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Algae and nitrogen fixers) and parasites of producers and c o n s u m e r s . Similarly, while m e a s u r e m e n t s of energy fixation 32 R. T. Coupland, R. Y. Zacharuk, and E. A. Paul and carbon assimilation by producers may be m a d e by both biomass and photosynthesis a p p r o a c h e s , these t w o activities will be less closely related than those of the physiologist and the micrometeorologist w h o will need to share equipment. C o n s e q u e n t l y , the organization of the activities at M a t a d o r (Fig.
H . G i n i n g h a m sponsored by Section P T . Hopefully, a large n u m b e r of e c o s y s t e m studies established in many countries during the I B P will result in detailed understanding of the organization of systems which are being d e p e n d e d upon for sustained production of food crops. T h e y will undoubtedly result in important a d v a n c e s in techniques of study. REFERENCES Alexander, Μ. 1964. Biochemical e c o l o g y of soil microorganisms. Ann. Rev. Microbiol. 18, 2 1 7 - 2 5 2 .
T h e p r o t o z o a and c h e m o - and p h o t o a u t o t r o p h s , if they are not covered in the p r o d u c e r or c o n s u m e r groups, should be considered. T h e goal of the initial surveys will be to estimate the relative importance of these major groups in terms of n u m b e r s and biomass in order to determine the microbiological homogeneity of the e c o s y s t e m . S y n e c o logical studies provide a m e a n s of assessing homogeneity and background information for studies of carbon and nitrogen turnover.