Spring Phytoplankton Assemblages in the Southern Ocean Between Australia and Antarctica

This dataset comprises of an excel spreadsheet of data collected on the CLIVAR-SR3 cruise in November to December 2001.  The spreadsheet contains plankton and carbon data.
From the abstract of the referenced publication:
Variations of phytoplankton assemblages were studied in November-December 2001, in surface waters of the Southern Ocean along a transect between the Sub-Antarctic Zone (SAZ) and the Seasonal Ice Zone (SIZ; 46.9-64.9 degrees S; 142-143 degrees E; CLIVAR-SR3 cruise).  Two regions had characteristic but different phytoplankton assemblages.  Nanoflagellates (less than 20 microns) and pico-plankton (~2 microns) occurred in similar concentrations along the transect, but were dominant in the SAZ, Sub-Antarctic Front (SAF), Polar Front Zone (PFZ) and the Inter-Polar Front Zone (IPFZ), (46.9-56.9 degrees S).  Along the entire transect their average cell numbers in the upper 70 m of water column, varied from 300,000 to 1,100,000 cells per litre.  Larger cells (greater than 20 microns), diatoms and dinoflagellates, were more abundant in the Antarctic Zone-South (AZ-S) and the SIZ (60.9-64.9 degrees S).  In AZ-S and SIZ diatoms ranged between 270,000 and 1,200,000 cells per litre, dinoflagellates from 31,000 to 102,000 cells per litre.  A diatom bloom was in progress in the AZ-S showing a peak of 1,800,000 cells per litre.  Diatoms were dominated by Pseudo-nitzschia spp., Fragilariopsis spp., and Chaetoceros spp.  Pseudo-nitzschia spp. outnumbered other diatoms in the AZ-S.  Fragilariopsis spp. were most numerous in the SIZ.  Dinoflagellates contained autotrophs (eg Prorocentrum) and heterotrophs (Gyrodinium/Gymnodinium, Protoperidinium).  Diatoms and dinoflagellates contributed most to the cellular carbon: 11-25 and 17-124 micrograms of carbon per litre, respectively.  Small cells dominated in the northern region characterised by the lowest N-uptake and new production of the transect.  Larger diatom cells were prevalent in the southern area with higher values of N-uptake and new production.  Diatom and nanoflagellate cellular carbon contents were highly correlated with one another, with primary production, and productivity related parameters.  They contributed up to 75% to the total autotrophic C biomass.  Diatom carbon content was significantly correlated to nitrate uptake and particle export, but not to ammonium uptake, while flagellate carbon was well correlated to ammonium uptake, but not to export.  Diatoms have contributed highly to particle export along the latitudinal transect, while flagellates played a minor role in the export.
This work was completed as part of ASAC project 1343 (ASAC_1343).
The fields in this dataset are:
Station (depth, position, date, comments)
Species
Cells per millilitre
cell carbon - micrograms per litre

Tags: AMD, AMD/AU, Aurora Australis, CEOS, CONTINENT > ANTARCTICA, CTD, CTD > Conductivity, Temperature, Depth, EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > PLANTS > MICROALGAE > DIATOMS, EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > PROTISTS > DIATOMS, EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > PROTISTS > FLAGELLATES > DINOFLAGELLATES, EARTH SCIENCE > BIOSPHERE > ECOSYSTEMS > AQUATIC ECOSYSTEMS > PLANKTON > PHYTOPLANKTON, EARTH SCIENCE > BIOSPHERE > ECOSYSTEMS > AQUATIC ECOSYSTEMS > PLANKTON > ZOOPLANKTON, EARTH SCIENCE > BIOSPHERE > VEGETATION > CARBON, EARTH SCIENCE > OCEANS > OCEAN CHEMISTRY > CARBON, GEOGRAPHIC REGION > POLAR, NISKIN BOTTLES, OCEAN > SOUTHERN OCEAN, R/V AA > R/V Aurora Australis, SHIPS, assemblages, carbon, phytoplankton, plankton
Organization: Australian Ocean Data Network