Resumen
Protected areas require long-term monitoring to understand the influence and extent of ecosystem stress to inform management and conservation decisions. As long-term data are not always available, paleolimnological methods offer a way of extending our knowledge of past environmental conditions necessary to use as context for remediation. Here, we examine four sediment cores and additional surface sediments from 14 ponds located on Sable Island National Park Reserve Canada (SINPR), where long-term ecological changes and vulnerability to disturbance are not well defined. We develop a paleolimnological approach to assessing environmental vulnerability through the use of biological indicators (Diptera: Chironomidae), where shifts in the environment are inferred by shifts in chironomid assemblages over time. Analysis of surface sediments show four distinct assemblage types reflecting four different habitat conditions; primarily represented by the presence of Glyptotendipes, Chironomus, Microtendipes, and Dicrotendipes. Differences in habitat conditions through time based on these results are then compared to biostratigraphic analysis of sediment cores from four of the ponds. We found that two ponds had large shifts in chironomids assemblages that were associated with changes in habitat over time, while two others that were not as exposed to the influence of erosion and influx of sand dunes did not. Our findings established a baseline of historical change in SINPR, broadening the scope of long-term monitoring, which is essential for defining goals for management and conservation of the ecological integrity of Sable Island.
Idioma original | English |
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Publicación | Science Progress |
Volumen | 105 |
N.º | 4 |
DOI | |
Estado | Published - oct. 2022 |
Nota bibliográfica
Funding Information:The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: This work was supported by the Marine Environmental Observation Prediction and Response Network, the City of Halifax, and Dalhousie University (Fathom Fund, projectDAL)
Funding Information:
Nova Scotia and Sable Island National Park Reserve are located in Mi’kma’ki, the unceded and ancestral territory of the Mi’kmaq People; we are grateful for the opportunity to research on this land. Logistical and field sampling support was provided by Parks Canada. We thank Frederica Jacks and Michael Bakaic for field sampling assistance, and Connor Nishikawa, Kathleen Hipwell, and Jennifer Eamer for laboratory assistance. We thank Jordan Eamer for discussions on Sable Island’s changing morphology. Logan Horrocks assisted with creation of the map used in Figure 1. Samples were collected under a Parks Canada research permit: SINP-2019-32317. The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: This work was supported by the Marine Environmental Observation Prediction and Response Network, the City of Halifax, and Dalhousie University (Fathom Fund, projectDAL)
Publisher Copyright:
© The Author(s) 2022.
ASJC Scopus Subject Areas
- General
PubMed: MeSH publication types
- Journal Article