“…The East Asian mainland differs from Europe and North America by having remained largely unglaciated during the Pleistocene (Feng, Mao, Sandel, Swenson, & Svenning, ; Hewitt, ; Li, Shu, Zhou, Zhao, & Zhang, ). Relevant studies in this region are rare and have primarily focused on southwestern China and adjacent areas with their complex topography and high mountains, such as the Himalayas (e.g., Gao, Zhang, Gao, & Zhu, ; He & Jiang, ).…”