As the JOIDES Resolution
arrived in Galveston, Texas, last September after completing its 110th and final
Ocean Drilling Program (ODP) expedition, scientists celebrated the many advances
made during the program. During its nearly 20 years of operations, ODP collected
more than 700,000 feet of core from 1,700 holes advancing our understanding
of climate change, earthquakes, natural resources and microbiology. Yet much
of the seafloor remains to be explored.
The derrick was installed on the center of
the Chikyu in the Nagasaki Shipyard and Machinery Works on Sept. 26,
2003. Lifting the derrick, which is 92 meters tall and weighs 1,200 tons, required
Kaisho, Japans biggest crane ship. All images courtesy of the Integrated
Ocean Drilling Program.
Although the number of holes drilled by ODP is impressive, it only represents
one hole per an area about the size of Colorado. The Integrated Ocean Drilling
Program (IODP), which began on Oct. 1, 2003, will continue the exploration started
by ODP and, before that, the Deep Sea Drilling Project, to investigate Earths
regions and processes that were previously inaccessible and poorly understood.
Scientific vessels
The most visible difference between IODP and its predecessors is the use of
multiple vessels for exploration. Three different types of drilling vessels
riser, riserless and mission-specific platforms will be available
to achieve the programs scientific goals. The riserless and mission-specific
platforms will begin work this summer with respective expeditions to the Pacific
northeast and the high Arctic. Like its predecessors, IODP expeditions are proposal-driven
and are planned after extensive international scientific and safety review.
Aboard these vessels, IODP proposals will address three main themes raised in
the IODP Initial Science Plan, Earth, Oceans, and Life the deep biosphere
and subseafloor; environmental change, processes and effects; and solid earth
cycles and geodynamics. The different capabilities of the vessels make each
integral to achieving the goals set forth in the plan.
Riser vessel
Supplied by Japan and led by the Japan Marine Science and Technology Center,
a new research platform for IODP is the Chikyu (which translates to Earth),
a massive riser vessel that is 210 meters long. It will eventually have a 12,000-meter
drill string for coring in water depths up to 4,000 meters. Still under construction,
it will begin international operations in late 2006, most likely spending the
first several years studying the seismogenic zone in the Nankai Trough off Japan.
Riser technology will allow IODP to conduct long-term (many months to yearlong)
expeditions in areas previously inaccessible to scientific ocean drilling. The
riser, a metal tube extending from the seafloor to the Chikyu, contains a device
to prevent blow-out, which allows for drilling in areas with hydrocarbon potential.
It also uses drilling mud rather than seawater as a drilling fluid, which is
advantageous in unstable holes or areas with slow penetration.
Using a riser vessel will also allow scientists to drill holes deep into the
crust at both passive and convergent margins and will thus be invaluable to
studying the solid Earth cycle: the breaking apart of continents and formation
of sedimentary basins; the creation, evolution, and recycling of oceanic and
large igneous province lithosphere; and the creation of new continental lithosphere.
Drilling, logging and installing observatories by both the Chikyu and the riserless
drillship will also provide information on the behavior of rocks, sediments
and fluids in the seismogenic zone the region where most earthquakes
are generated. Drilling will also advance our progress toward a goal made in
the 1950s, a goal that spawned all ocean drilling programs: drilling to the
mantle beneath ocean crust. IODP plans to recover a complete section of oceanic
crust and uppermost mantle generated at a fast-spreading ridge in an effort
known as the 21st Century Mohole.
Riserless drilling
The United States through the alliance of the Joint Oceanographic Institutions
(JOI),Lamont-Doherty Earth Observatory of Columbia University and Texas A&M
University will operate a riserless drillship, similar to the vessel
used in ODP. In fact, for the first year, it will be the same vessel
the JOIDES Resolution. Riserless drilling is most effective in moderate to deep
water and allows for sampling over the majority of the worlds oceans.
Riserless drilling is also key to looking at the deep biosphere and subseafloor
ecosystem. Scientists will study the microbial populations that live beneath
the seafloor, as well as characterize fluid flow in the crust. IODP plans to
define the environmental conditions that support and limit the subseafloor biosphere,
as well as evaluate the biogeochemical impacts of the microbiota. IODP will
also continue the research conducted by ODP on gas hydrates, with aims to determine
hydrate dependence on microbes and quantify rates at which the gas is generated.
