The antiapoptotic effect of overexpression c -erBb2 in breast cancer

Overexpression of the receptor tyrosine kinase p185ErbB2 confers taxol resistance in breast cancers and activation of p34Cdc2 is required for taxol-induced apoptosis and cytotoxicity. Here, we investigated the underlying mechanisms and found that overexpression of p185 ErbB2 inhibits taxol-induced apoptosis through two branches to inhibit activation of p34Cdc2. ^ Overexpression of p185ErbB2 in MDA-MB-435 cells by transfection transcriptionally upregulated p21Cip1, which associates with p34Cdc2, inhibits taxol-mediated p34Cdc2 activation, delays cell entrance to G2/M phase, and thereby inhibits taxol-induced apoptosis. In p21Cip1 antisense-transfected MDA-MB-435 cells or in p21−/− MEF cells, p185ErbB2 was unable to inhibit taxol-induced apoptosis. Therefore, p21Cip1 participates in the regulation of a G2/M checkpoint that contributes to resistance to taxol-induced apoptosis in p185ErbB2-overexpressing breast cancer cells. ^ Direct phosphorylation on Tyrosine-15 of p34Cdc2 by p185 ErbB2 receptor tyrosine kinase inhibits p34Cdc2 activation. The wild-type p185ErbB2 but not the kinase-defective mutant, when overexpressed in breast cancer cells, can phosphorylate p34Cdc2 on tyrosine (Tyr)15, an inhibitory phosphorylation site of p34 Cdc2. The kinase domain of the ErbB2 receptor was sufficient for binding to p34Cdc2 and directly phosphorylating the recombinant Cdc2. Phosphospecific Cdc2-Tyr15 immunoblot analyses, immunocomplex kinase assays, and phospho-amino acid analyses revealed that p185ErbB2 specifically phosphorylates Cdc2 on Tyr15. Phosphorylation of Cdc2-Tyr15 by ErbB2 is modulated during cell cycle and corresponded with delayed cell entry into G2/M phase. The kinase-defective p185ErbB2, which incapable of phosphorylating Cdc2-Tyr15, failed to inhibit taxol-induced activation and apoptosis, whereas the wild-type and the constitutive-active p185ErbB2 did. Increased Cdc2-Tyr15 phosphorylation was found in Erb132-overexpressing tumors from breast cancer patients. Thus, direct phosphorylation of Cdc2-Tyr15 by p185 ErbB2 RTK in breast cancer cells inhibits taxol-induced p34 Cdc2 activation and apoptosis, thereby conferring taxol resistance. ^

Calibration and application of B/Ca, Cd/Ca, and d11B in Neogloboquadrina pachyderma (sinistral)

The North Atlantic and Norwegian Sea are prominent sinks of atmospheric CO2 today, but their roles in the past remain poorly constrained. In this study, we attempt to use B/Ca and d11B ratios in the planktonic foraminifera Neogloboquadrina pachyderma (sinistral variety) to reconstruct subsurface water pH and pCO2 changes in the polar North Atlantic during the last deglaciation. Comparison of core-top results with nearby hydrographic data shows that B/Ca in N. pachyderma (s) is mainly controlled by seawater [B(OH)4]?/[HCO3]? with a roughly constant partition coefficient (KD =([B/Ca]of CaCO3)/([B(OH)4]-/[HCO3]-)of seawater) of 1.48 ± 0.15 * 10**-3 (2sigma), and d11B in this species is offset below d11B of the borate in seawater by 3.38 ± 0.71 per mil (2sigma). These values represent our best estimates with the sparse available hydrographic data close to our core-tops. More culturing and sediment trap work is needed to improve our understanding of boron incorporation into N. pachyderma (s). Application of a constant KD of 1.48 * 10**-3 to high resolution N. pachyderma (s) B/Ca records from two adjacent cores off Iceland shows that subsurface pCO2 at the habitat depth of N. pachyderma (s) (~50 m) generally followed the atmospheric CO2 trend but with negative offsets of ~10-50 ppmv during 19-10 ka. These B/Ca-based reconstructions are supported by independent estimates from low-resolution d11B measurements in the same cores. We also calibrate and apply Cd/Ca in N. pachyderma (s) to reconstruct nutrient levels for the same down cores. Like today's North Atlantic, past subsurface pCO2 variability off Iceland was significantly correlated with nutrient changes that might be linked to surface nutrient utilization and mixing within the upper water column. Because surface pCO2 (at 0 m water depth) is always lower than at deeper depths and if the application of a constant KD is valid, our results suggest that the polar North Atlantic has remained a CO2 sink during the calcification seasons of N. pachyderma (s) over the last deglaciation.