Foraminiferal community response to seasonal anoxia in Lake Grevelingen (the Netherlands)
Over the last decades, hypoxia in marine coastal environments has become more and more widespread, prolonged and intense. Hypoxic events have large consequences for the functioning of benthic ecosystems. In severe cases, they may lead to complete anoxia and the presence of toxic sulfides in the sedi...
Gespeichert in:
Veröffentlicht in: | Biogeosciences 2020-03, Vol.17 (6), p.1415-1435 |
---|---|
Hauptverfasser: | , , , , , , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
Zusammenfassung: | Over the last decades, hypoxia in marine coastal
environments has become more and more widespread, prolonged and intense.
Hypoxic events have large consequences for the functioning of benthic
ecosystems. In severe cases, they may lead to complete anoxia and the presence
of toxic sulfides in the sediment and bottom-water, thereby strongly
affecting biological compartments of benthic marine ecosystems. Within these
ecosystems, benthic foraminifera show a high diversity of ecological
responses, with a wide range of adaptive life strategies. Some species are
particularly resistant to hypoxia–anoxia, and consequently it is interesting
to study the whole foraminiferal community as well as species-specific
responses to such events. Here we investigated the temporal dynamics of
living benthic foraminiferal communities (recognised by
CellTracker™ Green) at two sites in the saltwater Lake
Grevelingen in the Netherlands. These sites are subject to seasonal anoxia
with different durations and are characterised by the presence of free
sulfide (H2S) in the uppermost part of the sediment. Our results
indicate that foraminiferal communities are impacted by the presence of
H2S in their habitat, with a stronger response in the case of longer
exposure times. At the deepest site (34 m), in summer 2012, 1 to 2
months of anoxia and free H2S in the surface sediment resulted in an
almost complete disappearance of the foraminiferal community. Conversely, at
the shallower site (23 m), where the duration of anoxia and free H2S
was shorter (1 month or less), a dense foraminiferal community was found
throughout the year except for a short period after the stressful event.
Interestingly, at both sites, the foraminiferal community showed a delayed
response to the onset of anoxia and free H2S, suggesting that the
combination of anoxia and free H2S does not lead to increased
mortality, but rather to strongly decreased reproduction rates. At the
deepest site, where highly stressful conditions prevailed for 1 to 2
months, the recovery time of the community takes about half a year. In Lake
Grevelingen, Elphidium selseyense and Elphidium magellanicum are much less affected by anoxia and free H2S than
Ammonia sp. T6. We hypothesise that this is not due to a higher tolerance for
H2S, but rather related to the seasonal availability of food sources,
which could have been less suitable for Ammonia sp. T6 than for the elphidiids. |
---|---|
ISSN: | 1726-4189 1726-4170 1726-4189 |
DOI: | 10.5194/bg-17-1415-2020 |