“…Fossil remains of the genus are frequently found from the Early Cretaceous to the Early Pleistocene in the middle to high latitudes of North America and Eurasia (LePage, 2007;Vikulin et al, 2007Vikulin et al, , 2008Vikulin et al, , 2010Vikulin et al, , 2011. Fossil vegetative and fertile twigs, seed cones, pollen cones, and wood remains of Glyptostrobus are often found in association with those of Metasequoia, Sequoia, and Taxodium (Florin, 1922;Becker, 1969;Matsuo, 1970;Schweitzer, 1974;WGCPC, 1978;Guo & Li, 1979;SIGMR, 1980;Li & Yang, 1984;Guo et al, 1984;Tao & Xiong, 1986;He & Tao, 1994Guo, 2000;Vikulin et al, 2007Vikulin et al, , 2008Vikulin et al, , 2010Vikulin et al, , 2011Wang et al, 2010), complicating their taxonomic identification, given that leaf shape and phyllotaxis of all these four genera are similar (Ma & Gu, 2000;Ma et al, 2005bMa et al, , 2009Ma, 2009). It is difficult to distinguish unequivocally fossil shoots of all four genera based purely on their vegetative morphology.…”