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    Available online:January 05, 2024, DOI: 10.19800/j.cnki.aps.2023013
    [PDF 5.70 M] (10914)
    Abstract:
    The Carboniferous strata are widely exposed around the Junggar Basin in northern Xinjiang, among which parts of the Upper Carboniferous consist of marine volcanic-sedimentary sequences, including the Halaalate and Aladeyikesai formations in the West Junggar region, the Shiqiantan Formation in the East Junggar region, and the Qijiagou and Aoertu formations in the southern part of the basin. In this study, nine genera and seventeen species of rugose corals as well as two genera and three species of tabulate corals were obtained from the limestone beds or interbeds and siliciclastic rocks in the abovementioned strata. Three new dissepimented solitary rugose coral species were described from the Shiqiantan Formation. The geological age of these corals ranges mainly from Bashkirian to Moscovian. The abundance and diversity of corals in the West Junggar region are significantly lower than those in the eastern and southeastern regions. In terms of the composition of coral fauna, the species of Caninophyllum found in the Halaalate Formation together with the widespread distribution of genus Cystodendropora, we suggest that the coral assemblages from various regions around the Junggar Basin are comparable. Furthermore, in conjunction with a compilation of the published data from the Upper Carboniferous strata around the Junggar Basin, almost half of the known coral species are endemic elements. This study suggests that the distribution and composition of coral fauna are closely tied to the formation of trapped Junggar Ocean during the Late Carboniferous period.
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      [PDF 40.22 M] (25899)
      Abstract:
      The Ordovician in Yunkai area of western Guangdong Province mainly consists of sandstone, pelitic siltstone, silty mudstone and pebbly sandstone, and mudstone with intercalated carbonate rock lenses and conglomerates. The Ordovician includes the Lower Ordovician Luohong Formation and Luodong Formation, Middle Ordovician Dongchong Formation, and Upper Ordovician Lanweng Formation. Fossil bivalves, including the new taxa described in this paper, were collected from an about 2-meter-thick bed of gray to grayish yellow silty mudstone and pelitic siltstone of the upper part of the Dongchong Formation. The collection includes about one thousand bivalve specimens, which represent more than 22 species of 16 and several unnamed genera and may a possible new taxon. We report a group of unique bivalves including two new species of Yunannia gen. nov. of a new family Yunanniidae Zhang et Niu and a new superfamily Yunannioidea Zhang et Niu. This group demonstrate combined features normally attributed to different bivalve taxa. A small number of trilobites, including Nileus sp., Lonchobasilicus sp., Calymenesun tingi Sun, Calymenesun sp., Asaphopsis? sp., and brachiopods, including Paralenorthis sp., Aegira sp., Leptellina sp., Obolus? sp., Strophomena sp. and Nicolella sp., cooccur with the bivalves and indicate the Middle Ordovician age. SYSTEMATIC PALEONTOLOGYClass Bivalvia Linnaeus, 1758 in 1758–1759 Subclass Autobranchia Grobben, 1849 Infraclass Pteriomorphia Beurlen, 1944 Cohort Uncertain Superfamily Yunannioidea Zhang et Niu superfam. nov. Description Shell small, mytiliform, umbos anterior to terminal; strong inequilateral; buyssal sinus faint; the area beneath and anterior umbo edentulous; posterior to umbo a row of discrete chevron taxodont teeth; large anterior adductor muscle scar located in the umbonal angle and occupies the large and wide umbonal septum together with the anterior pedo-byssal retractors; posterior muscle scar unknown; external ligament, opisthodetic, submarginal; ligamental area narrow with 2-ranks of ligamental grooves and ridges, which are gently arched and extended continuously away from the dorsal margin; shell surface with faint comarginal growth lines. Remarks The Yunannioidea, a new superfamily of pteriomorphians is established based on the genus Yunannia proposed in the present paper. The Yunannia, the sole genus of the new superfamily Yunannioidea, is characterized by mytiliform outline, one posterior row of chevroned teeth, the large anterior adductor muscle scar located in the umbonal angle and inserted on the umbonal septum together with the anterior pedo-byssal retractor, and the arched two ranks of ligamental grooves and ridges which extend continuously away from dorsal margin. On the basis of features such as mytiliform, the musculature, and ligament, the Yunannioidea may be placed into the Cohort Mytilomorphi!. However, the genus Yunannia has only one row of posterior chevroned teeth. Together with its unusual hinge dentition, the new superfamily can be distinctly distinguished from other members of the same cohort. Meanwhile, features including the taxodont dentiotion and the two ranks of ligament indicate that Yunannia is likely in connection with Subcohort Ostreioni. Hence, the position of Yunannia at cohort level is undetermined. The genus Yunnania most possibly represents a new order of the infraclass Pteriomorphia. Family Yunannidae Zhang et Niu fam. nov. urn:lsid:zoobank.org:act:8A609836-4A82-4C6A-97B1-18168E761 891 Type genus Yunannia Zhang et Niu Yunannidae is the sole family of the new superfamily Yunannioidea. Distribution Middle