radiolaria - rads_cenozoic - Cypassis irregularis radiolaria - rads_cenozoic - Cypassis irregularis

Cypassis irregularis


Classification: rads_cenozoic -> Coccodiscidae -> Cypassis -> Cypassis irregularis
Sister taxa: C. irregularis, C. sp.

Taxonomy

Citation: Cypassis irregularis Nigrini 1968
taxonomic rank: species
Basionym: Cypassis irregularis
Synonyms:
1912 ?Spongoliva ellipsoides - Popofsky p. 117; text-fig. 28
1960 Spongoliva sp. - Hollande and Enjumet pl. 63
1966 Spongoliva cf. ellipsoides - Benson p. 190-193; pl. 8, figs. 6-7
1968 Cypassis irregularis - Nigrini p. 53; pl. 1, figs. 2a-c
1977 Cypassis irregularis - Kling p. 215; pl. 2. fig. 5
1983 Cypassis irregularis - Benson p. 502

From Suzuki Paleotax db:

1968 Cypassis irregularis n. sp. Nigrini p. 53, pl. 1, fig. 2a, 2b, 2c
1973 Cypassis irregularis Nigrini Barwiczp. 234, pl. 3, fig. 7
1977 Cypassis irregularis Nigrini Kling p. 215, pl. 2, fig. 5
1979 Cypassis irregularis Nigrini Kling p. 309, pl. 1, fig. 3
1980 Cypassis irregularis Nigrini Johnson & Nigrini p. 121, text-fig. 5f, pl. 1, fig. 18
1992 Cypassis irregularis Nigrini Nigrini & Caulet p. 145, pl. 1, figs. 5-7
1993 Cypassis irregularis Nigrini Tan p. 210-211, pl. 3, figs. 4, 5
1996 Cypassis irregularis Nigrini Chen & Tan p. 179-180, pl. 12, figs. 1-4
1998 Cypassis irregularis Nigrini Tan p. 198-199, text-fig. 192, pl. 13, figs. 3, 4
1999 Cypassis irregularis Nigrini Tan & Chen p. 202, pl. 7, figs. 9, 19; text-fig. 5.113
Taxonomic discussion: Nigrini 1968; Sanfilippo and Riedel, 1970

Catalog entries: Cypassis irregularis

Original description: Cortical twin shell spiny, slightly constricted equatorially, with subcircular to subangular pores having no definite arrangement; pores variable in size, tending to be smaller equatorially. Poles of twin shell not closed by a definite lattice, always spiny. In some specimens these spines support an irregular, usually incomplete, spongy meshwork. When complete, this meshwork forms an ellipsoidal shell around the cortical shell. Polar caps have not been observed.
Outer medullary shell ellipsoidal, connected to an inner, spherical medullary shell by radial beams; numerous radial beams also connect outer medullary shell to cortical twin shell at the equatorial constriction.

Length of cortical twin shell 118-1 84µm. Maximum breadth of cortical twin shell 63-99µm,
Remarks on original description: Rare in samples from along the coast of Central and South America; absent from all other samples examined (text-figure 4).

Description


Published descriptions


Benson 1966 - Spongoliva ellipsoides

Complete tests with two medullary shells joined by numerous (15-20 or more, confined to the equatorial region) cylindrical radial beams to the slight equatorial constriction of the subcylindrical cortical shell which, in most specimens, is present as a distinct, latticed shell, shaped like a figure 8, but with its polar surfaces not closed by a definite lattice, instead either more or less open or covered only by a few irregular bars; numerous, relatively heavy, cylindrical spines or beams arise from the surface of the cortical shell, divide into irregular branches which anastomose to form an irregular but loose spongy structure; this terminates in a definite outer ellipsoidal shell which completely surrounds the test and has an irregular but smooth surface and a definite lattice consisting of unequal, irregular pores separated by very thin intervening bars. Most tests incomplete, with polar regions undeveloped, outer spongy structure in variable state of development around the cortical shell. Inner medullary shell spherical; outer one ellipsoidal, compressed in the polar axis of the shell; both with small, subequal, subpolygonal pores. Lattice of cortical shell with large, unequal, irregular pores, smaller in the equatorial region, becoming larger and elongated in the polar axis toward each pole, 5-8 on the half circumference. One specimen observed with a second outer shell (length 283 µm, breadth 178 µm).

