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    Tytuł:
    Reconstruction of Oligocene and Neogene freshwater fish faunas - an actualistic study on cypriniform otoliths
    Autorzy:
    Schulz-Mirbach, T
    Reichenbacher, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/20987.pdf
    Data publikacji:
    2006
    Wydawca:
    Polska Akademia Nauk. Instytut Paleobiologii PAN
    Tematy:
    utricular otolith
    fish
    Miocene
    cypriniform otolith
    Oligocene
    morphology
    freshwater fish
    reconstruction
    lapillus
    paleontology
    Opis:
    Fossil utricular otoliths (= lapilli) from cypriniform fishes have long been recorded from European Oligocene and Neogene freshwater and oligohaline sediments. Until now, their determination was limited to the family level owing to the lack of morphological investigations on lapilli of Recent cypriniforms. The present study introduces a terminology for the lapillus morphology that is based on the lapilli of 134 specimens of 20 cyprinid and one balitorid species. It is demonstrated that the lapillus has valuable characters for taxonomic classification. As a result, fossil lapilli from Oligocene and Miocene continental deposits from the western Mediterranean, the Swiss and the South German Molasse Basin, the Mainz Basin, and additionally from Anatolia could be determined. Nine species were identified: aff. Abramis sp. vel aff. Alburnus sp., aff. Alburnoides sp., aff. Barbus sp., cf. Leuciscussp., Palaeoleuciscus sp., Palaeotinca moeddeni sp. nov., Palaeotinca sp. 1, aff. Phoxinus sp., and aff. Rutilus sp. vel aff. Scardinius sp. Our study includes the oldest record of a Phoxinus−related and a Palaeotinca species from Europe. Additionally, aff. Abramis sp. vel aff. Alburnus sp. and aff. Alburnoides have been identified as fossils for the first time. The determination of the fossil lapilli has been supported by means of pharyngeal teeth, with the exception of aff. Abramis sp. vel aff. Alburnus sp., whose lapilli were found together with pharyngeal teeth of Palaeocarassius sp. It is suggested that these so−called Palaeocarassius pharyngeal teeth do not belong to an ancestor of the Carassiuslineage, but to a forerunner of the Abramis or Alburnuslineage. Our results support the previously described turnover in the Paratethys freshwater fish fauna about 17–18 Ma ago, when Palaeotinca spp. became extinct and the first appearance of Palaeoleuciscussp. and Palaeocarassiussp. (= aff. Abramissp. vel aff. Alburnus sp.) occurred. The Oligocene and Miocene cypriniform fishes did not evolve any provincialism from southern France throughout the Molasse Basin to the Mainz Basin.
    Źródło:
    Acta Palaeontologica Polonica; 2006, 51, 2
    0567-7920
    Pojawia się w:
    Acta Palaeontologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Comparison of Hard Structures for Age Estimation and Chemical Composition Analysis of Otoliths of Perch from Lake Trzesiecko under Reclamation
    Przydatności struktur do szacowania wieku i analiza składu chemicznego otolitów okonia Perca fluviatilis (L.) z Jeziora Trzesiecko, poddanego zabiegom w celu obniżenia trofii wód
    Autorzy:
    Lampart-Kałużniacka, M.
    Heese, T.
    Powiązania:
    https://bibliotekanauki.pl/articles/1813889.pdf
    Data publikacji:
    2017
    Wydawca:
    Politechnika Koszalińska. Wydawnictwo Uczelniane
    Tematy:
    okoń
    Perca fluviatilis
    otolity
    łuski
    promienie płetw
    wiek
    skład chemiczny w otolitach
    perch
    otolith
    scales
    rays fins
    age
    chemical compositions of otolith
    Opis:
    The study revealed that the ray of the dorsal fin D was the most readable structure for age estimation in perch from Lake Trzesiecko. Otoliths turned out to be more problematic structures. Age estimation based on otoliths was difficult, and the structures were very brittle, which made it impossible to prepare microscope slides. This was probably related to their crystal structure. Growth rate could only be calculated based on the scale. In the case of older specimens aged 5+ and more, however, it was difficult to identify the mark related to the first year of life due to the low readability of the middle part of the scale. This results in inflated results obtained for group L1. Studies on age of fish should be conducted based on several structures due to the possibility of verification of the obtained results. Performing the analysis of only one selected element results in high variability of the obtained data, and therefore inaccurate conclusions. The recorded presence of iron atoms in the otoliths suggests the accumulation of the metal resulting from the application of chemical compounds by man in living organisms.
