Reconstruction of past changes in salinity and climate using a diatom-based transfer function


THE prospect of global warming has focused attention on the role of palaeoecology in testing the accuracy and sensitivity of climate-model predictions, in identifying past analogues for future climate change, and in placing model-predicted climate responses in the context of natural climate variability1,2. Proxy data for climate reconstruction can be… (More)
DOI: 10.1038/352706a0


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