Fuxianhuiida Bousfield, 1995
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publication ID |
https://doi.org/10.4202/app.00508.2018 |
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persistent identifier |
https://treatment.plazi.org/id/781E87C5-4C08-FFE2-6233-FA20FBF63AD7 |
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Felipe |
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Fuxianhuiida Bousfield, 1995 |
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Order Fuxianhuiida Bousfield, 1995 Family Fuxianhuiidae Hou and Bergström, 1997
Emended diagnosis.—Fuxianhuiid with a subtrapezoidal cephalic carapace at least 2–2.8 wider than long, covering a prothorax composed of three tergites. The remaining trunk is divided into an anterior, limb-bearing, opisthothorax with well developed, subtriangular pleural margins, and a caudal, limbless abdomen, the posteriormost segment of which is elongate and subtriangular. Endopods with a rounded termination (emended from Yang et al. 2018).
Remarks. —A sister-taxon relationship between Guangweicaris and Fuxianhuia is well established ( Yang et al. 2008, 2018; Legg et al. 2013), as is a sister-taxon relationship between Fuxianhuiidae and Chengjiangocarididae ( Legg et al. 2013; Yang et al. 2018) and so does not need discussing further, however, the diagnostic features of the Fuxianhuiidae , as presented in Yang et al. (2018) are in need of emendation based on new observations made herein. The latter stated the length to width ratio of the head shield (carapace herein sensu Chen et al. 2018), to be 1: 4. Whilst this is true of some specimens attributed to species of Fuxianhuia (DAL personal observation), this is not the case for Guangweicaris , which has a ratio closer to 1: 2.5. This is still greater than that observed in chengjiangocaridids, however, and so is emended rather than deleted from the diagnosis of this group. Likewise, Yang et al. (2018) stated that the endopods of fuxianhuiids did not extend beyond the pleural margins of the parent tergite and/or carapace, however, this feature could not be actually and accurately determined for Guangweicaris as appendages are rare, and when present, appear to extend beyond the tergite lateral margins, although it is unclear if this is a genuine feature or due to post-mortem detachment.
Genus Guangweicaris Luo, Fu, and Hu in Luo et al., 2007
Type species: Guangweicaris spinatus Luo, Fu, and Hu in Luo et al., 2007; Gaoloufang section, China, Cambrian Series 2, Stage 4, by monotypy .
Emended diagnosis.—As for type species by monotypy, see below.
Remarks.—The diagnosis of Yang et al. (2008), although accurate, is lacking a number of features that have been discovered herein, in particular, the presence of a cephalic bulge, a pair of SPAs and a tripartite hypostome; subpentagonal spines on the opisthothoracic appendage podomeres, a set of posteroventral spines on the terminal abdominal segment, and a subtriangular telson.
Guangweicaris spinatus Luo, Fu, and Hu in Luo et al., 2007
1999 Habelia ? sp.; Luo et al. 1999: 39, pl. 31: 10, 11.
2007 Guangweicaris spinatus sp. nov.; Luo et al. 2007: 6–7, pl. 1: 1–6, pl. 2: 1–6.
2008 Guangweicaris spinatus Luo, Fu and Hu, 2007 ; Luo et al. 2008: 84–85, pl. 24: 1–6.
2008 Guangweicaris spinatus Luo, Fu and Hu, 2007 ; Yang et al. 2008: 117–119, text-figs. 2–4, pl. I: A–F.
2010 Guangweicaris spinatus Luo, Fu and Hu, 2007 ; Hu et al. 2010: 1769, text-fig. 4a.
2013 Guangweicaris spinatus Luo, Fu and Hu, 2007 ; Hu et al. 2013: 106–109, text-figs. 133–138.
2013 Guangweicaris spinatus Luo, Fu and Hu, 2007 ; Edgecombe and Legg 2013: 396.
2016 Guangweicaris spinatus Luo, Fu and Hu, 2007 ; Liu et al. 2016: 1940, text-fig. 2e, f.
2018 Guangweicaris spinatus Luo, Fu and Hu, 2007 ; Chen et al. 2018: 553.
2019 Guangweicaris spinatus Luo, Fu and Hu, 2007 ; Wu and Liu 2019: 543–548, text-figs. 1–3.
Type material: Holotype: YIGS Kgs-1-26 (SOM: fig. 1A), two prothoracic segments, five opisthothoracic segments, and seven abdominal segments, without preserving the carapace and tail . Paratypes: YIGS Kgs-1-36, 37, 62. In addition to the type material, Luo et al. (2007) noted 101 specimens of this species, the majority of which are poorly preserved and incomplete, some of them are figured herein ( Figs. 1B, C View Fig , 2A View Fig ; SOM: fig. 1B–E) .
