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1

Zhou, Zhonghe. "The Rising of Paleontology in China: A Century-Long Road." Biology 11, no. 8 (July 25, 2022): 1104. http://dx.doi.org/10.3390/biology11081104.

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In this paper, the history of paleontology in China from 1920 to 2020 is divided into three major stages, i.e., 1920–1949, 1949–1978, and 1979–2020. As one of the first scientific disciplines to have earned international fame in China, the development of Chinese paleontology benefitted from international collaborations and China’s rich resources. Since 1978, China’s socio-economic development and its open-door policy to the outside world have also played a key role in the growth of Chinese paleontology. In the 21st century, thanks to constant funding from the government and the rise of the younger generation of paleontologists, Chinese paleontology is expected to make even more contributions to the integration of paleontology with both biological and geological research projects by taking advantage of new technologies and China’s rich paleontological resources.
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2

Zhou, Zhonghe, and Jin Meng. "The heyday of paleontology in China." National Science Review 1, no. 4 (November 17, 2014): 486. http://dx.doi.org/10.1093/nsr/nwu064.

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3

Perkins, Sid. "Paleontology: From China, the tiniest pterodactyl." Science News 173, no. 8 (February 23, 2008): 125–26. http://dx.doi.org/10.1002/scin.2008.5591730814.

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4

Ding, Y. "PALEONTOLOGY: China Regains Fossils Seized in California." Science 296, no. 5577 (June 28, 2002): 2311a—2311. http://dx.doi.org/10.1126/science.296.5577.2311a.

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5

Ding, Y. "PALEONTOLOGY: China Issues Rules on Fossil Excavation." Science 297, no. 5589 (September 20, 2002): 1981. http://dx.doi.org/10.1126/science.297.5589.1981.

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6

Gibbons, A. "Paleontology: Early Birds Rise From China Fossil Beds." Science 274, no. 5290 (November 15, 1996): 1083–0. http://dx.doi.org/10.1126/science.274.5290.1083.

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7

Jia, Hepeng. "Paleontology: advancing China's international leadership." National Science Review 6, no. 1 (November 12, 2018): 171–76. http://dx.doi.org/10.1093/nsr/nwy132.

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Abstract In recent years, Chinese scientists have achieved significant progress in paleontological discoveries and scientific studies. Series of studies published in top journals, such as Science, Nature and Proceedings of the National Academy of Sciences of the United States of America (PNAS), have astonished the world by presenting beautiful fossils that furnish robust evidence to enrich the understanding of organismic evolution, major extinctions and stratigraphy. It has been portrayed as the heyday in the paleontology of China. What is the status of the field? What factors have caused the avalanche of fossil discoveries in China? What implications can these new discoveries provide for our understanding of current evolution theories? How, given their significant contribution to the world's paleontology scholarship, can Chinese scientists play a due leadership role in the field? At an online forum organized by the National Science Review (NSR), its associate editor-in-chief, Zhonghe Zhou, asked four scientists in the field as well as NSR executive editor-in-chief Mu-ming Poo to join the discussion. Jin Meng Paleobiologist at American Museum of Natural History Mu-ming Poo Neurobiologist at Center for Excellence in Brain Science and Intelligence Technology, Chinese Academy of Sciences Shuzhong Shen Stratigrapher at Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences Shuhai Xiao Paleobiologist and geobiologist at Virginia Polytechnic Institute and State University Zhonghe Zhou (Chair) Paleobiologist at Institute of Vertebrate Paleontology and Paleoanthropology (IVPP), Chinese Academy of Sciences
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8

Stiller, Frank. "Frühjurassische flachmarine Muscheln aus Xiaping, Süd-Hunan, China." Palaeontographica Abteilung A 274, no. 1-2 (February 27, 2006): 1–70. http://dx.doi.org/10.1127/pala/274/2006/1.

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9

Stokstad, E. "PALEONTOLOGY IN CHINA: A Peek at China's Paleontological Bounty." Science 291, no. 5502 (January 12, 2001): 234–35. http://dx.doi.org/10.1126/science.291.5502.234.

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Stokstad, E. "PALEONTOLOGY: Fossil Bird From China Turns Tail, Spills Guts." Science 297, no. 5581 (July 26, 2002): 495a—495. http://dx.doi.org/10.1126/science.297.5581.495a.

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11

Lucas, Spencer G., and Thomas E. Williamson. "Systematic position and biochronological significance of Yuodon and Palasiodon, supposed Paleocene "condylarths" from China." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 196, no. 1 (March 27, 1995): 93–107. http://dx.doi.org/10.1127/njgpa/196/1995/93.

