Acrosaleniidae
Gregory, 1900, p.306
Genre type : Acrosalenia
Agassiz, 1840, p.39
Description succinte de la famille : Apex
hémicyclique (ds certains genre, les oculaires I et V sont insertes), tubercules perforés et crénelés.
Présence de suranales. Chez Acrosalenia, périprocte en position
excentrée arrière sur l'axe antéro-postérieur, Ambulacres trigéminés.
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Genre
Acrosalenia
Agassiz, 1840
Description des Echinodermes de la
Suisse, II, p.39
Espèce type
Acrosalenia spinosa
Agassiz, 1840 (désignation originale)
Extension
stratigraphique (bibliographique,
non vérifiée) :
Hettangien-Sinémurien - Valanginien |
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Diagnose originale du genre par Agassiz |
Description des échinodermes fossiles de la Suisse, 1840, p.38 |
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22e Genre.
ACROSALENIA Ag.
Les Acrosalénies sont des Oursins de petite taille,
très-reconnaissables à la structure de leur appareil oviducal, qui
rappelle à tous égards celui des vraies Salénies. Les pièces qui le
composent sont au nombre de onze, savoir : cinq plaques ovariales,
cinq plaques interovariales, et une onzième plaque que j'ai appelée
suranale, parce qu'elle occupe une grande partie du pourtour de
l'anus. Toutes ces plaques sont intimement soudées les unes aux
autres, et forment un apparSeil très-solide et fortement adhérent au
test, absolument comme dans les vraies Salénies. Le seul caractère qui
les distingue de ce groupe, c'est que les mamelons de leurs tubercules
sont perforés. Ce caractère, quelque insignifiant qu'il
paraisse au premier coup-d'oeil, est cependant très-constant et
d'autant plus significatif, qu'il se raporte à des fossiles de deux
formations géologiques très-distinctes : en effet, les espèces à
tubercules perforés (les Acrosalénies) sont propres à la formation
jurassique, tandis que les espèces à tubercules non perforés (groupe
des Salénies) ne se sont rencontrées jusqu'ici que dans la
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formation crétacée. A part cette
particularité de structure, les Acrosalénies présentent tous les
caractères génériques des vraies Salénies. Les ambulacres sont
très-étroits ; les tubercules des aires ambulacraires sont petits et
nombreux, tandis que ceux des aires interambulacraires sont beaucoup
plus gros et en très-petit nombre. Les pores, disposés par simples
paires, tantôt convergent en droite ligne de la base au sommet, tantôt
forment des zones plus ou moins ondulées. Parmi les espèces de Suisse,
il y en a qui ont la plaque suranale de l'apareil oviducal en avant ,
celles-là correspondent à la première division de mes Salénies (le
A. aspera) ; d'autres l'ont en arrière (le A. spinosa), et
correspondent à la seconde division des Salénies (voir mes
Monographies d'Echinodermes 1re lir. p. 6). |
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Acrosalenia spinosa
Agassiz, 1840 |
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Description de l'espèce par Agassiz |
Description des échinodermes fossiles de la Suisse, 1840, p.39 |
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I.
Acrosalenia spinosa
Ag.
Tab. 18, fig.
1-5.
Catal. Sys. Ectyp. Mus. Neoc. p.9.
L'espèce dont il est ici question est du nombre de celles qui ont la
plaque suranale de l'appareil oviducal en avant, et dans
lesquelles par conséquent l'ouverture anale est refoulée en arrière.
