Type species

Monstrocrinus securifer Schmidt, Reference Schmidt1941.

Other species

Monstrocrinus granosus Schmidt, Reference Schmidt1941; and M. incognitus Scheffler et al., Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011.

Emended diagnosis

Rhodocrinitid with a medium bowl- to globe-shaped calyx, distal corners of infrabasal plates not visible in lateral view, proximal regular interrays with 1–3 plating, proximal CD interrays with 1–3 plating, median ray ridges absent, anitaxial ridge absent, primaxil hexagonal, calyx plates with various types of long spines attached to calyx plates, fixed pinnules absent, 20(?) free arms that divide once, brachials chisel biserial.

Occurrence

Upper Emsian (Lower Devonian) to lower Eifelian (Middle Devonian) of Europe (Rhenish Slate Mountains, North Rhine-Westphalia, Rhineland-Palatinate, and Hesse, Germany; and province of Teruel, Aragon, Spain). Middle and upper Eifelian (Middle Devonian) of South America (states of Pará and Tocantins, Brazil) (Ferreira and Fernandes, Reference Ferreira and Fernandes1989; Fernandes et al., Reference Fernandes, Fonseca and Ferreira2000; Scheffler et al., Reference Scheffler, Fernandes and Da Fonseca2006, Reference Scheffler, Fernandes and Da Fonseca2009, Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011, Reference Scheffler, Da Fonseca and Fernandes2015; Gama Jr. and Scheffler, Reference Gama and Scheffler2007; Scheffler, Reference Scheffler2010, Reference Scheffler2015). The occurrence of the genus Monstrocrinus in the Emsian–Eifelian boundary interval of the lowermost part of the Chefar El Ahmar Formation of the Ougarta Mountains in the Sahara province of Béni Abbès in southwestern Algeria in the Maghreb region of North Africa (see Le Menn, Reference Le Menn1990, Reference Le Menn1997) is not proven taxonomically.

Remarks

In addition to complete specimens of Orthocrinus tuberculatus Schmidt, Reference Schmidt1913, and Arthroacantha Williams, Reference Williams1883, Schmidt (Reference Schmidt1924, p. 17) mentioned a new crinoid genus “with unusually monstrous, axe-shaped spines on the basals and radials” from the former brickworks mine in the Osterbachtal, northwest of Olpe-Lütringhausen (see “Location and stratigraphy”). Seventeen years later, Schmidt (Reference Schmidt1941, p. 213–215) described this as Monstrocrinus n. gen. and considered this new discovery to have been a free-living benthic rhodocrinitid genus, which is characterized by “monstrous floating spines” (he interpreted the paddle-like, equatorially projecting spiny appendages of the calyx as useful elements for passive drifting on the sea bottom; see Fig. 2.3) and “very flexible, two-lined arms.” However, he pointed out that the genus was incompletely known and required a full description (Schmidt, Reference Schmidt1941, p. 213). His diagnosis was based on various disarticulated plates of the calyx as well as remains of the “floating spines.” This material was from different specimens and localities, which systematically cannot be assigned unequivocally to a genus or to one of the two Monstrocrinus species described by him. Nevertheless, Schmidt (Reference Schmidt1941, p. 213) combined these individual parts into a genus and species description. In addition, Schmidt (Reference Schmidt1941, p. 213) justified the lack of a stem with the alleged lack of a “stem scar” on the aboral side of the calyx; the column lumen was said to be closed by the fact that the proximal plates of the calyx are supposed to have grown together until the “column hole” was completely closed (Schmidt, Reference Schmidt1941, p. 215). The inconclusive evidence for this is a gelatin cast of the interior of a single calyx remnant preserved as a mold and required a full description (Schmidt, Reference Schmidt1941, p. 216). However, our re-examination of the type material revealed that this assumption was incorrect. Furthermore, Schmidt (Reference Schmidt1941, p. 215) deduced from disarticulated arm remains of his type specimen for M. granosus that the arms of all Monstrocrinus species must have been relatively short.

Figure 2.

(1) Calyx plate diagram of Monstrocrinus securifer according to Schmidt (Reference Schmidt1941, p. 214, Fig. 60a). (2) Schematic reconstruction drawing of a Monstrocrinus calyx with “broken off floating spines” and “indicated arms” after Schmidt (Reference Schmidt1941, p. 214, Fig. 60b). (3) Reconstruction drawing of Monstrocrinus securifer, previously interpreted as a stemless crinoid, with “completely preserved floating spines” (after Schmidt, Reference Schmidt1941, p. 214, Fig. 60b); arms are simplified.

