. ^tTgmTl3l4l5l6l7lBl9 110 I II I IZl 131 I4ll5l 16 I I7l 18 I l9l20l2lla|g3la4lzSlZ6l27l2al29l30l3ll32l33!34l3SI36l37l3BI39|40|4) I42I43I^45|46|47|46| 40 50 90 110 HOUR 2310 0 02 03 04 05 07 oa 09 13 13^0 15 00 Fig. 9. Variations in the numbers of the predominant plankton organisms on Records 11 and 12; the division between these records where the ship stopped for soundings is indicated by the vertical broken line. arctica stretching for 75 miles and followed by a small but almost equally dense patch some 12 miles farther on. An interesting feature of the record is the dense concentration of
. ^tTgmTl3l4l5l6l7lBl9 110 I II I IZl 131 I4ll5l 16 I I7l 18 I l9l20l2lla|g3la4lzSlZ6l27l2al29l30l3ll32l33!34l3SI36l37l3BI39|40|4) I42I43I^45|46|47|46| 40 50 90 110 HOUR 2310 0 02 03 04 05 07 oa 09 13 13^0 15 00 Fig. 9. Variations in the numbers of the predominant plankton organisms on Records 11 and 12; the division between these records where the ship stopped for soundings is indicated by the vertical broken line. arctica stretching for 75 miles and followed by a small but almost equally dense patch some 12 miles farther on. An interesting feature of the record is the dense concentration of the larval Euphausiacea which occurred in the gap between the two patches of phyto- plankton. The significance of the inverse correlation between the phyto- and the zoo- plankton has been discussed at length by the author recently (in Hardy and Gunther, 1935). In this record it is impossible to decide whether the concentration of the euphausians is to be attributed to an exclusive influence of the phytoplankton or
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Keywords: ., bookcentury1900, booksubjectocean, booksubjectscientificexpediti
