Some Phanerozoic biotic radiations in the marine realm led to marine biodiversity additions, i.e., increases in the global number of genera to unprecedented levels. Each of the two alternative biodiversity curves implies five post-Cambrian events of this kind, which coincided with parts of the biotic radiations. However, differences between these curves do not allow to find coherent marine biodiversity additions with the only exception of those occurred at the interval of the Great Ordovician Biodiversification. The attempted interpretations indicate that the marine biodiversity additions increased the number of marine genera by 10-30 % (from the previous unprecedented level to that new). All additions were relati...
Most early Palaeozoic acritarchs are thought to represent a part of the marine phytoplankton and so ...
International audienceFollowing the appearance of numerous animal phyla during the 'Cambrian Explosi...
International audienceDiversification is a key property of life. Building on John Phillips' (1860) c...
International audienceIn this study, we examine how metazoan biodiversity has accumulated from the l...
International audienceThe early Palaeozoic radiation has generally been documented through the promo...
The Cambrian 'Explosion', located by many authors between 540 and 520 million years ago (Ma), is con...
Long-term transitions in the composition of EarthÕs marine biota during the Phanero-zoic have histor...
Contrasts between the Cambrian Explosion (CE) and the Great Ordovician Biodiversification Event (GOB...
The ‘Great Ordovician Biodiversification Event’ (GOBE) saw a spectacular increase in marine biodiver...
The early Palaeozoic Era records the initial biodiversification of the Phanerozoic. The increase in ...
The ‘Great Ordovician Biodiversification Event’ comprises the rapid diversification of marine organi...
Most early Palaeozoic acritarchs are thought to represent a part of the marine phytoplankton and so ...
International audienceFollowing the appearance of numerous animal phyla during the 'Cambrian Explosi...
International audienceDiversification is a key property of life. Building on John Phillips' (1860) c...
International audienceIn this study, we examine how metazoan biodiversity has accumulated from the l...
International audienceThe early Palaeozoic radiation has generally been documented through the promo...
The Cambrian 'Explosion', located by many authors between 540 and 520 million years ago (Ma), is con...
Long-term transitions in the composition of EarthÕs marine biota during the Phanero-zoic have histor...
Contrasts between the Cambrian Explosion (CE) and the Great Ordovician Biodiversification Event (GOB...
The ‘Great Ordovician Biodiversification Event’ (GOBE) saw a spectacular increase in marine biodiver...
The early Palaeozoic Era records the initial biodiversification of the Phanerozoic. The increase in ...
The ‘Great Ordovician Biodiversification Event’ comprises the rapid diversification of marine organi...
Most early Palaeozoic acritarchs are thought to represent a part of the marine phytoplankton and so ...
International audienceFollowing the appearance of numerous animal phyla during the 'Cambrian Explosi...
International audienceDiversification is a key property of life. Building on John Phillips' (1860) c...