NDLI: Inozoid sponges from Upper Triassic (Norian-Rhaetian) reefs of the Nayband Formation (NE and Central Iran)

Content Provider	Springer Nature Link
Author	Senowbari Daryan, Baba
Copyright Year	2005
Abstract	Die obertriassischen (Nor-Rhät), siliziklastisch-karbonatischen Ablagerungen der Nayband-Formation gehören zu einer der wichtigsten geologischen Einheiten der zentraliranischen Mikroplatte, einem Teil des kimmerischen Kontinents. Kleine Korallen- oder Schwamm-dominierte Biokonstruktionen sind in stratigraphisch unterschiedlichen Horizonten eingebettet und in mehreren Lokalitäten im Zentral- und Nordostiran aufgeschlossen.Die Schwamm-Fauna dieser Biokonstruktionen besteht überwiegend aus corallinen Schwämmen („Inozoida“, Sphinctozoida“, „Chaetatida“ einschließlich „Spongiomorphida“) und seltenen Hexactinellida. In früheren Arbeiten wurden bereits folgende inozoide Schwämme aus diesen Biokonstruktionen beschrieben (Senowbari-Daryan et al. 1997,Senowbari-Daryan 2003):Radiofibra norica, Permocorynella maxima, Sestrostomella robusta, Marawandia iranica, Enaulofungia? triassica undPeronidella iranica.Im Rahmen dieser Arbeit werden folgende inozoide Schwämme aus verschiedenen Lokalitäten im Zentral- und Ostiran beschrieben:Molengraaffia regularis Vinassa de Regny,Anguispongia parva nov. gen., nov. sp.,Anguispongia magna nov. sp.,Aliabadia diversilata nov. gen., nov. sp.,Lutia pustulata nov. gen., nov. sp.,Prestellispongia maxima nov. sp.,Prestellispongia stellata nov. sp.,Vermispongiella delijanensis nov. sp.,Grossotubenella variabilis nov. sp. undPeronidella? tenuiparietallis nov. sp.The Upper Triassic (Norian-Rhaetian) siliciclastic-carbonatic deposits of the Nayband Formation are one of the most important geological groups of the central Iranian microplate as a part of the Cimmerian Continent. Small-scaled coral- or sponge-dominated bioconstructions are embedded within the different stratigraphic levels of the Nayband Formation cropping out in several localities in central and northeast Iran.The sponge fauna of these bioconstructions is dominated by coralline sponges (“Inozoida”, “Sphinctozoida”, “Chaetetida” including “Spongiomorphida”) and rarely Hexactinellida. In earlier publications following inozoid sponges from these bioconstructions were already described (Senowbari-Daryan et al. 1997,Senowbari-Daryan 2003):Radiofibra norica, Permocorynella maxima, Sestrostomella robusta, Marawandia iranica, Enaulofungia? triassica andPeronidella iranica.In this paper following inozoid sponges from different localities in central and east Iran are described:Molengraaffia regularis Vinassa de Regny,Anguispongia parva nov. gen., nov. sp.,Anguispongia magna nov. sp.,Aliabadia diversilata nov. gen., nov. sp.,Lutia pustulata nov. gen., nov. sp.,Prestellispongia maxima nov. sp.,Prestellispongia stellata nov. sp.,Vermispongiella delijanensis nov. sp.,Grossotubenella variabilis nov. sp.,Peronidella? tenuiparietallis nov. sp.
Starting Page	261
Ending Page	299
Page Count	39
File Format	PDF
ISSN	00372110
Journal	Palaeobiodiversity and Palaeoenvironments
Volume Number	85
Issue Number	2
Language	English
Publisher	Springer-Verlag
Publisher Date	2005-01-01
Publisher Place	Berlin, Heidelberg
Access Restriction	Subscribed
Subject Keyword	Sponge Upper Triassic Norian Rhaetian Reef Nayband Formation Iran Paleontology Biodiversity Animal Systematics/Taxonomy/Biogeography Plant Systematics/Taxonomy/Biogeography Freshwater & Marine Ecology
Content Type	Text
Resource Type	Article
Subject	Paleontology

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