Cruising to an OASIS

Bridgit Boulahanis, a graduate student at Lamont-Doherty Earth Observatory, joined a team of 18 scientists from across the United States on an expedition to the eastern Pacific Ocean. Their mission: to investigate a chain of submarine volcanoes, or seamounts, along the East Pacific Rise. The OASIS (Off Axis Seamounts Investigation at Siqueros) team will be mapping the sea floor in detail never before seen for this region and generating an entirely new data set of bathymetry, magnetics and gravity measurements. During the day, scientists will go deep in a research submarine to explore the volcanoes up close and collect samples. At night, they will use an autonomous underwater vehicle to make highly detailed maps and take chemical measurements. Follow Bridgit’s explorations here and on Twitter and Instagram at midoceanbridg.

Location: Eastern Pacific Ocean
Purpose: Studying submarine volcanoes
Date: November 2016

 

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Posted By: Guest Blogger on November 26, 2016

The view of life on the sea floor at Avery Seamount from the windows of a research submarine. Photo courtesy of P. Gregg (U. Illinois), D. Fornari (WHOI), M. Perfit (U. Florida), co-chief scientists of OASIS cruise AT37-05 on RV Atlantis funded by the National Science Foundation. Image taken from DSV Alvin using WHOI MISO Facility deep-sea camera systems. Copyright WHOI.

The view of life on the sea floor at Avery Seamount as Bridgit Boulahanis saw it from the portholes of a research submarine. Seafloor photos courtesy of P. Gregg (U. Illinois), D. Fornari (WHOI), M. Perfit (U. Florida), co-chief scientists of OASIS cruise AT37-05 on RV Atlantis funded by the National Science Foundation. Image taken from DSV Alvin using WHOI MISO Facility deep-sea camera systems. Copyright WHOI.

By Bridgit Boulahanis

The biggest question driving the OASIS mission is simple: how old are the lava flows along the 8°20’N Seamount Chain. Answering that question is far from simple, requiring a plethora of data, multitudinous methods of sample collection, and many experts in order to conduct the analysis.

We can get information about the magnetic polarity of the rocks below us from our magnetometer, allowing us to understand the relative age of the seafloor in relation to known magnetic pole reversals. We can use shipboard multibeam and autonomous underwater vehicle multibeam to gain an idea of the character of the seafloor we survey, generating maps of the major features and preliminary analysis of the sediment cover in the region. We can use dredges, large metal baskets lowered overboard with weights, to pick up rocks across a broad area in order to characterize the chemical composition of lavas in that region. Each of these forms of data collection is adds an important piece to the puzzle we are trying to solve.

However, the most exciting form of data collection is the sampling we can do with Human Occupied Vehicle (HOV) Alvin. Alvin allows us to get precise samples of specific lava flows and morphological features, ensuring that we know exactly where the rocks we chemically analyze come from. Beyond its incredible sampling capabilities, it is the most exciting way to learn about the seafloor. Last week, I had my first opportunity to dive in the submersible, and while the science is what drew me here, it was the thrill of seeing firsthand what was on the bottom of the ocean that had me wide awake many hours before launch, standing on deck as the sun came up, staring over the side into the depths that I would soon be exploring. In the morning air it was hard to imagine that soon I would be under thousands of meters of water, seeing with my own eyes what I have been studying for years.

Bridgit Boulahanis and Mike Perfit prepare for their dive to the seamount. Photo courtesy of Dan Fornari.

Bridgit Boulahanis and Mike Perfit prepare for their dive to the seamount, with the research submarine in the background. Photo courtesy of Dan Fornari.

After a small breakfast and what felt like years of excited pacing, we entered the submersible. I was diving with Alvin pilot Jefferson Grau and Dr. Mike Perfit, Distinguished Professor of Geology at University of Florida. The tight space that makes up the human occupied space of Alvin has just enough room for three, and so as the submersible was lowered into the sea off of the R/V Atlantis, we settled in for a cozy nine hours.

