radiolaria - rads_cenozoic - Acrobotrys teralans radiolaria - rads_cenozoic - Acrobotrys teralans

Acrobotrys teralans


Classification: rads_cenozoic -> Cannobotryidae -> Cannobotryidae inc sed -> Acrobotrys -> Acrobotrys teralans
Sister taxa: A. chelinobotrys, A. cribosa, A. disolenia, A. sphaerothorax, A. teralans, A. tessarolobon, A. tritubus, A. sp.

Taxonomy

Citation: Acrobotrys teralans Renz 1976
Taxonomic rank: species
Basionym: Acrobotrys teralans
Synonyms:
1966 Acrobotrys cf. disolenia - Benson p. 339-341; pl. 23, figs. 13-14; text-fig. 21
1971 Gen. et sp. indet. - Riedel and Sanfilippo pl. 1J, figs. 17-18
1974 Acrobotrys sp. - Renz p. 787; pl. 18, fig. 9
1976 Acrobotrys teralans - Renz p. 152-153; pl. 7, fig. 10 (not 8)
1983 Acrobotrys sp. cf. A. disolenia - Benson p. 499; pl. 9, figs. 6-7
1987 Acrobotrys sp. B - Bjørklund and de Ruiter fig. 5, nos. 12-13
1990 ? Ceratobotrys riedeli - Nishimura p. 169-170; figs. 37-1, -2, -3
1991 Acrobotrys teralans - Takahashi p. 133; pl. 45, figs. 18-19
1995 ?Botryopyle riedeli - van de Paverd p. 257; pl. 77, figs. 10-12
1998 Acrobotrys spp. - Boltovskoy fig. 15.171

From Suzuki Paleotax db:

1976 Acrobotrys teralans n. sp. Renz p. 152-153, pl. 7, fig. 8
1984 Acrobotrys teralans Renz Nishimura & Yamauchi p. 66, pl. 41, fig. 2
1991 Acrobotrys teralans Renz Takahashi p. 133, pl. 45, figs. 18, 19

Catalog entries: Acrobotrys teralans

Original description: Description: Cephalis trilobate with a single straight cylindrical tube on the post- cephalic lobe and a strong apical spine fused to the wall of the antecephalic lobe and protruding from its apex. The cephalic and postcephalic lobes ovate but unequal in size, being approximately 1/2 as large as the helmet-shaped antecephalic lobe. Thorax ovate, about 1 1/2 times as long as the cephalis. Three small triangular, latticed wings extend from the base of the collar stricture. Latticework delicate with very small and numerous pores.

Dimensions: (10 specimens) length: 60-80 µ, Md 76; breadth: 36-52 µ, Md 42.

Type locality: 11°N, 155°W, plankton, 0-25 m.

Remarks: This species is similar to Acrobotrys sp. C described by Petrushevskaya (1965) except that it lacks an aperature or tube at the tip of the antecephalic lobe, and the additional tube extending from the dorsal spine. In all specimens the apical spine extends outside the antecephalic lobe and 3 small wings extend from the collar stricture. The specific name teralans is an anagram of the word sternala meaning toward the rear.

Description


Published descriptions


Benson 1966 - Acrobotrys teralans

Smooth cephalis with two lobes separated by a constriction coincident with a thin rib--a smaller, rounded, ventral lobe, and a larger dorsal lobe.A smooth, subcylindrical thorax with slightly constricted mouth separated from both cephalic lobes by a constriction coincident with a thin rib.A ventral latticed tube present in all specimens on the upper ventral face of the thorax. In a few specimens one or two additional latticed tubes present, one coincident with the short apical spine, the other ascending dorsally in the sagittal plane from the upper surface of the dorsal cephalic lobe. Pores of cephalic lobes and thorax similar, circular to subcircular, small, subequal, but irregularly arranged. Internal structure shown in text-fig. 21B.The ribs outlining the ventral lobe correspond to the apical-lateral arches and the ventral arch. The median bar short, underlies the ventral lobe. Apical bar an internal columella which extends as a rib along the ventral edge of the dorsal lobe and projects as a short, apical spine. Vertical bar terminates near the proximal portion of the ventral tube. The dorsal and primary lateral bars pierce the thoracic wall and extend as short spines that are joined by a lattice to the wall of the thorax. Secondary lateral bars terminate at the constriction separating the dorsal cephaliclobe from the thorax.

