Carbon flux to seabirds in waters with different mixing regimes in the southeastern Bering Sea
Carbon flux to seabirds in waters with different mixing regimes in the southeastern Bering Sea
复制标题
白令海东南部不同混合模式水域海鸟的碳通量
DOI:
10.1007/bf00397674
复制
发表时间:
1982
期刊:
影响因子:
2.4
通讯作者:
G. Hunt
中科院分区:
文献类型:
--
作者:
D. Schneider;G. Hunt
The southeastern Bering Sea is characterized by three mixing regimes, separated by fronts associated with the 50, 100, and 200 m isobaths. Phytoplankton to zooplankton transfer-rates are high in waters over the outer shelf and slope (seaward of the 100 m front) relative to transfer in waters over the middle shelf (between the 50 and 100 m fronts). To see whether this difference is reflected at a higher trophic level, we computed carbon flux to the 11 commonest seabird species. Bird-density data (for the period 1975 through 1979) were combined with daily caloric requirement, which is an allometric function of body size in this endothermic group. Minimum transfer to seabirds over a 153 d period (April–August) was 30 mg C m-2for the middle shelf and 48 mg C m-2for outer shelf and slope waters. Trophic transfer to subsurface-feeding birds (shearwaters, murres and auklets) differed little between regions. In contrast, trophic transfer to surface-feeding birds (fulmars, petrels, and kittiwakes) in the outer shelf and slope waters was 3 times greater than in the waters of the middle shelf. Thus, for seabirds as a whole, pathways of energy transfer differed more between regions than did total carbon flux.