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Johanna

Johanna

Thursday, 15 December 2011 15:28

Archipelago Sea, Finland

Archipelago Sea, Finland

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Seasonal hypoxia in theArchipelago Sea is caused by coastal eutrophication, which has been the greatest threat to the Archipelago ecosystem since the 1970s. Hypoxia has caused changes in species composition.  

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Fisheries

Spatial scale of the case study

  • Local/landscape (e.g. lake, catchment, community)

Continent or Ocean

  • Europe

Region

  • North Europe

Countries

  • Finland

Locate with Google Map

Key References

  1. Bonsdorff E, Blomqvist EM, Mattila J, Norkko A. 1997. Coastal eutrophication: causes, consequences and perspectives in the archipelago areas of the Northern Baltic Sea. Estuarine, Coastal and Shelf Science 44, 63-72.

Citation

Johanna Yletyinen. Archipelago Sea, Finland. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-11 12:08:56 GMT.
Thursday, 15 December 2011 14:53

Åland Archipelago, Finland

Åland Archipelago, Finland

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Åland archipelago is an eutrophic area receiving nutrient inputs from numerous sources. Algae has increased in the area since the early 1990s. Hypoxia and anoxia occur frequently and have caused benthic mortality. Fish have decreased in abundance, biomass and diversity during the occurrence of algal mats.

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Fisheries

Spatial scale of the case study

  • Sub-continental/regional (e.g. southern Africa, Amazon basin)

Continent or Ocean

  • Europe

Region

  • North Europe

Countries

  • Finland

Locate with Google Map

Key References

  1. Bonsdorff E, Blomqvist EM, Mattila J, Norkko A. 1997. Coastal eutrophication: causes, consequences and perspectives in the archipelago areas of the Northern Baltic Sea. Estuarine, Coastal and Shelf Science 44, 63-72.

Citation

Johanna Yletyinen. Åland Archipelago, Finland. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-12 10:31:22 GMT.
Thursday, 15 December 2011 14:35

Thames Estuary, UK

Thames Estuary, UK

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Seasonal hypoxia in the Thames estuary was first recorded in the 1920s. Compared to the 1930-1970s, the hypoxic conditions have now improved due to nutrientmanagement.  

Type of regime shift

Ecosystem type

  • Freshwater lakes & rivers

Land uses

  • Fisheries

Spatial scale of the case study

  • Local/landscape (e.g. lake, catchment, community)

Continent or Ocean

  • Europe

Region

  • Southern England

Countries

  • United Kingdom

Locate with Google Map

Key References

  1. Andrews MJ, Rickard DG. 1980. Rehabilition of the inner Thames estuary. Marine Pollution Bulletin 11, 327-332.

Citation

Johanna Yletyinen. Thames Estuary, UK. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-12 10:09:09 GMT.
Thursday, 15 December 2011 14:27

Mersey Estuary, UK

Mersey Estuary, UK

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

The Mersey river has been calledone of the most polluted rivers in Europe. It has received discharges since the beginning of the Industrial Revolution from manufacturing processes and population centres. Mersey Estuary has seasonal hypoxia annually at least in one spot upriver. Hypoxic conditions have improved from nutrient managent. Due to recovery fish (e.g. Salmon) have returned to the waters.

Type of regime shift

Ecosystem type

  • Freshwater lakes & rivers

Land uses

  • Fisheries

Spatial scale of the case study

  • Local/landscape (e.g. lake, catchment, community)

Continent or Ocean

  • Europe

Region

  • North west England

Countries

  • United Kingdom

Locate with Google Map

Key References

  1. Jones, PD. 2000. The Mersey Estuary - Back from the dead? Solving a 150-year old problem. Water and Environmental Journal 14, 124-130.

Citation

Johanna Yletyinen. Mersey Estuary, UK. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-12 07:39:55 GMT.
Thursday, 15 December 2011 14:10

Forth Estuary, UK

Forth Estuary, UK

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

The Fourth Estuary receives domestic and industrial wasteand develops hypoxia especially under low river discharge conditions, which usually occur at summer. Fish kills have been reported.

