The rising temperature of the world's oceans has become a major threat to coral reefs globally as the severity and frequency of mass coral bleaching and mortality events increase. In 2005, high ocean temperatures in the tropical Atlantic and Caribbean resulted in the most severe bleaching event ever recorded in the basin. Satellite-based tools provided warnings for coral reef managers and scientists, guiding both the timing and location of researchers' field observations as anomalously warm conditions developed and spread across the greater Caribbean region from June to October 2005. Field surveys of bleaching and mortality exceeded prior efforts in detail and extent, and provided a new standard for documenting the effects of bleaching and for testing nowcast and forecast products. Collaborators from 22 countries undertook the most comprehensive documentation of basin-scale bleaching to date and found that over 80% of corals bleached and over 40% died at many sites. The most severe bleaching coincided with waters nearest a western Atlantic warm pool that was centered off the northern end of the Lesser Antilles. Thermal stress during the 2005 event exceeded any observed from the Caribbean in the prior 20 years, and regionally-averaged temperatures were the warmest in over 150 years. Comparison of satellite data against field surveys demonstrated a significant predictive relationship between accumulated heat stress (measured using NOAA Coral Reef Watch's Degree Heating Weeks) and bleaching intensity. This severe, widespread bleaching and mortality will undoubtedly have long-term consequences for reef ecosystems and suggests a troubled future for tropical marine ecosystems under a warming climate.

The anthozoan sub-class Octocorallia, comprising approximately 3000 species of soft corals, gorgonians, and sea pens, remains one of the most poorly understood groups of the phylum Cnidaria. Efforts to classify the soft corals and gorgonians at the suprafamilial level have long thwarted taxonomists, and the subordinal groups in current use are widely recognized to represent grades of colony forms rather than clades. Molecular phylogenetic analyses of the sub-class do not support either the current morphologically based subordinal or familial-level taxonomy. To date, however, the resolution necessary to propose an alternative, phylogenetic classification of Octocorallia or to elucidate patterns of morphological evolution within the group is lacking. Attempts to understand boundaries between species and interspecific or intraspecific phylogenetic relationships have been hampered by the very slow rate of mitochondrial gene evolution in Octocorallia, and a consequent dearth of molecular markers with variation sufficient to distinguish species (or sometimes genera). A review of the available ITS2 sequence data for octocorals, however, reveals a yet-unexplored phylogenetic signal both at sequence and secondary-structure levels. In addition, incongruence between mitochondrial and nuclear gene trees suggests that hybrid speciation and reticulate evolution may be an important mechanism of diversification in some genera. Emerging next-generation genomic-sequencing technologies offer the best hope for a breakthrough in our understanding of phylogenetic relationships and of evolution of morphological traits in Octocorallia. Genome and transcriptome sequencing may provide enough characters to resolve relationships at the deepest levels of the octocoral tree, while simultaneously offering an efficient means to screen for new genetic markers variable enough to distinguish species and populations.