State of the Environment

2006

Indicator: AAT-08 Plankton populations

Data

Seasonal changes in total zooplankton abundance

Seasonal changes in total zooplankton abundance

Source: Hosie, G.W, Fukuchi, M. & Kawaguchi, S 2003, Development of the Southern Ocean Continuous Plankton Recorder Survey

Latitudinal change in total zooplankton abundance (November to February)

Latitudinal change in total zooplankton abundance (November to February)

Source: Hosie, G.W, Fukuchi, M. & Kawaguchi, S 2003, Development of the Southern Ocean Continuous Plankton Recorder Survey

What the data mean

The data relating to seasonal changes in total zooplankton abundance shows that there are lower abundances of plankton during the winter months, with the lowest values in August. Abundances peak through November to February. Scientists noted that most of the data for 1999-2000 was well above the average whereas that for 2000-01 was consistently lower (Hosie et al, 2003).

The latitudinal change data showed that there was marked differences in abundance across latitudes. Low abundances were found in the Sub-Antarctic Zone (SAZ) north of the Sub-Antarctic Front (SAF), and in the sea-ice zone south of the Southern Antarctic Circumpolar Front (SACCF). Species diversity was also lowest in the sea-ice zone. Highest abundances were found in the area between SACCF and SAF and the region between the Polar Front (PF) and SACCF (Hosie et al, 2003).

Future surveys and analysis of data will provide trend data.

Source: Hosie, G.W, Fukuchi, M. & Kawaguchi, S. 2003, Development of the Southern Ocean Continuous Plankton Recorder Survey.

Data Limitations

Forty years of surveying will be required to make an assessment of true interannual and interdecadal patterns. Another 5 to 10 years of sampling will be needed before any assessment could be made on biodiversity and associated spatial patterns.

Issues for which this is an indicator and why

Australian Antarctic Territory — Environment - Marine ecosystems 

Antarctica and surrounding waters are expected to be particularly sensitive and vulnerable to climate change. Zooplankton may respond to climatic forcing and may be sensitive to slight increases in UV levels and changes in other environmental conditions such as circulation patterns, sea-ice cover and pollution. In addition, plankton are an important part of the food web and therefore monitoring the number and composition of plankton is vital.

Other indicators for this issue:

Biodiversity — Species, habitats and ecological communities - Conservation status of species and ecological communities 

Plankton are an important part of the food web and therefore monitoring the number and composition of plankton is vital to understanding pressures on biodiversity not just in the AAT but throughout the world’s oceans.

Other indicators for this issue:

Biodiversity — Species, habitats and ecological communities - Condition of marine biodiversity: Condition of species, habitat and ecological communities 

Plankton are an important part of the food web and therefore monitoring the number and composition of plankton is vital to understanding the condition of marine biodiversity not just in the AAT but throughout the world’s oceans.

Other indicators for this issue:

Coasts and Oceans — Condition of the ocean and coastal waters - Condition of species, habitats and ecosystems 

Plankton are an important part of the food web and therefore monitoring the number and composition of plankton is vital to understanding the condition of marine biodiversity not just in the AAT but throughout the world’s oceans.

Other indicators for this issue:

Further Information

Key

   Links to another web site
   Links to data in the DRS
   Opens a pop-up window

PDF files

Adobe Acrobat Reader  is required to view PDF files.

If you are unable to access a PDF file, please contact us to organise a suitable alternative format.