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Relevant bibliographies by topics / Ostracodes

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Journal articles

Academic literature on the topic 'Ostracodes'

Author: Grafiati

Published: 4 June 2021

Last updated: 22 June 2024

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Journal articles on the topic "Ostracodes"

1

CHATTERJEE, TAPAS, IGOR DOVGAL, ROSAURA MAYÉN-ESTRADA, and GREGORIO FERNANDEZ-LEBORANS. "A checklist of ciliates (Ciliophora) inhabiting on ostracods (Crustacea, Ostracoda)." Zootaxa 4763, no. 1 (2020): 17–30. http://dx.doi.org/10.11646/zootaxa.4763.1.2.

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A compilation of the ciliated species found on freshwater and marine ostracods as epibiont or parasite (endobiont) has been carried out based on published records. The checklist includes the taxonomic position of each species of epibiontic and endobiontic ciliate, the species of basibiont ostracodes, the geographic zones and the bibliographic references where they were recorded. Altogether 7 suctorian, 29 peritrich, one apostome and one scuticociliatid species were listed. Two of recorded suctorian species are possible specific to marine ostracodes, whereas only one, Tokophrya sibirica to fres

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2

Holmes, Jonathan A. "Future Trends and Goals in Ostracode Research." Paleontological Society Papers 9 (November 2003): 275–90. http://dx.doi.org/10.1017/s1089332600002254.

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In recent decades, research on ostracodes has grown dramatically. While many aspects of the group have been investigated, this review focuses on the paleoenvironmental applications of ostracodes from marine and nonmarine environments. It is argued that while ostracodes have great potential as paleoenvironmental tools, much of that potential has not yet been fully realized because of our imperfect understanding of ostracode biology, taxonomy, systematics and ecology. Future developments will be sure to result from additional studies in these areas, and will also be effected by exchange of ideas

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3

Friedman, Gerald M., and Robert F. Lundin. "Freshwater ostracodes from upper Middle Devonian fluvial facies, Catskill Mountains, New York." Journal of Paleontology 72, no. 3 (1998): 485–90. http://dx.doi.org/10.1017/s0022336000024240.

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Leperditiocope ostracodes identified asSollenella? sp. were discovered in the Gilboa Formation (upper Givetian, uppermost Middle Devonian) within the continental Catskill Magnafacies of New York State. The deposits in which the ostracodes were found are meandering-fluvial facies that were part of a vast alluvial plain that sloped westward from the eroding Acadian Mountains. Hence, ostracodes colonized freshwater habitats earlier than heretofore thought. It has been widely accepted that, until now, the oldest known unequivocal occurrences of freshwater ostracodes are of Late Carboniferous age.

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4

Yasuhara, Moriaki, Yuanyuan Hong, Skye Yunshu Tian, et al. "Early Miocene marine ostracodes from southwestern India: implications for their biogeography and the closure of the Tethyan Seaway." Journal of Paleontology 94, S80 (2020): 1–36. http://dx.doi.org/10.1017/jpa.2020.44.

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AbstractTwenty-six genera and 34 species of early Miocene Indian shallow-marine ostracodes were examined for taxonomy and paleobiogeography. A new genus Paractinocythereis and new species Costa ponticulocarinata were described. Early Miocene Indian ostracode fauna shows strong affinity to Eocene–Miocene Eastern and Western Tethyan ostracode faunas and Miocene–Recent Indo-Pacific ostracode fauna, supporting the Hopping Hotspot Hypothesis that the Tethyan biodiversity hotspot has shifted eastward through Arabia to Indo-Australian Archipelago (IAA) together with concomitant biogeographic shifts o

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5

Ito, Emi, Patrick De Deckker, and Stephen M. Eggins. "Ostracodes and Their Shell Chemistry: Implications for Paleohydrologic and Paleoclimatologic Applications." Paleontological Society Papers 9 (November 2003): 119–52. http://dx.doi.org/10.1017/s1089332600002187.

