James P. Kennett


Latest Quaternary oxygen (delta18O) and carbon (delta13C) isotopic records from benthic foraminifers are presented at relatively high chronologic resolution (~450 to 1000 yr) for Hole 893A, a continuous 200-m sediment sequence from Santa Barbara Basin, Southern California. The oxygen isotope stratigraphy records a continuous ~160-k.y. sequence from isotope Stage 6.4 to the present day, the first of its kind from this region of the Pacific Ocean. The oxygen isotopic record, representing the last two interglacial and glacial cycles, closely resembles the well-dated deep sea reference sequence, and thus provides a detailed chronologic framework. Site 893 has much potential for ultra-high-resolution stable isotopic investigations because of the very high sedimentation rates (reaching ~1.6 mm per yr), and greatly reduced bioturbation. Variability of late Quaternary oxygen isotopic change in Hole 893A is distinctly larger during the last glacial episode (~70 to 11 ka), as for the Greenland Ice Sheet, and is considered to reflect significant climatic instability.

Unlike the oxygen isotopic record, carbon isotopic values of each of the benthic foraminifers exhibit relatively little consistent change during the latest Quaternary, and the delta13C record does not resemble the typical records of deep-sea sediments. Instead, the carbon isotopic values are inferred to have been dominated by benthic microenvironments. Offsets in carbon isotopic values between five taxa are maintained throughout the sequence. Uvigerina peregrina curticosta has delta13C values ~2 higher than Bolivina tumida; the other taxa have intermediate values. Our data suggest that Uvigerina peregrina curticosta lives closer to the sediment/water interface in microenvironments inferred to have higher oxygen and organic carbon concentrations. Bolivina tumida lives deeper in the sediment under lower oxygen concentrations. Carbon isotopic values of Uvigerina are similar in both laminated and nonlaminated sediment intervals that represent dysaerobic/aerobic cycles in Santa Barbara Basin. This suggests that surface sediments of the basin continued to be dominated by local dysaerobic processes, even during glacial maxima when oxygen levels in bottom waters increased sufficiently to support bioturbating organisms.

Date of initial receipt: 2 September 1994
Date of acceptance: 8 February 1995

Return to Contents of Leg 146B
Return to Contents of Scientific Results