# Systematics, morphology, and appendages of Anacheirurus (Pilekiinae, Trilobita) from the Fezouata Shale and the early diversification of Cheiruridae

Francesc Pérez-Peris, Lukas Laibl, Muriel Vidal, Allison C Daley

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Francesc Pérez-Peris, Lukas Laibl, Muriel Vidal, Allison C Daley. Systematics, morphology, and appendages of Anacheirurus (Pilekiinae, Trilobita) from the Fezouata Shale and the early diversification of Cheiruridae. Acta Palaeontologica Polonica, 2021, 66 (4), pp.857-877. 10.4202/app.00902.2021. hal-05251522

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# Systematics, morphology, and appendages of an Early Ordovician pilekiine trilobite *Anacheirurus* from Fezouata Shale and the early diversification of Cheiruridae

FRANCESC PÉREZ-PERIS, LUKÁŠ LAIBL, MURIEL VIDAL, and ALLISON C. DALEY

<figure><img src="image_2.png" /></figure>

Pérez-Peris, F., Laibl, L., Vidal, M., and Daley, A.C. 2021. Systematics, morphology, and appendages of an Early Ordovician pilekiine trilobite *Anacheirurus* from Fezouata Shale and the early diversification of Cheiruridae. *Acta Palaeontologica Polonica* 66 (4): 857–877.

Pilekiines are the earliest diverging members of the successful trilobite family Cheiruridae. The pilekiine genus *Anacheirurus* is characterized by sub-quadratic to sub-oval glabella, pitted genae, and a distinct trunk with elongated pleural spines in its posterior part. *Anacheirurus adserai* is a common component of the Fezouata Shale (Lower Ordovician, Morocco), where it was initially included into several species of the genus *Lehua*. This assignment and taxonomic over-splitting created confusion, overestimated cheirurid diversity at this locality, and simultaneously underestimated morphological variability within *A. adserai*. In this contribution we examine new material of *A. adserai* from the Fezouata Shale, clarifying its morphology and systematics. A detailed re-description of the species shows that *Anacheirurus* is distinct from *Lehua*, the latter being a more derived member of Cheiruridae. The comparison of *Anacheirurus* with other pilekiines shows that morphological variability within this subfamily is mostly constrained to the trunk region. Exceptionally preserved specimens of *A. adserai* from the Fezouata Shale show details of appendages, revealing the endopodite and exopodite morphologies in early members of Cheiruridae. The endopodite of *A. adserai* is unique among trilobites in possessing comparatively longer distal podomeres 5 and 6, but otherwise, it has the same general morphology as other described trilobite endopodites. The exopodite morphology of *A. adserai* shows characters typical of some Cambrian species but differs in several aspects from those known in post-Cambrian taxa. It is concluded that trilobite exopodite morphology was probably more variable than the endopodite morphology, which remains rather conservative across different taxa. Morphological diversity of trilobite exopodites in post-Cambrian taxa might be related to ecological escalations during the Ordovician biodiversification and the transition between Cambrian and Ordovician trilobite faunas.

**Key words:** Trilobita, Cheiruridae, Pilekiinae, biodiversification, ecology, endopodite, exopodite, Ordovician, Morocco.

Francesc Pérez-Peris [francesc.perezperis@unil.ch]; ORCID: 0000-0002-4526-9308], Allison C. Daley [allison.daley@unil.ch]; ORCID: 0000-0001-5369-5879], Institute of Earth Sciences, University of Lausanne, Géopolis, CH-1015 Lausanne, Switzerland.

Lukáš Laibl [lukaslaibl@gmail.com]; ORCID: 0000-0001-9049-3811], Czech Academy of Sciences, Institute of Geology, Rozvojová 269, 165 00 Prague 6, Czech Republic; Institute of Geology and Palaeontology, Faculty of Science, Charles University, Albertov 6, Prague, 12843, Czech Republic.

Muriel Vidal [muriel.vidal@univ-brest.fr]; ORCID: 0000-0003-3699-2083], Université de Brest, CNRS, IUEM Institut Universitaire Européen de la Mer, UMR 6538 Laboratoire Géosciences Océan, Place Nicolas Copernic, 29280 Plouzané, France.

Received 4 May 2021, accepted 9 September 2021, available online 25 November 2021.

Copyright © 2021 F. Pérez-Peris et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License (for details please see http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

## Introduction

With 440 Ordovician species, the family Cheiruridae Hawle and Corda, 1847, is one of the most diverse trilobite families during the Ordovician (Adrain 2013). The first record of Cheiruridae comes from Furongian (late Cambrian) of Siberia (Rosova 1960), while the last members went extinct

during Givetian (Middle Devonian; Lane 1971; Přibyl et al. 1985; Feist 1991; Adrain 2013). Cheiruridae is currently subdivided into eight subfamilies (Acanthoparyphinae, Cheirurinae, Cyrtometopinae, Deiphoninae, Eccoptochilinae, Heliomerinae, Pilekiinae, and Sphaerexochinae; Adrain 2013). Their validity is still under discussion and only Acanthoparyphinae, Deiphoninae, Sphaerexochinae, and
Eccoptochilinae have been subjected to phylogenetic analy-
ses (Adrain 1998; Congreve and Lieberman 2010, 2011; Gapp
et al. 2012). The subfamily Pilekiinae Sdzuy, 1955, is strati-
graphically the oldest group within cheirurid trilobites, with
their record going as far back as Furongian (Rosova 1960),
and surviving until the Darriwilian (Middle Ordovician;
Fortey 1980; Edgecombe et al. 1999). Pilekiinae is the only
cheirurid subfamily present in the Tremadocian strata and
has a worldwide distribution. This subfamily represents one
or several early-diverging lineages within Cheirurina (Reed
1896; Kobayashi 1934; Ross 1951; Harrington in Moore
1959; Lane 1971; Demeter 1973; Přibyl et al. 1985; Jell 1985;
Peng 1990; Lee and Chatterton 1997) making them cru-
cial for understanding the early evolutionary history and
Ordovician biodiversification of Cheirurina.

The trilobite-rich sediments of the Fezouata Shale strati-
graphically range from Tremadocian to Floian, Lower
Ordovician (Lefebvre et al. 2018), and offer a perfect oppor-
tunity to explore the first steps of the Ordovician biodiver-
sification of trilobites, including cheirurids. Of the 26 trilo-
bite species belonging to 21 different genera that have been
recorded in the Fezouata Shale (Martin et al. 2016b), one
of the most common is the pilekiid *Anacheirurus adserai*
(Vela and Corbacho, 2007). The species was originally de-
scribed as *Lehua adserai* by Vela and Corbacho (2007), and
during the following years several other species of *Lehua*
Barton, 1915, from the same locality were erected (Vela
2007; Corbacho 2008; Corbacho and Vela 2011). Such an
approach resulted in taxonomic over-splitting, with a total
of seven species erected and, therefore, an overestimation of
cheirurid diversity in Fezouata Shale. In their study of the
trilobite assemblages from Fezouata, Martin et al. (2016b)
found only one species of the taxon belonging to *Lehua*
and assigned it to the *Anacheirurus* Reed, 1896. This ap-
proach was based on the work done by Whittard (1967), who
considered *Lehua* as a junior synonym of *Anacheirurus*.
However, several other authors disagreed and continued
to consider them as two different genera (e.g., Lane 1971;
Přibyl et al. 1985). Herein, we describe new material and ad-
vocate the generic assignment of Martin et al. (2016b), while
also presenting a more detailed discussion of the differences
between *Lehua* and *Anacheirurus*.

Another important aspect of the Fezouata Shale is that
some levels preserve non-biomineralized fossils and body
parts (e.g., Van Roy et al. 2010, 2015a, b; Saleh et al. 2020a,
b). Among trilobites and trilobitomorphs, not only hard bio-
mineralized parts are preserved, but also appendages and di-
gestive structures are found (Martin et al. 2016b; Gutiérrez-
Marco et al. 2017; Pérez-Peris et al. 2021). This offers a
unique opportunity to understand the morphological diver-
sification of trilobite soft parts during the Ordovician bio-
diversification. Unlike the dorsal parts of the exoskeleton,
trilobite appendages were only slightly sclerotized (Hughes
2003) and for that reason, they are extremely rare in the fossil
record. One of the first reports of trilobite appendages was
made by Billings (1870) who found appendages in the genus

*Isotelus* Dekay, 1824. Since then, numerous works have described appendages (e.g., Beecher 1893; Walcott 1918; Raymond 1920; Broili 1930; Størmer 1939, 1951; Seilacher 1962; Bergström 1972, 1973; Stürmer and Bergström 1973; Cisne 1975, 1981; Whittington 1975, 1980; Whittington and Almond 1987; Bruton and Haas 1999; Gutiérrez-Marco et al. 2017; Holmes et al. 2020) in several trilobite species (see Zeng et al. 2017: table 1 for a comprehensive summary). Although the general appendage morphology is comparatively well known, several questions remain unresolved. From all the work carried out on trilobite appendages during more than one century, there is information available for only about 30 trilobite species, from more than 19 000 erected species (cf. Adrain 2011; Zeng et al. 2017; Holmes et al. 2020). Moreover, 18 of the species with appendages preserved are known solely from Cambrian Konservat-Lagerstätten with Burgess Shale-type preservation of carbonaceous compressions (Butterfield 2003; Gaines et al. 2008; Daley et al. 2018). Data from post-Cambrian taxa are much rarer, as they were usually preserved under different conditions than during the Cambrian (Butterfield 1995; Daley et al. 2018). *Ceraurus pleurexanthemus* Green, 1832, from the Trenton Group (Upper Ordovician, New York State, USA) is the only member of the family Cheiruridae with appendages preserved in the fossil record (Størmer 1939, 1951), despite the huge diversity of the family. *C. pleurexanthemus* is also one of the few trilobites from the Ordovician with a more complete appendage record, together with *Triarthrus eatoni* (Hall, 1838) and *Cryptolithus bellulus* (Ulrich, 1879). This knowledge gap exists not only for cheirurid trilobites but for all Ordovician trilobites in general. New information about trilobite appendages is required to understand the post-Cambrian evolution and ecology of the group.