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Fisheries

Spatial scale of the case study

  • Local/landscape (e.g. lake, catchment, community)

Continent or Ocean

  • Europe

Region

  • North Sea

Countries

  • United Kingdom

Locate with Google Map

Key References

  1. Balls PW, Brockie N, Dobson J, Johnston W. 1996. Dissolved Oxygen and Nitrification in the Upper Forth Estuary During Summer (1982–92): Patterns and Trends. Estuarine, Coastal and Shelf Sciece 42, 117-134.

Citation

Johanna Yletyinen. Forth Estuary, UK. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-11 13:50:09 GMT.
Thursday, 15 December 2011 13:54

Alexandria Harbor, Egypt

Alexandria Harbor, Egypt

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Alexandria Harbor hypoxia is seasonal. The harbor is an eutrophic area with many input sources: maritime activities, agriculture, stored fertilizers, domestic and industrial waste.

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Fisheries

Spatial scale of the case study

  • Local/landscape (e.g. lake, catchment, community)

Continent or Ocean

  • Africa

Region

  • North Africa

Countries

  • Egypt

Locate with Google Map

Key References

  1. Abdel-Aziz NE, Fahmy MA, Dorgham MM. 2001. Hydrography, nutrients and plankton abundance in the hot spot of Abu Qir Bay, Alexandria, Egypt. Mediterr. Mar. Sci. 2, 17-31.
  2. Dorgham M, El-Deeb K, Okbah M. 2004. Eutrophication problems in the Western Harbour of Alexandria, Egypt. Oceanologia 46, 25-44.
  3. Ismael A, Dorgham M. 2003. Ecological indices as a tool for assessing pollution in El-Dekhaila Harbour (Alexandria, Egypt). Oceanologia 45, 121-131.

Citation

Johanna Yletyinen. Alexandria Harbor, Egypt. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-11 11:59:39 GMT.
Thursday, 15 December 2011 13:43

Vejle Fjord, Denmark

Vejle Fjord, Denmark

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Hypoxia and anoxia are to a certain scale natural phenomena in many deep fjords. Since the early 1980s, more or less widespread hypoxia has been observed nearly every autumn in Danish coastal waters. The causes of hypoxia in Denmark are related to increased nutrient loads and natural physical factors (e.g. weather) affecting the timing and duration of hypoxia.
The most severe and widespread open waters hypoxia occurred in 2002 when a combination of unusually high winter precipitation and unusually calm, warm weather in late summer and autumn. Hypoxic events in Danish estuaries are not in phase with the open waters; the most severe hypoxic episode in estuaries was reported in 1997 when parts of the Mariager Fjord turned completely anoxic.
The response of marine benthic macrofaunal communities to seasonal hypoxia in coastal Denmark is a collapse or mass mortality. 

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Fisheries

Spatial scale of the case study

  • Local/landscape (e.g. lake, catchment, community)

Continent or Ocean

  • Europe

Region

  • The Baltic Sea

Countries

  • Denmark

Locate with Google Map

Key References

  1. Conley J, Carstensen J, Ærterbjerg G, Christensen PB, Dalsgaard T, Hansen J, Josefsen A. 2007. Long-term changes and impacts of hypoxia in Danish coastal waters. Ecological Applications 17, 165-184.
  2. Karlson K, Rosenberg R, Bonsdorff E. 2002. Temporal and spatial large-scale effects of eutrophication and oxygen deficiency on benthic fauna in Scandinavian and Baltic waters: A review. Oceanography and Marine Biology 40, 427-489.
  3. Lundholm N, Clarke A, Ellegaard M. 2010. A 100-year record of changing Pseudo-nitzschia species in a sill-fjord in Denmark related to nitrogen loading and temperature. Harmful Algae 9, 449-475.

Citation

Johanna Yletyinen. Vejle Fjord, Denmark. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2011-12-19 15:30:43 GMT.
Thursday, 15 December 2011 13:33

Skive Fjord, Denmark

Skive Fjord, Denmark

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Hypoxia and anoxia are to a certain scale natural phenomena in fjords. The causes of hypoxia in Denmark are related to increased nutrient loads and natural physical factors (e.g. weather) affecting the timing and duration of hypoxia.  

Type of regime shift

Ecosystem type

  • Marine & coastal
  • Freshwater lakes & rivers

Land uses

  • Fisheries

Spatial scale of the case study

  • Local/landscape (e.g. lake, catchment, community)

Continent or Ocean

  • Europe

Region

  • Northern Europe

Countries

  • Denmark

Locate with Google Map

Key References

  1. Karlson K, Rosenberg R, Bonsdorff E. 2002. Temporal and spatial large-scale effects of eutrophication and oxygen deficiency on benthic fauna in Scandinavian and Baltic waters: A review. Oceanography and Marine Biology 40, 427-489.

