Within the NSF, the Earth Sciences Division supports research on the continental and coastal record of sedimentary basins, while the Ocean Sciences Division supports ocean basin and
deep ocean water research.
Not exact matches
A new study in Marine Biology
Research tackles this issue by comparing the physical characteristics of two similar octopus species that live on the
ocean floor, as
deep as 9,500 feet (almost 2,900 m) below the
water's surface.
«The undersides of glaciers in
deeper valleys are exposed to warm, salty Atlantic
water, while the others are perched on sills, protected from direct exposure to warmer
ocean water,» said Romain Millan, lead author of the study, available online in the American Geophysical Union journal Geophysical
Research Letters.
But
research published yesterday in the journal Nature rebuts this idea, suggesting that it was changes in
ocean circulation, not winds, that predominantly led the
deep water to surface near Antarctica and exhale carbon dioxide to the atmosphere.
Research begun at Princeton University found that the numerous small sea animals that migrate from the surface to
deeper water every day consume vast amounts of what little oxygen is available in the
ocean's aptly named «oxygen minimum zone» daily.
«These results show that the effect of
ocean acidification on deep - water corals may not be as severe as predicted,» said David Garrison, a program director in the National Science Foundation's Division of Ocean Sciences, which funded the rese
ocean acidification on
deep -
water corals may not be as severe as predicted,» said David Garrison, a program director in the National Science Foundation's Division of
Ocean Sciences, which funded the rese
Ocean Sciences, which funded the
research.
This enabled the
research team to reconstruct, for the first time, a detailed picture of the environmental conditions at the
ocean's surface, as well as in
deeper water layers, over the last 30,000 years.
One morning last August, the Monterey Bay Aquarium
Research Institute's
deep - sea robot, named Doc Ricketts, was snooping around the
ocean floor in 1,812 meters of very cold
water off the coast of northern California.
This
research not only provides the first clear evidence that microorganisms were directly involved in the deposition of Earth's oldest iron formations; it also indicates that large populations of oxygen - producing cyanobacteria were at work in the shallow areas of the ancient
oceans, while
deeper water still reached by the light (the photic zone) tended to be populated by anoxyenic or micro-aerophilic iron - oxidizing bacteria which formed the iron deposits.
A young polar bear stands on pack ice over
deep waters in the Arctic
Ocean in October 2009, during a major
research project headed by the University of Wyoming.
The team sailed from the Monterey Bay Aquarium
Research Institute in California to a well - studied part of the
ocean known as Line 67, where the
water is
deep yet poor in nutrients.
In his
research published in the December issue of the journal Geology of the Geological Society of America, Czaja and his colleagues Nicolas Beukes from the University of Johannesburg and Jeffrey Osterhout, a recently graduated master's student from UC's department of geology, reveal samples of bacteria that were abundant in
deep water areas of the
ocean in a geologic time known as the Neoarchean Eon (2.8 to 2.5 billion years ago).
Research cruises such as Tara
Oceans and the Global
Ocean Sampling Expedition have begun to sample, sequence and analyze the ocean microbiome, from the sunlit surface waters that are mixed by the wind to dark deep layers that relatively unpertu
Ocean Sampling Expedition have begun to sample, sequence and analyze the
ocean microbiome, from the sunlit surface waters that are mixed by the wind to dark deep layers that relatively unpertu
ocean microbiome, from the sunlit surface
waters that are mixed by the wind to dark
deep layers that relatively unperturbed.
Even in the absence of oxygen, the
research team found that the respiration of organic carbon occurring in the anoxic
waters of the Black Sea is not as different from that occurring in the
deep ocean.
Deeply
researched and compellingly presented,
Deep Water is as much about one man's misadventures on the
ocean as it is about loneliness, desperation and the danger of dreams.
As researchers concluded in a new study published in Geophysical
Research Letters,
ocean iron fertilization can only prove successful as a climate geoengineering approach if, in addition to phytoplankton bloom stimulation, «a proportion of the particulate organic carbon (POC) produced must sink down the
water column and reach the main thermocline or
deeper before being remineralized... and the third phase is long - term sequestration of the carbon at depth out of contact with the atmosphere.»
In recent years
research tied the Bølling - Allerød warming to the release of heat from warm
waters originating from the
deep North Atlantic
Ocean, possibly triggered by a strengthening of the Atlantic meridional overturning circulation (AMOC) at the time.
New Dutch
research has shown for instance the overturning has been relatively weak in recent years [which means cold
water has accumulated close to the surface instead of sinking to
deeper waters, one of two reasons why there has been a lull in upper
ocean warming].
The «strong trade winds,» says study co-author Gerald Meehl of the U.S. National Center for Atmospheric
Research, «are bringing cooler
water to the surface in the equatorial Pacific and mixing more heat into the
deeper ocean.»
Research programs at the Monterey Bay Aquarium
Research Institute (MBARI) encompass the entire
ocean, from the surface
waters to the
deep seafloor, and from the coastal zone to the open sea.
One, on the effects of oil spills into Canadian marine
waters released in 2015 by an expert panel of the Royal Society of Canada, concluded that more
research is required «to better understand the environmental impact of spilled crude oil in high - risk and poorly understood areas, such as Arctic
waters, the
deep ocean and shores or inland rivers and wetlands.»