The northern Patagonian fjords lie on the interface between the high Andes Mountains in the east and the South Pacific Ocean, formed thousands of years ago through erosive glacial activity and tectonic sinking. Around 12,000 years ago the icefields in the Chiloé Interior Sea began to open, leaving behind over 15,000km2 of fjords, channels and gulfs. The waters within the fjords are influenced by strong tides, large volumes of freshwater runoff, and upwelling of deep-ocean waters as well as steep climatic gradients from north to south. This dynamic environment has resulted in extremely high biodiversity and endemism, yet this region is one of the least studied areas of the world. It was just a few years ago that deep-sea corals were found inhabiting this region at unusually shallow depths (less than 10m) and in extremely high densities (greater than 1500 individuals per m2). One species in particular, Desmophyllum dianthus, is one of the most widespread hard corals in deep-sea habitats around the globe, yet there have been no ecological studies because of the difficulty in sampling at depths below traditional SCUBA. Cold-water corals are important structural engineers, creating habitat for thousands of associated invertebrates and fish, forming the principle foundation of many benthic ecosystems. These shallow fjord communities present a unique opportunity to form baseline data on ecological and population processes, acting as an accessible window into a deep-sea ecosystem. In recent years environmental and anthropogenic pressures in the northern Patagonian fjord region have mounted (particular from intense salmon farming) leading to a situation where these unique ecosystems may be lost before they can be documented and fully understood. Reproduction is a foundation ecological process for which every species on the planet needs to undergo to survive through time, and is essential information to understanding recruitment, recolonization, population connectivity and recovery from damage. In light of the urgency in gaining basic scientific information to aid in the conservation and preservation of these ecosystems, this project provided support for two field expeditions and continuous monitoring of three sites within this sensitive region. This area was used as a living laboratory, giving us a window into a deep-sea ecosystem. Though the analysis phase of this project is just beginning, the field expeditions and collections were a huge success. Through this joint National Science Foundation and National Geographic Society project, three areas within the Comau and Renhihue fjord systems were monitored over the course of a year (2012 - 2013). In 2012 we set up monitoring sites in three locations - Pt Huinay (impacted by salmon farming), Lilihuape (unimpacted) and Pt Mammuro (Renihue fjord, unimpacted). At each site long-term loggers were deployed to measure temperature, salinity and light, and 10-15 corals were collected and preserved for reproductive analysis. Extensive exploration was also completed in the region to locate new coral populations, and in turn discovered many impacted and areas of dead corals, most likely from widespread anoxic events and over sedimentation from salmon farming. Every three months thereafter collaborators in Chile collected additional coral samples, and in 2013 we collected the loggers, took additional samples and continued examining other areas within the fjords for coral diversity. The samples from this project will be used to analyze how, when and how much these corals reproduce, under what conditions do these corals reproduce and whether there are fundamental reproductive differences between impacted and unimpacted sites. These data are essential for the effective managment of coral populations around the globe. At present a masters level graduate student is just beginning to work up samples collected and shipped back to the University of Maine. Last Modified: 05/14/2014 ...
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