After bobbing with the waves on the surface for several minutes as the pilot and crew did their final safety checks, we began our descent. Almost immediately upon leaving the surface the motion of the waves faded away and the submarine felt still enough to almost trick me into believing we weren’t moving at all. However, soon the bright blue of the shallow ocean faded to the black of the deep, and bursts of bioluminescence surrounded the submersible. More seasoned colleagues had told me that I should keep an eye out for bioluminescence, but there was so much of it that it would have been hard to miss! It looked as if we were descending through a field full of fireflies, with occasional fireworks popping up as we passed larger organisms bursting out of the darkness.

It took us almost 90 minutes to reach the seafloor, and I spent the entire time looking out the two portholes I could reach from my side of the submersible. I was already enamored with the experience, and we hadn’t even gotten to the ocean bottom. During our final approach we turned on all of Alvin’s external lights, suddenly bringing daytime to a previously eternally dark part of the world. Jefferson and Dr. Perfit, both veterans of Alvin exploration, advised that I look out my side porthole to catch the soonest glimpse of the seafloor. For several minutes I waited, staring down to where light blue faded to darkness. Then, suddenly, it was there – sandy sediment extending in every direction with pillow basalts peaking out around.

A red shrimp swims into view beside basalts on the seafloor. Photo courtesy of P. Gregg (U. Illinois), D. Fornari (WHOI), M. Perfit (U. Florida), cochief scientists of OASIS cruise AT37-05 on RV Atlantis funded by the National Science Foundation. Image taken from DSV Alvin using WHOI MISO Facility deep-sea camera systems. Copyright WHOI.

A red shrimp swims into view among basalts on the seafloor.

Immediately we began collecting samples of the rocks around us using Alvin’s two manipulator arms, while writing descriptions of the area and recording audio descriptions of everything we saw. Following a dive track laid out before our descent, we traversed up the side of Avery Seamount while noting the characteristics of everything we passed. Dr. Perfit pointed out rocks for Jefferson to sample, while I operated cameras to ensure we attained high quality footage of each sampling location. Our conversations were filled with preliminary analysis, with Dr. Perfit guiding me in identifying the differences between the various rocks outside our window.

Midway through our dive we came to a steep wall approximately 30 meters high, a cliff face at a 90 degree angle to the seafloor. Even in the best multibeam maps of the ocean floor we cannot represent such rapid depth changes accurately – our sonar will smooth even the largest crags automatically, making knowing about these sorts of cliff faces elusive without underwater vehicles. Despite my years of looking at these maps, I never pictured vertical cliffs rising off of the seafloor. To say this realization rocked my world would not be hyperbole, but it would be a bad pun.

Our dive track took us past the steep wall, and so Alvin rose up, floating along the cliff face that seemed to climb endlessly from the sediment below. Soon the dark pillow basalts became speckled with sea life – corals and anemones, starfish and sponges. Everywhere we looked, life was not only present but appeared to be thriving. While as geologists and geophysicists we do not sample any of the living organisms we find, it was very exciting to see, and we noted their location to pass on to biologist colleagues who might return.

Alvin’s sample basket was almost completely full by the time we approached the summit of Avery Seamount, and we spent our last moments on the seafloor extracting one last rock for later analysis. Though the dive lasted its full nine hours, it passed far too quickly. Too soon we were rising to the surface, passing back up through the bioluminescence and the lightening shades of blue until we were again hoisted on board the ship.

Basalt and sediment on the sea floor, as seen from the research submarine.

Basalt, sediment, and sea life on the sea floor, as seen from the research submarine.

Upon exiting Alvin we were met with a cheering science party, a tradition every time the submersible comes back on deck. After applause and hugs we scientists did what we do best – got straight to work on the analysis. We classified the samples we had collected and began the description and photography process, logging each rock carefully so when they get back to a laboratory on land the geochemists have all of the information they might need.

