TREMATODISCOIDEA Haeckel, 1862
Superfamily TREMATODISCOIDEA Haeckel, 1862 sensu Suzuki emend. herein Trematodiscida Haeckel, 1862: 240, 485, 491 [as a tribe]; 1882: 459 [as a tribe]; 1887: 484, 491 [as a subfamily]. Trematodiscea – Zittel 1876-1880: 124 [rank unknown]. Trematodiscacea – Kozur & Mostler 1978: 125-126 [as a sup...
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Biodiversity Taxonomy Suzuki, Noritoshi Caulet, Jean-Pierre Dumitrica, Paulian TREMATODISCOIDEA Haeckel, 1862 |
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Biodiversity Taxonomy |
description |
Superfamily TREMATODISCOIDEA Haeckel, 1862 sensu Suzuki emend. herein Trematodiscida Haeckel, 1862: 240, 485, 491 [as a tribe]; 1882: 459 [as a tribe]; 1887: 484, 491 [as a subfamily]. Trematodiscea – Zittel 1876-1880: 124 [rank unknown]. Trematodiscacea – Kozur & Mostler 1978: 125-126 [as a superfamily]; 1990: 217-218 [as a superfamily]. Stylodictyoidea – Suzuki in Matsuzaki et al. 2015: 25. DIAGNOSIS. — Flat or convex lens shape with circular outline. Central structure consisting of many discontinuous rings connected by short radial beams or a microsphere with four decussated primary radial spines. REMARKS This superfamily includes only the family Trematodiscidae. Homeomorphy between Spongodiscoidea and Trematodiscoidea was first detected by a molecular phylogenetic study (Ishitani et al. 2012). The group of Schizodiscus , Spongobrachiopyle , Flustrella and Stylodictya was analyzed by molecular studies and further subdivided into two subgroups, namely a subgroup of Schizodiscus and Spongobrachiopyle (originally Spongopyle ) as Clade L2, and a subgroup of Flustrella and Stylodictya as Clade J (Sandin et al. 2021). The former group morphologically corresponds to the Spongopylidae and the latter to the Trematodiscidae. The general morphology of Spongopylidae closely resembles that of Spongodiscidae (Spongodiscoidea). It is estimated that identifying the classical Spongodiscidae family, used to include the Spongodiscoidea and Trematodiscoidea is difficult. However, this is largely due to an insufficient observation of many taxonomical markers. In particular, the difference in the disk’s lateral profiles is almost completely ignored. This complicates the taxonomic process. The structural difference between the “empty” space and “thin” structural parts must be carefully recognized upon dark to bright appearance of disc parts under a light microscope. An “empty” space can be bright irrespective of disk thickness. Meanwhile, a “thin” place may be bright based on its relationship to the disk thickness. It is sometimes presumptively concluded, to a fault, that differences in brightness may be caused by supplemental gowns on both faces of the disk. If this is observed, shallow depth focused photos are essential. Many previous papers repeatedly noticed the different lateral profiles of the classical Spongodiscidae (Müller 1859b: pl. 1, figs 8, 9; Haeckel 1862: pl. 27, figs 3, 5; pl. 28, figs 6, 9; 1887: pl. 42, figs 5, 6, 9, 10; Hertwig 1879: pl. 6, 7a, 7b, 8a; JØrgensen 1905: pl. 10, figs 39a, 40b, 41c; Riedel 1953: pl. 84, fig. 6; Kozlova 1960; Krasheninnikov 1960: 3, figs 5-7; Moksyakova 1961: pl. 1, fig. 11; 1972: pls 1-9; Kozlova & Gorbovetz 1966: pl. 14, figs 1-2; Petrushevskaya 1967: pl. 19, fig. 2; pl. 20, figs 2, 4; pl. 