Fig. 2From: Australian Summer Monsoon variability in the past 14,000 years revealed by IODP Expedition 356 sedimentsLithology, %K, and major elemental (Ca, K, and Ti) variation at Site U1461 for the top 1400 cm. The shipboard analysis generated the lithology, units, and bulk mineralogy. The %K contents were obtained from a shipboard NGR analysis and the MATLAB code from De Vleeschouwer et al. (2017). The major elemental analysis (Ca, K, and Ti) on Hole C sediments was conducted by XRF scanning at the IODP Texas Gulf RepositoryBack to article page