51 research outputs found
Late Quaternary Aboriginal hunter-gatherer occupation of the Greater Swan Region, south-western Australia
Palynological evidence for the age of the Brewer Conglomerate, Amadeus Basin, central Australia
An assemblage of spores recovered from the Undandita Member of the Brewer Conglomerate, the uppermost unit of the Pertnjara Group in the Amadeus Basin of central Australia, establishes the age of that formation as Late Devonian. Comparison with spore assemblages from sedimentary basins in Western Australia indicates that the central Australian assemblage is dateable within the post-early Frasnian to pre-late Famennian interval. Fish remains and spores previously described from the Parke Siltstone at the base of the Pertnjara Group are of probable early Frasnian age, so it now appears that the entire group was deposited during the Late Devonian. The Brewer Conglomerate is of synorogenic origin, and was deposited during uplift associated with the Alice Springs Orogeny; the spore data thus indicate that this tectonic event began in the Late Devonian. Isotopic age determinations in the Arltunga Nappe Complex and the Strangways Range of the Arunta Block have yielded Early Carboniferous dates. These possibly reflect a later stage of deformation than that which was responsible for the deformation and folding of the Brewer Conglomerate
Palaeokarst, tidal erosion surfaces and stromatolites in the Silurian Eke Formation of Gotland, Sweden
Banksia species (Proteaceae) from severely phosphorus-impoverished soils exhibit extremem efficiency in the use and re-mobilization of phosphorus
Banksia species (Proteaceae) occur on some of the most phosphorus (P)-impoverished soils in the world. We hypothesized that Banksia spp. maximize P-use efficiency through high photosynthetic P-use efficiency, long leaf lifespan (P residence time), effective P re-mobilization from senescing leaves, and maximizing seed P concentration. Field and glasshouse experiments were conducted to quantify P-use efficiency in nine Banksia species. Leaf P concentrations for all species were extremely low (0.14ā0.32 mg P gā1 DM) compared with leaf P in other species reported and low relative to other plant nutrients in Banksia spp.; however, moderately high rates of photosynthesis (13.8ā21.7 Āµmol CO2 mā2 sā1), were measured. Some of the Banksia spp. had greater P proficiency (i.e. final P concentration in senesced leaves after re-mobilization; range: 27ā196 Āµg P gā1 DM) than values reported for any other species in the literature. Seeds exhibited significantly higher P concentrations (6.6ā12.2 mg P gā1 DM) than leaves, and species that sprout after fire (āre-sproutersā) had significantly greater seed mass and P content than species that are killed by fire and regenerate from seed (āseedersā). Seeds contained only small amounts of polyphosphate (between 1.3 and 6 Āµg gā1 DM), and this was not correlated with P concentration or fire response. Based on the evidence in the present study, we conclude that Banksia species are highly efficient in their use of P, explaining, in part, their success on P-impoverished soils, with little variation between species.Matthew D. Denton, Erik J. Veneklaas, Florian M. Freimoser and Hans Lamber
A novel hotspot of vertebrate endemism and an evolutionary refugium in tropical Australia
Banksia species (Proteaceae) from severely phosphorus-impoverished soils exhibit extreme efficiency in the use and re-mobilization of phosphorus
Chronology of Quaternary coastal aeolianite deposition and the drowned shorelines of southwestern Western Australia ā a reappraisal
Relationships between cyclicity and stromatolite form in the Late Proterozoic Bitter Springs Formation, Australia
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