The climate evolution of the South Shetland Islands during the last c. 2000 years is inferred from the multiproxy analyses of a long (928 cm) sediment core retrieved from Maxwell Bay off King George I
This dataset is about: Concentrations of biogenic components and mass accumulation rates from sediment core NH22P. Please consult parent dataset @ https://doi.org/10.1594/PANGAEA.855307 for more infor
This dataset is about: Grain density in sediment core SO106-286KL. Please consult parent dataset @ https://doi.org/10.1594/PANGAEA.761569 for more information.