Coral Reefs Essay -- Environment, Global Degradation

Coral reefs have been undergoing orbicular degradation due to increasing ingrained and anthropogenic impacts for at least the last half-century. The intensity and frequency of stressors, including global climate change, have rapidly increased in number oer recent years (Hughes & Connell 1999 Hoegh-Guldberg et al. 2007 Pandolfi et al. 2011). Frequent disturbances such as hurricanes/cyclones, predation outbreaks, diseases and stack bleaching events eat-away at the percent of living coral cover and without recovery, the available pose is colonized by sponges, soft corals, and macroalgae. These alternative organisms are often private-enterprise(a) dominants in less than ideal conditions (Norstrm et al. 2009). The transition is termed a phase-shift from a coral-dominated landscape to one that is dominated by other benthic organisms. Phase-shifts are also often associated with low-herbivory (from disease and/or overfishing) and nutrient enrichment (from run-off and coastal eutrop hication)(see congener Dominance Model in Littler et al. 2006 2009). The resilience of particular coral species to recover and/or resist disturbance and subsequent phase-shifts may be indicative of which coral reefs are more or less imperiled. Macroalgae are frequently the competitive dominant driving phase-shifts, thus coral-macroalgal phase-shifts is widely use to describe unusually low-levels of coral cover and a persistent arouse of high macroalgal cover. There have been a number of studies and reviews describing the negative set up of macroalgae and phase-shifts on coral reefs (Done 1992 Hughes & Connell 1999 Hughes et al. 2003 Hughes et al. 2007 McCook et al. 2001 McManus & Polsenberg 2004 Birrell et al. 2008 Bruno et al. 2009). Potential competitive... ...(SML) microbial samples were collected in Belize, the Florida Keys, and St. doubting Thomas U.S.V.I. along interaction gradients between two ubiquitous Caribbean corals (Montastraea faveolata and Porites astreoides), a nd their interaction with foliose brown macroalgae (Dictyota menstrualis), and calcareous green macroalgae (Halimeda opuntia). These macroalgae were chosen because they are known to drop coral growth rates, increase coral tissue mortality, and produce squiffy allelochemicals that are active against coral reef microorganisms (Ballantine et al. 1987 Lirman 2001 Beach et al. 2003 Rashar & Hay 2010 Morrow et al. 2011). We give tongue to that macroalgae can shift M. faveolata microbial assemblages more readily than P. astreoides. We also lay down that coral microbial assemablages of both species were less stable in Florida than at Belize or St. Thomas sampling sites.