Timing of recovery from the end-Permian extinction: Geochronologic and biostratigraphic constraints from south China: COMMENT AND REPLY: COMMENT | Zendy

Hugo Bucher | Zendy; Peter A. Hochuli | Zendy; Maria Ovtcharova | Zendy; Thomas Galfetti | Zendy; Arnaud Brayard | Zendy; Nicolas Goudemand | Zendy; J. Guex | Zendy

Open Access

Timing of recovery from the end-Permian extinction: Geochronologic and biostratigraphic constraints from south China: COMMENT AND REPLY: COMMENT

Author(s) -

Hugo Bucher,

Peter A. Hochuli,

Maria Ovtcharova,

Thomas Galfetti,

Arnaud Brayard,

Nicolas Goudemand,

J. Guex

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/g23609c.1

Subject(s) - geology , permian–triassic extinction event , paleontology , extinction event , bracketing (phenomenology) , permian , china , boundary (topology) , extinction (optical mineralogy) , archaeology , geography , demography , epistemology , biological dispersal , population , structural basin , sociology , philosophy , mathematical analysis , mathematics

[Lehrmann et al. (2006)][1] recently interpolated a new age of 247.2 Ma for the Early-Middle Triassic boundary in Guandao (Guizhou Province, south China) where four new U-Pb ages were measured from ash layers bracketing this boundary as defined by conodonts. Along with previous data of [Lehrmann et

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