Protein translocation: Rehearsing the ABCs

AbstractRecent evidence that vacuolar enzymes in yeast can be delivered directly from the cytosol, rather than via the secretory pathway, alerts us to the increasing evidence for ‘non-classical’ forms of protein translocation that may involve ABC transporters

The AP2 binding site of synaptotagmin 1 is not an internalization signal but a regulator of endocytosis

One characteristic linking members of the synaptotagmin family to endocytosis is their ability to bind the heterotetrameric AP2 complex via their C2B domain. By using CD4/synaptotagmin 1 chimeras, we found that the internalization signal of synaptotagmin 1 lies at the extreme COOH-terminus of the protein and can function in the absence of the C2B domain that contains the AP2 binding site. However, although not essential for internalization, the C2B domain of synaptotagmin 1 appeared to control the recognition of the internalization motif. By mutagenesis, two sites have been identified that modify regulation by the C2B domain in the neuroendocrine PC12 cell line. Mutation of a dilysine motif in the β sandwich core of the domain eliminates endocytosis. This site is known to be a site of protein–protein interaction. Mutations in the calcium binding region, or in its close proximity, also affect internalization in PC12 cells. In fibroblasts, the C2B domain inhibits the COOH-terminal internalization signal, resulting in an absence of internalization in those cells. Thus, internalization of synaptotagmin 1 is controlled by the presence of a latent internalization signal in the COOH-terminal region and a regulatory region in the C2B domain. We propose that internalization of synaptotagmin 1 is regulated in this way to allow it to couple the processes of endocytosis and calcium-mediated exocytosis in cells of the neuroendocrine lineage

The Replication of Bacteriophage MS2: IX. Structure and Replication of the Replicative Intermediate

Experiments are described to determine whether the ribonuclease-sensitive component of the replicative intermediate formed during RNA bacteriophage infection is the nascent strand (conservative replication), or is a displaced portion of the viral strand of the RNA duplex (semi-conservative replication). Appropriate labeling experiments indicate that this component arises in each replicative intermediate molecule, with equal probability, from either origin. Those replicative intermediate molecules in which the nascent strand is ribonuclease-sensitive are more readily denatured than those in which the viral strand is partially displaced. The two types of replicative intermediate can be distinguished on this basis. It is proposed that each replicative intermediate molecule replicates both conservatively and semi-conservatively, equally often

Zircon ages in granulite facies rocks: decoupling from geochemistry above 850 °C?

Granulite facies rocks frequently show a large spread in their zircon ages, the interpretation of which raises questions: Has the isotopic system been disturbed? By what process(es) and conditions did the alteration occur? Can the dates be regarded as real ages, reflecting several growth episodes? Furthermore, under some circumstances of (ultra-)high-temperature metamorphism, decoupling of zircon U–Pb dates from their trace element geochemistry has been reported. Understanding these processes is crucial to help interpret such dates in the context of the P–T history. Our study presents evidence for decoupling in zircon from the highest grade metapelites (> 850 °C) taken along a continuous high-temperature metamorphic field gradient in the Ivrea Zone (NW Italy). These rocks represent a well-characterised segment of Permian lower continental crust with a protracted high-temperature history. Cathodoluminescence images reveal that zircons in the mid-amphibolite facies preserve mainly detrital cores with narrow overgrowths. In the upper amphibolite and granulite facies, preserved detrital cores decrease and metamorphic zircon increases in quantity. Across all samples we document a sequence of four rim generations based on textures. U–Pb dates, Th/U ratios and Ti-in-zircon concentrations show an essentially continuous evolution with increasing metamorphic grade, except in the samples from the granulite facies, which display significant scatter in age and chemistry. We associate the observed decoupling of zircon systematics in high-grade non-metamict zircon with disturbance processes related to differences in behaviour of non-formula elements (i.e. Pb, Th, U, Ti) at high-temperature conditions, notably differences in compatibility within the crystal structure