Transport, capture and exocytosis of single synaptic vesicles at active zones

To sustain high rates of transmitter release, synaptic terminals must rapidly re-supply vesicles to release sites and prime them for exocytosis. Here we describe imaging of single synaptic vesicles near the plasma membrane of live ribbon synaptic terminals. Vesicles were captured at small, discrete active zones near the terminal surface. An electric stimulus caused them to undergo rapid exocytosis, seen as the release of a fluorescent lipid from the vesicles into the plasma membrane. Next, vesicles held in reserve about 20 nm from the plasma membrane advanced to exocytic sites, and became release-ready 250 ms later. Apparently a specific structure holds vesicles at an active zone to bring v-SNAREs and t-SNAREs, the proteins that mediate vesicle fusion, within striking distance of each other, and then allows the triggered movement of such vesicles to the plasma membrane.     

Permian tetrapods from the Sahara show climate-controlled endemism in Pangaea

New fossils from the Upper Permian Moradi Formation of northern Niger provide an insight into the faunas that inhabited low-latitude, xeric environments near the end of the Palaeozoic era (approximately 251 million years ago). We describe here two new temnospondyl amphibians, the cochleosaurid Nigerpeton ricqlesi gen. et sp. nov. and the stem edopoid Saharastega moradiensis gen. et sp. nov., as relicts of Carboniferous lineages that diverged 40-90 million years earlier. Coupled with a scarcity of therapsids, the new finds suggest that faunas from the poorly sampled xeric belt that straddled the Equator during the Permian period differed markedly from well-sampled faunas that dominated tropical-to-temperate zones to the north and south. Our results show that long-standing theories of Late Permian faunal homogeneity are probably oversimplified as the result of uneven latitudinal sampling.