A xandarellid artiopodan from Morocco – a middle Cambrian link between soft-bodied euarthropod communities in North Africa and South China

Xandarellida is a well-defined clade of Lower Palaeozoic non-biomineralized artiopodans that is exclusively known from the early Cambrian (Stage 3) Chengjiang biota of South China. Here we describe a new member of this group, Xandarella mauretanica sp. nov., from the middle Cambrian (Stage 5) Tatelt Formation of Morocco, making this the first non-trilobite Cambrian euarthropod known from North Africa. X. mauretanica sp. nov. represents the youngest occurrence of Xandarellida – extending its stratigraphic range by approximately 10 million years – and expands the palaeobiogeographic distribution of the group to the high southern palaeolatitudes of West Gondwana. The new species provides insights into the lightly sclerotized ventral anatomy of Xandarellida, and offers stratigraphically older evidence for a palaeobiogeographic connection between Burgess Shale-type euarthropod communities in North Africa and South China, relative to the (Tremadocian) Fezouata biota.


Taxon Classification Age Locality References
Cindarella eucalla* Xandarellida Cambrian Stage 3 Chiungchussu Fm., Chengjiang, South China Chen et al. 1 Ramsköld et al. 3 Hou and Bergström 2 Xandarella spectaculum Xandarellida Cambrian Stage 3 Chiungchussu Fm., Chengjiang, South China Hou et al. 4 Ramsköld et al. 3 Hou and Bergström 2 There is a well-established trilobite biostratigraphy for the Cambrian of southern Morocco 17,18 within which the Tatelt Formation spans the Sectigena, Hupeolenus and Morocconus notabilis Biozones (Fig. 3). Unfortunately, this biostratigraphy is not well constrained by radiometric ages or chemostratigraphy, and a high degree of trilobite endemism has hindered correlation beyond the Iberian Peninsula and, to some extent, Avalonia 19,20 . A single radiometric age from the upper Lemdad Formation, Antatlasia guttapluviae Zone (Fig. 3), of 515.56 ± 1.16 Ma 21 (recalculated from 517.0 ± 1.5 Ma 22 ) provides a lower age boundary in this section. However, the Tatelt Formation is generally considered to straddle the lower -middle Cambrian (Series 2-3) boundary in Morocco, with the upper part deposited in Stage 5 15,16,20 .
The specimen was recovered from a medium-bedded well-indurated fine sand-to siltstone unit with simple trace fossils near the top of the Tatelt Formation in the Lemdad Syncline (Fig. 2B), in the Morocconus notabilis Zone (Fig. 3). This has been correlated to near the base of Cambrian Stage 5, possibly contemporaneous with Iberian Bilbilian/Leonian boundary and the Lapworthella Limestone (Ad) of the British Comley Series 18-20 .
Remarks. The new taxon can be assigned to Artiopoda based on the preserved ventral morphology 23 , notably the antenniform first appendage pair attached at either side of a strongly sclerotized ventral hypostome, followed by numerous pairs of homonomous walking legs that gradually decrease in size along the body, and the possession of hourglass-shaped sternites. In particular, hourglass-shaped sternites rule out comparisons with non-artiopodan Cambrian euarthropods -which lack sternites altogether -such as fuxianhuiids 24,25 , bivalved stem-group euarthropods 26,27 , megacheirans 28,29 , and marrellomorphs 30,31 . Although the presence of a first pair of antenniform limbs is symplesiomorphic within Deuteropoda Ortega-Hernández 32 (i.e. upper stem-group Euarthropoda + crown-group Euarthropoda) 33,34 , the combination of this character with post-oral limbs that gradually decrease in size and become differentiated into a caudal region (e.g. pygidium) are exclusive to Artiopoda. Remarks. Hou and Bergström 2 and Ramsköld et al. 3 independently proposed definitions of Xandarellida that differ somewhat in their emphasis on particular morphological characters. We follow the diagnosis provided by Ramsköld et al. 3 as this is based on a more comprehensive consideration of the organization of the cephalic appendages, hypostome morphology, and presence of segmental mismatch between the trunk limbs and tergites.
