Silicified fragments of false-trunks of the fern, Tempskya judithae sp. nov., are described from lower Cretaceous (latest Albian) sediments near Winton, central-western Queensland. The species is characterised by a three-layered sclerenchymatous cortex and a two-layered pith of sclerenchyma cells. In possessing these characters, T judithae is more similar to T readii than to other species of Tempskya. However, the Australian species differs from T readii in the abaxial shape of the petiole xylem trace (concave in T judithae, convex in T readii) and in symmetry attributes of the leaf-bases within the false-trunk (random in T judithae and radially symmetrical in T readii). T judithae is the first record of Tempskya from Australia and the seco...
ABSTRACT: Tropical rainforests in the northeast of Australia have been interpreted as being either c...
Diverse Cenozoic (possibly latest Oligocene to mid–late Miocene) macrofossils from the Lightning Rid...
"The Australian vegetation is the end result of a remarkable history of climate change, latitudinal ...
New specimens of the tree fern Tempskya are described from the Mulichinco Formation (Valanginian), N...
Nonmarine Cretaceous sediments representing fluvial/lacustrine deposits occur in 22 of Australia's 2...
Six new records of ferns from the late Albian flora of Alexander Island, Antarctic Peninsula, provid...
The fossil megaflora of the middle Clarence valley, South Island, New Zealand, contains leaf forms a...
The montane vegetation of northeastern Australasia represents a modified sample of the late Cretaceo...
Rozefelds, A.C., Dettmann, M.E., Clifford, H.T. & Lewis, D., August 2015. Macrofossil evidence of ea...
A flora of dispersed spores, pollen grains, and algal microfossils is recorded from subsurface equiv...
The Early Cretaceous high-paleolatitude palynofloras from the Otway and Gippsland basins of southeas...
Seed ferns, dominant elements of the vegetation in many parts of the world from the Triassic to Cret...
Premise of the study: The origin of biomes is of great interest globally. Molecular phylogenetic and...
Sclerophyllous Adenanthos and Stirlingia (Proteoideae) are now restricted to the S Australian Medite...
Seed ferns, dominant elements of the vegetation in many parts of the world from the Triassic to Cret...
ABSTRACT: Tropical rainforests in the northeast of Australia have been interpreted as being either c...
Diverse Cenozoic (possibly latest Oligocene to mid–late Miocene) macrofossils from the Lightning Rid...
"The Australian vegetation is the end result of a remarkable history of climate change, latitudinal ...
New specimens of the tree fern Tempskya are described from the Mulichinco Formation (Valanginian), N...
Nonmarine Cretaceous sediments representing fluvial/lacustrine deposits occur in 22 of Australia's 2...
Six new records of ferns from the late Albian flora of Alexander Island, Antarctic Peninsula, provid...
The fossil megaflora of the middle Clarence valley, South Island, New Zealand, contains leaf forms a...
The montane vegetation of northeastern Australasia represents a modified sample of the late Cretaceo...
Rozefelds, A.C., Dettmann, M.E., Clifford, H.T. & Lewis, D., August 2015. Macrofossil evidence of ea...
A flora of dispersed spores, pollen grains, and algal microfossils is recorded from subsurface equiv...
The Early Cretaceous high-paleolatitude palynofloras from the Otway and Gippsland basins of southeas...
Seed ferns, dominant elements of the vegetation in many parts of the world from the Triassic to Cret...
Premise of the study: The origin of biomes is of great interest globally. Molecular phylogenetic and...
Sclerophyllous Adenanthos and Stirlingia (Proteoideae) are now restricted to the S Australian Medite...
Seed ferns, dominant elements of the vegetation in many parts of the world from the Triassic to Cret...
ABSTRACT: Tropical rainforests in the northeast of Australia have been interpreted as being either c...
Diverse Cenozoic (possibly latest Oligocene to mid–late Miocene) macrofossils from the Lightning Rid...
"The Australian vegetation is the end result of a remarkable history of climate change, latitudinal ...