![]() | You can help expand this article with text translated from the corresponding article in Chinese. (October 2022)Click [show] for important translation instructions.
|
![]() | You can help expand this article with text translated from the corresponding article in French. (October 2022)Click [show] for important translation instructions.
|
The Qingjiang biota are a major discovery of fossilized remains dating from the early Cambrian period approximately 518 million years ago. [1] The remains consist at least 20,000 individual specimens, and were discovered near the Danshui River in the Hubei province of China in 2019. [2] The site is particularly notable due to both the large proportion of new taxa represented (approximately 53% of the specimens), [1] and due to the large amount of soft-body tissue of the ancient specimens that was preserved, likely due to the organisms being rapidly covered in sediment prior to fossilization, that allowed for the detailed preservation of even fragile, soft-bodied creatures such as jellyfish. Shelly fossils found at the site include trilobites, radiodonts, lobopods, bradoriids, brachiopods, hyolithids, mollusks, chancelloriids, kinorhynchs, priapulids, and articulated sponge spicules.
The site is a Burgess Shale type preservation, [1] and has been widely compared [1] [3] [4] to the Burgess Shale in terms of the site's richness and significance. The discovery has been described as one of the most significant of its kind in the last 100 years. [2] Initial publications regarding the site stated that 4,351 of the collected specimens had been examined, [2] and 101 species had been identified, 53 of which were new to science. [5]
Talks are reportedly underway with local government to protect the site to ensure the longevity of continued research on the deposited specimens. [4]
Genus | Species | Phylum | Notes | Image |
---|---|---|---|---|
Qingjiangonema [6] | Q. cambria | Thermodesulfobacteriota | "Qingjiangonema is a long filamentous form comprising hundreds of cells filled by equimorphic and equidimensional pyrite microcrystals with a light sulfur isotope composition. Multiple lines of evidence indicate Qingjiangonema was a sulfate-reducing bacterium that exhibits similar patterns of cell organization to filamentous forms within the phylum Desulfobacterota, including the sulfate-reducing Desulfonema and sulfide-oxidizing cable bacteria." |
Genus | Notes | Image |
---|---|---|
Chuaria [7] | Chuaria is a spheroidal and thick-walled eukaryote that is typically regarded as having algal affinities based on cell walls and biogeochemical analyses. It appears to have existed from the late Paleoproterozoic (1670–1640 Ma) to the Qingjiang Formation (518 Ma). "Like many Precambrian microfossils (Simpson, 1944, Schopf, 1994, Dvořák et al., 2015), its extraordinarily slow rate of evolutionary change was probably due to the asexual reproduction and wide ecological tolerance. Accordingly, if Chuaria represented a homogeneous eukaryote, it would make sense that it retained a consistent morphology for an exceptionally long geological time. Such hypobradytelic organism can be seen in macro-organisms as well, e.g., Marchantites Brongniart, 1849 of bryophyte (Li et al., 2014), or Lampetra Bonnaterre, 1788 of chordate (Gess et al., 2006)." | ![]() |
Genus | Species | Clade | Notes | Image |
---|---|---|---|---|
Megaspirellus? [1] | Megaspirellus was originally identified as an alga but has been more recently tentatively re-interpreted as a cololite (fossilized intestinal casts of faecal material) and a junior synonym of Cilindrotomaculum . [8] | |||
Qingjiangthallus [9] | Q. cystocarpium | Florideophyceae | A red alga. "Thalli comprise flat and ribbon‐shaped branches showing different branching patterns, some short branchlets, discoid or globose holdfasts and an unexpected occurrence of possible cystocarps (reproductive bodies)." | |
Sinocylindra [1] | Chlorophyta? | "Smooth cylindrical ribbons 0.19–2.2mm wide and up to 74.0 mm long. Ribbons are flexible and can be curved, looped or folded, but are not regularly coiled as in Megaspirellus or Grypania . No branching or holdfast structures are associated with the ribbons." [10] |
Genus | Species | Phylum | Class | Order | Family | Notes | Image |
---|---|---|---|---|---|---|---|
