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  4. Evaluating the multidecadal response of historic seawater incursion events and salinity-induced meromixis at Laytons Lake, Nova Scotia, Canada
 
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Evaluating the multidecadal response of historic seawater incursion events and salinity-induced meromixis at Laytons Lake, Nova Scotia, Canada

Journal
Lake and Reservoir Management
Journal Volume
37
Journal Issue
4
Pages
378-390
Date Issued
2021
Author(s)
McGuire H.E
Dunnington D.W
Loder A.L
Spooner I.S
Mallory M.L
McLellan N.R
CHIH-CHIEH SU  
DOI
10.1080/10402381.2021.1941446
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85111039179&doi=10.1080%2f10402381.2021.1941446&partnerID=40&md5=fa1ba1fb4def693f68c1ad25bf4db952
https://scholars.lib.ntu.edu.tw/handle/123456789/606350
Abstract
McGuire HE, Dunnington DW, Loder AL, Spooner IS, Mallory ML, McLellan NR, Su, C-C. 2021. Evaluating the multidecadal response of historic seawater incursion events and salinity-induced meromixis at Laytons Lake, Nova Scotia, Canada. Lake Reserv Manage. 37:378–390. Long-term monitoring data from freshwater lakes can be challenging to retrieve yet are valuable for assessing lakes at risk of saltwater intrusion. We demonstrate the use of an applied paleolimnological method to identify the response of a freshwater lake to seawater incursion and salinity-induced meromixis by examining the geochemistry of lake sediments deposited over the past century. Laytons Lake is located 1.5 km from the Bay of Fundy coastline, and experienced documented seawater incursion events in 1944 and 1949 leading to a period of extended meromixis (>40 yr). Our limnological measurements indicate that meromixis no longer exists at Laytons Lake, and hypolimnetic phosphorus (P) concentrations and conductivity values have declined since 1982. Meromictic conditions, the establishment of the chemocline, and high sedimentation rates collectively preserve a geochemical record of seawater incursion, which was identified as a short-duration, positive chloride (Cl-) excursion followed by the precipitation of iron sulfide (FeS2). A decline in Cl- concentration after the incursion events in the paleorecord may represent the deterioration of the chemocline, and the reestablishment of thermal stratification and mixing. We suspect that seawater incursions can have a multidecadal impact on aquatic systems, and that bulk geochemical analysis of paleolimnological records is a useful, low-cost tool that can provide a long-term perspective on the limnological consequences of such events. These long-term data can inform the assessment of aquatic systems at risk of saltwater incursion due to sea-level rise. ? 2021 North American Lake Management Society.
Subjects
Bulk geochemistry
coastal management
lake stratification
meromixis
salinity
seawater incursion
SDGs

[SDGs]SDG14

Type
journal article

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