2017
DOI: 10.1016/j.ecolind.2017.06.035
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Assessing nature and dynamics of POM in transitional environment (the Curonian Lagoon, SE Baltic Sea) using a stable isotope approach

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Cited by 20 publications
(5 citation statements)
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“…Indeed, a field study showed a relatively small POC:Chl ratio (160~170 g:g) in the western subarctic region 38 . Overall, the observed POC:Chl ratios are close to the value (~200 g:g) representing the predominance of local biological activities in POC production 39,40 , indicating that biological processes are largely responsible for the higher levels of surface POC observed in the subarctic region.…”
Section: Discussionsupporting
confidence: 64%
“…Indeed, a field study showed a relatively small POC:Chl ratio (160~170 g:g) in the western subarctic region 38 . Overall, the observed POC:Chl ratios are close to the value (~200 g:g) representing the predominance of local biological activities in POC production 39,40 , indicating that biological processes are largely responsible for the higher levels of surface POC observed in the subarctic region.…”
Section: Discussionsupporting
confidence: 64%
“…We also found a significant (p < 0.01) negative correlation between C/N and PN and a positive correlation between C/N and δ 15 N (Table 2; Figure 3), indicating the disturbance from anthropogenic nitrogen inputs to the middle and lower basin of the Iyidere River and changes the composition of POM. Similar δ 15 N values (>8‰) were also reported for the eutrophication of rivers with high nutrient and municipal wastewater loads that enter the Baltic Sea (Lesutienė et al, 2014;Remeikaitė-Nikienė et al, 2017;Amir et al, 2019).…”
Section: Spring Seasonsupporting
confidence: 82%
“…The high d 15 N range on the Odra Bank could be due to either, the benthic invertebrate community covering two trophic levels, if considering a trophic fractionation factor of ~3‰ (Post, 2002), or, and most likely, high variability in d 15 N values of basal sources. d 15 N values of basal sources in the coastal Baltic Sea are highly spatially and seasonally variable due to a combination of factors including availability of inorganic nitrogen, riverine versus marine influence and seasonal phytoplankton succession (Maksymowska et al, 2000;Lesutienėet al, 2014;Remeikaite-Nikienėet al, 2017). Studies in the Curonian lagoon showed that the d 15 N values of particulate organic matter (POM) potentially range within one year from -0.9 ‰ to 15.5 ‰ (Remeikaite-Nikienėet al, 2017).…”
Section: Isotopic Variability In Prey Speciesmentioning
confidence: 99%