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12

Cai, Chongyang, Shya Chitaley, and Yawei Dou. "Studies on some permineralized lycopsid remains from the Upper Devonian of North Xinjiang, NW China." Palaeontographica Abteilung B 262, no. 5-6 (October 21, 2002): 119–36. http://dx.doi.org/10.1127/palb/262/2002/119.

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13

Mattern, Frank. "Meso-Cenozoic tectonic development and basin evolution of the lower Yangtze reaches (Anhui Province, China)." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 194, no. 2-3 (December 21, 1994): 413–32. http://dx.doi.org/10.1127/njgpa/194/1994/413.

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14

Xu, Jing-Xian, Stephen Blackmore, Yu-Fei Wang, and Cheng-Sen Li. "Late Pliocene vegetation and climate of Yangyi region, Yunnan of China, based on palynological data." Palaeontographica Abteilung B 269, no. 1-6 (December 30, 2004): 131–48. http://dx.doi.org/10.1127/palb/269/2004/131.

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15

Zhiyan, Zhou, Wu Xiangwu, and Zhang Bole. "Tharrisia, a new fossil leafy organ genus, with description of three Jurassic species from China." Palaeontographica Abteilung B 256, no. 4-6 (February 7, 2000): 95–109. http://dx.doi.org/10.1127/palb/256/2000/95.

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16

Normile, D. "PALEONTOLOGY: China Clamps Down on Mining to Preserve Cambrian Site." Science 305, no. 5692 (September 24, 2004): 1893–94. http://dx.doi.org/10.1126/science.305.5692.1893.

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17

Xing, Lida, Adrienne Mayor, Yu Chen, Jerald D. Harris, and Michael E. Burns. "The Folklore of Dinosaur Trackways in China: Impact on Paleontology." Ichnos 18, no. 4 (October 2011): 213–20. http://dx.doi.org/10.1080/10420940.2011.634038.

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18

Bucur, Ioan I., Paul Enos, and Marcello Minzoni. "Middle Triassic calcareous algae and microproblematica from south China." Micropaleontology 69, no. 1 (2023): 61–102. http://dx.doi.org/10.47894/mpal.69.1.02.

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The Yangtze carbonate platform (Southern China) recorded a long sedimentary evolution from Neoproterozoic to the basal Upper Triassic. During the Early and Middle Triassic, this platform was dominated by shallow-water carbonates. In various sectors of the platform, the Middle Triassic (Anisian-Ladinian) succession contain abundant assemblages of benthic foraminifera and calcareous algae. Following a previous paper about the Middle Triassic dasycladalean algae from SW Guizhou Province, the present study describes algae and microproblematic organisms from three sections: Honyan, Longtou and Guanling. Some dasycladalean algae are well known from the Alpine-Dinaric domain: Diplopora annulatissima, D. annulata, Euteutloporella triasina, Macroporella dinarica, Oligoporella minutula, O. pilosa pilosa, Poncetella hexaster and Pseudodiplopora proba. However, the dasycladalean association is dominated by species belonging to the genus Kantia, including K. cf. dolomitica and K. cf. comelicana. New Kantia species (K. intusannulata n. sp., K. granieri n. sp., K. muxinanii n. sp.) are characterized by the presence of intusannulation, a feature unknown from the Kantia species in the Alpine domain. The dasycladalean association also contains new species of the genus Mizzia and specimens belonging to the organo-genus Acicularia and/or Terquemella. Besides, rare specimens of "Solenopora" and Rivularia-type cyanobacteria are also present. The algal association is accompanied by microproblematic organisms including Tubiphytes sp., Zorniella obscura, Plexoramea cerebriformis, Ladinella porata, and Baccanella floriformis. Anisian-Ladinian foraminifera complete the micropaleontological spectrum of the sections studied. The most important are Meandrospira dinarica, Endotriadella wirzi, Paleolituonella meridionalis, and Turriglomina mesotriasica. The microfossils from the Middle Triassic Yangtze carbonate platform of south China belong to the Eastern Tethys province. Some of these species are also present in the Western Tethys (Alpine Domain). The new species presented in this study are absent from the Alpine Domain and probably represent endemic species for the Eastern Tethys.
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19

Zhang, Qian-Qi, Jun Chen, and Hai-Chun Zhang. "The first Procercopidae (Insecta: Hemiptera) from the Jurassic Sangonghe Formation of northwestern China." Palaeontographica Abteilung A 322, no. 5-6 (May 17, 2022): 117–24. http://dx.doi.org/10.1127/pala/2022/0126.

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20

Tongiorgi, Marco, Leiming Yin, and Anna di Milia. "Lower Yushanian to lower Zhejiangian palynology of the Yangtze Gorges area (Daping and Huanghuachang sections), Hubei Province, South China." Palaeontographica Abteilung B 266, no. 1-6 (October 29, 2003): 1–160. http://dx.doi.org/10.1127/palb/266/2003/1.

