Abstract

We used continuous measurements of dissolved oxygen (DO) in dark bottles to characterise patterns of the dark respiration rate (Rdark) for three marine phytoplankton monocultures and in natural-water samples from two marine coastal systems. Furthermore, patterns of ecosystem community respiration rate were determined from open-water changes in DO in a fjord and in a lake. We considered two models of Rdark to describe temporal changes in DO: constant Rdark and decreasing Rdark; increasing Rdark. In addition, the effect of incubation time on Rdark was investigated in bottle incubations. Constant Rdark was observed in short-term (12-h) bottle incubations in natural-water samples from two marine coastal systems. Declining Rdark was observed in marine phytoplankton cultures and open-water measurements in a lake. Increasing Rdark was observed in open-water measurements in a fjord, particularly during summer. Long-term (120-h) bottle incubations in natural-water samples showed an increase in Rdark after 48 and 72h. We show that the conventional expectation of constant rates of respiration in darkness is far from typical, because non-linear changes are common under both controlled experimental conditions, as well as for open-water measurements of ecosystem respiration.

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