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Timing of recovery from the end-Permian extinction: Geochronologic and biostratigraphic constraints from south China: COMMENT AND REPLY: REPLY
Author(s) -
Daniel J. Lehrmann,
Jahandar Ramezani,
Samuel A. Bowring,
M. W. Martin,
Paul Montgomery,
Paul Enos,
Jonathan L. Payne,
Michael J. Orchard,
Hongmei Wang,
Jiayong Wei
Publication year - 2007
Publication title -
geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.609
H-Index - 215
eISSN - 1943-2682
pISSN - 0091-7613
DOI - 10.1130/g23941y.1
Subject(s) - geology , permian , paleontology , extinction event , permian–triassic extinction event , china , extinction (optical mineralogy) , archaeology , history , demography , sociology , biological dispersal , population , structural basin
[Bucher et al.'s Comment (2007)][1] questioned the validity of our 247.2 Ma age estimate for the Early-Middle Triassic (Olenekian-Anisian, O-A) boundary based on a comparison of recent data from Lower Guandao section presented by us ([Lehrmann et al., 2006][2]) with preliminary data reported from

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