Bactroceras boliviensis Aubrechtová, 2015

Kröger, Björn & Pohle, Alexander, 2021, Early-Middle Ordovician cephalopods from Ny Friesland, Spitsbergen - a pelagic fauna with Laurentian affinities, European Journal of Taxonomy 783 (1), pp. 1-102 : 36-42

Bactroceras boliviensis Aubrechtová, 2015

Figs 12E, H, J , 13C , 24–27 , 28A–B , 29B

Bactroceras boliviensis Aubrechtová, 2015: 206–207 , fig. 6a–d, g.

Bactroceras aff. avus Holm – Marek et al. 2000: 56.

Bactroceras angustisiphonatum (Rüdiger) – Evans 2005: 27–31, pl. 3 figs 12–13, 15, 17–18, pl. 4 figs 2, 16.

Diagnosis

Bactroceras with a large shell diameter (> 45 mm), ornamented with transverse striae, and with concavity of septa of 30%; siphuncle tubular, marginal; diameter of siphuncle ⅛ to ¹/7 of the corresponding conch diameter; connecting ring very thin (after Aubrechtová 2015).

Material examined

Sixty-eight specimens (see Supp. file 1 for list of specimens); one from bed PO 7, two from bed PO 7.5, two from bed PO 123.3, and 62 from bed PO 131, 4 m, 4.5 m, 120.3 m, and 128 m above base of Olenidsletta Member, V1–V2 trilobite zone, Blackhillsian, Floian. An additional number of 15 microscopic specimens from bed PO 131.

Description

The conchs are straight and expand gradually with a low angle of expansion, ca 4° (mean 3.7°; 1 st –3 rd quantile: 2.7–4.5; n = 37) ( Fig. 24 ). The conch cross section is invariantly circular. The largest specimen in the sample is a fragmentary body chamber with a maximum diameter of ca 48 mm and a length of

92 mm (specimen FMNH-P30179). At the base of the body chamber, where the diameter is 38 mm, a narrow paired dorsomyarian muscle scar is preserved ( Fig. 25A ).

The conch surface is ornamented with striae, which are directly transverse and run parallel to the sutures ( Figs 13C , 25B–D ). The striae are very slightly shifted toward the apex at the prosiphuncular side, forming a very shallow ventral sinus. The striae have partly an imbricated profile in well preserved specimens and are rounded in less well preserved and smaller specimens. The spacing of the striae increases with growth in relation to the conch diameter ( Fig. 24 ), reaching densities between 1–20 lirae per one millimeter.

The relative chamber length varies between 0.6 in the smallest preserved growth stages with diameters of less than 5 mm and 0.2 in the largest specimens with diameters> 35 mm. The diameter of the septal foramen is ca ¹/6 of corresponding conch cross section (mean rSD = 0.17; 1 st –3 rd quantile: 0.15–0.19; n = 55) ( Fig. 26 ). The rSD decreases with conch diameter toward 0.15 at a maximum conch diameter of 43 mm ( Fig. 26 ). The siphuncle is eccentric, positioned between the center of the conch and the conch margin in early growth stages with conch cross section diameters <6 mm, and it is nearly marginal in later growth stages ( Fig. 26 ). The septal necks are orthochoanitic and the siphuncular segments are tubular and have a thin connecting ring ( Fig. 27 ).

The siphuncles of specimen FMNH-P30215 from bed PO 131, and specimens FMNH-P30243 and FMNH-P30259 from bed PO 7.5 ( Figs 27A–D , 28A–B ), contain an irregular conical continuous endosiphuncular lining, which adapically fills the entire siphuncle but thins out adorally within a length of ca 20–30 mm at conch diameters of up to 38 mm.

The conch apex consists of a nearly spherical protoconch with a mean diameter of 1.1 mm (1 st –3 rd quantile: 1.1–1.2; n = 15) and a mean length of 1 mm (1 st –3 rd quantile: 1.0–1.1; n = 15), which is distinguished from a shaft by a shallow, often very indistinct constriction ( Figs 12J , 29B ). The spherical initial part is smooth, without a cicatrix ( Fig. 12H ), and the following ca 5–10 mm of the initial part of the conch is nearly smooth. In some well-preserved specimens a faint, narrow, transverse ornamentation is visible, which becomes more pronounced during growth. The shaft and the following ca 5–10 mm are almost straight and have a very low angle of expansion or are tubular. At a distance of 25 mm from the apical tip the conch is only 2.7 mm wide in specimen FMNH-P30165. The caecum is elongated; in specimen FMNH-P30176 it is ca 0.4 mm long and 0.3 mm wide, directly marginal and reaches only through the adoral half of the initial chamber, which is 0.7 mm long. Septal crowing occurs in specimen FMNH-P30176 between the second to fourth septum with a distance between 0.4 and 0.5 mm, and the subsequent four chambers have a length of 0.7–0.9 mm ( Fig. 29B ).

