By Joseph L. (ed) Reid
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Published by way of the yankee Geophysical Union as a part of the Antarctic learn Series.
The Antarctic waters supply one of many severe units of features for the world's oceans. Its waters are chilly, low in salinity, dense, and excessive in dissolved oxygen, and, even if related values will be present in the Norwegian Sea, it's the out-flow from the Antarctic that fills many of the deep ocean basins of the area. The interplay of those high-latitude waters with these having the features of tropical or North Atlantic waters has lengthy been one of many significant stories of oceanology, but in simple terms within the previous few a long time have we been capable of start to gather the suitable facts.
Recent advancements, reminiscent of the reputation of the idea that of continental go with the flow and sea ground spreading, have made the antarctic areas as very important to geologists and geophysicists as to actual oceanographers and biologists.
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Extra resources for Antarctic Oceanology I
See figure legends further information. 9 and 10 for Antarctic Research Series Antarctic Oceanology I Vol. 15 37 FERROMANGANESE DEPOSITS OF THE SOUTHERN OCEAN Fig. 9 Fig. 10 Bottom sediments from the crest of the Albatross Cordillera (location 5 5 ° 5 9 ' S , 1 3 4 ° 2 7 ' W ; water depth 1740 f m ; camera station 15-18). The bottom sediments are a light olive gray (5Y6/2) ferromanganese deposits, pavements of manganese nodules calcareous ooze. Ripple marks, huge concretionary masses of (not s h o w n ) , and angular jointed and brecciated basalt flows are all seen at this camera station, an association which is common at many other camera stations.
2 ( G e o l o g y ) , 3 7 ( 1 ) , 1-14, 1965. Asano, K . , J. planktonic C. , foraminiferal Proceedings First Microfossils, Geneva, and sequence International in northeastern Conference on Japan, Planktonic vol. 1, edited by P. Bronnimann and H . H . Renz, pp. 1 4 - 2 5 , E . J. Brill, Leiden, 1969. Bandy, 0 . , The geologic significance of coiling ratios in the foraminifer Globigerina Soc. Am. Bull, 70(12-2), pachyderma (Ehrenberg), Geol. 1708, 1959. Bandy, 0 . , Planktonic foraminiferal criteria for paleoclimatic zonation, Sci.
Many authors have characterized the color of con cretions as ranging from blue-black through reddishbrown to yellow-brown, with the darker colors having higher Mn concretions. Detrital mineralogy, which may vary from less than 1% to more than 5 0 % , has been reported as rock fragments, quartz, feldspars, ferromagnesian and other heavy minerals, clay minerals, volcanic shards, animal remains, and assorted artifacts [Murray and Copyright American Geophysical Union Antarctic Research Series Antarctic Oceanology I 30 Vol.
Antarctic Oceanology I by Joseph L. (ed) Reid