Languages

antartica

English

Ocean Acidification destroying Antarctic marine life

 

Ocean Acidification destroying Antarctic marine life
The Southern Ocean
 
The research took place in the Southern Ocean
 

Marine snails in seas around Antarctica are being

affected by ocean acidification, scientists have found.

An international team of researchers found that the snails' shells are being

corroded.

Experts says the findings are significant for predicting the future impact of

ocean acidification on marine life.

The results of the study are published in the journal Nature Geoscience.

The marine snails, called "pteropods", are an important link in the oceanic

food chain as well as a good indicator of ecosystem health.
 

"They are a major grazer of phytoplankton and... a key

prey item of a number of higher predators - larger plankton, fish, seabirds,

whales," said Dr Geraint Tarling, Head of Ocean Ecosystems at the British

Antarctic Survey (BAS) and co-author of the report.

The study was a combined project involving researchers from the BAS, the

National Oceanic and Atmospheric Administration (NOAA), the US Woods Hole

Oceanographic Institution and the University of East Anglia's school of

Environmental Sciences.

Ocean acidification is a result of burning fossil fuels: some of the

Methane greenhouse gas to be released from Antartica

Antarctic may host methane stores

[[{"type":"media","view_mode":"media_crop","fid":"127","attributes":{"alt":"","class":"media-image","id":"media_crop_6810678576135","media_crop_h":"0","media_crop_image_style":"-1","media_crop_instance":"17","media_crop_rotate":"0","media_crop_scale_h":"0","media_crop_scale_w":"0","media_crop_w":"0","media_crop_x":"0","media_crop_y":"0","typeof":"foaf:Image"}}]]

 
Ancient organic matter could be converted to methane by microbes.
 

Large volumes of methane - a potent

greenhouse gas - could be locked beneath the ice-covered regions of Antarctica,

according to a new study.

It says this methane could be released into the atmosphere as ice retreats,

contributing to climate warming.

The findings indicate that ancient deposits of organic matter may have been

converted to methane by microbes under the ice.

An international team reported the results in Nature journal.

Study leader Jemima Wadham, from Bristol University, said: "This is an

immense amount of organic carbon, more than ten times the size of carbon stocks

in northern permafrost regions.

"Our laboratory experiments tell us that these sub-ice environments are also

biologically active, meaning that this organic carbon is probably being

metabolised to carbon dioxide and methane gas by microbes."

They estimate that there could be hundreds of billions of tonnes of carbon

Email Addresses