Coral, Ecosystems, and Climate:
Can Ancient Corals Tell the Story?
Department of Geological Sciences
University of Alabama
Coral has long attracted the attention of scientists. It is an interesting organism with an equally interesting ecology. Coral reefs represent some of the most diverse, complex, and fragile ecosystems in the world. Ecological and climatic variables, such as nutrient availability and water temperature, significantly influence coral growth.
Much of the coral research today focuses on understanding how coral grows, how coral interacts with other organisms, and the ways in which human activity affects the health of coral reefs. Another important but lesser-known avenue of investigation is studying the ways in which corals act as “recorders” of the world around them as they grow. The calcium carbonate skeleton that the organism leaves behind contains evidence of these environmental variables that affect the coral's growth. Ancient coral can, therefore, contain information about ancient climate and ecology.
Skeletons leave a record of growth
Corals are actually very small, soft-bodied organisms that secrete the hard skeletons we see. As corals grow, they leave behind their old skeleton and grow a new skeleton on top of it. The old skeleton is preserved underneath the living coral, leaving a record of growth. Shallow-water corals often create vast reefs as they grow, with the help of symbiotic algae and tropical sunlight. Deep-water corals produce much less skeleton and survive in the cold, dark water by feeding on passing nutrients.
Corals that grow on reefs in shallow tropical water are relatively easy to visit and study, but deep-water corals are far more difficult to observe. Even simple measurements like growth rate are comparatively hard to make.
Growth rate is a critical variable in our understanding of coral ecology. By measuring growth rate, we can unlock what coral can teach us about past climates. (Also, deep-water corals are now being impacted more and more by human activity. It is, therefore, increasingly important that we understand how our actions may affect these organisms.) Since we cannot directly observe deep-water coral growth in their natural habitat for long periods of time, we must use other methods to determine growth rate. One way might be to mark the size of a coral (without damaging it), leave it alone for a period, then return to see how much it has grown.
Fortunately, corals leave behind their own marks as they grow, in much the same way as trees. To make use of these growth marks, or "increments," we must determine what length of time they actually represent. Once we know that, determining growth rate is fairly simple. (Unfortunately, this method is not practical for deep-water corals.)
Unlocking a chemical portrait
One method we use to determine incremental growth rate is the analysis of chemicals locked in the coral skeletons. Some aspects of coral chemistry are controlled by variables like water temperature. In some deep-water environments, such as the Charleston Bump, temperature varies over time throughout the year. Therefore, the chemistry of the skeleton may record the time of the year and permit us to measure how fast these corals grow.
We have observed many different coral growth patterns on the Blake Plateau. Hard surfaces are often covered, to one degree or another, with small “twigs” of coral, each only a few centimeters high. Some areas have many of these corals packed tightly together, while other areas have only a few widely scattered corals. In a few areas, large tangles of corals that resemble bushes cover the bottom. Other areas have no corals at all.
None of these patterns are likely to be random, and by simply knowing how fast these corals grow, we may be able to determine the most important factors that control the formation these different growth habits.
The uncertain future
An unfortunate variable that impacts deep-water coral growth habits in other parts of the world -- but not the Blake Plateau -- is the use of fishing methods that destroy large areas of coral as dredges and other equipment are dragged across the bottom. How fast can coral recover from these disturbances? When will the ecosystems within which the corals live return to these areas after they are destroyed? Simple age measurements are critical to answering these questions and understanding these processes.
Some areas we have visited on other expeditions contained the skeletons of corals that appeared to have died some time ago. By studying the chemical records in these older corals, we hope to unlock clues about the ecosystems and climates of the times in which these corals lived. These long-dead corals may give insight into how the local and global climate has varied over time. Much of what is known about past climates is derived from records trapped in shallow tropical corals. Deep-water corals may contain a similar record of change.