21, figs 3, 6; pl. 22, fig. 7; pl. 25, figs 3, 5; 1975: pl. 34, figs 1, 2; pl. 36, figs 3, 5; pl. 38, figs 1, 3, 7; pl. 39, figs 2; pl. 40, fig. 4, Barwicz-Piskorz 1978: pl. 5, figs 1-3; Zaynutdinov 1978: pl. 7, figs 1-3; pl. 12, fig. 7; Petrushevskaya & Kozlova 1979: figs 431, 432, 434, 438, 441; Nakaseko & Nishimura 1982: pl. 29, fig. 1c; pl. 31, figs 2b, 3a; pl. 32, fig. 3; pl. 34, fig. 2a; pl. 37, fig. 1b; pl. 40, fig. 6b; pl. 41, fig. 2a; pl. 42, figs 1, 4; pl. 43, figs 1b, 2a; Poluzzi 1982: pl. 20, fig. 17; O’Connor 1997b: text-fig. 2; pl. 4, figs 4, 6; Ogane & Suzuki 2006: pl. 1, figs 6, 9; pl. 2, fig. 2; Onodera et al. 2011: pl. 6, fig. 6). The difference of lateral profile in classic Spongodiscidae is directly related to the fundamental rule of skeletal growth patterns and construction scheme of a biological design. Regardless of the repeated rediscovery of this profile difference, systematic examination regarding these differences have been under-appreciated and the majority of studies identify a spongy disk without radial spines as Spongodiscus , a spongy disk without radial spines as Spongotrochus , a spongy disk with a pylome as Spongopyle , a concentric disk without radial spines as Porodiscus , and/or a concentric disk with radial spines as Stylodictya . Everyone empirically knows that this simple scheme does not work for any real specimens. This is easily recognizable if we look at names such as Spongodiscus spp., Spongodiscidae gen. et sp. indet. and other ambiguous indications for classic Spongodiscidae. Nevertheless, the validity of described genera such as Schizodiscus , Spongobrachiopyle, Spongospira and Staurospira was rejected without any further careful anatomical considerations. It is noteworthy that some studies still strongly adhere to this flawed principle, despite the clear rejection of this treatment by the molecular phylogeny (Ishitani et al. 2012). To understand these groups, shallow focus photos like pl. 13, fig. 3a of Suzuki et al. (2009d) are essential. Otherwise, progress is stifled. : Published as part of Suzuki, Noritoshi, Caulet, Jean-Pierre & Dumitrica, Paulian, 2021, A new integrated morpho- and molecular systematic classification of Cenozoic radiolarians (Class Polycystinea) - suprageneric taxonomy and logical nomenclatorial acts, pp. 405-573 in Geodiversitas 43 (15) on page 433, DOI: 10.5252/geodiversitas2021v43a15, http://zenodo.org/record/5101757 : {"references": ["HAECKEL E. 1862. - Die Radiolarien (Rhizopoda Radiaria). Eine Monographie. Reimer, Berlin, 572 p. https: // doi. org / 10.5962 / bhl. title. 10155", "KOZUR H. & MOSTLER H. 1978. - Beitrage zur Erforschung der mesozoischen Radiolarien Teil II: Oberfamilie Trematodiscacea HAECKEL 1862 emend. und Beschreibung ihrer triassischen Vertreter. Geologisch Palaontologische Mitteilungen Innsbruck 8: 123 - 182.", "MATSUZAKI K. M., SUZUKI N. & NISHI H. 2015. - Middle to Upper Pleistocene Polycystine Radiolarians from Hole 902 - C 9001 C, Northwestern Pacific. Paleontological Research 19 (supplement 1): 1 - 77. https: // doi. org / 10.2517 / 2015 PR 003", "ISHITANI Y., UJIIE Y., DE VARGAS C., NOT F. & TAKAHASHI K. 2012. - Phylogenetic Relationships and Evolutionary Patterns of the Order Collodaria (Radiolaria). PLoS ONE 7 (5): e 35775. https: // doi. org / 10.1371 / journal. pone. 0035775", "SANDIN M. M., BIARD T., ROMAC S., O'DOGHERTY L., SUZUKI N. & NOT F. 2021. - A morpho-molecular perspective on the diversity and evolution of Spumellaria (Radiolaria). Protist 172: https: // doi. org / 10.1016 / j. protis. 