Here, we present a first comprehensive description of the
morphology of the pilekiine *Anacheirurus adserai* from the
Fezouata Shale, based on numerous well-preserved speci-
mens. The late post-embryonic development of this species
is also briefly described. We clarify the taxonomy of *A.
adserai* and describe the morphology of its appendages.
This work provides new insight into the morphological vari-
ability, biodiversification, and appendage evolution within
Pilekiinae, and helps to clarify the early evolutionary steps
of Cheiruridae.

*Institutional abbreviations*.—GMSB, Geological Museum of the Seminary of Barcelona, Spain; JV, Czech Geological Survey, Prague, Czech Republic; MGB, Museum of Natural Sciences of Barcelona, Spain; MGL, Musée cantonal de Géologie de Lausanne, Switzerland; ML, Natural History Museum of Lyon, France; NM L, National Museum, Prague, Czech Republic; YPM, Yale Peabody Museum of Natural History, New Haven, USA.

*Other abbreviations*.—exsag., exsagittal; L1, L2, L3, glabel-
lar lobes one to three; SO, S1, S2, S3, occipital furrow and
glabellar furrows one to three, respectively; sag., sagittal; tr.,
transversal; Tr3, third stage slice of the Tremadocian.
## Geological setting

The Lower Ordovician of the Anti-Atlas region in Morocco belongs to the Outer Feijas Group. The Outer Feijas Group is subdivided into the Lower and Upper Fezouata formations, the Zini Formation, and the Tachilla Formation, and comprise a succession stratigraphically ranging from Tremadocian to lower Darriwilian (Choubert et al. 1947; Destombes et al. 1985). In the Zagora region, the Lower and Upper Fezouata formations are grouped into a single unit called the Fezouata Shale, because the boundary between both units is unclear (Martin et al. 2016b). The Fezouata Shale is an approximately 850 m thick succession composed of argillites with sandy mudstone and siltstone beds (Destombes et al. 1985). The depositional environment facilitated a rapid burial of autochthonous communities in an open shallow marine environment (Martin et al. 2016a), ranging from offshore to the foreshore with a depth range from 50 to 150 m (Vaucher et al. 2016; Martin et al. 2016a).

The Fezouata Shale contains a Burgess Shale-type Konservat-Lagerstätte, the Fezouata Biota, that is renowned for its exceptional preservation of soft, cuticulized, and lightly sclerotized parts of a highly diverse marine biocenosis (Van Roy et al. 2010, 2015a, b: Saleh et al. 2020b). The Fezouata Biota provides a critical link between the Cambrian Explosion and the Great Ordovician Biodiversification Event, due to its temporal position between both events (Servais et al. 2010; Landing et al. 2018; Servais and Harper 2018). Exceptional preservation in the Fezouata Shale is restricted to two intervals (Martin et al. 2016a; Lefebvre et al. 2018), the lower of which is about 70 m thick and situated 260–330 m above the Cambrian/Ordovician contact, and the second of which is about 50 m thick and 570–620 m above the Cambrian/Ordovician contact. The lower interval with exceptional preservation is situated mostly within the *Araneograptus murrayi* Zone and lowermost parts of the *Hunnegraptus copiosus* Zone, which both correspond to the third slice of the Tremadocian stage (or Tr3, see Gutiérrez-Marco and Martin 2016; Lefebvre et al. 2018). This age is further corroborated by acritarchs and conodonts (Lehnert et al. 2016; Nowak et al. 2016). The upper interval with exceptional preservation most likely belongs to the ?*Baltograptus jacksoni* Zone, which is of Floian age (Lefebvre et al. 2018), but is stratigraphically less well understood.

## Material and methods

Material examined includes over 50 specimens of *Anacheirurus adserai* from the Fezouata Shale. All specimens come from the lower fossiliferous interval of the *Araneograptus murrayi* Zone (upper Tremadocian, Lower Ordovician). Specimens are held at the Musée cantonal de Géologie de Lausanne, Switzerland, the University of Lyon (France), the Natural History Museum of Lyon (France), the

University of Brest (France), and the Yale Peabody Museum of Natural History (New Haven, USA). Figured specimens are held in the Musée cantonal de Géologie de Lausanne, Switzerland (MGL 102153, 102170, 102172, 102179, 102225, 103863, 104146, 104533), Yale Peabody Museum of Natural History (YPM 226573, 517074, 522182, 525125, 530933) and the Natural History Museum of Lyon (ML20-269198). Specimens of *Lehua vinculum* (Barrande, 1852) from the Dobrotivá Formation (upper Darriwilian–lowermost Sandbian, Middle–Upper Ordovician) of the Czech Republic that are examined and figured here are held in the National Museum, Prague (NM L 19066 and 19075) and the Czech Geological Survey (JV 1607).

Specimens were photographed with a Canon EOS 800D camera with an associated CANON MACRO LENS MP-E 65 mm 1:2.8 1-5Xlens. The lens was equipped with a polarizing filter to reduce reflections, and a second polarizer on the light source created crossed polarization to increase contrast. Specimens were photographed with low-angle NW lighting or high light from directly above the specimens. Some specimens were covered by ammonium chloride before photography, to enhance their topography. Specimens MGL 102172, 102225, and 103863, were photographed submerged in ethanol to improve the appendages contrast. The images were processed in Adobe Photoshop CC 19.0, to enrich brightness, contrast, shadows, highlights, and saturation. Line drawings were made directly from photographs using Adobe Illustrator CC 22.01, like a digital camera lucida (Antcliffe and Brasier 2011).

## Systematic palaeontology

Order Phacopida Salter, 1864

Suborder Cheirurina Harrington and Leanza, 1957

Family Cheiruridae Hawle and Corda, 1847

Subfamily Pilekiinae Sdzuy, 1955

*Genera included.*—*Anacheirurus* Reed, 1896, *Chashania* Lu and Sun in Zhou et al., 1977, *Courtessolium*? Přibyl and Vaněk in Přibyl et al. 1985, *Emsurina* Sivov in Egorova et al., 1955, *Eocheirurus* Rozova, 1960, *Koraipsis* Kobayashi, 1934, *Landyia* Jell, 1985, *Macrogrammus* Whittard, 1966, *Metapilekia* Harrington, 1938, *Metapliomerops* Kobayashi, 1934, *Parapilekia* Kobayashi, 1934, *Pilekia* Barton, 1915, *Pseudopliomera* Lu and Qian in Yin and Li, 1978, *Seisonia* Kobayashi, 1934, *Sinoparapilekia* Peng, 1990, *Tesselacauda* Ross, 1951, *Tienshihuia* Lu in Lu et al., 1976, *Victorispina* Jell, 1985, *Yinaspis* Zhang and Fan, 1960.

*Emended diagnosis.*—Cheiruridae with thoracic pleura divided into anterior and posterior bands by a deep, long (tr.) pleural furrow; broad (tr.) proximal part of thoracic pleura with fulcrum situated distally 2/3 from the axis; pygidium with at least two first pleural tergites displaying a deep
pleural furrow that divide the pleura into anterior and posterior bands, as in the thoracic pleura.

*Remarks*.—Pilekiinae has been considered as a subfamily of Pliomeridae (Harrington in Moore 1959; Vaněk 1965; Demeter 1973; Peng 1984; Mergl 1984), as a subfamily of Cheiruridae (Fortey 1980; Přibyl et al. 1985; Edgecombe et al. 1999; Adrain 2013; Adrain and Karim 2019) or as a separate family Pilekiidae (Sdzuy 1955; Whittington 1961; Jell 1985; Peng 1990; Lee and Chatterton 1997; Ebbestad 1999; Jell and Adrain 2002; Pärnaste 2004; Mergl 2006). In this paper, we consider pilekiids as a subfamily of Cheiruridae. This suggestion is based on Adrain and Karim (2019), who have shown that pilekiids and the rest of cheirurids share a similar morphology of the rostral plate and the hypostome.

## Genus *Anacheirurus* Reed, 1896

*Type species:* *Cheirurus* (Eccoptochile) *frederici* Salter, 1864; Tremadocian Slates; Wales, upper Tremadocian, Upper Ordovician.