The type species, Monstrocrinus securifer Schmidt, Reference Schmidt1941, p. 215–217, was described as a large representative of the genus, which was characterized by vertically positioned, axe-shaped “floating spines.” The surface of the crown ossicles is unornamented. The specimens described by Schmidt (Reference Schmidt1941) are from the uppermost section of the Emsian Orthocrinus Beds in the area around Olpe; these are: (1) the former brickworks mine NW of Olpe-Lütringhausen (see Location and stratigraphy); (2) the abandoned “Waukemicke Quarry” (Olpe-Wauckemicke); (3) several fossil localities near Olpe-Oberveischede; and (4) the fossil localities at the “Siele Farmyard” (between Olpe-Lütringhausen and Olpe-Waukemicke). Schmidt also mentioned M. securifer remains from localities outside Olpe (Bad Laasphe–Feudingen in the Siegen–Wittgenstein district in North Rhine-Westphalia and the “Old Paper Mill Haiger Hut,” NE-Haiger in the northern part of the Lahn–Dill district in central Hesse).

The second species, M. granosus Schmidt, Reference Schmidt1941, p. 217–218, was described as a medium-sized species that is characterized by a granular ornamentation of the calyx, by single-pointed and forked “floating spines,” and by “two-lined arms.” The species occurs in the upper Emsian Mandeln Formation within the “iron-shed greywacke schist” in the “Old Municipality Quarry” at the northern Hauberg Hill in Dietzhölztal–Mandeln in the Lahn–Dill district in central Hesse, north-northeast of Dillenburg. The original material was discovered by the late geologist Gerhard Solle (1911–1981), who found the specimen in 1935. It is deposited in the Senckenberg Research Institute and Natural History Museum Frankfurt under catalog number SMF-XXIII-113a. Forty-three years later Ettensohn (Reference Ettensohn1984) discussed genus Monstrocrinus as a stemless crinoid genus that was passively moved by current.

Le Menn (Reference Le Menn1990) described an isolated plate with preserved appendages from the upper Emsian Pena Negra Formation northeast of the municipality of Loscos in the province of Teruel, Aragon, Spain (Le Menn, Reference Le Menn1990, p. 151–153). This specimen has a striking elk-antler-like morphology (Le Menn, Reference Le Menn1990, p. 152, figs. 1a, b; see Fig. 3.3). This extreme morphology was considered distinct from the “floating spines” of the type species, M. securifer, described by Schmidt (Reference Schmidt1941). Thus, Le Menn (Reference Le Menn1990) described the new species M. aliformis Le Menn, Reference Le Menn1990. However, new specimens of M. securifer described herein from the lowermost Eifelian of the Ahrdorf- and Hillesheim Eifel synclines demonstrate that the spine morphology of M. aliformis falls within the range of variation of the spine processes of M. securifer. Therefore, M. aliformis is treated herein as a subjective junior synonym of M. securifer. These new specimens also have an effect on our understanding of the evolutionary development of the “floating spines” as postulated by Le Menn (Reference Le Menn1990, p. 156, fig. 3). According to Le Menn's model, the tapering Acanthocrinus spines (Reference Le Menn1990, p. 156, fig. 3a) were first modified to form the forked Monstrocrinus granosus spines (Le Menn, Reference Le Menn1990, p. 156, fig. 3b; see Fig. 3.2), which then became the elk-antler-like spines of the species M. aliformis (Le Menn, Reference Le Menn1990, p. 156, fig. 3c, see Fig. 3.3), and finally adopted the “paddle-like floating prong shape” of the species M. securifer (Le Menn, Reference Le Menn1990, p. 156, fig. 3d). This development was said to have taken place between the lower to the uppermost Emsian. Beside the fact that the M. granosus spine shown in Schmidt (Reference Schmidt1941, p. 217, fig. 61, no. b2) has no particular taxonomic relevance, it was wrongly interpreted by Le Menn (Reference Le Menn1990, p. 156, fig. 3b). The prong-shaped extension (Fig. 3.2) was interpreted as pointing to the calyx plate (proximally). However, it is not a backward-pointing prong but a distally tapering bifurcation (cf., Schmidt, Reference Schmidt1941, p. 217). The proposed evolutionary model is furthermore refuted by the common occurrence of different forms of spinous calyx plate appendages of all Monstrocrinus species.

Figure 3.

The isolated spiny calyx plate appendages of genus Monstrocrinus depicted in the literature. (1) Monstrocrinus securifer (after Schmidt, Reference Schmidt1941, pl. 16). (2) Monstrocrinus granosus (after Schmidt, Reference Schmidt1941, p. 217, fig. 61, no. b2), the upper figure shows a disarticulated distally forking spiny calyx plate appendage. Le Menn (Reference Le Menn1990, p. 156, fig. 3b) wrongly interpreted the prong-shaped extension as pointing proximally toward the calyx plate (see lower figure); however, the prong-shaped extension is not a backward-pointing prong, but a distally tapering bifurcation (see Schmidt, Reference Schmidt1941, p. 217). (3) “Monstrocrinus aliformis” (after Le Menn, Reference Le Menn1990, p. 152, fig. 1b). The species is interpreted in the present work as a subjective younger synonym of M. securifer. (4) “Monstrocrinus sp.” according to Le Menn (Reference Le Menn1990, p. 152, fig. 1d; 1997, pl. IV, fig. 14). The plate fragment cannot be clearly assigned to the genus Monstrocrinus. (5) Monstrocrinus incognitus (after Scheffler et al., Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011, p. 1191–1192, figs. 3, 4.1–4.6). (6) “Monstrocrinus securifer” (after Scheffler et al., Reference Scheffler, Fernandes and Da Fonseca2006, p. 238, fig. 3A–3E), either belonging to M. incognitus or to another species (further investigations are needed). The isolated spine shown at the bottom of the figure cannot be unequivocally assigned to the genus Monstrocrinus.