Type locality: Specimens were collected from a short interval, roughly 5 m thick, of yellowish-brown mudstone, located in the vicinity of Guangwei village within the Gaoloufang section, Kunming, Yunnan Province, southwest China .
Type horizon: Palaeolenus Trilobite Zone of the Wulongqing Member (Canglangpu Formation), Cambrian Series 2, Stage 4, which is dated 513–512 million years old ( Hou et al. 2017).
Additional material.— Since the initial description of this species, twelve additional specimens have been described and figured including YKLP 11564–11568 ( Yang et al. 2008), NIGPAS Kgs-1-137, prior to preparation ( Luo et al. 2008), and NIGPAS Kgs-6-108, NIGPAS Kgs-1-137, and an unnumbered NIGPAS specimen, after preparation ( Hu et al. 2013), and ELI-LBSG-0006B, 0046A, 0047, 0022B ( Wu and Liu 2019). To this we add 51 specimens: YKLP 11140– 11188, 11201, 11202. All from Gaoloufang section, China, Cambrian Series 2, Stage 4. Another specimen assigned to Guangweicaris spinatus by Hu et al. (2013: 108, fig. 135) does not actually belong to this taxon, and may instead belong to the “trilobitomorph” Longquania bispinosa Luo and Hu in Luo et al., 2008 (see Remarks).
Diagnosis.— Fuxianhuiid possessing a wide carapace with a medial cephalic bulge; a pair of specialized post-antennal appendage and a tripartite hypostome; an opisthothorax composed of five segments, the posterior four of which possess an extensive posteromedial axial spine and posterolateral spinose extensions of the pleurae; opisthothoracic appendages composed of, at least, 11 podomeres, each bearing a subpentagonal spine; an abdomen consisting of seven tergites all bearing a posteromedial axial spine and a terminal abdominal segment bearing a subtriangular telson, two pairs of posteroventral spines, and a pair of lateral, phylliform processes (emended from Yang et al. 2008).
Description. —Carapace: The carapace ( Figs. 3A 1 View Fig , 4A View Fig 1, B, D 1 View Fig ) is subreniform in outline with a broad anterior margin, and widely curved lateral margins, which abruptly change angle at their postero-lateral edge, resulting in an acute margin that then curves gently towards the posteromedial axis. The carapace is between 2.0 and 2.8 times wider than long (SOM: table 1), with most variation in aspect ratio caused by differences in burial orientation, which also causes the anterior margin to appear more strongly curved in some specimens (cf. Figs. 3A 1 View Fig and 4B View Fig ). Lateral wrinkling (see for examples Figs. 3A 1 View Fig and 4D View Fig 1 View Fig ), is no doubt the result of compaction, indicating the anterior-medial area of the carapace was somewhat bulbous. A medial hinge or suture is lacking. It is unclear, due to a lack of ventrally preserved specimens, if a marginal doublure is present. The posterior margin of the carapace entirely covers the prothoracic segments and overlaps the anterior margin of the first opisthothoracic tergite ( Fig. 3A 1 View Fig ).
