Reply on RC1

Abstract

Marine plankton is an important component of the global carbon cycle. Whereas the production and seafloor export of organic carbon produced by the plankton, the biological pump, has received much attention, the long-term variability in plankton calcification, controlling the carbonate counter pump, remains less well understood. Yet, it has been shown that on geological time scales, changes in pelagic calcification (biological compensation) could affect the ocean's buffering capacity and thus regulate global carbon budget. Here we use Neogene pelagic sediments deposited on the Ceara Rise in the tropical Atlantic to characterise the variability in pelagic carbonate production with focus on warm climates. A re-evaluation of published records of carbonate accumulation at Ceara Rise reveals a systematic increase in sedimentation rates since the late Miocene, but the carbonate accumulation rate does not show a clear trend. Instead, we observe substantial orbital time-scale variability in carbonate accumulation and an effect of carbonate preservation, especially at sites located below 4 km. To evaluate long-term changes against possible orbital-scale variability, we generated new high-resolution records of carbonate accumulation rate at ODP Site 927 across two Quaternary interglacials (MIS 5 and MIS 9), the Pliocene warm period (MIS KM5) and the Miocene climate optimum (MCO). We observe that the highest carbonate accumulation rates occurred during the Pliocene but that each interval was characterised by large orbital-scale variability. Prominent variations in carbonate accumulation prior to the Quaternary preservation cycles appear to follow obliquity and eccentricity. These results imply that pelagic carbonate production in the tropical ocean, buffered from large temperature changes, varied on orbital time scales similarly or even more than on longer time scales. Since preservation can be excluded as a driver of these changes prior to the Quaternary, the observed variations must reflect changes in the export flux of pelagic biogenic carbonate. We conclude that the overall carbonate production by pelagic calcifiers responded to local changes in light, temperature and nutrients delivered by upwelling, which followed long orbital cycles, as well as to long-term shifts in climate and/or ocean chemistry. The inferred changes on both time scales were sufficiently large such that when extrapolated on a global scale, they could have played a role in the regulation of the carbon cycle and global climate evolution during the transition from the Miocene warm climates into the Quaternary icehouse.