scholarly article | Q13442814 |
P356 | DOI | 10.1016/S0967-0645(02)00005-X |
P50 | author | Robert F. Anderson | Q47303403 |
John J. Marra | Q58150240 | ||
Zanna Chase | Q58325638 | ||
Mark A Brzezinski | Q87957196 | ||
P2093 | author name string | Ken O Buesseler | |
David M Nelson | |||
Michael R Hiscock | |||
Richard T Barber | |||
Roger François | |||
William R Martin | |||
Susumu Honjo | |||
Mary-Lynn Dickson | |||
Raymond N Sambrotto | |||
Daniel E Sigmon | |||
Frederick L Sayles | |||
Robert W Collier | |||
P2860 | cites work | A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization. | Q33922706 |
The silica balance in the world ocean: a reestimate. | Q34006121 | ||
Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica | Q55880358 | ||
On the meridional extent and fronts of the Antarctic Circumpolar Current | Q56038454 | ||
Ocean Carbon Pumps: Analysis of Relative Strengths and Efficiencies in Ocean-Driven Atmospheric CO2 Changes | Q56083048 | ||
A comparison of four methods for determining planktonic community production1 | Q56168536 | ||
Glacial-interglacial CO2 change: The Iron Hypothesis | Q56455131 | ||
VERTEX: carbon cycling in the northeast Pacific | Q57201646 | ||
Global distribution of the flux to ocean sediments constrained by GCM modelling | Q57813363 | ||
Influence of iron availability on nutrient consumption ratio of diatoms in oceanic waters | Q59055102 | ||
Iron-limited diatom growth and Si:N uptake ratios in a coastal upwelling regime | Q59059965 | ||
Nutrient depletion indicates high primary productivity in the Weddell Sea | Q59060073 | ||
Simulated response of the ocean carbon cycle to anthropogenic climate warming | Q59061520 | ||
Particulate organic matter flux and planktonic new production in the deep ocean | Q59069182 | ||
Carbon-cycle imbalances in the Sargasso Sea | Q59082092 | ||
Resolving the ‘opal paradox’ in the Southern Ocean | Q59091329 | ||
Increased biological productivity and export production in the glacial Southern Ocean | Q59091342 | ||
Evidence for lower productivity in the Antarctic Ocean during the last glaciation | Q59091406 | ||
Silicon-isotope composition of diatoms as an indicator of past oceanic change | Q59099218 | ||
Trapping efficiencies of sediment traps from the deep Eastern North Atlantic: | Q59308574 | ||
Spring development of phytoplankton biomass and composition in major water masses of the Atlantic sector of the Southern Ocean | Q59383355 | ||
The Southern Ocean's biological pump during the Last Glacial Maximum | Q59768380 | ||
Benthic remineralization and burial of biogenic SiO2, CaCO3, organic carbon, and detrital material in the Southern Ocean along a transect at 170° West | Q59768385 | ||
A review of the Si cycle in the modern ocean: recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy | Q59768393 | ||
The US Southern Ocean Joint Global Ocean Flux Study: an introduction to AESOPS | Q59768397 | ||
The supply and accumulation of silica in the marine environment | Q60017399 | ||
Upper ocean export of particulate organic carbon in the Arabian Sea derived from thorium-234 | Q60976294 | ||
P433 | issue | 9-10 | |
P921 | main subject | Southern Ocean | Q7354 |
P304 | page(s) | 1645-1674 | |
P577 | publication date | 2002-01-01 | |
P1433 | published in | Deep-Sea Research. Part 2: Topical Studies in Oceanography | Q15755936 |
P1476 | title | Vertical budgets for organic carbon and biogenic silica in the Pacific sector of the Southern Ocean, 1996–1998 | |
P478 | volume | 49 |
Q58111964 | A comparison between excess barium and barite as indicators of carbon export |
Q58390396 | A synthesis of global particle export from the surface ocean and cycling through the ocean interior and on the seafloor |
Q59768367 | Accumulation of biogenic and lithogenic material in the Pacific sector of the Southern Ocean during the past 40,000 years |
Q59768385 | Benthic remineralization and burial of biogenic SiO2, CaCO3, organic carbon, and detrital material in the Southern Ocean along a transect at 170° West |
Q58250275 | Chapter Seven Paleoceanographical Proxies Based on Deep-Sea Benthic Foraminiferal Assemblage Characteristics |
Q59768345 | Comparing glacial and Holocene opal fluxes in the Pacific sector of the Southern Ocean |
Q59768351 | Diatom productivity in the equatorial Pacific Ocean from the last glacial period to the present: A test of the silicic acid leakage hypothesis |
Q60558085 | Importance of particle formation to reconstructed water column biogenic silica fluxes |
Q59768350 | Opal burial in the equatorial Atlantic Ocean over the last 30 ka: Implications for glacial-interglacial changes in the ocean silicon cycle |
Q57084856 | Quantifying the opal belt in the Atlantic and southeast Pacific sector of the Southern Ocean by means of230Th normalization |
Q58044916 | Relevance of silicon isotopes to Si-nutrient utilization and Si-source assessment in Antarctic waters |
Q60558088 | Si and C interactions in the world ocean: Importance of ecological processes and implications for the role of diatoms in the biological pump |
Q60558093 | Si/C decoupling in the world ocean: is the Southern Ocean different? |
Q59768391 | The US Southern Ocean Joint Global Ocean Flux Study: Volume Two |
Q64455998 | The cadmium-phosphate relationship in brine: biological versus physical control over micronutrients in sea ice environments |
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