Great Ordovician Biodiversification Event information
Evolutionary radiation of animal life throughout the Ordovician period
The Great Ordovician Biodiversification Event (GOBE), was an evolutionary radiation of animal life throughout[1] the Ordovician period, 40 million years after the Cambrian explosion,[2] whereby the distinctive Cambrian fauna fizzled out to be replaced with a Paleozoic fauna rich in suspension feeder and pelagic animals.[3]
It followed a series of Cambrian–Ordovician extinction events, and the resulting fauna went on to dominate the Palaeozoic relatively unchanged.[4]
Marine diversity increased to levels typical of the Palaeozoic,[5] and morphological disparity was similar to today's.[6]
The diversity increase was neither global nor instantaneous; it happened at different times in different places.[4] Consequently, there is unlikely to be a simple or straightforward explanation for the event; the interplay of many geological and ecological factors likely produced the diversification.[1]
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^Cite error: The named reference Servais2010 was invoked but never defined (see the help page).
^ abCite error: The named reference Droser2003 was invoked but never defined (see the help page).
^Marshall, C. R. (2006). "Explaining the Cambrian "explosion" of Animals". Annual Review of Earth and Planetary Sciences. 34: 355–384. Bibcode:2006AREPS..34..355M. doi:10.1146/annurev.earth.33.031504.103001.
^Bambach, R. K.; Bush, A. M.; Erwin, D. H. (2007). "Autecology and the Filling of Ecospace: Key Metazoan Radiations". Palaeontology. 50 (1): 1–22. Bibcode:2007Palgy..50....1B. doi:10.1111/j.1475-4983.2006.00611.x.
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jawless fish) and corals. This process is known as the GreatOrdovicianBiodiversificationEvent or GOBE. Trilobites began to be replaced by articulate...
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Yong-Yi, Zhen (2004). "31. Receptaculitids and Algae". The GreatOrdovicianBiodiversificationEvent. pp. 336–347. doi:10.7312/webb12678-032. ISBN 9780231126786...
fossils appearing in the GreatOrdovicianBiodiversificationEvent, and largely became extinct in the Capitanian mass extinction event and the Permian-Triassic...
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explosion, the greatOrdovicianbiodiversificationevent, and the recoveries from the end-Permian and end-Triassic mass extinction events. Empirical data...
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clathrodictyid stromatoporoids during the GreatOrdovicianBiodiversificationEvent: insights from the Upper Ordovician Xiazhen Formation of South China". Journal...
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