Effect of early marine diagenesis on coral reconstructions of surface-ocean 13C/12C and carbonate saturation state
Recent research suggests that future decreases in the carbonate saturation state of surface seawater associated with the projected build-up of atmospheric CO2 could cause a global decline in coral reef-building capacity. Whether significant reductions in
|Collections||ANU Research Publications|
|Source:||Global Biogeochemical Cycles|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.