A recent study by Moffitt and colleagues
of seafloor sediments from the end of the last Ice Age, around 10,000 to 17,000 years ago, revealed that Pacific Ocean ecosystems from the Arctic to Chile «extensively and abruptly lost oxygen when the planet warmed through deglaciation,» she said.
On the last day of a research cruise off the coast of Antarctica this spring, Hamilton College marine geologist Eugene Domack and his team lowered a video camera overboard to capture images
of the seafloor sediments they had been studying.
This is an acorn worm, a scavenger
of seafloor sediment that the researchers found in the North Atlantic.
The idea is that as they dug and wiggled, these early multicellular creatures — some were likely worms as long as 40 cm — exposed new layers
of seafloor sediment to the ocean's water.
The researchers studied cores
of seafloor sediment representing 500,000 years of deposition, spanning about 6,000 miles of the Pacific equator, from near Papua New Guinea to near Ecuador's Galapagos Islands — nearly a quarter of the globe's girth.
Not exact matches
The foundation
of the research involved tracking the changes in ocean circulation in new detail by studying three
sediment cores extracted from the
seafloor of the Gulf
of Mexico in 2010 during a scientific cruise.
Essentially an x-ray
of the
seafloor, this technique allowed the team to reconstruct the thickness and likely composition
of buried
sediment layers.
In fact, the cells show so few signs
of life that it wasn't until 2011 that researchers confirmed that microbes in
sediments below the
seafloor are, indeed, living.
The team analysed the chemical composition
of tiny shells built by organisms (foraminifera) that had lived in the water column and at the sea bottom before their shells became embedded in the
seafloor sediments.
Led by Ken Buesseler, a senior scientist and marine chemist at the Woods Hole Oceanographic Institution (WHOI), the team found that a small fraction
of contaminated
seafloor sediments off Fukushima are moved offshore by typhoons that resuspend radioactive particles in the water, which then travel laterally with southeasterly currents into the Pacific Ocean.
His team bored several three - meter - long columns
of sediment from parts
of the
seafloor that were covered by Larsen B until its collapse.
The researchers drilled down 1,500 meters below the
seafloor in two places off the coast
of Sumatra, extracting narrow cylinders
of sediment.
Working in remote conditions, researchers in the winter
of 2012 ran a drill through 450 meters
of ice and 500 meters
of ocean to collect
seafloor sediments on either side
of this lost bulwark.
In addition to a marine biologist's typical tools — water samplers to measure salinity and temperature, plankton nets — the team's toolbox will hold cameras, coring systems to collect
seafloor sediment, and hydroacoustic equipment to map the topography
of the now - exposed seabed.
IODP is a collaboration
of scientists from 23 countries; the organization coordinates voyages to study the history
of the Earth recorded in
sediments and rocks beneath the
seafloor.
Methane gets squeezed out
of the deepest layers
of sediments like water from a sponge and migrates up toward the
seafloor.
Hundreds
of yards below the
seafloor, microbes called archaea produce methane from hydrogen and carbon extracted from organic
sediments.
The purpose was to create a bathymetric picture
of the sea bottom and to collect reflection seismic data, which allows researchers to peer into the
sediments and rocks underneath the
seafloor.
The levees disconnect the river and an estimated 210 million tons
of sediment that would naturally flow down to the delta and build the wetlands and the
seafloor.
During the 20th century, thousands
of dams were built on Mississippi River tributaries stopping the flow
of fine silt, clay and other
sediment from reaching the delta and
seafloor to offset erosion.
In addition, the total amount
of cesium retained more than 3 feet deep in the sands is higher than what is found in
sediments on the
seafloor offshore
of the beaches.
The shale, named for the town
of Eagle Ford, TX, is a geologic remnant
of the ancient ocean that covered present day Texas millions
of years ago, when the remains
of sea life (especially ancient plankton) died and deposited onto the
seafloor, were buried by several hundred feet
of sediment, eventually turning into the rich source
of hydrocarbons we have today.The shale was first tapped in 2008 and now has around 20 active fields good producing over 900 million cubic feet per day
of natural gas.
Knudson and Ravelo based their findings on an analysis
of carbon and oxygen isotopes in the calcium carbonate shells
of tiny marine organisms called foraminifera, which are preserved in
seafloor sediments.
Surprise find The team's actual mission was to survey ocean currents near the Ross Ice Shelf, a slab
of ice extending more than 600 miles (970 kilometers) northward from the grounding zone
of the West Antarctic Ice Sheet into the Ross Sea, to model the behavior
of a drill string, a length
of pipe extending to the
seafloor which delivers drilling fluids and retrieves
sediment samples.
Dr. Edwards took deep
sediment core samples to further understand the geology
of the region including the unusual
seafloor mound where these samples were collected.
