Works matching IS 00721050 AND DT 2006 AND VI 41 AND IP 3/4
Results: 13
Distinguishing anomalocaridids from arthropods and priapulids.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 259, doi. 10.1002/gj.1050
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The mammal fauna in the Early Cretaceous Jehol Biota: implications for diversity and biology of Mesozoic mammals.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 439, doi. 10.1002/gj.1054
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Brachiopod diversity patterns from Carboniferous to Triassic in South China.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 345, doi. 10.1002/gj.1047
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Pterosaur assemblages of the Jehol Biota and their implication for the Early Cretaceous pterosaur radiation.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 405, doi. 10.1002/gj.1046
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Feathers and 'feather-like' integumentary structures in Liaoning birds and dinosaurs.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 395, doi. 10.1002/gj.1057
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Diversity patterns of Carboniferous and Permian rugose corals in South China.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 329, doi. 10.1002/gj.1041
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Evolutionary radiation of the Jehol Biota: chronological and ecological perspectives.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 377, doi. 10.1002/gj.1045
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Preface.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 255, doi. 10.1002/gj.1056
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The rise of ginkgoalean plants in the early Mesozoic: a data analysis.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 363, doi. 10.1002/gj.1049
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β-diversity fluctuations in Early-Mid Ordovician brachiopod communities of South China.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 271, doi. 10.1002/gj.1040
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Ordovician graptolite evolutionary radiation: a review.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 289, doi. 10.1002/gj.1051
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Non-avian dinosaur fossils from the Lower Cretaceous Jehol Group of western Liaoning, China.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 419, doi. 10.1002/gj.1044
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An introduction to Ordovician bivalves of southern China, with a discussion of the early evolution of the Bivalvia.
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- Geological Journal, 2006, v. 41, n. 3/4, p. 303, doi. 10.1002/gj.1048
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