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Seasonal changes in the size distribution of copepods is affected by coastal upwelling
Rosa, J.; Matos, T.; da Silva, D.; Reis, C.; Dias, C.; Konno, T.; Dias de Almeida Fernandes, L. (2023). Seasonal changes in the size distribution of copepods is affected by coastal upwelling. Diversity 15(637): 1-17. https://dx.doi.org/10.3390/d15050637
In: Diversity. MDPI: Basel. ISSN 1424-2818; e-ISSN 1424-2818, more
Peer reviewed article  

Available in  Authors 

Author keywords
    size classes; top-down control; time series; FlowCAM; ImageJ

Project Top | Authors 
  • Towards the Sustainable Development of the Atlantic Ocean: Mapping and Assessing the present and future status of Atlantic marine ecosystems under the influence of climate change and exploitation, more

Authors  Top 
  • Rosa, J.
  • Matos, T.
  • da Silva, D.
  • Reis, C.
  • Dias, C.
  • Konno, T.
  • Dias de Almeida Fernandes, L.

Abstract
    Water temperature controls the physiology, growth rate, distribution, and behavior of most plankton populations in the sea and thus affects the energy transfer in marine ecosystems. The present study focuses on the influence of seasonal changes in sea surface temperature on phytoplankton and the size distribution of copepods in the Arraial do Cabo Upwelling System (Brazil), where a wind-driven coastal upwelling can lead to multiple distinct bottom-up cascade effects on the food web. To address the potential effect of the seasonal changes, environmental data were obtained and the abundance of plankton determined from monthly samples collected in triplicate from 2010 to 2014. The samples were analyzed on a Benchtop FlowCAM (FC), and copepods (<1000 µm) were classified according to their Ellipses Equivalent Major Axis using image analysis software ImageJ (IJ). For IJ analysis, a batch-processing macro was built to open all FC raw images and then crop each copepod individually into a single picture. Using these images, prosome and urosome lengths were manually measured with the straight-line tool in IJ. With the combinations of measurements obtained in the IJ adjusted as FC measurements, we established a new, faster, and more effective way to measure copepods. With the copepod size classification, we found that there is a cycle in copepod size combined with the upwelling cycle that is related to temperature rather than to phytoplankton growth. Copepod abundance as a whole peaked during the autumn, winter, and spring seasons. The method performed here proved that FC is an effective tool for classifying copepod sizes and detecting seasonal variation.

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