Un autre caractère non moins marqué réside dans la forme des
ambulacres, qui sont légèrement renflés, ce qui détermine la forme
subpentagonale du test : ils convergent de plus en droite ligne de la
base au sommet, et sont pourvus de deux rangées de dix à douze
tubercules très-petits, il est vrai, mais cependant mamelonnés et
perforés ; l'espace intermédiaire est garni de très-fines granules
qu'on n'aperçoit guère qu'à l'aide d'une forte loupe (fig.4). Les
pores sont disposés par simples paires obliques, formant, de chaque
côté de l'aire ambulacraire, une double rangée rectiligne. Les aires
ambulacraires ont une largeur double de celles des aires
interambulacraires ; elles portent deux séries de tubercules surmontés
d'un memlon très-petit, relativement à la base du tubercule, mais
néanmoins très-visible (voir le dessin grossi fig.3). Ces tubercules
sont très-saillans jusqu'au milieu de la circonférence ; mais passé
cette limite, ils diminuent sensiblement de grosseur, et dans toute la
partie qui avoisine l'appareil oviducal ils ne sont pas sensiblement
plus gros que ceux des aires ambulacraires. Chaque tubercule est en
outre entouré d'un cercle de très-petites verrues. L'ouverture buccale
est grande et assez profondément échancrée. Quant à l'appareil
oviducal, voici comment il est construit : les quatre plaques
ovariales paires sont à-peu-près d'égale forme et d'égale grandeur ;
la plaque impaire, contrairement à ce que l'on voit ordinairement, est
plus petite, pour ainsi dire atrophiée, absolument comme dans la
division des Salénies, qui ont la plaque suranale en avant ; et l'on
conçoit en effet que la plaque suranale, en refoulant l'ouverture
anale en arrière, empêche le développement de la plaque impaire. La
contre-épreuve de ce fait nous est donnée dans les espèces qui ont la
plaque suranale en arrière, par
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exemple dans
le A. apera, où ce sont les ovariales antérieures qui
sont les plus petites (comparez les fig. 5 et 10). La plaque suranale
est un peu moins grande que les avariales paries ; sa forme est
distinctement pentagonale ; elle embrasse environ le tiers du pourtour
de l'anus. Les plaques interovariales sont petites et d'insèrent entre
les angles saillans des ovariales, excepté toutefois les deux
postérieures, qui bordent immédiatement l'ouverture anale. Il résulte
de ceci que la partie la plus développée de l'appareil oviducal est en
avant de l'ouverture anale ; l'anus lui-même est légèrement allongé.
Toutes les plaques sont finement granulées.
L'original de mes figures a été trouvé par M. le curé Strohmeyer dans
les marnes à Ostrea acuminata (oolite inférieure) du canton de
Soleure. La même espèce se retrouve en assez grande abondance dans
l'oolite de Caen.
Planche 18, fig.
1-5, d'après Agassiz
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Acrosalenia spinosa
Agassiz, 1840 - Meurthe et
Moselle |
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Bathonien inférieur 16 mm |
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Bajocien supérieur 9 mm |
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Bathonien inférieur 12 mm |
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Acrosalenia bouchardi,
Desor,1858 |
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Diagnose originale de l'espèce par Desor, 1858 |
Synopsis des échindes fossiles, p.142 |
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Bouchardi nov. sp. Grande espèce très voisine, au premier abord, de l'A.
Lamarckii, mais à tubercules ambulacraires plus gros et à zone
miliaire proportionnellement moins large et moins revêtue.
Grande
Oolite (Bathonien) de Marquise.
Coll.
Michelin, Mus. Neufchâtel.
Nota. Comme la
précédente, cette espèce est rapportée au genre Acrosalenia à
cause de sa ressemblance avec l'A. Larmarckii. Le disque apical n'est
pas connu. Plusieurs personnes l'ont étiquetée à tort du nom de
Hemicidaris Luciensis d'Orbigny. |
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Acrosalenia
bouchardi Desor, 1858, amb, Bathonien, Midelt, Haut-Atlas, Maroc,
19 mm |
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Acrosalenia
hemicidaroides, Wright, 1851 |
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Diagnose originale de l'espèce par Wright |
On the Cidaridae of the Oolites, 1851, p.154 |
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Acrosalenia hemicidaroides, Wright, n.s. Pl. IV. fig. 1 a,b,c,d.
Test hemispherical, considerably
depressed ; ambulacral areae with two ranges of from fourteen to six
teen small perforated tubercles, gradually decreasing in size from the
base to the apex ; interambulacral areae with two ranges of primary
tubercles, eight in each range. The supra-anal plate is composed of
several elements ; the anus is situated before and to the left side ;
the surface of the ovarial, ocular, and supra-anal plates is studded
with small granulations ; primary spines long, tapering, smooth and
slightly compressed ; secondary spines small and needle-shaped ; mouth
large and decagonal ; margin reflexed.