*Species included:* *Anacheirurus* *frederici* (Salter, 1864); *Anacheirurus* *adserai* (Vela and Corbacho, 2007); *Anacheirurus* *nanus* (Mergl, 1984); *Anacheirurus* *bohemicus* (Růžička, 1926); *Anacheirurus? plutonis* Bulman and Rushton, 1973; *Anacheirurus? atecae* (Hammann, 1971); *Anacheirurus? sougyi* (Destombes in Destombes et al., 1969).

*Diagnosis*.—A genus of Pilekiinae with glabella sub-quadrate to sub-oval in shape, with smooth surface; pleura deeply furrowed, with posterior band extended distally in a spine of variable length; posterior tergites of the trunk bear elongated spines directed backward; pygidium with two to three axial rings, and with one to three pair of pygidial spines; pygidial pleurae furrowed with a deep furrow as in the thoracic pleurae, pygidial spines oriented mainly backward.

*Remarks*.—*Anacheirurus* has been recognized as bearing three pairs of pygidial spines (Bulman and Rushton 1973; Fortey 1980; Peng 1990; Mergl 2006). However, the type species of the genus, *Anacheirurus* *frederici*, probably bears only two pairs of pygidial pleural spines (Lane 1971). *Anacheirurus* *adserai*, a species otherwise morphologically nearly identical to *A. frederici*, bears only one pair of pygidial pleural spines. The number of pleural spines allocated within pygidium seems to be a highly variable character in early members of Cheiruridae, and consequently of little use when defining genera or even higher taxa. On the other hand, both *A. frederici* and *A. adserai* share the same overall morphology of the trunk, with the last seven pairs of spines elongated. Considering the uniqueness of this character within Pilekiinae and morphological similarity between these two species, it seems likely they are both form a monophyletic group. For that reason, we suggest using these elongated posterior spines as a diagnostic character of *Anacheirurus*, being aware this might restrict the original concept of the genus (and consequently the number of species assigned to it). Except for *A. frederici* and *A. adserai*, the remaining species assigned to *Anacheirurus* lack the thoracic information. We decided to keep them within the genus until the thoracic information is available.

## *Anacheirurus adserai* (Vela and Corbacho, 2007)

Figs. 1, 2A, B, 3–7.

?1969 *Parapilekia sougyi* n. sp.; Destombes in Destombes et al. 1969: 192, text-fig. 6, pl. 4: 7–11.

1985 *Parapilekia* sp.; Destombes in Destombes et al. 1985: 189.

2006 *Parapilekia* sp.; Destombes 2006: pl. 2: 5.

2007 *Anacheirurus* *frederici* (Salter, 1864); Vela 2007: 27.

2007 *Lehua* *adserai* n. sp.; Vela and Corbacho 2007: text-figs. 3–6.

2007 *Lehua* *corbachoi* n. sp.; Vela 2007: 28, text-figs. 2, 3.

2007 *Lehua* *colli* n. sp.; Vela 2007: 29, text-fig. 4.

2007 *Lehua* *ponti* n. sp.; Vela 2007: 30, text-figs. 5–7.

2008 *Anacheirurus* *frederici* (Salter, 1864); Corbacho 2008: 4.

2008 *Lehua* *adserai* Vela and Corbacho, 2007; Corbacho 2008: 4.

2008 *Lehua* *corbachoi* Vela, 2007; Corbacho 2008: 4.

2008 *Lehua* *colli* Vela, 2007; Corbacho 2008: 4.

2008 *Lehua* *ponti* Vela, 2007; Corbacho 2008: 4.

2008 *Lehua* *velai* n. sp.; Corbacho 2008: 5, text-figs. 1–3.

2008 *Lehua* *iannacconnei* n. sp.; Corbacho 2008: 6, text-fig. 4.

2008 *Lehua* *tahirii* n. sp.; Corbacho 2008: 7, text-fig. 7.

2010 *Lehua* *vinculum* (Barrande, 1852); Bonino and Kier 2010: 290, pl. 84: a.

2010 *Lehua* sp.; Bonino and Kier 2010: 290, pl. 84: b.

2010 *Lehua* *corbachoi* Vela, 2007; Bonino and Kier 2010: 290, pl. 84: c.

2010 *Lehua* *velai* Corbacho, 2008; Bonino and Kier 2010: 290, pl. 84: d.

2010 *Lehua* *ponti* Vela, 2007; Bonino and Kier 2010: 290, pl. 84: e.

2011 *Lehua* *adserai* Corbacho and Vela, 2007; Corbacho and Vela 2011: 48, pl. 1: 1; 49, pl. 2: 6.

2011 *Lehua* *corbachoi* Vela, 2007; Corbacho and Vela 2011: 48, 49, pl. 1: 2; pl. 2: 2, 4, 7.

2011 *Lehua* *tahirii* Corbacho, 2008; Corbacho and Vela 2011: 48, 49, pl. 1: 3; pl. 2: 8, 9.

2011 *Lehua* *velai* Corbacho 2008; Corbacho and Vela 2011: 48, 49, pl. 1: 4; pl. 2: 1, 3, 5.

2015 *Lehua* *adserai* Corbacho and Vela, 2007; Van Roy et al. 2015a: 546.

2015 *Lehua* *corbachoi* Vela, 2007; Van Roy et al. 2015a: 546.

2015 *Lehua* *tahirii* Corbacho, 2008; Van Roy et al. 2015a: 546.

2015 *Lehua* *velai* Corbacho, 2008; Van Roy et al. 2015a: 546.

?2015 *Parapilekia* sp.; Van Roy et al. 2015a: 546.

2015 *Lehua* *adserai* Corbacho and Vela, 2007; Valent and Corbacho 2015: 51.

2015 *Lehua* *corbachoi* Vela, 2007; Valent and Corbacho 2015: 51.

2015 *Lehua* *tahirii* Corbacho, 2008; Valent and Corbacho 2015: 51.

2015 *Lehua* *velai* Corbacho, 2008; Valent and Corbacho 2015: 51.

2016 *Anacheirurus* *adserai* (Vela and Corbacho, 2007); Martin et al. 2016b: 149, figs. 2, 3, 5, table 1.

2018 *Lehua* *corbachoi* Vela, 2007; Lebrun 2018: 107, fig. D.

*Type material:* Holotype: GMSB 73845, complete specimen (selected by Vela and Corbacho 2007). Paratype: MGB 46755, complete specimen (selected by Vela and Corbacho 2007).

*Type locality:* Fezouata Shale in the central Anti-Atlas of Morocco, presumably located north of the city of Zagora. The original material doubtfully assigned to the locality "Tanssikhte" (see section Remarks for details).

*Type horizon:* Fezouata Shale, Upper Tremadocian (Tr3) (*Araneograp-
tus* murrayi Zone), Lower Ordovician. The type locality was incorrectly assigned by Vela and Corbacho (2007) stratigraphically to the Upper Fezouata Shale, "lower-middle Arenig" (= Floian age). See section Remarks for details.

*Material*.—Assigned specimens MGL 102153, MGL 102170, MGL 102172, MGL 102179, MGL 102225, MGL 103863, MGL 104146, MGL 104533, YPM 226573, YPM 517074, YPM
<figure><img src="image_3.png" /><figcaption>Fig. 1. Cheirurid trilobite *Anacheirurus adserai* (Vela and Corbacho, 2007) from the Fezouata Shale, *Araneograptus murrayi* Zone, Tremadocian, Lower Ordovician, near Beni Zouli, Zagora Province, Morocco. A. MGL 102179, complete specimen (A₁) and anterior region of the counterpart (A₂); arrow pointing the antennae. B. MGL 102170, close-up of the posterior region of the trunk; arrow pointing the disarticulated pygidium. C. ML20-269198, latex cast of the counterpart. D. YPM 525125, close up of the posterior region of the trunk; arrow pointing the articulation between the thorax and the pygidium. Specimens in A₁ and C coated with ammonium chloride. Scale bars 1 mm.</figcaption></figure>

522182, YPM 525125, YPM530933, ML20-269198. All the material come from the Fezouata Shale, Upper Tremadocian (Tr3), *Araneograptus murrayi* Zone, Lower Ordovician.

