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

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 mult...

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Bibliographic Details
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: 55674751000, 55675097100, 6603675433, 6602569062, 6701465678, 16645098300
Format: Article in Journal/Newspaper
Language:English
Published: 0142-7873 2014
Subjects:
251001 Oceanografía biológica
Metabolic state
Normalized biomass size spectra
South Shetland Islands
Antarctic
Antarctic Peninsula
The Antarctic
Antarc*
Copepods
Online Access:http://hdl.handle.net/10553/49860
https://doi.org/10.1093/plankt/fbu042
Description
Summary: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).

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