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Hydrochemistry during METEOR cruise M77/3
This dataset has no description
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Stable Silicon Isotopes data, biogenic opal concentrations and bulk sediment ...
The data includes silicon isotope signatures, biogenic opal concentrations and bulk sediment nitrogen isotope signatures of three short cores between 11 and 15 degrees South of... -
Diatom assemblages and biogenic silica from IODP Site 383-U1539
From the complete downcore record of IODP Site 383-U1539, sampling was conducted at 1 m resolution. Quantitative diatom slides were prepared following the settling method of... -
Biogenic silica (BSi) content for the Eemian sediment sequence retrieved from...
The dataset provides quantifications of biogenic silica (BSi) content for the Eemian sediment sequence retrieved from Sokli (Finland) in 2010. Amounts of BSi are presented as... -
Compilation of downward flux observations from sediment trap deployments in t...
We provide a compilation of downward fluxes (total mass, POC, PON, BSiO2, CaCO3, PIC and lithogenic/terrigenous fluxes) from over 6000 sediment trap measurements distributed in... -
Biogenic silica, carbon, and nitrogen analyses of sediment core LVC18_S1 from...
This dataset has no description
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Seawater carbonate chemistry and coccolithophores and diatoms resilient to oc...
Here, we investigatethe impacts of moderate (~700 μmol/kg) and high (~2700 μmol/kg) limestone-inspired alkalinity additionson two biogeochemically and ecologically important... -
Seawater carbonate chemistry and growth, elemental composition,biomass produc...
Sea ice retreat, changing stratification, and ocean acidification are fundamentally changing the light availability and physico-chemical conditions for primary producers in the... -
Seawater carbonate chemistry and physiological parameters of Thalassiosira sp...
Marine diatoms are one of the marine phytoplankton functional groups, with high species diversity, playing important roles in the marine food web and carbon sequestration. In... -
Seawater carbonate chemistry and growth, production rates, and elemental quot...
The potential for adaptation of phytoplankton to future climate is often extrapolated based on single strain responses of a representative species, ignoring variability within... -
Ocean acidification decreases the light-use efficiency in an Antarctic diatom...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2015) was used to compute a complete and consistent set of... -
Concentrations of chlorophyll a, phaeopigments, and particulate matter during...
Here we present concentrations of chlorophyll a, phaeopigments, particulate organic carbon and nitrogen from water samples collected at discrete depths with a CTD-rosette during... -
Seawater carbonate chemistry and elemental composition of the particulate and...
Although the dissolved inorganic carbon concentration, pH, and nutrient regimes of seawater dramatically change in coastal regions, the synergistic effects of changes in the CO2... -
Physiological responses of coastal and oceanic diatoms to diurnal fluctuation...
Diel and seasonal fluctuations in seawater carbonate chemistry are common in coastal waters, while in the open-ocean carbonate chemistry is much less variable. In both of these... -
Effects of high CO2 levels on the ecophysiology of the diatom Thalassiosira w...
Iron availability in seawater, namely the concentration of dissolved inorganic iron ([Fe']), is affected by changes in pH. Such changes in the availability of iron should be... -
Export flux of particles of trap FLUPAC_PF-II
Data represent mean +/- SD, over 2-3 replicats at each deployment. -
Export flux of particles of trap FLUPAC_PF-I
Data represent mean +/- SD, over 2-3 replicats at each deployment. -
Silica and particulate organic carbon and nitrogen in sediment trap ANTARES-I...
This dataset has no description
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Silica and particulate organic carbon and nitrogen in sediment trap ANTARES-I...
This dataset has no description
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Lipid biomarkers and productivity proxies of sediment core AMD16-117Q
Version 2, 2022-03-10: Previous version doi:10.1594/PANGAEA.939224 contains errors due to data processing.
