End-Permian extinction and subsequent recovery of the Ophiuroidea (Echinodermata)

Chen, Z. Q. and McNamara, K. J. (2006) End-Permian extinction and subsequent recovery of the Ophiuroidea (Echinodermata). Palaeogeography Palaeoclimatology Palaeoecology, 236 (3-4). pp. 321-344. ISSN 0031-0182 DOI https://doi.org/10.1016/j.palaeo.2005.11.014

PDF McNamara_PalPalPal_236_2006.pdf Restricted to Registered users only Download (1MB)

Abstract

A worldwide stratigraphical survey of Late Palaeozoic and Early Mesozoic ophiuroids (Echinodermata) reveals unique extinction and recovery patterns during and after the end-Permian mass extinction event. The Ophiuroidea suffered the loss of all Palaeozoic genera. However, this clade profited greatly from the event by undergoing a significant increase in species number in the postextinction oceans. Although both sampling and taphonomic biases may have affected ophiuroid diversity changeover patterns across the Permian/Triassic (P/Tr) transition to some extent, both biases cannot explain adequately the abrupt increase in species numbers and geographically wide distributions of ophiuroids in the Early Triassic oceans. The Ophiuroidea recovery follows Erwin's model of “a logistic increase in diversity beginning immediately after the end of the mass extinction” without the survival interval. Morphological innovation (i.e., emergence of advanced canal systems), diversification of life habitats and biogeographical dispersal over the Palaeotethyan and Gondwanan regions enabled the Ophiuroidea to occupy efficiently vacant ecospace created by the end-Permian extinction, enabling the clade to recover and radiate in the Early Triassic oceans. Previously reported ophiuroids from the Upper Permian to Lower Triassic of China are also taxonomically revised. These, Ophiaulaxoides bijieensis (Feng), Huangzhishania gulinensis (Feng), “Ophiolepis”? shanxiensis Yang and “Ophioderma”? schistovertebrata Yang, were described from the Lower Triassic; while Aganaster? qingchangensis (Feng) and Syntomospina? kaiyangensis Feng came from the Upper Permian.

Item Type:	Article
Uncontrolled Keywords:	NIL AREP 2006 P
Subjects:	04 - Palaeobiology
Divisions:	04 - Palaeobiology
Journal or Publication Title:	Palaeogeography Palaeoclimatology Palaeoecology
Volume:	236
Page Range:	pp. 321-344
Identification Number:	https://doi.org/10.1016/j.palaeo.2005.11.014
Depositing User:	Sarah Humbert
Date Deposited:	16 Feb 2009 13:01
Last Modified:	23 Jul 2013 10:06
URI:	http://eprints.esc.cam.ac.uk/id/eprint/202

Actions (login required)

View Item