The amino acid sequence of ferredoxin from the alga Mastigocladuslaminosus

Ferredoxin was purified from the thermophilic blue-green alga, Mastigocladuslaminosus. The physicochemical properties of this ferredoxin are similar to those of other [2Fe-2S] plant ferredoxins except for its unusual thermal stability. The primary structure of the protein was determined and consists of 98 amino acid residues, 5 of which are cysteines. The positions of 4 cysteines which bind the iron atoms of the active centre are identical to those in other ferredoxins. The primary structure of the ferredoxin does not reveal any special features to account for its high thermal stability.     

Microfossils,a Key to Unravel Cold-Water Carbonate Mound Evolution through Time: Evidence from the Eastern Alboran Sea

Cold-water coral (CWC) ecosystems occur worldwide and play a major role in the ocean''s carbonate budget and atmospheric CO₂ balance since the Danian (~65 m.y. ago). However their temporal and spatial evolution against climatic and oceanographic variability is still unclear. For the first time, we combine the main macrofaunal components of a sediment core from a CWC mound of the Melilla Mounds Field in the Eastern Alboran Sea with the associated microfauna and we highlight the importance of foraminifera and ostracods as indicators of CWC mound evolution in the paleorecord. Abundances of macrofauna along the core reveal alternating periods dominated by distinct CWC taxa (mostly Lophelia pertusa, Madrepora oculata) that correspond to major shifts in foraminiferal and ostracod assemblages. The period dominated by M. oculata coincides with a period characterized by increased export of refractory organic matter to the seafloor and rather unstable oceanographic conditions at the benthic boundary layer with periodically decreased water energy and oxygenation, variable bottom water temperature/density and increased sediment flow. The microfaunal and geochemical data strongly suggest that M. oculata and in particular Dendrophylliidae show a higher tolerance to environmental changes than L. pertusa. Finally, we show evidence for sustained CWC growth during the Alleröd-Younger-Dryas in the Eastern Alboran Sea and that this period corresponds to stable benthic conditions with cold/dense and well oxygenated bottom waters, high fluxes of labile organic matter and relatively strong bottom currents     

Accessibility of the ribosomal genes to micrococcal nuclease in Physarum polycephalum.

In Physarum polycephalum most genes coding for ribosomal RNA are not integrated in chromosomes, but are located in many copies in the nucleolus as plasmid-like palindromic DNA molecules. To find out whether coding sequences of rDNA are organized in a chromatin-like structure similar to that of bulk chromatin, nuclei were treated with micrococcal nuclease and DNA fragments were isolated. From bulk chromatin multimers of a basic unit of 170-180 base pairs were obtained. Nuclease fragmented DNA hybridized with labelled 19-S + 26-S rRNA was found to give the same saturation value as did unfragmented control DNA. No preferential degradation of ribosomal genes to acid soluble products was observed. A more detailed analysis of the nuclease degradation products was carried out with fragments separated by preparative gel electrophoresis. DNA eluted from the gels was hybridized in solution with labelled 19-S + 26-S rRNA. The coding sequences of rRNA were found to be degraded to approximately nucleosome size slightly more quickly than was the DNA of bulk chromatin. However, the distribution of the rDNA fragments on the gels did not coincide with the distribution of the fragments derived from bulk chromatin nucleosomes and their oligomers. The amount of rDNA in the interband regions was about intermediate between that found in the two adjacent bands. These results lead to the conclusion that the ribosomal genes, most of which are presumably active during rapid growth, are protected by proteins, probably histones. However, the ribosomal genes are present in a structure differing in some way from that of bulk chromatin.     

Non-condensation of one segment of a chromosome No. 2 in a male with an otherwise normal karyotype (and severe hypospadias)

Summary A child with severe hypospadias is presented, whose karyotype showed in about 11% of mitoses of peripheral blood one member of chromosome pair No. 2 with a non-condensed region near the centromere. The non-condensed segment does not show late replication, however, it is situated very close to the late replicating segment of the long arms of chromosome No. 2. The nature and possible implications of this kind of aberration are discussed. It is held that non-condensation can produce localized chromosome breaks by a mechanism possibly different from any of the classical breakage mechanisms.