The influence of phytoplankton assemblage composition on biogeochemical characteristics and cycles in the southern Ross Sea, Antarctica

• Published in: Deep-sea research. Part I, Oceanographic research papers Vol. 48; no. 1; pp. 137 - 161
• Main Authors: Smith, Walker O, Asper, Vernon L
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 2001; Elsevier; Pergamon Press Inc
• Subjects: Animal and plant ecology; Animal, plant and microbial ecology; Antarctica; Biochemistry; Biological and medical sciences; Carbon; Diatoms; Ecosystems; Fundamental and applied biological sciences. Psychology; Life cycles; Marine; Nitrogen; Phaeocystis; Phaeocystis antarctica; Phytoplankton; Pigments; Plankton; Polynya; Ross Sea; Sea water ecosystems; Synecology; Ross Sea; Southern Ocean; PS, Ross Sea; Phaeocystis; Pigments; Phytoplankton; Ross Sea; Antarctica; Nitrogen; Diatoms; Polynya; Carbon; Community structure; Floristic composition; Algae; Biogeochemical cycle; Marine environment; Heterokontophyta; Bacillariophyta; Thallophyta
• ISSN: 0967-0637; 1879-0119
• DOI: 10.1016/S0967-0637(00)00045-5

To test the hypothesis that phytoplankton assemblages dominated by different taxa have distinct biogeochemical characteristics and cycles, the temporal and spatial variations in phytoplankton biomass and composition were studied within the Ross Sea polynya, where diatoms and the haptophyte Phaeocystis antarctica are thought to have spatially distinct distributions. Two cruises were completed, with the first conducted in spring, 1994, and the second in late spring–early summer, 1995/1996. Ice concentrations decreased substantially from spring to summer. Mixed layer depths for the region decreased markedly in early spring and were relatively invariant thereafter; the strength of the stratification varied both in time and space. Mixed layers were greater in spring in assemblages dominated by diatoms (as determined by HPLC pigment concentrations) than those dominated by Phaeocystis antarctica, whereas in summer no difference was observed. Nutrient concentrations were initially high and near winter values, but decreased throughout November and December. Nitrate : phosphate removal ratios varied widely, with ratios exceeding 20 in spring but decreasing below 14 in summer. N : P removal ratios at stations dominated by diatoms were less than the Redfield ratio in both spring and summer, and at those stations dominated by P. antarctica the N : P removal ratio was ca. 19 in both seasons. Chlorophyll and particulate matter concentrations increased as nutrients decreased. Spatial and temporal variations of phytoplankton pigments occurred, with 19′-hexanoylfucoxanthin, a pigment of P. antarctica, exceeding 3.9 μg l −1 during spring in the south-central polynya, and fucoxanthin, an accessory pigment of diatoms, found in concentrations >1 μg l −1 in the western Ross Sea. The distributions were not mutually exclusive, and concentrations of both pigments were greatest in spring. The early growth of P. antarctica appears to be related to earlier stratification and disappearance of ice from the south-central Ross Sea. Ratios of FUCO/CHL were relatively invariant, but substantial changes in the HEX/CHL and POC/CHL ratios were observed through time. A one-dimensional nitrogen budget for the spring–early summer period suggests that much of the surface production was partitioned into particles, most (53%) of which remained in the upper 200 m. The rest was partitioned into dissolved organic matter (14%), remineralized as ammonium (19%), or sank from the surface layer as particles (13%). The region may serve as a useful analog to other polar systems, and an understanding of the processes controlling assemblage composition, production, and biomass accumulation may provide insights into biogeochemical cycles of other Antarctic environments.