2015
DOI: 10.1016/j.palwor.2015.03.003
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The Great Ordovician Biodiversification Event: Reviewing two decades of research on diversity's big bang illustrated by mainly brachiopod data

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Cited by 75 publications
(53 citation statements)
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“…It has been suggested on numerous occasions that the Ordovician Radiation was rooted in the Cambrian and is an extension of the Cambrian Explosion (Harper , ; Harper et al . ). It appears that not only were the majority of body plans established before diversifications at lower taxonomic levels took place (Harper , ; Harper et al .…”
Section: Cambrian‐ordovician Comparisons and The Ecospace Flat Ironmentioning
confidence: 97%
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“…It has been suggested on numerous occasions that the Ordovician Radiation was rooted in the Cambrian and is an extension of the Cambrian Explosion (Harper , ; Harper et al . ). It appears that not only were the majority of body plans established before diversifications at lower taxonomic levels took place (Harper , ; Harper et al .…”
Section: Cambrian‐ordovician Comparisons and The Ecospace Flat Ironmentioning
confidence: 97%
“…It appears that not only were the majority of body plans established before diversifications at lower taxonomic levels took place (Harper , ; Harper et al . ), but also life strategies, at least in the Brachiopoda (Figs , ).…”
Section: Cambrian‐ordovician Comparisons and The Ecospace Flat Ironmentioning
confidence: 99%
“…The Great Ordovician Biodiversification Event (GOBE) was a global increase in the ecological complexity and diversity of skeletal fossils at the generic, familial and ordinal levels during the Ordovician Period (Sepkoski 1981(Sepkoski , 1995Harper 2006;Servais et al 2010;Harper et al 2015). Groups typical of the later Palaeozoic (e.g.…”
mentioning
confidence: 99%
“…rhynchonelliform brachiopods, bryozoans, crinoids, corals) flourished, whereas typical Cambrian groups seemingly declined (e.g. Sepkoski & Sheehan 1983;Harper et al 2015). Although many groups began to diversify during the Floian (Servais et al 2010), the spatial and temporal patterns of the GOBE differed markedly for different organisms; for example, phytoplankton diversification appears to have begun during the late Cambrian (Servais et al 2016), but corals did not diversify until the Late Ordovician (Webby et al 2004a).…”
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confidence: 99%
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