*Description*.—*Exoskeleton*: Exoskeleton micropygous (Fig. 1A, B, C), ovoid to sub-ovoid in outline (excluding spines) (Fig. 1A₁, C). The sagittal length of the observed holaspid individuals ranges from 5.6 mm (MGL 101262) to 35 mm

(YPM 522182). Cephalon semi-elliptical in outline, relatively short (sag.), length/width ratio ranges from 1.04 to 0.88. Glabella sub-quadratic in shape, parallel-sided, slightly tapering anteriorly. Anterior glabellar margin bowed anteriorly. Posterior glabellar margin slightly bowed anteriorly medially. Three pairs of well-defined lateral glabellar furrows (Fig. 1C). S1 deeper, longer (tr.), and wider (sag.) than S2 and S3, directed inwards and slightly backwards, adaxially
<figure><img src="image_4.png" /><figcaption>Fig. 2. Cheirurid trilobites *Anacheirurus adserai* (Vela and Corbacho, 2007) from the Fezouata Shale, *Araneograptus murrayi* Zone, Tremadocian, Lower Ordovician, near Beni Zouli, Zagora Province, Morocco (A, B) and *Lehua vinculum* (Barrande, 1852) from the Dobrotivá Formation, upper Darriwilian to lowermost Sandbian, Zaječov-Svatá Dobrotivá, Czech Republic (C-E). A. YPM 522182, part, complete holaspid with hypostome impressed. B. YPM 530933, complete holaspid. C. NM L19066, complete holaspid. D. NM L19075, complete cranidium. E. JV1607, anterior half of an holaspid specimen. Specimens in C-E covered by ammonium chloride.</figcaption></figure>

strongly curved backwards, not connected with the occipital furrow. S2 and S3 sub-parallel, directed inwards and slightly backwards. L1 sub-oval in shape, L2 and L3 rectangular in shape. Frontal lobe wider (tr.) than longer (sag.), with an inverted triangular shape. Occipital ring sub-rectangular in shape, slightly narrower (tr.) than the glabella, longer (sag.) in medial part, tapering distally, the medial part of anterior margin slightly convex anteriorly. Anterior border short (sag.), slightly bowed anteriorly almost transversal. Anterior border furrow narrow (sag.), relatively shallow, of the same depth as the axial furrow. Posterior border furrow long (sag.), deeply incised. Posterior border short (sag.) proximally, expanding (sag.) gradually distally, expanding abruptly beyond the medial region of the fixigenal field, wider at the genal angle, distally curving forward and slightly inward. Lateral border widest (tr.) next to the genal angle, tapering forward. Genal spines developed at a genal angle, relatively long, directed backwards, thick at the base, and tapering backward. Fixigenal field sub-triangular in shape, with narrow (tr.) anterior part triangular in shape and wide (tr.) rectangular posterior part. The anterior part of the fixigenal field crossed by the eye ridge. Librigenal field small with an elongated triangular shape, outer margin convex outwardly. Eye lobe semi-circular in shape, outwardly convex, narrow (Fig. 1A₁).

Fixigenal and librigenal fields densely sculpted by small pits equally distributed around the surface. Small palpebral lobe, elongated, oval in shape, not differentiated from the eye ridge, posterior tip opposite (exsag.) to anterior part of L2. Palpebral furrow deeply incised, narrow, going from the posterior tip of the palpebral lobe through eye ridge to the axial furrow. Eye ridge prominent, directed slightly obliquely forward, reaching the axial furrow on the S3. Cephalic doublure is not preserved.

Proparian facial suture. Anterior branch shorter than posterior, running posteriorly slightly outwardly, lightly curved. Posterior branch mostly transverse, almost perpendicular to the sagittal axis, turning posteriorly abruptly beyond the border furrow.

Conterminant hypostome (Figs. 1A₂, 2A). Anterior part not well preserved. Anterior margin almost transversal (Fig. 2A). Middle body oval in outline with an anterior lobe oval in shape, ventrally vaulted. Posterior lobe shorter (sag.) than the anterior lobe, U-shaped. Posterior border expanded, gently curved posteriorly, smooth without spines.

Thorax composed of eleven tergites (e.g., Fig. 2B). Thoricax axial ring sub-rectangular in outline, distal tips lightly rounded, slightly shorter (sag.) medially, width (tr.) less than one-third of the pleural width, gradually narrowing (tr.) in
posterior tergites. Articulation half-ring with sagittal length half of the axial ring length, longer medially, tapering distally, anterior margin bowed anteriorly. Thoracic pleurae unconstrained, narrow flange in the anterior and posterior margin, carrying a deep, oblique pleural furrow that divides the pleura into an anterior and posterior band. Fulcrum subGLEBT, situated in the distal second third of the pleura. Anterior band with the same length (sag.) as the posterior, but narrower (tr.). The posterior band extended beyond the fulcrum in the pleural spine, needle-like and sub-circular in cross-section. Five anterior tergites with short pleural spines that are directed posterolaterally, and increasing subtly in length from anterior toward posterior tergites. Six posterior tergites with long, thick, rather posteriorly directed pleural spines (Figs. 1C, D, 2A). Pleural spine of the sixth tergite longer and thicker than the rest, curved outward and backward, and extending (exsag.) beyond the pygidial terminal piece. Pleural spines in posterior trunk decreasing in size gradually from the sixth to the eleventh tergite.

Pygidium reduced with two axial rings plus terminal piece and one pair of pleural spines (Fig. 1B, D). Articulating half-ring short (sag.) with half of the length of the first axial ring, longer (sag.) medially, tapering distally, anterior margin anteriorly bowed. First pygidial axial ring rectangular in outline, longer (sag.) and wider (tr.) than the second pygidial axial ring. Terminal piece narrower (tr.) than pygidial axial rings, similar in length (sag.) to second axial ring; anterior margin transversal, posterior margin slightly bowed posteriorly. One pleural tergite strongly curved backwards, with a distinct pleural furrow dividing the pleura in anterior and posterior bands, the posterior band extended in a pair of long pleural spines directed backwards.

*Ontogeny:* The smallest recorded specimen (MGL 104146) is a late meraspid stage that is 2.6 mm long (Fig. 3A). The cephalon of this juvenile stage is generally identical to the cephala of the adult individuals, only the genal spines are proportionally longer (such longer genal spines are evident also in some small holaspid specimens, Fig. 3B, C). The trunk bears at least ten or eleven axial rings, posteriors of which are difficult to recognize, and twelve pairs of pleural spines. In contrast to the holaspids, the pleural spines of this small individual show a slightly different pattern in respect to their mutual sizes. The spines of tergites one to seven are quite long with equal or nearly equal length. The spines on tergites one to five are not significantly smaller than the rest, as is the case for holaspids. From the seventh tergite, the spine sizes decrease in length rapidly, such that the tenth to twelve pairs are minute. The equal number of pleural spines between this juvenile specimen and the adults suggests that this juvenile might have already reached the total number of trunk segments characteristic for *A. adserai*, despite the posterior-most axial rings not being recognizable. It is not clear whether the last pre-terminal tergite (no. 13) was present, for this one does not bear any spines in the holaspid individuals. Seven anterior trunk tergites are separated by articulating structures, forming the thorax. The

<figure><img src="image_5.png" /></figure>

<figure><img src="image_6.png" /></figure>

Fig. 3. Juveniles of the cheirurid trilobite *Anacheirurus adserai* from the Fezouata Shale, *Araneograptus murrayi* Zone, Tremadocian, Lower Ordovician, near Beni Zouli, Zagora Province, Morocco. A. MGL 104146, late meraspid stage. B. MGL 102153, early holaspid stage. C. MGL 104533, early holaspid stage. Specimens in B, C covered by ammonium chloride. Scale bars 1 mm.

posterior tergites, bearing five pairs of pleural spines, are still fused, forming a meraspid pygidium. This tergite-rich meraspid pygidium suggests that the *A. adserai* holaspid pygidium developed into its final form by depletion of the conjoined tergites of the thorax, as is known in many other trilobites (e.g., Hughes et al. 2006, Laibl et al. 2014). MGL 101262 (5.6 mm long) and MGL 104533 (5.9 mm long) are the smallest holaspids found (Fig. 3B, C). The morphology of the pleural spines is similar to the morphology of the adult specimens. The only differences to fully-grown individuals are proportionally longer genal spines and the slightly larger size of the first five thoracic pleural spines.

*Appendages: Antennae:* A uniramous antenna is partially visible in the counterpart of MGL 102179 (Fig. 1A₂, white
<figure><img src="image_7.png" /></figure>

A₂

<figure><img src="image_8.png" /></figure>

<figure><img src="image_9.png" /></figure>

B₂

<figure><img src="image_10.png" /></figure>

Fig. 4. Endopodites of the cheirurid trilobite *Anacheirurus adserai* (Vela and Corbacho, 2007) from the Fezouata Shale, *Araneograptus murrayi* Zone, Tremadocian, Lower Ordovician, near Beni Zouli, Zagora Province, Morocco. A. MGL 103863, photograph under alcohol with polarized light (A₁), explanatory drawing with podomere numbers (A₂). B. MGL 102225, photograph under alcohol with polarized light (B₁), explanatory drawing with endopodite numbers (B₂). Scale bars 1 mm. Abbreviations: ar, axial ring.
<figure><img src="image_11.png" /><figcaption>Fig. 5. Endopodites of the cheirurid trilobite *Anacheirurus adserai* (Vela and Corbacho, 2007) from the Fezouata Shale, *Araneograptus murrayi* Zone, Tremadocian, Lower Ordovician, near Beni Zouli, Zagora Province, Morocco. A. Part of YPM 226573, general view (A₁), close-up of the endopodites (A₂) and explanatory drawing (A₄), close-up of the distal claw (A₃) and explanatory drawing (A₅). B. Counterpart of YPM 226573, general view (B₁), close up of the endopodites (B₂) and explanatory drawing (B₃), close up of the endopodites (B₄) and explanatory drawing (B₅), close up of the area pointed out in B₄ (B₆), arrows showing long endites on podomere 2 and 3. Numbers represent podomere number. Abbreviations: ar, axial ring.</figcaption></figure>

arrow). The proximal part of the right antenna is preserved in the front of the cephalon. The individual podomeres are poorly recognizable but seem to be rather short, and qua-

dratic in outline. The total number of podomeres and the total length of the antenna are not known because the distal tip is missing.
<figure><img src="image_12.png" /><figcaption>Fig. 6. Cheirurid trilobite *Anacheirurus adserai* (Vela and Corbacho, 2007) (MGL 102172) from the Fezouata Shale, *Araneograptus murrayi* Zone. Tremadocian, Lower Ordovician, near Beni Zouli, Zagora Province, Morocco. Photographs under alcohol: general view (A₁), close-up of the exopodites (A₂) and explanatory drawing (A₃). Scale bars 1 mm. Abbreviations: ar, axial ring.</figcaption></figure>

**Protopodites:** The protopodite is not preserved in any of the studied specimens. In general, the appendages in the Fezouata Shale trilobites are visible in the parts where the exoskeleton has been removed. The protopodite should be located below the axial region, which usually is not removed. As a consequence, the proximal parts of the appendages are not visible. In MGL 10225 and YPM 226573 some structures can be interpreted as a part of the protopodite (Figs. 4B, 5A₂, A₄), however, the nature of the structures is not clear and not enough information is available to interpret the morphology or the presence of a gnathobase.

