Morozovella edgari Premoli Silva & Bolli 1973 from: Pearson, P.N.Olsson, R.K.Hemleben, C.Huber, B.T.Berggren, W.A. (2006): Atlas of Eocene Planktonic Foraminifera. p. 1-513 . |
Notice: This catalogue page may contain unedited data.
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Species Morozovella edgari Premoli Silva & Bolli 1973 |
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Diagnosis / Definition: |
Pearson et al. (2006):
DESCRIPTION.
Type of wall: Muricate, nonspinose, normal
perforate.
Test morphology: Low to moderately conical
trochospiral; weakly lobulate peripheral outline, 5-6
gradually enlarging , cuneiform-shaped chambers in last
whorl, intercameral sutures on umbilical side radial,
straight and weakly incised; on spiral side chambers
trapezoidal in shape, separated by distinctly curved
sutures which are flush with the test; early part/chambers
of the test raised (i.e., the test exhibits an unequal
biconvexity); umbilicus narrow, deep; distinct
muricocarina extends to final chamber; aperture a low
umbilical-extraumbilical arch extending nearly to the
periphery; surface distinctly muricate with concentration
of pustules decreasing towards terminal chambers.
Size: Dimensions of holotype: maximum
diameter: 0.2 1 mm. |
Discussion / Comments: |
Toumarkine & Luterbacher (1985):
This species is characterized by its small size, fragile aspect with only a weakly developed ' keel', and the relatively large number of chambers (4 to 6) in the last whorl.
It differs from Morozovella subbotinae by the larger number of chambers in the last whorl and the less lobate peripheral outline. M. formosa gracilis is more robust and has a better-developed 'keel'.
Pearson et al. (2006):
DISTINGUISHING FEATURES.-
This taxon is
characterized by its relatively small size, narrow and
deep umbilicus, and weakly developed peripheral
muricocarina. It bears a close resemblance to juvenile
individuals of M. velascoensis from which it is believed
to have evolved (Kelly and others, 2001).
DISCUSSION.-
This minute morozovellid (test
diameter ranges from 0.2-0.25 mm) is associated with,
and ranges beyond, terminal members of the
Morozovella velascoensis group. Kelly and others (200 1,
p. 507) have suggested that edgari descended from
velascoensis by a process called "terminal progenesis"
in which the diminutive descendant (edgari) with an
adult morphology resembles the juvenile stages of the
ancestral form velascoensis.
Morozovella finchi Blow is placed in the
synonomy of this taxon. It shares most morphologic
features in common with edgari except that the holotype
is somewhat larger (0.32 mm) in diameter. It was
described from Zone P5 (of Blow, 1979) and said to
range to Zone P7 (=E4 of this paper), a range comparable
to that ascribed to edgari here. Blow (1 979, p. 999-1000)
was of the opinion that finchi descended from "Acarinina " trichotrocha and even included a paratype
from the Hornerstown Formation (Zone P4) of New
Jersey (erroneously ascribed to Zone P5) in his new taxon
,finchi, but our examination of this form at the USNM
suggests that this specimen is not ascribable to ,finchi
(=edgari).
PHYLOGENETIC RELATIONSHIPS.-
This taxon
evolved from Morozovella velascoensis (by means of a
gradual decrease in test size and truncation of the ancestral ontogenetic sequence; Kelly and others, 2001)
but does not appear to have left any descendants.
STRATIGRAPHIC RANGE.-
Zone E2 (uppermost
part) to Zone E3.
GEOGRAPHIC DISTRIBUTION.-
Probably widely
distributed in (sub)tropical regions (Caribbean, Atlantic
Ocean and Pacific Ocean) but records are sparse owing
to this taxon having been overlooked heretofore. We have
found this form relatively commonly distributed in lower
Eocene strata (Esna Shales) of Egypt.
STABLE ISOTOPE PALEOBIOL0GY.-
Shallow-intermediate
depth-habitat (Kelly and others, 2001). |
Systematics: |
15 Classis Foraminifera
Genus Morozovella
Species Morozovella edgari
35 Ordo Foraminiferida
Superfamilia Globigerinaceae
Familia Truncorotaloididae
Genus Morozovella
Species Morozovella edgari
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Synonym list: |
Toumarkine & Luterbacher (1985):
1973 Globorotalia edgari Premoli Silva & Bolli. - Premoli Silva & Bolli : p.525 pl 7 figs 10-12, pl 8 figs 1-12 (type reference)
1985 Morozovella edgari Premoli Silva & Bolli. - Toumarkine & Luterbacher : p.113 fig 15.6
Pearson et al. (2006):
1973 Globorotalia edgari Premoli Silva & Bolli. - Premoli Silva & Bolli : p.526 pl. 7, fig. 10-12;
pl. 8, fig. 1 (holotype)-12 [Globorotalia
edgari Zone, DSDP Site 152, Nicaragua Rise, Caribbean
Sea]
1985 Morozovella edgari Premoli Silva & Bolli. - Toumarkine & Luterbacher : p.114 text-fig. 15.6a (holotype) and 6b, c (paratypes)reillustrated
2001 Morozovella edgari Premoli Silva & Bolli. - Kelly et al. : p.509 text-fig. 1D-F;
text-fig. 3C [lower Eocene, ODP Hole 865B, Allison Guyot, Mid-Pacific Mountains, Pacific Ocean];
text-fig. 2E [Zone P6a, DSDP Site 152,
Caribbean Sea]
2006 Morozovella edgari Premoli Silva & Bolli. - Pearson et al. : p.356 pl. 11.6; fig. 1-16 (Pl. 11.6, Figs. 1-7: reillustrations of holotype and
paratypes of Globorotalia edgari Premoli Silva and
Bolli)
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Specimen: |
National Museum of Natural History, Basel, Inventory number: C-29482
National Museum of Natural History, Basel, Inventory number: C-29483
National Museum of Natural History, Basel, Inventory number: C-29484
National Museum of Natural History, Basel, Inventory number: C-29485
National Museum of Natural History, Basel, Inventory number: C-29486
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References: |
Premoli Silva,I. and Bolli,H.M. (1973): Late Cretaceous to Eocene planktonic foraminifera and stratigraphy of Legs 15 sites in the Carribean Sea. In: Initial Reports of the Deep Sea Drilling Program Vol. 15 p. 449-547
Blow,W.H. (1979): The Cainozoic Globigerinida. 3 Vols p. 1413 pp
Toumarkine,M. and Luterbacher,H.P. (1985): Paleocene and Eocene Planktic Foraminifera. In: Plankton Stratigraphy p. 87-154
Kelly,D.C.; Bralower,T.J. and Zachos,J.C. (2001): On the demise of the Early Paleogene Morozovella velascoensis lineage: terminal progenesis in the planktonic Foraminifera . Palaios Vol. 16 p. 507-523
Pearson,P.N.; Olsson,R.K.; Hemleben,C.; Huber,B.T. and Berggren,W.A. (2006): Atlas of Eocene Planktonic Foraminifera. p. 1-513
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