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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://dirros.openscience.si/IzpisGradiva.php?id=19207"><dc:title>Palaeoecological significance of the trace fossil Circulichnis Vyalov, 1971 from the Carboniferous of the Donets Basin, Ukraine</dc:title><dc:creator>Dernov,	Vitaly	(Avtor)
	</dc:creator><dc:subject>trace fossils</dc:subject><dc:subject>Circulichnis</dc:subject><dc:subject>Pennsylvanian</dc:subject><dc:subject>Ukraine</dc:subject><dc:description>The  ichnogenus  Circulichnis  Vyalov  is  a  horizontal  a  ring-  or  ellipse-shaped  burrow  and/or  locomotion  trace  of  an  unknown producer, most likely an annelid or a “worm”, preserved on the bedding plane. This ichnogenus is known over a  wide  age  interval  (Ediacaran–Oligocene).  Circulichnis  demonstrates  a  wide  ecological  range  and  has  been  found  in  continental  (Mermia  ichnofacies),  shelf,  and  relatively  deep-water  (turbidites)  deposits.  It  is  commonly  interpreted  as  a  sediment  feeding  trace,  but  the  peculiarities  of  its  formation  remain  somewhat  mysterious,  as  it  is  unclear  how  the  tracemaker reached the sediment surface, as lateral branches of the ring-shaped traces are extremely rare and have only been  observed  by  a  few  researchers.  A  rather  large  specimen  of  Circulichnis  montanus  Vyalov,  1971  with  a  preserved  lateral  branch  was  found  in  the  Mospyne  Formation  (upper  Bashkirian,  Lower  Pennsylvanian)  of  the  Donets  Basin.  This  discovery  confirmed  the  assumption  made  by  Alfred  Uchman  and  Bruno  Ratazzi  regarding  the  peculiarities  of  formation of Circulichnis. According to these authors, a single ring-shaped Circulichnis indicates an attempt to forage at a specific level in the sediment, while the lateral branches of Circulichnis are part of a vertical shaft leading to another level within the sediment. The study of Circulichnis montanus from the Donets Basin has confirmed that at least variant C of the Circulichnis formation scheme proposed by Uchman and Ratazzi is correct, i.e. the lateral branch is a horizontal or subhorizontal part of a generally vertical shaft. However, it is important to note that the correctness of variants A and B of the Uchman and Ratazzi scheme cannot be excluded. To answer this question unequivocally, new finds of well-preserved Circulichnis are necessary.</dc:description><dc:publisher>Geološki zavod Slovenije</dc:publisher><dc:date>2024</dc:date><dc:date>2024-07-09 08:32:14</dc:date><dc:type>Neznano</dc:type><dc:identifier>19207</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
