|
Laganidae
Agassiz, 1873,p.516
Genre type : Laganum
Link, 1807
Description succinte de la famille : Piliers
internes partitionnant le test sur son pourtour externe. Périprocte infère,
situé entre les premières et les secondes plaques post basicoronales paires.
Présence de sillons nourriciers.
|
|
|
|
|
|
|
|
|
|
Sous-famille
Laganinae
Agassiz,
1873
description succinte :
Laganidae avec structure d'assules simples sur les ambulacres. Plaques
basicoronales en forme d'étoile, les plaques ambulacraires étant plus
longues. |
|
|
|
|
|
|
Genre
Jacksonaster
Lambert & Thiery,1914
Essai de nomenclature
raisonnée des échinides, p.313
Espèce type
Laganum depressum
Agassiz,1841 (désignation subséquente de
Lambert & Thiery,1914,
Essai de nomenclature raisonnées des échinides, p.313)
Monographies
d'échinodermes, des Scutelles, p.110
Extension
stratigraphique (bibliographique,
non vérifiée) : Miocène -
Actuel
|
|
|
|
|
| |
Jacksonaster
depressum
Agassiz,1841,
Pléistocène, Egypte, 53 mm |
|
|
|
|
|
|
|
|
| |
Jacksonaster
depressum
Agassiz,1841,
Pléistocène, Jordanie, 46 mm |
|
|
|
|
|
|
|
|
| |
Jacksonaster
depressum
Agassiz,1841,
Plio - Pléistocène, Egypte, 23 et 16 mm |
|
|
|
|
|
|
|
|
|
|
|
|
|
Genre
Peronella
Gray,1855
Catalogue of the
recent echinida of sea eggs in the collection of the British Museum, p.13
Espèce type
Laganum peronii
Agassiz,1841 (désignation originale)
Extension
stratigraphique (bibliographique,
non vérifiée) : Pléistocène -
Actuel
Syn.
-
Lambertiella
Checchia Rispoli, 1917,
p.57 ; espèce type : Lambertiella pulchra
Checchia Rispoli, 1917
|
|
|
|
|
| |
Peronella
orbicularis
(Leske,1778),
Pléistocène, Dampier Limestone, Australie de l'Ouest, 20 mm |
|
|
|
|
|
|
|
|
|
|
|
|
|
Genre
Rumphia
Desor,1858
synopsis des échinides
fossiles, p.229
Espèce type
Laganum rostratum
Agassiz,1841 (désignation originale)
Extension
stratigraphique (bibliographique,
non vérifiée) : Miocène -
Actuel
Syn.
-
Polyaster
Michelin, 1859, non
Gray, 1840
-
Peronellites
Hayasaka & Morishita, 1947,
p.101 ; espèce type : Peronellites ovalis
Hayasaka & Morishita,1947
|
|
|
|
|
|
|
| |
Rumphia ova
(Mc Namara,1996),
Pliocène supérieur, Australie de l'Ouest, 30 mm |
|
|
|
|
|
|
|
|
| |
Rumphia ricta
(Gregory,1892) |
|
|
|
|
|
diagnose originale de
l'espèce par Gregory, 1892 |
|
Further additions to Australian fossil Echinoidea, p.433 |
|
|
|
Species,
Laganum decagonale, Lesson. Var. rictum, n. var. Pl. XII. Fig. 1.
Diagnosis (of the
Variety).
Form : elongated elliptic ; the posterior end is longer and
narrower than the anterior ; the anterior end is semicircular ; the
sides taper backward. The base is flat ; the margins are tumid, and
are separated from the slightly conical apex by either a flat platform
or a slight broad depression.
Ambulacra : Petals extend two-thirds of the distance from the
apex to the ambitus ; the lateral pairs are equal in length ; the
anterior ambulacrum is the longest. The petals are sharply closed
below ; the width of the pore area expands rather gradually to the
distal end of the petal, then is there closed somewhat abrubtly. The
interporiferous areas are large, and taper slightly to the blunt
distal end.
