966 results on '"Xiao, ShuHai"'
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2. Near-collapse of the geomagnetic field may have contributed to atmospheric oxygenation and animal radiation in the Ediacaran Period
3. The Ediacara Biota of the Wood Canyon formation: Latest Precambrian macrofossils and sedimentary structures from the southern Great Basin
4. Carbonate δ13C chemostratigraphy of the Hunjiang Group in North China and a tentative stratigraphic framework for the Meso-Neoproterozoic transition
5. Phylotranscriptomics unveil a Paleoproterozoic-Mesoproterozoic origin and deep relationships of the Viridiplantae
6. Recurrent photic zone euxinia limited ocean oxygenation and animal evolution during the Ediacaran
7. Tonian carbonaceous compressions indicate that Horodyskia is one of the oldest multicellular and coenocytic macro-organisms
8. Mid-latitudinal habitable environment for marine eukaryotes during the waning stage of the Marinoan snowball glaciation
9. Ordovician origin and subsequent diversification of the brown algae
10. Trace element evidence for diverse origins of superheavy pyrite in Neoproterozoic sedimentary strata
11. The Proterozoic Qinggouzi microfossil assemblage and its biostratigraphic constraints on the Great Unconformity in northeastern North China Craton
12. New record of the green algal fossil Proterocladus and coexisting microfossils from the Meso-Neoproterozoic Diaoyutai Formation in southern Liaoning, North China
13. Phosphatized microfossils from the Miaohe Member of South China and their implications for the terminal Ediacaran biodiversity decline
14. Saccorhytus is an early ecdysozoan and not the earliest deuterostome
15. Biomineralization by particle attachment in early animals
16. Enigmatic provenance of carbonate clasts in Cryogenian glacial diamictite of the Nantuo Formation in South China
17. Integrated study of the Doushantuo Formation in northwestern Hunan Province: Implications for Ediacaran chemostratigraphy and biostratigraphy in South China
18. An authigenic response to Ediacaran surface oxidation: Remarkable micron-scale isotopic heterogeneity revealed by SIMS
19. A microfossil assemblage from the Ediacaran Doushantuo Formation in the Shennongjia area (Hubei Province, South China): Filling critical paleoenvironmental and biostratigraphic gaps
20. Earliest Ediacaran speleothems and their implications for terrestrial life after the Marinoan snowball Earth
21. Phylotranscriptomic insights into a Mesoproterozoic–Neoproterozoic origin and early radiation of green seaweeds (Ulvophyceae)
22. Preservation of early Tonian macroalgal fossils from the Dolores Creek Formation, Yukon
23. Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China
24. Organic-walled microfossils from the Ediacaran Sete Lagoas Formation, Bambuí Group, Southeast Brazil: taxonomic and biostratigraphic analyses
25. Deposition or diagenesis? Probing the Ediacaran Shuram excursion in South China by SIMS
26. Ediacaran sponges, animal biomineralization, and skeletal reefs
27. One-billion-year-old epibionts highlight symbiotic ecological interactions in early eukaryote evolution
28. The Proterozoic macrofossil Tawuia as a coenocytic eukaryote and a possible macroalga
29. Distribution of Ediacaran acanthomorphic acritarchs in the lower Doushantuo Formation of the Yangtze Gorges area, South China: Evolutionary and stratigraphic implications
30. Iron phosphate in the Ediacaran Doushantuo Formation of South China: A previously undocumented marine phosphate sink
31. The terminal Ediacaran tubular fossil Cloudina in the Yangtze Gorges area of South China
32. Seawater barium and sulfide removal improved marine habitability for the Cambrian Explosion of early animals.
33. Probable benthic macroalgae from the Ediacara Member, South Australia
34. Seaweeds through time: Morphological and ecological analysis of Proterozoic and early Paleozoic benthic macroalgae
35. Raman spectroscopy and structural heterogeneity of carbonaceous material in Proterozoic organic-walled microfossils in the North China Craton
36. A tale of three taphonomic modes: The Ediacaran fossil Flabellophyton preserved in limestone, black shale, and sandstone
37. Using SIMS to decode noisy stratigraphic δ13C variations in Ediacaran carbonates
38. Hydrothermal influence on barite precipitates in the basal Ediacaran Sete Lagoas cap dolostone, São Francisco Craton, central Brazil
39. Wide but not ubiquitous distribution of glendonite in the Doushantuo Formation, South China: Implications for Ediacaran climate
40. Cryptic terrestrial fungus-like fossils of the early Ediacaran Period
41. A one-billion-year-old multicellular chlorophyte
42. Corrigendum to “The Ediacara Biota of the Wood Canyon formation: Latest Precambrian macrofossils and sedimentary structures from the southern Great Basin” [Global and Planetary Change (2024) 104547; 1–17]
43. A new record of late Ediacaran acritarchs from La providencia group (Tandilia System, Argentina) and its biostratigraphical significance
44. Repositioning the Great Unconformity at the southeastern margin of the North China Craton
45. Detrital graphite particles in the Cryogenian Nantuo Formation of South China: Implications for sedimentary provenance and tectonic history
46. Musculature of an Early Cambrian cycloneuralian animal
47. The earliest Elcanidae (Insecta, Orthoptera) from the Upper Triassic of North America
48. Breaking down the lithification bias : the effect of preferential sampling of larger specimens on the estimate of species richness, evenness, and average specimen size
49. TAPHONOMY AND BIOLOGICAL AFFINITY OF THREE-DIMENSIONALLY PHOSPHATIZED BROMALITES FROM THE MIDDLE ORDOVICIAN WINNESHIEK LAGERSTÄTTE, NORTHEASTERN IOWA, USA
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