Measurements: based on 17 specimens from stations 46, 56, 81, 92, 106, 133, 184, and 191: length of outer shell (polar axis) 185-295 µm, of cortical shell 113-228 µm (some specimens incomplete); maximum breadth of outer shell 123-160 µm, of cortical shell 68-96 µm; breadth of equatorial region of cortical shell 54-77 µm; diameter of inner medullary shell 14-21 µm; equatorial diameter of outer medullary shell 34-41 µm, polar diameter 31-37 µm.

Remarks: There is no doubt that this species is the same as the form illustrated by Hollande and Enjumet (1960, Pl. 63) and placed by them within the genus Spongoliva Haeckel. Only the outline of the figure-8 shaped cortical shell is shown, the remainder of this shell having been broken away. Popofsky's illustration of S. ellipsoides (1912, text fig. 28) is an incomplete drawing. It differs from the Gulf specimens in what appears to be a very dense, spongy meshwork at the limit of the outer shell. Popofsky shows the two medullary shells and a portion of the cortical shell, but the details of the spongy structure between the latter and the outer shell are not illustrated. His description, however, agrees fairly well with that of the Gulf species, but because his illustration lacks details, identification is not positive. Because the cortical shell of this species has an equatorial stricture it was placed within the family Cyphantellidae. Campbell (1954, p. D74) places Spongoliva within the family Sponguridae because Haeckel (1887, p. 351) did this originally. Haeckel, however, did not illustrate any of the species belonging to this genus. Subsequent illustrations (Popofsky, Hollande and Enjumet) and study of the Gulf species of this genus establish the affinity of at least these forms with the family Cyphantellidae. The affinity of Haeckel s species of Spongoliva must await study of his type material.

Distribution: This species is cosmopolitan but rare throughout the Gulf, occurring as far north as station 206.It is absent at stations 27, 95, 99, 130, 194, 203, 208, and 214. Its frequency does not undergo any significant changes; therefore its relationship to areas of upwelling is unknown. Its occurrence in the northern Gulf suggests its tolerance for waters of higher than average salinity and temperature. Popofsky (1912, p. 117) reported Spongo1iva ellipsoides from the equatorial part of the central Atlantic. Hollande and Enjumet (1960) did not discuss Spongoliva sp. but only illustrated it. It is presumably from the Bay of Algiers. The lack of positive identification of the Gulf species makes analysis of its world-wide distribution impossible. It is at least a tropical species. \ From: Benson. 1966, p. 190-193; pl. 8, figs. 6-7:Spongoliva cf. ellipsoides Popofsky ?Spongoliva ellipsoides Popofsky, 1912, Deutsche Sdpolar-Exped., vol. 13, p. 117, text fig. 28. Spongoliva sp. Hollande and Enjumet, 1960, Paris, Mus. Nat. d Hist. Natur., Archives, vol. 7, ser. 7, Pl. 63.


Biogeography and Palaeobiology

Biostratigraphic distribution

Geological Range:
Last occurrence (top): Extant. Data source: Lazarus et al. 2015 - "R age group"
First occurrence (base): within Quaternary Period (0.00-2.59Ma, base in Gelasian stage). Data source: Lazarus et al. 2015 - "R age group"

Plot of occurrence data:

References:

Benson, R. N. (1966). Recent Radiolaria from the Gulf of California. Thesis, Minnesota University. 1-577. gs

Benson, R. N. (1983). Quaternary radiolarians from the Mouth of the Gulf of California, Deep Sea Drilling Project Leg 65. Initial Reports of the Deep Sea Drilling Project. 65: 491-523. gs

Hollande, A. & Enjumet, M. (1960). Cytologie, evolution et systematique des Sphaeroides (Radiolaires). Archives du Museum National d'Histoire Naturelle, Paris. 7: 1-134. gs

Kling, S. A. (1977). Local and regional imprints on radiolarian assemblages from California coastal basin sediments. Marine Micropaleontology. 2(2): 207-221. gs

Nigrini, C. A. (1968). Radiolaria from eastern tropical Pacific sediments. Micropaleontology. 14(1): 51-63. gs

Popofsky, A (1912). Die Sphaerellarien des Warmwassergebietes. Deutsche Sudpolar-Expedition 1901-1903. 13(5): 73-159. gs

Sanfilippo, A. & Riedel, W. R. (1970). Post-Eocene "closed" theoperid radiolarians. Micropaleontology. 16(4): 446-462. gs


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Cypassis irregularis compiled by the radiolaria@mikrotax project team viewed: 15-9-2024

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