Height
7/10ths of an inch, transverse diameter 1 inch and 1/10th. One large
specimen measures 1 inch and 3/10ths in diameter, but the proportional
height cannot be ascertained, as its base is crushed.
Description. - Test spheroidal, depressed ; ambulacral areae
slightly sinuous, nearly uniform in breadth, tapering towards both
poles, and supporting two rows of secondary mammillated perforated
tubercles, which are largest at the inferior third of the area,
diminishing in size as they approach the mouth and the anus. The
tubercles, from fourteen to sixteen in number in each row, are
situated alternately on the margins of the area ; a zigzag line of
granulations, with lateral branches passing down the centre of the
area, separates the tubercles from each other. The poriferous avenues
consist of about forty-five pairs of pores set obliquely in a single
file. The interambulacral areae are three times the breadth of the
ambulacral ; each area is composed of two columns. There ar eight
plates in each column, and each plate supports a large smooth
mammillated eminence surmounted by a tubercle, which occupies the
greater part of the plate ; it is of a conical form, and is encircled
by a concave smooth areaola. The summits of the mammae are sculptured
on their margins with eleven crenulations, in the centre of which a
deeply perforated tubercle rises, with a rather depressed articular
surface. In some specimens the areaolae of the mammae are confluent,
in others they are separated by a row of small granules. the external
and internal margins of the plates are furnished with rows of small
granulations, with still smaller granules here and there interspersed
; on the external side of each plate there are nine granulations,
which, with those of the adjoining plates, form a sinuous granulated
line which defines the internal boundary of the poriferous avenues.
The internal row of granulations, with those of the opposite and
adjoining plates, form a double granulated zigzag space, occupying the
centre of the areae, and forming an elevated ridge which serves to
separate the two ranges of primary tubercles from each other.
The
mouth is large and decagonal, and is one-half the diameter of the
test. The margin is deeply notched with ten indentations. The
divisions of the circumference are not equal, as the arch over the
ambulacral is one-half greater than the arch over the interambulacral
areae.
The
apical disc is greatly developed, occupying more than one-third the
diameter of the test ; it is of a pentagonal form, the left anterior
angle being more developed than the right. The madreporiform plate is
large, and divided into a posterior porous and an anterior non-porous
segment. The posterior pair of ovarial plates are likewise large, the
anterior pair are small and imperfectly develope ; the left plate is
rudimentary, in consequence of the anal opening being eccentric and
situated before and towards the left side ; the supra-anal plate is in
general of a pentagonal form, and composed of from four to six
elements united together and set round the posterior border of the
anal opening. The ocular plates are triangular and well-developed ;
all the plates of the apical disc are studded with small granules.
This species belongs to Agassiz's first division of the
Salenians which have the
sur-anal plate and the oviductal apparatus situated before the
madreporiform plate. The primary spines (fig. 1d) are long,
tapering, and slightly compressed, so that a transverse section of one
of ther forms an ellipsis in the specimen before me. They are in
length about twice the diameter of the test. The body of the spine is
smooth througthout ; the base is encircled with a prominent elevated
ring of small oblong closely-set granulations ; a smaller circle of
larger crenulations surrounding the margin of the concave articulating
surface. The secondary spines articulating with the tubercles of the
ambulacral areae resemble the primaries in miniature, some of them
measuring 3/10ths of an inch in length.
The
dental apparatus is well-developed. The teeth are strong, triangular,
and slightly curved towards the point.
Affinities and differences. - Acrosalenia hemicidaroides is
distinguished from its congeners by its size, the number and
regularity of the primary tubercles, the compound structure of the
supra-anal plate, and the granular surface of the apical disc. This
Urchin so much resembles a Hemicidaris in the form of the test,
the structure of the ambulacra and poriferous avenues, that it was not
until we had obtained specimens with the apical disc preserved that we
were satisfied of its being an Acrosalenia, of which it
certainly forms the finest species. The genera Hemicidaris and
Acrosalenia have so many characters in common, which are
almost always well-preserved, and so few that are special, and
which ar for the most part either broken or absent, that it is
difficult to decide upon the genus unless the apical disc is more or
less preserved ; it is for this reason we conjecture that so few
Acrosaleniae have geen hitherto catalogued from the Oolites, most
of the species having been erroneously referred to other genera.
