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Limiting global warming to 2 °C is unlikely to save most coral reefs

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TLDR
It is shown that preserving >10% of coral reefs worldwide would require limiting warming to below 1.5C (atmosphere-ocean general circulation models (AOGCMs) range: 1.3-1.8C) relative to pre-industrial levels.
Abstract
Comprehensive computer simulations show that coral reefs are likely to suffer extensive long-term degradation resulting from mass bleaching events even if the expected increase in global mean temperature can be kept well below 2 °C Without major mitigation efforts to limit global warming significantly, the fate of coral reef ecosystems seems to be sealed

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Pervasive human-driven decline of life on Earth points to the need for transformative change

Sandra Díaz, +37 more
- 13 Dec 2019 - 
TL;DR: The first integrated global-scale intergovernmental assessment of the status, trends, and future of the links between people and nature provides an unprecedented picture of the extent of the authors' mutual dependence, the breadth and depth of the ongoing and impending crisis, and the interconnectedness among sectors and regions.
References
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Journal ArticleDOI

Global assessment of coral bleaching and required rates of adaptation under climate change

TL;DR: This article conducted a comprehensive global assessment of coral bleaching under climate change by adapting the NOAA Coral Reef Watch bleaching prediction method to the output of a low and high-climate sensitivity GCM.
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The future of coral reefs

TL;DR: The fossil record suggests that corals as a group are more likely to suffer extinctions than some of the groups that associate with them, whose habitat requirements may be less stringent.
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Coral reefs may start dissolving when atmospheric CO2 doubles

TL;DR: In this paper, the authors provided a global estimate of the decline in calcification of coral reefs as a result of increase in sea surface temperature and partial pressure of CO2, which is based on an empirical rate law developed from field observations for gross community calcification as a function of aragonite degree of saturation (Ωarag), sea surface temperatures and live coral cover.
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The effect of carbonate chemistry on calcification and photosynthesis in the hermatypic coral Acropora eurystoma

TL;DR: In this article, the authors report the results of three laboratory experiments designed specifically to separate the effects of different carbonate chemistry parameters (pH, CO 22 3,C O2 [aq], total alkalinity [AT], and total inorganic carbon [CT]) on the calcification, photosynthesis, and respiration of the hermatypic coral Acropora eurystoma.
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Remote sensing of sea surface temperatures during 2002 Barrier Reef coral bleaching

TL;DR: Early in 2002, satellites of the U.S. National Oceanic and Atmospheric Administration (NOAA) detected anomalously high sea surface temperatures (SST) developing in the western Coral Sea, midway along Australia's Great Barrier Reef (GBR) as discussed by the authors.
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