Choia [1] | Porifera | Demospongiae | Protomonaxonida | Choiidae | | ||
Crumillospongia [1] | Porifera | Demospongiae | Protomonaxonida | Hazeliidae | |||
Halichondrites [1] | Porifera | Demospongiae | Protomonaxonida | Halichondritidae | ![]() | ||
Hazelia [1] | Porifera | Demospongiae | Protomonaxonida | Hazeliidae | |||
Leptomitella [1] | Porifera | Demospongiae | Protomonaxonida | ||||
Leptomitus [1] | Porifera | Demospongiae | Protomonaxonida | Leptomitidae | |||
Paraleptomitella [1] | Porifera | Demospongiae | Protomonaxonida | Leptomitidae | |||
Saetaspongia [1] | Porifera | Demospongiae | Protomonaxonida [11] | ||||
Sanshapentella [12] | S. tentoriformis | Porifera | Hexactinellida | "Owing to the presence of definite hexactines and hexactine-derived spicules, Sanshapentella can be assigned to Hexactinellida... Sponge body is composed of a stout trunk (usually 10–35 mm in thickness) and four or five conical branches at the top." | |||
Allonnia [1] | Possible stem-group Eumetazoa [13] | Chancelloriida | Chancelloriidae | ![]() | |||
Xianguangia [1] | X. sinica | Stem-group Ctenophora [14] | Dinomischidae | Resolved as being in the monophyletic family Dinomischidae with Daihua and Dinomischus . | |||
Dinomischus [1] | Stem-group Ctenophora [14] | Dinomischidae | |||||
Sphenothallus [1] | Cnidaria | Conulatae | Their shell composition and microstructure indicate relatedness to conulariids [15] | ![]() |
Genus | Species | Phylum | Class | Order | Family | Notes | Image |
---|---|---|---|---|---|---|---|
Ambrolinevitus [1] | Possible stem-group Lophotrochozoa [16] | Hyolitha | |||||
Archotuba [1] | Possible stem-group Lophotrochozoa [16] | Hyolitha | |||||
Burithes [1] | B. yunnanensis | Possible stem-group Lophotrochozoa [16] | Hyolitha | ||||
Qingjianglepas [17] | Q. elegans | Mollusca | Helcionelloida | "Limpet-formed shell, flattened, with elliptical aperture. Radial sculpture of numerous high and narrow primary and secondary ribs, intersecting the concentric growth lines as imbrications. A prominent fold on anterior flank of shell, extending from apical region toward the anterior edge of aperture." | |||
Heliomedusa [1] | H. orienta | stem-group Brachiopoda | Mickwitziidae | Whether Heliomedusa and Mickwitzia are the same genus is debated. [18] | |||
Diandongia [1] | Brachiopoda | Lingulata | Lingulida | Neobolidae [19] | "The generic composition of the Botsfordiidae was recently emended by Popov et al. (2015), who restricted the family to include only genera exhibiting a pitted larval shell, a finely pustulose postlarval shell and lacking well-developed muscle platforms as well as a prominent dorsal median ridge. The linguloid family Neobolidae was reintroduced, encompassing several early Cambrian lingulide genera that previously had been assigned to the Botsfordiidae, including Neobolus and Edreja (Holmer and Popov, 2000). " | ||
Lingulella [1] | Brachiopoda | Lingulata | Lingulida | Obolidae | ![]() |
Genus | Species | Phylum | Class | Order | Family | Notes | Image |
---|---|---|---|---|---|---|---|
Alalcomenaeus [1] | Arthropoda | Megacheira | Leanchoiliida | Leanchoiliidae | ![]() | ||
Amplectobelua ? [20] | Arthropoda | Radiodonta | Amplectobeluidae | ![]() | |||
Branchiocaris [1] | B. yunnanensis | Arthropoda | Hymenocarina | Protocarididae | ![]() | ||
Burgessia [1] | Arthropoda | The affinities of Burgessia are contentious. It may be a basally derived crown-arthropod [21] . | ![]() | ||||
Combinivalvula [1] | C. chengjiangensis | Arthropoda | Sunellidae | The family Sunnellidae includes three genera: Combinivalvula, Sunella , and Jinningella . "Sunellids resemble Isoxys Walcott, 1890 to which they may be closely related; both possess a bivalved, elongated carapace with cardinal spines that almost entirely covers the body. However, neither cephalic appendages nor proximal portions of trunk limbs are visible in sunellids, and thus, their systematic position remains uncertain." [22] | |||
Duplapex [23] | D. anima | Arthropoda | Hymenocarina | Tuzoiidae | "The general morphology of Duplapex gen. nov. clearly indicates affinity with the Family Tuzoiidae, supported by the unmineralized bivalved carapace, reticulate ornamentation, small marginal spines and annulated eye stalks. However, its layered valves are distinguished from those of Tuzoia (the only genus found in the Family Tuzoiidae), and Duplapex has unique ventral notches and doublure spines. These justify the erection of a new genus within the Family Tuzoiidae." | ![]() | |
