Phragmoteuthis polzbergensis, Lukeneder & Fuchs & Lukeneder, 2024
publication ID |
https://doi.org/10.1186/s13358-024-00319-4 |
persistent identifier |
https://treatment.plazi.org/id/EB37F410-5047-D42B-D92B-A57CB5CF12D8 |
treatment provided by |
Felipe |
scientific name |
Phragmoteuthis polzbergensis |
status |
sp. nov. |
Phragmoteuthis polzbergensis nov sp.
( Figures 7 View Fig , 8 View Fig , 9 View Fig , 11a, b View Fig ). non 2022b Phragmoteuthis bisinuata (Bronn) .
Lukeneder & Lukeneder (2022b), p. 273; Figs. 1B View Fig , 3 View Fig , 4 View Fig . non 2007b Phragmoteuthis bisinuata (Bronn) .
Doguzhaeva & Summesberger (2007b), p. 273; Figs. 2 View Fig ,
3B–D View Fig .
http://zoobank.org/ 46869B54-F172-462D-AE2A-5E2B1 912FAC5
Etymology: Named after the type locality, the Polzberg Konservat-Lagerstätte (Lower Austria).
Holotype: NHMW 2006 View Materials z0005/0021 is the only specimen with a proostracum, differentiated arm hooks and a cephalic cartilage preserved.
Type locality and horizon: Reingraben shales at Polzberg main section at 0 cm to − 50 cm, Carnian, Late Triassic.
Material: Eight specimens from recent excavations, at the lowermost 3 m of the Reingraben Shales at Polzberg, from sequence Po − 50 cm to Po 320 cm, inventoried at the NHMW ( NHMW 2021 View Materials /0001/0002; NHMW 2021 View Materials /0016/0400; NHMW 2021 View Materials /0123/0005, 0013, 0057, 0090, 0218, 0424) ; eight specimens from historical NHMW collections; NHMW 2005 View Materials z/0005/0021, 0040; NHMW 2012 View Materials / 0117/0011, 0025; NHMW 2012 View Materials / 0228/0495, 0512; NHMW 2020 View Materials / 0033/0003; NHMW 2021 View Materials /0124/0038. No mantle remains are preserved. If preserved, the oval-shaped carbonised ink sac is located near the centre of the specimens.
Description: Shell complex: Phragmocones and proostraca are flattened as in the type locality of P. bisinuata ; width measurements and indices are therefore equivocal. Phragmocone lengths range from 14.17 to 22.63 mm, proostracum lengths were measured from 20.41 to 88.31. Te ratio phragmocone length to proostracum length varies between 0.65 and 0.75. Opening angles cannot be determined exactly because of compaction; they range between about 25° and 30°
Sutures appear simple and densely spaced, but statements about septal spacing are speculative.
Te proostracum can be subdivided into a median field and adjacent hyperbolar zones and lateral fields. Te anterior margin of the median field is rounded. Dorsolaterally, the retracted hyperbolar zones are evenly arcuated and occupy c. 83% of the total shell length (ratio hyperbolar zone length to total shell length = 0.83). Te projected lateral fields are likewise evenly rounded and take c. 88% of the total shell length.
Arm complex: NHMW 2021 View Materials /0123/0021 stems from the lower, calcareous part of the section and comprises the proostracum, the cephalic cartilage and parts of a differentiated arm crown. Te proostracum of the specimen NHMW 2021 View Materials /0123/0090 only appears poorly preserved, but includes the complete arm crown with differentiated hooks, as well as both beaks. Te specimen’s total length is 88.3 mm, with a maximum width of 28.2 mm. Te arm crown of NHMW 2021 View Materials /0123/0090 is also preserved in situ and consists of different arm hook types (type 3, 5) .
All of the specimens possess both the stylet shaped (type 3) and curved (type 5) arm hooks ( Fig. 12a View Fig ). Closer investigation reveals that the strongly curved hooks preferentially represent at least one modified arm pair, each of them equipped with complementary hook pairs of stylet shaped and curved hooks. Te remaining arms are equipped with the stylet shaped hooks ( Figs. 8 View Fig , 9 View Fig ).
Head complex: The holotype shows a squashed, but determinable cephalic cartilage of type A. The well preserved cephalic cartilage of specimen NHMW 2012 View Materials /0123/0057 with arm hooks identical to those of the holotype and NHMW 2021 View Materials /0123/0090 confirms the presence of type A. Further cephalic cartilages of type A are present in specimens NHMW 2021 View Materials /0001/0002; NHMW 2012 View Materials /0117/0011, 0025; NHMW 2021 View Materials /0016/0400 ( Fig. 11a View Fig ); NHMW 2021 View Materials / 0123/0013, 0424. The carbonised, furcate type of cartilage ( Fig. 11a View Fig ; supplementary S1c Figure; Type A cartilage) appears to be a bilaterally symmetric paired structure with a calcite-filled channel system, which follows the geometry of the fossil (see also Lukeneder & Lukeneder, 2022b). It is a distinct, characteristic “C-structure” with a prolonged processus (supplementary S1c Figure). Additional triangularelongate “wing elements” ( Fig. 10a View Fig ) are located next to the C-shaped structure .
NHMW 2021 View Materials /0123/0013 with the type A cartilage displays a carbonized upper beak illustrating the outline of the inner (lateral wall, crest) and outer lamella (rostrum, hood, wings) .
NHMW |
Naturhistorisches Museum, Wien |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.