Furthermore, Le Menn (Reference Korn1990, p. 152, figs. 1c, d) figured two isolated calyx plates with narrow appendages as Monstrocrinus sp. from Emsian–Eifelian boundary of the lowermost part of the Chefar El Ahmar Formation of the Ougarta Mountains in the Sahara province of Béni Abbès in southwestern Algeria (also illustrated in Le Menn, Reference Le Menn1997, pl. 4, fig. 14). The plate fragment (Fig. 3.4) shown in Le Menn (Reference Le Menn1990, p. 152, figs. 1c, d) cannot be clearly assigned to the genus Monstrocrinus. Le Menn postulated that Monstrocrinus was stratigraphically restricted to the upper Emsian and that none of the species crossed the Lower–Middle Devonian boundary (Le Menn, Reference Le Menn1990, p. 149–150), which is refuted by specimens from the Lauch Formation of the lower Eifelian of the Eifel synclines and by the Monstrocrinus discoveries from the Eifelian strata of Brazil (see below).

Scheffler et al. (Reference Scheffler, Fernandes and Da Fonseca2006) described “Monstrocrinus securifer” from the middle Eifelian Maecuru Formation along the Maecuru River in the northwestern part of the State of Pará in Brazil. In addition to the characteristic “floating spines,” the authors also depicted an Acanthocrinus-like spine for the first time and assigned it to “M. securifer” (Scheffler et al., Reference Scheffler, Fernandes and Da Fonseca2006, p. 238, fig. 3E). This isolated calyx plate can only be assigned to the genus Monstrocrinus with reservation because numerous members of the family Rhodocrinitidae Roemer, Reference von Roemer and Bronn1855, have similar plates. Nevertheless, the articulated specimen described in the present work proves that Monstrocrinus had Acanthocrinus-like spines in addition to differently designed “floating spines.”

Scheffler et al. (Reference Scheffler, Fernandes and Da Fonseca2009) described additional remains of the calyx and crown of the genus Monstrocrinus and stated that each arm divided twice, resulting in four free arms per ray. Scheffler et al. (Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011) erected the new species Monstrocrinus incognitus from the middle to upper Eifelian Pimenteira Formation of the Parnaíba Basin in the State of Estado do Tocantins in Brazil. To date, this is the youngest species of the genus and was considered an intermediate form between “M. securifer” (with regard to the “floating spines” of Scheffler et al., Reference Scheffler, Fernandes and Da Fonseca2006, identified from the Maecuru Formation in Brazil) and “M. aliformis” from the Pena Negra formation of Spain (Scheffler et al., Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011, p. 1189). In contrast to these species, the “floating spines” should be characterized by short webs between the calyx plate attachment and the distal “wings” as well as by distally widened “wing appendages.” Note that the incomplete calyx plate in Scheffler et al. (Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011, p. 1192, fig. 4.2) has a longer web between the base of the plate and the distal “wing end” in comparison with the other examples illustrated (Scheffler et al., Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011, p. 1192, figs. 4.1, 4.3–4.6). This could indicate an insufficiently recorded morphological variability, as demonstrated for the type species in the present work. According to Scheffler et al. (Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011, p. 1192), the widened outer edge of the distal “floating spines” could have been useful for both an increase in the water turbulence in the direction of the arms in the parabolic filter position and for anchoring on the substrate (Scheffler et al., Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011, p. 1197).

The first two steps toward an understanding of Monstrocrinus is a standardized method for describing calyx spines, which then allows a means to describe spine variability more precisely on a single individual, from a single fossiliferous horizon, and intra- and interspecific variability. Figure 4 is a model for description of calyx spine shapes that builds on Scheffler et al. (Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011, fig. 3). The height and width of the entire calyx spine can be measured. The spine base has an outline shape and a height and width. Similarly, the spine neck (immediately abaxial from the spine base) has a cross-sectional shape and a height and width. The remainder of the calyx spine is referred to as the spine blade. This is the highly variable portion of the spine. The shape of spines is largely a function of different shapes of the upper edge, external edge, and lower edge (Fig. 4).

Figure 4.

Morphological features of Monstrocrinus spines (modified from Scheffler et al., Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011, p. 1191, fig. 3).

There is a wide range of spine shapes in Monstrocrinus. Based on the examined fossil material it is now possible to distinguish eight standardized morphological spine types (Fig. 5). They are the following types:

• Type 1: tapering, pointed spine.—Entire spine circular to subcircular in cross section; tapers to a point at terminus (Figs. 6.2, 9.2, 10, 12.1, 12.3, 12.4).

