Census of Marine Life-affiliated scientists, plumbing the secrets of a vast underwater mountain range south of New Zealand, captured the first images of a novel “Brittlestar City” established against daunting odds on the peak of a seamount – an underwater summit taller than the world’s tallest building.
Its cramped starfish-like inhabitants, tens of millions living arm tip to arm tip, owe their success to the seamount’s shape and to the swirling circumpolar current flowing over and around it at roughly four kilometers per hour. It allows Brittlestar City’s underwater denizens to capture passing food simply by raising their arms, and it sweeps away fish and other hovering would-be predators.
Discovery of this marine metropolis, announced today along with important new insights into seamount geology and physics, highlighted a month-long April expedition to survey the Macquarie Ridge aboard the Research Vessel Tangaroa of New Zealand’s National Institute of Water & Atmospheric Research, host of the Census of Marine Life seamount programme, CenSeam. The voyage was largely funded by the New Zealand Foundation for Research, Science and Technology.
Formed at least 12.5 million years ago, Macquarie Ridge stretches 1,400 km south from New Zealand to just above the Antarctic Circle. A multi-disciplinary scientific team from New Zealand and Australia extensively sampled this intriguing ecosystem deep beneath waves familiar to fishing trawlers but rarely reached by scientists.
Usually corals and sponges dominate seamount peaks, filtering food that arrives on the current. Biologists aboard the Tangaroa believe Brittlestar City is the first dense aggregation of another filter feeder, the brittlestar, ever found atop a seamount, and they credit the summit’s shape and extraordinary current circumstances there, 750-meters above the ocean floor.
They photographed brown-black brittlestars numbering hundreds per square meter and estimate tens of millions of them populate the 100 square km flat top of the seamount.
Brittlestars are echinoderms, relatives to starfish, sea cucumbers, sea lilies, and sea urchins. The two brittlestar species observed were tentatively identified via photographs sent from the ship to the Museum Victoria in Melbourne, Australia.
There, taxonomist Tim O’Hara determined that the smaller, densely packed brown-black brittlestar species, found living arm tip to arm tip on the sand and cobble substrate of the peak, were likely Ophiacantha otagoensis or Ophiacantha fidelis.
Larger orange-red species discovered down the seamount’s flanks, filmed waving arms in the current to collect passing food, were likely Ophiacantha rosea.
“We were excited to see such a huge assemblage of brittlestars on the Macquarie Ridge seamount. Not only is it amazing to see a vast array of one type of organism but the implications of the find for our understanding of the relative uniqueness of seamount assemblages are potentially far-reaching.” said ecologist Dr. Ashley Rowden of NIWA.
Piecing together the Brittlestar City ecosystem
The ship towed special sleds to collect seamount organisms. Thousands of specimens of all kinds were gathered from eight seamounts in over 30 sled collections and now fill almost 1,600 vials, jars and bags, to be sent from NIWA to taxonomists in New Zealand, Australia and overseas.
Full identifications may take many years. The eight biologists on board believe some species collected have never before been recorded in the region while some may be new to science.
A Deep Towed Imaging System (DTIS) vehicle, meanwhile, designed and constructed at NIWA by Peter Hill, was “flown” over the seafloor, snapping still photos and high definition video of the animals and their habitat. DTIS captured over 20 hours of video and thousands of photos of a part of Earth never seen before by humankind.
An abundance of deepwater cardinal fishes (Epigonus species) was found sheltering below a rock ledge on the seamount. In the lee of the rock, biologists believe, the fish could both conserve energy and access food.
Several Morid cods (family Moridae) were found in the folds of a large bubblegum coral (nearly two meters high, and likely hundreds of years old). These fish were also believed to be finding shelter from the current and perhaps benefiting in other ways from their close association with the coral.
Oceans worldwide contain an estimated 100,000 seamounts rising at least one km above the seabed; fewer than 200 have been sampled in any detail.
Undersea mountains can be highly productive and biodiverse, sometimes host unique species and serve as feeding grounds for fishes, marine mammals and seabirds. They also may serve as important way stations for marine migrations. The scientists’ work sheds light on factors underpinning seamount biodiversity, suggesting ways to improve their environmental management.
The odd shape and circumstances of Brittlestar City seamount
Tangaroa’s acoustic “multibeam” technology mapped the sizes, shapes and depths of the Macquarie Ridge.
