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Johanna

Johanna

Tuesday, 06 December 2011 12:52

Manila Bay, Philippines

Manila Bay, Philippines

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Manila Bay is a semi-enclosed estuary facing the China Sea. More than 10 million people live in the Manila Bay catchment area. The bay is highly eutrophic due to nutrient loading from surrounding areas. Eutrophication may further lower the dissolved oxygen content in Manila bay. Hypoxia occurs in the middle of Manila Bay during the northeast monsoon and during the southwest monsoon months (wet season), when the hypoxia is more intense and widespread. The drivers for the northeast monsoon hypoxia are suggested to be the physical features of the bay (deep midsection favoring stratification and allowing sediments to accumulate), two gyres in the middle of the bay (sediments with organic matter may accumulate and decompose in the convergence area of the two gyres) and high amount of organic matter in the sediments. The southwest monsoon hypoxia is more intense due to increased stratification caused by river run-off.


 

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

  • Asia

Region

  • Southeast Asia

Countries

  • Philippines

Locate with Google Map

Key References

  1. Chang KH, Amano A, Miller T, Isobe T, Maneja R, Siringan F, Imai H, Nakano S. 2009. Pollution study in Manila Bay: Eutrophication and its impact on plankton community. Interdisciplinary Studies on Environmental Chemistry - Environemntal Reserach in Asia. Eds., Y. Obayashi, T. Isobe, A. Subramanian, S. Suzuki and S. Tanabe, pp. 261–267.
  2. Jacinto G, Sotto LP, Senal MI, San Diego-McGlone, ML, Escobar Ma. T, Amano A, Willer T. 2011. Hypoxia in Manila Bay, Philippines during the northeast monsoon. Marine Pollution Bulletin 60, 243-248.

Citation

Johanna Yletyinen. Manila Bay, Philippines. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2011-12-19 16:13:42 GMT.
Thursday, 01 December 2011 14:16

Paracas Bay, Peru

Paracas Bay, Peru

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Paracas Bay on the coast of Peru is an area which is a part of the Paracas National Reserve as well as an important area for fishing and fisheries-related factories. Harmful algal blooms often cause hypoxia in Paracas Bay as a result of algal respiration and decomposition. A devastating bloom of the dinoflagellate Gymnodinium sanguineum occurred in 2004 and caused anoxia, which together with toxins produced by algal blooms resulted in massive fish and shellfish deaths.The massive fish deaths and closing of the port caused huge economic losses for fish industry and aquaculture.


It has been concluded that the 2004 mass mortality of benthic species was partly caused by untreated waste from the fish meal factories.

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

  • South America

Region

  • Coastal Peru

Countries

  • Peru

Locate with Google Map

Key References

  1. Kahru M, Mitchell B, Diaz A, Miura M. 2004. MODIS detects a devastating algal bloom in Paracas Bay, Peru. Eos 85, 465-472.

Citation

Johanna Yletyinen. Paracas Bay, Peru. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-12 08:37:42 GMT.
Thursday, 01 December 2011 13:51

Cape Rodney, New Zealand

Cape Rodney, New Zealand

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Episodic hypoxia and anoxia near Cape Rodney covers 8000 square kilometers. It is related to harmful algal blooms and has resulted in fish mortalities. Hypoxia in Cape Rodney has been observed since the 1980s.

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Conservation
  • Tourism

Spatial scale of the case study

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

Continent or Ocean

  • Australia & New Zealand

Region

  • North Island of New Zealand

Countries

  • New Zealand

Locate with Google Map

Key References

  1. Shears N. 2009. Blooms of benthic dinoflagellates of the genus Ostreopsis; an increasing and ecologically important phenomenon on temperate reefs in New Zealand and worldwide. Harmful Algae 8, 916-925.

