“…Early attempts to use computers for log correlation have relied on the cross-correlation algorithm to find time-equivalent sample pairs (Rudman and Lankston, 1973;Mann and Dowell, 1978). Later it became obvious that the dynamic time warping (DTW) algorithm handles better logs that differ significantly from each other, a common problem unless the stratigraphy is extremely simple (Lineman et al, 1987;Fang et al, 1992;Zoraster et al, 2004;Hladil et al, 2010;Lallier et al, 2012;Wheeler and Hale, 2014;Wheeler, 2015;Lallier et al, 2016;Grant et al, 2018;Wu et al, 2018). Dynamic time warping has also been used to correlate paleo-proxy records of environmental change (e.g., Lisiecki and Lisiecki, 2002;Lisiecki and Raymo, 2005;Hay et al, 2019;Ajayi et al, 2020).…”