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21

Yang, Zhihua, Xiuchun Jing, Hongrui Zhou, Xunlian Wang, Hui Ren, Yang Shen, and Ru Fan. "Katian (Late Ordovician) conodonts on the northwestern margin of the North China Craton." Journal of Paleontology 95, no. 4 (March 5, 2021): 805–26. http://dx.doi.org/10.1017/jpa.2021.11.

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AbstractUpper Ordovician strata exposed from the Baiyanhuashan section is the most representative Late Ordovician unit in the northwestern margin of the North China Craton (NCC). In total, 1,215 conodont specimens were obtained from 24 samples through the Wulanhudong and Baiyanhuashan formations at the Baiyanhuashan section. Thirty-six species belonging to 17 genera, including Tasmanognathus coronatus new species, are present. Based on this material, three conodont biozones—the Belodina confluens Biozone, the Yaoxianognathus neimengguensis Biozone, and the Yaoxianognathus yaoxianensis Biozone—have been documented, suggesting that the Baiyanhuashan conodont fauna has a stratigraphic range spanning the early to middle Katian. The Baiyanhuashan conodont fauna includes species both endemic to North China and widespread in tropical zones, allowing a reassessment of the previous correlations of the Katian conodont zonal successions proposed for North China with those established for shallow-water carbonate platforms at low latitudes.UUID: http://zoobank.org/7cedbd4a-4f7a-4be6-912f-a27fd041b586
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22

Bai, Lingqi, Pu Huang, Ning Yang, Wenxin Ju, Jianbo Liu, James F. Basinger, Honghe Xu, and Jinzhuang Xue. "A new Late Devonian flora from Sonid Zuoqi, Inner Mongolia, northeastern China." Journal of Paleontology 96, no. 2 (October 22, 2021): 462–84. http://dx.doi.org/10.1017/jpa.2021.93.

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AbstractThe Silurian and Devonian plant fossil record is the basis for our understanding of the early evolution of land plants, yet our appreciation of early global phytogeographic evolution has been constrained by the focus of most studies on deposits from Europe, North America, and, more recently, South China. Devonian plants have been recorded rarely from northeastern China, and among previous records, few plants have been illustrated and formally described. In this article, megafossil plants representing a Late Devonian-aged (probably Famennian) flora are described from a locality at northern Sonid Zuoqi, Inner Mongolia, NE China. The flora includes Melvillipteris sonidia new species, Archaeopteris sp., and fragments of some other plants. The new plant shows main axes and two orders of lateral branches. The first-order branches of this plant show a typical zigzag appearance and are borne in pairs on main axes. Second-order branches are straight or slightly flexed, and are borne helically or alternately on first-order branches. Sterile ultimate appendages and fertile structures of M. sonidia n. sp. are borne alternately on second-order branches. An associated palynological assemblage, as well as U-Pb ages of detrital zircon grains from adjacent horizons, are also reported, indicating a Late Devonian age in accord with the megafossil plants. The present study contributes to our appreciation of the Devonian floristic diversity of the Xing'an Block, and, through our review of the record of early vascular plants from NE China, more broadly to the understanding of the mid-latitude vegetation of the Northern Hemisphere during the Late Devonian.
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23

Wei, Xin, Zhi-Qiang Zhou, Ren-Bin Zhan, Rong-Chang Wu, Fang-Yi Gong, and Jian-Bo Liu. "Darriwilian (Middle Ordovician) new trilobites from the Upper Yangtze Region, South China, and their macroevolutionary and paleobiogeographic implications." Journal of Paleontology 96, no. 2 (December 9, 2021): 394–411. http://dx.doi.org/10.1017/jpa.2021.110.

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AbstractTwo new genera and six new species of trilobites are systematically documented herein: Sinagnostus mirabilis new genus new species, Yanpingia punctata n. gen. n. sp., Illaenus taoyuanensis n. sp., Panderia striolatus n. sp., Nileus yichongqiaoensis n. sp., and Paratiresias peculiaris n. sp. The materials were collected from the Darriwilian (late Middle Ordovician) strata in the Upper Yangtze Region, South China. Also provided is an emended diagnosis of the genus Paratiresias based on the new species Paratiresias peculiaris, which is the oldest known species of this genus with an extremely narrow (sag. and exsag.) preglabellar field. Those Chinese species previously referred to Nanillaenus are reassigned to Illaenus sensu lato. These trilobites add new data for the Darriwilian trilobite macroevolution and show highly endemic to South China and the faunal exchanges between South China and Tarim, Kazakhstan, Alborz, as well as Sibumasu and North China.UUID: http://zoobank.org/ec3be9be-b003-4367-910d-7a0ac4edc982
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24

Guo, Junfeng, Jian Han, Heyo Van Iten, Zuchen Song, Yaqin Qiang, Wenzhe Wang, Zhifei Zhang, and Guoxiang Li. "A ten-faced hexangulaconulariid from Cambrian Stage 2 of South China." Journal of Paleontology 95, no. 5 (March 29, 2021): 957–64. http://dx.doi.org/10.1017/jpa.2021.25.