Ordovician, Guangdong, China. Genus Yunannia Zhang et Niu gen. nov. urn:lsid:zoobank.org:act:B09DAFBA-A54D-4621-8FCD-07D8882 A6584 Type species Yunannia gankengensis Zhang et Niu gen. et sp. nov. Diagnosis Shell mytiliform, umbos anterior to terminal, with a row of posterior, discrete chevron taxodont teeth; anterior adductor muscle scar large and pedo-byssal retractor inserted on umbonal septum; ligament external and opisthodetic, extending continuously away from dorsal margin. Description The shell is small with height less than 21 mm. The shell shape is strongly inequilateral, mytiliform or narrow ovate with height longer than length. The umbos is anterior to terminal, projected and slightly incurved. Anterior lobe is absent. The dorsal-posterior margins are merged and widely arched. The anterior flange is thickened. The umbnal cavity is large and deep, separated by a lunate inner septum. The anterior adductor muscle scar is large and elliptical, located in the umbonalangle, and inserted on the umbanl septum together with the posteriorly extended pedo-byssal retractor. The growth line of anterior adductor muscle scar is present in one specimen. The anterior end of the anterior adductor scar is acuminate, likely marking the position of the pedal protractor but is obviously merged with the anterior adductor. The posterior adductor and posterior pedal retractor are unknown. The holotype, a left valve, bears about 20 teeth and sockets, while each half of a paratype bears about 8–15 teeth. The area anterior to and beneath umbo is edentulous. All teeth are discrete and chevroned with concavities towards distal end. The anterior two or three teeth are small and the rest become gradually larger posteriorly, achieving the maximum size about midway along the row of teeth. The teeth diminish gradually in size toward the posterior end of hinge plate. The ligament is external and opisthodetic, submarginal, sub-parallel to the gently arched dorsal-posterior shell margin. The ligamental area is narrow and extends posteriorly to about 3/4–4/5 height of shell, with one rather coarse ligamental ridge and two grooves above and below it (as the first-rank of ligament), while the weak and faint ligamental ridges and grooves (as the second-rank of ligament) within the first-rank ligamental grooves and ridge. Because of the number of first-rank ligamental groove-ridge couplets, it is likely the preduplivincular ligament. However, if the second-rank of ligament is also considered, the total number of ligamnental groove-rige couplets is more than two or three. Hence, it is likely the duplivincular ligament, rather than the preduplivincular ligament. In addition, the arched shape of ligamental area is similar to the simple arched ligament. The holotype specimen shows faint growth lines on the inner surface of shell wall. Etymology Yunan, a geographic name of a county in Guangdong Province. Remarks This genus is the sole representative of Yunannioidea superfam. nov. It is characterized by features such as the mytiliform shell having a posterior row of chevroned teeth, and the arched two ranks of ligamental groove-ridge couplets extending continuously away from the dorsal margin. The large anterior adductor located in the umbonal angle and inserted on the umbanl septum together with anterior pedo-byssal retractor. In addition, the large and wide umbonal septum is another distinguishing feature of Yunannia. The new genus combines some main features normally attributed to different bivalve taxa. Its dentition of taxodont teeth is similar to the Paleotaxodonta. The new genus and Ambonychioidea of Pteriomorphia share some features, including the mytiliform shape, terminal umbos and byssal sinus. Both the new genus Yunannia and cyrtodontoids have the same characteristic of sub-umbonaledentulous area. The present new genus and Dreissenoidea of Heteroconcha have common characters such as the anterior muscle scar inserted on umbonal septum, the submarginal, long, extended arched ligament. With the combination of features listed above, the new genus clearly distinguishes itself from all other genera in those taxa. Age and distribution Middle Ordovician; Guangdong, China. Yunannia gankengensis Zhang et Niu gen. et sp. nov. urn:lsid:zoobank.org:act:67E7B718-0211-4EBB-ADA9-898045A3 8637 (Figs. 3–5) Materials 8 specimens of internal moulds including 5 left valves and 3 right valves. Holotype: No. Ng4032, Paratypes: Ng4033, Ng4030, Ng4031, Ng1041. Diagnosis Height/length(width) ratio less than 1.5; ventral part of shell expanded and swollen. Description The shell is small, mytiliform, strongly inequilateral with height less than 20 mm. The height is longer than the length (width) with height/length(width) ratio less than 1.5. The umbos is terminal, projected and slightly incurved. The anterior lobe is absent. A faint byssal sinus is present at the upper part of anterior margin. The dorsal-posterior margins are merged and widely arched. A long and thickened anterior flange is present behind the anterior margin. A large umbnal cavity is separated by a lunate umbonal septum. The elliptical and large anterior adductor muscle scar is located in the umbonal angle, together with anterior pedo-byssal retractor, occupying the umbonal septum. The anterior adductor muscle scar being covered by growth line is showed in one paratype specimen (No. Ng1041). The anterior end of the anterior adductor scar is acuminate, which likely marks the position