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, FEBRUARY 2011, 62, 1, 103—106 doi: 10.2478/v10096-011-0009-8
SHORT COMMUNICATION
A new Middle Miocene Niveria Jousseaume, 1884
(Mollusca: Gastropoda: Trivioidea) from Hungary
DIRK FEHSE
Nippeser Str. 3, D-12524 Berlin, Germany; Dirk.Fehse@rohde-schwarz.com
(Manuscript received November 23, 2010; accepted in revised form December 16, 2010)
Abstract: A new species of Niveria from the Middle Miocene (Badenian) of the Paratethys of Borsodbóta, Hungary is
described. This species is characterized by its callused dorsum and dorsal depression. Niveria jozefgregoi sp. nov. is
discussed with comparative species from the Badenian of Hungary, the Pliocene of the Mediterranean region, Florida
and Recent species from Madeira and the Islas Galápagos.
Key words: Badenian, Paratethys, taxonomy, molluscs, Triviidae.
Introduction
The Miocene Triviidae of Europe have yet to be revised as the
original illustrations and original descriptions are insufficient
and the type specimens are difficult to locate (e.g. collection
Grateloup: Bruno Cahuzac, Université Bordeaux, pers.
comm.). The shell morphology of most species is more or less
similar to Niveria nix (Schilder, 1922) – the type species of
the genus Niveria Jousseaume, 1884 (syn. Sulcotrivia
Schilder, 1933). They are characterized by a dorsal sulcus or a
dorsal depression where the ribs are bisected or depressed.
Therefore, the new species is assigned to the genus Niveria.
There is a small group of species among Niveria that possess
dorsal callosities. Taxa of this group are Niveria permixta (de
Cristofori & Jan, 1832) from the Mediterranean Pliocene,
Niveria floridana (Olsson & Harbison, 1952) and Niveria
incomparabilis Fehse, in print from the Florida Pliocene,
Niveria pulloidea (Dall & Ochsner, 1928) from the Pleis-
tocene and Recent of the Islas Galápagos (Fehse, in print) and
Niveria grohorum Fehse & Grego, 2008 from Madeira. The
first species from the Miocene has been discovered from the
Badenian of the Paratethys of Borsodbóta, Hungary and it is
described herein as Niveria jozefgregoi sp. nov.
Abbreviations
ANSP – Academy of Natural Sciences, Philadelphia,
Pennsylvania, U.S.A.
DFB – Dirk Fehse collection, Berlin, Germany.
GIH – Geological Institute of Hungary, Budapest, Hungary.
JGS – Jozef Grego collection, Banská Bystrica, Slovakia.
ZSM – Zoological State Collection, Munich, Germany.
Superfamily: Trivioidea Troschel, 1863
Family: Triviidae Troschel, 1863
Subfamily: Triviinae Troschel, 1863
Genus: Niveria Jousseaume, 1884
T y p e s p e c i e s: Cypraea nivea Gray, 1824 [ = Trivia nix
Schilder, 1922] by original designation. Recent, Caribbean.
Niveria jozefgregoi sp. nov.
Fig. 1.1—3, Fig. 2.1—5.
H o l o t y p e: Fig. 1.1a—d (ZSM, No. 20100658)
P a r a t y p e 1: Fig. 1.2a—d (DFB, No. 10094-1)
T y p e l o c a l i t y: Borsodbóta, “Királdi-útbevágás”, county
Borsod-Abaúj-Zemplén, Hungary.
T y p e s t r a t u m: Middle Badenian, Tortonian, Middle
Miocene.
D e r i v a t i o n o m i n i s: Named in honour of Jozef Grego,
a personal friend of the author.
S h e l l f o r m u l a: L = 6.7—8.8, W = 75—83 % of length,
D = 63—68 % of length, LT = 17—22, CT = 15—19, RR = 16—20.
A modified shell formula is used herein. This formula is
derived from measurements taken from all available fully
mature and normally formed specimens. L – length in mm,
W – width/length ratio in %, H – height/length ratio in %,
LT – number of labral teeth, CT – number of columellar
teeth, RR – number of dorsal ribs.
Description
Shell small sized, solid and roundly ovate. Spire slightly el-
evated and covered by callus. Body whorl ovate, inflated and
Academy of Natural Sciences, Philadelphia,
Pennsylvania, U.S.A.