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AbstractHexangulaconulariids (Cambrian stages 1–2) are an extinct group of medusozoan polyps having a biradially symmetrical, fan-shaped periderm that is distinct from those of medusozoan polyps showing three-, four-, five-, or six-fold radial symmetry. Hexangulaconulariids exhibit substantial variation in gross morphology, including variation in the number of faces on each of the two major sides of the periderm. An intermediate taxon of hexangulaconulariids with ten faces (five on each major side) was expected. Here we describe a new hexangulaconulariid, Decimoconularia isofacialis new genus new species from Bed 5 of the Yanjiahe Formation (Cambrian Stage 2) in the Three Gorges area of Hubei Province, China. The new taxon differs from other hexangulaconulariids (Arthrochites, Hexaconularia, and Septuconularia) mainly in possessing a total of ten faces. The two lateral margins are each marked by a ridge in about the apertural half of the periderm and by a collinear furrow in about the apical half, while the five faces on each major side are bounded by a furrow in about the apertural half and by a collinear ridge in about the apical half. Among hexangulaconulariids, Decimoconularia and Septuconularia may be more closely related to each other than either genus is to Arthrochites or Hexaconularia.UUID: http://zoobank.org/ca270a3b-25ee-4d1f-bdeb-91a963370e70
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25

Wang, Yaquiong, Jingeng Sha, Yanhong Pan, and Xiaolin Zhang. "Early Cretaceous nonmarine ostracod biostratigraphy of western Liaoning area, NE China." Micropaleontology 61, no. 1-2 (2015): 135–45. http://dx.doi.org/10.47894/mpal.61.1.10.

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The Early Cretaceous ostracod fauna in western Liaoning is divided into eight successive ostracod assemblages. These assemblages have provided information about age constraint of relevant nonmarine Early Cretaceous strata: Yixian Formation – Hauterivian to Barremian, probably up to Aptian; Jiufotang Formation – Barremian to Aptian; Fuxin Formation – Aptian; Sunjiawan Formation – Albian. According to the revised age for the upper part of the Yixian Formation in the Kazuo – Chaoyang Basin, which is Hauterivian – Barremian, Ziziphocypris linchengensis is the earliest record of the genus Ziziphocypris. This work demonstrates that the supra-regionally distributed ostracod species, including species of Cypridea, are useful for biostratigraphic correlation and age determination of lacustrine deposits. In contrast, the endemic Cypridea species are helpful for regional biostratigraphic correlation of scattered basins within western Liaoning.
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26

Qin, Junge, Yuting Zhong, Lidong Zhu, Wenguang Yang, and Yaqiong Wang. "Temporal constraints on the Dalazi Biota from Luozigou Basin, northeast China." Cretaceous Research 128 (December 2021): 104977. http://dx.doi.org/10.1016/j.cretres.2021.104977.

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27

Wang, Ye, Yue Wang, Wei Du, Yulan Li, Fan Liu, and Mingsheng Zhao. "Ediacaran pithy macroalga Lanceaphyton n. gen. from South China." Journal of Paleontology 96, no. 2 (November 15, 2021): 452–61. http://dx.doi.org/10.1017/jpa.2021.98.

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AbstractWith differentiated tissues and organs, a high-level eukaryotic macroalga Lanceaphyton xiaojiangensis n. gen. n. sp. lived on the middle–late Ediacaran (ca. 560–551 Ma) seafloor in South China. Its body had a pith (perhaps mechanical tissue) and outer tissue (perhaps epidermis and/or cortex). The lance-like macroalga consists of an unbranching thallus that grew over the sediment surface for sunlight and a holdfast grown into sediments to keep the thallus fixed on the seafloor. The pithy stipe (lower thallus) might have served to support the upper pithless thallus for photosynthesis. The holdfast is composed of a tapering pithy rhizome growing down into the sediments, with many filamentous pithless rhizoids dispersedly growing within the sediments. With the differentiated tissues and organs, especially the pith accounting for about half of the width of the rhizome and stipe, Lanceaphyton n. gen. was a high-level eukaryotic macroalga, similar to phaeophytes in morphological features, but further research is needed on its microstructural details. The pithy macroalga shows that the macroalgal pith had emerged in the Ediacaran.UUID: http://zoobank.org/bc924c5c-84e4-4170-9ca1-caee0d56c6d5.
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28

Wu, Yixiao, Jianguo Li, Miaoqin Lin, and Eva Koppelhus. "Triprojectacites in the Songliao Basin, Northeast China: Systematics, biostratigraphy and evolution." Cretaceous Research 135 (July 2022): 105193. http://dx.doi.org/10.1016/j.cretres.2022.105193.

