As Konradv has already pointed out, this article is hardly one that a denialist should pick to post. But then, as we have seen in the past, Walleyes has a problem with reading comprehension.
New evidence that it was once possible to sail acrossAntarctica - Journal - Your Site Name
"When we found groups of strikingly similar bryozoans hundreds of miles apart we knew we were onto something very interesting. Perhaps these species had survived the last ice age whereas in all other regions of Antarctica they were wiped out. We know that after the last ice age groups of bryozoans dispersed freely between many of the regions we studied. But because the larvae of these animals sink and this stage of their life is short and the adult form anchors itself to the seabed it's very unlikely that they would have dispersed the long distances carried by ocean currents. For the bryozoans on both the Weddell and Ross sea continental shelves to be more similar to one another than to any of those found in the waters in between is striking indeed. Our conclusion is that the colonization of both these regions is a signal that both seas were connected by a trans-Antarctic seaway in the recent past."
This seaway could have opened up as recently as 125,000 years ago, during an interglacial warm period in which the sea levels were about fifteen feet higher than they are now. We don't know the exact processes that caused this seaway to open up, but they created an opening through what's now over a mile of solid ice.
The ancient seaway also calls into question how stable Antarctica's ice is today.
The West Antarctic Ice Sheet, which is the region through which this trans-Antarctic seaway must have traveled, is thought to be unstable and in danger of collapsing, partially as a result of climate change. If the ice sheet does collapse, it could increase global sea levels by 10 to 15 feet, which could displace billions of people from their homes. The bryozoan discovery could, however, help us better understand how a melting Antarctica fits into current climate change. Barnes explains:
"The West Antarctic Ice Sheet can be considered the Achilles heel of Antarctica and because any collapse will have implications for future sea level rise it's important that scientists get a better understanding of big deglaciation events. This biological evidence is one of the novel ways that we look for clues that help us reconstruct Antarctica's ice sheet history. Our new research provides compelling evidence that a seaway stretching across West Antarctica could have opened up only if the ice sheet had collapsed in the past."
........................................................................................
At the maximum of the last interglacial, the CO2 level was at 300 ppm. Today it is at 387 ppm, and rising fast. The CH4 level was at about 700 ppb. Today it is at 1800 ppb. And rising even faster than the CO2 rate of change.