Budgets of organic C (C-org), CaCO3 and opal have been constructed for the Pacific equatorial region at 140 degrees W between 5 degrees N and 5 degrees S. Measurements of the rain and benthic remineralization rate of biogenic materials have been adjusted and normalized to account for sampling biases. Sea surface temperature serves as a master variable in normalizing sediment trap and benthic remineralization data to average conditions. The rain and remineralization rates for C(o)rg are nearly equal: 0.40+/-0.05 and 0.46+/-0.06 mmol m(-2) d(-1), respectively;thus only a minor fraction of this constituent is buried. Rain and dissolution rates for biogenic opal are similarly balanced respectively; thus only a minor fraction of this constituent is buried. Rain and dissolution rates (0.38+/-0.06 and 0.36+/-0.01 mmol m(-2) d(-1)) and consistent with the value for opal burial (0.03+/-0.004). The CaCO3 budget appears to have changed during the Holocene. The best estimates of modern CaCO3 dissolution (0.58+/-0.03 mmol m(-2) d(-1)) and rain rate (0.61+/-0.06) are consistent with Th-230-normalized carbonate accumulation rates for the late Holocene (0.1 mmol m(-2) d(-1)). However, the balance between dissolution and rain is not consistent with early Holocene carbonate accumulation (0.3 mmol m(-2) d(-1)), and this imbalance suggests: 1)a recent increase in the rate of CaCO3 dissolution on the sea floor, or 2) a decrease in the rain rate of carbonate particles. Modeling Th-230 profiles in sediments from this region define the last 3000 years as the duration of increased dissolution or decreased particle rain. Pa-231/Th-230 ratios in sediments indicate that particle rain rates have remained constant or possibly increased slightly through the Holocene. Two potential causes for increased dissolution were investigated; a change in deep water carbonate saturation or a change in C-org/CaCO3 rain ratios. A model describing carbonate dissolution as a function of the degree of undersaturation and the amount of organic carbon oxidation within sediments indicates that the recent increase in dissolution is more likely due to changes in bottom water chemical composition. We propose that Pacific Ocean bottom water carbonate ion concentration has decreased by 10-15 mu M over the last 3000 years. (C) 1998 Elsevier Science Ltd. All rights reserved.
Zt582Times Cited:34Cited References Count:64