Thursday, January 10, 2013
Antarctica Braces for Influx of Invasive Species
Antarctica and the Southern Ocean may seem very far away from civilization, but they are at great risk of losing their unique qualities due to human activities. Warmer temperatures and human visitation are increasing the likelihood that invasive species can take up residence in the Antarctic, and potentially cause major changes. Two studies have found evidence of invasions both on land (from a midge) and at sea (from crabs). The remoteness of the Antarctic can no longer protect it from potentially destructive invaders. Forget about The Thing – the scariest alien invaders in the Antarctic come from our own planet.
Concern about a possible crab invasion of Antarctica began in 2007, when ecologist Sven Thatje saw a few king crabs on the outer continental slope of the Antarctic Peninsula. Their presence raised immediate alarms. Unlike more famous invaders like lionfish or brown tree snakes, crabs have yet to gain notoriety as ecosystem destroyers. But in the Antarctic, cold water has long kept out crustaceans like crabs and lobsters, which cannot survive at temperatures below 1°C (just under 34°F). The result is that many seafloor creatures in the Southern Ocean today have not evolved the same defenses against crushing claws as species in other regions. So the discovery of Neolithodes yaldwyni, a species of king crab, by a submersible surveying shallower areas closer to the Antarctic Peninsula (one of the fastest warming areas in the world) was unwelcome news. This indicates that the crabs are more firmly established, and have become truly invasive. The researchers who discovered the crabs estimate that there are 1.5 million crabs in the Palmer Deep. As warming of ocean water increases, the range of these crabs will expand further.
On land, researchers have also recently found evidence of unwelcome invaders that could make life very difficult for native species. This time, the invading species is the midge Eretmoptera murphyi, and they appear to be speeding up the rate at which decay occurs in Antarctic soil. The midge hails from the sub-Antarctic South Georgia Island, but the ecosystem on that island is very different from the one on the Antarctic Peninsula, where the midge has now established itself. Decay in peninsular soil is “not very active,” according to Peter Convey, one of the scientists who discovered the presence of the midge, so the insect will introduce a new process to the ecosystem. Unfortunately for the peninsula, though its ecosystem is composed of different species, the midge can still survive in its climate. Although one tiny insect might not seem to be very disruptive on a continent without many terrestrial species, it has been well established that many Antarctic species are highly vulnerable to disturbances, so introducing a new ecosystem process could introduce a major shift.
Unlike the crab invasion, however, the midge invasion and other invasions of land species can be slowed or prevented by following strict rules that reduce the possibility that species can tag along with humans visiting different areas of the Antarctic. Even so, it’s virtually impossible to eliminate the transfer of invasive species entirely. In the sea, it will be very difficult to slow down the global warming that allows new species to colonize the Southern Ocean, so we will have to wait and see if a crustacean-generated apocalypse occurs for Antarctica’s unique seafloor communities. The presence of these invaders, it seems, only further indicates that humans have impacted the environment in virtually every place on earth, with possibly disastrous results for the world’s biodiversity.
The growing problem of invasive species is yet another reason to designate marine protected areas (MPAs) in Antarctica as soon as possible. By restricting some types of human activities, MPAs provide reference areas that can be compared with areas where activities aren’t restricted, thus helping scientists understand what ecosystem changes are caused by invasive species or climate change versus those caused by fishing or pollution. MPAs can also minimize some human-induced stressors on threatened ecosystems. Unfortunately, MPAs can’t keep king crabs out, but they can help scientists obtain a better grasp on the seismic changes taking place in the frozen south.
Friday, May 6, 2011
Ozone hole over Antarctica makes it rain in the tropics
Thursday, April 28, 2011
The Ups and Downs of Krill
"The lack of sea ice is good news for the whales in the short term, providing them with all-you-can-eat feasts as the krill migrate vertically toward the bay's surface each night. But it is bad news in the long term for both species, and for everything else in the Southern Ocean that depends on krill," says Ari S. Friedlaender, co-principal investigator on the project and a research scientist at Duke.
Wednesday, March 9, 2011
A Better Understanding of Climate Change
According to the Alfred Wegner Institute (AWI) for Polar and Marine Research, there may be more to long-standing theories regarding ice ages and climate change. In a recent submission to the journal Nature, three scientists from AWI’s working group “Dynamics of the Palaeoclimate” show new findings on the linkage between long-term changes in the global climate and natural insolation.
Analyzing temperature reconstructions based on ice cores removed from Antarctica, the AWI scientists took into account, for the first time, that winter temperatures have a greater influence than the summer temperatures in the recorded signal in the ice cores. Including this factor allows scientists to reconstruct temperature changes isolated to the southern hemisphere.
