Organism-Sediment Interactions Govern Post-Hypoxia Recovery of Ecosystem Functioning

Hypoxia represents one of the major causes of biodiversity and ecosystem functioning loss for coastal waters. Since eutrophication-induced hypoxic events are becoming increasingly frequent and intense, understanding the response of ecosystems to hypoxia is of primary importance to understand and predict the stability of ecosystem functioning. Such ecological stability may greatly depend on the recovery patterns of communities and the return time of the system properties associated to these patterns. Here, we have examined how the reassembly of a benthic community contributed to the recovery of ecosystem functioning following experimentally-induced hypoxia in a tidal flat. We demonstrate that organism-sediment interactions that depend on organism size and relate to mobility traits and sediment reworking capacities are generally more important than recovering species richness to set the return time of the measured sediment processes and properties. Specifically, increasing macrofauna bioturbation potential during community reassembly significantly contributed to the recovery of sediment processes and properties such as denitrification, bedload sediment transport, primary production and deep pore water ammonium concentration. Such bioturbation potential was due to the replacement of the small-sized organisms that recolonised at early stages by large-sized bioturbating organisms, which had a disproportionately stronger influence on sediment. This study suggests that the complete recovery of organism-sediment interactions is a necessary condition for ecosystem functioning recovery, and that such process requires long periods after disturbance due to the slow growth of juveniles into adult stages involved in these interactions. Consequently, repeated episodes of disturbance at intervals smaller than the time needed for the system to fully recover organism-sediment interactions may greatly impair the resilience of ecosystem functioning.

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Main Authors: van Colen, C., Rossi, F., Montserrat, F., Andersson, M.G.I., Gribsholt, B., Herman, P.M.J., Degraer, S., Vincx, M., Ysebaert, T., Middelburg, J.J.
Format: Article/Letter to editor biblioteca
Language:English
Subjects:bacterial assemblages, benthic community, biodiversity, biogeochemistry, bioturbation, coastal marine-sediments, diversity, intertidal sediments, model, tidal flat,
Online Access:https://research.wur.nl/en/publications/organism-sediment-interactions-govern-post-hypoxia-recovery-of-ec
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spelling dig-wur-nl-wurpubs-4413352025-01-21 van Colen, C. Rossi, F. Montserrat, F. Andersson, M.G.I. Gribsholt, B. Herman, P.M.J. Degraer, S. Vincx, M. Ysebaert, T. Middelburg, J.J. Article/Letter to editor PLoS ONE 7 (2012) 11 ISSN: 1932-6203 Organism-Sediment Interactions Govern Post-Hypoxia Recovery of Ecosystem Functioning 2012 Hypoxia represents one of the major causes of biodiversity and ecosystem functioning loss for coastal waters. Since eutrophication-induced hypoxic events are becoming increasingly frequent and intense, understanding the response of ecosystems to hypoxia is of primary importance to understand and predict the stability of ecosystem functioning. Such ecological stability may greatly depend on the recovery patterns of communities and the return time of the system properties associated to these patterns. Here, we have examined how the reassembly of a benthic community contributed to the recovery of ecosystem functioning following experimentally-induced hypoxia in a tidal flat. We demonstrate that organism-sediment interactions that depend on organism size and relate to mobility traits and sediment reworking capacities are generally more important than recovering species richness to set the return time of the measured sediment processes and properties. Specifically, increasing macrofauna bioturbation potential during community reassembly significantly contributed to the recovery of sediment processes and properties such as denitrification, bedload sediment transport, primary production and deep pore water ammonium concentration. Such bioturbation potential was due to the replacement of the small-sized organisms that recolonised at early stages by large-sized bioturbating organisms, which had a disproportionately stronger influence on sediment. This study suggests that the complete recovery of organism-sediment interactions is a necessary condition for ecosystem functioning recovery, and that such process requires long periods after disturbance due to the slow growth of juveniles into adult stages involved in these interactions. Consequently, repeated episodes of disturbance at intervals smaller than the time needed for the system to fully recover organism-sediment interactions may greatly impair the resilience of ecosystem functioning. en application/pdf https://research.wur.nl/en/publications/organism-sediment-interactions-govern-post-hypoxia-recovery-of-ec 10.1371/journal.pone.0049795 https://edepot.wur.nl/265090 bacterial assemblages benthic community biodiversity biogeochemistry bioturbation coastal marine-sediments diversity intertidal sediments model tidal flat Wageningen University & Research
institution WUR NL
collection DSpace
country Países bajos
countrycode NL
component Bibliográfico
access En linea
databasecode dig-wur-nl
tag biblioteca
region Europa del Oeste
libraryname WUR Library Netherlands
language English
topic bacterial assemblages
benthic community
biodiversity
biogeochemistry
bioturbation
coastal marine-sediments
diversity
intertidal sediments
model
tidal flat
bacterial assemblages
benthic community
biodiversity
biogeochemistry
bioturbation
coastal marine-sediments
diversity
intertidal sediments
model
tidal flat
spellingShingle bacterial assemblages
benthic community
biodiversity
biogeochemistry
bioturbation
coastal marine-sediments
diversity
intertidal sediments
model
tidal flat
bacterial assemblages
benthic community
biodiversity
biogeochemistry
bioturbation
coastal marine-sediments
diversity
intertidal sediments
model
tidal flat
van Colen, C.