Apical system : at the apex of the test. The madreporite is
raised, large, and central. There are four large genital pores. Of the
radial (ocular) pores the right antero-lateral is very large ; those
of the right postero-lateral and left antero-lateral ambulacra are
small ; the left postero-lateral pore is not developed.
Peristome : mouth somewhat pentagonal ; large ; the width is
half as much again as the length. It is situated before the centre.
There are no interradial actinal furrows.
Periproct : the anus is large and almost circular ; it is close to the
margin.
Distribution. -
Cainozoic. Shark's Bay, West Australia.
Collected by
Harry Page Woodward,
Esq., F.G.S.
Affinities and Differences.
- The specimen on which this species is founded is unquestionably a
very close ally of Laganum decagonale, Less., though as to
whether it should be regarded as a variety or a distinct species, I do
not care to express an opinion on a single specimen. It differs from
that
|
|
species by the
elliptical and somewhat pentagonal shape of the mouth, and the absence
of the five interradial furrows which radiate from the mouth. The
British Museum contains a large series of specimens of that species,
but the circular form of the mouth is constant ; the actinal
depressions do vary in debree of development, but I have not seen one
in which it is not quite distinct. These two characters may not
improbably be of specific value.
The shape of the test differs from the normal decagonal form ; but
some specimens of the species have a form identical with the fossil.
Herklots figured a specimen from the Java Tertiaries as Scutella
decagona, n. sp., Martin referred this to Peronella decagonalis,
Ag., and included L. angulosum, Herklots, as a synonym ; but as
Herklots neither figured nor described the actinal side, a certain
amount of doubt must remain as to the accuracy of this determination.
As the present variety differs from the previously known species in
the same points as L. decagonalis, it need not be compared more
closely with them.
planche XII
(extrait)
|
|
|
|
| |
Rumphia ricta
(Gregory,1892),
Lutétien supérieur, Gironde, 27 mm |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Genre
Sismondia
Desor,1857
synopsis des échinides
fossiles, p.225
Espèce type
Scutella occitana
Defrance,1827 (désignation subséquente de
Pomel (1883)
Classification
méthodique et genera des echinides vivants et fossiles, p.72)
Extension
stratigraphique (bibliographique,
non vérifiée) : Eocène moyen - Miocène
inférieur
Syn.
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
| |
Sismondia
occitana
(Defrance,1827),
Lutétien supérieur, Gironde, 27 mm |
|
|
|
|
|
|
|
|
| |
Sismondia
archiaci
Cotteau,1883,
Lutétien , Charente Maritime, 23 mm |
|
|
|
|
|
|
|
|
|
|
| |
Sismondia
intermedia
Fabre,
Lutétien , Médoc, 13 mm |
|
|
|
|
|
|
|
|
| |
Sismondia
testudo
Cotteau,1891,
Bartonien, Calcaire de Blaye, Médoc, 8 & 10 mm |
|
|
|
|
|
|
|
|
|
|
|
| |
Sous-famille
Neolaganinae
Durham,1954
description succinte :
Laganidae avec structure d'assules pseudo-composée sur les ambulacres. Plaques basicoronales
arrangées pentagonalement. |
|
|
|
|
| |
Genre
Wythella
Durham,1954
Classification of
clypeasteroid echinoids, p.682
Espèce type
Laganum eldridgei
Twitchell,1915 (désignation originale)
Extension
stratigraphique (bibliographique,
non vérifiée) : Eocène moyen -
fini Oligocène |
|
|
|
|
| |
Whytella
eldridgei
Twitchell,1915 |
|
|
|
|
|
diagnose originale de l'espèce par
Twitchell |
|
Mesozoic and
Cenozoic chinodermata of the United States, 1915, p.160. |
|
|
|
Laganum eldridgei
Twitchell, n. sp.
Plate LXXIV,
figures 2a-d.