The similar style of preservation observed on the limbs and the hypostome strongly suggest that the new taxon lacked a biomineralized exoskeleton, and thus rules out potential affinities with Trilobita. The fossil is recognized as a member of Xandarellida based on similarities in limb morphology and possession of a natant hypostome associated with frontal organs (see detailed discussion below).
Xandarella Hou et al. 4 . Emended diagnosis. Semicircular head shield with small sessile eyes placed laterally. Suture or unfused overlap between shield portions extending from eye to lateral margin. Natant hypostome with elongate suboval outline. Head with antennae and up to six appendage pairs under large head shield; endopod of first post-antennal appendage reduced. Each tergite on anterior half of trunk covers a single pair of biramous appendages. Each succeeding tergite on posterior half of trunk covers an increasing number of appendage pairs, ranging from two to twelve (or more). Endopods slender, with up to a dozen podomeres. Pygidium with median posterior spine.
Remarks. The diagnosis of Xandarella has been revised from Hou et al. 4 and Hou and Bergström 2 to reflect the variability in the ventral morphology in this taxon, in light of the new specimen from Morocco (Fig. 4). The  Arthroaspis 40 ) as also expressed in several extant representatives, and generally resolved as the ancestral state for crown-group Euarthropoda 41 . By contrast, X. spectaculum and the new species described here are typified by the presence of post-antennal endopods with approximately 12 podomeres, leading us to propose this character as a diagnostic feature of Xandarella. A high podomere count is not exclusive to Xandarella among Palaeozoic euarthropods, however, as a similar condition is also known in some early Cambrian forms, such as megacheirans (e.g. Fortiforceps 2 ), fuxianhuiids (e.g. Fuxianhuia 24 ; Chengjiangocaris 25 ), and bivalved stem-group euarthropods (e.g. Jugatacaris 42 ). The substantial phylogenetic distance between these euarthropods and Xandarella (see topology in Legg et al. 43 ), however, suggests that endopods with more than seven podomeres are a symplesiomorphy of Deuteropoda 29,33,34,41 , and its occurrence within Xandarellida is most likely a result of homoplasy. Thus, the taxonomic utility of this character for Xandarella is only applicable within the context of Artiopoda. Xandarella mauretanica sp. nov. Figs 4 and 5.
Etymology. From the Latin mauretanicus, in reference to Mauretania, a historical region that corresponds to part of North Africa, including the Mediterranean coast of Morocco.
Diagnosis. Xandarellid with robust antennae, and a prominent hypostome with paired frontal organs located medially. At least 22 pairs of post-antennal limbs are present along the body. Endopod of first pair of post-antennal limbs half the length relative to that of the succeeding appendages. Description. The holotype is an articulated, and almost complete, individual with a total length of 21 mm (sagittal; including the antennae), and maximum width of 8 mm (transverse) (Fig. 4). The specimen represents an exceptionally preserved impression of the lightly sclerotized underside of the body, including appendages and ventral exoskeletal elements. Details of the dorsal exoskeleton, including cephalon and trunk tergite morphology, are entirely absent. The cephalic region incorporates a prominent hypostome with an elongate suboval outline (ca. 4 mm length, sag.; 1.8 mm maximum width, trans.), expressed as a deep concave impression, and typified by a medial transverse constriction that conveys an approximately lemniscate appearance. Two convex rounded structures (ca. 0.9 mm diameter) are associated with the medial constriction; these features are tentatively interpreted as a pair of frontal organs, simple ocelli-like structures found on the anterior region of various artiopodans 5,44 .
