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Estuarine, Coastal and Shelf Science
journal homepage: www.elsevier.com/locate/ecss
Intertidal foraminifera in the Spartina patens floral zone of the LaHave
Estuary, Canada: A baseline for assessing organic pollution remediation
Brent Wilson
a,b,*
, Lee-Ann C. Hayek
c
, Stella Marguerite Bowles
d
a
Cedar Lodge, Maenygroes, Ceinewydd, Ceredigion SA45 9RL, United Kingdom
b
Petroleum Geoscience Programme, Department of Chemical Engineering, The University of the West Indies, St. Augustine, Trinidad and Tobago
c
Smithsonian Institution, Mathematics and Statistics, MRC-121, P O Box 37012, Washington DC 20013-7012, USA
d
6308 Hwy 332 Upper LaHave, Nova Scotia B4V 7B3, Canada
ARTICLE INFO
Keywords:
Atlantic Canada
Middle marsh
Straight pipes
Pollution remediation
Mercury
ABSTRACT
The LaHave Estuary is polluted with domestic waste delivered via straight pipes. These are to be replaced with
septic tanks. The impact of this remediation on the wider biotic community will need to be assessed. Intertidal
foraminifera are ideal for mitigation assessment in the LaHave and comparable estuaries, estuary banks sup-
porting small beds of intertidal vegetation. This paper provides a baseline for future comparisons of the total
LaHave intertidal benthic foraminiferal assemblage and presents a method applicable to other estuaries.
Regarding the LaHave Estuary, any biotic change must be viewed against the backdrop of other pollutants like
mercury near the town of Bridgewater.
Four 10 cm
3
replicates (push cores) were taken at four sites along the estuary's eastern bank: Miller Point
Peace Park (MPPP, near Bridgewater), Dayspring, Upper LaHave and East LaHave. A fifth replicate was tested for
%C and %N. To constrain altitude, the replicates were taken immediately inland of a zone of the marsh grass
Spartina alterniflora, typically among swirl-patterned (cowlicked) S. patens.
The washed replicates were picked clean of foraminifera, 3821 being recovered. Recovery comprised only (in
rank order of abundance) Entzia macrescens, Trochammina inflata and Miliammina fusca. The number per replicate
ranged from 29 (East LaHave) to 816 (MPPP). Scheffé’s test following ANOVA showed the mean MPPP for-
aminiferal density to be significantly different from the other sites, which acted as a group. The most upstream
assemblage was dominated by E. macrescens, the most downstream by M. fusca.
There were no significant correlations between %C, %N and the mean foraminiferal densities of species. The
mean population densities per 10 cm
3
of E. macrescens differed between sites, (a) MPPP, (b) Dayspring and Upper
LaHave, and (c) East LaHave forming non-overlapping subsets that will need to be monitored separately.
Trochammina inflata mean population densities were distinct only at East LaHave. Miliammina fusca population
densities presented a peculiar pattern, MPPP and East LaHave forming one group, and the intervening Dayspring
and Upper LaHave sites forming another. The transformed mean proportions per site of E. macrescens and T.
inflata were not significantly correlated with %C or %N, but those of M. fusca were positively correlated with
both. It may be that high trace metal concentrations near Bridgewater are affecting foraminiferal distributions
and abundances. This must be taken into account when using the benthic foraminiferal assemblage to assess the
impact of the organic pollution remediation.
1. Introduction
Intertidal foraminifera associated with marsh vegetation have a long
history of study (Phleger, 1970; Phleger and Walton, 1950). Work has
concentrated on large marshes underlain by considerable thicknesses of
sediment. Modern assemblages at such sites have been used to develop
training sets for deciphering the Holocene fossil record within cores.
This has allowed modelling of Holocene sea-level change (Boomer and
Horton, 2006; Horton and Edwards, 2006; Scott and Medioli, 1980a,
1986). There have as yet been few attempts to develop baselines using
intertidal foraminiferal communities as part of an assessment of the
efficacy of pollution remediation efforts (Armynot du Châtelet and
Debenay, 2010; Armynot du Châtelet et al., 2018; Morvan et al., 2004;
Wilson and Hayek, 2018), and especially not along the length of
https://doi.org/10.1016/j.ecss.2018.08.028
Received 17 June 2018; Received in revised form 17 August 2018; Accepted 23 August 2018
*
Corresponding author. Cedar Lodge, Maenygroes, Ceinewydd, Ceredigion SA45 9RL, United Kingdom.
E-mail address: brentforam@gmail.com (B. Wilson).
Estuarine, Coastal and Shelf Science 213 (2018) 230–235
Available online 26 August 2018
0272-7714/ © 2018 Elsevier Ltd. All rights reserved.
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