Diel variations in inorganic carbon and nitrogen uptake by phytoplankton in an arctic lake

Time—depth variations in inorganic carbon and nitrogen uptake by phytoplankton in Toolik Lake were examined over 36 h using isotope tracer techniques. Rates of dissolved inorganic carbon (DIC = CO 2 + <f>$${\hbox{ HCO }}_{3}^{-}$$</f> + <f>$${\hbox{ CO }}_{3}^{2-}$$</f>) and...

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Bibliographic Details
Published in:Journal of Plankton Research
Main Authors: Whalen, S.C., Alexander, V.
Format: Text
Language:English
Published: Oxford University Press 1984
Subjects:
Online Access:http://plankt.oxfordjournals.org/cgi/content/short/6/4/571
https://doi.org/10.1093/plankt/6.4.571
Description
Summary:Time—depth variations in inorganic carbon and nitrogen uptake by phytoplankton in Toolik Lake were examined over 36 h using isotope tracer techniques. Rates of dissolved inorganic carbon (DIC = CO 2 + <f>$${\hbox{ HCO }}_{3}^{-}$$</f> + <f>$${\hbox{ CO }}_{3}^{2-}$$</f>) and maximum <f>$${\hbox{ NO }}_{3}^{-}$$</f> uptake were phased with the did high light/low light regime characteristic of the brief arctic summer with the amplitude of oscillation greater for DIC than for <f>$${\hbox{ NO }}_{3}^{-}$$</f>. Ammonium uptake was continuous at uptake-saturating concentrations. No conclusive evidence was found for a diel periodicity in nitrogenous nutrient levels or uptake of <f>$${\hbox{ NO }}_{3}^{-}$$</f> and <f>$${\hbox{ NH }}_{4}^{+}$$</f> ambient concentrations. A pronounced light—temperature effect on dissolved inorganic nitrogen (DIN = <f>$${\hbox{ NO }}_{3}^{-}$$</f> + <f>$${\hbox{ NH }}_{4}^{+}$$</f>) uptake was evident at depth when rates of uptake were maximum. Depth-integrated daily C/N uptake ratios (mol) estimated as the mean of four consecutive 6 h incubations ranged from 1.8–6.4 under conditions of substrate saturation and from 6.0–16.1 at ambient levels of DIN. The efficacy of 24 h incubations to estimate accurately day-rates of DIC and substrate-saturated DIN uptake was assessed by comparing estimates obtained from 24 h exposures to those approximated by summing results from serial short-term incubations. Experiments of 24 h duration accurately predicted day-rates of maximum <f>$${\hbox{ NO }}_{3}^{-}$$</f> uptake but underestimated daily DIC uptake by 13 � 7% (<f>$$\stackrel{\¯}{\hbox{ X }}$$</f> � SD). Day-length incubations introduced serious errors in the estimation of day-rates of maximum <f>$${\hbox{ NH }}_{4}^{+}$$</f> uptake, effecting an underestimation of 29 � 5% (<f>$$\stackrel{\¯}{\hbox{ X }}$$</f> � SD).