Beyond the Fe-P-redox connection: preferential regeneration of phosphorus from organic matter as a key control on Baltic Sea nutrient cycles

Patterns of regeneration and burial of phosphorus (P) in the Baltic Sea are strongly dependent on redox conditions. Redox varies spatially along water depth gradients and temporally in response to the seasonal cycle and multidecadal hydrographic variability. Alongside the well-documented link betwee...

Full description

Bibliographic Details
Main Authors: T. Jilbert, C. P. Slomp, B. G. Gustafsson, W. Boer
Format: Article
Language:English
Published: Copernicus Publications 2011-06-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/8/1699/2011/bg-8-1699-2011.pdf
_version_ 1819266461249568768
author T. Jilbert
C. P. Slomp
B. G. Gustafsson
W. Boer
author_facet T. Jilbert
C. P. Slomp
B. G. Gustafsson
W. Boer
author_sort T. Jilbert
collection DOAJ
description Patterns of regeneration and burial of phosphorus (P) in the Baltic Sea are strongly dependent on redox conditions. Redox varies spatially along water depth gradients and temporally in response to the seasonal cycle and multidecadal hydrographic variability. Alongside the well-documented link between iron oxyhydroxide dissolution and release of P from Baltic Sea sediments, we show that preferential remineralization of P with respect to carbon (C) and nitrogen (N) during degradation of organic matter plays a key role in determining the surplus of bioavailable P in the water column. Preferential remineralization of P takes place both in the water column and upper sediments and its rate is shown to be redox-dependent, increasing as reducing conditions become more severe at greater water-depth in the deep basins. Existing Redfield-based biogeochemical models of the Baltic may therefore underestimate the imbalance between N and P availability for primary production, and hence the vulnerability of the Baltic to sustained eutrophication via the fixation of atmospheric N. However, burial of organic P is also shown to increase during multidecadal intervals of expanded hypoxia, due to higher net burial rates of organic matter around the margins of the deep basins. Such intervals may be characterized by basin-scale acceleration of all fluxes within the P cycle, including productivity, regeneration and burial, sustained by the relative accessibility of the water column P pool beneath a shallow halocline.
first_indexed 2024-12-23T21:01:38Z
format Article
id doaj.art-3c93a7d35dbf4c5b915713b4dcfd78c8
institution Directory Open Access Journal
issn 1726-4170
1726-4189
language English
last_indexed 2024-12-23T21:01:38Z
publishDate 2011-06-01
publisher Copernicus Publications
record_format Article
series Biogeosciences
spelling doaj.art-3c93a7d35dbf4c5b915713b4dcfd78c82022-12-21T17:31:20ZengCopernicus PublicationsBiogeosciences1726-41701726-41892011-06-01861699172010.5194/bg-8-1699-2011Beyond the Fe-P-redox connection: preferential regeneration of phosphorus from organic matter as a key control on Baltic Sea nutrient cyclesT. JilbertC. P. SlompB. G. GustafssonW. BoerPatterns of regeneration and burial of phosphorus (P) in the Baltic Sea are strongly dependent on redox conditions. Redox varies spatially along water depth gradients and temporally in response to the seasonal cycle and multidecadal hydrographic variability. Alongside the well-documented link between iron oxyhydroxide dissolution and release of P from Baltic Sea sediments, we show that preferential remineralization of P with respect to carbon (C) and nitrogen (N) during degradation of organic matter plays a key role in determining the surplus of bioavailable P in the water column. Preferential remineralization of P takes place both in the water column and upper sediments and its rate is shown to be redox-dependent, increasing as reducing conditions become more severe at greater water-depth in the deep basins. Existing Redfield-based biogeochemical models of the Baltic may therefore underestimate the imbalance between N and P availability for primary production, and hence the vulnerability of the Baltic to sustained eutrophication via the fixation of atmospheric N. However, burial of organic P is also shown to increase during multidecadal intervals of expanded hypoxia, due to higher net burial rates of organic matter around the margins of the deep basins. Such intervals may be characterized by basin-scale acceleration of all fluxes within the P cycle, including productivity, regeneration and burial, sustained by the relative accessibility of the water column P pool beneath a shallow halocline.http://www.biogeosciences.net/8/1699/2011/bg-8-1699-2011.pdf
spellingShingle T. Jilbert
C. P. Slomp
B. G. Gustafsson
W. Boer
Beyond the Fe-P-redox connection: preferential regeneration of phosphorus from organic matter as a key control on Baltic Sea nutrient cycles
Biogeosciences
title Beyond the Fe-P-redox connection: preferential regeneration of phosphorus from organic matter as a key control on Baltic Sea nutrient cycles
title_full Beyond the Fe-P-redox connection: preferential regeneration of phosphorus from organic matter as a key control on Baltic Sea nutrient cycles
title_fullStr Beyond the Fe-P-redox connection: preferential regeneration of phosphorus from organic matter as a key control on Baltic Sea nutrient cycles
title_full_unstemmed Beyond the Fe-P-redox connection: preferential regeneration of phosphorus from organic matter as a key control on Baltic Sea nutrient cycles
title_short Beyond the Fe-P-redox connection: preferential regeneration of phosphorus from organic matter as a key control on Baltic Sea nutrient cycles
title_sort beyond the fe p redox connection preferential regeneration of phosphorus from organic matter as a key control on baltic sea nutrient cycles
url http://www.biogeosciences.net/8/1699/2011/bg-8-1699-2011.pdf
work_keys_str_mv AT tjilbert beyondthefepredoxconnectionpreferentialregenerationofphosphorusfromorganicmatterasakeycontrolonbalticseanutrientcycles
AT cpslomp beyondthefepredoxconnectionpreferentialregenerationofphosphorusfromorganicmatterasakeycontrolonbalticseanutrientcycles
AT bggustafsson beyondthefepredoxconnectionpreferentialregenerationofphosphorusfromorganicmatterasakeycontrolonbalticseanutrientcycles
AT wboer beyondthefepredoxconnectionpreferentialregenerationofphosphorusfromorganicmatterasakeycontrolonbalticseanutrientcycles