Paleoecology and Sedimentation in Part of the Arctic Basin

Sedimentary regimes in Arctic's Amerasian and Eurasian Basins: Clues to differences in sedimentation rates

“…The T-3 cores were split up into 15-cm-long segments upon recovery and the paleomagnetic polarity was determined from 2 cm samples taken at 5 cm intervals in each segment (Steuerwald et al, 1968;Clark, 1969). Unfortunately, only the interpreted zones of paleomagnetic polarity directions are available because the measurements were never published for the T-3 cores, nor were any intensity, declination or inclination values calculated (Darby, 1989).…”

Late Quaternary Climatic Changes: Evidence from Deep-Sea Cores of Norwegian and Greenland Seas

“…(4) Much climatic work has been done in the regions surrounding the Norwegian Sea. Arctic Ocean sediments have been studied by Be (1960), Clark (1969Clark ( , 1970, Darby (1971), Ericson and others (1964a), Mullen and others (1972), Steuerwald and others (1968), Steuerwald and Clark (1972), and others. The deep-ice core from Camp Century, Greenland, reveals a climatic record spanning what may be more than 100,000 yr (Dansgaard and others, 1971).…”

Arctic Paleo-Oceanography in Late Cenozoic Time

“…Reinterpretation of the paleomagnetic data of core 224, upon which my time scale was based, by Clark (6) suggests that the earlier paleomagnetic ages (7,8) were apparently overestimated. Consequently, a modified chronology for the T3 Alpha Rise cores has been presented (3,4); according to the new data, the time interval represented by the longest core, T3-67-12, exceeds 3 million years.…”