Homeostatic transcriptional regulation of bcl-2 in the epidermis

Bcl-2, a crucial regulator of cell survival, is frequently overexpressed in basal cell carcinomas (BCCs), the most commonly diagnosed cancers. Regulation of bcl-2 expression in epidermal keratinocytes is not well characterized. In the epidermis, bcl-2 is expressed only in keratinocytes of the basal layer and the outer root sheath of hair follicles and no bcl-2 expression in suprabasalar keratinocytes. The calcium gradient in the epidermis is a potent regulator of keratinocyte differentiation. Increasing calcium concentrations associated with differentiation, resulted in the downregulation of a 2.9 kb bcl-2 promoter luciferase construct. The AP-1 family of transcription factors is differentially expressed in the strata of the epidermis and has been shown to be involved in the stage specific expression of numerous differentiation markers in the epidermis. In silico analysis of the bcl-2 promoter and gene reporter assays showed that co-transfection of JUNB and JUND, but not other AP-1 dimers, caused a significant upregulation of the bcl-2 promoter in primary keratinocytes. Immunoelectrophoretic mobility shift assays, in vivo chromatin immunoprecipitation (ChIP) studies and mutational analysis of AP-1 binding site 3 on the bcl-2 promoter identified it as the site involved in bcl-2 regulation. Utilizing site directed mutants, we determined that phosphorylation at Ser90/Ser100 residues of JUND is required for the activation of the bcl-2 promoter. ^ The sonic hedgehog (SHH) pathway is frequently deregulated in BCCs and, we have shown that GLI1 upregulates bcl-2 in keratinocytes. While examining potential regulation of the SHH pathway extracellular calcium, we found that higher calcium concentrations are associated with lowered HH pathway activity and upregulation of suppressor of fused (SUFU) which negatively regulates the SHH pathway. ChIP assays, and in vivo mouse models, show that ΔNp63α, a crucial regulator of epidermal development, binds and activates the SUFU promoter in differentiating keratinocytes. Increasing SUFU levels prevent transactivation of the bcl-2 promoter. In vitro SUFU knockdown along with in vivo SUFU+/− murine models demonstrate a significant upregulation of bcl-2 expression. ^ In conclusion, the spatial and temporal expression of bcl-2 during keratinocyte differentiation in the epidermis is a complex process requiring cooperative interactions of specific signaling cascades and transcription factors. ^

A Novel Mechanism of Skin Tumor Promotion Involving Interferon-gamma (IFNγ)/Signal Transducer and Activator of Transcription-1 (Stat1) Signaling in Epidermis

The JAK-STAT pathway is a major signaling pathway involved in many biological processes including proliferation, apoptosis, and differentiation. Aberrant expression of STATs has been reported in multiple human cancers and murine mouse models of tumorigenesis. Previous studies from our lab and others have established a critical role for Stat3 in epithelial tumorigenesis, but the role of Stat1 is largely unknown. The current study was designed to explore the role of Stat1 during multistage skin carcinogenesis. Topical treatment with both TPA and the anthrone derivative chrysarobin (CHRY) led to rapid phosphorylation of Stat1 on both tyrosine (Tyr701) and serine (Ser727) residues in epidermis. CHRY treatment also led to upregulation of unphosphorylated Stat1 (uStat1) at later time points. In addition, CHRY treatment also led to upregulation of IRF-1 mRNA and protein which was dependent on Stat1. Further analyses demonstrated that topical treatment with CHRY but not TPA upregulated interferon-gamma (IFNg) mRNA in the epidermis and that the induction of both IRF-1 and uStat1 was dependent on IFNg signaling. Stat1 deficient (Stat1-/-) mice were highly resistant to skin tumor promotion by CHRY. In contrast, the tumor response (in terms of both papillomas and squamous cell carcinomas) was similar in Stat1-/- mice and wild-type littermates with TPA as the promoter. Histological evaluation of the proliferative response confirmed the data obtained from the tumor study for both TPA and CHRY. In addition, maximal induction of both cyclooxygenase-2 and inducible nitric oxide synthase in epidermis following treatment with CHRY was also dependent on the presence of functional Stat1. Following CHRY treatment, Stat1-/- mice exhibited reduced macrophage infiltration and reduced production of many immune cell derived chemokines/cytokines. These studies define a novel mechanism associated with skin tumor promotion by the anthrone class of tumor promoters involving upregulation of IFNg signaling in the epidermis and downstream signaling through activated (phosphorylated) Stat1 and subsequent upregulation of IRF-1 and uStat1.