The development of from four to six larger mammillated tubercles
at the base of the ambulacral areae is a good character for
Hemicidaris. In A. hemicidaroides the tubercles in this region
are well developed, but are not so well defined as in Hemicidaris.
When doubts exist, they can only be solved by the discovery of the
apical disc with its supra-anal plate.
Locality and stratigraphical range. - I have collected this
beautiful Urchin from the upper beds of the Inferior Oolite at
Leckhampton, and the Rev. P. B. Brodie found it with its spines
attached in the same zone at Selsley Hill. It is found in the planking
beds of the Great Oolite at Minchinhampton, and in the Cornbrash near
Chippenham. Several fine specimens with the spines attached to the
test were obtained from the Forest marble near Malmsbury in Wilts,
which are now in the British Museum and the Museum of Economic Geology,
and several private cabinets. We have the same species from Kiddington,
Oxforshire, in slabs of Great Oolite. From these facts we infer that
this large Acrosalenian had not only a considerable
stratigraphical range, but likewise that the species was very abundant.
Pl. IV. fig. 1
a,b,c,d, d'après Wright
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Description de l'espèce par Wright |
Monograph of the British fossil Echinodermata of the Oolitic
Formations, p.234 |
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Acrosalenia hemicidaroides,
Wright. Pl. XV, fig.4 a, b, c, d, e, f, g, h, l, m.
Acrosalenia hemicidaroides |
Wright, Annals
and Magazine of Natural History, 2d ser., vol. viii, p. 161, pl.
11, fig. 1. |
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Forbes, Memoirs
of the Geological Survey, Decade IV, l. 2. |
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Forbes, in
Morris's Catalogue of British Fossils, 2d edit., p. 70. |
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Desor, Synopsis
des Echinides Fossiles, p. 144. |
Test
hemispherical, more or less depressed, sometimes elevated ; ambulacral
areas narrrow, undulated, with two rows of small, perforated tubercles,
fourteen to sixteen in each row, which alternate on the borders of the
area, and gradually diminish in size from the base to the apex ;
inter-ambulacral areas with large prominent tubercles on the sides,
and small tubercles near the disc ; arealas sub-confluent ; miliary
zone narrow, with two rows of granules ; apical disc very large ;
sur-anal plate composed of six elements ; mouth large, decagonal ;
peristome deeply notched ; primary spines twice or more in lenght the
diameter of the test ; stem sub-angular, tapering, or slightly
compressed ; extremity sometimes bifid or trifid.
Dimensions. - This species varies so much in size and figure, that I
have selected four specimens on account of their differences, the
comparative dimensions of which are shown in the following table :
Acrosalenia hemicidaroides
Wright. |
Largest form. |
Elevated form. |
Depressed form. |
Common small form. |
Inch. |
Inch. |
Inch. |
Inch. |
Transverse diameter of test
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1
4/10 |
0
3/20 |
1
1/10 |
0
6/10 |
Height of test .
. . |
0
9/10 |
0
74/10 |
0
6/10 |
0
1/3 |
Diameter of mouth opening
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0
7/10 |
0
11/20 |
0
1/2 |
0
1/3 |
Length of apical disc
. . |
0
5/10 |
0
9/20 |
0
4/10 |
0
3/10 |
Description. - This is the most common and best preserved of all
our fossil sea-urchins ; it has long been known as a Cornbash species,
but was neither named, figured, nor described, until I gave its
history, with figures and details, in my "Memoir on the Cidaridae of
the Oolites ;" since then it has been figured and described by
Professor Forbes in the fourth Decade of the "Memoirs of the
Geological Survey;" nd by M. Desor, in tabl. XX, figs. 19-23, of his
valuable "Synopsis des Echinides Fossiles." This species
exhibits much variation in size and figure, but its diagnostic
characters are preserved with remarkable uniformity throughout these
different phases of form and magnitude.
