Figure F1. Location of Site 1146 in the South China Sea and major drainage systems. The thick line offshore corresponds to the present 100-m isobath, approximating the lowest sea level during glacial maxima. The location of the major rivers on the emerged glacial shelf, corresponding to paleorivers, are adapted from Wang et al. (1999) and Hiscott (2001).

Figure F1. Location of Site 1146 in the South China Sea and major drainage systems. The thick line offshore corresponds to the present 100-m isobath, approximating the lowest sea level during glacial maxima. The location of the major rivers on the emerged glacial shelf, corresponding to paleorivers, are adapted from Wang et al. (1999) and Hiscott (2001).