Reconstructed pCO2 data from tree ring cellulose d13C during 1902-2005 at 10 sites in the Tropics and Northern Subtropics

This is the reconstructed pCO2 data from Tree ring cellulose d13C data with estimation errors for 10 sites (location given below) by a geochemical model as given in the publication by Trina Bose, Supriyo Chakraborty, Hemant Borgaonkar, Saikat Sengupta. This data was generated in Stable Isotope Laboratory, Indian Institute of Tropical Meteorology, Pune - 411008, India

Reconstructed glaciation limits in Eurasia (digitized from map Fig.1)

Based on field investigations in northern Russia and interpretation of offshore seismic data, we have made a preliminary reconstruction of the maximum ice-sheet extent in the Barents and Kara Sea region during the Early/Middle Weichselian and the Late Weichselian. Our investigations indicate that the Barents and Kara ice sheets attained their maximum Weichselian positions in northern Russia prior to 50 000 yr BP, whereas the northeastern flank of the Scandinavian Ice Sheet advanced to a maximum position shortly after 17000 calendar years ago. During the Late Weichselian (25 000-10000 yr BP), much of the Russian Arctic remained ice-free. According to our reconstruction, the extent of the ice sheets in the Barents and Kara Sea region during the Late Weichselian glacial maximum was less than half that of the maximum model which, up to now, has been widely used as a boundary condition for testing and refining General Circulation Models (GCMs). Preliminary numerical-modelling experiments predict Late Weichselian ice sheets which are larger than the ice extent implied for the Kara Sea region from dated geological evidence, suggesting very low precipitation.

Cenomanian/Turonian sea surface temperatures of the equatorial Atlantic reconstructed from geochemical data

Oceanic anoxic event 2 (OAE-2) occurring during the Cenomanian/Turonian (C/T) transition is evident from a globally recognized positive stable carbon isotopic excursion and is thought to represent one of the most extreme carbon cycle perturbations of the last 100 Myr. However, the impact of this major perturbation on and interaction with global climate remains unclear. Here we report new high-resolution records of sea surface temperature (SST) based on TEX86 and d 18O of excellently preserved planktic foraminifera and stable organic carbon isotopes across the C/T transition from black shales located offshore Suriname/French Guiana (Demerara Rise, Ocean Drilling Program Leg 207 Site 1260) and offshore Senegal (Cape Verde Basin, Deep Sea Drilling Project Leg 41 Site 367). At Site 1260, where both SST proxy records can be determined, a good match between conservative SST estimates from TEX86 and d 18O is observed. We find that late Cenomanian SSTs in the equatorial Atlantic Ocean (33°C) were substantially warmer than today (27°-29°C) and that the onset of OAE-2 coincided with a rapid shift to an even warmer (35°-36°C) regime. Within the early stages of the OAE a marked (4°C) cooling to temperatures lower than pre-OAE conditions is observed. However, well before the termination of OAE-2 the warm regime was reestablished and persisted into the Turonian. Our findings corroborate the view that the C/T transition represents the onset of the interval of peak Cretaceous warmth. More importantly, they are consistent with the hypotheses that mid-Cretaceous warmth can be attributed to high levels of atmospheric carbon dioxide (CO2) and that major OAEs were capable of triggering global cooling through the negative feedback effect of organic carbon-burial-led CO2 sequestration. Evidently, however, the factors that gave rise to the observed shift to a warmer climate regime at the onset of OAE-2 were sufficiently powerful that they were only briefly counterbalanced by the high rates of carbon burial attained during even the most extreme interval of organic carbon burial in the last 100 Myr.