“…The sediment size of samples may be favorable to the accumulation of phytoliths (finer particles, such as silt and clay), or may, when coarse (sandy), allow their percolation to deeper layers (Coe et al, 2017). However, the main sediment size in this core is fine-grained, from top to bottom (0-60 cm) (Ledru et al, 2020). In the readable layers, from 1962 until 1970, there was an increasing frequency of globular granulate and globular echinate, and a decreasing frequency of GSSC.…”