Dirk Fehse collection, Berlin, Germany.
Geological Institute of Hungary, Budapest, Hungary.
Jozef Grego collection, Banská Bystrica, Slovakia.
Zoological State Collection, Munich, Germany.
ANSP
DFB
GIH
JGS
ZSM
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rounded, about 90 % of total height, with both terminals pro-
duced and blunt terminal tips. Dorsum highly elevated, with a
hump nearly on mid-portion and a mid-dorsal depression that
bisects or depresses the ribs. Ribs coarse, somewhat irregular,
covered by callus on dorsal summit. Ventrum slightly convex
with straight terminals. Aperture narrow, almost straight, wid-
ened slightly at the fossular section. Labrum roundly callused,
narrow, widened at its mid-portion, curved, keeled towards its
inner margin, anteriorly declivous. Outer labral margin acute-
ly shouldered. Labrum bears on its inner margin 17—22 fine
denticles. Denticles continued as fine folds onto labrum, be-
coming broader onto dorsum and ventrum, narrowing onto
columella and fossula. Siphonal and anal canals follow shell
profile. Columella is concave, broad and tapering steeply in-
wards. Parietal lip slightly roundly callused, bears 15—19 fine
ribs. Fossula broadly concave, not clearly delimited from the
rest of the columella. Inner fossular and columellar edge den-
ticulated, covered by labrum on ventral view. Inner fossular
edge slightly protruded.
Variations
Shell outline varies from almost circular to ovate. Mid-
dorsal callosity more or less developed. Dorsal depression
sometimes obscured. The development of the dorsal hump
varies slightly. The dorsal ribs are sometimes somewhat
broader than in some specimens.
Fig. 1. 1a,b,c,d – Niveria
jozefgregoi nov. sp. Holotype,
ZSM, No. 20100658, Middle
Badenian, Middle Miocene,
Borsodbóta, county Borsod-
Abaúj-Zemplén,
Hungary.
2a,b,c,d – Niveria jozefgregoi
nov. sp. Paratype 3, coll. JGS,
No. T0701/1, Middle Bade-
nian, Middle Miocene, Bor-
sodbóta,
county
Borsod-
Abaúj-Zemplén,
Hungary.
3a,b,c,d – Niveria jozefgregoi
nov. sp. Paratype 4, coll. JGS,
No. T0701/2, Middle Bade-
nian,
Middle
Miocene,
Borsodbóta, county Borsod-
Abaúj-Zemplén,
Hungary.
4a,b,c,d – Niveria jozefgregoi
nov. sp. Paratype 5, coll. JGS,
No. T0701/3, Middle Bade-
nian, Middle Miocene, Bor-
sodbóta,
county
Borsod-
Abaúj-Zemplén, Hungary.
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A NEW MIDDLE MIOCENE NIVERIA JOUSSEAUME, 1884 (MOLLUSCA: GASTROPODA: TRIVIOIDEA)
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Material and measurements
Total number of 8 specimens were examined in detail. This
material was collected by the author and J. Grego at “királdi út-
bevágás” Borsodbóta village during the years 2003 and 2005.
Holotype: L = 8.8 mm, W = 6.8 mm, D = 5.8 mm, CT 19,
LT 22, RR 20 (ZSM, No. 20100658)
Paratype 1: L = 7.1 mm, W = 5.7 mm, D = 4.7 mm, CT 15,
LT 18, RR 18 (DFB, No. 10094-1)
Paratype 2: L = 7.2 mm, W = 5.4 mm, D = 4.5 mm, CT 15,
LT 17, RR 16 (DFB, No. 10094-2)
Paratype 3: L = 8.0 mm, W = 6.6 mm, D = 5.4 mm, CT 16,
LT 17, RR 18 (coll. JGS, No. T0701/1)
Paratype 4: L = 7.4 mm, W = 5.8 mm, D = 4.8 mm, CT 15,
LT 17, RR 16 (coll. JGS, No. T0701/2)
Paratype 5: L = 7.0 mm, W = 5.6 mm, D = 4.7 mm, CT 16,
LT 17, RR 18 (coll. JGS, No. T0701/3)
Paratype 6: L = 6.7 mm, W = 5.0 mm, D = 4.4 mm, CT 15,
LT 17, RR 20 (coll. JGS, No. T0701/4)
Discussion
The new species is assigned to the genus Niveria Jous-
seaume, 1884 because all taxa in the genus have a dorsal fur-
row or depression that is crossed by ribs.
