A COMPARISON OF CHLOROPLAST MEMBRANE SURFACES VISUALIZED BY FREEZE-ETCH AND NEGATIVE STAINING TECHNIQUES; AND ULTRASTRUCTURAL CHARACTERIZATION OF MEMBRANE FRACTIONS OBTAINED FROM DIGITONIN-TREATED SPINACH CHLOROPLASTS

Author:

Arntzen C. J.1,Dilley R. A.1,Crane F. L.1

Affiliation:

1. From the Charles F. Kettering Research Laboratory, Yellow Springs, Ohio 45387, and from the Department of Biological Sciences, Purdue University, W. Lafayette, Indiana 47906

Abstract

Spinach chloroplast lamellae were washed free of negatively staining surface particles (carboxydismutase and coupling factor protein) and the resulting smooth-surfaced lamellae still showed the usual large (175 A) and small (110 A) particles seen by freeze-etching. Therefore, the freeze-fracture plane probably occurs along an internal surface of the chloroplast membrane. Fractions obtained by differential centrifugation of digitonin-treated chloroplast membranes were studied by negative staining, thin sectioning, and freeze-etching techniques for electron microscopy. The material sedimenting between 1,000 g and 10,000 g, enriched in photosystem II activity, was shown to consist of membrane fragments. These freeze-etched membrane fragments were found to have large particles on most of the exposed fracture faces. The large particles had the same size and distribution pattern as the 175 A particles seen in intact chloroplast membranes. The material sedimenting between 50,000 g and 144,000 g, which had only photosystem I activity, was found to consist of particles in various degrees of aggregation. Freeze-etching of this fraction revealed only small particles corresponding to the 110 A particles seen in intact chloroplasts. A model is presented suggesting that chloroplast lamellar membranes have a binary structure, which digitonin splits into two components. The two membrane fragments have different structures, revealed by freeze-etching, and different photochemical and biochemical functions.

Publisher

Rockefeller University Press

Subject

Cell Biology

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