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Brief Report Acta Palaeontologica Polonica 61 (3): 621–626, 2016

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Brief Report Acta Palaeontologica Polonica 61 (3): 621–626, 2016 Brief report Acta Palaeontologica Polonica 61 (3): 621–626, 2016 A new tubeworm of possible serpulid affinity from the Permian of Sicily ROSSANA SANFILIPPO, AGATINO REITANO, GIANNI INSACCO, and ANTONIETTA ROSSO A new tubeworm, Palaeotubus sosiensis gen. et sp. nov., is for its morphology. Unfortunately, the tube inner microstruc- described from the Permian Pietra di Salomone limestone ture is not preserved owing to diagenetic recrystallisation. (Sosio Valley, W Sicily). The new species is characterized This lack of information coupled with the scarcity of presently by a thick tube ornamented with slightly flared peristomes available material, consisting of a single incomplete specimen, and numerous longitudinal keels. The internal structure of prevented an unequivocal taxonomic attribution. The new the tube was obliterated during diagenesis, which prevents tubeworm has been cautiously considered as incertae sedis but the tube unequivocal systematic attribution. Nevertheless, its alleged affinities to serpulids have been highlighted. all preserved morphological characters strongly suggest that the new tube belongs to serpulids. When confirmed by Institutional abbreviations.—MSNC, Palaeontological Collec- further findings, the positive attribution of this new spe- tions, Museo Civico di Storia Naturale di Comiso, Ragusa, Italy. cies to serpulids will imply that it represents the ancestor of the Serpulidae, and the earliest evidence of calcareous Material and methods tubeworm polychaetes from the Palaeozoic. The single specimen examined in the present paper comes from the Pietra di Salomone, one of the fossiliferous megablocks Introduction cropping out near Palazzo Adriano in the Sicani Mountains, Calcareous tubeworms are common fossils throughout the western Sicily (Fig. 1A, B). These Permian limestone mega- Phanerozoic, but their systematics were addressed in detail blocks are included in debris flow and turbidite sediments de- only recently, when studies of the skeletal microstructure al- posited in a base-of-slope setting (Fig. 1C, D). Flügel et al. (1991) lowed to discern tentaculitids, cornulitids, trypanoporids, and considered these blocks as mainly Wordian (Murghabian) in other fossil tubeworms like spirorbids and serpulids (Vinn and age. However, some reef-derived pebbles within them, are pos- Mutvei 2009). Serpulids (i.e., Serpulidae) are common and sibly Capitanian (Midian) or even Wuchiapingian (Dzhulfian) widely distributed in the fossil record, with about 46 genera in age. The same age, and probably even a Changhsingian and 350 species (ten Hove and Kupriyanova 2009) and are (Dorashamian) age, was suggested by Jenny-Deshusses et al. quite abundant in the modern seas, where they are widespread, (2000) for the Pietra di Salomone megablock. Therefore, the also colonizing extreme environments (e.g., Di Geronimo studied specimen might be of Wordian to latest Permian age. et al. 1997; Kupriyanova et al. 2009, 2010, 2014; Sanfilippo Further information about geological setting and age is given 2009; Rosso et al. 2010, 2013; Sanfilippo et al. 2013, 2015; in Flügel et al. (1991). Vinn et al. 2013). The group is still virtually unknown from The “Sosio Limestone” is world-wide famous for its well the Palaeozoic and the earliest records, related to the small preserved and very rich invertebrate fauna. Overall, more than Filograna-like forms, date back to the Middle Triassic (ca. 244 520 species have been described from the Sosio Limestone Ma) (see Ippolitov et al. 2014). Paleozoic records of presumed and more than 300 species from the Pietra di Salomone mega- serpulids (e.g., Sandberger and Sandberger 1856; Dalvé 1948; block (Fig. 2). This fauna comprises foraminifera, sponges, Clausen and Álvaro 2002; Ziegler 2006) consist of erroneous corals, bryozoans, brachiopods, gastropods, bivalves, ammo- interpretations of tube-like organism remains. Seemingly to noid and nautiloid cephalopods, trilobites, ostracodes, and all Palaeozoic spirorbids, later attributed to microconchids other crustaceans, as well as crinoids, blastoids, and fossils (Weedon 1994; Taylor and Vinn 2006), these problematic fos- of uncertain taxonomic assignment (see Flügel et al. 1991; sils, commonly reported as “Serpula” in early papers, proved Jenny-Deshusses et al. 2000; Ernst 2000; Jones et al. 2015, to be trypanoporids, cornulitids, tentaculits, or hederelloids and references therein). The specimen described herein was when their tube microstructures have been carefully analyzed found in the white crinoid-rich limestone from the upper part (see Weedon 1991; Vinn and Taylor 2007; Taylor and Wilson of the Pietra di Salomone, by one of us (AR) in October 