Citation

Johanna Yletyinen. Cape Rodney, New Zealand. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2011-12-05 08:04:20 GMT.
Thursday, 01 December 2011 12:57

Wadden Sea

Wadden Sea

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

The Wadden Sea is a large, relatively flat coastal environment. Strong increases in nutrient concentrations and primary production took place in the Wadden Sea in the late 1970s and 1980s. Indications of hypoxia in Wadden Sea were first observed in 1988. In 1996, large anoxic areas occurred in the East Frisian basin. It is debated whether hypoxia in the Wadden Sea is natural or not, but the signs of eutrophication are clear.  

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

  • Northwest continental Europe

Countries

  • Netherlands
  • Germany

Locate with Google Map

Key References

  1. Colijn C, van Beusekorn J. 2005. Effects of eutrophication of phytoplankton community and growth in the Wadden Sea. In: Wilson, J (Ed.). 2005. THe intertidal Ecosystem: The Value of Ireland's Shores, 58-68.
  2. Hoppema J. 1991. The oxygen budget of the western Wadden Sea, The Netherlands. Estuarine, Coastal and Shelf Science 32, 483-502.
  3. Kaiser J, Lutter S. 1998. Do we have the right strategeis to combat eutrophication in the Wadden Sea? - A critical review of current policies. Senckenbergiana Maritima 29, 17-24.

Citation

Johanna Yletyinen. Wadden Sea. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2011-12-05 08:11:29 GMT.
Thursday, 01 December 2011 10:44

Mauritania Coast, Mauritania

Mauritania Coast, Mauritania

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

The Mauritanian benthic fauna faces periodical, severe hypoxic and anoxic conditions caused mainly by dry climatic conditions. Hypoxic episodes have dramatically increased under the arid and dry climates of the 1970s, 1980s and 1990s. Strong northeast trade winds bring the settled nutrients from the deep ocean water to the surface, giving rise to phytoplankton blooms.
The rapid intensification of Mauritanian agriculture may indirectly increase hypoxia through fertilizer usage. Point and non-point source pollution into Mauritanian's coastal waters should be managed to protect the benthic biodiversity.
 

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

  • Africa

Region

  • West Africa

Countries

  • Mauritania

Locate with Google Map

Key References

  1. Le Loeuff P, von Cosel R. 1998. Biodiversity patterns of the marine benthic fauna of the Atlantic Coast of tropical Africa in relation to hydroclimatic conditions and paleogeographic events. Acta Oecologica 19, 309-321.
  2. Le Loeuff, P. 1999. The benthic macrofauna of the variable saline waters ecosystems along the Atlantic coast of tropical Africa; biodiversity variations with the current climatic conditions (rainfall) and the regional climatic history. Zoosystema 21, 557-571.

Citation

Johanna Yletyinen. Mauritania Coast, Mauritania. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2011-12-02 17:06:18 GMT.
Thursday, 01 December 2011 10:12

Donegal Bay, Ireland

Donegal Bay, Ireland

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Donegal Bay experienced mortalities of marine fauna in 2005. It has been suggested that the kills were brought about by oxygen depletion, which was caused by intense blooms of Karenia mikimotoi, the most common local dinoflagellate species causing red tides. The large scale of the blooms had never been observed before. Large quantities of dead sea urchins and lugworms were deposited on the beaches of west Ireland, and several cultured and wild fish species died. Hypoxia may have been caused by dinoflagellate respiration or decompostion and it may have acted as a cause to mortalities or as a significant stress factor indirectly leading to the death of fauna.

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Fisheries
  • Tourism

Spatial scale of the case study

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

Continent or Ocean

  • Europe

Region

  • Northwest Ireland

Countries

  • Ireland

Locate with Google Map

Key References

  1. O'Boyle S, Silke J. 2010. A review of phytoplankton ecology in estuarine and coastal waters around Ireland. Journal of Plankton Research 32, 99-118.
  2. Silke J, O’Beirn F, Cronin M. 2005. Karenia mikimotoi: An exceptional dinoflagellate bloom in western Irish waters, summer 2005. Marine Environment and Health Series 21.