• Type 2: blunt spine.—Entire spine higher than wide, elliptical in cross section; upper and lower edges either slightly expanding, parallel, or slightly narrowing; tapers to a flat, blunt terminus (Fig. 9.2).

• Type 3: narrow paddle-shaped spine.—Neck long, much higher than wide, flat ellipse in cross section, gradually increases in height toward outer edge; upper and lower edges concave; entire spine expands gradually toward outer edge, lower edge longer, strongly asymmetrical; outer edge at an acute angle to horizontal; smooth or serrated (Fig. 8.1–8.3).

• Type 4: broad paddle-shaped spine.—Neck short, much higher than wide, flat ellipse in cross section, rapidly increases in height toward outer edge; upper and lower edges sharply concave; entire spine expands rapidly in height, upper and lower edges very convex and expand at different rates yielding an asymmetrical spine; outer edge at a high angle to horizontal; straight or broadly convex; smooth or serrated. Type 4 spine shapes can be subdivided into two subtypes: (1) subtype 4a—upper edge longer and higher, spine asymmetrical upward; and (2) subtype 4b—lower edge longer and lower, spine asymmetrical downward (Fig. 8.4).

• Type 5: flat, high fan.—Neck variable in shape, much higher than wide, flat ellipse in cross section; upper and lower edges parallel or broadly concave; entire spine shape variable; outer edge at high angle to horizontal, smooth. Type 5 spine shapes can be subdivided into two subtypes: (1) subtype 5a—neck short; upper and lower edges broadly concave, entire spine relatively short, gradually expanding in height toward outer edge; outer edge broadly convex; and subtype 5b—neck long, short, or undifferentiated; upper and lower edges very broadly concave or subparallel; entire spine gradually expanding from the neck, shortest at mid-spine position, or rectilinear; outer edge concave with or without upper and lower blunt extensions.

• Type 6: bifurcating spine.—Neck long or short, much higher than wide, flat ellipse in cross section; entire fan gradually expanding in height toward outer edge, upper and lower edges broadly concave, bifurcates into two spines near or away from the spine base, entire spine symmetrical or asymmetrical; terminal extensions circular to subcircular in cross section, taper to a blunt point (Figs. 8.5, 12.2).

• Type 7: forked spine.—Neck of various lengths, much higher than wide, flat ellipse in cross section; entire spine gradually expanding in height toward outer edge, upper and lower edges broadly concave; outer margin with various spine sizes and arrangements, spines may be long or short, may assume a serrated appearance, are arranged symmetrically or asymmetrically; spine cross section circular to elliptical. (Figs. 8.6, 8.7, 9.2, 10, 12.2, 12.4).

• Type 8: strongly asymmetrical paddle shaped spine with spinose outer margin.—Neck short, much higher than wide, flat ellipse in cross section, rapidly increases in height toward outer edge; entire spine with upper and lower edges concave, expanding in height distally, lower edge more convex, longer, and lower; highly asymmetrical; outer edge at a high angle to horizontal, straight or broadly concave, serrated or with small spines (Fig. 8.8, 8.9).

Figure 5.

Categorization of transitions between calyx plate and spine and definition of standardized morphological calyx spine types and subtypes.

Figure 6.

Recast holotype of Monstrocrinus securifer Schmidt, Reference Schmidt1941 (no. IGPB-SCHMIDT, W.E.-18a) from the uppermost section of the Emsian Orthocrinus Beds (Polygnathus costatus patulus Conodont Biozone) of the former brick factory in the Osterbachtal, northwest of Olpe-Lütringhausen (administrative district Arnsberg, Sauerland, North Rhine–Westphalia, Germany). (1, 2) Aboral view of the calyx, showing pentalobate axial canal (white arrows), which were not shown in the original illustration by Schmidt (Reference Schmidt1941, pl. 16, fig. 2b); (3) lateral view of the calyx with rudimentarily preserved type 1 spines (white T1). Scale bars = 1 cm.

These eight morphological types can be divided into two additional categories (Category A and B), because calyxes of Monstrocrinus have two different types of transitions between the proximally positioned calyx plate and the distally projecting end of the spine. Category A is a spine that truly seems to be completely a physical part of the calyx plate, whereas Category B appears to be an attachment onto the calyx plate, which is either positioned immediately proximal to a more planar calyx plate (e.g., in M. granosus), or somewhat higher, at the distal end of a funnel-shaped calyx plate projecting externally (e.g., in M. securifer; see Fig. 8.10–8.12). In M. granosus, the outer portion of the calyx plate is coarsely granulated, whereas the center of the plate has much less granulation. Here it seems that both the spine and spinous process were able to detach immediately from the flat and heavily granulated calyx plate. Category B possibly can be interpreted as a kind of “secondary spine.” Category A can be observed in morphological spine Types 1 and 2, and category B occurs in Types 3–8.

