Secret Lifeoficebergstext by Kenneth L. Smith, Jr.photographs by Rob SherlockDrifting islands of ice, sculpted by fragmentation,erosion, and melting, icebergs have become harbingersof climate change. And nowhere on Earth are <strong>the</strong>ymore prevalent than in <strong>the</strong> Sou<strong>the</strong>rn Ocean along <strong>the</strong>Antarctic Peninsula, a curved finger that juts out to<strong>the</strong> nor<strong>the</strong>ast from <strong>the</strong> main ice-shrouded continent,separating <strong>the</strong> Amundsen Sea to <strong>the</strong> west from <strong>the</strong>Weddell Sea to <strong>the</strong> east. It is along <strong>the</strong> eastern boundaryof <strong>the</strong> Antarctic Peninsula that a major nor<strong>the</strong>rlyflow from <strong>the</strong> sou<strong>the</strong>rly reaches of <strong>the</strong> Weddell Seahas been dubbed “iceberg alley. “<strong>The</strong> recent breakup of <strong>the</strong> huge ice shelves along<strong>the</strong> western boundary of <strong>the</strong> Weddell Sea has calveda large number of icebergs. <strong>The</strong>se sculptures of blueand white ice, tens of thousands of years old, occurin an endless variety of tabular and pinnacle forms as<strong>the</strong>y proceed along iceberg alley on a nor<strong>the</strong>rly “deathmarch” into <strong>the</strong> warmer waters of <strong>the</strong> Scotia Sea andSouth Atlantic.46I have been fascinated by icebergs since my firstoceanographic cruise to <strong>the</strong> Antarctic more than30 years ago. I reasoned that as guardians of<strong>the</strong> ice-shrounded continent, <strong>the</strong>se magnificentfrozen sculptures, with <strong>the</strong>ir large underwatermass, would be havens for enhanced marine life.Indeed, on many subsequent cruises I have observeda preponderance of seabirds associatedwith most icebergs.In 1992, one of my post-doctoral students,Ron Kaufmann, and I decided to place a seriesof upward-looking acoustic arrays moored to<strong>the</strong> sea floor of <strong>the</strong> Weddell Sea to observe anddocument <strong>the</strong> pelagic communities associatedwith <strong>the</strong> advancing and receding of <strong>the</strong> seasonalpack ice. It became clear from <strong>the</strong> data we collectedthat icebergs drifting north through clearwater, free of pack ice, did not travel alone butwith an entourage of zooplankton and nekton.<strong>The</strong> author prepares to deploy an ROV from <strong>the</strong> deck of <strong>the</strong> RV L.M. Gould
seabirds such as Cape Petrels were more abundant around icebergs than in <strong>the</strong> open waters of <strong>the</strong> Weddell Sea. <strong>The</strong> waterfall behind <strong>the</strong>m is meltwater from <strong>the</strong> iceberg, which nourishes its surrounding waters .Delighted with our findings, I asked colleaguesinterested in icebergs if <strong>the</strong>y would be willing tolaunch a multidisciplinary study of <strong>the</strong>se driftingislands in <strong>the</strong> Sou<strong>the</strong>rn Ocean. <strong>The</strong> scientificreviewers of my grant proposals, however, werenot convinced that icebergs could influence <strong>the</strong>pelagic ecosystem. Despite my enthusiasm for <strong>the</strong>research project, it failed to generate any significantinterest. Eventually, we succeeded in obtaininga small grant for exploratory research from <strong>the</strong>National Science Foundation (NSF) for a modest,month-long research expeditionto <strong>the</strong> WeddellSea. Our team of sevenconsisted of BruceRobison (Monterey BayAquarium ResearchInstitute), who wouldstudy <strong>the</strong> communityof organisms under<strong>the</strong>ice surface; MariaVernet (University ofCalifornia, San Diego),who would study <strong>the</strong>phytoplankton; RonKaufmann (Universityof San Diego), whowould study <strong>the</strong> macrozooplanktonandmicronekton; Tim Shaw(University of South Carolina), who would study<strong>the</strong> detrital material associated with <strong>the</strong> icebergs;John Helly (UCSD), who would study icebergstructure and assess iceberg populations fromsatellite imagery; and Robert Wilson (UCSD) andHenry Ruhl (MBARI), who would study seabirds.On November 27, 2005, our group departedfrom Punta Arenas, at <strong>the</strong> sou<strong>the</strong>rn tip of Chile,aboard <strong>the</strong> RV L. M. Gould, a 76-meter researchship with an orange ice-streng<strong>the</strong>ned hull. Onboard were laboratories and expansive deckspace to conduct over-<strong>the</strong>-side sampling. <strong>The</strong>ship was outfitted with a large multiple openingclosingtrawl system and a CTD, a device thatcould be lowered into <strong>the</strong> water to record salinityand temperature with depth, and a variety of watersamplers. A remotely operated underwater vehicle(ROV) was also on board for observing andsampling under <strong>the</strong> icebergs. Over <strong>the</strong> course ofa month, we were able to study two free-driftingicebergs in <strong>the</strong> Weddell Sea.<strong>The</strong> smaller iceberg was approximately twokilometers long and 41 meters high, with a submergeddepth greater than 300 meters. To documentchanges in flora and fauna associated with<strong>the</strong> iceberg, we put <strong>the</strong> ship on a spiral track thatbegan at 20 meters out from <strong>the</strong> island of ice. We<strong>the</strong>n began circling it, taking samples at ever-increasingdistances from it up to nine kilometers.<strong>The</strong> second iceberg was some 21 kilometerslong and 30 meters high, with a submerged depthof more than 230 meters. This iceberg was far toolarge for us to embarkon <strong>the</strong> spiral samplingused on <strong>the</strong> smallerone, so we put <strong>the</strong> shipon a course of paralleltransects along eachlength of <strong>the</strong> iceberg,out to a distance ofnine kilometers.As <strong>the</strong> icebergsslowly melt, <strong>the</strong>y shediron-rich terrigenousmaterial, likely pickedup as wind-blowndust and from glaciallyground bedrock when<strong>the</strong> ice was forming.Nutrients from thisterrigenous materialincreased phytoplankton growth in <strong>the</strong> vicinity of<strong>the</strong> iceberg. Elevated concentrations of phytoplankton,being at <strong>the</strong> base of <strong>the</strong> pelagic foodchain, in turn nourished <strong>the</strong> zooplankton (krill)around <strong>the</strong> iceberg, which were significantly increasedin number compared to more peripheralwaters. <strong>The</strong> highest level of <strong>the</strong> food web, <strong>the</strong> seabirds—dominatedby Cape petrels and Antarcticfulmars—were also substantially higher in numberaround <strong>the</strong> iceberg, feeding on <strong>the</strong> abundant krill.Watching <strong>the</strong> real-time video from <strong>the</strong> ROV,secured to <strong>the</strong> ship with a 300-meter electromechanicalte<strong>the</strong>r, we observed something quiteunexpected—extensive “fields” of attached algae(diatoms) growing on small fragments of volcanicrock embedded in <strong>the</strong> surface of <strong>the</strong> submergedice. <strong>The</strong>se algae bloomed where down-wellinglight was sufficient for growth to depths as deepas 60 meters. We also saw swarms of krill ando<strong>the</strong>r zooplankton associated with crevasses andoutcrops on <strong>the</strong> undersurface of <strong>the</strong> ice.<strong>the</strong> <strong>explorers</strong> <strong>journal</strong>