All scientific data collected by the Australian Antarctic program (AAp) are eventually described in the Catalogue of Australian Antarctic and Subantarctic Metadata (CAASM). CAASM can be used to search through AAp data descriptions, and it also provides links to access publicly available datasets, which can either be immediately downloaded or obtained from the Australian Antarctic Data Centre (AADC).

Citation
McMinn, A. (2005) Phytoplankton and hydrological succession in Omega and Taynaya Bays, eastern Antarctica, Ver. 1, Australian Antarctic Data Centre - doi:10.4225/15/55F0CC41E5C16, Accessed: 2026-06-27
Title
Phytoplankton and hydrological succession in Omega and Taynaya Bays, eastern Antarctica
Data Centre
Australian Antarctic Data Centre, Australia
DOI
doi:10.4225/15/55F0CC41E5C16
Created Date
2000-08-11
Revision Date
2017-04-26
Expected Date of Data Release
2005-06-03
Data Version
1
Parent record
None

Description

Metadata record for data from ASAC Project 2146
See the link below for public details on this project.

From the abstracts of the referenced papers:

Early season phytoplankton communities in both Omega and Taynaya Bays are characterised by diatoms sedimenting out of the overlying sea ice. Initial nitrate, phosphate and silicate levels are high and the bay waters are covered with ice and well mixed. In Taynaya Bay the ice cover is retained throughout the season while Omega Bay is free for 6-8 weeks. After ice break out in Omega Bay, the phytoplankton community changes from one dominated by diatoms to one dominated by the phtyoflagellates, Pyramimonas spp., Cryptomonas sp. and Gymnodinium sp. In Taynaya Bay the ice remained and even though phtyoflagellates became more common, diatoms still dominated. These differences in community composition result from differences in light climate, extent of stratification and nutrient levels.

Sediment cores from Abel and Platcha Bays, in the Vestfold Hills, east Antarctica, contain evidence for a local late Holocene increase in fast ice extent and a possible ice cap retreat at approximately 1750 yr BP, a similar time to the Chelnock Glaciation. Prior to this time both bays experienced periods of isolation that lead to changes in their diatom flora, C:N ratio, percentage of biogenic silica and total organic carbon. Three new diatom indices are proposed; the fast ice index, based on the proportion of benthic taxa and the snow index, based on the proportion of Berkelaya adeliense and Thalassiosira australis. These indices show strong relationships with the percentage of biogenic silica, total organic carbon and percentage sand. A weak relationship exists between the fast ice index and delta 13 C and no relationship with the C:N ratio.

The fields in these datasets are:

Date
Julian Day
Sample
Volume filtered (L)
Acetone Volume (ml)
Abs
Chlorophyll
Phytoplankton

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Access

These data are publicly available for download from the provided URL.

Copies of some of the referenced papers are available for download to AAD staff only.

Temporal Coverages

Spatial Coverages

Science Keywords

Additional Keywords

  • ABS
  • ACETONE
  • CHLOROPHYLL
  • CHLOROPHYLL A
  • DATE
  • DIATOMS
  • JULIAN DAY
  • NUTRIENTS
  • PHYTOPLANKTON
  • PIGMENTS
  • SALINITY
  • SAMPLE
  • SUCCESSION
  • TEMPERATURE

Locations

  • OCEAN > SOUTHERN OCEAN
  • CONTINENT > ANTARCTICA
  • GEOGRAPHIC REGION > POLAR

Platforms

  • FIELD INVESTIGATION
  • FIELD SURVEYS

Instruments

  • SEDIMENT CORERS

Researchers

  • mcminn, andrew (INVESTIGATOR,TECHNICAL CONTACT)
  • connell, dave (DIF AUTHOR)

Use Constraints

This data set conforms to the CCBY Attribution License
(http://creativecommons.org/licenses/by/4.0/).

Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=ASAC_2146 when using these data.

Project

    ISO Topic

    • BIOTA
    • OCEANS

    Dataset Language

    • ENGLISH

    Orignating Centre

    • Australian Antarctic Division

    Dataset Progress

    • COMPLETE

    IDN Node

    • AMD/AU
    • CEOS
    • AMD

    Publications

    • McMinn A. (2000) Late Holocene increase in sea ice extent in fjords of the Vestfold Hills, Eastern Antarctica, Antarctic Science, 12(2), 80-88
    • McMinn A., Bleakley N., Roberts D., Trenerry L. (2000) Effect of permanent sea ice cover and different nutrient regimes on the phytoplankton succession of fjords of the Vestfold Hills Oasis, Eastern Antarctica, Journal of Plankton Research, 22(2), 287-303

    Metadata Revision History

      2010-07-26 - record updated by Dave Connell to change URL Content Type. 2015-09-10 - record updated by Dave Connell. Basic updates.

    Creative Commons License