The Great Ordovician Biodiversification Event (GOBE) is Not a Single Event

نویسندگان

چکیده

The Ordovician biodiversification is considered one of the most significant radiations in marine ecosystems entire Phanerozoic. Originally recognized as ‘Ordovician Radiation’, a label retained during 1980s and 1990s, term ‘Great Biodiversification Event’ (GOBE) was coined late 1990s subsequently adopted by scientific community. biodiversification, has always been long-term adaptive radiation, resulting sum different individual diversifications all groups organisms that occurred diachronously Ordovician. More recently, based on palaeontological datasets, comprising data from palaeogeographical areas, radiation interpreted to occur at times places. This probably related palaeogeography Ordovician, when major palaeocontinents were variously located low latitudes develop biodiversity ‘hotspots’ time intervals. In particular, some authors, using potentially biased dataset Paleobiology Database (PBDB), have GOBE be an early Middle global bio-event. Accordingly, thus apparently corresponds relatively short interval, with dramatic diversity fluctuations profound change environments scale, visible pulse fossil around world. A critical analysis published curves our own confirm traditional view; complex, process multiple biodiversifications organisms. Rapid increases can identified for groups, regional or palaeocontinental levels, particular within limited datasets. However, short, event triggered pulses level interval oversimplification.

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ژورنال

عنوان ژورنال: Paleontological Research

سال: 2021

ISSN: ['1880-0068', '1342-8144']

DOI: https://doi.org/10.2517/2021pr001