So what? Up to now, there has been no proven linkage between climate activity in the northern hemisphere and that of the southern hemisphere. Scientists originally postulated that temperature and climate change varied greatly with the constant slow change of the earth’s axis. This new data allows scientists to gain a better understanding of the effects of long-term physical mechanisms that influence the alterations of ice ages and warm periods.
The new data from ice cores has been corroborated by marine sediments, which also display similar seasonal shifts. According to the AWI physicists, these new high quality data and climate models may provide insights into the dynamics of climate change. This will allow us to better gage how the Earth’s climate change cycles have worked in the past and what we may expect into the future. The AWI scientists note however that they did not bring to account any possible anthropogenic climate change catalysts, in their study.
Thursday, February 17, 2011
Martha T. Muse Prize
Nominations recently opened up for the Martha T. Muse Prize for Science and Policy in Antarctica. This honor is awarded to individuals who show clear potential for sustained and significant contributions that enhance our understanding of Antarctic issues and promote Antarctica’s preservation.
Last year’s winner, Helen Amanda Fricker, was recognized for her work with iceberg calving and basal melting and freezing, which has major global climate change implications. She is also known for her work with the hydrology of Antarctica’s subglacial lake systems. Steven Chown, the first prize-winner, was recognized for his research on the effects on Antarctica from humans, climate change and invasive species.
You can learn more about the prize here.
Wednesday, December 1, 2010
Better Understanding the Implications of Ice Melt in the Antarctic
Surprisingly, as of late, issues concerning ice berg ‘calving’ have not played a major role in producing sea-level rise estimates as a result of climate change. Calving is the release or breaking off of a mass of ice from a glacier, ice berg, or other large ice formations. Thanks to the efforts of Dr. Jeremy Bassis and his colleagues, the role of calving will be better understood.
Dr. Bassis, of the University of Chicago’s Department of Atmospheric, Oceanic and Space Sciences, says that “Current models cannot predict about half of the sea ice balance." It appears that even though calving is connected with the speed-up of the ice-retreat process, the scientific community remains unclear as far as to what extent.
Bassis and his colleagues are working on a statistical methodology that allows them to predict the average iceberg calving rate and what different icy regions can expect in the years and decades to come as a result of climate change. Through this we should be able to have a better of idea of what icy areas will experience the greatest amount of melt, in the years to come, and we will have a more accurate picture of the global implications.
In a nutshell, as predictions state that sea level could rise anywhere from four inches to two and a half feet over the next hundred or so years, Bassis is working to narrow that wide margin, by better understanding calving’s contribution to sea level rise. With so much of the world’s population living near the coast, this is an imperative avenue of study.
Tuesday, November 9, 2010
Everybody loves Adelies
Wednesday, August 4, 2010
New penguin species added to endangered species list
Monday, May 17, 2010
"Does anyone wish to address the comma?"
Wednesday, March 24, 2010
A bellwether for climate change
Scientist Joseph Torres is providing dispatches from Antarctica, where he's studying the disappearance of the Antarctic silverfish and the resulting effect on other animals. The decline is thought to be due to global warming. Silverfish are like krill in that many animals eat them (see a graphic of the silverfish's role in the food web here). Dr. Torres thinks that the fish are a bellwether for climate change - if silverfish go, other parts of the food web may be next. TampaBay.com has put together a very thorough overview of this issue and you should definitely check out the site.
Friday, March 5, 2010
Bill Gates in Antarctica
Thursday, February 4, 2010
No good news on ocean acidification
Below is a video about the research:
Oceans Reveal Further Impacts of Climate Change, Says UAB Expert from uabnews on Vimeo.
Friday, December 11, 2009
Congratulations to Dr. Steven Chown...
Prof. Chown has been studying Antarctica and sub-Antarctic ecology for the better part of twenty years. He and his team have not only demonstrated that substantial numbers of seeds actually enter the region, but also that many of them are from species typically known to be invasive elsewhere on the planet. They have also been able to demonstrate how simple interventions concerning proper warehousing, cleaning of clothing and different shipping routes can greatly reduce the risks and problems associated with the transfer of invasive species to the region.
The Martha T. Muse prize brings him well-earned recognition and an award of $100,000. We wish him the best in continuing his research on this most important issue so we may keep Antarctica unspoiled.
Friday, October 23, 2009
Prince Albert to Receive Revelle Prize
Tuesday, October 20, 2009
Separating fact from fiction on Antarctic melting
Monday, July 13, 2009
How will animals respond to climate change?
