Jump to content
Main menu
Main menu
move to sidebar
hide
Navigation
Main page
Recent changes
Random page
Help about MediaWiki
Special pages
Niidae Wiki
Search
Search
Appearance
Create account
Log in
Personal tools
Create account
Log in
Pages for logged out editors
learn more
Contributions
Talk
Editing
Kattegat
(section)
Page
Discussion
English
Read
Edit
View history
Tools
Tools
move to sidebar
hide
Actions
Read
Edit
View history
General
What links here
Related changes
Page information
Appearance
move to sidebar
hide
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
== Biology == The [[salinity]] in the Kattegat has a pronounced two-layer structure. The upper layer's salinity is between 18‰ and 26‰, while that of the lower layer (separated by a strong [[halocline]] at around {{convert|15|m|abbr=on}}) has a salinity between 32‰ and 34‰. The lower layer consists of inflowing seawater from the Skagerrak, with a salinity on par with most other coastal seawaters, while the upper layer, consisting of inflowing seawater from the Baltic Sea, has a much lower salinity, comparable to [[brackish water]], but still a great deal higher than the rest of the Baltic. These two opposing flows transport a net surplus of {{convert|475|km3|cumi|abbr=on}} of seawater from the Baltic to the Skagerrak every year.<ref>{{cite web|url=http://www2.dmu.dk/1_viden/2_miljoe-tilstand/3_vand/4_eutrophication/hydrography.asp |title=Hydrography |author=Ærtebjerg, G., Andersen, J.H. and Schou Hansen |publisher=Danish Environmental Protection Agency and National Environmental Research Institute |website=Nutrients and Eutrophication in Danish Seawaters |date=2003 |access-date=30 January 2016}}</ref> During strong winds, the Kattegat's layers are completely mixed in places such as the [[Great Belt]], making the overall salinity highly variable. This leads to some distinctive conditions for [[sealife]] in the area.<ref>{{cite book|url=https://books.google.com/books?id=csLKtvZNV98C&pg=PA74 |title=Physical Oceanography of the Baltic Sea|author=Matti Leppäranta and Kai Myrberg|date=2009 |publisher=Springer-Praxis |access-date=30 January 2016 |pages=72–74|isbn=9783540797036}}</ref> [[Cold seep]]s, known locally as ''bubbling reefs'' ({{langx|da|boblerev}}), can be found in the northern Kattegat. Unlike those in most other places (including the North Sea and Skagerrak), the Kattegat's cold seeps are at relatively shallow depths, generally from {{convert|0|to(-)|30|m|ft|abbr=on|-2}} below the surface.<ref name=Jensen1992>{{cite journal|author1=Jensen |author2=Aagaard |author3=Burke |author4=Dando |author5=Jørgensen |author6=Kuijpers |author7=Laier |author8=O'Hara |author9=Schmaljohann | year=1992 | title="Bubbling reefs" in the Kattegat: Submarine landscapes of carbonate-cemented rocks support a diverse ecosystem at methane seeps | journal=Marine Ecology Progress Series | volume=83 | pages=103–112 | doi=10.3354/meps083103|bibcode=1992MEPS...83..103J |doi-access=free }}</ref><ref name=HelcomCS>{{cite web|url=http://helcom.fi/Red%20List%20of%20biotopes%20habitats%20and%20biotope%20complexe/HELCOM%20Red%20List%201180%20Submarine%20structures%20made%20by%20leaking%20gases.pdf | title=Red List – Submarine structures made by leaking gases | publisher=[[HELCOM]] | year=2013 | access-date=16 June 2017}}</ref> The seeps rely on methane deposited during the [[Eemian]] period and during calm weather the bubbles can sometimes be seen on the surface of the water.<ref name=HelcomCS/> Carbonate [[Cementation (geology)|cementation]] and [[lithification]] form slaps or pillars up to {{convert|4|m|ft|abbr=on}} tall and support a rich [[biodiversity]].<ref name=Jensen1992/><ref name=HelcomCS/> Due to their distinct properties, the Kattegat bubbling reefs are under protection and are recognised by the [[European Union]] (EU) as a [[Natura 2000]] habitat (type 1180).