of the pedal protractor, but is obviously merged with the anterior adductor (as to otherwise indistinguishable). The posterior adductor and posterior pedal retractor are unknown. The area anterior to and beneath the umbo is edentulous. Posterior to the umbo there is a row of teeth consisting of 13–20 discrete and chevroned teeth with concavities towards the distal end. The anterior and posterior two or three teeth are small with the maximum size at the midway along the tooth row. The ligament is external and opisthodetic, submarginal, sub-parallel to the gently arched dorsal-posterior shell margin. The ligamenal area is narrow, extending posteriorly away from dorsal margin to about 4/5 height of the shell with one rather coarse ligamental ridge and two grooves laid above and below it (as the first rank of ligament), which are subdivided by the weak and faint (as the second rank) ligamental ridges and grooves. Because of the number of the first rank ligamental groove and ridge couplets, it is likely the preduplivincular ligament. However, if the second-rankof ligament is also considered, the total number of ligamnental groove-rige couplets is more than 2–3. Hence, it is likely the duplivincular ligament, rather than the preduplivincular ligament. Faint growth lines are present on the shell surface. Measurement Holotype: No. Ng4032: height 17.5 mm, length 13, H/L = 1.35. Etymology Gankeng, a geographic name of Guangdong. Comparison The present new species evidently differs from Yunannia yunkaiensis gen. et sp. nov. in having mytiliform shape, shell becoming gradually wider towards ventral side, with the maximum width near the ventral part of the shell, and a height/length ration less than 1.5. The latter species has a narrow and narrow ovate shape and a height/length ration about 2. Occurrence Gankeng Village, Yunan County, Guangdong Province; Dongchong Formation, Middle Ordovician. Yunannia yunkaiensis Zhang et Niu gen. et sp. nov. urn:lsid:zoobank.org:act:BE7BF3A3-3F07-4049-88F3-2EE989D4 E914 (Fig. 6) Materials 3 internal moulds of left valve. Holotype: No. Ng4035, Paratypes: Ng074, Ng4034. Diagnosis Shape narrow ovate and H/L ratio about 2.0. Description The shell is small, narrow ovate, strongly in-equilateral, 16.5–21 mm high. The height is much longer than the length with a H/L ratio of 2.0. The umbos is projected and slightly incurved. The anterior lobe is absent. The dorsal-posterior margins are merged and gently arched. The thickened anterior flange is relatively narrow. The umbonal cavity is separated by lunate, relatively narrow umbonal septum. The large and elliptical anterior adductor muscle scar is located in the umbonal angle, and together with the pedo-byssal retractor, inserted on umbanl septum. The anterior end of the anterior adductor scar is deeply inserted and becomes shallow poster-ventrally. The posterior adductor and posterior pedal retractor are unknown. The area anterior to and beneath umbo is edentulous with a posterior row of hinge tooth consisting of more than 8 to 13 discrete and chevroned teeth with concavities towards the distal end. The ligament is external and epithetic, submarginal. The ligamental area is narrow, sub-parallel to the gently arched dorsal-posterior shell margin, extending posteriorly away from dorsal margin to about 3/4 height of shell, and with one rather coarse ligamental ridge and two grooves above and below it (as the first rank of ligament). The four weak and faint ligamental groove-ridge couplets (as the second rank of ligament) extend about 5 mm in length in the dorsal side of the groove of the first rank ligament. Surface ornaments of the shell are unknown. Measurement Holotype: No. Ng4035; height 21 mm, length 10 mm, ratio H/L = 2.0. Etymology Yunkai, a regional geographic name in Guangdong Province. Comparison The present new species is distinguished from the genotype, Yunannia gankenensis (gen. et sp. nov) by the narrow ovate shape with a H/L ratio of 2, and the slightly incurved umbo. In contrast to the latter species’ mytiliform shape and a H/L ratio less than 1.5. On the respect of shell shape, the present species is more or less similar to Mytilarca chenmungensis (Conrad) (Pojeta, 1966, pl. 37, figs. 8–18; pl. 38, figs. 1–5, 10), but it differs from the latter species by having a subumbonal edentulous area, a posterior row of taxodont teeth, a large anterior adductor muscle scar, and large anterior pedo-byssal retractors laid on unmbonal septum. Occurrence Gankeng Village, Yunan County, Guangdong Province, Dongchong Formation, Middle Ordovician.
      [PDF 12.61 M] (24764)
      Abstract:
      The Florian in Zhongxiang, Hubei Province is mainly composed of grayish black shale with siltstone and limestone lens, and has high abundance and diversity of fossils. Thirty-one species belonging to 7 genera of graptolites were identified in Wen-xiakou section through systematic collection and identification, which are common genera and species in Yangtze platform area. There are Didymograptellus bifidus Biozone, Corymbograptus deflexus Biozone and Azygograptus suecicus Biozone in ascending order, which is consistent with Yichang and Nanzhang area, but the composition of fossil genera and species is quite different. Zhongxiang area is located at the margin of Yangtze Platform in Floian with rich nutrients and low oxygen environment, which are beneficial to the flourishing of graptolite fauna and the preservation of graptolite fossils.
