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Zooplankton variability on the Faroe Shelf and in the surrounding oceanic area in relation to phytoplankton and physical conditions. E. Gaard, H. Debes, B. Hansen, H. Hátún, K. M. H. Larsen Faroe Marine Research Institute. - PowerPoint PPT Presentation
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Zooplankton variability on the Faroe Shelf and in the surrounding oceanic area
in relation to phytoplankton and physical conditions
E. Gaard, H. Debes, B. Hansen, H. Hátún, K. M. H. LarsenFaroe Marine Research Institute
ICES/NAFO Symposium on the Variability of the North Atlantic and its Marine Ecosystems during 2000-2009.
Santander, Spain, 10-12 May 2011
Nordic Seas
Content
• Variability:
– North of the Faroes • Warm Atlantic • Cold East Icelandic current water
– Outside the shelf front
– On the Faroe shelf
North of the Faroes
Copepod life cycle
Calanus life cycle
Calanus finmarchicusMay 1993-2009
Chlorophyll aMay 1993-2009
TemperatureAnnual mean
N1
N14
The Faroe Shelf Ecosystem
• Separate water mass
• Distinct ecosystem
• Largely neritic zooplankton.
• Mixed with variable abundances of oceanic zooplankton
Copepods on and around the Faroe shelf19-27 June 2009
Copepods
Calanus finmarchicus
Zooplankton monitoringLate June
< 100 m bottom depthZooplankton biomass
> 150 m bottom depthZooplankton biomass
M icroscopic examinations (Shelf)
M icroscopic examinations (Outside she lf)
Zooplankton dry weight (g/m2)Outside the shelf, late June
Outside the shelf front, late June
Zooplankton biomass
Calanus finmarchicusStage composition
Calanus finmarchicusRelative stage composition
Faroe Self copepodsSeasonal development, 2004
Zooplankton dry weight (g/m2)Shelf and Outside the shelf, late June
Faroe shelfLate June, 1992-2009
Copepods Calanus finmarchicus
Temora: 10 X increase
Shelf temperature and chl. a
Chl. a: 15 April - 30 June
Temperature Mean, 15 April – 30 June
Calanus finmarchicusStage duration
5°C
8°C
7°C
Summary
• Atlantic and shelf water:– 10x increase in Temora (shelf), 1995-2009– Zooplankton biomass increase (C. finmarchicus) during the 2000s– Phenology changes.– No relationship with chlorophyll a.– Shorter stage duration induced by higher temperature (~1°C) only
shortherns the generation time ~1 weak.
• East-Icelandic current water:– Large phenology shift in 2003-2004. Earlier reproduction.– No relationship with chlorophyll a– Most like caused by temperature increase and/or changes in
currents