Nocturnal dissolved organic matter release by turf algae and its role in the microbialization of reefs.

The increased release of dissolved organic matter (DOM) by algae has been associated with the fast but inefficient growth of opportunistic microbial pathogens and the ongoing degradation of coral reefs. Turf algae (consortia of microalgae and macroalgae commonly including cyanobacteria) dominate benthic communities on many reefs worldwide. Opposite to other reef algae that predominantly release DOM during the day, turf algae containing cyanobacteria may additionally release large amounts of DOM at night. However, this night-DOM release and its potential contribution to the microbialization of reefs remains to be investigated.We first tested the occurrence of hypoxic conditions at the turf algae-water interface, as a lack of oxygen will facilitate the production and release of fermentation intermediates as night-time DOM. Second, the dissolved organic carbon (DOC) release by turf algae was quantified during day time and nighttime, and the quality of day and night exudates as food for bacterioplankton was tested. Finally, DOC release rates of turf algae were combined with estimates of DOC release based on benthic community composition in 1973 and 2013 to explore how changes in benthic community composition affected the contribution of night-DOC to the reef-wide DOC production.A rapid shift from supersaturated to hypoxic conditions at the turf algae-water interface occurred immediately after the onset of darkness, resulting in night-DOC release rates similar to those during daytime. Bioassays revealed major differences in the quality between day and night exudates: Night-DOC was utilized by bacterioplankton two times faster than day-DOC, but yielded a four times lower growth efficiency. Changes in benthic community composition were estimated to have resulted in a doubling of DOC release since 1973, due to an increasing abundance of benthic cyanobacterial mats (BCMs), with night-DOC release by BCMs and turf algae accounting for >50% of the total release over a diurnal cycle.Night-DOC released by BCMs and turf algae is likely an important driver in the microbialization of reefs by stimulating microbial respiration at the expense of energy and nutrient transfer to higher trophic levels via the microbial loop, thereby threatening the productivity and biodiversity of these unique ecosystems. Read the free Plain Language Summary for this article on the Journal blog.

El incremento de la liberación de materia orgánica disuelta (MOD) por parte de las algas se ha asociado con el crecimiento rápido pero ineficaz de microorganismos patógenos oportunistas y la continua degradación de los arrecifes coralinos. Los céspedes algales (consorcios de micro y macroalgas que suelen incluir cianobacterias) dominan las comunidades bentónicas de muchos arrecifes de todo el mundo. A diferencia de otras algas de arrecife que liberan predominantemente MOD durante el día, los céspedes algales que contienen cianobacterias pueden liberar adicionalmente grandes cantidades de MOD durante la noche. Sin embargo, esta liberación nocturna de MOD y su potencial contribución a la microbialización de los arrecifes aún falta por ser investigada.En primer lugar, investigamos la existencia de condiciones de hipoxia en la interfase entre los céspedes algales y el agua, ya que la falta de oxígeno facilitaría la producción y liberación de productos intermedios de fermentación como MOD nocturna. En segundo lugar, cuantificamos la liberación de carbono orgánico disuelto (COD) por los céspedes algales durante el día y la noche, y se comprobó la calidad de los exudados diurnos y nocturnos como alimento para el bacterioplancton. Finalmente, las tasas de liberación de MOD de los céspedes algales se combinaron con las estimaciones de liberación de COD basadas en la composición de la comunidad bentónica en 1973 y 2013 para explorar cómo los cambios en la composición de la comunidad bentónica afectaron a la contribución de MOD nocturna y a su vez a la producción de COD en todo el arrecife.En ausencia de luz, se produjo inmediatamente un cambio rápido de condiciones sobresaturadas a condiciones hipóxicas en la interfaz entre los céspedes algales y el agua, lo que dio lugar a tasas de liberación de COD nocturnas similares a las diurnas. Los bioensayos revelaron importantes diferencias en la calidad de los exudados diurnos y nocturnos: el bacterioplancton utilizó el COD nocturno dos veces más rápido que el COD diurno, pero su eficiencia de crecimiento fue cuatro veces menor. Se estimó que los cambios en la composición de la comunidad bentónica han dado lugar a una duplicación de la liberación de MOD desde 1973 debido a la creciente abundancia de tapetes de cianobacterias bentónicas, y que la liberación nocturna de COD por parte de estos tapetes y los céspedes algales representa >50% de la liberación total durante un ciclo diurno.El COD nocturno que es liberado por los tapetes de cianobacterias bentónicas y los céspedes algales es probablemente un importante promotor de la microbialización de los arrecifes al estimular la respiración microbiana a expensas de la transferencia de energía y nutrientes a los niveles tróficos superiores a través del bucle microbiano y, por tanto, amenaza la productividad y la biodiversidad de estos ecosistemas únicos.