The test is sometimes elevated and globular, like a Hemicidaris
; indeed, the large forms, the dimensions of which are given in the
first column of the table of measurements, are commonly so named ; the
absence of semi-tubercles at the base of the ambulacra, and the large
size of the elongated discal opening, are the only characters by which
they ca be distinguished from that genus. In the more common form
(fig. 4 c), the body is spheroidal and depressed on the upper
surface ; and, when the flattening is excessive, it produces the
depressed form of the third column.
The ambulacral areas are narrow and moderately prominent (fig. 4 a)
; they are nearly of a uniform width, gradually expanding in the lower
half, and tapering in the upper ; they exhibit a very slight
undulating contour, and have two rows of small, nearly equal-sized
secondary tubercles, from sixteen to eighteen in each row (fig. 4 c)
; the tubercles at the basal angle are the largest (fig. 4 b,
e), and they imperceptibly diminish in size from the
circumference to the disc (fig. 4 a), they are all perforated
and raised on bosses, which have ten crenulations on their summits
(fig. 4 d) ; the tubercles of each row alternate, and in the
centre of the area there are one or two rows of granules, which send
off small lateral branches to encircle the areolas (fig. 4 d, e).
The inter-ambulacral areas are nearly four times as wide as the
ambulacral ; they consist of two columns, each composed of seven or
eight plates, each plate bearing a primary tubercle (fig.4d) ;
the two plates nearest the peristome are very small (fig. 4b),
the four on the sides are very large (fig.4c), and the two near
the disc are small(fig.4a) ; the tubercles are elevated on very
large bosses (fig.4f), which have ten or more deep crenulations
on their summits, the tubercles themselves are perforated ; around the
base of the boss there is a wide, smooth areola ; the plates are
bordered by a single row of granules (fig.4d), which, however,
is sometimes absent from the upper and lower borders, the areolas then
being confluent ; the miliary zone is narrow, and is formed of two
rows of granules, with the intermediate angles having a few smaller
additional granules introduced ; the areolas are separated from the
poriferous zones by a row of granules on the zonal side of the plates
(fig.4d).
The poriferous zones are narrow, the pores unigeminal throughout,
except at the base, where they fall into triple oblique rows ; the
septa form small elevations on the surface, and a beaded line thereby
passes down the zone between the pores forming a pair (fig.4d),
and there are nine or ten pairs of pores opposite each tubercular
plate.
The apical disc is often admirably preserved in this beautiful urchin
; the study of its curious structure first enabled me to correct M.
Agassiz's erroneous supposition, that the genital plate, which carries
the madreporiform body, is the single plate, and represents the
posterior side of the animal, instead of the right antero-lateral
plate which occupies the same relative position in all the
Echinoidea.
The disc is one third the width of the test, and in cosequence of the
projection of the genital plates has a pentagonal form ; it is
slightly convex and prominent, the anterior and posterior pair of
genital plates are nearly of the same size (fig.4 a, i), the
right anterior is the largest, and carriest on its front part the
madreporiform body ; the small crescentic-shaped single plate forms
the posterior boundary of the vent (fig. 4i) ; the oviductal
holes are all near the apices ; the sur-anal plate is composed of xis
or seven pieces arranged like mosaic before the anal opening ; the
ocular plates are small and firmly wedged between the genital and
sur-anal elements. All the plates of the apical disc have numerous
granules scattered on their surface.
The mouth opening is wide, nearly one half the diameter of the text ;
the peristome is decagonal ; the ambulacral being larger than the
inter-ambulacral lobes, the ten deep notches, with reflected edges,
indent the bases of the inter-ambulacra, and extend as far as the
areolas of the second or third tubercles.
