Monterey Bay Aquarium Research Institute


Volcanoes and Seamounts Logbook
Day 8: Alarcón Rise
April 28, 2012 • (Leer en Español)

Today we dove on five active hydrothermal vents and several more inactive chimneys. The active vents spew hot, chemical- and mineral-rich water through chimneys which slowly grow through the precipitation of minerals. Some of these chimneys grow to 12 or more meters in height (40 feet) and the black, mineral-rich water we measured at one vent today reached temperatures of 550 degrees Fahrenheit. Biologically these vents are of interest because a diverse community of organisms is found here which is not dependent upon surface productivity, or photosynthesis. Photosynthesis occurs in the sunlit surface waters of the ocean and most organisms in the deep are dependent upon this surface productivity which slowly falls to the seafloor in the form of marine snow. However, at hydrothermal vents bacteria use the chemical rich water as a source of energy, a process known as chemosynthesis.

These chemosynthetic bacteria support dense populations of worms, snails, crabs, clams, and fish. The giant tube worms found here have no gut but instead farm the chemosynthetic bacteria inside their bodies. The worms provide a home and bring oxygen to the bacteria with their hemoglobin-rich blood. The bacteria, in turn, provide nutrition for the worms. Some of the giant tube worms we find are very large; one specimen collected today was nearly 1.2 meters (five feet) long!

Large grouping of tube worms
A dense community of organisms grows upon the hydrothermal chimney. These giant tube worms can grow to two meters (six feet) in length and provide food and habitat for a variety of other worms, snails, crabs, and fish.

Adjacent to the chimneys, lower temperature water is often released from the seafloor over a wider area. These areas of diffuse venting are home to large vesicomyid clams, which also house chemosynthetic bacteria in their bodies, similar to the giant tube worms.

We've collected samples of these vent organisms in an effort to understand the relationship between the populations living here and those living at other hydrothermal vents in the Pacific Ocean. We use molecular markers, or gene regions on the organisms' DNA, to determine the relatedness of organisms found here and elsewhere. Molecular tools can also be used to tell us something about the evolutionary process such as when and how a new species emerged or how one species is related to other similar species. For example, we know that these giant tube worms are related to the bone-devouring worms (Osedax spp.) because of molecular tools. Interestingly, we found mammal bones in a lava channel on today's dive and, although we did not find Osedax, we found snails and mussels like we find on whale bones and, also using molecular tools, we will be able to tell the relatedness of species found on these bones to those on bones of whales we have surveyed in the Monterey Canyon.

A piece of bone with several small animals attached.
This mammal bone we collected was home to a variety of snails and mussels. These animals are also found on whale bones in Monterey Canyon. Using molecular tools will be used to show the relationship between the two populations.

We also collected samples of the sulfide chimneys, both active and inactive, and will determine the ages of the inactive ones using radioactive radium. Later in the dive, we surveyed more of the large lava sheet flow that hosts all the active hydrothermal sites we have found. Analysis of the dozen or so samples we have collected from this one large flow will allow us to evaluate magma-mixing processes in the magma chamber that underlies the ridge axis at a depth of one to two kilometers below the seafloor. At the end of the dive, we determined the relative ages of a few older sheet flows and collected samples for dating and chemical analysis. They will contribute to our understanding of the eruption history of the entire Alarcón Rise.

Black smoke spews from chimney
Hot, mineral rich water spews from a hydrothermal vent on the seafloor. Also known as black smoker, the mineral rich water appears as a column of black smoke rising from the seafloor. White, floculent bacterial mat is seen on the surface of the chimney below the black smoker.
Long, white clams over a large area.
A dense bed of clams was observed in an area of diffuse venting adjacent to a hydrothermal chimney.

— Lonny Lundsten and Dave Clague

Brian Dreyer
Brian Dreyer at the camera controls in the ROV control room.
Ronald and Rigorberto
Ronald Spelz and Rigoberto Guardado reload the push core racks on the ROV in preparation for the next dive.
Ronald and Pat.
Ronald and Pat Castillo describe rock samples in the lab that we collected on the dive.

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Volcanoes & Seamounts
 Equipment

R/V Western Flyer

The R/V Western Flyer is a small water-plane area twin hull (SWATH) oceanographic research vessel measuring 35.6 meters long and 16.2 meters wide. It was designed and constructed for MBARI to serve as the support vessel for ROV operations. Her missions include the Monterey Bay as well as extended cruises to Hawaii, Gulf of California and the Pacific Northwest.