      Abstract:
      The journey to understand the Cambrian explosion started with Creation, was subsequently succeeded by Darwinism, and became increasingly impacted by the theory of explosive evolution. The Cambrian explosion by nature is an explosion of animal body plans alongside episodic biomineralization, pulsed change of generic diversity, body size variation, and increase of ecosystem complexity. It is a polythetic event in natural history and manifested in many aspects. No simple, single cause can explain the entire phenomenon. Intrinsic and extrinsic causes were extensively discussed but they are merely prerequi-sites for the Cambrian explosion. Without the molecular evolution, there could be no Cambrian explosion. However, the de-velopmental system alone is insufficient to explain Cambrian explosion. Time-equivalent environmental changes were often considered as extrinsic causes, but the time coincidence is also insufficient to establish causality. Like any other evolutionary event, it is the ecology that makes the Cambrian explosion possible though ecological processes failed to cause a burst of new body plans in the subsequent evolutionary radiations. While the Cambrian explosion did take place under circumstances when the world oceans became habitable for various forms of animals, the developmental Gene Regulatory Networks (GRNs) were sufficiently complex for constructing complex forms, and resource supply was less restricted. It seems that opportunities were in every corner! Early metazoans shared seafloors with vendobionts for the last 20 million years of the Ediacaran, although their ecological relationships are less known. Metazoans followed the path of evolving organs and sys-tems, developing orderly repetition of body parts, and attempting possibilities, which enable the evolution of morphological, physiological, ecological variations and complexity. While vendobionts kept their less differentiated body designs, tis-sue-grade organization, and probably osmotic physiology. Consequently, Ediacarans died off at the end of their era for un-known reasons. Thereafter metazoans rapidly diversified and generated numbers of phylum-rank stem or crown lineages with different fates. The Cambrian explosion ultimately resulted in the critical transition from microbially-dominated ecosys-tems in the Precambrian to metazoan-dominated ecosystems in the Phanerozoic. However, the temporospatial pattern of eco-systems during the Cambrian explosion is poorly understood, largely because our current knowledge is biased in metazoan evolution and redox conditions, and thus insufficient to reconstruct an ecosystem that is an integrative entirety of biotic and abiotic components. Therefore, we proposed a facies-dependent integrative approach as a working hypothesis toward a more comprehensive understanding of ecosystem evolution during the Cambrian explosion.
      [PDF 21.00 M] (14550)
      Abstract:
      Populus L. is an ecologically important tree genus in the Northern Hemisphere temperate forest. In this paper we summarize the Populus fossil records from the Paleogene and Neogene of the Tibetan Plateau with updated stratigraphic and chronological data. Fossil evidence shows that Populus first occurred in the plateau in the latest Eocene. The genus is well-documented in the southern and northern Tibetan Plateau in the Oligocene and Miocene, but lacking in the central plateau. Most of the fossil floras in the Tibetan Plateau containing Populus are temperate, deciduous and broadleaved, riparian vegetation, further confirming that the genus had favored a temperate and riparian environment in their early evolutionary history. Besides, the high diversity and prominent dominance of Populus in early Oligocene flora in the northern Tibetan Plateau suggests this region had played an important role in the early diversification stage of Populus.
      [PDF 10.70 M] (14522)
      Abstract:
      In accordance with the cranidia structures, the method of “Q-mode cluster analysis” used in the present paper for a taxonomic study of 18 species of the genus Mufushania, that was established or adopted by Lin Tian-rui (1965), Li Shan-ji (1978),Zhang Wen-tang et al. (1980), Sun Zhen-hua (1982), Zhou Zhi-qiang et al. (1982), Guo Hong-jun et al. (1996), Yuan Jin-liang and Li Yue (1999), Peng Shan-chi et al. (2001), Yuan Jin-liang et al. (2002). The statistical measurement of similarity is incremental sum of error squares (ΔE). The use of the variability by the author is the eight quantitative ratio values (see table 1). The resemblance relation matrices of all specimens are formed through calculation of the increments of sum of error squares between those specimens (see table 2). These data show that M. shalangensis Zhang and Zhou in Zhang et al. 1980(5), M. angustilimbata Zhang and Zhou in Zhang et al.,1980 (7) and M. kailiensis (Yuan in Yuan et al., 2002) (13) species should not be a member of the Mufushania, not belonging to species of Mufushania. Finally, through the application of combined cluster analysis with traditional qualitative analysis in the study of fifteen species of Mufushania trilobites in this paper, of which M. changi Lin, 1965 (2) is regarded as a junior synonym of the type species (1) and M. zhanjiaxiangensis Sun, 1982 (10) is regarded as a junior synonym of M. ezhongensis Sun, 1982 (9), too, the other thirteen species of Mufushania in the opinion on lumping and transferring the studied species is proposed (see table 3).
      [PDF 16.78 M] (14038)
      Abstract:
      The value of the discoveries of Hamipterus tianshanensis and their 3D eggs fossils?are of?great importance.?These fossils preserved in Beijing for several years, the surrounding rocks have been powdering and flaking, which seriously endanger the safety to fossils. This paper intends to use XRF and other methods to detect surrounding rock to explore its corrosion mechanism. The analysis shows that the surrounding rock of fossils is composed of sandstone with boulder clay, which contains some clay minerals such as montmorillonite. The?sandstone?with?calcareous?and?salt?cementation contains large amounts of soluble ions such as Cl-, NO3-, Na+ and Mg2+. The mechanism of the deterioration is as followed, when the humidity changes, the soluble salt also generates large crystal pressure, as well as the expansion of clay minerals produces huge pressing force, leading the surrounding rocks to powder and flake gradually. The?solution?of?salt?existing?as the cement results in the escape and?migration of?particles, which?is?an important reason for fossil deterioration.?Based on the above understanding, this paper also gives suggestions about the protection of fossils.
