Half-att site substrates reveal the homology independence and minimal protein requirements for productive synapsis in lambda excisive recombination

The early events in site-specific excisive recombination were studied with phage lambda half-att sites that have no DNA to one side of the strand exchange region; they carry a single core-type integrase binding site and either P or P' arm flanking DNA. These half-attR and half-attL sites exhibit normal properties for the initial (covalent) top-strand transfer and form stable intermediates independent of later steps in the reaction. With these novel substrates we show that Xis specifically promotes the first strand exchange and that attL enhances Int cleavage at the top-strand site of attR. It is also shown that synapsis and initial strand transfers do not require DNA-DNA pairing but are mediated by protein-protein and protein-DNA interactions. These involve the two top-strand Int binding sites (required for the first strand exchange) and, in addition, one of the two bottom-strand sites (C') responsible for the second strand exchange.     

Autonomous DNA binding domains of lambda integrase recognize two different sequence families

The 40 kd lambda Integrase protein is shown to contain two autonomous DNA binding domains with different sequence specificities. Competition experiments in which the binding activity of Int is assayed through nuclease protection demonstrate the functional independence of the two DNA recognition specificities. Proteolytic cleavage of Int and footprinting analysis of the resulting two major peptides allow the physical separation and identification of two DNA binding domains: an amino-terminal peptide that interacts with "arm-type" sites and a carboxy-terminal peptide that binds to "core-type" sequences. In addition, the data suggest that the two domains can bind DNA simultaneously, consistent with a model in which Integrase would link two disparate DNA sequences.     

Acardiac fetus in a triplet pregnancy

The acardiac monster represents one of the most severe but rare congenital anomalies. It occurs only in multiple gestations associated with vascular anastomoses between the affected fetus and its co-twin. The prenatal diagnosis of an acardiac fetus must be suspected in any multiple gestation in which cardiac activity cannot be documented sonographically in a growing fetus. We report an acardiac fetus occurring in a spontaneously conceived triplet pregnancy. A review of the literature, including pathogenetic theories and sonographic reports, is discussed.     

Effects of decreased atmospheric deposition on the sulfur budgets of two Dutch moorland pools

The chemical composition of surface waters of two Dutch moorland pools and of incident precipitation, was monitored from 1982 to 1990. For this period, sulfur and water budgets were calculated using a hydrochemical model developed for well-mixed non-stratifying lakes. Total atmospheric deposition of S decreased significantly after 1986 at both locations. A model describing the sulfur budget in terms of input, output and reduction/oxidation processes predicted a fast decrease of pool water SO₄ ²⁻ concentrations after a decrease of atmospheric input. However, SO₄ ²⁻ concentrations in the surface water was lowered only slightly or remained constant. Apparently a source within the lake caused the unexpectedly high SO₄ ²⁻ concentrations. The possible supply of SO₄ ²⁻ from the sediment through regulation by (K-)Al-SO₄ containing minerals or desorption of SO₄ ²⁻ from positively charged surfaces in the sediment was evaluated. Solubility calculations of pore water with respect to alunite, basaluminite and jurbanite indicated that SO₄ ²⁻ concentration was not regulated by these minerals. It is suggested here (1) that desorption of SO₄ ²⁻ from peaty sediments may account for the estimated SO₄ ²⁻ supply provided that the adsorption complex is periodically recharged by partial oxidation of the upper bottom sediments and (2) that because of exposure of a part of the pool bottom to the atmosphere during dry summers and subsequent oxidation of reduced S, the amount of SO₄ ²⁻ may be provided which complements the decreasing depositional SO₄ ²⁻ input. In future research these two mechanisms need to be investigated.     

Modulation of lambda integrase synthesis by rare arginine tRNA

Lambda's int gene contains an anomalously high frequency of the rare arginine codons AGA and AGG when compared to genes of Escherichia coli or to the rest of phage lambda. These are the least frequent codons in genes of E. coli and are recognized by the rarest tRNAs. The presence of these codons reduces the translation rate and, depending on the context, this can strongly modulate translational efficiency by a variety of mechanisms. In this study, we show that expression of the natural int gene may also be modulated by rare arginine codon usage, and we explore this mechanism.     

HindII, HindIII, and HpaI restriction fragment maps of bacteriophage lambda DNA

The site-specific restriction endonucleases isolated from Hemophilus influenzae strains Rc (HincII) and Rd (HindII + III), and Hemophilus parainfluenzae (HpaI) were used to digest bacteriophage lambda DNA into 34, 40, and 15 specific fragments, respectively. The sites cleaved by each of these enzymes were localized on the lambda physical map and the fragments resulting from these cleavages were electrophoretically identified on gels by (1) analysis of the digestion profiles of deletion and transducing derivatives of lambda; and (2) digesting individual fragments produced by one restriction endonuclease with another restriction endonuclease. This paper presents the HindII, HindIII, and HpaI restriction fragment maps for the entire lambda genome, and the data used to derive these maps for the region of the lambda genome between the attachment site (at 57.3% lambda) and the right vegetative end (100% lambda). The data for mapping the left arm of lambda may be found in the accompanying paper (Robinson and Landy, 1977).     

Sulfate reduction and S-oxidation in a moorland pool sediment

In an oligotrophic moorland pool in The Netherlands, S cycling near the sediment/water boundary was investigated by measuring (1) SO₄ ^2– reduction rates in the sediment, (2) depletion of SO₄ ^2– in the overlying water column and (3) release of³⁵S from the sediment into the water column. Two locations differing in sediment type (highly organic and sandy) were compared, with respect to reduction rates and depletion of SO₄ ^2– in the overlying water.Sulfate reduction rates in sediments of an oligotrophic moorland pool were estimated by diagenetic modelling and whole core³⁵SO₄ ^2– injection. Rates of SO₄ ^2– consumption in the overlying water were estimated by changes in SO₄ ^2– concentration over time in in situ enclosures. Reduction rates ranged from 0.27–11.2 mmol m^–2 d^–1. Rates of SO₄ ^2– uptake from the enclosed water column varied from –0.5, –0.3 mmol m^–2 d^–1 (November) to 0.43–1.81 mmol m^–2 d^–1 (July, August and April). Maximum rates of oxidation to SO₄ ^2– in July 1990 estimated by combination of SO₄ ^2– reduction rates and rates of in situ SO₄ ^2– uptake in the enclosed water column were 10.3 and 10.5 mmol m^–2 d^–1 at an organic rich and at a sandy site respectively.Experiments with³⁵S^2– and³⁵SO₄ ^2– tracer suggested (1) a rapid formation of organically bound S from dissimilatory reduced SO₄ ^2– and (2) the presence of mainly non SO₄ ^2–-S derived from reduced S transported from the sediment into the overlying water. A³⁵S^2– tracer experiment showed that about 7% of³⁵S^2– injected at 1 cm depth in a sediment core was recovered in the overlying water column.Sulfate reduction rates in sediments with higher volumetric mass fraction of organic matter did not significantly differ from those in sediments with a lower mass fraction of organic matter.Corresponding author