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They make up about 25% of all microbial plankton cells, and in the summer they may account for approximately half the cells present in temperate ocean surface water. The total abundance of P. ubique and relatives is estimated to be about 2 × 10 28 microbes. [ 73 ]
This vast air–water interface sits at the intersection of major air–water exchange processes spanning more than 70% of the global surface area . Bacteria in the surface microlayer of the ocean, called bacterioneuston, are of interest due to practical applications such as air-sea gas exchange of greenhouse gases, production of climate-active ...
Furthermore, bacteria can reproduce in as little as 20 minutes, [11] which allows for fast adaptation, meaning new strains of bacteria can evolve quickly. This has become an issue regarding antibiotic resistant bacteria. [citation needed] Thermophile bacteria from deep-sea vent. This organism eats sulfur and hydrogen and fixes its own carbon ...
Oxygen concentrations in the atmosphere remained around or below 0.001% of today's level until 2.4 Ga ago (the Great Oxygenation Event). [179] The rise in oxygen may have caused a fall in the concentration of atmospheric methane, and triggered the Huronian glaciation from around 2.4 to 2.1 Ga ago. In this way, cyanobacteria may have killed off ...
This vast air–water interface sits at the intersection of major air–water exchange processes spanning more than 70% of the global surface area . Bacteria in the surface microlayer of the ocean, called bacterioneuston, are of interest due to practical applications such as air-sea gas exchange of greenhouse gases, production of climate-active ...
Winds drive ocean currents in the upper 100 meters of the ocean's surface. However, ocean currents also flow thousands of meters below the surface. These deep-ocean currents are driven by differences in the water's density, which is controlled by temperature (thermo) and salinity (haline). This process is known as thermohaline circulation.
Vibrio vulnificus is expanding its range north at nearly 30 miles annually. So far 3 NC residents have died from Vibrio infections this year.
Hydrothermal vent plumes contain high concentrations of methane and carbon monoxide with methane concentration reaching 10 7 times of the surrounding ocean water. [11] [12] Deep ocean water is also a large reservoir of carbon and concentration of carbon dioxide species such as dissolved CO 2 and HCO 3 − around 2.2mM. [13]