This page has been marked as archived, and is here for historical reference only.
Information provided may be out of date, and you are advised to check for newer sources in this section.
This content may be removed at a later date.
IceCUBE - Antarctic coastal marine ecosystems
IceCUBE (Coastal Underwater Benthic Ecosystems) is the umbrella name for our coastal marine research project that had its first field year in 2001/02. The project aims to understand the structure and functioning of Antarctic coastal benthic (seafloor) ecosystems, and better predict responses to future environmental change.
We are particularly interested in how seafloor communities are influenced by large-scale environmental drivers such as sea ice. This understanding will enable us to better predict the response of this unique ecosystem to environmental change, including warming and acidification.
The coastal zone of the Ross Sea is one of the least modified on earth and offers unique opportunities to study natural ecosystems. The seafloor in this region contains an amazing diversity and density of organisms. These are often very slow-growing and long-lived, and their populations are therefore slow to recover from disturbance. The integrity of this region is potentially under threat from the increasing pressures of global climate change and other anthropogenic influences, such as fishing and tourism.
The Ross Sea coastline spans several degrees of latitude – from McMurdo Sound in the south, where Scott Base is situated (at around 77oS), to Cape Adare in the north (at 72oS). Environmental conditions vary along this latitudinal gradient and can influence seafloor communities. These include:
- water temperature
- disturbance by ice (including anchor ice and icebergs)
- sea ice (extent, persistence, and thickness)
For instance, sea ice conditions affect how much light is available for phytoplankton and other microscopic plants to grow. This affects the food supply for seafloor organisms.
The goal of our Ross Sea research is to better understand the structure (what’s actually there – the diversity of organisms, ecosystems, and habitats) and function (how different species interact with each other and their habitat) of coastal seafloor communities. Our overarching hypothesis is that ice dynamics influence the structural and functional properties of coastal seafloor communities along the latitudinal gradient of the western Ross Sea coast.
We compare coastal seafloor ecosystems at different places along this coastline that differ in ice cover, light intensity, and circulation, and thus productivity (see graphic right). This will give us new information on links between animals and their environment, including feeding relationships.
Methods: Using dive surveys and remote video techniques, we conduct surveys of seafloor habitats and communities, and sample key organisms to determine spatial and temporal variation and trophic linkages [e.g., via isotopic signatures (see below)]. We also conduct experiments, both in the laboratory back in New Zealand, and in situ under the ice, to understand potential effects of future warming and ocean acidification on key species and on natural, intact ecosystems.
Location: Various places along the Ross Sea coastline, from McMurdo Sound to Cape Adare (see map right).
Applications: Understanding what makes these ecosystems tick will help us to better predict how they will respond to environmental change, such as that resulting from fisheries, tourism, and climate change.
Links: This research is part of Antarctica New Zealand's previous Latitudinal Gradient Project (LGP), and was an International Polar Year (IPY) project (#1216 'Ross Sea coastal benthic ecosystems') within key IPY project #137 ‘Evolution and Biodiversity in the Antarctic’ (EBA). It is currently linked to one of SCAR's new biology programmes, AnT-ERA (Antarctic Thresholds – Ecosystem Resilience and Adaptation).
- AnT-ERA (Antarctic Thresholds – Ecosystem Resilience and Adaptation
- Latitudinal Gradient Project (LGP)
- Ross Sea coastal benthic ecosystems
- Evolution and Biodiversity in the Antarctic
In 2009 we had NZ Royal Society Teacher Fellow Trisha Korth with us on the ice.
Current funding: Royal Society of New Zealand Marsden Fund and NIWA.
Stable isotopes are great tools for studying food web linkages, particularly in environments where simply sitting and watching interactions between organisms is not an option. Tissues of organisms contain carbon and nitrogen, which they get through their diet. Isotopic signatures of this carbon and nitrogen provides information about where in the food chain an organism sits.
- Cummings, V., Thrush, S. 2011. Massive icebergs and Antarctic ecosystems. Antarctic 29(1): 20-21.
- Wishart, S. 2010. Deep freeze: science under the ice. New Zealand Geographic 105: 70-79.
- Budd, R.G. 2010. Dive Antarctica. Fishing Coast to Coast New Zealand 56: 126 - 127. August.
- Budd, R.G. 2010. Ice Diving. Antarctic 28(3 & 4): 46-50.
- Cummings, V.J., Lyver, P., Metcalf, V., Ryan, K., Sewell, M. 2010. Marine research in the LGP. Antarctic 28(2): 30-33.
- Water & Atmosphere 16(1) 2008, p 4. 'Update from IceCUBE'
- Water & Atmosphere 16(1) 2008, p 27. 'Under the ice with Rod Budd'
- Aquatic Biodiversity & Biosecurity Update 26, Feb 2008. 'Sea ice effects on Ross Sea food webs'
- Water & Atmosphere 13(3), 2005, pp 24-25. 'Life beneath the ice'
- Water & Atmosphere 11(3) 2003, pp 10-12. 'Assessing biodiversity on the Antarctic sea floor'
- Water & Atmosphere 11(3) 2003, pp 14-15. 'Life in the dark: plant growth beneath the sea ice'