δ18O of Fissurella maxima as a proxy for reconstructing Early Holocene sea surface temperatures in the coastal Atacama desert (25°S).

δ18O of Fissurella maxima as a proxy for reconstructing Early Holocene sea surface temperatures in the coastal Atacama desert (25°S).  Palaeogeography, Palaeoclimatology, Palaeoecology  499:22-34   doi:10.1016/j.palaeo.2018.03.031