This standardized typing and categorization, which is distributed among the examined Monstrocrinus species as shown in Figure 5, enables the subsequent differential diagnosis of the individual Monstrocrinus species. Species-diagnostic characters include the relative size of the calyx, calyx plate sculpturing, presence, or absence of depressions at calyx plate triple junctions, spine categories, and spine types.

Monstrocrinus securifer Schmidt, Reference Schmidt1941
Figures 2, 3.1, 3.3, 6–8

Reference Schmidt1941

Monstrocrinus securifer Schmidt, p. 214–217, fig. 60a–c, pl. 16, figs. 1–7.

Reference Ubaghs, Moore and Teichert1978b

Monstrocrinus securifer; Ubaghs, p. T428, T429, fig. 237a, b.

Reference Le Menn1990

Monstrocrinus securifer; Le Menn, p. 156, fig. 3d.

Reference Le Menn1990

Monstrocrinus aliformis Le Menn, p. 151–153, 156, figs. 1a, b, 3c.

Reference Hauser2012

Monstrocrinus securifer; Hauser, p. 1–4, text-figs. 4–6 (non text-fig 3).

non Reference Hauser2012

Monstrocrinus granosus or Acanthocrinus sp.; Hauser, p. 4, text-fig. 6, no. 2a (= holotype of M. securifer).

Figure 7.

Recast paratype of Monstrocrinus securifer Schmidt, Reference Schmidt1941 (no IGPB-SCHMIDT, W.E.-18c) from the uppermost section of the Emsian Orthocrinus Beds (Polygnathus costatus patulus Conodont Biozone) of the former brick factory in the Osterbachtal, northwest of Olpe-Lütringhausen (administrative district Arnsberg, Sauerland, North Rhine–Westphalia, Germany). (1, 2) Internal aboral view of isolated base of a calyx, showing narrow stem axial canal impression (white arrows), which Schmidt mistakenly interpreted as closed (see Schmidt, Reference Schmidt1941, pl. 16, fig. 3). Scale bars = 1 cm.

Figure 8.

Calcite-preserved spines (1–9) and isolated calyx plates (10–12) of Monstrocrinus securifer Schmidt, Reference Schmidt1941, from the Lauch Formation (Polygnathus costatus partitus to lowermost P. costatus costatus Conodont biozones) of the lower Eifelian of the Eifel synclines, Germany; (1, 4–12) are from the “Eschfelder Seifen,” southeast of Dollendorf, north-northwest of Leudersdorf, North Rhine–Westphalia; (2, 3) are from the northern Ahbach Valley, north-northeast of Üxheim–Ahütte, Rhineland–Palatine). (1–3) Type 3 spines (T3); (4) subtype 4b spine (T4b); (5) type 6 spine (T6); (6, 7) type 7 spines (T7); (8, 9) type 8 spines (T8); (10, 11) isolated calyx plates with “Category B” transitions between the proximally positioned calyx plates and the distally projecting end of the spines (“secondary spines,” not preserved). The spine attachment shows eight-shaped concavities. Scale bars = 1 cm.

Figure 9.

Recast holotype of Monstrocrinus granosus Schmidt, Reference Schmidt1941 (no. SMF XXIII 113a) from the upper Emsian Mandeln Formation (Polygnathus serotinus Conodont Biozone) of Dietzhölztal–Mandeln in the Lahn–Dill district in central Hesse, north-northeast of Dillenburg. (1) Strongly disarticulated crown with longer part stem in matrix (until the present study, the stem was not interpreted as belonging to the individual); (2) detailed view, showing remains of spine types 1, 2, and 7 (T1, T2, T7) and granulated calyx plates. Scale bars = 3 cm in (1) and 1 cm in (2).

Figure 10.

Lateral view of the cast of the most complete known Monstrocrinus (no. NHMMZ PWL 2021/6145-LS), M. granosus Schmidt, Reference Schmidt1941, from the uppermost section of the Emsian Orthocrinus Beds (Polygnathus costatus patulus Conodont Biozone) of the former brick factory in the Osterbachtal, northwest of Olpe-Lütringhausen (administrative district Arnsberg, Sauerland, North Rhine–Westphalia, Germany). The specimen in matrix shows a longer part of stem, partly articulated spines, especially spine types 1 and 7 (T1 and T7), which are well preserved, and brachials preserved. The specimen shows evidence of non-lethal predation of its arms in which the distal portions are narrower than the proximal arms. Similarly, in two rays on the right portion of the organism, the free arm bifurcation is lower than in other arms, and the arms above the bifurcation are narrower. Scale bar = 3 cm.

Types

Holotype: mold of an isolated calyx with rudimentarily preserved spines in matrix, no. IGPB-SCHMIDT, W.E.-18a (recast and re-illustrated in Fig. 6), original of Schmidt (Reference Schmidt1941, pl. 16, figs. 2a, b). Paratype: mold of an isolated base of a calyx in matrix, no. IGPB-SCHMIDT, W.E.-18c (recast and re-illustrated in Fig. 7), original of Schmidt (Reference Schmidt1941, pl. 16, fig. 3).

