Dataset - B2FIND

Oxygen consumption and inorganic nutrient fluxes of deep-water hexactinellid ...

During R/V Sonne cruise SO254 around New Zealand (January-February 2017), deep-sea sponges were incubated in-situ and ex-situ to measure oxygen consumption, inorganic nutrient...

Contribution of various Nitrogen cycle processes to the nitrogen budget of th...

The Amazon River is known as a region of intense biochemical reactivity. As a result of increased anthropogenic impacts in its catchment (e.g. population growth, agriculture,...

Mesocosm concentration, regeneration and absorption studies of Lanvéoc/Bay of...

This dataset has no description

Mesocosm concentration, regeneration and absorption studies of Lanvéoc/Bay of...

This dataset has no description

Mesocosm concentration, regeneration and absorption studies of Lanvéoc/Bay of...

This dataset has no description

Seawater carbonate chemistry and uptake of dissolved inorganic nitrogen and N...

We conducted a minicosm experiment with pre-acclimated cultures of the globally significant diazotroph Crocosphaera watsonii strain WH8501 ("Crocosphaera"). PH and temperature...

Seawater carbonate chemistry and growth rate of a bloom forming macroalga

Introduction: The coastal macroalgal genus, Ulva, is found worldwide and is considered a nuisance algal genus due to its propensity for forming vast blooms. The response of Ulva...

Seawater carbonate chemistry and physiological performance of the rhodolith S...

Fish farming in coastal areas has become an important source of food to support the world's increasing population. However, intensive and unregulated mariculture activities have...

Effects of CO2 enrichment on photosynthesis, growth, and nitrogen metabolism ...

Seagrass ecosystems are expected to benefit from the global increase in CO2 in the ocean because the photosynthetic rate of these plants may be Ci-limited at the current CO2...

Experiment: Elevated CO2 levels affect the activity of nitrate reductase and ...

The concentration of CO2 in global surface ocean waters is increasing due to rising atmospheric CO2 emissions, resulting in lower pH and a lower saturation state of carbonate...