The qual ity of palaeoenvironmental re con struc tions based on macrofossil car bon ate crit i
cally de pends on pres er va tion of the shell ma te rial be cause post-depositional pro …

Natural variations in the isotopic composition of some 50 chemical elements are now being
used in geochemistry for studying transport processes, estimating temperature …

The 2nd Edition of Carbonate Reservoirs aims to educate graduate students and industry
professionals on the complexities of porosity evolution in carbonate reservoirs. In the …

Calcite growth experiments have been performed in the presence of aqueous Mg at 25° C
and 1bar pCO2 to quantify magnesium partition coefficient DMg=(Mg/Ca) solid (Mg/Ca) fluid …

Ca isotope fractionation during inorganic calcite formation was experimentally studied by
spontaneous precipitation at various precipitation rates (1.8< logR< 4.4 μmol/m2/h) and …

Stable oxygen isotopic fractionation during inorganic calcite precipitation was
experimentally studied by spontaneous precipitation at various pH (8.3< pH< 10.5) …

Paleotemperature reconstructions rely on knowledge of the equilibrium separation of
oxygen isotopes between aqueous solution and calcium carbonate. Although oxygen …

Ca isotope geochemistry has great potential for improving our understanding of magmatic
systems and for tracing the deep Earth carbon cycle. There are still many open questions …

Abstract “Clumped-isotope” thermometry is an emerging tool to probe the temperature
history of surface and subsurface environments based on measurements of the proportion of …

The chemical and isotopic composition of speleothem calcite and particularly that of
stalagmites and flowstones is increasingly exploited as an archive of past environmental …