Growth rates of Porites astreoides and Orbicella franksi in mesophotic habitats surrounding St. Thomas Sarah H. Groves1,5,*, Daniel M. Holstein2, Ian C. Enochs3,4, Graham Kolodzeij3, Derek P. Manzello3, Marilyn E. Brandt5, Tyler B. Smith5 1. National Centers for Coastal Ocean Science Marine Spatial Ecology Division, National Oceanic and Atmospheric Administration, 101 Pivers Island Rd., Beaufort, NC 28516, USA 2. Duke University Marine Laboratory, Nicholas School of the Environment, Duke University, 135 Duke Marine Lab Rd., Beaufort, NC 28516 3.Atlantic Oceanographic and Meteorological Laboratories (AOML), NOAA, 4301 Rickenbacker Cswy., Miami, FL 33149, USA 4. Cooperative Institute for Marine and Atmospheric Studies, Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Cswy., Miami, FL 33149, USA 5. Center for Marine and Environmental Studies, University of the Virgin Islands, 2 John Brewer’s Bay, St. Thomas, Virgin Islands 00802, USA *Communicating author:
[email protected] Keywords Mesophotic coral ecosystems, Sclerochronology, Refugia, Shelf edge reefs, Orbicella spp. Abstract Mesophotic coral ecosystems (MCEs) are deep (>30 m), light-dependent communities that are abundant in many parts of the global ocean. MCEs are potentially connected to shallow reefs via larval exchange and may act as refuges for reef organisms. However, MCE coral community recovery after disturbance, and thus, community resilience, are poorly understood components of their capacity as refuges. To assess the potential for disturbance and growth to drive community structure on MCEs with differential biophysical conditions and coral communities, we collected colonies of Orbicella franksi and Porites astreoides and used computerized tomography to quantify calcification. The divergence of coral growth rates in MCEs with different environmental conditions may be species specific; habitat-forming O.