2014, 2008; Vinn 2013). during field works lead by the MSNC, within the Riserva A new tubeworm, Palaeotubus sosiensis gen. et sp. nov., Naturale Orientata Monti di Palazzo Adriano e Valle del Sosio. found in the Permian Pietra di Salomone limestone (western Associated faunas include the crinoids Palermocrinus jaekeli Sicily), is here described. This new species is certainly attrib- Gislen, 1924 and Heterobrachiocrinus fabianii Yakovlev, 1938, utable to a calcareous tubeworm, strongly recalling a serpulid the gastropods Bellerophon sosiensis Gemmellaro, 1889 and Acta Palaeontol. Pol. 61 (3): 621–626, 2016 http://dx.doi.org/10.4202/app.00209.2015 622 ACTA PALAEONTOLOGICA POLONICA 61 (3), 2016 San Calogero Flysh Pietra di Salomone limestone Palaeotubus sosiensis sp. nov. (Middle– Late Permian) (Wordian to Upper Permian) Figs. 3, 4. cherty limestone 1m Halobia Etymology: Named after the type locality, in the Sosio Valley area. Mediterranean with Sea (Late Carnian A C marl and calcilutite (Carnian) to Rhaetian) Holotype: A unique incomplete unattached tube (MSNC 4499) broken Palazzo debris and landslides (Recent) at both ends. Adriano Palazzo sandy clay and globigerind marl Type locality: Sosio Valley, western Sicily (Italy). Adriano Sicily (Middle Langhian– Serravallian) sandy clay and glauconit arenite Type horizon: Pietra di Salomone limestone, Wordian to Upper Permian. B (Oligocene– Early Miocene) globigerinid limestone “Scaglia” Diagnosis.—Tube free, relatively thick and solid, circular in (Early Cretacaeous – Eocene) cross-section. Longitudinal keels smooth. Peristomes circular 4 pelagic limestone and radiolarite (Jurassic) and slightly flared. Halobia 3 cherty limestone with (Late Carnian– Rhaetian) Description.—The holotype is 17 mm long and slightly bend- marl and calcilutite (Carnian) ing, due to a change in growth direction in correspondence of San Calogero Flysh (Middle– Late Permian) a feeble peristome. The specimen consists of a tube fragment 2 undifferentiated blocks rather massive and solid, not increasing in diameter, circular in (Permian Triassic)– T. San CalogeroSan Sosio limestone blocks cross-section, 3.8 mm in diameter at its distal end (Fig. 3A, B). (Permian) Lumen 2.7 mm wide (Figs. 3C, 4D). Sculpture consisting of 12 1 dipping tectonic boundary continuous, straight, robust, and smooth longitudinal keels, in axis of syncline equal distances of about 900 μm from each other (Fig. 4B, C). main thrust fault N Two low prominent transverse rings representing peristomes, road one of which slightly flared indicating the growth direction and the pristine position of the tube opening (Figs. 3A, B, 4A, B). A change in growth direction is evident in correspondence of a slight peristome, increasing the bent aspect of the tube (Fig. Cozzo di 500 m 40° 3A, B). Feeble transverse growth lines revealed by careful ob- D Pietrafucile 30° servation, best visible in the interspaces between keels. They Fig. 1. Location of the study area in Mediterranean (A) and Sicily (B). are ca. 0.2 mm spaced, their faint concavity facing distally Section across the Torrente San Calogero and the Pietra di Salomone block (Fig. 4B, C). Tube outline regularly undulated in cross section, (C), modified from Flügel et al. 1984. Geological map of the Palazzo Adri- for the alternation of shallow rounded depressions and angular ano area (D), showing the location of the Pietra di Salomone block (mod- peaks, these latter corresponding to the transverse keels’ pro- ified from Di Stefano and Gullo 1997). 1, Pietra di Salomone limestone; files (Fig. 4D, E). Tube wall ca. 0.5 mm thick, the structure pre- 2, Rupe di Passo di Burro; 3, Petra dei Saracini; 4, Rupe di San Calogero. sumably obliterated by diagenetic recrystallisation, but with an inner part formed by prevailing small and relatively loose Plocostoma piazzii (Gemmellaro, 1889), and the brachiopods crystals (Fig. 4F), grading to an outer part mostly with larger (Gemmellaro, 1894) and sp. Coscinaria communis Martinia and more densely patched crystals (Fig. 4G). The specimen was separated mechanically from the slightly cemented calcilutite containing cm-sized fossils and Remarks.—The studied tube of P. sosiensis gen. et sp. nov. accurately cleaned to examine the whole external surface. Low only superficially resembles those of other common Palaeozoic magnification photos were acquired with a Zeiss Discovery organisms with the only character in common being the tubu- V8A stereomicroscope equipped with an Axiovision acquisi- lar calcareous skeleton. Among these fossils are the sabellid tion system, in order to document general tube morphology. Glomerula Nielsen, 1931 and other tubeworms such as ten- The specimen was also examined uncoated under a LMU taculitids, cornulitids, and trypanoporids in the past affiliated Tescan Vega Scanning Electron Microscope in Low Vacuum with annelids
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