Metabolic state along a summer north-south transect near the Antarctic Peninsula: A size spectra approach

• Published in: Journal of Plankton Research
• Main Authors: García Muñoz, Cristina, García, Carlos M., Lubián, Luis M., López Urrutia, Ángel, Hernández León, Santiago, Ameneiro, Julia
• Other Authors: Ministerio de Educación y Ciencia (España), European Commission, Consejo Superior de Investigaciones Científicas (España)
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Oxford University Press 2014
• Subjects: Normalized biomass size spectra; South Shetland Islands; Metabolic state; Antarctic; Antarctic Peninsula; The Antarctic; Antarc*; Copepods
• Online Access: http://hdl.handle.net/10261/102844; https://doi.org/10.1093/plankt/fbu042; https://doi.org/10.13039/501100000780; https://doi.org/10.13039/501100003339

To establish a metabolic state along a north-south transect in Antarctic waters, we approached community respiration (CR) from a combined perspective based on the metabolic theory of ecology (MTE) and the size-scaling of the whole planktonic community. A detailed analysis of a summer integrated multi-trophic normalized biomass size spectra (NBSS), from heterotrophic bacteria to zooplankton, was carried out. To acquire individual size data, different techniques were combined: flow cytometry for smaller fractions (<20 μm of equivalent spherical diameter), FlowCAM for larger nano- and microplankton and scanning and image analysis for the zooplankton fractions. The distribution of the NBSS was linear at all stations (R2 values: 0.87-0.93) but dome-shape features appeared related to phytoplankton cell distribution which are responsible for a large fraction of microbial respiration. Generally, the region showed an autotrophic budget south of the archipelago due to gross primary production (GPP) values up to 2804 mg C m-2 day-1, where salps could significantly contribute to the carbon export flux. Contrastingly, higher CR rates (.1000 mg C m-2 day-1) were found at the northern stations due to a higher phytoplankton respiration activity associated with increasing sea water temperatures and a higher presence of heterotrophic organisms (microheterotrophs, chaetognaths and copepods) resulting in a net heterotrophic metabolic state (GPP/CR < 1). © 2014 The Author. Published by Oxford University Press. All rights reserved. This work was supported by project COUPLING CTM2008-06343-C02-02/ANT from the Spanish Ministry of Science and Education. C.G-M.'s work was supported by a pre-doctoral fellowship from the Spanish Council for Research (CSIC), JAE-Predoc 2009. Peer Reviewed