Citation

Johanna Yletyinen. Skive Fjord, Denmark. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-12 09:32:40 GMT.
Thursday, 15 December 2011 13:10

Skagerrak Coast

Skagerrak Coast

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Since the early 1980s, more or less widespread hypoxia has been observed nearly every autumn in Danish coastal waters. Water exchange in Skagerrak is limited and hypoxic conditions in deep basin are common, because water renewal, which takes place only once a year, causes stagnation period with hypoxia in the winter. Several fjords on the Swedish and Norwegian Skagerrak coast have shown negative trends in dissolved oxygen content, and some of them lack benthic fauna in the deeper parts for several months or more. Swedish fjords of the Skagerrak coast experience hypoxia and anoxia for most of the year. In Norway, for instance in Oslofjord, the benthic fauna has suffered from mortality and behavioral changes. Since around 1960-70s, dissolved oxygen content has reclined in Oslofjord. Improvements in sewage treatment and discharge practices have been made.

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Fisheries

Spatial scale of the case study

  • Sub-continental/regional (e.g. southern Africa, Amazon basin)

Continent or Ocean

  • Europe

Region

  • Northern Europe

Countries

  • Norway
  • Sweden
  • Denmark

Locate with Google Map

Key References

  1. Conley J, Carstensen J, Ærterbjerg G, Christensen PB, Dalsgaard T, Hansen J, Josefsen A. 2007. Long-term changes and impacts of hypoxia in Danish coastal waters. Ecological Applications 17, 165-184.
  2. Rabalais N (Ed.), Turner RE (Ed.). 2002. Coastal hypoxia: Consequences for living resources and ecosystems (Coastal and estuarine sciences, 58). Amer Geophysical Union, Washington
  3. Rosenberg R, Cato I, Förlin L, Grip K, Rorhe J. Marine environment quality assessment of the Skagerrak - Kattegat. Journal of Sea Research 35, 1-8.

Citation

Johanna Yletyinen. Skagerrak Coast. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-12 09:31:37 GMT.
Thursday, 15 December 2011 12:37

Roskilde Fjord, Denmark

Roskilde Fjord, Denmark

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Since the early 1980s, more or less widespread hypoxia has been observed nearly every autumn in Danish coastal waters. The causes of hypoxia in Denmark are related to increased nutrient loads and natural physical factors (e.g. weather) affecting the timing and duration of hypoxia.
The most severe and widespread open waters hypoxia occurred in 2002 when a combination of unusually high winter precipitation and unusually calm, warm weather in late summer and autumn. Hypoxic events in Danish estuaries are not in phase with the open waters; the most severe hypoxic episode in estuaries was reported in 1997 when parts of the Mariager Fjord turned completely anoxic. Roskilde Fjord has been particularly negative affected by the coastal Kattegat hypoxia.
The response of marine benthic macrofaunal communities to seasonal hypoxia in coastal Denmark is a collapse or mass mortality. 

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Timber production

Spatial scale of the case study

  • Local/landscape (e.g. lake, catchment, community)

Continent or Ocean

  • Europe

Region

  • The Baltic Sea

Countries

  • Denmark

Locate with Google Map

Key References

  1. Clarke A, Juggins S, Conley D. 2003. A 150-year reconstruction of the history of coastal eutrophication in Roskilde Fjord, Denmark. Marine Pollution Bulletin 46, 1615-1618.
  2. Conley J, Carstensen J, Ærterbjerg G, Christensen PB, Dalsgaard T, Hansen J, Josefsen A. 2007. Long-term changes and impacts of hypoxia in Danish coastal waters. Ecological Applications 17, 165-184.
  3. Karlson K, Rosenberg R, Bonsdorff E. 2002. Temporal and spatial large-scale effects of eutrophication and oxygen deficiency on benthic fauna in Scandinavian and Baltic waters: A review. Oceanography and Marine Biology 40, 427-489.

Citation

Johanna Yletyinen. Roskilde Fjord, Denmark. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2011-12-19 15:30:53 GMT.