The Brittlestar City seamount displayed several geological faults affecting its shape and geomorphology. The odd rectangular edge of its southern peak was formed by the intersection of two perpendicular faults. Because the upper surface is relatively flat, experts believe it was once at sea level, or slightly submerged. The flat topography suggests wave erosion occurred during the last ice age 18,000 years ago, when sea level was low. Although the base of Brittlestar City seamount is 850 meters below surface, its peak is just 90 meters underwater.
Intrigued by the dynamics of the Antarctic Circumpolar Current as it passed over and through ridge gaps, physicists aboard the Tangaroa calculated its speed over the top of the seamount at a “rattling” 2 knots (about 4 km per hour).
“This current is estimated to be 110 to 150 times larger than all the water flowing in all the rivers of the world,” says Dr. Mike Williams of NIWA. “In terms of the world’s oceans, New Zealand sits right beside the motorway.”
The Macquarie Ridge creates a strategic marine junction. “Understanding this current will shed light on how much water flows into the Pacific as opposed to continuing to circumnavigate Antarctica. This is important for understanding, and ultimately predicting, the impact of potential changes in the current on climate throughout the Southwest Pacific.”
Data was collected from nine strings of metering instruments, anchored a year earlier in two gaps or "choke points" in the Ridge, through which the current squeezes. Experts were astonished to find the current had pushed the top instruments on some strings to a depth of one kilometer below the surface.
Scientists also took this ocean area’s temperature and salinity readings for the first time since the 1960s, looking for climate-related changes, and obtained water samples to measure and compare levels of marine life nutrients.
April’s Tangaroa voyage continues the recent collaboration of scientists in New Zealand (NIWA, TePapa and other institutes) and Australia (CSIRO, Museum Victoria and other institutes) to document invertebrate and fish life on seamounts that range between the two countries.
The Census of Marine Life CenSeam programme
Seamount biology research over the years has been uncoordinated, causing lost opportunities for collaborative studies, inefficient sampling that left major gaps, and data that can’t be compared across regions.
In Newport, Oregon, in 2003, some 33 seamount scientists from 11 countries reviewed the state of knowledge on seamounts and agreed on three key themes that should guide world research:
1) What factors drive seamount community structure, diversity and endemism both at the scale of whole seamounts and individual habitats within seamounts?
The diversity and rates of peculiarity of organisms inhabiting a seamount is often high but can vary considerably, even between seamounts close to each other. CenSeam scientists are looking for factors that influence a seamount’s biodiversity and community structure, e.g: depth, shape, size, location, isolation, surface productivity, hydrology, geological age, and substrate type. The knowledge may lead to tools for modeling and predicting biodiversity levels on tens of thousands of unexplored seamounts.
It will also help answer questions such as how much of the ocean’s biodiversity is contributed by seamounts? How significant are seamounts as incubators for new species?
2) What processes cause differences between seamounts, and between seamount and non-seamount regions?
CenSeam scientists also focus on the evolutionary biology of seamounts, including such questions as:
* Are seamount organisms genetically isolated?
* To what degree do seamounts interact with surrounding deep habitats, both pelagic (in the water column) and benthic (ocean floor)?
* What factors support the high biomass often observed on seamounts?
3) How do fisheries impact seamounts?
Many offshore fisheries are known to exploit seamounts, but information detailing where, how frequently and to what extent seamounts are fished, is lacking. CenSeam research questions therefore include:
* How much have seamounts been impacted already?
* How much do various fisheries depend on seamounts?
* What is the likely impact of fishing activities on seamount communities?
CenSeam officially joined the Census of Marine Life in February 2005. CenSeam’s secretariat is hosted by NIWA in Wellington, New Zealand.
CenSeam, alongside the other Census of Marine Life programmes, will extend until 2010 and consists of three key phases. In 2009 CenSeam will enter its final phase, which will concentrate on information integration and dissemination.
“Seamount ecosystems are extremely valuable to the global environment. They are also the target of offshore commercial fishing, and are of potential interest for seabed mining,” says Dr. Rowden of NIWA. “The long term impacts of such commercial activities need to be quantified.”
Census of Marine Life (www.coml.org)
CoML is an international science research program uniting researchers from more than 70 nations with the goal of assessing and explaining the diversity, distribution and abundance of marine life – past, present and future – by 2010.