. O lO 2 O 3-0 CCS SCALE Fig. 3. Vertical distribution of the standing crop of zooplankton in 80° W. Observations in o°, 200 E and 8o° W in other years (Fig. 4) The observations in o°, 200 E and 8o° W present a more or less complete series extending over a 12-month period from which it has been possible to gain some idea of the vertical distribution of the standing crop in any one month. Conditions, however, may not be the same in different years, particularly in Antarctic regions where the presence or absence of pack ice can influence the biology of the whole area. In order to see what year t
. O lO 2 O 3-0 CCS SCALE Fig. 3. Vertical distribution of the standing crop of zooplankton in 80° W. Observations in o°, 200 E and 8o° W in other years (Fig. 4) The observations in o°, 200 E and 8o° W present a more or less complete series extending over a 12-month period from which it has been possible to gain some idea of the vertical distribution of the standing crop in any one month. Conditions, however, may not be the same in different years, particularly in Antarctic regions where the presence or absence of pack ice can influence the biology of the whole area. In order to see what year to year differences are likely to occur, observations in
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