New insights on Antarctic gorgonians' age, growth and their potential as paleorecords

11 pages, 6 figures, 4 tables, supplementary material https://dx.doi.org/10.1016/j.dsr.2016.03.007 Antarctic benthic communities have long been regarded as relicts of the past, since they have developed in a very stable environment and are formed by slow-growing and extraordinary long-lived organism...

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Bibliographic Details
Published in:Deep Sea Research Part I: Oceanographic Research Papers
Main Authors: Martínez-Dios, Ariadna, Dominguez-Carrió, Carlos, Zapata, Rebeca, Gili, Josep Maria
Format: Article in Journal/Newspaper
Language:unknown
Published: Pergamon Press 2016
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Online Access:http://hdl.handle.net/10261/133353
https://doi.org/10.1016/j.dsr.2016.03.007
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Summary:11 pages, 6 figures, 4 tables, supplementary material https://dx.doi.org/10.1016/j.dsr.2016.03.007 Antarctic benthic communities have long been regarded as relicts of the past, since they have developed in a very stable environment and are formed by slow-growing and extraordinary long-lived organisms. However, little is known about the life history traits of gorgonian species, which are considered key components of the Antarctic benthos. In this study, age, Radial Growth Rates (RGR) and skeletal composition of Thouarella variabilis, Fannyella abies and Fannyella rossii colonies (Octocorallia, Primnoidae) that inhabit Antarctic shelf waters were examined. The radioisotopes C and Pb used for dating revealed that these colonies are long-lived, with ages spanning from 50 to 1100 years, thus confirming the archaic character of the Antarctic ecosystem. Some RGR obtained are among the lowest rates ever reported for primnoid species and gorgonians as a whole, with Thouarella species showing rates of 5.08 μm yr. Growth ring deposition seemed to occur every 2-3 years on average, although this result cannot be confirmed. Irregularities in the growth rings could be observed under the Scanning Electron Microscope (SEM) as fluctuations in the skeletal composition, which may be indicative of changes in the environmental conditions, most possibly primary production This research was funded by ECOWED Project (CTM2012-39350-C02-01) Peer Reviewed