2021.125806", "MULLER J. 1859 b. - Einige neue bei St. Tropez am Mittelmeer beobachtete Polycystinen und Acanthometren. Monatsberichte der Koniglich Preussischen Akademie derWissenschaften zu Berlin (1858): 154 - 155. https: // www. biodiversitylibrary. org / page / 11071854", "HERTWIG R. 1879. - Der Organismus der Radiolarien. G. Fischer, Jena, Germany, iv + 149 p. https: // archive. org / details / denkschriftender 02 medi / page / 126 / mode / 2 up", "JORGENSEN E. 1905. - The protist plankton and the diatoms in bottom samples, in NORDGAARD O. (ed.), Hydrographical and Biological Investigation in Norwegian Fiords. Bergens Museums skrifter, Bergen, 1905: 49 - 151. https: // www. biodiversitylibrary. org / page / 7110326", "RIEDEL W. R. 1953. - Mesozoic and late Tertiary Radiolaria of Rotti. Journal of Paleontology 27 (6): 805 - 813. https: // www. jstor. org / stable / 1300029", "KOZLOVA G. E. 1960. - Radiolarians of the Middle and Upper Miocene of Northern Sakhalin. Proceedings of the All Union Petroleum Scientific Research Institute for Geological Survey (VNIGRI) 153: 307 - 325. [in Russian]", "KRASHENINNIKOV V. A. 1960. - Some radiolarians of the Lower and Middle Eocene of the Westen Caucasus. Mineralogicko-Geologicka i Okhrana Nedr SSSR Vsesoyuznogo Nauchno-Issledovatelskogo Geologorazved Neftyanogo Instituta 16: 271 - 308. [in Russian]", "MOKSYAKOVA A. M. 1961. - The radiolarians of the Kumsk horizon of the Upper Eocene in western Turkmenistan. Trudy VNIGNI 44: 231 - 246. [in Russian]", "KOZLOVA G. E. & GORBOVETZ A. N. 1966. - Radiolarians of the Upper Cretaceous and Upper Eocene deposits of the West Siberian Lowland. Proceedings of the All Union Petroleum Scientific Research Institute for Geological Survey (VNIGRI) 248: 1 - 159. [In Russian]", "PETRUSHEVSKAYA M. G. 1967. - Antarctic Spumelline and Nasselline radiolarians, Issledovaniya Fauny Morei, Resultaty Biologicheskikh Issledovanii Sovetskoi Antarkticheskoi Ekspeditsii 1955 - 1958. Vol. 4. Zoologicheskii Institut Academiya Nauk SSSR: 5 - 186. [in Russian]", "ZAYNUTDINOV A. A. 1978. - Vozrastinyie komleksyi ploskikh diskoidey iz eotsenovyikh otlozheniy nekotoryikh rayonov Sredney Azii. Drevnie Radiolyarii Sredney Azii 5: 68 - 129. [in Russian]", "PETRUSHEVSKAYA M. G. & KOZLOVA G. E. 1979. - Description of the radiolarian genera and species, in STERLKOV A. A. & M. G. P. (eds), The history of the microplankton of the Norwegian Sea (on the Deep Sea Drilling materials). Vol. 23. Nauka Academy of Sciences of the USSR, Zoological Institute, Leningrad, USSR: 86 - 157. [in Russian]", "NAKASEKO K. & NISHIMURA A. 1982. - Radiolaria from the bottom sediments of the Bellingshausen Basin in the Antarctic Sea, Report of the Technology Research Center, Japan National Oil Corporation, 91 - 244 p.", "POLUZZI A. 1982. - I radiolari quaternari di un ambiente idrotermale del Mar Tirreno. Memorie della Societa Italiana di Scienze Naturali e del Museo Civico di Storia Naturale di Milano 23 (2): 48 - 72.", "O'CONNOR B. 1997 b. - Lower Miocene Radiolaria from the Kopua Point, Kaipara Harbour, New Zealand. Micropaleontology 43 (2): 101 - 128. https: // doi. org / 10.2307 / 1485777", "OGANE K. & SUZUKI N. 2006. - Morphological terms describing discoidal radiolarians. Revue de Micropaleontologie 49 (2): 97 - 104. https: // doi. org / 10.1016 / j. revmic. 