**Endopodites:** The endopodites are preserved in the MGL 103863 (Fig. 4A), MGL 10225 (Fig. 4B), and YPM 226573 (Fig. 5). The proximal parts of the endopodites are poorly preserved, and the attachment point to the protopodite is not visible in any of the specimens. The three anterior-most endopodites belong to the cephalon (Fig. 4A₂, B₂), corresponding with attachment sites on S2, S1, and SO (Fig. 4A, B). In the thorax, each tergite bears a pair of endopodites (Fig. 4B). The posterior thoracic (behind the tenth tergite) and the pygidial endopodites are not preserved.

The endopodites are divided into seven podomeres (numbered in Fig. 5A₂, A₄). The most proximal podomeres 1–3

have a rectangular shape and are more robust than the rest of the podomeres. The podomere 3 is just slightly shorter and thinner than the previous ones (1 and 2). The following podomeres (4–6) are much narrower and more elongated in shape. They gradually decrease in width and increase in length distally, with the podomere 6 being the narrowest and most elongated (Fig. 5A₂, A₄). The podomeres 5 and 6 are both nearly twice as long as the most proximal podomeres. The podomere 7 is reduced, forming a tripartite claw, with a fork shape (Fig. 5A₃, A₅).

The morphology of the endopodites is consistent along the body, at least up to the tenth thoracic endopodite. The cephalic endopodites are shorter than the thoracic ones, with thicker proximal podomeres (Fig. 4A, B). Large endites are visible in the posterior endopodites, but no endites are visible in the anterior endopodites. In YPM 226573, one of the posterior endopodites bears two large endites on podomeres 2 and 3 (Fig. 5B₄, B₆, B₅). The endopodites are usually flexed at a joint between the third and the fourth endopodite. In most of the specimens, the proximal part of each endopodite is directed anterolaterally while the distal region beyond the joint is directed posterolaterally.

**Exopodites:** The exopodites are preserved in MGL 102172 (Fig. 6) and YMP 517074 (Fig. 7), with the latter
<figure><img src="image_13.png" /><figcaption>Fig. 7. Exopodities of the cheirurid trilobite *Anacheirurus adserai* (Vela and Corbacho, 2007) (YPM 517074) from the Fezouata Shale, *Araneograptus murrayi* Zone, Tremadocian, Lower Ordovician, near Beni Zouli, Zagora Province, Morocco. Photographs: general view (A₁), close-up of the exopodites (A₂) and explanatory drawing (A₃), close up to the ninth exopodite (A₄) and explanatory drawing (A₅). Scale bars 1 mm. Abbreviations: ar, axial ring; ex, exopodite.</figcaption></figure>

preserving the only complete exopodite (ninth thoracic exopodite; Fig. 7A₄, A₅). The rest of the exopodites are partially covered in the anterior region, obscuring the complete shape. The exopodite consists of a flat, elongated, wider (tr.) than longer (sag.) flap. Around the flap, there is a reinforced marginal rim (Fig. 7A₅) showing a smooth surface. The anterior margin of the flap is slightly concave, while the posterior is almost straight, with the distal part curving forward. The flap is divided into two separate lobes by an articulation that extends from the anterior to the posterior region in an almost straight line, perpendicular to the main

axis of the flap (Fig. 7A₄). The proximal lobe is sub-rectangular in outline, longer (tr.) and wider (exsag.) than the distal lobe. Attached to the posterior rim, there are long and flat imbricated lamellae (Figs. 6A₂, A₃, 7A₂–A₅). The distal lobe is sub-oval in outline, also with bristles attached to the posterior margin. The lamellae on the proximal lobe are directed posteriorly, reaching the posterior tergite border, and are wider in the transversal section and longer than the bristles on the distal lobe, which are shorter and thinner. The bristles on the distal lobe are directed slightly outwards. The joint between the protopodite and the exopodite is not
visible; it is covered by the thoracic axial rings. The three anterior exopodites in YPM 517074 display a similar morphology, bearing long and robust lamellae attached to the posterior rim of the flap, however, the anterior region of the flaps is overlapped by the lamella of the next most anterior exopodite (Fig. 7A₂, A₃). The exopodites show different spatial distributions between specimens. In YMP 517074 the posterior exopodite is oriented transversally (Fig. 7), perpendicular to the sagittal axis, with the lamellae pointing backward. In MGL 102172 the exopodite is forwardly and slightly outwardly oriented with the lamellae pointing transversally to the sagittal axis (Fig. 6).

*Remarks*.—The species discussed herein was originally described by Vela and Corbacho (2007) as *Lehua adserai*. These authors assigned this species to the genus *Lehua* Barton, 1915, but unfortunately did not provide any justification or discussion why they did so. The *Lehua* was erected by Barton (1915). The characters defining *Lehua*, as presented by Barton (1915), are: glabella not tumid; eyes absent or extremely rudimentary; genal spines present; frontal lobe much less than one-third of the glabella; pleura with transverse constriction or node; the inner portion cut by a diagonal furrow and pygidium not differentiated from the thorax. Later, Prantl and Přibyl (1947: 18), amended the description of *Lehua* as having: “... 11 thoracic segments and six-lobate pygidium. Free cheeks small, shifted forward. Facial suture forming a small arc; at first, it runs close along the margin of the glabella and at the level of the first lateral glabellar lobe it turns back in an arc to the lateral margin of the cephalon. Neither visual organs nor palpebral lobes are developed. Pygidium with raised subtriangular axis composed of four rings, the fourth being completely stunted. Three pairs of sword-like curved, free, flat pleurae of unequal length. The lower margin of the pygidium is sharply cut off in a straight line perpendicular to the axis.” These diagnostic features of *Lehua* are not present in the species described by Vela and Corbacho (2007) as *Lehua adserai*, making this generic assignment questionable. On the contrary, *L. adserai* shows numerous similarities with the type species of the *Anacheirurus* (*A. frederici*) and should be therefore placed within this genus. Both *A. adserai* and *A. frederici* are morphologically nearly identical. *Anacheirurus adserai* differs from *A. frederici* in having a shorter (sag.) anterior border, an eye ridge not adjacent to facial suture, by the absence of S4, and by the number of pygidial spines with probably two pairs in *A. frederici* and one pair in *A. adserai*.

Whittard (1967: 285) pointed out that the morphological differences between *Lehua* and *Anacheirurus* are not enough to warrant two different genera, suggesting *Lehua* should be considered as a junior synonym of *Anacheirurus*, an argument later followed by Martin et al. (2016b) in their review of Fezouata Shale trilobites. Based on the new material studied herein, we advocate for the idea formulated by Lane (1971) that *Lehua* is a valid genus different from *Anacheirurus*. *Lehua vinculum* (Fig. 2C–E), shows several major morphological differences when compared to *A. frederici*. First, the

glabella of *L. vinculum* is slightly expanded in the front, while in *A. frederici* it is sub-parallel with the median part slightly wider. Second, the posterior margin of the cephalon in *L. vinculum* is not transverse; the more distal parts are curved slightly forward. In *A. frederici*, on contrary, the distal part of the posterior margin is curved backward, creating a slightly expanded posterior border close to the genal spines. Third, the palpebral lobes and eye ridges are not present in *L. vinculum*, whereas in *A. frederici* they are prominent and well developed (however the lack of eyes in *Lehua* could be taphonomic, as the anterior part of the fixigena is not well preserved in the type species). Finally, the main difference between *L. vinculum* and *A. frederici* is related to the morphology and arrangement of the thoracic pleurae. In *L. vinculum*, all the thoracic and pygidial pleural spines are of the same size (only slightly decreasing in length posteriorly on the pygidium), contrary to *A. frederici*, which has posterior thoracic and pygidial spines that are longer than the anterior thoracic pleural spines. The thoracic pleurae of *L. vinculum* are divided into an inner and outer parts, with the inner part consisting of one-quarter of the length of the pleura and the outer part three quarters. Only the inner part of the pleura in *L. vinculum* bears an oblique pleural furrow. The pleurae in *A. frederici* are not divided into an inner and an outer part, instead, the pleural furrow is deep, oblique, and traversing the whole width (tr.) of the pleura dividing it into anterior and posterior parts of similar size.

