Dataset - B2FIND

Biogeochemistry of Mesocosms during METEOR cruise M77/3

The mesocosms were filled with 70 L each, using natural seawater from 10 m depth (Niskin bottles from CTD-casts), which was pre-screened (200 µm mesh size) to remove...

Combined in-situ and ex-situ measurements at a water depth of 5m from the Gui...

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The organic sea-surface microlayer in the upwelling region off the coast of P...

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(Table 3) Integrated TEP concentrations in the water column during POLARSTERN...

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(Table 2) Protist carbon flux and surface standing stock of diatoms, flagella...

Standing stock represents the average over all IN or all OUT stations. Total POC for standing stock is the sum of protist C, bacteria C and copepods (<1 mm) C from Schulz et al.

Organic matter and gel particles of Maria S. Merian cruise MSM85

The discrete biogeochemical measurements from RV Maria S. Merian MSM85 sampled for dissolved organic matter, microbial cell abundances and gel particles. The parameters include...

Biopolymers form a gelatinous microlayer at the air-sea interface when Arctic...

The interface layer between ocean and atmosphere is only a couple of micrometers thick but playsa critical role in climate relevant processes, including the air-sea exchange of...

PeECE I - Pelagic Ecosystem CO2 Enrichment Study, Raunefjord, Bergen, Norway,...

The effects of CO2-induced seawater acidification on plankton communities were also addressed in a series of 3 mesocosm experiments, called the Pelagic Ecosystem CO2 Enrichment...

Experiment: Organic matter exudation by Emiliania huxleyi under simulated fut...

Emiliania huxleyi (strain B 92/11) was exposed to different nutrient supply, CO2 and temperature conditions in phosphorus controlled chemostats to investigate effects on organic...

Seawater carbonate chemistry, POC, PIC, TPC, SPM, N, TEP and growth rate duri...

The response of three coccolithophores (Emiliania huxleyi, Calcidiscus leptoporus and Syracosphaera pulchra) to elevated partial pressure (pCO2) of carbon dioxide was...