Argoviacrinus Rarissimus N. G. N. Sp., a New Crinoid (Echinodermata) from the Middle Oxfordian of Northern Switzerland

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Argoviacrinus Rarissimus N. G. N. Sp., a New Crinoid (Echinodermata) from the Middle Oxfordian of Northern Switzerland Argoviacrinus rarissimus n. g. n. sp., a new crinoid (Echinodermata) from the Middle Oxfordian of northern Switzerland Autor(en): Hess, Hans / Spichiger, Pia Ursula Objekttyp: Article Zeitschrift: Eclogae Geologicae Helvetiae Band (Jahr): 94 (2001) Heft 3 PDF erstellt am: 01.10.2021 Persistenter Link: http://doi.org/10.5169/seals-168907 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. 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Basel. 2001 Argoviacrinus rarissimus n. g. n. sp., a new crinoid (Echinodermata) from the Middle Oxfordian of northern Switzerland Hans Hess1 & Pia Ursula Spichiger2 Key words: Crinoid. Argoviacrinus rarissimus n. g. n. sp.. Middle Oxfordian. Switzerland, description, affinities, palaeoecology ZUSAMMENFASSUNG ABSTRACT Aus den Birmenstorf Schichten (mittleres Oxford) von Holderbank (Kt. Aargau) The unique specimen of a new crinoid. Argoviacrinus rarissimus n. g. n. sp., from the Middle Oxfordian Birmenstorf Member of Holderbank wird eine neue Crinoiden-Art. Argoviacrinus rarissimus n. g. n. sp.. (Canton is beschrieben. Der Einzelfund ist ein kleiner Kelch aus Radialkranz. Basalia Aargau) a small cup with radiais, basais and a stem-like cirriferous is und stielartigem Cenlrodorsale mit Zirren: die Gelenkfläche zum Stiel isl eine centrodorsal. The articular facet to the stem a circular inflexible cryptosym- unbewegliche Krypto-Symplexie mit Randwulst und Kôrnerbelag. die eine plexy with rim and granules, transformed from a cryptosynarthry during the the dominant ursprüngliche Synarthrie überlagert. Die Aehnlichkeit der Gelenkfläche mit development. The morphological similarity to stems of cyrtocrinids. Stielgliedern der sessilen Cyrtocriniden. die dominierenden Crinoiden der crinoids of these strata, is considered to be due to convergence. The form Birmenstorf Schichten, dürfte eine Konvergenzerscheinung sein. Die Form wird is thought to he related to the Thiolliericrinidae and. thus, is an aberrant member als Weiterentwicklung der Thiolliericrinidae und somit als aberrantes Mitglied of the Order Comatulida. der Ordnung Comatulida angesehen. 1. Introduction menstorf Member is exposed along a length of about 150 m as The Middle Oxfordian sponge facies of northern Switzerland a roughly 30 m high inclined wall with vegetation at the top. ("Argovian" Birmenstorf Beds) is popular with fossil collectors The beds strike roughly NW-SE with a 30-60° dip. The for its rich fauna of ammonites, sponges, bryozoans and stratigraphically higher Effingen Member is exposed in other parts brachiopods but, perhaps, even more for its echinoderms of the quarry. The Birmenstorf Member has been characterized (echinoids. crinoids). Indeed, the clove-like cups of as a basinal spongolite (Gygi 2000a) with siliceous Eugeniacrinites cariophilites were first figured by Scheuchzer in 1702. sponges making up as much as 30 % of the rock volume. It is a Of special interest is the rich fauna of peculiar and at times succession of micritic limestones, marly limestones and marls bizarre crinoids of the Order Cyrtocrinida that were extensively with a thickness of 4 to 4.5 m at the Chalch quarry. The Effingen described in the classic monographs of Loriol (1877-1879: Member, a basinal argillaceous mudstone. is a succession 1882-1889) and Quenstedt (1874-1876) (see also Hess 1975). It of blue-grey marls with interbedded marly limestones and pure came as a big surprise that a completely new type of crinoid limestones; it reaches a thickness of about 240 m in the has been found in these extensively searched strata by the Holderbank area (R. Allenbach. pers. comm.. 2001). The junior author during her diploma work. Birmenstorf Member was deposited during the Transversarium Zone; the Effingen Member includes the Bifurcatus and the lower part ofthe Bimammatum Zones (Gygi 2000b). 