2006.03.001", "ONODERA J., OKAZAKI Y., TAKAHASHI K., OKAMURA K. & MURAYAMA M. 2011. - Distribution of polycystine Radiolaria, Phaeodaria and Acantharia in the Kuroshio Current off Shikoku Island and Tosa Bay during Cruise KT 07 - 19 in August 2007. Memoirs of the Faculty of Science, Kyushu University, Series D, Earth and Planetary Sciences 32 (3): 39 - 61. https: // catalog. lib. kyushu-u. ac. jp / opac _ download _ md / 19196 / p 039. pdf", "SUZUKI N., OGANE K. & CHIBA K. 2009 d. - Middle to Late Eocene polycystine radiolarians from the Site 1172, Leg 189, Southwest Pacific. News of Osaka Micropaleontologists, special Volume 14: 239 - 296."]} |
format |
Text |
author |
Suzuki, Noritoshi Caulet, Jean-Pierre Dumitrica, Paulian |
author_facet |
Suzuki, Noritoshi Caulet, Jean-Pierre Dumitrica, Paulian |
author_sort |
Suzuki, Noritoshi |
title |
TREMATODISCOIDEA Haeckel, 1862 |
title_short |
TREMATODISCOIDEA Haeckel, 1862 |
title_full |
TREMATODISCOIDEA Haeckel, 1862 |
title_fullStr |
TREMATODISCOIDEA Haeckel, 1862 |
title_full_unstemmed |
TREMATODISCOIDEA Haeckel, 1862 |
title_sort |
trematodiscoidea haeckel, 1862 |
publisher |
Zenodo |
publishDate |
2021 |
url |
https://dx.doi.org/10.5281/zenodo.5106720 https://zenodo.org/record/5106720 |
long_lat |
ENVELOPE(-86.200,-86.200,-77.800,-77.800) ENVELOPE(-58.383,-58.383,-62.067,-62.067) ENVELOPE(51.083,51.083,-66.633,-66.633) ENVELOPE(-152.500,-152.500,-70.000,-70.000) |
geographic |
Antarctic The Antarctic Norwegian Sea Pacific New Zealand Bergen Reimer O'Connor Kozlova Bellingshausen Basin |
geographic_facet |
Antarctic The Antarctic Norwegian Sea Pacific New Zealand Bergen Reimer O'Connor Kozlova Bellingshausen Basin |
genre |
Antarc* Antarctic Norwegian Sea Sakhalin |
genre_facet |
Antarc* Antarctic Norwegian Sea Sakhalin |
op_relation |
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https://doi.org/10.5281/zenodo.5106720 https://doi.org/10.5252/geodiversitas2021v43a15 https://doi.org/10.5281/zenodo.5106719 |
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ftdatacite:10.5281/zenodo.5106720 2023-05-15T13:36:10+02:00 TREMATODISCOIDEA Haeckel, 1862 Suzuki, Noritoshi Caulet, Jean-Pierre Dumitrica, Paulian 2021 https://dx.doi.org/10.5281/zenodo.5106720 https://zenodo.org/record/5106720 unknown Zenodo http://zenodo.org/record/5101757 http://publication.plazi.org/id/FFB4A20BFF94FE350535FFD1FFF94F6C http://zoobank.org/urn:lsid:zoobank.org:pub:DC259A19-9B35-4B33-AD9F-44F4E1DA9983 https://zenodo.org/communities/biosyslit https://dx.doi.org/10.5252/geodiversitas2021v43a15 http://zenodo.org/record/5101757 http://publication.plazi.org/id/FFB4A20BFF94FE350535FFD1FFF94F6C http://zoobank.org/urn:lsid:zoobank.org:pub:DC259A19-9B35-4B33-AD9F-44F4E1DA9983 https://dx.doi.org/10.5281/zenodo.5106719 https://zenodo.org/communities/biosyslit Open Access Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 info:eu-repo/semantics/openAccess CC0 Biodiversity Taxonomy Taxonomic treatment article-journal Text ScholarlyArticle 2021 ftdatacite https://doi.org/10.5281/zenodo.5106720 https://doi.org/10.5252/geodiversitas2021v43a15 https://doi.org/10.5281/zenodo.5106719 2022-02-08T12:55:18Z