Determinative characters. - Test large, subpentagonal to
subdecagonal in marginal outline, longitudinally elongate, truncated
at the anterior and posterior ends, more or less undulating along the
sides. Whole form greatly depressed, margin thin bhut thicker than
slightly concave submarginal area, petaloidal region tumid. Apex and
apical system subcentral. Lower surface flat. Ambulacral petals long,
elongate elliptical, extending two-thirds the way to the margin,
pointed and closed at the ends ; pairs of pores conjugated by very
narrow more or less wavy grooves. Ambulacral areas very wide at margin,
narrowing rapidly to ends of petals. Peristome moderate in size,
subcentral, subpentagonal to subelliptical, transversely elongate.
Ambulacral grooves apparently simple and straight, each groove having
a fine line on both sides which rapidly diverge from the main groove.
Periproct relatively large, suboval, longitudinally elongate, one-fourth
the way from the margin to the peristome.
Dimensions. - Length 96 millimeters ; width 75 millimeters ;
height 10 millimeters.
Description. - The only specimens known of this large and
handsome Laganum, the largest representative of the genus from
American deposits, were collected in Florida by the late G. H.
Eldridge of the United states Geological Survey and the species is
therefore named in his honor. The test is large, being 3 to 4 inches
long and 21/2 to 3 inches wide. In marginal outline it is
subpentagonal to decagonal, decidedly longer than broad ; margin thin
but thicker than the submarginal area, truncated at anterior and
posterior ends, more or less undulating along the sides. The whole
form is greatly depressed, the upper surface slightly concave around
the submarginal area, arising centrally in the form of a low mound
which involves the whole petaloidal area ; apex subcentral ; lower
surface flat.
The ambulacral areas are very wide at the margin, being there about
four times the width of the interambulacral areas, narrowing rapidly
to near the ends of the petals. The petals are long, elliptical in
outline, extending two-thirds the way to the margin, pointed and
closed at the ends. The anterior pair shorter than the other three,
which are subequal in length. The poriferous zones are wide, more than
half the width of the rather narrow interporiferous areas, inner row
of pores elliptical, outer row very narrowly slitlike, hardly
discernible, pairs of pores conjugated by very narrow more or less
wavy grooves.
The interambulacral areas are very narrow at the margin, widen rather
rapidly to near the ends of the petals, and narrow again toward the
apical region. The whole test is closely set with very small tubercles,
among which are scattered at irregular distances some larger ones in
deep scrobicules.
The apical system is subcentral, at the summit of the tumid area.
There are four large genital pores, of which the anterior pair are set
closer together than the posterior pair. No other details could be
made out on the specimens.
The peristome is of moderate size, subcentral, slightly to the rear of
the apical system, subpentagonal to subelliptical, transversely
elongate. The details of the ambulacral grooves could not be mad out
satisfactorily on the specimens studied. As they leave the peristome
there appears to be a single straight groove on each side of which are
two fine lines which rapidly diverge from the main groove. These side
lines may be the boundary lines of what on better preserved specimens
would prove to be finely granulated areas, thus forming a peristomial
star.
The periproct is relatively large, about half the size of the
peristome, suboval, longitudinally elongate, situated about one-fourth
the way from the margin to the peristome.
Related forms. - L. eldridgei is readily distinguished
from all other American forms. It closely resembles L. elongatum
Agassiz, whose origin is unknown and which is not even stated to be
fossil, being very similar in size, general form, and marginal outline,
but differs from it in having a suboval instead of circular periproct,
placed a little farther from the posterior margin.
Locality. - Suwanee River, Fla.
Geologic horizon. - Vicksburg group, lower Oligocene.
Collection. - U.S. National Museum (164683).
Extrait planche
LXXIV
|
|
|
|
| |
Whytella
eldridgei
Twitchell,1915, Eocène
supérieur, Floride, 42 mm |
|
|
|
|
|
|
|
|
|
|
|
| |
Genre
Weisbordella
Durham,1954
Classification of
clypeasteroid echinoids, p.682
Espèce type
Peronella caribbeana
Weisbord,1934 (désignation originale)
Extension
stratigraphique (bibliographique,
non vérifiée) : Eocène
supérieur |
|
|
|
|
| |
Weisbordella
cubae
(Weisbord), Eocène
supérieur, Hernanco county, Floride, 43 mm |
|
|
|
|
|
|
|
|
|
|
|