2 research outputs found
Key biogeochemical factors affecting soil carbon storage in Posidonia meadows
Unidad de excelencia MarÃa de Maeztu MdM-2015-0552Biotic and abiotic factors influence the accumulation of organic carbon (Corg) in seagrass ecosystems. We surveyed Posidonia sinuosa meadows growing in different water depths to assess the variability in the sources, stocks and accumulation rates of Corg. We show that over the last 500 years, P. sinuosa meadows closer to the upper limit of distribution (at 2-4m depth) accumulated 3- to 4-fold higher Corg stocks (averaging 6.3 kg Corg m¯²/ at 3- to 4-fold higher rates (12.8 gCorg m¯² yr¯¹/ compared to meadows closer to the deep limits of distribution (at 6-8m depth; 1.8 kg Corg m¯² and 3.6 g Corg m¯² yr¯¹/. In shallower meadows, Corg stocks were mostly derived from seagrass detritus (88% in average) compared to meadows closer to the deep limit of distribution (45% on average). In addition, soil accumulation rates and fine-grained sediment content (< 0.125 mm) in shallower meadows (2.0mm yr¯¹ and 9 %, respectively) were approximately 2-fold higher than in deeper meadows (1.2mm yr¯¹ and 5 %, respectively). The Corg stocks and accumulation rates accumulated over the last 500 years in bare sediments (0.6 kg Corg m¯² and 1.2 g Corg m¯² yr¯¹/ were 3- to 11-fold lower than in P. sinuosa meadows, while fine-grained sediment content (1 %) and seagrass detritus contribution to the Corg pool (20 %) were 8- and 3-fold lower than in Posidonia meadows, respectively. The patterns found support the hypothesis that Corg storage in seagrass soils is influenced by interactions of biological (e.g., meadow productivity, cover and density), chemical (e.g., recalcitrance of Corg stocks) and physical (e.g., hydrodynamic energy and soil accumulation rates) factors within the meadow. We conclude that there is a need to improve global estimates of seagrass carbon storage accounting for biogeochemical factors driving variability within habitats
Key biogeochemical factors affecting soil carbon storage in <i>Posidonia</i> meadows
Biotic and abiotic factors influence the accumulation of organic carbon
(C<sub>org</sub>) in seagrass ecosystems. We surveyed <i>Posidonia sinuosa</i> meadows growing in
different water depths to assess the variability in the sources, stocks and
accumulation rates of C<sub>org</sub>. We show that over the last 500 years, <i>P. sinuosa</i>
meadows closer to the upper limit of distribution (at 2–4 m depth)
accumulated 3- to 4-fold higher C<sub>org</sub> stocks (averaging 6.3 kg C<sub>org</sub> m<sup>−2</sup>) at 3- to
4-fold higher rates (12.8 g C<sub>org</sub> m<sup>−2</sup> yr<sup>−1</sup>)
compared to meadows closer to the deep limits of distribution (at 6–8 m
depth; 1.8 kg C<sub>org</sub> m<sup>−2</sup> and 3.6 g C<sub>org</sub> m<sup>−2</sup> yr<sup>−1</sup>). In
shallower meadows, C<sub>org</sub> stocks were mostly derived from seagrass
detritus (88 % in average) compared to meadows closer to the deep limit of
distribution (45 % on average). In addition, soil accumulation rates and
fine-grained sediment content (< 0.125 mm) in shallower meadows (2.0 mm yr<sup>−1</sup> and 9 %, respectively) were approximately 2-fold higher than
in deeper meadows (1.2 mm yr<sup>−1</sup> and 5 %, respectively). The C<sub>org</sub>
stocks and accumulation rates accumulated over the last 500 years in bare
sediments (0.6 kg C<sub>org</sub> m<sup>−2</sup> and 1.2 g C<sub>org</sub> m<sup>−2</sup> yr<sup>−1</sup>)
were 3- to 11-fold lower than in <i>P. sinuosa</i> meadows, while fine-grained sediment
content (1 %) and seagrass detritus contribution to the C<sub>org</sub> pool
(20 %) were 8- and 3-fold lower than in <i>Posidonia</i> meadows, respectively. The
patterns found support the hypothesis that C<sub>org</sub> storage in seagrass
soils is influenced by interactions of biological (e.g., meadow productivity,
cover and density), chemical (e.g., recalcitrance of C<sub>org</sub> stocks) and
physical (e.g., hydrodynamic energy and soil accumulation rates) factors
within the meadow. We conclude that there is a need to improve global
estimates of seagrass carbon storage accounting for biogeochemical factors
driving variability within habitats