    Prezentowany Porównanie przydatności struktur twardych do szacowania wieku i analiza składu chemicznego otolitów okonia Perca fluviatilis (L.) pochodzącego z rekultywowanego Jeziora Trzesiecko. Prowadzone badania wskazały, że najbardziej czytelną strukturą do szacowania wieku u okonia pochodzącego z Jeziora Trzeskiecko był promień płetwy grzbietowej D. Otolity okazały się strukturami bardziej problematycznymi. Trudno było na ich podstawie szacować wiek, jednocześnie były bardzo „kruche”, co uniemożliwiło wykonanie na ich podstawie preparatów mikroskopowych. Prawdopodobnie było to związane z ich budową krystaliczną. Tempo wzrostu można było obliczyć tylko na podstawie łuski. Stąd rozsądne wydaje się działanie w którym, szacowanie wieku i wyznaczanie tempa wzrostu prowadzi się w oparciu o kilka elementów. Opieranie badań tylko na jednej wybranym elemencie, skutkuje dużą zmiennością uzyskiwanych wyników. Świadczyć o tym może, chociażby brak zgodności danych, uzyskiwanych w czasie badań, prowadzonych przez różne osoby, które szacowały wiek dla ryb w oparciu o te same struktury twarde. Odnotowanie atomów żelaza w otolitach, może być efektem kumulacji tego metalu w organizmach żywych, a źródłem jego jest związek chemiczny, aplikowany do jeziora w celu poprawy jego stanu ekologicznego.
    Źródło:
    Rocznik Ochrona Środowiska; 2017, Tom 19; 809-823
    1506-218X
    Pojawia się w:
    Rocznik Ochrona Środowiska
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The relationship between fish length and otolith size and weight of Acanthopagrus arabicus Iwatsuki, 2013 (Sparidae) collected from the Iraqi marine waters
    Związek między długoscią całkowitą a wielkością i masą otolitu u Acanthopagrus arabicus, Iwatsuki 2013, (Sparidae) złowionego w irackich wodach morskich
    Autorzy:
    Jawad, L.
    Qasim, A.
    Al-Zaidy, F.M.
    Waryani, B.
    Rutkayová, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/3131491.pdf
    Data publikacji:
    2021
    Wydawca:
    Zachodniopomorski Uniwersytet Technologiczny w Szczecinie. Wydawnictwo Uczelniane ZUT w Szczecinie
    Tematy:
    fish size
    fish length
    otolith
    yellowfin seabream
    Acanthopagrus arabicus
    Sparidae
    sea water
    Iraq
    Źródło:
    Acta Scientiarum Polonorum. Zootechnica; 2021, 20, 1; 27-33
    1644-0714
    Pojawia się w:
    Acta Scientiarum Polonorum. Zootechnica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Marine fishes (Elasmobranchii, Teleostei) from the Glendon Limestone Member of the Byram Formation (Oligocene, Rupelian) at site AWa-9, Washington County, Alabama, USA, including a new species of gobiid (Gobiiformes: Gobiidae)
    Autorzy:
    Ebersole, Jun A.
    Cicimurri, David J.
    Stringer, Gary L.
    Powiązania:
    https://bibliotekanauki.pl/articles/2024054.pdf
    Data publikacji:
    2021
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    chondrichthyes
    Teleostei
    otolith
    Paleogene
    Gulf Coastal Plain
    Vicksburg Group
    ryby chrzęstnoszkieletowe
    otolity
    paleogen
    Opis:
    The Oligocene (Rupelian) Byram Formation (Vicksburg Group) in Alabama, USA, is divided into three members, including (in ascending order) the Glendon Limestone, unnamed marl, and the Bucatunna Clay. The Oligocene marine units in Alabama have been historically under-investigated, but bulk samples recently obtained from Glendon Limestone Member exposures at site AWa-9 in Washington County yielded 20 unequivocal elasmobranch and teleost taxa. This surprisingly diverse paleofauna, based on isolated teeth, bones and otoliths, includes the new taxon, Gobiosoma? axsmithi sp. nov., as well as “Aetomylaeus” sp., Albula sp., Aplodinotus gemma Koken, 1888, Ariosoma nonsector Nolf and Stringer, 2003, Balistidae indet., Citharichthys sp., Myliobatoidei indet., Diretmus? sp., Hemipristis sp., Negaprion aff. N. gilmorei (Leriche, 1942), Pachyscyllium sp., Paralbula sp., Physogaleus sp., Preophidion meyeri (Koken, 1888), Sciaena pseudoradians (Dante and Frizzell in Frizzell and Dante, 1965), Sciaenops? sp., Sparus? elegantulus Koken, 1888, Sphyraena sp., and Syacium sp. Additional remains were recovered but could not be identified beyond undetermined Elasmobranchii or Teleostei. All these taxa represent first occurrences within the Glendon Limestone Member in Alabama, and the “Aetomylaeus” sp., Pachyscyllium sp., Paralbula sp., and Sciaenops? sp. specimens represent the first occurrences of each in the Oligocene of the Gulf Coastal Plain of the USA. We also report the first record of Oligocene Paralbula Blake, 1940 teeth, and the first occurrence of an Oligocene member of the Balistidae in the Western Hemisphere. This marine vertebrate assemblage indicates that the Glendon Limestone Member at site AWa-9 represented a subtropical to temperate, middle shelf paleoenvironment with a paleowater depth interpreted as 30–100 m.
