But the latest research into sulphur - producing algae, ancient ice cores, and
sea sediments from the North Atlantic region could help climatologists
Not exact matches
Inadequate flood protection infrastructure, which right now might not contain high tides in El Nino years; Lack of action on annual
sediment removal
from spring freshets, which each year move over 30 million m3 of
sediment and leave about 3 million m3 of silt in the navigation and secondary channels of the lower reaches; and, By the end of this century
sea levels at the mouth of the river could potentially rise more than one meter due to climate change overtopping the diking system.
Sediment resources on the OCS are leased to local communities or federal agencies to help them restore shorelines or wetlands in an effort to address chronic erosion,
sea level rise, impacts
from major storms, or to protect valuable infrastructure and habitat.
This age was based on isotopic dating of 5 meteorites and a representative sample of modern Earth lead
from a Pacific deep -
sea sediment, all of which plot along a linear isochron on a graph of 207Pb / 204Pb versus 206Pb / 204Pb (Patterson, 1956).
Using the Great Barrier Reef as their study case, they estimated the evolution of the region over the last 14,000 years and showed that (1) high
sediment loads
from catchments erosion prevented coral growth during the early phase of
sea level rise and favoured deep offshore
sediment deposition; (2) how the fine balance between climate,
sea level, and margin physiography enabled coral reefs to thrive under limited shelf sedimentation rates at 6,000 years before present; and, (3) how over the last 3,000 years, the decrease of accommodation space led to the lateral extension of coral reefs consistent with available observational data.
By validating model results against geological observations, the study indicates that changes in runoff,
sea level and wave energy have profoundly affected the past evolution of the Great Barrier Reef not only in regard to reefs evolution but also
sediment fate
from source - to - sink.
Confirmation arrived in February this year, when an international team extracted 34
sediment cores
from three sites on the seabed, revealing a fossilised coral reef that reaches 110 metres into the
sea floor.
The team investigated
sediment cores collected
from Pine Island Bay in the Amundsen
Sea from the German research vessel RV Polarstern on two expeditions in 2006 and 2010.
Two meters (six and a half feet) below the surface he encountered a layer of
sediment marked by coral fragments, mollusk shells and coarse beach sand that could only have come
from the
sea.
They note that it is completely buried by
sediments from more recent eras, which indicates it was formed long before its surroundings, and that it has no topographic expression on the present
sea floor.
Across the species» range
from Baja California, Mexico, to Alaska, bioerosion on urchin - covered sandstone reefs, the researchers report, produces
sediment approximately equivalent to that delivered to the coast by a river — some 200 tons of
sediment per hectare — suggesting that when you stroll along the beach, a not insignificant chunk of the sand is, in fact,
sea urchin waste.
«We know the
sediments are of deep
sea and terrestrial origin, including those eroded
from the high Himalayas and transported thousands of kilometres into the Bay of Bengal and eastern Indian Ocean.
In a million years, barring profound shifts, the climate should have returned to its natural rhythms but any cities buried in
sediment by rising
seas should still be preserved, along with those signs of anthroturbation, human - induced disturbances underground, like the plutons
from underground explosions of nuclear bombs.
David Anderson of the University of Colorado at Boulder and his colleagues extracted cores of this fossil - filled
sediment from the floor of the Arabian
Sea to reconstruct monsoon intensity over the past 1,000 years.
From the geochemical analyses carried out on the sediments deposited during the past 10,000 years in the Laguna de Rio Seco lagoon, a remote alpine lake in Sierra Nevada, at 3,020 m. above sea level, evidence has been found of atmospheric pollution from l
From the geochemical analyses carried out on the
sediments deposited during the past 10,000 years in the Laguna de Rio Seco lagoon, a remote alpine lake in Sierra Nevada, at 3,020 m. above
sea level, evidence has been found of atmospheric pollution
from l
from lead.
Real - world data back the claim: Accumulations of calcium carbonate in deep -
sea Pacific
sediments show that the Pliocene ocean experienced huge shifts at the time, with waters churning all the way
from the surface down to about three kilometers deep, as would be expected
from a conveyor belt — type circulation.
The data come
from deep -
sea sediment cores dating to 205 million years ago that contain inorganic carbon - rich minerals as well as the organic remains of single celled marine phytoplankton.
Microorganisms living in basaltic
sea floor buried beneath
sediments derive energy
from inorganic components
from the host rocks that interact with infiltrating seawater, which brings dissolved oxygen and other trace nutrients with it.
Globally, salt marshes are being lost to waves, changes in land use, higher
sea levels, loss of
sediment from upstream dams and other factors.
Each of the river's identities — as the fertile nurturer and the wanton killer — derives
from the same feature: the 1 billion tons of
sediment that washes down each year
from the Loess Plateau to the Bohai
Sea.
Over a five - month period
from December 2004 to April 2005, the traps collected samples of
sediments and larva while the meters recorded deep -
sea current velocities.
Other papers in the issue examine how deep
sea sediments may affect seismic wave readings, and evaluate how the Cascadia Initiative's data collection
from ocean bottom seismometers has improved over the first three years of the study.
In extreme rain events,
sediment and associated pollution have already been shown to flow out to
sea in a pulse reaching as far out as 100 kilometers (62 miles) that can be seen
from space, said Richmond.
