Plankton

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LifeLinkedtoIce Algae and phytoplankton

Ice algae accounts for less than 1% of the annual primary production at this coastal location, but the bloom occurs at least a month before any primary production is available from phytoplankton. Farther offshore, ice algae contribute much more to the total annual production: as much as over 50% [4]. 

 

Adapted from Mikkelsen et al. 2008 [58]

 

 

Conservation of Arctic Flora and Fauna (CAFF) 

The data can be downloaded freely. Users are requested to reference the source.

Eamer, J., Donaldson, G.M., Gaston, A.J., Kosobokova, K.N., Lárusson, K.F., Melnikov, I.A., Reist, J.D., Richardson, E., Staples, L., von Quillfeldt, C.H. 2013. Life Linked to Ice: A guide to sea-ice-associated biodiversity in this time of rapid change. CAFF Assessment Series No. 10. Conservation of Arctic Flora and Fauna, Iceland. ISBN: 978-9935-431-25-7.

 

LifeLinkedtoIce Sea ice Ecosystem structure

Change in ecosystem structure that may result from reduction of sea ice and related temperature changes: an illustration based on the Chukchi Sea food web 

 

Adapted from Hopcroft et al. 2008 [95], based on Carroll and Carroll 2003 [98] 

 

 

Conservation of Arctic Flora and Fauna (CAFF) 

The data can be downloaded freely. Users are requested to reference the source.

Eamer, J., Donaldson, G.M., Gaston, A.J., Kosobokova, K.N., Lárusson, K.F., Melnikov, I.A., Reist, J.D., Richardson, E., Staples, L., von Quillfeldt, C.H. 2013. Life Linked to Ice: A guide to sea-ice-associated biodiversity in this time of rapid change. CAFF Assessment Series No. 10. Conservation of Arctic Flora and Fauna, Iceland. ISBN: 978-9935-431-25-7.

 

 

 

95. Hopcroft, R., Bluhm, B., and Gradinger, R. (eds). 2008. Arctic Ocean synthesis: Analysis of climate change impacts in the Chukchi and Beaufort seas with strategies for future research. Institute of Marine Sciences, University of Alaska, and North Pacific Research Board, Fairbanks, Alaska.

 

98. Carroll, M.L., and Carroll, J. 2003. The Arctic seas. In Biogeochemistry of Marine Systems. Edited by Black, K.D., and Shimmield, G.B. CRC Press, Boca Raton, US. pp. 127-156.

 

 

LifeLinkedtoIce Phytoplankton

 

The number of species depends partly on what has been studied. Proportions vary somewhat around the Arctic, but diatoms and dinoflagellates are the most diverse groups everywhere. The greatest sampling effort has been in the Laptev Sea, Hudson Bay, and the Norwegian sector of the Barents Sea. Species shown are among the most commonly recorded.
Data from Poulin et al. 2011 [65]

Photos (taken through light microscopes): clockwise from top right Dr. Gerhard Dieckmann/Alfred Wegener Institute; Gert Hansen/Nordic Microalgae (www.nordicmicroalgae.org); Alexandra/Alfred Wegener Institute; Marine Productivity
Laboratory, Fisheries and Oceans Canada

 

Conservation of Arctic Flora and Fauna (CAFF) 

The data can be downloaded freely. Users are requested to reference the source.

Eamer, J., Donaldson, G.M., Gaston, A.J., Kosobokova, K.N., Lárusson, K.F., Melnikov, I.A., Reist, J.D., Richardson, E., Staples, L., von Quillfeldt, C.H. 2013. Life Linked to Ice: A guide to sea-ice-associated biodiversity in this time of rapid change. CAFF Assessment Series No. 10. Conservation of Arctic Flora and Fauna, Iceland. ISBN: 978-9935-431-25-7.

LifeLinkedtoIce Phytoplankton density

Samples are from the upper ocean during summer. Points on the graphs are averages of data for 23 stations that were distributed across the Canada Basin.

From Li et al. 2009 [127]

 

Conservation of Arctic Flora and Fauna (CAFF) 

The data can be downloaded freely. Users are requested to reference the source.

Eamer, J., Donaldson, G.M., Gaston, A.J., Kosobokova, K.N., Lárusson, K.F., Melnikov, I.A., Reist, J.D., Richardson, E., Staples, L., von Quillfeldt, C.H. 2013. Life Linked to Ice: A guide to sea-ice-associated biodiversity in this time of rapid change. CAFF Assessment Series No. 10. Conservation of Arctic Flora and Fauna, Iceland. ISBN: 978-9935-431-25-7.

LifeLinkedtoIce Phytoplankton blooms

 

 

The rate of change is very rapid at some locations. For example, the peak algal bloom occurred in early September in Foxe Basin and in the Kara Sea in the mid-1990s but had shifted to mid-July by 2009, a change of about 50 days.
Source: Kahru et al. 2011 [214]

 

 

 

Conservation of Arctic Flora and Fauna (CAFF) 

The data can be downloaded freely. Users are requested to reference the source.

