(Table 2) Concentration of phytoplankton pigments in Adventfjorden in spring and summer of 1997 ...

The study was carried out from April 30 until July 13 of 1997 in Adventfjorden (Spitsbergen). Formation of a less saline and warmer surface water (~1 m thick) caused by melting of the ice was observed in the fjord during the first days of May. In summer the less saline surface layer was about 3 m th...

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Bibliographic Details
Main Authors: Dobrzyn, P, Tatur, A, Keck, Alexander
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.727233
https://doi.pangaea.de/10.1594/PANGAEA.727233
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Summary:The study was carried out from April 30 until July 13 of 1997 in Adventfjorden (Spitsbergen). Formation of a less saline and warmer surface water (~1 m thick) caused by melting of the ice was observed in the fjord during the first days of May. In summer the less saline surface layer was about 3 m thick. Euphotic depth measured under the ice sheet reached 12 m, whereas load of mineral matter brought with riverine discharge in summer (content of total particulate matter in the fjord reached 1.66 kg/m**2) dramatically reduced euphotic zone depth to 0.35 m. By pigment measurement three phases of phytoplankton development in Adventfjorden were distinguished: (1) spring bloom that has started under fast ice and reached maximum in the mid of May, (2) stagnation period in June, (3) increase of pigment concentration in July, what could indicate start of the next algae bloom. Analyses of chlorophylls and carotenoids revealed that diatoms (chl c, fucoxanthin), and green algae (chl b, lutein) dominated phytoplankton ... : Coordinates of the Adv-1 station were estimated from the map in the paper with use of Google Earth. ...