East Diamante Volcano: Another Amazing Place on the Mariana Arc
April 5, 2004
Pacific Marine Environmental Laboratory
NOAA Vents Program
A close encounter with an angel fish as it swims by a black smoker. (QuickTime, 620 Kb)
Sea life around the hydrothermal vents at the East Diamante volcano (QuickTime, 1.9 Mb)
It was difficult for us to leave NW Rota 1 and the Brimstone Pit area, knowing that it may have been the first time submarine volcanic activity was witnessed as it was happening. We didnt know if our next site, East Diamante volcano, would be equally exciting, but we steamed north with hopeful anticipation. The summit of this large volcano is topped by an ancient caldera, collapsed in the center and with heavily eroded rims, suggesting that the volcanic activity sputtered out long ago. This aged appearance made our detection of a strong hydrothermal plume in 2003 that much more enigmatic. The plume found in 2003 surrounded a group of small lava cones near the center of the caldera. Magmatic events, over the course of thousands of years, can build a central dome complex. Each small volcano may be equivalent to a different eruptive episode. Our CTD team provided clues to which of the domes might likely be the sources of the venting. The depth of the major plume was at 320 m (1,050 ft) depth, so the source had to be deeper than the plume horizon.
We were in for two major surprises during a stunning discovery dive. After reaching the sea floor, low-temperature diffuse venting was quickly recognized amidst the boulder-strewn slope. The presence of barnacles (possibly a new species) coined the name of the first site as Barnacle Beach." After a short search around the rim of the cone, we came across a line of sulfide chimneys (named the Black Forest) upslope of Barnacle Beach. These represented the first sulfide-depositing hydrothermal systems found along the Mariana Volcanic Arc. They may also be the shallowest active sulfide vents yet seen. The mineralogy and metal content of the deposits are of great interest to those studying the formation of ore deposits found on land.
Chemosynthetic microbial mats cover red algae and coral, which are photosynthetic. Hydrothermal vent and coral reef communities are overlapping here at 190 m depth. Click image for larger view and more details.
This may be a unique photograph of a shallow-water tropical fish swimming among active black smoker chimneys at Black Forest vent field. The chimneys rise up to 7 m tall. Click image for larger view.
From the first site we proceeded west to a cone that rises to 168 m, named Pinnacle Cone." The first surprise was to find the slope of the cone completely covered with a thin, filamentous microbial mat. Rising up to 200 m depth, we began to see red and green encrusting algae on surface of the rocks. The microbial mats party covered these surfaces as well. This site is a unique environment where a chemosynthetic ecosystem (represented by the microbial mat) intersects with the photosynthetic ecosystem of the shallow ocean. This juxtaposition of two ecosystems was of great interest to the biologists on board (Kim Juniper, Verena Tunnicliffe, Anna Metaxas, and John Dower). At this depth, the ROPOS ROV (remotely operated vehicle) could see using only the filtered sunlight from the surface. The top of the cone consisted of several large pinnacles of volcanic rock with vertical walls. A myriad of fish, basket sea stars, various types of corals, and other organisms populated the spires. We named the site Aquarium for its colorful variety of sea life.
Were now headed north to Maug, a mile-wide caldera surrounded by the remnants of a massive volcanic event that occurred thousands of years ago. These remnants form a circle of three small islands guarding the shallowly submerged caldera floor. This site yielded one of the most intense plumes found in 2003. Who knows what we will find on the sea-floor rocks of Maug?
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