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V. Garilli, 2008 Page 29
whorls. Protoconch I consisting of about 0.8 whorls (ex CMGR 008/49, coll. V. Garilli); paratype 4 (4.2 × 2.9
sculptured by 5–6 fine spiral lirae interspersed spirally mm), MNHN A25950 (ex CMGR 009/492, coll. V.
and irregularly with microscopic granules. Protoconch II Garilli); paratype 5 (4.6 × 3.1 mm), DGUP CMGR 010/
consisting of about 1.2 whorls sculptured by pimples, 493, coll. V. Garilli; paratype 6 (4.5 × 3.1 mm), DGUP
which are irregular in size and arrangement. They are CM GR 011/494, coll. V. Garilli. All type material is from
larger and less numerous in the adapical position; fused the type locality, 3D1 layer. DATE?
into very short prosocline tracts in central part. In the
abapical part of late protoconch, groups of pimples are Etymology: The species honors the name of both
irregularly fused into fine, discontinuous spiral ridges. Francesco Garilli senior, my father and first mentor in
Protoconch/teleoconch transition well-marked and sinu- my life, and of Francesco Garilli junior, my son.
ous. Teleoconch consisting of 3.8–4.6 (4.2 in holotype)
rather convex whorls, with strong cancellate sculpture Habitat: All the shells came from the 3D1 layer of
formed by intersection of equally developed spiral cords Costa (1989). The paleoenviromental reconstruction for
and axial ribs. Cords are narrow and well raised, num- this layer was characterized by Costa (1989) as compa-
bering 2, 6–7 (6 in holotype) and 13–15 (14 in holotype) rable with the Mediterranean marine-marginal modern
in early, penultimate and body whorl, respectively. Two ecotone HP (Posidonia beds)-SVMC (sensu Pérès and
adapical cords are usually more pronounced in penulti- Picard, 1964). It is interesting that the 3D1 layer is quite
mate and last whorl. Cords are markedly stronger and rich in Posidonia remains mainly consisting of leaves.
more widely spaced on base. Secondary cords may com-
mence on late body whorl, at a certain distance from Distribution: This species is known from type locality
outer lip. Axial sculpture consists of narrow raised ribs only, lower Pleistocene of Cartiera Mulino, Vittoria, Ra-
numbering 24–32 (26 in holotype) on the penultimate gusa, SE Sicily.
whorl. On base, ribs progressively become very narrow to
obsolete toward columellar area. Intersection of spiral Remarks: This quite characteristic species shows a ga-
and axial sculpture, producing nodular small knobs, leodiniform shape, having a quite inflated and well-
forms a rectangular pattern (with major side of rect- developed (also with double varix) last whorl and a large
angles perpendicular to shell axis) except on last whorl, aperture provided with an internally smooth outer lip.
where a quadrangular to rhomboidal pattern occurs (Fig- However, its spiral sculpture does not markedly prevail
ure 43). Microsculpture of very early teleoconch whorls over the axial, as in the typical Alvania carinata. Its mi-
consists of micropustules, sometimes fused, forming spi- crosculpture, limited to the early teleoconch whorls, is
rally, discontinuous and irregular rows, mainly occurring similar to that observed in the analogous whorls of A.
between spiral cords (Figure 42); weak growth lines are carinata, but in the latter this microsculpture is distrib-
present. Fine sculpture of the rest of teleoconch limited uted over the entire teleoconch.
to weak growth lines (Figure 43). Suture slightly in-
clined. Last whorl well-developed, comprising about The strongly cancellated sculptural pattern of A.
three fourths of shell height. It may bear single (paratype francescoi new species, consisting of well-raised, sub-
6) or double (paratype 4, Figure 37) varices, at angles of equal spiral and axial elements forming marked nodular
about 50° and 70° respectively. Aperture wide, ovate, intersections, resembles that shown by A. cimicoides
and with a rounded profile in the posterior part, com- (Forbes, 1844). The latter species, showing a more typi-
prising about two thirds to three fourths of last whorl cal Alvania shape, has a more slender shell, a less inflated
height. Outer lip orthocline, internally smooth, externally and much less developed last whorl, and a proportionally
markedly thickened by a strong, sometimes doubled smaller aperture with denticulations on the inner part of
(Figure 31), rim, occurring very close to its edge and the outer lip.
covered by spiral cords. Inner lip moderately arcuate and
rather thickened, with thin callus delimitating very nar- Alvania francescoi new species can also be compared
row umbilical chink. with A. rosariae new species described later in this re-
port. Remarks on their similarities and differences will
Type Locality: Lower Pleistocene of Cartiera Mulino be dealt with in the section dedicated to the latter spe-
(36°56Ј57Љ N, 14°34Ј03Љ E), Vittoria, Ragusa, SE Sicily. cies.
The stratotype is the phanerogams-rich 3D1 layer of
Costa (1989). This deposit crops out at about one hun- Alvania lactea (Michaud, 1830)
dred meters from the abandoned paper-mill known as (Figures 44–49 and 53–61)
Cartiera Mulino. Paleoenvironmental and stratigraphic
information about this site are given by Costa (1989). Rissoa lactea Michaud, 1830: 9–10, figs. 11–12
Type Material: Holotype (4.3 × 2.8 mm), DGUP Rissoa (Massotia) lactea Michaud.—Bucquoy et al., 1884: 298,
CMRG 005/488, coll. V. Garilli. Paratype 1 (4.1 × 2.7 pl. 25, figs. 7–13
mm), DGUP CMRG 006/489, coll. V. Garilli; paratype 2
(4.8 × 3 mm), ZMA Moll. 4.07.007 (ex CM GR 007/490, Massotia Dajerleini Monterosato ex-Schwartz ms, 1889: 33.
coll. Garilli); paratype 3 (4 × 2.7 mm), ZMB MB.Ga.2479 Massotia lactea (Michaud) forma Dajerleini Monterosato,
1917: 12.
Description: Shell sturdy, conical-ovate to cylindrical-
ovate, occasionally almost pupoid, reaching 5.2 mm in