We introduce and briefly summarize a collection of papers contextualizing the onset of the Great Ordovician Biodiversification Event, initiated during the first meeting of IGCP project 653 at Van Mildert College, Durham University, UK, in September 2016
Rock successions in Britain and Ireland, and more especially those in North Wales, were instrumental...
In the Central Anti-Atlas (Morocco), the lower part of the Fezouata Shale has yielded locally abunda...
The lower Cambrian Lagerstätte of Sirius Passet, Nansen Land, North Greenland, is one of the oldest ...
We introduce and briefly summarize a collection of papers contextualizing the onset of the Great Ord...
Following the appearance of numerous animal phyla during the ‘Cambrian Explosion’, the ‘Great Ordovi...
The Great Ordovician Biodiversification Event (GOBE) was the most rapid and sustained increase in ma...
The breakup of the L-chondrite parent body in the asteroid belt 466 million years (Ma) ago still del...
A review of biodiversity curves of marine organisms indicates that, despite fluctuations in amplitud...
In 1997, IGCP Project No. 410 was established to appraise known records of Ordovician biotas, in ord...
Nectocaridids are soft-bodied Cambrian organisms that have been controversially interpreted as primi...
A bivalve-dominated molluscan fauna is described from the Darriwilian (Middle Ordovician) Stairway S...
Brachiopods are among the first animal phyla to emerge from the Cambrian Explosion, rapidly diversif...
In the last decade, at least thirty individual hypotheses have been invoked to explain the Cambrian ...
Classification of extinction events and their severity is generally based on taxonomic counts. The e...
The Hirnantian mass extinction is recognized as the first of the "big three" extinctions and, along ...
Rock successions in Britain and Ireland, and more especially those in North Wales, were instrumental...
In the Central Anti-Atlas (Morocco), the lower part of the Fezouata Shale has yielded locally abunda...
The lower Cambrian Lagerstätte of Sirius Passet, Nansen Land, North Greenland, is one of the oldest ...
We introduce and briefly summarize a collection of papers contextualizing the onset of the Great Ord...
Following the appearance of numerous animal phyla during the ‘Cambrian Explosion’, the ‘Great Ordovi...
The Great Ordovician Biodiversification Event (GOBE) was the most rapid and sustained increase in ma...
The breakup of the L-chondrite parent body in the asteroid belt 466 million years (Ma) ago still del...
A review of biodiversity curves of marine organisms indicates that, despite fluctuations in amplitud...
In 1997, IGCP Project No. 410 was established to appraise known records of Ordovician biotas, in ord...
Nectocaridids are soft-bodied Cambrian organisms that have been controversially interpreted as primi...
A bivalve-dominated molluscan fauna is described from the Darriwilian (Middle Ordovician) Stairway S...
Brachiopods are among the first animal phyla to emerge from the Cambrian Explosion, rapidly diversif...
In the last decade, at least thirty individual hypotheses have been invoked to explain the Cambrian ...
Classification of extinction events and their severity is generally based on taxonomic counts. The e...
The Hirnantian mass extinction is recognized as the first of the "big three" extinctions and, along ...
Rock successions in Britain and Ireland, and more especially those in North Wales, were instrumental...
In the Central Anti-Atlas (Morocco), the lower part of the Fezouata Shale has yielded locally abunda...
The lower Cambrian Lagerstätte of Sirius Passet, Nansen Land, North Greenland, is one of the oldest ...
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