The genome of the sea urchin Strongylocentrotus purpuratusAn Early Cambrian problematic fossil: Vetustovermis and its possible affinitiesPrecambrian animal life: probable developmental and adult cnidarian forms from Southwest ChinaSmall bilaterian fossils from 40 to 55 million years before the cambrianMercury anomalies and the timing of biotic recovery following the end-Triassic mass extinctionA microbial carbonate response in synchrony with the end-Triassic mass extinction across the SW UKReorganization of sea urchin gene regulatory networks at least 268 million years ago as revealed by oldest fossil cidaroid echinoidEarly Triassic wrinkle structures on land: stressed environments and oases for lifeSponge grade body fossil with cellular resolution dating 60 Myr before the CambrianComplexity and diversity of eyes in early Cambrian ecosystemsHomology and Potential Cellular and Molecular Mechanisms for the Development of Unique Feather Morphologies in Early BirdsComplex embryos displaying bilaterian characters from Precambrian Doushantuo phosphate deposits, Weng'an, Guizhou, ChinaProlonged Permian Triassic ecological crisis recorded by molluscan dominance in Late Permian offshore assemblagesRaman spectra of a Lower Cambrian ctenophore embryo from southwestern Shaanxi, ChinaPetrographic analysis of new specimens of the putative microfossil Vernanimalcula guizhouena (Doushantuo Formation, South China)Phanerozoic trends in the global diversity of marine invertebrates.Paleogenomics of echinoids reveals an ancient origin for the double-negative specification of micromeres in sea urchins.Paleogenomics of echinoderms.Development of lower Triassic wrinkle structures: implications for the search for life on other planets.Juvenile skeletogenesis in anciently diverged sea urchin clades.Eric Davidson's career as a paleontologist.Geochemistry. Life in the Early Triassic ocean.The early evolution of animals.Phosphatized polar lobe-forming embryos from the Precambrian of southwest China.Ecological ranking of Phanerozoic biodiversity crises: The Serpukhovian (early Carboniferous) crisis had a greater ecological impact than the end-OrdovicianNew probable cnidarian fossils from the lower Cambrian of the Three Gorges area, South China, and their ecological implicationsQuantitative analysis of substrate preference in Carboniferous stem group echinoidsEarly Cambrian animal diapause embryos revealed by X-ray tomographyMeroblastic cleavage identifies some Ediacaran Doushantuo (China) embryo-like fossils as metazoansA new ecological-severity ranking of major Phanerozoic biodiversity crisesLower Pennsylvanian (Bashkirian) echinoids from the Marble Falls Formation, San Saba, Texas, USAEarly Triassic stromatolites as post-mass extinction disaster formsA diverse assemblage of Permian echinoids (Echinodermata, Echinoidea) and implications for character evolution in early crown group echinoidsAftermath of the Permian-Triassic mass extinction event: Paleoecology of Lower Triassic carbonates in the western USAEvidence for seafloor microbial mats and associated metazoan lifestyles in Lower Cambrian phosphorites of Southwest ChinaA diverse trackway-dominated marine ichnoassemblage from the Lower Triassic in the northern Paleotethys: Ichnology and implications for biotic recoveryMicrobial mats in the terrestrial Lower Triassic of North China and implications for the Permian–Triassic mass extinctionThe prelude of the end-Permian mass extinction predates a postulated bolide impactAdditional records of ichnogenus Rhizocorallium from the Lower and Middle Triassic, South China: Implications for biotic recovery after the end-Permian mass extinctionA global marine sedimentary response to the end-Permian mass extinction: Examples from southern Turkey and the western United States
P50
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P50
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