315 results on '"Yuan, XunLai"'
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2. Statistical estimation of the early to middle Ediacaran ocean redox architecture in the Yangtze block of South China
3. Tonian carbonaceous compressions indicate that Horodyskia is one of the oldest multicellular and coenocytic macro-organisms
4. Chuaria and Tawuia fossils from ∼1.0 Ga rocks in North China: Implications for a polyphyletic origin of Chuaria and a potential biological link between these two widespread Proterozoic taxa
5. Tonian discoidal fossils from North China: Relating discs to worm-like annulated tubes and their paleoecological and evolutionary implications
6. The Proterozoic Qinggouzi microfossil assemblage and its biostratigraphic constraints on the Great Unconformity in northeastern North China Craton
7. Detrital zircon geochronology and stratigraphy of the Proterozoic strata in the Olongbuluke terrane of Northwest China: Implications for the Great Unconformity
8. SIMS Pb-Pb dating of phosphates in the Proterozoic strata of SE North China Craton: Constraints on eukaryote evolution
9. Taphonomic study of Chuaria fossils from the Ediacaran Lantian biota of South China
10. One-billion-year-old epibionts highlight symbiotic ecological interactions in early eukaryote evolution
11. The Proterozoic macrofossil Tawuia as a coenocytic eukaryote and a possible macroalga
12. Distribution of Ediacaran acanthomorphic acritarchs in the lower Doushantuo Formation of the Yangtze Gorges area, South China: Evolutionary and stratigraphic implications
13. Raman spectroscopy and structural heterogeneity of carbonaceous material in Proterozoic organic-walled microfossils in the North China Craton
14. A tale of three taphonomic modes: The Ediacaran fossil Flabellophyton preserved in limestone, black shale, and sandstone
15. A one-billion-year-old multicellular chlorophyte
16. Repositioning the Great Unconformity at the southeastern margin of the North China Craton
17. Death march of a segmented and trilobate bilaterian elucidates early animal evolution
18. A Uniquely Preserved Ediacaran Fossil with Direct Evidence for a Quilted Bodyplan
19. Lichen-like Symbiosis 600 Million Years Ago
20. Phosphatized Multicellular Algae in the Neoproterozoic Doushantuo Formation, China, and the Early Evolution of Florideophyte Red Algae
21. Controls on fossil pyritization: Redox conditions, sedimentary organic matter content, and Chuaria preservation in the Ediacaran Lantian Biota
22. Macroscopic Carbonaceous Compressions in a Terminal Proterozoic Shale: A Systematic Reassessment of the Miaohe Biota, South China
23. Morphological Reconstruction of Miaohephyton bifurcatum, a Possible Brown Alga from the Neoproterozoic Doushantuo Formation, South China
24. Composition and pore characteristics of black shales from the Ediacaran Lantian Formation in the Yangtze Block, South China
25. Spiculogenesis and biomineralization in early sponge animals
26. Organic-walled microfossils from the Tonian Gouhou Formation, Huaibei region, North China Craton, and their biostratigraphic implications
27. New material of the biomineralizing tubular fossil Sinotubulites from the late Ediacaran Dengying Formation, South China
28. The rangeomorph fossil Charnia from the Ediacaran Shibantan biota in the Yangtze Gorges area, South China
29. Orbisiana linearis from the early Ediacaran Lantian Formation of South China and its taphonomic and ecological implications
30. The origin and early evolution of complex organisms
31. Biostratigraphic and chemostratigraphic constraints on the age of early Neoproterozoic carbonate successions in North China
32. An integrated carbon, oxygen, and strontium isotopic studies of the Lantian Formation in South China with implications for the Shuram anomaly
33. Fluctuation of shelf basin redox conditions in the early Ediacaran: Evidence from Lantian Formation black shales in South China
34. Interactions between Ediacaran animals and microbial mats: Insights from Lamonte trevallis, a new trace fossil from the Dengying Formation of South China
35. EXCEPTIONAL PRESERVATION OF MACROFOSSILS FROM THE EDIACARAN LANTIAN AND MIAOHE BIOTAS, SOUTH CHINA
36. PHOSPHATIZED ACANTHOMORPHIC ACRITARCHS AND RELATED MICROFOSSILS FROM THE EDIACARAN DOUSHANTUO FORMATION AT WENG'AN (SOUTH CHINA) AND THEIR IMPLICATIONS FOR BIOSTRATIGRAPHIC CORRELATION
37. Organic-walled microfossils from the early Neoproterozoic Liulaobei Formation in the Huainan region of North China and their biostratigraphic significance
38. Trace fossil evidence for Ediacaran bilaterian animals with complex behaviors
39. Cell differentiation and germ-soma separation in Ediacaran animal embryo-like fossils
40. Yangtziramulus zhangi New Genus and Species, a Carbonate-Hosted Macrofossil from the Ediacaran Dengying Formation in the Yangtze Gorges Area, South China
41. Pulsed Oxidation and Biological Evolution in the Ediacaran Doushantuo Formation
42. Ediacaran seawater temperature: Evidence from inclusions of Sinian halite
43. Carbon, sulfur, and oxygen isotope evidence for a strong depth gradient and oceanic oxidation after the Ediacaran Hankalchough glaciation
44. Cellular and Subcellular Structure of Neoproterozoic Animal Embryos
45. Evolution of Holdfast Diversity and Attachment Strategies of Ediacaran Benthic Macroalgae
46. Tetraradial symmetry in early poriferans
47. Carbon and sulfur isotope chemostratigraphy of the Neoproterozoic Quanji Group of the Chaidam Basin, NW China: Basin stratification in the aftermath of an Ediacaran glaciation postdating the Shuram event?
48. SHRIMP zircon U–Pb age constraints on Neoproterozoic Quruqtagh diamictites in NW China
49. New morphological observations for Paleoproterozoic acritarchs from the Chuanlinggou Formation, North China
50. The Lantian biota: A new window onto the origin and early evolution of multicellular organisms
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