Nitrogen and phosphorus uptake rates of different species from a coral reef community after a nutrient pulse.

Terrestrial runoff after heavy rainfall can increase nutrient concentrations in waters overlying coral reefs that otherwise experience low nutrient levels. Field measurements during a runoff event showed a sharp increase in nitrate (75-fold), phosphate (31-fold) and ammonium concentrations (3-fold) in waters overlying a fringing reef at the island of Curaçao (Southern Caribbean). To understand how benthic reef organisms make use of such nutrient pulses, we determined ammonium, nitrate and phosphate uptake rates for one abundant coral species, turf algae, six macroalgal and two benthic cyanobacterial species in a series of laboratory experiments. Nutrient uptake rates differed among benthic functional groups. The filamentous macroalga Cladophora spp., turf algae and the benthic cyanobacterium Lyngbya majuscula had the highest uptake rates per unit biomass, whereas the coral Madracis mirabilis had the lowest. Combining nutrient uptake rates with the standing biomass of each functional group on the reef, we estimated that the ammonium and phosphate delivered during runoff events is mostly taken up by turf algae and the two macroalgae Lobophora variegata and Dictyota pulchella. Our results support the often proposed, but rarely tested, assumption that turf algae and opportunistic macroalgae primarily benefit from episodic inputs of nutrients to coral reefs.

Organic matter degradation drives benthic cyanobacterial mat abundance on Caribbean coral reefs.

Benthic cyanobacterial mats (BCMs) are impacting coral reefs worldwide. However, the factors and mechanisms driving their proliferation are unclear. We conducted a multi-year survey around the Caribbean island of Curaçao, which revealed highest BCM abundance on sheltered reefs close to urbanised areas. Reefs with high BCM abundance were also characterised by high benthic cover of macroalgae and low cover of corals. Nutrient concentrations in the water-column were consistently low, but markedly increased just above substrata (both sandy and hard) covered with BCMs. This was true for sites with both high and low BCM coverage, suggesting that BCM growth is stimulated by a localised, substrate-linked release of nutrients from the microbial degradation of organic matter. This hypothesis was supported by a higher organic content in sediments on reefs with high BCM coverage, and by an in situ experiment which showed that BCMs grew within days on sediments enriched with organic matter (Spirulina). We propose that nutrient runoff from urbanised areas stimulates phototrophic blooms and enhances organic matter concentrations on the reef. This organic matter is transported by currents and settles on the seabed at sites with low hydrodynamics. Subsequently, nutrients released from the organic matter degradation fuel the growth of BCMs. Improved management of nutrients generated on land should lower organic loading of sediments and other benthos (e.g. turf and macroalgae) to reduce BCM proliferation on coral reefs.

High dissolved organic carbon release by benthic cyanobacterial mats in a Caribbean reef ecosystem.

Benthic cyanobacterial mats (BCMs) are increasing in abundance on coral reefs worldwide. However, their impacts on biogeochemical cycling in the surrounding water and sediment are virtually unknown. By measuring chemical fluxes in benthic chambers placed over sediment covered by BCMs and sediment with BCMs removed on coral reefs in Curaçao, Southern Caribbean, we found that sediment covered by BCMs released 1.4 and 3.5 mmol C m(-2) h(-1) of dissolved organic carbon (DOC) during day and night, respectively. Conversely, sediment with BCMs removed took up DOC, with day and night uptake rates of 0.9 and 0.6 mmol C m(-2) h(-1). DOC release by BCMs was higher than reported rates for benthic algae (turf and macroalgae) and was estimated to represent 79% of the total DOC released over a 24 h diel cycle at our study site. The high nocturnal release of DOC by BCMs is most likely the result of anaerobic metabolism and degradation processes, as shown by high respiration rates at the mat surface during nighttime. We conclude that BCMs are significant sources of DOC. Their increased abundance on coral reefs will lead to increased DOC release into the water column, which is likely to have negative implications for reef health.