about
Links between global taxonomic diversity, ecological diversity and the expansion of vertebrates on landThe diversity of Odonata and their endophytic ovipositions from the Upper Oligocene Fossillagerstätte of Rott (Rhineland, Germany)The last "pelycosaur": a varanopid synapsid from the Pristerognathus Assemblage Zone, Middle Permian of South AfricaCorrected placement of Mus-Rattus fossil calibration forces precision in the molecular tree of rodentsMacroevolutionary patterns in the Aphidini aphids (Hemiptera: Aphididae): diversification, host association, and biogeographic originsEstimating the age of fire in the Cape flora of South Africa from an orchid phylogenyREDESCRIPTION OF PLATYCRANIELLUS ELEGANS (THERAPSIDA, CYNODONTIA) FROM THE LOWER TRIASSIC OF SOUTH AFRICA, AND THE CLADISTIC RELATIONSHIPS OF EUTHERIODONTSAnkylosaurs from the Price River Quarries, Cedar Mountain Formation (Lower Cretaceous), east-central UtahThe timetable of evolution.Anthropogenic transformation of the terrestrial biosphere.Extinction space--a method for the quantification and classification of changes in morphospace across extinction boundaries.Interdependence of specialization and biodiversity in Phanerozoic marine invertebrates.Recent long-distance dispersal overshadows ancient biogeographical patterns in a pantropical angiosperm family (Simaroubaceae, Sapindales).Mesozoic dinosaurs from Brazil and their biogeographic implications.Fossil-calibrated molecular phylogenies reveal that leaf-mining moths radiated millions of years after their host plants.Using fossils to break long branches in molecular dating: a comparison of relaxed clocks applied to the origin of angiosperms.New information on Riograndia guaibensis Bonaparte, Ferigolo & Ribeiro, 2001 (Eucynodontia, Tritheledontidae) from the Late Triassic of southern Brazil: anatomical and biostratigraphic implications.Status of Divisions of the International Geologic Time ScalePlant fossil record and survival analysesImpacts, volcanism and mass extinction: random coincidence or cause and effect?Phylogenetic relationships of procolophonid parareptiles with remarks on their geological recordThe two Suvasvesi impact structures, Finland: Argon isotopic evidence for a “false” impact crater doubletAN EARLY HERBIVOROUS LIZARD FROM THE LOWER CRETACEOUS OF JAPANThe impact of the Congo River and its tributaries on the rodent genus Praomys: speciation origin or range expansion limit?The late rifting phase and continental break-up of the southern South Atlantic: the mode and timing of volcanic rifting and formation of earliest oceanic crustPalaeomagnetism in the Sines massif (SW Iberia) revisited: evidences for Late Cretaceous hydrothermal alteration and associated partial remagnetizationReconciling Cretaceous paleomagnetic and marine magnetic data for Iberia: New Iberian paleomagnetic polesTesting Iberian kinematics at Jurassic-Cretaceous timesPetrophysical properties in the Iberian Range and surrounding areas (NE Spain): 1-densityDeformation of a young salt giant: regional topography of the Red Sea Miocene evaporitesTesting the role of biological interactions in the evolution of mid-Mesozoic marine benthic ecosystemsHistory, philosophy, and application of the Global Stratotype Section and Point (GSSP)Phylogenetic analyses of band-winged grasshoppers (Orthoptera, Acrididae, Oedipodinae) reveal convergence of wing morphology
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P2860
description
im Juni 2004 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в червні 2004
@uk
name
Geologic Time Scale 2004 - why, how, and where next!
@en
Geologic Time Scale 2004 - why, how, and where next!
@nl
type
label
Geologic Time Scale 2004 - why, how, and where next!
@en
Geologic Time Scale 2004 - why, how, and where next!
@nl
prefLabel
Geologic Time Scale 2004 - why, how, and where next!
@en
Geologic Time Scale 2004 - why, how, and where next!
@nl
P2860
P1433
P1476
Geologic Time Scale 2004 - why, how, and where next!
@en
P2860
P304
P356
10.1080/00241160410006483
P577
2004-06-01T00:00:00Z