Phytoplankton biomass and production during late austral spring (1991) and summer (1993) in the Bransfield Strait

Phytoplankton biomass and productivity were measured during two cruises in the Bransfield Strait in December 1991 (D91) and January/February 1993 (J93). Strong seasonal variability in productivity values was observed due to differences in the physiological response of phytoplankton. However, althoug...

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Bibliographic Details
Published in:Polar Biology
Main Authors: Basterretxea, Gotzon, Arístegui, Javier
Other Authors: Aristegui, Javier, 6601976436, 7006816204, 778770, 227201
Format: Article in Journal/Newspaper
Language:English
Published: 0722-4060 1999
Subjects:
Online Access:http://hdl.handle.net/10553/51669
https://doi.org/10.1007/s003000050328
Description
Summary:Phytoplankton biomass and productivity were measured during two cruises in the Bransfield Strait in December 1991 (D91) and January/February 1993 (J93). Strong seasonal variability in productivity values was observed due to differences in the physiological response of phytoplankton. However, although the photosynthetic capacity of phytoplankton was markedly lower in D91 [P m B=0.61 ± 0.25 mg C (mg Chla)−1 h−1] than in J93 [P m B=2.18 ± 0.91 mg C (mg Chla)−1 h−1], average water column chlorophyll values in different areas of the strait were approximately similar in D91 (49–78 mg Chla m−2) and J93 (22–76 mg Chla m−2). The spatial distribution of chlorophyll was patchy and generally associated with the influence of the different water masses that meet together in the Bransfield Strait. No correlation was found between the mixed layer depth and either the integrated chlorophyll or the productivity. Our results suggest that major phytoplankton blooms in the Bransfield Strait are advected from the nearby Gerlache Strait or Bellingshausen Sea following the main eastward surface currents.