Emended diagnosis

Monstrocrinus with a relatively large calyx, smooth plate sculpturing, shallow depressions at calyx plate triple junctions, spine categories (A, spine that is physically part of a calyx plate; B, spine articulated with calyx plate); spine types (1, tapering point; 3, narrow paddle shaped; 4, broad paddled shape; 6, bifurcating; 7, forked; 8, strongly asymmetrical with spines on outer margin).

Occurrence

The locus typicus of M. securifer is the former brickworks mine (slopes north, east, and south of the former brick factory, at UTM: 51°02′22.73″N, 7°51′51.02″E) in the Osterbachtal on today's federal road B54, northwest of Olpe-Lütringhausen (administrative district Arnsberg, Sauerland, North Rhine-Westphalia, Germany). The classic site is located at the southeastern flank of the Middle Devonian Attendorn–Elspe Double Syncline in the transition to the Lower Devonian Siegen Anticline and stratigraphically belongs to the uppermost section of the Emsian (Lower Devonian) Orthocrinus Beds (Polygnathus costatus patulus Conodont Biozone). Additional specimens described by Schmidt (Reference Schmidt1941) are from the abandoned “Waukemicke Quarry” (Olpe-Wauckemicke); from several fossil localities near Olpe-Oberveischede; and from the fossil localities at the “Siele Farmyard” (between Olpe-Lütringhausen and Olpe-Waukemicke). Schmidt also mentioned M. securifer remains from localities outside Olpe (Bad Laasphe–Feudingen in the Siegen–Wittgenstein district in North Rhine–Westphalia and the “Old Paper Mill Haiger Hut,” NE-Haiger in the northern part of the Lahn–Dill district in central Hesse, Germany).

Additional material studied in the course of this work is from two outcrops within the Eifel synclines. The first locality is the northern embankment at the “Eschfelder Seifen” on the southwestern flank of the Middle Devonian Ahrdorf Syncline, in the transition area to the Lower Devonian Wiesbaum Anticline (southeast of Dollendorf, NNW of Leudersdorf, North Rhine–Westphalia; UTM: 50°21′45.62″N, 6°43′44.14″E). The second location is in the northern Ahbach Valley, on the north-northeastern flank of the Middle Devonian Hillesheim Syncline, in the transition area to the Lower Devonian Hoffeld Anticline (north-northeast of Üxheim–Ahütte, Rhineland–Palatinate; UTM: 50°20′56.25″N, 6°46′35.71″E) and stratigraphically belongs to the Lauch Formation (Polygnathus costatus partitus to lowermost P. costatus costatus Conodont biozones) of the lower Eifelian.

Because “M. aliformis” sensu Le Menn, Reference Le Menn1990 is treated herein as a subjective junior synonym of M. securifer, the species also occurs in the upper Emsian part of the Pena Negra Formation, northeast of the municipality of Loscos in the province of Teruel, Aragon, Spain.

Emended description

Calyx medium in size, medium to high globe-shaped calyx with a shallow basal concavity, calyx height:width ratio 1.25; depressions at calyx plate triple junctions present; plate sculpturing around spine bases smooth. Infrabasal plates confined to basal concavity, not visible in lateral view; five infrabasal plates. Five basal plates form part of calyx base and proximal portion of the calyx vertical wall. Radial circlet with ten plates (all radial plates alternate with interradial plates); presumably five radial plates, large, hexagonal, approximately as high as wide, with broad plications that connect to like plications on adjoining plates. Calyx plates with various long spines including spine categories A (spine that is physically part of a calyx plate) and B (spine articulated with calyx plate), and spine types 1 (tapering point), 3 (narrow paddle shaped), 4 (broad paddled shape), 6 (bifurcating), 7 (forked), and 8 (strongly asymmetrical with spines on outer margin). Proximal regular interradial plates large, approximately the same size as radial plates. First interradial plate higher than wide. CD interray not known. Fixed brachials present but the number is unknown, median ray ridges absent. Tegmen and free arms unknown. Column shape presumably circular, nodals wider than internodals, pentalobate lumen.

Remarks

Re-examination of the historical type material of Schmidt (Reference Schmidt1941) revealed that the base of the calyx of Monstrocrinus securifer has a stem attachment with a central pentalobate axial canal, which confirms that the M. securifer crown was attached to a column as an adult (see Figs. 6.1, 6.3, 7). Thus, a free-living life mode of a passively rolling or drifting crinoid is refuted, and the type species is reinterpreted as an attached, stalked crinoid.