Rossi, F.
Montserrat, F.
Andersson, M.G.I.
Gribsholt, B.
Herman, P.M.J.
Degraer, S.
Vincx, M.
Ysebaert, T.
Middelburg, J.J.
Organism-Sediment Interactions Govern Post-Hypoxia Recovery of Ecosystem Functioning
description Hypoxia represents one of the major causes of biodiversity and ecosystem functioning loss for coastal waters. Since eutrophication-induced hypoxic events are becoming increasingly frequent and intense, understanding the response of ecosystems to hypoxia is of primary importance to understand and predict the stability of ecosystem functioning. Such ecological stability may greatly depend on the recovery patterns of communities and the return time of the system properties associated to these patterns. Here, we have examined how the reassembly of a benthic community contributed to the recovery of ecosystem functioning following experimentally-induced hypoxia in a tidal flat. We demonstrate that organism-sediment interactions that depend on organism size and relate to mobility traits and sediment reworking capacities are generally more important than recovering species richness to set the return time of the measured sediment processes and properties. Specifically, increasing macrofauna bioturbation potential during community reassembly significantly contributed to the recovery of sediment processes and properties such as denitrification, bedload sediment transport, primary production and deep pore water ammonium concentration. Such bioturbation potential was due to the replacement of the small-sized organisms that recolonised at early stages by large-sized bioturbating organisms, which had a disproportionately stronger influence on sediment. This study suggests that the complete recovery of organism-sediment interactions is a necessary condition for ecosystem functioning recovery, and that such process requires long periods after disturbance due to the slow growth of juveniles into adult stages involved in these interactions. Consequently, repeated episodes of disturbance at intervals smaller than the time needed for the system to fully recover organism-sediment interactions may greatly impair the resilience of ecosystem functioning.
format Article/Letter to editor
topic_facet bacterial assemblages
benthic community
biodiversity
biogeochemistry
bioturbation
coastal marine-sediments
diversity
intertidal sediments
model
tidal flat
author van Colen, C.
Rossi, F.
Montserrat, F.
Andersson, M.G.I.
Gribsholt, B.
Herman, P.M.J.
Degraer, S.
Vincx, M.
Ysebaert, T.
Middelburg, J.J.
author_facet van Colen, C.
Rossi, F.
Montserrat, F.
Andersson, M.G.I.
Gribsholt, B.
Herman, P.M.J.
Degraer, S.
Vincx, M.
Ysebaert, T.
Middelburg, J.J.
author_sort van Colen, C.
title Organism-Sediment Interactions Govern Post-Hypoxia Recovery of Ecosystem Functioning
title_short Organism-Sediment Interactions Govern Post-Hypoxia Recovery of Ecosystem Functioning
title_full Organism-Sediment Interactions Govern Post-Hypoxia Recovery of Ecosystem Functioning
title_fullStr Organism-Sediment Interactions Govern Post-Hypoxia Recovery of Ecosystem Functioning
title_full_unstemmed Organism-Sediment Interactions Govern Post-Hypoxia Recovery of Ecosystem Functioning
title_sort organism-sediment interactions govern post-hypoxia recovery of ecosystem functioning
url https://research.wur.nl/en/publications/organism-sediment-interactions-govern-post-hypoxia-recovery-of-ec
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