Late afternoon seasonal transition to dissolution in a coral reef: An early warning of a net dissolving ecosystem?

• Main Authors: Stoltenberg, Laura, Schulz, Kai G, Lantz, Coulson A, Cyronak, Tyler, Eyre, Bradley D
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: NSUWorks 2021
• Subjects: coral reef metabolism; dissolution; community calcification; Great Barrier Reef; calcium carbonate; ocean acidification; Marine Biology; Oceanography and Atmospheric Sciences and Meteorology; Austral; Ocean acidification
• Online Access: https://nsuworks.nova.edu/occ_facarticles/1137; https://nsuworks.nova.edu/cgi/viewcontent.cgi?article=2151&context=occ_facarticles

There are concerns that reefs will transition from net calcifying to net dissolving in the near future due to decreasing calcification and increasing dissolution rates. Here we present in situ rates of net ecosystem calcification (NEC) and net ecosystem production (NEP) on a coral reef flat using a slack-water approach. Up until dusk, the reef was net calcifying in most months but shifted to net dissolution in austral summer, coinciding with high respiration rates and a lower aragonite saturation state (Ωarag). The estimated sediment contribution to NEC ranged from 8 – 21 % during the day and 45 – 78 % at night, indicating that high rates of sediment dissolution may cause the transition to reef dissolution. This late afternoon seasonal transition to negative NEC may be an early warning sign of the reef shifting to a net dissolving state and may be occurring on other reefs.