      [PDF 52.16 M] (13979)
      Abstract:
      The Renyi Section is a newly discovered section in the vicinity of Renyi Town, Hezhou City of Guangxi, in which a continuous marine sedimentary succession of the Middle and Upper Devonian is well developed and out-cropped. The succession yields abundant benthic and pelagic fossils. This paper presents a preliminary research resulton the conodonts and brachiopods from the middle part of the Middle-Upper Devonian Baqi Formation (ca. 80 m thick) at this section. Ten species (or subspecies) of three genera of conodonts are recognized from the studied interval, including Polygnathus alatus, P. cf. collieri, P. cristatus, P. dubius, P. dengleri, P. dengleri sagitta, P. webbi, P. xylus, Klapperina disparalvea and Schmidtognathus wittekindti. Seventeen species of 16 genera of brachiopods are also reported herein, including Schizophoria sp., Gypidula sp., productoid gen. et sp. indet., Leiorhynchus kwangsiensis, Coeloterorhynchus sp., Hypothyridina sp., Uncinulus? sp., Fitzroyella sp., “Ypsilorhychus” subellipticus, Desquamatia sp., Spinatrypina douvillii, Spinatrypina sp., Emanuella sp., Mucrospirifer sp., Undispiriferoides tianqipuensis, Cryptonella? sp. and Oligothyrina? sp. According to the distribution of the conodonts, three conodont zones (S. hermanni, P. cristatus and K. disparilis zones) have been recognized from the studied interval, suggesting an age of late Givetian of the Middle Devonian. The brachiopods were mainly collected from two fossiliferous layers near the base and top of the studied interval, representing two different brachiopod assemblages. The brachiopod fauna from the lower fossiliferous layer (ca. 20 cm thick, S. hermanni Zone) is relatively monotonous in composition, mainly consisting of L. kwangsiensis. This finding verifies the Middle Devonian occurrence of the genus Leiorhynchus in South China. The upper fossiliferous layer (ca. 3 m, upper K. disparilis subzone) yields a diverse brachiopod fauna, including at least 15 genera and displaying the highest diversity of brachiopods ever recorded in a single fossiliferous bed from the upper Givetian of South China.
      [PDF 12.07 M] (13734)
      Abstract:
      This study describes the Guadalupian (Middle Permian) fusulines from the northern Zhabuye area in the Lhasa Block and discusses their palaeobiogeography. In total, the fusuline fauna comprises 6 genera and 16 species, including Yangchienia tobleri Thompson, Yangchienia haydeni Thompson, Chusenella brevipola (Chen), C. schwagerinaeformis Sheng, C. cf. brevis (Chen), C. sp., Nankinella rarivoluta Wang, Sheng and Zhang, N. complanata Wang, Sheng and Zhang, Kahlerina tenuitheca Wang, Sheng and Zhang, K. pachytheca Kochansky-Devidé and Ramov?, Verbeekina americana Thompson, Wheeler and Danner, V. tenuispira Sheng, Neoschwagerina cheni Sheng, N. colaniae Ozawa, N. craticulifera (Schwager) and N. brevis Thompson, Wheeler and Danner. This fauna suggests a Wordian age, as evidenced by the presence of Kahlerina and the thick spirotheca and less-developed secondary transverse septula in Neoschwagerina species. The fauna from the Zhabuye area is correlatable with the contemporaneous faunas from other regions in the Lhasa Block including the Shiquanhe area, the Xiadong area in Tsochen County, Xainza County and Lhunzhub County. The synchronous appearances of Guadalupian warm-water fusuline faunas in the whole Lhasa Block exhibit a pronounced difference in palaeobiogeography from the Tethys Himalaya region with persistent cold-water brachiopod faunas during the middle and late Permian. It is unlikely that the Lhasa Block and the Tethya Himalaya region adjoined together before the late Triassic. Therefore, it is considered that the Lhasa Block has been separated from the Gondwanaland by Wordian time.
      [PDF 8.68 M] (12388)
      Abstract:
      Nail-shaped sclerites are common small shelly fossils (SSFs) with mineralized sclerites in the early Cambrian strata of South China. In this paper, we focus on the systematic study of the nail-shaped sclerites from the Gezhongwu Formation in Zhijin County, Guizhou Province. The results show that these nail-shaped fossils are mainly composed of zhijinitids and problematic cambroclavids. They include nine species in four genera with some taxa first found in Zhijin County, such as Zhijinites tumourifomis, Z. lubricus, Z. clavus, ?Deiradoclavus sp. and ?Cambroclavussp. Based on observations of their preservation modes and morphology, we find that different nail-shaped fossil species have different structures, such as the contracting inner wall of the spine and the vertically crossed fibers in some specimens of Zhijinites and the concave structure on the bottom surface of the plates of many Zhijinites species, indicating morphological similarities and variations in different genera and species. Analysis of the spatial and temporal distributions of these nail-shaped sclerites suggests that they first occurred in the Zhijin area, then radiated and spread to other areas of the Yangtze Platform and adjacent landmasses. In addition, this problematic cambroclavids from the lower part of Gezhongwu Formation may represent the earliest record of this group and extends its age to the Fortunian, providing new important information for the discussion of their evolution and stratigraphic significance.
