Scientists devised ingenious techniques to recover evidence from the distant past, first from deposits left on land, then also
from sea floor sediments, and then still better by drilling deep into ice.
>... there are still ways of discovering the temperatures of past centuries,... tree rings... Core samples from drilling in ice fields... historical reconstruction... coral growth, isotope data
from sea floor sediment, and insects, all of which point to a very warm climate in medieval times.
Not exact matches
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.
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.
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.
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.
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.
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.
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.
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.
See Page 4 - 22, Figure 9: Geomagnetic field intensity level derived
from composite volcanic records, not
sea floor sediments, for the past 45 kyr.
The most likely explanation is the mass release of methane
from sediments on the
sea floor, where the gas was sequestered, as it is now, in a solid form as methane hydrate.
The gray whale is unique in the use of its baleen feeding technique as contrasted to other baleen whales.According to the National Marine Mammal Laboratory, «Gray whales are bottom feeders, and suck
sediment and the «benthic» amphipods that are their prey
from the
sea floor.
So if you want to check whether erosion and
sediment transport were taking place during the Pliocene, the best bet is to sample the
sediments on the
sea -
floor dating
from that time, by drilling through them and taking cores.
In a core of
sediments taken
from the
sea floor that was once covered by the Larsen A Ice Shelf, researchers led by Dr. Eugene W. Domack, a professor of geology at Hamilton College in Clinton, N.Y., found the tiny fossils of marine algae.
They live only in a few borderline places, however; for global temperatures scientists use not only other species of trees but a wide variety of «proxies»
from ice cores, coral reefs, cave deposits, the
sea floor, pollen in lake
sediments, boreholes in rock and so forth.
However, most of the methane produced
from dissociating marine hydrates will be consumed by anaerobic processes in the top few metres of sulphate - rich near -
sea -
floor sediments and all of the rest will be dissolved and oxidized in
sea water and will not be released to the atmosphere as methane, although the dissolved CO2 will equilibrate with atmosphere after a few centuries.
From their trawlers scraping the floors of the seas to their dams impounding sediment by the gigatonne, from their stripping of forests to their irrigation of farms, from their mile - deep mines to their melting of glaciers, humans were bringing about an age of planetary cha
From their trawlers scraping the
floors of the
seas to their dams impounding
sediment by the gigatonne,
from their stripping of forests to their irrigation of farms, from their mile - deep mines to their melting of glaciers, humans were bringing about an age of planetary cha
from their stripping of forests to their irrigation of farms,
from their mile - deep mines to their melting of glaciers, humans were bringing about an age of planetary cha
from their mile - deep mines to their melting of glaciers, humans were bringing about an age of planetary change.
Proxy data such as those generated
from ice core samples, measurements of tree rings intervals, bore samples taken
from sediments from the ocean and
sea floor, and measurement of gases
from bubbles trapped in ice are some examples of preserved physical characteristics of the past used by scientists to reconstruct prevailing climatic conditions in the past.
Much of the color likely comes
from resuspended
sediment dredged up
from the
sea floor in shallow waters.
To measure how the system has shifted over long timescales, researchers collected long cores of
sediment from the
sea floor.
Episodic and explosive escapes of gaseous methane
from the
sediment column have been documented by kilometer - scale «wipeout zones» in seismic images (Riedel et al., 2002), and pockmarks on the
sea floor, called eruption craters (Hill et al., 2004).
According to the invention,
sediments including clathrate - rich material disturbed
from the
sea floor are carried upward, with the aid of injection gas.
In the 1970s, the first comprehensive analysis of oxygen isotopes in
sediments from cores taken
from the
sea floor established for the first time that the timing of the Ice Ages was linked to subtle changes in the Earth's orbit around the Sun as suggested long ago by Serbian mathematician Milutin Milankovitch.