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Melchin et al.—Llandovery retiolitine graptolites from Arctic Canada


attached to transverse rods by connecting rods. Ancora sleeve of very largemeshes, better developed on reverse side, seams facing out. No evidence of the presence of stomata. List surfaces smooth to very finely striated.


Etymology.—cancellatus: L; cross-barred, lattice; referring to basket-like ancora umbrella.


Remarks.—See remarks for genus and for Aeroretiolites? sp.


Aeroretiolites? sp. Figure 14.6–14.8


Materials.—One very well-preserved, mature specimen with a complete ancora umbrella.


Occurrence.—L. convolutus Zone from Cape Manning, Corn- wallis Island.


Description.—Tubarium of five thecal pairs, widening gradually from 1.2mm across ancora umbrella to a maximum of 1.88mm distally. 2TRD 1.75–2.0mm. Prosicula not preserved, prosicular interval and virgella ~1.2mm long. Ancora umbrella simple and very shallow, with four radial lists, saucer shaped, with an irregular rim. Mid-ventral lists moderately inclined, slightly convex. Mid-ventral list of theca 11 attached to rim of umbrella; distal mid-ventral lists relatively long, slightly convex. Ventral side orifice present under theca 12, none under theca 11. Thecal lateral apertural rods and looping apertural rim horizontal. Nema attached by connecting rods to transverse rods. Zigzag lists define reverse wall. Pleural lists connected to each other directly at lateral apertural rods, and are parallel to each other on both lateral walls. No ancora sleeve. List surfaces smooth to very finely striated.


Remarks.—Aeroretiolites? sp. is a represented by only a single, very well-preserved specimen that is similar in most respects to Aeroretiolites cancellatus.Itdiffers,however,inits possessionof a simpler and shallower ancora umbrella without spiral lists, pleural lists that are straight, vertical and continuously connected, and thecal apertural rims that are horizontal. In addition, the single specimen shows no prosicula or ancora sleeve lists, although these features are sometimes inconsistently preserved in some retiolitines. Considering that there is only a single specimen, we identify it as Aeroretiolites?sp. The specimen of Aeroretiolites? sp. appears similar in


many respects to those of Eorograptus spirifer but differs in that the former possesses mid-ventral thecal lists and lacks spiral lists on the ancora.


Genus Paraplectograptus Příbyl, 1948


Type species.—Retiolites eiseli Manck, 1917, by original designation.


Paraplectograptus? sp. Figure 15.1–15.6


Materials.—Nine fragmentary, somewhat compressed speci- mens, all immature, of which five are well preserved, and most complete consists of ancora umbrella and up to three thecae.


Occurrence.—S. guerichi Zone, Snowblind Creek and Rookery Creek, Cornwallis Island. Three additional questionable specimens fromSnowblind Creek and one questionable specimen from the L. convolutus Zone at CapeManning.


Description.—Sicula 0.4–0.49mm long, virgella 0.6–0.7mm, prosicula partially to completely preserved, with longitudinal rods. Ancora umbrella simple, shallow, consisting of four radial lists that may divide distally, with complete, undulatory rim, 1.2–1.5mm wide. Openings under theca 1² about twice as large as that under theca 11. Transverse rods present. Pleural lists inclined slightly, connected to lateral apertural list declined strongly outwardly, and to horizontal apertural rim. Apertural lips looped, horizontal. No thecal mid-ventral lists. Nema attached to connecting rods. Zigzag lists on reverse side, outside of which are a few weak ancora sleeve lists; none observed on obverse side. List micro-ornament smooth or weakly longitudinally striated.


Remarks.—These specimens may represent a new species, possibly representing a new genus, but because of the limited number of distorted specimens, and their immaturity, they are questionably referred to the genus Paraplectograptus,with which they share a similar ancora umbrella and tubarium construction (see Bates et al., 2005, fig. 6F). Our phylogenetic analysis (see above) suggests that this is a stem taxon to the clade that includes Paraplectograptus, Sokolovograptus and all of the more derived species previously regarded as “plectograptines.” Paraplectograptus? sp. appears to con- sistently possess a preserved prosicula. Its micro-ornamentation consists of fine parallel striae, in contrast to the pustular ornamentation of Paraplectograptus s.s. and more derived “plectograptines.”


Acknowledgments


M.J.M and A.C.L. acknowledge the long-term financial support from Natural Sciences and Engineering Research Council (Canada) (NSERC), and logistical support from the Polar Continental Shelf Project. A.K. acknowledges a financial grant from Ministerstwo Nauki i Szkolnictwa Wyższego decision number 499/N (Poland) and collaborative support from NSERC 2009/0. Field support from A. McCracken, M. Coniglio, J. Lukasik, J. Russel-Houston, E. MacDonald, P. Noble,


Figure 15. Scanning electron microscopy images of Paraplectograptus?sp.:(1) GSC137657, stereopair of a slightly deformed immature specimen with well-preserved prosicula with weakly developed longitudinal rod, and one thecal pair, section LL1B, S. guerichi or S. turriculatus Zone; (2, 3) GSC137658, (2) proximo-lateral view of interior of simple ancora umbrella, (3) lateral view of moderately distorted specimen; section LL1B, S. guerichi or S. turriculatus Zone; (4, 6) GSC137659, (4) enlargement of ancora list showing weakly striated micro-ornament and fusellar insert seams, (6) shallow and simple ancora umbrella and remnant of prosicula, section LL1-77, S. guerichi or S. turriculatus Zone; (5) GSC 137660, stereopair of well-preserved specimen showing ancora umbrella, partially preserved prosicula, and the first thecal pair, pleural lists (a) and lateral apertural rods (b), sectionMSC07, 3m a above 01G, S. guerichi Zone?.


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