Superfamily TREMATODISCOIDEA Haeckel, 1862 sensu Suzuki emend. herein Trematodiscida Haeckel, 1862: 240, 485, 491 [as a tribe]; 1882: 459 [as a tribe]; 1887: 484, 491 [as a subfamily]. Trematodiscea – Zittel 1876-1880: 124 [rank unknown]. Trematodiscacea – Kozur & Mostler 1978: 125-126 [as a superfamily]; 1990: 217-218 [as a superfamily]. Stylodictyoidea – Suzuki in Matsuzaki et al. 2015: 25. DIAGNOSIS. — Flat or convex lens shape with circular outline. Central structure consisting of many discontinuous rings connected by short radial beams or a microsphere with four decussated primary radial spines. REMARKS This superfamily includes only the family Trematodiscidae. Homeomorphy between Spongodiscoidea and Trematodiscoidea was first detected by a molecular phylogenetic study (Ishitani et al. 2012). The group of Schizodiscus , Spongobrachiopyle , Flustrella and Stylodictya was analyzed by molecular studies and further subdivided into two subgroups, namely a subgroup of Schizodiscus and Spongobrachiopyle (originally Spongopyle ) as Clade L2, and a subgroup of Flustrella and Stylodictya as Clade J (Sandin et al. 2021). The former group morphologically corresponds to the Spongopylidae and the latter to the Trematodiscidae. The general morphology of Spongopylidae closely resembles that of Spongodiscidae (Spongodiscoidea). It is estimated that identifying the classical Spongodiscidae family, used to include the Spongodiscoidea and Trematodiscoidea is difficult. However, this is largely due to an insufficient observation of many taxonomical markers. In particular, the difference in the disk’s lateral profiles is almost completely ignored. This complicates the taxonomic process. The structural difference between the “empty” space and “thin” structural parts must be carefully recognized upon dark to bright appearance of disc parts under a light microscope. An “empty” space can be bright irrespective of disk thickness. Meanwhile, a “thin” place may be bright based on its relationship to the disk thickness. It is sometimes presumptively concluded, to a fault, that differences in brightness may be caused by supplemental gowns on both faces of the disk. If this is observed, shallow depth focused photos are essential. Many previous papers repeatedly noticed the different lateral profiles of the classical Spongodiscidae (Müller 1859b: pl. 1, figs 8, 9; Haeckel 1862: pl. 27, figs 3, 5; pl. 28, figs 6, 9; 1887: pl. 42, figs 5, 6, 9, 10; Hertwig 1879: pl. 6, 7a, 7b, 8a; JØrgensen 1905: pl. 10, figs 39a, 40b, 41c; Riedel 1953: pl. 84, fig. 6; Kozlova 1960; Krasheninnikov 1960: 3, figs 5-7; Moksyakova 1961: pl. 1, fig. 11; 1972: pls 1-9; Kozlova & Gorbovetz 1966: pl. 14, figs 1-2; Petrushevskaya 1967: pl. 19, fig. 2; pl. 20, figs 2, 4; pl. 21, figs 3, 6; pl. 22, fig. 7; pl. 25, figs 3, 5; 1975: pl. 34, figs 1, 2; pl. 36, figs 3, 5; pl. 38, figs 1, 3, 7; pl. 39, figs 2; pl. 40, fig. 4, Barwicz-Piskorz 1978: pl. 5, figs 1-3; Zaynutdinov 1978: pl. 7, figs 1-3; pl. 12, fig. 7; Petrushevskaya & Kozlova 1979: figs 431, 432, 434, 438, 441; Nakaseko & Nishimura 1982: pl. 29, fig. 1c; pl. 31, figs 2b, 3a; pl. 32, fig. 3; pl. 34, fig. 2a; pl. 37, fig. 1b; pl. 40, fig. 6b; pl. 41, fig. 2a; pl. 42, figs 1, 4; pl. 43, figs 1b, 2a; Poluzzi 1982: pl. 20, fig. 17; O’Connor 1997b: text-fig. 2; pl. 4, figs 4, 6; Ogane & Suzuki 2006: