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Rho family members play a critical role in malignant transformation. Anchorage-independent growth and the ability to avoid apoptosis caused by loss of anchorage (anoikis) are important features of transformed cells. Here we show that constitutive activation of Rac1 inhibits anoikis in Madin-Darby canine kidney (MDCK) epithelial cells. Constitutively active Rac1-V12 decreases DNA fragmentation and caspase activity by 50% in MDCK cells kept in suspension. In addition, expression of Rac1-V12 in MDCK cells in suspension conditions causes an increase in the number of surviving cells. We also investigated the signaling pathways that are activated by Rac1 to stimulate cell survival. We show that expression of Rac1-V12 in MDCK cells in suspension stimulates a number of signaling cascades that have been implicated in the control of cell survival, including the p42/44 ERK, p38, protein kinase B, and nuclear factor kappaB pathways. Using specific chemical or protein inhibitors of these respective pathways, we show that Rac1-mediated cell survival strongly depends on phosphatidylinositol 3-kinase activity and that activation of ERK, p38, and NF-kappaB are largely dispensable for Rac1 survival signaling. In conclusion, these studies demonstrate that Rac1 can suppress apoptosis in epithelial cells in anchorage-independent conditions and suggest a potential role for Rac1-mediated survival signaling in cell transformation.

Chemical and mineralogical data for samples collected from a surge sequence from La Fossa cone (Vulcano Island, Italy) show a wide variety of alteration states between adjoining beds, the macroscopic features of which are expressed by various degrees of reddening. The effects of the alteration processes on pyroclastic rocks are as follows: hydration and oxidation of each component of the pyroclastic rocks to varying degrees; formation of authigenic smectite; precipitation of a large variety of soluble salts; and corrosion on the surface of glass fragments (pitting). Dry surge beds, emplaced from a two-phase, dry steam + solid, suspension do not show significant alteration. By contrast, wet surge deposits, suggesting an emplacement from free water-bearing turbulent flows, show an increasing degree of alteration, passing from grey to red coloured beds. The strict relationship between the present alteration state and the depositional unit rules out any post-depositional processes. The occurrence of alteration in wet surge beds and the lack of alteration in dry beds shows that the main controlling agent was water condensed from the eruptive cloud and suggests a syn-depositional character to the alteration itself. These observed differences can be ascribed to the different chemical reactivities of the water, probably related to the amounts of acidic species carried by the eruptive cloud and/or by the efficiency of their capture during the condensation of the water vapour.