Ikaros is required to survive positive selection and to maintain clonal diversity during T-cell development in the thymus.

The zinc-finger protein Ikaros is a key player in T-cell development and a potent tumor suppressor in thymocytes. To understand the molecular basis of its function, we disabled Ikaros activity in vivo using a dominant negative Ikaros transgene (DN-IkTg). In DN-IkTg mice, T-cell development was severely suppressed, and positively selected thymocytes clonally expanded, resulting in a small thymus with a heavily skewed T-cell receptor (TCR) repertoire. Notably, DN-IkTg induced vigorous proliferation concomitant to downregulation of antiapoptotic factor expression such as Bcl2. Ikaros activity was required during positive selection, and specifically at the CD4(+)CD8(lo) intermediate stage of thymocyte differentiation, where it prevented persistent TCR signals from inducing aberrant proliferation and expansion. In particular, DN-IkTg induced the accumulation of CD4 single-positive (SP) thymocytes with a developmentally transitional phenotype, and it imposed a developmental arrest accompanied by massive apoptosis. Thus, we identified an in vivo requirement for Ikaros function, which is to suppress the proliferative potential of persistent TCR signals and to promote the survival and differentiation of positively selected thymocytes.

Stability of the infection marker struvite in urinary stone samples.

BACKGROUND AND PURPOSE: Struvite in kidney stones is an important marker for infection. In kidney stone samples, struvite is known to be prone to chemical breakdown, but no data exist on the stability of samples stored in dry form. The objective of this study was to examine stability of struvite under increasingly poor conditions of storage. MATERIALS AND METHODS: Samples of struvite kidney stones were broken to obtain 38 pieces averaging 67 mg in weight, and these were randomized into four storage conditions: Airtight containers stored in the dark, open containers in the dark, open containers in ambient light, and open containers at elevated temperature (40°C). Pieces were left for 6 months, and then analyzed for changes using micro CT and Fourier transform infrared spectroscopy (FT-IR). RESULTS: Initial samples proved to be struvite, indicating no transformation in the large specimens that had been stored in airtight containers in the dark for more than 6 years before this study. Pieces of struvite taken from these large specimens appeared unchanged by micro CT and FT-IR after being stored in closed containers for 6 months, but 8 of 9 pieces in open containers showed the presence of newberyite in surface layers, as did 10 of 10 pieces in open containers out in ambient light. All pieces stored at 40°C showed transformation of struvite, with 60% of the pieces showing the presence of amorphous phosphates, indicating complete breakdown of struvite in the surface layers of the pieces. CONCLUSION: We conclude that struvite in dry kidney stone samples is stable when the specimens are stored in airtight containers at room temperature, even after several years.