Carbon isotopes in fossil emu (Dromaius novaehollandiae) eggshell from Lake Eyre, South Australia, demonstrate that the relative abundance of C4 grasses varied substantially during the past 65,000 years. Currently, C4 grasses are more abundant in region
First published: 09 August 2021Records of Australian palaeoclimate beyond the last glacial cycle are...
As part of the Australasian INTIMATE palaeoclimate initiative, we have collated records of terrestri...
A blocked tributary has provided a rare site of long-term sediment accumulation in montane southeast...
Stable carbon isotopes in emu eggshell (EES) reflect emu diets and consequently the vegetation avail...
Throughout the Quaternary, the flora and fauna of Australia evolved and adapted to the high-amplitud...
Since the late Miocene, plants using the C₄ photosynthetic pathway have increased to become major co...
Riverine Plain palaeochannels record periods of fluvial activity for Late Pleistocene southeastern A...
Riverine Plain palaeochannels record periods of fluvial activity for Late Pleistocene southeastern A...
The moisture balance across northern and central Australia is dominated by changes in the strength o...
The cause(s) of the late Pleistocene megafauna extinction on the Australian continent remains largel...
C4 grasses account for >25% of global primary productivity and dominate tropical, subtropical, and w...
Aim Numerous studies have examined the climatic factors that influence the abundance of C4 species w...
A substantial extinction of megafauna occurred in Australia between 50 and 45 kyr ago, a period that...
Palynomorphs from the ODP Site 820 marine core have provided a detailed record of terrestrial enviro...
This item is only available electronically.Reconstructing canopy closure is difficult and has up unt...
First published: 09 August 2021Records of Australian palaeoclimate beyond the last glacial cycle are...
As part of the Australasian INTIMATE palaeoclimate initiative, we have collated records of terrestri...
A blocked tributary has provided a rare site of long-term sediment accumulation in montane southeast...
Stable carbon isotopes in emu eggshell (EES) reflect emu diets and consequently the vegetation avail...
Throughout the Quaternary, the flora and fauna of Australia evolved and adapted to the high-amplitud...
Since the late Miocene, plants using the C₄ photosynthetic pathway have increased to become major co...
Riverine Plain palaeochannels record periods of fluvial activity for Late Pleistocene southeastern A...
Riverine Plain palaeochannels record periods of fluvial activity for Late Pleistocene southeastern A...
The moisture balance across northern and central Australia is dominated by changes in the strength o...
The cause(s) of the late Pleistocene megafauna extinction on the Australian continent remains largel...
C4 grasses account for >25% of global primary productivity and dominate tropical, subtropical, and w...
Aim Numerous studies have examined the climatic factors that influence the abundance of C4 species w...
A substantial extinction of megafauna occurred in Australia between 50 and 45 kyr ago, a period that...
Palynomorphs from the ODP Site 820 marine core have provided a detailed record of terrestrial enviro...
This item is only available electronically.Reconstructing canopy closure is difficult and has up unt...
First published: 09 August 2021Records of Australian palaeoclimate beyond the last glacial cycle are...
As part of the Australasian INTIMATE palaeoclimate initiative, we have collated records of terrestri...
A blocked tributary has provided a rare site of long-term sediment accumulation in montane southeast...