Poster's note : obliquely relevant to OIF and to some of the coral
protection work done recently - but mainly of interest as an "off topic"
post on the severe (but neglected) issue of marine impacts of AGW. A very
readable blog post on this paper is at
http://www.climatecentral.org/news/ocean-warming-species-change-19051

http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate2650.html

Future vulnerability of marine biodiversity compared with contemporary and
past changes

Grégory Beaugrand, Martin Edwards, Virginie Raybaud, Eric Goberville &
Richard R. Kirby

Nature Climate Change (2015) doi:10.1038/nclimate2650

Published online 01 June 2015

Abstract

Many studies have implied significant effects of global climate change on
marine life. Setting these alterations into the context of historical
natural change has not been attempted so far, however. Here, using a
theoretical framework, we estimate the sensitivity of marine pelagic
biodiversity to temperature change and evaluate its past (mid-Pliocene and
Last Glacial Maximum (LGM)), contemporaneous (1960–2013) and future
(2081–2100; 4 scenarios of warming) vulnerability. Our biodiversity
reconstructions were highly correlated to real data for several pelagic
taxa for the contemporary and the past (LGM and mid-Pliocene) periods. Our
results indicate that local species loss will be a prominent phenomenon of
climate warming in permanently stratified regions, and that local species
invasion will prevail in temperate and polar biomes under all climate
change scenarios. Although a small amount of warming under the RCP2.6
scenario is expected to have a minor influence on marine pelagic
biodiversity, moderate warming (RCP4.5) will increase by threefold the
changes already observed over the past 50 years. Of most concern is that
severe warming (RCP6.0 and 8.5) will affect marine pelagic biodiversity to
a greater extent than temperature changes that took place between either
the LGM or the mid-Pliocene and today, over an area of between 50 (RCP6.0:
46.9–52.4%) and 70% (RCP8.5: 69.4–73.4%) of the global ocean.

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