    Źródło:
    Acta Geologica Polonica; 2021, 71, 4; 481--518
    0001-5709
    Pojawia się w:
    Acta Geologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Określenie wieku kozy (Cobitis taenia) i kozy złotawej (Sabanejewia aurata) z wykorzystaniem niektórych struktur twardych
    Age Validation of Spined Loach (Cobitis taenia) and Golden Loach (Sabanejewia aurata) Using Some Calcinated Structures
    Autorzy:
    Lampart-Kałużniacka, M.
    Pietraszewski, D.
    Marszał, L.
    Heese, T.
    Przybylski, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/1819042.pdf
    Data publikacji:
    2013
    Wydawca:
    Politechnika Koszalińska. Wydawnictwo Uczelniane
    Tematy:
    określanie wieku kozy
    struktury twarde
    otolith growth
    fin rays
    population
    fish
    lake
    temperature
    precision
    accuracy
    biology
    scales
    Opis:
    Age is one of the most important life history variables of fish used to estimate growth rate, mortality rate and production. Age determining is usually carried out by analyzing any of several calcified structures, such as scales, otoliths (more frequently) or fin rays (rather seldom). Scales are easy to collect and this is the reason why this structure has been widely used, but for several reasons annuli may be ambiguous to discern on scales, especially in the loaches. The material was collected in May 2010 in the Pilica River. A total of 29 fish individuals, including 16 spined loach and 13 golden loach, were examined. The range of total length (TL) of the fishes in the sample studied was 43–102 mm in the former and 35 do 70 mm in the latter species, respectively. The precision of ageing using the cross-sections of dorsal, caudal, anal, pectoral and ventral fins rays were compared with age determination on the basis of otoliths. The analysis of the annuli of the investigated structures revealed that individuals aged 2 to 5 years (golden loach) and aged 3 to 7 years (spined loach) occurred in the material (Table 1 and 2, respectively). The obtained results indicate that in natural water bodies older individuals than formerly presumed may occur. Microscopic slides of the cross sections of otoliths and fins are most reliable for ageing such structures. The anal fin (A) it the most reliable structure for ageing, i.e. the age obtained from the fin is least divergent from the age obtained from the otolith. While planning the investigations of the age structure of populations it is necessary to establish the periods of sampling in a way that will be most congruent with the period of annuli formation.
    Źródło:
    Rocznik Ochrona Środowiska; 2013, Tom 15, cz. 2; 1041-1052
    1506-218X
    Pojawia się w:
    Rocznik Ochrona Środowiska
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Fish remains, mostly otoliths, from the non-marine early Miocene of Otago, New Zealand
    Autorzy:
    Schwarzhans, W.
    Scofield, R.P.
    tennyson, A.J.D.
    Worthy, J.P.
    Worthy, T.H.
    Powiązania:
    https://bibliotekanauki.pl/articles/23337.pdf
    Data publikacji:
    2012
    Wydawca:
    Polska Akademia Nauk. Instytut Paleobiologii PAN
    Tematy:
    fish remains
    remains
    otolith
    Early Miocene
    Miocene
    Otago
    New Zealand
    Pisces
    Eleotridae
    Galaxiidae
    Retropinnidae
    Mataichthys
    freshwater fish
    Bannockburn Formation
    Mataichthys bictenatus
    Galaxias angustiventris
    Galaxias bobmcdowalli
    Galaxias brevicauda
    Galaxias papilionis
    Galaxias parvirostris
    Galaxias tabidus
    Prototroctes modestus
    Prototroctes vertex
    Mataichthys procerus
    Mataichthys rhinoceros
    Mataichthys taurinus
    Opis:
    Fish remains described from the early Miocene lacustrine Bannockburn Formation of Central Otago, New Zealand, consist of several thousand otoliths and one skeleton plus another disintegrated skull. One species, Mataichthys bictenatus Schwarzhans, Scofield, Tennyson, and T. Worthy gen. et sp. nov., an eleotrid, is established on a skeleton with otoliths in situ. The soft embedding rock and delicate, three−dimensionally preserved fish bones were studied by CT−scanning technology rather than physical preparation, except where needed to extract the otolith. Fourteen species of fishes are described, 12 new to science and two in open nomenclature, representing the families Galaxiidae (Galaxias angustiventris, G. bobmcdowalli, G. brevicauda, G. papilionis, G. parvirostris, G. tabidus), Retropinnidae (Prototroctes modestus, P. vertex), and Eleotridae (Mataichthys bictenatus, M. procerus, M. rhinoceros, M. taurinus). These findings prove that most of the current endemic New Zealand/southern Australia freshwater fish fauna was firmly established in New Zealand as early as 19–16 Ma ago. Most fish species indicate the presence of large fishes, in some cases larger than Recent species of related taxa, for instance in the eleotrid genus Mataichthys when compared to the extant Gobiomorphus. The finding of a few otoliths from marine fishes corroborates the age determination of the Bannockburn Formation as the Altonian stage of the New Zealand marine Tertiary stratigraphy.
    Źródło:
    Acta Palaeontologica Polonica; 2012, 57, 2
    0567-7920
    Pojawia się w:
    Acta Palaeontologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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