Abstract Warming shifts the thermal optimum of net photosynthesis (ToptA) to higher temperatures. However, our knowledge of this shift is mainly derived from seedlings grown in greenhouses under ambient atmospheric carbon dioxide (CO2) conditions. It is unclear whether shifts inToptAof field-grown trees will keep pace with the temperatures predicted for the 21stcentury under elevated atmospheric CO2concentrations. Here, using a whole-ecosystem warming controlled experiment under either ambient or elevated CO2levels, we show thatToptAof mature boreal conifers increased with warming. However, shifts inToptAdid not keep pace with warming asToptAonly increased by 0.26–0.35 °C per 1 °C of warming. Net photosynthetic rates estimated at the mean growth temperature increased with warming in elevated CO2spruce, while remaining constant in ambient CO2spruce and in both ambient CO2and elevated CO2tamarack with warming. Although shifts inToptAof these two species are insufficient to keep pace with warming, these boreal conifers can thermally acclimate photosynthesis to maintain carbon uptake in future air temperatures.
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A century of change in the California Current: upwelling system amplifies acidification
Predicting the pace of acidification in the California Current System (CCS), a productive upwelling system that borders the west coast of North America, is complex because the anthropogenic contribution is intertwined with other natural sources. A central question is whether acidification in the CCS will follow the pace of increasing atmospheric CO2, or if climate effects and other biogeochemical processes will either amplify or attenuate acidification. Here, we apply the boron isotope pH proxy to cold-water orange cup corals to establish a historic level of acidification in the CCS and the Salish Sea, an associated marginal sea. Through a combination of complementary modeling and geochemical approaches, we show that the CCS and Salish Sea have experienced amplified acidification over the industrial era, driven by the interaction between anthropogenic CO2and a thermodynamic buffering effect. From this foundation, we project future acidification in the CCS under elevated CO2emissions. The projected change inpCO2over the 21stcentury will continue to outpace atmospheric CO2, posing challenges to marine ecosystems of biological, cultural, and economic importance.
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- Award ID(s):
- 2048373
- PAR ID:
- 10660582
- Publisher / Repository:
- Nature
- Date Published:
- Journal Name:
- Nature Communications
- Volume:
- 16
- Issue:
- 1
- ISSN:
- 2041-1723
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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