The primary purpose
of the expedition was to map the Arctic
seafloor and the
sediments beneath.
Look at these distances: It requires almost a thousand kilometers
of seafloor spreading to record the same amount
of time that you find in 150 meters
of mountain
sediment, so the earth is running two magnetic tape recorders.
Now
seafloor sediments reveal that Larsen B's grounding line had remained stable for thousands
of years before the ice shelf's collapse.
The lack
of oxygen on the local
seafloor kept the area free
of bottom - dwelling scavengers, and
sediment quickly covered the animals» corpses, preserving them in unprecedented detail.
In addition to methane hydrates, carbon - rich permafrost that is tens
of thousands
of years old — and found throughout the Arctic on land and in
seafloor sediments — can produce methane once this material thaws in response to warming.
The first Ediacaran to begin crawling around would have discovered a world devoid
of predatory animals, with a
seafloor covered either in thick bacterial mats or toxic
sediment and, possibly, a climate thawing from a worldwide glaciation event known as «Snowball Earth.»
Finally, they used a
seafloor - crawling robot, the Benthic Rover, to measure the amount
of oxygen being consumed by animals and microbes in the
sediment.
When dozens
of meters
of new
sediment settle on the
seafloor, the solid compounds dissociate at the base
of the hydrate stability zone, while new hydrates can form at the upper end
of the stability zone.
From this, they calculated that sinkers contribute 7.6 grams
of carbon per square meter
of seafloor each year, an uncanny match to a food deficit found in a study using
sediment traps.
They suspended conical «
sediment traps» above the
seafloor to collect and measure the amount
of marine snow falling through the water.
Researchers
of the Senckenberg Biodiversity and Climate Research Centre, the Goethe University in Frankfurt and the University
of Toronto have now detected evidence
of this oceanographic event and an earlier sudden sea - level rise in the fossils
of tiny calcifying marine algae preserved in
seafloor sediments in the Aegean Sea.
Not only is there a much higher diversity
of microbes under the
seafloor than originally thought, large and active populations exist much deeper in the
sediments than was believed, the team reports 21 July in Nature.
Meanwhile, researchers at the University
of Tokyo reported at a conference in Tokyo in June that they have discovered
seafloor sediments in Japanese waters that contain an estimated 6.8 million tonnes
of rare - earth elements.
This picture may be about to change in light
of a study
of deep - sea rocks and
sediments led by John Parkes, a microbiologist at Cardiff University in the U.K.. By visiting oil - drilling projects at two sites in the Pacific in 2002, Parkes and colleagues obtained samples as deep as 400 meters beneath the
seafloor.
Karla Knudson analyzed isotopes in the shells
of tiny marine organisms preserved in
seafloor sediments to find chemical signatures
of past water temperatures and other oceanographic conditions.
They lived at the bottom
of shallow seas and were able to bury into the muddy
sediment of the
seafloor.
Abrupt Rise in Sea Level Delayed the Transition to Agriculture in Southeastern Europe (22/03/2018) Researchers
of the Senckenberg Biodiversity and Climate Research Centre, the Goethe University in Frankfurt and the University
of Toronto have detected evidence
of this oceanographic event in the fossils
of tiny calcifying marine algae preserved in
seafloor sediments in the Aegean Sea.
It discusses the clay mineral composition
of sediment samples taken from the
seafloor surface and marine cores in order to decipher spatial and temporal changes in the
sediment provenance.
Their data from the other pole, from the Antarctic ice sheet, bring us an important step closer to nailing down the mechanism
of the mysterious abrupt climate jumps in Greenland and their reverberations around the world, which can be identified in places as diverse as Chinese caves, Caribbean
seafloor sediments and many others.
Her work immediately brought to mind the ceramics
of Joan Lederman, an artist in Woods Hole, Mass., who creates glazes from
seafloor sediments retrieved by oceanographers roaming the world from the nearby Woods Hole Oceanographic Institution:
Large amounts
of methane are stored in
seafloor sediments as gas hydrate, and as these melt the gas is released into the water column.
Data on bathymetry, demersal fish, sponges and
sediments, and oceanographic data, were used to identify a suite
of unique
seafloor bioregions comprising 41 provinces, three depth - related biomes on the continental slope, and geomorphic units that represent clusters
of geomorphic features around the EEZ.
Methane hydrates that are on the edge
of stabilization can be disturbed by global warming in two additional ways, temperature and pressure: Warming
of the Earth's crust as heat penetrates
sediments on the
seafloor.
Most
of Earth's gas hydrates occur at low saturations and in
sediments at such great depths below the
seafloor or onshore permafrost that they will barely be affected by warming over even 1000 yr.
Nearly four years ago, geological surveys
of the Arctic Ocean
seafloor revealed the presence
of shells buried deep in its
sediment.