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29

Liang, Junhui, Ying Wang, Chungkun Shih, and Dong Ren. "Chuanblatta gen. nov. sexually dimorphic cockroaches of Raphidiomimidae (Blattaria) from the Jiulongshan Formation in China." Palaeontographica Abteilung A 321, no. 1-6 (January 10, 2022): 3–17. http://dx.doi.org/10.1127/pala/2021/0113.

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30

Ling, Chenchen, Jin Peng, Hui Zhang, Yifan Wang, Yunbin Shao, Quanyi Sun, and Qiujun Wang. "Saetaspongia sponges from the Cambrian (Stage 4) Balang Formation of Guizhou, China." Journal of Paleontology 95, no. 5 (May 7, 2021): 944–56. http://dx.doi.org/10.1017/jpa.2021.29.

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AbstractSaetaspongia so far cannot be confidently assigned to any class-level crown group. Clarifying its phylogenetic position requires new information provided by more detailed studies of previously described and/or new material. Some sponge fossils with the typical skeletal architecture of Saetaspongia have recently been recognized in the Cambrian (Stage 4) Balang Biota of Guizhou, China, including S. jianhensis new species and S. cf. S. densa. The new taxon is characterized by the following features: spicules are fine monaxons and are inclined to be loosely to densely arranged into plumose arrays; skeleton is composed primarily of one major plumose bundle, with an uncertain number (perhaps two) of small plumose arrays; and primary skeleton is occasionally interspersed with some irregularly oriented individual spicules. An additional specimen consisting of large monaxons, with plumose structures and overlying irregular coarse monaxons, closely fits the description and illustrations of previously described S. cf. S. densa. By combining information from previous studies and the present research, fossil evidence indicates that the plumose architecture is a critical feature diagnostic of Saetaspongia and that there are no hexactine-based spicules in this genus. The new material from the Balang Biota further supports the notion that Saetaspongia has a protomonaxonid rather than a hexactinellid affinity. Fossil evidence suggests that Saetaspongia had a wide biogeographic distribution during the early Cambrian and the stratigraphic distribution of this genus extends up to Stage 4.UUID: http://zoobank.org/e9ca5e4a-134c-4daa-9266-19085e32614f.
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Luo, Yanchao, Xindong Cui, Tuo Qiao, and Min Zhu. "A new dipnoan genus from the Middle Devonian of Huize, Yunnan, China." Journal of Systematic Palaeontology 19, no. 18 (September 17, 2021): 1303–15. http://dx.doi.org/10.1080/14772019.2022.2042409.

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32

Li, Gang, and Zijie Wu. "Early Cretaceous clam shrimp Yanjiestheria (Spinicaudata, Crustacea) from eastern Liaoning, northeastern China." Cretaceous Research 128 (December 2021): 104962. http://dx.doi.org/10.1016/j.cretres.2021.104962.

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33

Roček, Zbyněk, Liping Dong, Marissa Fabrezi, Yufen Rong, and Yuan Wang. "Carpus in Mesozoic anurans: The Early Cretaceous anuran Genibatrachus from northeastern China." Cretaceous Research 129 (January 2022): 104984. http://dx.doi.org/10.1016/j.cretres.2021.104984.

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34

Zheng, Wenjie, Masateru Shibata, Chun-Chi Liao, Soki Hattori, Dongchun Jin, Changzhu Jin, and Xing Xu. "First definitive ankylosaurian dinosaur from the Cretaceous of Jilin Province, northeastern China." Cretaceous Research 127 (November 2021): 104953. http://dx.doi.org/10.1016/j.cretres.2021.104953.

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35

Chen, Z. Q. "Lower Permian reef-dwelling brachiopod faunas from the Tarim Basin, Northwest-China: biostratigraphy, palaeoecology and biogeography." Palaeontographica Abteilung A 272, no. 1-4 (December 15, 2004): 1–96. http://dx.doi.org/10.1127/pala/272/2004/1.

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36

Chen, Z. Q., and G. R. Shi. "Early Carboniferous brachiopod faunas and their biogeographical affinities from the western Kunlun Mountains, North-west China." Palaeontographica Abteilung A 268, no. 4-6 (April 29, 2003): 103–87. http://dx.doi.org/10.1127/pala/268/2003/103.