The primary spines are finely preserved in situ in fig. 4 k ;
they are variable in size in the same and in different specimens, and
are proportionally shorter in young than in old urchins ; sometimes
they are three times the length of the diameter of the body (fig.4
b), and are sometimes nearly three inches and a half in length ;
the head is conical, with a truncated extremity marked by deep
creulations (fig.4 m), the ring is prominent, and the milling
is angular and sharp ; the stem (fig. 4b) swells out beyond the
ring, it is more or less irregularly sub-angular, with the angles
rounded ; a transverse section of one of the spines exhibits an
irregularly elliptical figure ; sometimes the spine tapers to a
conical point, or the distal end terminates in a bifid or trifid
extremity. The secondary spines articulating with the ambulacral
tubercles (fig. 4 n) are short, about three tenths of an inch
in length, they are round, and taper gently from the ring to the
point, their surface being covered with fine longitudinal lines (fig.
4n).
The jaws are preserved in one or two specimens (fig. 4 g) ; the
lantern is strong (fig.4 h), the teeth conical, and in its
general appearance the dental apparatus closely resembles that of an
Echinus.
Affinities and differences. - This urchin very much resembles a
Hemicidaris ; in fact, Acrosalenia and Hemicidaris
have so many characters in common, which are always well preserved,
and so few that are diagnostic, and which for the most part are either
broken or absent, that it requires considerable practice, when the
apical disc is wanting, to determine the genus ; the absence of semi-tubercles
at the base of the ambulacrea and the magnitude and pentagonal form of
the discal opening serve as good guides to the genus. Acrosalenia
hemicidaroides is distinguished from A. Lycettii by having a
larger and more spheroidal test, larges bosses on the sides, and
smaller ambulacral tubercles ; the apical disc is larger, and the
sur-anal plate is composed of a greater number of pieces.
Acrosalenia hemicidaroides is distinguished from A. pustulata
in having regular rows of secondary tubercles in the ambulacral areas,
which are larger and more fully developed ; the miliary zone is
narrower, with only two row of granules ; the primary tubercles are
more developed at the upper surface, and the apical disc is likewise
larger.
The same characters distinguish it from A. Wiltonii ; but
besides those already enumerated, that species has four rows of fine
granules in the miliary zone, smaller tubercles, suddenly diminishing
at the upper surface, and a much smaller mouth opening. The complex
character of the sur-anal plate, the size of the test and of its
primary tubercles, readily separate it from A. spinosa.
Locality and Stratigraphical position. - The finest specimens
of this urchin with their spines attached (fig. 4 k) have been
collected by Mr. William Buy, from the Forest Marble, near Malmesbury,
in a thin vein of clay, which, according to that acute and careful
collector, separates the Cornbrash from the Forest Marble. The beauty
of these specimens, and the admirable state of preservation in which
they are found, forms one of the marvels of the Oolitic fauna ; a
great quantity of fine tests are collected from the gray brashy beds
of the Cornbrash near Chippenham. Mr. Bristow obtained it from the
Cornbrash near Wincanton ; Mr. Pratt from the Forest Marble at Hinton
Abbey ; Mr. Hull found very large specimens in a cream-coloured,
calcareous, semi-indurated, marly bed of the Great Oolite near Burford,
in a quarry not far from the Bird-in-hand Inn. I discovered two
specimens in the Great Oolite limestone of Minchinhampton Common. The
specimens said to have been found in the Inferior Oolite have been
ascertained to be A. Lycetti. The Rev. A. W. Griesbach
collected quinquefid spines of this urchin in the Great Oolite at
Wollaston, Northamptonshire, along with Acrosalenia pustulata.
This species, therefore, belongs to the Bathonian stage, and is a very
characteristic urchin of this great zone of life.
Pl. XV, fig.4
a, b, c, d, e, f, g, h, l, m, d'après Wright
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Type de
Acrosalenia
pustulata
Forbes,1850, considéré ici
comme synonyme subjectif de Acrosalenia hemicidaroides conservé
au British Geologica Survey |
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Diagnose originale de l'espèce pustulata par Forbes 1852 |
Figures and description of British Organic Remains, decae IV, p.4 |
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non différencié |
crédit
British Geological Survey
specimen BGS GSM43891
Forbes 1850
Figures & description of British Organic Remains, dec. IV, p.4
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Acrosalenia
hemicidaroides, Wright, 1851 -
Bathonien supérieur, Haut Rhin, test 30mm |
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Acrosalenia
hemicidaroides
WRIGHT,1851 var.
bradfordensis
Rigaux, 1881 - Bathonien
supérieur, Suisse, 32 mm |
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Acrosalenia
lapparenti
Cotteau, 1879 |
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diagnose originale de l'espèce par Cotteau |
Paléontologie française, terrains jurassiques, échinides réguliers, p.378 |
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N° 245. -
Acrosalenia Lapparenti, Cotteau, 1879
Pl. 245, fig.
