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A fourteen-faced hexangulaconulariid from the early Cambrian (Stage 2) Yanjiahe Formation, South China

Published online by Cambridge University Press:  07 August 2019

Junfeng Guo
Affiliation:
School of Earth Science and Land Resources, Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, P.R. China , <2695489023@qq.com>, <757542074@qq.com>, <512718116@qq.com>
Jian Han*
Affiliation:
Shaanxi Key Laboratory of Early Life and Environment, State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, 229 Taibai Road, Xi'an 710069, P.R. China , <799179701@qq.com>,
Heyo Van Iten
Affiliation:
Department of Geology, Hanover College, Hanover, IN 47243, USA and Department of Invertebrate Paleontology, Cincinnati Museum Center, 1301 Western Avenue, Cincinnati, Ohio 45203, USA
Xing Wang
Affiliation:
Shaanxi Key Laboratory of Early Life and Environment, State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, 229 Taibai Road, Xi'an 710069, P.R. China , <799179701@qq.com>,
Yaqin Qiang
Affiliation:
School of Earth Science and Land Resources, Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, P.R. China , <2695489023@qq.com>, <757542074@qq.com>, <512718116@qq.com>
Zuchen Song
Affiliation:
School of Earth Science and Land Resources, Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, P.R. China , <2695489023@qq.com>, <757542074@qq.com>, <512718116@qq.com>
Wenzhe Wang
Affiliation:
School of Earth Science and Land Resources, Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, P.R. China , <2695489023@qq.com>, <757542074@qq.com>, <512718116@qq.com>
Zhifei Zhang
Affiliation:
Shaanxi Key Laboratory of Early Life and Environment, State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, 229 Taibai Road, Xi'an 710069, P.R. China , <799179701@qq.com>,
Guoxiang Li
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, P.R. China
*
*Corresponding author.

Abstract

Extant medusozoans (phylum Cnidaria) are dominated by forms showing tetraradial symmetry, but stem-group medusozoans of early Cambrian age collectively exhibit tetra-, bi-, penta-, and hexaradial symmetry. Moreover, the developmental and evolutionary relationships between four-fold and other types of radial symmetry in medusozoans remain poorly understood. Here we describe a new hexangulaconulariid, Septuconularia yanjiaheensis new genus new species, from Bed 5 of the Yanjiahe Formation (Cambrian Stage 2) in the Three Gorges area of Hupei Province, China. The laterally compressed, biradially symmetrical periderm of this species possesses 14 gently tapered faces, the most of any hexangulaconulariid described thus far. The faces are bordered by longitudinal ridges and crossed by short, irregularly spaced transverse ribs. Longitudinally, the periderm consists of three regions that probably correspond, respectively, to an embryonic stage, a transient juvenile stage, and a long adult stage. Septuconularia yanjiaheensis may have been derived from six-faced Hexaconularia (Fortunian Stage), which is morphologically intermediate between Septuconularia yanjiaheensis and Arthrochites. Furthermore, conulariids sensu stricto, carinachitids, and hexangulaconulariids may constitute a monophyletic group united by possession of an organic or organophosphatic periderm exhibiting longitudinal (corner) sulci, a facial midline, and offset of transverse ribs along the facial midline.

UUID: http://zoobank.org/01a972aa-aef3-4eef-a9a5-c2d8c3dda615

Information

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Articles
Copyright
Copyright © 2019, The Paleontological Society 
Figure 0

Figure 1.Location and stratigraphy of the Terreneuvian (Cambrian Stage 2) Yanjiahe Formation in the Three Gorges area near Yichang, Hubei Province, China. (1) Sketch map of the People's Republic of China, showing the position of the collecting locality in Hubei Province. (2) Simplified geological map of the Three Gorges area, Hubei Province, showing outcrops of Cambrian strata (gray box in the Yanjiahe area denotes area enlarged for additional details). (3) Detailed geological map of the Yanjiahe area, showing outcrops of the Yanjiahe Formation. (4) Stratigraphic sequence of lower Cambrian strata in the Yanjiahe section, Yangtze Gorges area, indicating the horizons where specimens of Septuconularia yanjiaheensis n. gen. n. sp. were collected.

