Following the recent rapid increase in the reports of tetrapod tracksites in the Cretaceous, especially from the Lower Cretaceous, of China and other parts of East Asia, notably South Korea, a review of the ichnofaunal database from these regions is presented as the basis for comparisons with other Lower Cretaceous ichnofaunas that are abundant and reasonably well documented. These areas include parts of North and South America, especially the western USA, and parts of Europe, including the United Kingdom, Northern Germany, Spain, Italy and Croatia. The Chinese database presently includes about 70 Cretaceous sites, the majority of which are Early Cretaceous in age. Although abundant data are available from many regions, much of it has yet to be synthesized in detail or in standard formats. Moreover, ichnotaxonomy may be variable (provincial) between different regions. Thus, while comprehensive lists of sites are available for some regions (China and South America), in other regions such as South Korea and the western USA data have been compiled primarily on a formation by formation basis. The record for Europe is moderately good, but scattered in the primary literature and in need of further synthesis. The record for Australia and Africa is sparse and also in need of synthesis. The most notable regional differences between ichnofaunas appears to be in the relative abundance of distinctive bird and pterosaur track ichnotaxa in China and Korea in comparison with their scarcity or absence in other regions. The distinctive ichnogenus Minisauripus is also known only in China and Korea as are the majority of known dromaeosaurid track occurrences. Ornithopod‐dominated and ornithopod‐rich ichnofaunas are widespread and particularly abundant in the late Early Cretaceous Barremian to Albian, of some regions. Most well documented Early Cretaceous ichnofaunas are associated with siliciclastic facies and evidently differ from those associated with carbonate facies. © 2014 The Linnean Society of London, Biological Journal of the Linnean Society, 2014, 113, 770–789.