Estaingia | Arthropoda | Trilobita | Ptychopariida | Estaingiidae | ![]() | ||
Isoxys [24] | I. minor | Arthropoda | Isoxyida | Isoxyidae | I. minor appears to have produced many eggs (approximately 300 per clutch), and egg-bearing individuals were about half the size of adults, indicating r-selection in this species. This is currently the earliest diverging arthropod that displays brood behavior. | ![]() | |
Leanchoilia [1] | Arthropoda | Megacheira | Leanchoiliida | Leanchoiliidae | ![]() | ||
Misszhouia [1] | M. longicaudata | Arthropoda | Nektaspida | Naraoiidae | ![]() | ||
Mollisonia [1] | Arthropoda | Mollisoniida | Stem-group Chelicerata | ![]() | |||
Naraoia [1] | N. spinosa | Arthropoda | Nektaspida | Naraoiidae | ![]() | ||
Redlichia [1] | Arthropoda | Trilobita | Redlichiida | Redlichiidae | ![]() | ||
Stanleycaris [20] | S.qingjiangensis | Arthropoda | Radiodonta | Hurdiidae | ![]() | ||
Sunella [1] | S. grandis | Arthropoda | Sunellidae |
Genus | Species | Clade | Notes | Image |
---|---|---|---|---|
Eldonia [1] | Stem-group Ambulacraria [25] | A member of the stem-ambulacrarian clade Cambroernida. | ![]() | |
Yunnanozoon [1] | Possible stem-group Deuterostome [25] | ![]() | ||
Banffia [1] | Possible stem-group Deuterostome [26] | Banffia is a member of the clade Vetulicolia, which may belong to stem-Deuterostomia. | |
Amplectobelua is an extinct genus of late Early Cambrian amplectobeluid radiodont, a group of stem arthropods that mostly lived as free-swimming predators during the first half of the Paleozoic Era.
Anomalocarididae is an extinct family of Cambrian radiodonts, a group of stem-group arthropods.
Haplophrentis is a genus of tiny shelled hyolithid which lived in the Cambrian Period. Its shell was long and conical, with the open end protected by an operculum, from which two fleshy arms called helens protruded at the sides. These arms served to elevate the opening of the shells above the sea floor, acting like stilts.
Tuzoia is an extinct genus of large bivalved arthropod known from Early to Middle Cambrian marine environments from what is now North America, Australia, China, Europe and Siberia. The large, domed carapace reached lengths of 180 millimetres (7.1 in), making them amongst the largest known Cambrian arthropods.
This is a list of fossils found at Maotianshan Shales, whose most famous assemblage of organisms are referred to as the Chengjiang biota.
Isoxys is a genus of extinct bivalved Cambrian arthropod; the various species of which are thought to have been freely swimming predators. It had a pair of large spherical eyes, and two large frontal appendages used to grasp prey.
Radiodonta is an extinct order of stem-group arthropods that was successful worldwide during the Cambrian period. Radiodonts are distinguished by their distinctive frontal appendages, which are morphologically diverse and were used for a variety of functions. Radiodonts were among the earliest large predators, but they also included sediment sifters and filter feeders. Some of the most famous species of radiodonts are the Cambrian taxa Anomalocaris canadensis, Hurdia victoria, Peytoia nathorsti, Titanokorys gainesi, Cambroraster falcatus and Amplectobelua symbrachiata. The later surviving members include the subfamily Aegirocassisinae from the Early Ordovician of Morocco and the Early Devonian member Schinderhannes bartelsi from Germany.
Mollisonia is an extinct genus of Cambrian arthropod. 4 species had been described from North America and China. Studies suggest it is a basal member of Chelicerata, a group which includes horseshoe crabs and arachnids.
Stanleycaris is an extinct genus of hurdiid radiodont from the Cambrian. The type species is Stanleycaris hirpex. Stanleycaris was described from the Stephen Formation near the Stanley Glacier and Burgess Shale locality of Canada, as well as Wheeler Formation of United States. A second species, S. qingjiangensis is known from the Qingjiang biota of China. The genus was characterized by the rake-like frontal appendages with robust inner spines.