The frontal organs superficially bisect the hypostome. The anterior half has a slightly acute anterior margin and ) on the distal end of the 2 nd leg indicate podomeres that are of subequal length and width, or slightly longer than wide; similar impressions more proximally also indicate podomeres that are slightly longer than wide, suggesting the presence of up to a dozen podomeres per limb, at least on the cephalic region. The 4 th leg pair is slightly shorter than the preceding one (ca. 3 mm length, sag.), and is laterally splayed rather than flexed anteriorly. Unlike the 2 nd and 3 rd legs, the 4 th pair evinces a distal curvature towards the posterior end, which becomes more accentuated in the subsequent appendages. The subtle decrease in size and shift in appendage orientation suggest that the 4 th leg pair could correspond to the last set of cephalic appendages; if correct, this interpretation would imply that the head includes the antennae and four pairs of (arguably) biramous appendages. This interpretation may be supported by the fact that the 2 nd to 4 th legs display a regular separation of 1 mm (sag.), whereas the spacing between the succeeding pairs progressively decreases towards the posterior end of the specimen. The 5 th to 15 th legs have the same overall construction, consisting of a laterally oriented concave impression with a small posterior curvature at the distal end, and only differ slightly in their dimensions. Although the 5 th leg has an approximate length of 2.4 mm (sag.) and width of 0.6 mm (trans.), the same measurements are 1.6 mm (sag.) and 0.4 mm (trans.) for the 15 th leg, reflecting a gentle decrease in overall size towards the posterior end. This organization gives the appearance of a narrowed trunk relative to the anterior cephalic region, although this is mostly applicable to the proximal parts of the limbs, and thus there is no reason to assume that the dorsal exoskeleton would necessarily follow this morphology. The 16 th to 22 nd legs show a more drastic decrease in size resulting in a triangular tapering of the body; although the 16 th leg is only slightly shorter than the preceding limb (ca. 1.3 mm, sag.), the 22 nd leg is only expressed as a suboval impression of approximately 0.15 mm in length (sag.). This sharp change in appendage length may reflect the fusion of posterior segments into a discrete pygidium. The caudal termination of the trunk is not observed.
The only exoskeletal elements preserved on the ventral side -other than the hypostome -correspond to the sternite (i.e. ventral sclerotized plate) series, which occupies a longitudinal axial position between the limb pairs. Unlike the appendages, the sternite series is differentially preserved as a convex impression that reflects the pattern of segmentation through an alternating series of light and dark bands of sediment. The light bars are aligned with the appendage impressions and generally possess a narrower profile (trans.) relative to the dark bands; this disposition indicates that the bands represent the sternites and tendinous bars (i.e. intersegmental arthrodial membrane) respectively. The length of the individual sternites mirrors the spacing of the appendage pairs along the body, and thus the longest (sag.) are located between the 3 rd and 5 th legs, and become progressively shorter towards the rear termination of the body. Despite the gradual reduction in appendage size, the width of Remarks. X. mauretanica sp. nov. differs from X. spectaculum in that the 1 st leg pair in the former is distinctively reduced (Figs 4 and 5), whereas in the latter species these appendages follow a more gentle gradation in size with the succeeding cephalic legs 2,45 . X. spectaculum also differs in featuring up to 36 pairs of post-antennal leg pairs 2 , compared to the 22 leg pairs preserved in the new taxon. Whether this difference may be attributed to the preservation of X. mauretanica sp. nov., or if it reflects actual interspecific variability, remains uncertain. It is also possible that the different number of post-antennal legs can be attributed to ontogeny, as the holotype X. mauretanica sp. nov. is significantly smaller (length 21 mm, sag.) than type material of X. spectaculum (e.g. holotype, length 51 mm length, sag. 2 ). Clarification on these issues will require the input of additional material of X. mauretanica sp. nov., or studies on the ontogeny of X. spectaculum.

Discussion
Phylogenetic affinities. Although only details of the ventral anatomy are preserved in the available material, the similarities between X. mauretanica sp. nov. and X. spectaculum support their close phylogenetic affinities, and offers new insights on the morphological variability within Xandarellida. The new taxon confirms the presence of hourglass-shaped sternites connected by intersegmental tendinous bars -previously suggested 2 or inferred 3 for members of Xandarellida -similarly to the ventral exoskeletal anatomy of other artiopodans 36,38,46,47 . The appendicular organization in X. mauretanica sp. nov. and X. spectacullum share various symplesiomorphies of Artiopoda, most notably the presence of antennae at either side of a sclerotized hypostome, the homonomous construction of the post-oral appendages, and the progressive reduction in size of the legs towards the posterior end of the body. However, the presence of post-antennal endopods with approximately 12 podomeres is unique to Xandarella within the evolutionary context of Artiopoda 48 .
