Latest Ordovician–early Silurian chitinozoans from the eastern Alborz Mountain Range, Kopet–Dagh region, northeastern Iran: biostratigraphy and palaeobiogeography

Review of Palaeobotany and Palynology (Impact Factor: 1.66). 06/2007; 145(1-2):173-192. DOI: 10.1016/j.revpalbo.2006.10.003
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    ABSTRACT: Although there were Late Ordovician spiriferides in the superfamily Cyrtioidea, namely Eospirifer and Odakella, only the former genus survived the terminal Ordovician extinction, and only Eospirifer is known from the earliest Llandovery (Rhuddanian). However, in the succeeding mid-Llandovery (Aeronian), the spiriferides radiated to include not only more species within Eospirifer and Striispirifer in the Eospiriferidae, but also the new genus Iranospirifer described here, which is the earliest representative of the other family within the superfamily, the Hedeinopsidae. The Ordovician species were confined to the South China continent and the Boshchekul volcanic island arc in Kazakhstan, but by the Aeronian the superfamily had spread westwards to various other continents, including the main Gondwanan superterrane (which included Iran) in the early Aeronian, and Avalonia-Baltica and Laurentia in the late Aeronian. The new species Eospirifer ghobadiae and Iranospirifer qarabilensis are both described from the lower Aeronian of Iran, and there is a note on the Aeronian rhynchonellide Stegocornu, which is endemic to Iran and nearby areas.
    Alcheringa An Australasian Journal of Palaeontology 12/2013; 37(4):558–564. DOI:10.1080/03115518.2013.828254 · 0.90 Impact Factor
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    ABSTRACT: We date Late Ordovician preglacial deposits by mean of chitinozoans•We record damaged reworked chitinozoans in synglacial deposits•We date earliest Silurian postglacial deposits by mean of chitinozoans•Chitinozoan vesicles are an excellent carbon source for δ13C analysis
    Review of Palaeobotany and Palynology 11/2014; 212. DOI:10.1016/j.revpalbo.2014.10.005 · 1.66 Impact Factor
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    ABSTRACT: In the early 1930s Alfred Eisenack first reported unknown, bottle-shaped, organic-walled microfossils that he had discovered in erratic boulders from the south-eastern shores of the Baltic Sea. Eisenack erected the new group Chitinozoa to classify these strange microfossils of unknown biological affinity. From the 1930s to the 1950s, a few publications appeared reporting new findings and providing descriptions of these fossil organisms. It was only since the 1960s, with the development of the oil industry and the intensive biostratigraphical use of organic-walled microfossils, that publications dealing with chitinozoans became more numerous and that the description of new genera and species rapidly increased. The peak of description of new species was reached in the 1960s, but the number of publications remained high into the late 1990s. Since the 1990s the research activities on chitinozoans are conducted by a much smaller number of scientists. One of the major driving forces of chitinozoan research in the last forty years was Florentin Paris at the University of Rennes (Brittany, France). He first established a high-resolution chitinozoan biostratigraphy of the Ordovician of southern Europe and played an active role in bringing all scientists together for the development of global biostratigraphical schemes and palaeobiogeographical scenarios of the Ordovician, Silurian and Devonian. It was also Florentin Paris, together with his Estonian colleague Jaak Nõlvak, who suggested the now widely accepted biological interpretation that Chitinozoa are most probably egg cases of a planktonic organism unknown from the fossil record. F. Paris was also the first to collaborate w ith experts to use biogeochemical analyses and the C isotope signal of the chitinozoans to better understand their biological affinity and detect biogeochemical changes in Palaeozoic oceans.
    Review of Palaeobotany and Palynology 11/2013; 198:2–13. DOI:10.1016/j.revpalbo.2013.08.001 · 1.66 Impact Factor

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