-
Hepatozyten Respiration obtained using closed system respirometry
This dataset has no description
-
Community composition
This dataset has no description
-
Energy cost of protei synthesis
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
Energy cost of H+ transport
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
Energy cost of Ca2+ tranposrt
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
Culture experiments with Coccolithus pelagicus ssp. braarudii
Carbonate chemistry and physiological growth data of experiments with C. pelagicus. Mean TA and DIC were calculated as average of initial and final values. pH, pCO2, HCO3-,... -
(Table 2) Chlorophyll content, chlorophyll a/b ratio, number of algal cells p...
All data given per (milli)gram dry weight (DW). -
Long-term dynamics of adaptive evolution in a globally important coccolithoph...
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 complete and consistent set of... -
Adaptation of a globally important coccolithophore to ocean warming and acidi...
This dataset has no description
-
Expression of biomineralization-related ion transport genes in Emiliania huxl...
This dataset has no description
-
(Table 2) Bacterial abundance, carbon production and respiration in samples o...
Averages of stations depicted in Table 1. Respiration parameter all Q10 corrected. Potential and specific bacterial respiration and respiration rate based on the equation BR =... -
Seawater carbonate chemistry, particulate inorganic and organic carbon and gr...
This dataset has no description
-
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 lipid content, particulate organic carbon/ni...
Coccolithophores are a calcifying unicellular phytoplankton group that are at the base of the marine food web, and their lipid content provides a source of energy to consumers.... -
Influence of temperature, pCO2, and dissolved nutrients on the oxidative stre...
We conducted a full-factorial lab experiment to study the individual and combined effects of temperature (18°C and 21°C), pCO2 (400 and 1000 ppm), and dissolved N:P ratio (16... -
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, chain length, silica content, and to...
Phytoplankton induce defensive traits in response to chemical alarm signals from grazing zooplankton. However, these signals are potentially vulnerable to changes in pH and it... -
Seawater carbonate chemistry and elemental contents and macromolecules of the...
Elemental contents change with shifts in macromolecular composition of marine phytoplankton. Recent studies focus on the responses of elemental contents of coccolithophores, a... -
Seawater carbonate chemistry and the physiological response of Acropora cervi...
Knowledge of multi-stressor interactions and the potential for tradeoffs among tolerance traits is essential for developing intervention strategies for the conservation and... -
Seawater carbonate chemistry and growth rates, carbon utilization and the int...
Ocean acidification (OA) appears to have diverse impacts on calcareous coccolithophores, but the cellular processes underlying these responses are not well understood. Here we...
