Advanced search
Start date
Betweenand
Related content
(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Organic N and P in eutrophic fjord sediments - rates of mineralization and consequences for internal nutrient loading

Full text
Author(s):
Valdemarsen, T. [1] ; Quintana, C. O. [2, 1] ; Flindt, M. R. [1] ; Kristensen, E. [1]
Total Authors: 4
Affiliation:
[1] Univ Southern Denmark, Inst Biol, Odensee - Denmark
[2] Univ Sao Paulo, Inst Oceanog, Sao Paulo - Brazil
Total Affiliations: 2
Document type: Journal article
Source: BIOGEOSCIENCES; v. 12, n. 6, p. 1765-1779, 2015.
Web of Science Citations: 13
Abstract

Nutrient release from the sediments in shallow eutrophic estuaries may counteract reductions of the external nutrient load and prevent or prolong ecosystem recovery. The magnitude and temporal dynamics of this potential source, termed internal nutrient loading, is poorly understood. We quantified the internal nutrient loading driven by microbial mineralization of accumulated organic N (ON) and P (OP) in sediments from a shallow eutrophic estuary (Odense Fjord, Denmark) Sediments were collected from eight stations within the system and nutrient production and effluxes were measured over a period of similar to 2 years. Dissolved inorganic nitrogen (DIN) effluxes were high initially but quickly faded to low and stable levels after 50-200 days, whereas PO43- effluxes were highly variable in the different sediments. Mineralization patterns suggested that internal N loading would quickly (<200 days) fade to insignificant levels, whereas internal PO43- loading could be sustained for extended time (years). When results from all stations were combined, internal N loading and P loading from the fjord bottom was up to 121 x 103 kgNyr(-1) (20 kgN ha(-1) yr(-1)) and 22 x 10(3) kg P yr(-1) (3.6 kg P ha(-1) yr(-1)) corresponding to 6 (N) and 36% (P) of the external nutrient loading to the system. We conclude that the internal N loading resulting from degradation of accumulated ON is low in shallow eutrophic estuaries, whereas microbial mineralization of accumulated OP is a potential source of P. Overall it appears that, in N-limited eutrophic systems, internal nutrient resulting from mineralization of ON and OP in sediments is of minor importance. (AU)

FAPESP's process: 12/06121-1 - Pathways of organic matter degradation in marine coastal sediments: implications to ecosystem functioning
Grantee:Cintia Organo Quintana
Support Opportunities: Scholarships in Brazil - Post-Doctoral