2019
DOI: 10.1098/rsbl.2018.0831
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Variation of carbon contents in eelgrass ( Zostera marina ) sediments implied from depth profiles

Abstract: Seagrass meadows are able to store significant amounts of organic carbon in their underlying sediment, but global estimates are uncertain partly owing to spatio-temporal heterogeneity between and within areas and species. In order to provide robust estimates, there is a need to better understand the fate of, and mechanisms behind, organic carbon storage. In this observational study, we analyse a suite of biotic and abiotic parameters in sediment cores from 47 different eelgrass ( Zostera marina … Show more

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Cited by 15 publications
(18 citation statements)
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“…Some tropical seagrass species can, for instance, be a direct source of inorganic carbon to the sediment by formation of aragonite crystals in the leaves (Enríquez & Schubert, ); this has, however, not been seen in any temperate seagrass species. The C: N ratio was similar to previous studies on the Swedish west coast (Dahl, Deyanova, Gütschow, et al, ; Pihl et al, ) and elsewhere in the region (Kindeberg et al, ), with low nitrogen content in relation to organic carbon levels, which is also commonly found in other seagrass areas (Gullström et al, ; Santos et al, ). The highest nitrogen content was found in the carbon‐rich, sheltered site of Getevik, as the nitrogen content is known to positively correlate to both carbon‐ and silt‐clay content (Kindeberg et al, ).…”
Section: Discussionsupporting
confidence: 89%
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“…Some tropical seagrass species can, for instance, be a direct source of inorganic carbon to the sediment by formation of aragonite crystals in the leaves (Enríquez & Schubert, ); this has, however, not been seen in any temperate seagrass species. The C: N ratio was similar to previous studies on the Swedish west coast (Dahl, Deyanova, Gütschow, et al, ; Pihl et al, ) and elsewhere in the region (Kindeberg et al, ), with low nitrogen content in relation to organic carbon levels, which is also commonly found in other seagrass areas (Gullström et al, ; Santos et al, ). The highest nitrogen content was found in the carbon‐rich, sheltered site of Getevik, as the nitrogen content is known to positively correlate to both carbon‐ and silt‐clay content (Kindeberg et al, ).…”
Section: Discussionsupporting
confidence: 89%
“…This study highlights the within‐year dynamics of sedimentary carbon content and the influence of seasonality on carbon stock levels in cold‐temperate seagrass meadows. Not only does Z. marina meadows display a large spatial variation in carbon storage (Dahl, Deyanova, Gütschow, et al, ; Green et al, ; Kindeberg et al, ; Röhr et al, ), but as shown in this study, there is also a high seasonal variability (at all sediment depth layers down to at least 30 cm) where sedimentary carbon levels both increased and decreased over the year. Our findings show a peak carbon density in June (0.0139 ± 0.0009 g cm −3 ) and the lowest in August (0.0089 ± 0.0008 g cm −3 ), and the PLS model indicated that there was a negative correlation between TOC stocks and NCP.…”
Section: Resultssupporting
confidence: 54%
“…S3 b,c). The average (± SE) carbon and nitrogen stocks were 2,219 ± 335 gC m −2 and 215 ± 32 gN m −2 , respectively (for site-specific stock data, see Table 1 ), which are in the range of previous estimates for the Skagerrak area 15 , 33 . The sediment density (gDW cm −3 ) in the deeper part of the meadows was also positively correlated to wave exposure (d.f.…”
Section: Resultssupporting
confidence: 62%
“…There were no changes in carbon and nitrogen content along the sediment depth profiles down to the maximum depth of about 60 cm, which strengthens the argument that the surface content (0-5 cm) sampled for the 53 meadows in the large survey is valid for evaluating meadows for long-term carbon storage, as similar values between the surface-and deeper sediment layers are expected. However, this might also indicate that there is a mixing of the sediment layers 33 , for instance from bioturbation, as the organic matter content would otherwise decrease due to remineralization 64 . Therefore, the upper 50-60 cm of the sediment might potentially still be within the remineralization zone 65 , with declining carbon and nitrogen content and refractory accumulation occurring in deeper layers of the sediment 51 .…”
Section: Discussionmentioning
confidence: 99%
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