Since the morphology of the pleural furrow is relevant for the classification of different groups inside the family Cheiruridae (e.g., Barrande 1852; Salter 1864; Schmidt 1881; Reed 1896; Barton 1915; Öpik 1937; Lane 1971), this character has a broader implication for the systematic position of *A. adserai*. *Anacheirurus adserai* displays a pleural morphology diagnostic of the subfamily Pilekiinae (Lee and Chatterton 1997), whereas *L. vinculum* displays a pleural morphology typical of the subfamily Cheirurinae (Lane 1971). *Lehua* is a more derived taxon belonging to a late diverging group that contains highly derived taxa such as *Cheirurus* and *Crotalocephalus*.

Some authors (Bulman and Rushton 1973; Přibyl et al. 1985; Sdzuy et al. 2001) suggested that *Parapilekia sougyi* (Destombes in Destombes et al., 1969), described from the Zemmour locality (Mauritania) by Destombes in Destombes et al. (1969) should also belong to the *Anacheirurus*. The morphology of the cephalon of *P. sougyi* and *A. adserai* is generally identical, with the only notable difference in glabellar furrows, which are not connected to the axial furrow in *Parapilekia sougyi*. This character might be, however, caused by differences in the preservation. Destombes et al. (1969) also described a fragmentary pygidium with three axial rings (two rings and a terminal piece?) and one pair of spines directed backward. Such a morphology corresponds with what is seen in *Anacheirurus adserai*. This suggests that *Parapilekia sougyi* is a species of *Anacheirurus*, possibly even synonymous with *A. adserai* (in which case the name *A. adserai* would be a junior sub-
jective synonym of *A. sougyi*). However, the type material of *A. sougyi* does not allow more detailed comparison, due to its fragmentary nature. Until more complete specimens of *A. sougyi* from the type and/or nearby localities are available, we recommend keeping *A. sougyi* and *A. adserai* as two separate species.

Seven species of *Anacheirurus*, assigned previously to *Lehua*, were originally described in the area of Zagora, Morocco (Vela and Corbacho 2007; Vela 2007; Corbacho 2008). In the following years, Vela and Corbacho (2011) considered three of them (*A. colli*, *A. ponti*, and *A. iannacconnei*) as junior synonym of *A. corbachoi*, keeping four different species of *Anacheirurus* from the Fezouata Shale. Their characters separating individual species are in general related to the shape of the cephalon and the glabella, the presence and morphology of the anterior notch in the cephalon, and the number and shape of posterior pygidial spines. These species are based on specimens that were heavily prepared, a process that may modify or exaggerate the original morphology, and can lead to misinterpretations of anatomical characters (Fortey 2009; Gutiérrez-Marco et al. 2017; Gutiérrez-Marco and García-Bellido 2018). Martin et al. (2016b) in a study about the trilobite community in the Fezouata Shale concluded that there is only one morphotype of pilekiid, and it was assigned to *Anacheirurus adserai* which is the oldest species of *Anacheirurus* described. Detailed observations of numerous specimens from Fezouata Shale, which had not undergone the same degree of preparation suggest, in concordance with Martin et al. (2016b), that all the species may be junior subjective synonyms of *A. adserai* for the following reasons.

Firstly, the anterior cephalic notch that is variously developed in some specimens (Vela and Corbacho 2011: pl. 1: 2) represents the dorsal arching of the cephalon. Such arching is expressed to a higher or lower degree on the compressed specimens, ranging from an indistinct or distinct notch to a protrusion, depending on the original orientation of the cephalon to the bedding plane. Hughes and Rushton (1990) explained how similar variability in the pygidial shape of trilobite *Cermatops discoidalis* (Salter, 1866) is caused by different depositional orientations of the pygidium. Similarly, Hughes (1995) listed morphological characters in trilobite *Bailiella lantenoisi* Mansuy, 1916, that can be a subject of taphonomic variation when preserved in shales. Four of these characters (frontal area length, border length, preglabellar field depression, and anterior border furrow) are generally related to the shape of the anterior cephalic margin (see Hughes 1995: table 1), corroborating this part of the trilobite exoskeleton is prone to taphonomic variation when preserved in shales. These examples demonstrate that certain types of variation in trilobite body parts, when preserved in shales, should not be considered as real biological features, but taphonomic artifacts.

Secondly, the exact number of pygidial spines is generally hard to determine in complete individuals of *Anancheirurus*, as the boundary between the thorax and the py-

gidium is difficult to identify owing to the similarity of thoracic and pygidial pleurae. Especially in species where both thoracic and pygidial pleurae bear spines but otherwise do not show any major morphological differences between thorax and pygidium, the last articulation structure is not easy to discern (see Esteve et al. 2017 for a similar issue). The variation in the number of pygidial spines in individual species described by Corbacho and Vela (2011) may be subject to such a bias, especially in heavily prepared specimens.

There is also an uncertainty regarding the exact stratigraphic position of several *Anacheirurus* species from the Anti-Atlas region. The type locality of *A. adserai*, *A. corbachoi* (and its subjective synonyms *A. colli*, *A. ponti*, *A. iannacconnei*), *A. tahirii*, and *A. velai* was named as “Tanssikhte”, west of Zagora (Vela and Corbacho 2007: fig. 1; Vela 2007: fig. 1). The type locality was assigned stratigraphically to the Upper Fezouata Shales, “lower-middle Arenig” (= Floian age). Thirty additional trilobite species were identified, with some of them typical for Floian strata (belonging to genera *Foulonia*, *Pateraspis*, or *Ormathops*), but others typical for Tremadocian (such as *Bavarilla zemmourensis*) (Vela and Corbacho 2007; Vela 2007). However, the latest review of trilobite stratigraphic distribution in the Fezouata Shale made by Martin et al. (2016b) shows that *Anacheirurus adserai* is restricted to *Araneograptus murrayi* Zone of the upper Tremadocian. We agree with Martin et al. (2016b) statement and we question the original locality and stratigraphic assignment *Anacheirurus adserai*.

*Stratigraphic and geographic range.*—Anti-Atlas of Morocco and possibly also northern Mauritania (= *A. sougyi*, see section Remarks for details). Fezouata Shale, *Araneograptus murrayi* Zone, Tremadocian, Lower Ordovician.

## Discussion

**Morphological disparity of Pilekiinae.**—Trilobites of the subfamily Pilekiinae represent the earliest radiation of Cheiruridae, which is one of the major post-Cambrian trilobite groups. During the Tremadocian, pilekiines reached a high global diversity (over 50 species) being a common worldwide faunal component of shallow marine communities. From the morphological perspective, it is interesting to analyze how the cranidia and pygidia vary in shape within the group. In general, the cephalic morphology of Pilekiinae is characterized by the following features: glabella sub-rectangular to expanded posteriorly and tapering forwards, anterior border short (sag.), eyes in anterior position, small palpebral lobe, thick well-defined eye-ridge, reduced librigenal field, fixigenal field sculpted by small pits. The main differences found between the cephala of various taxa are small variations in the shape of the glabella, length of the genal spines, shape of the anterior border and small changes in the position of palpebral lobes (Fig. 8A₁, B₁, C₁, D₁, E₁). Some early putative pliomerids (for example the *Rossaspis*
<figure><img src="image_14.png" /><figcaption>Fig. 8. Reconstructions of cranidia ($A_1-E_1$) and pygidia ($A_2-E_2$) of different members of the subfamily Pileiinae. A. *Anacheirurus adserai* (Vela and Corbacho, 2008). B. *Parapilekia olesnaensis* (Růžička, 1935), based on Mergl (2006). C. *Tesselacauda depressa* Ross, 1951, based on Adrain and Karim (2019). D. *Landyia elizabethae* Jell, 1985, based on Jell (1985). E. *Macroprogrammus rafi* Edgecombe, Chatterton, Vaccari, and Waisfeld, 1999, based on Edgecombe et al. (1999).</figcaption></figure>

Harrington, 1957; see Adrain et al. 2014: fig. 20) also share a cephalic morphology similar to pileiines. In contrast, the pygidia of pileiines show a broader range of morphologies. This is evident, especially when comparing the pygidia of various pileiid species (Fig. 8A₂, B₂, C₂, D₂, E₂). The main differences are the overall shape, the number of axial rings, the number and length of pleural spines, and the size and shape of the terminal piece. For example, the pygidium of *Tesselacauda depressa* displays four broad and short adjacent pygidial pleurae with rounded tips, (Fig. 8C₂; e.g., see Adrain and Karim 2019: pl. 6), whereas the pygidium of *Parapilekia olesnaensis* has the pygidial spines arranged in a radial disposition with a space between them (Fig. 8B₂; see Mergl 2006: fig. 19K). The pygidium of *Anacheirurus adserai* (Fig. 8A₂) is unique with its extremely long pleural

spines that project posteriorly from the end of the pygidium. The pygidium of *Macroprogrammus rafi* has the pygidial spines strongly curved backward and the terminal piece extremely reduced (Fig. 8E₂; see Edgecombe et al. 1999: fig. 8), whereas the pygidium of *Landyia elizabethae* has a prominent terminal piece and four pleurae with a pleural furrow that do not reach the pleural margin and very short pygidial spines (Fig. 8D₂; see Jell 1985: pl. 31: 2B). The number of pygidial segments, as well as the number of pleural spines, also differ considerably among the group. The range of axial rings goes from two axial rings plus terminal piece (A. adserai; Fig. 8A₂) to five axial rings plus terminal piece (e.g., *Parapilekia speciosa*; see Ebbestad 1999: fig. 79; Fig. 8B₂), with all the intermediate cases. The range of pygidial spines goes from one pair of pygidial spines (A. adserai; Fig. 8A₂) to four pairs of pygidial spines, with examples of two pairs (*Seisonia sphericaudata*) and three pairs (e.g., *Anacheirurus nanus*) and multiple cases of four pairs (e.g., *Macroprogrammus rafi*). The pygidium of A. adserai is the most reduced pygidium (in terms of segmentation) recorded among Pileiinae. *Anacheirurus frederici* may have also a reduced pygidium, however, it is not well known how many segments are allocated in its pygidium, as the boundary between the thorax and pygidium is obscure (owing to the strong similarity between the thoracic and the pygidial morphology and the tectonic deformation of the holotype).

