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Heat Transfer in Corals and Implications for Coral Bleaching

Isabel Jimenez-Denness

Current Appointment: PhD Candidate

Contact:
Institute for Water and Environmental Resource Management
Department of Environmental Sciences
Aquatic Photosynthesis Group
University of Technology, Sydney
PO Box 123
Broadway NSW 2007
Australia
Office: Building 4, Level 5, Room 66 (City Campus)
Phone: 9514 8345
Fax: 9514 4079
Email: Isabel.Jimenez@student.uts.edu.au



Project Outline

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This project investigates the thermal processes that govern a coral’s heat budget and how this affects its temperature. This will allow a better understanding of the transfer of heat between a coral and its surroundings and predict physical conditions responsible for coral bleaching.

During a bleaching event, corals lose their symbiotic dinoflagellate algae, known as zooxanthellae. This makes the underlying calcium carbonate skeleton visible below the living tissue and results in the vivid white colour of bleached corals. More often than not it also leads to the death of the coral host, which relies on the symbiotic micro-algae for survival. Abnormally high sea surface temperatures (1-2 ºC above mean seasonal maximum, associated with global climate change) and intense light have been identified as major factors causing widespread and devastating bleaching events, which are becoming increasingly frequent around the world.


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On large geographical scales it is possible to detect abnormally high sea surface temperatures and thus identify bleaching “hot spots”, or regions of the world’s tropical oceans that are at risk. However at the scale of a coral reef it is much more difficult to predict the onset or even the severity of a bleaching event. Individual coral colonies don’t bleach at the same time or with the same intensity. To address this still poorly understood aspect of bleaching, this project focuses on the temperature of the calcium carbonate skeleton, at the scale of individual colonies, and investigates the response to environmental factors such as surrounding water temperature, flow, and solar radiation.






Supervisors

Associate Professor Peter Ralph

Professor Greg Skilbeck