. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. -10 300 200 400. DEPTH BELOW TOP (CM) Fig. 5. Paleotemperature curves of five deep-sea cores, determined by means of oxygen- - isotopic analysis. Core numbers to the right. Arrows indicate last occurrence of Olohorotalia menardii flexuosa. Core 280, North Atlantic (34° 57'N, 44° 16'W, 4256 m); core 234, equatorial Atlantic (5° 45'N, 21° 43'W, 3577 m); core 246, equatorial Atlantic (0° 48'N, 31° 28'W, 3210 m); core A240-M1, Caribbean (15° 26'N, 68° 30'W, 4180 m); core A179-4, Caribbean (16° 36'N, 74° 48'W, 2965 m).. Please
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. -10 300 200 400. DEPTH BELOW TOP (CM) Fig. 5. Paleotemperature curves of five deep-sea cores, determined by means of oxygen- - isotopic analysis. Core numbers to the right. Arrows indicate last occurrence of Olohorotalia menardii flexuosa. Core 280, North Atlantic (34° 57'N, 44° 16'W, 4256 m); core 234, equatorial Atlantic (5° 45'N, 21° 43'W, 3577 m); core 246, equatorial Atlantic (0° 48'N, 31° 28'W, 3210 m); core A240-M1, Caribbean (15° 26'N, 68° 30'W, 4180 m); core A179-4, Caribbean (16° 36'N, 74° 48'W, 2965 m).. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Hill, M. N. (Maurice Neville), 1919-. New York : Interscience Pub.
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Keywords: ., bookcentury1900, bookcollectionbiodivers, booksubjectoceanbottom
