Well sorted, fine lithic sandstone within the Drygalski Formation at Cape Lockyer on the southern tip of Heard Island, preserves a diverse terrestrial palynoflora as well as marine diatoms and a few foraminifera. A combination of these elements suggests a Late Miocene age (10-5 Ma). The palaeovegetation was markedly different from that presently on the island, and appears to comprise at least two ecologically distinct communities: open heath or herbfield dominated by grasses and Asteraceae, and a more mesophytic community dominated by ferns but also including lycopods and angiosperms such as Gunnera. This may have represented a coastal flora similar to the 'fern-bush' community that exists now on Southern Ocean islands north of the Antarcti...
Sparse terrestrial palynomorphs (spores and pollen) were recovered from glacigene Lower Miocene and ...
The palaeontological yield of the 1138.54 metre-long AND-2A sedimentary rock core provides unique d...
New Zealand has a good Neogene plant fossil record. During the Miocene it was without high topograph...
The New Zealand landmass occupies an area on the edge of the Southern Ocean at 35–47°S. Though situa...
Known Early-Middle Miocene terrestrial strata of southern New Zealand are represented by alluvial pl...
Published online: 31 Mar 2014A fossil flora from the basal Chatton Formation at Cosy Dell farm near ...
Aim: Geological and fossil records are critical for historical biogeography studies. A plant fossil ...
Evidence for major vegetation and climatic changes during the Tertiary in the south-west-ern Cape ha...
Assemblages of fossil leaves ranging in age from Upper Oligocene to Upper Miocene or Lower Pliocene ...
Locations of climatic zones at four time intervals during Miocene are reconstructed from ranges of p...
A late Miocene (6-6.5 Ma; Kapitean and latest Tongaporutuan stages) fossil leaf locality is situated...
The Late Miocene flora and paleogeography of north-western Wairarapa were determined by examining an...
Well-preserved palynofloras extracted from flavial sediments of the Cainozoic Elliott Formation in t...
The modern New Zealand flora has a relatively low number of families and genera in relation to land ...
An exceptional triple palynological signal (unusually high abundance of marine, freshwater, and ter...
Sparse terrestrial palynomorphs (spores and pollen) were recovered from glacigene Lower Miocene and ...
The palaeontological yield of the 1138.54 metre-long AND-2A sedimentary rock core provides unique d...
New Zealand has a good Neogene plant fossil record. During the Miocene it was without high topograph...
The New Zealand landmass occupies an area on the edge of the Southern Ocean at 35–47°S. Though situa...
Known Early-Middle Miocene terrestrial strata of southern New Zealand are represented by alluvial pl...
Published online: 31 Mar 2014A fossil flora from the basal Chatton Formation at Cosy Dell farm near ...
Aim: Geological and fossil records are critical for historical biogeography studies. A plant fossil ...
Evidence for major vegetation and climatic changes during the Tertiary in the south-west-ern Cape ha...
Assemblages of fossil leaves ranging in age from Upper Oligocene to Upper Miocene or Lower Pliocene ...
Locations of climatic zones at four time intervals during Miocene are reconstructed from ranges of p...
A late Miocene (6-6.5 Ma; Kapitean and latest Tongaporutuan stages) fossil leaf locality is situated...
The Late Miocene flora and paleogeography of north-western Wairarapa were determined by examining an...
Well-preserved palynofloras extracted from flavial sediments of the Cainozoic Elliott Formation in t...
The modern New Zealand flora has a relatively low number of families and genera in relation to land ...
An exceptional triple palynological signal (unusually high abundance of marine, freshwater, and ter...
Sparse terrestrial palynomorphs (spores and pollen) were recovered from glacigene Lower Miocene and ...
The palaeontological yield of the 1138.54 metre-long AND-2A sedimentary rock core provides unique d...
New Zealand has a good Neogene plant fossil record. During the Miocene it was without high topograph...