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The origin of deep ocean microseisms in the North Atlantic Ocean
microseisms wave – wave interaction acoustic resonance wave model Stoneley waves
2014/4/10
Oceanic microseisms are small oscillations of the ground, in the frequency range of 0.05–0.3 Hz, associated with the occurrence of energetic ocean waves of half the corresponding frequency. In 1950, L...
Biotic stoichiometric controls on the deep ocean N:P ratio
Biotic stoichiometric controls deep ocean N:P ratio
2010/1/14
We re-examine what controls the deep ocean N:P ratio in the light of recent findings that the C:N:P stoichiometry of phytoplankton varies with growth rate, nutrient and light limitation, species and p...
Deserts on the seafloor: Edward Forbes and his azoic hypothesis for a lifeless deep ocean by Tom Anderson（图）
Marine Life
2007/4/11
5 April 2007，Deserts on the seafloor: Edward Forbes and his azoic hypothesis for a lifeless deep ocean by Tom Anderson，While dredging in the Ægean Sea during the mid-19th century, Manxman, Edwar...
Focusing of phytodetritus deposition beneath a deep-ocean front, Chatham Rise, New Zealand
Focusing of phytodetritus deposition beneath deep-ocean front Chatham Rise New Zealand
2014/4/22
In October 2001, we observed a deep-ocean phytodetritus deposition event on Chatham Rise beneath the Subtropical Front (STF). The origin of this phytodetritus was probably an extensive phytoplankton b...
Rapid climate change and conditional instability of the glacial deep ocean from the thermobaric effect and geothermal heating
Rapid climate change conditional instability glacial deep ocean thermobaric effect geothermal heating
2014/4/9
Previous results from deep-sea pore fluid data demonstrate that the glacial deep ocean was filled with salty, cold water from the South. This salinity stratification of the ocean allows for the possib...
Dissolution from a liquid CO2 lake disposed in the deep ocean
Dissolution liquid CO2 lake disposed deep ocean
2014/5/20
The dissolution from a liquid CO2 lake source located at a flat ocean bottom at 3,000 m depth is investigated. Using the unsteady, two-dimensional advection-diffusion equation, temporal and spatial di...
The Salinity, Temperature, and 18O of the Glacial Deep Ocean
The Salinity Temperature 18O Glacial Deep Ocean
2014/4/9
We use pore fluid measurements of the chloride concentration and the oxygen isotopic composition from Ocean Drilling Program cores to reconstruct salinity and temperature of the deep ocean during the ...
Role of the oxygen-deficient zone in transfer of organic carbon to the deep ocean
the oxygen-deficientzone in transfer organic carbon the deep ocean
2014/6/10
Benthic carbon oxidation rates and carbon burial rates have been determined for two contrasting continental margins and their sum has been used as an estimate of carbon rain rate to the sediments. On ...