The dates on two
other ocean sediment cores (Stott et al 2004 — # 14 and # 15) are on the correct scale thankfully, but are still marginal in terms of resolution (29 and 44 years respectively, but effectively longer still due to bioturbation of the sediments).
Not exact matches
These samples augment
other marine records such as coral and seashells, which provide detailed records over a short time period, and deep -
ocean sediments, which preserve thousands of years of history but are harder to date precisely.
Other hostile conditions deep in
ocean sediments, such as scarce nutrients, high pressure, or extreme salinity, probably set life's limit in some places.
This time Becker, Basu, and four
other coauthors described a submarine hump called Bedout High that is buried in
ocean sediments 100 miles off the northwest coast of Australia.
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.
There are
other proxies, such as tree rings or
ocean sediments, but their messages have to be decoded and interpreted by scientists.
Tides, storms and
other disturbances in shallow water will stir up the bottom, while further from shore, where the water is deeper, turbulence can not reach the
ocean floor, allowing
sediment to settle undisturbed.
The increased wave action reaches down and stirs up
sediments on shallow continental shelves, releasing radium and
other chemicals that are carried up to the surface and swept away into the open
ocean by currents such as the Transpolar Drift.
These organisms are important because they churn up
sediments from the bottom of the
ocean, a process known as «bioturbation», playing a vital role in returning nutrients to surrounding water as food for
other creatures.
In most places in the world's
oceans, microbes consume all the oxygen less than 10 centimeters into the
sediment and below that depth switch to using
other compounds for respiration.
An analysis of
sediment from 17 seabed sites — from European estuaries to the Great Barrier Reef in Australia and the deep Atlantic
Ocean — found that the bathyal region of the Rockall Trough has more species than any
other area so far measured.
Carbonic acid dissociated to form hydrogen ions, which found their way into the structures of weathering minerals, and bicarbonate, which was carried down rivers and streams to be deposited as limestone and
other minerals in
ocean sediments.
In addition, they are now extending MOSART to simulate how
sediment, carbon and
other nutrients move from the landscape through the rivers and into the
ocean.
Microorganisms dominate all
other life everywhere scientists have looked, including the human body, the Earth's soils and
sediments, the
oceans and fresh waterways, the atmosphere and even extreme environments such as hydrothermal vents and subglacial lakes.
Ancient
sediments that once resided on a lake bed and the
ocean floor show sulfur isotope ratios unlike those found in
other samples from the same time, calling into question accepted ideas about when the Earth's atmosphere began to contain oxygen, according to researchers from the U.S., Canada and Japan.
While this view has been changing for some time, a revolution in our thinking came with the discovery of Lokiarchaeum («Loki») and
other members of the «Asgard» clade of archaea through metagenomic sampling of
ocean sediments in 2015.
The team also correlated their findings with
other studies of California climate history, and for the first time, cross-referenced these with histories of the Pacific
Ocean's temperature taken from marine
sediment cores and
other sources.
But I got weathered Into wet
sediments Carried to the
ocean There the little bits of me Layered with
other sediments.
[15] Through study of Pacific
Ocean sediments, other researchers have shown that the transition from warm Eocene ocean temperatures to cool Oligocene ocean temperatures took only 300,000 years, [11] which strongly implies that feedbacks and factors other than the ACC were integral to the rapid coo
Ocean sediments,
other researchers have shown that the transition from warm Eocene
ocean temperatures to cool Oligocene ocean temperatures took only 300,000 years, [11] which strongly implies that feedbacks and factors other than the ACC were integral to the rapid coo
ocean temperatures to cool Oligocene
ocean temperatures took only 300,000 years, [11] which strongly implies that feedbacks and factors other than the ACC were integral to the rapid coo
ocean temperatures took only 300,000 years, [11] which strongly implies that feedbacks and factors
other than the ACC were integral to the rapid cooling.
If there is — say some combination of
other elements adding to produce a better structure for the «cage» of water molecules that trap methane, say occurring naturally in pore spaces in
sediment or leaf litter washed into the
ocean — it ought to be discoverabe.
I think the ice core is considered the most reliable, especially in terms of better temporal resolution, than the
other proxies from
ocean sediment.
Examinations of paleoclimate temperatures and
other variables recorded in both North Atlantic
ocean sediments and Greenland ice cores (e.g., Lehman and Keigwin, 1992; Alley et al., 1993; Taylor et al., 1993) have led to suggestions that the AMOC
They found that the dense, salty water from the Marmara Sea — which leads out to the Aegean and Mediterranean Seas at the
other end of the Bosphorus — is flowing out of the strait and along the bottom of the Black Sea, carrying along
sediment and nutrients that could be key in providing vital nutrients to remote parts of the
ocean.