| Summary: | Upper Miocene foraminiferal nannofossil ooze and chalk from DSDP Hole 552A in the northeast Atlantic Ocean have been closely sampled for biostratigraphic, paleomagnetic, and stable-isotopic studies. Sampling at 10-cm intervals resulted in an uppermost Miocene isotope stratigraphy with a 1000- to 3000-yr. resolution. Covariance in benthic (Planulina wuellerstorfi) and planktonic (Globigerina bulloides) foraminiferal δ^O¸ records is taken as evidence for variability in continental ice volume. Our best estimate is that glacial maxima occurred at ~ 5.0 and ~ 5.5 Ma and lasted no more than 20,000 yrs. These events probably lowered sea level by 60 m below the latest Miocene average. There is little oxygen-isotope evidence, however, for a prolonged glaciation during the last 2 m.y. of the late Miocene. High- and low-frequency variability in the δ^13C record of foraminifers is useful for correlation among North Atlantic DSDP Sites 408, 410, 522, 610, and 611, and for correlation with sites in other oceans. Similar δ^13C changes are seen in P. wuellerstorfi and G. bulloides, but the amplitude of the signal is always greater in G. bulloides. Variability in δ^13C common to both species probably reflects variability in the δ^13C of total CO2 in seawater. Major long-term features in the δ^13C record include a latest Miocene maximum (P. wuellerstorfi = 1.5‰) in paleomagnetic Chron 7, an abrupt decrease in δ^13C at -6.2 Ma, and a slight increase at -5.5 Ma. The decrease in δ^13C at -6.2 Ma, which has been paleomagnetically dated only twice before, occurs in the upper reversed part of Chronozone 6 at Holes 552A and 611C, in excellent agreement with earlier studies. Cycles in δ^13C with a period of ~ 104 yrs. are interpreted as changes in seawater chemistry, which may have resulted from orbitally induced variability in continental biomass. Samples of P. wuellerstorfi younger than 6 Ma from throughout the North Atlantic have δ^13C near 1‰, on average ~ 1‰ greater than samples of the same age in the Pacific Ocean. Thus, there is ...
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