We suggest an extension ofconnexinorthology relationships across the major vertebrate lineages. We first show that the conserved domains of mammalianconnexins(encoding the N-terminus, four transmembrane domains and two extracellular loops) are subjected to a considerably more strict selection pressure than the full-length sequences or the variable domains (the intracellular loop and C-terminal tail). Therefore, the conserved domains are more useful for the study of family relationships over larger evolutionary distances. The conserved domains ofconnexinswere collected from chicken,Xenopus tropicalis, zebrafish, pufferfish, green spotted pufferfish,Ciona intestinalisandHalocynthia pyriformis(two tunicates). A total of 305connexinsequences were included in this analysis. Phylogenetic trees were constructed, from which the orthologies and the presumed evolutionary relationships between the sequences were deduced. The tunicateconnexinsstudied had the closest, but still distant, relationships to vertebrateconnexin36,39.2,43.4,45and47. The main structure in theconnexinfamily known from mammals pre-dates the divergence of bony fishes, but some additional losses and gains ofconnexinsequences have occurred in the evolutionary lineages of subsequent vertebrates. Thus, theconnexingene family probably originated in the early evolution of chordates, and underwent major restructuring with regard to gene and subfamily structures (including the number of genes in each subfamily) during early vertebrate evolution.

Gap junction intercellular communication (GJIC) and hemichannel permeability may have important roles during an ischemic insult. Our aim was to evaluate the effect of ischemia on gap junction channels and hemichannels. We used neonatal rat heart myofibroblasts and simulated ischemia with a HEPES buffer with high potassium, low pH, absence of glucose, and oxygen tension was reduced by dithionite. Microinjection, western blot, immunofluorescence, cell viability and dye uptake were used to evaluate the effects induced by dithionite. Isolated perfused rat hearts were used to analyse infarct size. Short period with simulated ischemia reduced the ability to transfer a dye between neighbouring cells, which indicated reduced GJIC. Prolonged exposure to simulated ischemia caused opening of hemichannels, and cell death was apparent while gap junction channels remained closed. Connexin 43 became partially dephosphorylated and the total amount decreased during simulated ischemia. We were not able to detect the alternative hemichannel-forming protein, Pannexin 1, in these cells. The potential importance of Connexin 43 or Pannexin 1 hemichannels in ischemia-induced infarct in the intact heart was studied by perfusion of the heart in the presence of peptides that block one or the other type of hemichannels. The connexin-derived peptide, Gap26, significantly reduced the infract/risk zone ratio (control 48.7±4.2% and Gap26 19.4±4.1%, p<0.001), while the pannexin-derived peptide, (10)Panx1, did not change infarct/risk ratio. Connexin 43 is most likely responsible for both closure of gap junction channels and opening of hemichannels during simulated ischemia in neonatal rat heart myofibroblasts. Opening of connexin 43 hemichannels during ischemia-reperfusion seems to be an important mechanism for ischemia-reperfusion injury in the heart. By preventing the opening of these channels during early ischemia-reperfusion the infarct size becomes significantly reduced.

Dispersal limitation, not just environmental selection, plays an important role in microbial biogeography. The distance–decay relationship is thought to be weak in habitats where dispersal is high, such as in the pelagic environment, where ocean currents facilitate microbial dispersal. Most studies of microbial community composition to date have observed little geographical heterogeneity on a regional scale (100 km). We present a study of microbial communities across a dynamic frontal zone in the southwest Indian Ocean and investigate the spatial structure of the microbes with respect to the different water masses separated by these fronts. We collected 153 samples of free-living microorganisms from five seamounts located along a gradient from subtropical to subantarctic waters and across three depth layers: (i) the sub-surface chlorophyll maximum (approx. 40 m), (ii) the bottom of the euphotic zone (approx. 200 m), and (iii) the benthic boundary layer (300–2000 m). Diversity and abundance of microbial operational taxonomic units (OTUs) were assessed by amplification and sequencing of the 16S rRNA gene on an Illumina MiSeq platform. Multivariate analyses showed that microbial communities were structured more strongly by depth than by latitude, with similar phyla occurring within each depth stratum across seamounts. The deep layer was homogeneous across the entire survey area, corresponding to the spread of Antarctic intermediate water. However, within both the sub-surface layer and the intermediate depth stratum there was evidence for OTU turnover across fronts. The microbiome of these layers appears to be divided into three distinct biological regimes corresponding to the subantarctic surface water, the convergence zone and subtropical. We show that microbial biogeography across depth and latitudinal gradients is linked to the water masses the microbes persist in, resulting in regional patterns of microbial biogeography that correspond to the regional scale physical oceanography.