Influence
of local anthropogenic terrestrial runoff on energy subsidies and
trophic dynamics of coral reefs in Tobago.
[Final Report]
J.R. Foley (james.foley@ncl.ac.uk)
MSc Tropical Coastal Management
Department of Tropical Coastal Management
School of Marine Science &
Technology
Newcastle University, Newcastle, NE1 7RU, United Kingdom
Abstract
Coral reefs in Tobago have exhibited accelerated
rates of degradation and reduced biodiversity over the past two decades
[1]. Signs of eutrophication indicate elevated nutrient inputs to
be the cause, particularly phosphorus (P) and nitrogen (N) [2]. Opinions
differ on the cause of elevated N and P concentrations in coastal
waters around Tobago. Stable isotope analysis (SIA) reveals higher
nitrogen isotope ratios (d15N) with increasing proximity to point
sources, such as sewage outfalls, fish processing plant discharges
etc. [1]; [3]; [4], and non-point sources (deforestation, agricultural
and urban runoff) of terrigenous anthropogenic effluent [4]. However,
signatures of Orinoco flooding in skeletally dense bands in radiograph
scans of cross-sections of corals indicate influence on Tobago reefs
by seasonal influxes of nutrient-rich, high turbidity freshwater runoff
from the Orinoco River in Venezuela during the wet season (June to
December) [5], and particulate organic matter (POM) and sediments
transported from the Amazon River by the coastal Guyana current [6].
A likely reality is that reef degradation in Tobago has resulted from
the combined effects of all these factors. Baseline data is needed
to assess the relative importance of continental riverine nutrient
inputs versus local nutrient inputs in influencing coral reef food
webs, and to evaluate the potential roles of these inputs as energy
subsidisers acting to promote productivity on Tobago’s coral
reefs. In contribution to the larger-scale project currently being
conducted by the Buccoo Reef Trust (BRT) in Tobago, this project uses
stable isotope analysis (SIA) to determine relative influence of local
runoff on reef function & tropic cascades during the dry season,
at six sites subject to varying degrees of local anthropogenic effluent
impact on the Caribbean coast of Tobago. This study will test the
null hypothesis that there is no effect of sewage on d15N during the
dry season, updating existing quantitative data pertaining to the
relevance of local anthropogenic nutrient inputs on coral reefs in
Tobago, and providing essential comparison with subsequent wet season
data. Combined d15N and d13C data will provide an understanding of
trophic relationships in local coral reef food webs, serving as valuable
information for use in the context of the larger-scale BRT project,
and thus contributing to the continuum of research efforts leading
towards sustainable and long-lasting management solutions for coral
reef degradation in Tobago. This will potentially provide an effective
model for tropical coastal management strategies on both regional
and global scales.
Collaborators
Prof. Nicholas Polunin, Newcastle University, UK;
Dr Jennie Mallela, University of the West Indies, Trinidad;
Dr Chris Harrod, Queens University, Northern Ireland, UK;
Dr Richard Langton, University of Maine, USA & Buccoo Reef Trust,
Tobago;
Dr Owen Day, Buccoo Reef Trust, Tobago.
References
[1] Lapointe,
B. E. (2003) Impacts of Land-Based Nutrient Pollution on Coral
Reefs in Tobago. Buccoo Reef Trust Website.
[2] IMA (1994) The formulation of a management
plan for the Buccoo Reef Marine Park. Volume 3. Biological investigations
and water quality monitoring. Institute of Marine Affairs. Prepared
for the Tobago House of Assembly 58pp.
[3] John, G. M. (1996) Quantitative Characterisation
of Land-Based Sources of Marine Pollution in the Vicinity of the
Buccoo Reef Marine Park, Tobago. University of the West Indies.
(Unpublished Thesis).
[4] Young, K. (1998) An Ecological Assessment of
Buccoo Reef/Bon Accord Lagoon Complex, Tobago: ‘Evaluating
the Trade-offs between Users of Marine Protected Areas in the Caribbean.’
Literature Review for UEA/UWI Collaborative Project.
[5] Risk, M. J., Van Wissen, F. A., Carriquiry
Beltran, J. (1992) Schlerochronology of Tobago Corals: A record
of the Orinoco? Proc. 7th Int. Cor. Reef. Symp., Guam, Vol 1.
[6] Medina, E, Francisco, M, Sternberg, L., Anderson,
W. T. (2005) Isotopic signatures of organic matter in sediments
of the continental shelf facing the Orinoco Delta: Possible contributions
of organic carbon from savannas. Estuarine, Coastal and Shelf Science
63:527-536.
[7] Humboldt-Innovation GmbH, Humboldt Universität
zu Berlin, Ziegelstraße 13c, 10117, Berlin, Deutschland http://www.humboldt-innovation.de/home/index.shtml