The Resolution sets sail on its maiden IODP voyage in June to explore fluids
in the oceanic crust at the Juan de Fuca Ridge in the northeast Pacific Ocean.
It will conduct five expeditions over the next year (see
sidebar) before an approximate year-long hiatus in drilling. During this
time, a vessel (the Resolution or a similar vessel) will be converted
to meet the long-term needs of IODP. Riserless expeditions are then expected
to resume on the upgraded ship in mid-2006.
Mission-specific platforms
An expedition
to the Arctic will take place this summer the first major drilling expedition
conducted there. A proposal to drill on the Lomonosov Ridge in the central Arctic
Ocean to study climate change and paleoceanography was the highest ranked proposal
for the final years of ODP, but the program was unable to conduct the expedition.
Sedimentologists and petrologists take turns describing cores recovered by the
JOIDES Resolution. For the first year of operations, scientists will continue
to conduct experiments aboard the Resolution as part of the Integrated
Ocean Drilling Program.
The logistics for a mission to the Arctic are complex coordinating three
icebreakers from different countries during the limited weather window of six
to eight weeks each summer when drilling is most feasible. IODP plans to use
the Vidar Viking as the scientific drillship, the Swedish icebreaker
Oden, and a third unnamed icebreaker to support the mission during the
voyage this summer. Through the expedition, scientists hope to understand both
the long-term climate history of the central Arctic Ocean and its role in Earths
transition from one extreme (Paleogene greenhouse) to another (Neogene icehouse
with glaciation at both poles). They also hope to gain insight into the shorter-term
climate history, connecting the Arctic Ocean to the North Atlantic Ocean at
sub-millennial scale resolution.
The European Consortium for Ocean Research Drilling, made up of 13 European
countries, will operate this and future mission-specific expeditions in shallow
waters and in ice-covered regions. These expeditions will be vital to achieving
IODPs initiatives of understanding extreme climates and rapid climate
changes. Although no future expeditions have been scheduled, scientists expect
to drill in the Tahiti/Great Barrier Reef area in 2005 to study sea-level rise
and climate change over the past 20,000 years.
International funding
Not only will IODPs multiple platforms obtain records worldwide, but support
for the programs will also be global. In that way, the international composition
of the scientific parties and advisory committees will differ from ODP.
During ODP, the United States contributed more than 50 percent of the costs
and therefore had half of the berths and membership on advisory committees.
The remaining 22 members shared the rest of the berth space and committee seats
in proportion to their financial contributions. In IODP, the United States and
Japan are equal partners, known as lead agencies. Organizations
in other countries, particularly European ones, will also participate at a significant
level. Although the proportion of U.S. scientists will decrease on each leg,
the increased number of platforms will allow for greater U.S. participation
overall. Meanwhile, opportunities for scientists from other nations will increase
in both relative and absolute terms.
Finally, scientists will notice the involvement of more funding agencies and
organizations. Because there are multiple lead agencies, each operating a vessel,
IODP Management International has been established to manage the programs
science operations. Furthermore, many countries have established national programs
to provide for their scientists, such as the U.S. Science Support Program. Education
and outreach opportunities will be conducted at all levels of IODP, providing
a much stronger presence than in previous programs.
Beyond the science
When the active phase of drilling in IODP commences in June of this year, nearly
a decade of planning for IODP will begin to draw to a close. During this planning
effort, the scientific imperatives of the program have been well defined. The
goals have provided the rationale for nearly 20 nations around the globe to
come together for the third phase of ocean drilling. These countries have done
so based on the conviction that the research to be undertaken will provide results
and understanding that will inform debate on many topics of global significance,
including climate change, sea-level rise, the carbon cycle, geologic hazards,
methane hydrate and other potential mineral and energy resources.
JOI President Steven Bohlen recently spoke to the IODP Science Planning and
Policy Oversight Committee about broadening the goals of the program to extend
beyond the initial science plan. The success of IODP will not be measured
only in terms of enhanced scientific understanding and discovery, Bohlen
said. Success will be measured by how much the public learns to appreciate
that Earths oceans are a critical, yet vastly undersampled and unexplored,
part of the earth system.
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