EGU25-12515, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-12515
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 28 Apr, 08:30–10:15 (CEST), Display time Monday, 28 Apr, 08:30–12:30
 
Hall X1, X1.39
Combining sediment analysis with geospatial mapping to quantify carbon sequestration by an eelgrass bed on the Nova Scotian coast, eastern Canada. 
Emma Taniguchi1, Amy Mui2, Kristina Boerder3, Markus Kienast1, and Craig Brown1
Emma Taniguchi et al.
  • 1Dalhousie University, Department of Oceanography, Halifax, Canada (emmataniguchi@dal.ca)
  • 2Dalhousie University, Department of Earth and Environmental Sciences, Halifax, Canada
  • 3Dalhousie University, Department of Biology, Halifax, Canada

In recent years, seagrass has been presented as a solution to sequester excess carbon emissions from the atmosphere, with studies reporting that seagrass meadows are responsible for burying as much as 10% of anthropogenic carbon per year (Fourqurean et al. 2012). However, this estimate has started to seem improbable as more recent research, specifically from North American study sites, are reporting carbon stock estimates much lower than the global average. Here, we present estimates of organic carbon (OC) stock in an eelgrass meadow on the Eastern Shore of Nova Scotia, Canada. To quantify sediment OC stock, we combined sediment geochemical analysis with geospatial mapping based on high-resolution optical aerial imagery collected by drone flights. Three sediment cores, plus a control, were extracted from the meadow in regions with differing levels of vegetative cover. The control core was used to establish a background signal for sediment OC, which we assume to be representative of nearshore unvegetated sediments in the region.

Despite the health and anecdotally reported longevity of this eelgrass meadow measuring 4.7 Ha in size, the carbon stock is estimated to be less than 10 Mg OC/Ha. This is significantly lower than the global average estimates of ~163.3-660 Mg/Ha (Fourqurean et al. 2012) but is comparable to other reports emerging from the North American east coast (eg. 3.7 Mg/Ha from coastal Virginia, US: Greiner et al. 2013). From the individual core slices, the maximum sediment OC did not exceed 2.5 weight % even in the densest, healthiest part of the meadow. There was also a notable correlation between presence of coarse biomass and higher sediment OC in the bulk sample, suggesting that the carbon is mostly associated with living biomass rather than being buried and stored in sediments. Further, radiocarbon ages of the bulk OC of up to 1140 years in the topmost sediment layer imply a significant admixture of pre-aged, likely terrestrial, OC to the bulk OC, rendering the stock estimates absolute maximum estimates. Overall, this study adds to the growing body of evidence that suggests that global estimates of OC storage in eelgrass beds need to be carefully reevaluated. 

How to cite: Taniguchi, E., Mui, A., Boerder, K., Kienast, M., and Brown, C.: Combining sediment analysis with geospatial mapping to quantify carbon sequestration by an eelgrass bed on the Nova Scotian coast, eastern Canada. , EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-12515, https://doi.org/10.5194/egusphere-egu25-12515, 2025.