Vertical, spatial, size, and taxonomic variations in stable isotopes (δ13C and δ15N) of zooplankton and other pelagic organisms in the western North Pacific

Stable isotopes (δ13C and δ15N) of zooplankton and other marine organisms are useful for evaluating trophic levels and the food web structure of marine ecosystems. Further, taxonomic variations and regressions between δ15N and δ13C can provide details of regional differences in the food web structure. Despite their ecological importance, information on the taxonomic differences in the stable isotopes of various pelagic biota and vertical, latitudinal, and size variations in the stable isotopes of the mesozooplankton are scarce in the western North Pacific. In this study, we compared regional differences in the taxonomic variations of the stable isotopes of the all pelagic organisms collected by gillnets and various plankton nets in the subarctic and transitional domains (37–44°N) of the western North Pacific during spring. Additionally, we evaluated the vertical, size, and latitudinal variations in the stable isotopes of mesozooplankton in the western North Pacific. Regressions between δ15N and δ13C were highly significant for the subarctic and transitional domains, while they varied significantly between the two regions (P < 0.0001, ANCOVA). These regional differences in the stable isotopes were characterised by the high δ15N and low δ13C values in the subarctic region, whereas the opposites trend was observed in the transitional domains. Vertical observations from the sea surface to a depth of 3000 m at five stations (29°, 31°, 33°, 37°, and 41°N) showed that there were no significant changes in the δ13C stable isotope of mesozooplankton with depth across the stations. However, for δ15N, the significance of regressions increased with increasing depths at the subtropical stations (29°, 31°, and 33°N), while no significant trends with depth were observed for the subarctic and transitional domain stations (37°, 41°N). The dominance of interzonal copepods (e.g., Neocalanus spp.) in the mesozooplankton biomass in the subarctic and transitional region may mask the vertical changes in δ15N values in that region. Further, δ13C varied neither with size nor latitude. In contrast, δ15N showed clear size and latitudinal patterns. Thus, δ15N values increased with increasing zooplankton size (112 μm < 407 μm < 925 μm), and significant regressions increased with increasing latitude for all three size classes (P < 0.001). Subsequent ANCOVA revealed that the regression did not vary with organism size. Thus, the changing latitudinal patterns in δ15N values (higher for high latitude) had much greater effects than the size differences for mesozooplankton.