The longest spine of M. securifer examined by us is 7.5 cm long, with the base missing (Fig. 8.8). So, it was originally about 8.0 cm long. Our measurements show that the largest-known calyxes (without preserved spines) have at least 4.0 cm in equatorial cross-section. If this calyx is now placed between two of our approximately 8.0-cm long spines on the equatorial plane, the result is a maximum total diameter of a calculated adult calyx of 20.0 cm. This value would probably be somewhat lower (~15 cm) if the spines were slightly inclined in the aboral direction. The ratio of the maximum calyx diameter with preserved spines to maximum crown length (calyx with arms) is at least 1:1. On this basis, we calculated total crown height of 40.0 cm (or 30.0 cm with slightly aborally inclined spines), as well as a truly “monstrous” fan when the arms were deployed in a feeding position.

Monstrocrinus securifer is distinguished from other species because it has a relatively large calyx, smooth calyx plate sculpturing, and shallow depressions at calyx plate triple junctions. It also had spine categories A (spines that are physically part of a calyx plate) and B (spine articulated with calyx plate), and the following spine types: (1) tapering point, (3) narrow paddle shaped, (4) broad paddled shape, (6) bifurcating, (7) forked, and (8) strongly asymmetrical with spines on outer margin. In contrast, M. granosus has a relatively small calyx, fine granulose calyx plate sculpturing, and shallow depressions at calyx plate triple junctions are absent. It also had spine categories A (spines that are physically part of a calyx plate) and B (spines articulated with calyx plate), and the following spine types: (1) tapering point, (2) blunt spine, (6) bifurcating, and (7) forked. The morphology of the calyx in M. incognitus is poorly preserved, but diagnostic characters that are known include smooth calyx plate sculpturing, spine categories A (spine that is physically part of a calyx plate) and B (spines articulated with calyx plate), and spine types (1) tapering point, (4) broad paddle-shaped spine, and (5) flat high spine.

Monstrocrinus granosus Schmidt, Reference Schmidt1941
Figures 3.2, 9–12

Reference Schmidt1941

Monstrocrinus granosus Schmidt, p. 217–218, text-figs. 61a, 61b1, 61b2, 61c, 61d, 61e1, 61e2.

Reference Le Menn1990

Monstrocrinus granosus; Le Menn, p. 151, 153–154, 156 (non fig. 3b).

Figure 11.

Digitally cropped view of the specimen shown in Figure 10. Scale bar = 3 cm.

Figure 12.

(1–4) Detail views of the specimen from Figures 10 and 11. (1) Lateral view of the spined calyx with well-preserved spine type 1 (T1). (2–4) Casts of the counter plates: (2) lateral view of two well-preserved spines of types 6 and 7 (T6, T7); (3) lateral view of part of the arms and calyx, showing spine type 1 (T1); (4) lateral view of spine types 1 and 7 (T1, T7). Scale bars = 2 cm in (1) and 1 cm in (2–4).

Holotype

Mold of a disarticulated crown with longer stem part in matrix, no. SMF XXIII 113a (recast and re-illustrated in Fig. 9), original of Schmidt (Reference Schmidt1941, p. 217, text-figs. 61.a, 61.b1, 61.b2, 61.c, 61.d, 61.e1, 61.e2).

Emended diagnosis

Monstrocrinus with a relatively small calyx; fine granulose calyx plate sculpturing; shallow depressions at calyx plate triple junctions absent; spine categories (A) spine that is physically part of a calyx plate and (B) spine articulated with calyx plate; and spine types (1) tapering point, (2) blunt spine, (6) bifurcating, and (7) forked.

Occurrence

The species occurs in the upper Emsian Mandeln Formation (Polygnathus serotinus Conodont Biozone) within the “iron-shed greywacke schist” in the “Old Municipality Quarry” at the northern Hauberg Hill in Dietzhölztal–Mandeln in the Lahn–Dill district in central Hesse (Germany), north northeast of Dillenburg (type locality at UTM: 50°51′22.52″N, 8°20′51.41″E). The examined material is from the locus typicus of the type species M. securifer, the former brickworks mine (slopes north, east, and south of the former brick factory, at UTM: 51°02′22.73″N, 7°51′51.02″E) in the Osterbachtal on today's federal road B54, northwest of Olpe-Lütringhausen (administrative district Arnsberg, Sauerland, North Rhine–Westphalia, Germany). The classic site is located at the southeastern flank of the Middle Devonian Attendorn–Elspe Double Syncline in the transition to the Lower Devonian Siegen Anticline and stratigraphically belongs to the uppermost section of the Emsian (Lower Devonian) Orthocrinus Beds (Polygnathus costatus patulus Conodont Biozone).

