Bazzi M D, Nelsestuen G L
Department of Biochemistry, University of Minnesota, St. Paul 55108.
Biochemistry. 1988 Sep 6;27(18):6776-83. doi: 10.1021/bi00418a020.
The association of protein kinase C (PKC) with phospholipid (PL) monolayers spread at the air-water interface was examined. PKC-PL binding induced surface pressure changes that were dependent on the amount of PKC, the phospholipid composition of the monolayers, the presence of Ca2+, and the initial surface pressure of the monolayer (pi 0). Examination of surface pressure increases induced by PKC as a function of phospholipid surface pressure, pi 0, revealed that PKC-phosphatidylserine (PS) association had a critical pressure of 43 dyn/cm. Above this surface pressure, PKC cannot cause further surface pressure changes. This high critical pressure indicated that PKC should be able to penetrate many biological membranes which appear to have surface pressures of about 30 dyn/cm. PKC-induced surface pressure changes were Ca2+ dependent only for PL monolayers spread at a pi 0 greater than 26 dyn/cm. PKC alone (in the absence of PL) formed a film at the air-water interface with a surface pressure of about 26 dyn/cm. Calcium-dependent binding was studied at the higher surface pressures which effectively excluded PKC from the air-water interface. Subphase depletion measurements suggested that association of PKC with PS monolayers consisted of two stages: a rapid Ca2+-dependent interaction followed by a slower process that resulted in irreversible binding of PKC to the monolayer. The second stage appeared to involve penetration of PKC into the hydrocarbon region of the phospholipid. The commonly used in vitro substrates for PKC, histone and protamine sulfate, also associated with and penetrated PS monolayers with critical pressures of 50 and 60 dyn/cm, respectively.(ABSTRACT TRUNCATED AT 250 WORDS)
研究了蛋白激酶C(PKC)与在空气-水界面铺展的磷脂(PL)单分子层的结合情况。PKC与PL的结合引起表面压力变化,该变化取决于PKC的量、单分子层的磷脂组成、Ca2+的存在以及单分子层的初始表面压力(pi 0)。将PKC诱导的表面压力增加作为磷脂表面压力pi 0的函数进行研究,结果表明PKC与磷脂酰丝氨酸(PS)的结合具有43达因/厘米的临界压力。高于此表面压力,PKC不能引起进一步的表面压力变化。这种高临界压力表明PKC应该能够穿透许多似乎具有约30达因/厘米表面压力的生物膜。PKC诱导的表面压力变化仅在pi 0大于26达因/厘米时铺展的PL单分子层中依赖于Ca2+。单独的PKC(在没有PL的情况下)在空气-水界面形成了一个表面压力约为26达因/厘米的膜。在较高表面压力下研究了钙依赖性结合,这有效地将PKC排除在空气-水界面之外。亚相耗尽测量表明,PKC与PS单分子层的结合包括两个阶段:快速的Ca2+依赖性相互作用,随后是一个较慢的过程,导致PKC与单分子层的不可逆结合。第二阶段似乎涉及PKC渗透到磷脂的烃区域。PKC常用的体外底物组蛋白和硫酸鱼精蛋白也分别以50和60达因/厘米的临界压力与PS单分子层结合并渗透。(摘要截短于250字)