Seasonal variations in planktonic foraminiferal flux and oxygen isotopic composition in the western North Pacific: Implications for paleoceanographic reconstruction

Abstract

The oxygen isotopic composition (δ 18 O) of planktonic foraminiferal shells in seafloor sediment provides information on past surface oceanography. Knowledge of seasonal and depth habitat, as well as the δ 18 O disequilibrium (vital effect), is essential to constrain the interpretation of sedimentary δ 18 O. Here, we present a 1-year time series of planktonic foraminiferal shell fluxes and δ 18 O from a sediment trap moored in the northwestern margin of the North Pacific. The vital effect and calcification depth for four species were estimated by comparing shell δ 18 O and the predicted values of equilibrium calcite calculated from temperature and estimated δ 18 O in seawater. Six major species ( Neogloboquadrina incompta , Neogloboquadrina dutertrei , Neogloboquadrina pachyderma , Globigerina quinqueloba , Globigerina bulloides , and Globorotalia scitula ) constituted 97% of the total foraminiferal flux. Most major species showed large fluxes in June and December, corresponding to periods of the development and disruption of the seasonal thermocline, implying the importance of nutrient injection and/or circulation for foraminiferal fluxes. Additional peaks in N. dutertrei and N. pachyderma were observed in August. The seasonal successions of foraminiferal fluxes corresponded to surface ocean stratification conditions and food availability, which are closely related to circulation of local currents. Vital effect estimations suggest that shells calcified in equilibrium for G. bulloides and N. pachyderma [sinistral (s)] and with a − 0.7‰ offset for N. dutertrei [dextral (d)], a − 1.0‰ offset for N.incompta (d), and a − 0.3‰ offset for N. pachyderma (d). The calculation of flux-weighted δ 18 O values reveals that the sedimentary δ 18 O values of G. bulloides , N. dutertrei (d), and N. incompta (d) reflect surface temperature in winter season, and those of N. pachyderma (s) and N. pachyderma (d) reflect summer and annual mean subsurface temperature, respectively. The shallow calcification depths for the four species suggest that δ 18 O between different species (Δδ 18 O) in the western North Pacific does not work for reconstructing past stratification conditions, unlike in other regions. Rather, the Δδ 18 O between N. pachyderma (s) and G. bulloides , N. dutertrei (d) or N. incompta (d) may be a more suitable proxy for past seasonality. • Seasonal variations in planktonic foraminiferal shell flux and δ 18 O are observed. • Stratification condition plays a major role in shell flux variations. • The δ 18 O vital effects and calcification depths for four species were determined. • Multi-species Δδ 18 O as a proxy of the past seasonality in the western North Pacific.