In evergreen conifers, where the foliage amount changes little with season, accurate detection of the underlying "photosynthetic phenology" from satellite remote sensing has been difficult, presenting challenges for global models of ecosystem carbon uptake. Here, we report a close correspondence between seasonally changing foliar pigment levels, expressed as chlorophyll/carotenoid ratios, and evergreen photosynthetic activity, leading to a "chlorophyll/carotenoid index" (CCI) that tracks evergreen photosynthesis at multiple spatial scales. When calculated from NASA's Moderate Resolution Imaging Spectroradiometer satellite sensor, the CCI closely follows the seasonal patterns of daily gross primary productivity of evergreen conifer stands measured by eddy covariance. This discovery provides a way of monitoring evergreen photosynthetic activity from optical remote sensing, and indicates an important regulatory role for carotenoid pigments in evergreen photosynthesis. Improved methods of monitoring photosynthesis from space can improve our understanding of the global carbon budget in a warming world of changing vegetation phenology.carotenoid pigments | evergreen conifers | gross primary productivity | chlorophyll/carotenoid index | CCI T he biosphere helps regulate atmospheric composition and climate, in part through the exchange of radiatively active gases, primarily carbon dioxide. About half of the "extra" carbon added to the atmosphere by human activity is rapidly absorbed by the biosphere, effectively slowing climate change relative to what would occur without this uptake (1, 2). The exact mechanism and spatiotemporal distribution of the terrestrial component of this carbon sink have been ongoing research topics for many years. In a warming world, the timing of photosynthetic activity is also changing, with unknown impacts on ecosystem productivity. These shifting patterns of seasonal photosynthetic activity, or "photosynthetic phenology," affect the biospheric-atmospheric gas exchange, further influencing atmospheric composition and climate (3-5). Faced with these uncertainties, quantifying the spatial and temporal patterns of biosphere/atmosphere carbon fluxes for different biomes and understanding their proximal controls remain central goals of global carbon cycle science.Northern forests make a large contribution to global photosynthetic carbon fixation and are an important component of the global carbon budget. However, northern evergreen conifers, including evergreen conifers of the vast boreal regions, present particular challenges to global carbon cycle monitoring (6). Their seasonal activity may be changing with an earlier growing season, with important implications for the biospheric carbon budget. A simple hypothesis has been that a longer growing season results in greater carbon uptake, particularly for northern ecosystems where photosynthetic activity has been temperature-limited (3, 7). By contrast, warmer growing seasons are also more likely to cause drought, restricting ecosystem carbon uptake...