      Abstract:
      Cambrian Konservat-Lagerst?tten preserve the original states of marine communities and provide valuable materials for community ecological studies. However, few quantitative ecological analyses have been conducted on the Cambrian Balang Fauna (Stage 4, Series 2) from Guizhou Province. In this study, we report a new fossil assemblage from the Pingding section in Majiang County and perform multivariate statistical analyses. This fossil assemblage contains 31 genera and 33 species belonging to six phyla (Brachiopoda, Cnidaria, Arthropoda, Hyolitha, Chancelloriida, and Priapulida) and 12 ecological types. Among these phyla, brachiopods are the most abundant component (61.5%) whilst arthropods exhibit the highest taxonomic diversity at species level (60%). Furthermore, sessile benthos dominate the community followed by active swimming predators. By comparing this fossil assemblage from the Pingding section with communities from other Cambrian faunas, we confirm the heterogeneity among the Cambrian marine communities and suggest that arthropods play a crucial role in shaping the community structure and influencing ecospace occupation. Additionally, expansion of epibenthos in marine ecological communities with increasing water depth also reflects the role of the environmental factors in shaping the community structure.
      Abstract:
      The Ediacaran-Cambrian transition witnessed significant changes in the Earth-life system and was a pivotal time in the evolution of complex multicellular organisms. South China yields essential fossil and stratigraphic records for conducting related research; however, prior investigations have primarily focused on fossil-rich shallow-water platform facies, leaving the biosphere in deep-water regions insufficiently understood. This study presents a detailed examination of a fossil assemblage from the Liuchapo Formation at the Jiaobang section, Jianhe County, Guizhou Province. The Liuchapo Formation represents a slope setting. Through acid etching and thin section observations, we have discovered abundant fossils, including sponge spicules, hyoliths, potential protoconodonts (? Protohertzina sp.)and zhijinitids (? Zhijinites sp.), spherical acritarchs, Megathrix longus and various types of multicellular algae, as well as problematic Poratusiramus sp., globular fossils, and morphologically diverse filamentous and sheet-like fossils. This fossil assemblage belongs to the Fortunian (earliest Cambrian), and the skeletal remains are dominated by sponge spicules. This fossil assemblage includes taxa shared with shallow-water environments and taxa exclusive to deep-water settings. These results augment the palaeontological data from the Fortunian slope facies. This assemblage is significant for potential stratigraphic correlation and evolutionary studies.
      [PDF 6.31 M] (8395)
      Abstract:
      The Cambrian period represents a pivotal time interval in evolution and ecological innovations, characterized by the rapid diversification of metazoans and known as the Cambrian Explosion. During the past forty years, extensive research based on Cambrian Lagerst?tten has significantly contributed to revealing the detailed processes of the Cambrian Explosion, the origins of major animal phyla, and ecological evolution. Guizhou, known as the mecca of palaeontology, not only has yielded abundant exquisite fossils, but also presents a continuous evolutionary sequence of the fossil assemblages across various regions. This is of great importance for studying animal origins and evolution, global stratigraphic correlation, and community paleoecology. In recent years, the discoveries of several biotas, such as the Small Shelly Fossils faunas and the Niutitang, Balang, Jianhe and Kaili biotas, have provided new insights into early metazoans. These discoveries have provided evidences for the missing links of the evolutionary chain of Konservat-Lagerst?tten in China and even worldwide. They offer unique perspectives for revealing the community structures, the diversification process of early metazoans, and the succession of marine communities. Finally, these discoveries provide crucial evidences for a deeper understanding of the processes and mechanisms of the Cambrian Explosion. This paper briefly summarizes the major contributions to palaeontology of researchers from Guizhou Province. In conjunction with global research progress on palaeontology, the authors also discuss current issues and future research directions in this field.
      [PDF 5.57 M] (8193)
      Abstract:
      Tuzoia is one of the most common and globally distributed Cambrian bivalved arthropods. However, the morphology of their rarely and incompletely preserved soft-parts can hardly be utilized to evaluate their swimming and migration abilities. Computational fluid dynamics (CFD) offers quantitative data for inferring the movement patterns of fossilized animals based on the morphology of their often well-preserved exoskeletons. In this paper, Tuzoia retifera and T. canadensis from the Burgess shale are simulated using CFD in benthic and pelagic environments. The differences in fluid performance and vertical flexibility of these two species are compared. Fluid simulation results indicate that T. retifera is subject to less drag force and greater lift force than T. canadensis under the same speed. The results indicate that T. retifera potentially has a faster swimming speed and better vertical migration ability than T. canadensis does. Tuzoia canadensis is probably a benthic species, while T. retifera may occupy wider habitat and has a pelagic swimming lifestyle. We suggest that niche partititoning within a genus occurred as early as the Wuliuan, Cambrian.
