Open Spaces for Arts Education ‐ The ALTO Ecosystem

Casey, J., Greller, W., Davies, H., Follows, C., Turner, N., & Webb-­Ingall, E. (2011, 27-30 September). Open Spaces for Arts Education - The ALTO Ecosystem Model. Paper presentation of "Future Learning Spaces", at the 7th annual Designs on E-learning 2011 (DeoL) conference, Helsinki, Finland.Presenting the open educational practice for Arts education model

Polyphosphates as a source of enhanced P fluxes in marine sediments overlain by anoxic waters: Evidence from (31)P NMR

Sedimentary phosphorus (P) composition was investigated in Effingham Inlet, a fjord located on the west coast of Vancouver Island in Barkley Sound. Solid-state (31)P nuclear magnetic resonance (NMR) spectroscopy was applied to demineralized sediment samples from sites overlain by oxic and anoxic bottom waters. The two sites were similar in terms of key diagenetic parameters, including the mass accumulation rate, integrated sulfate reduction rate, and bulk sediment organic carbon content. In contrast, P benthic fluxes were much higher at the anoxic site. (31)P NMR results show that P esters and phosphonates are the major organic P species present at the surface and at depth in sediments at both sites. Polyphosphates were only found in the surface sediment of the site overlain by oxic waters. The varying stability of polyphosphates in microorganisms under different redox conditions may, in part, explain their distribution as well as differences in P flux between the two sites

Biogeochemistry: Early phosphorus redigested

Atmospheric oxygen was maintained at low levels throughout huge swathes of Earth's early history. Estimates of phosphorus availability through time suggest that scavenging from anoxic, iron-rich oceans stabilized this low-oxygen world

Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing

The evolution of burrowing animals forms a defining event in the history of the Earth. It has been hypothesised that the expansion of seafloor burrowing during the Palaeozoic altered the biogeochemistry of the oceans and atmosphere. However, whilst potential impacts of bioturbation on the individual phosphorus, oxygen and sulphur cycles have been considered, combined effects have not been investigated, leading to major uncertainty over the timing and magnitude of the Earth system response to the evolution of bioturbation. Here we integrate the evolution of bioturbation into the COPSE model of global biogeochemical cycling, and compare quantitative model predictions to multiple geochemical proxies. Our results suggest that the advent of shallow burrowing in the early Cambrian contributed to a global low-oxygen state, which prevailed for ~100 million years. This impact of bioturbation on global biogeochemistry likely affected animal evolution through expanded ocean anoxia, high atmospheric CO2 levels and global warming

London Community Video Archive

Based at Goldsmiths, University of London, the London Community Video Archive (LCVA) preserves, archives and shares community videos made in the 1970s/80s in London and the South East. Portable video recording — now a technology routinely embodied in smartphones — became available for the very first time back in the early 1970s, making it possible for individuals and communities to make their own television. The medium was taken up by people ignored or under-represented in the mainstream media – tenants on housing estates, community action groups, women, black and minority ethnic groups, youth, gay and lesbian people, and the disabled. With an overriding commitment to social empowerment and to combating exclusion, 'Community Video' dealt with issues which still have a contemporary resonance — housing, play-space, discrimination, youth arts