The Antarctic polar icecap is 33.6 million years old, research finds

May 27, 2013, University of Granada
A typical, simple dinoflagellate associated with the early Oligocene epoch and found in 33 million year-old sediments. Source: IODP

The Antarctic continental ice cap came into existence during the Oligocene epoch, some 33.6 million years ago, according to data from an international expedition led by the Andalusian Institute of Earth Sciences (IACT)—a Spanish National Research Council-University of Granada joint centre. These findings, based on information contained in ice sediments from different depths, have recently been published in the journal Science.

Before the ice covered Antarctica, the Earth was a warm place with a . In this region, plankton diversity was high until glaciation reduced the populations leaving only those capable of surviving in the new climate.

The Integrated international expedition has obtained this information from the paleoclimatic history preserved in sediment strata in the Antarctic depths. IACT researcher Carlota Escutia, who led the expedition, explains that "the of dinoflagellate cyst communities reflects the substantial reduction and specialization of these species that took place when the ice cap became established and, with it, marked seasonal ice-pack formation and melting began".

The appearance of the Antarctic polar icecap marks the beginning of plankton communities that are still functioning today. This ice-cap is associated with the ice-pack, the frozen part that disappears and reappears as a function of seasonal climate changes.

The article reports that when the ice-pack melts as the Antarctic summer approaches, this marks the increase in primary productivity of endemic plankton communities. When it melts, the ice frees the nutrients it has accumulated and these are used by the plankton. Dr Escutia says "this phenomenon influences the dynamics of global primary productivity".

Iceberg in coastal waters off Antarctica. Photo taken in 2010. Source: IODP

Since ice first expanded across Antarctica and caused the dinoflagellate communities to specialize, these species have been undergoing constant change and evolution. However, the IACT researcher thinks "the great change came when the species simplified their form and found they were forced to adapt to the new climatic conditions".

Pre-glaciation sediment contained highly varied dinoflagellate communities, with star-shaped morphologies. When the ice appeared 33.6 million years ago, this diversity was limited and their activity subjected to the new seasonal climate.

Explore further: Sea-ice ecosystem possibly triggered evolution of baleen whales and penguins

More information: Alexander J. P. Houben, Peter K. Bijl, Jörg Pross, Steven M. Bohaty, Sandra Passchier, Catherine E. Stickley, Ursula Röhl, Saiko Sugisaki, Lisa Tauxe, Tina van de Flierdt, Matthew Olney, Francesca Sangiorgi, Appy Sluijs, Carlota Escutia Henk Brinkhuis and the Expedition 318 Scientists. Reorganization of Southern Ocean Plankton Ecosystem at the Onset of Antarctic Glaciation. Science. DOI: 10.1126/science.1223646

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3 / 5 (12) May 27, 2013
Wow, almost as old as denialist talking points!
1.4 / 5 (9) May 29, 2013
Wow, almost as old as denialist talking points!

Yet your stupidity never gets old.
3 / 5 (12) May 29, 2013
Wow, almost as old as denialist talking points!

Yet your stupidity never gets old.

On the other hand, your stupidity grew very old very quickly.
3 / 5 (8) May 31, 2013
Wow, almost as old as denialist talking points!

Yet your stupidity never gets old.

Grasshopper, what does not exist cannot age.

You do a nice job of illustrating the Dunning-Kruger effect, but otherwise... keep your day job.

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