Thousands of years ago,
sea sediments made by different chemical compounds formed these striped patterns across the land.
Not exact matches
The study suggests that layers of
sediments perhaps 10 to 20 meters thick can seal the
sea floor and
make seamounts the most important conduits for heat and fluid flow — especially on the sloping flank of a midocean ridge, says oceanographer John Sclater of the Scripps Institution of Oceanography in La Jolla, California.
More than 12,000 years ago, Pine Island and Thwaites glaciers were grounded on top of a large wedge of
sediment, and were buttressed by a floating ice shelf,
making them relatively stable even though they rested below
sea level.
Most of our
sea - level records are based on the chemical
make - up of
sediment cores, which are hard to date — estimates can be thousands of years out.
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 new measurements in this research were
made with cores that showed the results of massive amounts of
sediments released by subsea landslides during a subduction zone earthquake — a catastrophic event beneath the
sea as well as on land.
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.
In their study of
sediments from the Black
Sea, Eckert et al. (2013, p. 431 in this issue of Geology),
make this step by providing, for the first time, a basin - wide reconstruction of the evolution of the chemocline in this silled coastal basin over the Holocene.
It is also possible for cold climates to increase chemical weathering in some ways, by lowering
sea level to expose more land to erosion (though I'd guess this can also increase oxydation of C in
sediments) and by supplying more
sediments via glacial erosion for chemical weathering (of course, those
sediments must
make it to warmer conditions to
make the process effective — downhill and downstream, or perhaps via pulsed ice ages -LRB-?)-RRB-.
This is not necessarily a contradiction to the other data series, because the two
sediment cores used are located in the area of the deep outflow of Labrador
Sea Water — but this is only one of two deep currents that together
make up the southward part of the overturning circulation of the Atlantic, and thus the heat transport to the north.
Then, by analysing the
sediments for chemical fossils
made by certain microscopic plants that live in
sea ice and the surrounding oceans, Knies and his co-workers were able to fingerprint the environmental conditions as they changed through time.
Union of Concerned Scientists: Human Fingerprints Science Daily: Deep -
sea Sediments Could Safely Store Man -
made Carbon Dioxide Discovery Channel: Global Warming
External stressors can
make it difficult to define the parameters of target ecosystem services: While an emerging blue carbon PES scheme might successfully protect a mangrove from deforestation, it may have little influence on changes in upstream
sediment loads or on
sea - level rise.
That
makes me wonder, is there a critical rate of
sea level rise above which the reefs can't collect
sediment quickly enough to keep up?
There is a diffrence of permafrost and
sea sediment methane — why not
make the diffrence?
Hemant Shah, president and CEO of Newark, Calif. - based RMS, identifies three troubling factors: the city is sinking due to thick
sediments accumulating along the Atlantic Ocean's basin; accelerated climate change in
making the
sea level rise, and the level of Atlantic basin hurricane activity has increased in recent years.