Loss of mouse fibroblast cell response to phorbol esters restored by microinjected protein kinase C

The phorbol esters in addition to being among the most potent mouse skin tumour promoters profoundly affect many different biological systems. It is postulated that they act through activation of protein kinase C, but substantial heterogeneity in their pharmacological and binding behaviour in some systems has caused concern about whether this is their only target. Evidence linking protein kinase C activation with biological responses to the phorbol esters includes similarity in structure-activity relations for binding and response; in vitro phosphorylation of specific proteins by protein kinase C at the same sites at which phorbol ester treatment induces phosphorylation in intact cells; and correlation in certain cell types between down regulation of protein kinase C on chronic phorbol ester treatment and loss of cellular responsiveness to the phorbol ester. Here we report that microinjection of purified protein kinase C into Swiss 3T3 fibroblasts pretreated with the phorbol ester phorbol 12,13-dibutyrate (PDBu) restores the mitogenic response of the cells to PDBu, directly establishing the involvement of protein kinase C in this response.     

Cell-free synthesis and processing of multiple precursors to glucagon

Glucagon, a polypeptide hormone of 29 amino acids, is synthesized in the islets of Langerhans and immunoreactive forms of the molecule have been found in several tissues. Like many other polypeptide hormones, glucagon is synthesized via a larger precursor molecular, proglucagon; however, estimates of its size vary considerably and the biosynthetic relationship between some of the putative precursors and authentic secreted glucagon is unclear. Consequently it was of interest to investigate the primary translation product of glucagon mRNA to relate its size to that of previously described glucagon precursors. Here we provide evidence for three distinct immunoreactive preproglucagon molecules, two of which have an apparent molecular weight (MW) of approximately 16,000 (16K). Furthermore, when microsomal membranes were present during translation, the nascent 14K preproglucagon polypeptides were processed to proglucagon with a higher apparent MW of 15,000. In contrast, the nascent 16K preproglucagon was co-translationally processed to a slightly smaller polypeptide. The data indicate that the 14K and 16K preproglucagons undergo different types of post-translational modification.     

Simplification of the ecdysteroid radioimmunoassay by the use of protein A fromStaphylococcus aureus

Summary Three methods of separating antibody-bound ligand from free ligand were compared for an ecdysteroid radioimmunoassay. Ecdysteroid antibody concentration and ligand specific radioactivity were adjusted to measure 2 ranges of ecdysone concentrations (0.01–2.0 ng and 0.25–32.0 ng). In comparison with the tradiotional separating agent, ammonium sulfate, neither protein A nor polyethylene glycol altered sensitivity or specificity of the radioimmunoassays. The protein A immunoglobulin precipitation method is quick and simple, making it a preferred alternative protocol for terminating ecdysteroid radioimmunoassays.Supported by grants AM-30118 from the National Institutes of Health and PCM-8116931 from the National Science Foundation.     

The landing of the NEAR-Shoemaker spacecraft on asteroid 433 Eros

The NEAR-Shoemaker spacecraft was designed to provide a comprehensive characterization of the S-type asteroid 433 Eros (refs 1,2,3), an irregularly shaped body with approximate dimensions of 34 x 13 x 13 km. Following the completion of its year-long investigation, the mission was terminated with a controlled descent to its surface, in order to provide extremely high resolution images. Here we report the results of the descent on 12 February 2001, during which 70 images were obtained. The landing area is marked by a paucity of small craters and an abundance of 'ejecta blocks'. The properties and distribution of ejecta blocks are discussed in a companion paper. The last sequence of images reveals a transition from the blocky surface to a smooth area, which we interpret as a 'pond'. Properties of the 'ponds' are discussed in a second companion paper. The closest image, from an altitude of 129 m, shows the interior of a 100-m-diameter crater at 1-cm resolution.     

A physical map of the chicken genome

Strategies for assembling large, complex genomes have evolved to include a combination of whole-genome shotgun sequencing and hierarchal map-assisted sequencing. Whole-genome maps of all types can aid genome assemblies, generally starting with low-resolution cytogenetic maps and ending with the highest resolution of sequence. Fingerprint clone maps are based upon complete restriction enzyme digests of clones representative of the target genome, and ultimately comprise a near-contiguous path of clones across the genome. Such clone-based maps are used to validate sequence assembly order, supply long-range linking information for assembled sequences, anchor sequences to the genetic map and provide templates for closing gaps. Fingerprint maps are also a critical resource for subsequent functional genomic studies, because they provide a redundant and ordered sampling of the genome with clones. In an accompanying paper we describe the draft genome sequence of the chicken, Gallus gallus, the first species sequenced that is both a model organism and a global food source. Here we present a clone-based physical map of the chicken genome at 20-fold coverage, containing 260 contigs of overlapping clones. This map represents approximately 91% of the chicken genome and enables identification of chicken clones aligned to positions in other sequenced genomes.     

Effect of dead carbon on the ^14C dating of the speleothem

Based on the comparison of dating results among high-precision TIMS U-series and AMS ^14C as well as the published ^14C dating results and their band counting ages(i.e. calendar ages), this paper discusses the effect of dead carbon on the speleothem ^14C dating. The result shows that the fraction of incorporated dead carbon during the formation of speleothem varies. The change in the fraction of dead carbon would result in big deviation in the ^14C age of the speleothem. It is indispensable to take the dead carbon into consideration when dating the speleothem using the ^14C method or studying the atmospheric ^14C concentration during the past with the speleothem.