Fig. 2. 1a,b,c,d – Niveria jozefgregoi
nov. sp. Paratype 2, coll. DFB,
No. 10094-1, Middle Badenian, Middle
Miocene, Borsodbóta, county Borsod-
Abaúj-Zemplén, Hungary. 2a,b,c,d –
Niveria jozefgregoi nov. sp. Paratype 6,
coll. JGS, No. T0701/4, Middle Bade-
nian, Middle Miocene, Borsodbóta,
county Borsod-Abaúj-Zemplén, Hun-
gary. 3a,b,c,d – Trivia eszterae Fehse
& Vicián, 2006. Holotype, GIH,
No. M.06.24, Middle Badenian, Middle
Miocene, Borsodbóta, county Borsod-
Abaúj-Zemplén, Hungary. 4 – Niveria
floridana (Olsson & Harbison, 1952).
Holotype, ANSP, No. 18611. Pinecrest
Beds, Zanclean, Early Pliocene, St. Pe-
tersburg,
Florida,
U.S.A.
Length
11.1 mm. 5 – Niveria incomparabilis
Fehse, in print. Pinecrest Beds, Zan-
clean, Early Pliocene, Bird Road dig,
Miami, Dade County, Florida, U.S.A.
(after Petuch, 1994: pl. 24, figs. L, M).
Length 12 mm.
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Niveria jozefgregoi sp. nov. is separated from all Miocene
Triviidae by its mid-dorsal callosity. The paratype 5 in
Fig. 1.4 shows only traces of the callosity between the dorsal
ribs four and six. In other specimens the dorsal callosity is
much more developed (e.g. holotype). The congener Trivia
eszterae Fehse & Vicián, 2006 has a similar shell outline and
dorsal hump but lacks the dorsal depression and especially the
dorsal callosity. Furthermore, the ribs are coarser in N.
jozefgregoi sp. nov. The first species with dorsal callosities
were so far known only from the Pliocene with Niveria
permixta (De Cristofori & Jan, 1832) from the north-western
Mediterranean, N. floridana (Olsson & Harbison, 1952) and
N. incomparabilis Fehse, in print, from Florida (Fehse & Lan-
dau 2003; Fehse, in print). The new species differs from N.
permixta by coarser and less numerous ribs (16—20 ribs in N.
jozefgregoi sp. nov. vs. 30—34 in N. permixta), by a smaller
size (average 7.5 mm in N. jozefgregoi sp. nov. vs. 12.6 mm
in N. permixta (Fehse & Landau, 2003)), by a less developed
dorsal depression, narrower columella and fossula and a more
circular shell outline. Niveria floridana and N. incomparabilis
differ from N. jozefgregoi sp. nov. by their well-developed
dorsal sulcus and the formation of their dorsal callosities. The
new species has its callosity on the dorsal summit and the
Florida species have callosities on both sides of their sulcus.
The Florida species also have a different shell morphology.
Niveria floridana has an ovate shell, narrower columella and
fossula, finer ribs and a more developed parietal lip. Niveria
incomparabilis has a broader labrum, a very unique columella
and fossula and finer dorsal ribs. The Pleistocene and Recent
N. pulloidea from the Islas Galápagos is separated from the
new species by the broader labrum, narrower columella and
fossula, indented terminal tips and well-developed parietal lip.
The Recent N. grohorum Fehse & Grego, 2008 is separated
from N. jozefgregoi sp. nov. by the elongated shell outline, the
narrow columella and fossula, well-developed parietal lip,
shorter terminals and less elevated dorsum.
Conclusion
Niveria jozefgregoi sp. nov. appears to be the oldest mem-
ber of a group of species with dorsal callosities. The shell
shape of all the species is superficially similar and indicates
their relationship. At the moment there is a large stratigraph-
ic gap between N. jozefgregoi sp. nov. and N. permixta in the
Late Miocene. Further research in the layers of the Late Mio-
cene especially of the Messinian should close the gap.
Acknowledgments: I am very grateful to Dr. József Kókay
for his help with information about the geology of the locali-
ty. Many thanks to Lindsey T. Groves from the Los Angeles
County Museum, U.S.A. for reviewing the manuscript and
helpful suggestions.
References
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