Remarks

The assignment of the specimens described above to B. boliviensis is justified herein by the combination of the distinctively pronounced transverse ornamentation, a relatively wide siphuncle, and a relatively large adult size. The relative siphuncular diameter of the Olenidsletta Member specimens is on average slightly wider than that of the holotype and syntype of B. boliviensis . However, the range of measurements of the two types is well within the range of our specimens (see Fig. 24 ).

Another species of Bactroceras with a similarly wide siphuncle (rSD = ¹/6) is B. wilsoni Flower, 1968 from the Antelope Valley Limestone, Nevada, USA, which differs, however, in lacking the distinctively striated ornamentation. The types of B. angustisiphonatum ( Rüdiger, 1889) differ from the Bactroceras specimens of the Olenidsletta Member in having a very narrow siphuncle with an rSD of ca ¹/12 ( Holm 1898: 9) to ¹/11 ( Rüdiger 1889: 37). Additionally, the ornamentation of B. angustisiphonatum , as originally described by Rüdiger (1889: 37), is weak; Rüdiger (1889) referred to it as “Anwachsstreifen”, i.e., growth lines (this is in contrast to his use of the term “Ringlinien”, i.e., transverse striae, e.g., Rüdiger 1889: 38). The relatively weak ornamentation, with growth lines only, of the original material of B. angustisiphonatum is also explicitly mentioned in Holm (1898: 9). Bactroceras sandbergeri (Barrande, 1867) differs also in having a siphuncle with a diameter of <0.1 of the corresponding conch cross section ( Aubrechtová 2015).

Evans (2005) described an assemblage of ca 40 specimens from the Olenidssletta Member, collected by R.A. Fortey and D.L. Bruton, under “ B. angustisiphonatum (Rüdiger, 1891) ” (sic!). The assemblage came from “the top of division V 2 ” ( Evans 2005: 28), with high probability from exactly the same horizon as most of the specimens assigned to B. boliviensis herein. Bactroceras boliviensis is distinctive within the orthocones of the Olenidssletta Member and occurs in great numbers at 128 m above the base of the member at Profilstranda. The specimens from the Olenidssletta Member described by Evans (2005) are therefore with high probability in large part conspecific with the specimens described herein under B. boliviensis . Our measurements add to the knowledge of the variability of this assemblage, and specifically the dimensions and characters of the apical parts are almost identical (compare Evans 2005: text-fig. 8e). However, B. boliviensis co-occurs with Ethanoceras solitudines gen. et sp. nov., which differs in having a less pronounced ornamentation and a non-marginal, eccentrically positioned siphuncle throughout its entire growth. This makes the distinction between Bactroceras and Ethanoceras difficult or impossible in specimens with diameters <6 mm and without well preserved outer shell or extreme apical parts. Therefore, we measured only specimens with a well-preserved shell surface. Our results differ slightly from the measurements of Evans (2005: text-fig. 8) in having a strictly marginal siphuncle position in B. boliviensis in specimens with diameters>ca 6–7 mm. This difference is potentially a result of unrecognized specimens of Ethanoceras solitudines gen. et sp. nov. in the sample of Evans (2005).

Stratigraphic and geographic range

The types and previously only known specimens of B. boliviensis are from the Pircancha Formation, Bolivia, Baltograptus minutus graptolite zone, which is time equivalent to the lower part of the Didymograptus bifidus graptolite zone (see Gutiérrez-Marco & Martin 2016). The D. bifidus graptolite zone reaches into the upper part of the V 1 division of the Olenidsletta Member ( Cooper & Fortey 1982). The specimens described herein are from V 1 –V 2 trilobite zones; hence the species is known from the Blackhillsian, late Floian of Bolivia and Spitsbergen.

Figures

Fig. 12 (previous page). Apical parts of orthoconic cephalopods from the Olenidsletta Member, Floian, Ordovician, near Hinlopenstretet, Ny Friesland, Spitsbergen. A. Cyptendoceras sp. B., FMNH-P30472 from Profilbekken river basin, locality PR-phosphatic. Lateral view with siphuncle toward the left. B. Svalbardoceras sterna gen. et sp. nov, FMNH-P30169, from PO 7.5. Lateral view with siphuncle toward left. C, F–G. Eosomichelinoceras borealis sp. nov. C. Specimen FMNH-P30171, from bed PO 123.3. Lateral view with prosiphuncular side toward the right. D. Bactroceras fluvii sp. nov., FMNH-P30168, from Profilbekken river basin, locality PR-phosphatic, showing the ventral side with ventral sutural lobe. E, H, J. Bactroceras boliviensis Aubrechtová, 2015 from bed PO 131. E. Specimen FMNH-P30165, nearly dorsal view, showing the transition of the extreme apical part toward the juvenile part of the conch. F. Specimen FMNH-P30182, lateral view with siphuncle toward the right. G. Specimen FMNH-P30184, lateral view with siphuncle toward the left. H. Specimen FMNH-P30183, apical view, showing the smooth apical surface of the protoconch. I. Ethanoceras solitudines gen. et sp. nov., FMNH-P30173, from bed PO 123.3, note the fine transverse striation. J. FMNH-P30160, showing details of fine transverse ornamentation. Scale bar = 2 mm for all figures.

