as well as

sometimes

attheirconnection withthefirstradialsabove.

The round

indentations atthe anglesofthe subradial

and

firstradial plates, presenta rather

marked

character inthisspecies.

Locality

and

position. Burlington, Iowa. Burlington Limestone. Mr.

Charles

Wachsmuth's

collection*

Poteriockinus tenuibrachiatfs.

Body

small, calyculate, or turbinatebelow the

summit

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,

(12)

NATURAL SCIENCES OF PHILADELPHIA. 139

others. First radial plates

somewhat

largerthan thesuhradials, wider than long

and

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

resting

between

the upper sloping sides of

two

of the subradial pieces, whileanother

on

theleft restsagainstthis,

and upon

thesuperiortruncated side ofoneof thesubradials.

A

third pieceis supported

on

the

upper

trun- cated side of the subanal piece,

and

projects

more

thanhalf itslength above thefirst radial

on

its right.

The

succeeding

primary

radial piecesafterthe

first,are distinctly smaller,

and

alittlewider thanlong. Inallexcepting the anterior ray,

where

the bifurcationtakesplace

on

thefifthplate,thefirstdivi- sion of the

arms

takes place

on

the fourth

primary

radial.

Above

this the arms,

which

are very long, slender

and

rounded, divideagain

on

thefourth piece, after

which

the divisions bifurcate three or four times,

and become

veryattenuate.

Each

divisionis

composed

ofa singleseriesof pieces, usually abouttwice aslongaswide.

The

proboscisconnectsdirectlywith the analplatesalreadydescribed,

and

is

made up

ofhexagonalplates, along the sutures ofwhich, distinct vertical rangesofrather large

and

distinctpores are seen.

The

entire surfaceisfinely granulose.

The

suturesare linear

and

not groovedor impressed. This spe- ciesissimilar to P. calyculatus of Hall,but

may

beat once distinguished

by

itssuturesnot being excavated,

and by

its

much more

slender arms,

which

are

composed

of elongate, instead of short

wedge-formed

pieces.

Locality

and

position. Burlington, Iowa. Burlington Limestone. Collec- tionofMr. Charles

Wachsmuth.

Poteriocrinus carinatus.

Body

small, basin-shaped or rather rapidly spreading below the arms. Base verysmall,

having

the formofapentagonal star,the angles of

which

projectbut slightly

beyond

the

column.

Subradial pieces small, aboutaswideas long, four of

them

hexagonal, (the

form

ofthe one

on

theanalsideisnot distinctly visible in the

specimen examined

;)all ratherprominent,

and

provided with avertical carinanearthe

upper

angle.

First radial pieces abouttwice as large as the subradials, aswide again as high,

and

pentagonalin form,the

upper

sidebeingtruncated,

and

longer

than

either ofthe others.

Second

radials slightly larger thanthefirst,wider

than

high, quadrangular,

and

alittleconstricted

around

the middle.

Thirdradials about thesizeof the first,pentagonal in form,

and

like the secondslightlyconstricted, the

upper

angles being rathersalient.

The

anal plates arenotallpreservedinthe specimenbefore us,

though we

canseethat thefirstorsubanalpieceisof

moderate

size,pentagonal in form,

and

extends sofar

down between two

of the subradials, as to connect (apparently)

by

a veryshortside, with the

produced

extremityofone of thebasal pieces. Its rightsuperior sloping side supports oneedge of a firstradial above,

and

it

evidently supported another piece

on

its superior truncated edge, while it

connects

on

theleftwith anotherresting

on

the

upper

truncatedside of

one

ofthesubradials.

Afterthefirstdivision of the third radials

some

ofthe

arms

bifurcateagain on thefifth,sixth or seventh piece, while others

seem

to be simple.

They

areall

composed

of pieces

which

are a little constricted

around

the middle, aslong as wide,

and

alternatelylonger

and

shorter

on

opposite sides, the

upper

extremityof the longerside ofeach being alittleprojectingforthere- ception of the tentacles, so astogive a zigzagappearance to thearms.

The

tentacles arelarge,

and composed

of ratherlongjoints.

Owing

tothe length ofthe

arm

pieces,

and

the fact that onlyeveryalternate piece

on

the

same

sidesupports a tentacle, theyarevery widely separated

and

alternately ar- ranged.

The

surface

seems

tobegranulose,

and

each rayisprovided witha distinct linear carina,

commencing

onthe

middle

ofeachfirstradial piece

and

extend-

1861.]

Referensi

Dokumen terkait

While they agreed that communicative language teaching activities can assist learners to build and create new knowledge, they attributed the poor implementation of CLT to a lack of

Fig.3.1 IM7 AND IM1 4 RESULT DISCUSSION The goal of our approach is to justify bounding box algorithm separately and with which is based on Anisotropic Diffusion Filter .Dataset