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Climate models require an understanding of ecosystem-scale respiration and photosynthesis, yet there is no way of measuring these two fluxes directly; here, new instrumentation is used to determine these fluxes in a temperate forest, showing, for instance, that respiration is less during the day than at night. Seasonal variation in forest productivity Much of the carbon dioxide emitted into the atmosphere is taken up by forest ecosystems. Forest carbon sink estimates are based on the idea that ecosystem respiration is greater during the day than at night and that the efficiency of photosynthetic light use declines after spring. Rick Wehr et al. determine ecosystem photosynthesis and daytime respiration in a temperate deciduous forest over a three-year period on the basis of the isotopic composition of net ecosystem exchange. The work reveals that ecosystem respiration is in fact lower during the day than at night -- evidence of the inhibition of leaf respiration by light (the Kok effect) at the ecosystem scale. The authors argue that current approaches for estimating photosynthesis and daytime respiration do not take this effect into account and therefore overestimate ecosystem photosynthesis and daytime respiration at their forest site, and portray ecosystem photosynthetic light-use efficiency as declining when it is in fact stable. The findings may have implications for estimates of biospheric productivity and carbon cycle-climate interactions. Terrestrial ecosystems currently offset one-quarter of anthropogenic carbon dioxide (CO.sub.2) emissions because of a slight imbalance between global terrestrial photosynthesis and respiration.sup.1. Understanding what controls these two biological fluxes is therefore crucial to predicting climate change.sup.2. Yet there is no way of directly measuring the photosynthesis or daytime respiration of a whole ecosystem of interacting organisms; instead, these fluxes are generally inferred from measurements of net ecosystem-atmosphere CO.sub.2 exchange (NEE), in a way that is based on assumed ecosystem-scale responses to the environment. The consequent view of temperate deciduous forests (an important CO.sub.2 sink) is that, first, ecosystem respiration is greater during the day than at night; and second, ecosystem photosynthetic light-use efficiency peaks after leaf expansion in spring and then declines.sup.3, presumably because of leaf ageing or water stress. This view has underlain the development of terrestrial biosphere models used in climate prediction.sup.4,5 and of remote sensing indices of global biosphere productivity.sup.5,6. Here, we use new isotopic instrumentation.sup.7 to determine ecosystem photosynthesis and daytime respiration.sup.8 in a temperate deciduous forest over a three-year period. We find that ecosystem respiration is lower during the day than at night--the first robust evidence of the inhibition of leaf respiration by light.sup.9,10,11 at the ecosystem scale. Because they do not capture this effect, standard approaches.sup.12,13 overestimate ecosystem photosynthesis and daytime respiration in the first half of the growing season at our site, and inaccurately portray ecosystem photosynthetic light-use efficiency. These findings revise our understanding of forest-atmosphere carbon exchange, and provide a basis for investigating how leaf-level physiological dynamics manifest at the canopy scale in other ecosystems., Author(s): R. Wehr [sup.1] , J. W. Munger [sup.2] , J. B. McManus [sup.3] , D. D. Nelson [sup.3] , M. S. Zahniser [sup.3] , E. A. Davidson [sup.4] , [...]