These comparisons are further strengthened by the presence of a natant hypostome in X. mauretanica sp. nov. and X. spectaculum. Several Cambrian artiopodans possess a concomitant hypostome that is widely attached to the anterior margin of the cephalon, and may be expressed as an extension of the cephalic doublure with or without a suture (e.g. Triarthrus 36 ; Emeraldella 23 ; Squamacula 49 ; Aglaspis 48 ) (Fig. 6B,C) or occur in association with an anterior sclerite (e.g. Conciliterga 2,44 ; see also char. 12 in Edgecombe and Ramsköld 5 ). By contrast, the natant hypostome of Xandarellida is situated further back, in a position closer to the sagittal midline of the head 2,3 . Although the natant hypostome is also known in various non-trilobite artiopodans (e.g. Cheloniellon 35 ; Nektaspida 10,38 ; Campanamuta 50 ; Arthroaspis 40 ) (Fig. 6A), none of these taxa combine this character with the presence of endopods with more than seven podomeres as observed in Xandarella.
The ventral anatomy of X. mauretanica sp. nov. is broadly comparable to that of Cindarella eucalla in terms of overall appendage organization. However, these taxa differ in that the 1 st leg pair of the latter is not reduced 3 , and the hypostome of the former is more elongate and bears the paired frontal organs (Figs 4 and 5); the endopods of C. eucalla also differ in evidently having archetypal endopods with seven podomeres 3 . Comparisons with the recently described xandarellid Luohuilinella rarus are problematic because this taxon is only known from the dorsal exoskeleton 6 . However, the posterior end of the body in X. mauretanica sp. nov. and L. rarus exhibits a sharp Ortega-Hernández et al. 71 Lerosey-Aubril et al. 61 Bivalved stem euarthropods none Van Roy et al. 54 Yang et al. 75 García-Bellido et al. 26 Briggs 76 Fu and Zhang 42 Legg and Caron 27 Conciliterga none none Hou and Bergström 2 Paterson et al. 9 Whittington 51 Ortega-Hernández 44 Marrellomorpha none Van Roy et al. 56 Liu 78 none García-Bellido and Collins 30 Legg 77 Megacheira none Van Roy et al. 54 Chen et al. 79 Edgecombe et al. 81 Haug et al. 28 Liu et al. 80 Paterson et al. 55 Aria et al. 29 Mollisoniida none Van Roy et al. 56 Zhang et al. 65 none Walcott 82 Nektaspida none Van Roy et al. 54 Zhang et al. 38 Paterson et al. 10 Walcott 82 Whittington 58 Xandarellida this study none Ramsköld et al. 3 none none Zhang et al. 6 Xenopoda none none Zhang et al. 63 Edgecombe et al. 66 Stein and Selden 23 Stein 39  decrease in width that produces a distinctive subtriangular caudal tapering, which is otherwise not observed in either X. spectaculum or C. eucalla 2,3 , or other non-trilobite artiopodan groups (e.g. Cheloniellida 35 ; Conciliterga 51 ; Nektaspida 38 ; Xenopoda 23 ). Outside the Xandarellida, the morphology of X. mauretanica sp. nov. shares similarities with the petalopleuran Sinoburius lunaris 4 . With the exception of the 1 st leg pair in X. mauretanica sp. nov., the cephalic appendages of both taxa are noticeably longer than those in the trunk region; however, the possibility that this appearance in the new taxon may be a taphonomic artefact cannot be entirely discarded at present given the preferential preservation of the proximal portion of the appendages (Fig. 4). S. lunaris may further resemble X. mauretanica sp. nov., in the possession of four legs in the head region, yet again, assuming that the extrapolation of the cephalic shield based on the anatomy of the anterior appendages is correct. The preservation of S. lunaris only reveals the outline of the endopods, and thus the number of constituent podomeres is uncertain. Less cryptically, the paired frontal organs in the hypostome of X. mauretanica sp. nov. draw a parallel to similar structures in S. lunaris 2,5 , although the natant hypostome in the latter taxon is comparatively smaller and has a subtriangular outline. The frontal organs of S. lunaris appear to be located in a slightly anterior position relative to the hypostome, however, and thus it is uncertain if they reflect an identical organization to that observed in X. mauretanica sp. nov. The pygidial segmentation of S. lunaris also displays a sharp decrease in limb size, comparable to that of X. mauretanica sp. nov. (Fig. 4) and L. rarus 6 .