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37

Soto, Francisco, and Liao Weihua. "Corales rugosos (Tryplasmatidae, Mucophyllidae y Cystiphyllidae) de la Formación Arpishmebulaq (Lochkoviense) en el SE de las montakas ke Tian-Shan (NO de China)." Spanish Journal of Palaeontology 16, no. 2 (September 21, 2021): 255. http://dx.doi.org/10.7203/sjp.16.2.21603.

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En el presente trabajo se describen siete especies de corales rugosos pertenecientes a los géneros Tryplasma Lonsdale, 1845, Pseudotryplasma Ivaniya, 1958 y Mesophyllum Schlüter, l889 [subgénero Mesophyllum (Cystiphylloides) Chapman, 1893, sensu Birenheide, 1974] procedentes de la Formación Arpishmebulaq (Lochkoviense), en la sección estratigráfica de Arpishmebulaq (provincia de Xinjiang, SE de las Montañas de Tian-Shan, NO de China). Con la excepción de las especies Mesophyllum (Cystiphylloides) corniculum (Regnell, 1941) y M. (C.) cf. laticystis (Regnell, 1941) que eran conocidas ya en las Montañas de Tian-Shan (NO de China), las demás especies/subespecies incluidas en el trabajo, Tryplasma aequabile Lonsdale, 1845, Typlasma hercynica (Peetz, 1901), T. cf. tomtchumyshensis Zheltonogova, 1961, Pseudotryplasma sp. A y Mesophyllum (Cystiphylloides) macrocystis cf. macrocystis (Schlüter, 1889) han sido citadas en determinadas localidades, especialmente de la Federación Rusa. Las distribuciones geográfica y estratigráfica de las mencionadas especies confirman unas relaciones paleobiogeograficas estrechas, durante el Lochkoviense, con el este de los Urales, Altay, el Salair, así como con el E de China (provincia de Jilin). Tales relaciones, aunque más moderadas, existen tambien con Tajikistan, Kazakhstan, E de Australia y E de Norte América (Nevada y Yukon) y han sido puestas ya de manifiesto por los autores (Soto y Liao, 1998, 1999) para otros taxones de corales rugosos procedentes de la misma formación y localidad.
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38

Boles, Walter E., and Trevor H. Worthy. "Foreword to published works from the Proceedings of the VII International Meeting of the Society of Avian Paleontology and Evolution held at the Australian Museum, in Sydney, from 18–23 August, 2008." Records of the Australian Museum 62, no. 1 (May 26, 2010): 2–3. http://dx.doi.org/10.3853/j.0067-1975.62.2010.1532.

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This volume comprises the Proceedings of the VII International Meeting of the Society for Avian Paleontology and Evolution (SAPE). The previous six meetings were held in North America, Europe and China. This seventh meeting marks the first gathering of the Society in the Southern Hemisphere. It was hosted by, and held at, the Australian Museum, in Sydney, from 18–23 August, 2008.
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39

Dai, Tao, Nigel C. Hughes, Xingliang Zhang, and Shanchi Peng. "Development of the early Cambrian oryctocephalid trilobite Oryctocarella duyunensis from western Hunan, China." Journal of Paleontology 95, no. 4 (March 17, 2021): 777–92. http://dx.doi.org/10.1017/jpa.2020.111.

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AbstractAbundant articulated specimens of the oryctocarine trilobite Oryctocarella duyunensis from the lower Cambrian (Stage 4, Series 2) Balang Formation at the Bulin section in western Hunan Province, South China, permit the description of all meraspid degrees. The maximum number of thoracic segments observed in this collection is 11. Meraspid growth was accompanied by progressive and gradual change in overall form, and this animal showed an homonymously segmented trunk with variation in the number of pygidial segments during ontogeny. Such variation permits a variety of plausible explanations, but a model of successive instars defined by the number of thoracic segments, and in suborder by the number of pygidial segments, is highly unlikely to explain the growth pattern because it would result in the loss of trunk segments between some instars. Degree-based ontogenetic staging is compatible with the variation observed.
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40

Fernando, Allan Gil S., Adrian Raymund C. Fernandez, and Martin G. Wiesner. "Braarudosphaera bigelowii morphotypes in the surface sediments of the southwestern South China Sea." Micropaleontology 59, no. 6 (2013): 579–86. http://dx.doi.org/10.47894/mpal.59.6.04.

