Phytoplankton pigment concentrations during POLARSTERN cruise PS121 from North Sea to Fram in August to September 2019

• Main Authors: Bracher, Astrid, Wiegmann, Sonja
• Format: Dataset
• Language: English
• Published: PANGAEA 2022
• Subjects: 19-Butanoyloxyfucoxanthin; 19-Hexanoyloxyfucoxanthin; AC3; Alloxanthin; alpha-Carotene; Antheraxanthin; Arctic Amplification; Astaxanthin; beta-Carotene; Chlorophyll a; Chlorophyll b; Chlorophyll c1+c2; Chlorophyll c3; CT; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH; water; Diadinoxanthin; Diatoxanthin; Dinoxanthin; Event label; Exploitation of Sentinel-5-P for Ocean Colour Products; FRAM; Fram Strait; FRontiers in Arctic marine Monitoring; Fucoxanthin; Gyroxanthin diester; HPLC analysis; Improving the prediction of photophysiology in the Southern Ocean by accounting for iron limitation; optical properties and spectral satellite data information; IPSO; LATITUDE; LONGITUDE; Lutein; Neoxanthin; North Greenland Sea; North Sea; Peridinin; Pheophorbide a; Pheophytin a; Pheophytin b; phytoplankton pigments; Polarstern; Prasinoxanthin; PS121; PS121_1-2; PS121_12-2; PS121_15-1; Alvarez; Arctic; Barlow; Greenland; Southern Ocean; Greenland Sea; North Greenland; Phytoplankton
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.941011; https://doi.org/10.1594/PANGAEA.941011

Phytoplankton pigments were determined in the water column of a transect from the North Sea to Fram Strait during RV Polarstern expedition PS121 from 11 Aug to 10 Sep 2019. Water samples were collected from CTD Niskin bottles at five to six different depths from the upper 100 m at CTD stations and from underway sampling. This were the same water samples as in Bracher et al. (https://doi.pangaea.de/10.1594/PANGAEA.938260). Between 0.2 to 3.5 L of each seawater sample was filtered through Whatman GF/Ffilters. The sample filters were then shock‐frozen in liquid N2 and kept at−80 °C until analysis. High Pressure Liquid Chromatography (HPLC) was performed to quantify various phytoplankton pigments (see Table 1 in Taylor et al. 2011) following the method of Barlow et al. (1997) that was adjusted to our temperature‐controlled instruments as detailed in Alvarez et al. (2022).