ROV Doc Ricketts

ROV Doc Ricketts is MBARI's next generation ROV. The system breaks new ground in providing an integrated unmanned submersible research platform, with many powerful features providing efficient, reliable and precise sampling and data collection in a wide range of missions.

Push cores

A push-core looks like a clear plastic tube with a rubber handle on one end. Just as its name implies, the push core is pushed down into loose sediment using the ROV's manipulator arm. As the sediment fills up the core, water exits out the top through one-way valves. When the core is pulled up again, these valves close, which (most of the time) keeps the sediment from sliding out of the core tube. When we bring these cores back to the surface, we typically look for living animals and organic material in the sediments.

Niskin bottles

Niskin bottles are used to collect water samples as well as the tiny bacteria and plankton in that volume. The caps at both ends are open until the bottles are tripped, when the caps snap closed.


Biobox

The box fits in a partition in the sample drawer. It is shown open, with an animal being placed into it by the ROV's manipulator. When the lid is closed, the box will hold water to protect the animals inside.


Rock crusher

This device is used to collect volcanic glass fragments from the surface of a flow. It is made of about 450kg of lead and steel and is launched over the stern of the ship on a wire. Fragments of rock that break off of the lava flow on impact are trapped in wax-tipped cones mounted around the crusher. The wax is melted in the lab to liberate the rock particles for analysis.

Benthic toolsled

The benthic toolsled is attached to the bottom of the ROV for our geology dives. Its components are the manipulator arm and the sample drawer. The sample drawer is shown open on deck, full of rocks. Normally it is closed when the vehicle is operating and is opened only when a sample needs to be stowed. Partitions in the drawer help us keep the rocks in order. The rocks often look alike, but the conditions and chemistries of the eruptions are different so it is important that we know where each came from.

Glass suction sampler

This equipment is used to vacuum glass particles and larval animals from cracks and crevices. The carousel of small plastic jars fitted with wire mesh will be mounted in the benthic toolsled. The hose will be held by the ROV's manipulator and a suction will be drawn by the pump.

Sediment scoops

Canvas bags on a T-handle for collecting gravel or other materials that fall out of a push-core.


Temperature probe

Held by the ROV's manipulator, the wire on the right is placed into the fluid emitted from a hydrothermal vent to record the temperature.


Vibracores

Vibracoring is a common technique used to obtain samples from water-saturated sediment. These corers work by attaching a motor that induces high frequency vibrations in the core liner that in turn liquefies the sediment directly around the core cutter, enabling it to pass through the sediment with little resistance.


 Crew

R/V Western Flyer

Ian Young
Master


 

George Gunther
First Mate


 

Matt Noyes
Chief Engineer


 

Andrew McKee
Second Mate


 

Lance Wardle
First Engineer


 

Shaun Summer
Relief First Engineer


 

Olin Jordan
Oiler


 

Craig Heihn
Relief Deckhand


 

Jason Jordan
Relief Deckhand


 

Dan Chamberlain
Electronics Officer


 

Patrick Mitts
Steward


 

ROV Doc Ricketts

Knute Brekke
Chief ROV Pilot


 

Mark Talkovic
Senior ROV Pilot


 

Randy Prickett
Senior ROV Pilot


 

Bryan Schaefer
ROV Pilot/Technician


 

Eric Martin
ROV Pilot/Technician


 

 Research Team

Dave Clague
Chief Scientist
MBARI

Dave's research interests are nearly all related to the formation and degradation of oceanic volcanoes, particularly Hawaiian volcanoes, mid-ocean ridges, and isolated seamounts. Topics of interest include: compositions of mantle sources for basaltic magmas and conditions of melting; volatile and rare-gas components in basaltic magmas and their degassing history; chronostratigraphic studies of eruption sequence and evolution of lava chemistry during volcano growth; subsidence of ocean volcanoes and its related crustal flexure, plate deformation, and magmatic activity; geologic setting of hydrothermal activity; origin of isolated seamounts; and monitoring of magmatic, tectonic, and hydrothermal activity at submarine and subaerial volcanoes.

Jenny Paduan
Research Specialist
MBARI

Jenny works with Dave Clague in the submarine volcanism project, processing the high-resolution MBARI mapping AUV data and interpreting the maps using ROV observations and samples from our research sites. On this cruise, she will stand watches in the ROV control room, help with rock and sediment sample workup and curation once the vehicle is on deck, and coordinate these cruise logs. She is now quite solidly a marine geologist, but her degrees are in biochemistry (Smith College) and biological oceanography (Oregon State University). She is thankful for the opportunities that have led her to study volcanoes, and loves being involved with the research and going to sea. She looks forward to discovering more about how Earth works.

