Here, we describe and illustrate by transmitted light and scanning electron microscopy the first Australian Jurassic megaspore assemblages. The megaspores and other mesofossils were isolated from terrestrial deposits of the Marburg Subgroup (late Pliensbachian) at Inverleigh Quarry, Clarence-Moreton Basin, eastern Australia. Nine megaspore taxa are identified including one new species: Paxillitriletes rainei. Miospore assemblages recovered from the same samples at Inverleigh reveal a slightly higher diversity of lycophyte microspores. The collective megaspore suite from Inverleigh shares several genera with mid-Mesozoic assemblages from widely distributed parts of the world, but most of the Inverleigh species have subtle morphological differences from congeneric forms elsewhere. The megaspores accumulated in fluvial floodplain facies and are associated with mostly dissociated isoetalean leaf debris. Other mesofossils in the sampled interval include annelid egg cases, dispersed seeds and charcoal. Invertebrate burrows and possible vertebrate tracks also occur in this succession. Lycophyte macrofossils are otherwise known from only two other Australian Jurassic deposits. The richness of the megaspore and microspore suites attest to a significant diversity of lycophytes in the Australian Jurassic floras not hitherto appreciated from described macrofloras.Keywords: lycophyte megaspores, Isoetales, mesofossils, microspores, Pliensbachian, Clarence-Moreton Basin, GondwanaThe Hettangian-basal Toarcian interval is bracketed by two globally recognised mass extinction events. In the Gondwanan terrestrial realm, the RhaetianHettangian transition is marked by the collapse of the Dicroidium/Falcisporites flora that had dominated most of the Triassic (Anderson et al., 1999). In its place arose a flora rich in Bennettitales, Caytoniales and cheirolepidiacean conifers (Gould, 1975;Hill et al., 1999). A further transition in the Toarcian saw a decline in cheirolepids and increases in araucariacean and podocarpacean conifers and pentoxylalean gymnosperms in Australia (Turner et al., 2009). The Australian Hettangian-Toarcian floras remain poorly understood, being represented by only a few macrofloral assemblages from central eastern Australia that have yet to be fully described (Jones & de Jersey, 1947;Gould, 1968Gould, , 1974Gould, , 1975Pattemore, 2000;Pattemore & Rigby, 2005;Jansson et al., 2008b). Palynofloras provide a broader picture of Australia's Early Jurassic floristic succession (Evans, 1966;de Jersey, 1975;Filatoff, 1975;Burger, 1976Burger, , 1994Helby et al., 1987;Turner et al., 2009), but the biological affinities of some palynomorphs remain poorly resolved (Balme, 1995) and spore-pollen assemblages may be subject to significant taphonomic sorting (Holmes, 1994). Mesofossils (0.2-5.0 mm remains including megaspores, sporangia, seeds and charcoalfied plant fragments) represent an additional avenue for evaluating fossil plant diversity. However, mesofossil suites have been largely neglected in past palaeobotani...