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The present study reports on the distribution and occurrence of Braarudosphaera bigelowii in the surface sediments of the western part of the South China Sea (SCS), along the coast of Vietnam. This part of the SCS is a known upwelling region, characterized by low salinity conditions due to high annual rainfall and river run-off, confirming the results of earlier studies regarding the occurrence of B. bigelowii in shallow bays, nearshore, low salinity marine waters and upwelling areas. Morphometric analysis of B. bigelowii pentaliths in the western SCS revealed the presence of the 3 morphotypes proposed by Takano et al. (2006) based on the pentalith side lengths from coccospheres encountered in surface water samples. This paper also reports the occurrence of a new B. bigelowii morphotype in the SCS, corresponding to specimens with a pentalith side length of 3.5-4.0 microm. An attempt to relate the distribution of these morphotypes with temperature and salinity proved to be inconclusive, suggesting the possibility that other factors could be influencing the occurrence of the morphotypes in the study area.
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41

Pei, Rui, Yuying Qin, Aishu Wen, Qi Zhao, Zhe Wang, Zhanmin Liu, Weilesi Guo, et al. "A new troodontid from the Upper Cretaceous Gobi Basin of inner Mongolia, China." Cretaceous Research 130 (February 2022): 105052. http://dx.doi.org/10.1016/j.cretres.2021.105052.

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42

Soto, Francisco, and Wiehua Liao. "Rhizaphyllum Lindstrom, 1866 (Rugosa) del Devónico Inferior (Lochkoviense) en el SE de las Montañas de Tian-Shan (NO de China)." Spanish Journal of Palaeontology 13, no. 2 (March 3, 2022): 197. http://dx.doi.org/10.7203/sjp.24053.

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En el presente trabajo se describen varias especies del genero Rhizaphyllum Lindstrom, procedentes de la Formación Arpishmebulaq (Lochkoviense), en el SE de las Montañas de Tian-Shan (provincia de Xinjiang, NO de China). Las descripciones realizadas comprenden cinco especies, de !as cuales Rhizophyllum extensum se propone como nueva, R. sp. A y R. sp. B son también, probablemente, nuevas, pero la falta de material más abundante y mejor conservado hace que ias mantengamos, por el momento, en nomenclatura abierta. R. hedini (Regnell) era conocida solo por su morfología externa y ahora se describen por primera vez sus estructuras internas. Finalmente, R. cf. enorme (Etheridge) no habia sido citada nunca en China y su presencia en el area de Arpishmebulaq confirma relaciones biogeograficas durante el Lochkoviense con los Montes Urales, Salair, Asia Central (Altai) y Este de Australia.
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43

Ye, Yunqi, Dangpeng Xi, Lixin Sun, Dermeval Aparecido Do Carmo, Lucas Silveira Antonietto, Amanda Moreira Leite, Zuohuan Qin, and Xiaoqiao Wan. "Ostracoda from the Santonian–Campanian (Upper Cretaceous) Nenjiang and Sifangtai formations, Songliao Basin, northeastern China." Journal of Paleontology 96, no. 1 (October 5, 2021): 174–95. http://dx.doi.org/10.1017/jpa.2021.70.

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AbstractDespite the abundant literature on limnic Cretaceous ostracode faunas, the database on mid-Late Cretaceous taxa is still scarce. The Songliao Basin in northeastern China preserves a diverse assemblage of ostracode fossils from the Santonian–Campanian Nenjiang and Sifangtai formations. This rather unique material is of major importance to comprehend Early to mid-Late Cretaceous (Cenomanian–Campanian) limnic ostracode faunas and therefore the evolution of Late Cretaceous basins in China. A study of this fauna was conducted to detail the taxonomy of ostracode species from members 1 and 2 of the Nenjiang and Sifangtai formations in the Songliao Basin. Well-preserved specimens of 14 ostracode species were recovered from samples of the ZKY2-1 well in southwestern Songliao Basin: Scabriculocypris liaukhenensis Liu in Netchaeva et al., 1959, Ilyocyprimorpha netchaevae Su in Netchaeva et al., 1959, Cypridea acclinia Netchaeva in Netchaeva et al., 1959, Cypridea cavernosa Galeeva, 1955, Cypridea gracile Netchaeva in Netchaeva et al., 1959, Cypridea lepida Ye in DOFEAD, 1976, Cypridea squalida Sou in Netchaeva et al., 1959, Fabaeformiscandona? Disjuncta (Hao in Hao et al., 1974), Lycopterocypris profunda Lübimova, 1956, Mongolocypris magna (Hou, 1958), Mongolocypris tera (Su in Netchaeva et al., 1959), Talicypridea obliquecostae (Szczechura and Błaszyk, 1970), Talicypridea reticulata (Szczechura, 1978) and Renicypris renalata (Su in Hao et al., 1974). Four of the species identified received emended descriptions and diagnoses. Other important results include the first discussion on sexual dimorphism in Cypridea acclinia and Fabaeformiscandona? disjuncta, the first study on the ontogeny of Ilyocyprimorpha netchaevae, and the reassignment of Cypridea liaukhenensis to the genus Scabriculocypris. Several species recorded herein are also found in other continental far-eastern Asian basins, while genera range from worldwide to far-eastern Asian distribution; these results support strong affinities among faunas of Mongolia, China, and Japan.
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44

Fortelius, Mikael, and Zhaoqun Zhang. "An Oasis in the Desert? History of Endemism and Climate in the Late Neogene of North China." Palaeontographica Abteilung A 277, no. 1-6 (October 30, 2006): 131–41. http://dx.doi.org/10.1127/pala/277/2006/131.