Tamisiocarididae is a family of radiodonts, extinct marine animals related to arthropods, that bore finely-spined appendages that were presumably used in filter-feeding. When first discovered, the clade was named Cetiocaridae after a speculative evolution artwork, Bearded Ceticaris by John Meszaros, that depicted a hypothetical filter-feeding radiodont at a time before any were known to exist. However, the family name was not valid according to the International Code of Zoological Nomenclature, as no real genus named "Cetiocaris" exists, and in 2019 it was formally replaced by the name Tamisiocarididae, after the only valid genus of the clade at the time. The family is only known from Series 2 of the Cambrian, unlike other radiodont families, which persisted longer into the Cambrian. All known species would have lived in tropical or subtropical waters, suggesting a preference for warmer waters.
Vetulicola rectangulata is a species of extinct animal from the Early Cambrian of the Chengjiang biota of China. Regarded as a deuterostome, it has characteristic rectangular anterior body on which the posterior tail region is attached. It was described by Luo Huilin and Hu Shi-xue in 1999.
Ramskoeldia is a genus of amplectobeluid radiodont described in 2018. It was the second genus of radiodont found to possess gnathobase-like structures and an atypical oral cone after Amplectobelua. The type species, Ramskoeldia platyacantha, was discovered in the Chengjiang biota of China, the home of numerous radiodontids such as Amplectobelua and Lyrarapax.
Robert Riepma Gaines is an American geologist who teaches at Pomona College in Claremont, California. He presently serves as acting President of Pomona College. From July 2019 to June 2022, he served as the Vice President of Academic Affairs and Dean of the college. He is known for his research on fossils in Burgess Shale-type deposits, having been a member of two teams that made two of the most important fossil discoveries in recent decades, one in Kootenay National Park in British Columbia, Canada and the other in the Yangtze Gorges area in South China.
Houcaris is a possibly paraphyletic radiodont genus, tentatively assigned to either Amplectobeluidae, Anomalocarididae or Tamisiocarididae, known from Cambrian Series 2 of China and the United States. The type species is Houcaris saron which was originally described as a species of the related genus Anomalocaris. Other possible species include H. magnabasis and H. consimilis. The genus Houcaris was established for the two species in 2021 and honors Hou Xianguang, who had discovered and named the type species Anomalocaris saron in 1995 along with his colleagues Jan Bergström and Per E. Ahlberg.
Duplapex is an extinct genus of bivalved arthropod known from the Cambrian Stage 3 aged Qingjiang biota of Hubei, China, with a single species. D. anima. It is thought to be a close relative of Tuzoia, but unlike it, the reticulated bivalved carapace was interpreted to have opened at a wide angle. The carapace had a pair of spines projecting posteriorly. In its original description, it was suggested to have eyes on annulated stalks, but later research suggested that these may have been preservational artifacts instead.
Isoxyids are members of the order Isoxyida and the family Isoxyidae, a group of basal arthropods that existed during the Cambrian period. It contains two genera, Isoxys, with 20 species found worldwide, and Surusicaris known from a single species found in the Burgess Shale of Canada. They are distinguished by their bivalved carapaces and pair of upward curving grasping frontal appendages.
Guanshancaris is an extinct genus of amplectobeluid radiodont known from the Cambrian Stage 4 Guanshan Biota of southern China. It is only known from a single species. G. kunmingensis which was described in 2013 as a species of Anomalocaris before being placed in a new genus in 2023. Like many other radiodonts, it is only known from fragmentary remains, including its frontal appendages and the oral cone. It has been suggested to have been durophagous. Base on proportion of Anomalocaris, it is estimated to have reached up to 22.2–32.8 cm (8.7–12.9 in) long.
Lenisicaris is a Cambrian anomalocaridid radiodont, known from the Maotianshan Shales of China and the Kinzers Formation of Pennsylvania.
Shucaris is a genus of radiodont of uncertain taxonomic placement from the Lower Cambrian Maotianshan Shales in Yunnan, South China. The type and only species is S. ankylosskelos, known from multiple specimens comprising frontal appendages, multiple endites, gnathobase‐like structures, a nearly complete body, a head carapace complex, and one body flap associated with setal blades.