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Chris Langdon

Researcher at Oregon State University

Publications -  246
Citations -  16394

Chris Langdon is an academic researcher from Oregon State University. The author has contributed to research in topics: Oyster & Crassostrea. The author has an hindex of 60, co-authored 237 publications receiving 14990 citations. Previous affiliations of Chris Langdon include York University & Lamont–Doherty Earth Observatory.

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Geochemical Consequences of Increased Atmospheric Carbon Dioxide on Coral Reefs

TL;DR: A coral reef represents the net accumulation of calcium carbonate (CaCO3) produced by corals and other calcifying organisms, and if calcification declines, then reef-building capacity also declines.
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Losers and winners in coral reefs acclimatized to elevated carbon dioxide concentrations

TL;DR: In this article, the authors investigated coral reefs, seagrasses and sediments that are acclimatized to low pH at three cool and shallow volcanic carbon dioxide seeps in Papua New Guinea.
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Effect of elevated pCO2 on photosynthesis and calcification of corals and interactions with seasonal change in temperature/irradiance and nutrient enrichment

TL;DR: In this article, the effects of elevated pCO2 on the net production and calcification of an assemblage of corals maintained under near-natural conditions of temperature, light, nutrient, and flow were investigated.
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Effect of calcium carbonate saturation state on the calcification rate of an experimental coral reef

TL;DR: In this article, the authors investigated the effect of projected changes in seawater carbonate chemistry on the calcification of coral reef organisms at the community scale and found that there were consistent and reproducible changes in the rate of calcification in response to their manipulations of the saturation state.
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The Pacific oyster, Crassostrea gigas, shows negative correlation to naturally elevated carbon dioxide levels: Implications for near-term ocean acidification effects

TL;DR: Both larval production and midstage growth of the oyster Crassostrea gigas were significantly negatively correlated with the aragonite saturation state of waters in which larval oysters were spawned and reared for the first 48 h of life.