pl. 1, figs 6, 9; pl. 2, fig. 2; Onodera et al. 2011: pl. 6, fig. 6). The difference of lateral profile in classic Spongodiscidae is directly related to the fundamental rule of skeletal growth patterns and construction scheme of a biological design. Regardless of the repeated rediscovery of this profile difference, systematic examination regarding these differences have been under-appreciated and the majority of studies identify a spongy disk without radial spines as Spongodiscus , a spongy disk without radial spines as Spongotrochus , a spongy disk with a pylome as Spongopyle , a concentric disk without radial spines as Porodiscus , and/or a concentric disk with radial spines as Stylodictya . Everyone empirically knows that this simple scheme does not work for any real specimens. This is easily recognizable if we look at names such as Spongodiscus spp., Spongodiscidae gen. et sp. indet. and other ambiguous indications for classic Spongodiscidae. Nevertheless, the validity of described genera such as Schizodiscus , Spongobrachiopyle, Spongospira and Staurospira was rejected without any further careful anatomical considerations. It is noteworthy that some studies still strongly adhere to this flawed principle, despite the clear rejection of this treatment by the molecular phylogeny (Ishitani et al. 2012). To understand these groups, shallow focus photos like pl. 13, fig. 3a of Suzuki et al. (2009d) are essential. Otherwise, progress is stifled. : Published as part of Suzuki, Noritoshi, Caulet, Jean-Pierre & Dumitrica, Paulian, 2021, A new integrated morpho- and molecular systematic classification of Cenozoic radiolarians (Class Polycystinea) - suprageneric taxonomy and logical nomenclatorial acts, pp. 405-573 in Geodiversitas 43 (15) on page 433, DOI: 10.5252/geodiversitas2021v43a15, http://zenodo.org/record/5101757 : {"references": ["HAECKEL E. 1862. - Die Radiolarien (Rhizopoda Radiaria). Eine Monographie. Reimer, Berlin, 572 p. https: // doi. org / 10.5962 / bhl. title. 10155", "KOZUR H. & MOSTLER H. 1978. - Beitrage zur Erforschung der mesozoischen Radiolarien Teil II: Oberfamilie Trematodiscacea HAECKEL 1862 emend. und Beschreibung ihrer triassischen Vertreter. Geologisch Palaontologische Mitteilungen Innsbruck 8: 123 - 182.", "MATSUZAKI K. M., SUZUKI N. & NISHI H. 2015. - Middle to Upper Pleistocene Polycystine Radiolarians from Hole 902 - C 9001 C, Northwestern Pacific. Paleontological Research 19 (supplement 1): 1 - 77. https: // doi. org / 10.2517 / 2015 PR 003", "ISHITANI Y., UJIIE Y., DE VARGAS C., NOT F. & TAKAHASHI K. 2012. - Phylogenetic Relationships and Evolutionary Patterns of the Order Collodaria (Radiolaria). PLoS ONE 7 (5): e 35775. https: // doi. org / 10.1371 / journal. pone. 0035775", "SANDIN M. M., BIARD T., ROMAC S., O'DOGHERTY L., SUZUKI N. & NOT F. 2021. - A morpho-molecular perspective on the diversity and evolution of Spumellaria (Radiolaria). Protist 172: https: // doi. org / 10.1016 / j. protis. 