Turbid reef - The DigitalGlobe Foundation
Transcription
Turbid reef - The DigitalGlobe Foundation
Distribution and environmental controls on contemporary and late-Holocene inshore coral reef growth under conditions of high terrigenous sediment inputs on the central Great Barrier Reef K. Morgan1, C. Perry1, S. Smithers2, J. Daniell2 and J. Johnson1 1 Department of Geography, University of Exeter, Exeter, United Kingdom 2 School of Marine Biology, James Cook University, Townsville, Australia Clear-water reef Turbid reef Clear-water reef Turbid reef • Naturally high sedimentation >100 Nephelometric Turbidity Units (NTU) >10 NTU 46% of time • Sediment detrimental to reef “health” – Growth and calcification – Abundance and diversity – Disease and mortality • Evidence of high coral cover and rapid reef development (<2000 y) Great Barrier Reef Shelf Poor understanding of: • • • • Distribution Extent Ecology Growth history Outer shelf Study area: Inshore Inner-shelf Townsville 24 km Mid-shelf Townsville Area: Central Great Barrier Reef (Beaman et al. 2010) Paluma Shoals Reefs, Halifax Bay, GBR, Australia OPSB “Juvenile” OPSA OPSC & OPSD “Juvenile” “Early juvenile” OPS “Mature” Coral carpets “Incipient coral community” Paluma Shoals “Late mature” 1 km • Close to coast (3 km) • Experiences high turbidity • Spectrum of reef developmental states • At risk of land-based threats Satellite image courtesy of the DigitalGlobe Foundation Paluma Shoals Morphology Subaqueous linear ridges (1.5 x 0.3 km) Approx. 130 km of survey tracks Coalescing reef structures Live reef growth on higher elevation nodes Flat, featureless inter-reefal areas (-3 m LAT) Inter-tidal sand flats (+0.5 m LAT) Shore-attached reef structure Distribution and abundance of coral communities • Up to 95% live coral cover • 21 coral genera – Montipora sp., Acropora sp., Turbinaria sp. & Porites sp. • • Coral growth on ridges, mud/sand inter-reefal areas Heterotrophic coral feeding in all genera Mixed coral framework Foliose Montipora sp. Submassive Pectinia sp. Turbinaria sp. coral carpets Montipora sp. & branching Acropora sp. Large Acropora sp. colony Habitat classification (dendrogram): Delineation of reef habitat zones Habitat distribution (1-6): H1) Sand-dominated with massive Porites sp. bommies H2) Sand & mud substrates H3) Turbinaria sp. coral carpets H4) Mixed Montipora sp. & Acropora sp. coral framework H5) Rubble substrates with Acropora sp. and Montipora sp. H6) Mixed rubble-sand with isolated 'other' coral genera Turbidity-driven shifts in coral assemblages Hard coral cover vs. depth: • Coral growth is depth-dependent • Light penetration controlled by water turbidity and depth • 0 - 4 m below LAT suitable for coral growth • At high tide (+3.6 m LAT) corals rely on heterotrophy for energy requirements • Shifts in coral assemblages across narrow depth range Depth-stratification of coral genera: Z1 0 – 2 m– Mixed Montipora sp. and Acropora sp. framework Z2 2 – 4 m– Turbinaria sp. ‘coral carpets’ and Porites sp. bommies Z3 4 – 6 m– Isolated ‘other’ coral genera (e.g. Lobophyllia sp. & Galaxea sp.) Palaeoecological records: Late-Holocene reef development and coral paleoecology • Reef initiation on Pleistocene clays and clastic marine sands – 921 – 2078 cal y BP • Rapid reef development (1.18 – 3.0 mm/y) under high sedimentation • High coral diversity (59 species identified) • Good preservation of coral clasts Montipora sp. Acropora sp. – Rapid framework infilling Turbinaria sp. • Past coral assemblages had similar depth-distribution as contemporary reefs Euphyllia sp. Inshore reefs of Halifax Bay, GBR • Despite high turbidity, diverse and persistent coral communities • Ironically, coral cover most significant in shelf areas perceived unsuitable for growth • Clear topographic control on coral distribution • Corals inhabiting naturally turbid areas buffered from effects of increased anthropogenic sediment • Implications for inner-shelf areas if similar coral cover is applied – current underestimate of GBR coral cover? • Future work to focus on modelling trajectories and evolution of inshore reefs Central GBR coral cover 2012/2013 (%): Future trajectories of inshore reefs: (NE/J023329/1)