Seawater carbonate chemistry and carbon and nitrogen allocation strategy in Posidonia oceanica

DOI

Rising atmospheric CO2 causes ocean acidification that represents one of the major ecological threats for marine biota. We tested the hypothesis that long-term exposure to increased CO2 level and acidification in a natural CO2 vent system alters carbon (C) and nitrogen (N) metabolism in Posidonia oceanica L. (Delile), affecting its resilience, or capability to restore the physiological homeostasis, and the nutritional quality of organic matter available for grazers. Seawater acidification decreased the C to N ratio in P. oceanica tissues and increased grazing rate, shoot density, leaf proteins and asparagine accumulation in rhizomes, while the maximum photochemical efficiency of photosystem II was unaffected. The 13C-dilution in both structural and non-structural C metabolites in the acidified site indicated quali-quantitative changes of C source and/or increased isotopic fractionation during C uptake and carboxylation associated with the higher CO2 level. The decreased C:N ratio in the acidified site suggests an increased N availability, leading to a greater storage of 15N-enriched compounds in rhizomes. The amount of the more dynamic C storage form, sucrose, decreased in rhizomes of the acidified site in response to the enhanced energy demand due to higher shoot recruitment and N compound synthesis, without affecting starch reserves. The ability to modulate the balance between stable and dynamic C reserves could represent a key ecophysiological mechanism for P. oceanica resilience under environmental perturbation. Finally, alteration in C and N dynamics promoted a positive contribution of this seagrass to the local food web.

Supplement to: Scartazza, Andrea; Moscatello, Stefano; Gavrichkova, Olga; Buia, Maria-Cristina; Lauteri, Marco; Battistelli, Alberto; Lorenti, Maurizio; Garrard, Samantha Laird; Calfapietra, Carlo; Brugnoli, Enrico (2017): Carbon and nitrogen allocation strategy in Posidonia oceanica is altered by seawater acidification. Science of the Total Environment, 607-608, 954-964

Identifier
DOI https://doi.org/10.1594/PANGAEA.890444
Related Identifier IsSupplementTo https://doi.org/10.1016/j.scitotenv.2017.06.084
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.890444
Provenance
Creator Scartazza, Andrea; Moscatello, Stefano; Gavrichkova, Olga ORCID logo; Buia, Maria-Cristina (ORCID: 0000-0002-2370-898X); Lauteri, Marco ORCID logo; Battistelli, Alberto ORCID logo; Lorenti, Maurizio ORCID logo; Garrard, Samantha Laird ORCID logo; Calfapietra, Carlo; Brugnoli, Enrico ORCID logo
Publisher PANGAEA
Publication Year 2017
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 414 data points
Discipline Earth System Research
Spatial Coverage (13.966 LON, 40.730 LAT)