How do temperature,dissolved organic matter and nutrients influence the response of Leptodiaptomus ashlandi to UV radiation in a subalpine lake?

1. Ultraviolet radiation (UV) is an important stressor for zooplankton in alpine lake ecosystems. Multiple environmental variables such as dissolved organic matter (DOM), temperature and nutrient availability may alter how UV affects zooplankton. 2. We conducted a week‐long experiment manipulating UV, nutrients and DOM in enclosures suspended at the surface of cold and warm alpine lakes to determine the interactive effects of these variables on ovigerous Leptodiaptomus ashlandi (Marsh, 1893), a calanoid copepod. 3. UV had a negative effect on nauplii and gravid females at the colder temperature and at low, ambient DOM levels, but had no effect at the warmer temperature or when DOM was added. At the warmer temperature, fewer nauplii were produced in the +nutrient compared to ?nutrient treatment. Adult survival was not affected by UV or any other experimental variable. 4. These results demonstrate that the extent of the impact of UV radiation on zooplankton in alpine systems is altered by other environmental variables, and that these effects may not be apparent from experiments that look only at the survival of adult organisms that are better defended against UV.     

Does the 13C of foliage‐respired CO2 and biochemical pools reflect the 13C of recently assimilated carbon?

Isotopic labelling experiments were conducted to assess relationships among ¹³C of recently assimilated carbon ( δC _A), foliage respiration ( δC _F), soluble carbohydrate ( δC _SC), leaf waxes ( δC _LW) and bulk organic matter ( δC _OM). Slash pine, sweetgum and maize were grown under ¹³C depleted CO₂ to label biomass and then placed under ambient conditions to monitor the loss of label. In pine and sweetgum, δC _F of labelled plants (∼−44 and −35‰, respectively) rapidly approached control values but remained depleted by ∼4–6‰ after 3–4 months. For these tree species, no or minimal label was lost from δC _SC, δC _LW and δC _OM during the observation periods. δC _F and δC _SC of labelled maize plants rapidly changed and were indistinguishable from controls after 1 month, while δC _LW and δC _OM more slowly approached control values and remained depleted by 2–6‰. Changes in δC _F in slash pine and sweetgum fit a two-pool exponential model, with the fast turnover metabolic pool (∼3–4 d half-life) constituting only 1–2% of the total. In maize, change in δC _F fits a single pool model with a half-life of 6.4 d. The ¹³C of foliage respiration and biochemical pools reflect temporally integrated values of δC _A, with change in isotopic composition dampened by the size of metabolic carbon reserves and turnover rates.