Measurements: based on 5 specimens from stations 191 and 192: length of dorsal lobe 37-50 m, of ventral lobe (measured from median bar) 21-25 µm, of thorax 37-58 µm; breadth of dorsal lobe 22-30 µm, of ventral lobe 18-20 µm, of thorax 53-59 µm, length of ventral tube 6-9 µm, diameter 6-9 µm; length of dorsal and primary lateral spines 12-33 µm.

Remarks: This species is rare in the Gulf sediments; therefore, its complete range of variation was not determined. Because the number of latticed tubes is variable within this species, this character should not be used in defining the species. Whether or not the thoracic mouth is closed by a lattice could not be determined from the few specimens studied. None of the species of Acrobotrys illustrated by Haeckel conform to the Gulf species in shape and size of cephalic lobes. In number of tubes A. diso1enia Haeckel (1887, p. 1114, Pl. 96, fig. 10) is similar to the Gulf species; however, Haeckel indicates a third lobe from which originates the ventral tube, but in the Gulf specimens the internal primary lateral bars appear to separate a third lobe but actually do not. Haeckel may have misinterpreted the third lobe. Unless Haeckel's type material can be studied, identification of the Gulf species as A. disolenia is not positive.

Distribution: This species is rare in the Gulf but occurs as far north as stations 191 and 192.Besides these stations it is present at stations 56, 60, 93, 106, 115, 136, and 151.Its presence in the northern half of the Gulf may be related to upwelling there. Its very rare occurrence and spotty distribution, however, indicates its lack of great affinity for Gulf waters. Haeckel reported Acrobotrys disolenia from the central Pacific at Challengerstations 265-274.Because identification of the Gulf species is not positive, analysis of its world-wide distribution cannot be made. \ From: Benson, 1966, p. 339-341; pl. 23, figs. 13-14; text-fig. 21:Acrobotrys cf. disolenia Haeckel?Acrobotrys disolenia Haeckel, 1887, Challenger Rept., Zool., vol. 18, p. 1114, Pl. 96, fig. 10.


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

Bjørklund, K. R. & de Ruiter, R. (1987). Radiolarian preservation in eastern Mediterranean anoxic sediments. Marine Geology. 75: 271-281. gs

Boltovskoy, D. (1998). Classification and distribution of south Atlantic recent polycystine Radiolaria. Palaeontologia Electronica. (2): -. gs

Nishimura, H. (1990). Taxonomic study on Cenozoic Nassellaria (Radiolaria). Science Reports of the Institute of Geosciences, University of Tsukuba. 11: 69-172. gs

Renz, G. W. (1974). Radiolaria from Leg 27 of the DSDP. Initial Reports of the Deep Sea Drilling Project. 27: 769-841. gs O

Renz, G. W. (1976). The distribution and ecology of Radiolaria in the central Pacific: plankton and surface sediments. Bulletin of the Scripps Institution of Oceanography. 22: 1-267. gs

Riedel, W. R. & Sanfilippo, A. (1971). Cenozoic Radiolaria from the western tropical Pacific, Leg 7. Initial Reports of the Deep Sea Drilling Project. 7: 1529-1666. gs

Takahashi, K. (1991). Radiolaria: Flux, ecology, and Taxonomy in the Pacific and Atlantic. Ocean Biocoenosis Series. 3: 1-301. gs

van de Paverd, P. J. (1995). Recent Polycystine Radiolaria from the Snellius-II Expedition. Thesis, Free University Amsterdam. 1-351. gs


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Acrobotrys teralans compiled by the radiolaria@mikrotax project team viewed: 19-11-2025

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