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- W1574354408 abstract "Living cold-water coral reefs occur over a wide bathymetric and hydrographical range. We found that cold-water coral reefs are limited to different intermediate water masses. Measurements of the physical and geological properties showed that parameters such as temperature, salinity, dissolved oxygen content, current intensities, and different substrates vary widely without specifically impacting the distribution of living cold-water coral reefs. The habitat of living reefs along the Atlantic European continental margin comprises a temperature-salinity field, with its lower boundary equivalent to the Intermediate Salinity Maximum (ISM). Therefore, cold-water corals of these reefs may report environmental changes, present and past, if the proper geochemical tools are applied. Sr-isotopes seem to be a very promising proxy, since they portray very well the temperature conditions of the ambient seawater from which the coral precipitates. The correlation of established proxies such as 18 O and 13 C with temperature is possible as well, however, it remains difficult since there is no direct temperature equation applicable as in shallow-water corals. Other temperature proxies such as Sr/Ca, Mg/Ca and U/Ca are in?uenced by the complex microstructure of the aragonite skeleton, the rate of calci?cation, and other vital effects observed for coral species. We will present a variety of established and new proxies and will discuss their application and interpretation potential." @default.
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- W1574354408 date "2009-04-01" @default.
- W1574354408 modified "2023-09-28" @default.
- W1574354408 title "European Cold-Water Corals: Hydrography and Geochemistry. What is the message?" @default.
- W1574354408 hasPublicationYear "2009" @default.
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