Eamer, J., Donaldson, G.M., Gaston, A.J., Kosobokova, K.N., Lárusson, K.F., Melnikov, I.A., Reist, J.D., Richardson, E., Staples, L., von Quillfeldt, C.H. 2013. Life Linked to Ice: A guide to sea-ice-associated biodiversity in this time of rapid change. CAFF Assessment Series No. 10. Conservation of Arctic Flora and Fauna, Iceland. ISBN: 978-9935-431-25-7.

LifeLinkedtoIce Primary production by phytoplankton

Estimates of average annual primary production by size class were based on relationships with pigment types as 

detected by satellite monitoring, 1998 to 

2007.

 

Data from Uitz et al. 2010 [107]

 

 

  

Conservation of Arctic Flora and Fauna (CAFF) 

The data can be downloaded freely. Users are requested to reference the source.

Eamer, J., Donaldson, G.M., Gaston, A.J., Kosobokova, K.N., Lárusson, K.F., Melnikov, I.A., Reist, J.D., Richardson, E., Staples, L., von Quillfeldt, C.H. 2013. Life Linked to Ice: A guide to sea-ice-associated biodiversity in this time of rapid change. CAFF Assessment Series No. 10. Conservation of Arctic Flora and Fauna, Iceland. ISBN: 978-9935-431-25-7.

LifeLinkedtoIce Phytoplankton bloom Barents Sea small

 

The color in this satellite image is created by a massive phytoplankton bloom. The milky blue areas indicate a high abundance of coccolithophores, plankton that are plated with white calcium carbonate. Other colors may be from other plankton types and suspended sediment. The graphs, which are from a study over approximately the same area, show the relationship between the timing of blooms and the timing of sea ice. Diatoms (indicated by chlorophyll concentrations) dominate the earlier bloom that is associated with ice melt. Coccolithophores (indicated by calcite concentrations) dominate late summer bloom. They thrive in stable surface layers of warm, low-salinity, low-nutrient water. Coccolithophore blooms are becoming more frequent in the southern Barents Sea and expanding northward to the high Arctic.
All data shown are based on analysis of satellite imagery. This natural-color image was taken by the Moderate Resolution
Imaging Spectroradiometer (MODIS) sensor on the Aqua satellite.
NASA image courtesy Jeff Schmaltz, MODIS Rapid Response Team at NASA GSFC; graph from Signorini and McClain 2009 [153]; caption based on Signorini and McClain 2009 [153], Carlowicz and Riebeek 2012 [154] 

 

  

Conservation of Arctic Flora and Fauna (CAFF) 

The data can be downloaded freely. Users are requested to reference the source.

Eamer, J., Donaldson, G.M., Gaston, A.J., Kosobokova, K.N., Lárusson, K.F., Melnikov, I.A., Reist, J.D., Richardson, E., Staples, L., von Quillfeldt, C.H. 2013. Life Linked to Ice: A guide to sea-ice-associated biodiversity in this time of rapid change. CAFF Assessment Series No. 10. Conservation of Arctic Flora and Fauna, Iceland. ISBN: 978-9935-431-25-7.

LifeLinkedtoIce First year pollock

 

 

 

Predation, cannibalism by larger pollock, and starvation in winter increase for first-year pollock in years with earlier sea ice melt (top diagram).
From Hunt et al. 2011 [212]

 

 

 

 

Conservation of Arctic Flora and Fauna (CAFF) 

The data can be downloaded freely. Users are requested to reference the source.

Eamer, J., Donaldson, G.M., Gaston, A.J., Kosobokova, K.N., Lárusson, K.F., Melnikov, I.A., Reist, J.D., Richardson, E., Staples, L., von Quillfeldt, C.H. 2013. Life Linked to Ice: A guide to sea-ice-associated biodiversity in this time of rapid change. CAFF Assessment Series No. 10. Conservation of Arctic Flora and Fauna, Iceland. ISBN: 978-9935-431-25-7.

ABA 2013 14 13 Icecover 

Arctic Biodiversity Assessment (ABA) 2013.

Figure 14.13. Seasonal succession of ice cover, phytoplankton, copepods and protozooplankton (ciliates and dinoflagellates) in Disko Bay, W Greenland, 1996-1997. Sea ice cover is represented in white in a). The vertical blue line indicates the time when the bulk of Calanus spp. biomass leaves the surface layer giving room for an additional peak in protozooplankton biomass. (Adapted from Madsen et al. 2001 and Levinsen et al. 2000.)

 

Conservation of Arctic Flora and Fauna (CAFF)

www.caff.is 

The data can be downloaded freely.

Users are requested to reference it source.

Meltofte, H. (ed.) 2013. Arctic Biodiversity Assessment. Status and trends in Arctic biodiversity. Conservation of Arctic Flora and Fauna, Akureyri.

ABA 2013 14 14 Plankton 

Arctic Biodiversity Assessment (ABA) 2013.

Figure 14.14. Conceptual model of seasonal plankton succession in W Greenland in a) current and b) future warming conditions.(Adapted from Rysgaard & Glud 2007.)

 

Conservation of Arctic Flora and Fauna (CAFF)

www.caff.is 

The data can be downloaded freely.

Users are requested to reference it source.

Meltofte, H. (ed.) 2013. Arctic Biodiversity Assessment. Status and trends in Arctic biodiversity. Conservation of Arctic Flora and Fauna, Akureyri.

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