作者: Uwe Brand , K. Azmy , E. Griesshaber , M.A. Bitner , A. Logan
DOI: 10.1016/J.CHEMGEO.2015.06.021
关键词: Dissolved organic carbon 、 Terebratulida 、 Isotopes of oxygen 、 Seawater 、 Geology 、 Equilibrium fractionation 、 Oceanography 、 Carbon cycle 、 Isotopes of carbon 、 Calcite 、 Mineralogy
摘要: … (2010) found that calcite of the innermost part of the secondary layer is in carbon and oxygen isotopic disequilibrium with seawater, which may be equivalent to the transition zone …