The variable number of pygidial segments in Pileiinae contrasts with the rest of cheirurid subfamilies. Cheirurinae displays a stable configuration with three segments plus a terminal piece. Deiphoninae display three to four segments plus terminal piece. Acanthoparyphinae varies from two to three pygidial segments. Sphaerexochinae display three pygidial segments plus a terminal piece. Heliomerinae shows two pygidial segments. Eccoptychilinae shows from three to four pygidial segments plus a terminal piece.

Pileiines display a homonomous trunk (i.e., the thoracic and pygidial tergites are generally of equal morphology; see Hughes 2003, 2005). In some younger members of Cheiruridae the pygidium is clearly differentiated from the thorax (heteronomous trunk), for example in the genera *Ceraurinella*, *Ceraurus*, *Hemisphaerocoryphe*, *Sphaerocoryphe*, *Deiphon*, *Holia*, or *Nieszkowskia*. The degree of differentiation varies, with some taxa having less differentiated trunk than the aforementioned examples, e.g., *Actinopeltis*. Such trunk differentiation could drive the fixation of the number of pygidial tergites. Another factor that has been claimed as a constraint for the variation in the number of trunk segments is enrollment (Hughes et al. 1999; Hughes 2003, 2005; Esteve et al. 2011, 2013). Pileiines display a thoracic articulation composed of a short (exsag.) flange in the anterior margin of the pleura and a less-developed fulcrum positioned far from the axis anteriorly and progressively positioned closer to the axis posteriorly. The articulating facet is not developed in pileiines. No evidence of coaptative structures has been found. The simple flange-hinged articulation and the lack of ar-
ticulating facets and coaptative structures suggest that the enrollment of pilekiines was non-encapsulated, similar to those seen in some Cambrian trilobites (Ortega-Hernández et al. 2013; Esteve and Yuan 2017). In contrast, most of the other members of Cheiruridae have developed thoracic devices to achieve spheroidal (and likely also encapsulated) enrollment. These taxa show a well-developed fulcrum that is situated closer (adaxially) to the axis, a fulcral process and socket (e.g., Cheirurinae), or a faceted outer pleural part (e.g., *Kawina*). In addition, some taxa have developed coaptative structures as a pair of spines in the rostral plate in *Cyrtometopus clavifrons* (Dalman, 1827), which fit between the pygidial spines when fully enrolled (see Lane 2002 for more information) or a furrow in the doublure in the genus *Sphaerexochus* (see Chatterton and Ludvigsen 1976: pl. 13: 35, 36) for accommodating the first thoracic pleura. It is believed that spheroidal enrollment requires a precisely co-ordinated scaling of the body proportions (Hughes 2007), therefore the stable number of pygidial tergites in strati-graphically young cheirurids might be an adaptation to this particular enrollment style.

**Comparison of trilobite appendages.**—Broadly speaking, the general morphology of the appendages of *A. adserai* is similar to the appendages of other trilobites. They consist of anterior pair of uniramous antennae composed of multiple podomeres followed by a series of homonomous biramous limbs (cf. Scholtz and Edgecombe 2005, 2006; Ortega-Hernández et al. 2017). The number of appendages belonging to the pygidium is unknown. The protopodite and the junction between the protopodite and the ventral part of the body are not preserved in any specimen of *A. adserai*, so its morphology and structure cannot be described. Each endopodite is composed of seven podomeres, with the most distal reduced (Fig. 9). The exopodite is a flap bearing long filaments (Fig. 9).

The detailed appendage morphology of *A. adserai* shows several important differences when compared to known appendages of other trilobites. One of the unique character-

<figure><img src="image_15.png" /><figcaption>Fig. 9. Biramous appendages reconstruction for the cheirurid trilobite *Anacheirurus adserai*, showing the anterior (A) and the posterior (B) morphology. Dashed lines indicate inferred proximal parts of the appendages.</figcaption></figure>

istics of *A. adserai* is the elongated podomere 5 and 6 of the endopodite (Fig. 9), which are approximately two times longer than the first four podomeres. In other trilobites, the podomeres are of equal or nearly equal length (e.g., Holmes et al. 2020), or they gradually shorten distally (e.g., Whittington 1975: Whittington and Almond 1987: Zeng et al. 2017). Similar elongated distal podomeres, as in *A. adserai*, can be found in other non-trilobite arthropods such as *Emeraldella brocki* (Stein and Selden 2012), where the fourth and sixth podomeres are elongated, or in the second cephalic endopodite in *Mollisonia plenovenatrix*, which has an elongated sixth podomere (Aria and Caron 2019).

The cephalic endopodites in *A. adserai* are shorter than those of the thorax. The overall pattern of the endopodite length is similar to *Olenoides serratus*, which has the longest endopodites between the fourth and thirteenth appendage (Whittington 1975), or *Triarthrus eatoni*, which displays a progressive increase in size from the second to the fourth endopodite, after which the size remains constant until an abrupt reduction in endopodite size in the most posterior part of the thorax and the pygidium (Whittington and Almond 1987). *Megistaspis hammondi*, also from the Fezouata Shale, shows a different pattern, with the anterior endopodites being more robust and more spinose than the posterior ones (Gutiérrez-Marco et al. 2017). Such heteropody is not present in *A. adserai*, although there might be a slight difference in the spinosity between the anterior and posterior endopodites. Indeed, some posterior endopodites show long endites in proximal podomeres (Fig. 9), while anterior endopodites seem to lack these endites. Whether this is a real morphological feature or just a difference in endite preservation is uncertain. Some other trilobites, such as *Olenoides serratus*, *Triarthrus eatoni*, or *Hongshiyanaspis yiliangensis* preserve endites on all the endopodites (Whittington 1980; Whittington and Almond 1987; Zeng et al. 2017). In these trilobites, the endites are also more prominent in proximal podomeres, as in *A. adserai*. Contrary to all the previous examples, *Redlichia rex* has no endites on the endopodites (Holmes et al. 2020). In *Triarthrus eatoni*, the more posterior endopodites have more prominent endites (Whittington and Almond 1987). This might also explain why we observe endites only on the posterior endopodites of *A. adserai*.

The morphology of the exopodites of *A. adserai* resembles those of Cambrian trilobites, namely *Olenoides serratus*, *Hongshiyanaspis yiliangensis*, *Eoredlichia intermediata*, *Redlichia rex*, *Kootenia burgessensis*, or *Kuanyangia pustulosa* (Whittington 1975; Hou et al. 2008; Zeng et al. 2017; Holmes et al. 2020; Fig. 10A–D). Their exopodites consist of an elongated flap, with long imbricated lamellae that are attached to the posterior margin of the flap, and with shorter bristles in its distal part. The flap itself can be bipartite (e.g., in *Olenoides serratus*, *Eoredlichia intermediata*, *Kuanyangia pustulosa*, *Kootenia burgessensis*), or tripartite (e.g., in *Redlichia rex*, *Hongshiyanaspis yiliangensis*). In both cases, the overall shape of the flap is sim-
<figure><img src="image_16.png" /><figcaption>Cambrian exopodites</figcaption></figure>

<figure><img src="image_17.png" /><figcaption>Ordovician exopodites</figcaption></figure>

<figure><img src="image_18.png" /><figcaption>Devonian exopodites</figcaption></figure>

Fig. 10. Trilobite exopodite reconstructions grouped by geological age. A. *Eoredlichia intermediata* (Lu, 1940), based on Ramsköld and Edgecombe (1996). B. *Hongshiyanaspis yiliangensis* Zhang and Lin in Zhang et al., 1980, based on Zeng et al. (2017). C. *Redlichia rex* Holmes, 2019, based on Holmes et al. (2019). D. *Olenoides serratus* (Rominger, 1887), based on Whittington (1980). E. *Anacheirurus adserai* (Vela and Corbacho, 2007). F. *Ceraurus pleurexanthemus* Green, 1832, based on Størmer (1951). G. *Triarthrus eatoni* (Hall, 1838), based on Whittington and Almond (1987). H. *Cryptolithus bellulus* (Ulrich, 1879), based on Campbell (1975). I. *Chotecops ferdinandi* (Kayser, 1880), based on Bruton and Haas (1999).

ilar, with the most proximal lobe being bigger and bearing long lamellae and the most distal lobe being reduced in size and bearing bristles. The exopodite morphology of *A. adserai* resembles these Cambrian taxa as the flap is wide and flat, and has a bipartite morphology, with longer lamellae in the proximal part and shorter bristles in the distal part.