4-11.
Espèce de trande taille, subcirculaire, médiocrement renflée en
dessus, presque plane en dessous. Zones porifères, à fleur du test,
formées de pores simples séparés par un etit renflement granuliforme
très taillant, se multipliant à peine aux approches du péristome.
Aires ambulacraires étroites, légèrement bombées, garnies de deux
rangées de petits tubercules crénelés, perforés et très régulièrement
espacés, augmentant un peu de volume au fur et à mesure qu'ils
s'éloignent du sommet. L'espace qui sépare les deux rangées est assez
large et rempli de granules inégaux groupés autour des tubercules en
séries d'autant plus régulières qu'on se rapproche de l'ambitus et de
la face inférieure. De petites verrues microscopiques se montrent ça
et là au milieu des granules. Aires interambulacraires pourvues de
deux rangées de tubercules principaux, au nombre de douze à treize par
série, fortement crénelés et perforés, très saillants, serrés et
elliptiques vers l'ambitus et à la face supérieure, beaucoup plus
petits et plus espacés au approches du sommet. Le scrobicule qui
entoure les tubercules, très elliptique à l'ambitus, circulaire et
presque nul à la face supérieur, est bordé de granules serrés,
inégaux, à peu près identiques à ceux qui remplissent l'espace
intermédiaire. La bande de test séparant les scrobicules des zones
porifères est assez large et garnie comme la zone miliaire, de
granules inégaux, irrégulièrement disposés, et auxquels se mêlent de
petites verrues microscopiques. La zone miliaire est bien développée,
peu sinueuse, presque nue à la face supérieure. Péristome relativement
peu étendu, un peu enfoncé, marqué d'entailles profondes et relevées
sur les bords. L'appareil apical n'est pas conservé dans l'exemplaire
unique que nous avons sous les yeux ; à en juger par l'empreinte qu'il
a laissée, il était grand, pentagonal et un peu allongé dans le sens
du diamètre antéro-postérieur.
Hauteur, 17 millimètres ; diamètre, 31 millimètres.
Rapports et différences.
- Ce n'est pas sans quelque hésitation que nous avons séparé cette
espèce de l'A. hemicidaroides ; elle nous an paru cependant, en
l'étudiant avec détail, s'en éloigner par plusieurs caractères qui ne
manquent pas d'importance, par sa taille plus forte, par sa forme
générale plus circulaire, |
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moins élevée, par ses aires
ambulacraires présentant deux rangées de petits tubercules séparées
par une zone miliaire plus développée et plus granuleuse, par ses
tubercules interambulacraires plus petits à la face supérieure, plus nombreux et
plus serrés vers l'ambitus, éloignés des zones porifères par une bande
de test plus étendue, par sa zone miliaire plus large, moins sinueuse
et garnie vers l'ambitus de granules plus serrés et plus abondants.
Localité. - Raucourt
(Ardennes). Très rare. Etage bathonien, zone à Terebratula cardium.
Ecole
des mines (M. de Lapparent).
Explication des figures.
- Pl. 245, fig. 4, A. Lapparenti, vu de côté ; fig. 5, face
sup. ; fig. 6, face inf. ; fig. 7, portion de l'aire ambulacraire
prise à la face supérieure, grossie ; fig. 8, portion de l'iare
ambulacraire prise à la face inférieure, grossie ; fig. 9, plaques
interambulacraires de la face supérieure grossies; fig. 10, plaques
interambulacraires prises vers l'ambitus grossies ; fig. 11, tubercule
interambulacraire grossi, vu de profil.
