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Phosphorus recycling and burial in Baltic Sea sediments with contrasting redox conditions
Stockholms universitet, Stockholm Resilience Centre, Baltic Nest Institute.ORCID-id: 0000-0003-1048-8452
2010 (engelsk)Inngår i: Geochimica et Cosmochimica Acta, ISSN 0016-7037, E-ISSN 1872-9533, Vol. 74, nr 4, s. 1350-1362Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

In this study, redox-dependent phosphorus (P) recycling and burial at 6 sites in the Baltic Sea is investigated using a combination of porewater and sediment analyses and sediment age dating (Pb-210 and Cs-117). We focus on sites in the Kattegat, Danish Straits and Baltic Proper where present-day bottom water redox conditions range from fully oxygenated and seasonally hypoxic to almost permanently anoxic and sulfidic. Strong surface enrichments of Fe-oxide bound P are observed at oxic and seasonally hypoxic sites but not in the anoxic basins. Reductive dissolution of Fe-oxides and release of the associated P supports higher sediment-water exchange of PO4 at hypoxic sites (up to similar to 800 mu mol P m(-2) d(-1)) than in the anoxic basins. This confirms that Fe-bound P in surface sediments in the Baltic acts as a major internal source of P during seasonal hypoxia, as suggested previously from water column studies. Most burial of P takes place as organic P. We find no evidence for significant authigenic Ca-P formation or biogenic Ca-P burial. The lack of major inorganic P burial sinks makes the Baltic Sea very sensitive to the feedback loop between increased hypoxia, enhanced regeneration of P and increased primary productivity. Historical records of bottom water oxygen at two sites (Bornholm, Northern Gotland) show a decline over the past century and are accompanied by a rise in values for typical sediment proxies for anoxia (total sulfur, molybdenum and organic C/P ratios). While sediment reactive P concentrations in anoxic basins are equal to or higher than at oxic sites, burial rates of P at hypoxic and anoxic sites are up to 20 times lower because of lower sedimentation rates. Nevertheless, burial of reactive P in both hypoxic and anoxic areas is significant because of their large surface area and should be accounted for in budgets and models for the Baltic Sea.

sted, utgiver, år, opplag, sider
2010. Vol. 74, nr 4, s. 1350-1362
Emneord [en]
EASTERN MEDITERRANEAN SAPROPELS; CONTINENTAL-MARGIN SEDIMENTS; AUTHIGENIC APATITE FORMATION; MARINE-SEDIMENTS; WATER INTERFACE; ORGANIC-MATTER; NORTH-SEA; BRITISH-COLUMBIA; ANOXIC SEDIMENTS; OXYGEN
HSV kategori
Forskningsprogram
geokemi
Identifikatorer
URN: urn:nbn:se:su:diva-50071DOI: 10.1016/j.gca.2009.11.016ISI: 000273824800013OAI: oai:DiVA.org:su-50071DiVA, id: diva2:382729
Merknad
authorCount :4Tilgjengelig fra: 2011-01-03 Laget: 2010-12-21 Sist oppdatert: 2018-01-24bibliografisk kontrollert

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