      [PDF 9.82 M] (8190)
      Abstract:
      Trilobites are among the most attractive Paleozoic arthropods whose exoskeletons show extremely high diversity. Compared with mineralized exoskeletons that are relatively easy to be preserved, the soft-body structures of trilobites are often difficult to be preserved in the fossil record, resulting in the difficulty in investi gating the internal anatomy and evolution of the trilobites. The exceptional conditions of the Burgess Shale-type Konservat-Lagerst?tten enable the opportunities for the preservation of delicate soft-body structures of the trilobites, providing material for examining their internal structures. Here we describe the soft-body structures of the trilobite <i style="letter-spacing: 0.1pt;">Malongocephalus</i> <i style="letter-spacing: 0.1pt;">yunnanensis </i>Zhang and Lin in Zhang <i style="letter-spacing: 0.1pt;">et al</i>., 1980 from the Hongjingshao Formation (Cambrian, Series 2, Stage 3) at the Xiazhuang section, Chenggong, Kunming, Yunnan, China. The specimens show that the antenna of <i style="letter-spacing: 0.1pt;">M</i>. <i style="letter-spacing: 0.1pt;">yunnanensis</i> is composed of at least 13 podomeres and that post-antennal appendages consist of flap-like exopodites. The digestive tract is differentiated into foregut, midgut, and hindgut, with three pairs of digestive glands in the head. This paper represents the first report of soft-body structures in the Family Redlichiida of Order Abadiellidae, which enriches the anatomical information of the early Cambrian trilobites. This study also compares and analyses the differences of relative lengths of antennae among members of Order Redlichiida, and discusses the structures of digestive system of the trilobites.
      [PDF 7.84 M] (8151)
      Abstract:
      For a long time, Fuchouia has been regarded as a crucial taxon for biostratigraphic division and correlation of Jialao Formation in Jianhe, Guizhou. However, the systematic positions of Fuchouia and Parafuchouia still remain controversial, with the following three main viewpoints: Parafuchouia is a subgenus of Fuchouia; Parafuchouia is a junior synonym of Fuchouia; and Parafuchouia can be elevated to a separate genus. Based on the specimens of Fuchouia collected from Jialao Formation in Jianhe and previously reported as Parafuchouia or Fuchouia (Parafuchouia), and the specimens of Fuchouia and Parafuchouia previously reported by other authors, we perform statistical analysis on morphological characters of the cranidia of Parafuchouia and Fuchouia using linear measurements. The results indicate that Parafuchouia is a junior synonym of Fuchouia, and its distinguishing features from Fuchouia can be viewed as intraspecific morphological variation. Thus, the Jialao Formation may be the lowest horizon that yields Fuchouia in the world. Although Fuchouia is widely distributed in China, the Democratic People’s Republic of Korea, India-Himalayas, Australia, Kazakhstan and other countries around the world, its occurrences span a wide range of horizons, mostly from the Ptychagnostus atavus Zone of the Drumian Stage to Lejopyge laevigata Zone of the Guzhangian Stage. Hence, it is difficult to use Fuchouia for biostratigraphic correlations. The established Fuchouia biostratigraphic zone of the Cambrian Jialao Formation in Guizhou needs to be further reviewed, and index fossils at the species level or other index fossils need to be selected to make better stratigraphic correlations with the Cambrian slope facies of South China or the Cambrian of North China platform.
      [PDF 4.88 M] (8145)
      Abstract:
      The Kuanchuanpu Biota (535 Ma; Fortunian, Cambrian) represents an exceptionally phosphatized fossil Lagerst?tte, yielding abundant fossils of embryonic and adult soft-bodied animals, small shelly fossils, and algae.This biota serves as a crucial taphonomic window for unraveling the marine ecosystem during the very beginning of the Cambrian Explosion. However, previous studies have primarily focused on well-known groups such as the cnidarians represented by Olivooides and the ecdysozoans represented by scalidophorans (e.g., Eokinorhynchus), leaving numerous enigmatic taxa of this fossil assemblage uninvestigated. This study reports a newly discovered enigmatic fossil taxon, Linglongsphaera ornata n. gen. n. sp., from the Kuanchuanpu Biota. This taxon is characterized by a spherical body with its diameter ranging from 544 to 1088 μm. Its surface is ornamented with nodular projections, and its interior consists of cells with an average diameter of 24 μm. During different developmental stages, Linglongsphaera ornata exhibits a variable number of chambers ranging from 8 to over 180. The volume of an individual chamber increases at the beginning and then gradually decreases as the overall number of chambers increases. The chambers are distributed from the periphery to throughout the interior, with the total volume of chambers being stabilized at approximately 36% of the total volume of the organism body. Based on available evidence, we propose that Linglongsphaera ornata may represent an extinct multicellular eukaryote, with possible close affinity to multicellular algae. However, its precise classification and phylogenetic position remain uncertain. This discovery contributes to a more comprehensive understanding of the diverse and enigmatic taxa of the Kuanchuanpu Biota, and sheds light on the complex early Cambrian biosphere during the Cambrian Explosion.
