z
416 General
Notes.shell is larger, the
apex more
blunt, the greater obliquityof
thevolutions,
and
in theirgreater convexity beingat
orbelow
the centre.Position
and
locality,Rockford
shales,Owens Grove
(southexposure),
Cerro Gordo
county,Iowa.
Loxonema
owenensis, n. sp.—
Shellvery
largeand
robust, subco-niform;
spire rather rapidly ascending,apex
blunt.Volutions
eight to ten or
more, very
oblique, strongly inflated,most prom-
inently so
below
the centre,rounded. Suture deeply channeled;
shell
from two mm.
to sixmm.
in thickness ; aperture subovate.Surface apparently smooth. The depth of
the suture in this speciesis
very much
greaterthan
the suture in eitherthe
foregoing or fol-lowing
species.Height
of adultspecimens from
fourteen to six-teen
and one-half
centimetres ;diameter of body
volutionfrom
fourto five centimetres.
This
is,we
believe, the largest species of theyet described. Position
and
locality,Rockford
shales,Grove
(south exposure),Iowa.
Loxonema
crassum, n. sp.—
Shell large,subconiform
depressed,rapidly
broadening from
theblunt
apex.Volutions from
five toseven, slightly flattened or
broadly rounded
; suture stronglychan-
neledbelow
; shellvery
thick ; surfaceapparently smooth
; apertureovate.
This
species differsfrom L. gigantea
in itsmore
robust,depressed
form, and
the lessconvexity and
obliquityof
its volutions.Position
and
locality,Rockford
Shales,Owens Grove
(southexposure),
Iowa. Quite
a largenumber of specimens of each of
thespecies described
have been
secured,and
their specific differencesare
shown
tobe
constantand
wellmarked.
—
Clement L.
Webster,Charles City,
Iowa.
Some Extinct Scleroderms.— In 1887,
in theMemorie
delhxSodda
Italiana delle Scienzeof Naples (3d
series, v. 6,No.
4), 1Baron
Achillede Zigno has published
descriptionsand
illustrationsof two very
interestingScleroderms from
theEocene beds of
Italy.One of
these is the Protobalistum /' ngo, the other a previouslyunknown
species considered tobe congeneric with
theformer and named Protobalistum Omboni; both were
obtainedfrom
the celebrated
Mount Bolca
beds.The most
casualexamination
will
convince one who has had much
experiencewith
recent fishesthat the
two
specieshave
little incommon and belong
tovery
dif-ferent
genera
if not families.Both
are,however, important
for thelight
they may throw on
the genetic relationsand former
distribu-tion
of
theScleroderms, but each owes
itsimportance
toa
different> del Veronese. (8 pp., 2 pi.)
Geology and
Palaeontology.447
which
arecommon
to thetwo
forms,which does
notappear
tobe
justified
by
thespecimens
;on
thedevelopment of 4
to 6 dorsalspines,
of spinous
rays toeach
pectoral (" pectorales radiisduobus
spinosis "),
and of
1 to3
spines toeach
ventral (" ventrales radiis1—3
spinosis, retro-flexis ").Such
features as the lasttwo
are soncompatible with
the structureof
livingScleroderms
that the spicion is
unavoidable
that their ascription to the extinctforms
idue
tosome
errorof observation
or interpretation.The
principai described
and
corroboratedby
the illustrations is the ir
ber
of
dorsal spines.The arrangement of the
spines is neverthe-less
very
different in thetwo
species.The
typicalProtobalistum
(P. imperiale)has
six (or seven) dorsal.ther
widely
separatefrom each
other,extending from
overfar
back upon
the posterior halfof
thebody, and very
elongate (the
foremost
especially) ; the soft dorsal as well as anal arevery
short.No
pectoralsand
ventrals are represented in thefigure,
although
it is asserted that there isa
ventral spine. 1The
character
of
the dorsal fin isvery
differentfrom
that exemplifiedin
any of
the Balistids or Triacanthids.None of
the Balistidshave more than
three dorsal spines,and
allhaving
thatnumber
have
thesecond
closebehind
the first,and modified
to lock it inerection, in
such
amanner
as tohave
obtained for the species thename
Trigger-fish.The Protobalistum should
thereforebe appar-
ently considered as
the type of
a peculiar family with generalizedcharacters
and
allied to the progenitorsof the*Siganids and Teu-
thidids
; the
family name
insuch
casewould of
coursebe
Proto-balistidce.
