Merkle C J, Chandler D E
Department of Zoology, Arizona State University, Tempe 85287-1501.
Dev Biol. 1991 Dec;148(2):429-41. doi: 10.1016/0012-1606(91)90262-2.
Cortical granule exocytosis in sea urchins was studied using hyperosmotic and polymer-containing seawater to halt granule matrix dispersal. Addition of Na2SO4-containing seawater (2.5 osmole/kg) to Strongylocentrotus purpuratus eggs 10 to 40 sec after insemination resulted in arrest of the exocytic wave during propagation. EM examination of these eggs revealed that matrix disassembly occurred in distinct stages. In the earliest stage, granule-plasma membrane fusion had occurred, but the matrix remained completely intact. This early stage was observed in hyperosmotic media, either ionic or nonionic, suggesting that matrix hydration is required for disassembly and exocytic pore widening, but not for membrane fusion. Subsequent stages, in which partially disassembled matrices remained within omega-configured pockets, were captured by activating eggs in 30% dextran in seawater. Stability of these intermediates stages required the presence of Ca2+ and Mg2+; in the absence of divalent cations the matrices completely disassembled and the exocytic pockets flattened. Divalent cations appeared to prevent fragmentation of the matrix lamellae. Late stages of matrix disassembly, in which the lamellae fragmented and formed small particles, were inhibited by media of high ionic strength. Hyperosmolality alone, provided by sucrose, was unable to halt these late stages suggesting that water availability does not play an important role once a critical point in matrix dispersal has been reached.
利用高渗和含聚合物的海水来阻止颗粒基质扩散,对海胆的皮质颗粒胞吐作用进行了研究。在受精后10至40秒向紫球海胆卵中添加含硫酸钠的海水(2.5渗透压摩尔/千克),导致胞吐波在传播过程中停止。对这些卵进行电子显微镜检查发现,基质解体分不同阶段发生。在最早阶段,颗粒-质膜融合已经发生,但基质仍完全完整。在高渗介质(离子型或非离子型)中观察到了这个早期阶段,这表明基质水合作用是解体和胞吐孔扩大所必需的,但不是膜融合所必需的。随后的阶段,即部分解体的基质留在ω形小袋内,是通过在海水中用30%葡聚糖激活卵来捕获的。这些中间阶段的稳定性需要Ca2+和Mg2+的存在;在没有二价阳离子的情况下,基质完全解体,胞吐小袋变平。二价阳离子似乎能防止基质薄片破碎。基质解体的后期阶段,即薄片破碎并形成小颗粒,受到高离子强度介质的抑制。仅由蔗糖提供的高渗性无法阻止这些后期阶段,这表明一旦达到基质扩散的临界点,水的可用性并不起重要作用。