Figure 1

Figure 2.Septuconularia yanjiaheensis n. gen. n. sp. from the lower Cambrian (Stage 2) Yanjiahe Formation (Bed 5) in the Three Gorges area near Yichang, Hubei Province, China. (1, 2) Side view of the holotype, CUBar90-4; (3–6) CUBar38-2; (7–9) CUBar9-2; (10–14) CURBar5. (15–17) Longitudinal subdivision of the periderm from the base adapertureward into three parts corresponding to the embryonic, juvenile, and adult stages, respectively. (15) CUBar2-1; (16) CUBar9-6; (17) CUBar38-7. aab = apical-abapical boundary; abr = abapical region; am = apertural margin; ap = aperture; apr = apical region; as = adult stage; cf = central face; es = embryonic stage; js = juvenile stage; lf = longitudinal furrow; lfs = lateral faces; lmg = longitudinal median groove; lr = longitudinal ridge; mf = marginal face; tr = transverse rib.

Figure 2

Figure 3.S. yanjiaheensis as for the species by monotypy from the lower Cambrian (Stage 2) Yanjiahe Formation (Bed 5) in the Three Gorges area near Yichang, Hubei Province, China. (1–15) CUBar119-12, CUBar115-31, CUBar9-7, CUBar99-2, CUBar60-4, CUBar38-8, CUBar115-38, CUBar99-9, CUBar99-8, CUBar90-6, CUBar9-1, CUBar38-1, CUBar99-1, CUBar79-1, CUBar10-23, respectively. All photos share the same scale bar to illustrate hypothesized extensional growth of the periderm by addition of transverse ribs.

Figure 3

Table 1.Measurements of S. yanjiaheensis as for the species by monotypy.

Figure 4

Figure 4.Micro-CT tomography of the holotype specimen (CUBar90-4) of Septuconularia yanjiaheensis n. gen. n. sp. (1) 3D volume rendering of the periderm; (2) virtual intersection along the maximum width and the oral–aboral axis of the periderm; (3) virtual intersection close to the minimum width along the oral–aboral axis; (4) virtual horizontal intersection at the level indicated by 4' in (1); (5) virtual horizontal intersection at the level of the boundary between the apical and abapical regions. Scale bars = 100 μm.

Figure 5

Table 2.Measurements of Hexaconularia sichuanensis. NXC9-01 quoted from Steiner et al. (2004, fig. 8.1); He22–99 from Steiner et al. (2014, fig. 7.20); GMPKU3132, GMPKU3134, and GMPKU3135 from Duan et al. (2017, fig. 5(a), (f), (h)); NIGP160430 from Xian et al. (2018, fig. 3A); NIGP150159, NIGP150161, and NIGP150162 from Van Iten et al. (2010, text-fig. 1A, D, E). Other specimens from early Cambrian Kuanchuanpu Formation in Ningqiang and Hexi section (provided by J. Han).

Figure 6

Figure 5.Scatter diagrams for selected aspects of the gross morphology of Septuconularia yanjiaheensis n. gen. n. sp. (1) Linear relationship between the maximum width and the longitudinal height of the periderm; (2) linear relationship between the longitudinal height and the number of transverse ribs per 1 mm on a peridermal face.

Figure 7

Figure 6.Comparisons of the apical angles of the central face between Septuconularia yanjiaheensis n. gen. n. sp. and Hexaconularia sichuanensis. (1) Bar chart showing apical angles of adult specimens; (2) bar chart showing apical angles of the central face.

Figure 8

Figure 7.Three-dimensional reconstructions of Septuconularia yanjiaheensis n. gen. n. sp. with hypothetical aperture, highlighting key anatomical features and terms used herein. (1–3) Lateral, oral, and oblique lateral views, respectively. aab = apical-abapical boundary; abr = abapical region; am = apertural margin; ap = aperture; apr = apical region; as = adult stage; cf = central face; es = embryonic stage; js = juvenile stage; lf = longitudinal furrow; lfs = lateral faces; lmg = longitudinal median groove; lr = longitudinal ridge; mf = marginal face; tr = transverse rib.

Figure 9

Figure 8.Phylogenetic hypothesis for carinachitiids, olivooids, hexangulaconulariids, and conulariids.

Supplementary material: Link

Guo et al. Dataset

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