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(Figure 5) Relationship between Ammonia sp. diameter and duration of pH decre...
This dataset has no description
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(Figure 4) pH and Ca**2+ dynamics of an adult Ammonia sp. individual (diamete...
This dataset has no description
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(Figure 3) Relationship between Ammonia sp. diameter and decreases of pH duri...
This dataset has no description
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(Figure 2) Differences between pH- and Ca**2+-decreases and the bulk seawater...
This dataset has no description
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Raman spectra obtained at different skeletal region of the tropical coral Por...
Confocal Raman microscopy (CRM) mapping was used to investigate the microstructural arrangement and organic matrix distribution within the skeleton of the coral Porites lutea.... -
The morphological response of Emiliania huxleyi to seawater carbonate chemist...
Four strains of the coccolithophore Emiliania huxleyi (RCC1212, RCC1216, RCC1238, RCC1256) were grown in dilute batch culture at four CO2 levels ranging from ~200 µatm to ~1200... -
Seawater carbonate chemistry and benthic foraminifera Ammonia sp. uranium inc...
The chemical and isotopic composition of foraminiferal shells (so-called proxies) reflects the physico-chemical properties of the seawater. In current day paleoclimate research,... -
Seawater carbonate chemistry and benthic foraminifera Ammonia sp. mass, size,...
About 30% of the anthropogenically released CO2 is taken up by the oceans; such uptake causes surface ocean pH to decrease and is commonly referred to as ocean acidification... -
Seawater carbonate chemistry, nutrients, and Calcidiscus leptoporus (strain R...
The coccolithophore Calcidiscus leptoporus was grown in batch culture under nitrogen (N) as well as phosphorus (P) limitation. Growth rate, particulate inorganic carbon (PIC),... -
Seawater carbonate chemistry and biological processes of Emiliania huxleyi (s...
With respect to their sensitivity to ocean acidification, calcifiers such as the coccolithophore Emiliania huxleyi have received special attention, as the process of... -
Seawater carbonate chemistry, growth rate and morphology of Calcidiscus lepto...
The coccolithophore Calcidiscus leptoporus (strain RCC1135) was grown in dilute batch culture at CO2 levels ranging from ~200 to ~1600 µatm. Increasing CO2 concentration led to... -
pH and calcium change in the microenvironment of a benthic foraminifer (Ammon...
Calcareous foraminifera are well known for their CaCO3 shells. Yet, CaCO3 precipitation acidifies the calcifying fluid. Calcification without pH regulation would therefore... -
Isotope ratios, trace elements and ultrastructure results of Mytilus gallopro...
Bivalve shells can provide excellent archives of past environmental change but have not been used to interpret ocean acidification events. We investigated carbon, oxygen and... -
Villefranche MedSeA mesocosm experiment 2013: field studies
<0= below detection limits. In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne et al, 2014) was used to compute a... -
Villefranche MedSeA mesocosm experiment 2013: perturbation studies
<0= below detection limits. In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne et al, 2014) was used to compute a... -
Stareso MedSeA mesocosm experiment 2012: field studies
<0= below detection limits.In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne et al, 2014) was used to compute a... -
Stareso MedSeA mesocosm experiment 2012: perturbation studies
<0= below detection limits. In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne et al, 2014) was used to compute a... -
Morphological parameters of Globigerinoides ruber, Globigerina bulloides and ...
This dataset has no description
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Environmental parameters of the MedSea2013 cruise water samples
This dataset has no description
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(Table 3) Dead (not stained) benthic foraminifera from stations in the northe...
Samples taken in 0-2 cm sediment depth.