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45

Maletz, Jörg, Chuanshang Wang, Wei Kai, and Xiaofeng Wang. "Upper Ordovician (Hirnantian) to Lower Silurian (Telychian, Llandovery) graptolite biostratigraphy of the Tielugou section, Shennongjia anticline, Hubei Province, China." PalZ 95, no. 3 (March 4, 2021): 453–81. http://dx.doi.org/10.1007/s12542-020-00544-5.

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AbstractThe Tielugou section, Shennongjia Anticline, Hubei Province (China) includes a relatively complete succession of Hirnantian (latest Ordovician) to basal Telychian (Llandovery, early Silurian) graptolite faunas. The section shows the first record of a fauna of the late Aeronian Stimulograptus halli Biozone from South China, even though the index species was not reported. The Stimulograptus sedgwickii Biozone may not be represented, indicating a possible gap at the base of the Stimulograptus halli Biozone. The interval yields a number of taxa that are elsewhere reported to originate only in the Stimulograptus halli Biozone. The youngest graptolitic levels are included in the Spirograptus guerichi Biozone based on specimens of Parapetalolithus dignus and Parapetalolithus palmeus not known from earlier intervals. Spirograptus guerichi is not represented in the section. The Tielugou section provides the first detailed information on the faunas and thickness of the encountered biostratigraphic units for the Shennongija region.
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Tsukiji, Yuta, Xingsheng Jin, Tianmin Du, Yoichi Azuma, Soki Hattori, Kentaro Nakada, Kentaro Nakayama, Yoshikazu Noda, and Wenjie Zheng. "First discovery of a deinonychosaur trackway from the lower Upper Cretaceous of southeastern China." Cretaceous Research 125 (September 2021): 104874. http://dx.doi.org/10.1016/j.cretres.2021.104874.

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47

Forel, Marie-Beatrice, Antoine Bercovici, and Jianxin Yu. "Ostracods after the end-Permian extinction in South China: insights into non-microbial survival." Micropaleontology 66, no. 5 (September 1, 2020): 377–96. http://dx.doi.org/10.47894/mpal.66.5.02.

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The taxonomy of ostracods from one deep-water, one shallow shelf and three paralic sections spanning the end-Permian extinction in South China (Guizhou and Yunnan) is summarized and discussed.We report on the occurrence of nine species, including mass occurrences of Hollinella panxiensis Wang, on the surface of these clastic Permian-Triassic transitional beds. The preservation of the material allows for the description of the central muscle scar field of Langdaia suboblonga Wang, which is the first observation of this character for the genus. These firstly described assemblages differ from those from post-extinction microbial deposits in being dominated by Palaeocopida. They illustrate survival without recovery after the end-Permian crisis, as none of the reported taxa participated in the subsequent Triassic diversification. We relate this phenomenon to clastic input and show that the patchy survival of benthic faunas following the crisis is an interplay between environments and adaptive potential. The persistence of Palaeocopida as a function of their depth distribution is discussed with the illustration of short-term survival of Hollinellidae in shallow areas, as opposed to the survival of Kirkbyidae in deep-marine waters until, at least, the Late Triassic.
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48

Yang, Xiao-Ju, and Jian-Guo Li. "A petrified wood Brachyoxylon from the Lower Cretaceous of Bangoin, Tibet (Xizang), Southwest China." Cretaceous Research 130 (February 2022): 105064. http://dx.doi.org/10.1016/j.cretres.2021.105064.

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49

Wang, Xin, Chungkun Shih, Zhong-Jian Liu, Longbiao Lin, and Kamal Jeet Singh. "Reconstructing the Callianthus plant–An early aquatic angiosperm from the Lower Cretaceous of China." Cretaceous Research 128 (December 2021): 104983. http://dx.doi.org/10.1016/j.cretres.2021.104983.

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50

Liu, Yi-Long, Lie-Bin Huang, Rui-Wen Zong, and Yi-Ming Gong. "The oldest eugaleaspiform (Galeaspida) from the Silurian Fentou Formation (Telychian, Llandovery) of Wuhan, South China." Journal of Systematic Palaeontology 19, no. 4 (February 16, 2021): 253–64. http://dx.doi.org/10.1080/14772019.2021.1883755.

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