      Abstract:
      The Cambrian Explosion represents the mysterious radiation of disparate bilaterian animals and the first emergence of marine ecosystems dominated by the animal kingdom. Brachiopods are one of the most important contributors to the tiering complexity through the Palaeozoic. The lower Cambrian strata of South China yield such a wide variety of monospecific or paucispecific brachiopod shell concentrations. Here we present the first record of a brachiopod-dominated community from the Kaili Biota (Wuliuan, Miaolingian) at the Chengduo, Jinyinshan and Miaobanpo sections in Jianhe County, Guizhou Province, South China. The association occurs on the same bedding plane that is dominated by linguloid brachiopod Palaeobolus bretonensis, commonly alongside pelagic pagetiids, infaunal worms, epibenthic molluscs, and eocrinoids. The shells of P. bretonensis on the bedding plane, both juveniles and adults, appear to be randomly orientated. Nearly all individuals of P. bretonensis are disarticulated, but shells with fine concentric sculptures are common and concordant to the bedding plane. Polished sections perpendicular to the bedding plane show that the layer containing the brachiopod shell concentrations lacks other sedimentary structures and bioturbations, indicating a quiet, low energy environment. Taphonomic and sedimentological evidences demonstrate that the shell pavements herein are basically biogenic and preserved in situ. Ecological structural models for the brachiopod-supported communities from the Kaili and the Guanshan biotas are partly overlapping. However, the Kaili Biota shows a higher biodiversity and more complexity in ecological tiering or feeding strategies. The shell pavements of P. bretonensis from the Kaili Biota probably had an effect in hardening the soft substrates and provided more possible niches for other benthos such as the eocrinoids during the middle Cambrian.
      Abstract:
      Cardiodictyon catenulum is a common lobopodian in the early Cambrian Chengjiang fauna. The functional morphology of its trunk sclerites has long been controversial. Here, we show that the trunk of C. catenulum has a longitudinal series of saddle-shaped sclerites, each corresponding to a body segment and extending from the dorsum to both sides of the trunk. Thus, its trunk sclerites are significantly different from those of other Cambrian lobopodians which possessed paired or circular trunk sclerites. The trunk sclerite of C. catenulum has a conical dorsal projection at the center. The brim of each sclerite is obviously thickened and serrated, which may have in creased its overall rigidity and indicate an enhanced function of protection and defense. In this study, we also report a sieve-like microstructure on the surface of the sclerites, resembling the net-like microstructure on sclerites of Hallucigenia, Microdictyon, and Onychodictyon. The equidistantly arrayed pores are diagenetically permineralizsed with pyrite and preserved as numerous pyritized micro-tubercles. These pores might have served as exits for micro-papillae. We consider that the trunk sclerites of Cambrian lobopodians are in general with a sieve-like microstructure, which may have had protective sensory function. A single sclerite corresponding to a trunk segment in C. catenulum is an autapomorphy of the Cambrian lobopodians. The distinctive arrangement of trunk plates in C. catenulum might represent the prototype of trunk sclerites, or alternatively a derived trait, i.e., secondary fusion of paired sclerites, of early lobopodians.
      Abstract:
      The evolutionary history of testate amoebae can be traced back to the early Neoproterozoic. The earliest testate amoebae are represented by vase-shaped microfossils found in shallow marine carbonate rocks and shales in North America, North China, Norway, Australia, and other areas. In the Phanerozoic, the earliest fossil record of testate amoebae occurs in the Lower Devonian, whereas there has been no unambiguous fossil evidence of such protists known in the early Paleozoic rocks for a long time. By means of standard palynological acid maceration techniques, we obtained fossil specimens preserved in situ by grinding thin slices of rocks. We found several organic microfossils bearing strange ornamentations from the Balang Formation (Stage 4, Series 2, Cambrian) at the Jiaobang section in Jianhe County, eastern Guizhou. Based on their micromorphological characteristics and the results of laser Raman spectroscopy, these organic-walled microfossils are proposed as remains of the early Cambrian testate amoebae, and they are morphologically very similar to those of Euglyphida. In particular, they can be morphologically compared with extant testate amoebae Assulina Greef, 1888. Thus, our specimens, previously described as acritrach Plagasphaera balangensis and Plagasphaera sp. A, are now re-classified here as Palaeoassulina balangensis gen. et sp. nov., and ?Palaeoassulina sp. A, respectively, based on their morphological similarity to extant testate amoeba Assulina Greef, 1888. This discovery not only extends the fossil record of testate amoebae from the previously known late Paleozoic to the early Cambrian, but also provides key fossil evidence for understanding the evolution of testate amoebae.
      Abstract:
      Phosphatization is a critical pathway for the exceptional preservation of soft-bodied fossils, with microbes potentially playing a significant role in the process. Previous taphonomic experiments have demonstrated that microbes can rapidly proliferate within soft tissues such as animal embryos, fill the internal spaces of the organism, and replicate its original morphology through microbial pseudomorphisation. However, whether the phosphatization process of fossils is identical to the process simulated by these taphonomic experiments remains contentious. In this study, a new type of reticulate microfossils from the early Cambrian Kuanchuanpu Biota is described. The preservation of these fossils can be categorized into three types based on the extent of proliferation of microbial filaments, indicating the complete taphonomic procedure from the organism's death to microbial invasion and proliferation, and finally to the phosphatization. These specimens indicate that microbial pseudomorphisation plays a significant role in the phosphatization of soft tissues but is not a required pathway, especially when the organisms possess structures with high resistance to decay, such as mineralized skeletons or chitinous cuticles. These new microfossils are mostly preserved as fragments with consistent structures on both sides, featuring characteristic columnar arrangements of nearly circular and dumbbell-shaped perforations Due to the simplicity of the fossil structures and the paucity of biological traits, their phylogenetic positions remain unclear, making them a group of enigmatic fossils that warrant further investigation.


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