The ocean’s biological carbon pump plays a central role in regulating atmospheric CO2 levels. In particular, the depth at which sinking organic carbon is broken down and respired in the mesopelagic zone is critical, with deeper remineralisation resulting in greater carbon storage. Until recently, however, a balanced budget of the supply and consumption of organic carbon in the mesopelagic had not been constructed in any region of the ocean, and the processes controlling organic carbon turnover are still poorly understood. Large-scale data syntheses suggest that a wide range of factors can influence remineralisation depth including upper-ocean ecological interactions, and interior dissolved oxygen concentration and temperature. However these...
The “biological carbon pump” causes carbon sequestration in deep waters by downward transfer of orga...
The ocean region known as the mesopelagic zone, which is at depths of about 100–1,000 m, harbours on...
The biological pump is a process whereby CO2 in the upper ocean is fixed by primary producers and tr...
The ocean’s biological carbon pump plays a central role in regulating atmospheric CO2 levels. In par...
The ocean's biological carbon pump plays a central role in regulating atmospheric CO2 levels. In par...
Through the constant rain of sinking marine particles in the ocean, carbon (C) trapped within is exp...
The biological carbon pump, which transports particulate organic carbon (POC) from the surface to th...
The sinking of photosynthetically produced organic carbon from the ocean surface to its interior is ...
Today, the key role played by oceans in the Earth's carbon cycle is widely recognized. The important...
© The Authors, 2011. This article is distributed under the terms of the Creative Commons Attributio...
The oceans’ biological pump (BP) exports large amounts of particulate organic carbon (POC) to the me...
This paper reviews progress on understanding biological carbon sequestration in the ocean with speci...
The ocean carbon cycle plays a fundamental role in the Earth’s climate system, on decadal to multi-m...
Author Posting. © American Geophysical Union, 2008. This article is posted here by permission of Am...
Presented at the workshop : Modelling the response of marine ecosystems to increasing levels of CO2....
The “biological carbon pump” causes carbon sequestration in deep waters by downward transfer of orga...
The ocean region known as the mesopelagic zone, which is at depths of about 100–1,000 m, harbours on...
The biological pump is a process whereby CO2 in the upper ocean is fixed by primary producers and tr...
The ocean’s biological carbon pump plays a central role in regulating atmospheric CO2 levels. In par...
The ocean's biological carbon pump plays a central role in regulating atmospheric CO2 levels. In par...
Through the constant rain of sinking marine particles in the ocean, carbon (C) trapped within is exp...
The biological carbon pump, which transports particulate organic carbon (POC) from the surface to th...
The sinking of photosynthetically produced organic carbon from the ocean surface to its interior is ...
Today, the key role played by oceans in the Earth's carbon cycle is widely recognized. The important...
© The Authors, 2011. This article is distributed under the terms of the Creative Commons Attributio...
The oceans’ biological pump (BP) exports large amounts of particulate organic carbon (POC) to the me...
This paper reviews progress on understanding biological carbon sequestration in the ocean with speci...
The ocean carbon cycle plays a fundamental role in the Earth’s climate system, on decadal to multi-m...
Author Posting. © American Geophysical Union, 2008. This article is posted here by permission of Am...
Presented at the workshop : Modelling the response of marine ecosystems to increasing levels of CO2....
The “biological carbon pump” causes carbon sequestration in deep waters by downward transfer of orga...
The ocean region known as the mesopelagic zone, which is at depths of about 100–1,000 m, harbours on...
The biological pump is a process whereby CO2 in the upper ocean is fixed by primary producers and tr...