The main findings of the study, which examined DNA from old elephant seal carcasses found on the Victoria Land Coast (VLC) in the Ross Sea (hooray for Antarctic weather and its remarkable preservation qualities), were that when the VLC became ice-free about 8,000 years ago, elephant seals quickly moved to the area from Macquarie Island. When the ice returned, some went back, but all departed from the Ross Sea. The researchers examined changes in mitochondrial DNA to determine changes in population diversity. Genetic diversity expanded quickly (within a few generations) after the a colony was established on the VLC. The implications for this are that species that are highly mobile, as elephant seals are, can respond quickly to changing habitat situations. Other species that are less mobile will probably not fare as well in the face of climate change. Their findings will be useful for researchers who try to predict how various species will react to climate change, and use those findings to develop conservation plans.
Also, it's pretty frickin' cool that they got so much usable DNA from 8,000 year old elephant seal remains.
Wednesday, July 8, 2009
More News on Antarctic Melting
see more Fail Blog
Friday, June 5, 2009
Don't Buy that Beachfront Property Just Yet
It appears that the revised estimates represent not a brighter future, but slightly less catastrophic future. As someone who would prefer a no-catastrophe future, I can't say that this news is as reassuring as some headlines would suggest. The Telegraph (UK) headlined its article "West Antarctic ice sheet collapse 'exaggerated', scientists say," and conveniently left out quotes from the leader of the team that developed the new estimates in which he noted that even a 1-2 meter rise would be "very, very serious." The problem with presenting new information about climate change as "good" just because it less dire is that it overlooks the fact that even small climate disruptions are going to have major impacts on human life. Scientists keep saying that climate change is serious for a reason. They might need to edit some conclusions from time to time, but that doesn't mean that global warming is just going to mean a slightly longer summer. Just ask a farmer who got too much rain at the wrong time and faces a drastically diminished crop yield. Whether it's one meter or six, the fact that formerly solid ice has suddenly started melting should worry us all.
Thursday, April 30, 2009
Trends in Antarctic Ice
The ozone hole will no doubt continue to shrink, thanks to the global ban on chlorofluorocarbons (CFCs), and conditions will return to normal, meaning the effects of climate change will be more obvious. But try telling that to Dimitri Zinchenko, a Russian Antarctic sea captain who asserts that his personal experience with the ice over the past few years does not lead him to believe in climate change. Certainly Captain Zinchenko is telling the truth about what he's seen, but again, one set of observations does not give the entire story about a complex phenomenon such as climate change. The effects of climate change will be and have been varied and unpredictable. The main problem is that global systems are being disrupted. Regardless of whether these disruptions are of the classic, ice-melting, thermometer-busting kind we've come to associate with climate change, they can have serious impacts on ecosystems and human systems.
So when you hear about Antarctic ice in the news, don't be confused when the news isn't all melting and sea rise and cities underwater oh my. There may be far less dramatic changes that are also slowly adding to the growing pile of evidence in favor of an anthropogenically warming world.
Wednesday, April 29, 2009
Reflections on Climate Change, Consensus, and Icebergs
The idea at hand (I can't say too much about the exact details since the debates are not necessarily on the record) was not even suggested as a Resolution, which is binding. This was merely the first step in a fairly tentative consideration of an emerging, but ultimately minor, issue. Before it had even been studied, some Parties were worried about an outcome unfavorable to them. Now imagine the foot-dragging that must occur in similar fora that address issues with extremely broad ramifications, such as climate change. After seeing the painful process of developing an international consensus (and among less than thirty countries!) up close, I understand, if not approve of, the lack of action at the UN and similar bodies. When the climate change conference in Copenhagen rolls around this December, try not to only be angry at countries that hold up progress. Show support for the countries who are striving for progress. Believe me, they are just as frustrated as you are. Probably more.
All this is a roundabout way of saying that Copenhagen is probably going to be a fairly difficult process, even though the impact of climate change grows by the day. The European Space Agency (ESA) has been releasing excellent images of the continuing breakup of the Wilkins Ice Shelf in Antarctica. Earlier this month, the land bridge connecting the shelf to an island collapsed, and now the ice shelf has become more destabilized, with icebergs beginning to calve. The danger with the continued breakup of the ice shelf is not that the icebergs will have any appreciable impact on sea level, but that ice shelves typically hold back glaciers and land ice. In the absence of the shelf, these other kinds of ice slide towards the ocean faster, and they can raise sea level. Many in the environmental community reacted to news about the Wilkins Ice Shelf with a hope that the unfortunate event would at least spur governments to take more decisive action. We'll see in December whether it will be business as usual or if goverments can put aside some of their differences and work a bit more cooperatively.