Emended description

Calyx small in size, medium globe-shaped calyx with a shallow basal concavity, calyx height:width ratio 1.25; depressions at calyx plate triple junctions absent; finely granulose calyx plate sculpturing on plates and may be on adaxial portion of spines. Infrabasal plates confined to basal concavity, not visible in lateral view; presumably five infrabasal plates, pentagonal. Five basal plates form part of calyx base and proximal portion of the calyx vertical wall. Radial circlet with ten plates (all radial plates alternate with interradial plates); radial plates large, presumably five, hexagonal, approximately as high as wide, lacking broad folds. Calyx plates with long spines on at least basal plates, radial plates, proximal interradial plates, and some fixed brachials; spine categories (A) spine that is physically part of a calyx plate and (B) spine articulated with calyx plate; spine types (1) tapering point, (2) blunt spine, (6) bifurcating, and (7) forked. Proximal regular interradial plates large, hexagonal (more distal regular interray plates not known). First interradial plate in regular interrays approximately the same size as radial plates and as high as wide. CD interray not known. Fixed brachials present but the number is unknown, median ray ridges absent. Tegmen unknown. Free arms presumably 20; high; one isotomous division; initially project obliquely downward, then abaxially, and finally obliquely upward. Proximal free brachials subrectangular, free brachials after division sharply convex, all brachials chisel biserial. Pinnules very long and slender, proximal pinnulars rectangular, higher than wide. Column circular, pentalobate lumen; nodal–internodal pattern N1; nodals wider than internodals. Proportions of different features on columnal facets: 12% narrow crenularium, 52% aereola, 8% perilumen, 28% lumen.

Remarks

After recasting the holotype of Monstrocrinus granosus Schmidt, Reference Schmidt1941 (no. SMF XXIII 113a), which was kindly provided by the Senckenberg Research Institute and Natural History Museum Frankfurt on the Main (Germany), important morphological characters came to light that were not recorded in the original description (compare Schmidt, Reference Schmidt1941, p. 217, figs. 61a–e with our Fig. 9). The holotype of M. granosus is far more complete than previously reported. It is a highly disarticulated crown embedded together with an associated long part of the stem (Fig. 9). In addition, further details of the spine morphology could be recorded. The previously unappreciated knowledge about the spine morphology led to an incorrect interpretation of a granosus spine by Le Menn (Reference Le Menn1990, p. 156, Fig. 3b). The latter author understood the prong-shaped extension of Schmidt's fig. 61b2 (1941, p. 217) as pointing proximally toward the calyx plate. In fact, it is not a backward-pointing prong, but a distally tapering bifurcation (see Schmidt, Reference Schmidt1941, p. 217).

Whereas the holotype of M. granosus was found within the upper Emsian Mandeln Formation of the “Old Municipality Quarry” (Paleontological Ground Monument of the Federal State of Hesse, no. “Mandeln 991″) at the northern Hauberg Hill in Dietzhölztal–Mandeln in the Lahn–Dill district in central Hesse (Germany), the material examined by us comes from the uppermost section of the Emsian (Lower Devonian) Orthocrinus Beds of the M. securifer type locality, the former brickworks mine northwest of Olpe-Lütringhausen (administrative district Arnsberg, Sauerland, North Rhine-Westphalia, Germany). To date, this locality in Germany is the only fossil site where both species co-occur.

It should be noted that the endoskeletons of M. granosus are consistently smaller in size than in the comparatively larger type species M. securifer. Monstrocrinus granosus is compared to other species of Monstrocrinus in the remarks section of M. securifer.

Noteworthy is that the distal portion of some distal arms are of variable widths. Also, the position of the free arm division is variable. One hypothesis is that these differences among free arms were a consequence of non-lethal predation on this specimen.

Types

The type material of M. incognitus is housed in the paleontological collection of the Departamento de Geologia e Paleontologia do Museu Nacional, Universidade Federal do Rio de Janeiro (UFRJ), Brazil, under institutional abbreviation no. MN8277-Id. (holotype) and nos. MN8277-Ia, and MN8277-Ib (paratypes).

Emended diagnosis

Monstrocrinus with calyx size unknown; smooth calyx plate sculpturing; calyx plate triple junctions character unknown; spine categories (A) spine that is physically part of a calyx plate and (B) spine articulated with calyx plate; and spine types (1) tapering point, (4), broad paddle-shaped, (5), flat, high fan.

Occurrence

Monstrocrinus incognitus was reported from the western edge of the Parnaíba Basin from three outcrops (Fazenda Encantada II, Estância Cantilena, and Mirante Taquaruçu) in the district of Taquaruçu (Municipality de Palmas, state of Tocantins, Brazil), and, according to Scheffler et al. (Reference Scheffler, Dias-Da-Silva, Gama, Da Fonseca and Fernandes2011), occurs in outcrops positioned near the base of the middle to upper Eifelian Pimenteira Formation.

Remarks

Monstrocrinus incognitus is characterized in particular by the distinctive type 4a spines, which have a shorter length and a generally shorter and taller neck compared to those in M. granosus and M. securifer. This feature clearly justifies designation of a distinct species.

Scheffler et al. (Reference Scheffler, Fernandes and Da Fonseca2006, p. 238, fig. 3A–3E) described “Monstrocrinus securifer” from the middle Eifelian Maecuru Formation along the Maecuru River in the northwestern part of the State of Pará in Brazil. In our opinion, this material belongs either to M. incognitus or to another species of Monstrocrinus (compare Fig. 3.5 and 3.6 of the present study). Therefore, it could be possible that the species diversity of Monstrocrinus in Brazil is higher than currently known (further investigations are necessary).