▲    Animal fossils from the lower Ediacaran Lantian Formation of South China (Wan et al., 2016,Palaeontology).

▲    New Cretaceous fossils shed light on the early evolution of ants (Perrichot et al., 2016,Current Biology).

▲    A unique angiosperm from the Middle Jurassic of Inner Mongolia, China (Liu et al., 2016, Historical Biology).

▲    Middle Visean (Late Devonian) coral biostrome found in South China (Yao et al., 2016,Palaeo-3).

▲    New fossil insect order elucidates major transition from chewing to piercing mouthparts (Huang et al., 2015,Scientific Reports).

▲    New findings of fossil wood from the Early Cretaceous Jehol Biota (Ding et al., 2016, Cretaceous Research).

▲    Paleoatmospheric CO₂levels reconstructed based on fossil Ginkgoites from Triassic and Jurassic in China (Wu et al., 2016, Paläontologische Zeitschrift).

▲    Discovery of the Jehol Biota from Bayingebi Basin, northwest China (Li et al., 2016, Palaeoworld).

▲    New brachiopod from Norway and South China in the recovery interval after the end Ordovician mass extinction (Huang et al., 2016., Alcheringa).

▲    A whole plant herbaceous angiosperm from the Middle Jurassic of China (Han et al., 2016, Acta Geologica Sinica).

▲    Morphological analysis of Ozarkodin (Emsian conodonts) from South China (Lu, 2016, Alcheringa).

▲    Recovery brachiopod associations from the lower Silurian of South China (Huang et al., 2016, Canadian Journal of Earth Sciences).

▲    The earliest known cormose rhizomorph of putative lycopsid affinity from China (Xu & Wang, 2016, Review of Palaeobotany and Palynology).

▲    Furongian (upper Cambrian) Guole Konservat-Lagerstätte in South China (Zhu et al., 2016, Acta Geologica Sinica).

▲    Newly recognized Hirnantian (latest Ordovician) postglacial carbonate rocks and the shelly fossils of South China (Wang et al., 2016, Canadian Journal of Earth Sciences).

▲    First record of Norian (Triassic) fossil wood from the Junggar Basin, northwest China (Wan et al., 2016. Palaeo-3).

▲    New results obtained from the studies on the Mesozoic Dipteridaceae ferns (Wang et al., 2015. Journal of Plant Research).

▲    Oceanic redox evolution across the end-Permian mass extinction at Shangsi, South China (Xiang,2016, Palaeo-3 ).