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.
Paleontologists must instead assemble timelines
from fragments, such as
sediment layers
from short - lived inland
seas.
Fumio Inagaki
from the Japan Agency for Marine - Earth Science and Technology, who made the discovery, says the lake probably formed when carbon dioxide seeped out through the ocean floor
from a deep -
sea volcano and pooled under a blanket of solid, icelike CO2 hydrate and deep -
sea sediment.
Records of
sea surface temperature
from oceanic
sediment cores, for example, show that the magnitude of warming following several previous glaciations are well - correlated (www.ncdc.noaa.gov/paleo/recons.html).
While this research was done with
sediments from South China, the
sea levels during the Early Triassic behaved globally.
Lutz and Falkowski cite one study where unique chemical compounds isolated
from an actinomycete strain inhabiting deep -
sea sediments about 3.3 kilometers down in the South China Sea have shown potent activities against three cancerous tumor cell lines and also showed antibacterial activiti
sea sediments about 3.3 kilometers down in the South China
Sea have shown potent activities against three cancerous tumor cell lines and also showed antibacterial activiti
Sea have shown potent activities against three cancerous tumor cell lines and also showed antibacterial activities.
The slimy mats acted as a barrier between the water above and the
sediments below, preventing oxygen
from reaching under the
sea floor and making it largely uninhabitable.
Radioactive materials released into the Irish
Sea from the Sellafield reprocessing plant over the past 40 years may eventually accumulate in thick sandy
sediments midway between Ireland and the Isle of Man, according to the British government's Directorate of Fisheries Research.
A
sediment sample
from a knoll at a depth of 1170 metres identified a remarkable cold - water coral community of both living and fossil cold - water coral species, gorgonian
sea whips, bamboo corals, molluscs and stalked barnacles.
Warming and the
seas — both on the rise Those ancient samples of
sediment from 10 coastal wetlands in North Carolina provide some of the best evidence that
sea - level rise closely follows warmer temperatures, Rahmstorf says.
The team also found DNA
from a form of marine alga in 9300 - year - old
sediments, though the alga doesn't show up in the fossil record until 2500 years ago, says molecular paleoecologist Marco Coolen of the Woods Hole Oceanographic Institution in Massachusetts and an author of the Black
Sea paper.
The researchers, which include U.S. teams
from NOAA, the U.S. Geological Survey (USGS), and the University of New Hampshire, will be collecting seismic data
from this region by bouncing sound blasts off the
sea floor to determine its
sediment makeup, as well conducting a multibeam analysis that will give them an idea of the shape of the ridge.
Martinez - Boti and his colleagues dug out
sediments from the Caribbean
Sea and tropical Atlantic Ocean.
Coolen's finding of marine species invading the Black
Sea earlier than had been thought «is not something you could see
from looking at fossils or
sediment properties,» Kucera says.
They found that the embankments that protect the land
from the river and
sea had also robbed it of fresh supplies of
sediment: during the five decades of its existence, the polder had sunk by a full meter relative to the land outside the embankments because it was not being replenished.
18Oc measured in foraminifera collected
from deep
sea sediment cores (Lisiecki et al., 2005).
Many others, he notes, suggest that samples are too easily contaminated during drilling by microbes that live in overlying
sediments, or by inadequate precautions while handling the samples once they've been retrieved
from the
sea floor.
There, they collected mud
from the
sea floor, which builds up for millions of years like a giant layer cake as newer
sediments pile on top of older ones.
Evidence for approximately contemporaneous global cooling in
sediments that do contain YTT glass shards has been found in marine core oxygen isotope records
from the South China
Sea (3), as have terrestrial carbon isotope and pollen records
from Northern India and Bengal (23).
By studying
sediment cores
from the deep Pacific near the Philippines, paleoclimatologist Lowell Stott of the University of Southern California in Los Angeles and his colleagues revealed that the temperatures of the deepest
seas rose by around 2 degrees Celsius (3.6 degrees Fahrenheit) at least 1,000 years before
sea - surface temperatures.
They analysed
sediments from a shallow Atlantic Ocean shelf where
sediment accumulates faster than it does in the deep
sea, making it easier to see seasonal fluctuations in the amount deposited.
Heavy metals including cadmium and lead are unusually common in
sediments from the South China
Sea, hinting that run - off
from farms was spilling into the ocean 4000 years ago
As the Earth continued to cool
from Years 0.1 to 0.3 billion, a torrential rain fell that turned to steam upon hitting the still hot surface, then superheated water, and finally collected into hot or warm
seas and oceans above and around cooling crustal rock leaving
sediments.
«We have recovered two new high - resolution paleomagnetic records of the Laschamp Excursion (~ 41,000 calendar years B.P.)
from deep -
sea sediments of the western North Atlantic Ocean.
Jorgenson, M.T., and J. Brown, 2005: Classification of the Alaskan Beaufort
Sea Coast and estimation of carbon and
sediment inputs
from coastal erosion.
See Page 4 - 22, Figure 9: Geomagnetic field intensity level derived
from composite volcanic records, not
sea floor
sediments, for the past 45 kyr.
Those same
sediments held another clue as well — the fossilized shells of plankton (small floating
sea organisms)
from the dinosaur days.