The CO2 Content of the Carboniferous Atmosphere Derived from High Resolution δ13C Records of Brachiopod Calcite — Implications for the Transition from Greenhouse to Icehouse

The CO₂ Content of the Carboniferous Atmosphere Derived from High Resolution δ¹³C Records of Brachiopod Calcite — Implications for the Transition from Greenhouse to Icehouse

P. Bruckschen

Institut für Geologie, Ruhr-Universität Bochum, 44780 Bochum, Germany

Mineralogical Magazine; 1998 v. 62A; no. 1; p. 242-243; DOI: 10.1180/minmag.1998.62A.1.128
© 1998, The Mineralogical Society
Mineralogical Society (www.minersoc.org)