Trunk: The trunk is divided into three distinct sections, or pseudotagmata: a prothorax composed of three segments, an opisthothorax bearing five segments, and finally an abdomen of seven segments ( Fig. 1A View Fig ). The anterior-most prothoracic tergite is the least commonly preserved; it is very small, measuring about half the length and a third the width of the second tergite (SOM: table 2), and almost semi-circular in outline ( Fig. 1A, B View Fig ). The second tergite is subtrapezoidal with a slightly bowed anterior, and expansive and rounded lateral margins ( Fig. 1A, B, D View Fig ). The third and final prothoracic tergite curves around the second tergite resulting in an almost trapezoidal outline with anteriorly deflected posterolateral margins ( Fig. 1A, B, D, E View Fig ). The second tergite is roughly two thirds the length, and three quarters the width of the third prothoracic tergite (SOM: table 2). The third prothoracic tergite is nestled within the anteriomedial margin of the first opisthothoracic tergite, and is the widest prothothoracic tergite ( Fig. 1A, B, D, E View Fig ).
The first opisthothoracic segment is over twice as wide as the preceding tergite, and between two and three times as long (SOM: table 2). It is almost semi-circular in outline ( Fig. 1A, B View Fig ). Its rounded lateral margins slope away from anterior tergal boundary at roughly 50°, before terminating at an acute posterolateral edge ( Fig. 1A, B View Fig ). Although the posterior margin of the first opisthothoracic tergite is often poorly preserved ( Fig. 1D, E View Fig ), presumable occurring during excavation and preparation, well preserved specimens indicate that it was relatively straight and featureless (e.g., Fig. 1B View Fig ). The lateral margins of the second opisthothoracic tergite are contiguous with those of the preceding segment Fig. 1A View Fig ).
Isolated opisthothoracic tergites demonstrate that the anterior margins were relatively straight ( Fig. 1C View Fig ), with an observed medial deflection attributable to deformation caused by post-burial compression. With only a few exceptions, which can be attributed to taphonomic variance, the second opisthothoracic tergite is always the widest (SOM: table 3). The second opisthothoracic tergite is only a fraction larger than the adjacent tergites, with a more pronounced decrease in width occurring in tergites 4 and 5. The latter measures just two-thirds the width of the second tergite (SOM: table 3). Like the first opisthothoracic tergite, the lateral margins of the remaining opisthothoracic tergite are rounded, however, unlike the former their posterolateral margins are extended into a small subtriangular spine Fig. 1A, C–E View Fig ). The second opisthothoracic tergite, and all more posterior tergites, possess an extensive medial axial spine ( Fig. 1A, C–E View Fig ). These spines are often broken in dorsally preserved specimens, and are best observed in laterally preserved specimens, e.g., YKLP 11140 ( Fig. 1D View Fig ), and YKLP 11162 ( Fig. 1E View Fig ). These specimens reveal that the longest axial spines typically belong to the second opisthothoracic tergite, with successive tergal spines progressively decreasing in length. The fifth axial tergal spine measures roughly 60% the length of the first (SOM: table 4). Both the observed length of the axial spines and their angle of deflection, measured along the posterior spine margin, are controlled by their angle of burial, appearing shorter and more posteriorly arched in obliquely preserved specimens cf. Fig. 1A, D View Fig ). The angle of posterior deflection typically measuring between 130–150° (compared to the dorsum of parent tergite), with the more posterior spines showing a greater degree of displacement (SOM: table 4).
The abdomen is defined by an abrupt change in width compared to the preceding tergite, typically measuring 60– 80% of the fifth opisthothoracic tergite (SOM: table 3). As with all post-prothoracic tergites, the first abdominal tergite possesses a posteromedial axial spine ( Fig. 1A, E View Fig ). The posterior margin of this tergite, and the following abdominal tergites, curve in a posteromedial orientation towards this spine ( Fig. 1A View Fig ). This spine is typically longer than that of the preceding tergite and with an increased posterior deflection SOM: table 4). The terminal abdominal spine measured nearly three times the length of the first abdominal spine SOM: table 4). Posterior spines also show a greater degree of posterior deflection, ranging 120–140° from the anterior tergites to the posterior (SOM: table 4). This is taken to the extreme in the terminal abdominal tergite, in which the main body of the tergite is more than twice as long as the preceding tergite (SOM: tables 3, 4), and the accompanying spine is orientated parallel to the dorsum of its parent tergite ( Fig. 2 View Fig ). The terminal abdominal segment preserved in lateral aspect and demonstrates that at least one spinose process ( Fig. 2A, B View Fig , arrows) occurs on the posteroventral margin. Such processes also appear to be present in YKLP 11566 ( Fig. 2C View Fig ), where two pairs of triangular spines consisting of an enlarged outer spine ( Fig. 2C 2 View Fig , C 3, white arrows), and a subordinate inner spine ( Fig. 2C 2 View Fig , C 3, black arrows), are present on the posteroventral margin.