Planche 245,
fig.4-11 d'après Cotteau
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Acrosalenia
lapparenti
Cotteau, 1879 -
Bajocien, Orne, 25 mm |
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Acrosalenia
lapparenti
Cotteau, 1879 -
Bajocien supérieur, Arçonnay, Orne, 15 mm |
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Acrosalenia
lycetti
WRIGHT,1851 |
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Diagnose originale de l'espèce par Wright |
On the Cidaridae of the Oolites, 1851, p.156 |
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Acrosalenia Lycetti, Wright, n.s. Pl. IV. fig. 2 a,b,c,d.
Test hemispherical,
depressed ; circumference subpentagonal ; ambulacral areae prominent,
having a double series of small tubercles ; interambulacral areae with
two ranges of large tubercles ; mammillary eminences of both areae
conical and projecting ; tubercles of the interambulacral areae
disproportionately small.
Height
half an inch, transverse diameter 1 inch.
Description. - This Urchin resembles A. hemicidaroides in
many of its characters, but presents others which justify its
separation from that species. The ambulacral areae are straight,
prominent, and furnished with a double row of small well-developed
tubercles, about twelve in each row ; a zigzag line of small granules
descends down the centre of the areae, sending out lateral branches
which inclose the areolae of the tubercles for about two-thirds of
their circumference, leaving the areolae open to the poriferous
avenues. The interambulacral areae are nearly three times the width of
the ambulacral, and possess a double range of primary tubercles from
seven to eight in each range. The mammillary eminences supporting them
are very prominent, and are surrounded by an elliptical areola. The
summits of the mammae are scultured with about ten crenulations. The
tubercles are disproportionately small when compared with the
development of the mammae supporting them ; the two ranges of
tubercles are separated by four rows of granulations which form zigzag
granular bands descending down the centre of the areae ; similar gands
of granulations bound the external borders of the interambulacra, and
separate the ranges of the principal tubercles from the poriferous
avnues ; the upper and lower borders of the areolae are confluent, but
the other parts of their circumberence are surrounded by a wreath of
granules. The mammillary eminences and tubercles are largest at the
equator, gradually diminishing as they approach the oral and anal
poles. The pores are large and disposed obliquely in simple pairs. The
mouth-opening is large and decagonal, the marginal notches being of
moderate depth. The apical disc is absent in all the specimens we have
found ; it is therefore impossible to state whether the anal opening
was situate before or behind the single madreporiform plate.
Affinities and differences. - This species is distinguished from
A. hemicidaroides in having the areaolae more excavated and
elliptical. The granules occupying the intertubercular spaces are
smaller and more numerous. The tubercles of the interambulacra are
disproportionately small when compared with the development of their
mammae ; the circumference has in general a subpentagonal outline,
from the prominence of the ambulacral areae, the double row of
tubercles on which is more fully developed than in A.
hemicidaroides. These differences between the tests of our two
species although inconsiderable are nevertheless connected with others,
which although not seen may be inferred, as the differences in the
size and form of the primary and secondary spines belonging to the
tubercles of both areae leave no doubt on our mind that A. Lycetti
is distinct from A. hemicidaroides, and we know of no other
species among its congeners for which it could be mistaken. A
granulated spine, and of which we give a figure (2 d), found
frequently in the same beds with A. Lycetti, and probably belonging to
this species, if proved to be such, would from an important specific
character.
Locality and stratigraphical range. - We collected this Urchin
from the lower ferruginous beds, Pea-grit, of Crickley Hill, and have
found it in the same stratum at Leckhampton, Cleeve, and Brockhampton
quarries. The specimens are in general much crushed, and the apical
disc is always absent.
The two
specimens which have preserved their form and served for the foregoing
description were only obtained within the las few days ; all those
previously collected having been too much injured to serve for minute
observation.
I
dedicate this species to my friend John Lycett, Esq., one of the
learned authors of a monograph of the Mollusca from the Great Oolite.
Pl. IV. fig. 2
a,b,c,d, d'après Wright
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Acrosalenia
lycetti
WRIGHT,1851
- Bajocien
supérieur, Meurthe et Moselle, 20 mm |
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Acrosalenia
mideltensis
Vadet,2010
- Bajocien, Maroc, 14 mm |
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