Stable isotopes (delta O-18 and delta C-13), trace and minor element compositions of Recent scleractinians and Last Glacial bivalves at the Santa Maria di Leuca deep-water coral province, Ionian Sea

The aragonitic skeletons of bathyal cold-water corals have a high potential as geochemical in situ archives for paleoceanography. Oxygen isotopes and stable carbon isotopes (δ18O and δ13C) have been analyzed, as well as trace and minor element compositi

Bibliographic Details
Published in:Deep Sea Research Part II: Topical Studies in Oceanography
Main Authors: Correa, Matthias López, Montagna, Paolo, Vendrell-Simon, Begona, McCulloch, Malcolm, Taviani, Marco
Format: Article in Journal/Newspaper
Language:unknown
Published: Pergamon-Elsevier Ltd
Subjects:
Keywords: Adriatic
Biological fractionation
Bottom water
Central Mediterranean
Cold-water corals
Coral growth
Deepwater
Dissolved inorganic carbon
Dissolved inorganic nutrients
Environmental conditions
Environmental parameter
Equilibrium value
Gaussian Cold-water corals
Lophelia pertusa
Stable isotopes
Trace elements
Vital effects
Online Access:http://hdl.handle.net/1885/67924
https://doi.org/10.1016/j.dsr2.2009.08.016
https://openresearch-repository.anu.edu.au/bitstream/1885/67924/5/f2965xPUB1565.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/67924/7/01_Correa_Stable_isotopes_%28delta_O-18_2010.pdf.jpg
Description
Summary:The aragonitic skeletons of bathyal cold-water corals have a high potential as geochemical in situ archives for paleoceanography. Oxygen isotopes and stable carbon isotopes (δ18O and δ13C) have been analyzed, as well as trace and minor element compositi

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