During occupational trainings given to Polish employees, one can quite often observe complaining. The instructor can use it for problem-solving or for purification. Thus, complaining plays an instrumental or cathartic function. This has consequences for the entire training process. The aim of the article is to present the phenomenon of complaining during training courses and to discuss its correlation with different variables such as learning results, participants’ mood and the evaluation of the training course. Questions were therefore posed about which function of complaining would be more conducive to the process of learning the material and result in an improvement of the participants’ mood, as well as how the instructor would be evaluated, at the response level, depending on which function of complaining is activated during the training. In order to answer these questions, the authors designed an experiment in which complaining was induced in members of an organization, performing either an instrumental function or a cathartic function. The results show that the most effective strategy is the use of its object as a point of departure for problem solution.
The material discussed in this paper was collected in the Drake Passage and Bransfield Strait (Antarctica) within the framework of the BIOMASS-SIBEX programme. Samples were collected by hauling Nansen nets verticaly through the 100 — 0, 300—100 and 500 — 300 m layers in December 1983 and January 1984. Of the six species recorded — Metaconchoecia isocheira, Alacia hettacra, Alacia belgicae, Metaconchoecia skogsbergi, Boroecia antipoda and Discoconchoecia off. elegans — the first three, endemic to Antarctic waters — were predominant (92.9%). Ostracoda were found most abundantly in the eastern part of the study area — between Elephant Island and South Orkney Islands, and in the south-western part of Bransfield Strait. Their vertical distribution depended on the hydrological conditions. Ostracoda were most numerous in the 500—300 m and 300 — 100 m layers; very few were recorded in the 100—0 m surface layer.