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δ15N and δ13C analysis of a Posidonia sinuosa seagrass bed
Smit, A.J.; Brearley, A.; Hyndes, G.A.; Lavery, P.S.; Walker, D.I. (2006). δ15N and δ13C analysis of a Posidonia sinuosa seagrass bed. Aquat. Bot. 84(3): 277-282. http://dx.doi.org/10.1016/j.aquabot.2005.11.005
In: Aquatic Botany. Elsevier Science: Tokyo; Oxford; New York; London; Amsterdam. ISSN 0304-3770; e-ISSN 1879-1522, meer
Peer reviewed article  

Beschikbaar in  Auteurs 

Trefwoorden
    Algae
    Aquatic organisms > Marine organisms > Aquatic animals > Marine invertebrates
    Fauna > Aquatic organisms > Aquatic animals > Fish
    Flora > Weeds > Marine organisms > Seaweeds > Sea grass
    Isotopes
    Isotopes > Stable isotopes
    Posidonia sinuosa Cambridge & Kuo, 1979 [WoRMS]
    Marien/Kust
Author keywords
    stable isotope; invertebrate; seagrass; macroalgae; fish; Posidoniasinuosa

Auteurs  Top 
  • Smit, A.J.
  • Brearley, A.
  • Hyndes, G.A.
  • Lavery, P.S.
  • Walker, D.I.

Abstract
    Potential food sources and dominant invertebrates and fishes were collected for the examination of variability in 13C/12C and 15N/14N to determine the sources of carbon available to consumers within a Western Australian Posidonia sinuosa-dominated seagrass bed. Autotrophs showed a wide distribution of δ13C values, with P. sinuosa at −11.3 ± 0.8‰ and macroalgae ranging from −16.6 to −31.7‰. This variation allowed us to successfully identify macroalgae as the main contributor of carbon to the trophic structure, although no distinction could be made between epiphytic macroalgae on seagrass, or allochthonous macroalgal sources. The range in δ15N ratios among potential food items at the trophic base was too small to make it useful as tracer of nitrogen flow pathways, but it consistently increased from macrophytes and detritus (4.1–6.8‰), to invertebrates (5.7–7.4‰) located near the middle of the food web, to fishes (8.3–11.9‰), with piscivorous species such as Leviprora inops generally having a higher 15N. δ13C of seston (−12.8‰) and sedimentary organic matter (−8.7‰) indicate that seagrass material is the main contributor to these two carbon pools, and that very little of it contributes to animal biomass.

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