rap th relatively long-ranging, extending into the Silurian, the extinction rate is low throughout the Period, increasing only slightly in the latest Late Ordovician. The normalised diversity curve is characterised by an increasing trend in the Mid Ordovician, followed by a jaw-bearing polychaetes took place during theOrdovician (Mid Ordovician) time onwards (Hints et al., 2004). Because the soft-body anatomy of polychaete annelids has very low preservation potential, scolecodonts provid
Studies of size trends have increased in recent times. This work continues a growing number of studi...
Abstract: The extinctions that occurred in the latest Ordovician and earliest and latest Wenlock, we...
The Upper Ordovician to Lower Silurian shallow marine succession of Anticosti Island, eastern Canada...
rap th relatively long-ranging, extending into the Silurian, the extinction rate is low throughout t...
Scolecodonts are common microfossils in Palaeozoic rocks, bearing witness to the extensive radiation...
Eunicidan polychaetes formed a significant part of Early Palaeozoic marine invertebrate communities,...
The Great Ordovician Biodiversification Event (GOBE) refers to one of the greatest increases in biod...
The extent to which biological diversity affects rates of diversification is central to understandin...
The extent to which biological diversity affects rates of diversification is central to understandin...
Graptoloid evolutionary dynamics show a marked contrast from the Ordovician to the Silurian. Subdued...
The extent to which biological diversity affects rates of diversification is central to understandin...
Two distinct regimes of extinction dynamic are present in the major marine zooplankton group, the gr...
The early Palaeozoic Era records the initial biodiversification of the Phanerozoic. The increase in ...
The End Ordovician Extinction Event (EOEE) had little impact on supra-specific diversity and dispari...
During the Ordovician Radiation, domination of benthic marine communities shifted away from trilobit...
Studies of size trends have increased in recent times. This work continues a growing number of studi...
Abstract: The extinctions that occurred in the latest Ordovician and earliest and latest Wenlock, we...
The Upper Ordovician to Lower Silurian shallow marine succession of Anticosti Island, eastern Canada...
rap th relatively long-ranging, extending into the Silurian, the extinction rate is low throughout t...
Scolecodonts are common microfossils in Palaeozoic rocks, bearing witness to the extensive radiation...
Eunicidan polychaetes formed a significant part of Early Palaeozoic marine invertebrate communities,...
The Great Ordovician Biodiversification Event (GOBE) refers to one of the greatest increases in biod...
The extent to which biological diversity affects rates of diversification is central to understandin...
The extent to which biological diversity affects rates of diversification is central to understandin...
Graptoloid evolutionary dynamics show a marked contrast from the Ordovician to the Silurian. Subdued...
The extent to which biological diversity affects rates of diversification is central to understandin...
Two distinct regimes of extinction dynamic are present in the major marine zooplankton group, the gr...
The early Palaeozoic Era records the initial biodiversification of the Phanerozoic. The increase in ...
The End Ordovician Extinction Event (EOEE) had little impact on supra-specific diversity and dispari...
During the Ordovician Radiation, domination of benthic marine communities shifted away from trilobit...
Studies of size trends have increased in recent times. This work continues a growing number of studi...
Abstract: The extinctions that occurred in the latest Ordovician and earliest and latest Wenlock, we...
The Upper Ordovician to Lower Silurian shallow marine succession of Anticosti Island, eastern Canada...