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Impact of extreme coastal events on a brackish lake on the Burin Peninsula, Newfoundland, Canada.
Pleskot, Krzysztof; Cwynar, Les C; Kolaczek, Piotr; Mroczkowska, Agnieszka; Suchora, Magdalena; Kowalczyk, Cyprian; Kokocinski, Mikolaj.
Afiliação
  • Pleskot K; Geohazards Research Unit, Institute of Geology, Adam Mickiewicz University, Krygowskiego 12, 61-680 Poznan, Poland. Electronic address: krzypl@amu.edu.pl.
  • Cwynar LC; Department of Biology, University of New Brunswick, Fredericton, NB E3B 5A3, Canada. Electronic address: cwynar@unb.ca.
  • Kolaczek P; Climate Change Ecology Research Unit, Adam Mickiewicz University, Krygowskiego 10, 61-680 Poznan, Poland. Electronic address: piotr.kolaczek@amu.edu.pl.
  • Mroczkowska A; Polish Academy of Sciences, Institute of Geography and Spatial Organization, Past Landscape Dynamics Laboratory, 51/55 Twarda St., Warsaw 00-818, Poland. Electronic address: agnieszka.mroczkowska@twarda.pan.pl.
  • Suchora M; Institute of Earth and Environmental Sciences, Maria Curie-Sklodowska University, Krasnicka 2 d, 20-718 Lublin, Poland. Electronic address: magdalena.suchora@mail.umcs.pl.
  • Kowalczyk C; Department of Hydrobiology, Adam Mickiewicz University, Uniwersytetu Poznanskiego 6, 61-614 Poznan, Poland. Electronic address: cyprian.kowalczyk@amu.edu.pl.
  • Kokocinski M; Department of Hydrobiology, Adam Mickiewicz University, Uniwersytetu Poznanskiego 6, 61-614 Poznan, Poland. Electronic address: mikolaj.kokocinski@amu.edu.pl.
Sci Total Environ ; 935: 173330, 2024 Jul 20.
Article em En | MEDLINE | ID: mdl-38777054
ABSTRACT
The impacts of extreme coastal events (ECEs), such as marine inundations or extreme wind events, on lake ecosystems vary widely from minimal to catastrophic. Accurately predicting the response of a specific system remains challenging due to a limited understanding of the attributes that drive the resilience of lakes. In an attempt to better understand the possible impacts of ECEs on shallow brackish lakes, we employed a paleolimnological approach to reconstruct the responses of Broad Pond to four ECEs identifiable from clear sedimentary markers and dated to ca. 1740, 1790, 1862, and 1993 CE. We aimed to evaluate the overall impacts of ECEs on Broad Pond and their specific effects on various hydrobiont groups. We reinvestigated a previously studied sediment core covering the last ca. 400 years by examining terrestrial and aquatic pollen, spores and non-pollen palynomorphs, cladocerans, and chironomids. Additionally, available diatom data were reexamined. Overall, Broad Pond exhibited resilient responses to ECEs, as indicated by mostly limited compositional turnovers in our proxy records. Statistically significant relationships between species composition and ECEs were observed only for diatoms. The only prolonged change identified is the spread of previously near-absent chironomids in the aftermath of a slight lake refreshment likely associated with the ca. 1740 CE event. This event was also followed by a short-lived (ca. 15 years) five-fold increase in the abundance of Scenedesmus that could have been triggered by the effects of the ECE on nutrient availability. The impact of the remaining three ECEs was discernible only in the diatom record, consistently showing a decline in two calcifobic and oligotrophic species, Achnanthidium petersenii and Platessa oblongella, also evident for the ca. 1740 CE event. The relatively minor ecosystem alteration induced by ECEs in Broad Pond lacks a single explanation and requires consideration of multiple site- and event-specific factors.
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Texto completo: 1 Base de dados: MEDLINE Assunto principal: Lagos / Monitoramento Ambiental País como assunto: America do norte Idioma: En Ano de publicação: 2024 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Lagos / Monitoramento Ambiental País como assunto: America do norte Idioma: En Ano de publicação: 2024 Tipo de documento: Article