Integrated stratigraphy and clay mineralogy of the Owadów-Brzezinki section (Lower-Upper Tithonian transition, Central Poland): implications for correlations between the Boreal and the Tethyan domains and palaeoclimate

Supplementary Fig. 2. Stepwise acquisition of the isothermal remanent magnetization (values of S-ratio indicated) and thermal demagnetization of the three axes IRM acquired in the fields 1.4 T, 0.4 T and 0.1 T. Note presence of magnetite in samples OB3, and OB9 and magnetite + hematite in sample OB24.