Monteiroconus strauszi (Kovacs & Vician, 2023)
Monteiroconus subparvicaudatus (Kovacs & Vician, 2014)
Monteiroconus
strauszi (Kovacs &
Vician, 2023)
Diagnosis(2) – Monteiroconus species with moderately large shell, low spire, striate spire whorls,
rounded shoulder, smooth body
whorl, moderately deep, asymmetrically curved
subsutural flexure, colour
pattern of numerous spirals of subrectangular patches on the last whorl.
Description(2) – Moderately large shell (max. SL 69). Low, conical
spire, eroded protoconch, slightly convex and striate spire whorls. Rounded
shoulder, maximum diameter slightly below the shoulder. Elongate, conical last whorl with weak concavity in
the middle, widely spaced spiral cords on the lower half. Moderately narrow,
anteriorly widening aperture. Moderately deep, asymmetrically curved subsutural
flexure. The colour pattern is visible in normal light, it consists of broad
and reddish flammulae on later spire whorls and shoulder, and approx. 20
spirals of reddish, subrectangular patches on the last whorl of adult
specimens.
Remarks(2) – Based on the revised diagnosis
of Monteiroconus by Harzhauser & Landau (2016: 102) (moderately
large to large, relatively solid shells, wide to moderately wide last whorl,
low to almost fl at spire, generally striate spire whorls, medium deep to deep,
moderately to strongly curved and moderately to strongly asymmetrical
subsutural flexure), the new species is assigned to this genus. The size and
morphology of Monteiroconus strauszi n. sp. are close to the holotype of
M. parvicaudatus (Sacco 1893, pl. 3, fi g. 25, refigured by Ferrero
Mortara et al. 1984, pl. 17, fig. 6) from the Middle Miocene of Italy, but the
colour pattern clearly differs as parvicaudatus bears numerous densely
spaced spirals of fine dashes. Monteiroconus hoernesi (Doderlein) is
distinguishable in morphology by shorter shell, and smooth or weakly striate,
canaliculated spire whorls (see Harzhauser & Landau 2016, pl. 26A–C). Monteiroconus strauszi n. sp. is
characterized by moderate intraspecific variability in the height of spire.
Type strata(2)
– Lower Badenian (Middle Miocene)
clayey sand (Lajta Limestone Formation).
Type locality(2)
– Letkés, W Börzsöny Mts, Hungary.
Other locality - Piedmont
Derivation of name(2) – In honour of László Strausz,
Hungarian palaeontologist (1901–1988).
|
Monteiroconus strausziMiddle
Miocene Börzsöny
(Hungary) Fig. 28 : v. Fig. 75 - Conus subparvicaudatus (1), Holotype INV
2013.237 mm. 58 x 34 Fig. 29 : v. Fig. 74 - Conus subparvicaudatus (1), Holotype INV
2013.237 mm. 58 x 34 Fig. 30 : HNHM
PAL 2023.3.1 Fig. 31 : HNHM
PAL 2023.4.1 Fig. 32 : HNHM
PAL 2023.4.1 Fig. 33 : v. Fig. 16 - Conus subparvicaudatus (2014), PCV.2018.08.01., Coll. Zoltán
Vicián |
Monteiroconus subparvicaudatus (Kovacs & Vician, 2014)
L’articolo non
mi sembra che sia mai stato pubblicato. Descrizione, caratteristiche e immagini
provengono da un documento inviatomi personalmente da Vician:
Si tratta di una conchiglia abbastanza grande, con la spira bassa, le cui spirali sono striate; la spalla č arrotondata, con il corpo principale liscio. La curva subuturale č moderatamente profonda, asimmetricamente curva; la colorazione č formata da numerose spirali di macchie subrettangolari sull'ultima spirale.
Holotype:
INV 2013.247.. Hungarian Natural History Museum, Budapest, SL 58.
(Kovacs & Vician 2014. figs 74-75. refigured here on Plate 2, figs
14-15).