Telson and associated structures: YKLP 11566 ( Fig. 2C View Fig ) is also significant in possessing a ventral medial, subtriangular extension, presumably a telson under the posterodorsal spine. This structure, and the associated spine, were previously identified as the furcae of a “tail” (lateral processes sensu Chen et al. 2018), by Yang et al. (2008), however, the medial extension is in fact flanked by two, albeit poorly preserved, phylliform projections, herein interpreted as lateral processes, comparable to those in other specimens ( Fig. 2C View Fig ). These processes are each associated with the aforementioned pair of triangular spines.
Eyes: The eyes, and associated structures, are preserved in a single specimen, YKLP 11141 ( Fig. 3A 1 View Fig , A 2 View Fig ). The eyes are small and ovoid, measuring just 1.25 mm, along their widest axis, compared to the carapace width, which is 21 mm. The left eye is the better preserved, although it is doubtful if an associated structure represents the right eye that appears to be attached to a small, subrectangular eyestalk ( Fig. 3A 2 View Fig ), although the base of this structure is poorly preserved. Anterior sclerite ( Figs. 3A 1 View Fig , 4A View Fig 1 View Fig , A 2 View Fig ) could be recognised and partially covered by a carapace. Unlike, other fuxianhuiids, it appears that the eyes did not project far beyond the anterior of the carapace.
Head appendages: Like other fuxianhuiids, G. spinatus possessed two pairs of post-ocular head appendages. Antennae are present in four specimens ( Fig. 3A 1 View Fig , 4A View Fig 1, B, D 1 View Fig ), and it consists of at least 21 podomeres ( Fig. 4B View Fig ). The proximal podomeres are wider than long, with successive podomeres becoming smaller and gradually more elongate, resulting in a more rectangular shape in the distal segments, accompanied by a reversal in the length to width ratio when compared to the proximal elements ( Figs. 3A 1 View Fig , 4B View Fig ). Accessory antennal spines, or setae are not present in the described material. A tripartite hypostome and a pair of specialized post-antennal appendages forming the mouth part are well preserved in only one specimen ( Fig. 4A View Fig ), where the carapace is completely separated from the head appendages. Posterior to the anterior sclerite is a large boomerang-shaped region. The middle area of the hypostome is subrhombic, and the lobes on both sides ( Fig. 4A View Fig 2 View Fig , white arrows) are suboval. The mouth opening is expected to situate at the posterior margin of the hypostome, where indications of tiny teeth can be observed ( Fig. 4A View Fig 2 –A View Fig 4 View Fig ). A pair of robust appendages, the so-called SPAs ( Fig. 4A View Fig 2 View Fig , A 3), are partly covered the hypostome. The medial margin of the basal podomere appears spinose ( Fig. 4A View Fig 2 –A View Fig 4 View Fig ). Possible section is in SPA ( Fig. 4A View Fig 2 View Fig , black arrow). The proximal and middle part is transverse, and the distal part is curved backwards.
Trunk appendages: Biramous trunk appendages are preserved in seven specimens, of which five are figured herein ( Figs. 1D View Fig , 3A 1 View Fig , 4B–D View Fig ). The endopod of every biramous trunk appendage is composed of 11 podomeres ( Fig. 4D View Fig 2 View Fig ). Most podomeres are subrhombic to subtrapezoidal, each possessing a medial, subpentagonal spine ( Fig. 4B, C View Fig , white arrowheads). The distal podomere, by contrast, is in subtriangular shape and without a spine ( Fig. 4C View Fig , black arrow). Due to different angles of compression, nodes instead of spines are observed in other specimens ( Fig. 4D View Fig 2 View Fig , white arrowheads). The most proximal part of the appendage is only partly revealed, being hidden by the proceeding appendage. The anterior appendages ( Fig. 4B View Fig , white arrows) are presumably derived from the prothoracic segments, with the lager, succeeding appendages ( Fig. 4B View Fig , black arrows) presumably derived from the first and second opisthothoracic segments, akin to the arrangement seen in other fuxianhuiids (see for example Yang et al. 2013). More posterior appendages become shorter, progressively. The number of attachments at the proximal podomeres of appendages indicates that each opisthothoracic segment possesses two pairs of appendages ( Fig. 4B, C View Fig , black arrowheads). Flaps indicating exopods can be observed in two specimens ( Figs. 3A 3, 4B View Fig ). Apart from these, no more evidence for the exopod is observed in our material.