The exopodite morphology from post-Cambrian trilobites is less well known, but the available data suggest a different morphology than that seen in Cambrian trilobites. The Ordovician taxa *Ceraurus pleurexanthemus*, *Cryptolithus bellulus*, and *Triarthrus eatoni* (Størmer 1939; Bergström 1972; Whittington and Almond 1987), and the Devonian *Chotecops fernandi* (Bruton and Haas 1999) are the best-studied examples (Fig. 10F–I). *Cryptolithus bellulus* and *Thriarthrus eatoni* both come from Beecher’s Trilobite Bed in the Frankfort Formation, Upper Ordovician, New York. The exopodite of *T. eatoni* consists of a slender shaft annulated by 15 oblique grooves with the filaments attached to the upper side of the shaft, and a small lobe at the tip of the shaft (Cisne 1975, 1981; Whittington and Almond 1987; Fig. 10G). In *Cryptolithus bellulus* the morphology is unclear. All of the different interpretations, however, agree that it has a series of bristles attached to a slender shaft (Raymond 1920; Størmer 1939; Bergström 1972, 1973; Campbell 1975; Fig. 10H), more similar to the morphology present in the species of *Triarthrus* than to the flap-shaped exopodites present in Cambrian taxa and the species of *Anacheirurus*. The exopodites of *Ceraurus pleurexanthemus* from the Trenton Limestone, Upper Ordovician, New York, are preserved inside the body cavity of enrolled specimens, by authigenic mineralisation with calcite (Walcott 1918; Raymond 1920; Størmer 1939, 1951), and can be examined only in thin section. The overall morphology of the appendages of *Ceraurus pleurexanthemus* remains difficult to determine. Størmer (1939, 1951) reconstructed an exopodite divided into five segments with long bristles only on the last segment (Fig. 10F).

The appendage morphology described above does not resemble that seen in *Anacheirurus adserai*, a difference that is striking because *C. pleurexanthemus* and *A. adserai* are both members of the family Cheiruridae. The similarity between Cambrian trilobites and *A. adserai* exopods on the one side, and the difference between the exopods within Cheiruridae on the other, can be explained by two hypotheses. Either *Anacheirurus* retained the plesiomorphic Cambrian exopodite morphology, which was subsequently modified within Cheiruridae, or the exopodite of *Anacheirurus* convergently evolved into a similar form to that seen in Cambrian taxa owing to similar ecological pressures. Zeng et al. (2017) argued that the variations in the morphology of exopodites might be the result of different ecological adaptations, which would rather favor the latter hypothesis.

The last example of trilobite appendages is *Chotecops ferdinandi* from the Hunsrück Slate, Lower Devonian, Germany, which has been studied mainly using the X-rays (Stürmer 1968, 1970; Stürmer and Bergström 1973; Bruton and Haas 1999). The exopodite remains of *C. ferdinandi* are fragmentary and the general morphology is not known in detail. Bruton and Haas (1999) suggested there is an exopodite with broad filaments attached along the margin of a thinner smooth shaft (Fig. 10I). Bruton and Haas (1999)
have not found any evidence of a bipartite shaft with different bristles in the distal region.

**Implications for evolutionary trends and the Ordovician biodiversification.**—During the Ordovician major changes in trilobite faunal composition took place (Adrain et al. 1998, 2004) which were a part of the Ordovician biodiversification and the Great Ordovician Biodiversification Event (sensu Stigall et al. 2019, 2020). Changes in the morphology of trilobite appendages (especially exopodites) also happened during this time interval. Interestingly, these changes in appendage morphology are coincident with a major diversification of the ichnogenus *Cruziana* during the Early Ordovician.

Adrain et al. (1998, 2004) recognized several diversifications of Ordovician trilobite faunas, with the major diversification occurring during the Middle Ordovician. Within Cheiruridae, pileiines diversified during the Tremadocian and reduced drastically in diversity during the Floian (Fig. 11). Hence, pileiines are not part of this Middle Ordovician trilobite diversification (Adrain et al. 1998). In contrast, the rest of the family Cheiruridae diversified from the Floian to the Sandbian (Fig. 11), better matching the aforementioned diversification (Adrain et al. 1998, 2004) as well as the Great Ordovician Biodiversification Event (sensu Stigall et al. 2019, 2020).

Although trilobite appendage data from the Ordovician are sparse, the Ordovician diversification of trilobites might explain higher post-Cambrian variability of trilobite exopodites. If the exopodite morphology was indeed driven by ecological adaptations, as Zeng et al. (2017) suggested, then the appendage data follows the increasing complexity of Middle Ordovician ecosystems (Bambach 1983; Signor and Vermeij 1994; Droser and Finnegan 2003; Stigall et al. 2019). This would also explain why the “Cambrian-type” exopodites are present in *Anacheirurus*, an Early Ordovician member of Pilekiinae.

The sparse appendage data from the Ordovician can be supplemented by examining the trace fossil record, in particular the changes observed within the ichnogenus *Cruziana*. *Cruziana* records the imprints of trilobite appendages as they move through and over the sediments, therefore a change in *Cruziana* morphology can reflect a change in the appendage morphology. Different morphologies and ichnospecies of *Cruziana* have been identified across the Paleozoic and clustered in groups (Seilacher 1970, 1991, 1994). In the transition from the Cambrian to the Ordovician, two groups of *Cruziana* ichnospecies are identified. The *Cruziana semiplicata* group ranges from the Lower Cambrian to the Tremadocian (Seilacher 1970, 1991) and is characterized by prominent lateral lobes defined by exopodal brushings flanked by marginal thin ridges (Seilacher 1970, 1991; Crimes 1975). The *Cruziana rugosa* group from the upper Tremadocian to Darriwilian (Seilacher 1970, 1994; Baldwin 1975, 1977; Buatois and Mángano 2011) is characterized by an absence of the external lobe (exopodal markings), and an internal pattern

<figure><img src="image_19.png" /><figcaption>Fig. 11. Ordovician diversity of Cheiruridae species across individual time slices, as defined in Adrain (2013). The dashed line represents the boundary between Tremadocian and Floian; blue, members of the subfamily Pilekiinae; red, members of the rest of Cheiruridae subfamilies excluding pilekiids. Data based on Adrain (2013, personal communication 2020).</figcaption></figure>

composed by sharp scratches from up to twelve subequal claws (Seilacher 1970, 1991; Crimes 1975). Both groups with different patterns overlap in the Tremadocian. This Early Ordovician change in the *Cruziana* morphology may record the diversification and the specialization of trilobite appendages (including the exopodites). Although *Cruziana* is hard to link to exact trilobite taxa, the change in trilobite faunal composition and the change in appendages morphologies are coincident in time with the change in traces.

## Conclusions

Only one species of *Anacheirurus*, *Anacheirurus adserai*, is present in the Fezouata Shale, and is restricted to the upper Tremadocian strata. This species is diagnosed by eleven thoracic segments in the thorax, pygidium reduced with two axial rings plus terminal piece and one pair of pleural spines and seven posterior trunk pleural spines elongated.

*Anacheirurus* is a member of Pilekiinae, a subfamily of Cheiruridae characterized by bearing a wide pleural furrow that divides the thoracic pleura in the anterior and posterior part. Pilekiinae have rather conservative cranidia but highly variable pygidia. The number of pygidial tergites and the morphology of pygidial spines are the major characters that vary across the group.

The endopodites of *Anacheirurus adserai* have seven podomeres, with a reduced distal podomere carrying a tripartite claw, and elongated podomeres 5 and 6. The exopodites consist of a bipartite flap, with a proximal lobe carrying elongated lamellae in its posterior margin and a smaller distal lobe carrying shorter bristles. The overall morphology of the exopodite is similar to “Cambrian-type” and dissimilar to “post-Cambrian” trilobite appendages.

The changes in the Ordovician trilobite diversity are linked with major changes in trilobite exopodite morphology and with the diversification of the ichnogenus *Cruziana*.
Acknowledgements

We are grateful to the reviewers Juan Carlos Gutiérrez-Marco (Instituto de Geociencias, CSIC, UCM, Madrid, Spain) and Jorge Esteve (Universidad de los Andes, Bogotá, Colombia) for their comments which improved the manuscript. Specimen access was facilitated by Antoine Pictet (MGL); Susan Butts and Jessica Utrup (YPM); Bertrand Lefebvre (University of Lyon, France). We also gratefully acknowledge Jonathan Adrain (University of Iowa, Iowa City, USA) and Jorge Esteve for valuable discussions. This research was funded by the Swiss National Science Foundation, grant number 205321_179084 entitled "Arthropod Evolution during the Ordovician Radiation: Insights from the Fezouata Biota" and awarded to ACD. LL's research was funded by the Czech Science Foundation (grant no. 20-23550Y), by the Center for Geosphere Dynamics (UNCE/SCI/006), and was conducted within institutional support RVO 67985831 of the Institute of Geology of the Czech Academy of Sciences.

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