Characterization of osteopontin charge forms produced by osteoblasts

Osteopontin (OPN) is a highly-phosphorylated extracellular matrix protein localized in bone, kidney, placenta, T-lymphocytes, macrophages, smooth muscle of the vascular system, milk, urine, and plasma. In ROS 17/2.8 osteoblast-like osteosarcoma cells, 1,25-dihydroxyvitamin D3 [1,25(OH)2D 3] regulates OPN at the transcriptional level resulting in increased steady state mRNA levels and increased production of OPN protein, maximal at 48 hours. Using ROS 17/2.8 cells as an osteoblast model, OPN was purified from culture medium after three hour treatments of either vehicle (ethanol) or 1,25(OH)2D3 via barium citrate precipitation followed by immunoaffinity chromatography. ^ Here, further evidence of regulation of OPN by 1,25(OH)2D 3 at the posttranslational level is presented. Prior to the up-regulation of OPN at the transcriptional level, 1,25(OH)2D3 induces a shift in OPN isoelectric point (pI) detected on two-dimensional gels from pI 4.6 to pI 5.1. Loading equal amounts of [32P]-labeled OPN recovered from ROS 17/2.8 cells exposed to 1,25(OH)2D3 or vehicle alone for three hours reveals that the shift from pI 4.6 to 5.1 is the result of reduced phosphorylation. Using structural analogs to 1,25(OH) 2D3, analog AT [25-(OH)-16-ene-23-yne-D3], which triggers Ca2+ influx through voltage sensitive Ca2+ channels but does not bind to the vitamin D receptor, mimicked the OPN pI shift while analog BT [1,25(OH)2-22-ene-24-cyclopropyl-D 3], which binds to the vitamin D receptor but does not allow Ca 2+ influx, did not. Inclusion of the Ca2+ channel blocker nifedipine also blocks the charge shift conversion of OPN. Further analysis of the signaling pathway initiated by 1,25(OH)2D3 reveals that inhibition of the cyclic 3′,5′ -adenosine monophosphate-dependent kinase, protein kinase A, or inhibition of the cyclic 3′,5′-guanine monophosphate-dependent kinase, protein kinase G, also prevents the charge shift conversion. ^ Isolation of OPN from rat femurs and tibiae provides evidence for the existence of these two OPN charge forms in vivo, evidenced by differential migration on isoelectric focusing gels and sodium dodecyl sulfate-polyacrylamide gels. Peptide sequencing of rat long bone fractions revealed the presence of a presumed dentin specific protein, dentin matrix protein-1 (DMP-1). Western blot analysis confirmed the existence of DMP-1 in these fractions. ^ Using the OPN charge forms in functional assays, it was determined that the charge forms have differential roles in both cell surface and mineralization functions. In cell attachment assays and Ca2+ influx assays using PC-3 prostate cancer cells, the pI 5.1 charge form of OPN was found to permit binding and increase intracellular Ca2+ concentrations of PC-3 cells. The increase in intracellular Ca2+ concentration was found to be integrin αvβ3-dependent. In mineralization assays, the pI 4.6 charge form of OPN promoted hydroxyapatite formation, while the pI 5.1 charge form had improved Ca2+ binding ability. ^ In conclusion, these findings suggest that 1,25(OH) 2D3 regulates OPN not only at the transcriptional level, but also plays a role in determination of the OPN phosphorylation state. The latter involves a short term (less than three hours) treatment and is associated with membrane-initiated Ca2+ influx. Functional assays utilizing the two OPN charge forms reveal the dependence of OPN post-translational state on its function. ^

Comparing barriers and predictors for colorectal cancer screening between African Americans and Whites

Colorectal cancer (CRC) has been one of the leading causes of cancer death in the United States. Although incidence and mortality rates of colorectal cancer in the United States have decreased in recent years, the disparity in CRC incidence and mortality between African Americans and Whites remain. Disparity in CRC screening rates is believed to be one of the causes that contribute to the disparity in CRC incidence and mortality between these two races. Finding the differences in CRC screening barriers and predictors between these two groups can help us to design more effective intervention programs to improve CRC screening rates for African Americans. However, most of the previous studies have investigated different types of CRC screening barriers for African Americans and/or Whites, but no studies have compared the same CRC screening barriers between African Americans and Whites. The purpose of this study is to describe and compare the same CRC screening barriers between these two races. Using chi-square analysis, significant differences between African Americans and Whites were found for marital status, income and education. Compared to Whites, African Americans were less aware of CRC screening procedures and lacked CRC knowledge. Significant differences were found between African Americans and Whites in the awareness of sigmoidoscopy, colonoscopy and barium enema. After adjusting for sex, education, marital status, and household income, six out of thirteen CRC screening barriers and two out of nine CRC screening predictors remained to be statistically significantly different between African Americans and Whites. The results of this study indicated that different CRC screening barriers and predictors had different impact on African Americans, and African Americans had more CRC barriers to overcome than Whites.^

Fate and effects of drilling wastes in a shallow estuarine mesocosm

To address concerns expressed about the possible effect of drilling mud discharges on shallow, low-energy estuarine ecosystems, a 12 month study was designed to detect alterations in water quality and sediment geochemistry. Each drilling mud used in the study and sediments from the study site were analyzed in the laboratory for chemical and physical characteristics. Potential water quality impacts were simulated by the EPA-COE elutriation test procedure. Mud toxicity was measured by acute and chronic bioassays with Mysidopsis bahia, Mercenaria mercenaria, and Nereis virens.^ For the field study, a relatively pristine, shallow (1.2 m) estuary (Christmas Bay, TX) without any drilling activity for the last 30 years was chosen for the study site. After a three month baseline study, three stations were selected. Station 1 was an external control. At each treatment station (2, 3), mesocosms were constructed to enclose a 3.5 m$\sp3$ water column. Each treatment station included an internal control site also. Each in situ mesocosm, except the controls, was successively dosed at a mesocosm-specific dose (1:100; 1:1,000; or 1:10,000 v/v) with 4 field collected drilling muds (spud, nondispersed, lightly-treated, and heavily-treated lignosulfonate) in sequential order over 1.5 months. Twenty-four hours after each dose, water exchange was allowed until the next treatment. Station 3 was destroyed by a winter storm. After the last treatment, the enclosures were removed and the remaining sites monitored for 6 months. One additional site was similarly dosed (1:100 v/v) with clean dredged sediment from Christmas Bay for comparison between dredged sediments and drilling muds.^ Results of the analysis of the water samples and field measurements showed that water quality was impacted during the discharges, primarily at the highest dose (1:100 v/v), but that elevated levels of C, Cr (T,F), Cr$\sp{+3}$ (T, F), N, Pb, and Zn returned to ambient levels before the end of the 24 hour exposure period or immediately after water exchange was allowed (Al, Ba(T), Chlorophyll ABC, SS, %T). Barium, from the barite, was used as a geochemical tracer in the sediments to confirm estimated doses by mass balance calculations. Barium reached a maximum of 166x background levels at the high dose mesocosm. Barium levels returned to ambient or only slightly elevated levels at the end of the 6 month monitoring period due to sediment deposition, resuspension, and bioturbation. QA/QC results using blind samples consisting of lab standards and spiked samples for both water and sediment matrices were within acceptable coefficients of variation.^ In order to avoid impacts on water quality and sediment geochemistry in a shallow estuarine ecosystem, this study concluded that a minimal dilution of 1:1,000 (v/v) would be required in addition to existing regulatory constraints. ^