Abstract
The devastating earthquake (moment magnitude: 8.8 MW) that struck Chile on 27 Feb- ruary 2010 and the following tsunami waves produced widespread damage, coastal coseismic uplifts, and large-scale mortality of rocky intertidal and shallow subtidal organisms. The effects were partic- ularly remarkable around the Gulf of Arauco, Santa Maria Island and the Bay of Concepcion (~36 to 38° S). Measurements of rocky intertidal and shallow subtidal belt-forming (biomarker) species con- ducted a few weeks after the earthquake indicated coastal uplifts ranging from ~0.2 to 3.1 m, which are similar to uplifts estimated by FitzRoy (1839; Voyages of the Adventure and Beagle, Vol. II) and Darwin (1839; Voyages of the Adventure and Beagle, Vol. III) after the 1835 Chilean earthquake. In major uplifted sites, there was massive mortality of the main intertidal and shallow subtidal belt- forming species, such as lithothamnioid melobesioid coralline algae, brown kelps and mussels, and dramatic changes in the marine rocky intertidal ecosystem. We suggest that in the southeastern Pacific, drastic and rapid coastal deformations seriously impinge on rocky shore populations, commu- nities and ecosystems and may have significance for management and conservation practices, as for example in connection with alterations of parental stocks and recruitment rates.
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