Title of article :
Impact of a flood event on benthic and pelagic coupling in a sub-tropical east Australian estuary (Brunswick)
Author/Authors :
Bradley D. Eyre، نويسنده , , Angus J.P. Ferguson، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2006
Abstract :
We examined the impact of a 1:3 year return period flood on benthic and pelagic coupling in the river-dominated sub-tropical Brunswick
Estuary. The flood had a significant impact on the study site flushing it with freshwater, reducing the flushing time 0.6 days, increasing nutrient
concentrations in the water column and scouring the sediment surface. In the three weeks post-flood the benthic and pelagic systems alternated
between being coupled and un-coupled via dissolved, particulate and living material pathways. Immediately post-flood benthic and pelagic coupling
via the deposition of phyto-detritus and viable algal cells was reduced due to the scouring of the top sediment layers, and benthic respiration
and productivity and NH4
C effluxes all decreased correspondingly. In contrast, benthic and pelagic coupling was enhanced via the uptake
and denitrification of NO3
due to elevated NO3
concentrations in the water column. Some of the NO3
consumed by the sediments may have
also been converted to DON. Two weeks post-flood benthic and pelagic coupling was significantly enhanced via the deposition of phyto-detritus
and viable algal cells associated with a phytoplankton bloom in the water column. This increased supply of phyto-detritus and viable algal cells
rapidly increased benthic respiration and productivity and NH4
C efflux. The depletion of water column DIN by the phytoplankton bloom resulted
in a de-coupling of the benthic and pelagic systems via the uptake and denitrification of NO3
. However, benthic and pelagic coupling was enhanced
via the uptake of NH4
C by benthic microalgae. Three weeks post-flood the phytoplankton bloom had collapsed and the coupling between
the benthic and pelagic systems via the deposition of phyto-detritus and living algal cells had diminished. Again benthic and pelagic coupling
was enhanced via the uptake and denitrification of NO3
due to elevated NO3
concentrations in the water column associated with the recycling of
bloom material. Overall the sediments became less heterotrophic (increasing benthic productivity/respiration ratio) following the flood. Floods
can cause rapid and complex changes in the coupling between benthic and pelagic systems in sub-tropical estuaries.
Keywords :
benthic nutrient fluxes , denitrification , Tropical , benthic and pelagic coupling , flood , benthic metabolism
Journal title :
Estuarine, Coastal and Shelf Science
Journal title :
Estuarine, Coastal and Shelf Science