Lonny Lundsten
Senior Research Technician
MBARI

On this cruise, Lonny will be in charge of biological sample collection and processing and video data management. This work entails identifying unique biological and geological features that will be seen during the dive, while using MBARI-designed software to log the observations. He is especially excited about this expedition, because no one has surveyed this particular seamount before, and he expects to find many new species on this cruise.

Julie Martin
Senior Research Technician
MBARI

Julie works with the submarine volcanism group, where she currently produces high resolution maps of the seafloor that are used to identify geologic features along submarine ridges and seamounts. Her research interests also include modeling of volcanic ash from sub-aerial, large-scale explosive eruptions.

Ryan Portner
Postdoctoral Fellow
MBARI

Ryan's work with the submarine volcanism project primarily focuses on the formation and distribution of volcaniclastic deposits on active and extinct seamounts and mid-ocean ridges. By categorizing the diversity in these deposits with respect to volcanic landforms he hopes to better understand the underlying controls on explosive vs. non-explosive deep marine eruptions. His background research on deep-marine gravity flow deposits preserved in sedimentary-volcanic successions exposed on land lends a comparable platform to study similar deposits of the modern oceans.

Julie Bowles
Collaborator

Julie is a Research Associate and Staff Scientist with the Institute for Rock Magnetism at the University of Minnesota. As a paleomagnetist, Julie studies variations in Earth's magnetic field and how those variations get recorded in rocks and sediments. One of Julie's particular interests involves using paleofield variations recorded in mid-ocean ridge lava flows to place age constraints on the flows. On this expedition, Julie is interested both in using this technique to try to date some of the young lava flows and in gaining a better understanding of how the Earth's field has varied in this particular location.

Paterno Castillo
Collaborator

Pat is a Professor of Geology at the Scripps Institution of Oceanography, University of California, San Diego. His research interests include petrology and geochemistry of magmas produced within and along divergent and convergent boundaries of tectonic plates, magmatic and tectonic evolution of continental margins and mantle geodynamics. On this expedition, Pat is interested in the petrologic and tectonic evolution of the newly formed oceanic basement in the Gulf of California.

Brian Dreyer
Isotope Geologist
UC Santa Cruz
Institute of Marine Sciences

Brian studies the recent magmagenesis and petrology of the Juan de Fuca Ridge. His interest in mid-ocean ridges began during his postdoctoral fellowship with MBARI's submarine volcanism project; there, he utilized uranium-series disequilibria within individual lavas of Axial Seamount to clarify eruption and petrogenetic timescales. At mid-ocean ridge systems globally, Brian is interested in a) how variability in lava morphology, geochemistry, and petrology reflect deeper mantle-melting and magmatic processes and their complex interplay with tectonism and b) improving the chronological framework of the ridge magmatic plumbing systems. Brian received his Ph.D. in Earth and Planetary Science from Washington University in St. Louis in 2007.

Rigoberto Guardado
Collaborator
Universidad Autónoma de Baja California

Rigoberto Guardado is a teacher and research scientist with the Facultad de Ciencias Marinas (Marine Sciences Faculty) at the University of Baja California in Mexico. As a oceanographer, Rigoberto studies sedimentation processes in the ocean. On this expedition, Rigoberto is interested in learning more about the sediments in this area of the Gulf of California.

Ronald Michael Spelz Madero
Collaborator
CICESE

Ronald Spelz earned his Ph.D. in earth sciences from Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE) in 2008. His research interests are mainly focused in the structural geology and tectonic geomorphology of fault bounded basins and mountain range-fronts in northern Baja California. He is also part of the multidisciplinary research team studying the origin and effects of the El Mayor-Cucapah 7.2 magnitude earthquake which struck northern Baja in April 4, 2010. Ronald presently works in the Marine Sciences Faculty at the Universidad Autónoma de Baja California.

Hiram Rivera
Collaborator
Universidad Autónoma de Baja California

Hiram Rivera is part of the Coastal Management group and teacher in the Faculty of Marine Science at Universidad Autónoma de Baja California. Since 2008 he has worked as a technician with geographic information systems (GIS) applied to fisheries resource management. From 2010 to now he has worked with his students in public participation geographic information systems (PPGIS) 3D models applied to the use of GIS to broaden public involvement in policymaking. His interest for this cruise is to learn about the techniques associated with digital cartography of the Gulf of California.



Last updated: Apr. 30, 2012