The descriptions and samples we collected while on the bottom will help us to characterize how old Avery Seamount might be, providing valuable insight into the processes that formed this expansive seamount chain. Having contributed to increasing scientific understanding in such a hands on way is absolutely thrilling. Now when I look over the edge of the ship it is impossible not to picture of the varied terrain that must be slipping past me deep below, teeming with life and calling out for me to visit again soon.

Bridgit Boulahanis after the dive. Photo courtesy of Dan Fornari.

Bridgit Boulahanis after the dive. Photo courtesy of Dan Fornari.

Bridgit Boulahanis, a graduate student at Columbia University’s Lamont-Doherty Earth Observatory, is in the eastern Pacific Ocean aboard the R/V Atlantis on an expedition to investigate a chain of submarine volcanoes along the East Pacific Rise. Learn more about the expedition in her blog and on the OASIS Facebook page and YouTube channel.

Posted By: Earth Institute on November 15, 2016

By Bridgit Boulahanis

Ocean scientists are, in their hearts, explorers. Our group aboard the R/V Atlantis may be more infected with the exploration bug than most. The first goal of our expedition makes that clear: We aim to map regions of the seafloor never before seen by human eyes. After a two-day transit to our survey site, the first four days of our research program are dedicated solely to mapping.

An unexplored seamount is our first mapping target. Prior to our expedition, the region was only known to be a shallow area because of satellite-derived maps. Information from satellites gives scientists the global seafloor map that we use in the absence of data of better quality. Unfortunately, this data resolution is on the order of a kilometer, which provides a general idea of the major features of a region but misses many crucial details that may be scientifically important.

With our shipboard mapping system, we can create maps at 75-meter resolution. This is similar to the difference between seeing that there is a large green feature in the middle of the island of Manhattan, and being able to pick out the exact location of the Delacorte Theater within the park.

Watching the Liona Seamount come into focus.

Scientists aboard Atlantis watch the Liona Seamount come into focus.

Knowing all of this, it makes sense that when the R/V Atlantis arrived on station to map what was this week dubbed, the entire science party was gathered in front of one computer. As each new swath of data came in, scientists called out features they could immediately identify and began debating the origin and age of the seamount springing up before our eyes.

This is just the first stage of exploration and discovery for our month-long expedition. Liona Seamount stands at the western edge of a long chain of seamounts extending from the East Pacific Rise at a latitude of approximately 8°20’N. Our mission, titled Off-Axis Seamount Investigations at Siqueiros (OASIS), aims to characterize this entire chain of submarine volcanoes. We will use every resource at our disposal to increase scientific understanding of these seamounts.

The Liona seamount.

A 3D map of Liona Seamount. Courtesy of Dan Fornari and Trish Greg

The next phase of our survey will include even higher resolution maps made by the Autonomous Underwater Vehicle Sentry. If our shipboard maps revealed the Delacorte Theater in Central Park, Sentry’s maps would allow us to see people sitting in the seats. We will also be utilizing cameras designed to be towed just above the seafloor and provide thousands of high-resolution images of the features below.

Physical samples of rocks from our seamounts are also crucial to this study, and will be brought on board through overnight dredging and collection using the research submarine Alvin.

The first round of data is already in the hands of the eight graduate students aboard, rapidly being processed and parsed for in-depth analysis. In addition to new maps covering several hundred kilometers of seafloor, we have collected magnetic data giving us the approximate age of the seamounts we are studying, and gravity data that will help us to gain a rough understanding of the structure of the oceanic crust.

The results we have gotten so far are thrilling, but no doubt some of the most exciting data of our expedition is still ahead of us.

bridgit-boulahanisBridgit Boulahanis, a graduate student at Lamont-Doherty Earth Observatory, is sailing in the eastern Pacific Ocean aboard the R/V Atlantis on an expedition to investigate a chain of submarine volcanoes along the East Pacific Rise. Learn more about the expedition on the OASIS Facebook page and YouTube channel.