TY - JOUR
T1 - Sediment dynamics of natural and restored Bolboschoenus maritimus saltmarsh
AU - Taylor, Benjamin W.
AU - Paterson, David M.
AU - Baxter, John M.
N1 - The authors received funding from the MASTS pooling initiative (The Marine Alliance for Science and Technology for Scotland) and Scottish Natural Heritage (SNH), their support is gratefully acknowledged. MASTS is funded by the Scottish Funding Council (grant reference HR09011) and contributing institutions.
PY - 2019/6/26
Y1 - 2019/6/26
N2 - Saltmarshes are biogeomorphic ecosystems comprising halophytic plant
communities typically located on low energy temperate coasts. Their
distribution and structure are controlled by several key drivers,
including sediment supply, type of vegetation, elevation, and local
hydrodynamics. These dynamic systems are highly vulnerable and estimated
to be experiencing annual losses of 1–2% globally. Past restoration
efforts have largely implemented managed realignment strategies,
however, examples of, and research on, conservation initiatives
employing direct transplantation of saltmarsh vegetation into damaged or
receding saltmarsh stands is less common. Here an example of
transplantation restoration was investigated to understand its influence
on sediment dynamics. Sediment settlement, deposition, and accretion
rates of natural and restored vegetation (Bolboschoenus maritimus)
and adjacent bare mudflats in a small estuary system were studied
across consecutive seasons from summer 2015 to spring 2016 to examine
the success of transplantation. Natural areas of B. maritimus were shown to be most effective at retaining deposited material, although experiencing the least amount of deposition (an average of 48 g/m2
per day), accreting by nearly 7.5 mm over the experimental period.
Mudflat areas experienced the most deposition (an average of 322 g/m2
per day) whilst exhibiting the greatest erosion over the study, a
decrease in level of 6 mm. Restored areas experience similar rates of
deposition as their natural counterparts, however, did not retain this
material as efficiently, presenting an erosion of 1.6 mm. The study
indicates certain biogeomorphic processes have been altered within the
restored area and beginning to reflect those of the natural area.
However, the restored vegetation does not yet fully match the
functionality of the natural B. maritimus stand, specifically
where the natural stand displayed a net accretion of material the
restored area did not. Such discrepancies may impact on the continued
survival of the restoration site, which may have implications for the
potential of transplanting to deliver ecosystem services, such as
climate change mitigation through carbon burial.
AB - Saltmarshes are biogeomorphic ecosystems comprising halophytic plant
communities typically located on low energy temperate coasts. Their
distribution and structure are controlled by several key drivers,
including sediment supply, type of vegetation, elevation, and local
hydrodynamics. These dynamic systems are highly vulnerable and estimated
to be experiencing annual losses of 1–2% globally. Past restoration
efforts have largely implemented managed realignment strategies,
however, examples of, and research on, conservation initiatives
employing direct transplantation of saltmarsh vegetation into damaged or
receding saltmarsh stands is less common. Here an example of
transplantation restoration was investigated to understand its influence
on sediment dynamics. Sediment settlement, deposition, and accretion
rates of natural and restored vegetation (Bolboschoenus maritimus)
and adjacent bare mudflats in a small estuary system were studied
across consecutive seasons from summer 2015 to spring 2016 to examine
the success of transplantation. Natural areas of B. maritimus were shown to be most effective at retaining deposited material, although experiencing the least amount of deposition (an average of 48 g/m2
per day), accreting by nearly 7.5 mm over the experimental period.
Mudflat areas experienced the most deposition (an average of 322 g/m2
per day) whilst exhibiting the greatest erosion over the study, a
decrease in level of 6 mm. Restored areas experience similar rates of
deposition as their natural counterparts, however, did not retain this
material as efficiently, presenting an erosion of 1.6 mm. The study
indicates certain biogeomorphic processes have been altered within the
restored area and beginning to reflect those of the natural area.
However, the restored vegetation does not yet fully match the
functionality of the natural B. maritimus stand, specifically
where the natural stand displayed a net accretion of material the
restored area did not. Such discrepancies may impact on the continued
survival of the restoration site, which may have implications for the
potential of transplanting to deliver ecosystem services, such as
climate change mitigation through carbon burial.
KW - Accretion
KW - Restoration
KW - Saltmarsh
KW - Seasonal
KW - Sediment deposition
U2 - 10.3389/fevo.2019.00237
DO - 10.3389/fevo.2019.00237
M3 - Article
AN - SCOPUS:85068602006
SN - 2296-701X
VL - 7
JO - Frontiers in Ecology and Evolution
JF - Frontiers in Ecology and Evolution
M1 - 237
ER -