Taphonomic implications. The preservation of X. mauretanica sp. nov. is noteworthy in comparison to other xandarellid specimens, and indeed to other soft-bodied Cambrian euarthropods. Previously described xandarellid fossils from the Chengjiang biota are expressed as pyritized carbonaceous compressions in shale, as is typical for non-trilobite euarthropods 52 . The holotype of X. mauretanica sp. nov. is three-dimensionally preserved in a fine sand-to siltstone (Fig. 4) and was probably pyritized during early diagenesis, which would account for the exceptional preservation of the lightly sclerotized ventral morphology; however, the appearance of the fossil strongly suggests a more recent exposure to oxidation and intense weathering. This peculiar style of three-dimensional preservation contrasts with that of Burgess Shale-type Cambrian deposits in Laurentia, consisting of flattened carbonaceous films 53 , and also with the non-biomineralized euarthropods from the Early Ordovician Fezouata biota of Morocco 54 . Thus, the taphonomy of the fossils at the Tatelt Formation requires further investigation, but demonstrates that soft-bodied Burgess Shale-type euarthropods can be found in atypical sedimentological settings.
Stratigraphic and palaeobiogeographic significance. The discovery of X. mauretanica sp. nov. from the middle Cambrian Tatelt Formation in the High Atlas Mountains of Morocco provides the youngest known record of xandarellids, extending their stratigraphic range by approximately 10 million years. More significantly, this finding substantially expands the palaeobiogeographic and palaeolatitudinal range of Xandarellida out of tropical South China (Chengjiang biota) and onto polar Gondwana at high southern latitudes during the Cambrian (Fig. 7). Given that xandarellids are not known from the early Cambrian (Stage 4) Emu Bay Shale in South Australia 11,55 , X. mauretanica sp. nov. represents the only direct connection between communities of non-biomineralized artiopodans in continental Gondwana (North Africa) and South China (Chengjiang biota) during the Cambrian (Fig. 7). The close palaeobiogeographical links between Morocco and South China only become evident later on during the latest Tremadocian (Lower Ordovician) thanks to the euarthropod diversity preserved in the Fezouata biota, which includes representatives of several typically Cambrian groups such as marrellomorphs, leanchoiliids, mollisoniids, nektaspids and aglaspidids 54,56,57 (Table 2). This raises the possibility that Burgess Shale-type euarthropod communities in Gondwana are not necessarily restricted to the Emu Bay Shale in South Australia, but that they may also extend to the early Cambrian of Morocco.
The discovery of X. mauretanica sp. nov. draws attention to the absence of xandarellids from several Cambrian Burgess Shale-type faunas in North America (Fig. 7) (Table 2). Given the intense efforts invested in the systematic description of non-biomineralized Cambrian euarthropods from Laurentia over the last 50 years, the absence of xandarellids from this palaeocontinent may reflect a real palaeobiogeographic signal, rather than an artefact of taphonomic or collection bias. Future work on the Tatelt Formation offers great potential for the discovery of additional exceptionally preserved fossils in the middle Cambrian of Morocco that will help further refine the palaeobiogeographic and stratigraphic distribution of Burgess Shale-type faunas.

Materials and Methods
A single available specimen collected from the upper Tatelt Formation (Morocconus notabilis Zone) of Morocco. Specimen MHNM-HA-TT-CA-1A corresponds to the external mould of the ventral side of the body in dorsoventral view, preserved in a medium-bedded well-indurated mudstone and sandstone unit. Photographs were taken with a Nikon 3100 DSLR. The material is housed at the MHNM (Natural Museum History of Marrakesh).