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
Methods and Data are provided on three sediment properties from a series of Polarstern cores (Hubberten and al., 1995) and on a Jan Mayen core (Husum, 2007). In addition, tables of some aspects of dat
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