Fig. 13. Details of the conch surface of transversally ornamented orthocones from the Olenidsletta Member, Floian, Ordovician, Profilstranda section, Ny Friesland, Spitsbergen. A. Ethanoceras solitudines gen. et sp. nov., FMNH-P30383, holotype, from bed PO 131. B. Eosomichelinoceras borealis sp. nov., FMNH-P30279, holotype, from bed PO 123.3. C. Bactroceras boliviensis Aubrechtová, 2015, FMNH-P30232, from bed PO 131, conch section with nearly cyclic spacing of transverse striae. Scale bar = 10 mm for all figures.

Fig. 24. Diagrams of spacing of ornamentation, angle of expansion, and relative chamber length of Bactroceras boliviensis Aubrechtová, 2015 from the Olenidsletta Member (Olen. Mbr), Floian, Ordovician, Profilstranda section, Ny Friesland, Spitsbergen. Data of type specimens from Aubrechtová (2015). See Supp. file 1 for details of measurements.

Fig. 25. Bactroceras boliviensis Aubrechtová, 2015, from bed PO 131, from the Olenidsletta Member, Floian, Ordovician, Profilstranda section, Ny Friesland, Spitsbergen. A. Specimen FMNH-P30430, lateral view of body chamber with dorsomyarian muscle impression at base ventral, prosiphuncular side toward the left. B. Specimen FMNH-P30231, view of ventral, prosiphuncular side. C. Specimen FMNH-P30248, lateral view of specimen with partly cyclic spacing of ornamentation; ventral, prosiphuncular side toward the right. D. Specimen FMNH-P30215, with fine transverse ornamentation; ventral, prosiphuncular side toward the right. Scale bar = 10 mm for all figures.

Fig. 26. Diagrams of relative siphuncular diameter and relative siphuncular distance of Bactroceras boliviensis Aubrechtová, 2015, from the Olenidsletta Member (Olen. Mbr), Floian, Ordovician, Profilstranda section, Ny Friesland, Spitsbergen. Data of type specimen from Aubrechtová (2015). See Supp. file 1 for details of measurements.

Fig. 27. Median sections of phragmocones of Bactroceras boliviensis Aubrechtová, 2015, from the Olenidsletta Member, Floian, Ordovician, Profilstranda section, Ny Friesland, Spitsbergen. Note conical endisiphuncular lining in A–D. A. Specimen FMNH-P30215, from bed PO 131. B. Specimen FMNH-P30259, from bed PO 7.5. C–D. Specimen FMNH-P30243, from bed PO 7.5. E. Specimen FMNH-P30383, from bed PO 131. Scale bars: A–C, E = 5 mm; D = 1 mm.

Fig. 28.Reconstructionand interpretation of detailsof connecting ring and septal necks.A–B. Bactroceras boliviensisAubrechtová, 2015.A. Specimen FMNH-P30243, see Fig. 27D.B. Specimen FMNH-P30215, see Fig.29A.C. Eosomichelinoceras borealis sp. nov., from the Olenidsletta Member, Floian, Ordovician, Profilstranda section, Ny Friesland, Spitsbergen, specimen FMNH-P30305, see Fig. 33C. Black: septal neck and septum. Dark grey: connecting ring. Light grey: endosiphuncular deposits. Without scale.

Fig. 29. Median sections of phragmocones of Bactroceras Holm, 1898. A, C–D. Bactroceras fluvii sp. nov., from Profilbekken river basin, locality PR-phosphatic. A. Specimen FMNH-P30159, with adapical siphuncular segment, taphonomically slightly distorted.B. Bactroceras boliviensisAubrechtová, 2015, FMNH-P30176 from bed PO 131, extreme apical part. C–D. Specimen FMNH-P30177, holotype. C. Details of the protoconch. D. Apical part with transition toward juvenile growth stages; note the slightly expanded siphuncular segments. Scale bars: A = 5 mm; B–C = 1 mm; D = 2 mm.