The new information presented herein was used to produce a new reconstruction of Guangweicaris spinatus Fig. 5 View Fig ).
Remarks.—A total of five specimens, which now form part of the type series of Guangweicaris spinatus , were originally attributed to Habelia sp. ( Luo et al. 1999: pl. 31). Of these, three, Kg-f-1-55–57, were derived from the Gangtoucun section of the Wulongqing Member, whilst the others, Yl-f-1-12 and Yl-f-1-13, came from Lihuazhuang in Yiliang County. ELI-XLC-GS0042 figured by Liu et al. (2016: fig. 2e, f), and ELI-XLCG-0022B by Wu and Liu (2019: fig. 1B) was reported from the Xinglongcun section of the Wulongqing Formation. Whilst undertaking this study it became apparent that a specimen ( Hu et al. 2013: 108, fig. 135) formerly attributed to G. spintus belongs to a different species. This specimen has several unique features that are not present in G. spintus : (i) a notch in the carapace; (ii) three slightly shortened segments exposed behind its carapace, with the third one bearing pleural processes; (iii) lack of narrower abdomen segments; (iv) long and thin pleurae; (v) lack of enlarged axial spines on the trunk tergites. These differences suggest an assignment of the specimen to Longquania bispinosa Luo and Hu in Luo et al., 2008, but further studies are required to confirm this suggestion.
Stratigraphic and geographic range.—Wulongqing Member, Canglangpu Formation, Cambrian Series 2, Stage 4, Yunnan province, China.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Fuxianhuiida Bousfield, 1995
| Chen, Hong, Legg, David A., Zhai, Da-You, Liu, Yu & Hou, Xian-Guang 2020 |
Guangweicaris spinatus Luo, Fu and Hu, 2007
| Wu, Y. & Liu J. 2019: 543 |
Guangweicaris spinatus Luo, Fu and Hu, 2007
| Chen, A. & Chen, H. & Legg, D. A. & Liu, Y. & Hou, X. 2018: 553 |
Guangweicaris spinatus Luo, Fu and Hu, 2007
| Liu, J. & Han, J. & Li, J. & Wu, Y. & Peng, J. & Qi, N. & Yang, Y. & Li, J. 2016: 1940 |
Guangweicaris spinatus Luo, Fu and Hu, 2007
| Hu, S. & Zhu, M. & Luo, H. & Steiner, M. & Zhao, F. & Li, G. & Liu, Q. & Zhang, Z. 2013: 106 |
Guangweicaris spinatus Luo, Fu and Hu, 2007
| Edgecombe, G. D. & Legg, D. A. 2013: 396 |
Guangweicaris spinatus Luo, Fu and Hu, 2007
| Hu, S. & Zhu, M. & Steiner, M. & Luo, H. & Zhao, F. & Liu, Q. 2010: 1769 |
Guangweicaris spinatus Luo, Fu and Hu, 2007
| Luo, H & Li, Y. & Hu, S. & Fu, X. & Hou, S. & Liu, X. & Chen, C. & Li, F. & Pang, J. & Liu, Q. 2008: 84 |
Guangweicaris spinatus Luo, Fu and Hu, 2007
| Yang, J. & Hou, X. & Dong, W. 2008: 117 |
Guangweicaris spinatus
| Luo, H. & Fu, X. & Hu, S. & Li, Y. & Hou, S. & You, T. & Pang, J. & Liu, Q. 2007: 6 |
Habelia
| Luo, H. & Hu, S. & Chen, L. & Zhang, S. & Tao, Y. 1999: 39 |
