Contents lists available at ScienceDirect Estuarine, Coastal and Shelf Science journal homepage: www.elsevier.com/locate/ecss Intertidal foraminifera in the Spartina patens oral 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 fth replicate was tested for %C and %N. To constrain altitude, the replicates were taken immediately inland of a zone of the marsh grass Spartina alterniora, 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 inata and Miliammina fusca. The number per replicate ranged from 29 (East LaHave) to 816 (MPPP). Scheés test following ANOVA showed the mean MPPP for- aminiferal density to be signicantly dierent 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 signicant correlations between %C, %N and the mean foraminiferal densities of species. The mean population densities per 10 cm 3 of E. macrescens diered 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 inata 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. inata were not signicantly 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 aecting 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 ecacy of pollution remediation eorts (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. T