2021.125806", "MULLER J. 1859 b. - Einige neue bei St. Tropez am Mittelmeer beobachtete Polycystinen und Acanthometren. Monatsberichte der Koniglich Preussischen Akademie derWissenschaften zu Berlin (1858): 154 - 155. https: // www. biodiversitylibrary. org / page / 11071854", "HERTWIG R. 1879. - Der Organismus der Radiolarien. G. Fischer, Jena, Germany, iv + 149 p. https: // archive. org / details / denkschriftender 02 medi / page / 126 / mode / 2 up", "JORGENSEN E. 1905. - The protist plankton and the diatoms in bottom samples, in NORDGAARD O. (ed.), Hydrographical and Biological Investigation in Norwegian Fiords. Bergens Museums skrifter, Bergen, 1905: 49 - 151. https: // www. biodiversitylibrary. org / page / 7110326", "RIEDEL W. R. 1953. - Mesozoic and late Tertiary Radiolaria of Rotti. Journal of Paleontology 27 (6): 805 - 813. https: // www. jstor. org / stable / 1300029", "KOZLOVA G. E. 1960. - Radiolarians of the Middle and Upper Miocene of Northern Sakhalin. Proceedings of the All Union Petroleum Scientific Research Institute for Geological Survey (VNIGRI) 153: 307 - 325. [in Russian]", "KRASHENINNIKOV V. A. 1960. - Some radiolarians of the Lower and Middle Eocene of the Westen Caucasus. Mineralogicko-Geologicka i Okhrana Nedr SSSR Vsesoyuznogo Nauchno-Issledovatelskogo Geologorazved Neftyanogo Instituta 16: 271 - 308. [in Russian]", "MOKSYAKOVA A. M. 1961. - The radiolarians of the Kumsk horizon of the Upper Eocene in western Turkmenistan. Trudy VNIGNI 44: 231 - 246. [in Russian]", "KOZLOVA G. E. & GORBOVETZ A. N. 1966. - Radiolarians of the Upper Cretaceous and Upper Eocene deposits of the West Siberian Lowland. Proceedings of the All Union Petroleum Scientific Research Institute for Geological Survey (VNIGRI) 248: 1 - 159. [In Russian]", "PETRUSHEVSKAYA M. G. 1967. - Antarctic Spumelline and Nasselline radiolarians, Issledovaniya Fauny Morei, Resultaty Biologicheskikh Issledovanii Sovetskoi Antarkticheskoi Ekspeditsii 1955 - 1958. Vol. 4. Zoologicheskii Institut Academiya Nauk SSSR: 5 - 186. [in Russian]", "ZAYNUTDINOV A. A. 1978. - Vozrastinyie komleksyi ploskikh diskoidey iz eotsenovyikh otlozheniy nekotoryikh rayonov Sredney Azii. Drevnie Radiolyarii Sredney Azii 5: 68 - 129. [in Russian]", "PETRUSHEVSKAYA M. G. & KOZLOVA G. E. 1979. - Description of the radiolarian genera and species, in STERLKOV A. A. & M. G. P. (eds), The history of the microplankton of the Norwegian Sea (on the Deep Sea Drilling materials). Vol. 23. Nauka Academy of Sciences of the USSR, Zoological Institute, Leningrad, USSR: 86 - 157. [in Russian]", "NAKASEKO K. & NISHIMURA A. 1982. - Radiolaria from the bottom sediments of the Bellingshausen Basin in the Antarctic Sea, Report of the Technology Research Center, Japan National Oil Corporation, 91 - 244 p.", "POLUZZI A. 1982. - I radiolari quaternari di un ambiente idrotermale del Mar Tirreno. Memorie della Societa Italiana di Scienze Naturali e del Museo Civico di Storia Naturale di Milano 23 (2): 48 - 72.", "O'CONNOR B. 1997 b. - Lower Miocene Radiolaria from the Kopua Point, Kaipara Harbour, New Zealand. Micropaleontology 43 (2): 101 - 128. https: // doi. org / 10.2307 / 1485777", "OGANE K. & SUZUKI N. 2006. - Morphological terms describing discoidal radiolarians. 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News of Osaka Micropaleontologists, special Volume 14: 239 - 296."]} Text Antarc* Antarctic Norwegian Sea Sakhalin DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic Norwegian Sea Pacific New Zealand Bergen Reimer ENVELOPE(-86.200,-86.200,-77.800,-77.800) O'Connor ENVELOPE(-58.383,-58.383,-62.067,-62.067) Kozlova ENVELOPE(51.083,51.083,-66.633,-66.633) Bellingshausen Basin ENVELOPE(-152.500,-152.500,-70.000,-70.000) |