<ref>{{cite web| title=Proposed measures for fisheries management in Natura 2000-sites in the Danish territorial area of the Kattegat and Samsø Belt | url=https://naturerhverv.dk/fileadmin/user_upload/NaturErhverv/Filer/Fiskeri/Natura_2000_hav/Rev/Forslag_til_fiskeriregulering_Kattegat.pdf | series=Meeting at the AgriFish Agency, Copenhagen | publisher=[[Minister for Food, Agriculture and Fisheries (Denmark)]] | date=20 March 2012 | access-date=16 June 2017}}</ref> ===Ecological collapse=== The Kattegat, characterised by widespread [[oceanic anoxic event|anoxia]],<ref name="DruonEtAl2004">{{cite journal |last1=Druon |first1=Jean-Noël |last2=Schrimpf |first2=Wolfram |last3=Dobricic |first3=Srdjan |last4=Stips |first4=Adolf |date=19 May 2004 |title=Comparative assessment of large-scale marine eutrophication: North Sea area and Adriatic Sea as case studies |url=https://www.int-res.com/articles/meps2004/272/m272p001.pdf |journal=Marine Ecology Progress Series |volume=272 |pages=1–23 |doi=10.3354/meps272001 |bibcode=2004MEPS..272....1D |access-date=10 August 2023}}</ref> was one of the first marine [[dead zone (ecology)|dead zone]]s to be noted in the 1970s, when scientists began to study the effects of heavy industry on the natural world.<ref>{{cite web|url=http://www.unep.org/Documents.Multilingual/Default.asp?DocumentID=486&ArticleID=5393&l=en|title=Further Rise in Number of Marine 'Dead Zones'|publisher=[[UNEP]]|date=19 October 2006|access-date=30 January 2016|archive-date=4 October 2009|archive-url=http://arquivo.pt/wayback/20091004170617/http%3A//www.unep.org/Documents.Multilingual/Default.asp?DocumentID%3D486%26ArticleID%3D5393%26l%3Den|url-status=dead}}</ref><ref>{{cite book|url=https://books.google.com/books?id=9fEKAAAAQBAJ&pg=PA4 |title=Introduction to Marine Biology |author=Karleskint, Turner and Small |publisher=Brooks/Cole |page=4|date=2013 |edition=4|isbn=978-1285402222 }}</ref> Since then, research has leant much insight into processes like [[eutrophication]], and how to deal with it. Since the first Action Plan for the Aquatic Environment in 1985, Denmark and the EU have begun costly, far-reaching domestic projects to stop, repair and prevent these environmentally destructive and economically damaging processes<ref>{{Cite book |doi=10.1029/CE052p0155|chapter = Benthic macrofauna and demersal fish|title = Eutrophication in Coastal Marine Ecosystems| volume=52| pages=155–178|series = Coastal and Estuarine Studies|year = 1996|last1 = Hagerman|first1 = Lars| last2=Josefson| first2=Alf B.| last3=Jensen| first3=Jørgen N.| isbn=978-0-87590-266-1}}</ref> and are now busy implementing the fourth Action Plan. The action plans sum up a broad range of initiatives and include the so-called Nitrate Directives.<ref>[http://www.mst.dk/English/Agriculture/nitrates_directive/implementation_in_denmark/ Implementation of the Nitrates directive in Denmark] {{Webarchive|url=https://web.archive.org/web/20131203112345/http://www.mst.dk/English/Agriculture/nitrates_directive/implementation_in_denmark/ |date=3 December 2013 }} Danish Ministry of the Environment</ref> The action plans have generally been viewed as a success, although the work is not finished and not all goals have been met yet.<ref>{{cite web|url=http://politiken.dk/debat/analyse/ECE1422611/vandmiljoeplaner-har-vaeret-en-succes/|title=Action Plans for the Aquatic Environment have been a success|newspaper=Politiken|author1=Jesper H. Andersen |author2=Jacob Carstensen |date=25 October 2011|language=da|access-date=24 November 2014}}</ref>
Summary:
Please note that all contributions to Niidae Wiki may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see
Encyclopedia:Copyrights
for details).
Do not submit copyrighted work without permission!
Cancel
Editing help
(opens in new window)
Search
Search
Editing
Kattegat
(section)
Add topic