The
so-callednew Protobalistum
(P.Omboni) has
four dorsalspines
moderately approximated and
confined to theforward
partof
theback;
the first spine isvery
strongand
the othersvery
short; the soft dorsal is elongated,
and
the anal isoblong;
the cau-dal
peduncle
is long.In
fact, the specieshas
thephysiognomy
aswell as the structural
characteristics (so far as
known) of
the Tria-canthids,
and
thereappears
to beno
reason fordoubt
that it belongsto that family,
and
that it is related to thegenera
Triaeonthadesand
Hollardia,with
which
it agrees in theconvex caudal
fin,? U
-a
perIla
P
s tnedevelopment of one
ortwo
axillar rays,besides the
elongated
ventral spines.("Le
ventralisono
constituteda
tre soli raggispinosi rivolti all' indietro e addentellati net loro
margmi,
di cui ilprimo
elungo 27
millimetri, ilsecondo 25
el ilterzo 20, e
cadauno
alia baseha
ildiam.-tm
di 2 millimetri.")The
-uuai nu
isvery
large,and has
aconvex
|littering
from
thatdeveloped
in the Triacanthinae.No
genericcaudal fin is
very
large,and
differing
from
thatdevelop
ventoft ^""T
11uon
8i 8Corname being
available for the fossil, itmay be named Protacanthodes
Omborii, the
name
recalling that theforemost elements of
thespinous
dorsal as well as ventrals areenlarged
spines, as well asthat it is
a forerunner
of the Triacanthids. It differsfrom Hollardia and Triacanthodes
in theobloug caudal peduncle and
enlarged caudal
finwhile
itsphysiognomy
rather recalls the true Iriacanthi.The
occurrenceof
aform
so closely related tothe
Triacanthodes of
theJapanese
sea,and
to theHollardia of
theCaribbean
in theeocene
seasof Europe,
isworthy of
special note,and
this is a sufficient reason for the present
communication.
The
nearest extinct associateof Protacanthodes
isnot
Protobalis-tum but Acanthopleurus Ag. The two belong
to thesame family
but appear
tobe
otherwise distantly related.The
other extinctgenera of Scleroderms, Balistomorphus
Gill,Acanthoderma Ag.
1843, not Cantraine,1835, and BucMandium Koenig
—
Glyptocephalus
Ag.)
are rather tobe
associatedwith
the Balistids.The
exact charactersand
relations of all these fishesremain
to beknown.-
Theo. Gill.The Phylogeny of the Horses.
1— This brochure of 71
pages,illustrated
by two
excellent plates,cannot
fail to instruct the studentwho
is unfamiliarwith
this subject.The
authoressshows
a greatdegree of
familiarity with the historyof
the factsknown
in thisconnection
and they
are set forthwith
considerable fulnessof
detail.She has been more
fortunatethan some of her
predecessorsin
avoiding
record in extensoof
themythology
of the subject,which has been long
sinceconsigned
to its place in thewaste-basket by
American
palaeontologists.We
allude to theEohippus, Miohippus, and
Pliohippus,which
stillappear
occasionally in theologicalworks and school-books of America and England. A
considerable partof
the essay isdevoted
to theendeavor
toprove
that the generaPalseotheriuni
and Bippotherium must be excluded from
the lineof
descent,which
hascontinued from Protogonia
puercensisthrough
Phenacodus, Hyracotherium,
etc., to Equiis.She
describesand
figures
with much
care certainbones of
thecarpus and
tarsus ofAnchitherium, Hippotherium, and Equus,
inevidence of
this posi-tion as regards
Hippotherium. We
saywith
reference to thisquestion, that in discussing the
phylogeny of
genera,one must
confine
himself
to generic characters,and
it is necessary to ascertainwhat
these are in the skeleton beforewe can
usethem
properly.There
aresome
speciesof supposed Hippotherium of North Amer-
ica
which approach Equus
so closely in dental characters thatthe descent
of some
speciesof
the latterfrom them
looks probable.Probably
the speciesof Equus
are polyphyletic,2some coming from
i
Etudes
sur l'Histoire Palseontologique ties Ongules, II, leDeveloppe
ment
dea Equidse.Par Marie Pavlow. Moscow,
1888.2 I