Cargando…

Benthic primary production in an upwelling-influenced coral reef, Colombian Caribbean

In Tayrona National Natural Park (Colombian Caribbean), abiotic factors such as light intensity, water temperature, and nutrient availability are subjected to high temporal variability due to seasonal coastal upwelling. These factors are the major drivers controlling coral reef primary production as...

Descripción completa

Detalles Bibliográficos
Autores principales: Eidens, Corvin, Bayraktarov, Elisa, Hauffe, Torsten, Pizarro, Valeria, Wilke, Thomas, Wild, Christian
Formato: Online Artículo Texto
Lenguaje:English
Publicado: PeerJ Inc. 2014
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4157237/
https://www.ncbi.nlm.nih.gov/pubmed/25237604
http://dx.doi.org/10.7717/peerj.554
Descripción
Sumario:In Tayrona National Natural Park (Colombian Caribbean), abiotic factors such as light intensity, water temperature, and nutrient availability are subjected to high temporal variability due to seasonal coastal upwelling. These factors are the major drivers controlling coral reef primary production as one of the key ecosystem services. This offers the opportunity to assess the effects of abiotic factors on reef productivity. We therefore quantified primary net (P(n)) and gross production (P(g)) of the dominant local primary producers (scleractinian corals, macroalgae, algal turfs, crustose coralline algae, and microphytobenthos) at a water current/wave-exposed and-sheltered site in an exemplary bay of Tayrona National Natural Park. A series of short-term incubations was conducted to quantify O(2) fluxes of the different primary producers during non-upwelling and the upwelling event 2011/2012, and generalized linear models were used to analyze group-specific O(2) production, their contribution to benthic O(2) fluxes, and total daily benthic O(2) production. At the organism level, scleractinian corals showed highest P(n) and P(g) rates during non-upwelling (16 and 19 mmol O(2) m(−2) specimen area h(−1)), and corals and algal turfs dominated the primary production during upwelling (12 and 19 mmol O(2) m(−2) specimen area h(−1), respectively). At the ecosystem level, corals contributed most to total P(n) and P(g) during non-upwelling, while during upwelling, corals contributed most to P(n) and P(g) only at the exposed site and macroalgae at the sheltered site, respectively. Despite the significant spatial and temporal differences in individual productivity of the investigated groups and their different contribution to reef productivity, differences for daily ecosystem productivity were only present for P(g) at exposed with higher O(2) fluxes during non-upwelling compared to upwelling. Our findings therefore indicate that total benthic primary productivity of local autotrophic reef communities is relatively stable despite the pronounced fluctuations of environmental key parameters. This may result in higher resilience against anthropogenic disturbances and climate change and Tayrona National Natural Park should therefore be considered as a conservation priority area.