Citation

Johanna Yletyinen. Donegal Bay, Ireland. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-11 13:33:32 GMT.
Thursday, 01 December 2011 08:54

Schönberger Strand, Germany

Schönberger Strand, Germany

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Hypoxia in Schönberger Strand is caused by both natural and anthropogenic causes. Fish kills and other symptons caused by oxygen depletion were reported already in the late 1800s and early 1900s.

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Fisheries
  • Tourism

Spatial scale of the case study

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

Continent or Ocean

  • Europe

Region

  • Germany's Baltic Sea coastline

Countries

  • Germany

Locate with Google Map

Key References

  1. Gerlach S (Ed). 1984. Oxygen depletion 1980 - 1983 in coastal waters of the Federal Republic of Germany. First report of the working group "Eutrophication of the North Sea and the Baltic". Institut fur Meereskunde.

Citation

Johanna Yletyinen. Schönberger Strand, Germany. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2012-01-12 09:24:45 GMT.
Thursday, 01 December 2011 08:25

Hohwacht Bay, Germany

Hohwacht Bay, Germany

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

Hypoxia in Hohwacht Bay is caused by a combination of anthropogenic and natural factors. Fish kills caused by hypoxia were first reported in 1875, 1913, 1928 and 1938-37. In 1981 the Hohwacht Bay hypoxia was estimated to be worse than ever before in the past 100 years.

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

  • Germany's Baltic Sea coastline

Countries

  • Germany

Locate with Google Map

Key References

  1. Gerlach S (Ed.). 1984. Oxygen Depletion 1980-1983 in Coastal Waters of the Federal Republic of Germany. First Report of the Working Group "Eutrophication of the North Sea and the Baltic". Institut för Meereskunde nr 130.

Citation

Johanna Yletyinen. Hohwacht Bay, Germany. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2011-12-02 17:02:54 GMT.
Wednesday, 30 November 2011 16:10

Bay of Vilaine, France

Bay of Vilaine, France

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

The Bay of Vilaine is a sheltered and shallow ecosystem in Southern Brittany in north-west France. Eutrophication due to high nutrient inputs of the river Vilaine has been evident since the 1980s. In the summer of 1982, hypoxia killed dozens of tons of fish in the bay.
The Bay of Vilaine hypoxia is periodic and mainly caused by phytoplanktonic biomass degradation.

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-west France

Countries

  • France

Locate with Google Map

Key References

  1. Chapelle A, Lazure P, Ménesguen A. 1994. Modelling Eutrophication Events in a Coastal Ecosystem. Sensitivity Analysis. Estuarine, Coastal and Shelf Science 39, 519-548.
  2. Le Bris H, Glemarec M. 1995. Macrozoobenthic communities of an oxygen under-saturated coastal ecosystem: The Bay of Vilaine (Southern Brittany). Oceanologica acta 18,573-581.

Citation

Johanna Yletyinen. Bay of Vilaine, France. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2011-12-02 16:50:34 GMT.
Wednesday, 30 November 2011 15:31

Bude Bay, United Kingdom

Bude Bay, United Kingdom

Main Contributors:

Johanna Yletyinen

Other Contributors:

Summary

The Bude Bay located in the south-west England experiences episodic hypoxia, which has caused mortality in the benthic fauna along the coastline. Hypoxic areas have been observed in vicinity to sewage outfall.
Hypoxia may have affected the massive kill of a dog-whelk (Nucella lapillus), which occurred in the Bude Bay in 1995.

Type of regime shift

Ecosystem type

  • Marine & coastal

Land uses

  • Tourism

Spatial scale of the case study

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

Continent or Ocean

  • Europe

Region

  • South-west England

Countries

  • United Kingdom

Locate with Google Map

Key References

  1. Gibbs P, Green J, Pascoe P. 1999. A massive summer-kill of the dog-whelk, Nucella lapillus, on the north Cornwall coast in 1995: freak or forerunner? Journal of the Marine Biological Association of the United Kingdom 79, 103-109.

Citation

Johanna Yletyinen. Bude Bay, United Kingdom. In: Regime Shifts Database, www.regimeshifts.org. Last revised 2011-12-02 16:51:29 GMT.