Paratypes: 1: INV 2013.239., HNHM, SL26,
(illustration: Kovacs &Vician 2014, fig. 76), 2: PCV.2018.08.01., Private
Coll. Zoltan Vician, SI. 37, (Plate 2, figs 16-17).
Type strata: Lower Badenian (Middle Miocene) clayey
sand(Leitha Limestone Formation).
Type locality: Letkets. W Borzsony Mts, Hungary.
Derivation of name: Reference to the similarity to Monteiroconus
parvicaudatus (sacco. 1893).
Material: 72 specimens.
Diagnosis: Moderately large shell, low spire, striate
spire whorls, rounded shoulder, smooth body whorl, moderately deep,
asymmetrically curved subsutural flexure, color pattern of numerous spirals of
subrectangular patches on the last whorl.
Description: Moderately large shell (SI. max. 69).
Low, conical spire, eroded protoconch, slightly convex and striate spire
whorls. Rounded shoulder, maximum diameter slightly below the shoulder. Elongate, conical last whorl
with weak concavity in the middle, widely spaced spiral cords on the lower
half. Moderately narrow, anteriorly widening aperture. Moderately deep,
asymmetrically curved subsulural flexure. The color pattern is visible in
normal light, it consists
of broad and reddish flammulae on later spire whorls and shoulder, and approx.
20 spirals of reddish, subrectangular patches on the last whorl of adult
specimens.
Remarks: Based on the revised diagnosis of genus Monteiroconus
by hakzhauser & landau (2016: 102) (moderately large to
large, relatively solid shells, wide to moderately wide last whorl, low to
almost flat spire, generally striate spire whorls, medium deep to deep,
moderately to strongly curved and moderately To strongly asymmetrical subsutural flexure) the
new species is assigned to genus Monteiroconus. The size and morphology
of M. subparvicaudatus n. sp. Is close to holotype of Monteiroconus
parvicaudatus (Sacco, 1893, pl. 3 fig. 25, refigured
by Ferrero Mortara et. Al. 1984, pl. 17, fig. 6) from the Middle Miocene of
Italy, but the color pattern clearly differs as parvicaudatus bears
numerous densely spaced spiral of fine dashes.
M. hornesi (Doderline, 1863) is
distinguishable in morphology by shorter shell, and smooth or weakly striate,
canaliculate spire whorls.
Asymmetrical
subsutural flexure) the new species is assigned to genus Monteiroconus.
The size and morphology of M. subparvicaudatus n. sp. is close to
holotype of Monteiroconus
parvicaudatus (Sacco, 1893, pl. 3 fig. 25, refigured by Ferrero Mortara
et. Al. 1984, pl. 17, fig. 6) form the Middle Miocene of Italy, but the color
pattern clearly differs as parvicaudatus
bears numerous densely spaced spiral of fine dashes. M. hornesi
(Doderline, 1863) is distinguishable in morphology by shortes shell, and smooth
or weakly striate, canaliculate spire whorls.
Conus subparvicaudatus (1) – Conus strauszi Holotype
INV 2013.237 mm. 58 x 34 |
Conus parvicaudatus (Sacco, 1893) Conus strauszi Tav. III fig. 25 |
Conus subparvicaudatus - Conus
strauszi |
|
Conus subparvicaudatus -
Conus strauszi mm.
55,7 x 32,6 Miocene
(Badeniano) Letkes
– Ungheria [AZFC N. 531-01] |
|
Conus subparvicaudatus- Conus
strauszi mm.
48,2 x 28,7 Miocene
(Badeniano) Letkes
– Ungheria [AZFC N. 531-02]
|
|
|
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Conus subparvicaudatus (1) Conus strauszi INV
2013.237 mm. 58 x 34 Miocene
(Badeniano) Letkes
– Ungheria |
Conus subparvicaudatus
Conus strauszi mm.
55,7 x 32,6 Miocene
(Badeniano) Letkes
– Ungheria [AZFC
N. 531-01] |
Conus
subparvicaudatus
Conus strauszi mm.
48,2 x 28,7 Miocene
(Badeniano) Letkes
– Ungheria [AZFC N. 531-02]
|
Bibliografia Consultata