Dust impact on marine biota and atmospheric CO2during glacial periods
about
Ecosystem dynamics based on plankton functional types for global ocean biogeochemistry modelsCarbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation.Greenhouse gases in the Earth system: a palaeoclimate perspective.Southern Ocean sea-ice extent, productivity and iron flux over the past eight glacial cycles.Biogeochemical fluxes through mesozooplanktonEvaluation of climate models using palaeoclimatic dataLowering of glacial atmospheric CO2in response to changes in oceanic circulation and marine biogeochemistryNitrogen fixation amplifies the ocean biogeochemical response to decadal timescale variations in mineral dust depositionSensitivity of global ocean biogeochemical dynamics to ecosystem structure in a future climatePotential impact of changes in river nutrient supply on global ocean biogeochemistryBiosphere dynamics: Challenges for Earth system modelsThe PMIP4 contribution to CMIP6 – Part 4: Scientific objectives and experimental design of the PMIP4-CMIP6 Last Glacial Maximum experiments and PMIP4 sensitivity experimentsLarge inert carbon pool in the terrestrial biosphere during the Last Glacial MaximumFrom monsoon to marine productivity in the Arabian Sea: insights from glacial and interglacial climatesImplications of coral reef buildup for the controls on atmospheric CO2since the Last Glacial MaximumHigh-resolution reconstruction of southwest Atlantic sea-ice and its role in the carbon cycle during marine isotope stages 3 and 2The significance of the episodic nature of atmospheric deposition to Low Nutrient Low Chlorophyll regionsImproving the parameters of a global ocean biogeochemical model via variational assimilation of in situ data at five time series stationsWhat does temporal variability in aeolian dust deposition contribute to sea-surface iron and chlorophyll distributions?Response of diatoms distribution to global warming and potential implications: A global model studyAtmospheric global dust cycle and iron inputs to the oceanTemperature-induced marine export production during glacial periodImplications of the glacial CO2“iron hypothesis” for Quaternary climate changeQuantitative interpretation of atmospheric carbon records over the last glacial terminationA modeling assessment of the interplay between aeolian iron fluxes and iron-binding ligands in controlling carbon dioxide fluctuations during Antarctic warm eventsCombined Effects of Atmospheric and Seafloor Iron Fluxes to the Glacial OceanEnhanced sensitivity of oceanic CO2 uptake to dust deposition by iron-light colimitationDust-induced changes in phytoplankton composition in the Tasman Sea during the last four glacial cyclesTesting the sensitivity of past climates to the indirect effects of dustWhat have we learnt from palaeoclimate simulations?Last Glacial Maximum CO2 and δ13C successfully reconciledVolcanic Ash versus Mineral Dust: Atmospheric Processing and Environmental and Climate Impacts
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Dust impact on marine biota and atmospheric CO2during glacial periods
description
im Juni 2003 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в червні 2003
@uk
name
Dust impact on marine biota and atmospheric CO2during glacial periods
@en
Dust impact on marine biota and atmospheric CO2during glacial periods
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type
label
Dust impact on marine biota and atmospheric CO2during glacial periods
@en
Dust impact on marine biota and atmospheric CO2during glacial periods
@nl
prefLabel
Dust impact on marine biota and atmospheric CO2during glacial periods
@en
Dust impact on marine biota and atmospheric CO2during glacial periods
@nl
P2860
P50
P356
P1433
P1476
Dust impact on marine biota and atmospheric CO2during glacial periods
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P2093
Karen E. Kohfeld
P2860
P356
10.1029/2002PA000810
P577
2003-06-01T00:00:00Z