Abstract

Volcanically active islands abound in the tropical Pacific and harbor complex coral communities. Whereas lava streams and deep ash deposits are well-known to devastate coral communities through burial and smothering, little is known about the effect of moderate amounts of small particulate ash deposits on reef communities. Volcanic ash contains a diversity of chemical compounds that can induce nutrient enrichments triggering changes in benthic composition. Two independently collected data sets on the marine benthos of the pristine and remote reefs around Pagan Island, Northern Mariana Islands, reveal a sudden critical transition to cyanobacteria-dominated communities in 2009–2010, which coincides with a period of continuous volcanic ash eruptions. Concurrently, localized outbreaks of the coral-killing cyanobacteriosponge Terpios hoshinota displayed a remarkable symbiosis with filamentous cyanobacteria, which supported the rapid overgrowth of massive coral colonies and allowed the sponge to colonize substrate types from which it has not been documented before. The chemical composition of tephra from Pagan indicates that the outbreak of nuisance species on its reefs might represent an early succession stage of iron enrichment (a.k.a. “black reefs”) similar to that caused by anthropogenic debris like ship wrecks or natural events like particulate deposition from wildfire smoke plumes or desert dust storms. Once Pagan's volcanic activity ceased in 2011, the cyanobacterial bloom disappeared. Another group of well-known nuisance algae in the tropical Pacific, the pelagophytes, did not reach bloom densities during this period of ash eruptions but new species records for the Northern Mariana Islands were documented. These field observations indicate that the study of population dynamics of pristine coral communities can advance our understanding of the resilience of tropical reef systems to natural and anthropogenic disturbances.

Highlights

  • Critical transitions in tropical reef systems are often characterized by a shift from a coral-dominated state to a macroalgaldominated system [1], which is mediated by a change in the microbial communities of the coral holobiont [2]

  • Cyanobacterial bloom A spatial comparison of benthic data from 222 survey sites showed a significant difference in cyanobacterial cover between the islands of Guam, Pagan, and Tinian in the Mariana Arc (F2,219 = 20.008, P,0.001; Fig. 2)

  • Post-hoc comparisons indicated that the cyanobacterial cover of Pagan in 2010 (14.162.4%; mean 6 SE) was significantly higher than that of the other two neighboring islands

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Summary

Introduction

Critical transitions in tropical reef systems are often characterized by a shift from a coral-dominated state to a macroalgaldominated system [1], which is mediated by a change in the microbial communities of the coral holobiont [2]. A recent study reported on the effects of volcanic ash deposits on the benthic communities and the reef fish populations of Anatahan Island in the Mariana Arc [15]. Since pyroclastic deposits were high during the 2003 eruption of Anatahan, the benthic assemblages of the island were mainly affected by ash burial and smothering resulting in a low cover of live coral, crustose coralline algae and other macroalgae.

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