Dataset: Zill et al 2017 Coral Growth

In June-August 2012, we conducted a 54-day field experiment on the north shore of Moorea, French Polynesia. We manipulated the presence of the vermetid Ceraesignum maximum (formerly Dendropoma maximum) and high sedimentation, yielding four fully-crossed treatments. In response to which, we measured the growth of the reef-building coral massive Porites (a species complex mostly composed of P. lobata and P. lutea, see Veron 1995).

This study was performed in a shallow lagoonal backreef area, where vermetid densities can be quite high (up to >100 per m2: Smalley 1984; Shima et al. 2010). We selected 36 large (approximately 1 meter in diameter), mostly-dead colonies of massive Porites to serve as deployment sites for our experimental corals. These colonies occurred at a similar depth along a 150-m transect that was roughly parallel to the reef crest and perpendicular to prevailing water currents. Because differences in water flow could affect vermetid net casting efficacy and sediment removal rates, we quantified relative flow variation among sites using calibrated clod cards (Jokiel & Morrissey 1993). The flat top of each site was home to an average of 5 ± 1 (SD) vermetids in a 400 square centimeter area, ensuring that mucus nets would consistently cover the experimental corals receiving the “+vermetid” treatments. We randomly assigned the four experimental treatments to our sites, from half of which we removed all vermetids to create the “–vermetid” treatments. Our experimental corals were 36 juvenile massive Porites colonies that we collected from a nearby location. Each coral was attached to a small plastic base using marine epoxy, and buoyantly weighed (following Davies 1989). They were then assigned to nine blocks of four corals based on similarity in morphology, and outplanted to each deployment site using u-nails.

After 54 days, corals were retrieved, sediments were removed, the corals’ final buoyant mass (Davies 1989) and surface area (using the aluminum foil method of Marsh 1970) were quantified to calculate the per-tissue-area change in coral mass.