Productivity of the glacial ocean: Discussion of the iron hypothesis
- Scripps Institution of Oceanography, La Jolla (United States)
- Univ. Bremen (Germany)
An increase in the productivity of the glacial-age Southern Ocean has been postulated to explain the decrease in pCO{sub 2} of the atmosphere observed in ice cores. A plausible mechanism has been proposed elsewhere that productivity is limited by the availability of Fe in this region and that the greater supply of eolian dust during glacial time removed this limit. Recently published evidence from cores from the Southern Ocean suggests that in fact there was no change in productivity in the assumed manner. Glacial-age productivity was indeed greatly increased in the equatorial Pacific and in the eastern boundary upwelling systems. The cause, presumably, was the mechanical action of glacial-age winds rather than a greater supply of Fe. However, a role of increased supply of micronutrients from the continents in the increase of equatorial productivity during glacial time cannot be excluded. Such enhancement from increased supply of dust would have the interesting corollary of more efficient export transfer to depth, possibly contributing to nutrient depletion in glacial-age, deep intermediate waters. There is some indication, as well, of a general decrease in nutrient content in the tropical thermocline in the western Pacific during the last several million years, a depletion that may have been fostered by increasing supply of dust from emerging Asian highlands. Alternative explanations are available. The case for Fe as a major modifier of productivity and biogenic sedimentation on geological time scales cannot be made in the absence of criteria diagnostic for Fe supply as opposed to stirring and upwelling.
- OSTI ID:
- 6994201
- Journal Information:
- Limnology and Oceanography; (United States), Vol. 36:8; ISSN 0024-3590
- Country of Publication:
- United States
- Language:
- English
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63 RADIATION, THERMAL, AND OTHER ENVIRON. POLLUTANT EFFECTS ON LIVING ORGS. AND BIOL. MAT.
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ANTARCTIC OCEAN
BIOGEOCHEMISTRY
CARBON DIOXIDE
ECOLOGICAL CONCENTRATION
IRON
BIOLOGICAL AVAILABILITY
PHYTOPLANKTON
PRODUCTIVITY
CARBON SINKS
CHLOROPHYLL
NUTRIENTS
UPWELLING
AQUATIC ORGANISMS
CARBON COMPOUNDS
CARBON OXIDES
CARBOXYLIC ACIDS
CHALCOGENIDES
CHEMISTRY
ELEMENTS
GEOCHEMISTRY
HETEROCYCLIC ACIDS
HETEROCYCLIC COMPOUNDS
METALS
ORGANIC ACIDS
ORGANIC COMPOUNDS
ORGANIC NITROGEN COMPOUNDS
OXIDES
OXYGEN COMPOUNDS
PHYTOCHROMES
PIGMENTS
PLANKTON
PLANTS
PORPHYRINS
PROTEINS
SEAS
SINKS
SURFACE WATERS
TRANSITION ELEMENTS
540320* - Environment
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560300 - Chemicals Metabolism & Toxicology
580000 - Geosciences
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