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The shell chemistry of ostracodes is a useful indicator of past environmental conditions especially when the chemistry data are considered along with other proxy data. The complexities involved with the chemical and isotopic changes accompanying hydrologic change, solute evolution, and the autoecology of ostracodes all point to the need to exercise caution when interpreting shell chemistry. Nevertheless, the stable-isotope values and cation ratios (e.g., Mg/Ca, Sr/Ca) as well as the species assemblage of ostracodes can provide powerful tools for the reconstruction of paleoclimate and paleohydr

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6

Sugumaran, S., H. M. Nagaraj, and U. B. Mallikarjuna. "Ostracode fauna from the Patti Formation (Late Cretaceous) of Vridhachalam area, Tamil Nadu, India." Journal of Palaeosciences 46, no. (1-2) (1997): 133–40. http://dx.doi.org/10.54991/jop.1997.1327.

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An ostracode fauna is recorded from the Patti Formation (Late Cretaceous) of Vridhachalam area, Tamil Nadu. The assemblage includes Bairdia pentagonalis, B. cretacea, B. supplanata, Macrocypris limburgensis and Paracypris limburgensis, which are typical of Maestrichtian age. The ostracodes show strong affinities with those recorded from the Ariyalur and Pondicherry areas, and those described from the type-Maestrichtian of Holland. The above assemblage and the presence of distinct Paleocene ostracodes in the overlying Pondicherry Formation throw light on K/T transition in the Vridhachalam area.

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7

Tinn, Oive, and Tõnu Meidla. "Ordovician ostracodes from the Komstad Limestone." Bulletin of the Geological Society of Denmark 46 (December 20, 1999): 25–30. http://dx.doi.org/10.37570/bgsd-1999-46-03.

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The results of a pilot study on late Arenigian ostracodes of Bornholm, Denmark, are reported. The hard thermally altered limestone was disintegrated with sodium hyposulphite, the yielded ostracode material is of satisfactory preservation. The ten identified genera include palaeocopes (Glossomorphites, Aulacopsis, Ctenentoma, Asteusloffia, Euprimites), eridostracans (Conchoprimitia), cytherelliformes (Unisulcopleura) and metacopes (Elliptocyprites, Longiscula, Microcheilinella and “Silenis”). The studied ostracode assemblage shows resemblance to that of the Central Baltoscandian Confacies Belt.

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8

Cronin, Thomas M., and Gary S. Dwyer. "Deep Sea Ostracodes and Climate Change." Paleontological Society Papers 9 (November 2003): 247–64. http://dx.doi.org/10.1017/s1089332600002230.

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Ostracodes are bivalved Crustacea whose fossil shells constitute the most abundant and diverse metazoan group preserved in sediment cores from deep and intermediate ocean water depths. The ecology, zoogeography, and shell chemistry of many ostracode taxa makes them useful for paleoceanographic research on topics ranging from deep ocean circulation, bottom-water temperature, ecological response to global climate change and many others. However, the application of ostracodes to the study of climate change has been hampered by a number of factors, including the misconception that they are rare or

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9

Ayress, Michael A. "Crescenticythere, a new enigmatic ostracode from the Tertiary of New Zealand." Journal of Paleontology 67, no. 5 (1993): 905–6. http://dx.doi.org/10.1017/s0022336000037197.

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During examination of the large ostracode assemblage collections at the Department of Scientific and Industrial Research, Geology & Geophysics, Lower Hutt, New Zealand, a single specimen of unusual shape was encountered. So unusual is the crescentic outline and infolding of the entire shell periphery that assignment even to a phylum was difficult, and it was only upon scanning electron microscopic study that subcentral muscle scars were clearly observed and these enabled confident identification of the specimen as an ostracode. One specimen is not usually considered sufficient to propose a

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10

Crasquin, Sylvie, Milan Sudar, Divna Jovanovic, and Tea Kolar-Jurkovsek. "Upper Permian ostracode assemblage from the Jadar Block (Vardar zone, NW Serbia)." Annales g?ologiques de la Peninsule balkanique, no. 71 (2010): 23–35. http://dx.doi.org/10.2298/gabp1071023c.

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Ostracodes from the Changhsingian (latest Permian age) in the uppermost part of the ?Bituminous Limestone? Formation of the Komiric Section in NW Serbia (Jadar Block, Vardar Zone) are described and illustrated. Three new species of ostracodes are introduced: Basslerella jadarensis n. sp., Acratia serbianella n. sp., and Knoxiella vardarensis n. sp. The ostracode assemblage, together with conodonts and foraminifers, is the first record of the youngest Late Permian age microfaunas from Serbia and from the central part of the Balkan Peninsula.

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