Carbon and nitrogen stable isotope ratios of pelagic zooplankton elucidate ecohydrographic features in the oligotrophic Red Sea

Benjamin Kürten, Ali M. Al-Aidaroos, Saskia Kürten, Mohsen M. El-Sherbiny, Reny P. Devassy, Ulrich Struck, Nikolaos Zarokanellos, Burton H. Jones, Thomas Hansen, Gerd Bruss, Ulrich Sommer

Research output: Contribution to journalArticle

18 Citations (Scopus)

Abstract

Although zooplankton occupy key roles in aquatic biogeochemical cycles, little is known about the pelagic food web and trophodynamics of zooplankton in the Red Sea. Natural abundance stable isotope analysis (SIA) of carbon (δ13C) and N (δ15N) is one approach to elucidating pelagic food web structures and diet assimilation. Integrating the combined effects of ecological processes and hydrography, ecohydrographic features often translate into geographic patterns in δ13C and δ15N values at the base of food webs. This is due, for example, to divergent 15N abundances in source end-members (deep water sources: high δ15N, diazotrophs: low δ15N). Such patterns in the spatial distributions of stable isotope values were coined isoscapes. Empirical data of atmospheric, oceanographic, and biological processes, which drive the ecohydrographic gradients of the oligotrophic Red Sea, are under-explored and some rather anticipated than proven. Specifically, five processes underpin Red Sea gradients: (a) monsoon-related intrusions of nutrient-rich Indian Ocean water; (b) basin scale thermohaline circulation; (c) mesoscale eddy activity that causes up-welling of deep water nutrients into the upper layer; (d) the biological fixation of atmospheric nitrogen (N2) by diazotrophs; and (e) the deposition of dust and aerosol-derived N. This study assessed relationships between environmental samples (nutrients, chlorophyll a), oceanographic data (temperature, salinity, current velocity [ADCP]), particulate organic matter (POM), and net-phytoplankton, with the δ13C and δ15N values of zooplankton collected in spring 2012 from 16°28' to 26°57'N along the central axis of the Red Sea. The δ15N of bulk POM and most zooplankton taxa increased from North (Duba) to South (Farasan). The potential contribution of deep water nutrient-fueled phytoplankton, POM, and diazotrophs varied among sites. Estimates suggested higher diazotroph contributions in the North, a greater contribution of POM in the South, and of small phytoplankton in the central Red Sea. Consistent variation across taxonomic and trophic groups at latitudinal scale, corresponding with patterns of nutrient stoichiometry and phytoplankton composition, indicates that the zooplankton ecology in the Red Sea is largely influenced by hydrographic features. It suggests that the primary ecohydrography of the Red Sea is driven not only by the thermohaline circulation, but also by mesoscale activities that transports nutrients to the upper water layers and interact with the general circulation pattern. Ecohydrographic features of the Red Sea, therefore, aid in explaining the observed configuration of its isoscape at the macroecological scale.

Original languageEnglish
Pages (from-to)69-90
Number of pages22
JournalProgress in Oceanography
Volume140
DOIs
Publication statusPublished - Jan 1 2016

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Red Sea
nitrogen isotope
stable isotopes
zooplankton
stable isotope
nitrogen-fixing bacteria
phytoplankton
carbon
nutrients
food webs
nitrogen
particulate organic matter
nutrient
food web
water
thermohaline circulation
deep water
nutrient transport
stoichiometry
aerosols

ASJC Scopus subject areas

  • Aquatic Science
  • Geology

Cite this

Kürten, B., Al-Aidaroos, A. M., Kürten, S., El-Sherbiny, M. M., Devassy, R. P., Struck, U., ... Sommer, U. (2016). Carbon and nitrogen stable isotope ratios of pelagic zooplankton elucidate ecohydrographic features in the oligotrophic Red Sea. Progress in Oceanography, 140, 69-90. https://doi.org/10.1016/j.pocean.2015.11.003

Carbon and nitrogen stable isotope ratios of pelagic zooplankton elucidate ecohydrographic features in the oligotrophic Red Sea. / Kürten, Benjamin; Al-Aidaroos, Ali M.; Kürten, Saskia; El-Sherbiny, Mohsen M.; Devassy, Reny P.; Struck, Ulrich; Zarokanellos, Nikolaos; Jones, Burton H.; Hansen, Thomas; Bruss, Gerd; Sommer, Ulrich.

In: Progress in Oceanography, Vol. 140, 01.01.2016, p. 69-90.

Research output: Contribution to journalArticle

Kürten, B, Al-Aidaroos, AM, Kürten, S, El-Sherbiny, MM, Devassy, RP, Struck, U, Zarokanellos, N, Jones, BH, Hansen, T, Bruss, G & Sommer, U 2016, 'Carbon and nitrogen stable isotope ratios of pelagic zooplankton elucidate ecohydrographic features in the oligotrophic Red Sea', Progress in Oceanography, vol. 140, pp. 69-90. https://doi.org/10.1016/j.pocean.2015.11.003
Kürten, Benjamin ; Al-Aidaroos, Ali M. ; Kürten, Saskia ; El-Sherbiny, Mohsen M. ; Devassy, Reny P. ; Struck, Ulrich ; Zarokanellos, Nikolaos ; Jones, Burton H. ; Hansen, Thomas ; Bruss, Gerd ; Sommer, Ulrich. / Carbon and nitrogen stable isotope ratios of pelagic zooplankton elucidate ecohydrographic features in the oligotrophic Red Sea. In: Progress in Oceanography. 2016 ; Vol. 140. pp. 69-90.
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