2. Geological setting The fossils were collected from the surface at the foot of During the Late Jurassic the study area was situated in an the eastern part of the wall and the talus below. They all epicontinental sea structured into local basins and swells. Coeval belong to the Birmenstorf Member as the situation at the outcrop platform deposits are found toward the northwest. In the prevents contamination by fossils from the Effingen Beds. In northern part of the large Chalch (also called "Schiimel") the lower Effingen Beds, about 5 m above the top of the quarry at Holderbank (coordinates: 655.900/253.500). the Bir¬ Birmenstorf Member (a bed covered with sponges), a 25 mm 1 Naturhistorisches Museum. Augustinergasse 2. CH-4001 Basel. Switzerland. E-mail: [email protected] 2 Unt. Siedlungsweg 7. CH-4914 Roggwil. Switzerland. E-mail: bup.spichiger(8"datacomm.ch A new crinoid from the Oxfordian of northern Switzerland 489 thick lens occurs packed with crinoid ossicles from species that signed to Cyrtocrinus nutans. As already discussed by Jaekel occur in the underlying Birmenstorf Beds. Their relatively (1891. p. 622). the two forms are linked by intermediates and may small size (the largest elements are less than 5 mm in diameter) at most be distinguished by their surface structure, a character suggests that they were well sorted before they accumulated, that we now regard as part of the intraspecific variation, an opinion possibly during a tempestite event. The echinoderm species in shared by Loriol (1877-1879. p. 209 and 1882-1889. p.l 15). the lower parts of the Effingen Member also occur in the Cups attached to proximal columnal 27 Birmenstorf Member, but species diversity and number of specimens Cups (isolated) 144 in the Effingen Member is lower. Proximal columnals (with facet to cup) 382 Columnals (including 28 pluricolumnals) 707 Brachials 118 3. Fauna Eugeniacrinites cariophilites (caryophyHaitis) The richly fossiliferous Birmenstorf Member is characterized (V. SCHLOTHEIM) by abundant siliceous sponges, ammonites, echinoderms and Cups attached to proximal columnal 2 brachiopods. The fauna is similar to the somewhat younger Cups (isolated) 57 Lochen Beds (Bimammatum Zone) of the Swabian Alb. Second primibrachials (IBr2 primaxillary) 19 deposited at the margins of sponge-algal bioherms (Ziegler Columnals 395 1977). The crinoids listed below have been collected at Holder- Pilocrinus moussoni (Desor) bank during a time period of 200-250 hours by the junior Cups 23 author. A relatively large number (several hundreds) of mostly Brachials 89 very small brachials and columnals is not listed because of Columnals (including 4 pluricolumnals) 98 doubtful assignment. A list of the total fauna collected will be Gymnocrinus moeschi de Loriol reported elsewhere (Spichiger. in preparation). Remark: These brachials may belong to Pilocrinus moussoni, the taxonomic position of Gymnocrinus will be discussed in List of crinoids from the Birmenstorf Member of the the forthcoming revision of the Treatise on Invertebrate Chalch quarry. Holderbank (assignment based on Hess 1975). Paleontology, Pt. T Crinoidea) Isocrinida Second primibrachials (IBr2 primaxillary) 9 Isocrinus cingulatus (Münster in Goldfuss) Tetracrinus moniliformis Goldfuss Pluricolumnals (stem fragments) and columnals 66 Basal circlets 5 Brachials (including 6 with aboral spine) 7 Radiais (isolated) 12 Balanocrinus subteres (Münster in Goldfuss) Brachials 584 Pluricolumnals and columnals 324 Pinnulars (fused, dagger-like) 3 Brachials 1 Columnals 1 Plicatocrinus hexagonus Münster Cyrtocrinida Cups 1 Cyrtocrinus nutans (Goldfuss) Comatulida Remarks: Cups of this species have variation in height, great Archaeometra scrobiculata (Münster) ornamentation and in the ratio of radial cavity diameter to cup Cups with centrodorsal 2 diameter, which is between 0.8 and 0.2 (a ratio of 0.4 to 0.5 being Brachials ("Archaeometra aspera [Quenstedt]") 399 the most common). Correspondingly, the radial articular facets vary considerably in size. Brachials with granulated surface, Undetermined ossicles previously assigned to Sclerocrinus compressus Gammarocrinites Isocrinid cirrals (Isocrinus cingulatus or Balanocrinus compressus in the Treatise on Invertebrate Paleontology. subteres) 197 Rasmussen 1978, T831) (Hess 1975, PI.25. figs. 2 and 3) are here as¬ Attachment discs of cyrtocrinids 19 Fig. 1-8. Holotype of Argoviacrinus rarissimus n. g. n. sp. Birmenstorf Member. Holderbank. Natural
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