The first week in April Mass. Division of Marine Fisheries divers Wes Dukes and Vin
Malkoski surveyed our West Falmouth eelgrass monitoring sites and this is what they saw.
They observed algae coating the eelgrass
plants and moorings in a fluffy flocculent layer. The
pictures above are from a site in the outer harbor, where there is more flushing
and better water quality than most of the rest of the harbor. The first two show algae coating the bottom over eelgrass and a mooring line and the third picture is of fouling on a conservation mooring floating rode. Are we observing the spring macroalgal peak biomass?
Or was this amount of algae here all winter? A study in Waquoit Bay (Fox et al. 2008) showed peak algae biomass from
May to June. However they also found that nitrogen stressed embayments experienced both larger seasonal
differences in algae biomass and a larger persistent crop of algae during
the seasonal low. After a long winter which didn't seem to be over in the beginning of April, I wonder if this algae bloom is an early spring bloom or the persistent
winter standing crop? If it is the
latter, then the biomass of algae may be a warning of
further declining conditions to come.
A little bit about bloom-forming algae and nutrient loading:
Benthic and epiphytic algae (Algae on the harbor bottom and
growing on eelgrass, etc.) grow rapidly and utilize nutrients quickly, compared to non-bloom, slower growing seagrass. Therefore they are an indicator of poor water quality and high
nutrient loading to a system. Algal blooms
can shade the water column preventing light from getting to eelgrass
plants and eventually killing them.
When algae dies the decomposing process consumes large amounts of oxygen creating an inhospitable environment for many fish and invertebrates as well as eelgrass.
When algae dies the decomposing process consumes large amounts of oxygen creating an inhospitable environment for many fish and invertebrates as well as eelgrass.
Nutrients
can come overland from stormwater and snowmelt, running off lawns and roads,
or from the groundwater. West Falmouth
harbor is a eutrophic, ground water-fed
estuary. That means that nutrient
(nitrogen) levels are high and that most of the freshwater input is coming from
the groundwater. Estuarine
eutrophication can lead to hypoxia (low oxygen), habitat degradation (eelgrass
decline), loss of biodiversity and increase in harmful algal blooms. In 2003 West Falmouth
harbor had three times as much nitrogen in the water as it did in the mid 1990s
(Thoms et al 2003). The increased nitrogen was found to be mainly coming from the groundwater plume
from Falmouth’s wastewater treatment plant (Thoms et al. 2003).
In
Waquoit Bay, Fox et al (2008) found that
total macroalgal biomass increased with increasing nitrogen loads and that the
two dominant macroalgae showed greater
biomass in the high nitrogen load systems, while eelgrass was the dominant primary
producer only in the low nitrogen estuaries.
Over the last two decades, eelgrass has disappeared from most of the
Waquoit Bay estuary and shading by algae, together with degraded water and sediment conditions, is cited as the likely cause. Will West Falmouth have the same fate?
What do “conservation moorings” have to do with water
quality in West Falmouth harbor?
We are now in our second season of a project to test "eelgrass friendly moorings" or "conservation moorings" in West Falmouth harbor. Below is a picture of the two different systems used in West Falmouth, the Hazelett rode and the Eco-mooring rode with a helix anchor shown too.
We have seen from our work in Manchester Harbor that reducing or eliminating
chain drag enables eelgrass to grow in a former mooring scar. But another consequence may be improved water
quality. The conventional mooring chain stirs up and resuspends the
sediment causing increased turbidity (cloudy water) and possibly resuspension of
nitrogen back into the water column.
Conservation moorings do no drag on the harbor bottom because they are
constructed with floating mooring chain and helix anchors to minimize impacts
to the bottom. So it is possible that minimizing chain drag may reduce suspended turbidity and suspended nutrients in West Falmouth Harbor.
References:
Fox SE, E. Stieve, I. Valiela, J. Hauxwell. J.
McClelland. (2008) Macrophyte abundance
in Waquoit Bay:effects of land-derived nitrogen loads on seasonal and multi-year
biomass patterns. Estuaries and Coasts Vol. 31 pp. 532-541
Thoms T, A.E. Giblin, K.H. Foreman. (2003) Multiple approaches to tracing nitrogen loss in the west Falmouth waste water plume. The Biological Bulletin, Vol. 205, pp. 242-243
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