ALBERT

Description: Abstract 1843 Poster Board I-869 Introduction: The mammalian target of rapamycin (mToR) plays a crucial role in cell growth due to its role as nutrient dependent regulator of important cytokine signaling pathways. In multiple myeloma, mToR is involved in the phosphoinositide-3-kinase (PI3K)-AKT pathway which can be activated by the loss of the tumor suppressor phosphatase and tensin homolog (PTEN) or by stimulation with growth and survival factors such as interleukin-6 (IL-6) and insulin-like growth factor-1 (IGF-1). Inhibitors of the mToR pathway (sirolimus/rapamycin, everolimus and temsirolimus) are approved for immunosuppression and/or cancer treatment. However, the clinical activity of mToR inhibitors may be limited by the fact that, after inhibition of the rapamycin-sensitive mToR-Raptor complex, AKT is activated by the rapamycin-insensitive mToR-Rictor complex. In this regard, the inhibitory effect of mToR inhibitors was evaluated in combination with PI3K inhibitors in vitro and in vivo. Results: Rapamycin and everolimus induced a dose-dependent growth inhibition in six human malignant plasma cell lines. Growth inhibition was mediated by G1 cell cycle arrest and in a subset of cell lines by induction of apoptosis. Overexpression of Bcl-XL or Mcl-1 proteins did not prevent from apoptosis induction by mToR inhibitors, nor did sensitivity to rapamycin-induced apoptosis correlate with the p53 mutation status. In the INA-6 SCID mouse xenograft model, treatment with rapamycin resulted in a significant survival benefit compared to untreated mice. Six out of 14 rapamycin treated mice did not develop plasmacytomas during the observation period of 149 days. Remarkably, short term treatment of plasmacytoma bearing mice led to a significant shrinkage of the plasma cell tumor. Explanted tissue showed apoptotic plasma cells, a finding confirmed by immunohistological staining using an antibody specific for the human cleaved form of poly (ADP-ribose) polymerase (PARP). The combination of rapamycin and the PI3K inhibitor Ly294002 led to an increase of growth inhibition in all tested plasma cell lines. The additional growth inhibition by Ly294002 appeared to be due to AKT activation upon mToR inhibition by the rapamycin-insensitive Rictor complex, indicated by increased AKT phosphorylation at Ser473 as determined by Western blot analysis. Conclusion: Clinical trials currently evaluate mToR inhibitors for their potential to expand treatment options for myeloma patients. The data presented here suggest that a combination of mToR inhibitors with PI3K inhibitors may lead to additive therapeutic chances. Disclosures: Guenther: Novartis: Consultancy, Research Funding. Gramatzki:Novartis: Consultancy, Research Funding, Speakers Bureau.

Description: The biomisation method is used to reconstruct Latin American vegetation at 6000±500 and 18 000±1000 radiocarbon years before present (14C yr BP) from pollen data. Tests using modern pollen data from 381 samples derived from 287 locations broadly reproduce potential natural vegetation. The strong temperature gradient associated with the Andes is recorded by a transition from high altitude cool grass/shrubland and cool mixed forest to mid-altitude cool temperate rain forest, to tropical dry, seasonal and rain forest at low altitudes. Reconstructed biomes from a number of sites do not match the potential vegetation due to local factors such as human impact, methodological artefacts and mechanisms of pollen representivity of the parent vegetation. At 6000±500 14C yr BP 255 samples are analysed from 127 sites. Differences between the modern and the 6000±500 14C yr BP reconstruction are comparatively small. Patterns of change relative to the modern reconstruction are mainly to biomes characteristic of drier climate in the north of the region with a slight more mesic shift in the south. Cool temperate rain forest remains dominant in western South America. In northwestern South America a number of sites record transitions from tropical seasonal forest to tropical dry forest and tropical rain forest to tropical seasonal forest. Sites in Central America also show a change in biome assignment to more mesic vegetation, indicative of greater plant available moisture, e.g. on the Yucatán peninsula sites record warm evergreen forest, replacing tropical dry forest and warm mixed forest presently recorded. At 18 000±1000 14C yr BP 61 samples from 34 sites record vegetation that reflects a generally cool and dry environment. Cool grass/shrubland prevalent in southeast Brazil, Amazonian sites record tropical dry forest, warm temperate rain forest and tropical seasonal forest. Southernmost South America is dominated by cool grass/shrubland, a single site retains cool temperate rain forest indicating that forest was present at some locations at the LGM. Some sites in Central México and lowland Colombia remain unchanged in their biome assignments, although the affinities that these sites have to different biomes do change between 18 000±1000 14C yr BP and present. The "unresponsive" nature of these sites results from their location and the impact of local edaphic influence.

Description: The biomisation method is used to reconstruct Latin American vegetation at 6000±500 and 18 000±1000 radiocarbon years before present (14C yr BP) from pollen data. Tests using modern pollen data from 381 samples derived from 287 locations broadly reproduce potential natural vegetation. The strong temperature gradient associated with the Andes is recorded by a transition from high altitude cool grass/shrubland and cool mixed forest to mid-altitude cool temperate rain forest, to tropical dry, seasonal and rain forest at low altitudes. Reconstructed biomes from a number of sites do not match the potential vegetation due to local factors such as human impact, methodological artefacts and mechanisms of pollen representivity of the parent vegetation. At 6000±500 14C yr BP 255 samples are analysed from 127 sites. Differences between the modern and the 6000±500 14C yr BP reconstruction are comparatively small; change relative to the modern reconstruction are mainly to biomes characteristic of drier climate in the north of the region with a slight more mesic shift in the south. Cool temperate rain forest remains dominant in western South America. In northwestern South America a number of sites record transitions from tropical seasonal forest to tropical dry forest and tropical rain forest to tropical seasonal forest. Sites in Central America show a change in biome assignment, but to more mesic vegetation, indicative of greater plant available moisture, e.g. on the Yucatán peninsula sites record warm evergreen forest, replacing tropical dry forest and warm mixed forest presently recorded. At 18 000±1000 14C yr BP 61 samples from 34 sites record vegetation reflecting a generally cool and dry environment. Cool grass/shrubland is prevalent in southeast Brazil whereas Amazonian sites record tropical dry forest, warm temperate rain forest and tropical seasonal forest. Southernmost South America is dominated by cool grass/shrubland, a single site retains cool temperate rain forest indicating that forest was present at some locations at the LGM. Some sites in Central Mexico and lowland Colombia remain unchanged in the biome assignments of warm mixed forest and tropical dry forest respectively, although the affinities that these sites have to different biomes do change between 18 000±1000 14C yr BP and present. The "unresponsive" nature of these sites results from their location and the impact of local edaphic influence.